﻿PT	AU	BA	BE	GP	AF	BF	CA	TI	SO	SE	BS	LA	DT	CT	CY	CL	SP	HO	DE	ID	AB	C1	C3	RP	EM	RI	OI	FU	FP	FX	CR	NR	TC	Z9	U1	U2	PU	PI	PA	SN	EI	BN	J9	JI	PD	PY	VL	IS	PN	SU	SI	MA	BP	EP	AR	DI	DL	D2	EA	PG	WC	WE	SC	GA	PM	OA	HC	HP	DA	UT
S	Van Iten, H; Gutierrez-Marco, JC; Muir, LA; Simoes, MG; Leme, JM		Hunter, AW; Alvaro, JJ; Lefebvre, B; VanRoy, P; Zamora, S		Van Iten, Heyo; Carlos Gutierrez-Marco, Juan; Muir, Lucy A.; Simoes, Marcello G.; Leme, Juliana M.			Ordovician conulariids (Scyphozoa) from the Upper Tiouririne Formation (Katian), eastern Anti-Atlas Mountains, southern Morocco	GREAT ORDOVICIAN BIODIVERSIFICATION EVENT: Insights from the Tafilalt Biota, Morocco	Geological Society Special Publication		English	Article; Book Chapter							TREPOSTOMATE BRYOZOANS; LIFE; MICROSTRUCTURE; MODE	Storm-dominated siliciclastic shelf deposits in the upper half of the Upper Tiouririne Formation (Upper Ordovician, upper Berounian-c. Katian 1-2) of southern Morocco contain large specimens of at least two species of Archaeoconularia (A. aff. consobrina and A. cf. imperialis). Pseudoconularia cf. grandissima occurs in basal beds of the formation, but is far less abundant than Archaeoconularia. The large size of the Archaeoconularia (>500 mm long in some cases) suggests gigantism induced by cold, nutrient-rich waters. Specimens preserving the apical end terminate in a schott, indicating that the conulariids were severed near the apex prior to final burial. Many of the Archaeoconularia occur in monospecific aggregations in which the component specimens exhibit preferential alignment, probably owing to entrainment and burial by storm currents or flows. Some Archaeoconularia are encrusted by edrioasteroids and/or craniid brachiopods, which in certain cases are so closely spaced as to interfere with growth. The edrioasteroids and brachiopods were probably epibionts attached to living, erect or semi-erect conulariids that were partially infaunal. More generally, Late Ordovician conulariid assemblages of South Polar Gondwana and adjacent terranes exhibit low generic diversity relative to those of low- to mid-latitude terranes (Baltica and Laurentia), and are dominated numerically by Archaeoconularia.	[Van Iten, Heyo] Hanover Coll, Dept Geol, Hanover, IN 47243 USA; [Van Iten, Heyo] Cincinnati Museum Ctr, Dept Invertebrate Paleontol, 1301 Western Ave, Cincinnati, OH 45203 USA; [Carlos Gutierrez-Marco, Juan] UCM, CSIC, Inst Geociencias, Jose Antonio Novais 12, Madrid 28040, Spain; [Carlos Gutierrez-Marco, Juan] Fac Ciencias Geol, Dept Geodinam Estratig & Paleontol, Jose Antonio Novais 12, Madrid 28040, Spain; [Muir, Lucy A.] Amgueddfa Cymru Natl Museum Wales, Dept Nat Sci, Cathays Pk, Cardiff CF10 3NP, Wales; [Simoes, Marcello G.] Sao Paulo State Univ, Dept Zool, BR-18618000 Botucatu, SP, Brazil; [Leme, Juliana M.] Univ Sao Paulo, Geosci Inst, R Lago 562, BR-05508080 Sao Paulo, Brazil	Complutense University of Madrid; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC-UCM - Instituto de Geociencias (IGEO); Universidade Estadual Paulista; Universidade de Sao Paulo	Van Iten, H (autor correspondente), Hanover Coll, Dept Geol, Hanover, IN 47243 USA.; Van Iten, H (autor correspondente), Cincinnati Museum Ctr, Dept Invertebrate Paleontol, 1301 Western Ave, Cincinnati, OH 45203 USA.	vaniten@hanover.edu	Simoes, Marcello G/C-2373-2012		Hanover College Faculty Development Committee; Spanish Ministry of Science, Innovation and Universities [CGL2017-87631-P]	Hanover College Faculty Development Committee; Spanish Ministry of Science, Innovation and Universities(Spanish Government)	Partial funding of the senior author's travel expenses was granted by the Hanover College Faculty Development Committee. Field work in Morocco (J.C.G.-M.) was supported by the project CGL2017-87631-P of the Spanish Ministry of Science, Innovation and Universities. This paper is a contribution to Project IGCP 653, 'The Onset of the Great Ordovician Biodiversification Event'.	ALVARO J.J., GREAT ORDOVICIAN BIO, V485, DOI [10.1144/SP485.XXX, DOI 10.1144/SP485.XXX]; Barrande J., 1867, SYSTEME SILURIEN CTR, V3; Begg J. 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Soc. Spec. Publ.		2022	485						177	199		10.1144/SP485.5	http://dx.doi.org/10.1144/SP485.5			23	Geology; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Paleontology	BT1OH					2023-06-23	WOS:000799718200009
J	Ruy, ADD; Alves, RMD; Hewer, TLR; Pontes, DD; Teixeira, LSG; Pontes, LAM				Ruy, Alisson Dias da Silva; Alves, Rita Maria de Brito; Hewer, Thiago Lewis Reis; Pontes, Danilo de Aguiar; Teixeira, Leonardo Sena Gomes; Magalhaes Pontes, Luiz Antonio			Catalysts for glycerol hydrogenolysis to 1,3-propanediol: A review of chemical routes and market	CATALYSIS TODAY			English	Review						Glycerol; Hydrogenolysis; 1; 3-propanediol; Catalytic routes; Market	GAS-PHASE DEHYDRATION; SELECTIVE HYDROGENOLYSIS; CRUDE GLYCEROL; ACID SITES; WOX; CONVERSION; IR; SUPPORT; LIQUID; LEWIS	1,3-propanediol (1,3-PDO) is obtained from renewable and environmentally friendly glycerol. The current industrial production uses high cost genetically modified microorganisms. Researchers have studied heterogeneous catalysts for more efficient processes leading to higher competitiveness in the 1,3-PDO market. In this context, a review of studies involving chemical routes for its production was performed, evaluating process variables and, in particular, the influence of active acid and metallic phases on the activity and selectivity to the desired product. Platinum, iridium, and copper were verified to be the most promising metals. Bronsted sites are responsible for the higher selectivity to 1,3-PDO, while the reaction rate strongly depends on Lewis sites since glycerol adsorption takes place in these sites. Moreover, in order to decrease operating costs, important parameters such as temperature, glycerol concentration in the feed stream and the reactor type must be optimized.	[Ruy, Alisson Dias da Silva; Pontes, Danilo de Aguiar; Teixeira, Leonardo Sena Gomes; Magalhaes Pontes, Luiz Antonio] Univ Fed Bahia, Escola Politecn, Dept Engn Quim, Rua Prof Aristides Novis 2,2nd Floor, BR-40210630 Salvador, BA, Brazil; [Ruy, Alisson Dias da Silva; Alves, Rita Maria de Brito; Hewer, Thiago Lewis Reis] Univ Sao Paulo, Escola Politecn, Dept Engn Quim, Av Prof Luciano Gualberto 380,Tv 3, BR-05508010 Sao Paulo, SP, Brazil	Universidade Federal da Bahia; Universidade de Sao Paulo	Pontes, LAM (autor correspondente), Univ Fed Bahia, Aristides Novis 02,2nd Floor, BR-40210630 Salvador, BA, Brazil.	uolpontes@uol.com.br	Pontes, Luiz/GXN-0596-2022; Alves, Rita M B/B-9853-2014; Teixeira, Leonardo/J-9131-2016	Pontes, Luiz/0000-0003-4158-4033; Alves, Rita M B/0000-0002-1914-5133; Teixeira, Leonardo/0000-0003-0320-8299	RCGI Research Centre for Gas Innovation; FAPESP - the State of Sao Paulo Research Foundation [2014/50279-4]; Shell Brasil; FAPESB - the State of Bahia Research Foundation; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES - Coordination for the Improvement of Higher Education Personnel) [001]	RCGI Research Centre for Gas Innovation; FAPESP - the State of Sao Paulo Research Foundation(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Shell Brasil; FAPESB - the State of Bahia Research Foundation; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES - Coordination for the Improvement of Higher Education Personnel)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors gratefully acknowledge the support of the RCGI Research Centre for Gas Innovation, hosted by the University of Sao Paulo (USP) and sponsored by FAPESP - the State of Sao Paulo Research Foundation (2014/50279-4), and Shell Brasil. The authors also acknowledge FAPESB - the State of Bahia Research Foundation. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES - Coordination for the Improvement of Higher Education Personnel) - Finance Code 001.	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Today	DEC 1	2021	381				SI		243	253		10.1016/j.cattod.2020.06.035	http://dx.doi.org/10.1016/j.cattod.2020.06.035		SEP 2021	11	Chemistry, Applied; Chemistry, Physical; Engineering, Chemical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Engineering	UZ0LQ					2023-06-23	WOS:000701904800008
J	Martins, SEM; Franca, MC; Seddique, AA; Sial, AN; Pessenda, LCR; de Camargo, PB; Valenca, LMM; Santos, LROC; Barcellos, RL				Matos Martins, Silvio Eduardo; Franca, Marlon Carlos; Seddique, Ashraf Ali; Sial, Alcides Nobrega; Pessenda, Luiz Carlos R.; de Camargo, Plinio Barbosa; Mafra Valenca, Lucia Maria; Castro Santos, Larissa Roberta O.; Barcellos, Roberto Lima			Holocene vegetation changes according to sea-level and climate dynamics on tidal flats of the Formoso River estuary, northeastern Brazil	QUATERNARY INTERNATIONAL			English	Article						Holocene; Sea-level fluctuations; Estuary; Isotopes; Palynology; Pernambuco's coast	LATE QUATERNARY VEGETATION; SOUTHEASTERN BRAZIL; LATE PLEISTOCENE; CARBON ISOTOPES; DOCE RIVER; MANGROVE DYNAMICS; ORGANIC-MATTER; ESPIRITO-SANTO; EVOLUTION; CHARCOAL	The aim of this work was to carry out a paleoenvironmental study of Holocene sedimentary deposits in the southern sector of Pernambuco's coast (northeastern Brazil). This work addresses an important aspect of Quaternary research that has implications for current climate debates, for instance, how does vegetation react to changing climate and rising sea levels. Thus, we provide a combined approach using sedimentological, palynological, geochemical analyses (stable isotopes i.e., delta C-13, delta N-15 and C:N), in addition to AMS 14C dating from two surficial sediment cores i.e. T4 (up to 150 cm depth) and T5 (up to 136 cm depth) collected from the Formoso River estuarine system. Climatic oscillations show variation in precipitation and atmosphere humidity, marked by areas of expansion and/or retraction of herbaceous plain and forest vegetation. Variations in vegetation composition over the last 7168-7260 cal yr BP in the Formoso River estuary reflects the strong influence of sealevel variations, which were responsible for changes in coastal paleogeography and paleogeomorphology. Changes in vegetation composition indicate its close relationship with transgressive and regressive marine events and corresponding variation of the depositional environment like lakes to coastal lagoons, tidal channels, sandy strand-plain, and the modern estuary of the Formoso River.	[Matos Martins, Silvio Eduardo] Univ Fed Pernambuco, Grad Program Geosci, Av Prof Moraes Rego 1235 Cidade Univ, Recife, PE, Brazil; [Matos Martins, Silvio Eduardo] Fed Univ West Para, Inst Engn & Geosci, Santarem, Brazil; [Franca, Marlon Carlos] Fed Inst Espirito Santo, Sedimentol & Environm Dynam Grp, R Augusto Costa de Oliveira 660, BR-29285000 Piuma, ES, Brazil; [Seddique, Ashraf Ali] Jatiya Kabi Kazi Nazrul Islam Univ, Dept Environm Sci & Engn, Trishal 2204, Mymensingh, Bangladesh; [Sial, Alcides Nobrega; Mafra Valenca, Lucia Maria] Univ Fed Pernambuco, Dept Geol, NEG LABISE, Recife, PE, Brazil; [Pessenda, Luiz Carlos R.; de Camargo, Plinio Barbosa] Univ Sao Paulo, Ctr Nucl Energy Agr, Piracicaba, Brazil; [Barcellos, Roberto Lima] Univ Fed Pernambuco, Dept Oceanog, Recife, PE, Brazil; [Franca, Marlon Carlos; Castro Santos, Larissa Roberta O.] Fed Univ Para, Grad Program Geol & Geochem, Belem, Para, Brazil	Universidade Federal de Pernambuco; Universidade Federal do Oeste do Para; Instituto Federal do Espirito Santo (IFES); Universidade Federal de Pernambuco; Universidade de Sao Paulo; Universidade Federal de Pernambuco; Universidade Federal do Para	Franca, MC (autor correspondente), Fed Inst Espirito Santo Brazil, R Augusto Costa de Oliveira 660, BR-29285000 Piuma, ES, Brazil.	marlon.franca@ifes.edu.br	de Camargo, Plínio B./D-6635-2012; Seddique, Ashraf Ali/HJH-4956-2023; Sial, Alcides/AAD-1901-2021; Franca, Marlon/C-7896-2013	de Camargo, Plínio B./0000-0002-0696-3778; Ruiz Pessenda, Luiz Carlos/0000-0001-9119-8195; Seddique, Prof. Dr. Ashraf Ali/0000-0001-7430-1226; Franca, Marlon/0000-0002-3784-7702	CNPq [142391/2013-1, 305074/2017-2]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	First of all, we would like to thank the reviewers for their careful reading of our manuscript and their many insightful comments and suggestions. The authors thank the National Council for Scientific and Technological Development (CNPq), Graduate Program in Geosciences of Federal University of Pernambuco (PPGEOC - UFPE), IMAT group of Oceanography department. Stable Isotope Laboratory (LABISE-UFPE), 14C Laboratory of Center for Nuclear Energy in Agriculture (CENA-USP), Laboratory of Oceanography - Federal Institute of Para (IFPA), students from the GSGmar and the support and infrastructure of Laboratory of Geological Oceanography (LABOGEO - UFPE). The first author thanks a fellowship from CNPq (Process 142391/2013-1). The second author would like to thank CNPq for research fellowship (Process 305074/2017-2). This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001>.	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Int.	NOV 20	2021	602				SI		39	48		10.1016/j.quaint.2020.07.032	http://dx.doi.org/10.1016/j.quaint.2020.07.032		AUG 2021	10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	UD7ZB					2023-06-23	WOS:000687421900005
J	Restrepo, M; Bustamante, C; Cardona, A; Beltran-Trivino, A; Bustamante, A; Chavarria, L; Valencia, VA				Restrepo, Marcela; Bustamante, Camilo; Cardona, Agustin; Beltran-Trivino, Alejandro; Bustamante, Andres; Chavarria, Luisa; Valencia, Victor A.			Tectonic implications of the jurassic magmatism and the metamorphic record at the southern Colombian Andes	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Northern andes; Continental arc magmatism; Oblique convergence; Farallon plate; Jurassic metamorphism; Cajamarca complex	TRACE-ELEMENT GEOCHEMISTRY; UPPER MAGDALENA VALLEY; ICP-MS GEOCHRONOLOGY; U-PB GEOCHRONOLOGY; CENTRAL CORDILLERA; EXPERIMENTAL CALIBRATION; EASTERN CORDILLERA; IN-SITU; ZIRCON; ROCKS	The Jurassic magmatism and metamorphism of Colombia result from the convergent relation between the Farall acute accent on plate and the northwestern continental margin of South America. However, the geodynamic process that generated both magmatism and metamorphism is still unclear. Field relations, U-Pb geochronology and trace elements in zircons, whole-rock geochemistry, and mineral chemistry from a series of plutonic and metamorphic rocks found in Narin tilde o and Putumayo regions (southern Colombia) were used to constrain their composition, age, relation, and tectonic setting, as well correlate them with the Jurassic continental magmatic arc of Colombia. The plutonic rocks vary compositionally from diorite to granite. Whole-rock geochemical analyses show relative enrichment of Large Ion Lithophile Elements (LILE) and Light Rare Earth Elements (LREE) compared with High Field Strength Elements (HFSE) and Heavy Rare Earth Elements (LREE), and negative Nb and Ti anomalies, which reveal that the samples were formed in a volcanic arc setting. U-Pb zircon geochronology indicates that the granitoids crystallized during the Late Jurassic (ca. 163-153 Ma). On the other hand, the metamorphic rocks are hornblende-biotite schists that yield a U-Pb age of 160.8 +/- 0.8 Ma, considered the crystallization age of the protolith. Pressure-temperature (P-T) calculations indicate that the schists underwent metamorphism at similar to 700 degrees C and 0.45 GPa. The results obtained enable us to correlate the granitoids with the Jurassic magmatic arc of the Colombian Andes. Furthermore, the hornblende-biotite schist is probably contemporaneous with amphibolites and metapelites reported farther north in the Central Cordillera (Cajamarca Complex), which indicates that they could be part of a regional scale metamorphic belt either exposing different structural levels or recording metamorphic conditions from different positions in an arc-related setting.	[Restrepo, Marcela; Bustamante, Camilo; Beltran-Trivino, Alejandro; Chavarria, Luisa] Univ EAFIT, Dept Ciencias Tierra, Carrera 49 7 Sur 50, Medellin, Colombia; [Cardona, Agustin] Univ Nacl Colombia, Fac Minas, Dept Proc & Energia, Carrera 80 65-223, Medellin, Colombia; [Bustamante, Andres] Univ Fed Pernambuco, Dept Geol, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Valencia, Victor A.] Washington State Univ, Sch Environm, Pullman, WA 99164 USA	Universidad EAFIT; Universidad Nacional de Colombia; Universidade Federal de Pernambuco; Washington State University	Restrepo, M (autor correspondente), Univ EAFIT, Dept Ciencias Tierra, Carrera 49 7 Sur 50, Medellin, Colombia.	marest56@eafit.edu.co	Bustamante, Andres/H-3920-2012; Beltran-Trivino, Alejandro/AAC-3201-2022; Bustamante, Camilo/HPG-2071-2023	Beltran-Trivino, Alejandro/0000-0001-7838-337X; Chavarria Chavarria, Luisa Fernanda/0000-0001-6172-7295; Restrepo, Marcela/0000-0002-0818-4751	Vicerrectoria de Descubrimiento y Creacion (Universidad EAFIT) [851-000016, 828-000061, 881-000071]	Vicerrectoria de Descubrimiento y Creacion (Universidad EAFIT)	This study was funded by the Vicerrectoria de Descubrimiento y Creacion (Universidad EAFIT) and is part of the project "Evolucion del magmatismo de arco Jurasico de la Cordillera Central de Colombia y su relacion con la tectonica Mesozoica de los Andes del Norte" (851-000016, 828-000061 and 881-000071). Authors are grateful to Tomas Roquemen for the acquisition of mineral chemistry data. Comments made by Veronica Oliveros and an Anonymous reviewer helped to improve the quality of this manuscript. This is a contribution to the Semillero de Investigacion en Mineralogia y Petrologia (Universidad EAFIT).	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South Am. Earth Sci.	NOV	2021	111								103439	10.1016/j.jsames.2021.103439	http://dx.doi.org/10.1016/j.jsames.2021.103439		JUL 2021	29	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	UY7BO					2023-06-23	WOS:000701674900002
J	Piauilino, PF; Hauser, N; Dantas, EL				Piauilino, Pedro F.; Hauser, Natalia; Dantas, Elton L.			From passive margin to continental collision: Geochemical and isotopic constraints for E-MORB and OIB-like magmatism during the neoproterozoic evolution of the southeast Brasilia Belt	PRECAMBRIAN RESEARCH			English	Article						E-MORB; OIB; Brasilia Belt; U-Pb; Sm-Nd; Lu-Hf	PLASMA-MASS SPECTROMETRY; ANAPOLIS-ITAUCU COMPLEX; SM-ND DATA; U-PB; LU-HF; CENTRAL BRAZIL; SEDIMENTARY PROVENANCE; CRUSTAL ACCRETION; HAFNIUM ISOTOPE; TRACE-ELEMENT	Metamorphic rocks derived from mafic rocks can be found in metamorphic belts, and their geochemical and isotopic characteristics may be valuable sources of information for interpretation of ancient geologic magmatic scenarios. The southern Brasilia Belt, between the Amazonian and Sao Francisco cratons in Central Brazil exhibits different amphibolite rocks that were emplaced into Verissimo Sequence and Araxa Group metasedimentary sequences, during the Neoproterozoic. The obtained results indicate that the studied amphibolite rocks from Pires do Rio-Catalao area represent three magmatic events associated with three magmatic environments: 1) a passive margin development at 979 Ma, a forearc/back-arc basin at similar to 819 Ma, and a continental collision at similar to 651 Ma. The first magmatic event, related to continental extension and passive margin development is represented by the emplacement at 979 +/- 17 Ma of E-MORB low-K tholeiitic basalts with positive epsilon(Nd(t)) values between +4.4 and 2 and T-DM between 1.26 and 1.82 Ga, related with the Verissimo metavolcanosedimentary Sequence. The zircon populations include a high amount of metamorphic, inherited grains. The second magmatic event, related with an forearc/back-arc extension is represented by E-MORB basalts with negative Nb-Ta anomalies and slightly positive epsilon(Nd(t)) values of +0.78 to +2.71, cogenetic with the Araxa Group. An OIB-like basalt sample is also related to this stage and has a U-Pb age of 819.7 +/- 6.3 Ma. epsilon(Nd(t)) values of +1.82 to +2.57, epsilon(Hf(t)) in zircon around-zero and TDM ages from 1.03 to 1.18 Ga. The third event is represented by syn- to late-tectonic OIB-like basaltic/gabbroic magmatism at 651 +/- 6 Ma, with positive epsilon(Nd(t)) value of +2.57 and younger T-DM age at 1.18 Ga, that can be associated to regional continental collision and closure of the Neoproterozoic ocean. Also, provenance studies into metasedimentary rocks support that passive and active margins could be successively superposed during the main thrusting tectonic event in the Brasiliano orogeny, but slices of different stratigraphic units preserve their depositional isotopic signature. These findings suggest that the occurrence of main mafic magmatic events over a timespan as long as the entire evolution of the Brasilia Belt (1.0-0.6 Ma) might be a key to individualize superposed tectonic basins in Central Brazil.	[Piauilino, Pedro F.; Hauser, Natalia; Dantas, Elton L.] Univ Brasilia, Inst Geosci, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia	Piauilino, PF (autor correspondente), Univ Brasilia, Inst Geosci, BR-70910900 Brasilia, DF, Brazil.	pfpiauilino@gmail.com; nataliah@unb.br; elton@unb.br	Hauser, Natalia/H-2041-2012		Brazilian National Council for Scientific and Technological Development (CNPq) fellowship [45272/2014-6, 308312/2014-7]	Brazilian National Council for Scientific and Technological Development (CNPq) fellowship(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF))	This work was supported by Brazilian National Council for Scientific and Technological Development (CNPq) fellowship (Grants 45272/2014-6 e 308312/2014-7). We thank the Geochronology Laboratory of the University of Brasilia and its staff for all support during analyses, especially Drs. A. R. Fuck, M. M. Pimentel, W. U. Reimond and M. Matteini, for their support and discussion. We also thank P. B. Klein and J. E. G. Campos, and all colleagues from the Undergraduate Pires do Rio Trabalho Final project for allowing access to data and samples.	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JUL 1	2021	359								105345	10.1016/j.precamres.2019.105345	http://dx.doi.org/10.1016/j.precamres.2019.105345		MAY 2021	30	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	SE5IW					2023-06-23	WOS:000652106800001
J	Bertolini, G; Hartley, AJ; Marques, JC; Healy, D; Frantz, JC				Bertolini, G.; Hartley, A. J.; Marques, J. C.; Healy, D.; Frantz, J. C.			The effects of basaltic lava flows on the petrophysical properties and diagenesis of interbedded aeolian sandstones: an example from the Cretaceous Parana Basin, Brazil	PETROLEUM GEOSCIENCE			English	Article							GRANDE-DO-SUL; SOUTHERN BRAZIL; HYDROTHERMAL ACTIVITY; BOTUCATU FORMATION; MAGMATIC PROVINCE; RESERVOIR-QUALITY; FLUID INCLUSION; FLOOD BASALTS; K-FELDSPAR; HUAB BASIN	An analysis of the petrophysical and diagenetic effects of the emplacement of Cretaceous basaltic lava flows (Serra Geral Formation) on aeolian sandstones (Botucatu Formation) has been undertaken on core samples from the Parana Basin, Brazil. Between 0.1 and 1 m from the contact zone, acoustic wave velocities and porosities in sandstones show a significantly wider scatter than those located >1 m away from the lava contact. Higher P-wave values (average 3759.3 m s(-1)) occur between 0.1 and 1 m from the lava contact in contrast to those areas >1 m away (average 3376.8 m s(-1)), whilst the average porosity is 6.5% near the contact (0.1-1 m) and 10.7% away from the contact (>1 m). Petrographical evaluation reveals two diagenetic pathways responsible for modification of the petrophysical properties: early hydrothermal Mg-rich authigenesis (Type 1) and early chemical dissolution (Type 2). Type 3 diagenesis occurs away from the lava-sediment contact (>1 m), with the appearance of poikilitic calcite and smectite. The sandstone samples associated with Type 1 and Type 2 diagenesis display a decrease in porosity and increased acoustic velocities in relation to Type 3, while Type 3 samples show little or no variation in reservoir properties. The lava-induced diagenetic effects at the sandstone-lava contacts (0.1-1 m) may form a baffle or seal to fluids around the margins of the sandstone bodies. Therefore, whilst diagenesis associated with lava emplacement may hinder reservoir quality around the margins, the original reservoir properties are preserved within these large sandstone bodies. Supplementary material: Petrophysical and petrographical data are available at	[Bertolini, G.; Hartley, A. J.; Healy, D.] Univ Aberdeen, Kings Coll, Sch Geosci, Aberdeen AB24 3FX, Scotland; [Bertolini, G.; Marques, J. C.; Frantz, J. C.] Univ Fed Rio Grande do Sul, Inst Geociencias, BR-90040060 Porto Alegre, RS, Brazil	RLUK- Research Libraries UK; University of Aberdeen; Universidade Federal do Rio Grande do Sul	Bertolini, G (autor correspondente), Univ Aberdeen, Kings Coll, Sch Geosci, Aberdeen AB24 3FX, Scotland.; Bertolini, G (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, BR-90040060 Porto Alegre, RS, Brazil.	gabertol@gmail.com	Marques, Juliana C/R-1965-2018; FRANTZ, JOSE C/R-1953-2018	Marques, Juliana C/0000-0003-0143-6925; FRANTZ, JOSE C/0000-0002-8890-7250; Hartley, Adrian/0000-0002-5799-4734; Bertolini, Gabriel/0000-0002-3873-6190				Ahmed W, 2002, B CHEM SOC ETHIOPIA, V16, P37; Alves TM, 2015, INTERPRETATION-J SUB, V3, pA1, DOI 10.1190/INT-2014-0106.1; Angkasa SS, 2017, INTERPRETATION-J SUB, V5, pSK83, DOI 10.1190/INT-2016-0162.1; ANJOS SMC, 2000, AAPG BULL, V84, P19, DOI DOI 10.1306/8626C375-173B-11D7-8645000102C1865D; Araujo LM, 1999, HYDROGEOL J, V7, P317, DOI 10.1007/s100400050205; Baksi AK, 2018, J VOLCANOL GEOTH RES, V355, P66, DOI 10.1016/j.jvolgeores.2017.02.016; Barker CE, 1998, INT J COAL GEOL, V37, P73, DOI 10.1016/S0166-5162(98)00018-4; Beaufort D, 2015, CLAY MINER, V50, P497, DOI 10.1180/claymin.2015.050.4.06; Beckner J.R., 1998, ORIGIN SPATIAL DISTR, V26, P27; Bertolini G, 2020, SEDIMENTOLOGY, V67, P2672, DOI 10.1111/sed.12715; BIRCH F, 1960, J GEOPHYS RES, V65, P1083, DOI 10.1029/JZ065i004p01083; Bjorkum PA, 1996, J SEDIMENT RES, V66, P147; BJORLYKKE K, 1999, GROWTH DISSOLUTION P, P381; Blott SJ, 2001, EARTH SURF PROC LAND, V26, P1237, DOI 10.1002/esp.261; Cardoso OR, 2015, J S AM EARTH SCI, V62, P58, DOI 10.1016/j.jsames.2015.04.004; Davies GR, 1997, B CAN PETROL GEOL, V45, P624; De Ros LF, 1998, SEDIMENT GEOL, V116, P99; De Ros LF, 2012, SPEC PUBL INT ASS SE, P105; DEROS LF, 1994, J SEDIMENT RES A, V64, P778; DICKINSON WW, 1995, J GEOL, V103, P339, DOI 10.1086/629751; Eidel JJ., 1990, INTERIOR CRATONIC BA, V51, P681; Ernesto M, 1999, J GEODYN, V28, P321, DOI 10.1016/S0264-3707(99)00013-7; Fagents S.A., 1999, LUNAR PLANETARY SCI; Folk R. 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J	Mussa, A; Kalkreuth, W; Mizusaki, AMP; Gonzalez, MB; da Silva, TF; Bicca, MM				Mussa, Agostinho; Kalkreuth, Wolfgang; Pimentel Mizusaki, Ana Maria; Gonzalez, Marleny Blanco; da Silva, Tais Freitas; Bicca, Marcos Muller			Evaluation of the hydrocarbon generation potential of the Pimenteiras Formation, Parnaiba Basin (Brazil) based on total organic carbon content and Rock-Eval pyrolysis data	ENERGY EXPLORATION & EXPLOITATION			English	Article						Parnaiba Basin; Pimenteiras Formation; TOC; Rock-Eval pyrolysis; igneous intrusions; hydrocarbon potential	PETROLEUM SYSTEMS	The Parnaiba Basin is a Paleozoic to Mesozoic intraplate volcano-sedimentary basin where the Pimenteiras Formation (Devonian) is the main sequence with potential of hydrocarbon generation, mostly natural gas. The present paper evaluates the potential of hydrocarbon generation of Pimenteiras Formation based on Total Organic Carbon (TOC) and Rock-Eval pyrolysis parameters. In this work, 1077 shale samples of the Pimenteiras Formation distributed in 32 wells were evaluated. The TOC content varies between 0.1 to 4.7 wt.%, partially reflecting the accumulation and preservation rates of the organic matter in marine and coastal depositional environments controlled by regressive-transgressive cycles. The oxic and anoxic conditions vary significantly with deposition in this situation, which were evidenced by HI and OI variations through sample profiles. In the north and center of the basin, the Pimenteiras Formation has a higher potential for hydrocarbon generation relative to the south, probably due to higher anoxic conditions during deposition. The Hydrogen Index indicates the predominance of kerogen types II and III with minor occurrences of types I and IV. The Tmax values indicate general immature conditions and locally postmature, where the lowest temperatures represent the basin ' s burial history, whereas the higher ones were influenced by igneous intrusions and thermogenic anomalies related to the Transbrasiliano Lineament. In addition, the excessive heat around the intrusions altered the Rock-Eval pyrolysis parameters as well as the type of organic matter, resulting in a relative increase of the kerogen types III and IV, which explains the great potential for gas generation in this basin.	[Mussa, Agostinho; Kalkreuth, Wolfgang; Pimentel Mizusaki, Ana Maria; Gonzalez, Marleny Blanco; da Silva, Tais Freitas; Bicca, Marcos Muller] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91509970 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Mussa, A (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91509970 Porto Alegre, RS, Brazil.	agostinhomussa@gmail.com	Silva, Tais Freitas/Q-2914-2018	Silva, Tais Freitas/0000-0003-1541-0902; Mussa, Agostinho/0000-0002-6717-0157	Coordination for the Improvement of Higher Education Personnel (CAPES)	Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: The authors thank the Coordination for the Improvement of Higher Education Personnel (CAPES) for giving the PhD scholarship to the first author.	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J	Benigno, APA; Saraiva, AAF; Sial, AN; Lacerda, LD				Benigno, Ana Paula A.; Saraiva, Antonio A. F.; Sial, Alcides N.; Lacerda, Luiz D.			Mercury chemostratigraphy as a proxy of volcanic-driven environmental changes in the Aptian-Albian transition, Araripe Basin, northeastern Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Mercury; Araripe basin; Stable isotopes; Organic carbon; Biological crisis		The stratigraphy of mercury (Hg) in sections of the Araripe Basin straddling the Aptian-Albian transition, encompassing the Romualdo, Ipubi, Crato and Barbalha (formerly Rio da Batateira)Formations showed positive excursions of Hg concentrations without correlation with organic carbon (C-org) contents. These incursions occurred during the deposition of the Barbalha Formation, which occurred in the Aptian under warm climate and high bio-productivity; in the Crato Formation, in the Albian, and also during the deposition of the Romualdo Formation. The Hg enrichments suggest external sources of Hg to the basin. The positive Hg excursion in the Ipubi Formation, unlike the others, was shown to be correlated with an increase in the deposition of C-org, suggesting internal processes as major river of Hg accumulation in sediments. The positive Hg excursions independent of C-org accumulation are concomitant to periods of intense volcanic activity in the Kerguelen Large Igneous Provinces (LIP). The excursion observed in the Ipubi Formation, however, seems associated with an event of anoxia, resulting in sediments rich in C-org, scavenging Hg from the water column. The Hg chemostratigraphy helps to understand of the paleoenvironmental changes in the Araripe basin, allowing understanding some of the drivers of such changes as the influence of volcanic activity and events of anoxia, as well as major biological crises.	[Benigno, Ana Paula A.; Lacerda, Luiz D.] Univ Fed Ceara, Inst Marine Sci, LABOMAR, BR-60165081 Fortaleza, CE, Brazil; [Benigno, Ana Paula A.] Fed Inst Ceara, IFCE, Campus Umirim, BR-62660000 Umirim, CE, Brazil; [Saraiva, Antonio A. F.] Reg Univ Cariria, Dept Phys & Biol Sci, Crato, CE, Brazil; [Sial, Alcides N.] Univ Fed Pernambuco, Dept Geol, LABISE, NEG, BR-50740530 Recife, PE, Brazil	Universidade Federal do Ceara; Instituto Federal do Ceara (IFCE); Universidade Federal de Pernambuco	Lacerda, LD (autor correspondente), Univ Fed Ceara, Inst Marine Sci, LABOMAR, BR-60165081 Fortaleza, CE, Brazil.	lldrude@pq.cnpq.br	Saraiva, António/HPD-3031-2023; Sial, Alcides/AAD-1901-2021		Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) [No.INT0159-00009.01.00/19]; Brazilian Council for Scientific and Technological Development (CNPq) [405.244/2018-5]	Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); Brazilian Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was funded by the Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP), Proc. No.INT0159-00009.01.00/19 and grants to L.D. Lacerda from the Brazilian Council for Scientific and Technological Development (CNPq), Proc. No.405.244/2018-5.	Aguiar JE., 2007, GEOCHIM BRAS, V21, P304; Assine M. 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J	Bustamante, A; Bustamante, C; Cardona, A; Juliani, C; da Silva, SP				Bustamante, Andres; Bustamante, Camilo; Cardona, Agustin; Juliani, Caetano; da Silva, Salviano Pereira			Jambalo blueschist and greenschist protoliths in the Central Cordillera of the Colombian Andes and their tectonic implications for Late Cretaceous Caribbean-South American interactions	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						High-pressure metamorphism; Northern Andes; Caribbean tectonics; Jambalo blueschists	RASPAS METAMORPHIC COMPLEX; GEOLOGICAL HISTORY; SUBDUCTION ZONES; GEOCHEMICAL DATA; ARC; ROCKS; GEOCHRONOLOGY; CONSTRAINTS; COLLISION; TERRANE	Whole-rock geochemistry and Nd isotopes were used to constrain the nature of the protoliths and provide clues on the metamorphic conditions of the Jambal?o blueschists in the Central Cordillera (Colombian Andes). Blueschist-facies rocks and related greenschists belong to a Cretaceous?Paleocene subduction complex. The blueschist occurs as a lens surrounded by greenschist-facies rocks, suggesting that the latter resembles retrograde products of high-pressure rocks. The geochemical composition of blueschists and greenschists indicates similar protoliths, implying that the Jambal?o rocks were probably part of a unique and coherent block exposed to different degrees of retrograde metamorphism. Th/La ratios above 0.19 and 143Nd/144Nd compositions of 0.51272 and 0.51259 indicate subduction zone sedimentary input or some crustal contamination, interpreted as the interaction of arc-derived sediments with basalts formed in a supra-subduction zone. The Jambal?o schists may represent the youngest exposure of high-pressure metamorphic rocks along the Andes and records of Late Cretaceous Caribbean and South American convergence.	[Bustamante, Andres; da Silva, Salviano Pereira] Univ Fed Pernambuco, Dept Geol, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Bustamante, Camilo] Univ EAFIT, Dept Ciencias Tierra, Carrera 49 7 Sur 50, Medellin, Colombia; [Cardona, Agustin] Univ Nacl Colombia, Dept Proc & Energia, Carrera 80 65-223, Medellin 65223, Colombia; [Juliani, Caetano] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil	Universidade Federal de Pernambuco; Universidad EAFIT; Universidad Nacional de Colombia; Universidade de Sao Paulo	Bustamante, A (autor correspondente), Univ Fed Pernambuco, Dept Geol, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil.	andresbl@aim.com	Juliani, Caetano/E-2069-2014; da Silva, Salviano/AAI-3447-2021; Bustamante, Andres/H-3920-2012; Bustamante, Camilo/HPG-2071-2023	Juliani, Caetano/0000-0002-0128-993X; da Silva, Salviano/0000-0002-5876-501X; 	Colombian Fundacion para la Promocion de la Investigacion y la Tecnologia [1819]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2004/10203-7, 2009/17380-5]; National Council for Scientific and Technological Development (CNPq) [141946/2005-9]	Colombian Fundacion para la Promocion de la Investigacion y la Tecnologia; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We would like to thank Thais Hyppolito for her major discussions during the development of this project and Antonio Garcia Casco for support on EMPA analyses. Ralf Halama, Samuele Papeschi and an anonymous reviewer are acknowledged by their important comments and improvements. The authors also thanks to the Colombian Fundacion para la Promocion de la Investigacion y la Tecnologia (grant 1819) and, from Brazil, the Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP, grants 2004/10203-7 and 2009/17380-5), and the National Council for Scientific and Technological Development (CNPq, grant 141946/2005-9) for their financial support.	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South Am. Earth Sci.	APR	2021	107								102977	10.1016/j.jsames.2020.102977	http://dx.doi.org/10.1016/j.jsames.2020.102977		APR 2021	12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	RJ5QX					2023-06-23	WOS:000637657700003
J	da Silva, MF; Dantas, EL; Vidotti, RM				da Silva, Marcelo Ferreira; Dantas, Elton Luiz; Vidotti, Roberta Mary			Shortening history of the Neoproterozoic oroclinal bending in Paraguay belt, Central Brazil, based on structural interpretation of field work and high resolution aerogeophysical data	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Shortening and folds; Oroclinal bending; Neoproterozoic Paraguay Belt		Different phases of the orogen?s evolutionary history can be geometrically restored by identifying associated tectonic features in the thrust-and-fold belts in the foreland basin. The geometry and fold styles allow understanding the rate of crustal shortening of the Paraguay Belt Neoproterozoic oroclinal. We suggest that high resolution airborne geophysical data provides critical information to understand the tectonic history of Brasiliano fold belts. Geophysical studies integrated to structural analysis in field mapping may unveil the crustal architecture as well as the sequence of events of rocks exposed in two structural windows of the basement in the region of Planalto da Serra and Nova Xavantina, in the state of Mato Grosso, northern segment of the Paraguay Belt, Central Brazil. The evolutive history of rocks exposed southwards of the Amazonian craton margin represents extensional tectonics followed by the development of a passive margin. It is estimated that the original width of the depositional space was -350 km during the formation of the hyperextended platform and, after the intense shortening during the Brasiliano orogenesis, the oroclinal was restricted to -130 km wide, in the post-deformation phase. Planalto da Serra region is characterized by asymmetrical, harmonic folds with thickened hinge zones. They show variable styles between tight and isoclinal and form pairs of EW and NE anticlines and synclines. In Nova Xavantina structural window, the magnetic lineaments mark important lithospheric discontinuities represented by the Campin?apolis (CAL) and General Carneiro (GCL) lineaments, which seem to be the deep basement faults that controlled the extension and where the rift axial zone developed. The Transbrasiliano Lineament (TBL) is a major shear zone that controls the secondary lineaments propagation, forming a network of folds and drag faults, with lateral escapes and vertical movement. Between the two main lineaments occurred the deposition of sediments and volcanic successions related to Nova Xavantina Metavolcanosedimentary Sequence representing a marginal ocean basin. The transition from EW trending features of the Paraguay Belt to NE trend Araguaia Belt lies within Nova Xavantina region and is marked by the direct influence of TBL. TBL is evident in the magnetic images, forming a mosaic of different crustal blocks and corresponding to various curvilinear shear zones with unidirectional trend N30-45E. It is composed of mega-sigmoids interlaced with mainly dextral kinematics, within shallow and deep levels. During the Neoproterozoic orogeny, a foreland basin system was formed in response to the flexural subsidence due to the tectonic inversion of the basin. Several depocenters were formed and served as accumulation sites for the deposition of sediments of the Alto Paraguay Group (Raizama, Sepotuba and Diamantino formations). Gravimetric data allowed individualization of the foreland basin system, which is characterized by four discrete depozones (back-bulge, forebulge, foredeep and wedge-top), between the Amazonian Craton and the inner structural zone.	[da Silva, Marcelo Ferreira; Dantas, Elton Luiz; Vidotti, Roberta Mary] Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [da Silva, Marcelo Ferreira] CPRM Geol Survey Brazil, Recife, PE, Brazil	Universidade de Brasilia	Vidotti, RM (autor correspondente), Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil.	marcelo.ferreira@cprm.gov.br; elton@unb.br; roberta@unb.br	Vidotti, Roberta M/O-8019-2014	Vidotti, Roberta M/0000-0003-1951-3431; Dantas, Elton Luiz/0000-0002-7954-5059	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [305769/2019-7, 304739/2018-9]; Instituto Nacional de Ciencia e Tectonologia para Estudos Tectonicos (INCT-ET); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brazil [001]; Geological Survey of Brazil, project named Mato Grosso -area I [1072]; Geological Survey of Brazil, project Rondonopolis-Dom Aquino [1111]; Geological Survey of Brazil, project Southeast Mato Grosso [1113]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Instituto Nacional de Ciencia e Tectonologia para Estudos Tectonicos (INCT-ET); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brazil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Geological Survey of Brazil, project named Mato Grosso -area I; Geological Survey of Brazil, project Rondonopolis-Dom Aquino; Geological Survey of Brazil, project Southeast Mato Grosso	This paper is the outcome of the PhD thesis of the first author, at Universidade de Brasilia, Brazil. The authors thank the Universidade de Brasilia geochronology lab staff. We also thank Geological Survey of Brazil (CPRM) for the geological mapping executed and for the geophysical survey made available. M. F. S. acknowledges the colleagues Massimo Matteini, Antonio Frasca, Jonatas Carneiro and Natalia Rossi by comments in the discussion. ELD and RMV acknowledges Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for research fellowships, processes 305769/2019-7 and 304739/2018-9, respectively. We also thank Instituto Nacional de Ciencia e Tectonologia para Estudos Tectonicos (INCT-ET) for financial support. This study was partially financed by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brazil, under Finance Code 001. 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J	Pessano, PC; Ganade, CE; Tupinamba, M; Teixeira, W				Pessano, Pedro C.; Ganade, Carlos E.; Tupinamba, Miguel; Teixeira, Wilson			Updated map of the mafic dike swarms of Brazil based on airborne geophysical data	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Mafic dikes; Dike swarms; LIPs; Airborne geophysical maps; Brazil	LARGE IGNEOUS PROVINCES; SAO FRANCISCO CRATON; U-PB GEOCHRONOLOGY; NORTH CHINA CRATON; DYKE SWARM; BADDELEYITE; MAGMATISM; ATLANTIC; MANTLE; AGE	Identification of mafic dike swarms and LIPs (Large Igneous Provinces) are of vital importance in geologic history because they provide information on geodynamics, mantle geochemistry, and paleomagnetism. These data provide key information for paleogeographic reconstructions with the aid of barcode matches and precise radiometric ages. Considering such issues, the Brazilian Precambrian shield can be used as a case for refining the cartography of the relevant intraplate activity (e.g., dikes, sills, flood basalts) in space and time. This work presents an updated map of Brazilian mafic dike swarms produced from airborne geophysical maps (Series 1000 ? Geological Survey of Brazil). Linear and strong anomalies found on aeromagnetic maps using First Vertical Derivative of the Magnetic Field and Amplitude of the Analytic Signal were mapped on a GIS platform. The obtained data were compared to ternary radiometric maps and geological maps in order to exclude those that do not correspond to mafic dikes. The remaining structures - those believed to represent mafic dikes - were classified based on data compiled from the literature. The updated map exhibits more than 5000 elements, including dikes and magmatic suites, in which about 75% were geologically identified and divided into 60 dike swarms and 10 igneous suites and/or units. The dikes were grouped into sixteen extensional episodes from the Archean to the Cenozoic, although some are related to extension/transtension domains within regional compressive zones akin to orogenic settings. The most frequent records refer to the Proterozoic, representing intraplate episodes, some of them consistent with LIPs. The dataset also includes a large record of the Mesozoic age, which corresponds to major LIP events related to the opening of the Atlantic Ocean and the fragmentation of Gondwana.	[Pessano, Pedro C.] Observ Nacl, Programa Posgrad Geofis, R Gal Jose Cristino 77, BR-20921400 Rio De Janeiro, RJ, Brazil; [Pessano, Pedro C.; Tupinamba, Miguel] Univ Estado Rio de Janeiro, Fac Geol, Rua Sao Francisco Xavier 524, BR-20550900 Rio De Janeiro, RJ, Brazil; [Pessano, Pedro C.; Ganade, Carlos E.] Ctr Desenvolvimento Tecnol CEDES, Serv Geol Brasil SBG CPRM, Av Pasteur 404, BR-22290240 Rio De Janeiro, RJ, Brazil; [Teixeira, Wilson] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil	Universidade do Estado do Rio de Janeiro; Universidade de Sao Paulo	Pessano, PC (autor correspondente), Observ Nacl, Dept Geofis, R Gal Jose Cristino 77, BR-20921400 Rio De Janeiro, RJ, Brazil.	ppessano@gmail.com	TUPINAMBA, MIGUEL/A-4890-2014	TUPINAMBA, MIGUEL/0000-0003-1486-8591; Pessano, Pedro/0000-0001-8211-026X	Geological Survey of Brazil (FACC) [2018/00429-0, 4600598014]; CNPq (National Council for Scientific and Technological Development); Petroleo Brasileiro S.A (Petrobras)	Geological Survey of Brazil (FACC); CNPq (National Council for Scientific and Technological Development)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Petroleo Brasileiro S.A (Petrobras)(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras)	This work is the result of an undergraduate thesis done by the corresponding author in 2019 while he was an intern at the Geological Survey of Brazil under the supervision of Dr. Carlos E. Ganade, and a geology student at Rio de Janeiro State University (UERJ). This paper was only possible due to the infrastructure, and academic support of the above-mentioned institutions.; Pedro Pessano and Carlos E. Ganade acknowledge Petroleo Brasileiro S.A (Petrobras) for supporting their ongoing R&D project in partnership with the Geological Survey of Brazil (FACC grant number 2018/00429-0, cooperation term number 4600598014).; Miguel Tupinamba and Wilson Teixeira acknowledge CNPq (National Council for Scientific and Technological Development) for their research grants.; Also, the authors wish to thank Juliana Fernandes Bonifacio (UERJ/CPRM-RJ) for her assistance with the reconstruction of South America and Africa. Caroline Ribeiro and Alexandre Lago are also thanked for the help in tracing part of the dykes from the magnetic images.	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South Am. Earth Sci.	APR	2021	107								103076	10.1016/j.jsames.2020.103076	http://dx.doi.org/10.1016/j.jsames.2020.103076		APR 2021	16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	RJ5WP					2023-06-23	WOS:000637672900003
J	Taufner, R; Lagoeiro, L; Cavalcante, C; Barbosa, P; Silveira, CS				Taufner, Rhander; Lagoeiro, Leonardo; Cavalcante, Carolina; Barbosa, Paola; Silveira, Camila Santos			Deformation mechanisms accommodating progressive simple shear thrusting of quartzite and metacarbonate in the southwestern Espinhaco Range, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Ara?ua? orogen; Quartz; Calcite; Dissolution-precipitation creep; Dislocation creep; EBSD	DISSOLUTION-PRECIPITATION CREEP; SAO-FRANCISCO CRATON; C-AXIS FABRICS; CALCITE MARBLE; HELVETIC NAPPES; MINAS-GERAIS; EVOLUTION; BELT; ZONE; MICROSTRUCTURES	The accommodation of low-temperature ductile deformation in foreland fold-and-thrust belts is often described in terms of outcrop-based geometric analysis, but microtextural observations are also important, as they relate stress, strain, fluids and temperature and thus the rheology in the peripheral part of the orogen. Such microtextural observations are lacking from the foreland part of the Ara?ua? orogen in Brazil, and are here investigated through EBSD-based textural analysis of quartzites and metacarbonate samples from the southwestern Espinha?o Range. The quartzites overthrust the metacarbonates, and deform solely by the activation of dissolutionprecipitation creep, whereas the metacarbonates show a much greater variety of deformation mechanisms that closely relate to grain-size, composition and strain, in the long (low-angle) and short (steep) limbs of shearrelated folds. The metacarbonates show a centimeter-scale alternation of coarse-grained domains of calcite and quartz, and fine-grained domains of a mix of phases (calcite, dolomite, phyllosilicates, quartz, and apatite). In the strongly sheared long limbs, coarse calcite was deformed by dislocation creep with slip on (c) a c c axis orientation parallel to X. This study demonstrates that the foreland thrust zone of the Ara?ua? orogen underwent consistent W-directed progressive thrusting, and that this deformation produced a wide variety of texture types in the metacarbonates while a simpler structural and textural pattern developed in adjacent quartzitic metasediments.	[Taufner, Rhander; Lagoeiro, Leonardo; Cavalcante, Carolina; Silveira, Camila Santos] Univ Fed Parana, Dept Geol, Ctr Politecn, Ave Cel Francisco Her aclito dos Santos S-n, BR-81531980 Curitiba, Parana, Brazil; [Cavalcante, Carolina] UiT Univ Tromso, Arctic Univ Norway, Dept Geosci, Dramsveien 201, N-9037 Tromso, Norway; [Taufner, Rhander; Barbosa, Paola] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro ICC Ala Cent, BR-70910900 Brasilia, DF, Brazil	Universidade Federal do Parana; UiT The Arctic University of Tromso; Universidade de Brasilia	Taufner, R (autor correspondente), Univ Fed Parana, Dept Geol, Ctr Politecn, Ave Cel Francisco Her aclito dos Santos S-n, BR-81531980 Curitiba, Parana, Brazil.; Taufner, R (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro ICC Ala Cent, BR-70910900 Brasilia, DF, Brazil.	rhander.taufner@aluno.unb.br	Barbosa, Paola/AAK-8478-2021	Barbosa, Paola/0000-0001-7661-455X; TAUFNER, RHANDER/0000-0002-2803-6836; Silveira, Camila/0000-0003-0685-5897	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil [CAPES] [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq] [425412/2018-0, 305232/2018-5, 434202/2018-5]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil [CAPES](Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq](Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The manuscript has been improved by the reviews of Dr. Simone Papa, Dr. Rudiger Kilian and two anonymous reviewers. Special thanks are due to Paulo Roberto Roscoe Papini and Maria Cristina Lamego Papini for their hospitality during our stay at Serra do Cipo, and Lucinha for preparing nice meals for the field lunch. Flavia Afonso is acknowledged for helping to prepare marvelous thin sections. Haakon Fossen and Carlos Alberto Rosiere are thanked for fruitful discussions and critical comments on the manuscript. We appreciate the Channel Software personnel for technical support throughout the EBSD data processing. Rhander Taufner thanks the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil [CAPES], for the granting of the master's scholarship [Finance Code 001]. This study was funded by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq project numbers 425412/2018-0 and 305232/2018-5 to Leonardo Lagoeiro and 434202/2018-5 to Carolina Cavalcante].	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G. F, 1979, PETROGENESIS METAMOR; Wintsch RP, 2005, CAN MINERAL, V43, P327, DOI 10.2113/gscanmin.43.1.327	85	2	2	1	7	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	APR	2021	107								102944	10.1016/j.jsames.2020.102944	http://dx.doi.org/10.1016/j.jsames.2020.102944		APR 2021	18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	RJ5UA		Green Accepted			2023-06-23	WOS:000637666000002
J	Toscani, R; Campos, JEG; Matos, DR; Martins-Ferreira, MAC				Toscani, R.; Campos, J. E. G.; Matos, D. R.; Martins-Ferreira, M. A. C.			Complex depositional environments on a siliciclastic-carbonate platform with shallow-water turbidites: The Natividade Group, central Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Natividade group; Shallow water turbidites; Paleo-mesoproterozoic basins; Mixed platforms	SAO FRANCISCO CRATON; U-PB; WESTERN MARGIN; BRASILIA BELT; PARANOA GROUP; CONSTRAINTS; BASIN; SEDIMENTATION; EXAMPLE; EVENTS	The Natividade Group is a Paleo-Mesoproterozoic metasedimentary sequence outcropping in the external zone of the Northern Brasilia Belt, western margin of the Sa?o Francisco Craton, Brazil. The present study delimited eleven sedimentary rock types grouped into four rock assemblages: i) Sand-Silt-Carbonate; ii) SandConglomerate; iii) Sand, iv) Silt-Clay. A geological map for the region was produced, and six stratigraphic columns were composed. Based on the descriptions of rock types and on lateral variation of rock assemblages, it was possible to establish four depositional environments for the Natividade Group, including mixed platform (siliciclastic-carbonate deposition), internal siliciclastic platform, open-marine siliciclastic platform, and a shallow water turbidite (mass flow slope deposition). The mixed platform was controlled by the basement paleogeography, which allowed the deposition of carbonates in warm, agitated, and clean, shallow water conditions in parallel to deposition in deeper water setting, where thin siliciclastic sediments were deposited. The siliciclastic internal platform consists mostly of quartzite, originating from sandy sediments, probably indicating deposition dominated by bedload currents under shallow water shoreface conditions. The open-marine siliciclastic platform is dominated by fine-grained sediments, indicating deepening water conditions under lower shoreface conditions below the fair-weather wave base. Shallow water turbidite occurs in the southern parts of the study area. The elevated paleorelief in the southeast of the Natividade basin is considered as the provenance area providing suitable slope environments for density flow initiation. The basin was shallower in the southern portion with a predominance of carbonate and gravitational flux deposits and deeper to the north, evidenced by the northward predominance of fine-grained sediments. Finally, the study shows that the Natividade Group was deposited in a basin controlled by thermo-flexural subsidence.	[Toscani, R.] Marinha Brasil, Ctr Hidrog Marinha, Diretoria Hidrog & Navegacao, Rio De Janeiro, RJ, Brazil; [Campos, J. E. G.] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Matos, D. R.] Serv Geol Brasil, Div Geol Econ, Rio De Janeiro, RJ, Brazil; [Martins-Ferreira, M. A. C.] Univ Fed Goias, Setor Conde Arcos, Fac Ciencias & Tecnol, BR-74968755 Aparecida De Goiania, Go, Brazil	Universidade de Brasilia; Universidade Federal de Goias	Toscani, R (autor correspondente), Marinha Brasil, Ctr Hidrog Marinha, Diretoria Hidrog & Navegacao, Rio De Janeiro, RJ, Brazil.	toscanisilveira@gmail.com			Brazilian National Council for Scientific and Technological Development (CNPq)	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We would like to thankt the journal reviewers whose contribution resulted in a significant improvement in the final manuscript. The support of Brazilian National Council for Scientific and Technological Development (CNPq) for funding the fieldwork and the University of Brasilia (Geosciences Institute) for equipments and laboratories.	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South Am. Earth Sci.	APR	2021	107								102939	10.1016/j.jsames.2020.102939	http://dx.doi.org/10.1016/j.jsames.2020.102939		APR 2021	21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	RJ3QO					2023-06-23	WOS:000637512900001
J	Farias, BDM; Schultz, CL; Soares, MB				Macedo Farias, Brodsky Dantas; Schultz, Cesar Leandro; Soares, Marina Bento			Bone microstructure of the pareiasaur Provelosaurus americanus from the Middle Permian of southern Brazil	HISTORICAL BIOLOGY			English	Article						Parareptilia; Pareiasauria; osteohistology; life history; growth record; dermal armor	OSTEOLOGICAL DESCRIPTION; KAROO BASIN; GROWTH; PARAREPTILIA; OSTEODERMS; PHYLOGENY; HISTOLOGY; ANATOMY; HISTORY	Provelosaurus americanus from the Guadalupian of Brazil, is the only species of pareiasaur known from South America and its studies are limited to anatomical descriptions. Here, we examined the microstructure of limb bones, a rib fragment and osteoderms of P. americanus, aiming to answer questions related to its paleobiology. The bone tissues of this specimen comprise poorly vascularised parallel-fibred bone interrupted by growth marks indicating slow, cyclical growth. This is consistent with the pattern found in other pareisaurs from South Africa. However, the space between the LAGs are irregular and there is no clear decreasing in vascularity toward the periphery of the bone, suggesting that it did not reach skeletal maturity. The highest number of LAGs was found in the rib, suggesting that our sample lived a minimum of fifteen years. The osteoderms present a trilaminar structure consisting of a diploe composed of a cancellous core surrounded by two cortical layers. A diploe is absent from the osteoderms of previously studied South African pareiasaurs. The osteogenesis of the osteoderms is intramembraneous, but a metaplastic ossification during the early developmental stage cannot be entirely discarded, due to extensive remodeling in the central core that could have destroyed potential metaplastic tissue.	[Macedo Farias, Brodsky Dantas; Schultz, Cesar Leandro; Soares, Marina Bento] Univ Fed Riogrande Sul, Programa Posgrad Geociencias, Inst Geociencias, Porto Alegre, RS, Brazil; [Schultz, Cesar Leandro; Soares, Marina Bento] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Farias, BDM (autor correspondente), Univ Fed Riogrande Sul, Programa Posgrad Geociencias, Inst Geociencias, Porto Alegre, RS, Brazil.	brodskymacedo@gmail.com	Soares, Marina/AAN-8513-2020	Soares, Marina/0000-0002-8393-2406; Farias, Brodsky/0000-0001-5534-9785				Cerda IA, 2013, GEOBIOS-LYON, V46, P273, DOI 10.1016/j.geobios.2013.01.004; Amprino R., 1947, ARCH BIOL, V58, P315; Andrade RCLP., 2015, CAD CULT CIENCS, V14, P200; ARAUJO DCF, 1986, AN ACAD BRAS CIENC, V58, P387; ARAUJO DCF, 1985, AN ACAD BRAS CIENC, V57, P67; ARAUJO DCF, 1985, AN ACAD BRAS CIENC, V57, P63; ARAUJO DCF, 1986, AN ACAD BRAS CIENC, V58, P379; Araujo DCF., 1987, PAULA COUTIANA, V1, P11; ARAUJO-BARBERENA D C, 1989, Anais da Academia Brasileira de Ciencias, V61, P285; Araujo-Barberena DCF., 1989, ACAD BRASIL CIENCE, V61, P209; Barberena MC., 1998, AN ACAD BRAS CIENC, V70, P125; Barberena MC., 1975, TUCUM, V1, P497; Benton MJ., 2014, PALAEONTOLOGY, V4; Boos ADS, 2015, J S AM EARTH SCI, V63, P375, DOI 10.1016/j.jsames.2015.09.003; Canoville A, 2017, ANAT REC, V300, P1039, DOI 10.1002/ar.23534; Canoville A, 2014, LETHAIA, V47, P266, DOI 10.1111/let.12056; CASTANET J, 1994, GERONTOLOGY, V40, P174, DOI 10.1159/000213586; Castanet J, 1993, BONE, P245; Chinsamy A., 1992, Palaeontologia Africana, V29, P39; Chinsamy A, 1998, CRETACEOUS RES, V19, P225, DOI 10.1006/cres.1997.0102; Chinsamy A., 2005, MICROSTRUCTURE DINOS; Chinsamy-Turan A., 2012, FORERUNNERS MAMMALS; Cisneros Juan Carlos, 2005, Revista Brasileira de Paleontologia, V8, P13; Cisneros JC, 2012, P NATL ACAD SCI USA, V109, P1584, DOI 10.1073/pnas.1115975109; Cisneros JC, 2011, SCIENCE, V331, P1603, DOI 10.1126/science.1200305; Cormack D.H., 1987, HAMS HISTOLOGY; de Buffrenil V, 2011, CR PALEVOL, V10, P427, DOI 10.1016/j.crpv.2011.03.010; de Ricqles A., 1976, Annales Paleont (Vert), V62, P71; de Ricqles A, 1976, MORPHOLOGY BIOL REPT, V3, P123; de Ricqles AJ, 2011, CR PALEVOL, V10, P509, DOI 10.1016/j.crpv.2011.03.013; Francillon-Vieillot H., 1990, SKELETAL BIOMINERALI, V1, P471, DOI DOI 10.1029/SC005P0175; Gordon Jr.M., 1947, NOTAS PRELIMINARES E, V38, p20P; Holz M, 2010, J S AM EARTH SCI, V29, P381, DOI 10.1016/j.jsames.2009.04.004; Horner JR, 1999, PALEOBIOLOGY, V25, P295, DOI 10.1017/S0094837300021308; Houssaye A, 2016, BIOL J LINN SOC, V117, P350, DOI 10.1111/bij.12660; Kriloff A, 2008, J EVOLUTION BIOL, V21, P807, DOI 10.1111/j.1420-9101.2008.01512.x; Lee Michael S.Y., 1997, Modern Geology, V21, P231; Looy CV, 2016, PALAEOGEOGR PALAEOCL, V451, P210, DOI 10.1016/j.palaeo.2016.02.016; Malabarba Maria Claudia, 2003, Revista Brasileira de Paleontologia, V6, P49; Meglhioratti T., 2005, GONDW 12 C, V12, P316; Milani E.J., 2007, B GEOCIENCIAS PETROB, V15, P265, DOI DOI 10.1144/SP294.17; Pacheco CP, 2017, J SYST PALAEONTOL, V15, P241, DOI 10.1080/14772019.2016.1164763; Padian K, 2013, BONE HISTOLOGY OF FOSSIL TETRAPODS: ADVANCING METHODS, ANALYSIS, AND INTERPRETATION, P1; Ponce DA, 2017, ACTA PALAEONTOL POL, V62, P819, DOI 10.4202/app.00381.2017; Ponton F, 2004, ACTA ORNITHOL, V39, P137, DOI 10.3161/068.039.0210; Reid R.E.H., 1996, Brigham Young University Geology Studies, V41, P25; Rey K, 2016, GONDWANA RES, V37, P384, DOI 10.1016/j.gr.2015.09.008; Ricqles AD, 1974, ANN PAL ONTOL, V62, P71; Rohn R., 2007, 1 WORKSH PROBL W GON, P151; Rohn R., 2008, BRAS LIA CPRM, V2; Santos RV, 2006, GONDWANA RES, V9, P456, DOI 10.1016/j.gr.2005.12.001; Sayao JM, 2014, GEOL SOC SPEC PUBL, V217, P335; Scheyer TM, 2009, J EVOLUTION BIOL, V22, P1153, DOI 10.1111/j.1420-9101.2009.01732.x; Scheyer TM, 2004, J VERTEBR PALEONTOL, V24, P874, DOI 10.1671/0272-4634(2004)024[0874:HOAOIF]2.0.CO;2; Scheyer TM, 2011, PALAEONTOLOGY, V54, P1289, DOI 10.1111/j.1475-4983.2011.01098.x; Smith RMH, 2014, PALAEOGEOGR PALAEOCL, V396, P99, DOI 10.1016/j.palaeo.2014.01.002; Spencer PS, 2000, J PALEONTOL, V74, P1191, DOI 10.1666/0022-3360(2000)074<1191:AJEAEG>2.0.CO;2; Strapasson A, 2015, ACTA PALAEONTOL POL, V60, P844, DOI 10.4202/app.00059.2014; Tsuji LA., 2015, J VERT PALEONTOL PRO, V2015, P227; Tsuji LA., 2011, THESIS; Tsuji LA, 2012, J VERTEBR PALEONTOL, V32, P45, DOI 10.1080/02724634.2012.626004; Tsuji LA, 2009, FOSS REC, V12, P71, DOI 10.1002/mmng.200800011; Vickaryous MK, 2008, J MORPHOL, V269, P398, DOI 10.1002/jmor.10575; Waskow K, 2017, CR PALEVOL, V16, P425, DOI 10.1016/j.crpv.2017.01.003; Waskow K, 2014, J VERTEBR PALEONTOL, V34, P852, DOI 10.1080/02724634.2014.840645; Woodward HN, 2011, J HERPETOL, V45, P339	66	2	2	1	5	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0891-2963	1029-2381		HIST BIOL	Hist. Biol.	MAR 4	2021	33	3					328	339		10.1080/08912963.2019.1617288	http://dx.doi.org/10.1080/08912963.2019.1617288			12	Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Paleontology	QI9UW					2023-06-23	WOS:000619336300005
J	Ferreira, L; Marotta, GS; Madden, EH; Horbe, AMC; Santos, RV; Costa, JMN				Ferreira, Lavoisiane; Marotta, Giuliano S.; Madden, Elizabeth H.; Horbe, Adriana M. C.; Santos, Roberto V.; Costa, Jose M. N.			Vertical Displacement Caused by Hydrological Influence in the Amazon Basin	JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH			English	Article						GNSS; hydrologic loading; TWS; vertical displacement	WATER STORAGE; SPATIOTEMPORAL VARIABILITY; CONTINENTAL WATER; RIVER-BASIN; DEFORMATION; EARTH; GRACE; GROUNDWATER; CLIMATE; BRAZIL	Hydrologic loading studies are related to variables such as soil moisture, precipitation, and groundwater. These parameters are associated with water mass movements, which may affect the positioning of the Global Navigation Satellite System (GNSS) stations and the gravitational field in a seasonal mode. This study addresses the relationship between displacement and deformation variations observed in the Amazon Basin and local geological and climatic features. It also aims to understand mechanisms that may influence the water distribution and mass movement during the hydrological cycle. We have correlated the vertical displacement with soil moisture at different depths in the Amazon Basin. Our approach takes into consideration topography, soil type, water storage, hydrologic deformation model used, sediment thickness, and geology. We show that amplitude variation of soil moisture and water storage parameters depends on the region's geological nature, that is, whether it is dominated by sedimentary or igneous/metamorphic rocks. In areas dominated by sedimentary rocks, soil moisture increases with depth, while in regions dominated by igneous and metamorphic rocks, soil moisture decreases with depth. We conclude that geology and topography influence the vertical displacement associated with the hydrologic loading. We further show an East-West gradient in the Amazon Basin, in which the largest amplitudes of vertical displacement occur in the sedimentary basins to the East. A few stations in the sedimentary basins have less vertical displacement than expected. We argue that these areas may be associated with thinner and more compact sedimentary rock, or even with intrusive igneous rocks.	[Ferreira, Lavoisiane; Marotta, Giuliano S.; Madden, Elizabeth H.] Univ Brasilia, Inst Geosci, Seismol Observ, Brasilia, DF, Brazil; [Horbe, Adriana M. C.; Santos, Roberto V.] Univ Brasilia, Inst Geosci, Brasilia, DF, Brazil; [Costa, Jose M. N.] Natl Ctr Nat Disaster Monitoring & Alerts CEMADEN, Sao Jose Dos Campos, SP, Brazil	Universidade de Brasilia; Universidade de Brasilia	Ferreira, L (autor correspondente), Univ Brasilia, Inst Geosci, Seismol Observ, Brasilia, DF, Brazil.	lavoisiane@outlook.com; ahorbe@unb.br; rventura@unb.br; jose.costa@cemaden.gov.br	Santos, Roberto Ventura V/B-8163-2015; Marotta, Giuliano S/K-3036-2015; Horbe, Adriana/AAK-8783-2021	Santos, Roberto Ventura V/0000-0001-6071-8100; Marotta, Giuliano S/0000-0003-1073-0683; Horbe, Adriana/0000-0001-6915-6685; Madden, Elizabeth/0000-0002-6753-6788	Seismological Observatory -UnB; FURNAS; CAPES; Petrobras [2017/00161-5]; INCTET [465613/2014-4]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]; CPRM	Seismological Observatory -UnB; FURNAS; CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Petrobras(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); INCTET; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CPRM	The authors would like to thank the journal editor, Paul Tregoning, to the associate editor, Annette Eicker, and the reviewers, Donald Argus and one anonymous reviewer, for their feedback that greatly improved this manuscript. The authors also thank: the Seismological Observatory -UnB, FURNAS, CAPES, CPRM, Petrobras (2017/00161-5) and INCTET (465613/2014-4) for financial support; UnB for providing the necessary infrastructure for conducting the research; Chanard et al. (2014) for provided the script of hydrologic deformation modeling and Jean-Philippe Avouac for updated version (in http://web.gps.caltech.edu/similar to avouac/software.html).This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001.	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Geophys. Res.-Solid Earth	MAR	2021	126	3							e2020JB020691	10.1029/2020JB020691	http://dx.doi.org/10.1029/2020JB020691			22	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	RK1VR		hybrid			2023-06-23	WOS:000638091600013
J	Quinteiro, RVS; Conceica, RV; Carniel, LC; Leitzke, FP; Cunha, JBM; Souza, MR; Gomes, MEB				Quinteiro, R. V. S.; Conceica, R. V.; Carniel, L. C.; Leitzke, F. P.; Cunha, J. B. M.; Souza, M. R.; Gomes, M. E. B.			The role of celadonite on mantle metasomatism in subduction settings	APPLIED CLAY SCIENCE			English	Article						Celadonite; Mantle metasomatism; Experimental petrology; Altered oceanic crust		Celadonite is the most abundant K-rich hydrated mineral formed during basalt alteration. In convergent margins, celadonite from the altered oceanic crust sinks into the mantle and contributes to the mantle wedge metasomatism, recorded by incompatible element enrichment in lavas and mantle xenoliths samples from these settings. However, experimental data on the role of celadonite in subduction zones as a function of P-T are still scarce. Therefore, celadonite stability under "hot" and "cold" subduction settings is investigated experimentally in this study. Results show an early silica loss, with quartz/coesite replacing celadonite from 400 to 600 degrees C and 2.5-7.7 GPa. At 700 degrees C and 2.5 GPa, celadonite is partially converted to phlogopite-annite, and at 800 degrees C and 4.0 GPa celadonite is absent. At temperatures above 800 degrees C, enstatite and phlogopite are the stable silicate phases from 2.5 to 7.7 GPa. Mossbauer spectroscopy and X-ray diffraction analyses show that the reaction of celadonite to phlogopite-annite is progressive and controlled by the Fe3+ to Fe2+ reduction in the octahedral site. Coupled to this, there is a transition of pyrite to pyrrhotite and the release of reducing fluids enriched in H2S, SiO2, OHand K+ in the mantle wedge. These fluids have the potential to mobilize chalcophile elements (e.g. Cu, Zn) and act as mineralizing agents in shallower and more oxidizing crustal environments. Data in this study demonstrate that celadonite-phlogopite-annite series minerals are stable down to at least 230 km in the mantle, contributing to the sources of mantle metasomatism, arc-related magma genesis and possibly chalcophile mineralization.	[Quinteiro, R. V. S.; Conceica, R. V.; Souza, M. R.; Gomes, M. E. B.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias PPGGEO, BR-91501970 Porto Alegre, RS, Brazil; [Carniel, L. C.; Leitzke, F. P.] Univ Fed Rio Grande do Sul, Inst Geociencias, BR-91501970 Porto Alegre, RS, Brazil; [Cunha, J. B. M.] Univ Fed Rio Grande do Sul, Dept Fis, Inst Fis, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Conceica, RV (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias PPGGEO, BR-91501970 Porto Alegre, RS, Brazil.	rommulo.conceicao@ufrgs.br			PETROBRAS Science and Technology development program [2017/00216-4]	PETROBRAS Science and Technology development program	We acknowledge the technical and scientific staff at the Geosciences Institute, Federal University of Rio Grande do Sul (UFRGS) for assistance. This study has received funding from PETROBRAS Science and Technology development program (2017/00216-4) .	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Clay Sci.	MAR 1	2021	202								105951	10.1016/j.clay.2020.105951	http://dx.doi.org/10.1016/j.clay.2020.105951		FEB 2021	11	Chemistry, Physical; Materials Science, Multidisciplinary; Mineralogy	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Materials Science; Mineralogy	QR1KT					2023-06-23	WOS:000624976300001
J	Teixeira, NA; Campos, LD; de Paula, RR; Lacasse, CM; Ganade, CE; Monteiro, CF; Lopes, LBL; de Oliveira, CG				Teixeira, Noevaldo Araujo; Campos, Leandro Duarte; de Paula, Rodolfo Reis; Lacasse, Christian Michel; Ganade, Carlos Eduardo; Monteiro, Cimara Francisca; Leao Lopes, Leonardo Brenguere; de Oliveira, Claudinei Gouveia			Caraj ' as Mineral Province-Example of metallogeny of a rift above a cratonic lithospheric keel	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						sequence (CPVSS); Metallogenic model; SCLM; High-heat flow rift-basin; Lithospheric keel	U-PB GEOCHRONOLOGY; AMAZONIAN CRATON; HYDROTHERMAL ALTERATION; CU-AU; RE-OS; IRON; BRAZIL; DEPOSIT; GEOCHEMISTRY; EVOLUTION	The Caraj ' as Mineral Province (CMP) is located on the southeastern margin of the Amazonian Craton, in northern Brazil. It is the largest producer of high-grade iron ore and a major world supplier of copper, nickel, manganese and gold. This article presents the CMP as a product of oblique rift evolution (2.76-2.06 Ga) controlled by the Canaa similar to and Cinzento strike slip system. The Caraj ' as rift is hosted in the tonalite-trondhjemite-granodiorite (TTG)greenstone Rio Maria terrains (3.0-2.85 Ga). It overlies a subcratonic lithospheric mantle (SCLM) keel as indicated by seismic tomography and is filled by the Caraj ' as plutonic-volcanic sedimentary sequences (CPVSS) that host the CMP. The rifting stage (Gra similar to o Par ' a Group) began with intense tholeiitic fissure volcanism with basalt and rhyolite flows, coeval intrusions of alkali granites and mafic-ultramafic bodies, BIFs, shales and restricted tuff beds. The Azul and ' Aguas Claras Formations consist mainly of shales and sandstones deposited during the sag stage. The calc-alkaline signature of the Gra similar to o Par ' a metavolcanic rocks was demonstrated to reflect the composition of the melted TTG basement. The high magnesium and platinum-group elements (PGE) contents of Puma and Onca mafic-ultramafic complexes indicate extensive partial fusion, conditions that are indicative of a plume origin. We are proposing that CMP's IOCG deposits were formed from saline carbonate fluids exsolved from deep-seated metasomatic mantellic magmas (MMM), channelled and concentrated along jogs and step-overs in strike-slip fault systems in the Caraj ' as rift. The CMP comprises three main ore-forming stages: (1) a plume stage, ca. 2.76-2.73 Ga, creating supergiant exhalative sedimentary biogenic Fe deposits (Serra Norte, Serra sul and Serra Leste), syngenetic exhalative Cu-Au-Zn (Pojuca deposit), exhalative Mn (Antonio Vicente), Ni-PGE-reef deposits in a magma mixing zone of layered intrusions (e.g. Luanga deposit), and Siqueirinho IOCG deposit; (2) a metasome stage including crustal extension and mantle flash melting (60-100 km depth), ca. 2.68-2.50 Ga, forming the most important IOCG deposits like Salobo, Alema similar to o and Igarape ' Bahia. and (3) a sag stage, ca. 2.68-2.06 Ga, with sedimentary Mn deposited in a redox-controlled stratified oceanic environment. The deposits related to granitic intrusion, ca. 1.88 Ga, with Cu-(Au-Mo-W-Sn) greisen (Breves deposit) and Cu-(Au-Mo-F) veins (Gameleira and Alvo 118 deposits) are associated with the A-type magmatism that affected the entire central Amazonian Craton. These deposits are, in contrast, related to an intracratonic silicic large igneous province (SLIP) and have no relation to the Archean Caraj ' as cratonic lithosphere keel rift evolution. The CMP is directly related to the thinning of the lithosphere above a mantle plume, beneath a sub-continental lithospheric mantle (SCLM) keel.	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South Am. Earth Sci.	JUN	2021	108								103091	10.1016/j.jsames.2020.103091	http://dx.doi.org/10.1016/j.jsames.2020.103091		FEB 2021	16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	SU8YO					2023-06-23	WOS:000663417400003
J	Correia, AT; Moura, A; Triay-Portella, R; Santos, PT; Pinto, E; Almeida, AA; Sial, N; Muniz, AA				Correia, A. T.; Moura, A.; Triay-Portella, R.; Santos, P. T.; Pinto, E.; Almeida, A. A.; Sial, N.; Muniz, A. A.			Population structure of the chub mackerel (Scomber colias) in the NE Atlantic inferred from otolith elemental and isotopic signatures	FISHERIES RESEARCH			English	Article						Pelagic fish; Sagittae; Chemical analysis; Stock delineation	FISH OTOLITHS; TRACE-ELEMENTS; CHEMISTRY; WATERS; ESTUARINE; EXPOSURE; GROWTH; DISCRIMINATION; FINGERPRINTS; VARIABILITY	The Atlantic chub mackerel (Scomber colias) is one of the main small pelagic fish resources in the North-East (NE) Atlantic. At present, for fisheries management purposes, a single stock of this species in the NE Atlantic is considered. Over the last years, fishing pressure has greatly increased in this species, but the information regarding its population structure, necessary in order to maintain a sustainable fishery, is still limited. One hundred and eighty individuals of S. colias were collected off the Portugal mainland (Matosinhos, Sesimbra and Portimao) and in the Atlantic Oceanic Islands (Azores, Madeira and Canaries) from January to March 2018. Following age estimation by counting the annual growth increments, 30 pre-selected individuals of the same age group (2 years old) from each sampling location were used for further otolith chemical analyses. Data were analysed by univariate and multivariate statistics to assess the degree of separation between the individuals of these geographic regions. Overall reclassification accuracy rate, obtained from a quadratic discrimination function analysis, was 80 % suggesting that fish passed through their life enough time in heterogeneous water masses to have a distinct chemical signature. Moreover, fish from the islands were fully discriminated (100 % reclassification rate). Regional differences were driven mainly by Sr:Ca, Na:Ca, Ba:Ca, Mg:Ca, Li:Ca, Mn:Ca, delta C-13 and delta O-18, showing a clear separation of four population-units of S. colias in the NE Atlantic, namely Azores, Madeira, Canaries and Portugal mainland. The hereby results provide support for treatment of these fisheries as different regional management units.	[Correia, A. T.; Moura, A.; Muniz, A. A.] CIMAR, Ctr Interdisciplinar Invest Marinha & Ambiental, Terminal Cruzeiros Porto Leixoes, CIIMAR, Ave Gen Norton Matos S-N, P-4450208 Matosinhos, Portugal; [Correia, A. T.] Univ Fernando Pessoa FCS UFP, Fac Ciencias Saude, Rua Calos Maia 296, P-4200150 Porto, Portugal; [Correia, A. T.] Univ Porto ICBAS UP, Inst Ciencias Biomed Abel, Rua Jorge Viterbo Ferreira 228, P-4050313 Porto, Portugal; [Triay-Portella, R.] Univ Las Palmas Gran Canaria ULPGC, Calle Juan Quesada 30, Las Palmas Gran Canaria 35001, Las Palmas, Spain; [Santos, P. T.; Muniz, A. A.] Univ Porto FCUP, Fac Ciencias, Rua Campo Alegre 1021-1055, P-4169007 Porto, Portugal; [Pinto, E.; Almeida, A. A.] Univ Porto FFUP, Fac Farmacia, Lab Associado Quim Verde LAQV REQUIMT, Rua Jorge Viterbo Ferreira 228, P-4050313 Porto, Portugal; [Sial, N.] Univ Fed Pernambuco UFPE, Dept Geol, Nucleo Estudos Geoquim, BR-50670000 Recife, PE, Brazil; [Sial, N.] Univ Fed Pernambuco UFPE, Dept Geol, Lab Isotopos Estaveis NEG LABISE, BR-50670000 Recife, PE, Brazil	Universidade do Porto; Universidade do Porto; Universidad de Las Palmas de Gran Canaria; Universidade do Porto; Universidade do Porto; Universidade Federal de Pernambuco; Universidade Federal de Pernambuco	Correia, AT (autor correspondente), CIMAR, Ctr Interdisciplinar Invest Marinha & Ambiental, Terminal Cruzeiros Porto Leixoes, CIIMAR, Ave Gen Norton Matos S-N, P-4450208 Matosinhos, Portugal.	atcorreia.ciimar@gmail.com	Pinto, Edgar/F-1921-2015; Santos, Paulo T/B-5742-2009; Triay-Portella, Raül/G-4847-2019; Almeida, Agostinho/D-4925-2013	Pinto, Edgar/0000-0002-8021-4783; Santos, Paulo T/0000-0002-2537-5904; Triay-Portella, Raül/0000-0002-7591-6254; Almeida, Agostinho/0000-0002-1297-3198	FCT - Foundation for Science and Technology [UIDB/04423/2020, UIDP/04423/2020, UIDB/50006/2020]; MARINFO [NORTE01 0145-FEDER-000,035]	FCT - Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); MARINFO	This research was supported by national funds through FCT - Foundation for Science and Technology within the scope of UIDB/04423/2020, UIDP/04423/2020 and UIDB/50006/2020, and by the NORTE01 0145-FEDER-000,035 (MARINFO).	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J	Bantim, RAM; de Andrade, RCLP; Ferreira, JS; Saraiva, AAF; Kellner, AWA; Sayao, JM				Machado Bantim, Renan Alfredo; Lima Pedroso de Andrade, Rafael Cesar; Ferreira, Jennyfer Sobreira; Feitosa Saraiva, Antonio Alamo; Armin Kellner, Alexander Wilhelm; Sayao, Juliana Manso			Osteohistology and growth pattern of a large pterosaur from the Lower Cretaceous Romualdo Formation of the Araripe Basin, Northeastern Brazil	CRETACEOUS RESEARCH			English	Article						Pterosauria; Anhangueridae; Ontogeny; Osteohistology; Araripe Basin; Cretaceous	DETERMINATE GROWTH; BONE-HISTOLOGY; ONTOGENY; PTERODACTYLOIDEA; PALEOHISTOLOGY; ANHANGUERIDAE; AGE	A pteranodontoid pterosaur with anhanguerid affinities (MPSC R 1935) from the Romualdo Formation (Lower Cretaceous, Aptian), is described here and provides one of the few cases where the ontogenetic stage is established by comparison of skeletal fusion and detailed osteohistological analyses. The specimen comes from the Baixa Grande locality (Araripe Municipality - Ceara State) and is one of the few pterosaurs from the Araripe Basin with precise geographic and stratigraphic data. It consists of a left forelimb, comprising an incomplete humerus, metacarpal IV, pteroid and digits I, II, III, IV, including unguals. This specimen has an estimated maximized wingspan between 5.76 m and 5.84 m and a normal wingspan between 5.47 m and 5.54 m, and despite its large dimensions, is considered as an ontogenetically immature individual. Where observable, all bone elements are unfused, such as the extensor tendon process of the first phalanx and the carpal series. The absence of some microstructures such as bone resorption cavities, endosteal lamellae, an external fundamental system (EFS), and growth marks supports this interpretation. Potentially, this individual could have reached a gigantic wingspan, contributing to the hypothesis that such large flying reptiles might have been abundant during the Early Cretaceous of what is now the northeastern portion of Brazil. (C) 2020 Elsevier Ltd. All rights reserved.	[Machado Bantim, Renan Alfredo; Lima Pedroso de Andrade, Rafael Cesar] Univ Fed Pernambuco, Programa Posgrad Geociencias, Ctr Tecnol & Geociencias, Ave Acad Helio Ramos S-N,Cidade Univ, Recife, PE, Brazil; [Machado Bantim, Renan Alfredo; Ferreira, Jennyfer Sobreira; Feitosa Saraiva, Antonio Alamo] Univ Reg Cariri, Lab Paleontol URCA, Rua Carolino Sucupira S-N, BR-63100000 Crato, Ceara, Brazil; [Armin Kellner, Alexander Wilhelm; Sayao, Juliana Manso] Univ Fed Rio de Janeiro, Lab Sistemat & Tafon Vertebrados Fosseis, Dept Geol & Paleontol, Museu Nacl, BR-20940040 Rio De Janeiro, RJ, Brazil; [Sayao, Juliana Manso] Univ Fed Pernambuco, Lab Paleobiol & Microestruturas, Ctr Acad Vitoria, Rua Alto Reservatorio S-N, BR-55608680 Vitoria De Santo Antao, PE, Brazil	Universidade Federal de Pernambuco; Universidade Regional do Cariri; Universidade Federal do Rio de Janeiro; Universidade Federal de Pernambuco	Bantim, RAM (autor correspondente), Univ Fed Pernambuco, Programa Posgrad Geociencias, Ctr Tecnol & Geociencias, Ave Acad Helio Ramos S-N,Cidade Univ, Recife, PE, Brazil.	renanbantimbiologo@gmail.com	Bantim, Renan/J-4076-2014; Saraiva, António/HPD-3031-2023	Sayao, juliana/0000-0002-3619-0323	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico e CNPq [420687/2016-5, 313461/2018-0, 458164/2014-3, 311715/2017-6, 140555/2013-7]; Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico - FUNCAP [BMD-0124-00302.01.01/19]; Fundacao Carlos Chagas Filho de Amparoa Pesquisa do Estado do Rio de Janeiro -FAPERJ [E-26/202.905/2018]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico e CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico - FUNCAP; Fundacao Carlos Chagas Filho de Amparoa Pesquisa do Estado do Rio de Janeiro -FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	The authors thank the late Dr. Placido Cidade Nuvens (1943-2016), former director of the Museu de Paleontologia Placido Cidade Nuvens for access to the specimen MPSC R 1395. We also would like to thank Taissa Rodrigues (UFES), Fabiana Costa Nunes (UFABC), Gustavo Oliveira (UFRPE), and Bruno Vila Nova (FFCL-USP) for valuable discussions. We thank two anonymous reviewers for several suggestions. As this manuscript was shown as a pre-proof version, one of the reviewers and some colleagues pointed out some errors regarding the wingspan estimate of MPSC R 1395, enabling us to make the necessary corrections. We are greatfull to them for having pointed this out and Eduardo Koutsoukos (Editor-in-Chief) for allowing the rectification. This project was partially funded by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico e CNPq with grants to AWAK (#420687/2016-5 and #313461/2018-0), JMS (#458164/2014-3; #311715/2017-6) and RAMB (#140555/2013-7), the Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico - FUNCAP (#BMD-0124-00302.01.01/19 fellowships to RAMB) and the Fundacao Carlos Chagas Filho de Amparoa Pesquisa do Estado do Rio de Janeiro -FAPERJ (#E-26/202.905/2018; to AWAK).	Andrade R. C. L. P., 2015, CAD CULT 101 NCIA, V14, P200, DOI [10.14295/cad.cult.cienc.v14i1.932, DOI 10.14295/CAD.CULT.CIENC.V14I1.932]; [Anonymous], PLOS ONE; Arai M, 2020, CRETACEOUS RES, V116, DOI 10.1016/j.cretres.2020.104610; Assine ML., 2014, B GEOCI PETROBRAS, V22, P3, DOI DOI 10.25249/0375-7536.1992289300; Averianov A.O., 2005, Paleontologicheskii Zhurnal, V4, P91; Bantim RAM, 2014, ZOOTAXA, V3869, P201, DOI 10.11646/zootaxa.3869.3.1; Bennett S. 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Res.	FEB	2021	118								104667	10.1016/j.cretres.2020.104667	http://dx.doi.org/10.1016/j.cretres.2020.104667			14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	PA9GU					2023-06-23	WOS:000595936500006
J	Sekhon, N; Novello, VF; Cruz, FW; Wortham, BE; Ribeiro, TGR; Breecker, DO				Sekhon, Natasha; Novello, Valdir F.; Cruz, Francisco W.; Wortham, Barbara E.; Ribeiro, Tulio G. R.; Breecker, Daniel O.			Diurnal to seasonal ventilation in Brazilian caves	GLOBAL AND PLANETARY CHANGE			English	Article						Cave ventilation; Tropical and subtropical caves; Brazil; Diurnal; Seasonal; Buoyancy	SPELEOTHEM DELTA-O-18 RECORDS; AMERICAN MONSOON SYSTEM; CARBON-DIOXIDE; CALCITE PRECIPITATION; GROUND AIR; VARIABILITY; DRIPWATER; RAINFALL; TEMPERATURE; CALIBRATION	Limited studies, particularly in the low-latitudes, exist that monitor cave ventilation, an important process dictating cave geochemical properties. To investigate cave ventilation, we present multi-year monitoring results, including observations of cave-air CO2, cave-air temperature, and cave-air relative humidity, from three Brazilian caves: Paraiso (4.07 degrees S, 55.45 degrees W), Tamboril (16.19 degrees S, 46.59 degrees W), and Jaragua (21.08 degrees S, 56.58 degrees W). Cave ventilation regimes on numerous temporal scales are established. Highest concentrations of cave-air CO2 are recorded during austral summers from a multi-year monitoring effort at Jaragua Cave. Conversely, lowest cave-air CO2 concentration are recorded during austral winters. The variability in cave-air CO2 is attributed to seasonally varying temperature contrasts between surface- and cave-air, which results in buoyancy-driven cave-air CO2 exchange with surface-air CO2. Speleothem growth as calcite precipitation is expected to be biased towards the austral winter season when cave-air CO2 is lowest. This understanding of cave ventilation affects the geochemical interpretation of speleothems as recorders of past climate change from caves in the low-latitudes. Next, continuous CO2 measurements near the entrance of Tamboril Cave suggest diurnal ventilation attributed to diurnal cave- and surface-air temperature differences. CO2 monitored from the deeper part of Paraiso and Jaragua Cave do not exhibit this diurnal cycle. Further, virtual temperature calculations suggest that buoyancy contrasts between cave- and surface-air drive daily to weekly cave ventilation in all three caves. The established cave ventilation regimes provide an additional framework to interpret speleothem based terrestrial environmental change spanning the low- and mid-latitudes. By investigating spatially disparate caves across Brazil, we find buoyancy driven cave ventilation to be a unifying mechanism. Our results suggest that exchange between cave- and surface-air occurs seasonally in caves across the low- and mid-latitudes. These results suggest buoyancy driven ventilation is important not only at mid-latitudes but also in the tropics where speleothems are typically suited to investigate paleomonsoon variability. Therefore, prior knowledge of cave ventilation in caves that contain speleothems suitable for paleoclimate reconstructions is critical to robustly infer subsequent geochemical trends across different timescales (seasonal - centennial).	[Sekhon, Natasha; Breecker, Daniel O.] Univ Texas Austin, Dept Geol Sci, Jackson Sch Geosci, Austin, TX 78712 USA; [Novello, Valdir F.; Cruz, Francisco W.] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil; [Wortham, Barbara E.] Univ Calif Davis, Dept Earth & Planetary Sci, Davis, CA 95616 USA; [Ribeiro, Tulio G. R.] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Ribeiro, Tulio G. R.] Dossel Ambiental Consultoria & Projetas Ltda, Brasilia, DF, Brazil	University of Texas System; University of Texas Austin; Universidade de Sao Paulo; University of California System; University of California Davis; Universidade de Brasilia	Sekhon, N (autor correspondente), Univ Texas Austin, Dept Geol Sci, Jackson Sch Geosci, Austin, TX 78712 USA.	nsekhon@utexas.edu	Novello, Valdir F./P-5824-2015	Novello, Valdir F./0000-0002-0120-3745; Breecker, Dan/0000-0003-0200-223X	National Science Foundation [AGS 1912100]; Sao Paulo Research Foundation (FAPESP) [2016/15807-5, 2017/50085-3]	National Science Foundation(National Science Foundation (NSF)); Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	Support for this study was provided by the National Science Foundation grant AGS 1912100 awarded to D.O.B. Sao Paulo Research Foundation (FAPESP) grants 2016/15807-5 for V.F.N and 2017/50085-3 for F.W.C. We would like to thank the Instituto Chico Mendes de Concervacao da Biodiversidade (ICMBio) to provide the permission (number 22424-8) for the cave studies in Brazil. We would also like to acknowledge the effort put in by Leda Zogbi to provide the map for Paraiso Cave. The study would not have been possible without Dr. Corinne Wong and graduate student Brittany Ward. Finally, we thank Dr. Jed Kaplan and an anonymous reviewer for their extensive and helpful reviews.	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Planet. Change	FEB	2021	197								103378	10.1016/j.gloplacha.2020.103378	http://dx.doi.org/10.1016/j.gloplacha.2020.103378			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	PY4OV		Bronze			2023-06-23	WOS:000612026100001
J	Souza, VHP; Bezerra, FHR; Vieira, LC; Cazarin, CL; Brod, JA				Souza, Victor H. P.; Bezerra, Francisco H. R.; Vieira, Lucieth C.; Cazarin, Caroline L.; Brod, Jose A.			Hydrothermal silicification confined to stratigraphic layers: Implications for carbonate reservoirs	MARINE AND PETROLEUM GEOLOGY			English	Article						Hydrothermal silicification; Silicified reservoir; Porosity; Permeability; Fluid flow; Brazil	SAO-FRANCISCO CRATON; NORTHERN CAMPOS BASIN; PRECAMBRIAN CARBONATES; ESPINHACO SUPERGROUP; CAVE SYSTEM; TARIM BASIN; KARST; POROSITY; ORIGIN; FLOW	Hydrothermal silicification generates secondary porosity and permeability and could play an important role in carbonate reservoirs. We investigated the Cristal Cave, which is hosted in carbonate units of the Caboclo Formation, Sao Francisco Craton, Brazil, to assess the role of sedimentary facies and stratigraphy in hydrothermal silicification. Our results indicate that in the cave area, the carbonate units are composed of (1) ooidal grainstones, (2) intraclastic grainstones and rudstones, (3) heterolites, (4) marls, (5) stromatolites, (6) oncolithicintraclastic grainstones and rudstones, and (7) hydraulic breccias. QEMSCAN and energy dispersive X-ray spectroscopy (EDS) analyses show that hydrothermal silicification is the most common diagenetic process in these rocks and reveal a mineral paragenesis composed of quartz, chalcedony, K-feldspar, barite, hyalophane (Bafeldspar), talc, and chlorite. The marls (Unit 4) are impermeable rocks that represent a maximum flooding surface and divide the sedimentary succession into a bottom and an upper interval. They behaved as a sealing unit that prevented the upward flow of silica, channeling hydrothermal silicification in the bottom stratigraphic interval. Within the silicified interval, units 1, 2, and 3 show great differences in the degree of silicification since the ooidal grainstones (Unit 1) concentrated the hydrothermal fluids, reaching the highest degree of silicification in the stratigraphic column. We conclude that the stratigraphic framework can control the vertical distribution of hydrothermal fluids and the development of layer-parallel fluid flow conduits. The Cristal cave serves as an analog, which could contribute to the understanding of silicified carbonate reservoirs.	[Souza, Victor H. P.] Petrobras SA, Ave Henrique Valadares 28, BR-20231030 Rio De Janeiro, RJ, Brazil; [Bezerra, Francisco H. R.] Univ Fed Rio Grande do Norte, Dept Geol, Natal, RN, Brazil; [Souza, Victor H. P.; Vieira, Lucieth C.] Univ Brasilia, Inst Geosci, Brasilia, DF, Brazil; [Cazarin, Caroline L.] Petrobras SA, Res & Dev Ctr CENPES, BR-21941915 Rio De Janeiro, RJ, Brazil; [Brod, Jose A.] Fed Univ Goias FCT UFG, Fac Sci & Technol, BR-74968755 Aparecida De Goiania, Go, Brazil	Petrobras; Universidade Federal do Rio Grande do Norte; Universidade de Brasilia; Petrobras	Souza, VHP (autor correspondente), Petrobras SA, Ave Henrique Valadares 28, BR-20231030 Rio De Janeiro, RJ, Brazil.	victor_proenca@petrobras.com.br	Vieira, Lucieth/AAK-9508-2021; Brod, Jose/AAL-2913-2021	Vieira, Lucieth/0000-0003-2900-7452; Brod, Jose/0000-0002-4265-2571	Petrobras/Federal University of Rio Grande do Norte project (3D Digital model of the Cristal cave, Morro do Chapeu, Bahia, CristalDOM); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; University of Brasilia; University of Goias (CRTI - Centro Regional para o Desenvolvimento Tecnologico e Inovacao)	Petrobras/Federal University of Rio Grande do Norte project (3D Digital model of the Cristal cave, Morro do Chapeu, Bahia, CristalDOM); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); University of Brasilia; University of Goias (CRTI - Centro Regional para o Desenvolvimento Tecnologico e Inovacao)	We thank two anonymous reviewers and MPG associate editor Carmine Apollaro for constructive reviews that significantly improved our work. We thank the Brazilian Agency of Oil, Gas, and Biofuels (Agencia Nacional do Petroleo, Gas e Biocombustiveis, ANP). This work was sponsored by a Petrobras/Federal University of Rio Grande do Norte project (3D Digital model of the Cristal cave, Morro do Chapeu, Bahia, CristalDOM) and partially financed by the Coordenac a "This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001". We also thank the University of Brasilia for support to VHPS during his MSc and Mylene Berbert-Born from the Brazilian Geological Survey for the cave maps. The MEV-EDS analyses were performed at the University of Goias (CRTI - Centro Regional para o Desenvolvimento Tecnologico e Inovacao), which provided support for this study.	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Pet. Geol.	FEB	2021	124								104818	10.1016/j.marpetgeo.2020.104818	http://dx.doi.org/10.1016/j.marpetgeo.2020.104818			18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PP2FT					2023-06-23	WOS:000605684000001
J	Dal Olmo-Barbosa, L; Koester, E; Vieira, DT; Porcher, CC; Cedeno, DG				Dal Olmo-Barbosa, L.; Koester, E.; Vieira, D. T.; Porcher, C. C.; Cedeno, D. G.			Crystallization ages of the basic intrusive Ediacaran magmatism in the southeastern Dom Feliciano Belt, southernmost Brazil: Implications in the belt geodynamic evolution	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Geochronology; Zircon U-Pb SHRIMP; LA-ICP-MS; Passo da Fabiana Gabbros; Alto Alegre diorite	PB-HF ISOTOPES; U-PB; CALC-ALKALINE; NEOPROTEROZOIC JUVENILE; TECTONIC EVOLUTION; GABBRO-DIORITE; CRUSTAL; SHRIMP; GEOCHRONOLOGY; COMPLEX	The participation of mantle-derived magmas, especially hydrous basaltic liquids, in the evolution of granitic belts in both orogenic and post-collisional environments is crucial to evaluate both mantle and crustal evolution, as well as the material transference processes between these two reservoirs. Besides, this transition in the geodynamic context creates specific conditions, promoting the generation of voluminous magmatism. The Dom Feliciano Belt is a mobile belt in southernmost Brazil, generated during the Brasiliano-Pan-African Orogeny. It comprises an eastern unit, the Pelotas Terrane, essentially formed by Cryogenian and Ediacaran granitoids, with minor dioritic and gabbroic rocks in the southeast of the area. This paper presents geochronological studies to determine the crystallization ages (zircon U-Pb SHRIMP) of the most representative bodies of two associations of basic rocks, the Passo da Fabiana Gabbros (PFG), and the Alto Alegre Diorite (AAD). Besides, two granites in the PFG region were analyzed (zircon U-Pb LA-ICP-MS) to evaluate its emplacement, when compared to those of the basic magmas. The results show that PFG yield a crystallization age of 591.2 +/- 3.5 Ma (MSWD = 1.3), while the AAD presented a crystallization age of 562 +/- 3.7 Ma (MSWD = 0.73). In the PFG region, a biotite monzogranite, included in the Cerro Grande Suite, yielded an age of 612 +/- 1 Ma (MSWD = 0.00083), and a leucosyenogranite of the Dom Feliciano Suite, showed crystallization age of 588 +/- 2 Ma (MSWD = 0.00037). Considering the tectonic context of the Dom Feliciano Belt, it is necessary to highlight that an important mantle component, responsible for the generation of water-rich high-alumina calc-alkaline basaltic liquids, was involved in the belt late evolution (590-560 Ma). In this period, the belt was already in post-collisional settings, in a geodynamic context where compressive tensions were cessing, followed by an extensional regime. These conditions enabled mantlepartial melting, which was responsible for the basic rocks generation, with deep regional structures controlling its evolution and emplacement.	[Dal Olmo-Barbosa, L.; Vieira, D. T.; Cedeno, D. G.] Univ Fed Rio Grande Sul UFRGS, Inst Geociencias, Programa Posgrad Geociencias, Bento Goncalves Ave 9500, BR-91501970 Porto Alegre, RS, Brazil; [Koester, E.; Porcher, C. C.] Univ Fed Rio Grande Sul UFRGS, Inst Geociencias, Dept Geol, Bento Goncalves Ave 9500, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Dal Olmo-Barbosa, L (autor correspondente), Dept Geol, Av Bento Goncalves 9500,Predio 43126,Sala 208a, BR-91540000 Porto Alegre, RS, Brazil.	dal.barbosa@ufrgs.br	Koester, Edinei/L-3684-2017; Porcher, Carla C/R-1419-2018	Koester, Edinei/0000-0002-4424-4782; Porcher, Carla C/0000-0002-0418-3954; Dal Olmo-Barbosa, Laercio/0000-0002-2732-8634	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [140461/2016-7, 141335/2017-3, 307378/2017-9]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) : PhD Scholarships, process no 140461/2016-7 (Vieira, D.T.) and 141335/2017-3 (Dal OlmoBarbosa, L.) ; research grant no 307378/2017-9 (Koester, E.) .	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South Am. Earth Sci.	JUN	2021	108								103143	10.1016/j.jsames.2020.103143	http://dx.doi.org/10.1016/j.jsames.2020.103143		JAN 2021	16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	SU8ZM					2023-06-23	WOS:000663419900003
J	Famelli, N; Lima, EF; Carmo, ID				Famelli, Natalia; Lima, Evandro F.; Carmo, Isabela de O.			Lithostratigraphy of the Serra Geral Formation in the northern portion of the Parana-Etendeka Igneous Province: A tool for tracking Early Cretaceous paleoenvironmental changes	JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH			English	Article								A detailed lithofacies analysis in Continental Flood Basalt Provinces allows the comprehension of their evolution and paleoenvironmental significance. In the northern portion of the Parana-Etendeka Igneous Province (PEIP), in Brazil (Uberlandia-Araguari area), a volcanological and stratigraphic approach provided evidence that the basaltic volcanic succession is not monotonous, involving different lava flow morphologies and architecture. The volcanic succession reaches a thickness of ca. 300 m and includes four lithofacies associations: pillow lavas, compound pahoehoe, simple pahoehoe, and sediment-matrix basalt breccia. Pillow lavas, simple pahoehoe, and compound pahoehoe characterize the onset of volcanic activity in the area. Sediment-matrix basalt breccia and thick simple pahoehoe lavas occur in upper stratigraphic levels. Some of these thick igneous bodies can represent invasive lavas or shallow intrusions. In the study area, the common presence of volcanic deposits and structures formed in wet conditions is evidenced by the occurrence of pillow lavas, undulatory columns, and interleaved lacustrine and fluvial sedimentary rocks. These deposits reflect different environmental conditions from those previously described as arid in other portions of the PEIP. Low-temperature post-depositional alteration has affected the volcanic and sedimentary rocks of the study area, obliterating many of the primary sedimentary structures. The subaerial and subaqueous lavas are chemically similar, and compatible with high-TiO2 Pitanga magma type. The Uberlandia-Araguari area and the southern part of the PEIP have a similar stratigraphic style both characterized by the dominance of compound pahoehoe lavas at the base and by an intermittent volcanism, which is evidenced by the intercalation of sedimentary deposits with lavas. (c) 2020 Elsevier B.V. All rights reserved. <comment>Superscript/Subscript Available</comment	[Famelli, Natalia; Lima, Evandro F.] Univ Fed Rio Grande Do Sul, Inst Geociencias, Av Bento Goncalves 9500,Predio 43136,Caixa Postal, BR-91501970 Porto Alegre, RS, Brazil; [Famelli, Natalia; Carmo, Isabela de O.] PETEROBRAS, Ctr Pesquisas & Desenvolvimento Leopoldo Amer Mig, Cidade Univ,Av Horacio Macedo 950, BR-21941915 Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio Grande do Sul	Famelli, N (autor correspondente), PETEROBRAS, Ctr Pesquisas & Desenvolvimento Leopoldo Amer Mig, Cidade Univ,Av Horacio Macedo 950, BR-21941915 Rio De Janeiro, RJ, Brazil.	natalia.famelli@petrobras.com.br		Famelli Pereira, Natalia/0009-0002-4180-4032	Petrobras (CENPES RD Projects) [PT166.01.11923, PT-166.01.13484]; CNPq [402400/2016-0]; FAPERGS [19/2551-0001755-3]; Federal University of Rio Grande do Sul	Petrobras (CENPES RD Projects)(Petrobras); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPERGS(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); Federal University of Rio Grande do Sul	This work was supported by Petrobras (CENPES R&D Projects PT166.01.11923 and PT-166.01.13484), CNPq (402400/2016-0), and FAPERGS (19/2551-0001755-3). The Federal University of Rio Grande do Sul is acknowledged for additional support. Natalia Famelli specially acknowledges to G. Marins, J. Millett, M. Hole, J. Weschenfelder, R. Re, H. Seer, L. Moraes, F. Lourenco, J. Neto, B. Carvalho, I. Loutfi, Y. Parizek, L. De Ros, L. Bevilaqua for their support during fieldwork, discussions and/or software support. We thank the grinding plant of the 2 degrees BFv, Arpasa, Ecobrix, Dois Irmaos, BT Construcoes, Sao Lucas quarries and the Ferrovia Centro-Atlantica (FCA -VLI Logistica) for the permission to access the outcrop areas. We thank reviewers JocelyneMcPhie and Dougal Jerram for insightful reviews that considerably improved this manuscript.	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Volcanol. Geotherm. Res.	FEB	2021	410									10.1016/j.jvolgeores.2020.107152	http://dx.doi.org/10.1016/j.jvolgeores.2020.107152		JAN 2021	21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QT0FI					2023-06-23	WOS:000626267800005
J	Cordeiro, RC; Monteiro, FF; Santelli, RE; Moreira, LS; Figueiredo, AG; Bidone, ED; Pereira, RS; Anjos, LC; Meniconi, MFG				Cordeiro, R. C.; Monteiro, F. F.; Santelli, R. E.; Moreira, L. S.; Figueiredo, A. G.; Bidone, E. D.; Pereira, R. S.; Anjos, L. C.; Meniconi, M. F. G.			Environmental and anthropic variabilities at Guanabara Bay (Brazil): A comparative perspective of metal depositions in different time scales during the last 5,500 yrs	CHEMOSPHERE			English	Article						Anthropogenic signals; Metals; Sediments; Guanabara bay; Holocene; Palaeoenvironment	RIO-DE-JANEIRO; HEAVY-METALS; JURUJUBA SOUND; SEA-LEVEL; SEDIMENTS; ESTUARY; CONTAMINATION; MANGROVE; BIOAVAILABILITY; ACCUMULATION	The determination of age-dated metal sediment accumulation rates in a representative South American bay is able to portray the dimension of human impacts during the colonial occupation and industrial periods. Many studies have assessed metal distribution and chronology at Guanabara Bay, in Brazil. However, understanding natural variabilities associated to paleoclimatic changes and comparing these natural variabilities to anthropogenic processes are not well established to date. Accurate geochrono-logical control integrating ages determined by Pb-210 and C-14 chronologies through an exponential spline fit model allowed for a precise definition of changes associated to the holocene marine transgression, as well as the colonial period, leading to intense land use changes, and the industrial period. The reference values of the system were defined based on their concentrations and the accumulation rates of eco-toxicologically important metals. Al, Ba, Fe, Cd, Cu, Cr, Li, Ni, Mn, Pb, Si, Ti, V, and Zn distributions were determined in a Guanabara Bay core (BG-28) by the EPA 3051 method. Elemental distribution profile assessment allowed for the identification of variabilities associated to weathering processes, predomi-nantly of lithogenic origin, mainly for Al, Ba, Fe, Li, Si, and V. Weathering processes occurred simultaneously to land use changes in the drainage basin since the colonial period, at 400 cal yr BP, and during the industrial period, mainly after the 1960s, denoted by Cd, Cr, Cu, Mn, Pb and Zn increases. The highest average metal enrichment values metals associated to industrial processes reached 5.95, with 119.1-fold higher accumulation rates than the background accumulation values observed between 4200 and 500 cal yr BP. (C) 2020 Elsevier Ltd. All rights reserved.	[Cordeiro, R. C.; Monteiro, F. F.; Santelli, R. E.; Moreira, L. S.; Bidone, E. D.; Pereira, R. S.; Anjos, L. C.] Univ Fed Fluminense, Programa Geoquim, Niteroi, RJ, Brazil; [Monteiro, F. F.] Secretaria Meio Ambiente Cidade Rio de Janeiro SM, Rio De Janeiro, RJ, Brazil; [Santelli, R. E.] Univ Fed Rio de Janeiro, Dept Quim Analit, Rio De Janeiro, RJ, Brazil; [Figueiredo, A. G.] Univ Fed Fluminense, Dept Geol & Geofis LAGEMAR, Niteroi, RJ, Brazil; [Pereira, R. S.] Inst Brasileiro Geog & Estat, Coordenacao Recursos Nat & Estudos Ambientais, Rio De Janeiro, Brazil; [Meniconi, M. F. G.] Petr Brasileiro SA PETROBRAS, Res & Dev Ctr CENPES, Rio De Janeiro, Brazil	Universidade Federal Fluminense; Universidade Federal do Rio de Janeiro; Universidade Federal Fluminense; Petrobras	Cordeiro, RC (autor correspondente), Univ Fed Fluminense, Programa Geoquim, Niteroi, RJ, Brazil.	rccordeiro@id.uff.br	Figueiredo, Alberto G./AAL-2141-2021; Moreira, luciane Silva/AAF-9913-2021; Campello Cordeiro, Renato/J-8870-2013	Moreira, luciane Silva/0000-0002-8721-8752; Campello Cordeiro, Renato/0000-0002-6785-601X	PETROBRAS; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES, Brazil); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ, Brazil: Apoio a Grupos Emergentes de Pesquisa do Rio de Janeiro 2010) [E-26/111.625/2011]	PETROBRAS(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES, Brazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ, Brazil: Apoio a Grupos Emergentes de Pesquisa do Rio de Janeiro 2010)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	The authors would like to thank PETROBRAS for funding the Environment Assessment of Guanabara Bay Project coordinated by CENPES. They also thank the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES, Brazil), and Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ, Brazil: Apoio a Grupos Emergentes de Pesquisa do Rio de Janeiro 2010, Process number E-26/111.625/2011) for financial support and fellowships. 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J	Ferreira, VD; Almeida, JS; Lemos, VA; de Oliveira, OMC; Garcia, KS; Teixeira, LSG				Ferreira, Vanessa de Jesus; Almeida, Jorge S.; Lemos, Valfredo A.; de Oliveira, Olivia M. C.; Garcia, Karina S.; Teixeira, Leonardo S. G.			Determination of Cu, Ni, Mn, and Pb in diesel oil samples using reversed-phase vortex-assisted liquid-liquid microextraction associated with energy dispersive X-ray fluorescence spectrometry	TALANTA			English	Article						Reversed-phase vortex-assisted liquid-liquid microextraction; Diesel oil; Energy dispersive X-ray fluorescence spectrometry; Multielement determination	PLASMA-MASS SPECTROMETRY; DRIED-SPOT TECHNIQUE; CHELATING-AGENT; ETHANOL FUEL; PRECONCENTRATION; GASOLINE; COPPER; WATER; ZINC; ZN	A method was developed based on reversed-phase vortex-assisted liquid-liquid microextraction (RP-VALLME) combined with energy dispersive X-ray fluorescence (EDXRF) spectrometry for the determination of Cu, Mn, Ni, and Pb in diesel oil samples. In this procedure, a nitric acid solution was used as the extraction phase to isolate analytes from organic samples. After a centrifugation step, the aqueous phase was added dropwise to a filter paper disc for EDXRF determinations. The following variables were optimized: type of extraction phase solution, concentration of the extraction phase, stirring time, and sample volume. Some instrumental parameters were also evaluated: atmospheric condition, irradiation energy, and irradiation time. Using 100 mu L of a 0.075 mol L-1 nitric acid solution as the extraction phase for a sample volume of 5.0 mL and a stirring time of 45 s, the limits of detection were 14, 8, 10, and 7 mu g L-1 for Cu, Mn, Ni, and Pb, respectively. The enrichment factors obtained were 34 (Cu), 62 (Mn), 59 (Ni), and 64 (Pb). The precisions, expressed as relative standard deviations (RSDs, %), were calculated from ten replications of the experiment under optimized conditions using standard solutions containing 200 mu g L-1 and 400 mu g L-1 of all four analytes and ranged between 2.1 and 6.4%. The results of recovery tests ranged from 87 to 112%. The proposed procedure was efficiently applied to the determination of the four analytes in diesel oil samples. The results were compared with those obtained by inductively coupled plasma optical emission spectrometry (ICP-OES) after sample digestion, and no significant differences were found.	[Ferreira, Vanessa de Jesus; Almeida, Jorge S.; Teixeira, Leonardo S. G.] Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Lemos, Valfredo A.] Univ Estadual Sudoeste Bahia, Lab Quim Analit, Rua Jose Moreira Sobrinho S-n, BR-45206190 Jequie, BA, Brazil; [de Oliveira, Olivia M. C.; Garcia, Karina S.] Univ Fed Bahia, Inst Geociencias, Campus Univ Ondina, BR-40170280 Salvador, BA, Brazil; [Teixeira, Leonardo S. G.] Univ Fed Bahia, INCT, Energia & Ambiente, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Estadual do Sudoeste da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia	Teixeira, LSG (autor correspondente), Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.	lsgt@ufba.br	LEMOS, VALFREDO AZEVEDO/I-7647-2014; de Almeida, Jorge Santos/ABF-4979-2020; de Oliveira, Olivia Maria Cordeiro/AAB-3246-2021; Teixeira, Leonardo S G/J-9131-2016	LEMOS, VALFREDO AZEVEDO/0000-0002-6029-3218; de Almeida, Jorge Santos/0000-0002-9450-1062; Teixeira, Leonardo S G/0000-0003-0320-8299	Fundacao de Amparoa Pesquisa do Estado da Bahia (FAPESB, Brazil); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	Fundacao de Amparoa Pesquisa do Estado da Bahia (FAPESB, Brazil); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors are grateful for the support granted by Fundacao de Amparoa Pesquisa do Estado da Bahia (FAPESB, Brazil) and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil) for providing grants, fellowships and other financial support. This study also was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001.	Almeida JS, 2015, SPECTROCHIM ACTA B, V107, P159, DOI 10.1016/j.sab.2015.03.002; Korn MDA, 2007, TALANTA, V73, P1, DOI 10.1016/j.talanta.2007.03.036; Bahadir Z, 2018, J IRAN CHEM SOC, V15, P1347, DOI 10.1007/s13738-018-1333-z; Cabaleiro N, 2013, ANAL METHODS-UK, V5, P323, DOI 10.1039/c2ay25830g; Daly K, 2018, APPL SPECTROSC, V72, P1661, DOI 10.1177/0003702818787165; de Almeida ON, 2018, SPECTROCHIM ACTA B, V150, P92, DOI 10.1016/j.sab.2018.10.013; Ebrahimzadeh H, 2014, ANAL METHODS-UK, V6, P4617, DOI 10.1039/c4ay00201f; FANG ZL, 1992, J ANAL ATOM SPECTROM, V7, P293, DOI 10.1039/ja9920700293; Teixeira LSG, 2012, ANAL CHIM ACTA, V722, P29, DOI 10.1016/j.aca.2012.02.014; Hashemi P, 2010, TALANTA, V80, P1926, DOI 10.1016/j.talanta.2009.10.051; Hosseini M, 2015, J SEP SCI, V38, P663, DOI 10.1002/jssc.201401172; Kalschne DL, 2020, FOOD ANAL METHOD, V13, P230, DOI 10.1007/s12161-019-01606-4; Kalschne DL, 2020, TALANTA, V208, DOI 10.1016/j.talanta.2019.120409; Kocot K, 2012, SPECTROCHIM ACTA B, V73, P79, DOI 10.1016/j.sab.2012.05.003; Lemos VA, 2015, WATER AIR SOIL POLL, V226, DOI 10.1007/s11270-015-2392-8; Lima LC, 2017, ENERG FUEL, V31, P9491, DOI 10.1021/acs.energyfuels.7b01430; Lobo AMG, 2020, SEP SCI PLUS, V3, P44, DOI 10.1002/sscp.201900088; Lourenco EC, 2019, TALANTA, V199, P1, DOI 10.1016/j.talanta.2019.02.054; Luz MS, 2013, TALANTA, V115, P409, DOI 10.1016/j.talanta.2013.05.034; Margui E, 2010, APPL SPECTROSC REV, V45, P179, DOI 10.1080/05704920903584198; Meira LA, 2018, MICROCHEM J, V142, P144, DOI 10.1016/j.microc.2018.06.025; Mohebbi M, 2018, J ANAL CHEM+, V73, P30, DOI 10.1134/S1061934818010069; Nomngongo PN, 2015, RSC ADV, V5, P72500, DOI 10.1039/c5ra12706h; Nomngongo PN, 2014, SPECTROCHIM ACTA B, V98, P54, DOI 10.1016/j.sab.2014.06.001; Pytlakowska K, 2019, J ANAL ATOM SPECTROM, V34, P1416, DOI [10.1039/c9ja00081j, 10.1039/C9JA00081J]; Pytlakowska K, 2013, ANAL METHODS-UK, V5, P6192, DOI 10.1039/c3ay40695d; Rathod TD, 2018, APPL RADIAT ISOTOPES, V135, P57, DOI 10.1016/j.apradiso.2018.01.014; Shemirani F, 2018, J IRAN CHEM SOC, V15, P1907, DOI 10.1007/s13738-018-1372-5; Wang SF, 2018, SPECTROSC SPECT ANAL, V38, P1648, DOI 10.3964/j.issn.1000-0593(2018)05-1648-07; Wang YF, 2017, J SEP SCI, V40, P4805, DOI 10.1002/jssc.201700744	30	11	11	2	43	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0039-9140	1873-3573		TALANTA	Talanta	JAN 15	2021	222								121514	10.1016/j.talanta.2020.121514	http://dx.doi.org/10.1016/j.talanta.2020.121514			7	Chemistry, Analytical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	OS2AN	33167225				2023-06-23	WOS:000589966900006
J	Pereira, LG; Fornari, M; Erthal, F; Leme, JM; Giannini, PCF				Pereira, Luiz Gustavo; Fornari, Milene; Erthal, Fernando; Leme, Juliana Moraes; Fonseca Giannini, Paulo Cesar			Multivariate taphonomic analysis of mollusk shell concentrations in Holocene deposits of southern Brazil: An integrated approach	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Actuopaleontology; GPR; Holocene; Coastal dynamics; Relative sea-level; Siliciclastic deposits	SANTA-CATARINA-STATE; SILICICLASTIC-CARBONATE SETTINGS; ANOMALOCARDIA-BRASILIANA GMELIN; FORMATION PLEISTOCENE-HOLOCENE; SEA-LEVEL CHANGES; DEATH ASSEMBLAGES; SEQUENCE STRATIGRAPHY; FOSSIL CONCENTRATIONS; BIVALVE TAPHONOMY; JAGUARUNA REGION	Shell concentrations are one of the most distinctive features of the Holocene coastal stratigraphy in the southern portion of Santa Catarina State, southern Brazil. In this paper, we integrated stratigraphic, geochronological, geophysical, and taphonomic data to discuss the processes involved in the genesis of shell concentrations in a siliciclastic and subtropical setting, a useful analogy for ancient shell concentrations in semi-closed environments affected by storms. The data indicated the succession of three facies associations (FA): bay, lagoon, and backbarrier. This succession implies a grain size fining-upward trend that is representative of a gradual shallowing. Interpretation of GPR sections revealed that the passage from the bay to lagoonal deposits occurred by forming a laterally continuous, high-amplitude surface overlain by sigmoidal reflections, which characterized the progressive basinward backstepping of the lagoonal margin. Shell concentrations in bay deposits are an allochthonous product of storm flows in shallow waters. In contrast, accumulations of the bivalve Anomalocardia brasiliana had their valves reworked in the lagoonal margins and transported to the bottom, characterizing a parautochthonous accumulation. In this study, the correlation of taphonomy and grain size indicates that in bay FA, the loss of periostracum is correlated with increased gradients of fine sand, and part of the shell samples correlates to corrosion and abrasion in increased gradients of medium sand and decreased ones of fine sand. Additionally, in the lagoon FA, the loss of periostracum depends on the decrease in mud-enriched sediments and the increase in fine and medium sand, whereas brightness loss and color alteration are related to the increase in fine and medium sand, as well as margin modification. Corrosion was positively correlated to the mud-dominated fraction.	[Pereira, Luiz Gustavo] Univ Bonn, Inst Geowissensch, Nussallee 8, D-53115 Bonn, Nord Rhine West, Germany; [Fornari, Milene] Sao Paulo State Univ UNESP, Biosci Inst, Coastal Campus,Praca Infante Dom Henrique S-N, BR-11330900 Sao Paulo, SP, Brazil; [Erthal, Fernando] Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias, Dept Paleontol & Estratig, BR-91501970 Porto Alegre, RS, Brazil; [Leme, Juliana Moraes; Fonseca Giannini, Paulo Cesar] Univ Sao Paulo, Inst Geociencias, Programa Posgrad Geoquim & Geotecton, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil	University of Bonn; Universidade Estadual Paulista; Universidade Federal do Rio Grande do Sul; Universidade de Sao Paulo	Pereira, LG (autor correspondente), Univ Bonn, Inst Geowissensch, Nussallee 8, D-53115 Bonn, Nord Rhine West, Germany.	guhhrexx@gmail.com; milene.fornari@unesp.com; fer.erthal@gmail.com; leme@usp.br; pcgianni@usp.br	Pereira, Luiz Gustavo/AAS-3210-2021; Erthal, Fernando/C-5941-2013; Giannini, Paulo César Fonseca/D-1871-2015	Pereira, Luiz Gustavo/0000-0002-8390-2346; Erthal, Fernando/0000-0001-8036-192X; Giannini, Paulo César Fonseca/0000-0003-1046-0177	CNPq (National Council for Scientific and Technological Development)	CNPq (National Council for Scientific and Technological Development)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank CNPq (National Council for Scientific and Technological Development) for financial support, especially Francisco Buchmann (Chico) and Erick Antal for the assistance and sample collection during fieldwork. 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J	Caxito, FA; Basto, CF; Santos, LCMD; Dantas, EL; de Medeiros, VC; Dias, TG; Barrote, V; Hagemann, S; Alkmim, AR; Lana, C				Caxito, Fabricio Andrade; Basto, Camila Franco; Santos, Lauro Cezar Montefalco de Lira; Dantas, Elton Luiz; de Medeiros, Vladimir Cruz; Dias, Tatiana Goncalves; Barrote, Vitor; Hagemann, Steffen; Alkmim, Ana Ramalho; Lana, Cristiano			Neoproterozoic magmatic arc volcanism in the Borborema Province, NE Brazil: possible flare-ups and lulls and implications for western Gondwana assembly	GONDWANA RESEARCH			English	Article						Continental arc magmatism; West Gondwana; Back-arc basin; Wilson Cycle; Introversion tectonics		New zircon U-Pb (SHRIMP and LA-ICPMS), elemental and Nd-Sr geochemistry data on rhyolitic metavolcanic and metavolcaniclastic rocks of NE Brazil characterize widespread arc-related phenomena during the Neoproterozoic, related to the Conceicao-type or Stage I plutonic rocks. U-Pb zircon dating pinpoint the main phase of magmatic activity at ca. 635-600 Ma in the 700-km long sigmoidal Pianco-Alto Brigida domain, but other important flare-ups might have taken place at ca. 670-690, 730-760, 810-820 and 860-880 Ma. A comprehensive compilation of detrital zircon data from metavolcanosedimentary successions of the entire Borborema Province (n=5532) confirms the occurrence of a quasi-continuum Neoproterozoic spectra punctuated by peaks at those same age intervals separated by minor lulls. Low Th/U rims of zircon crystals dated at ca. 577 Ma provide an estimate of the age of regional transpressional metamorphism. Samples of all age ranges are mostly calc-alkaline, magnesian and peraluminous, with moderately to highly fractionated LREE enrichment, negative Nb-Ta anomalies akin to convergent settings, and plot mainly within the volcanic arc field in tectonic discrimination diagrams. Nd-Sr isotope systematics indicate the involvement of juvenile Neoproterozoic melts from the mantle wedge, which upon mixing with Archean-Paleoproterozoic basement and contamination with the host metasedimentary rocks yield Mesoproterozoic T-DM mainly at 1.14-1.44 Ga, near-chondritic epsilon Nd(t) and Sr-87/Sr-86(i) 0.703-0.710. We put forward a model involving a major continental back-arc zone related to the development of the Conceicao magmatic arc, akin to the modern-day Taupo volcanic zone of New Zealand, crosscutting NE Brazil and presumably continuing through the schist belts of Nigeria and Cameroon. The main magmatic flare ups might have been induced by extra-arc phenomena, such as collision of the West African paleocontinent with the northwestern Borborema edge due to closure of the exterior Goias-Pharusian Ocean, force-speeding subduction in the interior V-shaped oceanic basins that constituted the Transnordestino-Central African Ocean and generating clockwise windshield-wiper-like rotation of the blocks back towards the Sao Francisco-Congo paleocontinent in a complete Wilson Cycle. (C) 2020 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.	[Caxito, Fabricio Andrade; Dias, Tatiana Goncalves] Univ Fed Minas Gerais CPMTC IGC UFMG, Inst Geociencias, Ctr Pesquisa Manoel Teixeira da Costa, Campus Pampulha,Ave Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Basto, Camila Franco] Geol Survey Brazil, Ave Brasil 1731, BR-30140002 Belo Horizonte, MG, Brazil; [Santos, Lauro Cezar Montefalco de Lira] Univ Fed Pernambuco, Dept Geol, Recife, PE, Brazil; [Dantas, Elton Luiz] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [de Medeiros, Vladimir Cruz] Geol Survey Brazil, R Prof Antonio Henrique de Melo 2010, BR-59078580 Natal, RN, Brazil; [Barrote, Vitor] Monash Univ, EAE, Isotopia Lab, Melbourne, Vic 3800, Australia; [Hagemann, Steffen] Univ Western Australia, Sch Earth & Environm, Ctr Explorat Targeting, 35 Stirling Highway, Crawley, WA 6009, Australia; [Alkmim, Ana Ramalho; Lana, Cristiano] Univ Fed Ouro Preto, Escola Minas, Dept Geol, Lab Geoquim Isotop, BR-35400000 Ouro Preto, MG, Brazil	Universidade Federal de Pernambuco; Universidade de Brasilia; Monash University; University of Western Australia; Universidade Federal de Ouro Preto	Caxito, FA (autor correspondente), Univ Fed Minas Gerais CPMTC IGC UFMG, Inst Geociencias, Ctr Pesquisa Manoel Teixeira da Costa, Campus Pampulha,Ave Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.	caxito@ufmg.br	Caxito, Fabricio A/J-1317-2016; de Lira Santos, Lauro Cézar Montefalco/E-5536-2015; Dantas, Elton Luiz/AAK-8464-2021	Caxito, Fabricio A/0000-0002-0335-3667; de Lira Santos, Lauro Cézar Montefalco/0000-0001-6098-1873; Dantas, Elton Luiz/0000-0002-7954-5059; Barrote, Vitor/0000-0001-7442-9748	CNPq, Brazil [303566/2019-1]; Instituto Serrapilheira [Serra-191231510]	CNPq, Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Instituto Serrapilheira	FAC, ELD and CL are recipients of Research Productivity grants from CNPq, Brazil, and acknowledge the support received, especially through grant number 303566/2019-1. The U-Pb analyseswere performed using a SHRIMP II probe at the John DeLaeter Centre of the Curtin University, Perth, Western Australia, enabled by NCRIS via AuScope. We thank all of the Centre crew, especially NealMcNaughton, which guided the sample mounting and analysis process, and Allen Kennedy and Hao Gao, which aided in the analysis. This is a contribution to Project Mobile (geolifemobile.com), supported by Instituto Serrapilheira (Serra-191231510). An original version of the paper was improved after comments and suggestions by two anonymous reviewers.	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APR	2021	92						1	25		10.1016/j.gr.2020.11.015	http://dx.doi.org/10.1016/j.gr.2020.11.015		JAN 2021	25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QL4NE					2023-06-23	WOS:000621054900001
J	Haag, MB; de Freitas, RB; Sommer, CA; Savian, JF; Lima, EF; Gambeta, JH; Lyra, DD; da Trindade, RIF				Haag, Mauricio Barcelos; de Freitas, Rayane Bastos; Sommer, Carlos Augusto; Savian, Jairo Francisco; Lima, Evandro Fernandes; Gambeta, Johnathan Henrique; Lyra, Diego da Silveira; Ferreira da Trindade, Ricardo Ivan			Multi-proxy case study of a Neoproterozoic rhyolite flow in southernmost Brazil: Emplacement mechanisms and implications for ancient felsic lavas	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Rhyolite flow; Emplacement; Rheology; AMS; High-silica lava	MAGNETIC-ANISOTROPY; PREFERRED ORIENTATION; VISCOSITY; ROCKS; DISCRIMINATION; SUSCEPTIBILITY; VOLCANISM; RHEOLOGY; ERUPTION; HETEROGENEITY	Rhyolites compose an important record in the volcanic history of Earth, with significant occurrences in volcanic arcs, large igneous provinces and post-collisional terranes, often associated with explosive events. In several geologic provinces, rhyolites dominate as the most expressive geologic units (e.g., Silicic Large Igneous Provinces - SLIPs). Despite their importance, several aspects related to the emplacement of rhyolite flows are still enigmatic. Recent studies in modern rhyolite lavas suggest similar emplacement mechanisms to basaltic lavas, implying a more dynamic growth model for silicic flows, including outbreak lobes and outpour structures. Despite these advances, studies related to the recognition of these features in ancient flows are still rare. In this work we perform a multi-proxy study of an ancient (Neoproterozoic) rhyolitic lava flow combining fieldwork, petrography, geochemistry, rheology and magnetic fabric analysis. The Cerro do Perau outcrop (CP, southern Brazil) consists of a natural laboratory for the study of rhyolite lavas, presenting excellent exposure of a partially preserved flow with distinct flow features and folds. CP flow consists of a high-silica and low-crystal content rhyolite, suggesting its emplacement as an obsidian flow. Rheology data indicates high liquidus temperatures (>957 ?C), with maximum viscosities of 108.5 Pa s and glass transition temperatures (Tg) of 750 ?C. The absence of brittle features suggests little to none displacement below Tg. Structural analysis indicates the predominance of sub-vertical foliation planes, including axial planes of folds, indicative of proximal (near-vent) regions in rhyolite flows. The absence of lineations favors a predominantly planar accommodation of the flow-induced deformation, which is confirmed by the shape of the magnetic fabric ellipsoids. Several of these ellipsoids display a high degree of anisotropy, mostly related to an oblate fabric, indicative of the development of high-strain zones within the flow. Our data suggest that CP flow presents some similarities with recently proposed field-based emplacement models for rhyolitic flows, highlighting the significant data that can be extracted from a combination of magnetic fabrics and rheological analyses.	[Haag, Mauricio Barcelos; de Freitas, Rayane Bastos; Sommer, Carlos Augusto; Savian, Jairo Francisco; Lima, Evandro Fernandes; Gambeta, Johnathan Henrique; Lyra, Diego da Silveira] Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil; [Ferreira da Trindade, Ricardo Ivan] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226, Sao Paulo, SP, Brazil	Universidade Federal do Rio Grande do Sul; Universidade de Sao Paulo	Haag, MB (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil.	mauricio.haag@ufrgs.br	Savian, Jairo Francisco/J-4782-2015; Sommer, Carlos A/Q-9077-2018; Trindade, Ricardo IF/A-8146-2008	Savian, Jairo Francisco/0000-0002-5032-3217; Sommer, Carlos A/0000-0001-8696-7084; Trindade, Ricardo IF/0000-0001-9848-9550; Barcelos Haag, Mauricio/0000-0001-5038-4418	Brazilian National Council for Scientific and Technological Development (CNPq) [303015/2015-2, 441766/2014-5, 304036/2018-8, 406925/2018-6]	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We would like to thank the reviewers Eric Ferr ' e and Irine Raposo, and the editors Augusto Rapalini and Andres Folguera for their comments and careful review, which helped improve the manuscript. This work was partially funded by the Brazilian National Council for Scientific and Technological Development (CNPq), projects 303015/2015-2, 441766/2014-5, 304036/2018-8, and 406925/2018-6.	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South Am. Earth Sci.	APR	2021	107								102982	10.1016/j.jsames.2020.102982	http://dx.doi.org/10.1016/j.jsames.2020.102982		JAN 2021	14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	RJ5QX					2023-06-23	WOS:000637657700004
J	Alencar, ML; Correia, OJ; de Miranda, TS; Barbosa, JA; Celestino, MAL; Ramos, GMS; de Araujo, AFL; Neumann, VH; Topan, JGD; Roemers-Oliveira, E				Alencar, Marcio Lima; Correia Filho, Osvaldo Jose; de Miranda, Tiago Siqueira; Barbosa, Jose Antonio; Lima Celestino, Maria Alcione; Silva Ramos, Germano Mario; Lima de Araujo, Araly Fabiana; Neumann, Virginio Henrique; de Oliveira Topan, Joao Gabriel; Roemers-Oliveira, Eduardo			Soft-sediment deformation structures in Aptian lacustrine laminites: Evidence of post-rift paleoseismicity in the Araripe basin, NE Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Crato formation; Tectonic reactivation; Soft-sediment deformation; Post-rift phase; Araripe Basin	WATER-ESCAPE STRUCTURES; GREEN RIVER FORMATION; EARTHQUAKE MAGNITUDE; CONTINENTAL-MARGIN; STRESS-FIELD; ORDOS BASIN; SE SPAIN; SEISMITES; LIQUEFACTION; DEPOSITS	Soft-sediment deformation structures (SSDS) represent synsedimentary structures that can be formed under different tectonic regimes and are considered of great importance for studies associated with the paleoseismic activity. SSDS represent depositional heterogeneities and play an important role in fluid flow, thus influencing hydrocarbon or groundwater reservoirs. This paper describes the SSDS in Aptian lacustrine finely laminated limestones of Crato Formation, the post-rift sequence of Araripe Basin, NE Brazil. SSDS occur in laterally continuous beds, with an average thickness of 5 cm. The set of studied structures comprises loop beddings, convolute laminations, micro faults, fluid escape structures, simple and pendulous load cast, and detached pseudonodules. We interpreted that these structures resulted from seismic activity associated with brittle reactivation of the Patos shear zone, a major structure that borders the Araripe Basin. This interpretation points to a long history of post-rift tectonic activity of the Borborema Province (NE, Brazil). The diversity and abundance of these structures in these post-rift deposits show that this type of heterogeneities can be formed in tectonicsedimentary sequences otherwise considered less, or non-affected, by seismic activities.	[Alencar, Marcio Lima; Correia Filho, Osvaldo Jose; Barbosa, Jose Antonio; Silva Ramos, Germano Mario; Lima de Araujo, Araly Fabiana; de Oliveira Topan, Joao Gabriel] Univ Fed Pernambuco, Dept Geol, GEOQUANTT, Pesquisa Geociencias, Av Arquitetura S-N,Cid Univ, BR-50740550 Recife, PE, Brazil; [de Miranda, Tiago Siqueira; Lima Celestino, Maria Alcione; Neumann, Virginio Henrique] Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil; [Roemers-Oliveira, Eduardo] Petrobras Res Ctr, Av Horacio Macedo 950,Cidade Univ, BR-21941915 Rio De Janeiro, RJ, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Petrobras	Alencar, ML (autor correspondente), Av Arquitetura 953-995,Cidade Univ, BR-50740540 Recife, PE, Brazil.	mlimaalencar@gmail.com; osv.correia@gmail.com; tiago.smiranda@ufpe.br; jose.antoniob@ufpe.br; alcionelimma22@gmail.com; nonogermano@gmail.com; aralyfabiana23@gmail.com; neumann@ufpe.br; gabrieltopan@gmail.com; roemers@petrobras.com.br	Miranda, Tiago S/P-8113-2018; BARBOSA, JOSE ANTONIO/AAB-4437-2020	Miranda, Tiago S/0000-0001-9099-1271; BARBOSA, JOSE ANTONIO/0000-0001-8754-6310; Neumann, Virginio/0000-0002-8827-6022	Petrobras	Petrobras(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras)	This study was supported by Petrobras that funded the projects "Crato" and "Pseudo-pocos" through research agreements approved by the National Agency of Petroleum, Natural Gas and Biofuels (ANP). 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South Am. Earth Sci.	JAN	2021	105								102955	10.1016/j.jsames.2020.102955	http://dx.doi.org/10.1016/j.jsames.2020.102955			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	4M4AY					2023-06-23	WOS:000853267600001
J	Carreira, RS; de Albergaria-Barbosa, ACR; Arguelho, MDPM; Garcia, CAB				Carreira, Renato S.; de Albergaria-Barbosa, Ana Cecilia R.; Arguelho, Maria de Lara P. M.; Garcia, Carlos A. B.			A lipid biomarker investigation of the sources and distribution of organic matter in river-influenced shelf sediments of NE Brazil	ORGANIC GEOCHEMISTRY			English	Article						Sergipe-Alagoas continental shelf; Organic matter; Molecular markers; Sterols; n-Alcohols; Taraxerol	SAO FRANCISCO RIVER; SURFACE SEDIMENTS; CARBON-CYCLE; COASTAL ZONE; CONTINENTAL-MARGIN; CLIMATE-CHANGE; SW ATLANTIC; TERRESTRIAL; ESTUARY; OCEAN	A better understanding of the sources - continental or marine - and distribution of organic matter (OM) in shelf sediments of areas under distinct natural and anthropogenic forces is essential to obtain a global view of the carbon cycle. In this study, we evaluated the influence of river discharge on the OM accumulation pattern in a portion of the NE Brazilian continental margin (10-15 degrees S) by considering a suite of lipid biomarkers (sterols, n-alcohols, phytol and taraxerol) in surface sediments. A total of 36 samples were collected adjacent to river mouths representing drainage basins of varying size and representing different human intervention levels, namely the Sao Francisco, Vaza Barris, Sergipe and Piaui-Real rivers. The average concentration of the total quantified lipids was 3.77 +/- 1.93 mu g g(-1), with the lowest values detected at the Sao Francisco River pro-delta. This result seems to reflect the reductions in the Sao Francisco river flow during the last decades caused by human interventions (diverse water use and urbanization, among others) and climate change (reduced precipitation) along its drainage basin, which seems to affect other smaller basins to a lesser extent. Our findings highlight that human interventions and climate change are relevant drivers for biogeochemical processes even in shelves receiving the flow from small to medium rivers in Brazil, which agree with other records worldwide. Finally, we hope the data presented herein contribute to the development of a management system based on a watershed-coastal ocean scaling and socio-environmental perspective for the Sergipe and Alagoas shelf. (C) 2020 Elsevier Ltd. All rights reserved.	[Carreira, Renato S.] Pontificia Univ Catolica Rio de Janeiro PUC Rio, LabMAM, Dept Quim, BR-22451900 Rio De Janeiro, Brazil; [de Albergaria-Barbosa, Ana Cecilia R.] Univ Fed Bahia UFBA, Dept Oceanog, GeoqMar, BR-40170020 Salvador, BA, Brazil; [Arguelho, Maria de Lara P. M.; Garcia, Carlos A. B.] Univ Fed Sergipe UFS, Dept Quim, LQA, BR-49100000 Sergipe, Brazil	Universidade Federal de Sergipe	Carreira, RS (autor correspondente), Pontificia Univ Catolica Rio de Janeiro PUC Rio, LabMAM, Dept Quim, BR-22451900 Rio De Janeiro, Brazil.	carreira@puc-rio.br	Carreira, Renato S/I-5559-2012; Garcia, Carlos Alexandre Borges/A-8406-2013; de Albergaria-Barbosa, Ana Cecília/AAC-6940-2021	Carreira, Renato S/0000-0002-1308-6611; Garcia, Carlos Alexandre Borges/0000-0001-5260-5093; 	CNPq [402459/2012-1, 309347/2017-3]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank Petrobras for providing the samples under the ``Environmental characterization of the Sergipe and Alagoas continental margin"project and to provide the information of sediment granulometry displayed in Fig. 1. A.C.R.A-Barbosa was supported by a post-doc fellowship from CNPq (proc. no. 402459/2012-1). R.S. Carreira is a CNPq research fellow (proc. no. grant 309347/2017-3). We also thank Co-Editor-in-Chief Dr. John Volkman, Associate Editor Dr. Isla Castaneda, Dr. Nemiah Ladd and an anonymous reviewer for their comments and suggestions, which greatly improved this manuscript.	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Geochem.	JAN	2021	151								104162	10.1016/j.orggeochem.2020.104162	http://dx.doi.org/10.1016/j.orggeochem.2020.104162			9	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	PY3YP					2023-06-23	WOS:000611983000005
J	Cheng, X; Bantim, RAM; Sayao, JM; Zhang, XJ; Jiang, SX; Kellner, AWA; Wang, XL; Saraiva, AAF				Cheng, Xin; Bantim, Renan A. M.; Sayao, Juliana M.; Zhang, Xinjun; Jiang, Shunxing; Kellner, Alexander W. A.; Wang, Xiaolin; Saraiva, Antonio A. F.			Short note on the vertebral column of the Tapejaridae (Pterosauria, Pterodactyloidea) based on a new specimen from the Crato Formation (late Aptian, Early Cretaceous), northeast Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Flying reptiles; Ontogeny; Axial skeleton; Notarium; Synsacrum; Evolutionary trend	JIUFOTANG FORMATION; WESTERN; ONTOGENY	The Tapejaridae compose a pterodactyloid clade of pterosaurs that is one of the most abundant flying reptiles in the deposits of the Early Cretaceous Crato Formation from the Araripe Basin, northeast Brazil. Until now, only one tapejarid specimen from this locality shows a relatively complete vertebral column. Here we describe a second specimen (LPU 1535) and compare it with more complete tapejarine tapejarids from western Liaoning (China). Among the most striking differences are the absence of a notarium in the Chinese material and the lesser number of dorsal elements in the Brazilian specimens, the latter perhaps being an evolutionary trend in the Tapejarinae. The new material confirms that the number of dorsal elements forming the notarium and taking part in the synsacrum increase during ontogeny. Some member of the Tapejaridae might share the dorsal part of the postacetabular process of ilia extending medially and fusing to the neural spines of the sacral vertebrae, a feature previously observed in the pteranodontid pterodactyloid Pteranodon.	[Cheng, Xin; Bantim, Renan A. M.; Saraiva, Antonio A. F.] Univ Reg Cariri, Lab Paleontol URCA, Rua Carolino Sucupira S-N, BR-63100000 Crato, CE, Brazil; [Cheng, Xin] Jilin Univ, Key Lab Evolut Life & Environm Northeast Asia, Minist Educ, Ximinzhu St 6, Changchun 130061, Jilin, Peoples R China; [Cheng, Xin] Jilin Univ, Coll Earth Sci, Jianshe St 2199, Changchun 130061, Jilin, Peoples R China; [Cheng, Xin; Jiang, Shunxing] Nanjing Inst Geol & Palaeontol CAS, State Key Lab Palaeobiol & Stratig, East Beijing Rd 39, Nanjing 210008, Jiangsu, Peoples R China; [Sayao, Juliana M.; Kellner, Alexander W. A.] Univ Fed Rio de Janeiro, Lab Systemat & Taphon Fossil Vertebrates, Dept Geol & Paleontol, Museu Nacl, Quinta da Boa Vista S-N, BR-20940040 Sao Cristovao, RJ, Brazil; [Zhang, Xinjun; Jiang, Shunxing; Wang, Xiaolin] Chinese Acad Sci, Key Lab Vertebrate Evolut & Human Origins, Inst Vertebrate Paleontol & Paleoanthropol, Xizhimenwai St 142, Beijing 100044, Peoples R China; [Zhang, Xinjun; Jiang, Shunxing; Wang, Xiaolin] CAS Ctr Excellence Life & Paleoenvironm, Xizhimenwai St 142, Beijing 100044, Peoples R China; [Zhang, Xinjun; Wang, Xiaolin] Univ Chinese Acad Sci, Yuquan Rd 19, Beijing 100049, Peoples R China	Universidade Regional do Cariri; Jilin University; Jilin University; Chinese Academy of Sciences; Universidade Federal do Rio de Janeiro; Chinese Academy of Sciences; Institute of Vertebrate Paleontology & Paleoanthropology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Cheng, X (autor correspondente), Univ Reg Cariri, Lab Paleontol URCA, Rua Carolino Sucupira S-N, BR-63100000 Crato, CE, Brazil.	chengxin@jlu.edu.cn	Saraiva, António/HPD-3031-2023; Bantim, Renan/J-4076-2014	ZHANG, Xinjun/0000-0002-1503-1980	Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) [DCR-0024-02039.01.00/, BMD-0124-00302.01.01/19]; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS) [193106, 183113]; National Natural Science Foundation of China [42072017, 41602011, 41688103, 41572020]; Fundamental Research Funds for the Central Universities, JLU [45119031B048]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [458164/2014-3, 420687/2016-5, 313461/2018-0, 311715/2017-6]; Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [E-26/202.905/2018]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001, 88887.162865/2018-00]; Strategic Priority Research Program of Chinese Academy of Sciences [XDB18000000]	Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS)(Chinese Academy of Sciences); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Fundamental Research Funds for the Central Universities, JLU; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Strategic Priority Research Program of Chinese Academy of Sciences(Chinese Academy of Sciences)	We thank Jennyfer Sobreira Ferreira from Pontificia Universidade Catolica do Rio Grande do Sul (PUC-RS) for previous preparation of LPU 1535. This study was supported by the Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) under Grant to XC DCR-0024-02039.01.00/and RAMB #BMD-0124-00302.01.01/19, State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS) under Grant to XC No.193106 and to SXJ No.183113, the National Natural Science Foundation of China under Grant to XC 42072017, to SXJ 41602011 and to XLW (41688103, 41572020) and the Fundamental Research Funds for the Central Universities, JLU under Grant to XC 45119031B048; the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) under Grant to AAFS 458164/2014-3, to AWAK 420687/2016-5 and 313461/2018-0, and to JMS 311715/2017-6; the Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) under Grant to AWAK E-26/202.905/2018; the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) Finance Code 001 to RAMB CAPES #88887.162865/2018-00; and the Strategic Priority Research Program of Chinese Academy of Sciences under Grant to XLW (XDB18000000).	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South Am. Earth Sci.	JAN	2021	105								102921	10.1016/j.jsames.2020.102921	http://dx.doi.org/10.1016/j.jsames.2020.102921			6	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PQ8LV					2023-06-23	WOS:000606795900002
J	Correa, RS; Oliveira, CG; Dantas, EL; Della Giustina, MES; Hollanda, MHBM				Correa, R. S.; Oliveira, C. G.; Dantas, E. L.; Della Giustina, M. E. S.; Hollanda, M. H. B. M.			The root zones of the Serido W-skarn system, northeastern Brazil: Constraints on the metallogenesis of a large Ediacaran tungsten Province	ORE GEOLOGY REVIEWS			English	Article							OXIDE-COPPER-GOLD; DETRITAL ZIRCON AGES; GRANDE-DO-NORTE; BORBOREMA PROVINCE; NE-BRAZIL; NORTHWEST-TERRITORIES; WEST GONDWANA; STRUCTURAL CONTROL; ORE-DEPOSITS; RE-OS	In the literature, skarn deposits have their genesis commonly explained by the interaction between a magmatic-hydrothermal fluid and carbonate rocks. There are, however, a large number of exceptions to this rule. One of the best examples may be the Serido Mineral Province, where more than 700 scheelite deposits and occurrences have produced around 60,000 t of WO3 over the last hundred years. Important deposits, such as Bonfim, Brejui, Bodo and Barra Verde, develop classic skarn alteration in the contact with marbles, forming diopside- and/or garnet-dominant parageneses. Other types of occurrences account for amphibole- and/or biotite-dominant assemblages interpreted respectively as Ca(Ba) and K hydrothermal alteration rocks that occur along granitoid basement rocks. Apart from pegmatitic dykes, the Ca(Ba) and K metasomatic rocks do not show any clear association with carbonate rocks and/or plutonic bodies. Instead, most of these W-bearing rocks are strongly associated with subvertical N20 degrees E-trending shear zones, being more structurally controlled than lithologically dependent. Some of the most representative skarn, Ca(Ba) and K alteration deposits and occurrences of the area, which occur in different geological units, were studied in this work. Whole rock geochemistry analyses of the metasomatic rocks of the Ca(Ba) alteration point to Ca, Mg, Fe, Ba, Na and REE metasomatism, while rocks of the K alteration are characterized by Na, K, Si, Mo and W metasomatism. The scheelite-bearing metasomatic Ca(Ba) and K rocks are hosted in different basement granitoid wallrocks. In the Bonfim deposit, relict Paleoarchean zircon grains yielded an age of 3324 +/- 33 Ma; Neoarchean crystals yielded an age of 2699 +/- 11 Ma in Pedro Tomas; relict Paleoproterozoic grains from Salgadinho held ages of 2217 +/- 6 Ma and 2177 +/- 16 Ma; and a Paleoproterozoic age of 2194 +/- 31 Ma was verified in the Cacador occurrence. W +/- Mo mineralization is correlated with the Neoproterozoic-Ediacaran Brasiliano Cycle. In the Salgadinho occurrence, the core of a single grain along with the borders of some crystals provided concordant ages of 575 +/- 3 Ma, 558 +/- 4 Ma and 536 +/- 3 Ma, which may be correlated to peak orogenic and metasomatic events. Results of similar age were identified by 40Ar/39Ar analyses in amphibole, with the ages 553 +/- 3 Ma and 548 +/- 2 Ma for Bonfim and 557 +/- 7 Ma for Salgadinho; while analyses in biotite produced the ages 498 +/- 2 Ma and 501 +/- 2 Ma for Cacador. Following a new model for the area, the rocks studied in this work are interpreted as the root zones of the W +/- Mo-skarns, presenting spatial and temporal associations with them. The Ca(Ba) and K alteration rocks along with skarns are part of the same system, but formed under different pressure, temperature, chemical, pH and REDOX conditions, as well as distinct fluid/rock ratios and hydrothermal solution and wallrock compositions. The regional-scale zoning between W +/- Mo and relatively coeval Au deposits in the Serido Mineral Province also suggests that they are cogenetic, being part of an Intrusion-Related system. In the literature, skarn deposits have their genesis commonly explained by the interaction between a magmatic-hydrothermal fluid and carbonate rocks. There are, however, a large number of exceptions to this rule. One of the best examples may be the Serido Mineral Province, where more than 700 scheelite deposits and occurrences have produced around 60,000 t of WO3 over the last hundred years. Important deposits, such as Bonfim, Brejui, Bodo and Barra Verde, develop classic skarn alteration in the contact with marbles, forming diopside- and/or garnet-dominant parageneses. Other types of occurrences account for amphibole- and/or biotite-dominant assemblages interpreted respectively as Ca(Ba) and K hydrothermal alteration rocks that occur along granitoid basement rocks. Apart from pegmatitic dykes, the Ca(Ba) and K metasomatic rocks do not show any clear association with carbonate rocks and/or plutonic bodies. Instead, most of these W-bearing rocks are strongly associated with subvertical N20 degrees E-trending shear zones, being more structurally controlled than lithologically dependent. Some of the most representative skarn, Ca(Ba) and K alteration deposits and occurrences of the area, which occur in different geological units, were studied in this work. Whole rock geochemistry analyses of the metasomatic rocks of the Ca(Ba) alteration point to Ca, Mg, Fe, Ba, Na and REE metasomatism, while rocks of the K alteration are characterized by Na, K, Si, Mo and W metasomatism. The scheelite-bearing metasomatic Ca(Ba) and K rocks are hosted in different basement granitoid wallrocks. In the Bonfim deposit, relict Paleoarchean zircon grains yielded an age of 3324 +/- 33 Ma; Neoarchean crystals yielded an age of 2699 +/- 11 Ma in Pedro Tomas; relict Paleoproterozoic grains from Salgadinho held ages of 2217 +/- 6 Ma and 2177 +/- 16 Ma; and a Paleoproterozoic age of 2194 +/- 31 Ma was verified in the Cacador occurrence. W +/- Mo mineralization is correlated with the Neoproterozoic-Ediacaran Brasiliano Cycle. In the Salgadinho occurrence, the core of a single grain along with the borders of some crystals provided concordant ages of 575 +/- 3 Ma, 558 +/- 4 Ma and 536 +/- 3 Ma, which may be correlated to peak orogenic and metasomatic events. Results of similar age were identified by 40Ar/39Ar analyses in amphibole, with the ages 553 +/- 3 Ma and 548 +/- 2 Ma for Bonfim and 557 +/- 7 Ma for Salgadinho; while analyses in biotite produced the ages 498 +/- 2 Ma and 501 +/- 2 Ma for Cacador. Following a new model for the area, the rocks studied in this work are interpreted as the root zones of the W +/- Mo-skarns, presenting spatial and temporal associations with them. The Ca(Ba) and K alteration rocks along with skarns are part of the same system, but formed under different pressure, temperature, chemical, pH and REDOX conditions, as well as distinct fluid/rock ratios and hydrothermal solution and wallrock compositions. The regional-scale zoning between W +/- Mo and relatively coeval Au deposits in the Serido Mineral Province also suggests that they are cogenetic, being part of an Intrusion-Related system. In the literature, skarn deposits have their genesis commonly explained by the interaction between a magmatic-hydrothermal fluid and carbonate rocks. There are, however, a large number of exceptions to this rule. One of the best examples may be the Serido Mineral Province, where more than 700 scheelite deposits and occurrences have produced around 60,000 t of WO3 over the last hundred years. Important deposits, such as Bonfim, Brejui, Bodo and Barra Verde, develop classic skarn alteration in the contact with marbles, forming diopside- and/or garnet-dominant parageneses. Other types of occurrences account for amphibole- and/or biotite-dominant assemblages interpreted respectively as Ca(Ba) and K hydrothermal alteration rocks that occur along granitoid basement rocks. Apart from pegmatitic dykes, the Ca(Ba) and K metasomatic rocks do not show any clear association with carbonate rocks and/or plutonic bodies. Instead, most of these W-bearing rocks are strongly associated with subvertical N20 degrees E-trending shear zones, being more structurally controlled than lithologically dependent. Some of the most representative skarn, Ca(Ba) and K alteration deposits and occurrences of the area, which occur in different geological units, were studied in this work. Whole rock geochemistry analyses of the metasomatic rocks of the Ca(Ba) alteration point to Ca, Mg, Fe, Ba, Na and REE metasomatism, while rocks of the K alteration are characterized by Na, K, Si, Mo and W metasomatism. The scheelite-bearing metasomatic Ca(Ba) and K rocks are hosted in different basement granitoid wallrocks. In the Bonfim deposit, relict Paleoarchean zircon grains yielded an age of 3324 +/- 33 Ma; Neoarchean crystals yielded an age of 2699 +/- 11 Ma in Pedro Tomas; relict Paleoproterozoic grains from Salgadinho held ages of 2217 +/- 6 Ma and 2177 +/- 16 Ma; and a Paleoproterozoic age of 2194 +/- 31 Ma was verified in the Cacador occurrence. W +/- Mo mineralization is correlated with the Neoproterozoic-Ediacaran Brasiliano Cycle. In the Salgadinho occurrence, the core of a single grain along with the borders of some crystals provided concordant ages of 575 +/- 3 Ma, 558 +/- 4 Ma and 536 +/- 3 Ma, which may be correlated to peak orogenic and metasomatic events. Results of similar age were identified by 40Ar/39Ar analyses in amphibole, with the ages 553 +/- 3 Ma and 548 +/- 2 Ma for Bonfim and 557 +/- 7 Ma for Salgadinho; while analyses in biotite produced the ages 498 +/- 2 Ma and 501 +/- 2 Ma for Cacador. Following a new model for the area, the rocks studied in this work are interpreted as the root zones of the W +/- Mo-skarns, presenting spatial and temporal associations with them. The Ca(Ba) and K alteration rocks along with skarns are part of the same system, but formed under different pressure, temperature, chemical, pH and REDOX conditions, as well as distinct fluid/rock ratios and hydrothermal solution and wallrock compositions. The regional-scale zoning between W +/- Mo and relatively coeval Au deposits in the Serido Mineral Province also suggests that they are cogenetic, being part of an Intrusion-Related system. In the literature, skarn deposits have their genesis commonly explained by the interaction between a magmatic-hydrothermal fluid and carbonate rocks. There are, however, a large number of exceptions to this rule. One of the best examples may be the Serido Mineral Province, where more than 700 scheelite deposits and occurrences have produced around 60,000 t of WO3 over the last hundred years. Important deposits, such as Bonfim, Brejui, Bodo and Barra Verde, develop classic skarn alteration in the contact with marbles, forming diopside- and/or garnet-dominant parageneses. Other types of occurrences account for amphibole- and/or biotite-dominant assemblages interpreted respectively as Ca(Ba) and K hydrothermal alteration rocks that occur along granitoid basement rocks. Apart from pegmatitic dykes, the Ca(Ba) and K metasomatic rocks do not show any clear association with carbonate rocks and/or plutonic bodies. Instead, most of these W-bearing rocks are strongly associated with subvertical N20 degrees E-trending shear zones, being more structurally controlled than lithologically dependent. Some of the most representative skarn, Ca(Ba) and K alteration deposits and occurrences of the area, which occur in different geological units, were studied in this work. Whole rock geochemistry analyses of the metasomatic rocks of the Ca(Ba) alteration point to Ca, Mg, Fe, Ba, Na and REE metasomatism, while rocks of the K alteration are characterized by Na, K, Si, Mo and W metasomatism. The scheelite-bearing metasomatic Ca(Ba) and K rocks are hosted in different basement granitoid wallrocks. In the Bonfim deposit, relict Paleoarchean zircon grains yielded an age of 3324 +/- 33 Ma; Neoarchean crystals yielded an age of 2699 +/- 11 Ma in Pedro Tomas; relict Paleoproterozoic grains from Salgadinho held ages of 2217 +/- 6 Ma and 2177 +/- 16 Ma; and a Paleoproterozoic age of 2194 +/- 31 Ma was verified in the Cacador occurrence. W +/- Mo mineralization is correlated with the Neoproterozoic-Ediacaran Brasiliano Cycle. In the Salgadinho occurrence, the core of a single grain along with the borders of some crystals provided concordant ages of 575 +/- 3 Ma, 558 +/- 4 Ma and 536 +/- 3 Ma, which may be correlated to peak orogenic and metasomatic events. Results of similar age were identified by 40Ar/39Ar analyses in amphibole, with the ages 553 +/- 3 Ma and 548 +/- 2 Ma for Bonfim and 557 +/- 7 Ma for Salgadinho; while analyses in biotite produced the ages 498 +/- 2 Ma and 501 +/- 2 Ma for Cacador. Following a new model for the area, the rocks studied in this work are interpreted as the root zones of the W +/- Mo-skarns, presenting spatial and temporal associations with them. The Ca(Ba) and K alteration rocks along with skarns are part of the same system, but formed under different pressure, temperature, chemical, pH and REDOX conditions, as well as distinct fluid/rock ratios and hydrothermal solution and wallrock compositions. The regional-scale zoning between W +/- Mo and relatively coeval Au deposits in the Serido Mineral Province also suggests that they are cogenetic, being part of an Intrusion-Related system. In the literature, skarn deposits have their genesis commonly explained by the interaction between a magmatic-hydrothermal fluid and carbonate rocks. There are, however, a large number of exceptions to this rule. One of the best examples may be the Serido Mineral Province, where more than 700 scheelite deposits and occurrences have produced around 60,000 t of WO3 over the last hundred years. Important deposits, such as Bonfim, Brejui, Bodo and Barra Verde, develop classic skarn alteration in the contact with marbles, forming diopside- and/or garnet-dominant parageneses. Other types of occurrences account for amphibole- and/or biotite-dominant assemblages interpreted respectively as Ca(Ba) and K hydrothermal alteration rocks that occur along granitoid basement rocks. Apart from pegmatitic dykes, the Ca(Ba) and K metasomatic rocks do not show any clear association with carbonate rocks and/or plutonic bodies. Instead, most of these W-bearing rocks are strongly associated with subvertical N20 degrees E-trending shear zones, being more structurally controlled than lithologically dependent. Some of the most representative skarn, Ca(Ba) and K alteration deposits and occurrences of the area, which occur in different geological units, were studied in this work. Whole rock geochemistry analyses of the metasomatic rocks of the Ca(Ba) alteration point to Ca, Mg, Fe, Ba, Na and REE metasomatism, while rocks of the K alteration are characterized by Na, K, Si, Mo and W metasomatism. The scheelite-bearing metasomatic Ca(Ba) and K rocks are hosted in different basement granitoid wallrocks. In the Bonfim deposit, relict Paleoarchean zircon grains yielded an age of 3324 +/- 33 Ma; Neoarchean crystals yielded an age of 2699 +/- 11 Ma in Pedro Tomas; relict Paleoproterozoic grains from Salgadinho held ages of 2217 +/- 6 Ma and 2177 +/- 16 Ma; and a Paleoproterozoic age of 2194 +/- 31 Ma was verified in the Cacador occurrence. W +/- Mo mineralization is correlated with the Neoproterozoic-Ediacaran Brasiliano Cycle. In the Salgadinho occurrence, the core of a single grain along with the borders of some crystals provided concordant ages of 575 +/- 3 Ma, 558 +/- 4 Ma and 536 +/- 3 Ma, which may be correlated to peak orogenic and metasomatic events. Results of similar age were identified by 40Ar/39Ar analyses in amphibole, with the ages 553 +/- 3 Ma and 548 +/- 2 Ma for Bonfim and 557 +/- 7 Ma for Salgadinho; while analyses in biotite produced the ages 498 +/- 2 Ma and 501 +/- 2 Ma for Cacador. Following a new model for the area, the rocks studied in this work are interpreted as the root zones of the W +/- Mo-skarns, presenting spatial and temporal associations with them. The Ca(Ba) and K alteration rocks along with skarns are part of the same system, but formed under different pressure, temperature, chemical, pH and REDOX conditions, as well as distinct fluid/rock ratios and hydrothermal solution and wallrock compositions. The regional-scale zoning between W +/- Mo and relatively coeval Au deposits in the Serido Mineral Province also suggests that they are cogenetic, being part of an Intrusion-Related system.	[Correa, R. S.; Oliveira, C. G.; Dantas, E. L.; Della Giustina, M. E. S.] Univ Brasilia, Inst Geociencias, Campus Asa Norte, BR-70910900 Brasilia, DF, Brazil; [Hollanda, M. H. B. M.] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, SP, Brazil	Universidade de Brasilia; Universidade de Sao Paulo	Correa, RS (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Asa Norte, BR-70910900 Brasilia, DF, Brazil.	robertodesiqueiracorrea@gmail.com	Della Giustina, Maria Emilia S/L-9910-2015; Dantas, Elton Luiz/AAK-8464-2021	Della Giustina, Maria Emilia S/0000-0001-8516-102X; Dantas, Elton Luiz/0000-0002-7954-5059; Hollanda, Maria Helena Bezerra Maia/0000-0003-2231-7917	CAPES; CNPq [474380/2006-8, 308312/2014-7]	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to thank the Earth Sciences Institute of the University of Brasilia for providing the analytical infrastructure, CAPES for the financial support, CNPq for the research grants (projects 474380/2006-8 and 308312/2014-7), the kind geologist Valdir Silveira (Brazilian Geological Survey -CPRM) for the help during the field work and professor Rongqing Zhang and an anonymous reviewer for their relevant comments and corrections.	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Rev.	JAN	2021	128								103884	10.1016/j.oregeorev.2020.103884	http://dx.doi.org/10.1016/j.oregeorev.2020.103884			29	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	PO9TC					2023-06-23	WOS:000605513300001
J	Ferreira, BF; Marques, JC; Frantz, JC; de Souza, RG; Campos, MP; Figueiredo, FLAD; Padilha, NL				Ferreira, Bruna Fiscuk; Marques, Juliana Chara; Frantz, Jose Carlos; de Souza, Renan Guilherme; Campos, Marcelo Pereira; Antoniazzi de Rezende Figueiredo, Frederico Lana; Padilha, Nicole Lopes			Stratigraphy and U-Pb detrital zircon provenance, Crixas Greenstone Belt, Goias-Brasil: Gold-bearing vs barren siliciclastic rocks	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Crixas greenstone belt; Detrital zircon; U-Pb dating; Provenance analysis; Gold deposit	MARA ROSA ARC; TOCANTINS PROVINCE; SM-ND; TECTONIC EVOLUTION; GEOCHRONOLOGY; DEPOSIT; ORTHOGNEISSES; CONSTRAINTS; OCCURRENCES; CYCLE	The Crixas Greenstone Belt, located in an Archean-Paleoproterozoic terrane within the Neoproterozoic Tocantins Province, hosts an important gold deposit in Brazil with an endowment of 7 Moz currently operated by AngloGold Ashanti. Its stratigraphy is composed of an Archean komatiite and basalt basal sequence followed by a Paleoproterozoic sedimentary sequence composed of carbonaceous phyllites, dolomite-rich marbles with minor siliciclastic lenses (Ribeirao das Antas Formation) followed by a uniform siliciclastic sequence (Corrego Geral Formation). At the mining area, the entire sequence is stratigraphically overturned and metamorphosed under greenschist to lower amphibolite facies conditions. The orebodies are structurally controlled by thin-skinned lowangle thrust faults, and are mainly hosted by the sedimentary sequence in dilation zones named locally, from the shallowest to the deepest, as Structure Palmeiras, Structure IV and Structure III. The gold mineralization occurs in association with disseminated sulfides, massive sulfide lenses or quartz veins. Structure III is the deepest mineralized structure with gold mostly occurring in quartz veins cutting carbonaceous phyllites. Siliciclastic lenses occurring within the Structure III interval show variable gold grades, while siliciclastic rocks from the uniform deeper sequence just below Structure III are barren. The chronology of the sedimentary deposition, metamorphism and mineralization is still poorly understood. Detailed drill core logging, petrography and U-Pb geochronology of detrital zircons from siliciclastic rocks were carried out in order to better understand the relationship between the two metasedimentary packages and gold distribution. Petrographically there are no relevant differences between Au-bearing siliciclastic rocks (Ribeirao das Antas Formation) and barren siliciclastic rocks (Corrego Geral Formation), except for the presence of sulfides in the former. The new dataset of detrital zircon U-Pb ages revealed a ubiquitous Paleoproterozoic peak in all samples, with nearly no Archean contribution. K-feldspar and lithic angular fragments, zircons with low to medium roundness, and the U-Pb results indicate a Rhyacian provenance from a proximal source. Neoproterozoic overgrowths are found on detrital zircons from the barren siliciclastic interval of the Corrego Geral Formation, providing unequivocal evidence of a Neoproterozoic event around 600 Ma that affected the rocks. The Neoproterozoic partial reset, possibly related to the overriding of the Mara Rosa Magmatic Arc onto the Crixas Greenstone Belt, is unlikely to be linked to the mineralization considering that zircons from the barren rocks are the most thermally affected by this event. The Au mineralization is more likely related to Paleoproterozoic events, a time period known as a major global episode of orogenic gold deposit formation.	[Ferreira, Bruna Fiscuk; Marques, Juliana Chara; Frantz, Jose Carlos; Padilha, Nicole Lopes] Univ Fed Rio Grande do Sul, Inst Geociencias, Lab Modelagem Recursos Nat, Av Bento Goncalves,9500,Predio 43129-2 Andar, BR-91501970 Porto Alegre, RS, Brazil; [Ferreira, Bruna Fiscuk; Marques, Juliana Chara; Frantz, Jose Carlos] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves,9500,Predio 43113-207, BR-91501970 Porto Alegre, RS, Brazil; [de Souza, Renan Guilherme; Campos, Marcelo Pereira; Antoniazzi de Rezende Figueiredo, Frederico Lana] AngloGold Ashanti Ltd, Unidade Serra Grande, Rodovia GO-336,97000 Km 97, BR-76510000 Crixas, Go, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Marques, JC (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Lab Modelagem Recursos Nat LERN, Av Bento Goncalves,9500,Predio 43129-2 Andar, BR-91501970 Porto Alegre, RS, Brazil.	juliana.marques@ufrgs.br; jose.frantz@ufrgs.br	Ferreira, Bruna/HZJ-4183-2023; Marques, Juliana C/R-1965-2018; FRANTZ, JOSE C/R-1953-2018	Marques, Juliana C/0000-0003-0143-6925; FRANTZ, JOSE C/0000-0002-8890-7250; Ferreira, Bruna/0000-0001-6953-9213; Padilha, Nicole/0000-0003-1952-4122; de Souza, Renan/0000-0001-8925-0943	AngloGold Ashanti (Serra Grande-Brazil) through the R&D Cooperation Agreement ("Metallogeny and Geochronology of the Crixas Greestone Belt Gold District-GO" project) under UFRGS; CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) [309519/2018-7]; CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) [1770107]	AngloGold Ashanti (Serra Grande-Brazil) through the R&D Cooperation Agreement ("Metallogeny and Geochronology of the Crixas Greestone Belt Gold District-GO" project) under UFRGS; CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work is part of the Msc. dissertation of Bruna Fiscuk developed at the PPGGeo/UFRGS (Programa de Pos-Graduacao em Geoci <^>encias/Universidade Federal do Rio Grande do Sul). The authors gratefully acknowledge support from AngloGold Ashanti (Serra Grande-Brazil) through the R&D Cooperation Agreement ("Metallogeny and Geochronology of the Crixas Greestone Belt Gold District-GO" project) under development at UFRGS. The authors would like to thank former chief of exploration Bruno Araujo dos Santos and former general manager Diogo Afonso Costa, from AngloGold Ashanti (Serra Grande-Brazil), for geological discussions and for idealizing the R&D Cooperation Agreement. We also acknowledge Prof. Miguel Angelo Stipp Basei for his support on U-Pb dating at the Centro de Pesquisas Geocronologicas/Universidade de Sao Paulo, Mark Badham for proofreading the manuscript, Benedicte Kifumbi and Gabriel Bertolini for geological discussions and helping with figures. JCM acknowledges the CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) for her research fellow support (grant 309519/2018-7) and BF thanks CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) for her scholarship (grant 1770107). The authors are also grateful to the anonymous reviewers for their suggestions to improve de manuscript.	Arndt N.T., 1989, CONTR MINERAL PETROL, V74, P549; Aurifera Mineralizacao, 2006, THESIS U FEDERAL RIO; Blum M.L.B., 1996, 1 S ARCH TERR S AM P, P33; Castoldi M.A.S., 2018, THESIS; Cawood PA, 2012, GEOLOGY, V40, P875, DOI 10.1130/G32945.1; Cordeiro PFD, 2017, PRECAMBRIAN RES, V298, P403, DOI 10.1016/j.precamres.2017.06.021; Cordeiro PFD, 2014, PRECAMBRIAN RES, V251, P49, DOI 10.1016/j.precamres.2014.06.002; DESABOIA LA, 1983, PRECAMBRIAN RES, V22, P23, DOI 10.1016/0301-9268(83)90057-8; Filgueiras BD, 2020, J S AM EARTH SCI, V103, DOI 10.1016/j.jsames.2020.102739; Fortes P.T.F.O., 1997, INT GEOL REV, V39, P449; Fortes P.T.F.O., 1996, THESIS; Fortes PDFD, 2003, J S AM EARTH SCI, V16, P503, DOI 10.1016/j.jsames.2003.07.001; Fuck RA, 2014, PRECAMBRIAN RES, V244, P53, DOI 10.1016/j.precamres.2013.12.003; Gehrels G, 2014, ANNU REV EARTH PL SC, V42, P127, DOI 10.1146/annurev-earth-050212-124012; Giustina MESD, 2009, GEOL SOC SPEC PUBL, V323, P255, DOI 10.1144/SP323.12; Goldfarb RJ, 2017, ECON GEOL, V112, P123; Goldfarb RJ, 2010, ECON GEOL, V105, P459, DOI 10.2113/gsecongeo.105.3.459; Goldfarb RJ, 2001, ORE GEOL REV, V18, P1, DOI 10.1016/S0169-1368(01)00016-6; Hastie ECG, 2018, ORE GEOL REV, V94, P24, DOI 10.1016/j.oregeorev.2018.01.016; Jackson SE, 2004, CHEM GEOL, V211, P47, DOI 10.1016/j.chemgeo.2004.06.017; Jost H, 2001, MINER DEPOSITA, V36, P358, DOI 10.1007/s001260100171; JOST H, 1991, J S AM EARTH SCI, V4, P201, DOI 10.1016/0895-9811(91)90031-F; Jost H., 1995, REV BRAS GEOCIENCIAS, V25, P51; Jost H., 1993, REV BRASIL GEOCIENC, V23, P352; Jost H., 2011, CONTRIBUICOES METALO, V1, P27; Jost H., 2001, J BRAZIL EARTH SCI, V31, P315; Jost H, 2019, J S AM EARTH SCI, V96, DOI 10.1016/j.jsames.2019.102329; Jost H, 2013, J S AM EARTH SCI, V47, P201, DOI 10.1016/j.jsames.2013.07.002; Jost H, 2010, ORE GEOL REV, V37, P127, DOI 10.1016/j.oregeorev.2010.01.003; Junges SL, 2002, PRECAMBRIAN RES, V117, P101, DOI 10.1016/S0301-9268(02)00077-3; Lawley CJM, 2015, ECON GEOL, V110, P1425, DOI 10.2113/econgeo.110.6.1425; Ludwig K. 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South Am. Earth Sci.	JAN	2021	105								102994	10.1016/j.jsames.2020.102994	http://dx.doi.org/10.1016/j.jsames.2020.102994			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PQ8NR					2023-06-23	WOS:000606800700002
J	Loureiro, PO; Koester, E; Weinberg, RF; Lenz, C; Porcher, CC; Ramos, RC; Vieira, DT; Bastos, VA; Knijnik, D; Pimentel, MM				Loureiro, Paula O.; Koester, Edinei; Weinberg, Roberto F.; Lenz, Cristine; Porcher, Carla C.; Ramos, Rodrigo C.; Vieira, Daniel T.; Bastos, Vivianne A.; Knijnik, Daniel; Pimentel, Marcio M.			Recycling and hybridization of incremental episodes of magma intrusions: Pinheiro Machado Complex, Southeastern Dom Feliciano Belt, Brazil Paula	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Dom Feliciano Belt; Pinheiro Machado Complex; Magmatic recycling; Hybridization; Long-lived batholiths; Water-fluxed melting	LA-ICP-MS; U-PB; ZIRCON GEOCHRONOLOGY; TECTONIC EVOLUTION; PELOTAS BATHOLITH; LADAKH BATHOLITH; PORONGOS COMPLEX; SOUTHERN BRAZIL; SIERRA-NEVADA; SHEAR ZONE	The Pinheiro Machado Complex extends for over 10,000 km(2) as part of the Brasiliano-age Dom Feliciano Belt in Rio Grande do Sul, Brazil. In the Monte Bonito region, the complex is exposed in three quarries, which record multiple and complex magmatic structures revealing competing magmatic processes. Older magmatic rocks are eroded by younger ones, evidenced by several stages of disaggregation of magmatic xenoliths into fragments and schlieren, and by their deformation by ductile dragging. Hybridization is evidenced by mafic microgranular enclaves in granitic rocks close to contacts with diorite intrusions, and by diffuse, gradational boundaries between different magma mafic and felsic batches. Syenogranites represent the latest magma intrusion episode and recycle host mushes and rocks intruded earlier. In this process, zircons were recycled forming antecrysts. Finally, as the body evolved, some rocks underwent anatexis evidenced by patchy leucosomes with peritectic hornblende and/or titanite or magnetite, sometimes forming stictolithic or fleck texture. U-Pb SHRIMP ages obtained for zircons from an early diorite and a late-intrusive magnetite granite yielded crystallization ages of 616 +/- 3 Ma and 608 +/- 4 Ma, respectively. High U zircon rims yield Concordia ages around 600 Ma in both rock types, which can be related to crystallization of highly fractionated melts, late anatexis evidenced for example by fleck texture in rocks of both stages, or Pb loss. Thus, the geology and magma crystallization ages obtained for the Monte Bonito region of the Pinheim Machado Complex indicate that batholith growth was punctuated by intervals of melt influx separated by periods of relative quiescence. The magmatic structures resulted from a variety of recycling and hybridization processes, that evolved as a function of changing rheological contrasts between intruding magmas and previously intruded batches at different stages of crystallization.	[Loureiro, Paula O.; Vieira, Daniel T.; Bastos, Vivianne A.; Knijnik, Daniel] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Ave Bento Goncalves,9500,Campus Vale, BR-91570900 Porto Alegre, RS, Brazil; [Koester, Edinei; Porcher, Carla C.] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Geol, Ave Bento Goncalves,9500,Campus Vale, BR-91570900 Porto Alegre, RS, Brazil; [Weinberg, Roberto F.] Monash Univ, Sch Earth Atmosphere & Environm, Clayton, Vic 3800, Australia; [Lenz, Cristine] Univ Fed Sergipe, Dept Geol, Cidade Univ Prof Jose Aloisio de Campos, BR-49100000 Aracaju, SE, Brazil; [Ramos, Rodrigo C.] Secretaria Meio Ambiente & Preservacao Ecol, Ave Joao Correa 808, BR-93800222 Sapiranga, RS, Brazil; [Pimentel, Marcio M.] Univ Brasilia, Inst Geociencias, Geochronol Lab, ICC Ctr Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Monash University; Universidade Federal de Sergipe; Universidade de Brasilia	Loureiro, PO (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Ave Bento Goncalves,9500,Campus Vale, BR-91570900 Porto Alegre, RS, Brazil.	paulageoufrgs@gmail.com	Koester, Edinei/L-3684-2017; Porcher, Carla C/R-1419-2018	Koester, Edinei/0000-0002-4424-4782; Porcher, Carla C/0000-0002-0418-3954; Andrade Bastos, Vivianne/0000-0002-4460-5285; Chaves Ramos, Rodrigo/0000-0001-7116-5062; Vieira, Daniel/0000-0003-0616-5407	Programa de Posgraduacao em Geociencias (PPGGeo) of the Universidade Federal do Rio Grande do Sul (UFRGS); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [307378/2017-9]	Programa de Posgraduacao em Geociencias (PPGGeo) of the Universidade Federal do Rio Grande do Sul (UFRGS); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We appreciate the institutional support of the Programa de Posgraduacao em Geociencias (PPGGeo) of the Universidade Federal do Rio Grande do Sul (UFRGS) and the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for the financial support (process: 307378/2017-9). 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South Am. Earth Sci.	JAN	2021	105								102922	10.1016/j.jsames.2020.102922	http://dx.doi.org/10.1016/j.jsames.2020.102922			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PR9GU					2023-06-23	WOS:000607539900002
J	Severino, HGD; Pinto, CBD; Spigolon, ALD; de Mello, CSB; da Silva, TF; Leal, KZ				Severino, Hemmely Guilhermond de Souza; Pinto, Christiane Beatrice Duyck; Spigolon, Andre Luiz Durante; Mello, Carlos Siqueira Bandeira de; Silva, Tais Freitas da; Leal, Katia Zaccur			EVALUATION OF THE CHEMICAL COMPOSITION AND STRUCTURE OF ASPHALTENES FROM THREE OFFSHORE BRAZILIAN BIODEGRADED HEAVY OILS	QUIMICA NOVA			English	Article						asphaltene; heavy oil; biodegradation; occluded hydrocarbon	TRACE-ELEMENTS; CRUDE OILS; FRACTIONS; PYROLYSIS; GAS; N-ALK-1-ENES; PORPHYRINS; BIOMARKERS; PRODUCTS; ORIGIN	Asphaltenes fractions were extracted and purified from three heavy Brazilian oils. Their mass compositions of C, H, N, Ni and V were obtained from elemental analysis and S and O atomic percentages from EDS. The H/C ratios showed high degree of unsaturation, while the O atomic percentages indicated more pronounced biodegradation effects on two samples. Quantitative data on N, Ni, and V and semi-quantitative data on S were related to oils origins. The structural data of asphaltenes were explored by combining Fourier transform infrared spectroscopy (FTIR) and proton nuclear magnetic resonance (1H NMR). The oil with the lower degree of biodegradation contained asphaltenes with a lower level of condensed aromatic rings and longer aliphatic chain substituents. The asphaltenes obtained from the two most biodegraded oils showed similarities of polar groups and the presence of carboxylic functions, as well as lower contents of aliphatic substituents. The quality and quantity of occluded hydrocarbons were assessed after the mild oxidation of the separated asphaltenes fractions. It was suggested that the severe biodegradation which altered these structures may also be responsible to affect their occluded hydrocarbons.	[Severino, Hemmely Guilhermond de Souza; Pinto, Christiane Beatrice Duyck; Leal, Katia Zaccur] Univ Fed Fluminense, Inst Quim, BR-24020141 Niteroi, RJ, Brazil; [Spigolon, Andre Luiz Durante; Mello, Carlos Siqueira Bandeira de] Ctr Pesquisa Leopoldo Amer Miguez Mello, BR-21941915 Rio De Janeiro, RJ, Brazil; [Silva, Tais Freitas da] Univ Fed Rio Grande do Sul, Inst Geociencias, BR-90650001 Porto Alegre, RS, Brazil	Universidade Federal Fluminense; Universidade Federal do Rio Grande do Sul	Severino, HGD (autor correspondente), Univ Fed Fluminense, Inst Quim, BR-24020141 Niteroi, RJ, Brazil.	hemmelyguilhermond@id.uff.br	Duyck, Christiane/AEJ-1818-2022; Guihermond, Hemmely/AAD-2304-2022	Duyck, Christiane/0000-0002-2837-4173; Guilhermond, Hemmely/0000-0003-0375-6092	National Research Council of Brazil (CNPq); Research and Development Center of Petrobras (CENPES); Petroleum National Agency (ANP)	National Research Council of Brazil (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Research and Development Center of Petrobras (CENPES); Petroleum National Agency (ANP)	The authors thank the National Research Council of Brazil (CNPq) for the grants, and the Research and Development Center of Petrobras (CENPES) and Petroleum National Agency (ANP) for all financial support. Special thanks to D. J. Miller, S. M. C. de Menezes and L. S. Chinelatto Jr from CENPES, for their valuable contribution.	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G., 2014, CHEM TECHNOLOGY PETR; Spigolon A. L. D., 2016, ASPHALTENES FUNDAMEN; van Bree LGJ, 2014, GEOCHIM COSMOCHIM AC, V145, P89, DOI 10.1016/j.gca.2014.08.035; Yang CP, 2009, ENERG FUEL, V23, P820, DOI 10.1021/ef8007294; Zhao J, 2010, APPL GEOCHEM, V25, P1330, DOI 10.1016/j.apgeochem.2010.06.003	50	0	0	3	10	SOC BRASILEIRA QUIMICA	SAO PAULO	CAIXA POSTAL 26037, 05599-970 SAO PAULO, BRAZIL	0100-4042	1678-7064		QUIM NOVA	Quim. Nova		2021	44	4					391	401		10.21577/0100-4042.20170697	http://dx.doi.org/10.21577/0100-4042.20170697			11	Chemistry, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	TJ4OM		gold, Green Published			2023-06-23	WOS:000673462900002
S	Zvirtes, G; Hurst, A; Philipp, RP; Palladino, G; Grippa, A		Silcock, S; Huuse, M; Bowman, M; Hurst, A; Cobain, S		Zvirtes, G.; Hurst, A.; Philipp, R. P.; Palladino, G.; Grippa, A.			The Tumey Giant Injection Complex, Tumey Hill, California (USA)	SUBSURFACE SAND REMOBILIZATION AND INJECTION	Geological Society Special Publication		English	Article; Book Chapter							SANDSTONE INTRUSIONS INSIGHTS; DOMENGINE FORMATION EOCENE; SAN-JOAQUIN BASIN; SEDIMENTARY BASINS; INTERNAL STRUCTURES; NORTH-SEA; EMPLACEMENT; EVOLUTION; GEOMETRY; VALLEY	The Tumey Giant Injection Complex (TGIC) is a regionally developed sandstone intrusion complex emplaced into the deep-water Kreyenhagen Shale (Eocene) in the San Joaquin Basin, Central California. Detailed geological mapping, stratigraphic reconstruction and outcrop description, supported by structural analysis, allowed the architectural characterization of the TGIC. The complex is described as two main stratigraphically constrained intervals: (1) a lower interval (250 m thick) emplaced into clay-rich mudrock, consisting dominantly of sills with stepped and multilayered geometry; and (2) an upper interval (200 m thick) characterized by injection breccia and large wing-like intrusions (c. 600 m width x 100 m high) emplaced within predominantly biosiliceous mudrock strata. The intrusions in both intervals were derived from turbiditic channel fills intensely modified by sand fluidization. Sandstone intrusions and fractures affecting host strata are dominantly oriented sub-parallel to the basin axis striking between NW-SE and N-S, mainly dipping to NE and forming asymmetric saucer-shaped intrusions, suggesting structurally driven hydraulic fracturing and sand emplacement. The absence of a deep aquifer and potential sand sources underlying the complex suggests a lateral contribution of fluid flow. The TGIC occurs at a scale similar to injection complexes recognized in the subsurface and is a valuable reservoir analogue for hydrocarbon accumulations associated with sand injectites.	[Zvirtes, G.; Hurst, A.; Palladino, G.; Grippa, A.] Univ Aberdeen, Sch Geosci, Dept Geol & Petr Geol, Aberdeen AB24 3FX, Scotland; [Zvirtes, G.] Univ Fed Rio Grande do Sul, Geosci Postgrad Program PPGGEO, AV Bento Goncalves, BR-9500 Porto Alegre, RS, Brazil; [Philipp, R. P.] Univ Fed Rio Grande do Sul, Dept Mineral & Petr, AV Bento Goncalves, BR-9500 Porto Alegre, RS, Brazil; [Palladino, G.] Univ Basiicata, Dipartimento Sci, Potenza, Italy	University of Aberdeen; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Zvirtes, G (autor correspondente), Univ Aberdeen, Sch Geosci, Dept Geol & Petr Geol, Aberdeen AB24 3FX, Scotland.; Zvirtes, G (autor correspondente), Univ Fed Rio Grande do Sul, Geosci Postgrad Program PPGGEO, AV Bento Goncalves, BR-9500 Porto Alegre, RS, Brazil.	zvirtes.gustavo@gmail.com		Zvirtes, Gustavo/0000-0001-9728-0464	Shell Brazil; National Council for Scientific and Technological Development (CNPq)	Shell Brazil; National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	GZ is grateful to the Shell Brazil and the National Council for Scientific and Technological Development (CNPq) for funding.	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Soc. Spec. Publ.		2021	493						181	214		10.1144/SP493-2019-3	http://dx.doi.org/10.1144/SP493-2019-3			34	Geochemistry & Geophysics; Geology	Book Citation Index– Science (BKCI-S)	Geochemistry & Geophysics; Geology	BS7DC		Green Accepted			2023-06-23	WOS:000759073400011
J	Uhlein, GJ; Caxito, FA; Frei, R; Uhlein, A; Sial, AN; Dantas, EL				Uhlein, Gabriel J.; Caxito, Fabricio A.; Frei, Robert; Uhlein, Alexandre; Sial, Alcides N.; Dantas, Elton L.			Microbially induced chromium isotope fractionation and trace elements behavior in lower Cambrian microbialites from the Jaiba Member, Bambui Basin, Brazil	GEOBIOLOGY			English	Article						carbonate sedimentology; chemostratigraphy; metal reduction; microbial metabolism; rare earth elements	RARE-EARTH-ELEMENTS; SAO FRANCISCO CRATON; CR(VI) REDUCTION; HEXAVALENT CHROMIUM; ORGANIC-MATTER; IRON; SEAWATER; GEOCHEMISTRY; REE; CARBONATES	In east-central Brazil, the Ediacaran-Cambrian Bambui Basin has the potential to provide a record of unique geochemical responses of Earth's ocean and atmosphere evolution during this key time interval. From this perspective, we studied an interval of the upper Bambui Basin using sedimentologic, stratigraphic, and chemostratigraphic tools. The lower Cambrian Jaiba Member of the uppermost Serra da Saudade Formation is an interval of up to 60 m-thick of carbonate rocks disposed into two shallowing upward trends. Inner to outer ramp and high-energy shoal deposits are described, in which laminated microbialites are the prevailing sedimentary facies. REE + Y data suggest contamination by iron (oxy)hydroxides that are dissociated from the riverine detritic flux. Sedimentary iron enrichment may be related to the settling of iron nanoparticles in coastal environments, diagenetic iron mobilization, or both. MREE enrichment is caused by microbial degradation of organic matter in the iron reduction zone during the anoxic early-diagenetic stage. Chromium isotopes yielded negatively fractionated values (delta Cr-53 = -0.69 to -0.27 parts per thousand), probably resulting from biotic and abiotic reduction of dissolved Cr(VI) to light and less toxic Cr(III) within pores of microbial mats. The delta Cr-53 data of the Jaiba microbialite are thus a product of metabolic reactions in microbial mats and do not reflect seawater signal. The isotopic offset from seawater is feasible from molecular diffusion of Cr into pore water and reduction reactions occurring deep inside the mat, although the exact mechanism and consequences are not yet fully understood due to the poor preservation of metabolic reactions in the geological record. Our study suggests that Cr isotopes can be used to reconstruct Cr and other metals cycling within ancient microbial mats, and that caution should be taken when using past microbialites to infer seawater Cr records and redox state of the atmosphere and ocean.	[Uhlein, Gabriel J.; Caxito, Fabricio A.; Uhlein, Alexandre] Univ Fed Minas Gerais, Inst Geociencias, Ctr Pesquisas Manoel Teixeira Costa, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Frei, Robert] Univ Copenhagen, Dept Geosci & Nat Resource Management, Copenhagen, Denmark; [Sial, Alcides N.] Univ Fed Pernambuco, NEG LABISE, Dept Geol, Recife, PE, Brazil; [Dantas, Elton L.] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil	Universidade Federal de Minas Gerais; University of Copenhagen; Universidade Federal de Pernambuco; Universidade de Brasilia	Uhlein, GJ (autor correspondente), Univ Fed Minas Gerais, Inst Geociencias, Ctr Pesquisas Manoel Teixeira Costa, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.	guhlein@ufmg.br	Sial, Alcides/AAD-1901-2021; Caxito, Fabricio A/J-1317-2016; Dantas, Elton Luiz/AAK-8464-2021; Frei, Robert/N-6798-2014	Caxito, Fabricio A/0000-0002-0335-3667; Dantas, Elton Luiz/0000-0002-7954-5059; Frei, Robert/0000-0001-7708-9881; Uhlein, Gabriel/0000-0001-8988-3783	Fundacao de Amparo a Pesquisa do Estado de Minas Gerais [Serra-1912-31510]; Styrelsen for Forskning og Innovation [APQ-0091414, APQ-01711-14, PPM-00618-18]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [11-103378];  [303566/2019-1];  [447449/2014-1]	Fundacao de Amparo a Pesquisa do Estado de Minas Gerais(Fundacao de Amparo a Pesquisa do Estado de Minas Gerais (FAPEMIG)); Styrelsen for Forskning og Innovation; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); ; 	Instituto Serrapilheira, Grant/Award Number: Serra-1912-31510; Fundacao de Amparo a Pesquisa do Estado de Minas Gerais, Grant/Award Number: APQ-0091414, APQ-01711-14 and PPM-00618-18; Styrelsen for Forskning og Innovation, Grant/Award Number: 11-103378; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, Grant/Award Number: 303566/2019-1 and 447449/2014-1	Alibo DS, 1999, GEOCHIM COSMOCHIM AC, V63, P363, DOI 10.1016/S0016-7037(98)00279-8; BACON MP, 1988, PHILOS T R SOC A, V325, P147, DOI 10.1098/rsta.1988.0048; Bae WC, 2000, J MICROBIOL, V38, P36; Basu A, 2014, GEOCHIM COSMOCHIM AC, V142, P349, DOI 10.1016/j.gca.2014.07.024; BAU M, 1995, CHEM ERDE-GEOCHEM, V55, P1; Bau M, 1996, PRECAMBRIAN RES, V79, P37, DOI 10.1016/0301-9268(95)00087-9; Bauer KW, 2019, CHEM GEOL, V529, DOI 10.1016/j.chemgeo.2019.119286; Bayon G, 2004, EARTH PLANET SC LETT, V224, P477, DOI 10.1016/j.epsl.2004.05.033; Benitez-Nelson CR, 2000, EARTH-SCI REV, V51, P109, DOI 10.1016/S0012-8252(00)00018-0; Berger A, 2014, GEODERMA, V213, P521, DOI 10.1016/j.geoderma.2013.09.004; Bolhar R, 2007, PRECAMBRIAN RES, V155, P229, DOI 10.1016/j.precamres.2007.02.002; Bonnand P, 2013, EARTH PLANET SC LETT, V382, P10, DOI 10.1016/j.epsl.2013.09.001; Bonnand P, 2011, J ANAL ATOM SPECTROM, V26, P528, DOI 10.1039/c0ja00167h; Brandes JA, 1997, GEOCHIM COSMOCHIM AC, V61, P1793, DOI 10.1016/S0016-7037(97)00041-0; Bruggmann S, 2020, MINERALS-BASEL, V10, DOI 10.3390/min10100928; BURNE R V, 1987, Palaios, V2, P241, DOI 10.2307/3514674; CANFIELD DE, 1993, GEOCHIM COSMOCHIM AC, V57, P3867, DOI 10.1016/0016-7037(93)90340-3; Castanier S, 2000, MICROBIAL SEDIMENTS, P32; Caxito FA, 2018, CHEM GEOL, V481, P119, DOI 10.1016/j.chemgeo.2018.02.007; Caxito FA, 2016, PRECAMBRIAN RES, V282, P97, DOI 10.1016/j.precamres.2016.07.001; Caxito FD, 2012, PRECAMBRIAN RES, V200, P38, DOI 10.1016/j.precamres.2012.01.005; CAXITO FD, 2012, REV BRAS GEOCIENC, V42, P523; CHAFETZ H S, 1992, Palaios, V7, P277, DOI 10.2307/3514973; Charette MA, 2005, GEOCHIM COSMOCHIM AC, V69, P2095, DOI 10.1016/j.gca.2004.10.024; Chasse M, 2017, GEOCHEM PERSPECT LET, V3, P105, DOI 10.7185/geochemlet.1711; Chiavegatto J. 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Environmental Sciences & Ecology; Geology	QG1IC	33347697				2023-06-23	WOS:000600508100001
J	Gerolin, CR; Pupim, FN; Sawakuchi, AO; Grohmann, CH; Labuto, G; Semensatto, D				Gerolin, Cristiano Rezende; Pupim, Fabiano Nascimento; Sawakuchi, Andre Oliveira; Grohmann, Carlos Henrique; Labuto, Georgia; Semensatto, Decio			Microplastics in sediments from Amazon rivers, Brazil	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Microplastics pollution; River sediment; Amazon	POLLUTION; CONTAMINATION; PARTICLES; INGESTION; FISHES	We assessed the concentrations of microplastics in sediment samples collected in seven sites from Solimoes, Negro and Amazon rivers, upstream and downstream the metropolitan region of Manaus. Concentrations ranged from 417 to 8178 particles/kg of dried sediment (microplastics: 0.063-5 mm), and from 0 to 5725 particles/kg of dried sediment (microplastics: 0.063-1 mm). The highest microplastics concentrations were observed in samples from shallow water (water depth of 5-7 m) sites with lower water velocity of the Negro river surrounding Manaus, and the lowest concentration in farthest sample collected in deeper zone (water depth of 34 m) of the Amazon river around 110 km downstream Manaus. The variation of microplastics concentrations within the studied area can be related to hydraulic characteristics defining the erosive-depositional behavior of the sampling sites and their proximity to Manaus. Our results represent the first report to show the ubiquitous presence and widespread distribution of microplastics in sediments from the lower Solimoes, lower Negro and upper Amazon rivers. (C) 2020 Elsevier B.V. All rights reserved.	[Gerolin, Cristiano Rezende; Labuto, Georgia; Semensatto, Decio] Univ Fed Sao Paulo Unifesp, Lab Integrated Sci LabInSci, BR-09972270 Diadema, SP, Brazil; [Pupim, Fabiano Nascimento; Semensatto, Decio] Univ Fed Sao Paulo Unifesp, Dept Environm Sci, BR-09972270 Diadema, SP, Brazil; [Sawakuchi, Andre Oliveira] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, SP, Brazil; [Grohmann, Carlos Henrique] Univ Sao Paulo, Inst Energia & Ambiente, BR-05508010 Sao Paulo, SP, Brazil; [Labuto, Georgia] Univ Fed Sao Paulo Unifesp, Dept Chem, BR-09972270 Diadema, SP, Brazil	Universidade Federal de Sao Paulo (UNIFESP); Universidade Federal de Sao Paulo (UNIFESP); Universidade de Sao Paulo; Universidade de Sao Paulo; Universidade Federal de Sao Paulo (UNIFESP)	Semensatto, D (autor correspondente), Univ Fed Sao Paulo Unifesp, Lab Integrated Sci LabInSci, BR-09972270 Diadema, SP, Brazil.	decio.semensatto@unifesp.br	Sawakuchi, André O/D-1445-2013; Semensatto, Décio/AAD-4472-2020; Pupim, Fabiano N/J-7869-2012; Labuto, Geórgia/A-8796-2015; Grohmann, Carlos/A-9030-2008; Semensatto, Décio/A-6315-2008	Semensatto, Décio/0000-0002-4253-6351; Pupim, Fabiano N/0000-0001-7452-1376; Labuto, Geórgia/0000-0002-5403-8974; Grohmann, Carlos/0000-0001-5073-5572; Semensatto, Décio/0000-0002-4253-6351	Sao Paulo Research Foundation (FAPESP, Brazil) [2011/06609-1, 2014/23334-4, 2016/06271-4]; National Council for Scientific and Technological Development (CNPq, Brazil) [302411/2018-6, 304727/2017-2, 304413/2018-6]; Coordination of Superior Level Staff Improvement (CAPES, Brazil)	Sao Paulo Research Foundation (FAPESP, Brazil)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Council for Scientific and Technological Development (CNPq, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordination of Superior Level Staff Improvement (CAPES, Brazil)	Authors are grateful to Sao Paulo Research Foundation (FAPESP, Brazil) grants #2011/06609-1, #2014/23334-4 and 2016/06271-4. FNP, AOS and CHG are supported by National Council for Scientific and Technological Development (CNPq, Brazil) grants #302411/2018-6, #304727/2017-2 and #304413/2018-6. CRG is thankful for themaster's degree scholarship from Coordination of Superior Level Staff Improvement (CAPES, Brazil).	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Total Environ.	DEC 20	2020	749								141604	10.1016/j.scitotenv.2020.141604	http://dx.doi.org/10.1016/j.scitotenv.2020.141604			6	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	OG3MX	32829281				2023-06-23	WOS:000581793800090
J	Ribeiro, BV; Mulder, JA; Faleiros, FM; Kirkland, CL; Cawood, PA; O'Sullivan, G; Campanha, GAC; Finch, MA; Weinberg, RF; Nebel, O				Ribeiro, B., V; Mulder, J. A.; Faleiros, F. M.; Kirkland, C. L.; Cawood, P. A.; O'Sullivan, G.; Campanha, G. A. C.; Finch, M. A.; Weinberg, R. F.; Nebel, O.			Using apatite to resolve the age and protoliths of mid-crustal shear zones: A case study from the Taxaquara Shear Zone, SE Brazil	LITHOS			English	Article						Apatite dating; Muscovite dating; Mid-crustal shear zones; Trace element geochemistry; Ribeira Belt	TRACE-ELEMENT COMPOSITIONS; PLASMA-MASS SPECTROMETRY; DOM FELICIANO BELT; U-PB GEOCHRONOLOGY; DE-LA-PLATA; RIBEIRA BELT; 40AR/39AR AGES; WEST GONDWANA; KAOKO BELT; POSTOROGENIC TRANSITION	Shear zones accommodate strain and facilitate migration of hydrothermal fluid and magma through the crust. Unravelling the deformation history of shear zones requires correspondence between the closure temperature of mineral geochronometers and the temperature of deformation. Here, we adopt apatite U-Pb-trace element analysis as a tool for dating deformation and tracing the protoliths of mid-crustal shear zones through a case study of the Taxaquara Shear Zone (TSZ), a major transpressional shear zone in the southern Ribeira Belt of SE Brazil. Apatite from mylonites in the TSZ yield U-Pb ages of 558-536 Ma, considering uncertiainties, which slightly overlap with 40Ar/39Ar ages of 538 +/- 2 Ma from muscovite in the lower limit. The closure temperature of apatite is estimated at 500-460 degrees C, which is slightly higher than that estimated for syn-kinematic muscovite (445-420 degrees C). Apatite from shear zone mylonites has Sr/Y and LREE systematics typical of apatite from S- and I-type granitoids, suggesting the adjacent and undeformed Pilar do Sul and Piedade granites are the likely protoliths of the mylonites. This interpretation is supported by new U-Pb ages of ca. 605 Ma from prekinematic zircon and titanite from mylonites, which corresponds closely with new U-Pb apatite ages and previously published U-Pb monazites ages fromthe Pilar do Sul Granite. Wesuggest the U-Pb systemof apatite in the TSZ was reset via volume diffusion during rapid cooling given that it preserves the igneous geochemical signatures. Moreover, this interpretation is consistent with the lower apatite closure temperature (500-460 degrees C) relatively to the temperature of deformation (530-480 degrees C). The revised similar to 560-535 Ma age for the TSZ demonstrates that it post-dates the collisional phase of the Ribeira Belt (620-595 Ma and 595-565 Ma), indicating protracted strain accommodation during the Brasiliano-Pan African orogeny, and supports correlation with the 600-550Ma and 570-550 Ma transpressional Dom Feliciano and Kaoko Belts. This study demonstrates that apatite is a powerful tool for unravelling the history of mid-crustal shear zones as it is stable in a wide range of lithotypes, has trace element compositions that are sensitive to the environment of formation, and Pb closure temperatures typical of mid-crust conditions. U-Pb-trace element analysis of apatite provides a robustmeans to date shear zones that can be complimentary to, or independent of, more traditional 40Ar/39Ar analysis of mica or amphibole. (C) 2020 Elsevier B.V. All rights reserved.	[Ribeiro, B., V; Mulder, J. A.; Cawood, P. A.; Finch, M. A.; Weinberg, R. F.; Nebel, O.] Monash Univ, Sch Earth Atmosphere & Environm Sci, Clayton, Vic 3800, Australia; [Ribeiro, B., V; Faleiros, F. M.; Campanha, G. A. C.] Univ Sao Paulo, Dept Mineral & Geotecton, Rua Lago 562, BR-05508900 Sao Paulo, Brazil; [Kirkland, C. L.] Curtin Univ, Timescales Mineral Syst Grp, Ctr Explorat Targeting Curtin Node, Sch Earth & Planetary Sci, Perth, WA 6102, Australia; [O'Sullivan, G.] Univ Coll Dublin, UCD Sch Earth Sci, Dublin 4, Ireland; [Ribeiro, B., V] 9 Rainforest Walk, Clayton, Vic 3800, Australia	Monash University; Universidade de Sao Paulo; Curtin University; University College Dublin	Ribeiro, BV (autor correspondente), Monash Univ, Sch Earth Atmosphere & Environm Sci, Clayton, Vic 3800, Australia.; Ribeiro, BV (autor correspondente), 9 Rainforest Walk, Clayton, Vic 3800, Australia.	bruno.vieiraribeiro1@monash.edu	Vieira Ribeiro, Bruno/HOC-3421-2023; Faleiros, Frederico Meira/F-6138-2010; Nebel, Oliver/B-2694-2008	Vieira Ribeiro, Bruno/0000-0002-3652-1831; Faleiros, Frederico Meira/0000-0003-2199-8116; Cawood, Peter/0000-0003-1200-3826; Nebel, Oliver/0000-0002-5068-7117; Finch, Melanie/0000-0001-9699-2769	FAPESP (Sao Paulo Research Foundation) [2018/00320-9, 2018/16307-1, 2018/10012-0, 2015/03737-0]; CNPq [443439/2014-1, 305074/2015-6, 307732/2019-3]; Australian Research Council [FL160100168]	FAPESP (Sao Paulo Research Foundation)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Australian Research Council(Australian Research Council)	This work was supported by FAPESP (Sao Paulo Research Foundation) via postgraduate scholarships 2018/00320-9 and 2018/16307-1 to BVR, and research grants 2018/10012-0 to FMF and 2015/03737-0 to MAS Basei, CNPq grants 443439/2014-1, 305074/2015-6 to GACC and 307732/2019-3 to FMF and Australian Research Council grant FL160100168 to PAC. Ashlea Wainwright and Massimo Raveggi are thanked for the assistance with U-Pb and trace element analysis. GrahamHutchinson is thanked for assistancewith SEMimaging. Fred Jourdan is thanked for assistancewith 40Ar/39Ar and comments on an earlier version of thismanuscript. We greatly appreciate the constructive comments of Sebatian Oriolo and an anonymous reviewer and EditorMarco Scambelluri for efficient and helpful editorial handling.	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J	Trevisan, CL; Vicente, MC; Rocha, BCS; Wasserman, JC				Trevisan, Cleuza Leatriz; Vicente, Murilo Carvalho; Rocha, Bruno Cesar S.; Wasserman, Julio Cesar			Development of a Dredging Sensitivity Index, applied to an industrialized coastal environment in Brazil	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Sediment; Physico-chemical parameters; Biotic; Socioeconomic; Coastal management; Sepetiba Bay, Brazil	RIO-DE-JANEIRO; MULTICRITERIA DECISION-ANALYSIS; SEPETIBA BAY; CONTAMINATED SEDIMENTS; HEAVY-METALS; TRACE-ELEMENTS; MANAGEMENT; MANGROVE; QUALITY; ESTUARY	Ports link world commerce via maritime routes, and dredging services are essential to establish and maintain these connections. However, one question is critical when dredging is being considered: where are the best places to do it? To try to answer this question, a Dredging Sensitivity Index (DSI) was developed as a management tool to be used in project planning steps. In order to diminish environmental damages and quality-of-life losses, DSI provides alternatives by identifying sensitivity areas. This new methodology quantifies impacts caused by the sediment removal step and points out favorable areas to dredge, with a simple map. Parameters such as fine-grain content (% < 63 mu m), Acid Volatile Sulfides (AVS), Shannon-Wiener Index and fisheries, among others, were used to calculate the DSI. Formulas were used to weight and aggregate both, the parameters and the DSI itself. Sepetiba Bay was chosen to apply this methodology because of its relevant economic and environmental aspects. The methodology was applied to dredging situations, but it can be used to indicate areas for dredged material disposal, with a few modifications in the DSI formulas. A DSI map was a final result of this methodology, and showed that the northern portion of the bay, close to the littoral is a more sensitive area, where dredging should be avoided, or carried out very carefully. DSI is a very useful tool for reducing damages from dredging services, it contributes with zonation and it provides alternatives to decision-makers who manage these areas. (C) 2020 Elsevier B.V. All rights reserved.	[Trevisan, Cleuza Leatriz; Vicente, Murilo Carvalho; Rocha, Bruno Cesar S.; Wasserman, Julio Cesar] Univ Fed Fluminense, Inst Chem, Grad Programme Geochem, Outeiro Sao Joao Baptista S-N Ctr, BR-24020141 Niteroi, RJ, Brazil; [Wasserman, Julio Cesar] UFF Network Environm & Sustainable Dev, Inst Geosci, Suite 406 Ave Litoranea S-N, BR-24030346 Niteroi, RJ, Brazil	Universidade Federal Fluminense	Wasserman, JC (autor correspondente), Univ Fed Fluminense, Inst Chem, Grad Programme Geochem, Outeiro Sao Joao Baptista S-N Ctr, BR-24020141 Niteroi, RJ, Brazil.; Wasserman, JC (autor correspondente), UFF Network Environm & Sustainable Dev, Inst Geosci, Suite 406 Ave Litoranea S-N, BR-24030346 Niteroi, RJ, Brazil.	cltrevisan@id.uff.br; murilovicente@hotmail.com; brurocha@gmail.com; geowass@vm.uff.br	Wasserman, Julio Cesar/K-3863-2014; Wasserman, Julio/HGA-8235-2022	Wasserman, Julio Cesar/0000-0002-7828-5240; Wasserman, Julio/0000-0002-7828-5240; TREVISAN, CLEUZA/0000-0002-8632-4457; Vicente, Murilo/0000-0002-8520-308X	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, CNPq [302741/2017-8]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are thankful to Universidade Federal Fluminense and Geochemistry Department for the infrastructure. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -grant #001. JCWalso thanks Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, CNPq for his fellowship (grant #302741/2017-8).	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Total Environ.	DEC 15	2020	748								141294	10.1016/j.scitotenv.2020.141294	http://dx.doi.org/10.1016/j.scitotenv.2020.141294			12	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	OF2MX	33113704				2023-06-23	WOS:000581049800036
J	Utida, G; Cruz, FW; Santos, RV; Sawakuchi, AO; Wang, H; Pessenda, LCR; Novello, VF; Vuille, M; Strauss, AM; Borella, AC; Strikis, NM; Guedes, CCF; De Andrade, FRD; Zhang, HW; Cheng, H; Edwards, RL				Utida, Giselle; Cruz, Francisco W.; Santos, Roberto V.; Sawakuchi, Andre O.; Wang, Hong; Pessenda, Luiz C. R.; Novello, Valdir F.; Vuille, Mathias; Strauss, Andre M.; Borella, Ana Claudia; Strikis, Nicolas M.; Guedes, Carlos C. F.; Dias De Andrade, Fabio Ramos; Zhang, Haiwei; Cheng, Hai; Edwards, R. Lawrence			Climate changes in Northeastern Brazil from deglacial to Meghalayan periods and related environmental impacts	QUATERNARY SCIENCE REVIEWS			English	Article						Stable isotopes; ITCZ; Speleothems; Holocene; Northeastern Brazil; Archaeology; Demographic impacts	MONSOON; VEGETATION; ISOTOPES; FOREST; RECORD; SCALE	Changes in insolation driven by precession and obliquity are considered the major driver of tropical precipitation on orbital time scales, and responsible for vegetation and physical landscape changes during the Late Holocene over tropical South America. Here we investigate the environmental changes in the karst region of Chapada do Apodi - Northeastern Brazil (NEB), using a multi-proxy approach including carbon (delta C-13), oxygen (delta O-18) and strontium (Sr-87/Sr-86) isotopic analyses on speleothems from different caves, carbonate bedrock, and clastic cave deposits. This approach reveals that the balance between soil formation and erosion and their alternating impact on vegetation and precipitation changes occurred in response to variations in the position and intensity of the Intertropical Convergence Zone (ITCZ) over the region. The high delta C-13 and delta O-18 and low Sr-87/Sr-86 values at 4,200 yrs BP indicate a massive episode of soil erosion, resulting in the exposure of carbonate bedrocks over a large area of the karst terrain. This event marks the beginning of the Meghalayan chronozone, characterized as the aridification of this region, decline in soil production, drying out of underground drainages, and increased dominance of dry-adapted flora species, characteristic of a more open vegetation (caatinga). We investigated if the Holocene climatic changes affected human occupation in the NEB and found that the overall demographic course is virtually identical to the well-established curve characterized by population deflation during Middle Holocene. (C) 2020 Elsevier Ltd. All rights reserved.	[Utida, Giselle; Cruz, Francisco W.; Sawakuchi, Andre O.; Novello, Valdir F.; Dias De Andrade, Fabio Ramos] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508090 Sao Paulo, SP, Brazil; [Santos, Roberto V.] Univ Brasilia, Dept Geol, Brasilia, DF, Brazil; [Wang, Hong] Beijing Normal Univ, Interdisciplinary Res Ctr Earth Sci Frontier, Beijing, Peoples R China; [Pessenda, Luiz C. R.] Univ Sao Paulo, 14C Lab, Piracicaba, SP, Brazil; [Vuille, Mathias] SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY USA; [Strauss, Andre M.; Borella, Ana Claudia] Univ Sao Paulo, Museu Arqueol & Etnol, Sao Paulo, SP, Brazil; [Strikis, Nicolas M.] Univ Fed Fluminense, Dept Geoquim, Niteroi, RJ, Brazil; [Guedes, Carlos C. F.] Univ Fed Parana, Dept Geol, Curitiba, Parana, Brazil; [Zhang, Haiwei; Cheng, Hai] Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710054, Peoples R China; [Cheng, Hai] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China; [Cheng, Hai] Inst Karst Geol, Key Lab Karst Dynam, MLR, CAGS, Guilin 541004, Peoples R China; [Edwards, R. Lawrence] Univ Minnesota, Dept Earth Sci, Minneapolis, MN USA	Universidade de Sao Paulo; Universidade de Brasilia; Beijing Normal University; Universidade de Sao Paulo; State University of New York (SUNY) System; State University of New York (SUNY) Albany; Universidade de Sao Paulo; Universidade Federal Fluminense; Universidade Federal do Parana; Xi'an Jiaotong University; Chinese Academy of Sciences; Institute of Earth Environment, CAS; University of Minnesota System; University of Minnesota Twin Cities	Utida, G (autor correspondente), Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508090 Sao Paulo, SP, Brazil.	giselleutida@hotmail.com	Novello, Valdir F./P-5824-2015; Sawakuchi, André O/D-1445-2013; Guedes, Carlos Conforti Ferreira/F-3639-2015; Strauss, André M/K-4089-2015; CHENG, HAI/H-3413-2017	Novello, Valdir F./0000-0002-0120-3745; Guedes, Carlos Conforti Ferreira/0000-0001-8816-9174; Strauss, André M/0000-0002-2336-1381; CHENG, HAI/0000-0002-5305-9458; Ruiz Pessenda, Luiz Carlos/0000-0001-9119-8195; Utida, Giselle/0000-0002-7134-5220; Zhang, Haiwei/0000-0002-0855-1283	FAPESP, Brazil through PIRE NSF-FAPESP [2017/50085-3, 2020/02737-4, 2016/15807-5, 2017/16451-2, 2019/12981-2, 2019/15914-4]; NSF, United States [AGS-1303828, OISE-1743738, 1103403]; NSFC, China [NSFC 41888101]; CNPq, Brazil [423573/2018-7, 308769/2018-0]; CAPES, Brazil [88887.310301/2018-00]; CAPES; Directorate For Geosciences; Div Atmospheric & Geospace Sciences [1103403] Funding Source: National Science Foundation	FAPESP, Brazil through PIRE NSF-FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); NSF, United States(National Science Foundation (NSF)); NSFC, China(National Natural Science Foundation of China (NSFC)); CNPq, Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES, Brazil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Directorate For Geosciences; Div Atmospheric & Geospace Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We thank Christian Millo, Alyne Barros M. Lopes and Osmar Antunes (LES-IGc-USP, Brazil), and Luiz Mancini (LAIS-IGc-UNB, Brazil) for their support during the analyses, Andre Zular (IGc-USP, Brazil) for support during the field trip and grain-size analysis, Johan Etourneau (Universite de Bordeaux, France) for comments about this paper. We are grateful to Leda Zogbi for the Trapia cave map and to Professor Dr. Francisco Hilario Bezerra (UFRN, Brazil) and A.N.P., Brazil for aerial images, and Carlos Mazocca (IGc-USP, Brazil) for images editing. We thank Jocy Brandao Cruz, Diego de Medeiros Bento, Jose Iatagan Mendes de Freitas, Darcy Jose dos Santos, Uilson Paulo Campos (CECAV/RN), Antonio Idaelson do Nascimento and Geilson Goes Fernandes for all support in the field trip, information and data about the caves. This work was supported by the FAPESP, Brazil through PIRE NSF-FAPESP [2017/50085-3 to F.W.C], as well as the fellowships to G.U. [2020/02737-4]. V.F.N [2016/15807-5], A.S. [2017/16451-2] and A.C.B. [2019/12981-2], and the regular research grant [2019/15914-4 to A.S.]. The NSF, United States support through grants [AGS-1303828 and OISE-1743738] to MV and 1103403 to R.L.E and H.C. is acknowledged. The NSFC, China support through grant [NSFC 41888101] to H.C. is acknowledged. N.M.S. acknowledges the support of CNPq, Brazil [Grants 423573/2018-7; 308769/2018-0] and CAPES, Brazil [Grant 88887.310301/2018e00]. G.U. is grateful to CAPES for the PhD and PosDoc fellowships through the Programa de Pos-Graduacao em Geoquimica e Geotectonica at Universidade de Sao Paulo, Brazil.	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J	Leal-Alves, DC; Weschenfelder, J; Albuquerque, MD; Espinoza, JMD; Ferreira-Cravo, M; de Almeida, LPM				Leal-Alves, Deivid Cristian; Weschenfelder, Jair; Albuquerque, Miguel da Guia; de Almeida Espinoza, Jean Marcel; Ferreira-Cravo, Marlize; Melo de Almeida, Luis Pedro			Digital elevation model generation using UAV-SfM photogrammetry techniques to map sea-level rise scenarios at Cassino Beach, Brazil	SN APPLIED SCIENCES			English	Article						Coastal geomorphology; Unmanned aerial vehicle; Coastline benchmark; Climate change; Bathtub approach	GRANDE-DO-SUL; ATMOSPHERIC CONDITIONS; COASTAL; VULNERABILITY; TOPOGRAPHY; INUNDATION; EVOLUTION; BEHAVIOR; IMPACTS; SYSTEMS	The Cassino Beach is a low-lying coast with high inundation susceptibility in southern Brazil. To map this vulnerability, a low cost alternative to the increasingly employed fine-scale remote sensing is the employment of a digital camera coupled with unmanned aerial vehicle (UAV). However, this was only achieved through the adoption of photogram-metric principles and computational advances of structure-from-motion (SfM) algorithms. The study objectives were: a topographic reconstruction of the Cassino beach; an accurate digital terrain model (DTM) generation from the dense cloud classification; and inundation maps based on representative concentration pathway (RCP) scenarios from the Intergovernmental Panel on Climate Change using the bathtub approach. The primary input of the inundation model was a DTM with spatial resolution of 0.1294 m and an RMSE elevation of 0.0607 m. The high-resolution and vertical precision were appropriated to the bathtub approach, with the mapping identifying the exposed areas with the drowning potential correctly connected to the source. The inundation maps revealed that: in the 2046-2065 RCP scenario, the urban drowned area has varied between 37 and 41%; in the 2081-2100 RCP scenario, the urban drowned area has varied between 51 and 73%; and in the 2100 RCP scenario, the urban drowned area has varied between 54 and 82%. The bathtub modeling shows that low-lying coasts are highly susceptible to sea-level rise effects, and the use of UAV-SfM technology in the production of topographic data was suitable for the study area.	[Leal-Alves, Deivid Cristian; Weschenfelder, Jair] Univ Fed Rio Grande Sul UFRGS, Posgrad Geociencias, Ave Bento Goncalves,9500 Predio 43113 Sala 207, BR-91501970 Porto Alegre, RS, Brazil; [Albuquerque, Miguel da Guia] Inst Fed Educ Ciencia & Tecnol Rio Grande Sul IFR, Campus Rio Grande,Rua Engn Alfredo Huch 475, BR-96201460 Rio Grande, RS, Brazil; [de Almeida Espinoza, Jean Marcel] Inst Fed Educ Ciencia & Tecnol Santa Catarina IFS, Campus Cacador,Ave Fahdo Thome 3000, BR-89500000 Cacador, SC, Brazil; [Ferreira-Cravo, Marlize] Inst Fed Parana IFPR, Campus Paranagua,Rua Antonio Carlos Rodrigues 453, BR-83215750 Paranagua, Parana, Brazil; [Melo de Almeida, Luis Pedro] Univ Fed Rio Grande FURG, Ave Italia,Km 8 Bairro Carreiros, BR-96203900 Rio Grande, RS, Brazil	Universidade Federal do Rio Grande do Sul; Instituto Federal de Santa Catarina (IFSC); Instituto Federal do Parana; Universidade Federal do Rio Grande	Leal-Alves, DC (autor correspondente), Univ Fed Rio Grande Sul UFRGS, Posgrad Geociencias, Ave Bento Goncalves,9500 Predio 43113 Sala 207, BR-91501970 Porto Alegre, RS, Brazil.	dclealalves@gmail.com; jair.weschenfelder@ufrgs.br; miguel.albuquerque@riogrande.ifrs.edu.br; jean.espinoza@ifsc.edu.br; lizedomar@gmail.com; melolp@gmail.com	Ferreira-Cravo, Marlize/G-4119-2011; Alves, Deivid Cristian Leal/ABE-5453-2020; da Guia Albuquerque, Miguel/D-7762-2017; Albuquerque, Miguel/AAH-6952-2021; Weschenfelder, Jair/C-3390-2013	Ferreira-Cravo, Marlize/0000-0003-3319-3905; Alves, Deivid Cristian Leal/0000-0002-5255-123X; da Guia Albuquerque, Miguel/0000-0002-2063-492X; Albuquerque, Miguel/0000-0002-2063-492X; Weschenfelder, Jair/0000-0002-2075-4067; Almeida, Luis Pedro/0000-0001-7805-9086; Espinoza, Jean/0000-0002-7933-2897	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico-CNPQ [141939/2016-8]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico-CNPQ(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was supported by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico-CNPQ (141939/2016-8).	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Sci.	DEC 12	2020	2	12							2181	10.1007/s42452-020-03936-z	http://dx.doi.org/10.1007/s42452-020-03936-z			19	Multidisciplinary Sciences	Emerging Sources Citation Index (ESCI)	Science & Technology - Other Topics	PF1QL		Bronze			2023-06-23	WOS:000598837000001
J	Loureiro, AMS; da Paz, SPA; Angelica, RS				Silva Loureiro, Alexandre Maximo; Aranha da Paz, Simone Patricia; Angelica, Romulo Simoes			How to Estimate the Binder: Aggregate Ratio From Lime-Based Historic Mortars for Restoration?	FRONTIERS IN MATERIALS			English	Article						wet chemical Analysis; XRD; DSC; historic mortars; binder; aggregate ratio; brazilian mortars; old mortars; Rietveld Method	POWDER DIFFRACTION; ANCIENT MORTARS; CONSERVATION; BYZANTINE; VATERITE; CHURCH	One of the most important studies from historic mortars is the binder:aggregate ratio, which is usually obtained through wet chemical analysis. Instrumental techniques and benchtop equipment have become increasingly important tools in the characterization of historic materials. The analysis of such materials has become more practical, faster and more accurate, and the sample preparation methods require less and less material. Thus, this article aims to investigate the validity of the results obtained by some of the methods and techniques used in historic materials analysis and determine the possibility of estimating the binder:aggregate ratio with adequate accuracy and precision. For this purpose, historic mortars from Belem do Para, in northern Brazil, were selected, and the following quantification techniques were employed: wet chemical analysis, XRD, DSC and XRF. The results showed that the amounts of the components in the mortars could be quantified with the use of approximately 3 g of sample, thus providing one of the main pieces of information needed for the production of a restoration mortar: the binder:aggregate ratio.	[Silva Loureiro, Alexandre Maximo] Fed Univ Para, Inst Geosci, Lab Mineral Characterizat, Belem, Para, Brazil; [Silva Loureiro, Alexandre Maximo; Aranha da Paz, Simone Patricia; Angelica, Romulo Simoes] Fed Univ Para, Inst Technol, Lab Conservat Restorat & Rehabil, Belem, Para, Brazil	Universidade Federal do Para; Universidade Federal do Para	Loureiro, AMS (autor correspondente), Fed Univ Para, Inst Geosci, Lab Mineral Characterizat, Belem, Para, Brazil.; Loureiro, AMS (autor correspondente), Fed Univ Para, Inst Technol, Lab Conservat Restorat & Rehabil, Belem, Para, Brazil.	loureiro1@ufpa.br	Angélica, Rômulo/AAD-2612-2021; Angelica, Romulo/G-6245-2010	Angelica, Romulo/0000-0002-3026-5523; Loureiro, Alexandre/0000-0003-3341-2653	CAPES (Brazilian Federal Agency for Support and Evaluation of Graduate Education); CNPq (National Council for Scientific and Technological Development); Dean's Office for Graduate and Research Studies (Education) (Federal University of Para)	CAPES (Brazilian Federal Agency for Support and Evaluation of Graduate Education)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq (National Council for Scientific and Technological Development)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Dean's Office for Graduate and Research Studies (Education) (Federal University of Para)	The authors thank the Brazilian agencies CAPES (Brazilian Federal Agency for Support and Evaluation of Graduate Education) and CNPq (National Council for Scientific and Technological Development) for the doctoral scholarship granted to the first author of this article. We also thank the laboratories where the analyses were performed: a) the Mineral Characterization Laboratory (LCM) and b) the Conservation, Restoration and Rehabilitation Laboratory (LACORE). We thank Rosario Veiga (LNEC) for the critical reading of and contributions to the manuscript. We also thank DPHAC (Department of Historic, Artistic and Cultural Heritage of Para) for permission to collect the samples used in this study. The authors also thank the Dean's Office for Graduate and Research Studies (Education) (Federal University of Para) for funding the translation of the article through the Support Program for Translation and Publication of Brazilian Authors (PUBLIC NOTICE PAPQ 2019).	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S., 2010, RILEM PUBLICATIONS S, V6, P345; Loureiro AMS, 2020, CONSTR BUILD MATER, V233, DOI 10.1016/j.conbuildmat.2019.117284; Singh M, 2016, CONSTR BUILD MATER, V112, P386, DOI 10.1016/j.conbuildmat.2016.02.191; Theodoridou M, 2013, J ARCHAEOL SCI, V40, P3263, DOI 10.1016/j.jas.2013.03.027; Toby BH, 2006, POWDER DIFFR, V21, P67, DOI 10.1154/1.2179804; Velosa A. L., 2016, CINPAR 12 INT C STRU, P12	41	3	3	0	4	FRONTIERS MEDIA SA	LAUSANNE	AVENUE DU TRIBUNAL FEDERAL 34, LAUSANNE, CH-1015, SWITZERLAND	2296-8016			FRONT MATER	Front. Mater.	DEC 11	2020	7								597411	10.3389/fmats.2020.597411	http://dx.doi.org/10.3389/fmats.2020.597411			13	Materials Science, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Materials Science	PJ2HC		gold			2023-06-23	WOS:000601594800001
J	de Jesus, JS; Pupim, FD; Sawakuchi, AO; Felipe, LB				de Jesus, Jandessa Silva; Pupim, Fabiano do Nascimento; Sawakuchi, Andre Oliveira; Felipe, Leonardo Brasil			Geomorphology of fluvial deposits in the middle Tocantins River, eastern Amazon	JOURNAL OF MAPS			English	Article						Fluvial geomorphology; geomorphological mapping; digital elevation model; Tocantins River; Maraba	FLOODPLAIN GEOMORPHOLOGY; WADEABLE STREAMS; VEGETATION; EVOLUTION; CHANNEL; BRAZIL; BIODIVERSITY; HYDROPOWER; BASIN; MAP	This paper presents the geomorphological mapping at a 1:100,000 scale of fluvial deposits in the middle Tocantins River. The region preserves an important sedimentary archive of environmental changes of the Amazon and Cerrado biomes. Yet, the region is under influence of diverse anthropogenic activities, including planned or operational hydropower plants, and detailed geomorphological mapping is lacking. The mapping combined interpretation of surface geomorphic features, morphometric analysis, and field surveys. Three main geomorphic units were defined: (i) fluvial plain, (ii) fluvial terraces, and (iii) paleo-alluvial fans. The detailed mapping survey allowed a hierarchical organization of geomorphological units as well as their relative chronology of formation. Our results improve the understanding on the complex geomorphological processes which shape the current fluvial landscape. Specifically, improving the understanding of the Tocantins River floodplains is crucial to support conservation of flooded forests, sustainable use of natural resources and minimize socio-economic losses and damages.	[de Jesus, Jandessa Silva; Pupim, Fabiano do Nascimento; Sawakuchi, Andre Oliveira] Univ Sao Paulo, Inst Geosci, Rua Lago,562 Cidade Univ, Sao Paulo, Brazil; [Pupim, Fabiano do Nascimento] Univ Fed Sao Paulo, Dept Environm Sci, Diadema, Brazil; [Felipe, Leonardo Brasil] Univ Fed Sul & Sudeste Para, Inst Geosci & Engn, Maraba, Brazil	Universidade de Sao Paulo; Universidade Federal de Sao Paulo (UNIFESP); Universidade Federal do Sul e Sudeste do Para	de Jesus, JS (autor correspondente), Univ Sao Paulo, Inst Geosci, Rua Lago,562 Cidade Univ, Sao Paulo, Brazil.	jandessa@usp.br	Pupim, Fabiano N/J-7869-2012; Sawakuchi, André O/D-1445-2013	Pupim, Fabiano N/0000-0001-7452-1376; Jesus, Jandessa/0000-0002-8425-9532; Felipe, Leonardo/0000-0002-8049-907X	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior [001]; National Council for Scientific and Technological Development (CNPq, Brazil) [302411/2018-6, 304727/2017-2]; Sao Paulo Research Foundation (FAPESP, Brazil) [2014/23334-4, 2016/02656-1]; Sao Paulo Research Foundation (FAPESP, Brazil); National Science Foundation; National Aeronautics and Space Administration; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo [1241066, 2012/50260-6]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council for Scientific and Technological Development (CNPq, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Sao Paulo Research Foundation (FAPESP, Brazil)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Sao Paulo Research Foundation (FAPESP, Brazil)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Science Foundation(National Science Foundation (NSF)); National Aeronautics and Space Administration(National Aeronautics & Space Administration (NASA)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	This work was supported by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior [Grand ID 001]; National Council for Scientific and Technological Development (CNPq, Brazil): [Grant Number 302411/2018-6,304727/2017-2]; Sao Paulo Research Foundation (FAPESP, Brazil): [Grant Number 2014/23334-4,2016/02656-1]; Sao Paulo Research Foundation (FAPESP, Brazil), National Science Foundation, National Aeronautics and Space Administration, Fundacao de Amparo a Pesquisa do Estado de Sao Paulo 1241066 (Grant ID 2012/50260-6).	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Maps	DEC 9	2020	16	2					710	723		10.1080/17445647.2020.1822938	http://dx.doi.org/10.1080/17445647.2020.1822938			14	Geography; Geography, Physical	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Geography; Physical Geography	NW3ZQ		Green Submitted, gold			2023-06-23	WOS:000574949100001
J	Gonzalez, PAA; Hauser, N; Carvalho, MD; Valeriano, CD; Cayo, LE; Barrientos, A; Impiccini, A; Reimold, WU; Heilbron, M; Pimentel, MM				Aparicio Gonzalez, Pamela A.; Hauser, Natalia; Carvalho, Manuela de Oliveira; Valeriano, Claudio de Morisson; Cayo, Lubin Eric; Barrientos, Andrea; Impiccini, Agnes; Reimold, Wolf Uwe; Heilbron, Monica; Pimentel, Marcio M.			The Neoproterozoic-lower Paleozoic sequence of the Sierra de Mojotoro, Eastern Cordillera: Sedimentary provenance (Sr-Nd, U-Pb, and clay mineralogy) and its tectonic implications for western Gondwana	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Eastern Cordillera; Andean basement; Clay minerals; Sr-Nd isotopes; U-Pb on Zircon; Basin tectonics	GRADE METASEDIMENTARY ROCKS; PLASMA-MASS SPECTROMETRY; NORTHWESTERN ARGENTINA; PUNCOVISCANA FORMATION; CRUSTAL EVOLUTION; PAMPEAN OROGENY; TRACE-ELEMENT; CHLORITE-MICA; CENTRAL ANDES; NW ARGENTINA	Comparative analysis of mineralogy and post-depositional thermal evolution, as well as Sr-Nd and U-Pb on zircon isotope analysis of metapelites/pelites and sandstones of the Neoproterozoic to Paleozoic succession (Puncoviscana Complex, Meson and Santa Victoria groups) in the Sierra de Mojotoro of northwestern Argentina has been conducted. Samples are mainly composed of different phyllosilicate minerals: illite, chlorite, kaolinite, illite/chlorite, corrensite, and K-bentonite. Some could have been incorporated through an inheritance process, whereas others probably originate from the alteration of volcanic precursor minerals (from Pampean and Famatinian magmatism). The Nd-Sr fingerprints for the Eastern Cordillera and the Puna are defined. For the Eastern Cordillera Epsilon Nd is more negative, the Nd model age is a little older (until 1.7 Ga), and these rocks show more radiogenic Sr-87/Sr-86 ratios when compared with Puna rocks. Nd isotopes and U-Pb ages on zircon suggest that the sedimentary rocks of the Eastern Cordillera were formed during the Paleozoic from reworking of continental crust. The detrital zircon data for samples from the Santa Victoria Group (Floresta, San Bernardo and Mojotoro formations) show a main population of lower-middle Cambrian age, and only one contemporaneous zircon grain of volcanic origin yielded a Floian age (473 Ma). The new data, when compared with previous data from the Puna and other parts of the Eastern Cordillera, allow us to delineate a model for the Neoproterozoic to lower Paleozoic evolution of NW Argentina that involves the evolution from an active margin.	[Aparicio Gonzalez, Pamela A.] UBA Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Geol, INGEIS Inst Geocronol & Geol Isotop, Ciudad Univ,C1428EHA, Buenos Aires, DF, Argentina; [Hauser, Natalia; Reimold, Wolf Uwe; Pimentel, Marcio M.] Univ Brasilia, Inst Geociencias, Lab Geochronol & Isotope Geochem, BR-70910900 Brasilia, DF, Brazil; [Carvalho, Manuela de Oliveira; Valeriano, Claudio de Morisson; Heilbron, Monica] FGEL UERJ, FGEL UERJ TEKTOS Grp Pesquisas Geotecton, Rio De Janeiro, Brazil; [Carvalho, Manuela de Oliveira; Valeriano, Claudio de Morisson; Heilbron, Monica] FGEL UERJ, LAGIR Lab Geochronol & Radiogen Isotopes, Geochronol & Radiogen Isotopes, Rio De Janeiro, Brazil; [Cayo, Lubin Eric; Barrientos, Andrea] Univ Nacl Salta, Salta 3700, Argentina; [Impiccini, Agnes] UNCOMA Univ Nacl Comahue, Neuquen, Argentina	Universidade de Brasilia; Universidad Nacional del Comahue	Gonzalez, PAA (autor correspondente), UBA Univ Buenos Aires, Dept Geol, INGEIS Inst Geocronol & Geol Isotop, Fac Ciencias Exactas & Nat, Ciudad Univ,C1428EHA, Buenos Aires, DF, Argentina.	pamelaaparicio@gmail.com	de Morisson Valeriano, Claudio/A-6090-2013; Hauser, Natalia/H-2041-2012; Reimold, Wolf Uwe/AAI-6226-2021; Heilbron, Monica/T-1389-2017; Heilbron, Monica/AAC-9663-2021	de Morisson Valeriano, Claudio/0000-0002-9341-2615; Heilbron, Monica/0000-0002-3521-9251; Heilbron, Monica/0000-0002-3521-9251; Hauser, Natalia/0000-0002-6975-6186; Barrientos, Andrea/0000-0002-4976-6731; Reimold, Wolf Uwe/0000-0001-6588-0887; Cayo, Lubin Eric/0000-0002-5367-3933	CONICET; Brazilian National Council for Scientific and Technological Development (CNPq) [309878/2019-5, 305761/2019-6]	CONICET(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The first author would like to thank for postdoctoral fellowships from CONICET. Reviewers Vanesa BarberOn and Carita Augustsson provided very useful comments. C. Casquet and M. Do Campo are thanked for commenting on a preliminary version of this paper. V. Ramos provided useful comments on the tectonic setting and is thanked for editorial handling. N. Hauser and W.U. Reimold are supported by the Brazilian National Council for Scientific and Technological Development (CNPq) fellowship grants (309878/2019-5 and 305761/2019-6, respectively).	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DEC	2020	104								102818	10.1016/j.jsames.2020.102818	http://dx.doi.org/10.1016/j.jsames.2020.102818			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TT					2023-06-23	WOS:000600272600003
J	Huhn, SRB; Silva, AM; Ferreira, FJF; Braitenberg, C				Bacelar Huhn, Sergio Roberto; Silva, Adalene Moreira; Fonseca Ferreira, Francisco Jose; Braitenberg, Carla			Mapping New IOCG Mineral Systems in Brazil: The Vale do Curaca and Riacho do Pontal Copper Districts	MINERALS			English	Article						3D data integration; IOCG; Palaeoproterozoic; gravimetric and magnetic inversion; Riacho do Pontal; Brazil	SAO-FRANCISCO CRATON; HYDROTHERMAL ALTERATION; GOLD DEPOSITS; CU-AU; METALLOGENIC EVOLUTION; PB GEOCHRONOLOGY; CARAJAS PROVINCE; STABLE-ISOTOPE; IRON; BAHIA	The Vale do Curaca and Riacho do Pontal copper districts are located within the northern part of the Archaean Sao Francisco Craton and represent two pulses of mineralization. The copper districts have been identified as Iron-Oxide-Copper-Gold (IOCG) classes of deposits. An older metallogenic event associated with the Caraiba copper deposit, which is located in the Vale do Curaca district, is related to Palaeoproterozoic (ca. 2 to 2.2 Ga) hydrothermal processes. A younger Neoproterozoic (ca. 750 to 570 Ma) episode of volcanism and associated plutonism is represented by the Riacho do Pontal mineral district. Seismic tomography data from across east-central Brazil show that the multiage Carajas province and Vale do Curaca and Riacho do Pontal copper districts sit along either side of a prominent NW-trending upper lithospheric high-velocity zone. The edges of the high-velocity zone point to long-lived subparallel transcrustal structures that have been the focus of multiple reactivations and copper mineralization events. Regional gravity and magnetic maps show that the Vale do Curaca copper district extends over an area greater than 110 km by 22 km. The magnetic and gravity values show significant variations correlated with this area. The district includes high gravity values associated with the Caraiba copper mine (>-35 mGal), which has a greater density (3.13 g/cm(3)) than the nonmineralized host rock density (2.98 g/cm(3)). The gravity anomaly signature over the Riacho do Pontal copper district is characterized by a 40-km long NW-SE trending Bouguer gravity low. The Ria4 occurrences of the Riacho do Pontal copper district are situated in these regional low-gravity domains. Data from regional airborne magnetic and ground gravity surveys were inverted to obtain a 3D magnetic susceptibility and density model, respectively, for the known districts. The results show that the Caraiba deposit is characterized by a both dense and magnetic source showing structural control by thrust shear zones. The 2D and 3D geological models show two main NNW prospective trends. Trends I and II have a sigmoidal shear shape and are positioned in the contact zone between domains with high magnetic susceptibility (SI > 0.005) and density > 0 g/cm(3)). Trend I is 40 km x 10 km in size and hosts the Caraiba, Surubim, and Vermelho copper mines and other minor deposits. The results obtained from the 3D magnetic inversion model for the region of the Riacho do Pontal district show weak magnetic anomaly highs extending along a NW-SE magnetic gradient trend. The gradient is related to mapped shear zones that overprint older and deeper NE-SW features of the Sao Francisco cratonic root. The area includes high gravity values associated with the Caraiba copper deposit, which has a greater density (3.13 g/cm(3)) than the nonmineralized host rock density (2.4 g/cm(3)).	[Bacelar Huhn, Sergio Roberto] Univ Fed Ceara UFC, Dept Geol, Campus PICI, BR-60440554 Fortaleza, Ceara, Brazil; [Silva, Adalene Moreira] Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Fonseca Ferreira, Francisco Jose] Univ Fed Parana, Lab Geofis Aplicada, BR-81531980 Curitiba, Parana, Brazil; [Braitenberg, Carla] Univ Trieste, Dept Math & Geosci, I-34149 Trieste, Italy	Universidade Federal do Ceara; Universidade de Brasilia; Universidade Federal do Parana; University of Trieste	Huhn, SRB (autor correspondente), Univ Fed Ceara UFC, Dept Geol, Campus PICI, BR-60440554 Fortaleza, Ceara, Brazil.	sergio.bacelar@ufc.br; adalene@unb.br; francisco.ferreira@ufpr.br; berg@units.it	Braitenberg, Carla/B-5882-2013; Ferreira, Francisco/AAG-9483-2020; Ferreira, Francisco/H-8151-2013	Braitenberg, Carla/0000-0001-7277-816X; Ferreira, Francisco/0000-0002-0269-5833	National Council for Scientific and Technological Development (CNPq) [307177/2014-9]	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	A.M. Silva gratefully acknowledges the National Council for Scientific and Technological Development (CNPq) for research grant 307177/2014-9.	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J	Bahr, A; Doubrawa, M; Titschack, J; Austermann, G; Koutsodendris, A; Nurnberg, D; Albuquerque, AL; Friedrich, O; Raddatz, J				Bahr, Andre; Doubrawa, Monika; Titschack, Juergen; Austermann, Gregor; Koutsodendris, Andreas; Nurnberg, Dirk; Albuquerque, Ana Luiza; Friedrich, Oliver; Raddatz, Jacek			Monsoonal forcing of cold-water coral growth off southeastern Brazil during the past 160 kyr	BIOGEOSCIENCES			English	Article							DEEP-SEA CORALS; FOOD-SUPPLY MECHANISMS; BENTHIC FORAMINIFERA; NORTHEAST ATLANTIC; WESTERN BOUNDARY; SOLENOSMILIA-VARIABILIS; MEDITERRANEAN OUTFLOW; OCEAN ACIDIFICATION; UPWELLING SYSTEM; LOPHELIA-PERTUSA	Cold-water corals (CWCs) constitute important deep-water ecosystems that are under increasing environmental pressure due to ocean acidification and global warming. The sensitivity of these deep-water ecosystems to environmental change is demonstrated by abundant paleorecords drilled through CWC mounds that reveal characteristic alterations between rapid formation and dormant or erosive phases. Previous studies have identified several central parameters for driving or inhibiting CWC growth such as food supply, oxygenation, and the carbon saturation state of bottom water, yet there are still large uncertainties about the relative importance of the different environmental parameters. To advance this debate we have performed a multiproxy study on a sediment core retrieved from the 25 m high Bowie Mound, located at 866 m water depth on the continental slope off southeastern Brazil, a structure built up mainly by the CWC Solenosmilia variabilis. Our results indicate a multifactorial control on CWC growth at Bowie Mound during the past similar to 160 kyr, which reveals distinct formation pulses during northern high-latitude glacial cold events (Heinrich stadials, HSs) largely associated with anomalously strong monsoonal rainfall over the continent. The ensuing enhanced runoff elevated the terrigenous nutrient and organic-matter supply to the continental margin and likely boosted marine productivity. The dispersal of food particles towards the CWC colonies during HSs was facilitated by the highly dynamic hydraulic conditions along the continental slope that prevailed throughout glacial periods. These conditions caused the emplacement of a pronounced nepheloid layer above Bowie Mound, thereby aiding the concentration and along-slope dispersal of organic matter. Our study thus emphasizes the impact of continental climate variability on a highly vulnerable deep-marine ecosystem.	[Bahr, Andre; Doubrawa, Monika; Austermann, Gregor; Koutsodendris, Andreas; Friedrich, Oliver] Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234, D-69120 Heidelberg, Germany; [Doubrawa, Monika] Katholieke Univ Leuven, Earth & Environm Sci, Celestijnenlaan 200e, B-3001 Leuven, Belgium; [Titschack, Juergen] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany; [Titschack, Juergen] Marine Res Dept, Senckenberg Meer, D-26382 Wilhelmshaven, Germany; [Nurnberg, Dirk] GEOMAR Helmholtz Ctr Ocean Res, Wischhofstr 1-3, D-24148 Kiel, Germany; [Albuquerque, Ana Luiza] Univ Fed Fluminense, Dept Geoquim, Outeiro Sao Joao Baptista S-N Ctr, Niteroi, RJ, Brazil; [Raddatz, Jacek] Goethe Univ, Inst Geosci, Altenhoferallee 1, D-60438 Frankfurt, Germany	Ruprecht Karls University Heidelberg; KU Leuven; University of Bremen; Senckenberg Gesellschaft fur Naturforschung (SGN); Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; Universidade Federal Fluminense; Goethe University Frankfurt	Bahr, A (autor correspondente), Heidelberg Univ, Inst Earth Sci, Neuenheimer Feld 234, D-69120 Heidelberg, Germany.	andre.bahr@geow.uni-heidelberg.de	Koutsodendris, Andreas/G-8966-2013; Titschack, Jürgen/L-2095-2015; Albuquerque, Ana Luiza S/C-5167-2013	Koutsodendris, Andreas/0000-0003-4236-7508; Titschack, Jürgen/0000-0001-9373-9688; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Friedrich, Oliver/0000-0002-6046-7513; Raddatz, Jacek/0000-0002-5713-9682; Doubrawa, Monika/0000-0003-4885-688X; Austermann, Gregor/0000-0003-0728-3341	Deutsche Forschungsgemeinschaft [HO5927/1-1, EXC-2077 -390741603]	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	This research has been supported by the Deutsche Forschungsgemeinschaft (grant nos. HO5927/1-1 to Andre Bahr and EXC-2077 -390741603 to Jurgen Titschack).	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J	Barros, RD; Caxito, FD; Egydio-Silva, M; Dantas, EL; Pinheiro, MAP; Rodrigues, JB; Basei, MAS; das Virgens, J; Freitas, MD				Barros, Renato de Assis; Caxito, Fabricio de Andrade; Egydio-Silva, Marcos; Dantas, Elton Luiz; Piacentini Pinheiro, Marco Aurelio; Rodrigues, Joseneusa Brilhante; Stipp Basei, Miguel Angelo; das Virgens-Neto, Joaquim; Freitas, Magno de Sa			Archean and Paleoproterozoic crustal evolution and evidence for cryptic Paleoarchean-Hadean sources of the NW Sao Francisco Craton, Brazil: Lithochemistry, geochronology, and isotope systematics of the Cristalandia do Piaui Block	GONDWANA RESEARCH			English	Article						Rhyacian-Orosirian orogeny; Crustal evolution; Cryptic Hadean, and Paleoarchean source	U-PB ZIRCON; PRETO FOLD BELT; MIRANTE SUPRACRUSTAL BELT; SOUTHERN GAVIAO BLOCK; A-TYPE GRANITES; MINEIRO BELT; LU-HF; TRACE-ELEMENTS; NE BRAZIL; BORBOREMA PROVINCE	The Cristalandia do Piaui Block, located in the northwestern margin of the Sao Francisco Craton, represents the basement of the Rio Preto Fold Belt. It is composed of Archean orthogneisses of ca. 3.2 Ga reworked at 2.81 and 2.68 Ga with juvenile to moderately juvenile eHf values between -1.51 and -8.07, and high-K syenogranites dated at 2.65 Ga with crustal eHf values between -10.37 and -19.54, both with model ages (TDMc) varying from 3.57 to 4.33 Ga, indicating cryptic Paleo- to Eoarchean and even Hadean sources. Metamafic-ultramafic rocks, iron formations, metacherts, and graphite schists occur in association with the Archean orthogneiss. The whole set is intruded by Paleoproterozoic (ca. 2.2 Ga) metagranitoids with compositions varying from granodioritic with sanukitoid-type signatures tomonzogranitic, and alkali-feldspar graniticwith crustal signatures. They are related to the Rhyacian-Orosirian orogeny, responsible for the complex deformation patterns printed in the Archean basement. Orosirian metasedimentary rocks are represented by garnet-biotite paragneiss with maximum depositional age of ca. 1.95 Ga. Intrusive mafic dikes in the complex show ages of ca. 2.07 Ga and isotopic features of mantle-derived magmas. Considering the presented data, the Cristalandia do Piaui Block represents a metacratonic domain corresponding to part of the Guanambi-Correntina Paleoplate, wich had been involved in crustal accretion and reworking from the Archean to the Paleoproterozoic. Many of the elements of the evolutionary stageswich are present in the Sao Francisco-Congo Paleocontinent can be recognized, suggesting an evolution of this crustal segment amounts to the Eoarchean era and disclosing the existence of cryptic Paleoarchean or even Hadean nuclei, reworked in at least three metamorphic events during the Rhyacian-Orosirian orogeny. (C) 2020 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.	[Barros, Renato de Assis; Caxito, Fabricio de Andrade] Univ Fed Minas Gerais CPMTC IGC UFMG, Ctr Pesquisas Prof Manoel Teixeira da Costa, Dept Geol, Inst Geociencias, Av Antonio Carlos 6-627, BR-31270901 Belo Horizonte, MG, Brazil; [Barros, Renato de Assis; Piacentini Pinheiro, Marco Aurelio] Geol Survey Brazil, Av Brasil 1731, BR-30140002 Belo Horizonte, MG, Brazil; [Egydio-Silva, Marcos; Stipp Basei, Miguel Angelo] Univ Sao Paulo, Inst Geociencias, R Lago 562,Cidade Univ, BR-05508900 Sao Paulo, SP, Brazil; [Dantas, Elton Luiz] Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Rodrigues, Joseneusa Brilhante] Geol Survey Brazil, St Bancario Norte Q2, BR-70040020 Brasilia, DF, Brazil; [das Virgens-Neto, Joaquim] Geol Survey Brazil, Av Sul 2291, BR-50770011 Recife, PE, Brazil; [Freitas, Magno de Sa] Geol Survey Brazil, R Goias 312, BR-64001620 Teresina, PI, Brazil	Universidade de Sao Paulo; Universidade de Brasilia	Barros, RD (autor correspondente), Univ Fed Minas Gerais CPMTC IGC UFMG, Ctr Pesquisa Manoel Teixeira da Costa, Inst Geociencias, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.	renato.barros@cprm.gov.br; caxitoe@ufmg.br	Caxito, Fabricio A/J-1317-2016; Dantas, Elton Luiz/AAK-8464-2021; Basei, Miguel A S/C-1915-2013	Caxito, Fabricio A/0000-0002-0335-3667; Dantas, Elton Luiz/0000-0002-7954-5059; Basei, Miguel A S/0000-0002-3857-7089; de Assis Barros, Renato/0000-0001-7210-8078; Pinheiro, Marco Aurelio Piacentini/0000-0003-4455-1798	Brazilian Federal Government	Brazilian Federal Government	The Geological Survey of Brazil (SGB/CPRM), through the ARIM Northwestern Craton Sao Francisco Project, as part of the programof basic geological mapping funded by the Brazilian Federal Government. FAC, MES, MASB, and ELD are Fellows of the Brazilian Research Council (CNPq), which they acknowledge for the support received. We thank Luiz Carlos da Silva (Luizao) for the discussion and suggestions that greatly improved this article. A previous version of the paper was improved after comments and suggestions by Lauro Cezar Montefalco de Lira Santos, Carlos Eduardo Ganade de Araujo, and Toshiaki Tsunogae.	Alkmim F.F., 2004, GEOLOGIA CONTINENTE, P17; Almeida F. F. 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DEC	2020	88						268	295		10.1016/j.gr.2020.07.004	http://dx.doi.org/10.1016/j.gr.2020.07.004			28	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OP4TW					2023-06-23	WOS:000588076900014
J	Bordalo, RA; dos Santos, TJS; Dantas, EL				Bordalo, Rogerio Alves; Saraiva dos Santos, Ticiano Jose; Dantas, Elton L.			Structural evolution and U/Pb zircon age of the Xambioa gneiss dome, contributions to the Araguaia fold belt tectonic history	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Araguaia belt; Structural geology; U-Pb Geochronology; Tectonics	U-PB GEOCHRONOLOGY; CARAJAS PROVINCE; BRAZIL; ORIGIN; ROCKS	The Araguaia belt in central Brazil is an important key to re-access ancient geological settings, as it records the Gondwana agglutination and the final stages of an oceanic basin closure. Small basement inliers occur along transversal position in the Araguaia belt and could compose the extension of Amazonian craton. The structural analysis of the Xambioa gneiss dome region shows that three main deformational events were responsible for the actual scenario. The first deformational event was a NW-SE non-coaxial compression event (Dn), which led to the formation of ductile structures, such as open and slightly open folds (Fn), from a previous Sn-1 structures, axial plane foliation and spaced foliation (Sn), in the mantling metasedimentary sequence, and the mylonitic foliation (Sn) in dome rocks. This event was associated with a thrust system developed under regional greenschist to local upper amphibolite facies. The second deformational event Dn+1 was characterized by refolding with Sn transposition, followed by asymmetric Fn+1 folds and transposed foliation (Sn+1), and local stretching patterns forming boudins and Ln+1 lineations. The third deformational event Dn+2 is represented by WNW-ESE sinistral transcurrent faults (Sn+2) which sectioned the Dn structures and formed shear zones of different scales. U-Pb zircon ages in gneiss and in a migmatite of the Xambioa dome indicate Mesoarchean (similar to 2.93 Ga) crystallization ages. U-Pb zircon provenance ages from metasedimentary rocks bordering the Xambioa dome show significant contribution of Archean to Neoproterozoic sources. The consistent loss of Pb in the dome rocks evidences tectono-metamorphic events presumably connected to the lithosphere ocean closure and continental collision responsible for the Araguaia Belt edification during Neoproterozoic-Cambrian period.	[Bordalo, Rogerio Alves; Saraiva dos Santos, Ticiano Jose] Univ Estadual Campinas, UNICAMP, Geosci Inst, BR-13083970 Campinas, SP, Brazil; [Dantas, Elton L.] Univ Brasilia, UnB, BR-13083970 Brasilia, DF, Brazil	Universidade Estadual de Campinas; Universidade de Brasilia	Bordalo, RA (autor correspondente), Univ Estadual Campinas, UNICAMP, Geosci Inst, BR-13083970 Campinas, SP, Brazil.	rogerbordalo@gmail.com; ticiano@unicamp.br; elton@unb.br	Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059; Saraiva dos Santos, Ticiano Jose/0000-0002-9491-1213; Bordalo, Rogerio/0000-0002-6095-3423	Sao Paulo Research Foundation (FAPESP) [12/15824-6]; Brazilian Research Council for Science and Technology (CNPq) [310836/2015-8]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [12/15824-6] Funding Source: FAPESP	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Brazilian Research Council for Science and Technology (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	We would like to thank the Sao Paulo Research Foundation (FAPESP Proc. 12/15824-6) for the financial support, and the Brazilian Research Council for Science and Technology (CNPq) for the scholarship (RAB) and research grant (TJSS -Proc. 310836/2015-8).	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South Am. Earth Sci.	DEC	2020	104								102753	10.1016/j.jsames.2020.102753	http://dx.doi.org/10.1016/j.jsames.2020.102753			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TV					2023-06-23	WOS:000600272800002
J	Bortolin, EC; Weschenfelder, J; Fernandes, EH; Bitencourt, LP; Moller, OO; Garcia-Rodriguez, F; Toldo, E				Bortolin, E. C.; Weschenfelder, J.; Fernandes, E. H.; Bitencourt, L. P.; Moller, O. O.; Garcia-Rodriguez, F.; Toldo, E.			Reviewing sedimentological and hydrodynamic data of large shallow coastal lagoons for defining mud depocenters as environmental monitoring sites	SEDIMENTARY GEOLOGY			English	Review						Back-Barrier Lagoon; Sedimentology; Hydrodynamics; Morphometry; Mud depocenter	SOUTHERN BRAZILIAN COAST; SEA-LEVEL CHANGES; GRANDE-DO-SUL; PATOS LAGOON; EL-NINO; RIVER DISCHARGE; CASSINO BEACH; EVOLUTION; QUATERNARY; BARRIER	We reviewed historical data on surface sediment composition/distribution and hydrodynamics of the Patos-Mirim lagoonal system, the largest coastal shallow limnological system of the world, located in eastern South America, which is ca. 15,000 km(2), the maximum length is almost 500 km and maximum depth is around 7 m. We inferred the geographical position of six mud depocenters in relation to the hydrodynamic conditions evolved from predominant winds and morphometry. Littoral zones of sediment resuspension dominated by sand were identified where current velocity was higher than 0.2 m s(-1) and depth was <5 m. In addition, central zones were susceptible to deposition of fine sediment fractions, where current velocity was close to 0.1 m s(-1) and depth was >5 m. Such conditions observed for the central zones represent appropriate morphodynamic controls for mud depocenter formation. The six permanent Holocene depocenters for the whole Patos-Mirim system were all dominated mostly by silty clayey fades and exhibited an Mz value equal to or higher than 7.5. Because of the dominance of the fine fraction, we propose them as future potential key-spots for monitoring the environmental quality of the system to assist regional sustainable management. (C) 2020 Elsevier B.V. All rights reserved.	[Bortolin, E. C.; Fernandes, E. H.; Bitencourt, L. P.; Moller, O. O.; Garcia-Rodriguez, F.] Univ Fed Rio Grande FURG, Inst Oceanog, Rio Grande, Brazil; [Weschenfelder, J.; Toldo, E.] Univ Fed Rio Grande do Sul UFRGS, Ctr Estudos Geol Costeira & Ocean CECO, Inst Geociencias, Porto Alegre, RS, Brazil; [Garcia-Rodriguez, F.] Ctr Univ Reg Este, Sede CURE Rocha, Ruta 9 S-N, Rocha 27000, Uruguay	Universidade Federal do Rio Grande; Universidade Federal do Rio Grande do Sul	Bortolin, EC (autor correspondente), Univ Fed Rio Grande FURG, Inst Oceanog, Rio Grande, Brazil.	edubortolin@gmail.com	Fernandes, Elisa Helena/GLU-4155-2022; Weschenfelder, Jair/C-3390-2013; Moller, Osmar O/ISB-2973-2023	Weschenfelder, Jair/0000-0002-2075-4067; Paranhos Bitencourt, Liliane/0000-0001-5225-7498; Fernandes, Elisa/0000-0003-1869-0233; Moller, Osmar/0000-0002-7207-1022	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [301668/2017-5, 304007/2019-6, 302231/2010-2, 307143/2017-1]; Office of Naval Research [N62909-19-1-2145]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Office of Naval Research(Office of Naval Research)	We acknowledge the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for the research grants J. Weschenfelder (Process No 301668/2017-5), F. Garcia-Rodriguez (Process No 304007/2019-6), Osmar O. Moller (302231/2010-2), E.E. Toldo (307143/2017-1), and the LOAD Project - Long-term analysis of Suspended Particulate Matter concentrations Affecting port areas in Developing countries, sponsored by the Office of Naval Research (contract N62909-19-1-2145). Special thanks to Grasiela L.L Pinho formotivation to undertake this study. Eduardo Bortolin dedicates this paper to the loving memory of his brother, Rafael Bortolin, who recently passed away diving during an expedition in Colombia.	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J	Brown, MT; Fuck, RA; Dantas, EL				Brown, Matthew T.; Fuck, Reinhardt A.; Dantas, Elton L.			Provenance of neoproterozoic ophiolitic melange sediments in the brasilia belt, central Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Araxa group; Detrital zircon; Hf isotopes; Nd model ages	ULTRAHIGH-TEMPERATURE METAMORPHISM; DETRITAL-ZIRCON GEOCHRONOLOGY; PLASMA-MASS SPECTROMETRY; ANAPOLIS-ITAUCU COMPLEX; U-PB GEOCHRONOLOGY; TECTONIC EVOLUTION; SM-ND; TRACE-ELEMENT; PALEOPROTEROZOIC CRUST; GRANITIC MAGMATISM	Melanges are a chaotic mixture of different rock assemblages that can be associated with orogenic belts and suture zones. The Brasilia Belt is a Neoproterozoic orogenic belt in central Brazil, which contains a poorly understood ophiolitic melange. In order to better understand the sedimentation that was associated with this melange, isotopic U-Pb and Lu-Hf analyses on single zircon grains, and Sm-Nd on whole rock samples was conducted on melange metasedimentary rock (garnet-mica-quartz schists and quartzites) and basement (mylonitic granites) assemblages. The quartzite samples have a maximum age of deposition of about 930 Ma, while their negative epsilon(Nd) (T) values and T-DM, -7.78 to -11.57 and 1.70 to 2.07 Ga, respectively, are similar to other metasedimentary rock units interpreted to have formed in a passive margin environment. epsilon(Hf) and Hf T-DM model values from the quartzite samples range from -12.72 to 8.99 and 2.56 to 1.36 Ga, respectively. The mylonitic granite has an age of similar to 2.1 Ga, epsilon(Hf) values ranging from -0.97 to 2.18, and T-DM model values ranging from 2.38 to 2.53 Ga, indicating that it was derived from juvenile Paleoproterozoic basement. Results of the garnet-mica schists reveal that they represent two different rock units, defined by two different periods of sedimentation. The first group of garnet-mica schist has a maximum age of deposition of 672 Ma and epsilon(Nd) (T) values and T-DM -7.90 to -7.62 and 1.82 to 1.88 Ga, respectively. epsilon(df) and T-DM model values range from -23.50 to 11.69 and 3.23 to 1.45 Ga, respectively, and indicate the presence of similar zircon populations as the passive margin sequence and basement zircon population; there is also a contribution of a younger zircon population derived from older reworked crustal material. The second group of garnet-mica schists is marked by a maximum age of deposition of 616 Ma and epsilon(Nd) (T) values and T-DM ranging from 0.61 to 0.22 and 1.16 to 1.25 Ga, respectively. epsilon(df) and T-DM model values range from -8.24 to 16.04 and 2.97 to 0.79 Ga, respectively. These results also indicate the presence of passive margin and basement zircon populations, but the younger zircon populations are derived from juvenile sources. The depositional periods of the garnet-mica schists occurred between roughly 800 to 650 Ma and 650 to 600 Ma, and indicate that the rocks from the Brasilia Belt register the presence of different depositional environments and basins, which opened, closed and were later dismembered. The quartzites, mylonitic granites and ophiolites most likely represent blocks that were introduced into the melange by sedimentation or tectonic processes.	[Brown, Matthew T.; Fuck, Reinhardt A.; Dantas, Elton L.] Univ Brasilia, Inst Geociencias, Lab Geocronol, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia	Brown, MT (autor correspondente), Univ Brasilia, Inst Geociencias, Lab Geocronol, BR-70910900 Brasilia, DF, Brazil.	brownmt7@gmail.com	Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059; Fuck, Reinhardt/0000-0003-1396-125X	Brazilian National Council for Scientific and Technological Development (CNPq); Instituto Nacional de Ciencia e Tecnologia Estudos TectOnicos (CNPq); (Instituto Nacional de Ciencia e Tecnologia Estudos TectOnicos) CAPES; Instituto Nacional de Ciencia e Tecnologia Estudos TectOnicos (FAP-DF); CNPq; Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) [001]	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Instituto Nacional de Ciencia e Tecnologia Estudos TectOnicos (CNPq)(Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); (Instituto Nacional de Ciencia e Tecnologia Estudos TectOnicos) CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Instituto Nacional de Ciencia e Tecnologia Estudos TectOnicos (FAP-DF); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The first author would like to acknowledge the Brazilian National Council for Scientific and Technological Development (CNPq) for the doctoral scholarship. The authors also acknowledge the Instituto Nacional de Ciencia e Tecnologia Estudos TectOnicos (CNPq, CAPES, FAP-DF) for financial support. Reinhardt A. Fuck and Elton L. Dantas acknowledge CNPq research fellowships. This study was financed in part by the Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) - Finance Code 001.	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D辑, 地球科学, Science in China], V35, P1131	85	2	2	0	2	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	DEC	2020	104								102825	10.1016/j.jsames.2020.102825	http://dx.doi.org/10.1016/j.jsames.2020.102825			25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TU					2023-06-23	WOS:000600272700003
J	Caetano, LS; Pollery, RCG; Kerr, R; Magrani, F; Neto, AA; Vieira, R; Marotta, H				Caetano, Ludmila S.; Pollery, Ricardo C. G.; Kerr, Rodrigo; Magrani, Fabio; Ayres Neto, Arthur; Vieira, Rosemary; Marotta, Humberto			High-resolution spatial distribution of pCO(2) in the coastal Southern Ocean in late spring	ANTARCTIC SCIENCE			English	Article						Antarctic Peninsula; carbon cycle; CO2 fluxes; subpolar bay	NORTHERN ANTARCTIC PENINSULA; NET COMMUNITY PRODUCTION; INORGANIC CARBON; CO2; SEA; ACIDIFICATION; BALANCE; STRAIT; ISLAND; BASIN	We present a high-resolution spatial study of ocean surface carbon dioxide partial pressure (pCO(2)), temperature and salinity coupled with a seismic survey performed in subpolar waters with a variable presence of glaciers along the coastal margins of Admiralty Bay and the Bransfield Strait, northern Antarctic Peninsula, during the late spring season. Three zones were identified in this bay. The shallow and relatively fresh SHALLOW GLACIER THAW zone in the inner portion of the bay had high freshwater inputs from active glacial meltwater channels, representing higher pCO(2) levels (median similar to 438 mu atm) than the shallow and relatively salty SHALLOW zone without glaciers along the margins and dominated by macroalgae communities at the bottom, which showed relatively low pCO(2) levels (median similar to 371 mu atm). The deep and relatively salty CENTRE zone was highly influenced by seawater intrusions from the Bransfield Strait, representing intermediate pCO(2) levels (median similar to 397 mu atm). The net sea-air CO2 fluxes in late spring obtained from the high-resolution surface survey in Admiralty Bay indicate a condition of near neutral air-sea CO2 flux, with a median (25-75% interquartile range) value of -0.07 mmol m(-2) day(-1) (ranging from -12.21 to +4.33 mmol m(-2) day(-1)), contrasting with the slight source to the atmosphere estimated from measurements only in the CENTRE zone. This finding suggests that temperature-sensitive metabolic and physical-chemical processes may cause significant variability in the ocean surface distribution of CO2 over short shoreline distances in the northern Antarctic Peninsula.	[Caetano, Ludmila S.; Vieira, Rosemary; Marotta, Humberto] Fed Fluminense Univ UFF, Grad Program Geog, Dept Geog, Sedimentary & Environm Proc Lab LAPSA UFF, Av Gal Milton Tavares de Souza S-N, BR-24210346 Niteroi, RJ, Brazil; [Caetano, Ludmila S.; Marotta, Humberto] Fed Fluminense Univ UFF, Grad Program Geosci Environm Geochem, Biomass & Water Management Res Ctr NAB UFF, Ecosyst & Global Change Lab LEMG UFF,Int Lab Glo, Av Edmundo March S-N, BR-24210310 Niteroi, RJ, Brazil; [Pollery, Ricardo C. G.] Fed Univ Rio De Janeiro UFRJ, Hlth Sci Ctr, Multiuser Unit Environm Anal, Predio Inter Bloco A-F,Av Carlos Chagas Filho, BR-21941971 Rio De Janeiro, RJ, Brazil; [Kerr, Rodrigo] Fed Univ Rio Grande FURG, Inst Oceanog, Ocean & Climate Studies Lab, Av Italia Km 8 S-N, BR-96203900 Rio Grande, RS, Brazil; [Magrani, Fabio; Ayres Neto, Arthur] Fed Fluminense Univ UFF, Grad Program Geosci Dynam Oceans & Earth, Lab Marine Geophys LAGEMAR UFF, Av Gal Milton Tavares de Souza S-N, BR-24210346 Niteroi, RJ, Brazil; [Magrani, Fabio] Univ Bern, Inst Geol Sci, Baltzerstr 3, CH-3012 Bern, Switzerland	Universidade Federal Fluminense; Universidade Federal Fluminense; Universidade Federal do Rio Grande; Universidade Federal Fluminense; University of Bern	Marotta, H (autor correspondente), Fed Fluminense Univ UFF, Grad Program Geog, Dept Geog, Sedimentary & Environm Proc Lab LAPSA UFF, Av Gal Milton Tavares de Souza S-N, BR-24210346 Niteroi, RJ, Brazil.; Marotta, H (autor correspondente), Fed Fluminense Univ UFF, Grad Program Geosci Environm Geochem, Biomass & Water Management Res Ctr NAB UFF, Ecosyst & Global Change Lab LEMG UFF,Int Lab Glo, Av Edmundo March S-N, BR-24210310 Niteroi, RJ, Brazil.	humbertomarotta@id.uff.br	Kerr, Rodrigo/I-2494-2012; Marotta, Humberto/F-9554-2012; Neto, Arthur Ayres/AAL-2963-2021	Kerr, Rodrigo/0000-0002-2632-3137; Marotta, Humberto/0000-0002-2828-6595; Neto, Arthur Ayres/0000-0002-2982-245X; Vieira, Rosemary/0000-0003-0312-2890; Magrani, Fabio/0000-0002-9487-5849	Brazilian Ministry of the Environment (MMA); Brazilian Ministry of Science, Technology, Innovation and Communication (MCTIC); Council for Research and Scientific Development of Brazil (CNPq) through Brazilian National Institute of Science and Technology of Cryosphere (INCT-CRIOSFERA; CNPq) [573720/2008-8, 465680/2014-3]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]; project CLIMATE-PRINT-CAPES/UFF [88887.310301/2018-00]; project FEEDBACKS-PRINT-CAPES/UFF [99997.310301/2018-00]; CNPq [573720/2008-8, 311380/2019-0, 304937/2018-5]; Research Support Foundation of the State of Rio de Janeiro (FAPERJ) [E-26/201.503/2014, E-26/010.001639/2016]	Brazilian Ministry of the Environment (MMA); Brazilian Ministry of Science, Technology, Innovation and Communication (MCTIC); Council for Research and Scientific Development of Brazil (CNPq) through Brazilian National Institute of Science and Technology of Cryosphere (INCT-CRIOSFERA; CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); project CLIMATE-PRINT-CAPES/UFF; project FEEDBACKS-PRINT-CAPES/UFF; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Research Support Foundation of the State of Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	\PROANTAR projects have been funded by and have received logistical support from the Brazilian Ministry of the Environment (MMA), the Brazilian Ministry of Science, Technology, Innovation and Communication (MCTIC) and the Council for Research and Scientific Development of Brazil (CNPq) through grants from the Brazilian National Institute of Science and Technology of Cryosphere (INCT-CRIOSFERA; CNPq grant nos. 573720/2008-8 and 465680/2014-3). In addition, this study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001 and the projects CLIMATE-PRINT-CAPES/UFF (88887.310301/2018-00) and FEEDBACKS-PRINT-CAPES/UFF (99997.310301/2018-00). LSC, RV and RK received support from CNPq fellowship 573720/2008-8 and research grant nos. 311380/2019-0 and 304937/2018-5, respectively. HM received support from the Research Support Foundation of the State of Rio de Janeiro (FAPERJ grant nos. E-26/201.503/2014 and E-26/010.001639/2016).	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Sci.	DEC	2020	32	6					476	485		10.1017/S0954102020000334	http://dx.doi.org/10.1017/S0954102020000334			10	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	OS9LW					2023-06-23	WOS:000590479300006
J	Carniel, LC; Conceicao, RV; Klemme, S; Berndt, J; Jalowitzki, T				Carniel, Larissa Colombo; Conceicao, Rommulo Vieira; Klemme, Stephan; Berndt, Jasper; Jalowitzki, Tiago			Origin and redox conditions of the Rosario-6 alnoite of southern Brazil: Implications for the state of the mantle during Gondwana breakup	LITHOS			English	Article						Alkaline igneous province; Metasomatized mantle; Mineral chemistry; Redox mantle conditions	SPINEL OXYGEN GEOBAROMETER; TRACE-ELEMENT; FLOOD BASALTS; IGNEOUS ROCKS; ULTRAMAFIC LAMPROPHYRES; PARTITION-COEFFICIENTS; LITHOSPHERIC MANTLE; CATIO3 PEROVSKITE; OXIDATION-STATE; PHASE-RELATIONS	The Rosario-6 alnoite is an alkaline occurrence that belongs to the Rosario do Sul kimberlitic field, situated in the south-eastern edge of the Parana Basin, in the South of Brazil, and erupted concomitant or just after the volcanism of the Parana-Etendeka Large Igneous Province (LIP). Following recent published nomenclature, Rosario-6 was classified as a kimberlite from a deep mantle source with a distinctive inequigranular texture resulting from the presence of olivine macrocrysts set in a finer-grained matrix. Trace element compositions of olivine, monticellite, spinel, phlogopite, perovskite and apatite show an enrichment of Nb, Ce, Ta and U, which implies that the Rosario-6 mantle source was enriched by recycled oceanic crust. The positive anomalies of Rb, Ba and Sr, the enrichment in LREE, and the negative anomalies of HREE in the Rosario-6 minerals, are indicative of a metasomatic process in the mantle source that could be caused by fluids from recycled oceanic crust. Temperature, pressure and redox conditions (fO(2)) of Rosario-6 crystallization are estimated from olivine, spinel, perovskite and monticellite compositions: Rosario-6 crystallization temperatures using olivine-spinel geothermobarometry were around 1390(+/- 56)degrees C at a pressure of 2GPa, and 1405(+/- 56)degrees C at 3 GPa with Delta NNO= 2.8, at pressures constrained by the silica activity limited by the crystallization of monticellite. Using a perovskite oxybarometer, we obtained a larger range of Delta NNO (from -2.8 to 3.4), whereas the monticellite oxybarometer results in fO(2) of -2.6 to -0.8 Delta NNO units. The fO(2) indicate that the mantle source of Rosario-6 at the time of crystallization was possibly oxidized by materials from ancient subduction, which may be the cause for Rosario-6's low potential to carry and preserve diamonds. Horizontal tomographic images derived from P-wave velocity data constrain the thickness of the lithosphere in this region and the overall information indicates that mantle cooling at depths below 200 km may have resulted of an accumulation of oceanic plate slabs from old subduction. The geochemical data in conjunction with the geophysical characterizes the conditions of Rosario-6 mineral crystallization and also the mantle of this part of South America during Gondwana breakup. (C) 2020 Elsevier B.V. All rights reserved.	[Carniel, Larissa Colombo; Conceicao, Rommulo Vieira] Univ Fed Rio Grande do Sul, Lab Geoquim & Petrol Expt LAGEPE, Porto Alegre, RS, Brazil; [Conceicao, Rommulo Vieira] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias PPGGEO, Porto Alegre, RS, Brazil; [Klemme, Stephan; Berndt, Jasper] Westfalische Wilhelms Univ Munster, Inst Mineral, Munster, Germany; [Jalowitzki, Tiago] Univ Brasilia UnB, Inst Geociencias, Brasilia, DF, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; University of Munster; Universidade de Brasilia	Carniel, LC (autor correspondente), Univ Fed Rio Grande do Sul, Lab Geoquim & Petrol Expt LAGEPE, Porto Alegre, RS, Brazil.	larissa.colombo@ufrgs.br	Conceição, Rommulo Vieira/D-6030-2014; Jalowitzki, Tiago/AAK-8760-2021	Conceição, Rommulo Vieira/0000-0001-7934-7098; Jalowitzki, Tiago/0000-0001-9857-7876; Klemme, Stephan/0000-0001-7859-9779	CNPq (National Counsel of Technological and Scientific Development), the program "Science without Borders" from Brazil; project "Diamante Brasil" of Geological Survey of Brazil (CPRM)	CNPq (National Counsel of Technological and Scientific Development), the program "Science without Borders" from Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); project "Diamante Brasil" of Geological Survey of Brazil (CPRM)	We thank the financial support for this research, provided by CNPq (National Counsel of Technological and Scientific Development), the program "Science without Borders" from Brazil and the project "Diamante Brasil" of Geological Survey of Brazil (CPRM). We are very grateful to Beate Schmitte and Maik Trogisch from Insitut fur Mineralogie, Universitat Munster, Prof. Fernanda Gervasoni from Universidade Federal de Goias, for their assistance and help with the ICP-MS analysis, Prof. Andrea Sander from CPRM (Servico Geologico do Brasil) and Prof. Marcelo Peres Rocha from Universidade de Brasilia, for his help with the mineralogical interpretation and tectonic modeling. We are also very grateful to Prof. Sebastian Tappe from University of Johannesburg, Hugh O'Brien from the Geological Survey of Finland and an anonymous reviewer, for their constructive reviews and helpful suggestions.	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J	Cohen, MCL; Rodrigues, E; Rocha, DOS; Freitas, J; Fontes, NA; Pessenda, LCR; de Souza, AV; Gomes, VLP; Franca, MC; Bonotto, DM; Bendassolli, JA				Cohen, Marcelo C. L.; Rodrigues, Erika; Rocha, Denise O. S.; Freitas, Jaine; Fontes, Neuza A.; Pessenda, Luiz C. R.; de Souza, Adriana, V; Gomes, Vivian L. P.; Franca, Marlon Carlos; Bonotto, Daniel M.; Bendassolli, Jose A.			Southward migration of the austral limit of mangroves in South America	CATENA			English	Article						Anthropocene; Drone; Global warming; Laguncularia	SEA-LEVEL CHANGES; CLIMATE-CHANGE; ESTUARINE MANGROVES; LATE QUATERNARY; CHANGE IMPACTS; SOIL MATTER; DOCE RIVER; C/N RATIOS; HOLOCENE; EXPANSION	Temperature influences the global distribution of mangroves, and global warming may be causing a poleward mangrove expansion. Sedimentary features, pollen, and isotopes data from six sediment cores, as well as C-14 datings, indicated a marine transgression during the Holocene, and it contributed to the expansion of tidal flats occupied by saltmarshes. Environmental conditions suitable for mangroves development occurred on the study site during the Holocene, but, according to Pb-210 and C-14 dating, the establishment of mangroves mainly represented by Laguncularia trees only began between similar to 1957 and similar to 1986 (AD) on the studied tidal flats. Spatialtemporal analysis, based on satellite and drone images, revealed a mangrove expansion of similar to 10 ha in the study area between 2003 (96.1 ha) and 2019 (106.1 ha). Nowadays, in the study area, saltmarshes, mainly characterized by Spartina and Acrostichum, are sharing tidal flats with mangroves, represented by Laguncularia (<= 5 m tall) and Avicennia (<= 11 m tall). Probably, the absence of mangroves during the Holocene, followed by their establishment and expansion during the Anthropocene in the subtropical zone, is associated with a migration of the austral mangrove limit into the temperate zone, caused by the gradual increase in winter temperatures. This process may be related to a poleward mangrove migration since the late Holocene, caused by a natural Holocene global warming. However, the industrial-era warming must have intensified the mangrove expansion into temperate zones.	[Cohen, Marcelo C. L.; Rodrigues, Erika; Rocha, Denise O. S.; Freitas, Jaine; Fontes, Neuza A.; de Souza, Adriana, V; Gomes, Vivian L. P.] Fed Univ Para, Grad Program Geol & Geochem, Av Perimentral 2651, BR-66077530 Belem, Para, Brazil; [Pessenda, Luiz C. R.] Univ Sao Paulo, CENA 14C Lab, Av Centenario 303, BR-13400000 Piracicaba, SP, Brazil; [Franca, Marlon Carlos] Fed Inst Para, Av Alm Barroso 1155, BR-66090020 Belem, Para, Brazil; [Bonotto, Daniel M.] Univ Estadual Paulista Julio de Mesquita Filho UN, Inst Geociencias & Ciencias Terra, Rio Claro, SP, Brazil; [Bendassolli, Jose A.] Univ Sao Paulo, CENA Stable Isotopes Lab, Sao Paulo, Brazil	Universidade Federal do Para; Universidade de Sao Paulo; Instituto Federal do Para; Universidade Estadual Paulista; Universidade de Sao Paulo	Cohen, MCL (autor correspondente), Fed Univ Para Brazil, Rua Augusto Correa 01, BR-66075110 Belem, Para, Brazil.	mcohen@ufpa.br	rodrigues, érika do socorro ferreira/CAA-0326-2022; Bonotto, Daniel M/F-3690-2015; Cohen, Marcelo Cancela Lisboa/AAQ-8080-2020; rodrigues, érika do socorro ferreira/AFY-6065-2022; Franca, Marlon/C-7896-2013	Cohen, Marcelo Cancela Lisboa/0000-0001-9892-4719; rodrigues, érika do socorro ferreira/0000-0002-0554-5160; Ruiz Pessenda, Luiz Carlos/0000-0001-9119-8195; Franca, Marlon/0000-0002-3784-7702; Fontes, Neuza/0000-0002-2780-6229	FAPESP [2011/00995-7, 2017/03304-1]; Brazilian Council for Technology and Science-CNPq [307497/2018-6]	FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Brazilian Council for Technology and Science-CNPq	We want to thank the members of the Laboratory of Coastal Dynamic (LADIC-UFPA), Center for Nuclear Energy in Agriculture (CENA-USP), the students from the Laboratory of ChemicalOceanography (UFPA), and Laboratory of C-14 (CENA-USP) for their support. This study was financed by FAPESP (2011/00995-7, 2017/03304-1), and the Brazilian Council for Technology and Science-CNPq (Project #307497/2018-6).	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J	Craveiro, GS; Villas, RNN; Xavier, RP				Craveiro, Gustavo Souza; Nobre Villas, Raimundo Netuno; Xavier, Roberto Perez			A fluid inclusion and stable isotope (O, H, S and C) study of the Archean IOCG Cristalino deposit, Carajas mineral Province, Brazil: Implications to ore genesis	ORE GEOLOGY REVIEWS			English	Article						Cristalino deposit; Iron oxide-copper-gold deposits; Carajas Mineral Province; Fluid inclusions; Stable isotopes		The hydrothermal history of the Archean Cu-Au Cristalino deposit is recorded in moderately to intensely altered host rocks, which evolved from similar to 550 degrees C to similar to 150 degrees C. Distal sodic and proximal calcic-ferric, potassic and propylitic alterations developed successively with variable intensity. Two main mineralization types are also recognized: an earlier one characterized by a chalcopyrite + pyrite + magnetite + Au association that occurs as disseminations and breccias in calcic-ferric zones, and a later one represented by a chalcopyrite +/- pyrite +/- hematite +/- Au association that occurs as breccias and veins mainly in potassic and propylitic zones. Estimated pressures (0.6 to 2.6 Kbar) are consonant with brittle and ductile-brittle deformational environments where both alteration and mineralization took place. The ore-bearing fluid was hot (T as high as similar to 550 degrees C), acidic and hypersaline (55.1% wt. NaCl equiv.) and chemically approached by the H2O-NaCl-CaCl2-CO2 +/- MgCl2 +/- FeCl2 system. Salinity might have exceeded 55 wt% NaCl equiv. in the early alteration stages but decreased progressively to 7.9 wt% NaCl equiv. from 250 degrees C onwards, due to incursion of surficial water into the deposit site. The fluid was initially O-18-enriched and D-depleted (delta O-18(v-smow) = +9.73 to +6.48 parts per thousand; delta Dv-smow = 30.17 to -40.25 parts per thousand) and most likely derived from magmatic sources. As result of dilution caused by mixing with meteoric water, the fluid became relatively O-18-depleted and D-enriched (delta O-18(v-smow) = +5.57 to 0.28 parts per thousand; delta Dv-smow = -19.15 to 22.24%). The delta C-13(v-pdb) values for vein and breccia calcite ( 6.5 to 3.8 parts per thousand) are consistent with a deep source for CO2, likely of mantellic origin. Most delta S-34(v-cdt) values for chalcopyrite show narrow variation (+1.6 to +3.5 parts per thousand) and could indicate a homogeneous reservoir for sulfur. However, a few samples reveal significant influence of sedimentary rocks on their isotope composition (delta S-34(v-cdt) = 32.6 parts per thousand), showing that sulfur may have been sourced from various reservoirs. It is inferred that most Cu and Au were transported as chloride complexes (>350 degrees C), and precipitated in response to decrease in temperature and Cl- activity, and increase in pH. The formation of the chalcopyrite +/- pyrite +/- hematite +/- Au association was especially favored by an oxygen fugacity increase during the late stages of the hydrothermal alteration. Secondary fluid inclusions reveal that an aqueous, colder (200-150 degrees C) and relatively less saline (21-3.1 wt% NaCl equiv.) fluid of uncertain origin circulated in the Cristalino deposit area, which is likely related to a nearby Paleoproterozoic granitic intrusion. In comparison with other Archean Carajas IOCG deposits, particularly those that lie in the southern sector of the Carajas Domain, the Cristalino deposit shows similar structural styles, hydrothermal assemblages, and ore fluid composition and evolution. The data presented here support previous interpretations that consider Cristalino as of IOCG typology.	[Craveiro, Gustavo Souza; Nobre Villas, Raimundo Netuno] Fed Univ Para UFPA, Grad Program Geol & Geochem, Geosci Inst, Rua Augusto Correa,01 Guama,POB 1611, BR-66075110 Belem, PA, Brazil; [Xavier, Roberto Perez] Univ Estadual Campinas, Inst Geociencias, R Joao Pandia Calogeras 51, BR-13083970 Campinas, SP, Brazil	Universidade Federal do Para; Universidade Estadual de Campinas	Craveiro, GS (autor correspondente), Fed Univ Para UFPA, Grad Program Geol & Geochem, Geosci Inst, Rua Augusto Correa,01 Guama,POB 1611, BR-66075110 Belem, PA, Brazil.	craveiro@ufpa.br; netuno@ufpa.br; xavier@ig.unicamp.br		Souza Craveiro, Gustavo/0000-0002-6469-5070				DOCEGEO, 1988, CONGRESSO BRASILEIRO, V35, P11; ZANG W, 1995, MINER DEPOSITA, V30, P30	2	5	5	0	7	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0169-1368	1872-7360		ORE GEOL REV	Ore Geol. Rev.	DEC	2020	127								103822	10.1016/j.oregeorev.2020.103822	http://dx.doi.org/10.1016/j.oregeorev.2020.103822			23	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	PE4HY					2023-06-23	WOS:000598327200001
J	Gorayeb, PSD; Cordani, UG; Neto, JJAD; Sato, K; Maurer, VC				de Sousa Gorayeb, Paulo Sergio; Cordani, Umberto Giuseppe; Andrade da Silva Neto, Juvenal Juarez; Sato, Kei; Maurer, Victor Camara			U-Pb SHRIMP zircon ages of Ediacaran-Cambrian granitic bodies in central Brazil: Implications for the tectonic evolution of the Araguaia belt	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Granitogenesis; Neoproterozoic; Geocronology; Araguaia belt	NORTHERN BRAZIL; NE-BRAZIL; SUITE; DISCRIMINATION; OPHIOLITE; GONDWANA; AFRICAN; RECORDS; BASALTS	The small granitic plutons of the Ramal do Lontra, Presidente Kennedy, Barrolandia and Santa Luzia are emplaced into the Estrondo Group metasedimentary rocks of the Neoproterozoic Araguaia Belt. They have similar petrographic and compositional characteristics and are coeval with the medium-grade regional meta-morphism of the belt. New U-Pb SHRIMP zircon data yielded quite robust ages. These results fall within the experimental error, and the integrated Concordia age of 542 +/- 3 Ma was chosen as representative of their magmatic crystallization. A relevant number of inherited grains are present, showing overgrowth rims with high-U content, formed during the later stage of magmatic crystallization. LA-ICP-MS U-Pb dating on detrital zircon grains from a metasedimentary rock of the Estrondo Group yielded several Paleoproterozoic ages and a few Neoarchean ages, but the major peak in the histogram was between 1000 and 1200 Ma. The youngest grains indicate an Ediacaran age near 600 Ma, which is considered a reasonable upper limit for the deposition of the Estrondo Group. The Araguaia Belt started as an intracontinental system, segmenting the Amazonian Craton, formed by rifting during the breakup of Rodinia and was after occupied by a sedimentary basin which evolved to form an oceanic lithosphere. In the Ediacaran, the huge continental collisions that formed the West Gondwana Orogen most likely caused its remote activation, producing tectonic inversion with vergence to the west. Granitic plutons were emplaced in the last stages of the evolution of the Araguaia Belt, during the Brasiliano-PanAfrican orogenesis, at the Ediacaran-Cambrian boundary.	[de Sousa Gorayeb, Paulo Sergio; Andrade da Silva Neto, Juvenal Juarez] Fed Univ Para, Geosci Inst, Geol & Geochem Grad Program, Belem, PA, Brazil; [Cordani, Umberto Giuseppe; Sato, Kei] Univ Sao Paulo, Geosci Inst, Sao Paulo, SP, Brazil; [Maurer, Victor Camara] Univ Fed Ouro Preto, Ouro Preto, MG, Brazil	Universidade Federal do Para; Universidade de Sao Paulo; Universidade Federal de Ouro Preto	Gorayeb, PSD (autor correspondente), Fed Univ Para, Geosci Inst, Geol & Geochem Grad Program, Belem, PA, Brazil.	gorayebp@ufpa.br; ucordani@usp.br; juvenal@ufpa.br; keisato@usp.br; camaramaurer@gmail.com	Cordani, Umberto/F-3686-2014	Cordani, Umberto/0000-0003-4425-5905	project "Geosciences Institute of Amazonia" (GEOCIAM) -INCT-CNPq/MCT/FAPESPA [573733/2008-2]; project "Petrologia, geochronologia e tectonica das rochas magmaticas do Cinturao Araguaia" (CNPq-Universal Project) [427225/2016-7]; CNPq [132208/2014-8]; Sao Paulo State Research Support Foundation (FAPESP) [13/12754-0]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [13/12754-0] Funding Source: FAPESP	project "Geosciences Institute of Amazonia" (GEOCIAM) -INCT-CNPq/MCT/FAPESPA; project "Petrologia, geochronologia e tectonica das rochas magmaticas do Cinturao Araguaia" (CNPq-Universal Project); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Sao Paulo State Research Support Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	This study was conducted by the research group "Petrology and Crustal Evolution" (CNPq-UFPA) and the Graduate Program in Geology and Geochemistry, Geosciences Institute of the Federal University of Path (PPGG/IG/UFPA). The research was supported by the projects "Geosciences Institute of Amazonia" (GEOCIAM) -INCT-CNPq/MCT/FAPESPA (Proc. No. 573733/2008-2), and "Petrologia, geochronologia e tectonica das rochas magmaticas do Cinturao Araguaia" (CNPq-Universal Project -Proc. No. 427225/2016-7). JJASN would like to thank CNPq for the Master's scholarship (CNPq, Proc. No. 132208/2014-8) and of Maria Rosalva Coelho in behalf of the Geological Survey of Brazil (CPRM-Belem), by help and support during the separation of heavy minerals. UGC would like to thank the Sao Paulo State Research Support Foundation (FAPESP) for the financial support of the project "Geocronologia de precisao pelos metodos U Pb SHRIMP e LA-ICP-MS em zircao: contribuicao para o aprimoramento do conhecimento da evolucao tectonica da America do Sul" (FAPESP -Proc. No. 13/12754-0).	Alvarenga C. J. 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South Am. Earth Sci.	DEC	2020	104								102804	10.1016/j.jsames.2020.102804	http://dx.doi.org/10.1016/j.jsames.2020.102804			19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2UE					2023-06-23	WOS:000600273700003
J	Dillenburg, SR; Barboza, EG; Rosa, MLCC; Caron, F; Cancelli, R; Santos-Fischer, CB; Lopes, RP; Ritter, MD				Dillenburg, Sergio R.; Barboza, Eduardo G.; Rosa, Maria Luiza C. C.; Caron, Felipe; Cancelli, Rodrigo; Santos-Fischer, Cristiane B.; Lopes, Renato P.; do Nascimento Ritter, Matias			Sedimentary records of Marine Isotopic Stage 3 (MIS 3) in southern Brazil	GEO-MARINE LETTERS			English	Article							SEA-LEVEL CHANGES; STRANDPLAIN SYSTEM IMPLICATIONS; TRANSGRESSIVE BARRIER; COASTAL-PLAIN; QUATERNARY; EVOLUTION; CLIMATE; TERRACES	In this paper, a reinterpretation of the older C-14 ages of the Pleistocene substrate of the Holocene barrier-lagoon system of three coastal localities in southern Brazil is presented (Hermenegildo, Cassino, and Curumim). Sedimentological, geochronological, palynological, and diatom analyses of a sedimentary deposit formed in an estuarine/shallow marine environment are examined. This sedimentary deposit is presently found between 22 and 25 m depth below sea level in the Pinheira coastal plain. Results from all studied sites indicate that the deposit was formed under a former sea level of Marine Isotopic Stage 3 (MIS 3) that may have oscillated in the study region between 5 and 23 m depth below present sea level, from 36.2 to 47.7 ka. These results are reinforced by studies of nearby sites, including southeast Brazil. The Pleistocene substrate of the Holocene lagoonal-barrier system, at depths lower than 5 m below sea level, seems to correspond to sedimentary deposits of the Pleistocene barrier formed during MIS 5, while at depths greater than 5 m below sea level, they might correspond to sedimentary deposits that were formed during the relative high sea levels of MIS 3.	[Dillenburg, Sergio R.; Barboza, Eduardo G.; Rosa, Maria Luiza C. C.] Univ Fed Rio Grande do Sul, Ctr Estud Geol Costeira & Ocean, Inst Geociencias, Porto Alegre, RS, Brazil; [Barboza, Eduardo G.; Caron, Felipe; do Nascimento Ritter, Matias] Univ Fed Rio Grande do Sul, Ctr Estud Costeiros Limnol & Marinhos, Campus Litoral, Tramandai, RS, Brazil; [Cancelli, Rodrigo; Santos-Fischer, Cristiane B.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Inst Geociencias, Porto Alegre, RS, Brazil; [Lopes, Renato P.] Univ Fed Santa Catarina, Lab Oceanog Costeira, Florianopolis, SC, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal de Santa Catarina (UFSC)	Dillenburg, SR (autor correspondente), Univ Fed Rio Grande do Sul, Ctr Estud Geol Costeira & Ocean, Inst Geociencias, Porto Alegre, RS, Brazil.	sergio.dillenburg@ufrgs.br	Lopes, Renato Pereira/AFQ-4934-2022; Ritter, Matias/A-1500-2013; Dillenburg, Sergio/C-4027-2013; Barboza, Eduardo Guimarães/C-7579-2012	Lopes, Renato Pereira/0000-0002-4865-6426; Ritter, Matias/0000-0001-8150-4443; Dillenburg, Sergio/0000-0003-0072-7018; Barboza, Eduardo Guimarães/0000-0003-2107-6904				Angulo RJ, 2008, MAR GEOL, V252, P111, DOI 10.1016/j.margeo.2008.03.006; Capitoli Ricardo R., 2004, Atlantica, V26, P27; da Silva ALC, 2014, BRAZ J GEOL, V44, P191, DOI 10.5327/Z2317-4889201400020002; CHAPPELL J, 1986, NATURE, V324, P137, DOI 10.1038/324137a0; Cooper JAG, 2018, MAR GEOL, V397, P1, DOI 10.1016/j.margeo.2017.11.011; Rosa MLCD, 2017, BRAZ J GEOL, V47, P183, DOI 10.1590/2317-4889201720160138; Dillenburg SR, 2017, MAR GEOL, V390, P106, DOI 10.1016/j.margeo.2017.06.007; Dillenburg SR, 2014, GEOL SOC SPEC PUBL, V388, P333, DOI 10.1144/SP388.16; Dillenburg SR, 2014, SEDIMENTOLOGY, V61, P2205, DOI 10.1111/sed.12132; Dillenburg SR, 2009, LECT NOTES EARTH SCI, V107, P53; Fgri K., 1989, J BIOGEOGR, V4th; Gonzalez I, 2008, J STAT SOFTW, V23, P1; Hein CJ, 2013, SEDIMENTOLOGY, V60, P469, DOI 10.1111/j.1365-3091.2012.01348.x; Hesp P.A., 2009, GEOLOGY GEOMORPHOLOG, V107, P53; Heusser CJ, 2006, QUATERNARY SCI REV, V25, P446, DOI 10.1016/j.quascirev.2005.04.008; Howe JA, 2002, MAR GEOL, V191, P55, DOI 10.1016/S0025-3227(02)00498-X; Isla FI, 2016, SPRING EARTH SYST SC, P147, DOI 10.1007/978-3-319-40000-6_8; INMAN DL, 1971, J GEOL, V79, P1, DOI 10.1086/627583; Jara-Munoz J, 2015, QUATERNARY RES, V83, P216, DOI 10.1016/j.yqres.2014.10.002; Lambeck K, 2002, NATURE, V419, P199, DOI 10.1038/nature01089; Lambeck K, 2001, SCIENCE, V292, P679, DOI 10.1126/science.1059549; Lima LG, 2013, J S AM EARTH SCI, V42, P27, DOI 10.1016/j.jsames.2012.07.002; Linsley BK, 1996, NATURE, V380, P234, DOI 10.1038/380234a0; Cohen MCL, 2014, PALAEOGEOGR PALAEOCL, V415, P48, DOI 10.1016/j.palaeo.2013.12.001; Mahiques MM, 2011, AN ACAD BRAS CIENC, V83, P817, DOI 10.1590/S0001-37652011005000028; Pappas JL, 1996, J PHYCOL, V32, P693, DOI 10.1111/j.0022-3646.1996.00693.x; Peltier WR, 2006, QUATERNARY SCI REV, V25, P3322, DOI 10.1016/j.quascirev.2006.04.010; Pico T, 2017, NAT COMMUN, V8, DOI 10.1038/ncomms15612; Pico T, 2016, QUATERNARY SCI REV, V152, P72, DOI 10.1016/j.quascirev.2016.09.012; Rios E. 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J	Dunkl, I; von Eynatten, H; Ando, S; Lunsdorf, K; Morton, A; Alexander, B; Aradi, L; Augustsson, C; Bahlburg, H; Barbarano, M; Benedictus, A; Berndt, J; Bitz, I; Boekhout, F; Breitfeld, T; Cascalho, J; Costa, PJM; Ekwenye, O; Feher, K; Flores-Aqueveque, V; Fuhring, P; Giannini, P; Goetz, W; Guedes, C; Gyurica, G; Hennig-Breitfeld, J; Hulscher, J; Jafarzadeh, M; Jagodzinski, R; Jozsa, S; Kelemen, P; Keulen, N; Kovacic, M; Liebermann, C; Limonta, M; Luzar-Oberiter, B; Markovic, F; Melcher, F; Miklos, DG; Moghalu, O; Mounteney, I; Nascimento, D; Novakovic, T; Obbagy, G; Oehlke, M; Omma, J; Onuk, P; Passchier, S; Pfaff, K; Linconir, LP; Power, M; Razum, I; Resentini, A; Sagi, T; Salata, D; Salgueiro, R; Schonig, J; Sitnikova, M; Sternal, B; Szakmany, G; Szokaluk, M; Thamo-Bozso, E; Toth, A; Tremblay, J; Verhaegen, J; Villasenor, T; Wagreich, M; Wolf, A; Yoshida, K				Dunkl, Istvan; von Eynatten, Hilmar; Ando, Sergio; Luensdorf, Keno; Morton, Andrew; Alexander, Bruce; Aradi, Laszlo; Augustsson, Carita; Bahlburg, Heinrich; Barbarano, Marta; Benedictus, Aukje; Berndt, Jasper; Bitz, Irene; Boekhout, Flora; Breitfeld, Tim; Cascalho, Joao; Costa, Pedro J. M.; Ekwenye, Ogechi; Feher, Kristof; Flores-Aqueveque, Valentina; Fuehring, Philipp; Giannini, Paulo; Goetz, Walter; Guedes, Carlos; Gyurica, Gyorgy; Hennig-Breitfeld, Juliane; Huelscher, Julian; Jafarzadeh, Mahdi; Jagodzinski, Robert; Jozsa, Sandor; Kelemen, Peter; Keulen, Nynke; Kovacic, Marijan; Liebermann, Christof; Limonta, Mara; Luzar-Oberiter, Borna; Markovic, Frane; Melcher, Frank; Miklos, Dora Georgina; Moghalu, Ogechukwu; Mounteney, Ian; Nascimento, Daniel; Novakovic, Tea; Obbagy, Gabriella; Oehlke, Mathias; Omma, Jenny; Onuk, Peter; Passchier, Sandra; Pfaff, Katharina; Pinto Linconir, Luisa; Power, Matthew; Razum, Ivan; Resentini, Alberto; Sagi, Tamas; Salata, Dorota; Salgueiro, Rute; Schoenig, Jan; Sitnikova, Maria; Sternal, Beata; Szakmany, Gyorgy; Szokaluk, Monika; Thamo-Bozso, Edit; Toth, Agoston; Tremblay, Jonathan; Verhaegen, Jasper; Villasenor, Tania; Wagreich, Michael; Wolf, Anna; Yoshida, Kohki			Comparability of heavy mineral data - The first interlaboratory round robin test	EARTH-SCIENCE REVIEWS			English	Article						Heavy mineral analysis; Provenance; SEM-EDX; Raman spectroscopy; Interlaboratory comparison	GRAIN-SIZE DEPENDENCE; FISSION-TRACK; JURASSIC SANDSTONES; PROVENANCE; AGES	Heavy minerals are typically rare but important components of siliciclastic sediments and rocks. Their abundance, proportions, and variability carry valuable information on source rocks, climatic, environmental and transport conditions between source to sink, and diagenetic processes. They are important for practical purposes such as prospecting for mineral resources or the correlation and interpretation of geologic reservoirs. Despite the extensive use of heavy mineral analysis in sedimentary petrography and quite diverse methods for quantifying heavy mineral assemblages, there has never been a systematic comparison of results obtained by different methods and/or operators. This study provides the first interlaboratory test of heavy mineral analysis. Two synthetic heavy mineral samples were prepared with considerably contrasting compositions intended to resemble natural samples. The contributors were requested to provide (i) metadata describing methods, measurement conditions and experience of the operators and (ii) results tables with mineral species and grain counts. One hundred thirty analyses of the two samples were performed by 67 contributors, encompassing both classical microscopic analyses and data obtained by emerging automated techniques based on electron-beam chemical analysis or Raman spectroscopy. Because relatively low numbers of mineral counts (N) are typical for optical analyses while automated techniques allow for high N, the results vary considerably with respect to the Poisson uncertainty of the counting statistics. Therefore, standard methods used in evaluation of round robin tests are not feasible. In our case the 'true' compositions of the test samples are not known. Three methods have been applied to determine possible reference values: (i) the initially measured weight percentages, (ii) calculation of grain percentages using estimates of grain volumes and densities, and (iii) the best-match average calculated from the most reliable analyses following multiple, pragmatic and robust criteria. The range of these three values is taken as best approximation of the 'true' composition. The reported grain percentages were evaluated according to (i) their overall scatter relative to the most likely composition, (ii) the number of identified components that were part of the test samples, (iii) the total amount of mistakenly identified mineral grains that were actually not added to the samples, and (iv) the number of major components, which match the reference values with 95% confidence. Results indicate that the overall comparability of the analyses is reasonable. However, there are several issues with respect to methods and/or operators. Optical methods yield the poorest results with respect to the scatter of the data. This, however, is not considered inherent to the method as demonstrated by a significant number of optical analyses fulfilling the criteria for the best-match average. Training of the operators is thus considered paramount for optical analyses. Electron-beam methods yield satisfactory results, but problems in the identification of polymorphs and the discrimination of chain silicates are evident. Labs refining their electron-beam results by optical analysis practically tackle this issue. Raman methods yield the best results as indicated by the highest number of major components correctly quantified with 95% confidence and the fact that all laboratories and operators fulfil the criteria for the best-match average. However, a number of problems must be solved before the full potential of the automated high-throughput techniques in heavy mineral analysis can be achieved.	[Dunkl, Istvan; von Eynatten, Hilmar; Luensdorf, Keno; Fuehring, Philipp; Schoenig, Jan; Wolf, Anna] Univ Gottingen, Dept Sedimentol & Environm Geol, Geosci Ctr, Goldschmidtstr 3, D-37077 Gottingen, Germany; [Ando, Sergio; Limonta, Mara; Resentini, Alberto] Univ Milano Bicocca, Dept Earth & Environm Sci, Piazza Sci 4, I-20126 Milan, Italy; [Morton, Andrew] HM Res Associates, Musselwick Rd, St Ishmaels SA62 3TJ, Pembrokeshire, Wales; [Alexander, Bruce] Univ Greenwich, Sch Sci, Cent Ave, Chatham ME4 4TB, Kent, England; [Aradi, Laszlo] Eotvos Lorand Univ, Lithosphere Fluid Res Lab, Pazmany P Setany 1-C, H-1117 Budapest, Hungary; [Augustsson, Carita] Inst Energiressurser, N-4036 Stavanger, Norway; [Bahlburg, Heinrich; Boekhout, Flora] Westfalische Wilhelms Univ, Inst Geol & Palaontol, Corrensstr 24, D-48149 Munster, Germany; [Barbarano, Marta] Chemostrat Ltd 1, Ravenscroft Court, Buttington Enterprise Pk, Welshpool SY21 85L, Wales; [Benedictus, Aukje; Omma, Jenny] Rocktype Ltd, 87 Divin Rd, Oxford OX4 1LN, England; [Berndt, Jasper] Westfalische Wilhelms Univ, Inst Mineral, Corrensstr 24, D-48149 Munster, Germany; [Bitz, Irene] Landesamt Bergbau Energie & Geol Geozentrum, Hannover, Germany; [Breitfeld, Tim; Hennig-Breitfeld, Juliane; Liebermann, Christof] Royal Holloway Univ London, Earth Sci Dept, SE Asia Res Grp, Queens Bldg,Egham Hill, Egham TW20 0EX, Surrey, England; [Cascalho, Joao] Univ Lisbon, Inst D Luiz, Edificio C6, P-1749016 Lisbon, Portugal; [Cascalho, Joao] Univ Lisbon, Dept Geol, Edificio C6, P-1749016 Lisbon, Portugal; [Costa, Pedro J. M.] Univ Coimbra, Dept Ciencias Terra, Coimbra, Portugal; [Ekwenye, Ogechi; Moghalu, Ogechukwu] Univ Nigeria, Dept Geol, Nsukka 410001, Enugu State, Nigeria; [Feher, Kristof; Jozsa, Sandor; Kelemen, Peter; Miklos, Dora Georgina; Sagi, Tamas; Szakmany, Gyorgy; Toth, Agoston] Eotvos Lorand Univ, Dept Petr & Geochem, Pazmany P Setany 1-C, H-1117 Budapest, Hungary; [Flores-Aqueveque, Valentina] ARQMAR Ctr Maritime Archaeol Res Southeastern Pac, Casilla 21, Valparaiso 2340000, Chile; [Giannini, Paulo] Univ Sao Paulo, Inst Geosci, Rua Lago,562 Cidade Univ, BR-05508080 Sao Paulo, Brazil; [Goetz, Walter; Oehlke, Mathias] Max Planck Inst Sonnensystemforschung, Justus von Liebig Weg,3, D-37077 Gottingen, Germany; [Guedes, Carlos] Univ Fed Parana, Geol Dept, 210 Jardim Amer, BR-81531980 Curitiba, Parana, Brazil; [Gyurica, Gyorgy] Min & Geol Survey Hungary, Dept Appl & Environm Geol, Stefania Ut 14, H-1143 Budapest, Hungary; [Hennig-Breitfeld, Juliane] Royal Holloway Univ London, Dept Earth Sci, Egham Hill, Egham TW20 0EX, Surrey, England; [Huelscher, Julian] Free Univ Berlin, Inst Geol Wissensch Tekton & Sedimentare Syst, Malteserstr 74-100, D-12249 Berlin, Germany; [Jafarzadeh, Mahdi] Shahrood Univ Technol, Fac Earth Sci, Hafte Tir Sq, Shahrood, Iran; [Jagodzinski, Robert; Sternal, Beata] Adam Mickiewicz Univ, Inst Geol, Geohazards Lab, Bogumila Krygowskiego 12, PL-61680 Poznan, Poland; [Keulen, Nynke] Geol Survey Denmark & Greenland, Dept Petr & Econ Geol, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark; [Kovacic, Marijan; Markovic, Frane] Univ Zagreb, Inst Mineral & Petr, Dept Geol, Horvatovac 95, HR-10000 Zagreb, Croatia; [Luzar-Oberiter, Borna; Novakovic, Tea] Univ Zagreb, Dept Geol, Geologko Paleontologki Zavod, Fac Sci,Prirodoslovno Matemat Fak, Horvatovac 102, HR-10000 Zagreb, Croatia; [Melcher, Frank; Onuk, Peter] Univ Leoben, Chair Geol & Econ Geol, Peter Tunner Str 5, A-8700 Leoben, Austria; [Mounteney, Ian] British Geol Survey, Hill Keyworth, Nottingham NG12 5GG, England; [Nascimento, Daniel] Univ Fed Ceara, Dept Geol, Campus PICI,Bloco 912, BR-60440554 Fortaleza, CE, Brazil; [Obbagy, Gabriella] Hungarian Acad Sci, Inst Nucl Res, Bem Sq 18-c, H-4026 Debrecen, Hungary; [Passchier, Sandra] Montclair State Univ, Dept Earth & Environm Studies, CELS 220,1 Normal Ave, Montclair, NJ 07043 USA; [Pfaff, Katharina] Colorado Sch Mines, 1516 Illinois St, Golden, CO 80401 USA; [Pinto Linconir, Luisa; Villasenor, Tania] Univ Chile, Dept Geol, FCFM, Plaza Ercilla 803,Casilla 13518,Correo 21, Santiago, Chile; [Power, Matthew] SGS Canada Inc, Oil Gas & Chem Serv, 3260 Prod Way, Burnaby, BC V5A 4W4, Canada; [Razum, Ivan] Croatian Nat Hist Museum, Demetrova 1, HR-10000 Zagreb, Croatia; [Salata, Dorota] Jagiellonian Univ, Inst Geol Sci, Fac Geog & Geol, Gronostajowa 3a, PL-30387 Krakow, Poland; [Salgueiro, Rute] LNEG Lab Nacl Energia & Geol, Estr Portela,Apartado 7586-Alfragide, P-2610999 Amadora, Portugal; [Sitnikova, Maria] BGR B2 1 Geophys Erkundung Tech Mineral, Stilleweg 2, D-30655 Hannover, Germany; [Szokaluk, Monika] Adam Mickiewicz Univ, Inst Geol, Dept Mineral & Petr, Str Bogumila Krygowskiego 12, PL-61680 Poznan, Poland; [Thamo-Bozso, Edit] Min & Geol Survey Hungary, Dept Geol Basic Res, Stefania Ut 14, H-1143 Budapest, Hungary; [Tremblay, Jonathan] IOS Serv Geosci Inc, 1319 St Paul Blvd, Quebec City, PQ G7J 3Y2, Canada; [Verhaegen, Jasper] Katholieke Univ Leuven, Dept Earth & Environm Sci, Celestijnenlaan 200E, B-3001 Heverlee, Belgium; [Wagreich, Michael] Univ Vienna, Dept Geodynam & Sedimentol, Ctr Earth Sci, Althanstr 14, A-1090 Vienna, Austria; [Yoshida, Kohki] Shinshu Univ, Dept Geol, Fac Sci, Asahi 3-1-1, Matsumoto, Nagano 3908621, Japan	University of Gottingen; University of Milano-Bicocca; University of Greenwich; Eotvos Lorand University; University of Munster; University of Munster; University of London; Royal Holloway University London; Universidade de Lisboa; Universidade de Lisboa; Universidade de Coimbra; University of Nigeria; Eotvos Lorand University; Universidade de Sao Paulo; Max Planck Society; Universidade Federal do Parana; University of London; Royal Holloway University London; Free University of Berlin; Shahrood University of Technology; Adam Mickiewicz University; Geological Survey Of Denmark & Greenland; University of Zagreb; University of Zagreb; University of Leoben; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universidade Federal do Ceara; Eotvos Lorand Research Network; Hungarian Academy of Sciences; Hungarian Institute for Nuclear Research; Montclair State University; Colorado School of Mines; Universidad de Chile; Jagiellonian University; Laboratorio Nacional de Energia e Geologia IP (LNEG); Adam Mickiewicz University; KU Leuven; University of Vienna; Shinshu University	Dunkl, I (autor correspondente), Univ Gottingen, Dept Sedimentol & Environm Geol, Geosci Ctr, Goldschmidtstr 3, D-37077 Gottingen, Germany.	istvan.dunkl@geo.uni-goettingen.de; hilmar.von.eynatten@geo.uni-goettingen.de; sergio.ando@unimib.it; kluensd@gwdg.de; heavyminerals@hotmail.co.uk; B.Alexander@greenwich.ac.uk; aradi.laszloelod@gmail.com; carita.augustsson@uis.no; bahlbur@uni-muenster.de; martabarbarano@chemostrat.com; aukje.benedictus@rocktype.com; jberndt@uni-muenster.de; Irene.Bitz@lbeg.niedersachsen.de; boekhout@uni-muenster.de; t.breitfeld@es.rhul.ac.uk; jpcascalho@fc.ul.pt; ppcosta@dct.uc.pt; ogechi.ekwenye@unn.edu.ng; lorcs@hotmail.hu; v.flores.a@gmail.com; philipp.fuehring@stud.uni-goettingen.de; pcgianni@usp.br; goetz@mps.mpg.de; ccfguedes@gmail.com; gyuricza.gyorgy@mbfsz.gov.hu; j.hennig@es.rhul.ac.uk; julian.huelscher@fu-berlin.de; m_jafarzadeh@shahroodut.ac.ir; jagodus@amu.edu.pl; sandor-jozsa@caesar.elte.hu; kelemenpeter1991@gmail.com; ntk@geus.dk; marijan.kovacic@gfz.hr; chris.liebermann@gmail.com; mara.limonta@unimib.it; bluzar@geol.pmf.hr; frane.markovic@geol.pmf.hr; Frank.Melcher@unileoben.ac.at; miklosdoragina94@gmail.com; ogechukwu.moghalu@unn.edu.ng; iaian1@bgs.ac.uk; daniel.rodrigues@ufc.br; teanovakovic@gmail.com; obbagy.gabriella@atomki.mta.hu; oehlke@gmx.de; jenny.omma@rocktype.com; Peter.Onuk@unileoben.ac.at; passchiers@mail.montclair.edu; kpfaff@mines.edu; lpinto@ing.uchile.cl; matt@powerotero.com; irazum@hpm.hr; alberto.resentini@unimib.it; sagi.tamas@ttk.elte.hu; dorota.salata@uj.edu.pl; rute.salgueiro@lneg.pt; jan.schoenig@uni-goettingen.de; MariaAlexandrovna.Sitnikova@bgr.de; sternal@amu.edu.pl; szakmany@caesar.elte.hu; monika.szokaluk@amu.edu.pl; bozso.edit@mbfsz.gov.hu; toth.agoston01@gmail.com; jtremblay@iosgeo.com; jasper.verhaegen@kuleuven.be; tania.villasenor.j@gmail.com; michael.wagreich@univie.ac.at; anna.fe@gmx.de; kxyoshid@shinshu-u.ac.jp	Costa, Pedro JM/I-1216-2012; Jafarzadeh/AAH-8368-2020; Jagodziński, Robert/B-5155-2019; Villaseñor, Tania/U-3226-2017; Razum, Ivan/GLV-1374-2022; Passchier, Sandra/AAQ-2243-2021; Flores-Aqueveque, Valentina/Q-8688-2016; Guedes, Carlos Conforti Ferreira/F-3639-2015; Passchier, Sandra/GYU-2381-2022; Villaseñor, Tania/GNE-7379-2022; Verhaegen, Jasper/S-5729-2019; Giannini, Paulo César Fonseca/D-1871-2015; Keulen, Nynke/G-9235-2018; Schönig, Jan/AAI-1455-2020; Aradi, László Előd/AAK-9147-2020; Salgueiro, Rute/AHA-0574-2022; Cascalho, Joao/J-8644-2013	Costa, Pedro JM/0000-0001-6573-0539; Jagodziński, Robert/0000-0002-8469-215X; Villaseñor, Tania/0000-0002-8353-3130; Passchier, Sandra/0000-0001-7204-7025; Guedes, Carlos Conforti Ferreira/0000-0001-8816-9174; Villaseñor, Tania/0000-0002-8353-3130; Verhaegen, Jasper/0000-0002-9629-2655; Giannini, Paulo César Fonseca/0000-0003-1046-0177; Keulen, Nynke/0000-0002-3257-0468; Schönig, Jan/0000-0001-9296-7582; Aradi, László Előd/0000-0003-0276-3119; Salgueiro, Rute/0000-0002-3740-2965; Flores-Aqueveque, Valentina/0000-0003-2388-3363; Yoshida, Kohki/0000-0002-1379-0975; von Eynatten, Hilmar/0000-0002-2823-3194; Limonta, Mara/0000-0002-3535-4971; Breitfeld, H. Tim/0000-0002-9563-1862; Thamo-Bozso, Edit/0000-0003-4152-847X; Wagreich, Michael/0000-0002-8828-0857; Alexander, Bruce/0000-0002-6377-7197; Lunsdorf, Nils Keno/0000-0002-2738-8469; Kelemen, Peter/0000-0002-3964-9056; Cascalho, Joao/0000-0001-7831-1069; Miklos, Dora Georgina/0009-0009-1774-8510; Pfaff, Katharina/0000-0002-6605-2722; Razum, Ivan/0000-0002-9764-0666	NERC [bgs06001] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Ando S, 2020, MINERALS-BASEL, V10, DOI 10.3390/min10030273; Ando S, 2014, GEOL SOC SPEC PUBL, V386, P395, DOI 10.1144/SP386.2; Ando S, 2012, SEDIMENT GEOL, V280, P165, DOI 10.1016/j.sedgeo.2012.03.023; Ando S, 2011, REND LINCEI-SCI FIS, V22, P327, DOI 10.1007/s12210-011-0142-4; Ando S, 2009, SPECTROCHIM ACTA A, V73, P450, DOI 10.1016/j.saa.2008.11.005; [Anonymous], 2017, ISO 18310 1 E, P1, DOI DOI 10.1109/IEEESTD.2017.8016712; [Anonymous], 2003, E130195 ASTM ASTM IN; [Anonymous], 2012, D7778 ASTM ASTM INT; [Anonymous], 2005, 22971 ISOTR; [Anonymous], 2013, E691 ASTM ASTM INT; [Anonymous], 2017, SEDIMENT ROUTING SYS; Artini E., 1891, GIORNALE MINERALOGIA, VII, P177; Bernstein S, 2008, J GEOCHEM EXPLOR, V96, P25, DOI 10.1016/j.gexplo.2007.06.002; Boenigk W., 1983, SCHWER MINERAL ANAL; Boswell P.G.H., 1933, MINERALOGY SEDIMENTA; Caracciolo L, 2020, GEOL SOC SPEC PUBL, V484, P275, DOI 10.1144/SP484-2018-136; CHAYES F, 1949, AM MINERAL, V34, P1; Dick A.B., 1887, NATURE, V36, P91; DICKINSON WR, 1979, AAPG BULL, V63, P2164; DODSON MH, 1988, J GEOL SOC LONDON, V145, P977, DOI 10.1144/gsjgs.145.6.0977; Finkelman R.B., 1984, 932 USGS; Fleet WF, 1926, GEOL MAG, V63, P505, DOI 10.1017/S0016756800085484; GALBRAITH RF, 1990, NUCL TRACKS RAD MEAS, V17, P207; GALBRAITH RF, 1988, TECHNOMETRICS, V30, P271, DOI 10.2307/1270081; Garzanti E, 2008, EARTH PLANET SC LETT, V273, P138, DOI 10.1016/j.epsl.2008.06.020; Garzanti E, 2019, MINERALS-BASEL, V9, DOI 10.3390/min9030148; Garzanti E, 2009, EARTH PLANET SC LETT, V277, P422, DOI 10.1016/j.epsl.2008.11.007; Gonfiantini R, 2003, GEOSTANDARD NEWSLETT, V27, P41, DOI 10.1111/j.1751-908X.2003.tb00711.x; Hackley PC, 2015, MAR PETROL GEOL, V59, P22, DOI 10.1016/j.marpetgeo.2014.07.015; Heroy DC, 2003, SEDIMENT GEOL, V155, P343, DOI 10.1016/S0037-0738(02)00186-0; Hubert J.F., 1962, J SEDIMENT PETROL, V32, P440, DOI DOI 10.1306/74D70CE5-2B21-11D7-8648000102C1865D; International Organization for Standardization, 2010, 11432010 ISO, P1; International Organization for Standardization (ISO), 2015, IEEE STD 80 2013 REV, P1, DOI [DOI 10.1109/IEEESTD.2015.7118618, DOI 10.1109/IEEESTD.2015.7106435, DOI 10.1109/IEEESTD.2015.7109078]; Ketcham RA, 2015, AM MINERAL, V100, P1452, DOI 10.2138/am-2015-5167; Kosler J, 2013, GEOSTAND GEOANAL RES, V37, P243, DOI 10.1111/j.1751-908X.2013.00245.x; KROGH TE, 1982, GEOCHIM COSMOCHIM AC, V46, P637, DOI 10.1016/0016-7037(82)90165-X; Ludwig K. 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DEC	2020	211								103210	10.1016/j.earscirev.2020.103210	http://dx.doi.org/10.1016/j.earscirev.2020.103210			27	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PG6JW		Green Published			2023-06-23	WOS:000599840700003
J	Freitas, L; Appolinario, L; Calegario, G; Campeao, M; Tschoeke, D; Garcia, G; Venancio, IM; Cosenza, CAN; Leomil, L; Bernardes, M; Albuquerque, AL; Thompson, C; Thompson, F				Freitas, Lucas; Appolinario, Luciana; Calegario, Gabriela; Campeao, Mariana; Tschoeke, Diogo; Garcia, Gizele; Venancio, Igor Martins; Cosenza, Carlos A. N.; Leomil, Luciana; Bernardes, Marcelo; Albuquerque, Ana Luiza; Thompson, Cristiane; Thompson, Fabiano			Glacial-interglacial transitions in microbiomes recorded in deep-sea sediments from the western equatorial Atlantic	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Metagenomics; Sediment core; Bioindicator; Amazon river; Microbiome modulation	ORGANIC-MATTER; BACTERIA; TERRESTRIAL; QUALITY; OCEAN	In the late Quaternary, glacial-interglacial transitions are marked by major environmental changes. Glacial periods in the western equatorial Atlantic (WEA) are characterized by high continental terrigenous input, which increases the proportion of terrestrial organic matter (e.g. lignin, alkanes), nutrients (e.g. iron and sulphur), and lower primary productivity. On the other hand, interglacials are characterized by lower continental contribution and maxima in primary productivity. Microbes can serve as biosensors of past conditions, but scarce information is available on deep-sea sediments in the WEA. The hypothesis put forward in this study is that past changes in climate conditions modulated the taxonomic/functional composition of microbes from deep sediment layers. To address this hypothesis, we collected samples from a marine sediment core located in the WEA, which covered the last 130 kyr. This region is influenced by the presence of the Amazon River plume, which outputs dissolved and particulate nutrients in vast oceanic regions, as well as the Parnaiba river plume. Core GL-1248 was analysed by shotgun metagenomics and geochemical analyses (alkane, lignin, perylene, sulphur). Two clusters (glacial and interglacial-deglacial) were found based on taxonomic and functional profiles of metagenomes. The interglacial period had a higher abundance of genes belonging to several sub-systems (e.g. DNA, RNA metabolism, cell division, chemotaxis, and respiration) that are consistent with a past environment with enhanced primary productivity. On the other hand, the abundance of Alcanivorax, Marinobacter, Kangiella and aromatic compounds that may serve as energy sources for these bacteria were higher in the glacial. The glacial period was enriched in genes for the metabolism of aromatic compounds, lipids, isoprenoids, iron, and Sulphur, consistent with enhanced fluvial input during the last glacial period. In contrast, interglacials have increased contents of more labile materials originating from phytoplankton (e.g. Prochlorococcus). This study provides new insights into the microbiome as climatic archives at geological timescales. (C) 2020 Published by Elsevier B.V.	[Freitas, Lucas; Appolinario, Luciana; Calegario, Gabriela; Campeao, Mariana; Tschoeke, Diogo; Garcia, Gizele; Thompson, Cristiane; Thompson, Fabiano] Fed Univ Rio De Janeiro UFRJ, Inst Biol, Rio De Janeiro, Brazil; [Freitas, Lucas; Appolinario, Luciana; Calegario, Gabriela; Campeao, Mariana; Tschoeke, Diogo; Garcia, Gizele; Cosenza, Carlos A. N.; Leomil, Luciana; Thompson, Cristiane; Thompson, Fabiano] Univ Fed Rio de Janeiro, COPPE, SAGE, Rio de Janeiro, Brazil; [Venancio, Igor Martins] Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Cachoeira Paulista, Brazil; [Venancio, Igor Martins; Bernardes, Marcelo; Albuquerque, Ana Luiza] Fed Fluminense Univ, Gradutate Program Geosci Geochem, Niteroi, RJ, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Instituto Nacional de Pesquisas Espaciais (INPE); Universidade Federal Fluminense	Thompson, C; Thompson, F (autor correspondente), Fed Univ Rio De Janeiro UFRJ, Inst Biol, Rio De Janeiro, Brazil.; Albuquerque, AL (autor correspondente), Fed Fluminense Univ, Gradutate Program Geosci Geochem, Niteroi, RJ, Brazil.	ana_albuquerque@id.uff.br; thompsoncristiane@gmail.com; fabianothompson1@gmail.com	Venancio, Igor M/I-5893-2014; Tschoeke, Diogo A/F-9913-2019; Garcia, Gizele Duarte/GLS-9270-2022; Tschoeke, Diogo/AAB-4739-2021; Bernardes, Marcelo/H-7869-2012; Albuquerque, Ana Luiza S/C-5167-2013; Freitas, Lucas/S-2923-2016	Venancio, Igor M/0000-0003-3118-4247; Tschoeke, Diogo A/0000-0001-8134-4259; Garcia, Gizele Duarte/0000-0001-9844-6729; Bernardes, Marcelo/0000-0002-4338-4353; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Thompson, Fabiano/0000-0002-7562-1683; Freitas, Lucas/0000-0002-8766-0890	CNPq; CAPES; FAPERJ	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	The authors thank CNPq, CAPES, and FAPERJ.	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Total Environ.	DEC 1	2020	746								140904	10.1016/j.scitotenv.2020.140904	http://dx.doi.org/10.1016/j.scitotenv.2020.140904			10	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	OC7XQ	32763595				2023-06-23	WOS:000579371300014
J	Garcia, VB; Schutesky, ME; Oliveira, CG; Whitehouse, MJ; Huhn, SRB; Augustin, CT				Garcia, Victor B.; Schutesky, Maria Emilia; Oliveira, Claudinei G.; Whitehouse, Martin J.; Huhn, Sergio R. B.; Augustin, Claudia T.			The Neoarchean GT-34 Ni deposit, Carajas mineral Province, Brazil: An atypical IOCG-related Ni sulfide mineralization	ORE GEOLOGY REVIEWS			English	Article						IOCG; Carajas; Orthopyroxene-scapolite alteration; hydrothermal Ni sulfide deposit	OXIDE-COPPER-GOLD; U-PB GEOCHRONOLOGY; HYDROTHERMAL ALTERATION; INCIPIENT CHARNOCKITE; AMAZONIAN CRATON; GREENSTONE-BELT; CHLORIDE COMPLEXES; YILGARN CRATON; RE-OS; MAGMATISM	The GT-34 deposit, located 12 km to the SW of the Sossego copper-gold mine in the Carajas Province, northern Brazil, represents an unusual Ni sulfide mineralization. The deposit occurs along a NE-SW-trending sub-vertical shear zone marked by progressive Mg-alkalic alteration zones, predominantly hosted in granitic and locally in granodioritic to tonalitic orthogneisses. Initial alteration zones result in unique scapolite-orthopyroxene assemblage, which is partially preserved within pervasive hornblende-chlorapatite +/- plagioclase replacement zones. Nickel mineralization occurs mainly as matrix-supported breccias characterized by a pentlandite-pyrrhotite-rich matrix and rounded fragments chiefly of hornblende and chlorapatite. Irregular stockworks and net textured veins containing chalcopyrite-pentlandite are less common. Phlogopite +/- talc +/- actinolite alteration and late-stage veinlets crosscut the previous alteration zones and the mineralization. The phlogopite +/- talc +/- actinolite alteration occurs as irregular veins and chalcopyrite-pyrrhotite-magnetite are commonly observed where such alteration intersects the Ni mineralization. Late-stage veinlets are represented by K feldspar-epidotechlorite-calcite and quartz-albite-chlorite-calcite-epidote veins, both containing minor amounts of millerite, pyrite and F-OH-apatite. High-resolution SIMS U-Pb zircon geochronology obtained for the GT-34 deposit revealed an age of 2828 +/- 4 Ma for zircon grains inherited from the host orthogneisses. The timing of the mineralization altered zircon grains from the scapolite-orthopyroxene and phlogopite +/- talc +/- actinolite alteration zones, is attributed to an age interval between 2751 and 2720 Ma. Although poorly constrained, the geochronological data corroborate a Neoarchean age for the GT-34 Ni mineralization, similar to that of other IOCG deposits in the Carajas Province and coeval with the bimodal magmatism in the area. The atypical orthopyroxene-marialite mineral chemistry support a metasomatic crystallization at high temperatures (> 700 degrees C), low aH2O (< 0.5) and pressures between 5 and 7 kbar. Hypersaline fluids, as the ones described for the IOCG deposits in Carajas at such PxT conditions, would enable the orthopyroxene-marialite crystallization, as supported by experimental studies available in the literature. Mineralogical and geochemical considerations on the nature of the Ni sulfide mineralization points toward a metasomatic origin, feasible with the predicted P-T-fluid scenario for the hydrothermal alteration. Such conditions raise the initial temperature and pressure estimates of the IOCG metasomatic alteration by at least 200 degrees C and pressure up to 7 kbar, making it the hottest and probably deepest IOCG-related metasomatic alteration known to date for Carajas.	[Garcia, Victor B.; Schutesky, Maria Emilia] Univ Ottawa, Ottawa, ON, Canada; [Garcia, Victor B.; Schutesky, Maria Emilia; Oliveira, Claudinei G.; Augustin, Claudia T.] Univ Brasilia, Brasilia, DF, Brazil; [Whitehouse, Martin J.] Swedish Museum Nat Hist, Dept Geosci, Box 50007, SE-10405 Stockholm, Sweden; [Huhn, Sergio R. B.] Univ Ceara, Fortaleza, Ceara, Brazil	University of Ottawa; Universidade de Brasilia; Swedish Museum of Natural History; Universidade Estadual do Ceara	Schutesky, ME (autor correspondente), Univ Ottawa, Ottawa, ON, Canada.; Schutesky, ME (autor correspondente), Univ Brasilia, Brasilia, DF, Brazil.	emiliadellagiustina.unb@gmail.com	Schutesky, Maria/L-9910-2015	Schutesky, Maria/0000-0001-8516-102X	CNPq; Swedish Research Council; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Swedish Research Council(Swedish Research CouncilSwedish Research Council for Health Working Life & Welfare (Forte)Swedish Research Council Formas); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors appreciate the logistical support provided by VALE during sampling. Fernando Matos, Wolney Rosa and Denisson Oliveira are acknowledged for the discussions on the Carajas metallogeny and the constructive commentaries on the GT-34 deposit. The authors are thankful for the continuous financial support received from CNPq and from The Swedish Research Council. This study was also financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001. Finally, we would like to thank Dr. Lena Monteiro, as guest editor, for her constructive comments, and Dr. David Howell, Dr. Peter Pollard and two anonymous reviewers, whose suggestions significantly improved the paper.	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Rev.	DEC	2020	127								103773	10.1016/j.oregeorev.2020.103773	http://dx.doi.org/10.1016/j.oregeorev.2020.103773			19	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	PF0UK					2023-06-23	WOS:000598779600001
J	da Silva, IMG; de Moura, WAL; Correia, OJ; Carrino, TA; Correa, MM; Neto, JAD				Gomes da Silva, Isis Mayara; Lima de Moura, Willian Alexandre; Correia Filho, Osvaldo Jose; Carrino, Thais Andressa; Correa, Marcelo Metri; de Souza Neto, Joao Adauto			Early evidence of pyrometamorphism and a late hydrothermal alteration related to Albian volcanism in the Pernambuco sedimentary basin, northeast Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Ipojuca magmatic suite; Buchite; Argillic alteration; Pernambuco basin	EASTERN BORBOREMA PROVINCE; REFLECTANCE SPECTROSCOPY; NE BRAZIL; GEOCHEMISTRY; SUPERGENE; PROSPECT; DEPOSITS; HYPOGENE; ORIGIN; MAGMA	Pyrometamorphic aureoles and late hydrothermal alterations linked to Albian alkaline volcanism of the Ipojuca Magmatic Suite are described for the first time in the Pernambuco Basin, northeast Brazil. Field features, petrography, scanning electron microscopy (SEM-WDS), reflectance spectroscopy and X-ray diffraction data were used to characterize the mineral assemblage related to these two geological features. The pyrometamorphic aureoles occur when trachybasalts and arcosian sandstones (upper Cabo Formation) are in contact and were classified as buchites, due to the mineral assemblage composed of mullite, spinel (hercynite), tridymite, pyrrhotite and montmorillonite. The sanidinite facies (high temperature and lower pressure) is attributed to the mineral assemblage described above. Regarding the late hydrothermal alteration, two main events occurred in shallow conditions (up to 1 km). The first event is marked by an argillic alteration along NE-SW and NW-SE faults and fractures. The mineral assemblage is composed of kaolinite, quartz and minor magnetite. This alteration is also characterized by a reflectance spectral signature demonstrated by the high crystallinity of kaolinite that could also indicate its hypogene origin, in temperatures ranging from 100 to 250 degrees C. The second event is characterized by amygdales and veinlets in basalts lava flows that are filled with smectite (e.g montmorillonite), the formation of which is attributed to alkaline hydrothermal fluids with temperatures between 75 and 150 degrees C. Both events have been associated with the same fluid source. However, the first event occurred at higher temperatures and with acidic fluids, while the second presented lower temperatures and alkaline fluids.	[Gomes da Silva, Isis Mayara; Lima de Moura, Willian Alexandre; Correia Filho, Osvaldo Jose; Carrino, Thais Andressa; de Souza Neto, Joao Adauto] Univ Fed Pernambuco, Programa Pos Grad Geociencias, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Carrino, Thais Andressa; de Souza Neto, Joao Adauto] Univ Fed Pernambuco, Dept Geol, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Correa, Marcelo Metri] Univ Fed Rural Pernambuco, Dept Agron, Ave Born Pastor Boa Vista,S-N, BR-55292272 Garanhuns, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal Rural de Pernambuco (UFRPE)	da Silva, IMG (autor correspondente), Univ Fed Pernambuco, Programa Pos Grad Geociencias, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil.	isismayara.gomes@gmail.com	Carrino, Thais Andressa/AAH-1292-2020; Correa, Marcelo/AAI-1232-2021; Souza Neto, João Adauto/D-6810-2016; Neto, João Adauto Souza/AAG-6672-2021	Carrino, Thais Andressa/0000-0001-8528-5225; Correa, Marcelo/0000-0003-0929-4634; Souza Neto, João Adauto/0000-0002-9870-7113; Neto, João Adauto Souza/0000-0002-9870-7113; Gomes da Silva, Isis Mayara/0000-0001-9533-6989	National Council for Scientific and Technological Development (CNPq); CNPq [312.275/2017-0]	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	I.M.G.S, W.A.L.M and O.J.C.F authors are grateful to the National Council for Scientific and Technological Development (CNPq) for the graduate scholarships. J.A.S.N is also grateful to CNPq for his research grant (process number 312.275/2017-0). All authors also thank Dr. Carlos Roberto de Souza Filho and Dr. Rebecca Scafutto (UNICAMP) for providing access to the ASD-FieldSpec, and Dr. Edval Santos (Devices and Nanostructures Laboratory-UFPE) for the SEM-WDS data. Our thanks also go to Prof. Carlinda Campelo for her contribution in helping to interpret the XRD data. We also thank the two anonymous reviewers and regional editor Martin Valencia-Moreno for the comments that improved the first version of this manuscript.	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South Am. Earth Sci.	DEC	2020	104								102907	10.1016/j.jsames.2020.102907	http://dx.doi.org/10.1016/j.jsames.2020.102907			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TS					2023-06-23	WOS:000600272500001
J	Hueck, M; Wemmer, K; Basei, MAS; Philipp, RP; Oriolo, S; Heidelbach, F; Oyhantcabal, P; Siegesmund, S				Hueck, Mathias; Wemmer, Klaus; Basei, Miguel A. S.; Philipp, Ruy P.; Oriolo, Sebastian; Heidelbach, Florian; Oyhantcabal, Pedro; Siegesmund, Siegfried			Dating recurrent shear zone activity and the transition from ductile to brittle deformation: White mica geochronology applied to the Neoproterozoic Dom Feliciano Belt in South Brazil	JOURNAL OF STRUCTURAL GEOLOGY			English	Article						Shear zones; Ductile-brittle transition; White mica Ar geochronology; Strain localization; Structural inheritance; Brasiliano/Pan-African orogenic cycle	DE-LA-PLATA; PB-HF ISOTOPES; EDIACARAN PORONGOS GROUP; U-PB; PARANA BASIN; ZIRCON GEOCHRONOLOGY; SOUTHERNMOST BRAZIL; TECTONIC EVOLUTION; PELOTAS BATHOLITH; 40AR/39AR GEOCHRONOLOGY	Argon geochronology of white mica has a good potential of recording recurrent dynamic recrystallization in shear zones in the transition from ductile to brittle deformation, as temperature ranges for mineral crystallization and isotopic closure of different grain-size fractions overlap between ca. 275-425 degrees C. This study presents over 40 K-Ar ages of coarse-grained muscovite and multiple clay-sized white mica fractions extracted from mylonites and fault gouges in southernmost Brazil, complemented by detailed structural and XRD characterization. The widespread obtained ages are best explained in the context of recurrent deformation under retrograde conditions during progressive strain localization and transition from low-grade ductile deformation into brittle faulting. The onset of the Ibar ' e Shear Zone is constrained in the Tonian, followed by reactivation during the Ediacaran evolution of the adjacent Dom Feliciano Belt, which records a remarkable long-term history of recurrent deformation for over 100 Myr. New data extends the geochronological constraints of the Dorsal do Cangucu Shear Zone into low-temperature conditions, estimating the onset of brittle activity at 525-470 Ma by dating early fault gouges formed shortly after final syn-kinematic white mica crystallization in the hosting mylonites. Dating of recurrent faulting events during the Paleo-Mesozoic complement the regional sedimentary and thermochronological record.	[Hueck, Mathias; Basei, Miguel A. S.] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil; [Hueck, Mathias; Wemmer, Klaus; Siegesmund, Siegfried] Georg August Univ Gottingen, Geosci Ctr, Gottingen, Germany; [Philipp, Ruy P.] Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil; [Oriolo, Sebastian] Univ Buenos Aires, CONICET, Inst Geociencias Basicas Aplicadas & Ambientales, Buenos Aires, DF, Argentina; [Heidelbach, Florian] Univ Bayreuth, Bayer Geoinst, Bayreuth, Germany; [Oyhantcabal, Pedro] Univ Republica, Inst Ciencias Geol, Montevideo, Uruguay	Universidade de Sao Paulo; University of Gottingen; Universidade Federal do Rio Grande do Sul; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires; University of Bayreuth; Universidad de la Republica, Uruguay	Hueck, M (autor correspondente), Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil.	mathiashueck@gmail.com	Basei, Miguel A S/C-1915-2013	Basei, Miguel A S/0000-0002-3857-7089; Hueck, Mathias/0000-0001-8911-4124; PHILIPP, RUY PAULO/0000-0003-2875-0914	CNPq; FAPESP [2015/03737-0]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	M. Hueck thanks CNPq for a PhD scholarship within the Science Without Borders Program and FAPESP for a post-doctoral fellowship. M. A.S. Basei and M. Hueck thank FAPESP for funding from the Thematic Project 2015/03737-0. R.P. Philipp thanks CNPq for a researcher fellowship grant. M. Hueck thanks Caio A. Santos and Jessica Lima for very helpful assistance during field work. Joao Hippertt and an anonymous reviewer offered constructive and encouraging suggestions that improved the manuscript.	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Struct. Geol.	DEC	2020	141								104199	10.1016/j.jsg.2020.104199	http://dx.doi.org/10.1016/j.jsg.2020.104199			22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OZ9PN					2023-06-23	WOS:000595250500015
J	Bellos, LI; Diaz-Alvarado, J; Lopez, JP; Rodriguez, N; Nagle, AEA; Tassinari, CCG; Altenberger, U; Schleicher, A				Iudith Bellos, Laura; Diaz-Alvarado, Juan; Pablo Lopez, Jose; Rodriguez, Natalia; Acosta Nagle, Ana Eugenia; Gaeta Tassinari, Colombo Celso; Altenberger, Uwe; Schleicher, Anja			The juxtaposition of Cambrian and early Ordovician magmatism in the Tafi del Valle area. Characteristics and recognition of Pampean and Famatinian magmatic suites in the easternmost Sierras Pampeanas	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Silica-rich granitic rocks; Petrogenesis; AFC process; Famatinian magmatic arc; Pampean belt; Southwestern Gondwana	S-TYPE GRANITES; PROTO-ANDEAN MARGIN; HF-ISOTOPE DATA; NW ARGENTINA; NORTHWESTERN ARGENTINA; WESTERN GONDWANA; SOUTH-AMERICA; METAMORPHIC EVOLUTION; IGNEOUS ROCKS; FOLD BELT	Along more than 1000 km, the boundary between the Pampean and Famatinian belts separates the Cambrian magmatism to the east (540-515 Ma) from the easternmost granitic rocks ascribed to the Famatinian orogeny to the west (early Ordovician). The geochronological and geochemical study presented in this work has revealed the first Cambrian magmatism in the Sierras de Aconquija and Cumbres Calchaquies at the northeastern edge of the Famatinian belt. Pabell ' on (522 +/- 2.8 Ma) and Nunorco Grande (478.3 +/- 2.3 Ma) intrusive units form part of the small plutons exposed together in the Tafi del Valle area, which have been related according to their geochemical characteristics. The good correlation observed between ages and characteristic geochemical signatures have motivated the comparison with other intrusive complexes along the Pampean and eastern Famatinian belts, resulting in regional diagnostic geochemical features and a petrogenetic and evolutive proposal for the Cambrian and early Ordovician magmatism in the eastern Sierras Pampeanas. Easternmost early Ordovician granitic rocks constitute a calcic, weak to moderately peraluminous series. They are Sr-rich tonalitic to monzogranitic magmas (SiO2 >62 %wt.) with steep REE patterns, positive and negative Eu anomalies, high Sr/Y and moderate Ce/Yb ratios. Accordingly, the water-fluxed melting of a mafic source under high to moderate pressures may be involved in the origin of silicaand Ca-rich parental magma. The shallower evolution of these melts consists of Pl-dominated fractionation trends that finally constituted Pl-rich crystal mushes (tonalites) and more felsic residual liquids. Regarding Cambrian granodiorites and monzogranites, any petrogenetic scheme must consider the magnesian, high-K calc-alkalic characteristics for a short-range silica variation, low to moderate peraluminosity and high zircon saturation temperatures (>850 degrees C). Source conditions are determined by the presence of Pl and Hbl in the solid assemblage based on the REE patterns. These geochemical characteristics point to the extensive HT-LP melting of a dominantly crustal source, probably assisted by the injection of hot H2O-rich mafic melts.	[Iudith Bellos, Laura; Pablo Lopez, Jose; Acosta Nagle, Ana Eugenia] UNT, CONICET, INSUGEO, Fac Ciencias Nat, Miguel Lillo 205, RA-4000 San Miguel De Tucuman, Tucuman, Argentina; [Iudith Bellos, Laura; Pablo Lopez, Jose; Acosta Nagle, Ana Eugenia] UNT, IML, Miguel Lillo 205, RA-4000 San Miguel De Tucuman, Tucuman, Argentina; [Diaz-Alvarado, Juan] Inst Geol & Minero Espana IGME, C Rios Rosas 23, Madrid 28003, Spain; [Diaz-Alvarado, Juan] Univ Huelva, Dept Ciencias Tierra, Campus El Carmen, Huelva 21071, Spain; [Rodriguez, Natalia] Univ Atacama, Dept Geol, Copayapu 485, Copiapo, Chile; [Gaeta Tassinari, Colombo Celso] Univ Sao Paulo, High Resolut Geochronol Lab, Rua Lago 562, Sao Paulo, SP, Brazil; [Altenberger, Uwe] Univ Potsdam, Inst Geoschiences, Potsdam, Germany; [Schleicher, Anja] German Res Ctr Geosci GFZ, Helmholtz Ctr, Potsdam, Germany	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad Nacional de Tucuman; Universidad Nacional de Tucuman; Universidad de Huelva; Universidad de Atacama; Universidade de Sao Paulo; University of Potsdam; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences	Bellos, LI (autor correspondente), UNT, CONICET, INSUGEO, Fac Ciencias Nat, Miguel Lillo 205, RA-4000 San Miguel De Tucuman, Tucuman, Argentina.; Bellos, LI (autor correspondente), UNT, IML, Miguel Lillo 205, RA-4000 San Miguel De Tucuman, Tucuman, Argentina.	laubel@csnat.unt.edu.ar		LOPEZ, JOSE PABLO/0000-0003-2320-7090; Schleicher, Anja/0000-0003-4052-8654	FONDECYT of CONICYT [11140722]; DIUDA [2016-22320]; PIUNT [26/G623]	FONDECYT of CONICYT(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDECYT); DIUDA; PIUNT	This study has been funded with FONDECYT Project No.11140722 of CONICYT, with the fund support of DIUDA 2016-22320 and PIUNT 26/G623 projects. We would like to express our gratitude to the staff of the Geochronological Research Center of the University of Sao Paulo for their kindness and facility and to Antje Musiol and Dr. Christina Gunter for their help in the geochemical laboratories. We are grateful to the reviewers, to Dr. Juan Otamendi and another anonymous reviewer, their comments allowed us to improve the manuscript, and to Dr. Pablo Alasino for editorial handling.	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South Am. Earth Sci.	DEC	2020	104								102878	10.1016/j.jsames.2020.102878	http://dx.doi.org/10.1016/j.jsames.2020.102878			23	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2UL					2023-06-23	WOS:000600274400004
J	Justo, AP; Dantas, EL; Bau, M; Freitas-Silva, FH; Santos, RV; Schorscher, JHD				Justo, Ana Paula; Dantas, Elton Luiz; Bau, Michael; Freitas-Silva, Flavio Henrique; Santos, Roberto Ventura; Daniel Schorscher, Johann Hans			Paleobasinal to band-scale REE plus Y distribution in iron formations from Carajas, Amazon Craton, Brazil	ORE GEOLOGY REVIEWS			English	Article						Carajas; Banded iron formations; REE plus Y; GOE; Neoarchean-Paleoproterozoic transition	RARE-EARTH-ELEMENTS; MID-ATLANTIC RIDGE; SERRA-DOS-CARAJAS; GRAO-PARA GROUP; TRACE-ELEMENT; MINAS-GERAIS; SCHIST BELT; ND ISOTOPES; QUADRILATERO FERRIFERO; HYDROTHERMAL FLUIDS	Banded Iron Formations (BIFs) from the Carajas Mineral Province (CMP), southeastern Amazonian Craton, are the protolith of the world-class iron deposits of the CMP. Besides being one of the largest iron ore deposits in the world, they recorded important paleoenvironmental and regional geodynamic markers across the NeoarcheanPaleoproterozoic transition. We investigate the secular variation of geochemical signature, from several deposit of Carajas Province. The low contents of Al2O3 and of 19 other immobile trace elements (e.g., Zr, Th, Hf, Ti) in 26 high-resolution detritus-free BIF samples indicate their detritus- free nature. Their positive shale-normalized (subscript SN) La and Gd anomalies are similar to those of modern seawater; whereas their Y/Ho ratios are higher. These BIF samples also display large positive chondrite-normalized (subscript CN) Eu anomalies, reflecting the influence of high-temperature hydrothermal vents and bottom solutions. In contrast to modern seawater and to most other Neoarchean/Paleoproterozoic detritus-free BIFs, the Carajas BIFs do not show the typical heavy rare earth element (REE) enrichment relative to light REE; instead they do show variable light to heavy REE fractionation trends (YbSN/PrSN ratios: 0.05-4.91). The Th/U ratios of both bulk BIFs and mesobands are generally lower than the upper-crustal ratio. Although the bulk BIFs show mostly chondritic values, the individual Fe and Si bands exhibit distinctly higher ratios. The general absence of negative CeSN anomalies attests for rather reducing paleoenvironmental conditions. Unlike the great majority of the data which lack negative anomalies of Ce, a few samples do display such anomalies, which may be compatible to the oxidizing conditions shown by the low Th/U ratios of most the Carajas BIFs. Such low Th/U ratios may register terrestrial weathering conditions, which cause preferential U input into the oceans in response to the oxidation of immobile ;U4+ to more mobile U6+.	[Justo, Ana Paula; Dantas, Elton Luiz; Freitas-Silva, Flavio Henrique; Santos, Roberto Ventura] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Justo, Ana Paula] Serv Geol Brasil, Sao Paulo, Brazil; [Bau, Michael] Jacobs Univ Bremen gGmbH, Dept Phys & Earth Sci, Bremen, Germany; [Daniel Schorscher, Johann Hans] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil	Universidade de Brasilia; Jacobs University; Universidade de Sao Paulo	Justo, AP (autor correspondente), Geol Survey Brazil CPRM SGB, Superintendencia Reg Sao Paulo, Rua Costa 55, BR-01304010 Sao Paulo, Brazil.	ana.justo@cprm.gov.br	Dantas, Elton Luiz/AAK-8464-2021; Bau, Michael/D-4457-2016	Dantas, Elton Luiz/0000-0002-7954-5059; Bau, Michael/0000-0002-7746-3762	CNPq [308312/2014-7, 454272/2014-6]; CAPES [133242/2016-01]; IG-UnB; CPRM; Vale S.A.	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); IG-UnB; CPRM; Vale S.A.	We acknowledge CNPq (308312/2014-7 and 454272/2014-6) and CAPES (133242/2016-01) for providing research funding; the support from the Geological Survey of Brazil (CPRM) for the field campaigns and from Vale S.A for granting access to the mining areas and to drillcore material. We also acknowledge the technical/financial support given by IG-UnB, CPRM and Vale S.A. to the confection of thin-sections, preparation and analyzes of the geochemical and isotopic samples. We are very grateful to the Geochemistry Lab team of Jacobs University Bremen, for the support on the high-resolution geochemistry analyses. We also appreciate the valuable comments on the manuscript of OGR reviewers S. Hagemann and K. Konhauser.	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Rev.	DEC	2020	127								103750	10.1016/j.oregeorev.2020.103750	http://dx.doi.org/10.1016/j.oregeorev.2020.103750			22	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	PF2RM					2023-06-23	WOS:000598908200001
J	Kuchenbecker, M; Pedrosa-Soares, AC; Babinski, M; Reis, HLS; Atman, D; da Costa, RD				Kuchenbecker, Matheus; Pedrosa-Soares, Antonio Carlos; Babinski, Marly; Reis, Humberto Luis Siqueira; Atman, Dora; da Costa, Ricardo Diniz			Towards an integrated tectonic model for the interaction between the Bambui basin and the adjoining orogenic belts: Evidences from the detrital zircon record of syn-orogenic units	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Gondwana; Sao Francisco craton; Aracuai orogen; Brasilia belt; Bambui foreland system	SAO-FRANCISCO CRATON; NEOPROTEROZOIC MACAUBAS GROUP; WEST-CONGO OROGEN; ARACUAI OROGEN; U-PB; FOREBULGE GRABENS; EASTERN BRAZIL; BRASILIA BELT; SE BRAZIL; EVOLUTION	The Sao Francisco craton and its surrounding orogens are some of the most important tectonic elements of South America, and key regions to understanding the assembly of Western Gondwana in the Proterozoic-Palaeozoic transition. During this major tectonic event, diachronic collisions between small continents developed an intricated orogenic system, where several orogens evolved in unique paths through time and space. In such collisional settings, there are some tectonic processes that promote subsidence, thus controlling the formation of orogenic-related sedimentary basins. Furthermore, the tectonic activity in collisional orogens generates dynamic landscapes that usually favor increased erosion and sediment generation to feed these basins, making them key places to seek for clues about the tectonic evolution of their surroundings. On the Sao Francisco craton, the Bambui Group records a complex foreland system, which evolved in response to the lithospheric overload exerted by the uplift of both Brasilia belt and Aracuai orogen. In turn, both Salinas Formation and Ibi ' a Group comprise orogenic deposits resting within the Aracuai orogen and Brasilia belt, respectively, whose tectonic significance is still under debate. Here we present new U-Pb (LA-ICP-MS and SHRIMP) and Lu-Hf isotopic analyses on a great amount of detrital zircon grains extracted from the rocks of the Bambui Group and Salinas Formation, together with a thorough data compilation from the literature. The two units present similar provenance patterns, sharing the major detrital zircon age peaks (550-650 Ma, 950-1050 Ma, 1750-2000 Ma, 2600-2800 Ma) and maximum depositional age in c. 550 Ma. The Ediacaran zircons recovered from the Bambui Group show a wide range of the epsilon Hf(t), ranging from c.-17 to +15, which suggest the existence of multiple late Neoproterozoic sources, some of them juvenile and some with a long crustal residence. The variation in detrital zircon age patterns and epsilon Hf(t) values from different units within the Bambui Group provided additional clues of provenance changes occurred during the evolution of the basin. The new data obtained for the Salinas Formation constrain its deposition between 548 and 500 Ma, which have an important implication on its tectonic significance. We propose that in both Brasilia belt and Aracuai orogen sides, the early foredeep deposits of the Bambui basin should have been incorporated to the orogenic domains, which could explain the apparent lack of deposits recording the climax of the Brasilia belt uplift (c. 630 Ma) within the cratonic area. In this same direction, we consider that both Salinas Formation and Ibia Group could represent remnants of these early foreland deposits related to the uplift of Brasilia belt and Aracuai orogen, respectively, incorporated to the orogenic wedges due to the advance of the deformational fronts. Therefore, what we know as Bambui Group is in fact the remaining record of an advanced stage of the foreland system, when subsidence was already influenced by the two evolving orogens. Altogether, the analyses of the stratigraphic, structural and geochronological data converge towards an integrated tectonic model for the interaction between the Bambuf basin and the surrounding orogens during West Gondwana amalgamation.	[Kuchenbecker, Matheus] Univ Fed Vales Jequitinhonha & Mucuri, Inst Ciencia & Tecnol, Lab Estudos Tecton, Ctr Estudos Geociencias, Diamantina, MG, Brazil; [Kuchenbecker, Matheus; Pedrosa-Soares, Antonio Carlos; da Costa, Ricardo Diniz] Univ Fed Minas Gerais, Inst Geociencias, Ctr Pesquisa Prof Manoel Teixeira da Costa, BR-31270901 Belo Horizonte, MG, Brazil; [Babinski, Marly] Univ Sao Paulo, Inst Geociencias, Ctr Pesquisas Geocronol, Sao Paulo, SP, Brazil; [Reis, Humberto Luis Siqueira] Univ Fed Ouro Preto, Dept Geol, Escola Minas, Lab Modelagem Tecton, Ouro Preto, Brazil; [Atman, Dora] Hidrovia SA, Itaituba, Brazil	Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM); Universidade Federal de Minas Gerais; Universidade de Sao Paulo; Universidade Federal de Ouro Preto	Pedrosa-Soares, AC (autor correspondente), Univ Fed Vales Jequitinhonha & Mucuri, Inst Ciencia & Tecnol, Lab Estudos Tecton, Ctr Estudos Geociencias, Diamantina, MG, Brazil.	matheusk@ict.ufvjm.edu.br; pedrosa@pq.cnpq.br; babinski@usp.br; humbertosiqueira@gmail.com; doraabh@gmail.com; biduufmg@gmail.com	Kuchenbecker, Matheus/P-9876-2016; Reis, Humberto L S/P-9902-2016; Babinski, Marly/B-9403-2013	Kuchenbecker, Matheus/0000-0003-2974-839X; Reis, Humberto L S/0000-0002-7675-789X; Babinski, Marly/0000-0003-2444-2404	CODEMIG; Brazilian research and development agency: CNPq [309106/2017-6]; Brazilian research and development agency: FAPESP; Brazilian research and development agency: FAPEMIG [CRA -APQ-02459-16]; Brazilian research and development agency: CODEMIG; Brazilian research and development agency: CPRM	CODEMIG; Brazilian research and development agency: CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Brazilian research and development agency: FAPESP; Brazilian research and development agency: FAPEMIG; Brazilian research and development agency: CODEMIG; Brazilian research and development agency: CPRM	This paper integrates a JSAES Special Issue in tribute to Marcio Pimentel, whose investigations were essential to the geoscientific knowledge of South America. The authors acknowledge financial support provided by the CODEMIG mapping projects and by Brazilian research and development agencies: CNPq (309106/2017-6), FAPESP, FAPEMIG (CRA -APQ-02459-16), CODEMIG and CPRM. We also thank the staff of the geochronological laboratories of the University of Sao Paulo and Australian National University. M. Kuchenbecker, A. C. Pedrosa-Soares and M. Babinski are fellows of the Brazilian Research Council and acknowledge its support. We are also grateful to Prof. Patrice Baby and an anonymous JSAES reviewer, whose suggestions greatly improved this manuscript.	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J	Leitzke, FP; Gervasoni, F; Simoes, M; Sommer, CA; de Lima, E; Conceicao, RV				Leitzke, F. P.; Gervasoni, F.; Simoes, M. S.; Sommer, C. A.; de Lima, E. F.; Conceicao, R. V.			Magmatic evolution of ediacaran alkali rhyolites from the Acampamento Velho volcanism in the Tupanci area, southern Brazil: A study based on mineral chemistry, LA-ICP-MS Ti-in-quartz and zircon saturation geothermometry	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Rhyolites; Ediacaran; Geothermometry; Post-collisional; Volcanism; Brasiliano/pan-african orogeny	RIO-GRANDENSE SHIELD; DOM FELICIANO BELT; A-TYPE GRANITES; U-PB; AMAZONIAN CRATON; NEOPROTEROZOIC-III; RUTILE SATURATION; MILDLY ALKALINE; INTRUSIVE SUITE; RAMADA PLATEAU	Post-eruptive, metamorphic, and weathering processes are issues that affect not only the identification of geochemical signature but also mineral paragenesis on ancient volcanic successions. Still, the estimate of pressure, temperature and oxygen fugacity conditions prevalent during magma crystallization can be achieved for volcanic systems of any age by combining experimental, thermodynamic and natural data using geothermobarometers. In this regard, highly resistant minerals such as zircon and quartz can provide key information on the origin and evolution of silicic magmatic chambers. For example, the substitution of Ti4+ for Si4+ in quartz is a function of the activity of TiO2 in the magma and in the crystal, temperature and pressure. Therefore, the aim of this study is to apply Ti-in-quartz (TitaniQ) coupled to Zircon saturation geothermometry to provide a better insight into the igneous processes that originated post-collisional Ediacaran sodic-alkaline rhyolites from the Acampamento Velho in southern Brazil. Zircon saturation geothermometry estimates range from ca. 825 degrees C-1000 degrees C (within an error of similar to 25 degrees C), in agreement with previously reported zircon crystallization temperatures for the Acampamento Velho volcanism in the Ramada and Taquaremb ' o plateaus. Temperature estimates using the Ti in quartz thermometer range from 700 to 710 degrees C for the intrusive rocks and from 710 to 810 degrees C for the lava flows that show quartz zonation. The Ti zonation pattern in quartz was probably generated by partial phenocryst dissolution in response to a magma chamber recharge and increase in the pre-eruption temperature. This type of process could be similar to the injection of mafic melts rich in volatiles that originated giant magma bodies, indicating that the Acampamento Velho volcanism was likely formed in a supereruption event with associated caldera collapse, as previously evidenced by detailed petrography studies in other occurrences in the Sul-Rio-Grandense shield.	[Leitzke, F. P.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ctr Estudos Petr & Geoquim, Lab Geol Isotap, BR-91509900 Porto Alegre, RS, Brazil; [Leitzke, F. P.; Conceicao, R. V.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ctr Estudos Petr & Geoquim, Lab Geoquim & Petr Expt, BR-91509900 Porto Alegre, RS, Brazil; [Gervasoni, F.] Univ Fed Goias, Fac Ciencias & Tecnol, BR-74968755 Aparecida De Goiania, Brazil; [Sommer, C. A.; de Lima, E. F.; Conceicao, R. V.] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Pasgrad Geociencias, BR-91509900 Porto Alegre, RS, Brazil; [Simoes, M. S.] Companhia Pesquisa Recursos Minerals CPRM, Serv Geol Brasil, Superintendencia Reg Manaus AM, BR-69067375 Manaus, Amazonas, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal de Goias; Universidade Federal do Rio Grande do Sul	Leitzke, FP (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ctr Estudos Petr & Geoquim, Lab Geol Isotap, BR-91509900 Porto Alegre, RS, Brazil.	felipe.leitzke@ufrgs.br	Conceição, Rommulo Vieira/D-6030-2014; Gervasoni, Fernanda/C-5947-2018; Sommer, Carlos A/Q-9077-2018; DE LIMA, EVANDRO FERNANDES/AAA-8150-2020	Conceição, Rommulo Vieira/0000-0001-7934-7098; Gervasoni, Fernanda/0000-0002-9533-4008; Sommer, Carlos A/0000-0001-8696-7084; DE LIMA, EVANDRO FERNANDES/0000-0002-4101-3161; Simoes, Matheus/0000-0003-2012-6738	Brazilian National Council for Scientific and Technological Development (CNPq) [248562/2013-4]	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We acknowledge the Brazilian National Council for Scientific and Technological Development (CNPq-grant 248562/2013-4) for a PhD. scholarship to F.P.L. Editor A. Folguera and two anonymous reviewers are thanked for valuable comments and inputs that improved the quality of the manuscript.	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South Am. Earth Sci.	DEC	2020	104								102814	10.1016/j.jsames.2020.102814	http://dx.doi.org/10.1016/j.jsames.2020.102814			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TT					2023-06-23	WOS:000600272600005
J	dos Santos, JPL; Lobato, AKDL; Moraes, C; Cunha, AD; Marques, JJ; dos Santos, LCL				Lobo dos Santos, Joao Paulo; de Carvalho Lima Lobato, Ana Katerine; Moraes, Caetano; Cunha, Acto de Lima; Marques, Jose Jailton; Lobato dos Santos, Luiz Carlos			Simulation and scale-up of the desulphurization of gas streams by adsorption method using numerical simulation	JOURNAL OF NATURAL GAS SCIENCE AND ENGINEERING			English	Article						Natural gas; Hydrogen sulfide; Adsorption; Scale-up; Simulation	FIXED-BED ADSORPTION; HYDROGEN-SULFIDE H2S; NATURAL-GAS; SOUR GAS; ELEMENTAL SULFUR; REMOVAL; ZEOLITE; CO2; DEPOSITION	Natural Gas usually contains H2S as a major contaminant, and its presence in gas streams can lead to corrosion of equipment and pipelines. Adsorption is a commonly used technique for removing sulfur compounds from gas streams at low concentrations. The desulphurization process is very complex, requiring experimental and pilot scale studies before the development of a full-scale adsorption column. Such studies often involve simulation and scale-up techniques. Approaches for scale-up techniques applied to the removal of H2S from natural gas in real conditions of transport lacks discussions in the literature. The present study aimed to perform a scale-up of experimental pilot-scale equilibrium data for the real conditions of natural gas transport through gas pipelines using numerical simulation. We evaluated the influence of operating parameters (bed length/diameter ratio, pressure, and temperature) on the removal of H2S from a gas stream in the range of 1.5-3.5, 50-110 bar, and 298-328 K, respectively. The predicted results match real process data providing the elaboration of a scale-up for gas transport conditions in a pipeline. The results showed that at the confidence level of 95%, only pressure was statistically significant, and the optimization of operating conditions increased the amount adsorbed in the equilibrium from 3.71 to 4.70 mol/kg. Bed saturation time was estimated for different operating flows, and the results are in agreement with data reported in the literature.	[Lobo dos Santos, Joao Paulo; Cunha, Acto de Lima] Univ Fed Sergipe, Petr Engn Core, Ave Marechal Rondon S-N, BR-49100000 Sao Cristovao, SE, Brazil; [de Carvalho Lima Lobato, Ana Katerine] Univ Salvador, Sch Exact & Technol Sci, R Dr Jose Peroba,251-Stiep, BR-41770235 Salvador, BA, Brazil; [Moraes, Caetano] Univ Fed Rio de Janeiro, Dept Chem Engn, Ave Horario Macedo 2030, BR-21941909 Rio De Janeiro, RJ, Brazil; [Marques, Jose Jailton] Univ Fed Sergipe, Dept Environm Engn, Ave Marechal Rondon S-N, BR-49100000 Sao Cristovao, SE, Brazil; [Lobato dos Santos, Luiz Carlos] Univ Fed Bahia, Postgrad Program Chem Engn, R Prof Aristides Novis,2-2 Andar, BR-40210630 Salvador, BA, Brazil	Universidade Federal de Sergipe; Universidade Salvador (UNIFACS); Universidade Federal do Rio de Janeiro; Universidade Federal de Sergipe; Universidade Federal da Bahia	dos Santos, JPL (autor correspondente), Univ Fed Sergipe, Petr Engn Core, Ave Marechal Rondon S-N, BR-49100000 Sao Cristovao, SE, Brazil.	jplobo2011@gmail.com	Santos, Luiz Carlos Lobato/F-2805-2013; Santos, Joao/AAJ-5807-2020; LOBATO, A. K. C. LIMA/F-2815-2013	Santos, Luiz Carlos Lobato/0000-0003-3824-7802; Santos, Joao/0000-0003-2947-718X; LOBATO, A. K. C. LIMA/0000-0003-2006-5074	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001.	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Nat. Gas Sci. Eng.	DEC	2020	84								103693	10.1016/j.jngse.2020.103693	http://dx.doi.org/10.1016/j.jngse.2020.103693			10	Energy & Fuels; Engineering, Chemical	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Engineering	PB8VW					2023-06-23	WOS:000596593100002
J	Lopes, RL; Santos-Mallet, JR; Barbosa, CF; Gomes, SAO; Spiegel, CN				Lopes, Rosane L.; Santos-Mallet, Jacenir R.; Barbosa, Catia F.; Gomes, Suzete A. O.; Spiegel, Carolina N.			Morphological and ultrastructural analysis of an important place of sexual communication of Rhodnius prolixus (Heteroptera: Reduviidae): the Metasternal Glands	TISSUE & CELL			English	Article						Rhodnius prolixus; Metasternal Glands; Light microscopy; Electron microscopy; Sex pheromone	PHEROMONE PRODUCTION; TRIATOMA-INFESTANS; TRYPANOSOMA-CRUZI; BRINDLEYS GLANDS; FINE-STRUCTURE; HEMIPTERA; BUG; PSYCHODIDAE; PHYSIOLOGY; VOLATILES	Rhodnius prolixus is an important vector of Trypanosoma cruzi, the etiological agent of Chagas disease. Insect adults have a pair of Metasternal Glands (MGs) and the secretion emitted by these glands acts as sex pheromone. Recent studies have focused on the chemical composition of this pheromone, electrophysiological responses to MGs compounds and mating behavior assays. Morphological studies of these glands are still scarce. Thus, considering the relevance of MGs in the sex pheromone biosynthesis, we investigated the morphology and ultrastructure of R. prolixus MGs. The glandular apparatus presents a tubular structure containing secretory cells with canalicules that fuse with the central duct which conducts the secretion to a pear-shaped reservoir connected to the exterior by a droplet-shape orifice. The secretory cells are classified as class III, they present a welldeveloped rough and smooth endoplasmic reticulum. Smooth endoplasmic reticulum is a site of lipid biosynthesis that may be involved in the mevalonate pathway, a probable route of the sex pheromone biosynthesis in this insect. The presence of rough endoplasmic reticulum indicates a possible peptides/proteins secretions site which were still not characterized in MGs. Several mitochondria are scattered in the cytoplasm that may suggest a high metabolic activity. Further studies should be carried out to correlate these data with the sex pheromone biosynthesis in this vector.	[Lopes, Rosane L.; Gomes, Suzete A. O.; Spiegel, Carolina N.] Univ Fed Fluminense, Inst Biol, Postgrad Program Sci & Biotechnol, Niteroi, RJ, Brazil; [Lopes, Rosane L.; Gomes, Suzete A. O.] Univ Fed Fluminense, Inst Biol, Dept Biol Geral, Lab Insects & Pathogen Biodivers, Niteroi, RJ, Brazil; [Santos-Mallet, Jacenir R.] Fundacao Oswaldo Cruz FIOCRUZ, Inst Oswaldo Cruz IOC, Interdisciplinary Lab Entomol Surveillance Dipter, Rio De Janeiro, RJ, Brazil; [Santos-Mallet, Jacenir R.] Univ Iguacu UNIG, Nova Iguagu, RJ, Brazil; [Barbosa, Catia F.] Univ Fed Fluminense, Inst Quim, Dept Geoquim, Niteroi, RJ, Brazil; [Spiegel, Carolina N.] Univ Fed Fluminense, Inst Biol, Dept Biol Celular & Mol, Niteroi, RJ, Brazil	Universidade Federal Fluminense; Universidade Federal Fluminense; Fundacao Oswaldo Cruz; Universidade Federal Fluminense; Universidade Federal Fluminense	Gomes, SAO (autor correspondente), Univ Fed Fluminense, Inst Biol, Postgrad Program Sci & Biotechnol, Niteroi, RJ, Brazil.; Gomes, SAO (autor correspondente), Univ Fed Fluminense, Inst Biol, Dept Biol Geral, Lab Insects & Pathogen Biodivers, Niteroi, RJ, Brazil.	rosanelopes@id.uff.br; jacenir@ioc.fiocruz.br; catiafb@id.uff.br; suzetearaujo@id.uff.br; carolinaspiegel@id.uff.br	Mallet, Jacenir Reis dos Santos/GRO-4228-2022; Mallet, Jacenir R S/F-5001-2017		Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors are grateful to Plataforma Microscopia EletronicaUniversidade Federal Fluminense, Nucleo de Estudos em Agua e Biomassa (NAB) -Universidade Federal Fluminense-Niteroi-Brazil, Plataforma de Microscopia Eletronica Rudolf Barth-Fundacao Oswaldo Cruz-Rio de Janeiro-Brazil, Laboratorio Interdisciplinar de vigilancia Entomologica em Diptera e Hemiptera Instituto Oswaldo Cruz/Fundacao Oswaldo Cruz Rio de Janeiro-Brazil, Dr. Maria Denise Feder (Laboratorio de Biologia de Inseto/Universidade Federal Fluminense-Niteroi-Brazil) and R. prolixus Colony (Instituto de Bioquimica Medica/Universidade Federal do Rio de Janeiro-Rio de Janeiro-Brazil) for technical assistance. 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J	Macedo, RJA; Pereira, NS; Manso, VAV				Macedo, R. J. A.; Pereira, N. S.; Manso, V. A. V.			Morphometric analysis of the Inner Continental Shelf in northeastern Brazil for seabed geomorphic classification	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Digital terrain analysis; Inner shelf; Geomorphometry; Reefs; Paleo-lagoon; Paleo-spit	CORAL-REEFS; TERRAIN; INTERPOLATION; GEOMETRY; FEATURES; LINKING	Advances in geomorphometry have allowed geoscientists to map landscapes through digital terrain analysis, although seascapes still remain poorly described as compared to continental area. We carried out a systematic morphometric analysis of the inner continental shelf using bathymetric data at Tamandare', in northeastern Brazil. The methodology was based on the extraction of primary terrain attributes from an interpolated digital surface model of the study area, with descriptive statistics, and geomorphic classifications. The combination of maps and data analysis provided a new geomorphic feature classification of the region. At least four reef steps occur at five paleo-terrace boundaries. Additionally, a new shelf valley location is defined at shallow depths that is connected to a submerged paleo-coastal lagoon at approximately -20 m, fronted by a paleo-spit, and backed by a possible beach ridge. The orientations of those two ancient bottom landforms suggest structural control by normal faults of the Pernambuco Basin.	[Macedo, R. J. A.] Univ Fed Vale Sao Francisco UNIVASF, Colegiado Ciencias Nat, Sao Raimundo Nonato, Piaui, Brazil; [Pereira, N. S.] Univ Estado Bahia UNEB, Paulo Afonso, BA, Brazil; [Manso, V. A. V.] Univ Fed Pernambuco UFPE, Dept Geol, Lab Geol & Geofis Marinha LGGM, Recife, PE, Brazil	Universidade Federal do Vale do Sao Francisco; Universidade do Estado Bahia; Universidade Federal de Pernambuco	Macedo, RJA (autor correspondente), Univ Fed Vale Sao Francisco UNIVASF, Colegiado Ciencias Nat, Sao Raimundo Nonato, Piaui, Brazil.	rene.macedo@univasf.edu.br	Macêdo, Renê J A/J-9731-2012; Pereira, Natan S/A-9643-2015	Macêdo, Renê J A/0000-0001-5943-6317; Pereira, Natan S/0000-0002-3307-2655				Camargo J.M.R., 2007, REV BRASILEIRA GEOF, V25, P79, DOI DOI 10.1590/S0102-261X2007000500008; Castro CB, 2001, B MAR SCI, V69, P357; Conti LA, 2009, BRAZ J OCEANOGR, V57, P113, DOI 10.1590/S1679-87592009000200004; Costa MBSF, 2016, GEOMORPHOLOGY, V253, P318, DOI 10.1016/j.geomorph.2015.11.001; Ferreira Junior A.V., 2011, GEOCIENCIAS, V30, P545; Filho O.J.C., 2017, THESIS, P116; Finkl CW, 2008, J COASTAL RES, V24, P823, DOI 10.2112/08A-0001.1; Fontes VC, 2020, SEAFLOOR GEOMORPHOLOGY AS BENTHIC HABITAT: GEOHAB ATLAS OF SEAFLOOR GEOMORPHIC FEATURES AND BENTHIC HABITATS, 2ND EDITION, P561, DOI 10.1016/B978-0-12-814960-7.00033-6; Gomes MP, 2014, MAR GEOL, V355, P150, DOI 10.1016/j.margeo.2014.06.002; Graler B, 2016, R J, V8, P204; GRANMAR, 2005, PROJ GRANM BRAS; Guerra NC, 2005, AN ACAD BRAS CIENC, V77, P343, DOI 10.1590/S0001-37652005000200011; Hani AFM, 2011, COMPUT GEOSCI-UK, V37, P177, DOI 10.1016/j.cageo.2010.05.021; Hengl T., 2007, PRACTICAL GUIDE GEOS; Hiemstra PH, 2009, COMPUT GEOSCI-UK, V35, P1711, DOI 10.1016/j.cageo.2008.10.011; Hijmans RJ, 2018, RASTER GEOGRAPHIC DA; HORN BKP, 1981, P IEEE, V69, P14, DOI 10.1109/PROC.1981.11918; Iampietro PJ, 2005, MAR TECHNOL SOC J, V39, P83, DOI 10.4031/002533205787442495; Ismail K, 2015, MAR GEOL, V362, P17, DOI 10.1016/j.margeo.2015.01.006; Jordan G, 2003, EARTH SURF PROC LAND, V28, P807, DOI 10.1002/esp.469; Kaskela AM, 2012, ESTUAR COAST SHELF S, V100, P150, DOI 10.1016/j.ecss.2012.01.008; Kienzle S., 2004, T GIS, V8, P83, DOI [10.1111/j.1467-9671.2004.00169.x, DOI 10.1111/J.1467-9671.2004.00169.X, 10.1111/j.1467-9671.2004.00169]; Dominguez JML, 2013, GEOMORPHOLOGY, V203, P46, DOI 10.1016/j.geomorph.2013.07.004; Lecours V, 2016, HYDROL EARTH SYST SC, V20, P3207, DOI 10.5194/hess-20-3207-2016; Li J., 2008, REV SPATIAL INTERPOL, DOI DOI 10.1016/J.EC0INF.2010.12.003; Lima Filho M., 2006, GEOCIENCIAS, V25, P117; Lucieer V, 2008, ISPRS J PHOTOGRAMM, V63, P496, DOI 10.1016/j.isprsjprs.2008.01.003; Lundblad E.R., 2006, MAR GEOD, V29, P89, DOI DOI 10.1080/01490410600738021; Manso V.A.V., 2003, PESQUISAS GEOCI NCIA, V30, P17, DOI DOI 10.22456/1807-9806.19587; Martin Louis, 1994, V60, P41; Micallef A, 2007, J GEOPHYS RES-EARTH, V112, DOI 10.1029/2006JF000505; Michelli M., 2001, REV PESQUI GEOCIEN, V28, P25, DOI DOI 10.22456/1807-9806.20266; Mitas L., 1998, GEOGR INF SYST PRINC, V1; MITASOVA H, 1993, MATH GEOL, V25, P657, DOI 10.1007/BF00893172; MOORE ID, 1991, HYDROL PROCESS, V5, P3, DOI 10.1002/hyp.3360050103; PENNOCK DJ, 1987, GEODERMA, V40, P297, DOI 10.1016/0016-7061(87)90040-1; Camargo JMR, 2015, REG STUD MAR SCI, V2, P203, DOI 10.1016/j.rsma.2015.10.009; Shary PA, 2002, GEODERMA, V107, P1, DOI 10.1016/S0016-7061(01)00136-7; Smith WHF, 1997, SCIENCE, V277, P1956, DOI 10.1126/science.277.5334.1956; Vasconcelos DL, 2019, TECTONOPHYSICS, V751, P23, DOI 10.1016/j.tecto.2018.12.019; Weiss A, 2001, ESRI US C SAN DIEG C; Wilson MFJ, 2007, MAR GEOD, V30, P3, DOI 10.1080/01490410701295962; Yamamoto J.K., 2013, GEOSTATISTICA CONCEI, P215; Young M., 1978, REPORT 5 GRANT ERO 5, P18; Zieger S, 2009, MAR GEOL, V264, P209, DOI 10.1016/j.margeo.2009.06.002	45	0	0	1	3	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	DEC	2020	104								102847	10.1016/j.jsames.2020.102847	http://dx.doi.org/10.1016/j.jsames.2020.102847			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TX					2023-06-23	WOS:000600273000004
J	Martinez, F; Giambiagi, L; Audemard, MFA; Parra, M				Martinez, F.; Giambiagi, L.; Audemard, M. F. A.; Parra, M.			Thrust and fold belts of South America	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Caribeean tectonics; Andean tectonics; Thrust belts; Mounatin and basins		In South America several fold and thrust belts are located along the northern and western margin, being they related to the Caribbean and Pacific oceanic plates interactions with the continent. For many decades, several geophysical and geological studies have been developed, in order to discover new oil and gas reserves and mineral recourses. The data derived from these, have partially allowed understand their surface and subsurface structure. A mix of thin and thick-skinned contractional structural style are recognized, which are responsible of the present-day configuration of the mountain ranges. In this special issue, we present a series of scientific contributions along different regions of South America, from Venezuela to the Patagonia, which show new structural, geochronological and stratigraphic data oriented to understand the mechanisms, styles and timing of deformation of the fold and thrust belts established over and along the South America.	[Martinez, F.] Univ Catolica Norte, Dept Ciencias Geol, Antofagasta, Chile; [Giambiagi, L.] Conycet, Mendoza, Argentina; [Audemard, M. F. A.] Univ Cent Venezuela, Caracas, Venezuela; [Parra, M.] Univ Sao Paulo, Sao Paulo, Brazil	Universidad Catolica del Norte; University of Central Venezuela; Universidade de Sao Paulo	Martinez, F (autor correspondente), Univ Catolica Norte, Dept Ciencias Geol, Antofagasta, Chile.	martinezfjh@hotmail.com	Giambiagi, Laura/AAA-6243-2021; Parra, Mauricio/B-7497-2013	Giambiagi, Laura/0000-0001-6286-7206; Parra, Mauricio/0000-0002-5955-6105; MARTINEZ, FERNANDO/0000-0002-4461-4392					0	1	1	0	5	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	DEC	2020	104								102822	10.1016/j.jsames.2020.102822	http://dx.doi.org/10.1016/j.jsames.2020.102822			3	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TU					2023-06-23	WOS:000600272700001
J	Miranda, TS; Neves, SP; Celestino, MAL; Roberts, NMW				Miranda, Tiago S.; Neves, Sergio P.; Celestino, Maria Alcione L.; Roberts, Nick M. W.			Structural evolution of the Cruzeiro do Nordeste shear zone (NE Brazil): Brasiliano-Pan-African-ductile-to-brittle transition and Cretaceous brittle reactivation	JOURNAL OF STRUCTURAL GEOLOGY			English	Article						Borborema province; Mylonite; Jatoba Basin; Cataclasite; U-Pb; C alcite	EASTERN BORBOREMA PROVINCE; TUCANO-JATOBA RIFT; NORTHEAST BRAZIL; CONTINENTAL-SCALE; FAULT ZONE; PERNAMBUCO LINEAMENT; TECTONIC EVOLUTION; BASEMENT CONTROL; SERIDO BELT; KAOKO BELT	The Borborema Province (NE Brazil) is characterized by the development of continental-scale transcurrent shear zones related to the Neoproterozoic Brasiliano-Pan-African Orogeny. These shear zones commonly border Cretaceous intraplate sedimentary basins. This work presents a structural and microstructural study of the Cruzeiro do Nordeste shear zone (CNSZ), which limits the northern border of the Jatoba Basin. The ductile deformation of the CNSZ is marked by high-angle, ENE-trending foliation bearing subhorizontal stretching lineation, with numerous kinematic indicators showing dextral shearing. We documented a continuous transition from high-temperature (high-T) to low-temperature (low-T) (c. 650 degrees C to c. 300 degrees C) ductile fabrics characterized, at the high-T end, by quartz recrystallization by grain boundary migration and feldspar recrystallization by subgrain rotation, and, at the low-T end, by bulging recrystallization of quartz and extensive fracturing of feldspars. The cooler semi-brittle to brittle deformation superimposed on the mylonites is characterized by conjugate pairs of strike-slip mesoscopic faults. The orientation of these faults (WNW-ESE, dextral, and N-S, sinistral) suggests they were formed under the same stress field than the ductile fabrics and thus evidence a continuum deformational from the ductile to the brittle field associated with exhumation during transcurrent tectonics. Brittle reactivation of the CNSZ is characterized by normal faults overprinting the mylonitic foliation. We report a U-Pb age from fault-hosted calcite slickenfibres of 135 +/- 4.7 Ma, which provides constraints on the timing of brittle reactivation that can be associated with opening of the South Atlantic Ocean.	[Miranda, Tiago S.; Neves, Sergio P.] Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil; [Celestino, Maria Alcione L.] Univ Fed Pernambuco, Geosci Grad Program, BR-50740530 Recife, PE, Brazil; [Roberts, Nick M. W.] British Geol Survey, Geochronol & Tracers Facil, Ctr Environm Sci, Nottingham NG12 5GG, England; [Miranda, Tiago S.] Ave Arquitetura,953-995 Cidade Univ, BR-50740 Recife, PE, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Miranda, TS (autor correspondente), Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil.; Miranda, TS (autor correspondente), Ave Arquitetura,953-995 Cidade Univ, BR-50740 Recife, PE, Brazil.	tiago.smiranda@ufpe.br; serpane@hotlink.com.br; alcionelimma22@gmail.com; nirob@bgs.ac.uk	Neves, Sergio/A-2086-2008; Roberts, Nick M W/C-2694-2008; Miranda, Tiago S/P-8113-2018	Neves, Sergio/0000-0001-6690-3278; Roberts, Nick M W/0000-0001-8272-5432; Miranda, Tiago S/0000-0001-9099-1271	NERC [bgs06001] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Adeoti B, 2017, J AFR EARTH SCI, V131, P117, DOI 10.1016/j.jafrearsci.2017.04.008; 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Struct. Geol.	DEC	2020	141								104203	10.1016/j.jsg.2020.104203	http://dx.doi.org/10.1016/j.jsg.2020.104203			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OZ9PN					2023-06-23	WOS:000595250500019
J	Monteiro, CB; Oleinik, PH; Leal, TF; Kirinus, ED; Toldo, EE; Marques, WC; Lopes, BDFL				Monteiro, Caroline Barbosa; Oleinik, Phelype Haron; Leal, Thalita Fagundes; Kirinus, Eduardo de Paula; Toldo Junior, Elirio Ernestino; Marques, Wiliam Correa; Lopes, Bruna de Carvalho Faria Lima			Susceptibility to oil spill spreading using case studies and simulated scenarios	ENVIRONMENTAL POLLUTION			English	Article						Oil spill modelling; Susceptibility; Environmentally sensitive areas	POLYCYCLIC AROMATIC-HYDROCARBONS; CRUDE-OIL; ENVIRONMENTAL SENSITIVITY; EVAPORATION RATE; CASSINO BEACH; PATOS LAGOON; STORM SURGES; WATER; MODEL; SOUTH	Fossil fuels still prevail over other energy sources in the world's consumption energy matrix. Thus, oil transportation and operations over maritime routes have been in high demand for a long time. Although oil spill accidents caused by these activities have reduced significantly over the last few decades, they still cause great concern. From this perspective, this paper presents simulation analyses of oil spill case studies using TELEMAC-3D hydrodynamic model coupled with an oil model. Hence a location susceptible to such accidents was selected and three real oil spills were simulated, for each of which there were official technical monitoring reports available. The obtained results contribute to the knowledge of oil pollution susceptibility in environmentally sensitive areas, as well as provide information concerning oil slick behaviour. Additionally, similarities between the modelled results and the technical reports were confirmed. These findings are useful for contingency planning and responding to these probable accidents. (c) 2020 Elsevier Ltd. All rights reserved.	[Monteiro, Caroline Barbosa] Fed Univ Rio Grande, Inst Oceanog, Postgrad Program Oceanol, Rio Grande, RS, Brazil; [Oleinik, Phelype Haron; Leal, Thalita Fagundes; Kirinus, Eduardo de Paula] Fed Univ Rio Grande, Sch Engn, Rio Grande, RS, Brazil; [Toldo Junior, Elirio Ernestino] Univ Fed Rio Grande do Sul, Inst Geosci, Porto Alegre, RS, Brazil; [Marques, Wiliam Correa] Fed Univ Rio Grande, Inst Math Stat & Phys, Rio Grande, RS, Brazil; [Lopes, Bruna de Carvalho Faria Lima] Univ Strathclyde, Civil & Environm Engn Dept, Glasgow, Lanark, Scotland	Universidade Federal do Rio Grande; Universidade Federal do Rio Grande; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande; University of Strathclyde	Monteiro, CB (autor correspondente), Fed Univ Rio Grande, Inst Oceanog, Postgrad Program Oceanol, Rio Grande, RS, Brazil.	monteirocbm@gmail.com	De Carvalho Faria Lima Lopes, Bruna/H-6138-2017	De Carvalho Faria Lima Lopes, Bruna/0000-0001-7669-7236; Oleinik, Phelype/0000-0002-4290-9971; Monteiro, Caroline/0000-0002-5197-1689	Coordenacao de Aperfeioamento de Pessoal de Nivel Superior Brasil (CAPES) [001]; CNPq [304227/2016-1, 17/2551-0001159-7]; FAPERGS [304227/2016-1, 17/2551-0001159-7]	Coordenacao de Aperfeioamento de Pessoal de Nivel Superior Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPERGS(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS))	This study was partially financed by Coordenacao de Aperfeioamento de Pessoal de Nivel Superior Brasil (CAPES) and has Finance Code 001. We thank the resources provided by CAPES to support the Postgraduate Program in Oceanology. The authors also acknowledge the support of the CNPq and FAPERGS for sponsoring the research (contracts 304227/2016-1 and 17/2551-0001159-7).	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Pollut.	DEC	2020	267								115451	10.1016/j.envpol.2020.115451	http://dx.doi.org/10.1016/j.envpol.2020.115451			12	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	OY0TN	33254713	Green Submitted			2023-06-23	WOS:000593967100017
J	Monteiro, CF; de Oliveira, IL; Brod, JA; Dantas, EL; de Araujo, CEG; Zacchi, ENP; Fuck, RA				Monteiro, Cimara Francisca; de Oliveira, Italo Lopes; Brod, Jose Affonso; Dantas, Elton Luiz; Ganade de Araujo, Carlos Eduardo; Pedro Zacchi, Erico Natal; Fuck, Reinhardt Adolfo			Nd-Sr-Hf isotopes and U-Pb ages of mesoproterozoic Tres Estradas Alkaline-Carbonatite Complex, Brazil: Implications for Sul-Riograndense Shield evolution and rodinia break-up	PRECAMBRIAN RESEARCH			English	Article						Tres Estradas; Carbonatite; Sul-Riograndense Shield; Rio de la Plata Craton; Rodinia	DOM FELICIANO BELT; LA-PLATA CRATON; LU-HF; SOUTHERN BRAZIL; TRACE-ELEMENT; SM-ND; TECTONIC EVOLUTION; GRENVILLE PROVINCE; BRASILIANO OROGEN; NEPHELINE SYENITE	The first occurrence of Mesoprotemzoic carbonatite in the Rio de la Plata Craton - RDPC indicates extensional event prior to the opening of the Charrua Ocean. Nd-Sr-Hf Isotopic and U-Pb on zircon geochronological data are presented for the Tres Estradas Alkaline-Carbonatite Complex - TEC, located in southernmost Brazil. The complex consists predominantly of ultramafic rocks, carbonatites and, subordinate, deformed fenitized syenites metamorphosed under greenschist to amphibolite facies conditions. U-Pb ages between 1110 +/- 4.8 Ma and 1123 +/- 15 Ma, respectively derived from a dolomite metacarbonatite and an associated metasyenite, constrain the TEC emplacement timing. The Nd-Sr-Hf isotopic signatures indicate that the TEC rocks were derived from a heterogeneous mantle, isotopically depleted in Sm-Nd and slightly depleted to enriched in Rb-Sr, with little influence of ancient crust and that these rocks are derived from the same source of parental magma probably submitted to intense metasomatism. The Nd-Sr isotopic signatures and crystallization ages of the TEC allow correlating it to the carbonatitic intrusions of the Alkaline provinces of Ontario and Grenville, Canada, in Laurentia, associated with the Keweenawan magmatic event (1.11-1.09 Ga), to which extension efforts would be related causing ruptures in RDPC edge and Laurentia, probably juxtaposed in that time interval. According to paleogeographic reconstructions of Rodinia, the Kalahari Craton would only have joined Laurentia and the RDPC at 1050 Ma. Around 920 Ma there is the generation of an oceanic crust in the Rio de la Plata Craton with the installation of the Charrua Ocean and the beginning of the formation of the Dom Feliciano Belt, concluded at 540 Ma, with peak deformation and metamorphism at 650-630 Ma.	[Monteiro, Cimara Francisca; de Oliveira, Italo Lopes; Brod, Jose Affonso; Dantas, Elton Luiz; Pedro Zacchi, Erico Natal; Fuck, Reinhardt Adolfo] Univ Brasilia, Inst Geociencias, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Monteiro, Cimara Francisca] Ctr Desenvolvimento Tecnol CEDES, Serv Geol Brasil SGB CPRM, BR-70040904 Brasilia, DF, Brazil; [Brod, Jose Affonso] Univ Fed Goias, Fac Ciencias & Tecnol, Campus Aparecida Goiania, BR-74968755 Aparecida De Goiania, Go, Brazil; [Ganade de Araujo, Carlos Eduardo] Ctr Desenvolvimento Tecnol CEDES, Serv Geol Brasil SGB CPRM, BR-22290255 Rio De Janeiro, RJ, Brazil	Universidade de Brasilia; Universidade Federal de Goias	Monteiro, CF (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil.; Monteiro, CF (autor correspondente), Ctr Desenvolvimento Tecnol CEDES, Serv Geol Brasil SGB CPRM, BR-70040904 Brasilia, DF, Brazil.	cimara.monteiro@cprm.gov.br	Dantas, Elton Luiz/AAK-8464-2021; Brod, Jose/AAL-2913-2021	Dantas, Elton Luiz/0000-0002-7954-5059; Brod, Jose/0000-0002-4265-2571; Oliveira, Italo/0000-0001-5219-508X	Aguia Resources Ltd mining company; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]; INCT Estudos Tectonicos (CNPq-CAPESFAPDF); CNPq	Aguia Resources Ltd mining company; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); INCT Estudos Tectonicos (CNPq-CAPESFAPDF); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to thank Aguia Resources Ltd mining company for supporting field work, accessing core samples, and for assigning petrography data, to the Laboratorio de Estudos Ambientais e Geodinamicos from the Instituto de Geociencias of the Universidade de Brasilia for geochronological and isotopic analyses and to the Centro de Desenvolvimento Tecnologico (CEDES) of the Servico Geologico do Brasil-CPRM. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) - Finance Code 001. ELD and RAF thank INCT Estudos Tectonicos (CNPq-CAPESFAPDF) for financial support and CNPq for research fellowship. We thank Professor Marcio M. Pimentel (in memorian) for his contributions and Dr. Rodrigo R. Adorno for English text formatting. We finally thank the two anonymous reviewers that contributed significantly to enhance the final version of this paper.	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DEC	2020	351								105963	10.1016/j.precamres.2020.105963	http://dx.doi.org/10.1016/j.precamres.2020.105963			25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OZ8DF					2023-06-23	WOS:000595149400017
J	Morfulis, M; Baez, W; Retamoso, S; Bardelli, L; Filipovich, R; Sommer, CA				Morfulis, Marcos; Baez, Walter; Retamoso, Santiago; Bardelli, Lorenzo; Filipovich, Ruben; Sommer, Carlos Augusto			Quantitative spatial distribution analysis of mafic monogenic volcanism in the southern Puna, Argentina: Implications for magma production rates and structural control during its ascent	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Monogenic volcanic fields; Nearest neighbor analysis; Volcanic alignments; Southern puna	PASTO VENTURA REGION; BACK-ARC; BASALTIC VOLCANISM; CENTRAL ANDES; TELESEISMIC TOMOGRAPHY; MICHOACAN-GUANAJUATO; NW ARGENTINA; PLATEAU; FIELD; BENEATH	Establishing the factors that control the pathways of magma ascent is an important issue in the study of monogenic mafic volcanism since it provides information about the relationship between the source of the ascending magma and the regional and local tectonic frameworks. We have quantitatively analyzed the spatial distribution of the volcanic centers in the monogenic volcanic fields (MVFs) of the Southern Puna using Nearest-Neighbor Analysis to assess the degree of randomness between individual centers. We also performed alignment analysis which highlights the structural weaknesses that magmas use to ascend. We integrate these novel data with published structural, petrologic, and geophysical data to propose a source-to-surface model which explains the spatial distribution of monogenic mafic centers of the Southern Puna. We find that MVFs display two distinct spatial patterns related to different magmatic production rates. Specifically, in those areas where the magmatic production is long-lasting and relatively high, the magma exerts strain rates suffciently high to reactivate preexisiting discontinuities with random orientations with respect to the current local stress conditions. As a result the volcanic centers are arranged with a clustered spatial distribution. We define these as MVFs controlled by magmatism or high flux fields (MVFs-M). On the other hand, low magmatic production rates tend to produce areas where mafic centers display a Poisson distribution, because strain rates are only sufficient to reactivate preexisting discontinuities that are nearly parallel to the maximum compressive stress. This latter group is defined as MVFs controlled by tectonism or low flux fields (MVFs-T). Available petrological and geophysical data indicate that both groups are fed by a complex lower crustal MASH zone where magma production is associated with lithospheric foundering and subduction-related mantle melting. Spatial distribution of the MVFs in the Southern Puna are also affected by the development of upper crustal magma storage zones.	[Morfulis, Marcos; Baez, Walter; Retamoso, Santiago; Bardelli, Lorenzo; Filipovich, Ruben] Univ Nacl Salta UNSa, Av Bolivia 5150, RA-4400 Salta, Argentina; [Baez, Walter; Filipovich, Ruben] Inst Bio & Geociencias Noroeste Argentino UNSa CO, 9 Julio 14, RA-4405 Rosario De Lerma, Salta, Argentina; [Sommer, Carlos Augusto] Univ Fed Rio Grande do Sul, Geosci Inst, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Morfulis, M (autor correspondente), Univ Nacl Salta UNSa, Av Bolivia 5150, RA-4400 Salta, Argentina.	marcosmorfulis@gmail.com	Sommer, Carlos A/Q-9077-2018; Filipovich, Rubén/HHT-0232-2022	Sommer, Carlos A/0000-0001-8696-7084; Filipovich, Rubén/0000-0003-2177-6097	Ministry of Science, Technology and Innovation [PICT (B)-2016-1359, PICT (A) 2014-3436]; Brazilian National Council for Scientific and Technological Development (CNPq) [304036/2018-8, 406925/2018-6]	Ministry of Science, Technology and Innovation(Ministry of Energy, Science, Technology, Environment and Climate Change (MESTECC), Malaysia); Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was partially funded by the Ministry of Science, Technology and Innovation, projects PICT (B)-2016-1359, PICT (A) 2014-3436 and by Brazilian National Council for Scientific and Technological Development (CNPq), projects 304036/2018-8, and 406925/2018-6. We gratefully acknowledge Chuck Lewis, Abdullah Alohali, and Shanaka de Silva from Oregon State University for the English writing assistance and comments that have significantly enhanced our presentation.	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South Am. Earth Sci.	DEC	2020	104								102852	10.1016/j.jsames.2020.102852	http://dx.doi.org/10.1016/j.jsames.2020.102852			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TX					2023-06-23	WOS:000600273000005
J	Nedel, IM; Fuck, RA; Ruiz, AS; Matos, R; Ferreira, ACD				Nedel, Ingrid Moerschberger; Fuck, Reinhardt A.; Ruiz, Amarildo Salina; Matos, Ramiro; Dantas Ferreira, Alanielsonda Camara			U-Pb geochronology and geochemistry of grenville-age plutons in the Sunsas Belt - Bolivia, SW Amazonian Craton: Tectonic and magmatic implications	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Sunsas magmatism; Amazonian craton; Rodinia supercontinent; Bolivia	A-TYPE GRANITES; ANOROGENIC MAGMATISM; EASTERN BOLIVIA; EVOLUTION; ORIGIN; CLASSIFICATION; PROVINCES; ZIRCONS; DISCRIMINATION; PROVENANCE	The Sunsas syn-to post-orogenic high-K calc-alkaline magmatism is crucial to understand the tectonic and thermodynamic history of the Sunsas Orogeny in the southwestern part of the Amazonian Craton. This orogeny is correlated with the Grenville orogenic cycle (c. 1.3 to 0.95 Ga) of Laurentia. Three granitic intrusions from Sunsas belt were classified as fractionated I-type and hybrid A-type granites. The first, the Nomoca granodiorite presents calc-alkaline affinity with peraluminous-magnesian composition (Mg0 = 1.61 wt%), and typical characteristics of intermediate magmas (SiO2 = 67.3 w%). The La Asunta and Nocemano syenogranites have calcalkaline affinity with peraluminous-ferrous composition (FeO = 2.26-3.31 wt%) and characteristics of silicarich magmas (SiO2 = 70.4-74.9 w%). Geochemical fractionation patterns suggest that the granites were derived from the reworking of two crustal protolith sources in the same tectonic environment. The Nomoca, La Asunta and Nocemano intrusions yield crystallization ages between 1.17 and 1.08 Ga. Inherited zircon cores with 3.63 and 2.91 Ga Archean ages from Nomoca and Nocemano intrusions may be correlated to the Superior Province evolution, which is located in the south-central part of the Canadian Shield. These U-Pb ages strengthen the geotectonic model for the Rodinia supercontinent with Laurentia-Baltica-Amazonia configuration. Paleoproterozoic (2.12-1.69 Ga) and Mesoproterozoic (1.4-1.3 Ga) U-Pb inherited zircon ages from these intrusions support intensive reworking of the Paragua basement. A concordant age of 555 Ma for zircon rims suggests reworking of the Sunsas Province during the Neoproterozoic Brasiliano Orogeny.	[Nedel, Ingrid Moerschberger; Fuck, Reinhardt A.] Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Ruiz, Amarildo Salina] Univ Fed Mato Grosso, Fac Geociencias, Cuiaba, MT, Brazil; [Matos, Ramiro] Univ Mayor San Andres UMSA, Inst Invest Geol & Medio Ambiente, Pabellein Geol, Calle 27,Campus Univ Cota Cota, La Paz, Bolivia; [Dantas Ferreira, Alanielsonda Camara] Univ Fed Rio Grande Sul UFRGS, Lab Geoquim & Petrol Expt LAGEPE, BR-91501970 Porto Alegre, RS, Brazil	Universidade de Brasilia; Universidade Federal de Mato Grosso; Universidad Mayor de San Andres; Universidade Federal do Rio Grande do Sul	Nedel, IM (autor correspondente), Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil.	ingrid_mn@hotmail.com	; Ruiz, Amarildo Salina/M-3634-2014	Moerschberger Nedel, Ingrid/0000-0002-8070-5320; Ruiz, Amarildo Salina/0000-0002-7800-2837; Ferreira, Alanielson/0000-0001-8054-0047	LaboratOrio de Geocronologia (Universidade de Brasilia); Grupo de Pesquisa em Evolucao Crustal e TectOnica (Guapore); Comissao de Aperfeicoamento de Pessoal do Nivel Superior (CAPES) [88882.347151/2010-01]; Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF); INCT Estudos TectOnicos (CNPq-FAPDF); CAPES; Programa de Excelencia Academica (PROEX); CNPq	LaboratOrio de Geocronologia (Universidade de Brasilia); Grupo de Pesquisa em Evolucao Crustal e TectOnica (Guapore); Comissao de Aperfeicoamento de Pessoal do Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)); INCT Estudos TectOnicos (CNPq-FAPDF); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Programa de Excelencia Academica (PROEX); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors acknowledge the support of the LaboratOrio de Geocronologia (Universidade de Brasilia) and the Grupo de Pesquisa em Evolucao Crustal e TectOnica (Guapore). The authors also acknowledge Comissao de Aperfeicoamento de Pessoal do Nivel Superior (CAPES, Project 88882.347151/2010-01), Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF) and INCT Estudos TectOnicos (CNPq-FAPDF) for financial support. IMN thanks CAPES and Programa de Excelencia Academica (PROEX, Edital - 0487) for granting the Doctorate scholarship. RAF and ASR acknowledge CNPq for research fellowship.	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South Am. Earth Sci.	DEC	2020	104								102845	10.1016/j.jsames.2020.102845	http://dx.doi.org/10.1016/j.jsames.2020.102845			21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TP					2023-06-23	WOS:000600272200001
J	Oliveira, TS; Xavier, DD; Santos, LD; Franca, EJ; Sanders, CJ; Passos, TU; Barcellos, RL				Oliveira, Thais S.; Xavier, Diego de A.; Santos, Luciana D.; Franca, Elvis J.; Sanders, Christian J.; Passos, Tiago U.; Barcellos, Roberto L.			Geochemical background indicators within a tropical estuarine system influenced by a port-industrial complex	MARINE POLLUTION BULLETIN			English	Article						Suape estuarine system; Mangrove sediments; Pb-210; Metal; Anthropogenic impacts	HEAVY-METAL CONTAMINATION; COASTAL SEDIMENTS; MARINE-SEDIMENTS; TRACE-ELEMENTS; BASE-LINE; NORMALIZATION; RIVER; GULF; LEAD; ACCUMULATION	This study aims to determine the background values for metals in the Suape estuarine system, Brazil, and to identify contamination caused by anthropogenic sources. Two cores were sampled. Sedimentation rates and metal content were analysed. The Al-normalized method was used to infer the background values, and to identify anthropic influences, the enrichment and contamination factors and the geoaccumulation index were employed. The results revealed an Mn, Ni, Zn, Ga, Pb, Sr, Ti, Mg, V and Fe content (mg kg(-1)) of 101.8, 5.7, 24.4, 8.3, 14.5, 41.9, 2744.6, 4581, 14.9 and similar to 1% respectively. After the installation of the Suape port, an increase in metal contents and in fluxes were recorded. Increases in Zn, Ga, V and Pb are supported by the indexes showing moderate contamination, enrichment and suggest an area moderately polluted. The other studied metals do not reflect an anthropogenic impact, with low values of contamination, enrichment factors and geoaccumulation indexes.	[Oliveira, Thais S.; Santos, Luciana D.; Barcellos, Roberto L.] Univ Fed Pernambuco, Recife, PE, Brazil; [Xavier, Diego de A.] Museu Paraense Emilio Goeldi, Northeast, Belem, Para, Brazil; [Franca, Elvis J.] Nucl Sci Reg Ctr, Northeast, Rio De Janeiro, Brazil; [Sanders, Christian J.] Southern Cross Univ, Lismore, NSW, Australia; [Passos, Tiago U.] Univ Sydney, Sydney, NSW, Australia	Universidade Federal de Pernambuco; Museu Paraense Emilio Goeldi; Southern Cross University; University of Sydney	Oliveira, TS (autor correspondente), Univ Fed Pernambuco, Recife, PE, Brazil.	thais1ufpe@gmail.com	Barcellos, Roberto/AAH-3829-2020; Xavier, Diego/AAK-8351-2021; Sanders, Christian J/AAM-6906-2021	Barcellos, Roberto/0000-0003-1304-4603; Xavier, Diego/0000-0003-1644-3837; Sanders, Christian J/0000-0003-0090-0896; U. Passos, Tiago/0000-0002-7080-7905	FACEPE [APQ 0260-1.08/15]	FACEPE(Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco (FACEPE))	We are grateful to the FACEPE for financial support of the project: "Holocene sedimentation in the region of influence of the Suape port-industrial complex (PE) (Suape-GeoSub)" (APQ 0260-1.08/15).	Aloupi M, 2001, ENVIRON POLLUT, V113, P211, DOI 10.1016/S0269-7491(00)00173-1; [Anonymous], 2009, PRINCIPIOS ANALISE I; Appleby P.G., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; Baptista Neto J. A., 2000, Environmental Pollution, V109, P1, DOI 10.1016/S0269-7491(99)00233-X; Barcellos R. 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Pollut. Bull.	DEC	2020	161		A						111794	10.1016/j.marpolbul.2020.111794	http://dx.doi.org/10.1016/j.marpolbul.2020.111794			8	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	PG6NS	33158545				2023-06-23	WOS:000599850900008
J	Ramos, SJ; Gastauer, M; Mitre, SK; Caldeira, CF; Silva, JR; Neto, AEF; Oliveira, G; Souza, PWM; Siqueira, JO				Ramos, Silvio J.; Gastauer, Markus; Mitre, Simone K.; Caldeira, Cecilio F.; Silva, Joyce R.; Furtini Neto, Antonio E.; Oliveira, Guilherme; Souza Filho, Pedro W. M.; Siqueira, Jose O.			Plant growth and nutrient use efficiency of two native Fabaceae species for mineland revegetation in the eastern Amazon	JOURNAL OF FORESTRY RESEARCH			English	Article						Fertilizer application; Mining soil; Tropical forest; Nutrient use efficiency	NITROGEN-FIXATION; ECOLOGICAL THEORY; PLANTATIONS; TOPSOIL; INDEX	The primary challenge of mineland revegetation is the establishment of species able to cope with low availability of nutrients, especially in steep slopes such as of mine pits. We evaluated plant growth response and nutrient use efficiency (NUE) of two promising native Fabaceae species (Dioclea apurensis-liana from metalliferous savannas;Bauhinia longipedicellata-tree from Amazon rainforest) from the Carajas Mineral Province, eastern Amazon-Brazil. Plants were grown separately in 2-kg pots filled with mining waste. Substrates were fertilized with nitrogen, phosphorus, potassium (NPK), lime, and micronutrients. The results showed increments on growth of both species when nutrients were applied to the mining waste.D. apurensisshowed increases in leaf area, plant height, stem diameter, and shoot dry mass production when NPK or NPK + micronutrients were applied, whileB. longipedicelatawas responsive to application of NPK + lime or NPK + lime + micronutrients. Further,D. apurensisshowed higher NUE thanB. longipedicelata, especially at the lowest doses of N, P and K. These findings may indicate a substantial advantage ofD. apurensisfor mineland revegetation, as this species may require lower nutrient inputs, being, therefore, a more sustainable way to revegetate degraded areas.	[Ramos, Silvio J.; Gastauer, Markus; Mitre, Simone K.; Caldeira, Cecilio F.; Silva, Joyce R.; Furtini Neto, Antonio E.; Oliveira, Guilherme; Souza Filho, Pedro W. M.; Siqueira, Jose O.] Inst Tecnol Vale, Rua Boaventura da Silva 955, BR-66055090 Belem, Para, Brazil; [Siqueira, Jose O.] Univ Fed Lavras, Dept Ciencia Solo, BR-37200000 Lavras, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Universidade Federal de Lavras	Ramos, SJ (autor correspondente), Inst Tecnol Vale, Rua Boaventura da Silva 955, BR-66055090 Belem, Para, Brazil.	silvio.ramos@itv.org	Neto, Antonio/HSE-4895-2023; Gastauer, Markus/GMW-6022-2022; Frois, Cecilio/HQZ-9386-2023					[Anonymous], 2004, SER INT PRIM EC REST; Broadley M, 2012, MARSCHNER'S MINERAL NUTRITION OF HIGHER PLANTS, 3RD EDITION, P191, DOI 10.1016/B978-0-12-384905-2.00007-8; Candeias C, 2014, APPL GEOCHEM, V44, P12, DOI 10.1016/j.apgeochem.2013.07.009; Carvalho JM, 2018, RESTOR ECOL, V26, P303, DOI 10.1111/rec.12572; EMBRAPA-Empresa Brasileira de Pesquisa Agropecuaria, 2009, MAN AN QUIM SOL PLAN, P627; ERICSSON T, 1995, PLANT SOIL, V168, P205, DOI 10.1007/BF00029330; Garibaldi LA, 2014, FRONT ECOL ENVIRON, V12, P439, DOI 10.1890/130330; Gastauer M, 2018, AMBIO, V48, P1; Gaur D., 2017, INT J CHEM STUD, V5, P215; Giannini TC, 2017, AUSTRAL ECOL, V42, P510, DOI 10.1111/aec.12470; Goel VL, 2004, BIOMASS BIOENERG, V27, P403, DOI 10.1016/j.biombioe.2004.04.004; Gon┬u┬║alves J.L.M., 2000, NUTR FERTILIZACAO FL, P309; Hawkesford M, 2012, MARSCHNER'S MINERAL NUTRITION OF HIGHER PLANTS, 3RD EDITION, P135, DOI 10.1016/B978-0-12-384905-2.00006-6; Holdo RM, 2013, PLOS ONE, V8, DOI 10.1371/journal.pone.0069625; JORGENSEN SE, 1994, ECOL MODEL, V75, P5, DOI 10.1016/0304-3800(94)90003-5; Pilon NAL, 2018, RESTOR ECOL, V26, P73, DOI 10.1111/rec.12534; Lobato LM, 2005, CARACTERIZACAO DEPOS, P20; Matson AL, 2015, BIOGEOCHEMISTRY, V122, P281, DOI 10.1007/s10533-014-0041-8; Mattos Cilene Mara Jordão de, 2018, Rodriguésia, V69, P1147, DOI 10.1590/2175-7860201869323; Mukhopadhyay S, 2013, ECOL ENG, V57, P133, DOI 10.1016/j.ecoleng.2013.04.017; Palmer MA, 1997, RESTOR ECOL, V5, P291, DOI 10.1046/j.1526-100X.1997.00543.x; Perring MP, 2016, GLOBAL CHANGE BIOL, V22, P1361, DOI 10.1111/gcb.13146; Pinto AP, 2018, BIOGEOTECHNOLOGIES M, P159, DOI [10.1016/B978-0-12-812986-9.00010-5., DOI 10.1016/B978-0-12-812986-9.00010-5]; R Core Team, 2019, R LANG ENV STAT COMP; Reed SC, 2007, BIOTROPICA, V39, P585, DOI 10.1111/j.1744-7429.2007.00310.x; Roberts TL, 2008, TURK J AGRIC FOR, V32, P177; Rosiere CA, 2018, REGION GEOL REV, P493, DOI 10.1007/978-3-319-68920-3_18; Sheoran V., 2010, INT J SOILS SEDIMENT, V3, P1; SIDDIQI MY, 1981, J PLANT NUTR, V4, P289, DOI 10.1080/01904168109362919; Silva JR, 2018, FLORA, V246, P109, DOI 10.1016/j.flora.2018.08.001; Stover HJ, 2017, ECOL ENG, V103, P141, DOI 10.1016/j.ecoleng.2017.03.012; Suding K, 2015, SCIENCE, V348, P638, DOI 10.1126/science.aaa4216; Zheng MH, 2016, BIOL FERT SOILS, V52, P665, DOI 10.1007/s00374-016-1109-5	33	12	12	3	33	NORTHEAST FORESTRY UNIV	HARBIN	NO 26 HEXING RD, XIANGFANG DISTRICT, HARBIN, 150040, PEOPLES R CHINA	1007-662X	1993-0607		J FORESTRY RES	J. For. Res.	DEC	2020	31	6					2287	2293		10.1007/s11676-019-01004-w	http://dx.doi.org/10.1007/s11676-019-01004-w			7	Forestry	Science Citation Index Expanded (SCI-EXPANDED)	Forestry	OC5AQ					2023-06-23	WOS:000579169400023
J	Redes, LA; Hauser, N; Ruiz, AS; Matos, R; Reimold, WU; Dantas, EL; Schmitt, RT; Lima, BAF; Zacchi, ENP; Chaves, JGS; Osorio, LFB; Pimentel, MM				Redes, Leticia A.; Hauser, Natalia; Ruiz, Amarildo S.; Matos, Ramiro; Reimold, Wolf Uwe; Dantas, Elton L.; Schmitt, Ralf-Thomas; Ferreria Lima, Barbara Alcantra; Pedro Zacchi, Erico Natal; Silva Chaves, Jeane Grasyelle; Baumotte Osorio, Luis Felipe; Pimentel, Marcio Martins			U-Pb and Hf isotopes in granitoids from the Eastern Bolivian basement: Insights into the Paleoproterozoic evolution of the western part of South America	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Basement; Eastern Bolivia; Paleoproterozoic granites; U-Pb/Lu-Hf geochronology; Sm-Nd isotopes; Rio Apa Block	PLASMA-MASS SPECTROMETRY; TRACE-ELEMENT; LU-HF; HAFNIUM ISOTOPE; ZIRCON; REGION; CRATON; DISCRIMINATION; GEOCHRONOLOGY; PROVINCES	Granitoids from the Eastern Bolivian basement at Santo Corazon, Correreca, and Santa Terezita, and the Santana Gneiss from the Corumba region (Mato Grosso de Sul state, Brazil) were studied by geochemistry and Sm-Nd and U-Pb isotope analysis. The granites have a medium to high calcium-alkaline potassic character and are typically peraluminous S-type granites. For The Santo Corazon quartz monzonite and the Correreca granite we obtained Orosirian upper intercept U-Pb zircon ages of 1874 +/- 15 Ma and 1862 +/- 7 Ma. For Santa Terezita granite two upper intercept U-Pb zircon ages of 1849 +/- 11 and 1852 +/- 6 Ma were obtained. The geochemical and Nd and U-Pb isotope data suggest that these complexes were part of a crust created between 2.23 and 1.96 Ga, which was reworked mainly in Orosirian times in a magmatic arc setting. This is further supported by Hf isotope data for zircon from the Correreca granite. The garnet-hornblende-biotite Santana Gneiss gave an upper intercept zircon U-Pb age of 1764 +/- 23 Ma, which is interpreted as the crystallization age of the igneous protolith, a quartz-monzonite to granodiorite. The petrological, geochemical, and Nd as well as U-Pb isotope data show similarity between the Eastern Bolivian basement granites (EBB) and the Santana Gneiss with the Alumiador Intrusive Suite and the Caracol Gneiss, respectively. This suggests that this crustal fragment could have been an extension to the west of the Rio Apa Block, which today extends for 300 km from the southwest of Mato Grosso do Sul and northeast of Paraguay to Eastern Bolivia. The presence of continental crust that dates back to 1.7-1.8 Ga is inferred from isotope data for the cores of zircon from the Santana Gneiss and the Eastern Bolivian granites (EBB). In contrast, U-Pb ages obtained in rims of zircon crystals may indicate that two collisional events took place: a first one at 1.7 Ga, which we can relate to the collision of the Eastern and Western terranes of the Rio Apa Block with the Paragua Block located to the west; and a second one at 1.3 Ga, related to the collision between the Paragua Block, Eastern Bolivian basement granite terrane and the Rio Apa Block (EBB + RAB) with the Amazonian Craton during the San Ignacio Orogeny. This assemblage remained stable during the amalgamation into the Rodinia supercontinent.	[Redes, Leticia A.; Hauser, Natalia; Reimold, Wolf Uwe; Dantas, Elton L.; Ferreria Lima, Barbara Alcantra; Pedro Zacchi, Erico Natal; Silva Chaves, Jeane Grasyelle; Baumotte Osorio, Luis Felipe; Pimentel, Marcio Martins] Univ Brasilia, Inst Geociencias, Lab Geocronol & Geoquim Isotop, BR-70910900 Brasilia, DF, Brazil; [Ruiz, Amarildo S.] Univ Mato Grosso, Fac Geociencias, Ave Fernando Correa da Costa 2367, BR-78060900 Cuiaba, MT, Brazil; [Matos, Ramiro] Univ Mayor San Andres, Inst Geol Econ & Medio Ambiente, Calle 27, La Paz, Bolivia; [Schmitt, Ralf-Thomas] Museum Nat Kunde, Leibniz Inst Evolut & Biodivers Sci, Invalidenstr 43, D-10115 Berlin, Germany	Universidade de Brasilia; Universidade Federal de Mato Grosso do Sul; Universidad Mayor de San Andres; Leibniz Institut fur Evolutions und Biodiversitatsforschung	Redes, LA (autor correspondente), Univ Brasilia, Inst Geociencias, Lab Geocronol & Geoquim Isotop, BR-70910900 Brasilia, DF, Brazil.	leticiaredes@hotmail.com	Hauser, Natalia/H-2041-2012; Dantas, Elton Luiz/AAK-8464-2021; Reimold, Wolf Uwe/AAI-6226-2021; Ruiz, Amarildo Salina/M-3634-2014	Dantas, Elton Luiz/0000-0002-7954-5059; Ruiz, Amarildo Salina/0000-0002-7800-2837; Hauser, Natalia/0000-0002-6975-6186; Reimold, Wolf Uwe/0000-0001-6588-0887	National Council for Scientific and Technological Development (CNPq) of Brazil [141387/2015-7]; INCTET grant; Brazilian National Council for Scientific and Technological Development (CNPq) [309878/2019-5, 465613/2014-4, 305761/2019-6]	National Council for Scientific and Technological Development (CNPq) of Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); INCTET grant; Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was possible thanks to financial support from the National Council for Scientific and Technological Development (CNPq) of Brazil under grant 141387/2015-7 to L.A.R., and an INCTET grant. 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J	Rodrigues, SK; Machado, W; Guerra, JV; Geraldes, M; Morales, S; Vinzon, SB				Rodrigues, Sarah K.; Machado, Wilson; Guerra, Josefa V.; Geraldes, Mauro; Morales, Sheron; Vinzon, Susana B.			Changes in Cd and Zn distribution in sediments after closure of an electroplating industry, Sepetiba bay, Brazil	MARINE POLLUTION BULLETIN			English	Article						Enrichment factors; Sediment quality guidelines; Remediation; Trace metals attenuation	ENVIRONMENTAL-CHANGES; METALS; BIOAVAILABILITY; CONTAMINATION; HISTORY	The spatiotemporal attenuation of Cd and Zn concentrations was assessed in sediments from Sepetiba Bay, which is a coastal system that has been historically impacted by industrial wastes. The evolution of contamination over the years shortly before and after cessation of electroplating industry activities, by the end of 1990's, was elucidated by reviewing the existing datasets for the whole bay area. Metal concentrations exceed Brazilian Sediment Quality Guidelines in most regions, corresponding to concentrations 3 to 4 orders of magnitude higher than background levels and Enrichment Factors reaching values significantly higher than 40 for both elements. In the second decade after electroplating industry closure, the levels of Cd and Zn lowered in most regions of the bay. However, an increase in the relative importance of diffuse sources can mislead the current and future identification of Cd and Zn input, bringing new challenges for environmental monitoring and management for Sepetiba bay.	[Rodrigues, Sarah K.; Vinzon, Susana B.] Univ Fed Rio de Janeiro, Technol Ctr, Ocean Engn Dept, Lab Cohes Sediments Dynam LDSC, Athos Silveira Ramos SN,Bloco I,Sl 100, BR-21941902 Rio De Janeiro, Brazil; [Rodrigues, Sarah K.] Univ Espirito Santo State, Dept Oceanog, BR-29075910 Vitoria, ES, Brazil; [Machado, Wilson] Fed Fluminense Univ, Geochem Program, Outeiro Sao Joao Baptista S-N, BR-24020141 Niteroi, RJ, Brazil; [Guerra, Josefa V.; Geraldes, Mauro; Morales, Sheron] Univ Estado Rio De Janeiro, Sch Oceanog FAOC, Av Sao Francisco Xavier 524,4 Andar,Bloco E,Sala, BR-20550900 Maracana, RJ, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal Fluminense; Universidade do Estado do Rio de Janeiro	Rodrigues, SK (autor correspondente), Univ Fed Rio de Janeiro, Technol Ctr, Ocean Engn Dept, Lab Cohes Sediments Dynam LDSC, Athos Silveira Ramos SN,Bloco I,Sl 100, BR-21941902 Rio De Janeiro, Brazil.	sarah.skr@gmail.com	Geraldes, Mauro Cesar/AAA-6499-2022; Guerra, Josefa/AAV-5846-2020; Guerra, Josefa/M-8781-2019; Machado, Wilson/P-8047-2019	Geraldes, Mauro Cesar/0000-0003-2914-2814; Guerra, Josefa/0000-0001-9406-6470; Machado, Wilson/0000-0003-3117-8584; Rodrigues, Sarah/0000-0001-5838-8923	Coordination for the Improvement of Higher Education Personnel (CAPES) [001, 530/2010]; CNPq	Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	S.K.R thanks the Coordination for the Improvement of Higher Education Personnel (CAPES) for the scholarship. WM is grateful for support from CAPES (finance code 001). S.B.V. thanks CNPq (PQ Grant), and JVG thanks CAPES (grant #530/2010 Ciencias do Mar).	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DEC	2020	161		A						111758	10.1016/j.marpolbul.2020.111758	http://dx.doi.org/10.1016/j.marpolbul.2020.111758			7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	PG6NS	33096407				2023-06-23	WOS:000599850900003
J	Santos, MR; Roisenberg, A; Iwashita, F; Roisenberg, M				Rossi Santos, Matheus; Roisenberg, Ari; Iwashita, Fabio; Roisenberg, Mauro			Hydrogeochemical spatialization and controls of the Serra Geral Aquifer System in southern Brazil: A regional approach by self-organizing maps and k-means clustering	JOURNAL OF HYDROLOGY			English	Article						Serra Geral Aquifer System; SGAS; Regional hydrogeochemistry; Self-organizing maps; SOM; k-Means clustering	PARANA PLATEAU BRAZIL; SAO-PAULO STATE; HYDROCHEMICAL FACIES; GROUNDWATER; EVOLUTION; HYDROGEOLOGY; AMERICA; LAVAS	The aim of this study is to investigate the regional hydrogeochemical spatialization and controls of the Serra Geral Aquifer System (SGAS), a transboundary fractured aquifer, across the southern region of Brazil. An extensive dataset of 1564 groundwater wells represented by 16 attributes was analyzed to identify spatial patterns and groups with similar hydrogeochemical facies. An unsupervised machine learning approach, self-organizing maps (SOM), was used in combination with k-means clustering to carry out the analysis. SOM produces two-dimensional representations, allowing visual interpretation of nonlinear relationships between the attributes. The stochastic Davies-Bouldin index pointed out to an optimal number of four clusters, highlighting significant differences in geochemistry. Cluster 1 is the most abundant and widespread, corresponding to meteoric recharge; cluster 2 is influenced by the weathering of basaltic rocks, being widely distributed, but with a higher density at the southeastern region; cluster 3 is recognized as a mixing between all the other groups, with a sparse distribution, mostly in the extreme north of the area; cluster 4 is dominated by ascending flow from the underlying sedimentary aquifers, occurring in restricted areas. This study shows that SOM can identify large-scale spatial hydrogeochemical patterns of the SGAS driven by structural and stratigraphic elements.	[Rossi Santos, Matheus; Roisenberg, Ari] Univ Fed Rio Grande do Sul, Inst Geociencias, Campus Vale,Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Iwashita, Fabio] Univ Andes, Dept Geociencias, Cra 1a 18-12, Bogota, Colombia; [Roisenberg, Mauro] Univ Fed Santa Catarina, Dept Informat & Estat, BR-88040900 Florianopolis, SC, Brazil	Universidade Federal do Rio Grande do Sul; Universidad de los Andes (Colombia); Universidade Federal de Santa Catarina (UFSC)	Santos, MR (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Campus Vale,Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	matheus.rossi@ufrgs.br; ari.roisenberg@ufrgs.br; f.iwashita1@uniandes.edu.co; mauro.roisenberg@ufsc.br	ROISENBERG, ARI/N-8687-2013	ROISENBERG, ARI/0000-0001-6267-8296; Rossi Santos, Matheus/0000-0002-1604-381X	Brazilian National Council for Scientific and Technological Development (CNPq)	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the Brazilian National Council for Scientific and Technological Development (CNPq) for the scholarship granted to M.R.S. and the anonymous reviewers whose comments and suggestions helped to improve the article.	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Hydrol.	DEC	2020	591								125602	10.1016/j.jhydrol.2020.125602	http://dx.doi.org/10.1016/j.jhydrol.2020.125602			10	Engineering, Civil; Geosciences, Multidisciplinary; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Geology; Water Resources	PG5EL					2023-06-23	WOS:000599757800105
J	Saboia, AM; de Oliveira, CG; Dantas, EL; Scandolara, JE; Cordeiro, P; Rodrigues, JB; de Sousa, IMC				Saboia, Andre Menezes; de Oliveira, Claudinei Gouveia; Dantas, Elton Luis; Scandolara, Jaime Estevao; Cordeiro, Pedro; Rodrigues, Joseneusa Brilhante; Cordeiro de Sousa, Isabela Moreno			The 2.26 to 2.18 Ga Arc-Related Magmatism of the Almas-Conceicao do Tocantins Domain: An Early Stage of the Sao Francisco Paleocontinent Assembly in Central Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						I-type granites; Paleoproterozoic basement; Brasilia belt; Whole-rock geochemistry	MINEIRO BELT; GRANITOID TYPES; TRACE-ELEMENT; EVOLUTION; PB; SUPERCONTINENT; GEOCHEMISTRY; ROCK; DISCRIMINATION; GEOCHRONOLOGY	Paleoproterozoic (Rhyacian) rocks dominate within the basement of the Neoproterozoic Brasilia Belt and their genesis has been attributed to the orogenic amalgamation event that assembled the Sao Francisco-Congo paleocontinent from 2.18 to 2.07 Ga. However, the tectonic framework and genesis of the building blocks involved in this continent-wide amalgamation event are unclear, particularly in relation to terranes from the Almas-Conceicao do Tocantins Domain, in the Goi ' as Massif, central Brazil. This work provides new whole-rock chemical and geochronological data, which indicate the generation of felsic to intermediate magmatism around 2.29 and 2.28 Ga corresponding to the Monzogranitic Unit and the Quartz-dioritic Suite, respectively. Later magmatic events occurred in a continental arc setting, around 2.26 to 2.2 Ga represented by metaluminous to peraluminous I-type magmatism of the Granodioritic to Tonalitic Suite (GTS) and the Serra do Boqueirao Suite. Around 2.2 to 2.18 Ga a peraluminous I-type magmatism took place and generated the Peraluminous Suite (PS). Our data show that after an earlier Siderian magmatic event around 2.45-2.34 Ga, reported in previous works, the Almas do Conceicao do Tocantins Domain oversaw additional Rhyacian events of magmatic activity around 2.29 Ga to 2.18 Ga. Regional geotectonic correlations with the Sao Francisco Craton and other pericratonic belts indicate coeval magmatic events taking place during the early stages of the Columbia Supercontinent amalgamation.	[Saboia, Andre Menezes; Scandolara, Jaime Estevao; Rodrigues, Joseneusa Brilhante] Geol Survey Brazil, Setor Bancario Norte SBN, Quadra 02 Asa Norte,BLoco H,Edificio Cent Brasili, BR-70040904 Brasilia, DF, Brazil; [Saboia, Andre Menezes; de Oliveira, Claudinei Gouveia; Dantas, Elton Luis; Cordeiro de Sousa, Isabela Moreno] Univ Brasilia, Brazil Inst Geociencias, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Cordeiro, Pedro] Pontificia Univ Catolica Chile, Av Libertador Bernardo OHiggins 340, Santiago, Region Metropol, Chile	Universidade de Brasilia; Pontificia Universidad Catolica de Chile	Saboia, AM (autor correspondente), SQN 215,Bloco G,Apartamento 103, BR-70874070 Brasilia, DF, Brazil.	andre.saboia@cprm.gov.br; gouveia@unb.br; elton@unb.br; jaime.scandolara@cprm.gov.br; pedro.cordeiro@ing.puc.cl; joseneusa.rodrigues@cprm.gov.br; isabelamcds@gmail.com	Dantas, Elton Luiz/AAK-8464-2021; Cordeiro, Pedro/E-3044-2017	Dantas, Elton Luiz/0000-0002-7954-5059; Cordeiro, Pedro/0000-0003-1996-9551	CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) [305769/2019-7]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; INCT Estudos Tectonicos	CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); INCT Estudos Tectonicos	We thank the Institute of Geosciences of the University of Brasilia (IG/UnB) and the Geological Survey of Brazil (CPRM) for the field work support and the laboratory analysis. The CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) is acknowledged for grants provided to CGO (process number 305769/2019-7). We are grateful to Dr. Natalia Hauser, Dr. Andres Folguera and Dr. Reinhardt Fuck for handling this paper and to the three anonymous reviewers for the valuable suggestions and corrections that helped improve the article. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001 and the INCT Estudos Tectonicos.	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South Am. Earth Sci.	DEC	2020	104								102757	10.1016/j.jsames.2020.102757	http://dx.doi.org/10.1016/j.jsames.2020.102757			18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TL					2023-06-23	WOS:000600271800001
J	Santiago, R; Caxito, FD; Pedrosa-Soares, A; Neves, MA; Dantas, EL				Santiago, Raissa; Caxito, Fabricio de Andrade; Pedrosa-Soares, Antonio; Neves, Mirna Aparecida; Dantas, Elton Luiz			Tonian island arc remnants in the northern Ribeira orogen of Western Gondwana: The Caxixe batholith (Espirito Santo, SE Brazil)	PRECAMBRIAN RESEARCH			English	Article						LA-ICPMS; SHRIMP U-Pb geochronology; Hf-Nd-Sr isotope geochemistry; Magmatic arc; Adamastor Ocean; Brasiliano orogeny; Plate tectonics	NEOPROTEROZOIC CRUSTAL ACCRETION; CEARA CENTRAL DOMAIN; PROVINCE NE-BRAZIL; PB-HF ISOTOPES; U-PB; ARACUAI OROGEN; ANTI-ATLAS; BORBOREMA PROVINCE; TECTONIC EVOLUTION; BRASILIANO OROGEN	The Tonian Serra da Prata magmatic arc is part of an association of several magmatic arcs of the Ribeira orogenic system in Southeastern Brazil. Along with the Cryogenian Rio Negro arc, the Serra da Prata arc represents an infra-oceanic arc system while the Ediacaran Rio Doce arc represents an active continental margin arc. Here, we characterize the northernmost segment of the Serra da Prata arc, based on lithochemical and isotopic (whole-rock Sm-Nd and Rb-Sr, and zircon U-Pb and Lu-Hf) data from the Caxixe batholith, located in Espirito Santo State. The Caxixe batholith mostly consists of granodioritic to granitic and minor tonalitic to gabbroic rocks, with calc-alkaline, metaluminous to slightly peraluminous, magnesian, I-type signature and magmatic arc affinity. The rocks display LREE enrichment, positive to slightly negative Eu and negative Nb-Ta anomalies. Zircon U-Pb (LA-ICP-MS and SHRIMP) data reveal magmatic crystallization ages from 859 +/- 7 Ma to 847 +/- 8 Ma (for zircon cores) and a probably metamorphic age of 834 +/- 9 Ma (for zircon rims). Hf Isotopic data yield positive epsilon Hf-(t) values between + 10 and +14, and T-DM Hf model ages from 1.01 Ga to 0.84 Ga, in agreement with whole-rock Nd and Sr data with epsilon Nd-(t) values from + 0.9 to + 6.4 and T-DM Nd model ages between 1.2 Ga and 0.8 Ga, and Sr-87/Sr-86((i)) of 0.6979-0.7035. Our data characterize a juvenile magmatic arc with striking mantle contribution, formed on a supra-subduction intra-oceanic setting similar to modern island arcs. As a whole, the Serra da Prata juvenile arc points to a large ocean that underwent infra-oceanic subduction in the Early Tonian. As a corollary, the Angola, Congo - Sao Francisco and Paranapanema paleocontinental blocks should be far from each other during the Early Tonian, separated by that large ocean. In a broad scenario, involving ophiolites and juvenile arcs of southern and central Brazil, several cratons of Western Gondwana once had been parts of paleocontinental pieces separated by very extensive Tonian-Cryogenian oceanic realms, including the Neoproterozoic Goias-Pharusian and Adamastor oceans.	[Santiago, Raissa; Caxito, Fabricio de Andrade; Pedrosa-Soares, Antonio] Univ Fed Minas Gerais CPMTC IGC UFMG, Programa Posgrad Geol, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Santiago, Raissa; Caxito, Fabricio de Andrade; Pedrosa-Soares, Antonio] Univ Fed Minas Gerais CPMTC IGC UFMG, Ctr Pesquisas Manoel Teixeira Costa, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Neves, Mirna Aparecida] Univ Fed Espirito Santo, Ctr Ciencias Exatas Nat & Saude, Alto Univ S-N Guararema, BR-29500000 Alegre, ES, Brazil; [Dantas, Elton Luiz] Univ Brasilia, Inst Geociencias, Lab Geocronol, BR-70910900 Brasilia, DF, Brazil; [Caxito, Fabricio de Andrade] Brazilian Sci Council CNPq, Brasilia, DF, Brazil	Universidade Federal do Espirito Santo; Universidade de Brasilia	Santiago, R (autor correspondente), Univ Fed Minas Gerais CPMTC IGC UFMG, Programa Posgrad Geol, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.; Santiago, R (autor correspondente), Univ Fed Minas Gerais CPMTC IGC UFMG, Ctr Pesquisas Manoel Teixeira Costa, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.	raissa.smendes@gmail.com; caxito@ufmg.br; pedrosasoares@gmail.com; mirnaan@gmail.com; elton@unb.br	Caxito, Fabricio A/J-1317-2016; Dantas, Elton Luiz/AAK-8464-2021	Caxito, Fabricio A/0000-0002-0335-3667; Dantas, Elton Luiz/0000-0002-7954-5059	CNPq; CAPES; Instituto Serrapilheira [Serra-1912-31510];  [303566/2019-1]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Instituto Serrapilheira; 	The authors are grateful to the Brazilian research and development agencies (CNPq and CAPES) for financial support. SHRIMP work at the John de Laeter Center is enabled by NCRIS via AuScope. We thank Neal McNaughton, Allen Kennedy, Hao Gao and all of the John de Laeter staff for guidance and support during the analysis. FAC, ACPS and ELD are fellows of the Brazilian Scientific Council (CNPq) and acknowledge the financial support received, especially through grant 303566/2019-1 to FAC. An earlier version of this paper was greatly enhanced after comments and suggestions by Monica Heilbron and Donnelly Archibald. This paper is a contribution to Project MOBILE: Mountains Belts and the Inception of Complex Life on Earth (geolifemobile.com), supported by Instituto Serrapilheira (Serra-1912-31510).	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J	Santos, AS; dos Santos, LO; Pereira, JB; de Oliveira, FM; Ferreira, SLC				Santos, Adilson Santana; dos Santos, Liz Oliveira; Pereira Junior, Joao B.; de Oliveira, Fernando M.; Ferreira, Sergio L. C.			Development of reference material from powdered milk: Uncertainties and interlaboratory evaluation through confidence ellipses	MICROCHEMICAL JOURNAL			English	Article						Characterization; Uncertainty evaluation; Confidence ellipses; Reference material	CERTIFICATION; REQUIREMENTS; HOMOGENEITY	Characterization and evaluation of the uncertainty of new powdered milk laboratory reference material were proposed following the recommendations of the ISO Guide 35. A characterization was established through the interlaboratory comparison with the participation of 15 laboratories, being one international. To obtain the property value, initially, the data from the collaborative trial were statistically evaluated using the Grubbs, Cochran, and z-scores tests to identify possible outliers. One-way ANOVA and linear regression analysis were employed to obtain the standard uncertainties associated with characterization (u(char)), between-bottle homogeneity (u(bb)), and long-term stability (u(lts)). The properties values and combined uncertainty (U-RM) for at the 95% confidence level (k = 2) were as follows (mg g(-1)): Ca (8.795 +/- 1.137), Fe (0.107 +/- 0.017), K (11.727 +/- 1.983), Mg (0.841 +/- 0.125), Na (3.654 +/- 0.672), P (7.572 +/- 1.174), and Zn (0.032 +/- 0.005). Based on the confidence ellipses obtained in the results of the laboratories, it was possible to infer the causes that led to the dispersion of the values. The new material can be a good alternative to evaluate routine procedures, quality control, and validation of analytical methods related to samples of milk and dairy products.	[Santos, Adilson Santana; dos Santos, Liz Oliveira; Pereira Junior, Joao B.; Ferreira, Sergio L. C.] Univ Fed Bahia, Inst Quim, Grp Pesquisa Quim & Quimiometria, Campus Ondina, BR-40170270 Salvador, BA, Brazil; [Santos, Adilson Santana; dos Santos, Liz Oliveira; Pereira Junior, Joao B.; Ferreira, Sergio L. C.] Univ Fed Bahia, Inst Nacl Ciencia & Tecnol, Energia & Ambiente, INCT, BR-40170290 Salvador, BA, Brazil; [dos Santos, Liz Oliveira] Univ Fed Reconcavo Bahia, Ctr Ciencia & Tecnol Energia & Sustentabilidade C, BR-44085132 Feira De Santana, BA, Brazil; [de Oliveira, Fernando M.] Labwin Serv Especializados Ltda, Av Luis Viana Filho,Km 10,S 405, BR-41730101 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal do Reconcavo da Bahia	Santos, AS (autor correspondente), Univ Fed Bahia, Inst Quim, BR-40170270 Salvador, BA, Brazil.	adilsonquesb@gmail.com	PEREIRA JUNIOR, JOAO B/J-1487-2016; dos Santos, Liz Oliveira/Q-8289-2019	PEREIRA JUNIOR, JOAO B/0000-0002-7851-8235; dos Santos, Liz Oliveira/0000-0003-2064-2097	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	Authors are grateful to Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), to Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB) and to Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) Finance Code 001 for providing grants and fellowships and for financial support. The authors are also grateful to the laboratories that contributed to the collaborative trial (see Table S1 in the Supplementary Material).	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DEC	2020	159								105330	10.1016/j.microc.2020.105330	http://dx.doi.org/10.1016/j.microc.2020.105330			7	Chemistry, Analytical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	PF0NS					2023-06-23	WOS:000598762000002
J	Scherer, CMS; Mello, RG; Ferronatto, JPF; Amarante, FB; Reis, AD; Souza, EG; Goldberg, K				Scherer, Claiton M. S.; Mello, Raquel G.; Ferronatto, Joao P. F.; Amarante, Francyne B.; Reis, Adriano D.; Souza, Ezequiel G.; Goldberg, Karin			Changes in prevailing surface-palaeowinds of western Gondwana during Early Cretaceous	CRETACEOUS RESEARCH			English	Article						Palaeowinds; Southwest Gondwana; Late Jurassic-Early Cretaceous; Megamonsson	CENTRAL NEUQUEN BASIN; PARANA BASIN; HADLEY CIRCULATION; BOTUCATU FORMATION; LOWSTAND WEDGE; STRATIGRAPHY; PRESERVATION; CLIMATE; EXAMPLE; BRAZIL	The comparison between reconstructed paleocurrent data from eolian dune deposits and models for atmospheric circulation shows that a monsoonal circulation pattern operated in the low latitudes of Gondwana until the Hauterivian. Trade winds from the Northern Hemisphere crossed the Equator and were re-oriented to the south, shifting the Intertropical Convergence Zone to paleolatitudes around 25 degrees S, where the convergence with westerlies winds occurred. The rupture of the monsoonal pattern and the establishment of a zonal pattern, characterized by dry trade winds blowing to NW in the low latitudes of Gondwana, occurred in the Barremian as a result of the fragmentation of Gondwana. (C) 2020 Elsevier Ltd. All rights reserved.	[Scherer, Claiton M. S.; Mello, Raquel G.; Ferronatto, Joao P. F.; Amarante, Francyne B.; Reis, Adriano D.] Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil; [Souza, Ezequiel G.] Univ Fed Pampa, Cacapava Do Sul, Brazil; [Goldberg, Karin] Kansas State Univ, Dept Geol, Manhattan, KS 66506 USA	Universidade Federal do Rio Grande do Sul; Universidade Federal do Pampa; Kansas State University	Scherer, CMS (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil.	claiton.scherer@ufrgs.br	Reis, Adriano/E-3744-2015; Amarante, Francyne/AAO-7294-2020	Reis, Adriano/0000-0003-1892-8459; Amarante, Francyne/0000-0003-4452-8635; Santos Scherer, Claiton Marlon dos/0000-0002-7520-1187; Galvao de Souza, Ezequiel/0000-0003-3829-0747; Gewehr de Mello, Raquel/0000-0002-4445-8369	Brazilian Research Council (CNPq)	Brazilian Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank Drs. Michel Holz and Chihua Wu for their constructive reviews of the manuscript, as well as Eduardo Koutsoukos for editorial assistance. This work was supported by Brazilian Research Council (CNPq). The authors wish to thank Dr. Christopher Scotese for access to the paleogeographic reconstructions and correction of mean paleocurrent vectors.	Arai M., 1995, 14 C BRAS PAL UB, P2; Scotti AA, 2019, SEDIMENTOLOGY, V66, P2191, DOI 10.1111/sed.12597; Brierley CM, 2009, SCIENCE, V323, P1714, DOI 10.1126/science.1167625; Costa I.P., 2007, B GEOCIENCIAS PETROB, V15, P445; do Amarante FB, 2019, J S AM EARTH SCI, V90, P355, DOI 10.1016/j.jsames.2018.12.024; Do CARMO D. 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R., 2016, PALEOMAP PALEOATLAS; Scotese CR, 1986, GEOBYTE, V1, P28; SGARBI G.N.C., 2000, REV BRAS GEOSCI, V30, P450, DOI 10.25249/0375-7536.2000303450452; Thiede DS, 2010, GEOLOGY, V38, P747, DOI 10.1130/G30919.1; Veiga GD, 2005, GEOL SOC SPEC PUBL, V252, P139, DOI 10.1144/GSL.SP.2005.252.01.07; Veiga GD, 2002, SEDIMENTOLOGY, V49, P1001, DOI 10.1046/j.1365-3091.2002.00487.x; Veiga GD, 2007, GONDWANA RES, V11, P286, DOI 10.1016/j.gr.2006.05.002; Viana C.F., 1971, B TECNICO PETROBRAS, V14, P157; Webster PJ, 1987, MONSOONS, P3; Wiederkehr F., 2010, THESIS, P100	35	12	12	0	4	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	DEC	2020	116								104598	10.1016/j.cretres.2020.104598	http://dx.doi.org/10.1016/j.cretres.2020.104598			9	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	OD4KR					2023-06-23	WOS:000579821800023
J	Schultz, CL; Martinelli, AG; Soares, MB; Pinheiro, FL; Kerber, L; Horn, BLD; Pretto, FA; Muller, RT; Melo, TP				Schultz, Cesar L.; Martinelli, Agustin G.; Soares, Marina B.; Pinheiro, Felipe L.; Kerber, Leonardo; Horn, Bruno L. D.; Pretto, Flavio A.; Muller, Rodrigo T.; Melo, Tomaz P.			Triassic faunal successions of the Parana Basin, southern Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Middle-Late Triassic; Faunal associations; South America; Fossil record; Biostratigraphy		The Parana Basin was filled by a sedimentary package deposited in successive sedimentation episodes related to the tectonic events that hit the SW portion of the Gondwana. The Triassic portion of this package, known worldwide for its continental tetrapod fauna, occurs only in the southern portion of the basin and is represented by 2 s-order sequences: the Sanga do Cabral Supersequence (SCS Early Triassic) and the Santa Maria Supersequence (SMS Middle-Late Triassic). The SCS fauna, including temnospondyls, parareptiles (mainly Procolophon), archosauromorphs, putative synapsids, and a number of indeterminate specimens, is traditionally considered Early Triassic and corresponds to the "Procolophon abundant zone" of the Karoo Basin (the upper levels of the Lystrosaurus AZ), in the upper Katberg Formation, which is Induan to early Olenekian in age. The sedimentary environment of the SCS is thought to be a wide alluvial plain, in which small and shallow channels spread northwards into a vast semiarid environment. By its turn, the Middle-Upper Triassic Santa Maria Supersequence is divided into four third-order sequences, from base to top: Pinheiros-Chiniqua, Santa Cruz, Candelaria and Mata. Each of these sequences begins with fluvial deposition (low sinuosity rivers) that is overlain by transgressive shallow lacustrine deposits. The first three of these sequences present a very rich record of fossil tetrapods, including four successive faunal associations: Dinodontosaurus Assemblage Zone (Ladinian, within the Pinheiros-Chiniqua Sequence), Santacruzodon AZ (Ladinian/Carnian, in the Santa Cruz Sequence), Hyperodapedon AZ (Carnian) and the Riograndia AZ (early Norian), the latter two respectively at the base and top of the Candel ' aria Sequence. In general, the lower portion of the package (Pinheiros-Chiniqua and Santa Cruz Sequences) was deposited under more basic and dried environmental conditions and are dominated by synapsids, while the top of the section (Candelaria Sequence) is characterized by more acid and humid conditions and by a shift in the faunal content, with diapsids as dominating forms and presenting an increase of diversity compared to the lower biozones.	[Schultz, Cesar L.; Melo, Tomaz P.] PPGGeo Univ Fed Rio Grande Sul, Ave Bento Goncalves,9500, BR-91540000 Porto Alegre, RS, Brazil; [Martinelli, Agustin G.] CONICET Museo Argentino Ciencias Natr Bernardino, Ave Angel Gallardo 470,C1405 DJR, Buenos Aires, DF, Argentina; [Soares, Marina B.] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Quinta Boa Vista S-N, BR-20940040 Rio De Janeiro, Brazil; [Pinheiro, Felipe L.] Univ Fed Pampa, Lab Paleobiol, Ave Antonio Trilha,1847, Sao Gabriel, Brazil; [Kerber, Leonardo; Pretto, Flavio A.; Muller, Rodrigo T.] Univ Fed Santa Maria, Ctr Apoio Pesquisa Paleontol Quarta Colonia CAPPA, Sao Joao Do Polesine, RS, Brazil; [Horn, Bruno L. D.] Superintendencia Reg Porto Alegre, Serv Geol Brasil CPRM, Rua Banco Prov,105, BR-90840030 Porto Alegre, RS, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Pampa; Universidade Federal de Santa Maria (UFSM)	Schultz, CL (autor correspondente), PPGGeo Univ Fed Rio Grande Sul, Ave Bento Goncalves,9500, BR-91540000 Porto Alegre, RS, Brazil.	cesar.schultz@ufrgs.br; agustin_martinelli@yahoo.com.ar; marina.soares@mn.ufrj.br; felipepinheiro@unipampa.edu.br	Melo, Tomaz P/I-5304-2017; Kerber, Leonardo/O-3980-2017; Melo, Tomaz Panceri/AFV-5804-2022; Kerber, Leonardo/M-3969-2019; Soares, Marina/M-9477-2017	Melo, Tomaz P/0000-0002-6203-560X; Kerber, Leonardo/0000-0001-8139-1493; Melo, Tomaz Panceri/0000-0002-6203-560X; Kerber, Leonardo/0000-0001-8139-1493; Soares, Marina/0000-0002-8393-2406; Martinelli, Agustin/0000-0003-4489-0888; Pinheiro, Felipe/0000-0003-3354-914X	Fundacno de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [16/2551-0000271-1]; Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico [407969/2016-0, 305758/2017-9]	Fundacno de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS); Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Initially, we would like to thank Drs. Claudia Marsicano, Leandro Gaetano and Randall Irmis for the invitation to produce a chapter for this Special Volume on the Triassic at JSAES. For access to collections we thank: Carlos Nunes Rodrigues (MMACR), Belarmino Stefanello (MMACR), Ana Maria Ribeiro (MCN-FZB), Jorge Ferigolo (MCN-FZB), Marco Brandalise de Andrade (MCP-PUC), Rodrigo Machado (MCT), and DiOgenes de Almeida Campos (MCT). Several photographs of this contribution were skillfully taken by Luiz Flavio Lopes (UFRGS). MB S is supported by grant from Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico (CNPq process numbers 407969/2016-0). FLP is supported by grants from Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico (CNPQ process numbers 407969/2016-0, 305758/2017-9) and Fundacno de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS process number 16/2551-0000271-1). Finally, the comments made by the reviewers Max C. Langer and Martin D. Ezcurra greatly improved the ms.		0	40	40	3	14	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	DEC	2020	104								102846	10.1016/j.jsames.2020.102846	http://dx.doi.org/10.1016/j.jsames.2020.102846			24	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2TP					2023-06-23	WOS:000600272200002
J	Schutesky, ME; de Oliveira, CG				Schutesky, Maria Emilia; de Oliveira, Claudinei Gouveia			From the roots to the roof: An integrated model for the Neoarchean Carajas IOCG System, Brazil	ORE GEOLOGY REVIEWS			English	Article						Iron-oxide copper-gold deposits; Carajas Mineral Province; Neoarchean; Vertical zoning; Magnetite-chalcopyrite-gold ore	OXIDE-COPPER-GOLD; MAGMATIC-HYDROTHERMAL PROCESSES; TRACE-ELEMENT GEOCHEMISTRY; APATITE IOA DEPOSITS; U-PB GEOCHRONOLOGY; MINERAL PROVINCE; AMAZONIAN CRATON; RE-OS; ORE-DEPOSIT; DOS-CARAJAS	The Carajas Mineral Province, located in northern Brazil, comprises the oldest iron-oxide copper-gold mineralizing system on Earth and is one of the world's most significant cluster of large-tonnage IOCG deposits. Based on a critical assessment of the literature a new integrated model for the Carajas Neoarchean IOCG deposits. The model considers the hydrothermal alteration footprint and the rock textures, the geometry of the mineralization and the ore assemblage, and the isotopic and geochronological signature. The majority of the deposits form in the hypozonal domain. Pervasive and well-developed sodic (-magnesian) and calcic-iron hydrothermal alteration halos form through magmatic-derived hydrothermal fluids. The occurrence of hydrothermal orthopyroxene (-marialite) in the Ni-rich GT-34 and Salobo deposits extend further the P-T boundaries to temperatures of up to 700 degrees C and > 5 kbars, thus co is proposedrresponding to the mot zone of the system. Epizonal deposits, conversely, are characterized by low-temperature potassic (biotite/phlogopite), propylitic and chlorine-hydrolytic hydrothermal assemblages, towards shallower crustal levels. Although a mantle contribution to the hydrothermal fluids is recognized, the O-B stable isotopic signature reveals the participation of surface-derived, basinal brines, in the ore-forming process. The occurrence of polymetallic ooids in the Alerono orebody (Igarape-Bahia deposit), hosting identical hydrothermal alteration mineralogy to the chalcopyrite breccias of other IOCG deposits in the Carajas Mineral Province suggests that the mineralizing fluids may have reached the paleo-surface of the Carajas basin in the Neoarchean, representing the roof of the IOCG system. Conversely, the ore mineralogy is consistent throughout the vertical scheme. Magnetite is the only iron oxide formed and precipitate from ironrich hydrothermal alteration accompanying the calcic alteration. Similarly, chalcopyrite represents the Cu sulfide. There is no transition to more oxidized assemblages towards shallower zones, supporting that the overall system was relatively reduced since more oxidizing phases (hematite, bornite) are not observed as part of the Neoarchean IOCG system. Thus, the Neoarchean Carajas IOCG System represents a crustal-scale continuum, of a vertical paleo-hydrothermal system formed coevally to the voluminous, bimodal magmatism and the formation of the world-class, banded iron formation hosted iron ore.	[Schutesky, Maria Emilia; de Oliveira, Claudinei Gouveia] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, Brasilia, DF, Brazil	Universidade de Brasilia	Schutesky, ME (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, Brasilia, DF, Brazil.	maria_emilia@unb.br	Schutesky, Maria/L-9910-2015	Schutesky, Maria/0000-0001-8516-102X	Brazilian Research Council (CNPq); Coordenacno de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]; Swedish Link Programme [348-2012-6165]	Brazilian Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacno de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Swedish Link Programme	MESDG and CGO are thankful to Dr. Steffen Haggemann, as guest editor, for his exhaustive and careful review. Dr. Martin Reich and three anonymous reviewers are acknowledged for their constructive commentaries, which significantly improved the paper. VALE is recognized for logistics and support during fieldwork and sampling in Carajas; special thanks are due to Dr. Sergio Huhn and Fernando Matos for the discussions on the Cara.* metallogeny. The authors are grateful for the continuous support from the Brazilian. Research Council (CNPq). Part of this study was funded by The Swedish Link Programme (project #348-2012-6165) and also by the Coordenacno de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001. This paper is a contribution of the Precambrian Metallogenesis Research Group (DGP-CNPq).	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J	Neto, BMT; Combi, T; Taniguchi, S; Albergaria-Barbosa, ACR; Ramos, RB; Figueira, RCL; Montone, RC				Sotao Neto, Basilio M. T.; Combi, Tatiane; Taniguchi, Satie; Albergaria-Barbosa, Ana C. R.; Ramos, Raissa B.; Lopes Figueira, Rubens Cesar; Montone, Rosalinda C.			Persistent organic pollutants (POPs) and personal care products (PCPs) in the surface sediments of a large tropical bay (Todos os Santos Bay, Brazil)	MARINE POLLUTION BULLETIN			English	Article						Legacy contaminants; Emerging contaminants; Mass inventories; GC/MS/MS	POLYCHLORINATED-BIPHENYLS PCBS; PEARL RIVER DELTA; ORGANOCHLORINE PESTICIDES OCPS; UV-FILTERS; ENVIRONMENTAL OCCURRENCE; MARINE-SEDIMENTS; AROMATIC-HYDROCARBONS; SPATIAL-DISTRIBUTION; METAL CONTAMINATION; MUSK FRAGRANCES	The occurrence and spatial distribution of persistent organic pollutants (POPs) and personal care products (PCPs) were investigated in surface sediments of Todos os Santos Bay. Samples were Soxhlet-extracted and analyzed by gas chromatography coupled with tandem mass spectrometry. Quantification limits (QL) ranged from 0.0025 ng g(-1) for POPs to 0.25 ng g(-1) for PCPs. Of the POPs studied, only PCBs and DDTs were detectable, with concentrations ranging from <QL to 4.66 ng g(-1), with increased concentrations near urban and industrial areas. PCPs ranged from <QL to 27.5 ng g(-1) and presented a homogeneous spatial distribution, probably related to the continuous inputs of these compounds from diffuse sources. Mean contaminant inventories ranged from 0.33 +/- 0.23 ng cm(-2) for DDTs to 8.3 +/- 8.4 ng cm(-2) for fragrances. To the best of our knowledge, this is the first study on the occurrence of UV filters in sediments from Brazilian coastal environments.	[Sotao Neto, Basilio M. T.; Taniguchi, Satie; Ramos, Raissa B.; Lopes Figueira, Rubens Cesar; Montone, Rosalinda C.] Univ Sao Paulo, Inst Oceanog, Praca Oceanog 191, BR-05508120 Sao Paulo, SP, Brazil; [Combi, Tatiane; Albergaria-Barbosa, Ana C. R.] Univ Fed Bahia, Inst Geociencias, Dept Oceanog, Rua Barao Jeremoabo, BR-40170020 Salvador, BA, Brazil	Universidade de Sao Paulo; Universidade Federal da Bahia	Combi, T (autor correspondente), Univ Fed Bahia, Inst Geociencias, Dept Oceanog, Rua Barao Jeremoabo, BR-40170020 Salvador, BA, Brazil.	tatiane.combi@ufba.br	de Albergaria-Barbosa, Ana Cecília/AAC-6940-2021; Combi, Tatiane/AAC-9936-2021; Taniguchi, Satie/D-2552-2013; Combi, Tatiane/O-3004-2016	Taniguchi, Satie/0000-0002-6825-6390; RAMOS, RAISSA/0000-0002-7652-2249; Combi, Tatiane/0000-0001-6769-7445	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001]; CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico); Bahia Science Foundation (FAPESB) [9017/2014]; Sao Paulo Research Foundation (FAPESP) [2016/18348-1]; FAPESP [2016/21368-4]; CNPq [PQ 305210/2019-0, PQ 305373/2018-8]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Bahia Science Foundation (FAPESB); Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was developed as part of a graduate course on Oceanography at the Oceanographic Institute of the University of Sao Paulo (PPGO-IOUSP), supported by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) - financial code 001. Sotao Neto thanks CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) for the MSc. Scholarship. This study was supported by the Bahia Science Foundation (FAPESB, project number 9017/2014) and the Sao Paulo Research Foundation (FAPESP, project number 2016/18348-1; for the use of GC/MS/MS). The authors would like to thank Dr. Rosivaldo Mendes from Evandro Chagas Institute for providing information about insecticide stocks in Brazil. We are indebted to the Belov Engenharia Ltda for the financial support during the sampling campaigns. Combi thanks FAPESP for the postdoctoral fellowship (grant number 2016/21368-4). Albergaria-Barbosa (PQ 305210/2019-0) and Montone (PQ 305373/2018-8) thank CNPq for the grants received.	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Pollut. Bull.	DEC	2020	161		B						111818	10.1016/j.marpolbul.2020.111818	http://dx.doi.org/10.1016/j.marpolbul.2020.111818			8	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	PG6KZ	33160119				2023-06-23	WOS:000599843800013
J	Souza, JSB; Ferreira, JM; Simonelli, G; Souza, JR; Gois, LMN; Santos, LCL				Souza, J. S. B.; Ferreira Junior, J. M.; Simonelli, G.; Souza, J. R.; Gois, L. M. N.; Santos, L. C. L.			Removal of oil contents and salinity from produced water using microemulsion	JOURNAL OF WATER PROCESS ENGINEERING			English	Article						Produced water treatment; Microemulsion; Oil and grease content; Salinity		Recently, the region of Winsor II has been used to treat produced water to decrease heavy metals amount and oils and greases contents (OGC). However, it usually demands high temperature, and the interaction effect of the process factors have not yet been investigated. This study has the objective of treating synthetic and real produced water using the region of Winsor IV (microemulsions) to reduce the oil and grease content and also the salinity. Besides, we also statistically investigated the effect of temperature, time, and microemulsion amount. Synthetic produced water (SPW) treatment was studied through the experimental design with combinations for three variables: time (30-90 min), temperature (25-45 degrees C), and microemulsion percentage (10-50%). The conditions established for the treatment of real produced water (RPW) were: 30 min, 35 degrees C, and 50 % of the microemulsion. It was observed that on the treatment of SPW, the OGC reduction ranged from 69.98 % to 97.98 % and the salinity from 18.74 % to 34.66 %. Regarding the treatment of RPW, the OGC reduction was 86.23 %, from 146.56 mg.L-1 to 20.18 mg.L-1, and the reduction of salinity was 11.86 %, from 35,090.20 mg.L-1 to 30,928.50 mg.L-1. We concluded that the treatments of SPW and RPW using microemulsion to reduce OGC and salinity were efficient.	[Souza, J. S. B.; Ferreira Junior, J. M.; Simonelli, G.; Santos, L. C. L.] Univ Fed Bahia, Postgrad Program Chem Engn, R Prof Aristides Novis 2,2 Andar, BR-40210630 Salvador, BA, Brazil; [Souza, J. R.] Joule Energy Ltda, R Alvares de Azevedo 203, BR-13465573 Americana, SP, Brazil; [Gois, L. M. N.] Univ Salvador, Campus Rio Vermelho,Av Juracy Magalhaes Jr 209, BR-41940060 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Salvador (UNIFACS)	Santos, LCL (autor correspondente), Univ Fed Bahia, Postgrad Program Chem Engn, R Prof Aristides Novis 2,2 Andar, BR-40210630 Salvador, BA, Brazil.	josysbsouza@yahoo.com.br; jmfj@ufba.br; gsimonelli@ufba.br; jrobert9@gmail.com; luiz.gois@unifacs.br; lclsantos@ufba.br	Santos, Luiz Carlos Lobato/F-2805-2013; Simonelli, George/W-5235-2019; Ferreira Jr, José Mario/G-4147-2016	Santos, Luiz Carlos Lobato/0000-0003-3824-7802; Simonelli, George/0000-0002-8031-1401; Ferreira Jr, José Mario/0000-0003-4295-6417	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Programa de Recursos Humanos em Petroleo e Meio Ambiente da UFBA; Agencia Nacional de Petroleo, Gas Natural e Biocombustiveis (ANP); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Programa de Recursos Humanos em Petroleo e Meio Ambiente da UFBA; Agencia Nacional de Petroleo, Gas Natural e Biocombustiveis (ANP); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors are grateful to the Brazilian fomentation agencies Fundacao de Amparo.a Pesquisa do Estado da Bahia (FAPESB) and Programa de Recursos Humanos em Petr.oleo e Meio Ambiente da UFBA, of the Agencia Nacional de Petr.oleo, Gas Natural e Biocombustiveis (ANP) for financial support. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001.	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Water Process. Eng.	DEC	2020	38								101548	10.1016/j.jwpe.2020.101548	http://dx.doi.org/10.1016/j.jwpe.2020.101548			9	Engineering, Environmental; Engineering, Chemical; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Water Resources	PE1PQ					2023-06-23	WOS:000598143500007
J	Tschoeke, DA; Coutinho, FH; Leomil, L; Cavalcanti, G; Silva, BS; Garcia, GD; dos Anjos, LC; Nascimento, LB; Moreira, LS; Otsuki, K; Cordeiro, RC; Rezende, CE; Thompson, FL; Thompson, CC				Tschoeke, Diogo A.; Coutinho, Felipe H.; Leomil, Luciana; Cavalcanti, Giselle; Silva, Bruno S.; Garcia, Gizele D.; dos Anjos, Leandro Candeia; Nascimento, Larissa Borges; Moreira, Luciane S.; Otsuki, Koko; Cordeiro, Renato C.; Rezende, Carlos E.; Thompson, Fabiano L.; Thompson, Cristiane C.			New bacterial and archaeal lineages discovered in organic rich sediments of a large tropical Bay	MARINE GENOMICS			English	Article						Guanabara Bay; Metagenome; Genome; Guanabacteria	COMPLETE GENOME SEQUENCE; ANAEROBIC OXIDATION; STRATIFIED COMMUNITIES; METHANOGENIC ARCHAEA; ACTIVE ARCHAEA; GUANABARA BAY; METHANE; SULFUR; BATHYARCHAEOTA; METABOLISM	The nutrient and oxygen gradient present in marine sediments promotes high levels of microbial diversity. We applied metagenomics and biogeochemical tools to analyze microbial communities in different sediment depths (0-4 m below sea floor, mbsf) from Guanabara Bay, Brazil, a brackish tropical ecosystem with a history of massive anthropogenic impacts, and a largely unknown sediment microbial diversity. Methanogens (e.g. Methanosarcinales, Methanomicrobiales) were more abundant at 1 mbsf, while sulphate-reducing microbes (Desulfurococcales, Thermoprotales, and Sulfolobales) were more abundant at deeper layers (4 mbsf; corresponding to 3 K Radiocarbon years before present, Holocene Epoch). Taxonomic analyzes and functional gene identification associated with anaerobic methane oxidation (e.g. monomethylamine methyltransferase (mtmB), trimethylamine methyltransferase (mttB) and CO dehydrogenase/acetyl-CoA synthase delta subunit) and sulfate reduction indicated the dominance of Campylobacteria (Sulfurimonas) at deeper sediment layers. Gene sequences related to assimilation of inorganic sulfur increased with depth, while organic sulfur related sequences decrease, accompanying the clear reduction in the concentration of sulfur, organic carbon and chla torwards deeper layers. Analyzes of metagenome assembled genomes also led to the discovery of a novel order within the phylum Acidobacteriota, named Guanabacteria. This novel order had several in silico phenotyping features that differentiate it from closely related phylogenetic neighbors (e.g. Acidobacteria, Aminicenantes, and Thermoanaerobaculum), including several genes (carbon monoxide dehydrogenase, CO dehydrogenase/CO-methylating acetyl-CoA synthase complex subunit beta, heterodisulfide reductase, sulfite exporter TauE/SafE family protein, sulfurtransferase) that relevant for the S and C cycles. Furthermore, the recovered Bathyarchaeota genome SS9 illustrates the methanogenic potential in deeper sediment layer.	[Tschoeke, Diogo A.; Coutinho, Felipe H.; Leomil, Luciana; Cavalcanti, Giselle; Silva, Bruno S.; Garcia, Gizele D.; Otsuki, Koko; Thompson, Fabiano L.; Thompson, Cristiane C.] Univ Fed Rio De Janeiro UFRJ, Inst Biol, Lab Microbiol, Rio De Janeiro, RJ, Brazil; [Tschoeke, Diogo A.; Leomil, Luciana; Cavalcanti, Giselle; Silva, Bruno S.; Otsuki, Koko; Thompson, Fabiano L.; Thompson, Cristiane C.] Univ Fed Rio De Janeiro UFRJ, Ctr Gestao Tecnol CT2, Nucleo Prof Rogerio Valle Prod Sustentavel SAGE C, Rio De Janeiro, RJ, Brazil; [Tschoeke, Diogo A.] Univ Fed Rio De Janeiro UFRJ, COPPE, Programa Engn Biomed, CT, Rio De Janeiro, RJ, Brazil; [Coutinho, Felipe H.] Univ Miguel Hernandez, Dept Prod Vegetal & Microbiol, Evolutionary Genom Grp, Alicante, Spain; [Garcia, Gizele D.] Univ Fed Rio De Janeiro UFRJ, Dept Ensino Graduacao, Campus UFRJ, Macae, RJ, Brazil; [dos Anjos, Leandro Candeia; Nascimento, Larissa Borges; Moreira, Luciane S.; Cordeiro, Renato C.] Univ Fed Fluminense, Inst Quim, Dept Geoquim, Programa Geoquim, Niteroi, RJ, Brazil; [Rezende, Carlos E.] Univ Estadual Norte Fluminense, UENF, Ctr Biociencias & Biotecnol, Lab Ciencias Ambientais, Campos Dos Goytacazes, RJ, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidad Miguel Hernandez de Elche; Universidade Federal do Rio de Janeiro; Universidade Federal Fluminense; Universidade Estadual do Norte Fluminense	Tschoeke, DA; Thompson, CC (autor correspondente), CCS, IB, Lab Microbiol, Av Carlos Chagas Fo S-N,Bloco Anexo A3,Sl 302, BR-21941599 Rio De Janeiro, RJ, Brazil.	diogoat@peb.ufrj.br; cristianethompson@biologia.ufrj.br	Tschoeke, Diogo A/F-9913-2019; Rezende, Carlos EE/N-7819-2017; Garcia, Gizele Duarte/GLS-9270-2022; Moreira, luciane Silva/AAF-9913-2021; Tschoeke, Diogo/AAB-4739-2021; Silva, Bruno Sergio/ISV-5972-2023; Cordeiro, Renato C/J-8870-2013	Tschoeke, Diogo A/0000-0001-8134-4259; Rezende, Carlos EE/0000-0002-6072-4284; Garcia, Gizele Duarte/0000-0001-9844-6729; Moreira, luciane Silva/0000-0002-8721-8752; Cordeiro, Renato C/0000-0002-6785-601X; Thompson, Fabiano/0000-0002-7562-1683; Coutinho, Felipe/0000-0001-6430-7069	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [E-26/111.625/2011]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	We thank the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) and Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ), project "Variabilidade climatica, oceanica e antropica na Baia de Guanabara: perspectiva comparativa em diversas escalas temporais" (E-26/111.625/2011) for financial support and fellowships.	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Genom.	DEC	2020	54								100789	10.1016/j.margen.2020.100789	http://dx.doi.org/10.1016/j.margen.2020.100789			12	Genetics & Heredity; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Genetics & Heredity; Marine & Freshwater Biology	OY0GD	32563694				2023-06-23	WOS:000593931800006
J	Uchoa, EB; Silva, NCV; Magini, C; Branco, RMGC; Fuck, RA; da Silva, FM; Martins, JA; Silva, CRME				Uchoa, Elenilton Bezerra; Vieira Silva, Nilton Cesar; Magini, Christiano; Gomes Castelo Branco, Raimundo Mariano; Fuck, Reinhardt Adolfo; da Silva, Fabiano Mota; Martins, Jackson Alves; Maia e Silva, Charles Regis			Magnetotelluric transect across the Sao Luis cratonic fragment, the Gurupi belt and the Parnaiba basin, N-NE Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Magnetotellurics; Sao Luis cratonic fragment; Lineaments	EVOLUTION; DECOMPOSITION; TENSOR	The study area is located in the N-NE region of Brazil where Precambrian rocks of the Sao Luis Cratonic Fragment and the Gurupi belt are overlain by Phanerozoic sediments of the Parnaiba and Sao Luis basins, making the assessment of the extents of these geotectonic domains difficult. One of the main objectives of the present study was to elaborate a NNW-SSE-trending, 180-km long magnetotelluric transect, aiming to identify the geotectonic domains of the study area by means of their geoelectric characteristics. The magnetotelluric (MT) technique is a geophysical method that detects the natural variations of the terrestrial electric and magnetic fields so as to investigate the geoelectric characteristics of the subsurface. By means of a MT survey for field data acquisition, calculation of impedance tensors and 2D inversion modeling, the geophysical transect and additionally an interpretive geological model were elaborated for the study area. The combined transverse electric (TE) and transverse magnetic (TM) geophysical model revealed superficial conductive (Parnaiba and Sao Luis basins and sedimentary coverings), resistive (Sao Luis Cratonic Fragment) and very resistive (Gurupi mobile belt) portions up to depths of the order of 15 km. These results attested for correlations between the Sao Luis Craton (South American Plate) and the West African Craton (African Plate), especially regarding the Gurupi Belt (in Brazil) and the Rokelide Belt (in Liberia), which are considered to be the boundaries of a triple junction related to the supercontinent Rodinia taphrogenesis. Besides presenting an unprecedented geophysical investigation along the Sao Luis Cratonic Fragment and the Gurupi Belt, this study promotes the discussion on the correlations between the Brazilian Gurupi and the African Rokelide belts for metallogenetic purposes.	[Uchoa, Elenilton Bezerra] Inst Fed Educ Ciencia & Tecnol, Campus Sobral,Av Dr Guarani 317, BR-62040730 Sobral, CE, Brazil; [Vieira Silva, Nilton Cesar; Gomes Castelo Branco, Raimundo Mariano; da Silva, Fabiano Mota; Martins, Jackson Alves; Maia e Silva, Charles Regis] Univ Fed Ceara, Dept Geol, LGPSR, Campus Pici, BR-60440554 Fortaleza, Ceara, Brazil; [Magini, Christiano] Univ Fed Ceara, Dept Geol, Campus Pici, BR-60440554 Fortaleza, Ceara, Brazil; [Fuck, Reinhardt Adolfo] Univ Brasilia, Inst Geociencias, Campus Univ,Asa Norte, BR-70910900 Brasilia, DF, Brazil	Instituto Federal do Sertao Pernambucano; Universidade Federal do Ceara; Universidade Federal do Ceara; Universidade de Brasilia	Uchoa, EB (autor correspondente), Inst Fed Educ Ciencia & Tecnol, Campus Sobral,Av Dr Guarani 317, BR-62040730 Sobral, CE, Brazil.	elenilton.uchoa@ifce.edu.br; niltoncvs@gmail.com; magini2005@hotmail.com; mariano@ufc.br; reinhardt@unb.br; jackson_geologia@yahoo.com.br; charles_rms@yahoo.com.br		Magini, Christiano/0000-0002-5552-996X	CAPES; INCT	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); INCT	The authors would like to thank CAPES and INCT for financing field data acquisition. They also wish to thank the Geophysics, Prospecting and Remote Sensing Laboratory (LGPSR) - UFC for providing the equipment and support during the data processing stage.	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J	Venancio, IM; Shimizu, MH; Santos, TP; Lessa, DO; Dias, BB; Chiessi, CM; Mulitza, S; Kuhnert, H; Tiedemann, R; Vahlenkamp, M; Bickert, T; Belem, AL; Sampaio, G; Albuquerque, ALS; Nobre, C				Venancio, I. M.; Shimizu, M. H.; Santos, T. P.; Lessa, D. O.; Dias, B. B.; Chiessi, C. M.; Mulitza, S.; Kuhnert, H.; Tiedemann, R.; Vahlenkamp, M.; Bickert, T.; Belem, A. L.; Sampaio, G.; Albuquerque, A. L. S.; Nobre, C.			Ocean-atmosphere interactions over the western South Atlantic during Heinrich stadials	GLOBAL AND PLANETARY CHANGE			English	Article							SEA-SURFACE TEMPERATURE; TROPICAL ATLANTIC; PLANKTONIC-FORAMINIFERA; MERIDIONAL CIRCULATION; SEASONAL VARIABILITY; CONVERGENCE ZONE; CLIMATE-CHANGE; LAST; BRAZIL; PRECIPITATION	Slowdowns of the Atlantic meridional overturning circulation during Heinrich stadials (HS) caused reductions in cross-equatorial heat transport, southward shifts of the Intertropical Convergence Zone and intensification of precipitation over eastern tropical South America. While these changes are well described, the associated spatial sea surface temperature (SST) patterns are still unclear. Here, we analyze proxy data to assess changes in ocean-atmosphere interactions during HS over the western South Atlantic. Our SST proxy records show contrasting patterns between the tropical (warming) and the subtropical (no change) western South Atlantic during HS. We propose that the distinct SST behavior in the subtropics was associated with the cloud cover effect of the South Atlantic Convergence Zone over the upper ocean.	[Venancio, I. M.; Shimizu, M. H.; Sampaio, G.] Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Cachoeira Paulista, Brazil; [Venancio, I. M.; Santos, T. P.; Lessa, D. O.; Dias, B. B.; Albuquerque, A. L. S.] Univ Fed Fluminense, Programa Geociencias Geoquim, Niteroi, RJ, Brazil; [Chiessi, C. M.] Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, Brazil; [Mulitza, S.; Kuhnert, H.; Vahlenkamp, M.; Bickert, T.] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Tiedemann, R.] Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany; [Venancio, I. M.; Belem, A. L.] Univ Fed Fluminense, Programa Posgrad Dinam Oceanos & Terra, Niteroi, RJ, Brazil; [Nobre, C.] Univ Sao Paulo, Inst Adv Studies, Sao Paulo, Brazil	Instituto Nacional de Pesquisas Espaciais (INPE); Universidade Federal Fluminense; Universidade de Sao Paulo; University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Universidade Federal Fluminense; Universidade de Sao Paulo	Venancio, IM (autor correspondente), Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Cachoeira Paulista, Brazil.	igor.venancio@inpe.br	Santos, Thiago P./AAN-6506-2021; Dias, Bruna Borba/AAV-4379-2020; Chiessi, Cristiano Mazur/E-1916-2012; Albuquerque, Ana Luiza S/C-5167-2013; Belem, Andre L/C-8682-2013; Venancio, Igor M/I-5893-2014	Dias, Bruna Borba/0000-0001-5518-2807; Chiessi, Cristiano Mazur/0000-0003-3318-8022; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Belem, Andre L/0000-0002-8865-6180; Venancio, Igor M/0000-0003-3118-4247; Shimizu, Marilia Harumi/0000-0003-0895-555X; Santos, Thiago/0000-0002-9273-3329; Kuhnert, Henning/0000-0001-5242-4495	CAPES [88,887.156152/2017-00, 88,881.161151/2017-01, 564/2015, 88,881.313535/2019-01]; FAPESP [2018/15123-4, 2016/24014-9, 2017-50,085-3]; CAPES/PDSE [99,999.007924/2014-03]; CAPES/FAPERJ [202.134/2015]; CNPq [306,385/2013-9, 99,999.002675/2015-03, 302,607/2016-1, 422,255/2016-5]; Alexander von Humboldt Foundation; CNPq Project RAiN [406,322/2018-0]; CAPES-ASPECTO project [88,887.091731/2014-01]; DFG Research Center/Cluster of Excellence "The Ocean in the Earth System"; Helmholtz Climate Initiative REKLIM	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES/PDSE(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CAPES/FAPERJ(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Alexander von Humboldt Foundation(Alexander von Humboldt Foundation); CNPq Project RAiN; CAPES-ASPECTO project; DFG Research Center/Cluster of Excellence "The Ocean in the Earth System"(German Research Foundation (DFG)); Helmholtz Climate Initiative REKLIM	We thank R. Kowsman (CENPES/Petrobras) and Petrobras Core Repository staff (Macae/Petrobras) for providing sediment core GL1248 employed in this research. We thank S. Pape and M. Kolling for performing Mg/Ca analysis. CAPES financially supported I.M.V. with a scholarship (grant 88,887.156152/2017-00 and 88,881.161151/2017-01). M.H.S. would like to acknowledge FAPESP for the financial support (grant 2016/24014-9 and 2017-50,085-3). T.P.S. acknowledges the financial support from CAPES/PDSE (grant 99,999.007924/2014-03). B.B.D. appreciates the financial support from CAPES/FAPERJ (grant 202.134/2015). A.L.A. is a CNPq senior researcher (grant 306,385/2013-9) and thanks them for financial support (grant 99,999.002675/2015-03). C.M.C. acknowledges the financial support from FAPESP (grant 2018/15123-4), CAPES (grants 564/2015 and 88,881.313535/2019-01), CNPq (grants 302,607/2016-1 and 422,255/2016-5) and the Alexander von Humboldt Foundation. CNPq Project RAiN (grant 406,322/2018-0) supported this study. This study was also supported by CAPES-ASPECTO project (grant 88,887.091731/2014-01). This work was also funded through the DFG Research Center/Cluster of Excellence "The Ocean in the Earth System" and by the Helmholtz Climate Initiative REKLIM. The data reported in this paper will be archived in Pangaea (www.pangaea.de).	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Planet. Change	DEC	2020	195								103352	10.1016/j.gloplacha.2020.103352	http://dx.doi.org/10.1016/j.gloplacha.2020.103352			8	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	OV7BR					2023-06-23	WOS:000592361000005
J	Vianna, SQ; Lafon, JM; Neto, JMM; Silva, DPB; Barros, CED				Vianna, Samia Queiroz; Lafon, Jean Michel; Milhomem Neto, Joao Marinho; Balieiro Silva, Desaix Paulo; Barros, Carlos Eduardo de Mesquita			U-Pb geochronology, Nd-Hf isotopes, and geochemistry of Rhyacian granitoids from the Paleoproterozoic Lourenco domain (Brazil), southeastern Guiana Shield	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Transamazonian granitoids; U-Pb-Hf zircon Geochronology; Rhyacian magmatic arc; Southeastern Guiana Shield; Amazonian craton	WEST-AFRICAN CRATON; ARCHEAN CRUSTAL EVOLUTION; GA BIRIMIAN OROGEN; CONTINENTAL-CRUST; AMAZONIAN CRATON; AMAPA BLOCK; INSIGHTS; GROWTH; ROCKS; DISCRIMINATION	The southern sector of the Paleoproterozoic Lourenco domain in the central-eastern region of the Amapa state, northern Brazil, consists mainly of Rhyacian granite-greenstone terranes with some Archean fragments. It is located at the transition with the Archean Amapa block, a Meso-Neoarchean continental landmass (2.85-2.60 Ga), strongly reworked during the Transamazonian orogeny (2.26-1.95 Ga). Geochemical and petrographic data together with combined zircon U-Pb and Lu-Hf (LA-ICP-MS) as well as whole-rock Sm-Nd (TIMS) dating, establish the chronology and petrogenesis of the granitoids and record the crustal growth and reworking at the transition between the Archean and Paleoproterozoic domains in the southeastern Guiana Shield. Two episodes, dated at similar to 2.18-2.16 Ga and 2.14-2.13 Ga, respectively, include medium-to high-K calc-alkaline and metaluminous to peraluminous rocks of the Flexal and Papa-Vento intrusive suites, emplaced in a magmatic arc environment. A third episode, dated at similar to 2.08 Ga, encompasses mostly peraluminous granites with a medium-to high-K calc-alkaline signature, of the syn-to late-collisional Vila Bom Jesus Suite. The zircon epsilon(Hf) (-3.5 to-4.3) and whole-rock epsilon(Nd) (-2.7 to-4.3) signatures with respective Hf-T-DM(C) (2.9-3.1 Ga) and Nd-TDM (2.6-2.7 Ga) model ages indicate a mixture of Rhyacian juvenile material with a Mesoarchean crustal component for the magma sources of the Flexal and Papa-Vento intrusive suites. The geochemical characteristics, zircon epsilon(Hf) (-6.6 to-12.5) and whole rock epsilon(Nd) (-3.7 to-5.4) signatures, and Hf-T-DM(C) (2.9-3.6 Ga) and Nd-T-DM (2.7-2.9 Ga) model ages, together with the presence of Rhyacian (2.19 Ga) and Mesoarchean (2.82 Ga) inherited zircon crystals in the Vila Bom Jesus Suite, indicate dominant crustal reworking of Rhyacian magmatic arc rocks and Archean rocks from the adjacent Amap ' a Block during the arc-continent collision. The geochemical and isotopic signatures of the magmatic arc granitoids (Flexal and Papa-Vento intrusive suites) may be attributed to the incorporation in the juvenile magmatic sources of Archean continental sediments or hidden crustal fragments from the Amap ' a Block during the subduction processes. Geochemical affinities with continental magmatic arc and subchrondritic Hf-Nd isotopic signatures are consistent with a scenario of a long-lived Mesorhyacian (-2.20-2.13 Ga), Cordilleran-type magmatic arc setting, which evolved to a collisional setting with the amalgamation of the Archean Amapa block and the Rhyacian Lourenco domain during the Neorhyacian (2.11-2.08 Ga).	[Vianna, Samia Queiroz; Lafon, Jean Michel; Milhomem Neto, Joao Marinho] Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, BR-66075110 Belem, PA, Brazil; [Vianna, Samia Queiroz; Lafon, Jean Michel; Milhomem Neto, Joao Marinho] Univ Fed Para, Inst Geociencias, Lab Geol Isotop, BR-66075110 Belem, Para, Brazil; [Balieiro Silva, Desaix Paulo] CPRM Serv Geol Brasil, Companhia Pesquisa Recursos Minerais, Ave Dr Freitas 3645, BR-66095110 Belem, PA, Brazil; [Barros, Carlos Eduardo de Mesquita] Univ Fed Parana, Dept Geol, BR-81531990 Curitiba, PR, Brazil	Universidade Federal do Para; Universidade Federal do Para; Universidade Federal do Parana	Lafon, JM (autor correspondente), Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, BR-66075110 Belem, PA, Brazil.	lafonjm@ufpa.br	Jean Michel, Lafon/AAY-6287-2021	Jean Michel, Lafon/0000-0003-0854-3053	Brazilian National Council for Scientific and Technological Development (CNPq) [133936/2013-9, 307199/2015-0, 309625/2015-7]	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We acknowledge the Brazilian National Council for Scientific and Technological Development (CNPq) for granting a research scholarship to the first author (Process No. 133936/2013-9), J.M. Lafon (Process No. 307199/2015-0) and C.E.M. Barros (Process No. 309625/2015-7). We also thank the Geological Survey of Brazil (CPRM-Belem) for the CL images, and the technical staff of the Isotope Geology Laboratory of the Federal University of Path (Pard-Iso/UFPA) for the U-Pb, Lu-Hf, and Sm-Nd analyses. We are also grateful to the Microanalyses Laboratory of the UFPA for the CL and BSE images acquired in SEM. We thank Dr. Andres Folguera and an anonymous reviewer, who provided helpful comments and recommendations.	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South Am. Earth Sci.	DEC	2020	104								102937	10.1016/j.jsames.2020.102937	http://dx.doi.org/10.1016/j.jsames.2020.102937			19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PH2VB					2023-06-23	WOS:000600276000002
J	Werle, M; Hartmann, LA; Queiroga, GN; Lana, C; Pertille, J; Michelin, CRL; Remus, MVD; Roberts, MP; Castro, MP; Leandro, CG; Savian, JF				Werle, M.; Hartmann, L. A.; Queiroga, G. N.; Lana, C.; Pertille, J.; Michelin, C. R. L.; Remus, M. V. D.; Roberts, M. P.; Castro, M. P.; Leandro, C. G.; Savian, J. F.			Oceanic crust and mantle evidence for the evolution of Tonian-Cryogenian ophiolites, southern Brasiliano Orogen	PRECAMBRIAN RESEARCH			English	Article						Ophiolite; Metasomatic tourmaline; Mantle-derived Cr-spinel; B isotopes; Crustal evolution	DOM FELICIANO BELT; PB-HF ISOTOPES; LA-PLATA CRATON; EDIACARAN PORONGOS GROUP; U-PB; NEOPROTEROZOIC JUVENILE; SPINEL COMPOSITIONS; TECTONIC EVOLUTION; DETRITAL ZIRCONS; TRACE-ELEMENTS	Unravelling the complexity of tonian-cryogenian (950-680 Ma) evolution of ophiolites requires the search for rare mineral systems and their quantification with varied techniques. Ophiolites in the Brasiliano Orogen are widely distributed over 2,000 km along the eastern half of South America. We selected two ophiolites from different geotectonic settings of the Sul-Riograndense Shield, southern Brasiliano Orogen, to delimit the evolution of the oceanic phase of the orogen. The southern portion of the Bossoroca ophiolite is inserted in the Sao Gabriel juvenile terrane and contains rare metasomatic tourmaline in chloritite close to serpentinite and metamorphosed Cr-spinel. The southern Bossoroca ophiolite was intruded by Cerro da Cria and Ramada Granites and the U-Pb-Hf isotopic study of zircon from these rocks constrains the crustal evolution of the Sao Gabriel juvenile terrane. Capane ophiolite has similar age (793-715 Ma) as the Bossomca ophiolite and was inserted in the Porongos fold-thrust belt with preserved Cr-spinel of mantellic composition. Integrated use of Cr-spinel mineral chemistry, B isotopes in tourmaline in the Bossomca ophiolite and zircon U-Pb-Hf isotopes of granites associated with the southern Bossomca ophiolite revealed several steps in the evolution of the ophiolites in the Dom Feliciano Belt. Capane Cr-spinel cores have mantle-derived compositions (Mg# 0.66 - 0.69; Cr# 0.51 - 0.53), tourmaline from the Bossoroca ophiolite is dravite and has delta B-11 = 0 to + 3, and granites crystallization ages are 578 +/- 3.2 and 612 +/- 12 Ma (epsilon Hf-zrn = -10 to -25). Zircon from other dravite occurrences of the Bossoroca ophiolite were previously dated at 920 Ma. We unraveled the main steps in the evolution of ophiolites from the southern Brasiliano Orogen, with emphasis on the Bossomca and Capane ophiolites, during their trajectory from mid-ocean ridge (920 Ma), formation of dravite in oceanic crust, preservation of mantellic cores in Cr-spinel, and intrusion of craton-generated granites at 612-578 Ma.	[Werle, M.; Hartmann, L. A.; Michelin, C. R. L.; Remus, M. V. D.; Leandro, C. G.; Savian, J. F.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Queiroga, G. N.; Lana, C.; Castro, M. P.] Univ Fed Ouro Preto, Dept Geol, Escola Minas, BR-35400000 Ouro Preto, MG, Brazil; [Pertille, J.] Univ Fed Pelotas, Ctr Desenvolvimento Tecnol, Pelotas, RS, Brazil; [Roberts, M. P.] Univ Western Australia, Ctr Microscopy Characterisat & Microanal, Crawley, Australia	Universidade Federal do Rio Grande do Sul; Universidade Federal de Ouro Preto; Universidade Federal de Pelotas; University of Western Australia	Werle, M (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	marianawerle96@gmail.com	Queiroga, Gláucia/AAJ-1823-2021; Hartmann, Léo A/D-7663-2013	Queiroga, Gláucia/0000-0002-1730-0638; Hartmann, Léo A/0000-0001-7863-5071; Werle, Mariana/0000-0001-6083-892X	Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (CNPq) -Brazilian Government; CNPq	Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (CNPq) -Brazilian Government(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Tiara Cerva Alves and Vitor Casagrande Dias participated in field work and sample preparation. This article is a result of the undergraduate senior thesis by Mariana Werle at Universidade Federal do Rio Grande do Sul. She held a scholarship from Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (CNPq) -Brazilian Government, during the investigation. Leo A. Hartmann acknowledges a research scholarship with linked grant, and overall support from CNPq. We also thank the Microscopy and Microanalysis Laboratory (LMic) of Universidade Federal de Ouro Preto, a member of FAPEMIG-supported Microscopy and Microanalysis Network of Minas Gerais, Brazil. We are grateful to Guest Editor Mathias Schannor, Ralf Halama and an anonymous reviewer that made significant contributions to the improvement of the article.	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DEC	2020	351								105979	10.1016/j.precamres.2020.105979	http://dx.doi.org/10.1016/j.precamres.2020.105979			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OZ8DF		Green Published			2023-06-23	WOS:000595149400022
J	Dumont, MV; Santucci, RM; de Andrade, MB; de Oliveira, CEM				Dumont Jr, Marcos V.; Santucci, Rodrigo M.; de Andrade, Marco Brandalise; de Oliveira, Carlos Eduardo Maia			Paleoneurology of Baurusuchus (Crocodyliformes: Baurusuchidae), ontogenetic variation, brain size, and sensorial implications	ANATOMICAL RECORD-ADVANCES IN INTEGRATIVE ANATOMY AND EVOLUTIONARY BIOLOGY			English	Article						Baurusuchus; brain; endocast; nerves; ontogeny; paleoneurology	CAMPINASUCHUS-DINIZI CROCODYLIFORMES; SEMICIRCULAR CANAL SYSTEM; OLFACTORY-BULB; ALLIGATOR-MISSISSIPPIENSIS; PHYLOGENETIC-RELATIONSHIPS; ANATOMY; EVOLUTION; MORPHOLOGY; BEHAVIOR; SKULL	Knowledge on crocodyliform paleoneurology has significantly improved with development of computed tomography. However, studies so far have been able to reconstruct brain endocasts based only on single specimens for each taxon. Here for the first time, we reconstructed brain endocasts for multiple fossil specimens of the same crocodyliform taxon (Baurusuchus), consisting of complete skulls of two medium sized specimens, one large adult, and a late juvenile. In addition, we were able to reconstruct the inner ear anatomy of a fragmentary skull using microtomography. We present estimates of brain size using simple models, based on modern Crocodylia, able to adapt brain to endocranial cavity ratios to expected ontogenetic variation instead of using fixed ratios. We also analyzed relative brain sizes, olfactory ratios, facial sensation, alert head posture, best hearing frequencies, and hearing range. The calculated endocranial volumes showed that they can be greatly altered by taphonomic processes, altering both total and partial endocranial volumes. Reconstructed endocasts are compatible with different degrees of occupation along the endocranial cavity and some of their characteristics might be useful as phylogenetic characters. The relative brain size of Baurusuchus seems to be small in comparison to modern crocodilians. Sensorial abilities were somewhat similar to modern crocodilians and hearing ranges and best mean frequencies remarkably similar to modern taxa, whereas olfactory ratio values are a little higher. Differing from its modern relatives, Baurusuchus hypothesized alert head posture is compatible with a terrestrial habit.	[Dumont Jr, Marcos V.] Fed Inst Brasilia, Campus Planaltina, Brasilia, DF, Brazil; [Dumont Jr, Marcos V.; Santucci, Rodrigo M.] Univ Brasilia, Brasilia, DF, Brazil; [de Andrade, Marco Brandalise] Pontificia Univ Catolica Rio Grande do Sul, PUCRS, Sch Hlth & Life Sci, Porto Alegre, RS, Brazil; [de Oliveira, Carlos Eduardo Maia] Fed Inst Educ Sci & Technol Sao Paulo, Votuporanga, Brazil	Instituto Federal de Brasilia; Universidade de Brasilia; Pontificia Universidade Catolica Do Rio Grande Do Sul; Instituto Federal de Sao Paulo (IFSP)	Dumont, MV (autor correspondente), Fed Inst Brasilia, Campus Planaltina, Brasilia, DF, Brazil.	dumont.marcos@gmail.com	Santucci, Rodrigo M/E-2189-2013	Santucci, Rodrigo/0000-0002-4326-743X	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [401784/2010-0]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, Grant/Award Number: 401784/2010-0	Akaike H., 1998, 2 INT S INFORM THEOR, DOI DOI 10.1007/978-1-4612-1694-0_15; Amorim PH, 2011, INVESALIUS SOFTWARE; Baird I. 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Rec.	OCT	2022	305	10			SI		2670	2694		10.1002/ar.24567	http://dx.doi.org/10.1002/ar.24567		NOV 2020	25	Anatomy & Morphology	Science Citation Index Expanded (SCI-EXPANDED)	Anatomy & Morphology	4H3AN	33211405	Green Published			2023-06-23	WOS:000590358600001
J	Caxito, FD; Hagemann, S; Dias, TG; Barrote, V; Dantas, EL; Chaves, AD; Campello, MS; Campos, FC				Caxito, Fabricio de Andrade; Hagemann, Steffen; Dias, Tatiana Goncalves; Barrote, Vitor; Dantas, Elton Luiz; Chaves, Alexandre de Oliveira; Campello, Marcos Santos; Campos, Filippe Couto			A magmatic barcode for the Sao Francisco Craton: Contextual in-situ SHRIMP U-Pb baddeleyite and zircon dating of the Lavras, Para de Minas and Formiga dyke swarms and implications for Columbia and Rodinia reconstructions	LITHOS			English	Article						Paleocontinental reconstructions; Dyke swarms; U-Pb SHRIMP geochronology; Magmatic barcode; Columbia; Rodinia	NORTH CHINA CRATON; LARGE IGNEOUS PROVINCES; MA MAFIC DYKES; MESOPROTEROZOIC SUPERCONTINENT; TECTONIC CORRELATION; ARCHEAN EVOLUTION; ZIMBABWE CRATON; BREAK-UP; BRAZIL; AGES	Eoarchean to Rhyacian crust is preserved in the Sao Francisco Craton of eastern Brazil.To position this crustal segment in paleocontinental reconstructions, precise, accurate and robust geochronological data are necessary, especially for the diverse regional-scale mafic dyke swarms that crosscut the cratonic basement. This geochronological database can then be used to construct a magmatic barcode and compare it to the barcode of other cratons around the world, in search of similarities that might help to position these pieces in the paleocontinental puzzles. New U-Pb SHRIMP contextual in-situ (thin section) dating of baddeleyite and zircon from six samples of three different dyke swarms in the southern Sao Francisco Craton, in addition to novel lithogeochemical and Nd-Sr isotopic data, allow to pinpoint dyke emplacement at ca. 2.55 Ga (Lavras I swarm; epsilon Nd(t) = -6 to +2; T-DM not calculable), ca. 1.8-1.7 Ga (Para de Minas I and II dyke swarms; epsilon Nd (t) -10 to -5; T-DM = 2.5-3.0 Ga) and at ca. 900 Ma (Formiga dyke swarm; epsilon Nd(t) = -7 to 0; T-Dm = 1.4-23 Ga). The new geochronological data suggest a link between the regional dyke swarms and extensional stresses during the onset of crustal rifting related to the evolution of the Minas, Espinhaco and Macailbas basins, respectively. A barcode comparison shows strong similarity between the Sao Francisco and North China cratons (Lavras-Taipingzhai/Naoyumen swarms, Para de Minas-Taihang/Miyun swarms, Formiga/Pedro Lessa-Sariwon/Dashigou swarms; and possible correlations of the poorly dated 22-2.0 Ga Paraopeba swarm with similar aged swarms in North China), suggesting proximity of those two cratonic blocks, whether they were part or not of Proterozoic paleocontinents such as Columbia and Rodinia. The novel geochronological data support previous interpretations based on paleomagnetic data and provide further refinements of the geochronological record of the southern hemisphere cratonic blocks, allowing for better-tied global correlations. (C) 2020 Elsevier B.V. All rights reserved.	[Caxito, Fabricio de Andrade; Dias, Tatiana Goncalves; Chaves, Alexandre de Oliveira; Campello, Marcos Santos; Campos, Filippe Couto] Univ Fed Minas Gerais CPMTC IGC UFMG, Inst Geociencias, Ctr Pesquisa Prof Manoel Teixeira da Costa, Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Caxito, Fabricio de Andrade; Hagemann, Steffen; Dias, Tatiana Goncalves] Univ Western Australia, Sch Earth & Environm, Ctr Explorat Targeting, 35 Stirling Highway, Crawley, WA 6009, Australia; [Barrote, Vitor] Monash Univ, EAE, Isotopia Lab, Melbourne, Vic 3800, Australia; [Dantas, Elton Luiz] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil	University of Western Australia; Monash University; Universidade de Brasilia	Caxito, FD (autor correspondente), Univ Fed Minas Gerais CPMTC IGC UFMG, Inst Geociencias, Ctr Pesquisa Prof Manoel Teixeira da Costa, Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.	caxito@ufmg.br	Chaves, A. O./F-8832-2014; Caxito, Fabricio A/J-1317-2016; Dantas, Elton Luiz/AAK-8464-2021	Caxito, Fabricio A/0000-0002-0335-3667; Dantas, Elton Luiz/0000-0002-7954-5059; Barrote, Vitor/0000-0001-7442-9748	CNPq (Brazilian Research Council) [201355/2018-3]	CNPq (Brazilian Research Council)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This project was supported by CNPq (Brazilian Research Council) through a post-doctoral research grant (nb. 201355/2018-3) to FAC at the University of Western Australia. FAC is also a Research Fellow of CNPq and thanks for the ongoing support. The U\\Pb analyseswere performed using a SHRIMP II probe at the John DeLaeter Centre of the Curtin University, Perth, Western Australia, enabled by NCRIS via AuScope. We thank NealMcNaughton for guidance and support during the preparation and analysis of the SHRIMPmounts and Allen Kennedy and Hao Gao for support during the analysis, and the UWA/CET staff and alumni, especially Andreas Petterson, Steve Denyszyn and Luis Parra-Avila for the help and discussions. We also thank Cristina Burgos and all of the staff of the Brazilian Geological Survey in Salvador, Brazil, for the tips and help in baddeleyite separation. FAC thanks Joao Orestes Schneider Santos for the support and incentive to conduct a post-doctoral research term in the geochronology facilities of UWA and Curtin University. An earlier version was greatly improved after comments and suggestions by R. Ernst and an anonymous reviewer.	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J	do Vale, TO; de Magalhaes, RS; de Almeida, PF; Matos, JBTL; Chinalia, FA				do Vale, Tatiana Oliveira; de Magalhaes, Roberta Santoro; de Almeida, Paulo Fernando; Torres Lima Matos, Josilene Borges; Chinalia, Fabio Alexandre			The impact of alkyl polyglycoside surfactant on oil yields and its potential effect on the biogenic souring during enhanced oil recovery (EOR)	FUEL			English	Article						Lauryl glucoside; Sulphate-reducing bacteria; Souring; EOR	REDUCING BACTERIA; SULFATE; FOAM; FIELD; EMULSIFICATION; EFFICIENCY; CORROSION; SALINITY; BIOCIDE; NITRATE	The aim of this work is to quantify the effect of using alkyl polyglycoside (APG) surfactant as the main agent for oil recovery and to quantify its potential impact on biogenic souring. Sand-pack column replicates were subjected to two surfactant concentration injection events both in the presence and absence of oil. The activity of sulphate-reducing bacteria (SRB) was tested using the distinct resultant produced waters (PWs) or with surfactant solutions as the additional carbon source. The results suggested that a surfactant concentration of 2% (w/v) can recover 7.7 fold more oil than 0.1% (w/v). The PWs SRB-activity testing identified that surfactant concentrations below 1% (w/v) can significatively increase microbial activity (256 mu gSO(4)/L/h) - which enhances biogenic souring. PWs with higher surfactant concentrations inhibited SRB-activity in the presence of oil. SRB-microbes can utilize surfactant as the sole carbon source (concentrations below 2% w/v). Thus, the mixture of surfactant and oil increased or decreased SRB-activity depending on their concentration (low/high, respectively). Surfactant can not only assist in enhancing biogenic souring but, at a higher concentration, may control it without the need of employing significant amounts of biocide.	[do Vale, Tatiana Oliveira; de Magalhaes, Roberta Santoro; Chinalia, Fabio Alexandre] Univ Fed Bahia, Inst Ciencias Saude ICS, Lab Microbiol & Bioproc Moacyr Durham Moura Costa, Salvador, BA, Brazil; [de Almeida, Paulo Fernando; Torres Lima Matos, Josilene Borges] Univ Fed Bahia, Inst Ciencias Saude ICS, Lab Biotecnol & Ecol Microorganismos LABEM, Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia	Chinalia, FA (autor correspondente), Univ Fed Bahia, Inst Ciencias Saude ICS, Lab Microbiol & Bioproc Moacyr Durham Moura Costa, Salvador, BA, Brazil.	chinalia@hotmail.com	Almeida, Paulo F/HTQ-3119-2023		CAPES	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors thank the support of the funding agency CAPES and the contributions of MSc. Sueli Carvalho dos Santos (in memoriam).	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J	Loureiro, AMS; Paz, SPA; Veiga, MD; Angelica, RS				Loureiro, Alexandre Maximo S.; Paz, Simone Patricia A.; Veiga, Maria do Rosario; Angelica, Romulo Simoes			Assessment of compatibility between historic mortars and lime-METAKAOLIN restoration mortars made from amazon industrial waste	APPLIED CLAY SCIENCE			English	Article						Lime-Metakaolin mortars; Metakaolin; Restoration mortars historic mortars; Compatibility assessment; Contour plots; Mineralogical characterization; XRD; DSC; Brazilian mortars		In the field of conservation and restoration, incompatibility between historic materials and restoration materials should be avoided, and, therefore, a lot of studies are aimed at assessing compatibility in restoration projects. Thus, this work aims to evaluate the mineralogical, physical, and mechanical compatibility between historic mortars and lime-metakaolin (MK) restoration mortars, using MK derived from the industrial waste from the Amazon region. It is worth mentioning that this is the first attempt to use this kind of residue for the restoration of cultural heritage. Historical samples used in this work are from the 18th and 19th centuries, from Belem do Para (northern Brazil). The composition of the restoration mortars was determined using a complete factorial duplicated in 22 with three central points. The evaluation of mineralogical compatibility was performed by XRD and DSC-TG, and the evaluation of physical and mechanical compatibility occurred by determining the compressive strength, open porosity, capillarity coefficient, and drying rate. As expected, lime mortars were the most compatible with historic mortars in terms of mineralogical composition. The mineralogy of lime-MK mortars resulted in the immediate formation of hydraulic products in the first days of curing, indicating rapid hardening and high initial mechanical strength. In general, the physical and mechanical properties of restoration mortars were compatible with historic mortars, which was influenced by the adopted features and mineralogy. The results indicate restoration mortars with lower mechanical resistance and greater open porosity, capillarity coefficient, and drying rate. This indicates that some of the restoration materials would not cause excessive stress on the old structure, favor gas exchange, and reduce the prolonged presence of moisture. The results also indicate that restoration mortars with MK are probably more resistant to weathering than restoration mortars without this additive, especially the prolonged presence of water, a common situation in the humid tropics. Thus, the conclusions of this work can be useful both for the field of conservation and restoration and for the field of applied clay science, as it directs towards the sustainable use of clays from industrial wastes as an additive in restoration mortars.	[Loureiro, Alexandre Maximo S.; Paz, Simone Patricia A.; Angelica, Romulo Simoes] Fed Univ Para, Inst Geosci, Mineral Characterizat Lab LCM, Belem, Para, Brazil; [Loureiro, Alexandre Maximo S.] Fed Univ Para UFPA, Inst Technol ITEC, Lab Conservat Restorat & Rehabil LACORE, Belem, Para, Brazil; [Veiga, Maria do Rosario] Natl Lab Civil Engn LNEC, Dept Bldg, Lisbon, Portugal	Universidade Federal do Para; Universidade Federal do Para; National Civil Engineering Laboratory	Loureiro, AMS (autor correspondente), Univ Fed Para, Lab Caracterizacao Mineral, Av Augusto Correa 1, BR-66075110 Belem, PA, Brazil.	loureiro1@ufpa.br	Angelica, Romulo/G-6245-2010; Veiga, Rosário/A-7100-2013	Angelica, Romulo/0000-0002-3026-5523; Veiga, Rosário/0000-0002-7135-8603; Loureiro, Alexandre/0000-0003-3341-2653	Brazilian Federal Agency for the Support and Evaluation of Graduate Education (Portuguese acronym: CAPES); National Council for Scientific and Technological Development (Portuguese acronym: CNPq) [305.392/2014-0]; Office of the Dean for Research and Graduate Studies (Federal University of Para; UFPA)	Brazilian Federal Agency for the Support and Evaluation of Graduate Education (Portuguese acronym: CAPES); National Council for Scientific and Technological Development (Portuguese acronym: CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Office of the Dean for Research and Graduate Studies (Federal University of Para; UFPA)	The authors thank the following Brazilian funding agencies for granting a doctoral scholarship to the first author: the Brazilian Federal Agency for the Support and Evaluation of Graduate Education (Portuguese acronym: CAPES) and the National Council for Scientific and Technological Development (Portuguese acronym: CNPq), for a grant to the last author (305.392/2014-0). We thank the following laboratories for technical support during the performance of the study, a) Mineral Characterization Laboratory (Portuguese acronym: LCM); b) Laboratory of Conservation, Restoration and Rehabilitation (Portuguese acronym: LACORE); c) Department of Buildings of the National Laboratory for Civil Engineering (Portuguese acronym: LNEC) and d) Sedimentology Laboratory (Portuguese acronym: LABSED); and especially the technicians Aldemir Sotero (LCM), Everaldo Cunha (LABSED) and Anabela Manteigas and Dora Santos (LNEC) and Professor Rose Norat and Professor Thais Sanjad (LACORE). We thank the Office of the Dean for Research and Graduate Studies (Federal University of Para; UFPA) for funding the translation of the article through the Qualified Publication Support Program (PAPQ; 2019 PAPQ NOTICE).	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Clay Sci.	NOV 15	2020	198								105843	10.1016/j.clay.2020.105843	http://dx.doi.org/10.1016/j.clay.2020.105843			16	Chemistry, Physical; Materials Science, Multidisciplinary; Mineralogy	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Materials Science; Mineralogy	PE1IW					2023-06-23	WOS:000598125900011
J	Pasqualon, NG; Savian, JF; Lima, EF; Luz, FR; Moncinhatto, TR; Trindade, RIF				Pasqualon, Natalia G.; Savian, Jairo F.; Lima, Evandro F.; Luz, Fernando R.; Moncinhatto, Thiago R.; Trindade, Ricardo I. F.			Emplacement dynamics of alkaline volcanic and subvolcanic rocks in Trindade Island, Brazil	JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH			English	Article						Magnetic fabric; Magnetic mineralogy; AMS; AARM; Magma flow	MAGNETIC PARTICLE-SYSTEMS; TRISTAN-DA-CUNHA; SOUTH-ATLANTIC; MANTLE PLUME; MAGMA FLOW; INTERNAL STRUCTURE; AMS MEASUREMENTS; TOOTHPASTE LAVA; DIKE SWARM; SUSCEPTIBILITY	Anisotropy of magnetic susceptibility (AMS) and anhysteretic remanent magnetization (AARM) are tools to characterize flow structures and emplacement conditions of volcanic and subvolcanic bodies, directly related to magnetic fabrics. An AMS and AARM study was performed to contribute to the understanding of the processes involved in magma transportation and emplacement dynamics of the volcanic and subvolcanic rocks of Trindade Island, and their implications on the evolution of the volcanic field. Trindade Island is located in the South Atlantic Ocean, at 1260 km to the east of the Espirito Santo state coast in Brazil. The island is composed of lava flows, intrusions and pyroclastic rocks of alkaline, SiO2 undersaturated nature, forming five geological units aged 3.9-0.25 Ma. During fieldwork, 17 sampling sites were established in the phonolitic necks and melanephelinitic dyke of the oldest unit (Trindade Complex) and in the melanephelinitic 'a'a flows of the youngest units (Morro Vermelho, Valado and ParedAo Volcano formations), totaling 160 oriented mini-cores and 504 rock specimens. The analysis of petrofabric, magnetic mineralogy, AMS and AARM diagrams suggests the dominance of a low-coercivity magnetic mineral phase, represented by low-Ti titanomagnetite/titanomagnetite in the phonolitic necks and melanephelinitic dyke. These bodies display normal fabric (multi-domain and vortex grains) and sub-vertical/high-angle magnetic foliation and lineation. The melanephelinitic 'a'a lavas present at least two magnetic mineral phases of high and low-coercivity (titanomagnetite, maghemite and hematite), with normal, intermediate or inverse fabrics (vortex or single domain grains). Mean magnetic foliation and lineation suggest that lavas flowed to NE. Data interpretation indicates that the subvolcanic bodies were emplaced vertically during the initial stages of island formation, followed by lavas flowing to the northeast. The orientation of the dyke and lava feeders along NNW-SSE leads to the conclusion that the tensional field during the evolution of volcanism remained the same, with NW direction for sigma during approximately 4 My. This study is an example for the understanding of physical processes in the evolution of world oceanic islands. (C) 2020 Elsevier B.V. All rights reserved.	[Pasqualon, Natalia G.; Savian, Jairo F.; Lima, Evandro F.; Luz, Fernando R.] Univ Fed Rio Grande do Sul, Inst Geociencias, BR-91501970 Porto Alegre, RS, Brazil; [Moncinhatto, Thiago R.; Trindade, Ricardo I. F.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, BR-05509090 Sao Paulo, SP, Brazil	Universidade Federal do Rio Grande do Sul; Universidade de Sao Paulo	Pasqualon, NG (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, BR-91501970 Porto Alegre, RS, Brazil.	nati_pasqualon@yahoo.com.br	Trindade, Ricardo IF/A-8146-2008	Trindade, Ricardo IF/0000-0001-9848-9550; Gauer Pasqualon, Natalia/0000-0001-7390-7621	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [442812/2015-9]; CNPq [141141/2020-4, 304022/2018-7, 302125/2016-7]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors acknowledge financial support from Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) through grant no 442812/2015-9. Natalia G. Pasqualon held a CNPq scholarship no141141/2020-4 during the studies and Jairo F. Savian and Evandro F. de Lima had financial support from CNPq through grants no 304022/2018-7 and no 302125/2016-7. We thank the Brazilian Navy (Marinha do Brasil) for the logistics during field activities, and the suggestions and English revision by Leo Afraneo Hartmann. We also acknowledge the expertise of the anonymous reviewers and CraigMagee for carefully revising and providing many meaningful suggestions that improved considerably the article.	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Volcanol. Geotherm. Res.	NOV 15	2020	406								107078	10.1016/j.jvolgeores.2020.107078	http://dx.doi.org/10.1016/j.jvolgeores.2020.107078			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OV7QU					2023-06-23	WOS:000592400300001
J	Tonha, MS; Garnier, J; Araujo, DF; Cunha, BCA; Machado, W; Dantas, E; Araujo, R; Kutter, VT; Bonnet, MP; Seyler, P				Tonha, Myller S.; Garnier, Jeremie; Araujo, Daniel F.; Cunha, Bruno C. A.; Machado, Wilson; Dantas, Elton; Araujo, Rafael; Kutter, Vinicius T.; Bonnet, Marie-Paule; Seyler, Patrick			Behavior of metallurgical zinc contamination in coastal environments: A survey of Zn from electroplating wastes and partitioning in sediments	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Zinc isotopes; Sequential extraction; Zinc speciation; Bioavailability; Metallurgical wastes; Coastal environment	STABLE-ISOTOPE FRACTIONATION; SEQUENTIAL EXTRACTION PROCEDURE; SEPETIBA BAY SE; ANTHROPOGENIC SOURCES; MANGROVE SEDIMENTS; TRACE-METALS; CU ISOTOPES; CD; PB; BRAZIL	The contamination of coastal environments by metallurgical wastes involves multiple biogeochemical processes; accordingly, understanding metal behavior and risk evaluation of contaminated areas, such as Sepetiba Bay (Rio de Janeiro. Brazil), remains challenging. This study coupled Zn isotopic analyses with sequential extractions (BCR) to investigate the mechanisms of Zn transfer between legacy electroplating waste and the main environments in Sepetiba Bay. This metallurgical waste showed a light bulk isotopic signature (delta(66/64) Znbulk(JMC )= +0.30 +/- 0.01 parts per thousand 2 s, n = 3) that was not distinct from the lithogenic geochemical baseline, but was different from signature of mangrove sediment considered as anthropogenic end member (delta(66/64) Zn-JMC = +0.86 +/- 0.15 parts per thousand) in a previous isotopic study in this area. Zn isotopic compositions of sediment samples (ranging from +0.20 to +0.98 parts per thousand) throughout the bay fit a mixing model involving multiple sources, consistent with previous studies. In the metallurgic zone, the exchangeable/carbonate fraction (ZnF1) exhibited high Zn concentrations (ZnF1 9840 mu g g(-1)) and a heavy isotopic composition (delta(66/64) ZnF1(JMC) = +1.10 +/- 0.01 parts per thousand). This finding showed that, in some cases, the bulk isotopic signature of waste is not the most relevant criterion for evaluating trace metal dispersion in the environment. Indeed, based on the BCR. it was observed that part of the anthropogenic metallurgical Zn was redistributed from the exchangeable/carbonate fraction in the waste to the surrounding mangrove sediment. Then, this contaminated sediment with heavy delta(66/64) Zn values was exported to other coastal environments. In Sepetiba Bay, contaminated sediments revealed a large concentration of ZnF1 fraction (up to 400 mu g g(-1)) with a heavy Zn isotopic signature. This signature also matched the Zn isotopic signature of oysters in Sepetiba Bay reported by other studies; hence, measurement of the isotopic exchangeable/carbonate fraction has important implications for tracing the transfer of anthropogenic Zn to biota. (C) 2020 Elsevier B.V. All rights reserved.	[Tonha, Myller S.; Garnier, Jeremie; Dantas, Elton; Araujo, Rafael] Univ Brasilia, Inst Geociencias, Campus Darcy Ribeiro 12, Brasilia, DF, Brazil; [Garnier, Jeremie; Bonnet, Marie-Paule; Seyler, Patrick] Univ Brasilia, Lab Mixte Int Observ Changements Environm LMI OCE, Inst Rech Dev, Campus Darcy Ribeiro, Brasilia, DF, Brazil; [Araujo, Daniel F.] Ifremer, Lab Biogeochim Contaminants Metall, Ctr Atlantique, F-44311 Nantes 3, France; [Cunha, Bruno C. A.] Univ Sao Paulo, Inst Geosci, Rua Lago 562, BR-05508080 Sao Paulo, Brazil; [Machado, Wilson] Univ Fed Fluminense, Dept Geoquim, Campus Valonguinho, Niteroi, RJ, Brazil; [Kutter, Vinicius T.] Univ Fed Fluminense, Programa Pos Grad Geociencias Geoquim, Outeiro Sao Joao Batista S-N Ctr, BR-24020141 Niteroi, RJ, Brazil; [Seyler, Patrick] Univ Montpellier, Inst Rech Dev, Unite Mixte Rech Hydrosci Montpellier 5569, Montpellier, France	Universidade de Brasilia; Institut de Recherche pour le Developpement (IRD); Universidade de Brasilia; Ifremer; Universidade de Sao Paulo; Universidade Federal Fluminense; Universidade Federal Fluminense; Institut de Recherche pour le Developpement (IRD); Universite de Montpellier	Garnier, J (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Darcy Ribeiro 12, Brasilia, DF, Brazil.	garnier@unb.br	Machado, Wilson/P-8047-2019; Tonha, Myller/G-4838-2018; Bonnet, Marie-Paule/J-6888-2016; garnier, jeremie/AAK-8470-2021; Dantas, Elton Luiz/AAK-8464-2021	Machado, Wilson/0000-0003-3117-8584; Tonha, Myller/0000-0002-6111-965X; Bonnet, Marie-Paule/0000-0002-3950-4041; garnier, jeremie/0000-0001-9571-7933; Dantas, Elton Luiz/0000-0002-7954-5059	CAPES; CNPq [400029/2015-4, 420697/2018-7, 302722/2018-1]; LMI-OCE	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); LMI-OCE	The authors acknowledge the students and researchers who participated in the field investigations. The authors acknowledge the staff from the Geosciences Institute of UnB, and Hydrosciences Montpellier, particularly Dr. Remi Freydier, Barbara Alcantara Lima and the PPGG and PPGGAG. The authors acknowledge the Little Chicks and the Casa for the logistics and their assistance in the field. Myller acknowledges the CAPES and the CNPq for support during his Ph.D. Analytical work in Brazil and France was partly funded by the LMI-OCE and CNPq 400029/2015-4, 420697/2018-7. Jeremie Garnier was supported by CNPq grant 302722/2018-1.	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J	Castellan, P; Viegas, G; Faleiros, FM				Castellan, Paulo; Viegas, Gustavo; Faleiros, Frederico M.			Brittle-ductile fabrics and P-T conditions of deformation in the East Pernambuco shear zone (Borborema Province, NE Brazil)	JOURNAL OF THE GEOLOGICAL SOCIETY			English	Article							MINERAL EQUILIBRIA CALCULATIONS; GRAIN-SIZE REDUCTION; MAGMA EMPLACEMENT; NORTHEAST BRAZIL; STRAIN LOCALIZATION; TECTONIC EVOLUTION; QUARTZ; SYSTEM; CONSTRAINTS; FELDSPAR	Fabrics of the East Pernambuco shear zone (EPSZ) were studied via microstructural analysis, mineral chemistry and isochemical phase diagram modelling to constrain the pressure and temperature conditions of deformation during shearing. Granitic mylonites show fractured feldspar porphyroclasts embedded in a fine-grained, recrystallized quartzo-feldspathic matrix. These mylonites grade laterally into banded ultramylonites characterized by stretched feldspar clasts alternated with recrystallized quartz bands. Fractures in these ultramylonites are filled by phyllosilicates. The mineral chemistry of the feldspars points to systematic changes between porphyroclasts, grains within fractures and fine-grained mixtures. Quartz crystallographic fabrics in the mylonites suggest activation of prism slip, while the ultramylonites show the activation of both rhomb and basal slip systems. Thermodynamic modelling suggests that the mylonites were formed at 4.75 +/- 0.25 kbar and 526 +/- 9 degrees C, while the ultramylonites yield conditions of 5.9 +/- 1 kbar and 437 +/- 17 degrees C. These observations suggest that the EPSZ records a heterogeneous path of strain accommodation, marked by decreasing temperature from its western sector to its eastern termination. The differences in metamorphic conditions are consistent with a transitional, brittle-ductile strain regime. Such characteristics indicate that the EPSZ is a Neoproterozoic shear belt nucleated and heterogeneously exhumed at the brittle-ductile transition, possibly in an intracontinental setting. Supplementary Material: EPMA analysis of feldspars in Caruaru and Gravata domains and T-X(O-2) pseudosections are available at	[Castellan, Paulo; Viegas, Gustavo] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Faleiros, Frederico M.] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil	Universidade de Brasilia; Universidade de Sao Paulo	Castellan, P (autor correspondente), Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil.	paulo.castellan@gmail.com	Faleiros, Frederico Meira/F-6138-2010; Viegas, Gustavo/AAK-8437-2021	Faleiros, Frederico Meira/0000-0003-2199-8116; Viegas, Gustavo/0000-0002-9945-6256; Medeiros, Paulo/0000-0003-0657-6716	Fundacao de Apoio a Pesquisa do Distrito Federal [0193.001510/2017]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo [14/01114-2]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior [88882.347155/2019-01]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [307732/2019-3]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [14/01114-2] Funding Source: FAPESP	Fundacao de Apoio a Pesquisa do Distrito Federal(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	This work was funded by the Fundacao de Apoio a Pesquisa do Distrito Federal (0193.001510/2017), Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (14/01114-2), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (88882.347155/2019-01) and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (307732/2019-3).	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Geol. Soc.	JAN	2021	178	1							jgs2020-109	10.1144/jgs2020-109	http://dx.doi.org/10.1144/jgs2020-109		NOV 2020	19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PZ9OJ					2023-06-23	WOS:000592092600001
J	Sena, MVD; Bantim, RAM; Saraiva, AAF; Sayao, JM; Oliveira, GR				Sena, Mariana Valeria de Araujo; Bantim, Renan Alfredo Machado; Saraiva, Antonio Alamo Feitosa; Sayao, Juliana Manso; Oliveira, Gustavo Ribeiro			Osteohistology and microanatomy of a new specimen of Cearachelys placidoi (Testudines: Pleurodira) a side-necked turtle from the lower Cretaceous of Brazil	ANATOMICAL RECORD-ADVANCES IN INTEGRATIVE ANATOMY AND EVOLUTIONARY BIOLOGY			English	Article						Araripe Basin; bothremydidae; Gondwana; pleurodire; shell histology	SHELL BONE-HISTOLOGY; BOTHREMYDIDAE; MORPHOLOGY	Pelomedusoides had a recognised diverse Early Cretaceous fauna of turtles in Northeast Brazil. Within them, the bothremydid Cearachelys placidoi has a relatively abundant record. This diversity contrasts with the scarcity of osteohistological studies in this group. The relatively well-preserved shell of C. placidoi (UFRPE 5600), from the Aptian age of Araripe Basin, is studied here for the purpose of filling this gap. We performed the osteohistological description of the plastron of a new specimen of C. placidoi. Also, to conduct a comparative study, we carried out histological sections in bones of the recent chelid Phrynops sp. Our histological findings indicate similarities between the histological pattern of freshwater turtles and the coastal marine C. placidoi. Moreover, osteohistological features imply metaplastic incorporation of dermal interwoven structural fiber bundles. Lastly, the xiphiplastron of C. placidoi shows an increase of bone compactness over its craniocaudal axis. This microanatomical feature is exclusive to Cearachelys so far.	[Sena, Mariana Valeria de Araujo] Univ Fed Pernambuco, Dept Geol, Programa Posgrad Geociencias PPGEOC, Ave Prof Moraes Rego 1235, BR-50670901 Recife, PE, Brazil; [Sena, Mariana Valeria de Araujo] Ctr Univ Vitoria Santo Antao, Loteamento Sao Vicente Ferrer 71, BR-55610050 Vitoria De Santo Antao, PE, Brazil; [Bantim, Renan Alfredo Machado; Saraiva, Antonio Alamo Feitosa] Univ Reg Cariri, Lab Paleontol URCA, Rua Carolino Sucupira S-N, BR-63105000 Crato, Ceara, Brazil; [Sayao, Juliana Manso] Univ Fed Rio de Janeiro, Museu Nacl, Lab Paleobiol & Paleogeog Antart, Quinta Da Boa Vista S-N, BR-20940040 Rio De Janeiro, RJ, Brazil; [Oliveira, Gustavo Ribeiro] Univ Fed Rural Pernambuco, Dept Biol, Lab Paleontol & Sistemat, Rua Dom Manoel Medeiros S-N, BR-52171900 Recife, PE, Brazil	Universidade Federal de Pernambuco; Universidade Regional do Cariri; Universidade Federal do Rio de Janeiro; Universidade Federal Rural de Pernambuco (UFRPE)	Sena, MVD (autor correspondente), Univ Fed Pernambuco, Dept Geol, Programa Posgrad Geociencias PPGEOC, Ave Prof Moraes Rego 1235, BR-50670901 Recife, PE, Brazil.	mari.araujo.sena@gmail.com	Oliveira, Gustavo R/F-7432-2012; Sena, Mariana V A/K-9347-2018; Sena, Mariana/AAC-4283-2020; Oliveira, Gustavo/IQW-7983-2023; Bantim, Renan/J-4076-2014; Saraiva, António/HPD-3031-2023; Saraiva, Antonio/K-6211-2015	Oliveira, Gustavo R/0000-0002-9871-1235; Sena, Mariana V A/0000-0003-4708-999X; Sena, Mariana/0000-0003-4708-999X; Sayao, juliana/0000-0002-3619-0323; Saraiva, Antonio/0000-0003-0127-8912	Fundac~ao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico [BP3-013900202]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico	Fundac~ao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Fundac~ao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico, Grant/Award Number: BP3-013900202; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico	Arai M, 2020, CRETACEOUS RES, V116, DOI 10.1016/j.cretres.2020.104610; Chinsamy A., 1992, Palaeontologia Africana, V29, P39; Danilov IG, 2018, PALEONTOL J+, V52, P188, DOI 10.1134/S0031030118010070; de Broin France de Lapparent, 2000, Palaeontologia Africana, V36, P43; Enlow D. 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Rec.	JUN	2021	304	6			SI		1294	1304		10.1002/ar.24556	http://dx.doi.org/10.1002/ar.24556		NOV 2020	11	Anatomy & Morphology	Science Citation Index Expanded (SCI-EXPANDED)	Anatomy & Morphology	SJ3XN	33103362	Bronze			2023-06-23	WOS:000587029600001
J	Ferreira, ACD; Dantas, EL; Fuck, RA				Ferreira, Alanielson C. D.; Dantas, Elton L.; Fuck, Reinhardt A.			The previously missing c. 2.9 Ga high-K continental crust in West Gondwana revealed in Northeast Brazil	TERRA NOVA			English	Article						2.9-Ga magmatism; Archean crust; West Gondwana	SAO FRANCISCO CRATON; BORBOREMA PROVINCE; NE BRAZIL; ARCHEAN GRANITOIDS; CAMPESTRE MASSIF; PLATE-TECTONICS; U-PB; GROWTH; EVOLUTION; ORIGIN	2.9 Ga is an uncommon magmatic age in Archean evolution worldwide, especially in West Gondwana. We identified so far unknown 2.97-2.92 Ga high-K calc-alkaline magmatism in the Borborema Province, northeast Brazil. It appears to indicate that the transition to high-K magmas occurred before c. 2.7 Ga in Earth's history. The 2.9 Ga protoliths were reworked and progressively changed composition to 2.65 Ga and 2.25 Ga higher-K granites in early magmatic arcs. Therefore, despite several reworking events from the Archean to Proterozoic times, these rare relicts of K-rich magmatism indicate that reworking of felsic components was significant for the growth and differentiation of continental crust from c. 2.9 Ga onwards in West Gondwana.	[Ferreira, Alanielson C. D.; Dantas, Elton L.; Fuck, Reinhardt A.] Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia	Ferreira, ACD (autor correspondente), Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil.	alanielson.ferreira@ufrgs.br	Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059; Fuck, Reinhardt/0000-0003-1396-125X; Ferreira, Alanielson/0000-0001-8054-0047	INCT Estudos Tectonicos [CAPES/CNPq-465613/2014-4, FAPDF-193.001.263/2017]; CNPq; CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES) [001]	INCT Estudos Tectonicos; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study is part of the first author's PhD thesis developed at the Institute of Geosciences, Universidade de Brasilia. The authors acknowledge support from INCT Estudos Tectonicos (CAPES/CNPq-465613/2014-4, FAPDF-193.001.263/2017). ELD and RAF acknowledge CNPq research fellowships. This study was financed in part by the CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES)-Finance Code 001.	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Nova	APR	2021	33	2					184	194		10.1111/ter.12504	http://dx.doi.org/10.1111/ter.12504		NOV 2020	11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QV3OB					2023-06-23	WOS:000585369900001
J	Avila, CF; Archanjo, CJ; Hollanda, MHBM; de Macedo, AA; Lemos-Santos, DD				Avila, Carlos F.; Archanjo, Carlos J.; Hollanda, Maria Helena B. M.; de Macedo Filho, Antomat A.; Lemos-Santos, Daniel do, V			Shear zone cooling and fabrics of synkinematic plutons evidence timing and rates of orogenic exhumation in the northwest Borborema Province (NE Brazil)	PRECAMBRIAN RESEARCH			English	Article						Magnetic fabrics; Ar/Ar thermochronology; Multi-stage exhumation; Shear zone cooling; Borborema Province	U-PB; ZIRCON; ROCKS; GEOCHRONOLOGY; 40AR/39AR; GRANITE; CEARA; ALPS; AGE; DEFORMATION	Ediacaran convergence and collision resulting from amalgamation of West Gondwana are documented in the Borborema Province by high-pressure rock units, contractional tectonics and anatexis. Thermochronological (zircon U-Pb and amphibole-biotite Ar-Ar) and structural (Anisotropy of Magnetic Susceptibility) constraints from shear zone-bounding synkinematic plutons in the Ceara Central Domain provide timing and rates of their subsequent post-collisional evolution. Our results show that: (i) U-Pb ages of zircons of 585-571 Ma record magma crystallisation and a protracted history of assembly for the Taua batholith, synchronous with deformation in the bounding transcurrent shear zone junction; (ii) AMS fabrics document chamber construction processes and the effect of long-lived strongly localized shear zone deformation; and (iii) 40Ar/39Ar plateau ages of amphibole and biotite from the synkinematic plutons at 577-562 and 559-554 Ma, respectively, yield cooling rates of 20-40 degrees C/Myr characterising differential cooling paths. Integration of various thermochronometers available for the strike-slip shear zones and the internal high-pressure domain reveals a fast isothermal decompression (long-term unroofing rate of 1.9-5.8 mm/yr), which exhumed high-pressure rock units. Subsequently, fast nearly isobaric cooling (20-40 degrees C/Myr) occurred in the whole terrane until 590 Ma, with temperatures falling below 320 degrees C. Due to enhanced magmatic activity during the deformation, the shear zones experienced much higher temperatures at that same depth at 584 Ma followed by fast cooling (20-40 degrees C/Myr) to temperatures below 320 degrees C at 560 Ma. These final cooling episodes were accompanied by slow unroofing at an estimated rate of 0.3-0.9 mm/yr, sufficient to bring these rocks close to the surface at 540 Ma, when molassic, pull-apart basins were formed.	[Avila, Carlos F.; Archanjo, Carlos J.; Hollanda, Maria Helena B. M.; de Macedo Filho, Antomat A.; Lemos-Santos, Daniel do, V] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, SP, Brazil	Universidade de Sao Paulo	Avila, CF (autor correspondente), Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, SP, Brazil.	carlosavila@usp.br	Macêdo Filho, Antomat Avelino de/AFR-2728-2022; Archanjo, Carlos/E-9062-2012	Macêdo Filho, Antomat Avelino de/0000-0003-3150-7560; Archanjo, Carlos/0000-0003-4618-7790; do Valle Lemos Santos, Daniel/0000-0001-7640-5192; Avila, Carlos Fernando/0000-0002-2389-8736; Hollanda, Maria Helena Bezerra Maia/0000-0003-2231-7917	Sao Paulo Science Foundation (FAPESP) [2016/22226-9, 2017/21440-0, 2019/10167-6]; CNPq [305084/17-8, 8303201/19-3]; CAPES	Sao Paulo Science Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	C. Avila and C. Archanjo thank Sao Paulo Science Foundation (FAPESP) for financial sponsorship (grants 2016/22226-9, 2017/21440-0 and 2019/10167-6). C. Archanjo and M. H. B. M. Hollanda are also grateful to CNPq (305084/17-8 and 8303201/19-3). All authors thank CAPES for supporting this research. U-Pb SHRIMP, Ar-Ar and Anisotropy of Magnetic Susceptibility (AMS) analyses data used in this study are available in further detail in the Supplementary material. Airborne geophysical survey data that aided in geological mapping are available in the Brazilian Geological Survey database (http://geosgb.cprm.gov.br/). Maps for this study were created in QGIS (QGIS.org, 2020. QGIS Geographic Information System. Open Source Geospatial Foundation Project. http://qgis.org). We would like to thank Wilson Teixeira and Elson Oliveira for careful handling of the manuscript. Alain Vauchez and Sergio Neves are acknowledged for thorough and constructive comments that considerably helped us improve this manuscript.	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J	Cabral, RL; Ferreira, TO; Nobrega, GN; Barcellos, D; Roiloa, SR; Zandavalli, RB; Otero, XL				Cabral, Raiana L.; Ferreira, Tiago O.; Nobrega, Gabriel N.; Barcellos, Diego; Roiloa, Sergio R.; Zandavalli, Roberta B.; Otero, Xose L.			How Do Plants and Climatic Conditions Control Soil Properties in Hypersaline Tidal Flats?	APPLIED SCIENCES-BASEL			English	Article						rhizosphere; seasonal changes; coastal wetlands; soil salinity; apicun	GREENHOUSE-GAS EMISSIONS; PHYSIOLOGICAL INTEGRATION; FRAGARIA-VESCA; ECOSYSTEM; NITROGEN; AMMONIUM; GROWTH; DENITRIFICATION; COMPETITION; TOLERANCE	Hypersaline tidal flats (HTF) are ecotones associated with mangrove ecosystems in arid and semiarid coasts. They are predominantly vegetated by halophytes which are related to environmental stabilization and fauna protection. Some plants thrive in HTF by modifying soil biogeochemical conditions at their rhizospheres, expanding across barren soils. Thus, we aimed to study rhizospheric and the adjacent bulk soils of the three most abundant plant species in HTF under a seasonal semiarid climate of northeastern Brazil. We analyzed both rhizospheric and bulk soils of vegetation patches in wet and dry seasons. We found that HTF soils are a heterogeneous system highly influenced by water availability and plant activity. The soils were mostly sandy textured, containing low C and N contents, and hypersaline conditions. Comparing bulk and rhizospheric soils, we concluded that plants changed their own rhizosphere by creating nutrient pools to improve survival under saline conditions. Seasonal changes also affected soil biogeochemical processes in HTF, mainly the bulk soils by changing water availability. Understanding rhizospheric changes by halophytes, their expansion over barren soils, and the amelioration of soil physicochemical conditions, are fundamental to provide support for preservation and management of coastal ecosystems, including HTF.	[Cabral, Raiana L.; Zandavalli, Roberta B.] Univ Fed Ceara, Dept Biol, UFC, Programa Posgrad Ecol & Recursos Nat, Campus Pici, BR-60440900 Fortaleza, Ceara, Brazil; [Ferreira, Tiago O.; Barcellos, Diego] Univ Sao Paulo, Coll Agr Luiz de Queiroz, Dept Soil Sci, ESALQ USP, Av Padua Dias 11, BR-13418 Piracicaba, SP, Brazil; [Nobrega, Gabriel N.] Fed Fluminense Univ, Dept Geochem, Grad Program Geosci Geochem, Campus Valonguinh, BR-24020 Niteroi, RJ, Brazil; [Roiloa, Sergio R.] Univ A Coruna, Fac Ciencias, Dept Biol, La Coruna 15008, Spain; [Otero, Xose L.] Univ Santiago de Compostela, Fac Biol, CRESTUS Inst, Dept Edafol & Quim Agr, Rua Lope G Marzoa S-N,Campus Sur, Santiago De Compostela 15782, Spain	Universidade Federal do Ceara; Universidade de Sao Paulo; Universidade Federal Fluminense; Universidade da Coruna; Universidade de Santiago de Compostela	Ferreira, TO (autor correspondente), Univ Sao Paulo, Coll Agr Luiz de Queiroz, Dept Soil Sci, ESALQ USP, Av Padua Dias 11, BR-13418 Piracicaba, SP, Brazil.; Otero, XL (autor correspondente), Univ Santiago de Compostela, Fac Biol, CRESTUS Inst, Dept Edafol & Quim Agr, Rua Lope G Marzoa S-N,Campus Sur, Santiago De Compostela 15782, Spain.	raianalira@amaniinstitute.org; toferreira@usp.br; gabrielnn@id.uff.br; diego.barcellos@usp.br; sergio.roiloa@udc.es; zandavalli@ufc.br; xl.otero@usc.es	Ferreira, Tiago Osório/D-3340-2015; Barcellos, Diego/AAI-5073-2020; Nóbrega, Gabriel Nuto/AAQ-4189-2020	Ferreira, Tiago Osório/0000-0002-4088-7457; Barcellos, Diego/0000-0002-4198-2843; Nóbrega, Gabriel Nuto/0000-0001-7008-4201	CAPES; National Council for Scientific and Technology Development (CNPq) [305996/2018-5, 409593/2018-4]; Conselleria de Innovacion e Industria-Xunta de Galicia [PGIDIT08MDS036000PR]; Cross-Research in Environmental Technologies of the Santiago de Compostela University (CRETUS) strategic group [AGRUP2015/02]; Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (GNN, JCNE Grant) [FAPERJE-26/202.757/2019]; Sao Paulo Research Foundation (FAPESP) [2019/02855-0]	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council for Scientific and Technology Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Conselleria de Innovacion e Industria-Xunta de Galicia(Xunta de Galicia); Cross-Research in Environmental Technologies of the Santiago de Compostela University (CRETUS) strategic group; Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (GNN, JCNE Grant); Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The first author would like to thank CAPES for the financial support to R.LC., T.O.F, and X.L.O. We thank the members of Nucleo de Pesquisa em Pedologia (Nuppe/UFC) for field and laboratory support and Maria J. Santiso for laboratory assistance. The authors are grateful for the financial support provided by National Council for Scientific and Technology Development (CNPq, process 305996/2018-5; 409593/2018-4); Conselleria de Innovacion e Industria-Xunta de Galicia (PGIDIT08MDS036000PR); Cross-Research in Environmental Technologies of the Santiago de Compostela University (CRETUS) strategic group (AGRUP2015/02), Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (GNN, JCNE Grant FAPERJE-26/202.757/2019), and Sao Paulo Research Foundation (FAPESP, DB: Grant #2019/02855-0	Abed RMM, 2015, GEOMICROBIOL J, V32, P119, DOI 10.1080/01490451.2014.932033; Albuquerque A., 2015, THESIS; Albuquerque AGBM, 2014, SOIL RES, V52, P140, DOI 10.1071/SR13179; Alvarez E, 2011, J SOIL SEDIMENT, V11, P221, DOI 10.1007/s11368-010-0295-2; An JX, 2019, GEODERMA, V337, P290, DOI 10.1016/j.geoderma.2018.09.035; AUGSPURGER CK, 1984, J ECOL, V72, P777, DOI 10.2307/2259531; Barcellos D, 2019, MAR POLLUT BULL, V142, P58, DOI 10.1016/j.marpolbul.2019.03.031; 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Sci.-Basel	NOV	2020	10	21							7624	10.3390/app10217624	http://dx.doi.org/10.3390/app10217624			18	Chemistry, Multidisciplinary; Engineering, Multidisciplinary; Materials Science, Multidisciplinary; Physics, Applied	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Engineering; Materials Science; Physics	OQ8PS		Green Published, gold			2023-06-23	WOS:000589038700001
J	Carneiro, AF; Carneiro, CN; Pires, LD; Teixeira, LSG; Azcarate, SM; Dias, FD				Carneiro, Angelica F.; Carneiro, Candice N.; Pires, Lais de N.; Teixeira, Leonardo S. G.; Azcarate, Silvana M.; Dias, Fabio de S.			D-optimal mixture design for the optimization of extraction induced by emulsion breaking for multielemental determination in edible vegetable oils by microwave-induced plasma optical emission spectrometry	TALANTA			English	Article						Edible oils; Metals; D-optimal mixture design; Extraction; Emulsion breaking	LIQUID-LIQUID MICROEXTRACTION; ULTRASOUND-ASSISTED EXTRACTION; MASS SPECTROMETRY; DOEHLERT MATRIX; TRACE-ELEMENTS; MIP-OES; ICP-AES; SAMPLES; CADMIUM; METALS	A sample pretreatment based on an extraction process by emulsion breaking for multi-element determination in edible oils was developed. The determination of eight trace elements (Al, Ba, Cu, Cr, P, Ni, Ti, and Zn) was carried out by microwave-induced plasma optical emission spectrometry (MIP OES) after the extraction procedure. A D-optimal mixture experimental design was used to obtain the best experimental conditions for the extraction induced by emulsion breaking (EIEB). The proportion of HNO3 solution, Triton X-100 solution and sample was evaluated in a multivariate manner. The best recovery efficiency was obtained with 1.0 mL of 30% (v/v) HNO3, 1.0 mL of 30% (w/v) Triton-X 100 and 3.0 mL of the sample. The precisions, established as the relative standard deviation (RSD, %), were better than 2.5% for all analytes. The developed method was applied to the analysis of commercial vegetable oils with low limits of detection and good precision.	[Carneiro, Angelica F.; Carneiro, Candice N.] Univ Fed Do Reconcavo Bahia, Ctr Ciencias Exatas & Tecnol, Campus Univ Cruz Das Almas, BR-44380000 Cruz Das Almas, Bahia, Brazil; [Pires, Lais de N.; Teixeira, Leonardo S. G.; Dias, Fabio de S.] Univ Fed Bahia, Campus Univ Ondina, Inst Quim, Dept Quim Analit, BR-40170115 Salvador, BA, Brazil; [Teixeira, Leonardo S. G.] Univ Fed Bahia, Campus Univ Ondina, Inst Quim, INCT Energia & Ambiente, BR-40170115 Salvador, BA, Brazil; [Azcarate, Silvana M.] Univ Nacl La Pampa, Fac Ciencias Exactas & Nat, Av Uruguay 151,L6300CLB, Santa Rosa, La Pampa, Argentina; [Azcarate, Silvana M.] Inst Ciencias La Tierra & Ambient La Pampa INCITA, Av Uruguay 151,L6300CLB, Santa Rosa, La Pampa, Argentina; [Azcarate, Silvana M.] Consejo Nacl Invest Cient & Tecn CONICET, Godoy Cruz 2290,C1425FQB, Caba, Argentina	Universidade Federal da Bahia; Universidade Federal da Bahia	Dias, FD (autor correspondente), Univ Fed Bahia, Campus Univ Ondina, Inst Quim, Dept Quim Analit, BR-40170115 Salvador, BA, Brazil.	fsdias@ufba.br	Teixeira, Leonardo S G/J-9131-2016; de Souza Dias, Fabio/I-4716-2013	Teixeira, Leonardo S G/0000-0003-0320-8299; CARNEIRO, CANDICE NOBREGA/0000-0001-5403-4570; Azcarate, Silvana/0000-0002-3736-4540	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) Finance Code 001. The authors are also grateful to Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB) and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for providing grants, fellowships and financial support.	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J	Chaves, AD; Porcher, CC				Chaves, Alexandre de Oliveira; Porcher, Carla Cristine			Petrology, geochemistry and Sm-Nd systematics of the Paleoproterozoic Itaguara retroeclogite from Sao Francisco/Congo Craton: One of the oldest records of the modern-style plate tectonics	GONDWANA RESEARCH			English	Article						Eclogite; Sao Francisco Craton; Paleoproterozoic; Plate tectonics	QUADRILATERO-FERRIFERO; EMPIRICAL CALIBRATION; GREENSTONE-BELT; DETRITAL ZIRCON; MINEIRO BELT; SE BRAZIL; EVOLUTION; PB; OROGENY; BASEMENT	Paleoproterozoic retrogressed eclogite (retroeclogite) occurs in the Itaguara Sequence included in the suture zone formed by collision between the Archean Divinopolis and Campo Belo/Bonfim Complexes in the southern Sao Francisco Craton, which represents the South American counterpart of the African Congo Cra ton. The Itaguara retroeclogite contains scarce omphacite and phengite but abundant garnet porphyroblasts embedded in a finegrained, amphibole, biotite and quartz-bearing matrix. The 2.20 +/- 0.05 Ga edogitization event (garnet and whole rock Sm-Nd isochronic age) of the E-MORB protolith (T-DM similar to 2.47 Ga) is recorded by omphad te formation during high-pressure prograde stage in amphibole edogite fades due to similar to 70 km depth subduction process. Amphibole eclogite fades metamorphic peak stage of 17-20 kbar and 600-700 degrees C occurred during similar to 2.1 Ga continental collision. Tectonic exhumation-related decompression during collision probably triggered partial melting of the eclogitic rock. Finally, decompression late stage estimated between 5 and 8 kbar and 550-650 degrees C under amphibolite fades overprint during orogenic collapse was responsible for appearance of kelyphitic reaction rims (symplectite) around garnet crystals. As its Paleoproterozoic contemporary analogues from Congo Craton, the Itaguara retroedogite is one of the oldest records of the modern-style plate tectonics. (C) 2020 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.	[Chaves, Alexandre de Oliveira] Fed Univ Minas Gerais CPMTC IGC UFMG, Manoel Teixeira da Costa Res Ctr, Inst Geosci, Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Porcher, Carla Cristine] Fed Univ Rio Grande do Sul LGI IG UFRGS, Inst Geosci, Isotope Geol Lab, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil		Chaves, AD (autor correspondente), Fed Univ Minas Gerais CPMTC IGC UFMG, Manoel Teixeira da Costa Res Ctr, Inst Geosci, Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.	alochaves@yahoo.com.br	Porcher, Carla C/R-1419-2018	Porcher, Carla C/0000-0002-0418-3954	CNPq (National Council for Scientific and Technological Development)	CNPq (National Council for Scientific and Technological Development)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Authors thank CNPq (National Council for Scientific and Technological Development) for the research productivity grant, to Ramon O. Aranda for supporting in field and lab, to K. Cutts for constructive comments and for aiding with P-T pseudosection, to V. Schenk and anonymous reviewers for constructive comments.	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J	Correa, RS; Oliveira, CG; Dantas, EL; Botelho, NF				Correa, R. S.; Oliveira, C. G.; Dantas, E. L.; Botelho, N. F.			Hydrothermal footprint related to regional-scale shear zone-controlled scheelite mineralization, Serido W-skarn system, northeastern Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Serido mineral Province; Tungsten metallogenesis; Skarn deposits; Root zones of magmatic-hydrothermal systems	BORBOREMA PROVINCE NE; DETRITAL ZIRCON AGES; OXIDE-COPPER-GOLD; GA SAO-JOSE; U-PB; NORTHWEST-TERRITORIES; CAMPESTRE MASSIF; WEST GONDWANA; PORPHYRY CU; BELT	Tungsten deposits and occurrences in the Serido Mineral Province represent metasomatic assemblages that differ from the garnet-diopside skarn deposits described in the area. The six W(+/- Mo +/- Au) selected for study show no spatial association with carbonate rocks or igneous intrusions, but are strongly controlled by regional-scale N20 degrees E-trending shear zones formed during the Neoproterozoic-Ediacaran (ca. 615 Ma to 530 Ma) Brasiliano Cycle. Throughout the area, this omgenic event affected both basement and supracrustal rocks, forming scheelite-bearing rocks in both domains. The alteration process is characterized by three mineral associations: (1) diopside-amphibole-feldspars (DAF), (2) amphibole-feldspars (AF), and (3) biotite-rich (BR); and each deposit or occurrence may present one, two or all mineral assemblages. Some of the studied locations are also spatially associated with the mineralized garnet-diopside skarns (MGDS) of the province, where the three mineral associations generally occur tens to hundreds of meters below them. These associations represent a continuously evolving system that records changes in physicochemical properties over time. These changes are documented by mineral chemistry analyses for pyroxene, amphibole, feldspars, biotite, epidote group minerals, titanite and apatite. Earlier, higher temperature metasomatism enriched the system in Mg, Fe, Ca, Ba and REE, whereas later, lower temperature stages are characterized by an enrichment in Na, K, Si, W and Mo. The studied mines and occurrences provide important information on the distal, deeper hydrothermal alteration haloes of tungsten skarn deposits in the Serido Mineral Province.	[Correa, R. S.; Oliveira, C. G.; Dantas, E. L.; Botelho, N. F.] Univ Brasilia, Inst Geociencias, Campus Asa Norte, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia	Correa, RS (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Asa Norte, BR-70910900 Brasilia, DF, Brazil.	robertodesiqueiracorrea@gmail.com	Dantas, Elton Luiz/AAK-8464-2021; Botelho, Nilson Francisquini/T-9470-2017	Dantas, Elton Luiz/0000-0002-7954-5059; Botelho, Nilson Francisquini/0000-0001-9090-799X	CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior); CNPq (Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico) [474380/2006-8, 308312/2014-7]	CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq (Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to thank the Earth Sciences Institute of the University of Brasilia for providing the analytical infrastructure, CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) for the financial support, CNPq (Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico) for the research grants (projects 474380/2006-8 and 308312/2014-7), the geologists Luiz Neto and Eduardo for the aid with this research and the anonymous reviewers for their relevant comments and corrections.	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NOV	2020	103								102755	10.1016/j.jsames.2020.102755	http://dx.doi.org/10.1016/j.jsames.2020.102755			28	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NS6MG					2023-06-23	WOS:000572372500001
J	da Silva, RC; Lopes, JM; da Silva, LB; Domingues, AM; Pinheiro, CD; da Silva, LF; da Silva, AX				da Silva, Roberto Cruz; Lopes, Jose Marques; da Silva, Leandro Barbosa; Domingues, Alessandro Mariano; Pinheiro, Carla da Silva; da Silva, Lucas Faria; da Silva, Ademir Xavier			Radiological evaluation of Ra-226, Ra-228 and K-40 in tea samples: A comparative study of effective dose and cancer risk	APPLIED RADIATION AND ISOTOPES			English	Article						Naturally occurring radionuclides; Tea consumption; Committed effective dose	MEDICINAL HERBS; RADIONUCLIDES; RADIOACTIVITY; 137CS; SOUTH	Activity concentrations of tea samples were determined using high resolution gamma spectrometry.The values ranged from (421.00 +/- 17.00) to (732.00 +/- 30.00) Bq.kg(-1) for K-40 and from (3.00 +/- 0.80) to (27.00 +/- 3.00) Bq.kg(-1) for Ra-228. The values for Ra-226 were below 27.00 Bq.kg(-1). The committed effective dose was estimated at 4.74-78.89 mu Sv.y(-1) for adults and 13.55-445.84 mu Sv.y(-1) for children. The cancer risk was higher for females. However, results showed that the tea consumption do not represent a radiological health risk to the population.	[da Silva, Roberto Cruz; da Silva, Leandro Barbosa; Domingues, Alessandro Mariano; da Silva, Ademir Xavier] Univ Fed Rio de Janeiro, Nucl Engn Dept, Av Horacio Macedo 2030,Bloco G,Sala 206-CT, BR-21945970 Rio De Janeiro, RJ, Brazil; [Lopes, Jose Marques] Univ Fed Bahia, Geochem Dept Pospetro, Rua Barao de Jeremoabo S-N, BR-40170110 Salvador, BA, Brazil; [Pinheiro, Carla da Silva] Brazilian Marine Corps Technol Ctr, Av Brasil,Parada de Lucas 13478, BR-21010076 Rio De Janeiro, RJ, Brazil; [da Silva, Lucas Faria] Univ Fed Rio de Janeiro, Chem Sch, Av Athos da Silveira Ramos 149, BR-21941909 Rio De Janeiro, CT, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal da Bahia; Universidade Federal do Rio de Janeiro	da Silva, RC (autor correspondente), Univ Fed Rio de Janeiro, Nucl Engn Dept, Av Horacio Macedo 2030,Bloco G,Sala 206-CT, BR-21945970 Rio De Janeiro, RJ, Brazil.	rcruz@con.ufrj.br		Silva, Lucas Faria/0000-0003-1209-3091; Barbosa da Silva, Leandro/0000-0002-8544-8634; Marques Lopes, Jose/0000-0001-7819-6646	FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro); CNPq (Conselho Nacional de Pesquisa e Desenvolvimento); Technological Center of Navy Corps	FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); CNPq (Conselho Nacional de Pesquisa e Desenvolvimento)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Technological Center of Navy Corps	The authors would like to thank FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro) and CNPq (Conselho Nacional de Pesquisa e Desenvolvimento) for the financial support and Technological Center of Navy Corps for support and foment for this research, without their help this work would not be possible.	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Bras., V22, P566, DOI 10.1590/S0102-05362004000300013; Ribeiro FCA, 2018, J ENVIRON RADIOACTIV, V182, P34, DOI 10.1016/j.jenvrad.2017.11.017; Ribeiro F.C.A., 2018, RADIAT PHYS CHEM; Ribeiro FCA., 2016, BRAZ J RAD SCI, V4, P1; Scheibel V, 2007, J FOOD COMPOS ANAL, V20, P650, DOI 10.1016/j.jfca.2007.04.005; Souza José Roberto P de, 2006, Hortic. Bras., V24, P233, DOI 10.1590/S0102-05362006000200023; UNSCEAR, 2000, GEN ASS ANN UN NEW Y; USEPA (United States Environmental Protection Agency), 1999, 402R99001 USEPA; WHO, 1999, MON SEL MED PLANTS	37	8	8	0	3	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0969-8043			APPL RADIAT ISOTOPES	Appl. Radiat. Isot.	NOV	2020	165								109326	10.1016/j.apradiso.2020.109326	http://dx.doi.org/10.1016/j.apradiso.2020.109326			6	Chemistry, Inorganic & Nuclear; Nuclear Science & Technology; Radiology, Nuclear Medicine & Medical Imaging	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Nuclear Science & Technology; Radiology, Nuclear Medicine & Medical Imaging	NN3NM	32777740				2023-06-23	WOS:000568698100019
J	Ferreira, ADD; Dantas, EL; dos Santos, TJS; Fuck, RA; Tedeschi, M				Dantas Ferreira, Alanielson da Camara; Dantas, Elton Luiz; Saraiva dos Santos, Ticiano Jose; Fuck, Reinhardt A.; Tedeschi, Mahyra			High-pressure metamorphic rocks in the Borborema Province, Northeast Brazil: Reworking of Archean oceanic crust during proterozoic orogenies	GEOSCIENCE FRONTIERS			English	Article						Archean oceanic crust; Proterozoic orogens; Borborema province	PLASMA-MASS SPECTROMETRY; SOUTHERN BRASILIA BELT; NE BRAZIL; U-PB; ISOTOPE COMPOSITIONS; BELOMORIAN PROVINCE; CONTINENTAL-CRUST; HAFNIUM ISOTOPE; GARNET GROWTH; ZIRCON	We present the first evidence of Archean oceanic crust submitted to Proterozoic high-pressure (HP) metamorphism in the South American Platform. Sm-Nd and Lu-Hf isotopic data combined with U-Pb geochronological data from the Campo Grande area, Rio Grande do Norte domain, in the Northern Borborema Province, reflect a complex Archean (2.9 Ga and 2.6 Ga) and Paleoproterozoic (2.0 Ga) evolution, culminating in the Neoproterozoic Brasiliano/Pan-African orogeny (ca. 600 Ma). The preserved mafic rocks contain massive poikiloblastic garnet and granoblastic amphibole with variable proportions of plagioclase + diopside in symplectitic texture, typical of high-pressure rocks. These clinopyroxene-garnet amphibolites and the more common garnet amphibolites from the Campo Grande area are exposed as rare lenses within an Archean migmatite complex. The amphibolite lenses represent 2.65 Ga juvenile tholeiitic magmatism derived from depleted mantle sources (positive epsilon(Hf)(t) values of +3.81 to +30.66) later enriched by mantle metasomatism (negative epsilon(Nd)(t) values of -7.97). Chondrite and Primitive Mantle-normalized REE of analyzed samples and discriminant diagrams define two different oceanic affinities, with E-MORB and OIB signature. Negative Eu anomalies (Eu/Eu* = 0.75-0.95) indicate depletion of plagioclase in the source. Inherited zircon cores of 3.0-2.9 Ga in analyzed samples indicate that the Neoarchean tholeiitic magmatism was emplaced into 2923 +/- 14 Ma old Mesoarchean crust (epsilon(Nd)(t) = -2.58 and Nd T-DM = 3.2 Ga) of the Rio Grande do Norte domain. The age of retro-eclogite facies metamorphism is not yet completely understood. We suggest that two high-grade metamorphic events are recognized in the mafic rocks: the first at 2.0 Ga, recorded in some samples, and the second, at ca. 600 Ma, stronger and more pervasive and recorded in several of the mafic rock samples. The Neoproterozoic zircon grains are found in symplectite texture as inclusions in the garnet grains and represent the age of HP conditions in the area. These zircon grains show a younger cluster of concordant analyses between 623 +/- 3 Ma and 592 +/- 5 Ma with epsilon(Hf)(t) values of +0.74 to -65.88. Thus, the Campo Grande rock assemblage is composed of Archean units that were amalgamated to West Gondwana during Neoproterozoic Brasiliano orogeny continent-continent collision and crustal reworking.	[Dantas Ferreira, Alanielson da Camara; Dantas, Elton Luiz; Fuck, Reinhardt A.] Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Saraiva dos Santos, Ticiano Jose] Univ Estadual Campinas, Inst Geociencias, Dept Geol & Recursos Nat, UNICAMP, BR-13083970 Campinas, SP, Brazil; [Tedeschi, Mahyra] Univ Fed Minas Gerais UFMG, Inst Geociencias, BR-31270901 Belo Horizonte, MG, Brazil	Universidade de Brasilia; Universidade Estadual de Campinas	Ferreira, ADD (autor correspondente), Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil.	ferreira.acd@ufrgs.br	Dantas, Elton Luiz/AAK-8464-2021; Tedeschi, Mahyra/E-7298-2019	Dantas, Elton Luiz/0000-0002-7954-5059; Ferreira, Alanielson/0000-0001-8054-0047; Tedeschi, Mahyra/0000-0001-6573-0846; Saraiva dos Santos, Ticiano Jose/0000-0002-9491-1213	INCT Estudos Tectonicos [CAPES/CNPq-465613/2014-4, FAPDF-193.001.263/2017]; CNPq	INCT Estudos Tectonicos; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study is part of the first author's PhD thesis in development at the Institute of Geosciences (Universidade de Brasilia). The authors acknowledge the support of the INCT Estudos Tectonicos (CAPES/CNPq465613/2014-4 and FAPDF-193.001.263/2017). ELD, TJSS, RAF and MT acknowledge CNPq research fellowships.	Albarede F, 2004, GEOCHIM COSMOCHIM AC, V68, P2725, DOI 10.1016/j.gca.2003.11.024; Amaral WS, 2017, J S AM EARTH SCI, V79, P409, DOI 10.1016/j.jsames.2017.08.022; Archanjo CJ, 2013, GONDWANA RES, V23, P701, DOI 10.1016/j.gr.2012.05.005; Arthaud MH, 2008, GEOL SOC SPEC PUBL, V294, P49, DOI 10.1144/SP294.4; Bau M, 1996, CONTRIB MINERAL PETR, V123, P323, DOI 10.1007/s004100050159; Bau M, 1999, CHEM GEOL, V155, P77, DOI 10.1016/S0009-2541(98)00142-9; BlichertToft J, 1997, EARTH PLANET SC LETT, V148, P243, DOI 10.1016/S0012-821X(97)00040-X; BRITO NEVES B. 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Front.	NOV	2020	11	6					2221	2242		10.1016/j.gsf.2020.03.004	http://dx.doi.org/10.1016/j.gsf.2020.03.004			22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OI1IY		gold			2023-06-23	WOS:000583042200022
J	De Castro, MP; Queiroga, GN; Martins, M; Pedrosa-Soares, AC; Dias, L; Lana, C; Babinski, M; Alkmim, AR; da Silva, MA				De Castro, Marco Paulo; Queiroga, Glaucia Nascimento; Martins, Maximiliano; Pedrosa-Soares, Antonio Carlos; Dias, Leon; Lana, Cristiano; Babinski, Marly; Alkmim, Ana Ramalho; da Silva, Marco Antonio			Provenance shift through time in superposed basins: From Early Cryogenian glaciomarine to Late Ediacaran orogenic sedimentations (Aracuai Orogen, SE Brazil)	GONDWANA RESEARCH			English	Article						U-Pb and Lu-Hf isotopes; Glaciomarine; Orogenic sedimentation; Aracuai - West Congo orogen; Brasiliano - Pan-African event	SAO-FRANCISCO CRATON; PB-HF ISOTOPES; ZIRCON U-PB; NEOPROTEROZOIC CRUSTAL ACCRETION; WEST-CONGO OROGEN; DETRITAL-ZIRCON; EASTERN BRAZIL; TECTONIC EVOLUTION; RIBEIRA BELT; MAGMATIC ARC	Records of Precambrian glaciation have been reported from southeastern Brazil for over a century. We present sedimentological, stratigraphic and isotopic (U-Pb and Lu-Hf on detrital zircons, C and O on carbonates) studies on diamictite-rich to diamictite-free successions of the Aracuai Orogen, the Brazilian counterpart of the Aracuai West Congo Orogenic System (AWCO). From base to top, the Chapada Acacia - Formation (Macafibas Group) includes a diamictite-rich unit, with lenses of graded sandstone and last-supported conglomerate, that gradually passes to graded sandstone, pelite with sparse oversized dasts and rare carbonate lenses on top, representing mass flow and turbidity current deposits of submarine fan, followed by finer-grained turbiditic sedimentation with iceberg discharges along fan fringes, from glaciomarine to post-glacial scenarios. The Salinas Formation comprises a deep-sea sand-mud sequence composed of pelites and pelitic wackes. The Chapada Acacia Formation was deposited in-between 750 and 667 Ma. It shows wide spectra of zircon ages (typical of continental rift to passive margin settings) that start around 3.2 Ga and display main age peaks indicating sediment provenance from the Rhyacian-Orosirian basement (epsilon Hf-(t) = +14.6 to -18.5) and Early Tonian anorogenic rocks (950-880 Ma; epsilon Hf-(t) = -3.2 to -23.2) for the diamictite-rich lower unit and, for the upper unit, also in Early Cryogenian anorogenic rocks (ca. 715 Ma, epsilon Hf-(t) = -9.6). In contrast, the Salinas Formation shows most ages in-between 676 and 620 Ma and a maximum sedimentation age around 551 Ma, with epsilon Hf-(t) from +6.9 to -18.2, unravelling an important shifting of sediment provenance to sources located in magmatic arcs and collisional granites of the Aragtai and Ribeira orogens. The Early Cryogenian age and negative Hf signature for the gladomarine Chapada Acacia Formation point to sediment sources in the 720-670 Ma anorogenic igneous rocks found in AWCO and adjacent Congo - Sao Francisco Craton, and suggest correlation with the Sturtian global glaciation. (C) 2020 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.	[De Castro, Marco Paulo; Queiroga, Glaucia Nascimento; Martins, Maximiliano; Dias, Leon; Lana, Cristiano; Alkmim, Ana Ramalho; da Silva, Marco Antonio] Univ Fed Ouro Preto, DEGEO EM, BR-35400000 Ouro Preto, MG, Brazil; [Pedrosa-Soares, Antonio Carlos] Univ Fed Minas Gerais, CPMTC IGC UFMG, Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Babinski, Marly] Univ Sao Paulo, IG USP, Cidade Univ, Sao Paulo, SP, Brazil; [Queiroga, Glaucia Nascimento] Brazilian Res Council CNPq, Brasilia, DF, Brazil	Universidade Federal de Ouro Preto; Universidade Federal de Minas Gerais; Universidade de Sao Paulo	De Castro, MP (autor correspondente), Univ Fed Ouro Preto, DEGEO EM, BR-35400000 Ouro Preto, MG, Brazil.	marco.castro@ufop.edu.br	Queiroga, Gláucia/AAJ-1823-2021; Babinski, Marly/B-9403-2013; Martins, Maximiliano/AAP-7741-2021	Queiroga, Gláucia/0000-0002-1730-0638; Babinski, Marly/0000-0003-2444-2404; Martins, Maximiliano/0000-0001-9118-6020	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico-CNPq [430789/2016-5]; Universidade Federal de Ouro Preto [22/2019, 23109.004080/2019-88]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico-CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Universidade Federal de Ouro Preto	This article is part of the PhD thesis by Marco Paulo de Castro at Programa de Pos-Graduacao em Evolucao Crustal e Recursos Naturais, Universidade Federal de Ouro Preto, MG, Brazil. This work was financially supported by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico-CNPq (grant number 430789/2016-5 to G. Queiroga) and by project of Universidade Federal de Ouro Preto (Auxilio Pesquisador 22/2019, process 23109.004080/2019-88 to G. Queiroga). We are grateful to Leo A. Hartmann for very useful and constructive comments. The authors acknowledge the Laboratory of Geochronology and the Laboratory of Microscopy andMicroanalyses (LMic) of UFOP. G. Queiroga, A.C. Pedrosa-Soares, M. Babinski and C. Lana are fellows of the Brazilian Research Council (CNPq) and acknowledge systematic support.	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NOV	2020	87						41	66		10.1016/j.gr.2020.05.019	http://dx.doi.org/10.1016/j.gr.2020.05.019			26	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NS7BF					2023-06-23	WOS:000572412000003
J	de Oliveira, FA; Santucci, RM				de Oliveira, Fabio Antonio; Santucci, Rodrigo Miloni			Palynological analysis of coprolites from the Marilia Formation, Bauru Group (Upper Cretaceous), Minas Gerais, Brazil	CRETACEOUS RESEARCH			English	Article						Bauru Group; Coprolites; Palynomorphs; Marilia Formation; Cretaceous	MAASTRICHTIAN LAMETA FORMATION; SANTA-CRUZ PROVINCE; DINOSAUR COPROLITES; VERTEBRATE COPROLITES; MEDICINE FORMATION; ARARIPE BASIN; SERGIPE BASIN; TANO BASIN; POLLEN; MORPHOLOGY	The deposits of the Serra da Galga Member, Marilia Formation (Bauru Group), in Uberaba, state of Minas Gerais, Brazil, provided a rich fauna of vertebrates of Maastrichtian age. Despite the great faunistic diversity, the plant material recorded so far in these deposits is scarce. Together with the vertebrate remains, a relatively large number of coprolites has been reported for at least two localities in Uberaba, but this material received little attention so far. In this work, we present the first record of palynomorphs found within some coprolites from the Peiropolis and Serra da Galga sites. Monoporate, ephedroid, Gnetaceaepollenites?, Monosulcites?, and Podocarpidites pollen types were found. This pollen set shows that the flora was composed of shrubs (probably Gnetophyta), arboreal conifers, and cycads that lived under arid climate conditions. Moreover, saprophytic fungal remains were found within a few coprolites, representing the first record of this kind for the Bauru Group deposits in Minas Gerais. (C) 2020 Elsevier Ltd. All rights reserved.	[de Oliveira, Fabio Antonio] Univ Brasilia, Inst Geosci, BR-70910900 Brasilia, DF, Brazil; [Santucci, Rodrigo Miloni] Univ Brasilia, UnB Planaltina Campus, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia; Universidade de Brasilia	Santucci, RM (autor correspondente), Univ Brasilia, UnB Planaltina Campus, BR-70910900 Brasilia, DF, Brazil.	paleofabio@gmail.com; rodrigoms@unb.br	Santucci, Rodrigo M/E-2189-2013	Oliveira, Fabio Antonio de/0000-0001-8125-6339; Santucci, Rodrigo/0000-0002-4326-743X	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico (CNPq)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank Luiz Carlos Borges Ribeiro (Museum of Dinosaurs/CPP L. I. Price) for all support during the development of the work. We also thank the Laboratory of X-ray Diffraction of the Institute of Geosciences (University of Brasilia) for the analysis of the samples and M. Barberi (Laboratory of Paleoecology of Pontifical Catholic University of Goias, PUC-GO), where the palynological samples were processed and analyzed. We thank M. Arai (UNESP) for their suggestions regarding the taxonomic identification of some palynomorphs found in our study. We are also grateful to the editors and two anonymous reviewers whose comments substantially improved an earlier draft of this manuscript. FAO was supported by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), finance code 001 and by Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico (CNPq).	ALVIN KL, 1982, REV PALAEOBOT PALYNO, V37, P71, DOI 10.1016/0034-6667(82)90038-0; AMSTUTZ G. 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Res.	NOV	2020	115								104545	10.1016/j.cretres.2020.104545	http://dx.doi.org/10.1016/j.cretres.2020.104545			16	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	NN4NR					2023-06-23	WOS:000568766700005
J	de Oliveira, OMC; Queiroz, AFD; Cerqueira, JR; Soares, SAR; Garcia, KS; Pavani, A; Rosa, MDD; Suzart, CM; Pinheiro, LD; Moreira, ITA				de Oliveira, Olivia M. C.; Queiroz, Antonio F. de S.; Cerqueira, Jose R.; Soares, Sarah A. R.; Garcia, Karina S.; Pavani Filho, Aristides; Rosa, Maria de L. da S.; Suzart, Caroline M.; Pinheiro, Liliane de L.; Moreira, Icaro T. A.			Environmental disaster in the northeast coast of Brazil: Forensic geochemistry in the identification of the source of the oily material	MARINE POLLUTION BULLETIN			English	Article						Petroleum; Forensic geochemistry; Oil spill; Stable carbon isotopes; Heavy oil	OS SANTOS BAY; PETROLEUM-HYDROCARBONS; SPILL; DIFFERENTIATION; IMPACTS	The characterization of petroleum or its products spilled in the environment in relation to its source rocks is an important tool to assist in the resolution of issues of environmental impact and legal responsibility since it clarifies the possible region or the producing country of that type of petroleum. This article analyzes the ap-plication of analytical techniques for petroleum geochemistry to identify the type and origin of oily material collected from beaches in Northeast Brazil in 2019. Samples of the oily material collected on the beaches in the states of Bahia and Sergipe were analyzed and for comparison purposes, samples of crude oils produced in Brazil, Middle East, Nigeria and Venezuela were also analyzed. The analytical results showed that the oily material that reached the beaches has geochemical characteristics compatible with those of the Venezuelan oil, indicating it was severely weathered or a product made with heavy oil produced.	[de Oliveira, Olivia M. C.; Queiroz, Antonio F. de S.; Soares, Sarah A. R.] Fed Univ Bahia UFBA, Geosci Inst, St Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil; [de Oliveira, Olivia M. C.; Queiroz, Antonio F. de S.; Cerqueira, Jose R.; Soares, Sarah A. R.; Garcia, Karina S.; Suzart, Caroline M.; Pinheiro, Liliane de L.; Moreira, Icaro T. A.] Fed Univ Bahia UFBA, Geosci Inst, LEPETRO, St Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil; [Pavani Filho, Aristides] Minist Sci Technol & Innovat MCTI, Brasilia, DF, Brazil; [Rosa, Maria de L. da S.] Fed Univ Sergipe UFS, Dept Geol, Av Marechal Rondon S-N, Aracaju, SE, Brazil; [Moreira, Icaro T. A.] Fed Univ Bahia UFBA, Polytech Sch, Dept Environm Engn, St Prof Aristides Novis 2, BR-40170290 Salvador, BA, Brazil		Moreira, ITA (autor correspondente), Fed Univ Bahia UFBA, Polytech Sch, Dept Environm Engn, St Prof Aristides Novis 2, BR-40170290 Salvador, BA, Brazil.	icarotam@ufba.br	Queiroz, Antonio Fernando de Souza/ABH-6682-2020; Pavani, Aristides/AAB-3769-2021; de Oliveira, Olivia Maria Cordeiro/AAB-3246-2021; Cerqueira, José Roberto/AAY-9852-2021	Reis, AlessanRSS/0000-0001-8486-7469	Coordination for the Improvement of Higher Education Personnel - Brazil (CAPES) [001]	Coordination for the Improvement of Higher Education Personnel - Brazil (CAPES)	We thank Prof. Dr. Marcos de Oliveira Melo from the State University of Feira de Santana (UEFS), for his support in collecting samples. And to Prof. Dr. Jose Roberto from the Laboratory of Stable Isotopes of the Physics Institute of UFBA, for carrying out the Isotope analyses. We also had the support of the Coordination for the Improvement of Higher Education Personnel - Brazil (CAPES) Financing Code 001.	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Pollut. Bull.	NOV	2020	160								111597	10.1016/j.marpolbul.2020.111597	http://dx.doi.org/10.1016/j.marpolbul.2020.111597			7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	OO8KV	32896715				2023-06-23	WOS:000587624600012
J	de Oliveira, SB; Juliani, C; Monteiro, LVS; Tassinari, CCG				de Oliveira, Saulo B.; Juliani, Caetano; Monteiro, Lena V. S.; Tassinari, Colombo C. G.			Structural control and timing of evaporite-related Mississippi Valley-type Zn-Pb deposits in Pucara Group, northern central Peru	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Pucara Basin; MVT deposits; Chambara Formation; Rb-Sr sphalerite	FOLD-THRUST BELT; FLORIDA CANYON; SAN VICENTE; RB-SR; BONGARA DISTRICT; MIXING PROCESSES; FORELAND BASIN; MINERALIZATION; EVOLUTION; SULFIDE	The South America MVT belt comprises the deposits of San Vicente, Shalipayco, Florida Canyon, and some minor Zn-Pb occurrences hosting in the carbonates and evaporites of the Pucara Group, in an extension of more than a thousand kilometers from the center to the north of Peru. Structural constraints of the MVT Peruvian deposits are conditioned by deep sub-vertical secondary extension structures with general N, NNE or NNW direction related to strike-slip movements superimposed on previous Andean NW thrust structures. Recent studies on Shalipayco and Florida Canyon deposits point to similar processes of rock formation, diagenesis and mineralization acting in province scale. New isotopic data of Pb-Pb and Rb-Sr in sulfides summed with a compilation of the available data for the evaporite-related MVT deposits and studies on the structural and tectonic evolution of the Peruvian Andes allowed establishing correlations of local process of the deposits to the regional Andean tectonic events. The Florida Canyon saline dome structure was attributed to Junta Orogeny (157-152 Ma). The stage of dolomitization forming the porous dolostone and evaporite breccia during burial diagenesis is attributed to the period between Junta and Mochica stages. The oil migration to these reservoir rocks occurred probably during Mochica event (100-95 Ma). The Rb-Sr dating of sphalerite from the Florida Canyon deposit together with temporal field relations indicated that the Zn-Pb sulfide ore formed in or just after Peruvian Orogeny (86-83 Ma).	[de Oliveira, Saulo B.; Juliani, Caetano; Monteiro, Lena V. S.; Tassinari, Colombo C. 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South Am. Earth Sci.	NOV	2020	103								102736	10.1016/j.jsames.2020.102736	http://dx.doi.org/10.1016/j.jsames.2020.102736			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NS6KI					2023-06-23	WOS:000572367500002
J	Meira, RCD; da Paz, SPA; Correa, JAM				de Souza Meira, Rose Caldas; Aranha da Paz, Simone Patricia; Martins Correa, Jose Augusto			XRD-Rietveld analysis as a tool for monitoring struvite analog precipitation from wastewater: P, Mg, N and K recovery for fertilizer production	JOURNAL OF MATERIALS RESEARCH AND TECHNOLOGY-JMR&T			English	Article						Struvite; Struvite analog; Rietveld refinement; X-ray diffraction - XRD	STANDARD PXRD METHOD; PHOSPHORUS RECOVERY; LE BAIL; DECOMPOSITION; PROPOSAL; AMMONIA; BAUXITE	The objective of this study was to select between four proposed synthesis conditions, which one would be the most propitious for struvite precipitation from wastewater and, on such product, detail its crystallochemical aspects using the Rietveld refinement method to determine the chemical formula and chemistry analyses by Wavelength Dispersive X-ray Fluorescence (WDXRF) for validation. The struvite synthesis was investigated for pH 10 and 12 and phosphorus concentrations of 100 and 300 mg/L under the same room temperature (RT) condition and a magnesium to phosphorus to nitrogen (Mg: P: N) molar ratio of 1: 1: 2. Struvite was successfully obtained under a moderately alkaline pH (10). No struvite precipitation occurred under the same temperature and Mg: P: N molar ratio for a highly alkaline pH (12). Under RT condition, 300 mg/L P, a Mg: P: N molar ratio of 1: 1: 2, and a pH of 10, a product with two struvite phases was obtained: an 75% struvite analog ([K-0.34(NH4)(0.66)] MgPO4 center dot 6H(2)O) and 25% struvite (NH4MgPO4 center dot 6H(2)O). Last, the Rietveld tool is useful for monitoring struvite production from wastewaters, since the chemical ratio (stoichiometry of the phase) is what will define its classification in: struvite, struvite analog, K-struvite or mixed. In addition, it will help in the classification of the fertilizer product (chemical content of nutrients). (C) 2020 The Author(s). Published by Elsevier B.V.	[de Souza Meira, Rose Caldas; Aranha da Paz, Simone Patricia; Martins Correa, Jose Augusto] UFPA Inst Geociencias, Programa Posgrad Geol Geoquim, BR-66075110 Belem, PA, Brazil; [de Souza Meira, Rose Caldas] UFOPA Univ Fed Oeste Para, Inst Ciencias & Tecnol Aguas, BR-68040255 Santarem, PA, Brazil	Universidade Federal do Oeste do Para	Meira, RCD (autor correspondente), UFPA Inst Geociencias, Programa Posgrad Geol Geoquim, BR-66075110 Belem, PA, Brazil.; Meira, RCD (autor correspondente), UFOPA Univ Fed Oeste Para, Inst Ciencias & Tecnol Aguas, BR-68040255 Santarem, PA, Brazil.	rosecsmeira@gmail.com	Correa, José Augusto/HGC-3705-2022		CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior); CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) [Edital MCTIC/CNPq N 28/2018, 429756/2018-6]	CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the Brazilian agencies: CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) for a Ph.D. scholarship to the first author. Funding: This work was supported by CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) for financial support (Edital MCTIC/CNPq N 28/2018, Processo: 429756/2018-6).	Angelica RS, 2018, MINER ENG, V122, P148, DOI 10.1016/j.mineng.2018.03.039; [Anonymous], IOP CONF SER MAT SCI; BANKS E, 1975, INORG CHEM, V14, P1634, DOI 10.1021/ic50149a041; Brasil. Ministerio do Desenvolvimento Regional. 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Mater. Res. Technol-JMRT	NOV-DEC	2020	9	6					15202	15213		10.1016/j.jmrt.2020.10.082	http://dx.doi.org/10.1016/j.jmrt.2020.10.082			12	Materials Science, Multidisciplinary; Metallurgy & Metallurgical Engineering	Science Citation Index Expanded (SCI-EXPANDED)	Materials Science; Metallurgy & Metallurgical Engineering	PQ3DQ		gold			2023-06-23	WOS:000606428400001
J	Filgueiras, BD; de Oliveira, CG; de Sousa, IMC; Cordeiro, P				Filgueiras, Bernardo de Carvalho; de Oliveira, Claudinei Gouveia; Cordeiro de Sousa, Isabela Moreno; Cordeiro, Pedro			Further evidence of Rhyacian arc magmatism in the basement of the Brasilia Belt, western Sao Francisco pericraton	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Goias massif; Artulandia area; Campinorte arc; Brasilia belt; Rhyacian	PLASMA-MASS SPECTROMETRY; CENTRAL BRAZIL; U-PB; TECTONIC EVOLUTION; PALEOPROTEROZOIC CRUST; ESPINHACO SUPERGROUP; TOCANTINS PROVINCE; TRACE-ELEMENT; SOUTH-AMERICA; GUIANA SHIELD	A recently mapped area in central Brazil revealed a slice of Paleoproterozoic basement within Neoproterozoic metasedimentary rocks of the Brasilia Belt. The area, named here the Artulandia area for its proximity to the homonymous village, contains metatonalites and metagranodiorites in tectonic contact with a meta-volcanosedimentary sequence that encompasses felsic, intermediate and mafic metavolcanic rocks interlayered with clastic and chemical metasedimentary rocks. A sample of felsic orthogneiss from the metavolcano-sedimentary sequence, yielded a U-Pb zircon age of 2142 +/- 4.4 Ma, which is interpreted as the crystallization age of the volcanic protolith. Samples from the metagranite unit returned U-Pb zircon ages of 2130 +/- 7.4 Ma for a biotite metatonalite, 2157 +/- 9 for a biotite metagranite, and 2147 +/- 5 Ma for a sulfide-bearing meta-granodiorite, indicating roughly contemporaneous plutonic activity. Whole-rock geochemistry shows calcalkaline signatures for both units, and trace element results are compatible with an extensional setting, such as back-arc or intra-arc, for the metavolcano-sedimentary sequence, and a magmatic arc system for the metagranite unit. These rocks were generated in an episode of juvenile crust formation, as suggested by epsilon(Nd)(2.14Ga) values between 0 and +3.18. Based on lithological association, age and chemical signature, we suggest that the studied rocks represent a lateral continuation of the Campinorte Arc beyond the Rio Maranhao Thrust. Thus, the occurrence of Campinorte Arc rocks on both sides of the thrust argues against the thrust being a Neoproterozoic collisional suture. The geology of the Artulandia area in the context of the Campinorte Arc attests to the complexity of the Rhyacian amalgamation that generated the Sao Francisco Paleocontinent during a Rhyacian Orogeny.	[Filgueiras, Bernardo de Carvalho; de Oliveira, Claudinei Gouveia; Cordeiro de Sousa, Isabela Moreno] Univ Brasilia, Brasilia, DF, Brazil; [Cordeiro, Pedro] Pontificia Univ Catolica Chile, Santiago, Chile	Universidade de Brasilia; Pontificia Universidad Catolica de Chile	de Sousa, IMC (autor correspondente), Univ Brasilia, Brasilia, DF, Brazil.	isabela.sousa@unb.br	Cordeiro, Pedro/E-3044-2017	Cordeiro, Pedro/0000-0003-1996-9551	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work was supported by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES). The University of Brasilia is gratefully acknowledged for fieldwork support and access to laboratory facilities. 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South Am. Earth Sci.	NOV	2020	103								102739	10.1016/j.jsames.2020.102739	http://dx.doi.org/10.1016/j.jsames.2020.102739			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NT3HK					2023-06-23	WOS:000572836100001
J	Jesus, AP; Mateus, A; Benoit, M; Tassinari, CCG; Bento dos Santos, T				Jesus, A. P.; Mateus, Antonio; Benoit, Mathieu; Tassinari, C. C. G.; Bento dos Santos, Telmo			The timing of sulfide segregation in a Variscan synorogenic gabbroic layered intrusion (Beja, Portugal): Implications for Ni-Cu-PGE exploration in orogenic settings	ORE GEOLOGY REVIEWS			English	Article						Beja gabbro; Synorogenic layered intrusion; magmatic sulfides, PGE depletion; Sr-Nd-Pb-S isotopes	MELT DISTRIBUTION COEFFICIENTS; PLATINUM-GROUP ELEMENTS; OSSA-MORENA ZONE; SLAB BREAK-OFF; VOISEYS BAY; ISOTOPIC CONSTRAINTS; CHALCOPHILE ELEMENTS; ULTRAMAFIC ROCKS; OXYGEN BAROMETRY; TIBET PLATEAU	A growing number of magmatic Ni-Cu sulfide deposits discovered in orogenic environments has renewed the interest on this category and reinforced that most orogenic mafic magmas are PGE depleted. The Beja Layered Gabbroic Sequence (LGS) was emplaced during the same Variscan tectono-magmatic event as the Aguablanca Ni-Cu-PGE deposit in Spain, however, no economic mineralization was yet found in LGS. Here we analyze three sulfide ore-showings developed within different environments of LGS that provide a unique frame to assess sulfide segregation in orogenic mafic magmas: the Internal Sulfides hosted at the core of the layered suite, the Marginal Sulfides located at a complex domain where the LGS is intruded by late magmatic anorthosite-tonalitetrondhjemite (ATT) suite and the Sulfide Veins, associated to late magmatic-hydrothermal activity. For this we performed detailed mineralogical (electron probe micro-analysis, enabling to assess integral S-2-T for sulfide equilibrium), whole-rock and isotopic (sulfur and lead) geochemistry for the sulfide occurrences which are further supported by a wide data-set available for LGS and related mesocratic suites. The Internal Sulfides developed under low sulfidation, non-dynamic magmatic conditions, similar to those of the accessory sulfides in LGS gabbros. They segregated from chalcophile depleted melts at the end of a crystal fractionation cycle, without contribution from external sulfur. The Marginal Sulfides have a pyrite-bearing, magmatic sulfide assemblage hosted in exceptionally coarsegrained clinopyroxenites at the LGS SW border. The metal-poor, Sulfide Veins occur within a metasomatic halo adjoining amphibole-albite pegmatoid dykes. The latter two sulfide types share geochemical affinities and re present late-magmatic systems developed during uplift and intrusion by evolved, lower-crustal contaminated magmas. The Marginal Sulfides are mafic precursors of the coeval magmatic-hydrothermal system to which pegmatoid dykes and Sulfide Veins are related. Although estimated primary PGE abundances for LGS magmas are within the range of MORBs, all sulfide types derived from PGE +/- Ni depleted melts due to sulfide segregation during underplating. The presence of deep crustal faults that prevent magma stalling and sulfide sa turation at depth is paramount to generate orogenic magmatic sulfide deposits of economic value.	[Jesus, A. P.; Mateus, Antonio; Bento dos Santos, Telmo] Univ Lisboa FCUL, Inst Dom Luiz, La Fac Ciencias, Ed C6,Piso 3, P-1749016 Lisbon, Portugal; [Mateus, Antonio; Bento dos Santos, Telmo] FCUL, Dept Geol, Ed C6,Piso 4, P-1749016 Lisbon, Portugal; [Benoit, Mathieu] CNRS, Geosci Environm Toulouse Observ Midi Pyrenees GET, 14 Ave Edouard Belin, F-31400 Toulouse, France; [Tassinari, C. C. G.] Univ S Paulo, Inst Geociencias, Sao Paulo, Brazil	Universidade de Lisboa; Universidade de Lisboa; Centre National de la Recherche Scientifique (CNRS)	Jesus, AP (autor correspondente), Univ Lisboa FCUL, Inst Dom Luiz, La Fac Ciencias, Ed C6,Piso 3, P-1749016 Lisbon, Portugal.	ana.jesus@fc.ul.pt	Bento dos Santos, Telmo/F-8075-2012; Mateus, António Manuel/D-3727-2011; Jesus, Ana P/AAC-5232-2022; Jesus, Ana/AAC-7414-2020	Bento dos Santos, Telmo/0000-0003-4589-0222; Mateus, António Manuel/0000-0003-2623-1539; Jesus, Ana P/0000-0001-6258-5890; Jesus, Ana/0000-0001-6258-5890	Fundacao Ciencia Tecnologia (FCT) [POCTI/35630/CTA2000-FEDER, UI: 263, Pest-OE/CTE/UI0263/2011, UID/GEO/50019/2019 -IDL]; IDL [UIDB/50019/2020]; FCT-PhD Grant [SFRH/BD/6355/2001]; Fundação para a Ciência e a Tecnologia [SFRH/BD/6355/2001, PEst-OE/CTE/UI0263/2011] Funding Source: FCT	Fundacao Ciencia Tecnologia (FCT); IDL; FCT-PhD Grant(Fundacao para a Ciencia e a Tecnologia (FCT)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	We dedicate this manuscript to the loving memory of Dr Vitor Oliveira. The analytical support of Iberian Resources (Rio Narcea) Ltd. for a late sampling survey of BRG II Series. Logistic support provided by Centro de Geologia/CREMINER (now IDL) Research Units (FCUL), the analytical support Centro de Pesquisas Geocronologicas (U.S. Paulo) and CNRS Geosciences Environment Toulouse-OMP are deeply acknowledged. Photo credits of hand samples are acknowledged to Prof Fernando Barriga. We would like to thank the reviewers and Ass. Editor Dr Margaux Le Vaillant for the stimulating discussion and their thoughtful suggestions that greatly improved our manuscript; careful handling by Ed. in Chief Dr. Franco Pirajno is also deeply appreciated. AP Jesus thanks W Maier and S Barnes for sharing datasets and common interest in exploring olivine chemistry. The work was supported by Fundacao Ciencia Tecnologia (FCT) through the projects MODELIB (POCTI/35630/CTA2000-FEDER), POCA-PETROLOG (CeGUL, UI: 263; POCTI/FEDER), Pest-OE/CTE/UI0263/2011 and UID/GEO/50019/2019 -IDL. The recent additional backing from the project UIDB/50019/2020 (IDL) is also appreciated. Ana Jesus benefited from an FCT-PhD Grant (SFRH/BD/6355/2001).	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Rev.	NOV	2020	126								103767	10.1016/j.oregeorev.2020.103767	http://dx.doi.org/10.1016/j.oregeorev.2020.103767			26	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	OR0SV					2023-06-23	WOS:000589188900001
J	Klein, EL; Lopes, ECS; Rodrigues, JB; Souza-Gaia, SM; Cordani, UG				Klein, Evandro L.; Lopes, Elem C. S.; Rodrigues, Joseneusa B.; Souza-Gaia, Sulsiene M.; Cordani, Umberto G.			Rhyacian and Neoproterozoic magmatic associations of the Gurupi Belt, Brazil: Implications for the tectonic evolution, and regional correlations	GEOSCIENCE FRONTIERS			English	Article						Neoproterozoic; Paleoproterozoic; Accretionary orogeny; Intracontinental orogeny; West Gondwana; Isotope geology	SAO-LUIS CRATON; WEST-AFRICAN CRATON; NORTHERN BRAZIL; ZIRCON GEOCHRONOLOGY; METAVOLCANIC ROCKS; CRUSTAL EVOLUTION; GREENSTONE-BELT; GEOCHEMICAL CHARACTERISTICS; VOLCANIC-ROCKS; PARNAIBA BASIN	The Gurupi Belt, in north-northeastern Brazil, is a mobile belt developed in the south-southwestern margin of the Sao Luis cratonic fragment and crops out as a tectonic and erosional window within the Phanerozoic cover. Field, petrographic, geochemical, geochronological, and Nd isotopic information (new and published) constrain the timing and types of magmatic associations present in the belt and the tectonic settings in which they formed. The Rhyacian was the main period of magmatic activity, which can be grouped into two main stages. (1) similar to 2185-2130 Ma: pre-collisional, juvenile, calc-alkaline magnesian and calcic ferroan granitoid suites, and minor calc-alkaline and tholeiitic mafic plutonism (now amphibolites), formed in intra-oceanic to transitional/continental arcs; and intra- or back-arc volcano-sedimentary basin. (2) similar to 2125-2070 Ma: syn- (two-mica granites) to late-collisional (potassic to shoshonitic granites and quartz-syenite) plutonic suites produced after crustal thickening and melting, with localized migmatization, that intruded during the compressive D-1 deformational phase and concomitantly with greenschist to amphibolite metamorphism. There is a zonation of the Rhyacian episodes, with intra-oceanic stages occurring to the northeast, and the continental arc and collisional phases occurring to the southwest, indicating the presence of an active continental margin to the southwest, and subduction from NE to SW (present-day configuration). This magmatic framework is a continuation to the south of what is described for the Sao Luis cratonic fragment to the north, and the orogenic scenario is identical to what is observed for the same period in the West African Craton (Eburnean/Birrimian orogen), which additionally supports previous geological correlations. In the Neoproterozoic, a few magmatic occurrences are recognized. An extensional event allowed the intrusion of an anorogenic, nepheline syenite at ca. 730 Ma, which was followed by the intrusion of a crustal, calc-alkaline microtonalite, of uncertain tectonic setting, a 624 Ma. Both intrusions underwent greens-chist to amphibolite facies metamorphism between 580 Ma and 529 Ma. This metamorphic event is probably related to crustal thickening, which produced crustal melting and intrusion of two-mica granites between 595 Ma and 549 Ma. The absence of oceanic and arc-related assemblages, along with geophysical information about the basement of the Phanerozoic cover indicates an intracontinental setting for the Neoproterozoic-Early Cambrian evolution of the Gurupi Belt, with rifting and posterior closure of the basin, without oceanization. Rifting and closure correlate in time with the onset of Rodinia breakup and West Gondwana assembly, respectively, but we interpret the events in the Gurupi Belt as having no direct role in these two global supercontinent-related events, but, instead, as being related to orogenic events occurring in the periphery of the West African and Amazonian cratons at that time.	[Klein, Evandro L.; Rodrigues, Joseneusa B.] Geol Survey Brazil SBN, Quadra 02,Bloco H,Ed Cent Brasilia,1 Andar, BR-70040904 Brasilia, DF, Brazil; [Klein, Evandro L.] Univ Fed Para, PPGG Programa Posgrad Geol & Geoquim, GPGE Grp Pesquisa Geol Econ, Belem, Para, Brazil; [Lopes, Elem C. S.; Souza-Gaia, Sulsiene M.] Geol Survey Brazil, Av Dr Freitas 3645, BR-66095110 Belem, Para, Brazil; [Cordani, Umberto G.] Univ Sao Paulo, Inst Geociencias, Rua Lago,562,Cidade Univ, BR-05508080 Sao Paulo, SP, Brazil	Universidade Federal do Para; Universidade de Sao Paulo	Klein, EL (autor correspondente), Geol Survey Brazil SBN, Quadra 02,Bloco H,Ed Cent Brasilia,1 Andar, BR-70040904 Brasilia, DF, Brazil.	evandro.klein@cprm.gov.br	Klein, Evandro L/G-5973-2012; Gaia, Sulsiene/HTQ-3622-2023; Cordani, Umberto/F-3686-2014	Klein, Evandro L/0000-0003-4598-9249; Gaia, Sulsiene/0000-0002-0679-0643; Cordani, Umberto/0000-0003-4425-5905	Brazilian "Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico" (CNPq) [306798/2016-6]	Brazilian "Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico" (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This paper is mostly an outcome of institutional projects developed by CPRM/Geological Survey of Brazil in the Gurupi Belt, with the additional support of the Brazilian "Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico" (CNPq) to the first author (research grant 306798/2016-6). Kotaro Uchigasaki and Luisa Sousa (CPRM) are thanked for helping with zircon imagery and figures. The authors acknowledge the insightful comments and criticisms of two GSF anonymous reviewers and from the Handing Editor (Nick Roberts), which allowed us to improve the manuscript.	Abreu F.A.M., 1985, 2 S GEOL AM AN, V1, P7; Almeida F., 1976, B I GEOCIENCIAS USP, V7, P45, DOI DOI 10.11606/ISSN.2316-8978.V7I0P45-80; Alvarenga C.J.S., 2000, PARAGUAY ARAGUAIA BE; BETTENCOURT JS, 1991, BRAZIL GOLD 91, P203; Bispo-Santos F, 2014, PRECAMBRIAN RES, V244, P123, DOI 10.1016/j.precamres.2013.08.005; Black LP, 2004, CHEM GEOL, V205, P115, DOI 10.1016/j.chemgeo.2004.01.003; Black LP, 2003, CHEM GEOL, V200, P155, DOI 10.1016/S0009-2541(03)00165-7; Block S, 2016, PRECAMBRIAN RES, V287, P1, DOI 10.1016/j.precamres.2016.10.011; Boynton W.V., 1985, RARE EARTH ELEMENT G, P63, DOI [10.1016/B978-0-444-42148-7.50008-3, DOI 10.1016/B978-0-444-42148-7.50008-3]; BRITO NEVES B. 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J	Lahna, AA; Youbi, N; Tassinari, CCG; Basei, MAS; Ernst, RE; Chaib, L; Barzouk, A; Mata, J; Gartner, A; Admou, H; Boumehdi, MA; Soderlund, U; Bensalah, MK; Bodinier, JL; Maacha, L; Bekker, A				Lahna, Abdelhak Ait; Youbi, Nasrrddine; Gaeta Tassinari, Colombo Celso; Stipp Basei, Miguel Angelo; Ernst, Richard E.; Chaib, Latifa; Barzouk, Abdelhafed; Mata, Joao; Gaertner, Andreas; Admou, Hassan; Boumehdi, Moulay Ahmed; Soderlund, Ulf; Bensalah, Mohamed Khalil; Bodinier, Jean-Louis; Maacha, Lhou; Bekker, Andrey			Revised stratigraphic framework for the lower Anti-Atlas Supergroup based on U-Pb geochronology of magmatic and detrital zircons (Zenaga and Bou Azzer-El Graara inliers, Anti-Atlas Belt, Morocco)	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Morocco; Anti-Atlas Belt; Proterozoic; Lower Anti-Atlas Supergroup; U-Pb geochronology	WEST-AFRICAN CRATON; EAST EUROPEAN CRATON; TRANS-HUDSON-OROGEN; 1380 MA EVENT; TAOUDENI BASIN; VOLCANIC-ROCKS; ICP-MS; TECTONIC EVOLUTION; CRUSTAL EVOLUTION; DRAA INLIER	U-Pb geochronology of magmatic and detrital zircons (Zenaga and Bou Azzer-El Graara inliers, Anti-Atlas Belt, Morocco) and a reassessment of the published constraints suggest a revised stratigraphic framework for the lower Anti-Atlas Supergroup. Five major unconformity-bounded lithostratigraphic packages are here distinguished: the two lower units of Paleoproterozoic age are named the Tasserda-Taghatine Group (2030-1706 Ma) and the Oumoula (Mimount) Formation (ca. 1745-1650 Ma); the third unit of Paleoproterozoic to Neoproterozoic age (ca. 1650 to >883 Ma) is the Tizi n'Taghatine Group; the fourth and fifth units of Neoproterozoic age are the ca. 883 Ma Tachdamt and the ca. 700 Ma Bleida formations. Implications of this revised stratigraphic framework include: 1) the Tasserda-Taghatine Group might be linked to the post-orogenic collapse after the Eburnean Orogeny; 2) the Tizi n'Taghatine Group might be ca. 1.1 Ga in age based on proposed correlation with the Taoudeni Basin succession in Mauritania; 3) the Bleida Formation likely reflects deposition in the foreland basin at the early stage of the Pan-African Orogeny; 4) the Oumoula (Mimount) Formation, Tizi n'Taghatine Group, and Tachdamt Formation potentially record extensional events within the Nuna/Columbia and Rodinia super-continents; 5) the provenance of the lower Anti-Atlas Supergroup (based on our new detrital zircon dating) is mainly from the West African craton along with possible contributions from other cratons such as Amazonia and the Sahara Metacraton; 6) the flood basalt sequence of the Tachdamt Formation likely belongs to the ca. 885-883 Ma intraplate Iguerda-Taifast Large Igneous Province (LIP) event defined by previously dated dykes in the Iguerda and Taifast inliers; and 7) the 1650 Ma Zenaga LIP can be potentially linked with LIP magmatism in Baltica and Laurentia.	[Lahna, Abdelhak Ait; Youbi, Nasrrddine; Chaib, Latifa; Barzouk, Abdelhafed; Admou, Hassan; Boumehdi, Moulay Ahmed; Bensalah, Mohamed Khalil] Cadi Ayyad Univ, Fac Sci Semlalia, Dept Geol, Prince Moulay Abdellah Blvd,POB 2390, Marrakech, Morocco; [Youbi, Nasrrddine; Mata, Joao; Boumehdi, Moulay Ahmed; Bensalah, Mohamed Khalil] Univ Lisbon, Fac Ciencias, Inst Dom Luiz, P-1749016 Lisbon, Portugal; [Gaeta Tassinari, Colombo Celso] Univ Sao Paulo, Inst Geociencias IG, Ctr Pesquisas Geocronol CPGeo, Caixa Postal 11348, BR-05422970 Sao Paulo, SP, Brazil; [Stipp Basei, Miguel Angelo] Univ Sao Paulo, Inst Geociencias IG, Dept Mineral & Geotecton GMG, Rua Lago,562 Cidade Univ, BR-05508080 Sao Paulo, SP, Brazil; [Ernst, Richard E.] Carleton Univ, Dept Earth Sci, 1125 Colonel By Dr, Ottawa, ON K1S 5B6, Canada; [Ernst, Richard E.] Tomsk State Univ, Fac Geol & Geog, 36 Lenin Ave, Tomsk 634050, Russia; [Gaertner, Andreas] Senckenberg Nat Hist Sarnmlungen Dresden, Sekt Geochronol, Museum Mineral & Geol, GeoPlasma Lab, Konigsbracker Landstr 159, D-01109 Dresden, Germany; [Soderlund, Ulf] Lund Univ, Dept Geol, Solvegatan 12, SE-22362 Lund, Sweden; [Soderlund, Ulf] Swedish Museum Nat Hist, SE-11418 Stockholm, Sweden; [Bodinier, Jean-Louis] Mohammed VI Polytech Univ, Geol & Sustainable Min Dept, Hay Moulay Rachid 43150, Ben Guerir, Morocco; [Bodinier, Jean-Louis] Univ Montpellier 2, Geosci Montpellier, Cc 60,Pl Eugene Bataillon, F-34095 Montpellier 05, France; [Maacha, Lhou] Managem Grp, Twin Ctr, Angle Blvd Zerktouni & Al Massira Al Khadra, Casablanca, Morocco; [Bekker, Andrey] Univ Calif Riverside, Dept Earth & Planetary Sci, Riverside, CA 92521 USA; [Bekker, Andrey] Univ Johannesburg, Dept Geol, ZA-2006 Auckland Pk, South Africa	Cadi Ayyad University of Marrakech; Universidade de Lisboa; Universidade de Sao Paulo; Universidade de Sao Paulo; Carleton University; Tomsk State University; Lund University; Swedish Museum of Natural History; Mohammed VI Polytechnic University; Universite de Montpellier; University of California System; University of California Riverside; University of Johannesburg	Lahna, AA (autor correspondente), Cadi Ayyad Univ, Fac Sci Semlalia, Dept Geol, Prince Moulay Abdellah Blvd,POB 2390, Marrakech, Morocco.	abdelhak.aitlahna@ced.uca.ma; youbi@uca.ac.ma; ccgtassi@usp.br; baseimas@usp.br; Richard.Ernst@carleton.ca; latifa_918@yahoo.fr; barzoukabdelhafed@gmail.com; jmata@fc.ul.pt; Andreas.Gaertner@senckenberg.de; admou@uca.ac.ma; boumehdi@uca.ac.ma; Ulf.Soderlund@geol.lu.se; bensalah@uca.ac.ma; JeanLouis.Bodinier@um6p.ma; L.maacha@managemgroup.com; andrey.bekker@ucr.edu	Mata, João/I-3352-2012; Basei, Miguel A S/C-1915-2013; Youbi, Nasrrddine/P-6226-2019; Bensalah, Mohamed Khalil/AAR-2325-2021; Gärtner, Andreas/AAE-9791-2020	Mata, João/0000-0001-5769-7708; Basei, Miguel A S/0000-0002-3857-7089; Youbi, Nasrrddine/0000-0003-3466-2400; Gärtner, Andreas/0000-0002-1670-7305; Boumehdi, Moulay Ahmed/0000-0001-5084-1551; Ait lahna, Abdelhak/0000-0002-3366-3412	Academy Hassan II for Science and Technology; Academy Hassan II for Science and Technology [HIIAST/SDU/2016.02]; Medyna; FCT (Portugal)-CNRST (Morocco); Russian Federation [14.Y26.31.0012]; FCT [UIDB/50019/2020 -IDL]	Academy Hassan II for Science and Technology; Academy Hassan II for Science and Technology; Medyna; FCT (Portugal)-CNRST (Morocco)(Fundacao para a Ciencia e a Tecnologia (FCT)); Russian Federation(Russian Federation); FCT(Fundacao para a Ciencia e a Tecnologia (FCT))	Most of this work was carried out at the Department of Geology of the Faculty of Sciences-Semlalia, Cadi Ayyad University of Marrakech and the "Centro de Pesquisas Geocronologicas (CPGeo), Instituto de Geociencias (IG), Universidade de Sao Paulo-USP, Sao Paulo (SP), Brazil" within the framework of the scientific and technical agreement between the Sao Paulo University and the Cadi Ayyad University (responsibles Colombo Celso Gaeta Tassinari and Nasrrddine Youbi). We acknowledge the Academy Hassan II for Science and Technology for funding studentship for Abdelhak Ait Lahna in 2016-2018. Financial support for this work was also provided by several research projects: (i) the Academy Hassan II for Science and Technology (HIIAST/SDU/2016.02) to Nasrrddine Youbi and co-workers; (ii) Medyna; and (iii) FCT (Portugal)-CNRST (Morocco) to Nasrrddine Youbi and Joao Mata. Richard E. Ernst was partially supported from MegaGrant 14.Y26.31.0012 of the Russian Federation. Joao Mata acknowledges the financial FCT support through project UIDB/50019/2020 -IDL. The Editor Prof. Damien Delvaux is gratefully acknowledged for his comments, patience, and support. We greatly appreciate thoughtful comments of reviewers Prof. David Evans and Dr. Shuan-Hong Zhang that helped to improve the manuscript.	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Afr. Earth Sci.	NOV	2020	171								103946	10.1016/j.jafrearsci.2020.103946	http://dx.doi.org/10.1016/j.jafrearsci.2020.103946			27	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OF4TZ		Green Submitted			2023-06-23	WOS:000581203500011
J	Lorente, FL; Castro, DF; Francisquini, MI; Pessenda, LCR; Fontes, NA; Cohen, MCL; Bendassolli, JA; Piccolo, MD; Macario, K				Lorente, Flavio Lima; Castro, Darcilea Ferreira; Francisquini, Mariah Izar; Ruiz Pessenda, Luiz Carlos; Fontes, Neuza Araujo; Lisboa Cohen, Marcelo Cancela; Bendassolli, Jose Albertino; Piccolo, Marisa de Cassia; Macario, Kita			An integrated analysis of palynofacies and diatoms in the Jucurucu River valley, northeastern Brazil: Holocene paleoenvironmental changes	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Holocene; Palynofacies; Relative sea-level; Diatoms	SEA-LEVEL FLUCTUATIONS; ORGANIC-MATTER; LATE QUATERNARY; FRESH-WATER; SOUTHEASTERN BRAZIL; ESTUARINE MANGROVES; ESPIRITO-SANTO; LAKE; EVOLUTION; SEDIMENTS	This study demonstrates the usefulness of palynofacies as a tool for characterizing the origin, transport, and settling of particulate organic matter preserved in fluvial plain sediments and its integration with diatoms for inferring past depositional environments. Palynofacies, diatoms, and organic geochemistry (S, C/S) data from a sediment core (PR07) collected from the Jucurucu River valley in coastal southern Bahia, northeastern Brazil were used to better understand ecosystem changes that occurred in the region during the last similar to 7.5k years. Elemental values (S: 0.15-5.9%; C/S: 0.12-41.5) suggest marine and fluvial influences in the valley during the Holocene, and organic matter was derived from freshwater and marine phytoplankton. The presence of heterolithic deposits, brackish/marine diatoms, predominance of amorphous group, non-opaque phytoclasts, pyrite crystals, and marine microfossils suggests that a tidal flat formed during a mid-Holocene sea-level highstand. A fluvial plain developed in the last 5k years, due to marine regression and an increase in fluvial sediment supply to the region.	[Lorente, Flavio Lima; Castro, Darcilea Ferreira; Francisquini, Mariah Izar; Ruiz Pessenda, Luiz Carlos; Bendassolli, Jose Albertino; Piccolo, Marisa de Cassia] Ctr Nucl Energy Agr CENA, Ave Centenario 303, BR-13416000 Piracicaba, SP, Brazil; [Fontes, Neuza Araujo; Lisboa Cohen, Marcelo Cancela] Fed Univ Para, Belem, Para, Brazil; [Macario, Kita] Fluminense Fed Univ, Niteroi, RJ, Brazil	Universidade Federal do Para; Universidade Federal Fluminense	Lorente, FL (autor correspondente), Ctr Nucl Energy Agr CENA, Ave Centenario 303, BR-13416000 Piracicaba, SP, Brazil.	flimalorente@yahoo.com.br	Macario, Kita/ADE-6381-2022; Lorente, Flávio Lima/D-4601-2013; Cohen, Marcelo Cancela Lisboa/AAQ-8080-2020; piccolo, marisa de Cássia/D-6149-2012	Cohen, Marcelo Cancela Lisboa/0000-0001-9892-4719; piccolo, marisa de Cássia/0000-0003-2163-5630; Fontes, Neuza/0000-0002-2780-6229; Ruiz Pessenda, Luiz Carlos/0000-0001-9119-8195	Sao Paulo Foundation for Research (FAPESP) [2011/00995-7, 2015/05111-0]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [470210/2012-5, 405060/2013-0]	Sao Paulo Foundation for Research (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was financed by Sao Paulo Foundation for Research (FAPESP), grants 2011/00995-7, and 2015/05111-0, and by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), grants 470210/2012-5 and 405060/2013-0. We gratefully acknowledge Vale Nature Reserve (Linhares, Brazil) for supporting the fieldwork. We also wish to thank Professor Francisca Oboh-Ikuenobe (Missouri University of Science and Technology) for English revision. Reviews from Silvia Grill, Mohamed Zobaa and an anonymous reviewer improved the manuscript.	Andrade ACS, 2002, B PARANAENSE GEOCIEN, V51, P9; Angulo RJ, 2006, QUATERNARY SCI REV, V25, P486, DOI 10.1016/j.quascirev.2005.03.008; [Anonymous], 1999, THESIS; Augustinus P. G., 1995, DEV SEDIMENTOL, V53, P333, DOI DOI 10.1016/S0070-4571(05)80032-9; Batten D. 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NOV	2020	103								102731	10.1016/j.jsames.2020.102731	http://dx.doi.org/10.1016/j.jsames.2020.102731			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NT3HQ					2023-06-23	WOS:000572836700003
J	Garcia, RJL; da Silva, JB; Abreu, IM; Soares, SAR; Araujo, RGO; de Souza, ES; Ribeiro, HJS; Hadlich, GM; Queiroz, AFD				Lorenzo Garcia, Rui Jesus; da Silva Junior, Jucelino Balbino; Abreu, Ilene Matano; Rocha Soares, Sarah Adriana; Oliveira Araujo, Rennan Geovanny; de Souza, Eliane Soares; Severiano Ribeiro, Helio Jorge; Hadlich, Gisele Mara; de Souza Queiroz, Antonio Fernando			Application of PCA and HCA in geochemical parameters to distinguish depositional paleoenvironments from source rocks	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Oil-bearing rock; Rare earth elements; Geochemical parameters; Chemometrics	ORGANIC-MATTER; PETROLEUM; SEDIMENTS; OIL	Oil-producing rocks can be characterized by organic, inorganic and palynological geochemical parameters to assess the quantity and quality of organic matter. In the present study, samples of source rocks collected from different formations (Fm) from the sedimentary basins of the Parnaiba (Pimentairas Formation) and Parana (Irati and Ponta Grossa Formations) were evaluated through the geochemical correlation between the types of organic matter and their different depositional paleoenvironments using chemometric tools. Among the inorganic geochemical parameters used in this evaluation are the concentrations and the diagnostic ratios between the transition elements (Co, Ni, V, and Mo) and internal transition (lanthanides and U). The analysis of the transition and internal transition elements were performed by ICP OES (Ni and V) and ICP MS (Co, Mo, La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Tm, Yb, Lu, and U). The organic geochemical parameters selected for the characterization of the quantity and quality of the organic matter present in the samples of source rocks involved the determination of their total carbon content (%TOC) and sulfur (%1S), of the potential generator (52) the amount of hydrocarbons produced by Rock-Eval pyrolysis and the calculation of the hydrogen (HI) and oxygen (OI) indexes. To compose the matrix of the multivariate analysis (PCA), were used ratios Ni/Co, V/Ni, U/Mo, V/V + Ni, TOC/TS the values of S2, HI, OI and the sum of rare earth elements (REE). The kerogen type, obtained through the HI and OI data, were also included in the matrix, information on the origin of the organic matter, and on the type of depositional paleoenvironment of each sample, obtained from previous works. It was observed the formation of three groups of data characterizing the formations Irati, Ponta Grossa and Pimenteiras according to the type of kerogen and organic matter, and also of its depositional paleoenvironment, showing that the exploratory data analysis allows the obtaining of rapid and efficient information on the chemical similarity between the complex samples from each formation.	[Lorenzo Garcia, Rui Jesus; da Silva Junior, Jucelino Balbino; Hadlich, Gisele Mara; de Souza Queiroz, Antonio Fernando] Fed Univ Bahia UFBA, Inst Geosci, Postgrad Program Geochem Petr & Environm POSPETRO, St Barao de Jeremoabo S-N, BR-40170270 Salvador, BA, Brazil; [Abreu, Ilene Matano; Rocha Soares, Sarah Adriana] Fed Univ Bahia UFBA, LEPETRO Excellence Geochem Oil Energy & Environm, St Barao de Jeremoabo S-N, BR-40170270 Salvador, BA, Brazil; [Oliveira Araujo, Rennan Geovanny] Univ Fed Bahia, Inst Chem, Dept Analyt Chem, Univ Campus Ondina, BR-40170110 Salvador, BA, Brazil; [de Souza, Eliane Soares; Severiano Ribeiro, Helio Jorge] Univ Estadual Norte Fluminense, Ctr Sci & Technol, Lab Engn & Explorat Petr, BR-27925310 Macae, RJ, Brazil	Universidade Federal da Bahia; Universidade Estadual do Norte Fluminense	da Silva, JB (autor correspondente), Fed Univ Bahia UFBA, Inst Geosci, Postgrad Program Geochem Petr & Environm POSPETRO, St Barao de Jeremoabo S-N, BR-40170270 Salvador, BA, Brazil.	jucejr@ufba.br	Queiroz, Antonio Fernando de Souza/ABH-6682-2020; da Silva, Jucelino Balbino/AAA-3611-2021; Abreu, Ilene Matanó/AAB-6052-2021; Hadlich, Gisele/AAO-4708-2020	Souza, Eliane Soares de/0000-0002-9374-3641; OLIVEIRA ARAUJO, RENNAN GEOVANNY/0000-0001-6955-8115; Hadlich, Gisele Mara/0000-0002-6304-0988	BG E & P BRASIL LTDA, SHELL; CAPES [001, PNPD 2311/2011]; CNPq	BG E & P BRASIL LTDA, SHELL; CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank BG E & P BRASIL LTDA, a current SHELL subsidiary, for support and funding in this research; CAPES financial code 001 for the postdoctoral fellowship (PNPD 2311/2011) attached to Jucelino Balbino da Silva Jimior and CNPq for the scholarships and the assistance to foment the research.	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J	Marquetto, L; Kaspari, S; Simoes, JC				Marquetto, Luciano; Kaspari, Susan; Simoes, Jefferson Cardia			Mass and Number Size Distributions of rBC in Snow and Firn Samples From Pine Island Glacier, West Antarctica	EARTH AND SPACE SCIENCE			English	Article						rBC; SP2; size distribution; snow; West Antarctica	BLACK CARBON DEPOSITION; ICE-CORE RECORD; PHYSICAL-PROPERTIES; DUST VARIABILITY; PARTICLES; CLIMATE; AEROSOL; THICKNESS; PLATEAU; PART	An extended-range Single Particle Soot Photometer (SP2) coupled to a Marin-5 nebulizer was used to measure the refractory black carbon (rBC) mass and number size distributions in 1,004 samples from a West Antarctica snow/firn core. The SP2 was calibrated using Aquadag and a Centrifugal Particle Mass Analyzer for BC particles ranging from 0.5 to 800 fg. Our results indicate a significant contribution of rare, large particles of mass-equivalent diameter (D-BC) > 500 nm to the total rBC mass (36%), while small particles (D-BC < 100 nm) are abundant but contribute <8% to total rBC mass. We observed a primary mass median diameter of 162 +/- 40 nm, smaller than reported for snow in other regions of the globe but similar to East Antarctica rBC size distributions. In addition, we observed other modes at 673, 1,040, and >1,810 nm (uncontained mode). We compared two sets of samples from different seasons (wet vs. dry) and observed that dry season concentrations are 3.4 and 2 times that of the wet season in the ranges of 80 nm D-BC < 500 nm (small particles) and 500 nm D-BC < 2,000 nm (large particles), respectively, while number of particles in the dry season is 3.5 and 2 times that of the wet season for the same size ranges. Millimeter thick melt layers have been observed in some samples, although they did not change the observed median diameter. This study provides the first detailed rBC mass and number size distribution from West Antarctica. Plain Language Summary Black carbon (BC) is a particle produced by the incomplete combustion of biomass burning and fossil fuels and plays an important role in the climate system due to its strong light absorption properties. The size of BC particles in snow is important for determining the effects that BC has on the cryosphere and provides insight into the processes controlling BC emission history, transport, and deposition. Past studies indicate spatial differences of BC size distributions in snow, but these studies are limited in number, and more are needed to address this spatial variability. Here the size distribution is presented of BC particles from 1,004 samples from a Pine Island Glacier ice core, West Antarctica, in a region where there is no information of BC particle size in snow. BC in West Antarctica is smaller than other regions of the globe but large, rare particles are also present. These large BC particles are larger than what other studies have reported and could be a result of long-range transport from other continents and/or agglomeration from small particles during transport or deposition.	[Marquetto, Luciano; Kaspari, Susan] Cent Washington Univ, Dept Geol Sci, Ellensburg, WA 98926 USA; [Marquetto, Luciano; Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul, Ctr Polar & Climat, Porto Alegre, RS, Brazil; [Simoes, Jefferson Cardia] Univ Maine, Climate Change Inst, Orono, ME USA	Central Washington University; Universidade Federal do Rio Grande do Sul; University of Maine System; University of Maine Orono	Marquetto, L (autor correspondente), Cent Washington Univ, Dept Geol Sci, Ellensburg, WA 98926 USA.; Marquetto, L (autor correspondente), Univ Fed Rio Grande do Sul, Ctr Polar & Climat, Porto Alegre, RS, Brazil.	luciano.marquetto@gmail.com	Simoes, Jefferson Cardia/D-7232-2013	Simoes, Jefferson Cardia/0000-0001-5555-3401; Kaspari, Susan/0000-0001-5815-2873; Marquetto, Luciano/0000-0003-0943-3729	Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program [200386/2018-2]; CNPq [465680/2014-3, 442761/2018-0]; CAPES project "INCT da Criosfera" [88887.136384/2017-00]; PROANTAR project [88887.314450/2019-00]; Centro Polar e Climatico (CPC/UFRGS)	Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES project "INCT da Criosfera"(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); PROANTAR project; Centro Polar e Climatico (CPC/UFRGS)	This research is part of the Brazilian Antarctic Program (PROANTAR) and was financed with funds from the Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program (no. 200386/2018-2), from the CNPq projects 465680/2014-3 and 442761/2018-0, CAPES project "INCT da Criosfera" 88887.136384/2017-00, and PROANTAR project 88887.314450/2019-00. We thank the Centro Polar e Climatico (CPC/UFRGS) and the Department of Geological Sciences (CWU) faculty and staff for supporting this work. We also thank authors of Khan et al. (2018), Kinase et al. (2019), Ohata et al. (2013), Schwarz et al. (2013), Sinha et al. (2018), and Mori et al. (2019) for data availability and Joshua Schwarz and the two anonymous referees for their expertise and helpful suggestions. We also thank Martin Gysel, Anja Eicher, and Theo Jenk for their comments on internal calibration of the SP2 for snow samples.	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J	Matos, CRL; Berredo, JF; Machado, W; Sanders, CJ; Metzger, E; Cohen, MCL				Matos, Christiene R. L.; Berredo, Jose F.; Machado, Wilson; Sanders, Christian J.; Metzger, Edouard; Cohen, Marcelo C. L.			Carbon and nutrient accumulation in tropical mangrove creeks, Amazon region	MARINE GEOLOGY			English	Article						Blue carbon; Organic matter source; Macrotidal estuary; Creek mudflat; Brazilian Amazon coast	SEDIMENTARY ORGANIC-MATTER; SEA-LEVEL CHANGES; SPARTINA-ALTERNIFLORA; PRESERVATION; NITROGEN; ECOSYSTEMS; ISOTOPES; DYNAMICS; COAST; RECONSTRUCTIONS	The Marapanim River estuary (MRE) is part of the Amazon estuarine system located in northern Brazil, which is characterized as having extensive mangrove forests. Given that previous studies reported CO2 and CH4 fluxes from mangrove creeks in this region, here we investigate the potential organic carbon sequestration of the creek mudflats to get a better understanding of the carbon cycling through these systems. Sediment accumulation rates derived from Pb-210 dating indicated that sampled cores represent the previous 24 (+/- 4) yr. The approximately 24-year total organic carbon (TOC), total nitrogen (TN) and total phosphorus (TP) burial rates were estimated to be 192.5 (+/- 43.5), 15.3 (+/- 4.1) and 3.2 (+/- 0.8) g m(-2) yr(-1), respectively. A binary source mixing model based on carbon stable isotopes (delta C-13) revealed that the sedimentary organic matter (OM) is mainly influenced by marine phytoplankton input (49% to 95%). Furthermore, the TOC accumulation rates found here were slightly higher than the global averages estimated for within mangrove forests, suggesting that these unaccounted carbon sinks along creek mudflat environments are relevant for carbon budgets in mangrove-colonized coastal zones. The highest contents, stocks and accumulation rates were found in the tidal creek sediments that are most influenced by nearby mangroves and are more protected than sediments from major river margins. Our results indicate that the creek mudflats play a major role in carbon and nutrients sequestration, directly related to grain size and OM sources.	[Matos, Christiene R. L.; Cohen, Marcelo C. L.] Univ Fed Para, Programa Posgrad Geol & Geoquim, Belem, Para, Brazil; [Berredo, Jose F.] Museu Paraense Emilio Goeldi MCTIC, Belem, Para, Brazil; [Machado, Wilson] Univ Fed Fluminense, Programa Posgrad Geoquim, Niteroi, RJ, Brazil; [Sanders, Christian J.] Southern Cross Univ, Natl Marine Sci Ctr, Coffs Harbour, NSW, Australia; [Metzger, Edouard] Univ Angers, CNRS LPG BIAF, UMR6112, Lab Bioindicateurs Actuels & Fossiles, Angers, France	Universidade Federal do Para; Universidade Federal Fluminense; Southern Cross University; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite d'Angers	Matos, CRL; Berredo, JF (autor correspondente), Museu Paraense Emilio Goeldi, Av Perimetral 1901, BR-66077830 Belem, Para, Brazil.	christienematos@hotmail.com; berredo@museu-goeldi.br; wmachado@geoq.uff.br; christian.sanders@scu.edu.au; edouard.metzger@univ-angers.fr; mcohen80@hotmail.com	Machado, Wilson/P-8047-2019; Sanders, Christian J/AAM-6906-2021; Cohen, Marcelo Cancela Lisboa/AAQ-8080-2020; Berrêdo, José Francisco/GQY-8383-2022; Matos, Christiene/GQZ-3926-2022	Machado, Wilson/0000-0003-3117-8584; Sanders, Christian J/0000-0003-0090-0896; Cohen, Marcelo Cancela Lisboa/0000-0001-9892-4719; Berrêdo, José Francisco/0000-0002-8590-2462; metzger, edouard/0000-0002-5838-4540	Brazilian Ministry of Education (CAPES); Brazilian Research Council (CNPq); Australian Research Council [DE160100443]; CNRS-EC2CO project Vubleu; Australian Research Council [DE160100443] Funding Source: Australian Research Council	Brazilian Ministry of Education (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Brazilian Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Australian Research Council(Australian Research Council); CNRS-EC2CO project Vubleu; Australian Research Council(Australian Research Council)	The authors thank the research grants from the Brazilian Ministry of Education (CAPES) and Brazilian Research Council (CNPq) to C.R.L. Matos and W. Machado. C.J. Sanders is supported by Australian Research Council (DE160100443) and E. Metzger by CNRS-EC2CO project Vubleu.	Alongi D.M., 2020, SCI, V2, P67, DOI [10.3390/sci2030067, DOI 10.3390/SCI2030057]; Alongi DM, 2014, ANNU REV MAR SCI, V6, P195, DOI 10.1146/annurev-marine-010213-135020; Alongi DM, 1992, TROPICAL MANGROVE EC, V41, P251, DOI [10.1029/ce041p0251, DOI 10.1029/CE041P0251]; [Anonymous], 2018, AGISOFT PHOTOSCAN PR; Appleby P. 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Geol.	NOV	2020	429								106317	10.1016/j.margeo.2020.106317	http://dx.doi.org/10.1016/j.margeo.2020.106317			13	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	NY4KO					2023-06-23	WOS:000576360700019
J	Neto, JMM; Lafon, JM				Milhomem Neto, Joao Marinho; Lafon, Jean-Michel			Crustal growth and reworking of Archean crust within the Rhyacian domains of the southeastern Guiana Shield, Brazil: Evidence from zircon U-Pb-Hf and whole-rock Sm-Nd geochronology	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Zircon U-Pb-Hf isotope data; Rhyacian crustal evolution; Southeastern Guiana Shield; Amazonian Craton	WEST-AFRICAN CRATON; PLASMA-MASS SPECTROMETRY; BAOULE-MOSSI DOMAIN; GA BIRIMIAN OROGEN; LU-HF; CONTINENTAL-CRUST; AMAZONIAN CRATON; ISOTOPIC COMPOSITION; GUINEA IMPLICATIONS; DETRITAL ZIRCONS	The southeastern Guiana Shield, northern Amazonian Craton, is part of a Paleoprotemzoic orogenic belt that was built up during the Transamazonian omgenic cycle (2.26-1.95 Ga). This cycle includes large segments of Rhyacian juvenile crust and some reworked Archean terranes. The geology in this region consists mainly of Paleoprotemzoic granulitic-migmatitic-gneissic complexes, deformed and metamorphosed metavolcanic and metasedimentary rocks, and granitoids (granitic and TTG magmatism). Three tectonic domains are distinguished in the Brazilian territory of the southeastern Guiana Shield. They are known as the Amapa Block, Lourenco Domain, and Carecuru Domain. The Amapa Block is a Meso-Neoarchean continental block that was intensely reworked during the Transamazonian orogeny. The other two domains represent Rhyacian landmasses, the evolution of which involved several stages of subduction of oceanic lithosphere in magmatic arc environments. There are also relics of reworked Archean continental crust, the formation of which was followed by a collisional stage of tectonic accretion of the magmatic arcs. Whole-rock Sm-Nd and U-Pb zircon geochronology have confirmed the juvenile character of much of this Transamazonian omgenic belt. However, for the Lourenco and Carecuru domains, Nd isotopic signatures indicate the participation of Meso-Neoarchean crustal material in the sources of the magmatic rocks. Combined zircon U-Pb and Lu-Hf isotopic analyses by LA-ICP-MS were performed on eleven Rhyacian granitoids and orthogneisses from the Lourenco and Carecuru domains. The aim was to verify the extension of the influence of the Archean continental crust in the adjacent Paleoproterozoic domains. The main magmatic episodes were identified in the Lourenco Domain (similar to 2.17-2.18, 2.14 and 2.12-2.09 Ga) and Carecuru Domain (2.14 Ga) by U-Pb zircon geochronology. The Lu-Hf isotope data point to the predominance of crustal reworking processes (epsilon(Hf(2)(.2-2.1 Ga)) < 0; 67% of zircon crystals) during the formation of Lourenco and Carecuru domains. Hf model ages were found to be mostly Archean (98.4%), even for zircon grains that have positive epsilon(Hf(2)(.2-2.1 Ga)) values. For the terrane at the border of the Lourenco and Carecuru domains with the Amapa Block, assimilation of Archean crust of different ages and proportions in a magmatic arc environment accounts for the Hf-Nd isotopic signatures and Hf model ages of Rhyacian magmatism. In the northwestern part of the Lourenco Domain, more than 100 km north of the Amapa Block, the Hf-Nd isotopic signatures and Hf model ages indicate the participation of Archean crustal material, either as continental fragments and/or through incorporation of continental sediments in island arc environments, similar to what has been recorded for some Birimian terranes of the West African Craton in Ghana.	[Milhomem Neto, Joao Marinho; Lafon, Jean-Michel] Univ Fed Para UFPA, Inst Geociencias IG, Programa Posgrad Geol & Geoquim PPGG, Belem, Para, Brazil; [Milhomem Neto, Joao Marinho; Lafon, Jean-Michel] UFPA, Lab Geol Isotop Iso, IG, Belem, De, Brazil	Universidade Federal do Para; Universidade Federal do Para	Neto, JMM (autor correspondente), Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa 1, BR-66075110 Belem, Para, Brazil.	milhomem@ufpa.br	Jean Michel, Lafon/AAY-6287-2021	Jean Michel, Lafon/0000-0003-0854-3053	Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico (CNPq) [141778/2016-4, 307199/2015-0]; CNPq/Universal Project [485539/2012-8]; Instituto Nacional de Ciencia e Tecnologia de Geociencias da Amazonia (INCT/GEOCIAM) [610010/2009-3]	Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq/Universal Project; Instituto Nacional de Ciencia e Tecnologia de Geociencias da Amazonia (INCT/GEOCIAM)	This paper is part of the PhD dissertation of the first author (JMMN). We express our special thanks to Marcio Pimentel (in memoriam) for his invaluable contribution to the evaluation and interpretations of the results as a member of the PhD defense committee. We acknowledge the Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico (CNPq) for the research scholarship granted to the authors (Grant 141778/2016-4 and 307199/2015-0) and thank the Geological Survey of Brazil Belem Regional Superintendence (CPRM/SUREG-BE) for providing some of the samples. This work was also supported by CNPq/Universal Project (Grant 485539/2012-8) and the Instituto Nacional de Ciencia e Tecnologia de Geociencias da Amazonia (INCT/GEOCIAM; Grant 610010/2009-3). We extend our thanks to the Para-Iso/UFPA team for the technical support during the analytical work. We thank Natalia Hauser and two anonymous reviewers, who provided helpful comments and recommendations. 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South Am. Earth Sci.	NOV	2020	103								102740	10.1016/j.jsames.2020.102740	http://dx.doi.org/10.1016/j.jsames.2020.102740			29	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NS6PI					2023-06-23	WOS:000572380700001
J	Nina, L; Paula-Santos, GM; Sial, AN; Bark, G; Wanhainen, C; Jimenez, G; Blanco, M				Nina, L.; Paula-Santos, G. M.; Sial, A. N.; Bark, G.; Wanhainen, C.; Jimenez, G.; Blanco, M.			Anoxic oceanic conditions during the late Permian mass extinction-evidence from the Chutani formation, Bolivia	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Carbon isotopes; Oxygen isotopes; Permian-triassic boundary; mass extinction	FORMATION TITICACA GROUP; PHOTIC ZONE EUXINIA; CARBON-ISOTOPE; TRIASSIC BOUNDARY; NORTHERN ALTIPLANO; VOLCANIC-ROCKS; SW CHINA; BASIN; OXYGEN; STRATIGRAPHY	We analyze diagenesis of carbonate rocks from the Late Permian Chutani Formation of western Bolivia (San Pablo de Tiquina section) in the southern Lake Titicaca zone, which is a sedimentary succession of semiarid tidal flat comprised of mixed carbonate and siliciclastic units. The diagenetic study includes petrographic analysis (conventional petrography and cathodoluminescence) and geochemical analysis (carbon and oxygen isotopes and minor element chemistry). An integrated study of lithofacies and isotope stratigraphy of carbonates shows a succession of five types of depositional environments: tidal barrier, tidal flat, shoal coastal and shoreface. The Chutani Formation was subjected to different diagenetic processes including micritization, cementation, mechanical compaction, dissolution, neomorphism, dolomitization and dedolomitization that occurred during marine to shallow burial stages. Carbon isotope (delta C-13) values range between -7 and 2.9 parts per thousand (VPDB) with variations linked to stratigraphic changes. The transgressive stage of the basin exhibits an upwards decreasing trend of delta C-13 values whereas regression is marked by an increase in such values. The oxygen isotope values (delta O-18) vary from -16.6 to -1 parts per thousand VPDB with lighter values towards the top of the stratigraphy. The transgressive trend may reflect mixing of meteoric water and/or volcanic-hydrothermal fluids with seawater or progressive oxygenation with enhanced circulation conditions. Heavier values during regression may reflect more evaporitic and anoxic conditions towards the Permian-Triassic boundary. Significant variation in isotope values among neighbouring samples is observed, especially during trangression, which may be the result of different diagenetic processes.	[Nina, L.; Bark, G.; Wanhainen, C.] Lulea Univ Technol, Div Geosci & Environm Engn, S-97187 Lulea, Sweden; [Paula-Santos, G. M.] Univ Estadual Campinas, Inst Geosci, Rua Carlos Gomes 250, Campinas, SP, Brazil; [Sial, A. N.] Univ Fed Pernambuco, Dept Geol, NEG LABISE, Recife, PE, Brazil; [Nina, L.; Blanco, M.] Mayor San Andres Univ, Geol Sci Fac, Inst Geol Res & Environm, La Paz 14500, Bolivia; [Jimenez, G.] Yacimientos Petroliferos Fiscales Bolivianos, La Paz, Bolivia	Lulea University of Technology; Universidade Estadual de Campinas; Universidade Federal de Pernambuco	Nina, L (autor correspondente), Lulea Univ Technol, Div Geosci & Environm Engn, S-97187 Lulea, Sweden.	mabellidia1114@hotmail.com	Sial, Alcides/AAD-1901-2021; Paula-Santos, Gustavo/G-7502-2015	Bark, Glenn/0000-0001-9846-1793; Paula-Santos, Gustavo/0000-0001-9630-1243	Swedish Development Agency (SIDA)	Swedish Development Agency (SIDA)	We thank Dr. Alcides N. Sial of the LaboratOrio Nncleo de Estudos Geoqufmicos-LabotatOrio de IsOtopos Estaveis (NEG-LABISE), Dept. of Geology, Federal University of Pernambuco, Recife, PE, Brazil. This study was supported by the Swedish Development Agency (SIDA). We express our gratitude to the Institute of Geology and Environment (IGEMA).	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South Am. Earth Sci.	NOV	2020	103								102693	10.1016/j.jsames.2020.102693	http://dx.doi.org/10.1016/j.jsames.2020.102693			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NS6NW					2023-06-23	WOS:000572376800001
J	dos Reis, LKO; Vidotti, RM; Cordeiro, P; de Oliveira, CG				Oliveira dos Reis, Luciane Katiuscia; Vidotti, Roberta Mary; Cordeiro, Pedro; de Oliveira, Claudinei Gouveia			The western Sao Francisco pericraton interpreted from crustal magnetic and gravity sources	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Brasilia belt; Goias Massif; Rio maranhao thrust; Matched filtering; Brasiliano Orogeny	NEOPROTEROZOIC BRASILIA BELT; CENTRAL BRAZIL; U-PB; TOCANTINS PROVINCE; TECTONIC EVOLUTION; CONSTRAINTS; GOIAS; ORTHOGNEISSES; AMALGAMATION; COLLISION	The Neoproterozoic Brasiliano Orogeny shaped the former Sao Francisco paleocontinent into a preserved cratonic nucleus surrounded by a pericratonic region. In central Brazil, this pericraton crops out as the Goias Massif, the basement of the northern Brasilia Belt. The well-known difficulty of tracing suture zones on surface led to a longstanding dispute on whether the Rio Maranhao Thrust, a structure separating the Internal Zone and the External Zone of the Brasilia Belt, marked the Brasiliano suture. This interpretation was largely based on regional gravimetric data showing a steep discontinuity at depth, between these zones. However, the Rio Maranhao Thrust separates two pericratonic domains of the Goias Massif (Campinorte Domain and Cavalcante-Arraias Domain), which otherwise share similar Paleoproterozoic ages and geology. To properly address the main structural boundaries within the northern Brasilia Belt, this work was focused on comparing shallow and deep gravity and magnetic data processed as enhanced anomalies and through matched filter analysis. Our results show that the large mafic-ultramafic complexes within the Internal Zone of the Brasilia Belt are masking a smooth gravimetric transition into the External Zone. Additionally, the alleged suture zone is coincident with the Mesoproterozoic rift-related Juscelandia and Palmeiropolis volcano-sedimentary sequences, which have been largely ignored in their role as creating magnetic and gravity suture-like signatures. Along with previous structural and geochronological data, our results argue against the Rio Maranhao Thrust as a suture zone and, instead, support the alternative interpretation of the thrust as an intracontinental feature within a portion of the Sao Francisco pericraton. This pericratonic region, unliked the preserved cratonic core, was widely affected by Mesoproterozoic rifting and Neoproterozoic thick-skinned thrusting. The Rio Parana Thrust, on the other hand, is unnoticeable below 8 km depth in gravity and magnetic data, suggesting thin-skinned tectonics also associated with the Brasiliano Orogeny. Finally, the relative crustal homogeneity from the Sao Francisco craton into the Goias Massif evidenced by our gravity data and confirmed by first- and second-order magnetic lineaments confirms the nature of a pericraton with dominantly NE (N20-40E) trending lineaments. These lineaments were progressively overprinted by Brasiliano NNE (N45-70E) structures from the western margin of the External Zone into the Internal Zone.	[Oliveira dos Reis, Luciane Katiuscia; Vidotti, Roberta Mary; de Oliveira, Claudinei Gouveia] Univ Brasilia, Inst Geociencias, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Cordeiro, Pedro] Pontificia Univ Catolica Chile, Vicuna Mackenna 4860, Santiago 4860, Region Metropol, Chile	Universidade de Brasilia; Pontificia Universidad Catolica de Chile	Vidotti, RM (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil.	lucianekor@gmail.com; roberta@unb.br; pedro.cordeiro@ing.puc.cl; gouveia@unb.br	Cordeiro, Pedro/E-3044-2017; Vidotti, Roberta M/O-8019-2014	Cordeiro, Pedro/0000-0003-1996-9551; Vidotti, Roberta M/0000-0003-1951-3431; Reis, Luciane Katiuscia Oliveira/0000-0003-1462-4618	CNPq (Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico) [304739/2018-9]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]	CNPq (Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors thank the Geological Survey of Brazil (CPRM) for providing the aeromagnetic data. We also thank the Brazilian Institute of Geography and Statistics (IBGE); the Institute of Astronomy, Geophysics, and Atmospheric Sciences of the University of Sao Paulo (IAG/USP), and the Institute of Geosciences of the University of Brasilia (IG/UnB) for allowing the use of ground gravity data. The CNPq (Conselho Nacional de Desenvolvimento Cientffico e TecnolOgico) is acknowledged for grants provided to RMV (process 304739/2018-9) and CGO. Finally, we are grateful for the thorough handling of this submission by Natalia Hauser and Andres Folguera and the contributions of two anonymous reviewers and that of Wolf Uwe Reimold in the final editing. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001.	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NOV	2020	103								102716	10.1016/j.jsames.2020.102716	http://dx.doi.org/10.1016/j.jsames.2020.102716			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NS6OI					2023-06-23	WOS:000572378000003
J	Quadros, MLES; Giustina, MESD; Souza, VS; Scandolara, JE				Quadros, Marcos Luiz E. S.; Giustina, Maria Emilia S. D.; Souza, Valmir S.; Scandolara, Jaime E.			Geology, geochemistry and Sr-Nd isotopes of the Rio Branco Suite, Nova Brasilandia belt in southwest of the Amazon Craton: Evidence of a Rodinia pre-assembly accretionary phase (ca. 1137 and 1106 Ma) during the evolution of the Nova Brasilandia orogeny	LITHOS			English	Article						Rio Branco Suite; Nova Brasilandia belt; Amazon Craton; Sunsas orogen; Geochemistry	OIB-TYPE COMPONENTS; U-PB; TRACE-ELEMENT; SW PART; OPHIOLITES; GEOCHRONOLOGY; LAURENTIA; CLASSIFICATION; SUBDUCTION; HISTORY	The tectonic affinity of the Rio Branco Suite magmatism in the Nova Brasilandia belt, southwest of the Amazon Craton, is important in the understanding of Mesoproterozoic orogenetic events associated with the Rodinia supercontinent pre-assembly. The Rio Branco Suite (ca. 1119-1106 Ma) is composed of coeval mafic-felsic rocks (metagabbro, metatroctolite, massive metabasalt, metadiabase, amphibolite, metagranite, felsic metavolcanic rocks, and metatrondhjemite) exposed as rounded or oval intrusions, sills, and dikes. Whole-rock geochemical data show that the metamafic rocks of the Rio Branco Suite are sub-alkaline, medium- to low Ti tholeitic, with composition and predominant overlay signature of island arc tholeiite and back-arc basin basalt. In multi-element diagrams, the rocks show negative anomalies of Nb and Ta, positive anomalies of Pb, and gradual enrichment in Th relative to Nb and Ta The following features are also present: TiN = 10-50,1.4/Yb = 1.74-12.33 and Th/Yb = 0.10-3.56; low to high CeN (4.12-24.67) ratios; and low-ratios Ce/Pb (3.3-20.5), Nb/U (3.2-16.25), and Th/La (0.01-0.30). All these signatures are characteristic of mafic rocks generated in a subduction environment. Sr-Nd isotope composition showed epsilon Nd with slightly negative to positive values between -2.89 and + 1.66 (t = 1120 Ma) close to CHUR and varied Sr-87/Sr-86 ratios (0.7024-0.7138) and low Nd-143/Nd-144 ratios (similar to 0.51235), suggesting crustal contamination and metasomatism of the mantle wedge. Advanced geological data, such as geochemical and isotopic signatures of the Rio Branco Suite metarnafic component shown in discriminated tectonic diagrams and trace elements diagrams, are considered effective in the diagnosis of subduction. The results demonstrate that the Rio Branco Suite metamafic rocks were generated in an arc-back-arc environment developed by infra-oceanic subduction associated with the accretionary phase of the Nova Brasilandia orogeny between ca. 1137 and 1106 Ma. Published by Elsevier B.V.	[Quadros, Marcos Luiz E. S.] Serv Geol Brasil CPRM, Ave Dr Freitas 3645, BR-66095110 Belem, Para, Brazil; [Giustina, Maria Emilia S. D.; Souza, Valmir S.] Univ Brasilia UnB, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Scandolara, Jaime E.] Serv Geol Brasil CPRM, Setor Bancario Norte, Quadra 02,AN Bloco H,Ed Cent Brasilia, BR-70040904 Brasilia, DF, Brazil	Universidade de Brasilia	Quadros, MLES (autor correspondente), Serv Geol Brasil CPRM, Ave Dr Freitas 3645, BR-66095110 Belem, Para, Brazil.	marcos.quadros@cprm.gov.br	Souza, Valmir/AAL-2767-2021	Souza, Valmir/0000-0002-4957-5951	University of Brasilia-UnB; Geological Survey of Brazil-CPRM (ARIM Nova Brasilandia Project); Coordination for the Improvement of Higher Education Personnel (CAPES)	University of Brasilia-UnB; Geological Survey of Brazil-CPRM (ARIM Nova Brasilandia Project); Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work was supported by the University of Brasilia-UnB, Geological Survey of Brazil-CPRM (ARIM Nova Brasilandia Project), and by the Coordination for the Improvement of Higher Education Personnel (CAPES). The authors are grateful to the Geological Survey of Brazil-CPRM in Porto Velho, Rondonia and Belem cities, for assistance in fieldwork and access to laboratories for the preparation of the samples collected in the field. We also thank the geologists Luciano Castro da Silva, Anderson Alves de Souza, Joseneusa Brilhante Rodrigues and Livio Wagner Chaves Correa for the geological discussions during field activities and office work. We thank the mining technician Maria Rosalva Campos Coelho for her help in the preparation of samples for Sm-Nd and Sr analysis. We thank the CPRM and UnB technicians for their support and performing Sm-Nd and Sr analyses in the laboratory of the Geochronology Centre of the Institute of Geosciences of the University of Brasilia (Geocron-IG/UnB). Constructive revisions of this manuscript by reviewers are acknowledged with thanks.	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J	Ramos, RC; Koester, E; Vieira, DT				Ramos, Rodrigo Chaves; Koester, Edinei; Vieira, Daniel Triboli			Sm-Nd systematics of metaultramafic-mafic rocks from the Arroio Grande Ophiolite (Brazil): Insights on the evolution of the South Adamastor paleo-ocean	GEOSCIENCE FRONTIERS			English	Article						West Gondwana; Brasiliano orogenic cycle; Adamastor ocean	DOM-FELICIANO BELT; CUCHILLA DIONISIO TERRANE; PB-HF ISOTOPES; PAN-AFRICAN; U-PB; GARIEP BELT; CRUSTAL EVOLUTION; BRASILIANO OROGEN; TECTONIC EVOLUTION; MAGMATIC ARC	In this contribution we present new insights on the evolution of the Dom Feliciano Belt, southernmost Mantiqueira Province, integrating new whole-rock Sm-Nd isotopic data for the Arroio Grande Ophiolite (Punta del Este Terrane, Brazil/Uruguay border) with previously published bulk-rock and isotope geochemistry of the South Adamastor paleo-ocean metamafic rocks located in Uruguay (Paso del Dragon Complex, Punta del Este Terrane) and Namibia (Chameis Subterrane, Marmora Terrane, Gariep Belt). For the regional geology, the new data corroborate previous hypothesis and demonstrate the depleted mantle features of the amphibolites and metagabbros of the studied ophiolite. The Arroio Grande Ophiolite rocks are compared with its Uruguayan and Namibian counterparts, demonstrating their isotopic and geochemical similarities and differences, and the backarc affinity of the South Adamastor paleo-ocean. The MORB-affinity amphibolites from the Arroio Grande Ophiolite-Paso del Dragon Complex are, so far, the most juvenile rocks in the eastern sector of the Dom Feliciano Belt, yielding epsilon(Nd(640 Ma)) between +7.3 and +9, and high Sm-147/Nd-144 (>0.169) and Nd-143/Nd-144((640 Ma)) ratios (0.51219-0.51229). The South Adamastor is interpreted in this paper as an internal back-arc ocean, with limited lateral extension, opened at around 750-650 Ma as the result of the closure of the older Charrua-Goianide paleoocean during the Brasiliano/Pan-African orogenic cycle and final configuration of the West Gondwana paleocontinent.	[Ramos, Rodrigo Chaves; Vieira, Daniel Triboli] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, POB 15001, BR-91501970 Porto Alegre, RS, Brazil; [Koester, Edinei] Univ Fed Rio Grande do Sul, Dept Geol, Bento Goncalves Ave 9500, BR-91540000 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Ramos, RC (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, POB 15001, BR-91501970 Porto Alegre, RS, Brazil.	rodrigo.chaves@ufrgs.br; koester@ufrgs.br; daniel.triboli@ufrgs.br	Koester, Edinei/L-3684-2017	Koester, Edinei/0000-0002-4424-4782; Chaves Ramos, Rodrigo/0000-0001-7116-5062	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul [PqG 10/1509-0]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [PQ 305853/2010-4]	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the anonymous reviewers for their insightful comments and suggestions on the manuscript, and the Associate Editor Dr. Vinod Oommen Samuel for editorial handling of this contribution; Andre Neves (Mineracdo Visconde de Maua -Arroio Grande, RS, Brazil) for sharing the location of metaultramafic-metamafic outcrops; Dr. Julia Neri Gezatt (University of Aberdeen, UK) for improving the English writing of the manuscript. Funding: This work was supported by the Fundacdo de Amparo a Pesquisa do Estado do Rio Grande do Sul (Grant No. PqG 10/1509-0) and the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (Grant No. PQ 305853/2010-4).	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J	Ribeiro, BV; Cawood, PA; Faleiros, FM; Mulder, JA; Martin, E; Finch, MA; Raveggi, M; Teixeira, W; Cordani, UG; Pavan, M				Ribeiro, B., V; Cawood, P. A.; Faleiros, F. M.; Mulder, J. A.; Martin, E.; Finch, M. A.; Raveggi, M.; Teixeira, W.; Cordani, U. G.; Pavan, M.			A long-lived active margin revealed by zircon U-Pb-Hf data from the Rio Apa Terrane (Brazil): New insights into the Paleoproterozoic evolution of the Amazonian Craton	PRECAMBRIAN RESEARCH			English	Article						Rio Apa Terrane; Amazonian Craton; Zircon; Hf isotopes; Accretionary orogen; Paleoproterozoic tectonics	PLASMA-MASS SPECTROMETRY; ND ISOTOPIC COMPOSITION; TAPAJOS GOLD PROVINCE; MATO-GROSSO; ACCRETIONARY OROGENS; CRUSTAL EVOLUTION; VILA-RIOZINHO; LU-HF; MAGMATISM; RODINIA	We present the first regional in-situ zircon U-Pb-Hf isotopic data from metaigneous and metasedimentary rocks from the Paleo- to Mesoproterozoic Rio Apa Terrane (RAT), a crustal fragment outcropping in the central-western Brazil and north-eastern Paraguay. These new ages and Hf isotopic data delineate three magmatic events, which record the construction of the temporally and isotopically distinct Western and Eastern Terranes of the RAT. The Western Terrane comprises the 2100-1940 Ma Porto Murtinho Complex and the 1900-1840 Ma Amoguija Belt, which both define a crustal reworking array in epsilon Hf-T-time space evolving from a precursor source with Hf T-DM age of ca. 2700 Ma. The 1800-1720 Ma Caracol Belt constitutes the Eastern Terrane and yields suprachondritic epsilon Hf-T signatures up to + 7.1, indicating significant juvenile input. The metasedimentary Amolar Group and Rio Naitaca Formation in the Western Terrane have maximum depositional ages of 1850-1800 Ma and subchondritic epsilon Hf-T signatures down to - 5.7, similar to the underlying basement of the Amoguij5. Belt. In the Eastern Terrane, the Alto Terere Formation has a maximum depositional age of 1750 Ma and mostly suprachondritic epsilon Hf-T signatures, similar to magmatic rocks of the underlying Caracol Belt. Together, the new igneous and detrital zircon age and Hf isotopic data record a temporal and spatial transition from 2100 to 1840 Ma crustal reworking in the west to more juvenile magmatism at 1800-1720 Ma in the east. This transition is interpreted to reflect convergent margin magmatism associated with periods of subduction zone advance and retreat in an accretionary orogenic setting. Comparison of the epsilon Hf-T time signature of the RAT with the Amazonian Craton suggest penecontemporaneous development, with the Western and Eastern Terranes of the RAT being correlative with the Ventuari-Tapajos and Rio Negro-Juruena Province of the Amazonian Craton, respectively. Our new data also reveal that the epsilon Hf-T signatures of the RAT are distinct from the Maz terrane, which refutes the MARA Block hypothesis.	[Ribeiro, B., V; Cawood, P. A.; Mulder, J. A.; Martin, E.; Finch, M. A.; Raveggi, M.] Monash Univ, Sch Earth Atmosphere & Environm Sci, Clayton, Vic 3800, Australia; [Faleiros, F. M.; Teixeira, W.; Cordani, U. G.] Univ Sao Paulo, Dept Mineral & Geotecton, Rua Lago 562, BR-05508900 Sao Paulo, Brazil; [Pavan, M.] Geol Survey Brazil CPRM, Reg Superintendence Sao Paulo, Rua Costa 55, BR-01304010 Sao Paulo, SP, Brazil	Monash University; Universidade de Sao Paulo	Ribeiro, BV (autor correspondente), 9 Rainforest Walk, Clayton, Vic 3800, Australia.	bruno.vieiraribeiro1@monash.edu; peter.cawood@monash.edu; ffalei@usp.br; jack.mulder@monash.edu; erin.martin@monash.edu; melanie.finch@monash.edu; massimo.raveggi@monash.edu; wteixeir@usp.br; ucordani@usp.br; mauricio.pavan@cprm.gov.br	Vieira Ribeiro, Bruno/HOC-3421-2023; Faleiros, Frederico Meira/F-6138-2010; Martin, Erin/AAO-4678-2021; Cordani, Umberto/F-3686-2014; Silva, Mauricio Pavan/P-6742-2014; Martin, Erin/M-6413-2017	Vieira Ribeiro, Bruno/0000-0002-3652-1831; Faleiros, Frederico Meira/0000-0003-2199-8116; Cordani, Umberto/0000-0003-4425-5905; Silva, Mauricio Pavan/0000-0002-9711-6629; Finch, Melanie/0000-0001-9699-2769; Cawood, Peter/0000-0003-1200-3826; Martin, Erin/0000-0002-6426-3729	Australian Research Council [FL160100168]; Sao Paulo Research Foundation (FAPESP) [2013/12754-0]; co-funded Monash Graduate PhD scholarship; CNPq [307732/2019-3]	Australian Research Council(Australian Research Council); Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); co-funded Monash Graduate PhD scholarship; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This research was financially supported by the Australian Research Council grant FL160100168 to PAC and by the Sao Paulo Research Foundation (FAPESP grant 2013/12754-0 to UGC). BVR was supported by a co-funded Monash Graduate PhD scholarship. FMF was supported by the CNPq research grant 307732/2019-3. We thank Dr. Nicholas Gardiner for the comments on early draft of this manuscript. Two anonymous reviewers are thanked for constructive comments, and the author also thank the Editor Guochun Zhao and Associate Editor Elson Paiva for editorial handling.	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NOV	2020	350								105919	10.1016/j.precamres.2020.105919	http://dx.doi.org/10.1016/j.precamres.2020.105919			21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OR4DS					2023-06-23	WOS:000589423600031
J	Saboia, AM; de Oliveira, CG; Dantas, EL; Cordeiro, P; Scandolara, JE; Rodrigues, JB; de Sousa, IMC				Saboia, Andre Menezes; de Oliveira, Claudinei Gouveia; Dantas, Elton Luiz; Cordeiro, Pedro; Scandolara, Jaime Estevao; Rodrigues, Joseneusa Brilhante; Cordeiro de Sousa, Isabela Moreno			The Siderian crust (2.47-2.3 Ga) of the Goias Massif and its role as a building block of the Sao Francisco paleocontinent	PRECAMBRIAN RESEARCH			English	Article						TTG rocks; Biotite granites and hybrid granitoids; Brasilia Belt; Goias Massif; U-Pb geochronology; Whole-rock geochemistry	U-PB GEOCHRONOLOGY; CENTRAL BRAZIL; PLATE-TECTONICS; TRACE-ELEMENT; PALEOPROTEROZOIC CRUST; MAGMATIC SHUTDOWN; MINEIRO BELT; EVOLUTION; GEOCHEMISTRY; CRATON	The basement of the northern Brasilia Belt, in Central Brazil, is dominated by large volumes of TTG magmatism generated during the Early Paleoproterozoic, and represents a continental block formed prior to the welding of the Sao Francisco paleocontinent during the Rhyacian, holding important information concerning the mechanisms and products of Paleoproterozoic crustal growth and amalgamation. New U-Pb zircon geochronological data was obtained from metagranitoids and mafic-ultramafic intrusions from the Almas-Conceicao do Tocantins Domain (ACTD). This was coupled with geochemical data from the metagranitoids to better constrain the processes of continental crust evolution in this region during the Siderian period. Two main plutonic episodes were recognized in the mapped area: (i) an early suite (2.47 Ga) dominated by tonalites and trondhjemites with subordinate biotite granites (Ribeirao das Areias Complex - RAC); and (ii) a later suite (2.30 Ga) including tonalites and trondhjemites (Ribeirao Itaboca Suite - RIS). Most of the RAC trondhjemite-tonalite-granodiorite (TTG) rocks are marked by fractionated REE patterns with high (La/Yb)(N) = 15-107 and samples have medium to high Sr/Y ratio (28-257). These TTG include both high- and low-Al types and high- and medium-pressure groups. The RIS TTG suite displays higher HREE contents with high (La/Yb)(N) = 65-89 and high Sr/Y ratio (59-95) and contains the high-Al type and the medium pressure group. In spite of the wide age gap between them, both RAC and RIS are characterized by TTG rocks formed in a subduction-like tectonic setting. The biotite granites are related to a magmatic stage after the TTG formation. Mafic rocks of the Gameleira Suite have an abundance of zircon, interpreted as crustal contamination, with dominant (207)pb/(206)pb age populations of 2.48 and 2.30 Ga, and are interpreted to be associated with an extensional magmatic event following the Siderian period. Regional geotectonic correlations within the Sao Francisco Craton based on data compiled from the literature indicate a significant volume of Siderian crust generation that has been overlooked in continental amalgamation models and that TTG magmatism is a more common geochemical signature in Paleoproterozoic rocks than has been previously suggested.	[Saboia, Andre Menezes; Scandolara, Jaime Estevao; Rodrigues, Joseneusa Brilhante] Geol Survey Brazil, Setor Bancario Norte SBN, Quadra 02,Asa Norte,Bloco H, BR-70040904 Brasilia, DF, Brazil; [Saboia, Andre Menezes; de Oliveira, Claudinei Gouveia; Dantas, Elton Luiz; Cordeiro de Sousa, Isabela Moreno] Univ Brasilia, Inst Geociencias, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Cordeiro, Pedro] Pontificia Univ Catolica Chile, Av Vicuna Mackenna 4860, Santiago 4860, Region Metropol, Chile	Universidade de Brasilia; Pontificia Universidad Catolica de Chile	Saboia, AM (autor correspondente), SQN 215,Bloco G,Apartamento 103, BR-70874070 Brasilia, DF, Brazil.	andre.saboia@cprm.gov.br; gouveia@unb.br; elton@unb.br; pedro.cordeiro@ing.puc.cl; jaime.scandolara@cprm.gov.br; joseneusa.rodrigues@cprm.gov.br; isabela.sousa@unb.br	Dantas, Elton Luiz/AAK-8464-2021; Cordeiro, Pedro/E-3044-2017	Dantas, Elton Luiz/0000-0002-7954-5059; Cordeiro, Pedro/0000-0003-1996-9551	CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - Brasil) [305769/2019-7]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; INCT Estudos Tectonicos	CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - Brasil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); INCT Estudos Tectonicos	We thank the Institute of Geosciences of the University of Brasilia (IG/UnB) and the Geological Survey of Brazil (CPRM) for the field work support and the laboratory analysis. The CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - Brasil) is acknowledged for grants provided to CGO (process number 305769/2019-7). We are grateful to Dr. Wilson Teixeira for handling this paper and for the detailed reviews by Dr. Kathryn Cutts and an anonymous reviewer and their valuable suggestions and corrections that helped improve earlier versions of this work. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001 and the INCT Estudos Tectonicos.	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NOV	2020	350								105901	10.1016/j.precamres.2020.105901	http://dx.doi.org/10.1016/j.precamres.2020.105901			19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	OR4DS					2023-06-23	WOS:000589423600049
J	Garcia, MFT; Calderon, M; de Arellano, CR; Herve, F; Opitz, J; Theye, T; Fanning, CM; Pankhurst, RJ; Gonzalez-Guillot, M; Fuentes, F; Babinski, M				Torres Garcia, M. F.; Calderon, M.; Ramirez de Arellano, C.; Herve, F.; Opitz, J.; Theye, T.; Fanning, C. M.; Pankhurst, R. J.; Gonzalez-Guillot, M.; Fuentes, F.; Babinski, M.			Trace element composition of amphibole and petrogenesis of hornblendites and plutonic suites of Cretaceous magmatic arcs developed in the Fuegian Andes, southernmost South America	LITHOS			English	Article						Fuegian Batholith; Ushuaia Pluton; Cretaceous magmatism; Homblendites; Amphibole; Rocas Verdes Basin	MAGALLANES FORELAND BASIN; FIELD STRENGTH ELEMENTS; TIERRA-DEL-FUEGO; PATAGONIAN BATHOLITH; MARGINAL BASIN; EXPERIMENTAL CALIBRATION; ANTARCTIC PENINSULA; TECTONIC EVOLUTION; CORDILLERA DARWIN; CRUSTAL PRESSURES	The evolution of continental crust in convergent margins can be explored in southernmost South America (54-56 degrees S). Plutonic rocks of the Fuegian Batholith and the rear-arc satellite Ushuaia Pluton were emplaced within the magmatic arc and the Fuegian fold-and-thrust belt, respectively. They record subduction zone processes in two distinct tectonic settings during the evolution of the Rocas Verdes Basin. We report new U-Pb zircon geochronology, bulk rock chemistry, Sr-Nd isotope data, and EPMA and in-situ LA-ICP-MS analyses of amphibole from 'hornblendites' and gabbroic-granitoid suites in order to evaluate the origin and evolution of the magmatic plumbing systems in the upper plate of the subduction zone. Textural relationships and amphibole compositions in hornblendite indicate crystallization at lower crustal depths with pressures of 7-8 kbar in the Fuegian Batholith and of 5-6 kbar in the Ushuaia Pluton. Lower Cretaceous suites of hornblendite and talc-alkaline homblendegabbro, diorite and tonalite in the Fuegian Batholith have eNdt values ranging between +2 and +4. They were emplaced within an island arc coeval with mid-oceanic type spreading in the Rocas Verdes back-arc basin. Isotope ratios and amphibole compositions in hornblendite indicate crystallization from primitive and hydrous sub-alkaline basaltic melts with relatively low LREE/HREE and low alkali contents. The Late Cretaceous plutons in the fold-and-thrust belt were emplaced after the tectonic juxtaposition of Rocas Verdes ophiolitic complexes. The Ushuaia Pluton, consisting of clinopyroxene-hornblende cumulates, hornblende-gabbro, diorite and monzodiorite, was emplaced during the waning stage of Late Cretaceous magmatism. In this case hornblendite amphiboles show high contents of alkalis, LREE and incompatible elements with a strong crustal affinity (Th, Ba, Rb). The enriched incompatible trace element patterns indicate their derivation from K-rich transitional magmas formed in supra-subduction settings. Chemical variations in amphibole from homblendites and spatially related plutonic rocks are evaluated in terms of fluid flux from the subducted slab and partial melting of the subarc mantle, ultimately controlled by the thermal state of the subducted slab and convergence rates. (C) 2020 Elsevier B.V. All rights reserved.	[Torres Garcia, M. F.; Calderon, M.; Ramirez de Arellano, C.; Herve, F.] Univ Andres Bello, Carrera Geol, Sazie 2119, Santiago, Chile; [Herve, F.] Univ Chile, Dept Geol, Plaza Ercilla 803, Santiago, Chile; [Opitz, J.; Theye, T.] Univ Stuttgart, Inst Anorgan Chem, Pfaffenwaldring 55, D-70569 Stuttgart, Germany; [Fanning, C. M.] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia; [Pankhurst, R. J.] British Geol Survey, Nottingham NG12 5GG, England; [Gonzalez-Guillot, M.] Consejo Nacl Invest Cient & Tecn, Ctr Austral Invest Cient CADIC, B Houssay 200 V9410BFD, Ushuaia, Argentina; [Gonzalez-Guillot, M.] Univ Nacl Tierra del Fuego, Inst Ciencias Polares Ambiente & Recursos Nat, Fuegia Basquet 251 V9410BFD, Ushuaia, Argentina; [Fuentes, F.] Univ Cent, Fac Ingn, Carrera Geol, Santiago, Chile; [Babinski, M.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562,Cidade Univ, BR-05508080 Sao Paulo, Brazil	Universidad Andres Bello; Universidad de Chile; University of Stuttgart; Australian National University; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad Central de Chile; Universidade de Sao Paulo	Garcia, MFT (autor correspondente), Univ Andres Bello, Carrera Geol, Sazie 2119, Santiago, Chile.	mfernanda.torres.g@gmail.com	Herve, Francisco/HDO-6628-2022; Babinski, Marly/B-9403-2013	Babinski, Marly/0000-0003-2444-2404; Torres Garcia, Fernanda/0000-0002-0212-9778	Fondecyt [1161818]; Anillo Antartico projects [ARTG-04, ACT-105]; NERC [bgs06003] Funding Source: UKRI	Fondecyt(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDECYT); Anillo Antartico projects; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This work was supported by Fondecyt grant 1161818. Several samples were collected during the development of the Anillo Antartico projects ARTG-04 and ACT-105 in which Andres Gomez, Fernando Poblete and Moyra Montes participated. We are grateful to Captain Hugo Cardenas and the crew of the Marypaz II for their support during several field campaigns in the Patagonian fjords. Constructive comments by Michel Gregoire, an anonymous reviewer and Co-Editor-inChief Greg Shellnut helped to significantly improve the manuscript.	Acevedo R. D., 2002, Rev. Asoc. Geol. 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J	Vasconcelos, RN; Lima, ATC; Lentini, CAD; Miranda, GV; Mendonca, LF; Silva, MA; Cambui, ECB; Lopes, JM; Porsani, MJ				Vasconcelos, Rodrigo N.; Cunha Lima, Andre T.; Lentini, Carlos A. D.; Miranda, Garcia, V; Mendonca, Luis F.; Silva, Marcus A.; Cambui, Elaine C. B.; Lopes, Jose M.; Porsani, Milton J.			Oil Spill Detection and Mapping: A 50-Year Bibliometric Analysis	REMOTE SENSING			English	Article						bibliometric analysis; remote sensing; oil slicks; oil detection	SAR; IMPACT	Oil spill detection and mapping (OSPM) is an extremely relevant issue from a scientific point of view due to the environmental impact on coastal and marine ecosystems. In this study, we present a new approach to assess scientific literature for the past 50 years. In this sense, our study aims to perform a bibliometric and network analysis using a literature review on the application of OSPM to assess researchers and trends in this field of science. In methodological terms we used the Scopus base to search for articles in the literature, then we used bibliometric tools to access information and reveal quantifying patterns in this field of literature. Our results suggest that the detection of oil in the sea has undergone a great evolution in the last decades and there is a strong relationship between the technological evolution aimed at detection with the improvement of remote sensing data acquisition methods. The most relevant contributions in this field of science involved countries such as China, the United States, and Canada. We revealed aspects of great importance and interest in OSPM literature using a bibliometric and network approach to give a clear overview of this field's research trends.	[Vasconcelos, Rodrigo N.] Univ Estadual Feira de Santana UEFS, Programa Pos Grad Modelagem Ciencias Terra & Ambi, BR-44036900 Feira De Santana, BA, Brazil; [Cunha Lima, Andre T.; Lentini, Carlos A. D.; Miranda, Garcia, V; Lopes, Jose M.] Univ Fed Bahia UFBA, Inst Fis, Dept Fis Terra & Meio Ambiente, Campus Ondina, BR-40170115 Salvador, BA, Brazil; [Cunha Lima, Andre T.; Lentini, Carlos A. D.; Porsani, Milton J.] Univ Fed Bahia UFBA, Ctr Interdisciplinar Energia & Ambiente CIEnAm, BR-40170115 Salvador, BA, Brazil; [Lentini, Carlos A. D.; Mendonca, Luis F.; Lopes, Jose M.] Univ Fed Bahia UFBA, Inst Geociencias IGEO UFBA, Programa Posgrad Geoquim Petr & Meio Ambiente Pos, BR-40170115 Salvador, BA, Brazil; [Lentini, Carlos A. D.; Porsani, Milton J.] Univ Fed Bahia UFBA, Inst Geociencias IGEO UFBA, Programa Posgrad Geofis, BR-40170115 Salvador, BA, Brazil; [Mendonca, Luis F.] Univ Fed Bahia UFBA, Inst Geociencias, Dept Oceanog, Campus Ondina, BR-40170115 Salvador, BA, Brazil; [Silva, Marcus A.] Univ Fed Pernambuco UFPE Recife, Ctr Tecnol & Geociencias, LITPEG Lab Integrad Tecnol Petr Gas & Biocombusti, Campus Recife, BR-50670901 Recife, PE, Brazil; [Cambui, Elaine C. B.] Univ Fed Bahia UFBA, Inst Biol, Ecol Aplicada, BR-40170115 Salvador, BA, Brazil	Universidade Estadual de Feira de Santana	Vasconcelos, RN (autor correspondente), Univ Estadual Feira de Santana UEFS, Programa Pos Grad Modelagem Ciencias Terra & Ambi, BR-44036900 Feira De Santana, BA, Brazil.	rnvuefsppgm@gmail.com; at.cunhalima@ufba.br; clentini@ufba.br; vivasm@ufba.br; lfelipem@msn.com; marcus@ufpe.br; elainecambui@gmail.com; joseml@ufba.br; porsani@ufba.br	Silva, Marcus André/AAA-7830-2021; Lima, André Telles Cunha/N-9356-2018; Porsani, Milton José/AGH-4521-2022; Mendonça, Luís Felipe/AAV-2445-2020; Silva, Marcus A./B-8500-2013; Lentini, Carlos/C-9284-2013	Lima, André Telles Cunha/0000-0002-5987-2503; Mendonça, Luís Felipe/0000-0001-7836-200X; Lentini, Carlos/0000-0003-0406-1006; Cambui Barbosa, Elaine Cristina/0000-0001-5979-2178; Vasconcelos, Rodrigo/0000-0002-1368-6721; Silva, Marcus/0000-0001-9749-6644; Marques Lopes, Jose/0000-0001-7819-6646	INCT-GP; MCTI/CNPQ/CAPES/FAPS [16/2014, 465517/2014-5]; CNPQ [103189/2020-3, 381139/2020-4, 307828/2018-2, 380653/2020-6, 380671/2020-4, 424495/2018-0, 380652/2020-0]	INCT-GP; MCTI/CNPQ/CAPES/FAPS; CNPQ(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was funded by INCT-GP and MCTI/CNPQ/CAPES/FAPS No 16/2014 process 465517/2014-5, PROGRAMA INCT and additive project entitled "Modeling, remote sensing, and preventive detection of oil/fuel accidents by MCTI/CNPQ/CAPES/FAPS 2019. During this work, the following authors were supported by research fellowship: RNV (CNPQ, process 103189/2020-3), JML (CNPQ, process 381139/2020-4), JGVM (CNPQ, process 307828/2018-2), ATCL (CNPQ, process 380653/2020-6), CADL (CNPQ, process 380671/2020-4), LFM (CNPQ, process 424495/2018-0 and 380652/2020-0).	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NOV	2020	12	21							3647	10.3390/rs12213647	http://dx.doi.org/10.3390/rs12213647			18	Environmental Sciences; Geosciences, Multidisciplinary; Remote Sensing; Imaging Science & Photographic Technology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Remote Sensing; Imaging Science & Photographic Technology	OR3NS		gold			2023-06-23	WOS:000589381100001
J	Verane, J; dos Santos, NCP; da Silva, VL; de Almeida, M; de Oliveira, OMC; Moreira, ITA				Verane, Jessica; dos Santos, Naiara C. P.; da Silva, Veronica L.; de Almeida, Marcos; de Oliveira, Olivia M. C.; Moreira, Icaro T. A.			Phytoremediation of polycyclic aromatic hydrocarbons (PAHs) in mangrove sediments using Rhizophora mangle	MARINE POLLUTION BULLETIN			English	Article						PAHs; Petroleum; Phytoremediation; Mangrove; Rhizophora mangle	OS SANTOS BAY; TOTAL PETROLEUM-HYDROCARBONS; SURFACE SEDIMENTS; METAL CONTAMINATION; PARAGUACU ESTUARY; ECOLOGICAL RISK; SOIL; OIL; L.; RIVER	A phytoremediation experiment was carried out in mesocosms to investigate the performance of Rhizophora mangle in the remediation of polycyclic aromatic hydrocarbons (PAHs) in mangrove sediment contaminated with crude oil. The water pH of the experiments (phytoremediation and natural attenuation) ranged from 4.9 to 8.4 at 0 and 90 days, respectively. The oxy-reduction potential (Eh) ranged from oxidising (108.0 mV, time 0) to reducing (approximately -110.0 mV, time 90) environments. Dissolved oxygen (DO) ranged from 5.7 mg L-1 (time 0) to 4.5 mg L-1 and 3.6 mg L-1 (time 90) in phytoremediation and natural attenuation, respectively. The sediments had silty texture and an average concentration of 5% organic matter (OM). Phytoremediation (60.76%) showed better efficiency in the remediation of the 16 PAHs compared to natural attenuation (49.57%). Principal component analyses showed a correlation between the concentrations of PAHs with pH, Eh, OM and DO in both experiments.	[Verane, Jessica; de Almeida, Marcos; de Oliveira, Olivia M. C.] Fed Univ Bahia UFBA, Geosci Inst, St Barao Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil; [dos Santos, Naiara C. P.; da Silva, Veronica L.; Moreira, Icaro T. A.] Fed Univ Bahia UFBA, Polytech Sch, Dept Environm Engn, St Prof Aristides Novis 2, BR-40170290 Salvador, BA, Brazil		Verane, J (autor correspondente), Fed Univ Bahia UFBA, Geosci Inst, St Barao Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil.; Moreira, ITA (autor correspondente), Fed Univ Bahia UFBA, Polytech Sch, Dept Environm Engn, St Prof Aristides Novis 2, BR-40170290 Salvador, BA, Brazil.	veranelima@yahoo.com.br; icarotam@ufba.br	de Oliveira, Olivia Maria Cordeiro/AAB-3246-2021	MOREIRA, ICARO/0000-0002-3964-7368; Pereira Bomfim, Naiara Cristina/0000-0003-4156-5027; de Almeida, Marcos/0000-0002-9633-1386	CAPES - Brazilian Federal Agency for Support and Evaluation of Graduate Education - Finance [001]	CAPES - Brazilian Federal Agency for Support and Evaluation of Graduate Education - Finance	This study was financed by CAPES - Brazilian Federal Agency for Support and Evaluation of Graduate Education - Finance code 001.	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Pollut. Bull.	NOV	2020	160								111687	10.1016/j.marpolbul.2020.111687	http://dx.doi.org/10.1016/j.marpolbul.2020.111687			11	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	OO8LP	33181957				2023-06-23	WOS:000587626600008
J	Volz, WM; Koester, E; Pinto, VM; Debruyne, D; Cardozo, E; Vieira, DT; Dal Olmo-Barbosa, L; Bastos, VA				Volz, Wesllen Moraes; Koester, Edinei; Pinto, Viter Magalhaes; Debruyne, David; Cardozo, Emanuelle; Vieira, Daniel Triboli; Dal Olmo-Barbosa, Laercio; Bastos, Vivianne Andrade			Geochemistry and U-Pb (SHRIMP) geochronology of Grupelli Granite: New constraints on the cessation of felsic magmatism in the Pelotas Batholith, Dom Feliciano Belt	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Dom Feliciano; Pelotas batholith; Post-collisional; Granite; U-Pb zircon age	LA-PLATA CRATON; DISCRIMINATION; EVOLUTION; COLLISION; GEOLOGY; SERIES; ROCKS; AREA; SR	The Pelotas Batholith forms the eastern portion of the Neoprotemzoic Dom Feliciano Belt and records the final stages of the Neopmterozoic Brazilian-Pan-African orogeny. This granite-dominated belt experienced a complex tectonomagmatic evolution, yet constraints on the nature, and especially, the timing of the different magmatic stages are still scarce. This study provides new geochemical and geochmnological constraints on the Grupelli Granite, a post-deformational pluton located in the rural district of Quilombo, Pelotas, RS. This granite crops out as a series of sub-kilometric solid bodies along a NE-oriented fault zone, intruding the Pinheim Machado Complex that dominates the central and southeastern portion of the Pelotas Batholith. The studied granite is widely used as an ornamental rock due to its extremely leucocratic and isotropic appearance. The Grupelli Granite is homogeneous, relatively undeformed, inequigranular and typically medium-to coarse-grained (1-5 mm), with porphyritic and hypidiomorphic textures. Based on modal mineralogy the rock is a monzogranite with 40-50% quartz, 19-25% K-feldspar, and 15% oligoclase, 3-5% biotite, 2-3% magnetite and ilmenite, and accessory chlorite, zircon, apatite, chalcopyrite, and pyrite. Geochemically, the Grupelli Granite is characterized by high SiO2 (74-77 wt%) and K2O (5.08-5.65 wt%) contents combined with low FeOt (1.71-1.93 wt%), MgO and TiO2 (<0.2 wt%) concentrations. This highly evolved granite has a high-K calc-alkaline affinity, is weakly peraluminous, with I-type fingerprints. The combined data are consistent with formation in a post-tectonic environment by anatexis of mainly calk-alkaline sources, with a potential minor contribution of a metapelitic source. The low Sr-contents and concomitant high Ba/Sr ratios likely reflect plagioclase fractionation, while ilmenite fractionation may account for the pronounced negative Nb, Ta, and Ti anomalies. Although the rare earth element (REE) and other trace element patterns tend to parallel the patterns in the ca. 600 Ma Dom Feliciano Suite and the Cerro Grande Suite magmatism, the Grupelli Granite presents significantly lower heavy REE (HREE) concentrations and a smaller negative Eu anomaly. The HREE depletion can be attributed to retention of garnet in the source. These geochemical characteristics distinguish it from the earlier magmatic pulses in the Pelotas Batholith. The Grupelli Granite yielded a crystallization age of 578 +/- 3.9 Ma (U-Pb zircon SHRIMP), and is thus younger than the ca. 600 Ma Dom Feliciano and Cerro Grande suites. This crystallization age places new constraints on the felsic post-collisional magmatism during the final stages of the evolution of Pelotas Batholith.	[Volz, Wesllen Moraes; Vieira, Daniel Triboli; Dal Olmo-Barbosa, Laercio; Bastos, Vivianne Andrade] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Av Bento Goncalves 9-500, BR-91540000 Porto Alegre, RS, Brazil; [Koester, Edinei] Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9-500, BR-91540000 Porto Alegre, RS, Brazil; [Pinto, Viter Magalhaes; Debruyne, David; Cardozo, Emanuelle] Univ Fed Pelotas, Ctr Engenharias, Engn Geol, Rua Gomes Carneiro, BR-96010610 Pelotas, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal de Pelotas	Pinto, VM (autor correspondente), Univ Fed Pelotas, Ctr Engenharias, Engn Geol, Rua Gomes Carneiro, BR-96010610 Pelotas, RS, Brazil.	viter.pinto@gmail.com	Debruyne, David/AAE-9589-2020; Koester, Edinei/L-3684-2017	Debruyne, David/0000-0002-5896-2742; Koester, Edinei/0000-0002-4424-4782; Andrade Bastos, Vivianne/0000-0002-4460-5285; Dal Olmo-Barbosa, Laercio/0000-0002-2732-8634	CNPq/PQ-2 [307378/2017-9]	CNPq/PQ-2	This research was supported by the following grant: CNPq/PQ-2 (process: 307378/2017-9). This manuscript has benefitted greatly from the contributions of anonymous SAMES reviewers and the editorial handling by dr. Andres Folguera.	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South Am. Earth Sci.	NOV	2020	103								102746	10.1016/j.jsames.2020.102746	http://dx.doi.org/10.1016/j.jsames.2020.102746			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NS6JJ					2023-06-23	WOS:000572365000001
J	Zapata, S; Patino, A; Cardona, A; Parra, M; Valencia, V; Reiners, P; Oboh-Ikuenobe, F; Genezini, F				Zapata, S.; Patino, A.; Cardona, A.; Parra, M.; Valencia, V.; Reiners, P.; Oboh-Ikuenobe, F.; Genezini, F.			Bedrock and detrital zircon thermochronology to unravel exhumation histories of accreted tectonic blocks: An example from the Western Colombian Andes	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article							NORTHERN SIERRAS PAMPEANAS; NORTHWESTERN SOUTH-AMERICA; ARC-CONTINENT COLLISION; FISSION-TRACK; ANNEALING KINETICS; CENTRAL CORDILLERA; SANTANDER MASSIF; FAULT SYSTEM; EVOLUTION; TERRANES	The Northern Andes are the result of multiple tectonic phases, which include extensional and compressional volcanic arcs, strike-slip fragmentation, and accretion of exotic terranes. The alternations of these tectonic settings have overprinted and fragmented the geological record, which has hindered precise paleogeographic and tectonic reconstructions. In the western segment of the Colombian Andes, the oceanic-cored Western Cordillera (WC) and the continental Central Cordillera (CC) are separated by the Romeral Fault Zone (RFZ). This segment of the Andes preserves the record of Cretaceous back-arc extension, the onset of compression, and the accretion of the Caribbean plateau during the Late Cretaceous-Paleocene. To refine the tectonic evolution of the Western Colombian Andes, this study documents new detrital zircon fission-track (ZFT) data from the Meso-Cenozoic sedimentary cover in the CC, the RFZ, and the WC; new ZFT and zircon helium (ZHe) bedrock data from the CC and the RFZ; and new U-Pb detrital data from the Miocene sedimentary cover of the RFZ. Within the RFZ, we obtained bedrock ZFT ages of 239.0 +/- 11.0 Ma and 111.1 +/- 4.3 Ma, and detrital ZFT data from the Abejorral Formation are interpreted as the result of post-magmatic cooling and Cretaceous rifting. Late Cretaceous to Eocene ZFT and ZHe ages (similar to 61-50 Ma) in the CC and detrital ZFT data in the WC record exhumation and deformation of the CC during and after the collision of the Caribbean plateau with the continental margin. Finally, detrital U-Pb and ZFT data from the Amaga Formation record the formation of a Miocene intermountain basin. This study reconstructs the basin geometries and the deformation patterns before, during, and after the collision of the Caribbean plateau with the South American margin. We highlight that in accretionary orogens, in which prolonged deformation and erosion have removed the sedimentary cover, the quantification of differential basement exhumation is key to reconstruct thick-skin deformation and to define major tectonic boundaries.	[Zapata, S.] Smithsonian Trop Res Inst, Balboa, Ancon, Panama; [Zapata, S.; Oboh-Ikuenobe, F.] Missouri Univ Sci & Technol, Dept Geosci & Geol & Petr Engn, Rolla, MO 65409 USA; [Patino, A.; Parra, M.] Univ Sao Paulo, Inst Energy & Environm, Sao Paulo, Brazil; [Cardona, A.] Univ Nacl Colombia, Fac Minas, Dept Proc & Energia, Medellin, Colombia; [Cardona, A.] Univ Nacl Colombia, Grp Invest Geol & Geofis EGEO, Medellin, Colombia; [Valencia, V.] Washington State Univ, Sch Environm, Pullman, WA 99164 USA; [Reiners, P.] Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA; [Genezini, F.] Inst Pesquisas Energet & Nucl, Sao Paulo, Brazil	Smithsonian Institution; Smithsonian Tropical Research Institute; University of Missouri System; Missouri University of Science & Technology; Universidade de Sao Paulo; Universidad Nacional de Colombia; Universidad Nacional de Colombia; Washington State University; University of Arizona; Comissao Nacional de Energia Nuclear (CNEN); Instituto de Pesquisas Energeticas e Nucleares (IPEN)	Zapata, S (autor correspondente), Smithsonian Trop Res Inst, Balboa, Ancon, Panama.	szapatah@gmail.com	Parra, Mauricio/B-7497-2013	Parra, Mauricio/0000-0002-5955-6105; Zapata-Henao (Zapata S.), Sebastian/0000-0003-1213-544X	MST-STRI Bytnar Postdoctoral Fellowship; National University of Colombia [25452, 25340, 29182, 18593, 24208]; Fundacion para la Promocion de la Investigacion y la Tecnologia del Banco de la Republica de Colombia [3451]; Sao Paulo Research Foundation (FAPESP) JP grant [2013-03265-5]	MST-STRI Bytnar Postdoctoral Fellowship; National University of Colombia; Fundacion para la Promocion de la Investigacion y la Tecnologia del Banco de la Republica de Colombia; Sao Paulo Research Foundation (FAPESP) JP grant(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	We acknowledge the support for S. Zapata from the MST-STRI Bytnar Postdoctoral Fellowship. Funding from the National University of Colombia projects 25452, 25340, 29182, 18593, 24208, and the Fundacion para la Promocion de la Investigacion y la Tecnologia del Banco de la Republica de Colombia, project3451, and the Sao Paulo Research Foundation (FAPESP) JP grant 2013-03265-5. Colleagues from the EGEO research group at the National University of Colombia are acknowledged for their discussions. Maria Isabel Marin from EAFIT University (Medellin, Colombia) is acknowledged for allowing access to the Thermochronology Laboratory. German Bayona and Matthias Bernet are acknowledged for their valuable comments during the review of this manuscript.	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South Am. Earth Sci.	NOV	2020	103								102715	10.1016/j.jsames.2020.102715	http://dx.doi.org/10.1016/j.jsames.2020.102715			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NS6NG		Bronze			2023-06-23	WOS:000572375100004
J	Silva, CRE; Silva, EV				e Silva, Camila Rodrigues; Silva-Filho, Emmanoel Vieira			Radon concentration and radiation exposure levels in workplace buildings of downtown Rio de Janeiro City, SE, Brazil	JOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY			English	Article						Indoor radon; Annual effective dose; Potential radon map; Seasonal variation; RAD7	INDOOR RADON; ENVIRONMENTAL RADON; DISEASE; WATER; GAS	Radon, a noble radioactive gas, can reach levels that pose a risk to public health in poorly ventilated environments such as residences and buildings. It is a known carcinogenic agent, responsible for the incidence of about 14% of lung cancer in the world. In this work an evaluation of indoor radon, that downtown Rio de Janeiro workers are exposed in working daily life was carried out using an alpha detector (RAD7). The indoor radon concentration and effective dose are below the limits recommended by international standards.	[e Silva, Camila Rodrigues; Silva-Filho, Emmanoel Vieira] Fluminense Fed Univ, Chem Inst, Postgrad Program Geosci Environm Geochem, Outeiro Sao Joao Batista S-N Ctr, BR-24020141 Niteroi, RJ, Brazil	Universidade Federal Fluminense	Silva, CRE (autor correspondente), Fluminense Fed Univ, Chem Inst, Postgrad Program Geosci Environm Geochem, Outeiro Sao Joao Batista S-N Ctr, BR-24020141 Niteroi, RJ, Brazil.	camilae@id.uff.br	da Silva Filho, Emmanoel Vieira/Y-7281-2019	da Silva Filho, Emmanoel Vieira/0000-0001-6444-6851; Silva, Camila/0000-0002-1063-3333	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; National Council for Research and Development [CNPq 311847/2019-6]; Foundation for Research Support of the State of Rio de Janeiro [FAPERJ E-26/203.037/2017]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council for Research and Development; Foundation for Research Support of the State of Rio de Janeiro	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001. Silva-Filho is a senior researcher of the National Council for Research and Development (CNPq 311847/2019-6) and the Foundation for Research Support of the State of Rio de Janeiro (FAPERJ E-26/203.037/2017).	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Radioanal. Nucl. Chem.	DEC	2020	326	3					1709	1717		10.1007/s10967-020-07463-4	http://dx.doi.org/10.1007/s10967-020-07463-4		OCT 2020	9	Chemistry, Analytical; Chemistry, Inorganic & Nuclear; Nuclear Science & Technology	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Nuclear Science & Technology	PE1YM					2023-06-23	WOS:000584877900003
J	Deininger, M; McDermott, F; Cruz, FW; Bernal, JP; Mudelsee, M; Vonhof, H; Millo, C; Spotl, C; Treble, PC; Pickering, R; Scholz, D				Deininger, Michael; McDermott, Frank; Cruz, Francisco W.; Bernal, Juan Pablo; Mudelsee, Manfred; Vonhof, Hubert; Millo, Christian; Spoetl, Christoph; Treble, Pauline C.; Pickering, Robyn; Scholz, Denis			Inter-hemispheric synchroneity of Holocene precipitation anomalies controlled by Earth's latitudinal insolation gradients	NATURE COMMUNICATIONS			English	Article							HADLEY CIRCULATION; AFRICAN MONSOON; CONCEPTUAL-MODEL; STORM TRACKS; CLIMATE; DYNAMICS; RAINFALL; TEMPERATURE; TERMINATION; FEEDBACKS	Atmospheric circulation is a fundamental component of Earth's climate system, transporting energy poleward to partially offset the latitudinal imbalance in insolation. Changes in the latitudinal distribution of insolation thus force variations in atmospheric circulation, in turn altering regional hydroclimates. Here we demonstrate that regional hydroclimates controlled by the Northern Hemisphere mid-latitude storm tracks and the African and South American Monsoons changed synchronously during the last 10 kyrs. We argue that these regional hydroclimate variations are connected and reflect the adjustment of the atmospheric poleward energy transport to the evolving differential heating of the Northern and Southern Hemispheres. These results indicate that changes in latitudinal insolation gradients and associated variations in latitudinal temperature gradients exert important control on atmospheric circulation and regional hydroclimates. Since the current episode of global warming strongly affects latitudinal temperature gradients through Arctic amplification, our results can inform projections of likely inter-hemispheric precipitation changes in the future. Solar insolation is not equally distributed on the Earth's surface and such imbalances influence the atmospheric circulation. Here, the authors show that latitudinal insolation gradients synchronized the hydroclimate in the Northern mid-latitudes and the African and South American Monsoons throughout the Holocene.	[Deininger, Michael; Scholz, Denis] Johannes Gutenberg Univ Mainz, Inst Geosci, JJ Becher Weg 21, D-55128 Mainz, Germany; [McDermott, Frank] Univ Coll Dublin, Sch Earth Sci, Dublin 4, Ireland; [Cruz, Francisco W.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, Sao Paulo, Brazil; [Bernal, Juan Pablo] Univ Nacl Autonoma Mexico, Ctr Geociencias, Campus UNAM Juriquilla, Queretaro 76230, Mexico; [Mudelsee, Manfred] Climate Risk Anal, Kreuzstr 27, D-37581 Heckenbeck, Bad Gandersheim, Germany; [Mudelsee, Manfred] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bussestr 24, D-27570 Bremerhaven, Germany; [Vonhof, Hubert] Max Planck Inst Chem, Hahn Meitner Weg 1, D-55128 Mainz, Germany; [Millo, Christian] Univ Sao Paulo, Inst Oceanog, Praca Oceanog 191, Sao Paulo, Brazil; [Spoetl, Christoph] Univ Innsbruck, Inst Geol, Innrain 52, A-6020 Innsbruck, Austria; [Treble, Pauline C.] UNSW Sydney, Connected Waters Initiat Res Ctr, Kensington, NSW 2052, Australia; [Treble, Pauline C.] ANSTO, Locked Bag 2001, Kirrawee Dc, NSW 2232, Australia; [Pickering, Robyn] Univ Cape Town, Dept Geol Sci, Univ Ave, ZA-7701 Rondebosch, South Africa; [Pickering, Robyn] Univ Cape Town, Human Evolut Res Inst, ZA-7701 Rondebosch, South Africa	Johannes Gutenberg University of Mainz; University College Dublin; Universidade de Sao Paulo; Universidad Nacional Autonoma de Mexico; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Max Planck Society; Universidade de Sao Paulo; University of Innsbruck; University of New South Wales Sydney; Australian Nuclear Science & Technology Organisation; University of Cape Town; University of Cape Town	Deininger, M (autor correspondente), Johannes Gutenberg Univ Mainz, Inst Geosci, JJ Becher Weg 21, D-55128 Mainz, Germany.	michael.deininger@uni-mainz.de	Millo, Christian/I-7602-2013; Cruz, Francisco W/G-6059-2012; Mudelsee, Manfred/C-6063-2018; Scholz, Denis/G-1861-2016; Bernal, Juan Pablo/I-8012-2012; McDermott, Frank/F-3096-2010	Millo, Christian/0000-0002-7651-4679; Mudelsee, Manfred/0000-0002-2364-9561; Scholz, Denis/0000-0002-0055-8915; Bernal, Juan Pablo/0000-0001-8363-572X; Deininger, Michael/0000-0002-4930-4908; McDermott, Frank/0000-0001-7037-7936; Pickering, Robyn/0000-0002-2663-7574; Vonhof, Hubert/0000-0002-0897-8244; Treble, Pauline/0000-0002-1969-8555; Spotl, Christoph/0000-0001-7167-4940	German Research Foundation (DFG) [DE 2398/3-1]; Irish Research Council [GOIPD/2015/789]	German Research Foundation (DFG)(German Research Foundation (DFG)); Irish Research Council(Irish Research Council for Science, Engineering and Technology)	M.D. thanks Augusto Mangini, Norbert Frank and Yuval Burstyn for comments on an earlier version of this manuscript. M.D. acknowledges funding by the German Research Foundation (DFG) grant DE 2398/3-1. F.M.D. acknowledges funding from the Irish Research Council through grant GOIPD/2015/789.	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Commun.	OCT 28	2020	11	1							5447	10.1038/s41467-020-19021-3	http://dx.doi.org/10.1038/s41467-020-19021-3			9	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	OP4OD	33116129	Green Published, gold			2023-06-23	WOS:000588060400004
J	Ferreira, RD; Dias, FD; Tannus, CD; Santana, FB; dos Santos, DCMB; Dias, FD; de Castro, MS; Brandao, HN; Santos, FD; Silva, LCRCE; Chinalia, FA				da Cruz Ferreira, Rodrigo; de Souza Dias, Fernanda; de Aragao Tannus, Caroline; Santana, Filipe Barbosa; dos Santos, Daniele Cristina Muniz Batista; de Souza Dias, Fabio; de Castro, Marina Siqueira; Brandao, Hugo Neves; de Freitas Santos Junior, Anibal; Silva, Lidercia Cavalcanti Ribeiro Cerqueira e; Chinalia, Fabio Alexandre			Essential and Potentially Toxic Elements from Brazilian Geopropolis Produced by the Stingless Bee Melipona quadrifasciata anthidioides Using ICP OES	BIOLOGICAL TRACE ELEMENT RESEARCH			English	Article						Geopropolis; Trace elements; Microwave-assisted acid digestion; ICP OES; Exploratory analysis	OPTICAL-EMISSION SPECTROMETRY; HUMAN HEALTH; PROPOLIS; HONEY; SAMPLES; CONTAMINATION; SCUTELLARIS; METALS; PLANTS; ZINC	Melipona quadrifasciata anthidioides is a species of stingless bee popularly known in Brazil as "mandacaia". Products derived from bees for food and therapeutic uses, have stimulated the evaluation of the chemical composition of geopropolis. Concentrations of 24 essential and potentially toxic elements were determined in geopropolis samples, using a sequential optical emission spectrometer with inductively coupled plasma (ICP OES) after microwave-assisted acid digestion. Principal component analysis (PCA) and Hierarchical cluster analysis (HCA) were used to carry out an exploratory analysis of the samples. The following elements were quantified (in mg Kg(-1)): Al (320,414.40-36,911.1), As (<LoQ-4.37), Ba (38.36-211.11), Ca (672.38-94,527), Co (<LoQ-14.12), Cr (17.41-38.07), Cu (10.63-28.73), Fe (21,973.96-11,536.47), K (1974.38-9198.91), Mg (1961.17-7481.79), Mn (50.51-310.51), Na (154.55-340.46), Ni (2.28-21.74), P (16.59-51.07), Pb (3.45-8.55), Sb (<LoQ-1.64), Se (<LoQ-1.01), Sn (4.92-16.14), Sr (9.21-36.29), V (28.77-78.73) and Zn (24.34-50.31). Cd and Mo were found to be below the limit of detection (LoD) and quantification (LoQ) values of ICP OES in all investigated samples. Geopropolis can be a potential source of macro- and microelements for colonies and products derived from these bees for human consumption, contributing to their geographical origin and quality control, besides being an indicator of environmental monitoring.	[da Cruz Ferreira, Rodrigo; Silva, Lidercia Cavalcanti Ribeiro Cerqueira e; Chinalia, Fabio Alexandre] Univ Fed Bahia, Inst Hlth Sci, BR-40110100 Salvador, BA, Brazil; [de Souza Dias, Fernanda; de Aragao Tannus, Caroline; de Freitas Santos Junior, Anibal] Univ Estado Bahia, Dept Life Sci, BR-41195001 Salvador, BA, Brazil; [Santana, Filipe Barbosa; dos Santos, Daniele Cristina Muniz Batista] Univ Fed Bahia, Chem Inst, BR-40170115 Salvador, BA, Brazil; [de Souza Dias, Fabio] Univ Fed Bahia, Sci Technol & Innovat Inst, BR-42809000 Camacari, BA, Brazil; [de Castro, Marina Siqueira] Univ Estadual Feira de Santana, Dept Biol Sci, BR-44036900 Feira De Santana, BA, Brazil; [Brandao, Hugo Neves] Univ Estadual Feira de Santana, Dept Hlth, BR-44036900 Feira De Santana, BA, Brazil	Universidade Federal da Bahia; Universidade do Estado Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Estadual de Feira de Santana; Universidade Estadual de Feira de Santana	Santos, FD (autor correspondente), Univ Estado Bahia, Dept Life Sci, BR-41195001 Salvador, BA, Brazil.	afjunior@uneb.br	Dias, Fabio/ABB-1905-2020; 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Trace Elem. Res.	SEP	2021	199	9					3527	3539		10.1007/s12011-020-02455-7	http://dx.doi.org/10.1007/s12011-020-02455-7		OCT 2020	13	Biochemistry & Molecular Biology; Endocrinology & Metabolism	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Endocrinology & Metabolism	TE2TW	33094450				2023-06-23	WOS:000581597100001
J	Appolinario, LR; Tschoeke, D; Calegario, G; Barbosa, LH; Moreira, MA; Albuquerque, ALS; Thompson, CC; Thompson, FL				Appolinario, Luciana R.; Tschoeke, Diogo; Calegario, Gabriela; Barbosa, Luiz Henrique; Moreira, Manuel A.; Albuquerque, Ana Luiza S.; Thompson, Cristiane C.; Thompson, Fabiano L.			Oil leakage induces changes in microbiomes of deep-sea sediments of Campos Basin (Brazil)	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Marine sediments; Metagenomics; Oil biodegradation; Campos basin; Microbial diversity	BIODEGRADATION; HYDROCARBONS; QUALITY	The Campos Basin (100,000 km(2)) is located on the continental shelf of southeastern Brazil. Despite the significant oil and gas industrial activities underway in the Campos Basin, scarce information is available regarding the hydrocarbon contents and microbial communities in the deep-sea sediments. To gain new insights on these aspects, we first obtained deep-sea sediment samples with different degrees of oil exposure. We obtained samples from a seabed fissure (N = 28), surroundings (250 m to 500 m from the fissure: N = 24), and a control area (N = 4).We used shotgun metagenomics to characterize the taxonomic and metabolic diversity and analyzed biogeochemical parameters (metal and oil concentration) of all samples. The high levels of unresolved complex mixture of hydrocarbons in the fissure indicate a potentially recent petrogenic contribution in these sediments. The fissure area was found to have a higher abundance of hydrocarbonoclastic bacterial genera and hydrocarbon degradation genes. These bacteria may be used as biosensors of sediment contamination. The effects of oil contamination, mainly around the fissure, are less clear at 250 m and 500 m. suggesting that the surroundings may not have been heavily affected by the oil leakage. Our study demonstrates that metagenomics can disclose biosensors for environmental monitoring. (C) 2020 Elsevier B.V. All rights reserved.	[Appolinario, Luciana R.; Tschoeke, Diogo; Calegario, Gabriela; Barbosa, Luiz Henrique; Thompson, Cristiane C.; Thompson, Fabiano L.] Univ Fed Rio de Janeiro UFRJ, Inst Biol, Lab Microbiol, Rio De Janeiro, Brazil; [Tschoeke, Diogo] Univ Fed Rio de Janeiro, Ctr Technol & Biomed Engineer Program COPPE, Rio de Janeiro, Brazil; [Thompson, Fabiano L.] Univ Fed Rio de Janeiro UFRJ, Ctr Technol CT2, SAGE COPPE, Rio De Janeiro, Brazil; [Moreira, Manuel A.; Albuquerque, Ana Luiza S.] Univ Fed Fluminense UFF, Programa Posgrad Geoquim, Niteroi, RJ, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal Fluminense	Thompson, FL (autor correspondente), Univ Fed Rio de Janeiro UFRJ, Inst Biol, Lab Microbiol, Rio De Janeiro, Brazil.	thompsoncristiane@gmail.com	Tschoeke, Diogo A/F-9913-2019; Tschoeke, Diogo/AAB-4739-2021; Albuquerque, Ana Luiza S/C-5167-2013	Tschoeke, Diogo A/0000-0001-8134-4259; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Thompson, Fabiano/0000-0002-7562-1683	Brazilians funding agency CNPq; Brazilians funding agency FAPERJ; Coordenacao de Aperfeicoamento de Pessoal deNivel Superior - Brasil (CAPES) [001]; PetroRio	Brazilians funding agency CNPq; Brazilians funding agency FAPERJ; Coordenacao de Aperfeicoamento de Pessoal deNivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); PetroRio	The authors thank the Brazilians funding agencies CNPq and FAPERJ for funding. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal deNivel Superior - Brasil (CAPES) - Finance Code 001, and PetroRio. The present study is part of the Ph.D. thesis of LRA.	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Total Environ.	OCT 20	2020	740								139556	10.1016/j.scitotenv.2020.139556	http://dx.doi.org/10.1016/j.scitotenv.2020.139556			9	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	ND7CF	32554026				2023-06-23	WOS:000562059800012
J	Cotovicz, LC; Vidal, LO; de Rezende, CE; Bernardes, MC; Knoppers, BA; Sobrinho, RL; Cardoso, RP; Muniz, M; dos Anjos, RM; Biehler, A; Abril, G				Cotovicz Jr, Luiz C.; Vidal, Luciana O.; de Rezende, Carlos Eduardo; Bernardes, Marcelo C.; Knoppers, Bastiaan A.; Sobrinho, Rodrigo L.; Cardoso, Renan P.; Muniz, Marcelo; dos Anjos, Roberto Meigikos; Biehler, Antoine; Abril, Gwenael			Carbon dioxide sources and sinks in the delta of the Paraiba do Sul River (Southeastern Brazil) modulated by carbonate thermodynamics, gas exchange and ecosystem metabolism during estuarine mixing	MARINE CHEMISTRY			English	Article						Carbon dioxide; Carbonate chemistry; Thermodynamics; Tropical coastal deltas; Land-ocean continuum; Mangroves	DISSOLVED INORGANIC CARBON; RIO-DE-JANEIRO; ATMOSPHERIC CO2; FRESH-WATER; ORGANIC-CARBON; SPATIAL VARIABILITY; COASTAL WATERS; ATLANTIC-OCEAN; MASS-BALANCE; WIND-SPEED	Tropical estuarine deltas generally present poorly buffered waters in their freshwaters. Carbonate chemistry predicts that mixture of such warm freshwater with seawater will create rapid consumption of the freshwater carbon dioxide (CO2) by the carbonate buffering capacity of the seawater. In this study, we used the Paraiba do Sul River as a laboratory to investigate how thermodynamics compare with biological processes, gas exchange, and tidal advection from mangrove. We conducted three spatial surveys covering the salinity gradient of the main channel and surrounding mangrove waters and one 24-h mooring in a mangrove creek. In the main channel, dissolved inorganic carbon (DIC) and total alkalinity (TA) showed closely conservative distribution along the salinity gradient, increasing seaward. The partial pressure of CO2 (pCO(2)) followed a bell-shaped curve predicted by carbonate chemistry for conservative mixing of river and ocean endmembers. During high river flow, pCO(2) sharply decreased between salinities 0 and 5 (1800 to 390 ppmv), a pCO(2) drawdown attributed to riverine outgassing and thermodynamics. Indeed, the mixing of TA-poor freshwater (363 +/- 16 mu mol kg(-1)) with TA-rich seawater creates a deficit of dissolved CO2 not related to biotic processes. During low river flow, the entire mixing zone was undersaturated in pCO(2) with an increasing trend seaward. However, observed pCO(2) values were slightly above those predicted by conservativity. Approximately half of this deviation was attributed to biological activity (net heterotrophy), and remaining deviation was assigned to the effects of gas exchange (18%) and water heating (36%). The effect of gas exchange was higher in fresh and low salinity waters, reflecting the higher outgassing/ingassing of CO2, and lower buffering capacity. Water heating was more important in mid- to high-salinities as a result of diel patterns of solar irradiance. Heterotrophy was slight and not able to outcompete thermodynamics and generate outgassing during estuarine mixing. Consistently, stable isotopic signatures of DIC (delta C-13-DIC) presented slight deviations below the conservative mixing, corroborating net heterotrophy in the main channel. Areas of CO2 uptake due to phytoplankton activity were identified but restricted to the freshwater endmember during low river flow, with lowest pCO(2) (up to 41 ppmv) and the highest chlorophyll a (up to 21.3 mu g L-1). The estuary was a CO2 sink during low river flow ( - 1.34 to -5.26 mmolC m(-2) d(-1)) and a source during high river flow (5.71 to 19.37 mmolC m(-2) d(-1)). In the mangrove creek, the pCO(2), DIC, delta C-13-DIC and TA presented deviations from the conservativity, with slopes between TA and DIC demonstrating organic carbon degradation mediated by aerobic respiration and sulphate reduction. Mangrove creek waters were a CO2 source (average of 134.81 mmolC m(-2) d(-1)), exhibiting high values of pCO(2) (up to 21,720 ppmv). The results reveal that the low buffering capacity in the main channel of tropical estuarine deltas can be the predominant driver of pCO(2), generating CO2 undersaturation along the mixing zone, a process overlooked in estuarine systems. Moreover, air-water CO2 exchange, thermal variability, and biological activities contribute to deviation of the carbonate system from conservative mixing in specific estuarine areas, also modulating pCO(2) variability.	[Cotovicz Jr, Luiz C.; Bernardes, Marcelo C.; Knoppers, Bastiaan A.; Sobrinho, Rodrigo L.; Abril, Gwenael] Univ Fed Fluminense, Programa Geoquim, Niteroi, RJ, Brazil; [Cotovicz Jr, Luiz C.] Univ Fed Ceara, Inst Ciencias Mar LABOMAR, Fortaleza, Ceara, Brazil; [Vidal, Luciana O.; de Rezende, Carlos Eduardo] Univ Estadual Norte Fluminense, Ctr Biociencias & Biotecnol, Lab Ciencias Ambientais, Campos Dos Goytacazes, RJ, Brazil; [Cardoso, Renan P.; Muniz, Marcelo; dos Anjos, Roberto Meigikos] Univ Fed Fluminense, Inst Fis, Lab Radioecol & Alteracoes Ambientais, Niteroi, RJ, Brazil; [Biehler, Antoine] Univ Quebec Rimouski, Boreas Grp North Syst, Quebec Ocean, Canada Res Chair Geochem Coastal Hydrogeosyst, Rimouski, PQ, Canada; [Abril, Gwenael] UA, UCN, SU,CNRS,Museum Natl Hist Nat, IRD,Biol Organismes & Ecosyst Aquat BOREA,UMR 720, Paris, France	Universidade Federal Fluminense; Universidade Federal do Ceara; Universidade Estadual do Norte Fluminense; Universidade Federal Fluminense; University of Quebec; Universite du Quebec a Rimouski; UDICE-French Research Universities; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Museum National d'Histoire Naturelle (MNHN)	Cotovicz, LC (autor correspondente), Univ Fed Ceara, Inst Ciencias Mar LABOMAR, Fortaleza, Ceara, Brazil.	lcc.junior@gmail.com	Bernardes, Marcelo/H-7869-2012; Knoppers, Bastiaan/AAK-2311-2021; Abril, Gwenaël/C-7835-2011; Biehler, Antoine/AFM-0031-2022; de Rezende, Carlos Eduardo/I-1893-2015; Vidal, Luciana de Oliveira/V-4819-2019; dos Anjos, Roberto Meigikos/P-8055-2014	Bernardes, Marcelo/0000-0002-4338-4353; Abril, Gwenaël/0000-0002-4914-086X; dos Anjos, Roberto Meigikos/0000-0003-3314-8602; Vidal, Luciana/0000-0001-5065-0835	Laboratory of Environmental Sciences; Graduate Program in Ecology and Natural Resources of the State University of Norte Fluminense Darcy Ribeiro; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) [001]; Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [E-26/202.785/2016]; FAPERJ [E-26202.785/2016, E-26/202.916/2017, 210.883/2016]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [305217/2017-8]; CNPq [301572/2010-0]; CAPES [88882.314551/2019-01]; International Research Project VELITROP (Vulnerability of littoral tropical ecosystems to eutrophication) - French Institute of Environment and Ecology INEE-CNRS	Laboratory of Environmental Sciences; Graduate Program in Ecology and Natural Resources of the State University of Norte Fluminense Darcy Ribeiro; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); International Research Project VELITROP (Vulnerability of littoral tropical ecosystems to eutrophication) - French Institute of Environment and Ecology INEE-CNRS	The authors are grateful for the support from the Laboratory of Environmental Sciences and to the Graduate Program in Ecology and Natural Resources of the State University of Norte Fluminense Darcy Ribeiro. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brazil (CAPES)-Finance Code 001, and by the Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ; proc. no. E-26/202.785/2016). Luiz C. Cotovicz Jr. is a postdoctoral researcher of the FAPERJ (proc. no. E-26202.785/2016). Carlos E. Rezende thanks the financial support of Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (305217/2017-8) and FAPERJ (E-26/202.916/2017 and 210.883/2016). B.A. Knoppers is a senior scientist of CNPq (proc. no. 301572/2010-0). Luciana O. Vidal is a postdoctoral researcher of CAPES (proc. no. 88882.314551/2019-01). This research was also conducted with the support of the International Research Project VELITROP (Vulnerability of littoral tropical ecosystems to eutrophication) funded by the dFrench Institute of Environment and Ecology INEE-CNRS.	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Chem.	OCT 20	2020	226								103869	10.1016/j.marchem.2020.103869	http://dx.doi.org/10.1016/j.marchem.2020.103869			22	Chemistry, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Oceanography	OC2OZ		Green Submitted			2023-06-23	WOS:000579000900001
J	Albuquerque, MFD; Horbe, AMC; Danisik, M				dos Santos Albuquerque, Marcio Fernando; Coimbra Horbe, Adriana Maria; Danisik, Martin			Episodic weathering in Southwestern Amazonia based on (U-Th)/He dating of Fe and Mn lateritic duricrust	CHEMICAL GEOLOGY			English	Article						(U-Th)/He; Goethite; Hollandite; Lateritic duricrust; Weathering	GEOCHRONOLOGICAL CONSTRAINTS; LANDSCAPE EVOLUTION; MANGANESE DEPOSITS; WESTERN-AUSTRALIA; BAUXITE DEPOSITS; ANDEAN TECTONICS; COSMOGENIC HE-3; IRON DEPOSITS; 40AR/39AR; GEOCHEMISTRY	This study presents the results of mineralogical analysis and (U-Th)/He dating of micrometric grains of hematite, goethite, cryptomelane and hollandite from six samples of bauxite, Fe, Mn, Mn-Al-Fe, Mn-Al and Mn-Al-P duricrusts located in southwestern Amazonia (Brazil). The samples were collected at different elevations to constrain temporal epochs of lateritization and to provide insights into the cratonic landscape evolution of Proterozoic and Paleozoic terrains in Brazil. Three main phases of duricrust formation were recognized, indicating a long period of lateritic weathering: The first phase, preserved as a fragment in Fe duricrust on the Paleozoic sedimentary rocks, began in the Permian (similar to 290 Ma) and lasted until the Late Cretaceous (similar to 65 Ma). The second (and best preserved) phase formed Mn duricrusts on the Paleoproterozoic Apui lateritic surface (150-250 m a.s.l.) and on the Aripuana lateritic surface (< 170 m a.s.l.) between the Late Cretaceous (similar to 90 Ma) and Oligocene (similar to 32 Ma). The third phase of lateritic formation occurred from Late Oligocene to Early Miocene times (similar to 28 to similar to 19 Ma). A degradation process, indicated by a goethite cortex on hematite fragments, took place in the Early to Late Miocene (similar to 23 to similar to 13 Ma), affected all previous lateritic duricrusts, and can be correlated to an epoch of extensive bauxite duricrust formation in the region. These Fe, Mn and Al aggradation episodes indicate strong and widespread polyphasic weathering in southwestern Amazonia since similar to 290 Ma, as expected on stable cratonic terrains exposed to alternating hot, humid, and dry climate conditions over time.	[dos Santos Albuquerque, Marcio Fernando; Coimbra Horbe, Adriana Maria] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Danisik, Martin] Curtin Univ, John de Later Ctr, GPO Box U1987, Perth, WA 6845, Australia	Universidade de Brasilia; Curtin University	Albuquerque, MFD (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil.	malbuquerquegeo@gmail.com	Danisik, Martin/GQY-6103-2022	Danisik, Martin/0000-0002-0885-4938	University of Brasilia; CAPES; Post doctorate scholarship (Programa Doutorado Sanduiche, PSDE) [88881.135254/2016-01]; Post doctorate scholarship (Programa Nacional de Pos Doutorado, PNPD) [88882.305731/2013-01]; CNPq [471971/2010-3, 473359/2012, 302618/2016-3]; Australian Research Council (ARC) [DP160102427]; Curtin Research Fellowship; AuScope NCRIS2 program	University of Brasilia; CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Post doctorate scholarship (Programa Doutorado Sanduiche, PSDE); Post doctorate scholarship (Programa Nacional de Pos Doutorado, PNPD); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Australian Research Council (ARC)(Australian Research Council); Curtin Research Fellowship; AuScope NCRIS2 program(Australian GovernmentDepartment of Industry, Innovation and Science)	We thank to graduate Program in Geology from the University of Brasilia, to CAPES for granting a PhD scholarship and Post doctorate scholarship (Programa Doutorado Sanduiche, PSDE, grant no 88881.135254/2016-01 and Programa Nacional de Pos Doutorado, PNPD grant no 88882.305731/2013-01 to the first author and CNPq for financial support (grant no 471971/2010-3, 473359/2012 and 302618/2016-3) for the second author. We also thank to J.O.S. Santos for support in SEM analysis, B. Ware for technical help with solution ICPMS analyses, A. Frew for technical help, and I. Dunkl for sharing PepiFLEX software for ICPMS data reduction. MD was Australian Research Council (ARC) Discovery funding scheme (DP160102427) and Curtin Research Fellowship; John de Laeter Centre LTTF is partly supported by the AuScope NCRIS2 program. We also thank the anonymous referees that provided helpful suggestions for improving the manuscript.	Aleva G. J. 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Geol.	OCT 20	2020	553								119792	10.1016/j.chemgeo.2020.119792	http://dx.doi.org/10.1016/j.chemgeo.2020.119792			13	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	NW5XC					2023-06-23	WOS:000575085100003
J	Sahoo, PK; Dall'Agnol, R; Salomao, GN; Ferreira, JD; Silva, MS; Souza, PWME; da Costa, ML; Angelica, RS; Medeiros, CA; da Costa, MF; Guilherme, LRG; Siqueira, JO				Sahoo, Prafulla Kumar; Dall'Agnol, Roberto; Salomao, Gabriel Negreiros; Ferreira Junior, Jair da Silva; Silva, Marcio Sousa; Martins e Souza Filho, Pedro Walfir; da Costa, Marcondes Lima; Angelica, Romulo Simoes; Medeiros Filho, Carlos Augusto; da Costa, Marlene Furtado; Guimaraes Guilherme, Luiz Roberto; Siqueira, Jose Oswaldo			Regional-scale mapping for determining geochemical background values in soils of the Itacaiunas River Basin, Brazil: The use of compositional data analysis (CoDA)	GEODERMA			English	Article						Soil geochemical mapping; geochemical background threshold values (GBTV); potentially toxic elements (PTEs); Carajas Mineral Province; Brazilian Amazonia; Itacaitinas River Basin	CARAJAS MINERAL PROVINCE; POTENTIALLY TOXIC ELEMENTS; U-PB GEOCHRONOLOGY; A-TYPE GRANITES; STREAM SEDIMENTS; AMAZONIAN CRATON; HYDROTHERMAL ALTERATION; METALLOGENIC PROVINCE; STATISTICAL-ANALYSIS; TRACE-ELEMENTS	This study aims at providing high quality soil geochemical data at a regional scale (1 sample per 25 km(2)) to understand the source and distribution of potentially toxic elements (PTEs: Al, As, Ba, Cd, Cu, Co, Cr, Fe, Hg, Mo, Mn, Ni, Pb, Se, U, V, and Zn) and to define their geochemical background threshold values (GBTVs) in the Itacaitinas River Basin (IRB), Brazilian Amazon. A total of 2958 soil samples were collected at two depths (surface: 0-10 cm; bottom: 30-50 cm) and the fine fractions (< 0.117 mm) were analyzed by ICP-MS and ICP-AES after aqua-regia digestion. The compositional nature of geochemical data was evaluated using the log-ratio approach and compared with traditional methods. Results show that compared to raw/log-transformation, centred log-ratio (clr) transformation improves spatial mapping and also better separated variables in Principal Component Analysis (PCA). Correlation analysis based on the isometric log-ratio OW transformation in heatmaps provides reliable and better structure of the results. The spatial maps (clr) indicate that most of the elements in surface and bottom soils are mainly governed by underlying bedrock geology (parent lithologies and mineralization), while anthropogenic factors are insignificant. The resulting clr-based PCA and cluster analyses associated with geological information indicate that geochemical patterns of Fe-Ti-V-Cr-Sc can be linked to mafic to intermediate metavolcanic rocks and banded-iron formations, which are dominant in the Carajas basin, while Ni and Cr distribution pattern is attributed to mafic and ultramafic lithologies, and Cu anomalous values are mainly related to hydrothermal mineralized copper belts. Among the statistical methods applied for estimation of GBTVs, TIF produced the highest BTVs, followed by 98th and mMAD, with few exceptions, while mMAD was considered the more suitable for defining GBTVs. The number of potential anomalies of PTEs identified by these methods follow the order of MAD > 98th > TIF or MAD > TIF > 98th, and overall the anomalies are mostly related to the local lithology/mineralization with no indication of anthropogenic contamination. Compared with Brazilian guidelines (CONAMA Resolution No. 420/2009), the GBTVs determined for Cr, Co, Ni, and Cu by TIF, MAD, and 98th percentile mostly exceeded both IV and PV limits. However, these high values are due to the influence of local lithology. This reveals that the Brazilian CONAMA guidelines of these elements for the IRB are unrealistic because that suggests a large number of sites requiring investigation, which is not consistent with the geochemical evidence. Therefore, site-specific GBTVs must be considered for the accurate evaluation of anthropogenic contamination, as well as the ecological and human health risks of PTEs in this region.	[Sahoo, Prafulla Kumar; Dall'Agnol, Roberto; Ferreira Junior, Jair da Silva; Silva, Marcio Sousa; Martins e Souza Filho, Pedro Walfir; Siqueira, Jose Oswaldo] Inst Tecnol Vale ITV, Rua Boaventura da Silva 955, BR-66055090 Belem, Para, Brazil; [Sahoo, Prafulla Kumar] Cent Univ Punjab, Sch Environm & Earth Sci, Dept Environm Sci & Technol, Bathinda 151001, India; [Dall'Agnol, Roberto; Salomao, Gabriel Negreiros; Martins e Souza Filho, Pedro Walfir; da Costa, Marcondes Lima; Angelica, Romulo Simoes] Univ Fed Para UFPA, Inst Geociencias IG, Programa Posgrad Geol & Geoquim, Rua Augusto Correa 1, BR-66075110 Belem, Para, Brazil; [Silva, Marcio Sousa] IG UFPA, Programa Posgrad Ciencias Ambientais, Belem, Para, Brazil; [Medeiros Filho, Carlos Augusto] VALE SA Exploracao Mineral, Rua Grajau 63, BR-68516000 Parauapebas, SA, Brazil; [da Costa, Marlene Furtado] Gerencia Meio Ambiente Minas Carajas, Dept Ferrosos Norte, Estr Raymundo Mascarenhas,S-N Mina N4, BR-68516000 Parauapebas, PA, Brazil; [Guimaraes Guilherme, Luiz Roberto] Univ Fed Lavras, Dept Ciencia Solo, BR-37200000 Lavras, MG, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Central University of Punjab; Universidade Federal do Para; Universidade Federal do Para; Universidade Federal de Lavras	Sahoo, PK (autor correspondente), Inst Tecnol Vale ITV, Rua Boaventura da Silva 955, BR-66055090 Belem, Para, Brazil.; Sahoo, PK (autor correspondente), Cent Univ Punjab, Sch Environm & Earth Sci, Dept Environm Sci & Technol, Bathinda 151001, India.	prafulla.sahoo@itv.org	Guilherme, Luiz Roberto Guimaraes/B-3998-2009; Angelica, Romulo/G-6245-2010; Guilherme, Luiz Roberto Guimaraes/V-6163-2019; Souza, Pedro/GZH-1275-2022; Sahoo, Prafulla/N-5100-2018; Souza-Filho, Pedro Walfir M. M./J-4958-2012	Guilherme, Luiz Roberto Guimaraes/0000-0002-5387-6028; Angelica, Romulo/0000-0002-3026-5523; Guilherme, Luiz Roberto Guimaraes/0000-0002-5387-6028; Sahoo, Prafulla/0000-0003-3481-1787; Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; LIMA DA COSTA, MARCONDES/0000-0002-0134-0432	Vale (GABAN-DIFN); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), Brazil [380998/2019-0, 306108/2014-3, 443247/2015-3, 402727/2018-5, 304648/2019-1, 305.392/2014-0, 305015/2016-8]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]	Vale (GABAN-DIFN); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work was undertaken at Instituto Tecnologico Vale (ITV), Belem, Brazil, as part of the Itacaiunas Geochemical Mapping and Background Project, ItacGMBP. This project was financially supported by: Vale (GABAN-DIFN); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), Brazil [DTI scholarship to GNS (Proc. 380998/2019-0); grants to RD (proc. 306108/2014-3; proc. 443247/2015-3; proc. 402727/2018-5; proc. 304648/2019-1); RSA (proc. 305.392/2014-0); MLC (proc. 305015/2016-8)]. This study was also financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001. The authors acknowledge to Jose Francisco Berredo, Jose Francisco da Fonseca Ramos and Otavio Augusto Boni Licht for their scientific collaboration and valuable contribution to the ItacGMBP.	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J	Melo, CCA; Angelica, RS; Paz, SPA				Amorim Melo, Caio Cesar; Angelica, Romulo Simoes; Aranha Paz, Simone Patricia			A proposal for rapid grade control of gibbsitic bauxites using multivariate statistics on XRD data	MINERALS ENGINEERING			English	Article						Bauxite; Quality control; PLSR	STANDARD PXRD METHOD; COMBINED RIETVELD; LE BAIL; REFINEMENT; REGRESSION	Currently, traditional wet chemistry methods are used for quality control of bauxites. Such methods indirectly quantify the gibbsite and kaolinite content as available alumina (AvAl(2)O(3)) and reactive silica (RxSiO(2)), respectively, and it is very costly and time-consuming. In order to achieve a rapid and reliable method to estimate these parameters, as alternative to current wet chemistry methods, this study, evaluates the use of multivariate statistics - Partial Least Square Regression (PLSR) on XRD data of gibbsitic bauxites (Miltonia 3 plateau). The method was optimized through Principal Component Analysis (PCA) and factorial Design of Experiments (DOE). The results demonstrated that such method has a potential to be industrially applied to quality control of bauxites. In comparison with traditional method, the same precision is achieved for the ore samples, but faster, easier to implement and carry out the analyses, demands less laboratory space and manpower, and no reagent is necessary. In addition, the use of XRD for quality control makes it possible to track the mineralogy of the bauxite that feeds the Bayer process, and therefore, be aware of how it could impact the process.	[Amorim Melo, Caio Cesar; Aranha Paz, Simone Patricia] UFPA Univ Fed Para, Programa Posgrad Engn Recursos Nat PRODERNA, BR-66075110 Belem, Para, Brazil; [Angelica, Romulo Simoes; Aranha Paz, Simone Patricia] UFPA Univ Fed Para, Inst Geociencias, Lab Caracterizacao Mineral, BR-66075110 Belem, Para, Brazil	Universidade Federal do Para; Universidade Federal do Para	Melo, CCA (autor correspondente), UFPA Univ Fed Para, Programa Posgrad Engn Recursos Nat PRODERNA, BR-66075110 Belem, Para, Brazil.	eng.caiomelo@hotmail.com	Paz, Simone Patricia Aranha/AAF-3059-2019; Angelica, Romulo/G-6245-2010	Paz, Simone Patricia Aranha/0000-0002-5880-7638; Angelica, Romulo/0000-0002-3026-5523; Melo, Caio/0000-0002-5267-2111	Brazilian agency: CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior); Brazilian agency: CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) [12/2009, 550.297/2010-3]; Brazilian agency: FAPESPA (Fundacao Amazonia de Amparo a Estudos e Pesquisas) [027/2011]; Mineracao Paragominas SA Company (Norsk Hydro)	Brazilian agency: CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Brazilian agency: CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Brazilian agency: FAPESPA (Fundacao Amazonia de Amparo a Estudos e Pesquisas); Mineracao Paragominas SA Company (Norsk Hydro)	The authors thank the Brazilian agencies: CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) for a PhD scholarship to the first author; CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) for financial support (EditalMCT/CT-Mineral/VALE/CNPq No 12/2009, 550.297/2010-3); and FAPESPA (Fundacao Amazonia de Amparo a Estudos e Pesquisas), Edital 01/2010, ICAAF No. 027/2011, also for financial support. We also acknowledge the Mineracao Paragominas SA Company (Norsk Hydro) for the support.	Angelica RS, 2018, MINER ENG, V122, P148, DOI 10.1016/j.mineng.2018.03.039; Authier-Martin M, 2001, JOM-J MIN MET MAT S, V53, P36, DOI 10.1007/s11837-001-0011-1; Negrao LBA, 2018, MINERAL MAG, V82, P413, DOI 10.1180/minmag.2017.081.056; BREDELL JH, 1983, ECON GEOL, V78, P319, DOI 10.2113/gsecongeo.78.2.319; Bro R, 2014, ANAL METHODS-UK, V6, P2812, DOI 10.1039/c3ay41907j; Carneiro C. C, 2017, IMPUTATION REACTIVE, DOI [10.1109/WSOM.2017.8020008, DOI 10.1109/WSOM.2017.8020008]; Coathup D, 2019, J ELECTROCERAM, V43, P92, DOI 10.1007/s10832-019-00189-0; Cordella C.B., 2012, ANAL CHEM, P1; Faber NM, 2003, TRAC-TREND ANAL CHEM, V22, P330, DOI 10.1016/S0165-9936(03)00503-X; Feret F, 1997, CLAY CLAY MINER, V45, P418, DOI 10.1346/CCMN.1997.0450311; Feret F. 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OCT 1	2020	157								106539	10.1016/j.mineng.2020.106539	http://dx.doi.org/10.1016/j.mineng.2020.106539			9	Engineering, Chemical; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Mineralogy; Mining & Mineral Processing	NH2WI					2023-06-23	WOS:000564535400006
J	Araujo, RC; Nogueira, ACR; Araujo, RN				Araujo Filho, Roberto Costa; Nogueira, Afonso C. R.; Araujo, Raphael Neto			New stratigraphic proposal of a Paleoproterozoic siliciclastic succession: Implications for the evolution of the Carajas Basin, Amazonian craton, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Paleoproterozoic; Stratigraphic framework; Azul Formation; Amazonian craton; Columbia supercontinent	U-PB GEOCHRONOLOGY; SAO FRANCISCO CRATON; TUREE CREEK GROUP; GRAO-PARA GROUP; QUADRILATERO FERRIFERO; IRON-FORMATION; MINERAL PROVINCE; DETRITAL ZIRCON; BASEMENT REACTIVATION; DEPOSITIONAL MODELS	In this study, we propose a new stratigraphic framework for a well-preserved Paleoproterozoic succession of the Carajas Basin (Amazonian craton) in northern Brazil. A core-based facies analysis is coupled with a critical review of previous data on this succession. We are proposing that the studied succession, which was previously considered as a single lithostratigraphic unit called the Aguas Claras Formation, consists of two different formations of Paleoproterozoic age (similar to 2.37-2.06 Ga). The lower formation, which is composed of similar to 250-m-thick mudstone strata locally enriched with manganese, is formally proposed here and is designated as the Azul Formation, referring to the Azul mine, in which the type-section is described. The overlying Aguas Claras Formation is redefined as a stratigraphic unit composed exclusively of an similar to 800-m-thick succession of sandstone and conglomerate strata. The contact between these two formations is an easily recognizable surface; thus, these formations can be accurately mapped and distinguished within the basin. We suggest that the Azul and Aguas Claras formations are the stratigraphic record associated with a transgressive-regressive sequence, in which these formations are limited one from the other by a maximum flooding zone. The Azul Formation was deposited during a marine transgression related to the latest incursion of the Azul sea towards the Carajas protocontinent. On the other hand, the overlying Aguas Claras Formation was deposited in a fluvial system that developed during a period of marine regression. Whereas the marine transgression may have been influenced by the deglaciation occurred aftermath the Siderian-Rhyacian Serra Sul glaciation, the subsequent marine regression was triggered, at least in part, by uplifting related to the Transamazonian cycle (similar to 2.0 Ga). In addition to our results shed new light on the Carajas Basin evolution, they support the hypothesis that the Azul and Aguas Claras formations can be correlated with other Paleoproterozoic successions worldwide, mainly those registered in ancient landmasses that amalgamated and later formed the Columbia supercontinent during the Paleo-to Mesoproterozoic.	[Araujo Filho, Roberto Costa; Nogueira, Afonso C. R.; Araujo, Raphael Neto] Fed Univ Para, Postgrad Program Geol & Geochem, BR-66075110 Belem, Para, Brazil; [Araujo, Raphael Neto] Geol Survey Brazil, Management Geol & Mineral Resources, BR-66095904 Belem, Para, Brazil	Universidade Federal do Para	Araujo, RC (autor correspondente), Fed Univ Para, Postgrad Program Geol & Geochem, BR-66075110 Belem, Para, Brazil.	rcaraujo@ufpa.br		Araujo Filho, Roberto/0000-0001-9124-2133; NOGUEIRA, AFONSO/0000-0002-5225-9255	PROPESP/UFPA (Belem, Brazil); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [133399/2016-8]	PROPESP/UFPA (Belem, Brazil); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We are very grateful to Vale S.A. (Parauapebas, Brazil) for making the drill cores available for the research; the Geological Survey of Brazil (Belem, Brazil) for support during fieldwork; Luiz Claudio Costa and Alexandre Ribeiro for help during fieldwork; and the PROPESP/UFPA (Belem, Brazil) for supporting this work. This paper is part of the dissertation thesis of the first author, who gratefully acknowledges the grant from the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), process number 133399/2016-8. We are also very grateful to the anonymous peer-reviewers for reviewing our manuscript and to Michelangelo Martini for his editorial work.	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J	Barbosa, P; Lagoeiro, L; Nogueira, VME				Barbosa, Paola; Lagoeiro, Leonardo; Mota e Nogueira, Victor			Misorientation relationships in goethite, hematite and magnetite: a case study of iron-formation rocks from the Iron Quadrangle, Brazil	JOURNAL OF APPLIED CRYSTALLOGRAPHY			English	Article						orientation relationships; misorientation spaces; phase transformations; electron backscatter diffraction; EBSD; iron oxides	DEHYDRATION TRANSFORMATIONS; IN-SITU; CRYSTALS; TEXTURE; BOUNDARIES; MECHANISM	The transformation behavior between iron oxides and oxyhydroxides like magnetite, hematite and goethite is still not entirely understood. Crystallographic similarities allow one to predict topotactic relationships between them. The related crystallographic aspects have been explored by means of electron backscatter diffraction (EBSD). Samples from natural aggregates of magnetite, hematite and goethite were collected from iron-formation rocks that outcrop in the southeast of Brazil, in a region known for large deposits of iron and other ores. EBSD misorientation data indicate a pronounced relationship between these iron phases. The transformation seems to be related to the oxygen framework. The original close-packed cubic arrangement of O atoms in magnetite changes to a hexagonal close-packed framework in hematite, i.e. {111} of magnetite is parallel to {0001} of hematite. The matrix in which the magnetite grains are embedded is made of aggregates of hematite and goethite. In the matrix, the coincidence observed in the magnetite grains is not observed. On the other hand, the well known twin boundary relationships already described for these mineral phases can be observed here as an orientation relationship in three-dimensional misorientation space. The spatial data of axis-angle pairs suggest that the twin boundaries serve as facilitating surfaces for phase transformation in the Fe-O-OH system. The main conclusion of this study is that the transformation occurred in the solid state with the newly transformed goethite inheriting the crystallographic orientations of the former crystals and that this phenomenon is better recognized by combining observations of misorientation relationships. In the matrix, such a relation is not observed and, for that reason, the minerals in the matrix are thought to have been formed by a different process, which might have involved dissolution and precipitation of the phase newly out of solution.	[Barbosa, Paola; Mota e Nogueira, Victor] Univ Brasilia, Inst Geosci, Darcy Ribeiro Campus, BR-70834070 Brasilia, DF, Brazil; [Lagoeiro, Leonardo] Univ Fed Parana, Polytech Ctr, Dept Geomat, BR-81531990 Curitiba, Parana, Brazil	Universidade de Brasilia; Universidade Federal do Parana	Barbosa, P (autor correspondente), Univ Brasilia, Inst Geosci, Darcy Ribeiro Campus, BR-70834070 Brasilia, DF, Brazil.	paolabarbosa@unb.br	Barbosa, Paola/AAK-8478-2021	Barbosa, Paola/0000-0001-7661-455X	CNPq [305257/2014-5]; Brazilian Science Foundation FAPEMIG [CRA-APQ-02969-14]; Brazilian Science Foundation FAP-DF [0193.001526/2017]; Brazilian Science Foundation CNPq [425412/2018-0, 305232/2018-5, 406849/2016-1]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Brazilian Science Foundation FAPEMIG; Brazilian Science Foundation FAP-DF; Brazilian Science Foundation CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	LL acknowledges the fellowship awarded to him by the CNPq (Process 305257/2014-5). Financial support from the Brazilian Science Foundations FAPEMIG (CRA-APQ-02969-14), FAP-DF (0193.001526/2017) and CNPq (425412/2018-0, 305232/2018-5, 406849/2016-1) is also acknowledged.	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Appl. Crystallogr.	OCT	2020	53		5				1334	1342		10.1107/S1600576720010596	http://dx.doi.org/10.1107/S1600576720010596			9	Chemistry, Multidisciplinary; Crystallography	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Crystallography	NZ5XH					2023-06-23	WOS:000577178000019
J	Chahud, A; Fairchild, TR				Chahud, Artur; Fairchild, Thomas R.			A NEW INVERTEBRATE FROM THE PONTA GROSSA FORMATION (DEVONIAN), PARANA BASIN, BRAZIL	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						taphonomy; taxonomy; Gondwana; marine; Malvinokaffric Realm	HEXACTINELLID SPONGE	Pontagrossia reticulata n. gen. et sp. is described from the Lower Devonian (Emsian) Ponta Grossa Formation, Parana Basin. The species is based on morphological characteristics shared by three contiguous casts clearly representing a single species, if not the same individual. The shape and organization of the fossil resembles that in some sponges, but until diagnostic evidence of its affinities can be recognized in these specimens, the new taxon will be left in open nomenclature. Nevertheless, this fossil is unlike any other invertebrate, plant, or algal fossil already known from the Ponta Grossa Formation, and thus represents a novel addition to the diversified cold-water Devonian paleobiota of Brazil.	[Chahud, Artur; Fairchild, Thomas R.] Univ Sao Paulo, Dept Geol Sedimentar & Ambiental, Inst Geociencias, Rua Lago 562,Cidade Univ, BR-05508080 Sao Paulo, SP, Brazil	Universidade de Sao Paulo	Chahud, A (autor correspondente), Univ Sao Paulo, Dept Geol Sedimentar & Ambiental, Inst Geociencias, Rua Lago 562,Cidade Univ, BR-05508080 Sao Paulo, SP, Brazil.	arturchahud@yahoo.com; trfairch@usp.br	Fairchild, Thomas Rich/AAE-1835-2021; Chahud, Artur/B-6976-2012	Chahud, Artur/0000-0001-7690-3132				Bergamaschi S., 1999, THESIS; Bolzon RT, 2002, SITIOS GEOLOGICOS PA; Botting JP, 2018, PALAEOWORLD, V27, P1, DOI 10.1016/j.palwor.2017.07.001; Botting Joseph P., 2004, Journal of Systematic Palaeontology, V2, P31, DOI 10.1017/S147720190300110X; Botting JP, 2003, LETHAIA, V36, P41, DOI 10.1080/00241160310001263; Carrera MG, 2018, ACTA PALAEONTOL POL, V63, P63, DOI 10.4202/app.00403.2017; Carrera MG, 2015, J PALEONTOL, V89, P912; Carrera MG, 2009, AMEGHINIANA, V46, P449; Carrera Marcelo G., 1994, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V191, P201; Clarke J.M., 1913, MONOGRAHPIAS SERVICO, V1; de Melo J.H.G., 1988, Canadian Society of Petroleum Geologists Memoir, V14, P669; Fernandes A.C.S., 1996, THESIS; Kozlowski R., 1913, ANN PALEONTOL, V8, P105; Lange F.W., 1967, BOL PARANA GEOCIENC, V21, P5; MORSCH SM, 1986, AN ACAD BRAS CIENC, V58, P403; Mour LD, 2014, J PALEONTOL, V88, P171, DOI 10.1666/12-108; RICHTER R., 1942, SENCKENBERGIANA, V25, P156; Rodrigues S.C., 2003, REV BRAS GEOCIENC, V33, P381; Scheffler Sandro Marcelo, 2007, Arquivos do Museu Nacional Rio de Janeiro, V65, P83	19	1	1	0	2	SOC BRASILEIRA PALEONTOLOGIA	SAO LEOPOLDO	PPGEO UNISINOS, AV UNISINOS 950, SAO LEOPOLDO, RS 93022-000, BRAZIL	1519-7530	2236-1715		REV BRAS PALEONTOLOG	Rev. Bras. Paleontol.	OCT-DEC	2020	23	4					279	282		10.4072/rbp.2020.4.06	http://dx.doi.org/10.4072/rbp.2020.4.06			4	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	PI8VV		hybrid			2023-06-23	WOS:000601362500006
J	da Rosa, KK; Perondi, C; Veettil, BK; Auger, JD; Simoes, JC				da Rosa, Katia Kellem; Perondi, Cleiva; Veettil, Bijeesh Kozhikkodan; Auger, Jeffrey D.; Simoes, Jefferson Cardia			Contrasting responses of land-terminating glaciers to recent climate variations in King George Island, Antarctica	ANTARCTIC SCIENCE			English	Article						Admiralty Bay; climate change; multi-temporal analysis; proglacial systems	PENINSULA	In this study, we aim to analyse the glacier dynamics of land-terminating glaciers in King George Island (Antarctica) between 1956 and 2018. Glacial fluctuations are estimated using space-borne remote sensing data (SPOT, Landsat, PlanetScope, Sentinel-1, Sentinel-2, WorldView-2 and TanDEM-X). The eastern sector of Warszawa Icefield witnessed continuous glacier retreat during 1979-2018 (surface loss of 30%). The decreases in the ice-covered areas of the Tower, Windy, Ecology, Baranowski and Sphinx glaciers were 70%, 31%, 25%, 25% and 21%, respectively, with their accumulation area ratios (AARs) exhibiting negative mass balances. The winter air temperature was cooler during the 1970s with warming trends in the 1980s and early 2000s followed by a cooling trend until the present day. However, the annual time series has shown high interannual variability in air temperature during these periods. We show that the AAR, dimensions, length, frontal elevation, maximum elevation, slope and changes in the terminus position influence the glacier response to climate change at various timescales. Furthermore, three geomorphic activity intensity zones and a complete paraglacial sequence are identified while contrasting the proglacial systems. Overall, subglacial deposits predominate and indicate that meltwater flows on the bed, producing wet-based thermal regimes.	[da Rosa, Katia Kellem; Perondi, Cleiva; Auger, Jeffrey D.; Simoes, Jefferson Cardia] Univ Fed Rio Grande Sul UFRGS, Inst Geociencias, Ctr Polar & Climat, Porto Alegre, RS, Brazil; [da Rosa, Katia Kellem; Perondi, Cleiva] Univ Fed Rio Grande Sul UFRGS, Inst Geociencias, Programa Posgrad Geog, Porto Alegre, RS, Brazil; [da Rosa, Katia Kellem] Univ Fed Rio Grande Sul UFRGS, Programa Posgrad Sensoriamento Remoto, Porto Alegre, RS, Brazil; [Veettil, Bijeesh Kozhikkodan] Ton Duc Thang Univ, Dept Management Sci & Technol Dev, Ho Chi Minh City, Vietnam; [Veettil, Bijeesh Kozhikkodan] Ton Duc Thang Univ, Fac Environm & Lab Safety, Ho Chi Minh City, Vietnam	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Ton Duc Thang University; Ton Duc Thang University	Veettil, BK (autor correspondente), Ton Duc Thang Univ, Dept Management Sci & Technol Dev, Ho Chi Minh City, Vietnam.; Veettil, BK (autor correspondente), Ton Duc Thang Univ, Fac Environm & Lab Safety, Ho Chi Minh City, Vietnam.	bijeesh.veettil@tdtu.edu.vn	Simoes, Jefferson Cardia/D-7232-2013; Kozhikkodan Veettil, Bijeesh/Q-6489-2017; da Rosa, Kátia Kellem/AAO-8367-2020	Simoes, Jefferson Cardia/0000-0001-5555-3401; Kozhikkodan Veettil, Bijeesh/0000-0003-4158-4578; da Rosa, Kátia Kellem/0000-0003-0977-9658	Foundation for Research Support of the State of Rio Grande do Sul (FAPERGS); Brazilian Coordination for the Improvement of Higher Education Personnel (CAPES)	Foundation for Research Support of the State of Rio Grande do Sul (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); Brazilian Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work is a contribution of the Antarctic Science reviewers, Brazilian Antarctic Program (PROANTAR), and is supported by research grants from the Foundation for Research Support of the State of Rio Grande do Sul (FAPERGS). Cleiva Perondi is thankful to the Brazilian Coordination for the Improvement of Higher Education Personnel (CAPES) for a scholarship.	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Sci.	OCT	2020	32	5					398	407	PII S0954102020000279	10.1017/S0954102020000279	http://dx.doi.org/10.1017/S0954102020000279			10	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	NV8LQ		Bronze			2023-06-23	WOS:000574566200008
J	da Silva, FF; de Oliveira, DC; Dall'Agnol, R; da Silva, LR; da Cunha, IV				da Silva, Fernando Fernandes; de Oliveira, Davis Carvalho; Dall'Agnol, Roberto; da Silva, Luciano Ribeiro; da Cunha, Ingrid Viana			Lithological and structural controls on the emplacement of a Neoarchean plutonic complex in the Carajas province, southeastern Amazonian craton (Brazil)	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Granitoid; Shear zone; Archean; Carajas; Amazonian craton	GRANITE-GREENSTONE TERRANE; U-PB GEOCHRONOLOGY; DUCTILE SHEAR ZONE; A-TYPE GRANITE; DISLOCATION CREEP; ZIRCON GEOCHRONOLOGY; MINERAL PROVINCE; ARCHEAN GRANITE; GEOCHEMISTRY; DEFORMATION	New geological and geochronological (Pb-Pb evaporation) data from the Vila Jussara suite, a representative of the Neoarchean granitoids of the Carajns province, southeastern Amazonian craton (Brazil), are discussed. The Vila Jussara suite crops out as a series of coalescing plutons elongated in the E-W direction. These plutons generally have sigmoidal shapes, and steep dips (75-85 degrees) that follow the regional trend. The centermost areas of plutons are generally slightly deformed, while the marginal portions display mylonitic aspect and are delimited by sinistral shear zones belonging to the transcurrent system of the Itacaitinas shear belt. These granitoids cover a large compositional spectrum, with four main lithotypes: (i) Seriated biotite-hornblende monzogranite; (ii) biotite-hornblende tonalite; (iii) porphyritic biotite monzogranite-granodiorite; and (iv) porphyritic hornblendebiotite monzogranite-granodiorite. The microstructural analysis of the studied rocks reveals: (i) microfractures in feldspar phenocrysts, filled with a quartz-feldspar matrix; (ii) preferred orientation of euhedral feldspar crystals in an igneous matrix; and (iii) evidence of moderate-to high-temperature of solid-state deformation (>500 degrees C). These microstructures and field observations point to a continuum of deformation, from the (sub) magmatic state down to sub-solidus conditions. Dating of three types of granitoids out of four gives ages of 2754 +/- 2.2 Ma, 2752 +/- 5.7 Ma and 2745 +/- 3 Ma. The different granitoid varieties of the Vila Jussara suite were thus emplaced simultaneously. It is proposed that emplacement of the granitoids was controlled by shear zones reactivated during oblique collision and that plutons where constructed by multiple injections of magmas, generating extensive hybridization.	[da Silva, Fernando Fernandes; de Oliveira, Davis Carvalho; Dall'Agnol, Roberto; da Silva, Luciano Ribeiro; da Cunha, Ingrid Viana] Inst Geociencias IG, Grp Pesquisa Petrol Granitoides GPPG, Rua Augusto Correa 01, BR-66075900 Belem, Para, Brazil; [da Silva, Fernando Fernandes; de Oliveira, Davis Carvalho; Dall'Agnol, Roberto; da Silva, Luciano Ribeiro; da Cunha, Ingrid Viana] Univ Fed Para UFPA, IG UFPA, Programa Posgrad Geol & Geoquim, Belem, Para, Brazil; [Dall'Agnol, Roberto] Inst Tecnol Vale, Belem, Para, Brazil	Universidade Federal do Para; Instituto Tecnologico Vale Desenvolvimento Sustentavel	da Silva, FF (autor correspondente), Inst Geociencias IG, Grp Pesquisa Petrol Granitoides GPPG, Rua Augusto Correa 01, BR-66075900 Belem, Para, Brazil.	ffernandes@ufpa.br			Research Group on Granitoid Petrology (GPPG); Conselho Nacional de Desenvolvimento Cientffico e Tecnologico (CNPq) [140077/2018-9, 001]; Coordenacno de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [140077/2018-9, 001]; CNPq [311647/2019-7, 435552/2018-0, 306108/2014-3]; PROPESP (PAPQ)/UFPA	Research Group on Granitoid Petrology (GPPG); Conselho Nacional de Desenvolvimento Cientffico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacno de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); PROPESP (PAPQ)/UFPA	The authors would like to thank the Research Group on Granitoid Petrology (GPPG) for its support in the various stages of this work, the Institute of Geosciences (IG) of the Universidade Federal do Path (UFPA), the Post-Graduate Program in Geology and Geochemistry (PPGG) and F.V Guimardes for the Pb-Pb data acquisition and M.LT. Silva for the collect and organization of prior samples and petrographic data. We are also grateful to M.T. Galarza for assistance during the acquisition of Pb-Pb evaporation geochronology data at the Laboratorio de Geologia de Isotopica (PARAISO-UFPA). We also wish to express our gratitude to the anonymous reviewers for the careful reading and many insight thoughts on the manuscript. The first author (FF) thanks the Conselho Nacional de Desenvolvimento Cientffico e Tecnologico (CNPq) and Coordenacno de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) for a doctoral thesis scholarship (Proc. 140077/2018-9 and finance code 001). Funding for this project came from CNPq (D.C. Oliveira - Proc. 311647/2019-7 and 435552/2018-0; R. Dall'Agnol - Proc. 306108/2014-3) and PROPESP (PAPQ)/UFPA.	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South Am. Earth Sci.	OCT	2020	102								102696	10.1016/j.jsames.2020.102696	http://dx.doi.org/10.1016/j.jsames.2020.102696			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MS0ST					2023-06-23	WOS:000553997400038
J	Del Rey, GO; Santos, RV; da Cunha, LS; Ferreira, GS				Del Rey, Giovanna Orletti; Santos, Roberto Ventura; da Cunha, Luciano Soares; Ferreira, Gabriela Silva			Seasonal variations of geochemical parameters for a tropical landfill: Implications for landfill stabilization	APPLIED GEOCHEMISTRY			English	Article						Landfill stabilization process; Organic matter; Stable isotope; Redox; Methanogenesis	MUNICIPAL SOLID-WASTE; DISSOLVED ORGANIC-CARBON; BIOLOGICAL STABILITY; INORGANIC CARBON; STABLE-ISOTOPES; LEACHATE; OXIDATION; METHANE; WATER; BIOGEOCHEMISTRY	Landfills stabilization stages depend on parameters such as the age of the landfill, the refuse composition, and the confinement level of the buried material. In the absence of free oxygen, redox reactions (e.g., SO42- , NO3-) and methanogenesis control the decomposition of organic matter. Landfill's stabilization stage is usually assessed by parameters such as pH, biochemical oxygen demand, chemical oxygen demand, dissolved organic carbon, and biogas composition. This study evaluates the stabilization stage of a 50-year-old tropical landfill located in Central Brazil based on physicochemical parameters, dissolved carbon isotope data (delta C-13), redox reactions, and concentration of released gases CO2 and CH4. We show that seasonal variations of these parameters are modified by rainwater inflow, which carries free-oxygen into the landfill. An increase in free-oxygen leads to a(13)C-depletion in carbon isotopic composition of dissolved CO2 and an increase in redox-dependent species such as Fe3+, SO42- , and NO3- . Our data show that most of the landfill has reached the methanogenic stage and that periodic oxygen input by rainwater affects methane production. The studied site is a complex chemical system in which organic matter degradation occurs by aerobic, anaerobic, and methanogenic processes, depending on the recharge susceptibility.	[Del Rey, Giovanna Orletti; Santos, Roberto Ventura; da Cunha, Luciano Soares; Ferreira, Gabriela Silva] Univ Brasilia UnB, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia	Del Rey, GO (autor correspondente), Univ Brasilia UnB, BR-70910900 Brasilia, DF, Brazil.	giovannaodelrey@gmail.com			Coordination for the Improvement of Higher Education Personnel -Brazil (CAPES) [001]; National Council of Scientific and Technological Development -CNPq [428843/2016-6, 312941/2018-8]	Coordination for the Improvement of Higher Education Personnel -Brazil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council of Scientific and Technological Development -CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are thankful to the RAEESA Project (UnB/CEB Generation S.A. and CEB Lajeado S.A.) and to the University of Brasilia for the infrastructure and technical support, especially the Geochemistry Laboratory and the Geodynamic Studies Laboratory. We also thank the financial support of the Coordination for the Improvement of Higher Education Personnel -Brazil (CAPES) -Finance Code 001 and The National Council of Scientific and Technological Development -CNPq (Grants 428843/2016-6 and 312941/2018-8).	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Geochem.	OCT	2020	121								104686	10.1016/j.apgeochem.2020.104686	http://dx.doi.org/10.1016/j.apgeochem.2020.104686			9	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	NT3MJ					2023-06-23	WOS:000572849100003
J	Duarte, SK; Hartmann, LA; Santos, JOS; McNaughton, NJ				Duarte, Sandro Kucera; Hartmann, Leo Afraneo; Schneider Santos, Joao Orestes; McNaughton, Neal Jesse			Evolution of sand and silt injection and effusion around the rim and depocenter of Parana volcanic province	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Novo Hamburgo Complex; Parana volcanic province; U-Pb SHRIMP age barcode; Sandstone geochemistry; Sand elutriation; Chalcedony cement	U-PB GEOCHRONOLOGY; BOTUCATU FORMATION; SOUTHWESTERN MARGIN; AMAZONIAN CRATON; MATO-GROSSO; ZIRCON; BASIN; BRAZIL; STRATIGRAPHY; SANDSTONE	The Novo Hamburgo Complex (NHC) occurs widespread in the 1 million km(2), Early Cretaceous Parana volcanic province. Integrated field work with zircon dating and whole rock geochemistry supported the investigation. We used the sensitive high-resolution ion microprobe (SHRIMP II) to determine the U-Pb age of zircon from eight sandstones from pairs of parent Botucatu Formation (1.2 million km(2), largest paleoerg in geological history) (n = 3) and injectites, extrudites (n = 5), total = 718 analyses. Samples were collected from south to northeast to northwest of the complex. Integrated age peaks (in Ma) occur at 151 (one grain), 236 (minor), 280-288 (significant), 528-536-544-626-628 (approximate 520-630; highest peak at 544), 1043-1057 (approximate 900-1300), 1734, 1968, 2046-2098, 2691, and 3300 (one grain). U-Pb age distribution barcode is similar for both parent sandstones and injectites, extrudites. No zircon from the Cretaceous Serra Geral Group of basalt and rhyodacite (134 +/- 2 Ma) was dated in the sandstones. Differences between parent sandstones and injectites, extrudites originated by elutriation in 1-1700 m-high injection columns. Textural characteristics are bimodal, medium to fine grained in parent beds, and unimodal, fine grained in injectites, extrudites. Chemical differences are increase in Al, K, Na, Ca, Rb, Sr, Ba, ETR, Cu, U, Th in injectites, extrudites compared to parent beds. We conclude that the injected sandstone and contained zircon originated in the Botucatu Formation paleoerg ascending through the volcanic lavas in a sand (estimated 70 vol%) and water (30 vol%) slurry. This is a prime, unique example of paleoerg sand remobilization after aquifer heating and volcanic rock sealing in a huge injection complex.	[Duarte, Sandro Kucera; Hartmann, Leo Afraneo] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Schneider Santos, Joao Orestes] Univ Western Australia, Ctr Explorat Targeting, Sch Earth Sci, Crawley, WA 6009, Australia; [Schneider Santos, Joao Orestes] Univ Western Australia, Australian Res Council Ctr Excellence Core Crust, Sch Earth Sci, Crawley, WA 6009, Australia; [Schneider Santos, Joao Orestes] Univ Estado Amazonas, Manaus, Amazonas, Brazil; [McNaughton, Neal Jesse] Curtin Univ Technol, Perth, WA, Australia	Universidade Federal do Rio Grande do Sul; University of Western Australia; University of Western Australia; Universidade do Estado do Amazonas; Curtin University	Hartmann, LA (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	leo.hartmann@ufrgs.br	Santos, João/HHZ-5595-2022; Hartmann, Léo A/D-7663-2013; McNaughton, Neal/AAD-7067-2022	Hartmann, Léo A/0000-0001-7863-5071; 	project of excellence (PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil) on strategic minerals from southern Brazil [10/0021-8]	project of excellence (PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil) on strategic minerals from southern Brazil	Field work had participation of Juliana Pertille da Silva, Karine da Rosa Arena, Sergio Benjamin Baggio, Daniel Barbosa Knijnik, Gilmar J. Rizzotto and Romualdo H. P. Andrade; SHRIMP IIe at USP had supervision of Kei Sato; Tiara Cerva Alves helped with isotopic data handling. Financial support was provided by a project of excellence (grant number 10/0021-8, PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil) on strategic minerals from southern Brazil, coordinated by Leo A. Hartmann. Two journal reviewers made significant contributions that led to improvement of the article.	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South Am. Earth Sci.	OCT	2020	102								102651	10.1016/j.jsames.2020.102651	http://dx.doi.org/10.1016/j.jsames.2020.102651			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MS0ST					2023-06-23	WOS:000553997400010
J	Ferreira, HS; Gocyla, M; Ferreira, HS; Araujo, RGO; Almeida, CVS; Heggen, M; Dunin-Borkowski, RE; Eguiluz, KIB; Strasser, P; Salazar-Banda, GR				Ferreira, Hadla S.; Gocyla, Martin; Ferreira, Hadma S.; Araujo, Rennan G. O.; Almeida, Caio V. S.; Heggen, Marc; Dunin-Borkowski, Rafal E.; Eguiluz, Katlin I. B.; Strasser, Peter; Salazar-Banda, Giancarlo R.			A Comparative Study of the Catalytic Performance of Pt-Based Bi and Trimetallic Nanocatalysts Towards Methanol, Ethanol, Ethylene Glycol, and Glycerol Electro-Oxidation	JOURNAL OF NANOSCIENCE AND NANOTECHNOLOGY			English	Article						Nanostructured Materials; Core-Shell; Alcohols Electrooxidation; Fuel Cell	CORE-SHELL NANOPARTICLES; FUEL-CELLS; ELECTROCHEMICAL OXIDATION; ELECTROCATALYSTS; NANOWIRES; MEMBRANES; CARBON; RH/C	Carbon-supported platinum is used as an anode and cathode electrocatalyst in low-temperature fuel cells fueled with low-molecular-weight alcohols in fuel cells. The cost of Pt and its low activity towards the complete oxidation of these fuels are significant barriers to the widespread use of these types of fuel cells. Here, we report on the development of PtRhNi nanocatalysts supported on carbon made using a reduction chemistry method with different atomic rates. The catalytic activity of the developed catalysts towards the electro-oxidation of methanol, ethanol, ethylene glycol, and glycerol in acidic media was studied. The obtained catalysts performances were compared with both commercial Pt/C and binary Pt75Ni25/C catalyst. The nanostructures were characterized, employing inductively coupled plasma optical emission spectrometer, X-ray diffraction, scanning transmission electron microscopy, and energy-dispersive X-ray spectroscopy. The binary catalyst presents a mean particle size of around 2 nm. Whereas the ternary catalysts present particles of similar size and with some large alloy and core-shell structures. The alcohol oxidation onset potential and the current density measured after 3600 s of chronoamperometry were used to classify the catalytic activity of the catalysts towards the oxidation of methanol, ethanol, ethylene glycol, and glycerol. The best PtRhNi/C catalyst composition (i.e., Pt43Rh43Ni14/C) presented the highest activity for alcohols oxidation compared with all catalysts studied, indicating the proper tuning composition influence in the catalytic activity. The enhanced activity of Pt43Rh43Ni14/C can be attributed to the synergic effect of trimetallic compounds, Pt, Ni, and Rh.	[Ferreira, Hadla S.; Almeida, Caio V. S.; Eguiluz, Katlin I. B.; Salazar-Banda, Giancarlo R.] Inst Tecnol & Pesquisa, Lab Eletroquim & Nanotecnol, BR-49032490 Aracaju, SE, Brazil; [Gocyla, Martin; Heggen, Marc; Dunin-Borkowski, Rafal E.] Forschungszentrum Julich, Ernst Ruska Ctr Microscopy & Spect Electron, D-52425 Julich, Germany; [Gocyla, Martin; Heggen, Marc; Dunin-Borkowski, Rafal E.] Forschungszentrum Julich, Peter Grunberg Inst, D-52425 Julich, Germany; [Ferreira, Hadma S.; Araujo, Rennan G. O.] Univ Fed Bahia, Inst Quim, Campus Univ Ondina, BR-40290170 Salvador, BA, Brazil; [Almeida, Caio V. S.; Eguiluz, Katlin I. B.; Salazar-Banda, Giancarlo R.] Univ Tiradentes, Programa Posgrad Engn Proc, BR-49032490 Aracaju, SE, Brazil; [Strasser, Peter] Tech Univ Berlin, Dept Chem, Str 17 Juni 124, D-10623 Berlin, Germany	Helmholtz Association; Research Center Julich; Helmholtz Association; Research Center Julich; Universidade Federal da Bahia; Universidade Tiradentes; Technical University of Berlin	Salazar-Banda, GR (autor correspondente), Inst Tecnol & Pesquisa, Lab Eletroquim & Nanotecnol, BR-49032490 Aracaju, SE, Brazil.; Salazar-Banda, GR (autor correspondente), Univ Tiradentes, Programa Posgrad Engn Proc, BR-49032490 Aracaju, SE, Brazil.		Ferreira, Hadla Sousa/B-4045-2019; Salazar-Banda, Giancarlo Richard/A-5365-2008; Heggen, Marc/AAN-2888-2021; Dunin-Borkowski, Rafal/G-5597-2012; Almeida, Caio/HTQ-9011-2023; EGUILUZ, KATLIN IVON BARRIOS/V-3827-2019; Strasser, Peter/ABE-6795-2020	Ferreira, Hadla Sousa/0000-0001-5524-7447; Salazar-Banda, Giancarlo Richard/0000-0002-3252-1746; Heggen, Marc/0000-0002-2646-0078; Dunin-Borkowski, Rafal/0000-0001-8082-0647; Almeida, Caio/0000-0001-7198-720X; EGUILUZ, KATLIN IVON BARRIOS/0000-0002-4612-8590; Strasser, Peter/0000-0002-3884-436X; Reis, AlessanRSS/0000-0001-8486-7469	Brazilian National Council of Technological and Scientific Development (CNPq, Brazil) [303630/2012-4, 474261/2013-1, 407274/2013-8, 402243/2012-9, 400443/2013-9, 310366/2018-6, 310282/2013-6]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES, Brazil) [001]; Fundacao de Apoio a Pesquisa e a Inovacao Tecnologica do Estado de Sergipe (FAPITEC, Brazil); Deutsche Forschungsgemeinschaft (DFG) [STR 596/5-2, HE 7192/1-1, 7192/1-2]	Brazilian National Council of Technological and Scientific Development (CNPq, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES, Brazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Apoio a Pesquisa e a Inovacao Tecnologica do Estado de Sergipe (FAPITEC, Brazil); Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG))	The authors thank the Brazilian National Council of Technological and Scientific Development (CNPq, Brazil, grants: 303630/2012-4, 474261/2013-1, 407274/2013-8, 402243/2012-9, 400443/2013-9 and 310366/2018-6, 310282/2013-6), to the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES, Brazil, grant: 001) and Fundacao de Apoio a Pesquisa e a Inovacao Tecnologica do Estado de Sergipe (FAPITEC, Brazil) for the scholarships and financial support for this work. Financial support of the Deutsche Forschungsgemeinschaft (DFG) grant STR 596/5-2, HE 7192/1-1 and 7192/1-2 is gratefully acknowledged.	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Nanosci. Nanotechnol.	OCT	2020	20	10					6274	6285		10.1166/jnn.2020.18559	http://dx.doi.org/10.1166/jnn.2020.18559			12	Chemistry, Multidisciplinary; Nanoscience & Nanotechnology; Materials Science, Multidisciplinary; Physics, Applied; Physics, Condensed Matter	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Science & Technology - Other Topics; Materials Science; Physics	LM2IY	32384977				2023-06-23	WOS:000532076600035
J	Kerber, L; Martinelli, AG; Rodrigues, PG; Ribeiro, AM; Schultz, CL; Soares, MB				Kerber, Leonardo; Martinelli, Agustin G.; Rodrigues, Pablo Gusmao; Ribeiro, Ana Maria; Schultz, Cesar Leandro; Soares, Marina Bento			NEW RECORD OF PROZOSTRODON BRASILIENSIS (EUCYNODONTIA: PROZOSTRODONTIA) FROM ITS TYPE-LOCALITY (UPPER TRIASSIC, SOUTHERN BRAZIL): COMMENTS ON THE ENDOCRANIAL MORPHOLOGY	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						Eucynodontia; mu CT-Scan; endocranial anatomy; nasal cavity; vomer	GRANDE-DO-SUL; PARANA BASIN; THERAPSIDA; CYNODONT; TRITHELEDONTIDAE; BONAPARTE; SEQUENCE; ANATOMY; BRAIN	Here we described anew specimen (UFRGS-PV-0543-T) of the non-mamaliaform cynodont Prozostrodon brasiliensis, collected in the Faixa Nova locality (Santa Maria City, State of Rio Grande do Sul, Brazil), which is referred to the Upper Triassic, Hyperodapedon Assemblage Zone. The new specimen includes a portion of the cranium (fragmented nasals, lacrimals, prefrontals, frontals, palatines, vomer, and fragments of the right premaxilla, left maxilla, and pterygoid), preserving the natural endocast of the nasal cavity, and a fragmented right dentary. The specimen is assigned to P. brasiliensis based on the absence of the postorbital bar, the shape and extension of the snout, the height of the horizontal ramus of the dentary, the position of the Meckelian groove, the morphology of the last postcanine (the only one with the crown partially preserved), and fitting size. The natural endocast is composed of sediment that filled in the nasal cavity. On the dorsal surface of the endocast, there is a longitudinal median sulcus formed by the median bony ridge. Laterally to this median sulcus, there is a longitudinal sulcus on each side formed by the lateral crests. The vomer is low and robust, tapering anteriorly and showing a dorsal groove along its entire length. Other aspects of the endocranial anatomy of UFRGS-PV-0543-T, including wide olfactory region and marked ovalshaped olfactory bulbs, are similar to those of other Late Triassic probainognathian cynodonts.	[Kerber, Leonardo] Univ Fed Santa Maria UFSM, Ctr Apoio Pesquisa Paleontol Quarta Colonia CAPPA, Sao Joao Do Polesine, RS, Brazil; [Kerber, Leonardo] Coordenacao Ciencias Terra & Ecol, Museu Paraense Emilio Goeldi, Belem, Para, Brazil; [Martinelli, Agustin G.] Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat Bernardino Rivadavia, Av Angel Gallardo 470,C1405 DJR, Buenos Aires, DF, Argentina; [Rodrigues, Pablo Gusmao; Schultz, Cesar Leandro] Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias, Porto Alegre, RS, Brazil; [Ribeiro, Ana Maria] Secretaria Meio Ambiente & Infraestrutura, Museu Ciencias Nat, Seca Paleontol, Porto Alegre, RS, Brazil; [Soares, Marina Bento] Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Museu Nacl, Rio De Janeiro, RJ, Brazil	Universidade Federal de Santa Maria (UFSM); Museu Paraense Emilio Goeldi; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio de Janeiro	Kerber, L (autor correspondente), Univ Fed Santa Maria UFSM, Ctr Apoio Pesquisa Paleontol Quarta Colonia CAPPA, Sao Joao Do Polesine, RS, Brazil.; Kerber, L (autor correspondente), Coordenacao Ciencias Terra & Ecol, Museu Paraense Emilio Goeldi, Belem, Para, Brazil.	leonardokerber@gmail.com; agustin_martinelli@yahoo.com.ar; pablogr@bol.com.br; ana-ribeiro@sema.rs.gov.br; cesar.schultz@ufrgs.br; marina.soares@mn.ufrj.br	Ribeiro, Ana Maria/O-3345-2017; Kerber, Leonardo/M-3969-2019; Kerber, Leonardo/O-3980-2017	Ribeiro, Ana Maria/0000-0003-4167-8558; Kerber, Leonardo/0000-0001-8139-1493; Kerber, Leonardo/0000-0001-8139-1493; Martinelli, Agustin/0000-0003-4489-0888; Rodrigues, Pablo/0000-0003-3665-6522	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul [FAPERGS 17/25510000816-2]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq 422568/2018-0, 309414/2019-9]; PalSIRP Sepkoski Grants (2018); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET-Argentina); CNPq [306951/2017-7, 307711/20170, 307938/2019-0]; FAPERGS [19/2551-0000719-1]; FAPERJ [211.425/2019]	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); PalSIRP Sepkoski Grants (2018); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET-Argentina)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPERGS(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	L.K. is supported by the Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS 17/25510000816-2), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq 422568/2018-0; 309414/2019-9), PalSIRP Sepkoski Grants (2018); A.G.M. by Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET-Argentina); A.M. Ribeiro by CNPq (306951/2017-7); C.L. Schultz by CNPq (307711/20170) and FAPERGS (19/2551-0000719-1) and M.B. Soares by CNPq (307938/2019-0) and FAPERJ (211.425/2019). Comments by C. Kammerer and F. Abdala improved considerably the manuscript.	Abdala F, 2010, PALAEOGEOGR PALAEOCL, V286, P202, DOI 10.1016/j.palaeo.2010.01.011; [Anonymous], 2006, MAP GEOL EST RIO GRA; Barberena MC, 1987, AN 10 C BRAS PAL RIO, P67; Brust ACB, 2018, PLOS ONE, V13, DOI 10.1371/journal.pone.0201450; Bonaparte J. F., 1966, ACTA GEOL GICA LILLO, V8, P5; BONAPARTE JF, 1975, J PALEONTOL, V49, P931; Bonaparte JF, 2001, PALAEONTOLOGY, V44, P623, DOI 10.1111/1475-4983.00194; Bonaparte Jose F., 2005, Revista Brasileira de Paleontologia, V8, P25; Bonaparte Jose F., 2003, Revista Brasileira de Paleontologia, V5, P5; Bonaparte Jose F., 2001, Bulletin of the Museum of Comparative Zoology, V156, P59; Botha-Brink J, 2018, PEERJ, V6, DOI 10.7717/peerj.5029; BRINK A. 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J	de Souza, LSL; Campos, RD; Alves, VD; Cerqueira, TLO; da Silva, TM; Teixeira, LSG; Feitosa, ACR; Alves, CDD; Ramos, HE				Leone de Souza, Luciana Sant'Ana; Campos, Renata de Oliveira; Alves, Vitor dos Santos; Oliveira Cerqueira, Taise Lima; da Silva, Thiago Magalhaes; Gomes Teixeira, Leonardo Sena; Rodrigues Feitosa, Alina Coutinho; Dantas Alves, Cresio de Aragao; Ramos, Helton Estrela			Hypertension and Salt-Restrictive Diet Promotes Low Urinary Iodine Concentration in High-Risk Pregnant Women: Results from a Cross-Sectional Study Conducted After Salt Iodination Reduction in Brazil	BIOLOGICAL TRACE ELEMENT RESEARCH			English	Article						Iodine; Iodine deficiency; Pregnancy	NUTRITIONAL-STATUS; THYROID-DISEASE; DEFICIENCY; ASSOCIATION; PREVENTION; GUIDELINES; DIAGNOSIS; OUTCOMES	During pregnancy, the demand for daily iodine increases by 50-70% which occurs to reach around 250 mu g/day. Limited information is available on the association of high-risk pregnancy (HRP) with urinary iodine concentration (UIC) and variables such as socioeconomic factors. To analyze iodine nutritional status and socioeconomic, demographic and anthropometric characteristics among women with HRP screened at the main referral public health center at Bahia, Brazil, a cross-sectional study was conducted in 241 women with HRP (15-46 years old) in Salvador, Bahia, Brazil. The median UIC (MUIC) was 119 mu g/L (25-75th, 58.7-200.4 mu g/L), indicating mild iodine deficiency. Low UIC (< 150 mu g/L) was detected in 61.8% (n = 149) - 18.3% between 100 and 150 mu g/L, 24.5% between 50 and 100 mu g/L, and 19.1% with UIC < 50 mu g/L. Overall, 53% (n = 128) of our population adhered to a low-salt diet, and 32.5% (n = 77) had hypertension. Among the 73% of hypertensive women adhering to a salt-restricted diet, there was a 112% increased risk of iodine deficiency observed (OR = 2.127; 95% confidence interval [1.178-3.829];p = 0.011). Adhering to a salt-restricted diet was associated with iodine deficiency (OR = 1.82; 95% confidence interval [1.073-3.088], p = 0,026). Hypertension and salt restriction diet significantly increased susceptibility for iodine deficiency in HRP. Therefore, low-salt diet when prescribed to pregnant women (PW) might be carefully followed by iodine nutritional status assessment or universal preconception iodine supplementation.	[Leone de Souza, Luciana Sant'Ana; Campos, Renata de Oliveira; Alves, Vitor dos Santos; Oliveira Cerqueira, Taise Lima; Ramos, Helton Estrela] Univ Fed Bahia, Hlth & Sci Inst, Dept Bioregulat, Ave Reitor Miguel Calmon S-N,Room 301, Salvador, BA, Brazil; [Leone de Souza, Luciana Sant'Ana; Campos, Renata de Oliveira; Dantas Alves, Cresio de Aragao; Ramos, Helton Estrela] Univ Fed Bahia, Postgrad Program Interact Proc Organs & Syst, Hlth & Sci Inst, Salvador, BA, Brazil; [Leone de Souza, Luciana Sant'Ana] Escola Bahiana Med & Saude Publ, Salvador, BA, Brazil; [Campos, Renata de Oliveira; Rodrigues Feitosa, Alina Coutinho] Univ Fed Reconcavo Bahia, Santo Antonio De Jesus, BA, Brazil; [da Silva, Thiago Magalhaes] Southwestern State Univ Bahia, Dept Biol Sci, Jequie, BA, Brazil; [Gomes Teixeira, Leonardo Sena] Univ Fed Bahia, Inst Chem, Salvador, BA, Brazil; [Rodrigues Feitosa, Alina Coutinho] Maternidade Prof Jose Maria de Magalhaes Netto, Salvador, BA, Brazil; [Dantas Alves, Cresio de Aragao] Univ Fed Bahia, Dept Pediat, Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Escola Bahiana de Medicina e Saude Publica; Universidade Federal do Reconcavo da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia	Ramos, HE (autor correspondente), Univ Fed Bahia, Hlth & Sci Inst, Dept Bioregulat, Ave Reitor Miguel Calmon S-N,Room 301, Salvador, BA, Brazil.; Ramos, HE (autor correspondente), Univ Fed Bahia, Postgrad Program Interact Proc Organs & Syst, Hlth & Sci Inst, Salvador, BA, Brazil.	ramoshelton@gmail.com	Alves, Vitor/AAI-3692-2021; S. Alves, Vitor/AGO-5987-2022; Feitosa, Alina CR/B-5198-2013; Ramos, Helton E/H-7622-2012; Teixeira, Leonardo S G/J-9131-2016; da Silva, Thiago Magalhães/ITT-1917-2023	S. 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Trace Elem. Res.	OCT	2020	197	2					445	453		10.1007/s12011-020-02028-8	http://dx.doi.org/10.1007/s12011-020-02028-8			9	Biochemistry & Molecular Biology; Endocrinology & Metabolism	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Endocrinology & Metabolism	MZ7IP	31933280				2023-06-23	WOS:000559301300012
J	Lucio, T; Neto, JAS; Selby, D				Lucio, Thales; Souza Neto, Joao Adauto; Selby, David			Late Barremian/Early Aptian Re-Os age of the Ipubi Formation black shales: Stratigraphic and paleoenvironmental implications for Araripe Basin, northeastern Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Geochronology; Rhenium-osmium; Barremian-Aptian boundary; Restricted marine	EARLY CRETACEOUS PALEOGEOGRAPHY; ORGANIC-RICH SEDIMENTS; SANTANA FORMATION; CRATO FORMATION; OSMIUM-ISOTOPE; U-PB; SOUTH ATLANTIC; BREAK-UP; SYSTEMATICS; RHENIUM	The Ipubi Formation of the Santana Group, Araripe Basin, Brazil, is characterized by black shales and overlying evaporite deposits and is suggested to record the transition from lacustrine to marine depositional environments. To date, the age of the black shales, constrained only by microfossils, is poorly determined, with ages spanning similar to 25 myrs from 125 to 100.5 Ma (Aptian-Albian). Here we present new Re-Os elemental and isotopic data to provide the first absolute age for those rocks of the Ipubi Formation and an improved understanding of the depositional paleoenvironment of the Araripe Basin. The Re-Os isotope data for Ipubi Formation black shales yields a depositional age of 123 +/- 3.5 Ma, with a highly radiogenic initial Os-187/ Os-188 composition (Os-i) of 1.97 +/- 0.02. The Re-Os age indicates that the deposition of the Ipubi Formation black shales occurred during the Late Barremian/Early Aptian, prior to the onset of OAE 1a, in a highly restricted marine/lacustrine setting.	[Lucio, Thales; Souza Neto, Joao Adauto] Univ Fed Pernambuco, Dept Geol, Geochem Lab Appl Petr, Grad Program Geosci, BR-50740550 Recife, PE, Brazil; [Selby, David] Univ Durham, Dept Earth Sci, Durham DH1 3LE, England; [Selby, David] China Univ Geosci, Sch Earth Resources, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Hubei, Peoples R China	Universidade Federal de Pernambuco; N8 Research Partnership; Durham University; China University of Geosciences	Lucio, T (autor correspondente), Univ Fed Pernambuco, Ctr Tecnol & Geociencias, Dept Geol, Av Arquitetura S-N,Cidade Univ, BR-50740550 Recife, PE, Brazil.	thales.lucio@ufpe.br; adauto@ufpe.br	Silva, Thales/HHM-4282-2022; Neto, João Adauto Souza/AAG-6672-2021; Souza Neto, João Adauto/D-6810-2016	Neto, João Adauto Souza/0000-0002-9870-7113; Souza Neto, João Adauto/0000-0002-9870-7113; Lucio, Thales/0000-0002-2740-8335	Petrobras [25, 0050.0023165.06.4]; PRH-26 (Human Resources Program of the AnP) [48610.013803/2009-19]; CNPq [312.275/2017-0]; TOTAL Endowment Fund; Dida Scholarship (CUG Wuhan)	Petrobras(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); PRH-26 (Human Resources Program of the AnP); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); TOTAL Endowment Fund; Dida Scholarship (CUG Wuhan)	We gratefully acknowledge Petrobras (Agreement N 25, Cooperation term 0050.0023165.06.4) and PRH-26 (Human Resources Program of the AnP: process number 48610.013803/2009-19) for research funding. TL and JASN are grateful to the mining engineer Flavia Bastos from Campevi Mine for mine access and assistance during the sampling, and to Dr. Juliana Marques Charao for advices concerning sampling. JASN is also grateful to CNPq for his research grant (process number 312.275/2017-0). DS acknowledges the TOTAL Endowment Fund and the Dida Scholarship (CUG Wuhan) and Antonia Hoffman, Geoff Nowell, and Chris Ottley for analytical support.	Algeo TJ, 2004, CHEM GEOL, V206, P289, DOI 10.1016/j.chemgeo.2003.12.009; Ancelmi M.F., 2016, THESIS U ESTADUAL CA, P159; Antonietto LS, 2012, J PALEONTOL, V86, P659, DOI 10.1666/11-012R.1; Arai M., 2012, 46 C BRAS GEOL; Arai M., 1990, 1 S BAC AR BAC INT N; Arai M, 2014, BRAZ J GEOL, V44, P339, DOI 10.5327/Z2317-4889201400020012; ARTHUR MA, 1990, NATO ADV SCI I C-MAT, V304, P75; Assine M. 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South Am. Earth Sci.	OCT	2020	102								102699	10.1016/j.jsames.2020.102699	http://dx.doi.org/10.1016/j.jsames.2020.102699			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MS0ST		Green Accepted			2023-06-23	WOS:000553997400041
J	Marimon, RS; Trouw, RAJ; Dantas, EL				Marimon, Rodrigo S.; Trouw, Rudolph A. J.; Dantas, Elton L.			Significance of age periodicity in the continental crust record: The Sao Francisco Craton and adjacent Neoproterozoic orogens as a case study	GONDWANA RESEARCH			English	Review						Periodicity of the crustal age record; Secular isotopic variation; Regional and global tectonics; Sao Francisco Craton; Neoproterozoic orogens	U-PB GEOCHRONOLOGY; SOUTHERN BRASILIA OROGEN; SOCORRO-GUAXUPE NAPPE; CENTRAL RIBEIRA BELT; SM-ND DATA; DETRITAL ZIRCON GEOCHRONOLOGY; HIGH-GRADE METAMORPHISM; SALVADOR-CURACA BLOCK; STYLE PLATE-TECTONICS; NORTH CHINA CRATON	The Sao Francisco Craton, in Brazil, together with adjacent orogenic systems formed during Gondwana assemblage, are well-suited for the study of crustal growth processes. The region's geological history is marked by a series of complete tectono-metamorphic cycles, from the Archean to late Neoproterozoic, comprising arc-related magmatism followed by continental collisions and ultimately post-tectonic igneous events and rifting. In this contribution, a comprehensive isotopic database was compiled from the literature, composed mainly of high quality U-Pb magmatic and metamorphic ages (ca. 1000), together with Lu-Hf (ca. 1300) and Sm-Nd (ca. 300) data. Using this database, combined with a tectonic/geochemical synthesized review of the region, it is possible to test which of the available contending models can better explain the apparent periodicity in the formation of the continental crustal. Some interpreted the peaks and troughs in the crustal age record as periods of increased magmatic production, controlled by periodic mantellic events. Another hypothesis is that subduction-related rocks are shielded from tectonic erosion after continental amalgamation, the peaks thus reflecting enhanced preservation potential. The latter hypothesis is favored, as the variability regarding the timing of arc-related peak magmatic production (U-Pb age peaks) from different tectonic provinces around the globe and in the considered regions, coupled to the fact that peak arc-production is always closely followed in time by major continental amalgamations (supercontinent formation), precludes a unified global causation effect, such as mantellic overturns or slab avalanches, and supports the preservation bias hypothesis. Furthermore, the worldwide (including the Sao Francisco Craton) occurrence of plume-related magmatism is concentrated during the periods of supercontinent break-up (i.e. after major collisions), which better relates to a top-down control on mantle convection and opposes most of the models that advocate for the primary periodicity of magmatic production, which predict enhanced plume activity slightly prior or concomitant to supercontinent formation events. (c) 2020 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.	[Marimon, Rodrigo S.; Trouw, Rudolph A. J.] Univ Fed Rio de Janeiro, Inst Geociencias, BR-21949900 Rio De Janeiro, RJ, Brazil; [Dantas, Elton L.] Univ Brasilia, Lab Estudos Geodinam & Ambientais, BR-70297400 Brasilia, DF, Brazil	Universidade Federal do Rio de Janeiro; Universidade de Brasilia	Marimon, RS (autor correspondente), Univ Fed Rio de Janeiro, Inst Geociencias, BR-21949900 Rio De Janeiro, RJ, Brazil.	rsmarimon@hotmail.com	Marimon, Rodrigo Schwantes/AAB-5863-2021; Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059; Schwantes Marimon, Rodrigo/0000-0001-6157-8031	CAPES; National Council for Scientific and Technological Development (CNPq)	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	R.S. Marimon acknowledges a PhD scholarship provided by CAPES. R.A.J Trouw thanks the National Council for Scientific and Technological Development (CNPq) for financial support. Careful editorial handling by Prof. Sebastian Tappe and suggestions by anonymous reviewers are greatly acknowledged.	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OCT	2020	86						144	163		10.1016/j.gr.2020.05.010	http://dx.doi.org/10.1016/j.gr.2020.05.010			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NK9GT					2023-06-23	WOS:000567037800008
J	Mouro, LD; Pacheco, MLAF; Ricetti, JHZ; Scomazzon, AK; Horodyski, RS; Fernandes, ACS; Carvalho, MA; Weinschutz, LC; Silva, MS; Waichel, BL; Scherer, CMS				Mouro, Lucas D.; Alves Forancelli Pacheco, Mirian Liza; Ricetti, Joao H. Z.; Scomazzon, Ana K.; Horodyski, Rodrigo S.; Fernandes, Antonio C. S.; Carvalho, Marcelo A.; Weinschutz, Luiz C.; Silva, Mateus S.; Waichel, Breno L.; Scherer, Claiton M. S.			Lontras Shale (Parana Basin, Brazil): Insightful analysis and commentaries on paleoenvironment and fossil preservation into a deglaciation pulse of the Late Paleozoic Ice Age	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Late Paleozoic; Western Gondwana; Fjord Bay; Fossildiagenesis	ORGANIC PRESERVATION; WESTERN GONDWANA; ITARARE GROUP; SPONGE; OXYGEN; CONSTRAINTS; CONCRETIONS; GLACIATION; DEPOSITION; DIVERSITY	The Lontras Shale is a fossil site located in Mafra, Santa Catarina, south of Brazil. This Late Paleozoic (Pennsilvanian - Cisularian) stratum holds an important place with great potential for the synthesis of knowledge about paradigmatic events that happened on Gondwana. This marine fossil site, preserved into a 1.1 m black shale, comprises a combination of different kinds of preservation, in broad taphonomical spectra, including hard and/or soft-tissues of aquatic (e.g., fishes, poriferans and ammonoids) and terrestrial biotas (e.g., insect and woods), among other organisms that were well preserved under still unrevealed process and conditions. Considering the prevailing depositional settings and aiming to present fossil diagenetic aspects that led to some special preservation modes, we performed chemical analyses of sponges and insects by means of energy-dispersive spectroscopy (EDS), synchrotron micro-X-ray fluorescence (micro-XRF) and Raman spectroscopy. To date, we have identified the majority of fossils preserved as carbonaceous compressions or phosphatized forms. The well-preserved fossils have so far permitted new insights into metazoan evolution, especially regarding Insecta, Porifera, and Conodonta. Our findings not only allow suggestions regarding the chemical remains of soft tissues on these specimens but also can provide background data for future analyses of these groups in similar depositional settings.	[Mouro, Lucas D.; Waichel, Breno L.] Univ Fed Santa Catarina, Dept Geol, Posgrad Geol, PFRH PB 240, BR-88040900 Florianopolis, SC, Brazil; [Mouro, Lucas D.; Fernandes, Antonio C. S.; Carvalho, Marcelo A.] Univ Fed Rio de Janeiro, Dept Geol & Paleontol, Museu Nacl, BR-20940040 Rio De Janeiro, RJ, Brazil; [Alves Forancelli Pacheco, Mirian Liza] Univ Fed Sao Carlos, Dept Biol, Lab Estudos Paleobiol, Campus Sorocoaba, BR-18052780 Sorocaba, SP, Brazil; [Alves Forancelli Pacheco, Mirian Liza] Univ Sao Paulo, Inst Fis, Dept Fis Nucl, R Mateo 1371, BR-05508090 Sao Paulo, SP, Brazil; [Ricetti, Joao H. Z.; Scomazzon, Ana K.; Weinschutz, Luiz C.; Scherer, Claiton M. S.] Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, BR-91501970 Porto Alegre, RS, Brazil; [Ricetti, Joao H. Z.] Univ Contestado, Ctr Paleontol, BR-89300000 Mafra, SC, Brazil; [Horodyski, Rodrigo S.] Univ Vale Rio dos Sinos, Geol Grad Program, BR-93022750 Sao Leopoldo, RS, Brazil; [Silva, Mateus S.] Univ Fed Santa Catarina, PFRH PB 240, BR-88040900 Florianopolis, SC, Brazil	Universidade Federal de Santa Catarina (UFSC); Universidade Federal do Rio de Janeiro; Universidade Federal de Sao Carlos; Universidade de Sao Paulo; Universidade Federal do Rio Grande do Sul; Universidade do Contestado; Universidade do Vale do Rio dos Sinos (Unisinos); Universidade Federal de Santa Catarina (UFSC)	Mouro, LD (autor correspondente), Univ Fed Santa Catarina, Dept Geol, Posgrad Geol, PFRH PB 240, BR-88040900 Florianopolis, SC, Brazil.	lucas.delmouro@gmail.com	Horodyski, Rodrigo Scalise/A-3605-2014; Pacheco, Mírian LAF/P-3074-2014; Del Mouro, Lucas/AAY-4784-2021; Fernandes, Antonio C S/G-8455-2015	Horodyski, Rodrigo Scalise/0000-0001-7195-2170; Santos Scherer, Claiton Marlon dos/0000-0002-7520-1187; Del Mouro, Lucas/0000-0001-7829-0683; Ricetti, Joao Henrique Zahdi/0000-0003-3142-3869	Programa de Formacao em Recursos Humanos em Geologia da Petrobras [PFRH-PB 240]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [140446/2016-8]; Museu Nacional; Universidade Federal de Santa Catarina; Universidade Federal do Rio Grande do Sul; Universidade do Contestado	Programa de Formacao em Recursos Humanos em Geologia da Petrobras; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Museu Nacional; Universidade Federal de Santa Catarina; Universidade Federal do Rio Grande do Sul; Universidade do Contestado	This work had the financial support of Programa de Formacao em Recursos Humanos em Geologia da Petrobras (PFRH-PB 240), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), processo 140446/2016-8. We appreciate and are thankful for the support of the Museu Nacional, Universidade Federal de Santa Catarina, Universidade Federal do Rio Grande do Sul, Universidade do Contestado during all work phases. We also acknowledge the AstroLab (Laboratory of Astrobiology - Institute of Chemistry, USP) for providing research facilities to conduct the Raman spectroscopic analysis. We would like to thank LNLS/CNPEM for technical support and for providing infrastructure, in particular for allowing the use of the XRF beamline (proposal 20190140). To Neal S. Gupta for the kind permission of image use. To Katrin Treppow and the Terra Mineralia for providing access to the facilities.	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Paleoclimatol. Paleoecol.	OCT 1	2020	555								109850	10.1016/j.palaeo.2020.109850	http://dx.doi.org/10.1016/j.palaeo.2020.109850			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	MP3WW					2023-06-23	WOS:000552137900012
J	Ribeiro, V; Guerra-Sommer, M; Menegat, R; Kuhn, LA; Simoes, JC; Braga, RB; Bauermann, SG; da Silva, WG				Ribeiro, Veridiana; Guerra-Sommer, Margot; Menegat, Rualdo; Kuhn, Lidia Aumond; Simoes, Jefferson Cardia; Braga, Ricardo Burgo; Bauermann, Soraia Girardi; da Silva, Wagner Guimaraes			FIRE EVENTS AND VEGETATION DYNAMICS DURING THE LATE PLEISTOCENE-MEGHALAYAN INTERVAL IN THE SOUTHERNMOST BRAZILIAN COASTAL PLAIN	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						charcoal peak; palynology; climate; Holocene	LATE QUATERNARY VEGETATION; SEDIMENT-CHARCOAL RECORDS; POLLEN REPRESENTATION; POACEAE POLLEN; CLIMATE-CHANGE; SOURCE AREA; HISTORY; FOREST; BASIN; WILDFIRES	The present study analyzes the correspondence between charcoal concentrations and changes in the palynological composition in a core from Aguas Claras peatland (30 degrees 06'24.39 '' S; 50 degrees 49'04.90 '' W) in the coastal plain of southernmost Brazil (Rio Grande do Sul state) from approximately 38,900 yrs BP until 1,500 yrs BP. The dominance of grassland vegetation (mainly Poaceae) in Late Pleistocene sediments persisted into the Holocene during the development of a peatland. Analysis of fragment size distribution and concentration were useful to discriminate local fires from regional wildfires. Late Pleistocene regional fires registered in shallow pond deposits (older than 21,545 cal yrs BP) were distinguished from a local Holocene fire by the presence of higher proportions of small particles in charcoal assemblages. A charcoal peak related to a natural fire signal, composed by high concentration of charcoal with larger diameters, was identified at the topmost level of the peat facies (1,590-1,515 cal yrs BP). Correlated with palynological data, this charcoal peak originated by local fires indicates a change in vegetation during a dry climate interval that occurred around 1,500-1,600 yrs BP.	[Ribeiro, Veridiana] Univ Fed Rio Grande do Sul UFRGS, Programa Posgrad Geog, Ctr Polar & Climat, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Guerra-Sommer, Margot] Univ Fed Rio Grande do Sul, Programa Posgrad Geog, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Menegat, Rualdo] Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Kuhn, Lidia Aumond] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul, Programa Posgrad Geog, Inst Geociencias, Ctr Polar & Climat, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Braga, Ricardo Burgo] Univ Fed Rio Grande do Sul, Lab Gerenciamento Costeiro, Inst Geociencias, Ctr Estudos Geol Costeira & Ocean, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Bauermann, Soraia Girardi] Univ Luterana Brasil, Lab Palinol, Av Farroupilha 8001, BR-92425900 Canoas, RS, Brazil; [da Silva, Wagner Guimaraes] Inst Fed Educ Ciencia & Tecnol Rio Grande do Sul, Campus Restinga,Rua Alberto Hoffmann 285, BR-91791508 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Luterana do Brasil; Instituto Federal do Rio Grande do Sul (IFRS)	Ribeiro, V (autor correspondente), Univ Fed Rio Grande do Sul UFRGS, Programa Posgrad Geog, Ctr Polar & Climat, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	very.ribeiro@yahoo.com.br; margot.sommer@ufrgs.br; rualdo.menegat@ufrgs.br; lidiaak.lak@gmail.com; jefferson.simoes@ufrgs.br; burgobraga@gmail.com; soraia.bauermann@ulbra.br; wagner.guimaraes.silva@gmail.com	Simoes, Jefferson Cardia/D-7232-2013; Sommer, Margot Guerra/C-4951-2013	Simoes, Jefferson Cardia/0000-0001-5555-3401; Sommer, Margot Guerra/0000-0002-9517-4593; Ribeiro, Veridiana/0000-0001-7549-7697; Kuhn, Lidia/0000-0003-2120-1824; Guimaraes da Silva, Wagner/0000-0002-6356-6445; Burgo Braga, Ricardo/0000-0002-8696-8199; Girardi Bauermann, Soraia/0000-0001-7351-5847	INCT-Criosfera [CNPq 465680/2014-3, 573720/2008-8, FAPERGS 17/2551-0000518-0]	INCT-Criosfera	We thank Centro Polar e Climatico, Departamento de Paleontologia e Estratigrafia, the Centro de Estudos de Geologia Costeira e Oceanica and the Instituto de Geociencias of the Universidade Federal do Rio Grande do Sul (UFRGS) for field and laboratory assistance. Discussions with N.L.S. Gruber, S.R. Dillenburg and E.G. Barboza significantly improved the manuscript. Funding and scholarships were provided by the INCT-Criosfera (CNPq 465680/2014-3, 573720/2008-8 and FAPERGS 17/2551-0000518-0).	[Anonymous], 1989, J BIOGEOGR; Baptista L.R.D.M., 2012, CHECK LIST, V8, P224, DOI [10.15560/8.2.224, DOI 10.15560/8.2.224]; Barboza E.G., 2005, C ASS BRAS EST QUAT, V10; Barboza E.G., 2003, C ASS BRAS EST QUAT, V9; Barth O. 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J, 1995, NOTAS TE CNICAS, V8; Tomazelli L.J., 1996, ANAIS ACAD BRASILEIR, V68, P373; Torgan L.C., 2001, SERIE BOT, V56, P147; Uhl D, 2004, PALAEOGEOGR PALAEOCL, V207, P23, DOI 10.1016/j.palaeo.2004.01.019; Uhl D, 2011, GEOL J, V46, P34, DOI 10.1002/gj.1229; Villwock J.A, 1986, QUATERNARY S AM ANTA, P79; Walker M, 2018, EPISODES, V41, P213, DOI 10.18814/epiiugs/2018/018016; Walker R. G., 1992, FACIES MODELS RESPON, V1992, P1, DOI DOI 10.1016/J.EPSL.2006.03.014; Walker R.G., 2006, SPECIAL PUBLICATIONS, V84, P1; Wetzel R. G., 1975, LIMNOLOGY; Whitlock C, 2004, DEV QUA SCI, V1, P479; Whitlock C, 2007, QUATERNARY RES, V68, P28, DOI 10.1016/j.yqres.2007.01.012; YBERT JP, 1992, B I GEOL USP, V13, P47, DOI DOI 10.5935/0100-929X.19920009	93	0	0	3	8	SOC BRASILEIRA PALEONTOLOGIA	SAO LEOPOLDO	PPGEO UNISINOS, AV UNISINOS 950, SAO LEOPOLDO, RS 93022-000, BRAZIL	1519-7530	2236-1715		REV BRAS PALEONTOLOG	Rev. Bras. Paleontol.	OCT-DEC	2020	23	4					234	250		10.4072/rbp.2020.4.02	http://dx.doi.org/10.4072/rbp.2020.4.02			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	PI8VV		hybrid			2023-06-23	WOS:000601362500002
J	Rocha, HV; Mendes, M; Pereira, Z; Rodrigues, C; Fernandes, P; Lopes, G; Sant'Anna, LG; Tassinari, CCG; de Sousa, MJL				Rocha, H., V; Mendes, M.; Pereira, Z.; Rodrigues, C.; Fernandes, P.; Lopes, G.; Sant'Anna, L. G.; Tassinari, C. C. G.; Lemos de Sousa, M. J.			New palynostratigraphic data of the Irati (Assistencia Member) and the Corumbatai formations, Parana Basin, Brazil, and correlation with other south American basins	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Pollen; Spores; Palynology; Kungurian; Roadian; Permian; Gondwana	PALYNOLOGY; SUBGROUP; ARGENTINA; GONDWANA; URUGUAY; MARGIN; ZONE; AGE	This research presents the palynostratigraphy of organic-rich shales from the Irati and the Corumbatai formations, Parana Basin (PB), Southeastern Brazil, as part of an unconventional hydrocarbon source rock and CO2 reservoir assessment study. Thirty-four samples from the Corumbatai Formation and the Assistencia Member of the Irati Formation were collected in the states of Goias (northern border of the PB), Sao Paulo and Parana (eastern and southern border of the PB, respectively). The acquired data allowed to establish a comprehensive palynostratigraphic study across the basin where a total of 18 pollen genera (34 pollen species), seven spore genera, four microplankton genera (1 species), and Chlorophyceae algae species where identified. The palynostratigraphic analysis also reveals a clear dominance of bisaccate pollen grains such as Corisaccites alutas, Lueckisporites virkkiae, and Weylandites lucifer. The Lueckisporites virkkiae zone was identified in the upper part of the Irati Formation (Assistencia Member) and the lowermost part of the Corumbatai Formation, indicating a Kungurian to Roadian age for this part of the succession. Differences in the Guttulapollenites hannonicus and Tornopollenites toreutos biostratigraphic ranges, recovered in the Corumbatai Formation, suggest an earlier development of these species in the Parana Basin during the middle Permian. Therefore, to evaluate the differences in the first occurrences of key species within the Parana Basin, a close palynostratigraphic correlation between the main Guadalupian-Lopingian South American Gondwana basins is tentatively established.	[Rocha, H., V; Sant'Anna, L. G.; Tassinari, C. C. G.] Univ Sao Paulo, IEE Inst Energia & Ambiente, Av Prof Luciano Gualberto 1289, BR-05508010 Sao Paulo, SP, Brazil; [Rocha, H., V; Rodrigues, C.; Lemos de Sousa, M. J.] Univ Fernando Pessoa, FP ENAS, Praca 9 Abril 349, P-4249004 Porto, Portugal; [Mendes, M.] LNEG, Bairro Vale Oca Apartado 14, P-7601909 Aljustrel, Portugal; [Pereira, Z.] LNEG, Rua Amieira, P-4465965 Mamede De Infesta, Portugal; [Fernandes, P.; Lopes, G.] Univ Algarve, CIMA Ctr Invest Marinha & Ambiental, Campus Gambelas, P-8005130 Faro, Portugal	Universidade de Sao Paulo; Universidade Fernando Pessoa; Laboratorio Nacional de Energia e Geologia IP (LNEG); Laboratorio Nacional de Energia e Geologia IP (LNEG); Universidade do Algarve	Pereira, Z (autor correspondente), LNEG, Rua Amieira, P-4465965 Mamede De Infesta, Portugal.	zelia.pereira@lneg.pt	Mendes, Márcia/E-2897-2019; Fernandes, Paulo/J-6577-2014; Sant'Anna, Lucy Gomes/AAH-4629-2021; Pereira, Zélia/B-2740-2017; Lopes, Gilda/AAS-1742-2020; C.F. Rodrigues, C. Rodrigues/S-6536-2017; Sant'Anna, Lucy Gomes/D-4437-2014	Mendes, Márcia/0000-0003-2290-891X; Fernandes, Paulo/0000-0003-4888-0230; Sant'Anna, Lucy Gomes/0000-0002-4176-7684; Pereira, Zélia/0000-0003-3056-6219; Lopes, Gilda/0000-0002-6866-5127; C.F. Rodrigues, C. Rodrigues/0000-0002-7616-6985; Sant'Anna, Lucy Gomes/0000-0002-4176-7684	RCGI Research Centre for Gas Innovation - FAPESP [2014/50279-4]; Shell; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES)	RCGI Research Centre for Gas Innovation - FAPESP; Shell(Royal Dutch Shell); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors are thankful to Rosa Irene Sousa for the samples palynological preparation, and acknowledge the support of the RCGI Research Centre for Gas Innovation, sponsored by FAPESP (2014/50279-4) and Shell, as well as the financial support of Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES). Editor-in-Chief Andres Folguera, P. A. Souza and an anonymous reviewer are gratefully acknowledged for valuable comments that improved the article.	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South Am. Earth Sci.	OCT	2020	102								102631	10.1016/j.jsames.2020.102631	http://dx.doi.org/10.1016/j.jsames.2020.102631			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MS0ST					2023-06-23	WOS:000553997400004
J	dos Santos, ACS; Guerra-Sommer, M; Degani-Schmidt, I; Siegloch, AM; Carvalho, ID; Mendonca, JG; Mendonca, JD				Scaramuzza dos Santos, Angela Cristine; Guerra-Sommer, Margot; Degani-Schmidt, Isabela; Siegloch, Anelise Marta; Carvalho, Ismar de Souza; Mendonca Filho, Joao Graciano; Mendonca, Joalice de Oliveira			Fungus-plant interactions in Aptian Tropical Equatorial Hot arid belt: White rot in araucarian wood from the Crato fossil Lagerstatte (Araripe Basin, Brazil)	CRETACEOUS RESEARCH			English	Article						Basidiomycetes; Gymnosperms; Wood anatomy; Fungal decay; Fungus-plant interactions	NORTHERN GONDWANA; NORWAY SPRUCE; SP NOV.; MAGNOLIALEAN ANGIOSPERM; CLAMP CONNECTIONS; DISCOLORED WOOD; DECAYING FUNGI; GEN. NOV; SAPWOOD; CONIFER	For the first time, this study describes the dynamics of white rot fungal decay in a petrified conifer branch with clear araucarian affinity from the late Aptian Crato Lagerstatte (Santana Formation, Araripe Basin, northeastern Brazil). High resolution optical microscopy was used to identify tridimensional chemical and anatomical evidence in different regions of the bark and xylem tissues of permineralized shoots, and results support the hypothesis that the host responded to disease that may have started when it was still alive. The wood decay pattern was strongly indicative of the selective decay by white rot. The general pattern of interaction is consistent with pathogenic rather than saprophytic fungal activity. Analysis of fungus-plant interactions associated with growth ring patterns imply intermittent periods of favorable temperature-moisture inputs that were crucial for fungal activity during the deposition of the Crato fossil Lagerstatte included in the Tropical Equatorial Hot arid belt. (C) 2020 Elsevier Ltd. All rights reserved.	[Scaramuzza dos Santos, Angela Cristine; Guerra-Sommer, Margot; Siegloch, Anelise Marta] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, IGEO, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil; [Degani-Schmidt, Isabela] Univ Fed Rio de Janeiro, CCMN IGEO, Programa Posgrad Geol, Av Athos da Silveira Ramos 274,Bloco J1, BR-21941916 Rio De Janeiro, RJ, Brazil; [Carvalho, Ismar de Souza] Univ Fed Rio de Janeiro, CCMN IGEO, Dept Geol, Av Athos da Silveira Ramos 274,Bloco J1, BR-21941916 Rio De Janeiro, RJ, Brazil; [Mendonca Filho, Joao Graciano; Mendonca, Joalice de Oliveira] Univ Fed Rio de Janeiro, CCMN IGEO, Dept Geol, LAFO Lab Palinofaceis & Faceis Organ, Av Athos da Silveira Ramos 274,Bloco J1,Sala 20, BR-21941916 Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro	Guerra-Sommer, M (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, IGEO, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil.	margot.sommer@ufrgs.br	Carvalho, Ismar Souza/G-3603-2012; Sommer, Margot Guerra/C-4951-2013; Degani-Schmidt, Isabela/D-1798-2014; Mendonca Filho, Joao Graciano/C-2098-2013	Carvalho, Ismar Souza/0000-0002-1811-0588; Sommer, Margot Guerra/0000-0002-9517-4593; Degani-Schmidt, Isabela/0000-0001-9415-6230; Mendonca Filho, Joao Graciano/0000-0001-8997-0270	Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com pesquisa e Desenvolvimento" [141323/2017-5, 155508/2018-0, 303596/2016-3]; CNPq; COPPETEC/UFRJ [20758]; FAPERJ [E-26/202.910/2017]	Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com pesquisa e Desenvolvimento"; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); COPPETEC/UFRJ; FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	This study was conducted in association with the ongoing Research & Development project "Correlacao estratigrafica, evolucao paleoambiental e paleogeografica e perspectivasexploratorias do AndarAlagoas, which is registered as ANP 180321 and sponsored by Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com pesquisa e Desenvolvimento". A.C.S.S. (141323/2017-5), M.G.S., A.M.S. (155508/2018-0), I.S.C. (303596/2016-3), J.G.M.F. acknowledge the financial support of CNPq. I.D.S. acknowledges the financial support of COPPETEC/UFRJ n 20758. I.S.C. also acknowledges FAPERJ (E-26/202.910/2017). The authors are also grateful to Rommulo Vieira Conceicao, Ana Maria Pimentel Mizusaki, and Maria Lidia Medeiros Vignol Lelarge for the insightful discussions on mineralogy and geochemistry. Two anonymous referees are also gratefully acknowledged for the assistance with improving the text.	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Res.	OCT	2020	114								104525	10.1016/j.cretres.2020.104525	http://dx.doi.org/10.1016/j.cretres.2020.104525			20	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	MY9FD					2023-06-23	WOS:000558723900024
J	Siepierski, L; Ferreira, CF				Siepierski, Lincoln; Ferreira Filho, Cesar Fonseca			Magmatic structure and petrology of the Vermelho Complex, Carajas Mineral Province, Brazil: Evidence for magmatic processes at the lower portion of a mafic-ultramafic intrusion	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Mafic-ultramafic magmatism; Border zone; Carajas; Lithogeochemistry; Olivine	CU SULFIDE MINERALIZATION; BUSHVELD COMPLEX; CHROMITE DEPOSITS; LAYERED INTRUSION; MARGINAL REVERSAL; CONSTRAINTS; ORIGIN; CRATON; GEOCHRONOLOGY; GEOCHEMISTRY	The Vermelho Complex, located in the Carajas Mineral Province, is part of a cluster of Neoarchean (ca. 2.76 Ga) mafic-ultramafic layered intrusions best known for hosting world-class nickel laterite deposits (e.g., Onca-Puma, Jacare, Vermelho). Resources of nickel laterite hosted by the Vermelho Complex (220 Mt at 1.23 wt% Ni) occur in two plateau-type hills (known as V1 and V2) where a thick (similar to 30-40 m) weathered profile was preserved from erosion. This paper is the first detailed geological and petrological study of the layered rocks of the Vermelho Complex. Results reveal that the intrusive architecture of the Vermelho Complex includes a complex basal sequence of mafic-ultramafic rocks in contact with sialic host rocks, providing further evidence for the variability of marginal lower zones of layered complexes. In addition, our results add new insights into the potential of the Neoarchean mafic-ultramafic magmatism in Carajas to host magmatic deposits. The medium-size (similar to 9.5 km long and similar to 1.5 km wide) Vermelho Complex is a NE-SW trending mafic-ultramafic intrusion emplaced into granitic-gneissic rocks of the Xingu Complex (ca. 3.0 Ga). The magmatic structure consists of a horizontally layered pile of ultramafic rocks (Upper Zone) exposed in the plateau-like hills, overlying a complex but broadly subhorizontal basal sequence of mafic-ultramafic rocks (Lower Zone). The Lower Zone consists of three subzones: (1) interlayered dunite, harzburgite and orthopyroxenite at the base; (2) interlayered orthopymxenite and melanorite; and (3) gabbronorite and quartz-bearing leucogabbronorite in the upper subzone. The crystallization sequence of the Lower Zone consists of olivine + chmmite, orthopyroxene + chmmite, orthopyroxene, orthopymxene + plagioclase, orthopymxene + plagioclase + clinopyroxene, with abundant primitive olivine + chromite ultramafic cumulates in the lower subzone and fractionated quartz-bearing mafic cumulates in the upper subzone. The Lower Zone extends for more than 400 m below the V1 plateau where a conduit-type structure is suggested, and becomes progressively shallower toward the northeast and southwestern portions of the intrusion. Core samples from drill holes that intersect the contact of the ultramafic cumulates and country rocks consist of similar to 50 m of interlayered harzburgites and orthopyroxenites, with no fine-grained chilled margins. The most primitive mineral compositions of ultramafic cumulates occur dozens of meters away from the contact with country rocks, possibly due to fractionation of the parental magma in the feeding system when the first batches of magmas filled the magma chamber. Evidence for fully developed marginal reversals is not indicated by the sequence of cumulates and fractionation trends of the rocks located at the basal contact of the Vermelho Complex. The Upper Zone, just preserved in the V1 and V2 plateaus, consists of two subzones with a total thickness of about 175 m, broadly corresponding to the height of the V1 plateau. The lower subzone consists of up to 50 m thick orthopymxenite with associated chromitite pods. The sharp concordant contact of orthopyroxenite with underlying gabbmic rocks indicates a major break in the fractionation trend. Orthopyroxenite in the Upper Zone is a coarse-to medium-grained orthopyroxene + chromite adcumulate. Chromite occurs mainly as disseminated fine-grained euhedral crystals in orthopyroxenite, but also occurs in few centimeters thick chromite-rich pods or discontinuous layers. The upper subzone (up to 125 m thick) consists of extensively weathered dunite and harzburgite. The sharp contact between lower and upper subzones is well exposed in the slopes of the V1 and V2 hills. Due to pervasive weathering or serpentinization, primary silicates are not preserved in rocks from the upper subzone. Ultramafic rocks are serpentinized dunite and harzburgite with commonly preserved adcumulate to mesocumulate textures indicated by olivine and orthopyroxene pseudomorphs. Chromite, a conspicuous accessory mineral (2-3 vol%) in the serpentinites, occurs as partially altered euhedral crystals. The compositional range of cumulus olivine in the Vermelho Complex (Fo(85.6-90.5)) is comparable with those reported for layered intrusions originated from primitive parental magmas (i.e., high Mg#). The composition of the most primitive cumulus olivine of the Vermelho Complex is also comparable with those reported for olivine in layered intrusions hosting large Ni-laterite deposits in Carajas (e.g., Fo(92) for the Serra da Ono Complex; Fo(89) for the Serra do Puma Complex). The early crystallization of orthopyroxene relative to clinopyroxene in the Vermelho Complex suggests a silica-saturated primitive parental magma. Mantle-normalized incompatible trace element patterns of melanorite and gabbroic rocks of the Vermelho Complex are fractionated, as indicated by relative enrichment in LREE and Th, with pronounced negative Nb and Ta anomalies. These lithogeochemical features, together with the early crystallization of orthopyroxene, may be interpreted as the product of a primitive mantle melt partially contaminated with continental crust. Assimilation of older sialic crust during emplacement and/or ascent of the parental magma of the Vermelho Complex is also supported by Nd model ages between 2.90 and 3.30 Ga and epsilon Nd ((T=2 .77 Ga)) values from -7.3 to +0.1. These results, consistent with a primitive mantle melt variably contaminated with older continental crust, are supported by the crosscutting contact between mafic-ultramafic rocks and older country rocks of the Xingu Complex (ca. 3.0 Ga). The magmatic evolution of the Vermelho Complex is described as the result of two major events of magma emplacement, the first associated with the Lower Zone and the second with the Upper Zone. The sequence of cumulate rocks and orthopyroxene compositions resulting from both magmatic events is similar, suggesting that their parental magmas have close compositions. However, the presence of chromitites just associated with orthopyroxenites at the basal zone of the Upper Zone suggests that, different from the first event, the primitive magma of the second event was chromite-saturated. This scenario is consistent with chromitites resulting of chromite-saturated slurries during the second event of magma emplacement. Mafic-ultramafic intrusions in large igneous provinces are a primary host for magmatic mineralizations, including major Ni-Cu-(PGE) sulfide deposits. Several features commonly used as guidelines for regional exploration for Ni-Cu-(PGE) magmatic deposits, including abundant olivine-rich mafic-ulramafic rocks, dynamic magmatic systems and crustal scale structures, are contemplated in the mafic-ultramafic complexes in Carajas. Although no major magmatic deposits are known in Carajas, the potential for future discoveries in this under-explored region should not be disregarded.	[Siepierski, Lincoln; Ferreira Filho, Cesar Fonseca] Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Siepierski, Lincoln] Univ Fed Goias UFG, Fac Ciencias & Tecnol, Curso Geol, BR-74968755 Goiania, Go, Brazil	Universidade de Brasilia	Ferreira, CF (autor correspondente), Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil.	cesarf@unb.br	Filho, Cesar Ferreira/AAL-2105-2021		CNPq (Conselho Nacional de Desenvolvimento Cientffico e Tecnologico); VALE S.A. [550398/2010-4]	CNPq (Conselho Nacional de Desenvolvimento Cientffico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); VALE S.A.	This study was supported by CNPq (Conselho Nacional de Desenvolvimento Cientffico e Tecnologico) and VALE S.A. (Projeto 550398/2010-4). Analytical facilities at the Instituto de Geociencias of the University of Brasilia (UnB) provided additional support for this research. The authors acknowledge VALE's Exploration Managers for Brazil and Cara.* (Mr. Fernando Greco and Mr. Fernando Matos, respectively) for providing access to drill cores as well as geological and geochemical exploration data. Roberto Albuquerque and Walter Riehl from VALE are acknowledged for their support during fieldwork, interpretation of exploration data and stimulating discussions on the geology of the Cara.* Mineral Province. Cesar F. Ferreira Filho is a Research Fellow of CNPq since 1996, and acknowledges the continuous support through research grants and scholarships for the "Metalogenenese de DepOsitos Associados ao Magmatismo Mafico-Ultramafico" Research Group. This study is part of the first author's (Lincoln Siepierski) Ph.D. thesis developed at the Instituto de Geociencias (UnB). The authors thank the reviewers Dr. Robert Osborne and one anonymous for their constructive and helpful reviews, and Editor-in-Chief Dr. Andres Folguera for carefully handling the manuscript.	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South Am. Earth Sci.	OCT	2020	102								102700	10.1016/j.jsames.2020.102700	http://dx.doi.org/10.1016/j.jsames.2020.102700			25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MS0ST					2023-06-23	WOS:000553997400042
J	Silva, MJ; Soares, SAR; Santos, IDF; Pepe, IM; Teixeira, LR; Pereira, LG; Silva, LBA; Celino, JJ				Silva, Marcio J.; Soares, Sarah A. R.; Santos, Ingrid D. F.; Pepe, Iuri M.; Teixeira, Leandro R.; Pereira, Lucas G.; Silva, Lucas B. A.; Celino, Joil J.			Optimization of the photocatalytic degradation process of aromatic organic compounds applied to mangrove sediment	HELIYON			English	Article						Chromatography; Chemometrics; Physical chemistry; Environmental analysis; Environmental geochemistry; Environmental pollution; Photodegradation; Advanced oxidative processes; Heterogeneous photo catalysis; Experimental design; Multiple response	HYDROCARBONS PAHS; SOIL SURFACES; HETEROGENEOUS PHOTOCATALYSIS; CONTAMINATED SOILS; PHOTODEGRADATION; FUNDAMENTALS; PHENANTHRENE; REMOVAL; PYRENE; TIO2	Polycyclic aromatic hydrocarbons (PAHs) are part of a class of organic compounds resistant to natural degradation. In this way, heterogeneous photocatalysis becomes useful to degrade persistent organic pollutants, however it can be influenced by environmental variables (i.e.: organic matter) and experimental factors such as: mass of the photocatalyst and irradiation time. The objective of this research was to use a factorial design 2(k) as a function of the multiple response (MR) to evaluate simultaneously experimental conditions for the photodegradation of polycyclic aromatic hydrocarbons in contaminated mangrove sediment and its application in oil from Potiguar Basin in Brazil. The sediment samples collected in Belmonte city (Southern Bahia state) were contaminated with 0.25 mg kg(-1) of Acenaphthene, Anthracene, Benzo[a]Anthracene, Indene[1,2,3cd]pyrene, Dibenzo[ah] anthracene, Benzo[ghi]pyrene. Factors such as mass of the photocatalyst and irradiation time were evaluated in factorial design 2(2), with triplicate from the central point, to 1g of the PAH contaminated sediment. After performing the experiments, it was found that the best experimental condition for the degradation of all PAHs indicated by MR was the central point (0.5 g of photocatalyst and 12h of irradiation). For such conditions, the half-life of PAHs varied from 3.51 to 9.37 h and the degradation speed constant between 0.0740 to 0.1973 h(-1). The comparison of the optimized methodology between photolysis tests and heterogeneous photocatalysis was performed using the Kruskal-Wallis test, which indicated a difference for the reference solution, where heterogeneous photocatalysis was more efficient in the degradation of PAHs. The optimized methodology was apply in samples contaminated with crude oil from Potiguar Basin, no significant difference was observed in the aromatic fraction, using for the Kruskal-Wallis test. Heterogeneous photocatalysis has shown to be a promising remediation technique to remedy aromatic organic compounds in mangrove sediments.	[Silva, Marcio J.; Celino, Joil J.] Univ Fed Bahia, Geosci Inst, Postgrad Program Geochem Petr & Environm, Rua Barao Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil; [Soares, Sarah A. R.; Santos, Ingrid D. F.] Univ Fed Bahia, Geosci Inst, LEPETRO, Excellence Geochem Petr Energy & Environm, Rua Barao Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil; [Pepe, Iuri M.; Teixeira, Leandro R.; Pereira, Lucas G.; Silva, Lucas B. A.] Univ Fed Bahia, Inst Phys, Lab Opt Properties, Rua Barao Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia	Silva, MJ (autor correspondente), Univ Fed Bahia, Geosci Inst, Postgrad Program Geochem Petr & Environm, Rua Barao Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil.	msilva.quimica@gmail.com	Celino, Joil J/D-8106-2014	Celino, Joil J/0000-0002-2234-8724; Teixeira, Leandro do Rozario/0000-0001-6277-160X	Shell Brazil through the "Investment Commitment with Research and Development" [20075-8]; Coordination for the Improvement of Higher Education Personnel - Brazil (CAPES) [001]	Shell Brazil through the "Investment Commitment with Research and Development"; Coordination for the Improvement of Higher Education Personnel - Brazil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This research was carried out in association with the ongoing R&D project registered as ANP No20075-8, "Research Project for Petroleum Systems in Brazilian Sedimentary Basins" (UFBA/Shell Brazil/ANP), sponsored by Shell Brazil through the "Investment Commitment with Research and Development". We also had the support of the Coordination for the Improvement of Higher Education Personnel - Brazil (CAPES) - Financing Code 001.	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J	Toniolo, TD; Giannini, PCF; Angulo, RJ; de Souza, MC; Pessenda, LCR; Spotorno-Oliveira, P				Toniolo, Thiago de Freitas; Fonseca Giannini, Paulo Cesar; Angulo, Rodolfo Jose; de Souza, Maria Cristina; Ruiz Pessenda, Luiz Carlos; Spotorno-Oliveira, Paula			Sea-level fall and coastal water cooling during the Late Holocene in Southeastern Brazil based on vermetid bioconstructions	MARINE GEOLOGY			English	Article						Brazilian Coastal Current; La Plata Plume; Climate change; Santa Catarina coast; Petaloconchus varians	STABLE-ISOTOPE COMPOSITION; SOUTHERN BRAZIL; SURFACE-TEMPERATURE; BIOLOGICAL INDICATORS; GASTROPODA VERMETIDAE; MEDITERRANEAN SEA; CABO-FRIO; SHELF; VARIABILITY; MONSOON	The relative sea-level variation curve, obtained by dating and leveling vermetid shells from northern Santa Catarina State (26.3 degrees S), presents fall trend during all the last 4.0 cal ka BP, which matches previous results based on the same kind of indicator for the Brazilian coast between 3 degrees S and 28 degrees S. Chemical and isotopic analyses of 50 vermetid bioconstructions from distinct localities of south-southeastern Brazilian coast indicate possible changes in the coastal water temperature. These changes may have been caused by oscillations in the strength of Brazilian Coastal Current, which carries La Plata Plume northward, being therefore responsible for the penetration of cold and less saline water masses in the study area. This is a reasonable explanation for the scarcity of vermetid biolithites around 3.4-2.6 cal ka BP and 0.5-0 cal ka BP.	[Toniolo, Thiago de Freitas; Fonseca Giannini, Paulo Cesar] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil; [Angulo, Rodolfo Jose; de Souza, Maria Cristina] Univ Fed Parana, Dept Geol, Curitiba, Parana, Brazil; [Ruiz Pessenda, Luiz Carlos] Univ Sao Paulo, Ctr Energia Nucl Agr, Sao Paulo, Brazil; [Spotorno-Oliveira, Paula] Univ Fed Rio Grande, Inst Oceanog, Programa Posgrad Oceanol, Rio Grande, RS, Brazil	Universidade de Sao Paulo; Universidade Federal do Parana; Universidade de Sao Paulo; Universidade Federal do Rio Grande	Giannini, PCF (autor correspondente), Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil.	pcgianni@usp.br	Villanueva, Rita Guadalupe Angulo/I-8399-2017; Souza, maria cristina/AAF-1843-2021; Giannini, Paulo César Fonseca/D-1871-2015; Spotorno de Oliveira, Paula/C-5725-2013	Villanueva, Rita Guadalupe Angulo/0000-0003-2694-3501; Giannini, Paulo César Fonseca/0000-0003-1046-0177; Spotorno de Oliveira, Paula/0000-0001-7771-3402; Angulo, Rodolfo/0000-0001-9261-3004; Ruiz Pessenda, Luiz Carlos/0000-0001-9119-8195	Sao Paulo Research Foundation (FAPESP) [09/54232-4, 13/21941-8]; National Council for Scientific and Technological Development (CNPq) [308772/2018-0, 428341/2018-7, 477945/2012-0, 2017/033041]; Fundacao Araucaria [45725]; Programa Nacional de Pos-Doutorado/Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - PNPD/CAPES [88887.320380/2019-00]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [13/21941-8] Funding Source: FAPESP	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Araucaria(Fundacao Araucaria de Apoio ao Desenvolvimento Cientifico e Tecnologico do Estado do Parana FAFundacao de Amparo a Pesquisa e Inovacoo Estado de Santa Catarina (FAPESC)); Programa Nacional de Pos-Doutorado/Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - PNPD/CAPES; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The authors are grateful to Dr. Francisco W. da Cruz Junior and Alyne Barros, for the analyses in the Laboratorio de Isotopos Estaveis of the Universidade de Sao Paulo, Brazil; to Isaac J. Sayeg, Jordana A. Zampelli and Luciana Nogueira, for the technical support in laboratory work; to Thais A. da Silva, for the help with the drawings; to Hilton G. Fernandes, for the statistical consultancy; and to Dr. Gert De Lange and two anonymous reviewers for their suggestions and comments that contribute to improve this manuscript. This research was supported by: the Sao Paulo Research Foundation (FAPESP) (PCFG, Process Number: 09/54232-4 and TFT scholarship, Process Number: 13/21941-8); the National Council for Scientific and Technological Development (CNPq) (PCFG, Process Numbers: 308772/2018-0 and 428341/2018-7; RJA, Process Number: 477945/2012-0; LCRP Process Number: 2017/033041); the Fundacao Araucaria (RJA, senior grant 45725); and the Programa Nacional de Pos-Doutorado/Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -PNPD/CAPES (PSO, Process Number: 88887.320380/2019-00).	Almeida F. F. 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Geol.	OCT	2020	428								106281	10.1016/j.margeo.2020.106281	http://dx.doi.org/10.1016/j.margeo.2020.106281			13	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	NC4XB					2023-06-23	WOS:000561216500012
J	Perez, A; Machado, W; Gutierrez, D; Saldarriaga, MS; Sanders, CJ				Perez, Alexander; Machado, Wilson; Gutierrez, Dimitri; Saldarriaga, Maritza S.; Sanders, Christian J.			Shrimp farming influence on carbon and nutrient accumulation within Peruvian mangroves sediments	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Peruvian mangroves; Nutrient enrichment; Carbon accumulation; delta C-13 and delta N-15; Shrimp farming; Sea level rise	SEA-LEVEL RISE; ORGANIC-CARBON; POND EFFLUENT; NITROGEN BUDGET; WATER-QUALITY; C-N; MATTER; DYNAMICS; FORESTS; STORAGE	In order to investigate the influence of shrimp farming activities on carbon and nutrient accumulation, sediment cores were collected from two areas at different distances from shrimp farms within a Peruvian mangrove ecosystem. In both areas two sediment cores were collected in a transect, one from a mangrove-covered site and one from a mudflat site. At both study sites, the isotopic values of carbon and nitrogen as well as the C:N molar ratios suggest that the highest carbon accumulation rates were linked to terrestrial-derived organic matter, with higher carbon stocks and fluxes within mangrove-covered zones. The historical records indicate that since the mid-1970's, the areas nearest to the shrimp farming activity have been accumulating higher proportions of algal derived organic matter, which were likely triggered by the high nutrient influx derived from shrimp farming effluents. The carbon and nutrient fluxes were up to threefold higher within the area nearest to the shrimp farms, whereas the geochronologies showed that the carbon and nutrient stocks in this area increased by up to twofold. The results showed that mangrove-covered zones are more capable to keep pace with sea level rise (SLR) as compared to the mudflat zones, indicating the importance of mangrove vegetation in terms of the vulnerability of this region to SLR and an ongoing capacity to continue accumulating sediments. This study highlights the role that mangrove vegetation plays in mitigating the impact of shrimp farming activities, accumulating carbon and nutrients in pace with SLR.	[Perez, Alexander] Univ Peruana Cayetano Heredia, Fac Ciencias & Filosofia, Ctr Invest Desarrollo Integral & Sostenible CIDIS, Lab Invest & Desarrollo LID,Lab Biogeoci, Av Honorio Delgado 430, Lima, Peru; [Perez, Alexander; Machado, Wilson] Univ Fed Fluminense, Dept Geoquim, Rua Outeiro Sao Joao Baptista S-N, Niteroi, RJ, Brazil; [Gutierrez, Dimitri] Inst Mar Peru, Direcc Gen Invest Oceanog & Cambio Climat, Av Gamarra & Gen Valle S-N, Chucuito, Callao, Peru; [Gutierrez, Dimitri; Saldarriaga, Maritza S.] Univ Peruana Cayetano Heredia, Fac Ciencias & Filosofia, Programa Maestria Ciencias Mar, Av Honorio Delgado 430, Lima, Peru; [Sanders, Christian J.] Southern Cross Univ, Natl Marine Sci Ctr, Sch Environm Sci & Engn, Coffs Harbour, NSW 2450, Australia	Universidad Peruana Cayetano Heredia; Universidade Federal Fluminense; Instituto del Mar del Peru; Universidad Peruana Cayetano Heredia; Southern Cross University	Perez, A (autor correspondente), Univ Peruana Cayetano Heredia, Fac Ciencias & Filosofia, Ctr Invest Desarrollo Integral & Sostenible CIDIS, Lab Invest & Desarrollo LID,Lab Biogeoci, Av Honorio Delgado 430, Lima, Peru.	alexander.perez.s@upch.pe	Sanders, Christian J/AAM-6906-2021; Saldarriaga, Maritza/F-5637-2016; Machado, Wilson/P-8047-2019	Sanders, Christian J/0000-0003-0090-0896; Saldarriaga, Maritza/0000-0001-5947-8576; Machado, Wilson/0000-0003-3117-8584; Perez Segovia, Alexander/0000-0003-4343-1583	project: "Impacto de la Variabilidad y Cambio Climatico en el Ecosistema de Manglares de Tumbes" - International Development Research Centre (IRDC) of Canada; "Fondo Nacional de Desarrollo Cientifico Tecnologico y de Innovacion Tecnologica" (FONDECYT - PERU) [007-2017-FONDECYT, E038-2019-02-FONDECYT-BM]; "Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior" (CAPES) [001]; Australian Research Council [DE160100443, DP150103286, LE140100083]; Universidade Federal Fluminense (Brazil)	project: "Impacto de la Variabilidad y Cambio Climatico en el Ecosistema de Manglares de Tumbes" - International Development Research Centre (IRDC) of Canada; "Fondo Nacional de Desarrollo Cientifico Tecnologico y de Innovacion Tecnologica" (FONDECYT - PERU); "Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior" (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Australian Research Council(Australian Research Council); Universidade Federal Fluminense (Brazil)	The sampling campaign was supported by the project: "Impacto de la Variabilidad y Cambio Climatico en el Ecosistema de Manglares de Tumbes", which was granted by the International Development Research Centre (IRDC) of Canada under management of the Instituto Geoffsico del Peril (IGP). AP and DG is supported by the "Fondo Nacional de Desarrollo Cientifico Tecnologico y de Innovacion Tecnologica" (FONDECYT - PERU) thought the Magnet program (Grant no 007-2017-FONDECYT) and the "IncorporaciOn de Investigadores" program (Grant no E038-2019-02-FONDECYT-BM). WM and AP thank to "Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior" (CAPES) for the support (financial code 001) to the Geochemistry Doctoral Program from the Universidade Federal Fluminense. CJS is supported by the Australian Research Council (DE160100443, DP150103286 and LE140100083), in cooperation with Universidade Federal Fluminense (Brazil). We are also grateful to Dr. Ken Takahashi Guevara, who provided us with invaluable support. AP wrote the manuscript with input from the other authors. All authors designed the study, approved the final version of the manuscript and agree to be accountable for all aspects of this document.	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J	Limaverde, S; Pegas, RV; Damasceno, R; Villa, C; Oliveira, GR; Bonde, N; Leal, MEC				Limaverde, Saulo; Pegas, Rodrigo Vargas; Damasceno, Rafael; Villa, Chiara; Oliveira, Gustavo R.; Bonde, Niels; Leal, Maria E. C.			Interpreting character variation in turtles: Araripemys barretoi (Pleurodira: Pelomedusoides) from the Araripe Basin, Early Cretaceous of Northeastern Brazil	PEERJ			English	Article						Araripe; Sexual dimorphism; Cretaceous; Ontogeny; Araripemys; Intraspecific variation; Polymorphism	SEXUAL SIZE DIMORPHISM; SANTANA FORMATION; CRATO FORMATION; EARLY PALEOCENE; SOFT-TISSUE; PATAGONIA; FOSSIL; SHELL; BOTHREMYDIDAE; PRESERVATION	The Araripe Basin (Northeastern Brazil) has yielded a rich Cretaceous fossil fauna of both vertebrates and invertebrates found mainly in the Crato and Romualdo Formations, of Aptian and Albian ages respectively. Among the vertebrates, the turtles were found to be quite diverse, with several specimens retrieved and five valid species described to this date for the Romualdo Formation. There were also records of turtles from Ipubi and Crato Formations, mainly fragmentary material which precluded proper specific identification; however, Araripemys barretoi is supposed to occur on both Crato and Romualdo Formations. Here we describe thirteen specimens of A. barretoi-including the first description of an almost complete individual, bearing a skull, from the Crato Formation. We report a great amount of morphological variation, interpreted as being essentially of intraspecific nature, including individual, sexual and ontogenetic variation.	[Limaverde, Saulo] Univ Fed Ceara, Dept Geol, Ctr Ciencias, Fortaleza, Ceara, Brazil; [Pegas, Rodrigo Vargas] Univ Fed ABC, Lab Vertebrate Paleontol & Anim Behav, Sao Bernardo Do Campo, SP, Brazil; [Damasceno, Rafael; Oliveira, Gustavo R.] Univ Fed Rural Pernambuco, Dept Biol, Area Ecol, Lab Paleontol & Sistemat, Recife, PE, Brazil; [Villa, Chiara] Univ Copenhagen, Dept Forens Med, Lab Biol Anthropol, Copenhagen, Denmark; [Bonde, Niels] Univ Copenhagen, SNM, Zool Museum, Sect Biosystemat, Copenhagen, Denmark; [Bonde, Niels] Fur Museum, Museum Saling, Fur, Denmark; [Leal, Maria E. C.] Aarhus Univ, Fac Hlth, Aarhus, Denmark	Universidade Federal do Ceara; Universidade Federal do ABC (UFABC); Universidade Federal Rural de Pernambuco (UFRPE); University of Copenhagen; University of Copenhagen; Aarhus University	Leal, MEC (autor correspondente), Aarhus Univ, Fac Hlth, Aarhus, Denmark.	castroleal@post.au.dk	Villa, Chiara/AAA-9379-2019; Oliveira, Gustavo R/F-7432-2012; Oliveira, Gustavo/IQW-7983-2023	Villa, Chiara/0000-0002-9967-8131; Oliveira, Gustavo R/0000-0002-9871-1235; 	Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP); CNPq [131186/2017-5]	Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was supported by Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) and CNPq (CNPq/FUNCAP-DCR/305426/2014-1, DCR-0024-01186.01.00/14 and CNPq #131186/2017-5). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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J	Souza, PWM; Pinheiro, RVL; Costa, FR; Guimaraes, JTF; Sahoo, PK; Silva, MS; Silva, CG				Souza-Filho, Pedro Walfir M.; Pinheiro, Roberto Vizeu L.; Costa, Francisco R.; Guimaraes, Jose Tasso F.; Sahoo, Prafulla K.; Silva, Marcio S.; Silva, Cleverson G.			The role of fault reactivation in the development of tropical montane lakes	EARTH SURFACE PROCESSES AND LANDFORMS			English	Article						geomorphology; seismostratigraphic facies; structural geology; bathymetry; tropical lake; Quaternary; iron ore mountains	SERRA-DOS-CARAJAS; LACUSTRINE SEDIMENTS; LATE PLEISTOCENE; BASEMENT REACTIVATION; SOUTHEASTERN AMAZON; VEGETATION CHANGES; BRAZIL; EVOLUTION; TECTONICS; PLATEAU	This work details the role of fault reactivation in the development of tropical montane lakes by using basin morpho-structural analysis and seismostratigraphic studies. The upland lakes are severely faulted sinkholes, whose faults penetrate the Quaternary sedimentary units. Four main stages are related to the lake formation: (i) an Early Proterozoic tectonic deformation of the rocks along the southern border of the Carajas Structure, where the lake is placed; (ii) differential erosion by - and building of - the formation of the South Carajas Hill; (iii) Fe-rich crust formation by weathering and gravitational collapse faults following the E-W plateau border and the start of Violao Lake formation during the Pliocene-Pleistocene; and (iv) episodic fault-fracture reactivation by gravitational collapse causing pulses of subsidence in the lake and outlining its faulted borders. Dissolution of the lateritic crust and erosion by runoff drainage under wet climate conditions were coeval with fault activities, which allowed the deposition of relatively thick clastic deposits organized in three main seismostratigraphic units associated with major lake-level fluctuations. Initial fault reactivation under low-level water started lacustrine basin development with deposition of prograding fan deltas related to the main drainage. A second fault reactivation by gravitational collapse increased the lake accommodation space and resulted in the deposition of fine-grained sediments from dilute interflows or overflows until 36 000 cal year BP. At about 31 000 cal year BP, rapid decreases in the lake water level under redox conditions at the sediment/water interface allowed widespread siderite formation. A third gravitational collapse episode was responsible for the increase in the lake area and depth and the returning of clastic/organic deposition up to the present. This tropical montane lake can be seen as a representative example for understanding the formation of other upland lakes controlled by fault reactivation. (c) 2020 John Wiley & Sons, Ltd.	[Souza-Filho, Pedro Walfir M.; Sahoo, Prafulla K.] Inst Tecnol Vale, Belem, PA, Brazil; [Souza-Filho, Pedro Walfir M.; Pinheiro, Roberto Vizeu L.; Costa, Francisco R.; Guimaraes, Jose Tasso F.; Silva, Marcio S.] Univ Fed Para, Geosci Inst, Belem, PA, Brazil; [Costa, Francisco R.] Univ Fed Sul & Sudeste Para, Geosci & Engn Inst, Maraba, PA, Brazil; [Sahoo, Prafulla K.] Cent Univ Punjab, Sch Environm & Earth Sci, Dept Environm Sci & Technol, Bathinda, India; [Silva, Cleverson G.] Univ Fed Fluminense, Dept Geol, Niteroi, RJ, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Universidade Federal do Para; Universidade Federal do Sul e Sudeste do Para; Central University of Punjab; Universidade Federal Fluminense	Souza, PWM (autor correspondente), Inst Tecnol Vale, Belem, PA, Brazil.; Souza, PWM (autor correspondente), Univ Fed Para, Geosci Inst, Belem, PA, Brazil.	pedro.martins.souza@itv.org	Silva, Cleverson G/G-2518-2012; Souza-Filho, Pedro Walfir M. M./J-4958-2012; Souza, Pedro/GZH-1275-2022; Sahoo, Prafulla/N-5100-2018	Silva, Cleverson G/0000-0003-1731-7883; Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; Sahoo, Prafulla/0000-0003-3481-1787; GUIMARAES, JOSE TASSO/0000-0002-5772-5104; Sousa da Silva, Marcio/0000-0003-0748-0169	Vale S.A. Paleoclimate Project - Paleoclimate and evolution of tropical rain forest in the Eastern Amazon during the Quaternary [RBR000603.99]; Fundacao Amazonia de Amparo a Estudos e Pesquisas (FAPESPA) [355388/2014]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)	Vale S.A. Paleoclimate Project - Paleoclimate and evolution of tropical rain forest in the Eastern Amazon during the Quaternary; Fundacao Amazonia de Amparo a Estudos e Pesquisas (FAPESPA)(Fundacao Amazonia de Amparo a Estudos e Pesquisas (FAPESPA)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was carried out in the context of the Paleoclimate (# RBR000603.99) and Procav projects, with funding from Vale S.A. Paleoclimate Project - Paleoclimate and evolution of tropical rain forest in the Eastern Amazon during the Quaternary. It was also supported by the Fundacao Amazonia de Amparo a Estudos e Pesquisas (FAPESPA # 355388/2014). The authors thank the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for personal research grant concessions during this investigation (PWMSF, JTFG and CGS). 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J	Melo, RM; Guzman, J; Almeida-Lima, D; Piovesan, EK; Neumann, VHDL; Sousa, ADE				Melo, Robbyson Mendes; Guzman, Juliana; Almeida-Lima, Debora; Piovesan, Enelise Katia; de Miranda Lopes Neumann, Virginio Henrique; de Jesus e Sousa, Ariany			New marine data and age accuracy of the Romualdo Formation, Araripe Basin, Brazil	SCIENTIFIC REPORTS			English	Article							EARLY CRETACEOUS PALEOGEOGRAPHY; OCEANIC ANOXIC EVENTS; SOUTH ATLANTIC; PLANKTONIC-FORAMINIFERA; SERGIPE BASIN; NONMARINE OSTRACODS; ALAGAMAR FORMATION; NORTHEAST BRAZIL; POTIGUAR BASIN; PRE-GUITTARD	A combined biostratigraphic and palaeoecological study of foraminifera, ostracodes and microfacies was carried out on the Aptian in the Sitio Sobradinho section of the Araripe Basin, northeast Brazil. The analysed section represents a deepening-upward sequence with mid-ramp shoal and outer ramp to basin facies associations on a mixed siliciclastic-carbonate marine ramp. The analysed rocks are dominated by Early Cretaceous planktic foraminifera (Hedbergella aptiana, H. praelippa, H. sigali, Blesfucuiana cf. cumulus, Microhedbergella miniglobularis, Gorbachikella cf. kugleri, Pseudoguembelitria blakenosensis, Globigerinelloides clavatus, Globigerinelloides aff. aptiensis, Gubkinella sp. and Loeblichella sp.). Ostracoda fauna is composed mainly of Pattersoncypris crepata and Pattersoncypris micropapillosa. The occurrence of P. crepata associated with the Aptian planktic foraminifera demonstrates the potential of this ostracode species to date this interval. The planktic foraminifera from the upper Aptian (Microhedbergella miniglobularis Zone) of the Araripe Basin show characteristical Tethyan affinities.	[Melo, Robbyson Mendes; Guzman, Juliana; Almeida-Lima, Debora; Piovesan, Enelise Katia; de Miranda Lopes Neumann, Virginio Henrique; de Jesus e Sousa, Ariany] Univ Fed Pernambuco, Dept Geol, Lab Appl Micropaleontol LAGESE LITPEG, Recife, PE, Brazil; [de Jesus e Sousa, Ariany] Ilha Fundao, PETROBRAS CENPES PDGEO BPA, Rio De Janeiro, RJ, Brazil	Universidade Federal de Pernambuco	Melo, RM (autor correspondente), Univ Fed Pernambuco, Dept Geol, Lab Appl Micropaleontol LAGESE LITPEG, Recife, PE, Brazil.	robbysonmelo@gmail.com	Sousa, Ariany/CAH-4511-2022; Piovesan, Enelise Katia/Q-2953-2017	Sousa, Ariany/0000-0002-8847-6884; Piovesan, Enelise Katia/0000-0002-0433-0395; Guzman, Juliana/0000-0001-7898-049X; Mendes Melo, Robbyson/0000-0002-6557-3999	Brazilian National Petroleum Agency (ANP); PETROBRAS [2017/00263-2, 2018/00320-9]; CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)	Brazilian National Petroleum Agency (ANP); PETROBRAS(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors would like to acknowledge the Brazilian National Petroleum Agency (ANP) and PETROBRAS for financial support through the following projects: "ARTUNJA: Correlacoes bioestratigraficas dos sistemas fluvio-lacustres das fases rifte e pos-rifte das bacias do Araripe, Jatoba e Tucano Norte, NE do Brasil/no. 2017/00263-2" and "ImplantacAo da infraestrutura do Laboratorio de Micropaleontologia Aplicada da Universidade Federal de Pernambuco/no. 2018/00320-9". This study was financed in part by the CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES). We thank Brian T. Huber for the valuable support in identification of foraminifera. We are grateful to Edval Santos for his help in acquiring the MEV images. The authors thank to the reviewers and the editor for their significant suggestions that allowed us to improve the manuscript.	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J	Cheng, H; Zhang, HW; Spotl, C; Baker, J; Sinha, A; Li, HY; Bartolome, M; Moreno, A; Kathayat, G; Zhao, JY; Dong, XY; Li, YW; Ning, YF; Jia, X; Zong, BY; Brahim, YA; Perez-Mejias, C; Cai, YJ; Novello, VF; Cruz, FW; Severinghaus, JP; An, ZS; Edwards, RL				Cheng, Hai; Zhang, Haiwei; Spoetl, Christoph; Baker, Jonathan; Sinha, Ashish; Li, Hanying; Bartolome, Miguel; Moreno, Ana; Kathayat, Gayatri; Zhao, Jingyao; Dong, Xiyu; Li, Youwei; Ning, Youfeng; Jia, Xue; Zong, Baoyun; Brahim, Yassine Ait; Perez-Mejias, Carlos; Cai, Yanjun; Novello, Valdir F.; Cruz, Francisco W.; Severinghaus, Jeffrey P.; An, Zhisheng; Edwards, R. Lawrence			Timing and structure of the Younger Dryas event and its underlying climate dynamics	PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA			English	Article						Younger Dryas; timing; structure; event phasing; climate dynamics	CORE WD2014 CHRONOLOGY; LAST GLACIAL PERIOD; HIGH-RESOLUTION; MONSOON RECORD; ASIAN MONSOON; SPELEOTHEM RECORD; TROPICAL PACIFIC; HULU CAVE; OCEAN; AGE	The Younger Dryas (YD), arguably the most widely studied millennial-scale extreme climate event, was characterized by diverse hydroclimate shifts globally and severe cooling at high northern latitudes that abruptly punctuated the warming trend from the last glacial to the present interglacial. To date, a precise understanding of its trigger, propagation, and termination remains elusive. Here, we present speleothem oxygen-isotope data that, in concert with other proxy records, allow us to quantify the timing of the YD onset and termination at an unprecedented subcentennial temporal precision across the North Atlantic, Asian Monsoon-Westerlies, and South American Monsoon regions. Our analysis suggests that the onsets of YD in the North Atlantic (12,870 +/- 30 B.P.) and the Asian Monsoon-Westerlies region are essentially synchronous within a few decades and lead the onset in Antarctica, implying a north-to-south climate signal propagation via both atmospheric (decadal-time scale) and oceanic (centennial-time scale) processes, similar to the Dansgaard-Oeschger events during the last glacial period. In contrast, the YD termination may have started first in Antarctica at similar to 11,900 B.P., or perhaps even earlier in the western tropical Pacific, followed by the North Atlantic between similar to 11,700 +/- 40 and 11,610 +/- 40 B.P. These observations suggest that the initial YD termination might have originated in the Southern Hemisphere and/or the tropical Pacific, indicating a Southern Hemisphere/tropics to North Atlantic-Asian Monsoon-Westerlies directionality of climatic recovery.	[Cheng, Hai; Zhang, Haiwei; Baker, Jonathan; Li, Hanying; Kathayat, Gayatri; Zhao, Jingyao; Dong, Xiyu; Li, Youwei; Ning, Youfeng; Jia, Xue; Zong, Baoyun; Brahim, Yassine Ait; Perez-Mejias, Carlos; Cai, Yanjun] Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710054, Peoples R China; [Cheng, Hai; An, Zhisheng] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China; [Cheng, Hai] Chinese Acad Geol Sci, Inst Karst Geol, Key Lab Karst Dynam, Minist Land & Resources, Guilin 541004, Peoples R China; [Spoetl, Christoph] Univ Innsbruck, Inst Geol, A-6020 Innsbruck, Austria; [Sinha, Ashish] Calif State Univ Dominguez Hills, Dept Earth Sci, Carson, CA 90747 USA; [Bartolome, Miguel] CSIC, Museo Nacl Ciencias Nat, Dept Geol, Madrid 28034, Spain; [Moreno, Ana] CSIC, Inst Pirena Ecol, Zaragoza 50059, Spain; [Novello, Valdir F.; Cruz, Francisco W.] Univ Sao Paulo, Inst Geociencias, BR-05508090 Sao Paulo, Brazil; [Severinghaus, Jeffrey P.] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; [Edwards, R. Lawrence] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN 55455 USA; [Edwards, R. Lawrence] Nanjing Normal Univ, Sch Geog, Nanjing 210023, Peoples R China	Xi'an Jiaotong University; Chinese Academy of Sciences; Institute of Earth Environment, CAS; Chinese Academy of Geological Sciences; Ministry of Natural Resources of the People's Republic of China; University of Innsbruck; California State University System; California State University Dominguez Hills; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Museo Nacional de Ciencias Naturales (MNCN); Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Pirenaico de Ecologia (IPE); Universidade de Sao Paulo; University of California System; University of California San Diego; Scripps Institution of Oceanography; University of Minnesota System; University of Minnesota Twin Cities; Nanjing Normal University	Cheng, H (autor correspondente), Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710054, Peoples R China.; Cheng, H (autor correspondente), Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China.; Cheng, H (autor correspondente), Chinese Acad Geol Sci, Inst Karst Geol, Key Lab Karst Dynam, Minist Land & Resources, Guilin 541004, Peoples R China.	cheng021@xjtu.edu.cn	AN, Zhisheng/F-8834-2012; CHENG, HAI/H-3413-2017; Cai, Yanjun/A-9462-2010; Cruz, Francisco W/G-6059-2012; Novello, Valdir F./P-5824-2015	CHENG, HAI/0000-0002-5305-9458; Cai, Yanjun/0000-0001-7063-5050; Novello, Valdir F./0000-0002-0120-3745; Zhao, Jingyao/0000-0002-4252-6540; Reis, AlessanRSS/0000-0001-8486-7469; Zhang, Haiwei/0000-0002-0855-1283; Bartolome, Miguel/0000-0002-2924-6261; Spotl, Christoph/0000-0001-7167-4940; Moreno, Ana/0000-0001-7357-584X; Sinha, Ashish/0000-0001-5700-2451	National Nature Science Foundation of China (NSFC) [41888101, 41731174]; US NSF [1702816]	National Nature Science Foundation of China (NSFC)(National Natural Science Foundation of China (NSFC)); US NSF(National Science Foundation (NSF))	This work was supported by grants from National Nature Science Foundation of China (NSFC 41888101 and 41731174 to H.C.) and US NSF Grant (1702816 to R.L.E. and H.C.).	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Natl. Acad. Sci. U. S. A.	SEP 22	2020	117	38					23408	23417		10.1073/pnas.2007869117	http://dx.doi.org/10.1073/pnas.2007869117			10	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	NX7LU	32900942	hybrid, Green Published			2023-06-23	WOS:000575888700007
J	Sarmento, CCT; Sommer, CA; de Lima, EF; Barreto, CJS; Rossetti, LDM; Lafon, JM				Sarmento, Carla Cecilia Treib; Sommer, Carlos Augusto; de Lima, Evandro Fernandes; Barreto, Carla Joana Santos; Rossetti, Lucas de Magalhaes May; Lafon, Jean Michel			Mafic subvolcanic intrusions from the southernParana-EtendekaLarge Igneous Province, Brazil: Insights from geochemistry andSr-Nd-Pbisotopes	GEOLOGICAL JOURNAL			English	Article						crustal contamination; feeder dikes; mafic subvolcanic intrusions; Parana-Etendeka Igneous Province; Sr-Nd-Pb isotopes	CONTINENTAL FLOOD BASALTS; FLORIANOPOLIS DYKE SWARM; PARANA PLATEAU BRAZIL; MAGMATIC PROVINCE; TORRES SYNCLINE; SOUTH-ATLANTIC; DIKE SWARM; CHEMICAL CLASSIFICATION; CRUSTAL CONTAMINATION; MANTLE HETEROGENEITY	The Early Cretaceous Parana-Etendeka Igneous Province is a predominantly tholeiitic sequence of continental flood basalts and silicic magmatism that is intimately associated with the rupture of the western Gondwana. Intrusions of tholeiitic compositions are very common within the province and represent the magmatic plumbing system that fed the lavas at the surface. The investigated dikes are in the southeast of the Parana Basin, southermost Brazil. The Silica Saturated Olivine Tholeiite (SSOT) dikes show restricted isotopic ranges (Sr-87/Sr-86(i)= 0.70570 to 0.70585;eNd(i)= -1.01 to -4.49;Pb-206/Pb-204 = 18.031), with no equivalent low-Ti magma type in the Parana Province, but are close to the isotopic ratios of low-Ti magma types with MgO > 7 wt%, such as Nil Desperandum in the Etendeka Province. The Silica Supersaturated Tholeiite dikes show broader isotopic ranges (Sr-87/Sr-86(i)= 0.70787 to 0.71336;eNd(i)= -2.51 to -8.65;Pb-206/Pb-204 = 18.578-19.049), similar to the Gramado magma-type and Tafelberg magma-type in the Parana-Etendeka Province. This variation may have occurred due to the contamination at the time of magma rise and extrusion. Isotopic modelling showed that the fractional crystallization process and crustal assimilation played an important role from the magma rise through the conduits to the extrusion of the lavas. For the most primitive SSOT dikes, fractional crystallization was the most important factor for the magma evolution. The behaviour of the trace elements revealed that the assimilation of crust rocks with both Palaeoproterozoic and Neoproterozoic ages can be considered.	[Sarmento, Carla Cecilia Treib; Sommer, Carlos Augusto; de Lima, Evandro Fernandes] Univ Fed Rio Grande do Sul, Geosci Inst, Ave Bento Goncalves 9500 Predio 43136 Sala 107, BR-91501970 Porto Alegre, RS, Brazil; [Barreto, Carla Joana Santos] Univ Fed Pernambuco, Geol Dept, Recife, PE, Brazil; [Rossetti, Lucas de Magalhaes May] Univ Fed Mato Grosso, Geosci Fac, Cuiaba, Brazil; [Lafon, Jean Michel] Univ Fed Para, Geosci Inst, Belem, Para, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal de Pernambuco; Universidade Federal de Mato Grosso; Universidade Federal do Para	Sommer, CA (autor correspondente), Univ Fed Rio Grande do Sul, Geosci Inst, Ave Bento Goncalves 9500 Predio 43136 Sala 107, BR-91501970 Porto Alegre, RS, Brazil.	carlos.sommer@ufrgs.br	DE LIMA, EVANDRO FERNANDES/AAA-8150-2020; Jean Michel, Lafon/AAY-6287-2021; Rossetti, Lucas de Magalhaes May/AAM-1984-2020; barreto, carla/AAI-2807-2021; Sommer, Carlos A/Q-9077-2018	DE LIMA, EVANDRO FERNANDES/0000-0002-4101-3161; Jean Michel, Lafon/0000-0003-0854-3053; Sommer, Carlos A/0000-0001-8696-7084; Barreto, Carla/0000-0003-1938-4318; de Magalhaes May Rossetti, Lucas/0000-0002-1493-6104	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [304036/2018-8, 400724/2014-6, 406925/2018-6, 441766/2014-5, 302213/2012-0]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior; Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul [1180/12-8, PRONEX10/0045-6]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS))	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, Grant/Award Numbers: 304036/2018-8, 400724/2014-6, 406925/2018-6, 441766/2014-5, 302213/2012-0; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior; Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul, Grant/Award Numbers: 1180/12-8, PRONEX10/0045-6	ALLEGRE CJ, 1988, CHEM GEOL, V70, P211, DOI 10.1016/0009-2541(88)90094-0; Almeida VV, 2018, J VOLCANOL GEOTH RES, V355, P55, DOI 10.1016/j.jvolgeores.2017.01.018; BELLIENI G, 1986, J PETROL, V27, P915, DOI 10.1093/petrology/27.4.915; Bondre NR, 2006, J GEOL, V114, P155, DOI 10.1086/499568; Brueseke ME, 2007, J VOLCANOL GEOTH RES, V161, P187, DOI 10.1016/j.jvolgeores.2006.12.004; Bryan S, 2007, EPISODES, V30, P20, DOI 10.18814/epiiugs/2007/v30i1/004; Bryan SE, 2008, EARTH-SCI REV, V86, P175, DOI 10.1016/j.earscirev.2007.08.008; Coffin M., 1992, GEOL SOC SPEC PUBL, V68, P17; Corval A., 2008, GEOCHIMICA BRASILIEN, V22, P159, DOI [10.21715/gb.v22i3.286, DOI 10.21715/GB.V22I3.286]; Courtillot V, 1999, EARTH PLANET SC LETT, V166, P177, DOI 10.1016/S0012-821X(98)00282-9; Courtillot VE, 2003, CR GEOSCI, V335, P113, DOI 10.1016/S1631-0713(03)00006-3; Deckart K, 1998, J VOLCANOL GEOTH RES, V80, P67, DOI 10.1016/S0377-0273(97)00038-3; DePaolo D. 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J	Bastos, VA; Koester, E; Lenz, C; Dal Olmo-Barbosa, L; Porcher, CC; Loureiro, PO; Vieira, DT; Ramos, RC; Cedeno, DG				Bastos, Vivianne Andrade; Koester, Edinei; Lenz, Cristine; Dal Olmo-Barbosa, Laercio; Porcher, Carla C.; Loureiro, Paula O.; Vieira, Daniel T.; Ramos, Rodrigo C.; Cedeno, Daniel G.			Contribution to the understanding of the Pinheiro Machado Complex (Dom Feliciano Belt, Brazil): A study of textures, mineral chemistry, and crystallization conditions	GEOLOGICAL JOURNAL			English	Article						geothermobarometry; magmatic flow; mineral chemistry; Pinheiro Machado Complex recrystallization	EXPERIMENTAL CALIBRATION; CONTINENTAL-CRUST; SOUTHERN BRAZIL; U-PB; HORNBLENDE; AMPHIBOLE; DISCRIMINATION; PLAGIOCLASE; EMPLACEMENT; MAGMAS	This article presents textures, mineral chemistry, and geothermobarometric data for the southeastern Pinheiro Machado Complex rocks (PMC), eastern domain of the Dom Feliciano Belt, Rio Grande do Sul, Brazil. The PMC is composed by comagmatic intrusions of quartz diorite, tonalite, and granodiorite with medium- to fine-grained equigranular and medium-grained inequigranular textures with subordinate alkali-feldspar macrocrystals. Partial melting features are observed in the comagmatic as melt pools and melt films. Amphibolite xenoliths also occur, presenting sharp-angled to rounded contacts with the intrusions and evidences of partial assimilation, marked by mafic schlierens. Electron probe microanalyzer punctual analyses were used to classify amphibole, plagioclase, biotite, epidote, and titanite, as well as for the calculations of the crystallization P-T conditions. Amphiboles consist of pargasite for the comagmatic intrusions, and Mg-hornblende for the amphibolite. Plagioclase ranges from oligoclase to andesine (An(15-40)) in both units. Biotite corresponds to annite, with Fe/(Fe + Mg) > 0.3. The epidote has mostly magmatic characteristics in the comagmatic intrusions, with pistacite content 25-30%. Titanite has two distinct textures, titanite I is well formed, subhedral to euhedral, with up to 3 mm; while titanite II is anhedral with size >1 mm and rounded shapes, being both chemically homogeneous. The estimated P-T conditions for the amphibolite crystallization, using plagioclase-hornblende geothermometer are 650-850 degrees C and 3.62-4.95 kbar, whereas the conditions from the comagmatic intrusions are 714-871 degrees C and 4.44-6.10 kbar. In the mineral phases there is a prevalence in the recrystallization field between subgrain rotation (SGR) and grain boundary migration (GBM) in submagmatic flow. These new data indicate that possibly at the end of PMC crystallization, late magmatic fluids caused re-equilibrium of mineral phases, mainly in biotite and feldspars. Finally, we suggest that the PMC is the result of continuous and repeated comagmatic intrusions in a continental magmatic arc setting at a depth of 20-30 km in an amphibolitic continental crust.	[Bastos, Vivianne Andrade; Dal Olmo-Barbosa, Laercio; Loureiro, Paula O.; Vieira, Daniel T.; Cedeno, Daniel G.] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Porto Alegre, RS, Brazil; [Koester, Edinei; Porcher, Carla C.] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Geol, Porto Alegre, RS, Brazil; [Lenz, Cristine] Univ Fed Sergipe, Dept Geol, Sao Cristovao, Sergipe, Brazil; [Ramos, Rodrigo C.] Prefeitura Sapiranga, Sapiranga, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal de Sergipe	Bastos, VA (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Porto Alegre, RS, Brazil.	vivianneab@hotmail.com	Koester, Edinei/L-3684-2017; Porcher, Carla C/R-1419-2018	Koester, Edinei/0000-0002-4424-4782; Porcher, Carla C/0000-0002-0418-3954; Chaves Ramos, Rodrigo/0000-0001-7116-5062; Andrade Bastos, Vivianne/0000-0002-4460-5285; Dal Olmo-Barbosa, Laercio/0000-0002-2732-8634	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [141335/2017-3]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior [88882345526/2019-1]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, Grant/Award Number: 141335/2017-3; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, Grant/Award Number: 88882345526/2019-1	ABBOTT RN, 1979, CAN MINERAL, V17, P549; ABDELRAHMAN AFM, 1994, J PETROL, V35, P525, DOI 10.1093/petrology/35.2.525; Almeida D. 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J.	FEB	2021	56	2			SI		1012	1033		10.1002/gj.3980	http://dx.doi.org/10.1002/gj.3980		SEP 2020	22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QA5WN					2023-06-23	WOS:000571633200001
J	Akabane, TK; Sawakuchi, AO; Chiessi, CM; Kern, AK; Pinaya, JLD; Ceccantini, GCT; De Oliveira, PE				Akabane, Thomas Kenji; Sawakuchi, Andre Oliveira; Chiessi, Cristiano Mazur; Kern, Andrea K.; Diaz Pinaya, Jorge Luiz; Tapias Ceccantini, Gregorio Cardoso; De Oliveira, Paulo Eduardo			Modern pollen signatures of Amazonian rivers and new insights for environmental reconstructions	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palynology; Amazon drainage basin; Modern analogue; Riverbed sediments; Vegetation reconstruction	LATE QUATERNARY VEGETATION; FIRME DENSE FOREST; TERRA-FIRME; RAIN-FOREST; NEGRO RIVER; PALYNOLOGICAL DIFFERENTIATION; SOUTHEASTERN AMAZONIA; PLANT DIVERSITY; CLIMATE-CHANGE; DYNAMICS	Paleoenvironmental reconstructions based on Amazonian fluvial and marine pollen data are often hindered due to the scarcity of modern calibration data. In Amazonia, rivers are the main pathways for pollen from upland and flooded forests to continental and marine sediment sinks. Linking pollen assemblages transported by rivers to watershed vegetation is crucial to interpret palynological archives. In order to constrain the interpretation of palynological archives, we analysed the pollen content of 36 riverbed sediment samples distributed from the mouth of the Ica River (ca. 68 degrees W) to the Amazon estuary (ca. 49 degrees W) with support of grain size and major element analyses of the inorganic sedimentary content. The palynological analysis shows a strong imprint of the lowland floodplain vegetation as the main source of the riverborne pollen. The upper reaches of the Amazon River present abundant Cecropia, reflecting early-successional stages induced by intense floodplain disturbance. The middle and lower reaches of the Amazon River exhibit a progressive increase in herbs mainly represented by Poaceae and Cyperaceae, related to wider floodplains covered by seasonally inundated vegetation. Floodplain forests of whitewater rivers (varzeas) are palynologically characterized by Iriartea, Mauritia, Ilex, Pseudobombax, Acalypha, and Luehea/Laetia, with high frequency of Cecropia or herbs, and montane taxa. At the black- and clearwater rivers, the igapo floodplain forests provide high percentages of Symmeria, Myrtaceae, and Alchornea, and can be distinguished by Sapium/Sebastiana, Piranhea, Amanoa, Pouteria, Ferdinandusa/Genipa, Attalea/Astrocatyum, and Eschweilera which suggest conditions of higher stability and mature forests. Contribution from the non-flooded uplands, Andean Mountains, and savannas/Cerrado occur, but their signals are blurred by the high pollen production of the lowland floodplains. Our data provide a calibration set for environmental reconstructions of river-influenced deposits across the Amazon including offshore areas of the most iconic riverine dominated landscape in the world.	[Akabane, Thomas Kenji; Sawakuchi, Andre Oliveira; Kern, Andrea K.; De Oliveira, Paulo Eduardo] Univ Sao Paulo, Inst Geosci, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Chiessi, Cristiano Mazur] Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, SP, Brazil; [Diaz Pinaya, Jorge Luiz] Univ Sao Paulo, Polytech Sch, Sao Paulo, SP, Brazil; [Tapias Ceccantini, Gregorio Cardoso; De Oliveira, Paulo Eduardo] Univ Sao Paulo, Inst Biosci, Sao Paulo, SP, Brazil; [De Oliveira, Paulo Eduardo] Field Museum Nat Hist, Keller Sci Act Ctr, Chicago, IL 60605 USA	Universidade de Sao Paulo; Universidade de Sao Paulo; Universidade de Sao Paulo; Universidade de Sao Paulo; Field Museum of Natural History (Chicago)	Akabane, TK (autor correspondente), Univ Sao Paulo, Inst Geosci, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil.	thomas.akabane@usp.br	Chiessi, Cristiano Mazur/E-1916-2012; Akabane, Thomas/ABB-3401-2021; Sawakuchi, André O/D-1445-2013; Kern, Andrea K./V-5078-2017	Chiessi, Cristiano Mazur/0000-0003-3318-8022; Akabane, Thomas/0000-0003-1103-695X; Kern, Andrea K./0000-0002-9343-0696	National Council for Scientific and Technological Development - CNPq [130581/2017-8]; FAPESP [2018/15123-4, 2011/06609-1, 2012/50260-6, 2016/02656-1]; CAPES [564/2015, 88881.313535/2019-01]; CNPq [302607/2016-1, 422255/2016-5, 304727/2017-2]; Alexander von Humboldt Foundation; CAPES within the PrInt/CAPES fellowship program [88887.370034/2019-00]	National Council for Scientific and Technological Development - CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Alexander von Humboldt Foundation(Alexander von Humboldt Foundation); CAPES within the PrInt/CAPES fellowship program(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	T.K.A thanks the Institute of Geosciences of the University of Sao Paulo, the laboratory support of the colleagues Rudney Almeida, Dailson Bertassoli Jr., Vanda Medeiros, and Maicon Alicrin, and the financial support from the National Council for Scientific and Technological Development -CNPq (grant 130581/2017-8). C.M.C. acknowledges the financial support from FAPESP (grant 2018/151234), CAPES (grants 564/2015 and 88881.313535/2019-01), CNPq (grants 302607/2016-1 and 422255/2016-5), and the Alexander von Humboldt Foundation. A.O.S. was supported by CNPq (grant 304727/2017-2). Sediment sampling surveys were financially support by FAPESP (grant 2011/06609-1; 2012/50260-6; 2016/02656-1). A.K.K. was supported by CAPES within the PrInt/CAPES fellowship program (process number 88887.370034/2019-00). Henrique Oliveira Sawakuchi is acknowledged for providing sediment samples from the Amazon estuary and Para River. Daniel Atencio is acknowledged for providing the XRF equipment. We also thank the three reviewers who helped us to improve the manuscript.	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Paleoclimatol. Paleoecol.	SEP 15	2020	554								109802	10.1016/j.palaeo.2020.109802	http://dx.doi.org/10.1016/j.palaeo.2020.109802			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	MP3WQ					2023-06-23	WOS:000552137300012
J	Bicudo, TC; Sacek, V; de Almeida, RP				Bicudo, Tacio Cordeiro; Sacek, Victor; de Almeida, Renato Paes			Reappraisal of the relative importance of dynamic topography and Andean orogeny on Amazon landscape evolution	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						geodynamic modeling; dynamic topography; Amazon River; tectono-sedimentary processes	LATE MIOCENE ONSET; SEA FAN EVIDENCE; EASTERN CORDILLERA; SEDIMENTARY RECORD; DRAINAGE REVERSAL; RIVER; SURFACE; UPLIFT; PLATEAU; BASIN	The Cenozoic landscape of northern South America evolved under the influence of different geodynamic processes, culminating in the formation of the largest drainage basin on Earth, the Amazon drainage system. The orogeny of the Andean cordillera and the increase in surface denudation induced an asymmetric influx of sediments in Amazonia, which caused an eastward propagation of the Andean sedimentary wedge, reversing the topographic gradient and driving the drainage flow towards the Atlantic Equatorial margin. The low-relief topography of lowlands in Amazonia is also a factor that propitiates this reversal. Concomitantly, variations in the subduction angle of the Nazca plate under the continental lithosphere during the Miocene also contributed to create dynamic topography that perturbed the surface and modified the drainage pattern through time. In the last decade, both surface processes during Andean orogeny and dynamic topography were invoked independently to explain the formation of the present Amazon drainage system connecting the Andes and the equatorial margin. However, hitherto these mechanisms were not considered in a single model, hampering the evaluation of the contribution of each factor on the evolution of the Amazon River. To quantify the combined effect of the different geodynamic processes, in the present work we used numerical models that integrate orogeny, surface processes, dynamic topography and flexural isostasy of the lithosphere. In our results, we present new numerical scenarios for the Cenozoic landscape evolution of Amazonia, showing that the dynamic topography may have affected the environmental evolution in western Amazonia, favoring the development of a megawetland in this region before the establishment of the Amazon River as a transcontinental river. We conclude that, although the formation of the Amazon drainage system can be explained without the influence of mantle convection, variations in dynamic topography may have anticipated the establishment of the transcontinental drainage system a few million years. Furthermore, the stratigraphic evolution and the total Cenozoic sedimentation preserved in the Solimoes Basin is a function of the temporal variations in the amplitude of dynamic topography in northern South America. (C) 2020 Elsevier B.V. All rights reserved.	[Bicudo, Tacio Cordeiro; Sacek, Victor] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Sao Paulo, Brazil; [de Almeida, Renato Paes] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil	Universidade de Sao Paulo; Universidade de Sao Paulo	Bicudo, TC (autor correspondente), Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Sao Paulo, Brazil.	tacio.bicudo@iag.usp.br	Sacek, Victor/H-6548-2013; Almeida, Renato/AAF-6705-2020; Almeida, Renato/G-2567-2013	Sacek, Victor/0000-0001-9598-5081; Almeida, Renato/0000-0003-3664-1558; Bicudo, Tacio/0000-0002-4424-0722	FAPESP [2017/24870-5]; Petrobras [2017/00461-9]; CNPq [311315/2017-8]; Serrapilheira Institute [Serra-1812-26615]	FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Petrobras(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Serrapilheira Institute	We would like to thank Prof. Brian Horton and an anonymous reviewer for valuable comments and suggestions that significantly improved the quality of the manuscript. This work was supported by FAPESP (grant 2017/24870-5), Petrobras (project 2017/00461-9), CNPq (process 311315/2017-8), and Serrapilheira Institute (grant number Serra-1812-26615).	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Sci. Lett.	SEP 15	2020	546								116423	10.1016/j.epsl.2020.116423	http://dx.doi.org/10.1016/j.epsl.2020.116423			13	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	MP3VM					2023-06-23	WOS:000552134300009
J	de Souza, GA; Soares, MB; Brum, AS; Zucolotto, M; Sayao, JM; Weinschutz, LC; Kellner, AWA				de Souza, Geovane Alves; Soares, Marina Bento; Brum, Arthur Souza; Zucolotto, Maria; Sayao, Juliana M.; Weinschutz, Luiz Carlos; Kellner, Alexander W. A.			Osteohistology and growth dynamics of the Brazilian noasaurid Vespersaurus paranaensis Langer et al., 2019 (Theropoda: Abelisauroidea)	PEERJ			English	Article						Dinosauria; Cretaceous; Vespersaurus; Brazil; Abelisauroidea	BONE MICROSTRUCTURE; DETERMINATE GROWTH; BAURU GROUP; DINOSAUR; EVOLUTION; HISTOLOGY; OSTEOLOGY; PATAGONIA; TENDAGURU; BIRDS	Although the knowledge of bone histology of non-avian theropods has advanced considerably in recent decades, data about the bone tissue patterns, growth dynamics and ontogeny of some taxa such as abelisauroids are still limited. Here we describe the bone microstructure and growth dynamics of the Brazilian noasaurine Vespersaurus paranaensis using five femora and six tibiae and quantify the annual growth marks through retrocalculation of missing ones to estimate ontogenetic ages. The femoral series comprises four femoral histological classes (FHC I-IV), varying from two annuli or LAGs to seven LAGs. Femora show that sexual maturity was achieved around the seventh to tenth year of life, whereas the tibiae suggest it was earlier (around three to five years old). Tibiae represent three histological classes (THC I-III) displaying from three to nine LAGs. Two tibiae (THC III) exhibit an external fundamental system indicating that these specimens reached full skeletal size. The heterogeneous maturity observed in Vespersaurus hind limb bones could result from differential allometry scaling between femora and tibiae length with the body length. The predominant parallel-fibered bone matrix suggests that Vespersaurus grew more slowly than most theropods, including other abelisauroids, in a pattern shared with the noasaurines Masiakasaurus knopfleri from Madagascar and CPPLIP 1490 from Brazil. This deviation from the typical theropod growth pattern may be mainly correlated with small body size, but also may related to resource limitation imposed by the arid climate prevailing in southwestern Gondwana during Cretaceous. Moreover, given the ecological and phylogenetic similarities among these taxa, such features would probably be apomorphic within Noasauridae.	[de Souza, Geovane Alves; Brum, Arthur Souza] Univ Fed Rio de Janeiro, Museu Nacl, Programa Posgrad Zool PPGZoo, Rio De Janeiro, RJ, Brazil; [Soares, Marina Bento; Kellner, Alexander W. A.] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Lab Systemat & Taphon Fossil Vertebrates, Rio De Janeiro, RJ, Brazil; [Zucolotto, Maria] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Rio De Janeiro, RJ, Brazil; [Sayao, Juliana M.] Univ Fed Pernambuco, Ctr Acad Vitoria, Nucleo Biol, Vitoria De Santo Antao, PE, Brazil; [Weinschutz, Luiz Carlos] Univ Contestado, Ctr Paleontol, Mafra, SC, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal de Pernambuco; Universidade do Contestado	Kellner, AWA (autor correspondente), Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Lab Systemat & Taphon Fossil Vertebrates, Rio De Janeiro, RJ, Brazil.	kellner@mn.ufrj.br	Brum, Arthur Souza/ABB-9735-2020; Alves, Geovane/ABA-2121-2020; Kellner, Alexander/ABE-9591-2020; Souza, Geovane Alves de/HTN-7985-2023; Soares, Marina/M-9477-2017	Alves, Geovane/0000-0003-0979-1526; Kellner, Alexander/0000-0001-7174-9447; Souza, Geovane Alves de/0000-0003-0979-1526; da Costa, Arthur Souza Brum/0000-0003-3927-0318; Soares, Marina/0000-0002-8393-2406	Fundacao de Desenvolvimento Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [E-26/202.905/2018, E-26/010.002178/2019]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [420687/2016-5, 313461/2018-0, 311715/2017-6, 307938/2019-0]	Fundacao de Desenvolvimento Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This project was supported by the Fundacao de Desenvolvimento Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ #E-26/202.905/2018 to Alexander W.A. Kellner; #E-26/010.002178/2019 to Marina Bento Soares) and the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq #420687/2016-5 and #313461/2018-0 to Alexander W.A. Kellner; #311715/2017-6 to Juliana M. Sayao; #307938/2019-0 to Marina Bento Soares). There was no additional external funding received for this study. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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S., 2005, THESIS; Veiga FH, 2019, AN ACAD BRAS CIENC, V91, DOI 10.1590/0001-3765201920180643; Wang S, 2017, CURR BIOL, V27, P144, DOI 10.1016/j.cub.2016.10.043; Wilson Jeffrey A., 2003, Contributions from the Museum of Paleontology University of Michigan, V31, P1; Woodward H, 2007, MICROSC MICROANAL, V13, P508; Woodward HN, 2014, PEERJ, V2, DOI 10.7717/peerj.422; Woodward HN, 2013, BONE HISTOLOGY OF FOSSIL TETRAPODS: ADVANCING METHODS, ANALYSIS, AND INTERPRETATION, P195; Woodward HN, 2011, J HERPETOL, V45, P339; Woodward HN, 2011, PLOS ONE, V6, DOI 10.1371/journal.pone.0023339; Xu X, 2009, NATURE, V459, P940, DOI 10.1038/nature08124	79	3	3	0	3	PEERJ INC	LONDON	341-345 OLD ST, THIRD FLR, LONDON, EC1V 9LL, ENGLAND	2167-8359			PEERJ	PeerJ	SEP 15	2020	8								e9771	10.7717/peerj.9771	http://dx.doi.org/10.7717/peerj.9771			32	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	NO1QZ	32983636	gold, Green Published			2023-06-23	WOS:000569262600005
J	Francisquini, MI; Lorente, FL; Pessenda, LCR; Buso , AA; Mayle, FE; Cohen, MCL; Franca, MC; Bendassolli, JA; Giannini, PCF; Schiavo, J; Macario, K				Francisquini, Mariah Izar; Lorente, Flavio Lima; Ruiz Pessenda, Luiz Carlos; Buso Junior, Antonio Alvaro; Mayle, Francis Edward; Lisboa Cohen, Marcelo Cancela; Franca, Marlon Carlos; Bendassolli, Jose Albertino; Fonseca Giannini, Paulo Cesar; Schiavo, JolimarAntonio; Macario, Kita			Cold and humid Atlantic Rainforest during the last glacial maximum, northern Espirito Santo state, southeastern Brazil	QUATERNARY SCIENCE REVIEWS			English	Article						Palynology; Carbon isotopes; Radiocarbon dating; LGM; Tropical forest	SAO-PAULO STATE; LATE PLEISTOCENE; CARBON ISOTOPES; CLIMATE DYNAMICS; SOUTHERN BRAZIL; ORGANIC-MATTER; ATMOSPHERIC CIRCULATION; ENVIRONMENTAL-CHANGES; NORTHEASTERN BRAZIL; RESTINGA VEGETATION	The Atlantic Rainforest, covering the area from northern Espirito Santo to Southern Bahia states, has been considered as a stable forest during Pleistocene Glacial times. Aside from modelling and phylogenetic studies, this hypothesis has never been tested with empirical, fossil pollen, paleo-vegetation data. By using palynology, radiocarbon dating, and carbon and nitrogen elemental and isotopic analyses of organic matter, we reconstructed the vegetation dynamics and inferred climatic changes since the Late Pleistocene in the centre of this global biodiversity hotspot. Our results show that the forest biome was resilient to Last Glacial Maximum - LGM conditions, but that the floristic composition differed from that of today. Since the late glacial, the floristic composition of the dense forest changed from cold- to warm-adapted taxa. Structural, as well as floristic, changes occurred during drier conditions of the early and middle Holocene, with an opening of the forest, providing insights into the type of vegetation impacts that might be expected under predicted future drought. (C) 2020 Elsevier Ltd. All rights reserved.	[Francisquini, Mariah Izar; Lorente, Flavio Lima; Ruiz Pessenda, Luiz Carlos; Buso Junior, Antonio Alvaro; Bendassolli, Jose Albertino] Univ Sao Paulo, Ctr Nucl Energy Agr, Ave Centenario 303, BR-13416000 Piracicaba, SP, Brazil; [Mayle, Francis Edward] Univ Reading, POB 217, Whiteknights, England; [Lisboa Cohen, Marcelo Cancela] Fed Univ Para, R Augusto Correa 1, BR-66075110 Belem, Para, Brazil; [Franca, Marlon Carlos] Fed Inst Para Oceanog & Paleoenvironm Studies, BR-66090100 Belem, Para, Brazil; [Fonseca Giannini, Paulo Cesar] Univ Sao Paulo, Geosci Inst, BR-05508080 Sao Paulo, SP, Brazil; [Schiavo, JolimarAntonio] Mato Grosso Do Sul State Univ, Soil Dept, Rodovia Aquidauana,Km 12, BR-79200000 Aquidauana, MS, Brazil; [Macario, Kita] Fluminense Fed Univ, Phys Dept, LAC UFF AMS Lab, BR-24220900 Niteroi, RJ, Brazil	Universidade de Sao Paulo; University of Reading; Universidade Federal do Para; Universidade de Sao Paulo; Universidade Estadual de Mato Grosso do Sul; Universidade Federal Fluminense	Francisquini, MI (autor correspondente), Univ Sao Paulo, Ctr Nucl Energy Agr, Ave Centenario 303, BR-13416000 Piracicaba, SP, Brazil.	mariah@cena.usp.br	Lorente, Flávio Lima/D-4601-2013; Cohen, Marcelo Cancela Lisboa/AAQ-8080-2020; Giannini, Paulo César Fonseca/D-1871-2015; Buso, Antonio Alvaro/T-3077-2019; Macario, Kita/ADE-6381-2022; Francisquini, Mariah/I-5908-2014	Cohen, Marcelo Cancela Lisboa/0000-0001-9892-4719; Giannini, Paulo César Fonseca/0000-0003-1046-0177; Buso, Antonio Alvaro/0000-0002-5953-1944; Ruiz Pessenda, Luiz Carlos/0000-0001-9119-8195; Francisquini, Mariah/0000-0002-2560-4754; Mayle, Francis/0000-0001-9208-0519	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP, Brazil) [2013/15768-1, 2011/0095-7]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil) [200086/2016-2]	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP, Brazil)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was funded by Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP, Brazil 2013/15768-1 and 2011/0095-7) and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brazil 200086/2016-2). We thank the editors, an anonymous reviewer and Encarni Montoya for their constructive comments that helped us to improve this paper.	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Sci. Rev.	SEP 15	2020	244								106489	10.1016/j.quascirev.2020.106489	http://dx.doi.org/10.1016/j.quascirev.2020.106489			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	NK6ZY		Green Accepted			2023-06-23	WOS:000566884300001
J	Rodrigues, FCG; Giannini, PCF; Fornari, M; Sawakuchi, AO				Rodrigues, Fernanda C. G.; Giannini, Paulo C. F.; Fornari, Milene; Sawakuchi, Andre O.			Deglacial climate and relative sea level changes forced the shift from eolian sandsheets to dunefields in southern Brazilian coast	GEOMORPHOLOGY			English	Article						Eolian coastal systems; Morphological changes; LGM	SANTA-CATARINA STATE; LATE PLEISTOCENE; FLUVIAL SEDIMENT; HOLOCENE; LUMINESCENCE; EVOLUTION; QUARTZ; SINGLE; STABILITY; BARRIER	Quaternary sea level and climate changes can promote spatio-temporal shifts in themorphology of coastal eolian depositional systems. A shift of depositional features such as from sandsheets to dunefields occurs as response to a disequilibrium condition in the system promoted by changes in accumulation space and sediment supply balance. On the other hand, the eolian system migration, with maintenance of morphological patterns, points to an equilibrium conservation under minor variations in the external controlling factors of the system. The Santa Catarina coast in southern Brazil hosts widespread active and stabilized eolian depositional systems with varied morphology. In this study, geomorphologic and stratigraphic changes of eolian deposits of the southern coast of Santa Catarina were constrained by optically stimulated luminescence (OSL) dating. This allowed to assess how coastal eolian systems responded to late Quaternary climate and sea level changes. Eolian sandsheets initiated around 22 ka ago, during the Last Glacial Maximum (LGM), and persisted during most of the deglacial period under conditions characterized by sea level lowstand, wider exposition of shelf sediments, more continental and drier climate and scarcer vegetation cover in the study setting. The shift from eolian sandsheets to dunefields occurred approximately at 6 ka ago and marks the establishment of coastal conditions in the study setting. The development of dunefields since the middle Holocene would result from eolian system disequilibrium in response to a condition characterized by sea level highstand, wetter climate and denser vegetation cover. The maintenance of a dunefield morphology since 6 ka ago, despite its onshore migration, indicates a new equilibrium between accumulation space and sediment supply. Sandsheets evolved to dunefields around 6 ka ago when the coastline stabilized and the accumulation space was limited by onshore vegetation growth, favoring eolian sediment aggradation. The precipitation ridge in the inner margin of the dunefield has been successively stabilized, abandoned and repositioned seaward, accompanying the coastal progradation since 4 ka ago. The decreasing migration rate of dunefields since 4 ka ago is attributed to rainfall reduction, which deplete fluvial sediment supply to coastal systems and, therefore, slow down the coastal progradation rate. (C) 2020 Elsevier B.V. All rights reserved.	[Rodrigues, Fernanda C. G.; Giannini, Paulo C. F.; Sawakuchi, Andre O.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, Sao Paulo, SP, Brazil; [Fornari, Milene] Univ Estadual Paulista, Inst Biociencias, Campus Litoral Paulista, Sao Vicente, SP, Brazil	Universidade de Sao Paulo; Universidade de Sao Paulo; Universidade Estadual Paulista	Rodrigues, FCG (autor correspondente), Univ Sao Paulo, Inst Geociencias, Rua Lago 562, Sao Paulo, SP, Brazil.	cgrfernanda@usp.br	Giannini, Paulo César Fonseca/D-1871-2015; Sawakuchi, André O/D-1445-2013	Giannini, Paulo César Fonseca/0000-0003-1046-0177; Costa Goncalves Rodrigues, Fernanda/0000-0003-1236-7937	Graduate Program in Geosciences of the Instituto de Geociencias, Universidade de Sao Paulo; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [304727/20172, 308772/2018-0, 428341/2018-7, 131977/2015-6]; FAPESP [09/53988-8, 09/54232-4]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [09/53988-8] Funding Source: FAPESP	Graduate Program in Geosciences of the Instituto de Geociencias, Universidade de Sao Paulo; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	FCGR was funded by the Graduate Program in Geosciences of the Instituto de Geociencias, Universidade de Sao Paulo and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq grant 131977/2015-6). PCFG and AOS are funded by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq grants 304727/20172, 308772/2018-0, 428341/2018-7) and FAPESP (09/54232-4). The OSL datings were made in laboratory created under the auspices of FAPESP (09/53988-8).	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J	Romero, GR; Sanchez, EAM; Soares, JL; Nogueira, ACR; Fairchild, TR				Romero, Guilherme Raffaeli; Sanchez, Evelyn A. M.; Soares, Joelson Lima; Rodrigues Nogueira, Afonso Cesar; Fairchild, Thomas R.			Waxing and waning of microbial laminites in the aftermath of the Marinoan glaciation at the margin of the Amazon Craton (Brazil)	PRECAMBRIAN RESEARCH			English	Article						Marinoan cap carbonate; Microbialites; Tubestone structures; Araras Group; Early Ediacaran	PUGA CAP CARBONATE; SNOWBALL EARTH; ISOTOPE GEOCHEMISTRY; NOONDAY DOLOMITE; DEATH-VALLEY; EDIACARAN; STROMATOLITES; RECORD; SEDIMENTOLOGY; ORIGIN	At the margin of the Amazon Craton (west-central Brazil), the Mirassol D'Oeste Formation comprises an emblematic, 16 m-thick Marinoan cap dolostone deposited directly upon diamictites of the Puga Formation. Laterally continuous and morphologically simple microbialites, a common component of Marinoan cap carbonates, begin two meters above the base of the formation and continue upwards as stratiform, domical and irregular wavy microbial laminate boundstones for approximately 10 m. These microbialites consist of alternating thin and thick laminae of peloids (micritized remains of microbial colonies) and subordinate micrite with spar-filled fenestrae that differ in the greater relative abundance of fenestrae in the thicker laminae. The microbialites developed profusely in a calm platformal environment below storm-wave base level, but within the photoic zone, without any contribution of siliciclastics, the Waxing phase of growth. Vertical dolomicrite-filled tubestone structures up to 10 m, occupy the apical portion of the broad domical microbial laminites, Confined percolation of fluids seems the most plausible hypothesis for their origin. The wanning phase began in the final meter of the boundstone consists of irregularly wavy microbial laminites indicating prolonged oscillatory waveaction, followed by dolomitic peloidal grainstone-packstone with megaripple and millimetric macropeloids generated by oscillatory wave action during tradewinds. The hydrodynamic change and a rising sea level put an end to microbialite deposition in the Mirassol D'Oeste cap carbonate.	[Romero, Guilherme Raffaeli; Fairchild, Thomas R.] Univ Sao Paulo, Inst Geociencias, Dept Sedimentary & Environm Geol, Rua Lago 562, BR-05508080 Butanta, SP, Brazil; [Soares, Joelson Lima; Rodrigues Nogueira, Afonso Cesar] Univ Para, Fac Geol, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa S-N, BR-66075110 Belem, Para, Brazil; [Sanchez, Evelyn A. M.] Univ Fed Vales Jequitinhonha & Mucuri, Inst Ciencia & Tecnol, Rodovia MGT 376,Km 583,5000, BR-39100000 Diamantina, MG, Brazil	Universidade de Sao Paulo; Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM)	Romero, GR (autor correspondente), Univ Sao Paulo, Inst Geociencias, Dept Sedimentary & Environm Geol, Rua Lago 562, BR-05508080 Butanta, SP, Brazil.	graffaeli@usp.br	Fairchild, Thomas Rich/AAE-1835-2021; Bizan, Evelyn Aparecida Mecenero Sanchez/AAQ-1690-2021	Raffaeli Romero, Guilherme/0000-0001-9955-0878; NOGUEIRA, AFONSO/0000-0002-5225-9255	FAPESP (Fundacao de Apoio a Pesquisa do Estado de Sao Paulo) [2012/1331-8]; CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)	FAPESP (Fundacao de Apoio a Pesquisa do Estado de Sao Paulo)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors thank FAPESP (Fundacao de Apoio a Pesquisa do Estado de Sao Paulo) (Proc 2012/1331-8) for the doctoral scholarship provided to the first author and the Geochemical and Geotectonic Graduate Program of the Institutode Geociencias of the Universidade de Sao Paulo. To CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) for the postdoctoral scholarship in the PPGG (Programa de Pos-Graduacao em Geologia e Geoquimica) -Universidade Federal do Para. We also thank Ms. Bruno Kerber Becker for help with the figures and discussions. To Dr. Isaac Rudnitzki for the help in the field trip and revision of the manuscript, and Dr. Luana Morais for the discussions regarding the tubestone structures. The authors would like to thank the anonymous reviewers and Dr. Paul Hoffman and Dr. Paulo Cesar Boggiani for their suggestions and criticism of the manuscript.	Ahm ASC, 2019, EARTH PLANET SC LETT, V506, P292, DOI 10.1016/j.epsl.2018.10.046; Allen PA, 2005, NATURE, V433, P123, DOI 10.1038/nature03176; Alvarenga C. J. S., 2000, TECTONIC EVOLUTION S, P183; [Anonymous], 1969, GEOLOGICAL SURVEY CA; Babinski M., 2006, P 5 S AM S IS GEOL P, P303; Boggiani P. 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SEP 15	2020	348								105856	10.1016/j.precamres.2020.105856	http://dx.doi.org/10.1016/j.precamres.2020.105856			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NL0BK					2023-06-23	WOS:000567091500001
J	Carneiro, MT; Perez, DV; Feitosa, RC; Wasserman, JC				Carneiro, Marcos Tavares; Perez, Daniel Vidal; Feitosa, Renato Castiglia; Wasserman, Julio Cesar			Separation ofEscherichia colifrom natural samples for identification of sources and microcosm inoculation	BRAZILIAN JOURNAL OF MICROBIOLOGY			English	Article						Escherichia coli; Wastewater; Microbial source tracking; Bacteria decay; Wild strains	ESCHERICHIA-COLI; GENETIC-MARKERS; SOURCE TRACKING; WATER; BACTERIA; SURVIVAL; INDICATORS; DECAY; SAND	Obtaining unculturedEscherichia colifrom natural waters is an important step in the study of microbes in the environment, which are critical for bacterial decay and microbial source tracking. The quality of the samples used can influence the assays, because high contaminant concentrations, differing cell ages, and physiologic states can impair results. The proposed separation is based on a three-step filtration method applied to replicates of seven samples from a sewage plant affluent, collected in different periods. Aliquots of the leachate were inoculated into microcosms, aiming to observe the cultivability of the cells. The assay resulted in colimetry values ranging between 10(4)and 10(5)cells. In the leachate, averages of 1.05% of total coliforms and 1.10% ofEscherichia coliwere recovered from original samples. Although enduring unfavorable temperatures, salinities, and nutritional conditions, the inoculated microcosm populations grew approximately 310 times after 24 h. The final leachate contained cultivable cells in appropriate physiological states and quantities for inoculum in microcosm sets. The bacteria obtained from the leachate were also appropriate for surveys of microbial source tracking, because, in the developed procedure, organisms were separated from contaminants, while cell concentrations were sufficient for inocula.	[Carneiro, Marcos Tavares] Escola Engn UFF, Programa Posgrad Sistemas Gestao Sustentaveis, Niteroi, RJ, Brazil; [Carneiro, Marcos Tavares; Feitosa, Renato Castiglia] Fiocruz MS, Escola Nacl Saude Publ, Dept Saneamento, Rio De Janeiro, Brazil; [Perez, Daniel Vidal] EMBRAPA Solos, Rio De Janeiro, Brazil; [Wasserman, Julio Cesar] Univ Fed Fluminense, Network Environm & Sustainable Dev, Niteroi, RJ, Brazil; [Wasserman, Julio Cesar] Univ Fed Fluminense, Postgrad Program Geochem, Niteroi, RJ, Brazil; [Wasserman, Julio Cesar] Inst Geosci, Network Environm & Sustainable Dev, Av Litoranea S-N, BR-24210346 Niteroi, RJ, Brazil	Fundacao Oswaldo Cruz; Empresa Brasileira de Pesquisa Agropecuaria (EMBRAPA); Universidade Federal Fluminense; Universidade Federal Fluminense	Wasserman, JC (autor correspondente), Univ Fed Fluminense, Network Environm & Sustainable Dev, Niteroi, RJ, Brazil.; Wasserman, JC (autor correspondente), Univ Fed Fluminense, Postgrad Program Geochem, Niteroi, RJ, Brazil.; Wasserman, JC (autor correspondente), Inst Geosci, Network Environm & Sustainable Dev, Av Litoranea S-N, BR-24210346 Niteroi, RJ, Brazil.	geowass@vm.uff.br	Wasserman, Julio/HGA-8235-2022; Wasserman, Julio Cesar/K-3863-2014; Carneiro, Marcos T/O-7788-2018; Wasserman, Julio/GZL-6568-2022	Wasserman, Julio/0000-0002-7828-5240; Wasserman, Julio Cesar/0000-0002-7828-5240; Carneiro, Marcos T/0000-0002-8419-8549; Castiglia Feitosa, Renato/0000-0003-0724-1993	Brazilian Council of Scientific and Technological Development -CNPq [306714/2013-2]	Brazilian Council of Scientific and Technological Development -CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was supported by the Brazilian Council of Scientific and Technological Development -CNPq (grant number 306714/2013-2) to JCW.	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J. Microbiol.	DEC	2020	51	4					2015	2020		10.1007/s42770-020-00374-2	http://dx.doi.org/10.1007/s42770-020-00374-2		SEP 2020	6	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	QE2TU	32920714	Green Published			2023-06-23	WOS:000568639600001
J	de Almeida-Lima, DS; Piovesan, EK; Sayao, JM; de Lima, FJ				de Almeida-Lima, Debora Soares; Piovesan, Enelise Katia; Sayao, Juliana Manso; de Lima, Flaviana Jorge			Description and ontogeny of Pattersoncypris minima sp. nov. (Crustacea: Ostracoda), Araripe Basin, Northeast Brazil	ZOOTAXA			English	Article						Taxonomy; ostracod; taphonomy; Cretaceous; ontogenetic development	ALAGAMAR FORMATION; POTIGUAR BASIN; BIOSTRATIGRAPHY; TAXONOMY; SEQUENCE; JATOBA; GENERA	Representatives of the Class Ostracoda are widely used as tools in applied paleoecological and biostratigraphical studies in all continents. In the Araripe Basin. located in the northeastern of Brazil, the Romualdo Fonnation is one of the most studied, not only for the preservation but also for the abundance of its fossils. The ostracod genus Pattersoncypris Bate, 1972 is well-represented in this formation and it is the most abundant, which reinforces the importance of its taxonomic study. In this work, Pattersoncypris minima sp. nov. is described for the Romualdo Formation as a contribution to the knowledge on Brazilian Cretaceous non-marine ostracods. Taphonomic aspects are also presented, considering the complete ontogenetic stages of the material.	[de Almeida-Lima, Debora Soares] Univ Fed Pernambuco, Programa Posgrad Geociencias, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Piovesan, Enelise Katia] Univ Fed Pernambuco, Dept Geol, Programa Posgrad Geociencias, Litpeg, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Sayao, Juliana Manso] Univ Fed Pernambuco, Ctr Acad Vitoria, Lab Paleobiol & Microestruturas, Rua Alto Reservatorio S-N, BR-55608250 Vitoria De Santo Antao, PE, Brazil; [de Lima, Flaviana Jorge] Univ Reg Cariri, Dept Ciencias Biol, Lab Paleontol URCA, Rua Coronel Antonio Luis 1161, BR-63105000 Crato, Ceara, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Regional do Cariri	de Almeida-Lima, DS (autor correspondente), Univ Fed Pernambuco, Programa Posgrad Geociencias, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil.	deboraalmeeida@hotmail.com; katiapiovesan@gmail.com; jmsayao@gmail.com; flavianajorge@gmail.com	Piovesan, Enelise Katia/Q-2953-2017	Piovesan, Enelise Katia/0000-0002-0433-0395; Sayao, juliana/0000-0002-3619-0323				Aguilar-Alberola JA, 2013, J CRUSTACEAN BIOL, V33, P348, DOI 10.1163/1937240X-00002133; Almeida R, 2002, CAN J REMOTE SENS, V28, P96, DOI 10.5589/m02-006; Anderson F.W, 1966, B BRIT MUS NAT HIST, V11, P432; Antonietto LS, 2016, EUR J TAXON, V244, P1, DOI 10.5852/ejt.2016.244; Antonietto LS, 2012, J PALEONTOL, V86, P659, DOI 10.1666/11-012R.1; Assine ML., 2007, B GEOCIENCIAS PETROB, V15, P371; Assine ML., 2014, B GEOCI PETROBRAS, V22, P3, DOI DOI 10.25249/0375-7536.1992289300; Baird W., 1845, HIST BERWICKSHIRE NA, V2, P145, DOI DOI 10.1139/F83-210; BATE R H, 1972, Palaeontology (Oxford), V15, P379; Bate R.H., 1973, Stereo Atlas of Ostracod Shells, V1, P101; Bosquet J., 1852, EMOIRES COURONNES ME, V24, P1; Brady G.S., 1885, Q J GEOL SOC LOND, V41, P1, DOI 10.1144/GSL.JGS.1885.041.01-04.31; Brady G.S., 1889, SCI T ROYAL DUBLIN 2, V4, P63, DOI DOI 10.1080/00222938909460549; Branson C.C., 1936, J PALEONTOL, V10, P1; Carbonel P., 1988, P157; Chapman F., 1901, Annals of Natural History, V(7), P141; Coimbra JC, 2002, GEOBIOS-LYON, V35, P687; Do CARMO D. 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C., 1983, APPL OSTRACODA, P51; Wicher C.A., 1959, GEOL JB, V77, P35	59	3	3	0	1	MAGNOLIA PRESS	AUCKLAND	PO BOX 41383, AUCKLAND, ST LUKES 1030, NEW ZEALAND	1175-5326	1175-5334		ZOOTAXA	Zootaxa	SEP 9	2020	4851	1					171	179		10.11646/zootaxa.4851.1.8	http://dx.doi.org/10.11646/zootaxa.4851.1.8			9	Zoology	Science Citation Index Expanded (SCI-EXPANDED)	Zoology	NR3RM	33056743				2023-06-23	WOS:000571480900004
J	Ramos, BFM; de Almeida, PF; Chinalia, FA				Ramos, Bethania Felix Miranda; de Almeida, Paulo Fernando; Chinalia, Fabio Alexandre			Bacterial xanthan and ramnolipid simultaneous production using industrial oil produced water	ENVIRONMENTAL TECHNOLOGY			English	Article						Co-culture; bioprocess; EOR; xanthan gum; rhamnolipid	GUM; BIOSURFACTANT; RECOVERY	The present work aimed to give an economical destiny to the produced water, a residue generated by the oil and gas industry by means of producing bioactives such as xanthan gum and ramnolipid. These compounds are often used in combination during enhanced oil recovery strategies. On the other hand, reports on co-culture of bacterial strains that are responsible for their production are rare. This research shows a factorial design method associated with surface response analysis to optimize carbon sources, sucrose and crude glycerin, and fermentation agents for culturingXanthomonas campestrisandPseudomonas aeruginosausing the described conditions. After the critical point validation resulting in xanthan and ramnolipid production of 8.69 and 4.80 g L-1, quality tests showed an apparent viscosity of 1006 cP with an emulsifying activity abouve 50% for 94 h.	[Ramos, Bethania Felix Miranda] Univ Fed Bahia, Chem Engn Dept, Salvador, BA, Brazil; [de Almeida, Paulo Fernando; Chinalia, Fabio Alexandre] Univ Fed Bahia, Biointeract Sci Dept, Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia	Ramos, BFM (autor correspondente), Univ Fed Bahia, Chem Engn Dept, Salvador, BA, Brazil.	Bethania_ea@hotmail.com	Almeida, Paulo F/HTQ-3119-2023		Conselho Nacional de Desenvolvimento Cientifico e Tecnologico project [402822/2013-7]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico project	This work was supported by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico project Number 402822/2013-7.	ABURUWAIDA AS, 1991, ACTA BIOTECHNOL, V11, P315, DOI 10.1002/abio.370110405; Ahmadun FR, 2009, J HAZARD MATER, V170, P530, DOI 10.1016/j.jhazmat.2009.05.044; Al-Bahry SN, 2013, APCBEE PROC, V5, P242, DOI 10.1016/j.apcbee.2013.05.042; APHA, 2012, STAND METH EX WAT WA; Brandao LV, 2010, POLIMEROS, V20, P175, DOI 10.1590/S0104-14282010005000029; Chandrasekaran EV, 1980, METHODS CARBOHYDRATE, VIII; COOPER DG, 1987, APPL ENVIRON MICROB, V53, P224, DOI 10.1128/AEM.53.2.224-229.1987; Diniz DD, 2012, POLIMEROS, V22, P278, DOI 10.1590/S0104-14282012005000032; DUBOIS M, 1956, ANAL CHEM, V28, P350, DOI 10.1021/ac60111a017; Galindo E, 1996, ENZYME MICROB TECH, V19, P145, DOI 10.1016/0141-0229(95)00215-4; Garcia-Ochoa F, 2000, BIOTECHNOL ADV, V18, P549, DOI 10.1016/S0734-9750(00)00050-1; Haba E, 2000, J APPL MICROBIOL, V88, P379, DOI 10.1046/j.1365-2672.2000.00961.x; Han DK, 1999, J PETROL SCI ENG, V22, P181, DOI 10.1016/S0920-4105(98)00067-9; JEANES A, 1974, FOOD TECHNOL-CHICAGO, V28, P34; Kampen WH., 1997, FERMENTATION BIOCH E; Montgomery D., 2016, DESIGN ANAL EXPT, V8th; Nedjhioui M, 2005, DESALINATION, V185, P543, DOI 10.1016/j.desal.2005.05.013; Ochsner U A, 1996, Adv Biochem Eng Biotechnol, V53, P89; Palaniraj A, 2011, J FOOD ENG, V106, P1, DOI 10.1016/j.jfoodeng.2011.03.035; RAJESHWARI KV, 1995, LETT APPL MICROBIOL, V21, P173, DOI 10.1111/j.1472-765X.1995.tb01034.x; Raza ZA, 2007, J ENVIRON SCI HEAL A, V42, P73, DOI 10.1080/10934520601015784; REILING HE, 1986, APPL ENVIRON MICROB, V51, P985, DOI 10.1128/AEM.51.5.985-989.1986; Ronkart SN., 2012, 114 DION CORP THERM; Rottava I, 2009, CARBOHYD POLYM, V77, P65, DOI 10.1016/j.carbpol.2008.12.001; Shah AK, 1999, J IND MICROBIOL BIOT, V23, P442, DOI 10.1038/sj.jim.2900737; Silva MF, 2009, J FOOD ENG, V90, P119, DOI 10.1016/j.jfoodeng.2008.06.010; Stephenson MT., 1991, COMPONENTS PRODUCED, P25; Wei YH, 2005, BIOCHEM ENG J, V27, P146, DOI 10.1016/j.bej.2005.08.028; Willumsen PA, 1997, BIODEGRADATION, V7, P415, DOI 10.1007/BF00056425	29	2	2	1	9	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0959-3330	1479-487X		ENVIRON TECHNOL	Environ. Technol.	MAR 21	2022	43	7					983	990		10.1080/09593330.2020.1812729	http://dx.doi.org/10.1080/09593330.2020.1812729		SEP 2020	8	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	ZI4XE	32811371				2023-06-23	WOS:000569792600001
J	Soares, R; de Mello, MCS; da Silva, CM; Machado, W; Arbilla, G				Soares, Ricardo; Santiago de Mello, Marcia Cristina; da Silva, Cleyton M.; Machado, Wilson; Arbilla, Graciela			Online Chemistry Education Challenges for Rio de Janeiro Students during the COVID-19 Pandemic	JOURNAL OF CHEMICAL EDUCATION			English	Article						General Public; Interdisciplinary/Multidisciplinary; Professional Development; Distance Learning/Self Instruction; Internet/Web-Based Learning		Thirty-six days after the beginning of the 2020 school year in Brazil, the Rio de Janeiro state education system began an unprecedented disruptive period due to the COVID-19 crisis, which abruptly affected general educational activities, particularly chemistry teaching. An adaptation to a new paradigm of remote teaching and massive use of online educational technology alternatives was tentatively performed, generating lessons for improving implemented actions. Educational institutions prepared independent teaching strategies to provide remote chemistry classes for a total of nearly 397,700 students who were able to begin or continue chemistry classes. This snapshot of a daily-life reality faced by professionals engaged in chemistry education in Rio de Janeiros schools identified the following factors that negatively affected the implemented actions: the applied television broadcaster essentially covered only the heavily urbanized region, leaving out rural and impoverished areas; a significant absence of adequate technological equipment (e.g., smartphones, tablets, notebooks) for students; pedagogical limitations of instructors, without sufficient training to use online technologies; and inherent limitations of video classes, which do not adequately substitute for practical learning in chemistry laboratories. Strategy improvements are imperative, considering that students face the challenge of increasingly being protagonists for the organization and management of the teachinglearning process.	[Santiago de Mello, Marcia Cristina] Rio de Janeiro State Dept Educ, BR-20040000 Rio De Janeiro, RJ, Brazil; [da Silva, Cleyton M.] Univ Veiga de Almeida, BR-20271020 Rio De Janeiro, RJ, Brazil; [Soares, Ricardo; Machado, Wilson] Fed Fluminense Univ, Inst Chem, Geochem Program, BR-24020007 Niteroi, RJ, Brazil; [Arbilla, Graciela] Univ Fed Rio de Janeiro, Inst Chem, BR-21941909 Rio De Janeiro, RJ, Brazil	Universidade Veiga de Almeida (UVA); Universidade Federal Fluminense; Universidade Federal do Rio de Janeiro	Soares, R (autor correspondente), Fed Fluminense Univ, Inst Chem, Geochem Program, BR-24020007 Niteroi, RJ, Brazil.	ricardos@inea.rj.gov.br	Machado, Wilson/P-8047-2019; Arbilla, Graciela/X-5847-2019; da Silva, Cleyton Martins/AAC-4993-2020; Soares, Ricardo/AAM-7896-2021	Machado, Wilson/0000-0003-3117-8584; Arbilla, Graciela/0000-0001-7732-8336; da Silva, Cleyton Martins/0000-0002-5216-4977; Soares, Ricardo/0000-0002-0353-3174	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brasil [001]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brasil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brasil (Finance Code 001).	Croda J, 2020, REV SOC BRAS MED TRO, V53, DOI 10.1590/0037-8682-0167-2020; Dantas G, 2020, SCI TOTAL ENVIRON, V729, DOI 10.1016/j.scitotenv.2020.139085; Hensen C, 2019, J CHEM EDUC, V96, P2097, DOI 10.1021/acs.jchemed.9b00561; Holme TA, 2020, J CHEM EDUC, V97, P1219, DOI 10.1021/acs.jchemed.0c00377; Lichter J, 2012, J CHEM EDUC, V89, P1133, DOI 10.1021/ed200531j; Ministerio da Educacao, RED FED ED PROF; Potgieter M., 2019, RES PRACTICE CHEM ED; Ribeiro A., 2020, ESCOLAS PRIVADAS BUS; Siciliano B, 2020, SCI TOTAL ENVIRON, V737, DOI 10.1016/j.scitotenv.2020.139765; Silva CM, 2020, REV VIRTUAL QUIM, V12, P1001, DOI 10.21577/1984-6835.20200081; Smith DK, 2014, J CHEM EDUC, V91, P1594, DOI 10.1021/ed400715s; Thomas Michael S C, 2020, Prospects (Paris), V49, P87, DOI 10.1007/s11125-020-09468-z	12	11	13	2	19	AMER CHEMICAL SOC	WASHINGTON	1155 16TH ST, NW, WASHINGTON, DC 20036 USA	0021-9584	1938-1328		J CHEM EDUC	J. Chem. Educ.	SEP 8	2020	97	9					3396	3399		10.1021/acs.jchemed.0c00775	http://dx.doi.org/10.1021/acs.jchemed.0c00775			4	Chemistry, Multidisciplinary; Education, Scientific Disciplines	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Education & Educational Research	NP2MX					2023-06-23	WOS:000570016400171
J	Aguilera, O; Bencomo, K; de Araujo, OMO; Dias, BB; Coletti, G; Lima, D; da Silva-Caminha, SAF; Polck, M; Martins, MVA; Jaramillo, C; Kutter, VT; Lopes, RT				Aguilera, Orangel; Bencomo, Karen; Oliveira de Araujo, Olga M.; Dias, Bruna Borba; Coletti, Giovanni; Lima, Daniel; da Silva-Caminha, Silane A. F.; Polck, Marcia; Alves Martins, Maria Virginia; Jaramillo, Carlos; Kutter, Vinicius Tavares; Lopes, Ricardo Tadeu			Miocene heterozoan carbonate systems from the western Atlantic equatorial margin in South America: The Pirabas formation	SEDIMENTARY GEOLOGY			English	Article						Tropical South America; Fossil assemblages; Ichnofossils; miaoCT; Micro- and macroporosity	PARA STATE; MIDDLE MIOCENE; SEA-LEVEL; FORAMINIFERAL BIOSTRATIGRAPHY; ENVIRONMENTAL SIGNIFICANCE; CHILCATAY FORMATION; PISCO BASIN; FACIES; CHEILOSTOMATA; NEOGENE	Outcrops of Neogene carbonates of the North Brazilian platform occur exclusively along the equatorial coast and represent some of the few existing examples of Neogene carbonate systems of the Atlantic coast of South America. The Pirabas Formation (early-middle Miocene) is the northernmost part of this platform. Although onshore mainly consists of small and scattered outcrops, it considerably extends in the subsurface keeping record of relevant geological and paleontological episodes of tropical South American history. Intending to improve the knowledge of South American carbonate and providing a solid basis for future comparisons between the Pirabas Basin and other, largely subsurface, Cenozoic basins, this research investigates the Aricuru outcrops by combining a standard petrographical and paleontological approach with advanced microCT analyses. The Aricuru area is characterized by mixed silicidastic-carbonate sand-sized deposits, which probably deposited after the early Miocene according to the palynological assemblage. The bioclastic fraction of the rock is dominated by benthic foraminifera (mostly soritids, amphisteginids, small rotaliids, and small miliolids, typical of marginal marine environments), bryozoans, calcareous algae (Halimeda), echinoderms and mollusks. The abundant siliciclastic fraction together with the taxonomic composition of the foraminiferal, echinodermal, crustacean, ichnofossil and fish assemblages indicates deposition in a tropical coastal environment featuring both protected and more exposed sectors. The carbonate system probably developed under abundant nutrient supply, which fostered heterotroph suspension feeders over hermatypic corals. The demise of this system was most likely caused by a growth in silicidastic input due to increased rainfall in the coastal area. The sedimentary evolution of the Pirabas Formation is similar to the one of the Foz do Amazonas Basin, and fits well with the general evolutionary trend of Cenozoic carbonate factories of the region, indicating the potential of the Pirabas subsurface record for understanding other Cenozoic basins, their paleoenvironmental significance, and their potential as oil, gas and water reservoirs. (C) 2020 Elsevier B.V. All rights reserved.	[Aguilera, Orangel; Bencomo, Karen; Dias, Bruna Borba; Lima, Daniel] Fluminense Fed Univ UFF, Paleoecol & Global Changes Lab, Campus Gragoata,Bloco M,Lab 110, BR-24210200 Niteroi, RJ, Brazil; [Oliveira de Araujo, Olga M.; Lopes, Ricardo Tadeu] Fed Univ Rio de Janeiro UFRJ, Nucl Engn Program COPPE, Nucl Instrumentat Lab, Av Horacio Macedo,Cidade Univ, BR-21941450 Rio De Janeiro, Brazil; [Coletti, Giovanni] Univ Milano Bicocca, Dept Environm Sci & Earth Sci, Piazza Sci 4, I-20126 Milan, Italy; [da Silva-Caminha, Silane A. F.] Fed Univ Mato Grosso UFMT, Paleontol & Palynol Lab, Cuiaba, Mato Grosso, Brazil; [Polck, Marcia] Agencia Nacl Mineracao ANM, Ave Nilo Pecanha 50,7 Andar,Grp 709,713 Ctr, BR-20044900 Rio De Janeiro, RJ, Brazil; [Alves Martins, Maria Virginia] Rio de Janeiro State Univ UERJ, Sao Francisco Xavier 524,LabMicro 4037F, BR-20550013 Rio De Janeiro, RJ, Brazil; [Alves Martins, Maria Virginia] Aveiro Univ, Dept Geosci, GeoBioTec, Campus Santiago, P-3810197 Aveiro, Portugal; [Jaramillo, Carlos] Smithsonian Trop Res Inst, Balboa, Ancon, Panama; [Jaramillo, Carlos] Univ Montpellier, CNRS, EPHE, ISEM,IRD, Montpellier, France; [Kutter, Vinicius Tavares] Fed Univ Para UFPA, Geosci Inst, Belem, Para, Brazil	Universidade Federal Fluminense; University of Milano-Bicocca; Universidade Federal de Mato Grosso; Universidade Federal de Mato Grosso do Sul; Universidade do Estado do Rio de Janeiro; Universidade de Aveiro; Smithsonian Institution; Smithsonian Tropical Research Institute; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; UDICE-French Research Universities; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); Universidade Federal do Para	Aguilera, O (autor correspondente), Fluminense Fed Univ UFF, Paleoecol & Global Changes Lab, Campus Gragoata,Bloco M,Lab 110, BR-24210200 Niteroi, RJ, Brazil.	orangelaguilera@id.uff.br; ksegueri@id.uff.br; oaraujo@coppe.ufrj.br; brunaborbadias@id.uff.br; giovanni.coletti@unimib.it; djmlima@id.uff.br; Silane@ufmt.br; marcia.polck@gmail.com; virginia.martins@ua.pt; jaramilloC@si.edu; viniciuskutter@id.uff.br; ricardo@lin.ufrj.br	da Silva Caminha, Silane Aparecida Ferreira/M-6972-2016; Alves Martins, Maria Virginia Virginia/O-2893-2013; Aguilera, Orangel/D-5055-2013; Dias, Bruna Borba/AAV-4379-2020; Martins, Maria/IQT-0561-2023; Lima, Daniel/C-6387-2015; Lopes, Ricardo/CAH-3736-2022	da Silva Caminha, Silane Aparecida Ferreira/0000-0003-4853-2789; Alves Martins, Maria Virginia Virginia/0000-0001-8348-8862; Dias, Bruna Borba/0000-0001-5518-2807; Lima, Daniel/0000-0002-3039-9134; Araujo, Olga/0000-0002-6287-0592; jaramillo, carlos/0000-0002-2616-5079	Brazilian Council of Science and Technological Development - CNPq [404937/2018-7, 305269/2017-8, 302676/2019-8, 309481/2016-3]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) (grant PBMAC-UFF) [001]; Postgraduate Program in Marine Biology and Coastal Ecosystem (PBMAC-UFF internal grant), Research Support Foundation of the State of Rio de Janeiro-FAPERJ [202.927/2019]	Brazilian Council of Science and Technological Development - CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) (grant PBMAC-UFF)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Postgraduate Program in Marine Biology and Coastal Ecosystem (PBMAC-UFF internal grant), Research Support Foundation of the State of Rio de Janeiro-FAPERJ	The authorswould like to thank the National Mining Agency of Brazil (ANM) for authorization to collect samples at the Pirabas Formation in the Maracana municipality, Para state, Brazil (COPAL protocol 040/2019 and 011/2020). Many thanks to Afonso Nogueira and Afonso Quaresma de Lima from the Federal University of Para (UFPA), Brazil, for collaboration and support during the field trip to Aricuru locality. The authors are very grateful to Andreas Kroh from the Karl-Franzens Universitat Graz for review the identifications of ophiuroids and crinoids, Jorge Carrillo-Briceno from the University of Zurich for review the identifications of elasmobranchs, Andressa Nogueira from the UFPA for reviewing the identifications of ostracods, Kamil Zagorsek from the Technical University of Liberec for reviewing the identifications of bryozoans, Joelson Soares (UFPA) and Luis Quiroz fromthe University of Saskatchewan for the opportunity to discuss ichnofossils. Thanks to Vladimir Tavora (UFPA) for the friendly discussion and the opportunity to followhis pioneering contribution fromthe Aricuru outcrop and the microfossil assemblage, and toMaria Ines Feijo for the collaborative support to access crustacean decapod collections from the Emilio Goeldi Paraense Museum (MPEG), Brazil. We thanks to Joelma Lobo (UFPA) for helping us prepare petrographic thin sections. Thanks to Marco Helenio de Paula Alves Coelho, Celma Menezes and Sergio Bergamashi (UERJ), and Hilton Costi (MPEG) for helping to prepare SEM images. Many thanks to Ismar Carvalho, Leonardo Borghi and Luis Fernando Da Silva from the Federal University of Rio de Janeiro (UFRJ) for access to the Laboratory of Sedimentary Geology to use the petrographic microscope. Special thanks to Milene Freites Figueiredo and Christiano Ng from the CENPES-PETROBRAS for the incentive to the Pirabas Formation researches. Special thanks to Claudio Di Celma from the Camerino University and Alberto Collareta from the Pisa University for their revision of the final version of the paper and their useful and constructive suggestions. Thanks to Prof. Brian Jones, Editor of Sedimentary Geology and Sunoj Sankaran, Journal Manager for evaluated the manuscript. This study was funded by the Brazilian Council of Science and Technological Development - CNPq (grant 404937/2018-7 and productivity fellowships 305269/2017-8 to OA; grant 302676/2019-8 to MVM; 309481/2016-3 to RL), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) (grant PBMAC-UFF, finance code 001 to KB and DL), Postgraduate Program in Marine Biology and Coastal Ecosystem (PBMAC-UFF internal grant), Research Support Foundation of the State of Rio de Janeiro-FAPERJ (grand 202.927/2019 to MVM).	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Geol.	SEP	2020	407								105739	10.1016/j.sedgeo.2020.105739	http://dx.doi.org/10.1016/j.sedgeo.2020.105739			28	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NM5WD					2023-06-23	WOS:000568166300006
J	Almeida, LC; da Silva, JB; dos Santos, IF; de Carvalho, VS; Santos, AD; Hadlich, GM; Ferreira, SLC				Almeida, Lucas Cintra; da Silva Junior, Jucelino Balbino; dos Santos, Ivanice Ferreira; de Carvalho, Vanessa Sales; Santos, Adilson de Santana; Hadlich, Gisele Mara; Costa Ferreira, Sergio Luis			Assessment of toxicity of metals in river sediments for human supply: Distribution, evaluation of pollution and sources identification	MARINE POLLUTION BULLETIN			English	Article						Metals; Sediment; Environmental risk assessment; Temporary distribution; Joanes River	HEAVY-METALS; SURFACE SEDIMENTS; CONTAMINATION; BIOAVAILABILITY; MANGROVE; RISK; BAY; BIOACCUMULATION; POPULATION; UCIDIDAE	Ten surface sediments collected from Joanes River, Bahia, Brazil in rainy and drought periods in 2019 were evaluated according to the enrichment factor (EF), potential ecological risk index (RI), potential contamination index (PCI), pollution load index (PLI), and index of geoaccumulation (I-geo). Initially the dry sediment was subjected to granulometric analysis and determination of the concentration of organic matter. Then, the samples were digested in HNO3 and analyzed by Inductively Coupled Plasma Optical Emission Spectrometry (ICP OES) to determine the metals cadmium (Cd), copper (Cu), chromium (Cr), nickel (Ni), lead (Pb) and zinc (Zn). Zn and Cu were classified in that order as the most contaminated elements in most sediment. Comparison of the total metal concentrations with the threshold (TELs) and probable (PELs) effect levels in sediment quality guidelines sug- gested a more worrisome situation for Zn (648.83-1415.90 mu g g(-1); PELZn = 315 mu g g(-1)), of which con- centrations were occasionally associated with adverse biological effects in four sediments, followed by Cu in five sediments during dry and rainy periods; while adverse effects were rarely associated with Cd, Cr, Ni, and Pb. In another evaluation, Cd, Cu, Cr, and Zn could be considered the most dangerous in the entire river, as they were classified in the high levels of contamination by the PCI, associated with serious adverse effects in most samples. In an assessment regarding the ecological risks in the study environment, the sediment samples remained below the limit established by the risk index (IR). The Zn presented moderately severe enrichment (6.78-11.83) in all the collection stations in the dry and rainy periods, followed by the Cd that presented moderate enrichment (2.23-4.17), whose values exceeded almost 1000 times the background at one site. Through the PCA it was possible to evidence the existing correlation between metals, organic matter, and silt and clay fraction. The results obtained in the PCA represented more than 80% of the variance between the data. The environmental risk assessment revealed a significant increase in the risk associated with metals during the rainy season. This is probably due to the greater supply of organic matter from the leaching of the margins.	[Almeida, Lucas Cintra; de Carvalho, Vanessa Sales; Santos, Adilson de Santana; Costa Ferreira, Sergio Luis] Fed Univ Bahia UFBA, Chem Inst, Postgrad Program Chem, St Barao de Jeremoabo S-N, BR-40170270 Salvador, BA, Brazil; [da Silva Junior, Jucelino Balbino; Hadlich, Gisele Mara] Fed Univ Bahia UFBA, Geosci Inst, Postgrad Program Geochem Petr & Environm POSPETRO, St Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil; [dos Santos, Ivanice Ferreira] Univ Estadual Feira Santana UEFS, BR-44036900 Feira De Santana, BA, Brazil	Universidade Estadual de Feira de Santana	da Silva, JB (autor correspondente), Fed Univ Bahia UFBA, Geosci Inst, Postgrad Program Geochem Petr & Environm POSPETRO, St Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil.	jucejr@ufba.br	da Silva, Jucelino Balbino/AAA-3611-2021; Hadlich, Gisele/AAO-4708-2020	dos Santos, Ivanice/0000-0002-0390-2005; Hadlich, Gisele Mara/0000-0002-6304-0988	CAPES (Brazil) [001]; CAPES [PNPD 2311/2011]	CAPES (Brazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work was developed in the Postgraduate Program in Geochemistry: Oil and Environment from the Federal University of Bahia (UFBA), supported by CAPES (Brazil) -financial code 001. Silva Junior would like to thank CAPES for the postdoctoral fellowship (PNPD 2311/2011). The study was developed in partnership with the LEPETRO of the Geosciences Institute of the Federal University of Bahia (IGEO/UFBA).	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SEP	2020	158								111423	10.1016/j.marpolbul.2020.111423	http://dx.doi.org/10.1016/j.marpolbul.2020.111423			12	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	MU2JQ	32753207				2023-06-23	WOS:000555500000062
J	Bouougri, E; Lahna, AA; Tassinari, CCG; Basei, MAS; Youbi, N; Admou, H; Saquaque, A; Boumehdi, MA; Maacha, L				Bouougri, El Hafid; Lahna, Abdelhak Ait; Tassinari, Colombo C. G.; Basei, Miguel A. S.; Youbi, Nasrrddine; Admou, Hassan; Saquaque, Ali; Boumehdi, Moulay Ahmed; Maacha, Lhou			Time constraints on Early Tonian Rifting and Cryogenian Arc terrane-continent convergence along the northern margin of the West African craton: Insights from SHRIMP and LA-ICP-MS zircon geochronology in the Pan-African Anti-Atlas belt (Morocco)	GONDWANA RESEARCH			English	Article						Anti Atlas belt; Zircon U/Pb dating; Early Tonian Rifting; Cryogenian foreland basin; West African Craton; Rodinia breakup; Gondwana assembly	U-PB GEOCHRONOLOGY; BAS DRAA INLIER; PASSIVE MARGIN; LITHOSTRATIGRAPHIC FRAMEWORK; SOUTHEASTERN MARGIN; TECTONIC EVOLUTION; SEDIMENTARY-ROCKS; GRANITE GNEISS; SAO-FRANCISCO; YANGTZE BLOCK	The Neoproterozoic Anti-Atlas belt (Morocco) is a key segment in tracing the history of the northern margin of the West African craton (WAC) from Rodinia breakup to Gondwana assembly. In order to constrain geodynamic events related to rifting and convergence and their stratigraphic records, a radiometric study was carried out on the volcano-sedimentary Tachdamt and Bleida Formations. The volcaniclastic deposits of Tachdamt Fm. yield an age of ca. 883 Ma and provide a new constraint for the timing of the subaqueous volcanic eruption and the initiation of rifting in the Anti-Atlas. This age is similar to 100 my older than the previous age of 788 +/- 10 Ma obtained from Rb/Sr isotope dating (Clauer, 1976). Available zircon data from the interbedded clastic deposits from Tachdamt Fm. indicate major shifts in provenance during the rifting with sediments sourced from the WAC and a nearby Grenvillian terrane. Detrital zircon ages from metasiltstones of Bleida Fm. set a maximum depositional age at ca. 700 Ma. The age spectra discloses a major shift in sediment input with provenance from the WAC, Grenvillian terrane and an arc-related terrane (ca. 770-700 Ma) lying along the Anti-Atlas margin. The newly obtained results combined with existing radiometric data allowed the refinement of the stratigraphic and geotectonic framework of the pre-Pan-African strata in the WAC. The Early Tonian syn-rift volcanism has much in common with similar events in other cratons and provides a stratigraphic record for incipient Rodinia breakup. The overlying Bleida Fm. deposited in a peripheral foreland basin chronicles the Cryogenian arrival of the ca. 770-700 Ma Bou Azzer-Siroua arc-related terrane at the Anti-Atlas margin, and correlates with initial accretion in West Gondwana. The new results indicate that the Grenvillian detrital input in the Anti-Atlas during both geodynamic stages points toward a possible Mesoproterozoic terrane existing along the western margin of the WAC. (C) 2020 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.	[Bouougri, El Hafid; Lahna, Abdelhak Ait; Youbi, Nasrrddine; Admou, Hassan; Boumehdi, Moulay Ahmed] Cadi Ayyad Univ, Fac Sci Semlalia, Dept Geol, 3GEOLAB, Marrakech 40000, Morocco; [Tassinari, Colombo C. G.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508900 Sao Paulo, SP, Brazil; [Basei, Miguel A. S.] Univ Sao Paulo, Ctr Pesquisas Geocronol CPGeo, Inst Geociencias, Cidade Univ,Rua Lago 562, BR-05508080 Sao Paulo, Brazil; [Youbi, Nasrrddine; Boumehdi, Moulay Ahmed] Univ Lisbon, Fac Ciencias, Inst Dom Luiz, P-1749016 Lisbon 14, Portugal; [Saquaque, Ali; Maacha, Lhou] MANAGEM, Twin Ctr, BP 5199, Casablanca 20100, Morocco	Cadi Ayyad University of Marrakech; Universidade de Sao Paulo; Universidade de Sao Paulo; Universidade de Lisboa	Bouougri, E (autor correspondente), Cadi Ayyad Univ, Fac Sci Semlalia, Dept Geol, 3GEOLAB, Marrakech 40000, Morocco.	bouougri@uca.ma; ccgtassi@usp.br; baseimas@usp.br; youbi@uca.ma; admou@uca.ma; boumehdi@uca.ma; l.maacha@managemgroup.com	Basei, Miguel A S/C-1915-2013; Youbi, Nasrrddine/P-6226-2019	Basei, Miguel A S/0000-0002-3857-7089; Youbi, Nasrrddine/0000-0003-3466-2400; Ait lahna, Abdelhak/0000-0002-3366-3412; Boumehdi, Moulay Ahmed/0000-0001-5084-1551	Department of Geology-FSSM; Hassan II Academy of Science and Technology [HIIAST/SDU/2016.02]	Department of Geology-FSSM; Hassan II Academy of Science and Technology	The geochronological study was conducted under the scientific and technical agreement between the Sao Paulo University and the Cadi Ayyad University. The authors acknowledge the staffs of the Centro de Pesquisas Geocronologicas (CPGeo), Instituto de Geociencias (IG), Universidade de Sao Paulo-USP, Sao Paulo (SP), Brazil, for all supports provided to A. Ait Lahna. Special thanks to P. Eriksson who improved greatly the first draft of this manuscript. We thank the Department of Geology-FSSM for logistical and funding supports, O. Chourfi for thin sections preparation, and Managem for logistical support in the field. We acknowledge funding support from Hassan II Academy of Science and Technology (HIIAST/SDU/2016.02), and the funding studentship 2016-2018 awarded to AAL. We thank the reviewers (K. Hefferan and MF. Pereira) for their constructive reviews that improved this manuscript, and also the Associate Editor J. Meert for his prompt editing of this manuscript.	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J	Martins-Ferreira, MAC; Dias, ANC; Chemale, F; Campos, JEG				Cacador Martins-Ferreira, Marco Antonio; Coelho Dias, Airton Natanael; Chemale, Farid, Jr.; Guimaraes Campos, Jose Eloi			Intracontinental uplift of the Brazilian Central Plateau linked to continental breakup, orogenies, and basin filling, supported by apatite and zircon fission-track data	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Brazilian Central Plateau; Zircon fission track; Apatite fission track; Thermochronology; Intracratonic uplift	SAO FRANCISCO CRATON; U-PB; LANDSCAPE EVOLUTION; COLORADO PLATEAU; PARANA BASIN; GEOCHRONOLOGY; THERMOCHRONOLOGY; SEDIMENTATION; PROVENANCE; EXHUMATION	Fission-track analysis in zircon and apatite detrital grains from Mesoproterozoic sedimentary sequences show evidence of cooling episodes in central Brazil from Neoproterozoic to Cenozoic. Apatite fission-track ages reveal a main cooling episode during the Late Cretaceous-Early Paleogene, providing important clues on cooling by uplift and denudation during drifting of South America and Africa. Zircon data also suggest 3 distinct cooling events: (i) a Neoproterozoic-Cambrian event, probably related to orogenic exhumation of the Brasilia Belt and the thermal decay of West Gondwana assembly, (ii) a Devonian-Carboniferous event, probably related to the Late Famatinian orogeny and early stages of the Gondwanide orogeny, and (iii) an Early Permian to Triassic event, linked to the Late Gondwanide orogeny. These results indicate that the processes of assembly and breakup of supercontinents might significantly affect the plate interior, especially along with ancient orogenic belts. Zircon data has shown evidence of thermal decay during and after the West Gondwana assembly. Apatite data, on the other hand, has shown evidence of thermal decay during and after the breakup of Pangaea. The processes of assembly as well as the breakup of supercontinents can be tracked in the intracratonic setting, especially along with ancient orogenic belts. These assumptions take us back to the old concept of "mobile belts" as old orogenic regions that represent weak portions of the continental crust, assumed to have a greater tendency for mobility when solicited. In this case, the Brasilia Belt has shown to present great vertical mobility, accommodating tectonic far-field forces by uplift and as a result, feeding the Phanerozoic basins around it.	[Cacador Martins-Ferreira, Marco Antonio] Univ Fed Goias, Fac Ciencias & Tecnol, BR-74968755 Ap De Goiania, Go, Brazil; [Coelho Dias, Airton Natanael] Univ Fed Sao Carlos, Dept Fis Quim & Matemat, BR-18052780 Sorocaba, SP, Brazil; [Chemale, Farid, Jr.] Univ Vale Rio dos Sinos, Programa Posgrad Geol, BR-93022000 Sao Leopoldo, RS, Brazil; [Guimaraes Campos, Jose Eloi] Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil	Universidade Federal de Goias; Universidade Federal de Sao Carlos; Universidade do Vale do Rio dos Sinos (Unisinos); Universidade de Brasilia	Martins-Ferreira, MAC (autor correspondente), Univ Fed Goias, Fac Ciencias & Tecnol, BR-74968755 Ap De Goiania, Go, Brazil.	martinsmarco@gmail.com	Campos, Eloi/AAK-8599-2021; Cacador Martins-Ferreira, Marco Antonio/I-2983-2017	Chemale Junior, Farid/0000-0001-5003-5824; Cacador Martins-Ferreira, Marco Antonio/0000-0002-7212-8367	Brazilian foundation FAPESP (Sao Paulo Research Foundation) [2014/13792-5]	Brazilian foundation FAPESP (Sao Paulo Research Foundation)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	This research was financed by the Brazilian foundation FAPESP (Sao Paulo Research Foundation, grant #2014/13792-5).	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J. Geosci.	SEP 1	2020	13	17							891	10.1007/s12517-020-05885-8	http://dx.doi.org/10.1007/s12517-020-05885-8			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NN6CV					2023-06-23	WOS:000568875100004
J	Martins-Ferreira, MAC; Dias, ANC; Chemale, F; Campos, JEG; Seraine, M; Novais-Rodrigues, E				Cacador Martins-Ferreira, Marco Antonio; Coelho Dias, Airton Natanael; Chemale Jr, Farid; Guimaraes Campos, Jose Eloi; Seraine, Marina; Novais-Rodrigues, Eduardo			Multi-stage crustal accretion by magmatic flare-up and quiescence intervals in the western margin of the Sao Francisco Craton: U-Pb-Hf and geochemical constraints from the Almas Terrane	GONDWANA RESEARCH			English	Article						Accretionary orogeny; Almas Terrane; Sao Francisco-Congo Craton; Flare-up; Sao Francisco Paleocontinent	NORTH CHINA CRATON; CRIXAS GREENSTONE-BELT; CENTRAL BRAZIL; BRASILIA BELT; TOCANTINS PROVINCE; TECTONIC EVOLUTION; MINEIRO BELT; SM-ND; GA; ROCKS	The global plate tectonic regime in early Paleoproterozoic times is highly debated. The interval 2.45-2.2 Ga is known for a minima in juvenile magmatism, but this is not a global phenomenon. New results of whole-rock geochemistry and U-Pb-Hf analysis in igneous and detrital zircons, allied with existing isotopic and geophysical data, allow to identify and constrain the duration of magmatic flare-up and quiescence events in the western Sao Francisco Paleoplate. Igneous samples yield ages indicating three accretionary magmatic events, an older with ages ca. 2476.4 +/- 9 Ma to 2462 +/- 13 Ma, an intermediate at 2390 +/- 14 Ma, and a younger from 2235 +/- 26 Ma to 2201 +/- 5 Ma, all presenting magmatic arc geochemical signatures. Xenoliths of quartzite and volcanic tuff from the upper greenstone sequence (Morro do Carneiro Fm.) are hosted in the 2211 +/- 9 Ma tonalite and the maximum depositional age of the Morro do Carneiro basin is dated 2234 +/- 12 Ma, indicating a synorogenic setting for this basin. Detrital zircon U-Pb age distribution for quartzites of the greenstone sequence shows peaks at 2.65, 2.47, 2.39, 2.27 and 2.23 Ga. Altogether, the studied rocks record an accretionary orogeny with four distinct episodes: Episode S1: 2.52-2.46 Ga, epsilon Hf(t) values from +0.57 to +6.36; Episode S2: 2.43-2.37 Ga, epsilon Hf(t) values from +0.10 to +4.30; Episode R1: 2.32-2.26 Ga, epsilon Hf(t) values from +1.61 to -7.23 (from detrital zircons); Episode R2: 2.24-2.20 Ga, epsilon Hf(t) values from +0.39 to -2.73. These early Paleoproterozoic accretionary orogenies mark the onset of amalgamation of the Sao Francisco continental paleoplate that surrounds the craton, with accretions of an exoticmicro-block and continental magmatic arcs, indicating evolution from dominant Siderian juvenile magmatism to Rhyacian crustal magmatism. These patterns show striking similarities to the orogenies in the Mineiro Belt and North China Craton. (C) 2020 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.	[Cacador Martins-Ferreira, Marco Antonio] Univ Fed Goias, Fac Ciencias & Tecnol, Setor Conde Arcos, BR-74968755 Aparecida De Goiania, Go, Brazil; [Coelho Dias, Airton Natanael] Univ Fed Sao Carlos, Dept Fis Quim & Matemat, Campus Sorocaba, BR-18052780 Sorocaba, SP, Brazil; [Chemale Jr, Farid] Univ Vale Rio dos Sinos, Programa Posgrad Geol, BR-93022000 Sao Leopoldo, RS, Brazil; [Guimaraes Campos, Jose Eloi; Seraine, Marina; Novais-Rodrigues, Eduardo] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil	Universidade Federal de Goias; Universidade Federal de Sao Carlos; Universidade do Vale do Rio dos Sinos (Unisinos); Universidade de Brasilia	Martins-Ferreira, MAC (autor correspondente), Univ Fed Goias, Fac Ciencias & Tecnol, Setor Conde Arcos, BR-74968755 Aparecida De Goiania, Go, Brazil.	martinsmarco@gmail.com	Campos, Eloi/AAK-8599-2021; Cacador Martins-Ferreira, Marco Antonio/I-2983-2017	Cacador Martins-Ferreira, Marco Antonio/0000-0002-7212-8367; Chemale Junior, Farid/0000-0001-5003-5824	Sao Paulo Research Foundation -FAPESP [2017/12208-6]; National Council for Scientific and Technological Development-CNPq [305053/2014-0]	Sao Paulo Research Foundation -FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Council for Scientific and Technological Development-CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are grateful to the Federal University of Goias (UFG), the Federal University of Sao Carlos (UFSCar) and the University of Brasilia (UnB) for the laboratory and fieldwork support. This research was financed by Sao Paulo Research Foundation -FAPESP (grant #2017/12208-6) and National Council for Scientific and Technological Development-CNPq (grant #305053/2014-0).	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SEP	2020	85						32	54		10.1016/j.gr.2020.04.005	http://dx.doi.org/10.1016/j.gr.2020.04.005			23	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MH4MH					2023-06-23	WOS:000546704800003
J	Calca, CP; Fairchild, TR				Calca, Cleber Pereira; Fairchild, Thomas R.			A WIDESPREAD, NEARLY MONOSPECIFIC SILICIFIED COCCOIDAL MICROBIOTA FROM THE PERMIAN OF BRAZIL (ASSISTENCIA FORMATION, IRATI SUBGROUP, PARANA BASIN)	AMEGHINIANA			English	Article						Fossil Cyanobacteria; Assistencia Formation (Irati Subgroup); Chert; Parana Basin; Gloeodiniopsis lamellosa; Cyanosarcinopsis hachiroi; Coniunctiophycus sp.	ORGANIC-WALLED MICROFOSSILS; SUKHAYA TUNGUSKA FORMATION; SOUTHERN URAL MOUNTAINS; BLUE-GREEN-ALGAE; GREAT-SALT-LAKE; TURUKHANSK UPLIFT; BENTHIC CYANOBACTERIA; DRAKEN CONGLOMERATE; SALINITY GRADIENT; BELCHER ISLANDS	Well-preserved fossil microbiotas normally present relatively high taxonomic diversity, especially if the host-rock is distributed over a large area. Estimates of taxonomic diversity, however, require proper consideration of ontogenetic, taphonomic, and ecological influences on morphological variety. Otherwise, diversity may be overestimated. Chert in the Permian Assistencia Formation (Irati Subgroup, Parana Basin, Brazil) contains an abundant, well-preserved fossil microbiota that has been studied from seven localities distributed over about 500 km. Despite the great numbers of microfossils present, morphological analysis revealed a low apparent diversity. There is no evidence of filamentous microorganisms and the chroococcacean Gloeodiniopsis lamellosa is overwhelmingly dominant, accounting for 98.6% of counted individuals. In addition to G. lamellosa, only five taxa are recognized of which four are formally described: the chroococcaceans Cyanosarcinopsis hachiroi gen. et sp. nov. and cf. Coniunctiophycus sp. and two taxa considered incertae sedis: Myxococcoides sp. A (a probable cyanobacterium) and Myxococcoides sp. B (a possible delicate eukaryote). A unique but markedly different colony was designated as unnamed form (open nomenclature). Two hypotheses may explain the enigmatic absence of filaments: (i) environmental stress associated with hypersaline conditions that severely limited diversity or (ii) long-term optimal growth conditions for coccoidal cyanobacterial blooms due to sustained basin-wide eutrophic conditions.	[Calca, Cleber Pereira] Univ Fed Uberlandia, Inst Geog, Rodovia LMG 746,Km 1, BR-38500000 Monte Carmelo, Brazil; [Calca, Cleber Pereira; Fairchild, Thomas R.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, Brazil	Universidade Federal de Uberlandia; Universidade de Sao Paulo	Calca, CP (autor correspondente), Univ Fed Uberlandia, Inst Geog, Rodovia LMG 746,Km 1, BR-38500000 Monte Carmelo, Brazil.; Calca, CP (autor correspondente), Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, Brazil.	clebercalca@gmail.com; trfairch@hotmail.com	Fairchild, Thomas Rich/AAE-1835-2021		FAPESP (Fundacao de Amparo a Pesquisa de Sao Paulo); CAPES (Coordenadoria de Apoio ao Aperfeicoamento de Professores do Ensino Superior, Brazil)	FAPESP (Fundacao de Amparo a Pesquisa de Sao Paulo)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES (Coordenadoria de Apoio ao Aperfeicoamento de Professores do Ensino Superior, Brazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This paper resulted from research carried out as part of the requirement for the first author's doctorate obtained at the Instituto de Geociencias, Universidade de Sao Paulo (IGc-USP), Sao Paulo. We thank FAPESP (Fundacao de Amparo a Pesquisa de Sao Paulo) and CAPES (Coordenadoria de Apoio ao Aperfeicoamento de Professores do Ensino Superior, Brazil) for financial support for field and laboratory work and a scholarship (FAPESP) to CPC; the IGc-USP for research facilities and infrastructure necessary to complete this project; Jorge Hachiro (IGc-USP) for helpful discussions and assistance in the field; Paulo Alves de Souza (Universidade Federal do Rio Grande do Sul), Vladimir N. Sergeev (Geological Institute, Russian Academy of Sciences, Moscow), and Paula Cookie Nishimura (Instituto de Biologia-USP) for useful comments. We also thank the reviewers for their helpful criticism.	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J	Cubo, J; Sena, MVA; Aubier, P; Houee, G; Claisse, P; Faure-Brac, MG; Allain, R; Andrade, RCLP; Sayao, JM; Oliveira, GR				Cubo, Jorge; Sena, Mariana V. A.; Aubier, Paul; Houee, Guillaume; Claisse, Penelope; Faure-Brac, Mathieu G.; Allain, Ronan; Andrade, Rafael C. L. P.; Sayao, Juliana M.; Oliveira, Gustavo R.			Were Notosuchia (Pseudosuchia: Crocodylomorpha) warm-blooded? A palaeohistological analysis suggests ectothermy	BIOLOGICAL JOURNAL OF THE LINNEAN SOCIETY			English	Article						bone histology; ectothermy; endothermy; Metasuchia; Neosuchia; phylogenetic eigenvector maps; thermometabolism	RESTING METABOLIC-RATE; BONE-GROWTH RATE; BAURU BASIN; MARILIASUCHUS-AMARALI; MESOEUCROCODYLIA; EVOLUTION; CROCODYLIFORMES; MICROANATOMY; TEMPERATURE; HISTOLOGY	Most Notosuchia were active terrestrial predators. A few were semi-aquatic, or were insectivorous, omnivorous or herbivorous. A question relative to their thermometabolism remains to be answered: were Notosuchia warm-blooded? Here we use quantitative bone palaeohistology to answer this question. Two variables were used as proxies to infer thermometabolism: resting metabolic rate and red blood cell dimensions. Resting metabolic rate was inferred using relative primary osteon area and osteocyte size, shape and density. Blood cell dimensions were inferred using harmonic mean canal diameter and minimum canal diameter. All inferences were performed using phylogenetic eigenvector maps. Both sets of analyses suggest that the seven species of Notosuchia sampled in this study were ectotherms. Given that extant Neosuchia (their sister group) are also ectotherms, and that archosaurs were primitively endotherms, parsimony suggests that endothermy may have been lost at the node Metasuchia (Notosuchia-Neosuchia) by the Early Jurassic. Semi-aquatic taxa such as Pepesuchus may have had thermoregulatory strategies similar to those of recent crocodylians, whereas the terrestrial taxa (Araripesuchus, Armadillosuchus, Iberosuchus, Mariliasuchus, Stratiotosuchus) may have been thermoregulators similar to active predatory varanids. Thermal inertia may have contributed to maintaining a stable temperature in large notosuchians such as Baurusuchus.	[Cubo, Jorge; Aubier, Paul; Houee, Guillaume; Claisse, Penelope; Faure-Brac, Mathieu G.; Allain, Ronan] Sorbonne Univ, Museum Natl Hist Nat, CNRS, Ctr Rech Paleontol Paris,CR2P,UMR 7207, Paris, France; [Sena, Mariana V. A.] Univ Fed Pernambuco, Dept Geol, Programa Posgrad Geociencias PPGEOC, Recife, PE, Brazil; [Sena, Mariana V. A.] Ctr Univ Vitoria de Santo Antao, Vitoria De Santo Antao, PE, Brazil; [Andrade, Rafael C. L. P.; Sayao, Juliana M.] Univ Fed Pernambuco, Lab Paleobiol & Microestruturas, Vitoria De Santo Antao, PE, Brazil; [Oliveira, Gustavo R.] Univ Fed Rural Pernambuco, Dept Biol, Lab Paleontol & Sistemat, Recife, PE, Brazil	Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Museum National d'Histoire Naturelle (MNHN); UDICE-French Research Universities; Sorbonne Universite; Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal Rural de Pernambuco (UFRPE)	Cubo, J (autor correspondente), Sorbonne Univ, Museum Natl Hist Nat, CNRS, Ctr Rech Paleontol Paris,CR2P,UMR 7207, Paris, France.	jorge.cubo_garcia@upmc.fr	CUBO, Jorge/I-8498-2016; Sena, Mariana V A/K-9347-2018; Oliveira, Gustavo R/F-7432-2012; ALLAIN, Ronan/AAX-5801-2021; Sena, Mariana/AAC-4283-2020; Oliveira, Gustavo/IQW-7983-2023	CUBO, Jorge/0000-0002-8160-779X; Sena, Mariana V A/0000-0003-4708-999X; Oliveira, Gustavo R/0000-0002-9871-1235; Sena, Mariana/0000-0003-4708-999X; Faure-Brac, Mathieu/0000-0003-1099-6000; Claisse, Penelope/0000-0001-6932-2938				BUFFETAUT E, 1977, CR ACAD SCI D NAT, V284, P1663; Busbey A.B. 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J. Linnean Soc.	SEP	2020	131	1					154	162		10.1093/biolinnean/blaa081	http://dx.doi.org/10.1093/biolinnean/blaa081			9	Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Evolutionary Biology	OF1NN		Green Submitted			2023-06-23	WOS:000580983800012
J	de Santana, JR; Costa, AESF; Neumann-Leitao, S; Mafalda, PD; Veleda, D; Schwamborn, SHL				de Santana, Jana Ribeiro; Costa, Alejandro E. S. F.; Neumann-Leitao, Sigrid; Mafalda Jr, Paulo de O.; Veleda, Doris; Schwamborn, Silvia H. L.			Spatial variability of the ichthyoneuston around oceanic islands at the tropical Atlantic	JOURNAL OF SEA RESEARCH			English	Article						Fish early life stages; Fish larvae; Island mass effect	FERNANDO-DE-NORONHA; LARVAL FISH ASSEMBLAGES; SAINT-PAUL-ARCHIPELAGO; REEF FISH; ROCAS ATOLL; NEUSTONIC ICHTHYOPLANKTON; VERTICAL DISTRIBUTIONS; COMMUNITY STRUCTURE; WESTERN ATLANTIC; FEEDING ECOLOGY	Oceanic tropical waters are characteristically oligotrophic. However, current-topography interaction around oceanic islands promotes bio-physical processes, which may enrich surface waters. The ichthyoneuston assemblage at three areas around oceanic islands in the tropical Atlantic was investigated. The aim was to evaluate if the ichthyoneuston was influenced by physical oceanographic processes, such as possible mechanisms of plankton retention promoted by the presence of the islands. Samplings were performed by 20 min long diurnal and nocturnal 500-mu m plankton net hauls using a David-Hempel Catamaran at two transections in each area (Saint Peter and Saint Paul's archipelago, Fernando de Noronha archipelago, and Rocas Atoll). The transections were composed by three stations and were located at opposite sides of the archipelagos (windward and leeward sides of the archipelago). A total of 131 larvae and 3027 eggs, belonging to 16 families and 28 species were collected. Higher densities of eggs were found at the leeward side, which indicates the occurrence of a retention mechanism or spawning at this side. Higher densities of larvae were found at Fernando de Noronha, especially during the nocturnal period. Only one species, Ceratoscopelus warmingii, co-occurred at the three islands. Fernando de Noronha was highlighted as the area with the higher density, abundance and species richness. The waters around this island were positively correlated with chlorophyll -a, which indicates a higher availability of food items and stimulates the selection of this area as a favorable spot for reproduction and early nursery zone. This work highlighted the importance of the relation between abiotic factors and the distribution of fish eggs and larvae inhabiting the neustonic layer around South Atlantic oceanic islands, showing that favorable conditions, e.g. higher phytoplanktonic biomass, may be of fundamental importance to the spawning by adult individuals.	[de Santana, Jana Ribeiro; Costa, Alejandro E. S. F.; Neumann-Leitao, Sigrid; Veleda, Doris] Univ Fed Pernambuco, Dept Oceanog, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Mafalda Jr, Paulo de O.] Univ Fed Bahia, Inst Biol, Rua Barao de Jeremoabo,668,Ondina, BR-40170115 Salvador, BA, Brazil; [Schwamborn, Silvia H. L.] Univ Fed Pernambuco, Ctr Acad Vitoria, Rua Alto Reservatorio S-N, BR-55608680 Vitoria De Santo Antao, PE, Brazil; [de Santana, Jana Ribeiro] Univ Estado Bahia, Dept Ciencias Humanas & Tecnol DCHT, Campus 24,Rua Prof Carlos Santos,601, BR-47400000 Xique Xique, BA, Brazil	Universidade Federal de Pernambuco; Universidade Federal da Bahia; Universidade Federal de Pernambuco; Universidade do Estado Bahia	de Santana, JR (autor correspondente), Univ Fed Pernambuco, Dept Oceanog, Ave Arquitetura S-N, BR-50740550 Recife, PE, Brazil.; de Santana, JR (autor correspondente), Univ Estado Bahia, Dept Ciencias Humanas & Tecnol DCHT, Campus 24,Rua Prof Carlos Santos,601, BR-47400000 Xique Xique, BA, Brazil.	jribeiro.pesca@gmail.com	Veleda, Doris/I-1673-2012; Júnior, Paulo Mafalda/AAC-7002-2021	Veleda, Doris/0000-0003-2103-5950; 	"Conselho Nacional de Desenvolvimento Cientifico e Tecnologico" (CNPq); CNPq/FABESB [565054/2010-4, 8936/2011]	"Conselho Nacional de Desenvolvimento Cientifico e Tecnologico" (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq/FABESB	This work is a contribution of the projects Camadas Finas I and II and was supported by the "Conselho Nacional de Desenvolvimento Cientifico e Tecnologico" (CNPq) through a master's degree scholarship offered to JRS. The authors thank the Brazilian Navy, to the crew and researchers aboard of the NHO Cruzeiro do Sul for the support during the field work, to the Brazilian "Ministerio da Ciencia e Tecnologia" (MCT), to the project INCT AmbTropic -National Institute on Science and Technology for Tropical Marine Environments, CNPq/FABESB (565054/2010-4 and 8936/2011), and to the Department of Oceanography of the Federal University of Pernambuco for the availability of the facilities to the development of the study.	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Sea Res.	SEP	2020	164								101928	10.1016/j.seares.2020.101928	http://dx.doi.org/10.1016/j.seares.2020.101928			14	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	NN4VB					2023-06-23	WOS:000568786800002
J	Dias, LC; Bahia, PVB; do Amaral, DN; Machado, ME				Dias, Luise Carvalho; Bomfim Bahia, Pedro Victor; do Amaral, Diego Nery; Machado, Maria Elisabete			Nitrogen compounds as molecular markers: An overview of analytical methodologies for its determination in crude oils and source rock extracts	MICROCHEMICAL JOURNAL			English	Review						Nitrogen markers; Petroleum; Sample preparation; Gas chromatography	2-DIMENSIONAL GAS-CHROMATOGRAPHY; AROMATIC HETEROCYCLE FRACTIONS; SOLID-PHASE EXTRACTION; PETROLEUM SOURCE ROCKS; ALPINE FORELAND BASIN; DEGREES F DISTILLATE; COAL-TAR PITCH; CARBAZOLE DISTRIBUTIONS; BENZOCARBAZOLE DISTRIBUTIONS; ORGANIC-COMPOUNDS	Nitrogen compounds (N-compounds) used as markers in crude oils and source rocks are mainly present as alkylated aromatic heterocycles with a predominance of neutral pyrrolic structures over basic pyridinic forms. This study describes the molecular markers employed, with an overview of sample preparation methods and gas chromatographic techniques used in qualitative and quantitative characterization of N-compounds. The advantages, disadvantages, and applications of rock extraction procedures, such as Soxhlet extraction and ultrasound-assisted extraction, as well as modern techniques, such as Soxtherm rapid automatic system and accelerated solvent extraction, were assessed. Furthermore, pre-fractionation techniques in reducing matrix suppression, such as open column chromatography, medium pressure liquid chromatography, and solid-phase extraction, were described. Subsequently, the procedures for N-compound chromatographic analysis using gas chromatography-mass spectrometry, gas chromatography nitrogen phosphorous detector, and comprehensive two-dimensional chromatography were addressed, highlighting the potential of their applications.	[Dias, Luise Carvalho; Bomfim Bahia, Pedro Victor; Machado, Maria Elisabete] Univ Fed Bahia, Inst Quim, Programa Posgrad Quim, BR-40170115 Salvador, BA, Brazil; [do Amaral, Diego Nery; Machado, Maria Elisabete] Univ Fed Bahia, Inst Geociencias, Programa Posgrad Petr & Meio Ambiente, BR-40170115 Salvador, BA, Brazil; [Machado, Maria Elisabete] Univ Fed Bahia, Inst Nacl Ciencia & Tecnol Energia & Ambiente, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia	Machado, ME (autor correspondente), Univ Fed Bahia, Inst Quim, Programa Posgrad Quim, BR-40170115 Salvador, BA, Brazil.; Machado, ME (autor correspondente), Univ Fed Bahia, Inst Geociencias, Programa Posgrad Petr & Meio Ambiente, BR-40170115 Salvador, BA, Brazil.; Machado, ME (autor correspondente), Univ Fed Bahia, Inst Nacl Ciencia & Tecnol Energia & Ambiente, BR-40170115 Salvador, BA, Brazil.	maria.elisabete@ufba.br	Machado, Maria Elisabete/E-7742-2013	Machado, Maria Elisabete/0000-0001-8289-4842	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - Brazil (CNPq); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES)	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - Brazil (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors gratefully acknowledge the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - Brazil (CNPq), and Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) for fellowships.	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SEP	2020	157								105039	10.1016/j.microc.2020.105039	http://dx.doi.org/10.1016/j.microc.2020.105039			12	Chemistry, Analytical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	NK5ET					2023-06-23	WOS:000566754900006
J	Guerrini, VB; Matos, SA; Rohn, R; Varejao, FG; Warren, LV; Simoes, MG				Guerrini, Vitor B.; Matos, Suzana A.; Rohn, Rosemarie; Varejao, Filipe G.; Warren, Lucas, V; Simoes, Marcello G.			The last chapter of 30 million years of molluscan evolution: Permian non-marine bivalves of the Rio do Rasto Formation, Parana Basin, Brazil	PALZ			English	Article						SW Gondwana; Late Permian; Non-marine bivalves; Palaeomutelidae; Pachydomidae Astartidae	SW GONDWANA PALEOGEOGRAPHY; SOURCE-TO-SINK; PALEOENVIRONMENTS; CLASSIFICATION; PALEOECOLOGY; SYSTEMATICS; ASSEMBLAGE; SOUTHERN	The last chapter of the evolutionary history of the Permian (Artinskian-Wuchiapingian) endemic bivalves of the Passa Dois Group, Brazil, is depicted. They evolved in a vast, isolated epeiric sea under progressive continentalization. Previously, bivalves that thrived during times of marked non-marine (limnic) conditions have been poorly investigated. Hence, a systematic survey of the bivalves between theLeinzia similisassemblage (Serrinha Member) and thePalaeomutela platinensisassemblage (Morro Pelado Member), Rio do Rasto Formation, is presented. Over two hundred specimens were examined, and three bivalve assemblages were identified: (a) theTerraia decarinataassemblage in the uppermost part of the Serrinha Member, includingRelogiincola delicatagen. et sp. nov.,Palaeomutela australissp. nov., andPalaeomutela platinensis(Reed,1935); (b) theTerraiacf.decarinataassemblage in the transition between the Serrinha and Morro Pelado members, includingT. decarinata, andP. platinensis, and (c) thePalaeomutela australisassemblage in the lowermost part of the Morro Pelado Member, also includingR. delicataandP. platinensis. The investigated bivalves were recorded above the last occurrences ofTerraia altissima(Holdhaus,1918) andCowperesia emeritaMendes,1952in the Serrinha Member. In the Gai-As Formation, Huab Basin, Namibia, these species are found in well-constrained Wordian-Capitanian strata, suggesting a Capitanian-Wuchiapingian age for the studied assemblages. The Permian cosmopolitan freshwater genusPalaeomutelaoccurs in all three assemblages and is also found in the lower Beaufort Group (South and Central Africa). Therefore, our record may represent the maximum paleobiogeographic expansion ofPalaeomutelain Western Gondwana.	[Guerrini, Vitor B.; Rohn, Rosemarie; Varejao, Filipe G.; Warren, Lucas, V] Univ Estadual Paulista, Inst Geociencias & Ciencias Exatas, Dept Geol Aplicada, Campus Rio Claro 178, BR-13506900 Rio Claro, SP, Brazil; [Guerrini, Vitor B.; Matos, Suzana A.; Simoes, Marcello G.] Univ Estadual Paulista, Inst Biociencias, Dept Zool, Dist Rubiao Jr 510, BR-18618970 Botucatu, SP, Brazil	Universidade Estadual Paulista; Universidade Estadual Paulista	Simoes, MG (autor correspondente), Univ Estadual Paulista, Inst Biociencias, Dept Zool, Dist Rubiao Jr 510, BR-18618970 Botucatu, SP, Brazil.	vbguerrini@gmail.com; sumatos.s@gmail.com; rohn@rc.unesp.br; filipe.varejao@hotmail.com; lucas.warren@unesp.br; profmgsimoes@gmail.com	Varejão, Filipe/J-3015-2015; Simoes, Marcello G/C-2373-2012; Varejão, Filipe/GYD-3727-2022; Guerrini, Vitor Bonatto/AAW-2483-2020; Varejão, Filipe Giovanini/O-1943-2019; Warren, Lucas/M-9051-2015	Varejão, Filipe/0000-0002-3776-9476; Varejão, Filipe/0000-0002-3776-9476; Varejão, Filipe Giovanini/0000-0002-3776-9476; Matos da Silva, Suzana/0000-0001-6328-8871; Simoes, Marcello/0000-0002-8706-3199; Warren, Lucas/0000-0002-2050-6514				Aberhan M, 2015, P NATL ACAD SCI USA, V112, P7207, DOI 10.1073/pnas.1422248112; Alessandretti L, 2017, J S AM EARTH SCI, V76, P218, DOI 10.1016/j.jsames.2017.03.003; Alessandretti L, 2016, J S AM EARTH SCI, V70, P368, DOI 10.1016/j.jsames.2016.06.007; Alessandretti L, 2015, SEDIMENT GEOL, V326, P1, DOI 10.1016/j.sedgeo.2015.06.007; Amalitsky W., 1895, Quarterly Journal of the Geological Society, Vli, P337; Amalizky W., 1892, Palaeontogr, Vxxxix, P125; Anelli L.E., 2010, GEOL USP C, V10, P13; [Anonymous], [No title captured]; Azevedo LS, 2018, BRAZ J GEOL, V48, P821, DOI 10.1590/2317-4889201820170129; Bailey Jack Bowman, 2011, Bulletins of American Paleontology, P1; BAMBACH RK, 1973, AM J SCI, VA273, P409; Beurlen K., 1954, PALEONTOLOGIA PARANA, P107; Bond G., 1946, Transactions of the Royal Society of South Africa, V31, P125; Bond G, 1954, GEOLOGICAL MAGAZINE, V3, P189; BRADSHAW M, 1984, ALCHERINGA, V8, P305, DOI 10.1080/03115518408618952; BRAND U, 1993, CARBONATE EVAPORITE, V8, P199, DOI 10.1007/BF03175178; BRETT C E, 1986, Palaios, V1, P207, DOI 10.2307/3514686; Carter Joseph G., 2011, Paleontological Contributions, P1; Cisneros Juan Carlos, 2005, Revista Brasileira de Paleontologia, V8, P13; COX L. 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M., 1997, LATE GLACIAL POSTGLA, P111	112	3	3	0	1	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	0031-0220	1867-6812		PALZ	PalZ	SEP	2020	94	3					487	512		10.1007/s12542-019-00455-0	http://dx.doi.org/10.1007/s12542-019-00455-0			26	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	NG8OL					2023-06-23	WOS:000564239300008
J	Lacerda, JV; Fuck, RA; Ruiz, AS; Dantas, EL; Rodrigues, JB; Scandolara, JE				Lacerda Filho, J. V.; Fuck, R. A.; Ruiz, A. S.; Dantas, E. L.; Rodrigues, J. B.; Scandolara, J. E.			Rio Apa Block: A Juvenile Crustal Fragment in the Southwest Amazonian Craton and Its Implications for Columbia Supercontinent Reconstitution	JOURNAL OF GEOLOGY			English	Article							PALEO-MESOPROTEROZOIC SUPERCONTINENT; AMOGUIJA MAGMATIC ARC; U-PB; GEOCHRONOLOGY; EVOLUTION; RODINIA; CONFIGURATION; GRANITE; BREAKUP; CONTINENTS	The Rio Apa Block, a crustal fragment of 20,000 km(2) in the southern portion of the Amazonian Craton, is a Paleoproterozoic terrain, making up the basement of the Neoproterozoic Paraguay Belt. The block is not often considered in the evolution models of the Columbia supercontinent. Different hypotheses of the evolution of the Rio Apa Block consider this segment as part of the Amazonian Craton, and its correlation with other Paleoproterozoic accretionary systems remains controversial. We present new U-Pb and Sm-Nd data that suggest that the Rio Apa Block constitutes a continental arc system built around 1.8-1.7 Ga that can be a correlation element in supercontinent models. Recorded orogenic accretionary events and continental crust reworking divide the block into three main sectors. The western and central sectors comprise parts of the 1.88-1.71 Ga Amoguija arc. The eastern sector consists of Orosirian high-K calc-alkaline and postcollisional A-type granites. The western segment comprises Orosirian banded orthogneisses of the Porto Murtinho Complex, intruded by initial phase granitoids of the Amoguija arc. The central sector is characterized by weakly to moderately deformed granites of the Amoguija Suite, Serra da Bocaina Formation metavolcanic rocks, Serra da Alegria gabbro-anorthosite suite, and Morro do Triunfo gabbro, overlain by the Amolar Group sedimentary rocks. The eastern segment comprises the backarc basin generated Alto Terere Group, intruded by late to postorogenic granites of the Rio Apa Complex, including A-type granites. Mafic dikes and sill swarms related to a late extensional event intrude the preceding rocks. Two important metamorphic-deformational events are recorded in the opening of the Rb-Sr system in biotite around 1670 Ma, followed by thrust deformation and metamorphism probably related to the ca. 1300 Ma Rondonian-San Ignacio event, as indicated by Ar-Ar muscovite and U-Pb monazite ages.	[Lacerda Filho, J. V.; Rodrigues, J. B.; Scandolara, J. E.] Serv Geol Brasil CPRM, Rua 148,485, BR-74170110 Goiania, Go, Brazil; [Fuck, R. A.; Dantas, E. L.] Univ Brasilia, BR-70910900 Brasilia, DF, Brazil; [Ruiz, A. S.] Univ Fed Mato Grosso, Ave Fernando Correa S-N, BR-78060900 Cuiaba, Mato Grosso, Brazil	Universidade de Brasilia; Universidade Federal de Mato Grosso	Lacerda, JV (autor correspondente), Serv Geol Brasil CPRM, Rua 148,485, BR-74170110 Goiania, Go, Brazil.	joffre.lacerda@cprm.gov.br	Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059	CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico); CNPq; CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) [Elton 308312/2014-7, 454272/2014-6]	CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	We would like to thank Brasilia University, Mato Grosso Federal University, and CPRM-Geological Survey of Brazil. We would also like to thank the technical support from the staff of the Geochronological Laboratory of Brasilia University. Instituto Nacional de Ciencia e Tecnologia de Estudos Geotectonicos (INCT-ET) is acknowledged for support; R. A. Fuck, A. S. Ruiz, and E. L. Dantas thank CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) for research fellowships; and we acknowledge grants CNPq and CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior), Elton 308312/2014-7 and 454272/2014-6.	American Geophysical Union, 2010, AM GEOPH UN M AM FOZ, P3; Araujo H.J.T., 1982, PROJETO RADAMBRASIL, V28, P23; Bassin C, 2000, EOS T AGU, V81, pF897; Bickford ME, 2015, PRECAMBRIAN RES, V265, P286, DOI 10.1016/j.precamres.2014.11.024; Bispo-Santos F, 2012, PRECAMBRIAN RES, V196, P1, DOI 10.1016/j.precamres.2011.10.022; Buhn B, 2009, AN ACAD BRAS CIENC, V81, P99, DOI 10.1590/S0001-37652009000100011; Campos G. 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L., 2011, MINERAL MAG, P2074; Vasconcelos PN, 2002, AN ACAD BRAS CIENC, V74, P297, DOI 10.1590/S0001-37652002000200008; Yakubchuk A, 2010, J GEODYN, V50, P166, DOI 10.1016/j.jog.2010.03.001; Zhang SH, 2012, EARTH PLANET SC LETT, V353, P145, DOI 10.1016/j.epsl.2012.07.034; Zhang SH, 2009, EARTH PLANET SC LETT, V288, P588, DOI 10.1016/j.epsl.2009.10.023; Zhao GC, 2002, EARTH-SCI REV, V59, P125, DOI 10.1016/S0012-8252(02)00073-9; Zhao GC, 2004, EARTH-SCI REV, V67, P91, DOI 10.1016/j.earscirev.2004.02.003	91	5	6	0	5	UNIV CHICAGO PRESS	CHICAGO	1427 E 60TH ST, CHICAGO, IL 60637-2954 USA	0022-1376	1537-5269		J GEOL	J. Geol.	SEP 1	2020	128	5					415	444		10.1086/710999	http://dx.doi.org/10.1086/710999		SEP 2020	30	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PA2PC					2023-06-23	WOS:000588004300001
J	Celestino, MAL; de Miranda, TS; Mariano, G; Alencar, MD; de Carvalho, BRBM; Falcao, TD; Topan, JG; Barbosa, JA; Gomes, IF				Lima Celestino, Maria Alcione; de Miranda, Tiago Siqueira; Mariano, Gorki; Alencar, Marcio de Lima; Barbosa Melo de Carvalho, Bruno Raphael; Falcao, Thiago da Cruz; Topan, Joao Gabriel; Barbosa, Jose Antonio; Gomes, Igor Fernandes			Fault damage zones width: Implications for the tectonic evolution of the northern border of the Araripe Basin, Brazil, NE Brazil	JOURNAL OF STRUCTURAL GEOLOGY			English	Article						Brittle deformation; Fault damage zone; Fault core; Strike-slip	DEFORMATION BANDS; POROUS SANDSTONES; STATISTICAL-ANALYSIS; FRACTURE ATTRIBUTES; PARNAIBA BASIN; PEIXE BASIN; FLUID-FLOW; SYSTEM; GROWTH; INTENSITY	Fault zones commonly have spatially variable fault rocks and brittle structures. Differing fault-rock attributes may retard or increase cross- and along-fault permeability. Our work analyzed brittle deformation of a segment of the Patos shear zone, Triunfo Fault, which is located in the northern border of the Araripe Basin, NE Brazil. We investigated the structural evolution and tectonic implications of the Triunfo Fault by mapping damage zone width patterns and the types and distributions of breccia and brittle structure arrays within the fault zone using scanline fracture analysis techniques and topographic and aeromagnetometric data. Fractured rocks of the damage zone mainly comprise: mylonitic orthogneiss (footwall); and sandstone and carbonate rocks (hanging-wall). The fault core is composed of tectonic breccia and cataclasites occurring as lenses, with calcite-filled veins. Due to fault sinuosity and rheology heterogeneities, the width of the damage zone ranges from 240 to 290m (footwall), and 372-610m (hangingwall). Our analysis obtained from the topographic and gravimetric data combined with field data indicate the following sequential deformation phases: a) Dn, Brasiliano Orogeny, dextral shear zone; b) Dn+1, Paleozoic time, brittle-ductile deformation; and c) Dn+2, Lower Cretaceous time, brittle deformation.	[Lima Celestino, Maria Alcione; Alencar, Marcio de Lima; Topan, Joao Gabriel] Univ Fed Pernambuco, Geosci Grad Program, BR-50740530 Recife, PE, Brazil; [de Miranda, Tiago Siqueira; Mariano, Gorki; Barbosa, Jose Antonio] Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil; [Barbosa Melo de Carvalho, Bruno Raphael; Falcao, Thiago da Cruz] Petrobras Res Ctr CENPES, BR-21941915 Rio De Janeiro, Brazil; [Gomes, Igor Fernandes] Univ Fed Pernambuco, Dept Civil Engn, BR-50740530 Recife, PE, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Petrobras; Universidade Federal de Pernambuco	de Miranda, TS (autor correspondente), Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil.; de Miranda, TS (autor correspondente), Av Arquitetura 953-995 Cidade Univ, BR-50740540 Recife, PE, Brazil.	alcionelimma22@gmail.com; tiago.smiranda@ufpe.br; marianogorki@gmail.com; mlimaalencar@gmail.com; brcarvalho@petrobras.com.br; tfalcao@petrobras.com.br; gabrieltopan@gmail.com; barboant@hotmail.com; gomes@ufpe.br	BARBOSA, JOSE ANTONIO/AAB-4437-2020; Gomes, Igor/AAX-7409-2020; Miranda, Tiago S/P-8113-2018; Mariano, Gorki/AAI-3547-2021	BARBOSA, JOSE ANTONIO/0000-0001-8754-6310; Gomes, Igor/0000-0003-2474-383X; Miranda, Tiago S/0000-0001-9099-1271; Mariano, Gorki/0000-0002-7861-0947	Project Pseudopocos - Petrobras/Federal University of Pernambuco (UFPE)	Project Pseudopocos - Petrobras/Federal University of Pernambuco (UFPE)	We warmly thank the Editor Stephen Laubach and the reviewers Fabrizio Balsamo, Sonja Philipp and the two anonymous reviewers for their helpful comments, which greatly improved the early version of this manuscript. This study was carried out with financial support provided Project Pseudopocos - Petrobras/Federal University of Pernambuco (UFPE). We are grateful to Petrobras, National Agency of Petroleum, Natural Gas and Biofuels of Brazil (ANP) and Department of Geology UFPE. We thank Gabriel Matos for the fieldwork and fruitful discussions and everyone who directly or indirectly contributed to the elaboration of this work. We also thank Nick Roberts for the helpful English review. This work is part of a MSc of Maria Alcione under the postgraduate program in Geosciences of the Federal University of Pernambuco (PPGEOC-UFPE) and represents the contribution N. 01 of the Laborat.orio de Modelagem de Bacias (ModLad-UFPE).	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Struct. Geol.	SEP	2020	138								104116	10.1016/j.jsg.2020.104116	http://dx.doi.org/10.1016/j.jsg.2020.104116			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NK5RB					2023-06-23	WOS:000566788800001
J	Oliveira, SS; Ribeiro, VS; Almeida, TS; Araujo, RGO				Oliveira, Sidimar S.; Ribeiro, Vaniele S.; Almeida, Tarcisio S.; Araujo, Rennan Geovanny O.			Quantification of ytterbium in road dust applying slurry sampling and detection by high-resolution continuum source graphite furnace atomic absorption spectrometry	SPECTROCHIMICA ACTA PART B-ATOMIC SPECTROSCOPY			English	Article; Proceedings Paper	15th Rio Symposium on Atomic Spectrometry	OCT 06-11, 2019	Mendoza, ARGENTINA			Ytterbium; Road dust; Permanent chemical modifier; Sample preparation; HR-CS-GFAAS	RARE-EARTH-ELEMENTS; PLASMA-MASS SPECTROMETRY; STREET DUST; SOURCE APPORTIONMENT; ANIMAL FECES; METALS; VAPORIZATION; OPTIMIZATION; STRATEGY; MERCURY	In this work, the determination of ytterbium in road dust samples, employing a simple and fast methodology, based on sample preparation as slurry and analysis by high resolution-continuum source graphite furnace atomic absorption spectrometry (HR-CS-GFAAS), is purposed. The determinations were carried out on the Yb main line, 398.799 nm, using an integration time of 5.0 s. The optimum condition for the slurry preparation of road dust samples was established through a Doehlert matrix for two variables, which employed a HNO3 concentration of 0.24 mol L-1 and homogenization time of 34 min, using ultrasonic bath. The temperatures applied to the graphite furnace were optimized, wherein the pyrolysis and atomization temperatures were 1200 degrees C and 2700 degrees C, respectively, using 250 mu g of W as permanent chemical modifier. To investigate possible matrix interferences in the determination of Yb in road dust samples, external calibration and standard addition curves were compared. The comparison between slopes of the external and standard addition calibration curves showed difference of about 7.0%, an indication of absence of matrix effects for determination of Yb in road dust samples. The limit of detection (LOD) and limit of quantification (LOQ) were 22 and 72 ng g(-1), respectively, with a characteristic mass of 6.0 pg. The accuracy was confirmed through analyses of three certified reference materials (CRM): Trace Elements in Soil Containing Lead From Paint (NIST 2586), Rock (NCS DC 73301) and Geochemical Soil (TILL-1), and the good agreement between the found and certified values was obtained, 99 +/- 4 to 104 +/- 2%, corroborating the accuracy of the analytical method. The precision was expressed as relative standard deviation (RSD) for measurements in triplicate, being lower than or equal to 10.0%. The analytical method was used for Yb determination in eight samples of dust collected in an urban area of Salvador and Jaguaquara, Bahia State, Northeast, Brazil. The concentrations obtained for Yb ranged from 172 +/- 13 to 2065 +/- 122 ng g(-1). Thus, the proposed analytical method presents the characteristics of being fast, precise and accurate for the determination of Yb in road dust samples, employing slurry sampling and detection by HR-CS-GFAAS.	[Oliveira, Sidimar S.; Ribeiro, Vaniele S.; Almeida, Tarcisio S.; Araujo, Rennan Geovanny O.] Univ Fed Bahia, Inst Quim, Dept Quim Analit, BR-40170115 Salvador, BA, Brazil; [Ribeiro, Vaniele S.] Inst Fed Educ Ciencia & Tecnol Baiano, Campus Guanambi, BR-46430000 Guanambi, BA, Brazil; [Almeida, Tarcisio S.] Univ Estadual Feira de Santana, Dept Ciencias Exatas, BR-44036900 Feira De Santana, BA, Brazil; [Araujo, Rennan Geovanny O.] Univ Fed Bahia, Inst Nacl Ciencia & Tecnol CNPq INCT Energia & Am, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Instituto Federal Baiano (IFBAIANO); Universidade Estadual de Feira de Santana; Universidade Federal da Bahia	Araujo, RGO (autor correspondente), Univ Fed Bahia UFBA, Inst Quim, Dept Quim Analit, Grp Pesquisa Estudos Quim Analit & Ambiental GPEQ, BR-40170115 Salvador, BA, Brazil.	rennan@ufba.br	Oliveira, Sidimar S/A-3547-2017; Silva de Almeida, Tarcisio/U-4368-2017	Oliveira, Sidimar S/0000-0002-7057-4136; Silva de Almeida, Tarcisio/0000-0003-1963-3775; OLIVEIRA ARAUJO, RENNAN GEOVANNY/0000-0001-6955-8115	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB, Salvador, Brazil); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brasilia, Brazil); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES, Brasilia, Brazil) [001]	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB, Salvador, Brazil)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brasilia, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES, Brasilia, Brazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors are grateful for the infrastructure, scholarships and financial resources for research provided by the Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB, Salvador, Brazil) and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brasilia, Brazil). This study was also financed in part by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES, Brasilia, Brazil) -Finance Code 001.	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Acta Pt. B-Atom. Spectr.	SEP	2020	171								105938	10.1016/j.sab.2020.105938	http://dx.doi.org/10.1016/j.sab.2020.105938			8	Spectroscopy	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Spectroscopy	NS3FA					2023-06-23	WOS:000572149900013
J	Ribeiro, BV; Lagoeiro, L; Faleiros, FM; Hunter, NJR; Queiroga, G; Raveggi, M; Cawood, PA; Finch, M; Campanha, GAC				Ribeiro, B., V; Lagoeiro, L.; Faleiros, F. M.; Hunter, N. J. R.; Queiroga, G.; Raveggi, M.; Cawood, P. A.; Finch, M.; Campanha, G. A. C.			Strain localization and fluid-assisted deformation in apatite and its influence on trace elements and U-Pb systematics	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						microstructures; apatite recrystallization; EBSD; trace elements and U-Pb system; dynamic recrystallization; fluid-assisted recrystallization	PLASTIC-DEFORMATION; SHEAR ZONE; QUARTZ; MONAZITE; CONSTRAINTS; ORIENTATION; EQUILIBRIA; EVOLUTION; ZIRCON; MICROSTRUCTURES	This paper presents electron backscatter diffraction (EBSD), trace element and U-Pb data of apatite grains from a granitic mylonite from the Taxaquara Shear Zone (SE Brazil). The mylonite recrystallized under upper-greenschist facies and presents two types of apatite with distinct microstructures. Type-1 apatite appears in quartz-rich layers and does not exhibit any microstructural, crystallographic, or chemical evidence of deformation/recrystallization, and resembles the original igneous apatite. Type-2 apatite appears in mica-rich layers and exhibits core-and-mantle microstructures, and intragranular subgrain development, suggesting that they have undergone dynamic recrystallization. Recrystallized tails of type-2 apatite grains exhibit a strong c-axis crystallographic preferred orientation parallel to the X-direction (stretching lineation), and lack evidence of dislocation density. This evidence from type-2 apatite grains, combined with REE depletion, high La and a negative Ce anomaly compared to type-1 grains, suggests that type-2 apatite tails underwent recrystallization via dissolution-precipitation creep, whereas parental grains underwent crystal-plastic deformation and subgrain formation through dynamic recrystallization. Phase-equilibrium modelling and quartz CPO opening-angle thermometry are consistent with recrystallization at similar to 480 - 530 degrees C and 2.2 - 5.0 kbar. We were not able to determine precise deformation ages from type-2 apatite because fluid-assisted recrystallization appears to have substantially decreased the U/Pb ratio. We find that preferential fluid flow along high-strain, biotite-rich layers in the mylonite caused type-2 apatite to recrystallise, whereas type-1 apatite in low strain layers was unaffected and retained the characteristics of the protolith. (C) 2020 Elsevier B.V. All rights reserved.	[Ribeiro, B., V; Hunter, N. J. R.; Raveggi, M.; Cawood, P. A.; Finch, M.] Monash Univ, Sch Earth Atmosphere & Environm Sci, Clayton, Vic 3800, Australia; [Lagoeiro, L.] Univ Fed Parana, Geol Dept, 100 Francisco Heraclito dos Santos St,Bloco 6, BR-35400000 Curitiba, Parana, Brazil; [Faleiros, F. M.; Campanha, G. A. C.] Univ Sao Paulo, Dept Mineral & Geotecton, Rua Lago 562, BR-05508900 Sao Paulo, Brazil; [Queiroga, G.] DEGEO EM UFOP, BR-35400000 Ouro Preto, MG, Brazil; [Ribeiro, B., V] 9 Rainforest Walk, Clayton, Vic 3800, Australia	Monash University; Universidade Federal do Parana; Universidade de Sao Paulo	Ribeiro, BV (autor correspondente), Monash Univ, Sch Earth Atmosphere & Environm Sci, Clayton, Vic 3800, Australia.	bruno.vieiraribeiro1@monash.edu; leonardo.lagoeiro@ufpr.br; ffalei@usp.br; nicholas.hunter@monash.edu; glauciaqueiroga@ufop.edu.br; massimo.raveggi@monash.edu; peter.cawood@monash.edu; melanie.finch@monash.edu; ginaldo@usp.br	Faleiros, Frederico Meira/F-6138-2010; Vieira Ribeiro, Bruno/HOC-3421-2023; Queiroga, Gláucia/AAJ-1823-2021	Faleiros, Frederico Meira/0000-0003-2199-8116; Vieira Ribeiro, Bruno/0000-0002-3652-1831; Queiroga, Gláucia/0000-0002-1730-0638; Finch, Melanie/0000-0001-9699-2769; Hunter, Nicholas/0000-0002-3374-6584; Cawood, Peter/0000-0003-1200-3826	Sao Paulo Research Foundation (FAPESP) post-graduate fellowships [2018/00320-9, 2018/163071, 2018/10012-0]; CNPq [425412/2018-0, 305232/2018-5, 307732/2019-3, 305701/2019-3]; Australian Research Council (ARC) [FL160100168]	Sao Paulo Research Foundation (FAPESP) post-graduate fellowships(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Australian Research Council (ARC)(Australian Research Council)	This work was supported by the Sao Paulo Research Foundation (FAPESP) post-graduate fellowships 2018/00320-9 and 2018/163071 to B.V. Ribeiro, grant 2018/10012-0 to F.M. Faleiros, by CNPq grants 425412/2018-0 and 305232/2018-5 to L. Lagoeiro, 307732/2019-3 to F.M. Faleiros and 305701/2019-3 to G.A.C. Campanha. We also thank the Australian Research Council (ARC) for grant FL160100168 to P.A. Cawood. Bruna Gomes Dias from LACTEC (Brazil) is thanked for assistance during EBSD data acquisition. We thank the Microscopy and Microanalysis Laboratory (LMic) of UFOP, a member of the Fundacao de Amparo a Pesquisa do Estado de Minas Gerais (FAPEMIG). The authors are grateful for the comments provided by Emily Chin and Robert Holder, helping us to improve the manuscript. We also appreciate Editor An Yin for its efficient editorial handling.	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Sci. Lett.	SEP 1	2020	545								116421	10.1016/j.epsl.2020.116421	http://dx.doi.org/10.1016/j.epsl.2020.116421			13	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	ML0RC					2023-06-23	WOS:000549183200016
J	Santos, LGS; Paz, SPA; Cunha, EJS; Souza, JAS				Santos, L. G. S.; Paz, S. P. A.; Cunha, E. J. S.; Souza, J. A. S.			Non-halogenated flame-retardant additive from Amazon mineral waste	JOURNAL OF MATERIALS RESEARCH AND TECHNOLOGY-JMR&T			English	Article						Mineral waste; Retardancy; Composite	UNSATURATED POLYESTER RESINS; STANDARD PXRD METHOD; MECHANICAL-PROPERTIES; THERMAL-DEGRADATION; COMBINED RIETVELD; LE BAIL; BEHAVIOR; KAOLINITE; BAUXITE; FLAMMABILITY	Halogenated flame-retardant additives typically release toxic gases during combustion, which has led to the search for substitutes. In an attempt to avoid this harmful effect on human health, the aim of this study was to investigate using a hydroxide-rich mineral waste to formulate a polymer matrix composite. The waste is rich in gibbsite Al(OH)(3), goethite FeO(OH) and kaolinite Al2Si2O5(OH)(4), which, once heated, release water at similar to 270, similar to 350 and similar to 500 degrees C, respectively. This waste is derived from processing metallurgical bauxite and is discarded in large amounts in northern Brazil. The retardancy effects of this bauxite waste were investigated for production of unsaturated polyester resin (UPR) matrix composites with varying contents 1030% of waste. The mechanical properties were also evaluated and it was noticed that the increasing the amount of filler decrease tensile strength of composites. The flammability tests revealed that the waste significantly retarded flame propagation in the polyester and the rate burning in these composites were as effective as the rate burning of the composites containing the reference material (RM). Lastly, the gibbsite-kaolinite-goethite inorganic material, which is now considered only as waste, has the potential to become a sustainable coproduct of the bauxite industry and economical raw material (flame-retardant filler) for the production of polymer-matrix composites. (C) 2020 The Authors. Published by Elsevier B.V.	[Santos, L. G. S.; Cunha, E. J. S.; Souza, J. A. S.] UFPA Univ Fed Para, Programa Posgrad Engn Quim, BR-66075110 Belem, PA, Brazil; [Paz, S. P. A.; Souza, J. A. S.] UFPA Univ Fed Para, Programa Posgrad Engn Recursos Nat Amazonia, BR-66075110 Belem, PA, Brazil	Universidade Federal do Para; Universidade Federal do Para	Santos, LGS (autor correspondente), UFPA Univ Fed Para, Programa Posgrad Engn Quim, BR-66075110 Belem, PA, Brazil.	lesleyglenda@gmail.com	Santos, Lesley/HNI-5006-2023	de Sousa Cunha, Edinaldo Jose/0000-0001-8047-6786; Santos, Lesley/0000-0002-1473-5847	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel-Superior); CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) [01/2016, 402427/2016-5]; PROPESP/UFPA [01/2020]; Mineracao Paragominas SA Company (Norsk Hydro)	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel-Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); PROPESP/UFPA; Mineracao Paragominas SA Company (Norsk Hydro)(Norsk Hydro ASA)	The authors thank the Brazilian agencies: CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel-Superior) for a PhD scholarship to the first author; CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) for financial support (Edital MCT/CNPq/Universal No 01/2016,402427/2016-5) and we appreciate the financial support of PROPESP/UFPA (Edital PAPQ N. 01/2020). We also acknowledge the Mineracao Paragominas SA Company (Norsk Hydro) for the support.	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N., 2005, Cerâmica, V51, P239, DOI 10.1590/S0366-69132005000300011; Zhang S, 2003, PROG POLYM SCI, V28, P1517, DOI 10.1016/j.progpolymsci.2003.09.001	63	5	5	2	11	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	2238-7854	2214-0697		J MATER RES TECHNOL	J. Mater. Res. Technol-JMRT	SEP-OCT	2020	9	5					11531	11544		10.1016/j.jmrt.2020.08.007	http://dx.doi.org/10.1016/j.jmrt.2020.08.007			14	Materials Science, Multidisciplinary; Metallurgy & Metallurgical Engineering	Science Citation Index Expanded (SCI-EXPANDED)	Materials Science; Metallurgy & Metallurgical Engineering	OC7WE		gold			2023-06-23	WOS:000579367500183
J	Santos, LB; Barreto, JA; de Assis, RD; de Souza, CT; Ferreira, SLC; Novaes, CG; Lemos, VA				Santos, Luana Bastos; Barreto, Jeferson Alves; dos Santos de Assis, Rosivan; de Souza, Cheilane Tavares; Ferreira, Sergio Luis Costa; Novaes, Cleber Galvao; Lemos, Valfredo Azevedo			Solid-Phase Extraction and Detection by Digital Image Directly in the Sorbent: Determination of Nickel in Environmental Samples	WATER AIR AND SOIL POLLUTION			English	Article						Digital image; Solid-phase extraction; Nickel; Food; Water; Cigarette	ATOMIC-ABSORPTION-SPECTROMETRY; POLYURETHANE FOAM; ANALYTICAL-CHEMISTRY; OPTIMIZATION; FOOD; PRECONCENTRATION; SORPTION; DESIGNS; COPPER; ENHANCEMENT	Recently, analytical procedures based on computer vision related to the colorimetric analysis of digital images have been described in the scientific literature. In this sense, a novel analytical approach is presented based on digital image colorimetry for nickel determination. The method consists in the development of a system with solid-phase extraction, consisting basically of an extraction chamber filled with polystyrene divinylbenzene sorbent impregnated with the complexing reagent 1-(2-thiazolylazo)-p-cresol (TAC) and a portable microscope multifunction, used for image acquisition. The image of the sorbent after extraction of Ni is obtained. This image is related to the concentration of the elements. The variables (pH, flow, and sample volume) were evaluated using a full factorial design 2(3) for the screening and a Doehlert matrix to establish the significant variables' optimal levels. The enrichment factor and limit of detection were 148 and 0.8 mu g L-1, respectively. The method was applied to the determination of nickel in river water, coffee, and cigarette samples.	[Santos, Luana Bastos; Barreto, Jeferson Alves; dos Santos de Assis, Rosivan; Novaes, Cleber Galvao; Lemos, Valfredo Azevedo] Univ Estadual Sudoeste Bahia, Lab Quim Analit, Campus Jequie, BR-45208091 Jequie, BA, Brazil; [Santos, Luana Bastos; de Souza, Cheilane Tavares; Ferreira, Sergio Luis Costa; Lemos, Valfredo Azevedo] Univ Fed Bahia, Programa Posgrad Quim, Campus Univ Ondina, BR-40170280 Salvador, BA, Brazil; [Barreto, Jeferson Alves] Univ Fed Fluminense, Dept Quim Analit, Outeiro Sao Joao Batista S-N, BR-24020141 Niteroi, RJ, Brazil	Universidade Estadual do Sudoeste da Bahia; Universidade Federal da Bahia; Universidade Federal Fluminense	Lemos, VA (autor correspondente), Univ Fed Bahia, Programa Posgrad Quim, Campus Univ Ondina, BR-40170280 Salvador, BA, Brazil.	vlemos@uesb.edu.br	LEMOS, VALFREDO AZEVEDO/I-7647-2014; Santos, Luana Bastos/ABI-4967-2020	LEMOS, VALFREDO AZEVEDO/0000-0002-6029-3218; Santos, Luana Bastos/0000-0002-5063-201X	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [311419/2018-6]; Fundacao de Amparo a Pesquisa do Estado da Bahia	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado da Bahia	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) Finance Code 001. The authors also acknowledge the financial support of the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (311419/2018-6) and the Fundacao de Amparo a Pesquisa do Estado da Bahia.	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SEP 1	2020	231	9							476	10.1007/s11270-020-04838-x	http://dx.doi.org/10.1007/s11270-020-04838-x			9	Environmental Sciences; Meteorology & Atmospheric Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences; Water Resources	NO3ZE					2023-06-23	WOS:000569424000004
J	Santos, MVS; da Silva, JB; de Carvalho, CEV; Vergilio, CD; Hadlich, GM; de Santana, CO; de Jesus, TB				Silva Santos, Marcus Vinicius; da Silva Junior, Jucelino Balbino; Veiga de Carvalho, Carlos Eduardo; Vergilio, Cristiane dos Santos; Hadlich, Gisele Mara; de Santana, Carolina Oliveira; de Jesus, Taise Bomfim			Geochemical evaluation of potentially toxic elements determined in surface sediment collected in an area under the influence of gold mining	MARINE POLLUTION BULLETIN			English	Article						Metals; Geochemical indexes; Contamination assessment; Environmental risk; Tropical river	WATER-QUALITY; HEAVY-METALS; MINAS-GERAIS; POLLUTION; STATE; BAHIA	In this present paper, the distribution of toxic metals and sediment quality were evaluated in five sampling points of the Itapicuru-Mirim River located in the city of Jacobina, Bahia, Brazil. The concentration of the elements arsenic (As), cadmium (Cd), chromium (Cr), copper (Cu), iron (Fe), mercury (Hg), manganese (Mn), nickel (Ni), lead (Pb), and zinc (Zn) were determined from sediment samples collected from the superficial layer (0-10 cm) in November 2013. After the samples' total decomposition, the total concentration of metals was determined by inductively coupled plasma optical emission spectrometry (ICP OES), except for Hg, which was measured by inductively coupled plasma atomic emission spectrometry (ICP AES). A geochemical evaluation of sediment quality was performed using enrichment factor (EF), geoaccumulation index (I-geo), and pollution load index (PLIThe results of the total concentrations in the analyzed sediment samples were compared with the threshold effect levels (TELs) and probable (PELs) effect levels (PELs) in sediment quality guidelines (SQGs). For the fraction < 75 mu m, the decreasing order for the metal concentrations was (ppm): Fe (10.86%) > Mn (120.8) > Cr (122) > Zn (76.5) > Pb (49.6) > Cu (32.6) > Ni (28.6) > Hg (0.31) > Cd (0.13). I-geo suggested a moderate to seriously polluted category for Hg and moderately polluted for Cu. Generally, the results indicated probable risks to the biota caused by Cr, Ni, Pb, and Hg metals. However, only Hg, Cd, and Cu were of anthropogenic origin. Although the sediments are relatively preserved from pollution by these metals, there is a progressive deterioration of this compartment downstream of the Itapicuru-Mirim River in the city of Jacobina.	[Silva Santos, Marcus Vinicius; da Silva Junior, Jucelino Balbino; Hadlich, Gisele Mara] Fed Univ Bahia UFBA, Postgrad Program Geochem Petr & Environm POSPETRO, Geosci Inst, Rua Barao Jeremoabo S-N, BR-40170110 Salvador, BA, Brazil; [Silva Santos, Marcus Vinicius; de Santana, Carolina Oliveira; de Jesus, Taise Bomfim] Fed Inst Bahia IFBA, Tv Santo Amaro 44,Santo Amaro Campus, BR-44200000 Santo Amaro Da Purificac, BA, Brazil; [Veiga de Carvalho, Carlos Eduardo; Vergilio, Cristiane dos Santos] North Fluminense State Univ Darcy Ribeiro, Alberto Lamego Ave 2000,California Pk, BR-28013602 Campos Dos Goytacazes, RJ, Brazil	Instituto Federal da Bahia (IFBA)	da Silva, JB (autor correspondente), Fed Univ Bahia UFBA, Postgrad Program Geochem Petr & Environm POSPETRO, Geosci Inst, Rua Barao Jeremoabo S-N, BR-40170110 Salvador, BA, Brazil.	jucejr@ufba.br	Hadlich, Gisele/AAO-4708-2020; da Silva, Jucelino Balbino/AAA-3611-2021; Vergilio, Cristiane S/H-9172-2012; Carvalho, Carlos/V-4734-2018	dos Santos Vergilio, Cristiane/0000-0003-1711-7320; Hadlich, Gisele Mara/0000-0002-6304-0988; Carvalho, Carlos/0000-0002-7704-9588	CAPES-Brazil [PNPD 2311/2011]	CAPES-Brazil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	We thank the Environmental Studies Laboratory of the North Fluminense State University (UENF) for the analyses performed. This study was financed in part by the CAPES-Brazil for postdoctoral fellowship (PNPD 2311/2011).	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Pollut. Bull.	SEP	2020	158								111384	10.1016/j.marpolbul.2020.111384	http://dx.doi.org/10.1016/j.marpolbul.2020.111384			7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	MU2JQ	32573455				2023-06-23	WOS:000555500000025
J	Souza, CM; Shimbo, JZ; Rosa, MR; Parente, LL; Alencar, AA; Rudorff, BFT; Hasenack, H; Matsumoto, M; Ferreira, LG; Souza, PWM; de Oliveira, SW; Rocha, WF; Fonseca, AV; Marques, CB; Diniz, CG; Costa, D; Monteiro, D; Rosa, ER; Velez-Martin, E; Weber, EJ; Lenti, FEB; Paternost, FF; Pareyn, FGC; Siqueira, JV; Viera, JL; Neto, LCF; Saraiva, MM; Sales, MH; Salgado, MPG; Vasconcelos, R; Galano, S; Mesquita, VV; Azevedo, T				Souza Jr, Carlos M.; Shimbo, Julia Z.; Rosa, Marcos R.; Parente, Leandro L.; Alencar, Ane A.; Rudorff, Bernardo F. T.; Hasenack, Heinrich; Matsumoto, Marcelo; Ferreira, Laerte G.; Souza-Filho, Pedro W. M.; de Oliveira, Sergio W.; Rocha, Washington F.; Fonseca, Antonio, V; Marques, Camila B.; Diniz, Cesar G.; Costa, Diego; Monteiro, Dyeden; Rosa, Eduardo R.; Velez-Martin, Eduardo; Weber, Eliseu J.; Lenti, Felipe E. B.; Paternost, Fernando F.; Pareyn, Frans G. C.; Siqueira, Joao, V; Viera, Jose L.; Ferreira Neto, Luiz C.; Saraiva, Marciano M.; Sales, Marcio H.; Salgado, Moises P. G.; Vasconcelos, Rodrigo; Galano, Soltan; Mesquita, Vinicius V.; Azevedo, Tasso			Reconstructing Three Decades of Land Use and Land Cover Changes in Brazilian Biomes with Landsat Archive and Earth Engine	REMOTE SENSING			English	Article						land use; land cover change; Landsat; random forest; time-series; Brazilian biomes	ATLANTIC FOREST; ACCURACY ASSESSMENT; ESTIMATING AREA; DEFORESTATION; CONSERVATION; NEEDS; METHODOLOGY; RESPONSES; SCIENCE	Brazil has a monitoring system to track annual forest conversion in the Amazon and most recently to monitor the Cerrado biome. However, there is still a gap of annual land use and land cover (LULC) information in all Brazilian biomes in the country. Existing countrywide efforts to map land use and land cover lack regularly updates and high spatial resolution time-series data to better understand historical land use and land cover dynamics, and the subsequent impacts in the country biomes. In this study, we described a novel approach and the results achieved by a multi-disciplinary network called MapBiomas to reconstruct annual land use and land cover information between 1985 and 2017 for Brazil, based on random forest applied to Landsat archive using Google Earth Engine. We mapped five major classes: forest, non-forest natural formation, farming, non-vegetated areas, and water. These classes were broken into two sub-classification levels leading to the most comprehensive and detailed mapping for the country at a 30 m pixel resolution. The average overall accuracy of the land use and land cover time-series, based on a stratified random sample of 75,000 pixel locations, was 89% ranging from 73 to 95% in the biomes. The 33 years of LULC change data series revealed that Brazil lost 71 Mha of natural vegetation, mostly to cattle ranching and agriculture activities. Pasture expanded by 46% from 1985 to 2017, and agriculture by 172%, mostly replacing old pasture fields. We also identified that 86 Mha of the converted native vegetation was undergoing some level of regrowth. Several applications of the MapBiomas dataset are underway, suggesting that reconstructing historical land use and land cover change maps is useful for advancing the science and to guide social, economic and environmental policy decision-making processes in Brazil.	[Souza Jr, Carlos M.; Fonseca, Antonio, V] Inst Homem & Meio Ambiente Amazonia Imazon, BR-66055200 Belem, Para, Brazil; [Shimbo, Julia Z.; Alencar, Ane A.; Marques, Camila B.; Lenti, Felipe E. B.] Inst Pesquisa Ambiental Amazonia Ipam, BR-70863520 Brasilia, DF, Brazil; [Rosa, Marcos R.] Univ Sao Paulo, Fac Filosofia Letras & Ciencias Humanas, Programa Posgrad Geog Fis, BR-05508000 Sao Paulo, Brazil; [Parente, Leandro L.; Ferreira, Laerte G.; Mesquita, Vinicius V.] Fed Univ Goias UFG, Image Proc & GIS Lab LAPIG, BR-74001970 Goiania, Go, Brazil; [Rudorff, Bernardo F. T.; Saraiva, Marciano M.; Salgado, Moises P. G.] Agrosatelite Geotecnol Aplicada Ltda, BR-88050000 Florianopolis, SC, Brazil; [Hasenack, Heinrich; Velez-Martin, Eduardo] Univ Fed Rio Grande do Sul, Ctr Ecol, BR-91501970 Porto Alegre, RS, Brazil; [Matsumoto, Marcelo] WRI Brasil, BR-05422030 Sao Paulo, Brazil; [Souza-Filho, Pedro W. M.] Univ Fed Para, Inst Tecnol Vale, BR-66055090 Belem, Para, Brazil; [de Oliveira, Sergio W.] Ecostage, BR-01402002 Sao Paulo, Brazil; [Rocha, Washington F.; Costa, Diego; Vasconcelos, Rodrigo; Galano, Soltan] Univ Estadual Feira de Santana, Programa Posgrad Modelagem Ciencias Terra & Ambie, BR-44031460 Feira De Santana, BA, Brazil; [Diniz, Cesar G.; Ferreira Neto, Luiz C.] Solved Solut Geoinformat, BR-66077830 Belem, Para, Brazil; [Monteiro, Dyeden] Terras App Solut, BR-66055050 Belem, Para, Brazil; [Rosa, Eduardo R.; Paternost, Fernando F.] ArcPlan, BR-04026001 Sao Paulo, Brazil; [Weber, Eliseu J.] Univ Fed Rio Grande do Sul, Dept Interdisciplinar, BR-95590000 Tramandai, Brazil; [Pareyn, Frans G. C.; Viera, Jose L.] Assoc Plantas Nordeste, BR-50731280 Recife, PE, Brazil; [Siqueira, Joao, V] JVN SIQUEIRA ME, BR-66010000 Belem, Para, Brazil; [Sales, Marcio H.] MHR Sales Consultoria, BR-66010000 Belem, Para, Brazil; [Azevedo, Tasso] MapBiomas, Observ Clima, BR-05418060 Sao Paulo, Brazil	Universidade de Sao Paulo; Universidade Federal do Rio Grande do Sul; Instituto Tecnologico Vale Desenvolvimento Sustentavel; Universidade Federal do Para; Universidade Estadual de Feira de Santana; Universidade Federal do Rio Grande do Sul	Souza, CM (autor correspondente), Inst Homem & Meio Ambiente Amazonia Imazon, BR-66055200 Belem, Para, Brazil.	souzajr@imazon.org.br; julia.shimbo@ipam.org.br; marcosrosa@usp.br; leal.parente@discente.ufg.br; ane@ipam.org.br; bernardo@agrosatelite.com.br; hhasenack@ufrgs.br; marcelo.matsumoto@wri.org; laerte@ufg.br; pedro.martins.souza@itv.org; sergio.oliveira@ecostage.com.br; wrocha@uefs.br; antoniovictor@imazon.org.br; camila.balzani@ipam.org.br; cesar.diniz@solved.eco.br; diego.costa@uefs.br; dyedenm@gmail.com; eduardo@arcplan.com.br; evelezmartin@gmail.com; eliseu.weber@ufrgs.br; felipe.lenti@ipam.org.br; paternost@arcplan.com.br; franspar@rocketmail.com; joaovsiqueiral@gmail.com; jlvieira@gmail.com; luiz.cortinhas@solved.eco.br; marciano@agrosatelite.com.br; marcio.ribeirosales@wur.nl; moises@agrosatelite.com.br; rnv@uefs.br; soltan.galano@geodatin.com.br; mesquita@discente.ufg.br; tasso.azevedo@mapbiomas.org	Souza, CARLOS/AAK-8207-2021; Souza-Filho, Pedro Walfir M. M./J-4958-2012; Franca-Rocha, Washington/B-6184-2013; Souza, Pedro/GZH-1275-2022; Hasenack, Heinrich/AAD-7332-2022; Weber, Eliseu José/AAK-6525-2021	Souza, CARLOS/0000-0002-0205-6134; Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; Franca-Rocha, Washington/0000-0002-2175-2792; Weber, Eliseu José/0000-0003-4873-0232; Rudorff, Bernardo/0000-0003-2931-0427; Diniz, Cesar/0000-0001-7718-0992; Parente, Leandro/0000-0003-1589-0467; Marques, Camila/0000-0001-7696-8569; Lenti, Felipe/0000-0001-7790-7573; Salgado, Moises/0000-0001-5314-4698; Hasenack, Heinrich/0000-0002-8521-1266; Fonseca, Antonio/0000-0001-6309-6204; Mesquita, Vinicius/0000-0003-0400-4087; Alencar, Ane Auxiliadora Costa/0000-0001-5605-7469; Saraiva, Marciano/0000-0002-4697-5239; Velez-Martin, Eduardo/0000-0001-8028-8953; Costa, Diego/0000-0002-5117-898X; Rosa, Eduardo/0000-0003-1370-6558; Rosa, Marcos/0000-0001-5367-8059; Matsumoto, Marcelo/0000-0003-2899-6981	Norway's International Climate and Forest Initiative (NICFI); Gordon & Betty Moore Foundation; Arapyau Institute; Good Energies Foundation; Institute for Climate and Society (iCS); Humanize Institute; Children's Investment Fund Foundation; Wellspring Foundation; Quadrature Climate Foundation; Walmart Foundation; Global Wildlife Conservation; Climate and Land Use Alliance (CLUA); Oak Foundation	Norway's International Climate and Forest Initiative (NICFI); Gordon & Betty Moore Foundation(Gordon and Betty Moore Foundation); Arapyau Institute; Good Energies Foundation; Institute for Climate and Society (iCS); Humanize Institute; Children's Investment Fund Foundation; Wellspring Foundation; Quadrature Climate Foundation; Walmart Foundation; Global Wildlife Conservation; Climate and Land Use Alliance (CLUA); Oak Foundation	MapBiomas project is supported by Norway's International Climate and Forest Initiative (NICFI), Gordon & Betty Moore Foundation, Arapyau Institute, Good Energies Foundation, Institute for Climate and Society (iCS), Humanize Institute, Children's Investment Fund Foundation, Wellspring Foundation, Quadrature Climate Foundation, Walmart Foundation, Global Wildlife Conservation, Climate and Land Use Alliance (CLUA) and Oak Foundation.	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SEP	2020	12	17							2735	10.3390/rs12172735	http://dx.doi.org/10.3390/rs12172735			27	Environmental Sciences; Geosciences, Multidisciplinary; Remote Sensing; Imaging Science & Photographic Technology	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Environmental Sciences & Ecology; Geology; Remote Sensing; Imaging Science & Photographic Technology	NO7FD		gold, Green Published			2023-06-23	WOS:000569652700001
J	Warren, LV; Buatois, LA; Mangano, MG; Simoes, MG; Santos, MGM; Poir, DG; Riccomini, C; Assine, ML				Warren, L., V; Buatois, L. A.; Mangano, M. G.; Simoes, M. G.; Santos, M. G. M.; Poir, D. G.; Riccomini, C.; Assine, M. L.			Microbially induced pseudotraces from a Pantanal soda lake, Brazil: Alternative interpretations for Ediacaran simple trails and their limits	GEOLOGY			English	Article							MISTAKEN POINT FORMATION; TRACE FOSSILS; CAMBRIAN TRANSITION; TILTING MARKS; 1ST EVIDENCE; QUATERNARY; LOCOMOTION; EVOLUTION; ORIGIN; RECORD	Despite the absence of metazoans, structures resembling animal traces are common in a soda lake from the western Brazil Pantanal wetland. Pantanal soda lakes are ecologically extreme environments that preclude complex life, allowing extremophiles to flourish. Direct observation indicates that these structures are pseudotraces, representing groove marks that result from the interaction of wave-transported floating rafts of epibenthic microbial mat fragments with the substrate. Variations in wind/wave direction and intensity result in marks of different size and morphology. The most common pseudotraces are simple and slightly curved, narrow grooves (type 1), whereas others are straight and present raised lateral ridges (type 2). Both are V-shaped in cross section. Type 3 comprises long, sinuous, shallow grooves, displaying internal crescentic laminated infill and U-shaped cross section. The similarity of these pseudotraces to Ediacaran structures usually interpreted as animal trace fossils suggests that care should be exercised in their analysis. A set of criteria is proposed to differentiate microbially induced pseudotraces from trace fossils. Analysis of Ediacaran structures needs to be performed on a case-by-case basis, taking into account morphology, orientation, and preservation style of the structure, sedimentary environment, and presence or absence of microbial mats.	[Warren, L., V; Assine, M. L.] Sao Paulo State Univ, Dept Geol, BR-13506900 Rio Claro, Brazil; [Buatois, L. A.; Mangano, M. G.] Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada; [Simoes, M. G.] Sao Paulo State Univ, Dept Zool, BR-18618000 Botucatu, SP, Brazil; [Santos, M. G. M.] Univ Fed ABC, Ctr Engn Modelagem & Ciencias Sociais Aplicadas, BR-09210580 Santo Andre, SP, Brazil; [Poir, D. G.] Univ Nacl La Plata, CONICET, Ctr Invest Geol, RA-1900 La Plata, Argentina; [Riccomini, C.] Univ Sao Paulo, Inst Energia & Ambiente, BR-05508010 Sao Paulo, Brazil	Universidade Estadual Paulista; University of Saskatchewan; Universidade Estadual Paulista; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of La Plata; Universidade de Sao Paulo	Warren, LV (autor correspondente), Sao Paulo State Univ, Dept Geol, BR-13506900 Rio Claro, Brazil.	lucas.warren@unesp.br	Simoes, Marcello G/C-2373-2012; Assine, Mario L/C-1154-2013; Assine, Mario/S-6150-2019; Santos, Mauricio/H-6481-2014	Assine, Mario L/0000-0002-3097-5832; Assine, Mario/0000-0002-3097-5832; Santos, Mauricio/0000-0002-9165-4979; Poire, Daniel G./0000-0003-0966-122X	Brazilian National Council for Scientific and Technological Development (CNPq) [2014/068892, 2014/13937-3]; Sao Paulo Research Foundation (FAPESP) [2018/26230-6]; Natural Sciences and Engineering Research Council of Canada (NSERC) [311726-13, 311727-15]	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	We thank the Brazilian National Council for Scientific and Technological Development (CNPq; 2014/068892, 2014/13937-3), the Sao Paulo Research Foundation (FAPESP; 2018/26230-6), and the Natural Sciences and Engineering Research Council of Canada (NSERC; 311726-13, 311727-15) for funding; Barranco Alto Farm for financial and logistic support; and reviewers S. Darroch, P. Getty, and A. Liu for constructive suggestions.	Assine ML, 2015, BRAZ J GEOL, V45, P475, DOI 10.1590/2317-4889201520150014; Assine ML, 2004, QUATERN INT, V114, P23, DOI 10.1016/S1040-6182(03)00039-9; Bergier I., 2014, DYNAMICS PANTANAL WE, V37, P145, DOI [10.1007/698_2014_327, DOI 10.1007/698_2014_327]; Buatois L. 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J	Cardoso, LG; Duarte, JH; Andrade, BB; Lemos, PVF; Costa, JAV; Druzian, JI; Chinalia, FA				Cardoso, Lucas Guimaraes; Duarte, Jessica Hartwig; Andrade, Bianca Bomfim; Franca Lemos, Paulo Vitor; Vieira Costa, Jorge Alberto; Druzian, Janice Izabel; Chinalia, Fabio Alexandre			Spirulina sp. LEB 18 cultivation in outdoor pilot scale using aquaculture wastewater: High biomass, carotenoid, lipid and carbohydrate production	AQUACULTURE			English	Article						Aquaculture wastewater; Spirulina; Carbohydrate; Bioremediation	MICROALGAE BIOMASS; PLATENSIS; GROWTH; REMOVAL; PHOTOBIOREACTOR; ARTHROSPIRA; EFFLUENTS; CULTURE	The objective of this study was to integrate the treatment of aquaculture effluent with the biomass and macronutrients production by Spirulina sp. LEB 18. The first experiment was carried out in a photobioreactor (1 L) and the best biomass production condition was reproduced on a pilot scale in a raceway type bioreactor (5 L). The best treatment was T25 (100% of wastewater supplemented with 25% of Zarrouk nutrients). The biomass production in the raceway system (T25) was higher (3.33 g L-1) than the control (2.32 g L-1) and the carbohydrate (69.77%) and lipid (12.77%) were also higher. The content of carotenoids in T25 was significant (9.68 mu g mL(-1)). Spirulina sp. LEB 18 removed phosphate (99.97%); COD (89.34%) and nitrate (81.10%) from aquaculture effluent. The effluent showed absence of heavy metals and concentration of Al; Fe; Ca and Mg higher than the control culture with Zarrouk nutrients. The Spirulina sp. LEB 18 can be applied as a bioremediation agent of aquaculture wastewater with high production of biomass, carbohydrate, lipid and carotenoid.	[Cardoso, Lucas Guimaraes; Andrade, Bianca Bomfim; Franca Lemos, Paulo Vitor; Chinalia, Fabio Alexandre] Univ Fed Bahia, Inst Hlth Sci, Dept Biotechnol, Salvador, BA, Brazil; [Duarte, Jessica Hartwig; Vieira Costa, Jorge Alberto] Fed Univ Rio Grande, Coll Chem & Food Engn, Lab Biochem Engn, Rio Grande, Brazil; [Druzian, Janice Izabel] Univ Fed Bahia, Fac Pharm, Grad Program Food Sci, Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal do Rio Grande; Universidade Federal da Bahia	Cardoso, LG (autor correspondente), Fed Univ Bahia UFBA, Inst Hlth Sci, Dept Biotechnol, Salvador, BA, Brazil.	lucaseng.pesca@yahoo.com.br	Andrade, Bianca/M-4030-2017; Lemos, Paulo Vitor França/AAQ-7853-2021; Druzian, Janice Izabel/G-6884-2015; Costa, Jorge A V/L-3999-2013; Cardoso, Lucas/AAS-2431-2020; Andrade, Bianca Bomfim/GYU-6357-2022; Duarte, Jessica Hartwig/AAP-9443-2020	Andrade, Bianca/0000-0003-2945-1510; Lemos, Paulo Vitor França/0000-0002-7138-4297; Costa, Jorge A V/0000-0001-8042-7642; Cardoso, Lucas/0000-0002-6674-338X; Andrade, Bianca Bomfim/0000-0001-6439-8618; Druzian, Janice Izabel/0000-0001-8940-6098	FAPESB -Foundation for Research Support of Bahia [400710/2014-5]; MCTIC (Ministry of Technological Information and Communication Science) Brazil; Bahia Pesca	FAPESB -Foundation for Research Support of Bahia; MCTIC (Ministry of Technological Information and Communication Science) Brazil; Bahia Pesca	All authors acknowledge supported by FAPESB -Foundation for Research Support of Bahia to project CNPQ (400710/2014-5), MCTIC (Ministry of Technological Information and Communication Science) Brazil and Bahia Pesca.	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J	Garnier, JM; Garnier, J; Debnath, P; Prado, LF; Yokoyama, E; Das, RK; Mathe, PE; Islam, MS				Garnier, J-M; Garnier, J.; Debnath, P.; Prado, L. F.; Yokoyama, E.; Das, R. K.; Mathe, P-E; Islam, M. S.			Late Holocene paleoenvironmental records in Eastern Bangladesh from lake sediments: A multi-proxy approach	QUATERNARY INTERNATIONAL			English	Article						Lake sedimentation; Late Holocene; Multiproxy; Paleoclimate reconstitution; Medieval warm; Period little ice age transition; Bangladesh	ICE-AGE; MAGNETIC-SUSCEPTIBILITY; MONSOON VARIABILITY; VARVED SEDIMENTS; CLIMATE; CHINA; RECONSTRUCTION; ASIA	Lacustrine sediments in a poorly documented region regarding to lake sedimentation and paleo-environments (Bangladesh) were investigated using a multiproxy approach. Pukurpara Lake is located in eastern Bangladesh at an elevation of 360 m above sea level with a maximum water depth of 28 m. An age-depth model allowed us to investigate the changes in sedimentation that occurred since 850 CE. The high resolution multielement analyses by micro-X fluorescence scanning (mu XRF) showed multiple variations over short increments. Variation in the abundance of elements with depth as well the ratios of the abundance of some elements (Fe/Ti and Zr/Rb) suggested both rapid and long-term changes in the origin of the material deposited, which, in turn, suggested changes in weather conditions. Principal Components Analysis (PCAs) mixing mu XRF and Magnetic Susceptibility data allow identifying changes in geochemical redox processes between the Medieval Warm Period (MWP) and Little Ice Age (LIA). The drastic changes in the different proxies (magnetic susceptibility, diatom assemblages, fresh water/marine water diatom ratios, abundance of Fe and S, and the Fe/Ti ratio) were interpreted to be the result of climate change before and after the MWP-LIA transition period, the Little Ice Age period being relatively wet.	[Garnier, J-M; Mathe, P-E] Aix Marseille Univ, Coll France, CEREGE, INRA,IRD,CNRS, Aix En Provence, France; [Garnier, J.] Univ Brasilia, IG GMP ICC Ctr, Inst Geociencias, BR-70919970 Brasilia, DF, Brazil; [Debnath, P.] Ctr Environm & Geog Informat Serv CEGIS, Dhaka 1212, Bangladesh; [Prado, L. F.; Yokoyama, E.] Campus Univ Darcy Ribeiro ICC Ala Cent, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Das, R. K.] Bangladesh Ctr Coastal & Ocean Studies BACCOS, Dhaka 1000, Bangladesh; [Islam, M. S.] Univ Dhaka, Dept Geog & Environm, Coastal Res Unit CRU, Dhaka 1000, Bangladesh	Centre National de la Recherche Scientifique (CNRS); INRAE; Institut de Recherche pour le Developpement (IRD); UDICE-French Research Universities; Aix-Marseille Universite; Universite PSL; College de France; Universidade de Brasilia; University of Dhaka	Garnier, JM (autor correspondente), Aix Marseille Univ, Coll France, CEREGE, INRA,IRD,CNRS, Aix En Provence, France.	jmg.cerege@gmail.com; garnier.geol@gmail.com; prem10geo@gmail.com; lucianaprado@unb.br; eyokoyama@unb.br; dhrubotosh@gmail.com; shahidul.geoenv@du.ae.bd	Prado, Luciana Figueiredo/M-9312-2019	Prado, Luciana Figueiredo/0000-0002-6446-8986				Ahammed F, 2012, WATER INT, V37, P43, DOI 10.1080/02508060.2012.645191; Anderson NJ, 2000, EUR J PHYCOL, V35, P307, DOI 10.1017/S0967026200002857; Balsam WL, 2011, QUATERNARY SCI REV, V30, P2732, DOI 10.1016/j.quascirev.2011.06.002; Blaauw M, 2011, BAYESIAN ANAL, V6, P457, DOI 10.1214/ba/1339616472; Bradley R.S., 2015, RECONSTRUCTING CLIMA, P319; Cao L.L., 2012, MAR SCI B, V14, P70; Chen FH, 2006, SCI CHINA SER D, V49, P1280, DOI 10.1007/s11430-006-2027-4; Chen JH, 2015, QUATERNARY SCI REV, V107, P98, DOI 10.1016/j.quascirev.2014.10.012; Chu GQ, 2013, GFF, V135, P265, DOI 10.1080/11035897.2013.788550; Croudace IW, 2006, GEOL SOC SPEC PUBL, V267, P51, DOI 10.1144/GSL.SP.2006.267.01.04; Cuven S, 2011, QUATERNARY SCI REV, V30, P2651, DOI 10.1016/j.quascirev.2011.05.019; Das R.K., 2010, THESIS, V87; Debnath P., 2013, THESIS, P119; Francus P., 2009, PAGES (Past Global Changes) News, V17, P93; Holmgren K, 2012, J PALEOLIMNOL, V48, P311, DOI 10.1007/s10933-012-9596-3; Hu SY, 2000, SCI CHINA SER D, V43, P534, DOI 10.1007/BF02875315; Jin ZD, 2001, SCI CHINA SER D, V44, P652, DOI 10.1007/BF02875338; Jouve G, 2013, QUATERNARY SCI REV, V71, P191, DOI 10.1016/j.quascirev.2012.06.003; Kylander ME, 2011, J QUATERNARY SCI, V26, P109, DOI 10.1002/jqs.1438; Li Y, 2014, GLOBAL PLANET CHANGE, V116, P30, DOI 10.1016/j.gloplacha.2014.02.005; Ling Y, 2018, QUATERN INT, V487, P61, DOI 10.1016/j.quaint.2017.03.067; Liu JB, 2014, BOREAS, V43, P914, DOI 10.1111/bor.12072; Mooney SD, 2003, J ARCHAEOL SCI, V30, P511, DOI 10.1016/S0305-4403(02)00181-4; Nair K.M., 2014, JOUR GEOL SOC SRI LA, V16, P159; Peinerud EK, 2000, ENVIRON GEOL, V40, P64, DOI 10.1007/PL00013330; Polanski S, 2014, GLOBAL PLANET CHANGE, V122, P176, DOI 10.1016/j.gloplacha.2014.08.016; Reimer PJ, 2013, RADIOCARBON, V55, P1869, DOI 10.2458/azu_js_rc.55.16947; Round FE, 1990, BIOL MORPHOLOGY GENE, P747; Suokhrie T, 2018, QUATERN INT, V479, P128, DOI 10.1016/j.quaint.2017.05.037; Tooley M.J., 1981, ENV BRIT PREHISTORY, P1; Uberoi C., 2012, EOS T AM GEOPHYS UN, V93, P437, DOI [DOI 10.1029/2012EO440001, 10.1029/2012EO440001]; van der Bilt WGM, 2015, QUATERNARY SCI REV, V126, P201, DOI 10.1016/j.quascirev.2015.09.003; Veena MP, 2014, QUATERN INT, V325, P63, DOI 10.1016/j.quaint.2013.10.026; Warrier AK, 2017, GEOSCI FRONT, V8, P1349, DOI 10.1016/j.gsf.2017.01.004; Wilhelm B., 2012, QUAT RES; Williamson D, 1998, EARTH PLANET SC LETT, V155, P205, DOI 10.1016/S0012-821X(97)00217-3; Xiao JL, 2019, QUATERN INT, V527, P87, DOI 10.1016/j.quaint.2018.06.025; Yan H, 2015, NAT GEOSCI, V8, P315, DOI 10.1038/NGEO2375; Yang B, 2009, QUATERN INT, V194, P68, DOI 10.1016/j.quaint.2007.11.020; Zhang JW, 2011, QUATERNARY SCI REV, V30, P1973, DOI 10.1016/j.quascirev.2011.04.023; Zhou WJ, 1996, QUATERNARY RES, V46, P219, DOI 10.1006/qres.1996.0062	41	1	1	3	15	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	1040-6182	1873-4553		QUATERN INT	Quat. Int.	AUG 30	2020	558						39	46		10.1016/j.quaint.2020.06.049	http://dx.doi.org/10.1016/j.quaint.2020.06.049			8	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	OD4SP		Green Published, Bronze			2023-06-23	WOS:000579842700005
J	Lessa, D; Morard, R; Jonkers, L; Venancio, IM; Reuter, R; Baumeister, A; Albuquerque, AL; Kucera, M				Lessa, Douglas; Morard, Raphael; Jonkers, Lukas; Venancio, Igor M.; Reuter, Runa; Baumeister, Adrian; Albuquerque, Ana Luiza; Kucera, Michal			Distribution of planktonic foraminifera in the subtropical South Atlantic: depth hierarchy of controlling factors	BIOGEOSCIENCES			English	Article							WATER MASSES; NEOGLOBOQUADRINA-PACHYDERMA; INTERANNUAL VARIABILITY; LUNAR PERIODICITY; DISSOLVED-OXYGEN; SURFACE-WATER; SHELL FLUX; TEMPERATURE; OCEAN; SEA	Temperature appears to be the best predictor of species composition of planktonic foraminifera communities, making it possible to use their fossil assemblages to reconstruct sea surface temperature (SST) variation in the past. However, the role of other environmental factors potentially modulating the spatial and vertical distribution of planktonic foraminifera species is poorly understood. This is especially relevant for environmental factors affecting the subsurface habitat. If such factors play a role, changes in the abundance of subsurface-dwelling species may not solely reflect SST variation. In order to constrain the effect of subsurface parameters on species composition, we here characterize the vertical distribution of living planktonic foraminifera community across an east-west transect through the subtropical South Atlantic Ocean, where SST variability was small, but the subsurface water mass structure changed dramatically. Four planktonic foraminifera communities could be identified across the top 700 m of the transect. Gyre and Agulhas Leakage surface faunas were predominantly composed of Globigerinoides ruber, Globigerinoides tenellus, Trilobatus sacculifer, Globoturborotalita rubescens, Globigerinella calida, Tenuitella iota, and Globigerinita glutinata, and these only differed in terms of relative abundances (community composition). Upwelling fauna was dominated by Neogloboquadrina pachyderma, Neogloboquadrina incompta, Globorotalia crassaformis, and Globorotalia inflata. Thermocline fauna was dominated by Tenuitella fleisheri, Globorotalia truncatulinoides, and Globorotalia scitula in the west and by G. scitula only in the east. The largest part of the standing stock was consistently found in the surface layer, but SST was not the main predictor of species composition either for the depth-integrated fauna across the stations or at individual depth layers. Instead, we identified a pattern of vertical stacking of different parameters controlling species composition, reflecting different aspects of the pelagic habitat. Whereas productivity appears to dominate in the mixed layer (0-60 m), physical properties (temperature, salinity) become important at intermediate depths and in the subsurface, a complex combination of factors including oxygen concentration is required to explain the assemblage composition. These results indicate that the seemingly straightforward relationship between assemblage composition and SST in sedimentary assemblages reflects vertically and seasonally integrated processes that are only indirectly linked to SST. It also implies that fossil assemblages of planktonic foraminifera should also contain a signature of subsurface processes, which could be used for paleoceanographic reconstructions.	[Lessa, Douglas; Morard, Raphael; Jonkers, Lukas; Reuter, Runa; Baumeister, Adrian; Kucera, Michal] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Lessa, Douglas; Albuquerque, Ana Luiza] Univ Fed Fluminense, Programa Posgrad Geoquim Ambiental, BR-24020141 Niteroi, RJ, Brazil; [Venancio, Igor M.] Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Rodovia Pres Dutra, BR-12630000 Sao Paulo, Brazil	University of Bremen; Universidade Federal Fluminense	Lessa, D (autor correspondente), Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany.; Lessa, D (autor correspondente), Univ Fed Fluminense, Programa Posgrad Geoquim Ambiental, BR-24020141 Niteroi, RJ, Brazil.	dvolessa@id.uff.br	Kucera, Michal/ABH-6065-2020; Albuquerque, Ana Luiza S/C-5167-2013; Venancio, Igor M/I-5893-2014; Jonkers, Lukas/H-6314-2011; Kucera, Michal/B-9277-2009	Albuquerque, Ana Luiza S/0000-0003-1267-6190; Venancio, Igor M/0000-0003-3118-4247; Jonkers, Lukas/0000-0002-0253-2639; Kucera, Michal/0000-0002-7817-9018	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, CAPES/Brazil [001, 99999.000042/2017-00, 23038.001417/2914-71]; Deutsche Forschungsgemeinschaft (DFG) through Germany's Excellence Strategy [EXC-2077, 390741603]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, CAPES/Brazil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Deutsche Forschungsgemeinschaft (DFG) through Germany's Excellence Strategy(German Research Foundation (DFG))	This research has been supported by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, CAPES/Brazil, Finance Code 001 (grant nos. PE 99999.000042/2017-00 and 23038.001417/2914-71), and the Deutsche Forschungsgemeinschaft (DFG) through Germany's Excellence Strategy (EXC-2077, grant no. 390741603) to the Cluster of Excellence "The Ocean Floor -Earth's Uncharted Interface".	Aurahs R, 2011, MAR MICROPALEONTOL, V79, P1, DOI 10.1016/j.marmicro.2010.12.001; Be A.W.H., 1977, P1; Be A.W.H., 1971, MICROPALEONTOLOGY OC, P105; BE ALLEN W. 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J	Idalino, FD; da Rosa, KK; Acuna, FF; Veettil, BK; Simoes, JC; Souza, E				Idalino, Filipe Daros; da Rosa, Katia Kellem; Acuna, Francisco Ferrando; Veettil, Bijeesh Kozhikkodan; Simoes, Jefferson Cardia; Souza Jr, Enoil			Recent glacier variations on Mount Melimoyu (44 degrees 50'S-72 degrees 51'W), Chilean Patagonia, using Sentinel-2 data	GEOCARTO INTERNATIONAL			English	Article						Glacier Retreat; Geomorphometry; Remote Sensing; Chilean Patagonia; Sentinel-2	NORTHERN PATAGONIA; ANDES CORDILLERA; TROPICAL ANDES; ICE ELEVATION; MASS-BALANCE; PASCUA-LAMA; 20TH-CENTURY; INVENTORY; SHRINKAGE; ICEFIELD	This work analyzed the application of Sentinel-2 multispectral imagery and GLIMS data for mapping glacier retreat and to estimate glacier area changes of Mount Melimoyu, located in northern Patagonia, Chile for the period between 1970 and 2017. The results showed a decrease of about 35.61% in the area for the period analyzed and there is a continuing retreating trend in the region. The decreasing trend in mean annual precipitation may explain the recent glacier changes, which indicates a large sensibility for meteorological variability of glaciers, which is influenced by geomorphometry and glacier area, in the region. Using Sentinel 2 imagery, we provided inventory of rock glaciers in the study area. Glacier outlines obtained through manual delineation showed comparable results with the glacier outlines using Sentinel-2 MSI data in the study area, which shows greater accuracy in glacier mapping using Sentinel-2 data.	[Idalino, Filipe Daros] Univ Fed Rio Grande do Sul UFRGS, Ctr Polar & Climat, Programa Posgrad Geog, Porto Alegre, RS, Brazil; [da Rosa, Katia Kellem; Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul UFRGS, Ctr Polar & Climat, Inst Geociencias, Dept Geog, Porto Alegre, RS, Brazil; [Acuna, Francisco Ferrando] Univ Chile, Dept Geog, Santiago, Chile; [Veettil, Bijeesh Kozhikkodan] Ton Duc Thang Univ, Dept Management Sci & Technol Dev, Ho Chi Minh City, Vietnam; [Veettil, Bijeesh Kozhikkodan] Ton Duc Thang Univ, Fac Environm & Labour Safety, Ho Chi Minh City, Vietnam; [Souza Jr, Enoil] Univ Fed Rio Grande do Sul UFRGS, Ctr Polar & Climat CPC, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidad de Chile; Ton Duc Thang University; Ton Duc Thang University; Universidade Federal do Rio Grande do Sul	Veettil, BK (autor correspondente), Ton Duc Thang Univ, Dept Management Sci & Technol Dev, Ho Chi Minh City, Vietnam.; Veettil, BK (autor correspondente), Ton Duc Thang Univ, Fac Environm & Labour Safety, Ho Chi Minh City, Vietnam.	bijeesh.veettil@tdtu.edu.vn	da Rosa, Kátia Kellem/AAO-8367-2020; Simoes, Jefferson Cardia/D-7232-2013; Kozhikkodan Veettil, Bijeesh/Q-6489-2017	da Rosa, Kátia Kellem/0000-0003-0977-9658; Simoes, Jefferson Cardia/0000-0001-5555-3401; Kozhikkodan Veettil, Bijeesh/0000-0003-4158-4578; Idalino, Filipe/0000-0001-5587-5208	Brazilian Coordination for the Improvement of Higher Education Personnel (CAPES)	Brazilian Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The work is supported by the Brazilian Coordination for the Improvement of Higher Education Personnel (CAPES), Brazilian National Research Council for Scientific and Technological Development (CNPq), Programa de Pos-GraduacAo em Geografia - Universidade Federal do Rio Grande do Sul (UFRGS), INCT-Cryosphere and Polar and Climate Centre, UFRGS, Brazil.	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AUG 17	2020	35	11					1199	1213		10.1080/10106049.2018.1557262	http://dx.doi.org/10.1080/10106049.2018.1557262			15	Environmental Sciences; Geosciences, Multidisciplinary; Remote Sensing; Imaging Science & Photographic Technology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Remote Sensing; Imaging Science & Photographic Technology	MN6PR					2023-06-23	WOS:000550961300003
J	Lopes, RP; Pereira, JC; Kerber, L; Dillenburg, SR				Lopes, Renato Pereira; Pereira, Jamil Correa; Kerber, Leonardo; Dillenburg, Sergio Rebello			The extinction of the Pleistocene megafauna in the Pampa of southern Brazil	QUATERNARY SCIENCE REVIEWS			English	Article						Pleistocene; Pampa; Coastal plain; Megafauna; Extinction; Climate change; MIS 2; MIS 3	GRANDE-DO-SUL; ELECTRON-SPIN-RESONANCE; LAST GLACIAL TERMINATION; SAO RAIMUNDO NONATO; COASTAL-PLAIN; QUATERNARY VERTEBRATES; CLIMATE VARIABILITY; HUMAN COLONIZATION; HUMAN OCCUPATION; FAUNAL TURNOVER	The Late Pleistocene-early Holocene faunal turnover in South America was characterized by the extinction of all mammals with body mass >300 kg and several smaller taxa, but the driving mechanisms behind it are still poorly understood. Here is presented an analysis of the extinction in the Pampa of southern Brazil (Rio Grande do Sul state), based on fossil assemblages found in the coastal plain (CPRS) and western area of the state (WRS). The comparison between fossil and extant mastofaunas show that 90% of the mammals represented in fossil assemblages went extinct, and allowed distinguishing three groups: 1) taxa that underwent local extinction, i.e., disappeared locally but survived in other regions until becoming extinct later (including all megamammals); 2) pseudoextinct taxa that disappeared locally but survive until today in other areas, and 3) taxa that disappeared locally but returned during the Holocene. The faunal changes recorded along stratigraphic successions and available numerical ages indicate two phases of extinction, the first around 30 ka b2k in the CPRS (apparently also recorded in Argentina and Uruguay) would have been related to the onset of the cold and dry conditions of the stadial MIS 2, predating the arrival of humans to the region by about 25 kyrs. The second phase eliminated taxa that survived until about 12.7 ka BP in WRS in reduced suitable environments ('refugia') associated with perennial rivers; it coincides with the transition from glacial to interglacial conditions, but pollen data suggest that humans may have contributed for environmental modifications through fire. The results show that the Pleistocene xenarthran-dominated mastofauna was replaced by a Holocene fauna dominated by small rodents and carnivores, and indicate that climate-driven environmental changes, also influenced by sea-level oscillations, were a major agent in the Late Pleistocene mammalian extinctions in the Brazilian Pampa. (C) 2020 Elsevier Ltd. All rights reserved.	[Lopes, Renato Pereira; Dillenburg, Sergio Rebello] Univ Fed Rio Grande do Sul, Inst Geociencias, Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil; [Pereira, Jamil Correa] Museu Coronel Tancredo Fernandes de Melo, Rua Barao Rio Branco 467, BR-96230000 Do Palmar, RS, Brazil; [Kerber, Leonardo] Museu Paraense Emilio Goeldi, Coordenacao Ciencias Terra Ecol, Belem, PA, Brazil; [Kerber, Leonardo] Univ Fed Santa Maria, Ctr Apoio Pesquisa Paleontol Quarta Colonia CAPP, Rua Maximiliano Vizzotto 598, BR-97230000 Sao Joao Do Polesine, RS, Brazil	Universidade Federal do Rio Grande do Sul; Museu Paraense Emilio Goeldi; Universidade Federal de Santa Maria (UFSM)	Lopes, RP (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil.	paleonto_furg@yahoo.com.br; jamilpereira2168@gmail.com; leonardokerber@gmail.com; sergio.dillenburg@ufrgs.br	Kerber, Leonardo/O-3980-2017; Lopes, Renato Pereira/AFQ-4934-2022; Dillenburg, Sergio/C-4027-2013	Kerber, Leonardo/0000-0001-8139-1493; Lopes, Renato Pereira/0000-0002-4865-6426; Dillenburg, Sergio/0000-0003-0072-7018	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [150153/2014-7, 305393/2017-0]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to thank Dr. Jairo Savian (Universidade Federal do Rio Grande do Sul) for providing two of the OSL datings mentioned in the text. This research was funded by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) through the Postdoctoral Research Grant no. 150153/2014-7 to R.P. Lopes, and Research Fellowship no. 305393/2017-0 to S.R. Dillenburg.	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Sci. Rev.	AUG 15	2020	242								106428	10.1016/j.quascirev.2020.106428	http://dx.doi.org/10.1016/j.quascirev.2020.106428			23	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Physical Geography; Geology	MX7II					2023-06-23	WOS:000557893900017
J	Pinheiro, AP; Saraiva, AAF; Santana, W; Sayao, JM; Figueiredo, RG; Rodrigues, T; Weinschutz, LC; Ponciano, LCMD; Kellner, AWA				Pinheiro, Allysson P.; Feitosa Saraiva, Antonio Alamo; Santana, William; Sayao, Juliana Manso; Figueiredo, Rodrigo Giesta; Rodrigues, Taissa; Weinschutz, Luiz Carlos; Martins de Oliveira Ponciano, Luiza Corral; Armin Kellner, Alexander Wilhelm			New Antarctic clawed lobster species (Crustacea: Decapoda: Nephropidae) from the Upper Cretaceous of James Ross Island	POLAR RESEARCH			English	Article						Astacidea; Hoploparia; Metanephrops; Nephropoidea; Marambio Group	PALEOENVIRONMENTAL CHANGES; SEYMOUR ISLAND; FOSSIL RECORD; HOPLOPARIA; STRATIGRAPHY; EVOLUTION; BASIN; PALEOCENE; DIVERSITY; PATTERNS	A new species of nephropid lobster, Hoploparia echinata sp. nov., from the James Ross Island in the Antarctic Peninsula is here described and illustrated. The material was collected in the Santa Marta Formation (Santonian-Campanian), the basal unit of the Marambio Group, Larsen Basin, located in the western portion of the Antarctic Peninsula. Hoploparia echinata sp. nov. can easily be differentiated from its congeners by the presence of distinct short spines on dorsal and ventral margins on the third maxillipeds, merus of the chelipeds and pereopods; these are the characters not described in other Hoploparia species so far.	[Pinheiro, Allysson P.; Santana, William] Univ Reg Cariri, Lab Crustaceos Semiarido, Crato, CE, Brazil; [Pinheiro, Allysson P.; Feitosa Saraiva, Antonio Alamo; Santana, William] Univ Sagrado Coracao, Lab Systemat Zool, Proreitoria Pesquisa Posgrad, Rua Irma Arminda 10-50, BR-17011160 Bauru, SP, Brazil; [Feitosa Saraiva, Antonio Alamo] Univ Reg Cariri, Lab Paleontol, Crato, CE, Brazil; [Sayao, Juliana Manso] Univ Fed Rio de Janeiro, Museu Nacl, Lab Paleobiol & Paleogeog Antartica, Rio De Janeiro, RJ, Brazil; [Figueiredo, Rodrigo Giesta] Univ Fed Espirito Santo, Dept Biol, Alegre, ES, Brazil; [Rodrigues, Taissa] Univ Fed Espirito Santo, Ctr Ciencias Humanas & Nat, Dept Ciencias Biol, Lab Paleontol, Vitoria, ES, Brazil; [Weinschutz, Luiz Carlos] Univ Contestado, Ctr Paleontol, Mafra, SC, Brazil; [Martins de Oliveira Ponciano, Luiza Corral] Univ Fed Estado Rio de Janeiro, Dept Ciencias Nat, Lab Tafon & Paleoecol Aplicadas, Rio De Janeiro, Brazil; [Armin Kellner, Alexander Wilhelm] Univ Fed Rio de Janeiro, Lab Systemat & Taphon Fossil Vertebrates, Dept Geol & Paleontol, Museu Nacl, Rio De Janeiro, RJ, Brazil	Universidade Regional do Cariri; Universidade do Sagrado Coracao; Universidade Regional do Cariri; Universidade Federal do Rio de Janeiro; Universidade Federal do Espirito Santo; Universidade Federal do Espirito Santo; Universidade do Contestado; Universidade Federal do Estado do Rio de Janeiro; Universidade Federal do Rio de Janeiro	Santana, W (autor correspondente), Univ Sagrado Coracao, Lab Systemat Zool, Proreitoria Pesquisa Posgrad, Rua Irma Arminda 10-50, BR-17011160 Bauru, SP, Brazil.	willsantana@gmail.com	Saraiva, António/HPD-3031-2023; Kellner, Alexander/ABE-9591-2020; Rodrigues, Taissa/H-1220-2012; Pinheiro, Allysson/A-8726-2010; Saraiva, Antonio/K-6211-2015; Santana, William/A-4611-2008	Kellner, Alexander/0000-0001-7174-9447; Rodrigues, Taissa/0000-0001-7918-1358; Pinheiro, Allysson/0000-0003-1565-6371; Sayao, juliana/0000-0002-3619-0323; Saraiva, Antonio/0000-0003-0127-8912; Santana, William/0000-0003-3086-4419	PROANTAR (CNPq) [407670/2013-442677/2018-9]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [420687/2016-5-313461/2018-0, 312360/2018-5, 311715/2017-6]; Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [E-26/202.905/2018]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, Brasil [001, 88887.169169/2018-00, 775705/2012]	PROANTAR (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, Brasil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was supported by PROANTAR (CNPq no. 407670/2013-442677/2018-9 to AWAK), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq no. 420687/2016-5-313461/2018-0 to AWAK; no. 312360/2018-5 to TR; no. 311715/2017-6 to JMS), Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ no. E-26/202.905/2018 to AWAK) and Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, Brasil, finance code 001 (fellowship no. 88887.169169/2018-00 to WS and grant Proequipamentos no. 775705/2012 to APP).	AGUIRREURRETA MB, 1991, J PALEONTOL, V65, P795, DOI 10.1017/S0022336000037781; Kellner AWA, 2011, POLAR RES, V30, DOI 10.3402/polar.v30i0.7265; Ball H.W., 1960, UPPER CRETACEOUS DEC; Carvalho MD, 2013, SEDIMENT GEOL, V295, P53, DOI 10.1016/j.sedgeo.2013.08.002; Clarke A, 2004, ANTARCT SCI, V16, P559, DOI 10.1017/S0954102004002329; Crame J.A., 1989, Geological Society Special Publication, P1; Crame JA, 1996, J GEOL SOC LONDON, V153, P503, DOI 10.1144/gsjgs.153.4.0503; Crame JA, 1999, J GEOL SOC LONDON, V156, P957, DOI 10.1144/gsjgs.156.5.0957; Crame JA, 2004, CRETACEOUS RES, V25, P411, DOI 10.1016/j.cretres.2004.02.002; CRAME JA, 1991, J GEOL SOC LONDON, V148, P1125, DOI 10.1144/gsjgs.148.6.1125; Daley AC, 2016, ARTHROPOD STRUCT DEV, V45, P71, DOI 10.1016/j.asd.2015.09.004; Dana JD, 1852, P ACAD NAT SCI PHILA, V6, P6; El-Shazly S, 2015, J AFR EARTH SCI, V112, P299, DOI 10.1016/j.jafrearsci.2015.09.014; Feldman R.M., 1990, Antarctic Journal of the United States, V25, P45; Feldmann R.M., 1989, GEOLOGICAL SOC SPECI, V47, P183, DOI DOI 10.1144/GSL.SP.1989.047.01.14; FELDMANN RM, 1989, J PALEONTOL, V63, P64, DOI 10.1017/S0022336000040968; FELDMANN RM, 1987, J PALEONTOL, V61, P1194, DOI 10.1017/S0022336000029565; Feldmann RM, 1998, PALAEONTOLOGY, V41, P807; FELDMANN RM, 1993, PALEONTOLOGICAL SOC, V28, P1, DOI DOI 10.1017/S0022336000062077; Hathway B, 2000, J GEOL SOC LONDON, V157, P417, DOI 10.1144/jgs.157.2.417; Hathway B, 2001, ANTARCT SCI, V13, P67, DOI 10.1017/S0954102001000104; Holthuis L.B., 1991, FAO SPECIES CATALOG, V13; HOLTHUIS LB, 1974, B MAR SCI, V24, P723; Kellner A., 2019, CIENC CULT, V71, P4, DOI [10.21800/2317-66602019000300001, DOI 10.21800/2317-66602019000300001]; Kellner AWA, 2019, AN ACAD BRAS CIENC, V91, DOI 10.1590/0001-3765201920191300; Kellner AWA, 1996, J VERTEBR PALEONTOL, V16, P718, DOI 10.1080/02724634.1996.10011360; Latreille P. 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AUG 13	2020	39								3727	10.33265/polar.v39.3727	http://dx.doi.org/10.33265/polar.v39.3727			9	Ecology; Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Oceanography	NA6WT		gold			2023-06-23	WOS:000559959700001
J	Silva, RF; Dal Olmo-Barbosa, L; Koester, E; Vieira, DT				Silva, Rafael F.; Dal Olmo-Barbosa, Laercio; Koester, Edinei; Vieira, Daniel T.			Capaodo Leao Granite: Highly differentiated garnet-bearing magmatism in the southeastern Dom Feliciano Belt, Brazil	GEOLOGICAL JOURNAL			English	Article						garnet-bearing granite; highly differentiated felsic magmatism; Pelotas Batholith	A-TYPE GRANITES; DE-LA-PLATA; ALKALINE VOLCANIC-ROCKS; S-TYPE GRANITES; I-TYPE GRANITES; CALC-ALKALINE; U-PB; SOUTHERN BRAZIL; GEOCHEMICAL CLASSIFICATION; FRACTIONATED GRANITES	The Capao do Leao Granite (CLG; 583 +/- 3 Ma) occurs as two NE-oriented bodies, near the namesake city and Pedro Osorio, Rio Grande do Sul, Brazil. The CLG is linked to the voluminous Ediacaran magmatism in the SE Dom Feliciano Belt (Pelotas Batholith), intruded in post-collisional settings in the set of the non-deformed younger plutons in the area. This work presents field characterization, petrography, mineral chemistry and whole-rock geochemical affinities for the CLG. This granite exhibits miarolitic cavities, suggesting an epizonal emplacement, as well as mafic enclaves, which may represent source material, while mylonitic and S-C foliations are localized and post-magmatic. The analysed samples are massive, leucocratic, coarse- to medium-grained hypidiomorphic alkali-feldspar granites composed of quartz, orthoclase (Or(89-98)), albite (An(1-10)), oligoclase (An(11-16)), garnet (Sps(31-64)and Alm(24-56)), siderophyllite/annite, muscovite and Fe-chlorite (secondary), apatite, epidote/zoisite, zircon, and opaques. The dispersion in mineral compositions in each occurrence and between them suggest different magmatic evolutionary trends. The diverse textures, zoning patterns and chemistry in garnet indicate both equilibrium with highly evolved Al2O3-rich liquids, as well as a xenocrystic/restitic origin. The geochemistry shows subalkaline, high-K, and metaluminous to weakly peraluminous fingerprints. Samples are commonly enriched in Rb, Th, U, Pb, Nd, and Sm, and depleted in Ba, Sr, Eu, Nb, P, Zr and Ti, due to advanced fractional crystallization. The classification of the CLG into some traditional chemical patterns is difficult, due to the high differentiation and the overlap of petrologic processes, although its derivation from I-type liquids is proposed. The dispersion both in mineral and whole-rock chemistry indicates different evolutionary trends for the CLG, where fractionation coupled with crustal recycling by assimilation/contamination processes were responsible for the granite differentiation.	[Silva, Rafael F.; Dal Olmo-Barbosa, Laercio; Vieira, Daniel T.] Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias, Dept Geol, Programa Posgrad Geociencias, Ave Bento Goncalves 9500,Predio 43126,Sala 208a, BR-91540000 Porto Alegre, RS, Brazil; [Koester, Edinei] Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias, Dept Geol, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Dal Olmo-Barbosa, L (autor correspondente), Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias, Dept Geol, Programa Posgrad Geociencias, Ave Bento Goncalves 9500,Predio 43126,Sala 208a, BR-91540000 Porto Alegre, RS, Brazil.	dal.barbosa@ufrgs.br	Koester, Edinei/L-3684-2017	Koester, Edinei/0000-0002-4424-4782; Fernandes e Silva, Rafael/0000-0002-6217-8520; Dal Olmo-Barbosa, Laercio/0000-0002-2732-8634	FAPERGS; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [140461/2016-7, 141335/2017-3]	FAPERGS(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank the Institute of Geosciences (UFRGS) for technical and infrastructure support. We also thank FAPERGS and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for financial support and Ph.D. Scholarships process no 140461/2016-7 (Vieira, D.T.) and 141335/2017-3 (Dal Olmo-Barbosa, L.), as well as the careful revision and improvement in the text by the anonymous reviewers.	[Anonymous], [No title captured]; Arndt NT, 2013, GEOCHEM PERSPECT, V2, P405, DOI 10.7185/geochempersp.2.3; Arth J.G., 1988, AM J SCI A, V288-A, P461; Babinski M, 1997, J S AM EARTH SCI, V10, P263, DOI 10.1016/S0895-9811(97)00021-7; Bach P, 2012, J PETROL, V53, P1169, DOI 10.1093/petrology/egs012; Barbarin B, 1999, LITHOS, V46, P605, DOI 10.1016/S0024-4937(98)00085-1; Barboni M, 2013, LITHOS, V177, P328, DOI 10.1016/j.lithos.2013.07.005; Barnes CG, 2006, GEOL SOC AM SPEC PAP, V410, P269, DOI 10.1130/2006.2410(13); Basei M. A. 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J.	JAN	2021	56	1					79	101		10.1002/gj.3941	http://dx.doi.org/10.1002/gj.3941		AUG 2020	23	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	PR5TT					2023-06-23	WOS:000559385000001
J	Almeida, JS; Meira, LA; Oliveira, MS; Teixeira, LSG				Almeida, Jorge S.; Meira, Lucilia A.; Oliveira, Maiara S.; Teixeira, Leonardo S. G.			Direct multielement determination of Cd, Pb, Fe, and Mn in ground coffee samples using energy dispersive X-ray fluorescence spectrometry	X-RAY SPECTROMETRY			English	Article							GREEN COFFEE; BRAZILIAN COFFEES; ROASTED COFFEE; COCOA POWDER; PRECONCENTRATION; VARIETIES; METALS; RESOLUTION; NUTRIENTS; MANGANESE	An analytical method was proposed for the quantification of Cd, Pb, Mn, and Fe in ground coffee samples using energy dispersive X-ray fluorescence (EDXRF) spectrometry. External calibration was possible using the coffee matrix itself as standards with samples previously analyzed by inductively coupled plasma optical emission spectrometry (ICP OES). The ground coffee samples were analyzed in the form of pellets, which were placed in the center of the EDXRF measuring cell for the determination of the analytes. The limits of detection were 62, 55, 86, and 76 mu g/kg for Cd, Pb, Fe, and Mn, respectively. Good linearities were obtained for the calibration curves with coefficients of correlation (R) of 0.9959 for Cd, 0.9939 for Pb, 0.9929 for Fe, and 0.9909 for Mn. Precision, evaluated as the relative standard deviation (RSD) of 10 independent measurements of different cataloged samples with an approximate concentration of 400 mu g/kg for each analyte, was between 6 and 14% (n= 10), demonstrating that the preparation of the samples in form of pellets was sufficient to perform analyses by EDXRF. The proposed method was applied in the determination of Cd, Pb, Fe, and Mn in ground coffee samples collected in Salvador, Bahia, Brazil. In a parallel comparative procedure, coffee samples were also analyzed by ICP OES after sample pretreatment by acid digestion. A paired Student'sttest was carried out (confidence level of 95%,n= 5) and no significant difference was observed between the concentrations obtained by the proposed and comparative methods.	[Almeida, Jorge S.; Meira, Lucilia A.; Oliveira, Maiara S.; Teixeira, Leonardo S. G.] Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Almeida, Jorge S.; Teixeira, Leonardo S. G.] Univ Fed Bahia, Inst Nacl Ciencia & Tecnol Energia Ambiente INCT, Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia	Teixeira, LSG (autor correspondente), Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.	lsgt@ufba.br	Teixeira, Leonardo S G/J-9131-2016; de Almeida, Jorge Santos/ABF-4979-2020	Teixeira, Leonardo S G/0000-0003-0320-8299; de Almeida, Jorge Santos/0000-0002-9450-1062	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior [001]; Fundacao de Amparo a Pesquisa do Estado da Bahia	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado da Bahia	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, Grant/Award Number: 001; Fundacao de Amparo a Pesquisa do Estado da Bahia	Almeida JS, 2015, SPECTROCHIM ACTA B, V107, P159, DOI 10.1016/j.sab.2015.03.002; Amorim VR, 2007, J BRAZIL CHEM SOC, V18, P47, DOI 10.1590/S0103-50532007000100005; Andrey D, 2018, SPECTROCHIM ACTA B, V148, P137, DOI 10.1016/j.sab.2018.06.014; [Anonymous], 2011, NUCL EST PESQ AL TAC; Aranda PR, 2013, X-RAY SPECTROM, V42, P100, DOI 10.1002/xrs.2440; Brazilian Coffee Industry Association, ABIC 2020; Brito GB, 2017, MICROCHEM J, V134, P35, DOI 10.1016/j.microc.2017.05.001; Castro JT, 2009, TALANTA, V78, P1378, DOI 10.1016/j.talanta.2009.02.030; Choi MY, 2010, FOOD CHEM, V121, P1260, DOI 10.1016/j.foodchem.2010.01.035; Devi PSR, 2016, X-RAY SPECTROM, V45, P162, DOI 10.1002/xrs.2682; dos Santos JS, 2010, J BRAZIL CHEM SOC, V21, P1468, DOI 10.1590/S0103-50532010000800009; dos Santos JS, 2009, FOOD CHEM, V115, P1405, DOI 10.1016/j.foodchem.2009.01.069; Downey G, 1997, J AGR FOOD CHEM, V45, P4357, DOI 10.1021/jf970337t; Esteban-Diez I, 2004, ANAL CHIM ACTA, V514, P57, DOI 10.1016/j.aca.2004.03.022; Feleke HM, 2018, IOSR J ENV SCI TOXIC, V12, P51, DOI DOI 10.9790/2402-1204015170; Fernandes AP, 2005, SPECTROCHIM ACTA B, V60, P717, DOI 10.1016/j.sab.2005.02.013; Gallardo H, 2016, J FOOD COMPOS ANAL, V50, P1, DOI 10.1016/j.jfca.2016.04.007; Gothankar SS, 2009, SCI TOTAL ENVIRON, V407, P2868, DOI 10.1016/j.scitotenv.2009.01.014; Guild GE, 2017, PLANT SOIL, V419, P457, DOI 10.1007/s11104-017-3352-4; Haswell SJ, 1998, J ANAL ATOM SPECTROM, V13, P131, DOI 10.1039/a705317g; Herreros-Chavez L, 2019, FOOD CHEM, V278, P373, DOI 10.1016/j.foodchem.2018.11.065; ICO, 2020, HIST DAT GLOB COFF T; Jenkins R, 1995, QUANTITATIVE XRAY SP; KAUR J, 2016, AIP CONF PROC, V1728; KRIVAN V, 1993, MIKROCHIM ACTA, V110, P217, DOI 10.1007/BF01245106; Leyva D, 2007, X-RAY SPECTROM, V36, P355, DOI 10.1002/xrs.983; Martin MJ, 1999, FOOD CHEM, V66, P365, DOI 10.1016/S0308-8146(99)00092-8; Martin MJ, 1998, ANAL CHIM ACTA, V358, P177, DOI 10.1016/S0003-2670(97)00610-7; Masresha Feleke H., 2018, INT J SCI ENG RES, V9, P149; Mohapatra A, 2009, FOOD CHEM TOXICOL, V47, P2730, DOI 10.1016/j.fct.2009.07.037; Noda T, 2006, FOOD CHEM, V95, P632, DOI 10.1016/j.foodchem.2005.02.002; Oleszczuk N, 2007, TALANTA, V73, P862, DOI 10.1016/j.talanta.2007.05.005; Oliveira LB, 2020, FOOD ANAL METHOD, V13, P195, DOI 10.1007/s12161-019-01565-w; Oliveira M, 2012, FOOD CHEM, V130, P702, DOI 10.1016/j.foodchem.2011.07.113; Onianwa PC, 1999, FOOD CHEM, V66, P275, DOI 10.1016/S0308-8146(98)00257-X; Otaka A, 2014, FOOD CHEM, V147, P318, DOI 10.1016/j.foodchem.2013.09.142; Paltridge NG, 2012, PLANT SOIL, V361, P261, DOI 10.1007/s11104-012-1423-0; Peruchi LC, 2014, SPECTROCHIM ACTA B, V100, P129, DOI 10.1016/j.sab.2014.08.025; Pytlakowska K, 2016, APPL SPECTROSC, V70, P1891, DOI 10.1177/0003702816644758; Pytlakowska K, 2016, FOOD ANAL METHOD, V9, P2270, DOI 10.1007/s12161-016-0412-y; Salvador MJ, 2002, X-RAY SPECTROM, V31, P141, DOI 10.1002/xrs.546; Silva S. A. da, 2017, African Journal of Agricultural Research, V12, P221, DOI 10.5897/ajar2016.11832; Suseela B, 2001, FOOD ADDIT CONTAM, V18, P115, DOI 10.1080/02652030010008814; SYAHFITRI W, 2017, J PHYS CONF SER, V860; WHO Expert Committee on Trace Elements in Human Nutrition & World Health Organization, 1973, TRAC EL HUM NUTR REP	45	6	6	2	27	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0049-8246	1097-4539		X-RAY SPECTROM	X-Ray Spectrom.	JAN	2021	50	1					2	8		10.1002/xrs.3182	http://dx.doi.org/10.1002/xrs.3182		AUG 2020	7	Spectroscopy	Science Citation Index Expanded (SCI-EXPANDED)	Spectroscopy	PB8LG					2023-06-23	WOS:000557862100001
J	Gomes, VJC; Asp, NE; Siegle, E; McLachlan, RL; Ogston, AS; Silva, AMM; Nittrouer, CA; Souza, DF				Gomes, Vando J. C.; Asp, Nils E.; Siegle, Eduardo; McLachlan, Robin L.; Ogston, Andrea S.; Silva, Ariane M. M.; Nittrouer, Charles A.; Souza, Denise F.			Connection between macrotidal estuaries along the southeastern Amazon coast and its role in coastal progradation	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Estuarine connectivity; Tidal channels; Sediment transport; Mangroves	SEDIMENT DYNAMICS; MANGROVE ESTUARY; RIVER; CHANNEL; TIDE	Sediment transport in the southeastern Amazon coastal zone (SACZ) is substantially affected by tidal asymmetry, seasonal variation of the wind and wave regime and especially rainfall (i.e., river discharge). The regional climate and geological configuration have resulted in numerous estuaries and large mangrove-covered coastal plains that partially divide the estuarine basins, which are connected by tidal channels. Based on the investigation of the Furo Grande tidal channel, we assess the relevance of connectivity on the sediment transport and evolution of the similar to 8000 km(2) SACZ mangrove belt. Extensive sedimentologic and bathymetric surveys, as well as hydrodynamic measurements including water level, water and sediment flow, and physical-chemical characteristics of the water, were undertaken at different seasonal periods. Water-level variation along the channel shows that sediment-transport convergence (STC) tends to be formed within the connecting channel, as the tide propagates from both ends. Morphologic and sedimentologic results show the accumulation trend of fine sediments within the STC zone, and this is relevant for mud retention and further delivery to the mangrove plains, which may eventually lead to channel-connection closure. Despite the STC, results also show that there is an important net flux of suspended sediments between estuaries through the studied channel. However, the connected estuaries of Taperacu and Caete have substantial differences regarding riverine discharge, and thus estuarine processes, tidal propagation and sediment transport. Bottom sediments and morphology reflect longterm trends and show STC migration towards the Taperacu as a result of substantially smaller fluvial discharge in that estuary, and therefore higher sediment accumulation rates, compared to the Caet.e estuary. The migration of the STC prevents the closure of the connection, and its maintenance preserves these channels as sediment-flow conduits between estuaries. The connectivity is a key process to redistribute mainly muddy sediments along this coastal sector, which helps to explain the evolution and maintenance of the relatively homogeneous and widespread progradation of mangroves along the SACZ, with uneven mud supply.	[Gomes, Vando J. C.; Asp, Nils E.] Univ Fed Para UFPA, Programa Posgrad Biol Ambiental PPBA, Belem, Para, Brazil; [Asp, Nils E.] Univ Fed UFPA, Inst Estudos Costeiros, IECOS, Belem, Para, Brazil; [Siegle, Eduardo] Univ Sao Paulo, Inst Oceanog, IO, Sao Paulo, SP, Brazil; [McLachlan, Robin L.; Ogston, Andrea S.; Nittrouer, Charles A.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA; [Asp, Nils E.; Silva, Ariane M. M.] Univ Fed Para UFPA, Inst Geociencias, Programa Posgrad Geol & Geoquim, Belem, Para, Brazil; [Souza, Denise F.] Univ Fed Para UFPA, Fac Ciencias Nat, Belem, Para, Brazil	Universidade Federal do Para; Universidade Federal do Para; Universidade de Sao Paulo; University of Washington; University of Washington Seattle; Universidade Federal do Para; Universidade Federal do Para	Asp, NE (autor correspondente), Univ Fed Para UFPA, Programa Posgrad Biol Ambiental PPBA, Belem, Para, Brazil.; Asp, NE (autor correspondente), Univ Fed UFPA, Inst Estudos Costeiros, IECOS, Belem, Para, Brazil.; Asp, NE (autor correspondente), Univ Fed Para UFPA, Inst Geociencias, Programa Posgrad Geol & Geoquim, Belem, Para, Brazil.	vandojcg@yahoo.com.br; nilsasp@ufpa.br; esiegle@usp.br; mclachlan.rl@gmail.com; ogston@uw.edu; ariianemarques@hotmail.com; nittroue@uw.edu; denisefreitasdesouza@gmail.com.br	Siegle, Eduardo/F-5408-2010; Asp, Nils/J-6226-2012	Siegle, Eduardo/0000-0003-3926-1710; Asp, Nils/0000-0002-6468-6158; Silva, Ariane M. M./0000-0001-9320-9046	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), via the IODP/CAPES Brasil [0553/2015, 0554/2015]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), via Pro-Amazonia program [3290/2013]; U.S. Office of Naval Research Global [N62909-14-1N205]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -CNPq [446895/2014-8]; U.S. Office of Naval Research [N00014-15-1-2011, N00014-13-1-0127, N00014-13-1-0781]; National Science Foundation Graduate Research Fellowship [DGE1256082]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), via the IODP/CAPES Brasil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), via Pro-Amazonia program(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); U.S. Office of Naval Research Global(Office of Naval Research); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); U.S. Office of Naval Research(Office of Naval Research); National Science Foundation Graduate Research Fellowship(National Science Foundation (NSF))	This study was partially funded by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), via the IODP/CAPES Brasil (0553/2015 and 0554/2015) and Pro-Amazonia (3290/2013) programs, by the U.S. Office of Naval Research Global (N62909-14-1N205), as well as by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -CNPq (446895/2014-8). Additional funds were also provided by the U.S. Office of Naval Research (N00014-15-1-2011, N00014-13-1-0127, N00014-13-1-0781) and by the National Science Foundation Graduate Research Fellowship (DGE1256082). N.E.A. and E.S. are CNPq research fellows.	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Coast. Shelf Sci.	AUG 5	2020	240								106794	10.1016/j.ecss.2020.106794	http://dx.doi.org/10.1016/j.ecss.2020.106794			14	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	LR7GY		Bronze			2023-06-23	WOS:000535863600011
J	Barreto, IS; de Albergaria-Barbosa, ACR; Patire, VF; Silva, MD; Baldassin, P; Taniguchi, S; Montone, RC; Gallo, H; Maranho, A; Bicego, MC				Barreto, Isana Souza; Rizzatti de Albergaria-Barbosa, Ana Cecilia; Patire, Vinicius Farias; Silva, Marcio de Jesus; Baldassin, Paula; Taniguchi, Satie; Montone, Rosalinda Carmela; Gallo, Hugo; Maranho, Andrea; Bicego, Marcia Caruso			Bioavailability of polycyclic aromatic hydrocarbons to penguins on the coast of southeastern Brazil	MARINE POLLUTION BULLETIN			English	Article						Biliary metabolites; Biomarkers; Spheniscus magellanicus; HPLC/F	PERSISTENT ORGANIC POLLUTANTS; JUVENILE MAGELLANIC PENGUINS; SPHENISCUS-MAGELLANICUS; SAO-PAULO; METABOLITES; FISH; SEDIMENTS; PAHS; BILE; SEABIRDS	Bioavailability of polycyclic aromatic hydrocarbons on Sao Paulo state coast (southeastern Brazil) was evaluated through the analysis of biliary metabolites in Spheniscus magellanicus (n = 79). The animals analyzed in present study were either found dead during beach monitoring procedures or died at rehabilitation centers. Analyses of naphthalene (NAP), phenanthrene (PHE) and benzo[a]pyrene (BaP) metabolites were performed using a high-performance liquid chromatograph equipped with fluorescence detectors. Total metabolite (TM) concentrations ranged from below the method quantification limit to 270 mu g g(-1) of bile. TM concentrations were mainly composed of NAP metabolites, followed by PHE metabolites. BaP metabolites were detected in only two samples. This is the first study using PAHs metabolites in S. magellanicus to assess the bioavailability of these compounds in coastal regions.	[Barreto, Isana Souza; Rizzatti de Albergaria-Barbosa, Ana Cecilia; Silva, Marcio de Jesus] Univ Fed Bahia, Geosci Inst, Lab Oil Studies, Rua Barao Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil; [Rizzatti de Albergaria-Barbosa, Ana Cecilia] Univ Fed Bahia, Geosci Inst, Lab Marine Geochem, Rua Barao Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil; [Rizzatti de Albergaria-Barbosa, Ana Cecilia; Patire, Vinicius Farias; Baldassin, Paula; Taniguchi, Satie; Montone, Rosalinda Carmela; Bicego, Marcia Caruso] Univ Sao Paulo, Oceanog Inst, Lab Marine Organ Chem, Praca Oceanog 191, BR-05508900 Sao Paulo, SP, Brazil; [Patire, Vinicius Farias] Univ Fed Bahia, Interdisciplinary Ctr Energy & Environm, Rua Barao Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil; [Baldassin, Paula] BW Consultoria Vet, Rua Prof Suely Brasil Flores 88, BR-28970000 Ararucuna, RJ, Brazil; [Gallo, Hugo] Inst Argonauta Conservacao Costeira & Marinha, Rua Guarani 835, BR-11680000 Ubatuba, SP, Brazil; [Gallo, Hugo] Aquario Ubatuba, Rua Guarani 859, BR-1680000 Ubatuba, SP, Brazil; [Maranho, Andrea] Inst Gremar Pesquisa Educ & Gestao Fauna, Rua Joao Ruiz 799, BR-11420350 Guaruja, SP, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade de Sao Paulo; Universidade Federal da Bahia	Barreto, IS; de Albergaria-Barbosa, ACR (autor correspondente), Univ Fed Bahia, Geosci Inst, Lab Oil Studies, Rua Barao Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil.	isanabarreto@hotmail.com; cecilia.albergaria@ufba.br; rmontone@usp.br; hugo@aquariodeubatuba.com.br	de Albergaria-Barbosa, Ana Cecília/AAC-6940-2021; Montone, Rosalinda C/J-9110-2012; de+Albergaria+Barbosa, Ana/AAQ-3872-2020; Taniguchi, Satie/D-2552-2013; Bicego, Marcia C/D-1996-2013	Montone, Rosalinda C/0000-0002-9586-1000; Taniguchi, Satie/0000-0002-6825-6390; Albergaria-Barbosa, Ana Cecilia R./0000-0003-2121-9792; Faria Patire, Vinicius/0000-0002-7786-8241	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES [Coordination for the Advancement of Higher Education Personnel]) [001]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP [State of Sao Paulo Research Assistance Foundation] Grants) [2005/03801-8, 2012/10323-9, 2010/07227-2]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq [National Council of Scientific and Technological Development]); CAPES; FAPESP	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES [Coordination for the Advancement of Higher Education Personnel])(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP [State of Sao Paulo Research Assistance Foundation] Grants)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq [National Council of Scientific and Technological Development])(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	This work was developed by graduate students of the discipline GEOC53 "Aquatic Contamination Biomarkers" offered by the Graduate Program in Geochemistry: Petroleum and Environment (POSPETRO) of the Federal University of Bahia (UFBA) in partnership with the graduate programs in Energy and Environment (PPGEnAM) of UFBA and in Oceanography of the University of Sao Paulo (USP). These graduate programs are supported by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES [Coordination for the Advancement of Higher Education Personnel] -finance code 001). The fund used in the analytical instruments and analysis was provided by Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP [State of Sao Paulo Research Assistance Foundation] Grants 2005/03801-8, 2012/10323-9 and 2010/07227-2). Albergaria-Barbosa, Patire, Silva, Baldassin and Barretos thank Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq [National Council of Scientific and Technological Development]), CAPES and FAPESP for their graduation scholarships. Albergaria-Barbosa, Bicego and Montone thanks CNPq for their research grants. All authors thanks the rehabilitation centers that provided the samples and the authors also thank the anonymous reviewer for the constructive suggestions and comments that improved the manuscript.	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Pollut. Bull.	AUG	2020	157								111306	10.1016/j.marpolbul.2020.111306	http://dx.doi.org/10.1016/j.marpolbul.2020.111306			5	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	MK1FD	32658674				2023-06-23	WOS:000548531100010
J	Bicca, MM; Kalkreuth, W; da Silva, TF; de Oliveira, CHE; Genezini, FA				Bicca, Marcos Mueller; Kalkreuth, Wolfgang; da Silva, Tais Freitas; Engelmann de Oliveira, Christie Helouise; Genezini, Frederico Antonio			Thermal and depositional history of Early-Permian Rio Bonito Formation of southern Parana Basin - Brazil	INTERNATIONAL JOURNAL OF COAL GEOLOGY			English	Article						Parana Basin; Vitrinite reflectance; Apatite Thermochronology; Burial history	COAL-BEARING STRATA; FISSION-TRACK ANALYSIS; U-PB; TECTONIC CONTROL; SANTA-TEREZINHA; IRATI SHALE; LEAO-BUTIA; APATITE; COALFIELD; SEAMS	The Parana Basin is a large volcano-sedimentary basin with a complex depositional history from Ordovician to the Cretaceous period. During Permian significant amounts of organic-rich beds accumulated within the Rio Bonito and Irati formations representing deposition in coastal (deltaic and barrier lagoon) and shallow marine environments, respectively. In this work, the thermal history of these beds is examined from 16 vitrinite reflectance analyses of coal beds (Rio Bonito Formation), integrated with previous data on coal rank, and 21 apatite fission-track (AFT) analyses, collected from 17 well profiles in the south of the Parana Basin. Coal samples showed three different maturity levels. Two with reflectances of 0.4-0.6 and 0.6-0.8%Rr formed by the natural burial history of the basin (the latter is restricted to the Torres Syncline area). In contrast, the third group reached much higher values (1.0-5.0%Rr) related to intrusive igneous rocks. The AFT data show thermal consistency with the reflectance values. The sandstone samples related to the two lower reflectance patterns were partially reset, preserving AFT ages older than the stratigraphic age of the bed. Otherwise, the samples severely affected by the magmatism have Cretaceous and Early Cenozoic ages, but some were much younger than the last magmatic event, implying deep burial before cooling onset. The mean track length distribution of the partially reset samples is short due to the inheritance of tracks preserved from basement cooling history. However, the population of fully reset samples gives crucial information on the maximum temperature reached and the age when cooling started. At these conditions, around 1.0 to 3.0 km of the Parana Basin sequences would have been removed from the surface of the studied areas by erosion since Cretaceous. Regional variations in the amounts of removed sections were controlled by the structural framework, mostly regional NW-SE and NE-SW oriented structures.	[Bicca, Marcos Mueller; Kalkreuth, Wolfgang; da Silva, Tais Freitas] Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil; [Engelmann de Oliveira, Christie Helouise] Univ Vale Rio dos Sinos, Sao Leopoldo, RS, Brazil; [Genezini, Frederico Antonio] Univ Sao Paulo, Inst Pesquisas Energet & Nucl, Sao Paulo, Brazil	Universidade Federal do Rio Grande do Sul; Universidade do Vale do Rio dos Sinos (Unisinos); Comissao Nacional de Energia Nuclear (CNEN); Instituto de Pesquisas Energeticas e Nucleares (IPEN); Universidade de Sao Paulo	Bicca, MM (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil.	marcos.bicca@ufrgs.br	Silva, Tais Freitas/Q-2914-2018; Engelmann de Oliveira, Christie Helouise/N-8540-2018	Silva, Tais Freitas/0000-0003-1541-0902; Engelmann de Oliveira, Christie Helouise/0000-0002-8320-9410	National Council for Scientific and Technological Development (CNPq) of Brazil [150550_2017-0]; CNPq Research Grant	National Council for Scientific and Technological Development (CNPq) of Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq Research Grant(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF))	This study is part of the first author's postdoctoral project developed at the Institute of Geosciences of the Federal University of Rio Grande do Sul. We thank the National Council for Scientific and Technological Development (CNPq) of Brazil for financial support for the junior postdoctoral fellowship (150550_2017-0) of the first author and to a CNPq Research Grant for W. Kalkreuth. We also thank the Carbonifera do Cambui, Copelmi and Rio Deserto mining companies for the availability of sample collection and logistical support.	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M., 2004, CARTA GEOLOGICA BRAS; Philipp RP, 2018, J S AM EARTH SCI, V88, P216, DOI 10.1016/j.jsames.2018.08.018; Sachs L.L.B., 2004, CARTA GEOLOGICA BRAS; Saghafi A, 2008, INT J COAL GEOL, V73, P74, DOI 10.1016/j.coal.2007.05.003; Santos RV, 2006, GONDWANA RES, V9, P456, DOI 10.1016/j.gr.2005.12.001; Silva MB, 2008, INT J COAL GEOL, V73, P331, DOI 10.1016/j.coal.2007.08.002; Simas MW, 2012, J S AM EARTH SCI, V39, P1, DOI 10.1016/j.jsames.2012.06.001; Ting F. T. C., 1978, ANAL METHODS COAL CO, V1, P3; Vermeesch P, 2018, GEOSCI FRONT, V9, P1479, DOI 10.1016/j.gsf.2018.04.001; Wagner G A, 1992, FISSION TRACK DATING, P285, DOI DOI 10.1007/978-94-011-2478-2; WAPLES DW, 1980, AAPG BULL, V64, P916; Zerfass H, 2005, GONDWANA RES, V8, P163, DOI 10.1016/S1342-937X(05)71115-1; Zerfass H, 2004, SEDIMENT GEOL, V166, P265, DOI 10.1016/j.sedgeo.2003.12.008	71	5	5	0	3	ELSEVIER	AMSTERDAM	RADARWEG 29a, 1043 NX AMSTERDAM, NETHERLANDS	0166-5162	1872-7840		INT J COAL GEOL	Int. J. Coal Geol.	AUG 1	2020	228								103554	10.1016/j.coal.2020.103554	http://dx.doi.org/10.1016/j.coal.2020.103554			22	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Geology	PP1GY					2023-06-23	WOS:000605618200004
J	Brito, AD; Soares, JL; de Lima, SG; Nogueira, ACR; Romero, GR; Sousa, ED				Brito, Ailton da Silva; Soares, Joelson Lima; de Lima, Sidney Goncalo; Rodrigues Nogueira, Afonso Cesar; Romero, Guilherme Raffaeli; Sousa, Edymilais da Silva			Postglacial transgressive shales of Upper Devonian-Lower Carboniferous boundary of the Parnaiba Basin	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Organic geochemistry; Biomarkers; Kerogen; Sedimentary facies	HUMMOCKY CROSS-STRATIFICATION; SERGIPE-ALAGOAS BASIN; ROCK-EVAL PYROLYSIS; ORGANIC-MATTER; CRUDE OILS; ISOTOPE CHARACTERISTICS; MOLECULAR FOSSILS; WESTERN ARGENTINA; TOARCIAN SHALES; COMBINED-FLOW	Upper Devonian-Lower Carboniferous deposits in north Brazil show a postglacial transgressive event characterized by the formation of thick layers of gray to black shales. In the Parnaiba Basin, the shales of the Longa Formation overlap the Upper Famennian non-marine glacial deposits of the Cabecas Formation marked by a ravinement surface. The Longa shales exhibit wavy-lenticular beddings in their base, grading to gray-black shales locally interbedded with thin layers of sandstones with hummocky cross-stratification and megaripple bedding. These deposits were interpreted as having formed in shallow marine upper offshore to lower shoreface with episodic storm events. The organic matter analysis of the outcropping Longa shales using Total Organic Carbon (TOC), Rock-Eval pyrolysis, and biomarkers provide several geochemical parameters for the interpretation of the paleoenvironment, the origin of the organic matter and its thermal maturation. The Longa shales presented low TOC contents (less than 1%), very low numbers of free hydrocarbons (S1), and potential generators (S2). The maximum pyrolysis temperature (Tmax), as well as the thermal maturation biomarker parameters, indicate that the Longa shales are immature. The values of pristane/n-C-17, phytane/n-C-18, Hydrogen Index (HI) and Oxygen Index (OI) suggest kerogen types III and IV, which are formed from conical land leaves, needles, and plant waxes; this interpretation is also supported by total sulfur (TS) < 0.2 wt%, terrigenous/aquatic ratio (TAR), C-29-sterol, hopane/sterane and Methylphenanthrene (MPs). This organic matter was deposited in an epeiric sea with shallow water, oxidizing conditions, normal salinity, and low temperatures prevalence.	[Brito, Ailton da Silva; Soares, Joelson Lima; Rodrigues Nogueira, Afonso Cesar; Romero, Guilherme Raffaeli] Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim PPGG, Belem, PA, Brazil; [de Lima, Sidney Goncalo; Sousa, Edymilais da Silva] Univ Fed Piaui, Lab Geoquim Organ, Teresina, PI, Brazil	Universidade Federal do Para; Universidade Federal do Piaui	Brito, AD (autor correspondente), Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim PPGG, Belem, PA, Brazil.	asbrito@ufpa.br	de Lima, Sidney Gonçalo/J-5555-2019	de Lima, Sidney Gonçalo/0000-0001-8754-1499; Raffaeli Romero, Guilherme/0000-0001-9955-0878; NOGUEIRA, AFONSO/0000-0002-5225-9255; Brito, Ailton/0000-0001-9224-5563	National Council for Scientific and Technological Development (CNPq) [CNPq-132178/2015-0]	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the National Council for Scientific and Technological Development (CNPq) for their scholarships (CNPq-132178/2015-0) and financial support, Pro-Reitoria de Pesquisa e PosGraduacao (PROPESP/UFPA) for linguistic revision support, and Programa de Pos-Graduacao em Geologia e Geoquimica-PPGG of the Federal University of Para (UFPa). 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J	Conti, LA; da Mota, GT; Barcellos, RL				Conti, Luis Americo; da Mota, Giulia Torres; Barcellos, Roberto Lima			High-resolution optical remote sensing for coastal benthic habitat mapping: A case study of the Suape Estuarine-Bay, Pernambuco, Brazil	OCEAN & COASTAL MANAGEMENT			English	Article						Benthic habitats; Estuary; Bay; Port; WorldView-2; Benthic terrain modeler	WATER DEPTH; SUBLITTORAL HABITATS; SATELLITE IMAGERY; TROPICAL ESTUARY; CORAL-REEFS; CLASSIFICATION; BATHYMETRY; WORLDVIEW-2; HYDROCARBONS; SEDIMENTS	The benefits of high resolution remote sensing techniques and data for the mapping of coastal environments include their ability to capture the spatial variability of the rich and diverse sedimentary landforms and habitats of coastal systems as well as gather and manage different types of data and information using the same platform for multi-scale and multi-layer analysis. This work analyses the efficacy of high resolution satellite imagery for mapping benthic habitat and the seascape characteristics of a coastal lagoon (Suape Bay - 40 km south of Recife, Pernambuco, Brazil) subjected to high anthropogenic impact and exposed to different conditions of tides, suspended sediment regime, and wave dynamics, using different types of processing and classification methods. We analyzed two World View 2 images acquired in 2010 and 2015 in similar tidal conditions and low water turbidity. Preprocessing included the application of radiometric and atmospheric correction, sunglint removal, and land/sea areas masking. To extract the depth information, a Band Ratio and Simple Radiative Transfer Model were employed. The model was corrected and calibrated by using a set of 150 control points collected by echo sounding surveying. A benthic terrain model was developed to identify and map topographic features at broad and fine scales. Supervised Pixel and Object-Based classification methods were applied to visible bands of WV2 and bathymetric data to produce benthic habitat maps of the lagoon area. The analyses were validated by ground truthing based on bottom sediment sampling, underwater photographs, and side scan sonar surveys.	[Conti, Luis Americo; da Mota, Giulia Torres] Univ Sao Paulo, Escola Artes Ciencias & Humanidades Each, Av Arlindo Bettio 100, Sao Paulo, SP, Brazil; [Barcellos, Roberto Lima] Univ Fed Pernambuco, Dept Oceanog, Av Arquitetura S-N,Cidade Univ, BR-50740540 Recife, PE, Brazil	Universidade de Sao Paulo; Universidade Federal de Pernambuco	Conti, LA (autor correspondente), Univ Sao Paulo, Escola Artes Ciencias & Humanidades Each, Av Arlindo Bettio 100, Sao Paulo, SP, Brazil.	lconti@usp.br	Barcellos, Roberto/AAH-3829-2020	Barcellos, Roberto/0000-0003-1304-4603; /0000-0002-9507-3565	FACEPE - Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco, Brazil [APQ 0260-1.08/15]; FAPESP - Fundacao de Amparo a Pesquisa do Estado de Sao Paulo, Brazil [2015/18011-4, 2017/11669-0]	FACEPE - Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco, Brazil; FAPESP - Fundacao de Amparo a Pesquisa do Estado de Sao Paulo, Brazil(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	FACEPE - Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco, Brazil (Grant APQ 0260-1.08/15) and FAPESP - Fundacao de Amparo a Pesquisa do Estado de Sao Paulo, Brazil (Grants 2015/18011-4 and 2017/11669-0).	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AUG 1	2020	193								105205	10.1016/j.ocecoaman.2020.105205	http://dx.doi.org/10.1016/j.ocecoaman.2020.105205			14	Oceanography; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography; Water Resources	MA2JD					2023-06-23	WOS:000541741600002
J	Costa, NO; Botelho, NF; Garnier, J				Costa, N. O.; Botelho, N. F.; Garnier, J.			Concentration of rare earth elements in the Faixa Placha tin deposit, Pedra Branca A-Type Granitic Massif, central Brazil, and its potential for ion-adsorption-type REE-Y mineralization	ORE GEOLOGY REVIEWS			English	Article						REE-Y; Ion-adsorption; Tin deposit; Pedra Branca Granitic Massif; Brazil	MINERALOGICAL CHARACTERISTICS; GEOCHEMICAL CHARACTERISTICS; FRACTIONATION; DISCRIMINATION; OCCURRENCES; EXTRACTION; MOBILITY; CE(III); CERIUM; SERRA	The Goias Tin Province (GTP) in Brazil has great potential for rare earth elements (REE) deposits associated with A-type granites, such as the Pedra Branca Massif, which contains several Sn deposits and REE anomalies, hosted in its cupola and fracture greisens. The Faixa Placha is the most important fin deposit in the Pedra Branca Massif and has high REE-Y concentrations, both in the Sn ore and parent biotite granite, as well as greisenized granites and greisens, with the potential to be economically used as a byproduct of fin. The values exceed 1000 ppm in light rare earth elements (LREEs) and 500 ppm in heavy rare earth elements (HREEs) + Y in the parent granite. REE concentrations in greisenized granites and greisens are similar to that of the parent granite, indicating that the enrichment in REE is due to the presence of REE-bearing primary minerals and that greisenization did not affect the original magmatic primary REE content. The REE-bearing minerals in the parent granite are allanite, monazite, xenotime, thorite, apatite, and zircon. These minerals, except zircon, are altered to secondary monazite, silicates, fluorcarbonates, and oxyfluorides, which are responsible for the concentration of REE in greisenized granites and greisens and the availability of these metals for the clay fraction of saprolites and soils. Ion exchange analyses in the saprolites and soils of a Faixa Placha profile show that the extractions in the clay fraction are more enriched in REE-Y compared to the whole soil extractions, with values between 3425 and 36,762 ppm and between 2804 and 21,689 ppm, respectively. The REEs are more enriched in the basal part of the profile, especially the LREEs. These exchangeable REE-Y concentrations indicate the potential of the Faixa Placha and nearby areas to constitute an important REE-Y deposit of the ion-adsorption-type.	[Costa, N. O.; Botelho, N. F.; Garnier, J.] Univ Brasilia, Inst Geosci, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia	Botelho, NF (autor correspondente), Univ Brasilia, Inst Geosci, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil.	nilsonfb@unb.br	Botelho, Nilson Francisquini/T-9470-2017; garnier, jeremie/AAK-8470-2021	Botelho, Nilson Francisquini/0000-0001-9090-799X; garnier, jeremie/0000-0001-9571-7933	Brazilian National Council for Scientific and Technological Development (CNPq) [405839/2013-8, 311203/2014-0]; CAPES scholarship	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES scholarship(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work was possible thanks to financial support from the Brazilian National Council for Scientific and Technological Development (CNPq) under grants 405839/2013-8 and 311203/2014-0 and CAPES scholarship to NOC. Special thanks are offered to Prof. Valmir da Silva Souza and undergraduate student Gisele Rodrigues Gondin for their assistance in the fieldwork. We are also grateful to the Geosciences Institute of the University of Brasilia for the access to all laboratorial facilities.	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Rev.	AUG	2020	123								103606	10.1016/j.oregeorev.2020.103606	http://dx.doi.org/10.1016/j.oregeorev.2020.103606			16	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	LY0EE					2023-06-23	WOS:000540196600003
J	da Conceicao, DM; Iannuzzi, R; de Andrade, LS; Esperanca, MGF; Cisneros, JC; Siegloch, AM				da Conceicao, Domingas Maria; Iannuzzi, Roberto; de Andrade, Luiz Saturnino; Esperanca Junior, Mario G. F.; Cisneros, Juan Carlos; Siegloch, Anelise M.			First report of Cordaixylon Grand'Eury in the Permian of South America, Parnaiba Basin, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Parnaiba basin; Cisuralian; Systematics; Cordaitales; Paleoclimatology; Paleophytogeography	CORDAITALEAN SEED PLANTS; GYMNOSPERM WOODS; FOGO FORMATION; PART II; RECONSTRUCTION; CLIMATE; CHINA; PEDRA	We describe the morphology and anatomy of cordaitalean tree stems preserved in Cisuralian lacustrine deposits of the Pedra de Fogo Formation, Permian of the Parnaiba Basin, northeastern Brazil. The remains consist of seven samples of petrified stems with septate pith (Artisia type) and preserved primary and secondary xylem. The anatomical features of these specimens support their classification in the genus Cordaixylon Grand'Eury, 1877, which is the first evidence of this genus not only in South America, but also in Gondwana. The sedimentological indicators suggest climatic seasonality during the deposition of the Pedra de Fogo unit. However, on a local scale, this area may have had a humid to sub-humid regional climate due to the presence of a large lacustrine system, which would allow these plants to grow in similar habitats to their locations in the Northern Hemisphere. The Parnaiba Basin contains a relatively high number of endemic taxa, but this genus is typical of the Euramerican Province and occurs in at least two areas of this basin. The presence of these trees and some forms of tree-ferns that are also shared with the Euramerican Province suggests the existence of a phytogeographic connection consisting of dispersal through a landscape linkage between the Euramerican tropics and northern Gondwana in the Late Pennsylvanian. This would make it possible for species to migrate between these two floristic provinces, a hypothesis that can be confirmed through further taxonomic and geological data. Finally, the presence of Cordabcylon in the Pedra de Fogo Formation can be considered indicative of a Cisuralian age for these rocks.	[da Conceicao, Domingas Maria; Iannuzzi, Roberto; Esperanca Junior, Mario G. F.; Siegloch, Anelise M.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [de Andrade, Luiz Saturnino] UFPA, Inst Geociencias, Rua Augusto Correa 1, BR-66075110 Belem, PA, Brazil; [Cisneros, Juan Carlos] Univ Fed Piaui, Museu Arqueol & Paleontol, BR-64049550 Teresina, PI, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Para; Universidade Federal do Piaui	da Conceicao, DM (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	domingasmary@hotmail.com	Cisneros, Juan C/A-5258-2008; Iannuzzi, Roberto/G-3641-2012	Iannuzzi, Roberto/0000-0003-1432-8106; Esperanca Junior, Mario/0000-0002-5338-9000; Cisneros, Juan Carlos/0000-0001-6159-1981; Andrade, Luiz/0000-0001-7168-8787	Brazilian National Council for Scientific and Technological Development (CNPq) [141248/2016-5, 401848.2010-8, 456608/2014-1, PQ312747/2017-9]; Field Museum of Natural History - Negaunee Foundation	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Field Museum of Natural History - Negaunee Foundation	The authors wish to thank the Brazilian National Council for Scientific and Technological Development (CNPq) for a PhD scholarship to D. M. Conceicao (141248/2016-5), for grants to J. Cisneros (401848.2010-8) and to R. Iannuzzi (456608/2014-1, PQ312747/2017-9). The authors also gratefully acknowledge Ken Angielczyk (Field Museum of Natural History) for partial financial support of field studies, granted by The Negaunee Foundation. We are grateful to Renata L. S. Quaresma and Sara Cristina for kindly providing the necessary logistical help in the fieldwork, which was essential in obtaining the material studied. Thanks are extended to the anonymous reviewers that enhanced the manuscript with their comments.	Andrade L. 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J	Carvalhedo, ALD; Carmelo, AC; Botelho, NF				da Costa Carvalhedo, Alice Louzada; Carmelo, Adriana Chatack; Botelho, Nilson Francisquini			Geophysical-geological model of the Pedra Branca massif in the Goias Tin Province, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Magnetometry; Gamma-ray spectrometry; Geophysical model; Pedra Branca massif; Goias Tin province	2-DIMENSIONAL MAGNETIC BODIES; ANALYTIC SIGNAL; INVERSION; TRANSFORMS; EVOLUTION; RECORD	The Pedra Branca massif is located in central Brazil, northeast Goias, near the city of Nova Roma, occupying an area of approximately 80 km(2). It is part of the Goias Tin Province (GTP), located within the oldest fin subprovince, Rio Parana, which, together with the Rio Tocantins Subprovince, are the most economically important provinces of the GTP. The massif is part of the Pedra Branca suite and is defined as an A-type granite from the Paleoproterozoic (1.6-1.77 Ga), rich in several ores such as fin, fluorine and rare-earth elements (REE) with anomalous concentration of indium, niobium, uranium, and thorium. Its magmatic evolution is closely related to the continental evolution and bimodal volcanism of the Arai rift. The mineralization zones are pre-tectonic, hosted in greisens with the presence of cassiterite; the main mineralization zones are named Zona da Bacia and Faixa Placha. This area is characterized by metallogenic importance. However, only a few geophysical studies have focused on the granite area. The lack of geophysical information makes it difficult to establish the signature of the Pedra Branca massif. The main goal of this study is to increase geophysical information by determining the magnetic and gamma-ray spectrometric signatures of the granite massif, and to generate a geophysical-geological model representative of the surface and subsurface geological features. These signatures are investigated and related to the geological structures and fin mineralized zones (cassiterite) present in the massif. Based on the analysis of airborne and ground gamma-ray spectrometry data and geochemical data, it was possible to characterize the anomalous zones of uranium (U) and thorium (Th) of the granitic massif. From the magnetometric Total Gradient Amplitude (TGA) and Tilt Derivative (TDR) products, it was possible to define important magnetic signatures, as well as to delimit the intrusion and its contact with enclosing and surrounding rocks. These products, in conjunction with products generated by Matched Filtering and Euler Solutions, provide subsurface magnetic signature information and their depth estimates. The forward modeling and the inversion of the magnetic data generated from the Induced Magnetization Vector (MVI), were correlated in order to generate a 2D geophysical-geological model that presents main sources of shallow magnetic susceptibility (ca. 800 m) corresponding to the Faixa Placha (0.029SI) and sources of high susceptibility (0.012SI - MVI), located in greater depth (ca. 2 km) inside and outside the massif. Within the massif, the source of high susceptibility was interpreted as mafic pluton due to the bimodal magmatism of the Arai rift. On the surface, this mafic magmatism emerges as diabase dikes. The other magnetic source in the southeast edge is interpreted like a mafic magmatism body from the bimodal volcanism of Arai Group or Quartz Diorite Nova Roma. The interpretation of geophysical data is consistent with the underplating process, commonly accepted as responsible for the generation of type A magmas, based on the partial melting of the continental crust, caused by the rise of mafic magma.	[da Costa Carvalhedo, Alice Louzada; Carmelo, Adriana Chatack; Botelho, Nilson Francisquini] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil	Universidade de Brasilia	Carvalhedo, ALD (autor correspondente), Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil.	alicelcc@hotmail.com; chatack@unb.br; nilsonfb@unb.br	Carmelo, Adriana Chatack/AAK-9744-2021; Botelho, Nilson Francisquini/T-9470-2017	Carmelo, Adriana Chatack/0000-0003-0745-3072; Botelho, Nilson Francisquini/0000-0001-9090-799X	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) - Ministerio da Educacao, Brazil	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) - Ministerio da Educacao, Brazil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	A. L. Carvalhedo was supported in this research by a fellowship from Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) - Ministerio da Educacao, Brazil. 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J	Felix, WQ; Oliveira, DC; Silva, LR; Silva, FF				Felix, Williamy Queiroz; Oliveira, Davis Carvalho; Silva, Luciano Ribeiro; Silva, Fernando Fernandes			Charnockites from Carajas Province, SE Amazonian Craton (Brazil): Petrogenetic constraints and intensive crystallization parameters	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Magnesian charnockite; Carajas province; Post-collisional; Hydration; Fractional crystallization; Crystallization parameters	GRANITE-GREENSTONE TERRANE; NORTHERN MARGINAL ZONE; WIND-RIVER RANGE; A-TYPE GRANITES; MINERAL PROVINCE; EXPERIMENTAL CALIBRATION; TECTONIC SIGNIFICANCE; IGNEOUS CHARNOCKITES; ZIRCON GEOCHRONOLOGY; LIMPOPO BELT	The gabbronorite-charnockite-granite series rocks in the Carajas Province consist of three granitoid varieties: orthopyroxene granodiorite, clinopyroxene monzogranite and amphibole monzogranite; gabbronorites are spatially associated. They occur as a NE-SW-elongated pluton with minor E-W-oriented lenses. In general, the planar fabrics are defined by a NE-SW to E-W trend and steep dip (70-85 degrees) restricted to shear zones. The main mafic phases are pyroxene and amphibole. Biotite is annite with magmatic and subalkaline signature. Plagioclase includes labradorite and andesine. Amphibole thermometers estimates vary from 713 to 800 degrees C and 765-809 degrees C in the granitoids and gabbronorite, respectively. Pyroxenes gave higher temperatures of 1194-1573 degrees C. The pressures were 190-310 MPa during emplacement. The presence of primary magnetite together with geochemical and amphibole-biotite chemical data argues that the studied rocks have crystallized under oxidized conditions (NNO +/- 0.5 and NNO +1). The H2O contents are estimated as higher than 4%. The gabbronorite-charnockite-granite series has magnesian affinity, calc-alkaline to high-K calcic-alkaline trends and metaluminous character. The magnesian and oxidized character is inherited from the source, which was likely extracted from a depleted mantle (low HFSE contents). Geochemical modeling shows that the orthopyroxene granodiorite originated by fractional crystallization from a magma akin to the gabbronorite. Water activity was high in the monzogranites, and hydration had an important role in the magmatic evolution of the gabbronoritecharnockite-granite series. The emplacement of these rocks was controlled by a translithospheric-scale shear zone acting as a preexisting conduit for the migration of mantle-derived magmas to epizonal levels (7.0-10.5 km) in a sinistral transpressive regime in a post-collisional setting. Deep crustal levels favor crystallization of orthopyroxene-bearing rocks (poor water conditions), while at shallower crustal levels fluids tend to be dominant in the magma, leading to the generation of amphibole-bearing granite.	[Felix, Williamy Queiroz; Oliveira, Davis Carvalho; Silva, Luciano Ribeiro; Silva, Fernando Fernandes] Inst Geociencias IG, Grp Pesquisa Petrol Granitoides GPPG, Rua Augusto Correa 01, BR-66075900 Belem, PA, Brazil; [Felix, Williamy Queiroz; Oliveira, Davis Carvalho; Silva, Luciano Ribeiro; Silva, Fernando Fernandes] Univ Fed Para UFPA, Programa Posgrad Geol & Geoquim, IG UFPA, Belem, PA, Brazil	Universidade Federal do Para	Felix, WQ (autor correspondente), Inst Geociencias IG, Grp Pesquisa Petrol Granitoides GPPG, Rua Augusto Correa 01, BR-66075900 Belem, PA, Brazil.; Felix, WQ (autor correspondente), Univ Fed Para UFPA, Programa Posgrad Geol & Geoquim, IG UFPA, Belem, PA, Brazil.	williamy@ufpa.br; davis@ufpa.br; lucianor@ufpa.br; ffernandes@ufpa.br			Research Group on Granitoid Petrology (GPPG); Conselho Nacional de Desenvolvimento Tecnologico (CNPq) [311388/2016-7, 435552/2018-0, 311647/2019-7, 152306/2015-3]; PROPESP (PAPQ)/UFPA	Research Group on Granitoid Petrology (GPPG); Conselho Nacional de Desenvolvimento Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); PROPESP (PAPQ)/UFPA	The authors would like to thank the Research Group on Granitoid Petrology (GPPG) for their support in the various stages of this work and the Institute of Geosciences (IG) and the Post-Graduate Program in Geology and Geochemistry (PPGG) of Federal University of Para (UFPA) for technical support. M.N.S. Santos is acknowledged for the previous work on the Ourilandia do Norte area; G.T. Marques and C.N. Lamarao for assistance with the electron microprobe and scanning electron microscope mineral chemical analyses conducted at the Laboratorio de Microanalises of Universidade Federal do Para (UFPA). Journal reviewers are thanked for the comments that help to further clarify some aspects and produce the present version of the study. The first author (W.Q. Felix) also thanks the Conselho Nacional de Desenvolvimento Tecnologico (CNPq) for a master's scholarship (Proc. 152306/2015-3). Funding for this project came from the Conselho Nacional de Desenvolvimento Tecnologico (CNPq) (D.C. Oliveira Proc. 311388/2016-7; 435552/2018-0 and 311647/2019-7) and PROPESP (PAPQ)/UFPA.	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J	Friedrich, BM; Marques, JC; Olivo, GR; Frantz, JC; Joy, B; Queiroz, WJA				Friedrich, Betina Maria; Marques, Juliana Charao; Olivo, Gema Ribeiro; Frantz, Jose Carlos; Joy, Brian; Alves Queiroz, Waldemir Jose			Petrogenesis of the massive chromitite layer from the Jacurici Complex, Brazil: evidence from inclusions in chromite	MINERALIUM DEPOSITA			English	Article						Chromite deposit; Origin of chromitite; Hydrated inclusions in chromite; Carbonate inclusions in chromite; Chromite slurry	SAO-FRANCISCO CRATON; IPUEIRA-MEDRADO SILL; BUSHVELD COMPLEX; ULTRAMAFIC COMPLEX; TROODOS OPHIOLITE; MELT INCLUSIONS; ORIGIN; INTRUSIONS; ROCKS; BAHIA	The Jacurici Complex hosts the largest chromite deposit in Brazil in an up to 8-m-thick chromitite layer within a tectonically segmented 300-m-thick intrusion. The ore has been interpreted as the result of crustal contamination-driven crystallization in a magma conduit. This study addresses the stratigraphy, mineralogical and textural relationships, and mineral chemistry of the Monte Alegre Sul segment focusing on chromite-hosted inclusions from the Main Chromitite Layer to understand the role of volatiles in the genesis of the massive chromitite. Silicate inclusions (enstatite, phlogopite, magnesiohornblende, diopside and olivine) are commonly monomineralic and sub- to euhedral, and crystallized prior to, or coeval with, the chromite crystallization. Carbonate inclusions (dolomite and magnesite) are irregular or have negative crystal shapes, suggesting entrapment as melt droplets. Sulfides (pentlandite, millerite, heazlewoodite, polydymite, pyrite, and chalcopyrite) are often polymineralic, irregular, or hexagonal-shaped, indicating entrapment as sulfide melt and as monosulfide solid solution. The inclusions indicate an H2O- and S-saturated resident magma with immiscible droplets of carbonate melt during chromite crystallization. Inclusion-rich and inclusion-free chromites that occur together have similar compositions and are considered to have formed from the same magma in response to variations in the degree of Cr saturation. Hot primitive magma might have heated and mobilized CO(2)and probably water from devolatized and assimilated carbonate-rich wall rocks, increasingfO(2)and triggering chromite crystallization. We propose that the formation of the chromitite layer started as in situ crystallization with additional material added by slumping of locally remobilized chromite slurries, facilitated by the presence of volatiles.	[Friedrich, Betina Maria; Marques, Juliana Charao; Frantz, Jose Carlos] Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500,Predio 43129, Porto Alegre, RS, Brazil; [Olivo, Gema Ribeiro; Joy, Brian] Queens Univ, Dept Geol Sci & Geol Engn, Kingston, ON K7L 3N6, Canada; [Alves Queiroz, Waldemir Jose] Companhia Ferro Ligas Bahia FERBASA, Pojuca, Bahia, Brazil	Universidade Federal do Rio Grande do Sul; Queens University - Canada	Friedrich, BM (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500,Predio 43129, Porto Alegre, RS, Brazil.	friedrich.betina@gmail.com	Marques, Juliana C/R-1965-2018; FRANTZ, JOSE C/R-1953-2018	Marques, Juliana C/0000-0003-0143-6925; FRANTZ, JOSE C/0000-0002-8890-7250				Aird HM, 2013, CONTRIB MINERAL PETR, V166, P1143, DOI 10.1007/s00410-013-0913-2; Almeida F. F. 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J	Frozza, CF; Pivel, MAG; Suarez-Ibarra, JY; Ritter, MN; Coimbra, JC				Frozza, C. F.; Pivel, M. A. G.; Suarez-Ibarra, J. Y.; Ritter, M. N.; Coimbra, J. C.			Bioerosion on Late Quaternary Planktonic Foraminifera Related to Paleoproductivity in the Western South Atlantic	PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY			English	Article						drilled</AUTHOR_KEYWORD>; paleoceanography</AUTHOR_KEYWORD>; microboring</AUTHOR_KEYWORD>; paleoecology</AUTHOR_KEYWORD>; stable isotopes</AUTHOR_KEYWORD>; paleotemperature</AUTHOR_KEYWORD>	SEA-SURFACE TEMPERATURE; PREDATION; PRODUCTIVITY; CALIBRATION; CIRCULATION; DYNAMICS; PATTERNS; MODEL; BASIN; PLUME	Planktonic Foraminifera are widely used in paleoceanographic reconstructions, although studies of their trophic interactions are still rare, especially those focusing on predation. Drilling holes are the most frequent traces of bioerosion in foraminifer tests, but environmental factors that control bioerosion are not yet understood. To determine if paleoceanographic variables are associated with bioerosion rates in late Quaternary planktonic foraminifers of the western South Atlantic, geochemical and assemblage analyses were made on a 46 kyr record from a piston core. An age model was constructed based on 10 AMS(14)C dates. To reconstruct the paleoproductivity, delta C-13, benthic/planktonic foraminifer and the relative abundances ofGlobigerina bulloidesandGlobigerinoides ruber(high and low productivity, respectively) were used. Bioeroded tests were counted and found in 21 of the 25 identified species, with frequencies ranging from 8.84% to 16.7%. Bioerosion was different in two groups identified by cluster analysis, with a higher intensity during glacial times, showing a strong correlation with paleoceanographic fluctuations. Paleoproductivity estimates and bioerosion rates show a significant correlation, suggesting that bioerosion is more frequent in eutrophic environments and more inhibited in oligotrophic conditions. However, even with a strong correlation between bioerosion and productivity, there is also a negative correlation with sea surface temperature in the study area. Since conditions that promote higher productivity are accompanied by a decrease in surface temperature, the precise distinction between the influence of both variables is hampered. Further research will allow us to explore the potential of planktonic foraminiferal bioerosion as a tool in paleoceanographic studies.	[Frozza, C. F.; Suarez-Ibarra, J. Y.] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, 9500 Bento Goncalves Ave, BR-91501970 Porto Alegre, RS, Brazil; [Pivel, M. A. G.; Coimbra, J. C.] Univ Fed Rio Grande do Sul, Inst Geociencias, 9500 Bento Goncalves Ave, BR-91501970 Porto Alegre, RS, Brazil; [Ritter, M. N.] Univ Fed Rio Grande do Sul, Ctr Estudos Costeiros Limnol & Marinhos, Campus Litoral Norte,976 Tramandal Ave, BR-95625000 Imbe, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Frozza, CF (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, 9500 Bento Goncalves Ave, BR-91501970 Porto Alegre, RS, Brazil.	cristiane.frozza@ufrgs.hr	Suarez-Ibarra, Jaime Y./AGD-6019-2022; Frozza, Cristiane/AAV-4274-2021; Pivel, Maria Alejandra Gomez/F-5594-2013; Ritter, Matias/A-1500-2013; Coimbra, Joao Carlos/H-7500-2013	Suarez-Ibarra, Jaime Y./0000-0002-0227-4369; Frozza, Cristiane/0000-0002-6463-9853; Pivel, Maria Alejandra Gomez/0000-0003-3226-8047; Ritter, Matias/0000-0001-8150-4443; Coimbra, Joao Carlos/0000-0002-8980-6531	Coordination for the Improvement of Higher Education Personnel (CAPES) [88887.091727/2014-01]; National Council for Scientific and Technological Development (CNPq) [305128/2017-5]	Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the Coordination for the Improvement of Higher Education Personnel (CAPES) for supporting the IODP Program and for financial support through Grant 88887.091727/2014-01. We thank Prof. Adriana Leonhardt (LOG-FURG) for providing access to the core. This manuscript greatly benefitted from the contribution from reviewers Adriane R. Lam and R. Mark Leckie and from our colleagues Carla Bonetti, Cristianini T. Bergue, Daiane Ceolin, Everton Frigo, and Fernando Erthal. We appreciate all their suggestions and support. We are also thankful to Bruna da Silva Mota Netto and Kita Macario for the radiocarbon analyses. J. C. Coimbra and J. Y. Suarez-Ibarra express their gratitude to the National Council for Scientific and Technological Development (CNPq) for Grant 305128/2017-5 and for the MSc scholarship, respectively.	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J	Krahl, G; Bom, MHH; Kochhann, KGD; Souza, LV; Savian, JF; Fauth, G				Krahl, Guilherme; Bom, Marlone H. H.; Kochhann, Karlos G. D.; Souza, Lais, V; Savian, Jairo F.; Fauth, Gerson			Environmental changes occurred during the Early Danian at the Rio Grande Rise, South Atlantic Ocean	GLOBAL AND PLANETARY CHANGE			English	Article						South Atlantic Ocean; Early Danian; Cretaceous-Paleogene boundary; Carbonate dissolution; Bottom water oxygenation	CRETACEOUS/PALEOGENE BOUNDARY; SEDIMENT GEOCHEMISTRY; DECCAN TRAPS; CLIMATE; BASIN; PALEOCEANOGRAPHY; COLLAPSE; RECORD; KANSAS; SHIFTS	Early Danian environmental perturbations related to carbon isotope negative excursions (CIEs) were recognized at Deep Sea Drilling Project (DSDP) Hole 516F, Rio Grande Rise. Within the first similar to 160 kyr of the Danian, environmental stability is evidenced by well-oxygenated bottom waters, good carbonate preservation, and relatively high primary production. The preservation of carbonates and the oxygenation of the deep water decreased progressively, leading to the formation of red layers in the sediments between 65.86 Ma and 65.71 Ma. The onset of carbonate dissolution and the reduction in dissolved oxygen concentrations occurred approximately 50 kyr before the onset of the Dan-C2 event, and was probably related to the third volcanic event of the Deccan Traps (DT). Our results support the link between enhanced emissions of volcanic gasses and deep ocean carbonate dissolution and deoxygenation during the Early Danian. The CIEs at the Rio Grande Rise are positioned within the planktonic foraminiferal biozone Plb, suggesting that the first appearance of Subbotina triloculinoides within Chron C29r (at 65.89 Ma) is a diachronous datum.	[Krahl, Guilherme; Bom, Marlone H. H.; Kochhann, Karlos G. D.; Fauth, Gerson] Univ Vale do Rio dos Sinos, Itt Fossil Inst Tecnol Micropaleontol, Av UNISINOS 950, BR-93022000 Sao Leopoldo, RS, Brazil; [Krahl, Guilherme; Bom, Marlone H. H.; Kochhann, Karlos G. D.; Souza, Lais, V; Fauth, Gerson] Univ Vale do Rio dos Sinos, Programa Posgrad Geol, Av UNISINOS 950, BR-93022000 Sao Leopoldo, RS, Brazil; [Savian, Jairo F.] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Geol, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Krahl, G (autor correspondente), Univ Vale do Rio dos Sinos, Itt Fossil Inst Tecnol Micropaleontol, Av UNISINOS 950, BR-93022000 Sao Leopoldo, RS, Brazil.	geounikrahl@gmail.com	Kochhann, Karlos G. D./AAH-4636-2019; Fauth, Gerson/AAE-3353-2021; SOUZA, LAIS/GWZ-9113-2022; Hnnig Bom, Marlone/HKV-2689-2023	Kochhann, Karlos G. D./0000-0001-5339-1103; Krahl, Guilherme/0000-0003-2361-0541	National Council for Scientific and Technological Development (CNPq, Brazil) [201508/2009-5, 427280/2018-4]; Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS, Brazil) [16/2551-0000213-4]; Project IODP/Capes [88887.091703/2014-1]; Capes	National Council for Scientific and Technological Development (CNPq, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS, Brazil)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); Project IODP/Capes; Capes(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors are grateful to the International Ocean Discovery Program (IODP) for providing the studied material; to Capes for providing the post-graduate grant for the GK; to VIZLab and Laserca (Universidade do Vale do Rio dos Sinos) for the spectral reflectance measurements; and to Nils Andersen (Leibniz Laboratory for Radiometric Dating and Stable Isotope Research, Kiel) for the stable isotope measurements. Criticism by two reviewrs greatly improved the first version of the manuscript. JFS thanks the National Council for Scientific and Technological Development (CNPq, Brazil) grants #201508/2009-5; #427280/2018-4 and Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS, Brazil) grant #16/2551-0000213-4. This research is part of the Project IODP/Capes #88887.091703/2014-1.	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J	Costa, ISL; Rocha, MP; Klein, EL; Vasquez, ML				Lima Costa, Iago Sousa; Rocha, Marcelo Peres; Klein, Evandro Luiz; Vasquez, Marcelo Lacerda			Lithospheric structure of the southern Amazonian Craton from multiple-frequency seismic tomography: Preliminary insights on tectonic and metallogenic implications	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Seismic tomography; Body waves; Cratons; South America; Amazonian craton	CARAJAS MINERAL PROVINCE; TRAVEL-TIME; CROSS-CORRELATION; MANTLE; BRAZIL; EVOLUTION; PLUTONISM; KERNELS; BENEATH; REGION	We present a P-wave structure for the sub-continental lithospheric mantle (SCLM) beneath the southern segment of the Amazonian Craton (Central Brazil Shield - CBS) using multiple-frequency tomography. Our model includes 469 seismic events recorded between 2009 and 2017 through 314 seismic stations distributed over South America. From these events, we obtained 20507 P and 12329 PKIKP cross-correlation delays in six frequency bands centered at 0.03, 0.06, 0.13, 0.25, 0.5 and 1 Hz. Despite the limited and heterogeneous resolution throughout the CBS, because of the difficulty in the installation of seismographic stations in areas of dense coverage of tropical forest, our tests show reasonable resolution for lithospheric domains with dimensions greater than 390 x 390 km in most of the study area. We recognized a good correlation between the P-wave anomalies and the tectonic domains defined previously based on geochronology and geological data. The surface projection of these anomalies and their margins are associated with clusters of important Au, Cu-Au and IOCG deposits, as well as diamond-bearing kimberlite intrusions, allowing relating deep structures with shallow features and showing a province-scale control in the distribution of mineral deposits and occurrences in the southern Amazonian craton.	[Lima Costa, Iago Sousa; Klein, Evandro Luiz] CPRM Geol Survey Brazil, SBN, Quadra 02,Bloco H,2 Andar, Brasilia, DF, Brazil; [Lima Costa, Iago Sousa; Rocha, Marcelo Peres] Univ Brasilia UnB, Seismol Observ, Inst Geosci, Brasilia, DF, Brazil; [Vasquez, Marcelo Lacerda] CPRM Geol Survey Brazil, Av Perimetral 3645, Belem, Para, Brazil	Universidade de Brasilia	Costa, ISL (autor correspondente), SBN, Quadra 02,Bloco H,2 Andar, Brasilia, DF, Brazil.	iago.costa@cprm.gov.br; marcelorocha@unb.br; evandro.klein@cprm.gov.br; marcelo.vasquez@cprm.gov.br	Klein, Evandro L/G-5973-2012; Vasquez, Marcelo/AAB-9111-2021; Costa, Iago Sousa Lima/ABA-9358-2021; Rocha, Marcelo P/K-5215-2013	Klein, Evandro L/0000-0003-4598-9249; Vasquez, Marcelo/0000-0003-2729-9404; Costa, Iago Sousa Lima/0000-0002-3721-8957; Rocha, Marcelo P/0000-0002-6869-6468	CNPq-Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [31.1167/2015-2, 46.5613/2014-4, 30.6798/2016-6]	CNPq-Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank PETROBRAS and CPRM-Geological Survey of Brazil for providing resources to expand and maintain the Brazilian Seismographic Network (RSBR). We want to thank Dr. Paulo de Azevedo for his great assistance in the installation of seismographic stations in the Amazonian Craton, also all the staff that helped in stations installation and maintenance. Thanks also go to the Dr. Andres Folguera and an anonymous reviewer for their valuable suggestions and comments. Special thanks go to Dr. Guust Nolet, who provided the algorithms and all the necessary help for the development of the seismic tomographic models used in this work. We use data from additional stations of the Seismological Center of the University of Sao Paulo, Sao Paulo State Institute of Technological Research (IPT), Seismological Observatory and Laboratory of Lithospheric Studies of the University of Brasilia, GTSN and GEOSCOPE Networks, and a temporary deployment by ETH-Zurich. We employed the python library ObsPy (Beyreuther et al., 2010) to pre-processing the seismograms, and the library Matplotib (Hunter 2007) to plot the data. We thank CNPq-Conselho Nacional de Desenvolvimento Cientifico e Tecnologico for the research grants 31.1167/2015-2 and 46.5613/2014-4 INCT Estudos Tectonicos (Marcelo Rocha), and 30.6798/2016-6 (Evandro Klein).	Afonso JC, 2012, LITHOS, V134, P289, DOI 10.1016/j.lithos.2012.01.009; Althoff F, 2000, PRECAMBRIAN RES, V104, P187, DOI 10.1016/S0301-9268(00)00103-0; Amaral G, 1974, THESIS; [Anonymous], 2008, GEOLOGIA RECURSOS MI; Azevedo P., 2015, GEOPHYS J INT, V201, P61, DOI DOI 10.1093/GJI/GGV003; Bassin C, 2000, EOS T AGU, V81, pF897; BEGG GC, 2018, SPACE TIME, P1, DOI DOI 10.1016/B978-0-12-811159-8.00002-0; Begg GC, 2010, ECON GEOL, V105, P1057, DOI 10.2113/econgeo.105.6.1057; Beyreuther M, 2010, SEISMOL RES LETT, V81, P530, DOI 10.1785/gssrl.81.3.530; Bianchi MB, 2018, SEISMOL RES LETT, V89, P452, DOI 10.1785/0220170227; Bonnin M, 2014, GEOPHYS J INT, V198, P1458, DOI 10.1093/gji/ggu214; Borges F. 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South Am. Earth Sci.	AUG	2020	101								102608	10.1016/j.jsames.2020.102608	http://dx.doi.org/10.1016/j.jsames.2020.102608			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LW8CK		Green Submitted			2023-06-23	WOS:000539370500016
J	Palladino, G; Rizzo, RE; Zvirtes, G; Grippa, A; Philipp, RP; Healy, D; Alsop, GI				Palladino, Giuseppe; Rizzo, Roberto Emanuele; Zvirtes, Gustavo; Grippa, Antonio; Philipp, Ruy Paulo; Healy, David; Alsop, G. Ian			Multiple episodes of sand injection leading to accumulation and leakage of hydrocarbons along the San Andreas/San Gregorio fault system, California	MARINE AND PETROLEUM GEOLOGY			English	Article						Sandstone intrusions; Santa cruz injection complex; Santa cruz petroleum system; Sandstone-filled faults; Hydrocarbon leakage; San andreas/San Gregorio fault system; California	SANDSTONE INTRUSIONS; CRUZ; TECTONICS; COMPLEX; PERMEABILITY; EMPLACEMENT; GEOMETRY; INSIGHTS; GENESIS; FIELD	The presence of sand injections has been shown to enhance the likelihood of hydrocarbon traps within siliciclastic successions. Through the development of large interconnected networks of sills and dykes, sand injection complexes provide a volume of porous and permeable rocks within the low permeability host units. Overall, the formation of sand injection complexes requires extensive fracturing and hydrofracturing, which can be particularly pronounced when sand injections are coupled with brittle tectonic deformation. In some circumstances, this process may threaten the integrity of the reservoir top seal thereby preventing further hydrocarbon accumulation. Studying exceptional exposures along the coastal area of Santa Cruz in California, we report evidence for top seal failure associated with injection episodes. Two distinct sand injection episodes are proposed. The first event, datable to the Late Miocene, resulted in large volumes of sand being emplaced within the top-seal units, and was followed by accumulation of hydrocarbons within the newly injected sandstones. Later, a series of brittle tectonic events, associated with the San Andreas/San Gregorio Fault System, caused remobilization and accumulation of sand along newly formed fault planes. Our case study documents this combination of pervasive brittle deformation and sandstone injection along fault structures, which can ultimately disrupt the integrity of a host unit leading top seal failure and leakage of hydrocarbons.	[Palladino, Giuseppe; Rizzo, Roberto Emanuele; Zvirtes, Gustavo; Grippa, Antonio; Healy, David; Alsop, G. Ian] Univ Aberdeen, Sch Geosci, Dept Geol & Geophys, Aberdeen, Scotland; [Palladino, Giuseppe] Univ Basilicata, Dipartimento Sci, Potenza, Italy; [Rizzo, Roberto Emanuele] Heriot Watt Univ, Lyell Ctr, Inst GeoEnergy, Edinburgh, Midlothian, Scotland; [Philipp, Ruy Paulo] Univ Fed Rio Grande do Sul, Dept Mineral & Petrol, Porto Alegre, RS, Brazil	University of Aberdeen; University of Basilicata; Heriot Watt University; Universidade Federal do Rio Grande do Sul	Palladino, G (autor correspondente), Univ Aberdeen, Sch Geosci, Dept Geol & Geophys, Aberdeen, Scotland.	giuseppe.palladino@abdn.ac.uk		Alsop, Ian/0000-0003-4479-372X; Zvirtes, Gustavo/0000-0001-9728-0464; Rizzo, Roberto Emanuele/0000-0002-1607-6283; PHILIPP, RUY PAULO/0000-0003-2875-0914				[Anonymous], AAPG SEARCH DISCOVER; [Anonymous], US GEOLOGICAL SURVEY; [Anonymous], GEOLOGICAL SURVEY PR; [Anonymous], GEOLOGY TECTONICS CE; [Anonymous], 1998, GEOL SOC SPEC PUBL; [Anonymous], AAPG AM ASS PET GEOL; [Anonymous], US GEOLOGICAL SURVEY; 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Pet. Geol.	AUG	2020	118								104431	10.1016/j.marpetgeo.2020.104431	http://dx.doi.org/10.1016/j.marpetgeo.2020.104431			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LU4OQ		Green Submitted			2023-06-23	WOS:000537736900028
J	Ricardo, BS; Faleiros, FM; de Moraes, R; Siga, O; Campanha, GAC				Ricardo, Bruna S.; Faleiros, Frederico M.; de Moraes, Renato; Siga Junior, Oswaldo, Jr.; Campanha, Ginaldo A. C.			Tectonic implications of juxtaposed high- and low-pressure metamorphic field gradient rocks in the Turvo-Cajati Formation, Curitiba Terrane, Ribeira Belt, Brazil	PRECAMBRIAN RESEARCH			English	Article						Detrital zircon U-Pb ages; Metamorphic field gradients; Paired metamorphic belts; Pseudosection modeling; Ribeira Belt; Neoproterozoic	BARROVIAN METAMORPHISM; SANTANDER MASSIF; WESTERN GONDWANA; COMPLEX; EVOLUTION; COMPUTATION; EQUILIBRIA; DATASET	The Turvo-Cajati Formation (TCF) is an important unit forming the Curitiba Terrane, a major segment of the southern Ribeira Belt, SE Brazil. It is composed of rocks of greenschist (LTCF), amphibolite (MTCF) and granulite (HTCF) facies conditions. Previous studies in the HTCF indicate that the unit underwent extensive partial melting under high-pressure conditions (670-810 degrees C and 9.5-12 kbar), within the kyanite stability field. In this paper, a study of the metamorphic zoning within the LTCF and MTCF is undertaken using pseudosection modeling in the NCKFMASHTO and MnNCKFMASHTO model systems coupled with detrital zircon U-Pb geochronology. Four metamorphic zones are recognized for the LTCF and MTCF: biotite, garnet, staurolite and sillimanite zones, with predominance of sillimanite zone and pressures lower than 8 kbar, as staurolite breaks down straight to sillimanite, without formation of a kyanite zone. Pseudosections yielded metamorphic peak conditions of similar to 530-560 degrees C and similar to 6-7.5 kbar (garnet zone) and similar to 660-690 degrees C and similar to 6-7.5 kbar (sillimanite zone). The metamorphic field gradient is flat and of low to medium pressure, below the typical Barrovian-type baric regime, and different from the HTCF. Available petrological and geochronological data suggest that the TCF comprises a paired low-P and high-P metamorphic belt, associated with a major Ediacaran suture zone in the southern Ribeira Belt. Probability density plots from detrital zircon U-Pb ages indicate late-Cryogenian-Ediacaran arc-related and Rhyacian sources for all TCF sub-units. This scenario suggests that the TCF is made up of a collisional juxtaposition of an accretionary wedge (HTCF) and a back-arc basin (LTCF and MTCF) on the border of a microplate, which includes a Rhyacian basement microcontinent, the Atuba Complex. It is inferred the high metamorphic gradient recorded in the LTCF and MTCF was related with asthenospheric upwelling in the back-arc region, which also produced extensive partial melting in the Atuba Complex basement.	[Ricardo, Bruna S.; Faleiros, Frederico M.; de Moraes, Renato; Siga Junior, Oswaldo, Jr.; Campanha, Ginaldo A. C.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil	Universidade de Sao Paulo	Ricardo, BS (autor correspondente), Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil.	bruna.ricardo@usp.br; ffalei@usp.br; rmoraes@usp.br; osigajr@usp.br; ginaldo@usp.br	Ricardo, Bruna/HGC-4538-2022; Faleiros, Frederico Meira/F-6138-2010	Faleiros, Frederico Meira/0000-0003-2199-8116; da Silva Ricardo, Bruna/0000-0002-7241-1920	Sao Paulo Research Foundation (FAPESP) [2018/10012-0, 2018/01572-1, 2016/12986-6, 2015/04487-7]; National Counsel of Technological and Scientific Development (CNPq) [307732/2019-3]; Coordination of Superior Level Staff Improvement (CAPES)	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Counsel of Technological and Scientific Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordination of Superior Level Staff Improvement (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	Financial support was provided by grants 2018/10012-0, 2018/01572-1, 2016/12986-6 and 2015/04487-7 from Sao Paulo Research Foundation (FAPESP). FMF thanks the research productivity scholarship grant 307732/2019-3, National Counsel of Technological and Scientific Development (CNPq). BSR also thanks Coordination of Superior Level Staff Improvement (CAPES) for financial support by scholarship grant. We also thanks Monica Heilbron and an anonymous reviewer for comments and suggestions that help us improve this article. An earlier version of this paper was reviewed by Kathryn Cutts and an anonymous reviewer.	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J	Barrera, IAR; Nogueira, ACR; Bandeira, J				Romero Barrera, Ivan Alfredo; Rodrigues Nogueira, Afonso Cesar; Bandeira, Jose			The Silurian glaciation in the eastern Parnaiba Basin, Brazil: paleoenvironment, sequence stratigraphy and insights for the evolution and paleogeography of West Gondwana	SEDIMENTARY GEOLOGY			English	Article						West Gondwana; Silurian; Parnaiba Basin; Serra Grande Group; Glaciation	WATER-ESCAPE STRUCTURES; ICE-CONTACT FAN; LATE ORDOVICIAN; SNOWBALL EARTH; SEA-LEVEL; CRUSTAL STRUCTURE; SUBAQUEOUS FAN; DELTA DEPOSITS; ENVIRONMENTS; FACIES	Glacial strata are excellent stratigraphic markers in Paleozoic basins worldwide. The eastern Parnaiba Basin in northern Brazil is a highly favorable setting for studying episodes related to the Ordovician-Silurian glaciation. Previous studies in this region led to the recognition of unequivocally glaciogenic sediments associated with pre- and postglacial deposits, favoring the understanding of lower Paleozoic events that occurred in West Gondwana. Outcrop-based fades and stratigraphic analyses of the similar to 170 m-thick silicidastic succession of the Serra Grande Group indicate fluvial, glacial, and coastal depositional systems. Seventeen sedimentary fades are grouped into seven fades associations (FAs): FA1, interpreted as intermediary sheet braided plain deposits that consist of tabular cross-bedded coarse-grained sandstones and conglomerates; FA2-FA4, which correspond to subaqueous glacial deposits comprising massive to stratified diamictites, cross-laminated sandstones, diamictites and organic matter-rich black shales with dumpstone and dropstone structures; FA5-FA6, constituting organic matter-rich black shales, fine- to medium-grained sandstones with sigmoidal cross-bedding and occurrences of the ichnotaxon Arthrophyais interpreted as delta front deposits; and FA7, composed of medium- to coarse-grained pebbly sandstones interpreted as channel ized braided plain deposits. This interpretation partially confirms the previous paleoenvironmental interpretation discounting the presence of subaerial alluvial fan and outwash plain deposits for this unit. The sequence stratigraphy of the Serra Grande Group is refined mainly using the coherent interpretation of the key surfaces and comparing the systems tracts with the global sealevel curve, providing a more robust third-order sequential evolutionary model that includes three depositional sequences. The Middle Ordovician sheet braided deposits are the lowstand sediments of Sequence 1 truncated by an extensive unconformity that possibly removed the transgressive and high-stand strata. This unconformity generated by glacial dynamics represents 23 Myr during the Late Ordovician to early Silurian. The second sequence started with the advance of ice sheets in marginal areas of the basin, causing the deposition of ablation diamicton during the lowstand. The postglacial transgression is marked by ice-rafted debris from icebergs deposited onto organic matter-rich mud in the shoreface-offshore zone. The maximum flooding during the middle to late Silurian was succeeded by the highstand phase marked by the progradation of deltaic deposits. Biological activity is marked by the presence of polychaetes that reworked the marine seafloor. The Early Devonian featured extensive sea-level fall and renewed continental drainage with the formation of a braided plain marking a lowstand phase of Sequence 3. These new interpretations allow the global correlation of the Serra Grande Group and provide an improved understanding of the role of ice sheets and postglacial transgressions that affected West Gondwana during the Ordovician-Silurian periods. (C) 2020 Elsevier B.V. All rights reserved.	[Romero Barrera, Ivan Alfredo; Rodrigues Nogueira, Afonso Cesar; Bandeira, Jose] Univ Fed Para, Fac Geol, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa S-No, BR-66075110 Belem, Para, Brazil; [Rodrigues Nogueira, Afonso Cesar] CNPq, Res Prod, Brasilia, DF, Brazil	Universidade Federal do Para	Barrera, IAR (autor correspondente), Univ Fed Para, Fac Geol, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa S-No, BR-66075110 Belem, Para, Brazil.	ivan.barrera@ig.ufpa.br; anogueira@ufpa.br; jbandeira@ufpa.br		NOGUEIRA, AFONSO/0000-0002-5225-9255	National Council for Scientific and Technological Research (CNPq) [CNPq -133509/2018-4]; Programa de Pos-Graduacao em Geologia e Geoquimica (PPGG) of the Federal University of Para (UFPA) [460964/2014-3]	National Council for Scientific and Technological Research (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Programa de Pos-Graduacao em Geologia e Geoquimica (PPGG) of the Federal University of Para (UFPA)	We are very grateful to the National Council for Scientific and Technological Research (CNPq) for funding this research with a master scholarship (CNPq -133509/2018-4) awarded to the first author, to the Programa de Pos-Graduacao em Geologia e Geoquimica (PPGG) of the Federal University of Para (UFPA) for logistic and financial support from the CNPq project (Grant 460964/2014-3 to J. B.) and the PROPESP/UFPA for supporting the english proofreading serviceWe also thank Joelma Lobo for facilitating the production of thin sections and Afonso Quaresma, Andressa Nogueira and Sebastian Gomez for assistance during fieldwork; Werner Truckenbrodt, Ana Goes, Francisco Abrantes, Daniel Le Heron, and Jean-Francois Ghienne for his constructive comments on the manuscript; and to Brian Jones for his editorial	ARTHUR MA, 1994, ANNU REV EARTH PL SC, V22, P499, DOI 10.1146/annurev.ea.22.050194.002435; Assis AP, 2019, J S AM EARTH SCI, V95, DOI 10.1016/j.jsames.2019.102241; Bally A. 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Geol.	AUG	2020	406								105714	10.1016/j.sedgeo.2020.105714	http://dx.doi.org/10.1016/j.sedgeo.2020.105714			22	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NM5US					2023-06-23	WOS:000568162600002
J	Soares, JL; Nogueira, ACR; dos Santos, RF; Sansjofre, P; Ader, M; Truckenbrodt, W				Soares, Joelson Lima; Rodrigues Nogueira, Afonso Cesar; dos Santos, Renan Fernandes; Sansjofre, Pierre; Ader, Magali; Truckenbrodt, Werner			Microfacies, diagenesis and hydrocarbon potential of the Neoproterozoic cap carbonate of the southern Amazon Craton	SEDIMENTARY GEOLOGY			English	Article						Cap carbonate; Microfacies; Diagenesis sequence; Hydrocarbon potential; Marinoan; Neoproterozoic	SULFATE-REDUCING BACTERIA; DEATH-VALLEY; DOLOMITE; SEDIMENTARY; ARAGONITE; BRAZIL; ORIGIN; RECORD; PRECIPITATION; STRATIGRAPHY	The low-latitude Marinoan glaciation (635 Ma) record in the southern Amazon Craton has been one of the most important sites with strong evidence for the Neoproterozoic Snowball Earth hypothesis. In Central Brazil, the 50-m-thick carbonate succession of the post-Marinoan cap carbonate exposed in the Tangara da Serra region, Central Brazil, represents a complementary section of the classical occurrence of the Puga cap carbonate in Mirassol d'Oeste region, that overlies glaciogenic deposits marking the well-preserved Cryogenian-Ediacaran boundary in South America. The 8-m-thick cap dolostone that represents the Mirassol d'Oeste Formation consists of pinkish microaystalline peloidal dolomudstone, exhibiting even parallel to low-angle lamination locally tubestone, and megaripple bedded dolopackstone. The cap dolostone is succeeded upsection by the cap cementstone limestone (basal Guia Formation), comprising laminated lime mudstone rich in silt-sized terrigenous grains (quartz), and subordinately bituminous shale, dolomitic marls, intraformational breccias, and abundant calcite crystal fans and crusts. Crystal fans occur in isolated and decimetre-scale arrays and are considered aragonite pseudomorphs. Primary precipitation of dolomite, crystal fans, and micrite and the formation of tubestone are related to depositional processes. The cap dolostone was affected by the neomorphism of the dolomicrite, development of vug and interaystalline porosity, euhedral dolomite precipitation. synsedimentary fracturing, calcite and quartz precipitation, chemical compaction, Fe-oxide substitution, and precipitation. The diagenetic processes of the cap cementstone limestone were pyrite precipitation, calcite cementation, neomorphism of micrite and crystal fan, partial crystal fan dissolution, dolomitization, chemical compaction, fracturing, ferrous dolomite and calcite precipitation, pyrite (pseudomorph) and micrite replacement with Fe-oxide and replacement of rhombohedral dolomite by Mn-oxides. Hydrocarbons are rare and its migration represents the last diagenetic event being found: 1) in fractures and interpeloidal, vug and intercrystalline pores (similar to 2%) with low permeability and connectivity of the cap dolostone; and 2) in intercrystalline pores, fractures, and rare pores in crystal fans of the cap cementstone limestone. During the post-Marinoan sea-level rise occurred the establishment of a shallow to moderately deep microbially induced dolomitic platform locally influenced by storm-action. The progressive transgression led the implantation of a deep anoxic and CaCO3-oversaturated aragonitic platform. The similarities of cap carbonate microfades among the post-Marinoan succession worldwide reflects an extraordinary and non-recurring global precipitation event in geological history. In contrast, besides the majority of cap carbonate have the same textural and compositional framework, the diagenetic history seems to be regional and completely dependent on the tectonic, thermal, and burial history of the depositional basins where they were deposited. (C) 2020 Published by Elsevier B.V.	[Soares, Joelson Lima; Rodrigues Nogueira, Afonso Cesar; dos Santos, Renan Fernandes; Truckenbrodt, Werner] Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa S-No,R Augusto Correa 01, BR-66075110 Belem, Para, Brazil; [Sansjofre, Pierre] Museum Natl Hist Nat, 57 R Cuvier, F-75005 Paris, France; [Ader, Magali] Univ Paris, Globe Phys Inst Paris, CNRS, F-75005 Paris 10, France	Universidade Federal do Para; Museum National d'Histoire Naturelle (MNHN); Centre National de la Recherche Scientifique (CNRS); UDICE-French Research Universities; Universite Paris Cite	Soares, JL (autor correspondente), Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa S-No,R Augusto Correa 01, BR-66075110 Belem, Para, Brazil.	jlsoares@ufpa.br	IMPMC, ROCKS @/U-8478-2017; ader, magali/A-5613-2011	ader, magali/0000-0002-9239-1509; Santos, Renan/0000-0002-6068-3814; NOGUEIRA, AFONSO/0000-0002-5225-9255; Soares, Joelson Lima/0000-0003-3683-523X	INCT/GEOCIAMprogramme; MCT/CNPq [15/2007]	INCT/GEOCIAMprogramme; MCT/CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This researchwas supported by the INCT/GEOCIAMprogramme and the MCT/CNPq 15/2007-Universal project. This study is a work of the GSED-UFPA research group. To PROPESP/UFPA for supporting the English proofreading service. We thank Thomas Fairchild for the useful discussions and critical reading of the manuscript. Jose Bandeira, Roberto Cesar Barbosa and Rick Oliveira are thanked for their assistance in the fieldwork. We thank Virginio Neumann for the use of the Laboratory of Cathodoluminescence and Claudio Lamarao and Romulo Angelica for the analysis in the SEM/EDS and X-ray diffraction laboratories, respectively. We acknowledge Calcario Tangara S.A. for the provided logistical support and mine engineer Savio Santos for his valuable collaboration.	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Geol.	AUG	2020	406								105720	10.1016/j.sedgeo.2020.105720	http://dx.doi.org/10.1016/j.sedgeo.2020.105720			20	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	NM5US					2023-06-23	WOS:000568162600007
J	Spiekermann, R; Jasper, A; Benicio, JRW; Guerra-Sommer, M; Ricardi-Branco, FS; Uhl, D				Spiekermann, Rafael; Jasper, Andre; Benicio, Jose Rafael W.; Guerra-Sommer, Margot; Ricardi-Branco, Fresia Soledad; Uhl, Dieter			Late Palaeozoic lycopsid macrofossils from the Parana Basin, South America - an overview of current knowledge	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Review						Lycopsida; Pennsylvanian; Permian; Western Gondwana; Parana Basin; South America	RIO-BONITO FORMATION; GRANDE-DO-SUL; COAL-BEARING STRATA; MISSISSIPPIAN VEGETATION; ARBORESCENT LYCOPSIDS; CYCLODENDRON-LESLII; PERMIAN LYCOPOD; SANTA-CATARINA; PALYNOLOGY; PALEOECOLOGY	Lycopsids evolved arborescent and sub-arborescent growth habits and played a major paleoecological role during the late Palaeozoic. Here we provide an overview of lycopsid macrofossils documented so far in the late Palaeozoic deposits of the South American Parana'. Basin. Most of these lycopsid remains were reported from the Brazilian part of the basin, whereas only a few records have been documented from the Uruguayan and Paraguayan parts. The oldest well-documented macrofossil record of these plants in late Palaeozoic strata of this basin comes from Pennsylvanian interglacial deposits of the Itarare Group. As the late Palaeozoic ice retreated, arborescent and sub-arborescent lycopsids successfully colonized the Brazilian Cisuralian post-glacial palaeoenvironments represented by the Rio Bonito Formation, becoming important elements of the iconic Glossopteris flora. The late Palaeozoic transgression during the Artinskian coincided with the termination of the fluvio-deltaic and peat-forming systems of this formation in most areas of the basin, and this might have affected the lycopsids that grew in these peat-forming palaeoenvironments. Lycopsids again became significant components of the flora in the Brazilian part of the basin during the deposition of the Teresina and Corumbatai formations in the Guadalupian. After the increase of aridity in South America during the upper Permian, the group seems to have disappeared from the late Palaeozoic fossil record of the basin. The late Palaeozoic lycopsid macrofossil record of the Parana'. Basin consists mainly of fragmented and incompletely preserved specimens, which lack crucial parts for systematics, such as reproductive structures. Therefore many aspects of these plants are still poorly known. The discovery of more completely preserved specimens and reproductive structures is required to provide a robust taxonomical and systematical classification, and reliable palaeobiogeographical and evolutionary hypotheses for the distribution and evolution of these particular lycopsids.	[Spiekermann, Rafael; Jasper, Andre; Uhl, Dieter] Senckenberg Forschungsinstitut, Senckenberganlage 25, D-60325 Frankfurt, Germany; [Spiekermann, Rafael; Jasper, Andre; Uhl, Dieter] Nat Museum Frankfurt, Senckenberganlage 25, D-60325 Frankfurt, Germany; [Spiekermann, Rafael; Jasper, Andre; Benicio, Jose Rafael W.; Uhl, Dieter] Univ Vale Taquari Univates, Lab Paleobot & Evolucao Biomas, Ave Avelino Talini 171, BR-95914014 Lajeado, RS, Brazil; [Guerra-Sommer, Margot] Univ Fed Rio Grande Sul UFRGS, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Ricardi-Branco, Fresia Soledad] Univ Estadual Campinas UNICAMP, Inst Geociencias, Dept Geol & Recursos Nat, Carlos Gomes 250, BR-13083855 Campinas, SP, Brazil	Senckenberg Gesellschaft fur Naturforschung (SGN); Universidade Federal do Rio Grande do Sul; Universidade Estadual de Campinas	Spiekermann, R (autor correspondente), Senckenberg Forschungsinstitut, Senckenberganlage 25, D-60325 Frankfurt, Germany.; Spiekermann, R (autor correspondente), Nat Museum Frankfurt, Senckenberganlage 25, D-60325 Frankfurt, Germany.	rafael.spiekermann@senckenberg.de	Spiekermann, Rafael/W-6994-2019; Sommer, Margot Guerra/C-4951-2013; Jasper, André/C-2772-2008	Spiekermann, Rafael/0000-0001-8341-7140; Sommer, Margot Guerra/0000-0002-9517-4593; Jasper, André/0000-0001-8143-9733	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior and Deutscher Akademischer Austauschdienst [88881.199788/201801]; CAPES (Brazil) [8107-149]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (Brazil) [444330/2014-3, 19305436/2015-5]; Alexander von Humboldt Foundation [3.4-8151/18 025]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2013/11563-6, 2016/20927-0]; CNPq [303527/2017-0]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior and Deutscher Akademischer Austauschdienst; CAPES (Brazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Alexander von Humboldt Foundation(Alexander von Humboldt Foundation); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank Mary E. C. Bernardes-de-Oliveira for providing images of the lycopsids from Sitio Volpe outcrop, and Sven Trankner for reproducing Fig. 3B-F. R. Spiekermann acknowledges Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior and Deutscher Akademischer Austauschdienst (DOUTORADO-CAPES-DAAD - 88881.199788/201801) for doctoral fellowship. A. Jasper acknowledges CAPES (Brazil 8107-149), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (Brazil -444330/2014-3; 19305436/2015-5) and Alexander von Humboldt Foundation (Germany -3.4-8151/18 025). F. RicardiBranco acknowledges Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) (grant n degrees 2013/11563-6 and 2016/20927-0), and CNPq (grant n degrees 303527/2017-0) for the PQ grant. Last but not least, we are thankful to William A. DiMichele and an anonymous reviewer for their constructive comments, which helped to improve this manuscript considerably.	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J	Valentin, E; Botelho, NF; Dantas, EL				Valentin, Eduardo; Botelho, Nilson F.; Dantas, Elton L.			Monte Santo suite, an example of Ediacaran-Cambrian deformed alkaline rocks in the Araguaia Belt, Central Brazil. Implications for Western Gondwana evolution	LITHOS			English	Article						Nepheline Syenite; Monte Santo Suite; Deformed Alkaline Rocks; Araguaia Belt; Ediacaran-cambrian; Brasiliano/Pan-African	ND ISOTOPIC EVOLUTION; NEPHELINE SYENITES; HYDROTHERMAL ALTERATION; COMPOSITIONAL VARIATION; SOLID-SOLUTION; IVREA ZONE; ZIRCON; PB; PROVINCE; CRYSTALLIZATION	Deformed alkaline rocks and carbonatites (DARCs) can be important tectonic indicators of regions that have experienced two separate events of rifting and collision, but can also represent alkaline magmas that were synkinematically emplaced along major structures and were therefore generated and deformed in the same geologic event. The Monte Santo Suite consists of two foliated and variably deformed massifs (Estrela and Monte Santo) that crop out in the Araguaia Belt and are characterized by igneous and subsolidus microstructures. In this study, we use the chemistry, mineralogy and age of the Monte Santo Suite to understand its genesis and the relations between its emplacement, the Brasiliano-Pan-African orogeny and the final evolution of Western Gondwana. The intrusions are predominantly nepheline syenite and alkali feldspar syenite. Pyroxene varies in composition from ompharite to aegirine-augite to aegirine and has mixed igneous and metamorphic characteristics. Biotite varies from phlogopite to siderophyllite to annite and presents primary, reequilibrated and neoformed trends. Amphibole varies from hastingsite to taramite. Nepheline occurs as both high-temperature and low-temperature varieties. The REE and trace element patterns display parallel trends with significant bulk content variations, positive anomalies for Nb, Ta, Zr and Hf, and negative anomalies for Ba. Sr. P and Ti in multielement diagrams, The Zr/Hf ratios for all the rocks of the massifs are similar and whole-rock epsilon(Nd) values range from -10.1 to -3.0. Trace element and isotopic data suggest that these magmas experienced extensive fractional crystallization, crustal contamination, and evolved from the same source, probably an enriched mantle. The Monte Santo Suite crystallization age is dated to 545 Ma, when these magmas were generated and deformed synkinematically with shearing along major regional faults related to the Transbrasiliano Lineament. Thus, this suite is an example of alkaline rocks generated and deformed in the same geological event throughout Western Gondwana. (C) 2020 Elsevier B.V. All rights reserved.	[Valentin, Eduardo; Botelho, Nilson F.; Dantas, Elton L.] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910909 Brasilia, DF, Brazil	Universidade de Brasilia	Valentin, E (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910909 Brasilia, DF, Brazil.	eduardovalentindossantos@gmail.com; nilsonfb@unb.br; elton@unb.br	Dantas, Elton Luiz/AAK-8464-2021; Botelho, Nilson Francisquini/T-9470-2017	Dantas, Elton Luiz/0000-0002-7954-5059; Botelho, Nilson Francisquini/0000-0001-9090-799X; Valentin dos Santos, Eduardo/0000-0003-4616-4433	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [311203/2014-0]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001, and by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) under grants 311203/2014-0. We also thank all the laboratories staff of the Institute of Geosciences of the University of Brasilia.	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J	Voll, E; Silva, AM; Pedrosa-Soares, AC				Voll, Eliane; Silva, Adalene Moreira; Pedrosa-Soares, Antonio Carlos			Tracking iron-rich rocks beneath Cenozoic tablelands: An integration of geological, airborne geophysical and remote sensing data from northern Minas Gerais State, SE Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Iron formation; Glacial ironstone; Spatial model; Fuzzy logic; Macaubas Group	SAO FRANCISCO CRATON; CARAJAS MINERAL PROVINCE; ARACUAI OROGEN; LANDSAT TM; DEPOSITS; IMAGE; AGE	Integration of multisource data has been successfully used in geological mapping and mineral exploration projects around the world. In areas covered by extensive regolith, colluvial and/or alluvial deposits, with scarce rock outcrops, the application of airborne geophysics and remote sensing products has become a key tool to unravel the geological framework and lithological units. The integration of all those data files requires the use of geographic information systems (GIS) and spatial analysis techniques. More than 87,200 km of linear-collected airborne geophysics data have been acquired by government companies to subside mineral prospecting and geological mapping in northern Minas Gerais State, SE Brazil. Together, geomorphological, geological and geophysical data outline distinct domains on the studied region. The eastern domain shows large tablelands (plateaus) sustained by metadiamictite-quartzite-rich units of the Neoproterozoic Macatibas Group and related glaciogenic iron deposits, like those of the Nova Aurora Formation, comprising hematite- and/or magnetite-rich metadiamictites with 10-60 wt% Fe. However, on tablelands, the known Neoproterozoic iron deposits are largely hidden beneath Cenozoic covers, although there are scattered outcrops of iron-rich rocks well-preserved from lateritization, a weathering process that can reach dozens of meters deep in the region. Applying Fuzzy logic methodology, our thematic maps provide great progress to define lithological units and structural trends, supporting new guides to track iron-rich rocks. The favorability maps allow us to suggest new targets, and a prospective model to trace locations and structural trends of iron-anomalous rock units. The regional model shows scattered favorable areas with few high-density concentrations of probable iron-rich rocks or even iron ore deposits. Magnetic data images disclose the main occurrences of iron-rich rocks, although lacking resolution for more specific studies. Although gammaspectrometry and Landsat 8 data only reflect responses from surface materials, they may reduce information ambiguity after integrated with magnetic data on areas covered by laterites richer in iron. Our final integrated models constrain the most favorable areas for the occurrence of iron-rich rocks, even in the large tableland domains.	[Voll, Eliane; Pedrosa-Soares, Antonio Carlos] Univ Fed Minas Gerais, Programa Posgrad Geol, CPMTC, IGC, BR-31270901 Belo Horizonte, MG, Brazil; [Silva, Adalene Moreira] Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Silva, Adalene Moreira; Pedrosa-Soares, Antonio Carlos] Brazilian Res Council CNPq, Brasilia, DF, Brazil	Universidade Federal de Minas Gerais; Universidade de Brasilia	Voll, E (autor correspondente), Univ Fed Minas Gerais, Programa Posgrad Geol, CPMTC, IGC, BR-31270901 Belo Horizonte, MG, Brazil.	eliane.voll@gmail.com; adalene@unb.br; pedrosasoares@gmail.com			CNPq (Brazilian Scientific and Technological Council); CODEMIG-CODEMGE (Company for the Development of Minas Gerais State); CAPES; CNPq	CNPq (Brazilian Scientific and Technological Council)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CODEMIG-CODEMGE (Company for the Development of Minas Gerais State); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We are grateful to the Brazilian research and development agencies CNPq (Brazilian Scientific and Technological Council) and CODEMIG-CODEMGE (Company for the Development of Minas Gerais State) for financial support to our research work in the Laboratory of Geological Mapping and Geotectonics (MGD) of the CPMTC Research Centre, UFMG - Federal University of Minas Gerais. The first author acknowledges CAPES for her doctorate scholarship, and the coauthors are grateful to CNPq for their research productivity grants. Our gratitude to Odete Alves Pedrosa for the kind help on a first English version of the original manuscript, to Benjamin J. Drenth and an anonymous reviewer for their comments, corrections, and suggestions that greatly have helped us to improve the former manuscript of this article, and to Reinhardt Fuck for his kind and careful editorial work.	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R., 1997, AGSO Journal of Australian Geology and Geophysics, V17, P201; Yousefi M, 2019, ORE GEOL REV, V111, DOI 10.1016/j.oregeorev.2019.103005; ZACCHI E.N.P., 2010, REV BRAS GEOFIS, V28, P643, DOI DOI 10.1590/S0102-261X2010000400009	75	6	6	0	10	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	AUG	2020	101								102604	10.1016/j.jsames.2020.102604	http://dx.doi.org/10.1016/j.jsames.2020.102604			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LW8CK					2023-06-23	WOS:000539370500013
J	Moreira, LS; Moreira-Turcq, P; Cordeiro, RC; Turcq, B; Aniceto, KC; Moreira-Ramirez, M; Cruz, APS; Caquineau, S; Silva, VC				Moreira, Luciane Silva; Moreira-Turcq, Patricia; Cordeiro, Renato Campello; Turcq, Bruno; Aniceto, Keila Cristina; Moreira-Ramirez, Manuel; Soares Cruz, Anna Paula; Caquineau, Sandrine; Silva, Vanessa Cunha			Climate and hydrologic controls on late Holocene sediment supply to an Amazon floodplain lake	JOURNAL OF PALEOLIMNOLOGY			English	Article						Floodplain lakes; Paleoclimate; Late Holocene; Sediment organic matter	GRASS ECHINOCHLOA-POLYSTACHYA; LAST GLACIAL MAXIMUM; ENVIRONMENTAL-CHANGES; ORGANIC-MATTER; LLANOS ORIENTALES; SOLIMOES RIVER; CARBON; BASIN; RECORD; DYNAMICS	Organic and inorganic geochemical analyses on sediments from Preto Lake, a central Amazon basin floodplain water body, were used to document hydrological changes of the Solimoes River during the late Holocene. Between 3600 and 400 cal yr BP, Preto Lake received smectite-rich sediment from the Solimoes River, with high concentrations of Al (similar to 53 x 10(3) ppm) and Si (similar to 210 x 10(3) ppm). The high detrital input suggests there was a direct connection between Preto Lake and the main river channel. High river inflow maintained lake stage and was responsible for the contribution to sediments of phytoplankton-derived organic matter. Low sediment organic carbon concentrations characterized this period (mean similar to 3.8 wt%), probably because of dilution by river-borne lithogenic matter. Although the river inputs remained high, abrupt increases in TOC content around 1800 and 1200 cal yr BP suggest brief increases in fluvial nutrient supply to Preto Lake. During the last 400 cal yr, substantial declines in smectite (mean 40%), Al (similar to 29 x 10(3) ppm) and Si (138 x 10(3) ppm) suggest the establishment of a semi-isolated lake, with reduced river inflow. A large proportion of C3-plant-derived organic matter, supplied by runoff from the kaolinite-rich watershed, was observed during this period, and was accompanied by high autochthonous primary production, driven by development of an aquatic macrophyte community. This change in sediment organic matter source accounted for the greater TOC content (similar to 20%) of sediments deposited during this period. Although Holocene climate change was an important control on fluvial sediment supply to upper and lower Amazon Basin floodplain lakes, sedimentation processes in Preto Lake can also be linked to changes in the river's course. The transition to a semi-isolated lake could have been a consequence of lateral and vertical sediment accretion, which formed a natural levee that blocked fluvial input to Preto Lake.	[Moreira, Luciane Silva; Cordeiro, Renato Campello; Moreira-Ramirez, Manuel] Univ Fed Fluminense UFF, Dept Geoquim, Programa Posgrad Geociencias, Niteroi, RJ, Brazil; [Moreira-Turcq, Patricia] Inst Rech Dev IRD, GET Geosci Environm Toulouse, Bondy, France; [Turcq, Bruno; Caquineau, Sandrine] Inst Rech Dev IRD, LOCEAN Lab Oceanog & Climat, Bondy, France; [Aniceto, Keila Cristina; Silva, Vanessa Cunha] Univ Fed Amazonas, Programa Posgrad Geociencias, Manaus, Amazonas, Brazil; [Soares Cruz, Anna Paula] Calif State Univ Bakersfield, Dept Geol Sci, 9001 Stockdale Highway, Bakersfield, CA 93311 USA	Universidade Federal Fluminense; Institut de Recherche pour le Developpement (IRD); Institut de Recherche pour le Developpement (IRD); UDICE-French Research Universities; Sorbonne Universite; Universidade Federal de Amazonas; California State University System; California State University Bakersfield	Moreira, LS (autor correspondente), Univ Fed Fluminense UFF, Dept Geoquim, Programa Posgrad Geociencias, Niteroi, RJ, Brazil.	lucianebiouff@gmail.com; Patricia.Turcq@ird.fr; rcampello@yahoo.com; Bruno.Turcq@ird.fr; keilaniceto@ufam.edu.br; manuelmoreira@id.uff.br; acruz72@csub.edu; sandrine.caquineau@ird.fr; wanessavc01@gmail.com	Cordeiro, Renato C/J-8870-2013; Moreira, luciane Silva/AAF-9913-2021	Cordeiro, Renato C/0000-0002-6785-601X; Moreira, luciane Silva/0000-0002-8721-8752; Soares Cruz, Anna Paula/0000-0002-4890-0580; Aniceto, Keila/0000-0001-8258-1328	French Research Institute for Development (IRD); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	French Research Institute for Development (IRD); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This research was supported by the French Research Institute for Development (IRD) and by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001. We are also grateful for the comments from the reviewers that helped us improve this paper.	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Paleolimn.	DEC	2020	64	4					389	403		10.1007/s10933-020-00144-y	http://dx.doi.org/10.1007/s10933-020-00144-y		JUL 2020	15	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	NZ0ZA					2023-06-23	WOS:000554058500002
J	Ketzer, M; Praeg, D; Rodrigues, LF; Augustin, A; Pivel, MAG; Rahmati-Abkenar, M; Miller, DJ; Viana, AR; Cupertino, JA				Ketzer, Marcelo; Praeg, Daniel; Rodrigues, Luiz F.; Augustin, Adolpho; Pivel, Maria A. G.; Rahmati-Abkenar, Mahboubeh; Miller, Dennis J.; Viana, Adriano R.; Cupertino, Jose A.			Gas hydrate dissociation linked to contemporary ocean warming in the southern hemisphere	NATURE COMMUNICATIONS			English	Article							METHANE RELEASE; SEA-FLOOR; ANAEROBIC OXIDATION; WEST SVALBARD; STABILITY; SEDIMENTS; EMISSIONS; MARGIN; BASIN; EXAMPLES	Ocean warming related to climate change has been proposed to cause the dissociation of gas hydrate deposits and methane leakage on the seafloor. This process occurs in places where the edge of the gas hydrate stability zone in sediments meets the overlying warmer oceans in upper slope settings. Here we present new evidence based on the analysis of a large multi-disciplinary and multi-scale dataset from such a location in the western South Atlantic, which records massive gas release to the ocean. The results provide a unique opportunity to examine ocean-hydrate interactions over millennial and decadal scales, and the first evidence from the southern hemisphere for the effects of contemporary ocean warming on gas hydrate stability. Widespread hydrate dissociation results in a highly focused advective methane flux that is not fully accessible to anaerobic oxidation, challenging the assumption that it is mostly consumed by sulfate reduction before reaching the seafloor.	[Ketzer, Marcelo; Rahmati-Abkenar, Mahboubeh] Linnaeus Univ, Dept Biol & Environm Sci, Fac Hlth & Life Sci, SE-39181 Kalmar, Sweden; [Praeg, Daniel] Geoazur, 250 Rue Albert Einstein, F-06560 Valbonne, France; [Praeg, Daniel; Rodrigues, Luiz F.; Augustin, Adolpho; Cupertino, Jose A.] Pontificia Univ Catolica Rio Grande do Sul, Petr & Nat Resources Inst, BR-91619900 Porto Alegre, RS, Brazil; [Pivel, Maria A. G.] Univ Fed Rio Grande do Sul, Inst Geociencias, BR-91509900 Porto Alegre, RS, Brazil; [Miller, Dennis J.; Viana, Adriano R.] Petrobras Petr Brasileiro SA, BR-20031170 Rio De Janeiro, Brazil	Linnaeus University; UDICE-French Research Universities; Universite Cote d'Azur; Observatoire de la Cote d'Azur; Pontificia Universidade Catolica Do Rio Grande Do Sul; Universidade Federal do Rio Grande do Sul; Petrobras	Ketzer, M (autor correspondente), Linnaeus Univ, Dept Biol & Environm Sci, Fac Hlth & Life Sci, SE-39181 Kalmar, Sweden.	marcelo.ketzer@lnu.se	Pivel, Maria Alejandra Gomez/F-5594-2013; CNRS, Géoazur UMR7329/AAB-9070-2020; Ketzer, Marcelo/AAS-3282-2020; Rodrigues, Luiz Frederico/B-3409-2014; Rahmati-Abkenar, Mahboubeh/N-9990-2016	Pivel, Maria Alejandra Gomez/0000-0003-3226-8047; CNRS, Géoazur UMR7329/0000-0003-1107-3128; Ketzer, Marcelo/0000-0003-4796-8177; Rodrigues, Luiz Frederico/0000-0001-5960-4843; Miller, Dennis James/0000-0002-8587-4182; Rahmati-Abkenar, Mahboubeh/0000-0002-3193-9331; Cupertino, Jose Antonio/0000-0002-1684-1870	International Ocean Discovery Program pre-study project (IODP) [910-Full2]; Faculty of Health and Life Sciences (Linnaeus University); European Union [656821]; Brazilian Coordination of Superior Level Staff Improvement CAPES-IODP (2018-2019); Linnaeus University	International Ocean Discovery Program pre-study project (IODP); Faculty of Health and Life Sciences (Linnaeus University); European Union(European CommissionSpanish Government); Brazilian Coordination of Superior Level Staff Improvement CAPES-IODP (2018-2019); Linnaeus University	This publication results from major efforts by several actors during the CONEGAS project (2010-2019) to investigate gas hydrate occurrences in the Rio Grande Cone. We thank the Brazilian National Petroleum Agency (ANP) for allowing us to use seismic data under the scope of the International Ocean Discovery Program pre-study project (IODP proposal no. 910-Full2). We thank PETROBRAS for permission to publish data of the CONEGAS project. We also thank crew members of missions MD186 and MD195 (research vessel Marion Dufresne), and NR12 (support vessel Rig Supporter). M.K. thanks the Faculty of Health and Life Sciences (Linnaeus University) for financial support. D.P. acknowledges funding from the European Union's Horizon 2020 research and innovation program under Marie Skodowska-Curie grant agreement no. 656821, and from the Brazilian Coordination of Superior Level Staff Improvement CAPES-IODP (2018-2019). Open access funding provided by Linnaeus University.	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Commun.	JUL 29	2020	11	1							3788	10.1038/s41467-020-17289-z	http://dx.doi.org/10.1038/s41467-020-17289-z			9	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	MY8CD	32728027	Green Published, Green Submitted, gold			2023-06-23	WOS:000558642500008
J	Hou, A; Bahr, A; Raddatz, J; Voigt, S; Greule, M; Albuquerque, AL; Chiessi, CM; Friedrich, O				Hou, Alicia; Bahr, Andre; Raddatz, Jacek; Voigt, Silke; Greule, Markus; Albuquerque, Ana Luiza; Chiessi, Cristiano M.; Friedrich, Oliver			Insolation and Greenhouse Gas Forcing of the South American Monsoon System Across Three Glacial-Interglacial Cycles	GEOPHYSICAL RESEARCH LETTERS			English	Article							HIGH-RESOLUTION; ASIAN MONSOON; ATMOSPHERIC CIRCULATION; PLANKTONIC-FORAMINIFERA; TEMPERATURE-GRADIENTS; MILLENNIAL-SCALE; LATE PLEISTOCENE; DONGGE CAVE; CLIMATE; ATLANTIC	Precipitation extremes with devastating socioeconomic consequences within the South American Monsoon System (SAMS) are expected to become more frequent in the near future. The complexity in SAMS behavior, however, poses severe challenges for reliable future projections. Thus, robust paleomonsoon records are needed to constrain the high spatiotemporal variability in the response of SAMS rainfall to different climatic drivers. This study uses Ti/Ca ratios from X-ray fluorescence scanning of a sediment core retrieved off eastern Brazilian to trace precipitation changes over the past 322 Kyr. The results indicate that despite the spatiotemporal complexity of the SAMS, insolation forcing is the primary pacemaker of variations in the monsoonal system. Additional modulation by atmosphericpCO(2)suggests that SAMS intensity over eastern Brazil will be suppressed by rising CO(2)emissions in the future. Lastly, our record reveals an unprecedented strong and persistent wet period during Marine Isotope Stage 6 driven by anomalously strong trade winds.	[Hou, Alicia; Bahr, Andre; Greule, Markus; Friedrich, Oliver] Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany; [Raddatz, Jacek; Voigt, Silke] Goethe Univ Frankfurt, Inst Geosci, Frankfurt, Germany; [Albuquerque, Ana Luiza] Univ Fed Fluminense, Programa Geociencias Geoquim, Niteroi, RJ, Brazil; [Chiessi, Cristiano M.] Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, Brazil	Ruprecht Karls University Heidelberg; Goethe University Frankfurt; Universidade Federal Fluminense; Universidade de Sao Paulo	Hou, A (autor correspondente), Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany.	alicia.hou@geow.uni-heidelberg.de	Voigt, Silke/G-7270-2017; Chiessi, Cristiano Mazur/E-1916-2012; Albuquerque, Ana Luiza S/C-5167-2013	Voigt, Silke/0000-0002-2560-5933; Chiessi, Cristiano Mazur/0000-0003-3318-8022; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Raddatz, Jacek/0000-0002-5713-9682; Greule, Markus/0000-0002-9958-8371; Hou, Alicia Meng Xiao/0000-0003-3590-8679	Deutsche Forschungsgemeinschaft (DFG) [BA 3809/9-1]; FAPESP [2018/15123-4]; CAPES [564/2015, 88881.313535/2019-01]; CNPq [302607/2016-1, 422255/2016-5]; Alexander von Humboldt Foundation	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Alexander von Humboldt Foundation(Alexander von Humboldt Foundation)	We kindly acknowledge the captain and crew of the R/V METEOR during Expedition M125. We thank Stefanie Kaboth-Bahr for assistance with XRF scanning, Robert van Geldern for help with water isotope analysis, and Bernd Knape and Frank Keppler for support during foraminiferal stable isotope measurements. A. B. was funded by the Deutsche Forschungsgemeinschaft (DFG) (Grant BA 3809/9-1). C. M. C. was funded by FAPESP (Grant 2018/15123-4), CAPES (Grants 564/2015 and 88881.313535/2019-01), CNPq (Grants 302607/2016-1 and 422255/2016-5), and the Alexander von Humboldt Foundation.	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J	Silva, CRE; Smoak, JM; da Silva, EV				e Silva, Camila Rodrigues; Smoak, Joseph M.; da Silva-Filho, Emmanoel Vieira			Residential radon exposure and seasonal variation in the countryside of southeastern Brazil	ENVIRONMENTAL MONITORING AND ASSESSMENT			English	Article						Indoor radon concentration; Effective dose; Meteorological parameters; RAD7	INDOOR RADON; WATER-QUALITY; RURAL AREA; RN-222; VARIABILITY; PARAMETERS; DWELLINGS; URBAN	Poorly ventilated environments such as residences can accumulate radon gas to levels that are harmful to humans and thus produce a public health risk. To assess the risk from natural radiation due to indoor radon exposure,Rn-222 measurements, using an alpha RAD7 detector, were conducted in Timoteo, Minas Gerais state, southeastern Brazil. Indoor radon concentrations, along with meteorological parameters, were measured every 2 h during both wet and dry seasons in 2017 and 2018. The mean concentration of indoor radon varied between 18.0 and 412.8 Bq m(-3), which corresponded to an effective annual dose of 1.2 and 7.6 mSv y(-1). Average radon concentrations were significantly higher during the winter dry season, and there was a strong positive correlation with humidity in both wet and dry season. Furthermore, concentrations showed an inverse correlation with atmospheric pressure, wind speed, air temperature, and solar radiation. The radon levels are generally above the limits recommended by international standards, meaning that mitigation measures are needed to improve air quality to reduce human exposure and risk. Finally, through the statistical analysis, it was possible to determine the differences and similarities between the sampling points concerning the geology of the place and the geographical location.	[e Silva, Camila Rodrigues; da Silva-Filho, Emmanoel Vieira] Fluminense Fed Univ, Chem Inst, Postgrad Program Geosci Environm Geochem, BR-24020141 Niteroi, RJ, Brazil; [Smoak, Joseph M.] Univ S Florida, Sch Geosci, St Petersburg, FL 33701 USA	Universidade Federal Fluminense; State University System of Florida; University of South Florida	Silva, CRE (autor correspondente), Fluminense Fed Univ, Chem Inst, Postgrad Program Geosci Environm Geochem, BR-24020141 Niteroi, RJ, Brazil.	camilae@id.uff.br	Smoak, Joseph/E-2140-2012; da Silva Filho, Emmanoel Vieira/Y-7281-2019	Smoak, Joseph/0000-0002-4322-4042; da Silva Filho, Emmanoel Vieira/0000-0001-6444-6851; Silva, Camila/0000-0002-1063-3333	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) [001]; PRINT-UFF-FEEDBACKS Project [CAPES 88887.310301/2018-00]; Foundation for Research Support of the State of Rio de Janeiro [FAPERJ E-26/203.037/2017]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); PRINT-UFF-FEEDBACKS Project; Foundation for Research Support of the State of Rio de Janeiro	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) - Finance Code 001. The authors are also grateful for the support of the PRINT-UFF-FEEDBACKS Project (grant CAPES 88887.310301/2018-00). E. Silva-Filho is a senior researcher of the National Council for Research and Development (CNPq, Brazil) and the Foundation for Research Support of the State of Rio de Janeiro (FAPERJ E-26/203.037/2017).	[Anonymous], 1998, MEASUREMENT RADON RA; Asher-Bolinder S, 1991, FIELD STUDIES RADON, P23; Barazza F, 2015, RADIAT PROT DOSIM, V167, P75, DOI 10.1093/rpd/ncv209; Brasil, 2016, BRAZ MET STAT YB; Brasil, 2013, PROJ PLAN POC CALD P; Chege MW, 2009, J RADIOL PROT, V29, P95, DOI 10.1088/0952-4746/29/1/007; CPRM (Companhia de Pesquisa De Recursos Minerais. Servico Geologico Do Brasil), 2000, PROJ LEST MAP GEOL C; Durridge, 2016, RAD7 US MAN; Fior L., 2008, THESIS; Geraldo L.P., 2005, SP RADIOL BRAS, V38, P283, DOI DOI 10.1590/50100-39842005000400010; Hoffmann M, 2017, RADIAT PROT DOSIM, V175, P186, DOI 10.1093/rpd/ncw284; Hongyu K.U.A.N.G., 2015, ENG SCI, V5, P83, DOI DOI 10.18607/ES201653398; ICRP, 1993, ICRP PUBL, V65; ICRP International Commission on Radiological Protection, 1993, ANN ICRP, V23, P65; Idriss H, 2015, INDOOR BUILT ENVIRON, V24, P650, DOI 10.1177/1420326X14528190; Jilek K, 2014, RADIAT PROT DOSIM, V160, P57, DOI 10.1093/rpd/ncu091; Klumb-Oliveira A.A., 1999, P NAT S TECHN STUD; Klumb-Oliveira A.A., 2002, THESIS; Leghrouz AA, 2012, RADIAT PROT DOSIM, V148, P268, DOI 10.1093/rpd/ncr013; Lima RD, 2009, QUIM NOVA, V32, P263, DOI 10.1590/S0100-40422009000100044; Magalhaes MH, 2003, J ENVIRON RADIOACTIV, V67, P131, DOI 10.1016/S0265-931X(02)00175-3; Marley F, 2001, ATMOS ENVIRON, V35, P5347, DOI 10.1016/S1352-2310(01)00272-2; Martins LMO, 2016, ECOTOX ENVIRON SAFE, V133, P164, DOI 10.1016/j.ecoenv.2016.07.009; Mehra R, 2016, RADIAT PROT DOSIM, V171, P208, DOI 10.1093/rpd/ncw060; Minkin L, 2016, SCI TOTAL ENVIRON, V565, P1, DOI 10.1016/j.scitotenv.2016.04.131; Nonato EA, 2007, QUIM NOVA, V30, P797, DOI 10.1590/S0100-40422007000400008; Park TH, 2018, ENVIRON SCI POLLUT R, V25, P12678, DOI 10.1007/s11356-018-1531-3; Podstawczynska A, 2016, ATMOS ENVIRON, V126, P225, DOI 10.1016/j.atmosenv.2015.11.037; Podstawczynska A, 2010, NUKLEONIKA, V55, P543; Singh KP, 2004, WATER RES, V38, P3980, DOI 10.1016/j.watres.2004.06.011; Singh S, 2005, ATMOS ENVIRON, V39, P7761, DOI 10.1016/j.atmosenv.2005.08.030; Sun Quanfu, 2002, Radioisotopes, V51, P120, DOI 10.3769/radioisotopes.51.120; Tchorz-Trzeciakiewicz DE, 2017, SCI TOTAL ENVIRON, V584, P911, DOI [10.1016/j.scitotenv.2017.01.137, 10.1016/j.scitotenv2017.01.137]; Tchorz-Trzeciakiewicz DE, 2011, GEOCHEM J, V45, P455; Tchorz-Trzeciakiewicz DE, 2012, J ELEMENTOL, V17, P317, DOI 10.5601/jelem.2012.17.2.13; Trindade A. L. C, 2013, THESIS; Tung TCW, 2005, RADIAT MEAS, V40, P110, DOI 10.1016/j.radmeas.2004.12.016; United Nations Scientific Committee on the Effects of Atomic Radiation (UNSCEAR), 2000, SOURCES EFFECTS RISK; United States Environmental Protection Agency. Radon measurement in Schools, 1993, 402R92014 EPA; US EPA, 2003, 402R03003 US EPA OFF; World Health Organization, 2009, WHO HDB INDOOR RADON; Wysocka M, 2005, J ENVIRON RADIOACTIV, V82, P351, DOI 10.1016/j.jenvrad.2005.02.009; Xie D, 2015, RADIAT MEAS, V82, P52, DOI 10.1016/j.radmeas.2015.08.008	43	3	3	0	9	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0167-6369	1573-2959		ENVIRON MONIT ASSESS	Environ. Monit. Assess.	JUL 26	2020	192	8							544	10.1007/s10661-020-08513-w	http://dx.doi.org/10.1007/s10661-020-08513-w			14	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	MP5TB	32715319				2023-06-23	WOS:000552265700001
J	Nascimento, JR; Easson, CG; Jurelevicius, DD; Lopez, JV; Bidone, ED; Sabadini-Santos, E				Nascimento, Juliana R.; Easson, Cole G.; Jurelevicius, Diogo de A.; Lopez, Jose, V; Bidone, Edison D.; Sabadini-Santos, Elisamara			Microbial community shift under exposure of dredged sediments from a eutrophic bay	ENVIRONMENTAL MONITORING AND ASSESSMENT			English	Article						Guanabara Bay; Risk assessment; Quality ratio; Enzymes; Sequencing	RIO-DE-JANEIRO; GRADIENT GEL-ELECTROPHORESIS; GUANABARA-BAY; BACTERIAL COMMUNITIES; HEAVY-METALS; MARINE-SEDIMENTS; TOXICITY; SOIL; MANAGEMENT; ESTUARINE	Microbial communities occur in almost every habitat. To evaluate the homeostasis disruption of in situ microbiomes, dredged sediments from Guanabara Bay-Brazil (GB) were mixed with sediments from outside of the bay (D) in three different proportions (25%, 50%, and 75%) which we called GBD25, GBD50, and GBD75. Grain size, TOC, and metals-as indicators of complex contamination-dehydrogenase (DHA) and esterase enzymes (EST)-as indicators of microbial community availability-were determined. Microbial community composition was addressed by amplifying the 16S rRNA gene for DGGE analysis and sequencing using MiSeq platform (Illumina).We applied the quality ratio index (QR) to the GB, D, and every GBD mixture to integrate geochemical parameters with our microbiome data. QR indicated high environmental risk for GB and every GBD mixture, and low risk for D. The community shifted from aerobic to anaerobic profile, consistent with the characteristics of GB. Sample D was dominated byJTB255marine benthic group, related to low impacted areas.Milano-WF1B-44was the most representative of GB, often found in anaerobic and sulfur enriched environments. In GBD, the denitrifying sulfur-oxidizing bacteria,Sulfurovum, was the most representative, typically found in suboxic or anoxic niches. The canonical correspondence analysis was able to explain 60% of the community composition variation and exhibit the decrease of environmental quality as the contamination increases. Physiological and taxonomic shifts of the microbial assemblage in sediments were inferred by QR, which was suitable to determine sediment risk. The study produced sufficient information to improve the dredging plan and management.	[Nascimento, Juliana R.; Bidone, Edison D.; Sabadini-Santos, Elisamara] Univ Fed Fluminense, Inst Quim, Programa Posgrad Geociencias Geoquim, BR-24020150 Niteroi, RJ, Brazil; [Easson, Cole G.; Lopez, Jose, V] Nova Southeastern Univ, Halmos Coll Nat Sci & Oceanog, Dania, FL 33004 USA; [Easson, Cole G.] Middle Tennessee State Univ, Biol Dept, Murfreesboro, TN 37130 USA; [Jurelevicius, Diogo de A.] Univ Fed Rio de Janeiro, Ctr Ciencias Saude, Inst Microbiol Prof Paulo de Goes, BR-21944570 Rio De Janeiro, RJ, Brazil	Universidade Federal Fluminense; Nova Southeastern University; Middle Tennessee State University; Universidade Federal do Rio de Janeiro	Nascimento, JR (autor correspondente), Univ Fed Fluminense, Inst Quim, Programa Posgrad Geociencias Geoquim, BR-24020150 Niteroi, RJ, Brazil.	ju_0812@hotmaill.com	Bidone, Edison/AAE-9527-2021; Sabadini-Santos, Elisamara/AAD-3407-2021; Jurelevicius, Diogo A/I-8235-2014	Bidone, Edison/0000-0002-5771-5651; Sabadini-Santos, Elisamara/0000-0003-3783-4554; Jurelevicius, Diogo A/0000-0002-5719-5713; Nascimento, Juliana/0000-0003-2325-2684	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (Programa de Doutorado Sanduiche no Exterior) [88881.135581/2016-01]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq/Universal) [449631/2014-1]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq/PDJ) [155406/2018-3]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (Programa de Doutorado Sanduiche no Exterior); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq/Universal)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq/PDJ)	This study was financed by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES/Finance Code 001 and Programa de Doutorado Sanduiche no Exterior no. 88881.135581/2016-01) and by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq/Universal no 449631/2014-1 and CNPq/PDJ no. 155406/2018-3).	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Monit. Assess.	JUL 23	2020	192	8							539	10.1007/s10661-020-08507-8	http://dx.doi.org/10.1007/s10661-020-08507-8			16	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	MO4SJ	32705349				2023-06-23	WOS:000551517600001
J	Ardelean, CF; Becerra-Valdivia, L; Pedersen, MW; Schwenninger, JL; Oviatt, CG; Macias-Quintero, JI; Arroyo-Cabrales, J; Sikora, M; Ocampo-Diaz, YZE; Rubio-Cisneros, II; Watling, JG; de Medeiros, VB; De Oliveira, PE; Barba-Pingaron, L; Ortiz-Butron, A; Blancas-Vazquez, J; Rivera-Gonzalez, I; Solis-Rosales, C; Rodriguez-Ceja, M; Gandy, DA; Navarro-Gutierrez, Z; De La Rosa-Diaz, JJ; Huerta-Arellano, V; Marroquin-Fernandez, MB; Martinez-Riojas, LM; Lopez-Jimenez, A; Higham, T; Willerslev, E				Ardelean, Ciprian F.; Becerra-Valdivia, Lorena; Pedersen, Mikkel Winther; Schwenninger, Jean-Luc; Oviatt, Charles G.; Macias-Quintero, Juan I.; Arroyo-Cabrales, Joaquin; Sikora, Martin; Ocampo-Diaz, Yam Zul E.; Rubio-Cisneros, Igor I.; Watling, Jennifer G.; de Medeiros, Vanda B.; De Oliveira, Paulo E.; Barba-Pingaron, Luis; Ortiz-Butron, Agustin; Blancas-Vazquez, Jorge; Rivera-Gonzalez, Iran; Solis-Rosales, Corina; Rodriguez-Ceja, Maria; Gandy, Devlin A.; Navarro-Gutierrez, Zamara; de la Rosa-diaz, Jesus J.; Huerta-Arellano, Vladimir; Marroquin-Fernandez, Marco B.; Martinez-Riojas, L. Martin; Lopez-Jimenez, Alejandro; Higham, Thomas; Willerslev, Eske			Evidence of human occupation in Mexico around the Last Glacial Maximum	NATURE			English	Article							SINGLE-ALIQUOT; PHYTOLITH ASSEMBLAGES; RADIOCARBON; QUARTZ; AMS; RESIDUES; HOLOCENE; RECORDS; PLANT; DNA	Chiquihuite Cave (Zacatecas, Mexico) provides evidence of human presence in the Americas between about 33,000-31,000 and 14,000-12,000 years ago, and expands the cultural variability known from sites of this date. The initial colonization of the Americas remains a highly debated topic(1), and the exact timing of the first arrivals is unknown. The earliest archaeological record of Mexico-which holds a key geographical position in the Americas-is poorly known and understudied. Historically, the region has remained on the periphery of research focused on the first American populations(2). However, recent investigations provide reliable evidence of a human presence in the northwest region of Mexico(3,4), the Chiapas Highlands(5), Central Mexico(6)and the Caribbean coast(7-9)during the Late Pleistocene and Early Holocene epochs. Here we present results of recent excavations at Chiquihuite Cave-a high-altitude site in central-northern Mexico-that corroborate previous findings in the Americas(10-17)of cultural evidence that dates to the Last Glacial Maximum (26,500-19,000 years ago)(18), and which push back dates for human dispersal to the region possibly as early as 33,000-31,000 years ago. The site yielded about 1,900 stone artefacts within a 3-m-deep stratified sequence, revealing a previously unknown lithic industry that underwent only minor changes over millennia. More than 50 radiocarbon and luminescence dates provide chronological control, and genetic, palaeoenvironmental and chemical data document the changing environments in which the occupants lived. Our results provide new evidence for the antiquity of humans in the Americas, illustrate the cultural diversity of the earliest dispersal groups (which predate those of the Clovis culture) and open new directions of research.	[Ardelean, Ciprian F.; Navarro-Gutierrez, Zamara; de la Rosa-diaz, Jesus J.; Huerta-Arellano, Vladimir; Martinez-Riojas, L. Martin] Univ Autonoma Zacatecas, Unidad Acad Antropol, Zacatecas, Zacatecas, Mexico; [Ardelean, Ciprian F.] Univ Exeter, Dept Archaeol, Exeter, Devon, England; [Becerra-Valdivia, Lorena; Schwenninger, Jean-Luc; Higham, Thomas] Univ Oxford, Res Lab Archaeol & Hist Art, Oxford, England; [Becerra-Valdivia, Lorena] Univ New South Wales, Chronos Cycle Facil 14C, SSEAU, Sydney, NSW, Australia; [Pedersen, Mikkel Winther; Sikora, Martin; Willerslev, Eske] Univ Copenhagen, Lundbeck Fdn GeoGenet Ctr, Copenhagen, Denmark; [Oviatt, Charles G.] Kansas State Univ, Dept Geol, Manhattan, KS 66506 USA; [Macias-Quintero, Juan I.; Marroquin-Fernandez, Marco B.] Univ Ciencias & Artes Chiapas, Escuela Arqueol, Tuxtla Gutierrez, Mexico; [Arroyo-Cabrales, Joaquin; Lopez-Jimenez, Alejandro] Inst Nacl Antropol & Hist, Lab Arqueozool, Subdirecc Lab & Apoyo Acad, Mexico City, DF, Mexico; [Ocampo-Diaz, Yam Zul E.] Univ Autonoma San Luis Potosi, Fac Ingn, San Luis Potosi, San Luis Potosi, Mexico; [Ocampo-Diaz, Yam Zul E.; Rubio-Cisneros, Igor I.] Grp Geol Exogena & Sedimentario, San Luis Potosi, San Luis Potosi, Mexico; [Watling, Jennifer G.] Univ Sao Paulo, Lab Arqueol Trop, Museu Arqueol & Etnol, Sao Paulo, Brazil; [de Medeiros, Vanda B.; De Oliveira, Paulo E.] Univ Sao Paulo, Inst Geociencias, Lab Micropaleontol, Sao Paulo, Brazil; [De Oliveira, Paulo E.] Field Museum Nat Hist, Bot Dept, Chicago, IL 60605 USA; [Barba-Pingaron, Luis; Ortiz-Butron, Agustin; Blancas-Vazquez, Jorge] Univ Nacl Autonoma Mexico, Inst Invest Antropol IIA, Lab Prospecc Arqueol, Mexico City, DF, Mexico; [Rivera-Gonzalez, Iran] Escuela Nacl Antropol Hist ENAH, Lab Palinol, Mexico City, DF, Mexico; [Solis-Rosales, Corina; Rodriguez-Ceja, Maria] Univ Nacl Autonoma Mexico, Inst Fis, Lab Espectrometria Masas Con Acelerador, Mexico City, DF, Mexico; [Gandy, Devlin A.] Univ Cambridge, Dept Archaeol, Cambridge, England; [Willerslev, Eske] Sanger Inst, Welcome Trust, Hinxton, England; [Willerslev, Eske] Univ Southern Denmark, Danish Inst Adv Study, Odense, Denmark; [Willerslev, Eske] Univ Cambridge, Dept Zool, Cambridge, England	Universidad Autonoma de Zacatecas; University of Exeter; University of Oxford; University of New South Wales Sydney; University of Copenhagen; Kansas State University; Universidad Autonoma de San Luis Potosi; Universidade de Sao Paulo; Universidade de Sao Paulo; Field Museum of Natural History (Chicago); Universidad Nacional Autonoma de Mexico; Universidad Nacional Autonoma de Mexico; University of Cambridge; Wellcome Trust Sanger Institute; University of Southern Denmark; University of Cambridge	Ardelean, CF (autor correspondente), Univ Autonoma Zacatecas, Unidad Acad Antropol, Zacatecas, Zacatecas, Mexico.; Ardelean, CF (autor correspondente), Univ Exeter, Dept Archaeol, Exeter, Devon, England.; Willerslev, E (autor correspondente), Univ Copenhagen, Lundbeck Fdn GeoGenet Ctr, Copenhagen, Denmark.; Willerslev, E (autor correspondente), Sanger Inst, Welcome Trust, Hinxton, England.; Willerslev, E (autor correspondente), Univ Southern Denmark, Danish Inst Adv Study, Odense, Denmark.; Willerslev, E (autor correspondente), Univ Cambridge, Dept Zool, Cambridge, England.	aeci000206@uaz.edu.mx; ewillerslev@sund.ku.dk	Willerslev, Eske/A-9619-2011; Sikora, Martin/C-8609-2015; Willerslev, Eske/AAA-5686-2019; Ocampo-Diaz, Yam Zul Ernesto/A-2025-2013; Ocampo-Díaz, Yam Zul Ernesto/GQP-2454-2022; Ardelean, Ciprian F./AER-1665-2022; Pedersen, Mikkel Winther/GSN-8119-2022; Pedersen, Mikkel Winther/A-8151-2014	Willerslev, Eske/0000-0002-7081-6748; Sikora, Martin/0000-0003-2818-8319; Ocampo-Diaz, Yam Zul Ernesto/0000-0002-4695-442X; Ardelean, Ciprian F./0000-0002-0225-8107; Pedersen, Mikkel Winther/0000-0002-7291-8887; Macias Quintero, Juan Ignacio/0000-0001-5924-1309; Rivera, Iran/0000-0002-1098-423X; Gandy, Devlin/0000-0003-2253-6837; Becerra-Valdivia, Lorena/0000-0001-5501-5347	Government of the State of Zacatecas, through the Consejo Zacatecano de Ciencia, Tecnologia e Innovacion (COZCyT); CONACYT grant [CB-2016-286130]; NERC Radiocarbon Facility (NRCF); Merton College, Santander; Clarendon Fund; Lundbeck Foundation; Novo Nordic Foundation; Wellcome Trust Foundation; Carlsberg Foundation; Danish National Research Foundation; Lundbeck Foundation [R155-2013-16338] Funding Source: researchfish	Government of the State of Zacatecas, through the Consejo Zacatecano de Ciencia, Tecnologia e Innovacion (COZCyT); CONACYT grant(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); NERC Radiocarbon Facility (NRCF); Merton College, Santander; Clarendon Fund; Lundbeck Foundation(Lundbeckfonden); Novo Nordic Foundation(Novo Nordisk Foundation); Wellcome Trust Foundation(Wellcome Trust); Carlsberg Foundation(Carlsberg Foundation); Danish National Research Foundation(Danmarks Grundforskningsfond); Lundbeck Foundation(Lundbeckfonden)	The field explorations and part of the laboratory studies were made possible by the special sponsorship from the Government of the State of Zacatecas, through the Consejo Zacatecano de Ciencia, Tecnologia e Innovacion (COZCyT); we thank its consecutive directors, G. A. Mercado-Sanchez and A. Enciso-Munoz, and the Governor of Zacatecas, A. Tello-Cristerna. Seed money for cave exploration came from the Center for American Paleolithic Research (CAPR); we thank S. Holen, K. Holen and the members of the board. Fieldwork, laboratory analyses and publication expenses were partially covered by CONACYT grant CB-2016-286130. The Concepcion del Oro municipality, and A. Maldonado-Falcon, offered administrative and occasional financial assistance. Radiocarbon work at Oxford was supported by the NERC Radiocarbon Facility (NRCF), Merton College, Santander and the Clarendon Fund. We thank all colleagues at the ORAU. D. Peat contributed greatly to laboratory preparation of OSL samples. A. Ocana and I. Alarcon participated in the identification of animal bones. The environmental DNA work was supported by the Lundbeck Foundation, the Novo Nordic Foundation, the Wellcome Trust Foundation, the Carlsberg Foundation and the Danish National Research Foundation. 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J	Sayao, E; Franca, GS; Holanda, M; Goncalves, A				Sayao, Eveline; Franca, George Sand; Holanda, Maristela; Goncalves, Alexandro			Spatial database and website for reservoir-triggered seismicity in Brazil	NATURAL HAZARDS AND EARTH SYSTEM SCIENCES			English	Article								After confirming that impoundment of large reservoirs could cause earthquakes, studies on reservoir-triggered seismicity (RTS) have had a considerable scientific incentive. Most of the studies determined that the vertical load increase due to reservoir load, and the reduction of effective force due to the increase in pore pressure, can modify the stress field in the reservoir region, possibly triggering earthquakes. In addition, the RTS is conditioned by several factors such as pre-existing tectonic stresses, reservoir height/weight, area-specific geological and hydromechanical conditions, constructive interaction between the orientation of seismotectonic forces, and additional load caused by the reservoir. One of the major challenges in studying RTS is to identify and correlate the factors in the area of influence of the reservoir, capable of influencing the RTS process itself. A spatial seismicity-triggered reservoir database was created to facilitate the research in this field, based on the specifications of the national spatial data infrastructure (INDE), and to assemble data pertinent to the RTS study in the area of reservoirs. In this context, this work presents the procedures and results found in the data processing of seismotectonic factors (dam height, reservoir capacity, lithology, and seismicity) and compared first to the dams that triggered earthquakes and secondly to the Brazilian dam list. The list has been updated with four more cases, making a total of 30 cases. The results indicate that the occurrence of RTS increases significantly with dam height since dams less than 50 m high cause only 2 % of earthquakes while those higher than 100 m cause about 54 %. The reservoir volume also plays a role, and it was estimated that RTS occurrence requires a limiting minimum value of 1 x 10(-4) km(3). There was no clear correlation be- tween the geology and geological provinces with RTS. The delayed response time of the reservoirs represents 43 % of the total; that is, almost half of them have hydraulic behavior. The highest magnitude, 4.2, was observed at a reservoir with a volume greater than 10(-3) km(3). As a practical outcome, to assist the analysis by the general community, the web viewer RISBRA (Reservoir Induced Seismicity in Brazil) was developed to serve as an interactive platform for Reservoir-Triggered Seismicity Database (BDSDR) data.	[Sayao, Eveline; Franca, George Sand] Univ Brasilia, Inst Geosci, Seismol Observ, Campus Darcy Ribeiro,SG13, BR-70910900 Brasilia, DF, Brazil; [Holanda, Maristela; Goncalves, Alexandro] Univ Brasilia, Dept Comp Sci, SGAN, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia; Universidade de Brasilia	Sayao, E (autor correspondente), Univ Brasilia, Inst Geosci, Seismol Observ, Campus Darcy Ribeiro,SG13, BR-70910900 Brasilia, DF, Brazil.	evelinesayao@unb.br	de França, George Sand L A/F-9931-2012; Holanda, Maristela/G-3922-2018	de França, George Sand L A/0000-0002-2694-5868; Holanda, Maristela/0000-0002-0883-2579; A. Sayao, Eveline/0000-0002-1304-0867				Araujo D. P., 1991, 2 INT C BRAZ GEOPH S, VII, P508; Assumpcao M, 2002, PURE APPL GEOPHYS, V159, P597, DOI 10.1007/PL00001266; Assumpcao M., 1995, 4 INT C BRAZ GEOPH S, P961; BAECHER GB, 1982, B SEISMOL SOC AM, V72, P553; Barros L. V., 2003, 8 INT C BRAZ GEOPH S; Barros L. 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B., 1995, P ISORIS 95 BEIJ CHI, P205; Wilson MP, 2017, SEISMOL RES LETT, V88, P1560, DOI 10.1785/0220170112	57	2	2	0	4	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	1561-8633	1684-9981		NAT HAZARD EARTH SYS	Nat. Hazards Earth Syst. Sci.	JUL 22	2020	20	7					2001	2019		10.5194/nhess-20-2001-2020	http://dx.doi.org/10.5194/nhess-20-2001-2020			19	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences; Water Resources	MT4QG		gold, Green Submitted			2023-06-23	WOS:000554956400001
J	Valasques, GS; dos Santos, AMP; da Silva, DLF; Cerqueira, UMFD; Ferreira, SLC; dos Santos, WNL; Bezerra, MA				Valasques, Gisseli Souza; Pinto dos Santos, Ana Maria; FranCa da Silva, Daniel Levi; da Mata Cerqueira, Uillian Mozart Ferreira; Costa Ferreira, Sergio Luis; Lopes dos Santos, Walter Nei; Bezerra, Marcos Almeida			Extraction induced by emulsion breaking for As, Se and Hg determination in crude palm oil by vapor generation-AFS	FOOD CHEMISTRY			English	Article						Crude palm oil; Extraction induced by emulsion breaking; Arsenic; Selenium; Mercury; Atomic fluorescence spectrometry	ATOMIC-ABSORPTION-SPECTROMETRY; ULTRASOUND-ASSISTED EXTRACTION; RESPONSE-SURFACE METHODOLOGY; SOLID-PHASE EXTRACTION; EDIBLE OILS; FLUORESCENCE SPECTROMETRY; VEGETABLE-OILS; LEAD; COPPER; CADMIUM	In this work is presented the development of a method for As and Se determination in crude palm oil samples by hydride generation atomic fluorescence spectrometry and Hg by cold vapor atomic fluorescence spectrometry after ultrasound-assisted emulsification and extraction induced by emulsion breaking (EIEB). The optimization of the method was carried out by multivariate designs. The developed method has presented limits of quantification (LOQ) of 0.72, 0.12, and 1.5 mu g L-1 for As, Hg, and Se, respectively. The precisions of the proposed method expressed as repeatability were 0.92, 2.2, and 3.7% RSD for 2 mu g L-1 (n = 10) of As, Hg and Se, respectively. The developed methodology was applied in palm oil samples collected in the Bahia State. Concentrations (mu g L-1) found in the samples were between < LOQ - 1.3 for As and 3.0-15 for Se. For Hg, all analyzed samples were below the limit of quantification.	[Valasques, Gisseli Souza; Pinto dos Santos, Ana Maria; FranCa da Silva, Daniel Levi; da Mata Cerqueira, Uillian Mozart Ferreira; Costa Ferreira, Sergio Luis] Univ Fed Bahia, Inst Quim, Campus Federacao Ondina, BR-40170115 Salvador, BA, Brazil; [da Mata Cerqueira, Uillian Mozart Ferreira; Bezerra, Marcos Almeida] Univ Estadual Sudoeste Bahia, Dept Ciencias & Tecnol, Campus Jequie,Rua Jose Moreira Sobrinho S-N, BR-45206190 Jequie, BA, Brazil; [Lopes dos Santos, Walter Nei] Univ Estado Bahia, Dept Ciencias Exatas & Terra, Rua Silveira Martins 2555, BR-40170290 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Estadual do Sudoeste da Bahia; Universidade do Estado Bahia	Bezerra, MA (autor correspondente), Univ Estadual Sudoeste Bahia, Dept Ciencias & Tecnol, Campus Jequie,Rua Jose Moreira Sobrinho S-N, BR-45206190 Jequie, BA, Brazil.	mbezerra@uesb.edu.br	dos Santos, Walter Nei Lopes/G-2660-2016; da Mata Cerqueira, Uillian Mozart Ferreira/AAT-9297-2020; FERREIRA, SERGIO LUIS SLCF COSTA/I-1993-2013; Santos, Ana Maria/AAW-5900-2020	dos Santos, Walter Nei Lopes/0000-0001-9773-6660; da Mata Cerqueira, Uillian Mozart Ferreira/0000-0002-2158-379X; FERREIRA, SERGIO LUIS SLCF COSTA/0000-0001-7738-045X; 	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [304582/2018-2]; Financiadora de Estudos e Projetos (FINEP)	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Financiadora de Estudos e Projetos (FINEP)(Financiadora de Inovacao e Pesquisa (Finep))	Authors acknowledge the financial support of the Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Grant Number 304582/2018-2), and Financiadora de Estudos e Projetos (FINEP).	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J	Sayao, JM; Saraiva, AAF; Brum, AS; Bantim, RAM; de Andrade, RCLP; Cheng, X; de Lima, FJ; Silva, HD; Kellner, AWA				Sayao, Juliana Manso; Feitosa Saraiva, Antonio Alamo; Brum, Arthur Souza; Machado Bantim, Renan Alfredo; Lima Pedroso de Andrade, Rafael Cesar; Cheng, Xin; de Lima, Flaviana Jorge; Silva, Helder de Paula; Kellner, Alexander W. A.			The first theropod dinosaur (Coelurosauria, Theropoda) from the base of the Romualdo Formation (Albian), Araripe Basin, Northeast Brazil	SCIENTIFIC REPORTS			English	Article							CRETACEOUS SANTANA FORMATION; BAURU GROUP; CONTROLLED EXCAVATIONS; GROWTH-PATTERNS; LIFE-HISTORY; EVOLUTION; PTEROSAUR; REMAINS; AGE; GIGANTISM	The Romualdo Formation (Araripe Basin) is worldwide known for the large number of well-preserved fossils but the dinosaur record is rather scarce. Here we describe a new coelurosaur, which is the first tetrapod recovered from the basal layers of this stratigraphic unit that consist of dark shales. Aratasaurus museunacionali gen. et sp. nov. is known by an incomplete but articulated right hind limb with the distal portion of the femur, proximal half of tibia and incomplete pes. The new species differs from other coelurosaurs by a medial fossa in the tibia and digits II, III and IV being symmetric. The phylogenetic analysis recovered Aratasaurus museunacionali closely related to Zuolong salleei, forming a basal coelurosaur lineage. The paleohistology indicate that the specimen is a juvenile, with an estimated body length around 3.12 m. The new taxon represents the first occurrence of basal coelurosaurians in the Araripe Basin and suggests a widespread distribution of this group during the Lower Cretaceous.	[Sayao, Juliana Manso; Lima Pedroso de Andrade, Rafael Cesar] Univ Fed Pernambuco, Lab Paleobiol & Microestruturas, Ctr Acad Vitoria, Rua Alto Reservatorio, BR-55608680 Vitoria De Santo Antao, PE, Brazil; [Feitosa Saraiva, Antonio Alamo; Machado Bantim, Renan Alfredo; Cheng, Xin; de Lima, Flaviana Jorge] Univ Reg Cariri, Lab Paleontol URCA, Rua Carolino Sucupira S-N, BR-63100000 Crato, CE, Brazil; [Sayao, Juliana Manso; Brum, Arthur Souza; Silva, Helder de Paula; Kellner, Alexander W. A.] Univ Fed Rio de Janeiro, Museu Nacl, Lab Systemat & Taphon Fossil Vertebrates, Dept Geol & Paleontol, Quinta Boa Vista S-N, BR-20940040 Sao Cristovao, RJ, Brazil; [Brum, Arthur Souza] Univ Fed Rio de Janeiro, Museu Nacl, Programa Posgrad Zool, BR-20940040 Sao Cristovao, RJ, Brazil; [Cheng, Xin] Jilin Univ, Coll Earth Sci, Str Jianshe 2199, Changchun 130061, Jilin, Peoples R China	Universidade Federal de Pernambuco; Universidade Regional do Cariri; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Jilin University	Kellner, AWA (autor correspondente), Univ Fed Rio de Janeiro, Museu Nacl, Lab Systemat & Taphon Fossil Vertebrates, Dept Geol & Paleontol, Quinta Boa Vista S-N, BR-20940040 Sao Cristovao, RJ, Brazil.	kellner@mn.ufrj.br	Kellner, Alexander/ABE-9591-2020; Brum, Arthur Souza/ABB-9735-2020; Saraiva, António/HPD-3031-2023; Bantim, Renan/J-4076-2014	Kellner, Alexander/0000-0001-7174-9447; da Costa, Arthur Souza Brum/0000-0003-3927-0318	Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [E-26/202.905/2018]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [420687/2016-5, 313461/2018-0, 311715/2017-6, 305705/2019-9]; Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) [BMD-0124-00302.01.01/19, DCR-0024-02039.01.00, SPU: 9871903/2018]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001, 88887.162865/2018-00]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001, PROANTAR: 88887.336584/2019-00, 88887.162865/2019-00]	Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	We would like to thank Placido Cidade Nuvens (deceased in 2016) for obtaining the specimen studied here and Bruno C. Vila Nova (UFPE) for preparing part of the material. Diogenes de Almeida Campos (CPRM) and Francisco de Freitas Leite (URCA) are thanked for discussions regarding the name of the new species. A.S.B. acknowledges Lucy Gomes de Souza (Museu Nacional/Universidade Federal do Rio de Janeiro) for helping with the TNT software. The paleoartist Maurilio Oliveira is acknowledged for the life reconstruction of this new dinosaur. This study was partially founded by the Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ #E-26/202.905/2018 to A.W.A.K.), the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq #420687/2016-5 and #313461/2018-0 to A.W.A.K.; #311715/2017-6 to J.M.S.; #305705/2019-9 to F.J.L.), the Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP #BMD-0124-00302.01.01/19 to R.A.M.B., #DCR-0024-02039.01.00 to X.C. and SPU: 9871903/2018 to F.J.L.), and the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001 (CAPES #88887.162865/2018-00 to R.A.M.B.). A.S.B. acknowledges the doctoral fellowship from Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES - PROANTAR: 88887.336584/2019-00 and Finance code 001 CAPES #88887.162865/2019-00 to RAMB).	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J	Sabadini-Santos, E; Castilhos, ZC; Bidone, ED				Sabadini-Santos, Elisamara; Castilhos, Zuleica Carmen; Bidone, Edison Dausacker			Microbial Activities Response to Contamination in Soil and Sediments Rich in As Surrounding an Industrial Gold Mine	WATER AIR AND SOIL POLLUTION			English	Article						Paracatu; Risk assessment; Quality Ratio; Enzymes	MINING ACTIVITIES; MARINE-SEDIMENTS; HEAVY-METALS; GERAIS STATE; POLLUTION; HYDROGEOCHEMISTRY; COMMUNITIES; RESISTANCE; TOLERANCE; TOXICITY	Gold mines are widely recognized as important sources of arsenic (As) pollution and this work proposes the use of in situ microbial community enzymatic response to assess the risk of As in soil and sediments surrounding "Morro do Ouro," the largest industrial gold mine in Brazil. Bacterial community exposed to high metals concentrations deviates energy from growth to cell maintenance modifying enzymatic activity response. Even if the number of bacterial cells presented in soil and sediment samples was in the same order of 10(7) cell cm(-3), it declines in sediment samples closer to a mining area. Dehydrogenase activity (DHA) showed the same trend, suggesting inhibition by toxic effect of metals, while esterase activities (EST) behaved in the opposite way, representative of increasing energy demand by the community under environmental stress. The Quality Ratio (QR) index for environmental risk assessment was applied to integrate geochemical (grain size, total organic carbon contents, and metals as indicators of complex contamination) and microbial parameters (DHA-energy production into cell and EST-hydrolase organic matter outside the cell membrane). QR indicated that the risk associated with soil and sediment is driven by As levels and decreases from the mine facilities.	[Sabadini-Santos, Elisamara; Bidone, Edison Dausacker] Univ Fed Fluminense UFF, Curso Posgrad Geoquim Ambiental, Niteroi, RJ, Brazil; [Castilhos, Zuleica Carmen] Minist Ciencia Tecnol & Inovacao CETEM MCTI, Ctr Tecnol Mineral, Rio De Janeiro, Brazil	Universidade Federal Fluminense	Sabadini-Santos, E (autor correspondente), Univ Fed Fluminense UFF, Curso Posgrad Geoquim Ambiental, Niteroi, RJ, Brazil.	esabadini@id.uff.br	Bidone, Edison/AAE-9527-2021; Sabadini-Santos, Elisamara/AAD-3407-2021	Bidone, Edison/0000-0002-5771-5651; Sabadini-Santos, Elisamara/0000-0003-3783-4554	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) [001]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) - Finance Code 001.	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JUL 9	2020	231	7							366	10.1007/s11270-020-04734-4	http://dx.doi.org/10.1007/s11270-020-04734-4			9	Environmental Sciences; Meteorology & Atmospheric Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences; Water Resources	MP2JV					2023-06-23	WOS:000552036400003
J	Forero-Ortega, AJ; Campanha, GAC; Faleiros, FM; Yogi, MTAG				Forero-Ortega, A. J.; Campanha, G. A. C.; Faleiros, F. M.; Yogi, M. T. A. G.			Pure shear-dominated transpression and vertical extrusion in a strike-slip fault splay from the Itapirapua Shear Zone, Ribeira Belt, Brazil	TECTONOPHYSICS			English	Article							C-AXIS FABRICS; PARALLEL SUBGRAIN BOUNDARIES; MEASURED SECTIONAL ELLIPSES; DEFORMATION TEMPERATURES; MAGNETIC-SUSCEPTIBILITY; QUARTZ MICROSTRUCTURES; PLASTIC-DEFORMATION; VORTICITY ANALYSIS; STRAIN ELLIPSOIDS; SE	The Itapirapua Shear Zone is a major NE-trending dextral transcurrent zone from the southern Ribeira Belt (Brazil), which was active during the Neoproterozoic Brasiliano-Pan African Orogeny, related with West Gondwana assembly. Macroscopic sigmoid-shaped blocks in its northernmost splay termination present a NE-trending subvertical tectonic foliation and subvertical stretching lineation suggesting a transpressional tectonics. This paper investigates this splay termination using integration of data from geological mapping, thermodynamic modeling, microtectonics, quartz c-axis fabrics, kinematic vorticity and finite strain analysis. Distinct rock assemblages are placed in tectonic contacts along the splay termination, including Statherian sillimanite-biotite paragneiss and granitic orthogneiss (Apiai-Mirim Complex), Statherian phyllites (Bairro dos Prestes Formation), Calymmian chlorite-epidote-actinolite metabasites (Fazenda Velha Suite), Ediacaran phyllites, metalimestone and quartzite (Itaiacoca Group) and Ediacaran granite (Tres Corregos Suite). Isochemical phase diagrams constrain synkinematic metamorphic conditions of 490-510 degrees C and 11-12.5 kbar (chlorite-biotite-phengite phyllite), 520-560 degrees C and 9-10 kbar (biotite-phengite phyllite) and 680-690 degrees C and 5-6 kbar (sillimanite-biotite paragneiss), with isothermal decompression paths. Microstructural evidence suggests that increase in metamorphic temperatures were accompanied by changes in the dominant deformation mechanism in quartz aggregates from subgrain rotation to grain boundary migration recrystallization. Significant contribution of dissolution-precipitation creep indicates water-abundant deformational conditions. Strain ellipsoids are oblate-shaped and present NE-trending subvertical XY planes and subvertical X-axes in agreement with field tectonic fabric. Quartz c-axis fabrics in XZ sections of the strain ellipsoid are dominated by symmetrical crossed girdles, while the fabrics present dextral asymmetry in horizontal YZ sections, consistent with macroscopic structural deflection, indicating a subvertical vorticity axis. Vorticity results indicate 48-59% of pure shear contribution. The data indicate that strain in the Itapirapua Shear Zone northern termination was accommodated by a pure shear-dominated transpression with vertical extrusion at mid-crustal conditions, which contrasts with a transtensional deformation in the southeastern block.	[Forero-Ortega, A. J.; Campanha, G. A. C.; Faleiros, F. M.; Yogi, M. T. A. G.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Forero-Ortega, A. J.] Colombian Geol Serv SGC, Tecton Geodynam Res Grp, Diagonal 53 34-53, Bogota 110231, Colombia	Universidade de Sao Paulo	Forero-Ortega, AJ (autor correspondente), Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil.	ajforte056@gmail.com	Faleiros, Frederico Meira/F-6138-2010	Faleiros, Frederico Meira/0000-0003-2199-8116	Sao Paulo Research Foundation (FAPESP) [2018/10012-0, 2015/04487-7];  [443439/2014-1];  [305701/2019-3];  [307732/2019-3]	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); ; ; 	Financial support was provided by grants 2018/10012-0 and 2015/04487-7, Sao Paulo Research Foundation (FAPESP), and CNPq grants 443439/2014-1 and 305701/2019-3 to G.A.C. Campanha, and 307732/2019-3 to FMF. We thank Andre de Sousa Pires and Marcelo Takei Kawata for field work collaboration. The paper was substantially improved following detailed comments and suggestions by the reviewers Elena Druguet and Gustavo Viegas. We thank Editor Philippe Agard for his guidance during the editorial process.	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J	Omena, EC; da Silva, JLL; Sial, AN; Cherkinsky, A; Dantas, MAT				Omena, Erica Cavalcante; Lopes da Silva, Jorge Luiz; Sial, Alcides Nobrega; Cherkinsky, Alexander; Trindade Dantas, Mario Andre			Late Pleistocene meso-megaherbivores from Brazilian Intertropical Region: isotopic diet (delta C-13), niche differentiation, guilds and paleoenvironmental reconstruction (delta C-13,delta O-18)	HISTORICAL BIOLOGY			English	Article						Isotopic palaeoecology; Brazilian Intertropical Region; quaternary; mammals	STABLE-ISOTOPES; LATE QUATERNARY; SOUTH; ECOLOGY; PALEOECOLOGY; AMERICA; MAMMALS	Stable isotopes in enamel, dentin, and bone hydroxyapatite are an important tool in the investigation of the palaeoecology of extinct organisms and are applied as proxies for different environmental parameters (e.g. diet, temperature, guild) that assist in reconstitutions of past environments. Tooth and bone samples of late PleistoceneToxodon platensis, Eremotherium laurillardi, Notiomastodon platensis, Glyptotheriumsp.,Hippidion principale, Xenorhinotherium bahienseandNothrotherium maquinensefrom several localities in Brazilian Intertropical Region, had delta C-13 and delta O-18 analysed to infer their paleodiet, guild and niche breadth that allow a reconstruction of past environment in which they lived. Including isotopic data for the horseEquus(Amerhippus)neogeus, the giant lamaPalaeolama major, the CingulatasPanochthussp. andHolmesina paulacoutoi, and the giant ground slothValgipes bucklandi, we can suggest that the Brazilian Intertropical Region presented three guilds: browsers (N. maquinense, V. bucklandi, X. bahiense), mixed-feeders (H. principale, E. laurillardi, T. platensis, N. platensis, P. major, Panochthussp.,H. paulacoutoi) and grazer (E. (A.)neogeus, Glyptotheriumsp.). These results indicate a dry environment with mixed vegetation with a predominance of open savanna, suggesting that the area at the time was similar to the current in more arid and open areas of the shrub savanna.	[Omena, Erica Cavalcante] Univ Fed Pernambuco, Programa Posgrad Geociencias, Recife, PE, Brazil; [Omena, Erica Cavalcante] Univ Fed Pernambuco, Ctr Tecnol & Geociencias, Dept Geol, Recife, PE, Brazil; [Lopes da Silva, Jorge Luiz] Univ Fed Alagoas, Dept Leontol, Museu Hist Nat, Maceio, Alagoas, Brazil; [Sial, Alcides Nobrega] Univ Georgia, Ctr Appl Isotope Studies, Athens, GA 30602 USA; [Cherkinsky, Alexander; Trindade Dantas, Mario Andre] Univ Fed Bahia, Lab Ecol & Geociencias, Inst Multidisciplinar Saude, Campus Anisio Teixeira, Vitoria Da Conquista, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal de Alagoas; University System of Georgia; University of Georgia; Universidade Federal da Bahia	Dantas, MAT (autor correspondente), Univ Fed Bahia, Lab Ecol & Geociencias, Inst Multidisciplinar Saude, Campus Anisio Teixeira, Vitoria Da Conquista, Brazil.	matdantas@yahoo.com.br	Sial, Alcides/AAD-1901-2021		CAPES; CNPq [404684/2016-5, PQ/CNPq 311003/2019-2]	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	To CAPES for first author's masters' scholarship; To CNPq by financial support through Universal project [process 404684/2016-5] and research fellowship for MATD [PQ/CNPq 311003/2019-2].	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Biol.	OCT 3	2021	33	10					2299	2304		10.1080/08912963.2020.1789977	http://dx.doi.org/10.1080/08912963.2020.1789977		JUL 2020	6	Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Paleontology	UZ1LT					2023-06-23	WOS:000547385100001
J	Bitencourt, VB; Dillenburg, SR; Manzolli, RP; Barboza, EG				Bitencourt, Volney Junior Borges; Dillenburg, Sergio R.; Manzolli, Rogerio P.; Barboza, Eduardo G.			Control factors in the evolution of Holocene coastal barriers in Southern Brazil	GEOMORPHOLOGY			English	Article						Coastal evolution; Morphological-behavior model; Substrate slope; Sediment budget	SEA-LEVEL RISE; STRATIGRAPHY; QUATERNARY; DEPOSITION; MIGRATION; INSIGHTS; RETREAT; ISLANDS; SYSTEMS; BEACH	The evolution and behavior of coastal barriers are controlled by several allogenic and autogenic factors. Some of these may be more deterministic than others. In this study, the GEOMBEST morphostratigraphic model is used to evaluate the degree of influence of both the substrate slope and the long-term sedimentary budget on the evolution of an extensive lagoon-barrier system during the mid-late Holocene in the middle littoral of Rio Grande do Sul state (Southern Brazil). Along this coastal stretch there is a coexistence of barriers with regressive, transgressive and stationery morphological behavior over >200 km. The modern configuration of the Holocene system (shoreline position and the lagoon-barrier width) was reproduced through the variability of two factors: the substrate slope (which defines the horizontal and vertical distance that the barrier will translate and rotate) and the sedimentary budget (which controls the evolution of the barrier when sea level oscillates slowly). The substrate slope of the middle littoral, between 0.021 degrees and 0.149 degrees, determined the cross-shore position of the shoreline, and the exogenous input or removal of sediment (estimated between -8 to +4.5 m(3)/m/a) allowed establishing the type of barrier behavior in the last millennia. Thus, the substrate slope exerts both direct and indirect control on coastal evolution. According to sensitivity analysis, a small decrease in the slope of the substrate, on the order of 0.001 degrees, can increase the resulting barrier translation by >150 m, considering a 1-m rise in sea level over a 100-year interval. (C) 2020 Elsevier B.V. All rights reserved.	[Bitencourt, Volney Junior Borges; Dillenburg, Sergio R.; Barboza, Eduardo G.] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil; [Dillenburg, Sergio R.; Barboza, Eduardo G.] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, Inst Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil; [Manzolli, Rogerio P.] Univ La Costa, Dept Ingn Civil & Ambiental, Calle 58 55 66, Barranquilla, Colombia	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidad de la Costa	Bitencourt, VB (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil.	volney.bitencourt@ufrgs.br	Barboza, Eduardo Guimarães/C-7579-2012; Manzolli, Rogerio Portantiolo/E-9777-2019; de Bitencourt, Volney Junior Borges/AAD-9618-2019; Dillenburg, Sergio/C-4027-2013	Barboza, Eduardo Guimarães/0000-0003-2107-6904; Manzolli, Rogerio Portantiolo/0000-0002-0223-5634; de Bitencourt, Volney Junior Borges/0000-0002-1004-5179; Dillenburg, Sergio/0000-0003-0072-7018	CNPq [141007/2015-0]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Volney J.B. Bitencourt thanks CNPq for his doctoral scholarship (141007/2015-0). Sergio R. Dillenburg and Eduardo G. Barboza thank CNPq for their research productivity scholarships.	Abreu J. G. N., 2005, REV BRAS GEOFIS, V23, P123, DOI DOI 10.1590/S0102-261X2005000200002; Andrade MM, 2018, BRAZ J OCEANOGR, V66, DOI [10.1590/S1679-87592018017406603, 10.1590/s1679-87592018017406603]; Angulo RJ, 2006, QUATERNARY SCI REV, V25, P486, DOI 10.1016/j.quascirev.2005.03.008; [Anonymous], 1976, MARINE SEDIMENT TRAN, DOI DOI 10.1007/978-3-662-01141-6_10; AREJANO T.B., 2006, THESIS; Ashton AD, 2006, J GEOPHYS RES-EARTH, V111, DOI 10.1029/2005JF000422; Barboza EG, 2018, J COASTAL RES, P446, DOI 10.2112/SI85-090.1; Barletta RD, 2003, J COASTAL RES, P300; BELKNAP DF, 1985, MAR GEOL, V63, P235, DOI 10.1016/0025-3227(85)90085-4; BITENCOURT V. 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J	de Bitencourt, VB; Dillenburg, SR; Barboza, EG; Rosa, MLCD; Manzolli, RP				Borges de Bitencourt, Volney Junior; Dillenburg, Sergio Rebello; Barboza, Eduardo Guimaraes; Correa da Camara Rosa, Maria Luiza; Manzolli, Rogerio Portantiolo			STRATIGRAPHIC STACKING PATTERNS AND THEIR REFLECTIONS ON THE HOLOCENE COASTAL BARRIER MORPHOLOGY OF THE MIDDLE COAST OF RIO GRANDE DO SUL, BRAZIL	REVISTA BRASILEIRA DE GEOMORFOLOGIA			Portuguese	Article						Ground Penetrating Radar (GPR); Coastal Evolution; Sediment Budget; GIS	GROUND-PENETRATING RADAR; SOUTHERN BRAZIL; REGRESSIVE BARRIER; EVOLUTION; EROSION; GPR; QUATERNARY; ISLAND; CLASSIFICATION; VARIABILITY	In this work, the Holocene barrier of the middle coast of Rio Grande do Sul (RS), located between Estreito and Bacupari, was investigated in detail. This stretch of the coast corresponds to the most expressive large-scale coastal projection of the RS coast. Important discoveries were made through subsurface geophysical (GPR) and surficial geomorphology data. In the southern portion of the projection, between Estreito and the northern sector of Lagoa do Peixe, the Holocene barrier exhibits a predominantly retrogradational evolutionary behavior (probably from 6 ka and the present), which was determined by a negative sediment budget in the long term. On the other hand, in the northern portion of the projection, between Balneario Mostardense and Bacupari, the barrier shows a reversal from retrogradational to progradational behavior. Such evolutionary change, expressed in a progradation ranging from 230 to 1800 m, is possibly attributed to a change in the sediment budget (negative to positive budget) that may have occurred only a few centuries ago, or even a few millennia. The reversal towards a progradational stacking pattern showed an increase in size (length of the progradational record) from the middle to the north of the coastal projection. It is possible to suggest that these evolutionary trends on a geological scale (10(2)-10(3) years) will continue over the next decades. Information about the coastline evolutionary trends in the last centuries and millennia can be useful as subsidies for the coastal management of the middle coast of RS.	[Borges de Bitencourt, Volney Junior] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Av Bento Goncalves 9-500, BR-91501970 Porto Alegre, RS, Brazil; [Dillenburg, Sergio Rebello; Barboza, Eduardo Guimaraes; Correa da Camara Rosa, Maria Luiza] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, Av Bento Goncalves 9-500, BR-91501970 Porto Alegre, RS, Brazil; [Manzolli, Rogerio Portantiolo] Univ Costa, Dept Civil & Environm, Dept Atlantico, Barranquilla, Colombia	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidad de la Costa	de Bitencourt, VB (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Av Bento Goncalves 9-500, BR-91501970 Porto Alegre, RS, Brazil.	volneybitencourt@gmail.com; sergio.dillenburg@ufrgs.br; eduardo.barboza@ufrgs.br; luiza.camara@ufrgs.br; rportant1@cuc.edu.co	de Bitencourt, Volney Junior Borges/AAD-9618-2019; Manzolli, Rogerio Portantiolo/E-9777-2019; Barboza, Eduardo Guimarães/C-7579-2012	de Bitencourt, Volney Junior Borges/0000-0002-1004-5179; Manzolli, Rogerio Portantiolo/0000-0002-0223-5634; Barboza, Eduardo Guimarães/0000-0003-2107-6904				Abreu V.S., 2010, SEQUENCE STRATIGRAPH, P209; ABSALONSEN L., 2007, REV PESQUISAS GEOCIE, V34, P3, DOI [10.22456/1807-9806.19457, DOI 10.22456/1807-9806.19457]; Albuquerque M, 2013, J COASTAL RES, P1710, DOI 10.2112/SI65-289.1; Alvares CA, 2013, METEOROL Z, V22, P711, DOI 10.1127/0941-2948/2013/0507; Andrade MM, 2018, BRAZ J OCEANOGR, V66, DOI [10.1590/S1679-87592018017406603, 10.1590/s1679-87592018017406603]; Annan AP, 2009, GROUND PENETRATING RADAR THEORY AND APPLICATIONS, P3; AREJANO T.B., 2006, THESIS; Athanasiou P, 2019, EARTH SYST SCI DATA, V11, P1515, DOI 10.5194/essd-11-1515-2019; Bally A. 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J	Brito, GB; da Silva, JB; Dias, LC; Santos, AD; Hadlich, GM; Ferreira, SLC				Brito, Geysa Barreto; da Silva Junior, Jucelino Balbino; Dias, Luise Carvalho; Santos, Adilson de Santana; Hadlich, Gisele Mara; Costa Ferreira, Sergio Luis			Evaluation of the bioavailability of potentially toxic metals in surface sediments collected from a tropical river near an urban area	MARINE POLLUTION BULLETIN			English	Article						Sediment; Inorganics compounds; Urban area; Contamination; Paraguacu River	SIMULTANEOUSLY EXTRACTED METALS; HEAVY-METALS; WATER; CADMIUM; RISK; BAY	The objective of this study was to evaluate the bioavailability of the metals cadmium, copper, lead, nickel, and zinc from sediment samples collected in the Paraguacu river between the cities of Cachoeira and Sao Felix in the state of Bahia in Brazil. The method used was the acid extraction of volatile sulfides and metals extracted simultaneously (AVS-SEM) as described in the literature. For the extraction of sulfide, an argon drag system was used after acidification of the samples with HCl, releasing the volatile sulfides collected in the basic solution. Its determination was made by molecular absorption spectrophotometry using the methylene blue method. For quantification of the metals, the sediment with acid was filtered and the residual solution was analyzed by inductively coupled plasma mass spectrometry (ICP MS) in which the elements that were associated with the sulfide were released in solution. The bioavailability evaluation was done by the relation between the sum of the concentrations of the metals in solution (SEM) and the concentration of sulfide in each sample (AVS). When the SSEM/AVS ratio is > 1, the medium is considered contaminated by the high bioavailability of the metals to other environmental compartments. In the samples collected in the Paraguacu river in two campaigns, with an SSEM/AVS ratio of 0.007 to 1.082, the last value being the only critical > 1, while the other quantities in the metallic phase were not available for a biota. By comparing the metal concentration data with the internationally established tolerance limits, all the values found were below the critical values, presenting no toxic risks to the surrounding ecosystem.	[Brito, Geysa Barreto; Dias, Luise Carvalho; Santos, Adilson de Santana; Costa Ferreira, Sergio Luis] Fed Univ Bahia UFBA, Chem Inst, Postgrad Chem, St Barao Geremoabo S-N,Ondina Campus, BR-40170270 Salvador, BA, Brazil; [da Silva Junior, Jucelino Balbino; Hadlich, Gisele Mara] Fed Univ Bahia UFBA, Inst Geosci, Postgrad Program Geochem Petr & Environm, BR-40170020 Salvador, BA, Brazil		da Silva, JB (autor correspondente), Fed Univ Bahia UFBA, Inst Geosci, Postgrad Program Geochem Petr & Environm, Ctr Environm Studies NEA, BR-40170020 Salvador, BA, Brazil.	jucejr@ufba.br	FERREIRA, SERGIO LUIS SLCF COSTA/I-1993-2013; da Silva, Jucelino Balbino/AAA-3611-2021; Hadlich, Gisele/AAO-4708-2020	FERREIRA, SERGIO LUIS SLCF COSTA/0000-0001-7738-045X; Brito, Geysa/0000-0001-8327-926X; Hadlich, Gisele Mara/0000-0002-6304-0988	LEPETRO - excellence in geochemistry: petroleum, energy, and environment (LEPETRO/IGEO/UFBA); CNPq (Brazil) [150680/2015-5, 2311/2011]; FAPESB (Bahia, Brazil)	LEPETRO - excellence in geochemistry: petroleum, energy, and environment (LEPETRO/IGEO/UFBA); CNPq (Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESB (Bahia, Brazil)	The authors are grateful to the LEPETRO - excellence in geochemistry: petroleum, energy, and environment (LEPETRO/IGEO/UFBA) for the support and availability of analysis equipment, to the FAPESB (Bahia, Brazil), and the CNPq (Brazil) (grant 150680/2015-5 and grant 2311/2011) for providing grants, fellowships, and financial support.	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Pollut. Bull.	JUL	2020	156								111215	10.1016/j.marpolbul.2020.111215	http://dx.doi.org/10.1016/j.marpolbul.2020.111215			7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	LW5AS	32366365				2023-06-23	WOS:000539160000019
J	Campos, MC; Chiessi, CM; Venancio, IM; Pinho, TML; Crivellari, S; Kuhnert, H; Schmiedl, G; Diaz, RA; Albuquerque, ALS; Portilho-Ramos, RC; Bahr, A; Mulitza, S				Campos, Marilia C.; Chiessi, Cristiano M.; Venancio, Igor M.; Pinho, Taina M. L.; Crivellari, Stefano; Kuhnert, Henning; Schmiedl, Gerhard; Diaz, Rut A.; Albuquerque, Ana Luiza S.; Portilho-Ramos, Rodrigo C.; Bahr, Andre; Mulitza, Stefan			Constraining Millennial-Scale Changes in Northern Component Water Ventilation in the Western Tropical South Atlantic	PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY			English	Article						stable carbon isotopes</AUTHOR_KEYWORD>; Heinrich Stadials</AUTHOR_KEYWORD>; Northern Component Water</AUTHOR_KEYWORD>; sulfur</AUTHOR_KEYWORD>; western tropical South Atlantic</AUTHOR_KEYWORD>; Atlantic meridional overturning circulation</AUTHOR_KEYWORD>	DEEP-WATER; BENTHIC FORAMINIFERA; ATMOSPHERIC CO2; ISOTOPIC COMPOSITION; OCEAN CIRCULATION; ORGANIC-CARBON; VARIABILITY; CLIMATE; PROXY; AGE	Negative excursions in the stable carbon isotopic composition (delta C-13) at Atlantic intermediate to mid-depths are common features of millennial-scale events named Heinrich Stadials. The mechanisms behind these excursions are not yet fully understood, but most hypotheses agree on the central role played by the weakening of the Atlantic meridional overturning circulation. Marine records registering millennial-scale negative delta C-13 excursions in the Atlantic are mostly restricted to the Heinrich Stadials of the last deglacial, while the Heinrich Stadials of the last glacial are poorly studied. Here, we constrain changes in bottom water ventilation in the western tropical South Atlantic mid-depth during Heinrich Stadials of the last glacial and deglacial by investigating marine core M125-95-3. The concurrent decreases in benthic foraminifera delta C-13 and increases in bulk sediment sulfur indicate an increased Northern Component Water (NCW) residence time in the western tropical South Atlantic mid-depth during Heinrich Stadials. Furthermore, a coherent meridional pattern emerges from the comparison of our new data to previously published mid-depth records from the western South Atlantic. While our record shows the largest negative delta C-13 excursions during almost all Heinrich Stadials, the western equatorialAtlantic showed medium and the subtropical South Atlantic showed the smallest negative excursions. This meridional pattern supports the notion that during Heinrich Stadials, a reduction in the NCW delta C-13 source signal together with the accumulation of respired carbon at NCW depths drove the negative delta C-13 excursions. We suggest that the negative delta C-13 excursions progressively increase along the NCW southwards pathway until the signal dissipates/dilutes by mixing with Southern Component Water.	[Campos, Marilia C.; Chiessi, Cristiano M.] Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, Brazil; [Venancio, Igor M.] Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Cachoeira Paulista, Brazil; [Pinho, Taina M. L.; Crivellari, Stefano] Univ Sao Paulo, Inst Geosci, Sao Paulo, Brazil; [Kuhnert, Henning; Portilho-Ramos, Rodrigo C.; Mulitza, Stefan] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Schmiedl, Gerhard] Univ Hamburg, Ctr Earth Syst Res & Sustainabil, Inst Geol, Hamburg, Germany; [Diaz, Rut A.; Albuquerque, Ana Luiza S.] Fluminense Fed Univ, Grad Program Geochem, Niteroi, RJ, Brazil; [Bahr, Andre] Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany	Universidade de Sao Paulo; Instituto Nacional de Pesquisas Espaciais (INPE); Universidade de Sao Paulo; University of Bremen; University of Hamburg; Universidade Federal Fluminense; Ruprecht Karls University Heidelberg	Campos, MC (autor correspondente), Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, Brazil.	marilia.carvalho.campos@usp.br	Chiessi, Cristiano Mazur/E-1916-2012; Venancio, Igor M/I-5893-2014; Schmiedl, Gerhard/E-6644-2017; Albuquerque, Ana Luiza S/C-5167-2013; Campos, Marília/AFL-1717-2022; Pinho, Tainã Marcos Lima/AAN-6616-2021; Díaz, Rut/AAG-2748-2021	Chiessi, Cristiano Mazur/0000-0003-3318-8022; Venancio, Igor M/0000-0003-3118-4247; Schmiedl, Gerhard/0000-0002-2177-6858; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Campos, Marília/0000-0003-0059-9853; Pinho, Tainã Marcos Lima/0000-0001-6371-4498; Díaz, Rut/0000-0003-1883-7231; Kuhnert, Henning/0000-0001-5242-4495; Crivellari, Stefano/0000-0003-3847-8854; da Costa Portilho Ramos, Rodrigo/0000-0002-1182-1547	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2016/10242-0, 2018/06790-7, 2019/10642-6, 2018/15123-4]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [564/2015, 88881.313535/2019-01, 88887.156152/2017-00, 88881.161151/2017-01, 88887.196044/2018-00, 001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [302607/2016-1, 422255/2016-5, 406322/2018-0]; Alexander von Humboldt-Stiftung; Deutsche Forschungsgemeinschaft (DFG) Research Centre, Cluster of Excellence "The Ocean in the Earth System"; DFG [BA 3809/9-1]	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Alexander von Humboldt-Stiftung(Alexander von Humboldt Foundation); Deutsche Forschungsgemeinschaft (DFG) Research Centre, Cluster of Excellence "The Ocean in the Earth System"(German Research Foundation (DFG)); DFG(German Research Foundation (DFG))	Logistic and technical assistance was provided by the captain and crew of the R/V Meteor. New data shown herein are archived in Pangaea (doi: 10.1594/PANGAEA.915451). M. C. Campos acknowledges the financial support from Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) (Grants 2016/10242-0 and 2018/067907). C. M. Chiessi acknowledges the financial support from FAPESP (Grant 2018/15123-4), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) (Grants 564/2015 and 88881.313535/2019-01), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (Grants 302607/2016-1 and 422255/2016-5), and the Alexander von Humboldt-Stiftung. CAPES (Grants 88887.156152/2017-00 and 88881.161151/2017-01) and CNPq (Grant 406322/2018-0) currently support I. M. Venancio. T. M. L. Pinho acknowledges the financial support from FAPESP (Grant 2019/10642-6). S. Crivellari acknowledges the financial support from CAPES (Grant 88887.196044/2018-00). A. L. S. Albuquerque is a senior CNPq researcher (Grants 302521-2017-8 and 429767/2018-8) and acknowledges the financial support from CAPES (Finance Code 001). S. Mulitza and H. Kuhnert were funded through the Deutsche Forschungsgemeinschaft (DFG) Research Centre, Cluster of Excellence "The Ocean in the Earth System". A. Bahr received funding from the DFG via Grant BA 3809/9-1.	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Paleoclimatology	JUL	2020	35	7							e2020PA003876	10.1029/2020PA003876	http://dx.doi.org/10.1029/2020PA003876			14	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	MV9CM					2023-06-23	WOS:000556646600005
J	de Souza, CS; da Conceicao, LR; Freitas, TSS; Aboim, IL; Schwamborn, R; Neumann-Leitao, S; Mafalda, PD				de Souza, Christiane S.; da Conceicao, Laura R.; Freitas, Tamires S. S.; Aboim, Igor L.; Schwamborn, Ralf; Neumann-Leitao, Sigrid; Mafalda Junior, Paulo de O.			Size Spectra Modeling of Mesozooplankton over a Tropical Continental Shelf	JOURNAL OF COASTAL RESEARCH			English	Article						Normalized biomass size spectrum (NBSS); size diversity; mesozooplankton; ZooScan; continental shelf	ZOOPLANKTON SIZE; BIOMASS; PARTICLES; PROFILER; SYSTEM; WATERS; SEA; BAY	Size spectra analysis is a useful way of studying biomass and energy flow in ecosystems across trophic levels. The size spectrum reflects a balance of energy and matter between gains through growth and recruitment and losses though mortality in a size-structured community. Therefore, changes in biomass and normalized biomass size spectrum (NBSS) slope and intercept between time or environment can be used to assess the energy transfer efficiency within ecosystems. Linear models were developed to analyze zooplankton biomass and community size structure for the narrow continental shelf and shelf break off Salvador, Brazil, using samples that were collected during 10 oceanographic cruises, from April 2013 to October 2014, and analyzed with a ZooScan. Three descriptors of zooplankton size spectra were examined: size diversity, NBSS slope, and intercept. Copepods were always dominant in abundance. Size spectra varied considerably along a short coast-to-offshore transect of 17 km. The pattern of spatial change presented a predominance of larger size fractions nearshore (flat NBSS slope, -0.56) and the predominance of smaller sized organisms in oceanic waters (steep NBSS slope, -0.88). This gradient was mostly due to the higher abundance of large (>5 mm equivalent spherical diameter) gelatinous organisms (mainly hydromedusae) nearshore. The results suggest that the tropical zooplankton community at the continental shelf off Salvador was characterized by low productivity and low trophic efficiency, especially offshore. Although copepods were dominant in numbers, large-sized gelatinous predators were the key structuring zooplankton taxon in this area.	[de Souza, Christiane S.; Freitas, Tamires S. S.; Aboim, Igor L.; Mafalda Junior, Paulo de O.] Fed Univ Bahia UFBA, Inst Biol, Salvador, BA, Brazil; [da Conceicao, Laura R.] Fed Univ Espirito Santo UFES, Dept Oceanog & Ecol, Vitoria, ES, Brazil; [Schwamborn, Ralf; Neumann-Leitao, Sigrid] Fed Univ Pernambuco UFPE, Dept Oceanog, Recife, PE, Brazil	Universidade Federal da Bahia; Universidade Federal do Espirito Santo; Universidade Federal de Pernambuco	de Souza, CS (autor correspondente), Fed Univ Bahia UFBA, Inst Biol, Salvador, BA, Brazil.	chsampaio@ig.com.br	de Souza, Christiane Sampaio/AAC-7117-2021; Júnior, Paulo Mafalda/AAC-7002-2021	de Souza, Christiane Sampaio/0000-0002-3331-014X; 	Brazilian National Institute of Science and Technology for Tropical Marine Environments-INCT AmbTropic (CNPq/FAPESB) [565054/2010-4]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [381350/2016-9, 380789/2017-5]	Brazilian National Institute of Science and Technology for Tropical Marine Environments-INCT AmbTropic (CNPq/FAPESB); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This research was supported by the Brazilian National Institute of Science and Technology for Tropical Marine Environments-INCT AmbTropic (CNPq/FAPESB grants 565054/2010-4). Christiane Sampaio de Souza was supported by a research grant of the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq grants 381350/2016-9 and 380789/2017-5). The authors thank the Universidade Federal da Bahia (UFBA), Universidade Federal Pernambuco (UFPE), and the people who are part of UFPE's Zooplankton Laboratory for their technical support with Zooscan. We are indebted to all participants of the UFBA's Plankton Laboratory for their help during INCT-Bahia cruises.	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Coast. Res.	JUL	2020	36	4					795	804		10.2112/JCOASTRES-D-19-00102.1	http://dx.doi.org/10.2112/JCOASTRES-D-19-00102.1			10	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	MI4OG					2023-06-23	WOS:000547388800010
J	De Toni, GB; Bitencourt, MF; Konopasek, J; Martini, A; Andrade, PHS; Florisbal, LM; Campos, RS				De Toni, G. B.; Bitencourt, M. F.; Konopasek, J.; Martini, A.; Andrade, P. H. S.; Florisbal, L. M.; Campos, R. S.			Transpressive strain partitioning between the Major Gercino Shear Zone and the Tijucas Fold Belt, Dom Feliciano Belt, Santa Catarina, southern Brazil	JOURNAL OF STRUCTURAL GEOLOGY			English	Article						Transpression; Strain partitioning; Oblique collision; Cross section	POSTCOLLISIONAL GRANITIC MAGMATISM; BRUSQUE METAMORPHIC COMPLEX; PB ISOTOPE GEOCHEMISTRY; ZIRCON GEOCHRONOLOGY; DEFORMATION PATTERNS; TECTONIC EVOLUTION; METAVOLCANIC ROCKS; CAMBORIU COMPLEX; WHOLE-ROCK; ICP-MS	A composite cross section from the Florian.opolis Batholith towards the Tijucas Fold Belt in the northern Dom Feliciano Belt (southern Brazil) is divided in three structural domains: the Major Gercino Shear Zone, the suprastructural Brusque Complex and the infrastructural Camboriu Complex. A kinematic correlation among the structural domains is based on structural and petrological data integrated with geochronology. An oblique collisional event at 650-645 Ma affected all structural domains and is best recorded in the Porto Belo Complex, which shows migmatization (700 degrees C/4.3 kbar) and top-to-the-NNW+dextral shear along the Major Gercino Shear Zone. Subsequent strain partitioning led to progressive tangential movement recorded in the Quatro Ilhas Granitoids (625-615 Ma) followed by later granitic intrusions (after 615 Ma) controlled by dextral strike-slip. Meanwhile, the contractional component was absorbed by the Tijucas Fold Belt infrastructure, causing exhumation of the Camboriu Complex migmatites (from 5 to 3.4 kbar) and unroofing of the suprastructural Brusque Complex (around 635 Ma). Tectonic juxtaposition occurred along a dextral+normal detatchment zone between the complexes. As a consequence, heating of the Brusque Complex locally reached amphibolite-facies conditions and suprastructure thrusting inverted to extension, which is recorded in discrete shear structures with normal kinematics. The sequence of events and their age suggest that the hinterland Porto Belo Complex and the foreland Tijucas Fold Belt were juxtaposed already at ca. 650-645 Ma, which questions the validity of the subduction-related tectonic models in the northern Dom Feliciano Belt.	[De Toni, G. B.; Bitencourt, M. F.; Martini, A.; Andrade, P. H. S.] Univ Fed Rio Grande do Sul, Programa Pos Grad Geociencias, Av Bento Goncalves 9500, BR-91500000 Porto Alegre, RS, Brazil; [Konopasek, J.] UiT Arctic Univ Norway Troms, Dept Geosci, Postboks 6050, N-9037 Tromso, Norway; [Konopasek, J.] Czech Geol Survey, Klarov 3, Prague 11821, Czech Republic; [Florisbal, L. M.; Campos, R. S.] Univ Fed Santa Catarina UFSC, Programa Posgrad Geol PPGGeol, Florianopolis, SC, Brazil; [De Toni, G. B.] Univ Vale Rio Sinos UNISINOS, Polytech Sch, Av Unisinos 950, BR-93022750 Sao Leopolso, RS, Brazil; [Martini, A.] Univ Fed Vales Jequitinhonha & Mucuri, Inst Ciencia & Tecnol, Rodovia MGT 367 Km 583,5000, BR-39100000 Diamantina, MG, Brazil	Universidade Federal do Rio Grande do Sul; Czech Geological Survey; Universidade Federal de Santa Catarina (UFSC); Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM)	De Toni, GB (autor correspondente), Univ Fed Rio Grande do Sul, Programa Pos Grad Geociencias, Av Bento Goncalves 9500, BR-91500000 Porto Alegre, RS, Brazil.; De Toni, GB (autor correspondente), Univ Vale Rio Sinos UNISINOS, Polytech Sch, Av Unisinos 950, BR-93022750 Sao Leopolso, RS, Brazil.	gdetoni@ufrgs.br; fatimab@ufrgs.br; jiri.konopasek@uit.no; amosmartini@gmail.com; pedrohgeo@hotmail.com; geoluana@yahoo.com.br; beto.decampos@gmail.com	de Fátima Bitencourt, Maria/H-8957-2016; Konopasek, Jiri/J-6658-2016; Bitencourt, Maria de Fátima/GLR-8862-2022	de Fátima Bitencourt, Maria/0000-0001-7022-9175; Konopasek, Jiri/0000-0001-5625-3996; Bitencourt, Maria de Fátima/0000-0001-7022-9175; Andrade, Pedro/0000-0002-7739-009X	Brazilian National Research Council (CNPq) [311486/2015-0, 306605/2018-0, 481841/2012-1]; CNPq [141011/2015-7]; Coordenacao de Aperfeicoamento de Pessoal Docente [CAPES - 88881.117872/2016-01, 88887.141226/2017-00, SIU - TF-2016-CAPES-SIU/10024]; Czech Science Foundation [18-24281S]	Brazilian National Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal Docente; Czech Science Foundation(Grant Agency of the Czech Republic)	The authors acknowledge financial support of the Brazilian National Research Council (CNPq) through the productivity grants to M.F. Bitencourt (311486/2015-0) and L.V.S. Nardi (306605/2018-0), and through the Universal Project N. 481841/2012-1 (M.F. Bitencourt). PhD scholarship to G.B. De Toni (141011/2015-7) was also financed by CNPq. The authors acknowledge Coordenacao de Aperfeicoamento de Pessoal Docente for funding of the CAPES (Brazil) - SIU (Norway) cooperation program (CAPES - 88881.117872/2016-01 and 88887.141226/2017-00, SIU - TF-2016-CAPES-SIU/10024). J Konop.asek appreciates financial support of the Czech Science Foundation (grant no. 18-24281S). We thank Kai Neufeld and Susan Drago for their kind help with EDSB at UiT and microprobe analyses at UFRGS, respectively. The authors are also grateful to an anonymous reviewer and C. Fern.andez, whose critical reviews and comments have lead to significant improvement of this work.	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Struct. Geol.	JUL	2020	136								104058	10.1016/j.jsg.2020.104058	http://dx.doi.org/10.1016/j.jsg.2020.104058			26	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LW4DI		Green Accepted			2023-06-23	WOS:000539094300007
J	Dos Santos, TB; Pinheiro, ERD; Iannuzzi, R				Dos Santos, Thamiris Barbosa; De Souza Pinheiro, Esther Regina; Iannuzzi, Roberto			FIRST EVIDENCE OF SEED PREDATION BY ARTHROPODS FROM GONDWANA AND ITS EARLY PALEOZOIC HISTORY (RIO BONITO FORMATION, PARANA BASIN, BRAZIL)	PALAIOS			English	Article							NORTH-CENTRAL TEXAS; PERMIAN GLOSSOPTERIS FLORA; INSECT HERBIVORY; PLANTS; AGE; PATAGONIA; PATTERNS; TRACES; LEAVES; DAMAGE	Seeds are plant organs commonly found worldwide in late Paleozoic deposits. In Gondwana, the seeds are found in deposits from Southern Africa, Antarctica, Oceania, and South America, and are widely reported in the wellknown "Glossopteris Flora". Even with a significant record of these plant organs, little is known about plant-insect interactions with seeds during the Pennsylvanian and Permian periods. In the present paper, we recorded the first formal record of seed consumption by arthropods in Cordaicarpus and Samaropsis-like seeds for Gondwana from lower Permian (Artinskian) deposits in Southern Brazil. The material analyzed was collected from the Itanema H outcrop of Santa Catarina State and consisted of 34 seed specimens. Of these, eight specimens presented evidence for plant-insect interaction, representing 23.5% of all specimens that were attacked by seed predators. The consumption was inflicted by insects with stylate mouthparts, probably belonging to hemipteroid or paleodictyopteroid lineages. The damage is described as perforations and scale-insect marks along the seed body. We recorded one damage type as DT74 and three others as new damage types DT399, DT400, and DT401, some of which are specific to a few seed morphotypes, including one morphotype with subtending cupule still attached to the seed. The elevated frequency of seed predation indicates that seed consumption by insects was well established during the early Permian.	[Dos Santos, Thamiris Barbosa; De Souza Pinheiro, Esther Regina; Iannuzzi, Roberto] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Lab Paleobot, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Dos Santos, TB (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Lab Paleobot, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil.	thamiris.barbosa.santos@gmail.com	Iannuzzi, Roberto/G-3641-2012; dos Santos, Thamiris/ACP-6778-2022; Pinheiro, Esther RS/F-4923-2013	Iannuzzi, Roberto/0000-0003-1432-8106; dos Santos, Thamiris/0000-0001-7604-514X; 	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico of Brazil (Brazilian National Council for Scientific and Technological Development CNPq) [132175/2019-3, 430096/2016-0, PQ 312747/2017-9]; Coordenacao de Aperfeicoamento de Pessoal de N'ivel Superior (Coordination for the Improvement of Higher Education Personnel-CAPES) [88887.351 775/2019-00]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico of Brazil (Brazilian National Council for Scientific and Technological Development CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de N'ivel Superior (Coordination for the Improvement of Higher Education Personnel-CAPES)	We are grateful to Dr. Conrad C. Labandeira and the two anonymous reviewers for their important feedback. This research received support from the Conselho Nacional de Desenvolvimento Cient ' ifico e Tecnol ' ogico of Brazil (Brazilian National Council for Scientific and Technological DevelopmentCNPq) by research fellowships granted to senior author (132175/2019-3) and to RI (430096/2016-0; PQ 312747/2017-9) and from the Coordenacao de Aperfeicoamento de Pessoal de N ' ivel Superior (Coordination for the Improvement of Higher Education Personnel-CAPES) to ERSP (88887.351 775/2019-00). The authors are indebted with Luiz F. Lopez for the excellent photos taken from the seed material.	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J	Ferreira, E; Mateus, A; Azeredo, AC; Duarte, LV; Mendonca, J; Tassinari, CCG				Ferreira, Ezequiel; Mateus, Antonio; Azeredo, Ana C.; Duarte, Luis, V; Mendonca-Filho, Joao; Tassinari, Colombo C. G.			Tracing bottom-water redox conditions during deposition of Lower and Upper Jurassic organic-rich sedimentary rocks in the Lusitanian Basin (Portugal): Insights from inorganic geochemistry	MARINE AND PETROLEUM GEOLOGY			English	Article						Redox-sensitive elements; Redox conditions; Organic matter accumulation; Black-shales; Petroleum source rocks; Jurassic; Lusitanian Basin	CHILEAN UPWELLING SEDIMENTS; PENNSYLVANIAN-PERMIAN AGE; RARE-EARTH-ELEMENTS; BLACK SHALES; BALTIC SEA; PRIMARY PRODUCTIVITY; MATTER PRODUCTION; MARINE-SEDIMENTS; OCEANIC ANOXIA; IRON MINERALS	The Lower Jurassic Agua de Madeiros (AM Fm) and Vale das Fontes (VF Fm) Formations, and the Upper Jurassic Cabacos Formation (Cab Fm) are considered the most important units with petroleum source-rock potential in the Lusitanian Basin, and the likely sources for its widespread hydrocarbon occurrences. Nonetheless, the bottomwater redox conditions during their deposition remain debatable. To resolve this controversy, we investigated whole-rock inorganic geochemical data of the most significant organic-rich levels of the AM, VF and Cab Fms cropping out at basin scale. Significant variations in TOC, TS and redox-sensitive elements contents and their ratios are evident within and between the organic-rich levels of the studied units. A positive covariation between primary productivity proxies, TOC enrichment and paleo-redox proxies for the Lower Jurassic units clearly suggest an interdependence between enhanced primary productivity, organic matter accumulation and bottom-water redox conditions. For the AM Fm, the paleo-redox proxies indicate that the black shales deposition took place beneath bottom-waters that ranged from suboxic to strongly euxinic conditions, with a clear predominance of the latter. A TOC threshold of similar to 6-7 wt% clearly separates samples deposited under suboxic to anoxic conditions from those deposited under true euxinic conditions, and is interpreted as the minimum amount of organic matter (OM) accumulation within sediments required to sustain H2S production at rates that outpaced its consumption through precipitation of sulphides and/or OM sulphurization, allowing the diffusion of H2S to the bottom-waters. For the Vale das Fontes Fm, the paleo-redox proxies suggest a prevalence of suboxic to anoxic bottom-waters, despite all black shales displaying TOC contents greater than the above threshold. The less reducing conditions relative to the AM Fm euxinic black shales are attributed to: i) a larger proportion of continental OM; ii) lower reactivity of the OM reaching the sediment-water interface (decreasing oxygen consumption); and iii) higher availability of reactive iron (increasing the buffer effect to H2S produced through OM remineralization by sulphate-reducing bacteria). Both units display Mo-EF vs U-EF covariation patterns that deviate from the field of sediments deposited under unrestricted open-marine conditions, towards higher Mo enrichment relative to that of U, indicating an accelerated transport of aqueous Mo to the sediments, consistent with the operation of a metal-oxyhydroxide particulate shuttle linked to Mn and Fe redox cycling within the water column in a weakly-restricted basin. The Mo-COT regression-line slope indicates a moderate degree of bottom-water mass restriction, with [Mo](aq) concentration of similar to 60-70% of the present-day seawater value and bottom-water renewal times of similar to 10-20 years, akin to the presentday Cariaco Basin. The redox conditions of the Cab Fm organic-rich levels are dependent on the location of the depositional environment in the basin, with deposition taking place beneath oxygenated bottom-waters at Cabo Mondego, and under suboxic conditions at Vale de Ventos and Pedrogao, the latter denoting a larger degree of oxygen depletion than the former. In this context, the overall potential for OM preservation should increase from Cabo Mondego to Vale de Ventos and Pedrogao.	[Ferreira, Ezequiel] Univ Sao Paulo, Inst Geociencias, Programa Posgrad Geoquim & Geotecton, Rua Lago 562, BR-05508900 Sao Paulo, SP, Brazil; [Ferreira, Ezequiel; Mateus, Antonio; Azeredo, Ana C.] Univ Lisbon, Fac Ciencias, Inst Dom Luiz, P-1749016 Lisbon, Portugal; [Mateus, Antonio; Azeredo, Ana C.] Univ Lisbon, Fac Ciencias, Dept Geol, Ed C6,Piso 4, P-1749016 Lisbon, Portugal; [Duarte, Luis, V] Univ Coimbra, MARE, Polo 2,Rua Silvio Lima, P-3030790 Coimbra, Portugal; [Duarte, Luis, V] Univ Coimbra, Dept Ciencias Terra, Polo 2,Rua Silvio Lima, P-3030790 Coimbra, Portugal; [Mendonca-Filho, Joao] Univ Fed Rio de Janeiro, Dept Geol, BR-21949900 Rio De Janeiro, Brazil; [Tassinari, Colombo C. G.] Univ Sao Paulo, Inst Geociencias, Dept Geoquim & Geotecton, Rua Lago 562, BR-05508900 Sao Paulo, SP, Brazil	Universidade de Sao Paulo; Universidade de Lisboa; Universidade de Lisboa; Universidade de Coimbra; Universidade de Coimbra; Universidade Federal do Rio de Janeiro; Universidade de Sao Paulo	Ferreira, E (autor correspondente), Univ Lisbon, Fac Ciencias, Dept Geol, Ed C6,Piso 4, P-1749016 Lisbon, Portugal.	ezequiel.geo@gmail.com	Azerêdo, Ana C/B-6325-2013; Ferreira, Ezequiel/AAK-4100-2020; Duarte, Luis/F-5282-2013; Mateus, António Manuel/D-3727-2011	Azerêdo, Ana C/0000-0002-1244-4843; Ferreira, Ezequiel/0000-0002-3095-2745; Duarte, Luis/0000-0002-9025-5896; Mateus, António Manuel/0000-0003-2623-1539	Galp-Petrobras funds; Instituto Dom Luiz grant [UID/GEO/50019/2013 IDL]; Fundacao para a Ciencia e Tecnologia (FCT) [SFRH/BD/93376/2013]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ) [402797/2012-4]; FCT [UID/MAR/04292/2019]; National Institute of Science and Technology of Analytical Techniques Applied to Oil and Gas Exploration (INCT) Petrotec; Fundação para a Ciência e a Tecnologia [SFRH/BD/93376/2013] Funding Source: FCT	Galp-Petrobras funds; Instituto Dom Luiz grant; Fundacao para a Ciencia e Tecnologia (FCT)(Fundacao para a Ciencia e a Tecnologia (FCT)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FCT(Fundacao para a Ciencia e a Tecnologia (FCT)); National Institute of Science and Technology of Analytical Techniques Applied to Oil and Gas Exploration (INCT) Petrotec; Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	This study was partly supported (Ana C. Azeredo) by Galp-Petrobras funds under the scope of Carbonate Reservoir Geoengineering Advanced Courses (including fieldwork in the Lusitanian Basin); additional backing was provided through the Instituto Dom Luiz grant UID/GEO/50019/2013 IDL. Ezequiel Ferreira acknowledges the support of Fundacao para a Ciencia e Tecnologia (FCT) through PhD grant SFRH/BD/93376/2013. Clarice Paixao (Palynofacies and Organic Facies Laboratory of the Rio de Janeiro Federal University) is acknowledged for the assistance with the TOC determinations. Antonio Mateus appreciates the PVE grant #402797/2012-4 of Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ), Science Without Frontiers Programme. Luis Vitor Duarte was supported by FCT, through the strategic project UID/MAR/04292/2019 granted to the Marine and Environmental Sciences Centre (MARE, Portugal). Colombo C. G. Tassinari acknowledges funding through the National Institute of Science and Technology of Analytical Techniques Applied to Oil and Gas Exploration (INCT) Petrotec.	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Pet. Geol.	JUL	2020	117								104343	10.1016/j.marpetgeo.2020.104343	http://dx.doi.org/10.1016/j.marpetgeo.2020.104343			25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LU2FJ					2023-06-23	WOS:000537575300006
J	Uchoa, JCF; Toledo, CLB; Silva, AM; Mendonca, AF; Hagemann, SG; Kreuzer, OP; Carmelo, AC				Ferreira Uchoa, Juliane Cristina; Bemfica Toledo, Catarina Laboure; Silva, Adalene Moreira; Mendonca, Augusto Ferreira; Hagemann, Steffen G.; Kreuzer, Oliver P.; Carmelo, Adriana Chatack			Multi-process and multi-scale spatial predictive analysis of an orogenic Archean gold system, Rio das Velhas Greenstone Belt, Brazil	ORE GEOLOGY REVIEWS			English	Article						Multiscale; Orogenic gold; Predictive analysis; Spatial modeling; Rio das Velhas Greenstone Belt; Mineral systems approach	SAO-FRANCISCO CRATON; QUADRILATERO-FERRIFERO; MINAS-GERAIS; PROSPECTIVITY ANALYSIS; MINERAL SYSTEMS; FUZZY-LOGIC; YILGARN BLOCK; SPECIAL-ISSUE; DEPOSITS; EVOLUTION	There has always been a need for new methodologies and research to improve the decision-making process at the early stages of mineral exploration. This article presents a novel approach to integrating geodata in support of a mineral systems-based spatial analysis of orogenic gold deposits in the Rio das Velhas Greenstone Belt (RVGB), Quadrilkero Ferrffero Province, Brazil. The gold mineralization in the RVGB is spatially associated with thrust faults and shear zones and mainly hosted by iron-rich rocks such as mafic-ultramafic sequences and banded iron formations. To best represent the targeting elements of this mineral system spatially, a knowledge-based fuzzy logic method was employed to map the expressions of the gold depositional processes at the province (1:500,000), district (1:100,000) and camp (1:50,000) scales. At each scale, multivariate statistical techniques served to enhance multiple geological, geophysical, and geochemical datasets and extract from these data spatial proxies of the gold depositional processes. The results of this multi-scale predictive analysis were as follows: The first, province-scale model (M1) identified the entire gold prospective tract and the areas within it that may be of greatest relevance to future exploration. The second, district-scale model (M2) identified the different gold camps within the prospective tract and mapped the areas of gold favorability in a more detailed manner. The third, camp-scale model (M3) identified areas that, based on the current knowledge and distribution of high resolution geodata, are the most favorable whilst also being small enough as to permit target testing using conventional mineral exploration tools such as geophysics, geochemistry and/or drilling. The results obtained from our predictive models were validated by comparing them against the known gold occurrences using ROC (receiver operating characteristics) curves and AUC (area under the curve) graphs. According to these validations, model Ml scored an accuracy of 93.38%, whereas models M2 and M3 scored accuracies of 88.31% and 93.38%, respectively. A key observation made in the course of this study is that the gold prospective area as predicted by models M1, M2 and M3 varies according to the scale of the analysis. A novel factor in our approach is that we aimed assess the targeting criteria and spatial datasets that underpin them according to their spatial resolution and presented the results in form of integrated maps. In addition, the tools developed in this study have the capacity to reduce the cost of direct detection technologies regarding the transition from broad regional to camp scale at the early stages of mineral exploration, where the most initial decisions in search and area reduction are critical.	[Ferreira Uchoa, Juliane Cristina; Bemfica Toledo, Catarina Laboure; Silva, Adalene Moreira; Carmelo, Adriana Chatack] Univ Brasilia, Inst Geosci, Campus Univ Darcy Ribeiro S-N, BR-70910900 Brasilia, DF, Brazil; [Mendonca, Augusto Ferreira] Hidrogeo Consultoria, Av Cent 595, Brasilia, DF, Brazil; [Hagemann, Steffen G.] Ctr Explorat Targeting CET UWA, 35 Stirling Highway, Perth, WA 6009, Australia; [Kreuzer, Oliver P.] James Cook Univ, Coll Sci & Engn, Econ Geol Res Ctr EGRU, Townsville, Qld 4811, Australia; [Kreuzer, Oliver P.] Concept Discovery, POB 5128, Rockingham Beach, WA 6969, Australia	Universidade de Brasilia; James Cook University	Uchoa, JCF (autor correspondente), Univ Brasilia, Inst Geosci, Campus Univ Darcy Ribeiro S-N, BR-70910900 Brasilia, DF, Brazil.	ju.ferreira.uchoa@gmail.com.br; catarinatoledo@unb.br; adalene@unb.br; afmendonca@uol.com.br; steffen.hagemann@uwa.edu.au; opkreuzer@gmail.com; chatack@unb.br	Toledo, Catarina/AAK-9928-2021; Carmelo, Adriana Chatack/AAK-9744-2021	Toledo, Catarina/0000-0002-2280-0979; Carmelo, Adriana Chatack/0000-0003-0745-3072; Kreuzer, Oliver/0000-0003-1587-618X; Moreira Silva, Adalene/0000-0001-6290-2374	Coordination for Enhancement of Higher Education Personnel (CAPES)	Coordination for Enhancement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	We gratefully acknowledge the Brazilian Geological Survey for permitting the use of geological, geochemical, and geophysical data in this research. We also thank the Laboratory of Applied Geophysics of the University of Brasilia for the technical support. J. C. Uchoa thanks the Coordination for Enhancement of Higher Education Personnel (CAPES) for her scholarship toward her doctoral research and Prof. Lydia Lobato for the advice. The authors thank Dr. Mahyar Yousefi and two anonymous reviewers for their comments and suggestions that helped to significantly improve this contribution.	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J	Figueiredo, TS; Santos, TP; Costa, KB; Toledo, F; Albuquerque, ALS; Smoak, JM; Bergquist, BA; Silva, EV				Figueiredo, Thiago S.; Santos, Thiago P.; Costa, Karen B.; Toledo, Felipe; Albuquerque, Ana Luiza S.; Smoak, Joseph M.; Bergquist, Bridget A.; Silva-Filho, Emmanoel Vieira			Effect of deep Southwestern Subtropical Atlantic Ocean circulation on the biogeochemistry of mercury during the last two glacial/interglacial cycles	QUATERNARY SCIENCE REVIEWS			English	Article						Mercury concentration; Paleoproductivity; Atlantic meridional overturning circulation; Organic matter remineralization; Calcium carbonate.dissolution	MILLENNIAL-SCALE CHANGES; ISOTOPIC COMPOSITION; ATMOSPHERIC CO2; SOUTH-ATLANTIC; ANTHROPOGENIC MERCURY; GLACIAL MAXIMUM; CLIMATE-CHANGE; WATER MASSES; CARBON; NEODYMIUM	During glacial/interglacial cycles, changes in the strength of the Atlantic Meridional Overturning Circulation (AMOC) modified the intermediate and deep-water mass proportions and high latitude productivity in the Atlantic Ocean. These factors influence the distribution and geochemical partitioning of trace metals in the ocean. Mercury is a redox and productivity-sensitive trace metal, making it a potential proxy of paleoenvironmental changes. Therefore, this work examines the effect of Atlantic Ocean circulation changes during the last two glacial/interglacial cycles on the biogeochemistry of Hg. For this, a high-resolution record of the total Hg concentration was determined in core GL-1090 collected from the Southwestern Subtropical Atlantic that represents the last 185 thousand years. During the reported glacial/interglacial cycles, Hg showed a distinct trend throughout Marine Isotope Stages with higher concentrations during periods of enhanced penetration of northern component water into the southwestern Atlantic. This is supported by the similarity of mercury variability with benthic foraminifera delta C-13, suggesting a strong influence of deep ocean circulation on the availability and accumulation of this metal in deep-sea sediments. Mercury geochemistry and particle scavenging were correlated with organic matter (OM) input at the core site. We also noted that mercury responded to redox variation in sediment after Termination II, which can be explained by the increase in deep ocean ventilation due to AMOC strengthening. This hypothesis was confirmed by the antiphase behavior of Hg and Total Organic Carbon when compared with Mn/Al ratios and CaCO3. Our work, therefore, allows for a better understanding of the processes leading to long-term mercury removal to sediments. (C) 2020 Elsevier Ltd. All rights reserved.	[Figueiredo, Thiago S.; Santos, Thiago P.; Albuquerque, Ana Luiza S.; Silva-Filho, Emmanoel Vieira] Fluminense Fed Univ, Geosci Geochem Grad Program, Environm Geochem, BR-24020141 Niteroi, RJ, Brazil; [Costa, Karen B.; Toledo, Felipe] Univ Sao Paulo, Inst Oceanog, Lab Paleoceanog Atlantico, Praca Oceanog,191 Cidade Univ, BR-05508120 Sao Paulo, SP, Brazil; [Smoak, Joseph M.] Univ S Florida, Sch Geosci, St Petersburg, FL 33701 USA; [Bergquist, Bridget A.] Univ Toronto, Dept Earth Sci, Toronto, ON M5S 3B1, Canada	Universidade Federal Fluminense; Universidade de Sao Paulo; State University System of Florida; University of South Florida; University of Toronto	Figueiredo, TS (autor correspondente), Fluminense Fed Univ, Geosci Geochem Grad Program, Environm Geochem, BR-24020141 Niteroi, RJ, Brazil.	thiagof.bio@gmail.com	Albuquerque, Ana Luiza S/C-5167-2013; Santos, Thiago P./AAN-6506-2021; Smoak, Joseph/E-2140-2012; Costa, Karen B/N-5713-2015; da Silva Filho, Emmanoel Vieira/Y-7281-2019	Albuquerque, Ana Luiza S/0000-0003-1267-6190; Smoak, Joseph/0000-0002-4322-4042; Costa, Karen B/0000-0002-4757-0524; da Silva Filho, Emmanoel Vieira/0000-0001-6444-6851; Santos, Thiago/0000-0002-9273-3329	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; CAPESASpECTO project [88887.091731/2014-01]; PALEOCEANO-CAPES [23038.001417/2014-71]; CLIMATE-PRINT-UFF Project [CAPES 88887.310301/2018-00]; Foundation for Research Support of the State of Rio de Janeiro [FAPERJ E-26/203.037/2017]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CAPESASpECTO project; PALEOCEANO-CAPES; CLIMATE-PRINT-UFF Project; Foundation for Research Support of the State of Rio de Janeiro	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001. The authors are grateful for funding from CAPESASpECTO project (grant 88887.091731/2014-01) and PALEOCEANO-CAPES (23038.001417/2014-71). We thank R. Kowsman (CENPES/PETROBRAS) and PETROBRAS Core Repository staff (Macae/PETROBRAS) for supplying the sediment used in this study. The authors are also grateful for the support of the CLIMATE-PRINT-UFF Project (grant CAPES 88887.310301/2018-00). E. Silva-Filho is senior researcher of the National Council for Research and Development (CNPq, Brazil) and the Foundation for Research Support of the State of Rio de Janeiro (FAPERJ E-26/203.037/2017). 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Sci. Rev.	JUL 1	2020	239								106368	10.1016/j.quascirev.2020.106368	http://dx.doi.org/10.1016/j.quascirev.2020.106368			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	LZ3KI					2023-06-23	WOS:000541126600015
J	Fossen, H; Cavalcante, C; Konopasek, J; Meira, VT; de Almeida, RP; Hollanda, MHBM; Trompette, R				Fossen, Haakon; Cavalcante, Carolina; Konopasek, Jiri; Meira, Vinicius T.; de Almeida, Renato Paes; Hollanda, Maria Helena B. M.; Trompette, Roland			A critical discussion of the subduction-collision model for the Neoproterozoic Aracuai-West Congo orogen	PRECAMBRIAN RESEARCH			English	Article							SAO-FRANCISCO CRATON; PRESSURE METAMORPHIC ROCKS; SE BRAZIL IMPLICATIONS; MOLTEN MIDDLE CRUST; RIBEIRA BELT; MAGMATIC ARC; PAN-AFRICAN; TECTONIC EVOLUTION; EASTERN BRAZIL; INTRACONTINENTAL TERMINATION	The Neoproterozoic Aracuai-West Congo orogen in Brazil and Congo represents a branch of the Brasiliano/Pan-African orogenic system that is considered to terminate northward into a confined cratonic environment defined by the horseshoe-shaped pre-Atlantic Sao Francisco-Congo craton. The prevailing interpretation is that this orogen formed as a result of 50 m.y. of subduction leading to a classical continent-continent collision. This subduction-collision model hinges on interpretation of 630-580 Ma granitoids in the core of the orogen as being arc-related, and of locally exposed mafic and ultramafic metamorphic rocks as being ophiolitic. We show that when tested beyond geochemical signature, the model has fundamental problems that cannot be accounted for. In particular, there is an insurmountable oceanic space problem in this confined setting that is overlooked in most of the current literature. There are also problems with subduction initiation, lack of unambiguous evidence for oceanic crust, no trace of any high-P metamorphism and the abrupt termination of an ocean with no realistic way to transfer the large amount of oceanic opening displacement and subsequent convergence required by the model. We conclude that the prevailing subduction-collision model cannot possibly work and argue that the existing data are more consistent with hot intracontinental orogeny. We stress the importance of building tectonic models on more than one type of data, making realistic restorations and palinspastic reconstructions, and taking into account modern geotectonic knowledge.	[Fossen, Haakon] Univ Bergen, Museum Nat Hist, Dept Earth Sci, Postboks 7803, N-5020 Bergen, Norway; [Cavalcante, Carolina] Univ Fed Parana, Dept Geol, Ave Coronel Francisco H Santos 100, BR-81531980 Curitiba, Parana, Brazil; [Cavalcante, Carolina; Konopasek, Jiri] UiT Arctic Univ Norway, Postboks 6050 Langnes, N-9037 Tromso, Norway; [Konopasek, Jiri] Czech Geol Survey, Klarov 3, Prague 11821 1, Czech Republic; [Meira, Vinicius T.] Univ Estadual Campinas, Inst Geociencias, Campinas, Brazil; [de Almeida, Renato Paes; Hollanda, Maria Helena B. M.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508900 Sao Paulo, SP, Brazil; [Trompette, Roland] 35 Rue Pascal, F-75013 Paris, France	University of Bergen; Universidade Federal do Parana; UiT The Arctic University of Tromso; Czech Geological Survey; Universidade Estadual de Campinas; Universidade de Sao Paulo	Fossen, H (autor correspondente), Univ Bergen, Museum Nat Hist, Dept Earth Sci, Postboks 7803, N-5020 Bergen, Norway.	haakon.fossen@uib.no	Konopasek, Jiri/J-6658-2016; Fossen, Haakon/GQH-4511-2022; Meira, Vinícius T/S-5433-2016; Almeida, Renato/G-2567-2013	Konopasek, Jiri/0000-0001-5625-3996; Meira, Vinícius T/0000-0002-0947-9631; Hollanda, Maria Helena Bezerra Maia/0000-0003-2231-7917; Almeida, Renato/0000-0003-3664-1558	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo [2015/23572-5, 2010/03537-7, 2013/19061-0]; Czech Science Foundation [18-24281S]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [404767/2016-8]	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Czech Science Foundation(Grant Agency of the Czech Republic); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was supported by Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (grant 2015/23572-5 to HF, and 2010/03537-7 and 2013/19061-0 to CC), by the Czech Science Foundation (grant no. 18-24281S to JK) and by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (grant no. 404767/2016-8 to VTM). We are grateful to Olivier Vanderhaeghe and an anonymous second reviewer for very useful and constructive comments, and to Victoria Pease for excellent editorial handling.	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Vanderhaeghe O, 2009, TECTONOPHYSICS, V477, P119, DOI 10.1016/j.tecto.2009.06.021; Vauchez A, 2007, TERRA NOVA, V19, P278, DOI 10.1111/j.1365-3121.2007.00747.x; Vauchez A, 2019, TECTONOPHYSICS, V766, P500, DOI 10.1016/j.tecto.2019.05.013; Wakabayashi J, 2007, INT GEOL REV, V49, P873, DOI 10.2747/0020-6814.49.10.873; Xia LQ, 2019, GONDWANA RES, V65, P43, DOI 10.1016/j.gr.2018.08.006; [No title captured]	102	32	32	0	2	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0301-9268	1872-7433		PRECAMBRIAN RES	Precambrian Res.	JUL	2020	343								105715	10.1016/j.precamres.2020.105715	http://dx.doi.org/10.1016/j.precamres.2020.105715			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN3IN		Green Published, hybrid			2023-06-23	WOS:000532835600007
J	Fraga, GD; Ruy, ADS; Pontes, LAM; Campos, LMA; Teixeira, LSG				Fraga, Gabrielle das, V; Ruy, Alisson D. S.; Pontes, Luiz A. M.; Campos, Leila M. A.; Teixeira, Leonardo S. G.			PERSPECTIVES AND CHALLENGES OF ITACONIC ACID PRODUCTION FROM BIOMASS	QUIMICA NOVA			Portuguese	Review						itaconic acid; platform molecule; global market; Aspergillus terreus; microorganism	ASPERGILLUS-TERREUS; FILAMENTOUS FUNGI; FERMENTATION; ENZYMES; STARCH	Itaconic acid (IA) is a very promising platform molecule due to the possibility of it being used to obtain products such as methyl methacrylate and synthetic latex, with the prospect that its global market will grow at an average annual rate of 2.8% (CAGR) from 2021 to 2026, exceeding US$ 116.6 million in sales. The main technological route used to obtain itaconic acid is fermentation using different strains of Aspergillus terreus fungi. The main advancements are related to genetic engineering. as Aspergillus terreus is the most tolerant of the microorganisms employed in the process synthesis and optimization. The main substrate used is glucose (52%), followed by glycerol (25%). Among the results presented in this paper, the best production was achieved using Ustilago maydis, with 220 g of L-1, yielding 0.33 g g(-1), using glucose as a carbon source. Moreover, it is necessary to continue optimizing the biological process of IA production, since it is a platform molecule with major economic potential.	[Fraga, Gabrielle das, V; Ruy, Alisson D. S.; Pontes, Luiz A. M.] Univ Fed Bahia, Dept Engn Quim, BR-40210630 Salvador, BA, Brazil; [Campos, Leila M. A.] Univ Salvador, Escola Engn Arquitetura & TI, BR-41940560 Salvador, BA, Brazil; [Teixeira, Leonardo S. G.] Univ Fed Bahia, Inst Quim, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Salvador (UNIFACS); Universidade Federal da Bahia	Pontes, LAM (autor correspondente), Univ Fed Bahia, Dept Engn Quim, BR-40210630 Salvador, BA, Brazil.	uolpontes@uol.com.br	Pontesa, Luiz/AAL-1539-2021; Teixeira, Leonardo S G/J-9131-2016; Pontes, Luiz/GXN-0596-2022; Campos, Leila/ABD-5362-2020	Teixeira, Leonardo S G/0000-0003-0320-8299; Pontes, Luiz/0000-0003-4158-4033; 				Arcano Y. 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Nova	JUL	2020	43	7					951	958		10.21577/0100-4042.20170573	http://dx.doi.org/10.21577/0100-4042.20170573			8	Chemistry, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	ND6DB		gold			2023-06-23	WOS:000561987100015
J	Guimaraes, LM; De Franca, EJ; de Arruda, GN; de Albergaria-Barbosa, ACR				Guimaraes, Lucas Medeiros; De Franca, Elvis Joacir; de Arruda, Gilberto Nascimento; Rizzatti de Albergaria-Barbosa, Ana Cecilia			Historical inputs of polycyclic aromatic hydrocarbons in the preserved tropical estuary of the Itapicuru River, Bahia, Brazil	MARINE POLLUTION BULLETIN			English	Article						Atlantic ocean coast; Contamination; Sediment core; GC-MS	SEDIMENTS; PB-210	The aim of present study was to evaluate temporal changes in the distribution of polycyclic aromatic hydrocarbons (PAHs) in the estuary of the Itapicuru (Brazil). A sediment core was sampled in the study area. Concentrations of the 16 priority PAHs were analyzed using gas chromatography coupled to a mass spectrometry. A gas flow proportional counter was used to estimate the sedimentation rate through the determination of Pb-210. Granulometric fractions and total organic carbon (TOC) concentrations were also evaluated. Concentrations of TOC and PAHs ranged from 0.65 to 2.51% and 1.98 to 43.1 ng g(-1) (dry weight), respectively. Significant correlations (p<.05) were found between the mud content in the sediment core samples and concentrations of both TOC and PAHs. Higher PAH concentrations occurred after the 1950s. The main sources of PAHs over time were local human activities on the northern coast of the state of Bahia.	[Guimaraes, Lucas Medeiros; Rizzatti de Albergaria-Barbosa, Ana Cecilia] Univ Fed Bahia, Lab Geoquim Marinha, Inst Geociencias, Rua Barao de Jeremoabo Sn, BR-40170115 Salvador, BA, Brazil; [De Franca, Elvis Joacir; de Arruda, Gilberto Nascimento] Ctr Reg Ciencias Nucl Nordeste, Av Prof Luis Freire 200, BR-50740545 Recife, PE, Brazil; [Rizzatti de Albergaria-Barbosa, Ana Cecilia] Univ Fed Bahia, Lab Estudos Petr, Inst Geociencias, Rua Barao de Jeremoabo Sn, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia	de Albergaria-Barbosa, ACR (autor correspondente), Univ Fed Bahia, Lab Geoquim Marinha, Inst Geociencias, Rua Barao de Jeremoabo Sn, BR-40170115 Salvador, BA, Brazil.	cecilia.albergaria@ufba.br	de+Albergaria+Barbosa, Ana/AAQ-3872-2020; Guimarães, Lucas/AAN-2907-2020; de Albergaria-Barbosa, Ana Cecília/AAC-6940-2021; De França, Elvis/AAC-6986-2020	Guimarães, Lucas/0000-0001-6615-5812; De França, Elvis/0000-0002-0027-2028; Albergaria-Barbosa, Ana Cecilia R./0000-0003-2121-9792	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001]; Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB) [CNV0005/2013, CNV0025/2013]; CAPES; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ) [305210/2019-0]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was developed for the Programa de Pos-Graduacao em Geoquimica: Petroleo e Meio Ambiente (POSPETRO) of Universidade Federal da Bahia (UFBA) supported by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) -financial code 001. The study was mainly funded by the Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB; CNV0005/2013; CNV0025/2013). L. M. Guimaraes thanks CAPES for a scholarship. A.C.R. Albergaria-Barbosa thanks Conselho Nacional de Desenvolvimento Cientifico e Tecnologico for awarding a research grant (CNPQ; 305210/2019-0). The authors also thank Andre Luiz Amorim dos Santos Junior and the community of Siribinha (Conde, BA) for support regarding accommodations and sampling efforts during the collection period and Juliana de Souza Santana for the creation of the maps. The authors also thank the anonymous reviewer for the constructive suggestions and comments that improved the manuscript.	Albergaria-Barbosa A.C.R., 2017, MAR POLLUT B, V129, P822; Albuquerque PTF, 2019, J RADIOANAL NUCL CH, V321, P875, DOI 10.1007/s10967-019-06665-9; Almeida M., 2018, BRAZIL MAR POLLUT B, V137, P339; [Anonymous], REV BRASILEIRA GEOCI; Barcellos R. 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Pollut. Bull.	JUL	2020	156								111218	10.1016/j.marpolbul.2020.111218	http://dx.doi.org/10.1016/j.marpolbul.2020.111218			6	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	LW5AS	32510369				2023-06-23	WOS:000539160000030
J	Lourenco, RA; Combi, T; Alexandre, MD; Sasak, ST; Zanardi-Lamardo, E; Yogui, GT				Lourenco, Rafael Andre; Combi, Tatiane; Alexandre, Marcelo da Rosa; Sasak, Silvio Tarou; Zanardi-Lamardo, Eliete; Yogui, Gilvan Takeshi			Mysterious oil spill along Brazil's northeast and southeast seaboard (2019-2020): Trying to find answers and filling data gaps	MARINE POLLUTION BULLETIN			English	Article						Petroleum; Brazilian coast; Chemical characterization; Diagnostic ratios; Fingerprint; Forensic methodology		Large amounts of crude oil were found along Brazil's northeast and southeast seaboard from August 2019 to January 2020. Petroleum companies and oil tankers reported no accidents previously or during this period. The stranded oil on Brazilian beaches looks like tar; it has solid aspect and is denser than seawater. Chemical characterization of this oil showed that light hydrocarbons were still present, increasing the probability of negative effects to coastal organisms and ecosystems upon release in the water column. Diagnostic ratios, chromatogram pattern, and percentage-weathering plots proved that the oil samples share the same oil source. This work provides data for future comparison with oil samples that will likely be found stranded along the Brazilian shoreline in the years to come, helping to understand long term issues associated with the mysterious oil spill that made landfall in late 2019.	[Lourenco, Rafael Andre] Univ Sao Paulo, Inst Oceanog, Praca Oceanog 191,Cidade Univ, BR-05508120 Sao Paulo, Brazil; [Combi, Tatiane] Univ Fed Bahia IGEO UFBA, Inst Geociencias, BR-40170020 Salvador, BA, Brazil; [Alexandre, Marcelo da Rosa] Univ Fed Sergipe DQI UFS, Dept Quim, BR-49100000 Sao Cristovao, SE, Brazil; [Sasak, Silvio Tarou] Univ Fed Sul Bahia CFCAM UFSB, Ctr Formacao Ciencias Ambientais, BR-45810000 Itabuna, BA, Brazil; [Zanardi-Lamardo, Eliete; Yogui, Gilvan Takeshi] Univ Fed Pernambuco DOCEAN UFPE, Dept Oceanog, BR-50740550 Recife, PE, Brazil	Universidade de Sao Paulo	Lourenco, RA (autor correspondente), Univ Sao Paulo, Inst Oceanog, Praca Oceanog 191,Cidade Univ, BR-05508120 Sao Paulo, Brazil.	rafaell@usp.br	Lourenço, Rafael André/I-7041-2015; Yogui, Gilvan T/C-5021-2009; ZANARDI-LAMARDO, ELIETE/A-9084-2011; Combi, Tatiane/AAC-9936-2021; Combi, Tatiane/O-3004-2016	Lourenço, Rafael André/0000-0002-1446-5074; Yogui, Gilvan T/0000-0002-4720-3337; ZANARDI-LAMARDO, ELIETE/0000-0003-3546-6479; Combi, Tatiane/0000-0001-6769-7445	National Council funds GTY for Scientific and Technological Development - CNPq [310554/2019-5]	National Council funds GTY for Scientific and Technological Development - CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank Dr. P.S.M. Carvalho and Dr. A.S.X. Silva for collecting part of the oil samples. National Council funds GTY for Scientific and Technological Development - CNPq (grant no. 310554/2019-5). We thank the two anonymous reviewers for constructive comments, which substantially improved the manuscript.	Alford J.B., 2014, IMPACTS OIL SPILL DI, DOI [10.1201/b17633, DOI 10.1201/B17633]; ALI LN, 1995, MAR ENVIRON RES, V40, P319, DOI 10.1016/0141-1136(94)00149-J; Brum HD, 2020, SCIENCE, V367, P155, DOI 10.1126/science.aba0369; CEN, 2012, 1552222012 CENTR; Dahlmann G., 2015, HDB ENV CHEM, DOI [10.1007/698_2015_366, DOI 10.1007/698_2015_366]; Soares MD, 2020, MAR POLICY, V115, DOI 10.1016/j.marpol.2020.103879; Fingas M, 2015, HANDBOOK OF OIL SPILL SCIENCE AND TECHNOLOGY, P207; Gallotta F.D.C., 2018, OIL SPILL ENV FORENS, P515, DOI [10.1016/B978, DOI 10.1016/B978]; Guo Li-guo, 2010, Huanjing Kexue, V31, P1897; Magris RA, 2020, MAR POLLUT BULL, V153, DOI 10.1016/j.marpolbul.2020.110961; Peters K.E., 2007, BIOMARKER GUIDE, P1196; Radovic JR, 2014, MAR POLLUT BULL, V79, P268, DOI 10.1016/j.marpolbul.2013.11.029; Stout Scott A., 2008, V26, P54, DOI 10.1039/9781847558343-00054; Strom-Kristiansen T, 1997, 1997 INTERNATIONAL OIL SPILL CONFERENCE, P631; Wang ZD, 1999, J CHROMATOGR A, V843, P369, DOI 10.1016/S0021-9673(99)00120-X	15	55	55	5	14	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0025-326X	1879-3363		MAR POLLUT BULL	Mar. Pollut. Bull.	JUL	2020	156								111219	10.1016/j.marpolbul.2020.111219	http://dx.doi.org/10.1016/j.marpolbul.2020.111219			6	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	LW5AS	32366367				2023-06-23	WOS:000539160000048
J	Orellano, AP; Winocur, D; Rubinstein, NA; Tassinari, CCG				Orellano R, Ana Paula; Winocur, Diego; Rubinstein, Nora A.; Tassinari, Colombo C. G.			Age and origin of the Paramillos de Uspallata Pb-Zn-Ag vein deposit in the Cuyo basin, Argentina: Constraints from structural controls and isotopic evidence	ORE GEOLOGY REVIEWS			English	Article						Mesozoic metalogenesis; Cretaceous regime; Andean Precordillera	EVOLUTION; ANDES; PRECORDILLERA; MAGMATISM; RIFT; GEOCHRONOLOGY; GEOCHEMISTRY; DEFORMATION; METALLOGENY; PARALLEL	The Paramillos de Uspallata deposit, located in the Cuyo rift basin, is a Pb-Zn-Ag vein deposit hosted by Mesozoic Triassic volcano-sedimentary sequences. In the present study, new geological and isotopic data is used to constrain the age, source and structural controls of the ore forming fluids. The isotopic data suggest a Middle Cretaceous age for the mineralization and that mineralizing fluids were formed from a mixture of sources that includes the Permian volcanic rocks from the basin basement and the Triassic basalts, with Pb (and Sr) isotopic composition typical of the upper crust. Regional structural analysis allowed to conclude that the veins formed within large-scale reactivated structures that affect the basin basement. Local structural analysis showed that the mineralization was controlled by extensional and shear-extensional WNW-ESE to NW-SE and shear E-W trending structures. Kinematic analyses performed in the veins evidenced a transtensional environment with a NE extension direction and E-W dextral shear. In this scenario fluids were channeled by a strike-slip-faulting system connected with a deep weakness zone during the beginning of the Andean Orogeny. This study provides new insights into the genesis and the geodynamic scenario of Pb-Zn-Ag vein deposit.	[Orellano R, Ana Paula; Rubinstein, Nora A.] Univ Buenos Aires, Inst Geociencias Basicas Aplicadas & Ambientales, CONICET, Intendente Guiraldes 2160,Pabellon 2,Piso 1, Buenos Aires, Argentina; [Winocur, Diego] Univ Buenos Aires, Inst Estudios Andinos Don Pablo Groeber, Intendente Guiraldes 2160,Pabellon 2,Piso 1, Buenos Aires, Argentina; [Tassinari, Colombo C. G.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508900 Sao Paulo, SP, Brazil	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires; University of Buenos Aires; Universidade de Sao Paulo	Orellano, AP (autor correspondente), Univ Buenos Aires, Inst Geociencias Basicas Aplicadas & Ambientales, CONICET, Intendente Guiraldes 2160,Pabellon 2,Piso 1, Buenos Aires, Argentina.	anapaula.orri@gmail.com		Rubinstein, Nora/0000-0002-2752-7107	National Sciences and Technology Council, Argentina [PIP CONICET 112 201301 00107]; SEG	National Sciences and Technology Council, Argentina; SEG	This research was funded by the National Sciences and Technology Council, Argentina (PIP CONICET 112 201301 00107). The authors wish to thank the SEG for the student grant used to partially funded the isotopic analyses. Comments of Sebastian Oriolo and an anonymous reviewer help to eliminate inconsistences and improved the quality of the manuscript.	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Rev.	JUL	2020	122								103524	10.1016/j.oregeorev.2020.103524	http://dx.doi.org/10.1016/j.oregeorev.2020.103524			14	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	LU5OZ					2023-06-23	WOS:000537805900039
J	Pinto, VM; Koester, E; Debruyne, D; Chemale, F; Marques, JC; Porcher, CC; Passos, LH; Lenz, C				Pinto, Viter Magalhaes; Koester, Edinei; Debruyne, David; Chemale, Farid; Marques, Juliana Charao; Porcher, Carla Cristine; Passos, Luiz Henrique; Lenz, Cristine			Petrogenesis of the mafic-ultramafic Caninde layered intrusion, Sergipano Belt, Brazil: Constraints on the metallogenesis of the associated Fe-Ti oxide ores	ORE GEOLOGY REVIEWS			English	Article						Layered intrusion; Caninde Domain; Sergipano Belt; Fractional crystallization; Magnetitite ore; Metallogenesis	LARGE IGNEOUS PROVINCE; BUSHVELD COMPLEX; UPPER ZONE; OXYGEN FUGACITY; TRACE-ELEMENTS; SOUTH-AFRICA; SW CHINA; DEPOSITS; OLIVINE; ORIGIN	The Caninde layered intrusion is hosted by a Neoproterozoic volcano-sedimentary sequence and contains Fe-Ti mineralization in the Caninde Domain of the Brazilian Sergipano Belt. The petrochemistry of this layered complex and the metallogenesis of the associated Fe-Ti oxide mineralization are still enigmatic. The intrusion comprises three main outcropping rock units from north to south: Unit I contains melanotroctolite and olivine gabbro/gabbronorite, Unit II consists of gabbro and (leuco)troctolite, and the Fe-Ti mineralized Unit III contains leucogabbro with stringers or lenses of pegmatitic gabbro, apatite-bearing gabbro, hornblende-bearing gabbro, Fe-diorite, oxide gabbro, gabbro with Fe-Ti cumulate layers, and magnetitite. The mineralized Unit III contains low-Cr magnetite and ilmenite +/- hercynite occurring disseminated and as massive mineralization in layers and lenses within the leucogabbro, close to the contact aureoles with the surrounding calc-silicate and amphibolite rocks. LA-ICP-MS U-Pb zircon dating of a gabbro sample from Unit II yields an age of 703.5 +/- 1.6 Ma. The age-corrected epsilon(Nd) (t = 703 Ma) in the Caninde intrusion range from + 1.3 to + 4.3. Together with the depleted Sr-87/Sr-86, ratios of 0.7032-0.7040, these data strongly indicate a relatively depleted mantle source, with limited assimilation of crustal material. The low Sr-values may indicate a contribution from the subcontinental litho-spheric mantle (SCLM) and the observed isotopic heterogeneity can be accounted for by replenishment by distinct magma pulses and/or minor but varying crustal assimilation. Except for the magnetitites, all Caninde cumulates are enriched in LILE (Rb, K, Sr, Ba, and Pb). Their Nb-Ta and Zr-Hf depletions relative to the primitive mantle composition (Nb/Nb* 0.4-0.6; Zr/Zr* of 0.6-0.8) reflect their relative incompatibility in the early cumulates, and are at least partly compensated by Nb- and Zr-enriched magnetitites. Based on the observed petrochemical characteristics of the cumulates and comparison with similar layered intrusives, the inferred parental magma is similar to a hydrous tholeiitic basalt (Mg# 50-58) with intermediate Ti-content (1-2 wt% TiO2). Our petrogeochemical data further indicate that the Caninde rocks are predominantly related through cumulus-forming processes, with some assimilation in the border zones. Apatite saturation preceded magnetitite formation and was concentrated in apatite gabbro cumulates with <= 6 wt% MgO. The resulting phosphor-loss would have lowered Fe-solubility in the remaining liquid, and may thus have triggered formation of massive magnetitite Fe-Ti ore bodies at the top of the intrusion. Finally, no economic Ni-Cu resources were identified in the intermediate portions and drill core data are still needed to assess the potential for Cr-PGE resources in the unexposed lower portions.	[Pinto, Viter Magalhaes; Debruyne, David] Univ Fed Pelotas UFPEL, Ctr Engn, Engn Geol, Praca Domingos Rodrigues 02, BR-96010440 Pelotas, RS, Brazil; [Koester, Edinei; Marques, Juliana Charao; Porcher, Carla Cristine] Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias, Av Bento Goncalves 9500, BR-90501970 Pelotas, RS, Brazil; [Chemale, Farid] Univ Vale Rio dos Sinos UNISINOS, Programa Posgrad Geol, Av Unisinos 950, BR-93022000 Sao Leopoldo, RS, Brazil; [Passos, Luiz Henrique] Univ Brasilia UnB, Inst Geociencias, Campus Univ Darcy Ribeiro ICC Ala Cent, BR-70910900 Brasilia, DF, Brazil; [Lenz, Cristine] Univ Fed Sergipe, Dept Geol, Av Marechal Rondon S-N, BR-49100000 Sao Cristovao, SE, Brazil	Universidade Federal de Pelotas; Universidade Federal do Rio Grande do Sul; Universidade de Brasilia; Universidade Federal de Sergipe	Pinto, VM (autor correspondente), Univ Fed Pelotas UFPEL, Ctr Engn, Engn Geol, Praca Domingos Rodrigues 02, BR-96010440 Pelotas, RS, Brazil.	viter.pinto@gmail.com	Lenz, Cristine/HZJ-1012-2023; Porcher, Carla C/R-1419-2018; Koester, Edinei/L-3684-2017; Marques, Juliana C/R-1965-2018; Lenz, cristine/AAK-3293-2020; Debruyne, David/AAE-9589-2020	Porcher, Carla C/0000-0002-0418-3954; Koester, Edinei/0000-0002-4424-4782; Marques, Juliana C/0000-0003-0143-6925; Debruyne, David/0000-0002-5896-2742; lenz, cristine/0000-0002-5092-838X	CNPQ [484694/2011-1]	CNPQ(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank OGR reviewers Tong Hou and Zhong-Jie Bai for providing many helpful suggestions and constructive criticism that greatly improved this manuscript. VMP is supported by CNPQ grant nr. 484694/2011-1. Ingrid Mota, Francisco Dias De Souza Jr., and Rayane Gois provided invaluable assistance during the field campaigns.	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Rev.	JUL	2020	122								103535	10.1016/j.oregeorev.2020.103535	http://dx.doi.org/10.1016/j.oregeorev.2020.103535			18	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	LU5OZ					2023-06-23	WOS:000537805900032
J	Ribeiro, VS; Souza, SO; Costa, SSL; Almeida, TS; Soares, SAR; Korn, MGA; Araujo, RGO				Ribeiro, Vaniele S.; Souza, Sidnei O.; Costa, Silvanio Silverio L.; Almeida, Tarcisio S.; Soares, Sarah Adriana R.; Korn, Maria Gracas A.; Araujo, Rennan Geovanny O.			Speciation analysis of inorganic As and Sb in urban dust using slurry sampling and detection by fast sequential hydride generation atomic absorption spectrometry	ENVIRONMENTAL GEOCHEMISTRY AND HEALTH			English	Article						Urban dust; Arsenic and Antimony; Speciation chemical analysis; Doehlert matrix; Slurry sampling; FS-HG-AAS	AIRBORNE PARTICULATE MATTER; ROAD-DUST; HEAVY-METALS; HEALTH-RISK; CONTAMINATION ASSESSMENT; ANTIMONY SPECIATION; ARSENIC SPECIATION; BIOACCESSIBILITY; OPTIMIZATION; PARTICLES	In this work, a methodology for chemical speciation analysis of inorganic As and Sb in urban dust using slurry sampling and detection by fast sequential hydride generation atomic absorption spectrometry is proposed. Doehlert design and desirability function were used to find the optimum conditions for hydride generation (1.0 mol L-1HCl and 0.9% m v(-1)NaBH(4)). The accuracy of the analytical method was evaluated by analysis of reference material fly ash (BCR 176R), addition and recovery tests for inorganic As species, and comparison of independent methods for Sb determination in urban dust samples. The determination of the total concentrations of As and Sb and their inorganic species presented good accuracy, between 80 +/- 1 and 101 +/- 6%. Precision was expressed as the relative standard deviation and was better than 4.7% (n = 3). The limit-of-quantification values were 0.23 and 1.03 mg kg(-1)for As and Sb, respectively. The methodology was applied to eight samples of dust collected in an urban area of Salvador and Jaguaquara cities, Bahia, Northeast, Brazil, with an aerodynamic size lower than 38 mu m. Concentrations of pentavalent inorganic species (iAs(5+)and iSb(5+)) in relation to trivalent species (iAs(3+)and iSb(3+)) were found in urban dust collected in the city of Salvador, which are regarded as more toxic for both elements. The enrichment factor and geoaccumulation index (I-geo) values showed that for some samples, the concentrations of iAs and iSb presented strong enrichment and, and regarding environment, strong to moderately polluted by iAs and iSb, with an indication of anthropogenic contributions. The occurrence of these inorganic constituents in the urban area of Salvador can be related with intense industrial activities and vehicular traffic.	[Ribeiro, Vaniele S.; Souza, Sidnei O.; Almeida, Tarcisio S.; Korn, Maria Gracas A.; Araujo, Rennan Geovanny O.] Univ Fed Bahia, Inst Quim, Dept Quim Analit, BR-40170115 Salvador, BA, Brazil; [Ribeiro, Vaniele S.] Inst Fed Educ Ciencia & Tecnol Baiano, Campus Guanambi, BR-46430000 Guanambi, BA, Brazil; [Souza, Sidnei O.] Univ Fed Sergipe, Campus Lagarto, BR-49400000 Lagarto, Sergipe, Brazil; [Costa, Silvanio Silverio L.] Univ Fed Sergipe, Nucleo Petr & Gas, BR-49100000 Sao Cristovao, Sergipe, Brazil; [Soares, Sarah Adriana R.] Univ Fed Bahia, Inst Geociencias, Dept Oceanog, BR-40170020 Salvador, BA, Brazil; [Korn, Maria Gracas A.; Araujo, Rennan Geovanny O.] Univ Fed Bahia, Inst Nacl Ciencia & Tecnol, CNPq, INCT Energia & Ambiente, BR-40170115 Salvador, BA, Brazil; [Araujo, Rennan Geovanny O.] Univ Fed Bahia UFBA, Inst Quim, Dept Quim Analit, Grp Pesquisa Estudos Quim Analit & Ambiental GPEQ, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Instituto Federal Baiano (IFBAIANO); Universidade Federal de Sergipe; Universidade Federal de Sergipe; Universidade Federal da Bahia; Universidade Federal da Bahia	Araujo, RGO (autor correspondente), Univ Fed Bahia, Inst Quim, Dept Quim Analit, BR-40170115 Salvador, BA, Brazil.; Araujo, RGO (autor correspondente), Univ Fed Bahia, Inst Nacl Ciencia & Tecnol, CNPq, INCT Energia & Ambiente, BR-40170115 Salvador, BA, Brazil.; Araujo, RGO (autor correspondente), Univ Fed Bahia UFBA, Inst Quim, Dept Quim Analit, Grp Pesquisa Estudos Quim Analit & Ambiental GPEQ, BR-40170115 Salvador, BA, Brazil.	rgoa01@terra.com.br	COSTA, SILVÂNIO/AAV-1780-2021; de Oliveira Souza, Sidnei/AAA-5234-2020; Korn, Maria Graças/AAH-3445-2020; Silva de Almeida, Tarcisio/U-4368-2017	COSTA, SILVÂNIO/0000-0001-6094-209X; SOUZA, SIDNEI DE OLIVEIRA/0000-0001-8630-8599; OLIVEIRA ARAUJO, RENNAN GEOVANNY/0000-0001-6955-8115; Silva de Almeida, Tarcisio/0000-0003-1963-3775	Coordenação de Aperfeiçoamento de Pessoal de Nível Superior [001] Funding Source: Medline	Coordenação de Aperfeiçoamento de Pessoal de Nível Superior		AlSioufi L, 2016, MICROCHEM J, V124, P256, DOI 10.1016/j.microc.2015.09.004; Araujo RGO, 2008, TALANTA, V77, P400, DOI 10.1016/j.talanta.2008.06.047; Barra CM, 2000, QUIM NOVA, V23, P58, DOI 10.1590/S0100-40422000000100012; Bukowiecki N, 2010, ATMOS ENVIRON, V44, P2330, DOI 10.1016/j.atmosenv.2010.03.039; Calado V., 2003, E PAPERS SERVICOS ED; Candioti LV, 2014, TALANTA, V124, P123, DOI 10.1016/j.talanta.2014.01.034; Amorim FAC, 2008, QUIM NOVA, V31, P1784, DOI 10.1590/S0100-40422008000700033; Chen ML, 2014, TALANTA, V125, P78, DOI 10.1016/j.talanta.2014.02.037; Chen ZL, 2006, J SEP SCI, V29, P2671, DOI 10.1002/jssc.200500304; Correia CLT, 2010, MICROCHEM J, V96, P57; Ferreira SLC, 2010, APPL SPECTROSC REV, V45, P44, DOI 10.1080/05704920903435474; de Almeida TS, 2013, J BRAZIL CHEM SOC, V24, P700, DOI 10.5935/0103-5053.20130086; Feng SP, 2012, ENVIRON EARTH SCI, V66, P1881, DOI 10.1007/s12665-011-1412-2; Ferreira SLC, 2011, J ANAL ATOM SPECTROM, V26, P1887, DOI 10.1039/c1ja10108k; Garcia-Rico L, 2016, ARCH ENVIRON CON TOX, V70, P522, DOI 10.1007/s00244-015-0229-5; Goossens D, 2009, J ENVIRON MANAGE, V90, P3458, DOI 10.1016/j.jenvman.2009.05.031; Holler JF, 2009, PRINCIPIOS ANALISE I; Hu X, 2012, ATMOS ENVIRON, V57, P146, DOI 10.1016/j.atmosenv.2012.04.056; Iijima A, 2010, J ANAL ATOM SPECTROM, V25, P356, DOI 10.1039/b920597g; Izhar S, 2016, CHEMOSPHERE, V146, P582, DOI 10.1016/j.chemosphere.2015.12.039; Jadoon WA, 2018, ARCH ENVIRON CON TOX, V74, P32, DOI 10.1007/s00244-017-0475-9; Karanasiou A, 2011, ATMOS MEAS TECH, V4, P2409, DOI 10.5194/amt-4-2409-2011; LADEIRA A. 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L., 2003, GEOCHEMISTRY 2 EDITI, P1, DOI [DOI 10.1016/B978-0-08-095975-7.00301-6.4, DOI 10.1016/B0-08-043751-6/03016-4, 10.1016/B0-08-043751-6/03016-4]; Shao L, 2013, ACTA GEOCHIM, V32, P420, DOI 10.1007/s11631-013-0651-1; Shen ZX, 2016, SCI TOTAL ENVIRON, V569, P619, DOI 10.1016/j.scitotenv.2016.06.156; Silva MM, 2017, TALANTA, V165, P502, DOI 10.1016/j.talanta.2016.12.022; Varrica D, 2013, ATMOS ENVIRON, V64, P18, DOI 10.1016/j.atmosenv.2012.08.067; Vasconcellos PC, 2011, ATMOS ENVIRON, V45, P5770, DOI 10.1016/j.atmosenv.2011.07.018; Wuana R.A., 2011, ISRN ECOL, V2011, P1, DOI [10.5402/2011/402647, DOI 10.5402/2011/402647]; Zhao HT, 2016, SCI TOTAL ENVIRON, V550, P167, DOI 10.1016/j.scitotenv.2016.01.110; Zhao N, 2014, INT J ENV RES PUB HE, V11, P2536, DOI 10.3390/ijerph110302536	45	4	4	1	49	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0269-4042	1573-2983		ENVIRON GEOCHEM HLTH	Environ. Geochem. Health	JUL	2020	42	7					2179	2193		10.1007/s10653-019-00488-z	http://dx.doi.org/10.1007/s10653-019-00488-z			15	Engineering, Environmental; Environmental Sciences; Public, Environmental & Occupational Health; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology; Public, Environmental & Occupational Health; Water Resources	MP2DD	31853769				2023-06-23	WOS:000552019000023
J	Rocha, ERV; Marques, LS; Babinski, M; Machado, FB; Petronilho, LA; Nardy, AJR				Rocha-Junior, E. R., V; Marques, L. S.; Babinski, M.; Machado, F. B.; Petronilho, L. A.; Nardy, A. J. R.			A telltale signature of Archean lithospheric mantle in the Parana continental flood basalts genesis	LITHOS			English	Article						Parana continental flood basalts; Re-Os isotopic systematics; Heterogeneous lithospheric mantle; Paranapanema fragmented lithosphere; Archean lithosphere	MID-ATLANTIC RIDGE; RE-OS ISOTOPE; TRACE-ELEMENT; PERIDOTITE XENOLITHS; HIGH-TI; CRUSTAL CONTAMINATION; GEOCHEMICAL EVIDENCE; STRUCTURE BENEATH; SOUTHERN BRAZIL; PLATEAU BRAZIL	The origin of the Parana Continental Flood Basalts (PCFB), which constitute one of largest magmatic provinces in the world, remains a very controversial subject, particularly whether melts are sourced in the mesosphere (deep mantle plume), asthenosphere and/or lithosphere. In an effort to scrutinize those competing hypotheses, new measurements of Os, Nd, Sr and Pb isotopes, along with major and trace elements are presented for low-TiO2 tholeiites from the province. This suite occurs discreetly in the central-north of the province (termed Ribeira magmatype), whose lithospheric structure is characterized by higher P- and S- wave velocities, and high electrical resistivity. The initial Os-187/Os-188 isotopic compositions in Ribeira lavas, ranging from 0.10660 to 0.12575, are more unradiogenic than the other magma-types of the PCFB, as well as the estimates of the contemporary Depleted Mantle and are lower than any osmium isotopic ratio yet reported for continental flood basalts. These remarkably unradiogenic Os-187/Os-188 ratios preclude significant continental crust contamination and require the involvement of an ancient subcontinental lithospheric mantle source that evolved in a very low Re/Os environment. The fact that the Ribeira rocks occur on a peculiar lithospheric geophysical structure and have a unique unradiogenic osmium isotope signature reveals for the first time the existence of Archean lithosphere concealed by the Parana Basin, inserted in the Paranapanema fragmented lithosphere. On the other hand, the other magmatypes of the province, whose osmium isotopic signature is similar to the modern fertile mantle, occur close to more electrically conductive lithospheric structures. Thus, osmium isotopic information integrated with recent crustal and upper mantle geophysical soundings provides crucial information about the PCFB mantle sources. To account for the combined Os, Nd, Sr and Pb isotopic compositions of the Ribeira rocks, we propose that the primary melts formed from the heterogeneous lithospheric mantle (including Archean lithosphere fragments) that was variably hybridized by melts derived from recycling of eclogites related to multiple Neoproterozoic-Cambrian suture zones that surround the Parana Basin and subduction processes. (C) 2020 Elsevier B.V. All rights reserved.	[Rocha-Junior, E. R., V] Univ Fed Bahia, Inst Fis, Dept Fis Terra & Meio Ambiente, BR-40170115 Salvador, BA, Brazil; [Marques, L. S.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226, BR-05508090 Sao Paulo, SP, Brazil; [Babinski, M.; Petronilho, L. A.] Univ Sao Paulo, Inst Geociencias, BR-05422970 Sao Paulo, SP, Brazil; [Machado, F. B.] Univ Fed Parana, Dept Geol, BR-81270460 Curitiba, PR, Brazil; [Nardy, A. J. R.] Univ Estadual Paulista, Inst Geociencias & Ciencias Exatas, BR-13506900 Rio Claro, SP, Brazil	Universidade Federal da Bahia; Universidade de Sao Paulo; Universidade de Sao Paulo; Universidade Federal do Parana; Universidade Estadual Paulista	Rocha, ERV (autor correspondente), Univ Fed Bahia, Inst Fis, Dept Fis Terra & Meio Ambiente, BR-40170115 Salvador, BA, Brazil.	eduardo.junior@ufba.br	Babinski, Marly/B-9403-2013; Rocha-Júnior, Eduardo R. V./J-7888-2015; Rocha-Júnior, Eduardo R. V./L-3537-2016	Babinski, Marly/0000-0003-2444-2404; Rocha-Junior, Eduardo/0000-0003-1853-015X	Sao Paulo Research Foundation (FAPESP) [2013/02748-2]; FAPESP [2012/060826]	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	ERV Rocha-Juniorwas supported by Postdoctoral scholarship (Grant 2013/02748-2) of the Sao Paulo Research Foundation (FAPESP). We are grateful to Artur T. Onoe and Kei Sato for technical assistance. We also thank Naomi Ussami for very constructive comments and fruitful scientific discussions that improved the quality of the manuscript. Richard Carlson and Stefan Jung are thanked for insightful and very helpful reviews and comments.; The editorial handling of Greg Shelnuttwas greatly appreciated. This research is a contribution to the FAPESP Thematic Project 2012/060826. LS Marques and M Babinski are CNPq Fellow Researchers.	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J	Salomao, GN; Dall'Agnol, R; Sahoo, PK; Angelica, RS; de Medeiros, CA; Ferreira, JD; da Silva, MS; Souza, PWME; Nascimento, WR; da Costa, MF; Guilherme, LRG; de Siqueira, JO				Salomao, Gabriel Negreiros; Dall'Agnol, Roberto; Sahoo, Prafulla K.; Angelica, Romulo Simes; de Medeiros Filho, Carlos A.; Ferreira Junior, Jair da Silva; da Silva, Marcio Sousa; Martins e Souza Filho, Pedro Walfir; Nascimento Junior, Wilson Rocha; da Costa, Marlene F.; Guimaraes Guilherme, Luiz Roberto; de Siqueira, Jose Oswaldo			Geochemical mapping in stream sediments of the Carajas Mineral Province: Background values for the Itacaiunas River watershed, Brazil	APPLIED GEOCHEMISTRY			English	Article						Multi-element analysis; Stream sediments; Microcatchment-based geochemical mapping; Iron; Potentially toxic elements; Southeastern amazon	POTENTIALLY TOXIC ELEMENTS; U-PB GEOCHRONOLOGY; AMAZONIAN CRATON; HYDROTHERMAL ALTERATION; QUALITY GUIDELINES; BASE-LINE; DEPOSIT; AREA; MAGMATISM; THRESHOLD	Multi-elemental analysis of high-density (regional-scale) geochemical surveys is an important strategy for multipurpose applications, particularly in addressing geochemical background concentrations in different sampling media. This approach was applied to the Itacaiunas River Watershed (IRW), which is situated in the most prominent mining area of Brazil, the Carajas Mineral Province. Microcatchment-based mapping (similar to 50 km(2) each) covering the whole extent of IRW was delimited using remote sensing techniques and targeted for sampling. A total of 788 samples, including 27 duplicates, were collected in 2017. The <0.177 mm fraction of all samples was digested by aqua regia and 51 elements were analyzed by inductively coupled plasma atomic emission spectroscopy (ICP-AES) and inductively coupled plasma mass spectrometry (ICP-MS). Geochemical maps for Fe and potentially toxic elements (PTE; As, Ba, Cd, Co, Cr, Cu, Hg, Mn, Mo, Ni, Pb, Sn, V, and Zn) and microcatchment-based distribution maps based on threshold values were constructed for the whole IRW. The stream sediment geochemistry is mainly controlled by the local geologic setting and underlying lithology. Geochemical background (GB) values for 43 elements in stream sediments of the IRW were determined by a variety of methods (Tukey's inner fences - TIF, median +/- 2*median absolute deviation - MAD, and percentile-based techniques). The results provided from the different methods show a wide range of values, with the MAD method being considered the most appropriate for deriving GB concentrations. A comparison of reference levels for PTE contemplated in the Brazilian regulation in stream sediments, the threshold concentrations obtained for the IRW area, and different study cases around the world is presented in detail. Our findings provide not only valuable information for selecting potential areas for mineral exploration surveys, but also for evaluating geochemical contaminant effects with time-varying treatments. Studies conducted to determine background values at regional scale are needed for environmental decision making, as well as to attest actions in cases of potential contamination. In the absence of these studies, misleading interpretations of the magnitude of contamination levels in a certain area may cause under- or overestimation of ecological and/or human-health risks of PTE.	[Salomao, Gabriel Negreiros; Dall'Agnol, Roberto; Angelica, Romulo Simes; Martins e Souza Filho, Pedro Walfir] Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa 1, BR-66075110 Belem, Para, Brazil; [Salomao, Gabriel Negreiros; Dall'Agnol, Roberto; Sahoo, Prafulla K.; Ferreira Junior, Jair da Silva; da Silva, Marcio Sousa; Martins e Souza Filho, Pedro Walfir; Nascimento Junior, Wilson Rocha; de Siqueira, Jose Oswaldo] Inst Tecnol Vale, Rua Boaventura da Silva 955, BR-66055090 Belem, Para, Brazil; [Sahoo, Prafulla K.] Cent Univ Punjab, Sch Environm & Earth Sci, Dept Environm Sci & Technol, Bathinda 151001, India; [de Medeiros Filho, Carlos A.] Vale SA Exploracao Mineral, Rua Grajau 63, BR-68515000 Parauapebas, PA, Brazil; [da Silva, Marcio Sousa] Univ Fed Para, Inst Geociencias, Programa Posgrad Ciencias Ambientais, Rua Augusto Correa 1, BR-66075110 Belem, Para, Brazil; [da Costa, Marlene F.] Gerencia Meio Ambiente Minas Carajas, Dept Ferrosos Norte, Estr Raymundo Mascarenhas,S-N Mina N4, BR-68516000 Parauapebas, Para, Brazil; [Guimaraes Guilherme, Luiz Roberto] Univ Fed Lavras, Dept Ciencia Solo, BR-37200000 Lavras, MG, Brazil; [Salomao, Gabriel Negreiros] Rua Augusto Correa 01, BR-66075110 Belem, Para, Brazil	Universidade Federal do Para; Instituto Tecnologico Vale Desenvolvimento Sustentavel; Central University of Punjab; Universidade Federal do Para; Universidade Federal de Lavras	Salomao, GN (autor correspondente), Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa 1, BR-66075110 Belem, Para, Brazil.; Salomao, GN (autor correspondente), Rua Augusto Correa 01, BR-66075110 Belem, Para, Brazil.	salomao.gn@gmail.com	Guilherme, Luiz Roberto Guimaraes/V-6163-2019; Angelica, Romulo/G-6245-2010; Souza-Filho, Pedro Walfir M. M./J-4958-2012; Guilherme, Luiz Roberto Guimaraes/B-3998-2009; Souza, Pedro/GZH-1275-2022; Sahoo, Prafulla/N-5100-2018	Guilherme, Luiz Roberto Guimaraes/0000-0002-5387-6028; Angelica, Romulo/0000-0002-3026-5523; Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; Guilherme, Luiz Roberto Guimaraes/0000-0002-5387-6028; Sahoo, Prafulla/0000-0003-3481-1787	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [380998/2019-0, 306108/2014-3, 305392/2014-0, 443247/2015-3, 402727/2018-5]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The ItacGMBP project is currently under execution at Instituto Tecnol.ogico Vale Desenvolvimento Sustent.avel (ITVDS) with Vale funding (Ger<<^>>encia de Meio Ambiente Corredor Norte). This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) -Finance Code 001. This work was supported by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [grants 380998/2019-0 to GNS; 306108/2014-3 to RD; 305392/2014-0 to RSA; 443247/2015-3 and 402727/2018-5 projects coordinated by RD]. The authors acknowledge Marcondes Lima da Costa, Jos.e Francisco da Fonseca Ramos e Jos.e Francisco B<<^>>erredo Reis da Silva for their scientific collaboration with the Background project.	Albanese S, 2007, J GEOCHEM EXPLOR, V93, P21, DOI 10.1016/j.gexplo.2006.07.006; Almeida C.A., 2006, J BRAZ SOC ECOTOXICO, V1, P141, DOI [10.5132/jbse.2006.02.010, DOI 10.5132/JBSE.2006.02.010]; Alvarenga C. J. 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Geochem.	JUL	2020	118								104608	10.1016/j.apgeochem.2020.104608	http://dx.doi.org/10.1016/j.apgeochem.2020.104608			18	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	ME8FQ					2023-06-23	WOS:000544889100011
J	Silva, CM; Soares, R; Machado, W; Arbilla, G				Silva, C. M.; Soares, R.; Machado, W.; Arbilla, G.			The COVID-19 Pandemic: Living in the Anthropocene	REVISTA VIRTUAL DE QUIMICA			Portuguese	Article						COVID-19; globalization; urbanization; lockdown; environmental impact	IMPACT	A novel infectious disease was identified in Wuhan, China, in December 2019, and later named as COVID-19. In a few weeks, the epidemic became a pandemic and by the end of March 2020, half of the world was under some form of lockdown. The main goal of this work is to discuss the COVID-19 pandemic as a consequence of the main characteristics of Anthropocene, as well as the evidences of the human impact on the environment after the outbreak of the new coronavirus and the adoption of restrictive measures in many countries around the world. Urbanization, industrialization, globalization, climate change, deforestation and also social inequalities, mainly in middle- and low-income countries, which in general have weaker health systems and limited capacity to handle a rapid rise in cases, are contributing to an emerging global health crisis. Several examples of the environmental impacts are presented. Some examples of the decrease of primary atmospheric pollutants (mainly fine particulate matter and NO2) are discussed as well as other negative impacts, such as the increase in ozone tropospheric concentrations and medical waste. As a global phenomenon in the "Age of Humans", the COVID-19 pandemic requires the urgent and coordinated effort of all countries to overcome the crisis. The pandemic is an opportunity to take advantage of the spirit of cooperation, to embrace the socio-environmental diversity and arrive at a necessary common global agreement to manage the future of Earth collectively.	[Silva, C. M.; Soares, R.; Machado, W.; Arbilla, G.] Univ Fed Rio de Janeiro, Inst Quim, Dept Fisicoquim, BR-21941909 Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio de Janeiro	Arbilla, G (autor correspondente), Univ Fed Rio de Janeiro, Inst Quim, Dept Fisicoquim, BR-21941909 Rio De Janeiro, RJ, Brazil.	gracielaiq@gmail.com	da Silva, Cleyton Martins/AAC-4993-2020; Machado, Wilson/P-8047-2019; Arbilla, Graciela/X-5847-2019	da Silva, Cleyton Martins/0000-0002-5216-4977; Machado, Wilson/0000-0003-3117-8584; Arbilla, Graciela/0000-0001-7732-8336				[Anonymous], 2018, REV VIRTUAL QUIM, V10, P1618, DOI 10.21577/1984-6835.20180110; Areas JD, 2020, REV VIRTUAL QUIM, V12, P775, DOI 10.21577/1984-6835.20200061; ARRUDA Eucidio Pimenta, 2020, EMREDE REV ED DISTAN, V7, P257; Barreto A. C. 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Virtual Quim.	JUL-AUG	2020	12	4					1001	1016		10.21577/1984-6835.20200081	http://dx.doi.org/10.21577/1984-6835.20200081			16	Chemistry, Multidisciplinary	Emerging Sources Citation Index (ESCI)	Chemistry	OM5FF		gold			2023-06-23	WOS:000586049800001
J	Teixeira, CAS; Bello, RMS; Almeida, NS; Pestilho, A; Brochsztain, S; de Queiroz, TB; Andrade, LS; Gregorio, DF; Sawakuchi, AO				Teixeira, C. A. S.; Bello, R. M. S.; Almeida, N. S.; Pestilho, A.; Brochsztain, S.; de Queiroz, T. B.; Andrade, L. S.; Gregorio Junior, D. F.; Sawakuchi, A. O.			Hydrocarbon generation in the Permian Irati organic-rich shales under the influence of the early cretaceous Parana Large Igneous Province	MARINE AND PETROLEUM GEOLOGY			English	Article						Parana basin; Oil shale; Hydrocarbon fluid inclusions; Calcite and quartz veins; Vitrinite reflectance; Kerogen aromaticity; Nuclear magnetic resonance (NMR); Confocal scanning laser microscopy (CSLM)	MISSISSIPPIAN BARNETT SHALE; MOLECULAR GEOCHEMISTRY DATA; FLUID INCLUSION DATA; NORTH-CENTRAL TEXAS; BOHAI BAY BASIN; THERMAL MATURITY; OIL INCLUSIONS; HOMOGENIZATION TEMPERATURE; PETROLEUM CHARACTERISTICS; FLUORESCENCE EVOLUTION	The increasing global demand for natural gas and petroleum byproducts is turning organic-rich shales into an important target for hydrocarbon exploration and production. Current understanding about hydrocarbon generation in unconventional plays, such as oil shales and gas shales, is still evolving, especially in sedimentary basins where hydrocarbon generation is influenced by magmatism. This is the case for the Permian oil shales of the Irati Formation in the Parana Basin, southern South America. The Irati shales are considered an atypical petroleum system due to thermal effects of the Parana Large Igneous Province (LIP) emplaced during the Early Cretaceous. In this context, the focus of this study was to characterize the thermal conditions of hydrocarbon generation in the Irati Formation as well as the composition of related aqueous diagenetic fluids. The kerogen from the Irati organic-rich shales has an aromaticity around 30% (f(ar) approximate to 30%), as determined by carbon nuclear magnetic resonance (C-13-NMR), and vitrinite reflectance (R-o) of around 0.6%. Fluid inclusions in calcite and quartz veins present aqueous fluids with salinity of 0-5 wt% of NaCl equivalent and homogenization temperatures greater than 250 degrees C. Hydrocarbon fluid inclusions were classified as black oil through their vapor fraction volumes (F-v = 1.6-9.1%) and homogenization temperatures (Th) in the 60-80 degrees C range. Methane (CH4) or carbon dioxide (CO2) fluid inclusions were absent within the analyzed calcite and quartz veins. The PVT model for trapped fluid inclusions suggests a shallow hydrocarbon petroleum system (approximate to 2.5 km depth) active during the Early Cretaceous, synchronous with the Parana LIP.	[Teixeira, C. A. S.; Bello, R. M. S.; Almeida, N. S.; Sawakuchi, A. O.] Univ Sao Paulo, Inst Geosci, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Pestilho, A.] Petrobras R&D Ctr CENPES, Av Horacio Macedo 950,Cidade Univ, Rio De Janeiro, RJ, Brazil; [Brochsztain, S.] Fed Univ ABC, Ctr Engn Modelagem & Ciencias Sociais Aplicadas, Av Estados 5001, BR-09210580 Santo Andre, SP, Brazil; [de Queiroz, T. B.; Andrade, L. S.; Gregorio Junior, D. F.] Fed Univ ABC, Ctr Ciencias Nat & Humanas, Av Estados 5001, BR-09210580 Santo Andre, SP, Brazil	Universidade de Sao Paulo; Petrobras	Teixeira, CAS (autor correspondente), Univ Sao Paulo, Inst Geosci, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil.	carloscience13@gmail.com	dos Santos Andrade, Luana/P-9376-2019; Brochsztain, Sergio/G-4660-2012; Sawakuchi, André O/D-1445-2013; Andrade, Luana/B-6196-2019; Pestilho, André L S/M-5785-2018; Andrade, Luana dos Santos/AAM-7602-2020; Branquinho de Queiroz, Thiago/C-5066-2016	Brochsztain, Sergio/0000-0002-1129-8039; Pestilho, André L S/0000-0002-5497-4236; Andrade, Luana dos Santos/0000-0001-6825-8145; Sawakuchi, Andre/0000-0001-5016-2428; Branquinho de Queiroz, Thiago/0000-0003-3775-954X	Human Resources Training Program in Petroleum and Environmental Geology of Petroleo Brasileiro S.A. [PFRH-147, PFRH-241]; National Council for Scientific and Technological Development (CNPq) [304727/2017-2]	Human Resources Training Program in Petroleum and Environmental Geology of Petroleo Brasileiro S.A.; National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This project was funded by the Human Resources Training Program in Petroleum and Environmental Geology (PFRH-147 and 241) of Petroleo Brasileiro S.A. and National Council for Scientific and Technological Development (CNPq) (grant 304727/2017-2). The authors are grateful to the Multiuser Central Facilities of Federal University of ABC (Brazil) for NMR analyzes and to the Departamento de Geociencias, Ambiente e Ordenamento do Territorio da Universidade do Porto (Portugal) for the use of facilities for vitrinite reflectance analysis. Also, thanks to Msc. Carlos Mazoca for technical support and PhD. Ana Carolina Almeida for the manuscript review.	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Pet. Geol.	JUL	2020	117								104410	10.1016/j.marpetgeo.2020.104410	http://dx.doi.org/10.1016/j.marpetgeo.2020.104410			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LU2FJ					2023-06-23	WOS:000537575300045
J	Tome, CR; Bitencourt, MD; Raposo, MIB; Savian, JF				Tome, Camila Rocha; Bitencourt, Maria de Fatima; Bartolomeu Raposo, Maria Irene; Savian, Jairo Francisco			Magnetic fabric data on interactive syntectonic magmas of contrasting composition in composite dikes from south Brazil	JOURNAL OF GEODYNAMICS			English	Article						Anisotropy of magnetic susceptibility; Composite dikes; Rock magnetism; Magnetic fabric	PARTIAL ANHYSTERETIC REMANENCE; FLOW DIRECTIONS; GRANITE PLUTON; DYKE SWARM; SHEAR ZONE; GRAIN-SIZE; SUSCEPTIBILITY; ANISOTROPY; EMPLACEMENT; GEOCHRONOLOGY	The composite dikes of the Zimbros Bay in the Porto Belo-Bombinhas region, southern Brazil, are emplaced in the late stages of post-collisional magmatism, at ca. 590 Ma as NE-striking, subvertical tabular bodies intrusive in basement orthogneisses. The composite dikes are formed by a felsic core containing a swarm of mafic microgranular enclaves, bordered on both sides by mafic material of irregular thickness, and individual mafic dikes parallel to the main intrusion. The felsic and mafic rocks contain a well-developed magmatic foliation with solidstate deformation near the contacts. Stretching lineation is horizontal to sub-horizontal and better developed in the felsic rocks. The absence of a well-developed linear fabric in the mafic rocks hinders investigation of their emplacement based on conventional structural data. In order to investigate/explore the relationship between contemporaneous mafic and felsic rocks, as well as to understand the emplacement of these intrusions in relation to the transcurrent tectonics, a study on the magnetic fabric was made using anisotropy of magnetic susceptibility (AMS) and rock magnetism techniques for composite and individual mafic dikes. Magnetic mineralogy of both dikes is predominantly controlled by ferromagnetic minerals (e.g. magnetite and Ti-poor tinanomagnetite), with little contribution of paramagnetic minerals. The rock magnetism study shows that the magnetite grains have varied sizes. Individual mafic dikes have small grain sizes, whilst in the mafic borders, sizes vary from small to large. Felsic cores have large grain sizes. SEM data show oxyexsolution textures in the felsic core samples and in samples of individual mafic dikes. Only Ilmenite is found in the mafic border samples, either as anhedral grains or as thin lamellae, interpreted to result from intense oxyexsolution of magnetite. Increasing oxyexsolution degrees observed in samples from individual mafic dikes to felsic cores and mafic borders suggest different degrees of interaction between the original magmas. The studied intrusions show normal magnetic fabrics, with subvertical magnetic foliation (k(1)-k(2) plane) and subhorizontal (k(1)) lineation. Magnetic data are concordant with structural field measurements and indicate sub-horizontal magma flow during emplacement. The much larger volume and size of enclaves found in the southern portion of the dike is compatible with its northward directed emplacement. The obtained magnetic data are also in agreement with the syntectonic emplacement of the composite dikes relative to the transcurrent movement of the Major Gercino Shear Zone.	[Tome, Camila Rocha; Bitencourt, Maria de Fatima; Savian, Jairo Francisco] Univ Fed Rio Grande UFRGS, Programa Posgrad Geociencias PPGGEO, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Bartolomeu Raposo, Maria Irene] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, Brazil	Universidade de Sao Paulo	Tome, CR (autor correspondente), Univ Fed Rio Grande UFRGS, Programa Posgrad Geociencias PPGGEO, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	camilarocha.tome@gmail.com; fatimab@ufrgs.br; irene@usp.br; jairo.savian@ufrgs.br	Raposo, M. Irene B./D-6896-2013; de Fátima Bitencourt, Maria/H-8957-2016; Bitencourt, Maria de Fátima/GLR-8862-2022	de Fátima Bitencourt, Maria/0000-0001-7022-9175; Bitencourt, Maria de Fátima/0000-0001-7022-9175	Brazilian National Research Council (CNPq) [471266/2010-8]; Rio Grande do Sul State Research Foundation (FAPERGS) [10/0045-6]	Brazilian National Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Rio Grande do Sul State Research Foundation (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS))	This research received financial support from the Brazilian National Research Council (CNPq, Universal Program 471266/2010-8), and Rio Grande do Sul State Research Foundation (FAPERGS, 10/0045-6) granted to M.F. Bitencourt. The paper is part of Camila Rocha Tome's MSc thesis. We are grateful to Luis Alva-Valdivia and an anonymous reviewer for their careful reviews and suggestions that helped to significantly improve the manuscript.	[Anonymous], [No title captured]; Archanjo CJ, 2002, J GEOPHYS RES-SOL EA, V107, DOI 10.1029/2001JB000268; ARCHANJO CJ, 1994, J STRUCT GEOL, V16, P323, DOI 10.1016/0191-8141(94)90038-8; Archanjo CJ, 1999, TECTONOPHYSICS, V312, P331, DOI 10.1016/S0040-1951(99)00176-6; Bitencourt M.F., 1995, S NACL ESTUDOS TECTO, P178; Bitencourt M. 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Geodyn.	JUL	2020	138								101754	10.1016/j.jog.2020.101754	http://dx.doi.org/10.1016/j.jog.2020.101754			16	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	LZ3LF					2023-06-23	WOS:000541129000004
J	Cardoso, LG; Duarte, JH; Costa, JAV; Assis, DD; Lemos, PVF; Druzian, JI; de Souza, CO; Nunes, IL; Chinalia, FA				Cardoso, Lucas Guimaraes; Duarte, Jessica Hartwig; Vieira Costa, Jorge Alberto; Assis, Denilson de Jesus; Franca Lemos, Paulo Vitor; Druzian, Janice Izabel; de Souza, Carolina Oliveira; Nunes, Itaciara Larroza; Chinalia, Fabio Alexandre			Spirulinasp. as a Bioremediation Agent for Aquaculture Wastewater: Production of High Added Value Compounds and Estimation of Theoretical Biodiesel	BIOENERGY RESEARCH			English	Article						Biofuel; Biomass composition; Microalgae; Nutrient removal; Wastewater treatment	HYDROTHERMAL LIQUEFACTION; OIL PRODUCTION; CHLORELLA SP; MICROALGAE; CULTIVATION; BIOMASS; PLATENSIS; GROWTH; SEQUESTRATION; EXTRACTION	The rapid development of large-scale aquaculture leads to wastewater accumulation, increasing environmental problems. Microalga cultivation is a potential biotechnological alternative to treat aquaculture wastewater. While this microorganism consumes the wastewater nutrients, high added value biomass is produced. The role ofSpirulinain aquaculture wastewater treatment is not fully elucidated in the literature. Thus, this study aimed to reuse and treat aquaculture wastewater bySpirulinasp. LEB 18 cultures. The microalga growth parameters, the biochemical composition of the biomass produced, and theSpirulinaefficiency to nutrient removal from the aquaculture wastewater were evaluated. The assays were performed in closed photobioreactors (1 L) using 100% aquaculture wastewater (T-0) supplemented with 25 (T-25), 50 (T-50), and 75% (T-75) of the Zarrouk synthetic culture medium. The maximum biomass concentrations showed no statistical difference between the assays T-50 (1.02 g L-1), T-25 (1.10 g L-1), and control (1.05 g L-1). The biomass from the T-25 assay showed the highest concentrations of protein (65.73%), phycocyanin (16.60 mg/mL), polyunsaturated fatty acid (38.20%), and gamma-linolenico (23.29%). Besides that, theSpirulinasp. LEB 18 highest removal rate of sulfate (94.01%), phosphate (93.84%), bromine (96.77%), and COD (90.00%) was obtained from the T-25 assay. The biomass from T-25 and T-50 assays showed ideal properties for biodiesel application. TheSpirulinasp. LEB 18 cultures using 100% aquaculture wastewater supplemented with 25% of Zarrouk culture medium was the best option for the aquaculture wastewater treatment, producing added value biomass and reducing production cost.	[Cardoso, Lucas Guimaraes; Franca Lemos, Paulo Vitor; Chinalia, Fabio Alexandre] Univ Fed Bahia, Inst Hlth Sci, Dept Biotechnol, Salvador, BA, Brazil; [Duarte, Jessica Hartwig; Vieira Costa, Jorge Alberto] Fed Univ Rio Grande, Coll Chem & Food Engn, Lab Biochem Engn, Rio Grande, Brazil; [Assis, Denilson de Jesus] Univ Salvador, Sch Architecture Engn & Informat Technol, Salvador, BA, Brazil; [Druzian, Janice Izabel; de Souza, Carolina Oliveira] Univ Fed Bahia, Fac Pharm, Grad Program Food Sci, Salvador, BA, Brazil; [Nunes, Itaciara Larroza] Univ Fed Santa Catarina, Dept Food Sci & Technol, Grad Program Food Sci, Florianopolis, SC, Brazil	Universidade Federal da Bahia; Universidade Federal do Rio Grande; Universidad de El Salvador; Universidade Salvador (UNIFACS); Universidade Federal da Bahia; Universidade Federal de Santa Catarina (UFSC)	Cardoso, LG (autor correspondente), Univ Fed Bahia, Inst Hlth Sci, Dept Biotechnol, Salvador, BA, Brazil.	cardoso.lucas@ufba.br	Souza, Carolina O/G-8869-2015; Costa, Jorge A V/L-3999-2013; Lemos, Paulo Vitor França/AAQ-7853-2021; Cardoso, Lucas/AAS-2431-2020; Nunes, Itaciara/AAM-1072-2021; Nunes, Itaciara Larroza/F-7922-2017; Druzian, Janice Izabel/G-6884-2015; de Jesus Assis, Denilson/E-1586-2014	Costa, Jorge A V/0000-0001-8042-7642; Lemos, Paulo Vitor França/0000-0002-7138-4297; Cardoso, Lucas/0000-0002-6674-338X; de Jesus Assis, Denilson/0000-0002-9226-4155; Oliveira de Souza, Carolina/0000-0002-8028-5418; Nunes, Itaciara/0000-0003-1098-7139	FAPESB Foundation [400710/2014-5]; MCTIC (Ministry of Technological Information and Communication Science)-Brazil and Bahia Pesca	FAPESB Foundation; MCTIC (Ministry of Technological Information and Communication Science)-Brazil and Bahia Pesca	This study was supported by the FAPESB Foundation for Research Support of Bahia to project CNPQ (400710/2014-5) and by the MCTIC (Ministry of Technological Information and Communication Science)-Brazil and Bahia Pesca.	Andrade BB, 2019, BIORESOURCE TECHNOL, V284, P340, DOI 10.1016/j.biortech.2019.03.144; [Anonymous], 2008, NAT GAS BIOF; [Anonymous], 2003, 14104 UNE; [Anonymous], 2005, STANDARD METHODS EXA; Ansari FA, 2017, ALGAL RES, V21, P169, DOI 10.1016/j.algal.2016.11.015; Arias-Penaranda MT, 2013, BIORESOURCE TECHNOL, V140, P158, DOI 10.1016/j.biortech.2013.04.080; Barros MP, 2012, CHEM-BIOL INTERACT, V197, P58, DOI 10.1016/j.cbi.2012.03.005; Costa JAV, 2002, WORLD J MICROB BIOT, V18, P603, DOI 10.1023/A:1016822717583; Daneshvar E, 2018, BIORESOURCE TECHNOL, V255, P104, DOI 10.1016/j.biortech.2018.01.101; de Jesus CS, 2018, BIORESOURCE TECHNOL, V256, P86, DOI 10.1016/j.biortech.2018.01.149; Deshmukh S, 2019, FUEL PROCESS TECHNOL, V191, P232, DOI 10.1016/j.fuproc.2019.03.013; Duarte JH, 2020, APPL BIOCHEM BIOTECH, V190, P907, DOI 10.1007/s12010-019-03126-7; DUBOIS M, 1956, ANAL CHEM, V28, P350, DOI 10.1021/ac60111a017; Egloff S, 2018, ALGAL RES, V34, P68, DOI 10.1016/j.algal.2018.07.004; FAO, 2018, STAT WORLD FISH AQ, P223; Ferreira JG, 2015, AQUACULTURE, V447, P23, DOI 10.1016/j.aquaculture.2014.08.042; Francisco EC, 2010, J CHEM TECHNOL BIOT, V85, P395, DOI 10.1002/jctb.2338; Guiheneuf F, 2013, MAR DRUGS, V11, P4246, DOI 10.3390/md11114246; Huang YQ, 2016, FUEL, V183, P9, DOI 10.1016/j.fuel.2016.06.013; Jawaharraj K, 2016, RENEW ENERG, V98, P72, DOI 10.1016/j.renene.2016.02.038; Knothe G, 2005, FUEL PROCESS TECHNOL, V86, P1059, DOI 10.1016/j.fuproc.2004.11.002; Knothe G, 2007, FUEL PROCESS TECHNOL, V88, P669, DOI 10.1016/j.fuproc.2007.01.005; Krishnamoorthy S, 2019, J ENVIRON MANAGE, V234, P412, DOI 10.1016/j.jenvman.2019.01.014; Kuo CM, 2015, BIORESOURCE TECHNOL, V194, P326, DOI 10.1016/j.biortech.2015.07.026; Li X, 2010, BIORESOURCE TECHNOL, V101, P5494, DOI 10.1016/j.biortech.2010.02.016; LOWRY OH, 1951, J BIOL CHEM, V193, P265; Lu WD, 2019, BIORESOURCE TECHNOL, V271, P59, DOI 10.1016/j.biortech.2018.09.082; Malibari R, 2018, J CLEAN PROD, V198, P160, DOI 10.1016/j.jclepro.2018.07.037; Markou G, 2012, BIORESOURCE TECHNOL, V112, P234, DOI 10.1016/j.biortech.2012.02.098; Martins AP, 2018, ALGAL RES, V33, P316, DOI 10.1016/j.algal.2018.05.008; Mata SN, 2020, BIORESOURCE TECHNOL, V311, DOI 10.1016/j.biortech.2020.123495; Milhazes-Cunha H, 2017, ALGAL RES, V24, P416, DOI 10.1016/j.algal.2016.12.011; Mohammadi M, 2019, J ENVIRON CHEM ENG, V7, DOI 10.1016/j.jece.2018.102870; Nam K, 2017, J APPL PHYCOL, V29, P1171, DOI 10.1007/s10811-016-0987-0; Nascimento IA, 2014, BIOENERG RES, V7, P1002, DOI 10.1007/s12155-014-9440-x; Perez-Garcia O, 2011, WATER RES, V45, P11, DOI 10.1016/j.watres.2010.08.037; Ramsundar P, 2017, ALGAL RES, V28, P108, DOI 10.1016/j.algal.2017.10.006; de Alva MS, 2018, ALGAL RES, V34, P97, DOI 10.1016/j.algal.2018.07.006; Salama E, 2017, J CLEAN PROD, V168, P1017, DOI 10.1016/j.jclepro.2017.09.057; Samuel-Fitwi B, 2012, J CLEAN PROD, V32, P183, DOI 10.1016/j.jclepro.2012.03.037; Soares SAR, 2015, J BRAZIL CHEM SOC, V26, P955, DOI 10.5935/0103-5053.20150057; Sumprasit N, 2017, INT BIODETER BIODEGR, V119, P196, DOI 10.1016/j.ibiod.2016.11.006; Tripathi R, 2015, RENEW ENERG, V74, P774, DOI 10.1016/j.renene.2014.09.005; Vardon DR, 2011, BIORESOURCE TECHNOL, V102, P8295, DOI 10.1016/j.biortech.2011.06.041; Wuang SC, 2016, ALGAL RES, V15, P59, DOI 10.1016/j.algal.2016.02.009; Yang FF, 2016, J APPL PHYCOL, V28, P747, DOI 10.1007/s10811-015-0576-7; Zeng XH, 2012, CHEM ENG J, V183, P192, DOI 10.1016/j.cej.2011.12.062; Zhang LJ, 2019, BIORESOURCE TECHNOL, V278, P205, DOI 10.1016/j.biortech.2019.01.066; Zhang LJ, 2018, RENEW ENERG, V115, P276, DOI 10.1016/j.renene.2017.08.034	49	27	28	2	25	SPRINGER	NEW YORK	ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES	1939-1234	1939-1242		BIOENERG RES	BioEnergy Res.	MAR	2021	14	1					254	264		10.1007/s12155-020-10153-4	http://dx.doi.org/10.1007/s12155-020-10153-4		JUN 2020	11	Energy & Fuels; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Environmental Sciences & Ecology	QJ1GY					2023-06-23	WOS:000544205000001
J	Kalkreuth, W; Levandowski, J; Weniger, P; Krooss, B; Prissang, R; da Rosa, AL				Kalkreuth, W.; Levandowski, J.; Weniger, P.; Krooss, B.; Prissang, R.; da Rosa, A. Lima			Coal characterization and coalbed methane potential of the Chico-Loma Coalfield, Parana Basin, Brazil - Results from exploration borehole CBM001-CL-RS	ENERGY EXPLORATION & EXPLOITATION			English	Article						Brazil; Parana Basin; Chico-Loma Coalfield; Coal Characteristics; CBM	SANTA-TEREZINHA; SORPTION; CO2; ADSORPTION; GEOCHEMISTRY; TEMPERATURE; INTRUSIONS; CAPACITIES; DESORPTION; OUTBURSTS	The aim of this study was to determine the coal characteristics in the Chico-Loma coalfield, Brazil and to evaluate the potential of natural gas associated with the coal seams (CBM), by carrying out a test well (CBM001-CL-RS) for collecting coal samples, followed by gas desorption measurements, and petrographical and chemical analyses of the coals and their methane adsorption capacities. The gas collected was analyzed for gas composition, stable carbon and hydrogen isotopes. The results indicate a cumulative coal thickness of 11.46 m in well CBM001-CL-RS, associated with an igneous intrusion of 10 m thickness. In the contact zone with the intrusion, the organic matter is severely altered with partial transformation of the coal to natural coke at distances less than 2 m from the intrusion. The ash content, based on proximate analysis, shows a variation from 29.1 to 82.8 wt.%. The sulphur content ranges from 0.43 to 3.89 wt.% and shows higher values in samples from the top of the Rio Bonito Formation. The gas desorption measurements range from 0.05 to 0.74 cm(3)/g, with methane being the predominant gas (>90%). A thermal origin of the gas is suggested by C and H isotopes and the C1 (methane) to C3 (propane) hydrocarbon distribution. The methane adsorption capacity of the samples varies from 2.50 to 6.50 cm(3)/g. Changes in microporosity related to thermal alteration may have a significant impact on the gas-holding capacity of samples located near the contact to the intrusion. For the study area, a 3D geological model was generated to estimate the volume of coal in the coalfield, followed by assessment of the gas volume associated with the coal. Based on the 3D model, a preliminary appraisal indicates resources of 7.2 billion tons of coal for the Chico-Loma coalfield, associated with 2.7 billion m(3)of gas.	[Kalkreuth, W.; Levandowski, J.; da Rosa, A. Lima] Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil; [Weniger, P.] Fed Inst Geosci & Nat Resources BGR, Hannover, Germany; [Krooss, B.] Rhein Westfal TH Aachen, Inst Geol & Geochem Petr & Coal, Aachen, Germany; [Prissang, R.] FU Berlin, Inst Geol Wissensch, Berlin, Germany	Universidade Federal do Rio Grande do Sul; RWTH Aachen University; Free University of Berlin	Kalkreuth, W (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil.	wolfgang.kalkreuth@ufrgs.br		Prissang, Rene/0000-0002-2246-4477	FAPERGS/CNPq Project [10/0028-9]; CNPq	FAPERGS/CNPq Project; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: The study received support from FAPERGS/CNPq Project 10/0028-9, Financial Support for Centers of Excellence in Research. J. Levandowski thanks CNPq for providing financial support in form of a Ph.D. grant. W. Kalkreuth received from CNPq a research grant related to his scientific production.	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Exploit.	SEP	2020	38	5					1589	1630	0144598720931167	10.1177/0144598720931167	http://dx.doi.org/10.1177/0144598720931167		JUN 2020	42	Energy & Fuels	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels	NZ0SA					2023-06-23	WOS:000545566700001
J	Lemos, VA; Souza, LV; Santos, LB; Barreto, JA; Ferreira, SLC				Lemos, Valfredo Azevedo; Souza Junior, Lvanilson Vieira; Santos, Luana Bastos; Barreto, Jeferson Alves; Costa Ferreira, Sergio Luis			A New Simple and Fast Method for Determination of Cobalt in Vitamin B12 and Water Samples Using Dispersive Liquid-Liquid Microextraction and Digital Image Analysis	WATER AIR AND SOIL POLLUTION			English	Article						Digital image; Cobalt; DLLME; Water; Vitamin B12	SOLID-PHASE EXTRACTION; FOOD SAMPLES; PRECONCENTRATION; COLORIMETRY; SOLVENT; PHOSPHORUS; SEPARATION; SORPTION; NICKEL	In this work, a simple and fast method for the determination of cobalt in vitamin B12 and water samples was developed. The procedure is based on the preconcentration of the element using dispersive liquid-liquid microextraction (DLLME) and subsequent detection by digital image colorimetry. DLLME was performed with trichloroethylene (extraction solvent) and ethanol (dispersive solvent). The element was extracted in the form of its complex with 2-(2-thiazolylazo)-p-cresol (TAC). The optimal working conditions were obtained through univariate optimization. The variables studied were pH, the volume of extraction solvent, and the volume of dispersive solvent. Under optimal conditions, the method presented a limit of detection of 0.9 mu g L(-1)and precision (relative standard deviation) of 4.0%, for 25.0 mu g L(-1)cobalt solutions. The procedure was applied to the determination of cobalt in vitamin B12 and water samples. The method presents a simple, fast, and low-cost procedure, presenting itself as an excellent alternative to the determination of cobalt in the samples analyzed.	[Lemos, Valfredo Azevedo; Souza Junior, Lvanilson Vieira; Santos, Luana Bastos; Barreto, Jeferson Alves] Univ Estadual Sudoeste Bahia, Lab Quim Analit, Campus Jequie, BR-45208091 Jequie, BA, Brazil; [Lemos, Valfredo Azevedo; Santos, Luana Bastos; Costa Ferreira, Sergio Luis] Univ Fed Bahia, Programa Posgrad Quim, Campus Univ Ondina, BR-40170280 Salvador, BA, Brazil; [Barreto, Jeferson Alves] Univ Fed Fluminense, Dept Quim Analit, Outeiro de Sao Joao Batista S-N, BR-24020141 Niteroi, RJ, Brazil	Universidade Estadual do Sudoeste da Bahia; Universidade Federal da Bahia; Universidade Federal Fluminense	Lemos, VA (autor correspondente), Univ Fed Bahia, Programa Posgrad Quim, Campus Univ Ondina, BR-40170280 Salvador, BA, Brazil.	vlemos@uesb.edu.br	Santos, Luana Bastos/ABI-4967-2020; FERREIRA, SERGIO LUIS SLCF COSTA/I-1993-2013; LEMOS, VALFREDO AZEVEDO/I-7647-2014; Barreto, Jeferson Alves/AAV-4175-2020	Santos, Luana Bastos/0000-0002-5063-201X; FERREIRA, SERGIO LUIS SLCF COSTA/0000-0001-7738-045X; LEMOS, VALFREDO AZEVEDO/0000-0002-6029-3218; Barreto, Jeferson Alves/0000-0002-7595-3207	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [311419/2018-6]; Fundacao de Amparo a Pesquisa do Estado da Bahia	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado da Bahia	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) -Finance Code 001. The authors also received financial support from the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (311419/2018-6) and the Fundacao de Amparo a Pesquisa do Estado da Bahia.	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JUN 27	2020	231	7							334	10.1007/s11270-020-04680-1	http://dx.doi.org/10.1007/s11270-020-04680-1			8	Environmental Sciences; Meteorology & Atmospheric Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences; Water Resources	MG4CD					2023-06-23	WOS:000545979400001
J	Queiroz, HM; Ferreira, TO; Taniguchi, CAK; Barcellos, D; do Nascimento, JC; Nobrega, GN; Otero, XL; Artur, AG				Queiroz, Hermano Melo; Ferreira, Tiago Osorio; Kenji Taniguchi, Carlos Alberto; Barcellos, Diego; do Nascimento, Juliana Costa; Nobrega, Gabriel Nuto; Otero, Xose Luis; Artur, Adriana Guirado			Nitrogen mineralization and eutrophication risks in mangroves receiving shrimp farming effluents	ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH			English	Article						Inorganic nitrogen; Mangrove soils; Soil pollution	GREENHOUSE-GAS EMISSIONS; ORGANIC-MATTER; NUTRIENT ENRICHMENT; AVICENNIA-MARINA; SOIL CARBON; PHOSPHORUS; SEDIMENTS; WATER; INCREASE; GROWTH	Nitrogen (N) inputs originated from shrimp farming effluents were evaluated for potential changes in the net N mineralization for mangrove soils from Northeastern Brazil. Our study provides notable information and assessment for the potential enhancement of N mineralization in preserved and shrimp-impacted semi-arid mangrove soils of the Jaguaribe River estuary, which is one of the largest shrimp producers of Brazil, using an analytical and daily tidal variation experimental approach. Nitrogen-rich effluents promoted a significant (pvalue < 0.001) increase of the total soil N content (1998 +/- 201 mg kg(-1)on average) compared with the preserved sites (average: 1446 +/- 295 mg kg(-1)). The effluents also increased the N mineralization in the shrimp-impacted sites (N-min: 86.6 +/- 37.5 mg kg(-1)), when compared with preserved mangroves (N-min: 56.5 +/- 23.8 mg kg(-1)). Over a daily tidal variation experiment, we found that just 30% (36.2 +/- 20.6 mg kg(-1)) of mineralized N remains stored in the soil, whereas 70% (102.9 +/- 38.8 mg kg(-1)) was solubilized in tidal waters. Therefore, the N mineralization process may trigger eutrophication by increasing N inorganic bioavailability in mangrove soils receiving N-rich effluents from shrimp ponds, which in turn might increase primary producers' activity. This approach has not been studied so far in semi-arid mangroves, where the shrimp farming activity is one of the most important economic activities.	[Queiroz, Hermano Melo; Ferreira, Tiago Osorio; Barcellos, Diego; do Nascimento, Juliana Costa] Univ Sao Paulo ESALQ USP, Luiz de Queiroz Coll Agr, Av Padua Dias 11, BR-13418900 Piracicaba, SP, Brazil; [Queiroz, Hermano Melo; Artur, Adriana Guirado] Univ Fed Ceara, Dept Ciancias Solo, UFC, Av Mister Hull 2977,Campus Pici, BR-60440554 Fortaleza, Ceara, Brazil; [Kenji Taniguchi, Carlos Alberto] Embrapa Agoind Trop, Rua Dra Sara Mesquita St 2270, BR-60511110 Fortaleza, Ceara, Brazil; [Nobrega, Gabriel Nuto] Univ Fed Fluminense, Dept Geoquim, Progama Posgrad Geociancias Geoquim, Rua Outeiro Sao Joao Baptista S-N, BR-24020141 Niteroi, RJ, Brazil; [Otero, Xose Luis] Univ Santiago de Compostela, Fac Biol, Dept Edafoloxie & Quim Agr, Santiago, Spain	Universidade Federal do Ceara; Universidade Federal Fluminense; Universidade de Santiago de Compostela	Queiroz, HM (autor correspondente), Univ Sao Paulo ESALQ USP, Luiz de Queiroz Coll Agr, Av Padua Dias 11, BR-13418900 Piracicaba, SP, Brazil.; Queiroz, HM (autor correspondente), Univ Fed Ceara, Dept Ciancias Solo, UFC, Av Mister Hull 2977,Campus Pici, BR-60440554 Fortaleza, Ceara, Brazil.	hermanomelo@usp.br	Nóbrega, Gabriel Nuto/AAQ-4189-2020; Barcellos, Diego/AAI-5073-2020; Ferreira, Tiago Osório/D-3340-2015; Queiroz, Hermano Melo/P-8700-2019; Costa, Juliana/AAS-1925-2021	Nóbrega, Gabriel Nuto/0000-0001-7008-4201; Barcellos, Diego/0000-0002-4198-2843; Ferreira, Tiago Osório/0000-0002-4088-7457; Queiroz, Hermano Melo/0000-0003-4768-1248; Costa, Juliana/0000-0003-2375-5011	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [446457/2014-0, 305996/2018-5, 409593/2018-4]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES) [001]; Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) [15/2013]; Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro [E-26/202.757/2019]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo-FAPESP [2018/04259-2, 2019/02855-0]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo-FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The authors thank the financial research support from Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, grant no. 446457/2014-0; 305996/2018-5; 409593/2018-4), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES)-Finance Code 001, Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP, public notice 15/2013), Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (GNN, JCNE Grant E-26/202.757/2019), and Fundacao de Amparo a Pesquisa do Estado de Sao Paulo-FAPESP (grants no. 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OCT	2020	27	28			SI		34941	34950		10.1007/s11356-020-09720-1	http://dx.doi.org/10.1007/s11356-020-09720-1		JUN 2020	10	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	NH9ZY	32583107				2023-06-23	WOS:000543047600003
J	Sousa, LC; Rodrigues, CCS; Mendes, RA; Correa, JAM				Sousa, L. C.; Rodrigues, C. C. S.; Mendes, R. A.; Correa, J. A. M.			PAH Profiles in Suspended Particulate Matter from an Urbanized River Within the Brazilian Amazon	BULLETIN OF ENVIRONMENTAL CONTAMINATION AND TOXICOLOGY			English	Article						Polycyclic aromatic hydrocarbons; Organic pollutants; Suspended particulate matter; Amazon river; Gas chromatography	POLYCYCLIC AROMATIC-HYDROCARBONS; GUAJARA BAY; GUAMA RIVER; SEDIMENTS; CONTAMINATION; MARINE; PARTICLES; RATIOS; BELEM; BASIN	The distribution, seasonal variation and sources of 16 polycyclic aromatic hydrocarbons (PAH) from suspended particulate matter (SPM) of the Aura River, a small amazon typical river located in Northern Brazil, were determined. Gas chromatography-mass spectrometry analysis of SPM revealed a mixture of PAH from different origins and a seasonal variation of PAH primary source for the studied area. Pyrene was the dominant PAH in both studied periods. Total PAH content (sigma PAH) ranged from lower than quantification limit (< LOQ) to 2498.2 ng g(-1)dw during the dry season and < LOQ to 2865.8 ng g(-1)dw during the wet season. Low molecular weight PAH (LMW) represented 51% of sigma PAH during the dry season and 29% during the wet season. It was noted, by comparing previous data, that the main source of these compounds was altered after the deactivation of an irregular landfill next to the river.	[Sousa, L. C.; Rodrigues, C. C. S.; Correa, J. A. M.] Fed Univ Para, Geosci Inst, Belem, Para, Brazil; [Mendes, R. A.] Evandro Chagas Inst, Belem, Para, Brazil	Universidade Federal do Para; Instituto Evandro Chagas	Sousa, LC (autor correspondente), Fed Univ Para, Geosci Inst, Belem, Para, Brazil.	laricsouza@gmail.com; santos.camilac@gmail.com; rosivaldomendes@iec.gov.br; jamc@ufpa.br	Correa, José Augusto/HGC-3705-2022	Souza, Larissa/0000-0003-0973-3748	National Council for Scientific and Technological Development (CNPq) [130797/2017-1]	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the National Council for Scientific and Technological Development (CNPq) (130797/2017-1).	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Environ. Contam. Toxicol.	JUL	2020	105	1					86	94		10.1007/s00128-020-02912-y	http://dx.doi.org/10.1007/s00128-020-02912-y		JUN 2020	9	Environmental Sciences; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Toxicology	MJ7VP	32577782				2023-06-23	WOS:000542520000001
J	Pereira, WD; Kelecom, A; Lopes, JM; do Carmo, AS; Py, DD; da Silva, AX				de Souza Pereira, Wagner; Kelecom, Alphonse; Lopes, Jose Marques; do Carmo, Alessander Sa; de Azevedo Py Junior, Delcy; da Silva, Ademir Xavier			Evaluation of the radiological quality of water released by a uranium mining in Brazil	ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH			English	Article						Uranium mining; Effluent; Environmental radioprotection; Acid mine drainage	ENVIRONMENTAL-IMPACT; CALDAS; POCOS; TRANSPORT; SENSORS; SAMPLES; RA-226; MINE; SITE	A mine in an area of naturally occurring radioactive materials (NORM), characterized by acid mine drainage, generates effluents with natural radionuclide concentrations, usually above the limits authorized by the regulator. The plant exploiting NORM controls the water quality and discharges it into the aquatic environment after meeting technical requirements. Downstream, water usage is unrestricted. In order to reach activity concentrations in the released effluents below the authorized values, the facility applies a chemical treatment to the effluent. Then, to ensure the effectiveness of the treatment, the facility performs sampling of treated effluent and determines the activity concentration of natural radionuclides (U-nat,Ra-226, and(210)Pb from the uranium series and(232)Th and(228)Ra from the thorium series). In the current study, the proportion and distribution of these radionuclides between the soluble and particulate fractions were determined. The measured activity concentrations were compared with the values proposed by the World Health Organization and Brazilian legislation, as well as other authorities, as regards the potable use from the radioprotection point of view. It was observed that the radionuclides are not in secular equilibrium. The fractions contribute differently to the total release of radionuclide, and there is no linear relationship between the fractions. The average activity concentrations did not result in radiological restrictions to water use, and the committed effective dose due to ingestion was estimated at 0.06 mSv y(-1). Therefore, there is no radiological restriction to water use, since the dose which was found was below the constraint value for the public.	[de Souza Pereira, Wagner; de Azevedo Py Junior, Delcy] Ind Nucl Brasil INB, Rodovia Presidente Dutra Km 330,Engn Passos, BR-27555000 Resende, RJ, Brazil; [de Souza Pereira, Wagner; do Carmo, Alessander Sa; da Silva, Ademir Xavier] Univ Fed Rio de Janeiro UFRJ, BR-21941972 Rio De Janeiro, Brazil; [Kelecom, Alphonse] Univ Fed Fluminense UFF, Inst Biol, BR-24001970 Niteroi, RJ, Brazil; [Lopes, Jose Marques] Univ Fed Bahia UFBA, Inst Fis, BR-40170290 Salvador, BA, Brazil; [Lopes, Jose Marques] Univ Fed Bahia UFBA, Programa Posgrad Geoquim, BR-40170290 Salvador, BA, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal Fluminense	Pereira, WD (autor correspondente), Ind Nucl Brasil INB, Rodovia Presidente Dutra Km 330,Engn Passos, BR-27555000 Resende, RJ, Brazil.; Pereira, WD (autor correspondente), Univ Fed Rio de Janeiro UFRJ, BR-21941972 Rio De Janeiro, Brazil.	pereiraws@gmail.com	Pereira, Wagner de Souza/H-1356-2012; Pereira, Wagner/AAV-9797-2020	Pereira, Wagner de Souza/0000-0002-0581-9360; Marques Lopes, Jose/0000-0001-7819-6646				Agbalagba E. 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A., 2012, MALAYSIAN J ANAL SCI, V16, P187; USEPA, 1997, EXP FACT HDB; USEPA, 1997, EXP FACT HDB; USEPA, 1997, EXP FACT HDB; USEPA (United States Environmental Protection Agency), 1999, 402R99001 USEPA; Wang XX, 2019, SCI CHINA CHEM, V62, P933, DOI 10.1007/s11426-019-9492-4; WHO, 2018, MAN RAD DRINK WAT; Wu XM, 2019, TRAC-TREND ANAL CHEM, V118, P89, DOI 10.1016/j.trac.2019.04.026; Xiang Y, 2011, NAT CHEM, V3, P697, DOI [10.1038/NCHEM.1092, 10.1038/nchem.1092]; Xiao SJ, 2015, SENSOR ACTUAT B-CHEM, V210, P656, DOI 10.1016/j.snb.2015.01.014; Yin JC, 2013, SENSOR ACTUAT B-CHEM, V188, P147, DOI 10.1016/j.snb.2013.06.100	75	7	7	1	10	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	0944-1344	1614-7499		ENVIRON SCI POLLUT R	Environ. Sci. Pollut. Res.	OCT	2020	27	29					36704	36717		10.1007/s11356-020-09672-6	http://dx.doi.org/10.1007/s11356-020-09672-6		JUN 2020	14	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	NG0VY	32562235				2023-06-23	WOS:000541325300004
J	Pires, LN; Almeida, JS; Dias, FD; Teixeira, LSG				Pires, Lais N.; Almeida, Jorge S.; Dias, Fabio de S.; Teixeira, Leonardo S. G.			Sequential and simultaneous determination of chlorine, iron, and silicon in beer samples by high-resolution continuum source graphite furnace molecular and atomic absorption spectrometry	FOOD ANALYTICAL METHODS			English	Article						Multi-element determination; Beer; UV-radiation; HR-CS GF AAS; HR-CS GF MAS	BREWING PROCESS; TRACE-ELEMENTS; CACL MOLECULE; EXTRACTION; SPECIATION; CHROMATOGRAPHY; PHOSPHORUS; NONMETALS; METALS; ANIONS	An analytical method was proposed for the determination of Cl (via the InCl molecule at 267.2181 nm), Fe (252.7435 nm), and Si (252.8508 nm) in beer samples using sequential and simultaneous determination by high-resolution continuum source graphite furnace atomic absorption spectrometry (HR-CS GF AAS) in combination with high-resolution continuum source graphite furnace molecular absorption spectrometry (HR-CS GF MAS). First, Cl was determined using 600 degrees C and 1800 degrees C as the pyrolysis and vaporization temperatures, respectively, using In as a forming agent of the InCl molecule. Then, Si and Fe were simultaneously determined from the same sample aliquot using 2600 degrees C as the atomization temperature. A solution of Pd/Mg was used as a chemical modifier. The matrix effect was evaluated, and the results indicated that external calibration was possible using aqueous standard solutions. The limit of detection and quantification were 0.05 and 0.17 mg L(-1)for Cl, 0.08 and 0.26 mg L(-1)for Si, and 2.0 and 6.7 mu g L(-1)for Fe, respectively. Recovery tests presented interval between 85 and 120% for the three analytes. Accuracy was confirmed by comparing the results obtained by the proposed method with those obtained by inductively coupled plasma optical emission spectrometry for Si and Fe and by ion chromatography for Cl. The concentration range found in ten beer samples was 106-277 mg L(-1)for Cl, 15-37 mg L(-1)for Si, and < 20-73 mu g L(-1)for Fe.	[Pires, Lais N.; Almeida, Jorge S.; Teixeira, Leonardo S. G.] Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Almeida, Jorge S.; Teixeira, Leonardo S. G.] Univ Fed Bahia, INCT Energia & Ambiente, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Dias, Fabio de S.] Univ Fed Bahia, Inst Ciencias Tecnol & Inovacao, Campus Univ Camacari, BR-42809000 Camacari, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia	Teixeira, LSG (autor correspondente), Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.; Teixeira, LSG (autor correspondente), Univ Fed Bahia, INCT Energia & Ambiente, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.	lsgt@ufba.br	de Souza Dias, Fabio/I-4716-2013; de Almeida, Jorge Santos/ABF-4979-2020; Teixeira, Leonardo S G/J-9131-2016	de Almeida, Jorge Santos/0000-0002-9450-1062; Teixeira, Leonardo S G/0000-0003-0320-8299	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was funded by Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), and Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES).	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SEP	2020	13	9					1746	1754		10.1007/s12161-020-01787-3	http://dx.doi.org/10.1007/s12161-020-01787-3		JUN 2020	9	Food Science & Technology	Science Citation Index Expanded (SCI-EXPANDED)	Food Science & Technology	MP4VD					2023-06-23	WOS:000541302800001
J	De Toni, GB; Bitencourt, MF; Nardi, LVS; Florisbal, LM; Almeida, BS; Geraldes, M				De Toni, G. B.; Bitencourt, M. F.; Nardi, L. V. S.; Florisbal, L. M.; Almeida, B. S.; Geraldes, M.			Dom Feliciano Belt orogenic cycle tracked by its pre-collisional magmatism: The Tonian (ca. 800 Ma) Porto Belo Complex and its correlations in southern Brazil and Uruguay	PRECAMBRIAN RESEARCH			English	Article						Orogenic cycle; Pre-collisional magmatism; Dom Feliciano Belt; Arc magmatism; Back-arc rift; Occam's Razor	DE-LA-PLATA; GERCINO SHEAR ZONE; SAO-GABRIEL BLOCK; PB-HF ISOTOPES; TECTONIC EVOLUTION; BRASILIANO OROGEN; SANTA-CATARINA; RIBEIRA BELT; GEOCHRONOLOGICAL CONSTRAINTS; ZIRCON GEOCHRONOLOGY	The Porto Belo Complex orthogneisses are dominantly intermediate, high-K calc-alkaline rocks of Tonian age (ca. 800 Ma) that represent the hinterland basement of northern Dom Feliciano Belt. Their significance and correlation to other pre-collisional, Tonian orthometamorphic rocks of the same belt are discussed and integrated in an Occam's Razor model for the evolution of the Kaoko-Dom Feliciano-Gariep Orogenic System. The model proposes a single, eastward subduction with temporal variations of subduction angle leading to migration of arc-magmatism before the main collision, in the following stages: a) 925-880 Ma early subduction and forearc magmatism; b) 820-770 Ma flat-slab subduction and arc-magmatism migration towards the back-arc region, with generation of arc-related, Tonian magmatic protoliths; c) 765-700 Ma steepening subduction and arc-magmatism migration towards forearc, as the back-arc area is under extension, and rifting is triggered; d) 700-660 Ma accretionary phase, after final consumption of the oceanic plate; e) 660-640 Ma oblique collision leading to basin inversion and double-verging transpression, with hinterland high-T/low-P metamorphism and exhumation; f) 640-580 Ma post-collisional magmatism and shear belt development.	[De Toni, G. B.; Bitencourt, M. F.; Nardi, L. V. S.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias PPGGEO, Porto Alegre, RS, Brazil; [Florisbal, L. M.] Univ Fed Santa Catarina, Programa Posgrad Geol PPGGeol, Florianopolis, SC, Brazil; [Almeida, B. S.; Geraldes, M.] Univ Estadual Rio de Janeiro UERJ, Dept Geol Reg & Geotecton, Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal de Santa Catarina (UFSC); Universidade do Estado do Rio de Janeiro	De Toni, GB (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias PPGGEO, Porto Alegre, RS, Brazil.	gdetoni@ufrgs.br	de Fátima Bitencourt, Maria/H-8957-2016; Bitencourt, Maria de Fátima/GLR-8862-2022	de Fátima Bitencourt, Maria/0000-0001-7022-9175; Bitencourt, Maria de Fátima/0000-0001-7022-9175; Saar de Almeida, Bruna/0000-0002-2589-1669	Brazilian National Research Council (CNPq) [311486/2015-0]; Coordenacao de Aperfeicoamento de Pessoal Docente (CAPES) [88881.117872/2016-01, 88887.141226/2017-00];  [481841/2012-1];  [141011/2015-7]	Brazilian National Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal Docente (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); ; 	The authors acknowledge the Brazilian National Research Council (CNPq) for financial support to this project with productivity grants to M.F. Bitencourt (311486/2015-0) and L.V.S. Nardi, and funding through Universal Project N degrees 481841/2012-1 (M.F. Bitencourt), and PhD scholarship to G.B. De Toni (141011/2015-7), also supported by Coordenacao de Aperfeicoamento de Pessoal Docente (CAPES - 88881.117872/2016-01; 88887.141226/2017-00). A. Martini and P.H.S. Andrade are acknowledged for fieldwork assistance and further discussions, and J. Konopasek for friendly and fruitful discussions on collisional and pre-collisional settings. The authors are also grateful to Precambrian Research reviewers S. Oriolo and R. Schmitt whose critical reviews have lead to significant improvement of this work.	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JUN 15	2020	342								105702	10.1016/j.precamres.2020.105702	http://dx.doi.org/10.1016/j.precamres.2020.105702			25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6KT					2023-06-23	WOS:000528208200020
J	Nunes, S; Gastauer, M; Cavalcante, RBL; Ramos, SJ; Caldeira, CF; Silva, D; Rodrigues, RR; Salomao, R; Oliveira, M; Souza, PWM; Siqueira, JO				Nunes, Samia; Gastauer, Markus; Cavalcante, Rosane B. L.; Ramos, Silvio J.; Caldeira Jr, Cecilio F.; Silva, Daniel; Rodrigues, Ricardo R.; Salomao, Rafael; Oliveira, Mariana; Souza-Filho, Pedro W. M.; Siqueira, Jose O.			Challenges and opportunities for large-scale reforestation in the Eastern Amazon using native species	FOREST ECOLOGY AND MANAGEMENT			English	Article						Reforestation; Amazon; Natural regeneration; Species selection; Seed availability; Economic incentives; Socioeconomic benefits	TROPICAL FOREST RESTORATION; REMOTE-SENSING TECHNOLOGIES; LAND-USE CHANGE; ECOSYSTEM SERVICES; CARBON SEQUESTRATION; AGROFORESTRY SYSTEMS; DRY FOREST; BIODIVERSITY; DIVERSITY; SUCCESS	Reforestation and forest restoration are recognized as an effective means of halting biodiversity loss and increasing the performance of ecosystem services such as carbon sequestration and the protection and maintenance of water resources. The objective of this review is to describe the main challenges and opportunities for large-scale forest restoration and reforestation using native species in the Amazon, focusing on Para state and the Itacaiunas watershed. Large-scale forest restoration and reforestation in the Eastern Amazon may contribute to meeting national and global restoration commitments and reducing/eliminating the actual forest deficit caused by noncompliance with the Brazilian Native Vegetation Protection Law, concomitantly mitigating impacts on climate change, enhancing ecosystem services (e.g., protection of water resources and reduction of soil erosion) and maintaining biodiversity. The selection of active and passive reforestation approaches depends on land-use history, landscape context and reforestation targets, and the promotion of natural regeneration reduces implementation costs. To measure the ecological and socioeconomic success of forest restoration and reforestation, a large number of on-the-ground and remote indicators are available, and the use of a combination of both methods can reduce the monitoring cost. The socioeconomic benefits of reforestation include financial gains from restoration and carbon programs; furthermore, the commercialization of timber and non-timber products and their use for subsistence may improve livelihoods and farm incomes. Nevertheless, implementation of large-scale reforestation in the Eastern Amazon requires research regarding the selection and the nutritional demands of native species and the development of adequate soil management strategies that promote the growth of native species and yields. The insufficient availability of seeds and seedlings is a major bottleneck for large-scale forest restoration and reforestation with native species. Thus, increasing the availability, diversity and quality of seedlings and seeds of native species to supply the demand for planting activities, as well as the registration of producers in the National Register of Seeds and Seedlings, is necessary to achieve compliance with national legislation and international commitments. Competition between reforestation and the expansion of agricultural and cattle ranching frontiers combined with a lack of markets for commercial products from restored areas constrains the socioeconomic viability of large-scale reforestation. To outweigh deforestation incentives, regulation and effective implementation of markets and programs such as REDD+, CDM and PES is thus paramount. To enhance the integration of human well-being, socioeconomic enhancements and ecological functionality, forest and landscape restoration concepts offer promising tools for the region.	[Nunes, Samia; Gastauer, Markus; Cavalcante, Rosane B. L.; Ramos, Silvio J.; Caldeira Jr, Cecilio F.; Souza-Filho, Pedro W. M.; Siqueira, Jose O.] Inst Tecnol Vale, Rua Boaventura Silva 955, BR-66055090 Belem, Para, Brazil; [Silva, Daniel] Univ Texas Austin, Dept Geog & Environm, Austin, TX 78712 USA; [Rodrigues, Ricardo R.] Univ Sao Paulo ESALQ, BR-13418900 Piracicaba, Brazil; [Salomao, Rafael] Univ Fed Rural Amazonia, Belem, Para, Brazil; [Salomao, Rafael] Museu Paraense Emilio Goeldi, Belem, Para, Brazil; [Oliveira, Mariana] WRI Brasil, Rua Claudio Soares,N72,Cj 1510, BR-05422030 Sao Paulo, Brazil; [Souza-Filho, Pedro W. M.] Univ Fed Para, Geosci Inst, Rua Augusto Correa 1, BR-66075110 Belem, Para, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; University of Texas System; University of Texas Austin; Universidade Federal Rural da Amazonia (UFRA); Museu Paraense Emilio Goeldi; Universidade Federal do Para	Nunes, S (autor correspondente), Inst Tecnol Vale, Rua Boaventura Silva 955, BR-66055090 Belem, Para, Brazil.	samia.nunes@itv.org	Rodrigues, Ricardo Ribeiro/D-5557-2012; Frois, Cecilio/HQZ-9386-2023; Souza-Filho, Pedro Walfir M. M./J-4958-2012; Gastauer, Markus/GMW-6022-2022; Souza, Pedro/GZH-1275-2022	Rodrigues, Ricardo Ribeiro/0000-0003-4818-0736; Souza-Filho, Pedro Walfir M. 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Ecol. Manage.	JUN 15	2020	466								118120	10.1016/j.foreco.2020.118120	http://dx.doi.org/10.1016/j.foreco.2020.118120			15	Forestry	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Forestry	LK1SV					2023-06-23	WOS:000530639700004
J	Watling, J; Castro, MT; Simon, MF; Rodrigues, FO; de Medeiros, MB; De Oliveira, PE; Neves, EG				Watling, Jennifer; Castro, Martin Torres; Simon, Marcelo F.; Rodrigues, Flavio O.; de Medeiros, Marcelo Brilhante; De Oliveira, Paulo E.; Neves, Eduardo G.			Phytoliths from native plants and surface soils from the Upper Madeira river, SW Amazonia, and their potential for paleoecological reconstruction	QUATERNARY INTERNATIONAL			English	Article						Phytoliths; Reference collection; Amazonia	NEOTROPICAL ECOSYSTEMS; STARCH GRAINS; LAND-USE; ASSEMBLAGES; DYNAMICS; DIFFERENTIATION; HABITATION; RONDONIA; HOLOCENE; BUILDERS	Phytolith reference collections of plants and surface soils are a critical part of studies that use these microbotanical remains for archaeological and paleoecological reconstruction. In the archaeologically-rich region of the Upper Madeira river in Rondonia, Brazil, phytolith analysis is being applied in both on- and off-site contexts in order to shed light on human-environment interactions over a period that extends almost the entire Holocene. The present study brings together data on phytolith production patterns among 90 native species, representing 36 plant families, as well as 56 surface soil samples taken from underneath 11 monitored forest plots. Our discussion focuses on the comparison between the surface soil phytolith records and the above-ground floristic inventories, scrutinized considering the plant reference collection results. We found that the phytoliths of several species which produce diagnostic or potentially-diagnostic morphotypes were under-represented in the surface soils, including several understory herbs. While the phytolith assemblages from three forest types (palm, sororoca and dense forest) presented considerable overlap, in accordance with similarities in the floristic inventories, bamboo forest and different types of campinaranas were able to be distinguished based on their phytolith signatures.	[Watling, Jennifer; Neves, Eduardo G.] Univ Sao Paulo, Museum Archaeol & Ethnol, Ave Prof Almeida Prado 1466, BR-05508070 Sao Paulo, SP, Brazil; [Castro, Martin Torres; De Oliveira, Paulo E.] Univ Sao Paulo, Inst Geosci, Rua Do Lago 562, BR-05507070 Sao Paulo, SP, Brazil; [Simon, Marcelo F.; de Medeiros, Marcelo Brilhante] Embrapa Genet Resources & Biotechnol, Ave W5 Norte, BR-70770917 Brasilia, DF, Brazil; [Rodrigues, Flavio O.] Univ Fed Goias, Inst Biol Sci, Dept Ecol, Grad Program Ecol & Evolut,Setor Vila Itatiaia, Ave Esperanca S-N, BR-74690900 Goiania, Go, Brazil; [De Oliveira, Paulo E.] Field Museum Nat Hist, Keller Sci Act Ctr, 1400 S Lake Shore Dr, Chicago, IL 60605 USA	Universidade de Sao Paulo; Universidade de Sao Paulo; Empresa Brasileira de Pesquisa Agropecuaria (EMBRAPA); Universidade Federal de Goias; Field Museum of Natural History (Chicago)	Watling, J (autor correspondente), Univ Sao Paulo, Museum Archaeol & Ethnol, Ave Prof Almeida Prado 1466, BR-05508070 Sao Paulo, SP, Brazil.	jwatling@usp.br	Rodrigues, Flávio/A-8724-2014; simon, marcelo/HZH-8168-2023; Medeiros, Marcelo Brilhante/AAR-7172-2020; Simon, Marcelo F./AAA-7161-2019	Rodrigues, Flávio/0000-0001-8538-0089; Medeiros, Marcelo Brilhante/0000-0001-7619-6001; Simon, Marcelo F./0000-0002-5732-1716; Watling, Jennifer/0000-0001-7897-5105	Fundacao de Amparo a Pesquisa do Estado do Sao Paulo (FAPESP) [2014/21207-5, 2017/09718-2, 2017/25157-0]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [17/25157-0] Funding Source: FAPESP	Fundacao de Amparo a Pesquisa do Estado do Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	This research was made possible by grants from the Fundacao de Amparo a Pesquisa do Estado do Sao Paulo (FAPESP): 2014/21207-5 (to JW and EGN), 2017/09718-2 (to JW and MTC) and 2017/25157-0 (to JW). Special thanks go to Riccardo Rella for help with the statistical analyses, and to the two anonymous reviewers for their feedback to the article.	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Int.	JUN 10	2020	550						85	110		10.1016/j.quaint.2020.03.045	http://dx.doi.org/10.1016/j.quaint.2020.03.045			26	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Physical Geography; Geology	MT6OH					2023-06-23	WOS:000555091700008
J	McLachlan, RL; Ogston, AS; Asp, NE; Fricke, AT; Nittrouer, CA; Schettini, CAF				McLachlan, Robin L.; Ogston, Andrea S.; Asp, Nils E.; Fricke, Aaron T.; Nittrouer, Charles A.; Schettini, Carlos A. F.			Morphological evolution of a macrotidal back-barrier environment: The Amazon Coast	SEDIMENTOLOGY			English	Article						Amazon; back-barrier; estuary; mangroves; morphology; sediment; tidal channel	SEA-LEVEL RISE; MANGROVE-FOREST; TURBIDITY MAXIMUM; ESTUARINE SYSTEM; HUMAN IMPACT; SALT-MARSH; SEDIMENT; CHANNEL; DYNAMICS; PROGRADATION	Coastal barriers provide sheltered, low-energy settings for fine-grained sediment deposition and retention, although the process of back-barrier infilling and how tidal-channel connectivity impacts this process is not well-understood. Understanding how back-barrier environments infill and evolve is necessary to predict how they will respond to future changes in sea-level and sediment supply. With this motivation, in situ observations and sedimentary signatures from an Amazonian tidal-channel system are interpreted to create a conceptual model of morphological evolution in a macrotidal back-barrier environment that is rich in fine-grained sediment, vegetated by mangroves and incised by tidal channels with multiple outlets. Results indicate that within a high-connectivity back-barrier channel, tidal processes dominate sedimentation and morphological development. Sediment cores (<60 cm) exhibited millimetre-scale tidalites composed of sand and mud. High-connectivity channels allow tidal propagation from multiple inlets, and in this case, the converging flood waves promote delivery of sediment fluxing through the system to the mangrove flats in the convergence zone. Sediment preferentially deposits in regions with adequate accommodation space and dense vegetation, and in these zones, sediment grain size is slightly finer than that transiting through the system. The greatest sediment-accumulation rates (3 to 4 cm yr(-1)), calculated from steady-state Pb-210 profiles, were found in the convergence zone near the mangrove-channel edge. As tidal flats aggrade vertically and prograde into the channels, accommodation space diminishes. In effect, the channel's narrowest stretch is expected to migrate along the path of net-sediment flux towards regions with more accommodation space until it reaches the tidal-convergence zone. The location of recent preferential infilling is evidenced by relatively rapid sediment-accumulation rates, finer sediment and significant clustering of small secondary tidal channels. These findings shed light on how sediment transported through vegetated back-barrier environments is ultimately preserved and how evidence preserved in surface morphology and the geological record can be interpreted.	[McLachlan, Robin L.; Ogston, Andrea S.; Fricke, Aaron T.; Nittrouer, Charles A.] Univ Washington, Sch Oceanog, 1501 NE Boat St, Seattle, WA 98195 USA; [Asp, Nils E.] Univ Fed Para, Inst Estudos Costeiros, Campus Braganca,Alameda Leandro Ribeiro S-N, BR-68600000 Braganca, PA, Brazil; [Schettini, Carlos A. F.] Univ Fed Rio Grande, Inst Oceanog, Ave Italia Km 8, BR-96203900 Rio Grande, RS, Brazil	University of Washington; University of Washington Seattle; Universidade Federal do Para; Universidade Federal do Rio Grande	McLachlan, RL (autor correspondente), Univ Washington, Sch Oceanog, 1501 NE Boat St, Seattle, WA 98195 USA.	mclachlan.rl@gmail.com	Asp, Nils/J-6226-2012	Asp, Nils/0000-0002-6468-6158	U.S. Office of Naval Research [N00014-15-1-2011, N00014-17-1-2350, N00014-13-1-0127, N00014-13-1-0781]; U.S. Office of Naval Research Global [N62909-14-1-N205]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [3290/2013]; National Science Foundation Graduate Research Fellowship [DGE1256082]	U.S. Office of Naval Research(Office of Naval Research); U.S. Office of Naval Research Global(Office of Naval Research); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Science Foundation Graduate Research Fellowship(National Science Foundation (NSF))	We thank members of the Universidade Federal do Para Institute of Coastal Studies and the University of Washington Sediment Dynamics Lab for their generous efforts in the field and laboratory Nils E. Asp and Carlos A.F. Schettini are CNPq research fellows. This work was supported by the U.S. Office of Naval Research [grant numbers N00014-15-1-2011, N00014-17-1-2350, N00014-13-1-0127, N00014-13-1-0781], the U.S. Office of Naval Research Global [grant number N62909-14-1-N205], and the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [Finance Code 3290/2013]. This material is based upon work supported by the National Science Foundation Graduate Research Fellowship under Grant No. DGE1256082. Any opinion, findings, and conclusions or recommendations expressed in this material are those of the authors(s) and do not necessarily reflect the views of the National Science Foundation.	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J	Hartmann, LA; Duarte, SK				Hartmann, Leo Afraneo; Duarte, Sandro Kucera			Novo Hamburgo Complex formed by hydrothermal, explosive injection of Botucatu erg sand into extensive tracts of Parana Volcanic Province (S Brazil)	JOURNAL OF SEDIMENTARY ENVIRONMENTS			English	Article						Basalt-rhyodacite lavas; Extrudites; Sand-filled structures; Paleoerg; Porosity; Permeability; Geochemistry	AMETHYST; LAVAS; GEOCHEMISTRY; STRATIGRAPHY; DISTRICTS; URUGUAY; TORRES; QUARAI; SERRA; BASE	The Parana Volcanic Province follows Siberia as the second largest in the continents and offers a unique opportunity to study the hydrothermal relationship between basalt-rhyodacite lavas and buried erg-turned aquifer in an intraplate setting. Injected sand fluidized after basalt sealing and was succeeded by amethyst and agate geode opening and filling. Excellent exposures in the Herveiras cuesta, southern Brazil, allow the comparison of processes over long distances (1500 km) in the volcanic group. Fieldwork and basalt chemistry led to the identification of three hydrothermal processes-amygdales filling (H1), sand injection (H2) and amethyst geodes formation (H3). Sand injection was triggered by high temperature (150 celcius) and seismicity. These low-temperature processes identified in the Herveiras cuesta demonstrate the homogeneity of relationships between the paleoerg, giant aquifer and intraplate volcanic rocks across the volcanic province.	[Hartmann, Leo Afraneo; Duarte, Sandro Kucera] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Hartmann, LA (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	leo.hartmann@ufrgs.br	Hartmann, Léo A/D-7663-2013	Hartmann, Léo A/0000-0001-7863-5071; Duarte, Sandro/0000-0002-2380-4613	PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil) on strategic minerals from southern Brazil [10/0021-89]	PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil) on strategic minerals from southern Brazil	Financial support was provided by a project (Grant number 10/0021-89) PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil) on strategic minerals from southern Brazil, coordinated by Leo A. Hartmann.	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Sediment. Environ.	JUN	2020	5	2					187	198		10.1007/s43217-020-00015-6	http://dx.doi.org/10.1007/s43217-020-00015-6		JUN 2020	12	Environmental Sciences	Emerging Sources Citation Index (ESCI)	Environmental Sciences & Ecology	MG9OP					2023-06-23	WOS:000538693600001
J	de Oliveira, AD; de Oliveira, DT; Angelica, RS; Andrade, EHD; da Silva, JKD; Filho, GND; Coral, N; Pires, LHD; Luque, R; do Nascimento, LAS				de Oliveira, Alex de Nazare; de Oliveira, Deborah Terra; Angelica, Romulo Simoes; de Aguiar Andrade, Eloisa Helena; do Rosario da Silva, Joyce Kelly; da Rocha Filho, Geraldo Narciso; Coral, Natasha; de Oliveira Pires, Luiza Helena; Luque, Rafael; Santos do Nascimento, Luis Adriano			Efficient esterification of eugenol using a microwave-activated waste kaolin	REACTION KINETICS MECHANISMS AND CATALYSIS			English	Article						Eugenol; Eugenyl acetate; Flint kaolin; Microwaves; Heterogeneous catalysis; Esterification	ASSISTED ACID TREATMENT; HETEROGENEOUS CATALYST; DISSOLUTION KINETICS; PALM OIL; BENTONITE; ACETATE; DERIVATIVES; ADSORPTION; METAKAOLIN; CONVERSION	Eugenyl acetate has been investigated because of its beneficial bioactive antioxidant, antimicrobial and potential properties against the development of Aedes aegypti larvae. Here, we report, for the first time, the use of a catalyst prepared from flint kaolin with microwave irradiation for the acetylation of eugenol. A few kinetic parameters were evaluated in the experiments used for eugenol ester synthesis. High conversions (98%) were obtained after 1 h of reaction. The prepared material shows good activity (over 90%) even after 4 cycles of use. Therefore, the use of microwave radiation made it possible to prepare a catalyst in a very short time using a low-cost industrial by-product as a raw material that proved to be highly active, in addition to the additional advantage of being reusable, which would reduce possible environmental impacts caused by its disposal in the environment.	[de Oliveira, Alex de Nazare; de Aguiar Andrade, Eloisa Helena; do Rosario da Silva, Joyce Kelly; da Rocha Filho, Geraldo Narciso; Santos do Nascimento, Luis Adriano] Univ Fed Para, Grad Program Chem, Augusto Correa St, BR-66075110 Belem, PA, Brazil; [de Oliveira, Alex de Nazare; de Oliveira, Deborah Terra; da Rocha Filho, Geraldo Narciso; Santos do Nascimento, Luis Adriano] Univ Fed Para, Lab Oils Amazon, Perimetral Ave, BR-66075750 Belem, PA, Brazil; [de Oliveira, Alex de Nazare] Univ Fed Amapa, Dept Exact & Technol Sci, Rod Juscelino Kubitschek,Km 02 Jardim Marco Zero, BR-68903419 Macapa, AP, Brazil; [de Oliveira, Deborah Terra; do Rosario da Silva, Joyce Kelly; Santos do Nascimento, Luis Adriano] Univ Fed Para, Grad Program Biotechnol, Augusto Correa St, BR-66075110 Belem, PA, Brazil; [Angelica, Romulo Simoes] Univ Fed Para, Lab Xray Diffract, Augusto Correa St, BR-66075110 Belem, PA, Brazil; [de Aguiar Andrade, Eloisa Helena] Museu Paraense Emilio Goeldi, Bot Coordinating, Adolpho Ducke Lab, Perimetral Ave, BR-66077830 Belem, PA, Brazil; [Coral, Natasha; de Oliveira Pires, Luiza Helena] Univ Fed Para, High Sch Applicat, BR-66095780 Para, Brazil; [Luque, Rafael] Peoples Friendship Univ Russia, RUDN Univ, Res Inst Chem, Fac Sci, 6 Miklukho Maklaya Str, Moscow 117198, Russia; [Luque, Rafael] Univ Cordoba, Dept Organ Chem, Ctra Nnal 4-A,Km 396, Cordoba 14014, Spain	Universidade Federal do Para; Universidade Federal do Para; Fundacao Universidade Federal do Amapa; Universidade Federal do Para; Universidade Federal do Para; Museu Paraense Emilio Goeldi; Universidade Federal do Para; Peoples Friendship University of Russia; Universidad de Cordoba	do Nascimento, LAS (autor correspondente), Univ Fed Para, Grad Program Chem, Augusto Correa St, BR-66075110 Belem, PA, Brazil.; do Nascimento, LAS (autor correspondente), Univ Fed Para, Lab Oils Amazon, Perimetral Ave, BR-66075750 Belem, PA, Brazil.; do Nascimento, LAS (autor correspondente), Univ Fed Para, Grad Program Biotechnol, Augusto Correa St, BR-66075110 Belem, PA, Brazil.	alexoliveiraquimica@hotmail.com; deborahterra.o@gmail.com; rsangelica@gmail.com; eloisa@museu-goeldi.br; joycekellys@ufpa.br; geraldonrf@gmail.com; natasha.coral@yahoo.com.br; lulenapires@hotmail.com; adrlui1@yahoo.com.br	DA SILVA, JOYCE KELLY R./S-2494-2017; Filho, Geraldo N Rocha/J-5464-2013; Nascimento, Luís Adriano Santos do/A-4615-2013; de Oliveira, Alex de Nazaré/GPG-1822-2022; do Nascimento, Luís Adriano Santos/O-7466-2019; Angelica, Romulo/G-6245-2010	DA SILVA, JOYCE KELLY R./0000-0002-9351-876X; Nascimento, Luís Adriano Santos do/0000-0001-9947-4078; de Oliveira, Alex de Nazaré/0000-0002-7501-6344; do Nascimento, Luís Adriano Santos/0000-0001-9947-4078; Angelica, Romulo/0000-0002-3026-5523; NARCISO DA ROCHA FILHO, GERALDO/0000-0002-5712-8254; de Aguiar Andrade, Eloisa Helena/0000-0003-0640-7496	CNPQ [432221/2018-2]; Banco da Amazonia grant [2018/212]	CNPQ(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Banco da Amazonia grant	This research was funded by CNPQ, Grant Number 432221/2018-2 and Banco da Amazonia grant number 2018/212.	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Kinet. Mech. Catal.	AUG	2020	130	2					633	653		10.1007/s11144-020-01797-6	http://dx.doi.org/10.1007/s11144-020-01797-6		JUN 2020	21	Chemistry, Physical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	MU3MX					2023-06-23	WOS:000538209500001
J	Machado, JPSL; Jelinek, AR; Stephenson, R; Gaucher, C; Bicca, MM; Chiglino, L; Genezini, FA				Silveira Luiz Machado, Joao Pacifico; Jelinek, Andrea Ritter; Stephenson, Randell; Gaucher, Claudio; Bicca, Marcos Muller; Chiglino, Leticia; Genezini, Frederico Antonio			Low-temperature thermochronology of the South Atlantic margin along Uruguay and its relation to tectonic events in West Gondwana	TECTONOPHYSICS			English	Article						Thermochronology; Fission-tracks; (U-Th)/He; West Gondwana; South Atlantic; Uruguay	APATITE FISSION-TRACK; LA-PLATA CRATON; DOM FELICIANO BELT; NICO PEREZ TERRANE; HELIUM DIFFUSION KINETICS; CUCHILLA DIONISIO TERRANE; ZIRCON RADIATION-DAMAGE; (U-TH)/HE THERMOCHRONOMETRY; CONTINENTAL-MARGIN; BREAK-UP	The geodynamic forces acting during Jurassic-Cretaceous South Atlantic rifting provoked intense transformations in West Gondwana, such as the reactivation of ancient basement structures, voluminous magmatism and general uplift of the new continental margins. Low-temperature thermochronology records cooling associated with uplift syn- and post-breakup along the Brazilian margin, while further south, in Uruguay, mostly pre-breakup uplift is identified. Thermochronometry data are scarce in Uruguay, but previous studies suggest that basement cooling and exhumation preceded West Gondwana breakup by hundreds of millions of years. To improve our knowledge of Uruguay's thermotectonic evolution, in this study we present 19 apatite fission-track ages, 42 apatite and 40 zircon (U-Th)/He single crystal ages for the Uruguayan shield (UYS), from which we modeled 19 inverse thermal histories. Our results suggest that the UYS temperatures were below 200 degrees C since the early Paleozoic, and that cooling below 110 degrees C started during the Carboniferous, with continuous exhumation of the basement until Early Cretaceous. The onset of this long-term uplift is correlated with orogenesis and terrane accretions in the SW margin of West Gondwana during the Paleozoic. Lithosphere thinning and uplift preceding breakup contributed to the continuous Late Paleozoic to middle Mesozoic exhumation, until the voluminous volcanism of the Parana-Etendeka Large Igneous Province (c. 133 Ma). This magmatic event, combined with the thermal influence of the Tristao da Cunha mantle plume and rift spreading, likely raised the basement geotherm during the Late Cretaceous. Models suggest a slight increase in temperatures of the UYS from Late Cretaceous until the Oligocene, when a final cooling to surface temperatures took place. Our findings corroborate a long and complex thermal history for Uruguay, with crustal uplift occurring essentially before West Gondwana breakup.	[Silveira Luiz Machado, Joao Pacifico; Stephenson, Randell] Univ Aberdeen, Sch Geosci, Aberdeen, Scotland; [Silveira Luiz Machado, Joao Pacifico; Jelinek, Andrea Ritter; Bicca, Marcos Muller] Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil; [Gaucher, Claudio; Chiglino, Leticia] Univ Republica, Fac Ciencias, Montevideo, Uruguay; [Genezini, Frederico Antonio] Ctr Reator Pesquisas, Inst Pesquisas Energet & Nucl, Sao Paulo, Brazil	University of Aberdeen; Universidade Federal do Rio Grande do Sul; Universidad de la Republica, Uruguay; Comissao Nacional de Energia Nuclear (CNEN); Instituto de Pesquisas Energeticas e Nucleares (IPEN)	Machado, JPSL (autor correspondente), Univ Aberdeen, Sch Geosci, Aberdeen, Scotland.	j.luizmachado.18@abdn.ac.uk	Jelinek, Andrea/ABH-9386-2020; Genezini, Frederico A./C-8458-2012	Jelinek, Andrea/0000-0002-7375-5039; Stephenson, Randell/0000-0003-4868-8601; Machado, Joao Pacifico/0000-0002-3590-8428	Shell Brasil through the "Shell -BG05: UoA-UFRGS-SWB Sedimentary Systems" project at UFRGS; ANP through the R&D levy regulation; CNPq scholarship [SWE 204254/2017-5]; CNPq [303184/2017-5]	Shell Brasil through the "Shell -BG05: UoA-UFRGS-SWB Sedimentary Systems" project at UFRGS; ANP through the R&D levy regulation; CNPq scholarship(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors gratefully acknowledge the support from Shell Brasil through the "Shell -BG05: UoA-UFRGS-SWB Sedimentary Systems" project at UFRGS and the strategic importance of the support given by ANP through the R&D levy regulation. We thank Peter Reiners and his team at the Arizona Radiogenic Helium Dating Laboratory (US) for the (UeTh)/He analyses and support during the data evaluation. The first author thanks the CNPq scholarship (SWE 204254/2017-5) during the exchange period at the University of Aberdeen. A.R. Jelinek also thanks the support from CNPq (Project 303184/2017-5). This manuscript was improved after helpful reviews by Mathias Hueck and an anonymous reviewer.	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J	Birch, GF; Lee, JH; Tanner, E; Fortune, J; Munksgaard, N; Whitehead, J; Coughanowr, C; Agius, J; Chrispijn, J; Taylor, U; Wells, F; Bellas, J; Besada, V; Vinas, L; Soares-Gomes, A; Cordeiro, RC; Machado, W; Santelli, RE; Vaughan, M; Cameron, M; Brooks, P; Crowe, T; Ponti, M; Airoldi, L; Guerra, R; Puente, A; Gomez, AG; Zhou, GJ; Leung, KMY; Steinberg, P				Birch, G. F.; Lee, J. -H.; Tanner, E.; Fortune, J.; Munksgaard, N.; Whitehead, J.; Coughanowr, C.; Agius, J.; Chrispijn, J.; Taylor, U.; Wells, F.; Bellas, J.; Besada, V.; Vinas, L.; Soares-Gomes, A.; Cordeiro, R. C.; Machado, W.; Santelli, R. E.; Vaughan, M.; Cameron, M.; Brooks, P.; Crowe, T.; Ponti, M.; Airoldi, L.; Guerra, R.; Puente, A.; Gomez, A. G.; Zhou, G. J.; Leung, K. M. Y.; Steinberg, P.			Sediment metal enrichment and ecological risk assessment of ten ports and estuaries in the World Harbours Project	MARINE POLLUTION BULLETIN			English	Article						Sediment quality guidelines; Environmental indices; Anthropogenic change; Normalisation; Classification scheme	RIO-DE-JANEIRO; SIMON BAY RIA; HEAVY-METALS; GUANABARA BAY; SURFACE SEDIMENTS; MARINE-SEDIMENTS; SPATIAL-DISTRIBUTION; COASTAL LAGOON; TRACE-METALS; SOURCE APPORTIONMENT	Ten global harbours were assessed for sediment quality by quantifying the magnitude of anthropogenic change and ecological risk. Anthropogenic change (enrichment) was high for Derwent River and Sydney estuary, moderate for Santander Harbour, Rio de Janeiro and Dublin Port, slight for Hong Kong, minimal for Darwin. All 10 enrichment indices used showed similar results. Derwent River sediment was rated at high ecological risk, followed by Sydney and Santander estuaries with moderate risk. Auckland and Darwin sediments exhibited minimal ecological risk and sediment in the remaining harbours (Dublin, Hong Kong, Ravenna, Ria de Vigo and Rio de Janeiro) were assessed at slight ecological risk. The extraordinary variety of environments and types/quantities/qualities of data investigated resulted in as much a critique and development of methodology, as an assessment of human impact, including unique techniques for elemental normalisation and contaminant classification. Recommendations for an improved technical framework for sediment quality assessment are provided.	[Birch, G. F.; Lee, J. -H.] Univ Sydney, Sch Geosci, Sydney, NSW, Australia; [Lee, J. -H.] Lotsearch, 3-68 Alfred St, Milsons Point, NSW 2061, Australia; [Tanner, E.; Steinberg, P.] Sydney Inst Marine Sci, Mosman, NSW, Australia; [Fortune, J.] Dept Environm & Nat Resources, Aquat Hlth Unit, Palmerston, NT, Australia; [Munksgaard, N.] Charles Darwin Univ, Res Inst Environm & Livelihoods RIEL, Darwin, NT, Australia; [Whitehead, J.; Coughanowr, C.; Agius, J.; Chrispijn, J.; Taylor, U.; Wells, F.] DPIPWE, Derwent River Program, Hobart, Tas, Australia; [Bellas, J.; Besada, V.; Vinas, L.] Ctr Oceanog Vigo, Vigo 36390, Pontevedra, Spain; [Soares-Gomes, A.] Fed Fluminense Univ, Marine Biol Dept, Valonguinho Campus, Niteroi, RJ, Brazil; [Cordeiro, R. C.; Machado, W.] Fed Fluminense Univ, Geochem Dept, Valonguinho Campus, Niteroi, RJ, Brazil; [Santelli, R. E.] Rio de Janeiro Fed Univ, Chem Inst, Rio De Janeiro, RJ, Brazil; [Vaughan, M.; Cameron, M.] Auckland Council, Res & Evaluat Unit, Auckland, New Zealand; [Brooks, P.; Crowe, T.] Univ Coll Dublin, UCD Earth Inst, Dublin, Ireland; [Brooks, P.; Crowe, T.] Univ Coll Dublin, Sch Biol & Environm Sci, Dublin, Ireland; [Ponti, M.; Airoldi, L.] Univ Bologna, Dept Biol Geol & Environm Sci, I-48123 Ravenna, Italy; [Ponti, M.; Airoldi, L.; Guerra, R.] Univ Bologna, Interdept Res Ctr Environm Sci, I-48123 Ravenna, Italy; [Guerra, R.] Univ Bologna, Dept Phys & Astron, I-48123 Ravenna, Italy; [Puente, A.; Gomez, A. G.] Univ Cantabria, IHCantabria Inst Hidraul Ambiental, Avda Isabel Torres,15, Santander 39011, Spain; [Zhou, G. J.; Leung, K. M. Y.] Univ Hong Kong, Swire Inst Marine Sci, Pokfulam, Hong Kong, Peoples R China; [Zhou, G. J.; Leung, K. M. Y.] Univ Hong Kong, Sch Biol Sci, Pokfulam, Hong Kong, Peoples R China; [Leung, K. M. Y.] City Univ Hong Kong, State Key Lab Marine Pollut, Kowloon, Hong Kong, Peoples R China; [Gomez, A. G.] SOCIB, Balear Isl Coastal Observing & Forecasting Syst, Edificio Naorte,Bloque A,Parc Bit, Palma De Mallorca 07122, Spain	University of Sydney; Sydney Institute of Marine Science; Charles Darwin University; Spanish Institute of Oceanography; Universidade Federal Fluminense; Universidade Federal Fluminense; University College Dublin; University College Dublin; University of Bologna; University of Bologna; University of Bologna; Universidad de Cantabria; IHCantabria - Instituto de Hidraulica Ambiental de la Universidad de Cantabria; University of Hong Kong; University of Hong Kong; City University of Hong Kong	Birch, GF (autor correspondente), Univ Sydney, Sch Geosci, Sydney, NSW, Australia.	gavin.birch@sydney.edu.au	Ponti, Massimo/R-3093-2016; Gomez, Aina G./H-3086-2015; Puente, Araceli/ABG-9362-2021; Bellas, Juan/N-1594-2015; Zhou, Guangjie/Y-8164-2019; Cordeiro, Renato C/J-8870-2013; Airoldi, Laura/I-3553-2019; Machado, Wilson/P-8047-2019; Viñas, Lucía/B-7804-2008; Guerra, Roberta/B-8587-2012; 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J	Cerva-Alves, T; Hartmann, LA; Remus, MVD; Lana, C				Cerva-Alves, T.; Hartmann, L. A.; Remus, M. V. D.; Lana, C.			Integrated ophiolite and arc evolution, southern Brasiliano Orogen	PRECAMBRIAN RESEARCH			English	Article						Zircon U-Pb-Hf isotopes; Zircon rare earth elements; Dating of metamorphosed mantle; Brasiliano orogeny	DOM FELICIANO BELT; SAO-GABRIEL BLOCK; PB-HF ISOTOPES; VOLCANO-SEDIMENTARY SUCCESSIONS; NEOPROTEROZOIC CRUSTAL ACCRETION; ZIRCON REFERENCE MATERIALS; EDIACARAN PORONGOS GROUP; SUL-RIOGRANDENSE SHIELD; U-PB; TECTONIC EVOLUTION	Integrated study of Tonian ophiolite melanges and intra-oceanic arc of the Sao Gabriel juvenile terrane exposes a key geotectonic unit in the evolutionary history of Gondwana during Brasiliano Orogeny. LA-ICP-MS U-Pb geochronology in rutile and zircon were combined with Lu-Hf and rare earth elements in zircon. We report the first rutile dating of ultramafic rock in the Brazilian Shield of 787.6 +/- 2.6 Ma for the Cambaizinho ophiolite magnesian schist. Dating of rutile corresponds to the metamorphic age of the mantle section of the ophiolite. Sao Gabriel arc infrastructure is represented by the Cambai Complex, including the Vila Nova Suite metatonalite with zircon U-Pb age of 724.6 +/- 3.2 Ma and late Sanga do Jobim Suite monzogranite intrusions with two main pulses at 698.9 +/- 4.2 Ma and 673.9 +/- 6.8 Ma. Zircon epsilon Hf(t) values are positive for both rocks and range between +10.1 and +7.4 in metatonalite and +9.2 to +2.5 in monzogranite. Detrital zircon from metasedimentary rocks support superstructure arc investigation. Ages range from 817 to 650 Ma, with strong concentration between 750 and 730 Ma. Positive epsilon Hf(t) values and Rare Earth Elements (REE) signature point to main source of metasedimentary rocks in the arc, with ophiolitic contribution. Therefore, geotectonic processes in the Brasiliano Orogeny include the construction of Sao Gabriel terrane with Tonian oceanic crust evolving to intra-oceanic subduction until 650 Ma to final development along the margin of continental crust. Overthrusting of the Sao Gabriel terrane onto the Rio de La Plata Craton occurred at 650-620 Ma. Our data correlate with Tonian intra-oceanic arcs from Brasilia belt (Goias arc ca. 862-630 Ma) and Ribeira belt (Serra da Prata arc 856-838 Ma; Rio Negro arc - 790-620 Ma). Oceanic crust generation combined with subduction to form Tonian arcs along the Brasiliano Orogen were most significant for construction of West Gondwana.	[Cerva-Alves, T.; Hartmann, L. A.; Remus, M. V. D.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Lana, C.] Univ Fed Ouro Preto, Dept Geol, Escola Minas, BR-35400000 Ouro Preto, MG, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal de Ouro Preto	Cerva-Alves, T (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	tiara.geologia@gmail.com; leo.hartmann@ufrgs.br; marcus.remus@ufrgs.br; cristiano.lana@ufop.edu.br	Hartmann, Léo A/D-7663-2013	Hartmann, Léo A/0000-0001-7863-5071	Conselho Nacional do Desenvolvimento Cientifico e Tecnologico, Brazilian Government	Conselho Nacional do Desenvolvimento Cientifico e Tecnologico, Brazilian Government	This article is part of the PhD thesis by Tiara Cerva Alves at Programa de Pos-Graduacao em Geociencias, Universidade Federal do Rio Grande do Sul, Brazil. We acknowledge Conselho Nacional do Desenvolvimento Cientifico e Tecnologico, Brazilian Government, for a scholarship to Tiara and overall support to L. A. Hartmann. We also thank Glaucia Queiroga, Jorge Laux, Viter Pinto, Sandro Duarte, Amanda Juliano, Caroline Custodio and Carolina Leandro for field trip and discussions, Gilberto and Denise for mineral preparation. Editor Wilson Teixeira handled the manuscript efficiently and made contributions to the improvement of the article, along with reviewer Fabricio Caxito.	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JUN	2020	341								105648	10.1016/j.precamres.2020.105648	http://dx.doi.org/10.1016/j.precamres.2020.105648			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6KN					2023-06-23	WOS:000528207600010
J	Cruz, DJN; Gorayeb, PSS				Cruz, Danilo J. N.; Gorayeb, Paulo S. S.			Geology and petrology of the mafic dike swarms of the Araguaia Belt: Evidence for distinct events of intracontinental magmatism in central-northern Brazil and correlations with large igneous provinces	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Igneous petrology; Diabase dikes; Intracontinental magmatism; Large igneous provinces; Araguaia belt	CONTINENTAL BASALTS; GEOCHEMISTRY; DISCRIMINATION; CAMP; SR; ND; NOMENCLATURE; COEFFICIENTS; OPHIOLITE; PROGRAM	Extensive N-S and NNW-SEE-trending subparallel mafic dike swarms are intruded into metasedimentary rocks of the Tocantins Group, Araguaia Belt, Central-North of Brazil. They are under-examined, and there is little to no information about their origin and mantellic sources, as well as uncertainty about whether they are part of two different episodes of magmatism. Representative mafic dikes from the Santa Maria das Barreiras-Conceicao do Araguaia region, at the boundary between the states of Path and Tocantins, were studied in order to address these problems. It was possible to separate the dikes into two groups: one consisting of metadiabases affected by the Neoproterozoic regional metamorphism of the Araguaia Belt with varying degrees of transformations and mineral deformation; and the other consisting of unmetamorphosed and undeformed diabases and leucodiabases. The studied dikes are compositionally classified as subalkaline basalts with tholeiitic affinity and were interpreted to be originated in an intracontinental setting with the aid of Ti-V, Zr-Zr/Y, and Zr-Ti discrimination diagrams. However, metadiabases present an arc-like geochemical signature characterized by a pronounced Nb-Ta negative anomaly, whereas leucodiabases and diabases lack a negative Nb-Ta anomaly and show a LREE-enriched pattern, which resembles the signatures of plume-generated basaltic rocks. Also, there is evidence of an important contribution of enriched (EN) mantle components in the source of metadiabases and significant contribution of primitive mantle (PM) in the source of both leucodiabases and diabases. It was suggested, then, that the metadiabases represent the exposed plumbing system of arc-like intracontinental basalts which precede the regional Neoproterozoic metamorphism of the belt, and that the leucodiabases and diabases represent the exposed conduits of intracontinental basalts whose magmatism succeed the metamorphic event. Geochemical models were elaborated to demonstrate that fractional crystallization processes could account for the differentiation of the metadiabases and for the genesis of the leucodiabases via fractionation of the melt from which the diabases formed. The rocks from the earlier event share several similarities with Neoproterozoic mafic rocks from the eastern domain of the Araguaia Belt and nearby Tonian rocks of the 1100 Ma Rincon del Tigre-Huanchaca LIP event, while the rocks from the later event are remarkably similar to nearby CAMP basalts and diabase dikes.	[Cruz, Danilo J. N.; Gorayeb, Paulo S. S.] Fed Univ UFPA, Inst Geosci IG, Grad Program Geol & Geochem PPGG, 01 Augusto Correa St, BR-66075110 Belem, Para, Brazil	Universidade Federal do Para	Cruz, DJN (autor correspondente), Fed Univ UFPA, Inst Geosci IG, Grad Program Geol & Geochem PPGG, 01 Augusto Correa St, BR-66075110 Belem, Para, Brazil.	danilocruz@ufpa.br; gorayebp@ufpa.br		Cruz, Danilo/0000-0002-1402-2900	project "Petrologia, geocronologia e tectonica das rochas magmaticas do Cinturao Araguaia" of the National Council for Scientific and Technological Development (CNPq) [427225/2016-7]; CNPq [130794/2017-1]	project "Petrologia, geocronologia e tectonica das rochas magmaticas do Cinturao Araguaia" of the National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was supported by the project "Petrologia, geocronologia e tectonica das rochas magmaticas do Cinturao Araguaia" of the National Council for Scientific and Technological Development (CNPq) [Edital Universal - grant number 427225/2016-7]. The authors are thankful to the Graduate Program in Geology and Geochemistry (PPGG) at the Federal University of Para (UFPA) and to the Institute of Geosciences (IG) at the University of Brasilia (UnB) for providing the necessary resources and facilities. Furthermore, the first author is very thankful to CNPq for granting a scholarship [grant number 130794/2017-1] that allowed the development of this research.	Abreu FAM, 1978, AN 30 C BRAS GEOL RE, P539; Abreu fam, 1994, ANAIS 3 SIMP GEOL AM, P1; Almeida F.F.M., 1974, C GEOL 28 AN PORT AL, V4, P11; Alvarenga C. J. 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South Am. Earth Sci.	JUN	2020	100								102563	10.1016/j.jsames.2020.102563	http://dx.doi.org/10.1016/j.jsames.2020.102563			24	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900027
J	D'Elia, L; Bilmes, A; Varela, AN; Bucher, J; Lopez, M; Garcia, M; Santos, RV; Hauser, N; Naipauer, M; Sato, AM; Franzese, JR				D'Elia, Leandro; Bilmes, Andres; Varela, Augusto N.; Bucher, Joaquin; Lopez, Manuel; Garcia, Micaela; Ventura Santos, Roberto; Hauser, Natalia; Naipauer, Maximiliano; Maria Sato, Ana; Franzese, Juan R.			Geochronology, sedimentology and paleosol analysis of a Miocene, synorogenic, volcaniclastic succession (La Pava Formation) in the north Patagonian foreland: Tectonic, volcanic and paleoclimatic implications	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Syn-orogenic; La Pava Formation; Volcaniclastic; Geochronology; Sedimentology and paleosols analyses; Tectonic; volcanic and paleoclimatic implications	TECTONOSTRATIGRAPHIC IMPLICATIONS; NORTHWESTERN PATAGONIA; CLIMATIC OPTIMUM; NAZCA FARALLON; SOUTH-AMERICA; NEUQUEN BASIN; ALLUVIAL FANS; THRUST BELT; EVOLUTION; NEOGENE	The initial infill of the Patagonian Broken Foreland is related to Miocene, syn-orogenic, volcaniclastic successions accommodated in intermontane basins. In the last years several works have paid attention to these successions due to their role in the comprehension of the timing of deformation, the relationship between arc-volcanism and the environmental signals, and the climate changes related to the growth of the orogen. In this paper we perform the U-Pb geochronology and the sedimentologic and paleosols analyses of a Miocene, synorogenic, volcaniclastic succession (La Pava Formation) located at the northern part of Patagonian Broken Foreland. The results indicate that the syn-kinematic sedimentation (evidenced by growth strata and progressive unconformities) proceeded between similar to 19 Ma to similar to 14 Ma, associated with arc-derived volcaniclastic deposits, under alluvial conditions with profuse paleosols development. The facies analysis combined with the paleosols and provenance studies indicate episodic and cyclic supply of pyroclastic materials, which were mainly delivered from the catchment area of the system, affected by explosive volcanism. A succession of stacked paleosols was recorded into 3 sections, bounded by unconformities, which record from Alfisols-like, Vertisol-like to Andisols-like paleosols. Paleosols variations were related to the effects of tectonic events, climate changes or to the increase of volcanic supply in comparison to soil-forming processes. The results obtained in this work are considered substantial to unravel the tectonic, volcanic and paleoclimatic framework of the North Patagonian Andes.	[D'Elia, Leandro; Varela, Augusto N.; Bucher, Joaquin; Lopez, Manuel; Garcia, Micaela; Maria Sato, Ana; Franzese, Juan R.] CONICET UNLP, Ctr Invest Geol CIG, La Plata, Buenos Aires, Argentina; [Bilmes, Andres] CENPAT CONICET, Inst Patagon Geol & Paleontol IPGP, Puerto Madryn, Argentina; [Ventura Santos, Roberto; Hauser, Natalia] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Naipauer, Maximiliano] CONICET UBA, Inst Geocronol & Geol Isotop INGEIS, Buenos Aires, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Centro Nacional Patagonico (CENPAT); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidade de Brasilia; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires	D'Elia, L (autor correspondente), CONICET UNLP, Ctr Invest Geol CIG, La Plata, Buenos Aires, Argentina.	ldelia@cig.museo.unlp.edu.ar	Hauser, Natalia/H-2041-2012	Hauser, Natalia/0000-0002-6975-6186	Prestamo BID-PICT [2016-0023]; International Association of Sedimentologists Post-Doctoral Research Grant	Prestamo BID-PICT; International Association of Sedimentologists Post-Doctoral Research Grant	The authors would like to thank the inhabitants of the study area for their support and hospitality. This research was funded by the Prestamo BID-PICT 2016-0023 and by the 2019 International Association of Sedimentologists Post-Doctoral Research Grant. Our thanks go to the Dr. Giorgio Basilici for their constructive and helpful reviews and to the editor-in-Chief of Journal of South American Earth Sciences, Dr. Andres Folguera, for his support.	Aragon E, 2011, J S AM EARTH SCI, V32, P547, DOI 10.1016/j.jsames.2011.02.005; BARKER PF, 1977, MAR GEOL, V25, P15, DOI 10.1016/0025-3227(77)90045-7; Bechis F, 2014, J S AM EARTH SCI, V52, P72, DOI 10.1016/j.jsames.2014.02.003; Bellosi E, 2014, 14 REUN ARG SED ACT, P42; Bilmes A, 2013, TECTONOPHYSICS, V601, P98, DOI 10.1016/j.tecto.2013.05.001; Bilmes Andrés, 2014, Rev. Asoc. Geol. 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South Am. Earth Sci.	JUN	2020	100								102555	10.1016/j.jsames.2020.102555	http://dx.doi.org/10.1016/j.jsames.2020.102555			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900019
J	da Conceicao, DM; de Andrade, LS; Neregato, R; Iannuzzi, R; Crisafulli, A; Cisneros, JC				da Conceicao, Domingas Maria; de Andrade, Luiz Saturnino; Neregato, Rodrigo; Iannuzzi, Roberto; Crisafulli, Alexandra; Cisneros, Juan Carlos			New petrified gymnosperms from the Permian of Maranhao (Pedra de Fogo Formation), Brazil: Ductolobatopitys nov. gen. and Kaokoxylon	GEOBIOS			English	Article						Gymnosperm woods; Pedra de Fogo Formation; Lacustrine environment; Permian; Parnaiba Basin	PARNAIBA BASIN; SOUTHERN-HEMISPHERE; NORTHEASTERN BRAZIL; NEW-MEXICO; PART II; WOODS; CALAMITALEANS; PALEOCLIMATE; COMMUNITIES; SYSTEMATICS	Continuing the study of petrified gymnosperm trunks recovered from the Pedra de Fogo Formation, we identify here two new taxa from the Permian deposits of the Parnaiba Basin, northeastern Brazil. One taxon is an endemic form named Ductolobatopitys mussae Conceicao, Neregato et lannuzzi, nov. gen., nov. sp., characterized by solenoid, lobed and non-septate heterocellular pith, cauline bundles with endarch maturation, and secondary xylem with araucarian radial pitting on the tracheid walls. The other form is assigned to the genus Kaokoxylon, which has been recorded from most of Gondwana, including the Parnaiba Basin, but is recorded for the first time from the Pedra de Fogo Formation with the new species Kaokoxylon brasiliensis. It is characterized by solid, non-septate heterocellular pith with sclerenchyma cells, endarch cauline bundles, and uni-to triseriate radial pitting on the walls of the tracheids. The sedimentological interpretations of the outcrops where the fossils were collected indicate that these plants lived on the shores of large continental lakes, with relatively high humidity but possibly periods of drought. These inferences are supported by growth interruptions in the secondary xylem, the presence of calamitalean and tree-fern stems, and microbialites that crop in the same area. These new finds not only increase the known diversity of the flora in the Pedra de Fogo Formation, but also provide more accurate information for understanding the floristic elements that formed the subtropical flora during the Cisuralian in this basin in Western Gondwana. (C) 2020 Elsevier Masson SAS. All rights reserved.	[da Conceicao, Domingas Maria; Neregato, Rodrigo; Iannuzzi, Roberto] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Programa Posgrad Geociencias, Caixa Postal 15-001, BR-91509900 Porto Alegre, RS, Brazil; [de Andrade, Luiz Saturnino] Univ Fed Para, Inst Geociencias, Rua Augusto Correa 1, BR-66075110 Belem, Para, Brazil; [Crisafulli, Alexandra] Univ Nacl Nordeste, Fac Ciencias Exactas & Nat & Agrimensura, Ruta 5,Km 2,5, RA-3400 Corrientes, Argentina; [Crisafulli, Alexandra] CECOAL CONICET, Ruta 5,Km 2,5, RA-3400 Corrientes, Argentina; [Cisneros, Juan Carlos] Univ Fed Piaui, Museu Arqueol & Paleontol, BR-64049550 Teresina, PI, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Para; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidade Federal do Piaui	da Conceicao, DM (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Programa Posgrad Geociencias, Caixa Postal 15-001, BR-91509900 Porto Alegre, RS, Brazil.	domingas.paleonto@gmail.com	Cisneros, Juan C/A-5258-2008; Iannuzzi, Roberto/G-3641-2012	Iannuzzi, Roberto/0000-0003-1432-8106; da Conceicao, Domingas Maria/0000-0003-2917-0065; Andrade, Luiz/0000-0001-7168-8787; Crisafulli, Alexandra Maria Cristina/0000-0001-5078-3355; Cisneros, Juan Carlos/0000-0001-6159-1981	Brazilian funding agency: National Council of Technological and Scientific Development (CNPq) [141248/2016-5, 401848.2010-8, 456608/2014-1, PQ312747/2017-9]; Field Museum of Natural History - Negaunee Foundation, USA	Brazilian funding agency: National Council of Technological and Scientific Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Field Museum of Natural History - Negaunee Foundation, USA	This work is part of the first author's PhD Thesis. DMC acknowledges the Brazilian funding agency: National Council of Technological and Scientific Development (CNPq) for financial support for an internship at the Centro de Ecologia Aplicada del Litoral (CECOAL), Corrientes, Argentina, through a PhD scholarship (141248/2016-5), and for grants to J. Cisneros (401848.2010-8 and to R. Iannuzzi 456608/2014-1, PQ312747/2017-9). The authors are indebted to Ken Angielczyk (Field Museum of Natural History) for partial financial support of field studies granted by The Negaunee Foundation, USA. We also acknowledge Renata L. S. Quaresma for logistical help during the fieldwork, which was of fundamental importance in obtaining the material studied here. We acknowledge the anonymous reviewers for valuable suggestions that improved this study.	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J	da Costa, EO; Gomes, EM; Bitencourt, MD; De Toni, GB; Nardi, LVS				da Costa, Elisa Oliveira; Gomes, Eduarda Medeiros; Bitencourt, Maria de Fatima; De Toni, Giuseppe Betino; Stoll Nardi, Lauro Valentim			Reassessing the PT conditions of Neoproterozoic collisional metamorphism and partial melting in southernmost Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Migmatite; Geothermobarometry; Hot orogen; Dom Feliciano belt; Brasiliano cycle	DOM FELICIANO BELT; U-PB; TECTONIC EVOLUTION; CAPIVARITA COMPLEX; PELOTAS BATHOLITH; FELSIC GRANULITES; VARZEA; GRANITE; CONSTRAINTS; EQUILIBRIA	Partially equilibrated textures and partial melting products are key features in the study of high-grade metamorphic complexes, but their complexity limits the advancement of knowledge about the tectono-thermal history of ancient orogens. This difficulty is apparent in the wide interval of conditions (720-1000 degrees C/3-10 kbar) determined by previous studies in a high-grade complex formed during the amalgamation of West Gondwana in southernmost Brazil. In order to understand the orogen, we reanalyse the metamorphic evolution of the Varzea do Capivarita Complex through field data, petrography, whole-rock and mineral chemistry, and thermodynamic modelling. Peak metamorphic conditions (M-1) are constrained with diverse mineral assemblages (Bt-Crd-Sil-Grt-Ilm/Bt-Sil-Grt-Ilm/Bt-Grt-Ilm) and overlap at 800 degrees C/4.5 kbar, while the partially equilibrated domain (Crd-Hc-Sil) indicates post-peak conditions (M-2) of 680 degrees C/2.8 kbar. Models predict leucosome volume up to 20%, in agreement with field and petrographic estimates, attesting the migmatitic character. Leucogranitic veins correlating petrographically and compositionally with leucosome and melt estimates reinforce this character and the thermodynamic modelling, even with low correlations, which are explained by inherited minerals. Thus, M-1 and M-2 conditions indicate exhumation from depth of 16 to 10 km and high geothermal gradient, which are interpreted as due to anomalous mantle heat flow and rapid exhumation facilitated by large volumes of melt.	[da Costa, Elisa Oliveira; Gomes, Eduarda Medeiros; Bitencourt, Maria de Fatima; De Toni, Giuseppe Betino; Stoll Nardi, Lauro Valentim] Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias IGEO, Programa Posgrad Geociencias PPGGEO, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	da Costa, EO (autor correspondente), Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias IGEO, Programa Posgrad Geociencias PPGGEO, Porto Alegre, RS, Brazil.	elisa.oliveira@ufrgs.br; eduarda.gomes@ufrgs.br; fatimab@ufrgs.br; gdetoni@ufrgs.br; lauro.nardi@ufrgs.br	Bitencourt, Maria de Fátima/GLR-8862-2022; de Fátima Bitencourt, Maria/H-8957-2016	Bitencourt, Maria de Fátima/0000-0001-7022-9175; de Fátima Bitencourt, Maria/0000-0001-7022-9175; Medeiros Gomes, Eduarda/0000-0002-4359-3681; Oliveira da Costa, Elisa/0000-0001-8478-6255	Instituto de Geociencias, Universidade Federal do Rio Grande do Sul (UFRGS); Conselho Nacional do Desenvolvimento Cientifico e Tecnologico; Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul	Instituto de Geociencias, Universidade Federal do Rio Grande do Sul (UFRGS); Conselho Nacional do Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS))	Financial support from 'Instituto de Geociencias, Universidade Federal do Rio Grande do Sul (UFRGS)' for the BSc senior theses of E.O.C. and E.M.G. is appreciated; and both acknowledge scholarships from Conselho Nacional do Desenvolvimento Cientifico e Tecnologico and Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul. We thank Marcia Boscatto Gomes and Suzan Drago from the Electron Microprobe Laboratory for their efficiency in mineral chemistry and quantitative compositional maps, and also Jiri Konopasek for the teaching, discussions and help with thermodynamic modelling. JSAES reviewers and editor are acknowledged.	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South Am. Earth Sci.	JUN	2020	100								102584	10.1016/j.jsames.2020.102584	http://dx.doi.org/10.1016/j.jsames.2020.102584			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900035
J	da Silva, JB; Abreu, IM; de Oliveira, DAF; Hadlich, GM; Barbosa, ACRDA				da Silva Junior, Jucelino Balbino; Abreu, Ilene Matano; Francisco de Oliveira, Daiane Aparecida; Hadlich, Gisele Mara; Rizzatti de Albergaria Barbosa, Ana Cecilia			Combining geochemical and chemometric tools to assess the environmental impact of potentially toxic elements in surface sediment samples from an urban river	MARINE POLLUTION BULLETIN			English	Article						Exploratory analysis; Geochemical index; Heavy metals; Sediment; Tropical river	OS SANTOS BAY; RISK-ASSESSMENT; HEAVY-METALS; WATER; CONTAMINATION; LEAD; LAKE; SOIL; PB	This article investigates sediments collected from the banks of the Subae River located in Todos os Santos Bay in the state of Bahia, Brazil, in 2018, twenty-five years after the closing of a former lead alloy processing plant. Ten sediment samples were collected at different points of the course of the river and its estuarine region. Chemometric tools were used to determine geochemical correlations between the organic matter content and concentration of sulfides and potentially toxic metals. The inorganic geochemical variables (enrichment factor [EF]) used in this evaluation were concentrations of the Pb, Cd, Cu, Zn, and Ni. Chemical element analyses were performed using ICP-OES. To assess the interaction between metals and sulfide or metals and organic matter, concentrations of Pb, Cd, Cu, Zn, Ni, sulfide, and the silt-clay fraction constituted the organic geochemical parameters selected to characterize the amount of organic matter present in Subae River sediment samples, determining the carbon content (%TOC) to compose the matrix of the principal component analysis (PCA) and hierarchical cluster analysis. PCA showed that 88.3% of the samples were representative for assessing correlations between geochemical variables. A tendency toward binding was found among Cu, Cd, Ni, and sulfide, as well as the silt-clay fraction. The concentrations (mg kg(-1)) of lead, zinc, and copper were higher in both collection campaigns, ranging from 4.72 to 31.34, 12.76 to 54.24, and 5.34 to 31.37, respectively. Pb and Zn were presented in elemental form when assessed as a function of the pH and Eh of the environment. Except for Cd (EF: 0.51 to 5.49), the other elements exhibited little or no potential pollution in the aquatic environment of the Subae River.	[da Silva Junior, Jucelino Balbino; Abreu, Ilene Matano; Francisco de Oliveira, Daiane Aparecida; Hadlich, Gisele Mara; Rizzatti de Albergaria Barbosa, Ana Cecilia] Fed Univ Bahia UFBA, Postgrad Program Geochem Petr & Environm POSPETRO, Geosci Inst, Rua Barao Jeremoabo,S-N, BR-40170020 Salvador, BA, Brazil; [da Silva Junior, Jucelino Balbino; Abreu, Ilene Matano] Fed Univ Bahia UFBA, LEPETRO, Geosci Inst, Excellence Geochem Petr Energy & Environm, Rua Barao Jeremoabo,S-N, BR-40170020 Salvador, BA, Brazil		da Silva, JB (autor correspondente), Fed Univ Bahia UFBA, Postgrad Program Geochem Petr & Environm POSPETRO, Geosci Inst, Rua Barao Jeremoabo,S-N, BR-40170020 Salvador, BA, Brazil.	jucejr@ufba.br	Abreu, Ilene Matanó/AAB-6052-2021; de+Albergaria+Barbosa, Ana/AAQ-3872-2020; de Albergaria-Barbosa, Ana Cecília/AAC-6940-2021; Hadlich, Gisele/AAO-4708-2020; da Silva, Jucelino Balbino/AAA-3611-2021	Albergaria-Barbosa, Ana Cecilia R./0000-0003-2121-9792; Hadlich, Gisele Mara/0000-0002-6304-0988	Brazilian fostering agency Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES [Coordination for the Advancement of Higher Education Personnel]) [001]; CAPES [PNPD 2311/2011]	Brazilian fostering agency Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES [Coordination for the Advancement of Higher Education Personnel]); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work was developed at the Postgraduate Program in Geochemistry: Oil and Environment of the Federal University of Bahia (UFBA) and received funding from the Brazilian fostering agency Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES [Coordination for the Advancement of Higher Education Personnel] financial code 001). Silva Junior would like to thank CAPES for the postdoctoral fellowship (PNPD 2311/2011). The study was developed in partnership with LEPETRO of the Geosciences Institute of the Federal University of Bahia (IGEO/UFBA).	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Pollut. Bull.	JUN	2020	155								111146	10.1016/j.marpolbul.2020.111146	http://dx.doi.org/10.1016/j.marpolbul.2020.111146			7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	LS1XK	32469770				2023-06-23	WOS:000536184300025
J	Ferreira, SCG; de Lima, AMM; Correa, JAM				Gomes Ferreira, Susane Cristini; Meiguins de Lima, Aline Maria; Martins Correa, Jose Augusto			Indicators of hydrological sustainability, governance and water resource regulation in the Moju river basin (PA) - Eastern Amazonia	JOURNAL OF ENVIRONMENTAL MANAGEMENT			English	Article						Hydrological demand; Water availability; Environmental management; Payments for water use	CLIMATE	Water is one of the natural resources most impacted by the development model adopted in Brazil. This is related to the widespread sense that water is abundant in the country, which makes it difficult to fully engage all levels of government. However, this sense of abundance also obscures the real problems of pollution, demand, availability and water resources conflicts. This study aims to strengthen water management and contribute to the evaluation of the processes of development in the northeast region of the state of Para. This study uses Hydrographic Basin Sustainability Indices to consider the hydrological, environmental, social and water resources management situation of the Moju River Basin and to suggest a payment model for the use of its water resources. The results indicate that the existing framework of water use regulation is characterized by moderate sustainability and governance scores and a low degree of collection of fees for the use of water. In general, with the increase in the number of enterprises authorized to withdraw water from and release effluents into the river, there is a lack of information about water demand and availability. The water governance framework is characterized by poorly integrated environmental and water management common to most Amazonian municipalities. Thus, the Moju River Basin represents a pattern of unsatisfactory water resources management. This pattern highlights the importance of implementing existing water resources and environmental policies to reduce conflicts that involve land and water use.	[Gomes Ferreira, Susane Cristini] Fed Univ Para, Belem, Para, Brazil; [Gomes Ferreira, Susane Cristini] Conselho Nacl Desenvolvimento Cient & Tecnol CNPq, Natl Council Sci & Technol Dev, Brasilia, Brazil; [Meiguins de Lima, Aline Maria; Martins Correa, Jose Augusto] Fed Univ Para, Geosci Inst, Belem, Para, Brazil	Universidade Federal do Para; Universidade Federal do Para	Ferreira, SCG (autor correspondente), Fed Univ Para, Belem, Para, Brazil.	susane_cristini@hotmail.com	DE LIMA, ALINE MARIA MEIGUINS/AAF-8346-2021; Correa, José Augusto/HGC-3705-2022; Lima, Aline/AAF-8337-2021		Coordination for the Improvement of Higher Education Personnel (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, CAPES) of Brazil [001]	Coordination for the Improvement of Higher Education Personnel (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, CAPES) of Brazil	This study was funded in part by the Coordination for the Improvement of Higher Education Personnel (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior, CAPES) of Brazil under Finance Code 001.	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JUN 1	2020	263								110354	10.1016/j.jenvman.2020.110354	http://dx.doi.org/10.1016/j.jenvman.2020.110354			10	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	LJ5VK	32174519				2023-06-23	WOS:000530232700010
J	Lopes, RP; Pereira, JC; Dillenburg, SR; Tatumi, SH; Yee, M; Figueiredo, AMG; Kinoshita, A; Baffa, O				Lopes, Renato Pereira; Pereira, Jamil Correa; Dillenburg, Sergio Rebello; Tatumi, Sonia Hatsue; Yee, Marcio; Graciano Figueiredo, Ana Maria; Kinoshita, Angela; Baffa, Oswaldo			Late Pleistocene-Holocene fossils from Mirim Lake, Southern Brazil, and their paleoenvironmental significance: I - Vertebrates	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Quaternary; Pleistocene; Mirim lake; Paleoenvironment; Vertebrate paleontology; Geomorphology	GRANDE-DO-SUL; WHALES EUBALAENA-AUSTRALIS; COASTAL-PLAIN; CARCHARHINUS-LEUCAS; BULL SHARK; PATOS LAGOON; MAMMALS; STATE; LUMINESCENCE; QUATERNARY	Mirim Lake is located in the southern Brazilian/northeastern Urugayan coastal plain. Fossils of mollusks have been discovered on its shores since the XIX century, and in recent years, several new remains of invertebrates and vertebrates have been found in the Brazilian area of the lake that provide insights on the geological evolution and environmental changes that affected this lake during the late Quaternary. In this first of two papers describing these new findings we focus on vertebrates, consisting of aquatic and terrestrial taxa. The former include the first associated fossil remains of one adult and one juvenile balaenid whale known in Brazil, probably a female and calf of the southern right whale (baleia-franca) Eubalaena australis, besides bull sharks (Carcharhinus leucas) also recorded for the first time in southern Brazil, rays (Dasyatidae and Myliobatidae) and teleost fishes. The fossils of terrestrial vertebrates include several extinct mammals, found on the margins and retrieved from the lake bottom by fishermen at depths of up to 4 m. One molar tooth of Toxodon discovered in situ in one irrigation channel yielded an electron spin resonance (ESR) age of 68 +/- 13 ka, in agreement with an age of 32.8 +/- 5.1 ka obtained in quartz grains extracted from a caliche nodule collected above that fossil and dated by optically-stimulated luminescence (OSL). Other quartz grains in the same nodule that yielded ages of 16.9 +/- 2.5 ka indicate partial dissolution of the caliche by increased rainfall at the beginning of the last glacial-interglacial transition (Termination I) . The lake was invaded by marine waters and organisms during the Holocene sea-level highstand of +3 m around 5-6 ka b2k through paleo-connections with the Atlantic Ocean, becoming a paleo-lagoon. At that time coastal waters were warmer than today, as indicated by the presence of the tropical shark C. leucas. The ESR and OSL ages indicate chronocorrelation with the Pleistocene fossil-bearing Santa Vitoria Formation that outcrops to the east. The fossil and sedimentary records indicate that the geological evolution and environmental conditions of the lake were controlled by climate and sea-level oscillations related to glacial-interglacial cycles.	[Lopes, Renato Pereira; Dillenburg, Sergio Rebello] Univ Fed Rio Grande do Sul, Inst Geociencias, Agron, Ave Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil; [Pereira, Jamil Correa] Museu Coronel Tancredo Fernandes de Melo, Rua Barao do Rio Branco 467, BR-96230000 Santa Vitoria Do Palmar, RS, Brazil; [Tatumi, Sonia Hatsue; Yee, Marcio] Univ Fed Sao Paulo, UNIFESP, Campus Baixada Santista, BR-11015020 Sao Paulo, SP, Brazil; [Graciano Figueiredo, Ana Maria] Inst Pesquisas Energet & Nucl IPEN, Ave Lineu Prestes 2242,Cidade Univ, BR-05508000 Sao Paulo, SP, Brazil; [Kinoshita, Angela] Univ Sagrad Coracao USC, PRPPG, Rua Irma Arminda 10-50,Campus Univ, BR-17011160 Bauru, SP, Brazil; [Kinoshita, Angela] Univ Oeste Paulista UNOESTE, Rodovia SP-270,Km 572,Campus 2, BR-19067175 Presidente Prudente, SP, Brazil; [Baffa, Oswaldo] Univ Sao Paulo FFCLRP USP, Dept Fis, Fac Filosofia Ciencias & Letras Ribeirao Preto, Ave Bandeirantes 3900, BR-14040901 Ribeirao Preto, SP, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal de Sao Paulo (UNIFESP); Comissao Nacional de Energia Nuclear (CNEN); Instituto de Pesquisas Energeticas e Nucleares (IPEN); Universidade do Oeste Paulista	Lopes, RP (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil.	paleonto_furg@yahoo.com.br; jcorreapereira@bol.com.br; sergio.dillenburg@ufrgs.br; sonia.tatumi@gmail.com; marcioyee@hotmail.com; anamaria@ipen.br; angelamitie@gmail.com; baffa@usp.br	Yee, Marcio/N-9944-2013; Kinoshita, Angela/C-6946-2012; Lopes, Renato Pereira/AFQ-4934-2022; Figueiredo, Ana/GWU-6748-2022; Dillenburg, Sergio/C-4027-2013	Kinoshita, Angela/0000-0002-5057-1667; Lopes, Renato Pereira/0000-0002-4865-6426; Yee, Marcio/0000-0002-7639-7265; Tatumi, Sonia Hatsue/0000-0002-4990-4444; Dillenburg, Sergio/0000-0003-0072-7018	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [150153/2014-7]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to express their gratitude for the people who found and donated the fossils described here to the museum Coronel Tancredo Fernandes de Mello: Edmilson Pereira (antler PV1003), Eranio dos Santos Rodrigues (antler PV1006), Gilson Borges Moreno (antler 1102), Jaime Renato Silveira do Amaral (molar PV0435) Jandira Correa Borges (vertebrae PV1206, 1207 and 1208), Maicon Machado Souza (osteoderm PV1181 and phalanx 1182), Neurimar Borba Muniz (pterygiophore PV0457) and Oldemar Borges Moreno (femur PV0981). Thanks also to Dr. Pascal P. Deynat (ODONTOBASE Project) for the information and discussion on dermal structures of rays, and Dr. Gerardo De Iuliis (University of Toronto) for comments on the anatomy of the megatheriid femur. This research was funded by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) through the Postdoctoral Research Grant no. 150153/2014-7 to the first author.	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JUN	2020	100								102566	10.1016/j.jsames.2020.102566	http://dx.doi.org/10.1016/j.jsames.2020.102566			19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900029
J	Marimon, RS; Trouw, RAJ; Dantas, EL; Ribeiro, A				Marimon, Rodrigo Schwantes; Johannes Trouw, Rudolph Allard; Dantas, Elton Luiz; Ribeiro, Andre			U-Pb and Lu-Hf isotope systematics on detrital zircon from the southern Sao Francisco Craton's Neoproterozoic passive margin: Tectonic implications	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Detrital zircon; U-Pb and Lu-Hf geochronology; Passive margin; Provenance; Sao Francisco Craton; Congo Craton	KUNENE ANORTHOSITE COMPLEX; ANDRELANDIA NAPPE SYSTEM; PLASMA-MASS SPECTROMETRY; CRUST GENERATION EVENTS; SOCORRO-GUAXUPE NAPPE; CENTRAL RIBEIRA BELT; NORTH CHINA CRATON; JOAO-DEL-REI; SE BRAZIL; BRASILIA OROGEN	Isotopic Lu-Hf and U-Pb systematics can provide important insights into the tectono-metamorphic processes that occurred in the source regions of sedimentary/metasedimentary units, helping to further clarify regional crustal evolution. The studied metasedimentary sequence is located in the southern Brasilia Orogen, SE Brazil, a foldand-thrust belt composed of a thick nappe stack transported towards the southern Sao Francisco Craton (SFC) during the Neoproterozoic. Adjacent to the Cratonic border is a reworked Neoproterozoic metasedimentary passive margin sequence, that includes the Carrancas succession, for which we present new U-Pb and Lu-Hf detrital zircon analyses (ca. 700 grains in total). Results yielded a maximum depositional age of 0.988 +/- 0.013 Ga and an extensional tectonic setting for the precursor basin. Major source areas, constrained by comparing our data to isotopic analyses compiled from the existing literature, are probably located in the adjacent southern SFC. Lu-Hf analyses of Paleoproterozoic and Archean zircon grains, presented in this study, yielded similar results to those obtained for the basement of the SFC. However, important U-Pb age peaks found in this study do not have strong correlatives in the southern SFC (e.g. 1.84,1.87 and 1.88 Ga), with the exception of a few localized examples (e.g. Espinhaco I magmatism). These ages are abundant in the southwestern Congo Craton (CC), which was potentially relatively close to the studied area during sedimentation, since the SFC and CC probably constituted a single continental mass after the Paleoproterozoic until the opening of the south Atlantic in the Mesozoic.	[Marimon, Rodrigo Schwantes; Johannes Trouw, Rudolph Allard; Ribeiro, Andre] Univ Fed Rio de Janeiro, Inst Geociencias, BR-21949900 Rio De Janeiro, RJ, Brazil; [Dantas, Elton Luiz] Univ Brasilia, Lab Estudos Geodinam & Ambientais, BR-70297400 Brasilia, DF, Brazil	Universidade Federal do Rio de Janeiro; Universidade de Brasilia	Marimon, RS (autor correspondente), Univ Fed Rio de Janeiro, Inst Geociencias, BR-21949900 Rio De Janeiro, RJ, Brazil.	rsmarimon@hotmail.com	Marimon, Rodrigo Schwantes/AAB-5863-2021; Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059; Schwantes Marimon, Rodrigo/0000-0001-6157-8031	CAPES; National Council for Scientific and Technological Development (CNPq)	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	R.S. Marimon acknowledges a PhD scholarship provided by CAPES. R.A.J Trouw thanks the National Council for Scientific and Technological Development (CNPq) for financial support. The authors acknowledge the staff from the Geochronology Laboratory, University of Brasilia (UnB), especially B. Lima and E. Zacchi; and Prof. Natalia Hauser for excellent suggestions regarding data reduction. Careful editorial handling by A. Folguera and excellent suggestions by Sebastian Oriolo and an anonymous reviewer are greatly acknowledged.	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JUN	2020	100								102539	10.1016/j.jsames.2020.102539	http://dx.doi.org/10.1016/j.jsames.2020.102539			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900004
J	Martins, CMS; Cerqueira, JR; Ribeiro, HJPS; Garcia, KS; da Silva, NN; Queiroz, AFD				Martins, Cintia Mayra S.; Cerqueira, Jose Roberto; Ribeiro, Helio Jorge P. S.; Garcia, Karina S.; da Silva, Neiva N.; Queiroz, Antonio Fernando de S.			Evaluation of thermal effects of intrusive rocks on the kerogen present in the black shales of Irati Formation (Permian), Parana Basin, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Irati Formation; Igneous intrusion; Biomarkers; Thermal maturity; Depositional paleoenvironment; Organic matter	ORGANIC-MATTER; CONTACT-METAMORPHISM; PETROLEUM SYSTEMS; NEUQUEN BASIN; TETRACYCLIC POLYPRENOIDS; IGNEOUS INTRUSIONS; GENERATION; GEOCHEMISTRY; HYDROCARBONS; CONSTRAINTS	Shale samples from outcrops of the Irati Formation (Permian), Parana Basin, Brazil were analyzed based on organic geochemistry, palynofacies, and stable carbon isotopes with the aim of evaluating thermal effects of igneous intrusions on the kerogen. The potential for hydrocarbon generation, the depositional paleoenvironment, and the input of the organic matter were also studied. Most samples have high total organic carbon content, excellent hydrocarbon source potential, and type I kerogen, except some samples which showed changes in their compositional characteristic due alteration in the depositional paleoenvironment and due to the high maturation caused by the heat of diabase intrusions. The composition and distribution of saturate and aromatic biomarkers and stable carbon isotopes provided evidence that the composition of organic matter in the shales is marine, except at the upper part of the outcrops where the shales have contribution of terrestrial organic matter. Saturate biomarkers results indicated thermal immaturity for hydrocarbon generation, except the samples that were influenced by the heat of intrusive rocks.	[Martins, Cintia Mayra S.; Cerqueira, Jose Roberto; Garcia, Karina S.; da Silva, Neiva N.; Queiroz, Antonio Fernando de S.] Fed Univ Bahia UFBA, Inst Geosci, Grad Program Geochem Petr & Environm POSPETRO, Campus Ondina, BR-40170290 Salvador, BA, Brazil; [Ribeiro, Helio Jorge P. S.] Darcy Ribeiro North Fluminense State Univ UENF, BR-27930000 Macae, RJ, Brazil		Martins, CMS (autor correspondente), Fed Univ Bahia UFBA, Inst Geosci, Grad Program Geochem Petr & Environm POSPETRO, Campus Ondina, BR-40170290 Salvador, BA, Brazil.	cintiamayra7@gmail.com; jrkcerq@gmail.com; severiano.geologo@gmail.com; karina.ksg4@gmail.com; neiva.nasc5@gmail.com; afsqueiroz.ufba@gmail.com	Queiroz, Antonio Fernando de Souza/ABH-6682-2020; Cerqueira, José Roberto/AAY-9852-2021		Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com Pesquisa e Desenvolvimento" [20075-8]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com Pesquisa e Desenvolvimento"; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This research was carried out in association with the ongoing R&D project registered as ANP No20075-8, "Project Petroleum Systems Research in Brazilian Sedimentary Basins" (UFBA/Shell Brasil/ANP) - ANP project title (Pesquisas em Sistemas Petroliferos de Bacias Sedimentares Brasileiras), sponsored by Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com Pesquisa e Desenvolvimento" and financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001.	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South Am. Earth Sci.	JUN	2020	100								102559	10.1016/j.jsames.2020.102559	http://dx.doi.org/10.1016/j.jsames.2020.102559			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900023
J	Leite, CDN; Silva, CMD; De Ros, LF				Nardi Leite, Caroline De Oliveira; De Assis Silva, Carlos Manuel; De Ros, Luiz Fernando			DEPOSITIONAL AND DIAGENETIC PROCESSES IN THE PRE-SALT RIFT SECTION OF A SANTOS BASIN AREA, SE BRAZIL	JOURNAL OF SEDIMENTARY RESEARCH			English	Article							LACUSTRINE CARBONATE RESERVOIRS; NORTHERN CAMPOS BASIN; GREEN RIVER FORMATION; SULFATE REDUCTION; OFFSHORE BRAZIL; AMARGOSA DESERT; SANDSTONES; ORIGIN; PYRITE; STEVENSITE	This study aims to provide a better understanding of the genesis and diagenetic evolution of the rift pre-salt deposits of the Santos Basin, in the context of evolution of the lake system in which the sediments were deposited. The study of the syngenetic and early diagenetic constituents and their paragenetic relations allowed reconstruction of the evolution of lacustrinc environmental conditions during the rift stage in the central area of the basin. A petrological study was performed on cores and sidewall samples of a well drilled through the pre-salt rift section in the Lower Cretaceous of the central Santos Basin, eastern Brazilian coast. The studied rocks consist of carbonate and non-carbonate intrabasinal components, with extrabasinal non-carbonate contribution. During Barremian early rift sedimentation, intense syngenetic precipitation of magnesian clay minerals under highly alkaline conditions deposited arenites constituted by stevensite ooids and pcloids, as well as hybrid, resedimented deposits of the Picarras Formation. Freshening of the lacustrine environment provided the conditions required for the proliferation of bivalves and sedimentation of the coquinas of the Itapema Formation. The massive structure of the deposits, poor sorting, chaotic to concave-up orientation of the bioclasts, and mixing of bivalves with stevensite particles indicate redeposition by gravity flows. The main diagenetic processes in rift stevensite and hybrid rocks arc the cementation and replacement of grains by calcite, dolomite, and subordinately, silica and smectite. Siliciclastic-volcaniclastic mudrocks present intense replacement by dolomite. In the bivalve rudstones, the main diagenetic processes were dissolution of the shells and cementation of the intraparticle and interparticle pores by calcite and, subordinately, dolomite and silica.	[Nardi Leite, Caroline De Oliveira; De Assis Silva, Carlos Manuel] Petrobras Res Ctr, Ave Horacio Macedo,950,Cidade Univ, Rio De Janeiro, RJ, Brazil; [De Ros, Luiz Fernando] Rio Grande Sul Fed Univ, Geosci Inst, Porto Alegre, RS, Brazil	Petrobras	Leite, CDN (autor correspondente), Petrobras Res Ctr, Ave Horacio Macedo,950,Cidade Univ, Rio De Janeiro, RJ, Brazil.		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Sediment. Res.	JUN	2020	90	6					584	608		10.2110/jsr.2020.27	http://dx.doi.org/10.2110/jsr.2020.27			25	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MO6PY					2023-06-23	WOS:000551646500003
J	Nina, LM; Sial, AN; Barbosa, A; Neumann, VHM; Bark, G; Garcia, R; Wanhainen, C; Blanco, M				Nina, L. M.; Sial, A. N.; Barbosa, A.; Neumann, V. H. M.; Bark, G.; Garcia, R.; Wanhainen, C.; Blanco, M.			Diagenesis of the Pennsylvanian -Lower Permian Copacabana Formation, western Bolivian Altiplano	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						C isotope; O isotope; Titicaca sub-basin; Late paleozoic limestone	CARBONATE DIAGENESIS; ISOTOPE; SEAWATER; SECTION; RECORD; OXYGEN; SR	This contribution presents the diagenetic evolution of limestone deposits in the Copacabana Formation that occurs in the northern Altiplano, in the Lake Titicaca area of western Bolivia. The best-exposed stratigraphic succession of the Copacabana Formation occurs in the Yampupata section, and its division into five facies successions is based on petrographic analysis, cathodoluminescence, x-ray fluorescence analysis (chemical composition) and stable isotope data (delta O-18 and delta C-13). The results showed that the carbonate rocks experienced early marine diagenetic processes such as micritization during or after the deposition (eogenesis). The initial burial event (mesogenesis 1), characterized by stabilization of temperature-water carbonates by freshwater, and represented by bladed calcite-cement, equant calcite cement, dissolution, dolomitization, neomorphism, silicification and compaction (physical), occurred in shallow burial conditions. During the second burial episode (mesogenesis 2), in deeper burial environment the processes include: compaction (physical and chemical) and neomorphism. Diagenetic processes have affected reservoir quality in the Copacabana Formation during the mesodiagenesis, and reduced the conditions for development of high-quality conventional hydrocarbon reservoirs. Depleted O and C stable isotope signatures indicate that these carbonate rocks deposits underwent both meteoric and burial diagenesis including moderate water-rock interaction.	[Nina, L. M.; Bark, G.; Wanhainen, C.] Lulea Univ Technol, Div Geosci & Environm Engn, S-97187 Lulea, Sweden; [Sial, A. N.; Barbosa, A.; Neumann, V. H. M.] Univ Fed Pernambuco, NEG LABISE, Dept Geol, Recife, PE, Brazil; [Nina, L. M.; Garcia, R.; Blanco, M.] Mayor San Andres Univ, Inst Geol Res & Environm, Geol Sci Fac, La Paz 14500, Bolivia	Lulea University of Technology; Universidade Federal de Pernambuco	Nina, LM (autor correspondente), Lulea Univ Technol, Div Geosci & Environm Engn, S-97187 Lulea, Sweden.	Lidia.Nina@ltu.se	BARBOSA, JOSE ANTONIO/AAB-4437-2020; Sial, Alcides/AAD-1901-2021	BARBOSA, JOSE ANTONIO/0000-0001-8754-6310; Bark, Glenn/0000-0001-9846-1793	Swedish Development Agency (SIDA)	Swedish Development Agency (SIDA)	We thank Dr. Alcides N. Sial of the Laboratorio Nucleo de Estudos Geoquimicos-Labotatorio de Isotopos Estaveis (NEG-LABISE), Dept. of Geology, Federal University of Pernambuco, Recife, PE, Brazil. This study was supported by the Swedish Development Agency (SIDA). We express our gratitude to the Institute of Geology and Environment (IGEMA).	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South Am. Earth Sci.	JUN	2020	100								102540	10.1016/j.jsames.2020.102540	http://dx.doi.org/10.1016/j.jsames.2020.102540			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900005
J	Orue-Echevarria, D; Pelegri, J; Castellanos, P; Guallar, C; Marotta, H; Marrase, C; Martin, J; Masdeu-Navarro, M; Paniagua, GF; Pena-Izquierdo, J; Puigdefabregas, J; Rodriguez-Fonseca, B; Roget, E; Rosell-Fieschi, M; Salat, J; Salvador, J; Valles-Casanova, I; Vidal, M; Viudez, A				Orue-Echevarria, Dorleta; Pelegri, JosepL.; Castellanos, Paola; Guallar, Carles; Marotta, Humberto; Marrase, Celia; Martin, Jacobo; Masdeu-Navarro, Marta; Paniagua, Guillermina F.; Pena-Izquierdo, Jesus; Puigdefabregas, Joan; Rodriguez-Fonseca, Belen; Roget, Elena; Rosell-Fieschi, Miquel; Salat, Jordi; Salvador, Joaquin; Valles-Casanova, Ignasi; Vidal, Montserrat; Viudez, Alvaro			Dataset on the RETRO-BMC cruise onboard the R/V Hesperides, April 2017, Brazil-Malvinas Confluence	DATA IN BRIEF			English	Article; Data Paper						Brazil-Malvinas Confluence; Hydrographic data; SeaSoar data; Microstructure data		This dataset, gathered during the RETRO-BMC cruise, reports multiple-scale measurements at the Confluence of the Brazil and Malvinas Currents. The cruise was carried out between 8 and 28 April 2017 onboard R/V Hesperides, departing from Ushuaia and arriving to Santos. Along its track, the vessel recorded near-surface temperature and salinity, as well as the horizontal flow from 20 m down to about 800 m. A total of 33 hydrographic stations were completed in a region off the Patagonian Shelf, within 41.2 degrees S-35.9 degrees S and out to 53.0 degrees W. At each station, a multiparametric probe and velocity sensors were deployed inside the frame of a rosette used to collect water samples at selected depths; these samples were later used for several water analyses, including inorganic nutrient concentrations. Microstructure measurements were carried out in 11 of these hydrographic stations. In addition, two high-resolution three-dimensional surveys were conducted with an instrumented undulating vehicle between 40.6 degrees S-39.0 degrees S and 55.6 degrees W-53.8 degrees W. Lastly, eight high-frequency vertical profilers were deployed in the region and five position-transmitting drifters were launched. These data allow the description of the Confluence from the regional scale to the microscale, and provide a view of the variability of the frontal region on time scales from days to weeks. (C) 2020 The Author(s). Published by Elsevier Inc.	[Orue-Echevarria, Dorleta; Pelegri, JosepL.; Castellanos, Paola; Guallar, Carles; Masdeu-Navarro, Marta; Pena-Izquierdo, Jesus; Puigdefabregas, Joan; Rosell-Fieschi, Miquel; Salat, Jordi; Salvador, Joaquin; Valles-Casanova, Ignasi; Viudez, Alvaro] CSIC, Unidad Asociada ULPGC CSIC, Inst Ciencies Mar, Dept Oceanog Fis & Tecnol, Barcelona, Spain; [Castellanos, Paola] Univ Lisbon, Ctr Ciencias Mar & Ambiente, Lisbon, Portugal; [Guallar, Carles; Vidal, Montserrat] Univ Barcelona, Dept Biol Evolut Ecol & Ciencies Ambientals, Barcelona, Spain; [Marotta, Humberto] Univ Fed Fluminense, Biomass & Water Management Res Ctr, Grad Program Geosci Environm Geochem, Ecosyst & Global Change Lab,Int Lab Global Change, Niteroi, RJ, Brazil; [Marrase, Celia; Masdeu-Navarro, Marta] CSIC, Inst Ciencies Mar, Dept Biol Marina & Oceanog, Barcelona, Spain; [Martin, Jacobo] CADIC CONICET, Ushuaia, Argentina; [Paniagua, Guillermina F.] CONICET UBA, CIMA, Ctr Invest Mar & Atmosfera, Buenos Aires, DF, Argentina; [Paniagua, Guillermina F.] CONICET UBA, CNRS, UMI IFAECI, Buenos Aires, DF, Argentina; [Rodriguez-Fonseca, Belen] Univ Complutense Madrid, Dept Fis Tierra Astron & Astrofis, Madrid, Spain; [Roget, Elena] Univ Girona, Dept Fis, Girona, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Universidade de Lisboa; University of Barcelona; Universidade Federal Fluminense; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires; Complutense University of Madrid; Universitat de Girona	Orue-Echevarria, D; Pelegri, J (autor correspondente), CSIC, Unidad Asociada ULPGC CSIC, Inst Ciencies Mar, Dept Oceanog Fis & Tecnol, Barcelona, Spain.	dorleta@icm.csic.es; pelegri@icm.csic.es	Marotta, Humberto/F-9554-2012; Joaquin, Salvador/ABF-7075-2021; Vidal, Montserrat/L-6051-2014; Pelegrí, Josep L/L-5815-2014; Viúdez, Álvaro/A-8201-2008; Martin, Jacobo/F-1388-2011; Pena-Izquierdo, Jesus/L-5851-2015; Marrase, Celia/I-1166-2015; Roget, Elena/C-3689-2009	Marotta, Humberto/0000-0002-2828-6595; Vidal, Montserrat/0000-0002-7878-3290; Pelegrí, Josep L/0000-0003-0661-2190; Viúdez, Álvaro/0000-0001-7862-9835; Martin, Jacobo/0000-0001-8933-7731; Pena-Izquierdo, Jesus/0000-0002-9231-989X; Marrase, Celia/0000-0002-5097-4829; Rosell-Fieschi, Miquel/0000-0003-0247-3517; Roget, Elena/0000-0002-4950-0204; Orue-Echevarria, Dorleta/0000-0002-9459-5126; Castellanos, Paola/0000-0002-2281-5572	Spanish government (Ministerio de Economia and Competitividad through project VA-DE-RETRO) [CTM2014-56987-P]; Spanish government (Ministerio de Ciencia, Innovacion y Universidades through project SAGA) [RTI2018-100844-BC33]; Spanish government (Ministerio de Ciencia, Innovacion y Universidades) [FPU2013-02884, BES-2015-071314]; Portuguese government (Fundacao para a Ciencia e a Tecnologia through project COASTNET) [PINFRA/22128/2016]; Fundação para a Ciência e a Tecnologia [PINFRA/22128/2016] Funding Source: FCT	Spanish government (Ministerio de Economia and Competitividad through project VA-DE-RETRO); Spanish government (Ministerio de Ciencia, Innovacion y Universidades through project SAGA); Spanish government (Ministerio de Ciencia, Innovacion y Universidades); Portuguese government (Fundacao para a Ciencia e a Tecnologia through project COASTNET); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	We are very grateful to the crew, technicians and scientists in the R/V Hesperides for their work during the RETRO-BMC cruise. We thank Fernando Garcia, Mariana Miracca and Rafael Santana for their support during the cruise and Maravillas Abad for the nutrient analysis. This research has been supported by the Spanish government (Ministerio de Economia and Competitividad through project VA-DE-RETRO, CTM2014-56987-P, and Ministerio de Ciencia, Innovacion y Universidades through project SAGA, RTI2018-100844-BC33). Dorleta Orue-Echevarria (FPU2013-02884) and Ignasi Valles-Casanova (BES-2015-071314) have also been funded with PhD scholarships by the Spanish government (Ministerio de Ciencia, Innovacion y Universidades). Paola Castellanos has been partly supported by the Portuguese government (Fundacao para a Ciencia e a Tecnologia through project COASTNET, PINFRA/22128/2016).	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J	Santos, TP; Ballalai, JM; Franco, DR; Oliveira, RR; Lessa, DO; Venancio, IM; Chiessi, CM; Kuhnert, H; Johnstone, H; Albuquerque, ALS				Santos, Thiago P.; Ballalai, Joao M.; Franco, Daniel R.; Oliveira, Romulo R.; Lessa, Douglas O.; Venancio, Igor M.; Chiessi, Cristiano M.; Kuhnert, Henning; Johnstone, Heather; Albuquerque, Ana Luiza S.			Asymmetric response of the subtropical western South Atlantic thermocline to the Dansgaard-Oeschger events of Marine Isotope Stages 5 and 3	QUATERNARY SCIENCE REVIEWS			English	Article						South Atlantic central water; Abrupt millennial-scale events; Bipolar seesaw; Atlantic meridional overturning circulation; Paleoceanography; Climate dynamics	NORTH-ATLANTIC; MILLENNIAL-SCALE; GLACIAL CLIMATE; DEEP-WATER; PLANKTONIC-FORAMINIFERA; CLEANING PROCEDURES; ANTARCTIC ICE; OVERTURNING CIRCULATION; MG/CA PALEOTHERMOMETRY; CHRONOLOGY AICC2012	The last glacial period (116-11.7 ka BP) was an interval characterized by a sequence of abrupt millennial-scale events well documented in Greenland and Antarctica ice-cores. Throughout this period, Greenland cold stadials were accompanied by warm conditions in the thermocline to intermediate waters of the Atlantic Ocean that may have played a role in both the basal melting of ice shelves and the rapid atmospheric warming during the onset of warm interstadials. Climate model simulations indicated an accentuated response of the subtropical western South Atlantic thermocline to the disturbances in the Atlantic circulation. Such works encourage investigations upon thermocline/deep-dwelling planktic foraminifera in this region; however, a study with this aim was not performed. Here we present a paleoceanographic reconstruction from the subtropical western South Atlantic based on the thermocline planktic foraminifera Globorotalia inflata. Our high-resolution delta O-18 record for the last glacial period presents a millennial-scale variability that strongly resembles the structure of the Greenland Dansgaard-Oeschger cycles during Marine Isotope Stage (MIS) 5. During MIS 3, this millennial-scale variability is absent or considerably dampened. Mg/Ca-derived temperature and seawater delta O-18 corrected for ice-volume for the MIS 5 interval demonstrate that the region was warmer and saltier (colder and fresher) during early-glacial stadials (interstadials). Our data suggest a reorganization of the northward heat transport throughout the last glacial, in which regions as far south as 24 degrees S acted as heat reservoirs in periods of weakened Atlantic Meridional Overturning Circulation during MIS 5 but not necessarily (or only marginally) during MIS 3. (C) 2020 Elsevier Ltd. All rights reserved.	[Santos, Thiago P.; Ballalai, Joao M.; Lessa, Douglas O.; Albuquerque, Ana Luiza S.] Univ Fed Fluminense, Programa Geociencias Geoquim, Niteroi, RJ, Brazil; [Franco, Daniel R.; Oliveira, Romulo R.] Observ Nacl, Coordenacao Geofis, Rio De Janeiro, Brazil; [Venancio, Igor M.] Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Cachoeira Paulista, Brazil; [Chiessi, Cristiano M.] Univ Sao Paulo, Escola Artes Ciencias & Humanidades, Sao Paulo, Brazil; [Kuhnert, Henning; Johnstone, Heather] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany	Universidade Federal Fluminense; Instituto Nacional de Pesquisas Espaciais (INPE); Universidade de Sao Paulo; University of Bremen	Santos, TP (autor correspondente), Univ Fed Fluminense, Programa Geociencias Geoquim, Niteroi, RJ, Brazil.	thiagopds@id.uff.br	Venancio, Igor M/I-5893-2014; Franco, Daniel R/J-8724-2012; Santos, Thiago P./AAN-6506-2021; Albuquerque, Ana Luiza S/C-5167-2013; Chiessi, Cristiano Mazur/E-1916-2012	Venancio, Igor M/0000-0003-3118-4247; Franco, Daniel R/0000-0002-7790-1224; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Chiessi, Cristiano Mazur/0000-0003-3318-8022; Kuhnert, Henning/0000-0001-5242-4495; Ballalai, Joao Marcelo/0000-0002-8896-6816; Santos, Thiago/0000-0002-9273-3329	CAPES/IODP [88882.151088/2017-01]; CAPES [564/2015, 88881.313535/2019e01, 88887.156152/2017-00]; CNPq [302607/2016-1, 422255/2016-5, 306385/2013-9, 99999.002675/201503]; FAPESP [2018/15123-4]; Alexander von Humboldt Foundation; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [23038.001417/2914-71]; CNPq Project RAiN [406322/2018-0]	CAPES/IODP; CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Alexander von Humboldt Foundation(Alexander von Humboldt Foundation); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq Project RAiN	We thank R. Kowsman (CENPES/Petrobras) and Petrobras Core Repository staff (Maca~e/Petrobras) for providing the sediment core employed in this research. T.P.S acknowledges the financial support from CAPES/IODP (grant 88882.151088/2017-01). CAPES financially supported I.M.V. with a scholarship (grant 88887.156152/2017-00). A.L.A. is a CNPq senior researcher (grant 306385/2013-9) and thanks to them for financial support (grant 99999.002675/201503). C.M.C. acknowledges the financial support from FAPESP (grant 2018/15123-4), CAPES (grants 564/2015 and 88881.313535/2019e01), CNPq (grants 302607/2016-1 and 422255/2016-5) and the Alexander von Humboldt Foundation. This study was financed in part by the Coordenac~ao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -23038.001417/2914-71 (Paleoceano Project) and CNPq Project RAiN (grant 406322/2018-0). The data reported in this paper will be archived in Pangaea (www.pangaea.de).We are grateful to Julia Gottschalk, the editor Antje Volker and an anonymous reviewer for their insightful and constructive comments.	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J	Silva, VL; Pereira, S; Bustamante, A; Neves, SP				Silva, Valdielly L.; Pereira, Salviano; Bustamante, Andres; Neves, Sergio P.			Metamorphic evolution of metasedimentary rocks of the Feira Nova region: Tectonic implications for the Brasiliano Orogeny in eastern Borborema Province, Northeast Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Brasiliano-Pan-African orogeny; Borborema Province; Feira Nova region; Geothermobarometry	TEMPERATURE-TIME PATHS; EDIACARAN MAGMATIC ARC; P-T PATHS; NE-BRAZIL; U-PB; GRANITIC MAGMATISM; TRANSVERSAL ZONE; GRAVITATIONAL COLLAPSE; SUPRACRUSTAL SEQUENCES; SHEAR ZONES	Thermobarometric estimations and X-ray maps were combined to evaluate the metamorphic evolution of metasedimentary rocks (Surubim Complex) in the Feira Nova region, eastern Borborema Province (NE Brazil). Sillimanite-bearing biotite schists, garnet-biotite schists and gneisses were studied. X-ray maps show different growing phases and retrograde zoning patterns for biotite and garnet. High Ca and Mg contents in garnet cores along with high Ti in biotite are interpreted as equilibrium compositions at peak metamorphism. Lower contents of Ca and Mg at garnet rims and of Ti in biotite rims suggest cooling and decompression. Garnet-biotite geothermometer and garnet-Al2SiO5 -quartz-plagioclase (GASP) geobarometer constrain high temperature ( similar to 650-760 degrees C) and medium pressure ( similar to 0.6-0.9 GPa; burial to similar to 23-34 km) conditions for the metamorphic peak, which was synchronous to development of a flat-lying foliation and local anatexis. Garnet rims indicate exhumation to similar to 19-11 km (similar to 0.4-0.3 GPa) similar to 590-520 degrees C, probably during a transpressional regime. The data points to low exhumation and cooling rates. The lack of extensional fabrics in the region right after the Brasiliano Orogeny supports erosional unroofing rather than extensional collapse. Based on kyanite occurrences nearby, we infer a clockwise P-T path related to thickening in a predominant intracontinental setting, followed by exhumation with low erosional and cooling rates.	[Silva, Valdielly L.; Pereira, Salviano; Bustamante, Andres; Neves, Sergio P.] Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil	Universidade Federal de Pernambuco	Silva, VL (autor correspondente), Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil.	vallarisse@gmail.com	da Silva, Salviano/AAI-3447-2021; Neves, Sergio/A-2086-2008	da Silva, Salviano/0000-0002-5876-501X; Neves, Sergio/0000-0001-6690-3278	Brazilian Council of Research (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq); Votorantim Metais S.A.; CNPq	Brazilian Council of Research (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Votorantim Metais S.A.; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank the Brazilian Council of Research (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq) and Votorantim Metais S.A. for funding this work, and Sebastian Oriolo and an anonymous reviewer for their constructive comments. VLS thanks CNPq for the scholarship.	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South Am. Earth Sci.	JUN	2020	100								102590	10.1016/j.jsames.2020.102590	http://dx.doi.org/10.1016/j.jsames.2020.102590			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900038
J	Silva-Silva, LC; Oliveira, DC; de Souza, DB				Silva-Silva, Luana Camile; Oliveira, Davis Carvalho; de Souza, Diwhemerson Barbosa			Geology and geochemical constraints on the origin of the Mesoarchean granitoids from Carajas province, Amazonian craton	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Granitoid; Plutonism; Geochemistry; Archean; Carajas; Amazonian craton	TRONDHJEMITE-GRANODIORITE TTG; CRUST-MANTLE INTERACTIONS; EARLY CONTINENTAL-CRUST; U-PB GEOCHRONOLOGY; TONALITE-TRONDHJEMITE; A-TYPE; SANUKITOID SERIES; ARCHEAN CRUST; EXPERIMENTAL DEFORMATION; ZIRCON GEOCHRONOLOGY	The Carajas province (CP) is the largest preserved Archean core of the Amazonian craton. In this paper we present a detailed work about the Tucuma area located in the northwestern portion of the Rio Maria domain of the CP, where more detailed studies had not yet been carried out. The new geological and geochemical data obtained allowed the identification of Mesoarchean granitoids of different natures that resemble typical late-Archean granitoids (TTG, leucogranites, sanukitoids and hybrid granites) identified in several cratons around the world. The most extensive unit in the Tucuma area is the Leucomonzogranitic batholith which is intrusive in a tonalite crust of TTG affinity, that exhibits an older N-S structural pattern commonly found in oldest rocks (greenstone belt sequence). The batholith is coeval with small granitoid intrusions that occur as lenses controlled by NE-SW and E-W direction anastomosed shear zones. Apart from the tonalite, these granitoids show affinity with the calc-alkaline series and are individualized in four units. The porphyritic granodiorite is a magnesium-rich unit that has moderate K2O/Na2O ratio and higher levels of Ba, K and Th, indicating similarities with the Transitional TTG suites (Yilgarn craton). Equigranular granodiorites are equivalent of sanukitoid suites; they show enrichment in Sr and compatible elements (Mg, Cr, and Ni) and depletion in HREE. Hybrid granitoids were identified as High-HFSE granites (medium- and high-Ba) that share some geochemical affinities with Closepet granite of the Dharwar craton. The Leucomonzogranite is enriched in LILE and exhibit negative Eu anomalies, which indicate crustal reworking processes. This granitoids are syntectonic bodies that underwent a progressive deformation processes that started before the magma crystallization was complete, under high temperatures ( > 500 degrees C) conditions compatible with those of the amphibolite facies. Two phases of magmatism are recorded in the RMD, which would be responsible for the formation of these granitoids. The first phase (2.98-2.92 Ga) is related to formation of a thick TTG crust from parcial melting of an oceanic plateau or a thickened mafic crust. The second magmatism phase (similar to 2.87 Ga) initiated due to thermal events in a collisional setting, where both crustal rework processes and generation of juvenile magmatism occurred at the same time, resulting in the formation of heterogeneous plutons, at different crustal levels that were emplaced by mechanisms analogous to diapirs.	[Silva-Silva, Luana Camile; Oliveira, Davis Carvalho; de Souza, Diwhemerson Barbosa] Inst Geociencias, Grp Pesquisa Petrol Granitoides GPPG, Rua Augusto Correa 01, BR-66075900 Belem, De De De, Brazil; [Silva-Silva, Luana Camile; Oliveira, Davis Carvalho; de Souza, Diwhemerson Barbosa] Univ Fed Para UFPA IG UFPA, Programa Posgrad Geol & Geoquim, Belem, De &, Brazil		Silva-Silva, LC (autor correspondente), Inst Geociencias, Grp Pesquisa Petrol Granitoides GPPG, Rua Augusto Correa 01, BR-66075900 Belem, De De De, Brazil.	luana.silva@ig.ufpa.br; davis@ufpa.br; diw@ufpa.br			Research Group on Granitoid Petrology (GPPG); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) [001]; CAPES; CNPq [311388/2016-7, 435552/2018-0, 311647/2019-7]; PROPESP (PAPQ)/UFPA	Research Group on Granitoid Petrology (GPPG); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); PROPESP (PAPQ)/UFPA	The authors would like to thank the Research Group on Granitoid Petrology (GPPG), for their support in the various stages of this work, the Institute of Geosciences (IG), the Post-Graduate Program in Geology and Geochemistry (PPGG) of Federal University of Para (UFPA) for technical support. We gratefully acknowledge L. Florisbal and J. Almeida for their constructive comments and valuable suggestions. We gratefully acknowledge Oscar Laurent and an anonymous reviewer for their constructive comments and valuable notes, and Reinhardt Fuck for his efficient editorial handling. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brasil (CAPES) - Finance Code 001. The first author (LS) also thanks CAPES for a Masters thesis scholarship. Funding for this project came from CNPq (D.C. Oliveira - Proc. 311388/2016-7, 435552/2018-0 and 311647/2019-7), and PROPESP (PAPQ)/UFPA.	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J	Simon, Q; Ledru, MP; Sawakuchi, AO; Favier, C; Mineli, TD; Grohmann, CH; Guedes, M; Bare, E; Thouveny, N; Garcia, M; Tachikawa, K; Rodriguez-Zorro, PA				Simon, Quentin; Ledru, Marie-Pierre; Sawakuchi, Andre Oliveira; Favier, Charly; Mineli, Thays D.; Grohmann, Carlos H.; Guedes, Marco; Bare, Edouard; Thouveny, Nicolas; Garcia, Marta; Tachikawa, Kazuyo; Rodriguez-Zorro, Paula A.		ASTER Team	Chronostratigraphy of a 1.5 +/- 0.1 Ma composite sedimentary record from Colonia basin (SE Brazil): Bayesian modeling based on paleomagnetic, authigenic Be-10/Be-9, radiocarbon and luminescence dating	QUATERNARY GEOCHRONOLOGY			English	Article						Peat and lake sediments; Paleomagnetism; Luminescence dating; Radiocarbon; Authigenic Be-10/Be-9 dating; Deep drilling	OPTICALLY STIMULATED LUMINESCENCE; ATMOSPHERIC CIRCULATION; LACUSTRINE RECORD; PACIFIC-OCEAN; HALF-LIFE; LAKE; AGE; QUARTZ; SINGLE; PALEOINTENSITY	We present a new 52 m composite record (COL17c) composed of five sedimentary sequences retrieved from the Colonia basin (Southeastern Brazil). The COL17c record is composed of two main sub-units deposited under different regimes: a peatland above similar to 14 m and lacustrine sediments below. Sedimentary description and core scanning (MSCL and XRF) are first used to align individual cores in order to produce a nearly continuous composite record. We then established an original chronological framework based on radiocarbon, paleomagnetic, optically stimulated luminescence (OSL), post-infrared infrared stimulated luminescence at elevated temperature (pIRIR(290 degrees C)) and authigenic Be-10/Be-9 dating. We describe the protocols used for each technique and discuss the positive and negative results, as well as their implications for proxy interpretation. In spite of negative results of some techniques, mainly due to the absence of adequate sample material, the multi-proxy approach used is essential to maximize the chances of obtaining a satisfactory age model for this unique continental sedimentary sequence. All valid chronological proxies, comprising three AMS C-14 ages, one pIRIR(290 degrees C) age, two paleomagnetic constraints and eight authigenic Be-10/Be-9 datum, are integrated within a Bayesian age-depth modeling to produce a 1.5 +/- 0.1 Ma chronology for the whole COL17c sequence. This age model represents the first long-term chronological estimate of sediments deposition in the Colonia basin. The record allows to refine the age of the Colonia basin formation between 5.3 and 11.2 Ma, much older than previously estimated from short sedimentary cores.	[Simon, Quentin; Bare, Edouard; Thouveny, Nicolas; Garcia, Marta; Tachikawa, Kazuyo; ASTER Team] Aix Marseille Univ, CEREGE, CNRS, IRD,INRAE,Coll France,UM34, F-13545 Aix En Provence, France; [Ledru, Marie-Pierre; Favier, Charly; Rodriguez-Zorro, Paula A.] Univ Montpellier, ISEM, CNRS, IRD,EPHE, F-34095 Montpellier, France; [Sawakuchi, Andre Oliveira; Mineli, Thays D.] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, Brazil; [Grohmann, Carlos H.; Guedes, Marco] Univ Sao Paulo, Inst Energia & Ambiente, BR-05508080 Sao Paulo, Brazil	Centre National de la Recherche Scientifique (CNRS); INRAE; Institut de Recherche pour le Developpement (IRD); UDICE-French Research Universities; Aix-Marseille Universite; Universite PSL; College de France; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; UDICE-French Research Universities; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); Universidade de Sao Paulo; Universidade de Sao Paulo	Simon, Q (autor correspondente), Aix Marseille Univ, CEREGE, CNRS, IRD,INRAE,Coll France,UM34, F-13545 Aix En Provence, France.	simon@cerege.fr	Grohmann, Carlos/A-9030-2008; Simon, Quentin/D-9956-2017; Sawakuchi, André O/D-1445-2013; Guedes Pereira, Marco Aurelio/W-9564-2018	Grohmann, Carlos/0000-0001-5073-5572; Simon, Quentin/0000-0001-8247-0150; Sawakuchi, Andre/0000-0001-5016-2428; Guedes Pereira, Marco Aurelio/0000-0002-3273-6712; Ledru, Marie-Pierre/0000-0002-8079-9320	CLIMCOR program at INSU; C2FN in France; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [304727/2017-2]; INSU/CNRS; ANR; IRD; College de France; EQUIPEX ASTER-CEREGE; FAPESP [BIOTA 2013/50297-0]; NSF [DEB 1343578]	CLIMCOR program at INSU; C2FN in France; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); INSU/CNRS(Centre National de la Recherche Scientifique (CNRS)); ANR(French National Research Agency (ANR)); IRD; College de France; EQUIPEX ASTER-CEREGE; FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); NSF(National Science Foundation (NSF))	We thank Fabiano Pupim for assistance in fieldwork, Luciana Nogueira for assistance with gamma rays spectrometry, Francois Demory for its support with magnetic susceptibility measurements and Coralie Andreucci for assistance with the beryllium samples preparation. The CLIMCOR program at INSU and the C2FN in France are acknowledged for their support. Laurent Augustin and Alain de Moya (C2FN-DT-INSU) are thanked for assistance during the 2017 coring mission. We acknowledge Claudio Riccomini for sharing his knowledge about Colonia and constant support; and Ricardo Trindade for offering MSCL access at USP. The Suehara family, owner of the land, APA Capivari Monos, Associacao ACHAVE de Vargem Grande are thanked for granting access to drilling site. We also acknowledge Christian Zeeden and an anonymous reviewer for constructive and helpful comments. AOS is supported by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq grant 304727/2017-2). The ASTER AMS national facility (CEREGE, Aix en Provence) is supported by INSU/CNRS, ANR through the EQUIPEX ASTER-CEREGE action, and IRD. The AixMICADAS and its operation are funded by the College de France and the EQUIPEX ASTER-CEREGE. Yoann Fagault and Thibaut Tuna are thanked for performing analyses. This research is part of the projects "Dimensions of biodiversity" FAPESP (BIOTA 2013/50297-0), NSF (DEB 1343578) and NASA, the International Continental Deep Drilling Program (ICDP), "UV-Trop" INSU LEFE, the Labex-CEBA, "TROPICOL" Foundation BNP Paribas "Climate Initiative" (2017-2020). The data presented in this study are available within the supporting information.	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Geochronol.	JUN	2020	58								101081	10.1016/j.quageo.2020.101081	http://dx.doi.org/10.1016/j.quageo.2020.101081			18	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	LS3KQ		Bronze, Green Submitted			2023-06-23	WOS:000536287300009
J	Sousa, SHM; Yamashita, C; Semensatto, DL; Santarosa, ACA; Iwai, FS; Omachi, CY; Disaro, ST; Martins, MVA; Barbosa, CF; Bonetti, CHC; Vilela, CG; Laut, L; Turra, A				Sousa, S. H. M.; Yamashita, C.; Semensatto Jr, D. L.; Santarosa, A. C. A.; Iwai, F. S.; Omachi, C. Y.; Disaro, S. T.; Martins, M. V. A.; Barbosa, C. F.; Bonetti, C. H. C.; Vilela, C. G.; Laut, L.; Turra, A.		BIOFOM Grp	Opportunities and challenges in incorporating benthic foraminifera in marine and coastal environmental biomonitoring of soft sediments: from science to regulation and practice	JOURNAL OF SEDIMENTARY ENVIRONMENTS			English	Article						Benthic foraminifera; Bioindicator; Biomonitoring; Conservation biology	RIO-DE-JANEIRO; ECOLOGICAL QUALITY; BIO-INDICATORS; TAXONOMIC REVISION; POLLUTED SEDIMENTS; INDEX; BAY; ASSEMBLAGES; LAGOON; ESTUARINE	Scientific studies have demonstrated the usefulness of benthic foraminifera as bioindicators to assess the health of marine, coastal, and transitional ecosystems. Similar to macrofauna, these organisms are reliable proxies for biomonitoring. Despite recent scientific advances, Brazilian official monitoring plans using biotic indices on coastal and ocean environments with soft sediment areas remain mostly restricted to a few types of organisms. Therefore, to include benthic foraminifera in Brazilian biomonitoring routines regulated by national environmental guidelines and standards, the paper presents the challenges, which must be overcome, some recommendations and steps to move forward to implement foraminifera as bioindicators in biomonitoring routines. In light of it, it is essential to consider the contribution of the Brazilian foraminiferal research in this implementation process, improving ecological quality indices, adapting methods, and applying genetics tools. This paper is a step in this direction, which aims to strengthen the role of benthic foraminifera as a reliable tool in Brazilian biomonitoring.	[Sousa, S. H. M.; Yamashita, C.; Santarosa, A. C. A.; Iwai, F. S.; Omachi, C. Y.; Turra, A.] Univ Sao Paulo, Inst Oceanog, Sao Paulo, SP, Brazil; [Semensatto Jr, D. L.] Univ Fed Sao Paulo, Campus Diadema, Diadema, SP, Brazil; [Disaro, S. T.] Univ Fed Parana, Museu Ciencias Nat SCB, Curitiba, Parana, Brazil; [Martins, M. V. A.] Univ Estado Rio de Janeiro, Fac Geol, Rio De Janeiro, RJ, Brazil; [Martins, M. V. A.] Univ Aveiro, Dept Geociencias, GeoBioTec, Aveiro, Portugal; [Barbosa, C. F.] Univ Fed Fluminense, Ctr Estudos Gerais, Inst Quim, Niteroi, RJ, Brazil; [Bonetti, C. H. C.] Univ Fed Santa Catarina, Campus Univ, Florianopolis, SC, Brazil; [Vilela, C. G.] Univ Fed Rio de Janeiro, Inst Geociencias, Rio De Janeiro, RJ, Brazil; [Laut, L.] Univ Fed Estado Rio de Janeiro, Inst Biociencias, UNIRIO, Rio De Janeiro, RJ, Brazil	Universidade de Sao Paulo; Universidade Federal de Sao Paulo (UNIFESP); Universidade Federal do Parana; Universidade do Estado do Rio de Janeiro; Universidade de Aveiro; Universidade Federal Fluminense; Universidade Federal de Santa Catarina (UFSC); Universidade Federal do Rio de Janeiro; Universidade Federal do Estado do Rio de Janeiro	Sousa, SHM (autor correspondente), Univ Sao Paulo, Inst Oceanog, Sao Paulo, SP, Brazil.	smsousa@usp.br; cintiasea@gmail.com; semensattojr@gmail.com; anasantarosa@gmail.com; sayuri.iwai@gmail.com; comachi@gmail.com; stdisaro@ufpr.br; Virginia.martins@ua.pt; catiafb@id.uff.br; carla.bonetti@ufsc.br; vilela@geologia.ufrj.br; lazaro.laut@gmail.com; turra@usp.br	Martins, Maria/IQT-0561-2023; Alves Martins, Maria Virginia Virginia/O-2893-2013; Omachi, Claudia/A-5110-2008; Disaró, Sibelle/F-7575-2014; Turra, Alexander/G-1352-2012; de Mello e Sousa, Silvia Helena/ABH-5834-2020; Semensatto, Décio/AAD-4472-2020; Laut, Lazaro/O-4193-2019; Siegle, Eduardo/F-5408-2010; Lourenço, Rafael André/I-7041-2015; Semensatto, Décio/A-6315-2008	Alves Martins, Maria Virginia Virginia/0000-0001-8348-8862; Omachi, Claudia/0000-0002-1578-5440; Disaró, Sibelle/0000-0002-6299-0324; Turra, Alexander/0000-0003-2225-8371; Semensatto, Décio/0000-0002-4253-6351; Laut, Lazaro/0000-0002-5637-1930; Siegle, Eduardo/0000-0003-3926-1710; Lourenço, Rafael André/0000-0002-1446-5074; Semensatto, Décio/0000-0002-4253-6351; Mello e Sousa, Silvia Helena/0000-0002-8860-9042; Bouchet, Vincent/0000-0001-5458-1638	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo -FAPESP [FAPESP 2018/20639-0]; CEPEA; SALT; TETRATECH; BIOLABBRASIL; CNPq; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2017/00427-5]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [18/20639-0] Funding Source: FAPESP	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo -FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CEPEA; SALT; TETRATECH; BIOLABBRASIL; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	We acknowledge the Fundacao de Amparo a Pesquisa do Estado de Sao Paulo -FAPESP (FAPESP 2018/20639-0), CEPEA, SALT, TETRATECH and BIOLABBRASIL for funding the first BioFom Workshop. We are also grateful to the Oceanographic Institute and Geociscences Institute, both of the University of Sao Paulo for the support of the workshop. We thank all the BioFom participants which made contributions to the discussions during the workshop. SHMS, MVAM, AT, ES, MMM, RSLF are sponsored by CNPq research fellowships. CY was supported by Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) 2017/00427-5. 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Sediment. Environ.	JUN	2020	5	2					257	265		10.1007/s43217-020-00011-w	http://dx.doi.org/10.1007/s43217-020-00011-w			9	Environmental Sciences	Emerging Sources Citation Index (ESCI)	Environmental Sciences & Ecology	MG9OP					2023-06-23	WOS:000546362300007
J	Souza, VS; Teixeira, LSG; Santos, QO; Gomes, IS; Bezerra, MA				Souza, Valdinei S.; Teixeira, Leonardo S. G.; Santos, Queila O.; Gomes, Ivaldo S.; Bezerra, Marcos A.			Determination of Copper and Cadmium in Petroleum Produced Formation Water by Electrothermal Atomic Absorption Spectrometry after Cloud Point Extraction	JOURNAL OF THE BRAZILIAN CHEMICAL SOCIETY			English	Article						produced-formation water; constrained mixture design; cloud-point extraction; cadmium; copper	ULTRA-TRACE DETERMINATION; SPECIATION; CHROMIUM; SAMPLES	Cloud point extraction (CPE) in association with graphite furnace atomic absorption spectrometry (GF AAS) was proposed for preconcentration and quantification of trace amounts of copper and cadmium in samples of saline produced formation water from petroleum exploration. The procedure was based on the formation of hydrophobic complexes of the analytes with 1.5-diphenylthiocarbazone (dithizone) in a micellar media of the surfactant (1,1,3,3-tetramethyl butyl) phenyl-polyethylene glycol (Triton X-114). Constrained mixture design was performed for the optimization of the proportions of the three solutions employed in the CPE: Triton X-114. dithizone, and buffer solution. Under the recommended conditions, the CPE GF AAS procedure allowed to obtain emichment factors of 18 and 11 times, limits of quantification of 0.030 and 0.12 mu g L-1 and precision, expressed as relative standard deviation (RSD, n = 8, 2.0 mu g L-1), of 1.1 and 4.3% for copper and cadmium, respectively. The CPE GF AAS method was applied to the determination of copper and cadmium in samples of saline produced formation water from petroleum exploration, and its accuracy was accessed by analyzing certified reference material CASS-5 (Nearshore Seawater Reference Material for Trace Metals) from National Research Council (Canada).	[Souza, Valdinei S.] Inst Fed Educ Ciencia & Tecnol Baiano, Rodovia Santa Ines,BR 420, BR-45320000 Santa Ines, BA, Brazil; [Teixeira, Leonardo S. G.] Univ Fed Bahia, Inst Quim, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Santos, Queila O.] Inst Fed Educ Ciencia & Tecnol Baiano, Rodovia Itapetinga Itororo,Km 02, BR-45700000 Itapetinga, BA, Brazil; [Gomes, Ivaldo S.; Bezerra, Marcos A.] Univ Estadual Sudoeste Bahia, Dept Ciencias & Tecnol, Rua Jose Moreira Sobrinho S-N, BR-45208409 Jequie, BA, Brazil	Instituto Federal Baiano (IFBAIANO); Universidade Federal da Bahia; Instituto Federal Baiano (IFBAIANO); Universidade Estadual do Sudoeste da Bahia	Bezerra, MA (autor correspondente), Univ Estadual Sudoeste Bahia, Dept Ciencias & Tecnol, Rua Jose Moreira Sobrinho S-N, BR-45208409 Jequie, BA, Brazil.	mbezerra47@yahoo.com.br	Teixeira, Leonardo S G/J-9131-2016	Teixeira, Leonardo S G/0000-0003-0320-8299; Souza, Valdinei/0000-0003-4450-1280; Bezerra, Marcos/0000-0003-2933-893X	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [304582/2018-2]; Financiadora de Estudos e Projetos (FINEP); Programa de Formacao de Recursos Humanos da ANP PRH/ANP/MCT	Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Financiadora de Estudos e Projetos (FINEP)(Financiadora de Inovacao e Pesquisa (Finep)); Programa de Formacao de Recursos Humanos da ANP PRH/ANP/MCT	Authors acknowledge the financial support of the Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001, Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, No. 304582/2018-2), Financiadora de Estudos e Projetos (FINEP) and Programa de Formacao de Recursos Humanos da ANP PRH/ANP/MCT.	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A., 2006, EXTRACAO PONTO NUVEM, V1a; Depoi FD, 2012, J BRAZIL CHEM SOC, V23, P2211; Costa BED, 2015, FOOD CHEM, V178, P89, DOI 10.1016/j.foodchem.2015.01.014; Ferreira AC, 2004, MICROCHEM J, V78, P77, DOI 10.1016/j.microc.2004.03.014; Garcia S, 2015, J BRAZIL CHEM SOC, V26, P490, DOI 10.5935/0103-5053.20150001; Grenni P, 2019, MICROCHEM J, V147, P1010, DOI 10.1016/j.microc.2019.04.026; Khan A, 2019, INT J ENVIRON SCI TE, V16, P2295, DOI 10.1007/s13762-018-1849-x; Menezes J., 2018, MICROCHEM J, V138, P92; Miranda-Andrades JR, 2019, MICROCHEM J, V146, P1072, DOI 10.1016/j.microc.2019.02.045; Naeemullah, 2013, J AOAC INT, V96, P447, DOI 10.5740/jaoacint.11-128; Naeemullah, 2012, J ANAL METHODS CHEM, V2012, DOI 10.1155/2012/713862; Oliveira EP, 2008, MICROCHEM J, V89, P116, DOI 10.1016/j.microc.2008.01.002; Oliveira EP, 2011, J ANAL ATOM SPECTROM, V26, P578, DOI 10.1039/c0ja00108b; Silva SG, 2010, J BRAZIL CHEM SOC, V21, P234, DOI 10.1590/S0103-50532010000200007; Xie MD, 2019, AQUAT TOXICOL, V210, P106, DOI 10.1016/j.aquatox.2019.02.018; Zhu XS, 2005, WATER RES, V39, P589, DOI 10.1016/j.watres.2004.11.006	19	6	6	0	15	SOC BRASILEIRA QUIMICA	SAO PAULO	CAIXA POSTAL 26037, 05599-970 SAO PAULO, BRAZIL	0103-5053	1678-4790		J BRAZIL CHEM SOC	J. Braz. Chem. Soc.	JUN	2020	31	6					1186	1193		10.21577/0103-5053.20200004	http://dx.doi.org/10.21577/0103-5053.20200004			8	Chemistry, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	LK2KY		gold			2023-06-23	WOS:000530689400009
J	Temporim, FA; Trindade, RIF; Tohver, E; Soares, CC; Gouvea, LP; Egydio-Silva, M; Amaral, CAD; Souza, GF				Temporim, F. A.; Trindade, R. I. F.; Tohver, E.; Soares, C. C.; Gouvea, L. P.; Egydio-Silva, M.; Amaral, C. A. D.; Souza Jr, G. F.			Magnetic Fabric and Geochronology of a Cambrian "Isotropic" Pluton in the Neoproterozoic Aracuai Orogen	TECTONICS			English	Article						anisotropy of magnetic susceptibility</AUTHOR_KEYWORD>; magnetic fabric</AUTHOR_KEYWORD>; Aracuai Orogen</AUTHOR_KEYWORD>; emplacement model</AUTHOR_KEYWORD>	MOLTEN MIDDLE CRUST; WEST-CONGO OROGEN; SAN-JOSE TONALITE; INTRACONTINENTAL TERMINATION; EMPLACEMENT MECHANISM; EXTENSIONAL COLLAPSE; TECTONIC EVOLUTION; NORTHERN PORTUGAL; BAJA-CALIFORNIA; BRAZIL EVIDENCE	The Aracuai Orogen (AO) has been interpreted as a Neoproterozoic example of a large, "hot" orogen, based on a broad zone (250 km) of midcrustal metamorphic assemblages with a long, 70-Myr history of crustal melting and episodic magmatism throughout the late Neoproterozoic and earliest Paleozoic. Here, we present results of U-Pb sensitive high-resoution ion microprobe (SHRIMP) zircon dating and detailed anisotropy of magnetic susceptibility (AMS) study on a late Cambrian, bimodal pluton related to final period of collapse of the AO. New U-Pb zircon ages constrain the crystallization age of different suites within the Santa Angelica Pluton, 506 +/- 3 Ma for the early felsic phase and 498 +/- 5 Ma for the mafic core. New AMS data indicate that the emplacement of the Santa Angelica Pluton corresponds to two coupled plutons with concentric structures arrayed about a twin, bull's eye pattern. During the final stages of intrusion, upward relative movement of the northeastern lobe exposed the deeper levels of the intrusion, relative to the more shallowly eroded southwestern lobe. These observations suggest that magma emplacement was controlled by magma buoyancy forces, with little influence of regional tectonic stress. This behavior contrasts with the well-defined, tectonic-controlled fabrics of coeval plutons occurring to the north which was still hot, therefore highlighting the contrasting thermal evolution between different sectors of the orogen during its final stages.	[Temporim, F. A.; Trindade, R. I. F.; Tohver, E.; Amaral, C. A. D.; Souza Jr, G. F.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Dept Geofis, Sao Paulo, Brazil; [Soares, C. C.] Univ Fed Espirito Santo, Dept Geol, Alegre, Brazil; [Gouvea, L. P.] Univ Fed Rio de Janeiro, Dept Geol, Rio De Janeiro, Brazil; [Egydio-Silva, M.] Univ Sao Paulo, Inst Geociencias, Sao Paulo, SP, Brazil	Universidade de Sao Paulo; Universidade Federal do Espirito Santo; Universidade Federal do Rio de Janeiro; Universidade de Sao Paulo	Temporim, FA (autor correspondente), Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Dept Geofis, Sao Paulo, Brazil.	tilipetemporim@gmail.com	Egydio-SIlva, Marcos/G-1819-2012; Tohver, Eric/H-8080-2012; Trindade, Ricardo IF/A-8146-2008; Temporim, Filipe/AAR-9538-2021	Egydio-SIlva, Marcos/0000-0002-8758-2175; Tohver, Eric/0000-0002-3333-0917; Trindade, Ricardo IF/0000-0001-9848-9550; Temporim, Filipe/0000-0002-7417-4391; Ferreira Souza Junior, Gelson/0000-0002-5695-4239; Deiroz Amaral, Caio Augusto/0000-0002-2956-2061; Gouvea, Lucas/0000-0002-7574-7876	SAo Paulo Research Foundation (FAPESP) [2016/06114-6, 2017/11672-0]	SAo Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The authors would like to express their gratitude to C.R. Cioffi for his support in the acquisition of data during fieldwork, C. Guacaneme, J. W. L. Afonso, and T. R. Moncinhatto for their support in the geochronological analysis. The infrastructure and collaborations of the Laboratorio de Paleomagnetismo of the Universidade de SAo Paulo. This works was funded by grants of SAo Paulo Research Foundation (FAPESP) (# 2016/06114-6 and # 2017/11672-0).	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C., 2017, THESIS, P1; Zak J, 2013, TECTONICS, V32, P1493, DOI 10.1002/tect.20088; Zanon ML, 2015, BRAZ J GEOL, V45, P609, DOI 10.1590/2317-4889201520150005; [No title captured]	100	10	10	0	7	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA	0278-7407	1944-9194		TECTONICS	Tectonics	JUN	2020	39	6							e2019TC005877	10.1029/2019TC005877	http://dx.doi.org/10.1029/2019TC005877			21	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	MG4QX					2023-06-23	WOS:000546019000002
J	Vieira, DT; Koester, E; Ramos, RC; Porcher, CC; Fernandes, LAD				Vieira, Daniel Triboli; Koester, Edinei; Ramos, Rodrigo Chaves; Porcher, Carla Cristine; D'Avila Fernandes, Luis Alberto			SHRIMP U-Pb zircon ages for the synkinematic magmatism in the Dorsal de Cangucu Transcurrent Shear Zone, Dom Feliciano Belt (Brazil): Tectonic implications	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Geochronology; Neoproterozoic; Quiteria Granite; Cordilheira Suite; Sul-rio-grandense Shield	DE-LA-PLATA; SOUTHERN BRAZIL; PELOTAS BATHOLITH; GRANITIC MAGMATISM; SANTA-CATARINA; PAN-AFRICAN; ICP-MS; EVOLUTION; GEOCHRONOLOGY; DEFORMATION	The Dorsal de Cangucu Transcurrent Shear Zone (DCTSZ) is the main Neoproterozoic structure of the Dom Feliciano Belt in the Rio Grande do Sul sector (Brazil), developed during the late stages of the Brasilano/Pan-African orogenic cycle. This structure, together with its northern - Major Gercino Transcurrent Shear Zone (Santa Catarina sector, Brazil) - and southern extension - Sierra Ballena Transcurrent Shear Zone (Uruguay), constitute a 1000 km long discontinuous lineament. Synkinematic granitoids are widespread along the DCTSZ. The main units are represented by the porphyritic, calc-alkaline high-K Quiteria granite, and the peraluminous Arroio Francisquinho and Cordilheira granites (Cordilheira Suite). In order to better constrain the time frame of the synkinematic magmatism associated with the DCTSZ, we present in this paper new zircon SHRIMP (Sensitive High Resolution Ion Micro Probe) U-Pb ages for this magmatism. The Quiteria granite yielded a concordia U-Pb age of 618.9 +/- 4 Ma, interpreted as the magmatic crystallization age. The Arroio Francisquinho and Cordilheira granites yielded concordia U-Pb ages of, respectively, 615.2 +/- 13 Ma and 607.3 +/- 12 Ma, interpreted as the magmatic crystallization ages. The latter ages constrain the main phase of synkinematic magmatism in the DCTSZ. Zircon rims of the studied samples yielded U-Pb ages between 585 and 540 Ma might represent the influence of post-magmatic fluids and deformation caused by the transcurrent activity of the shear zone. Zircon crystals interpreted as inherited yielded U-Pb ages ranging from 1800 to 650 Ma for the three studied rocks. These inherited ages are similar to those found in detrital zircon from the regional gneissic basement. The new ages for the earliest synkinematic magmatism in the DCTSZ match those of the Major Gercino and Sierra Ballena Shear Zone, strengthen previous correlation between the shear zones.	[Vieira, Daniel Triboli; Ramos, Rodrigo Chaves] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Caixa Postal 15-001, BR-91501970 Porto Alegre, RS, Brazil; [Koester, Edinei; Porcher, Carla Cristine; D'Avila Fernandes, Luis Alberto] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Geol, Av Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Vieira, DT (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Caixa Postal 15-001, BR-91501970 Porto Alegre, RS, Brazil.	daniel.triboli@ufrgs.br; koester@ufrgs.br; rodrigo.chaves@ufrgs.br; carla.porcher@ufrgs.br; ladfernandes@gmail.com	Koester, Edinei/L-3684-2017; Porcher, Carla C/R-1419-2018	Koester, Edinei/0000-0002-4424-4782; Porcher, Carla C/0000-0002-0418-3954; Vieira, Daniel/0000-0003-0616-5407; Chaves Ramos, Rodrigo/0000-0001-7116-5062	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [PqG 10/1509-0]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [140461/20167]	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank: Editor Reinhardt Fuck, Dr. Sebastian Oriolo and other two anonymous reviewers for their insightful comments and suggestions on the manuscript. 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South Am. Earth Sci.	JUN	2020	100								102603	10.1016/j.jsames.2020.102603	http://dx.doi.org/10.1016/j.jsames.2020.102603			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900043
J	Weska, RK; Barbosa, PF; Martins, MVC; Souza, VS; Dantas, EL				Weska, R. K.; Barbosa, P. F.; Martins, M. V. C.; Souza, V. S.; Dantas, E. L.			Pectolite in the Carolina kimberlitic intrusion, Espigao D'Oeste - Rondonia, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Pectolite; Pimenta Bueno Kimberlite Field; Carolina kimberlite intrusion	PETROGENESIS; CEBOLLITE	In this study, we characterize pectolite that occurs in a Carolina kimberlitic intrusion from the Pimenta Bueno Kimberlite Field (PBKF). The PBKF is the only kimberlite field of Permo-Carboniferous age in Brazil and is found on the southern Amazonian Craton. Pectolite, an Na-Ca-silicate usually identified in alkaline rocks as a primary mineral, is not common in the mineral paragenesis of kimberlites and is described here for the first time in Brazil. The genesis of pectolite in kimberlite has been well-studied and can be interpreted as a primary or secondary mineral resulting from the infiltration of an Na-rich fluid into metasomatic reactions. In the rocks from the PBKF, pectolite mainly occurs as fibrous and radial aggregates enriched in K2O that grow between olivine partially altered to serpentine and phlogopite. The results of field and petrographic observations suggest that the PBKF pectolite is of secondary origin, having formed during the hydrothermal alteration of the Carolina kimberlitic intrusion.	[Weska, R. K.] Univ Fed Mato Grosso, Geosci Fac, BR-78060900 Cuiaba, MT, Brazil; [Barbosa, P. F.; Martins, M. V. C.; Souza, V. S.; Dantas, E. L.] Univ Brasilia, Inst Geosci, BR-70910900 Brasilia, DF, Brazil	Universidade Federal de Mato Grosso; Universidade de Brasilia	Weska, RK (autor correspondente), Univ Fed Mato Grosso, Geosci Fac, BR-78060900 Cuiaba, MT, Brazil.	rweska@ufmt.br	Barbosa, Paola/AAK-8478-2021; Dantas, Elton Luiz/AAK-8464-2021	Barbosa, Paola/0000-0001-7661-455X; Dantas, Elton Luiz/0000-0002-7954-5059				AGEE JJ, 1982, AM MINERAL, V67, P28; Akella J., 1979, KIMBERLITES DIATREME, V1, P172; Buerger M. J., 1956, Z KRISTALLOGR, V108, P248, DOI [10.1524/zkri.1956.108.3-4.248, DOI 10.1524/ZKRI.1956.108.3-4.248]; Buerger M.J., 1963, 3 GEN M INT MIN ASS, P293; BUERGER MJ, 1961, P NATL ACAD SCI USA, V47, P1884, DOI 10.1073/pnas.47.12.1884; Clement C., 1985, J GEOL, V88, P403; Costa M. A. C da, 2015, THESIS, P84; Deer W.A., 1963, SINGLE CHAIN SILICAT, V2, P379; Gaia V.C.S., 2014, DISSERTACAO MESTRADO, P75; Hunt L, 2009, LITHOS, V112, P843, DOI 10.1016/j.lithos.2009.04.018; Kamenetsky VS, 2014, EARTH-SCI REV, V139, P145, DOI 10.1016/j.earscirev.2014.09.004; KRUGER FJ, 1980, MINERAL MAG, V43, P583, DOI 10.1180/minmag.1980.043.329.04; KRUGER FJ, 1982, MINERAL MAG, V46, P274, DOI 10.1180/minmag.1982.046.339.18; Masun KM, 2008, J VOLCANOL GEOTH RES, V174, P81, DOI 10.1016/j.jvolgeores.2007.12.043; Mitchell RH, 1986, KIMBERLITES MINERALO, P442, DOI [10.1007/978-1-4899-0568-0, DOI 10.1007/978-1-4899-0568-0]; Paiva J.M.S., 2016, THESIS, P75; Reed SJB., 2006, ELECT MICROPROBE ANA, P232; SCHALLER WT, 1955, AM MINERAL, V40, P1022; SCHMID R, 1981, GEOLOGY, V9, P41, DOI 10.1130/0091-7613(1981)9<41:DNACOP>2.0.CO;2; Scott Smith B.H., 2018, GLOSSARY KIMBERLIT 2; Scott Smith B. H, 2018, GLOSSARY KIMBERLIT 3; Scott -Smith B.H., 2013, SPEC ISSUE J GEOL SO, V2, P1, DOI DOI 10.1007/978-81-322-1173-0_1; Scott-Smith B.S, 2018, GLOSSARY KIMBERLITE; SMITH BHS, 1983, MINERAL MAG, V47, P75, DOI 10.1180/minmag.1983.047.342.13; Stamm N, 2017, EARTH PLANET SC LETT, V474, P309, DOI 10.1016/j.epsl.2017.06.037; Villamizar M, 2011, BIOTECHNO 2011: THE THIRD INTERNATIONAL CONFERENCE ON BIOINFORMATICS, BIOCOMPUTATIONAL SYSTEMS AND BIOTECHNOLOGIES, P12	26	1	1	1	2	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811			J S AM EARTH SCI	J. South Am. Earth Sci.	JUN	2020	100								102583	10.1016/j.jsames.2020.102583	http://dx.doi.org/10.1016/j.jsames.2020.102583			7	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN2SZ					2023-06-23	WOS:000532794900034
J	Amorim, KB; Afonso, JWL; Leme, JD; Diniz, CQC; Rivera, LCM; Gmez-Gutirrez, JC; Boggiani, PC; Trindade, RIF				Amorim, Kamilla Borges; Afonso, Jhon Willy Lopes; Leme, Juliana de Moraes; Diniz, Cleber Quidute Clemente; Rivera, Laura Carolina Montenegro; Gomez-Gutierrez, Juan Camilo; Boggiani, Paulo Cesar; Trindade, Ricardo Ivan Ferreira			Sedimentary facies, fossil distribution and depositional setting of the late Ediacaran Tamengo Formation (Brazil)	SEDIMENTOLOGY			English	Article						Biomineralization; Ediacaran; environmental niches; fossil distribution; Tamengo Formation	PRECAMBRIAN-CAMBRIAN BOUNDARY; NAMA GROUP; ITAPUCUMI GROUP; METAZOAN REEFS; HUMMOCKY STRATIFICATION; CARBONATE PLATFORM; DENGYING FORMATION; NORTHERN PARAGUAY; STORM DEPOSITS; INDEX FOSSIL	Mixed carbonate-siliciclastic deposits of the Tamengo Formation (terminal Ediacaran), record the rise of calcifying metazoans and the origin of exoskeletons in animals. To explore the relationships between environmental setting and the first appearance of calcified metazoans and their ecology, this study presents detailed sedimentological and stratigraphic data of eight sections that capture the final stages of the Ediacaran (550 to 543 Ma). This study combines stratigraphic characterization with detailed facies descriptions and evaluates lateral heterogeneity and overall ramp sedimentation integrated with fossil distribution. The Tamengo Formation represents a storm-dominated ramp. The outer to mid-ramp is composed of very fine-grained siliciclastic rocks containing Corumbella body fossils and thin-bedded mudstone/wackestone containing Cloudina. The mid-inner ramp is dominated by wackestone/packstone with abundant Cloudina skeletal debris and ooid packstone/grainstone shoal deposits. Locally, fragments of Corumbella and Cloudina are found on the same horizon, which is a result of their high accumulation rate, resulting from the reworking and mixing of epifaunal organisms. In spite of taphonomic biases, the general distribution of Corumbella and Cloudina across the unit suggests that these organisms have been transported across ramp and/or probably show a differential response of fauna preservation. When compared to other occurrences worldwide, this dataset indicates an already complex ecosystem in the Ediacaran, where these early animals were capable of adapting to specific environmental niches.	[Amorim, Kamilla Borges] Univ Fed Mato Grosso, Fac Geociencias, Ave Fernando Correa da Costa 2367, BR-78060900 Cuiaba, Coxipo, Brazil; [Amorim, Kamilla Borges; Afonso, Jhon Willy Lopes; Trindade, Ricardo Ivan Ferreira] Univ Sao Paulo, Dept Geofis, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226, Sao Paulo, SP, Brazil; [Leme, Juliana de Moraes; Diniz, Cleber Quidute Clemente; Rivera, Laura Carolina Montenegro; Boggiani, Paulo Cesar] Univ Sao Paulo, Inst Geociencias, Dept Geol Sedimentar & Ambiental, Rua Lago 562, Sao Paulo, SP, Brazil; [Diniz, Cleber Quidute Clemente; Rivera, Laura Carolina Montenegro; Gomez-Gutierrez, Juan Camilo] Univ Sao Paulo, Inst Geociencias, Programa Posgrad Geoquim & Geotecton, Sao Paulo, SP, Brazil	Universidade Federal de Mato Grosso; Universidade de Sao Paulo; Universidade de Sao Paulo; Universidade de Sao Paulo	Amorim, KB (autor correspondente), Univ Fed Mato Grosso, Fac Geociencias, Ave Fernando Correa da Costa 2367, BR-78060900 Cuiaba, Coxipo, Brazil.; Amorim, KB (autor correspondente), Univ Sao Paulo, Dept Geofis, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226, Sao Paulo, SP, Brazil.	kamillaborges06@gmail.com	Trindade, Ricardo IF/A-8146-2008; Afonso, Jhon/HLQ-2808-2023	Trindade, Ricardo IF/0000-0001-9848-9550; Borges Amorim, Kamilla/0000-0002-5031-402X	Sao Paulo Research Foundantion (FAPESP) [2016/06114-6]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [153683/2016-3]	Sao Paulo Research Foundantion (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We would like to thank Chief Editor Dr Peir Pufahl for his helpful comments. We are very thankful for very thorough and thoughtful reviews by Marc Laflamme, Alexander Liu and anonymous reviewers. Also, we thank Dr Thomas Fairchild for additional comments on this paper. This study was funded by the Sao Paulo Research Foundantion (FAPESP) thematic project grant (2016/06114-6). This research was conducted during post doctoral at the Institute of Astronomy, Geophysic and Atmospheric Sciences (IAG-USP) with support of the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (153683/2016-3).	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J	Avila, DVL; Souza, SO; Cerda, V; Araujo, RGO				Avila, Dayara Virginia L.; Souza, Sidnei Oliveira; Cerda, Victor; Araujo, Rennan G. O.			Determination of total and bioavailable As and Sb in children's paints using the MSFIA system coupled to HG-AFS	ANALYTICAL METHODS			English	Article							FLOW-INJECTION ANALYSIS; TOYS SOLD; ANTIMONY; LEAD; BIOACCESSIBILITY; METALS	In this study, the use of hydride generation atomic fluorescence spectrometry (HG-AFS) coupled with the multi-syringe flow injection analysis (MSFIA) has been proposed in the application of the Doehlert design to optimise the determination of As and Sb in gouache and tempera children's paints. The determination of the total and bioavailable As and Sb in paint samples from various brands and colours was also investigated. The limits of quantification (LOQ) obtained for the determination of As and Sb were 14.0 and 8.6 ng g(-1), respectively. The accuracy and precision of the method were evaluated through recovery tests (by the analyte addition method) at three levels for both elements, and by the analysis of certified reference materials of clay (CRM 052, Loamy Clay 1) and river water (SLRS-4). Twenty paint samples, manufactured in China, Italy, Spain and Brazil, were analysed. The concentrations of As varied between below LOQ (<14 ng g(-1)) and 136.0 +/- 1.1 ng g(-1) (average value of 101.0 ng g(-1), n = 10), and Sb between below LOQ (<8.6 ng g(-1)) and 74.0 +/- 5.4 ng g(-1) (average value of 21.7 ng g(-1), n = 17). The children's paint samples presented As and Sb concentrations that were below the maximum values established by the National Institute of Metrology, Quality and Technology (INMETRO), as well as by the European legislation Directive 2009/48/EC. Based on the obtained results for the total As and Sb concentrations, eight samples were selected to evaluate the migration or bioavailability of As and Sb after solubilisation in HCl solution. The obtained results showed that for the eight analysed samples, the concentration of both elements after solubilisation in HCl solution were below the LOQ (<16.2 ng g(-1) for As and <7.1 ng g(-1) for Sb). These values correspond to the limits of analytical concentrations of As and Sb established by INMETRO and the Brazilian Association of Technical Standards (ABNT). The determined concentrations of As and Sb guarantee the safety (with regards to these elements) for children when using the analysed paint samples since they do not cause any health risk. The analytical method for the determination of the total and bioavailable As and Sb in children's paints was efficient, accurate and precise.	[Avila, Dayara Virginia L.; Souza, Sidnei Oliveira; Araujo, Rennan G. O.] Univ Fed Bahia, Dept Quim Analit, Inst Quim, BR-40170270 Salvador, BA, Brazil; [Souza, Sidnei Oliveira] Univ Fed Sergipe, Campus Lagarto, BR-49400000 Lagarto, Sergipe, Brazil; [Cerda, Victor] Univ Balearic Isl, Grp Analyt Chem Automat & Environm, Dept Chem, E-07122 Palma De Mallorca, Spain; [Araujo, Rennan G. O.] Univ Fed Bahia, Inst Nacl Ciancia & Tecnol, Energia & Ambiente, BR-40170290 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal de Sergipe; Universitat de les Illes Balears; Universidade Federal da Bahia	Araujo, RGO (autor correspondente), Univ Fed Bahia, Dept Quim Analit, Inst Quim, BR-40170270 Salvador, BA, Brazil.; Araujo, RGO (autor correspondente), Univ Fed Bahia, Inst Nacl Ciancia & Tecnol, Energia & Ambiente, BR-40170290 Salvador, BA, Brazil.	rgoa01@terra.com	ÁVILA, DAYARA VIRGÍNIA LINO/AAS-8503-2020; de Oliveira Souza, Sidnei/AAA-5234-2020; Ávila, Dayara/ABE-6154-2020	ÁVILA, DAYARA VIRGÍNIA LINO/0000-0002-2950-6430; OLIVEIRA ARAUJO, RENNAN GEOVANNY/0000-0001-6955-8115	FundacAo de Amparo a Pesquisa do Estado da Bahia (FAPESB, Salvador, Brazil); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brasilia, Brazil); CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES, Brasilia, Brazil) [001]; Spanish Agencia Estatal de Investigacion (AEI); European Funds for Regional Development (FEDER) [CTQ2016-77155-R]	FundacAo de Amparo a Pesquisa do Estado da Bahia (FAPESB, Salvador, Brazil); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brasilia, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES, Brasilia, Brazil); Spanish Agencia Estatal de Investigacion (AEI); European Funds for Regional Development (FEDER)(European Commission)	The authors are grateful for the infrastructure, scholarships and financial resources for research provided by the FundacAo de Amparo a Pesquisa do Estado da Bahia (FAPESB, Salvador, Brazil) and the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Brasilia, Brazil). This study was also financed in part by the CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES, Brasilia, Brazil) - Finance Code 001. The Spanish Agencia Estatal de Investigacion (AEI) and the European Funds for Regional Development (FEDER) are gratefully acknowledged for financial support through Project CTQ2016-77155-R.	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G. M., 2015, NATL I PUBLIC HLTH E; Zhao D, 2018, ENVIRON RES, V167, P299, DOI 10.1016/j.envres.2018.07.036	29	1	1	0	9	ROYAL SOC CHEMISTRY	CAMBRIDGE	THOMAS GRAHAM HOUSE, SCIENCE PARK, MILTON RD, CAMBRIDGE CB4 0WF, CAMBS, ENGLAND	1759-9660	1759-9679		ANAL METHODS-UK	Anal. Methods	MAY 28	2020	12	20					2621	2630		10.1039/c9ay02779c	http://dx.doi.org/10.1039/c9ay02779c			10	Chemistry, Analytical; Food Science & Technology; Spectroscopy	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Food Science & Technology; Spectroscopy	LU6MK	32930289				2023-06-23	WOS:000537867200010
J	Renac, C; Barats, A; Mexias, A; Barriere, J; Rozmaric, M; Gerbe, MC				Renac, Christophe; Barats, Aurelie; Mexias, Andre; Barriere, Jerome; Rozmaric, Martina; Gerbe, Marie-Christine			Oxic and post-oxic chemical changes related to eogenesis and mesogenesis in a Miocene paleolake	JOURNAL OF PALEOLIMNOLOGY			English	Article						Miocene; Eogenesis to mesogenesis; Oxic and anoxic cement; Geochemistry	SULFUR ISOTOPE FRACTIONATION; ELEMENT GEOCHEMISTRY; SULFIDE OXIDATION; HYDROGEN-SULFIDE; ARSENIC RELEASE; BASIN; LAKE; CHEMISTRY; DISPROPORTIONATION; REDUCTION	In the Forez Basin of the French Massif Central, clay-rich alluvial deposits include a series of red- and green-colored sediments and carbonate cement that record evaporation and oxidizing/reducing conditions related to intra-continental climate during the Early to Middle Miocene. The mineralogy, chemistry and relative chronology of authigenic calcite-ankerite, ferroan dolomite, pyrite, and analcite-clinoptilolite in clay-rich sediment enabled reconstruction of a series of processes related to deposition, eogenesis, and mesogenesis. The low-Mg calcite, ankerite, and ferroan-dolomite cement, systematically associated with zeolites (analcite and clinoptilolite), represent eogenetic precipitation associated with oxic to post-oxic water with Ca-Fe-Mg carbonic, then Na-Al-Si(OH)(4)-rich water. Occurrence of framboidal and cubic pyrites with low-Mg calcite and analcite is related to post-oxic conditions associated with deposition, eogenesis and times of early mesogenesis. Changes in the morphology, size, and chemistry of framboidal and cubic pyrite grains were related to reducing-oxidizing cycles and to the growth of grains. Sulfur isotope measures on framboidal and cubic pyrite suggest that both morphologies are related to bacterial reduction of SO(4)(2-)to H2S and HS-1. With the exception of some sample depths (0-40 m below surface), similar chemical contents (trace elements [TE], rare earth elements [REE] and platinoids) suggest a similar, constant reservoir of metal and metalloids associated with the clayey sediment and volcanic fragments. Moreover, the TE and REE chemistry of cubic pyrite, in contrast to carbonates, indicates growth of pyrite during eogenesis to mesogenesis stages. The mineralogical and chemical changes are interpreted as reflecting dissolution of iron oxyhydroxides, rather than ankerite and ferroan-dolomite. Chemical elements from dissolution of iron oxyhydroxides would have mixed with hydrogen monosulfide and contributed to the growth of cubic pyrite. The crystal size distributions of pyrite grains suggest a closed system with surface-controlled growth. Assuming those conditions, the growth time of framboidal to cubic pyrite, based on diffusion of HS(-1)in the clay-rich sediments, was estimated to have been from several days to a few years, to as much as 500 years (mm-scale pyrite).	[Renac, Christophe; Barats, Aurelie] Univ Cote dAzur, Observ Cote DAzur, IRD, CNRS,Geoazur,UMR 7329, 250 Rue Albert Einstein, F-06560 Valbonne, France; [Mexias, Andre] Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500 Campus Vale, Porto Alegre, RS, Brazil; [Barriere, Jerome] HYDRO INVEST, 514 Route DAgris, F-16430 Champniers, France; [Rozmaric, Martina] IAEA Environm Labs, 4a Quai Antoine 1er, MC-98000 Monaco, Principality Of, Monaco; [Gerbe, Marie-Christine] Univ N, UJM St Etienne, UMR 6524, Lab Magmas & Volcans,CNRS, F-42023 St Etienne, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Institut de Recherche pour le Developpement (IRD); UDICE-French Research Universities; Universite Cote d'Azur; Observatoire de la Cote d'Azur; Universidade Federal do Rio Grande do Sul; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Institut de Recherche pour le Developpement (IRD); Universite Clermont Auvergne (UCA); Universite Jean Monnet	Renac, C (autor correspondente), Univ Cote dAzur, Observ Cote DAzur, IRD, CNRS,Geoazur,UMR 7329, 250 Rue Albert Einstein, F-06560 Valbonne, France.	christophe.renac@unice.fr	Barriere, Jerome/AAP-2174-2021	Barriere, Jerome/0000-0002-9077-1639; Renac, Christophe/0000-0002-9278-6500				Arenas C, 1999, SEDIMENT GEOL, V125, P23, DOI 10.1016/S0037-0738(98)00146-8; Bhat HL, 2014, INTRO CRYSTAL GROWTH; Bottcher ME, 1998, CHEM GEOL, V146, P127, DOI 10.1016/S0009-2541(98)00004-7; Bottcher ME, 2001, GEOCHIM COSMOCHIM AC, V65, P1573, DOI 10.1016/S0016-7037(00)00622-0; Burley SD., 1985, GEOLOGICAL SOC LONDO, V18, P189, DOI [10.1144/GSL.SP.1985.018.01.10, DOI 10.1144/GSL.SP.1985.018.01.10]; Canfield DE, 2004, AM J SCI, V304, P839, DOI 10.2475/ajs.304.10.839; Canfield DE, 2001, REV MINERAL GEOCHEM, V43, P607, DOI 10.2138/gsrmg.43.1.607; Canfield DE, 1998, LIMNOL OCEANOGR, V43, P253, DOI 10.4319/lo.1998.43.2.0253; Canfield DE, 2010, GEOLOGY, V38, P415, DOI 10.1130/G30723.1; 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Paleolimn.	OCT	2020	64	3					193	210		10.1007/s10933-020-00131-3	http://dx.doi.org/10.1007/s10933-020-00131-3		MAY 2020	18	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	NI3AX					2023-06-23	WOS:000558858800001
J	Horak-Terra, I; Cortizas, AM; Da Luz, CFP; Silva, AC; Mighall, T; De Camargo, PB; Mendonca, CV; De Oliveira, PE; Cruz, FW; Vidal-Torrado, P				Horak-Terra, Ingrid; Martinez Cortizas, Antonio; Pinto Da Luz, Cynthia Fernandes; Silva, Alexandre Christofaro; Mighall, Tim; De Camargo, Plinio Barbosa; Mendonca-Filho, Carlos Victor; De Oliveira, Paulo Eduardo; Cruz, Francisco Willian; Vidal-Torrado, Pablo			Late Quaternary vegetation and climate dynamics in central-eastern Brazil: insights from a similar to 35k cal a bp peat record in the Cerrado biome	JOURNAL OF QUATERNARY SCIENCE			English	Article						geochemistry; paleoclimatology; peatlands; pollen; stable isotopes	AMERICAN SUMMER MONSOON; POLLEN RECORD; MINAS-GERAIS; MERCURY ACCUMULATION; CARBON ISOTOPES; TRACE-ELEMENTS; INSOLATION; SOUTHERN; FRUTA; SERRA	The late Quaternary evolution of central-eastern Brazil has been under-researched. Questions remain as to the origin of the Cerrado, a highly endangered biome, and other types of vegetation, such as the Capoes - small vegetation islands of semi-deciduous and mountain forests. We investigated the factors that influenced the expansion and contraction of the Cerrado and Capoes during the late Quaternary (last similar to 35 ka), using a multi-proxy approach: stable isotopes (delta C-13, delta N-15), geochemistry, pollen and multivariate statistics derived from a peat core (Pinheiro mire, Serra do Espinhaco Meridional). Five major shifts in precipitation, temperature, vegetation and landscape stability occurred at different timescales. Our study revealed that changes in the South Atlantic Convergence Zone (SACZ) seem to have been coeval with these shifts: from the Late Glacial Maximum to mid-Holocene the SACZ remained near (similar to 29.6 to similar to 16.5k cal a bp) and over (similar to 16.5 to similar to 6.1 k cal a bp) the study area, providing humidity to the region. This challenges previous research which suggested that climate was drier for this time period. At present, the Capoes are likely to be a remnant of a more humid climate; meanwhile, the Cerrado biome seems to have stablished in the late Holocene, after similar to 3.1 k cal a bp.	[Horak-Terra, Ingrid] Univ Fed Vales Jequitinhonha & Mucuri ICA UFVJM, Inst Ciencias Agr, BR 251 Av Univ 1000, BR-38610000 Unai, MG, Brazil; [Martinez Cortizas, Antonio] Univ Santiago de Compostela USC, Fac Biol, EcoPast GI 1553, Santiago De Compostela 15782, Spain; [Pinto Da Luz, Cynthia Fernandes] Secretaria Infraestrutura & Meio Ambiente Estado, Inst Bot, Nuc Pesquisa Palinol, BR-04301902 Sao Paulo, SP, Brazil; [Silva, Alexandre Christofaro] Univ Fed Vales Jequitinhonha & Mucuri UFVJM, Dept Engn Florestal, BR-39100000 Diamantina, MG, Brazil; [Mighall, Tim] Univ Aberdeen, Sch Geosci, G22 St Marys, Aberdeen, Scotland; [De Camargo, Plinio Barbosa] Ctr Energia Nucl Agr CENA USP, Lab Ecol Isotop, BR-13416903 Piracicaba, SP, Brazil; [Mendonca-Filho, Carlos Victor] Univ Fed Vales Jequitinhonha & Mucuri UFVJM, Dept Ciencias Biol, BR-39100000 Diamantina, MG, Brazil; [De Oliveira, Paulo Eduardo; Cruz, Francisco Willian] Inst Geociencias IGc USP, Dept Geol Sedimentar & Ambiental, BR-05508080 Sao Paulo, SP, Brazil; [Vidal-Torrado, Pablo] Escola Super Agr Luiz de Queiroz ESALQ USP, Dept Ciencia Solo, BR-13418900 Piracicaba, SP, Brazil	Universidade de Santiago de Compostela; Instituto de Botanica - Sao Paulo; Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM); University of Aberdeen; Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM)	Horak-Terra, I (autor correspondente), Univ Fed Vales Jequitinhonha & Mucuri ICA UFVJM, Inst Ciencias Agr, BR 251 Av Univ 1000, BR-38610000 Unai, MG, Brazil.	ingrid.horak@ufvjm.edu.br	Vidal-Torrado, Pablo/C-4020-2012; Luz, Cynthia Fernandes Pinto da/A-8539-2008; Martínez-Cortizas, Antonio/M-6196-2015; de Camargo, Plínio B./D-6635-2012; Cruz, Francisco W/G-6059-2012; Horák-Terra, Ingrid/G-8463-2012	Vidal-Torrado, Pablo/0000-0001-9228-9910; Luz, Cynthia Fernandes Pinto da/0000-0001-7908-155X; Martínez-Cortizas, Antonio/0000-0003-0430-5760; de Camargo, Plínio B./0000-0002-0696-3778; Cruz, Francisco/0000-0002-4030-4581; Horak-Terra, Ingrid/0000-0002-5078-5366	FundacAo de Amparo a Pesquisa do Estado de SAo Paulo (FAPESP)/Brazil [FAPESP 2010/51637-0, BEPE/FAPESP 2012/00676-1]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)/Brazil [14/2011-482815/2001-6]; Ministerio de Economia y Competitividad [CGL2010-20662]; Xunta de Galicia [10PXIB200182PR, ED431D2917/08, ED431B2018/20]	FundacAo de Amparo a Pesquisa do Estado de SAo Paulo (FAPESP)/Brazil(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)/Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Ministerio de Economia y Competitividad(Spanish Government); Xunta de Galicia(Xunta de Galicia)	This work was supported by FundacAo de Amparo a Pesquisa do Estado de SAo Paulo (FAPESP)/Brazil (grant to I.H.T. - regular doctoral scholarship FAPESP 2010/51637-0 and research internships abroad BEPE/FAPESP 2012/00676-1), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)/Brazil (Universal 14/2011-482815/2001-6), Ministerio de Economia y Competitividad (CGL2010-20662) and Xunta de Galicia (10PXIB200182PR, ED431D2917/08 and ED431B2018/20). 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Quat. Sci.	JUL	2020	35	5					664	676		10.1002/jqs.3209	http://dx.doi.org/10.1002/jqs.3209		MAY 2020	13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	LZ5KH		Green Submitted			2023-06-23	WOS:000533997600001
J	Buch, AC; Sautter, KD; Marques, ED; Silva, EV				Buch, Andressa Cristhy; Sautter, Klaus Dieter; Marques, Eduardo Duarte; Silva-Filho, Emmanoel Vieira			Ecotoxicological assessment after the world's largest tailing dam collapse (Fundao dam, Mariana, Brazil): effects on oribatid mites	ENVIRONMENTAL GEOCHEMISTRY AND HEALTH			English	Article						Bioaccumulation; Mine tailings; Mite density; Scheloribates praeincisus; Trace metals; Tropical soil	SCHELORIBATES-PRAEINCISUS ACARI; METAL ACCUMULATION; CONTAMINATED SOILS; SPECIES-DIVERSITY; COMMUNITIES; TOXICITY; CADMIUM; MERCURY; FOREST; MINE	Worldwide, environmental tragedies involving mining dam ruptures have become more frequent. As occurred a few years ago in Brazil (on 5 November 2015, in Minas Gerais state) the Fundao Dam rupture released 60 million m(3) of tailings into terrestrial and aquatic ecosystems. Since then, little information on the ecotoxicity of these tailings has been disclosed. In the laboratory, the acute, chronic and bioaccumulation effects of increased Fundao tailing concentrations on oribatid mites (Scheloribates praeincisus) were assessed. Additionally, the bioaccumulation of 11 trace metals (Al, As, Cd, Cr, Cu, Fe, Hg, Mn, Ni, Pb and Zn) and the total density of oribatid mites found in the areas contaminated by the Fundao tailings were determined. The percentages of mite survival and reproductive inhibition were higher than 60% and 80%, respectively, in all contaminated areas with the highest concentration (100% mine tailings). Field studies showed an expressive reduction in the total density of oribatids per m(-2) (up to 54 times) in the contaminated areas compared with the reference area. Metal accumulations in the field were 5.4 and 3.2 higher (for Ni and Hg, respectively) and up to two times higher (for most metals) than those in the laboratory for 42 days. The mite responses to the Fundao tailings found in this study suggest long-term interference in their biological development. In this sense, we can conclude that the introduction of mine tailings onto soils tended to compromise the functionality of the mites in the ecosystem, which causes imbalances to cascade other organisms of the trophic web. [GRAPHICS] .	[Buch, Andressa Cristhy; Silva-Filho, Emmanoel Vieira] Fluminense Fed Univ, Dept Environm Geochem, Outeiro Sao Joao Baptista S-N, BR-24020007 Niteroi, RJ, Brazil; [Sautter, Klaus Dieter] Univ Ctr Campos Andrade, R Joao Scuissiato 01, BR-81220090 Curitiba, PR, Brazil; [Marques, Eduardo Duarte] CPRM Geol Survey Brazil, Av Brasil 1731, BR-30140002 Belo Horizonte, MG, Brazil	Universidade Federal Fluminense	Buch, AC (autor correspondente), Fluminense Fed Univ, Dept Environm Geochem, Outeiro Sao Joao Baptista S-N, BR-24020007 Niteroi, RJ, Brazil.	andressabuch@hotmail.com	da Silva Filho, Emmanoel Vieira/Y-7281-2019	da Silva Filho, Emmanoel Vieira/0000-0001-6444-6851; Duarte Marques, Eduardo/0000-0003-1133-9408	FundacAo Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [202.453/2017]; CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	FundacAo Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was supported by FundacAo Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) with a scholarship to A. Buch (202.453/2017) and CoordenacAo de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001. The authors are grateful to Universidade Federal Fluminense (UFF), Empresa brasileira de Pesquisa Agropecuaria (EMBRAPA), Empresa de Assistencia Tecnica e ExtensAo Rural (EMATER-MG) and Companhia de Pesquisa de Recursos Minerais (CPRM-MG). The authors also thank Bianca Prestes for help with laboratory and field work and Tales de Campo Piedade, who helped with digital satellite image processing.	Agnieszka B, 2014, ECOTOXICOLOGY, V23, P1234, DOI 10.1007/s10646-014-1266-y; Aquino A. 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Árvore, V27, P393, DOI 10.1590/S0100-67622003000300017; Canovas CR, 2019, CHEMOSPHERE, V216, P19, DOI 10.1016/j.chemosphere.2018.09.018; Sanchez L.E., 2018, 1 IUCN; Schneider K., 2004, PHYTOPHAGA-PALERMO, P247; Seniczak A, 2002, EUR J SOIL BIOL, V38, P315, DOI 10.1016/S1164-5563(02)01166-4; Seniczak S, 1997, WATER AIR SOIL POLL, V94, P71, DOI 10.1023/A:1026427910943; Simoes RA, 2008, EXP APPL ACAROL, V44, P239, DOI 10.1007/s10493-008-9139-9; Skubala P, 2004, ENVIRON POLLUT, V132, P51, DOI 10.1016/j.envpol.2004.03.025; Skubala P, 2012, SCI TOTAL ENVIRON, V414, P364, DOI 10.1016/j.scitotenv.2011.11.006; Subias LS, 2004, GRAELLSIA, V60, P303; USDA-United States Department of Agriculture, 2017, PINT VALL MIN ENV IM, P219; USEPA - United States Environmental Protection Agency, 2001, 2007 USEPA; USEPA - United States Environmental Protection Agency, 1994, 2008 USEPA; USEPA - United States Environmental Protection Agency, 1986, 7471A USEPA; van Straalen NM, 2001, PEDOBIOLOGIA, V45, P451, DOI 10.1078/0031-4056-00099; VANSTRAALEN NM, 1989, ECOTOX ENVIRON SAFE, V17, P190, DOI 10.1016/0147-6513(89)90038-9; Wahl JJ, 2012, ECOTOX ENVIRON SAFE, V86, P250, DOI 10.1016/j.ecoenv.2012.09.027; Zaitsev AS, 2001, PEDOBIOLOGIA, V45, P467, DOI 10.1078/0031-4056-00100	77	8	8	0	15	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0269-4042	1573-2983		ENVIRON GEOCHEM HLTH	Environ. Geochem. Health	NOV	2020	42	11					3575	3595		10.1007/s10653-020-00593-4	http://dx.doi.org/10.1007/s10653-020-00593-4		MAY 2020	21	Engineering, Environmental; Environmental Sciences; Public, Environmental & Occupational Health; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology; Public, Environmental & Occupational Health; Water Resources	ON7AN	32409973				2023-06-23	WOS:000532879500001
J	Ferreira, ACD; Dantas, EL; Fuck, RA; Nedel, IM				Ferreira, Alanielson C. D.; Dantas, Elton L.; Fuck, Reinhardt A.; Nedel, Ingrid M.			Arc accretion and crustal reworking from late Archean to Neoproterozoic in Northeast Brazil	SCIENTIFIC REPORTS			English	Article							WEST-AFRICAN CRATON; BORBOREMA PROVINCE; CONTINENTAL-CRUST; NE BRAZIL; AGE DISTRIBUTION; EVOLUTION; GROWTH; GENERATION; GEOCHRONOLOGY; METAMORPHISM	New systematic Nd isotope and U-Pb geochronology data were applied to Precambrian rocks of northeastern Brazil to produce a crustal-age distribution map for a small basement inlier (1,500 km(2)). The results support episodic crustal growth with five short periods of crustal formation at ca. 2.9 Ga, 2.65 Ga, 2.25 Ga, 2.0 Ga, and 0.6 Ga. Based on the frequency histogram of U-Pb zircon ages and Nd isotopic data, we suggest that about 60% of the continental crust was formed during the Archean between 2.9 Ga and 2.65 Ga. The remaining 40% of crust was generated during the Rhyacian to Neoproterozoic (similar to 2.0-0.6 Ga). This overall continental growth is manifested by accretionary processes that involved successive accretions surrounding an older core, becoming younger toward the margin. Strikingly, this repetitive history of terrane accretion show a change from lithospheric peeling dominated accretionary setting during the late Archean to a more, modern-day akin style of arc-accretion during the Proterozoic. Similar tectonic processes are observed only in large continental areas (>1,000,000 km(2)) as in the North American continent basement and in the Amazonian Craton.	[Ferreira, Alanielson C. D.; Dantas, Elton L.; Fuck, Reinhardt A.; Nedel, Ingrid M.] Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia	Ferreira, ACD (autor correspondente), Univ Brasilia UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil.	ferreira.acd@gmail.com	Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059; Moerschberger Nedel, Ingrid/0000-0002-8070-5320; Ferreira, Alanielson/0000-0001-8054-0047	INCT Estudos Tectonicos [CAPES/CNPq -465613/2014-4, FAPDF -193.001.263/2017]; CNPq research fellowships	INCT Estudos Tectonicos; CNPq research fellowships(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF))	This study is part of the first author's Ph.D. thesis developed at the Institute of Geosciences, Universidade de Brasilia. The authors acknowledge support from INCT Estudos Tectonicos (CAPES/CNPq -465613/2014-4 and FAPDF -193.001.263/2017). IMN, ELD and RAF acknowledge CNPq research fellowships. The authors would like to warmly thank Chris Hawkesworth and an anonymous reviewer for their valuable contributions.	Albarede F, 2004, GEOCHIM COSMOCHIM AC, V68, P2725, DOI 10.1016/j.gca.2003.11.024; Archanjo CJ, 2013, GONDWANA RES, V23, P701, DOI 10.1016/j.gr.2012.05.005; BRITO NEVES B. B., 2014, PRECAMBRIAN RES, V244, P75, DOI DOI 10.1016/J.PRECAMRES.2013.09.020; Brito Neves B.B., 2000, P 31 INT GEOL C, P151; Brown M., 2008, CHARACTERISTIC THERM; Brown M, 2020, ANNU REV EARTH PL SC, V48, P291, DOI 10.1146/annurev-earth-081619-052705; Brown M, 2019, AM MINERAL, V104, P1065, DOI 10.2138/am-2019-6956; Buhn B, 2009, AN ACAD BRAS CIENC, V81, P99, DOI 10.1590/S0001-37652009000100011; Caro G, 2017, EARTH PLANET SC LETT, V457, P23, DOI 10.1016/j.epsl.2016.09.051; Cawood PA, 2013, GEOL SOC AM BULL, V125, P14, DOI 10.1130/B30722.1; Cawood PA, 2009, GEOL SOC SPEC PUBL, V318, P1, DOI 10.1144/SP318.1; Chowdhury P, 2020, EARTH PLANET SC LETT, V538, DOI 10.1016/j.epsl.2020.116224; Chowdhury P, 2017, NAT GEOSCI, V10, P698, DOI [10.1038/NGEO3010, 10.1038/ngeo3010]; Cloos M., 1988, PALEOPHYSICS, V128, P501; Condie K, 2015, PRECAMBRIAN RES, V259, P278, DOI 10.1016/j.precamres.2014.07.015; Condie KC, 2013, GONDWANA RES, V23, P394, DOI 10.1016/j.gr.2011.09.011; CONEY PJ, 1980, NATURE, V288, P329, DOI 10.1038/288329a0; Corfu F, 2003, REV MINERAL GEOCHEM, V53, P469, DOI 10.2113/0530469; Dantas EL, 2013, PRECAMBRIAN RES, V227, P120, DOI 10.1016/j.precamres.2012.08.006; Ferreira ADD, 2020, GEOSCI FRONT, V11, P2221, DOI 10.1016/j.gsf.2020.03.004; DEPAOLO DJ, 1991, J GEOPHYS RES-SOLID, V96, P2071, DOI 10.1029/90JB02219; DEPAOLO DJ, 1981, J GEOPHYS RES, V86, P470, DOI 10.1029/JB086iB11p10470; Eglinger A, 2017, PRECAMBRIAN RES, V292, P258, DOI 10.1016/j.precamres.2016.11.012; Ferreira A. 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D., 2019, THESIS; Ferreira ADD, 2019, J GEOL, V127, P483, DOI 10.1086/704256; Gioia SMCL, 2000, AN ACAD BRAS CIENC, V72, P219, DOI 10.1590/S0001-37652000000200009; Hawkesworth C, 2019, GEOSCI FRONT, V10, P165, DOI 10.1016/j.gsf.2018.02.004; Hawkesworth CJ, 2017, ANNU REV EARTH PL SC, V45, P169, DOI 10.1146/annurev-earth-063016-020525; Holder RM, 2019, NATURE, V572, P378, DOI 10.1038/s41586-019-1462-2; Hollanda MHBM, 2015, PRECAMBRIAN RES, V258, P186, DOI 10.1016/j.precamres.2014.12.009; Hollanda MHBM, 2011, J S AM EARTH SCI, V32, P287, DOI 10.1016/j.jsames.2011.02.008; Jackson SE, 2004, CHEM GEOL, V211, P47, DOI 10.1016/j.chemgeo.2004.06.017; Jardim de Sa E.F., 1994, THESIS U BRASILIA; Johnson TE, 2017, NATURE, V543, P239, DOI 10.1038/nature21383; Korenaga J, 2018, EARTH PLANET SC LETT, V482, P388, DOI 10.1016/j.epsl.2017.11.039; Laurent O, 2020, NAT GEOSCI, V13, P163, DOI 10.1038/s41561-019-0520-6; Ludwig K.R., 2008, USERS MANUAL ISOPLOT; MCLENNAN SM, 1992, GEOCHIM COSMOCHIM AC, V56, P887, DOI 10.1016/0016-7037(92)90034-G; Moresi L, 2014, NATURE, V508, P245, DOI 10.1038/nature13033; Moyen JF, 2012, LITHOS, V148, P312, DOI 10.1016/j.lithos.2012.06.010; Nance RD, 2014, GONDWANA RES, V25, P4, DOI 10.1016/j.gr.2012.12.026; Nebel O, 2018, PHILOS T R SOC A, V376, DOI 10.1098/rsta.2018.0103; Nebel-Jacobsen Y, 2018, SCI REP-UK, V8, DOI 10.1038/s41598-018-19397-9; Oliveira EP, 2019, PRECAMBRIAN RES, V331, DOI 10.1016/j.precamres.2019.105366; Palin RM, 2016, PRECAMBRIAN RES, V287, P73, DOI 10.1016/j.precamres.2016.11.001; Rollinson H, 2018, J AFR EARTH SCI, V143, P28, DOI 10.1016/j.jafrearsci.2018.03.018; Rollinson H, 2010, GEOLOGY, V38, P1083, DOI 10.1130/G31159.1; Rosas JC, 2018, EARTH PLANET SC LETT, V494, P42, DOI 10.1016/j.epsl.2018.04.051; Santos LCMD, 2018, TECTONICS, V37, P2727, DOI 10.1029/2018TC005130; Della Giustina MES, 2011, LITHOS, V124, P82, DOI 10.1016/j.lithos.2010.11.004; Sizova E, 2015, PRECAMBRIAN RES, V271, P198, DOI 10.1016/j.precamres.2015.10.005; Stern RJ, 2018, PHILOS T R SOC A, V376, DOI 10.1098/rsta.2017.0406; Stern RJ, 2010, INT GEOL REV, V52, P1, DOI 10.1080/00206810903332322; SUTTON J, 1963, NATURE, V198, P731, DOI 10.1038/198731b0; Tetreault JL, 2014, SOLID EARTH, V5, P1243, DOI 10.5194/se-5-1243-2014; Van Schmus WR, 2008, GEOL SOC SPEC PUBL, V294, P69, DOI 10.1144/SP294.5; Wiedenbeck M, 2004, GEOSTAND GEOANAL RES, V28, P9, DOI 10.1111/j.1751-908X.2004.tb01041.x	57	11	13	0	0	NATURE PORTFOLIO	BERLIN	HEIDELBERGER PLATZ 3, BERLIN, 14197, GERMANY	2045-2322			SCI REP-UK	Sci Rep	MAY 12	2020	10	1							7855	10.1038/s41598-020-64688-9	http://dx.doi.org/10.1038/s41598-020-64688-9			12	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	NA4IJ	32398674	Green Published, gold			2023-06-23	WOS:000559780100025
J	Marquetto, L; Kaspari, S; Simoes, JC				Marquetto, Luciano; Kaspari, Susan; Simoes, Jefferson Cardia			Refractory black carbon (rBC) variability in a 47-year West Antarctic snow and firn core	CRYOSPHERE			English	Article							ICE-CORE; SOUTH-POLE; CLIMATE; DEPOSITION; EMISSIONS; DUST; AEROSOLS; SURFACE; RECORD; SAMPLES	Black carbon (BC) is an important climate-forcing agent that affects snow albedo. In this work, we present a record of refractory black carbon (rBC) variability, measured from a 20m deep snow and firn core drilled in West Antarctica (79 degrees 55'34.6'' S, 94 degrees 21'13.3'' W, 2122m above sea level) during the 2014-2015 austral summer. This is the highest elevation rBC record from West Antarctica. The core was analyzed using the Single Particle Soot Photometer (SP2) coupled to a CETAC Marin-5 nebulizer. Results show a well-defined seasonality with geometric mean concentrations of 0.015 mu g L-1 for the wet season (austral summer-fall) and 0.057 mu g L-1 for the dry season (austral winter-spring). The core was dated to 47 years (1968-2015) using rBC seasonality as the main parameter, along with sodium (Na), sulfur (S) and strontium (Sr) variations. The annual rBC concentration geometric mean was 0.03 mu g L-1, the lowest of all rBC cores in Antarctica referenced in this work, while the annual rBC flux was 6.25 mu g m(-2) a(-1), the lowest flux in West Antarctica rBC records. No long-term trend was observed. Snow albedo reductions at the site due to BC were simulated using SNICAR online and found to be insignificant (-0.48 %) compared to clean snow. Fire spot inventory and BC emission estimates from the Southern Hemisphere suggest Australia and Southern Hemisphere South America as the most probable emission sources of BC to the drilling site, whereas HYSPLIT model particle transport simulations from 1968 to 2015 support Australia and New Zealand as rBC sources, with limited contributions from South America. Spectral analysis (REDFIT method) of the BC record showed cycles related to the Antarctic Oscillation (AAO) and to El Nino-Southern Oscillation (ENSO), but cycles in common with the Amundsen Sea Low (ASL) were not detected. Correlation of rBC records in Antarctica with snow accumulation, elevation and distance to the sea suggests rBC transport to East Antarctica is different from transport to West Antarctica.	[Marquetto, Luciano; Kaspari, Susan] Cent Washington Univ, Dept Geol Sci, Ellensburg, WA 98926 USA; [Marquetto, Luciano; Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul, Ctr Polar & Climat, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil; [Simoes, Jefferson Cardia] Univ Maine, Climate Change Inst, Orono, ME 04469 USA	Central Washington University; Universidade Federal do Rio Grande do Sul; University of Maine System; University of Maine Orono	Marquetto, L (autor correspondente), Cent Washington Univ, Dept Geol Sci, Ellensburg, WA 98926 USA.; Marquetto, L (autor correspondente), Univ Fed Rio Grande do Sul, Ctr Polar & Climat, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil.	luciano.marquetto@gmail.com	Simoes, Jefferson Cardia/D-7232-2013	Simoes, Jefferson Cardia/0000-0001-5555-3401	Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program [200386/20182]; CNPq [465680/2014-3, 442761/2018-0]; CAPES [88887.136384/2017-00, 88887.314450/2019-00]	Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This research is part of the Brazilian Antarctic Program (PROANTAR) and was financed with funds from the Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program (no. 200386/20182), from the CNPq projects 465680/2014-3 and 442761/2018-0, CAPES project "INCT da Criosfera" 88887.136384/2017-00 and PROANTAR project 88887.314450/2019-00.	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J	Salum, RB; Souza, PWM; Simard, M; Silva, CA; Fernandes, MEB; Cougo, MF; do Nascimento, W; Rogers, K				Salum, Rafaela B.; Souza-Filho, Pedro Walfir M.; Simard, Marc; Silva, Carlos Alberto; Fernandes, Marcus E. B.; Cougo, Michele F.; do Nascimento Junior, Wilson; Rogers, Kerrylee			Improving mangrove above-ground biomass estimates using LiDAR	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Mangrove; LiDAR; Above-ground biomass; Allometry; Blue carbon	BIOPHYSICAL PARAMETERS; CANOPY HEIGHT; CARBON STOCKS; BLUE CARBON; FORESTS; ECOSYSTEMS; ICESAT/GLAS; VEGETATION; DYNAMICS; IMAGERY	Tree height is a key parameter to accurately quantify above ground biomass (AGB) of trees. Approaches that integrate airborne light detection and ranging (LiDAR) with mapped extents of forests may improve estimation of mangrove heights by providing considerably more measurements of mangrove tree heights than can be achieved using field-based measurements alone. In this study, we present a validated method for quantifying mangrove AGB that was demonstrated for a mangrove forest at Guar.as Island, Brazil. The application of LiDAR to estimate mangrove height was confirmed by correlating 89 tree heights measured in the field with LiDAR-derived mangrove heights, resulting in highly robust relationships for Avicennia germinans, Laguncularia racemosa and Rhizophora mangle (R-2 = 0.90-0.97, RMSE of 1.24-0.67 m and RMSE% of 11.26%-25.97%). These relationships were used to calibrate a LiDAR-derived canopy height model (CHM) and develop robust relationships between the calibrated-CHM and field-based estimates of AGB (R-2 = 0.85-0.92, RMSE of 3.1 kg-42.53 kg, RMSE% of 20.66%-43.81%). This relationship was then applied to the CHM whilst accounting for tree density to estimate mangrove AGB. Total mangrove AGB per hectare was estimated to be 246.90 t ha(-1), corresponding closely with previous mangrove AGB measurements within the region. This study found that mangrove height and AGB are statistically related and these relationships can be applied to allometric equations for specific species to improve mangrove AGB estimates. This study demonstrates the capacity for LiDAR-derived tree heights to replace traditional approaches to estimating AGB and improving estimates of mangrove blue carbon storage. Application of LiDAR to determine tree heights will be particularly useful where mangrove is extensive and/or remote.	[Salum, Rafaela B.; Rogers, Kerrylee] Univ Wollongong, Sch Earth Atmospher & Life Sci, Northfields Ave, Wollongong, NSW 2522, Australia; [Souza-Filho, Pedro Walfir M.; do Nascimento Junior, Wilson] Vale Inst Tecnol, Rua Boaventura Silva 955, BR-66055090 Belem, Para, Brazil; [Salum, Rafaela B.; Souza-Filho, Pedro Walfir M.; Cougo, Michele F.] Univ Fed Para, Geosci Inst, BR-66075110 Belem, Para, Brazil; [Simard, Marc; Silva, Carlos Alberto] Jet Prop Lab, MS 300-227,4800 Oak Grove Dr, Pasadena, CA 91109 USA; [Fernandes, Marcus E. B.] Univ Fed Para, Coastal Studies Inst, BR-68600000 Braganca, Para, Brazil	University of Wollongong; Universidade Federal do Para; National Aeronautics & Space Administration (NASA); NASA Jet Propulsion Laboratory (JPL); Universidade Federal do Para	Rogers, K (autor correspondente), Univ Wollongong, Sch Earth Atmospher & Life Sci, Northfields Ave, Wollongong, NSW 2522, Australia.	kerrylee@uow.edu.au	Souza-Filho, Pedro Walfir M. M./J-4958-2012; Silva, Carlos Luiz/HPH-3230-2023; Rogers, Kerrylee/AAC-8093-2022; Souza, Pedro/GZH-1275-2022	Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; Silva, Carlos Luiz/0000-0002-7419-1722; Silva, Carlos Alberto/0000-0002-7844-3560; Rogers, Kerrylee/0000-0003-1350-4737	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPESBrazil); Conselho Nacional de Desenvolvimento Cientifico e Tecnol.ogico (CNPq-Brazil); Fundacao de Amparo Desenvolvimento da Pesquisa FADESP; University of Wollongong Global Challenges Program (Blue Carbon Futures)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPESBrazil)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnol.ogico (CNPq-Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo Desenvolvimento da Pesquisa FADESP; University of Wollongong Global Challenges Program (Blue Carbon Futures)	We would like to acknowledge the financial support provided by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPESBrazil), Conselho Nacional de Desenvolvimento Cientifico e Tecnol.ogico (CNPq-Brazil), Fundacao de Amparo Desenvolvimento da Pesquisa FADESP, University of Wollongong Global Challenges Program (Blue Carbon Futures). We also acknowledge LiDAR - Demarcacao de terreno de marinha e seus acrescidos, naturais ou artificiais, por meio da determinacao da posicao da Linha de Preamar M.edia de 1831 - LPM e da Linha dos Terrenos de Marinha - LTM and HGT Geoprocessing, which processed the flights campaign. Scientific support was provided by Universidade Federal do Par.a and University of Wollongong.	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Coast. Shelf Sci.	MAY 5	2020	236								106585	10.1016/j.ecss.2020.106585	http://dx.doi.org/10.1016/j.ecss.2020.106585			16	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	LG2CS					2023-06-23	WOS:000527916100008
J	Schossler, V; Aquino, FE; Reis, PA; Simoes, JC				Schossler, Venisse; Aquino, Francisco E.; Reis, Pedro A.; Simoes, Jefferson C.			Antarctic atmospheric circulation anomalies and explosive cyclogenesis in the spring of 2016	THEORETICAL AND APPLIED CLIMATOLOGY			English	Article							SOUTHERN-HEMISPHERE; AUSTRALIAN RAINFALL; SEA-ICE; CYCLONE CHARACTERISTICS; VARIABILITY; CLIMATOLOGY; BEHAVIOR	This work examines teleconnections between extratropical explosive cyclogenesis and the Antarctic region and its relationship with the Southern Annular Mode (SAM) and with the zonal wave three (ZW3) pattern at the end of October 2016. From 26 to 28 October, an explosive extratropical cyclone developed on the Brazilian southern coast. Then, from the 29th to the 31st, southern Australia, including Tasmania, was hit by an explosive extratropical cyclone originating in the Indian Ocean. Both events caused damages. The year 2016 also stands out as the warmest in the recorded record, both globally and in the Southern Hemisphere; further, in 2016, the smallest Antarctic sea ice extent (SIE) was recorded since 1979. This SIE reduction has been attributed to positive sea surface temperature anomalies, the ZW3 and a SAM negative phase. We reconstructed the geopotential height fields, wind vectors, zonal wind, and temperature using the ERA-Interim reanalysis data. These fields, associated to wave and tidal and wind records, denote that negative SAM and ZW3 influenced both events. This association favored intense cyclogenesis, which included a baroclinic increase in both cases, with well-organized vertical structure; thus, this combination formed meteorological "bombs" as a response to the tropic-pole temperature contrast, and an exceptional atmospheric circulation was observed between subtropical and polar latitudes in 2016.	[Schossler, Venisse; Aquino, Francisco E.; Reis, Pedro A.; Simoes, Jefferson C.] Rio Grande de Sul Fed Univ, Climate & Polar Ctr, Geosci Inst, BR-90650001 Porto Alegre, RS, Brazil		Schossler, V (autor correspondente), Rio Grande de Sul Fed Univ, Climate & Polar Ctr, Geosci Inst, BR-90650001 Porto Alegre, RS, Brazil.	venisse.schossler@ufrgs.br	Simoes, Jefferson Cardia/D-7232-2013	Simoes, Jefferson Cardia/0000-0001-5555-3401	Brazilian National Council for Scientific and Technological Development (CNPq); Foundation for Research of the State of Rio Grande do Sul (FAPERGS) through the Brazilian National Institute for Cryopsheric Sciences (INCT da Criosfera)	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Foundation for Research of the State of Rio Grande do Sul (FAPERGS) through the Brazilian National Institute for Cryopsheric Sciences (INCT da Criosfera)	The authors received financial support from the Brazilian National Council for Scientific and Technological Development (CNPq) and the Foundation for Research of the State of Rio Grande do Sul (FAPERGS) through the Brazilian National Institute for Cryopsheric Sciences (INCT da Criosfera).	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Appl. Climatol.	JUL	2020	141	1-2					537	549		10.1007/s00704-020-03200-9	http://dx.doi.org/10.1007/s00704-020-03200-9		MAY 2020	13	Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Meteorology & Atmospheric Sciences	MG0XE					2023-06-23	WOS:000531521900001
J	Angelo, TV; Egydio-Silva, M; Temporim, FA; Seraine, M				Angelo, Tiago Valim; Egydio-Silva, Marcos; Temporim, Filipe Altoe; Seraine, Marina			Midcrust deformation regime variations across the Neoproterozoic Aracual hot orogen (SE Brazil): Insights from structural and magnetic fabric analyses	JOURNAL OF STRUCTURAL GEOLOGY			English	Article						Magmatic flow; Anisotropy of magnetic susceptibility; Rock magnetism; Aracual belt; Magnetic fabric; Hot orogen	PLASMA-MASS SPECTROMETRY; BEARING GRANITE PLUTON; MOLTEN MIDDLE CRUST; RIBEIRA BELT; RHEOLOGICAL TRANSITIONS; EASTERN BRAZIL; TH/U RATIOS; SUSCEPTIBILITY; ANISOTROPY; ROCKS	The Neoproterozoic Aracuaf belt of eastern Brazil formed during the amalgamation of Western Gondwana and holds characteristics of a hot collisional belt, involving large amounts of magma, partial melting of the middle crust, and slow cooling rates. To improve our understanding of the mechanical behavior of the continental crust under these conditions we combined structural, magnetic, and geochronological studies to access information related to the flow of rocks, deformation history, and structural patterns associated with the behavior of this orogen. Anisotropy of magnetic susceptibility (AMS) coupled with rock magnetism investigations supports that the magnetic fabric is a good proxy of the structural fabric. Field and AMS measurements of syn-to late plutonic bodies hosted in metasedimentary rocks revealed four domains with contrasting fabric patterns. The structural patterns from W to E are characterized by westward thrusting orthogonal to the belt (region 1), orogen-parallel transpression induced strain partitioning (regions 2 and 3), and orogen-parallel flow and subsidiary eastward vergence magmatic flow (region 4). The use of AMS to determine the lineation was vital to unraveling the kinematics. The composite observed fabric results from the interplay of collision-driven and gravity-driven deformations, induced by the convergence between the Sao Francisco and Congo Cratons.	[Angelo, Tiago Valim; Egydio-Silva, Marcos] Univ Sao Paulo, Inst Geociencias, R Lago 562, BR-05508008 Sao Paulo, SP, Brazil; [Temporim, Filipe Altoe] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, R Matao 1226, BR-05508008 Sao Paulo, SP, Brazil; [Seraine, Marina] Univ Brasilia, Inst Geociencias, BR-70297400 Brasilia, DF, Brazil	Universidade de Sao Paulo; Universidade de Sao Paulo; Universidade de Brasilia	Angelo, TV (autor correspondente), Univ Sao Paulo, Inst Geociencias, R Lago 562, BR-05508008 Sao Paulo, SP, Brazil.	valim206@gmail.com	Temporim, Filipe/AAR-9538-2021; Egydio-SIlva, Marcos/G-1819-2012	Temporim, Filipe/0000-0002-7417-4391; Egydio-SIlva, Marcos/0000-0002-8758-2175; Valim Angelo, Tiago/0000-0002-1191-8664	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (Capes) [CAPES/SIU 0013]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (Capes)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (Capes) - Finance code CAPES/SIU 0013. This work has been partially performed at USPMag lab at Instituto de Astronomia, Geofisica e Ciencias Atmosf.ericas (IAG), Oceanographic Institute of the University of Sao Paulo (LabGeo), and Magnetic Anisotropies and Rock Magnetism Laboratory of the Instituto de Geociencias at the University of Sao Paulo (IGc/USP). The authors are grateful to the technical staff of the geochronological laboratories of Sao Paulo (USP) and Brasilia (University of Brasilia - UnB).	Almeida F. F. 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Struct. Geol.	MAY	2020	134								104007	10.1016/j.jsg.2020.104007	http://dx.doi.org/10.1016/j.jsg.2020.104007			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6BK					2023-06-23	WOS:000528183400005
J	Areas, JD; Pinheiro, CESC; Santell, RE; Machado, W; Bielschowsky, C; da Rocha, RT; Soares, R				Areas, Jennifer da Silva; Soares Canejo Pinheiro, Carlos Eduardo; Santell, Ricardo E.; Machado, Wilson; Bielschowsky, Caue; da Rocha, Rodrigo Tavares; Soares, Ricardo			Would the Contaminated Areas of Rio de Janeiro State a Legacy of the Great Acceleration in the Anthropocene?	REVISTA VIRTUAL DE QUIMICA			Portuguese	Article						Anthropocene; great acceleration; planetary boundary chemical pollution; contaminated areas cadastre; brownfields	GEOCHEMICAL BEHAVIOR; PLANETARY BOUNDARY; INDUSTRIAL-WASTE; SOILS; HYDROCARBONS; SPECIATION; POLLUTION; QUEIMADOS; METALS; RISK	The International Union of Geological Sciences ratified in 2018 the subdivision of the Holocene and the Meghalayan Age was officially recognized as the current geological time unit on Earth. However, the proposal for the formalization of the Anthropocene as a geological period is still under evaluation and has as one of the conceptual bases of epistemological support the post 1950 period known as "The Great Acceleration", in which there was an exponential increase in the use of energy and in the global population growth. The vertiginous increase in urbanization, associated with the technological advance evidenced in the "Great Acceleration", impelled the productive sector to innovate processes in the search for new materials and chemical products in large scale. However, the insificient control mechanisms provided anthropic activities with the generation of significant negative impacts on a global scale, threatening the vital processes of the Earth System. Chemical pollution constituted one of the nine Planetary Limits that delimit an "operationally safe space for humanity". Therefore, it is necessary to develop institutional measures to curb chemical pollution and remedy contaminated areas when they are identified. In this sense, this article aims to evaluate the evolution of the Registry of Contaminated Areas of the Rio de Janeiro State, observing that the fuel stations are the most polluting activities and are responsible for approximately 60 % of the contaminated areas of the state. In addition, metal pollution predominates over other types of contaminants and the cities with the most contaminated areas are: Rio de Janeiro, Duque de Caxias and Volta Redonda. Finally, bronwfields and decommissioned factories account for more than 60 % of contaminated industrial areas. Contaminated areas in Rio de Janeiro State reflect the lifestyle and consumption pattern adopted by urban society and constitute a legacy of the "Great Acceleration" in the Anthropocene.	[Areas, Jennifer da Silva] Univ Fed Fluminense, Dept Biol Marinha, Campus Valonguinho, BR-24020140 Niteroi, RJ, Brazil; [Areas, Jennifer da Silva; Soares Canejo Pinheiro, Carlos Eduardo] Univ Veiga de Almeida, Campus Maracana,R Ibituruna 108, BR-20271020 Rio De Janeiro, RJ, Brazil; [Santell, Ricardo E.] Univ Fed Rio de Janeiro, Dept Quim Analit, Ctr Tecnol, Bloco A,Av Athos da Silveira Ramos 149, BR-21941909 Rio De Janeiro, RJ, Brazil; [Machado, Wilson; Soares, Ricardo] Univ Fed Fluminense, Inst Quim, Dept Geoquim, Outeiro Sao Joao Batista S-N, BR-24020141 Niteroi, RJ, Brazil; [Bielschowsky, Caue; da Rocha, Rodrigo Tavares; Soares, Ricardo] Inst Estadual Ambiente, Ave Venezuela 110, BR-20081312 Rio De Janeiro, RJ, Brazil	Universidade Federal Fluminense; Universidade Veiga de Almeida (UVA); Universidade Federal do Rio de Janeiro; Universidade Federal Fluminense	Santell, RE (autor correspondente), Univ Fed Rio de Janeiro, Dept Quim Analit, Ctr Tecnol, Bloco A,Av Athos da Silveira Ramos 149, BR-21941909 Rio De Janeiro, RJ, Brazil.	resantelli@globo.com	Machado, Wilson/P-8047-2019; Soares, Ricardo/AAM-7896-2021	Machado, Wilson/0000-0003-3117-8584; 				Afonso JC, 2018, REV VIRTUAL QUIM, V10, P1849, DOI 10.21577/1984-6835.20180121; Agencia Nacional do Petroleo Gas Natural e Biocombustiveis (ANP), 2016, PAN AB COMB; Almeida FV, 2007, QUIM NOVA, V30, P1976, DOI 10.1590/S0100-40422007000800033; Andreoni V, 2004, CHEMOSPHERE, V57, P401, DOI 10.1016/j.chemosphere.2004.06.013; [Anonymous], 2018, REV VIRTUAL QUIM, V10, P1618, DOI 10.21577/1984-6835.20180110; Arbilla G, 2018, REV VIRTUAL QUIM, V10, P1758, DOI 10.21577/1984-6835.20180117; Bentes J. 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J	Baez, AD; Baez, W; Caselli, AT; Martini, MA; Sommer, CA				Baez, Alejandro D.; Baez, Walter; Caselli, Alberto T.; Martini, Mateo A.; Sommer, Carlos A.			The glaciovolcanic evolution of the Copahue volcano, Andean Southern Volcanic Zone, Argentina-Chile	JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH			English	Article						Glaciovolcanism; Volcano-ice interaction; Caviahue-Copahue volcanic complex; Late Pleistocene	SOUTHWESTERN BRITISH-COLUMBIA; CHEMICAL CLASSIFICATION; RADIOCARBON CHRONOLOGY; REYKJANES PENINSULA; FACIES ANALYSIS; MOUNT-RAINIER; LAVA; ICELAND; COMPLEX; RIDGE	Glaciovolcanism produces distinctive features that are useful paleoclimate proxies for the distribution of past ice sheets and glacier extent. The Copahue volcano located in the Andean Southern Volcanic Zone. Argentina-Chile, is an active composite volcano known to have glaciovolcanic features such as lava bodies with glassy margins and anomalous cooling fractures. However, the emplacement conditions of these products and the influence of Pleistocene glaciations on the evolution of the Copahue volcano remains poorly understood. In this contribution, we propose a model for glaciovolcanic evolution of the Copahue volcano based on the analysis, interpretation, and mapping of its products. Ten lithofacies are described on the eastern flank of Copahue volcano exhibiting several examples of glaciovolcanism. The evolution of the Copahue volcano can be divided into two main sequences: the Ancient Sequence (S1) and the Young Sequence (S2), separated by a major erosive phase. The S1 (early-middle Pleistocene-late Pleistocene) consists of an initial subaerial effusive stage followed by a major glaciovolcanic stage, during which a thick ice cap existed and the edifice grew beneath an englacial lake with the eventual formation of a lava-fed delta. The S2 (late Pleistocene-Present) is defined by mainly effusive activity during periods of glacial advance and retreat recorded by an alternation of unconfined subaerial lavas and ice-confined lavas. The evolution of the Copahue volcano therefore indicates two glaciations in the Copahue-Caviahue area during the late Pleistocene, in contrast to a single glaciation. Based on the glacial history in the area we associate the first glaciation with the end of Marine Isotope Stage 3 (57-29 ka) and/or the Last Glacial Maximum period (26.5-19.0 ka), and the second less-extensive glacial period with the Antarctic Cold Reversal (14.5-12.9 ka). (C) 2020 Elsevier B.V. All rights reserved.	[Baez, Alejandro D.; Caselli, Alberto T.] Univ Nacl Rio Negro, Inst Invest Paleobiol & Geol, Viedma, Rio Negro, Argentina; [Baez, Alejandro D.; Caselli, Alberto T.] Consejo Nacl Invest Cient & Tecn CONICET, Inst Invest Paleobiol & Geol, Viedma, Rio Negro, Argentina; [Baez, Walter] Univ Nacl Salta, CONICET, IBIGEO, Av Bolivia 5150,A4400FVY, Salta, Argentina; [Martini, Mateo A.] Univ Chile, Nucleo Milenio Paleoclima, Santiago, Chile; [Martini, Mateo A.] Pontificia Univ Catolica Chile, Inst Geog, Santiago, Chile; [Martini, Mateo A.] UNC, Ctr Invest Ciencias Tierra CICTERRA, CONICET, Fac Ciencios Exactas Fis & Nat, Cordoba, Argentina; [Sommer, Carlos A.] Univ Fed Rio Grande do Sul UFRGS, Av Bento Goncalves 9500,15001, BR-91501970 Porto Alegre, RS, Brazil	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad de Chile; Pontificia Universidad Catolica de Chile; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of Cordoba; Universidade Federal do Rio Grande do Sul	Baez, AD (autor correspondente), Univ Nacl Rio Negro, Inst Invest Paleobiol & Geol, Viedma, Rio Negro, Argentina.	adbaez@unrn.edu.ar	Martini, Mateo/ABF-3602-2020; Sommer, Carlos A/Q-9077-2018	Martini, Mateo/0000-0003-1704-9313; Sommer, Carlos A/0000-0001-8696-7084; Baez, Alejandro David/0000-0003-3346-0591	Universidad Nacional de Rio Negro [PI UNRN 2017 40 A 618]	Universidad Nacional de Rio Negro	This work was supported by Universidad Nacional de Rio Negro (project PI UNRN 2017 40 A 618). We thank Agostina Chiodi and Shanaka de Silva for the English writing assistance, as well as Gerardo Barion and Enzo Martinez for their help during fieldwork. We also acknowledge Jose Luis Macias for editorial handling, and Benjamin Edwards, James Kelly Russell and an anonymous reviewer for their helpful comments that have substantially improved this paper.	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J	Carvalho, ACB; Silva, LJ; Dick, DP; Moreira, VD; Vicente, MD; de Andrade, AFO; Bidone, ED; Sabadini-Santos, E				Carvalho, Angelo C. B.; Silva, Liberio J.; Dick, Deborah P.; Moreira, Vanessa de A.; Vicente, Murilo de C.; de Andrade, Antoni Felipe O.; Bidone, Edison Dausacker; Sabadini-Santos, Elisamara			SPECTROSCOPIC ANALYSIS OF ORGANIC MATTER IN SURFACE SEDIMENTS FROM SEPETIBA BAY, RIO DEJANEIRO, BRAZIL	QUIMICA NOVA			Portuguese	Article						DRIFT; molecular composition; coastal zone	DIFFUSE-REFLECTANCE; INFRARED-SPECTROSCOPY; MERCURY DISTRIBUTION; MARINE-SEDIMENTS; DE-JANEIRO; SE BRAZIL; C-13 NMR; CARBON; HYDROCARBONS; WATERS	Spectroscopic techniques are powerful tools for molecular organic matter assessment in sediments, which analysis request low sample mass and are cheap, fast and easy to obtain. The aim of this work was to evaluate the elemental (C, N) and molecular composition of the organic matter in relation to the grain-size distribution over surface sediments from Sepetiba Bay. Spatial distribution of grain-size was remarkable heterogeneous, with the internal area presenting the highest levels of fine sediments, organic carbon (0.20-3.45%) and total nitrogen (<LQ-0.36%). Concentrations of organic carbon from surface sediments at the study area seem to be lower when compared to other degraded coastal systems. C/N ratio vary between 10 and 20, suggesting a mix of allochthonous and autochthonous sources of organic matter to the sediments. DRIFT spectra presented prominent and marked bands assigned to organic and mineral functional groups bonding and the spectra identified chemical bonds of molecular composition such as aliphatic and aromatic functional groups.	[Carvalho, Angelo C. B.; Silva, Liberio J.; Moreira, Vanessa de A.; Vicente, Murilo de C.; de Andrade, Antoni Felipe O.; Bidone, Edison Dausacker; Sabadini-Santos, Elisamara] Univ Fed Fluminense, Dept Geoquim, BR-24020141 Niteroi, RJ, Brazil; [Dick, Deborah P.] Univ Fed Rio Grande do Sul, Inst Quim, Dept Fisicoquim, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal Fluminense; Universidade Federal do Rio Grande do Sul	Carvalho, ACB (autor correspondente), Univ Fed Fluminense, Dept Geoquim, BR-24020141 Niteroi, RJ, Brazil.	angelocarvalho@id.uff.br	dick, deborah p/E-4028-2013; Sabadini-Santos, Elisamara/AAD-3407-2021; Bidone, Edison/AAE-9527-2021; Carvalho, Angelo Cezar Borges/AAD-3408-2021; Silva, Libério Junio/AHC-5655-2022; moreira, vanessa/GQO-7744-2022	dick, deborah p/0000-0002-5615-8611; Sabadini-Santos, Elisamara/0000-0003-3783-4554; Bidone, Edison/0000-0002-5771-5651; Carvalho, Angelo Cezar Borges/0000-0001-8519-0365; Silva, Libério Junio/0000-0002-6677-4645; Moreira, Vanessa/0000-0002-3963-3679; Vicente, Murilo/0000-0002-8520-308X				Abdel-Gawad FK, 2012, SPECTROCHIM ACTA A, V97, P771, DOI 10.1016/j.saa.2012.07.050; BAES AU, 1989, SOIL SCI SOC AM J, V53, P695, DOI 10.2136/sssaj1989.03615995005300030008x; Bordovskiy OK, 1965, MAR GEOL, V3, P33, DOI [10.1016/0025-3227(65)90004-6, DOI 10.1016/0025-3227(65)90004-6]; Bornemann L, 2010, SOIL SCI SOC AM J, V74, P1147, DOI 10.2136/sssaj2009.0195; Burdige DJ, 2007, CHEM REV, V107, P467, DOI 10.1021/cr050347q; Calderon FJ, 2011, SOIL SCI SOC AM J, V75, P568, DOI 10.2136/sssaj2009.0375; Carreira RS, 2009, QUIM NOVA, V32, P1805, DOI 10.1590/S0100-40422009000700023; Chefetz B, 1996, J ENVIRON QUAL, V25, P776, DOI 10.2134/jeq1996.00472425002500040018x; Coimbra AG, 2003, THESIS; Dick D. 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Nova	MAY	2020	43	5					552	557		10.21577/0100-4042.20170518	http://dx.doi.org/10.21577/0100-4042.20170518			6	Chemistry, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	MH3SX		gold, Green Published			2023-06-23	WOS:000546654400005
J	da Conceicao, DM; Crisafulli, A; Lannuzzi, R; Neregato, R; Cisneros, JC; de Andrade, LS				da Conceicao, Domingas Maria; Crisafulli, Alexandra; Lannuzzi, Roberto; Neregato, Rodrigo; Cisneros, Juan Carlos; de Andrade, Luiz Saturnino			New petrified gymnosperms from the Permian of Maranhao (Pedra de Fogo Formation), Brazil: Novaiorquepitys and Yvyrapitys	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Petrified gymnosperm; Taxonomy; Maranhao State; Parnaiba Basin; Permian	FOREST-NATIONAL-PARK; PARNAIBA BASIN; NORTHEASTERN BRAZIL; SILICIFIED WOOD; SOUTHERN-HEMISPHERE; SILICA DIAGENESIS; SP-NOV; CALAMITALEANS; GEOCHEMISTRY; COMPLEX	Anatomically preserved gymnosperm stems are relatively abundant in the Permian outcrops of the Parnaiba Basin, but their anatomy has rarely been studied in detail. Here we describe two new fossil gymnosperm trunks from the Lower Permian (Cisuralian) strata of the Pedra de Fogo Formation in the municipality of Nova Iorque, southern Maranhao State, northeastern Brazil. Two new genera et species are described, Novaiorquepitys maranhensis and Yvyrapitys novaiorquensis. These taxa have a broad, non-septate pith containing sclerenchyma and secretory cells, a parenchyma sheath, and a system of lacunae. Pycnoxylic secondary xylem with growth interruptions and the radial bordered pits on the tracheid walls are araucarian and mixed types. The recognition of two endemic forms indicates both a high degree of endemism for the flora of the Pedra de Fogo Formation and a higher taxonomic diversity of gymnosperm woods than hitherto noted. In addition, the anatomical characters of these taxa, together with sedimentological data and the presence in the same area of plants that live on the banks of water bodies or in wetlands (e.g., tree ferns and tree-calamitaleans), indicate that these woody plants lived near the shores of large lakes. These findings show that studies of Paleozoic woods in this region are potentially valuable. (C) 2020 Elsevier B.V. All rights reserved.	[da Conceicao, Domingas Maria; Lannuzzi, Roberto; Neregato, Rodrigo] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Dept Pateontol & Estratig, Caixa Postal 15-001, BR-91509900 Porto Alegre, RS, Brazil; [Crisafulli, Alexandra] Univ Nacl Nordeste, Fac Ciencias Exactas & Nat & Agrimensura, Ruta 5,Km 2,5, RA-3400 Corrientes, Argentina; [Crisafulli, Alexandra] Consejo Nacl Invest Cient & Tecn, CECOAL, Ruta 5,Km 2,5, RA-3400 Corrientes, Argentina; [Cisneros, Juan Carlos] Univ Fed Piaui, Museu Arqueol & Paleontol, BR-64049550 Teresina, PI, Brazil; [Cisneros, Juan Carlos] Univ Fed Pernambuco, Programa Posgrad Geociencias, Recife, PE, Brazil; [de Andrade, Luiz Saturnino] UFPA, Inst Geociencias, Rua Augusto Correa 1, BR-66075110 Belem, Para, Brazil	Universidade Federal do Rio Grande do Sul; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidade Federal do Piaui; Universidade Federal de Pernambuco; Universidade Federal do Para	da Conceicao, DM (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Dept Pateontol & Estratig, Caixa Postal 15-001, BR-91509900 Porto Alegre, RS, Brazil.	domingasmary@hotmail.com	Cisneros, Juan C/A-5258-2008; Iannuzzi, Roberto/G-3641-2012	Andrade, Luiz/0000-0001-7168-8787; Iannuzzi, Roberto/0000-0003-1432-8106; Cisneros, Juan Carlos/0000-0001-6159-1981	National Council of Technological and Scientific Development (CNPq) [141248/2016-5, 401848.2010-8, 456608/2014-1, PQ312747/2017-9]; Negaunee Foundation	National Council of Technological and Scientific Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Negaunee Foundation	DMC acknowledges the National Council of Technological and Scientific Development (CNPq) for financial support for an internship at the Centro de Ecologia Aplicada del Litoral (CECOAL), Corrientes, Argentina, through a PhD scholarship (141248/2016-5), and for grants to JCC and RI (401848.2010-8, 456608/2014-1, PQ312747/2017-9). 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J	de Menezes, GCA; Porto, BA; Amorim, SS; Zani, CL; Alves, TMD; Sales, PA; Murta, SMF; Simoes, JC; Cota, BB; Rosa, CA; Rosa, LH				de Menezes, Graciele Cunha Alves; Porto, Barbara Alves; Amorim, Soraya Sander; Zani, Carlos Leomar; de Almeida Alves, Tania Maria; Junior, Policarpo Ademar Sales; Murta, Silvane Maria Fonseca; Simoes, Jefferson Cardia; Cota, Betania Barros; Rosa, Carlos Augusto; Rosa, Luiz Henrique			Fungi in glacial ice of Antarctica: diversity, distribution and bioprospecting of bioactive compounds	EXTREMOPHILES			English	Article						Antarctica; Ice; Fungi; Secondary metabolites	COMMUNITIES; THELEBOLUS; YEAST; MACROALGAE; MYCOBIOTA; ECOLOGY; WATER	We identified cultivable fungi present in the glacial ice fragments collected in nine sites across Antarctica Peninsula and assessed their abilities to produce bioactive compounds. Three ice fragments with approximately 20 kg were collected, melted and 3 L filtered through of 0.45 mu m sterilized membranes, which were placed on the media Sabouraud agar and minimal medium incubated at 10 degrees C. We collected 66 isolates classified into 27 taxa of 14 genera. Penicillium palitans, Penicillium sp. 1, Thelebolus balaustiformis, Glaciozyma antarctica, Penicillium sp. 7, Rhodotorula mucilaginosa, and Rhodotorula dairenensis had the highest frequencies. The diversity and richness of the fungal community were high with moderate dominance. Penicillium species were present in all samples, with Penicillium chrysogenum showing the broadest distribution. P. chrysogenum, P. palitans, and Penicillium spp. had trypanocidal, leishmanicidal, and herbicidal activities, with P. chrysogenum having the broadest and highest capability. H-1 NMR signals revealed the presence of highly functionalized secondary metabolites in the bioactive extracts. Despite extreme environmental conditions, glacial ice harbours a diverse fungal community, including species never before recorded in the Arctic and Antarctica. Among them, Penicillium taxa may represent wild fungal strains with genetic and biochemical pathways that may produce new secondary bioactive metabolites.	[de Menezes, Graciele Cunha Alves; Porto, Barbara Alves; Amorim, Soraya Sander; Rosa, Carlos Augusto; Rosa, Luiz Henrique] Univ Fed Minas Gerais, Inst Ciencias Biol, Dept Microbiol, BR-31270901 Belo Horizonte, MG, Brazil; [Zani, Carlos Leomar; de Almeida Alves, Tania Maria; Junior, Policarpo Ademar Sales; Murta, Silvane Maria Fonseca; Cota, Betania Barros] FIOCRUZ MG, Inst Rene Rachou, Belo Horizonte, MG, Brazil; [Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul, Ctr Polar & Climat, Porto Alegre, RS, Brazil	Universidade Federal de Minas Gerais; Fundacao Oswaldo Cruz; Universidade Federal do Rio Grande do Sul	Rosa, LH (autor correspondente), Univ Fed Minas Gerais, Inst Ciencias Biol, Dept Microbiol, BR-31270901 Belo Horizonte, MG, Brazil.	lhrosa@icb.ufmg.br	Cota, Betania Barros/AAO-2753-2021; Simoes, Jefferson Cardia/D-7232-2013; Murta, Silvane Fonseca Murta/ABE-9410-2021; Zani, Carlos Leomar/ABE-3936-2021; Alves, Tania Maria A/B-4814-2009	Cota, Betania Barros/0000-0002-0041-2043; Simoes, Jefferson Cardia/0000-0001-5555-3401; Murta, Silvane Fonseca Murta/0000-0002-8523-2155; Almeida Alves, Tania Maria/0000-0002-0582-3968; Alves Porto, Barbara/0000-0002-2249-2638; Cunha Alves de Menezes, Graciele/0000-0002-9427-1893				Abyzov S.S., 1993, ANTARCTIC MICROBIOLO, P265; Abyzov SS, 2004, ADV SPACE RES-SERIES, V33, P1222, DOI 10.1016/j.asr.2003.08.033; Altschul SF, 1997, NUCLEIC ACIDS RES, V25, P3389, DOI 10.1093/nar/25.17.3389; Alves IMS, 2019, EXTREMOPHILES, V23, P327, DOI 10.1007/s00792-019-01086-8; Anesio AM, 2012, TRENDS ECOL EVOL, V27, P219, DOI 10.1016/j.tree.2011.09.012; [Anonymous], 2008, DICT FUNGI; [Anonymous], IND FUNG CHECKL DAT; Antipova TV, 2018, MICROBIOLOGY+, V87, P642, DOI 10.1134/S002626171805003X; Bovio E., 2018, Fungal Systematics and Evolution, V1, P141, DOI 10.3114/fuse.2018.01.07; Branda E, 2010, FEMS MICROBIOL ECOL, V72, P354, DOI 10.1111/j.1574-6941.2010.00864.x; Brunati M, 2009, MAR GENOM, V2, P43, DOI 10.1016/j.margen.2009.04.002; Buzzini P, 2018, YEAST, V35, P487, DOI 10.1002/yea.3314; Callahan HL, 1997, ANTIMICROB AGENTS CH, V41, P818, DOI 10.1128/AAC.41.4.818; CASTELLA.A, 1967, J TROP MED HYG, V70, P181; CORTE AM, 1993, MYCOTAXON, V48, P343; Crous PW, 2004, STUD MYCOL, P19; D'Elia T, 2009, MYCOLOGIA, V101, P751, DOI 10.3852/08-184; Dayan FE, 2000, J CHEM ECOL, V26, P2079, DOI 10.1023/A:1005512331061; de Hoog GS, 2005, STUD MYCOL, P33; de Menezes GCA., 2019, FUNGI ANTARCTICA DIV, P127, DOI [10.1007/978-3-030-18367-7_6, DOI 10.1007/978-3-030-18367-7_6]; Saito RAD, 2018, FUNGAL ECOL, V36, P8, DOI 10.1016/j.funeco.2018.07.006; FELL JW, 1969, ANTON VAN LEE J M S, V35, P433, DOI 10.1007/BF02219163; Furbino LE, 2014, MICROB ECOL, V67, P775, DOI 10.1007/s00248-014-0374-9; GLASS NL, 1995, APPL ENVIRON MICROB, V61, P1323, DOI 10.1128/AEM.61.4.1323-1330.1995; Godinho VM, 2015, EXTREMOPHILES, V19, P585, DOI 10.1007/s00792-015-0741-6; Godinho VM, 2013, ISME J, V7, P1434, DOI 10.1038/ismej.2013.77; Goncalves DB, 2012, BIOCATAL AGRIC BIOTE, V1, P140, DOI 10.1016/j.bcab.2011.09.002; Goncalves VN, 2017, EXTREMOPHILES, V21, P851, DOI 10.1007/s00792-017-0947-x; Goncalves VN, 2012, FEMS MICROBIOL ECOL, V82, P459, DOI 10.1111/j.1574-6941.2012.01424.x; Gunde-Cimerman N, 2003, PHYS CHEM EARTH, V28, P1273, DOI 10.1016/j.pce.2003.08.056; Hammer Oyvind, 2001, Palaeontologia Electronica, V4, pUnpaginated; Houbraken J, 2012, PERSOONIA, V29, P78, DOI 10.3767/003158512X660571; JACOBS PH, 1964, ARCH DERMATOL, V89, P117, DOI 10.1001/archderm.1964.01590250123021; Knowlton Caitlin, 2013, Biology (Basel), V2, P206, DOI 10.3390/biology2010206; Kobayasi Y, 1967, ANNU REP I FERMENT O, V3, P1; Kornerup A, 1974, FARVER I FARVER; Kozlovsky AG, 2020, FOLIA MICROBIOL, V65, P95, DOI 10.1007/s12223-019-00708-0; Kurtzman CP, 2011, YEASTS: A TAXONOMIC STUDY, VOLS 1-3, 5TH EDITION, P1; Lachance MA, 1999, CAN J MICROBIOL, V45, P172, DOI 10.1139/cjm-45-2-172; Lutz S, 2015, FRONT MICROBIOL, V6, DOI 10.3389/fmicb.2015.00307; Malkus A, 2006, MYCOL RES, V110, P1152, DOI 10.1016/j.mycres.2006.07.015; Margesin R, 2007, INT J SYST EVOL MICR, V57, P2179, DOI 10.1099/ijs.0.65111-0; Margesin R, 2019, APPL MICROBIOL BIOT, V103, P2537, DOI 10.1007/s00253-019-09631-3; Nicoletti R, 2016, MAR DRUGS, V14, DOI 10.3390/md14020037; Perini L, 2019, SCI REP-UK, V9, DOI 10.1038/s41598-019-56290-5; Perini L, 2019, FRONT MICROBIOL, V10, DOI 10.3389/fmicb.2019.00557; Rogers SO, 2004, APPL ENVIRON MICROB, V70, P2540, DOI 10.1128/AEM.70.4.2540-2544.2004; Romanha AJ, 2010, MEM I OSWALDO CRUZ, V105, P233, DOI 10.1590/S0074-02762010000200022; Rosa LH, 2019, FUNGI ANTARCTICA DIV, P1, DOI [10.1007/978-3-030-18367-7_1, DOI 10.1007/978-3-030-18367-7]; Rosa LH, 2013, SYMBIOSIS, V60, P133, DOI 10.1007/s13199-013-0249-8; Rosa LH, 2009, POLAR BIOL, V32, P161, DOI 10.1007/s00300-008-0515-z; Sampaio J. 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New structural investigations indicate that the older metasedimentary rocks of the Cuiaba Group represent a Tonian-Cryogenian basement assemblage deformed in two contemporaneous fault-bounded structural sub-domains of wrench-dominated (rake <10 degrees) and contraction-dominated (rake similar to 30-40 degrees) sinistral transpression, with tectonic vergence towards the SE. The younger late Cryogenian to early Cambrian sedimentary rocks lying to the NW of the Cuiaba Group are non-metamorphic and display only pervasive brittle transtension characterized by normal-oblique faults, fractures and forced drag folds with no consistent vergence pattern. Our analyses suggest that an unconformity separates the metasedimentary Cuiaba Group basement of the Northern Paraguai Belt from the unmetamorphosed sedimentary cover. It is proposed that the latter units were deposited during a post-glacial marine transgression (after c. 635 Ma) in a post-collisional basin. The Paraguai Belt basement and its post-collisional sedimentary cover share a number of significant geological similarities with sequences in the Bassarides Belt and Taoudeni Basin in the SW portion of the West African Craton.	[dos Santos, Iara Maria; Pinheiro, Roberto Vizeu L.; Nogueira, Afonso Cesar R.; Santos, Hudson Pereira; Domingos, Fabio Henrique G.] Univ Fed Para, Fac Geol, Inst Geociencias, CP 1611, BR-66075900 Belem, PA, Brazil; [Holdsworth, Robert E.] Univ Durham, Dept Earth Sci, Sci Labs, Durham DH1 3LE, England	Universidade Federal do Para; N8 Research Partnership; Durham University	dos Santos, IM (autor correspondente), Univ Fed Para, Fac Geol, Inst Geociencias, CP 1611, BR-66075900 Belem, PA, Brazil.	iarageo13@gmail.com	Holdsworth, Robert E/C-2381-2008		GEOCIAM Project, UFPA, Brazil (2014-2015); CAPES	GEOCIAM Project, UFPA, Brazil (2014-2015); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	Fieldwork for this study was supported by GEOCIAM Project, UFPA, Brazil (2014-2015). We are grateful to CAPES for a MSc Scholarship to I.M.S.	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Geol. Soc.	MAY	2020	177	3					475	491		10.1144/jgs2018-184	http://dx.doi.org/10.1144/jgs2018-184			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LT7WY		Green Accepted			2023-06-23	WOS:000537278000002
J	Marcon, GTG; Sommer, MG; Mendonca, JG				Gadens Marcon, Gabrielli Teresa; Sommer, Margot Guerra; Mendonca-Filho, Joao Graciano			Paleoclimatic inferences for the Holocene of southern Brazil in environments influenced by different hydrological systems	ACTA BRASILIENSIS			English	Article						Continental areas; palynofacies; turfeiras; organic matter; shallow lakes		Organic matter preserved in continental deposits is an excellent archive of environmental and climate change, and various research tools are commonly used to access this information. The present study is the result of a study conducted in continental environments influenced by different hydrological systems and demonstrates the usefulness of these analyses in obtaining rainfall-related paleoclimatic data. The study area is located in the basalts of the Alto Uruguai region (Rio Grande do Sul, Brazil), known for its mineral riches such as amethyst geodes and hot springs. The methodology used integrates palynofacies and organic geochemistry techniques, complemented by radiocarbon dating. The results were obtained from three sedimentary profiles and showed a trend of relative decrease in rainfall levels in the region. However, the scale of these changes is also highly influenced by the hydrological system of the depositional environment that originated the sedimentary record at each site. Based on the data obtained, we advise the establishment of medium- and long-term policies involving better management of local natural resources in the investigated region.	[Gadens Marcon, Gabrielli Teresa] Univ Estadual Rio Grande do Sul, BR-91540000 Porto Alegre, RS, Brazil; [Sommer, Margot Guerra] Univ Estadual Rio Grande do Sul, Programa Posgrad Geociencias, BR-91540000 Porto Alegre, RS, Brazil; [Mendonca-Filho, Joao Graciano] Univ Fed Rio de Janeiro, Programa Posgrad Geol, BR-21941916 Rio De Janeiro, RJ, Brazil	Universidade Estadual do Rio Grande do Sul (UERGS); Universidade Estadual do Rio Grande do Sul (UERGS); Universidade Federal do Rio de Janeiro	Marcon, GTG (autor correspondente), Univ Estadual Rio Grande do Sul, BR-91540000 Porto Alegre, RS, Brazil.	gabrielli-marcon@uergs.edu.br	Sommer, Margot Guerra/C-4951-2013; Mendonca Filho, Joao Graciano/C-2098-2013; Gadens Marcon, Gabrielli/C-2448-2016	Sommer, Margot Guerra/0000-0002-9517-4593; Mendonca Filho, Joao Graciano/0000-0001-8997-0270; Gadens Marcon, Gabrielli/0000-0003-1834-1607				American Society for Testing and Materials (ASTM), 2008, 4239 ASTM; [Anonymous], [No title captured]; Bond G, 2001, SCIENCE, V294, P2130, DOI 10.1126/science.1065680; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; Duarte LC, 2009, J VOLCANOL GEOTH RES, V184, P427, DOI 10.1016/j.jvolgeores.2009.05.019; Freitas M.A., 2016, AGUAS SUBTERRANEAS, V30, P1, DOI 10.14295/ras.v30i1.28518; Gadens-Marcon G.T., 2014, AM J CLIMATE CHANGE, V3, P95, DOI DOI 10.4236/AJCC.2014.31009; Hartmann LA, 2010, GEOL MAG, V147, P954, DOI 10.1017/S0016756810000592; INTCAL04 Radiocarbon Age Calibration, 2004, INTCAL04, V46; Marcon G. T. G., 2014, ANN BRAZILIAN ACAD S, V86, P1077, DOI [10.1590/0001-3765201420130268, DOI 10.1590/0001-3765201420130268]; Mendonca Filho J.G., 2011, ICCP TRAINING COURSE, P33; Mendonca Filho J.G., 2012, EARTHS SYSTEM PROCES, P211; Menezes T.R., 2008, REV BRASIL GEOCI, V38, P80; Naranjo JA, 2004, REV GEOL CHILE, V31, P225, DOI 10.4067/S0716-02082004000200003; Ramirez J. D. V., 2018, ANUARIO I GEOCIENCIA, V41, P186, DOI [10.11137/2018_3_186_194, DOI 10.11137/2018_3_186_194]; Sallun AEM, 2012, QUATERNARY RES, V77, P31, DOI 10.1016/j.yqres.2011.09.007; Souza T. C. S., 2016, J SEDIMENTARY ENV, V1, P242, DOI [10.12957/jse.2016.23096, DOI 10.12957/JSE.2016.23096]; Strikis NM, 2011, GEOLOGY, V39, P1075, DOI 10.1130/G32098.1; Stuiver M, 1998, RADIOCARBON, V40, P1041, DOI 10.1017/S0033822200019123; Suarez-Ruiz I, 2012, INT J COAL GEOL, V99, P54, DOI 10.1016/j.coal.2012.02.004; Tyson RV., 1995, SEDIMENTARY ORGANIC, P615, DOI DOI 10.1007/978-94-011-0739-6; USEPA, 2002, NCEAC1282; Vanclay F, 2011, NEW DIRECTIONS IN SOCIAL IMPACT ASSESSMENT: CONCEPTUAL AND METHODOLOGICAL ADVANCES, P3	23	0	0	0	0	UNIV FEDERAL CAMPINA GRANDE	CAMPINA GRANDE PB	RUA APRIGIO VELOSO 882, BODO CONGO, CAMPINA GRANDE PB, 58109 090, BRAZIL	2526-432X	2526-4338		ACTA BRAS	Acta Bras.	MAY-AUG	2020	4	2					99	105		10.22571/2526-4338304	http://dx.doi.org/10.22571/2526-4338304			7	Agriculture, Multidisciplinary	Emerging Sources Citation Index (ESCI)	Agriculture	LT2CX		gold			2023-06-23	WOS:000536881500004
J	Giovannini, AL; Mitchell, RH; Neto, ACB; Moura, CAV; Pereira, VP; Porto, CG				Giovannini, Arthur L.; Mitchell, Roger H.; Bastos Neto, Artur C.; Moura, Candido A., V; Pereira, Vitor P.; Porto, Claudio G.			Mineralogy and geochemistry of the Morro dos Seis Lagos siderite carbonatite, Amazonas, Brazil	LITHOS			English	Article						Carbonatite evolution; Siderite carbonatite; Morro dos Seis Lagos Nb deposit; Amazon; Carbothermal fluid	COMPOSITIONAL VARIATION; NIOBIUM DEPOSIT; COMPLEX; PYROCHLORE; OXYGEN; ISOTOPES; PROVINCE; FERROCARBONATITE; TITANOMAGHEMITE; MAGMATISM	The Morro dos Seis Lagos niobium rare earth element, Ti-bearing lateritic deposit (Amazonas, Brazil) is derived from a primary siderite carbonatite. The complex is the only example of a Nb deposit in which Nb-rich rutile is the main Nb ore mineral. Apart from the laterites, at the current level of exposure the complex consists only of siderite carbonatite; silicate rocks are absent. Three types of siderite carbonatite are recognized: (1) a brecciated and oxidized core siderite carbonatite consisting of up to 95 vol% siderite together with: hematite; pyrochlore; Nb-brookite; Ti-maghemite; and thorobastnasite; (2) a REE- and P-rich variety of the core siderite carbonatite consisting of siderite (up to 95 vol%), hematite, minor pyrochlore, monazite and bastnasite; (3) a border hydrothermal siderite carbonatite with similar to 70 vol% siderite, barite (similar to 15 vol%), gorceixite (similar to 7 vol%) and minor rhabdophane and pyrochlore. The country rock gneiss in which the carbonatite was emplaced was affected by potassic fenitization, with the formation of phlogopite and orthoclase together with monazite, fluorapatite and bastnasite. The siderite carbonatites exhibit a wide variation of delta C-13 (-5.39 parts per thousand to 140 parts per thousand), accompanied by a significant variation in delta O-18 (17.13%. to 31.33%.), especially in the REE-rich core siderite carbonatite, and are explained as due to the presence of both H2O and CO2 in the magma. The core siderite carbonatite is the richest in Fe (48.64-70.85 wt% Fe2O3) and the poorest in Ca (up 0.82 wt% CaO) example of a siderite carbonatite yet recognized The ferrocarbonatite has significant contents of Mn, Ba, Th, Pb and LREE, and a very high Nb (up to 7667 ppm) content due to the presence of Nb-brookite. The substitution 3Ti(4+) = Fe2+ 2Nb(5+) recognized in Nb-rich brookite explains enrichment of Nb in the core siderite carbonatite and indicates formation in a reducing environment. The high Nblra ratio (1408-11,459) of the carbonatite is compatible with residual liquids derived by fractional crystallization. The Sr-87/Sr-86 (0.70411A.70573) and Nd-144/Nd-143 (0.512663-0.512715) isotopic data suggest the carbonatite is mantle-derived with essentially no crustal contamination and is younger than the maximum age of 1328 +/- 58 Ma (U-Pb in zircon). We suggest that the Morro dos Seis Lagos carbonatite complex represents the upper-most parts of a differentiated carbonalite magmatic system, and that the siderite carbonatite is related to laic-magmatic-to-carbo-hydrothermal processes. (C) 2020 Elsevier B.V. All rights reserved.	[Giovannini, Arthur L.; Bastos Neto, Artur C.] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Mitchell, Roger H.] Lakehead Univ, Dept Geol, 955 Oliver Rd, Thunder Bay, ON P7B 5E1, Canada; [Bastos Neto, Artur C.] Univ La Salle, Programa Posgrad Avaliacao Impactos Ambientais, Ave Victor Barreto 2288, BR-92010000 Canoas, RS, Brazil; [Moura, Candido A., V] Univ Fed Para, Inst Geociencias, Rua Augusto Correa 1, Belem, Para, Brazil; [Pereira, Vitor P.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Porto, Claudio G.] CPRM, SUREG, Av Pasteur 404, Rio De Janeiro, RJ, Brazil; [Porto, Claudio G.] Univ Fed Rio de Janeiro, Inst Geociencias, Cidade Univ,Ave Athos da Silveira Ramos S-N, BR-21949900 Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio Grande do Sul; Lakehead University; Universidade Federal do Para; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio de Janeiro	Giovannini, AL (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	arthur.giovannini@ufrgs.br; rmitchel@lakeheadu.ca; artur.bastos@ufrgs.br; candido@ufpa.br; vitor.pereira@ufrgs.br; porto@geologia.ufrj.br		Veloso Moura, Candido Augusto/0000-0003-2212-5800	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico CNPq [485415/2012-7, 405839/2013-8]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The present work would not have been possible without the support given by the Companhia de Pesquisa de Recursos Minerais, through Roberto Ventura Santos, Eduardo Camozatto, and Rene Luzardo. Nilson Botelho (UNB) is thanked by the microprobe analysis, Alcides Sial and Milton Formoso are thanked for the C and O isotopic analysis. We also want to thank the reviewer Dr. Pedro Cordeiro for the contribution to improve this manuscript. The Conselho Nacional de Desenvolvimento Cientifico e Tecnologico CNPq is acknowledged for the financial support (projects 485415/2012-7 and 405839/2013-8).	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J	Hou, A; Bahr, A; Schmidt, S; Strebl, C; Albuquerque, AL; Chiessi, CM; Friedrich, O				Hou, Alicia; Bahr, Andre; Schmidt, Stefan; Strebl, Cornelia; Albuquerque, Ana Luiza; Chiessi, Cristiano M.; Friedrich, Oliver			Forcing of western tropical South Atlantic sea surface temperature across three glacial-interglacial cycles	GLOBAL AND PLANETARY CHANGE			English	Article						Western tropical Atlantic; Sea surface temperature; Southeast trade winds; Marine Isotope Stage 6; Zonal temperature gradient; Meridional temperature gradient	BRAZIL CURRENT; GEOSTROPHIC TRANSPORT; FORAMINIFERAL MG/CA; CLEANING PROCEDURES; EQUATORIAL CURRENT; HEINRICH EVENTS; HEAT-BUDGET; CABO-FRIO; CLIMATE; OCEAN	The western tropical Atlantic (WTA) supplies warm and saline waters to the upper-limb of the Atlantic Meridional Overturning Circulation (AMOC) and may store excess heat and salinity during periods of AMOC slowdown. Since previous sea surface temperature (SST) reconstructions from the WTA typically focus on the Last Glacial Maximum and the last deglaciation, additional long-term records spanning multiple glacial-interglacial transitions are needed in order to elucidate the drivers of long-term WTA SST variability. We performed Mg/Ca analyses on the surface-dwelling planktic foraminifera Globigerinoides ruber (pink) from a sediment core raised from the southern WTA to reconstruct SST changes over the past 322 kyr. We evaluate the relative importance of atmospheric pCO(2), AMOC strength and trade-wind intensity in driving the thermal evolution of the WTA across three glacial-interglacial cycles. Our results indicate a lack of pronounced glacial-interglacial variability in the SST record, prompting us to exclude atmospheric pCO(2) as a direct driver of SST variations in the southern WTA. Similarly, we conclude that variations in AMOC strength also likely did not have a strong influence on long-term WTA SST, based on the low and relatively stable interhemispheric SST gradient over the past 322 kyr. Our results reveal high-amplitude variability in zonal SST gradients within the (sub)tropical South Atlantic and similarities between the long-term patterns of the intrahemispheric meridional SST gradient and our SST record. Based on these findings, we propose that changes in the intrahemispheric meridional SST gradient modulate southeast trade wind intensity, which in turn drives variations in zonal SST gradients and southern WTA SSTs.	[Hou, Alicia; Bahr, Andre; Schmidt, Stefan; Strebl, Cornelia; Friedrich, Oliver] Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany; [Albuquerque, Ana Luiza] Univ Fed Fluminense, Programa Geociencias Geoquim, Niteroi, RJ, Brazil; [Chiessi, Cristiano M.] Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, Brazil	Ruprecht Karls University Heidelberg; Universidade Federal Fluminense; Universidade de Sao Paulo	Hou, A (autor correspondente), Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany.	alicia.hou@geow.uni-heidelberg.de; andre.bahr@geow.uni-heidelberg.de; Strebl@stud.uni-heidelberg.de; ana_albuquerque@id.uff.br; chiessi@usp.br; Oliver.Friedrich@geow.uni-heidelberg.de	Chiessi, Cristiano Mazur/E-1916-2012; Albuquerque, Ana Luiza S/C-5167-2013	Chiessi, Cristiano Mazur/0000-0003-3318-8022; Albuquerque, Ana Luiza S/0000-0003-1267-6190	Deutsche Forschungsgemeinschaft (DFG) [BA 3809/9-1]; FAPESP [2018/15123-4]; CAPES [564/2015, 88881.313535/2019-01]; CNPq [302607/2016-1, 422255/2016-5]; Alexander von Humbdoldt Foundation, Germany	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Alexander von Humbdoldt Foundation, Germany	We kindly acknowledge the support by captain and crew of the R/V METEOR during expedition M125. We thank Bernd Knape and Christian Scholz for assistance with stable isotope and ICP-OES analyses, respectively. Andrea Jaeschke provided important contributions during manuscript preparation. We are grateful to the S. Szidat and the LARA team at the University of Bern for providing the <SUP>14</SUP>C dates. AB was funded by the Deutsche Forschungsgemeinschaft (DFG) via Grant BA 3809/9-1. CMC acknowledges the financial support from FAPESP (grants 2018/15123-4), CAPES (grants 564/2015 and 88881.313535/2019-01), CNPq (grants 302607/2016-1 and 422255/2016-5) and the Alexander von Humbdoldt Foundation, Germany.	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Planet. Change	MAY	2020	188								103150	10.1016/j.gloplacha.2020.103150	http://dx.doi.org/10.1016/j.gloplacha.2020.103150			10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	LE1YB					2023-06-23	WOS:000526519000003
J	Kern, AK; Gross, M; Galeazzi, CP; Pupim, FN; Sawakuchi, AO; Almeida, RP; Piller, WE; Kuhlmann, GG; Basei, MAS				Kern, Andrea K.; Gross, Martin; Galeazzi, Cristiano P.; Pupim, Fabiano N.; Sawakuchi, Andre O.; Almeida, Renato P.; Piller, Werner E.; Kuhlmann, Gabriel G.; Basei, Miguel A. S.			Re-investigating Miocene age control and paleoenvironmental reconstructions in western Amazonia (northwestern Solimoes Basin, Brazil)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palynology; Ostracods; Detrital zircon ages; Biostratigraphy; Neogene; Amazon rainforest	DEPOSITIONAL HISTORY; ANDEAN TECTONICS; SURFACE UPLIFT; MIDDLE MIOCENE; CLIMATE-CHANGE; NEOGENE; CRUSTACEA; ALTIPLANO; OSTRACODA; RIVER	The modern Amazonian rainforest has a great fascination and global significance, but our knowledge of past landscape changes is still limited due to sparse data and the lack of radiometric age constrains. Precise dating in records older than the late Pleistocene are difficult to obtain and often regionally confined, therefore biostratigraphic correlations are used to estimate depositional ages across sedimentary basins. Aiming for a better understanding of the Neogene changes in western Brazil, we studied palynology and ostracod assemblages from the Solimoes Formation, a key site for paleoenvironmental models to discuss the biotic changes in Amazonia. Further, we compare the biostratigraphic information of both groups with radiometric maximum deposition ages constrained by U/Pb measurements on detrital zircon grains. Down to the depth of similar to 95 m, zircon populations show a maximum deposition age of 11.42 +/- 0.66 Ma documenting Tortonian (late Miocene) or younger ages for the top of the Solimoes Formation. Palynological biostratigraphy show the Psilatricolporites caribbiensis zone (latest Miocene-Pliocene) down to a depth of 181.8 m, where the Grimsdalea magnaclavata zone suggests a late middle Miocene to early late Miocene age. In comparison, ostracod biostratigraphy indicates the Cyprideis cyrtoma zone (late Miocene) down to 176.0 m and the Cyprideis minipunctata (late middle to late Miocene) for the bottom of the section. Thus, both biostratigraphic concepts suggest ages close to the maximum ages indicated by the detrital zircons. This comparison of the biozonations with U/Pb maximum deposition ages represents the first independent calibration of these widely used methods for age determination in the Solimoes Basin. Palynological and ostracod data illustrate dynamic environments varying from fluvial settings with wetland forests and swamps to lakes and/or abandoned channels with temporary slightly saline conditions. Instead of a slow evolution of Neogene Amazonian environments, our results show migrating rivers and waterbodies surrounded by rainforest during the period recorded by the base and top of the studied core material, separated by a phase of more extensive lakes and swamps (core depth 90-120 m). Indicators for slightly elevated salinity are found until the topmost sample and thus persisted during the late Miocene. This highlights the importance of new age control to improve the regional biostratigraphic timescale and reconstructed environmental changes.	[Kern, Andrea K.; Galeazzi, Cristiano P.; Pupim, Fabiano N.; Sawakuchi, Andre O.; Almeida, Renato P.; Kuhlmann, Gabriel G.; Basei, Miguel A. S.] Univ Sao Paulo, Inst Geociencias, Sao Paulo, SP, Brazil; [Gross, Martin] Univ Joanneum, Dept Geol & Palaeontol, Graz, Austria; [Pupim, Fabiano N.] Univ Fed Sao Paulo, Dept Ciencias Ambientais, Diadema, SP, Brazil; [Piller, Werner E.] Karl Franzens Univ Graz, Inst Earth Sci, NAWI Graz Geocetr, Graz, Austria	Universidade de Sao Paulo; Universidade Federal de Sao Paulo (UNIFESP); University of Graz	Kern, AK (autor correspondente), Univ Sao Paulo, Inst Geociencias, Sao Paulo, SP, Brazil.	annkkern@gmail.com	Basei, Miguel A S/C-1915-2013; Sawakuchi, André O/D-1445-2013; Pupim, Fabiano N/J-7869-2012; Galeazzi, Cristiano/AGX-8001-2022; Almeida, Renato/AAF-6705-2020; Kern, Andrea K./V-5078-2017; Almeida, Renato/G-2567-2013	Basei, Miguel A S/0000-0002-3857-7089; Pupim, Fabiano N/0000-0001-7452-1376; Galeazzi, Cristiano/0000-0001-7285-2884; Gross, Martin/0000-0002-5113-6069; Kern, Andrea K./0000-0002-9343-0696; Almeida, Renato/0000-0003-3664-1558; Sawakuchi, Andre/0000-0001-5016-2428	project "Dimensions US-BIOTA-Sao Paulo: Assembly and evolution of the Amazonian biota and its environment: an integrated approach", a collaborative Dimensions of Biodiversity BIOTA grant [2012/50260-6]; Sao Paulo Research Foundation (FAPESP, Brazil); National Science Foundation (NSF, United States); NASA (United States); FAPESP [2014/05582-0, 2014/23334-4, 2017/06874-3]; Brazilian Foundation for Support and Evaluation of Graduate Education (CAPES) [88887.370034/2019-00]; National Council for Scientific and Technological Development (CNPq, Brazil) [302411/2018-6, 3009223/2014-8]; Austrian Science Fund project [P21748-N21]	project "Dimensions US-BIOTA-Sao Paulo: Assembly and evolution of the Amazonian biota and its environment: an integrated approach", a collaborative Dimensions of Biodiversity BIOTA grant; Sao Paulo Research Foundation (FAPESP, Brazil)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Science Foundation (NSF, United States)(National Science Foundation (NSF)); NASA (United States)(National Aeronautics & Space Administration (NASA)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Brazilian Foundation for Support and Evaluation of Graduate Education (CAPES); National Council for Scientific and Technological Development (CNPq, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Austrian Science Fund project(Austrian Science Fund (FWF))	This research had the main financial support of the project "Dimensions US-BIOTA-Sao Paulo: Assembly and evolution of the Amazonian biota and its environment: an integrated approach", a collaborative Dimensions of Biodiversity BIOTA grant supported by grant 2012/50260-6, Sao Paulo Research Foundation (FAPESP, Brazil), National Science Foundation (NSF, United States) and NASA (United States). Additional FAPESP grands supporting this research were grants 2014/05582-0, 2014/23334-4, 2017/06874-3, the Brazilian Foundation for Support and Evaluation of Graduate Education (CAPES) 88887.370034/2019-00 and the National Council for Scientific and Technological Development (CNPq, Brazil) grants #302411/2018-6, #3009223/2014-8 respectively. Additional funding was provided by the Austrian Science Fund project P21748-N21. Special thanks goes to cooperating the DNPM/Manaus, (especially Gert Woeltje) and CPRM/Manaus, (especially Marco Antonio de Oliveira) for sampling permits. This work benefited of the initial help in pollen identification by Carlos Jaramillo and Ingrid Romero at STRI in Panama City. This study would not have been possible without the support of Francisco W. Cruz. We further thank Cody C. Mason and an anonymous reviewer for their great comments and corrections.	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MAY 1	2020	545								109652	10.1016/j.palaeo.2020.109652	http://dx.doi.org/10.1016/j.palaeo.2020.109652			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	LE6HY		Bronze			2023-06-23	WOS:000526825900002
J	Nascimento, RKS; Porfirio, DM; Costa, ML				Nascimento, R. K. S.; Porfirio, D. M.; Costa, M. L.			Feasibility of Laser Induced-Breakdown Spectroscopy (LIBS) for Multivariate Discrimination of Edible Salts	REVISTA VIRTUAL DE QUIMICA			Portuguese	Article						Edible salts; LIBS; PCA	TABLE SALTS; CLASSIFICATION; ELEMENTS; SAMPLES	In the present study, the feasibility of Laser-Induced Breakdown Spectroscopy (LIBS) was investigated to analyze the main constituent chemical elements of 29 edible salt samples from Germany, Australia, Bolivia, Brazil, Cyprus, United States of America, France, the Himalayas, Iran and Pakistan. Such salts comprise iodized refined, iodized marine, ground iodized marine, hyposodic iodized marine, unrefined gourmet, Himalayan gourmet, yolk salt and food additive. The LIBS technique identified and evaluated the elements Al, Ca, Sr, Fe, Mg, Mn, K and Na. The data set obtained by LIBS was used in the developed multivariate classification model, principal components analysis (PCA). In the PCA 4 principal components (PC) were defined, which explain 83.77 % of the spectral information matrix that were used to discriminate the origin and identify profiles of edible salts in national and imported salts and hyposodium salts. LIBS then proves to be a tool for origin indication analysis or origin determination, being capable of identifying possible tampering. Therefore, LIBS classification analyzes are very promising and represent a simplification in the handling and preparation of samples for analysis.	[Nascimento, R. K. S.] Univ Fed Para, Inst Ciencias Exatas & Nat, Fac Quim, Campus Belem,R Augusto Correa 01, BR-66075110 Belem, Para, Brazil; [Nascimento, R. K. S.] Univ Fed Sao Carlos, Dept Quim, Programa Posgrad Quim, Campus Sao Carlos,Rod Washington Luiz S-N, BR-13565905 Sao Carlos, SP, Brazil; [Porfirio, D. M.] Ctr Tecnol Eletronorte Eletrobras, Rod Arthur Bernardes 2172, BR-66115000 Belem, Para, Brazil; [Costa, M. L.] Univ Fed Para, Inst Geociencias, Campus Belem,R Augusto Correa 01, BR-66075110 Belem, Para, Brazil	Universidade Federal do Para; Universidade Federal de Sao Carlos; Universidade Federal do Para	Porfirio, DM (autor correspondente), Ctr Tecnol Eletronorte Eletrobras, Rod Arthur Bernardes 2172, BR-66115000 Belem, Para, Brazil.	darilenap@yahoo.com.br	Nascimento, Rita de Kássia Silva do/GPW-5607-2022	Nascimento, Rita de Kássia Silva do/0000-0002-5173-3955				[Anonymous], 2011, ADITIVOS INGREDIENTE, V75, P26; Atkinson MJ, 1997, J AQUARICULTURE AQUA, VVIII, P39, DOI DOI 10.1080/19393210.2010.520340; Barakat A, 2015, ACS SYM SER, V1210, P101; BOLEN W. P., 2015, MINERALS YB SALT; Costa VC, 2019, QUIM NOVA, V42, P527, DOI 10.21577/0100-4042.20170325; Doker S, 2014, FOOD ANAL METHOD, V7, P683, DOI 10.1007/s12161-013-9675-8; Duggal H, 2015, INT J PHARM SCI REV, V35, P126; Eftekhari MH, 2014, J ENVIRON HEALTH SCI, V12, DOI 10.1186/2052-336X-12-10; Galvis-Sanchez AC, 2011, J AGR FOOD CHEM, V59, P11109, DOI 10.1021/jf202204d; Galvis-Sanchez AC, 2013, COMP ANAL C, V60, P719, DOI 10.1016/B978-0-444-59562-1.00026-8; Haas J. M., 2019, INOVACAO GESTAO SUST; Herrador MA, 1998, J FOOD PROTECT, V61, P891, DOI 10.4315/0362-028X-61.7.891; Heshmati A, 2014, INT J RES STUD BIOSC, V2, P21; Kagaya S, 2009, TALANTA, V79, P512, DOI 10.1016/j.talanta.2009.04.025; Lee Y, 2017, APPL SPECTROSC, V71, P651, DOI 10.1177/0003702817691288; Lee Y, 2016, SPECTROCHIM ACTA B, V118, P102, DOI 10.1016/j.sab.2016.02.019; Lee Y, 2014, SPECTROCHIM ACTA B, V101, P57, DOI 10.1016/j.sab.2014.07.012; Tan MM, 2012, APPL SPECTROSC, V66, P262, DOI 10.1366/11-06379; Millero FJ, 2008, DEEP-SEA RES PT I, V55, P50, DOI 10.1016/j.dsr.2007.10.001; Mohammad N., 2013, J SCI TECHNOLOGY, P9; Oliveira AA, 2012, QUIM NOVA, V35, P1299, DOI 10.1590/S0100-40422012000700004; Park G, 2015, B KOREAN CHEM SOC, V36, P189, DOI 10.1002/bkcs.10043; Pasquini C, 2007, J BRAZIL CHEM SOC, V18, P463, DOI 10.1590/S0103-50532007000300002; Porfirio D. M., 2017, AN 15 S GEOL AM BEL; Pourgheysari H, 2012, INT J ENV HLTH ENG, V1, P41; Powles J., 2013, BMJ OPEN, V3, P1; Sansonetti JE, 2005, J PHYS CHEM REF DATA, V34, P1559, DOI 10.1063/1.1800011; Shariatifar N, 2017, TOXIN REV, V36, P89, DOI 10.1080/15569543.2016.1262875; Singh VK, 2009, LASER MED SCI, V24, P917, DOI 10.1007/s10103-009-0659-2; Soylak M, 2003, TURK J CHEM, V27, P235; Soylak M, 2008, ENVIRON MONIT ASSESS, V143, P267, DOI 10.1007/s10661-007-9975-9; Stergiou C., 2016, B GEOLOGICAL SOC GRE, V50, P2018; Yousefian F, 2016, FLUORIDE, V49, P495	33	0	0	0	5	SOC BRASILEIRA QUIMICA	SAO PAULO	CAIXA POSTAL 26037, 05599-970 SAO PAULO, BRAZIL	1984-6835			REV VIRTUAL QUIM	Rev. Virtual Quim.	MAY-JUN	2020	12	3					724	735		10.21577/1984-6835.20200058	http://dx.doi.org/10.21577/1984-6835.20200058			12	Chemistry, Multidisciplinary	Emerging Sources Citation Index (ESCI)	Chemistry	OM5DR		gold			2023-06-23	WOS:000586045800015
J	Portner, DE; Rodriguez, EE; Beck, S; Zandt, G; Scire, A; Rocha, MP; Bianchi, MB; Ruiz, M; Franca, GS; Condori, C; Alvarado, P				Portner, Daniel Evan; Rodriguez, Emily E.; Beck, Susan; Zandt, George; Scire, Alissa; Rocha, Marcelo P.; Bianchi, Marcelo B.; Ruiz, Mario; Franca, George Sand; Condori, Cristobal; Alvarado, Patricia			Detailed Structure of the Subducted Nazca Slab into the Lower Mantle Derived From Continent-Scale Teleseismic P Wave Tomography	JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH			English	Article							RECEIVER FUNCTION-ANALYSIS; OCEANIC CRUSTAL STRUCTURE; SOUTHERN CENTRAL ANDES; PAMPEAN FLAT-SLAB; STRUCTURE BENEATH; RIDGE SUBDUCTION; TRANSITION ZONE; JOINT INVERSION; AMBIENT NOISE; PUNA PLATEAU	Nazca subduction beneath South America is one of our best modern examples of long-lived ocean-continent subduction on the planet, serving as a foundation for our understanding of subduction processes. Within that framework, persistent heterogeneities at a range of scales in both the South America and Nazca plates is difficult to reconcile without detailed knowledge of the subducted Nazca slab structure. Here we use teleseismic travel time residuals from >1,000 broadband and short-period seismic stations across South America in a single tomographic inversion to produce the highest-resolution contiguous P wave tomography model of the subducting slab and surrounding mantle beneath South America to date. Our model reveals a continuous trench-parallel fast seismic velocity anomaly across the majority of South America that is consistent with the subducting Nazca slab. The imaged anomaly indicates a number of robust features of the subducted slab, including variable slab dip, extensive lower mantle penetration, slab stagnation in the lower mantle, and variable slab amplitude, that are incorporated into a new, comprehensive model of the geometry of the Nazca slab surface to similar to 1,100 km depth. Lower mantle slab penetration along the entire margin suggests that lower mantle slab anchoring is insufficient to explain along strike upper plate variability while slab stagnation in the lower mantle indicates that the 1,000 km discontinuity is dominant beneath South America.	[Portner, Daniel Evan; Rodriguez, Emily E.; Beck, Susan; Zandt, George] Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA; [Portner, Daniel Evan] Carnegie Inst Sci, Dept Terr Magnetism, 5241 Broad Branch Rd NW, Washington, DC 20015 USA; [Scire, Alissa] New Mexico Inst Min & Technol, IRIS PASSCAL Instrument Ctr, Socorro, NM 87801 USA; [Rocha, Marcelo P.; Franca, George Sand; Condori, Cristobal] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Bianchi, Marcelo B.] Univ Sao Paulo, Dept Geofis, Inst Geofis Astron & Ciencias Atmosfer, Ctr Sismol, Sao Paulo, Brazil; [Ruiz, Mario] Escuela Politec Nacl, Inst Geofis, Quito, Ecuador; [Alvarado, Patricia] Univ Nacl San Juan, Fac Ciencias Exactas, Dept Geofis & Astron, Consejo Nacl Invest Cient & Tecn, San Juan, Argentina	University of Arizona; Carnegie Institution for Science; New Mexico Institute of Mining Technology; Universidade de Brasilia; Universidade de Sao Paulo; Escuela Politecnica Nacional Ecuador; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad Nacional de San Juan	Portner, DE (autor correspondente), Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA.; Portner, DE (autor correspondente), Carnegie Inst Sci, Dept Terr Magnetism, 5241 Broad Branch Rd NW, Washington, DC 20015 USA.	dportner@carnegiescience.edu	de Bianchi, Marcelo Belentani/P-6367-2015; de França, George Sand L A/F-9931-2012; QUISPE, CRISTOBAL CONDORI/AAS-1256-2020; Rocha, Marcelo P/K-5215-2013	de Bianchi, Marcelo Belentani/0000-0002-1650-4540; de França, George Sand L A/0000-0002-2694-5868; QUISPE, CRISTOBAL CONDORI/0000-0003-2657-147X; Rocha, Marcelo P/0000-0002-6869-6468; Portner, Daniel/0000-0002-3478-6203	National Science Foundation [EAR-3012040, EAR-3018390]; ChevronTexaco Geology Fellowship at University of Arizona	National Science Foundation(National Science Foundation (NSF)); ChevronTexaco Geology Fellowship at University of Arizona	The authors would like to thank the editors and two anonymous reviewers for their comments, Brandon Schmandt for sharing his teleseismic tomography code with us, and Chengxin Jiang and Nicholas Rawlinson for their help in incorporating 3-D ray tracing in our inversion process. Thank you also to Brandon Bishop for many helpful discussions. Lastly, the authors would like to thank the many investigators around the world who have collected the vast data set used in this study and the IRIS, GFZ, USP, and RSBR data centers for making that data easily accessible. Information about the collection of seismic data used in this study and its accessibility is included in Table S1. Most of the data are freely accessible at the IRIS (https://service.iris.edu), GFZ (eida.gfz-potsdam.de/webdc3), USP (http://www.moho.iag.usp.br), and RSBR (www.rsbr.gov.br/request.html) data centers through FDSN web services. Network XC is currently under restricted access but will be made public at the USP data center. Networks EC and XE were acquired through personal communication with collaborators in Ecuador. This research is supported by National Science Foundation grants EAR-3012040 and EAR-3018390. Portner was supported in this work by the ChevronTexaco Geology Fellowship at University of Arizona. The tomography model from this study will be made available online through the IRIS Earth Model Collaboration (ds. iris.edu/ds/products/emc) with the label SAM5_P_2019 and the slab model produced in this study is included in the article supplement.	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J	Bruno, MDR; Fauth, G; Watkins, DK; Savian, JF				Rodrigues Bruno, Mauro Daniel; Fauth, Gerson; Watkins, David K.; Savian, Jairo Francisco			Albian-Cenomanian calcareous nannofossils from DSDP Site 364 (Kwanza Basin, Angola): Biostratigraphic and paleoceanographic implications for the South Atlantic	CRETACEOUS RESEARCH			English	Article						Calcareous nannofossils; South Atlantic; Kwanza Basin; DSDP Site 364	DEEP-SEA SEDIMENTS; EQUATORIAL ATLANTIC; PALAEOCEANOGRAPHIC CHANGES; OCEANIC CIRCULATION; MAGNETIC-PROPERTIES; ANOXIC EVENTS; BLACK SHALES; NANNOPLANKTON; EVOLUTION; PALEOECOLOGY	The Albian-Cenomanian was an interval of extreme warmth due to greenhouse climatic conditions, as well as significant changes in the paleogeography and paleoceanography of the oceans, which affected the evolution of marine ecosystems on a global scale. This study analyzed the calcareous nannofossil assemblages from 72 samples that were recovered from Site 364 (Kwanza Basin, Angola), which was drilled by the Deep Sea Drilling Project (DSDP) Leg 40. A total of 103 calcareous nannofossil species were recovered, enabling the identification of biozones (CC 8 to CC 10a: or BC 23 to UC 1b/UC 4a) allowing to assign an Albian-Cenomanian interval for the deposition of the studied section. The recovered assemblages have a subtropical-tropical affinity and are indicative of a surface water connection between the Central Atlantic and the South Atlantic oceans, that extends at least as far as offshore Angola. The area sedimentation was predominantly calcareous and pelagic during this interval, with the exception of the basal section, where Albian black shales interbedded with dolomitic and marly limestones were deposited. Throughout the section, high concentrations of TOC and sulfur and the presence of dissolution-susceptible species likely indicate low euxinic conditions for the Kwanza Basin. Dissolution is a significant process for Site 364 in the majority of the studied samples, although not to the point where species richness was severely impacted, as small amounts of dissolution-susceptible taxa were observed. Dissolution showed a marked decrease in intervals in which paleontological and geochemical data indicated an increase in surface water fertility/productivity. (C) 2020 Elsevier Ltd. All rights reserved.	[Rodrigues Bruno, Mauro Daniel; Fauth, Gerson] Unisinos Univ, Inst Tecnol Micropaleontol, Itt Fossil, Av Unisinos 950, BR-93022000 Sao Leopoldo, RS, Brazil; [Watkins, David K.] Univ Nebraska, Dept Earth & Atmospher Sci, Lincoln, NE 68588 USA; [Savian, Jairo Francisco] Univ Fed Rio Grande do Sul, Dept Geol, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil	University of Nebraska System; University of Nebraska Lincoln; Universidade Federal do Rio Grande do Sul	Bruno, MDR (autor correspondente), Unisinos Univ, Inst Tecnol Micropaleontol, Itt Fossil, Av Unisinos 950, BR-93022000 Sao Leopoldo, RS, Brazil.	dbruno@unisinos.br; gersonf@unisinos.br; dwatkins1@unl.edu; jairo.savian@ufrgs.br	Rodrigues Bruno, Mauro Daniel/HGC-0717-2022; Fauth, Gerson/AAE-3353-2021; Watkins, David/AAJ-2571-2021	Rodrigues Bruno, Mauro Daniel/0000-0001-5290-9855	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [16/2551-0000213-4];  [IODP/CAPES 88887.091703/2014-01];  [IGCP 609];  [CAPES-PVE 88881.062157/2014-01]	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); ; ; 	We would like to thank the International Ocean Discovery Program (IODP) for providing the samples for this study; to Eduardo A. M. Koutsoukos and the anonymous reviewers of this paper for their valuable contributions and observations; to Andrea Concheyro and Karlos G. D. Kochhann for providing comments on an early draft of this manuscript. We thank the staff of the lnstituto Tecnologico de Micropaleontologia (itt Fossil) of the Unisinos University for the TOC/CaCO3 analyzes and for all support. We are grateful to the Paleomagnetism Laboratory (USPMag) of University of Sao Paulo for the magnetic susceptibility analyzes. The results of this paper are part of the projects: IODP/CAPES 88887.091703/2014-01; IGCP 609; and CAPES-PVE 88881.062157/2014-01. JFS acknowledges the Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) (16/2551-0000213-4) for financial support.	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J	Santiago, R; Caxito, FD; Neves, MA; Dantas, EL; de Medeiros, EB; Queiroga, GN				Santiago, Raissa; Caxito, Fabricio de Andrade; Neves, Mirna Aparecida; Dantas, Elton Luiz; de Medeiros Junior, Edgar Batista; Queiroga, Glaucia Nascimento			Two generations of mafic dyke swarms in the Southeastern Brazilian coast: reactivation of structural lineaments during the gravitational collapse of the Aracuai-Ribeira Orogen (500 Ma) and West Gondwana breakup (140 Ma)	PRECAMBRIAN RESEARCH			English	Article						Dyke swarm; Isotope geochemistry; Alkaline and tholeiitic magmatism; Paleocontinent rifting and breakup; Gravitational collapse of orogenic crust; Reactivation of structures	ETENDEKA MAGMATIC PROVINCE; CONTINENTAL FLOOD BASALTS; PARANA PLATEAU BRAZIL; TRACE-ELEMENT; CHEMICAL CLASSIFICATION; TECTONIC EVOLUTION; MANTLE SOURCES; HF ISOTOPES; DIKE SWARM; SE BRAZIL	Mafic dyke swarms emplaced in regional NW-SE trending structures crosscutting the Precambrian basement in the Southeastern Brazilian coast are commonly interpreted as associated to West Gondwana breakup. Recently, however, U-Pb dating suggested that at least some of those dykes were emplaced earlier, at ca. 500-490 Ma, during the gravitational collapse of the Aracuai Orogen. In order to clarify this issue, we studied dykes from the southern Espirito Santo State. Our results indicate that dykes emplaced in the same regional lineaments can be separated into two distinct groups, according to petrographic, geochemical, isotopic and geochronological characteristics. Group 1 is tholeiitic, with Sr-87/Sr-86((i)) of 0.7041-0.7065, epsilon Nd-(1) of -3.4 to -5.5 and TDM ages between 0.8 and 1.5 Ga. Zircon crystals from a dyke of this group yielded the first robust lower Cretaceous U-Pb age for mafic dykes of SE Brazil with a Concordia age of 141.9 +/- 1.9 Ma and epsilon Hf-(t) in a range of - 5.5 to - 7.9. Group 2 is alkaline, shows higher Sr-87/Sr-86((i)) of 0.7064-0.7088, evolved epsilon Nd-(t) < -12 and older TDM ages of 1.7-1.9 Ga. The youngest zircon crystals from a dyke of this group yielded a Concordia age of 504.7 +/- 6.9 Ma and epsilon Hf-(t) of -18.9. Our results suggest that the regional NW-SE trending lineaments of the Brazilian coast were active in at least three episodes, serving as conduits for mafic magmatism of distinct sources and tectonic settings: First, in the Cambrian, during the Aracuai-Ribeira Orogen collapse, when they served as conduits for both the post-tectonic G5 Supersuite (530-490 Ma; composed of granitic and mafic plutons) and the alkaline dykes of Group 2; second, during the lower Cretaceous breakup of West Gondwana, when they served as conduits for the tholeiitic dykes of Group 1, synchronous to syn-rift evolution of the Phanerozoic Brazilian coast basins; and third, during the Cenozoic, when they were reactivated as normal brittle faults.	[Santiago, Raissa; Caxito, Fabricio de Andrade] Univ Fed Minas Gerais CPMTC IGC UFMG, Programa Posgrad Geol, Campus Pampulha,Ave Antonio Carlos 6621, BR-31270901 Belo Horizonte, MG, Brazil; [Santiago, Raissa; Caxito, Fabricio de Andrade] Univ Fed Minas Gerais CPMTC IGC UFMG, Ctr Pesquisas Manoel Teixeira da Costa, Campus Pampulha,Ave Antonio Carlos 6621, BR-31270901 Belo Horizonte, MG, Brazil; [Neves, Mirna Aparecida] Alto Univ, Univ Fed Espirito Santo, Ctr Ciencias Exatas Nat & Saude, S-N Guararema, BR-29500000 Alegre, ES, Brazil; [Dantas, Elton Luiz] Univ Brasilia, Inst Geociencias, Lab Geocronol, BR-70910900 Brasilia, DF, Brazil; [de Medeiros Junior, Edgar Batista; Queiroga, Glaucia Nascimento] Univ Fed Ouro Preto, Dept Geol, Campus Morro Cruzeiro, BR-35400000 Ouro Preto, MG, Brazil	Universidade Federal do Espirito Santo; Universidade de Brasilia; Universidade Federal de Ouro Preto	Santiago, R (autor correspondente), Univ Fed Minas Gerais CPMTC IGC UFMG, Programa Posgrad Geol, Campus Pampulha,Ave Antonio Carlos 6621, BR-31270901 Belo Horizonte, MG, Brazil.; Santiago, R (autor correspondente), Univ Fed Minas Gerais CPMTC IGC UFMG, Ctr Pesquisas Manoel Teixeira da Costa, Campus Pampulha,Ave Antonio Carlos 6621, BR-31270901 Belo Horizonte, MG, Brazil.		Queiroga, Gláucia/AAJ-1823-2021; Dantas, Elton Luiz/AAK-8464-2021; Caxito, Fabricio A/J-1317-2016	Queiroga, Gláucia/0000-0002-1730-0638; Dantas, Elton Luiz/0000-0002-7954-5059; Caxito, Fabricio A/0000-0002-0335-3667	PETROBRAS Human Resources Training Program (PFRH) of Petroleo Brasileiro S.A.	PETROBRAS Human Resources Training Program (PFRH) of Petroleo Brasileiro S.A.(Petrobras)	We are grateful to the PETROBRAS Human Resources Training Program (PFRH) of Petroleo Brasileiro S.A. for the financial support in the form of a scholarship at the Programa de Pos-Graduacao em Geologia, IGC-UFMG; to CPMTC for the analytical facilities for petrographic studies and sample preparation; to the Laboratorio de Geocronologia of the Universidade de Brasilia for the isotopic and geochronological analysis; and to the Laboratorio de Microscopia e Microanalises (LMIc) of the Universidade Federal de Ouro Preto, Laboratory integrating the RMIc, Microscopy and Microanalyses Network of Minas Gerais - FAPEMIG, for the mineral chemistry analyzes. We thank Ana Ramalho Alkmim of the Laboratorio de Geoquimica Isotopica, UFOP, for the help in trace element analysis of zircon. FAC, ELD and GNQ are Fellows of the Brazilian Research Council (CNPq) and acknowledge for the support received. An original version of this paper was greatly enhanced after the comments and suggestions of Wilson Teixeira and two anonymous reviewers.	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J	Santos, LL; Miranda, D; Hatje, V; Albergaria-Barbosa, ACR; Leonel, J				Santos, L. L.; Miranda, D.; Hatje, V; Albergaria-Barbosa, A. C. R.; Leonel, J.			PCBs occurrence in marine bivalves and fish from Todos os Santos Bay, Bahia, Brazil	MARINE POLLUTION BULLETIN			English	Article						POPs; Bivalves; Fish; Contamination; Tropical bay	PERSISTENT ORGANIC POLLUTANTS; POLYBROMINATED DIPHENYL ETHERS; POLYCHLORINATED-BIPHENYLS PCBS; TRACE-METAL CONTAMINATION; RED-SEA COAST; ORGANOCHLORINE PESTICIDES; CHLORINATED PESTICIDES; PONTOPORIA-BLAINVILLEI; PBDE CONTAMINATION; SOUTHEASTERN COAST	In order to evaluate contamination by polychlorinated biphenyls (PCBs) in a tropical bay exposed to different anthropogenic pressures, samples of bivalves: mangrove oyster (Crassotrea rhizophorae), mangrove mussel (Mytella guyanensis)and clams (Anomalocardia brasiliana), were collected in different parts of Todos os Santos Bay, Bahia, Brazil. In addition, samples of bivalves and fish, purchased from a seafood market in the city of Salvador were analyzed to evaluate human exposure to PCBs through ingestion. Identification and quantification of PCBs were done by GC/MS after microwave extraction and purification with sulfuric acid. In bivalves, concentrations ranged from < 0.08 to 50.1 ng g(-1) (dry weight), with the highest values being detected in mangrove oyster, followed by clams and mangrove mussel of the Subae estuary and Madre de Deus/Mataripe; regions known to be impacted by anthropic activities. From the total of the 12 fish species analyzed, only 5 presented levels of PCBs above the detection limit, ranging from 0.23 to 4.55 ng g(-1) and 0.51 to 26.05 ng g(-1) by dry weight and lipid weight, respectively. In general, concentrations of PCBs on the bay are lower than in most regions around the world, especially those located in the Northern Hemisphere. Indexes indicated that local biota and seafood from the fish market are not adversely impacted by PCBs and do not represent a risk to human health.	[Santos, L. L.; Albergaria-Barbosa, A. C. R.] Univ Fed Bahia, Inst Geociencias, Lab Geoquim Marinha, GEOQMAR, BR-40170115 Salvador, BA, Brazil; [Miranda, D.; Hatje, V] Univ Fed Bahia, CIENAM, Ctr Interdisciplinar Energia & Ambiente, BR-40170115 Salvador, BA, Brazil; [Miranda, D.; Hatje, V] Univ Fed Bahia, Inst Quim, BR-40170115 Salvador, BA, Brazil; [Leonel, J.] Univ Fed Santa Catarina, Lab Poluicao & Geoquim Marinha, BR-88040900 Florianopolis, SC, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal de Santa Catarina (UFSC)	Santos, LL (autor correspondente), Univ Fed Bahia, Inst Geociencias, Lab Geoquim Marinha, GEOQMAR, BR-40170115 Salvador, BA, Brazil.	juoceano@gmail.com	de Albergaria-Barbosa, Ana Cecília/AAC-6940-2021; Miranda, Daniele A./AAC-6036-2019; de+Albergaria+Barbosa, Ana/AAQ-3872-2020; Leonel, Juliana/ABD-9781-2020; Miranda, Daniele/GRY-7466-2022	Miranda, Daniele A./0000-0002-5982-0172; Leonel, Juliana/0000-0003-1452-860X; Albergaria-Barbosa, Ana Cecilia R./0000-0003-2121-9792	CAPES [001]; FAPESB [CV0049/2008]; Foundation for Support and Research of the State of Bahia (FAPESB) [9017/2014, CNV0005/2013, CNV0025/2013]; National Council for Scientific and Technological Development (CNPq) [1697617/2017]; CNPq [310786/2018-5]	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); FAPESB(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Foundation for Support and Research of the State of Bahia (FAPESB); National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This research was done in the context of the Graduation Program in Geochemistry: Oil and Environment (POSPETRO - UFBA) with support from CAPES - financing code 001.The authors thank Gilmara F. Eca and Cristiane S. Fahning for providing the samples used in the article (FAPESB CV0049/2008); Group of Environmental Studies (NEA) for the use of their structure; Foundation for Support and Research of the State of Bahia (FAPESB) for the financial support(FAPESB Projects 9017/2014, CNV0005/2013; CNV0025/2013); the Chemical Oceanography Laboratory for the use of their facilities, and Marine Organic Chemistry Laboratory from Oceanographic Institute at Sao Paulo University (IO/USP) for the GC/MS analysis. L. L. Santos also thanks National Council for Scientific and Technological Development (CNPq) for his scholarship (1697617/2017). J. Leonel was sponsored by CNPq (310786/2018-5).	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Pollut. Bull.	MAY	2020	154								111070	10.1016/j.marpolbul.2020.111070	http://dx.doi.org/10.1016/j.marpolbul.2020.111070			8	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	LG6JW	32319897				2023-06-23	WOS:000528205900041
J	Sutherland, R; Dickens, GR; Blum, P; Agnini, C; Alegret, L; Asatryan, G; Bhattacharya, J; Bordenave, A; Chang, L; Collot, J; Cramwinckel, MJ; Dallanave, E; Drake, MK; Etienne, SJG; Giorgioni, M; Gurnis, M; Harper, DT; Huang, HHM; Keller, AL; Lam, AR; Li, H; Matsui, H; Morgans, HEG; Newsam, C; Park, YH; Pascher, KM; Pekar, SF; Penman, DE; Saito, S; Stratford, WR; Westerhold, T; Zhou, X				Sutherland, R.; Dickens, G. R.; Blum, P.; Agnini, C.; Alegret, L.; Asatryan, G.; Bhattacharya, J.; Bordenave, A.; Chang, L.; Collot, J.; Cramwinckel, M. J.; Dallanave, E.; Drake, M. K.; Etienne, S. J. G.; Giorgioni, M.; Gurnis, M.; Harper, D. T.; Huang, H-H M.; Keller, A. L.; Lam, A. R.; Li, H.; Matsui, H.; Morgans, H. E. G.; Newsam, C.; Park, Y-H; Pascher, K. M.; Pekar, S. F.; Penman, D. E.; Saito, S.; Stratford, W. R.; Westerhold, T.; Zhou, X.			Continental-scale geographic change across Zealandia during Paleogene subduction initiation	GEOLOGY			English	Article							SOUTHWEST PACIFIC; MOTION; PLATE; CONSTRAINTS; RECORD; STRATIGRAPHY; OPHIOLITE; REINGA; SEA	Data from International Ocean Discovery Program (IODP) Expedition 371 reveal vertical movements of 1-3 km in northern Zealandia during early Cenozoic subduction initiation in the western Pacific Ocean. Lord Howe Rise rose from deep (similar to 1 km) water to sea level and subsided back, with peak uplift at 50 Ma in the north and between 41 and 32 Ma in the south. The New Caledonia Trough subsided 2-3 km between 55 and 45 Ma. We suggest these elevation changes resulted from crust delamination and mantle flow that led to slab formation. We propose a "subduction resurrection" model in which (1) a subduction rupture event activated lithospheric-scale faults across a broad region during less than similar to 5 m.y., and (2) tectonic forces evolved over a further 4-8 m.y. as subducted slabs grew in size and drove plate-motion change. Such a subduction rupture event may have involved nucleation and lateral propagation of slip-weakening rupture along an interconnected set of preexisting weaknesses adjacent to density anomalies.	[Sutherland, R.] Victoria Univ Wellington, SGEES, POB 600, Wellington 6140, New Zealand; [Dickens, G. R.; Bhattacharya, J.] Rice Univ, Earth Environm & Planetary Sci, Houston, TX 77005 USA; [Blum, P.] Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX 77845 USA; [Agnini, C.] Univ Padua, Dipartimento Geosci, I-35131 Padua, Italy; [Alegret, L.] Univ Zaragoza, Dept Ciencias Tierra, Zaragoza 50009, Spain; [Alegret, L.] Univ Zaragoza, IUCA, Zaragoza 50009, Spain; [Asatryan, G.] Leibniz Inst Evolut & Biodiversitatsforsch, Museum Nat Kunde, D-10115 Berlin, Germany; [Bordenave, A.; Collot, J.; Etienne, S. J. G.] Geol Survey New Caledonia, BP 465, Noumea, New Caledonia; [Chang, L.] Peking Univ, Sch Earth & Space Sci, Beijing, Peoples R China; [Cramwinckel, M. J.] Univ Utrecht, Dept Earth Sci, NL-3584 CB Utrecht, Netherlands; [Dallanave, E.] Univ Bremen, Fac Geosci, D-28359 Bremen, Germany; [Drake, M. K.; Harper, D. T.] Univ Calif Santa Cruz, Ocean Sci Dept, Santa Cruz, CA 95064 USA; [Giorgioni, M.] Univ Brasilia, Inst Geociencia, Brasilia, DF, Brazil; [Gurnis, M.] CALTECH, Seismol Lab, Pasadena, CA 91125 USA; [Huang, H-H M.] Univ Tokyo, Atmosphere & Ocean Res Inst, Tokyo 1138654, Japan; [Keller, A. L.] Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USA; [Lam, A. R.] Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA; [Li, H.] Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Shandong, Peoples R China; [Matsui, H.] Tohoku Univ, Dept Earth Sci, Sendai, Miyagi 9808572, Japan; [Morgans, H. E. G.; Pascher, K. M.; Stratford, W. R.] GNS Sci, POB 30368, Lower Hutt 5040, New Zealand; [Newsam, C.] UCL, Dept Earth Sci, London WC1E 6BT, England; [Park, Y-H] Pusan Natl Univ, Dept Oceanog, Busan 46421, South Korea; [Pekar, S. F.] CUNY, Queens Coll, Sch Earth & Environm Sci, Flushing, NY 11451 USA; [Penman, D. E.] Yale Univ, Dept Geol & Geophys, New Haven, CT 06511 USA; [Saito, S.] Japan Agcy Marine Earth Sci & Technol JAMSTEC, Res & Dev Ctr Ocean Drilling Sci, Yokohama, Kanagawa 2360001, Japan; [Westerhold, T.] Univ Bremen, Ctr Marine Environm Sci MARUM, D-28359 Bremen, Germany; [Zhou, X.] Rutgers State Univ, Inst Marine & Coastal Sci, Rutgers, NJ 08854 USA	Victoria University Wellington; Rice University; Texas A&M University System; Texas A&M University College Station; University of Padua; University of Zaragoza; University of Zaragoza; Leibniz Institut fur Evolutions und Biodiversitatsforschung; Peking University; Utrecht University; University of Bremen; University of California System; University of California Santa Cruz; Universidade de Brasilia; California Institute of Technology; University of Tokyo; University of California System; University of California Riverside; University of Massachusetts System; University of Massachusetts Amherst; Chinese Academy of Sciences; Institute of Oceanology, CAS; Tohoku University; GNS Science - New Zealand; University of London; University College London; Pusan National University; City University of New York (CUNY) System; Queens College NY (CUNY); Yale University; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); University of Bremen; Rutgers State University New Brunswick	Sutherland, R (autor correspondente), Victoria Univ Wellington, SGEES, POB 600, Wellington 6140, New Zealand.		Lam, Adriane R./ABG-1582-2020; Chang, Liao/AAU-3724-2020; Collot, Julien/S-4917-2018; Alegret, Laia/B-5420-2008; Dallanave, Edoardo/AAS-6344-2020; Matsui, Hiroki/Q-2041-2016; Westerhold, Thomas/D-4581-2011; Harper, Dustin T/H-1713-2018	Lam, Adriane R./0000-0002-4131-1767; Chang, Liao/0000-0002-0165-1310; Collot, Julien/0000-0002-2043-2535; Alegret, Laia/0000-0002-8801-9544; Dallanave, Edoardo/0000-0003-4673-1792; Matsui, Hiroki/0000-0002-6985-7083; Westerhold, Thomas/0000-0001-8151-4684; Harper, Dustin T/0000-0002-4855-3849; Sutherland, Rupert/0000-0001-7430-0055; Agnini, Claudia/0000-0001-9749-6003; Huang, Huai-Hsuan/0000-0003-2764-5995; Bhattacharya, Joyeeta/0000-0002-7662-4122; Drake, Michelle/0000-0001-9618-1325; Aurelien, BORDENAVE/0000-0002-5917-6305; Dickens, Gerald/0000-0003-2869-4860; Cramwinckel, Margot J./0000-0002-6063-836X	U.S. National Science Foundation; IODP participating countries; Spanish Ministry of Economy and Competitiveness [CGL2017-84693-R]; Leonardo Grant, BBVA Foundation; Korean IODP (K-IODP); China grant NSFC [41473029, 91958110]; Brazil grant [183/2017-CII/CGPE/DPB/CAPES]; Fondo Europeo de Desarrollo Regional (FEDER) funds [CGL2017-84693-R]; NERC [NE/R009295/1] Funding Source: UKRI	U.S. National Science Foundation(National Science Foundation (NSF)); IODP participating countries; Spanish Ministry of Economy and Competitiveness(Spanish Government); Leonardo Grant, BBVA Foundation; Korean IODP (K-IODP); China grant NSFC(National Natural Science Foundation of China (NSFC)); Brazil grant; Fondo Europeo de Desarrollo Regional (FEDER) funds(European Commission); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We thank the International Ocean Discovery Program (IODP); the personnel of R/V JOIDES Resolution on Expedition 371; proponents unable to sail on Expedition 371; and everyone on surveys TAN1312, TAN1409, and TECTA. This work was funded by the U.S. National Science Foundation; IODP participating countries; New Zealand, France, and New Caledonia (site surveys); the Spanish Ministry of Economy and Competitiveness and Fondo Europeo de Desarrollo Regional (FEDER) funds project CGL2017-84693-R and a Leonardo Grant, BBVA Foundation (Alegret); Korean IODP (K-IODP) (Park); China grant NSFC 41473029, 91958110 (He Li); and Brazil grant 183/2017-CII/CGPE/DPB/CAPES (Giorgioni).	Aitchison JC, 2007, J GEOPHYS RES-SOL EA, V112, DOI 10.1029/2006JB004706; [Anonymous], 2017, GSA TODAY GEOL SOC A, DOI [10.1130/GSATG321A.1, DOI 10.1130/GSATG321A.1]; Arculus RJ, 2015, NAT GEOSCI, V8, P728, DOI 10.1038/NGEO2515; Bache F, 2012, EARTH PLANET SC LETT, V321, P41, DOI 10.1016/j.epsl.2011.12.041; Brovarone AV, 2018, EARTH-SCI REV, V178, P48, DOI 10.1016/j.earscirev.2018.01.006; Browne GH, 2016, NEW ZEAL J GEOL GEOP, V59, P396, DOI 10.1080/00288306.2016.1160940; Burns R.E., 1973, INITIAL REPORTS DEEP, V21, P271; Burns R. 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J	Otero, XL; Atiaga, O; Estrella, R; Tierra, W; Ruales, J; Zayas, L; Souza, V; Ferreira, TO; Nobrega, GN; Oliveira, DP; Queiroz, HM; Nunes, LM				Otero, X. L.; Atiaga, O.; Estrella, R.; Tierra, W.; Ruales, J.; Zayas, L.; Souza, V. Jr Jr; Ferreira, T. O.; Nobrega, G. N.; Oliveira, D. P.; Queiroz, H. M.; Nunes, L. M.			Geographical variations in arsenic contents in rice plants from Latin America and the Iberian Peninsula in relation to soil conditions	ENVIRONMENTAL GEOCHEMISTRY AND HEALTH			English	Article						Soil properties; Arsenic speciation; Phytoliths; Local and intercontinental variability	WATER MANAGEMENT; PADDY SOILS; FOOD-CHAIN; SPECIATION; ACCUMULATION; GRAIN; EXTRACTION; ELEMENTS; EXPOSURE; CADMIUM	Arsenic is a ubiquitous, toxic element that is efficiently accumulated by rice plants. This study assessed the spatial variability in the total As (tAs) contents and organic and inorganic forms in different types of rice, plant parts (husk, stem, leaves and phytoliths) and residues. Samples were collected in different countries in Latin America (Ecuador, Brazil and Peru) and the Iberian Peninsula (Spain and Portugal). The tAs content in commercial polished rice from the Latin American countries was similar (0.130-0.166 mg kg(-1)) and significantly lower than in the rice from the Iberian countries (0.191 +/- 0.066 mg kg(-1)), and together, the tAs concentration in brown rice (236 +/- 0.093 mg kg(-1)) was significantly higher than in polished and parboiled rice. The inorganic As (iAs) content in rice was similar in both geographical regions, and the aforementioned difference was attributed to dimethylarsinic acid (DMA). The relative abundance of organic species increased as the tAs content in rice grain increased. A meta-analysis of our and previously reported data confirmed the negative correlation between iAs/tAs and tAs. At low tAs concentrations, inorganic forms are dominant, while at higher values (tAs > 0.300 mg kg(-1)) the concentration of organic As increases substantially and DMA becomes the dominant form in rice grain. On the contrary, inorganic arsenic was always the dominant form, mainly as arsenate [As(V)], in leaves and stems. The presence in soils of high concentrations of amorphous Fe and Al oxides and hydroxides, which are capable of strongly adsorbing oxyanions (i.e. arsenate), was associated with low concentrations of As in rice plants. In addition, the presence of high concentrations of As(V) in stems and leaves, low concentration of As in phytoliths, and the As associated with organic matter in stems and husk, together suggest that rice plants take up more As(V) than As(III).	[Otero, X. L.; Atiaga, O.] Univ Santiago de Compostela, CRETUS Inst, Fac Bioloxia, Dept Edafoloxia & Quim Agr, Campus Sur, Santiago De Compostela 15782, Spain; [Atiaga, O.; Estrella, R.] Univ Fuerzas Armadas ESPE, Dept Ciencias Tierra & Construcc, Av Gen Ruminahui S-N,POB 171-5-231B, Sangolqui, Ecuador; [Tierra, W.; Ruales, J.] Escuela Politec Nacl, Dept Ciencia Alimentos & Biotecnol, Quito, Ecuador; [Zayas, L.; Ferreira, T. O.; Queiroz, H. M.] Univ Sao Paulo, ESALQ, Dept Ciencia Solo, Piracicaba, Brazil; [Souza, V. Jr Jr] Univ Fed Rural Pernambuco, Area Solo, Dept Agron, Recife, PE, Brazil; [Nobrega, G. N.] Univ Fed Fluminense, Dept Geoqufm, Outeiro Sao Joao Batista S-N,Campus Valonguinho, BR-2402014 Niteroi, RJ, Brazil	Universidade de Santiago de Compostela; Escuela Politecnica Superior del Ejercito; Escuela Politecnica Nacional Ecuador; Universidade de Sao Paulo; Universidade Federal Rural de Pernambuco (UFRPE); Universidade Federal Fluminense	Otero, XL (autor correspondente), Univ Santiago de Compostela, CRETUS Inst, Fac Bioloxia, Dept Edafoloxia & Quim Agr, Campus Sur, Santiago De Compostela 15782, Spain.	xl.otero@usc.es	Queiroz, Hermano Melo/P-8700-2019; Nóbrega, Gabriel Nuto/AAQ-4189-2020; Nunes, Luis M/D-7229-2016; Ferreira, Tiago Osório/D-3340-2015; Nunes, Luís/AFQ-5156-2022; Jimenez, Laís/GLV-4673-2022; Júnior, Valdomiro Severino Souza/G-1302-2016	Queiroz, Hermano Melo/0000-0003-4768-1248; Nóbrega, Gabriel Nuto/0000-0001-7008-4201; Nunes, Luis M/0000-0001-5606-970X; Ferreira, Tiago Osório/0000-0002-4088-7457; Nunes, Luís/0000-0001-5606-970X; Jimenez, Laís/0000-0002-1995-6083; Júnior, Valdomiro Severino Souza/0000-0002-1748-4019; Atiaga, Oliva/0000-0002-7653-512X	Universidad de las Fuerzas Armadas-ESPE [2015-PIC-017]; Xunta de Galicia-Conselleria de Educacion, Universidades e Formacion Profesional, Plan Galego IDT, Consolidation of competitive research groups [ED31C2018/12]; Sao Paulo Research Foundation-FAPESP [2018/04259-2]; Cross-Research in Environmental Technologies (CRETUS) [AGRUP2015/02, 2018-PG100]; Escuela Politecnica Nacional from Quito-Ecuador [PIJ15-10]; National Council for Scientific and Technology Development (CNPq) [305996/2018-5]; Proyecto PROMETEO (SENESCYT Ecuador)	Universidad de las Fuerzas Armadas-ESPE; Xunta de Galicia-Conselleria de Educacion, Universidades e Formacion Profesional, Plan Galego IDT, Consolidation of competitive research groups; Sao Paulo Research Foundation-FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Cross-Research in Environmental Technologies (CRETUS); Escuela Politecnica Nacional from Quito-Ecuador; National Council for Scientific and Technology Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Proyecto PROMETEO (SENESCYT Ecuador)	This study is part of a research project funded by the Universidad de las Fuerzas Armadas-ESPE through Project 2015-PIC-017, Xunta de Galicia-Conselleria de Educacion, Universidades e Formacion Profesional, Plan Galego IDT, Consolidation of competitive research groups (ref. ED31C2018/12), SAo Paulo Research Foundation-FAPESP (grant number 2018/04259-2), Cross-Research in Environmental Technologies (CRETUS, AGRUP2015/02, ref. 2018-PG100) and project PIJ15-10 financed by Escuela Politecnica Nacional from Quito-Ecuador. TOF thanks the National Council for Scientific and Technology Development (CNPq, process 305996/2018-5). XLOP is grateful for the financial support from the Proyecto PROMETEO (SENESCYT Ecuador). We thank Maria Jose Santiso for assistance with laboratory work and Augusto Perez Alberti and Esther Sierra Abrain for assistance with preparing the figures.	Abedin MJ, 2002, PLANT PHYSIOL, V128, P1120, DOI 10.1104/pp.010733; Alloway B. 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Geochem. Health	OCT	2020	42	10					3351	3372		10.1007/s10653-020-00581-8	http://dx.doi.org/10.1007/s10653-020-00581-8		APR 2020	22	Engineering, Environmental; Environmental Sciences; Public, Environmental & Occupational Health; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology; Public, Environmental & Occupational Health; Water Resources	NT0UD	32350805				2023-06-23	WOS:000529586200001
J	Cornaggia, F; Bernardini, S; Giorgioni, M; Silva, GLX; Nagy, AIM; Jovane, L				Cornaggia, Flaminia; Bernardini, Simone; Giorgioni, Martino; Silva, Gabriel L. X.; Nagy, Andre Istvan M.; Jovane, Luigi			Abyssal oceanic circulation and acidification during the Middle Eocene Climatic Optimum (MECO)	SCIENTIFIC REPORTS			English	Article							CONTESSA HIGHWAY SECTION; SOUTHERN-OCEAN; RAMAN-SPECTROSCOPY; ATMOSPHERIC CO2; MANGANESE; CALIBRATION; SEDIMENTS; MINERALS; HISTORY; SECTOR	The Middle Eocene Climatic Optimum (MECO) is a global warming event that occurred at around 40Ma and lasted about 500 kyr. We study this event in an abyssal setting of the Tasman Sea, using the IODP Core U1511B-16R, collected during the expedition 371. We analyse magnetic, mineralogical, and chemical parameters to investigate the evolution of the sea bottom conditions at this site during the middle Eocene. We observe significant changes indicating the response to the MECO perturbation. Mn oxides, in which Mn occurs under an oxidation state around +4, indicate a high Eh water environment. A prominent Mn anomaly, occurring just above the MECO interval, indicates a shift toward higher pH conditions shortly after the end of this event. Our results suggest more acid bottom water over the Tasman abyssal plain during the MECO, and an abrupt end of these conditions. This work provides the first evidence of MECO at abyssal depths and shows that acidification affected the entire oceanic water column during this event.	[Cornaggia, Flaminia; Silva, Gabriel L. X.; Jovane, Luigi] Univ Sao Paulo, Inst Oceanog, Sao Paulo, Brazil; [Bernardini, Simone] Univ Roma Tre, Dipartimento Sci, Rome, Italy; [Giorgioni, Martino] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Nagy, Andre Istvan M.] Fac Amer, Dept AI, Goiania, Go, Brazil; [Silva, Gabriel L. X.] INPE Inst Nacl Pesquisas Espaciais, Sao Jose Dos Campos SP, SP, Brazil	Universidade de Sao Paulo; Roma Tre University; Universidade de Brasilia; Instituto Nacional de Pesquisas Espaciais (INPE)	Cornaggia, F (autor correspondente), Univ Sao Paulo, Inst Oceanog, Sao Paulo, Brazil.	flaminia.cornaggia@gmail.com	Lucas Xavier da Silva, Gabriel/AAZ-6111-2021; Silva, Gabriel L.X./L-9936-2018; Jovane, Luigi/AAH-5438-2020	Lucas Xavier da Silva, Gabriel/0000-0003-2375-9370; Jovane, Luigi/0000-0003-4348-4714; Cornaggia, Flaminia/0000-0002-2832-2680; Giorgioni, Martino/0000-0003-0565-3150	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [11/22018-3, 16/24946-9, 18/17061-6]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [16/24946-9, 11/22018-3] Funding Source: FAPESP	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The authors thank the personnel of the XRD laboratory at the Geoscience Institute of the University of Brasilia, of the Scanning Electron Microscopy Laboratory of the Geosciences Institute of the University of Sao Paulo, of the Raman equipment of the Brazilian Research Unity in Astrobiology -NAP Astrobio Raman of the University of Sao Paulo, of the Infrared Spectroscopy Laboratory and Raman Spectroscopy Laboratory of the Department of Science of the Roma Tre University for the technical assistance during the analyses. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) -Finance Code 001 that granted the PhD fellowship of F.C. and the participation of M.G. in the IODP Expedition 371. This research is sponsored by the Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP projects 11/22018-3; 16/24946-9; 18/17061-6).	Anagnostou E, 2016, NATURE, V533, P380, DOI 10.1038/nature17423; [Anonymous], **NON-TRADITIONAL**; Bernardini S, 2020, RSC ADV, V10, P923, DOI 10.1039/c9ra08662e; BERNER RA, 1981, J SEDIMENT PETROL, V51, P359, DOI 10.1306/212F7C7F-2B24-11D7-8648000102C1865D; BEZDEK JC, 1984, COMPUT GEOSCI, V10, P191, DOI 10.1016/0098-3004(84)90020-7; Bijl PK, 2010, SCIENCE, V330, P819, DOI 10.1126/science.1193654; Bin H. 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J	Buso, VV; Milana, JP; di Pasquo, M; Paim, PSG; Philipp, RP; Aquino, CD; Cagliari, J; Chemale, F; Kneller, B				Buso, Victoria Valdez; Pablo Milana, Juan; di Pasquo, Mercedes; Gomes Paim, Paulo Sergio; Philipp, Ruy Paulo; Aquino, Carolina Danielski; Cagliari, Joice; Chemale Junior, Farid; Kneller, Ben			Timing of the Late Palaeozoic glaciation in western Gondwana: New ages and correlations from Paganzo and Parana basins	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Late Palaeozoic Ice Age; U-Pb zircon geochronology; Palynology; Paganzo Basin; Parana Basin	U-PB ZIRCON; SAN-JUAN PROVINCE; PLASMA-MASS SPECTROMETRY; GROUNDING-LINE SYSTEM; RIO BLANCO BASINS; ITARARE GROUP; TARIJA BASIN; ICP-MS; CARBONIFEROUS FORMATIONS; DEGLACIATION SEQUENCES	During the Late Palaeozoic, the Gondwana supercontinent formed an extensive Southern Hemisphere landmass that was affected by multiple glacial episodes, known collectively as the Late Palaeozoic Ice Age (LPIA). This resulted in the deposition of glacial, periglacial and deglacial sediments over much of the supercontinent. The Mississippian to early Pennsylvanian phase of glaciation is widely represented along the western margin of Gondwana. This constitutes one of the largest glaciations of the Phanerozoic in terms of its recorded extent and the widespread erosional hiatus it produced in the stratigraphic record. It was this mid Carboniferous glaciation, recorded in the Paganzo Basin of NW Argentina, that carved most of the paleovalleys and paleofjords present there. We report new U-Pb zircon ages from a single glacial succession (Guandacol Formation) of 326 +/- 3 Ma and 320 +/- 5 Ma, that in comparison with neighbouring dated sequences allow for the first time a reliable estimate of the timing and duration of glacial cycles. Palynological studies of these glacial-deglacial events yielded palynoassemblages of the MQ (Late Visean) and DMa (Sepukhovian-Bashkirian) Palynozones. The Carboniferous glacially-related strata and glacial cycles of the Paganzo Basin are compared here with equivalent units of the Parana Basin of SE Brazil, suggesting a similar climate record for most of western Gondwana. We propose a new correlation between these two basins. The new U-Pb zircon ages reported here indicate that a regional glacial peak occurred almost coincident with the Mississippian-Pennsylvanian boundary, suggesting that the ensuing postglacial transgression is the best regional marker to differentiate the Mississippian and Pennsylvanian as it forms an identifiable interbasinal horizon. The biostratigraphic and chronostratigraphic comparison with other LPIA successions from South America reinforces that the First Appearance Datum of monosaccate pollen grains occurs in the late Serpukhovian. Their correlation confirms that similar climate conditions prevailed across most of western Gondwana during this phase of the LPIA.	[Buso, Victoria Valdez; Kneller, Ben] Univ Aberdeen, Sch Geosci, Aberdeen AB24 3UE, Scotland; [Pablo Milana, Juan] Univ Nacl San Juan, Fac Ciencias Exactas Fis & Nat, CONICET, Av Ignacio de la Roza 590 O, RA-5400 San Juan, Argentina; [di Pasquo, Mercedes] CICYTTP CONICET ER UADER, Lab Palinoestratig & Paleobot, Dr Materi & Espana S-N,Diamante E3105BWA, Entre Rios, Argentina; [Gomes Paim, Paulo Sergio; Cagliari, Joice; Chemale Junior, Farid] Univ Vale Rio dos Sinos, Programa Posgrad, Av Unisinos 950, BR-93022000 Sao Leopoldo, RS, Brazil; [Philipp, Ruy Paulo] Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil; [Aquino, Carolina Danielski] UFPR Univ Fed Parana, Dept Geol, Av Cel Francisco H dos Santos 210, Curitiba, Parana, Brazil	University of Aberdeen; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad Nacional de San Juan; Universidade do Vale do Rio dos Sinos (Unisinos); Universidade Federal do Rio Grande do Sul; Universidade Federal do Parana	Buso, VV (autor correspondente), Univ Aberdeen, Sch Geosci, Aberdeen AB24 3UE, Scotland.	victoria.valdezbuso@abdn.ac.uk	Aquino, Carolina/AAD-4418-2020; Paim, Paulo Sergio Gomes/G-7274-2012; Aquino, Carolina Danielski/AAF-1372-2021; Cagliari, Joice/AAF-2983-2019	Cagliari, Joice/0000-0002-7074-9362; di Pasquo, Mercedes/0000-0003-3068-0089	BG Brazil E P Ltd.; ANP (Agencia Nacional do Petroleo, Gas Natural e Biocombustivel) [ANP BG 29]; Ciencias Sem Fronteiras Senior Researcher 2013 [PIP 0305, PIP 0812 (20151017)]; CICYTTP-CONICET-ER-UADER facilities; Brazilian National Council for Scientific and Technological Development (CNPq)	BG Brazil E P Ltd.; ANP (Agencia Nacional do Petroleo, Gas Natural e Biocombustivel); Ciencias Sem Fronteiras Senior Researcher 2013; CICYTTP-CONICET-ER-UADER facilities; Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work is part of a research project supported by BG Brazil E & P Ltd. entitled "Carboniferous de-Glacial record in the Parana Basin and its analogue in the Paganzo Basin of Argentina: Impacts on reservoir predictions". This project was carried out in collaboration with Universidade do Vale do Rio dos Sinos (UNISINOS), University of Aberdeen, Universidade Federal do Rio Grande do Sul (UFRGS), Universidad Nacional de San Juan (UNSJ), Argentina, and Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET). The authors would also like to acknowledge the ANP (Agencia Nacional do Petroleo, Gas Natural e Biocombustivel) (ANP BG 29) for its support to the project. Mercedes di Pasquo is grateful to Ciencias Sem Fronteiras Senior Researcher 2013 and PIP 0305 (2011-2013), PIP 0812 (20151017) and to CICYTTP-CONICET-ER-UADER facilities for their support. R.P. Philipp and P.S.G Paim express their thanks for the research grant from the Brazilian National Council for Scientific and Technological Development (CNPq).	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APR 15	2020	544								109624	10.1016/j.palaeo.2020.109624	http://dx.doi.org/10.1016/j.palaeo.2020.109624			23	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	KW4DT					2023-06-23	WOS:000521116600005
J	Rodriguez-Zorro, PA; Ledru, MP; Bard, E; Aquino-Alfonso, O; Camejo, A; Daniau, AL; Favier, C; Garcia, M; Mineli, TD; Rostek, F; Ricardi-Branco, F; Sawakuchi, AO; Simon, Q; Tachikawa, K; Thouveny, N				Rodriguez-Zorro, Paula A.; Ledru, Marie-Pierre; Bard, Edouard; Aquino-Alfonso, Olga; Camejo, Adriana; Daniau, Anne-Laure; Favier, Charly; Garcia, Marta; Mineli, Thays D.; Rostek, Frauke; Ricardi-Branco, Fresia; Sawakuchi, Andre Oliveira; Simon, Quentin; Tachikawa, Kazuyo; Thouveny, Nicolas			Shut down of the South American summer monsoon during the penultimate glacial	SCIENTIFIC REPORTS			English	Article							DIALKYL GLYCEROL TETRAETHERS; ATMOSPHERIC CIRCULATION; CLIMATE-CHANGE; POLLEN RECORD; SAO-PAULO; LAST; BRAZIL; PRECIPITATION; CARBON; SOILS	We analysed changes in mean annual air temperature (MAAT), vegetation and biomass burning on a long and continuous lake-peat sediment record from the Colonia basin, southeastern Brazil, examining the responses of a wet tropical rainforest over the last 180 ka. Stronger southern atmospheric circulation up to the latitude of Colonia was found for the penultimate glacial with lower temperatures than during the last glacial, while strengthening of the South American summer monsoon (SASM) circulation started during the last interglacial and progressively enhanced a longer wet summer season from 95 ka until the present. Past MAAT variations and fire history were possibly modulated by eccentricity, although with signatures which differ in average and in amplitude between the last 180 ka. Vegetation responses were driven by the interplay between the SASM and southern circulation linked to Antarctic ice volume, inferred by the presence of a cool mixed evergreen forest from 180 to 45 ka progressively replaced by a rainforest. We report cooler temperatures during the marine isotope stage 3 (MIS 3: 57-29 ka) than during the Last Glacial Maximum (LGM: 23-19 ka). Our findings show that tropical forest dynamics display different patterns than mid-latitude during the last 180 ka.	[Rodriguez-Zorro, Paula A.; Ledru, Marie-Pierre; Aquino-Alfonso, Olga; Favier, Charly] Univ Montpellier, ISEM, CNRS, EPHE,IRD, F-34095 Montpellier, France; [Bard, Edouard; Garcia, Marta; Rostek, Frauke; Simon, Quentin; Tachikawa, Kazuyo; Thouveny, Nicolas] Aix Marseille Univ, CEREGE, CNRS, IRD,INRAE,Coll France, F-13545 Aix En Provence, France; [Camejo, Adriana; Ricardi-Branco, Fresia] Univ Estadual Campinas, Inst Geosci, BR-13081970 Campinas, Brazil; [Daniau, Anne-Laure] Univ Bordeaux, UMR 5805, CNRS, EPOC, F-33615 Pessac, France; [Mineli, Thays D.; Sawakuchi, Andre Oliveira] Univ Sao Paulo, Inst Geosci, Sao Paulo, Brazil	Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; UDICE-French Research Universities; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); Centre National de la Recherche Scientifique (CNRS); INRAE; Institut de Recherche pour le Developpement (IRD); UDICE-French Research Universities; Aix-Marseille Universite; Universite PSL; College de France; Universidade Estadual de Campinas; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); UDICE-French Research Universities; Universite de Bordeaux; Universidade de Sao Paulo	Rodriguez-Zorro, PA (autor correspondente), Univ Montpellier, ISEM, CNRS, EPHE,IRD, F-34095 Montpellier, France.	paularsat@gmail.com	Camejo, Adriana Mercedes/AAA-5411-2022; Simon, Quentin/D-9956-2017; Sawakuchi, André O/D-1445-2013; Ricardi-Branco, Fresia/C-2034-2012; Daniau, Anne-Laure/O-2379-2017; Rodríguez-Zorro, Paula A./AAR-8099-2020; Favier, Charly/A-7516-2012	Camejo, Adriana Mercedes/0000-0002-3772-7057; Simon, Quentin/0000-0001-8247-0150; Daniau, Anne-Laure/0000-0002-1621-3911; Rodríguez-Zorro, Paula A./0000-0002-2476-1598; Sawakuchi, Andre/0000-0001-5016-2428; Favier, Charly/0000-0002-1126-6950; THOUVENY, Nicolas/0000-0001-6601-856X; Ledru, Marie-Pierre/0000-0002-8079-9320	FAPESP [BIOTA 2013/50297-0]; NSF [DEB 1343578]; Foundation BNP PARIBAS; CAPES; CNPq [304727/2017-2, 303527/2017-0]	FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); NSF(National Science Foundation (NSF)); Foundation BNP PARIBAS; CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This research is part of the projects "Dimensions of biodiversity" FAPESP (BIOTA 2013/50297-0), NSF (DEB 1343578) and NASA, the International Continental Deep drilling Program (ICDP), " UV-Trop " INSU LEFE, the Labex-CEBA, " TROPICOL " Foundation BNP Paribas " Climate Initiative " (2017-2020). P.A.R.Z and Q.S benefited from post-doctoral grants and O.A.A from a master grant from Foundation BNP PARIBAS. A.C benefited from a doctoral grant from CAPES. A.S is supported by CNPq (grants 304727/2017-2 and 303527/2017-0). We thank Laurent Augustin (C2FN, CNRS) and Laurent Bremond (EPHE) for coring CO14 during the ICDP workshop. We thank the Associacao ACHAVE for support at Colonia, and the Suehara family for allowing access to their property for the corings.	Adler RF, 2003, J HYDROMETEOROL, V4, P1147, DOI 10.1175/1525-7541(2003)004<1147:TVGPCP>2.0.CO;2; Aitken M.J., 1998, INTRO OPTICAL DATING, DOI DOI 10.1017/S0016756899551777; Baker PA, 2015, QUATERNARY SCI REV, V124, P31, DOI 10.1016/j.quascirev.2015.06.011; Bard E, 2009, NATURE, V460, P380, DOI 10.1038/nature08189; Bennett KD, 2012, HOLOCENE, V22, P1207, DOI 10.1177/0959683612450204; Bennett K. 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J	Zvirtes, G; Philipp, RP; Hurst, A; Palladino, G; De Ros, LF; Grippa, A				Zvirtes, G.; Philipp, R. P.; Hurst, A.; Palladino, G.; De Ros, L. F.; Grippa, A.			Petrofacies of Eocene sand injectites of the Tumey Giant Injection Complex, California(USA)	SEDIMENTARY GEOLOGY			English	Article						Sandinjection complex; Sandstone petrography; Injectite provenance; Reservoir petrofacies; Intragranular microfracturing; Fluid flow	VALLEY FORE-ARC; PREDICTING RESERVOIR QUALITY; DOMENGINE FORMATION EOCENE; DEEP-WATER SANDSTONES; CLASTIC INTRUSIONS; SEQUENCE STRATIGRAPHY; DEPOSITIONAL FACIES; INTERNAL STRUCTURES; JOAQUIN VALLEY; SIERRA-NEVADA	The forearc succession of Great Valley Group in Central California provides some of the best examples of giant sand injection complexes in the world and is therefore considered valuable analogues for injectite systems in the subsurface. Several sand injection complexes are well described in the outcrop and subsurface, however the petrographic characteristics of injectites are still poorly documented. In this paper, we present the results of an integrated study of field observations, quantitative and qualitative sandstone petrography, provenance, and petrofacies analysis of the Tumey Giant Injection Complex (TGIC) in order to understand its lithostratigraphy and petrological evolution, and its impacts on reservoir petrofacies characteristics and fluid migration. The TGIC intrudes into a 450 m thick deep-water succession of slope mudrocks and sandy channel-fills of the Kreyenhagen Shale (Eocene), forming an interconnected network of sandstone sills, dykes and injection breccias. The complex generated a horizontal and vertical plumbing system for fluid migration, connecting isolated sandy channel-fills among low-permeability mudrocks. The primary detrital composition, diagenetic products, microtextures, and provenance signatures allowed for the definition and discrimination of depositional and intrusive petrofacies and their genetic relations. Petrofacies associations confirm that the gypsum-cemented feldspathic litharenites from the Kreyenhagen Shale channel-fills are the only source for the injection complex. Eodiagenetic compaction and extensive gypsum cementation reduced the primary porosity of the complex, while telodiagenetic dissolution of autigenic constituents formed pervasive secondary porosity. The underlying calcite-cemented arkosic sandstones of the Lodo and Domengine formations acted as barriers for fluid flow, aiding lateral fluid migration and overpressure buildup within the overlying Kreyenhagen channel-fills. Intense grain microfracturing occurred during sand remobilization and injection along with erosion of the host mudrocks. This study has significance for the generation of reliable stratigraphic and petrological models for sand injection complex genesis and evolution that consequently can help the understanding and exploration of injectite complexes elsewhere. (C) 2020 Elsevier B.V. All rights reserved.	[Zvirtes, G.; Hurst, A.; Palladino, G.; Grippa, A.] Univ Aberdeen, Dept Geol & Petr Geol, Aberdeen AB24 3FX, Scotland; [Philipp, R. P.; De Ros, L. F.] Univ Fed Rio Grande do Sul, Dept Mineral & Petrol, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil; [Zvirtes, G.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias PPGGEO, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil; [Palladino, G.] Univ Basilicata, Dipartimento Sci, Potenza, Italy	University of Aberdeen; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; University of Basilicata	Zvirtes, G (autor correspondente), Univ Aberdeen, Dept Geol & Petr Geol, Aberdeen AB24 3FX, Scotland.	zvirtes.gustavo@gmail.com	; De Ros, Luiz Fernando/Q-5439-2018	PHILIPP, RUY PAULO/0000-0003-2875-0914; De Ros, Luiz Fernando/0000-0003-2651-8097; Zvirtes, Gustavo/0000-0001-9728-0464	Shell Braziland CNPq; UoA; ANP through the R&D levy regulation; Sand Injection Research Group (SIRG)	Shell Braziland CNPq; UoA; ANP through the R&D levy regulation; Sand Injection Research Group (SIRG)	The author sgratefully acknowledge support from Shell Braziland CNPq through the "BG05: UoA-UFRGS-SWB Sedimentary Systems" project at UFRGS and UoA and the strategic importance of the support given by ANP through the R&D levy regulation. We thank all the support from the Sand Injection Research Group (SIRG). We also wish to thank the support of the Bureau of Land Management (CA-USA) providing legal access to the study area.	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J	Marquetto, L; Kaspari, S; Simoes, JC; Babik, E				Marquetto, Luciano; Kaspari, Susan; Simoes, Jefferson Cardia; Babik, Emil			Refractory Black Carbon Results and a Method Comparison between Solid-state Cutting and Continuous Melting Sampling of a West Antarctic Snow and Firn Core	ADVANCES IN ATMOSPHERIC SCIENCES			English	Article						black carbon; West Antarctica; ice core; single particle soot photometer	ICE CORE; DEPOSITION; CLIMATE; VARIABILITY; AEROSOLS; RECORDS; DUST	This work presents the refractory black carbon (rBC) results of a snow and firn core drilled in West Antarctica (79 degrees 55 ' 34.6 '' S, 94 degrees 21 ' 13.3 '' W) during the 2014-15 austral summer, collected by Brazilian researchers as part of the First Brazilian West Antarctic Ice Sheet Traverse. The core was drilled to a depth of 20 m, and we present the results of the first 8 m by comparing two subsampling methods-solid-state cutting and continuous melting-both with discrete sampling. The core was analyzed at the Department of Geological Sciences, Central Washington University (CWU), WA, USA, using a single particle soot photometer (SP2) coupled to a CETAC Marin-5 nebulizer. The continuous melting system was recently assembled at CWU and these are its first results. We also present experimental results regarding SP2 reproducibility, indicating that sample concentration has a greater influence than the analysis time on the reproducibility for low rBC concentrations, like those found in the Antarctic core. Dating was carried out using mainly the rBC variation and sulfur, sodium and strontium as secondary parameters, giving the core 17 years (1998-2014). The data show a well-defined seasonality of rBC concentrations for these first meters, with geometric mean summer/fall concentrations of 0.016 mu g L-1 and geometric mean winter/spring concentrations of 0.063 mu g L-1. The annual rBC concentration geometric mean was 0.029 mu g L-1 (the lowest of all rBC cores in Antarctica referenced in this work), while the annual rBC flux was 6.1 mu g m(-2) yr(-1) (the lowest flux in West Antarctica records so far).	[Marquetto, Luciano; Kaspari, Susan; Babik, Emil] Cent Washington Univ, Dept Geol Sci, Ellensburg, WA 98926 USA; [Marquetto, Luciano; Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul, Polar & Climat Ctr, BR-91509900 Porto Alegre, RS, Brazil	Central Washington University; Universidade Federal do Rio Grande do Sul	Marquetto, L (autor correspondente), Cent Washington Univ, Dept Geol Sci, Ellensburg, WA 98926 USA.; Marquetto, L (autor correspondente), Univ Fed Rio Grande do Sul, Polar & Climat Ctr, BR-91509900 Porto Alegre, RS, Brazil.	luciano.marquetto@gmail.com	Simoes, Jefferson Cardia/D-7232-2013	Simoes, Jefferson Cardia/0000-0001-5555-3401	Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program [200386/2018-2]; CNPq [465680/2014-3, 442761/2018-0]	Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This research is part of the Brazilian Antarctic Program (PROANTAR) and was financed with funds from the Brazilian National Council for Scientific and Technological Development (CNPq) Split Fellowship Program (Grant No. 200386/2018-2) and from the CNPq projects 465680/2014-3 and 442761/2018-0. We thank the Centro Polar e Climatico (CPC/UFRGS) and the Department of Geological Sciences (CWU) faculty and staff for their support of this work. We also thank the anonymous reviewers for their comments and suggestions, as well as the Advances in Atmospheric Sciences team.	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A., 2014, ATMOS MEAS TECH DISC, V7, P3075, DOI [10.5194/amtd-7-3075-2014, DOI 10.5194/AMTD-7-3075-2014]; Winstrup M, 2017, CLIM PAST DISCUSS, DOI [10.5194/cp-2017-101, DOI 10.5194/CP-2017-101]	37	2	3	2	13	SCIENCE PRESS	BEIJING	16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA	0256-1530	1861-9533		ADV ATMOS SCI	Adv. Atmos. Sci.	MAY	2020	37	5			SI		545	554		10.1007/s00376-019-9124-8	http://dx.doi.org/10.1007/s00376-019-9124-8		APR 2020	10	Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Meteorology & Atmospheric Sciences	LE2HU		Bronze			2023-06-23	WOS:000523585200003
J	Porfirio, DM; Monteiro, LR; da Costa, ML				Porfirio, Darilena Monteiro; Monteiro, Lucilena Rebelo; da Costa, Marcondes Lima			Rainwater geochemistry inside the Barcarena power station at the mouth of the Tocantins River	ENVIRONMENTAL TECHNOLOGY			English	Article						Rainwater and pollution; enrichment factor; major ions; power plant; principal component analysis	CHEMICAL-COMPOSITION; PRECIPITATION; NITROGEN; DEPOSITION; CHEMISTRY; ACIDITY; EUROPE; PLANT; COAST	Most of South America lacks studies on rainwater composition. The present study evaluates rainwater composition and bulk deposition inside Barcarena power station, located at the mouth of the Tocantins River with Amazon River in Brazil. In 2012, 24-h rainwater samples were collected inside the ELETRONORTE power plant (n = 93), and pH, EC, cations and anions were analyzed. In order of abundance, the rainwater ions were Na+ > Cl- > SO4-2 > Ca+2 > K+ > F- > Mg+2 > NH4+-N > NO3--N. pH values ranged from 4.5 to 6.9, with 17 events with pH <5.6 and 5 events with pH < 5.0. Sodium and Cl- were the dominant ions with sea salt as main contribution. Acidity, enrichment factors and principal component analysis (PCA) indicate that F-, SO4-2 and NO3--N in the rainwater came from anthropogenic sources. Fluoride correlated strongly (>0.85) with Ca+2 and Mg+2, likely originated from same source in the aluminum production chain. Potassium originated from a mixture of anthropogenic and natural sources, with a good correlation (>0.70) with NO3--N and NH4+-N, indicating biomass burning and fertilizer origins. In 2012, Barcarena total bulk deposition ranged from 14,070 to 17,890 mg m(-2) y(-1) with significant contributions of SO4(-2) (2,385 to 2,851 mg m(-2) y(-1)), F- (419 to 479 mg m(-2) y(-1)) and NO3--N (128 to 280 mg m(-2) y(-1)). EC values (4 to 254 mu S cm(-1)) indicated a medium site pollution severity (> 175 mu S cm(-1)), which increased the risk of damage to electrical components.	[Porfirio, Darilena Monteiro] Ctr Tecnol Eletronorte Eletrobras OCT, BR-66115000 Belem, Para, Brazil; [Porfirio, Darilena Monteiro; da Costa, Marcondes Lima] Univ Fed Para PPGG UFPA, Programa Posgrad Geol & Geoquim, Belem, Para, Brazil; [Monteiro, Lucilena Rebelo] Ipen CNEN SP Inst Pesquisas Energet & Nucl, Sao Paulo, Brazil	Comissao Nacional de Energia Nuclear (CNEN); Instituto de Pesquisas Energeticas e Nucleares (IPEN)	Porfirio, DM (autor correspondente), Ctr Tecnol Eletronorte Eletrobras OCT, BR-66115000 Belem, Para, Brazil.; Porfirio, DM (autor correspondente), Univ Fed Para PPGG UFPA, Programa Posgrad Geol & Geoquim, Belem, Para, Brazil.	darilenap@yahoo.com.br	Monteiro, Lucilena/AAN-9557-2020	Monteiro, Lucilena/0000-0002-4457-4925; LIMA DA COSTA, MARCONDES/0000-0002-0134-0432	Agencia Nacional de Energia Eletrica -ANEEL from PROPESP/UFPA [4500078262]; National Council for Scientific and Technological Development - CNPq [305015/2016-8]	Agencia Nacional de Energia Eletrica -ANEEL from PROPESP/UFPA; National Council for Scientific and Technological Development - CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the financial support provided by Agencia Nacional de Energia Eletrica -ANEEL to the project "Desenvolvimento de Tecnologia para Avaliacao de Desempenho de Isoladores e Areas de Alta Agressividade contrato" #4500078262 from 2013 to 2016, PROPESP/UFPA and National Council for Scientific and Technological Development - CNPq (Grant number 305015/2016-8).	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A., 2017, Ambiente & Agua, V12, P435, DOI 10.4136/ambi-agua.1910; Pye KENNETH, 1987, AEOLIAN DUST DUST DE, P198; Pylarinos D, 2003, ADV ENV SCI DEV CHEM; Salve PR, 2008, B ENVIRON CONTAM TOX, V80, P242, DOI 10.1007/s00128-007-9353-x; Santos PSM, 2011, SCI TOTAL ENVIRON, V409, P3548, DOI 10.1016/j.scitotenv.2011.05.031; Satyamurty P, 2013, THEOR APPL CLIMATOL, V111, P195, DOI 10.1007/s00704-012-0637-7; Staelens J, 2005, ATMOS ENVIRON, V39, P7, DOI 10.1016/j.atmosenv.2004.09.055; Varejo-Silva MA, 2006, METEOROLOGIA CLIMATO; Vet R, 2014, ATMOS ENVIRON, V93, P3, DOI 10.1016/j.atmosenv.2013.10.060; Walna B, 2013, ENVIRON MONIT ASSESS, V185, P5497, DOI 10.1007/s10661-012-2962-9; WMO, 2004, MAN GAW PREC CHEM PR; Xiao J, 2016, ENVIRON EARTH SCI, V75, DOI 10.1007/s12665-015-4997-z; You CF, 2010, ENERGY, V35, P4467, DOI 10.1016/j.energy.2009.04.019	45	4	4	5	11	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0959-3330	1479-487X		ENVIRON TECHNOL	Environ. Technol.	APR 2	2020	41	8					981	996		10.1080/09593330.2018.1516801	http://dx.doi.org/10.1080/09593330.2018.1516801			16	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	KR1GF	30148424				2023-06-23	WOS:000517366600004
J	Althaus, CE; Scherer, CMD; Kuchle, J; dos Reis, AD; Ferronatto, JPF; De Ros, LF; Bardola, TP				Althaus, Camila Eliza; dos Santos Scherer, Claiton Marlon; Kuchle, Juliano; dos Reis, Adriano Domingos; Formolo Ferronatto, Joao Pedro; De Ros, Luiz Fernando; Bardola, Tatiana Pastro			Wave-dominated lacustrine margin of Aptian pre-salt: Mucuri Member, Espirito Santo Basin	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Lake wave-dominated; Pre-salt; Lacustrine system; Strontium isotopes in anhydrites; Aptian reservoirs	SEQUENCE STRATIGRAPHY; FACIES; SEDIMENTATION; ARCHITECTURE; DEPOSITS; MARINE	The Espirito Santo Basin, one of the Brazilian marginal basins formed during the Gondwana break-up, is composed by three main depositional units - rift, sag and drift phases. The Mucuri Member sandstones are the Aptian sag phase related, onshore reservoirs deposited at the margins of the lacustrine system were the pre-salt (preevaporitic succession) lacustrine carbonate reservoirs were generated. The main objective of this article focuses on the stratigraphic and sedimentological definition of depositional model from the top of the Mucuri Member, in the transition to Itatinas Member evaporites of Mariricu Formation, since the depositional conditions of this interval until date remain under discussions and can contribute to the understanding of the correlated pre-salt reservoirs. Core description in detailed scale (1:50) associated with gamma-ray logs allowed the identification of nineteen facies, grouped into five facies associations: gravelly fluvial channel, poorly confined fluvial channels, upper shoreface, lower shoreface and offshore. Stacking patterns of facies associations allowed the definition of four cycles: T, T-R, normal R and forced R cycles. Although these cycles are easily recognizable in the cores, their correlation between wells was not possible. Geochemical analyses of Sr-87/Sr-86 ratio from anhydrites layers interbedded with the Mucuri sandstones confirmed a non-marine composition for the precipitating fluids. The integrated evidence suggests a wave dominated lacustrine coastal environment for the subaqueous Mucuri Member deposits.	[Althaus, Camila Eliza; dos Reis, Adriano Domingos; Formolo Ferronatto, Joao Pedro; Bardola, Tatiana Pastro] Univ Fed Rio Grande do Sul, Agron, Programa Posgrad Geociencias, Av Bento Goncalves 9500,Predio 43137, BR-91501970 Porto Alegre, RS, Brazil; [dos Santos Scherer, Claiton Marlon; Kuchle, Juliano; De Ros, Luiz Fernando] Univ Fed Rio Grande do Sul, Inst Geociencias, Agron, Av Bento Goncalves 9500,Predio 43137, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Althaus, CE (autor correspondente), Univ Fed Rio Grande do Sul, Agron, Programa Posgrad Geociencias, Av Bento Goncalves 9500,Predio 43137, BR-91501970 Porto Alegre, RS, Brazil.	camila.althaus@ufrgs.br	Reis, Adriano/E-3744-2015; De Ros, Luiz Fernando/Q-5439-2018	Reis, Adriano/0000-0003-1892-8459; De Ros, Luiz Fernando/0000-0003-2651-8097; Santos Scherer, Claiton Marlon dos/0000-0002-7520-1187; althaus, camila eliza/0000-0003-4402-6037	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); Shell Brasil Petroleo Ltda; ANP (Brazil's National Oil, Natural Gas and Biofuels Agency) through the R&D levy regulation	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Shell Brasil Petroleo Ltda; ANP (Brazil's National Oil, Natural Gas and Biofuels Agency) through the R&D levy regulation	This work was supported by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), which provided the first author's Master's Degree scholarship. We thank to Carrel Kifumbi support with graphic model. The authors gratefully acknowledge support from Shell Brasil Petroleo Ltda and the strategic importance of the support given by ANP (Brazil's National Oil, Natural Gas and Biofuels Agency) through the R&D levy regulation.	AINSWORTH RB, 1994, J GEOL SOC LONDON, V151, P681, DOI 10.1144/gsjgs.151.4.0681; Aleali M, 2013, J ASIAN EARTH SCI, V75, P110, DOI 10.1016/j.jseaes.2013.07.017; ALLEN JRL, 1983, SEDIMENT GEOL, V33, P237, DOI 10.1016/0037-0738(83)90076-3; ALLEN JRL, 1963, SEDIMENTOLOGY, V2, P93, DOI 10.1111/j.1365-3091.1963.tb01204.x; Amorosi A, 2005, MAR GEOL, V222, P7, DOI 10.1016/j.margeo.2005.06.041; [Anonymous], 1998, THESIS; Blair T. 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J	Borba, ML; Tassinari, CCG; Kirk, J; Ruiz, J				Borba, Mauricio L.; Tassinari, Colombo C. G.; Kirk, Jason; Ruiz, Joaquin			Ages and isotope evolution of the Agua Rica Cu-Au porphyry-epithermal deposit, NW Argentina	ORE GEOLOGY REVIEWS			English	Article						Agua Rica; Cu-Au porphyry; Epithermal; Farallon Negro Volcanic Complex; U-Pb SHRIMP; Re-Os isotopes; Pb isotopes	NAZCA PLATE BENEATH; LA-ALUMBRERA; COPPER-GOLD; MAGMA CHAMBER; BAJO; NEGRO; ORE; SUBDUCTION; CATAMARCA; OSMIUM	The link between porphyry-epithermal deposits and continental-arc magmatism is widely accepted, but in flatslab settings the source of metals is still debated. The Central Andes region hosts numerous important mineral deposits within the flat-subduction zone including the world-class Agua Rica Cu-Au (Mo) porphyry-epithermal deposit, which is associated with the Farallon Negro Volcanic Complex. The suite of mineralization at Agua Rica includes a porphyry-Cu phase, an associated epithermal assemblage and a supergene enrichment overprint. The main mineralization is considered to be related to the Trampeadero and Seca Norte dacite porphyry intrusions, for which U-Pb SHRIMP zircon ages are 6.09 +/- 0.17 and 5.81 +/- 0.32 Ma to 5.41 +/- 0.25 respectively. Rhenium-Os dating of pyrite from the Trampeadero porphyry yielded an isochron with an age of 5.85 +/- 0.42 Ma, and molybdenite yielded a model age of 5.61 +/- 0.03 Ma. The Seca Norte body was responsible for the main porphyry-style mineralization, while the older Trampeadero porphyry served as a host rock. Magmatic-hydrothermal activity at Agua Rica commenced at approximately the same time as it was ending in other parts of the volcanic complex. Pb isotope signatures of sulfide samples from Agua Rica indicate a significant addition of crustal material to a mantle source. Neogene magmatism in the area is likely related to the subduction of the Juan Fernandez Ridge, which was subjacent to the deposit by the time of the porphyry intrusions. Upper crustal MASH (mixing, assimilation, storage, and homogenization) in the melting zone above the slab is inferred as the source of the shallow magma reservoir beneath the Farallon Negro Volcanic Complex.	[Borba, Mauricio L.; Tassinari, Colombo C. G.] Univ Sao Paulo, Inst Geosci, BR-05508080 Sao Paulo, Brazil; [Kirk, Jason; Ruiz, Joaquin] Univ Arizona, Dept Geosci, Tucson, AZ 85721 USA	Universidade de Sao Paulo; University of Arizona	Borba, ML (autor correspondente), Univ Sao Paulo, Inst Geosci, BR-05508080 Sao Paulo, Brazil.	mauriciolborba@usp.br	Borba, Mauricio Liska/AAX-3539-2020	Borba, Mauricio Liska/0000-0003-1598-1334	Brazilian National Council for Scientific and Technological Development [CNPq 142827/2011-8, CNPq 201916/2014-2, CNPq 302962/2010-7]	Brazilian National Council for Scientific and Technological Development(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The Brazilian National Council for Scientific and Technological Development supported this study (grant CNPq 142827/2011-8 and CNPq 201916/2014-2 and as part of the project: "Geologia Isotopica aplicada no estudo de processos tectonicos e metalogeneticos no tempo geologico", grant CNPq 302962/2010-7). We would like to thank the Minera Agua Rica team for help in the field and sampling, special thanks to geologist Pedro Ruiz. We are also thankful to Minera Alumbrera Ltd. team, mostly to geologists Ariana Carrazana and Julio Bruna and particularly to the technician Victor Acosta, for helping with the samples. We are also thankful to Dr. Marianne Landtwing, for sharing Agua Rica detailed maps and reports. The authors are also thankful to the isotope laboratory teams at the University of Sao Paulo and the University of Arizona, especially to Dr. Kei Sato, Rodrigo Azzi Silva and Mark Baker.	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Rev.	APR	2020	119								103395	10.1016/j.oregeorev.2020.103395	http://dx.doi.org/10.1016/j.oregeorev.2020.103395			14	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	LG2KR					2023-06-23	WOS:000527936800003
J	Brown, MT; Fuck, RA; Dantas, EL				Brown, Matthew T.; Fuck, Reinhardt A.; Dantas, Elton L.			Isotopic age constraints and geochemical results of disseminated ophiolitic assemblage from Neoproterozoic melange, central Brazil	PRECAMBRIAN RESEARCH			English	Article						Brasilia Belt; Neoproterozoic; Araxa Group; Ophiolite; Black-wall	SOUTHERN BRASILIA BELT; U-PB GEOCHRONOLOGY; ULTRAHIGH-TEMPERATURE METAMORPHISM; PLASMA-MASS SPECTROMETRY; ANAPOLIS-ITAUCU COMPLEX; ISUA SUPRACRUSTAL BELT; SM-ND GEOCHRONOLOGY; TECTONIC EVOLUTION; TRACE-ELEMENT; OCEANIC-CRUST	The Neoproterozoic Brasilia belt, central Brazil, formed during the amalgamation of West Gondwana, and contains a magmatic arc and a large metasedimentary pile. An ophiolitic melange is contained within one of the metasedimentary units from the pile, and includes bodies of metamafic and ultramafic assemblages in a metasedimentary rock matrix. One of these metamafic bodies encompasses a serpentinite body, which displays a well-developed metasomatic "black-wall" alteration zone at its contact. Samples of metamafic, serpentinite and black-wall rocks were collected, as well as two garnet-mica schists in contact with the metamafic assemblage. The metamafic assemblage is composed of epidote-amphibole schist, chemical analysis of which indicates that its protolith was a tholeiitic basalt with a MORB signature that may have been formed in a back-arc environment. U-Pb analyses indicate an age of crystallization of c. 800 Ma for the protolith of the epidote-amphibole schist. The black-wall is mostly composed of chlorite schist, with the exception of an albite-hornblende fels at the contact with the epidote-amphibole schist. The black-wall has a range of ages from c. 800 to 760 Ma. epsilon(Hf) values of selected zircon grains of the epidote-amphibole schist sample range from -21.67 to + 13.66, with T-DM ages of 0.80-4.22 Ga, while the black-wall samples have highly depleted epsilon(Hf) values ranging from + 9.16 to + 23.98, with T-DM model ages of 0.34-0.96 Ga. The studied garnet-mica schists have zircon population peaks of c. 790 to 890 Ma. epsilon(Hf) ranges from -14.87 to + 6.46 and T-DM ages from 1.47 to 1.91 Ga. The epidote-amphibole schist, serpentinite and black-wall assemblages all have positive epsilon(Nd) values from + 4.95 to + 7.89, indicating a mantle signature. epsilon(Nd) values for the mica schists are -8.31 and -8.16, and their T-DM values are 1.83 and 2.36 Ga, which indicate continentally derived components. The results suggest that the ophiolitic component of the Araxa melange formed in a back-arc basin environment, which formed at c. 800 Ma and lasted till c. 760 Ma, while the studied schists probably represent sediments deposited in the newly formed back-arc basin.	[Brown, Matthew T.; Fuck, Reinhardt A.; Dantas, Elton L.] Univ Brasilia, Inst Geosci, Lab Geochronolgy, BR-70910900 Brasilia, DF, Brazil	Universidade de Brasilia	Brown, MT (autor correspondente), Univ Brasilia, Inst Geosci, Lab Geochronolgy, BR-70910900 Brasilia, DF, Brazil.	brown.unb.2019@gmail.com	Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059	Brazilian National Council for Scientific and Technological Development (CNPq) [148938/2014-0]; CNPq [308312/2014-7, 454272/2014-6]	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The first author would like to acknowledge the Brazilian National Council for Scientific and Technological Development (CNPq) for the doctoral scholarship No. 148938/2014-0. Reinhardt A. Fuck and Elton L. Dantas acknowledge CNPq research fellowships No. 308312/2014-7 and No. 454272/2014-6.	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APR	2020	339								105581	10.1016/j.precamres.2019.105581	http://dx.doi.org/10.1016/j.precamres.2019.105581			33	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KR8FS					2023-06-23	WOS:000517852000011
J	Coimbra, JC				Coimbra, Joao Carlos			THE GENUS CYPRIDEA (CRUSTACEA, OSTRACODA) AND THE AGE OF THE QUIRICO FORMATION, SE BRAZIL: A CRITICAL REVIEW	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Review						biostratigraphy; Cretaceous; Minas Gerais State; paleolimnology; Quirico Formation	BASIN; TAXONOMY	The non-marine ostracod Cypridea Bosquet is surprisingly diverse worldwide, especially in the Cretaceous. Due to their short temporal distribution, many Cypridea species together with other typical Pre-Salt ostracod genera, such as Ilhasina Krommelbein, Paracypridea Swain, Petrobrasia Krommelbein, Reconcavona Krommelbein, and Theriosynoecum Branson, have provided a robust biostratigraphic framework for Brazilian and Western African basins. The Reconcavo-Tucano Basin, located in the Bahia State, was the first Brazilian oil basin. This huge Mesozoic paleolake has over a hundred of ostracod species, most of the genus Cypridea, which allowed the development of a biostratigraphic chart with nine biozones and several subzones. This biostratigraphic framework has been used for correlations with most of the non-marine sections of NE and SE Brazilian basins, including the Sanfranciscana Basin, whose lacustrine outcrops correspond to the Quirico Formation. Nevertheless, in a recent publication on ostracods and the age of the Quirico Formation, Cypridea species were erroneously identified. Consequently, a Valanginian age was wrongly proposed for the base of that formation, and the stratigraphic and geographical distributions of some species were erroneously extended. The present study reveals that none Cypridea species of the Quirico Formation is conspecific with the Reconcavo-Tucano Basin species, including Cypridea hystrix Krommelbein, and, consequently, a Valanginian age is discarded for the base of that formation.	[Coimbra, Joao Carlos] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Cx P 15001, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Coimbra, JC (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Cx P 15001, BR-91501970 Porto Alegre, RS, Brazil.	joao.coimbra@ufrgs.br	Coimbra, Joao Carlos/H-7500-2013	Coimbra, Joao Carlos/0000-0002-8980-6531	National Council for Scientific and Technological Development (CNPq) [305128/2017-5]	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	I express my gratitude to the National Council for Scientific and Technological Development (CNPq) for Grant 305128/2017-5. C.T. Bergue, E.K. Piovesan and M. Arai are thanked for their useful comments and suggestions that significantly improve the quality of the manuscript.	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J	de Souza, SRC; Botelho, NF; Dantas, EL; Jimenez, FAC; Reis, MA; Viana, CS				Cortez de Souza, Sebastido Rodrigo; Botelho, Nilson Francisquini; Dantas, Elton Luiz; Cuadros Jimenez, Federico Alberto; Reis, Mateus Andrade; Viana, Camila Salles			Geochemistry and isotopic geology of the Lagoa Seca gold deposit in the Andorinhas greenstone-belt, Carajas Province, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Orogenic gold deposit; Hydrothermal alteration; Isotopic geology; Amazonian Craton; Mesoarchean	U-PB GEOCHRONOLOGY; OROGENIC GOLD; ZIRCON GEOCHRONOLOGY; TRACE-ELEMENT; SOUTH-AFRICA; MINERALIZATION; GREENLAND; TERRANE; ORIGIN; CRATON	The Lagoa Seca is a gold deposit located in the Mesoarchean Andorinhas greenstone belt in the eastern portion of the Amazonian Craton, northern Brazil. It consists of clastic metasedimentary (metagreywacke and metasiltstone) and metavolcanic (metadacite and metaultramafic) rocks. It was operated by Troy Resources Ltd. as an open pit mine from 2008 to 2014, and it produced approximately 150 koz of gold. The hydrothermal alteration halo is directly associated with the internal zonation of the Lagoa Seca shear zone, and it includes i) a distal zone composed of chlorite-epidote-carbonate, ii) an intermediate zone with minerals from the distal alteration plus moderate silicification, iii) a proximal zone composed of biotite-magnetite (carbonate-amphibole-sulfide-gold), and iv) a gold-rich ore zone that has been affected by sulfidation and potassification. Whole-rock geochemistry and mineral chemistry studies on the hydrothermally altered host rocks show that Al2O5 and Na2O increase with silica content, while Fe2O3, MnO, MgO, CaO and the LOI decrease. The minor and trace elements are characterized by very good correlations among Zr, Nb, Ti and LREEs. The REE patterns of hydrothermal rocks show high to moderate fractionation with the La/Lu(cn) of the LREEs and HREEs towards the center of the hydrothermal conduit and are accompanied by a weak negative europium anomaly. The trace-element geochemistry is consistent with that of the subduction related calc-alkaline magmas in continental arcs. In addition, the tectonic discriminant diagrams show a calc-alkaline affinity and classify the host rocks as being derived from subduction processes. The hydrothermal chlorites are classified as brungsvite; mica is phlogopite and amphiboles range from actinolite, tremolite to Mg-hornblende. The main sulfide is pyrite, which is accompanied by minor amounts of chalcopyrite, galena, pyrrhotite and traces of millerite. The EPMA analysis of the pyrite shows that As, Co and Cu increase towards the center of the hydrothermal zone, as well as Zn, Ni and Au decrease in the opposite direction. Gold is present predominantly as inclusions in pyrite/chalcopyrite, with a high Au content. A chlorite geothermometer indicates that the temperatures ranged from 275 degrees C to 351 degrees C in the hydrothermal zones. The oxygen and carbon stable isotope data from the calcite of the ore zone return values of 8.12 parts per thousand SMOW and -6.36 parts per thousand PDB, respectively, which are compatible with a metamorphic fluid source. However, sulfur stable isotope displays 1.92 parts per thousand V-CDT, which may suggest a magmatic sulfur source. The composition of the fine-grained pyrite indicates that the hydrothermal fluid presents a deep crustal source of metamorphic origin, and it is accompanied by a mixed magmatic contribution, which was probably generated during the dominant TTG evolution of the area. The whole-rock Sm-Nd isotopic analyses produced a TDM of 2.92-3.04 Ga and an epsilon Nd (2.9) of + 0.39 to + 1.67 for metaultramafic rocks, a TDM of 2.78-2.92 Ga and an epsilon Nd of (2.9) + 1.61 to +2.92 for metasedimentary rocks, and a TDM of 2.79-2.83 Ga and an epsilon Nd of (2.9) + 2.83 to + 3.02 for metadacite rocks. An Sm-Nd isochron age of 2867 +/- 40 Ma indicates a Mesoarchean age for the host rocks.	[Cortez de Souza, Sebastido Rodrigo] Univ Fed Pernambuco UFPE, Dept Geol, Ave Arquitetura S-N,Cidade Univ, BR-50740550 Recife, PE, Brazil; [Botelho, Nilson Francisquini; Dantas, Elton Luiz; Cuadros Jimenez, Federico Alberto] Univ Brasilia UnB, Inst Geociencias, Campus Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Reis, Mateus Andrade; Viana, Camila Salles] Univ Brasilia UnB, Inst Geociencias, Programa Posgrad Geol, Campus Darcy Ribeiro ICC, BR-70910900 Brasilia, DF, Brazil	Universidade Federal de Pernambuco; Universidade de Brasilia; Universidade de Brasilia	de Souza, SRC (autor correspondente), Univ Fed Pernambuco UFPE, Dept Geol, Ave Arquitetura S-N,Cidade Univ, BR-50740550 Recife, PE, Brazil.	rodrigo.cortez@ufpe.br	Dantas, Elton Luiz/AAK-8464-2021; Jiménez, Federico Alberto Cuadros/AAK-8547-2021; Botelho, Nilson Francisquini/T-9470-2017	Dantas, Elton Luiz/0000-0002-7954-5059; Jiménez, Federico Alberto Cuadros/0000-0002-2297-9964; Botelho, Nilson Francisquini/0000-0001-9090-799X; Souza, Sebastiao Rodrigo Cortez de/0000-0001-5185-133X	Troy Resources Ltd (Reinarda Mineracao Ltda); brazilian agency CAPES	Troy Resources Ltd (Reinarda Mineracao Ltda); brazilian agency CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work is part of the first author's Ph.D. thesis project and was supported by Troy Resources Ltd (Reinarda Mineracao Ltda) which provide access to drill core and is published with permission. The authors would like to thank the Andorinhas Project geology team, in particular Augusto Mol, Ezequiel Costa e Silva, Wilson Bastos, Adriane Felipe and Natanael Lima, as well as Peter J. Doyle, VP of Troy's Exploration and Business Development. SRCS would like to acknowledge the brazilian agency CAPES for a research grant during part of his Ph.D. thesis. We are also thankful to the constructive comments of the three anonymous reviewers, which greatly improved the manuscript.	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APR	2020	99								102523	10.1016/j.jsames.2020.102523	http://dx.doi.org/10.1016/j.jsames.2020.102523			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6BC					2023-06-23	WOS:000528182600014
J	da Silva, CM; Arbilla, G; Machado, W; Soares, R				da Silva, Cleyton Martins; Arbilla, Graciela; Machado, Wilson; Soares, Ricardo			RADIONUCLIDES AS MARKERS OF A NEW TIME: THE ANTHROPOCENE	QUIMICA NOVA			Portuguese	Article						Anthropocene; The Great Acceleration; nuclear fallout; Cs-137; Chernobyl	STRATOTYPE SECTION; WORKING GROUP; ICE-CORE; SEDIMENTS; CS-137; GEOCHRONOLOGY; MARINE; BAY; DEFINITION; SIGNATURES	On May 2019, the members of the Anthropocene Working Group completed a binding vote to affirm some of the key questions that have been agreed in 2016: the Anthropocene should be considered as a formal chronostratigraphic unit, defined by a Global Boundary Stratotype Section and Point (GSSP), using one of the stratigraphic signals around the mid-twentieth century of the Common Era. The fallout from nuclear weapons testing appears as the most suitable GSSP. In this article, the main anthropogenic markers are discussed as well as the sources or human-made radiation and the signature of nuclear weapons testing. The appearance of Pu239+240 in the early 1950s and the clear peak, in 1963, makes a good marker. High resolution archives include layers of sedimentary rocks, lacustrine and marine sediments and corals and polar ice cores. A coupled application of other radioactive isotopes, as Cs-137, C-14 and Am-241, may be useful to categorize distinct fallout signatures. A site to define the Anthropocene (golden spike) would ideally be located between 30 degrees and 60 degrees north of the equator. Nevertheless, results obtained in sediments on the Brazilian coast showed that both Pu239+240 and Cs-137 signatures could be detected and quantified as markers of this "atomic age".	[da Silva, Cleyton Martins; Arbilla, Graciela] Univ Fed Rio de Janeiro, Inst Quim, Dept Fis Quim, BR-21941909 Rio De Janeiro, RJ, Brazil; [da Silva, Cleyton Martins] Univ Veiga Almeida, Campus Maracana, BR-20271020 Rio De Janeiro, RJ, Brazil; [Machado, Wilson; Soares, Ricardo] Univ Fed Fluminense, Dept Geoquim, Inst Quim, Outeiro Sao Joao Batista S-N, BR-24020141 Niteroi, RJ, Brazil; [Soares, Ricardo] Inst Estadual Ambiente, Ave Venezuela 110, BR-20081312 Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio de Janeiro; Universidade Veiga de Almeida (UVA); Universidade Federal Fluminense	Arbilla, G (autor correspondente), Univ Fed Rio de Janeiro, Inst Quim, Dept Fis Quim, BR-21941909 Rio De Janeiro, RJ, Brazil.	gracielaiq@gmail.com	da Silva, Cleyton Martins/AAC-4993-2020; Arbilla, Graciela/X-5847-2019; Machado, Wilson/P-8047-2019; Soares, Ricardo/AAM-7896-2021	da Silva, Cleyton Martins/0000-0002-5216-4977; Arbilla, Graciela/0000-0001-7732-8336; Machado, Wilson/0000-0003-3117-8584; 				Afonso JC, 2018, REV VIRTUAL QUIM, V10, P1849, DOI 10.21577/1984-6835.20180121; Bauska TK, 2015, NAT GEOSCI, V8, P383, DOI [10.1038/NGEO2422, 10.1038/ngeo2422]; Browne MA, 2011, ENVIRON SCI TECHNOL, V45, P9175, DOI 10.1021/es201811s; Corcoran P.L., 2014, GEOLSOCAMTODAY, V24, P4, DOI DOI 10.1130/GSAT-G198A.1; Crutzen E., 2006, EARTH SYSTEM SCI ANT, P13, DOI [DOI 10.1007/3-540-26590-2_3, 10.1007/3-540-26590-2]; Cunha IIL, 1999, J RADIOANAL NUCL CH, V239, P477, DOI 10.1007/BF02349054; Davies J., 2016, BIRTH ANTHROPOCENE; Ferreira PAD, 2016, ANTHROPOCENE, V14, P34, DOI 10.1016/j.ancene.2016.06.002; Ferreira PAD, 2013, SCI TOTAL ENVIRON, V443, P505, DOI 10.1016/j.scitotenv.2012.11.032; Druffel ERM, 1996, RADIOCARBON, V38, P563, DOI 10.1017/S0033822200030095; Ellis E., 2018, ANTHROPOCENE VERY SH, DOI 10.1093/ACTRADE/9780198792987.001.0001; Figueira RCL, 2006, SCI TOTAL ENVIRON, V357, P146, DOI 10.1016/j.scitotenv.2005.03.032; Figueira Rubens C. 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M., 2018, REV VIRTUAL QUIM, V10, P1648; Soares R, 2018, REV VIRTUAL QUIM, V10, P1693, DOI 10.21577/1984-6835.20180114; Soares R, 2018, REV VIRTUAL QUIM, V10, P1659, DOI 10.21577/1984-6835.20180113; Steffen W, 2015, ANTHROPOCENE REV, V2, P81, DOI 10.1177/2053019614564785; Steffen W, 2015, SCIENCE, V347, DOI 10.1126/science.1259855; Veiga J. E. da, 2019, ANTROPOCENO CIENCIA, V34; Walker MJC, 2012, J QUATERNARY SCI, V27, P649, DOI 10.1002/jqs.2565; Walker M, 2009, J QUATERNARY SCI, V24, P3, DOI 10.1002/jqs.1227; Waters C.N., 2016, SCIENCE, P6269; Waters CN, 2015, B ATOM SCI, V71, P46, DOI 10.1177/0096340215581357; Wendel CC, 2013, SCI TOTAL ENVIRON, V461, P734, DOI 10.1016/j.scitotenv.2013.05.054; Zalasiewicz J, 2017, ANTHROPOCENE, V19, P55, DOI 10.1016/j.ancene.2017.09.001; Zalasiewicz J, 2015, QUATERN INT, V383, P196, DOI 10.1016/j.quaint.2014.11.045	62	8	10	3	27	SOC BRASILEIRA QUIMICA	SAO PAULO	CAIXA POSTAL 26037, 05599-970 SAO PAULO, BRAZIL	0100-4042	1678-7064		QUIM NOVA	Quim. Nova	APR	2020	43	4					506	514		10.21577/0100-4042.20170503	http://dx.doi.org/10.21577/0100-4042.20170503			9	Chemistry, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	LY7LF		gold, Green Published			2023-06-23	WOS:000540708100016
J	Nascimento, JSD; Oliveira, EV; da Silva, JLL				de Oliveira Nascimento, Johnson Sarmento; Oliveira, Edison Vicente; Lopes da Silva, Jorge Luiz			Taxonomy and paleoenvironmental inferences from fossil vertebrates of Paripiranga Borboletas Cave, Northeastern Bahia, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Mammalia; Megafauna; Quaternary; South America; Underground cavities	CAT SMILODON-POPULATOR; BUENOS-AIRES PROVINCE; LATE PLEISTOCENE; QUATERNARY MAMMALS; PAMPEAN REGION; SOUTH; MACHAIRODONTINAE; NOTOUNGULATA; ARGENTINA; EXTINCT	The fossil mammals that lived in the Brazilian Intertropical Region during the Quaternary are found in different types of deposits (e.g. natural tanks, ponds, caves, rockshelter, and riverbeds) throughout the Brazilian territory. The state of Bahia, located on northeastern Brazil, stands out for the presence of large and important caves, which are characterized by the natural deposition of sediments and fossils. The study aims to identify the fauna found in the Borboletas Cave, and to provide the first paleoecological inferences for the environment during the Late Pleistocene-Holocene. Here we present the first record of Palaeolama major, Hippidion principale and Smilodon populator in Paripiranga, Bahia. Coendou sp., Mazama gouazoubira, and Toxodon platensis, already known to the region, were also collected and identified. Based on the chronological and geographical distribution of the taxa, it is suggested that the faunal content found lived during the Late Pleistocene - Holocene. The presence of the taxa found indicate an open paleoenvironment, similar to savanna, with areas covered with grasses associated with areas with forest cover. This study demonstrates that the Borboletas Cave is the richest paleontological site carrying the mammals in this region.	[de Oliveira Nascimento, Johnson Sarmento; Oliveira, Edison Vicente] Univ Fed Pernambuco, Ctr Tecnol & Geociencias, Dept Geol, Recife, PE, Brazil; [Lopes da Silva, Jorge Luiz] Univ Fed Alagoas, Museu Hist Nat, Setor Paleontol, Penedo, AL, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Alagoas	Nascimento, JSD (autor correspondente), Univ Fed Pernambuco, Ctr Tecnol & Geociencias, Dept Geol, Recife, PE, Brazil.	bio.johnsonson@gmail.com; vicenteedi@gmail.com; jluizlopess@gmail.com	Oliveira, Édison Vicente/A-8427-2011	Oliveira, Edison/0000-0001-6634-5480; Sarmento de Oliveira Nascimento, Johnson/0000-0003-1457-4761	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior CAPES	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors express their gratitude to the Grupo Mundo Subterraneo de Espeleologia - Paripiranga, Bahia, for the logistic support during the campaigns. We also would like to thanks Fernando Andrade, for the partnership and communication. To the employees of the Setor de Geologia e Paleontologia of the Museu de Historia Natural of Universidade Federal de Alagoas due to their help with the campaing. Our gratitude to the professor from PUC MINAS Castor Cartelle due to his important aid in the identification of some of the specimens; Best regards to the team of the Laboratorio de Paleontologia of Universidade Federal de Pernambuco -PALEO-LAB/UFPE for their support and provision of relevant bibliography. This study was funded by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior CAPES.	Alberdi M. 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South Am. Earth Sci.	APR	2020	99								102491	10.1016/j.jsames.2019.102491	http://dx.doi.org/10.1016/j.jsames.2019.102491			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6BC					2023-06-23	WOS:000528182600033
J	de Sousa, AAC; Sousa, ES; Rocha, MS; Sousa, GR; de Souza, IVAF; Brito, AS; Souza, AA; Lopes, JAD; Nogueira, ACR; de Lima, SG				de Sousa, Alek A. C.; Sousa, Edymilais S.; Rocha, Marcio S.; Sousa Junior, Gustavo R.; de Souza, Igor V. A. F.; Brito, Ailton S.; Souza, Alexandre A.; Lopes, Jose A. D.; Nogueira, Afonso C. R.; de Lima, Sidney G.			Aliphatic and aromatic biomarkers of the Devonian source rocks from the Western Parnaiba Basin Brazil: Pimenteiras Formation	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Parnaiba basin; Pimenteiras formation; Devonian; Biomarkers; C-30 steranes; Aromatic carotenoids	PHOTIC-ZONE EUXINIA; PURPLE SULFUR BACTERIA; ORGANIC-MATTER; CRUDE OILS; MOLECULAR INDICATORS; CAROTENOID DERIVATIVES; BIOLOGICAL MARKERS; ARYL ISOPRENOIDS; BLACK SHALE; SEDIMENTS	Previous geochemical studies carried out in the Parnaiba Basin (Brazil) show that natural gas deposits, whose source rock is formed by the shales of the Pimenteiras Formation (PF; Devonian), stimulated new research to understand the petroleum system. Despite previous studies of PF, ifs characterization with emphasis on the biomarker content is still incipient. In this work, the organic matter (OM) of outcrop samples of the Pimenteiras Formation outcrop samples was investigated through diagnostic biomarkers, to evaluate paleoenvironmental conditions of deposition, the thermal evolution, and the organic matter type. The general distribution of hydrocarbons suggested that the samples present low thermal evolution, marine depositional paleoenvironment, and dysoxic conditions. The molecular parameters based on steranes, hopanes, Pr/C-17 and Ph/C-18, presence of nC(25), n-C-27 and n-C-29 n-alkanes showed strong evidence of marine origin OM with higher plant input. The data also suggested that OM was not affected by igneous intrusions, being below the oil window. Also, the isomers 4 alpha(methyl)- and 4 beta(methyl)-24-ethylcholestane and 24-n-propylcholestane have been detected, which are indicative of a marine depositional system. Aromatic carotenoids and derivatives suggest that euxinic conditions have reached the photic zone, an environment conducive to the preservation of organic matter.	[de Sousa, Alek A. C.; Sousa, Edymilais S.; Rocha, Marcio S.; Souza, Alexandre A.; Lopes, Jose A. D.; de Lima, Sidney G.] Univ Fed Piaui, Dept Quim, Lab Geoquim Organ, Campus Minist Petronio Portela, BR-64049550 Teresina, PI, Brazil; [Sousa Junior, Gustavo R.] Univ Estadual Campinas, Inst Quim, BR-13083970 Campinas, SP, Brazil; [de Souza, Igor V. A. F.] Petrobras SA, CENPES, PDEP, GEOQ, Av Horacio Macedo 950,Cidade Univ Ilha Fundao, BR-21941915 Rio De Janeiro, RJ, Brazil; [Brito, Ailton S.; Nogueira, Afonso C. R.] Univ Fed Para, Inst Geosciencias, BR-66075900 Belem, Para, Brazil	Universidade Federal do Piaui; Universidade Estadual de Campinas; Petrobras; Universidade Federal do Para	de Lima, SG (autor correspondente), Univ Fed Piaui, Dept Quim, Lab Geoquim Organ, Campus Minist Petronio Portela, BR-64049550 Teresina, PI, Brazil.	sidney@ufpi.edu.br	ROCHA, MARCIO DOS SANTOS/AAZ-6825-2021; Sousa, Gustavo R./AAD-6435-2020; de Souza, Alexandre Araujo/B-1420-2015; de Lima, Sidney Gonçalo/J-5555-2019; de Sousa, Alek/R-3209-2017	Sousa, Gustavo R./0000-0002-9070-3775; de Souza, Alexandre Araujo/0000-0002-7896-6521; de Lima, Sidney Gonçalo/0000-0001-8754-1499; NOGUEIRA, AFONSO/0000-0002-5225-9255; Brito, Ailton/0000-0001-9224-5563; Rocha, Marcio dos Santos/0000-0001-6606-8268; de Sousa, Alek/0000-0003-2394-5544	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); Petroleo Brasileiro S.A. (PETROBRAS); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Universidade Federal do Piaui (UFPI)	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Petroleo Brasileiro S.A. (PETROBRAS)(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Universidade Federal do Piaui (UFPI)	The authors thank Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), Petroleo Brasileiro S.A. (PETROBRAS), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), and Universidade Federal do Piaui (UFPI) for financial support, Prof. Dr. Daniel M. Jarvie and an anonymous reviewer for thoughtful suggestions and corrections.	Aderoju T, 2018, ORG GEOCHEM, V119, P91, DOI 10.1016/j.orggeochem.2018.03.003; Almeida F. F. 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J	Dias, EV; Dias-Da-Silva, S; Schultz, CL				Dias, Eliseu Vieira; Dias-Da-Silva, Sergio; Schultz, Cesar Leandro			A NEW SHORT-SNOUTED RHINESUCHID FROM THE PERMIAN OF SOUTHERN BRAZIL	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						Rhinesuchidae; Temnospondyli; Rastosuchus; Guadalupian-Lopingian; Rio do Rasto Formation	FORMATION PARANA BASIN; TEMNOSPONDYL AUSTRALERPETON-COSGRIFFI; RASTO FORMATION; ARCHEGOSAURUS-DECHENI; PHYLOGENETIC ANALYSIS; KAROO BASIN; 1ST RECORD; U-PB; RIO; STEREOSPONDYLI	A new basal stereospondyl taxon from the Permian is described. The material used to erect the new taxon consists of a series of mandibles and some posteranial elements. A single badly preserved short-snouted skull is considered as referred material. Rastosuchus hammeri gen. et sp. nov. presents conical teeth along all coronoid bones, the prearticular extending anteriorly at the level of the precoronoid and enlarged anterior meckelian foramina. Based on the referred material, R. hammeri gen. et sp. nov. also presents posterior premaxillary teeth larger than anterior ones, the cultriform process of the parasphenoid compressed laterally forming a medial ventral keel, posterolateral ramus of the vomer extends posterior to the palatine tusks, and rounded orbit with flat orbital bones at the same level of the skull roof, features shared with Australerpeton cosgriffi and other rhinesuchids. Australerpeton cosgriffi and Rastosuchus hammeri gen. et sp. nov. are from the upper layers of the Rio do Rasto Formation (Parana Basin) in the Parana State, southern Brazil, and its deposition in freshwater continental environments is reinforced by the presence of temnospodyls amphibians.	[Dias, Eliseu Vieira] Univ Estadual Oeste Parana, Ctr Ciencias Biol & Saude, Rua Univ 2069, BR-85819110 Cascavel, PR, Brazil; [Dias-Da-Silva, Sergio] Univ Fed Santa Maria, Dept Ecol & Evolucao, Av Roraima 1000,Predio 17,Sala 1140-1, BR-97105900 Santa Maria, RS, Brazil; [Schultz, Cesar Leandro] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil	Universidade Estadual do Oeste do Parana; Universidade Federal de Santa Maria (UFSM); Universidade Federal do Rio Grande do Sul	Dias, EV (autor correspondente), Univ Estadual Oeste Parana, Ctr Ciencias Biol & Saude, Rua Univ 2069, BR-85819110 Cascavel, PR, Brazil.	eliseu.dias@unioeste.br; paleosp@gmail.com; cesar.schultz@ufrgs.br		Dias-da-Silva, Sergio/0000-0002-1262-0528	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [CNPq 150469/2003-9, CNPq 307711/2017-0, CNPq 308223/2019-5]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors dedicate this work to M. C. Barberena dagger who organized the expeditions to collect and started the study of temnospondyls in the Parana Basin. We also thank some of the field trip members U. Faccini, E. Lavina, S.A.K. Azevedo and V. Costa dagger, the late for the careful preparation of the specimens. We also thank E. Latimer, R. Damiani and C. Marsicano for gently sending us drawings, photos and for discussion regarding South African material. E.V. Dias and C.L. Schultz make a special reference to T. Kroeff for his first attempt to describe the mandibular materials of Rastosuchus gen. nov., G.S. Sipp for the CT-Scan images treatment and interpretation, and M. I. Preza for help on the map drawing. We would like to thank the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico for the financial support: EVD (CNPq 150469/2003-9), CLS (CNPq 307711/2017-0) and SDS (CNPq 308223/2019-5).	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APR-JUN	2020	23	2					98	122		10.4072/rbp.2020.2.03	http://dx.doi.org/10.4072/rbp.2020.2.03			25	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	MO4RG		Green Published			2023-06-23	WOS:000551514700003
J	Dillenburg, SR; Hesp, PA; Keane, R; da Silva, GM; Sawakuchi, AO; Moffat, I; Barboza, EG; Bitencourt, VJB				Dillenburg, Sergio R.; Hesp, Patrick A.; Keane, Robert; da Silva, Graziela Miot; Sawakuchi, Andre O.; Moffat, Ian; Barboza, Eduardo G.; Bitencourt, Volney J. B.			Geochronology and evolution of a complex barrier, Younghusband Peninsula, South Australia	GEOMORPHOLOGY			English	Article						Foredune ridges; Barrier progradation; The Granites; OSL dating	GROUND-PENETRATING RADAR; LEVEL RISE INSIGHTS; FOREDUNE DEVELOPMENT; PROGRADED BARRIER; SAND BARRIERS; ISLAND SYSTEM; DUNE SEQUENCE; BEACH; MORPHOLOGY; WALES	This study examines the southeastern end of the Younghusband Peninsula in South Australia at a location called The Granites in order to gain a better understanding of the processes of formation of the foredune ridge system, and to investigate the drivers that controlled its progradational development during the Holocene. Our findings are based on amorphological analysis, a ground penetrating radar survey, and C-14 and OSL dating. The Younghusband Peninsula at The Granites was formed by an initial aggradational phase resulting in a single complex foredune ridge, and which ended around 4.3 ka, and by a regressive (progradational) barrier phase (750 m wide) that developed in the last 4.3 ka, under very low rates of progradation (0.38 to 0.09 m/yr). The last part of this phase shows significant foredune ridge building in the last 1000 years or so. Barrier progradation via foredune ridge development is likely an effect driven by lowwave energy that favored conditions for coastal stability and foredune formation. Paleontological and GPR data indicate a maximum sea-level of +1.23 to +1.5 m, respectively, during initial barrier development. The foredune ridge plain of the barrier experienced at least three phases of significant aeolian activitywith ages centered at around 3.9, 3.4 and 3.0 ka suggesting their occurrence at 500 to 400-year events. Computer modelling indicates that sediments for the progradational phase of the barrier were provided by the forced regression produced by a sea-level fall over the past 4.3 ka. The large foredune complex formed during the last phase of progradation could be the result of both the very low progradation rate of 0.09 m/yr, and periods of disturbance possibly related to enhanced storm activity. (C) 2020 Elsevier B.V. All rights reserved.	[Dillenburg, Sergio R.; Barboza, Eduardo G.] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, Inst Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil; [Hesp, Patrick A.; Keane, Robert; da Silva, Graziela Miot] Flinders Univ S Australia, Coll Sci & Engn, Beach & Dune Syst Beads Lab, Sturt Rd, Bedford Pk, SA 5041, Australia; [Sawakuchi, Andre O.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Moffat, Ian] Flinders Univ S Australia, Coll Humanities & Social Sci, Archaeol, Sturt Rd, Bedford Pk, SA 5041, Australia; [Dillenburg, Sergio R.; Barboza, Eduardo G.; Bitencourt, Volney J. B.] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Flinders University South Australia; Universidade de Sao Paulo; Flinders University South Australia; Universidade Federal do Rio Grande do Sul	Dillenburg, SR (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil.	sergio.dillenburg@ufrgs.br	Barboza, Eduardo Guimarães/C-7579-2012; de Bitencourt, Volney Junior Borges/AAD-9618-2019; Sawakuchi, André O/D-1445-2013; Dillenburg, Sergio/C-4027-2013; Miot da Silva, Graziela/I-1551-2015; Hesp, Patrick/I-3403-2013	Barboza, Eduardo Guimarães/0000-0003-2107-6904; de Bitencourt, Volney Junior Borges/0000-0002-1004-5179; Dillenburg, Sergio/0000-0003-0072-7018; Miot da Silva, Graziela/0000-0003-1190-8076; Sawakuchi, Andre/0000-0001-5016-2428; Moffat, Ian/0000-0002-2171-7145; Hesp, Patrick/0000-0003-4573-2945	CAPES/Brasil [BEX 5287/14-6]; Flinders University College of Science and Engineering; CNPq/Brasil; BEADS Lab	CAPES/Brasil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Flinders University College of Science and Engineering; CNPq/Brasil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); BEADS Lab	We thank CAPES/Brasil funding to S. Dillenburg for a visiting sabbatical Fellowship at Flinders University (grant no BEX 5287/14-6) and Flinders University College of Science and Engineering for support. S. Dillenburg, E. Barboza and A. Sawakuchi also thank CNPq/Brasil for the provision of their research fellowships. P. Hesp. G. Miot da Silva, I. Moffat and R. Keane thank the BEADS Lab and Flinders University College of Science and Engineering for support.	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J	Albuquerque, MFD; Horbe, AMC; Soares, TM; Sousa, EMD; Iza, ERHD				dos Santos Albuquerque, Marcio Fernando; Coimbra Horbe, Adriana Maria; Soares, Tulio Marques; Dalat Sousa, Endel Muller; Herrera de Figueiredo Iza, Edgar Romeo			Airborne radiometric data for identifying lateritic surfaces in southwestern Amazonia, Brazil	JOURNAL OF APPLIED GEOPHYSICS			English	Article						Gamma-ray spectrometry; Altimetry; Boolean; Fuzzy; Regolith	GAMMA-RAY SPECTROMETRY; GEOCHEMISTRY; MINERALOGY; EVOLUTION; REGOLITH; (U-TH)/HE; AGREEMENT; 40AR/39AR; DEPOSITS; GEOLOGY	Airborne gamma-ray spectrometry and altimetric data have been used to recognize lateritic surfaces in southwestern Amazonia, Brazil. Three altimetric surfaces, marked by three main types of lateritic duricrust, comprise the landscape of the studied area. Surface 1 (SP1 <= 134 m a.s.l.) is dominated by a deep dissecting U-shaped valley, lowlands, steep slopes, and hills gathering Mn to Mn-Al-Fe duricrusts. Surface 2 (SP2-134 to 186 m a.s.l.) has rounded hills supported by Fe and Fe-Al duricrusts. Surface 3 (5P3-186 to 290 m a.s.l.) consists of strongly dissected plateaus to rounded hills sustained by bauxites, massive Fe duricrust, rare Mn-Al-Fe duricrusts, and Mn colluviums. Specifically, all lateritic duricrusts are associated with high values of eTh, and these data were employed in conjunction with SRTM data for generating favorability maps for lateritic surfaces using Boolean and fuzzy techniques. Altimetric data is an important input data in the boolean and fuzzy models since the boolean model overestimated the lateritic surfaces in surface 1, while not considering regional stratigraphic stacking when gathering ironstones as lateritic duricrust (lateritic duricrusts are older than ironstones). Both boolean and fuzzy models successfully recognized the lateritic duricrusts in surfaces 2 and 3 (134-290 m a.s.l.), even though the fuzzy product overestimated the lateritic surfaces above 134 m a.s.l. A lateritic index (LI - (eTh/eU) x K (eTh x eU)) was also applied as complementary method in relation to the fuzzy and boolean models. U divided the studied area into three main domains according to weathering intensity (lowest LI, low to intermediate LI, and high to extremely high U associated with duricrust). Although the U does not consider the altitude, the obtained model describes areas favorable for lateritic surface occurrences, being a useful and rapid method for preliminary large-scale mapping of lateritic surfaces. Mn duricrusts with K-bearing minerals were also identified by the intersection between F-factor (F=K x (eU/eTh)) and eTh fuzzy membership maps. Nevertheless, geological control is important, since protolith influences the F-factor responses. The combination among the eTh fuzzy membership map, ternary map of K, eTh and eU on the RGB channels, the geological and soil map database and some chemical analysis allowed improving future research on supergene deposits as bauxite and manganese duricrusts, phosphorous and gold-sulphides. (C) 2020 Elsevier B.V. All rights reserved. Airborne gamma-ray spectrometry and altimetric data have been used to recognize lateritic surfaces in southwestern Amazonia, Brazil. Three altimetric surfaces, marked by three main types of lateritic duricrust, comprise the landscape of the studied area. Surface 1 (SP1 <= 134 m a.s.l.) is dominated by a deep dissecting U-shaped valley, lowlands, steep slopes, and hills gathering Mn to Mn-Al-Fe duricrusts. Surface 2 (SP2-134 to 186 m a.s.l.) has rounded hills supported by Fe and Fe-Al duricrusts. Surface 3 (5P3-186 to 290 m a.s.l.) consists of strongly dissected plateaus to rounded hills sustained by bauxites, massive Fe duricrust, rare Mn-Al-Fe duricrusts, and Mn colluviums. Specifically, all lateritic duricrusts are associated with high values of eTh, and these data were employed in conjunction with SRTM data for generating favorability maps for lateritic surfaces using Boolean and fuzzy techniques. Altimetric data is an important input data in the boolean and fuzzy models since the boolean model overestimated the lateritic surfaces in surface 1, while not considering regional stratigraphic stacking when gathering ironstones as lateritic duricrust (lateritic duricrusts are older than ironstones). Both boolean and fuzzy models successfully recognized the lateritic duricrusts in surfaces 2 and 3 (134-290 m a.s.l.), even though the fuzzy product overestimated the lateritic surfaces above 134 m a.s.l. A lateritic index (LI - (eTh/eU) x K (eTh x eU)) was also applied as complementary method in relation to the fuzzy and boolean models. U divided the studied area into three main domains according to weathering intensity (lowest LI, low to intermediate LI, and high to extremely high U associated with duricrust). Although the U does not consider the altitude, the obtained model describes areas favorable for lateritic surface occurrences, being a useful and rapid method for preliminary large-scale mapping of lateritic surfaces. Mn duricrusts with K-bearing minerals were also identified by the intersection between F-factor (F=K x (eU/eTh)) and eTh fuzzy membership maps. Nevertheless, geological control is important, since protolith influences the F-factor responses. The combination among the eTh fuzzy membership map, ternary map of K, eTh and eU on the RGB channels, the geological and soil map database and some chemical analysis allowed improving future research on supergene deposits as bauxite and manganese duricrusts, phosphorous and gold-sulphides. (C) 2020 Elsevier B.V. All rights reserved.	[dos Santos Albuquerque, Marcio Fernando; Soares, Tulio Marques; Dalat Sousa, Endel Muller; Herrera de Figueiredo Iza, Edgar Romeo] Brasilia Univ, Geosci Inst, Grad Program Geol, Darcy Ribeiro Univ Campus, BR-70910900 Brasilia, DF, Brazil; [Coimbra Horbe, Adriana Maria] Brasilia Univ, Geosci Inst, Darcy Ribeiro Univ Campus, BR-70910900 Brasilia, DF, Brazil; [Herrera de Figueiredo Iza, Edgar Romeo] CPRM Brazilian Geol Survey, Av Ulysses Guimaraes 2862, BR-41213000 Salvador, BA, Brazil	Universidade de Brasilia; Universidade de Brasilia	Albuquerque, MFD (autor correspondente), Brasilia Univ, Geosci Inst, Grad Program Geol, Darcy Ribeiro Univ Campus, BR-70910900 Brasilia, DF, Brazil.	malbuquerquegeo@gmail.com		Dalat de Sousa, Endel Muller/0000-0002-9035-9118; Marques Soares, Tulio/0000-0003-1838-7410	Graduate Program in Geology from the University of Brasilia, CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior); CNPq (ConselhoNacional de Desenvolvimento Cientifico e Tecnologico) [471971/2010-3, 473359/2012, 302618/2016-3]	Graduate Program in Geology from the University of Brasilia, CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior); CNPq (ConselhoNacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the Graduate Program in Geology from the University of Brasilia, CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) for granting a Ph.D. scholarship to the first author and CNPq (ConselhoNacional de Desenvolvimento Cientifico e Tecnologico) for the financial support (process no 471971/2010-3 and 473359/2012) and research grants for the second (process no 302618/2016-3) author.	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Appl. Geophys.	APR	2020	175								103989	10.1016/j.jappgeo.2020.103989	http://dx.doi.org/10.1016/j.jappgeo.2020.103989			16	Geosciences, Multidisciplinary; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mining & Mineral Processing	LF3FP					2023-06-23	WOS:000527307000012
J	Duarte, SK; Hartmann, LA; Baggio, SB				Duarte, Sandro Kucera; Hartmann, Leo Afraneo; Baggio, Sergio Benjamin			Fluidized sand effusion over successive basalt flows of the northwestern Parana volcanic province	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Sand injectites complex; Parana volcanic province; Mato Grosso do Sul; Maracaju cuesta; Novo Hamburgo Complex	SOUTHERN BRAZIL; STRATIGRAPHY; LAVAS; SERRA; GEOCHEMISTRY; INJECTITES; BASIN; REMOBILIZATION; INTRUSIONS; DISTRICTS	A remarkable sand injectite complex (1 million km(2)) is hosted in Parana volcanic province, South America, and is here described. Named Novo Hamburgo Complex, these sand injectites originated by the interaction of several major geological processes, as presently described in Campo Grande and Serra de Maracaju cuesta, Mato Grosso do Sul, Brazil. The geologically unique relationship of a major continental flood basalt province with the underlying large freshwater Guarani aquifer - hosted in paleodune sands of the largest known paleoerg - resulted in a network of sand injectites where each basalt lava flow was injected and then covered by sand extrudite. The basaltic lavas were individualized by chemical characteristics and correlated (with cover extrudite) along the escarpment of the cuesta for 10-30 km. After cooling, each volcanic unit underwent prolonged hydrothermal alteration. Porosity vanished by sealing with chalcedony during continued percolation of hot water. The process culminated in the explosive injection and effusion of fluidized sand, resulting in the covering of each lava flow with a sand extrudite. Lavas were sealed in sequence above the underlying aquifer, resulting in the explosive injection and effusion of fluidized sand. The interplay of three major geological features was required in the Cretaceous Parana Basin to build the geology of Serra de Maracaju and Novo Hamburgo Complex: (1) a huge continental flood basalt province, (2) a huge underlying paleoerg, and (3) a large, underlying Guarani aquifer. An infinite volume of hot water and its vapor was available for the alteration, injection, and effusion processes of sand extrudites. Injection was triggered by residual volcanic heat and possibly earthquakes.	[Duarte, Sandro Kucera; Hartmann, Leo Afraneo; Baggio, Sergio Benjamin] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-95009150 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Hartmann, LA (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-95009150 Porto Alegre, RS, Brazil.	leo.hartmann@ufrgs.br	Hartmann, Léo A/D-7663-2013	Hartmann, Léo A/0000-0001-7863-5071	PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil) [10/0021-8]	PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil)	We thank Romualdo H. P. Andrade and staff of Campo Grande office of `Departamento Nacional da Producao Mineral, Ministerio de Minas e Energia, Governo do Brasil' for field support. We also acknowledge field support by Daniel B. Knijnik, Gilmar J. Rizzotto and Goiania office of CPRM (Geological Survey of Brazil). Financial support was provided by a project of excellence (grant number 10/0021-8 PRONEX-Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul/Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (Brazil) on strategic minerals from southern Brazil, coordinated by Leo A. Hartmann. Two journal reviewers made significant contributions to the improvement of the article.	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South Am. Earth Sci.	APR	2020	99								102505	10.1016/j.jsames.2020.102505	http://dx.doi.org/10.1016/j.jsames.2020.102505			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6BC					2023-06-23	WOS:000528182600010
J	Lobo, MTMPS; Scalize, PS; Kraus, CN; da Silva, WJ; Garnier, J; Marques, DD; Bonnet, MP; Nogueira, ID				Lobo, Maria Tereza Morais Pereira Souza; Scalize, Paulo Sergio; Kraus, Cleber Nunes; da Silva, Weliton Jose; Garnier, Jeremie; da Motta Marques, David; Bonnet, Marie-Paule; de Souza Nogueira, Ina			Biological index based on epiphytic diatom assemblages is more restrictive than the physicochemical index in water assessment on an Amazon floodplain, Brazil	ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH			English	Article						Canadian Council of Ministers of the Environment Water Quality Index; Water classes; Biological Diatom Index; Ecological status; Water Framework Directive	CYANOBACTERIAL TOXINS; QUALITY ASSESSMENT; LAGO GRANDE; FOOD WEBS; LAND-USE; RIVER; PHYTOPLANKTON; CONSERVATION; REDUNDANCY; HYPOXIA	Canadian Water Quality Index (CWQI) provides protection for freshwater life promoting healthy ecosystems and safeguarding human health. Biological Diatom Index (BDI) was developed to indicate the ecological status and water quality of freshwater systems. This paper evaluates the relations between the two different indices. During rising and falling, water samples were taken in the Curuai Floodplain, Brazil. CWQI was calculated using 14 physicochemical parameters and 1 microbiological parameter. The limits were established according to freshwater quality conditions and standards based on water use classes 1 and 2 determined in CONAMA 357 legislation and British Columbia. Canadian Water Quality Index categorization ranged from "marginal" to "excellent," most sampling units were "good" (71%), followed by "fair" (12%) and "excellent" (12%) water quality. Total phosphorus (38 times), chlorophyll a (20), dissolved oxygen (10), and total organic carbon (10) were the parameters that presented the most non-compliance values. Encyonema silesiacum (14%), Gomphonema parvulum (13%), and Navicula cryptotenella (12%) were the main taxa in the rising period, while G. lagenula, E. silesiacum, and Fragilaria capucina were the main taxa during the falling period. BDI ranges from I to V water quality classes. We observed "poor" to "very good" ecological status, with most sampling units "moderate" (52%) and "good" (29%). Water quality for class 2 was better than water quality for class 1, as the limits of the parameters evaluated were more restrictive in class 1 than in class 2 and the predominant uses of water require a higher degree of water purity. The biological index based on diatoms was the most restrictive index whose water classes and categorizations have shown an ecological status that could threaten the protection of aquatic communities on the Curuai floodplain. We suggest the combined use of both indices-physicochemical and biological for water quality assessment in this type of environment.	[Lobo, Maria Tereza Morais Pereira Souza; Scalize, Paulo Sergio; de Souza Nogueira, Ina] Univ Fed Goias, Programa Posgrad Ciencias Ambientais, Goiania 74690900, Go, Brazil; [Lobo, Maria Tereza Morais Pereira Souza; de Souza Nogueira, Ina] Univ Fed Goias, Lab Anal & Gerenciamento Ambiental Recursos Hidri, Campus Samambaia,Alameda Palmeiras,Quadra 1, Goiania 74690900, Go, Brazil; [Scalize, Paulo Sergio] Escola Engn Civil & Ambiental, Goiania 74605220, Go, Brazil; [Kraus, Cleber Nunes] Univ Brasilia, Programa Posgrad Ciencias Ambientais, Planaltina 73340710, DF, Brazil; [da Silva, Weliton Jose] Univ Estadual Londrina, Dept Biol Anim & Vegetal, Londrina 86057970, PR, Brazil; [Garnier, Jeremie] Univ Brasilia, Inst Geociencias, Lab Geoquim, Brasilia 70910900, DF, Brazil; [Garnier, Jeremie; Bonnet, Marie-Paule] Univ Brasilia, IRD, OCE Observ Environm Change, Joint Int Lab LMI, Brasilia 70910900, DF, Brazil; [da Motta Marques, David] Univ Fed Rio Grande do Sul, Inst Pesquisas Hidraul, Ave Bento Goncalves, Porto Alegre 91501970, RS, Brazil; [da Motta Marques, David; Bonnet, Marie-Paule] Inst Rech Dev, UMR Espace DEV, Maison Teledetect, 500 Rue JF Breton, Montpellier 34000, France; [de Souza Nogueira, Ina] Univ Fed Goias, Dept Bot, Goiania 74690900, Go, Brazil	Universidade Federal de Goias; Universidade Federal de Goias; Universidade de Brasilia; Universidade Estadual de Londrina; Universidade de Brasilia; Comissao Nacional de Energia Nuclear (CNEN); Instituto de Radioprotecao e Dosimetria; Universidade de Brasilia; Universidade Federal do Rio Grande do Sul; Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Universite des Antilles; University of La Reunion; UDICE-French Research Universities; Aix-Marseille Universite; Universidade Federal de Goias	Lobo, MTMPS (autor correspondente), Univ Fed Goias, Programa Posgrad Ciencias Ambientais, Goiania 74690900, Go, Brazil.; Lobo, MTMPS (autor correspondente), Univ Fed Goias, Lab Anal & Gerenciamento Ambiental Recursos Hidri, Campus Samambaia,Alameda Palmeiras,Quadra 1, Goiania 74690900, Go, Brazil.	mariatereza_lobo@yahoo.com.br	scalize, paulo Sérgio/ABG-6640-2020; garnier, jeremie/AAK-8470-2021; Kraus, Cleber N/M-1838-2016; Nogueira, Ina S/K-9012-2012; da Silva, Weliton José/K-2059-2012	scalize, paulo Sérgio/0000-0002-0833-7826; garnier, jeremie/0000-0001-9571-7933; Kraus, Cleber N/0000-0002-5116-3681; da Silva, Weliton José/0000-0003-2693-4648; da Motta Marques, David/0000-0002-3809-8053				Abril G, 2014, NATURE, V505, P395, DOI 10.1038/nature12797; Affonso AG, 2011, BRAZ J BIOL, V71, P601, DOI 10.1590/S1519-69842011000400004; Agencia-Nacional-de-Aguas-(Brasil)-ANA, 2012, PLAN ESTR REC HIDR A; Alves Maria Tereza Ribeiro, 2014, Acta Limnol. 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APR	2020	27	10					10642	10657		10.1007/s11356-020-07658-y	http://dx.doi.org/10.1007/s11356-020-07658-y			16	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	LJ9HG	31939021				2023-06-23	WOS:000530470700039
J	Galvao, JCM; Vieira, R; da Rosa, KK; Petsch, C; Ferreira, F; de Oliveira, AS; Simoes, JC				Medeiros Galvao, Janayna Cynthia; Vieira, Rosemary; da Rosa, Katia Kellem; Petsch, Carina; Ferreira, Fabricio; de Oliveira, Allan Sandes; Simoes, Jefferson Cardia			ANALYSIS OF SHALLOW LAKE SEDIMENTS IN THE FILDES PENINSULA, KING GEORGE ISLAND, MARITIME ANTARCTICA	REVISTA BRASILEIRA DE GEOMORFOLOGIA			English	Article						Antarctica; Chemical Weathering; Lakes; Sedimentology	SOUTH-SHETLAND-ISLANDS; LIVINGSTON-ISLAND; BYERS PENINSULA; ICE CAP; GEOCHEMISTRY; VARIABILITY; HISTORY; SOILS; PEDOGENESIS; DEPOSITION	The work analyzes the deglaciated area of Fildes Peninsula, King George Island, Maritime Antarctica, based upon the interpretation of shallow lacustrine sediment. CAMSIZE analyzer obtained the particle size distribution of sand fractions, and the silt samples were analyzed by the Malvern laser light scattering granulometer. The concentrations of major elements were determined by Energy-dispersive X-ray Spectroscopy, in <0,062 mm particle-size distribution. The mineralogical composition was determined by X-ray diffraction using the Brucker D8 Advance x-ray diffractometer. Chemical Index of Alteration and Plagioclase Index of Alteration were applied. Si was the most abundant chemical element in the samples, followed by Al, Fe, Ca, Mg, Ti and K. Chemical Index of Alteration and Plagioclase Index of Alteration indicated moderates values between 56.0-73.8, and 56.5-68.3, respectively, and increase towards the southern sector of the peninsula, early deglaciated and exposed to the weathering processes. X-ray diffraction reveals the presence of minerals belonging to the volcanic rocks: andesine and olivine. Principal Component Analysis and Cluster Analysis results suggest the sediments are related to the local basaltic rocks. It is also observed the influence of depositional processes on the granulometric and morphoscopic characteristics of the sediments. The climatic and topographic conditions play an important role in the composition and concentration of the elements in the lake sediments since moderate Chemical Index of Alteration and Plagioclase Index of Alteration are indicated.	[Medeiros Galvao, Janayna Cynthia; Vieira, Rosemary; Ferreira, Fabricio; de Oliveira, Allan Sandes] Univ Fed Fluminense, Niteroi, RJ, Brazil; [da Rosa, Katia Kellem; Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul, Porto Alegre, RS, Brazil; [Petsch, Carina] Univ Fed Santa Maria, Santa Maria, RS, Brazil	Universidade Federal Fluminense; Universidade Federal do Rio Grande do Sul; Universidade Federal de Santa Maria (UFSM)	Galvao, JCM (autor correspondente), Univ Fed Fluminense, Niteroi, RJ, Brazil.	mega.geociencias@gmail.com; rosemaryvieira@id.uff.br; katia.rosa@ufrgs.br; carinapetsch@gmail.com; ferreiraforams@gmail.com; allansandes@id.uff.br; jefferson.simoes@ufrgs.br	da Rosa, Kátia Kellem/AAO-8367-2020; Simoes, Jefferson Cardia/D-7232-2013; Ferreira, Fabricio/ABC-3867-2020	da Rosa, Kátia Kellem/0000-0003-0977-9658; Simoes, Jefferson Cardia/0000-0001-5555-3401; Ferreira, Fabricio/0000-0001-9811-4409; Vieira, Rosemary/0000-0003-0312-2890; Medeiros Galvao, Janayna Cynthia/0000-0001-9362-2543; Petsch, Carina/0000-0002-1079-0080	Brazilian National Research and Technology Council (CNPq); Brazilian National Institute for Cryospheric Sciences; Chilean staff at the Escudero Station	Brazilian National Research and Technology Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Brazilian National Institute for Cryospheric Sciences; Chilean staff at the Escudero Station	The authors thank the Brazilian National Research and Technology Council (CNPq) and Brazilian National Institute for Cryospheric Sciences for financing this research, and the Brazilian Antarctic Program for the logistics during the expedition. The authors also thank the Chilean staff at the Escudero Station during the summer of 2012/2013 for its support and, particularly, Dr. Ricardo Jana of the Antarctic Chilean Institute.	Abram NJ, 2013, NAT GEOSCI, V6, P404, DOI [10.1038/NGEO1787, 10.1038/ngeo1787]; Alfonso JA, 2015, ANTARCT SCI, V27, P462, DOI 10.1017/S0954102015000127; Ballantyne CK, 2002, QUATERNARY SCI REV, V21, P1935, DOI 10.1016/S0277-3791(02)00005-7; BENN DI, 1994, SEDIMENT GEOL, V91, P215, DOI 10.1016/0037-0738(94)90130-9; Bertrand S, 2008, CATENA, V73, P10, DOI 10.1016/j.catena.2007.08.003; Birkenmajer K., 1989, POL POLAR RES, V10, P555; BJORCK S, 1991, ANTARCT SCI, V3, P61, DOI 10.1017/S095410209100010X; Blott SJ, 2001, EARTH SURF PROC LAND, V26, P1237, DOI 10.1002/esp.261; Bockheim J, 2013, GLOBAL PLANET CHANGE, V100, P215, DOI 10.1016/j.gloplacha.2012.10.018; Braun G, 2002, MOUNTAIN BIODIVERSITY: A GLOBAL ASSESSMENT, P75; Cook AJ, 2005, SCIENCE, V308, P541, DOI 10.1126/science.1104235; COSTA J. 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Bras. Geomorfol.	APR-JUN	2020	21	2					217	234		10.20502/rbg.v21i2.1738	http://dx.doi.org/10.20502/rbg.v21i2.1738			18	Geography, Physical	Emerging Sources Citation Index (ESCI)	Physical Geography	LK5KJ		gold			2023-06-23	WOS:000530904800001
J	Moraes, AM; Sahoo, PK; Guimaraes, JTF; Leite, AS; Salomao, GN; Souza, PWM; Nascimento, W; Dall'Agnol, R				Moraes, Aline Mamede; Sahoo, Prafulla Kumar; Felix Guimaraes, Jose Tasso; Leite, Alessandro Saba; Salomao, Gabriel Negreiros; Martins Souza-Filho, Pedro Walfir; Nascimento Juniora, Wilson; Dall'Agnol, Roberto			Multivariate statistics and geochemical approaches for understanding source-sink relationship - a case study from close-basin lakes in Southeast Amazon	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Upland lakes; Sediment geochemistry; Source-sink relationship; Multivariate statistics; Provenances; Serra dos carajas	RARE-EARTH-ELEMENTS; LACUSTRINE SEDIMENTS; DOS CARAJAS; MELVILLE PENINSULA; SERRA SUL; PROVENANCE; EVOLUTION; BRAZIL; PLATEAU; SOILS	Multivariate statistical approaches were applied on geochemical data of lake sediments and the catchment basin materials (Al-enriched crusts and soils) from four upland lakes (namely LB1, LB2, LB3, and LB4) in the Serra da Bocaina, Southeast Amazon, to recognize the geochemical signatures of lake sediments and their link with source rocks. This is also compared with Fe-enriched crusts and soils, which collected from Serra Sul de Carajas. The major and trace elements were analyzed by Inductively Coupled Plasma Optical Emission Spectrometry (ICPOES) and X-ray Fluorescence (XRF), and Inductively Coupled Plasma Mass Spectrometry (ICP-MS), respectively. The data closure effect was reduced by centred log ratio (clr) transformation. The upper continental crust (UCC) normalized patterns show that sediments are mainly enriched with Ti, Fe, P, Se, V and Cr, similar to catchment basin crusts and soils. The distribution of elements varied between lakes, which is mainly influenced by the morphology and lithology of the basin. The chemical index of alternation (CIA) values were very high (> 90) for both lake sediments and catchment materials, which indicates intense source area weathering. Index of lateritization (IOL) shows that the catchment crusts are strongly lateralized and it identifies samples between extremely weathered and reworked samples that do not meet the criteria for strict in situ formation. The principal components analysis (PCA) and Spearman correlation matrices based on clr-transformed data revealed four geochemical groups in sediments. The major detritic geochemical association of sediments (Group 1: Al-Ti-Ga-Cr-V-Ti-Nb-Sc, which indicative of mafic/metavolcanic rock; and Group 2: Zr-Hf-HREEs, which refers to the heavy mineral fractions that remain stable during lateritization) had a close relationship with catchment lateritic crust, except a few alterations, which possibly influenced by weathering and transport processes. REE pattern normalized to chondrite and the geochemical ratios show the analogies between the lake sediments and the catchment lateritic crusts. The linear discriminant analysis (LD) and PCA distinguished Al-rich laterites from Ferich laterites and indicates that the former (which likely derived from mafic/metavolcanic rocks) is the main source of lake sediments.	[Moraes, Aline Mamede; Sahoo, Prafulla Kumar; Felix Guimaraes, Jose Tasso; Leite, Alessandro Saba; Salomao, Gabriel Negreiros; Martins Souza-Filho, Pedro Walfir; Nascimento Juniora, Wilson; Dall'Agnol, Roberto] Inst Tecnol Vale, Rua Boaventura da Silva 955, BR-66055090 Belem, PA, Brazil; [Sahoo, Prafulla Kumar] Cent Univ Punjab, Dept Environm Sci & Technol, Bathinda 151001, India; [Salomao, Gabriel Negreiros; Martins Souza-Filho, Pedro Walfir; Dall'Agnol, Roberto] Univ Fed Para UFPA, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa, BR-66075110 Belem, Para, Brazil; [Salomao, Gabriel Negreiros] CAGS, UNESCO Int Ctr Global Scale Geochem, Inst Geophys & Geochem Explorat, Langfang 065000, Hebei, Peoples R China	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Central University of Punjab; Universidade Federal do Para	Sahoo, PK (autor correspondente), Inst Tecnol Vale, Rua Boaventura da Silva 955, BR-66055090 Belem, PA, Brazil.	prafulla.sahoo@itv.org	Souza-Filho, Pedro Walfir M. M./J-4958-2012; Sahoo, Prafulla/N-5100-2018; Guimarães, José Tasso Felix/D-2079-2013; Souza, Pedro/GZH-1275-2022	Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; Sahoo, Prafulla/0000-0003-3481-1787; Guimarães, José Tasso Felix/0000-0002-5772-5104; Negreiros Salomao, Gabriel/0000-0003-3729-7840	Vale Institute of Technology; CNPq, Brazil [479182/2012-4, 442088/2014-0]; CNPq [306108/2014-3, 443247/2015-3, 302839/2016-0, 306450/2013-5, 380.418/2018-5]; National Forest of Carajas [SISBIO 35594-2]	Vale Institute of Technology; CNPq, Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); National Forest of Carajas	The authors are grateful to the financial support and field assistance provided by Vale Institute of Technology and CNPq, Brazil (479182/2012-4, 442088/2014-0). The authors also acknowledge CNPq [research scholarship/grants to RD (proc. 306108/2014-3; Proc. 443247/2015-3); JTFG (302839/2016-0) and PWSF (306450/2013-5); GNS (Proc. 380.418/2018-5)]. The authors thank the members of DIPF, DIST, GABAN, GELIF, LAMSF and LISF of Vale S.A. for the field support and scientific discussions. This project was carried out in the National Forest of Carajas under the permission of IBAMA (SISBIO 35594-2).	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J	Moreira, DS; Uhlein, A; Dussin, IA; Uhlein, GJ; Misuzaki, AMP				Moreira, Debora Silvano; Uhlein, Alexandre; Dussin, Ivo Antonio; Uhlein, Gabriel Jube; Pimentel Misuzaki, Ana Maria			A Cambrian age for the upper Bambui Group, Brazil, supported by the first U-Pb dating of volcaniclastic bed	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Geochronology; Petrography; Volcanic zircon; Direct dating; Glauconite	NEOPROTEROZOIC BRASILIA BELT; SAO FRANCISCO CRATON; LAGOAS CAP CARBONATE; K-BENTONITES; ISOTOPE STRATIGRAPHY; TECTONIC EVOLUTION; ZIRCON; BASIN; CONSTRAINTS; PROVENANCE	The Serra da Saudade Formation is part of the Bambui Group, a cratonic cover from the western Sao Francisco craton. It is composed by siliciclastic sediments deposited in a foreland basin during a transgressive event. The Serra da Saudade Formation is mainly represented by rhythmites, siltstones (locally glauconitic) and rare sandstones. The glauconitic siltstone was deposited during a maximum flooding surface and sediment starvation, which allowed high concentrations of probable volcanic-sourced potassium. The interpretation of the depositional age of the Bambui Group had multiple turnovers in the last decades. Finding and dating synsedimentary volcanic rocks is essential to solve this conundrum. This paper presents the first U-Pb direct dating of the Bambui Group from zircon grains recovered from a volcaniclastic layer interbedded with glauconitic siltstones from the upper Serra da Saudade Formation. A total of 107 U-Pb ages were obtained by LA-ICP-MS and plotted into a Concordia diagram. The provenance signature comprises a wide range of detrital zircon ages (1.0-2.8 Ga). These data represent inherited zircon grains incorporated into the magma during magmatic activity that produced the volcanic sediment, or to dilution and reworking of volcanic ashes that mixed to fine-grained clastic sediments prior to deposition. A significant amount of 10 highly concordant, prismatic zircon grains clustered into a well constrained age of 520.2 +/- 5.3 Ma, which represent the explosive volcanic eruption age, and by extent, the depositional age of the upper Serra da Saudade Formation. Since the currently final thrust stacking ages from the Brasilia Belt and the Aracuai Belt are dated ca. 600 and 540 Ma, respectively, one must carefully look for the real age of the deformation event that affected the Bambui Group over the Sao Francisco craton.	[Moreira, Debora Silvano] Univ Fed Minas Gerais, Inst Geociencias, Programa Posgrad Geol, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Uhlein, Alexandre; Uhlein, Gabriel Jube] Univ Fed Minas Gerais, Ctr Pesquisas Manoel Teixeira Costa, Inst Geociencias, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Dussin, Ivo Antonio] Univ Estado Rio de Janeiro, Fac Geol, Rua Sao Francisco Xavier 524,4 Andar,Bloco A, BR-20550013 Rio De Janeiro, RJ, Brazil; [Pimentel Misuzaki, Ana Maria] Univ Fed Rio Grande do Sul, Inst Geociencias, Campus Vale,Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal de Minas Gerais; Universidade Federal de Minas Gerais; Universidade do Estado do Rio de Janeiro; Universidade Federal do Rio Grande do Sul	Moreira, DS (autor correspondente), Univ Fed Minas Gerais, Inst Geociencias, Programa Posgrad Geol, Campus Pampulha,Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.	moreiradebora@yahoo.com			Fundacao de Amparo a Pesquisa do Estado de Minas Gerais (FAPEMIG CRA) [APQ-01711-14]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [447449/2014-1]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (Bolsa de Produtividade em Pesquisa, Chamada CNPq) [09/2018, 302202/2018-8]	Fundacao de Amparo a Pesquisa do Estado de Minas Gerais (FAPEMIG CRA)(Fundacao de Amparo a Pesquisa do Estado de Minas Gerais (FAPEMIG)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (Bolsa de Produtividade em Pesquisa, Chamada CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are thankful for the financial support received from Fundacao de Amparo a Pesquisa do Estado de Minas Gerais (FAPEMIG CRA - grant number APQ-01711-14) and from Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq Universal no 447449/2014-1 and Bolsa de Produtividade em Pesquisa, Chamada CNPq no 09/2018, grant number 302202/2018-8). We also acknowledge Verde AgriTech for drill cores and exploration data.	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South Am. Earth Sci.	APR	2020	99								102503	10.1016/j.jsames.2020.102503	http://dx.doi.org/10.1016/j.jsames.2020.102503			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6BC					2023-06-23	WOS:000528182600001
J	Mota, MD; Morte, AND; Silva, LCRCE; Chinalia, FA				Mota, Milleno Dantas; da Boa Morte, Airana Nascimento; Ribeiro Cerqueira e Silva, Lidercia Cavalcanti; Chinalia, Fabio Alexandre			Sunscreen protection factor enhancement through supplementation with Rambutan (Nephelium lappaceum L) ethanolic extract	JOURNAL OF PHOTOCHEMISTRY AND PHOTOBIOLOGY B-BIOLOGY			English	Article						Cosmetics; Sun protection factor; Photoprotection; Nephelium lappaceum L	PHENOLIC-COMPOUNDS; SUN	The use of plant bioactives in cosmetic formulations are increasing due to the search for new sustainable sources of raw materials, greater concern for safety and possible social impacts caused by the incorrect use of natural resources. Plant extracts have been the subject of several studies in several industrial areas. However, the potential use of tropical fruits extracts in cosmetic formulations remains largely unexplored. Considering the impact on public health and the possibility of using wastes from fruit processing, the aim of this work is to identify, evaluate and develop a sunscreen based on rambutan peel extracts (Nephelium lappaceum L) as a natural additive for enhancing the final product sun protection factor (SPF). The phytochemical screening revealed the presence of tannins and flavonoids and the absence of coumarins. Even presenting a low sunscreen factor when used alone (SPF value 0.4), rambutan extract at 1.00% FTP concentration improved the photoprotective result (11.2) of the formulation containing 7.5% of ethylhexyl metoxycinnamate (EHMC) by 134%. The addition of rambutan extract in the formulation shows the potential to reduce the use of synthetic photoprotectors by about 64% of the total synthetic organic filters used to achieve the SPF value of 26.3. In addition, the sunscreen formulation supplemented with rambutan extract containing 1.00% RTP shows the potential to minimize the risk of synthetic agent toxicity and a 45% reduction in the cost of sunscreen production.	[Mota, Milleno Dantas; da Boa Morte, Airana Nascimento] Univ Estado Bahia, Dept Life Sci, Silveira Martins St 2555, BR-41150000 Salvador, BA, Brazil; [Mota, Milleno Dantas] Univ Fed Bahia, Fac Pharm, Dept Med, Barao Jeremoabo St 147, BR-40170115 Salvador, BA, Brazil; [Ribeiro Cerqueira e Silva, Lidercia Cavalcanti; Chinalia, Fabio Alexandre] Univ Fed Bahia, Hlth Sci Inst, Postgrad Program Biotechnol, Principal Miguel Calmon Ave, BR-40110100 Salvador, BA, Brazil	Universidade do Estado Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia	Chinalia, FA (autor correspondente), Univ Fed Bahia, Hlth Sci Inst, Postgrad Program Biotechnol, Principal Miguel Calmon Ave, BR-40110100 Salvador, BA, Brazil.	chinalia@hotmail.com						Alkasim Kabiru Yunusa, 2018, Annals Food Science and Technology, V19, P774; [Anonymous], GLOB SUN CAR PROD MA; [Anonymous], SUNSCR SIM; [Anonymous], CANC TOM; [Anonymous], INT TRAV HLTH SIT 1; [Anonymous], GLOBAL RAMBUTAN MARK; [Anonymous], BRAZ PHARM NAT FOR; [Anonymous], 1997, INTRO FITOQUIMICA EX; [Anonymous], 2019, INT J ENV SCI NATURA; [Anonymous], CLEAN SCREEN MIN SPF; [Anonymous], EXP RAMB EUR; [Anonymous], SOL ULTR RAD; [Anonymous], BRASIL INFARMA CIENC; [Anonymous], 2017, FOOD RES; [Anonymous], FARMACOGNOSIA DO PRO; Araujo L, 2016, J YOUNG PHARM, V8, P144, DOI 10.5530/jyp.2016.2.17; Aryal S, 2019, PLANTS-BASEL, V8, DOI 10.3390/plants8040096; Azwanida N. 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APR	2020	205								111837	10.1016/j.jphotobiol.2020.111837	http://dx.doi.org/10.1016/j.jphotobiol.2020.111837			7	Biochemistry & Molecular Biology; Biophysics	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Biophysics	LB0QH	32146271				2023-06-23	WOS:000524342100021
J	Otero, XL; Araujo, JMC; Barcellos, D; Queiroz, HM; Romero, DJ; Nobrega, GN; Siqueira Neto, M; Ferreira, TO				Otero, Xose L.; Araujo, Jose M. C., Jr.; Barcellos, Diego; Queiroz, Hermano M.; Romero, Danilo J.; Nobrega, Gabriel N.; Siqueira Neto, Marcos; Ferreira, Tiago O.			Crab Bioturbation and Seasonality Control Nitrous Oxide Emissions in Semiarid Mangrove Forests (Ceara, Brazil)	APPLIED SCIENCES-BASEL			English	Article						Ucides cordatus; N2O; mangroves; greenhouse gas; estuarine fauna	GREENHOUSE-GAS EMISSIONS; UCIDES-CORDATUS; SULFUR BIOGEOCHEMISTRY; WETLAND SOILS; TRACE-METALS; WORLD MAP; CARBON; METHANE; FLUXES; IRON	Seasonality and crab activity affects the nutrients and physicochemical parameters in mangrove soils, thus, affecting the emissions of greenhouse gases, such as nitrous oxide (N2O). Climate change may intensify rainfall and/or enhance droughts, affecting mangroves and associated biota. Crabs are natural soil bioturbators responsible for soil aeration and turnover. We evaluated the effect of Ucides cordatus crab on N2O emissions from mangrove soils under a semiarid climate in Northeastern Brazil. Soil and gas samples were collected over the rainy and dry seasons in crab-naturally-bioturbated and crab-exclusion mangrove plots. We measured the soil's pH, redox potential, and the total contents of carbon, nitrogen, and sulfur. We found higher N2O emissions in the crab-exclusion sites compared to the bioturbated sites, as well as higher N2O emissions in the rainy season compared to the dry season. The fluxes of N2O (mu g m(-2) h(-1)) were 47.3 +/- 9.7 and 8.9 +/- 0.5 for the crab-exclusion sites, and 36.5 +/- 7.8 and 4.5 +/- 2.1 for the bioturbated sites (wet and dry seasons, respectively). The soil turning over by macrofauna led to lower N2O fluxes in natural crab-bioturbated areas, and seasonality was the environmental factor that contributed the most to the changes in N2O emissions. Broadly, anthropic activities and seasonality influence nitrogen fate, N2O emissions, and ecological services in coastal ecosystems.	[Otero, Xose L.] Univ Santiago de Compostela, CRESTUS Inst, Fac Biol, Dept Edafol & Quim Agr, Rua Lope G Marzoa S-N,Campus Sur, Santiago De Compostela 15782, Spain; [Araujo, Jose M. C., Jr.] Univ Fed Ceara, Grad Program Ecol & Nat Resources, Dept Biol, Campus Pici, BR-60440 Fortaleza, CE, Brazil; [Barcellos, Diego; Queiroz, Hermano M.; Romero, Danilo J.; Ferreira, Tiago O.] Univ Sao Paulo, Dept Soil Sci, Coll Agr Luiz de Queiroz, ESALQ USP, Av Padua Dias 11, BR-13418 Piracicaba, SP, Brazil; [Nobrega, Gabriel N.] Fed Fluminense Univ, Dept Geochem, Grad Program Geosci Geochem, Outeiro Sao Joao Batista S-N,Campus Valonguinho, BR-24020 Niteroi, RJ, Brazil; [Siqueira Neto, Marcos] CENA USP, Ctr Energia Nucl Agr, Lab Biogeoquim Ambiental, Av Centenario 303, BR-13400 Piracicaba, SP, Brazil	Universidade de Santiago de Compostela; Universidade Federal do Ceara; Universidade de Sao Paulo; Universidade Federal Fluminense	Ferreira, TO (autor correspondente), Univ Sao Paulo, Dept Soil Sci, Coll Agr Luiz de Queiroz, ESALQ USP, Av Padua Dias 11, BR-13418 Piracicaba, SP, Brazil.	xl.otero@usc.es; jmoacirj@gmail.com; diego.barcellos@usp.br; hermanomelo@usp.br; danilojromero@usp.br; gabrielnn@id.uff.br; msiqueir@usp.br; toferreira@usp.br	Barcellos, Diego/AAI-5073-2020; Nóbrega, Gabriel Nuto/AAQ-4189-2020; Romero, Danilo/ABA-7735-2020; Ferreira, Tiago Osório/D-3340-2015; Neto, Marcos Siqueira/AER-0799-2022; Queiroz, Hermano Melo/P-8700-2019	Barcellos, Diego/0000-0002-4198-2843; Nóbrega, Gabriel Nuto/0000-0001-7008-4201; Romero, Danilo/0000-0002-2280-3344; Ferreira, Tiago Osório/0000-0002-4088-7457; Queiroz, Hermano Melo/0000-0003-4768-1248; Siqueira Neto, Marcos/0000-0002-3982-7983; Araujo Junior, Jose Moacir de Carvalho/0000-0002-5705-6879	Sao Paulo Research Foundation (FAPESP) [2018/04259-2]; National Council for Scientific and Technology Development (CNPq) [305996/2018-5, 409593/2018-4]; Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP); Foundation for Research and Scientific and Technological Development of Maranhao and National Council of Technological and Scientific Development (FAPEMA/CNPq) [03572/2016]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES) [001]; Conselleria de Innovacion e Industria-Xunta de Galicia [PGIDIT08MDS036000PR]; Cross-Research in Environmental Technologies of the Santiago de Compostela University (CRETUS) strategic group [AGRUP2015/02]; Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro [202.757/2019]	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Council for Scientific and Technology Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); Foundation for Research and Scientific and Technological Development of Maranhao and National Council of Technological and Scientific Development (FAPEMA/CNPq); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselleria de Innovacion e Industria-Xunta de Galicia(Xunta de Galicia); Cross-Research in Environmental Technologies of the Santiago de Compostela University (CRETUS) strategic group; Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	The authors are grateful for the financial support provided by Sao Paulo Research Foundation (FAPESP, grant number 2018/04259-2), National Council for Scientific and Technology Development (CNPq, process 305996/2018-5; 409593/2018-4), Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP), Foundation for Research and Scientific and Technological Development of Maranhao and National Council of Technological and Scientific Development (FAPEMA/CNPq, grant #03572/2016), Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES)-Finance Code 001, Conselleria de Innovacion e Industria-Xunta de Galicia (PGIDIT08MDS036000PR), Cross-Research in Environmental Technologies of the Santiago de Compostela University (CRETUS) strategic group (AGRUP2015/02), and Fundacao de Amparo a Pesquisa do Estado do Rio de Janeiro (GNN, JCNE Grant #202.757/2019).	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Sci.-Basel	APR	2020	10	7							2215	10.3390/app10072215	http://dx.doi.org/10.3390/app10072215			16	Chemistry, Multidisciplinary; Engineering, Multidisciplinary; Materials Science, Multidisciplinary; Physics, Applied	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Engineering; Materials Science; Physics	LO0YT		gold, Green Published			2023-06-23	WOS:000533356200014
J	Petsch, C; Robaina, LED; Trentin, R; da Rosa, KK; de Figueiredo, AR; Simoes, JC				Petsch, Carina; de Souza Robaina, Luis Eduardo; Trentin, Romario; da Rosa, Katia Kellem; de Figueiredo, Anderson Ribeiro; Simoes, Jefferson Cardia			THE USE OF AUTOMATIC RELIEF MAPPING METHODS FOR ANALYSIS OF GLACIAL FORMS	REVISTA BRASILEIRA DE GEOMORFOLOGIA			Portuguese	Article						Automatic Classification; Glacial Geomorphology; Geomorphons	GEOMORPHONS; LANDFORMS; CLASSIFICATION; ELEMENTS; FLOW	Geomorphological mapping of glacial environments can be more accurate with the application of digital classification generated by Digital Elevation Models (MDEs). This paper evaluates the potential of geomorphon methodology for the identification of relief types in glacial mountain environments. New nomenclatures are proposed for the classification obtained directly by geomorphon when applied to glacial geomorphological mapping. The method is called Revised Geomorphon Digital Classification (RGDC). Morphometric and hydrological parameters, extracted from SRTMGL 1 and ALOS PALSAR MDEs, in a sector of the Cordillera Branca, Peru, were used in the new classification proposal. The identified classes were interpreted as horns, aretes, aretes strongly reworked by weathering, advancing moraines, slopes, circus valleys (amphitheater), U-valleys and V-valleys. The class of aretes is most easily identified using the geomorphons, same for horn classes. The results show the potential of the automatic method of digital classification of MDEs for the mapping of glacial relief shape types. Moraines with higher topographic amplitude were easily identified due to the spatial resolution and vertical accuracy of the DEMs used. The geomorphon identifies more relief types than classical methodologies for relief identification by MDEs, 7 relief types, while the Dikau et al. (1995) and ITP methods only provide 3 types. The ALOS PALSAR MDE, with higher spatial resolution, shows no difference in the identification of relief forms. The generated mapping can improve the reconstruction of geomorphological evolution, supporting paleoglaciological interpretation and understanding of territorial occupation along the Holocene.	[Petsch, Carina; de Souza Robaina, Luis Eduardo; Trentin, Romario] Univ Fed Santa Maria, Dept Geociencias, Av Roraima 1000,Predio 17, BR-97105900 Santa Maria, RS, Brazil; [da Rosa, Katia Kellem; de Figueiredo, Anderson Ribeiro; Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul, Ctr Polar & Climat, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil	Universidade Federal de Santa Maria (UFSM); Universidade Federal do Rio Grande do Sul	Petsch, C (autor correspondente), Univ Fed Santa Maria, Dept Geociencias, Av Roraima 1000,Predio 17, BR-97105900 Santa Maria, RS, Brazil.	carinapetsch@gmail.com; lesrobaina@yahoo.com.br; romario.trentin@gmail.com; katiakellem@gmail.com; anderson.figueiredo@ufrgs.br; jefferson.simoes@ufrgs.br	Trentin, Romario/AAH-5923-2020; Ribeiro de Figueiredo, Anderson/HJZ-2924-2023; Simoes, Jefferson Cardia/D-7232-2013; da Rosa, Kátia Kellem/AAO-8367-2020	Trentin, Romario/0000-0002-0615-2801; Ribeiro de Figueiredo, Anderson/0000-0002-0228-249X; Simoes, Jefferson Cardia/0000-0001-5555-3401; da Rosa, Kátia Kellem/0000-0003-0977-9658; Petsch, Carina/0000-0002-1079-0080				Allred Kory J., 2016, Annals of GIS, V22, P203, DOI 10.1080/19475683.2016.1195873; ANA- AUTORIDAD NACIONAL DEL AGUA, INV NAC GLAC LAG; [Anonymous], 1977, J GLACIOL, DOI DOI 10.3189/S0022143000021341; Arras C., 2017, EVALUATION VALIDATIO, P291, DOI [10.1007/978-3-319-54021-4_24, DOI 10.1007/978-3-319-54021-4_24]; BRUNSTEIN D., 2009, REV PALAEOBOT PALYNO, P269, DOI [10.1016/j. palaeo.2008.10.033, DOI 10.1016/J.PALAEO.2008.10.033]; Chandler BMP, 2018, EARTH-SCI REV, V185, P806, DOI 10.1016/j.earscirev.2018.07.015; Clapperton C. 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R., 2007, Glacier mass balance changes and meltwater discharge, P135; Sanches A. M., 2013, THESIS; Sarasan A, 2019, AREA, V51, P257, DOI 10.1111/area.12451; Stocker TF, 2014, CLIMATE CHANGE 2013: THE PHYSICAL SCIENCE BASIS, P1, DOI 10.1017/cbo9781107415324; WEISS A., 2001, ESRI USER C 2001 SAN, P1; Wen-Hung Liao, 2010, Proceedings of the 2010 20th International Conference on Pattern Recognition (ICPR 2010), P1003, DOI 10.1109/ICPR.2010.251	34	2	2	0	4	UNIAO GEOMORFOLOGIA BRASILEIRA	UBERLANDIA, BRAZIL	UNIV FEDERAL UBERLANDIA, AV JOAO NAVES AVILA 2160, UBERLANDIA, BRAZIL, 00000, BRAZIL	1519-1540	2236-5664		REV BRAS GEOMORFOL	Rev. Bras. Geomorfol.	APR-JUN	2020	21	2					253	269		10.20502/rbg.v21i2.1771	http://dx.doi.org/10.20502/rbg.v21i2.1771			17	Geography, Physical	Emerging Sources Citation Index (ESCI)	Physical Geography	LK5KJ		gold, Green Published			2023-06-23	WOS:000530904800003
J	Piovesan, EK; Fauth, G; Bergue, CT				Piovesan, Enelise Katia; Fauth, Gerson; Bergue, Cristianini Trescastro			LATE CRETACEOUS OSTRACODS FROM THE CENTRAL AREA OF THE POTIGUAR BASIN, NORTHEASTERN BRAZIL	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						taxonomy; Upper Cretaceous; paleoecology; neritic assemblages	FOSSOCYTHERIDEA SWAIN; BIOSTRATIGRAPHY; BROWN	The Jandaira Formation samples collected in the central region of the Potiguar Basin show a diverse Late Cretaceous ostracod fauna. The genera Cytherella, Bairdoppilata, Triebelina, Paracypris, Fossocytheridea, Ovocytheridea, Perissocytheridea, Protocosta, Soudanella, and Leguminocythereis indicate a marginal marine environment during the Santonian-Campanian. The analyzed material demonstrates that ostracods are significant indicators of changes in the depositional environment and paleoecological markers in marginal marine environments.	[Piovesan, Enelise Katia] Univ Fed Pernambuco, Lab Micropaleontol Aplicada LMA, Programa Posgrad Geociencias, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil; [Fauth, Gerson] Univ Vale Rio dos Sinos, Inst Tecnol Micropaleontol Itt Fossil, Av Unisinos 950, BR-93022750 Sao Leopoldo, RS, Brazil; [Bergue, Cristianini Trescastro] Univ Fed Rio Grande do Sul, Dept Interdisciplinar, Ctr Estudos Costeiros Limnol & Marinhos CECLIMA, Av Tramandai 976, BR-95625000 Imbe, RS, Brazil	Universidade Federal de Pernambuco; Universidade do Vale do Rio dos Sinos (Unisinos); Universidade Federal do Rio Grande do Sul	Piovesan, EK (autor correspondente), Univ Fed Pernambuco, Lab Micropaleontol Aplicada LMA, Programa Posgrad Geociencias, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil.	katiapiovesan@gmail.com; gersonf@unisinos.br; ctbergue@gmail.com	Fauth, Gerson/AAE-3353-2021; Piovesan, Enelise Katia/Q-2953-2017	Piovesan, Enelise Katia/0000-0002-0433-0395; Bergue, Cristianini/0000-0002-5007-3131; Fauth, Gerson/0000-0003-2594-1424				Andreu B., 1996, GEOLOGIE AFRIQUE ATL, P483; Apostolescu V., 1963, Revue de l'Institut Francais du Petrole, V18, P1675; Araripe P.T., 1994, B GEOCIENCIAS PETROB, V8, P127; Barros CD, 2018, J S AM EARTH SCI, V83, P117, DOI 10.1016/j.jsames.2018.02.001; dos Santos MAB, 2015, BRAZ J GEOL, V45, P23, DOI 10.1590/23174889201500010002; Bergue CT, 2011, REV BRAS PALEONTOLOG, V14, P149, DOI 10.4072/rbp.2011.2.03; Bismuth H., 1981, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V5, P193; Delicio MP, 2000, NEUES JAHRB GEOL P-A, V215, P321; Fauth G, 2005, J S AM EARTH SCI, V19, P285, DOI 10.1016/j.jsames.2005.01.007; Fauth G., 2012, B GEOCIENCIAS PETROB, V20, P229; Fauth G, 2018, R MICROPALEONTOL, V61, P139, DOI 10.1016/j.revmic.2018.10.003; Gebhardt Holger, 1999, Palaeontologische Zeitschrift, V73, P77; Grekoff N., 1951, Revue de l'Institut Francais du Petrole, V6, P53; Horne D. J., 2005, ENCY GEOLOGY, V3, P453; Mohriak W.U., 2003, GEOLOGIA TECTONICA R, P87; Monteiro M.C., 1988, C BRAS GEOL AN BEL, V35, P809; Neufville E.M.H., 1973, UPPER CRETACEOUS PAL, V1; Okosun E.A., 1987, OSTRACOD BIOSTRATIGR; OKOSUN EA, 1992, J AFR EARTH SCI, V14, P327, DOI 10.1016/0899-5362(92)90036-C; Pessoa-Neto O. C., 2007, B GEOCIENC PETROBRAS, V15, P357; Piovesan EK, 2015, REV BRAS PALEONTOLOG, V18, P21, DOI 10.4072/rbp.2015.1.02; Piovesan EK, 2015, PALAEOGEOGR PALAEOCL, V424, P40, DOI 10.1016/j.palaeo.2015.02.015; Piovesan EK, 2014, CARNETS GEOL, V14, P315; Piovesan EK, 2014, CARNETS GEOL, V14, P211; Reyment R. A., 1960, Stockholm Contributions in Geology, V7, P1; Viviere J.L., 1985, THESIS; VIVIERS M.C., 1995, ANAIS ACAD BRASILEIR, V67, P392; Viviers MC, 2000, CRETACEOUS RES, V21, P407, DOI 10.1006/cres.2000.0205	28	2	2	0	5	SOC BRASILEIRA PALEONTOLOGIA	SAO LEOPOLDO	PPGEO UNISINOS, AV UNISINOS 950, SAO LEOPOLDO, RS 93022-000, BRAZIL	1519-7530	2236-1715		REV BRAS PALEONTOLOG	Rev. Bras. Paleontol.	APR-JUN	2020	23	2					81	89		10.4072/rbp.2020.2.01	http://dx.doi.org/10.4072/rbp.2020.2.01			9	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	MO4RG		Green Published			2023-06-23	WOS:000551514700001
J	Raposo, MIB				Raposo, M. Irene B.			Emplacement of dike swarms from the island of Ilhabela (SE Brazil) and its relationship with the South Atlantic Ocean opening revealed by magnetic fabrics	PHYSICS OF THE EARTH AND PLANETARY INTERIORS			English	Article						AMS; AARM; Magma flow; Dike swarms; Ilhabela	SAO-FRANCISCO CRATON; FLOW DIRECTIONS; ROCK MAGNETISM; DYKE SWARMS; MAGMA FLOW; SUSCEPTIBILITY; ANISOTROPY; REMANENCE; TECTONICS; MODELS	Magnetic fabric and rock-magnetism studies were performed on 153 dikes from diabase, lamprophyre and alkaline dike swarms that outcrop on the island of Ilhabela, NE Sao Paulo State. The dikes crosscut Archean and Proterozoic polymetamorphic rocks. Their thicknesses range from a few centimeters to 4 or 5 m. They trend predominantly N30-60E with a very steep (similar to 60 degrees) to vertical dip. Magnetic fabrics were determined using anisotropy of low-field magnetic susceptibility (AMS) and anisotropy of anhysteretic remanent magnetization (AARM). Rock-magnetism measurements reveal that the magnetic mineral of the three swarms is magnetite mainly with grains in the range of 2-5 mu m. For a few dikes, these grains are the carriers of bulk magnetic susceptibility but are not responsible for the AMS, which is due to Fe-bearing minerals, as shown by AARM. The main AMS fabric recognized in the swarms is due to magma flow, in which the K-max-K-int plane is parallel to the dike's plane, and the magnetic foliation pole (K-min) is perpendicular to it. The analysis of the K-max inclination showed that the dikes were fed by horizontal to vertical flows. However, for the minority of the dikes, the AMS and AARM tensors are not coaxial. The AARM(max) is oriented N30-60 W, approximately perpendicular to the Kmax. The AARMmax orientation is similar to the direction of a fault system located mainly in the Santos marginal basin which, was formed in the Cretaceous rifting during the South Atlantic opening. The AARM fabric is tectonic in origin, and is parallel with the extensional paleostress responsible for the Gondwana break-up. The comparison of AMS and AARM fabrics suggests that diabase and lamprophyre dikes were emplaced in three distinct events in the earliest stages of the South Atlantic opening. Later, the alkaline dikes were emplaced in the final stages of the Atlantic opening.	[Raposo, M. Irene B.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, Brazil	Universidade de Sao Paulo	Raposo, MIB (autor correspondente), Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, Brazil.	irene@usp.br	Raposo, M. Irene B./D-6896-2013		Brazilian agency Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2007/56219-0]	Brazilian agency Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The author thanks the Brazilian agency Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) (Grant No. 2007/56219-0) for its financial support. Thanks to Ordiney Benedito da Silva for the construction of Fig. 2. Also, thanks the Editor (Dominique Jault), Bernard Henry, Manish A. Mamtani and Peter Selkin, whose comments greatly improved the manuscript.	Almeida F. F. 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APR	2020	301								106471	10.1016/j.pepi.2020.106471	http://dx.doi.org/10.1016/j.pepi.2020.106471			26	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	LE6KA					2023-06-23	WOS:000526831300009
J	Resende, RS; Saenz, CAT; Dantas, EL; Hackspacher, PC; Machaca, CAC; Glasmacher, UA				Resende, Rosana Silveira; Tello Saenz, Carlos Alberto; Dantas, Elton Luiz; Hackspacher, Peter Christian; Chavez Machaca, Cesar Anthony; Glasmacher, Ulrich A.			Thermochronology and exhumation history of the basement and sediments of the NNE border of the Parana basin, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Zircon; Fission-track method; U-Pb in situ dating; LA-MC-ICP-MS; Brasilia belt; Parana basin	ZIRCON FISSION-TRACK; U-PB ZIRCON; NEOPROTEROZOIC BRASILIA BELT; PLASMA-MASS SPECTROMETRY; SOUTH-AMERICAN PLATFORM; TECTONIC EVOLUTION; DECAY CONSTANT; THIN-FILM; SOUTHEASTERN BRAZIL; NEUTRON DOSIMETRY	Combined zircon fission-track (FT) and U-Pb dating were used to obtain correlated cooling ages and tectonic processes in the eastern border of the Phanerozoic Parana Basin, a large cratonic sedimentary basin in South America deposited over Precambrian basement, which is represented mainly by the Neoproterozoic Brasilia Orogenic Belt. Zircon ages obtained for clastic sediments suggest that the provenance history of the Parana Basin was derived chiefly from the proximal basement sources. Twelve zircon samples were collected, from which 194 grains were analyzed and simultaneously dated by the FT and U-Pb methods, and 146 zircon grains were additionally dated only through the fission-track method (FT). The standard sample of Fish Canyon Tuff (FCT) was also analyzed through FT and U-Pb, and the age results of 26.6 +/- 1.1 Ma, and 28.33 +/- 0.68 Ma, respectively, are consistent with the literature data. The fission-track ages, obtained for the Araxa (similar to 330 Ma) and Canastra (similar to 500 Ma) Groups, and Piumhi Massif (similar to 700 Ma) pertaining to the Brasilia Belt, in average increase towards the Sao Francisco Craton. This fission-track age pattern can be linked to the temperature and exhumation of each one of these units. The U-Pb detrital zircon ages obtained for the basement units range from 1.6 to 3.2 Ga and indicate different provenance sources in the evolution of the Brasilia Belt. However, it is clear that the main sources of metasedimentary rocks are derived from the Sao Francisco-Congo Craton. For samples collected in the NNE border of the Parana Basin, FT ages were obtained for 127 zircon grains with ages ranging between 100 and 600 Ma. Forty of these grains dated simultaneously with FT and U-Pb bear mean age populations of 0.6 and 1.0 Ga, and subordinately between 1.5 and 2.5 Ga. These results suggest that the units that represent the Sao Francisco Craton's Neoproterozoic passive margin were being formed with depositional sediments 1.0 Ga ago and their recycling was the main source for the zircon derivation recorded in the Parana Basin sediments. An important methodological result of this work is that U-Pb radiometric dating was done in the same areas of single zircon crystals employed to determine the FT ages, which improved the concordance in the U-Pb ages. As such, U-Pb dating on zircon micro areas that have undergone leaching, metamictization or another type of lattice damage was avoided.	[Resende, Rosana Silveira; Tello Saenz, Carlos Alberto] Univ Estadual Paulista, Dept Phys, UNESP, BR-19060900 Presidente Prudente, SP, Brazil; [Dantas, Elton Luiz; Chavez Machaca, Cesar Anthony] Univ Brasilia, Inst Geosci, Lab Geochronol Studies Geodynam & Environm, BR-70910900 Brasilia, DF, Brazil; [Hackspacher, Peter Christian] Univ Estadual Paulista, Inst Geosci & Exact Sci, UNESP, BR-13506900 Rio Claro, SP, Brazil; [Glasmacher, Ulrich A.] Heidelberg Univ, Inst Earth Sci, Thermochronol & Archaeometry Res Grp, Postfach 103980, D-69029 Heidelberg, Germany	Universidade Estadual Paulista; Universidade de Brasilia; Universidade Estadual Paulista; Ruprecht Karls University Heidelberg	Saenz, CAT (autor correspondente), Univ Estadual Paulista, Dept Phys, UNESP, BR-19060900 Presidente Prudente, SP, Brazil.	tello.saenz@unesp.br	Tello, Carlos Alberto/H-9863-2012; Dantas, Elton Luiz/AAK-8464-2021	Tello, Carlos Alberto/0000-0002-0369-8999; Dantas, Elton Luiz/0000-0002-7954-5059; Glasmacher, Ulrich Anton/0000-0002-1208-2838; Chavez Machaca, Cesar Anthony/0000-0001-5509-7514	Sao Paulo Research Foundation (FAPESP, Brazil) [2011/14943-9, 2014/158382]	Sao Paulo Research Foundation (FAPESP, Brazil)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	This work was financially supported by the Sao Paulo Research Foundation (FAPESP, Brazil) - grant #2011/14943-9 and 2014/158382. We are grateful to FRM II for closely accompanying the procedures involving the radioactive material. We also thank Dr. Hideki Iwano for the kindness of providing us the Fish Canyon Tuff zircon grains. Authors are indebted to Dr Julia Gezatt, for language help and writing assistance.	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South Am. Earth Sci.	APR	2020	99								102512	10.1016/j.jsames.2020.102512	http://dx.doi.org/10.1016/j.jsames.2020.102512			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6BC					2023-06-23	WOS:000528182600035
J	Schena, T; Lazzari, E; Primaz, C; Krause, LC; Machado, ME; Caramao, EB				Schena, Tiago; Lazzari, Eliane; Primaz, Carmem; Krause, Laiza Canielas; Machado, Maria Elisabete; Caramao, Elina Bastos			Upgrading of coconut fibers Bio-Oil: An investigation By GcxGc/Tofms	JOURNAL OF ENVIRONMENTAL CHEMICAL ENGINEERING			English	Article						Bio-Oil upgrading; Coconut fibers; Biomass pretreatment; Alkaline extraction; GCxGC/TOFMS	2-DIMENSIONAL GAS-CHROMATOGRAPHY; FAST PYROLYSIS; SUSTAINABLE PRODUCTION; SOXHLET EXTRACTION; SUPERCRITICAL CO2; ORGANIC-COMPOUNDS; AQUEOUS-PHASE; OPTIMIZATION; ACID; IDENTIFICATION	Pyrolysis of agroindustrial waste is an important way to add value to this material avoiding its discard in the environment. However, when residues are derived from oilseeds or similar, it is possible to find a large amount of fatty acid derivatives in the biomass and later in bio-oil composition. These compounds are not adequately thermo-degraded in pyrolysis processes, reducing the quality. Another common compound class and with a high added value present in bio-oils are phenols. In this work two forms of upgrading processes were performed in coconut fiber pyrolysis process. One of them is the alkaline extraction of coconut fiber bio-oil in order to produce a high acidic and a neutral fraction. The other upgrading process is a biomass pretreatment before the pyrolysis, using two different extraction techniques (Soxhlet and ultrasound). The two processes proved to be efficient and complimentary: in the first case, there was the pre-concentration of the phenols in a single fraction and in the second one, a great part of the fatty acids derivatives were removed from the bi-oil. These results indicate that the two techniques can be used to improve the quality of bio-oil produced by removing the free fatty acids from biomass and isolating compounds with high added value (in the case of phenols).	[Schena, Tiago; Lazzari, Eliane; Primaz, Carmem; Caramao, Elina Bastos] Univ Fed Rio Grande do Sul, Chem Inst, Porto Alegre, RS, Brazil; [Krause, Laiza Canielas; Caramao, Elina Bastos] Univ Tiradentes, PBI, Ind Biotechnol Post Grad Program, Aracaju, SE, Brazil; [Caramao, Elina Bastos] Univ Fed Bahia, INCT E&A, Salvador, BA, Brazil; [Machado, Maria Elisabete] Univ Fed Bahia, Chem Inst, Salvador, BA, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Tiradentes; Universidade Federal da Bahia; Universidade Federal da Bahia	Caramao, EB (autor correspondente), Univ Tiradentes, PBI, Ind Biotechnol Post Grad Program, Aracaju, SE, Brazil.	elinaufrgs@gmail.com	Machado, Maria Elisabete/E-7742-2013; Krause, Laiza Canielas/AAW-1766-2021; Lazzari, Eliane/ABE-5764-2020	Machado, Maria Elisabete/0000-0001-8289-4842; Krause, Laiza Canielas/0000-0001-5040-3586; LAZZARI, ELIANE/0000-0003-0286-4833; Schena, Tiago/0000-0001-8539-3381	PETROBRAS; CAPES; CNPq	PETROBRAS(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Authors would like to thank to PETROBRAS, CAPES and CNPq for the financial support of this work.	Abou-Yousef H, 2014, FUEL, V137, P115, DOI 10.1016/j.fuel.2014.07.067; Almeida TM, 2013, J AGR FOOD CHEM, V61, P6812, DOI 10.1021/jf401379s; Moraes MSA, 2012, J ANAL APPL PYROL, V98, P51, DOI 10.1016/j.jaap.2012.05.007; Barros JAS, 2018, MICROCHEM J, V137, P30, DOI 10.1016/j.microc.2017.09.015; Bispo MD, 2018, J ENVIRON CHEM ENG, V6, P2743, DOI 10.1016/j.jece.2018.04.029; Chong CT, 2019, ENERGY, V178, P804, DOI 10.1016/j.energy.2019.04.201; Maciel GPD, 2016, BIOMASS BIOENERG, V85, P198, DOI 10.1016/j.biombioe.2015.11.009; Das DD, 2009, BIORESOURCE TECHNOL, V100, P6524, DOI 10.1016/j.biortech.2009.06.104; Ghorbannezhad P, 2020, RENEW ENERG, V145, P663, DOI 10.1016/j.renene.2019.06.063; Hughes JM, 2003, ENERG FUEL, V17, P444, DOI 10.1021/ef010281b; Kanaujia PK, 2016, J ANAL APPL PYROL, V118, P202, DOI 10.1016/j.jaap.2016.02.005; Krause MC, 2019, J BRAZIL CHEM SOC, V30, P1608, DOI 10.21577/0103-5053.20190059; Lazzari E, 2018, IND CROP PROD, V111, P856, DOI 10.1016/j.indcrop.2017.11.005; Lazzari E, 2016, IND CROP PROD, V83, P529, DOI 10.1016/j.indcrop.2015.12.073; Li JH, 2010, J ANAL APPL PYROL, V89, P218, DOI 10.1016/j.jaap.2010.08.004; Link DD, 2005, ENERG FUEL, V19, P1693, DOI 10.1021/ef040095g; LIU ZY, 1991, J CHROMATOGR SCI, V29, P227, DOI 10.1093/chromsci/29.6.227; Lofrano G, 2013, SCI TOTAL ENVIRON, V461, P265, DOI 10.1016/j.scitotenv.2013.05.004; Mark R, 2019, J FUNCT FOODS, V57, P233, DOI 10.1016/j.jff.2019.04.008; Melecchi MIS, 2006, ULTRASON SONOCHEM, V13, P242, DOI 10.1016/j.ultsonch.2005.02.003; Michailof CM, 2016, WIRES ENERGY ENVIRON, V5, P614, DOI 10.1002/wene.208; Mohammadpour H, 2019, IND CROP PROD, V131, P106, DOI 10.1016/j.indcrop.2019.01.030; Mortensen PM, 2011, APPL CATAL A-GEN, V407, P1, DOI 10.1016/j.apcata.2011.08.046; Norouzi O, 2016, BIORESOURCE TECHNOL, V219, P643, DOI 10.1016/j.biortech.2016.08.017; Onorevoli B, 2014, IND CROP PROD, V52, P8, DOI 10.1016/j.indcrop.2013.09.034; Pfister DP, 2011, CHEMSUSCHEM, V4, P703, DOI 10.1002/cssc.201000378; Ramesh RS, 2018, MATER TODAY-PROC, V5, P25331, DOI 10.1016/j.matpr.2018.10.336; Rasrendra CB, 2011, CHEM ENG J, V176, P244, DOI 10.1016/j.cej.2011.08.082; Teixeira GL, 2018, J SUPERCRIT FLUID, V133, P122, DOI 10.1016/j.supflu.2017.10.003; VANDENDOOL H, 1963, J CHROMATOGR, V11, P463, DOI 10.1016/S0021-9673(01)80947-X; Zhao SW, 2014, SEP PURIF TECHNOL, V133, P443, DOI 10.1016/j.seppur.2014.07.018	31	7	7	0	8	ELSEVIER SCI LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND		2213-3437		J ENVIRON CHEM ENG	J. Environ. Chem. Eng.	APR	2020	8	2							103662	10.1016/j.jece.2020.103662	http://dx.doi.org/10.1016/j.jece.2020.103662			8	Engineering, Environmental; Engineering, Chemical	Science Citation Index Expanded (SCI-EXPANDED)	Engineering	LB6KW					2023-06-23	WOS:000524743700121
J	Dantas, MAT; Cherkinsky, A; Lessa, CMB; Santos, LV; Cozzuol, MA; Omena, EC; Da Silva, JLL; Sial, AN; Bocherens, H				Trindade Dantas, Mario Andre; Cherkinsky, Alexander; Bonfim Lessa, Carlos Micael; Santos, Luciano Vilaboim; Cozzuol, Mario Alberto; Omena, Erica Cavalcante; Lopes Da Silva, Jorge Luiz; Sial, Alcides Nobrega; Bocherens, Herve			ISOTOPIC PALEOECOLOGY (delta C-13,delta O-18) OF A LATE PLEISTOCENE VERTEBRATE COMMUNITY FROM THE BRAZILIAN INTERTROPICAL REGION	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						Quaternary; mammals; paleoecology; South America; stable isotopes	FEEDING ECOLOGY; STABLE-ISOTOPES; MAMMALIA; CARBON; BONE; C-13; HABITS; PREY; DIET; FRACTIONATION	Isotopes are one of the best tools to reconstruct the paleoecology of extinct taxa, allowing us to evaluate their diet (through carbon; C-3 and C-4 plants), their niche breadth (B-A) and the environment in which they lived. In the present work we go deeper in the use of isotopes, and explore a mathematical mixing model with the stable isotopic composition of one (carbon) and two elements (carbon and oxygen) to evaluate (i) the relative contributions of three types of food resources (leaves, fruits and C-4 grass) for meso- and megaherbivores (body mass > 100 kg) that lived during the late Pleistocene in Sergipe, Brasil, and (ii) which of these herbivores (together with some faunivorous taxa) could be potential preys for Smilodon populator and Caiman latirostris. Finally, we reconstructed the paleoenvironment in which the vertebrate community of Sergipe lived and concluded that the environment of Sergipe was a closer and drier landscape than African savannah nowadays, at least between 27 ka to 11 ka.	[Trindade Dantas, Mario Andre; Bonfim Lessa, Carlos Micael] Univ Fed Bahia, Inst Multidisciplinar Saude, Lab Ecol & Geociencias, Campus Anisio Teixeira, Vitoria Da Conquista, BA, Brazil; [Cherkinsky, Alexander] Univ Georgia, Ctr Appl Isotope Studies, Athens, GA 30602 USA; [Santos, Luciano Vilaboim; Cozzuol, Mario Alberto] Univ Fed Minas Gerais, Programa Posgrad Zool, Belo Horizonte, MG, Brazil; [Omena, Erica Cavalcante] Univ Fed Pernambuco, Programa Posgrad Geociencias, Recife, PE, Brazil; [Lopes Da Silva, Jorge Luiz] Univ Fed Alagoas, Dept Paleontol, Museu Hist Nat, Maceio, Alagoas, Brazil; [Sial, Alcides Nobrega] Univ Fed Pernambuco, Ctr Tecnol & Geociencias, Dept Geol, NEG LABISE, Recife, PE, Brazil; [Bocherens, Herve] Univ Tubingen, Biogeol, Dept Geosci, Holderlinstr 12, D-72074 Tubingen, Germany; [Bocherens, Herve] Univ Tubingen, Senckenberg Ctr Human Evolut & Palaeoenvironm HEP, Holderlinstr 12, D-72074 Tubingen, Germany	Universidade Federal da Bahia; University System of Georgia; University of Georgia; Universidade Federal de Minas Gerais; Universidade Federal de Pernambuco; Universidade Federal de Alagoas; Universidade Federal de Pernambuco; Eberhard Karls University of Tubingen; Eberhard Karls University of Tubingen; Senckenberg Gesellschaft fur Naturforschung (SGN)	Dantas, MAT (autor correspondente), Univ Fed Bahia, Inst Multidisciplinar Saude, Lab Ecol & Geociencias, Campus Anisio Teixeira, Vitoria Da Conquista, BA, Brazil.	matdantas@yahoo.com.br; acherkin@uga.edu; biologolessa@gmail.com; palaiosvilaboim@hotmail.com; mario.cozzuol@gmail.com; erica.omena@gmail.com; jluizlopess@gmail.com; sial@ufpe.br; herve.bocherens@uni-tuebingen.de	BOCHERENS, Hervé/F-3580-2011; Cozzuol, Mario A/H-8302-2012; Sial, Alcides/AAD-1901-2021	BOCHERENS, Hervé/0000-0002-0494-0126; Cozzuol, Mario A/0000-0003-3645-0401; Lopes, Jorge/0000-0001-9855-0411	CNPq [404684/2016-5, PQ/CNPq 311003/2019-2]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	To CNPq by financial support through Universal project (process 404684/2016-5) and research fellowship to MATD (PQ/CNPq 311003/2019-2); To A. Liparini (Laboratorio de Paleontologia/UFS) and C. Cartelle (PUC/MG) for allow measurements in fossils collection that they are responsible for; To biologist V. Gomes and L. Alves for help in Solver (Excel) analysis; To H. Araujo Jr., L. Asevedo and reviewers for critical evaluation of manuscript.	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J	Perez, A; Machado, W; Gutierrez, D; Smoak, JM; Breithaupt, JL; Saldarriaga, MS; Sanders, L; Marotta, H; Sanders, CJ				Perez, Alexander; Machado, Wilson; Gutierrez, Dimitri; Smoak, Joseph M.; Breithaupt, Joshua L.; Saldarriaga, Maritza S.; Sanders, Luciana; Marotta, Humberto; Sanders, Christian J.			Carbon and nutrient accumulation in mangrove sediments affected by multiple environmental changes	JOURNAL OF SOILS AND SEDIMENTS			English	Article						Carbon accumulation; Eutrophication; Mangroves; Organic matter source; Sea level rise	ORGANIC-CARBON; MARINE-SEDIMENTS; SEPETIBA BAY; NITROGEN; ESTUARY; DELTA-N-15; ISOTOPE; STORAGE; FORESTS; RATIOS	Purpose In order to assess the impact of anthropogenic activities on carbon and nutrient accumulation, total organic carbon (TOC), nitrogen (TN), and phosphorus (TP) accumulation rates were examined in a Pb-210-dated mangrove sediment core from Sepetiba Bay, Brazil, a coastal region impacted by multiple environmental changes during the previous century. Materials and methods A 50-cm length sediment core was collected from a mangrove forest in Sepetiba Bay. Sediment subsamples were analyzed to measure TOC, TN, delta C-13, and delta N-15 using an elemental analyzer attached to an isotope ratio mass spectrometer Thermo Finnigan Model Delta Plus XP, whereas colorimetric analysis were used to measure TP. For (210)Pbex analyses, gamma-ray measurements were performed in a semiplanar intrinsic germanium high purity coaxial detector, coupled to a multichannel analyzer, whereas the sediment accumulation rate (SAR) was calculated according to the constant initial concentration (CIC) method. Also, carbon and nutrient fluxes were calculated using SAR and TOC, TN, and TP contents, whereas statistical differences were evaluated by ANOVA + Tukey HSD analysis with previous data normalization. Results and discussion The calculated sedimentation rate (similar to 8.1 mm year(-1)) since the early 1900s was up to threefold higher than the global mean determined for mangrove forests (similar to 2.8 mm year(-1)) and the regional sea level rise (similar to 3.2 mm year(-1)). Significantly higher TOC, TN, and TP fluxes, up to nearly 1000, 90, and 15 g m(-2) year(-1), respectively, were observed after the water diversion from a nearby drainage basin in the 1950s and an increase in sewage effluent input, which increased in the early 1990s. After this period, lighter delta C-13 values (similar to - 25 parts per thousand) indicate an increased importance of the terrestrial organic matter source, while lower TOC:TN ratios (similar to 11) and heavier delta N-15 values (similar to + 9 parts per thousand) suggest an increased influence of anthropogenic fertilization on inorganic nitrogen accumulation. Conclusions The significantly higher accumulation rates during the last decades evidenced the role of mangrove sediments as sinks for anthropogenically enhanced inputs of carbon and nutrients. Also, studies on carbon and nutrient accumulation evidenced the need for further research in eutrophic coastal areas.	[Perez, Alexander; Gutierrez, Dimitri] Univ Peruana Cayetano Heredia, CEDIS, Fac Ciencias & Filosofia, Lab Biogeociencias,LID, Av Honorio Delgado 430, Lima, Peru; [Perez, Alexander; Machado, Wilson] Univ Fed Fluminensc, Dept Geoquim, Rua Outeiro Sao Joao Baptista S-N, Niteroi, RJ, Brazil; [Gutierrez, Dimitri] Inst Mar Peru, Direcc Gen Invest Oceanog & Cambio Climat, Av Gamarra & Gen Valle S-N, Chucuito, Callao, Peru; [Smoak, Joseph M.] Univ S Florida, Environm Sci, St Petersburg, FL USA; [Breithaupt, Joshua L.] Univ Cent Florida, Biol Dept, Orlando, FL 32816 USA; [Saldarriaga, Maritza S.] Univ Peruana Cayetano Heredia, Fac Ciencias & Filosofia, Programa Maestria Ciencias Mar, Av Honorio Delgado 430, Lima, Peru; [Sanders, Luciana] Southern Cross Univ, Southern Cross Geosci, POB 157, Lismore, NSW 2480, Australia; [Marotta, Humberto] Univ Fed Fluminense, Int Lab Global Change LINCGlobal, Grad Program Geosci Environm Geochem,Dept Geog, Biomass & Water Management Res Ctr NAB UFF,Ecosys, Av Edmund March S-N, BR-24210310 Niteroi, RJ, Brazil; [Marotta, Humberto] Univ Fed Fluminense, Dept Geog, Sedimentary & Environm Proc Lab LAPSA UFF, Grad Program Geog, Av Gal Milton Tavares de Souza S-N, BR-24210346 Niteroi, RJ, Brazil; [Sanders, Christian J.] Southern Cross Univ, Natl Marine Sci Ctr, Sch Environm Sci & Engn, Coffs Harbour, NSW 2450, Australia	Universidad Peruana Cayetano Heredia; Instituto del Mar del Peru; State University System of Florida; University of South Florida; State University System of Florida; University of Central Florida; Universidad Peruana Cayetano Heredia; Southern Cross University; Universidade Federal Fluminense; Universidade Federal Fluminense; Southern Cross University	Perez, A (autor correspondente), Univ Peruana Cayetano Heredia, CEDIS, Fac Ciencias & Filosofia, Lab Biogeociencias,LID, Av Honorio Delgado 430, Lima, Peru.; Perez, A (autor correspondente), Univ Fed Fluminensc, Dept Geoquim, Rua Outeiro Sao Joao Baptista S-N, Niteroi, RJ, Brazil.	alexander.perez.s@upch.pe	Saldarriaga, Maritza/F-5637-2016; Sanders, Christian J/AAM-6906-2021; Smoak, Joseph/E-2140-2012; Machado, Wilson/P-8047-2019; Marotta, Humberto/F-9554-2012	Saldarriaga, Maritza/0000-0001-5947-8576; Sanders, Christian J/0000-0003-0090-0896; Smoak, Joseph/0000-0002-4322-4042; Machado, Wilson/0000-0003-3117-8584; Marotta, Humberto/0000-0002-2828-6595; Breithaupt, Joshua/0000-0003-0963-3253; Perez Segovia, Alexander/0000-0003-4343-1583	"Fondo Nacional de Desarrollo Cientifico Tecnologico y de Innovacion Tecnologica" (Fondecyt, Peru), through the MAGNET research program [007-2017-FONDECYT]; "Fondo Nacional de Desarrollo Cientifico Tecnologico y de Innovacion Tecnologica" (Fondecyt, Peru), through the "Incorporacion de Investigadores" program [E038-2019-02-FONDECYT-BM]; University of South Florida, College of Marine Science, St. Petersburg Downtown Partnership Endowed Fellowship in Coastal Science; Brazilian Research Council (CNPq); Australian Research Council [DE160100443]; Universidade Federal Fluminense (UFF, Brazil); Research Support Foundation of the State of Rio de Janeiro (FAPERJ, "Programa Jovem Cientista do Nosso Estado"); Brazilian Research Council (CNPq, Programa Universal); CAPES [001]	"Fondo Nacional de Desarrollo Cientifico Tecnologico y de Innovacion Tecnologica" (Fondecyt, Peru), through the MAGNET research program; "Fondo Nacional de Desarrollo Cientifico Tecnologico y de Innovacion Tecnologica" (Fondecyt, Peru), through the "Incorporacion de Investigadores" program; University of South Florida, College of Marine Science, St. Petersburg Downtown Partnership Endowed Fellowship in Coastal Science; Brazilian Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Australian Research Council(Australian Research Council); Universidade Federal Fluminense (UFF, Brazil); Research Support Foundation of the State of Rio de Janeiro (FAPERJ, "Programa Jovem Cientista do Nosso Estado")(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Brazilian Research Council (CNPq, Programa Universal); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	AP is supported by the "Fondo Nacional de Desarrollo Cientifico Tecnologico y de Innovacion Tecnologica" (Fondecyt, Peru), through the MAGNET research program (Grant number 007-2017-FONDECYT) and the "Incorporacion de Investigadores" program (Grant number E038-2019-02-FONDECYT-BM). JLB was supported by the University of South Florida, College of Marine Science, St. Petersburg Downtown Partnership Endowed Fellowship in Coastal Science. We also are grateful to Dr. Bruno G. Libardoni, who provided us with invaluable suggestions.; WM is supported by research grants from the Brazilian Research Council (CNPq). CJS is supported by the Australian Research Council (DE160100443), in cooperation with Universidade Federal Fluminense (UFF, Brazil). HM received a research grant from the Research Support Foundation of the State of Rio de Janeiro (FAPERJ, "Programa Jovem Cientista do Nosso Estado") and the Brazilian Research Council (CNPq, Programa Universal). WM and AP thank the financial support from CAPES (Finance Code 001).	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Soils Sediments	MAY	2020	20	5					2504	2509		10.1007/s11368-020-02612-4	http://dx.doi.org/10.1007/s11368-020-02612-4		MAR 2020	6	Environmental Sciences; Soil Science	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Agriculture	LH2DU					2023-06-23	WOS:000522693300001
J	Dalmora, AC; Ramos, CG; Plata, LG; da Costa, ML; Kautzmann, RM; Oliveira, LFS				Dalmora, Adilson Celimar; Gindri Ramos, Claudete; Gomez Plata, Leandro; da Costa, Marcondes Lima; Kautzmann, Rubens Muller; Silva Oliveira, Luis Felipe			Understanding the mobility of potential nutrients in rock mining by-products: An opportunity for more sustainable agriculture and mining	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Mineral dissolution; Silicate rocks; Andesite; Dacite; Multi-nutrients source; Sustainable agriculture; Dissolution kinetics	POTASSIUM RELEASE; DISSOLUTION; SOIL; PHOSPHORUS; KINETICS; WASTE; RATES; PH; CLIMATE; PLANTS	The increase in demand for highly soluble fertilizers brings a global sustainability concern. Alternative sources for traditional fertilization are therefore needed. Rock powder use has been proposed as an alternative approach to soil rem ineralization. However, research on the agricultural potential of minerals and rocks as alternative sources of nutrients is limited to changes in soil chemical attributes or effects on crop yield. In this work, we report an experimental study addressing the dissolution of two silicate rock-derived powders (andesite and dacite) that were produced during mining activities in Southern Brazil. The rock powders were exposed to Milli-Q water at pH (7.4-8.8) range, in solutions of 0.1 mol L-1 dtric add at pH range 2.1-3.3, and Milli-Q water acidified with 0.5 mol l(-1) acetic add (pH 5-5.8), in a continuous mechanical rotatory shaker at room temperature. Dissolution kinetics were determined as a function of reaction times at 24 to 5760 h, and solution pH. Based on this kinetics, dissolution rates were determined for the individual powders and compared to expected values for aluminosilicates. Based on this comparison, it was shown that the application of andesite and dacite rock-derived powder to replace high soluble fertilizers is feasible due to high dissolution rates of their minerals. The average andesite dissolution rates in Milli-Q water, in dtric acid solution, and in Milli-Q water acidified with acetic acid were 2.1 x 10(-5), 1.92 x 10(-1) and 6.3 x 10(-4) mmol cm(-2) s(-1), respectively for Ca, being 183%, 22.6%, and 69.2% higher than for the dadte rodc.This make andesite rock a potential substitute for carbonate-based liming. In contrast, the average dadte dissolution rates in Milli-Q water, in dtric add solution, and in Milli-Q water acidified with acetic acid were 1.05 x 10(-5), 722 x 10(-5), and 3.72 x 10(-5) mrnol cm(-2) s(-1), respectively for K, being 72.0%, 61.4%, and 73.6% higher than the andesite rock. This highlights its potential use as a K source for agriculture to replace highly soluble K-fertilizers. (C) 2019 Elsevier B.V. All rights reserved.	[Dalmora, Adilson Celimar] Fed Univ Rio Grande do Sul UFRGS, Av Bento Goncalves,9500 Bldg 75,Room 122, BR-91501970 Porto Alegre, RS, Brazil; [Gindri Ramos, Claudete; Gomez Plata, Leandro; Silva Oliveira, Luis Felipe] Univ Costa, Dept Civil & Environm Engn, Calle 15 58 5566, Barranquilla, Colombia; [da Costa, Marcondes Lima] Fed Univ Para UFPA, Inst Geosci, R Augusto Correa 01, BR-66075110 Belem, PA, Brazil; [Kautzmann, Rubens Muller] La Salle Univ, Environm Impact Assessment, Victor Barreto 2288, BR-92010000 Canoas, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidad de la Costa; Universidade Federal do Para; Centro Universitario La Salle	Ramos, CG; Oliveira, LFS (autor correspondente), Univ Costa, Dept Civil & Environm Engn, Calle 15 58 5566, Barranquilla, Colombia.	claudeterms@gmail.com; felipeqma@hotmail.com	Silva, Luis F. O./S-9681-2017; Plata, leandro Gómez/AAR-1535-2020; Gindri, Claudete/ABB-6884-2021; Ramos, Claudete Gindri/AAV-3879-2021	Silva, Luis F. O./0000-0001-7678-9130; Plata, leandro Gómez/0000-0002-2944-4479; Ramos, Claudete Gindri/0000-0001-8809-458X; LIMA DA COSTA, MARCONDES/0000-0002-0134-0432	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq, Brazil [445435/2014-3]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq, Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to thank to Andrea Sander and Magda Bergmann of Companhia e Pesquisa de Recursos Minerais by petrographic description of the samples. We would also like to thank Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq, Brazil (Grant No. 445435/2014-3) for the financial support, to Incopel Industria e Comercio de Pedras Ltd. for supplying the vesicular andesite rock and to Sindicato da Industria de Extracao de Pedreiras de Nova Prata for supplying the dacite rock.	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Total Environ.	MAR 25	2020	710								136240	10.1016/j.scitotenv.2019.136240	http://dx.doi.org/10.1016/j.scitotenv.2019.136240			10	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	KI1EZ	31911256	Green Accepted			2023-06-23	WOS:000511088800154
J	Valero, A; Umbria-Salinas, K; Wallner-Kersanach, M; de Andrade, CF; Yabe, MJS; Contreira-Pereira, L; Wasserman, JC; Kuroshima, KN; Zhang, H				Valero, Astolfo; Umbria-Salinas, Karelys; Wallner-Kersanach, Monica; de Andrade, Carlos Ferreira; Santos Yabe, Maria Josefa; Contreira-Pereira, Leonardo; Wasserman, Julio Cesar; Kuroshima, Katia Naomi; Zhang, Hao			Potential availability of trace metals in sediments in southeastern and southern Brazilian shipyard areas using the DGT technique and chemical extraction methods	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						DGT; Trace metals; Shipyards; Porewater; Availability; Microelectrodes	RIO-DE-JANEIRO; ANTIFOULING PAINT PARTICLES; IN-SITU MEASUREMENT; HEAVY-METALS; DIFFUSIVE GRADIENTS; THIN-FILMS; PERFORMANCE-CHARACTERISTICS; QUALITY GUIDELINES; SURFACE SEDIMENTS; RIVER ESTUARY	Speciation and partitioning of trace metals, from solid to solution phases of sediments. control their bioavailability and thus their potential ecological risk to organisms. Therefore, in order to obtain a broad evaluation of their risk, it is necessary to couple methodologies that are able to assess metal mobility in sediment. In this study, the Diffusive Gradients in Thin Films (DGT) technique and the application of 0.1 M HCl acid extraction methods, together with solid-state voltammetric sensors, were used with the objective of assessing mobility and potential availability of Cr, Cu, Ni, Pb, V and Zn in sediment porewaters and solid sediments in southeastern and southern Brazilian shipyard areas. The highest labile metal concentrations were found in shipyards with the longest histories of operations. Trace metal distributions in porewater and in the solid phase of sediments (labile metals) and significant correlations among metals enabled to distinguish the contribution of anti-fouling paint components. The diffusive flux of every metal measured at the surface of the sediment indicated that CU DGT had the highest flux (3.66E-03 mmol.m(-2) d(-1)) in the shipyard with the longest operating time. Therefore, enrichment was observed for Cu, Pb and Zn in sediments, indicating a possible ecological risk level of 'Effects Range Median' to 'Apparent Effects Threshold' for oyster larvae (Mollusca) (Cu). bivalves (Pb) and the infaunal community (Zn). Probable Effect Concentrations (PEC) to sediment-dwelling biota can be expected as well, related to high concentrations of Cu and Zn in sediment. This study allowed a comprehensive evaluation of potential bioavailability and ecological risk of trace metals in aquatic systems where there is continuous and specific input of these elements. The use of the DGT technique with solid-state voltammetry in the sediment of distinct Brazilian estuarine systems demonstrated its potential to be applied in future environmental network programs. (C) 2019 Elsevier B.V. All rights reserved.	[Valero, Astolfo; Umbria-Salinas, Karelys; Wallner-Kersanach, Monica; de Andrade, Carlos Ferreira] Univ Fed Rio Grande, Inst Oceanog, Lab Hidroquim, BR-96203000 Rio Grande, Brazil; [Santos Yabe, Maria Josefa] Univ Estadual Londrina, Dept Quim, BR-86051990 Londrina, Brazil; [Contreira-Pereira, Leonardo] Univ Fed Pelotas, Ctr Desenvolvimento Tecnol, BR-96010610 Pelotas, RS, Brazil; [Wasserman, Julio Cesar] Univ Fed Fluminense, Programa Geoquim, BR-24030346 Niteroi, RJ, Brazil; [Kuroshima, Katia Naomi] Univ Vale Itajai, Escola Mar Ciencia & Tecnol, BR-88302202 Itajai, SC, Brazil; [Zhang, Hao] Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YQ, England	Universidade Federal do Rio Grande; Universidade Estadual de Londrina; Universidade Federal de Pelotas; Universidade Federal Fluminense; Universidade do Vale do Itajai; N8 Research Partnership; Lancaster University	Wallner-Kersanach, M (autor correspondente), Univ Fed Rio Grande, Inst Oceanog, Lab Hidroquim, BR-96203000 Rio Grande, Brazil.	monicawallner@furg.br	Wasserman, Julio Cesar/K-3863-2014; Zhang, Hao/E-5375-2010; Andrade, Carlos/AAJ-9211-2021; Wasserman, Julio/HGA-8235-2022; Wallner-Kersanach, Monica/J-4180-2019	Wasserman, Julio Cesar/0000-0002-7828-5240; Andrade, Carlos/0000-0002-2953-6568; Wasserman, Julio/0000-0002-7828-5240; Kuroshima, Katia/0000-0002-4261-9878; Wallner-Kersanach, Monica/0000-0001-7249-7835; Valero, Astolfo/0000-0003-2661-8733; Umbria, Karelys/0000-0002-7210-9377	National Council for Scientific and Technological Development (CNPq) [455010/2014-5]; Coordination for the Improvement of Higher Education Personnel (CAPES); National Council for Scientific and Technological Development [306714/2013-2]	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council for Scientific and Technological Development(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to thank the National Council for Scientific and Technological Development (CNPq; project no. 455010/2014-5) for providing financial support, and the Coordination for the Improvement of Higher Education Personnel (CAPES) for research funds granted to Astolfo Valero and Karelys Umbria. The National Council for Scientific and Technological Development also granted a research fellowship to Julio Cesar Wasserman (grant number 306714/2013-2).	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Total Environ.	MAR 25	2020	710								136216	10.1016/j.scitotenv.2019.136216	http://dx.doi.org/10.1016/j.scitotenv.2019.136216			13	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	KI1EZ	31923659				2023-06-23	WOS:000511088800107
J	Bertolini, G; Marques, JC; Hartley, AJ; Da-Rosa, AAS; Scherer, CMS; Basei, MAS; Frantz, JC				Bertolini, Gabriel; Marques, Juliana C.; Hartley, Adrian J.; Da-Rosa, Atila A. S.; Scherer, Claiton M. S.; Basei, Miguel A. S.; Frantz, Jose C.			Controls on Early Cretaceous desert sediment provenance in south-west Gondwana, Botucatu Formation (Brazil and Uruguay)	SEDIMENTOLOGY			English	Article						Botucatu desert; Cretaceous Parana Basin; desert accumulation; detrital zircon; heavy minerals; provenance analysis	LA-PLATA CRATON; HEAVY-MINERAL ASSEMBLAGES; FLOOD-BASALT VOLCANISM; NICO PEREZ TERRANE; DOM FELICIANO BELT; RUB AL-KHALI; U-PB AGES; PARANA BASIN; SOUTHERNMOST BRAZIL; STRATIGRAPHIC EVOLUTION	The Lower Cretaceous Botucatu Formation records the development of widespread dry-aeolian desert sedimentation throughout the Parana Basin in south-west Gondwana. To reconstruct the provenance of the aeolian sediment, petrography, granulometric analysis, U-Pb detrital zircon ages have been determined from along the southern basin margin in Rio Grande do Sul state (southern Brazil) and Uruguay (Tacuarembo region). The dataset reveals a mean composition Qt(89)F(8)L(3), comprising very fine to medium-grained quartozose and feldspatho-quartzose framework. Heavy mineral analysis reveals an overall dominance of zircon, tourmaline and rutile grains (mean ZTR(0.84)) with sporadic garnet, epidote and pyrolusite occurrences. The detrital zircon U-Pb ages are dominated by Cambrian to Neoproterozoic (515 to 650 Ma), Tonian to Stenian (900 to 1250 Ma) and Orosirian to Rhyacian (1.8 to 2.2 Ga) material. The detrital zircon dataset demonstrates a significant lateral variation in sediment provenance: Cambrian to Neoproterozoic detrital zircons dominate in the east, while Tonian to Stenian and Orosirian to Rhyacian ages predominate in the west of the study area. Sandstones are quartz-rich with dominantly durable zircon, tourmaline and rutile heavy mineral suite, with subtle but statistically significant along-strike differences in heavy mineral populations and detrital mineralogy which are thought to record local sediment input points into the aeolian system. The similar age spectra of Botucatu desert with proximal Parana Basin units, the predominance of quartzose, and zircon, tourmaline and rutile components, suggests that recycling is the mechanism responsible for the erg feeding.	[Bertolini, Gabriel] Univ Aberdeen, Kings Coll, Sch Geosci, Aberdeen AB24 3FX, Scotland; [Bertolini, Gabriel; Marques, Juliana C.; Scherer, Claiton M. S.; Frantz, Jose C.] Univ Fed Rio Grande do Sul, Inst Geociencias, BR-90040060 Porto Alegre, RS, Brazil; [Hartley, Adrian J.] Univ Aberdeen, Kings Coll, Geol & Petr Geol, Aberdeen AB24 3FX, Scotland; [Da-Rosa, Atila A. S.] Univ Fed Santa Maria, Dept Geociencias, Av Roraima,1000 Predio 17, BR-97105900 Santa Maria, RS, Brazil; [Basei, Miguel A. S.] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, SP, Brazil	University of Aberdeen; Universidade Federal do Rio Grande do Sul; University of Aberdeen; Universidade Federal de Santa Maria (UFSM); Universidade de Sao Paulo	Bertolini, G (autor correspondente), Univ Aberdeen, Kings Coll, Sch Geosci, Aberdeen AB24 3FX, Scotland.; Bertolini, G (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, BR-90040060 Porto Alegre, RS, Brazil.	gabertol@gmail.com	DaRosa, Atila A. S./E-1926-2013; Basei, Miguel A S/C-1915-2013; Marques, Juliana C/R-1965-2018; FRANTZ, JOSE C/R-1953-2018	DaRosa, Atila A. S./0000-0003-4074-0794; Basei, Miguel A S/0000-0002-3857-7089; Marques, Juliana C/0000-0003-0143-6925; FRANTZ, JOSE C/0000-0002-8890-7250; Santos Scherer, Claiton Marlon dos/0000-0002-7520-1187; Hartley, Adrian/0000-0002-5799-4734; Bertolini, Gabriel/0000-0002-3873-6190	Shell Brasil through 'UoA-UFRGS-SWB Sedimentary Basins' project at UFRGS ['BG05]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [203786/2017-3]	Shell Brasil through 'UoA-UFRGS-SWB Sedimentary Basins' project at UFRGS; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors gratefully acknowledge support from Shell Brasil through the 'BG05: UoA-UFRGS-SWB Sedimentary Basins' project at UFRGS and the strategic importance given by ANP through the R&D levy regulation. The authors would like to thank Renan Guilherme de Souza and Adriano Reis for help in Tacuarembo/Uy Field Trip. This work is part of the current dual-degree PhD from Gabriel Bertolini at Universidade Federal do Rio Grande do Sul and University of Aberdeen. We thank the editors, and Dr Eduardo Garzanti, Dr Luca Caracciolo and Dr Sebastian Oriolo for their kind and constructive reviews. We thank to Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) by the financial support (Grant: 203786/2017-3).	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J	Cardoso, AR; Romero, GR; Oses, GL; Nogueira, ACR				Cardoso, Alexandre Ribeiro; Romero, Guilherme Raffaeli; Oses, Gabriel Ladeira; Rodrigues Nogueira, Afonso Cesar			Taphonomy of lacustrine fish fossils of the Parnaiba Basin, northeastern Brazil: Spatial and causative relations of Konservat Lagerstatten in West Gondwana during Jurassic-Cretaceous	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Exceptional preservation; Fossildiagenesis; CAMP; Mass mortality; Articulated skeleton; Microbial mats	SOFT-TISSUE PRESERVATION; MICROBIAL MATS; SEDIMENTARY-ROCKS; GYPSUM DEPOSITS; BEHAVIOR; LAKE; MOLYBDENUM; GENESIS; ORIGIN; SHALES	Fossil bonanzas called Konservat Lagerstatten provide geological windows to the ecology of ancient life communities. These deposits often occur as cluster of fossil localities with similar geographic locations, geological ages and facies, as the fossils were generally preserved during special periods and large-scale events in Earth history within environments with exceptional taphonomic conditions. This work applied petrological and geochemical analyses to evaluate the taphonomic pathway of a Konservat Lagerstatten in the Muzinho Shale, Upper Jurassic-Lower Cretaceous of the Parnaiba Basin, northeastern Brazil. These lacustrine deposits include interbedded limestones and fossiliferous black shales deposited in anoxic, non-euxinic and saline environment. Black shales contain articulated skeletons of fish fossils, characterised by three-dimensional preservation of the skeletal tissue. The polytypical assemblage includes diverse ontogenetic stages and is concentrated in a specific stratigraphic level. Mass mortality was triggered by anoxia probably established by stratified water column, high C flux and thermocline demise. The specimens are encased in kerogen-bearing siliciclastic laminae and cementstone microfacies, both microbially-induced. The fossils were cemented by eodiagenetic poikilotopic calcite that filled the skeletal articulation, including bone trabeculae and voids originally filled by bone marrow. The short distance, similar fossil assemblages, ages and coincident palaeoenvironments suggest that Muzinho Shale (Parnaiba Basin) and Crato Formation (Araripe Basin) compose a cluster of exceptional preservation in West Gondwana. Lava flows and outgassing related to the Central Atlantic Magmatic Province (CAMP) resulted in the subaereal exposure of volcanic plains, acid rains and subsequent CO2 greenhouse crisis. CAMP-magmatism was especially voluminous in northern Brazilian basins, enhancing nutrient-rich waters and lacustrine eutrophication due to intensified chemical weathering in this area. Probably, other Konservat Lagerstatten remain unreported in West Gondwana. Despite similar causative events, the individual taphonomic pathways of Muzinho Shale and Crato Formation are very different, suggesting that in these cases local phenomena affected authigenesis and diagenesis.	[Cardoso, Alexandre Ribeiro; Romero, Guilherme Raffaeli; Rodrigues Nogueira, Afonso Cesar] Fed Univ Para Ufpa, Inst Geociences, Program Post Grad Geol & Geochem PPGG, Augusto Correa Ave 01, BR-66075110 Belem, Para, Brazil; [Cardoso, Alexandre Ribeiro] State Univ Campinas Unicamp, Inst Geosci, Dept Geol & Nat Resources, Carlos Gomes St 250, BR-13083870 Campinas, SP, Brazil; [Oses, Gabriel Ladeira] Univ Fed Sao Carlos, Program Postgrad Ecol & Nat Resources PPGERN, Washington Luis SP 310,KM 235, BR-13565905 Sao Carlos, SP, Brazil	Universidade Federal do Para; Universidade Estadual de Campinas; Universidade Federal de Sao Carlos	Cardoso, AR (autor correspondente), Fed Univ Para Ufpa, Inst Geociences, Program Post Grad Geol & Geochem PPGG, Augusto Correa Ave 01, BR-66075110 Belem, Para, Brazil.	a229678@dac.unicamp.br	Cardoso, Alexandre/AAK-3108-2020; Osés, Gabriel Ladeira/AAX-8158-2020	Cardoso, Alexandre/0000-0001-7562-6567; Osés, Gabriel Ladeira/0000-0002-4814-4893; Raffaeli Romero, Guilherme/0000-0001-9955-0878; NOGUEIRA, AFONSO/0000-0002-5225-9255	CAPES (Coordination for the Improvement of Higher Education Personnel) [001, CNPq - 130823/2017-1]; CNPq (National Council for Scientific and Technological Development) [CNPq - 130823/2017-1]; FAPESP (Fundaccio de Amparo a Pesquisa de Sao Paulo) [2017/21584-1]; Laboratory of Organic Stratigraphy and Geochemistry of the State University of the Rio de Janeiro (UERJ); Laboratorio de Quimiosfera of the State University of Sao Paulo (IQUSP) [FAPESP 2012/18936-0]	CAPES (Coordination for the Improvement of Higher Education Personnel)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq (National Council for Scientific and Technological Development)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESP (Fundaccio de Amparo a Pesquisa de Sao Paulo)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Laboratory of Organic Stratigraphy and Geochemistry of the State University of the Rio de Janeiro (UERJ); Laboratorio de Quimiosfera of the State University of Sao Paulo (IQUSP)	We thank CAPES (Coordination for the Improvement of Higher Education Personnel; financial code 001) and the CNPq (National Council for Scientific and Technological Development) for funding this research with a fellow scholarship (CNPq - 130823/2017-1). We also thank the Program of Post-Graduation in Geology and Geochemistry (PPGG) of the Federal University of Para (UFPa), the Program of Post-Graduation in Ecology and Natural Resources (PPGERN) of the Federal University of Sao Carlos (UFSCar), and the FAPESP (Fundaccio de Amparo a Pesquisa de Sao Paulo), Process 2017/21584-1. Logistic support for fieldwork was enabled by the Faculty of Geology (UFPa). This work was only possible due to the collaboration of many scientists and institutes listed below, to whom we are immensely grateful. Analyses carried out in the Federal University of Para included XRD (Laboratory of X-Ray Diffraction), SEM/EDS imaging (Laboratory of Microanalyses), cathodoluminescence analyses supported by Hudson Santos (Laboratory of Cathodoluminescence) and careful thin section preparations performed by Joelma Lobo (Laboratory of Lamination). Cleber Rabelo helped during fieldwork and sedimentological elaboration. Gustavo Paula-Santos guided the redox-sensitive geochemistry in the Laboratory of Geochemistry, and Erica Tonetto helped to acquire SEM imaging, both from the State University of Campinas (UNICAMP). TOC data was supported by Ailton Santos, Jaime Dias and the Laboratory of Organic Stratigraphy and Geochemistry of the State University of the Rio de Janeiro (UERJ). SR-mu XRF mapping was performed on the Brazilian Synchrotron Light Laboratory (LNLS/CNPEM), proposal 20180422, skillfully instructed by Carlos Perez. We also thank the Laboratorio de Quimiosfera of the State University of Sao Paulo (IQUSP), Raman Process FAPESP 2012/18936-0 for Raman spectroscopy, kindly supported by Fabio Rodrigues and Evandro Silva. We are very grateful to Daniel Fortier (Federal University of Piaui-UFPI) and Valeria Gallo (State University of the Rio de Janeiro-UERJ) for kindly providing photographs of well-preserved specimens. Cibele Voltani and Jairo Nascimento are acknowledged for their helpful suggestions. The authors are very grateful to the Editor Thomas Algeo, who handled this manuscript, A. Drew Muscente and an anonymous reviewer for very detailed and helpful corrections that greatly improved an earlier version of this work.	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Paleoclimatol. Paleoecol.	MAR 15	2020	542								109602	10.1016/j.palaeo.2020.109602	http://dx.doi.org/10.1016/j.palaeo.2020.109602			21	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	KR8FY					2023-06-23	WOS:000517852600007
J	Cheng, X; Bantim, RAM; Sayao, JM; Kellner, AWA; Wang, XL; Saraiva, AAF				Cheng, Xin; Bantim, Renan A. M.; Sayao, Juliana M.; Kellner, Alexander W. A.; Wang, Xiaolin; Saraiva, Antonio A. F.			The largest flying reptile from the Crato Formation, Lower Cretaceous, Brazil	HISTORICAL BIOLOGY			English	Article						Anhangueridae; Pterosauria; bone histology; Crato Formation; Cretaceous; Brazil	ROMUALDO FORMATION; ARARIPE BASIN; PTEROSAUR PTERODACTYLOIDEA; PALEOHISTOLOGY; ANHANGUERIDAE; TAPEJARIDAE; DIVERSITY; ONTOGENY; BONE	The Early Cretaceous deposits of the Araripe Basin in northeast Brazil has yielded numerous vertebrate fossils, in which pterosaurs are the predominant tetrapods. Almost all specimens of this extinct group of flying reptiles recovered from this basin come from two stratigraphic units, the Crato and Romualdo Formations, with the pterosaurs from the former being usually small to middle-sized and large individuals (with a maximized wingspan over 5 m) being only found in the latter. Here we report on a new specimen (MPSC R 1221) composed of a partial right wing, which is the largest pterosaur discovered from the Crato Formation so far, having an estimated maximized wingspan of 5.5 m. Despite the incompleteness of this material, MPSC R 1221 can be referred to the Anhangueridae based on the length ratio between the metacarpal IV and the first wing phalanx. According to the osteohistological study and the degree of fusion, MPSC R 1221 represents a sub-adult individual, showing that the animal had not reached the maximum size before its death. The present study shows that large-sized pterosaurs were also present in the Crato Formation and that their rarity might be an artefact of preservation.	[Cheng, Xin; Bantim, Renan A. M.; Saraiva, Antonio A. F.] Univ Reg Cariri, Lab Paleontol, Crato, CE, Brazil; [Cheng, Xin; Wang, Xiaolin] Chinese Acad Sci, Key Lab Vertebrate Evolut & Human Origins, Inst Vertebrate Paleontol & Paleoanthropol, Beijing, Peoples R China; [Sayao, Juliana M.] Univ Fed Pernambuco, Lab Paleobiol & Microestruturas, Ctr Acad Vitoria, Vitoria De Santo Antao, PE, Brazil; [Kellner, Alexander W. A.] Univ Fed Rio de Janeiro, Lab Systemat & Taphon Fossil Vertebrates, Dept Geol & Paleontol, Museu Nacl, Rio de Janeiro, RJ, Brazil; [Wang, Xiaolin] Univ Chinese Acad Sci, Beijing, Peoples R China	Universidade Regional do Cariri; Chinese Academy of Sciences; Institute of Vertebrate Paleontology & Paleoanthropology, CAS; Universidade Federal de Pernambuco; Universidade Federal do Rio de Janeiro; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Cheng, X (autor correspondente), Univ Reg Cariri, Lab Paleontol, Crato, CE, Brazil.; Cheng, X (autor correspondente), Chinese Acad Sci, Key Lab Vertebrate Evolut & Human Origins, Inst Vertebrate Paleontol & Paleoanthropol, Beijing, Peoples R China.	cheng_xin1982@126.com	CHENG, XIN/G-5664-2018; Bantim, Renan/J-4076-2014; Kellner, Alexander/ABE-9591-2020; Saraiva, António/HPD-3031-2023	CHENG, XIN/0000-0003-1415-1152; Kellner, Alexander/0000-0001-7174-9447; 	Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) [DCR-0024-02039.01.00, BMD-0124-00302.01.01/19]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [458164/2014-3, 304780/20138, 420687/2016-5, 311715/2017-6]; Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [E-26/202.893/2015]; National Natural Science Foundation of China [41688103, 41572020]; Strategic Priority Research Program of Chinese Academy of Sciences [XDB26000000]	Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Strategic Priority Research Program of Chinese Academy of Sciences(Chinese Academy of Sciences)	This study was supported by the Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) under Grant to XC DCR-0024-02039.01.00/and to RAMB BMD-0124-00302.01.01/19; the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) under Grant to AAFS 458164/2014-3, to AWAK 304780/20138 and 420687/2016-5 and to JMS 311715/2017-6; the Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) under Grant to AWAK E-26/202.893/2015; and the National Natural Science Foundation of China under Grant to XLW (41688103, 41572020) and the Strategic Priority Research Program of Chinese Academy of Sciences under Grant to XLW (XDB26000000).	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MAR 15	2020	32	3					321	329		10.1080/08912963.2018.1491567	http://dx.doi.org/10.1080/08912963.2018.1491567			9	Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Paleontology	KU9AV					2023-06-23	WOS:000520013600003
J	da Silva, CA; Santos, SD; Garcia, CAB; de Pontes, GC; Wasserman, JC				da Silva, Carlos Alberto; Santos, Silvia de Oliveira; Borges Garcia, Carlos Alexandre; de Pontes, Gabriela Cugler; Wasserman, Julio Cesar			Metals and arsenic in marine fish commercialized in the NE Brazil: Risk to human health	HUMAN AND ECOLOGICAL RISK ASSESSMENT			English	Article						toxicity; metals; target hazard quotient; marketed fish; maximum tolerance limits; health risk	HEAVY-METALS; TROPHIC TRANSFER; TOTAL MERCURY; CULTURED MILKFISH; TISSUE QUALITY; TRACE-METALS; FOOD-WEB; SEAFOOD; LEAD; CONSUMPTION	Arsenic, cadmium, lead, and mercury in fish is the result of long-term biomagnification in the food chain and is of public concern, due to the toxicity they engender. The objective of this research was to determine the concentrations of arsenic, cadmium, lead, and mercury in 13 species of marine fish broadly commercialized in Aracaju, SE, Brazil and to evaluate the risks of fish consumption associated with these trace elements, using the Target Hazard Quotient (THQ). As, Cd, and Pb levels were measured with inductively coupled plasma mass spectrometry (ICP-MS), and mercury was analyzed via cold vapor atomic absorption spectrometry. The results indicate a large variability in concentrations for arsenic (0.07-2.03 mg kg(-1)) and mercury (0.01-1.44 mg kg(-1)), associated with the animal dietary category. Cadmium (0.04-0.19 mg kg(-1)) and lead (<0.01-0.45 mg kg(-1)), on the other hand showed a mild variability. None of the evaluated specimens had As, Cd, and Pb THQ values higher than 1. The THQ values for mercury were higher but indicated no consumption risk, except for amberjack, and snook fish. Overall THQ indicates lower risk of consumption in fish that are at the base of the food chain, than in those that are top predators.	[da Silva, Carlos Alberto] Embrapa Coastal Tablelands, Aracaju, Brazil; [Santos, Silvia de Oliveira] Univ Fed Sergipe, FAPITEC, Aracaju, Brazil; [Borges Garcia, Carlos Alexandre] Fed Univ Sergipe UFS, Dept Chem, Aracaju, Brazil; [de Pontes, Gabriela Cugler] Univ Fed Fluminense, Dept Geoenvironm Anal, Niteroi, RJ, Brazil; [Wasserman, Julio Cesar] Univ Fed Fluminense, Inst Geosci, Postgrad Programme Geochem, Av Litoranea,Off 406, BR-24210346 Niteroi, RJ, Brazil; [Wasserman, Julio Cesar] Univ Fed Fluminense, Inst Geosci, Postgrad Programme Sustainable Syst Management, Av Litoranea,Off 406, BR-24210346 Niteroi, RJ, Brazil	Empresa Brasileira de Pesquisa Agropecuaria (EMBRAPA); Fundacao de Amparo a Pesquisa do Estado do Sergipe (FAPITEC); Universidade Federal de Sergipe; Universidade Federal Fluminense; Universidade Federal Fluminense; Universidade Federal Fluminense	Wasserman, JC (autor correspondente), Univ Fed Fluminense, Inst Geosci, Postgrad Programme Geochem, Av Litoranea,Off 406, BR-24210346 Niteroi, RJ, Brazil.; Wasserman, JC (autor correspondente), Univ Fed Fluminense, Inst Geosci, Postgrad Programme Sustainable Syst Management, Av Litoranea,Off 406, BR-24210346 Niteroi, RJ, Brazil.	geowass@vm.uff.br	Wasserman, Julio/HGA-8235-2022; Wasserman, Julio Cesar/K-3863-2014; Garcia, Carlos/A-8406-2013	Wasserman, Julio/0000-0002-7828-5240; Wasserman, Julio Cesar/0000-0002-7828-5240; Garcia, Carlos/0000-0001-5260-5093				Adel M, 2016, FOOD CHEM TOXICOL, V97, P135, DOI 10.1016/j.fct.2016.09.002; Afonso C, 2013, J FOOD COMPOS ANAL, V32, P59, DOI 10.1016/j.jfca.2013.06.008; Ahmad NI, 2015, ENVIRON SCI POLLUT R, V22, P3672, DOI 10.1007/s11356-014-3538-8; Alessio L, 2007, AM J IND MED, V50, P779, DOI 10.1002/ajim.20524; [Anonymous], B EST PESC AQ 2011; [Anonymous], MET PEIX PASC AL ARS; [Anonymous], EPA OFF MAR EST PROT; [Anonymous], MERCADO PESCADO ARAC; [Anonymous], TOX PROF ARS; [Anonymous], 2003, EH06 SOP USEPA; Augelli MA, 2007, FOOD CHEM, V101, P579, DOI 10.1016/j.foodchem.2006.02.017; Avigliano E, 2016, J FOOD COMPOS ANAL, V54, P27, DOI 10.1016/j.jfca.2016.09.011; Berk M, 2014, BMJ OPEN, V4, DOI 10.1136/bmjopen-2014-005142; Bosch AC, 2016, J SCI FOOD AGR, V96, P32, DOI 10.1002/jsfa.7360; Bratkic A, 2017, GEOMICROBIOL J, V34, P587, DOI 10.1080/01490451.2016.1247482; Burger J, 2005, ENVIRON RES, V99, P403, DOI 10.1016/j.envres.2005.02.001; Burger J, 2014, ENVIRON MONIT ASSESS, V186, P6721, DOI 10.1007/s10661-014-3885-4; Cabanero AI, 2005, BIOL TRACE ELEM RES, V103, P17, DOI 10.1385/BTER:103:1:017; Castro-Gonzalez MI, 2008, ENVIRON TOXICOL PHAR, V26, P263, DOI 10.1016/j.etap.2008.06.001; Chahid A, 2014, FOOD CHEM, V147, P357, DOI 10.1016/j.foodchem.2013.10.008; Chien LC, 2002, SCI TOTAL ENVIRON, V285, P177, DOI 10.1016/S0048-9697(01)00916-0; da Silva CA, 2011, BRAZ J OCEANOGR, V59, P259, DOI 10.1590/S1679-87592011000300006; Dural M, 2007, FOOD CHEM, V102, P415, DOI 10.1016/j.foodchem.2006.03.001; Eisler R., 1988, ARSENIC HAZARDS FISH; Elnabris K. 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Ecol. Risk Assess.	MAR 15	2020	26	3					695	712		10.1080/10807039.2018.1529552	http://dx.doi.org/10.1080/10807039.2018.1529552			18	Biodiversity Conservation; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	KT2RZ					2023-06-23	WOS:000518864500008
J	Andrade, RCLP; Sena, MVA; Araujo, EV; Bantim, RAM; Riff, D; Sayao, JM				de Andrade, Rafael Cesar Lima Pedroso; Sena, Mariana Valeria Araujo; Araujo, Esau Victor; Bantim, Renan Alfredo Machado; Riff, Douglas; Sayao, Juliana Manso			Osteohistological study on both fossil and living Caimaninae (Crocodyliformes, Crocodylia) from South America and preliminary comments on growth physiology and ecology	HISTORICAL BIOLOGY			English	Article						Bone tissue; Caiman yacare; osteohistology; Miocene; Caimaninae	BONE-HISTOLOGY; EVOLUTION; SKELETOCHRONOLOGY; OSTEODERMS; CROCODILES; DAUDIN; AGE	Caimaninae is a South American lineage of crocodylians widely distributed in Brazil and composed of six species within three genera. Currently, there is insufficient information regarding growth strategies, growth rates, and ecology extracted from the bone microstructure. Here we present the first osteohistological study of both Caiman yacare and an unidentified fossil Caiman. Long bones of one specimen of C. yacare and of one fossil Caiman found at Solimoes Formation (Acre Basin), were used to prepare the histological slides. The microstructure of C. yacare shows fibrolamellar complex present in the femur and tibia, while the humerus and radius of both C. yacare and the fossil Caiman revealed a slow-growing bone matrix with gradual decrease and effective stops. According to the results found here, Caimaninae seem to have the capability to adjust their growth rates in response to seasonal changes. The extant Caiman is classified as juvenile, but for the fossilized specimen no ontogenetic stage can be determined. Caiman yacare shows the presence of intraskeletal variability regarding the record of bone growth. We conclude that Caimaninae likely have been experiencing cyclical changes in growth rates in direct correlation to changes in seasons and environmental conditions since the Miocene.	[de Andrade, Rafael Cesar Lima Pedroso; Sena, Mariana Valeria Araujo] Univ Fed Pernambuco, Programa Posgrad Geociencias, Recife, PE, Brazil; [Araujo, Esau Victor; Sayao, Juliana Manso] Univ Fed Pernambuco, Ctr Acad Vitoria, Lab Paleobiol & Microestruturas, Vitoria De Santo Antao, PE, Brazil; [Bantim, Renan Alfredo Machado] Univ Reg Cariri, Museu Paleontol Placido Cidade Nuvens, Santana Do Cariri, CE, Brazil; [Riff, Douglas] Univ Fed Uberlandia, Lab Paleontol, Uberlandia, MG, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Regional do Cariri; Universidade Federal de Uberlandia	Andrade, RCLP (autor correspondente), Rua Antonio de Sa Leitao 139 Apt,1003 Boa Viagem, BR-51020090 Recife, PE, Brazil.	rafaclpa@gmail.com	Victor, Esaú/AAC-4282-2020; Riff, Douglas/B-5183-2012; Bantim, Renan/J-4076-2014; Sena, Mariana/AAC-4283-2020; Sena, Mariana V A/K-9347-2018	Victor, Esaú/0000-0003-3459-4495; Riff, Douglas/0000-0003-0805-2828; Sena, Mariana/0000-0003-4708-999X; Sena, Mariana V A/0000-0003-4708-999X	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [147466/2014-8]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior [88881.132283/2016-01]; Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco [BIC1327-2.04/17]; Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico [BMD0124-00302.01.01/19]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco(Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco (FACEPE)); Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP))	This work was supported by [Conselho Nacional de Desenvolvimento Cientifico e Tecnologico] [under the grant 147466/2014-8] to RCLPA; [Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior] [under the grant 88881.132283/2016-01] to RCLPA; [Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco] [under the grant BIC1327-2.04/17] to MVAS;[Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico] [under the grant BMD0124-00302.01.01/19] to RAMB.	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Biol.	MAR 15	2020	32	3					346	355		10.1080/08912963.2018.1493475	http://dx.doi.org/10.1080/08912963.2018.1493475			10	Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Paleontology	KU9AV					2023-06-23	WOS:000520013600006
J	Vieira, HM; Weschenfelder, J; Fernandes, EH; Oliveira, HA; Moller, OO; Garcia-Rodriguez, F				Vieira, Helen Maria; Weschenfelder, Jair; Fernandes, Elisa Helena; Oliveira, Heline Alves; Moller, Osmar Olinto; Garcia-Rodriguez, Felipe			Links between surface sediment composition, morphometry and hydrodynamics in a large shallow coastal lagoon	SEDIMENTARY GEOLOGY			English	Article						Deposition; Hydrodynamics; Morphometry; Resuspension	GRANDE-DO-SUL; SOUTHERN BRAZILIAN COAST; SEA-LEVEL CHANGES; PATOS LAGOON; QUATERNARY; EVOLUTION; ARGENTINA; DIATOM; LAKE	This study addresses the surface sediment composition and distribution in Mirim Lagoon, a large coastal shallow transboundary system located on the border of South Brazil and Uruguay. which is 3749 km(2) and maximum depth is around 6 m, in relation to the hydrodynamic conditions evolved from predominant winds. Surface water currents in the marginal area displayed maximum speed values of 0.25 to 0.3 m s(-1) flowing parallel to the coastline either under NE of SW wind predominance. The marginal zone, above the 6 m bathymetric contour comprise sandy sediments, indicating that under such a combination of bathymetric and hydrodynamic conditions, the resuspension of fine sediments is dominant. Lower surface current velocity observed in the central zone of the lagoon located below the 6 m isobath (i.e., 0.05 m s(-1)), together with an increase in the maximum width of the lagoon, promoted conditions for deposition of the day sediment fraction. Therefore, the combined use of sedimentological and hydrodynamic data represents a useful tool to infer patterns of deposition and resuspension in coastal systems. Given the large size of the Mirim Lagoon and associated difficulties in sampling and monitoring the system, the information presented here is important for environmental management, and particularly for planning future paleolimnological research and set the coring stations on appropriate coordinates within the central region, where relatively calm conditions and dominance of clay sediments are observed. (C) 2020 Elsevier B.V. All rights reserved.	[Vieira, Helen Maria; Fernandes, Elisa Helena; Oliveira, Heline Alves; Moller, Osmar Olinto; Garcia-Rodriguez, Felipe] Univ Fed Rio Grande FURG, Inst Oceanog, Lab Oceanog Costeira & Estuarina LOCOSTE, Rio Grande, Brazil; [Weschenfelder, Jair] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean CECO, Inst Geociencias, Porto Alegre, RS, Brazil; [Garcia-Rodriguez, Felipe] Ctr Univ Reg Este, Sede Cure Rocha, Ruta 9 S-N, Rocha 27000, Uruguay	Universidade Federal do Rio Grande; Universidade Federal do Rio Grande do Sul	Garcia-Rodriguez, F (autor correspondente), Univ Fed Rio Grande FURG, Inst Oceanog, Lab Oceanog Costeira & Estuarina LOCOSTE, Rio Grande, Brazil.	felipegr@fcienedu.uy	Moller, Osmar O/ISB-2973-2023; Fernandes, Elisa Helena/GLU-4155-2022; Weschenfelder, Jair/C-3390-2013	Weschenfelder, Jair/0000-0002-2075-4067; Moller, Osmar/0000-0002-7207-1022; Fernandes, Elisa/0000-0003-1869-0233	Financiadora de Estudos e Projetos FINEP [01.11.0141.01, 01.12.0064.00]; Conselho Nacional de Pesquisa CNPq [551436/2011-5, 308274/2011-3, 302231/2010-2]	Financiadora de Estudos e Projetos FINEP(Financiadora de Inovacao e Pesquisa (Finep)); Conselho Nacional de Pesquisa CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This paper is dedicated to the memory of H.M. Vieira who devoted her professional life to sedimentological research in Rio Grande, Brazil. Thanks to Financiadora de Estudos e Projetos FINEP for sponsoring the TRANSAQUA Project (www.transaqua.furg.br, grant 01.11.0141.01) and REHMANSA (grant 01.12.0064.00), and to Conselho Nacional de Pesquisa CNPq for the research grants 551436/2011-5 (EHF), 308274/2011-3 (EHF), and 302231/2010-2 (OOM). Jasper Knight and an anonymous reviewer provided helpful comments that improved this paper.	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J	Zhang, ZL; Cao, ZM; Grasse, P; Dai, MH; Gao, L; Kuhnert, H; Gledhill, M; Chiessi, CM; Doering, K; Frank, M				Zhang, Zhouling; Cao, Zhimian; Grasse, Patricia; Dai, Minhan; Gao, Lei; Kuhnert, Henning; Gledhill, Martha; Chiessi, Cristiano M.; Doering, Kristin; Frank, Martin			Dissolved silicon isotope dynamics in large river estuaries	GEOCHIMICA ET COSMOCHIMICA ACTA			English	Article						Stable Si isotopes; Conservative mixing; Biological fractionation; Riverine Si input; Large river estuaries	EAST CHINA SEA; AMAZON RIVER; BIOGENIC SILICA; CHANGJIANG ESTUARY; YANGTZE-RIVER; BIOGEOCHEMICAL PROCESSES; PARTICULATE MATERIAL; BIOLOGICAL UPTAKE; INORGANIC CARBON; CHESAPEAKE BAY	Estuarine systems are of key importance for the riverine input of silicon (Si) to the ocean, which is a limiting factor of diatom productivity in coastal areas. This study presents a field dataset of surface dissolved Si isotopic compositions (delta Si-30(Si(OH)4)) obtained in the estuaries of three of the world's largest rivers, the Amazon (ARE), Yangtze (YRE), and Pearl (PRE), which cover different climate zones. While delta Si-30(Si(OH)4) behaved conservatively in the YRE and PRE supporting a dominant control by water mass mixing, significantly increased delta Si-30(Si(OH)4) signatures due to diatom utilization of Si(OH) 4 were observed in the ARE and reflected a Si isotopic enrichment factor (30)epsilon of -1.0 +/- 0.4 parts per thousand- (Rayleigh model) or -1.6 +/- 0.4% (steady state model). In addition, seasonal variability of Si isotope behavior in the YRE was observed by comparison to previous work and most likely resulted from changes in water residence time, temperature, and light level. Based on the 30e value obtained for the ARE, we estimate that the global average delta Si-30(Si(OH)4) entering the ocean is 0.2-0.3% higher than that of the rivers due to Si retention in estuaries. This systematic modification of riverine Si isotopic compositions during estuarine mixing, as well as the seasonality of Si isotope dynamics in single estuaries, needs to be taken into account for better constraining the role of large river estuaries in the oceanic Si cycle. (C) 2020 Elsevier Ltd. All rights reserved.	[Zhang, Zhouling; Cao, Zhimian; Dai, Minhan] Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen 361102, Peoples R China; [Zhang, Zhouling; Cao, Zhimian; Dai, Minhan] Xiamen Univ, Coll Ocean & Earth Sci, Xiamen 361102, Peoples R China; [Grasse, Patricia; Gledhill, Martha; Doering, Kristin; Frank, Martin] GEOMAR Helmholtz Ctr Ocean Res Kiel, D-24148 Kiel, Germany; [Gao, Lei] East China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China; [Kuhnert, Henning] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Chiessi, Cristiano M.] Univ Sao Paulo, Sch Arts Sci & Humanities, BR-03828000 Sao Paulo, Brazil; [Doering, Kristin] Dalhousie Univ, Dept Oceanog, Halifax, NS B3H 4R2, Canada	Xiamen University; Xiamen University; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; East China Normal University; University of Bremen; Universidade de Sao Paulo; Dalhousie University	Cao, ZM (autor correspondente), Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen 361102, Peoples R China.	zmcao@xmu.edu.cn	Doering, Kristin/AAH-2255-2021; Gledhill, Martha/D-2819-2009; Doering, Kristin/ABD-4916-2020; DAI, M/GPS-8291-2022; Grasse, Patricia/AAJ-6483-2020; Cao, Zhimian/J-2122-2016; Gledhill, Martha/AAG-6062-2021; Chiessi, Cristiano Mazur/E-1916-2012; Dai, Minhan/G-3343-2010	Gledhill, Martha/0000-0003-3859-2112; Doering, Kristin/0000-0002-7900-2169; Grasse, Patricia/0000-0002-1745-4418; Gledhill, Martha/0000-0003-3859-2112; Chiessi, Cristiano Mazur/0000-0003-3318-8022; Dai, Minhan/0000-0003-0550-0701; Kuhnert, Henning/0000-0001-5242-4495; Zhang, Zhouling/0000-0002-8325-7148	National Natural Science Foundation of China (NSFC) [91858107, 41606089]; National Key Scientific Research Project - Ministry of Science and Technology of China [2015CB954003]; Graduate School of Xiamen University; DFG Research Center "The Ocean in the Earth System"; FAPESP [2012/17517-3]; Shiptime Sharing Project of the NSFC [NORC2015-03]; National Key Scientific Research Project [2015CB954001]	National Natural Science Foundation of China (NSFC)(National Natural Science Foundation of China (NSFC)); National Key Scientific Research Project - Ministry of Science and Technology of China; Graduate School of Xiamen University; DFG Research Center "The Ocean in the Earth System"(German Research Foundation (DFG)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Shiptime Sharing Project of the NSFC; National Key Scientific Research Project	This work was funded by the National Natural Science Foundation of China (NSFC; 91858107 and 41606089) and by the National Key Scientific Research Project (2015CB954003) sponsored by the Ministry of Science and Technology of China. Zhouling Zhang was co-supported by a scholarship under the Graduate School of Xiamen University and the National Key Scientific Research Project (2015CB954001). Henning Kuhnert was supported by the DFG Research Center "The Ocean in the Earth System". Cristiano M. Chiessi acknowledges the financial support from FAPESP (2012/17517-3). We thank the R/V Meteor cruise M147 crew and the R/V Maria S. Merian cruise MSM20/3 crew for technical support during sampling in the ARE. Data acquisition and sample collection in the YRE were conducted onboard R/V Runjiang I supported by a Shiptime Sharing Project of the NSFC (NORC2015-03). We thank Guipeng Yang for providing the Chl-a data and Zhiqiang Liu for providing the wind data in the YRE. We thank Kerstin Nachtigall, Andre Mutzberg, Lifang Wang, Biyan He, Wei Qian, Weidong Zhai, Pengfei Liu, and Gila Merschel for their assistance in sampling and/or analysis. We also thank Paul Treguer, Christina De La Rocha, and Shaily Rahman for providing helpful discussion. We would like to thank Damien Cardinal, Gregory de Souza, and two anonymous reviewers for their constructive comments on the manuscript.	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Cosmochim. Acta	MAR 15	2020	273						367	382		10.1016/j.gca.2020.01.028	http://dx.doi.org/10.1016/j.gca.2020.01.028			16	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	KN4TY		Green Accepted			2023-06-23	WOS:000514832600021
J	Santos, DC; Souza, PWM; Nascimento, WR; Cardoso, GF; dos Santos, JF				Santos, Diogo Correa; Martins Souza-Filho, Pedro Walfir; Nascimento Jr, Wilson Rocha; Cardoso, Gustavo Freitas; dos Santos, Jorge Filipe			Land cover change, landscape degradation, and restoration along a railway line in the Amazon biome, Brazil	LAND DEGRADATION & DEVELOPMENT			English	Article						Brazil; Carajas; iron ore mining; LANDSAT; remote sensing	ESTIMATING AREA; DEFORESTATION; ACCURACY; SATELLITE; RONDONIA; CLASSIFICATIONS; CALIBRATION; SETTLEMENT; IMPACTS; TRANSIT	Railways are known to have less influence on land use than other transportation systems. However, railways also affect biodiversity, water resources, socioeconomic outcomes, and land prices. In the context of changes in land cover and land use (LCLU) classes, this study analyses the changes arising from the establishment of the Carajas Mining Project in 1984 along the more than 900-km length of the Carajas Railway (CRW) in southeastern Amazonia. LANDSAT-5 (1984) and LANDSAT-8 (2014) satellite images and human settlement layers (1990 and 2015) along CRW were used to assess LCLU changes. Satellite images were analysed with the geographic object-based image analysis method to detect changes in LCLU classes, including municipalities located less than 50 km from the CRW. The results showed that in 1984, the areas of influence of the CRW consisted of 69% forest cover, 24% nonforest cover, 3% water, and 2% cloud cover. In 2014, forest area dropped significantly to 43%, whereas the nonforest class expanded to 46%. This analysis revealed that the conversion of forests to pastures represents the major landscape degradation that occupy 51% of the study site mainly in rural human settlement areas, which are interlinked with the construction of the CRW. Only 6% of the total area exhibits a trend of restoration marked by secondary vegetation growing. The land occupation model along the CRW is characterized by rural settlements, associated with roads and extensive pasturelands. Construction of this railway in a certain way prevented the fishbone occupation type as observed in the western Amazon.	[Santos, Diogo Correa; Martins Souza-Filho, Pedro Walfir; Nascimento Jr, Wilson Rocha; dos Santos, Jorge Filipe] Inst Technol Vale, Rua Boaventura da Silva, BR-66055090 Belem, Para, Brazil; [Martins Souza-Filho, Pedro Walfir] Univ Fed Para, Geosci Inst, Av Augusto Correa 1, Belem, Para, Brazil; [Cardoso, Gustavo Freitas] Fundacao Florestal, Protected Area, Av Prof Frederico Hermann Junior 345, Sao Paulo, SP, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Universidade Federal do Para	Souza, PWM (autor correspondente), Inst Technol Vale, Rua Boaventura da Silva, BR-66055090 Belem, Para, Brazil.	pedro.martins.souza@itv.org	dos Santos, Jorge Filipe/A-8104-2019; Souza, Pedro/GZH-1275-2022; Souza-Filho, Pedro Walfir M. M./J-4958-2012	dos Santos, Jorge Filipe/0000-0002-0737-8837; Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; Santos, Diogo/0000-0003-1828-3910	Brazilian National Council for Research and Development - CNPq [380481/2018-9]	Brazilian National Council for Research and Development - CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Brazilian National Council for Research and Development - CNPq, Grant/Award Number: 380481/2018-9	Aldrich S, 2012, ANN ASSOC AM GEOGR, V102, P103, DOI 10.1080/00045608.2011.620501; Alvares CA, 2013, METEOROL Z, V22, P711, DOI 10.1127/0941-2948/2013/0507; [Anonymous], 2004, AM J TRANSPLANT S7, V4, pS7; Araujo E., 2017, REV AMAZONIA LEGAL E; Baatz M., 2000, ANGEW GEOGRAPHISCHE, V12, P12, DOI DOI 10.3390/RS5010183; Barber CP, 2014, BIOL CONSERV, V177, P203, DOI 10.1016/j.biocon.2014.07.004; Batunacun, 2018, LAND DEGRAD DEV, V29, P1595, DOI 10.1002/ldr.2948; Blaschke T, 2014, ISPRS J PHOTOGRAMM, V87, P180, DOI 10.1016/j.isprsjprs.2013.09.014; BrandAo Jr A, 2017, EMISSOES SETOR MUDAN; Calvo FJ, 2013, TRANSPORT RES REC, P82, DOI 10.3141/2353-08; Castells M, 2005, NETWORK SOC KNOWLEDG; Coe MT, 2013, PHILOS T R SOC B, V368, DOI 10.1098/rstb.2012.0155; Congalton R. 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J	Barbosa, ESR; Brod, JA; Cordeiro, PFO; Junqueira-Brod, TC; Santos, RV; Dantas, EL				Rocha Barbosa, Elisa Soares; Brod, Jose Affonso; Oliveira Cordeiro, Pedro Filipe; Junqueira-Brod, Tereza Cristina; Santos, Roberto Ventura; Dantas, Elton Luiz			Phoscorites of the Salitre I complex: Origin and petrogenetic implications	CHEMICAL GEOLOGY			English	Article						Phoscorites; Carbonatite; APIP; Kamafugite-carbonatite association; Mineral chemistry	ALKALINE-CARBONATITE COMPLEX; PARANAIBA IGNEOUS PROVINCE; FE-TI OXIDES; LA-ICP-MS; KOLA-PENINSULA; COMPOSITIONAL VARIATION; MINERAL-CHEMISTRY; MANTLE PLUME; LIQUID IMMISCIBILITY; TURIY MASSIF	The Salitre I complex is a kidney-shaped alkaline-carbonatite-phoscorite complex part of the Late Cretaceous Alto Paranaiba Igneous Province, central Brazil. This complex is a key example where the phoscorite-carbonatite association was preserved from metasomatism by late-stage fluids and, thus, provides an opportunity to address the genesis of phoscorites. Salitre I is composed of two main coalescing intrusions: a) a northern one dominantly containing perovskite bebedourites (B1), with swarms of ring dykes of carbonatites and phoscorites and, b) a southern one containing melanite bebedourites (B2). Salitre I phoscorites can be subdivided into P1 and P2 based on modal abundance, mineral texture, chemistry and mode of emplacement. P1 phoscorites contain essential olivine, phlogopite and apatite, with accessory magnetite and traces of perovskite whereas P2 phoscorites are composed of the same essential phases but also contain carbonate-rich pockets, accessory pyrochlore and rare phlogopite. Carbonate C-O isotopes and whole-rock Sr-Nd show that Salitre I phoscorites crystallized from mantle-derived parental magmas, similar to other APIP carbonatite complexes. However, chemical and textural discrepancies between P1 and P2 suggest derivation from different magma sources and through distinct processes. For instance, P1 Al- and Ti-rich phlogopite, accessory perovskite and general trace element geochemical behaviour can be associated with the evolution of B1 perovskite bebedourites, i.e. genesis through fractional crystallization from a bebedourite magma. P2 phoscorites, on the other hand, have their evolution linked to a magmatic phase that underwent melt immiscibility, as suggested by trace element fractionation. Additionally, P2 contains pyrochlore, which is generally lacking in bebedourites. Therefore, whereas P1 phoscorites might have derived from a bebedourite magma, P2 phoscorites were generated from a carbonated magma enriched in phosphate and iron oxides.	[Rocha Barbosa, Elisa Soares; Brod, Jose Affonso; Junqueira-Brod, Tereza Cristina] Univ Fed Goias FCT UFG, Fac Ciencias & Tecnol, BR-74968755 Aparecida De Goiania, Go, Brazil; [Rocha Barbosa, Elisa Soares; Brod, Jose Affonso; Santos, Roberto Ventura; Dantas, Elton Luiz] Univ Brasilia IG UnB, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Oliveira Cordeiro, Pedro Filipe] Pontificia Univ Catolica Chile UC, Dept Ingn Mineria, Santiago, Chile; [Rocha Barbosa, Elisa Soares; Brod, Jose Affonso; Oliveira Cordeiro, Pedro Filipe; Junqueira-Brod, Tereza Cristina; Santos, Roberto Ventura; Dantas, Elton Luiz] CNPq Conselho Nacl Desenvolvimento Cient & Tecnol, Brasilia, DF, Brazil		Cordeiro, PFO (autor correspondente), Pontificia Univ Catolica Chile UC, Dept Ingn Mineria, Santiago, Chile.	pedro.cordeiro@ing.puc.cl	Brod, Jose/AAL-2913-2021; Dantas, Elton Luiz/AAK-8464-2021; Cordeiro, Pedro/E-3044-2017	Brod, Jose/0000-0002-4265-2571; Dantas, Elton Luiz/0000-0002-7954-5059; Cordeiro, Pedro/0000-0003-1996-9551	CNPq - Brazilian Council for Research and Development	CNPq - Brazilian Council for Research and Development(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the CNPq - Brazilian Council for Research and Development for Ph.D. grants to E.S.R.B. and P.F.O.C., research grants to J.A.B., T.C.J.B., E.L.D. and R.V.S., and financial support for the project. The University of Brasilia is thanked for access to analytical facilities, as is Fosfertil S/A for access and permission to sample the Salitre I drill cores. Professor S. Vlach and the University of Sao Paulo are thanked for their assistance with additional microprobe analyzes. Professors C. G. Oliveira, C. F. Ferreira Filho, and N. F. Botelho at the University of Brasilia are thanked for their review and discussions on an earlier version of this manuscript. Finally, Dr. K.M. Goodenough and an anonymous reviewer are thanked for their peer-review of this manuscript submission to Chemical Geology.	Almeida F. F. 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Geol.	MAR 5	2020	535								119463	10.1016/j.chemgeo.2020.119463	http://dx.doi.org/10.1016/j.chemgeo.2020.119463			18	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	KK7HD					2023-06-23	WOS:000512908800007
J	Teixeira, SS; Dall'Agnol, R; Sahoo, PK; Salomao, GN; Guimaraes, JTF; Costa, M				Teixeira, Sanderson Silva; Dall'Agnol, Roberto; Sahoo, Prafulla Kumar; Salomao, Gabriel Negreiros; Guimaraes, Jose Tasso Felix; Costa, Marlene			Water chemistry and estimation of background levels of elements in surface water bodies from a protected area in the vicinity of Fe deposits, Southeastern Amazon	ENVIRONMENTAL FORENSICS			English	Article						Water quality; baseline threshold values; iron mines; Serra dos Carajas; Carajas National Forest	HUMIC SUBSTANCES; RIVER-BASIN; LAND-USE; IRON; THRESHOLD; MANGANESE; DEFORESTATION; SEDIMENTS; BEHAVIOR; CARAJAS	This paper aimed to provide the knowledge of water chemistry and quality and background values of the elements in surface waters around the Fe-ore deposits of N3 and N4WSul of Serra dos Carajas, Brazil. Water samples were collected from 17 monitoring points monthly/quarterly between 2013 and 2016 and the elemental analyses were carried out using Inductively Coupled Plasma Mass Spectrometry (ICP-MS). The waters are slightly acidic to slightly alkaline in nature and are classified into "good" and "optimum" water quality category. Seasonal variation impacted water quality, with significantly higher content of metals (such as Fe-d, Fe-t, and Al-d) during the rainy period that is due to more intense surface-runoff and leaching. Comparing with CONAMA 357/05/WHO limits, nonconformities were mainly observed for pH, Fe and Mn, and in some cases for Al-d, Zn-t, Cu-d, Cd-t and Zn-t, and were significantly higher in the N4WSul area than in the N3. Although, Fe and Mn mostly enter the water bodies from catchment weathering, the poor correlation between Fe and Mn indicated that their source and transport processes are different. In fact, elevated Mn-d concentrations associated with low DO content in the dry period are explained by a reductive dissolution of manganese oxides via bacterial decomposition of OM. The background threshold values (BTVs) of elements were estimated by the upper 95% simultaneous limit (USL95; using ProUCL software) and the median +/- 2 Median Absolute Deviation (mMAD) method, while the former was considered as the most suitable method for defining BTVs. The BTVs for Al(d), Fe (d), Mn and Zn are mostly exceeding the maximum limits stipulated by the legislation. However, since these areas are located in a protected region, these values are seen as representative of the natural conditions of the study area and reflect geogenic influence.	[Teixeira, Sanderson Silva; Dall'Agnol, Roberto; Guimaraes, Jose Tasso Felix] ITV, Curso Mestrado Profiss Uso Sustentavel Recursos N, Belem, Para, Brazil; [Teixeira, Sanderson Silva; Costa, Marlene] Vale, Diretoria Ferrosos Norte, Nucleo Urbano Carajas, Gerencia Meio Ambiente, Parauapebas, Brazil; [Dall'Agnol, Roberto; Sahoo, Prafulla Kumar; Salomao, Gabriel Negreiros; Guimaraes, Jose Tasso Felix] ITV, Belem, Para, Brazil; [Sahoo, Prafulla Kumar] Cent Univ Punjab, Dept Environm Sci & Technol, Bathinda, India; [Salomao, Gabriel Negreiros] Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, Belem, Para, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Instituto Tecnologico Vale Desenvolvimento Sustentavel; Central University of Punjab; Universidade Federal do Para	Sahoo, PK (autor correspondente), ITV, Curso Mestrado Profiss Uso Sustentavel Recursos N, Belem, Para, Brazil.	prafulla.sahoo@itv.org	Sahoo, Prafulla/N-5100-2018; Guimarães, José Tasso Felix/D-2079-2013	Sahoo, Prafulla/0000-0003-3481-1787; Guimarães, José Tasso Felix/0000-0002-5772-5104; Negreiros Salomao, Gabriel/0000-0003-3729-7840	Vale; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [306.108/2014-3, 443.247/2015-3, 402727/2018-5, 380998/2019-0, 202864/2019-7]; National Forest of Carajas [SISBIO 35594-2]	Vale; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); National Forest of Carajas	We would like to acknowledge the financial support and field assistance provided by Vale. RD was supported by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [grant 306.108/2014-3, and 443.247/2015-3 and 402727/2018-5 projects with DTI scholarships to GNS, 380998/2019-0 and 202864/2019-7]. This project was carried out in the National Forest of Carajas under permission of IBAMA (SISBIO 35594-2).	Abouhend A. 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Forensics	APR 2	2020	21	2					176	194		10.1080/15275922.2020.1728436	http://dx.doi.org/10.1080/15275922.2020.1728436		MAR 2020	19	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	LK7IQ					2023-06-23	WOS:000518814100001
J	Beri, A; Martinez-Blanco, X; Varela, L; di Pasquo, M; de Souza, PA				Beri, Angeles; Martinez-Blanco, Ximena; Varela, Luciano; di Pasquo, Mercedes; de Souza, Paulo Alves			Sampling biases and Paleozoic sporomorphs diversity dynamics in Western Gondwana strata	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Sporomorphs; Diversity; Sampling; Gondwana; Extinction; Fossil record	GRANDE-DO-SUL; CARBONIFEROUS ITARARE SUBGROUP; RIO BONITO FORMATION; ASH FALL DEPOSITS; PARANA BASIN; SALTA PROVINCE; TAXONOMIC DIVERSITY; PLANT DIVERSITY; SOUTH-AMERICA; FOSSIL RECORD	A dataset consisting of presence-absence data of 137 pollen and spore genera was elaborated with published sources from Pennsylvanian and Permian Atlantic (Parana, Parnaiba, Amazonas, and Claromeco) and Pacific (Paganzo, Tarija, and Madre de Dios) basins of South America. The richness and origination, extinction, and sampling rates of sporomorphs were analyzed in order to address the effect of sampling biases over diversity estimations. Richness and sampling were estimated using the recently developed True Richness estimated using a Poisson Sampling (TRiPS) model. Origination, extinction, and sampling rates were estimated with Inverse Survivorship Models. The TRiPS analysis showed changes in richness during the studied interval. The highest richness was observed for the Cisuralian, and the lowest richness was recovered for the Pennsylvanian and Guadalupian. The best supported Inverse Survivorship Model revealed that the highest origination values occurred between the Gzhelian and Asselian, whereas the highest observed extinction rate occurred between the Kungurian and the Roadian. In particular, pollen grains showed higher net diversification than spores, while spores showed higher turnover than pollen grains. Also, an alternation in richness dominance was observed at the beginning of the Permian, with pollen grains showing higher richness after the Artinskian. Changes in total sporomorphs diversity, as well as differences between spores and pollen grains, may be related to changing climatic conditions in Western Gondwana during the late Paleozoic (from icehouse to greenhouse conditions) that could impact differently over plant communities. Although the fossil palynomorph record has been widely used as a biostratigraphic tool, our results highlight its importance and usefulness for the study of plant communities and their evolution in the past.	[Beri, Angeles; Martinez-Blanco, Ximena; Varela, Luciano] UdelaR, Dept Paleontol, Fac Ciencias, Igua 4225, Montevideo 11400, Uruguay; [di Pasquo, Mercedes] Consejo Nacl Invest Cient & Tecn, CICYTTR, Lab Palinoestratig & Paleobot, ER,UADER, CP E3105BWA, Entre Rios, Argentina; [de Souza, Paulo Alves] Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil	Universidad de la Republica, Uruguay; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidade Federal do Rio Grande do Sul	Beri, A (autor correspondente), UdelaR, Dept Paleontol, Fac Ciencias, Igua 4225, Montevideo 11400, Uruguay.	beri@fcien.edu.uy; ximenamblanco@gmail.com; luciano.lvr@gmail.com; medipa@cicyttp.org.ar; paulo.alves.souza@ufrgs.br	Varela, Luciano/R-2111-2018; Alves de Souza, Paulo/O-9779-2018	Varela, Luciano/0000-0002-9481-6558; Martinez-Blanco, Ximena/0000-0003-1516-7826; Alves de Souza, Paulo/0000-0001-9844-1530; di Pasquo, Mercedes/0000-0003-3068-0089	Comision Sectorial de Investigacion Cientifica (CSIC), Uruguay [project CSIC I + D 2014] [65]; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET), Argentina [PIP 0812/2015-2017]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), Brazil [313340/2018-8]; Brazilian Scientific Mobility Program "Ciencia sem Fronteiras" (2013)	Comision Sectorial de Investigacion Cientifica (CSIC), Uruguay [project CSIC I + D 2014]; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET), Argentina(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Brazilian Scientific Mobility Program "Ciencia sem Fronteiras" (2013)	This work was supported by the Comision Sectorial de Investigacion Cientifica (CSIC), Uruguay [project CSIC I + D 2014 ID 65], Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET), Argentina [project PIP 0812/2015-2017], Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), Brazil [project 313340/2018-8], and the Brazilian Scientific Mobility Program "Ciencia sem Fronteiras" (2013).	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J	Cecilio, RO; Dillenburg, SR				Cecilio, R. O.; Dillenburg, S. R.			An ocean wind-wave climatology for the Southern Brazilian Shelf. Part I: Problem presentation and model validation	DYNAMICS OF ATMOSPHERES AND OCEANS			English	Article						Wave modeling; Model validation; Nested grids; Bottom friction; WW3; SWAN	COASTAL REGIONS; IMPLEMENTATION; HINDCAST; ENERGY; SYSTEM	Geomorphological features and sparse visual wave measurements, presented in previous works, point out to the possible existence of alongshore wave energy gradients over the Southern Brazilian Shelf (SBS). After describing the two numerical models utilized and the model grids and settings, the present study evaluated the proposed validation of the basin-scale results against orbital altimetry and the regional-scale results against the two available wave-buoy data, discussing the extent to which the model reproduced local reality. The basin-scale model results of significant wave height could be considered as in good agreement with observations, presenting remarkable similarities with observed altimetry. Regarding the regional-scale modeling, both significant wave height and peak wave periods were considered as in good agreement with observations. The peak wave directions, however, were classified as in poor agreement, once the ESE waves were erroneously reproduced as E. Increased spatial resolution certainly played a role, but it was the lowering of bottom friction that represented the major improvement in the coastal grid simulations.	[Cecilio, R. O.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Porto Alegre, RS, Brazil; [Dillenburg, S. R.] Univ Fed Rio Grande do Sul, Ctr Escudos Geoi Costeira & Ocean, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Cecilio, RO (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Porto Alegre, RS, Brazil.	rececilio@gmail.com	Dillenburg, Sergio/C-4027-2013	Dillenburg, Sergio/0000-0003-0072-7018	Brazilian Research Council (CNPq - Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)	Brazilian Research Council (CNPq - Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors acknowledge the Brazilian Research Council (CNPq - Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) for the first author's Doctoral Studentship and for the Research Fellowship granted to Dr. Sergio Dillenburg.	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Atmos. Oceans	MAR	2020	89								101101	10.1016/j.dynatmoce.2019.101101	http://dx.doi.org/10.1016/j.dynatmoce.2019.101101			15	Geochemistry & Geophysics; Meteorology & Atmospheric Sciences; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics; Meteorology & Atmospheric Sciences; Oceanography	KW9PH					2023-06-23	WOS:000521515100001
J	D'Agrella, MS; Teixeira, W; da Trindade, RIF; Patroni, OAL; Prieto, RF				D'Agrella-Filho, Manoel S.; Teixeira, Wilson; da Trindade, Ricardo I. F.; Patroni, Oscar A. L.; Prieto, Raphael F.			Paleomagnetism of 1.79 Ga Para de Minas mafic dykes: Testing a Sao Francisco/Congo-North China-Rio de la Plata connection in Columbia	PRECAMBRIAN RESEARCH			English	Article						Paleomagnetism; Para de Minas dykes; Amazonian Craton; Columbia/Nuna	U-PB GEOCHRONOLOGY; PALEO-MESOPROTEROZOIC SUPERCONTINENT; ID-TIMS BADDELEYITE; CRATON EVIDENCE; CRUSTAL GROWTH; CENTRAL BRAZIL; PALEOPROTEROZOIC CRUST; TECTONIC CORRELATION; GEOMAGNETIC-FIELD; MAGNETIC FABRICS	Paleogeographic connections between Sao Francisco/Congo, North China and Rio de la Plata Cratons through the Paleoproterozoic have been proposed on the basis of geological and paleomagnetic data. We conducted new paleomagnetic analyses for mafic dykes of the 1790 Ma Para de Minas swarm, occurring in the southern Sao Francisco Craton. The data revealed south/southwestern, low inclination magnetic directions after alternating field (AF) and thermal demagnetization, providing a paleomagnetic pole at 39.8 degrees S, 196.8 degrees E (A(9S) = 17.0 degrees). The characteristic remanent magnetization is interpreted as a thermo-remanent magnetization carried by stable 'pseudo-single domain' magnetite grains, being acquired during the cooling of the dykes at 1790 Ma, as attested by a positive baked contact test performed on one of the dykes. The new pole in conjunction with 1790-1750 Ma paleomagnetic poles available for other blocks allowed an improved reconstruction of Columbia/Nuna supercontinent at this time frame. Laurentia, Baltica, Siberia, proto-Amazonia, West Africa and proto-Australia were positioned as in previously proposed models. The main difference from our reconstruction concerns the link of the Sao Francisco/Congo, North China and Rio de la Plata cratons, implying that much of the Columbia supercontinent had already agglutinated around 1850-1800 Ma ago. This configuration is consistent with the onset of eventual taphrogenic episodes over most blocks, accompanied by the emplacement of mafic dyke swarms and granitic intrusions at 1790-1750 Ma.	[D'Agrella-Filho, Manoel S.; da Trindade, Ricardo I. F.; Patroni, Oscar A. L.; Prieto, Raphael F.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Rua Metao 1226, BR-05508090 Sao Paulo, SP, Brazil; [Teixeira, Wilson] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil	Universidade de Sao Paulo; Universidade de Sao Paulo	D'Agrella, MS (autor correspondente), Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Rua Metao 1226, BR-05508090 Sao Paulo, SP, Brazil.	dagrella@iag.usp.br	Trindade, Ricardo IF/A-8146-2008; D'Agrella-Filho, Manoel Souza/C-5169-2013; Teixeira, Wilson/B-7570-2013	Trindade, Ricardo IF/0000-0001-9848-9550; D'Agrella-Filho, Manoel Souza/0000-0003-2135-9007; Teixeira, Wilson/0000-0003-1578-6846	CNPq [303130/2014-8]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank CNPq research fellowship to M. S. D'Agrella-Filho (303130/2014-8). We thank Augusto Rapalini and an anonymous reviewer for their comments that greatly improved the manuscript.	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Zijderveld J.D.A, 1967, METHODS PALAEOMAGNET, P254, DOI DOI 10.1016/B978-1-4832-2894-5.50049-5	113	20	20	1	7	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0301-9268	1872-7433		PRECAMBRIAN RES	Precambrian Res.	MAR	2020	338								105584	10.1016/j.precamres.2019.105584	http://dx.doi.org/10.1016/j.precamres.2019.105584			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KO3EY					2023-06-23	WOS:000515431900008
J	da Costa, RV; Trouw, RAJ; Marimon, RS; Nepomuceno, F; Mendes, JC; Dantas, E				da Costa, Rodrigo Vinagre; Johannes Trouw, Rudolph Allard; Marimon, Rodrigo Schwantes; Nepomuceno, Felipe; Mendes, Julio Cezar; Dantas, Elton			Sao Bento do Sapucai Shear Zone: Constraining age and P-T conditions of a collisional Neoproterozoic oblique shear zone, Ribeira Orogen, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Sao Bento do Sapucai Shear Zone; Structural geology; Metamorphism; Geochronology; Ribeira orogen	SOUTHERN BRASILIA OROGEN; PLASMA-MASS SPECTROMETRY; U-PB; SE-BRAZIL; NAPPE SYSTEM; PREFERRED ORIENTATIONS; TECTONIC EVOLUTION; INTERFERENCE ZONE; FAULT ZONE; BELT	The Sao Bento do Sapucai Shear Zone is a subvertical NE-SW anastomosing shear zone of at least 100 km length and few km wide. It affects orthogneisses, paragneisses and igneous rocks of the Socorro-Guaxupe Nappe, the uppermost nappe of a nappe stack, which constitutes the Southern Brasilia Orogen, part of a Neoproterozoic orogenic system surrounding the Sao Francisco Craton. The Socorro-Guaxupe Nappe is interpreted as the root of a magmatic arc. The nappe stack is partly affected by superposed deformation related to the slightly younger Ribeira Orogen. The mylonitic foliation of the shear zone dips steeply to both SE and NW, and contains a stretching lineation with shallow plunge predominantly to NE and locally to SW. Kinematic indicators including sigma and delta objects, asymmetric mica fish and synthetic shear bands point to oblique dextral movement with a SE-up component. Evidence of quartz and feldspar recrystallization-mechanisms was applied to estimate temperature during mylonitization as between 450 degrees C and 650 degrees C. The geothermobarometry calculated from the composition of mineral rims, partially or fully recrystallized during mylonitization, yielded a temperature of 479 +/- 66 degrees C and a pressure of 2.94 +/- 1.56 kbar. Geochronological investigation by LA-ICP-MS of U-Pb in zircon and monazite was applied in order to constrain the age of rocks which were affected by, or cross-cut the shear zone. Metamorphic rims on detrital zircon grains collected from a paragneiss indicate a main metamorphic episode at ca. 613 Ma. Analysis of a gabbronorite affected by the shear zone yielded a crystallization age of ca. 610 Ma; a pegmatitic leucogranite which cross-cuts the shear zone, produced various zircon ages between 656 and 611 Ma, interpreted as inheritance. Monazite crystals of the same leucogranite yielded an age of 552 Ma, interpreted as the age of crystallization. Hence the age of the shear zone is constrained between 610 and 552 Ma. The data produced in this study fit well the proposed evolutionary history of the Socorro-Guaxupe Nappe, where a magmatic arc developed between 680 and 630 Ma, followed by continental collision and associated metamorphism ranging from 630 to 600 Ma. The younger shear zone is related to the tectonics of the superimposed Ribeira Orogen in the time span 600-560 Ma.	[da Costa, Rodrigo Vinagre; Johannes Trouw, Rudolph Allard; Marimon, Rodrigo Schwantes; Nepomuceno, Felipe; Mendes, Julio Cezar] Univ Fed Rio de Janeiro, Dept Geol, IGEO, Rio De Janeiro, RJ, Brazil; [Dantas, Elton] Univ Brasilia, Inst Geosci, Lab Geochronol, Brasilia, DF, Brazil	Universidade Federal do Rio de Janeiro; Universidade de Brasilia	da Costa, RV (autor correspondente), Av Athos da Silveira Ramos 274,Room J2-24, BR-21941916 Rio De Janeiro, RJ, Brazil.	rodrigogeologo@yahoo.com.br	Marimon, Rodrigo Schwantes/AAB-5863-2021; Dantas, Elton Luiz/AAK-8464-2021	Dantas, Elton Luiz/0000-0002-7954-5059; Schwantes Marimon, Rodrigo/0000-0001-6157-8031; Nepomuceno, Felipe/0000-0001-9445-9530	Brazilian Research Council (CNPq)	Brazilian Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The Brazilian Research Council (CNPq) is acknowledged for research grants and for financial support. 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South Am. Earth Sci.	MAR	2020	98								102418	10.1016/j.jsames.2019.102418	http://dx.doi.org/10.1016/j.jsames.2019.102418			26	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KR5NJ					2023-06-23	WOS:000517664800002
J	do Amarante, FB; Kuchle, J; Iacopini, D; Scherer, CMD; Alvarenga, RD; Ene, PL; Schilling, AB				do Amarante, Francyne Bochi; Kuchle, Juliano; Iacopini, David; dos Santos Scherer, Claiton Marlon; Alvarenga, Renata dos Santos; Ene, Patrycia Leipnitz; Schilling, Andre Basso			Seismic tectono-stratigraphic analysis of the Aptian pre-salt marginal system of Espirito Santo Basin, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Pre-salt; South Atlantic; SE Brazil; Sag basin; Seismostratigraphy	LACUSTRINE CARBONATE RESERVOIRS; NORTHERN CAMPOS BASIN; RIFT; STRATIGRAPHY; TECTONICS	The Aptian sedimentary sequence of Mucuri Member, lower Mariricu Formation, constitutes the pre-salt of Espirito Santo Basin. Proximal successions are dominantly clastic consisting of fluvial and coastal sediments deposited within the margins of a wide lake, thus corresponding to the marginal deposits of lacustrine carbonate reservoirs located in distal portions of the basin. Economic interest for oil is centered on such distal reservoirs, consequently proximal sections lack detailed studies. The Espirito Santo Basin is located near pre-salt official polygon, with oil exploration active for over six decades. The main objective of this study is the tectono-stratigraphic analysis of the clastic Mucuri Member, Aptian sag succession of the Espirito Santo Basin. Leading methodology is a seismostratigraphic characterization based on 220 2D lines, 1 3D volume, 103 well log data and 1 cored well. Four seismostratigraphic units were identified, delimited by three conformable horizons. Unitbounding reflectors coincide with gamma ray maxima or minima interpreted to reflect shale or anhydrites deposited in deep water environments, corresponding to lacustrine maximum flooding surfaces. The structural framework is characterized by minor faults in the north onto shallow basement platforms, and in the south by half-graben bounded by normal faults developed during the rift phase. The Mucuri Member records an enlargement in depositional area from its base to top unit witnessing an overall lacustrine base level rise during depositon. The geometry of depositional area was initially influenced by the paleorelief of the preceding rift basins. The seismic units record a decrease in thickness as remnant topography was gradually filled and the upper units extended beyond the rift boundaries, covering a larger area. The Early Cretaceous Mucuri Member composes the first post-rift sequence of Espirito Santo Basin marked by the cessation of fault activity and the onset of thermal subsidence.	[do Amarante, Francyne Bochi; Kuchle, Juliano; dos Santos Scherer, Claiton Marlon; Alvarenga, Renata dos Santos; Ene, Patrycia Leipnitz; Schilling, Andre Basso] Univ Fed Rio Grande Do Sul, Inst Geociencias, Agron, 9500 Bento Goncalves Ave,Bldg 43137, BR-91501970 Porto Alegre, RS, Brazil; [Iacopini, David] Univ Aberdeen, Sch Geosci, Aberdeen, Scotland; [Iacopini, David] Univ Napoli Federico II, Dipartimento Sci Terra Ambiente & Risorse DiSTAR, Naples, Italy	Universidade Federal do Rio Grande do Sul; RLUK- Research Libraries UK; University of Aberdeen; University of Naples Federico II	do Amarante, FB (autor correspondente), Univ Fed Rio Grande Do Sul, Inst Geociencias, Agron, 9500 Bento Goncalves Ave,Bldg 43137, BR-91501970 Porto Alegre, RS, Brazil.	francyne.amarante@ufrgs.br	Iacopini, David/AAK-9414-2020; Amarante, Francyne/AAO-7294-2020	Iacopini, David/0000-0003-4925-9665; Amarante, Francyne/0000-0003-4452-8635; Santos Scherer, Claiton Marlon dos/0000-0002-7520-1187	CNPq (National Council for Scientific and Technological Development of Brazil); Shell Brasil Petroleo Ltda; ANP (Brazil's National Oil, Natural Gas and Biofuels Agency)	CNPq (National Council for Scientific and Technological Development of Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Shell Brasil Petroleo Ltda; ANP (Brazil's National Oil, Natural Gas and Biofuels Agency)	F.B.D. Amarante thanks CNPq (National Council for Scientific and Technological Development of Brazil) for the doctorate scholarship. The authors gratefully acknowledge support from Shell Brasil Petroleo Ltda and the strategic importance of the support given by ANP (Brazil's National Oil, Natural Gas and Biofuels Agency) through the R&D levy regulation. Special thanks to Leo A. Hartmann for valuable suggestions and revision of the manuscript. The authors are very grateful to Gonzalo Zamora and the anonymous reviewer for their constructive comments.	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South Am. Earth Sci.	MAR	2020	98								102474	10.1016/j.jsames.2019.102474	http://dx.doi.org/10.1016/j.jsames.2019.102474			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KR5NJ					2023-06-23	WOS:000517664800031
J	Ernesto, M; Demarco, PN; Xavier, P; Sanchez, L; Schultz, C; Pineiro, G				Ernesto, Marcia; Nunez Demarco, Pablo; Xavier, Pedro; Sanchez, Leda; Schultz, Cesar; Pineiro, Graciela			Age constraints on the Paleozoic Yaguari-Buena Vista succession from Uruguay: paleomagnetic and paleontologic information	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Yaguarf-buena vista succession; Paleomagnetism; Paleontology; Late paleozoic; Uruguay	PERMIAN MASS EXTINCTION; ASH FALL DEPOSITS; PARANA BASIN; TRIASSIC BOUNDARY; ZIRCON GEOCHRONOLOGY; SOUTH-AFRICA; BRAZIL; TEMNOSPONDYL; PROVINCE; SANGA	The Yaguarf and the Buena Vista formations from Uruguay are historically correlated to the Brazilian Rio do Rasto and Sanga do Cabral formations, respectively, as they have some lithostratigraphic similarities, indicating a Permo-Triassic or even Triassic age of the Yaguarf-Buena Vista succession. However, they differ in the fossil indexes that characterize the faunistic communities present in both countries. A paleomagnetic work was carried out on some sections of the Buena Vista and the Yaguarf formations, as well as on some layers of bentonites, underlying the Buena Vista sediments. The alternating field and thermal demagnetization procedures revealed both normal and reversed magnetization components, but the samples showed evidence of secondary magnetic minerals and possibly remagnetizations. The calculated paleomagnetic pole for the Yaguari-Buena Vista Formation plots near to the poles for the Choiyoi magmatism that is believed to be responsible for the bentonite accumulation, it is also in agreement with other Permian paleomagnetic poles for South America. Based on the paleomagnetic results, the available radiometric data for the bentonites, and the fossiliferous content, a Late Permian (Lopingian) age is assigned to the Yaguarf-Buena Vista rocks.	[Ernesto, Marcia] Univ Sao Paulo, Inst Astronom Geofis & Ciencias Atmosfericas, Sao Paulo, Brazil; [Nunez Demarco, Pablo; Sanchez, Leda] Fac Ciencias, Inst Ciencias Geol, Igua 4225, Montevideo 11400, Uruguay; [Xavier, Pedro; Schultz, Cesar] Univ Fed Rio Grande do Sul, Dept Estratigraf & Paleontol, Porto Alegre, RS, Brazil; [Pineiro, Graciela] Fac Ciencias, Dept Paleontol, Igua 4225, Montevideo 11400, Uruguay	Universidade de Sao Paulo; Universidad de la Republica, Uruguay; Universidade Federal do Rio Grande do Sul; Universidad de la Republica, Uruguay	Ernesto, M (autor correspondente), Univ Sao Paulo, Inst Astronom Geofis & Ciencias Atmosfericas, Sao Paulo, Brazil.	mernesto@usp.br	; Ernesto, Marcia/C-4330-2012	Nunez Demarco, Pablo/0000-0003-4689-7880; Xavier, Pedro Luis/0000-0001-9090-5361; Ernesto, Marcia/0000-0002-7778-9551	CNPq [458187/2014-3, 308475/2015-1]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are indebted to S. Geuna and the other two anonymous reviewers for helping in greatly improving the paper. We also thank Bruno L.D. Horn, Pablo Velozo, Sebastian Marmot and Antonella Celio for their help in the fieldwork and the Family Hastings for their kind hospitality. Funding from CNPq (Grants no 458187/2014-3 and no 308475/2015-1) is also acknowledged.	ABDALA F, 2002, PALAEONTOLOGIA AFRIC, V38, P92; Andreis R.R., 1982, B EXISTENCIA TRIASIC, V5, P1; Andreis R. 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V., 1987, REV BRAS GEOCIENC, V17, P242, DOI DOI 10.25249/0375-7536.1987242252	83	11	11	0	4	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811			J S AM EARTH SCI	J. South Am. Earth Sci.	MAR	2020	98								102489	10.1016/j.jsames.2019.102489	http://dx.doi.org/10.1016/j.jsames.2019.102489			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KR5NJ		Green Published, hybrid			2023-06-23	WOS:000517664800033
J	Ferreira, JM; Rajendran, V; Simonelli, G; Silva, ACM; Santos, LCL; Mattedi, S; Pontes, LAM; Costa, I; Rossi, JL; Baker, MA				Ferreira, J. M.; Rajendran, V.; Simonelli, G.; Silva, A. C. M.; Santos, L. C. L.; Mattedi, S.; Pontes, L. A. M.; Costa, I.; Rossi, J. L.; Baker, M. A.			Deposition and characterization of a sol-gel Mg-substituted fluorapatite coating with new stoichiometries	APPLIED SURFACE SCIENCE			English	Article						Implant; Magnesium; Coating; Fluorapatite; Hydroxyapatite; Sol-gel; Corrosion	COMPOSITE COATINGS; STAINLESS-STEEL; NANOSTRUCTURED HYDROXYAPATITE; SURFACE MODIFICATION; CORROSION BEHAVIOR; 316L SS; IN-SITU; TITANIUM; XPS; MAGNESIUM	The calcium substitution for magnesium on fluorapatite is attractive because this element is a natural substitute in biological apatites. There are several published stoichiometries for calcium substituted by magnesium fluorapatites and most works point out that the formation and fixation of biomimetic Ca-P coatings in Ringer's solution were strongly related to Mg2+ content and furthermore the Mg replacement improves the bioactivity of apatite. In the present study, fluorapatite (FA) and fluorapatite substituted with 6% and 7% of magnesium were obtained by deposition via sol-gel coating on substrates of AISI 316L stainless steel to investigate the effect of magnesium substitution on fluorapatite with not yet investigated stoichiometry. Characterization of coating thickness, chemical composition and crystalline structure was performed using scanning electron microscopy (SEM), X-ray photoelectron spectroscopy (XPS) and X-ray diffraction (XRD). The coating adhesion was evaluated using the pull-out test and the corrosion resistance was undertaken using potentiodynamic polarization and electrochemical impedance spectroscopy (EIS). The electrochemical results showed improvement in the corrosion resistance of magnesium-fluorapatite compared to fluorapatite coated on AISI 316L stainless steel substrates. The improvement corrosion protection and adhesion performance indicate that such magnesium fluorapatites coatings are very interesting candidates as bioactive coatings for implants.	[Ferreira, J. M.; Simonelli, G.; Silva, A. C. M.; Santos, L. C. L.; Mattedi, S.; Pontes, L. A. M.] Univ Fed Bahia, Postgrad Program Chem Engn, Rua Aristides Novis,N 02,2 Andar, BR-40210630 Salvador, Bahia, Brazil; [Rajendran, V.; Baker, M. A.] Univ Surrey, Dept Mech Engn Sci, Room Off 10AB03, Guildford GU2 7XH, Surrey, England; [Costa, I.; Rossi, J. L.] Univ Sao Paulo, Nucl & Energy Res Inst IPEN CNEN SP, Av Prof Lineu Prestes,2242 Butanta, BR-05508000 Sao Paulo, SP, Brazil; [Ferreira, J. M.] Univ Salvador UNIFACS, R Dr Jose Peroba,251 Stiep, BR-41770235 Salvador, BA, Brazil	Universidade Federal da Bahia; University of Surrey; Comissao Nacional de Energia Nuclear (CNEN); Instituto de Pesquisas Energeticas e Nucleares (IPEN); Universidade de Sao Paulo; Universidade Salvador (UNIFACS)	Ferreira, JM (autor correspondente), Univ Fed Bahia, Postgrad Program Chem Engn, Rua Aristides Novis,N 02,2 Andar, BR-40210630 Salvador, Bahia, Brazil.	jmfj@ufb.br; gsimonelli@ufba.br; acristinasilva@ufba.br; lclsantos@ufba.br; uolpontes@uol.com.br; icosta@ipen.br; jelrossi@ipen.br; m.baker@surrey.ac.uk	Ferreira Jr, José Mario/G-4147-2016; Simonelli, George/W-5235-2019; Santos, Luiz Carlos Lobato/F-2805-2013; da Silva, Ana Cristina Morais/AAP-2837-2021; baker, mark A/L-4481-2014; Pontes, Luiz/GXN-0596-2022; Pontesa, Luiz/AAL-1539-2021; Costa, Isolda/E-8506-2012	Ferreira Jr, José Mario/0000-0003-4295-6417; Simonelli, George/0000-0002-8031-1401; Santos, Luiz Carlos Lobato/0000-0003-3824-7802; da Silva, Ana Cristina Morais/0000-0002-3412-5990; baker, mark A/0000-0002-9534-2550; Pontes, Luiz/0000-0003-4158-4033; Costa, Isolda/0000-0002-4987-3334	Royal Academy of Engineering - Newton Research Collaboration, UK [(3)-NRCP1516/1/143]	Royal Academy of Engineering - Newton Research Collaboration, UK	The authors gratefully acknowledge the Royal Academy of Engineering - Newton Research Collaboration, UK, offering the financial support for this work (Newton Research Collaboration Programme (3)-NRCP1516/1/143). To professor John F. Watts and Steve Hinder from the University of Surrey for teaching and help with XPS results.	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Surf. Sci.	MAR 1	2020	505								144393	10.1016/j.apsusc.2019.144393	http://dx.doi.org/10.1016/j.apsusc.2019.144393			13	Chemistry, Physical; Materials Science, Coatings & Films; Physics, Applied; Physics, Condensed Matter	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Materials Science; Physics	KH7RE					2023-06-23	WOS:000510846500041
J	Ferreira, SLC; Pereira, JB; Almeida, LC; Santos, LB; Lemos, VA; Novaes, CG; de Oliveira, OMC; Queiroz, AFS				Ferreira, Sergio L. C.; Pereira Junior, Joao B.; Almeida, Lucas C.; Santos, Luana B.; Lemos, Valfredo A.; Novaes, Cleber G.; de Oliveira, Olivia M. C.; Queiroz, Antonio F. S.			Strategies for inorganic speciation analysis employing spectrometric techniques-Review	MICROCHEMICAL JOURNAL			English	Review							LIQUID-LIQUID MICROEXTRACTION; SOLID-PHASE EXTRACTION; CLOUD POINT EXTRACTION; ATOMIC FLUORESCENCE SPECTROMETRY; PHOTOCHEMICAL VAPOR GENERATION; NATURAL-WATER; SPECTROPHOTOMETRIC DETERMINATION; ABSORPTION-SPECTROMETRY; MAGNETIC NANOPARTICLES; INJECTION-ANALYSIS	This work shows a brief revision of the analytical methods which have been recently developed for speciation studies employing non-chromatographic speciation techniques. Advantages, limitations, and applications of this technique have been discussed, including a comparison to the chromatographic speciation analysis. Additionally, procedures proposed recently for speciation analysis utilizing chemical vapor generation, ion-imprinted polymers, microorganism, selective chemical reactions, and separation techniques have been highlighted, evidencing advantages, and drawbacks. The advantages and applications of the XANES spectroscopy as a technique for speciation analysis are also described.	[Ferreira, Sergio L. C.; Pereira Junior, Joao B.; Almeida, Lucas C.] Univ Fed Bahia, Inst Quim, Grp Pesquisa Quim & Quimiometria, Campus Ondina, BR-40170115 Salvador, BA, Brazil; [Ferreira, Sergio L. C.; Pereira Junior, Joao B.; Almeida, Lucas C.; Santos, Luana B.; Lemos, Valfredo A.; Novaes, Cleber G.] Univ Fed Bahia, Inst Nacl Ciencia & Tecnol, INCT Energia & Ambiente, BR-40170115 Salvador, BA, Brazil; [Santos, Luana B.; Lemos, Valfredo A.; Novaes, Cleber G.] Univ Estadual Sudoeste Bahia, Campus Jequie, BR-45208091 Jequie, BA, Brazil; [de Oliveira, Olivia M. C.; Queiroz, Antonio F. S.] Univ Fed Bahia, Inst Geociencias, Campus Ondina, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Estadual do Sudoeste da Bahia; Universidade Federal da Bahia	Ferreira, SLC (autor correspondente), Univ Fed Bahia, Inst Quim, Grp Pesquisa Quim & Quimiometria, Campus Ondina, BR-40170115 Salvador, BA, Brazil.; Ferreira, SLC; Lemos, VA (autor correspondente), Univ Fed Bahia, Inst Nacl Ciencia & Tecnol, INCT Energia & Ambiente, BR-40170115 Salvador, BA, Brazil.; Lemos, VA (autor correspondente), Univ Estadual Sudoeste Bahia, Campus Jequie, BR-45208091 Jequie, BA, Brazil.; Queiroz, AFS (autor correspondente), Univ Fed Bahia, Inst Geociencias, Campus Ondina, BR-40170115 Salvador, BA, Brazil.	slcf@ufba.br; vlemos@uesb.edu.br; queiroz@ufba.br	Queiroz, Antonio Fernando de Souza/ABH-6682-2020; FERREIRA, SERGIO LUIS SLCF COSTA/I-1993-2013; LEMOS, VALFREDO AZEVEDO/I-7647-2014; Santos, Luana Bastos/ABI-4967-2020; de Oliveira, Olivia Maria Cordeiro/AAB-3246-2021; PEREIRA JUNIOR, JOAO B/J-1487-2016	FERREIRA, SERGIO LUIS SLCF COSTA/0000-0001-7738-045X; LEMOS, VALFREDO AZEVEDO/0000-0002-6029-3218; Santos, Luana Bastos/0000-0002-5063-201X; PEREIRA JUNIOR, JOAO B/0000-0002-7851-8235	Conselho Nacional de Desenvolvimento Cientifico e Tecnologic (CNPq); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologic (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	Authors are grateful to Conselho Nacional de Desenvolvimento Cientifico e Tecnologic (CNPq), to Fundactio de Amparo a Pesquisa do Estado da Bahia (FAPESB) and to Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) Finance Code 001 for providing grants and fellowships and for financial support.	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MAR	2020	153								104402	10.1016/j.microc.2019.104402	http://dx.doi.org/10.1016/j.microc.2019.104402			7	Chemistry, Analytical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	KM5ZR					2023-06-23	WOS:000514218800044
J	Larrovere, MA; de los Hoyos, CR; Willner, AP; Verdecchia, SO; Baldo, EG; Casquet, C; Basei, MA; Hollanda, MH; Rocher, S; Alasino, PH; Moreno, GG				Larrovere, Mariano A.; de los Hoyos, Camilo R.; Willner, Arne P.; Verdecchia, Sebastian O.; Baldo, Edgardo G.; Casquet, Cesar; Basei, Miguel A.; Hollanda, Maria H.; Rocher, Sebastian; Alasino, Pablo H.; Moreno, Gabriel G.			Mid-crustal deformation in a continental margin orogen: structural evolution and timing of the Famatinian Orogeny, NW Argentina	JOURNAL OF THE GEOLOGICAL SOCIETY			English	Article							WESTERN SIERRAS PAMPEANAS; PROTO-ANDEAN MARGIN; TECTONO-METAMORPHIC EVOLUTION; EARLY PALEOZOIC EVOLUTION; DETRITAL ZIRCON AGES; U-PB AGES; SHEAR ZONE; NORTHWESTERN ARGENTINA; SOUTH-AMERICA; VALLE-FERTIL	New structural data from a mid-crustal segment in the Eastern Sierras Pampeanas, coupled with geochronological methods and P-T estimates, reveal polyphase contractional deformation and metamorphism during the Famatinian Orogeny over a long period of time. Peaks of metamorphic monazite and zircon ages are recorded at c. 500 Ma, between 484 and 465 Ma and at c. 440 Ma. Between 484 and 465 Ma the region attained high-temperature (HT) low-pressure (LP) conditions that resulted in widespread partial melting (peak at c. 470 Ma). A contractional phase occurred during this event, as suggested by syn-anatectic structures, as well as folding at subsolidus conditions. Renewed contraction under subsolidus conditions is evidenced by reverse ductile shearing and folding at c. 440 Ma. Thrusting along the La Chilca Shear Zone caused metamorphic inversion. The consistent orientation of folds in the Quebrada del Molle Metamorphic Complex, El Portezuelo MetamorphicIgneous Complex and the La Chilca Shear Zone as well as WSW-directed thrusting at the later shear zone indicate uniform WSW-ENE-directed shortening. This late deformation records the Ocloyic tectonic phase and brought the Famatinian Orogeny to an end in the Late Ordovician to Early Silurian.	[Larrovere, Mariano A.; Alasino, Pablo H.] Prov La Rioja UNLaR SEGEMAR UNCa CONICET, Ctr Reg Invest Cient & Transferencia Tecnol La Ri, Entre Rios & Mendoza S-N, RA-5301 Anillaco, Argentina; [Larrovere, Mariano A.; Rocher, Sebastian; Alasino, Pablo H.] Univ Nacl La Rioja INGeReN CENIIT UNLaR, Ctr Invest & Innovac Tecnol, Inst Geol & Recursos Nat, Avda Gob Vernet & Apostol Felipe, RA-5300 La Rioja, Argentina; [de los Hoyos, Camilo R.] SRK Consulting, Av Juan Domingo Peron 1303, RA-4400 Salta, Argentina; [Willner, Arne P.] Ruhr Univ, Inst Geol Mineral & Geophys, D-44780 Bochum, Germany; [Verdecchia, Sebastian O.; Baldo, Edgardo G.] Univ Nacl Cordoba, Ctr Invest Ciencias Tierra, Consejo Nacl Invest Cient & Tecn CICTERRA CONICET, Haya Torre S-N,Ciudad Univ,X5016, Cordoba, Argentina; [Casquet, Cesar] Univ Complutense, Inst Geociencias CSIC UCM, Dept Petrol & Geoquim, Madrid 28040, Spain; [Basei, Miguel A.; Hollanda, Maria H.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, Brazil; [Moreno, Gabriel G.] Geoconsult, Av Libertador 6550, Buenos Aires, DF, Argentina	Ruhr University Bochum; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of Cordoba; Complutense University of Madrid; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC-UCM - Instituto de Geociencias (IGEO); Universidade de Sao Paulo	Larrovere, MA (autor correspondente), Prov La Rioja UNLaR SEGEMAR UNCa CONICET, Ctr Reg Invest Cient & Transferencia Tecnol La Ri, Entre Rios & Mendoza S-N, RA-5301 Anillaco, Argentina.; Larrovere, MA (autor correspondente), Univ Nacl La Rioja INGeReN CENIIT UNLaR, Ctr Invest & Innovac Tecnol, Inst Geol & Recursos Nat, Avda Gob Vernet & Apostol Felipe, RA-5300 La Rioja, Argentina.	marianlarro@gmail.com	Basei, Miguel A S/C-1915-2013; Hollanda, Maria Helena B M/D-5614-2012; Casquet, Cesar/AAV-1508-2020; Baldo, Edgardo G. A./E-5404-2016	Basei, Miguel A S/0000-0002-3857-7089; Hollanda, Maria Helena B M/0000-0003-2231-7917; Casquet Martin, Cesar/0000-0002-1868-870X; Baldo, Edgardo G. A./0000-0002-3188-3964; Verdecchia, Sebastian Osvaldo/0000-0002-1912-3911	Universidad Nacional de La Rioja (UNLaR-SeCyT); Argentine National Scientific and Technical Research Council (CONICET); MINECO (Spain) [CGL2016-76439-P]	Universidad Nacional de La Rioja (UNLaR-SeCyT); Argentine National Scientific and Technical Research Council (CONICET)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); MINECO (Spain)	This study was supported through funding from Universidad Nacional de La Rioja (UNLaR-SeCyT) and by the Argentine National Scientific and Technical Research Council (CONICET). This paper also is a contribution to project CGL2016-76439-P (C. Casquet) of MINECO (Spain).	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Geol. Soc.	MAR	2020	177	2					233	257		10.1144/jgs2018-230	http://dx.doi.org/10.1144/jgs2018-230			25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LT7WF					2023-06-23	WOS:000537276100001
J	Leal-Alves, DC; Weschenfelder, J; Almeida, JCD; Albuquerque, MD; Espinoza, JMD; Gonzaga, BA				Leal-Alves, Deivid Cristian; Weschenfelder, Jair; Dominguez Almeida, Julia Carballo; Albuquerque, Miguel da Guia; de Almeida Espinoza, Jean Marcel; Gonzaga, Bento Almeida			Unmanned Aerial Vehicle and Structure from Motion Approach for Flood Assessment in Coastal Channels	JOURNAL OF COASTAL RESEARCH			English	Article						Geomorphology; coastal drainage; low-cost survey; flood modeling	BRAZIL ATMOSPHERIC CONDITIONS; SEA-LEVEL RISE; GRANDE-DO-SUL; BEACH; IMPACTS; UAV	High-resolution topographic data are the primary inputs for various scientific applications. For years, fine-scale digital elevations models have been restricted to LiDAR systems. Currently, the use of consumer-grade cameras coupled with Unmanned Aerial Vehicles (UAV) is a consolidated alternative and widely used in several research fields. The rapid diffusion of the topography UAV-based was possible by the combination of three factors: assimilation of photogrammetric principles; low-cost of planning and execution; computational efficiency of the Structure from Motion (SfM) algorithms. The systematization of these factors, combined with the ground control points GNSS-RTK, provides accurate results. Using the UAV-SfM approach, we performed low-altitude aerial surveys (50 meters) for two coastal channels on a low-lying sandy beach in southernmost Brazil. The main objectives were: (1) three-dimensional reconstruction of the two coastal channels (washouts); (2) generation of the Digital Terrain Models with the dense cloud classification; and (3) accuracy assessment of DTMs when comparing them with GNSS-RTK checkpoints. The two study areas comprise just over 14 hectares. After the mosaic alignment composed of 533 images, the GCPs were inserted (projection error less than half-pixel). The dense cloud alignment was classified, and IDW interpolated the ground features. The DTMs were confronted with 50 checkpoints, obtaining the RMSE elevation of 0.0475 for channel 1 and 0.05 for channel 2. With the morphometric goals achieved, flood simulations were performed using the bathtub model for three vertical levels of sea-level rise based on scenario RCP 8.5 of the Intergovernmental Panel on Climate Change. The results demonstrate the consolidation of the UAV-SfM approach, including when used to assess flooding in coastal areas. We emphasize that, even though it is robust and increasingly accessible, the use of UAV-SfM is limited to relatively small areas, meteorological conditions, and legal regulations.	[Leal-Alves, Deivid Cristian; Weschenfelder, Jair] Univ Fed Rio Grande do Sul, Inst Geosci, Porto Alegre, RS, Brazil; [Dominguez Almeida, Julia Carballo; Albuquerque, Miguel da Guia; de Almeida Espinoza, Jean Marcel] Inst Fed Rio Grande do Sul, Dept Geoproc, Rio Grande, RS, Brazil; [Gonzaga, Bento Almeida] Univ Rio Grande, Inst Oceanog, Rio Grande, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande	Leal-Alves, DC (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geosci, Porto Alegre, RS, Brazil.	dclealalves@gmail.com	Albuquerque, Miguel/AAH-6952-2021; Alves, Deivid Cristian Leal/ABE-5453-2020; da Guia Albuquerque, Miguel/D-7762-2017; Weschenfelder, Jair/C-3390-2013	Albuquerque, Miguel/0000-0002-2063-492X; Alves, Deivid Cristian Leal/0000-0002-5255-123X; da Guia Albuquerque, Miguel/0000-0002-2063-492X; Weschenfelder, Jair/0000-0002-2075-4067				Almeida L.E.S.B., 2006, EROSAO PROGRADACAO L, P446; Calliari J.L., 1993, PESQUI GEOCIENCIAS, V20, P45; Chen BQ, 2018, OCEAN COAST MANAGE, V160, P103, DOI 10.1016/j.ocecoaman.2018.04.007; Church J.A., 2013, CLIMATE CHANGE 2013: THE PHYSICAL SCIENCE BASIS; Dillenburg SR, 2017, MAR GEOL, V390, P106, DOI 10.1016/j.margeo.2017.06.007; DJI, 2016, PHANT 4 MAN; Elsner P, 2018, REMOTE SENS ENVIRON, V208, P15, DOI 10.1016/j.rse.2018.02.008; FIGUEIREDO S., 2005, GRAVEL, P47; Figueiredo SA, 2006, J COASTAL RES, P366; GOULART E. 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Coast. Res.	SPR	2020					95		1162	1166		10.2112/SI95-225.1	http://dx.doi.org/10.2112/SI95-225.1			5	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	NX5JL					2023-06-23	WOS:000575747100001
J	Leoncio, L; de Almeida, M; Silva, M; Oliveira, OMC; Moreira, ITA; Lima, DF				Leoncio, Lua; de Almeida, Marcos; Silva, Marcio; Oliveira, Olivia M. C.; Moreira, Icaro T. A.; Lima, Danusia Ferreira			Evaluation of accelerated biodegradation of oil-SPM aggregates (OSAs)	MARINE POLLUTION BULLETIN			English	Article						Petroleum; Nutrients; Dispersal	CRUDE-OIL; PETROLEUM-HYDROCARBONS; SEDIMENT INTERACTIONS; SANTOS BAY; BIOSTIMULATION; BIOREMEDIATION; SALINITY; BIOAUGMENTATION; NUTRIENTS; DEGRADATION	The studies of the formation of oil-Suspended Particulate Matter (SPM) aggregates (OSAs) have advanced significantly in the scientific community, however there is a need to accelerate oil biodegradation that was dispersed by the formation of OSAs. The present research presents a pioneering character regarding the addition of nutrients as biostimulus for autochthonous hydrocarboclastic bacteria in the biodegradation of Total Petroleum Hydrocarbons (TPH) dispersed by the formation of OSAs. Water aliquots were taken over 60 days from eight bioreactors to perform ionic species analysis, pH, salinity and temperature monitoring, liquid/liquid extraction, serial dilution methodology and filter membrane. TPH quantification was performed on the gas chromatograph with a flame ionisation detector (GC-FID). The addition of nutrients contributed positively to the rate and extent of biodegradation of TPH in association with field-collected SPM. The best result found was with the lowest nutrient concentration (Bio 1) with an average of 98.65% of TPH reduction.	[Leoncio, Lua; Silva, Marcio; Oliveira, Olivia M. C.] Univ Fed Bahia, Inst Geosci, Nucleo Escudos Ambientais NEA, Campus Ondina,R Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil; [de Almeida, Marcos] Univ Fed Pernambuco, Av Arquitetura S-N, BR-50740540 Recife, PE, Brazil; [Moreira, Icaro T. A.] Univ Fed Bahia, Polytech Sch, Dept Environm Engn, R Prof Aristides Novis S-N, BR-40210630 Salvador, BA, Brazil; [Lima, Danusia Ferreira] Univ Fed Bahia, Inst Geosci, LEPETRO, Campus Ondina,R Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal de Pernambuco; Universidade Federal da Bahia; Universidade Federal da Bahia	Leoncio, L (autor correspondente), Univ Fed Bahia, Inst Geosci, Nucleo Escudos Ambientais NEA, Campus Ondina,R Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil.	lmleoncio@hotmail.com; olivia@ufba.br	Ferreira, Danúsia Lima/AAB-3694-2021; de Oliveira, Olivia Maria Cordeiro/AAB-3246-2021; MOREIRA, ICARO/AAV-6503-2020	MOREIRA, ICARO/0000-0002-3964-7368; Leoncio, Lua Morena/0000-0002-2677-8836; de Almeida, Marcos/0000-0002-9633-1386	National Council for Scientific and Technological Development (CNPq), through the project "Development of Multibioprocess of Applicable Remediation in Coastal Areas Impacted by Petroleum Activities - DEMBPETRO" [4026663/2013-6, 30/2013]; Foundation for Research Support of the State of Bahia (FAPESB); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	National Council for Scientific and Technological Development (CNPq), through the project "Development of Multibioprocess of Applicable Remediation in Coastal Areas Impacted by Petroleum Activities - DEMBPETRO"(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Foundation for Research Support of the State of Bahia (FAPESB); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was funded by the National Council for Scientific and Technological Development (CNPq), through the project "Development of Multibioprocess of Applicable Remediation in Coastal Areas Impacted by Petroleum Activities - DEMBPETRO"-Case 4026663/2013-6, within the framework of the MCTI CALL/CNPq/CT-BIOTEC No. 30/2013. The author Lua Leoncio received a dissertation grant from the Foundation for Research Support of the State of Bahia (FAPESB). This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001" within the scope of the Graduate Program in Geochemistry: Petroleum and Environment (POSPETRO).	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Pollut. Bull.	MAR	2020	152								110893	10.1016/j.marpolbul.2020.110893	http://dx.doi.org/10.1016/j.marpolbul.2020.110893			13	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	ME3HK	32479280				2023-06-23	WOS:000544550000025
J	Mansur, ET; Ferreira, CF; Oliveira, DPL				Mansur, Eduardo T.; Ferreira Filho, Cesar F.; Oliveira, Denisson P. L.			The Luanga deposit, Carajas Mineral Province, Brazil: Different styles of PGE mineralization hosted in a medium-size layered intrusion	ORE GEOLOGY REVIEWS			English	Article						PGE; Nickel; Layered intrusion; Magmatic sulfide; Carajas	PLATINUM-GROUP ELEMENTS; J-M REEF; FAZENDA MIRABELA INTRUSION; BUSHVELD COMPLEX; MERENSKY REEF; STILLWATER COMPLEX; MOOKGOPHONG NABOOMSPRUIT; SULFIDE MINERALIZATION; SKAERGAARD INTRUSION; GEOCHEMISTRY	The Luanga Complex, located in the eastern portion of the Carajas Mineral Province, is part of a cluster of PGE-mineralized layered intrusions, grouped into what is known as the Serra Leste magmatic suite. The Luanga deposit, the largest PGE deposit in South America, has two distinct styles of PGE mineralization. The first type, termed as Sulfide Zone, consists of a 10-50 m thick interval with disseminated base metal sulfides (pendandite > pyrrhotite > > chalcopyrite) located along the upper contact of the intrusion's Ultramafic Zone. The Sulfide Zone extends along the entire length of the intrusion (similar to 3 km) and hosts the bulk of PGE resources of the Luanga Complex (i.e., 142 Mt at 1.24 ppm Pt + Pd + Au and 0.11% Ni). The second type of PGE mineralization, termed as low-S-high-Pt-Pd Zones, consists of 2-10 m thick stratabound PGE mineralization within a sequence of interlayered ultramafic and mafic cumulates located above the Sulfide Zone. Host rocks of the low-Shigh-Pt-Pd Zones consist mainly of sulfide-and chromite-free harzburgite and orthopyroxenite. These mineralized rocks do not show any distinctive texture or change in modal composition. The Sulfide Zone and low-Shigh-Pt-Pd Zons have distinct PGE distribution. The Sulfide Zone has Pt/Pd ratios of 0.52 and a positive correlation between PGE and S. The low-S-high-Pt-Pd Zones have Pt/Pd ratios of 1.2 and depletion in IPGE relative to primitive mantle. The platinum-group minerals (PGM) observed in the Sulfide Zone are predominantly Pt-Pd bismuthtellurides, stanides and arsenides, mainly enclosed within sulfide minerals. In contrast, the PGM observed in low-S-high-Pt-Pd Zones are mainly Pt-arsenides, stannides and antimonides, mostly enclosed within alteration silicates. Differences in texture, geochemistry and PGM assemblage between these mineralization styles suggest that they originated from distinct geological processes. The Sulfide Zone was formed by a major event of segregation of an immiscible sulfide liquid, whereas the low-S-high-Pt-Pd Zones formed by a sulfide liquid saturation followed by sulfur loss during post-magmatic alteration. The identification of PGE-rich layers in rocks without sulfides or chromite at the Carajas Mineral Province is important as these may have been overlooked during previous exploration programs.	[Mansur, Eduardo T.; Ferreira Filho, Cesar F.] Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil; [Oliveira, Denisson P. L.] VALE SA, Av Getulio Vargas 671-13, BR-30112020 Belo Horizonte, MG, Brazil; [Mansur, Eduardo T.] Univ Quebec Chicoutimi, Sci Terre, Chicoutimi, PQ G7H 2B1, Canada	Universidade de Brasilia; University of Quebec; University of Quebec Chicoutimi	Mansur, ET (autor correspondente), Univ Brasilia, Inst Geociencias, BR-70910900 Brasilia, DF, Brazil.; Mansur, ET (autor correspondente), Univ Quebec Chicoutimi, Sci Terre, Chicoutimi, PQ G7H 2B1, Canada.	etmansur@gmail.com			CNPq (Conselho Nacional de Desenvolvimento Cientifico e TeconolOgico); VALE S.A. [550398/2010-4]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)	CNPq (Conselho Nacional de Desenvolvimento Cientifico e TeconolOgico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)); VALE S.A.; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was supported by CNPq (Conselho Nacional de Desenvolvimento Cientifico e TeconolOgico) and VALE S.A. (Projeto 550398/2010-4). Analytical facilities of the Institute de Geociencias of the University of Brasilia (UnB) provided additional support for this research. The authors acknowledge VALE's Exploration Managers for Brazil and Carajas (Mr. Fernando Greco and Mr. Fernando Matos, respectively) for field support and access to exploration data. Cesar F. Ferreira Filho is a Research Fellow of CNPq and acknowledges the continuous support through research grants and scholarships for the "Metalogenenese de Depositos Associados ao Magmatismo Mafico-Ultramafico" Research Group. Eduardo T. Mansur received a scholarship from Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) and this study is part of his M.Sc. thesis developed at the Institute de Geociencias (Universidade de Brasilia). The authors thank the reviewers Dr. Steve Barnes and Dr. Wolfgang Maier, and guest editor Dr. Steffen Hagemann for carefully handling the manuscript.	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Rev.	MAR	2020	118								103340	10.1016/j.oregeorev.2020.103340	http://dx.doi.org/10.1016/j.oregeorev.2020.103340			18	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	KT0OD					2023-06-23	WOS:000518709000036
J	Marangoanha, B; de Oliveira, DC; Galarza, MA; Marques, GT				Marangoanha, Bhrenno; de Oliveira, Davis Carvalho; Galarza, Marco Antonio; Marques, Gisele Tavares			Crustal anatexis and mantle-derived magmas forming Neoarchean A-type granitoids in Carajas Province, northern Brazil: Petrological evidence and tectonic control	PRECAMBRIAN RESEARCH			English	Article						Hybridization; Neoarchcan granitoids; Geochemical modeling; U-Pb dating; Nd-Hf isotopes	U-PB GEOCHRONOLOGY; SIERRA-NEVADA BATHOLITH; ISOTOPE RATIO ANALYSIS; AMAZONIAN CRATON; MICROGRANULAR ENCLAVES; MINERAL PROVINCE; METALLOGENIC PROVINCE; ARCHEAN GRANITOIDS; GREENSTONE BELTS; MAFIC ENCLAVES	Neoarchean hybrid granitoids from the Vila Uniab suite are located in the central portion of the Canaa dos Carajas domain, Carajas Province (Amazonian craton, Brazil), and suggest that magma mixing events played an important role in their origin. According to complete evidence, including field observations, petrography, geochemical modeling, zircon SHRIMP and LA-MC-ICP-MS U-Pb ages, and Nd-Hf isotope data, we propose a geodynamic model based on initial mafic underplating promoted by lower crustal delamination, which generated mantle-derived mafic melts that were injected into the lower/middle crust (composed of Mesoarchean felsic granulite) and caused partial melting, producing leucogranitic melts. The interaction between these contrasting felsic and mafic magmas occurred by both mixing and mingling processes. The hybrid magma ascent and emplacement occurred in a N-S pure shear-dominated transpressional tectonic regime, with an E-W sinistral sense of tectonic movement, in which the hybrid melt was channeled into pre-existing shear zones trending E-W (Itacaiunas shear zone). This tectonic regime (transpressional) proceeded coevally with the hybrid magma cooling, producing 2.75-2.73 Ga Neoarchean deformed A-type granitoids with a syntectonic nature in the Vila Uniao suite, in addition to the Pium diopside-norite, which represents the mafic endmember generated by underplating.	[Marangoanha, Bhrenno; de Oliveira, Davis Carvalho; Marques, Gisele Tavares] Univ Fed Para UFPA, IG, GPPG, Rua Augusto Correa 01, BR-66075110 Belem, Para, Brazil; [Marangoanha, Bhrenno; de Oliveira, Davis Carvalho; Galarza, Marco Antonio] UFPA, IG, PPGG, Belem, Para, Brazil; [Galarza, Marco Antonio] UFPA, IG, Lab Geol Isotop Para Iso, Belem, Para, Brazil; [Marques, Gisele Tavares] UFPA, IG, Lab Microanal, Belem, Para, Brazil	Universidade Federal do Para; Universidade Federal do Para; Universidade Federal do Para; Universidade Federal do Para	Marangoanha, B (autor correspondente), Univ Fed Para UFPA, IG, GPPG, Rua Augusto Correa 01, BR-66075110 Belem, Para, Brazil.; Marangoanha, B (autor correspondente), UFPA, IG, PPGG, Belem, Para, Brazil.	bhrenno@ufpa.br	Galarza, Marco Antonio MAG/B-1736-2013	Marangoanha, Bhrenno/0000-0003-0741-5148	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [163874/2014-0]; CNPq [311388/2016-7, 485806/2013-4, 435552/2018-0]; Fundo de Amparo a Pesquisa do Estado do Para (FAPESPA) [133/2008-0]; Vale/FAPESPA (ICAAF) [053/2011]; INCT program (CNPq/FAPESPA/CAPES/PETROBRAS) [573733/2008-2]; PROPESP (PAPQ)/UFPA; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) [001]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundo de Amparo a Pesquisa do Estado do Para (FAPESPA)(Fundacao Amazonia de Amparo a Estudos e Pesquisas (FAPESPA)); Vale/FAPESPA (ICAAF); INCT program (CNPq/FAPESPA/CAPES/PETROBRAS); PROPESP (PAPQ)/UFPA; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors are grateful for the support in geological mapping provided by J.R.M. Mesquita, E.O. Gabriel, M.N.S. dos Santos and P.J.L. dos Santos and to the Laboratorio de Geologia Isotopica from Federal University of Para (Para-Iso/UFPA) staff for the Sm-Nd data. C.N. Lamarao is acknowledged for his support with the acquisition of the BSE images at the Laboratorio de Microanalises from UFPA. One of the authors (BM) thanks the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for a doctoral thesis scholarship (Proc. 163874/2014-0). Funding for this project came from CNPq (D.C. Oliveira -Proc. 311388/2016-7, 485806/2013-4 and 435552/2018-0), Fundo de Amparo a Pesquisa do Estado do Para (FAPESPA; Proc. 133/2008-0), Vale/FAPESPA (ICAAF n. 053/2011), INCT program (CNPq/FAPESPA/CAPES/PETROBRAS; Proc. 573733/2008-2) and PROPESP (PAPQ)/UFPA. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) - Finance Code 001. Constructive criticism from two anonymous reviewers substantially improved the quality of this paper. Wilson Teixeira and Elson P. Oliveira are thanked for their careful editorial handling and constructive comments.	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MAR	2020	338								105585	10.1016/j.precamres.2019.105585	http://dx.doi.org/10.1016/j.precamres.2019.105585			22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KO3EY					2023-06-23	WOS:000515431900011
J	Lima, BEM; Tedeschi, LR; Pestilho, ALS; Santos, RV; Vazquez, JC; Guzzo, JVP; De Ros, LF				Moreira Lima, Bruno Eustaquio; Tedeschi, Leonardo Ribeiro; Silva Pestilho, Andre Luiz; Santos, Roberto Ventura; Vazquez, Joselito Cabral; Poley Guzzo, Jarbas Vicente; De Ros, Luiz Fernando			Deep-burial hydrothermal alteration of the Pre-Salt carbonate reservoirs from northern Campos Basin, offshore Brazil: Evidence from petrography, fluid inclusions, Sr, C and O isotopes	MARINE AND PETROLEUM GEOLOGY			English	Article						Pre-salt; Lacustrine carbonates; Campos basin; Deep-burial; Hydrothermal alteration; Magmatic activity	THERMOCHEMICAL SULFATE REDUCTION; LAKE VALLEY FORMATION; SOUTH-ATLANTIC; DOLOMITE RESERVOIRS; SANTOS BASIN; PERVASIVE DOLOMITIZATION; TECTONIC EVOLUTION; BRITISH-COLUMBIA; ORGANIC-MATTER; RIFTED MARGINS	Petrographic, mineralogical, elemental, isotopic and fluid inclusion analyses were integrated to unravel the diagenetic evolution of Brazilian Pre-Salt Lacustrine carbonate reservoirs of northern Campos Basin, southeast Brazilian margin. Detailed thin section and cathodoluminescence petrography, scanning electron microscopy and electron microprobe analyses established a paragenetic evolution of diagenetic processes and products, comprising extensive dolomitization, silicification, and dissolution. A paragenesis including saddle dolomite, macrocrystalline calcite, mega-quartz, Sr-barite, celestine, fluorite, dickite, sphalerite, galena, and other metallic sulfides filling fractures and dissolution porosity, and aqueous fluid inclusions with homogenization tempera. tures of 92-152 degrees C and salinities between 13 and 26 wt % eq. NaCl characterized a hydrothermal system with some analogy to carbonate-hosted Pb-Zn Mississippi Valley (MVT) and Irish-type deposits. Petroleum inclusions and solid bitumen testify atypical oil generation and migration, associated with the hydrothermal flow. The host Pre-Salt spherulitic and fascicular carbonates present highly radiogenic Sr-87/Sr-86 ratios, indicating strong interaction with continental crust materials. Hydrothermal phases show delta O-18 values more negative than syngenetic and diagenetic carbonates. The delta C-13 values are interpreted as result of interaction between the hydro thermal fluids and the host rocks. The combined data set provides clear evidence of intense hydrothermal alteration of northern Campos Basin Pre-Salt reservoirs at deep-burial conditions (> 2 km), possibly related to Late Cretaceous or more probably Paleogene magmatic activity. Mixed-sourced fluids bearing a basinal signature fed the hydrothermal system and promoted dissolution of the host rocks. The hydrothermal alterations had strong impact on the porosity, permeability, and heterogeneity, contributing, together with the associated fracturing, to the excellent production performance of the Pre-Salt reservoirs.	[Moreira Lima, Bruno Eustaquio] Petrobras SA, Ave Henrique Valadares 28, BR-20231030 Rio De Janeiro, RJ, Brazil; [Moreira Lima, Bruno Eustaquio; De Ros, Luiz Fernando] Rio Grande Sul Fed Univ, Grad Program Geosci, Av Bento Goncalves 9500, BR-91540000 Porto Alegre, RS, Brazil; [Tedeschi, Leonardo Ribeiro; Silva Pestilho, Andre Luiz; Vazquez, Joselito Cabral; Poley Guzzo, Jarbas Vicente] Petrobras SA, Res Ctr CENPES, Ave Horacio Macedo,950 Cidade Univ, BR-21941915 Rio De Janeiro, RJ, Brazil; [Santos, Roberto Ventura] Univ Brasilia, Geosci Inst, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil	Petrobras; Petrobras; Universidade de Brasilia	Lima, BEM (autor correspondente), Petrobras SA, Ave Henrique Valadares 28, BR-20231030 Rio De Janeiro, RJ, Brazil.	brunolima@petrobras.com.br; leonardo.tedeschi@petrobras.com.br; andre.pestilho@petrobras.com.br; rventura@unb.br; joselitocv@petrobras.com.br; guzzo@petrobras.com.br; lfderos@inf.ufrgs.br	Pestilho, André L S/M-5785-2018; De Ros, Luiz Fernando/Q-5439-2018	Pestilho, André L S/0000-0002-5497-4236; De Ros, Luiz Fernando/0000-0003-2651-8097	Petroleo Brasileiro S.A. -Petrobras; Petrobras; Graduate Geosciences Program of Rio Grande do Sul Federal University (UFRGS)	Petroleo Brasileiro S.A. -Petrobras(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); Petrobras(Fundacao de Amparo a Pesquisa do Amapa (FAPEAP)Petrobras); Graduate Geosciences Program of Rio Grande do Sul Federal University (UFRGS)	The results and interpretations of this paper are part of the PhD research project of BEML, funded by Petroleo Brasileiro S.A. -Petrobras. The authors wish to thank Petrobras, for supporting this study and for the opportunity to publish this paper. In particular, we are extremely grateful to Gustavo Garcia, who provided useful insight and discussions about the burial-thermal history. We are grateful for the analytical and technical assistance provided by Petrobras Research Center (CENPES), the Federal University of Goias (UFG) Regional Center for Technological Development and Innovation (CRTI), the University of Brasilia (UnB) Geochronology Laboratory, and the University of Sao Paulo (USP). We would also like to thank the support of the Graduate Geosciences Program of Rio Grande do Sul Federal University (UFRGS). The authors wish also to thank the reviewers for their constructive suggestions that helped improve the manuscript.	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J	Pereira, R; de Lima, FJ; Simbras, FM; Bittar, SMB; Kellner, AWA; Saraiva, AAF; Bantim, RAM; Sayao, JM; Oliveira, GR				Pereira, Ricardo; de Lima, Flaviana Jorge; Simbras, Felipe M.; Bretas Bittar, Sheila Maria; Annin Kellner, Alexander Wilhelm; Saraiva, Antonio Alamo F.; Bantim, Renan A. M.; Sayao, Juliana M.; Oliveira, Gustavo R.			Biomarker signatures of Cretaceous Gondwana amber from Ipubi Formation (Araripe Basin, Brazil) and their palaeobotanical significance	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Amber; Gymnosperms; Terpenoids; Ipubi Formation; Cretaceous; GC	TERPENOID COMPOSITION; MOLECULAR COMPOSITION; NATURAL RESINS; SANTANA; GEOSPHERE; FATE	An amber (UFRPE 5037), from the black shales of the Ipubi Formation, Araripe Basin (Brazil), has been analyzed to understand its organic geochemical characteristics and possible botanical source using gas chromatography-mass spectrometry (GC-MS). The analyses carried out detected monoterpenes, hydrocarbonic sesquiterpenes, and aliphatic diterpanes like abietanes and norabietanes, as well as aromatic diterpanes such as simonellite, norsimonellite, retene, hinokiol, ferruginol and dehydroabietic acid. Such a combination of components is mainly known to have originated from gymnosperms. The individual identification of diterpenoids allowed the suggestion of Cheirolepidiaceae or Podocarpaceae families as possible amber producers, pointing to a flora similar to the underlying Crato Formation. Therefore, UFRPE 5037 consists on the first amber record in the Ipubi Formation, allowing the acquisition of important information regarding the botanical sources associated to new Brazilian amber occurrence described here.	[Pereira, Ricardo] Univ Fed Pernambuco, Ctr Tecnol & Geociencias, Dept Geol, BR-50740550 Recife, PE, Brazil; [de Lima, Flaviana Jorge; Saraiva, Antonio Alamo F.; Bantim, Renan A. M.] Univ Reg Cariri, Dept Ciencias Biol, Lab Paleontol URCA, Rua Coronel Antonio Luis 1161, BR-63105000 Crato, Ceara, Brazil; [Simbras, Felipe M.; Oliveira, Gustavo R.] Univ Fed Rural Pernambuco, Dept Biol, Lab Paleontol & Sistemat, Rua Dom Manuel de Medeiros S-N Dois Irmaos, Recife, PE, Brazil; [Bretas Bittar, Sheila Maria] Univ Fed Rural Pernambuco, Dept Agron, Rua Dom Manuel de Medeiros S-N Dois Irmaos, Recife, PE, Brazil; [Annin Kellner, Alexander Wilhelm] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Lab Systemat & Taphon Fossil Vertebrates, BR-20940040 Rio De Janeiro, RJ, Brazil; [Sayao, Juliana M.] Univ Fed Pernambuco, Lab Paleobiol & Microestruturas, Rua Alto Reservatorio S-N, Vitoria De Santo Antao, PE, Brazil	Universidade Federal de Pernambuco; Universidade Regional do Cariri; Universidade Federal Rural de Pernambuco (UFRPE); Universidade Federal Rural de Pernambuco (UFRPE); Universidade Federal do Rio de Janeiro; Universidade Federal de Pernambuco	Oliveira, GR (autor correspondente), Univ Fed Rural Pernambuco, Dept Biol, Lab Paleontol & Sistemat, Rua Dom Manuel de Medeiros S-N Dois Irmaos, Recife, PE, Brazil.	ricardo.geologia@yahoo.com.br; flavianajorge@gmail.com; felipe.simbras@gmail.com; sheila.schulze@ufrpe.br; kellner@mn.ufrj.br; alamocariri@yahoo.com.br; renanbandmbiologo@gmail.com; jmsayao@gmail.com; gustavoliveira@gmail.com	Saraiva, António/HPD-3031-2023; Oliveira, Gustavo/IQW-7983-2023; Bantim, Renan/J-4076-2014; PEREIRA, RICARDO/AAG-7297-2021; Kellner, Alexander/ABE-9591-2020; Oliveira, Gustavo R/F-7432-2012	Kellner, Alexander/0000-0001-7174-9447; Oliveira, Gustavo R/0000-0002-9871-1235	Universidade Federal Rural de Pernambuco; Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico FUNCAP [9871903/2018, BMD-0124-00302.01.01/19, BP3-013900202.01.00/18]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq [311715/2017-6, 305705/2019-9, 420687/2016-5, 313461/2018-0]; Fundacao de Desenvolvimento Carlos Chagas Filho de Amparo Pesquisa do Estado do Rio de Janeiro - FAPERJ [E-26/202.905/2018]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior; Brasil (CAPES) [001, 88887.162865/2018-00]	Universidade Federal Rural de Pernambuco; Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico FUNCAP(Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Desenvolvimento Carlos Chagas Filho de Amparo Pesquisa do Estado do Rio de Janeiro - FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior; Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors thank Professor Mario Kato and Laboraterio de Saneamento Ambiental/UFPE for analytical support and the use of GC-MS equipment. This project was partially funded by Universidade Federal Rural de Pernambuco to GRO, Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico FUNCAP to FJL (SPU: 9871903/2018), RAMB (#BMD-0124-00302.01.01/19) and AAFS (#BP3-013900202.01.00/18), Conselho Nacional de Desenvolvimento Cientifico e Tecnologico - CNPq to JMS (#311715/2017-6), FJL (#305705/2019-9) and to (AWAK #420687/2016-5; #313461/2018-0); Fundacao de Desenvolvimento Carlos Chagas Filho de Amparo Pesquisa do Estado do Rio de Janeiro - FAPERJ to AWAK (#E-26/202.905/2018), and the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior; Brasil (CAPES) to RAMB - Finance code 001 (CAPES #88887.162865/2018-00). We wish to thank to three referees for relevant comments and suggestions that improved the manuscript.	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J	Roddaz, M; Nauton-Fourteu, M; Santos, RV; Dantas, EL; Calves, G				Roddaz, Martin; Nauton-Fourteu, Martin; Santos, Roberto Ventura; Dantas, Elton Luiz; Calves, Gerome			Controls on the provenance of late Eocene to Quaternary Mozambique Channel shales (DSDP 25 Site 242)	MARINE GEOLOGY			English	Article							RARE-EARTH-ELEMENTS; LAST GLACIAL MAXIMUM; ND ISOTOPES; NEODYMIUM ISOTOPES; LAND-USE; ICP-MS; SEDIMENTS; SR; RIVER; TRACERS	Provenance determination of late Eocene to Quaternary sediments deposited at the DSDP 25 Site 242 may help to evaluate the mechanisms that have controlled the sediment deposition in the Mozambique Channel. To determine the provenance of the clay fraction, we measure major and trace element concentrations as well as strontium (Sr-87/Sr-86) and neodymium isotopic compositions (expressed as epsilon(Nd(0))) of thirty-six sedimentary samples from DSDP 25 Site 242 on the eastern flank of the Davie Fracture Zone. Light Rare Earth Element (LREE) enrichment and Heavy REE (HREE) depletions against Post Archean Australian Shales (PAAS) associated with Ce anomalies higher than or equal to 0.90 for all the analyzed samples suggest very little influence of authigenic smectite incorporation. The absence of correlation of Al/Si and CIA with REE content, Eu/Eu*, Cr/Th, Th/Sc, and Sr-87/Sr-86 and epsilon(Nd(0)) suggests that chemical weathering has not modified these provenance proxies. Slight increase of Eu/Eu*, Cr/Th ratios, epsilon(Nd(0)) values associated with slight decrease in Sr-87/Sr-86 and Th/Sc ratios from the late Eocene to the Quaternary point to input of less differentiated and younger detritus to the DSDP 25 Site 242 with age. Based on variations in epsilon(Nd(0)) and Nd concentrations, we estimate an overall decrease of the Southeast African rivers (Congo/Zambezi) contribution from similar to 65.7% (Standard Deviation (S.D.) similar to 13.2) in the late Eocene to similar to 28.5% (S.D. similar to 10.0) in the early Pliocene. The causes for the low epsilon(Nd(0)) values and high Southeast African contribution between the late Eocene and the early Oligocene remain to be determined. It could record the onset of modern sedimentation in the Zambezi delta or the discharge of the Paleo Congo river in the Indian Ocean. The decrease of Zambezi contribution between the late Oligocene and early Pliocene is attributed to the cumulative effect of increasing tectonic activity of the Davie Fracture Zone and intensification of the Mozambique Current. The late Pliocene to Quaternary glacial-interglacial cycles promoted higher Zambezi contribution during glacial sea-level lowstands and in turn lower epsilon(Nd(0)) detrital values, whereas low Zambezi contributions are favored during interglacial highstand causing higher epsilon(Nd(0)) values. Hence, the modern dispersal pattern of fine-grained sediments within the Mozambique Channel is no younger than late Pliocene.	[Roddaz, Martin; Calves, Gerome] Univ Toulouse, UPS SVT OMP, CNRS, Geosci Environm Toulouse,IRD, 14 Ave Edouard Belin, F-31400 Toulouse, France; [Roddaz, Martin; Santos, Roberto Ventura; Dantas, Elton Luiz] Univ Brasilia, Inst Geociencias, Lab Geocronol, BR-70910000 Brasilia, DF, Brazil; [Nauton-Fourteu, Martin] Natl Univ Ireland, Sch Nat Sci, iCRAG, Earth & Ocean Sci, Univ Rd, Galway, Ireland	Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Toulouse; Universite Toulouse III - Paul Sabatier; Universidade de Brasilia; Ollscoil na Gaillimhe-University of Galway	Roddaz, M (autor correspondente), Univ Toulouse, UPS SVT OMP, CNRS, Geosci Environm Toulouse,IRD, 14 Ave Edouard Belin, F-31400 Toulouse, France.	martin.roddaz@get.omp.eu	Dantas, Elton Luiz/AAK-8464-2021; Roddaz, Martin/AFR-7875-2022; Calves, Gerome/E-9337-2011	Dantas, Elton Luiz/0000-0002-7954-5059; Roddaz, Martin/0000-0001-8562-8582; Calves, Gerome/0000-0003-3829-131X; Nauton-Fourteu, Martin/0000-0001-7090-3916	INSU; CNRS; Total; IFREMER; BRGM; US National Science Foundation	INSU(Centre National de la Recherche Scientifique (CNRS)); CNRS(Centre National de la Recherche Scientifique (CNRS)); Total(Total SA); IFREMER; BRGM(Bureau de Recherches Geologiques et Minieres (BRGM)); US National Science Foundation(National Science Foundation (NSF))	This study was supported by the Actions Marges projects "Tracages des sources de la marge du nord ouest de l'Afrique" and "Quantification et modelisation des transferts continent-ocean aux differentes echelles de temps (actuel-100 Ma) exemple de la marge ouest de l'Afrique" funded by INSU,CNRS, Total, IFREMER and BRGM. This work used samples provided by the Deep Sea Drilling Project (DSDP), which is sponsored by the US National Science Foundation and participating countries under the management of the Joint Oceanographic Institutions (JOI), Inc. We also would like to thank Tristan Rousseau and Yannick Mourlot for having leached some of the DSDP samples when they were at GET. We would like to thank the editor and two anonymous reviewers for their comments that helped us to greatly improve this manuscript.	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Geol.	MAR	2020	421								106090	10.1016/j.margeo.2019.106090	http://dx.doi.org/10.1016/j.margeo.2019.106090			17	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	KH9DA		Green Published, Bronze			2023-06-23	WOS:000510948100005
J	Sawakuchi, AO; Rodrigues, FCG; Mineli, TD; Mendes, VR; Melo, DB; Chiessi, CM; Giannini, PCF				Sawakuchi, Andre Oliveira; Goncalves Rodrigues, Fernanda Costa; Mineli, Thays Desiree; Mendes, Vinicius Ribau; Melo, Dayane Batista; Chiessi, Cristiano Mazur; Fonseca Giannini, Paulo Cesar			Optically Stimulated Luminescence Sensitivity of Quartz for Provenance Analysis	METHODS AND PROTOCOLS			English	Article						sediment provenance; quartz fingerprint; luminescence; source-to-sink system	SEDIMENTS; OSL; SYSTEM; COMPONENTS; RAINFALL	Finding the source or provenance of quartz grains occurring in a specific location allows us to constrain their transport pathway, which is crucial information to solve diverse problems in geosciences and related fields. The optically stimulated luminescence (OSL) sensitivity (light intensity per unit mass per unit radiation dose) has a high capacity for discrimination of quartz sediment grains and represents a promising technique for provenance analysis. In this study, we tested the use of quartz OSL sensitivity (ultraviolet emission) measured under different preheating temperatures and with blue light stimulation at room temperature (similar to 20 degrees C) for sediment provenance analysis. Quartz OSL sensitivity measured at 20 degrees C is positively correlated with the sensitivity of an OSL signal measured using procedures (preheat at 190 degrees C for 10 s, blue stimulation at 125 degrees C and initial 1 s of light emission) to increase the contribution of the fast OSL component, which has been successfully applied for sediment provenance analysis. The higher OSL signal intensity measured without preheating and with light stimulation at room temperature allows the use of lower given doses, thus reducing measurement time. Additionally, the OSL sensitivity measured at 20 degrees C in polymineral silt samples of a marine sediment core is also suitable for provenance analysis, as demonstrated by comparison with other independent proxies. OSL signals obtained through light stimulation at room temperature have thus the potential to considerably expand measurement possibilities, including in situ measurements using portable OSL readers.	[Sawakuchi, Andre Oliveira; Goncalves Rodrigues, Fernanda Costa; Mineli, Thays Desiree; Fonseca Giannini, Paulo Cesar] Univ Sao Paulo, Inst Geociencias, Luminescence & Gamma Spectrometry Lab LEGaL, BR-05508080 Sao Paulo, Brazil; [Mendes, Vinicius Ribau; Melo, Dayane Batista] Univ Fed Sao Paulo, Inst Marine Sci, BR-11015020 Santos, SP, Brazil; [Chiessi, Cristiano Mazur] Univ Sao Paulo, Sch Arts Sci & Humanities, BR-03828000 Sao Paulo, Brazil	Universidade de Sao Paulo; Universidade Federal de Sao Paulo (UNIFESP); Universidade de Sao Paulo	Sawakuchi, AO (autor correspondente), Univ Sao Paulo, Inst Geociencias, Luminescence & Gamma Spectrometry Lab LEGaL, BR-05508080 Sao Paulo, Brazil.	andreos@usp.br; cgr.fernanda@gmail.com; thaysdesiree@gmail.com; vrm.unifesp@gmail.com; d.batista.melo@hotmail.com; chiessi@usp.br; pcgianni@usp.br	Sawakuchi, André O/D-1445-2013; Giannini, Paulo César Fonseca/D-1871-2015; Chiessi, Cristiano Mazur/E-1916-2012; mendes, vinicius ribau/P-7064-2016	Giannini, Paulo César Fonseca/0000-0003-1046-0177; Chiessi, Cristiano Mazur/0000-0003-3318-8022; mendes, vinicius ribau/0000-0003-1072-8292; Costa Goncalves Rodrigues, Fernanda/0000-0003-1236-7937; Sawakuchi, Andre/0000-0001-5016-2428	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [304727/2017-2, 308772/2018-0, 422255/2016-5]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2018/12472-8, 2013/21942-4]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	A.O.S., P.C.F.G., and C.M.C. are funded by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq grants 304727/2017-2, 308772/2018-0 and 422255/2016-5). 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MAR	2020	3	1							6	10.3390/mps3010006	http://dx.doi.org/10.3390/mps3010006			13	Biochemical Research Methods	Emerging Sources Citation Index (ESCI)	Biochemistry & Molecular Biology	UU7KR	31941007	Green Published, gold			2023-06-23	WOS:000698975300006
J	Simoes, MG; Neves, JP; Taboada, AC; Pagani, MA; Varejao, FG; Assine, ML				Simoes, Marcello Guimaraes; Neves, Jacqueline Peixoto; Taboada, Arturo Cesar; Pagani, Maria Alejandra; Varejao, Filipe Giovanini; Assine, Mario Luis			Macroinvertebrates of the Capivari marine bed, late Paleozoic glacial Itarare Group, northeast Parana Basin, Brazil: Paleoenvironmental and paleogeographic implications	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Permian; Taciba formation; Macroinvertebrate; Parana basin; Capivari	PERMIAN BIVALVES; PATAGONIA CHUBUT; COAL SUCCESSION; SOUTH CHINA; FAUNA; CLASSIFICATION; PALEOECOLOGY; STRATIGRAPHY; ARGENTINA; FAMILIES	A 2-m-thick silty shale bed within the Taciba Formation, Itarare Group, Parana Basin, State of Sao Paulo, southeastern Brazil, records marine sedimentation in a siliciclastic-dominated, low-energy, shelf setting, during a short-lived deglacial event. The bed is located 100-150 m below the base of the lower Permian, post-glacial Tatui Formation. The marine assemblage is dominated by rhynchonelliform brachiopods, with subordinate bivalves, gastropods and crinoids, recording the highest phylum-level diversity so far identified within a given fossil-bearing horizon in the uppermost portion of the Itarara Group. Two new species are described, one brachiopod Biconvexiella saopauloensis and one gastropod Peruvispira brasilensis. Additionally, shells of Lyonia rochacamposi, Rhynchopora grossopunctata, Quinquenella rionegrensis, Phestia tepuelensis, Streblopteria aff. S. lagunensis, Limipecten capivariensis, Praeundulomya cf. subelongata and Mourlonia (Woolnoughia)? sp. are identified. Crinoid columns were assigned to oPentaridica sp. (a genus based on elements of the columnal). This is the first systematic description of members of the Eurydesma-Lyonia fauna in the northeastern part of the Parana Basin, Brazil. The overwhelming majority of brachiopods belong to Biconvexiella saopauloensis, followed by Rhynchopora grossopunctata. The record of Lyonia rochacamposi closely resembles that of the uppermost part of the Taciba Formation in southern Brazil. Hence, the Capivari marine fauna correlates approximately with that of the upper part of the Taciba Formation. Lyonia rochacamposi also indicates correlation with Permian units of the Sauce Grande-Colorado (Argentina), Huab (Hardap shale of the Dwyka Group), Aranos area (Namibia), southwest Africa, and the Carnavon (Western Australia) basins. These correlations support a latest Asselian-earliest Sakmarian age for the fauna.	[Simoes, Marcello Guimaraes] Univ Estadual Paulista, Inst Biociencias, Dept Zool, Botucatu, SP, Brazil; [Neves, Jacqueline Peixoto] Univ Tecnol Fed Parana, Campus Dois Vizinhos, Dois Vizinhos, Parana, Brazil; [Taboada, Arturo Cesar] UNPSIB, CONICET, Ctr Invest Esquel Montana & Estepa Patagon, Esquel,U9200, Chubut, Argentina; [Pagani, Maria Alejandra] Consejo Nacl Invest Cient & Tecn, Museo Paleontol Egidio Feruglio, Ave Fontana 140,U9100GYO, Trelew, Chubut, Argentina; [Varejao, Filipe Giovanini; Assine, Mario Luis] Univ Estadual Paulista, Inst Geociencias & Ciencias Exatas, Dept Geol Aplicada, Campus Rio Claro, Rio Clam, SP, Brazil	Universidade Estadual Paulista; Pontificia Universidade Catolica do Parana; Universidade Tecnologica Federal do Parana; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidade Estadual Paulista	Neves, JP (autor correspondente), Univ Tecnol Fed Parana, Campus Dois Vizinhos, Dois Vizinhos, Parana, Brazil.	profmgsimoes@gmail.com; jacquelineneves@utfpr.edu.br; ataboada@unpata.edu; apagani@mef.org.ar; filipe.varejao@hotmail.com; assine@rc.unesp.br	Varejão, Filipe/GYD-3727-2022; Varejão, Filipe Giovanini/O-1943-2019; Simoes, Marcello G/C-2373-2012; Varejão, Filipe/J-3015-2015; Assine, Mario/S-6150-2019; Assine, Mario L/C-1154-2013	Varejão, Filipe/0000-0002-3776-9476; Varejão, Filipe Giovanini/0000-0002-3776-9476; Varejão, Filipe/0000-0002-3776-9476; Assine, Mario/0000-0002-3097-5832; Assine, Mario L/0000-0002-3097-5832	Institute de Geociencias, Universidade de Sio Paulo, Sao Paulo; FAPESP, Brazil; CNPq, Brazil; CONICET, Argentina; FAPESP [2013/25317-7, 2014/09149-0]; CNPq [304925/2017-9, 301023/94-3]	Institute de Geociencias, Universidade de Sio Paulo, Sao Paulo; FAPESP, Brazil(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq, Brazil(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CONICET, Argentina(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are very indebted to the Institute de Geociencias, Universidade de Sio Paulo, Sao Paulo, for access and support in the study of the invertebrate collection of the Capivari fossils. We also thank Ivone C. Gonzales, IGc/USP, for assistance with this collection. Julio Hlebszevitsch helped us with crinoid identification and Suzana A. Matos, IBB/UNESP, assisted us in the field. Hence, both are here acknowledged. Many thanks also to Paul A. Johnston, and two anonymous reviewers for their suggestions, corrections and comments that improved the final version of the manuscript. Editor-in-Chief, Francisco J. Vega is also acknowledged for the useful suggestions and corrections. Finally, we also thank the paleoillustrator Julio L.C. Bezerra for the "Capivari sea" paleoscene. Financial support was offered by FAPESP and CNPq, Brazil, and CONICET, Argentina. JPN was a fellow of FAPESP (grant 2013/25317-7). This project is a contribution to the following FAPESP projects: 2013/25317-7 and 2014/09149-0. CNPq grants: 304925/2017-9 to MLA and 301023/94-3 to MGS.	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South Am. Earth Sci.	MAR	2020	98								102433	10.1016/j.jsames.2019.102433	http://dx.doi.org/10.1016/j.jsames.2019.102433			21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KR5NJ					2023-06-23	WOS:000517664800008
J	Sutilli, M; Combi, T; Garcia, MRD; Martins, CC				Sutilli, Marina; Combi, Tatiane; Domingues Garcia, Marina Reback; Martins, Cesar C.			One century of historical deposition and flux of hydrocarbons in a sediment core from a South Atlantic RAMSAR subtropical estuary	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Sediment core; Petroleum biomarkers; Source identification; Flux; Guaratuba; South Atlantic	POLYCYCLIC AROMATIC-HYDROCARBONS; ECOLOGICAL RISK-ASSESSMENT; ORGANIC-MATTER SOURCES; ALIPHATIC-HYDROCARBONS; SURFACE SEDIMENTS; GUARATUBA BAY; PETROLEUM BIOMARKERS; SPATIAL-DISTRIBUTION; MARINE-SEDIMENTS; RIVER ESTUARY	Levels and fluxes of Polycyclic aromatic hydrocarbons (PAHs) and aliphatic hydrocarbons (AHs), including n-alkanes and petroleum biomarkers (PBMs), were measured in a sedimentary core from a nominated RAMSAR (Guaratuba Bay, Brazil) subtropical estuary experiencing relatively low human impacts, to describe the evolution of anthropogenic activities over the last century. TOC contents varied from 0.80 to 1.25%. No significant correlation between hydrocarbons and TOC with grain size (predominantly sand) was observed. Concentration and flux of total AHs ranged from 65.5 to 195 mu g g(-1) and 27.6 to 82.0 mu g cm(-2) y(-1), respectively, with the highest levels found in 1960-1966, when access routes to Guaratuba city were improved. Diagnostic ratios based on AH components showed an apparent change in the sources over time, with biogenic origins prevailing until 1966-1971, followed by subsequent increases in petroleum sources. Petroleum tricyclic terpanes were detected in the core (0.40 to 3.0 mu g g(-1)), suggesting the use of lubricating oil in the bay area. Hopanes were mainly attributed to biological sources. Concentration and flux of total PAHs ranged from 8.65 to 35.9 mu g g(-1) and 3.64 to 15.1 ng cm(-2) y(-1), respectively, with the highest levels found in the top core section, reflecting recently increased human activity, while a peak PAH concentration at approximately 1977-1983 can be assumed to be a delayed signal of increased human occupation as a consequence of the improvement of access roads to the area, which started in the 1960s. Alkylated were the most abundant group of PAHs throughout the core. Despite relatively low concentrations of hydrocarbon deposition over approximately 90 years, this study highlights the influence of human occupation and slight petroleum contamination in this preserved area, mainly in recent cure sections. (C) 2019 Elsevier B.V. All rights reserved.	[Sutilli, Marina; Domingues Garcia, Marina Reback] Univ Fed Parana, Programa Posgrad Sistemas Costeiros & Ocean PGSIS, Caixa Postal 61, BR-83255976 Pontal Do Parana, PR, Brazil; [Combi, Tatiane; Martins, Cesar C.] Univ Fed Parana, Ctr Estudos Mar, Caixa Postal 61, BR-83255976 Pontal Do Parana, PR, Brazil; [Combi, Tatiane] Univ Fed Bahia, Inst Geociencias, Rua Barao Jeremoabo S-N, BR-40170115 Salvador, BA, Brazil	Universidade Federal do Parana; Universidade Federal do Parana; Universidade Federal da Bahia	Sutilli, M (autor correspondente), Univ Fed Parana, Programa Posgrad Sistemas Costeiros & Ocean PGSIS, Caixa Postal 61, BR-83255976 Pontal Do Parana, PR, Brazil.; Martins, CC (autor correspondente), Univ Fed Parana, Ctr Estudos Mar, Caixa Postal 61, BR-83255976 Pontal Do Parana, PR, Brazil.	marinasutilli@gmail.com; ccmart@ufpr.br	Garcia, Marina Reback Domingues/O-4542-2017; Combi, Tatiane/AAC-9936-2021; Combi, Tatiane/O-3004-2016	Garcia, Marina Reback Domingues/0000-0003-3554-6065; de Castro Martins, Cesar/0000-0002-2515-5565; Combi, Tatiane/0000-0001-6769-7445	CNPq (Brazilian Council for Scientific and Technological Development) [564316/2008-3]; CNPq [101143-2016-8, 306468/2017-4]; CAPES; Fundacao Araucaria [401/12, 15.078]	CNPq (Brazilian Council for Scientific and Technological Development)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao Araucaria(Fundacao Araucaria de Apoio ao Desenvolvimento Cientifico e Tecnologico do Estado do Parana FAFundacao de Amparo a Pesquisa e Inovacoo Estado de Santa Catarina (FAPESC))	This study was funded by CNPq (Brazilian Council for Scientific and Technological Development) (564316/2008-3). M. Sutilli is thankful for the BSc and MSc scholarship (CNPq 101143-2016-8 and CAPES, respectively), and C.C. Martins is thankful for the PQ-2 Grant (CNPq 306468/2017-4). The authors acknowledge Fundacao Araucaria (401/12, 15.078) for their financial support. The authors thank R.C.L. Figueira and P.A.L. Ferreira from the Instituto Oceanografico da Universidade de So Paulo (IO/USP) for his assistance in the<SUP>210</SUP>Pb core analyses and Marines M. Wilhelm and Fernanda K. Ishii for support during the laboratory procedures and instrumental analysis.	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Total Environ.	MAR 1	2020	706								130017	10.1016/j.scitotenv.2019.136017	http://dx.doi.org/10.1016/j.scitotenv.2019.136017			12	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	KB3CF	31855633				2023-06-23	WOS:000506376300099
J	Teixeira, W; Cordani, UG; Faleiros, FM; Sato, K; Maurer, VC; Ruiz, AS; Azevedo, EJP				Teixeira, W.; Cordani, U. G.; Faleiros, F. M.; Sato, K.; Maurer, V. C.; Ruiz, A. S.; Azevedo, E. J. P.			The Rio Apa Terrane reviewed: U-Pb zircon geochronology and provenance studies provide paleotectonic links with a growing Proterozoic Amazonia	EARTH-SCIENCE REVIEWS			English	Review						Rio Apa Terrane; U-Pb zircon ages and sedimentary provenance; Paleo- to Mesoproterozoic evolution; Amazonian Craton; LIP	LA-PLATA CRATON; CENTRAL-EASTERN RONDONIA; TAPAJOS GOLD PROVINCE; TECTONIC EVOLUTION; MATO-GROSSO; MAGMATIC ARC; ISOTOPIC COMPOSITION; AMONGUIJA GROUP; CRUSTAL GROWTH; VILA-RIOZINHO	New and compiled data of zircon U-Pb ages and geochemical-isotopic constraints provide new insights into the orogenic evolution of the Rio Apa Terrane (RAT) and its close affinity with the Amazonia throughout the Proterozoic. Two terranes with distinct evolutionary histories built the RAT. The Porto Murtinho (2070-1940 Ma) and Amoguija (1870-1820 Ma) magmatic arcs generated the Western Terrane which is mainly composed of short-lived crustal components. Granitoid rocks (1870 Ma) in the distal Corumba Window indicate that the RAT is much larger in extent. The Caracol accretionary arc (1800-1740 Ma) and the associated Alto Terere back-arc basin formed away from the Amoguija belt, being roughly coeval with the adjoining Baia das Garcas suite (1776 Ma) and Paso Bravo granitoid rocks (1774-1752 Ma). These tectonic units constitute the Eastern Terrane, whilst the Nd-Hf isotopic constraints indicate derivation from a predominantly juvenile magma source with the minor input of crustal-derived contaminants. The youngest detrital zircon grains from the Alto Terere samples gave 1740-1790 Ma ages and unimodal age spectra were mainly present. The basin infill was, therefore, most likely concomitant with the exhumation of the Caracol belt. Alto Terere provenance study also included detritus from passive to active margin settings. The RAT underwent regional cooling between 1.35 and 1.27 Ga, documented mainly by 40Ar-39Ar and K-Ar ages. This age pattern matches a collisional episode that formed the accretionary margin of Amazonia, suggesting that the RAT was a close neighbor at Ectasian times. The geodynamic interplay between them lasted until 1.1 Ga ago, highlighted by some shared-components of a LIP event.	[Teixeira, W.; Cordani, U. G.; Faleiros, F. M.; Sato, K.] Univ Sao Paulo, Inst Geosci, Sao Paulo, Brazil; [Maurer, V. C.] Univ Fed Ouro Preto, Sch Mines, Dept Geol, Ouro Preto, Brazil; [Ruiz, A. S.] Univ Fed Mato Grosso, Fac Geosci, Cuiaba, Brazil; [Azevedo, E. J. P.] CPRM, Brazilian Geol Survey, Belo Horizonte, MG, Brazil	Universidade de Sao Paulo; Universidade Federal de Ouro Preto; Universidade Federal de Mato Grosso	Teixeira, W (autor correspondente), Univ Sao Paulo, Inst Geosci, Sao Paulo, Brazil.	wteixeir@usp.br	Ruiz, Amarildo Salina/M-3634-2014; Faleiros, Frederico Meira/F-6138-2010; Cordani, Umberto/F-3686-2014; Teixeira, Wilson/B-7570-2013	Ruiz, Amarildo Salina/0000-0002-7800-2837; Faleiros, Frederico Meira/0000-0003-2199-8116; Cordani, Umberto/0000-0003-4425-5905; Teixeira, Wilson/0000-0003-1578-6846	Sao Paulo Research Foundation (FAPESP) [2013/12754-0]; National Council of Technological and Scientific Development (CNPq -Brazil) [303498/2014-5, 302884/2015-7, 312811/2017-9]	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Council of Technological and Scientific Development (CNPq -Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Financial support was provided by grant 2013/12754-0 of the Sao Paulo Research Foundation (FAPESP), managed by UGC. WT, FMF, and ASR thank the National Council of Technological and Scientific Development (CNPq -Brazil) for the research productivity scholarship grants (303498/2014-5, 302884/2015-7 and 312811/2017-9 respectively). We acknowledge Editor Carlo Doglioni for his efficient handling of the manuscript. Very helpful comments on the manuscript by anonymous reviewers and Editor were greatly appreciated and helped to significantly improve the early drafts of this paper.	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J	Thom, G; Xue, AT; Sawakuchi, AO; Ribas, CC; Hickerson, MJ; Aleixo, A; Miyaki, C				Thom, Gregory; Xue, Alexander T.; Sawakuchi, Andre O.; Ribas, Camila C.; Hickerson, Michael J.; Aleixo, Alexandre; Miyaki, Cristina			Quaternary climate changes as speciation drivers in the Amazon floodplains	SCIENCE ADVANCES			English	Article							RIVER; AVES; THAMNOPHILIDAE; INFERENCE; DYNAMICS	The role of climate as a speciation driver in the Amazon has long been discussed. Phylogeographic studies have failed to recover synchronous demographic responses across taxa, although recent evidence supports the interaction between rivers and climate in promoting speciation. Most studies, however, are biased toward upland forest organisms, while other habitats are poorly explored and could hold valuable information about major historical processes. We conducted a comparative phylogenomic analysis of floodplain forest birds to explore the effects of historical environmental changes and current connectivity on population differentiation. Our findings support a similar demographic history among species complexes, indicating that the central portion of the Amazon River basin is a suture zone for taxa isolated across the main Amazonian sub-basins. Our results also suggest that changes in the fluvial landscape induced by climate variation during the Mid- and Late Pleistocene drove population isolation, leading to diversification with subsequent secondary contact.	[Thom, Gregory; Miyaki, Cristina] Univ Sao Paulo, Dept Genet & Biol Evolut, Rua Matao 277,Cidade Univ, BR-05508090 Sao Paulo, SP, Brazil; [Thom, Gregory] Amer Museum Nat Hist, Dept Ornithol, New York, NY 10024 USA; [Xue, Alexander T.; Hickerson, Michael J.] CUNY City Coll, Dept Biol, Marshak Sci Bldg, New York, NY 10031 USA; [Xue, Alexander T.] Rutgers State Univ, Human Genet Inst New Jersey, 604 Allison Rd, Piscataway, NJ 08854 USA; [Xue, Alexander T.] Rutgers State Univ, Dept Genet, 604 Allison Rd, Piscataway, NJ 08854 USA; [Xue, Alexander T.] Cold Spring Harbor Lab, Simons Ctr Quantitat Biol, One Bungtown Rd, Cold Spring Harbor, NY 11724 USA; [Sawakuchi, Andre O.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Ribas, Camila C.] INPA, Av Andre Araujo 2936, BR-69060001 Manaus, Amazonas, Brazil; [Hickerson, Michael J.] City Univ New York, Grad Ctr, New York, NY 10016 USA; [Hickerson, Michael J.] Amer Museum Nat Hist, New York Div Invertebrate Zool, New York, NY 10024 USA; [Aleixo, Alexandre] Museu Paraense Emilio Goeldi, Caixa Postal 399, BR-66040170 Belem, Para, Brazil; [Aleixo, Alexandre] Univ Helsinki, Finnish Museum Nat Hist, Helsinki, Finland	Universidade de Sao Paulo; American Museum of Natural History (AMNH); City University of New York (CUNY) System; City College of New York (CUNY); Rutgers State University New Brunswick; Rutgers State University New Brunswick; Cold Spring Harbor Laboratory; Universidade de Sao Paulo; Institute Nacional de Pesquisas da Amazonia; City University of New York (CUNY) System; American Museum of Natural History (AMNH); Museu Paraense Emilio Goeldi; University of Helsinki	Thom, G (autor correspondente), Univ Sao Paulo, Dept Genet & Biol Evolut, Rua Matao 277,Cidade Univ, BR-05508090 Sao Paulo, SP, Brazil.; Thom, G (autor correspondente), Amer Museum Nat Hist, Dept Ornithol, New York, NY 10024 USA.	biogrego@yahoo.com.br	Aleixo, Alexandre/L-3135-2013; Sawakuchi, André O/D-1445-2013; /J-2431-2015	Aleixo, Alexandre/0000-0002-7816-9725; Ribas, Camila/0000-0002-9088-4828; Sawakuchi, Andre/0000-0001-5016-2428; /0000-0002-9708-9202; Thom, Gregory/0000-0001-6200-0565	FAPESP (BIOTA) [2012/50260-6, 2013/50297-0]; NSF [DEB-1253710, DOB 1343578]; NASA; CNPq [310880/2012-2, 308927/2016-8, 303713/2015-1, 310593/2009-3, 574008/2008-0, 563236/2010-8, 471342/2011-4]; FAPESPA [ICAAF 023/2011]; CAPES [2014/00113-2, 2015/12551-7, 2018/17869-3, 2017/25720-7]; NASA through the Dimensions of Biodiversity Program [DOB 1343578]; FAPESP [2014/00113-2, 2015/12551-7, 2018/17869-3, 2017/25720-7]	FAPESP (BIOTA)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); NSF(National Science Foundation (NSF)); NASA(National Aeronautics & Space Administration (NASA)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESPA(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)Fundacao Amazonia de Amparo a Estudos e Pesquisas (FAPESPA)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); NASA through the Dimensions of Biodiversity Program(National Science Foundation (NSF)NSF - Directorate for Biological Sciences (BIO)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	This study was co-funded by FAPESP (BIOTA, 2012/50260-6 and 2013/50297-0), NSF (DOB 1343578), NASA, CNPq (310593/2009-3, 574008/2008-0, 563236/2010-8, and 471342/2011-4), PEER/USAID (AID-OAA-A-11-00012), and FAPESPA (ICAAF 023/2011). G.T. was granted by CAPES and then FAPESP scholarships (2014/00113-2, 2015/12551-7, 2018/17869-3, and 2017/25720-7). A.A., C.C.R., and C.M. are supported by CNPq research productivity fellowships (310880/2012-2, 308927/2016-8, and 303713/2015-1). M.J.H. was funded by FAPESP (BIOTA, 2013/50297-0), NASA through the Dimensions of Biodiversity Program (DOB 1343578), and the NSF (DEB-1253710).	Albernaz AL, 2012, J BIOGEOGR, V39, P869, DOI 10.1111/j.1365-2699.2011.02640.x; Aleixo A, 2006, BIOL J LINN SOC, V89, P383, DOI 10.1111/j.1095-8312.2006.00703.x; Avise J.C., 2000, PHYLOGEOGRAPHY HIST, DOI [DOI 10.2307/J.CTV1NZFGJ7, 10.2307/j.ctv1nzfgj7]; Beheregaray L. B., 2015, EVOLUTIONARY POPULAT, V5, P477, DOI DOI 10.3389/FGENE.2014; Bravo G. 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I., 2016, HDB BIRDS WORLD ALIV	49	39	42	2	17	AMER ASSOC ADVANCEMENT SCIENCE	WASHINGTON	1200 NEW YORK AVE, NW, WASHINGTON, DC 20005 USA	2375-2548			SCI ADV	Sci. Adv.	MAR	2020	6	11							eaax4718	10.1126/sciadv.aax4718	http://dx.doi.org/10.1126/sciadv.aax4718			11	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	KW0MB	32195336	Green Published, gold			2023-06-23	WOS:000520866800002
J	Valasques, GS; dos Santos, AMP; de Souza, VS; Teixeira, LSG; Alves, JPS; Santos, MD; dos Santos, WPC; Bezerra, MA				Valasques, Gisseli S.; dos Santos, Ana Maria P.; de Souza, Valdinei S.; Teixeira, Leonardo S. G.; Alves, Juscelia P. S.; Santos, Mirela de Jesus; dos Santos, Wagna P. C.; Bezerra, Marcos A.			Multivariate optimization for the determination of cadmium and lead in crude palm oil by graphite furnace atomic absorption spectrometry after extraction induced by emulsion breaking	MICROCHEMICAL JOURNAL			English	Article						Crude palm oil; Extraction induced by emulsion breaking; GF AAS; Cadmium; Lead; Multivariate optimization	EDIBLE OILS; FOOD SAMPLES; PRECONCENTRATION; MICROEXTRACTION; SELENIUM; SYSTEMS; PB(II); IONS; TOOL	The present work reports the development of an analytical method for the determination of trace amounts of Cd and Pb in crude palm oil using graphite furnace atomic absorption spectrometry (GF AAS) after extraction induced by emulsion breaking (EIEB). The method was based on an oil-in-water emulsion preparation to promote a high contact area between the sample drops and the acid extractant solution. Emulsification was assisted by ultrasound energy using HNO3 and Triton X-114 surfactant solutions to increase the efficiency of the extraction. Afterwards, the emulsion was broken by heating, and the acid aqueous phase in the bottom of conical glass tubes was collected for the determination of metals by GF AAS. Cadmium and lead extraction was simultaneously optimized using Doehlert design and desirability function. The best extractions were achieved using a sonication time of 18 min, a HNO3 concentration of 2.0 mol L-1 and a surfactant concentration of 4.4% (v v(-1)) at a breaking temperature of 90 degrees C. The developed method presented quantification limits of 0.17 and 0.13 mu g kg(-1) and precisions (repeatability,%RSD, 10.8 mu g kg(-1)) of 1.8 and 5.4% for Cd and Pb, respectively. Addition/recovery tests gave results between 88.5% and 112%. The amounts of Cd and Pb in the analyzed samples ranged from 1.5-2.5 and 2.53-6.76 mu g kg(-1), respectively.	[Valasques, Gisseli S.; dos Santos, Ana Maria P.; de Souza, Valdinei S.; Teixeira, Leonardo S. G.] Univ Fed Bahia, Inst Quim, Rua Barao de Jeremoabo S-N, BR-40170115 Salvador, BA, Brazil; [de Souza, Valdinei S.] Inst Fed Educ Ciencia & Tecnol Baiano, Rodovia BR 116, BR-45320000 Santa Ines, BA, Brazil; [Alves, Juscelia P. S.; Santos, Mirela de Jesus; Bezerra, Marcos A.] Univ Estadual Sudoeste Bahia, Dept Ciencias & Tecnol, Rua Jose Moreira Sobrinho S-N, BR-45206190 Jequie, BA, Brazil; [dos Santos, Wagna P. C.] Inst Fed Educ Ciencias & Tecnol, Rua Emidio dos Santos, BR-40301015 Salvador, BA, Brazil	Universidade Federal da Bahia; Instituto Federal Baiano (IFBAIANO); Universidade Estadual do Sudoeste da Bahia	Bezerra, MA (autor correspondente), Univ Estadual Sudoeste Bahia, Dept Ciencias & Tecnol, Rua Jose Moreira Sobrinho S-N, BR-45206190 Jequie, BA, Brazil.	mbezerra@uesb.edu.br	Santos, Wagna/ABB-3281-2020; Santos, Wagna Piler/N-2337-2017; Teixeira, Leonardo S G/J-9131-2016	Santos, Wagna/0000-0001-7494-5179; Santos, Wagna Piler/0000-0001-7494-5179; Teixeira, Leonardo S G/0000-0003-0320-8299; de Jesus Santos, Mirela/0000-0002-9730-9009	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Fundagdo de Amparo a Pesquisa do Estado da Bahia (FAPESB); Financiadora de Estudos e Projetos (FINEP); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [304582/2018-2]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundagdo de Amparo a Pesquisa do Estado da Bahia (FAPESB); Financiadora de Estudos e Projetos (FINEP)(Financiadora de Inovacao e Pesquisa (Finep)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) Finance Code 001. The authors are also grateful to Fundagdo de Amparo a Pesquisa do Estado da Bahia (FAPESB), Financiadora de Estudos e Projetos (FINEP) and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq, Grant Number 304582/2018-2) for providing grants, fellowships and financial support.	[Anonymous], [No title captured]; [Anonymous], [No title captured]; Ansari R, 2009, FOOD CHEM, V115, P318, DOI 10.1016/j.foodchem.2008.11.051; Bezerra MA, 2008, TALANTA, V76, P965, DOI 10.1016/j.talanta.2008.05.019; Bezerra MA, 2019, TALANTA, V194, P941, DOI 10.1016/j.talanta.2018.10.088; Canario CM, 2005, J ANAL ATOM SPECTROM, V20, P1386, DOI 10.1039/b506627c; Cassella RJ, 2010, J ANAL ATOM SPECTROM, V25, P1704, DOI 10.1039/c0ja00035c; Dugo G, 2004, FOOD CHEM, V87, P639, DOI 10.1016/j.foodchem.2003.12.035; Edem DO, 2002, PLANT FOOD HUM NUTR, V57, P319, DOI 10.1023/A:1021828132707; Freschi GPG, 2001, SPECTROCHIM ACTA B, V56, P1987, DOI 10.1016/S0584-8547(01)00331-7; Geca I, 2017, TALANTA, V171, P321, DOI 10.1016/j.talanta.2017.05.008; Jurowski K, 2019, J TRACE ELEM MED BIO, V51, P73, DOI 10.1016/j.jtemb.2018.10.007; Khan S, 2014, SPECTROCHIM ACTA A, V123, P194, DOI 10.1016/j.saa.2013.12.065; Lima EC, 1998, SPECTROCHIM ACTA B, V53, P1791, DOI 10.1016/S0584-8547(98)00227-4; Lopez-Garcia I, 2014, TALANTA, V124, P106, DOI 10.1016/j.talanta.2014.02.011; Burguera JL, 2012, TALANTA, V96, P11, DOI 10.1016/j.talanta.2012.01.030; Burguera JL, 2011, TALANTA, V83, P691, DOI 10.1016/j.talanta.2010.11.018; Massart D. 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MAR	2020	153								104401	10.1016/j.microc.2019.104401	http://dx.doi.org/10.1016/j.microc.2019.104401			8	Chemistry, Analytical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	KM5ZR					2023-06-23	WOS:000514218800043
J	Veras, MM; Young, AS; Born, CR; Szewczuk, A; Neto, ACB; Petter, CO; Sampaio, CH				Veras, Moacir Medeiros; Young, Aaron Samuel; Born, Cristiano Rocha; Szewczuk, Artur; Bastos Neto, Artur Cezar; Petter, Carlos Otavio; Sampaio, Carlos Hoffmann			Affinity of dual energy X-ray transmission sensors on minerals bearing heavy rare earth elements	MINERALS ENGINEERING			English	Article						DE-XRT; Rare earth elements; Attenuated energy X-ray; Sensor-based sorting equipment	ALBITE-ENRICHED GRANITE; AMAZONIA; PITINGA; IMPACT	This work demonstrates the effective use of automatic sensor-based sorting technology as a viable separation method for rare earth element (REE) rich ores composed primarily of xenotime minerals with gagarinite-(Y) and fluocerite-(Ce, La) inclusions. A dual energy X-ray transmission (DE-XRT) sensor affinity was used to evaluate forty-two heavy rare earth element (HREE) ore grab samples from the Madeira deposit. These samples and separated products were scanned by the sensor under many operating parameters. Subsequent analyses, including petrographic and multi-element chemical analyses were performed on the grab samples. Specific mass tests were also compared with energy attenuation curves from the sensor, which correlated strongly with every concentration stage the highest achieved density being 3.01 g/cm(3). The best estimated HREE recovery from laboratory-scale sorting of the samples identified by the sensor was effectively 100%, however this occurred in conjunction with a mass recovery equal to 97% of the feed. Such results are expected knowing that the sample method was not entirely representative. Ongoing research into automatic sorting technology for the upgrading of Brazilian ores is being performed by the Federal University of Rio Grande do Sul (UFRGS), Brazil.	[Veras, Moacir Medeiros] Fed Inst Amapa IFAP, Min, Macapa, Brazil; [Young, Aaron Samuel] Univ Utah, Min Engn, Salt Lake City, UT 84112 USA; [Born, Cristiano Rocha; Bastos Neto, Artur Cezar] Univ Fed Rio Grande do Sul, Geosci Inst, Porto Alegre, RS, Brazil; [Szewczuk, Artur] COMEX AS, Innovat Ind Technol, Wroclaw, Poland; [Petter, Carlos Otavio] Univ Fed Rio Grande do Sul, Postgrad Program Min Engn Met & Mat, Porto Alegre, RS, Brazil; [Sampaio, Carlos Hoffmann] Univ Politecn Cataluna, Dept Engn Minera Ind & TIC, Barcelona Tech, Barcelona, Spain	Utah System of Higher Education; University of Utah; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universitat Politecnica de Catalunya	Young, AS (autor correspondente), Univ Utah, Min Engn, Salt Lake City, UT 84112 USA.	moacir.veras@ifap.edu.br; aaronsyoung@gmail.com; artur.s@comex-group.com; artur.bastos@ufrgs.br; cpetter@ufrgs.br; carlos.hoffmann@upc.edu		Hoffmann Sampaio, Carlos/0000-0001-5840-1614; Medeiros Veras, Moacir/0000-0001-7346-0225	IFAP	IFAP	The authors would like to thank CNPq, LAPROM and IGEO-UFRGS, Mineracao Taboca and the Federal Institute of Amapa (IFAP). Their contributions and encouragement helped to develop, initiate, support and collaborate this research. The last institution, IFAP, specifically, helped support the graduation of the doctoral candidate throughout the process of this work.	Bastos Neto A.C., 2010, CAN MINERAL, P1329; Neto ACB, 2014, PRECAMBRIAN RES, V243, P181, DOI 10.1016/j.precamres.2013.12.021; Neto ACB, 2012, CAN MINERAL, V50, P1453, DOI 10.3749/canmin.50.6.1453; Costa F.E., 2001, DESENVOLVIMENTO CONJ; Ferron J.M.T.M., 2016, REV BRASILEIRA GEOCI, V36, P499; Ferron JMTM, 2010, J S AM EARTH SCI, V29, P483, DOI 10.1016/j.jsames.2009.05.001; Gaastra M.B.A.M., 2014, SENSOR TECHNOLOGIES, P25; Gill C. 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Eng.	MAR 1	2020	147								106151	10.1016/j.mineng.2019.106151	http://dx.doi.org/10.1016/j.mineng.2019.106151			10	Engineering, Chemical; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Mineralogy; Mining & Mineral Processing	KM3MA		Green Submitted			2023-06-23	WOS:000514023900011
J	Vieira, DT; Porcher, CC; Koester, E; Ramos, RC; Gross, AOMD; Masquelin, H; Fernandes, LAD				Vieira, Daniel Triboli; Porcher, Carla Cristine; Koester, Edinei; Ramos, Rodrigo Chaves; da Silva Gross, Andreia Oliveira Monteiro; Masquelin, Henri; D'Avila Fernandes, Luis Alberto			Chafalote Metamorphic Suite (Uruguay): Reflections on the evolution of the Punta del Este Terrane	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						High-grade metamorphism; Neoproterozoic; Geochronology; U-Pb; Sm-Nd	DOM FELICIANO BELT; U-PB; MONAZITE GEOCHRONOLOGY; UHP METAMORPHISM; ZIRCON; SHRIMP; CONSTRAINTS; BRAZIL; COMPLEX; ARC	The Chafalote Metamorphic Suite, located in the Uruguayan sector of the Punta del Este Terrane, southeasternmost Dom Feliciano Belt, comprises semipelitic, migmatitic metapelites, mafic granulites, and calc-silicate/amphibolitic gneisses. These supracrustal rocks occur as roof pendants in a granodiorite belonging to the Cerro Olivo Complex. The main structure of the Chafalote Metamorphic Suite is a composite S-0/S-1 banding, related to the main deformation event (D-1) developed under upper-amphibolite/granulite fades conditions. This work presents an integrated study on the latter rocks, involving different geochronological methods (monazite U-Pb LA-ICP-MS and zircon U-Pb SHRIMP) and whole rock Sm-Nd isotope data in order to better understand the metamorphic evolution of the Chafalote Metamorphic Suite during the amalgamation of the SW Gondwana paleocontinent in thi Neoproterozoic. The studied rocks record a peak metamorphic event (M-2) occurred at around 660 Ma (monazite U-Pb ages), which was followed by decompression and partial melting (M-3 event) at around 640 Ma (zircon U-Pb ages), probably during the late stages of the D-1 event. The retrograde methamorphic event (M-4) is related to the transition between the D-1 and the development of NE-SW striking, lowgrade sinistral shear zones (D-2 event) and intrusion of syn-to post-orogenic Brasiliano granitoids of the Aigua Batholith at around 600 Ma. The metamorphic conditions, together with geochronological and isotopic similarities, allow the correlation between the studied high-grade metasedimentary rocks and those from the Paso del Dragon Complex in Uruguay, and from the Virzea do Capivarita, Arroio Grande, and Telho Complex in Brazil. The latter rocks possibly share similar source areas and represent different portions of the Neoproterozoic fore-arc and/or back-arc basins developed in the Dom Feliciano Belt during the Brasiliano/Pan-African orogenic cycle.	[Vieira, Daniel Triboli; Ramos, Rodrigo Chaves] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, POB 15001, BR-91501970 Porto Alegre, RS, Brazil; [Porcher, Carla Cristine; Koester, Edinei; D'Avila Fernandes, Luis Alberto] Univ Fed Rio Grande do Sul, Dept Geol, Bento Goncalves Ave 9500, BR-91540000 Porto Alegre, RS, Brazil; [da Silva Gross, Andreia Oliveira Monteiro] Serv Geol Brasil CPRM, POB 105, BR-90840030 Porto Alegre, RS, Brazil; [Masquelin, Henri] Univ Republica, Fac Ciencias, Inst Ciencias Geol, Igua 4225, Montevideo 11400, Uruguay	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidad de la Republica, Uruguay	Vieira, DT (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, POB 15001, BR-91501970 Porto Alegre, RS, Brazil.	daniel.triboli@ufrgs.br; carla.porcher@ufrgs.br; koester@ufrgs.br; rodrigo.chaves@ufrgs.br; andreia.gross@cprm.gov.br; hmasquel@fcien.edu.uy; ladfernandes@gmail.com	Porcher, Carla C/R-1419-2018; Koester, Edinei/L-3684-2017	Porcher, Carla C/0000-0002-0418-3954; Koester, Edinei/0000-0002-4424-4782; Vieira, Daniel/0000-0003-0616-5407; Masquelin, Henri/0000-0002-6385-9715; Chaves Ramos, Rodrigo/0000-0001-7116-5062	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [PqG 10/1509-0]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [140461/2016-7]	Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the anonymous reviewers for their insightful comments and suggestions on the manuscript. 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South Am. Earth Sci.	MAR	2020	98								102420	10.1016/j.jsames.2019.102420	http://dx.doi.org/10.1016/j.jsames.2019.102420			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KR5NJ					2023-06-23	WOS:000517664800001
J	Santos, AS; dos Santos, LO; dos Santos, IF; dos Santos, KR; Ferreira, SLC				Santos, Adilson S.; dos Santos, Liz O.; dos Santos, Ivanice F.; dos Santos, Kelly R.; Ferreira, Sergio L. C.			Application of chemometric tools for homogeneity and stability evaluation during the preparation of a powdered milk laboratory reference material for inorganic analysis	ANALYTICAL METHODS			English	Article							CERTIFIED REFERENCE MATERIAL; TOXIC ELEMENTS; TRACE-ELEMENTS; UNCERTAINTY; SPECTROMETRY; SAMPLES; FOOD; LEAD; CERTIFICATION; PRINCIPLES	Powdered milk and its derivatives are widely consumed worldwide, which require the development of reference materials for the evaluation of analytical methodologies that are developed for the analysis of these samples. In this work, the homogeneity and stability of a powdered milk laboratory reference material candidate were evaluated using chemometric tools as an alternative to analysis of variance (ANOVA). Elements Ca, Fe, K, Mg, P, Na and Zn were quantified by inductively coupled plasma optical emission spectrometry (ICP OES) after the acid digestion procedure using microwave-assisted radiation. The results obtained through not only ANOVA, but also PCA and HCA allow us to state that the material can be considered homogeneous and stable. However, the application of the chemometric tools (PCA and HCA) allowed the extraction of more information compared to ANOVA, besides confirming the homogeneity and stability of the powdered milk laboratory reference material candidate.	[Santos, Adilson S.; dos Santos, Liz O.; dos Santos, Ivanice F.; Ferreira, Sergio L. C.] Univ Fed Bahia, Inst Quim, Grp Pesquisa Quim & Quimiometria, Campus Ondina, BR-40170270 Salvador, BA, Brazil; [Santos, Adilson S.; dos Santos, Liz O.; dos Santos, Ivanice F.; Ferreira, Sergio L. C.] Univ Fed Bahia, INCT, Energia & Ambiente, Inst Nacl Ciencia & Tecnol, BR-40170290 Salvador, BA, Brazil; [dos Santos, Liz O.] Univ Fed Reconcavo Bahia, Ctr Ciencia & Tecnol Energia & Sustentabilidade C, BR-44042280 Feira De Santana, BA, Brazil; [dos Santos, Ivanice F.] Univ Estadual Feira de Santana, BR-44036900 Feira De Santana, BA, Brazil; [dos Santos, Kelly R.] Univ Fed Bahia, Inst Quim, Lab Catalise & Mat, Campus Ondina, BR-40170280 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal do Reconcavo da Bahia; Universidade Estadual de Feira de Santana; Universidade Federal da Bahia	Ferreira, SLC (autor correspondente), Univ Fed Bahia, Inst Quim, Grp Pesquisa Quim & Quimiometria, Campus Ondina, BR-40170270 Salvador, BA, Brazil.; Ferreira, SLC (autor correspondente), Univ Fed Bahia, INCT, Energia & Ambiente, Inst Nacl Ciencia & Tecnol, BR-40170290 Salvador, BA, Brazil.	slcf@ufba.br	FERREIRA, SERGIO LUIS SLCF COSTA/I-1993-2013; dos Santos, Liz Oliveira/Q-8289-2019	FERREIRA, SERGIO LUIS SLCF COSTA/0000-0001-7738-045X; dos Santos, Liz Oliveira/0000-0003-2064-2097; dos Santos, Ivanice/0000-0002-0390-2005	Conselho Nacional de Desenvolvimento Cientico e Tecnologico (CNPq); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001]	Conselho Nacional de Desenvolvimento Cientico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors are grateful to Conselho Nacional de Desenvolvimento Cientico e Tecnologico (CNPq), to Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB) and to Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) Finance Code 001 for providing grants and fellowships and for financial support.	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Methods	FEB 28	2020	12	8					1055	1063		10.1039/c9ay02184a	http://dx.doi.org/10.1039/c9ay02184a			9	Chemistry, Analytical; Food Science & Technology; Spectroscopy	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Food Science & Technology; Spectroscopy	KS8MZ					2023-06-23	WOS:000518562700012
J	Ampuero, A; Strikis, NM; Apaestegui, J; Vuille, M; Novello, VF; Espinoza, JC; Cruz, FW; Vonhof, H; Mayta, VC; Martins, VTS; Cordeiro, RC; Azevedo, V; Sifeddine, A				Ampuero, A.; Strikis, N. M.; Apaestegui, J.; Vuille, M.; Novello, V. F.; Espinoza, J. C.; Cruz, F. W.; Vonhof, H.; Mayta, V. C.; Martins, V. T. S.; Cordeiro, R. C.; Azevedo, V.; Sifeddine, A.			The Forest Effects on the Isotopic Composition of Rainfall in the Northwestern Amazon Basin	JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES			English	Article							STABLE-ISOTOPE; PRECIPITATION DELTA-O-18; CLIMATE CONTROLS; SOUTH-AMERICA; CENTRAL ANDES; D-EXCESS; WATER; VARIABILITY; MONSOON; CIRCULATION	In the Amazon basin, intense precipitation recycling across the forest significantly modifies the isotopic composition of rainfall (delta O-18, delta D). In the tropical hydrologic cycle, such an effect can be identified through deuterium excess (dxs), yet it remains unclear what environmental factors control dxs, increasing the uncertainty of dxs-based paleoclimate reconstructions. Here we present a 4-year record of the isotopic composition of rainfall, monitored in the northwestern Amazon basin. We analyze the isotopic variations as a function of the air mass history, based on atmospheric back trajectory analyses, satellite observations of precipitation upstream, leaf area index, and simulated moisture recycling along the transport pathway. We show that the precipitation recycling in the forest exerts a significant control on the isotopic composition of precipitation in the northwestern Amazon basin, especially on dxs during the dry season (r = 0.71). Applying these observations to existing speleothem and pollen paleorecords, we conclude that winter precipitation increased after the mid-Holocene, as the expansion of the forest allowed for more moisture recycling. Therefore, forest effects should be considered when interpreting paleorecords of past precipitation changes.	[Ampuero, A.; Strikis, N. M.; Cordeiro, R. C.; Azevedo, V.] Univ Fed Fluminense, Dept Geoquim, Niteroi, RJ, Brazil; [Apaestegui, J.] Inst Geofis Peru, Lima, Peru; [Vuille, M.] SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY 12222 USA; [Novello, V. F.; Cruz, F. W.; Martins, V. T. S.] Univ Sao Paulo, Inst Geociencia, Sao Paulo, Brazil; [Espinoza, J. C.] Univ Grenoble Alpes, Inst Geosci Environm, Grenoble INP, IRD,CNRS,IGE,UMR 5001, Grenoble, France; [Vonhof, H.] Max Planck Inst Chem, Dept Climate Geochem, Mainz, Germany; [Mayta, V. C.] Univ Sao Paulo, Dept Ciencias Atmosfer, IAG, Sao Paulo, Brazil; [Sifeddine, A.] Sorbonne Univ, CNRS, IRD, UPMC,MNHN,UMR LOCEAN,Ctr IRD, Bondy, France	Universidade Federal Fluminense; State University of New York (SUNY) System; State University of New York (SUNY) Albany; Universidade de Sao Paulo; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Communaute Universite Grenoble Alpes; Institut National Polytechnique de Grenoble; UDICE-French Research Universities; Universite Grenoble Alpes (UGA); Institut de Recherche pour le Developpement (IRD); Max Planck Society; Universidade de Sao Paulo; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Museum National d'Histoire Naturelle (MNHN); UDICE-French Research Universities; Sorbonne Universite	Ampuero, A (autor correspondente), Univ Fed Fluminense, Dept Geoquim, Niteroi, RJ, Brazil.	angelaampuero@id.uff.br	Espinoza, Jhan Carlo/A-9396-2011; Martins, Veridiana T S/O-4235-2015; Cordeiro, Renato C/J-8870-2013; Vuille, Mathias/O-8128-2019; Cruz, Francisco W/G-6059-2012; Sifeddine, Abdel/H-9828-2015; Novello, Valdir F./P-5824-2015; Misailidis Strikis, Nicolas/H-6531-2015	Espinoza, Jhan Carlo/0000-0001-7732-8504; Martins, Veridiana T S/0000-0002-5886-4974; Cordeiro, Renato C/0000-0002-6785-601X; Vuille, Mathias/0000-0002-9736-4518; Novello, Valdir F./0000-0002-0120-3745; Apaestegui, James/0000-0002-9761-1806; Vonhof, Hubert/0000-0002-0897-8244; Cruz, Francisco/0000-0002-4030-4581; Mayta, Victor C/0000-0003-4037-1722; Misailidis Strikis, Nicolas/0000-0003-4721-3380; Ampuero Grandez, Angela/0000-0002-1264-9152; Azevedo Alves, Vitor/0000-0002-1893-1618	CAPES Grant; BELMONT FORUM PACMEDY [ANR-15-JCLI0003-03]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [423573/2018-7]; CLIMATE-PRINTUFF Project (CAPES) [88887.310301/2018-00]; Sao Paulo Research Foundation (FAPESP) Grant [2016/15807-5]; PIRE NSF-FAPESP Grant [2017/50085-3]; U.S. National Science Foundation NSF Grants [AGS-1303828, OISE1743738]; French AMANECER-MOPGA project - ANR, France [ANR-18-MPGA-0008]; IRD, France [ANR-18-MPGA-0008]; National Science Foundation [AGS-1841559]	CAPES Grant(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); BELMONT FORUM PACMEDY; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CLIMATE-PRINTUFF Project (CAPES); Sao Paulo Research Foundation (FAPESP) Grant(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); PIRE NSF-FAPESP Grant; U.S. National Science Foundation NSF Grants(National Science Foundation (NSF)); French AMANECER-MOPGA project - ANR, France(French National Research Agency (ANR)); IRD, France; National Science Foundation(National Science Foundation (NSF))	This study was undertaken as part of the PALEOTRACES project (IRD) in collaboration with the Instituto Geofisico del Peru (IGP) and supported by the CAPES Grant and ANR-15-JCLI0003-03 BELMONT FORUM PACMEDY. N. M. S. received support of Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) Grant 423573/2018-7 and CLIMATE-PRINTUFF Project (CAPES Grant 88887.310301/2018-00); V. F. N received support of Sao Paulo Research Foundation (FAPESP) Grant 2016/15807-5; F. W. C. received support of PIRE NSF-FAPESP Grant 2017/50085-3; M. V. received support of the U.S. National Science Foundation NSF Grants AGS-1303828 and OISE1743738; J. C. E. received support of the French AMANECER-MOPGA project funded by ANR and IRD, France (ref. ANR-18-MPGA-0008). V. M. is supported by the National Science Foundation under Grant AGS-1841559. We acknowledge NOAA Air Resources Laboratory (ARL) for the provision of the HYSPLIT transport and dispersion model and READY website (http://www.ready.noaa.gov) used in this publication. The data used in this paper were acquired from Goddard Earth System division and Information Service Center [TRMM 3B42 and GPM); http://disc.sci.gsfc.nasa.gov/] and ECMWF (ERA Interim reanalysis; http://apps.ecmwf.int/datasets/). The MODIS data used in this study were obtained from the USGS's Land Processes Distributed Archive Center MODIS (https://lpdaac.usgs.gov/). The manuscript was improved by the insightful comments of two anonymous reviewers.	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Geophys. Res.-Atmos.	FEB 27	2020	125	4							e2019JD031445	10.1029/2019JD031445	http://dx.doi.org/10.1029/2019JD031445			16	Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Meteorology & Atmospheric Sciences	KT7XS		Green Published, Bronze			2023-06-23	WOS:000519227000018
J	Tavares, GND; Boggiani, PC; Leme, JD; Trindade, RI				Tavares, Guilherme Navarro D.; Boggiani, Paulo Cesar; de Moraes Leme, Juliana; Trindade, Ricardo Ivan			The Inventory of the Geological and Paleontological Sites in the Area of the Aspirant Geopark Bodoquena-Pantanal in Brazil	GEOHERITAGE			English	Article						Geoconservation; Geoheritage; Geopark; Geopark Bodoquena-Pantanal; GEOSSIT; Inventory	SERRA-DA-BODOQUENA; GROSSO-DO-SUL; MATO-GROSSO; QUATERNARY MAMMALS; LUCIANOI BEURLEN; URUCUM DISTRICT; EDIACARAN; IRON; EVOLUTION; DEPOSITS	The interest in geoparks in Brazil began after the inclusion of the Araripe Geopark into the Global Geopark Network (GGN) in 2006. After that, several areas within Brazil were proposed as potential geoparks, two of which were then formalized-the Quadrilatero Ferrifero (Minas Gerais) and Bodoquena-Pantanal (Mato Grosso do Sul), and formal applications were submitted to GGN in 2010 but not accepted. In spite of the relevance in the geology and paleontology of both areas, the refusals were due to being only a project and not an actual functioning structured geopark yet working. No kind of inventory or quantification of the geological sites was carried out to both of the proposed geoparks. Furthermore, the purpose of the present work is to present an inventory of the sites of the area proposed for the Geopark Bodoquena-Pantanal (GBP) in an effort to demonstrate the significance of the geological heritage of the area. The area of the GBP includes Ediacaran animal fossils, which provide information about the geological record just before the Cambrian Explosion. This record created international interest in the area, together with sections with that record of global changes that characterized the end of the Neoproterozoic Eon, such as the iron formations of the Urucum Massif (Rapitan type) and Marinoan glacial sediments and limestone (Tamengo Formation). The present inventory was compiled by the GEOSSIT platform of the Geological Survey of Brazil (CPRM), which is based on the method of Brilha (2016), with modifications. The 51 sites investigated were distributed among 6 geological frameworks, defined to represent the geological history of the region, and 26 sites were considered as geosites, of which 12 present international relevance, specifically the sites of Corumba Group, due to the importance for the investigation of the Ediacaran period. The inventory and its numerical result show the scientific importance of the area, as already recognized by international meetings and publications on the geology, and is useful to future plan and revision of the proposed geopark.	[Tavares, Guilherme Navarro D.; Boggiani, Paulo Cesar; de Moraes Leme, Juliana] Univ Sao Paulo, Inst Geosci IGc USP, Sao Paulo, Brazil; [Trindade, Ricardo Ivan] Univ Sao Paulo, Inst Astron Geophys & Atmospher Sci IAG USP, Sao Paulo, Brazil	Universidade de Sao Paulo; Universidade de Sao Paulo	Tavares, GND (autor correspondente), Univ Sao Paulo, Inst Geosci IGc USP, Sao Paulo, Brazil.	guilherme.navarro.tavares@usp.br	de Moraes Leme, Juliana/C-3335-2012; Trindade, Ricardo IF/A-8146-2008	de Moraes Leme, Juliana/0000-0002-5833-4885; Trindade, Ricardo IF/0000-0001-9848-9550; Tavares, Guilherme/0000-0003-1315-4212	Sao Paulo Research Foundation (FAPESP) [2016/06114-6, 2017/07226-5]	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The study was supported by the Sao Paulo Research Foundation (FAPESP), by thematic project (Proc. 2016/06114-6), coordinated by Prof. Ricardo I. Trindade (Instituto de Astronomia e Ciencias Atmosfericas-USP), and scholarship (2017/07226-5) to the first author (Tavares GND). The authors (Boggiani PC, Leme, J. and Trindade, RC) are fellow researchers of the CNPq-Conselho Nacional de Pesquisa do Brasil (Proc. 307234/2016-9).	Adorno RR, 2017, PRECAMBRIAN RES, V301, P19, DOI 10.1016/j.precamres.2017.08.023; Almeida F.F.M., 1945, B DIVISAO GEOLOGIA M, V116, P1; Almeida FFM, 1946, B DIVISAO GEOLOGIA E, V119, P1; Alvarenga C.J.S., 1993, REV BRAS GEOSCI, V23, P18, DOI [10.25249/0375-7536.19932311830, DOI 10.25249/0375-7536.19932311830]; Babinski M, 2013, GONDWANA RES, V23, P988, DOI 10.1016/j.gr.2012.06.011; Becker-Kerber B, 2017, SCI REP-UK, V7, DOI 10.1038/s41598-017-05753-8; Boggiani P. 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F, 1987, AN 10 C BRAS PAL RIO, V2, P797; ZAINE MF, 1985, AN ACAD BRAS CIENC, V57, P130	62	8	8	1	7	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1867-2477	1867-2485		GEOHERITAGE	Geoheritage	FEB 22	2020	12	1							28	10.1007/s12371-020-00437-8	http://dx.doi.org/10.1007/s12371-020-00437-8			22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KS0RJ					2023-06-23	WOS:000518018900001
J	Boroni, NL; Perini, FA; Boggiani, P; Almeida, LHS; Toledo, PM; Salles, LO				Boroni, Natalia L.; Perini, Fernando A.; Boggiani, Paulo; Sapiensa Almeida, Luis Henrique; Toledo, Peter Mann; Salles, Leandro O.			Quaternary sigmodontines (Mammalia, Rodentia) from Serra da Bodoquena, Mato Grosso do Sul, Brazil	HISTORICAL BIOLOGY			English	Article						Sigmodontinae; Bibimys; Graomys; Thalpomys; Cerrado; Pantanal	BUENOS-AIRES PROVINCE; CRICETIDAE SIGMODONTINAE; ATLANTIC FOREST; GENUS HOLOCHILUS; CENTRAL ARGENTINA; CALOMYS RODENTIA; LATE PLEISTOCENE; SKULL VARIATION; LATE HOLOCENE; MARSH RATS	Sigmodontine rodents are extremely diversified in the Neotropics but their fossil record remains generally poorly known, especially in Brazil. Here, we examine the assemblage of sigmodontines from the limestone cave Nossa Senhora Aparecida (21 degrees 5MODIFIER LETTER PRIME27.89"S 56 degrees 34MODIFIER LETTER PRIME28.77"W), located in Serra da Bodoquena (Mato Grosso do Sul), a karstic region in southwestern Brazil. We describe cranial and dental fragments and recognise the presence of some new species not previously recorded for the region, as Bibimys sp., Graomys cf. G. chacoensis, Thalpomys lasiotis, and Pseudoryzomys simplex. This fossil assemblage is comparable to others fossil sites in Brazil, such as those from Goias and Rio Grande do Sul, with the predominance of species from open areas, including grasslands, and some of forested environments from Cerrado landscapes.	[Boroni, Natalia L.; Perini, Fernando A.] Univ Fed Minas Gerais, Programa Posgrad Zool, Ave Antonio Carlos 6627,Campus UFMG, BR-31270901 Belo Horizonte, MG, Brazil; [Boroni, Natalia L.; Perini, Fernando A.] Univ Fed Minas Gerais, Dept Zool, Inst Ciencias Biol, Belo Horizonte, MG, Brazil; [Boroni, Natalia L.; Salles, Leandro O.] Univ Fed Rio de Janeiro, Museu Nacl, Dept Vertebrados Mastozool, Rio De Janeiro, Brazil; [Boggiani, Paulo] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil; [Sapiensa Almeida, Luis Henrique] Univ Fed Rio de Janeiro, Inst Geociencias, Rio De Janeiro, Brazil; [Toledo, Peter Mann] INPE, Ctr Ciencia Sistema Terrestre, Sao Paulo, Brazil; [Salles, Leandro O.] Amer Museum Nat Hist, Vertebrate Zoool, New York, NY 10024 USA	Universidade Federal de Minas Gerais; Universidade Federal de Minas Gerais; Universidade Federal do Rio de Janeiro; Universidade de Sao Paulo; Universidade Federal do Rio de Janeiro; Instituto Nacional de Pesquisas Espaciais (INPE); American Museum of Natural History (AMNH)	Boroni, NL (autor correspondente), Univ Fed Minas Gerais, Programa Posgrad Zool, Ave Antonio Carlos 6627,Campus UFMG, BR-31270901 Belo Horizonte, MG, Brazil.; Boroni, NL (autor correspondente), Univ Fed Minas Gerais, Dept Zool, Inst Ciencias Biol, Belo Horizonte, MG, Brazil.; Boroni, NL (autor correspondente), Univ Fed Rio de Janeiro, Museu Nacl, Dept Vertebrados Mastozool, Rio De Janeiro, Brazil.	natalia_boroni@hotmail.com	Toledo, Peter M/P-3618-2015; Perini, Fernando/I-1452-2012	Toledo, Peter M/0000-0003-4265-2624; Perini, Fernando/0000-0002-4336-9284	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work was supported by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) -Finance Code 001.	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Avulsos Zool. (São Paulo), V55, P47, DOI 10.1590/0031-1049.2015.55.03; Voglino D, 2005, AMEGHINIANA, V42, P143; Voglino Damián, 2004, Mastozool. neotrop., V11, P243; Voss Robert S., 2015, P443; Voss Robert S., 1993, American Museum Novitates, V3085, P1; VOSS RS, 1991, B AM MUS NAT HIST, P414; Weksler M., 2005, ARQUIVOS MUSEU NACL, V63, P113; WEKSLER M., 2015, MAMMALS S AM, V2, P417, DOI DOI 10.7208/CHICAGO/9780226169606.001.0001; Weksler M, 2017, AM MUS NOVIT, P1; Weksler M, 2006, AM MUS NOVIT, P1, DOI 10.1206/0003-0082(2006)3537[1:TNGOOR]2.0.CO;2; Winge H., 1887, MUSEO LUNDII, V1, P1, DOI DOI 10.5962/BHL.TITLE.14696	176	5	5	0	0	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0891-2963	1029-2381		HIST BIOL	Hist. Biol.	SEP 2	2021	33	9					1598	1623		10.1080/08912963.2020.1722659	http://dx.doi.org/10.1080/08912963.2020.1722659		FEB 2020	26	Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Paleontology	UQ5BM					2023-06-23	WOS:000514067200001
J	Gastauer, M; Caldeira, CF; Ramos, SJ; Trevelin, LC; Jaffe, R; Oliveira, G; Vera, MPO; Pires, E; Santiago, FLD; Carneiro, MAC; Coelho, FTA; Silva, R; Souza, PWM; Siqueira, JO				Gastauer, Markus; Caldeira, Cecilio Frois; Ramos, Silvio Junio; Trevelin, Leonardo Carreira; Jaffe, Rodolfo; Oliveira, Guilherme; Ortiz Vera, Mabel Patricia; Pires, Eder; de Aguiar Santiago, Flavia Louzeiro; Carbone Carneiro, Marco Aurelio; Asoa Coelho, Felipe Tadashi; Silva, Rosilene; Souza-Filho, Pedro Walfir M.; Siqueira, Jose-Oswaldo			Integrating environmental variables by multivariate ordination enables the reliable estimation of mineland rehabilitation status	JOURNAL OF ENVIRONMENTAL MANAGEMENT			English	Article						Environmental monitoring; Ecological processes; Functional diversity; Environmental indicators; Primers for environmental rehabilitation; Urucum massif	RESTORATION SUCCESS; ECOLOGICAL RESTORATION; FUNCTIONAL DIVERSITY; VEGETATION STRUCTURE; FOREST RESTORATION; ORGANIC-CARBON; INDICATORS; BIODIVERSITY; FRACTIONS	Despite the wide variety of variables commonly employed to measure the success of rehabilitation, the assessment and subsequent definition of indicators of environmental rehabilitation status are not simple tasks. The main challenges are comparing rehabilitated sites with target ecosystems as well as integrating individual environmental and eventually collinear variables into a single tractable measure for the state of a system before effective indicators that track rehabilitation may be modeled. Furthermore, a consensus is lacking regarding which and how many variables need to be surveyed for a reliable estimation of rehabilitation status. Here, we propose a multivariate ordination to integrate variables related to ecological processes, vegetation structure, and community diversity into a single estimation of rehabilitation status. As a case, we employed a curated set of 32 environmental variables retrieved from nonrevegetated, rehabilitating and reference sites associated with iron ore mines from the Urucum Massif, Mato Grosso do Sul, Brazil. By integrating this set of environmental variables into a single estimation of rehabilitation status, the proposed multivariate approach is straightforward and able to adequately address collinearity among variables. The proposed methodology allows for the identification of biases towards single variables, surveys or analyses, which is necessary to rank environmental variables regarding their importance to the assessment. Furthermore, we show that bootstrapping permitted the detection of the minimum number of environmental variables necessary to achieve reliable estimations of the rehabilitation status. Finally, we show that the proposed variable integration enables the definition of case-specific environmental indicators for more rapid assessments of mineland rehabilitation. Thus, the proposed multivariate ordination represents a powerful tool to facilitate the diagnosis of rehabilitating sites worldwide provided that sufficient environmental variables related to ecological processes, diversity and vegetation structure are gathered from nonrehabilitated, rehabilitating and reference study sites. By identifying deviations from predicted rehabilitation trajectories and providing assessments for environmental agencies, this proposed multivariate ordination increases the effectiveness of (mineland) rehabilitation.	[Gastauer, Markus; Caldeira, Cecilio Frois; Ramos, Silvio Junio; Trevelin, Leonardo Carreira; Jaffe, Rodolfo; Oliveira, Guilherme; Ortiz Vera, Mabel Patricia; Pires, Eder; Souza-Filho, Pedro Walfir M.; Siqueira, Jose-Oswaldo] Inst Tecnol Vale, Rua Boaventura Silva 955, Belem, Para, Brazil; [Ortiz Vera, Mabel Patricia] Univ Fed Para, Programa Posgrad Genet & Biol Mol, Rua Augusto Correa 01, Belem, Para, Brazil; [de Aguiar Santiago, Flavia Louzeiro; Carbone Carneiro, Marco Aurelio] Univ Fed Lavras, Dept Ciencias Solo, Lavras, MG, Brazil; [Asoa Coelho, Felipe Tadashi; Silva, Rosilene] Vale Diretoria Ferrosos Ctr Oeste, Rua Cabral 1555, Corumba, MS, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Universidade Federal do Para; Universidade Federal de Lavras	Gastauer, M (autor correspondente), Inst Tecnol Vale, Rua Boaventura Silva 955, Belem, Para, Brazil.	markus.gastauer@itv.org	Trevelin, Leonardo/AAX-3233-2021; Jaffé, Rodolfo/K-3230-2013; Souza-Filho, Pedro Walfir M. M./J-4958-2012; Frois, Cecilio/HQZ-9386-2023; Gastauer, Markus/GMW-6022-2022; Souza, Pedro/GZH-1275-2022; Frois Caldeira, Cecilio/O-7184-2018	Trevelin, Leonardo/0000-0002-1041-6902; Jaffé, Rodolfo/0000-0002-2101-5282; Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; Frois Caldeira, Cecilio/0000-0003-4762-3515; Louzeiro de Aguiar, Flavia/0000-0003-3764-7468	Vale; CNPq [153535/2018-0, 305831/2016-0, 301616/2017-5, 402756/2018-5, 307479/2016-1, 306430/2013-5, 303580/2013-5]; CAPES [88887.130628/2016-00]; BBSRC under the Global Challenges Research Fund (GCRF) Growing Research Capability call [BB/P027849/1]; CABANA; BBSRC [BB/P027849/1] Funding Source: UKRI	Vale; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); BBSRC under the Global Challenges Research Fund (GCRF) Growing Research Capability call(UK Research & Innovation (UKRI)Biotechnology and Biological Sciences Research Council (BBSRC)); CABANA; BBSRC(UK Research & Innovation (UKRI)Biotechnology and Biological Sciences Research Council (BBSRC))	This work was funded by Vale (Canga Plant & Soil to PWMSF and Canga Plant Genomics to GO), and received additional support by CNPq to MG (153535/2018-0), SJR (305831/2016-0), RJ (301616/2017-5), GO (402756/2018-5, 307479/2016-1), PWMSF (306430/2013-5) and JOS (303580/2013-5), by CAPES to GO (88887.130628/2016-00), and by CABANA to GO, who was funded by the BBSRC under the Global Challenges Research Fund (GCRF) Growing Research Capability call, contract number BB/P027849/1 (www.ukri.org/research/global-ch allenges-research-fund/funded-projects/). We are grateful for the valuable comments of four anonymous reviewers.	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Environ. Manage.	FEB 15	2020	256								109894	10.1016/j.jenvman.2019.109894	http://dx.doi.org/10.1016/j.jenvman.2019.109894			9	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	KN9XK	31989973	Green Submitted			2023-06-23	WOS:000515200400042
J	Sial, AN; Chen, JB; Lacerda, LD; Korte, C; Spangenberg, JE; Silva-Tamayo, JC; Gaucher, C; Ferreira, VP; Barbosa, JA; Pereira, NS; Benigno, AP				Sial, A. N.; Chen, Jiubin; Lacerda, L. D.; Korte, C.; Spangenberg, J. E.; Silva-Tamayo, J. C.; Gaucher, C.; Ferreira, V. P.; Barbosa, J. A.; Pereira, N. S.; Benigno, A. P.			Globally enhanced Hg deposition and Hg isotopes in sections straddling the Permian-Triassic boundary: Link to volcanism	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						C isotopes; Hg/TOC chemostratigraphy; Hg isotopes; Hg source; Permian-Triassic transition	CRETACEOUS-PALEOGENE BOUNDARY; LARGE IGNEOUS PROVINCES; MASS EXTINCTION; MEISHAN SECTION; DECCAN VOLCANISM; MERCURY ISOTOPES; SOUTH CHINA; PERMIAN/TRIASSIC BOUNDARY; ORGANIC GEOCHEMISTRY; STRATOTYPE SECTION	Mercury (Hg/TOC) spikes from eight Permian-Triassic boundary (PTB) sections in this study display patterns similar to each other across the so-called extinction interval as well as strong variation in sedimentation rates from section to section. Mercury may have been originated from the synchronous magmatism of the Siberian Traps Large Igneous Province (STLIP). At the GSSP in Meishan, China, Hg/TOC peaks were observed in the latest Permian mass extinction interval (LPME) and Early Triassic mass extinctions (ETME). The successions at Hovea-3 (Australia), Ursula Creek (Canada), Idrijca (Slovenia), Rizvanusa (Croatia) exhibit Hg/TOC peaks at the LPME and PTB. The Rizvanusa section displays one peak at the ETME horizon, Zal and Abadeh (Iran) successions at the LPME and ETME horizons, while Misci/Seres (Tyrol/Italy) section shows an enrichment at the LPME. The largest Hg/TOC peaks at the LPME, PTB and ETME are, perhaps, linked to the beginning of stage 2 (extrusive hiatus) of the Siberian Traps LIP. The meaning of the Hg/TOC spike between the LPME event and the PTB in seven of these sections is fuzzy. In the delta Hg-202 (MDF) vs Delta Hg-201 (MIF) cross plot, the majority of samples from the extinction interval appear within the volcanic-emission box and a few samples plot in the sediment/soil/peat box. Hg-isotope signatures resulted from mixing processes of volcanic and normal marine sediment Hg, generating four horizontal trends whose Delta Hg-201 shows negligible to no variation. Less terrigenous-Hg influx was noticed in the sections closer to the STLIP (Rizvanusa, Idrijca and Seres/Misci, all in Europe) in which Delta Hg-201 (MIF) is close to zero. Marked influence occurs in sections far distant from the STLIP (Meishan, Ursula Creek and Hovea-3) that exhibit negative Delta Hg-201 (MIF). The two sections from Iran, at intermediate distance from the STLIP, exhibit the highest, positive Delta Hg-201 values (Abadeh section) and the lowest, negative Delta Hg-201 values (Zal section). A Delta Hg-199 (MIF) vs Hg (n.ng(-1)) cross plot suggests that volcanic Hg has been contaminated by normal marine source-Hg influx in these sections helping to shape two major curved trends. The negative C-isotope excursions and Hg/TOC enrichments in the studied sections are nearly coeval and this supports the hypothesis of synchronism between the Permian-Triassic transition biotic crises (LPME and ETME) and the start of the stage 2 of the Siberian Traps (sill-intrusion style of magmatism).	[Sial, A. N.; Ferreira, V. P.] Univ Fed Pernambuco, Dept Geol, NEG LABISE, BR-50740530 Recife, PE, Brazil; [Chen, Jiubin] Tianjin Univ, Inst Surface Earth Syst Sci, 92 Weijin Rd, Tianjin 300072, Peoples R China; [Lacerda, L. D.; Benigno, A. P.] Univ Fed Ceara, Inst Marine Sci, LABOMAR, BR-60165081 Fortaleza, Ceara, Brazil; [Korte, C.] Univ Copenhagen, Dept Geosci & Nat Resource Management, Oster Voldgade 10, DK-1350 Copenhagen, Denmark; [Spangenberg, J. E.] Univ Lausanne, Inst Earth Surface Dynam IDYST, CH-1015 Lausanne, Switzerland; [Silva-Tamayo, J. C.] Antonio Narino Univ, Fac Sci, Circunvalar Campus, Bogota, Colombia; [Gaucher, C.] Univ Republica, Fac Ciencias, Inst Ciencias Geol, Montevideo, Uruguay; [Barbosa, J. A.] Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil; [Pereira, N. S.] Univ Estado Bahia, Dept Biol, Campus 8, Paulo Afonso, Brazil	Universidade Federal de Pernambuco; Tianjin University; Universidade Federal do Ceara; University of Copenhagen; University of Lausanne; Universidad Antonio Narino; Universidad de la Republica, Uruguay; Universidade Federal de Pernambuco; Universidade do Estado Bahia	Sial, AN (autor correspondente), Univ Fed Pernambuco, Dept Geol, NEG LABISE, BR-50740530 Recife, PE, Brazil.	sial@ufpe.br	Korte, Christoph/F-2599-2015; Benigno, ANA/AAV-7209-2020; Sial, Alcides/AAD-1901-2021; BARBOSA, JOSE ANTONIO/AAB-4437-2020; Pereira, Natan S/A-9643-2015	Korte, Christoph/0000-0001-5974-9516; BARBOSA, JOSE ANTONIO/0000-0001-8754-6310; Pereira, Natan S/0000-0002-3307-2655; Spangenberg, Jorge E./0000-0001-8636-6414	NSFC [CNPq 471036/2012-9, 407171/2018-5, 1073-1.07/15, CNPq INCT-TMCOcean 573.601/2008-9, CNPq 576.601/2009-1, APQ1738-1.07/12]; Danish Natural Science Research Council [41625012, U1612442, 41830647, 41561134017]; University of Lausanne [11-103378, FNS-SCOPES IB7320-110885];  [290]	NSFC(National Natural Science Foundation of China (NSFC)); Danish Natural Science Research Council(Danish Natural Science Research Council); University of Lausanne; 	Grants to ANS (CNPq 471036/2012-9, 407171/2018-5; FACEPE APQ-1059-9.05/12, 1073-1.07/15), to LDL (CNPq INCT-TMCOcean 573.601/2008-9, CNPq 576.601/2009-1), to VPF (CNPq 471034/2012-6; FACEPE APQ1738-1.07/12) and NSFC grants to JBC (41625012, U1612442, 41830647, 41561134017) provided financial support to chemical and/or isotope analyses. CK thanks the Freie Universitat Berlin for sampling in South Tyrol and the Danish Natural Science Research Council for providing financial support for sampling in China and to QuanFeng Zheng for leading him in the field in Meishan (grant number 11-103378). JES acknowledges Tadej Dolenec for providing samples from the Idrijca Valley section, the FNS-SCOPES IB7320-110885 and the University of Lausanne for financial support for sampling of Croatian sections and all geochemical analyses. JCST wants to express his gratitude to Robert Newton and Paul Wignall by the cession of samples from Ursula Creek section and to Klity Grice for providing samples from the Hovea-3. We are grateful to Prof. Jun Shen (China University of Geosciences, Wuhan) and to an anonymous reviewer whose comments and suggestions on an earlier version of the manuscript greatly contributed to improve it. This is the NEG-LABISE scientific contribution n. 290.	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Paleoclimatol. Paleoecol.	FEB 15	2020	540								109537	10.1016/j.palaeo.2019.109537	http://dx.doi.org/10.1016/j.palaeo.2019.109537			20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	KL2WW					2023-06-23	WOS:000513290300005
J	Martinez, F; Lopez, C; Parra, M				Martinez, Fernando; Lopez, Cristopher; Parra, Mauricio			Effects of pre-orogenic tectonic structures on the Cenozoic evolution of Andean deformed belts: Evidence from the Salar de Punta Negra Basin in the Central Andes of Northern Chile	BASIN RESEARCH			English	Article							DE-ATACAMA BASIN; SALTA RIFT; CORDILLERA; STRATIGRAPHY; INVERSION; INSIGHTS; ARC; ARCHITECTURE; DEFORMATION; ARGENTINA	We integrated new field observations, two-dimensional (2-D) seismic profiles and new and previously reported chronological data to understand the effects of pre-orogenic structures on the tectonic evolution of the Salar de Punta Negra in the Central Andes. For first time a series of restored geological cross-sections are presented, thus showing the pre-orogenic tectonic architecture of the region and new ideas about the tectonic evolution of the inner forearc of the Central Andes. Our results show a series of east-dipping normal faults as the main pre-orogenic structures in the region, which resulted from lithospheric stretching of the western continental margin during the Paleozoic to Mesozoic (Triassic-Jurassic). These were later incorporated into the Andean orogen by tectonic inversion, forming west-verging inversion anticlines. The beginning of the tectonic inversion is constrained by the first on-lap of the Upper Cretaceous-Palaeocene syn-kinematic deposits on the top of the Mesozoic syn-rift successions, highlighting that inversion occurred during this period. These syn-kinematic deposits display zircons with older age peaks between ca. 200 and 300 Ma, thus indicating that some Carboniferous to Triassic sources of sediments were eroded during the uplift of the orogen. Other basement reverse faults affect the footwalls of normal inverted faults and the shoulders of ancient half-graben structures. These truncate and decapitate previous inverted faults and completely cut the infill of the basin, leading to exhumation of the pre-rift basement rocks. We propose that the propagation of these structures was favoured by the modified thermal-tectonic state of the lithosphere from the eastward migration of the volcanic arc, and not by the previous pre-orogenic structures. The structural and stratigraphic relationships recognized both in the field and 2-D seismic profiles indicate that many reverse faults originated after the initial tectonic inversion and continued to be active from the Eocene until the Pleistocene period.	[Martinez, Fernando; Lopez, Cristopher] Univ Catolica Norte, Fac Ingn & Ciencias Geol, Dept Ciencias Geol, Antofagasta 0610, Chile; [Parra, Mauricio] Univ Sao Paulo, Inst Energy & Environm, Sao Paulo, Brazil	Universidad Catolica del Norte; Universidade de Sao Paulo	Martinez, F (autor correspondente), Univ Catolica Norte, Fac Ingn & Ciencias Geol, Dept Ciencias Geol, Antofagasta 0610, Chile.	fernando.martinez@ucn.cl	Parra, Mauricio/B-7497-2013	Parra, Mauricio/0000-0002-5955-6105; MARTINEZ, FERNANDO/0000-0002-4461-4392	Fondo Nacional de Desarrollo Cientifico y Tecnologico [11170098]	Fondo Nacional de Desarrollo Cientifico y Tecnologico(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDECYT)	Fondo Nacional de Desarrollo Cientifico y Tecnologico, Grant/Award Number: 11170098	Allmendinger RW, 1997, ANNU REV EARTH PL SC, V25, P139, DOI 10.1146/annurev.earth.25.1.139; Amilibia A, 2008, J STRUCT GEOL, V30, P1520, DOI 10.1016/j.jsg.2008.08.005; Ardill J, 1998, J GEOL SOC LONDON, V155, P71, DOI 10.1144/gsjgs.155.1.0071; Arriagada C, 2006, TECTONICS, V25, DOI 10.1029/2004TC001770; Arriagada C, 2000, TECTONOPHYSICS, V326, P153, DOI 10.1016/S0040-1951(00)00151-7; Baby P, 1997, GEOLOGY, V25, P883, DOI 10.1130/0091-7613(1997)025<0883:NSCTCT>2.3.CO;2; BAHLBURG H, 1991, J S AM EARTH SCI, V4, P171, DOI 10.1016/0895-9811(91)90029-K; Bascunan S, 2019, TECTONOPHYSICS, V759, P58, DOI 10.1016/j.tecto.2019.04.008; Bascunan S, 2016, BASIN RES, V28, P365, DOI 10.1111/bre.12114; Bloch W, 2014, GEOPHYS J INT, V197, P1744, DOI 10.1093/gji/ggu084; Breitkreuz C, 1996, J S AM EARTH SCI, V9, P281, DOI 10.1016/S0895-9811(96)00014-4; Butler R. 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J	Montefeltro, FC; Bronzati, M; Langer, MC; Anelli, LE				Montefeltro, Felipe C.; Bronzati, Mario; Langer, Max C.; Anelli, Luiz E.			A new specimen of Susisuchus anatoceps (Crocodyliformes, Neosuchia) with a non-eusuchian-type palate	JOURNAL OF VERTEBRATE PALEONTOLOGY			English	Article							MESOEUCROCODYLIA; ORIGIN		[Montefeltro, Felipe C.] Univ Estadual Paulista, Fac Engn Ilha Solteira, Dept Biol & Zootecnia, Rua Moncao 226, BR-15385000 Ilha Solteira, SP, Brazil; [Bronzati, Mario; Langer, Max C.] Univ Sao Paulo, Fac Filosofia Ciencias & Letras Ribeirao Preto, Dept Biol, Ave Bandeirantes 3900, BR-14040901 Ribeirao Preto, SP, Brazil; [Anelli, Luiz E.] Univ Sao Paulo, Dept Geol Sedimentar & Ambiental, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil	Universidade Estadual Paulista; Universidade de Sao Paulo; Universidade de Sao Paulo	Montefeltro, FC (autor correspondente), Univ Estadual Paulista, Fac Engn Ilha Solteira, Dept Biol & Zootecnia, Rua Moncao 226, BR-15385000 Ilha Solteira, SP, Brazil.	fc.montefeltro@unesp.br; mariobronzati@gmail.com; mclanger@ffclrp.usp.br; luizeduardo.anelli@gmail.com	Anelli, Luiz Eduardo/AAC-4753-2021; Montefeltro, Felipe Chinaglia/AAQ-4003-2020; Langer, Max/F-7483-2012	Montefeltro, Felipe Chinaglia/0000-0001-6519-8546; Langer, Max/0000-0003-1009-4605				Benton M.J., 1988, Systematics Association Special Volume Series, P295; de Andrade MB, 2011, ZOOL J LINN SOC-LOND, V163, pS66, DOI 10.1111/j.1096-3642.2011.00709.x; De Andrade Marco Brandalise, 2006, REVISTA BRASILEIRA DE PALEONTOLOGIA, V9, P323; Dollman KN, 2018, AM MUS NOVIT, P1; Fortier DC, 2009, PALAEONTOLOGY, V52, P991, DOI 10.1111/j.1475-4983.2009.00894.x; Hart LJ, 2019, PEERJ, V7, DOI 10.7717/peerj.7166; Hay O. P., 1930, CARNEGIE I WASHINGTO, V2, P1; Leite KJ, 2018, PEERJ, V6, DOI 10.7717/peerj.5372; Montefeltro FC, 2013, NATURWISSENSCHAFTEN, V100, P835, DOI 10.1007/s00114-013-1083-9; Noto CR, 2020, ANAT REC, V303, P801, DOI 10.1002/ar.24174; Pol D, 2009, B AM MUS NAT HIST, P1; Salisbury SW, 2006, P ROY SOC B-BIOL SCI, V273, P2439, DOI 10.1098/rspb.2006.3613; Salisbury SW, 2003, PALAEONTOGR ABT A, V270, P3; Sayao JM, 2016, PLOS ONE, V11, DOI 10.1371/journal.pone.0155297; Tennant JP, 2016, ZOOL J LINN SOC-LOND, V177, P854, DOI 10.1111/zoj.12400; Turner AH, 2015, PLOS ONE, V10, DOI 10.1371/journal.pone.0118116; Turner AH, 2015, PEERJ, V3, DOI 10.7717/peerj.759	17	1	1	0	1	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0272-4634	1937-2809		J VERTEBR PALEONTOL	J. Vertebr. Paleontol.	SEP 3	2019	39	5							e1716240	10.1080/02724634.2019.1716240	http://dx.doi.org/10.1080/02724634.2019.1716240		FEB 2020	4	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	LA1ZB					2023-06-23	WOS:000514498600001
J	Loureiro, AMS; da Paz, SPA; Veiga, MD; Angelica, RS				Silva Loureiro, Alexandre Maximo; Aranha da Paz, Simone Patricia; Veiga, Maria do Rosario; Angelica, Romulo Simoes			Investigation of historical mortars from Belem do Para, Northern Brazil	CONSTRUCTION AND BUILDING MATERIALS			English	Article						Architectural heritage; Restoration; Old mortar; Mineralogical composition; Building conservation; Chemical composition; Wall coating system; Characterization; Ancient technology; Brazilian mortars	CEMENT MORTARS; LIME MORTARS; ANCIENT; CONSERVATION; RESTORATION; BYZANTINE; VATERITE; CHURCH; TOWER	Belem do Para, founded in 1616, still has layers of lime mortar on its historical buildings, which recurrently need restorative interventions. Intervention strategies need to include the use of building materials compatible with the original materials and, therefore, a good characterization of the original composition is necessary for the restoration of historical monuments. Thus, the main objective of this paper is the chemical, physical, and mineralogical characterization of historical mortars in Belem do Pars from the 18th and 19th centuries, as well as to evaluate their physical and mechanical properties. The results obtained showed the type of mortars used in different buildings and their main components, as well as the mortars behavior that helped the durability of the historic masonries. The conclusions leaded to useful information for seculars mortars restoration of northern Brazil. (C) 2019 Elsevier Ltd. All rights reserved.	[Silva Loureiro, Alexandre Maximo; Aranha da Paz, Simone Patricia; Angelica, Romulo Simoes] Fed Univ Para, Inst Geosci, Lab Mineral Characterizat LCM, Belem, Para, Brazil; [Silva Loureiro, Alexandre Maximo] Fed Univ Para, Inst Technol, Lab Conservat Restorat & Rehabil LACORE, Belem, Para, Brazil; [Veiga, Maria do Rosario] Natl Lab Civil Engn LNEC, Dept Bldg, Lisbon, Portugal	Universidade Federal do Para; Universidade Federal do Para; National Civil Engineering Laboratory	Loureiro, AMS (autor correspondente), Univ Fed Para, Lab Caracterizacao Mineral, Av Augusto Correa 1, BR-66075110 Belem, PA, Brazil.	ams.loureiro1@gmail.com	Paz, Simone Patricia Aranha/AAF-3059-2019; Veiga, Rosário/A-7100-2013; Angelica, Romulo/G-6245-2010	Paz, Simone Patricia Aranha/0000-0002-5880-7638; Veiga, Rosário/0000-0002-7135-8603; Angelica, Romulo/0000-0002-3026-5523; Loureiro, Alexandre/0000-0003-3341-2653	CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior); CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)	CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the Brazilian agencies: CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) and CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico), for a PhD scholarship to the first author. We also acknowledge the laboratories where the research was developed for the laboratory and personnel support: a) Laboratory of Mineral Characterization (LCM); b) Laboratory of Conservation, Restoration and Rehabilitation (LACORE); c) Department of Buildings of National Laboratory of Civil Engineering (LNEC); d) Laboratory of Scanning Electron Microscopy (LABMEV); e) Laboratory of Petrography (LABPET); and f) Laboratory of Sedimentology (LABSED). In special, thanks to Aldemir Sotero and Bruna Sena (LCM), Anabela Manteigas and Dora Santos (LNEC), Drs. Rose Norat and Thais Sanjad (LACORE). We also thank DPHAC (Departamento de Patrimonio Historic, Artistico e Cultural do Estado do Para) for the permission to collect the samples used in this research. The authors also thank ProReitoria de Pesquisa e Pos-Graduacao (Universidade Federal do Para) for the translation of the paper by Programa de Apoio a Publicacao Qualificada (EDITAL PAPQ 2018).	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FEB 10	2020	233								117284	10.1016/j.conbuildmat.2019.117284	http://dx.doi.org/10.1016/j.conbuildmat.2019.117284			16	Construction & Building Technology; Engineering, Civil; Materials Science, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Construction & Building Technology; Engineering; Materials Science	KL2YS					2023-06-23	WOS:000513295100049
J	Araujo, GS; Gusso-Choueri, PK; Favaro, DIT; Rocha, RCC; Saint'Pierre, TD; Hauser-Davis, RA; Braz, B; Santelli, RE; Freire, AS; Machado, WTV; Cruz, ACF; Abessa, DMS				Araujo, G. S.; Gusso-Choueri, P. K.; Favaro, D. I. T.; Rocha, R. C. C.; Saint'Pierre, T. D.; Hauser-Davis, R. A.; Braz, B.; Santelli, R. E.; Freire, A. S.; Machado, W. T. V.; Cruz, A. C. F.; Abessa, D. M. S.			Metal-Associated Biomarker Responses in Crabs from a Marine Protected Area in Southeastern Brazil	ARCHIVES OF ENVIRONMENTAL CONTAMINATION AND TOXICOLOGY			English	Article							CALLINECTES-DANAE S.; SAO-PAULO; BLUE-CRAB; SEDIMENT QUALITY; EXPOSURE; METALLOTHIONEIN; CONTAMINATION; TOXICITY; STRESS; WATER	The environmental quality of a Ramsar wetland site located at the Cananeia-Iguape-Peruibe Protected Area (CIP-PA), in Sao Paulo, Brazil, was assessed by geochemical analyses and biomarker assessments (GPx, GST, GSH, GST, MT, LPO, DNA damage) performed in swimming crab Callinectes danae Smith, 1869 organs (posterior and anterior gills and hepatopancreas) to estimate sediment contaminant bioavailability. The results indicated that two sampling stations, PT and PM, exhibited the worst environmental conditions, as sediments collected at both points contained metal contamination, while crabs exhibited significant responses for GPx, GST, and LPO (mostly during winter). Sediment contamination tended to be associated to fine sediments (both seasons) and organic matter (winter). During the summer survey, Pb concentrations in sediments of station PT exceeded the Brazilian Sediment Quality Guidelines (SQGs) and the Canadian Interim Marine Sediment Quality Guidelines. Metal concentrations in sediments sampled in winter were higher compared with summer, with Co, Ni, and Pb exceeding SQGs levels at PT, whereas Co, Ni, Hg, Zn, and Pb exceeded SQGs at PM. Biomarker induction during summer appeared to be caused by natural variables (water salinity and temperature, and molting cycle), whereas oxidative stress and tissue damage during winter appeared to be more clearly linked to metal contamination. Anterior gills presented the clearest signs of seasonal variability, being more responsive to sediment contamination. The results suggest that metals originated from the upper Ribeira de Iguape River are transported toward the estuarine system, causing effects on C. danae individuals. Additionally, seasonality is a strong factor concerning CIP-PA toxicity, since the rainfall regime significantly modifies the freshwater flow and, consequently, estuarine water salinity, suspended particle and metal inputs, as well as the location of depositional areas. Thus, efforts to mitigate CIP-PA contamination should be based on the control of upstream pollution sources.	[Araujo, G. S.; Cruz, A. C. F.] Univ Sao Paulo, Inst Oceanog, Sao Paulo, SP, Brazil; [Araujo, G. S.; Gusso-Choueri, P. K.; Cruz, A. C. F.; Abessa, D. M. S.] Univ Estadual Paulista Julio de Mesquita Filho UN, NEPEA, Campus Litoral Paulista, Sao Vicente, Brazil; [Favaro, D. I. T.] IPEN Nucl & Energy Res Inst, Res Reactor Ctr, Sao Paulo, Brazil; [Rocha, R. C. C.; Saint'Pierre, T. D.] Pontificia Univ Catolica Rio de Janeiro, Dept Chem QUI, Rio De Janeiro, Brazil; [Hauser-Davis, R. A.] Fundacao Oswaldo Cruz, Lab Avaliacao & Promocao Saude Ambiental, Inst Oswaldo Cruz, Rio De Janeiro, Brazil; [Braz, B.; Santelli, R. E.; Freire, A. S.] Univ Fed Rio de Janeiro, Inst Quim, Rio De Janeiro, RJ, Brazil; [Machado, W. T. V.] Univ Fed Fluminense, Programa Posgrad Geoquim, Dept Geoquim, Niteroi, RJ, Brazil	Universidade de Sao Paulo; Universidade Estadual Paulista; Comissao Nacional de Energia Nuclear (CNEN); Instituto de Pesquisas Energeticas e Nucleares (IPEN); Pontificia Universidade Catolica do Rio de Janeiro; Fundacao Oswaldo Cruz; Universidade Federal do Rio de Janeiro; Universidade Federal Fluminense	Araujo, GS (autor correspondente), Univ Sao Paulo, Inst Oceanog, Sao Paulo, SP, Brazil.; Araujo, GS (autor correspondente), Univ Estadual Paulista Julio de Mesquita Filho UN, NEPEA, Campus Litoral Paulista, Sao Vicente, Brazil.	giuliana_araujo@hotmail.com	Favaro, Deborah Ines Teixeira/AAJ-6136-2021; Gusso-Choueri, Paloma K/H-8222-2012; Cruz, Ana/AAQ-7172-2021; Hauser-Davis, Rachel Ann/C-7970-2013; Abessa, Denis/D-6507-2014; Araujo, Giuliana/F-8482-2018	Favaro, Deborah Ines Teixeira/0000-0002-0083-2523; Hauser-Davis, Rachel Ann/0000-0002-9451-471X; Abessa, Denis/0000-0003-4609-1668; Machado, Wilson/0000-0003-3117-8584; Ferreira Braz, bernardo/0000-0001-8280-2047; Saint Pierre, Tatiana/0000-0002-7619-5620; Araujo, Giuliana/0000-0002-8942-6969	Sao Paulo Research Foundation (FAPESP) [09/52762-6]; National Council for Scientific and Technological Development (CNPq) [479899/2013-4]; CNPq [303620/2008-0, 311609/2014-7, 311820/2017-4, 308649/2011]	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors thank the Sao Paulo Research Foundation (FAPESP, grant #09/52762-6) for financial support and the National Council for Scientific and Technological Development (CNPq) for Giuliana S. Araujo's master's fellowship (grant #479899/2013-4). Paloma K. Gusso-Choueri thanks the Coordination for the Qualification of Higher Level Staff in Brazil (CAPES). Tatiana D. Saint' Pierre thanks CNPq for grant #311820/2017-4. The authors are also grateful to the USP Oceanographic Institute for providing support to the field work in Cananeia. DMSA would like to thank CNPq for fellowships and financial support (grants #303620/2008-0, #308649/2011-and #311609/2014-7).	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Environ. Contam. Toxicol.	APR	2020	78	3					463	477		10.1007/s00244-020-00710-5	http://dx.doi.org/10.1007/s00244-020-00710-5		FEB 2020	15	Environmental Sciences; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Toxicology	KV4DR	32034428				2023-06-23	WOS:000515942500001
J	de Souza, VS; Teixeira, LSG; Lima, JSSO; Cerqueira, UMFD; de Oliveira, OMC; Queiroz, AFD; Bezerra, MA				de Souza, Valdinei Santos; Sena Gomes Teixeira, Leonardo; Lima, Joaly Sthefane Santos Oliveira; Ferreira da Mata Cerqueira, Uillian Mozart; Cordeiro de Oliveira, Olivia Maria; Queiroz, Antonio Fernando de Souza; Almeida Bezerra, Marcos			Analytical strategies for spectrometric determination of vanadium in samples of interest in the petroleum industry	APPLIED SPECTROSCOPY REVIEWS			English	Review						Vanadium; atomic spectrometry; petroleum industry; sample preparation	ATOMIC-ABSORPTION-SPECTROMETRY; MICROWAVE-INDUCED COMBUSTION; HEAVY CRUDE-OIL; INDUCED BREAKDOWN SPECTROSCOPY; OPTICAL-EMISSION SPECTROMETRY; PLASMA-MASS-SPECTROMETRY; ICP-MS; SPECIATION ANALYSIS; ELECTROTHERMAL VAPORIZATION; QUANTITATIVE-DETERMINATION	Vanadium is a trace metal that is found in crude oil and its derivatives, in water from oil production, and in rocks. Methods to determine the amount of vanadium in these materials is of great interest to the petroleum industry. Its presence is related to problems of corrosion in processing plants, poisoning of catalysts, undesirable side reactions in refining operations and it is in air pollution from burning fuels. In addition, the ratio of V/Ni concentration can be used to reveal the geographical origin of oil. In this review, strategies using atomic spectrometry techniques for the determination of vanadium in samples of interest to the petroleum industry are discussed. The analytical techniques already consolidated and those that have been developed in recent years, as well as methods of sample preparation are approached.	[de Souza, Valdinei Santos; Sena Gomes Teixeira, Leonardo] Univ Fed Bahia, Inst Quim, Dept Quim Analitica, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [de Souza, Valdinei Santos] Inst Fed Educ Ciencia & Tecnol Baiano, Campus Santa Ines, BR-45320000 Santa Ines, BA, Brazil; [Lima, Joaly Sthefane Santos Oliveira; Ferreira da Mata Cerqueira, Uillian Mozart; Almeida Bezerra, Marcos] Univ Estadual Sudoeste Bahia, Lab Quim Analitica, BR-45206190 Jequie, BA, Brazil; [Cordeiro de Oliveira, Olivia Maria; Queiroz, Antonio Fernando de Souza] Univ Fed Bahia, Inst Geociencias, Campus Univ Ondina, BR-40170290 Salvador, BA, Brazil	Universidade Federal da Bahia; Instituto Federal Baiano (IFBAIANO); Universidade Estadual do Sudoeste da Bahia; Universidade Federal da Bahia	Bezerra, MA (autor correspondente), Univ Estadual Sudoeste Bahia, Dept Ciencias & Tecnol, Campus Jequie,Rua Jose Moreira Sobrinho S-N, BR-45206190 Jequie, BA, Brazil.	mbezerra@uesb.edu.br	Queiroz, Antonio Fernando de Souza/ABH-6682-2020; de Oliveira, Olivia Maria Cordeiro/AAB-3246-2021; Teixeira, Leonardo S G/J-9131-2016; da Mata Cerqueira, Uillian Mozart Ferreira/AAT-9297-2020	Teixeira, Leonardo S G/0000-0003-0320-8299; da Mata Cerqueira, Uillian Mozart Ferreira/0000-0002-2158-379X				Ahmed A, 2016, SAE INT J FUELS LUBR, V9, P460, DOI 10.4271/2016-01-2166; Akinlua A, 2013, ANAL METHODS-UK, V5, P4929, DOI 10.1039/c3ay40278a; Ali MF, 2006, FUEL PROCESS TECHNOL, V87, P573, DOI 10.1016/j.fuproc.2006.03.001; Aliakbari A, 2014, MICROCHIM ACTA, V181, P1931, DOI 10.1007/s00604-014-1279-5; AlSwaidan HM, 1996, TALANTA, V43, P1313, DOI 10.1016/0039-9140(96)01885-1; Amato R, 2016, ELIFE, V5, DOI 10.7554/eLife.08714; Amorim FAC, 2007, TALANTA, V72, P349, DOI 10.1016/j.talanta.2006.12.015; Amorim FAC, 2007, J BRAZIL CHEM SOC, V18, P1566, DOI 10.1590/S0103-50532007000800018; Korn MDA, 2008, APPL SPECTROSC REV, V43, P67, DOI 10.1080/05704920701723980; Korn MDA, 2007, TALANTA, V73, P1, DOI 10.1016/j.talanta.2007.03.036; [Anonymous], 2013, N 1, V17, DOI DOI 10.1093/NDT/GFV100; ASTM, 2002, ANN BOOK ASTM STAND, DOI [10.1520/E0096, DOI 10.1520/D1238-13]; Aucelio RQ, 2004, MICROCHEM J, V78, P21, DOI 10.1016/j.microc.2004.02.018; Aydin I, 2010, OIL SHALE, V27, P331, DOI 10.3176/oil.2010.4.06; Aydin I, 2013, MICROCHEM J, V108, P64, DOI 10.1016/j.microc.2012.12.001; Bader NR., 2011, RASAYAN J CHEM, V4, P49, DOI DOI 10.1016/0584-8547(96)01507-8; Barceloux DG, 1999, J TOXICOL-CLIN TOXIC, V37, P265, DOI 10.1081/CLT-100102425; BERMEJOBARRERA P, 1990, ANAL CHIM ACTA, V236, P475, DOI 10.1016/S0003-2670(00)83353-X; Bettmer J, 2012, ANAL BIOANAL CHEM, V402, P269, DOI 10.1007/s00216-011-5420-6; Bjerketvedt D., 2015, GAS EXPLOSION HDB; Bok R., 1984, HDB DECOMPOSITION ME; Burguera JL, 2003, TALANTA, V61, P353, DOI 10.1016/S0039-9140(03)00275-3; Butler OT, 2016, J ANAL ATOM SPECTROM, V31, P35, DOI 10.1039/c5ja90061a; Silveira ELC, 2010, QUIM NOVA, V33, P1863, DOI 10.1590/S0100-40422010000900008; Cassella RJ, 2012, J ANAL ATOM SPECTROM, V27, P364, DOI 10.1039/c2ja10279j; Cassella RJ, 2011, FUEL PROCESS TECHNOL, V92, P933, DOI 10.1016/j.fuproc.2010.12.013; Cassella RJ, 2010, J ANAL ATOM SPECTROM, V25, P1704, DOI 10.1039/c0ja00035c; Caumette G, 2009, J ANAL ATOM SPECTROM, V24, P263, DOI 10.1039/b817888g; Christopher SJ, 2016, ANAL CHEM, V88, P4635, DOI 10.1021/acs.analchem.5b03981; Coetzee P. 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Spectrosc. Rev.	FEB 7	2020	55	2					128	157		10.1080/05704928.2018.1542600	http://dx.doi.org/10.1080/05704928.2018.1542600			30	Instruments & Instrumentation; Spectroscopy	Science Citation Index Expanded (SCI-EXPANDED)	Instruments & Instrumentation; Spectroscopy	LP1NX					2023-06-23	WOS:000534087600003
J	McLachlan, RL; Ogston, AS; Asp, NE; Fricke, AT; Nittrouer, CA; Gomes, VJC				McLachlan, R. L.; Ogston, A. S.; Asp, N. E.; Fricke, A. T.; Nittrouer, C. A.; Gomes, V. J. C.			Impacts of tidal-channel connectivity on transport asymmetry and sediment exchange with mangrove forests	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Sediment transport; Sediment dynamics; Mangrove swamps; Tidal channels; Tidal asymmetry; Amazon River	TURBIDITY MAXIMUM; ESTUARY; CURRENTS; PROGRADATION; DYNAMICS; HABITAT; EROSION; FISHES; SWAMP; BASIN	Mangrove forests provide many valuable services, including wave- and tidal-energy dissipation, sediment accumulation, and substrate stabilization. But, their global extent is rapidly shrinking. Sedimentary research that is needed to inform restoration projects has so far focused on characterizing flow patterns through forests associated with single rivers, nearshore environments, or terminating tidal channels. However, flows within the most extensive mangrove forests tend to be driven through channels that connect to multiple estuaries or other channels with temporally lagged tides. For this study, in-situ observations of water and sediment flux were obtained in two tidal channels near the Amazon River to characterize how connectivity impacts sediment transport in coastal mangrove forests. The low-connectivity channel connects to one estuary whereas the high-connectivity channel connects two estuaries. We conclude that channel connectivity controls the amount of sediment stored in channels that is available to supply mangrove forests. Although phase-duration asymmetry is flood dominant in both channels, velocity asymmetry becomes ebb dominant during tidal cycles when the mangrove flats are inundated. Additionally, tidal elevation and water velocity are not in quadrature for the high-connectivity channel, as they are for the low-connectivity channel. As a result, the high-connectivity channel acts as a conduit for sediment from one estuary to another rather than simply importing and retaining sediment like the low-connectivity channel. High-connectivity channels distribute point-source sediment along coastlines and provide sediment to estuaries and channels that may not have their own direct source. As restoration efforts of mangrove forests continue to grow in response to coastal threats such as sea-level rise and diminished fluvial-sediment delivery, the location of these efforts can benefit from the conclusion that channel connectivity influences spatial dispersal of sediment supply to mangrove forests.	[McLachlan, R. L.; Ogston, A. S.; Fricke, A. T.; Nittrouer, C. A.] Univ Washington, Sch Oceanog, Box 357940, Seattle, WA 98103 USA; [Asp, N. E.; Gomes, V. J. C.] Univ Fed Para, Inst Estudos Costeiros, Braganca, Para, Brazil	University of Washington; University of Washington Seattle; Universidade Federal do Para	McLachlan, RL (autor correspondente), Univ Washington, Sch Oceanog, Box 357940, Seattle, WA 98103 USA.	mclachlan.rl@gmail.com; ogston@uw.edu; nilsasp@ufpa.br; atfricke@uw.edu; nittroue@uw.edu; vandojcg@yahoo.com.br	Asp, Nils/J-6226-2012	Asp, Nils/0000-0002-6468-6158	U.S. Office of Naval Research [N00014-15-1-2011, N00014-13-1-0127, N00014-13-1-0781]; U.S. Office of Naval Research Global [N62909-14-1-N205]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [3290/2013]; National Science Foundation [DGE1256082]	U.S. Office of Naval Research(Office of Naval Research); U.S. Office of Naval Research Global(Office of Naval Research); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Science Foundation(National Science Foundation (NSF))	We thank everyone in the Universidade Federal do Path Institute of Coastal Studies and the University of Washington Sediment Dynamics Lab for their generous efforts in the field and lab. This work was supported by the U.S. Office of Naval Research [grant numbers N00014-15-1-2011, N00014-13-1-0127, N00014-13-1-0781], the U.S. Office of Naval Research Global [grant number N62909-14-1-N205], and the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [Finance Code 3290/2013]. This material is based upon work supported by the National Science Foundation Graduate Research Fellowship under Grant No. DGE1256082. Any opinion, findings, and conclusions or recommendations expressed in this material are those of the authors(s) and do not necessarily reflect the views of the National Science Foundation.	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Coast. Shelf Sci.	FEB 5	2020	233								106524	10.1016/j.ecss.2019.106524	http://dx.doi.org/10.1016/j.ecss.2019.106524			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	KO3JT		Bronze			2023-06-23	WOS:000515445400021
J	Alencar, DR; De Oliveira, GR; Pinheiro, AP; Saraiva, AAF				Alencar, Damares Ribeiro; De Oliveira, Gustavo Ribeiro; Pinheiro, Allysson Pontes; Feitosa Saraiva, Antonio Alamo			New findings on Dendrobranchiata fossils of the Romualdo Formation, Araripe Basin, Northeast of Brazil	ZOOTAXA			English	Article						Cretaceous; Fossil Sergestids; Redescription; Taxonomy; Penaeoidea	CONTROLLED EXCAVATIONS; SEDIMENTARY BASIN; CARIDEAN SHRIMP; CRUSTACEA; DECAPODA; GENUS	The Araripe Basin is the largest inland basin in northeastern Brazil is known for its preservation excellent, number of specimens and variety of fossil species. The Araripc Basin stands out for its fossiliferous content of well known fossil groups, from vertebrates to invertebrates, especially dccapod crustaceans. Thus, a morphological re-description of two shrimp species, Paleomattea deliciosa and Araripenaeus timidus, was carried out through taxonomic and moiphoanatomical analysis. The mechanical preparation methodology was adopted in the laboratory, with a total of 58 specimens were analyzed and photographed to determine which characters were preserved or not, as well as to compared these with holotypes. The results show that characters such as carapaces complete with the presence of spines, pleon with six somites, pereiopods and pleopods, in addition to uropods and telson were preserved in Paleomattea deliciosa, while carapaces, pleon complete and pereiopods were preserved in Araripenaeus timidus. Thus, the current study provides new species information which can be used in future species-type studies and contributes to a better understanding of these Araripe species.	[Alencar, Damares Ribeiro; Pinheiro, Allysson Pontes; Feitosa Saraiva, Antonio Alamo] Univ Reg Cariri URCA, Dept Ciencias Biol, Rua Carolino Sucupira S-N, BR-63100000 Crato, CE, Brazil; [De Oliveira, Gustavo Ribeiro] Univ Fed Rural Pernambuco UFRPE, Rua Dom Manuel de Medeiros, BR-52171900 Recife, PE, Brazil	Universidade Regional do Cariri; Universidade Federal Rural de Pernambuco (UFRPE)	Alencar, DR (autor correspondente), Univ Reg Cariri URCA, Dept Ciencias Biol, Rua Carolino Sucupira S-N, BR-63100000 Crato, CE, Brazil.	damarisalencar@hotmail.com; gustavoliveira@mail.com; allysson.pinheiro@urca.br; alamocariri@yahoo.com.br	Pinheiro, Allysson/AAH-1785-2020; Oliveira, Gustavo R/F-7432-2012; Saraiva, António/HPD-3031-2023; Oliveira, Gustavo/IQW-7983-2023	Pinheiro, Allysson/0000-0003-1565-6371; Oliveira, Gustavo R/0000-0002-9871-1235; 	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [BP3-00139-00166.01.07/18, BP3-0139-00202.01.00/18, BMD-0008-01255.01.04/17]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We would like to thank the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for financial support to the authors for the research (#BP3-00139-00166.01.07/18; BP3-0139-00202.01.00/18, BMD-0008-01255.01.04/17). We would also like to thank the Fundacao Cearense de Apoio ao Desenvolvimento Cientifico e Tecnologico (FUNCAP) and the Financiadora de Estudos e Projetos (FINEP) for the provided equipment, in addition to other partner institutions such as the Universidade Regional do Cariri (URCA), Universidade Federal Rural de Pernambuco (UFRPE) and the Universidade Federal de Pernambuco (UFPE). We thank RIBEIRO, J.E. for the graphical illustrations and MUNIZ, C. A. for the board collaborations and FAUSTINO, H. for their help with the map.	AGASSIZ L, 1841, EDINBURGH NEW PHILOS, V30, P82; Alencar DR, 2018, ZOOTAXA, V4527, P494, DOI 10.11646/zootaxa.4527.4.2; Assine M. 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M. M., 2003, Geologica Acta, V1, P261	42	1	2	0	1	MAGNOLIA PRESS	AUCKLAND	PO BOX 41383, AUCKLAND, ST LUKES 1030, NEW ZEALAND	1175-5326	1175-5334		ZOOTAXA	Zootaxa	FEB 4	2020	4731	1					63	74		10.11646/zootaxa.4731.1.4	http://dx.doi.org/10.11646/zootaxa.4731.1.4			12	Zoology	Science Citation Index Expanded (SCI-EXPANDED)	Zoology	KK0CW	32229828				2023-06-23	WOS:000512421100004
J	Almeida, ND; Sawakuchi, HO; Teixeira, CAS; Bertassoli, DJ; Furukawa, LY; Pelissari, M; Sawakuchi, AO				Almeida, Nazare da Silva; Sawakuchi, H. O.; Teixeira, C. A. S.; Bertassoli, D. J., Jr.; Furukawa, L. Y.; Pelissari, M.; Sawakuchi, A. O.			Incubation experiments to constrain the production of methane and carbon dioxide in organic-rich shales of the Permian Irati Formation, Parana Basin	MARINE AND PETROLEUM GEOLOGY			English	Article						Shallow gas systems; Shale gas; Parting basin; irati shale	MICROBIAL-PRODUCTION; ANAEROBIC-DIGESTION; FLUID INCLUSIONS; TEMPERATURE; GAS; BIODEGRADATION; GENERATION; HYDROGEN; PALEOTEMPERATURES; METHANOGENESIS	The Permian Irati Formation in Brazil hosts organic-rich shales and heavy hydrocarbons suitable for biogenic production of methane (CH4) and carbon dioxide (CO2). In this study, shale samples from the irati Formation were used in laboratory incubation experiments performed under different temperatures (22 degrees C, 50 degrees C, 70 degrees C and 80 degrees C) to evaluate the generation of CH4 and CO2 under thermal conditions compatible with biodegradation in shallow gas systems (< 80 degrees C). Despite our laboratory experiments do not represent natural subsurface temperature conditions, it is observed that the concentrations of CH4 and CO2 increase when shale samples are incubated under temperature higher than 22 degrees C. Samples incubated at 80 degrees C presented a maximum CH4 yield of 2.45 ml/t.d (milliliter per ton of shale per day) compared to 0,49 ml/t.d at 22 degrees C, 1.75 ml/t.d at 50 degrees C and 2.09 ml/t.d at 70 degrees C. The same trend of increasing production rates with higher temperatures was observed for CO2, with maximum potential production observed under a laboratory temperature of 80 degrees C, reaching 23.47 ml/t.d. Stable carbon isotopes (delta C-13) on CH4 and CO2 suggest a mixture of thermogenic and secondary microbial gas. However, the measured CH4 and CO2 can be generated through methanogenic degradation of heavy hydrocarbons present in the studied shales, difficulting the use of carbon isotope composition to discriminate between biogenic and thermogenic gases. The studied shale samples showed significant differences in CH4 and CO2 production rates, which are possibly related to the major elements composition of the mineral matrix. Higher CH4 and CO2 production rates occurred in samples with higher amount of sulfur. Besides sulfur, we highlight that others soluble elements in the mineral matrix, such as Ca and Mg, can play an important role for the generation of biogenic CH4 and CO2. The present work intends to alert for the importance of thermal conditions as well as the geochemical composition of the mineral matrix to build conceptual models about shallow gas systems, acting on organic-rich shales in sedimentary basins.	[Almeida, Nazare da Silva; Teixeira, C. A. S.; Bertassoli, D. J., Jr.; Furukawa, L. Y.; Pelissari, M.; Sawakuchi, A. O.] Univ Sao Paulo, Inst Geosci, Sedimentary & Environm Geol Dept, Rua Lago 562, Sao Paulo, SP, Brazil; [Sawakuchi, H. O.] Umea Univ, Dept Ecol & Environm Sci, KBC Huset, Linnaeus Vag 6, S-90187 Umea, Sweden; [Sawakuchi, H. O.] Linkoping Univ, Dept Themat Studies Environm Change, Campus Valla, S-58183 Linkoping, Sweden	Universidade de Sao Paulo; Umea University; Linkoping University	Almeida, ND (autor correspondente), Univ Sao Paulo, Inst Geosci, Sedimentary & Environm Geol Dept, Rua Lago 562, Sao Paulo, SP, Brazil.	nazare.almeida@thenavigatorcompany.com	Sawakuchi, André O/D-1445-2013; Oliveira Sawakuchi, Henrique/ABA-9796-2021; Pelissari, Maria Rogieri/AAC-2798-2021; Bertassoli, Dailson Jose/U-7335-2019; Oliveira Sawakuchi, Henrique/K-6194-2014	Bertassoli, Dailson Jose/0000-0003-3141-8533; Rogieri Pelissari, Maria/0000-0002-4649-075X; Sawakuchi, Andre/0000-0001-5016-2428; Oliveira Sawakuchi, Henrique/0000-0002-6815-7261	"Human Resources Formation Program in Petroleum and Environmental Geology" (Petrobras) [PFRH-241]; Brazilian National Council for Scientific and Technological Development (CNPq) [454362/2014-5]	"Human Resources Formation Program in Petroleum and Environmental Geology" (Petrobras); Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank Marcelo Camargo and Victor Alem for support in field work and with laboratory procedures. We also would like to thank Dr. Isaac Sayeg, Artur Takashi and Luciana Nogueira for technical support in the laboratory. The authors also thank Ana Carolina Almeida for language revision. This research was financially supported by the "Human Resources Formation Program in Petroleum and Environmental Geology" (PFRH-241, Petrobras) and Brazilian National Council for Scientific and Technological Development (CNPq, grant 454362/2014-5).	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Pet. Geol.	FEB	2020	112								104039	10.1016/j.marpetgeo.2019.104039	http://dx.doi.org/10.1016/j.marpetgeo.2019.104039			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KG0HP					2023-06-23	WOS:000509622600056
J	Biolchi, LG; Farina, L; Perotto, H				Biolchi, Luis Germano; Farina, Leandro; Perotto, Heitor			The influence of seamounts on ocean surface wave propagation in Northeast Brazil	DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS			English	Article						Ocean waves; Seamounts; SWAN; Wave model; Swell	MODEL; EROSION; SWAN; DEEP	General propagation patterns due to the multiple interaction of waves and seamounts located in Northeast Brazil are investigated using SWAN. After conducting a model sensitivity test using in situ data, four realistic cases (in which the maximum period of the incoming swells was 17.6s) and one synthetic case (using the maximum period as 21.3s) have been simulated. The incoming wave periods and the minimum seamount depth determine whether the interaction happens or not. When the interaction occurs, changes in wave direction, significant wave height (H-s), and shadow zone length increases with higher incoming wave periods. Shoaling and wave refraction occur concomitantly, leading to lower significant wave heights on the flanks of the seamounts and higher values of this variable over the shallowest parts. The observed wave alterations are also due to the topographic orientation of the seamounts' shallower portion relative to the incoming wave direction and to the interaction between waves affected by more than one seamount. For the shallowest seamount in the study area (minimum depth of 21m), the maximum significant wave height increased 43.7% and 25.3% relative to the incoming wave heights for the synthetic and realistic cases, respectively.	[Biolchi, Luis Germano; Farina, Leandro; Perotto, Heitor] Univ Fed Rio Grande do Sul, Ctr Estudos Costeiros & Ocean, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Biolchi, LG (autor correspondente), Univ Fed Rio Grande do Sul, Ctr Estudos Costeiros & Ocean, Porto Alegre, RS, Brazil.	luisgbiolchi@gmail.com; farina@mat.ufrgs.br; heitor_perotto@yahoo.com.br	Farina, Leandro/Q-5602-2018	Farina, Leandro/0000-0003-2744-515X	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]; CAPES; project ROAD-BESM -REGIONAL OCEANIC AND ATMOSPHERIC DOWNSCALING/CAPES [88881.146048/2017-01]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); project ROAD-BESM -REGIONAL OCEANIC AND ATMOSPHERIC DOWNSCALING/CAPES	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001. The first author would like to thank CAPES for the scholarship provided as part of the National Academic Excellence Support (Programa Nacional de Excelencia Academica -PROEX). Leandro Farina acknowledges support from the project ROAD-BESM -REGIONAL OCEANIC AND ATMOSPHERIC DOWNSCALING/CAPES (88881.146048/2017-01).	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Part I-Oceanogr. Res. Pap.	FEB	2020	156								103185	10.1016/j.dsr.2019.103185	http://dx.doi.org/10.1016/j.dsr.2019.103185			12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	KM6KU					2023-06-23	WOS:000514247800006
J	Cohen, MCL; Figueiredo, BL; Oliveira, NN; Fontes, NA; Franca, MC; Pessenda, LCR; de Souza, AV; Macario, K; Giannini, PCF; Bendassolli, JA; Lima, P				Cohen, Marcelo C. L.; Figueiredo, Beatriz L.; Oliveira, Nedra N.; Fontes, Neuza A.; Franca, Marlon Carlos; Pessenda, Luiz C. R.; de Souza, Adriana, V; Macario, Kita; Giannini, Paulo C. F.; Bendassolli, Jose A.; Lima, Paula			Impacts of Holocene and modern sea-level changes on estuarine mangroves from northeastern Brazil	EARTH SURFACE PROCESSES AND LANDFORMS			English	Article						climate changes; drone; palynology; satellite images; sea-level rise	RIO-DE-JANEIRO; SOUTHEASTERN BRAZIL; LATE QUATERNARY; LATE PLEISTOCENE; CLIMATE-CHANGE; MID-HOLOCENE; DYNAMICS; EASTERN; VEGETATION; RISE	Projections of the impacts of modern Relative Sea Level (RSL) rise on estuarine mangroves should be supported by coastal topographic data and records of mangrove dynamics under past RSL change. This work identified inland and seaward mangrove migrations along the Jucurucu River (Bahia, Northeastern Brazil), during the Holocene based on sedimentary features, palynological and geochemical (delta C-13, delta N-15, C/N) data integrated with digital elevation models. During the Middle Holocene, in response to RSL rise, the estuary saw mangrove forest establish up to ~37 km inland. RSL stood between -1.4 (+0.36/-2.2 m) and +1 (2.19/0.2 m) around 7400 cal yr BP, and rose to a highest position of +3.25 (4.22/2.45 m) reached around 5350 cal yr BP. That marine incursion caused the inland replacement of freshwater vegetation by mangroves on tidal flats. Since then, the estuary experienced RSL fall, reducing inland tidal water salinity towards the Late Holocene, making that the mangroves were replaced by freshwater floodplain vegetation. Today, in the seaward part of the estuary near its mouth, mangroves occupy an area of ~10 km(2) along tidal channels. Considering a RSL rise of 98 cm up to the end of the 21(st) century, at a rate significantly higher than that of Middle Holocene RSL rise (1.5 mm/yr) and fall (0.6 mm/yr), the current mangrove substrates are expected to drown and/or eroded near the coast, while new mangroves may establish inland, at topographically higher tidal flats in nowadays freshwater-tidal zones. Mangrove area could expand over 13 km(2) of coastal and flood plain. Following the same interaction between RSL/climate changes and Holocene mangrove dynamics, such upstream mangrove migration may be attenuated or intensified by changes in fluvial discharge. (c) 2019 John Wiley & Sons, Ltd.	[Cohen, Marcelo C. L.; Figueiredo, Beatriz L.; Oliveira, Nedra N.; Fontes, Neuza A.; de Souza, Adriana, V; Lima, Paula] Fed Univ, Grad Program Geol & Geochem, Av Perimentral 2651, BR-66077530 Belem, Para, Brazil; [Pessenda, Luiz C. R.] Univ Sao Paulo, CENA 14C Lab, Av Centenario 303, BR-13400000 Piracicaba, SP, Brazil; [Franca, Marlon Carlos] Fed Inst Para, Av Alm Barroso 1155, BR-66090020 Belem, Para, Brazil; [Macario, Kita] Fluminense Fed Univ, Phys Dept, LAC, UFF AMS Lab, Niteroi, RJ, Brazil; [Giannini, Paulo C. 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J	Combi, T; Pintado-Herrera, MG; Lara-Martin, PA; Lopes-Rocha, M; Miserocchi, S; Langone, L; Guerra, R				Combi, Tatiane; Pintado-Herrera, Marina G.; Lara-Martin, Pablo A.; Lopes-Rocha, Marilia; Miserocchi, Stefano; Langone, Leonardo; Guerra, Roberta			Historical sedimentary deposition and flux of PAHs, PCBs and DDTs in sediment cores from the western Adriatic Sea	CHEMOSPHERE			English	Article						Persistent organic pollutants (POPs); Sediment cores; Fluxes; Western adriatic sea; Eco-toxicological implications	POLYCYCLIC AROMATIC-HYDROCARBONS; POLYCHLORINATED-BIPHENYLS PCBS; PERSISTENT ORGANIC POLLUTANTS; CONTINENTAL-SHELF; ORGANOCHLORINE PESTICIDES; ALIPHATIC-HYDROCARBONS; SURFICIAL SEDIMENTS; MARINE-SEDIMENTS; TEMPORAL TRENDS; MASS-BALANCE	The sources and depositional history of polycyclic aromatic hydrocarbons (PAHs) and organochlorine compounds (OCs) over the last century were investigated in sediment cores from the North Adriatic Sea (Po River prodelta) and the South-Western Adriatic Margin (SWAM). Contaminant concentrations were higher in the Po River prodelta. Sigma 16PAHs ranged from 193 to 533 ng g(-1), Sigma(5)PCBs ranged from 0.9 to 5.2 ng g(-1) and Sigma DDTs (p,p'-DDD + p,p'-DDE) ranged from 0.1 to 2.5 ng g-1. In the SWAM, Sigma EPAHs ranged from 11 to 74 ng g(-1) while Sigma PCB and Sigma DDT concentrations were close to the MQL. Accordingly, contaminant fluxes were much higher in the northern (mean values of 152 31 ng cm(2) y(-1) and 0.70 +/- 0.35 ng cm(2) y(-1) for PAHs and OCs, respectively) than in the southern Adriatic (2.62 +/- 0.9 ng cm(2) y(-1) be influenced by the historical socioeconomic development and by changes in the composition of fossil fuel consumption (from petroleum derivatives to natural gas) in Italy from the end of the 19th century to the present. Similarly, vertical variations in DDT concentrations matched its historical use and consumption in Italy, which started around in the mid-late 1940s to fight typhus during the II World War. Contaminant concentrations detected in sediments does not seem to pose ecotoxicological risk for marine organisms in the Adriatic Sea. (C) 2019 Published by Elsevier Ltd.	[Combi, Tatiane] Univ Fed Bahia, Inst Geociencias, Dept Oceanog, Rua Barao de Jeremoabo, BR-40170020 Salvador, BA, Brazil; [Combi, Tatiane; Lopes-Rocha, Marilia; Guerra, Roberta] Univ Bologna, Ctr Interdipartimentale Ric Sci Ambientali, Via St Alberto 123, I-48123 Ravenna, Italy; [Pintado-Herrera, Marina G.; Lara-Martin, Pablo A.] Univ Cadiz, Dept Quim Fis, Fac Ciencias Mar & Ambientales, Campus Excelencia Int Mar CEI MAR, Cadiz 11510, Spain; [Miserocchi, Stefano; Langone, Leonardo] CNR, ISP, I-40129 Bologna, Italy; [Guerra, Roberta] Univ Bologna, Dipartimento Fis & Astron, Bologna, Italy	Universidade Federal da Bahia; University of Bologna; Universidad de Cadiz; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Polari (ISP-CNR); University of Bologna	Combi, T (autor correspondente), Univ Fed Bahia, Inst Geociencias, Dept Oceanog, Rua Barao de Jeremoabo, BR-40170020 Salvador, BA, Brazil.	tatiane.combi@ufba.br	Pintado, marina/AAM-8906-2020; Combi, Tatiane/AAC-9936-2021; Pintado-Herrera, Marina G./AAC-9165-2021; Guerra, Roberta/B-8587-2012; Lara-Martin, Pablo Antonio/K-8917-2014; Combi, Tatiane/O-3004-2016	Pintado-Herrera, Marina G./0000-0003-2982-257X; Guerra, Roberta/0000-0002-7151-6616; Lara-Martin, Pablo Antonio/0000-0002-2982-1297; Combi, Tatiane/0000-0001-6769-7445	Programa Ciencia sem Fronteiras [CNPq 237092/2012-3]; EC FP7 PERSEUS Project [287600]	Programa Ciencia sem Fronteiras; EC FP7 PERSEUS Project	Tatiane Combi wishes to thank the 'Programa Ciencia sem Fronteiras' for the PhD scholarship (CNPq 237092/2012-3). We are indebted to the Istituto Nazionale di Oceanografia e di Geofisica Sperimentale (OGS, Trieste, Italy) and the Consiglio Nazionale delle Ricerche -Istituto Scienze Marine (CNR-ISMAR, Bologna, Italy) for the support during sediment sampling and analysis of sediment features. This work has been partially funded by the EC FP7 PERSEUS Project (Grant. Agr. 287600).	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J	Cunha, GO; Santucci, RM; de Andrade, MB; de Oliveira, CEM				Cunha, Galuber Oliveira; Santucci, Rodrigo Miloni; de Andrade, Marco Brandalise; Maia de Oliveira, Carlos Eduardo			Description and phylogenetic relationships of a large-bodied sphagesaurid notosuchian from the Upper Cretaceous Adamantina Formation, Bauru Group, Sao Paulo, southeastern Brazil	CRETACEOUS RESEARCH			English	Article						Sphagesauridae; Cretaceous; Bauru group; Adamantina formation; Osteoderms; Appendicular skeleton	CLARKI CROCODYLIFORMES NOTOSUCHIA; MONTEALTOSUCHUS-ARRUDACAMPOSI CROCODYLIFORMES; BASIN; MESOEUCROCODYLIA; CROCODYLOMORPHA; OSTEODERMS; SKELETON; REMAINS	In this work we describe new remains and possible gastroliths of a sphagesaurid (Mesoeucrocodylia: Notosuchia) unearthed from the Adamantina Formation (Bauru Group, Upper Cretaceous) in the municipality of Fernandopolis-SP, which add new data about the dental, dermal shield, and the post-cranial skeleton morphology of these crocodilians. Phylogenetic analyses place the studied fossil within Sphagesauridae, in a polytomy with Armadillosuchus arrudai and Caryonosuchus pricei. The anatomical comparisons are congruent to the phylogenetic analysis since they also suggest that the specimen herein described is closely related to other larger-bodied Sphagesauridae species, such as Armadillosuchus arrudai. The new skull, appendicular, and dermal elements described in this work may provide data for the elaboration of new phylogenetic characters which can improve cladistic analyses concerning Sphagesauridae species, as well as they may help to better understand the morphological complexity of this family of crocodylomorphs, especially the large-bodied species. (C) 2019 Elsevier Ltd. All rights reserved.	[Cunha, Galuber Oliveira; Santucci, Rodrigo Miloni] Univ Brasilia, Campus Planaltina,Area Univ 1, Brasilia, DF, Brazil; [de Andrade, Marco Brandalise] Pontificia Univ Catolica Rio Grande do Sul, Porto Alegre, RS, Brazil; [Maia de Oliveira, Carlos Eduardo] Fed Inst Educ Sci & Technol Sao Paulo, Votuporanga, Brazil	Universidade de Brasilia; Pontificia Universidade Catolica Do Rio Grande Do Sul; Instituto Federal de Sao Paulo (IFSP)	Santucci, RM (autor correspondente), Univ Brasilia, Campus Planaltina,Area Univ 1, Brasilia, DF, Brazil.	rodrigoms@unb.br	Santucci, Rodrigo M/E-2189-2013; Andrade, Marco Brandalise de/D-2708-2014	Andrade, Marco Brandalise de/0000-0002-3452-801X; Santucci, Rodrigo/0000-0002-4326-743X	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brazil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (National Council for Scientific and Technological Development) [401784/2010-0]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brazil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (National Council for Scientific and Technological Development)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank Hussam Zaher and Alberto B. Carvalho (Museu de Zoologia da Universidade de Sao Paulo - MZUSP) and Thiago Marinho (Museu dos Dinossauros and Centro de Pesquisas Paleontologicas Llewellyn Ivor Price - UFTM) for access to the collections under their care. We also thank Thiago Marinho and an anonymous reviewer for their comments that improved an earlier version of this manuscript. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior Brazil (CAPES) - Finance code 001. RMS also thanks the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (National Council for Scientific and Technological Development) for supporting this research (process 401784/2010-0).	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FEB	2020	106								104259	10.1016/j.cretres.2019.104259	http://dx.doi.org/10.1016/j.cretres.2019.104259			25	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	JW8RB		Green Published			2023-06-23	WOS:000503313100019
J	Garcez, RWD; Lopes, JM; Perez, SD; Lauria, DD; Viglio, EP; da Cunha, FG; Ribeiro, FCA; da Silva, AX				Dutra Garcez, Ricardo Washington; Lopes, Jose Marques; Perez, Sueli da Silva; Lauria, Dejanira da Costa; Viglio, Eduardo Paim; da Cunha, Fernanda Goncalves; Araujo Ribeiro, Fernando Carlos; da Silva, Ademir Xavier			Activity concentration and mapping of radionuclides in Espirito Santo State soils, Brazil	RADIATION PHYSICS AND CHEMISTRY			English	Article; Proceedings Paper	14th International Symposium on Radiation Physics (ISRP)	OCT 07-11, 2018	Natl Univ Cordoba, Cordoba, ARGENTINA	Minist Sci & Technol Prov Cordoba, Minist Sci, Technol & Prod Innovat Argentine Nat, Ctr Excellence Prod & Proc Cordoba	Natl Univ Cordoba	Activity concentration; Soil; Map; Absorbed dose; Effective dose	NATURAL RADIOACTIVITY	Soils exhibit a wide range of radioactive elements and, therefore, the knowledge of the radioactivity levels that the human being is exposed to is of great importance for Radiological Protection. This study aims to determine the activity concentrations of K-40, Ra-226, and Ra-228 in soils of Brazilian state of Espirito Santo, to produce radionuclide concentration distribution maps to understand their occurrence, and to evaluate both the absorbed and effective doses. Sixty six samples were collected, covering all the state area, and analyzed by gamma spectrometry using a Hyperpure Germanium semiconductor detector (HPGe), with relative efficiency of 30%. The activity concentration of K-40 varied from 7 to 693 Bq/kg, while Ra-226 ranged from 11 to 88 Bq/kg, and Ra-228 ranged from 18 to 424 Bq/kg. The absorbed dose, at 1 m above the ground, ranged from 16 to 277 nGy/h. The outdoor annual effective dose ranged from 0.02 to 0.34 mSv/year. About 80% of the samples presented radionuclide content that result in mean annual effective dose above the global. The radionuclide that contributed to the dose was Ra-228, with approximately 78% of the total dose.	[Dutra Garcez, Ricardo Washington; Lopes, Jose Marques; da Silva, Ademir Xavier] Univ Fed Rio de Janeiro, Nucl Engn Program, Rua Horacio Macedo,Bloco G,2030-101 Cidade Univ, BR-2194145 Rio de Janeiro, RJ, Brazil; [Perez, Sueli da Silva; Lauria, Dejanira da Costa; Araujo Ribeiro, Fernando Carlos] Inst Radiat Protect & Dosimetry IRD, Ave Salvador Allende S-N Barra da Tijuca, BR-22783127 Rio De Janeiro, RJ, Brazil; [Viglio, Eduardo Paim; da Cunha, Fernanda Goncalves] Geol Survey Brazil CPRM, Ave Pasteur,404 Urca, BR-22290240 Rio De Janeiro, RJ, Brazil	Universidade Federal do Rio de Janeiro	Garcez, RWD (autor correspondente), Univ Fed Rio de Janeiro, Nucl Engn Program, Rua Horacio Macedo,Bloco G,2030-101 Cidade Univ, BR-2194145 Rio de Janeiro, RJ, Brazil.	rgarcez@nuclear.ufrj.br	Garcêz, Ricardo/G-7505-2019; Ribeiro, Fernando C.A./F-2995-2010; da Costa Lauria, Dejanira/E-3840-2016	Garcêz, Ricardo/0000-0003-4194-3729; Ribeiro, Fernando C.A./0000-0001-6113-8001; da Costa Lauria, Dejanira/0000-0002-9727-0001	CNPq (National Council for Scientific andOechnological Development), federal agency of Brazil [141541/2016-4]	CNPq (National Council for Scientific andOechnological Development), federal agency of Brazil	The authors would like to thank the financial support given by the CNPq (National Council for Scientific andOechnological Development), federal agency of Brazil to encourage research. Ph.D scholarship. Grant number: 141541/2016-4.	Amaral ECS, 1992, THESIS; Aquino RSS, 2010, THESIS; Ribeiro FCA, 2018, REV BRAS CIENC SOLO, V42, DOI 10.1590/18069657rbcs20170146; Barbosa C.T.P., 2007, P 11 C BRAS GEOQ AT; BERNARDI ACC, 2002, USO AGRICOLA SOLOS B, P61; Boyle R. 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Phys. Chem.	FEB	2020	167								108209	10.1016/j.radphyschem.2019.03.013	http://dx.doi.org/10.1016/j.radphyschem.2019.03.013			6	Chemistry, Physical; Nuclear Science & Technology; Physics, Atomic, Molecular & Chemical	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Chemistry; Nuclear Science & Technology; Physics	KB4KG					2023-06-23	WOS:000506465900078
J	Freire, MM; Amorim, LMF; Buch, AC; Goncalves, AD; Sella, SM; Cassella, RJ; Moreira, JC; Silva, EV				Freire, Marina Moreira; Fonte Amorim, Lidia Maria; Buch, Andressa Cristhy; Goncalves, Aline Domingos; Sella, Silvia Maria; Cassella, Ricardo Jorgensen; Moreira, Josino Costa; Silva-Filho, Emmanoel Vieira			Polycyclic aromatic hydrocarbons in bays of the Rio de Janeiro state coast, SE - Brazil: Effects on catfishes	ENVIRONMENTAL RESEARCH			English	Article						Benzo(a)pyrene diol epoxide; Biomarkers; Erythrocytic nuclear abnormalities; Ethoxyresorufin-O-Deethylase; Hepatic lesion; Tropical estuarine	TOXICOPATHIC HEPATIC-LESIONS; FLOUNDER PLATICHTHYS-FLESUS; SOLE PLEURONECTES-VETULUS; BILIARY PAH METABOLITES; PIKE ESOX-LUCIUS; ENGLISH SOLE; DNA-ADDUCTS; HISTOPATHOLOGICAL LESIONS; FUNDULUS-HETEROCLITUS; MARINE-ENVIRONMENT	The Brazilian coast of the Rio de Janeiro State has bays of great economic, ecological and social importance. However, these ecosystems have been suffering intense anthropogenic influence, mainly due to the contamination by polycyclic aromatic hydrocarbons (PAHs) from urban-industrial activities. Moreover, PAHs are organic pollutants of high toxicity and carcinogenicity causing global concern to human and environmental health. This study evaluated on catfish (Genidens genidens) a set of key parameters (sex, morphometric traits, condition factor (K), PAH metabolites in gallbladder, frequency of micronucleus (MN) and erythrocytic nuclear abnormalities (ENA) in blood. In addition we also evaluated histopathological hepatic effects, Ethoxyresorufin-O-deethylase (EROD) activity and Benzo(a)pyrene diol epoxide (BPDE)-DNA adducts) in liver samples, in order to indicate the fish health status and environmental pollution levels of three main Bays (Guanabara, Sepetiba and Ilha Grande) of the Rio de Janeiro State, in the Southeast of Brazil. In general, the worst physical and metabolic conditions in catfishes were evidenced in Guanabara Bay, possibly indicating the highest level of contamination by PAHs. Contrary evidence was observed in Ilha Grande Bay, showing lower biological changes in G. genidens. However in Sepetiba Bay, the influence of PAHs contamination showed the highest hepatic lesions in catfishes, prevailing foci of cellular alterations, megalocytic hepatosis and hydropic vacuolations. The employability of a set of biomarkers on catfish was efficient for screening pollution for PAHs in tropical environments. This reinforces the need for effective actions of monitoring and conservation strategies of bays of the Rio de Janeiro State (Brazil), in order to ensure quality and health to both human and environment.	[Freire, Marina Moreira; Buch, Andressa Cristhy; Goncalves, Aline Domingos; Silva-Filho, Emmanoel Vieira] Fluminense Fed Univ, Chem Inst, Postgrad Program Geosci Environm Geochem, BR-24020141 Niteroi, RJ, Brazil; [Fonte Amorim, Lidia Maria] Fluminense Fed Univ, Biol Inst, Postgrad Program Sci & Biotechnol, Niteroi, RJ, Brazil; [Fonte Amorim, Lidia Maria] Fluminense Fed Univ, Biol Inst, Postgrad Program Neurosci, Niteroi, RJ, Brazil; [Sella, Silvia Maria; Cassella, Ricardo Jorgensen] Fluminense Fed Univ, Chem Inst, Postgrad Program Chem, BR-24020141 Niteroi, RJ, Brazil; [Goncalves, Aline Domingos] Univ Fed Rio de Janeiro, Chem Inst, Analyt Chem Dept, BR-21941909 Rio De Janeiro, Brazil; [Moreira, Josino Costa] Fundacao Oswaldo Cruz, Natl Sch Publ Hlth, BR-21041210 Rio De Janeiro, Brazil	Universidade Federal Fluminense; Universidade Federal Fluminense; Universidade Federal Fluminense; Universidade Federal Fluminense; Universidade Federal do Rio de Janeiro; Fundacao Oswaldo Cruz	Silva, EV (autor correspondente), Fluminense Fed Univ, Chem Inst, Postgrad Program Geosci Environm Geochem, BR-24020141 Niteroi, RJ, Brazil.	emmanoelvieirasilvafilho@id.uff.br	Cassella, Ricardo Jorgensen/X-1445-2019; Sella, Silvia M/D-2204-2015; da Silva Filho, Emmanoel Vieira/Y-7281-2019; Amorim, Lidia M F/U-5896-2019	Cassella, Ricardo Jorgensen/0000-0003-2739-0873; da Silva Filho, Emmanoel Vieira/0000-0001-6444-6851; Amorim, Lidia M F/0000-0001-7282-9748	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) [001]; CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico); FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) - Finance Code 001. The authors are grateful to Dr. Regina M. Santella of the Department of Environmental Health at Columbia University, New York, for the BPDE-DNA analysis and Dr. Jayme da Cunha Bastos Neto of the Laboratory of Toxicological Biochemistry of the University of the State of Rio de Janeiro (UERJ) for the EROD activity analysis. The authors also acknowledge the financial support of CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico) and FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro), Brazilian governmental institutions, for funding this study.	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Res.	FEB	2020	181								108959	10.1016/j.envres.2019.108959	http://dx.doi.org/10.1016/j.envres.2019.108959			8	Environmental Sciences; Public, Environmental & Occupational Health	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Public, Environmental & Occupational Health	KG7DX	31784080				2023-06-23	WOS:000510109700001
J	de Oliveira, GJG; Reimold, WU; Crostaa, AP; Hauser, N; Mohr-Westheide, T; Tagle, R; Galante, D; Kaufmann, F				Goncalves de Oliveira, Grace Juliana; Reimold, Wolf Uwe; Crostaa, Alvaro Penteado; Hauser, Natalia; Mohr-Westheide, Tanja; Tagle, Roald; Galante, Douglas; Kaufmann, Felix			Petrographic characterization of Archaean impact spherule layers from Fairview Gold Mine, northern Barberton Greenstone Belt, South Africa	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Spherule layer; Distal impact ejecta; Archaean; Barberton greenstone belt; Micro-XRF analysis; Ni-Cr spinel	ICDP DRILL CORE; K-PG BOUNDARY; MOUNTAIN LAND; ORIGIN; BEDS; GEOCHEMISTRY; RECORD; BARB5; BOMBARDMENT; CONSTRAINTS	The oldest known evidence of large impacts in Early Earth history are Archaean to Palaeoproterozoic impact spherule layers of the Barberton Greenstone Belt in South Africa and the Pilbara craton in Western Australia. Four drill core sections (BH5901, BH5907, BH5911 and BH5949) containing spherule layers were intersected in exploration drilling at Fairview Gold Mine in the northern Barberton Greenstone Belt. Here, we provide a first detailed mineralogical study of these new spherule layer intersections. The spherule layers are densely packed with sand-sized, spherical to ovoid, i.e., in part strongly deformed, "beads". They generally have morphological and textural features similar to other 3.4-3.2 Ga old spherule layers of the Barberton Greenstone Belt. The Fairview spherule layers are stratigraphically positioned at the contact between the silicified volcanic tuff of the uppermost unit of the Onverwacht Group and the lowermost silicidastic rocks of the Fig Tree Group, like the S2 and S4 layers in the southern, and S3 layer in the northern, domain of the greenstone belt. Micro-XRF scanning allowed (i) to distinguish spherule layers from their host rocks by their major element distribution, and (ii) to characterize secondary alteration and micro-deformation features in the SL and host rocks. Ni-Cr spinel, the only primary mineral in evidence in these sections, is not distributed uniformly along a spherule layer intersection, and occurrences can not be stratigraphically correlated between the four layer intersections either. Spinel crystals vary with respect to Ni, Cr, Fe and Zn contents and respective zonation patterns for these elements. Zinc abundances are likely related to post-depositional hydrothermal overprint. The results of this investigation comprising geological, petrographic, semiquantitative micro-X-ray fluorescence spectrometry, and quantitative electron microprobe analysis on spinel support a complex and heterogeneous genetic process that must have taken place during spherule formation in an impact vapor plume and in post-depositional times. The Fairview spherule layers are thought to possibly represent the product of a single impact event. They represent fallout into deep-water conditions, as they lack evidence for reworking or sorting by current or wave action. The heterogeneous Ni-Cr spinet concentrations are similar to what has been reported for spinel occurrences in the S3 layer, but considering the complex tectonic overprint on this lithostratigraphic sequence at the changeover from the Onverwacht to the Fig Tree Group it is not possible to conclude whether or not these spherule layers represent the same impact event.	[Goncalves de Oliveira, Grace Juliana; Crostaa, Alvaro Penteado] Univ Estadual Campinas, Inst Geosci, R Carlos Gomes 250, BR-13083855 Campinas, SP, Brazil; [Reimold, Wolf Uwe; Hauser, Natalia] Univ Brasilia, Inst Geosci, Lab Geodynam Geochronol & Environm Sci, Darcy Ribeiro Campus,Asa Norte, BR-90190900 Brasilia, DF, Brazil; [Mohr-Westheide, Tanja; Kaufmann, Felix] Leibniz Inst Evolut & Biodivers Sci, Museum Nat Kunde, Invalidenstr 43, D-10115 Berlin, Germany; [Mohr-Westheide, Tanja] Free Univ Berlin, Inst Geol Wissensch, Malteserstr 74-100, D-12249 Berlin, Germany; [Tagle, Roald] Broker Nano GmbH, Studio 2 D, D-12489 Berlin, Germany; [Galante, Douglas] Brazilian Nanotechnol Natl Lab LNNano, R Giuseppe Maximo Scolfaro 10000, BR-13083970 Campinas, SP, Brazil	Universidade Estadual de Campinas; Universidade de Brasilia; Leibniz Institut fur Evolutions und Biodiversitatsforschung; Free University of Berlin	de Oliveira, GJG (autor correspondente), Univ Estadual Campinas, Inst Geosci, R Carlos Gomes 250, BR-13083855 Campinas, SP, Brazil.	gracejuliana.oliveira@gmail.com	Galante, Douglas/G-8752-2011; Hauser, Natalia/H-2041-2012; Crósta, Alvaro Penteado/A-9892-2008; Reimold, Wolf Uwe/AAI-6226-2021	Galante, Douglas/0000-0002-3265-2527; Crósta, Alvaro Penteado/0000-0003-0485-1147; Hauser, Natalia/0000-0002-6975-6186; Oliveira, Grace Juliana/0000-0002-4062-7188; Reimold, Wolf Uwe/0000-0001-6588-0887	Bruker Nano GmbH; Brazilian CNPq [GD-142442/2015-1, SWE 290132/2017-7]; Barringer Family Fund for Meteorite Impact Research; UNICAMP; MEV laboratory facilities at Unicamp	Bruker Nano GmbH; Brazilian CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Barringer Family Fund for Meteorite Impact Research; UNICAMP; MEV laboratory facilities at Unicamp	The authors would like to express their gratitude to Chris Rippon of the Fairview Mine Geology Department for providing the FV SL samples and important information regarding the geology of the drilled interval. We are also grateful to Axel Hofmann, who contributed important background information on the geology of South Africa and the BGB. We thank Bruker Nano GmbH, Berlin-Adlershof, with a special mentioning of Falk Reinhardt and Max Buegler, for the micro-XRF measurements and their support with data processing. G.J.G. Oliveira acknowledges the financial support from the Brazilian CNPq through grants GD-142442/2015-1 and SWE 290132/2017-7, and from the Barringer Family Fund for Meteorite Impact Research for a research grant awarded. G.J.G. Oliveira also acknowledges the Museum fiir Naturkunde, Berlin, which most kindly provided full support and access to the laboratory facilities necessary to carry out this research, under a cooperation agreement between UNICAMP and the MfN. G.J.G. Oliveira acknowledges the laboratory facilities at CNPEM/LNLS. G.J.G. Oliveira also acknowledges the MEV laboratory facilities at Unicamp, and Erica M. Tonetto for support with the analysis. 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Afr. Earth Sci.	FEB	2020	162								103718	10.1016/j.jafrearsci.2019.103718	http://dx.doi.org/10.1016/j.jafrearsci.2019.103718			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KG0FV					2023-06-23	WOS:000509618000027
J	Lopes, JM; Garcez, RWD; Silva, LB; Silva, RC; Domingues, AM; Silva, AX; Dam, RSF				Lopes, Jose M.; Garcez, Ricardo W. D.; Silva, Leandro B.; Silva, Roberto C.; Domingues, Alessandro M.; Silva, Ademir X.; Dam, Roos S. F.			Committed effective dose due to consumption of fruits and vegetables peels: Analysis on cancer risk increase	RADIATION PHYSICS AND CHEMISTRY			English	Article; Proceedings Paper	14th International Symposium on Radiation Physics (ISRP)	OCT 07-11, 2018	Natl Univ Cordoba, Cordoba, ARGENTINA	Minist Sci & Technol Prov Cordoba, Minist Sci, Technol & Prod Innovat Argentine Nat, Ctr Excellence Prod & Proc Cordoba	Natl Univ Cordoba	Naturally occurring radionuclides; Peels consumption; Committed effective dose	FOOD WASTE; FRACTIONS	The recommended daily intake is the amount of vitamins, minerals and proteins that should be consumed daily, in order to make the population healthier by obtaining proper nutritional needs. Food science has suggested that the unusable parts of fruits and vegetables could be used to food enrichment, reducing waste and increasing the nutritional value of meals. This study presents an analysis of K-40, Ra-226, Ra-228 and Th-228 activity concentrations in some fruits and vegetables using high-resolution gamma spectrometry. Furthermore, the activity concentrations of the radionuclides in fruits and vegetables coating tissue (peels) was analyzed. It can be noticed that there is no relationship when it comes to activity concentrations of these radionuclides in pulp and peel. However, an increase of the radionuclides activity concentration in peels can be notice, in general. For a diet whose amount of peels consumption in one year is equal to pulp consumption, and which considers the exclusive consumption of peels, the committed effective dose increase was 2.6-fold. Estimation about the cancer risks due to fruits and vegetables peels consumption exceeded the safety recommended values.	[Lopes, Jose M.; Garcez, Ricardo W. D.; Silva, Leandro B.; Silva, Roberto C.; Domingues, Alessandro M.; Silva, Ademir X.; Dam, Roos S. F.] Fed Univ Rio Janeiro, Nucl Engn Program, Ave Hordcio Macedo,2030,Bloco G,Sala 206 CT, BR-21945970 Rio De Janeiro, RJ, Brazil; [Silva, Ademir X.] Fed Univ Rio Janeiro, Polytech Sch, Ave Athos da Silveira Ramos 149, BR-21941909 Rio De Janeiro, RJ, Brazil; [Dam, Roos S. F.] Nucl Engn Inst IEN CNEN, Rua Helio de Almeida 75, BR-21941906 Rio De Janeiro, RJ, Brazil	Comissao Nacional de Energia Nuclear (CNEN)	Lopes, JM (autor correspondente), Fed Univ Rio Janeiro, Nucl Engn Program, Ave Hordcio Macedo,2030,Bloco G,Sala 206 CT, BR-21945970 Rio De Janeiro, RJ, Brazil.	marqueslopez@yahoo.com.br	Garcêz, Ricardo/G-7505-2019	Garcêz, Ricardo/0000-0003-4194-3729; Dam, Roos Sophia/0000-0001-5747-2314; Barbosa da Silva, Leandro/0000-0002-8544-8634; Marques Lopes, Jose/0000-0001-7819-6646	FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro) [n5 E26/112.087/2012]; CNPq (Conselho Nacional de Pesquisa e Desenvolvimento)	FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); CNPq (Conselho Nacional de Pesquisa e Desenvolvimento)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to thank FAPERJ (Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro, process n5 E26/112.087/2012) and CNPq (Conselho Nacional de Pesquisa e Desenvolvimento) for the financial support, without their help this work would not be possible.	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Technol (Campinas), V22, P259, DOI 10.1590/S0101-20612002000300011; Papargyropoulou E, 2014, J CLEAN PROD, V76, P106, DOI 10.1016/j.jclepro.2014.04.020; Scheibel V, 2007, J FOOD COMPOS ANAL, V20, P650, DOI 10.1016/j.jfca.2007.04.005; Storck CR, 2013, CIENC RURAL, V43, P537, DOI 10.1590/S0103-84782013000300027; U.S. EPA, 1999, 402R99001 US EPA; UNSCEAR, 2000, SOURC EFF ION RAD; Wolfe K, 2003, J AGR FOOD CHEM, V51, P609, DOI 10.1021/jf020782a; Wolfe KL, 2003, J AGR FOOD CHEM, V51, P1676, DOI 10.1021/jf025916z	30	9	9	0	8	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0969-806X			RADIAT PHYS CHEM	Radiat. Phys. Chem.	FEB	2020	167								108243	10.1016/j.radphyschem.2019.03.047	http://dx.doi.org/10.1016/j.radphyschem.2019.03.047			6	Chemistry, Physical; Nuclear Science & Technology; Physics, Atomic, Molecular & Chemical	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Chemistry; Nuclear Science & Technology; Physics	KB4KG					2023-06-23	WOS:000506465900074
J	Martins, ABD; de Assis, AHS; Cardoso, MS; Hatje, V; Moreira, ITA; de Albergaria-Barbosa, ACR				Martins, Adrielle Beatrice do O.; Silva de Assis, Arthur Henrique; Cardoso Filho, Milton Santos; Hatje, Vanessa; Andrade Moreira, Icaro Thiago; Rizzatti de Albergaria-Barbosa, Ana Cecilia			Concentration and distribution of polycyclic aromatic hydrocarbons in oysters from Todos os Santos Bay (Bahia, Brazil)	MARINE POLLUTION BULLETIN			English	Article						Contamination; Tropical bay; Crassostrea rhizophorae; Oyster; PAHs	CRASSOSTREA-RHIZOPHORAE; MANGROVE OYSTER; GEOCHEMICAL MARKERS; TEMPORAL TRENDS; SEDIMENTS; PAHS; CONTAMINATION; ESTUARY; MUSSELS; TRACE	The aim of the present study was to evaluate the presence of polycyclic aromatic hydrocarbons (PAHs) in oysters (Crassostrea rhizophorae) collected from Todos os Santos Bay (Bahia, Brazil). The total PAH concentration was highest in Madre de Deus (36.3 to 37.8 ng g(-1) in dry weight, dw), which is located near a petrochemical complex, oil refinery, and commercial port. In the Paraguagu river estuary, PAH concentrations varied between 23.2 and 25.7 ng g(-1) dw. The lowest concentrations (1.55 ng g(-1) dw) were found in the Jaguaribe river estuary, which can be considered a relatively preserved area. The main source of PAHs in the study areas was observed to be pyrogenic. Values of benzo[a]pyrene toxic equivalent ranged from 0.28 to 4.20. The concentrations of PAHs in oysters from the Paraguay river estuary and in Madre de Deus indicate the possible lifetime risk of developing cancer in humans who feed on it.	[Martins, Adrielle Beatrice do O.; Cardoso Filho, Milton Santos] Programa Posgrad Geoquim Petroleo & Meio Ambiente, Av Adhemar de Barros S-N, BR-40170110 Salvador, BA, Brazil; [Martins, Adrielle Beatrice do O.; Andrade Moreira, Icaro Thiago; Rizzatti de Albergaria-Barbosa, Ana Cecilia] Univ Fed Bahia, LEPETRO Inst Geociencias, Rua Barao de Jeremoabo,S-N Campus, BR-40170020 Salvador, BA, Brazil; [Martins, Adrielle Beatrice do O.; Silva de Assis, Arthur Henrique; Rizzatti de Albergaria-Barbosa, Ana Cecilia] Univ Fed Bahia, Inst Geociencias, Lab Geoquim Marinha, Rua Barao de Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil; [Hatje, Vanessa] Univ Fed Bahia, Inst Quim, Rua Barao de Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil; [Hatje, Vanessa] Univ Fed Bahia, Ctr Interdisciplinar Energia & Ambiente, Rua Barao de Jeremoabo S-N, BR-40170020 Salvador, BA, Brazil; [Andrade Moreira, Icaro Thiago] Univ Fed Bahia, Dept Engn Ambiental, Escola Politecn, Rua Prof Aristides Novis 2, BR-40170290 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia; Universidade Federal da Bahia	Martins, ABD; de Albergaria-Barbosa, ACR (autor correspondente), Univ Fed Bahia, LEPETRO Inst Geociencias, Rua Barao de Jeremoabo,S-N Campus, BR-40170020 Salvador, BA, Brazil.	adriellebeatrice@hotmail.com; vanessahatje@ufba.br; cecilia.albergaria@ufba.br	de Albergaria-Barbosa, Ana Cecília/AAC-6940-2021; de+Albergaria+Barbosa, Ana/AAQ-3872-2020; Moreira, Icaro/J-2040-2015; MOREIRA, ICARO/AAV-6503-2020	MOREIRA, ICARO/0000-0002-3964-7368; Albergaria-Barbosa, Ana Cecilia R./0000-0003-2121-9792; do O Martins, Adrielle Beatrice/0000-0002-9468-6618	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) [001]; Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB) [PET0035/2014, PET0034/2012, PET0035/2012, CNV0005/2013, CNV0025/2013]; FAPESB [25312017]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); FAPESB(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB))	This work was developed in the Programa de Pos-Graduacati em Geoqufmica: Petroleo e Meio Ambiente from Universidade Federal da Bahia, supported by Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) - financial code 001. It was funded by the Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB; PET0035/2014; PET0034/2012; PET0035/2012; CNV0005/2013; CNV0025/2013). A.B.O. Martins also thanks FAPESB for her scholarship (no. 25312017). We also acknowledged the anonymous referees for their suggestions that contributed to the improvement of this manuscript.	Abessa D., 2012, INT J OCEANOGR, V2012; Aguirre-Rubi JR, 2018, ENVIRON SCI POLLUT R, V25, P13396, DOI 10.1007/s11356-017-9159-2; Almeida M., 2018, BRAZIL MAR POLLUT B, V137, P339; Amado GM, 2008, BRAZ J BIOL, V68, P95, DOI 10.1590/S1519-69842008000100013; ANTAQ. 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Pollut. Bull.	FEB	2020	151								110781	10.1016/j.marpolbul.2019.110781	http://dx.doi.org/10.1016/j.marpolbul.2019.110781			7	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	KN3RQ	32056582				2023-06-23	WOS:000514758400092
J	Moncinhatto, TR; Haag, MB; Hartmann, GA; Savian, JF; Poletti, W; Sommer, CA; Caselli, AT; Trindade, RIF				Moncinhatto, Thiago R.; Haag, Mauricio B.; Hartmann, Gelvam A.; Savian, Jairo F.; Poletti, Wilbor; Sommer, Carlos A.; Caselli, Alberto T.; Trindade, Ricardo I. F.			Mineralogical control on the magnetic anisotropy of lavas and ignimbrites: a case study in the Caviahue-Copahue field (Argentina)	GEOPHYSICAL JOURNAL INTERNATIONAL			English	Article						AMS; AARM; Magnetic Mineralogy; Caviahue-Copahue Volcanic Complex	MAGMA FLOW; SUSCEPTIBILITY; AMS; ROCKS; DIRECTION; CALDERA; FABRICS; REMANENCE; COLLAPSE; PROVINCE	Anisotropy of magnetic susceptibility is a petrofabric tool used to estimate the alignment of minerals at the site-scale, the imbrication between the magnetic foliation and the emplacement surface being an indicator of flow direction. However, despite numerous studies examining the flow direction in pyroclastic deposits and lava flows, the effect of magnetic mineralogy and the domain state of ferromagnetic phases on the magnetic fabric remains poorly understood. This paper describes the magnetic mineralogy and its influence on the magnetic fabric of Plio-Pleistocene lava flows and ignimbrites of the Caviahue-Copahue Volcanic Complex in the Andean Southern Volcanic Zone, Argentina. Rock magnetism, anisotropy of magnetic susceptibility and anhysteretic remanent magnetization and petrographic observations were performed on 30 sites of the volcanic complex. Results revealed the extrusive and pyroclastic rocks present varied magnetic mineralogy, formed in different stages of the magmatic evolution. Magnetic mineralogy variations strongly affect the anisotropy of magnetic susceptibility data in volcanic rocks and associated ignimbrites, providing 'scattered' fabrics when late Tirich titanomagnetite phases dominate the fabric, and 'inverse' or 'intermediate' fabrics when single-domain grains are present. 'Normal' fabrics are typically found when early crystallized puremagnetite is present. Our results highlight the complexity in the interpretation of magnetic anisotropy data in volcanic rocks and ignimbrites.	[Moncinhatto, Thiago R.; Trindade, Ricardo I. F.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226, BR-05508090 Sao Paulo, SP, Brazil; [Haag, Mauricio B.; Savian, Jairo F.; Sommer, Carlos A.] Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Hartmann, Gelvam A.] Univ Estadual Campinas, Inst Geociencias, Rua Carlos Gomes 250, BR-13083855 Campinas, SP, Brazil; [Poletti, Wilbor] Univ Fed Vales Jequitinhonha & Mucuri, Inst Ciencias & Tecnol, Rodovia MGT 367,5000, BR-39100000 Diamantina, MG, Brazil; [Caselli, Alberto T.] Univ Nacl Rio Negro, Lab Estudio Seguimiento Volcanes Activos, Roca 1242, RA-8332 G Roca, Rio Negro, Argentina	Universidade de Sao Paulo; Universidade Federal do Rio Grande do Sul; Universidade Estadual de Campinas; Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM)	Moncinhatto, TR (autor correspondente), Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226, BR-05508090 Sao Paulo, SP, Brazil.	rmthiago@iag.usp.br	Sommer, Carlos A/Q-9077-2018; Hartmann, Gelvam/K-4856-2012; Haag, Mauricio Barcelos/AAL-8648-2020; Trindade, Ricardo IF/A-8146-2008	Sommer, Carlos A/0000-0001-8696-7084; Hartmann, Gelvam/0000-0001-6078-3893; Haag, Mauricio Barcelos/0000-0001-5038-4418; Trindade, Ricardo IF/0000-0001-9848-9550; Poletti, Wilbor/0000-0002-1128-7604	CNPq [144580/2016-0, 454609/2014-0, 441766/2014-5, 303015/2015-2]; CAPES [AUXPE 2043/2014]; CNPq/CAPES [400724/2014-6]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq/CAPES(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work was supported by CNPq grant 144580/2016-0 to TRM, CAPES AUXPE 2043/2014 and CNPq grant 454609/2014-0 to GAH, CNPq/CAPES grant 400724/2014-6 and CNPq grants 441766/2014-5 and 303015/2015-2 to CAS. We thank D. Brandt, G. Moreira e P. Jaqueto by the support during sample preparation and data acquisition. We thank two anonymous reviewers for their helpful and constructive comments.	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J. Int.	FEB	2020	220	2					821	838		10.1093/gji/ggz483	http://dx.doi.org/10.1093/gji/ggz483			18	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	KC0AH		Green Published			2023-06-23	WOS:000506848400007
J	Fonseca, PHM; Martinelli, AG; Marinho, TD; Ribeiro, LCB; Schultz, CL; Soares, MB				Morais Fonseca, Pedro Henrique; Martinelli, Agustin Guillermo; Marinho, Thiago da Silva; Borges Ribeiro, Luiz Carlos; Schultz, Cesar Leandro; Soares, Marina Bento			Morphology of the endocranial cavities of Campinasuchus dinizi (Crocodyliformes: Baurusuchidae) from the Upper Cretaceous of Brazil	GEOBIOS			English	Article						Mesoeucrocodylia; Endocast; Sinuses; Paleoecology; South America	BAURU BASIN; METRIORHYNCHID CROCODYLIFORM; CRANIAL ENDOCAST; FRONTAL SINUSES; SKULL ANATOMY; SALT-GLANDS; SP-NOV.; EVOLUTION; BRAINCASE; CROCODYLOMORPHA	Two specimens of Campinasuchus dinizi (CPPLIP 1319 and CPPLIP 1360) belonging to Baurusuchidae (Crocodyliformes, Notosuchia) from the Upper Cretaceous Bauru Group of Minas Gerais state (Brazil) were scanned in a Toshiba Aquilion 64 CT machine. Based on these data, it was possible to identify and reconstruct the paranasal sinuses, the nasal cavity proper, the nasopharyngeal duct, the encephalon, the paratympanic sinuses, and the semicircular canals of the inner ear. The paranasal sinuses present similar morphology to those of other mesoeucrocodylians, especially eusuchians. The nasal cavity proper occupies the entire rostral region, with an expansion in the olfactory region. The expansion in the nasal cavity is present in other notosuchians and theropod dinosaurs (e.g., Tyrannosaurus rex Osborn, 1905), but less developed in aquatic crocodilians, which may indicate an olfactory acuity related to terrestrial habits. The encephalon is similar in shape to that of other mesoeucrocodylians. The rostral semicircular canal is smaller than the caudal one, differing from most mesoeucrocodylians. The paratympanic sinuses are more developed in C. dinizi than in eusuchians, being more similar to Tyrannosaurus rex. Campinasuchus dinizi presents few variations in the internal structures of the skull in relation to taxa with different ecological niches, probably indicating that ecological factors do not strongly influence the morphology of these structures. (C) 2020 Elsevier Masson SAS. All rights reserved.	[Morais Fonseca, Pedro Henrique; Schultz, Cesar Leandro; Soares, Marina Bento] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Porto Alegre, RS, Brazil; [Martinelli, Agustin Guillermo] Museo Argentino Ciencias Nat Bernardino Rivadavia, CONICET, Buenos Aires, DF, Argentina; [Morais Fonseca, Pedro Henrique; Martinelli, Agustin Guillermo; Marinho, Thiago da Silva; Borges Ribeiro, Luiz Carlos] Univ Fed Triangulo Mineiro, Complexo Cultural & Cient Peiropolis, Ctr Pesquisas Paleontol Llewellyn Ivor Price, PROEXT, Uberaba, Brazil; [Marinho, Thiago da Silva] Univ Fed Triangulo Mineiro, ICENE, Uberaba, Brazil; [Schultz, Cesar Leandro; Soares, Marina Bento] Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Inst Geociencias, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); Universidade Federal do Triangulo Mineiro; Universidade Federal do Triangulo Mineiro; Universidade Federal do Rio Grande do Sul	Fonseca, PHM (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Porto Alegre, RS, Brazil.; Fonseca, PHM (autor correspondente), Univ Fed Triangulo Mineiro, Complexo Cultural & Cient Peiropolis, Ctr Pesquisas Paleontol Llewellyn Ivor Price, PROEXT, Uberaba, Brazil.	phmorais.bio@gmail.com	Soares, Marina/AAN-8513-2020; Martinelli, Agustin G./D-4632-2015	Soares, Marina/0000-0002-8393-2406; Fonseca, Pedro Henrique/0000-0001-7721-9818	CNPq	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank CNPq for the funding of the master's degree fellowship to PHMF as well support for the other authors. We are especially grateful to Dr. Eduardo Felix and Dr. Vicente Antunes Teixeira for access to the medical CT at the Hospital de Cli ' nicas of the Universidade Federal do Triangulo Mineiro. During the development of this work we benefited from discussions with Voltaire Dutra Paes Neto, Tomaz Panceri Melo, Lucas Fiorelli, Fabiano Iori and Felipe Montefeltro. We thank Gabriel Schaffer Sipp for help with the making of the 3D models. The studied specimens were collected and prepared with the assistance of Amarildo Martins Queiroz, Orlandina Martins de Freitas and Jorcelino Henrique de Freitas from Fazenda Tres Antas (Campina Verde), and the staff of the Complexo Cultural e Cientifico de Peiro ' polis (CCCP) of the Universidade Federal do Triangulo Mineiro (Uberaba, Minas Gerais), whom we thank for their continuous support. We finally thank the two anonymous reviewers and the Associate-Editor Dr. Jeremy Martin that provided numerous comments and suggestions that greatly improved the manuscript.	Balanoff A. 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J	Nascimento, FS; Gastauer, M; Souza, PWM; Nascimento, WR; Santos, DC; Costa, MF				Nascimento, Filipe Silveira; Gastauer, Markus; Souza-Filho, Pedro Walfir M.; Nascimento, Wilson R.; Santos, Diogo C.; Costa, Marlene F.			Land Cover Changes in Open-Cast Mining Complexes Based on High-Resolution Remote Sensing Data	REMOTE SENSING			English	Article						GEOBIA; canga ecosystem; Carajas National Forest; mine land revegetation; satellite images; environmental assessment	IMAGERY; AMAZON; AREA; CLASSIFICATION; ACCURACY; SEGMENTATION; RECLAMATION; DISTURBANCE; LANDTRENDR; DYNAMICS	Remote sensing technologies can play a fundamental role in the environmental assessment of open-cast mining and the accurate quantification of mine land rehabilitation efforts. Here, we developed a systematic geographic object-based image analysis (GEOBIA) approach to map the amount of revegetated area and quantify the land use changes in open-cast mines in the Carajas region in the eastern Amazon, Brazil. Based on high-resolution satellite images from 2011 to 2015 from different sensors (GeoEye, WorldView-3 and IKONOS), we quantified forests, cangas (natural metalliferous savanna ecosystems), mine land, revegetated areas and water bodies. Based on the GEOBIA approach, threshold values were established to discriminate land cover classes using spectral bands, the normalized difference vegetation index (NDVI), normalized difference water index (NDWI) and a light detection and range sensor (LiDAR) digital terrain model and slope map. The overall accuracy was higher than 90%, and the kappa indices varied between 0.82 and 0.88. During the observation period, the mining complex expanded, which led to the conversion of canga and forest vegetation to mine land. At the same time, the amount of revegetated area increased. Thus, we conclude that our approach is capable of providing consistent information regarding land cover changes in mines, with a special focus on the amount of revegetation necessary to fulfill environmental liabilities.	[Nascimento, Filipe Silveira] Vale SA Mina Aguas Claras MAC, BR-34006270 Nova Lima, MG, Brazil; [Nascimento, Filipe Silveira; Gastauer, Markus; Souza-Filho, Pedro Walfir M.; Nascimento, Wilson R.; Santos, Diogo C.] Inst Tecnol Vale, BR-66055090 Belem, Para, Brazil; [Souza-Filho, Pedro Walfir M.] Univ Fed Para, Geosci Inst, BR-66075110 Belem, Para, Brazil; [Costa, Marlene F.] Vale SA Gerencia Meio Ambiente Corredor Norte, BR-65085582 Sao Luis, Maranhao, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Universidade Federal do Para	Souza, PWM (autor correspondente), Inst Tecnol Vale, BR-66055090 Belem, Para, Brazil.; Souza, PWM (autor correspondente), Univ Fed Para, Geosci Inst, BR-66075110 Belem, Para, Brazil.	filipe.silveira@vale.com; markus.gastauer@itv.org; pedro.martins.souza@itv.org; wilson.nascimento@itv.org; diogo.correa@pq.itv.org; marlene.costa@vale.com	Souza-Filho, Pedro Walfir M. M./J-4958-2012; Souza, Pedro/GZH-1275-2022; Gastauer, Markus/GMW-6022-2022	Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; 	CNPq; Carajas National Forest [SISBIO 35594-2]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Carajas National Forest	The authors thank the Vale Institute of Technology (ITV) for its management support. The authors are also grateful to the Vale Mining Company for logistical support. PWMSF was supported by CNPq through research scholarships. This project was carried out in the Carajas National Forest with permission from IBAMA (SISBIO 35594-2).	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FEB	2020	12	4							611	10.3390/rs12040611	http://dx.doi.org/10.3390/rs12040611			21	Environmental Sciences; Geosciences, Multidisciplinary; Remote Sensing; Imaging Science & Photographic Technology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Remote Sensing; Imaging Science & Photographic Technology	KU2UY		gold			2023-06-23	WOS:000519564600022
J	Neves, SP; Teixeira, CML; Bruguier, O				Neves, Sergio P.; Teixeira, Cristiane M. L.; Bruguier, Olivier			Long-lived localized magmatism in central-eastern part of the Pernambuco-Alagoas Domain, Borborema Province (NE Brazil): Implications for tectonic setting, heat sources, and lithospheric reworking	PRECAMBRIAN RESEARCH			English	Article						U-Pb geochronology; Major and trace elements; Petrogenesis; Crustal evolution; Brasiliano Orogeny; Borborema Province	NEOPROTEROZOIC SERGIPANO BELT; A-TYPE GRANITES; CONTINENTAL-CRUST; WESTERN GONDWANA; SUPRACRUSTAL SEQUENCES; REGIONAL METAMORPHISM; ZIRCON GEOCHRONOLOGY; BRASILIANO OROGENY; PB GEOCHRONOLOGY; TONALITIC GNEISS	Magmatic activity circumscribed to a restricted area lasting for tenths of millions of years allows to link changes in magma chemistry to deformation, and thus to determine the tectonic evolution of a region. Here we describe an area of about 180 x 40 km in eastern Borborema Province (northeastern Brazil) where several pulses of magmatism occurred in the time interval 656-562 Ma. The oldest pulses are represented by orthogneisses bearing a flat-lying foliation resulting from deformation and metamorphism of granitoids emplaced in three stages: 656-645 Ma, 632-618 Ma, and 606-597 Ma. The oldest and most important unit (656-652 Ma-old) has large length/width ratio (c. 10), alkali-calcic signature, lacks pronounced negative Ta anomalies whereas showing positive Hf and Zr anomalies in normalized trace element diagrams, and yields crystallization age similar to the deposition age of surrounding, dominantly elastic metasedimentary units. These characteristics point to emplacement in an extensional setting and most probably fit in a rift/sag basin model, with thermal thinning of the lithosphere generating regional subsidence and magmatism. Rocks related to the 632-618 Ma-old stage are represented by orthogneisses with petrographic and geochemical characteristics akin to I-type granites, indicating a shift to an orogenic setting at around 640-630 Ma. Increased radioactive heating during continued thickening promoted anatexis of metasedimentary rocks at mid-crustal levels and segregation of small volumes of peraluminous melts at 606-597 Ma. The subsequent period of magmatic activity at 587-581 Ma witnesses the transition to a transcurrent regime, with intrusion of large granitic and syenitic batholiths with high-K calcalkalic to shoshonitic affinity. Intrusion of these plutons added to heat resulting from strain heating to produce peraluminous granites at 573-566 Ma through partial melting of metasedimentary sources. The final magmatic episode at c. 562 Ma suggests involvement of the lithospheric mantle and crustal sources, perhaps related to localized delamination. Generally, younger orthogneisses and plutons contain zircons inherited from previous magmatic events, pointing to important crustal reworking. Together with the geochemistry of the rocks, these results imply only modest addition of juvenile material and thus no net crustal growth in eastern Borborema Province during the 660-560 Ma time interval.	[Neves, Sergio P.] Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil; [Teixeira, Cristiane M. L.] Univ Fed Sul & Sudeste Para, Maraba, Brazil; [Bruguier, Olivier] Univ Montpellier, Geosci Montpellier, Montpellier, France	Universidade Federal de Pernambuco; Universidade Federal do Sul e Sudeste do Para; Universite de Montpellier	Neves, SP (autor correspondente), Univ Fed Pernambuco, Dept Geol, BR-50740530 Recife, PE, Brazil.	serpane@hotlink.com.br	Neves, Sergio/A-2086-2008	Neves, Sergio/0000-0001-6690-3278	Brazilian agency Conselho Nacional de Desenvolvimento CientIfico e Tecnologico (CNPq) [472582/2011-9]; CNPq	Brazilian agency Conselho Nacional de Desenvolvimento CientIfico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was supported through funding from the Brazilian agency Conselho Nacional de Desenvolvimento CientIfico e Tecnologico (CNPq; grant 472582/2011-9). CMLT also thanks scholarship from CNPq. Detailed comments by two anonymous reviewers on a previous version helped to significantly improve the manuscript. We thank D'el Rey Silva for his suggestions to improve the current version.	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FEB	2020	337								105559	10.1016/j.precamres.2019.105559	http://dx.doi.org/10.1016/j.precamres.2019.105559			32	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KH3DY					2023-06-23	WOS:000510527900022
J	Raddatz, J; Titschack, J; Frank, N; Freiwald, A; Conforti, A; Osborne, A; Skornitzke, S; Stiller, W; Rueggeberg, A; Voigt, S; Albuquerque, ALS; Vertino, A; Schroeder-Ritzrau, A; Bahr, A				Raddatz, J.; Titschack, J.; Frank, N.; Freiwald, A.; Conforti, A.; Osborne, A.; Skornitzke, S.; Stiller, W.; Rueggeberg, A.; Voigt, S.; Albuquerque, A. L. S.; Vertino, A.; Schroeder-Ritzrau, A.; Bahr, A.			Solenosmilia variabilis-bearing cold-water coral mounds off Brazil	CORAL REEFS			English	Article						Cold-water corals; South Atlantic; Th-230; U; Computed tomography	DEEP-SEA CORALS; LOPHELIA-PERTUSA SCLERACTINIA; EASTERN NORTH-ATLANTIC; CARBONATE-MOUND; WESTERN BOUNDARY; ROCKALL TROUGH; PACIFIC-OCEAN; FUGLOY REEF; NE ATLANTIC; ICE-CORE	Cold-water corals (CWC), dominantly Desmophyllum pertusum (previously Lophelia pertusa), and their mounds have been in the focus of marine research during the last two decades; however, little is known about the mound-forming capacity of other CWC species. Here, we present new Th-230/U age constraints of the relatively rarely studied framework-building CWC Solenosmilia variabilis from a mound structure off the Brazilian margin combined with computed tomography (CT) acquisition. Our results show that S. variabilis can also contribute to mound formation, but reveal coral-free intervals of hemipelagic sediment deposits, which is in contrast to most of the previously studied CWC mound structures. We demonstrate that S. variabilis only occurs in short episodes of < 4 kyr characterized by a coral content of up to 31 vol%. In particular, it is possible to identify distinct clusters of enhanced aggradation rates (AR) between 54 and 80 cm ka(-1). The determined AR are close to the maximal growth rates of individual S. variabilis specimens, but are still up to one order of magnitude smaller than the AR of D. pertusum mounds. Periods of enhanced S. variabilis AR predominantly fall into glacial periods and glacial terminations that were characterized by a 60-90 m lower sea level. The formation of nearby D. pertusum mounds is also associated with the last glacial termination. We suggest that the short-term periods of coral growth and mound formation benefited from enhanced organic matter supply, either from the adjacent exposed shelf and coast and/or from enhanced sea-surface productivity. This organic matter became concentrated on a deeper water-mass boundary between South Atlantic Central Water and the Antarctic Intermediate Water and may have been distributed by a stronger hydrodynamic regime. Finally, periods of enhanced coral mound formation can also be linked to advection of nutrient-rich intermediate water masses that in turn might have (directly or indirectly) further facilitated coral growth and mound formation.	[Raddatz, J.; Voigt, S.] Goethe Univ Frankfurt, Inst Geosci, Altenhoferallee 1, D-60438 Frankfurt, Germany; [Titschack, J.; Freiwald, A.] Univ Bremen, MARUM Ctr Marine Environm Sci, Leobener Str 8, D-28359 Bremen, Germany; [Titschack, J.; Freiwald, A.] Marine Res Dept, Sudstrand 40, D-26382 Wilhelmshaven, Germany; [Frank, N.; Schroeder-Ritzrau, A.] Heidelberg Univ, Inst Umweltphys, Neuenheimer Feld 229, D-69120 Heidelberg, Germany; [Conforti, A.] CNR, IAS, Ist Studio Impatti Antropici & Sostenibilita Ambi, Loc Sa Mardini Torregran, Oristano, Italy; [Osborne, A.] GEOMAR Helmholtz Ctr Ocean Res, Wischhofstr 1-3, D-24148 Kiel, Germany; [Skornitzke, S.; Stiller, W.] Heidelberg Univ Hosp, DIR, Neuenheimer Feld 110, D-69120 Heidelberg, Germany; [Rueggeberg, A.] Univ Fribourg, Dept Geosci, Chemin Musee 6, CH-1700 Fribourg, Switzerland; [Albuquerque, A. L. S.] Univ Fed Fluminense, Programa Geociencias Geoquim, Niteroi, RJ, Brazil; [Vertino, A.] Univ Ghent, Dept Geol, Krijgslaan 281,S8, B-9000 Ghent, Belgium; [Vertino, A.] Univ Milano Bicocca, Dept Earth & Environm Sci, Piazza Sci 4, I-20126 Milan, Italy; [Bahr, A.] Heidelberg Univ, Inst Geowissensch, Neuenheimer Feld 234-236, D-69120 Heidelberg, Germany	Goethe University Frankfurt; University of Bremen; Ruprecht Karls University Heidelberg; Consiglio Nazionale delle Ricerche (CNR); Istituto per lo Studio degli Impatti Antropici Sostenibilita in Ambiente Marino (IAS-CNR); Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; Ruprecht Karls University Heidelberg; University of Fribourg; Universidade Federal Fluminense; Ghent University; University of Milano-Bicocca; Ruprecht Karls University Heidelberg	Raddatz, J (autor correspondente), Goethe Univ Frankfurt, Inst Geosci, Altenhoferallee 1, D-60438 Frankfurt, Germany.	raddatz@em.uni-frankfurt.de	conforti, alessandro/M-7295-2015; 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J	Sbaraini, S; Raposo, MIB; Bitencourt, MD; Tome, CR				Sbaraini, Samuel; Raposo, M. Irene B.; Bitencourt, Maria de Fatima; Tome, Camila Rocha			Magnetic fabrics of the neoproterozoic piquiri syenite massif (Southernmost Brazil): Implications for 3D geometry and emplacement	JOURNAL OF GEODYNAMICS			English	Article						Magnetic fabric; AMS; Rock magnetism; Magma flow; Emplacement fabrics; Syenite	PARTIAL ANHYSTERETIC REMANENCE; GRANITE PLUTON; SUSCEPTIBILITY; ANISOTROPY	The study of magnetic fabrics and rock magnetic properties, together with geological and structural mapping, was carried out in a syenite pluton to investigate its shape and emplacement history. The Piquiri Syenite Massif (PSM) is an alkaline pluton which exhibits S > > L magmatic fabric and is interpreted to be part of the last Neoproterozoic post-collisional magmatic episodes in southernmost Brazil. Thermomagnetic curves, hysteresis data and coercivity spectra obtained from representative samples of different facies in the massif reveal that magnetic susceptibility is dominated by ferromagnetic minerals, especially magnetite. Magnetic fabric data were determined by using Anisotropy of Magnetic Susceptibility (AMS) and Anisotropy of Anhysteretic Remanence (AARM). Both fabrics are coaxial, and the parallelism of AMS and AARM tensors in more than 84 % of the sampled sites rules out the possibility of significant effects of Single Domain (SD) crystals. The magnetic foliation is concordant with the magmatic foliation field measurements, both parallel to pluton contacts, with high, inward dip angles. The magnetic lineation shows distinct but related behaviour from one facies to another. It is dominantly subvertical in the marginal fades rocks and plunges at moderate to shallow angles in the main facies. It is sub-horizontal in the quartz-syenites and plunges at shallow angles in the granitic rocks. Oxidizing conditions determined from the study of magnetic mineralogy leads to challenge former interpretation of in situ differentiation and crystallization and points to the multi-intrusive character of the pluton. Field relations such as fragments of marginal facies rocks found within the main facies rocks, which are in turn intruded by quartz-syenites, together with the general absence of contact metamorphism except near the marginal facies, lead to interpret that a sequence of magmatic pulses have built up the pluton. Thus, a first magmatic pulse may have heated the host rocks and resulted in the marginal facies which was followed by the next pulses to form the main fades and the quartz-rich varieties, therefore constructing the pluton from outside inwards.	[Sbaraini, Samuel; Bitencourt, Maria de Fatima; Tome, Camila Rocha] Univ Fed Rio Grande do Sul, Programa Pos Grad Geociencias, Av Bento Goncalves 9500, BR-1501970 Porto Alegre, RS, Brazil; [Raposo, M. Irene B.] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil	Universidade Federal do Rio Grande do Sul; Universidade de Sao Paulo	Sbaraini, S; Bitencourt, MD; Tome, CR (autor correspondente), Univ Fed Rio Grande do Sul, Programa Pos Grad Geociencias, Av Bento Goncalves 9500, BR-1501970 Porto Alegre, RS, Brazil.; Raposo, MIB (autor correspondente), Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil.	samueldesde82@gmail.com; Irene@usp.br; fatimab@ufrgs.br; camilarocha.tome@gmail.com	Raposo, M. Irene B./D-6896-2013; de Fátima Bitencourt, Maria/H-8957-2016; Bitencourt, Maria de Fátima/GLR-8862-2022	de Fátima Bitencourt, Maria/0000-0001-7022-9175; Bitencourt, Maria de Fátima/0000-0001-7022-9175	Rio Grande do Sul State Research Foundation (FAPERGS) [10/0045-6]; National Research Council (CNPq) [471266/2010-8]	Rio Grande do Sul State Research Foundation (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); National Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This paper is part of Samuel Sbaraini's MSc thesis. The research was supported by the Rio Grande do Sul State Research Foundation (FAPERGS, 10/0045-6) and National Research Council (CNPq, Universal Program 471266/2010-8) granted to M.F. Bitencourt.	ARCHANJO CJ, 1995, PHYS EARTH PLANET IN, V89, P63, DOI 10.1016/0031-9201(94)02997-P; Babinski M, 1997, J S AM EARTH SCI, V10, P263, DOI 10.1016/S0895-9811(97)00021-7; Bitencourt M. F., 2000, REV BRAS GEOCIENC, V30, P186, DOI [10.25249/0375-7536.2000301186189, DOI 10.25249/0375-7536.2000301186189]; Borradaile GJ, 1997, EARTH-SCI REV, V42, P49, DOI 10.1016/S0012-8252(96)00044-X; Bouchez JL, 1997, PETR STRU G, V8, P95; Cid JP, 2003, CONTRIB MINERAL PETR, V145, P444, DOI 10.1007/s00410-003-0451-4; Cruden AR, 1999, J GEOPHYS RES-SOL EA, V104, P10511, DOI 10.1029/1998JB900093; de Oliveira DC, 2010, TECTONOPHYSICS, V493, P27, DOI 10.1016/j.tecto.2010.07.018; HARGRAVES RB, 1991, GEOPHYS RES LETT, V18, P2193, DOI 10.1029/91GL01777; Hartmann L., 1999, PESQUI GEOCIE NCIAS, V26, P45, DOI [10.22456/1807-9806.21123, DOI 10.22456/1807-9806.21123]; JACKSON M, 1988, GEOPHYS RES LETT, V15, P440, DOI 10.1029/GL015i005p00440; JACKSON M, 1989, GEOPHYS RES LETT, V16, P1063, DOI 10.1029/GL016i009p01063; JELINEK V, 1978, STUD GEOPHYS GEOD, V22, P50, DOI 10.1007/BF01613632; JELINEK V, 1981, TECTONOPHYSICS, V79, pT63, DOI 10.1016/0040-1951(81)90110-4; Jelinek V., 1977, STAT THEORY MEASURIN; Martil M.M.D., 2007, MONOGRAFIA CONCLUSIO; Nardi LVS, 2007, MINER PETROL, V91, P101, DOI 10.1007/s00710-007-0186-4; NARDI L. V. S., 2002, PESQ GEOC, V29, P21; Nardi LVS, 2008, AN ACAD BRAS CIENC, V80, P353, DOI 10.1590/S0001-37652008000200014; OZDEMIR O, 1993, GEOPHYS RES LETT, V20, P1671, DOI 10.1029/93GL01483; Paterson SR, 1998, LITHOS, V44, P53, DOI 10.1016/S0024-4937(98)00022-X; Peternell M, 2011, J STRUCT GEOL, V33, P609, DOI 10.1016/j.jsg.2011.01.011; Philipp R.P., 2003, REV BRASILEIRA GEOCI, V32, P277, DOI [10.25249/0375-7536.2002322277290, DOI 10.25249/0375-7536.2002322277290]; Raposo MIB, 2009, TECTONOPHYSICS, V466, P18, DOI 10.1016/j.tecto.2008.10.015; Stabel L.Z., 2001, REV BRAS GEOSCI, V31, P211; Stahel L.Z., 2000, THESIS; STEPHENSON A, 1986, GEOPHYS J INT, V84, P185, DOI 10.1111/j.1365-246X.1986.tb04351.x; Tarling D., 1993, MAGNETIC ANISOTROPY, DOI DOI 10.1002/GJ.3350300111; Trubac J, 2009, J VOLCANOL GEOTH RES, V181, P25, DOI 10.1016/j.jvolgeores.2008.12.005	29	2	2	0	3	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0264-3707			J GEODYN	J. Geodyn.	FEB	2020	134								101691	10.1016/j.jog.2019.101691	http://dx.doi.org/10.1016/j.jog.2019.101691			13	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	KU4GI					2023-06-23	WOS:000519667600004
J	Vieira, TC; Rodrigues, APD; Amaral, PMG; de Oliveira, DFC; Goncalves, RA; Silva, CRE; Vasques, RO; Malm, O; Silva, EV; Godoy, JMD; Machado, W; Filippo, A; Bidone, ED				Vieira, Thatianne C.; Rodrigues, Ana Paula de C.; Amaral, Petrus M. G.; de Oliveira, Douglas F. C.; Goncalves, Rodrigo A.; Rodrigues e Silva, Camila; Vasques, Ricardo O.; Malm, Olaf; Silva-Filho, Emmanoel, V; Godoy, Jose M. de O.; Machado, Wilson; Filippo, Alejandra; Bidone, Edison D.			Evaluation of the bioaccumulation kinetics of toxic metals in fish (A. brasiliensis) and its application on monitoring of coastal ecosystems	MARINE POLLUTION BULLETIN			English	Article						Prognosis of metals concentrations; Polynomial regressions; Probit model; Incorporation rate model	RIO-DE-JANEIRO; SILVERSIDE ATHERINELLA-BRASILIENSIS; GUANABARA BAY; HEAVY-METALS; BRAZILIAN AMAZON; TROPICAL ESTUARY; MERCURY; SEDIMENTS; METHYLMERCURY; BIOMAGNIFICATION	This study proposes a pro-active approach for evaluations of methylmercury (MeHg), total mercury (THg), arsenic (As), cadmium (Cd) and lead (Pb) in situ bioaccumulation in fish (Atherinella brasiliensis) muscles, using specimens from the external sector of Guanabara Bay as a study case. This approach included an hierarchical sequence: analysis of the pollutants concentrations and their comparison to safety criteria; correlations between specimens concentrations vs length (as a proxy of exposure time); projections of concentrations in key lengths (sexual maturation, asymptotic, length limits for fishing and median of fish population) through polynomial regressions, dose-response analysis (Probit), decreasing curves and incorporation rates (using only three length intervals). The incorporation rates were ascending for MeHg and THg (continued bioaccumulation) and descending for As, Pb and Cd (possible biological dilution). The projections were satisfactory, evidencing their use for an improvement on the risks monitoring of fishing and fish consumption by humans in coastal environments.	[Vieira, Thatianne C.; Rodrigues e Silva, Camila; Vasques, Ricardo O.; Silva-Filho, Emmanoel, V; Machado, Wilson; Bidone, Edison D.] Univ Fed Fluminense, Postgrad Program Geochem, Niteroi, RJ, Brazil; [Rodrigues, Ana Paula de C.] Univ Fed Rio de Janeiro, Dept Marine Biol, Rio De Janeiro, RJ, Brazil; [Amaral, Petrus M. G.; Malm, Olaf] Univ Fed Rio de Janeiro, Inst Biophys Carlos Chagas Filho, Rio De Janeiro, RJ, Brazil; [de Oliveira, Douglas F. C.; Goncalves, Rodrigo A.; Godoy, Jose M. de O.] Pontif Univ Catolica Rio de Janeiro, Inst Chem, Rio De Janeiro, RJ, Brazil; [Filippo, Alejandra] Univ Fed Fluminense, Dept Zootechny & Dev Agr Social Environm Sustaina, Niteroi, RJ, Brazil	Universidade Federal Fluminense; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal Fluminense	Vieira, TC (autor correspondente), Univ Fed Fluminense, Postgrad Program Geochem, Niteroi, RJ, Brazil.	thatiannev@id.uff.br	Machado, Wilson/P-8047-2019; Rodrigues, Ana Paula C/M-2927-2016; da Silva Filho, Emmanoel Vieira/Y-7281-2019; Galvao, P./ABF-1623-2020; Bidone, Edison/AAE-9527-2021	Machado, Wilson/0000-0003-3117-8584; Rodrigues, Ana Paula C/0000-0001-7704-0201; da Silva Filho, Emmanoel Vieira/0000-0001-6444-6851; Galvao, P./0000-0002-4711-4406; Bidone, Edison/0000-0002-5771-5651; Santos, Alejandra/0000-0002-3934-4279; Malm, Olaf/0000-0002-4116-7160	Coordination for the Improvement of Higher Education Personnel (CAPES); National Council for Scientific and Technological Development (CNPq); Research Support Foundation for the State of Rio de Janeiro (FAPERJ); PROPPI/UFF	Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Research Support Foundation for the State of Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); PROPPI/UFF	We thank the staff of the Applied Ecology Laboratory, MZO, Veterinary School (UFF) for providing the material for study. We also thank the financial supports of this project: Coordination for the Improvement of Higher Education Personnel (CAPES) and National Council for Scientific and Technological Development (CNPq) - for students' grants; Research Support Foundation for the State of Rio de Janeiro (FAPERJ) and PROPPI/UFF - for research grant.	Abuchacra PFF, 2015, MAR POLLUT BULL, V100, P414, DOI 10.1016/j.marpolbul.2015.08.012; AKAGI H, 1994, ENV SCI, V3, P25; AMADOR ED, 1980, AN ACAD BRAS CIENC, V52, P723; Andreata Jose V., 1997, Revista Brasileira de Zoologia, V14, P121; Ansari N.R., 2015, THESIS; ANVISA. 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Pollut. Bull.	FEB	2020	151								110830	10.1016/j.marpolbul.2019.110830	http://dx.doi.org/10.1016/j.marpolbul.2019.110830			10	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	KN3RQ	32056622				2023-06-23	WOS:000514758400032
J	Zular, A; Sawakuchi, AO; Wang, H; Guedes, CCF; Hartmann, GA; Jaqueto, PF; Chiessi, CM; Cruz, FW; Giannini, PCF; Daros, VK; Atencio, D; Trindade, RIF				Zular, Andre; Sawakuchi, Andre O.; Wang, Hong; Guedes, Carlos C. F.; Hartmann, Gelvam A.; Jaqueto, Plinio F.; Chiessi, Cristiano M.; Cruz, Francisco W.; Giannini, Paulo C. F.; Daros, Vinicius K.; Atencio, Daniel; Trindade, Ricardo I. F.			The response of a dune succession from Lencois Maranhenses, NE Brazil, to climate changes between MIS 3 and MIS 2	QUATERNARY INTERNATIONAL			English	Article						Lencois maranhenses dunefield; Heinrich stadials; Last glacial maximum; Paleoclimate; Coastal eolian deposits; Optically stimulated luminescence; Multy-proxy approach	HEINRICH STADIAL 1; LAST GLACIAL MAXIMUM; DOSE-RATE; LATE QUATERNARY; GRAIN-SIZE; DUST ACCUMULATION; SINGLE GRAINS; LUMINESCENCE; QUARTZ; NORTH	In tropical Southern Hemisphere South America, late Quaternary marine core and speleothem records provide different proxies and accurate chronologies correlating millennial-scale intervals of increased precipitation with southward shifts of the Intertropical Convergence Zone (ITCZ). However, the climatic effect of these intervals on coastal landforms is poorly understood. Here we investigated the response of abrupt and long-lasting climate events during the Marine Isotope Stages 3 and 2 in a 13.8-m thick sand succession located in a large-scale coastal eolian system, the Lencois Maranhenses Dunefield, NE Brazil, where winds and precipitation are anti-phased and controlled by the single action of the ITCZ. A chronology of the sediment overburden determined by optically stimulated luminescence (OSL) dating of 14 sediment samples obtained at 1-m intervals showed ages between 132.2 +/- 7.0 and 12.9 +/- 0.6 thousand years ago in stratigraphic order. A multi-proxy approach based on grain size, surface grain texture, heavy minerals, thermoluminescence (TL) sensitivity, inorganic geochemistry, reflectance, and magnetic parameters from 268 sediment samples collected at 5-cm intervals indicated periods of dune building and stabilization. Significant stabilization periods are synchronous with Heinrich Stadials 6, 4, 3, 2, and 1, and Greenland Stadial 4, within age model uncertainties. Heavy mineral analysis indicated a steady sand source to the dune succession, while TL sensitivity analysis of quartz grains showed the input allochthonous sediments during stadials. The preservation of peak dune activity during the Last Glacial Maximum is attributed to the enduring precipitation brought by the subsequent Heinrich Stadial 1 event.	[Zular, Andre; Sawakuchi, Andre O.; Cruz, Francisco W.; Giannini, Paulo C. F.; Atencio, Daniel] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Wang, Hong] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Shaanxi, Peoples R China; [Wang, Hong] Beijing Normal Univ, Interdisciplinary Res Ctr Earth Sci Frontier, Beijing, Peoples R China; [Wang, Hong] Univ Illinois, Prairie Res Inst, Illinois State Geol Survey, Champaign, IL USA; [Guedes, Carlos C. F.] Univ Fed Parana, Dept Geol, Curitiba, Parana, Brazil; [Hartmann, Gelvam A.] Univ Estadual Campinas, Inst Geociencias, Campinas, SP, Brazil; [Jaqueto, Plinio F.; Trindade, Ricardo I. F.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Sao Paulo, SP, Brazil; [Jaqueto, Plinio F.] Univ Minnesota, Inst Rock Magnetism, Dept Earth & Environm Sci, Minneapolis, MN USA; [Chiessi, Cristiano M.] Univ Sao Paulo, Escola Artes Ciencias & Humanidades, Sao Paulo, SP, Brazil; [Daros, Vinicius K.] Univ Sao Paulo, Inst Matemat & Estat, Sao Paulo, SP, Brazil	Universidade de Sao Paulo; Chinese Academy of Sciences; Institute of Earth Environment, CAS; Beijing Normal University; University of Illinois System; University of Illinois Urbana-Champaign; Universidade Federal do Parana; Universidade Estadual de Campinas; Universidade de Sao Paulo; University of Minnesota System; University of Minnesota Twin Cities; Universidade de Sao Paulo; Universidade de Sao Paulo	Zular, A (autor correspondente), Univ Sao Paulo, Inst Geociencias, Luminescence & Gamma Spectrometry Lab, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil.	andrezular@usp.br	Trindade, Ricardo IF/A-8146-2008; Sawakuchi, André O/D-1445-2013; Guedes, Carlos Conforti Ferreira/F-3639-2015; Chiessi, Cristiano Mazur/E-1916-2012; Atencio, Daniel/C-1626-2013; Jaqueto, Plinio/O-4012-2019; Cruz, Francisco W/G-6059-2012; Giannini, Paulo César Fonseca/D-1871-2015; Hartmann, Gelvam/K-4856-2012	Trindade, Ricardo IF/0000-0001-9848-9550; Guedes, Carlos Conforti Ferreira/0000-0001-8816-9174; Chiessi, Cristiano Mazur/0000-0003-3318-8022; Atencio, Daniel/0000-0002-6943-5227; Jaqueto, Plinio/0000-0002-5907-1474; Giannini, Paulo César Fonseca/0000-0003-1046-0177; Hartmann, Gelvam/0000-0001-6078-3893; Cruz, Francisco/0000-0002-4030-4581; Sawakuchi, Andre/0000-0001-5016-2428	FAPESP [2009/54232-4, 2009/53988-8]; CAPES [564/2015]; CNPq [304727/2017-2, 306527/2017-0, 302607/2016-1, 422255/2016-5]	FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are grateful to the editor and the anonymous reviewer for their helpful comments and suggestions that improved the quality of this manuscript. We thank Isaac Jamil Sayeg for helping and discussing SEM analysis. We acknowledge Elaine Sinfronio and Jordana Zampelli for helping in the sedimentological analysis. We are grateful for Thelma Samara for helping in the final regional map and Arotec Industria e Comercio for providing the XRF equipment. We thank FAPESP for funding this research (grants 2009/54232-4 and 2009/53988-8). Cristiano M. Chiessi acknowledges the financial support from CAPES (grant 564/2015) and CNPq (grants 302607/2016-1, 422255/2016-5). Andre O. Sawakuchi and Gelvam A. Hartmann are supported by CNPq (grants 304727/2017-2 and 306527/2017-0, respectively).	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Int.	JAN 30	2020	537						97	111		10.1016/j.quaint.2019.12.012	http://dx.doi.org/10.1016/j.quaint.2019.12.012			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	KR6UO					2023-06-23	WOS:000517751500010
J	Coimbra, JC; Bergue, CT; Ramos, MIF				Coimbra, Joao Carlos; Bergue, Cristianini Trescastro; Feijo Ramos, Maria Ines			Is Copytus Skogsberg, 1939 (Crustacea: Ostracoda) a neocytherideid? With description of a new family and two new species	ZOOTAXA			English	Article						Ostracod; marine biodiversity; taxonomy; South Atlantic	COAST; NORTHEASTERN; ISLAND; GENUS	The genus Copytus Skogsberg, 1939 was erected based on C. caligula, recovered from bottom sediments of the South Georgia Island, Antarctica. However, we propose herein that Skogsberg's species is a junior synonym of Cvtherideis laevata Brady, 1880 also collected from Antarctica and, therefore, Copytus laevata (Brady, 1880) becomes the type species. The position of the genus Copytus in the family Neocytherideidae is discussed, and a new family is proposed. In addition, we consider the genus Neocopytus Kulkoyluoolu, Colin & Kilic, 2007 invalid, and some of its species are transferred to Copytus. Finally, two new species of Copytus are herein described, C. cuspidata sp. nov. and C. wuerdigae sp. nov.. and their geographic, bathymetric and stratigraphic distributions are discussed.	[Coimbra, Joao Carlos] Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Av Bento Goncalves 9500,Cx P 15001, BR-91501970 Porto Alegre, RS, Brazil; [Bergue, Cristianini Trescastro] Univ Fed Rio Grande do Sul, Ctr Estudos Costeiros Limnol & Marinhos, CECLIMAR, Av Tramandai 976, BR-95625000 Imbe, RS, Brazil; [Feijo Ramos, Maria Ines] Museu Paraense Emilio Goeldi, Av Perimetral 1901, BR-66077830 Belem, Para, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Museu Paraense Emilio Goeldi	Coimbra, JC (autor correspondente), Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Av Bento Goncalves 9500,Cx P 15001, BR-91501970 Porto Alegre, RS, Brazil.	joao.coimbra@ufrgs.br; ctbergue@gmail.com; mramos@museu-goeldi.br	Coimbra, J. C./H-7500-2013	Coimbra, J. C./0000-0002-8980-6531	National Council for Scientific and Technological Development (CNPq) [305128/2017-5]	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are grateful to Petroleo Brasileiro S.A (Petrobras), the Brazilian Navy and the Departamento de Geografia (Universidade Federal do Rio de Janeiro) for providing the samples. Thanks are due to late R.C. Whatley for the invaluable criticism, which improved the earlier version of this manuscript. The editor Renate Matzke-Karasz and Claudia Pinto Machado are thanked for their comments and suggestions. We are also indebted to two reviewers, especially Maria Cristina Cabral for her valuable suggestions on early drafts of this work. J.C. Coimbra thanks the National Council for Scientific and Technological Development (CNPq) for the grant 305128/2017-5.	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J	Miranda, DA; Chaves, AD; Dussin, IA; Porcher, CC				Miranda, Daniel Andrade; Chaves, Alexandre de Oliveira; Dussin, Ivo Antonio; Porcher, Carla Cristine			Paleoproterozoic khondalites in Brazil: a case study of metamorphism and anatexis in khondalites from Itapecerica supracrustal succession of the southern Sao Francisco Craton	INTERNATIONAL GEOLOGY REVIEW			English	Article						Khondalite; provenance; anatexis; petrology; geochronology; P-T-t path; Sao Francisco Craton	P-T PATH; MINERAL EQUILIBRIA CALCULATIONS; NORTH CHINA CRATON; U-PB; METASEDIMENTARY ROCKS; CRUSTAL EVOLUTION; MINEIRO BELT; GEOCHEMICAL CLASSIFICATION; QUADRILATERO-FERRIFERO; METAPELITIC GRANULITES	In Brazil, Paleoproterozoic khondalites were recognized in Ceara, Bahia, Goias, Tocantins, and Minas Gerais. The Itapecerica supracrustal succession in the Southern Sao Francisco Craton (Minas Gerais) contains sillimanite-cordierite-garnet-biotite gneiss (khondalite) with an anatectic record. The high-grade khondalite preserve representative mineral assemblages of peak and orogen collapse after post-peak decompressional stage. Based on petrographic observations and P-T pseudosections of bulk rock compositions, a clockwise pressure-temperature-time (P-T-t) path was inferred. The metamorphic peak assemblage is liquid + plagioclase +/- K-feldspar + garnet + biotite + ilmenite + sillimanite + quartz at 715-772oC and 5.5-7.5 kbar. In addition, the precursor sediments had mixed pelitic-wacke compositions resulting from erosion of different sources. Sediment deposition would have occurred at active continental marginal setting. Surrounding the khondalite occurs a peraluminous metagranite named here as agua Rasa, formed in syn- to post-collisional setting, whose epsilon Nd-(t) (-0.5 to -2.7) and Sr-87/Sr-86((t)) (1.04 to 1.08) and the data set indicate that the precursor magma of the agua Rasa metagranite originated from anatexis of the khondalitic rocks (crustal source) and associated amphibolites (mantle source) during the crustal thickening followed by tectonic exhumation at peak metamorphism and at decompressional stage during the orogenic collapse. The khondalite yielded ages from monazite U-Th-Pb-T dating of 2090 +/- 26 Ma and 1937 +/- 32 Ma, while the agua Rasa metagranite yielded ages of 2077 +/- 24 Ma and 1941 +/- 23 from monazite and 1934 +/- 74 Ma from zircon U-Pb. The ages of >2.0 Ga are related to the metamorphic peak, while the younger ones (similar to 1940 Ma) are related to the orogen collapse after post-peak decompressional stage. Similarities between the khondalite rocks of this study and of the North China Craton suggest that the Sao Francisco-Congo Craton was near the North China Craton in the supercontinent Columbia for the 2.1-1.9 Ga period.	[Miranda, Daniel Andrade; Chaves, Alexandre de Oliveira] Fed Univ Minas Gerais UFMG, Inst Geosci, Geol Dept, Av Antonio Carlos, BR-6627 Belo Horizonte, MG, Brazil; [Dussin, Ivo Antonio] State Univ Rio De Janeiro UERJ, Reg Geol & Geotecton Dept, Rio De Janeiro, Brazil; [Porcher, Carla Cristine] Fed Univ Rio Grande Do Sul UFRGS, Inst Geosci, Porto Alegre, RS, Brazil	Universidade Federal de Minas Gerais; Universidade do Estado do Rio de Janeiro; Universidade Federal do Rio Grande do Sul	Miranda, DA (autor correspondente), Fed Univ Minas Gerais UFMG, Inst Geosci, Geol Dept, Av Antonio Carlos, BR-6627 Belo Horizonte, MG, Brazil.	miranda.geologia@gmail.com	Porcher, Carla C/R-1419-2018; Chaves, A. O./F-8832-2014	Porcher, Carla C/0000-0002-0418-3954; 	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; FAPEMIG [APQ-00654-16]; CNPq	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); FAPEMIG(Fundacao de Amparo a Pesquisa do Estado de Minas Gerais (FAPEMIG)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	To the Nacional de Grafite Company, the geologist Lairton de Oliveira and geology supervisor Gilson dos Santos. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001. The second author thanks to CNPq the research productivity grant and to FAPEMIG for research support through the project APQ-00654-16.	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J	Cisneros, J; Best, J; van Dijk, T; de Almeida, RP; Amsler, M; Boldt, J; Freitas, B; Galeazzi, C; Huizinga, R; Ianniruberto, M; Ma, HB; Nittrouer, JA; Oberg, K; Orfeo, O; Parsons, D; Szupiany, R; Wang, P; Zhang, YF				Cisneros, Julia; Best, Jim; van Dijk, Thaienne; de Almeida, Renato Paes; Amsler, Mario; Boldt, Justin; Freitas, Bernardo; Galeazzi, Cristiano; Huizinga, Richard; Ianniruberto, Marco; Ma, Hongbo; Nittrouer, Jeffrey A.; Oberg, Kevin; Orfeo, Oscar; Parsons, Dan; Szupiany, Ricardo; Wang, Ping; Zhang, Yuanfeng			Dunes in the world's big rivers are characterized by low-angle lee-side slopes and a complex shape	NATURE GEOSCIENCE			English	Article							STAGE PLANE BEDS; SEDIMENT TRANSPORT; SUBAQUEOUS DUNES; TURBULENCE STRUCTURE; AMAZON RIVER; RHINE RIVER; GRAVEL-BED; FLOW; DYNAMICS; SAND	Dunes in the world's big rivers are dominated by lee-side slopes with angles of less than 10 degrees, according to a bedform analysis of high-resolution bathymetric datasets. Dunes form critical agents of bedload transport in all of the world's big rivers, and constitute appreciable sources of bed roughness and flow resistance. Dunes also generate stratification that is the most common depositional feature of ancient riverine sediments. However, current models of dune dynamics and stratification are conditioned by bedform geometries observed in small rivers and laboratory experiments. For these dunes, the downstream lee-side is often assumed to be simple in shape and sloping at the angle of repose. Here we show, using a unique compilation of high-resolution bathymetry from a range of large rivers, that dunes are instead characterized predominantly by low-angle lee-side slopes (<10 degrees), complex lee-side shapes with the steepest portion near the base of the lee-side slope and a height that is often only 10% of the local flow depth. This radically different shape of river dunes demands that such geometries are incorporated into predictions of flow resistance, water levels and flood risk and calls for rethinking of dune scaling relationships when reconstructing palaeoflow depths and a fundamental reappraisal of the character, and origin, of low-angle cross-stratification within interpretations of ancient alluvial sediments.	[Cisneros, Julia; Best, Jim; van Dijk, Thaienne] Univ Illinois, Dept Geol, Urbana, IL 61801 USA; [Best, Jim] Univ Illinois, Dept Geog, Urbana, IL 61801 USA; [Best, Jim] Univ Illinois, Dept GIS, Urbana, IL 61801 USA; [Best, Jim] Univ Illinois, Dept Mech Sci & Engn, Urbana, IL 61801 USA; [Best, Jim] Univ Illinois, Ven Te Chow Hydrosyst Lab, Urbana, IL 61801 USA; [van Dijk, Thaienne] Deltares, Dept Appl Geol & Geophys, Utrecht, Netherlands; [de Almeida, Renato Paes; Galeazzi, Cristiano] Univ Sao Paulo, Inst Geociencias, Sao Paulo, Brazil; [de Almeida, Renato Paes] Univ Sao Paulo, Inst Energia & Ambiente, Sao Paulo, Brazil; [Amsler, Mario] Natl Sci & Tech Res Council, Inst Nacl Limnol, Santa Fe, Argentina; [Boldt, Justin] US Geol Survey, Ohio Kentucky Indiana Water Sci Ctr, Louisville, KY USA; [Freitas, Bernardo] Univ Estadual Campinas, Fac Tecnol, Limeira, Brazil; [Huizinga, Richard] US Geol Survey, Cent Midwest Water Sci Ctr, Rolla, MO USA; [Ianniruberto, Marco] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Ma, Hongbo; Nittrouer, Jeffrey A.] Rice Univ, Dept Earth Environm & Planetary Sci, Houston, TX USA; [Oberg, Kevin] US Geol Survey, Cent MidWest Water Sci Ctr, Urbana, IL USA; [Orfeo, Oscar] Natl Sci & Tech Res Council, Ctr Ecol Aplicada, Corrientes, Argentina; [Parsons, Dan] Univ Hull, Energy & Environm Inst, Kingston Upon Hull, N Humberside, England; [Szupiany, Ricardo] Univ Nacl Litoral, Fac Engn & Water Sci, Int Ctr Large Rivers Res, Santa Fe, Argentina; [Wang, Ping; Zhang, Yuanfeng] Yellow River Inst Hydraul Res, Zhengzhou, Peoples R China	University of Illinois System; University of Illinois Urbana-Champaign; University of Illinois System; University of Illinois Urbana-Champaign; University of Illinois System; University of Illinois Urbana-Champaign; University of Illinois System; University of Illinois Urbana-Champaign; University of Illinois System; University of Illinois Urbana-Champaign; Deltares; Universidade de Sao Paulo; Universidade de Sao Paulo; United States Department of the Interior; United States Geological Survey; Universidade Estadual de Campinas; United States Department of the Interior; United States Geological Survey; Universidade de Brasilia; Rice University; United States Department of the Interior; United States Geological Survey; University of Hull; National University of the Littoral; Yangtze River Water Resources Protection Bureau	Cisneros, J; Best, J (autor correspondente), Univ Illinois, Dept Geol, Urbana, IL 61801 USA.; Best, J (autor correspondente), Univ Illinois, Dept Geog, Urbana, IL 61801 USA.; Best, J (autor correspondente), Univ Illinois, Dept GIS, Urbana, IL 61801 USA.; Best, J (autor correspondente), Univ Illinois, Dept Mech Sci & Engn, Urbana, IL 61801 USA.; Best, J (autor correspondente), Univ Illinois, Ven Te Chow Hydrosyst Lab, Urbana, IL 61801 USA.	jcisnrs2@illinois.edu; jimbest@illinois.edu	Freitas, Bernardo T/B-1081-2015; Almeida, Renato/AAF-6705-2020; Galeazzi, Cristiano/AGX-8001-2022; Ianniruberto, Marco/W-9704-2018; Van Dijk, Thaienne/AAB-8899-2020; Almeida, Renato/G-2567-2013; Best, Jim/P-8440-2015	Freitas, Bernardo T/0000-0001-6239-0137; Ianniruberto, Marco/0000-0002-9056-9668; Van Dijk, Thaienne/0000-0003-1702-1142; Oberg, Kevin/0000-0002-7024-3361; Galeazzi, Cristiano/0000-0001-7285-2884; Huizinga, Richard/0000-0002-2940-2324; Almeida, Renato/0000-0003-3664-1558; Boldt, Justin/0000-0002-0771-3658; Cisneros, Julia/0000-0001-6451-4180; Best, Jim/0000-0001-5314-6140	National Science Foundation Graduate Research Fellowship (NSF GRF); National Science Foundation Graduate Research Fellowship [DGE-1746047]; Department of Geology, University of Illinois; National Natural Science Foundation of China [51379087]; Sao Paulo Research Foundation (FAPESP) [2014/16739-8, 2017/06874-3]; Jack and Richard C. Threet chair	National Science Foundation Graduate Research Fellowship (NSF GRF)(National Science Foundation (NSF)); National Science Foundation Graduate Research Fellowship(National Science Foundation (NSF)); Department of Geology, University of Illinois; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Jack and Richard C. Threet chair	J.C. is supported by a National Science Foundation Graduate Research Fellowship (NSF GRF). This material is based on work supported by the National Science Foundation Graduate Research Fellowship under grant no. DGE-1746047. J.C. is also supported by the Department of Geology, University of Illinois, and the Jack and Richard C. Threet chair to J.B. The Huang He (Yellow) River single-beam echosounder data acquisition was supported by the National Natural Science Foundation of China (grant no. 51379087), the Department of Geology, University of Illinois, and the Jack and Richard C. Threet chair to J.B. We also thank the Sao Paulo Research Foundation (FAPESP) for Research Grant nos. 2014/16739-8 and 2017/06874-3, supporting the acquisition of the Amazon River Multibeam Echo Sounder data. J.B. would like to acknowledge many discussions with R. Kostaschuk, who first highlighted the importance of low-angle alluvial dunes. Any opinion, findings, and conclusions or recommendations expressed in this material are those of the authors and do not necessarily reflect the views of the National Science Foundation.	Allan J. 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Geosci.	FEB	2020	13	2					156	+		10.1038/s41561-019-0511-7	http://dx.doi.org/10.1038/s41561-019-0511-7		JAN 2020	18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KT7SZ		Green Accepted			2023-06-23	WOS:000508323400002
J	Suzuki, KN; Castro, RJM; Sondermann, MN; Machado, EC; Bellido, AB; Lopes, RT; Machado, W				Suzuki, K. N.; Castro, R. J. M.; Sondermann, M. N.; Machado, E. C.; Bellido, A. B.; Lopes, R. T.; Machado, W.			Removal of Zn and Cd from Overlying Water by Mangrove Sediments: Testing the Effects of Sediment Resuspension/Redeposition Events	WATER AIR AND SOIL POLLUTION			English	Article						Trace metals; Radiotracers; Removal kinetics; Diffusion; Sediments	SUSPENDED PARTICULATE MATTER; UPTAKE KINETICS; TRACE-METALS; TIDAL WATER; RADIONUCLIDES; ENVIRONMENTS; DIFFUSION; ECOSYSTEM; ZINC; FLUX	Coastal sediment redeposition after resuspension events may change the sediment capacity to sequester pollutants after the formation of new sediment-water interfaces. To test this hypothesis, radiotracer experiments were performed to evaluate zinc (Zn-65) and cadmium (Cd-109) removal kinetics by redeposited mangrove sediments. After 24-h experiments, average inventories within redeposited sediments were close to those from control sediments (similar to 20% lower in redeposited sediments), while average decreases of 41% (Cd-109) and 27% (Zn-65) in the half-removal times (t(1/2)) from overlying water were promoted by redeposited sediments in comparison with control sediments. High variability in metal removal rates, however, implied in no statistically significant differences between t(1/2) values, suggesting a low influence of sediment redeposition on the metal removal capacity of mangrove sediments. More limited depth diffusion of metals was observed within redeposited sediments, always within the uppermost centimeter. Possible benefits to water quality by a slightly faster metal diffusion into redeposited sediments may be less effective due to this trend since the metal retention very close to the sediment top can facilitate new remobilization to the overlying water.	[Suzuki, K. N.; Castro, R. J. M.; Sondermann, M. N.; Bellido, A. B.; Machado, W.] Univ Fed Fluminense, Inst Quim, Programa Posgrad Geoquim, BR-24020007 Niteroi, RJ, Brazil; [Suzuki, K. N.; Lopes, R. T.] Univ Fed Rio de Janeiro, COPPE, Lab Instrumentacao Nucl, BR-21945970 Rio De Janeiro, RJ, Brazil; [Sondermann, M. N.] Univ Lisbon, Inst Ciencias Sociais, Programa Doutoral Alteracoes Climat & Polit Desen, P-1600189 Lisbon, Portugal; [Machado, E. C.] Inst Fed Educ Ciencia & Tecnol Rio de Janeiro, BR-26530060 Nilopolis, RJ, Brazil	Universidade Federal Fluminense; Universidade Federal do Rio de Janeiro; Institute of Social Sciences, University of Lisbon (ICS-UL); Universidade de Lisboa; Instituto Federal do Rio de Janeiro (IFRJ)	Suzuki, KN (autor correspondente), Univ Fed Rio de Janeiro, COPPE, Lab Instrumentacao Nucl, BR-21945970 Rio De Janeiro, RJ, Brazil.	norisuzuki@gmail.com	Machado, Wilson/P-8047-2019; Lopes, Ricardo/CAH-3736-2022; Sondermann, Melissa Nogueira/GXH-4490-2022; Suzuki, Katia N/L-2509-2018	Machado, Wilson/0000-0003-3117-8584; Suzuki, Katia N/0000-0002-8192-9000	Rio de Janeiro State Research Foundation (FAPERJ); FAPERJ; Brazilian Ministry of Education (CAPES); CAPES [001]	Rio de Janeiro State Research Foundation (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); FAPERJ(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Brazilian Ministry of Education (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The Rio de Janeiro State Research Foundation (FAPERJ) provided financial support to RTL. MNS thanks FAPERJ and KNS thanks the Brazilian Ministry of Education (CAPES) for their research grants, respectively. WM and AVB thank the financial support from CAPES (finance code 001).	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JAN 20	2020	231	2							42	10.1007/s11270-020-4417-1	http://dx.doi.org/10.1007/s11270-020-4417-1			7	Environmental Sciences; Meteorology & Atmospheric Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences; Water Resources	KM2AG					2023-06-23	WOS:000513922300001
J	Lima, EA; Cunha, FAS; Junior, MMS; Lyra, WS; Santos, JCC; Ferreira, SLC; Araujo, MCU; Almeida, LF				Lima, Eduardo A.; Cunha, Francisco A. S.; Junior, Mario M. S.; Lyra, Wellington S.; Santos, Josue C. C.; Ferreira, Sergio L. C.; Araujo, Mario C. U.; Almeida, Luciano F.			A fast and sensitive flow-batch method with hydride generating and atomic fluorescence spectrometric detection for automated inorganic antimony speciation in waters	TALANTA			English	Article						Inorganic antimony speciation; Flow-batch analysis; Hydride generation; Atomic fluorescence spectrometry; Water analysis	ENVIRONMENT; EXTRACTION; ANALYZER	In this paper, a flow-batch analysis (FBA) system, hydride generation (HG), and atomic fluorescence spectrometry (AFS) are coupled for the first time to develop a fast and sensitive FBA-HG-AFS method for automated inorganic antimony speciation in waters, whether from the sea, mineral water, tap water, or lakes. Unlike previous automated flow methods that use confluent fluids and complex devices, the main advantage of the proposed FBA-HG-AFS method is an innovative use of a simple laboratory made flow-batch chamber to simultaneously perform mixing, homogenization, reactions, antimony hydride formation, and gas-liquid separation. The FBA-HG-AFS method was optimized using two-level full factorial and Box-Behnken designs, and validated on the basis of real repeated measurements and analysis of variance, yielding a satisfactory working range (100-2000 ng L-1), precision (RSD = 4%), sensitivity, and limit of detection (6 ng L-1) for the water samples analyzed. Accuracy was evaluated by recovery tests and analysis of a standard reference material (SRM 1643e) of trace elements in water (NIST, USA), resulting in recovery rates of from 90 to 114%, and relative error = 0.7%. The high sampling throughput (54 speciations h(-1)), together with low waste generation, low costs, low reagent and sample consumption make this FBA-HG-AFS method an interesting proposal for fast large-scale analysis in routine laboratoy according to the principles of green analytical chemistry.	[Lima, Eduardo A.; Lyra, Wellington S.; Araujo, Mario C. U.; Almeida, Luciano F.] Univ Fed Paraiba, Dept Quim, POB 5093, BR-58051970 Joao Pessoa, PB, Brazil; [Cunha, Francisco A. S.; Santos, Josue C. C.] Univ Fed Alagoas, Inst Quim & Biotecnol, Campus AC Simoes, BR-57072900 Maceio, AL, Brazil; [Junior, Mario M. S.; Ferreira, Sergio L. C.] Univ Fed Bahia, Inst Quim, Campus Ondina, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Paraiba; Universidade Federal de Alagoas; Universidade Federal da Bahia	Almeida, LF (autor correspondente), POB 5093, BR-58051970 Joao Pessoa, PB, Brazil.	luciano@quimica.ufpb.br	FERREIRA, SERGIO LUIS SLCF COSTA/I-1993-2013; Lyra, Wellington/ABD-8383-2021; Araujo, Mario C.U./H-6553-2013; Cunha, Francisco/N-2493-2019; Santos, Josue C C/F-6497-2016; da Silva Cunha, Francisco Antonio/N-9401-2019	FERREIRA, SERGIO LUIS SLCF COSTA/0000-0001-7738-045X; Lyra, Wellington/0000-0002-3499-6163; Araujo, Mario C.U./0000-0002-7976-3494; Cunha, Francisco/0000-0002-1247-1008; Santos, Josue C C/0000-0002-9525-5123; Antonio De Lima, Eduardo/0000-0002-5020-7443	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]; CNPq	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) Finance Code 001, and partly by CNPq. We also acknowledge David Peter Harding from USA for reviewing and correcting the English of the manuscript.	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J	Miranda, IM; Toldo, EE; Klein, AHD; Strauss, D; da Silva, GV				Malheiros Miranda, Inaie; Toldo, Elirio Ernestino, Jr.; da Fontoura Klein, Antonio Henrique; Strauss, Darrell; Vieira da Silva, Guilherme			The role of cuspate spits on wave attenuation and energy redistribution in a coastal lagoon, Lagoa dos Patos, Brazil	GEO-MARINE LETTERS			English	Article							WIND-SEA; BEACHES; DISSIPATION; EVOLUTION; TRANSPORT; EROSION; REGIONS; GROWTH; MODEL	This research uses a process-based model (Delft3D), validated with measured wave data, to investigate the controls that a cuspate shoreline and its associated submerged morphology have on wave generation, propagation, and attenuation within a large elongated lagoon (Lagoa dos Patos, Brazil). A method based on the Energy-Flux-Method was applied to the historical wind dataset to define representative wind cases to be used as forcing conditions in the model. The results show that, during extreme wind conditions, the spits dissipate wave energy in the lagoon. This (wave attenuation and the wave sheltering effect) controls the stability of the adjacent coastline. The wave attenuation varies between 18% and 46% along the submerged spit depending on the crest width and the amplitude of the incident waves. Waves are mainly attenuated in the proximal and central portions of the spits where the spits are wider, resulting in a reduced transmitted energy to the adjacent coastline, while larger waves are also attenuated on the distal end of the spits. The degree of attenuation depends on the direction of wave generation, the respective fetch, the spit width, and the water depth. A strong relationship of mutual co-adjustment between the morphology and the wave field results in a very low occurrence of oblique wave angles of incidence, especially for waves propagating across the long lagoon axis. Furthermore, the wave attenuation over the spits is also responsible for its progressive erosion, which, from decades to centuries, may lead to an increase of changes on the lagoon shorelines.	[Malheiros Miranda, Inaie; Toldo, Elirio Ernestino, Jr.] Univ Fed Rio Grande Sul UFRGS, Programa Posgrad Geociencias, Campus Vale Agron, BR-91501970 Porto Alegre, RS, Brazil; [Malheiros Miranda, Inaie; da Fontoura Klein, Antonio Henrique] Univ Fed Santa Catarina UFSC, Lab Oceanog Costeira, Coordenadoria Especial Oceanog OCN, Ctr Ciencias Fis & Matemat CFM, Campus Univ Trindade, BR-88040900 Florianopolis, SC, Brazil; [Toldo, Elirio Ernestino, Jr.] Univ Fed Rio Grande Sul UFRGS, Ctr Estudos Geol & Costeira Oceanica, Inst Geociencias, Campus Vale Agron, BR-91501970 Porto Alegre, RS, Brazil; [Strauss, Darrell; Vieira da Silva, Guilherme] Griffith Univ, Griffith Ctr Coastal Management, Room 2-01,Bldg G51, Gold Coast, Qld 4222, Australia	Universidade Federal do Rio Grande do Sul; Universidade Federal de Santa Catarina (UFSC); Universidade Federal do Rio Grande do Sul; Griffith University	Miranda, IM (autor correspondente), Univ Fed Rio Grande Sul UFRGS, Programa Posgrad Geociencias, Campus Vale Agron, BR-91501970 Porto Alegre, RS, Brazil.; Miranda, IM (autor correspondente), Univ Fed Santa Catarina UFSC, Lab Oceanog Costeira, Coordenadoria Especial Oceanog OCN, Ctr Ciencias Fis & Matemat CFM, Campus Univ Trindade, BR-88040900 Florianopolis, SC, Brazil.	miranda.inaie@gmail.com	Toldo, Elírio E/F-6382-2012; da Silva, Guilherme Vieira/AAJ-1699-2020; Strauss, Darrell/D-6489-2013	Toldo, Elírio E/0000-0002-5609-4339; da Silva, Guilherme Vieira/0000-0002-1109-0246; Strauss, Darrell/0000-0002-3411-0991; Malheiros Miranda, Inaie/0000-0003-1532-3630	CAPES; CNPQ [301597/2018-9]	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPQ(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors would like to acknowledge reviewers, especially reviewer 2, for their helpful comments which have greatly contributed to improving the paper. We also acknowledge PFRH-Petrobras program no. PB-215, for the student grant provided to the full-engagement development of the first author's Ph.D. thesis, and the research agency CAPES for funding an almost 1-year internship at the Griffith Centre for Coastal Management (GCCM), Griffith University (AU), which resulted in the present work. Productivity scholarship 1D CNPQ 301597/2018-9. The first author would also like to thank the GCCM Team for the good opportunity of working together, for their nice reception, willingness to share knowledge, and patience during the learning process. We also thank Rede Ondas Project (https://redeondas.furg.br/pt/), an initiative from the Intergovernmental Oceanographic Commission of UNESCO, coordinated by the Federal University of Rio Grande (FURG-Brazil) for providing the measured wave data (Datawell Waverider-Mark III) for the model validation.	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DEC	2020	40	6			SI		1069	1086		10.1007/s00367-019-00632-9	http://dx.doi.org/10.1007/s00367-019-00632-9		JAN 2020	18	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	OV2PV		Green Submitted			2023-06-23	WOS:000574069600001
J	Ivanoff, MD; Toldo , EE; Figueira, RCL; Ferreira, PAD				Ivanoff, Michel Doeppre; Toldo Jr, Elirio Ernestino; Lopes Figueira, Rubens Cesar; de Lima Ferreira, Paulo Alves			Use of Pb-210 and Cs-137 in the assessment of recent sedimentation in Patos Lagoon, southern Brazil	GEO-MARINE LETTERS			English	Article							EL-NINO; BAY	In this study, the sedimentation conditions of Lagoa dos Patos, southern Brazil, were analyzed by applying Pb-210 and Cs-137 geochronological methods on four geological cores. The sedimentation rates showed a decreasing north-to-south pattern, indicating a strong influence of the Guaiba River discharge (the main Patos Lagoon tributary) on the transport of sediments into the interior of the lagoon. Core PT02 (north) had the highest sedimentation rate (of the order of 7.0 mm year(-1)), while the central and central-southern drilling sites (PT04 and PT07) presented roughly lower values that corresponded to rates of 5.5 and 4.4 mm year(-1), respectively. This decreasing trend was reversed at the southernmost site (PT08), which showed a 4.8 mm year(-1) rate due to the joint influence of the Camaqua River and Sao Goncalo Channel discharges, combined with higher flocculation associated with the site's proximity to the estuary. Significant interannual oscillations of the sedimentation rates were observed when the CRS model was applied to the Pb-210 data. In general, the rates were higher in periods of higher precipitation, whereas the opposite took place in drier periods. The correlation between these anomalies and El Nino-Southern Oscillation (ENSO) events was identified. During El Nino years, the sedimentation rates increased by 135% in the northern sector (PT02); in the central and central-southern sectors, the rates increased by 164% (PT04) and 170% (PT07), respectively, while there was an increase of 262% to the south of the lagoon as observed at site PT08.	[Ivanoff, Michel Doeppre; Toldo Jr, Elirio Ernestino] Univ Fed Rio Grande do Sul, Inst Geociencias, Ctr Estudos Geol Costeira & Ocean, Ave Bento Goncalves 9-500, BR-91509900 Porto Alegre, RS, Brazil; [Lopes Figueira, Rubens Cesar; de Lima Ferreira, Paulo Alves] Univ Sao Paulo, Dept Oceanog Fis Quim & Geol, Praca Oceanog 191,Cidade Univ, BR-05508120 Sao Paulo, SP, Brazil	Universidade Federal do Rio Grande do Sul; Universidade de Sao Paulo	Ivanoff, MD (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ctr Estudos Geol Costeira & Ocean, Ave Bento Goncalves 9-500, BR-91509900 Porto Alegre, RS, Brazil.	mdi.ivanoff@gmail.com; toldo@ufrgs.br; rfigueira@usp.br; paulo.alves.ferreira@hotmail.com	Toldo, Elírio E/F-6382-2012; Ferreira, Paulo/H-3654-2012	Toldo, Elírio E/0000-0002-5609-4339; Ferreira, Paulo/0000-0001-9723-3166; Ivanoff, Michel/0000-0001-6421-7346				Ajayi IR, 2010, INT J PHYS SCI, V5, P154; Andrade MM, 2018, BRAZ J OCEANOGR, V66, DOI [10.1590/S1679-87592018017406603, 10.1590/s1679-87592018017406603]; APPLEBY PG, 2001, TRACKING ENV CHANGE, P171, DOI DOI 10.1007/0-306-47669-X_9; Baisch P., 1994, THESIS; Baitelli R, 2012, THESIS; Cooper JAG, 2012, OCEAN COAST MANAGE, V64, P1, DOI 10.1016/j.ocecoaman.2012.04.001; DILLENBURG SR, 1995, 5 C ASS BRAS EST QUA, P224; EMATER-RS/ASCAR, 2014, VAL PROD AGR PRINC G; FARSUL, 2013, BAL AGR 2013 PERSP 2; Gibbons SJA, 2006, GLOBAL ENVIRON CHANG, V16, P40, DOI 10.1016/j.gloenvcha.2005.10.002; Grimm AM, 1998, J CLIMATE, V11, P2863, DOI 10.1175/1520-0442(1998)011<2863:PAISBA>2.0.CO;2; Gruber NLS., 2006, PESQUISAS GEOCIENCIA, V33, P79, DOI [10.22456/1807-9806.19516, DOI 10.22456/1807-9806.19516]; Hartmann C., 1991, RS REV BRAS GEOCIENC, V21, P371, DOI [10.25249/0375-7536.1991371377, DOI 10.25249/0375-7536.1991371377]; IVANOFF MD, 2017, PESQUI GEOCIENC, V44, P489; Jung B.M., 2017, THESIS; Kathren R.R., 1984, RADIOACTIVITY ENV SO; Kjerfve B, 1997, CONT SHELF RES, V17, P1609, DOI 10.1016/S0278-4343(97)00028-9; KJERFVE B, 1989, MAR GEOL, V88, P187, DOI 10.1016/0025-3227(89)90097-2; Kjerfve B., 1986, COMP OCEANOGRAPHY CO; Krepper CM, 2003, INT J CLIMATOL, V23, P103, DOI 10.1002/joc.853; Ligero RA, 2005, J ENVIRON RADIOACTIV, V80, P87, DOI 10.1016/j.jenvrad.2004.06.006; Lubis AA, 2006, 210 PB J COAST DEV, V10, P9; Marques WC, 2010, J GEOPHYS RES, V115, P10; Martin L, 1994, COASTAL LAGOON PROCE, P41, DOI DOI 10.1016/S0422-9894(08)70008-4; Martins I.R., 1989, PESQUISAS, V22, P5; Moller O. 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E., 2006, REV ATLANTICA, V28, P87, DOI DOI 10.5088/atlantica.v28i2.790; Tomazelli L.J., 2000, REV BRASILEIRA GEOCI, V30, P474, DOI DOI 10.25249/0375-7536.2000303474476; Torres RJ, 2000, THESIS; United Nations Scientific Committee on the Effect of Atomic Radiation, 2008, GEN ASS SCI ANN; Vaz A.C., 2006, ATLANTICA, V28, P13, DOI DOI 10.5088/atlantica.v28i1.1724; Vieira E.F., 1988, PLANICIE COSTEIRA RI; Villwock JA, 1972, ESTUD SEDIMENTOL, V2, P13	46	15	15	1	7	SPRINGER	NEW YORK	ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES	0276-0460	1432-1157		GEO-MAR LETT	Geo-Mar. Lett.	DEC	2020	40	6			SI		1057	1067		10.1007/s00367-019-00633-8	http://dx.doi.org/10.1007/s00367-019-00633-8		JAN 2020	11	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	OV2PV					2023-06-23	WOS:000505433200001
J	Pinheiro, SMM; de Almeida, M; Oliveira, OMC; Moreira, ITA				Pinheiro, Samires Moura Malaquias; de Almeida, Marcos; Oliveira, Olivia Maria Cordeiro; Moreira, Icaro Thiago Andrade			Formation of OSA and dispersion of polycyclic aromatic hydrocarbons in a tropical estuary as a tool in the prevention of environmental impacts: influence of the biogeochemical characteristics of the estuary	ENVIRONMENTAL MONITORING AND ASSESSMENT			English	Article						Oil; Oil-suspended particulate material aggregates (OSAs); Ecotoxicological impacts; Todos os Santos Bay	SUSPENDED PARTICULATE MATTER; SANTOS BAY; PETROLEUM-HYDROCARBONS; CRUDE-OIL; SEDIMENTS; FATE; SALINITY; WATER; RIVER; BRAZIL	The formation of an oil-suspended particulate material aggregate (OSA) is one of the weathering processes that occur after the spill of oil in marine environments, responsible for the dispersion of hydrocarbons. Oil and particle aggregates are formed from the interaction between small oil droplets and suspended particulate matter (SPM). In general, SPM are fine particles which may be inorganic minerals or organic particles in the water column. OSAs provide vertical dispersion of oil along the water column depending on the acquired density (buoyancy), and may remain near the surface, water column, or bottom of water bodies. The present study examines the formation of these aggregates through the laboratory simulation of an oil spill in the waters of the Sao Paulo river estuary. The main objective was to investigate the dispersion of polycyclic aromatic hydrocarbons (PAHs), verifying which estuary characteristics most influenced the formation of OSAs and in addition to determine the regions of probable ecotoxicological impact due to the negative buoyancy of the formed aggregate. The results show that there was greater dispersion to the water column, mainly of lighter PAHs, ranging from 85,804.05 ng g(-1) (P11C) to 566,989.84 ng g(-1) (P17C). The percentage of dispersed PAH concentration per experimental unit ranged from 9.90% in unit P2 to 75.27% in unit P18. The formation of OSAs was influenced mainly by salinity and chlorophyll a. As the most vulnerable regions, the impacts are one mouth (P2 and P4), one central region (P7, P8, and P10), and one source (P18).	[Pinheiro, Samires Moura Malaquias; de Almeida, Marcos; Oliveira, Olivia Maria Cordeiro; Moreira, Icaro Thiago Andrade] Univ Fed Bahia, Lepetro Pospetro Inst Geosciences, Rua Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil; [Moreira, Icaro Thiago Andrade] Univ Fed Bahia, Polytech Sch, Dept Environm & Sanit Engn, Rua Prof Aristides Novis 2, BR-40210630 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia	Pinheiro, SMM (autor correspondente), Univ Fed Bahia, Lepetro Pospetro Inst Geosciences, Rua Barao de Jeremoabo S-N, BR-40170290 Salvador, BA, Brazil.	samires.moura7@gmail.com; marcosalmeida.mda@hotmail.com; olivia@ufba.br; icarotam@gmail.com	MOREIRA, ICARO/AAV-6503-2020; Moreira, Icaro/J-2040-2015; de Oliveira, Olivia Maria Cordeiro/AAB-3246-2021	MOREIRA, ICARO/0000-0002-3964-7368; Pinheiro, Samires/0000-0002-7044-0488; de Almeida, Marcos/0000-0002-9633-1386	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [4026663/2013-6, 30/2013]; Fundacao de Amparo a Pesquisa do Estado da Bahia [BOL0825/2017]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado da Bahia	This study was funded in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior-Brasil (CAPES)-finace cod 001 and by the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico in the project "Desenvolvimento de Multibioprocesso de Remediacao Aplicavel em areas Costeiras Impactadas por Atividades Petroliferas-DEMBPETRO" - Processo 4026663/2013-6, no ambito da CHAMADA MCTI/CNPq/CT-BIOTEC No. 30/2013, with laboratory support from the Centro de Excelencia em Geoquimica (Lepetro) at the Instituto de Geociencias (IGEO) of the Universidade Federal da Bahia (UFBA), developed at the Programa de Pos Graduacao em Petroleo e Meio Ambiente (POSPETRO). The author Samires Pinheiro received a scholarship grant from the Fundacao de Amparo a Pesquisa do Estado da Bahia (BOL0825/2017).	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J	Nagai, RH; Chiessi, CM; Kuhnert, H; Sousa, SHM; Wainer, IEKC; Figueira, RCL; Mahiques, MM				Nagai, Renata H.; Chiessi, Cristiano M.; Kuhnert, Henning; Sousa, Silvia H. M.; Wainer, Ilana E. K. C.; Figueira, Rubens C. L.; Mahiques, Michel M.			South Brazilian Bight mid- to late Holocene hydrographic fluctuations	GEO-MARINE LETTERS			English	Article							BOUNDARY UPWELLING SYSTEM; PLANKTONIC-FORAMINIFERA; CABO FRIO; ISOTOPIC COMPOSITION; CLEANING PROCEDURES; PLATA PLUME; ATLANTIC; SHELF; VARIABILITY; CLIMATE	Here, we present two high temporal resolution Holocene sea surface temperature (SST) and salinity (SSS) reconstructions for the SW Atlantic. Mg/Ca data together with the oxygen isotopic composition (delta O-18) of a shallow dwelling planktonic foraminifera species (Globigerinoides ruber(pink)). Two marine sediment cores collected at similar to 25 degrees S are used to assess mid- to late Holocene sea surface hydrographic conditions in the continental shelf of the South Brazilian Bight. Our results show multi-centennial-scale changes of up to 2.7 degrees C in SST and 0.8 parts per thousand in ice volume corrected seawater delta O-18 (a proxy for SSS, indicating changes of up to 2 salinity units). In phase, multicentennial-scale negative SST and SSS incursions were interpreted to indicate shelf-break upwelling events and the northward intrusion of the Plata Plume Water (PPW) under a strengthened Brazil Current (BC) flow. The latitudinal SST gradient between our two records (Delta SST7616-7610), applied here as a proxy for the BC strength, supports the existing hypothesis of antiphase between the BC and the North Brazil Current strength during the last 7 ka. Positive Delta SST(7616-7610)values suggest the presence of the PPW at latitudes of up to 25.5 degrees S, while negative Delta SST(7616-7610)values (centred at around 5.4, 4.3, 2.2 and 1.3 cal ka BP) occurring synchronously with cold events in the Northern Hemisphere suggests that the Atlantic Meridional Overturning Circulation played a central role in the SW Atlantic mid- to late Holocene surface hydrographic conditions.	[Nagai, Renata H.] Univ Fed Parana, Ctr Estudos Mar, Ave Beira Mar S-N, BR-83255976 Pontal Do Parana, PR, Brazil; [Chiessi, Cristiano M.] Univ Sao Paulo, Escola Artes Ciencias & Humanidade, Sao Paulo, Brazil; [Kuhnert, Henning] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Sousa, Silvia H. M.; Wainer, Ilana E. K. C.; Figueira, Rubens C. L.; Mahiques, Michel M.] Univ Sao Paulo, Inst Oceanog, Sao Paulo, Brazil; [Mahiques, Michel M.] Univ Sao Paulo, Inst Energia & Ambiente, Sao Paulo, Brazil	Universidade Federal do Parana; Universidade de Sao Paulo; University of Bremen; Universidade de Sao Paulo; Universidade de Sao Paulo	Nagai, RH (autor correspondente), Univ Fed Parana, Ctr Estudos Mar, Ave Beira Mar S-N, BR-83255976 Pontal Do Parana, PR, Brazil.	renatanagai@ufpr.br	Wainer, Ilana/B-4540-2011; Figueira, Rubens/AAC-1045-2022; Mahiques, Michel/D-1526-2010; Chiessi, Cristiano Mazur/E-1916-2012; de Mello e Sousa, Silvia Helena/ABH-5834-2020; Nagai, Renata Hanae/N-6643-2019	Wainer, Ilana/0000-0003-3784-623X; Figueira, Rubens/0000-0001-8945-4540; Mahiques, Michel/0000-0002-5249-5610; Chiessi, Cristiano Mazur/0000-0003-3318-8022; Nagai, Renata Hanae/0000-0002-1358-5074; Mello e Sousa, Silvia Helena/0000-0002-8860-9042; Kuhnert, Henning/0000-0001-5242-4495	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP) [2009/01594-6, 2010/09983-9, 2012/17517-3]	Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The authors want to acknowledge Dr. Stefan Mulitza for his collaboration in data acquisition and discussion. The authors also wish to thank Dr. Marcelo Rodrigues, Dr. Samara Cazzoli Y Goya, Mr. Clodoaldo Vieira Tolentino andMr. Edilson Faria for their help in sediment sampling. Thanks are due also to the crew of the R.V. `Prof. W. Besnard'. This work has been financially supported by Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP Proc. No. 2009/01594-6, 2010/09983-9 and 2012/17517-3).	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Lett.	DEC	2020	40	6			SI		1045	1055		10.1007/s00367-019-00616-9	http://dx.doi.org/10.1007/s00367-019-00616-9		JAN 2020	11	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	OV2PV					2023-06-23	WOS:000574069700001
J	Aguilera, O; de Araujo, OMO; Hendy, A; Nogueira, AAE; Nogueira, ACR; Maurity, CW; Kutter, VT; Martins, MVA; Coletti, G; Dias, BB; da Silva-Caminha, SAF; Jaramillo, C; Bencomo, K; Lopes, RT				Aguilera, Orangel; Oliveira de Araujo, Olga M.; Hendy, Austin; Nogueira, Anna A. E.; Nogueira, Afonso C. R.; Maurity, Clovis Wagner; Kutter, Vinicius Tavares; Alves Martins, Maria Virginia; Coletti, Giovanni; Dias, Bruna Borba; da Silva-Caminha, Silane A. F.; Jaramillo, Carlos; Bencomo, Karen; Lopes, Ricardo Tadeu			Palaeontological framework from Pirabas Formation (North Brazil) used as potential model for equatorial carbonate platform	MARINE MICROPALEONTOLOGY			English	Article						Marine Fossil; Western Atlantic; Miocene; Carbonate Platform; Micro CT	OLIGOCENE-MIOCENE TRANSITION; GREAT-BARRIER-REEF; SEA-LEVEL; BENTHIC FORAMINIFERA; ZAGROS BASIN; PALEOENVIRONMENTAL RECONSTRUCTION; CORALLINE ALGAE; FACIES ANALYSIS; MIDDLE MIOCENE; PARA STATE	The Pirabas Formation (early to middle Miocene) from the equatorial margin of North Brazil is characterized by a shallow-marine carbonate platform with high fossil diversity and abundant micro- and macrofossil remains. The Pirabas Formation represents a unique carbonate system along the Atlantic margin of South America that developed before the onset of the Amazon delta. We studied the palaeontology and lithofacies of outcrops of the uppermost Pirabas Formation and found that was deposited in a coastal marine environment with marginal lagoons under the influence of a tidal regime and tropical storms. The remains of calcareous algae, molluscs, crustaceans, echinoiderms, bryozoans, solitary corals, fish and marine mammals, together with foraminifera, ostracods and other marine microfossils, shaped a biogenic framework, that together with the post-depositional processes of dissolution of skeletal grains, is responsible for the mean packstone-floatstone porosity of 14.9%. The palaeontological framework and the petrophysical characterization of the carbonate rocks from the uppermost Pirabas Formation outcrop represent a baseline to interpret the entire Pirabas Formation in the subsurface stratigraphic sections (cores) of this important Neogene unit. Considering that carbonate rocks account for similar to 50% of oil and gas reservoirs around the world, this research provides a model for Neogene tropical carbonate deposits useful for carbonate petroliferous reservoirs in the Brazilian equatorial basins.	[Aguilera, Orangel; Dias, Bruna Borba; Bencomo, Karen] Fluminense Fed Univ UFF, Paleoecol & Global Changes Lab, Campus Gragoata,Bloco M,110, BR-24210200 Niteroi, RJ, Brazil; [Oliveira de Araujo, Olga M.; Lopes, Ricardo Tadeu] Fed Univ Rio de Janeiro UFRJ, Nucl Instrumentat Lab, Nucl Engn Program COPPE, Av Horacio Macedo,Cidade Univ, BR-21941450 Rio De Janeiro, Brazil; [Hendy, Austin] Nat Hist Museum Los Angeles Cty, 900 Exposit Blvd, Los Angeles, CA USA; [Nogueira, Anna A. E.; Nogueira, Afonso C. R.; Maurity, Clovis Wagner; Kutter, Vinicius Tavares] Fed Univ UFPA, Geosci Inst, Belem, Para, Brazil; [Alves Martins, Maria Virginia] Rio de Janeiro State Univ UERJ, R Sao Francisco Xavier,524 Lab 1006, BR-20550900 Maracana, RJ, Brazil; [Alves Martins, Maria Virginia] Aveiro Univ, Dept Geoscienses, GeoBioTec, Campus Santiago, P-3810197 Aveiro, Portugal; [Coletti, Giovanni] Univ Milano Bicocca, Dept Environm Sci & Earth Sci, Piazza Sci 4, I-20126 Milan, Italy; [da Silva-Caminha, Silane A. F.] Fed Univ Mato Grosso UFMT, Paleontol & Palynol Lab, Cuiaba, Mato Grosso, Brazil; [Jaramillo, Carlos] Smithsonian Trop Res Inst, Balboa, Ancon, Panama; [Jaramillo, Carlos] Univ Montpellier, CNRS, EPHE, ISEM,IRD, Montpellier, France	Universidade Federal Fluminense; Universidade Federal do Para; Universidade do Estado do Rio de Janeiro; Universidade de Aveiro; University of Milano-Bicocca; Universidade Federal de Mato Grosso; Universidade Federal de Mato Grosso do Sul; Smithsonian Institution; Smithsonian Tropical Research Institute; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; UDICE-French Research Universities; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE)	Aguilera, O (autor correspondente), Fluminense Fed Univ UFF, Paleoecol & Global Changes Lab, Campus Gragoata,Bloco M,110, BR-24210200 Niteroi, RJ, Brazil.	orangelaguilera@id.uff.br; ahendy@nhm.org; anogueira@ufpa.br; viniciuskutter@id.uff.br; virginia.martins@ua.pt; giovanni.coletti@unimib.it; brunaborbadias@id.uff.br; JaramilloC@si.edu; ricardo@lin.ufrj.br	Dias, Bruna Borba/AAV-4379-2020; da Silva Caminha, Silane Aparecida Ferreira/M-6972-2016; Aguilera, Orangel/D-5055-2013; Lopes, Ricardo/CAH-3736-2022; Alves Martins, Maria Virginia Virginia/O-2893-2013; Martins, Maria/IQT-0561-2023	Dias, Bruna Borba/0000-0001-5518-2807; da Silva Caminha, Silane Aparecida Ferreira/0000-0003-4853-2789; Alves Martins, Maria Virginia Virginia/0000-0001-8348-8862; NOGUEIRA, AFONSO/0000-0002-5225-9255; Segueri, Karen/0000-0002-8861-9662; Araujo, Olga/0000-0002-6287-0592	Brazilian Council of Science and Technological Development -CNPq [404937/2018-7, 305269/2017-8]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) (grant PBMAC-UFF) [001]	Brazilian Council of Science and Technological Development -CNPq; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) (grant PBMAC-UFF)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors would like to thank the National Mining Agency of Brazil (ANM) for authorization to collect samples at the Pirabas Formation in the Atalaia outcrop (COPAL Protocol number 043/2018 to OA). Many thanks to Stephen Cairns and Felix Rodriguez from the Smithsonian and Kamil Zagoegek from the Brno University of Technology of Czech Republic, for collaboration in the preliminary identification of corals and bryozoans (respectively). The authors are grateful to the participants in the PPGG-UFPA Paleontology postgraduate course 2018 for support this research during field trip and with laboratorial procedures. Thanks to Joelma Lobo (UFPA), Mauro Geraldes and Marcu Helenio (UERJ) by help us with the preparation of petrographic thin sections and SEM image respectively. Many thanks to Ismar Carvalho, Leonardo Borghi and Luis Fernando da Silva from the Federal University of Rio de Janeiro (UFRJ) by the access to the Laboratory of Sedimentary Geology to use the Petrographic Microscope. Flavia Figueiredo and Rafael da Silva collaborated with the access to the paleontological collections in the UFRJ and CPRM repository, respectively. Many thank to Daniel Lima from the Federal Fluminense University and to Christiano Ng from the CENPES-PETROBRAS for reviews the manuscript. The authors are grateful to Xavier Crosta (Associated Editor of Marine Micropaleontology) and anonymous reviewers for the comments, suggestions and corrections to improve the final manuscript. This study was funded by the Brazilian Council of Science and Technological Development -CNPq (grant 404937/2018-7 and productivity researches 305269/2017-8 to OA), and Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) (grant PBMAC-UFF, finance code 001 to KB).	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Micropaleontol.	JAN	2020	154								101813	10.1016/j.marmicro.2019.101813	http://dx.doi.org/10.1016/j.marmicro.2019.101813			23	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	KO0CZ		Bronze			2023-06-23	WOS:000515215200004
J	Amaral, L; Caxito, FD; Pedrosa-Soares, AC; Queiroga, G; Babinski, M; Trindade, R; Lana, C; Chemale, F				Amaral, Leandro; Caxito, Fabricio de Andrade; Pedrosa-Soares, Antonio Carlos; Queiroga, Glaucia; Babinski, Marly; Trindade, Ricardo; Lana, Cristiano; Chemale, Farid			The Ribeirao da Folha ophiolite-bearing accretionary wedge (Aracuai orogen, SE Brazil): New data for Cryogenian plagiogranite and metasedimentary rocks	PRECAMBRIAN RESEARCH			English	Article						U-Pb (LA-ICPMS, SHRIMP); Hf isotopes; Neoproterozoic ocean; Aracuat - West Congo orogen; Gondwana assembly	SAO-FRANCISCO CRATON; NEOPROTEROZOIC MACAUBAS GROUP; WEST-CONGO OROGEN; U-PB ZIRCON; DETRITAL ZIRCON; EASTERN BRAZIL; NE BRAZIL; SM-ND; ESPINHACO SUPERGROUP; GRANITIC MAGMATISM	The Aracuai orogen and West Congo belt make up a singular confined orogenic system, embraced by the San Francisco - Congo craton: the AWCO. It includes a southern sector with ophiolite bodies and magmatic arc, and a northern sector free of them, suggesting the precursor basin was an embayment partially floored by oceanic crust. The northernmost ophiolitic rock-assemblage found in the Aracuai orogen comprises metamafic and meta-ultramafic rocks with signatures of ocean-floor magmas, and associated pelagic to oceanic metasedimentary rocks of the Ribeirao da Folha Formation. Although tectonically dismembered and metamorphosed, those rocks resemble the classical ophiolite pseudostratigraphy. The Ribeirao da Folha Formation comprises rocks expected to be found in the upper units of an ophiolite edifice, like Al-rich micaschist (pelagic pelite), graphite-rich schist (black shale), sulfide-bearing metachert, diopsidite with massive sulfide, and banded iron formations (chemical-exhalative sediments), and sulfide-bearing fine-grained ortho-amphibolite with thin metachert intercalations (mafic volcanic unit). That formation hosts tectonic slices of banded ortho-amphibolite (dolerite) with plagiogranite veins, and coarse-grained massive ortho-amphibolite (gabbro), representing dismembered slivers from deeper mafic units, and slices of metaultramafic rocks from the deepest ophiolite units. Zircon crystals from a plagiogranite vein yielded the U-Pb SHRIMP age of 645 +/- 10 Ma, providing a new time constraint for ocean-floor emplacement, Micaschist samples show chemical attributes typical of distal passive margin pelites. Among three progressive deformation phases, the main ductile phase (D-n) shows kinematic indicators related to top to SW mass transport, associated with intermediate P-T (St, Ky, Sil) metamorphic zoning. Although the few youngest grains of detrital zircon from three siliciclastic samples have distinct ages (around 599 Ma, 741 Ma, and 816 Ma), their wide-range age spectra and Hf signatures suggest similar sediment sources. The wide lithological variety and stratigraphic complexity along with the intricate tectonic framework of the Ribeirao da Folha region, comprising thrust slices of ophiolitic rocks tectonically interleaved with older rift-related rocks, characterize an accretionary wedge that was scrapped off the subducted slab and involved in collisional tectonics, marking the AWCO suture zone for some 250 km between the Guanhaes basement block (lower plate) and Rio Doce magmatic arc (upper plate).	[Amaral, Leandro; Caxito, Fabricio de Andrade; Pedrosa-Soares, Antonio Carlos] Univ Fed Minas Gerais, CPMTC IGC UFMG, Programa Posgrad Geol, Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil; [Babinski, Marly; Trindade, Ricardo] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05580080 Sao Paulo, SP, Brazil; [Queiroga, Glaucia; Lana, Cristiano] Univ Fed Ouro Preto, Dept Geol, Escola Minas, BR-35400000 Morro Do Cruzeiro, MG, Brazil; [Chemale, Farid] Univ Vale Rio dos Sinos, Escola Politecn, BR-93022750 Sao Leopoldo, RS, Brazil; [Caxito, Fabricio de Andrade; Pedrosa-Soares, Antonio Carlos; Queiroga, Glaucia; Babinski, Marly; Trindade, Ricardo; Lana, Cristiano; Chemale, Farid] Brazilian Sci Council CNPq, Brasilia, DF, Brazil	Universidade Federal de Minas Gerais; Universidade de Sao Paulo; Universidade Federal de Ouro Preto; Universidade do Vale do Rio dos Sinos (Unisinos)	Amaral, L (autor correspondente), Univ Fed Minas Gerais, CPMTC IGC UFMG, Programa Posgrad Geol, Av Antonio Carlos 6627, BR-31270901 Belo Horizonte, MG, Brazil.	leandrosamaral@outlook.com; caxito@ufmg.br; pedrosasoares@gmail.com; glauciaqueiroga@yahoo.com.br; babinski@usp.br; ritrindad@gmail.com; cristianodeclana@gmail.com; faridcj@unisinos.br	Babinski, Marly/B-9403-2013; Trindade, Ricardo IF/A-8146-2008; Caxito, Fabricio A/J-1317-2016; Amaral, Leandro/A-6570-2019; Queiroga, Gláucia/AAJ-1823-2021; LANA, CRISTIANO/AAI-4176-2020	Babinski, Marly/0000-0003-2444-2404; Trindade, Ricardo IF/0000-0001-9848-9550; Caxito, Fabricio A/0000-0002-0335-3667; Amaral, Leandro/0000-0002-8144-3705; Queiroga, Gláucia/0000-0002-1730-0638; 	CNPq - Brazilian Research Council [446483/2014-1]; FAPESP - Sao Paulo Research Foundation [2016/06114-6]; Geotectonic Research Group of the CPMTC Research Center of the Federal University of Minas Gerais, Brazil; CNPq	CNPq - Brazilian Research Council(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESP - Sao Paulo Research Foundation(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Geotectonic Research Group of the CPMTC Research Center of the Federal University of Minas Gerais, Brazil; CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work was supported by funds from CNPq - Brazilian Research Council (grant 446483/2014-1), FAPESP - Sao Paulo Research Foundation (grant 2016/06114-6), and Geotectonic Research Group of the CPMTC Research Center of the Federal University of Minas Gerais, Brazil. Co-authors also thank the CNPq for their research productivity grants. We thank the staffs of the John de Laeter Centre, Curtin University, Perth, Western Australia, enabled by NCRIS via AuScope and the Laboratory of Isotope Geochemistry of Federal University of Ouro Preto, Brazil, and Bruno Arruda for field support. Our gratitude to Lauro Montefalco Santos and an anonymous reviewer for comments and suggestions that greatly have helped us to improve the first version of the paper, and Wilson Teixeira for editorial handling. The paper is a late tribute to Professor Hazel Prichardm for her great help in finding plagiogranite veins and better understanding the Ribeirao da Folha ophiolite.	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JAN	2020	336								105522	10.1016/j.precamres.2019.105522	http://dx.doi.org/10.1016/j.precamres.2019.105522			24	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KE7RK					2023-06-23	WOS:000508748600016
J	de Amorim, JVA; Ribeiro, VB; Guimaraes, ID; Farias, DJS; de Lima, JV; da Silva, AF				Antunes de Amorim, Jose Victor; Ribeiro, Vanessa Biondo; Guimaraes, Ignez de Pinho; Silva Farias, Douglas Jose; de Lima, Jefferson Valdemiro; da Silva Filho, Adejardo Francisco			Using airborne gamma-ray spectrometry and geochemistry to characterize the late Neoproterozoic ferroan magmatism in the Transversal subprovince of the Borborema Province, NE-Brazil	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						granitoids; ferroan; gamma-ray spectrometry; Borborema province; Geochemistry	A-TYPE GRANITOIDS; ALTO MOXOTO; PALEOPROTEROZOIC ACCRETIONARY; NORTHEASTERN BRAZIL; CENTRAL DOMAIN; TRACE-ELEMENT; ROCKS; BELT; CONSTRAINTS; ZONE	Ferroan granites (585-530 Ma) in the Transversal subprovince of the Borborema Province (BP) comprise two groups: G1) slightly peraluminous to metaluminous, alkali-calcic rocks (Aroeiras Complex and Serra Branca - Coxixola dike swarms (SBCDS)); G2) metaluminous to slightly peraluminous, alkalic to alkali-calcic rocks (Queimadas and Prata intrusions). G1 are transitional from collision to transcurrence (ca. 585 Ma), or transcurrence to transtension (ca. 545 Ma). G2 represents the granitoids intruded during post-collisional crustal thinning (ca. 550 Ma), or coeval with deposition of intracratonic basins (ca. 530 Ma). The large-ion lithophile elements (LILE) and high field strength elements (HFSE) enriched geochemical signature of these granitoids are recognizable in gamma spectrometric maps of regional scale, highest values of K(%), eTh(ppm), and eU(ppm) contrast significantly with country rocks and magnesian granites. This study shows that gamma-ray spectrometric regional maps reflect the geochemical characteristics of the ferroan intrusions. Moreover, in the local maps for each intrusion, it is possible to identify internal heterogeneities in these plutons, which correlate to geological processes, geochemistry, and petrography. Diorites and gabbros show low to medium values of K (1-3%), eTh (5-20 ppm) and eU (0.2-2 ppm), contrasting with the high values of regions with a dominance of ferroan granitoids (K, 3-6%; eTh, 15-60 ppm; eU, 2-4 ppm).	[Antunes de Amorim, Jose Victor; Ribeiro, Vanessa Biondo; Guimaraes, Ignez de Pinho; Silva Farias, Douglas Jose; de Lima, Jefferson Valdemiro; da Silva Filho, Adejardo Francisco] Univ Fed Pernambuco, Recife, PE, Brazil	Universidade Federal de Pernambuco	de Amorim, JVA (autor correspondente), Univ Fed Pernambuco, Recife, PE, Brazil.	josevictor.amorim@ufpe.br; van.biondo@gmail.com; ignez@ufpe.br; douglasjsfarias@yahoo.com.br; jefferson1901@hotmail.com; afsf@ufpe.br	DA SILVA FILHO, ADEJARDO FRANCISCO/C-2352-2014; de Amorim, José Victor Antunes/L-4233-2018	de Amorim, José Victor Antunes/0000-0002-1688-2218; DA SILVA FILHO, ADEJARDO/0000-0002-6341-2286; Silva Farias, Douglas Jose/0000-0003-4505-9623; Biondo Ribeiro, Vanessa/0000-0002-4573-6893	Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco (FACEPE) [IBPG-1074-1.07/15]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [470255/2013-7-CNPq]	Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco (FACEPE)(Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco (FACEPE)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We are grateful for the Brazilian Geological Survey (CPRM) for allowing us to use and publish geophysical data from the projects "Borda Leste do Planalto da Borborema" and "PernambucoParaiba airborne geophysical" surveys. We want to thank the Editor-in-Chief, the Associate Editor, and anonymous reviewers for their constructive criticism, and suggestions to improve the quality of the text. Furthermore, the corresponding author is exceptionally thankful for the support given and wisdom shared by Edilton Jose dos Santos and during the six-months of internship at CPRM in the year of 2015. This work was supported by Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco (FACEPE); under grant [IBPG-1074-1.07/15]; and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [470255/2013-7-CNPq].	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J	Arena, KR; Hartmann, LA; Lana, C; Queiroga, GN; Castro, MP				Arena, Karine R.; Hartmann, Leo A.; Lana, Cristiano; Queiroga, Glaucia N.; Castro, Marco P.			Geochemistry and delta B-11 evolution of tourmaline from tourmalinite as a record of oceanic crust in the Tonian Ibare ophiolite, southern Brasiliano Orogen	ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS			English	Article						boron isotopes; geochemistry; Ibare ophiolite; tourmalinite; southern Brasiliano Orogen	BORON ISOTOPE SYSTEMATICS; DOM FELICIANO BELT; PB-HF ISOTOPES; VOLCANO-SEDIMENTARY SUCCESSIONS; SAO-GABRIEL BLOCK; U-PB; NEOPROTEROZOIC JUVENILE; BRAZILIAN SHIELD; ZIRCON; ROCKS	The isotopic and geochemical evolution of tourmaline constrain the processes of paleo-oceanic lithosphere in ophiolites. The Brasiliano Orogen is a major structure of South America and requires characterization for the understanding of Gondwana supercontinent evolution. We made a pioneering investigation of tourmaline from a tourmalinite in the Ibare ophiolite by integrating field work with chemical analyses of tourmaline by electron microprobe (EPMA) and delta B-11 determinations via laser ablation inductively coupled plasma mass spectrometer (LA-ICP-MS). Remarkably massive tourmalinite (>90 vol.% tourmaline, some chlorite) enclosed in serpentinite has homogeneous dravite in chemical and isotopic composition (delta B-11 = +3.5 to +5.2 parts per thousand). These results indicate a geotectonic environment in the altered oceanic crust for the origin of the tourmalinite. This first delta B-11 characterization of tourmaline from tourmalinite sets limits to the evolution of the Neoproterozoic to Cambrian Brasiliano Orogen and Gondwana evolution.	[Arena, Karine R.; Hartmann, Leo A.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Lana, Cristiano; Queiroga, Glaucia N.; Castro, Marco P.] Univ Fed Ouro Preto, Dept Geol, Escola Minas, BR-35400000 Ouro Preto, MG, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal de Ouro Preto	Arena, KR (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	karinearena@gmail.com	Hartmann, Léo A/D-7663-2013; Queiroga, Gláucia/AAJ-1823-2021	Hartmann, Léo A/0000-0001-7863-5071; Queiroga, Gláucia/0000-0002-1730-0638; Lana, Cristiano/0000-0001-6302-9706; de Castro, Marco Paulo/0000-0001-8209-5995	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS)	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS))	This study is part of the PhD thesis by Karine da Rosa Arena at Programa de Pos-Graduacao em Geociencias, Universidade Federal do Rio Grande do Sul, Brazil. Karine held a scholarship during her PhD research from Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq). Financial support was provided by grant from Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) to Leo A. Hartmann. Reviewer Joao Orestes S. Santos is thanked for significant contributions that improved the manuscript.	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Acad. Bras. Cienc.		2020	92	1							e20180193	10.1590/0001-3765202020180193	http://dx.doi.org/10.1590/0001-3765202020180193			16	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	LC5WD	32267302	gold, Green Published			2023-06-23	WOS:000525401200001
J	Neto, RSB; Lamarao, CN; Marques, GT; Pinto-Coelho, CV				Barros Neto, Rubem Santa Brigida; Lamarao, Claudio Nery; Marques, Gisele Tavares; Pinto-Coelho, Cristina Valle			Morphological and compositional study of quartz and cassiterite of the Mocambo Granite, South Para Tin Province, Amazonian Craton	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Amazonian craton; SEM-CL images quartz textures; hydrothermal alteration; Tin mineralization; cassiterite	PORPHYRY COPPER-DEPOSIT; A-TYPE GRANITES; EASTERN ERZGEBIRGE; TRACE-ELEMENTS; MINERALIZED GRANITES; HYDROTHERMAL QUARTZ; GROWTH HISTORIES; CATHODOLUMINESCENCE; COMPLEX; GEOCHEMISTRY	Quartz and cassiterite crystals of granite, greisens, and quartz veins from Mocambo Granite, Carajas Province, were studied by scanning electron microscopy - cathodoluminescence and electron microprobe. Five types of quartz were identified: Qz1, magmatic and Qz2, Qz3, Qz4, and Qz5 hydrothermal. Qz1, anhedric to subhedric, luminescent and fractured at different intensities, predominating in less evolved rocks. Qz2, with low luminescence, is younger than Qz1; it occurs as irregular patches, filling fractures or forming veins that cut Qz1. Qz3, non-luminescent, resulting from continuous alteration, dissolution, and recrystallization processes; fills fractures that cut Qz1 and Qz2. Qz4 occurs in the most evolved and hydrothermalized rocks and in greisens bodies mineralized in cassiterite; is euhedral to subhedral, exhibits well-defined zoning, and has been interpreted as later than the previous one. Qz5 has poor luminescence; occurs in mineralized veins with wolframite and, secondarily, cassiterite. Qz1 shows Ti enrichment, while Qz4 associated with cassiterite is enriched with Al. Well-formed cassiterite crystals exhibit concentric zoning and low Fe, Ti, W, Nb and Mn contents. Qz5-associated cassiterite crystals form inclusions in the wolframite, suggesting that cassiterite and wolframite precipitated from hydrothermal processes at different times.	[Barros Neto, Rubem Santa Brigida; Lamarao, Claudio Nery; Marques, Gisele Tavares] Univ Fed Para, Programa Posgrad Geol & Geoquim, Inst Geociencias, Belem, Para, Brazil; [Barros Neto, Rubem Santa Brigida; Lamarao, Claudio Nery; Marques, Gisele Tavares] Univ Fed Para, Grp Pesquisa Petrol Granitoides, Belem, Para, Brazil; [Lamarao, Claudio Nery; Marques, Gisele Tavares] Univ Fed Para, Lab Microanal, Belem, Para, Brazil; [Pinto-Coelho, Cristina Valle] Univ Fed Parana, Programa Posgrad Geol, Curitiba, Parana, Brazil	Universidade Federal do Para; Universidade Federal do Para; Universidade Federal do Para; Universidade Federal do Parana	Neto, RSB (autor correspondente), Univ Fed Para, Programa Posgrad Geol & Geoquim, Inst Geociencias, Belem, Para, Brazil.; Neto, RSB (autor correspondente), Univ Fed Para, Grp Pesquisa Petrol Granitoides, Belem, Para, Brazil.	rubembarrosnt@gmail.com; lamarao@ufpa.br; gisele.ufpa@gmail.com; cristinavpc@ufpr.br	Lamarão, Claudio/AAZ-9577-2021	Marques, Gisele/0000-0003-3122-259X; Lamarao, Claudio/0000-0002-0672-3977; Pinto-Coelho, Cristina/0000-0003-1470-1337; Barros Neto, Rubem/0000-0001-7398-3202	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq); PQ-2 CNL research grant [305701/2014-2]; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Instituto de Geociencias of UFPA; Grupo de Pesquisa Petrologia de Granitoides (GPPG); MCTI/CNPQ/Universal Research Project [458941/2014-0]; Instituto de Geociencias da Amazonia -GEOCIAM (INCT-CNPq/MCT/FAPESPA) [573733/2008-2]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); PQ-2 CNL research grant; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Instituto de Geociencias of UFPA; Grupo de Pesquisa Petrologia de Granitoides (GPPG); MCTI/CNPQ/Universal Research Project; Instituto de Geociencias da Amazonia -GEOCIAM (INCT-CNPq/MCT/FAPESPA)	The authors are grateful to the reviewers and regional editor for their comments and suggestions, the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for the master's scholarship awarded to the first author and the PQ-2 CNL research grant (Process 305701/2014-2) for the second author. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001, the Instituto de Geociencias of UFPA, and the Grupo de Pesquisa Petrologia de Granitoides (GPPG). This study is a contribution to the MCTI/CNPQ/Universal Research Project (Process 458941/2014-0) and the Instituto de Geociencias da Amazonia -GEOCIAM (INCT-CNPq/MCT/FAPESPA-Proc. 573733/2008-2).	Abreu F.A.M., 1974, C BRASILEIRO GEOLOGI, V28, P11; Almeida J. A.C., 2006, BRAZ J GEOSCI, V36, P282; [Anonymous], 2013, GEOL USP SER CIENT, DOI DOI 10.5327/Z1519-874X2013000200004; Braz J. 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J. Geol.		2020	50	4							e20190096	10.1590/2317-4889202020190096	http://dx.doi.org/10.1590/2317-4889202020190096			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QF2AU		gold			2023-06-23	WOS:000616702600001
J	Benites, S; Sommer, CA; De Lima, EF; Savian, JF; Hagg, MB; Moncinhatto, TR; Da Trindade, RIF				Benites, Susana; Sommer, Carlos A.; De Lima, Evandro F.; Savian, Jairo F.; Hagg, Mauricio B.; Moncinhatto, Thiago R.; Da Trindade, Ricardo I. F.			Characterization of volcanic structures associated to the silicic magmatism of the Parana-Etendeka Province, in the Aparados da Serra region, southern Brazil	ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS			English	Article						Anisotropy of Magnetic Susceptibility; image processing; silicic lavas; volcanic morphologies	FLOOD BASALTS; TORRES SYNCLINE; CHEMICAL STRATIGRAPHY; PLATEAU BRAZIL; LAVAS; ROCKS; AGE; CLASSIFICATION; PETROLOGY; NAMIBIA	The Parana-Etendeka Magmatic Province is associated with the distensive tectonics that caused the rupture of the Gondwana continent during the Lower Cretaceous and generated an intense volcanism that covers South America and the NW portion of Namibia in Africa. In Brazil, this volcanic sequence is named Serra Geral Group and predominantly consists of basalts and subordinated silicic rocks. The goal of this study is to characterize the geomorphological features observed in the Aparados da Serra region, southern Brazil, and to evaluate the relationship between these structures and the primary silicic volcanic structures. The geomorphological features were first identified using remote sensing and then correlated with flow structures observed in the field, as well as petrographic and geochemical data. AMS data were used to determine magnetic patterns and the direction of magmatic flow of the rocks. Despite the low degree of anisotropy, clear patterns of lineation and foliation were identified in the studied rocks. Our data shows that Units I and II correspond to silicic lava flows linked to effusive fissure eruptions, presenting a dome morphology caused by differential erosion. Unit III rocks may correspond to true volcanic domes, whereas the Unit IV corresponds to the effusive feeder structures.	[Benites, Susana; Hagg, Mauricio B.] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500,Predio 43113, BR-91501970 Porto Alegre, RS, Brazil; [Sommer, Carlos A.] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Geodesia, Av Bento Goncalves 9500,Predio 43113, BR-91501970 Porto Alegre, RS, Brazil; [De Lima, Evandro F.] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Mineral & Petrol, Av Bento Goncalves 9500,Predio 43113, BR-91501970 Porto Alegre, RS, Brazil; [Savian, Jairo F.] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Geol, Av Bento Goncalves 9500,Predio 43113, BR-91501970 Porto Alegre, RS, Brazil; [Moncinhatto, Thiago R.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Programa Posgrad Geofis, Rua Matao 1226, BR-05508090 Sao Paulo, SP, Brazil; [Da Trindade, Ricardo I. F.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Dept Geofis, Rua Matao 1226, BR-05508090 Sao Paulo, SP, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade de Sao Paulo; Universidade de Sao Paulo	Benites, S (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500,Predio 43113, BR-91501970 Porto Alegre, RS, Brazil.	susanabenites@outlook.com	DE LIMA, EVANDRO FERNANDES/AAA-8150-2020; Savian, Jairo Francisco/J-4782-2015; Sommer, Carlos A/Q-9077-2018; Trindade, Ricardo IF/A-8146-2008	DE LIMA, EVANDRO FERNANDES/0000-0002-4101-3161; Savian, Jairo Francisco/0000-0002-5032-3217; Sommer, Carlos A/0000-0001-8696-7084; Trindade, Ricardo IF/0000-0001-9848-9550; Barcelos Haag, Mauricio/0000-0001-5038-4418	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [400724/2014-6, 441766/2014-5, 302213/2012-0, 303584/2009-2, 473683/2007, 5470641/2008-8, 470203/2007-2, 471402/2012-5, 303038/2009-8, 470505/2010-9]; Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) [1180/12-8, PRONEX 10/0045-6]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS))	This work had partial financial support to C.A. Sommer and E.F. Lima from Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (400724/2014-6, 441766/2014-5, 302213/2012-0, 303584/2009-2, 473683/2007, 5470641/2008-8, 470203/2007-2, 471402/2012-5, 303038/2009-8 and 470505/2010-9), and from the Fundacao de Amparo a Pesquisa do Estado do Rio Grande do Sul (FAPERGS) 1180/12-8, and PRONEX 10/0045-6. We thank the laboratory support from the IGEO/UFRGS and Laboratorio de Paleomagnetismo da Universidade de Sao Paulo (USPMag). We also thank the anonymous reviewers for their important contribution to the research paper.	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J	Bitencourt, VB; Dillenburg, SR				Borges Bitencourt, Volney Junior; Dillenburg, Sergio R.			Application of multivariate statistical techniques in alongshore differentiation of coastal barriers	MARINE GEOLOGY			English	Article						Coastal evolution; Beach morphodynamics; Principal Component Analysis (PCA); Hierarchical Cluster Analysis (HCA)	GRANDE-DO-SUL; SEA-LEVEL RISE; PRINCIPAL COMPONENT ANALYSIS; LATE-HOLOCENE; SEDIMENT TRANSPORT; SOUTHERN BRAZIL; WAVE-ENERGY; TRANSGRESSIVE DUNEFIELDS; BEACH MORPHODYNAMICS; ACCOMMODATION SPACE	This paper investigates the existence of statistical correlations and relationships between geological and oceanographic parameters along a coastal barrier system in southern Brazil. The existence of few statistical studies on coastal barriers motivated the use of multivariate statistical techniques that take environmental parameters such as coastal morphological-sedimentary features and their morphometric measurements into account. The Hierarchical Cluster Analysis (HCA) and Principal Component Analysis (PCA) were used to assess the spatial variations of fourteen parameters driving the current and past behavior of this coastal barrier system at fourteen locations. Through the application of HCA, these locations were divided into four groups (Groups 1, 2, 3, and 4). The HCA results were analyzed using PCA. The first (PC1) and the second (PC2) principal components together explained at least 76.4% of the variability of all four groups. The most important geological and oceanographic parameters that were correlated to PC1 and PC2 were different in each group. In general, the shoreface slope and shoreface dimensions were common to all groups as PC1-correlated parameters, being the most important ones regarding data variability. In addition, for the progradational (Groups 1 and 4), retrogradational (Group 2) and aggradational barriers (Group 3) PCA indicated that shoreline orientation (wave exposure) and beach type are secondary, but relevant factors controlling the past and current behavior of coastal barriers in southern Brazil.	[Borges Bitencourt, Volney Junior] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil; [Dillenburg, Sergio R.] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, Inst Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Bitencourt, VB (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil.	volney.bitencourt@ufrgs.br; sergio.dillenburg@ufrgs.br	Dillenburg, Sergio/C-4027-2013; de Bitencourt, Volney Junior Borges/AAD-9618-2019	Dillenburg, Sergio/0000-0003-0072-7018; de Bitencourt, Volney Junior Borges/0000-0002-1004-5179	Brazilian National Council for Scientific and Technological Development (CNPq) [141007/2015-0]	Brazilian National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank Carla Bonetti (UFSC) for the assistance with the multivariate statistical analysis. We also thank Pedro S. Pereira (UFSC) for sharing part of the data used in this paper. We wish to thanks to the Brazilian National Council for Scientific and Technological Development (CNPq) for the doctoral fellowship (V.J.B. Bitencourt, grant ID 141007/2015-0) and for the research fellowship (S.R. Dillenburg).	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Geol.	JAN	2020	419								106077	10.1016/j.margeo.2019.106077	http://dx.doi.org/10.1016/j.margeo.2019.106077			14	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	KE3WU					2023-06-23	WOS:000508490400018
J	Lisboa, VAC; Conceicao, H; Rosa, MLS; Marques, GT; Lamarao, CN; Lima, ALR				Carvalho Lisboa, Vinicius Anselmo; Conceicao, Herbet; Silva Rosa, Maria Lourdes; Marques, Gisele Tavares; Lamarao, Claudio Nery; Rezende Lima, Andre Luiz			Amphibole crystallization conditions as record of interaction between ultrapotassic enclaves and monzonitic magmas in the Gloria Norte Stock, South of Borborema Province	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						mineral chemistry; amphibole thermobarometry; Sergipano Orogenic System	MAFIC MICROGRANULAR ENCLAVES; IGNEOUS ROCK SERIES; CALCIC AMPHIBOLE; HORNBLENDE; PRESSURE; STABILITY; AL; GRANITOIDS; CHEMISTRY; EVOLUTION	The Gloria Norte Stock (GNS) is made up of predominantly porphyritic biotite-amphibole-bearing quartz monzonite, enclosing a large number of microgranular mafic enclaves (MME). The GNS MME are fine-grained rocks with rounded and ellipsoid shapes that show sharp and gradational contacts with the host rocks, suggesting they coexisted with the host monzonite as magmas. The studied amphibole crystals of the two rock types are calcic and correspond to pargasite, edenite, and magnesium-hornblende. Their compositions are influenced by substitutions involving Al3+, Na+, Fe2+, Si4+ and Mg2+ ions, reflecting the decrease in temperature and the increase in oxygen fugacity. They present low Ti and Al contents, and varied Si content (6.2-7.7 apuf). The mg# values range from 0.48-0.84. Pressures for the crystallization of the MME amphiboles vary between 2.6 and 7.8 kbar and the temperatures of solidus and liquidus were estimated between 600-659 and 887-908 degrees C, respectively. The early MME amphibole crystals with lower Si and Mg content were formed under high pressure (7.8 kbar) and temperature (908 degrees C). The presence of amphiboles with 862 degrees C and 5 kbar in MME and GNS reflects that the interaction between these magmas occurred at 18 km of depth.	[Carvalho Lisboa, Vinicius Anselmo; Conceicao, Herbet] Univ Fed Bahia, Salvador, BA, Brazil; [Carvalho Lisboa, Vinicius Anselmo] Inst Fed Educ Ciencia & Tecnol Paraiba, Picui, PB, Brazil; [Conceicao, Herbet; Silva Rosa, Maria Lourdes; Rezende Lima, Andre Luiz] Univ Fed Sergipe, Sao Cristovao, SE, Brazil; [Marques, Gisele Tavares; Lamarao, Claudio Nery] Univ Fed Para, Belem, Para, Brazil	Universidade Federal da Bahia; Instituto Federal da Paraiba (IFPB); Universidade Federal de Sergipe; Universidade Federal do Para	Lisboa, VAC (autor correspondente), Univ Fed Bahia, Salvador, BA, Brazil.; Lisboa, VAC (autor correspondente), Inst Fed Educ Ciencia & Tecnol Paraiba, Picui, PB, Brazil.	vinicius.lisboa@ifpb.edu.br; herbet@ufs.br; lrosa@ufs.br; gisele.ufpa@gmail.com; lamarao@ufpa.br; luizrezendelima@gmail.com	da Silva Rosa, Maria de Lourdes/AAB-4794-2021; Conceicao, Herbet/HTP-6867-2023; Lamarão, Claudio/AAZ-9577-2021	da Silva Rosa, Maria de Lourdes/0000-0002-5099-829X; Marques, Gisele/0000-0003-3122-259X; Herbet, Conceicao/0000-0002-9172-4519; Lamarao, Claudio/0000-0002-0672-3977; Carvalho Lisboa, Vinicius Anselmo/0000-0002-1976-3118	CNPq [140117/2015-6, 311008/2017-8, 310391/2017-2, 405387/2016-4]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The first author thanks the IFPB, Campus Picui, for granting the removal for completion of the Doctorate in Geology at UFBA. The authors thank CNPq processes: 140117/2015-6 (VACL Doctorate grant), 311008/2017-8 (CNPq-PQ), 310391/2017-2 (CNPq-PQ), 405387/2016-4 (CNPq-Universal 2016). We are grateful to the anonymous reviewers for the comments and suggestions that have improved considerably the original manuscript.	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J. Geol.		2020	50	2								10.1590/2317-4889202020190101	http://dx.doi.org/10.1590/2317-4889202020190101			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QF1ZK		gold, Green Published			2023-06-23	WOS:000616699000001
J	Caxito, FD; Santos, LCMD; Ganade, CE; Bendaoud, A; Fettous, EH; Bouyo, MH				Caxito, Fabricio de Andrade; Montefalco de Lira Santos, Lauro Cezar; Ganade, Carlos Eduardo; Bendaoud, Abderrahmane; Fettous, El-Hocine; Bouyo, Merlain Houketchang			Toward an integrated model of geological evolution for NE Brazil-NW Africa: The Borborema Province and its connections to the Trans-Saharan (Benino-Nigerian and Tuareg shields) and Central African orogens	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Borborema Province; West Gondwana; Neoproterozoic; Transaharan; Brasiliano/Pan-African	PERNAMBUCO-ALAGOAS DOMAIN; CEARA CENTRAL DOMAIN; PRETO FOLD BELT; NEOPROTEROZOIC SERGIPANO BELT; SAO-FRANCISCO CRATON; U-PB GEOCHRONOLOGY; SM-ND ISOTOPE; GRANULITE-FACIES METAMORPHISM; HIGH-PRESSURE GRANULITES; TRANSCURRENT SHEAR ZONE	Both the Borborema Province of NE Brazil and the geological provinces of NW Africa (the Trans-Saharan Orogen consisted of the Tuareg and Benino-Nigerian shields and the Central African Orogen of Cameroon, Chad, and Central African Republic) are complex geological regions with superposition of distinct deformational, metamorphic and magmatic events and final structural configuration during the Brasiliano/Pan-African Orogeny (ca. 625-510 Ma). These provinces represent the site of major mountain building processes in the Ediacaran/Cambrian transition that culminated in the amalgamation of West Gondwana after the collision of the West African-Sao Luis, Sao Francisco-Congo, and Saharan paleocontinents. In the last years, discovery and characterization of key tectonic units such as ophiolites, eclogites, HP/UHP rocks, and both oceanic and continental magmatic arcs are helping to clarify these processes and propose tectonic models for the geological evolution of NE Brazil-NW Africa. Connections of the marginal belts that frame these provinces, bordering the eastern margin of the West African-Sao Luis Craton (Medio Corean-Dahomeyides-Gourma-West Tuareg Shield) and the northern margin of the Sao Francisco-Congo Craton (Rio Preto-Riacho do Pontal-Sergipano-Yaounde-Central African) are progressively better constrained, while correlations within the interior, highly reworked and sectioned portions of both the Borborema Province, the Benino-Nigerian Shield, the Central and East Tuareg Shield, Western Cameroon, and Adamawa-Yade domains are more complicated and demand further investigation. Some of the questions of prime importance in this context are the continuation or not of the 1000-920 Ma Cariris Velhos Belt of NE Brazil into NW Africa, and if the basement-dominated North Borborema/Benino-Nigerian (NOBO-BEND and Alto Pajen-Alto Moxot6-Rio Capibaribe-Pernambuco-Alagoas/Adamawa-Yade (APAMCAPAY) domains could represent major decratonized blocks (such as LATEA in the Central Tuareg Shield), perhaps developed due to hyperextension and detachment of a Greater Sao Francisco-Congo paleocontinent northern margin. In this case, the Goias-Pharusian and Transnordestino-Central African oceanic realms along with restricted internal oceans such as the hypothetical Pianc6-Alto Brigida/Western Cameroon (PAB-WECA) Seaway probably separated these ancient paleocontinental blocks during the Neoproterozoic. The development of subduction zones and the docking of Neoproterozoic juvenile terranes welded the hyperextended Archean/Paleoproterozoic lithospheric fragments together and they became squeezed and reworked in between the major cratonic landmasses during the Brasiliano/Pan-African Orogeny. The quest for the sites of ancient oceans and continents that once composed NE Brazil and NW Africa goes on and tentative scenarios will surely benefit from novel geological, isotopic, and geochronological data put forward in the near future.	[Caxito, Fabricio de Andrade] Univ Fed Minas Gerais, Ctr Pesquisas Manoel Teixeira Costa, Belo Horizonte, MG, Brazil; [Montefalco de Lira Santos, Lauro Cezar] Univ Fed Pernambuco, Recife, PE, Brazil; [Ganade, Carlos Eduardo] Geol Survey Brazil, Rio De Janeiro, RJ, Brazil; [Bendaoud, Abderrahmane; Fettous, El-Hocine] Univ Sci & Technol Houari Boumediene, Lab Geodynam Geol Ingenieur & Planetol, Algiers, Algeria; [Bouyo, Merlain Houketchang] Ctr Geol & Min Res, Garoua, Cameroon	Universidade Federal de Minas Gerais; Universidade Federal de Pernambuco; University Science & Technology Houari Boumediene	Caxito, FD (autor correspondente), Univ Fed Minas Gerais, Ctr Pesquisas Manoel Teixeira Costa, Belo Horizonte, MG, Brazil.	caxitop@ufmg.br; lauromontefalco@gmail.com; caegeo@gmail.com; abendaoud@gmail.com; hfettous@gmail.com; mbouyou2001@yahoo.fr	Caxito, Fabricio A/J-1317-2016; de Lira Santos, Lauro Cézar Montefalco/E-5536-2015; BENDAOUD, Abderrahmane/L-6828-2013	Caxito, Fabricio A/0000-0002-0335-3667; 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J. Geol.		2020	50	2							e20190122	10.1590/2317-4889202020190122	http://dx.doi.org/10.1590/2317-4889202020190122			38	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MP8BI		gold			2023-06-23	WOS:000552424600001
J	Caxito, FD; Santos, LCMD; Uhlein, A; Dantas, EL; Alkmim, AR; Lana, C				Caxito, Fabricio de Andrade; de Lira Santos, Lauro Cezar Montefalco; Uhlein, Alexandre; Dantas, Elton Luiz; Alkmim, Ana Ramalho; Lana, Cristiano			New U-Pb (SHRIMP) and first Hf isotope constraints on the Tonian (1000-920 Ma) Cariris Velhos event, Borborema Province, NE Brazil	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						U-Pb SHRIMP geochronology; Hf isotope analysis; Cariris Velhos; Borborema Province	PERNAMBUCO-ALAGOAS DOMAIN; PONTAL OROGEN; NEOPROTEROZOIC EVOLUTION; NORTHEASTERN BRAZIL; CRUSTAL EVOLUTION; DETRITAL ZIRCONS; FOLD BELT; ICP-MS; RIACHO; GEOCHRONOLOGY	Orthogneisses associated with metavolcanosedimentary successions related to the 1000 - 920 Ma Cariris Velhos event occur mainly in a ca. 700 km-long sigmoidal-shaped belt that crosscuts the Transversal Zone of the Borborema Province and extends to the fold belts located in its southern or external zone (part of the Riacho do Pontal and Sergipano orogens). Despite its importance, the tectonic setting and the role of those rocks in the geological evolution of the Borborema Province are contentious and not yet well understood. New zircon U-Pb SHRIMP data on an augen-gneiss sill of the Afeicao Suite intruding mica-schists mapped as part of the Santa Filomena Complex yielded a Concordia Age of 974 +/- 11 Ma, indicating that at least part of the metasedimentary rocks in the internal zone of the Riacho do Pontal Orogen are Tonian or older and possibly related to the Cariris Velhos event. Hf-in-zircon isotope data are presented for the first time for Cariris Velhos-related ortho-derived rocks of the Afeicao Suite. Analyzed samples yielded MOO in a narrow range between -1.51 and +2.41, with associated T-DMHf of 1.6-1.4 Ga, similar to previously obtained Nd isotope data with epsilon Nd(t) = -1.0 to +3.1 and T-DMNd of 1.5-1.2 Ga. A possible scenario to explain both the geochemical features and the moderately juvenile to slightly evolved, near-chondritic Hf and Nd isotope signatures is a continental arc setting, where fractionated melts produced in the supra-subduction zone mantle wedge carrying a Tonian juvenile signature became contaminated with discrete amounts of Archean-Paleoproterozoic continental crust during ascent, producing Mesoproterozoic model ages which represent the mixture of those two end-members.	[Caxito, Fabricio de Andrade; Uhlein, Alexandre] Univ Fed Minas Gerais, Belo Horizonte, MG, Brazil; [de Lira Santos, Lauro Cezar Montefalco] Univ Fed Pernambuco, Recife, PE, Brazil; [Dantas, Elton Luiz] Univ Brasilia, Brasilia, DF, Brazil; [Alkmim, Ana Ramalho; Lana, Cristiano] Univ Fed Ouro Preto, Ouro Preto, MG, Brazil	Universidade Federal de Minas Gerais; Universidade Federal de Pernambuco; Universidade de Brasilia; Universidade Federal de Ouro Preto	Caxito, FD (autor correspondente), Univ Fed Minas Gerais, Belo Horizonte, MG, Brazil.	caxitop@ufmg.br; lauromontefalco@gmail.com; auhlein@gmail.com; elton@unb.br; ana_alkmim@yahoo.com.br; cristianodeclana@gmail.com	Dantas, Elton Luiz/AAK-8464-2021; de Lira Santos, Lauro Cézar Montefalco/E-5536-2015; Caxito, Fabricio A/J-1317-2016; Alkmim, Ana Ramalho/H-4646-2017	Dantas, Elton Luiz/0000-0002-7954-5059; de Lira Santos, Lauro Cézar Montefalco/0000-0001-6098-1873; Caxito, Fabricio A/0000-0002-0335-3667; Lana, Cristiano/0000-0001-6302-9706; Alkmim, Ana Ramalho/0000-0001-7835-2151	CAPES; FAPEMIG; CNPq	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); FAPEMIG(Fundacao de Amparo a Pesquisa do Estado de Minas Gerais (FAPEMIG)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This paper is an homage to the late Edilton Santos, whose lifetime of devotion to deciphering the geology of the Borborema Province is a standing incentive and role model to all of us. We would like to thank Brazilian funding agencies CNPq, CAPES, and FAPEMIG among others for the sustained support to conduct scientific research in Brazil. FAC, AU, ELD, and CL are recipients of CNPq Research Productivity grants and acknowledge the support received. The U-Pb analyses were performed using a SHRIMP II probe at the John DeLaeter Centre of the Curtin University, Perth, Western Australia, enabled by NCRIS via AuScope. We thank Neal McNaughton for guidance and support during the preparation and analysis of the SHRIMP mounts and Allen Kennedy and Hao Gao for support during the analysis. A previous version was greatly enhanced after comments and suggestions by three anonymous reviewers.	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J. Geol.		2020	50	2							e20190082	10.1590/2317-4889202020190082	http://dx.doi.org/10.1590/2317-4889202020190082			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LG6BY		gold, Green Published			2023-06-23	WOS:000528184900001
J	Chagas, MP; Teixeira, LSG; Santana, RC; Trindade, ASN; Barbosa, ID; Dantas, AF; Korn, MGA; Almeida, JS				Chagas, Manoel P.; Teixeira, Leonardo S. G.; Santana, Rafael C.; Trindade, Alex S. N.; Barbosa, Isa dos S.; Dantas, Alailson F.; Korn, Maria Gracas A.; Almeida, Jorge S.			Determination and Evaluation of Lead Migration for Foods Prepared in Clay Pots	FOOD ANALYTICAL METHODS			English	Article						Glazed clay pots; Toxic metals; Lead determination; Metal migration to food	GLAZED CERAMICS; ICP OES; ALUMINUM; CADMIUM; EXTRACTION; CONTAINERS; EXPOSURE; UTENSILS; COOKING; RELEASE	This work presents a study to evaluate the migration of lead to cooked foods prepared in clay pots produced in a small community in Brazil. Clay pots produced in Maragogipinho, Bahia, Brazil, go through an artisanal vitrification process by the addition of lead oxide to improve the visual appearance of the pot. To evaluate the migration of the lead to the food, samples of a fish-based delicacy (fish stew), with and without palm oil and coconut milk, were taken at different moments of contact with the clay container after cooking. Determination of lead concentrations was performed by inductively coupled plasma optical emission spectrometry (ICP-OES), and the concentrations found were higher than 2.0 mg kg(-1), which is the value regulated by the Brazilian Health Regulatory Agency. In addition, the highest concentrations of lead were detected in samples with a longer contact time with the pan. The longer the contact time was, the higher the lead content that migrated to the food. These results suggest that cooking and storing foods in the glazed clay pots pose a potential risk of lead contamination.	[Chagas, Manoel P.; Teixeira, Leonardo S. G.; Santana, Rafael C.; Trindade, Alex S. N.; Barbosa, Isa dos S.; Dantas, Alailson F.; Korn, Maria Gracas A.; Almeida, Jorge S.] Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Teixeira, Leonardo S. G.; Korn, Maria Gracas A.; Almeida, Jorge S.] Univ Fed Bahia, INCT Energia & Ambiente, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia	Almeida, JS (autor correspondente), Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.; Almeida, JS (autor correspondente), Univ Fed Bahia, INCT Energia & Ambiente, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.	jorgealmeidas@hotmail.com	Korn, Maria Graças/AAH-3445-2020; Teixeira, Leonardo S G/J-9131-2016; Almeida, Jorge/AAC-3022-2020; de Almeida, Jorge Santos/ABF-4979-2020	Teixeira, Leonardo S G/0000-0003-0320-8299; de Almeida, Jorge Santos/0000-0002-9450-1062				Abou-Arab AAK, 2001, FOOD CHEM, V73, P163, DOI 10.1016/S0308-8146(00)00256-9; Agarwal P, 1997, SCI TOTAL ENVIRON, V199, P271, DOI 10.1016/S0048-9697(97)05455-7; Almeida JS, 2019, FOOD CHEM, V273, P130, DOI 10.1016/j.foodchem.2018.01.112; [Anonymous], THESIS; [Anonymous], C73894 ASTM; [Anonymous], PORT 27 18 MARC 1996; [Anonymous], HARPER BIOQUIMICA IL; AVILA MH, 1991, ENVIRON HEALTH PERSP, V94, P117, DOI 10.2307/3431303; Bergkvist C, 2010, ENVIRON RES, V110, P718, DOI 10.1016/j.envres.2010.07.004; Bi SP, 1996, ENVIRON POLLUT, V92, P85, DOI 10.1016/0269-7491(95)00038-0; deMejia EG, 1996, ARCH ENVIRON CON TOX, V31, P581, DOI [10.1007/BF00212443, 10.1007/s002449900147]; Edem DO, 2002, HUM NUTR, V57, P3, DOI [10.1023/A:1021828132707, DOI 10.1023/A:1021828132707]; Gonzalez-Soto E, 2000, B ENVIRON CONTAM TOX, V65, P598, DOI 10.1007/s0012800165; ISKANDER FY, 1990, FOOD CHEM, V35, P197, DOI 10.1016/0308-8146(90)90033-Z; Kiyataka PHM, 2015, FOOD ANAL METHOD, V8, P2331, DOI 10.1007/s12161-015-0124-8; KULIGOWSKI J, 1992, ARCH ENVIRON CON TOX, V23, P211, DOI 10.1007/BF00212277; MATTE TD, 1994, LANCET, V344, P1064, DOI 10.1016/S0140-6736(94)91715-9; Miecznikowski JC, 2010, PROTEOME SCI, V8, DOI 10.1186/1477-5956-8-66; MOHAMED N, 1995, FOOD CHEM, V54, P245, DOI 10.1016/0308-8146(95)00035-H; Nelson D.L., 2011, PRINCIPIOS BIOQUIMIC, V5; Ni LX, 2008, SCI TOTAL ENVIRON, V389, P202, DOI 10.1016/j.scitotenv.2007.08.039; Quintaes KD, 2002, FOOD ADDIT CONTAM, V19, P134, DOI 10.1080/02652030110066206; ROMIEU I, 1995, ENVIRON HEALTH PERSP, V103, P1036, DOI 10.2307/3432632; Santos DCMB, 2014, J FOOD COMPOS ANAL, V34, P75, DOI 10.1016/j.jfca.2014.02.008; Scancar J, 2004, FOOD CHEM, V85, P151, DOI 10.1016/j.foodchem.2003.07.028; Semwal AD, 2006, J SCI FOOD AGR, V86, P2425, DOI 10.1002/jsfa.2635; Sheets RW, 1997, SCI TOTAL ENVIRON, V197, P167, DOI 10.1016/S0048-9697(97)05431-4; Tarantino TB, 2017, FOOD ANAL METHOD, V10, P1007, DOI 10.1007/s12161-016-0658-4; TROTTER RT, 1990, ENVIRON HEALTH PERSP, V89, P79, DOI 10.2307/3430901; Ustun I, 2015, FOOD ANAL METHOD, V8, P222, DOI 10.1007/s12161-014-9896-5; Valadez-Vega C, 2011, INT J MOL SCI, V12, P2336, DOI 10.3390/ijms12042336; Valles-Medina Ana M, 2014, Int Sch Res Notices, V2014, P474176, DOI 10.1155/2014/474176; Verissimo MIS, 2005, SENSOR ACTUAT B-CHEM, V111, P587, DOI 10.1016/j.snb.2005.05.004	33	2	2	2	12	SPRINGER	NEW YORK	ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES	1936-9751	1936-976X		FOOD ANAL METHOD	Food Anal. Meth.	JAN	2020	13	1			SI		268	274		10.1007/s12161-019-01614-4	http://dx.doi.org/10.1007/s12161-019-01614-4			7	Food Science & Technology	Science Citation Index Expanded (SCI-EXPANDED)	Food Science & Technology	KJ3SW					2023-06-23	WOS:000511978600030
J	Cordani, UG; Fairchild, TR; Ganade, CE; Babinski, M; Leme, JD				Cordani, Umberto G.; Fairchild, Thomas R.; Ganade, Carlos E.; Babinski, Marly; Leme, Juliana de Moraes			Dawn of metazoans: to what extent was this influenced by the onset of "modern-type plate tectonics"?	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						plate tectonics; mega-mountains; Ediacaran biota	RE-OS GEOCHRONOLOGY; EAST-AFRICAN OROGEN; DOUSHANTUO FORMATION; HUQF SUPERGROUP; EARLY HISTORY; WENGAN BIOTA; EVOLUTION; LIFE; OXYGENATION; CONSTRAINTS	The appearance of complex megascopic multicellular eukaryotes in the Ediacaran occurred just when the dynamics of a cooling Earth allowed establishment of a new style of global tectonics that continues to the present as "modern-type plate tectonics". The advent of this style was first registered in 620 Ma-old coesite-bearing Ultra-High Pressure eclogites within the Transbrasiliano-Kandi mega-shear zone along the site of the West Gondwana Orogeny (WGO). These eclogites comprise the oldest evidence of slab-pull deep subduction capable of inducing continental collisions and producing high-relief Himalayan-type mega-mountains. Life, prior to this time, was essentially microscopic. Yet with increasing Neoproterozoic oxygenation and intensified influx of nutrients to Ediacaran oceans, resulting from the erosion of these mountains, complex macroscopic heterotrophic eukaryotes arose and diversified, taking the biosphere to a new evolutionary threshold. The repeated elevation of Himalayan-type mega-mountains ever since then has continued to play a fundamental role in nutrient supply and biosphere evolution. Other authors have alluded to the influence of Gondwana mountain-building upon Ediacaran evolution, however we claim here to have identified when and where it began.	[Cordani, Umberto G.; Fairchild, Thomas R.; Ganade, Carlos E.; Babinski, Marly; Leme, Juliana de Moraes] Univ Sao Paulo, Sao Paulo, SP, Brazil	Universidade de Sao Paulo	Cordani, UG (autor correspondente), Univ Sao Paulo, Sao Paulo, SP, Brazil.	ucordani@usp.br; trfairch@usp.br; caegeo@gmail.com; babinski@usp.br; leme@usp.br	Cordani, Umberto/F-3686-2014; Fairchild, Thomas Rich/AAE-1835-2021; Babinski, Marly/B-9403-2013	Cordani, Umberto/0000-0003-4425-5905; Babinski, Marly/0000-0003-2444-2404; Ganade de Araujo, Carlos/0000-0002-2896-0551				Babinski M., 2011, THESIS, DOI [10.11606/T.44.2013.tde-26072013-151419, DOI 10.11606/T.44.2013.TDE-26072013-151419]; Babinski M, 2007, TERRA NOVA, V19, P401, DOI 10.1111/j.1365-3121.2007.00764.x; Bell EA, 2015, P NATL ACAD SCI USA, V112, P14518, DOI 10.1073/pnas.1517557112; BENGTSON S, 1992, SCIENCE, V257, P367, DOI 10.1126/science.257.5068.367; BOTTJER D.J., 2000, GSA TODAY, V10, P1; Bowring S., 2003, GEOPH RES ABSTR, V5, P219; Bowring SA, 2007, AM J SCI, V307, P1097, DOI 10.2475/10.2007.01; Brasier M, 2000, GEOLOGY, V28, P175, DOI 10.1130/0091-7613(2000)28<175:NUZDFT>2.0.CO;2; Brasier MD, 2001, PERS PALEOB, P69; Butterfield NJ, 2000, PALEOBIOLOGY, V26, P386, DOI 10.1666/0094-8373(2000)026<0386:BPNGNS>2.0.CO;2; Campbell IH, 2010, GEOCHIM COSMOCHIM AC, V74, P4187, DOI 10.1016/j.gca.2010.04.064; Canfield DE, 2005, ANNU REV EARTH PL SC, V33, P1, DOI 10.1146/annurev.earth.33.092203.122711; Cawood PA, 2018, PHILOS T R SOC A, V376, DOI 10.1098/rsta.2017.0405; Cohen PA, 2017, SCI ADV, V3, DOI 10.1126/sciadv.1700095; Cohen PA, 2012, J PALEONTOL, V86, P775, DOI 10.1666/11-138.1; Condon D, 2005, SCIENCE, V308, P95, DOI 10.1126/science.1107765; Cordani UG, 2013, BRAZ J GEOL, V43, P583, DOI 10.5327/Z2317-48892013000300012; Cunningham JA, 2017, J GEOL SOC LONDON, V174, P793, DOI 10.1144/jgs2016-142; Cunningham JA, 2017, BIOESSAYS, V39, DOI 10.1002/bies.201600120; Dodd MS, 2017, NATURE, V543, P60, DOI 10.1038/nature21377; dos Reis M, 2015, CURR BIOL, V25, P2939, DOI 10.1016/j.cub.2015.09.066; Erwin DH, 2011, SCIENCE, V334, P1091, DOI 10.1126/science.1206375; Feng T, 2008, ACTA GEOL SIN-ENGL, V82, P27; Fritz H, 2013, J AFR EARTH SCI, V86, P65, DOI 10.1016/j.jafrearsci.2013.06.004; GANADE DAC, 2014, LITHOS, V202, P167; de Araujo CEG, 2014, NAT COMMUN, V5, DOI 10.1038/ncomms6198; Gehling JG, 1996, J PALEONTOL, V70, P185, DOI 10.1017/S0022336000023283; Gold DA, 2015, EVOL DEV, V17, P315, DOI 10.1111/ede.12168; Hahn G., 1982, Geologica et Palaeontologica, V16, P1; Halverson GP, 2007, PALAEOGEOGR PALAEOCL, V256, P103, DOI 10.1016/j.palaeo.2007.02.028; Halverson GP, 2010, PRECAMBRIAN RES, V182, P337, DOI 10.1016/j.precamres.2010.04.007; Hoffman PF, 2017, SCI ADV, V3, DOI 10.1126/sciadv.1600983; Hoffman PF, 2009, PALAEOGEOGR PALAEOCL, V277, P158, DOI 10.1016/j.palaeo.2009.03.013; Hoffman PF, 1998, SCIENCE, V281, P1342, DOI 10.1126/science.281.5381.1342; Hoffmann KH, 2004, GEOLOGY, V32, P817, DOI 10.1130/G20519.1; Hofmann HJ, 2008, J PALEONTOL, V82, P1, DOI 10.1666/06-087.1; Holland HD, 2006, PHILOS T R SOC B, V361, P903, DOI 10.1098/rstb.2006.1838; HORODYSKI RJ, 1994, SCIENCE, V263, P494, DOI 10.1126/science.263.5146.494; Jahn B, 2001, CHEM GEOL, V178, P143, DOI 10.1016/S0009-2541(01)00264-9; Kendall B, 2006, GEOLOGY, V34, P729, DOI 10.1130/G22775.1; Kirschvink J., 1992, PROTEROZOIC BIOSPHER, P51; Knoll AH, 2000, PALEOBIOLOGY, V26, P1, DOI 10.1666/0094-8373(2000)26[1:DITHOL]2.0.CO;2; Knoll AH, 2017, SCI ADV, V3, DOI 10.1126/sciadv.1603076; Knoll AH, 2014, CSH PERSPECT BIOL, V6, DOI 10.1101/cshperspect.a016121; Kroner A, 2003, TECTONOPHYSICS, V375, P325, DOI 10.1016/S0040-1951(03)00344-5; Laflamme M, 2013, GONDWANA RES, V23, P558, DOI 10.1016/j.gr.2012.11.004; Lahr DJG, 2019, CURR BIOL, V29, P991, DOI 10.1016/j.cub.2019.01.078; Le Heron DP, 2013, SEDIMENTOLOGY, V60, P411, DOI 10.1111/j.1365-3091.2012.01346.x; Lenton TM, 2014, NAT GEOSCI, V7, P257, DOI 10.1038/ngeo2108; Li ZX, 2008, PRECAMBRIAN RES, V160, P179, DOI 10.1016/j.precamres.2007.04.021; Liu PJ, 2014, J PALEONTOL, V88, P1, DOI 10.1666/13-009; Love GD, 2009, NATURE, V457, P718, DOI 10.1038/nature07673; Lyons T. 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J. Geol.		2020	50	2							e20190095	10.1590/2317-4889202020190095	http://dx.doi.org/10.1590/2317-4889202020190095			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MP8AY		gold			2023-06-23	WOS:000552423600001
J	Corecco, L; Pereira, VP; Soares, MB; Schultz, CL				Corecco, Leonardo; Pereira, Vitor Paulo; Soares, Marina Bento; Schultz, Cesar Leandro			Geochemical study of the vertebrate assemblage zones of the Santa Maria Supersequence (Middle to Late Triassic), Parana Basin, Brazil	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						biostratigraphy; paleoclimatology; Gondwana; Carnian Pluvial Episode	SOUTHERN BRAZIL; POTRERILLOS; SEQUENCE; ORIGIN; STRATIGRAPHY; GONDWANA; PROVINCE; MENDOZA; AGE	The Middle-Upper Triassic section of the Parana Basin is included in the Santa Maria Supersequence. This stratigraphic unit is classified as a second-order Supersequence, being subdivided into three third-order sequences in which four Assemblage Zones (AZ) based on tetrapods are recognized. In this work, chemical analyses of fossils and hosting rocks of each AZ were performed in order to verify whether the geochemical patterns of the rocks could serve to distinguish them even in the absence of fossils. For this purpose, nine samples of fossils and their sedimentary matrices were analyzed, by ICP-MS. The results show that there were changes in the chemical parameters in force at the depositional time of each sequence (and corresponding AZ). In general, the lower portion of the package was deposited under more basic and dry environmental conditions, indicated by the Ca and Ba concentrations found in the rocks and bones that contains them. By its turn, the top of the section is characterized by more acid and humid conditions, evidenced by Al, Si, and Sr increase. Such a geochemical shift from dry to humid conditions occurred just at the beginning of the Late Triassic and is probably related to the Carnian Pluvial Episode.	[Corecco, Leonardo; Soares, Marina Bento; Schultz, Cesar Leandro] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Inst Geociencias, Porto Alegre, RS, Brazil; [Pereira, Vitor Paulo] Univ Fed Rio Grande do Sul, Dept Mineral & Petrol, Inst Geociencias, Porto Alegre, RS, Brazil; [Soares, Marina Bento] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, Rio De Janeiro, RJ, Brazil; [Schultz, Cesar Leandro] Univ Fed Rio Grande do Sul, Dept Paleontol & Estratig, Inst Geociencias, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio Grande do Sul	Corecco, L (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Inst Geociencias, Porto Alegre, RS, Brazil.	leocorecco@gmail.com; vitor.pereira@ufrgs.br; marina.soares@mn.ufrj.br; cesar.schultz@ufrgs.br	Pereira, Vitor Paulo/X-6185-2018	Pereira, Vitor Paulo/0000-0001-5875-2115; Corecco de Queiroz, Leonardo/0000-0001-9353-1211	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [001]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [476868/2010-6]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This work is the end product of L. Corecco's Master's degree dissertation by the Programa de Pos-graduacao em Geociencias, of Instituto de Geociencias, at Universidade Federal do Rio Grande do Sul. This study was financed, in part, by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -Finance Code 001, granting the scholarship for this student and, in part, by research project No. 476868/2010-6 attached to the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq), led by Dra. Marina Bento Soares. We also thank professors Paulo Alves de Souza and Claiton Marlon dos Santos Scherer; PhDs Bruno Ludovico Dihl Horn and Heitor Roberto Dias Francischini, as well as to the doctoral students Mauricio Rodrigo Schmitt, Francesco Battista, Voltaire Dutra Paes Neto, and Tomaz Panceri Melo for their helpful discussions about the theme.	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J. Geol.		2020	50	4							e20200014	10.1590/2317-4889202020200014	http://dx.doi.org/10.1590/2317-4889202020200014			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QF2CQ		gold			2023-06-23	WOS:000616707400001
J	da Silva, AS; Feio, GRL; Alves, JPS; Dall'Agnol, R; de Almeida, JDC; Gomes, ACB				da Silva, Arthur Santos; Lima Feio, Gilmara Regina; Silva Alves, Joao Paulo; Dall'Agnol, Roberto; Costa de Almeida, Jose de Arimateia; Brunelli Gomes, Allan Cardek			Mineralogy, petrology, and origin of the Pedra Branca Suite: a tonalitic-trondhjemitic association with high Zr, Ti and Y, Carajas Province, Amazonian Craton	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Petrogenesis; Pedra Branca Suite; Carajas Province; Neoarchean	U-PB GEOCHRONOLOGY; A-TYPE; EXPERIMENTAL CALIBRATION; EXPERIMENTAL CONSTRAINTS; BRAZIL IMPLICATIONS; CRUSTAL EVOLUTION; GRANODIORITE TTG; GEOCHEMISTRY; HORNBLENDE; GRANITE	The Pedra Branca suite (2.75 Ga) is located in the Canaa dos Carajas domain in the southeastern Amazonia Craton. It diverges from typical TTG in mineralogical and geochemical terms, by the presence of hornblende and clinopyroxene and because it has a high content of HFSE (Zr, Y, Ti, and Nb). It belongs to the low-K subalkaline series, which varies from metaluminous to peraluminous, and are mostly calc and ferroan granitoids. Amphibole is calcic and classified as ferroan-edenite, and hastingsite. Plagioclase is mainly oligoclase. The Fe/(Fe + Mg) ratios found in the amphiboles indicate that these granitoids were formed under high to moderate fO(2) conditions. Geobarometric calculations suggest pressures between 9.3 and 71 Kbar for the origin and 4.8-53.4 Kbar for the emplacement. Geothermometric calculations suggest initial crystallization temperatures between 945 and 862 degrees C, and the water content in the magma is estimated to be higher than 4 wt%. The magma source was defined as tholeiitic continental gabbro melted in an extensional setting (Carajas Rift) with geochemical features similar to diabase from Nova Canada (PA). The Pedra Branca magma was originated by partial melting (similar to 28%), leaving a residue with plagioclase (An40), hornblende, clinopyroxene, and may or may not have magnetite.	[da Silva, Arthur Santos] Univ Brasilia, Brasilia, DF, Brazil; [Lima Feio, Gilmara Regina; Costa de Almeida, Jose de Arimateia] Univ Fed Sul & Sudeste Para, Maraba, PA, Brazil; [Silva Alves, Joao Paulo; Brunelli Gomes, Allan Cardek] Univ Fed Para, Belem, Para, Brazil; [Dall'Agnol, Roberto] Inst Tecnol Vale, Belem, Para, Brazil	Universidade de Brasilia; Universidade Federal do Sul e Sudeste do Para; Universidade Federal do Para; Instituto Tecnologico Vale Desenvolvimento Sustentavel	da Silva, AS (autor correspondente), Univ Brasilia, Brasilia, DF, Brazil.	santos_arthur@hotmail.com; gilmarafeio@unifesspa.edu.br; joao.p-17@hotmail.com; robdal@ufpa.br; ari@unifesspa.edu.br; alanbrunelli@gmail.com	Feio, Gilmara Regina Lima/ABF-5668-2020	De Almeida, Jose de Arimateia Costa/0000-0002-5128-3026; Silva Alves, Joao Paulo/0000-0002-6258-6479; Feio, Gilmara/0000-0001-8523-6693; Santos da Silva Neri, Arthur/0000-0002-8363-4476	CNPq [0550739/2001-7, 476075/2003-3, 307469/2003-4, 484524/2007-0, 66.2103/1998-0]; Universidade do Sul e Sudeste do Para (Unifesspa)	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Universidade do Sul e Sudeste do Para (Unifesspa)	The Grupo de Petrologia de Granitoides from Universidade Federal do Para are acknowledged for their support in geological mapping and previous works in the studied area. M.J James is acknowledged for her support in writing, and P.V.F.S Alves for helping with the EPMA analysis. The reviews by Silvio RF Vlach, an anonymous reviewer, and the editorial handling of C. Ricominni were greatly appreciated and helped to improve the original manuscript. This research received financial support from CNPq (R. Dall'Agnol -Grants 0550739/2001-7, 476075/2003-3, 307469/2003-4, 484524/2007-0; PRONEX Proc. 66.2103/1998-0; G.R.L Feio -CNPq scholarship), and Universidade do Sul e Sudeste do Para (Unifesspa).	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J	da Silva, OB; Raposo, MIB				da Silva, Odirney Benedito; Raposo, Maria Irene B.			Emplacement of the Anta Granite from Rio de Janeiro State (SE, Brazil); determined by magnetic fabrics	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Magnetic Fabrics: anisotropy of low-field magnetic susceptibility; anisotropy of anhysteretic remanent magnetization; granite; Anta; Rio de Janeiro	PARTIAL ANHYSTERETIC REMANENCE; WESTERN GONDWANA; RIBEIRA BELT; MAGMATIC ARC; SUSCEPTIBILITY; PLUTON; ROCKS; ANISOTROPIES; EVOLUTION; GEOCHRONOLOGY	Magnetic fabric and rock magnetism studies were performed on the three facies of the Anta granite (SE of Rio de Janeiro State, southern Brazil). This intrusion is roughly elliptical (similar to 14 km(2)), NE-SW oriented and composed of granodiorite, monzodiorite, quartz-diorite, syenogranite, and monzogranite. It shows solid-state deformation and tectonic foliation at its borders and is apparently isotropic in the central part where the internal fabrics are impossible or very difficult to measure through classical techniques. Magnetic fabrics were determined by applying both anisotropy of low-field magnetic susceptibility (AMS) and anisotropy of anhysteretic remanent magnetization (AARM). The AMS and AARM fabrics are coaxial for all facies. The parallelism between AMS and AARM tensors excludes the presence of a single domain (SD) effect in the AMS fabric. Several rock-magnetism experiments performed on one specimen from each facies show that, for all units, magnetic susceptibility and fabrics are carried by magnetite grains. Most of the magnetic foliations are steeply dipping in all facies, and are roughly parallel or sub-parallel to the foliation measured in the field and in the country rocks. In contrast, the magnetic lineations present mostly low plunges for almost the whole pluton, except for one site where it is steep (> 60 degrees). Thin section analysis show that rocks from the borders of the Anta pluton are solid-state deformed, indicating that the borders of the pluton were affected by the regional strain during its emplacement. On the other hand, the lack of solid-state deformation at outcrop scale and in thin sections precludes deformation in the central part of the pluton to be determined, where igneous textures are preserved. This evidence allows us to interpret the magnetic fabrics observed in this part of the pluton as primary in origin (magmatic) and acquired when the rocks were solidified as a result of magma flow, in which steeply plunging magnetic lineation suggests that a feeder zone could underlain this area. Our data suggest that the regional deformation partially affected the emplacement of the Anta granite.	[da Silva, Odirney Benedito; Raposo, Maria Irene B.] Univ Sao Paulo, Inst Geociencias, Sao Paulo, SP, Brazil	Universidade de Sao Paulo	Raposo, MIB (autor correspondente), Univ Sao Paulo, Inst Geociencias, Sao Paulo, SP, Brazil.	obsilva@usp.br; irene@usp.br	Raposo, M. Irene B./D-6896-2013	Benedito da Silva, Odirney/0000-0002-2005-2284; Raposo, Maria Irene Bartolomeu/0000-0002-8300-7480	FAPESP [17/01120-0]; CNPq [134419/2016-2]	FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank FAPESP (17/01120-0 grant), Brazilian agency, for its financial support. Odirney Benedito da Silva thanks CNPq (Brazilian agency) for Msc scholarship (134419/2016-2 grant). We also, thank Emilio L. Pueyo and Wentian Liang, whose comments greatly improved the manuscript.	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J. Geol.		2020	50	4							e20200007	10.1590/2317-4889202020200007	http://dx.doi.org/10.1590/2317-4889202020200007			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QF2CE		gold			2023-06-23	WOS:000616706200001
J	da Silva, TR; Ferreira, VP; de Lima, MMC; Sial, AN				da Silva, Thyego Roberto; Ferreira, Valderez Pinto; Correia de Lima, Mariucha Maria; Sial, Alcides Nobrega			Rapid magma ascent and formation of the Aguas Belas-Caninde granitic batholith, NE Brazil: evidence of epidote dissolution and thermobarometry	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Pernambuco-Alagoas Domain; calc-alkaline orogenic granites; crystallization conditions; magmatic epidote; high ascension rates	PERNAMBUCO-ALAGOAS DOMAIN; K CALC-ALKALINE; INTERNATIONAL-MINERALOGICAL-ASSOCIATION; PERVASIVE MELT MIGRATION; BORBOREMA PROVINCE; CRYSTALLIZATION CONDITIONS; EXPERIMENTAL CALIBRATION; ISOTOPE COMPOSITIONS; BEARING MAGMAS; SHEAR ZONE	Mineral chemistry and intensive parameter estimates for the Major Isidoro (626 Ma) and Monteiropolis (627 Ma) magmatic epidote-bearing granitic plutons, emplaced along the Jacare dos Homens transpressional shear zone ( JHSZ), Borborema Province, are focused in this study. These plutons consist of medium-to-coarse grained equigranular to porphyritic tonalite to granite that show abundant dioritic enclaves. These granites contain biotite (Fe# 0.44 to 0.55), Fe-edenite (Major Isidoro), hastingsite (Monteiropolis), titanite, and epidote that often show allanite core as key mafic mineral phases. Pistacite molecular content in epidote is in the interval of 27 to 31 mol%, presenting TiO2 < 0.30%, typical for magmatic epidote. Estimated intensive parameters reveal crystallization at 6.5 +/- 1 (Major Isidoro) and 4.7 +/- 0.6 kbar (Monteiropolis), temperatures from similar to 940 degrees C (near-liquidus) to 675 +/- 35 degrees C (near-solidus) and oxidizing conditions. Partial corrosion of epidote took place during 15.6 to 32 (Major Isidoro) and 27-49 years (Monteiropolis), corresponding to rather high magma ascension rates of 365 to 750 and 395 to 635 m.years(-1), respectively. The JHSZ likely favored upward magma transport at the Sergipano and Pernambuco-Alagoas domains boundary, during the onset of the Brasiliano orogeny (650-620 Ma).	[da Silva, Thyego Roberto; Ferreira, Valderez Pinto; Correia de Lima, Mariucha Maria; Sial, Alcides Nobrega] Univ Fed Pernambuco, Recife, PE, Brazil	Universidade Federal de Pernambuco	da Silva, TR (autor correspondente), Univ Fed Pernambuco, Recife, PE, Brazil.	rthyego@yahoo.com; valderez.ferreira@ufpe.br; mariucha_geo@yahoo.com.br; alcides.sial@ufpe.br	Sial, Alcides/AAD-1901-2021; Silva, Thyego/ABC-2905-2020	Silva, Thyego/0000-0002-4072-9643; Lima, Mariucha/0000-0003-4169-2712; Ferreira, Valderez/0000-0003-3220-7113	CNPq [471034/2012-6]; FACEPE [APQ-1738-1.07/12]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FACEPE(Fundacao de Amparo a Ciencia e Tecnologia do Estado de Pernambuco (FACEPE))	We thank Edward Sawyer for discussions on the geology of the Major Isidoro pluton. Nilson M. Botelho is thanked for mineral chemistry laboratory facilities. We are grateful to Bruna Maria Borba de Carvalho for the acquisition of mineral chemistry at the Electron Microprobe Laboratory in the Universidade de Brasilia, Brazil, and Anderson de Abreu da Silva for the XRF chemical analyses at the Stable Isotope Laboratory (LABISE) in the Universidade Federal de Pernambuco, Brazil. Comments on drafts and revised versions of the manuscript by Maia de Lourdes, Anelise Bertoti, Julio Mendes, and Adejardo da Silva Filho, as members of Silva's thesis committee, are acknowledged. We are grateful to Claudio Ricomini, Chief Editor, for careful editorial handling, and especially to Olivier Vanderhaeghe, Silvio Vlach, and an anonymous reviewer for their positive, critical, and constructive comments, which greatly contribute to improve the paper. Obviously, any errors or omissions are solely the responsibility of the authors. VPF and ANS acknowledge the continuous financial support from the CNPq (process number 471034/2012-6) and FACEPE (process APQ-1738-1.07/12). This is the NEG-LABISE contribution n. 293.	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J. Geol.		2020	50	2							e20190110	10.1590/2317-4889202020190110	http://dx.doi.org/10.1590/2317-4889202020190110			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QF1ZN		Green Published, gold			2023-06-23	WOS:000616699300001
J	Danchana, K; Phansi, P; de Souza, CT; Ferreira, SLC; Cerda, V				Danchana, Kaewta; Phansi, Piyawan; de Souza, Cheilane T.; Ferreira, Sergio L. C.; Cerda, Victor			Spectrophotometric system based on a device created by 3D printing for the accommodation of a webcam chamber as a detection system	TALANTA			English	Article							MOBILE PHONE; SMARTPHONE; PLATFORM; O-2	The development of a simple and economical spectrophotometric system based on the use of a device created by 3D printing and the electronics necessary to control the intensity of the radiation source was described. The measurements are made with a low-cost digital webcam. The entire system is only powered through the USB outputs of a computer, which makes the portable and really practical system for the measurements in the field. This method was applied to determine iron (II) in waters using o-phenanthroline as chromogenic reagent giving a red complex, and also to hypochlorite determination using tetramethylbenzidine as the reagent providing a yellow color. The calibration curves were built using a mathematical algorithm making a RGB deconvolution. The intense of colors obtained from a webcam in each concentration of analyte had a relationship with the absorbance values. In order to confirm the accuracy and precision of this method, a traditional spectrophotometer was used for validation.	[Danchana, Kaewta; Cerda, Victor] Sciware Syst, Bunyola 07193, Spain; [Phansi, Piyawan] Thepsatri Rajabhat Univ, Dept Chem, Lopburi 15000, Thailand; [de Souza, Cheilane T.; Ferreira, Sergio L. C.] Univ Fed Bahia, Inst Quim, BR-40170290 Salvador, BA, Brazil; [Cerda, Victor] Univ Illes Balears, Dept Quim, Palma de Mallorca 07122, Spain	Thepsatri Rajabhat University; Universidade Federal da Bahia; Universitat de les Illes Balears	Cerda, V (autor correspondente), Sciware Syst, Bunyola 07193, Spain.	victor.cerda@uib.es	FERREIRA, SERGIO LUIS SLCF COSTA/I-1993-2013	FERREIRA, SERGIO LUIS SLCF COSTA/0000-0001-7738-045X; Danchana, Kaewta/0000-0002-4059-5534	Spanish Ministry of Economy and Competitiveness (MINECO) [CTQ-2016-77155-R]; FEDER funds; Conselleria d'Innovacio, Recerca I Turisme of the Govern de les Illes Balears; Fons Social Europea [FPI/1867/2016]; Thepsatri Rajabhat University	Spanish Ministry of Economy and Competitiveness (MINECO)(Spanish Government); FEDER funds(European Commission); Conselleria d'Innovacio, Recerca I Turisme of the Govern de les Illes Balears; Fons Social Europea; Thepsatri Rajabhat University	The authors acknowledge financial support from Spanish Ministry of Economy and Competitiveness (MINECO) through Project CTQ-2016-77155-R co-financed by FEDER funds. Kaewta Danchana acknowledges the financial support from the Conselleria d'Innovacio, Recerca I Turisme of the Govern de les Illes Balears and of the Fons Social Europea (FPI/1867/2016). The financial support from Thepsatri Rajabhat University for P. Phansi is gratefully acknowledged.	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J	Daneluz, J; Favero, JD; dos Santos, V; Weiss-Angeli, V; Gomes, LB; Mexias, AS; Bergmann, CP				Daneluz, Julia; Favero, Juliana da Silva; dos Santos, Venina; Weiss-Angeli, Valeria; Gomes, Lucas Bonan; Mexias, Andre Sampaio; Bergmann, Carlos Perez			The Influence of Different Concentrations of a Natural Clay Material as Active Principle in Cosmetic Formulations	MATERIALS RESEARCH-IBERO-AMERICAN JOURNAL OF MATERIALS			English	Article						clay minerals; cosmetics; formulation; gel	RAW-MATERIALS; MINERALS; HEALTH; FTIR	The clay minerals have characteristics and properties that allow their applicability in the cosmetic area, being incorporated into formulations as an active principle. Therefore, the aim of this work is characterizing and evaluating the influence of a clay from Miracema do Norte, Tocantins, Brazil, named Clay V, on the physicochemical characteristics of a hydrophilic gel of Aristoflex (R), a copolymer of the neutralized acryloyldimethyltaurate and vinylpyrrolidone sulphonic acid. Clay V was decontaminated and characterized through microbiological evaluation, crystalline phases present by X-Ray Diffraction (XRD), chemical composition by X-Ray Fluorescence (XRF), thermogravimetric analysis (TGA) and granulometric distribution by sieving. Gels were prepared using Clay V with particles in the range <= 180 mu m in three different concentrations: 1%, 3% and 5% (w/w) and a standard gel without clay. The formulations were evaluated according to organoleptic characteristics, pH, viscosity, spreadability and the centrifugation test. The microbiological evaluation showed that the clay sample is in compliance with the parameters established by the legislation. The following mineral phases were identified by XRD: kaolinite, illite, vermiculite and quartz, mainly composed of silica and alumina according to XRF. Thermal analysis showed that the clay has two thermal decomposition reactions, the largest being 547.6 degrees C. The granulometric analysis identified that the largest fraction (63.22%) was of particles with sizes greater than 710 mu m. The organoleptic characteristics presented by the formulations were suitable, with characteristic gel odor, homogeneous appearance, soft and refreshing texture and staining based on the concentration of Clay V used. The obtained pH values were within the range between 5.5 and 6.5, and it was verified that the gel has high spreadability, distributing evenly on the skin. The values obtained for viscosity showed that the formulations are non-Newtonian fluids with pseudoplastic behavior. The centrifugation test showed that the formulations are stable, with no phase separation. The results obtained with the tests showed that the natural clay V material is beneficial in cosmetic products and can be used for incorporation in cosmetic gel formulations of Aristoflex (R) type.	[Daneluz, Julia; Favero, Juliana da Silva; dos Santos, Venina; Weiss-Angeli, Valeria] Univ Caxias do Sul UCS, Rua Francisco Getulio Vargas 1130, BR-95070560 Caxias Do Sul, RS, Brazil; [Gomes, Lucas Bonan; Mexias, Andre Sampaio; Bergmann, Carlos Perez] Univ Fed Rio Grande do Sul UFRGS, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil	Universidade de Caxias do Sul; Universidade Federal do Rio Grande do Sul	Favero, JD (autor correspondente), Univ Caxias do Sul UCS, Rua Francisco Getulio Vargas 1130, BR-95070560 Caxias Do Sul, RS, Brazil.	vsantos2@ucs.br	Daneluz, Júlia/IAO-2637-2023; Bergmann, Carlos P Pérez/F-2225-2010	Daneluz, Júlia/0009-0003-7226-6385; Bergmann, Carlos P Pérez/0000-0002-8951-8943; Bonan Gomes, Lucas/0000-0003-4332-9212; dos Santos, Venina/0000-0002-6344-8094	Research Support Foundation of the Rio Grande do Sul State (FAPERGS); University of Caxias do Sul (UCS); Federal University of Rio Grande do Sul (UFRGS)	Research Support Foundation of the Rio Grande do Sul State (FAPERGS)(Fundacao de Amparo a Ciencia e Tecnologia do Estado do Rio Grande do Sul (FAPERGS)); University of Caxias do Sul (UCS); Federal University of Rio Grande do Sul (UFRGS)	Authors are beholden to the University of Caxias do Sul (UCS), to Federal University of Rio Grande do Sul (UFRGS) and to the Research Support Foundation of the Rio Grande do Sul State (FAPERGS) for financial support.	Akyuz S, 2008, VIB SPECTROSC, V48, P276, DOI 10.1016/j.vibspec.2008.02.011; [Anonymous], 2008, BRIT PHARMACOPEIA; ASTM: American Society for Testing Materials, 2008, D734808 ASTM; Baranova II, 2017, ASIAN J PHARM, V11, pS302; Bergaya F, 2006, DEV CLAY SCI, V1, P1, DOI 10.1016/S1572-4352(05)01001-9; Boulingui JE, 2015, APPL CLAY SCI, V115, P132, DOI 10.1016/j.clay.2015.07.029; Buhse L, 2005, INT J PHARM, V295, P101, DOI 10.1016/j.ijpharm.2005.01.032; Carretero MI, 2014, APPL CLAY SCI, V99, P131, DOI 10.1016/j.clay.2014.06.022; Carretero MI, 2007, APPL CLAY SCI, V36, P1, DOI 10.1016/j.clay.2006.09.001; Carretero MI, 2002, APPL CLAY SCI, V21, P155, DOI 10.1016/S0169-1317(01)00085-0; Chmielarz L, 2012, CATAL TODAY, V191, P25, DOI 10.1016/j.cattod.2012.03.042; Dario GM, 2014, MAT SCI ENG C-MATER, V43, P109, DOI 10.1016/j.msec.2014.06.024; Davis HM, 1977, NEWBURGERS MANUAL CO, p[1977, 32]; Moraes JDD, 2017, INT J PHARMACEUT, V534, P213, DOI 10.1016/j.ijpharm.2017.10.031; Dontsova KM, 2004, SOIL SCI SOC AM J, V68, P1218, DOI 10.2136/sssaj2004.1218; Estanqueiro M, 2016, INT J COSMETIC SCI, V38, P389, DOI 10.1111/ics.12302; Fairclough JPA, 2003, ANN RP CH C, V99, P243, DOI 10.1039/b208503h; Favero JD, 2016, APPL CLAY SCI, V124, P252, DOI 10.1016/j.clay.2016.02.022; Gomes CDF, 2007, APPL CLAY SCI, V36, P4, DOI 10.1016/j.clay.2006.08.006; Frost RL, 2006, J COLLOID INTERF SCI, V294, P47, DOI 10.1016/j.jcis.2005.07.014; Hammami-Ben Zaied F, 2015, APPL CLAY SCI, V112, P1, DOI 10.1016/j.clay.2015.03.027; Hong EJ, 2016, FOOD MICROBIOL, V53, P9, DOI 10.1016/j.fm.2015.08.002; Carretero MI, 2010, APPL CLAY SCI, V47, P171, DOI 10.1016/j.clay.2009.10.016; Carretero MI, 2009, APPL CLAY SCI, V46, P73, DOI 10.1016/j.clay.2009.07.017; Khiari I, 2014, APPL CLAY SCI, V101, P141, DOI 10.1016/j.clay.2014.07.029; Knorst M.T., 1991, THESIS U FEDERAL RIO; Lange MK, 2009, BRAZ J PHARM SCI, V45, P145, DOI 10.1590/S1984-82502009000100018; Leal LB, 2013, BRAZ J PHARM SCI, V49, P167, DOI 10.1590/S1984-82502013000100018; Lopez-Galindo A, 2007, APPL CLAY SCI, V36, P51, DOI 10.1016/j.clay.2006.06.016; Madejova J, 2003, VIB SPECTROSC, V31, P1, DOI 10.1016/S0924-2031(02)00065-6; Mako E, 2006, J COLLOID INTERF SCI, V294, P362, DOI 10.1016/j.jcis.2005.07.033; Mattioli M, 2016, APPL CLAY SCI, V119, P449, DOI 10.1016/j.clay.2015.10.023; Modabberi S, 2015, APPL CLAY SCI, V116, P193, DOI 10.1016/j.clay.2015.03.013; OINUMA K, 1965, AM MINERAL, V50, P1213; Poensin D, 2003, JOINT BONE SPINE, V70, P367, DOI 10.1016/S1297-319X(03)00064-2; Qtaitat MA, 2005, SPECTROCHIM ACTA A, V61, P1519, DOI 10.1016/j.saa.2004.11.008; Ritz M, 2014, VIB SPECTROSC, V70, P63, DOI 10.1016/j.vibspec.2013.11.007; Sax H, 2009, AM J INFECT CONTROL, V37, P827, DOI 10.1016/j.ajic.2009.07.003; Silva PSC, 2011, APPL CLAY SCI, V52, P145, DOI 10.1016/j.clay.2011.02.013; Viseras C, 2007, APPL CLAY SCI, V36, P37, DOI 10.1016/j.clay.2006.07.006; Viseras C., 2006, APPL CLAY SCI, V31, P272, DOI DOI 10.1016/J.CLAY.2005.11.002; Weiss-Angeli V, 2008, J BIOMED NANOTECHNOL, V4, P80, DOI 10.1166/jbn.2008.004; WHO: World Health Organization, 2008, CRYST SIL QUARTZ; Worasith N, 2011, CLAY MINER, V46, P539, DOI 10.1180/claymin.2011.046.4.539; Zhang D, 2010, APPL CLAY SCI, V50, P1, DOI 10.1016/j.clay.2010.06.019	45	5	5	2	11	UNIV FED SAO CARLOS, DEPT ENGENHARIA MATERIALS	SAO CARLOS	LABORATORIA DE MATERIAIS VITREOS, CAIXA POSTAL 676, SAO CARLOS, 13565-905SP, BRAZIL	1516-1439	1980-5373		MATER RES-IBERO-AM J	Mater. Res.-Ibero-am. J. Mater.		2020	23	2							e20190572	10.1590/1980-5373-MR-2019-0572	http://dx.doi.org/10.1590/1980-5373-MR-2019-0572			11	Materials Science, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Materials Science	LV4GE		gold, Green Published			2023-06-23	WOS:000538395000001
J	Souza, IMBAE; Guimaraes, ID; Barreto, SD; Santos, GL; Neto, JFD				de Albuquerque e Souza, Igor Manoel Belo; Guimaraes, Ignez de Pinho; Barreto, Sandra de Brito; Santos, Glenda Lira; de Araujo Neto, Jose Ferreira			Whole-rock and mineral chemistry characterization of contrasting granitoids, constraints on the source of the Vieiropolis NYF-type pegmatites, Northeastern Brazil	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Serra Branca amazonite pegmatite; NYF-type pegmatite; mineral chemistry; crystallization conditions; whole-rock geochemistry	EASTERN BORBOREMA PROVINCE; AMAZONITIC K-FELDSPAR; NE BRAZIL; TRACE-ELEMENT; EXPERIMENTAL CALIBRATION; ZIRCON SATURATION; CALCIC AMPHIBOLE; SHEAR ZONE; HORNBLENDE; AL	The Vieiropolis pegmatite field is characterized by amazonite pegmatites inserted in the Borborema Province. The Serra Branca pegmatite is hosted by the Serra Branca granites, which intruded partially the Serra Negra granites, and stands out by its amazonite mineralization. To comprehend the crystallization conditions and the source of this pegmatite and associated Serra Branca and Serra Negra granites, petrographic, mineral chemistry, geochronological and whole-rock geochemical data were used. The Serra Branca pegmatite is Cs-, Rb-, Pb-, Nb-, and Ta-rich. The Serra Branca granites (563 +/- 2 Ma) are metaluminous to weakly peraluminous, crystallized under high fO(2) conditions, pressure of 2.68-2.80 kbar and temperatures ranging from 667-670 degrees C, with many zircon grains showing inherited cores of Paleoproterozoic ages. The Serra Negra granites (594 +/- 4 Ma) comprises metaluminous granites crystallized under high fO(2) conditions, temperatures within 711-751 degrees C, pressure varying from 4.72 to 5.42 kbar. Both granites resulted from distinct partial melting degrees of a source similar to the Caico Complex orthogneisses. The Serra Branca pegmatite geochemical data suggests that it was originated by extreme fractionation of the Serra Branca granites magma. The Serra Branca amazonite pegmatite is the first pegmatite mineralogically and geochemically characterized as Nb-Y-F (NYF)-type from the gadolinite subtype in the Borborema Province.	[de Albuquerque e Souza, Igor Manoel Belo; Guimaraes, Ignez de Pinho; Barreto, Sandra de Brito; Santos, Glenda Lira; de Araujo Neto, Jose Ferreira] Univ Fed Pernambuco, Recife, PE, Brazil	Universidade Federal de Pernambuco	Souza, IMBAE (autor correspondente), Univ Fed Pernambuco, Recife, PE, Brazil.	igor.manoel.belopg@mail.com; ignez@ufpe.br; sandradebritobarreto@gmail.com; glendaliraa@gmail.com; araujoneto.geopg@mail.com	Barreto, Sandra/AAI-5380-2021; Santos, Glenda/AAY-6364-2020	Santos, Glenda/0000-0002-6271-950X; Barreto, Sandra/0000-0001-8464-7087; Belo de Albuquerque e Souza, Igor Manoel/0000-0002-2235-5668; Araujo Neto, Jose Ferreira de/0000-0002-1780-9469	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	We are grateful to the GRANISTONE S/A company for providing support to our research and for the supply of pegmatite samples. We also thank the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) for scholarships granted to Igor Manoel Belo de Albuquerque e Souza, Glenda Lira Santos and Jose Ferreira de Araujo Neto. We would like to express our gratitude to Dr. Axel Muller for his general assistance with this research. We also thank Professor Dr. Nilson Botelho (Universidade de Brasilia, Brazil) for the electron microprobe analysis.	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A., 2017, NGF ABSTRACTS P, V2, P177; Wise M.A., 1999, CAN MINERAL, V37, P802; WONES DR, 1989, AM MINERAL, V74, P744	94	1	1	4	5	SOC BRASILEIRA GEOLOGIA	SAO PAULO	CAIXA POSTAL 11348, SAO PAULO, SP 05422-970, BRAZIL	2317-4889	2317-4692		BRAZ J GEOL	Braz. J. Geol.		2020	50	2							e20190083	10.1590/2317-4889202020190083	http://dx.doi.org/10.1590/2317-4889202020190083			23	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MP8AR		gold			2023-06-23	WOS:000552422900001
J	de Andrade, LC; Oliveira, EV; Mothe, D; Maniesi, V				de Andrade, Luana Cardoso; Oliveira, Edison Vicente; Mothe, Dimila; Maniesi, Vanderlei			NEW RECORD OF AN IMMATURE NOTIOMASTODON CF. PLATENSIS (MAMMALIA, PROBOSCIDEA) FROM PERNAMBUCO STATE, NORTHEASTERN BRAZIL	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						South America; Quaternary; Proboscidea; immature; tank deposit	GOMPHOTHERIIDAE	Proboscideans are megamammals widely recorded in South America Quaternary deposits, especially in Brazil, where many specimens are found in tanks and caves. In tank deposits, the fossil remains are usually recognized as adult individuals, although highly and usually fragmented. The records of immature proboscideans are rare, consisting of isolated teeth and jaw fragments, especially from tank deposits. Here we describe a new and rare occurrence of an immature proboscidean - a second upper left deciduous premolar (DP2) of Notiomastodon cf. N. platensis - from Pernambuco State, Brazil. This record increases the number of immature individuals known for Notiomastodon in Brazil, contributes to the understanding of the frequency of immature individuals in tank deposits, and increases Notiomastodon geographic distribution in South America.	[de Andrade, Luana Cardoso; Oliveira, Edison Vicente] Univ Fed Pernambuco, Programa Posgrad Geociencias, Dept Geol, Lab Paleontol, Av Acad Helio Ramos S-N,Cidade Univ, BR-50740530 Recife, PE, Brazil; [Mothe, Dimila] Univ Fed Estado Rio de Janeiro, Inst Biociencias, Lab Mastozool, Av Pasteur 458,Sala 501, BR-22290240 Rio De Janeiro, RJ, Brazil; [Mothe, Dimila] Univ Fed Rio de Janeiro, Programa Posgrad Biodiversidade & Biol Evolut, Ctr Ciencias Saude, Av Carlos Chagas Filho 373,Cidade Univ, Rio De Janeiro, RJ, Brazil; [Maniesi, Vanderlei] Univ Fed Rondonia, Grp Pesquisa Geociencias, Dept Geog, Av Presidente Dutra 2965, BR-76801974 Porto Velho, Rondonia, Brazil	Universidade Federal de Pernambuco; Universidade Federal do Estado do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal de Rondonia	de Andrade, LC (autor correspondente), Univ Fed Pernambuco, Programa Posgrad Geociencias, Dept Geol, Lab Paleontol, Av Acad Helio Ramos S-N,Cidade Univ, BR-50740530 Recife, PE, Brazil.	luanacardosodeandrade@gmail.com; vicenteedi@gmail.com; dimothe@hotmail.com; maniesi@unir.br	Oliveira, Édison Vicente/A-8427-2011; Mothé, Dimila/ABE-8262-2020	Mothé, Dimila/0000-0002-4073-5963; Andrade, Luana/0000-0001-7529-5956; Maniesi, Vanderlei/0000-0003-0369-6069; Oliveira, Edison/0000-0001-6634-5480	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) [202.375/2018, 202.376/2018]; Department of Culture of the Capoeiras city (PE)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ)(Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio De Janeiro (FAPERJ)); Department of Culture of the Capoeiras city (PE)	This study was funded by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), and Fundacao Carlos Chagas Filho de Amparo a Pesquisa do Estado do Rio de Janeiro (FAPERJ) for the Post-doctoral scholarship 202.375/2018 and 202.376/2018 of author D.M. The authors thank the City council and the Department of Culture of the Capoeiras city (PE) for the support and the PaleoLab/UFPE paleontology team for the assistance during fieldwork. The authors thank the ICESI University (Cali, Colombia) for allowing access to the fossil collection. The authors thank the anonymous reviewer and editor who made important contributions to this work.	Alves R. S., 2007, ESTUDOS GEOLOGICOS, V17, P114; Araujo E, 2017, IEEE INT C BIOINF BI, P175, DOI 10.1109/BIBE.2017.00036; AraujoJunior H.I., 2017, ANUARIO I GEOCIANCIA, V40, P37; Cartelle C, 1992, THESIS U FEDERAL MIN; Castellanos A., 1948, NEY VIDAL CONTRIBUIC, P138; Dantas Mario Andre Trindade, 2007, Revista Universidade de Guarulhos Geociencias, V6, P191; de Araujo HI, 2015, PALAEOGEOGR PALAEOCL, V437, P1, DOI 10.1016/j.palaeo.2015.07.009; de Araujo HI, 2013, QUATERN INT, V317, P88, DOI 10.1016/j.quaint.2013.08.016; de Araujo HI, 2013, PALAEOGEOGR PALAEOCL, V378, P52, DOI 10.1016/j.palaeo.2013.04.001; Ferretti MP, 2008, J MAMM EVOL, V15, P37, DOI 10.1007/s10914-007-9057-3; Green JL, 2005, J VERTEBR PALEONTOL, V25, P702, DOI 10.1671/0272-4634(2005)025[0702:TDPOMA]2.0.CO;2; Holz M., 2002, ELEMENTOS FUNDAMENTA; Liendo- Lazarte M., 1946, ALGUNAS CONSIDERACIO; Lucas SG, 2013, J PALAEOGEOG-ENGLISH, V2, P19, DOI 10.3724/SP.J.1261.2013.00015; Moss Cynthia, 1996, P58; Mothe D., 2010, MONOGRAFIA; Mothe D, 2017, QUATERN INT, V443, P52, DOI 10.1016/j.quaint.2016.08.028; Mothe D, 2016, PLOS ONE, V11, DOI 10.1371/journal.pone.0147009; Mothe D, 2015, QUATERNARY SCI REV, V110, P23, DOI 10.1016/j.quascirev.2014.12.013; Mothe D, 2013, J MAMM EVOL, V20, P23, DOI 10.1007/s10914-012-9192-3; Mothe D, 2012, QUATERN INT, V276, P2, DOI 10.1016/j.quaint.2011.05.018; Rolim J.L., 1974, Anais Acad Bras Cienc, V46, P417; Rolim J.L., 1974, THESIS; Silva F.M., 2010, QUATERNARY ENV GEOSC, V2, P1, DOI [10.5380/adequa.v2il-2.14182, DOI 10.5380/ABEQUA.V2I1-2.14182]; Simpson G.G., 1957, B AM MUS NAT HIST, V112, P1; Tassy P, 1996, RECHERCHE, P26; Vaughan T.A., 2000, MAMMALOGY; Vidal N., 1946, Boletim Mus Nacional Brasil Rio de Janeiro, V6, P1; Wiest LA, 2016, PALAIOS, V31, P592, DOI 10.2110/palo.2016.053	29	2	2	0	2	SOC BRASILEIRA PALEONTOLOGIA	SAO LEOPOLDO	PPGEO UNISINOS, AV UNISINOS 950, SAO LEOPOLDO, RS 93022-000, BRAZIL	1519-7530	2236-1715		REV BRAS PALEONTOLOG	Rev. Bras. Paleontol.	JAN-MAR	2020	23	1					73	77		10.4072/rbp.2020.1.05	http://dx.doi.org/10.4072/rbp.2020.1.05			5	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	MO4QM					2023-06-23	WOS:000551512700005
J	Neves, BBD; Van Schmus, WR; Santos, LCMD				de Brito Neves, Benjamim Bley; Van Schmus, William Randall; Montefalco de Lira Santos, Lauro Cezar			Alto Moxoto Terrane, a fragment of Columbia supercontinent in the Transversal Zone interior: Borborema Province, Northeast Brazil	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Transversal Zone; Borborema Province; Rhyacian accretion; Cariris Velhos Fold System; Brasiliano	GEOCHRONOLOGY; GEOCHEMISTRY; COMMISSION; ITATUBA; ROCKS	In the central part or central subprovince of the Borborema Province, in the so-called Transversal Zone, an assemblage of Paleoproterozoic (predominantly Rhyacian) rocks occurs together with sparsely distributed Neoarchean nuclei. These rocks constitute the main basement of the Tonian (Cariris Velhos Cycle) and Ediacaran (Brasiliano Cycle) mobile belts. They are older tectonostratigraphic terranes and par excellence ramifying elements (as "inliers") of the Neoproterozoic orogenic constructions. This tectonostratigraphic terrane known as Alto Moxoto composes a litho-structural context typical of accretionary orogens, with the presence of granitic, granodioritic, and trondhjemitic orthogneisses (approximate to arc-type associations) that stretch out for some hundreds of kilometers (Floresta Suite) and are partially covered by medium-grade pelitic-psammitic sequences (Sertania Supergroup). This basement outline (Floresta Suite + Sertania Supergroup) depicts an irregular sigmoidal shape, from the interior of Pernambuco (meridian 39 degrees W) to the Paraiba coastal area (meridian 34 degrees 45'W), along about 450 km, varying from 40 to 80 km in width, resulting in a total area of ca. 28,000 km(2). This Rhyacian petrotectonic scenario is conditioned and delimited by extensive (shear + thrust) faults that configure a tectonostratigraphic terrane. Moreover, there are pieces of continuity evidence of this tectonostratigraphic terrane not only in the basement of the adjacent Neoproterozoic mobile belts to the North and South of the TAM in Brazil, but also in Northern Cameroon, in Africa. Within this broader predominantly Rhyacian belt, some small Neoarchean gneissic and migmatitic nuclei were identified. The Rhyacian lithologies reveal evidence (T-DM ages) of sources from a Neoarchean paleosubstrate. During the Statherian, the whole Rhyacian context was affected by a series of small-scale magmatic manifestations of varied petrologic composition: syenitic, granitic, granodioritic, and gabbro-anorthositic. In this paper, a synthesis of the bibliographic data is presented, including a series of unpublished (geologic and geochronologic) data that together validate our conviction that we are dealing with an extensive (reworked) fragment (TAM) derived from the basement of a Paleoproterozoic supercontinent (Columbia).	[de Brito Neves, Benjamim Bley] Univ Sao Paulo, Sao Paulo, SP, Brazil; [Van Schmus, William Randall] Univ Kansas, Lawrence, KS 66045 USA; [Montefalco de Lira Santos, Lauro Cezar] Univ Fed Pernambuco, Recife, PE, Brazil	Universidade de Sao Paulo; University of Kansas; Universidade Federal de Pernambuco	Neves, BBD (autor correspondente), Univ Sao Paulo, Sao Paulo, SP, Brazil.	bbleybn@usp.br; rvschums@ku.edu; lauromontefalco@gmail.com	de Lira Santos, Lauro Cézar Montefalco/E-5536-2015	de Lira Santos, Lauro Cézar Montefalco/0000-0001-6098-1873; de Brito Neves, Benjamim Bley/0000-0003-0789-7191	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico CNPq [3031140/2014, 303576/2019-7]; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo - FAPESP [2013/09484-0, 2016/23871-4]; FAPESP; CNPq	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo - FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was conducted under the auspices of Conselho Nacional de Desenvolvimento Cientifico e Tecnologico CNPq (Researcher 1A sponsorship to the senior author under processes 3031140/2014 and 303576/2019-7) and of Fundacao de Amparo a Pesquisa do Estado de Sao Paulo - FAPESP (two submitted and approved Research Projects, 2013/09484-0 and 2016/23871-4). These grants enabled the survey of many geologic-structural sections and petrographic studies and more than a hundred geochronologic determinations that have been developed in this tectonic unit since 2014. The authors would like to express their gratitude to the two reviewers and to the editors of this journal for their contribution.; Besides the financing agencies (FAPESP and CNPq), reviewers and editors, we are indebted to many geologists from the Recife SUREG-CPRM and lecturers from our and other departments of IGc-USP, UFPE and UnB. The constant and multiform collaboration, the exchange of information, the access to geological maps, among others were very important for the development of this work.	Acciolly A.C. A., 2011, ESTUDOS GEOLOGICOS, V21, P97; Accioly ACA., 2000, THESIS; Bouyo MH, 2019, J AFR EARTH SCI, V149, P215, DOI 10.1016/j.jafrearsci.2018.08.010; Buhn B, 2009, AN ACAD BRAS CIENC, V81, P99, DOI 10.1590/S0001-37652009000100011; CAVALCANTI JAD, 2014, METALOGENESE PROVINC, P343; CONDIE KC, 1982, AM J SCI, V282, P341, DOI 10.2475/ajs.282.3.341; Neves BBD, 2016, BRAZ J GEOL, V46, P491, DOI 10.1590/2317-4889201620160004; De Wit MJ, 2008, GEOL SOC SPEC PUBL, V294, P399, DOI 10.1144/SP294.20; DEPAOLO DJ, 1991, J GEOPHYS RES-SOLID, V96, P2071, DOI 10.1029/90JB02219; dos Santos EJ, 2013, PRECAMBRIAN RES, V224, P454, DOI 10.1016/j.precamres.2012.09.021; Easton RM, 2005, AAPG BULL, V89, P1459, DOI 10.1306/05230505015; Howell D.G., 1995, TOPICS EARTH SCI, V8; Lages GA, 2019, J S AM EARTH SCI, V91, P116, DOI 10.1016/j.jsames.2019.02.003; Meert JG, 2017, GONDWANA RES, V50, P67, DOI 10.1016/j.gr.2017.04.011; Melo O., 2004, REV BRASILEIRA GEOCI, V34, P521; Melo O.O., 2002, REV BRASIL GEOCI, V32, P197, DOI 10; Murphy MA, 1999, EPISODES, V22, P255; Oliveira R.G., 2008, THESIS; Rogers J. J. W., 2004, CONTINENTS SUPERCONT; Sa JM, 2002, J S AM EARTH SCI, V14, P851, DOI 10.1016/S0895-9811(01)00081-5; Santos E.J., 1997, S GEOL NORD 1997 FOR, V17; Santos E.J, 1995, THESIS; Santos E.J., 1996, C BRASILEIRO GEOLOGI, V6, P47; Santos E.J., 2004, REV GEOCIENCIAS USP, V4, P1, DOI [10.5327/s1519-874x2004000100001, DOI 10.5327/S1519-874X2004000100001]; SANTOS EJ, 2010, J S AM EARTH SCI, V29, P61; SANTOS L. M. J. F., 2012, THESIS; Santos L.R., 2017, THESIS, P34; Santos RV, 2013, GONDWANA RES, V23, P380, DOI 10.1016/j.gr.2012.04.010; Sato K., 1998, THESIS; Van Schmus WR, 2011, J S AM EARTH SCI, V31, P227, DOI 10.1016/j.jsames.2011.02.010; Van Schmus WR, 2008, GEOL SOC SPEC PUBL, V294, P69, DOI 10.1144/SP294.5; Zhao GC, 2002, EARTH-SCI REV, V59, P125, DOI 10.1016/S0012-8252(02)00073-9	32	10	10	0	0	SOC BRASILEIRA GEOLOGIA	SAO PAULO	CAIXA POSTAL 11348, SAO PAULO, SP 05422-970, BRAZIL	2317-4889	2317-4692		BRAZ J GEOL	Braz. J. Geol.		2020	50	2							e20190077	10.1590/2317-4889202020190077	http://dx.doi.org/10.1590/2317-4889202020190077			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MP7ZX		Green Published, gold			2023-06-23	WOS:000552420900001
J	de Figueiredo, AR; Simoes, JC; Heidrich, AL; Menegat, R				de Figueiredo, Anderson Ribeiro; Simoes, Jefferson Cardia; Heidrich, Alvaro Luiz; Menegat, Rualdo			Climate change and socio-territorial impacts of glacier-related disasters in Cordillera Blanca, Peru	CONFINS-REVUE FRANCO-BRESILIENNE DE GEOGRAPHIE-REVISTA FRANCO-BRASILEIRA DE GEOGRAFIA			Portuguese	Article						Peru; Cordillera Blanca; glacier-related disasters; deterritorialization; reterritorialization		This article discusses the history of natural disasters in the Cordillera Blanca, Peru, during the 1970-2011 period. The study analyzed general disaster data over this timeframe and more broadly about glacial disasters from 1725 to 2010 AD. Historically, the region has been affected by a series of glacial disasters that left more than 26,000 people dead. Thus, this article examines the impact of these glacial disasters, considering that they trigger processes of deterritorialization and reterritorialization in the region. The following methodological strategies were adopted: fieldwork; semi-structured interviews conducted with glacial disaster survivors and environmental managers; literature review on the subject. We propose that climate change increases the risk of glacier-related disasters. From these reports, it has been possible to verify that deterritorialization implies the affectation of the inhabitant's daily life, the break of relations and links with the place. Moreover, glacial disasters cause a process of abrupt deterritorialization and, consequently, a reterritorialization that will develop more slowly, opening an intense field of disputes between the different involved actors, arousing social conflicts.	[de Figueiredo, Anderson Ribeiro; Simoes, Jefferson Cardia] Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias, Ctr Polar & Climat, Porto Alegre, RS, Brazil; [de Figueiredo, Anderson Ribeiro; Simoes, Jefferson Cardia; Heidrich, Alvaro Luiz] Univ Fed Rio Grande do Sul, Programa Posgrad Geog, Porto Alegre, RS, Brazil; [Menegat, Rualdo] Univ Fed Rio Grande do Sul, Inst Geociencias, Departmento Paleontol & Estratig, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	de Figueiredo, AR (autor correspondente), Univ Fed Rio Grande do Sul UFRGS, Inst Geociencias, Ctr Polar & Climat, Porto Alegre, RS, Brazil.; de Figueiredo, AR (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geog, Porto Alegre, RS, Brazil.	anderson.figueiredo@ufrgs.br; jefferson.simoes@ufrgs.br; alvaro.heidrich@ufrgs.br; rualdo.menegat@ufrgs.br	Ribeiro de Figueiredo, Anderson/HJZ-2924-2023; Simoes, Jefferson Cardia/D-7232-2013	Ribeiro de Figueiredo, Anderson/0000-0002-0228-249X; Simoes, Jefferson Cardia/0000-0001-5555-3401				ANA, 2014, INVENTARIO NACL GLAC; BONNAMEISON Joel, 2002, GEOGRAFIA CULTURAL S, P83; Bonnemaison J., 1996, GEOGRAPHIE CULTURES, P7; Carey D, 2015, THEAT ART WORKBK, P219; Carey M, 2010, SHADOW MELTING GLACI; Carey M., 2014, GLACIARES CAMBIO CLI; Cloke P., 2004, PRACTISING HUMAN GEO; Costa C. S., 2009, SOCIOLOGIA DESASTRES, P236; Ericksen G.E., 1970, PRELIMINARY REPORT G; Evans SG, 2009, ENG GEOL, V108, P96, DOI 10.1016/j.enggeo.2009.06.020; Figueiredo A. C., 2017, THESIS; Figueiredo A.R., 2019, SOC NATUREZA, V31, P1; HAESBAERT R, 2005, CRUZANDO FRONTEIRAS, P00035; HAESBAERT R., 2002, REV GEOGRAPHIA NITER, V4, P7; Hastenrath S.T., 1998, SATELLITE IMAGE ATLA, P58; Heidrich A.L., 2016, ABORDAGENS PRATICAS, V1, P15; Heidrich A. L., 2010, TEORIAS PRATICAS TER, P25; Heidrich A, 2017, GEOGRAPHIA-UFF, V19, P29; HENRIQUE I. C., 2004, TEXTOS DE HIST, V12, P9; INDECI (Instituto Nacional de Defensa Civil), 2013, COMPENDIO ESTADISTIC, P495; Leon J.E.L., 2016, INCA; Menegat R., 2006, THESIS; Michelat G, 1982, CRITICA METODOLOGICA, P191; OLIVEIRA L., 2012, QUAL ESPACO LUGAR GE, P3; OLIVERSMITH A, 1979, MASS EMERGENCIES, V4, P39; Rabatel A, 2013, CRYOSPHERE, V7, P81, DOI 10.5194/tc-7-81-2013; Raffestin C., 1980, GEOGRAFIA PODER; Raffestin C., 1987, CAHIER GROUPE RESEAU, P2; Relph E., 1976, PLACE PLACELESSNESS; REYNOLDS JM, 1992, AGID GEO IN, P143; SANTOS M., 1994, TECNICA ESPACO TEMPO; Silva J.M., 2009, GEOGRAFIA PESQUISA Q, P91; Spalding Karen, 2016, INDIO CAMPESINO CAMB; UNISDR (United Nations International Strategy for Disaster Reduction), 2005, DESINVENTAR SERVER V	34	0	0	0	2	REVUES ORG	PARIS	CENTRE SOCIOLOGIE ORGANISATIONS CSO SCIENCES PO-CNRS, 27 RUE SAINT-GUILLAUME, PARIS, 75007, FRANCE	1958-9212			CONFINS	Confins		2020	47									10.4000/confins.33198	http://dx.doi.org/10.4000/confins.33198			20	Geography	Emerging Sources Citation Index (ESCI)	Geography	PH2YF		gold			2023-06-23	WOS:000600284200021
J	de Oliveira, JE; Scarelli, FM; Manzolli, R; Portz, LC; Barboza, EG				de Oliveira, Julio E.; Scarelli, Frederico M.; Portantiolo Manzolli, Rogerio; Portz, Luana C.; Barboza, Eduardo G.			Geomorphological Responses Due to Storm Wave Events at Praia da Barra, Garopaba - Santa Catarina State, Southern Brazil	JOURNAL OF COASTAL RESEARCH			English	Article						Coastal geomorphology; high-energy wave events; UAV survey; nearshore dynamics	COASTAL; SYSTEM	This work presents a beach morphodynamics analysis for Praia da Barra, located in the municipality of Garopaba, Santa Catarina State, Brazil. Praia da Barra has sectors with a natural beach/dune system and sectors where the foredune is completely anthropized. In 2017, during autumn and winter, eight storm wave events reached the study area, resulting in a coastline retreat and infrastructure damages at the site and along the southern Brazilian coastal zone. This work applied two methodologies to study the impacts of storm waves at the study area, 1) Four photogrammetric surveys using UAV high-resolution Orthophoto and DEMs for monitoring geomorphological changes at the site, before and after storm wave events in 2017; and 2) wave simulation using the SMC-Brazil platform to assess wave and current patterns from three main wave directions scenarios. The authors integrated the results from both methodologies to understand the behavior of Praia da Barra's beach/dune system when attacked by storm wave events. The authors identified erosive hot spots at Praia da Barra that are concentrated at the central sector of the beach, which presents more anthropization. While the northern and southern sectors present a vegetated and well-developed foredune system, they also presented a higher resilience against the storm events that hit Praia da Barra during the autumn and winter seasons of 2017.	[de Oliveira, Julio E.; Scarelli, Frederico M.; Barboza, Eduardo G.] Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil; [Portantiolo Manzolli, Rogerio; Portz, Luana C.] Univ La Costa, Fac Ciencias Ambientales, Barranquilla, Colombia; [Barboza, Eduardo G.] Univ Fed Rio Grande do Sul, Inst Geociencias, Ctr Estudos Geol Costeira & Ocean, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidad de la Costa; Universidade Federal do Rio Grande do Sul	de Oliveira, JE (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Porto Alegre, RS, Brazil.	jfogeo@gmail.com	Manzolli, Rogerio Portantiolo/E-9777-2019; Oliveira, Julio Fernandes de/HPF-1935-2023; Barboza, Eduardo Guimarães/C-7579-2012; Portz, Luana Carla/AAP-9020-2020	Manzolli, Rogerio Portantiolo/0000-0002-0223-5634; Oliveira, Julio Fernandes de/0000-0001-7758-7434; Barboza, Eduardo Guimarães/0000-0003-2107-6904; Portz, Luana Carla/0000-0001-9232-8086				Bird E., 2008, COASTAL GEOMORPHOLOG, DOI DOI 10.1029/01-O00219; Camus P, 2013, COAST ENG, V72, P56, DOI 10.1016/j.coastaleng.2012.09.002; de Oliveira JF, 2019, J S AM EARTH SCI, V96, DOI 10.1016/j.jsames.2019.102358; Giannini PCF, 2007, MAR GEOL, V237, P143, DOI 10.1016/j.margeo.2006.10.027; Gonzalez M, 2007, COMPUT GEOSCI-UK, V33, P916, DOI 10.1016/j.cageo.2006.12.005; Harley MD, 2017, SCI REP-UK, V7, DOI 10.1038/s41598-017-05792-1; Komar P. D., 1998, BEACH PROCESSES SEDI; Mahiques MM, 1998, ESTUAR COAST SHELF S, V47, P431; Martins E.M., 2014, GRAVEL, V12, P109; MMA-Ministerio do Meio Ambiente; MPOG-Ministerio do Planejamento Orcamento e Gestao, 2018, PAN ER COST BRAS; Pilkey OH, 2014, J COASTAL RES, P431, DOI 10.2112/SI70-073.1; Portz L., 2016, ENV SOC, V19, P137; Scarelli Frederico M., 2017, Remote Sensing Applications: Society and Environment, V7, P27, DOI 10.1016/j.rsase.2017.06.003; Scarelli FM, 2016, J COASTAL RES, P1232, DOI 10.2112/SI75-247.1; Snavely N, 2008, INT J COMPUT VISION, V80, P189, DOI 10.1007/s11263-007-0107-3; Turner IL, 2016, COAST ENG, V114, P19, DOI 10.1016/j.coastaleng.2016.03.011	16	5	5	0	3	COASTAL EDUCATION & RESEARCH FOUNDATION	COCONUT CREEK	5130 NW 54TH STREET, COCONUT CREEK, FL 33073 USA	0749-0208	1551-5036		J COASTAL RES	J. Coast. Res.		2020					95		474	478		10.2112/SI95-092.1	http://dx.doi.org/10.2112/SI95-092.1			5	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	LU1YE					2023-06-23	WOS:000537556600087
J	Gorayeb, PSD; Silva-Silva, LC; Galarza, MA				de Sousa Gorayeb, Paulo Sergio; Silva-Silva, Luana Camile; Galarza, Marco Antonio			Geology, geochronology Pb-Pb, U-Pb-Hf zircon and Sm-Nd T-DM of the Uruburetama batholith, Northern Borborema Province: contextualization in the Santa Quiteria Magmatic Arc	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Pb-Pb and U-Pb-Hf geochronology in zircon; Sm-Nd T-DM; Uruburetama Batholith; Santa Quiteria Magmatic Arc; NW-Borborema Province; West Gondwana Orogen	CEARA CENTRAL DOMAIN; NE-BRAZIL; ISOTOPIC COMPOSITION; MASS-SPECTROMETRY; CONTINENTAL-CRUST; LU-HF; CONSTRAINTS; GRANITOIDS; EVOLUTION; AGES	Records of large crustal masses in the northwest of Borborema Province (BP) spread over more than 300 km are found as numerous granitic bodies amid a high-grade metamorphic gneissic-migmatitic terrain. The Tamboril-Santa Quiteria Complex (TSQC) is a Neoproterozoic example of these records; it is located in the north of the Ceara Central Domain (CECD) and its origin is related to a continental magmatic arc at different evolutionary stages of the arc. The Uruburetama Granite (UG), object of this study, fits into this context and constitutes one of the most representative batholiths occupying an area of 1,500 km(2). Dozens of other similar plutons have been recorded in cartographic works that show similarities which suggests the grouping of these bodies in the Uruburetama Granitic Suite (UGS), previously included in the TSQC. The UG consists of a variety of plutonic rocks associated with mafic-dioritic dikes and its metamorphic products. Six petrographic facies were identified among the plutonic rocks: biotite-hornblende monzogranites and syenogranitic varieties, biotite-hornblende granodiorites, in addition to quartz syenite, leucomonzogranites, and diorites rocks. These rocks are affected by deformation, with greater intensity at the edges of the batholith, where thrust shear zones with transcurrent components were installed, generating tectonic fabrics (mylonitic foliations, stretch lineation, almond feldspar porphyroclasts, and ribbon quartz). Despite the superimposed deformational effects, magmatic relict textures are partially preserved, mainly toward the central portion of the pluton. The UG and the associated plutons are hosted by migmatized orthogneisses, paragneisses with garnet, sillimanite or kyanite, marbles, calcium-silicate gneisses, micaschists, sillimanite quartzites, and amphibolite lenses. The contact relations are diffuse with gradation for migmatites, and in rare cases, intrusive contacts with gneiss mega-xenolites are registered. The geochronological data obtained by Pb-evaporation zircon in two samples of the UG show average ages of 655 +/- 2 and 656 +/- 1 Ma. U-Pb zircon data for the same samples showed slightly younger age values of 559 +/- 10 and 634 +/- 10 Ma, respectively. The ages obtained are considered as representative of the magmatic phases of UG crystallization in the context of the evolution of the Santa Quiteria Magmatic Arc (SQMA), with the main magmatic phase of the UG in the Cryogenian. However, the age of 559 Ma would represent a younger magmatic event in the evolution of the arch. Overall, these ages correspond to the "Pre-Collisional I" or "Early-Sin-Orogenic" phase of a large collisional belt in the west of BP, and the younger ages must represent events related to the continuity of the orogen convergence of the Latest-Pre-collisional I (634 Ma) and Post-Collisional I (559 Ma) phases. Sm-Nd whole-rock isotopes data showed epsilon(Nd)(t) values predominantly negative (-25.6 and -0.9), and Nd-T-DM model ages of 2.90 and 1.2 Ga. The results of the Lu-Hf isotopes analysis for the Bt-Hbl monzogranite sample showed negative epsilon(Hf) values (-26.75 to -35.48) and Hf-T-DM(C) model ages of 3.12 to 3.65 Ga while the results for Bt-Hbl granodiorite showed epsilon(Hf) values of -2.07 to +1.08 and Hf-T-DM(C) model ages of 1.46 to 1.66 Ga. These data point to the existence of two distinct and older crustal sources in the generation of these granitoids, one in the Mesoarchean, and the other in the Mesoproterozoic. The Archean ages correspond to the basement in the south of the CECD (Troia Massif and Granjeiro Complex); on the other hand, the Mesoproterozoic ages are up for discussion, since terrains with this type of age do not occur adjacent to the BP. On the other hand, it can be interpreted as a mixture of sources, one of them probably juvenile, neoproterozoic, with contamination of the Archean crust. Thus, the UG is considered one of the most important records of the beginning of the evolution of the Santa Quiteria Magmatic Arc associated with a wide collisional belt in the "West Gondwana Orogen" in the west of Borborema Province.	[de Sousa Gorayeb, Paulo Sergio; Silva-Silva, Luana Camile; Galarza, Marco Antonio] Univ Fed Para, Belem, Para, Brazil; [Galarza, Marco Antonio] Univ Fed Para, Lab Para Iso, Belem, Para, Brazil	Universidade Federal do Para; Universidade Federal do Para	Gorayeb, PSD (autor correspondente), Univ Fed Para, Belem, Para, Brazil.	gorayebp@ufpa.br; luana.silva@ig.ufpa.br; antogt@ufpa.br	Galarza, Marco Antonio MAG/B-1736-2013	Gorayeb, Paulo/0000-0003-1877-9756; Silva-Silva, Luana Camile/0000-0002-5526-9846				Amaral W.S., 2010, THESIS; Amaral WD, 2012, GONDWANA RES, V22, P892, DOI 10.1016/j.gr.2012.02.011; Ancelmi MF, 2013, BRAZ J GEOL, V43, P235, DOI 10.5327/Z2317-48892013000200004; Andersen T, 2009, J GEOL SOC LONDON, V166, P233, DOI 10.1144/0016-76492007-166; [Anonymous], 2017, PESQUI GEOCIENC; [Anonymous], 1995, PETROGRAPHY PETROGEN; Archanjo CJ, 2009, INT J EARTH SCI, V98, P1793, DOI 10.1007/s00531-008-0342-z; Arthaud MH, 2008, GEOL SOC SPEC PUBL, V294, P49, DOI 10.1144/SP294.4; Arthaud M.H., 1989, ANNALS, V2, P77; Arthaud M.H., 2007, THESIS; Arthaud M.H., 2007, THESIS; Belousova EA, 2010, LITHOS, V119, P457, DOI 10.1016/j.lithos.2010.07.024; BENOTHMAN D, 1984, NATURE, V307, P510, DOI 10.1038/307510a0; Bizzi L.A., 2003, GEOLOGY TECTONICS MI; Bouvier A, 2008, EARTH PLANET SC LETT, V273, P48, DOI 10.1016/j.epsl.2008.06.010; CABY R, 1986, GEOLOGY, V14, P871, DOI 10.1130/0091-7613(1986)14<871:MPNOTB>2.0.CO;2; Castro N. 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J	Dillenburg, SR; Barboza, EG; Rosa, MLCC; Caron, F; Bitencourt, VJB				Dillenburg, Sergio R.; Barboza, Eduardo G.; Rosa, Maria Luiza C. C.; Caron, Felipe; Bitencourt, Volney J. B.			Changes in the Littoral Drift System of the Uruguayan Coast during the Holocene and its Influence in the Continuing Erosion in Southern Brazil	JOURNAL OF COASTAL RESEARCH			English	Article						Rocky promontories; Cabo Polonio; shelf morphology; La Coronilla; sediment bypass	SEA-LEVEL RISE; SEDIMENT BUDGET; EVOLUTION; BARRIER; RETREAT; ISLAND; SHELF	In northern Uruguay and southern Brazil, a littoral drift system dominates from southwest to northeast. This littoral drift is a consequence of higher wave-energy, generated in southern latitudes and that has been operating on a long-term scale, playing an important role not only in the evolution of coastal barriers of this region during the Holocene but also in coastal erosion that presently occurs in some parts of this coast. From La Coronilla to Cabo Santa Marta, which is a coastal sector 750 km - along the coast is gently undulating, showing gentle projections located to the south of gentle reentrances, that are dominated by transgressive/stationary and regressive barriers, respectively. In general, the regressive barriers have been developed by sediments brought into the reentrances by long-shore currents. The main source of these sediments had been the transgressive/stationary barriers that occur along the coastal projections. This differentiation of barrier behavior started at around 6-5 ka, at the end of the Postglacial Marine Transgression (PMT), when all rivers were drowned, finishing the delivery of new coarse sediments to the coast. Also, at this time the large rock promontories of the Uruguayan coast were formed and started to retain sediments of the littoral drift system, triggering a long-term coastal erosion in the southernmost coastal projection. Regarding erosion that is occurring in this stretch of coast the important issue to be considered in future coastal planning is that erosion will continue to operate in the long-term but will also be (and certainly has been already) amplified by sea-level rise in the next centuries as projected by the Intergovernmental Panel on Climate Change (IPCC).	[Dillenburg, Sergio R.; Barboza, Eduardo G.; Rosa, Maria Luiza C. C.; Caron, Felipe] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, BR-91509900 Porto Alegre, RS, Brazil; [Bitencourt, Volney J. B.] Univ Fed Rio Grande do Sul, PPGGEO, BR-91509900 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Dillenburg, SR (autor correspondente), Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, BR-91509900 Porto Alegre, RS, Brazil.	sergio.dillenburg@ufrgs.br	Barboza, Eduardo Guimarães/C-7579-2012; de Bitencourt, Volney Junior Borges/AAD-9618-2019; Dillenburg, Sergio/C-4027-2013	Barboza, Eduardo Guimarães/0000-0003-2107-6904; de Bitencourt, Volney Junior Borges/0000-0002-1004-5179; Dillenburg, Sergio/0000-0003-0072-7018	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Sergio Dillenburg and Eduardo Barboza thank the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for the provision of their research fellowships. We also thank Patrick Hesp for his thoughtful help with the English text	Angulo RJ, 2006, QUATERNARY SCI REV, V25, P486, DOI 10.1016/j.quascirev.2005.03.008; Barboza EG, 2003, J COASTAL RES, P260; Correa ICS, 1996, MAR GEOL, V130, P163, DOI 10.1016/0025-3227(95)00126-3; da Silva GM, 2013, J COASTAL RES, P1307, DOI 10.2112/SI65.221.1; da Silva GV, 2016, MAR GEOL, V379, P13, DOI 10.1016/j.margeo.2016.05.008; de Figueiredo SA, 2018, BRAZ J OCEANOGR, V66, P210, DOI [10.1590/S1679-87592018009806602, 10.1590/s1679-87592018009806602]; Dillenburg SR, 2014, GEOL SOC SPEC PUBL, V388, P333, DOI 10.1144/SP388.16; Dillenburg SR, 2009, LECT NOTES EARTH SCI, V107, P53; Dillenburg SR, 2000, J COASTAL RES, V16, P71; Duarte J., 2014, ACTAS 3AS JORN ENG H, P289; Goodwin ID, 2013, MAR GEOL, V341, P29, DOI 10.1016/j.margeo.2013.05.005; Lima LG, 2013, J S AM EARTH SCI, V42, P27, DOI 10.1016/j.jsames.2012.07.002; Lima S. F., 2001, PESQUISAS, V28, P99, DOI DOI 10.22456/1807-9806.20272; SANDERS JE, 1975, GEOL SOC AM BULL, V86, P65, DOI 10.1130/0016-7606(1975)86<65:EOSRAI>2.0.CO;2; SWIFT DJP, 1975, GEOLOGY, V14, P1; Verocai J., NUEVAS MIRADAS PROBL, P131	16	6	6	0	3	COASTAL EDUCATION & RESEARCH FOUNDATION	COCONUT CREEK	5130 NW 54TH STREET, COCONUT CREEK, FL 33073 USA	0749-0208	1551-5036		J COASTAL RES	J. Coast. Res.		2020					95		453	457		10.2112/SI95-088.1	http://dx.doi.org/10.2112/SI95-088.1			5	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	LU1YE					2023-06-23	WOS:000537556600083
J	do Amaral, DN; Cerqueira, JR; de Andrade, CLN; Ribeiro, HJPS; Garcia, KS; Miranda, FLEC; Oliveira, OM; Queiroz, AF; dos Santos, LCL				do Amaral, Diego Nery; Cerqueira, Jose Roberto; Navarro de Andrade, Consuelo Lima; Portugal Severiano Ribeiro, Helio Jorge; Garcia, Karina Santos; Miranda, Flavia Lima e Cima; Oliveira, Olivia Maria; Queiroz, Antonio Fernando; Lobato dos Santos, Luiz Carlos			Paleoenvironmental characterization of a Lower Cretaceous section of the Reconcavo Basin, Bahia, Brazil	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Reconcavo Basin; organic geochemistry; potential generator; biomarkers; palynofacies	ORGANIC-RICH ROCKS; CARBON	The objective of this work was to evaluate the paleodepositional conditions and potential for the hydrocarbons generation of the outcropping shales in the Southern Compartment of the Reconcavo Basin, indicative of the Candeias and Maracangalha Formations (Lower Cretaceous), from the organic geochemical characterization and analysis of palinofacies. For this, 23 samples of outcrops were collected near the cities of Santo Amaro, Sao Francisco do Conde and Simoes Filho, State of Bahia, Brazil. All samples were analyzed for total organic carbon (TOC), total sulfur, insoluble residue, Rock-Eval pyrolysis, whole oil chromatography, stable isotopes of oxygen, organic and inorganic carbon, saturated biomarkers and palynofacies, performed at the Center of Excellence in Geochemistry of the Institute of Geosciences of the Universidade Federal da Bahia (Lepetro), Brazil. The parameters provided by the geochemical analyzes indicate significant differences between the outcrops under study, mainly regarding the quantity and the quality of the organic matter, thus configuring a difference in the conditions of production and preservation of the organic matter during the time of deposition of the shales. There are layers rich in organic carbon, containing well-preserved type I kerogen, indicating anoxic depositional conditions. In contrast, poor layers of organic content, containing residual kerogen (type IV), occur, reflecting oxidizing conditions of the depositional environment. The observed differences suggest that the variability of the geochemical properties of the organic matter reflects the climatic variations occurred during the deposition of the sediments of the Candeias and Maracangalha Formations. As a consequence, there are levels with potential for generation and levels with no potential for hydrocarbon generation.	[do Amaral, Diego Nery; Cerqueira, Jose Roberto; Garcia, Karina Santos; Miranda, Flavia Lima e Cima; Oliveira, Olivia Maria; Queiroz, Antonio Fernando; Lobato dos Santos, Luiz Carlos] Univ Fed Bahia, Salvador, BA, Brazil; [Navarro de Andrade, Consuelo Lima] Univ Estadual Feira de Santana, Dept Ciencias Exatas DEXA, Feira De Santana, BA, Brazil; [Portugal Severiano Ribeiro, Helio Jorge] Univ Estadual Norte Fluminense, Rio De Janeiro, RJ, Brazil	Universidade Federal da Bahia; Universidade Estadual de Feira de Santana; Universidade Estadual do Norte Fluminense	do Amaral, DN (autor correspondente), Univ Fed Bahia, Salvador, BA, Brazil.	d.nery9@gmail.com; jrkcerq@gmail.com; consuelonavarro87@gmail.com; severiano.geologo@gmail.com; karina.ksg4@gmail.com; cimaflavia@gmail.com; olivia@ufba.br; queiroz@ufba.br; lclsantos@ufba.br	de Oliveira, Olivia Maria Cordeiro/AAB-3246-2021; Cerqueira, José Roberto/AAY-9852-2021; Queiroz, Antonio Fernando de Souza/ABH-6682-2020; Santos, Luiz Carlos Lobato/F-2805-2013	Santos, Luiz Carlos Lobato/0000-0003-3824-7802; Cima, Flavia/0000-0002-8312-2243; GARCIA, KARINA/0000-0003-3575-311X; Lima Navarro de Andrade, Consuelo/0000-0003-1995-8887; Amaral, Diego/0000-0002-8041-4953	Post-Graduate Program in Geochemistry: Petroleum and Environment (Pospetro) of the Universidade Federal da Bahia; Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com Pesquisa e Desenvolvimento" [ANP 20075-8]	Post-Graduate Program in Geochemistry: Petroleum and Environment (Pospetro) of the Universidade Federal da Bahia; Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com Pesquisa e Desenvolvimento"	The authors are grateful to the Post-Graduate Program in Geochemistry: Petroleum and Environment (Pospetro) of the Universidade Federal da Bahia, for all the support during the preparation of this article. Thanks also to the Agencia Nacional do Petroleo, Gas Natural e Biocombustiveis (ANP) for the data provided. Finally, the authors are extremely grateful for the valuable observations and suggestions provided by the geologist Paulo Milhomem.; This research was carried out in association with the ongoing R&D project registered as ANP 20075-8, "Advanced Molecular Characterization" (UFBA/Shell Brasil/ANP) -Project "Pesquisas em Sistemas Petroliferos de Bacias Sedimentares Brasileiras do Centro de Excelencia de Geoquimica do Petroleo do Instituto de Geociencias (IGEO) da Universidade Federal da Bahia (UFBA) - GEOQPETROL-BS", sponsored by Shell Brasil under the ANP R&D levy as "Compromisso de Investimentos com Pesquisa e Desenvolvimento".	Balbinot M, 2010, INT J COAL GEOL, V84, P286, DOI 10.1016/j.coal.2010.09.008; BERNER RA, 1983, GEOCHIM COSMOCHIM AC, V47, P855, DOI 10.1016/0016-7037(83)90151-5; BrandAo AT, 2015, THESIS; Caixeta J. 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W., 1987, ADV PETROLEUM GEOCHE, P1; LANGFORD FF, 1990, AAPG BULL, V74, P799; Magnavita L.P., 2005, B GEOC PETROBRAS, V13; Magnavita L.P., 1996, C BRASILEIRO GEOLOGI, V39, P335; MEDEIROS R.A., 1981, ROTEIRO GEOLOGICO BA ROTEIRO GEOLOGICO BA; MELLO MR, 1988, MAR PETROL GEOL, V5, P205, DOI 10.1016/0264-8172(88)90002-5; MELLO MR, 1994, AAPG MEMOIR, V60, P499; Milhomem P.S, 2003, BACIA RECONCAVO BACI; Parrish J.T., 1985, GLOBAL PALEOGEOGRAPH; PARRISH JT, 1982, PALAEOGEOGR PALAEOCL, V40, P31; Penteado H.L.B., 2000, AAPG BULL, V73, P179; Peters K. E., 2004, BIOMARKER GUIDE; Peters K. E., 1994, AAPG MEMOIR, V60, P93; REQUEJO AG, 1994, ORG GEOCHEM, V22, P441, DOI 10.1016/0146-6380(94)90118-X; Santos C.F., 2005, B GEOCIENCIAS PETROB, V13, P205; Santos CF., 1990, ORIGEM EVOLUCAO BACI, P367; SCOTESE CR, 1988, TECTONOPHYSICS, V155, P27, DOI 10.1016/0040-1951(88)90259-4; Silva HTF, 2000, AAPG STUD GEOL, P209; Soreghan MJ, 1996, AAPG BULL, V80, P382; Tyson R.V., 1995, SEDIMENTARY ORGANIC	33	0	0	0	2	SOC BRASILEIRA GEOLOGIA	SAO PAULO	CAIXA POSTAL 11348, SAO PAULO, SP 05422-970, BRAZIL	2317-4889	2317-4692		BRAZ J GEOL	Braz. J. Geol.		2020	50	3							e20190058	10.1590/2317-4889202020190058	http://dx.doi.org/10.1590/2317-4889202020190058			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MP8CS		gold			2023-06-23	WOS:000552428200001
J	Gallagher, K; Parra, M				Gallagher, Kerry; Parra, Mauricio			A new approach to thermal history modelling with detrital low temperature thermochronological data	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						detrital thermochronology; thermal history; inversion	ZIRCON GEOCHRONOLOGY; CATCHMENT EROSION; HELIUM DIFFUSION; APATITE; INFORMATION; VARIABILITY; INVERSION; KINETICS; SIGNAL; UPLIFT	We present an inverse modelling strategy to infer thermal history information from detrital low temperature thermochronological data from modern sediment sampling the outlet of a single catchment. As presented, the method relies on the assumption that the geological timescale thermal history was the same across the catchment. The detrital sample is assumed to represent a mixture of grains originating from a potentially unknown sampling of the present elevation range in the catchment. The approach also implements a method to infer a function describing the topographic sampling represented in the detrital sample. In practice, this may reflect variations in erosion with elevation but also lithological differences in the catchment (fertility) and the nature of erosion/transport processes in the catchment. A combination of detrital and in-situ bedrock data are recommended to improve the resolution of the topographic sampling function. We demonstrate the application of the approach to a set of fission track data from the Fundacion catchment in the Sierra Nevada de Santa Marta in northern Colombia. The inferred thermal history suggest a period of rapid cooling initiated around 50-30 Ma, followed by slower cooling to the present day, consistent with the regional geological history. The topographic sampling function estimates suggest that the hypsometric distribution is not appropriate in terms of the contributions from different elevations to the detrital sample. Rather, the data imply a higher proportion of sampling from lower elevations close to the location of the outlet where the detrital sample was collected. (C) 2019 Elsevier B.V. All rights reserved.	[Gallagher, Kerry] Univ Rennes, Geosci Rennes OSUR, F-35042 Rennes, France; [Parra, Mauricio] Univ Sao Paulo, Inst Energy & Environm, Av Prof Luciano Gualberto 1289, BR-05508010 Sao Paulo, SP, Brazil	Universite de Rennes; Universidade de Sao Paulo	Gallagher, K (autor correspondente), Univ Rennes, Geosci Rennes OSUR, F-35042 Rennes, France.	kerry.gallagher@univ-rennesl.fr; mparra@iee.usp.br	Parra, Mauricio/B-7497-2013	Parra, Mauricio/0000-0002-5955-6105; Gallagher, Kerry/0000-0002-8124-6242	FAPESP JP Project [2013/03265-5]; CNRS-FAPESP binational project [FAPESP Sprint 2017/50276-3]	FAPESP JP Project(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CNRS-FAPESP binational project	We would like to thank Nathan Niemi and Matthew Fox for useful reviews that helped us clarify certain aspects of this paper. Also we thank Maxime Bernard, Juan Sebastian Echeverri, Ana Maria Patiflo, Philippe Steer, and Peter van der Beek for comments and discussion over the last year or so. This work was facilitated through a CNRS-FAPESP binational project (FAPESP Sprint 2017/50276-3). M.P thanks FAPESP JP Project 2013/03265-5 for funding the data acquisition.	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Sci. Lett.	JAN 1	2020	529								115872	10.1016/j.epsl.2019.115872	http://dx.doi.org/10.1016/j.epsl.2019.115872			12	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	JM2GO		Green Submitted			2023-06-23	WOS:000496039600010
J	Galvao, P; de Souz, EL; Demetrio, JG; Baessa, MM				Galvao, Paulo; de Souz, Eliene Lopes; Demetrio, Jose Geilson; Baessa, Marcus Martins			Estimating groundwater resources of the Ica-Solimoes Aquifer System in the Urucu Oil Province Central Amazon Region, Brazil, focused on a balance between availability and water demand	RBRH-REVISTA BRASILEIRA DE RECURSOS HIDRICOS			English	Article						Hydrogeology; Aquifer system; Groundwater resources; Amazon	SAFE YIELD	Hydrogeologic information is still scarce in the Amazon region being required more studies for improving the understanding of local hydrogeologic contexts. The goal of this paper, focused on the Urucu Oil Province, Brazilian Central Amazon, is to quantitatively estimate groundwater resources of the Ica-Solimoes Aquifer System (ISAS) in the region. The work focuses on a balance between availability and water demand, considering current and future uses, contributing to a sustainable and integrated use of groundwater. Cartographic, lithologic and geophysical logs were analyzed coupled with ISAS hydraulic data (transmissivity, hydraulic conductivity, and storativity) and its local aquifer geometries, as well as the potentiometric surface map to estimate values of total and renewable groundwater resources, sustainable yields, and well-field facility capacities. Results showed the portion of the Ica-Solimoes Aquifer System has a total groundwater resource of 0.45 km(3). As there is a groundwater consumptive projection to 2050 close to 2.7 x 10(-3) km(3) yr(-1) and the aquifer system has a sustainable yield of 3 x 10(-3) km(3) yr(-1) the current resource allocation for future consumption rate appears to be sustainable.	[Galvao, Paulo] Univ Fed Minas Gerais, Belo Horizonte, MG, Brazil; [de Souz, Eliene Lopes] Univ Fed Para, Belem, Para, Brazil; [Demetrio, Jose Geilson] Univ Fed Pernambuco, Recife, PE, Brazil; [Baessa, Marcus Martins] Ctr Pesquisa & Desenvolvimento Leopoldo Amer Migu, Rio De Janeiro, RJ, Brazil	Universidade Federal de Minas Gerais; Universidade Federal do Para; Universidade Federal de Pernambuco	Galvao, P (autor correspondente), Univ Fed Minas Gerais, Belo Horizonte, MG, Brazil.	hidropaulo@gmail.com; elienelopes3009@gmail.com; geilson@ufpe.br; marcus.baessa@petrobras.com.br	Galvão, Paulo H/Q-7928-2017; DEMETRIO, JOSE GEILSON ALVES/AAI-5505-2021	Galvão, Paulo H/0000-0001-7183-0368; DEMETRIO, JOSE GEILSON ALVES/0000-0001-6695-7057; Demetrio, Jose Geilson Alves/0000-0002-4908-4888	Petrobras, through the project "Ecoeficiencia 3" [0050.0032737.07.2]	Petrobras, through the project "Ecoeficiencia 3"	This work was funded by Petrobras, through the project "Ecoeficiencia 3" (Contract No. 0050.0032737.07.2).	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L. de, 2015, Journal of Water Resource and Protection, V7, P131; Souza L.S.B., 2006, REV GEOLOGIA UFC, V19, P111; Tancredi A. C. F. N. S., 1996, THESIS; Todd D.K., 1959, GROUNDWATER HYDROLOG	38	1	1	0	0	ASSOC BRASILEIRA RECURSOS HIDRICOS-ABRH	PORTE ALEGRE	AV BENTO GONCALVES 9500, PORTE ALEGRE, RS 91501-970, BRAZIL	1414-381X	2318-0331		RBRH-REV BRAS RECUR	RBRH-Rev. Bras. Recur. Hidr.		2020	25								e6	10.1590/2318-0331.252020190058	http://dx.doi.org/10.1590/2318-0331.252020190058			10	Water Resources	Emerging Sources Citation Index (ESCI)	Water Resources	KW6QA		gold, Green Published			2023-06-23	WOS:000521290600001
J	Gonzaga, BA; Alves, DL; Albuquerque, MD; Espinoza, JMD; Almeida, LP; Weschenfelder, J				Gonzaga, Bento A.; Alves, Deivid Leal; Albuquerque, Miguel da G.; Espinoza, Jean M. de A.; Almeida, Luis Pedro; Weschenfelder, Jair			Development of a Low-cost Ultrasonic Sensor for Groundwater Monitoring in Coastal Environments: Validation using Field and Laboratory Observations	JOURNAL OF COASTAL RESEARCH			English	Article						Coastal management; flood risk; open source technologies; arduino platform	BEACHES	This study presents the development and validation of a low-cost ultrasonic sensor (HCSR 04), coupled to an open source Arduino microcontroller platform, for groundwater monitoring in coastal environments. Given the fact that low-lying coastal zones are regions naturally prone to flooding (due to oceanic forcing and pluviosity) and densely occupied, monitoring groundwater variations is crucial for the management of flood-related events. A groundwater monitoring well was built, (made of a PVC pipe with 100 mm in diameter and 2 m long) and installed on the ground of a dune field, located in Cassino beach, southern of Brazil. The system was deployed for 84 consecutive days and programmed to perform water level measurements every 10 min. In laboratory, three units with the same hardware setup of the unit installed in the field (ultrasonic sensor coupled to the Arduino microcontroller) were installed on a 20 liter graduated PVC tube. Varying water levels were tested in the laboratory along the time (changing 1 cm every 2 minutes during 4 hours) in order to reproduce the synthetic signal. Eighty measurements were obtained for each sensor, a total of 240 for each validation process. For the laboratory validation, the results for nonparametric statistical tests (Kruskal and Wallis, and Dunn) presented a correlation of 99%, with Root mean square error (RMSE) 0.4113 and bias 0.0418. For the field tests, 3262 data collected by an ultrasonic sensor during 240 hours showed a means registration of 0.543 m. The minimum and maximum cataloged is 0.40 and 0.70 m, respectively, with 0.1076 m of standard deviation. Groundwater classical measurements, using a measuring tape, showed a mean and standard deviation of 0.544 and 0.1069 m, respectively. These preliminary tests showed that the developed monitoring system performs observations with an accuracy and precision within standard methods, therefore can be applied to monitoring changes in the level of groundwater.	[Gonzaga, Bento A.; Almeida, Luis Pedro] Fed Univ Rio Grande, Inst Oceanog, Rio Grande, RS, Brazil; [Alves, Deivid Leal; Weschenfelder, Jair] Univ Fed Rio Grande do Sul, Inst Geosci, Porto Alegre, RS, Brazil; [Albuquerque, Miguel da G.; Espinoza, Jean M. de A.] Fed Inst Rio Grande Sul, Dept Geoproc, Rio Grande, RS, Brazil	Universidade Federal do Rio Grande; Universidade Federal do Rio Grande do Sul	Albuquerque, MD (autor correspondente), Fed Inst Rio Grande Sul, Dept Geoproc, Rio Grande, RS, Brazil.	migueldaguia@gmail.com	Weschenfelder, Jair/C-3390-2013; Albuquerque, Miguel/AAH-6952-2021; da Guia Albuquerque, Miguel/D-7762-2017; Alves, Deivid Cristian Leal/ABE-5453-2020	Weschenfelder, Jair/0000-0002-2075-4067; Albuquerque, Miguel/0000-0002-2063-492X; da Guia Albuquerque, Miguel/0000-0002-2063-492X; Alves, Deivid Cristian Leal/0000-0002-5255-123X	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	The authors thanks the Programa de Pos Graduacao em Gerenciamento Costeiro (PPGC) at the Universidade Federal do Rio Grande (FURG) and the Instituto Federal de Educacao, Ciencia e Tecnologia do Rio Grande do Sul, Campus Rio Grande (IFRS), for the logistic support. This study was financed in party by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) -Finance Code 001.	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Coast. Res.		2020					95		1001	1005		10.2112/SI95-195.1	http://dx.doi.org/10.2112/SI95-195.1			5	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	LU1YE					2023-06-23	WOS:000537556600187
J	Goodbred, SL; Dillehay, TD; Mora, CG; Sawakuchi, AO				Goodbred, Steven L., Jr.; Dillehay, Tom D.; Galvez Mora, Cesar; Sawakuchi, Andre O.			Transformation of maritime desert to an agricultural center: Holocene environmental change and landscape engineering in Chicama River valley, northern Peru coast	QUATERNARY SCIENCE REVIEWS			English	Article						Holocene; Geoarchaeology; South America; Sedimentology; Coupled human-natural systems	BEACH RIDGE COMPLEX; EL-NINO; FLOODPLAIN SEDIMENTATION; CULTURAL CONSEQUENCES; HUACA PRIETA; ENSO EVENTS; VARIABILITY; RECORD; RADIOCARBON; OSCILLATION	Some of the earliest Andean populations settled in the region's arid coastal river valleys, supported by abundant marine life despite having domesticated plant cultigens as early as similar to 10 ka. In the Chicama River valley, this maritime economy dominated at the Preceramic site, Huaca Prieta, until similar to 6 ka, after which agricultural production began to increase significantly. This agricultural expansion was motivated in part by the development of arable fine-grained soils along the coast as the result of slowing sea-level rise, enhanced river floods, and unique basin lithology. Local populations made use of the stabilized flood-plain and wetland settings to conduct raised-terrace farming. By similar to 3.5 ka, growth in agriculture and the new fine-grained sediment resources led to several major cultural developments, including the production of fired-ceramic pottery and adobe-brick monument construction associated with the Cupisnique culture. Populations thereafter expanded into the middle valley, where the Salinar and Gallinazo cultures used small water-control structures to farm local ravines. These cultural and technological developments all parallel natural environmental changes driven by increasing ENSO-related water and sediment discharge. By similar to 1.8 ka, though, further expansion of agriculture -and arable land- was driven primarily by direct human manipulation of the environment. The construction of an ever-expanding network of irrigation canals diverted increasing volumes of water and sediment to distal reaches of the Chicama valley, supporting the great Moche and Chimu civilizations, and persisting through the Inka and Colonial periods. This history of Chicama valley traces strongly coupled interactions between the human and natural environments, supporting significant socio-cultural, economic, demographic, and technological advances. (C) 2019 Elsevier Ltd. All rights reserved.	[Goodbred, Steven L., Jr.] Vanderbilt Univ, Dept Earth & Environm Sci, Nashville, TN 37235 USA; [Dillehay, Tom D.] Vanderbilt Univ, Dept Anthropol, Nashville, TN 37235 USA; [Dillehay, Tom D.] Univ Austral Chile, Escuela Arqueol, Puerto Montt, Chile; [Galvez Mora, Cesar] Acad Nacl Hist, Lima, Peru; [Sawakuchi, Andre O.] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo, SP, Brazil	Vanderbilt University; Vanderbilt University; Universidad Austral de Chile; Universidade de Sao Paulo	Goodbred, SL (autor correspondente), Vanderbilt Univ, Dept Earth & Environm Sci, Nashville, TN 37235 USA.	steven.goodbred@vanderbilt.edu	Sawakuchi, André O/D-1445-2013	Sawakuchi, Andre/0000-0001-5016-2428; Galvez Mora, Cesar/0000-0002-8751-6266; Goodbred, Steven/0000-0001-7626-9864	U.S. National Science Foundation [BCS 0914891]; National Geographic Society; Vanderbilt University Discovery Research program	U.S. National Science Foundation(National Science Foundation (NSF)); National Geographic Society(National Geographic Society); Vanderbilt University Discovery Research program	Funding for this research was provided by the U.S. National Science Foundation (BCS 0914891), the National Geographic Society, Becky and Spence Wilson, and the Vanderbilt University Discovery Research program. The authors thank Elizabeth Chamberlain and two anonymous reviewers for their constructive feedback on the paper.	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Sci. Rev.	JAN 1	2020	227								106046	10.1016/j.quascirev.2019.106046	http://dx.doi.org/10.1016/j.quascirev.2019.106046			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Social Science Citation Index (SSCI)	Physical Geography; Geology	JW5MQ		Bronze			2023-06-23	WOS:000503096400005
J	Lopez, L; Barreto, MB; Ruaro Peralba, MD; Barreto-Pittol, E; Lo Monaco, S; Diaz, R				Lopez, Liliana; Barreto, Maria Beatriz; Ruaro Peralba, Maria do Carmo; Barreto-Pittol, Eduardo; Lo Monaco, Salvador; Diaz, Rut			ANALYSIS OF POLYCYCLIC AROMATIC HYDROCARBONS (PAH) IN SOIL OF MANGROVE FOREST OF THE VENEZUELAN CARIBBEAN COAST	REVISTA INTERNACIONAL DE CONTAMINACION AMBIENTAL			English	Article						Morrocoy National Park; Cuare Inlet; mangroves; soluble organic matter; GC-MS; PAHs diagnostic ratios	ORGANIC-CARBON; SEDIMENTS; IDENTIFICATION; ENVIRONMENT; LAKE; CONTAMINATION; FINGERPRINTS; ECOSYSTEMS; HABITATS; PROFILES	In order to identify the levels of contamination of mangrove soils by polycyclic aromatic hydrocarbons (PAH), their concentration was determined by gas chromatography coupled to mass spectrometry in the fraction of aromatic hydrocarbons obtained from soluble organic matter (SOM). Soils are located in Cuare Inlet and Morrocoy National Park from Venezuela, and samples were collected in Punta La Matica (PLM) and Tucacas Bay (ETU) respectively. Naphthalene, acenaphthene. acenaphthalene, benzo(ghi)perylene, dibenzo(ah)anthracene and indene have concentrations lower than the detection threshold for the technique employed (<= 20 ng/g). Fluorene, phenanthrene, anthracene, fluoranthene, pyrene, benzo(a)anthracene, cluysene, benzo(k)fluoranthene, benzo(b)fluoranthene and benzo(a)pyrene present concentrations ranging from 24 to 967 ng/g, and in some cases were not detected (<= 20 ng/g). The PAHs concentration are classified in a pollution level from moderate to high in ETU and low in PLM. These results indicate a major anthropogenic pollution level of soils from ETU in relation to PLM soils. Based on the fact that the PAHs detected are not substituted and dominate the 3- and 4-rings, three diagnostic ratios to identify the contamination source were calculated: [anthracene/(anthracene+phenanthrene), fluoranthene/(fluoranthene+pyrene); and benzo(a)anthracene/(benzo(a)anthracene+chrysene)]; these ratios suggest a source from combustion of organic matter. Additionally, the normalization of total PAHs related to total organic carbon (TOC) or SOM represents a linear relationship between total PAHs with PAH/TOC and PAH/SOM, and suggests that the PAHs detected are from the same source, that is, the combustion of organic matter from anthropogenic activity or natural fires.	[Lopez, Liliana; Barreto-Pittol, Eduardo; Lo Monaco, Salvador; Diaz, Rut] Univ Cent Venezuela, Inst Ciencias Tierra ICT, Lab Geoquim Organ, Fac Ciencias, Caracas 1053, Venezuela; [Barreto, Maria Beatriz; Barreto-Pittol, Eduardo] Univ Cent Venezuela, Inst Zool & Ecol Trop IZET, Lab Ecol Vegetac, Fac Ciencias, Caracas 1053, Venezuela; [Ruaro Peralba, Maria do Carmo] Univ Fed Rio Grande do Sul, Inst Quim, BR-96201900 Porto Alegre 474, RS, Brazil; [Diaz, Rut] Univ Fed Fluminense, Dept Geoquim, Inst Quim, BR-1151 Niteroi 16, RJ, Brazil	University of Central Venezuela; University of Central Venezuela; Universidade Federal do Rio Grande do Sul; Universidade Federal Fluminense	Lopez, L (autor correspondente), Univ Cent Venezuela, Inst Ciencias Tierra ICT, Lab Geoquim Organ, Fac Ciencias, Caracas 1053, Venezuela.	liliana.lopez@ciens.ucv.ve	Díaz, Rut/AAG-2748-2021	Díaz, Rut/0000-0003-1883-7231	Consejo de Desarrollo Cientifico y Humanistico of the Universidad Central de Venezuela (CDCH-UCV) [PG03-00-5884-2005/1, PG-03-00-5885-2005/1]; Fondo Nacional de Ciencia Tecnologia e Innovacion (FONACIT) [G-2012002299]	Consejo de Desarrollo Cientifico y Humanistico of the Universidad Central de Venezuela (CDCH-UCV); Fondo Nacional de Ciencia Tecnologia e Innovacion (FONACIT)	This work was funded by research grants from the Consejo de Desarrollo Cientifico y Humanistico of the Universidad Central de Venezuela (CDCH-UCV), under research grants: PG03-00-5884-2005/1 and PG-03-00-5885-2005/1 and the Fondo Nacional de Ciencia Tecnologia e Innovacion (FONACIT), under research grant G-2012002299.	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Int. Contam. Ambient.		2020	36	3					677	687		10.20937/RICA.53573	http://dx.doi.org/10.20937/RICA.53573			11	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	NA9HD		Bronze, Green Submitted			2023-06-23	WOS:000560126900014
J	Machado, CP; Coimbra, JC; Bergue, CT				Machado, Claudia Pinto; Coimbra, Joao Carlos; Bergue, Cristianini Trescastro			PROVINCIALITY OF OSTRACODA (CRUSTACEA) IN THE NORTHEASTERN AND EASTERN BRAZILIAN SHELVES BASED ON NEONTOLOGICAL AND PALEONTOLOGICAL ANALYSES	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						South Atlantic; biodiversity; Podocopida; neritic zone	ZOOGEOGRAPHICAL SIGNIFICANCE; FAMILY TRACHYLEBERIDIDAE; CONTINENTAL-SHELF; SOUTHERN; TAXONOMY; NORTHERN; GENUS; RIVER; MACROCYPRIDIDAE; CIRCULATION	This study analyzes the geographical distribution of 131 podocopid ostracod species recovered from the Brazilian continental shelf between Cabo de Sao Roque (lat. 05 degrees 30'S) and Cabo Frio (lat. 23 degrees S). This very large area corresponds to the northeastern and eastern Brazilian marine regions. The 104 samples studied were collected in water depths ranging from 12 to 110 m as part of the legs 4 and 7 of the REMAC Project. The cosmopolitan species, as well as those shared with the Caribbean and/or Gulf of Mexico region, represent a small part of the ostracods herein studied and it is assumed that their dispersion was prompted by processes linked to events of relative sea level changes during the Neogene and Quaternary. The fossil record of some species spans to the Neogene, mostly from the Atlantic coast of North and Central America, while one species has Tethyan origin. Three species known from the Neogene of the Caribbean have been recorded as relicts in the study area. From the 131 species herein identified, 36.5% are more widespread in temperate waters south of Cabo Frio town, 46.5% of warm waters north of Cabo Frio town, 4% are present only in the studied area, and 11.5% are rare and probably restricted to the E region. A new province - the Brazilian Province - is herein proposed based on the species occurrence.	[Machado, Claudia Pinto] Univ Caxias Sul, Ctr Ciencias Exatas Nat & Tecnol, Alameda Joao Dal Sasso 800, BR-95700000 Bento Goncalves, RS, Brazil; [Coimbra, Joao Carlos] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, CxP 15001, BR-91501970 Porto Alegre, RS, Brazil; [Bergue, Cristianini Trescastro] Univ Fed Rio Grande do Sul, Dept Interdisciplinar, Campus Litoral Norte,Rodovia RS 030,Km 92, BR-95590000 Tramandai, RS, Brazil	Universidade de Caxias do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Machado, CP (autor correspondente), Univ Caxias Sul, Ctr Ciencias Exatas Nat & Tecnol, Alameda Joao Dal Sasso 800, BR-95700000 Bento Goncalves, RS, Brazil.	machadocpm@gmail.com; joao.coimbra@ufrgs.br; ctbergue@gmail.com	Coimbra, Joao Carlos/H-7500-2013	Coimbra, Joao Carlos/0000-0002-8980-6531; Machado, Claudia/0000-0001-7390-3268; Bergue, Cristianini/0000-0002-5007-3131	National Council for Scientific and Technological Development (CNPq) [305128/2017-5]	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We are thankful to Petroleo Brasileiro S.A. (Petrobras) for providing the samples and to Professor A.L. Carreno (UNAM/Mexico) for her suggestions and criticism in an early version of this paper. We offer special thanks to Dr. D. Ceolin and Professor F. Sciuto for providing useful comments for improving this work. J. C. C. gratefully acknowledges the National Council for Scientific and Technological Development (CNPq) for financial support (proc. 305128/2017-5).	Aiello Giuseppe, 2004, Bollettino della Societa Paleontologica Italiana, V43, P71; ALLISON E C, 1971, Transactions of the San Diego Society of Natural History, V16, P165; Sartori LAA, 2010, REV BRAS PALEONTOLOG, V13, P115, DOI 10.4072/rbp.2010.2.04; Bergue CT, 2016, ZOOTAXA, V4079, P65, DOI 10.11646/zootaxa.4079.1.5; Bergue CT, 2002, NEUES JAHRB GEOL P-M, P659; Bertels Alwine, 1997, Revista Espanola de Micropaleontologia, V29, P29; Bold W. 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Bras. Paleontol.	JAN-MAR	2020	23	1					3	31		10.4072/rbp.2020.1.01	http://dx.doi.org/10.4072/rbp.2020.1.01			29	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	MO4QM					2023-06-23	WOS:000551512700001
J	Massuda, AJ; Hartmann, LA; Queiroga, GN; de Castro, MP; Leandro, CG; Savian, JF				Massuda, Amanda Juliano; Hartmann, Leo Afraneo; Queiroga, Glaucia Nascimento; de Castro, Marco Paulo; Leandro, Carolina Goncalves; Savian, Jairo Francisco			Mineralogical evolution of the northern Bossoroca ophiolite, Sao Gabriel terrane	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Bossoroca ophiolite; chromite-talc-magnesite granofels; tourmalinite; metasomatism; aerogeophysics	PB-HF ISOTOPES; BRASILIANO OROGEN; NEOPROTEROZOIC OPHIOLITES; JUVENILE ACCRETION; SOUTHERN BRAZIL; ZIRCON; BELT; TOURMALINE; SHIELD; MA	Mineralogical evolution of ophiolites is significant to understand paleo-oceanic crust and mantle requiring multi-proxy techniques to identify steps in the processes. We studied the Bossoroca ophiolite from the southern Brasiliano Orogen, a prime example of Tonian accretion to an oceanic island arc. Integration of field geology, aeromagnetometry, aerogamaspectrometry, electron microprobe analyses, and compositional maps of minerals led to the decoding of oceanic and continental processes. The ophiolite is highly magnetic and low-K and is positioned at the base of the superstructure. We studied amphibolite, tourmalinite, and chromite-talc-magnesite granofels from the ophiolite, Capivaras diorite from the Cambai Complex infrastructure and one metavolcanoclastic rock from the Vacacai Group superstructure. Honblende is zoned in all rock types. Low-Ti hornblende is compatible with medium-pressure metamorphism at 7 kbar. This M1 to M2 amphibolite facies resulted in the widespread association of olivine + talc in metaserpentinite. Dravite is similar to tourmaline from the Ibare ophiolite. Andesine and oligoclase are dominant and albite minor. Cr-spinel in granofels recrystallized in greenschist facies; host rock originated by carbonatization of serpentinite formed in the oceanic crust along with chloritite and tourmalinite. Serpentinite rare earth elements (REE) suggest origin in depleted mantle peridotite. The ophiolite evolved in the Adamastor Ocean until incorporation into the island arc.	[Massuda, Amanda Juliano; Hartmann, Leo Afraneo; Leandro, Carolina Goncalves; Savian, Jairo Francisco] Univ Fed Rio Grande do Sul, Porto Alegre, RS, Brazil; [Queiroga, Glaucia Nascimento; de Castro, Marco Paulo] Univ Fed Ouro Preto, Ouro Preto, MG, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal de Ouro Preto	Hartmann, LA (autor correspondente), Univ Fed Rio Grande do Sul, Porto Alegre, RS, Brazil.	amanda.juliano027@gmail.com; leo.hartmann@ufrgs.br; glauciaqueiroga@yahoo.com.br; marco_pcastro@yahoo.com; carolina.leandro@ufrgs.br; jairo.savian@ufrgs.br	Hartmann, Léo A/D-7663-2013; Queiroga, Gláucia/AAJ-1823-2021; Savian, Jairo Francisco/J-4782-2015	Hartmann, Léo A/0000-0001-7863-5071; Queiroga, Gláucia/0000-0002-1730-0638; Savian, Jairo Francisco/0000-0002-5032-3217; Massuda, Amanda/0000-0001-8567-161X; de Castro, Marco Paulo/0000-0001-8209-5995; Leandro, Carolina/0000-0003-0371-4511	Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (CNPq) - Brazilian Government; CNPq; Laboratorio de Microscopia e Microanalises (LMIc) of UFOP, a member of FAPEMIG	Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (CNPq) - Brazilian Government(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Fundacao de Apoio a Pesquisa do Distrito Federal (FAPDF)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Laboratorio de Microscopia e Microanalises (LMIc) of UFOP, a member of FAPEMIG	We acknowledge support in the field by Tiara Cerva Alves, Mariana Werle, and Vitor Casagrande Dias. Amanda J. Massuda thanks Conselho Nacional do Desenvolvimento Cientifico e Tecnologico (CNPq) - Brazilian Government for MS scholarship. This study led to the Master of Science degree of Massuda at Programa de Pos-Graduacao em Geociencias, Universidade Federal do Rio Grande do Sul. Hartmann received systematic financial support, research scholarship, and grant from CNPq. Queiroga is a fellow of CNPq and acknowledges its support. The authors are also grateful to the Laboratorio de Microscopia e Microanalises (LMIc) of UFOP, a member of FAPEMIG-supported Microscopy and Microanalysis Network of Minas Gerais. We thank Geological Survey of Brazil (CPRM) for the aerogeophysical data. Fabricio Caxito and one anonymous reviewer made significant contributions to the improvement of the article.	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J. Geol.		2020	50	4							e20190120	10.1590/2317-4889202020190120	http://dx.doi.org/10.1590/2317-4889202020190120			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	QF2BI		gold, Green Published			2023-06-23	WOS:000616704000001
J	Melo, JC; Carvalho, WC; Morte, ESB; Araujo, RGO; Santos, DCMB				Melo, Joelem Carvalho; Carvalho, Wellington Correia; Boa Morte, Elane S.; Araujo, Rennan Geovanny O.; Santos, Daniele Cristina M. B.			Sequential Determination of Cd, Co, Cu, Fe, Mg, Mn, Ni, Pb, and Zn in Powdered Refreshments by FS-F AAS After a Simple Sample Treatment	FOOD ANALYTICAL METHODS			English	Article						Refreshment powdered; Inorganic constituents; FS-F AAS; Experimental design	FRUIT JUICES; OPTIMIZATION	In this work, a procedure is proposed for the direct analysis of powdered refreshments by fast sequential flame atomic absorption spectrometry (FS-F AAS), after a simple treatment of the sample. A full 2(3) factorial design was applied, and the variables chosen were as follows: acid concentration, acid type, and sonication time. Optimization provided the best conditions considering a mass of powdered refreshment of about 0.18 g diluted to a final volume of 15 mL with 0.5 mol L-1 HCl. The matrix effect was investigated, and external calibration was feasible for the determination of Cd, Co, Cu, Fe, Mg, Mn, Ni, Pb, and Zn. The limit of quantification (LoQ) obtained was between 0.6 (Cd) and 25 mg kg(-1) (Pb). The analyte addition and recovery test were applied to evaluate the accuracy, and recovery percentage values ranging from 83.9 to 109.7% were obtained, which is considered adequate for quantitative analysis. Precision was expressed as relative standard deviation (% RSD); it was less than or equal to 5.0% (n = 7) for all analytes. The procedure was applied to 21 samples of powdered refreshment commercialized in Salvador (Brazil) and Buenos Aires (Argentina). The concentration range and average of the analytes in the samples (in mg kg(-1)) commercialized in Brazil (BZ) and Argentina (AG) were as follows: Co (BZ < 6.4-9.94, average 8.85; AG < 6.4-10.3, average 9.92), Fe (BZ < 6.9-376, average 270; AG < 6.9-32.81, average 29.11), Mg (BZ < 8.9-363, average 140; AG 770-3139, average 1464), Mn (BZ < 3.2-4.88, average 4.24; AG < 6.9), and Zn (BZ < 1.4-1.68, average 1.68; AG < 1.4). The concentrations of Cd, Cu, Ni, and Pb were lower than the LoQ of the proposed analytical method. For refreshment samples commercialized in Buenos Aires (Argentina), high concentrations of Mg were found in their chemical composition, but Mg had been used as anti-caking agent along with the other components.	[Melo, Joelem Carvalho; Carvalho, Wellington Correia; Araujo, Rennan Geovanny O.; Santos, Daniele Cristina M. B.] Univ Fed Bahia, Inst Quim, Dept Quim Analit, BR-40170115 Salvador, BA, Brazil; [Carvalho, Wellington Correia] Inst Fed Educ Ciencia & Tecnol Bahia IFBA, Campus Porto Seguro, BR-45810000 Porto Seguro, BA, Brazil; [Boa Morte, Elane S.] Inst Fed Educ Ciencia & Tecnol Baiano IFBAIANO, Campus Catu, BR-48110000 Catu, BA, Brazil; [Araujo, Rennan Geovanny O.] Univ Fed Bahia, INCT Energia & Ambiente, CNPq, Inst Nacl Ciencia & Tecnol, BR-40170270 Salvador, BA, Brazil	Universidade Federal da Bahia; Instituto Federal da Bahia (IFBA); Instituto Federal Baiano (IFBAIANO); Universidade Federal da Bahia	Santos, DCMB (autor correspondente), Univ Fed Bahia, Inst Quim, Dept Quim Analit, BR-40170115 Salvador, BA, Brazil.	dc.muniz@yahoo.com.br	SANTOS, DANIELE CRISTINA M. B./AAI-9455-2021	SANTOS, DANIELE CRISTINA M. B./0000-0002-9106-8494; OLIVEIRA ARAUJO, RENNAN GEOVANNY/0000-0001-6955-8115; Carvalho de Melo, Joelem/0000-0002-7361-6055				Agencia Nacional de Vigilancia Sanitaria. (ANVISA), 2017, 166 ANVISA RDC, P1; ANVISA, 2004, ANVISA CONS PUBL, V80; Brandao GC, 2010, TALANTA, V81, P1357, DOI 10.1016/j.talanta.2010.02.033; Campos E. M. F. de, 2010, Arquivos de Ciencias da Saude da UNIPAR, V14, P11; Damodaram S, 2010, QUIMICA ALIMENTOS FE; de Assis RA, 2008, QUIM NOVA, V31, P1948, DOI 10.1590/S0100-40422008000800006; de Oliveira E, 2003, J BRAZIL CHEM SOC, V14, P174, DOI 10.1590/S0103-50532003000200004; de Sousa CP, 2006, REV APS, V9, P83; Ferrarezi AC, 2010, REV NUTR, V23, P667, DOI 10.1590/S1415-52732010000400016; Ferreira SLC, 2007, ANAL CHIM ACTA, V597, P179, DOI 10.1016/j.aca.2007.07.011; Ferreira S.L.C., 2015, INTRO TECNICAS PLANE, V1st; Froes RES, 2009, MICROCHEM J, V92, P68, DOI 10.1016/j.microc.2008.12.008; Galuch MB, 2018, J BRAZIL CHEM SOC, V29, P748, DOI 10.21577/0103-5053.20170197; King T, 2017, TRENDS FOOD SCI TECH, V68, P160, DOI 10.1016/j.tifs.2017.08.014; Krug F. 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Technol (Campinas), V26, P98, DOI 10.1590/S0101-20612006000100017; Pinho GP, 2009, QUIM NOVA, V32, P987, DOI 10.1590/S0100-40422009000400030; Projahn HD, 2004, ANAL BIOANAL CHEM, V378, P1083, DOI 10.1007/s00216-003-2200-y; Ribani M, 2004, QUIM NOVA, V27, P771, DOI 10.1590/S0100-40422004000500017; Santos JS, 2011, MICROCHEM J, V97, P113, DOI 10.1016/j.microc.2010.08.002; Silva CS, 2002, QUIM NOVA, V25, P1194, DOI 10.1590/S0100-40422002000700022; Szymczycha-Madeja A, 2014, TRAC-TREND ANAL CHEM, V55, P68, DOI 10.1016/j.trac.2013.12.005; Szymczycha-Madeja A, 2013, FOOD CHEM, V141, P3466, DOI 10.1016/j.foodchem.2013.06.067; Tormen L, 2011, J FOOD COMPOS ANAL, V24, P95, DOI 10.1016/j.jfca.2010.06.004	29	9	9	0	17	SPRINGER	NEW YORK	ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES	1936-9751	1936-976X		FOOD ANAL METHOD	Food Anal. Meth.	JAN	2020	13	1			SI		212	221		10.1007/s12161-019-01589-2	http://dx.doi.org/10.1007/s12161-019-01589-2			10	Food Science & Technology	Science Citation Index Expanded (SCI-EXPANDED)	Food Science & Technology	KJ3SW					2023-06-23	WOS:000511978600024
J	Santos, LCMD; Lima, HM; Lages, GD; Caxito, FD; Neto, JFD; Guimaraes, ID				Montefalco de Lira Santos, Lauro Cezar; Lima, Haroldo Monteiro; Lages, Geysson de Almeida; Caxito, Fabricio de Andrade; de Araujo Neto, Jose Ferreira; Guimaraes, Ignez de Pinho			Petrogenesis of the Riacho do Ico Stock: evidence for Neoproterozoic slab melting during accretion tectonics in the Borborema Province?	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Arc-related to syn-collisional magmatism; possible slab melting episode; accretion tectonics	CONTINENTAL ARC MAGMATISM; ALTO MOXOTO TERRANE; HF ZIRCON DATA; NE BRAZIL; NORTHEAST BRAZIL; WEST GONDWANA; EXPERIMENTAL CONSTRAINTS; GRANITIC MAGMATISM; TRANSVERSAL ZONE; PLUTONIC ROCKS	One of the main characteristics of the Borborema Province in northeastern Brazil is the abundance of granitic domains. The Lagoa das Pedras plutonic-volcanic Complex record remnants of early to late Neoproterozoic primitive to highly evolved magmas. U-Pb SHRIMP determinations and whole-rock geochemistry on the granitic to granodioritic Riacho do Ico Stock, which is the largest plutonic body of this complex, were conducted. Zircon dating reveals that this body was intruded in the crust at 607 +/- 3 Ma, whereas metamorphic overgrowths are coeval within uncertainty (600 +/- 8 Ma). Geochemical characteristics of this stock suggest that it corresponds to Cordilleran-type magmas injected in the lithosphere above a subduction zone. Sr and Y contents in addition to MgO and SiO2 values are compatible with high-silica adakite-like magmas, interpreted as the result of slab melting in deep-seated regions. Based on the integration of this study and literature data, we suggest that the Riacho do Ico intrusion might be a dismembered part of a major continental magmatic arc described in the Central Subprovince of the Borborema Province, marking the onset of the accretionary stage of the Brasiliano orogeny.	[Montefalco de Lira Santos, Lauro Cezar; de Araujo Neto, Jose Ferreira; Guimaraes, Ignez de Pinho] Univ Fed Pernambuco, Recife, PE, Brazil; [Lima, Haroldo Monteiro; Guimaraes, Ignez de Pinho] Univ Fed Ceara, Fortaleza, Ceara, Brazil; [Lages, Geysson de Almeida] Serv Geol Brasil, Recife, PE, Brazil; [Caxito, Fabricio de Andrade] Univ Fed Minas Gerais, Belo Horizonte, MG, Brazil	Universidade Federal de Pernambuco; Universidade Federal do Ceara; Universidade Federal de Minas Gerais	Santos, LCMD (autor correspondente), Univ Fed Pernambuco, Recife, PE, Brazil.	lauromontefalco@gmail.com; harolgogeologo@gmail.com; geysson.lages@cprm.gov.br; facaxito@yahoo.com.br; araujoneto.geo@gmail.com; ignez@ufpe.br	de Lira Santos, Lauro Cézar Montefalco/E-5536-2015; Monteiro Lima, Haroldo/GPG-1946-2022; Caxito, Fabricio A/J-1317-2016; de Almeida Lages, Geysson A/C-9314-2014	de Lira Santos, Lauro Cézar Montefalco/0000-0001-6098-1873; Caxito, Fabricio A/0000-0002-0335-3667; de Almeida Lages, Geysson A/0000-0001-7041-4944; Monteiro Lima, Haroldo/0000-0002-9744-7997; Araujo Neto, Jose Ferreira de/0000-0002-1780-9469	National Institute of Science and Technology for Tectonic Studies (INCT), Brazil	National Institute of Science and Technology for Tectonic Studies (INCT), Brazil	This paper is kindly dedicated to the memory of Edilton Jose dos Santos, known as "professor". The Riacho do Ico Stock represents one of his many geological curiosities and the authors are pleased for the opportunity to add information on the knowledge of the Borborema Province granites. Part of the geochemical data was obtained in the NEG-LABISE laboratory and we kindly appreciate the lab staff. We would like to thank Alcides Sial, Valderez Ferreira and Claudio Riccomini for the opportunity and the reviewers for their suggestions. This research was funded by the National Institute of Science and Technology for Tectonic Studies (INCT), Brazil.	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J. Geol.		2020	50	2							e20190127	10.1590/2317-4889202020190127	http://dx.doi.org/10.1590/2317-4889202020190127			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MP8BO		Green Published, gold			2023-06-23	WOS:000552425200001
J	Oliveira, LB; dos Santos, WPC; Teixeira, LSG; Korn, MGA				Oliveira, Luciane B.; dos Santos, Wagna P. C.; Teixeira, Leonardo S. G.; Korn, Maria Gracas A.			Direct Analysis of Cocoa Powder, Chocolate Powder, and Powdered Chocolate Drink for Multi-element Determination by Energy Dispersive X-ray Fluorescence Spectrometry	FOOD ANALYTICAL METHODS			English	Article						Cocoa powder; Chocolate powder; Powdered chocolate drink; Inorganic constituents; Direct analysis; EDXRF	INDUCED BREAKDOWN SPECTROSCOPY; TRACE-ELEMENTS; NI; PRECONCENTRATION; CADMIUM; IONS; LEAD; IRON; ZN; CU	The aim of this study was to evaluate the potential of applying energy dispersive X-ray fluorescence (EDXRF) spectrometry to determine Ca, K, P, Mg, Fe, Zn, Cu, Mn, and Al concentrations for direct analysis of cocoa powder, chocolate powder, and powdered chocolate drink samples. The proposed method was calibrated using samples previously analyzed by inductively coupled plasma optical emission spectrometry (ICP OES). For comparison purposes, the samples were also analyzed by ICP OES after an acid digestion procedure, and no significant differences were observed between the concentrations determined by EDXRF when compared to those by ICP OES. The coefficients of correlation (R) from the calibration curves and the limit of quantification (mg kg(-1)) were Ca (0.996, 0.030), K (0.985, 68), Mg (0.974, 0.020), P (0.986, 0.50), Mn (0.998, 3.6), Fe (0.981, 2.5), Cu (0.978, 1.3), Zn (0.996, 0.80), and Al (0.983, 7.5). The precisions obtained for the elements were between 1.5 and 7.8% (n = 7), indicating that the preparation of the pellets was efficient to perform analysis by EDXRF. Potassium was the macro-mineral with higher concentrations in the samples. In relation to the micro-minerals, Fe had the greatest concentration. Significant concentrations of Al were also found. It was found that, in general, samples of chocolate powder and powdered chocolate drink may be considered good sources for the ingestion of Mg, Mn, Ca, K, P, Fe, Zn, and Cu.	[Oliveira, Luciane B.; dos Santos, Wagna P. C.; Teixeira, Leonardo S. G.; Korn, Maria Gracas A.] Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Oliveira, Luciane B.] Inst Fed Alagoas, Campus Penedo, BR-57200000 Penedo, Alagoas, Brazil; [dos Santos, Wagna P. C.] Inst Fed Educ Ciencia & Tecnol Bahia, Dept Quim, Campus Salvador, BR-40300010 Salvador, BA, Brazil; [Teixeira, Leonardo S. G.; Korn, Maria Gracas A.] Univ Fed Bahia, Inst Quim, INCT Energia & Ambiente, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Instituto Federal de Alagoas (IFAL); Instituto Federal da Bahia (IFBA); Universidade Federal da Bahia	Korn, MGA (autor correspondente), Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.; Korn, MGA (autor correspondente), Univ Fed Bahia, Inst Quim, INCT Energia & Ambiente, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.	korn@ufba.br	Teixeira, Leonardo S G/J-9131-2016; Korn, Maria Graças/AAH-3445-2020; Santos, Wagna Piler/N-2337-2017; Santos, Wagna/ABB-3281-2020	Teixeira, Leonardo S G/0000-0003-0320-8299; Santos, Wagna Piler/0000-0001-7494-5179; Santos, Wagna/0000-0001-7494-5179				Andrey D, 2018, SPECTROCHIM ACTA B, V148, P137, DOI 10.1016/j.sab.2018.06.014; Association of official analytical chemists international-AOAC, 2016, GUID STAND METH PERF, P2; Bartos A, 2014, FOOD RES INT, V55, P412, DOI 10.1016/j.foodres.2013.11.044; Bertin E.P., 2012, PRINCIPLES PRACTICE; Bondy SC, 2014, TOXICOLOGY, V315, P1, DOI 10.1016/j.tox.2013.10.008; Brito GB, 2017, MICROCHEM J, V134, P35, DOI 10.1016/j.microc.2017.05.001; Costa VC, 2019, FOOD CHEM, V273, P91, DOI 10.1016/j.foodchem.2018.02.016; Crozier SJ, 2011, CHEM CENT J, V5, DOI 10.1186/1752-153X-5-5; Gallardo H, 2016, J FOOD COMPOS ANAL, V50, P1, DOI 10.1016/j.jfca.2016.04.007; Gothankar SS, 2009, SCI TOTAL ENVIRON, V407, P2868, DOI 10.1016/j.scitotenv.2009.01.014; Hartwig A, 2017, BUNDESGESUNDHEITSBLA, V60, P715, DOI 10.1007/s00103-017-2567-0; Hartwig CA, 2016, J ANAL ATOM SPECTROM, V31, P523, DOI [10.1039/c5ja00388a, 10.1039/C5JA00388A]; Herreros-Chavez L, 2019, FOOD CHEM, V278, P373, DOI 10.1016/j.foodchem.2018.11.065; Jenkins R, 1995, QUANTITATIVE XRAY SP; Kaur J, 2016, AIP CONF PROC, V1728, DOI 10.1063/1.4946401; Krug F. 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Meth.	JAN	2020	13	1			SI		195	202		10.1007/s12161-019-01565-w	http://dx.doi.org/10.1007/s12161-019-01565-w			8	Food Science & Technology	Science Citation Index Expanded (SCI-EXPANDED)	Food Science & Technology	KJ3SW					2023-06-23	WOS:000511978600022
J	Paula-Santos, GM; Caetano, S; Enzweiler, J; Navarro, MS; Babinski, M; Guacaneme, C; Kuchenbecker, M; Reis, H; Trindade, RIF				Paula-Santos, Gustavo Macedo; Caetano-Filho, Sergio; Enzweiler, Jacinta; Navarro, Margareth S.; Babinski, Marly; Guacaneme, Cristian; Kuchenbecker, Matheus; Reis, Humberto; Trindade, Ricardo I. F.			Rare earth elements in the terminal Ediacaran Bambui Group carbonate rocks (Brazil): evidence for high seawater alkalinity during rise of early animals	PRECAMBRIAN RESEARCH			English	Article						Late Ediacaran; Chemostratigraphy; Alkalinity; Biomineralization; Rare earth elements	SAO-FRANCISCO CRATON; PROTEROZOIC NAMA GROUP; LAGOAS CAP CARBONATE; TRACE-ELEMENT; NEOPROTEROZOIC LIMESTONES; DIAGENETIC CONSTRAINTS; ISOTOPE STRATIGRAPHY; FOREBULGE GRABENS; CERIUM ANOMALIES; METAZOAN REEFS	Rare earth elements plus yttrium (REY) mass fractions of ancient carbonate rocks are used to track changes in chemistry of past seawater. Here we investigate REY patterns in two carbonate sections from the Ediacaran Bambui Group, Sao Francisco Basin (Brazil), which comprise its two lowermost transgressive-regressive second order sedimentary sequences. Shale normalised distributions vary with the sequence stratigraphy framework. In the basal 2nd-order sequence, carbonate samples from the basal sequence transgressive systems tract display light REY (LREY) distributions slightly depleted to enriched that reflect input of freshwater, possibly in a post glacial episode. Upwards, carbonate rocks from the early highstand systems tract (EHST) yielded LREY enriched distributions, which progressively turns into LREY shale normalized depleted distributions on samples from the late highstand systems tract (LHST). This portion of the sequence also displays Y positive anomaly in some cases. Carbonate samples from the upper second-order sequence do not display coherent patterns. Ce/Ce* values > 1 in most samples throughout the two sections suggest permanent anoxia of seawater. The REY change from the EHST to LHST in the basal sequence marks an important paleoenvironmental overturn in the basin, with increasing alkalinity in seawater driving REY fractionation and LREY depletion. Confinement of the basin in the inner areas of West Gondwana due the uplift of marginal neoproterozoic orogens probably changed the weathering style of source areas to more congruent, thus delivering a higher ionic influx to a restricted setting, increasing alkalinity during LHST. Cloudina sp. fragments were reported in this stage of the Bambui Group and in carbonate rocks with high Sr mass fractions in other West Gondwana basins, supporting the hypothesis that the high alkalinity of seawater during late Ediacaran may have driven the appearance of the first biomineralizing organisms.	[Paula-Santos, Gustavo Macedo; Enzweiler, Jacinta; Navarro, Margareth S.] Univ Estadual Campinas, Inst Geociencias, Rua Carlos Gomes 250, BR-13083855 Campinas, SP, Brazil; [Caetano-Filho, Sergio; Babinski, Marly; Guacaneme, Cristian] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Kuchenbecker, Matheus] Univ Fed Vales Jequitinhonha & Mucuri, Inst Ciencia & Tecnol, Lab Estudos Tecton, Rodovia MGT 367,Km 583, BR-39100000 Diamantina, MG, Brazil; [Reis, Humberto] Univ Fed Ouro Preto, Dept Geol, Escola Minas, Lab Modelagem Tecton, Campus Morro Cruzeiro, BR-35400000 Ouro Preto, MG, Brazil; [Trindade, Ricardo I. F.] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226, BR-05508090 Sao Paulo, SP, Brazil; [Kuchenbecker, Matheus] Univ Fed Minas Gerais, Ctr Pesquisas Prof Manoel Teixeira da Costa, Av Antonio Carlos 6627, BR-66273127 Belo Horizonte, MG, Brazil	Universidade Estadual de Campinas; Universidade de Sao Paulo; Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM); Universidade Federal de Ouro Preto; Universidade de Sao Paulo; Universidade Federal de Minas Gerais	Paula-Santos, GM (autor correspondente), Univ Estadual Campinas, Inst Geociencias, Rua Carlos Gomes 250, BR-13083855 Campinas, SP, Brazil.	gustavomps@ige.unicamp.br	Babinski, Marly/B-9403-2013; Trindade, Ricardo IF/A-8146-2008; Reis, Humberto L S/P-9902-2016; Kuchenbecker, Matheus/P-9876-2016; Navarro, Margareth/HZJ-6051-2023; Filho, Sergio Caetano/H-3687-2016; Navarro, Margareth Sugano/Q-8244-2017; Enzweiler, Jacinta/B-9023-2012; Paula-Santos, Gustavo/G-7502-2015	Babinski, Marly/0000-0003-2444-2404; Trindade, Ricardo IF/0000-0001-9848-9550; Reis, Humberto L S/0000-0002-7675-789X; Kuchenbecker, Matheus/0000-0003-2974-839X; Navarro, Margareth Sugano/0000-0002-6054-2261; Enzweiler, Jacinta/0000-0003-2214-7356; Caetano Filho, Sergio/0000-0002-1631-5096; Paula-Santos, Gustavo/0000-0001-9630-1243	Sao Paulo Research Foundation (FAPESP) [2016/06114-6]; Brazilian Research Council [400764/2016-4]; FAPESP [2017/00399-1, 2016/11499-5]	Sao Paulo Research Foundation (FAPESP)(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Brazilian Research Council; FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP))	The authors would like to thank both anonymous reviewers that helped improve the manuscript. Sao Paulo Research Foundation (FAPESP; grant #2016/06114-6; Thematic Project) and Brazilian Research Council (grant #400764/2016-4) provided support and funding for the analyses. G.M.P.S and S.C.F. hold FAPESP scholarships (grants #2017/00399-1 and #2016/11499-5, respectively). M.B., R.T., M.K. and J.E. are fellows of the Brazilian Research Council (#307563/2013-8, #206997/2014-0, #309106/2017-6, and #311973/2017-5, respectively).	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JAN	2020	336								105506	10.1016/j.precamres.2019.105506	http://dx.doi.org/10.1016/j.precamres.2019.105506			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KE7RK					2023-06-23	WOS:000508748600012
J	Pinel, S; Bonnet, MP; Da Silva, JS; Sampaio, TC; Garnier, J; Catry, T; Calmant, S; Fragoso, CR; Moreira, D; Marques, DM; Seyler, F				Pinel, Sebastien; Bonnet, Marie-Paule; Da Silva, Joecila S.; Sampaio, Tania C.; Garnier, Jeremie; Catry, Thibault; Calmant, Stephane; Fragoso, Carlos R., Jr.; Moreira, Daniel; Marques, David Motta; Seyler, Frederique			Flooding Dynamics Within an Amazonian Floodplain: Water Circulation Patterns and Inundation Duration	WATER RESOURCES RESEARCH			English	Article							RADAR ALTIMETRY; RIVER-FLOODPLAIN; BASIN; VEGETATION; LAKE; DIVERSITY; HYDROLOGY; WETLANDS; ENVISAT; EXTENT	Flooding dynamics across a medium-size (Janauaca Lake, 786 km(2)) floodplain system along the Amazon/Solimoes River over a 9-year period (2006-2015) is studied through integration of remote sensing and limited in situ data in hydrologic-hydrodynamic modelling based on Telemac-2D model. Model accuracy varies through the hydrological year. We focus on seasonal and interannual spatial variability of water circulation and inundation duration. We highlight strong heterogeneities in water velocity magnitude between the different morphological domains of the floodplain, the highest velocities being encountered in the river-floodplain channel. In addition to topography, we emphasize the importance of the main channel and the local runoff in controlling the water circulation, at least during part of the hydrological year. From low water to early rising period, local runoff constrains the river incursion across the floodplain, while the rates of main channel rising/receding controls the flood duration. The comparison of several hydrological years highlights the interannual changes of these hydraulic controls and also the influence exerted by prior inundation conditions. While we observed few changes in water velocity distribution among hydrological years, the inundation duration is highly variable. Usually defined by maximum water level, extreme flood events may paradoxically induce positive (up to 40 days) but also negative (up to -20 days) anomalies of inundation duration.	[Pinel, Sebastien; Da Silva, Joecila S.; Sampaio, Tania C.] Amazon State Univ UEA, Lab Water Resources & Space Altimetry Amazon RHAS, Manaus, Amazonas, Brazil; [Pinel, Sebastien; Bonnet, Marie-Paule; Da Silva, Joecila S.; Sampaio, Tania C.; Garnier, Jeremie; Calmant, Stephane; Seyler, Frederique] Univ Brasilia UnB, Res Inst Dev IRD, Int Joint Lab LMI OCE Observ Changements Environn, Campus Darcy Ribeiro, Brasilia, DF, Brazil; [Pinel, Sebastien] Permanently Engn Sch Ales IMT Ales, Lab Ind Environm Engn LGEI, Ales, France; [Bonnet, Marie-Paule; Catry, Thibault; Seyler, Frederique] Espace DEV Res Inst Dev IRD, Maison Teledetect, UMR 228, Montpellier, France; [Garnier, Jeremie] Univ Brasilia UnB, Inst Geosci LAGEQ, Campus Darcy Ribeiro, Brasilia, DF, Brazil; [Calmant, Stephane] LEGOS Res Inst Dev IRD, UMR 5566, Toulouse, France; [Fragoso, Carlos R., Jr.] Fed Univ Alagoas UFAL, Ctr Technol, Maceio, Alagoas, Brazil; [Moreira, Daniel] Geol Survey Brazil CPRM, Rio De Janeiro, Brazil; [Marques, David Motta] Fed Univ Rio Grande Sul UFRGS, Hydraul Res Inst IPH, Porto Alegre, RS, Brazil	Universidade do Estado do Amazonas; Universidade de Brasilia; IMT - Institut Mines-Telecom; IMT Mines Ales; Universite de Montpellier; Universidade de Brasilia; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Toulouse; Universite Toulouse III - Paul Sabatier; Institut de Recherche pour le Developpement (IRD); Laboratoire d'Etudes en Geophysique et oceanographie spatiales; Universidade Federal de Alagoas; Universidade Federal do Rio Grande do Sul	Pinel, S (autor correspondente), Amazon State Univ UEA, Lab Water Resources & Space Altimetry Amazon RHAS, Manaus, Amazonas, Brazil.; Pinel, S; Bonnet, MP (autor correspondente), Univ Brasilia UnB, Res Inst Dev IRD, Int Joint Lab LMI OCE Observ Changements Environn, Campus Darcy Ribeiro, Brasilia, DF, Brazil.; Pinel, S (autor correspondente), Permanently Engn Sch Ales IMT Ales, Lab Ind Environm Engn LGEI, Ales, France.; Bonnet, MP (autor correspondente), Espace DEV Res Inst Dev IRD, Maison Teledetect, UMR 228, Montpellier, France.	sebpinel@gmail.com; marie-paule.bonnet@ird.fr	Da SILVA, Joecila Santos/B-1478-2014; Júnior, Carlos Ruberto Fragoso/I-8538-2019; Bonnet, Marie-Paule/J-6888-2016; Seyler, Frédérique/D-5518-2011; garnier, jeremie/AAK-8470-2021; PINEL, Sebastien/R-1310-2017	Júnior, Carlos Ruberto Fragoso/0000-0002-5853-6030; Bonnet, Marie-Paule/0000-0002-3950-4041; Seyler, Frédérique/0000-0002-3609-7524; garnier, jeremie/0000-0001-9571-7933; PINEL, Sebastien/0000-0001-9608-754X; da Motta Marques, David/0000-0002-3809-8053	CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, Brazil); IRD (Institut de Recherche pour le Developpement, France) [490634/2013-3]; LMI OCE (Laboratoire Mixte International Observatoire des Changements Environementaux); CNES/TOSCA; OSCA-Varz [CNPq-MCTI 400029/2015-4]; INCT ODISSEIA (CNPq/CAPES/FAP-DF) [16-2014]; European Union Horizon 2020 Research and innovation program under the Marie Sklodowska-Curie Grant [691053]; CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) in Brazil from the Guyamazon program - FAPEAM/IRD/French Embassy	CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, Brazil)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); IRD (Institut de Recherche pour le Developpement, France); LMI OCE (Laboratoire Mixte International Observatoire des Changements Environementaux); CNES/TOSCA; OSCA-Varz; INCT ODISSEIA (CNPq/CAPES/FAP-DF); European Union Horizon 2020 Research and innovation program under the Marie Sklodowska-Curie Grant; CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) in Brazil from the Guyamazon program - FAPEAM/IRD/French Embassy	Meteorological data and main channel stage were obtained from the Brazilian National Water Agency (http://hidroweb.ana.gov.br/) and the Brazilian national meteorological institute (www.inmet.gov.br/).Remotely sensed product can be freely assessed (i) at the Alaska Satellite Facility website (https://vertex.daac.asf.alaska.edu/) for the ALOS-1/PALSAR images and (ii) at the Center for Topographic studies of the Ocean and Hydrosphere (http://ctoh.legos.obsmip.fr/) website for the altimetry data. The processed data used in this work, including observations of floodplain stage, channel velocity exchanges, and bathymetry data, can be accessed through the following link (https://doi.org/10.17632/hvvpbnt8r3.1).This research was done under the auspices of CNPq (Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, Brazil) and IRD (Institut de Recherche pour le Developpement, France) 490634/2013-3, and LMI OCE (Laboratoire Mixte International Observatoire des Changements Environementaux). Several research programs supported it: (CNES/TOSCA), (OSCA-Varz) CNPq-MCTI 400029/2015-4, INCT ODISSEIA (Grant 16-2014 with funding from CNPq/CAPES/FAP-DF) and from the European Union Horizon 2020 Research and innovation program under the Marie Sklodowska-Curie Grant Agreement 691053 (H2020-MSCA-RISE-2015 ODYSSEA project). The first author is grateful to CAPES (Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior) in Brazil for financial support in the framework of the BIODIVA project from the Guyamazon program funded by FAPEAM/IRD/French Embassy. The authors declare that there is no conflict of interest.	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J	Sahoo, PK; Dall'Agnol, R; Salomao, GN; Ferreira, JD; da Silva, MS; Martins, GC; Souza, PWME; Powell, MA; Maurity, CW; Angelica, RS; da Costa, MF; Siqueira, JO				Sahoo, Prafulla Kumar; Dall'Agnol, Roberto; Salomao, Gabriel Negreiros; da Silva Ferreira Junior, Jair; da Silva, Marcio Souza; Martins, Gabriel Caixeta; E Souza Filho, Pedro Walfir Martin; Powell, Mike A.; Maurity, Clovis Wagner; Angelica, Romulo Simoes; da Costa, Marlene Furtado; Siqueira, Jose Oswaldo			Source and background threshold values of potentially toxic elements in soils by multivariate statistics and GIS-based mapping: a high density sampling survey in the Parauapebas basin, Brazilian Amazon	ENVIRONMENTAL GEOCHEMISTRY AND HEALTH			English	Article; Proceedings Paper	European-Geosciences-Union (EGU) Conference on Soil Contamination and Human Health - Advances and Problems of Risk Assessment	APR, 2018	Vienna, AUSTRIA	European Geosciences Union		Soil geochemical mapping; Potentially toxic elements; Geochemical background; Environmental contamination; Multivariate analysis; Southeastern Amazon	SEDIMENT GEOCHEMICAL DATA; QUALITY REFERENCE VALUES; HEAVY-METALS; CARAJAS PROVINCE; A-TYPE; SPATIAL-DISTRIBUTION; ULTRAMAFIC ROCKS; TRACE-ELEMENTS; CRATON; AREA	A high-density regional-scale soil geochemical survey comprising 727 samples (one sample per each 5 x 5 km grid) was carried out in the Parauapebas sub-basin of the Brazilian Amazonia, under the Itacaiunas Basin Geochemical Mapping and Background Project. Samples were taken from two depths at each site: surface soil, 0-20 cm and deep soil, 30-50 cm. The ground and sieved (< 75 mu m) fraction was digested using aqua regia and analyzed for 51 elements by inductively coupled plasma mass spectrometry (ICPMS). All data were used here, but the principal focus was on the potential toxic elements (PTEs) and Fe and Mn to evaluate the spatial distribution patterns and to establish their geochemical background concentrations in soils. Geochemical maps as well as principal component analysis (PCA) show that the distribution patterns of the elements are very similar between surface and deep soils. The PCA, applied on clr-transformed data, identified four major associations: Fe-Ti-V-Sc-Cu-Cr-Ni (Gp-1); Zr-Hf-U-Nb-Th-Al-P-Mo-Ga (Gp-2); K-Na-Ca-Mg-Ba-Rb-Sr (Gp-3); and La-Ce-Co-Mn-Y-Zn-Cd (Gp-4). Moreover, the distribution patterns of elements varied significantly among the three major geological domains. The whole data indicate a strong imprint of local geological setting in the geochemical associations and point to a dominant geogenic origin for the analyzed elements. Copper and Fe in Gp-1 were enriched in the Carajas basin and are associated with metavolcanic rocks and banded-iron formations, respectively. However, the spatial distribution of Cu is also highly influenced by two hydrothermal mineralized copper belts. Ni-Cr in Gp-1 are highly correlated and spatially associated with mafic and ultramafic units. The Gp-2 is partially composed of high field strength elements (Zr, Hf, Nb, U, Th) that could be linked to occurrences of A-type Neoarchean granites. The Gp-3 elements are mobile elements which are commonly found in feldspars and other rock-forming minerals being liberated by chemical weathering. The background threshold values (BTV) were estimated separately for surface and deep soils using different methods. The '75th percentile', which commonly used for the estimation of the quality reference values (QRVs) following the Brazilian regulation, gave more restrictive or conservative (low) BTVs, while the 'M-MAD' was more realistic to define high BTVs that can better represent the so-called mineralized/normal background. Compared with CONAMA Resolution (No. 420/2009), the conservative BTVs of most of the toxic elements were below the prevention limits (PV), except Cu, but when the high BTVs are considered, Cu, Co, Cr and Ni exceeded the PV limits. The degree of contamination (C-deg), based on the conservative BTVs, indicates low contamination, except in the Carajas basin, which shows many anomalies and had high contamination mainly from Cu, Cr and Ni, but this is similar between surface and deep soils indicating that the observed high anomalies are strictly related to geogenic control. This is supported when the C-deg is calculated using the high BTVs, which indicates low contamination. This suggests that the use of only conservative BTVs for the entire region might overestimate the significance of anthropogenic contamination; thus, we suggest the use of high BTVs for effective assessment of soil contamination in this region. The methodology and results of this study may help developing strategies for geochemical mapping in other Carajas soils or in other Amazonian soils with similar characteristics.	[Sahoo, Prafulla Kumar; Dall'Agnol, Roberto; Salomao, Gabriel Negreiros; da Silva Ferreira Junior, Jair; da Silva, Marcio Souza; Martins, Gabriel Caixeta; E Souza Filho, Pedro Walfir Martin; Maurity, Clovis Wagner; Siqueira, Jose Oswaldo] ITV, Rua Boaventura da Silva 955, BR-66055090 Belem, Para, Brazil; [Sahoo, Prafulla Kumar] Cent Univ Punjab, Sch Environm & Earth Sci, Dept Environm Sci & Technol, Bathinda 151001, India; [Dall'Agnol, Roberto; Salomao, Gabriel Negreiros; E Souza Filho, Pedro Walfir Martin; Maurity, Clovis Wagner; Angelica, Romulo Simoes] Univ Fed Para UFPA, Inst Geociencias, Programa Posgrad Geol & Geoquim, Rua Augusto Correa, BR-66075110 Belem, Para, Brazil; [da Silva, Marcio Souza] Univ Fed Para UFPA, Inst Geociencias, Programa Posgrad Ciencias Ambientais, Rua Augusto Correa, BR-66075110 Belem, Para, Brazil; [Powell, Mike A.] Univ Alberta, Fac Agr Life & Environm Sci ALES, Dept Renewable Resources, Edmonton, AB, Canada; [da Costa, Marlene Furtado] Dept Ferrosos Norte, Gerencia Meio Ambiente Minas Carajas, Estr Raymundo Mascarenhas,S-N Mina N4, BR-68516000 Parauapebas, PA, Brazil	Instituto Tecnologico Vale Desenvolvimento Sustentavel; Central University of Punjab; Universidade Federal do Para; Universidade Federal do Para; University of Alberta	Sahoo, PK (autor correspondente), ITV, Rua Boaventura da Silva 955, BR-66055090 Belem, Para, Brazil.	prafulla.sahoo@itv.org	Angelica, Romulo/G-6245-2010; Souza, Pedro/GZH-1275-2022; Souza-Filho, Pedro Walfir M. M./J-4958-2012; Sahoo, Prafulla/N-5100-2018	Angelica, Romulo/0000-0002-3026-5523; Souza-Filho, Pedro Walfir M. M./0000-0003-0252-808X; Sahoo, Prafulla/0000-0003-3481-1787; da Silva Ferreira Junior, Jair/0000-0003-0921-6660; Caixeta Martins, Gabriel/0000-0002-7271-0699; Negreiros Salomao, Gabriel/0000-0003-3729-7840	Vale (GABAN-DIFN); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [380.418/2018-5, 306108/2014-3, 443247/2015-3, RSA 305.392/2014-0]; CAPES [88887.160998/2017-00]	Vale (GABAN-DIFN); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This work is part of the Itacaiunas Geochemical Mapping and Background Project, ItacGMBP, currently being undertaken at Instituto Tecnologico Vale (ITV), Belem, Brazil. This was supported by Vale (GABAN-DIFN); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [DTI scholarship to GNS (Proc. 380.418/2018-5); Grants to RD (proc. 306108/2014-3; Proc. 443247/2015-3); RSA 305.392/2014-0]; and CAPES (scholarship to GCM, Proc. 88887.160998/2017-00). The authors acknowledge two anonymous reviewers for their constructive comments and insights and Marcondes Lima da Costa, Luiz Roberto Guimaraes Guilherme, Otavio Augusto Boni Licht, Jose Francisco da Fonseca Ramos e Jose Francisco Berredo for their scientific collaboration with the Background project.	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Geochem. Health	JAN	2020	42	1			SI		255	282		10.1007/s10653-019-00345-z	http://dx.doi.org/10.1007/s10653-019-00345-z			28	Engineering, Environmental; Environmental Sciences; Public, Environmental & Occupational Health; Water Resources	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Engineering; Environmental Sciences & Ecology; Public, Environmental & Occupational Health; Water Resources	KJ4ND	31401754				2023-06-23	WOS:000512034200018
J	Aragao, AJS; Gorayeb, PSD; Galarza, MA				Santana Aragao, Arthur Jeronimo; de Sousa Gorayeb, Paulo Sergio; Galarza, Marco Antonio			Magmatic and tectonic evolution of the Chaval Granite at the end of the Neoproterozoic, northwestern border of the Borborema Province	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Chaval Granite; Mylonites; Geochronology; Neoproterozoic; Santa Quiteria Magmatic Arc; Borborema Province	U-PB; HF ISOTOPES; NE-BRAZIL; GEOCHEMICAL CHARACTERISTICS; PLUTONIC ROCK; ZIRCON; DISCRIMINATION; CONSTRAINTS; STATE; CRUST	The northwestern region of Borborema Province is represented by the Ceara Central and Northwest Ceara crustal blocks connected by an extensive transcurrent shear zone that represents the northern portion of the Transbrasiliano Lineament in a complex geological context, which brings together geological units of nature, origin, and ages of the Archean to the Paleozoic. In this scenario, there is a large amount of granitic bodies, with different natures, age and tectonic environment, but predominantly representing a more intense granitogenesis in the Paleozoic Neoproterozoic and early Paleozoic, with plutons emplaced in different stages of the Brazilian Orogeny. In this context, the Chaval Granite corresponds to an isolated body in the extreme northwest of Borborema Province, located near the Atlantic coast, in the northern states of Ceara and Piaui. It is an intrusive batholith housed in Siderian orthogneisses (Granja Complex) and in Neoproterozoic supracrustal rocks (Martinopole Group), but is partly covered by sedimentary rocks from the Parnaiba Paleozoic Basin (Serra Grande Group), and coastal Cenozoic deposits. Field data and petrographic studies highlight the porphyritic texture with microcline megacrystals involved in coarce matrix as a remarkable feature. The predominant petrographic types are granodiorites, with variations for monzogranites and tonalites. The predominant primary mineral constituents are pertitic microcline, oligoclase, and quartz; biotite and rarely hornblende as qualified minerals and additionally titanite, apatite, zircon, alanite, and opaque minerals. Another peculiar characteristic is the deformational features related to the installation of the Santa Rosa Transcurrent Shear Zone along its eastern flank. The effects of the transcurrent shear deformation led to the modification of the original magmatic fabrics in much of the eastern half of the batolith, generating various types of mylonites. Thus, the typically igneous textures preserved in the western half of the pluton were gradually replaced by tectonic fabrics, which initially evolved into proto-mylonites in the central portion of the body, grading to mylonites eastward, highlighting strongly stretching, comminution associated with dynamic recrystallization, highlighting the formation of microcline and plagioclase porphyroclasts in a mylonitic matrix, which are involved by mylonitic foliation. Geochemical studies reveal compositional similarities, compatible with petrographic classifications, in which they mostly present granodioritic composition, followed by monzogranites and tonalites, classified as I-type granites, peraluminous with compatible with the calcium-alkaline series. The geochemical signatures of the Chaval Granite indicate the character of the tectonic magmatic arc environment. U-Pb zircon analysis by Mass Spectrometry (LA-ICP-MS) indicates crystallization age of 633 Ma, placing it in the Neoproterozoic, late Cryogenic-Early Ediacaran period, being one of the oldest granitoids in northwestern Borborema Province, correlated to the granites of the Santa Quiteria Magmatic Arc in the Ceara Central Domain. Hf-T-DM model ages (2.65 to 2.13 Ga) and epsilon Hf(t = 633 Ma) values from -9.6 to -18.1 suggest incorporation of neoarchean and paleoproterozoic crustal sources in their formation with a long crustal residence time. Similar Sm-Nd data in whole-rock indicate Nd-T-DM model ages of 1.27, 1.72 and 2.04 Ga and negative epsilon Nd(t = 633 Ma) values of -2.64 to -9.13, indicating paleoproterozoic and mesoproterozoic sources, with considerable crustal residence time implying a more evolved nature.	[Santana Aragao, Arthur Jeronimo; de Sousa Gorayeb, Paulo Sergio; Galarza, Marco Antonio] Univ Fed Para, Belem, Para, Brazil	Universidade Federal do Para	Aragao, AJS (autor correspondente), Univ Fed Para, Belem, Para, Brazil.	arthurjsaragao10@gmail.com; gorayebp@ufpa.br; antogt@ufpa.br	Galarza, Marco Antonio MAG/B-1736-2013	Gorayeb, Paulo/0000-0003-1877-9756; Aragao, Arthur/0000-0002-1284-3369	Coordination for the Improvement of Higher Education Personnel (CAPES)	Coordination for the Improvement of Higher Education Personnel (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	This study was conducted by the research group "Petrology and Crustal Evolution" (CNPq-UFPA) within the scope of the Graduate Program in Geology and Geochemistry (PPGG), Geosciences Institute (IG) of the Federal University of Para (UFPA). Thanks to the Isotope Geology Laboratory (ParaIso) -IG-PPGG for isotope analyzes and the IG/PPGG for the infrastructure. We are also grateful to the Microanalyses Laboratory for capturing images of catodoluminescence acquired in scanning electron microscopy (SEM). The first author would like to thank the Coordination for the Improvement of Higher Education Personnel (CAPES) for the grant of the Master's scholarship.	ABREU F. A. 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N., 1989, THESIS; Sibson RH., 1977, J GEOL SOC LONDON, V133, P191, DOI [10.1144/gsjgs.133.3.0191, DOI 10.1144/GSJGS.133.3.0191]; STRECKEISEN A, 1976, EARTH-SCI REV, V12, P1, DOI 10.1016/0012-8252(76)90052-0; Teixeira M.F.B., 2010, C BARS GEOL BEL AN C, V45; Teruggi M., 1974, ATLAS MYLONITES RELA, V29, P265; THOMPSON RN, 1982, SCOT J GEOL, V18, P49, DOI 10.1144/sjg18010049; Vernon R.H., 2008, PRACTICAL GUIDE ROCK; WHALEN JB, 1987, CONTRIB MINERAL PETR, V95, P407, DOI 10.1007/BF00402202; WHITE SH, 1980, J STRUCT GEOL, V2, P175, DOI 10.1016/0191-8141(80)90048-6; Wilson M., 1989, IGNEOUS PETROGENESIS, DOI 10.1007/978-1-4020-6788-4	81	4	4	2	5	SOC BRASILEIRA GEOLOGIA	SAO PAULO	CAIXA POSTAL 11348, SAO PAULO, SP 05422-970, BRAZIL	2317-4889	2317-4692		BRAZ J GEOL	Braz. J. Geol.		2020	50	1							e20190089	10.1590/2317-4889202020190089	http://dx.doi.org/10.1590/2317-4889202020190089			26	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MP7ZD		gold			2023-06-23	WOS:000552418900001
J	Santana, JR; Da Costa, AESF; Veleda, D; Schwamborn, SHL; Mafalda, PO; Schwambo, R				Santana, Jana R.; Da Costa, Alejandro E. S. F.; Veleda, Doris; Schwamborn, Silvia Helena L.; Mafalda Junior, Paulo O.; Schwambo, Ralf			Ichthyoplankton community structure on the shelf break off northeastern Brazil	ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS			English	Article						continental shelf-slope gradient; early life stages of fishes; indicator species; spatial distribution	SOUTH-ATLANTIC; CONTINENTAL-SHELF; FISH; LARVAL; CIRCULATION; PATTERNS; ASSOCIATIONS; CHLOROPHYLL; ASSEMBLAGES; VARIABILITY	Oceanographic features influence the early stages of fish to a high degree. We investigated the influence of continental shelf-slope gradient on the ichthyoplankton composition and distribution off Northeastern Brazil. Two oceanographic campaigns were performed during July-August 2010 and 2012. The samplings were performed along three transects composed by three stations, covering the continental shelf and slope areas. Abiotic data were obtained by an ADCP and a CTD. The ichthyoplankton was sampled through diurnal and nocturnal hauls using a 500-mu m bongo net from 200 m to the surface. A total of 1634 larvae and 4023 eggs, representing 91 genera and 76 species, were collected. Higher concentrations of fish eggs were found on the continental shelf, probably because of the North Brazil Undercurrent flux. Higher concentrations of larvae were found at night and could be associated with net avoidance or natural variation. Neritic, oceanic and transition groups of species association were determined. Larvae of neritic, demersal and pelagic fishes prevailed on the continental shelf, while larvae of oceanic, mesopelagic and bathypelagic fishes on the continental slope. Melanostomiidae, Scorpaena sp., Lestidium atlanticum, Lampadena sp. and Diaphus sp. were identified as indicators of the continental slope.	[Santana, Jana R.; Da Costa, Alejandro E. S. F.; Schwambo, Ralf] Univ Fed Pernambuco UFPE, Museu Oceanog Prof Petronio Alves Coelho, Av Arquitetura,S-N,Cidade Univ, BR-50740550 Recife, PE, Brazil; [Santana, Jana R.; Veleda, Doris] Univ Estado Bahia UNEB, Dept Ciencias Humanas & Teconol, Rua Prof Carlos Santos 601, BR-47400000 Xique Xique, BA, Brazil; [Schwamborn, Silvia Helena L.] Univ Fed Pemambuco UFPE, CAV, Rua Alto Reservatorio S-N, BR-55608680 Vitoria De Santo Antao, PE, Brazil; [Mafalda Junior, Paulo O.] Univ Fed Bahia UFBA, Inst Biol, Rua Barao de Jeremoabo 668, BR-40170115 Salvador, BA, Brazil	Universidade Federal de Pernambuco; Universidade do Estado Bahia	Santana, JR (autor correspondente), Univ Fed Pernambuco UFPE, Museu Oceanog Prof Petronio Alves Coelho, Av Arquitetura,S-N,Cidade Univ, BR-50740550 Recife, PE, Brazil.; Santana, JR (autor correspondente), Univ Estado Bahia UNEB, Dept Ciencias Humanas & Teconol, Rua Prof Carlos Santos 601, BR-47400000 Xique Xique, BA, Brazil.	jribeiro.pesca@gmail.co	Veleda, Doris/I-1673-2012	Veleda, Doris/0000-0003-2103-5950; Schwamborn, Ralf/0000-0001-9150-8720; Costa, Alejandro/0000-0002-4117-1987; Lima Schwamborn, Silvia Helena/0000-0002-6078-026X; Santana, Jana Ribeiro/0000-0001-6484-9482	Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico (CNPq); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Ministerio da Ciencia e Tecnologia (MO); INCT AmbTropic (CNPq/CAPES/FAPESB); Departamento de Oceanografia of the Universidade Federal de Pernambuco	Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Ministerio da Ciencia e Tecnologia (MO); INCT AmbTropic (CNPq/CAPES/FAPESB); Departamento de Oceanografia of the Universidade Federal de Pernambuco	This work is a contribution of the Projects Camadas Finas I and II. The Conselho Nacional de Desenvolvimento Cientifico e TecnolOgico (CNPq) supported]RS with a PhD scholarship, and RS with a productivity fellowship. The Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) supported AESFC with a PhD scholarship. The authors acknowledge Dr. Werner Ekau for his critical review of the manuscript, which has led to a significant improvement of its quality; the Marinha do Brasil and the crew members and researchers aboard of the NHO Cruzeiro do Sul for their support in the fieldwork; and the Ministerio da Ciencia e Tecnologia (MO), INCT AmbTropic (CNPq/CAPES/FAPESB), and the Departamento de Oceanografia of the Universidade Federal de Pernambuco for providing facilities and support.	Acha EM, 2004, J MARINE SYST, V44, P83, DOI 10.1016/j.jmarsys.2003.09.005; Ahlstrom E. 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M., 1991, Food Quality and Preference, V3, P89, DOI 10.1016/0950-3293(91)90028-D; RICHARDS WJ, 2006, EARLY STAGES ATLANTI, V1-2, P2640; Sabates A, 1996, MAR ECOL PROG SER, V135, P11, DOI 10.3354/meps135011; Sassa C, 2002, FISH OCEANOGR, V11, P1, DOI 10.1046/j.1365-2419.2002.00182.x; Schott FA, 2005, J PHYS OCEANOGR, V35, P2031, DOI 10.1175/JPO2813.1; SHANNON CE, 1948, BELL SYST TECH J, V27, P379, DOI 10.1002/j.1538-7305.1948.tb01338.x; Stramma L, 1999, J GEOPHYS RES-OCEANS, V104, P20863, DOI 10.1029/1999JC900139; Stramma L, 2005, J GEOPHYS RES-OCEANS, V110, DOI 10.1029/2005JC002939; Travassos P, 1999, ARCH FISH MAR RES, V47, P211; VELEDA D, 2012, J GEOPHYS RES, V117, P1	57	1	1	1	5	ACAD BRASILEIRA DE CIENCIAS	RIO JANEIRO	RUA ANFILOFIO DE CARVALHO, 29, 3 ANDAR, 20030-060 RIO JANEIRO, BRAZIL	0001-3765	1678-2690		AN ACAD BRAS CIENC	An. Acad. Bras. Cienc.		2020	92	2							020180851	10.1590/0001-3765202020180851	http://dx.doi.org/10.1590/0001-3765202020180851			19	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	LZ9IN	32520215	Green Published, gold			2023-06-23	WOS:000541532600001
J	Santos, AS; de Souza, CT; Leao, DJ; Correia, FO; Almeida, TS; Ferreira, SLC				Santos, Adilson S.; de Souza, Cheilane T.; Leao, Danilo J.; Correia, Felipo O.; Almeida, Tarcisio S.; Ferreira, Sergio L. C.			Simultaneous Determination of Chromium and Iron in Powdered Milk Using High-Resolution Continuum Source Graphite Furnace Atomic Absorption Spectrometry	FOOD ANALYTICAL METHODS			English	Article						Simultaneous determination; Chromium; Iron; Powdered milk; HR-CS GF AAS	TRACE-ELEMENTS; FE; SAMPLES; NI; SUPPLEMENTS; ALUMINUM; CADMIUM; MATRIX; LEAD; PB	This work proposes the simultaneous determination of chromium and iron in powdered milk samples using high-resolution continuum source graphite furnace atomic absorption spectrometry (HR-CS GF AAS) and sample digestion in microwave oven using nitric acid and hydrogen peroxide. The method was established using the primary line (357.869 nm) for chromium and the adjacent secondary line (358.120 nm) for iron while employing aluminum as the chemical modifier. The absorbance signals were measured by peak area using three pixels for both elements. Chromium and iron can be determined in powdered milk samples by the external calibration technique with limits of quantification of 28 ng g(-1) for chromium and 19 mu g g(-1) for iron. The precision was evaluated by using a milk sample with chromium and iron concentrations of 0.76 mu g g(-1) and 151.3 mu g g(-1), respectively. The results expressed as relative standard deviation (n = 10) were 2.6% for iron and 3.9% for chromium. The method accuracy was confirmed by the analysis of a milk sample by a comparison of results obtained by the proposed method and those found by employing inductively coupled plasma mass spectrometry (ICP-MS). Five samples were analyzed, and the analyte concentrations found varied from 408 to 805 ng g(-1) for chromium. Among the five samples, three had an iron concentration lower than 19 mu g g(-1) and in the other two samples, the iron concentrations varied from 151 to 199 mu g g(-1).	[Santos, Adilson S.; de Souza, Cheilane T.; Leao, Danilo J.; Correia, Felipo O.; Almeida, Tarcisio S.; Ferreira, Sergio L. C.] Univ Fed Bahia, Inst Quim, Grp Pesquisa Quim & Quimiometria, BR-40170270 Salvador, BA, Brazil; [Santos, Adilson S.; de Souza, Cheilane T.; Leao, Danilo J.; Ferreira, Sergio L. C.] Univ Fed Bahia, INCT, Energia & Ambiente, BR-40170290 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia	Ferreira, SLC (autor correspondente), Univ Fed Bahia, Inst Quim, Grp Pesquisa Quim & Quimiometria, BR-40170270 Salvador, BA, Brazil.; Ferreira, SLC (autor correspondente), Univ Fed Bahia, INCT, Energia & Ambiente, BR-40170290 Salvador, BA, Brazil.	slcf@ufba.br	de almeida, tarcisio S./U-4368-2017; Leão, Danilo Junqueira/AAE-2013-2021; FERREIRA, SERGIO LUIS SLCF COSTA/I-1993-2013	de almeida, tarcisio S./0000-0003-1963-3775; FERREIRA, SERGIO LUIS SLCF COSTA/0000-0001-7738-045X				Akele ML, 2017, ENVIRON MONIT ASSESS, V189, DOI 10.1007/s10661-017-6203-0; Almeida JS, 2019, FOOD CHEM, V273, P130, DOI 10.1016/j.foodchem.2018.01.112; Araujo-Barbosa U, 2017, TALANTA, V170, P523, DOI 10.1016/j.talanta.2017.04.034; Bakircioglu D, 2018, MICROCHEM J, V136, P133, DOI 10.1016/j.microc.2016.10.014; Boschetti W, 2016, J ANAL ATOM SPECTROM, V31, P1269, DOI 10.1039/c6ja00031b; Boschetti W, 2014, ANAL METHODS-UK, V6, P4247, DOI 10.1039/c4ay00241e; Brannon PM, 2017, NUTRIENTS, V9, DOI 10.3390/nu9121327; Buldini PL, 2002, MICROCHEM J, V72, P277, DOI 10.1016/S0026-265X(02)00039-5; Cama-Moncunill R, 2017, SPECTROCHIM ACTA B, V135, P6, DOI 10.1016/j.sab.2017.06.014; Valdivia AC, 2018, TALANTA, V179, P1, DOI 10.1016/j.talanta.2017.10.033; Costello RB, 2016, NUTR REV, V74, P455, DOI 10.1093/nutrit/nuw011; da Silva DG, 2011, ANAL METHODS-UK, V3, P2495, DOI 10.1039/c1ay05442b; Dittert IM, 2009, SPECTROCHIM ACTA B, V64, P537, DOI 10.1016/j.sab.2009.02.006; Dobrowolski R, 2017, SPECTROCHIM ACTA B, V132, P13, DOI 10.1016/j.sab.2017.03.011; dos Santos LO, 2017, FOOD ANAL METHOD, V10, P469, DOI 10.1007/s12161-016-0600-9; Esposito M, 2017, FOOD CHEM, V233, P378, DOI 10.1016/j.foodchem.2017.04.124; Ferreira SLC, 2018, TRAC-TREND ANAL CHEM, V100, P1, DOI 10.1016/j.trac.2017.12.012; Ferreira SLC, 2011, ANAL METHODS-UK, V3, P1168, DOI 10.1039/c0ay00768d; Filatova DG, 2018, SPECTROCHIM ACTA B, V140, P1, DOI 10.1016/j.sab.2017.12.003; Heitmann U, 2007, SPECTROCHIM ACTA B, V62, P1222, DOI 10.1016/j.sab.2007.10.011; Khan N, 2014, FOOD CHEM, V147, P220, DOI 10.1016/j.foodchem.2013.09.147; Kira CS, 2004, J AOAC INT, V87, P151; Kowalewska Z, 2017, SPECTROCHIM ACTA B, V132, P26, DOI 10.1016/j.sab.2017.03.020; Laczai N, 2016, SPECTROCHIM ACTA B, V117, P8, DOI 10.1016/j.sab.2015.12.008; Leao DJ, 2016, TALANTA, V153, P45, DOI 10.1016/j.talanta.2016.02.023; Lee JH, 2016, J KOREAN MED ASSOC, V59, P678, DOI 10.5124/jkma.2016.59.9.678; Nascimento CF, 2017, FOOD CHEM, V221, P1232, DOI 10.1016/j.foodchem.2016.11.034; Oreste EQ, 2016, FOOD ANAL METHOD, V9, P777, DOI 10.1007/s12161-015-0252-1; Ozbek N, 2016, TALANTA, V148, P17, DOI 10.1016/j.talanta.2015.10.041; Pozzatti M, 2017, MICROCHEM J, V133, P162, DOI 10.1016/j.microc.2017.03.021; Resano M, 2013, J ANAL ATOM SPECTROM, V28, P657, DOI 10.1039/c3ja30377b; Souza SO, 2018, MICROCHEM J, V143, P1, DOI 10.1016/j.microc.2018.07.019; Tinas H, 2018, SPECTROCHIM ACTA B, V140, P73, DOI 10.1016/j.sab.2017.12.002; Welz B, 2005, HIGH-RESOLUTION CONTINUUM SOURCE AAS: THE BETTER WAY TO DO ATOMIC ABSORPTION SPECTROMETRY, P1, DOI 10.1002/3527606513; Wong C., 2017, PAEDIAT CHILD HLTH U, V27, P527, DOI [10.1016/j.paed.2017.08.004, DOI 10.1016/J.PAED.2017.08.004]; Zambrzycka-Szelewa E, 2017, SPECTROCHIM ACTA B, V133, P81, DOI 10.1016/j.sab.2017.04.012	36	8	10	0	26	SPRINGER	NEW YORK	ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES	1936-9751	1936-976X		FOOD ANAL METHOD	Food Anal. Meth.	JAN	2020	13	1			SI		284	290		10.1007/s12161-019-01624-2	http://dx.doi.org/10.1007/s12161-019-01624-2			7	Food Science & Technology	Science Citation Index Expanded (SCI-EXPANDED)	Food Science & Technology	KJ3SW					2023-06-23	WOS:000511978600032
J	Santos, FG; Neto, MTOC; Ferreira, VP; Bertotti, AL				Santos, Frank Gurgel; Oliveira Cavalcanti Neto, Mario Tavares; Ferreira, Valderez Pinto; Bertotti, Anelise Losangela			Eo to Paleoarchean metamafic-ultramafic rocks from the central portion of the Rio Grande do Norte Domain, Borborema Province, northeast Brazil: The oldest South American platform rocks	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Archean; Mafic-ultramafic rocks; Caico complex; Borborema province; Petrology	BARBERTON GREENSTONE-BELT; DETRITAL ZIRCON AGES; GA SAO-JOSE; NE BRAZIL; U-PB; CRUSTAL EVOLUTION; CAMPESTRE MASSIF; SERIDO; GEOCHEMISTRY; REWORKING	Metamorphosed mafic-ultramafic rocks from the central portion of the Rio Grande do Norte Domain of the Borborema Province (BP), northeastern Brazil, have been studied here with the objective of gaining a better understanding of the Archean evolution of this portion of the BP. The study area is underlain by gneissic-migmatitic basement as well as biotite schists and paragneisses of the Serido and Jucurutu formations of the Serid6 Group. The mafic-ultramafic rocks (serpentinites, amphibole-schists and amphibolites) occur in lenses for 30 km along strike following the NNE regional foliation. The serpentinites occur as relatively small exposures of elongated bodies within paragneisses of the Jucurutu Formation and orthogneisses of the Caico Complex. They consist of xenoblastic serpentine (75-99%) that has replaced the primary ferromagnesian minerals of the protolith. The amphibole schists and amphibolites are whitish gray to green, depending on the dominant mineral phase, tremolite, talc or actinolite. The mafic-ultramafic rocks present high MgO, Ni and Cr2O3 contents and very low TiO2, Na2O and K2O contents, being compositionally similar to mafic-ultramafic rocks from other Archean greenstone belts worldwide. U-Pb (SHRIMP) dating of zircons returned concordia ages of 3526 +/- 5 Ma (MSWD = 0.0084) for the serpentinites of the Serra Verde Mine and 3747 +/- 12 Ma (MSWD = 9.8) for serpentinites from the Oiticica Mine. The petrographic and geochemical characteristics as well as the Eo to Paleoarchean ages of the studied rocks are significant as the basement of this portion of the BP is dominantly of Paleoproterozoic age. It is envisaged that these results will lead to further debate and a greater understanding of crustal evolution of the BP. We propose that these mafic-ultramafic rocks are part of a dismembered Archean greenstone belt, which present the oldest ages so far determined for the South American Platform.	[Santos, Frank Gurgel] Serv Geol Brasil CPRM, Superintendencia Reg Recife, Ave Sul 2291, Recife, PE, Brazil; [Oliveira Cavalcanti Neto, Mario Tavares] IFRN, Programa Posgrad Uso Sustentavel Recursos Nat IFR, Campus Natal Cent,Ave Senador Salgado Filho 1559, Natal, RN, Brazil; [Santos, Frank Gurgel; Ferreira, Valderez Pinto; Bertotti, Anelise Losangela] Univ Fed Pernambuco UFPE, Ctr Tecnol Geociencias, Dept Geol, Ave Arquitetura S-N, Recife, PE, Brazil	Instituto Federal do Rio Grande do Norte; Universidade Federal de Pernambuco	Santos, FG (autor correspondente), Serv Geol Brasil CPRM, Superintendencia Reg Recife, Ave Sul 2291, Recife, PE, Brazil.	90.frank@gmail.com	Bertotti, Anelise L/O-6797-2017; Ferreira, Valderez P/M-9835-2015	Bertotti, Anelise L/0000-0003-2222-6660; Gurgel Santos, Frank/0000-0001-9803-5479	CNPq [1533695260888392]	CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thanks to CNPq that provided financial resources to fieldwork stages, chemical and isotopic analyses by the project number 1533695260888392 granted to MTOCN. The UFPE and IFRN also thanked for providing infrastructure and logistic help. F.G. Santos thanks to Geological Survey of Brazil -CPRM by the incentive in the search for Master degree in Geology. To reviewers, Sergio Pacheco Neves and Lauro Cezar Montefalco de Lira Santos, we thanks for the valuable contributions and favorable opinion to publication.	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Earth Sci.	JAN	2020	97								102410	10.1016/j.jsames.2019.102410	http://dx.doi.org/10.1016/j.jsames.2019.102410			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KG0FR					2023-06-23	WOS:000509617600019
J	Seraine, M; Campos, JEG; Martins-Ferreira, MAC; Giorgioni, M; Angelo, TV				Seraine, Marina; Guimaraes Campos, Jose Eloi; Cacador Martins-Ferreira, Marco Antonio; Giorgioni, Martino; Angelo, Tiago Valim			Tectonic significance of abrupt immature sedimentation in a shallow cratonic margin basin: The Arkose Level, Mesoproterozoic Paranoa Group	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Braided-river deposits; Mesoproterozoic; Arkose Level; Paranoa Group	NEOPROTEROZOIC BRASILIA BELT; SAO FRANCISCO CRATON; PLASMA-MASS SPECTROMETRY; CENTRAL BRAZIL; U-PB; SM-ND; PROVENANCE; GEOCHRONOLOGY; EVOLUTION; EVENTS	Facies analysis, aided by X-ray diffraction, QemScan analysis, U-Pb detrital ages and field geological data are used in a detailed sedimentary characterization of the Arkose Level, an immature sedimentary unit that occurs abruptly and discontinuously in the upper Paranoa Group, a sequence of mature marine rhythmites deposited in a shallow cratonic margin basin. This basin was developed during the Mesoproterozoic in the western margin of the Sao Francisco Craton, central Brazil. The study reveals three facies associations in the Arkose Level: (1) Facies Association I (C), (2) Facies Association II (MC) and (3) Facies Association III (FM). The lithofacies are characterized by plane-parallel lamination and planar cross-bedding, trough cross-stratification, channel-fills, overturned cross-stratification, and convoluted structures. The sedimentological and paleocurrent data acquired in this study leads to the interpretation that this unit represents a record of braided-river deposit, which was influenced by marine reworking in the uppermost portion. The depositional model comprises a transitional continental-marine environment, with channels in the continental domain interpreted as a high-energy braided river system around the margins of a shallow intracratonic basin during the Mesoproterozoic. Compiled and newly acquired LA-ICP-MS detrital zircon U-Pb ages reveal a new source area contribution of 1.1 Ga in the Upper portion of the Paranoa Group. The abrupt deposition of braided-river deposits amid the mature Paranoa basin is most probably associated with local faulting, responsible for exposing the crystalline basement and the sedimentary rocks of previous basins, providing new and near-source areas of crystalline basement rocks. The inferred faulting can be associated to a Stenian unsuccessful rifting event, or to the early stages of opening the Goias-Pharusian ocean, in the Tonian.	[Seraine, Marina; Guimaraes Campos, Jose Eloi; Giorgioni, Martino] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil; [Cacador Martins-Ferreira, Marco Antonio] Univ Fed Goias, Fac Ciencias & Tecnol, BR-74968755 Aparecida De Goiania, Go, Brazil; [Angelo, Tiago Valim] Univ Sao Paulo, Inst Geociencias, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil	Universidade de Brasilia; Universidade Federal de Goias; Universidade de Sao Paulo	Seraine, M (autor correspondente), Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil.	marina.seraine@gmail.com	Campos, Eloi/AAK-8599-2021; Cacador Martins-Ferreira, Marco Antonio/I-2983-2017	Valim Angelo, Tiago/0000-0002-1191-8664; Cacador Martins-Ferreira, Marco Antonio/0000-0002-7212-8367; Seraine, Marina/0000-0001-9291-0455; Giorgioni, Martino/0000-0003-0565-3150	Geosciences Institute of the University of Brasilia (UnB), Brazil; Brazilian National Research Council (CNPq) [170906/2017-5]	Geosciences Institute of the University of Brasilia (UnB), Brazil; Brazilian National Research Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors are thankful to the Geosciences Institute of the University of Brasilia (UnB), Brazil for providing fieldwork financial and logistic support and the Brazilian National Research Council (CNPq) for the master's scholarship granted to the first author. Process number: 170906/2017-5.	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South Am. Earth Sci.	JAN	2020	97								102397	10.1016/j.jsames.2019.102397	http://dx.doi.org/10.1016/j.jsames.2019.102397			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KG0FR					2023-06-23	WOS:000509617600006
J	Silva, CD; Santana, GP; Paz, SPA				Silva, Ceel D.; Santana, Genilson P.; Paz, Simone P. A.			Determination of La, Ce, Nd, Sm, and Gd in mineral waste from cassiterite beneficiation by wavelength-dispersive X-ray fluorescence spectrometry	TALANTA			English	Article						WDXRF; Rare earth elements; Matrix effect; Empirical influence coefficients	RARE-EARTH-ELEMENTS; TRACE-ELEMENTS; ROCKS	The objective of this study was to establish the best parameters to correct for matrix effects in the chemical analysis of a siliceous geologic material rich in metallic elements of high economic value, such as La, Ce, Nd, Sm, and Gd (rare earth elements), using empirical influence coefficients applied to wavelength dispersive X-ray fluorescence (WDXRF). At present, this material is considered waste derived from the extraction of tin from cassiterite, a special ore from which niobium and tantalum are also processed. In this study, a reliable methodology for the analysis of rare earth elements in a siliceous matrix using the WDXRF technique was developed. This procedure may be useful in promoting industrial processes for chemical control in solid matrices, as the usual techniques are only possible in liquid media and require acid dissolution.	[Silva, Ceel D.; Santana, Genilson P.] Univ Fed Amazonas, Program Posgrad Quim, BR-69077000 Manaus, AM, Brazil; [Paz, Simone P. A.] Univ Fed Para, Inst Geociencias, Lab Caracterizacao Mineral, Programa Posgrad Geol & Geoquim, BR-66075110 Belem, PA, Brazil	Universidade Federal de Amazonas; Universidade Federal do Para	Silva, CD (autor correspondente), Univ Fed Amazonas, Program Posgrad Quim, BR-69077000 Manaus, AM, Brazil.	ceeldaniel@gmail.com	Paz, Simone Patricia Aranha/AAF-3059-2019	Paz, Simone Patricia Aranha/0000-0002-5880-7638	Geological Survey of Brazil - Companhia de Pesquisa de Recursos Minerais (GSB-CPRM)	Geological Survey of Brazil - Companhia de Pesquisa de Recursos Minerais (GSB-CPRM)	This work was supported by the Geological Survey of Brazil - Companhia de Pesquisa de Recursos Minerais (GSB-CPRM). The authors would also like to thank Taboca Mining for providing the material and logistical support for this study.	AFONIN VP, 1992, X-RAY SPECTROM, V21, P69, DOI 10.1002/xrs.1300210205; [Anonymous], 2010, SOFTW SUPERQ V5; ASTM, 1999, E162294 ASTM; Beckhoff B., 2006, HDB PRACTICAL XRAY F; Brouwer P., 2010, THEORY XRF; CRISS JW, 1968, ANAL CHEM, V40, P1080, DOI 10.1021/ac60263a023; DEBOER DKG, 1993, X-RAY SPECTROM, V22, P33, DOI 10.1002/xrs.1300220109; Barreda MFG, 2016, BOL SOC ESP CERAM V, V55, P185, DOI 10.1016/j.bsecv.2016.06.003; Gazulla MF, 2010, X-RAY SPECTROM, V39, P321, DOI 10.1002/xrs.1270; Helsen J. A., 2002, HDB XRAY SPECTROMETR, P110; Janssens K, 2004, COMP ANAL C, V42, P129, DOI 10.1016/S0166-526X(04)80008-4; Jenkins R., 1999, XRAY FLUORESCENCE SP; Kadachi AN, 2012, X-RAY SPECTROM, V41, P350, DOI 10.1002/xrs.2412; Kane JS, 2007, GEOSTAND GEOANAL RES, V31, P285, DOI 10.1111/j.1751-908X.2007.00869.x; Krishna AK, 2016, SPECTROCHIM ACTA B, V122, P165, DOI 10.1016/j.sab.2016.07.004; Lachance G.R., 1966, CAN SPECTROSC, V11, P43; LEYDEN DE, 1988, TRAC-TREND ANAL CHEM, V7, P321, DOI 10.1016/0165-9936(88)90023-4; Lu AX, 2010, SPECTROSC SPECT ANAL, V30, P2848, DOI 10.3964/j.issn.1000-0593(2010)10-2848-05; Markowicz AA, 2008, PORTABLE X-RAY FLUORESCENCE SPECTROMETRY: CAPABILITIES FOR IN SITU ANALYSIS, P13, DOI 10.1039/9781847558640-00013; Minuzzi ORR, 2008, AN ACAD BRAS CIENC, V80, P719, DOI 10.1590/S0001-37652008000400012; Mori Y, 2005, B KITAKYUSHU MUS N A, V3, P1; Garcia MVR, 2017, RESOUR POLICY, V53, P66, DOI 10.1016/j.resourpol.2017.05.004; Rousseau R., 2013, J GEOSCI GEOMATICS, V1, P1, DOI DOI 10.12691/JGG-1-1-1; Rousseau RA, 2004, SPECTROCHIM ACTA B, V59, P1491, DOI 10.1016/j.sab.2004.06.002; Rousseau RM, 2006, SPECTROCHIM ACTA B, V61, P759, DOI 10.1016/j.sab.2006.06.014; Sitko R, 2005, J ANAL ATOM SPECTROM, V20, P741, DOI 10.1039/b502994e; Sitko R., 2012, XRAY SPECTROSCOPY, P137, DOI [10.5772/29367, DOI 10.5772/29367]; Smolinski A, 2016, SPECTROCHIM ACTA B, V116, P63, DOI 10.1016/j.sab.2015.12.005; Suvorova D, 2017, X-RAY SPECTROM, V46, P200, DOI 10.1002/xrs.2747; Thompson M, 1996, GEOSTANDARD NEWSLETT, V20, P295, DOI 10.1111/j.1751-908X.1996.tb00191.x; UNCTAD, 2014, COMM GLANC SPEC ISS; Van Gosen B. S., 2017, RARE EARTH ELEMENTS; Willis J., 2010, GLASS BEADS BORATE F, V1st; Wu WQ, 2010, J RARE EARTH, V28, P30, DOI 10.1016/S1002-0721(10)60353-5; Yongqiang W., 2014, SPECTROMETRY, V88, P1300; Zambello F. R., 2001, ANALISE MULTIELEMENT	36	9	10	0	37	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0039-9140	1873-3573		TALANTA	Talanta	JAN 1	2020	206								120254	10.1016/j.talanta.2019.120254	http://dx.doi.org/10.1016/j.talanta.2019.120254			7	Chemistry, Analytical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	JB2VG	31514878				2023-06-23	WOS:000488416200076
J	Soares, R; Santos, MCB; Maddock, JEL; Machado, W; Bertolino, LC; de Campos, DVB; Freire, AS; Santelli, RE				Soares, Ricardo; Barreto Santos, Maria Carla; Lewis Maddock, John Edemond; Machado, Wilson; Bertolino, Luiz Carlos; Boas de Campos, David Vilas; Freire, Aline Soares; Santelli, Ricardo Erthal			POTENTIAL MOBILITY AND TOXICITY RISK OF METAL POLLUTANTS IN SOILS FROM A TROPICAL AREA AFFECTED BY INDUSTRIAL WASTES	REVISTA INTERNACIONAL DE CONTAMINACION AMBIENTAL			English	Article						soil pollution; industrial residues; metal contaminants; vertical mobility	SHOOTING RANGE; GEOCHEMICAL BEHAVIOR; HEAVY-METALS; LEAD; LEACHABILITY; IMMOBILIZATION; AVAILABILITY; REMEDIATION; MANAGEMENT; QUEIMADOS	The potential mobility of Cd, Cr. Cu, Ni. Pb and Zn in soils severely impacted by inadequate storage of industrial wastes in Rio de Janeiro State (Brazil) was evaluated by applying the Toxicity Characteristic Leaching Procedure (TCLP). This procedure allowed the estimation of toxicity risks for Cd, Cr and Pb. In a contamination hotspot within the study area, the following order of metal concentrations was observed: Pb > Zn > Cu > Ni > Cd > Cr, with significantly higher values than observed for a control site. Decades of soil exposure to wastes implied TCLP results for Pb above 300 mg/L in this hotspot, which exceed the TCLP regulatory threshold in two orders of magnitude, while Cd (up to 0.8 mg/L) and Cr (up to 0.3 mg/L) results were below the respective TCLP thresholds. Surface soil profile analysis (0-30 cm depth) indicates that Pb vertical migration occurs in the hotspot. TCLP concentrations of Pb were up to four orders of magnitude higher than the groundwater quality threshold preconized by Brazilian regulations for this metal (0.01 mg/L), suggesting that downward dispersion of large loadings of anthropogenic Pb is a major concern.	[Soares, Ricardo] State Environm Inst INEA, 103 Venezuela Ave, BR-20081312 Rio De Janeiro, Brazil; [Soares, Ricardo; Barreto Santos, Maria Carla; Lewis Maddock, John Edemond; Machado, Wilson] Fluminense Fed Univ, Dept Geochem, BR-24020150 Niteroi, RJ, Brazil; [Barreto Santos, Maria Carla] Fluminense Fed Univ, Dept Geog Campos dos Goytacazes, BR-28010385 Campos Dos Goytacazes, RJ, Brazil; [Bertolino, Luiz Carlos] Mineral Technol Ctr CETEM, BR-21941908 Rio De Janeiro, RJ, Brazil; [Boas de Campos, David Vilas] EMBRAPA Solos, BR-22460000 Rio De Janeiro, Brazil; [Freire, Aline Soares; Santelli, Ricardo Erthal] Univ Fed Rio de Janeiro, Technol Ctr, Dept Analyt Chem, BR-21941909 Rio De Janeiro, RJ, Brazil	Universidade Federal Fluminense; Universidade Federal Fluminense; Empresa Brasileira de Pesquisa Agropecuaria (EMBRAPA); Universidade Federal do Rio de Janeiro	Soares, R (autor correspondente), State Environm Inst INEA, 103 Venezuela Ave, BR-20081312 Rio De Janeiro, Brazil.; Soares, R (autor correspondente), Fluminense Fed Univ, Dept Geochem, BR-24020150 Niteroi, RJ, Brazil.	ricardosoaresuff@gmail.com	Machado, Wilson/P-8047-2019	Machado, Wilson/0000-0003-3117-8584				Ahmad M, 2012, J HAZARD MATER, V209, P392, DOI 10.1016/j.jhazmat.2012.01.047; Alloway B.J., 2012, HEAVY METALS SOILS; Alves BSQ, 2014, WATER AIR SOIL POLL, V225, DOI 10.1007/s11270-014-1963-4; Chen M, 2002, SOIL SEDIMENT CONTAM, V11, P1, DOI 10.1080/20025891106664; Cui HB, 2016, ECOTOX ENVIRON SAFE, V134, P148, DOI 10.1016/j.ecoenv.2016.07.005; Lima LRPD, 2011, J HAZARD MATER, V189, P692, DOI 10.1016/j.jhazmat.2011.02.091; Dungan RS, 2009, J ENVIRON MANAGE, V90, P539, DOI 10.1016/j.jenvman.2007.12.004; Ettler V, 2011, GEODERMA, V164, P73, DOI 10.1016/j.geoderma.2011.05.014; Fontes MPF, 2010, J SOIL SEDIMENT, V10, P774, DOI 10.1007/s11368-009-0157-y; Garcia-Guinea J, 2010, AN ACAD BRAS CIENC, V82, P267, DOI 10.1590/S0001-37652010000200003; Kabata-Pendias A., 2011, TRACE ELEMENTS SOILS; Kede MLFM, 2008, QUIM NOVA, V31, P579, DOI 10.1590/S0100-40422008000300022; Kede MLFM, 2017, J ENVIRON ENG, V143, DOI [10.1061/(asce)ee.1943-7870.0001170, 10.1061/(ASCE)EE.1943-7870.0001170]; Kede MLFM, 2014, INT J ENV RES PUB HE, V11, P11528, DOI 10.3390/ijerph111111528; Li XY, 2013, GEODERMA, V192, P50, DOI 10.1016/j.geoderma.2012.08.011; Macias F, 2012, J HAZARD MATER, V229, P107, DOI 10.1016/j.jhazmat.2012.05.080; PERLATTI F, 2016, WATER AIR SOIL POLL, V227, DOI DOI 10.1007/S11270-016-2840-O; Pinto E.M., 2002, THESIS; Prica M, 2010, ECOTOX ENVIRON SAFE, V73, P1370, DOI 10.1016/j.ecoenv.2010.06.014; Rao CRM, 2008, WATER AIR SOIL POLL, V189, P291, DOI 10.1007/s11270-007-9564-0; Santos M.C.B, 2014, CIENCIA HOJE, V53, P30, DOI DOI 10.1071/S11380-005-7866-1; Santos MCB, 2017, REV VIRTUAL QUIM, V9, P2135, DOI 10.21577/1984-6835.20170127; Santos R.D., 2013, HDB SOILS COLLECTION; Sethurajan M, 2016, ENVIRON SCI POLLUT R, V23, P7504, DOI 10.1007/s11356-015-6014-1; Soares R, 2017, REV VIRTUAL QUIM, V9, P2151, DOI 10.21577/1984-6835.20170128; Soares R, 2018, ENG SANIT AMBIENT, V23, P995, DOI [10.1590/s1413-41522018167298, 10.1590/S1413-41522018167298]; Soares R, 2009, CHEM SPEC BIOAVAILAB, V21, P153, DOI 10.3184/095422909X466095; Sposito G., 2016, CHEM SOILS, V3rd; US-EPA, 1992, S ENVIRONMENTAL PROT; Vann KN, 2006, WASTE MANAGE, V26, P293, DOI 10.1016/j.wasman.2005.06.016; Wang YM, 2001, J HAZARD MATER, V88, P63, DOI 10.1016/S0304-3894(01)00289-8; Weber J, 2018, J SOIL SEDIMENT, V18, P2387, DOI 10.1007/s11368-017-1715-3; Yin XQ, 2010, J HAZARD MATER, V179, P895, DOI 10.1016/j.jhazmat.2010.03.089; Zapusek U, 2009, GEODERMA, V154, P164, DOI 10.1016/j.geoderma.2009.10.012	34	1	1	2	8	CENTRO CIENCIAS ATMOSFERA UNAM	MEXICO CITY	CIRCUITO EXTERIOR, MEXICO CITY CU 04510, MEXICO	0188-4999			REV INT CONTAM AMBIE	Rev. Int. Contam. Ambient.		2020	36	4					857	864		10.20937/RICA.53659	http://dx.doi.org/10.20937/RICA.53659			8	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	OL1BW		Green Submitted, hybrid			2023-06-23	WOS:000585077600007
J	da Silva, ACS; da Costa, ML				Sousa da Silva, Aline Cristina; da Costa, Marcondes Lima			Genesis of the "soft" iron ore at S11D Deposit, in Carajas, Amazon Region, Brazil	BRAZILIAN JOURNAL OF GEOLOGY			English	Article						Banded iron formation-protore; lateritic profile; hematite; magnetite; geochemistry	MINERAL PROVINCE; HAMERSLEY PROVINCE; GEOCHEMISTRY; HEMATITE; ELEMENTS; SOILS; BASIN	The origin of the soft ore at the S11D iron mine in Carajas was investigated using 20 samples from a diamond drill hole. The methods of analyses were X-ray diffraction (XRD), optical microscopy, whole-rock chemistry, and scanning electron microscope coupled with energy-dispersive X-ray spectroscopy (SEM/EDS). The drill hole presents a profile through the substratum (protore, a banded iron formation - BIF) and three weathering horizons, defined from the base to the top, saprolite (coarse and fine), and crust. The soft iron ore occurs distributed along the saprolite horizon, and it is composed mainly of hematite and subordinate magnetite. The amount of quartz decreases upwards, whereas the amount of Fe-Al-(Ti-P)-minerals increases towards the top. The total iron is enriched in the fine saprolite when compared to the protore (42.55 to 97.62 wt.% Fe2O3, respectively). Trace elements such as Zr, Cr, Y, and rare earth elements (REE) show relative enrichment upward because they are generally located in residual minerals (as zircon and anatase). The REEs in iron ore samples exhibit enrichment of light rare earth elements (LREE) and depletion of heavy rare earth elements (HREE), with pronounced positive Eu anomaly, which reaffirms the connection between iron ore and BIF. Based on the mineralogy, chemistry, textures, and structures, a genetic laterite-supergene model is proposed for the origin of soft ore at the S11D deposit.	[Sousa da Silva, Aline Cristina; da Costa, Marcondes Lima] Univ Fed Para, Belem, Para, Brazil	Universidade Federal do Para	da Silva, ACS (autor correspondente), Univ Fed Para, Belem, Para, Brazil.	alinecs.silva@hotmail.com; mlc@ufpa.br		LIMA DA COSTA, MARCONDES/0000-0002-0134-0432; Sousa da Silva, Aline Cristina/0000-0001-8283-7506	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [304.519/2009-0, 305014/2016-8]; Instituto Nacional de Ciencia e Tecnologia -Geociencias da Amazonia (INCT-GEOCIAM) [573733/2008-2]; Instituto Tecnologico Vale - Universidade Federal do Para/Fundacao de Amparo e Desenvolvimento da Pesquisa (ITV-UFPA/FADESP) [3753]; Vale S. A.	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Instituto Nacional de Ciencia e Tecnologia -Geociencias da Amazonia (INCT-GEOCIAM); Instituto Tecnologico Vale - Universidade Federal do Para/Fundacao de Amparo e Desenvolvimento da Pesquisa (ITV-UFPA/FADESP); Vale S. A.	The authors would like to thank Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) (M.L.C. - grant number 304.519/2009-0 and 305014/2016-8 and A.C. S. S. - scholarship), Instituto Nacional de Ciencia e Tecnologia -Geociencias da Amazonia (INCT-GEOCIAM) (M.L.C. - grant number 573733/2008-2), and Instituto Tecnologico Vale - Universidade Federal do Para/Fundacao de Amparo e Desenvolvimento da Pesquisa (ITV-UFPA/FADESP) (M.L.C. - grant number 3753) for their financial support. The authors wish to acknowledge Vale S. A. for providing access to geological data and for the technical, logistic, and financial support. They are also grateful to the laboratories of Mineral Characterization and Microanalyses at the Geoscience Institute (UFPA). The authors would also like to thank Clovis Wagner Maurity (ITV) for his help, assistance, encouragement, and in numerous discussions.	[Anonymous], 1986, THESIS; Barrat JA, 2012, GEOCHIM COSMOCHIM AC, V83, P79, DOI 10.1016/j.gca.2011.12.011; Bosch J, 2010, APPL ENVIRON MICROB, V76, P184, DOI 10.1128/AEM.00417-09; BRAUN JJ, 1990, GEOCHIM COSMOCHIM AC, V54, P781, DOI 10.1016/0016-7037(90)90373-S; Buss H.L., 2013, TREATISE GEOCHEMISTR, DOI [10.1016/B978-0-08-095975-7.00504-0, DOI 10.1016/B978-0-08-095975-7.00504-0]; [Companhia Vale do Rio Doce (CVRD) DIGEB/DEPAB/GIMB/ SUMIC], 1996, GUIA EXC, P392; dos Santos PHC, 2016, BRAZ J GEOL, V46, P617, DOI 10.1590/2317-4889201620160101; Costa L.C.G., 2013, S GEOLOGIA AMAZONIA, V13, P671; Costa L. 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Geol.		2020	50	1							e20180128	10.1590/2317-4889202020180128	http://dx.doi.org/10.1590/2317-4889202020180128			19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	MP7YR		Green Published, gold			2023-06-23	WOS:000552417700001
J	Venancio, IM; Shimizu, MH; Santos, TP; Lessa, DO; Portilho-Ramos, RC; Chiessi, CM; Crivellari, S; Mulitza, S; Kuhnert, H; Tiedemann, R; Vahlenkamp, M; Bickert, T; Sampaio, G; Albuquerque, ALS; Veiga, S; Nobre, P; Nobre, C				Venancio, I. M.; Shimizu, M. H.; Santos, T. P.; Lessa, D. O.; Portilho-Ramos, R. C.; Chiessi, C. M.; Crivellari, S.; Mulitza, S.; Kuhnert, H.; Tiedemann, R.; Vahlenkamp, M.; Bickert, T.; Sampaio, G.; Albuquerque, A. L. S.; Veiga, S.; Nobre, P.; Nobre, C.			Changes in surface hydrography at the western tropical Atlantic during the Younger Dryas	GLOBAL AND PLANETARY CHANGE			English	Article							PLANKTONIC-FORAMINIFERA; NORTHEASTERN BRAZIL; LAST DEGLACIATION; GLACIAL CLIMATE; OCEAN; TEMPERATURE; CIRCULATION; IMPACT; PALEOCLIMATE; SYSTEM	During the Younger Dryas (YD), paleoceanographic proxies indicate a weakening of the Atlantic Meridional Overturning Circulation (AMOC) resulting in a widespread surface cooling of the North Atlantic and a southward displacement of the Intertropical Convergence Zone (ITCZ). In the western tropical Atlantic, competing ocean and atmospheric processes may result in contrasting surface hydrography scenarios north and south of the equator during the YD. Based on new and compiled data, we provide an up-to-date model-data comparison of changes in western tropical Atlantic surface hydrography during the YD. We show that both transient model simulations and proxy results indicate warming of sea surface temperatures (SST) in the western tropical South Atlantic, but disagree for the SST in the western tropical North Atlantic. Proxies also reveal a complex spatial pattern in surface salinity in the western tropical Atlantic, while a broad negative anomaly is observed in the model output. By comparing planktonic foraminiferal Ba/Ca records from different records in the western tropical Atlantic we constrain ITCZ shifts from the YD to the early Holocene. Based on the Ba/Ca records, the ITCZ reached its southernmost position between 13 and 11.8 ka and started to move northward reaching its northernmost position between 10.8 and 9.7 ka.	[Venancio, I. M.; Shimizu, M. H.; Sampaio, G.; Veiga, S.; Nobre, P.] Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Cachoeira Paulista, Brazil; [Santos, T. P.; Lessa, D. O.; Albuquerque, A. L. S.] Univ Fed Fluminense, Programa Geociencias Geoquim, Niteroi, RJ, Brazil; [Portilho-Ramos, R. C.; Mulitza, S.; Kuhnert, H.; Vahlenkamp, M.; Bickert, T.] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Chiessi, C. M.] Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, Brazil; [Crivellari, S.] Univ Sao Paulo, Inst Geosci, Sao Paulo, Brazil; [Tiedemann, R.] Alfred Wegener Inst Polar & Marine Res, Bremerhaven, Germany; [Nobre, C.] Univ Sao Paulo, Inst Adv Studies, Sao Paulo, Brazil	Instituto Nacional de Pesquisas Espaciais (INPE); Universidade Federal Fluminense; University of Bremen; Universidade de Sao Paulo; Universidade de Sao Paulo; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Universidade de Sao Paulo	Venancio, IM (autor correspondente), Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Cachoeira Paulista, Brazil.	igor.venancio@inpe.br	Chiessi, Cristiano Mazur/E-1916-2012; Albuquerque, Ana Luiza S/C-5167-2013; Santos, Thiago P./AAN-6506-2021; Venancio, Igor M/I-5893-2014; Veiga, Sandro F./ABC-3723-2021	Chiessi, Cristiano Mazur/0000-0003-3318-8022; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Venancio, Igor M/0000-0003-3118-4247; Santos, Thiago/0000-0002-9273-3329; Shimizu, Marilia Harumi/0000-0003-0895-555X; Ferreira Veiga, Sandro Miguel/0000-0002-4546-1893; Crivellari, Stefano/0000-0003-3847-8854; Kuhnert, Henning/0000-0001-5242-4495	CAPES [88887.156152/2017-00, 88881.161151/2017-01, 564/2015]; CAPES/PDSE [99999.007924/2014-03]; CNPq [302607/2016-1, 422255/2016-5, 306385/2013-9, 99999.002675/2015-03]; FAPESP [2018/15123-4]; Alexander von Humboldt Foundation; CAPES-ASPECTO project [88887.091731/2014-01]; DFG Research Center/Cluster of Excellence "The Ocean in the Earth System"; Helmholtz Climate Initiative REKLIM; CNPq Project RAiN [406322/2018-0]	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CAPES/PDSE(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Alexander von Humboldt Foundation(Alexander von Humboldt Foundation); CAPES-ASPECTO project; DFG Research Center/Cluster of Excellence "The Ocean in the Earth System"(German Research Foundation (DFG)); Helmholtz Climate Initiative REKLIM; CNPq Project RAiN	We thank R. Kowsman (CENPES/Petrobras) and Petrobras Core Repository staff (Macae/Petrobras) for providing the sediment core employed in this research. We thank S. Pape and M. Willing for performing Mg/Ca analysis. CAPES financially supported I. M. V. with a scholarship (grant 88887.156152/2017-00 and 88881.161151/2017-01). T. P. S. acknowledges the financial support from CAPES/PDSE (grant 99999.007924/2014-03). A. L. A. is a CNPq senior researcher (grant 306385/2013-9) and thanks them for financial support (grant 99999.002675/2015-03). C. M. C. acknowledges the financial support from FAPESP (grant 2018/15123-4), CAPES (grant 564/2015), CNPq (grants 302607/2016-1 and 422255/2016-5) and the Alexander von Humboldt Foundation. This study was supported by CAPES-ASPECTO project (grant 88887.091731/2014-01). This work was also funded through the DFG Research Center/Cluster of Excellence "The Ocean in the Earth System" and by the Helmholtz Climate Initiative REKLIM. The data reported in this paper will be archived in Pangaea (www.pangaea.de). This study was supported by CNPq Project RAiN (grant: 406322/2018-0).	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Planet. Change	JAN	2020	184								103047	10.1016/j.gloplacha.2019.103047	http://dx.doi.org/10.1016/j.gloplacha.2019.103047			7	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	KE3XD					2023-06-23	WOS:000508491500002
J	Wilson, B; Coimbra, JC; Hayek, LAC				Wilson, Brent; Coimbra, Joao C.; Hayek, Lee-Ann C.			Benthic foraminifera and Neogene sea level changes in the Pelotas Basin, offshore south Brazil	OCEAN AND COASTAL RESEARCH			English	Article						Miocene; Uvigerinidae; Argentine Zoogeographic Province; Pelotas Basin; Florianopolis Platform; maximum flooding surface	STRATIGRAPHY; PATTERNS	The Neogene benthic foraminiferal ecostratigraphy of offshore Pelotas Basin has not yet been researched. The benthic foraminifera were examined in twenty-nine ditch cuttings samples from Well 1-SCS-3B, present water depth 200 m. These samples ranged from the Lower Miocene Catapsydrax dissimilis planktonic foraminiferal Zone to the Pliocene Globigerinoides trilobus fistulosus Zone. Only ditch cuttings were available, which allowed us to present just broad paleoenvironmental trends within the studied section. Benthic foraminifera indicate deposition mostly between outer neritic to upper bathyal paleodepths. A peak in uvigerinid relative abundance marks a possible flooding surface or condensed section with a high nutrient flux, low diversity (marked by the Shannon Function H), and sluggish circulation within the Globorotalia mayeri Zone. This peak is bracketed by high abundances of Cibicidoides, which indicate stronger current action than within the condensed section. Biostratigraphic hiatuses within these Cibicidoides-rich intervals are concluded not to indicate subaerial exposure, but to reflect current action sufficiently strong to induce either non-deposition or seafloor scouring. A second possible flooding surface occurs at the top of the section, indicated by a decline in Cibicidoides associated with upticks in Sphaeroidina and Bolivina and a dip in H. The top of this younger maximum flood was not encountered, probably occurring above the studied section. That the timing of these floods differs from those recorded elsewhere in the Pelotas Basin implies that they were tectonically induced, perhaps as distal effects associated with the interaction between the South American and Nazca tectonic plates. Future studies with better quality core samples will add detail to this picture; such studies can incorporate eustatic sea-level changes into the model presented.	[Wilson, Brent] Cedar Lodge, Ceinewydd SA45 9RL, Ceredigion, Wales; [Wilson, Brent] Univ West Indies, Dept Chem & Proc Engn, Petr Geosci Programme, St Augustine, Trinidad Tobago; [Coimbra, Joao C.] Univ Fed Rio Grande do Sul, Inst Geociencias, Dept Paleontol & Estratig, Cx P 15001, BR-91501970 Porto Alegre, RS, Brazil; [Hayek, Lee-Ann C.] Smithsonian Inst, Math & Stat, POB 37012,MRC 121, Washington, DC 20013 USA	University West Indies Mona Jamaica; University West Indies Saint Augustine; Universidade Federal do Rio Grande do Sul; Smithsonian Institution; Smithsonian National Museum of Natural History	Wilson, B (autor correspondente), Cedar Lodge, Ceinewydd SA45 9RL, Ceredigion, Wales.; Wilson, B (autor correspondente), Univ West Indies, Dept Chem & Proc Engn, Petr Geosci Programme, St Augustine, Trinidad Tobago.	brentforam@gmail.com	Coimbra, Joao Carlos/H-7500-2013	Coimbra, Joao Carlos/0000-0002-8980-6531; Wilson, Brent/0000-0002-7415-9773; Hayek, Lee-Ann/0000-0002-4266-3270	National Council for Scientific and Technological Development (CNPq) [305128/2017-5]; University of the West Indies, St. Augustine Campus	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); University of the West Indies, St. Augustine Campus	The authors are grateful to Petroleo Brasileiro S.A (Petrobras) for providing the samples. JCC thanks the National Council for Scientific and Technological Development (CNPq) for the grant 305128/2017-5. BW would like to thank the University of the West Indies, St. Augustine Campus, for support during the early stages of this work. We thank the two anonymous reviewers for their constructive comments on our work.	Altenbach AV, 1999, J FORAMIN RES, V29, P173; Anjos G.S., 2004, REV BRAS PALEONTOLOG, V7, P127; BARRON JA, 1982, GEOLOGY, V10, P577, DOI 10.1130/0091-7613(1982)10<577:WMDHCW>2.0.CO;2; BERGGREN WA, 1995, GEOL SOC AM BULL, V107, P1272, DOI 10.1130/0016-7606(1995)107<1272:LNCNPI>2.3.CO;2; Bolli H.M., 1985, PLANKTON STRATIGRAPH; Bolli H. 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Res.		2020	68								e20333	10.1590/s2675-28242020068333	http://dx.doi.org/10.1590/s2675-28242020068333			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	OR3GN		gold			2023-06-23	WOS:000589362200019
J	Azevedo, V; Strikis, NM; Santos, RA; de Souza, JG; Ampuero, A; Cruz, FW; de Oliveira, P; Iriarte, J; Stumpf, CF; Vuille, M; Mendes, VR; Cheng, H; Edwards, RL				Azevedo, Vitor; Strikis, Nicolas M.; Santos, Rudney A.; de Souza, Jonas Gregorio; Ampuero, Angela; Cruz, Francisco W.; de Oliveira, Paulo; Iriarte, Jose; Stumpf, Cintia F.; Vuille, Mathias; Mendes, Vinicius R.; Cheng, Hai; Edwards, R. Lawrence			Medieval Climate Variability in the eastern Amazon-Cerrado regions and its archeological implications	SCIENTIFIC REPORTS			English	Article							SPELEOTHEM RECORD; MESOAMERICAN MONSOON; 2 MILLENNIA; HOLOCENE; RAINFALL; PRECIPITATION; CAVE; AGE; RECONSTRUCTION; TEMPERATURE	The South American Monsoon System is responsible for the majority of precipitation in the continent, especially over the Amazon and the tropical savannah, known as 'Cerrado'. Compared to the extensively studied subtropical and temperate regions the effect of the Medieval Climate Anomaly (MCA) on the precipitation over the tropics is still poorly understood. Here, we present a multiproxy paleoprecipitation reconstruction showing a consistent change in the hydrologic regime during the MCA in the eastern Amazon and 'Cerrado', characterized by a substantial transition from humid to drier conditions during the Early (925-1150 C.E.) to Late-MCA (1150-1350 C.E.). We compare the timing of major changes in the monsoon precipitation with the expansion and abandonment of settlements reported in the archeological record. Our results show that important cultural successions in the pre-Columbian Central Amazon, the transition from Paredao to Guarita phase, are in agreement with major changes in the hydrologic regime. Phases of expansion and, subsequent abandonment, of large settlements from Paredao during the Early to Late-MCA are coherent with a reduction in water supply. In this context we argue that the sustained drier conditions during the latter period may have triggered territorial disputes with Guarita leading to the Paredao demise.	[Azevedo, Vitor; Strikis, Nicolas M.; Ampuero, Angela] Fluminense Fed Univ, Geochem Dept, BR-24020141 Niteroi, RJ, Brazil; [Santos, Rudney A.; Cruz, Francisco W.; de Oliveira, Paulo] Univ Sao Paulo, Geosci Inst, BR-05508080 Sao Paulo, Brazil; [de Souza, Jonas Gregorio; Iriarte, Jose] Univ Exeter, Dept Archeol, Exeter, Devon, England; [Stumpf, Cintia F.] Univ Brasilia, Geociences Inst, BR-70910900 Brasilia, DF, Brazil; [Vuille, Mathias] SUNY Albany, Dept Atmospher & Environm Sci, Albany, NY 12222 USA; [Mendes, Vinicius R.] Univ Fed Sao Paulo, Marine Sci Dept, BR-11050020 Santos, SP, Brazil; [Cheng, Hai] Xi An Jiao Tong Univ, Inst Global Environm Change, Xian, Peoples R China; [Cheng, Hai; Edwards, R. Lawrence] Univ Minnesota, Dept Earth & Environm Sci, Minneapolis, MN USA	Universidade Federal Fluminense; Universidade de Sao Paulo; University of Exeter; Universidade de Brasilia; State University of New York (SUNY) System; State University of New York (SUNY) Albany; Universidade Federal de Sao Paulo (UNIFESP); Xi'an Jiaotong University; University of Minnesota System; University of Minnesota Twin Cities	Azevedo, V (autor correspondente), Fluminense Fed Univ, Geochem Dept, BR-24020141 Niteroi, RJ, Brazil.	vitorazevedoalves@gmail.com	mendes, vinicius ribau/P-7064-2016; Santos, Rudney/AAD-5301-2022; Iriarte, Jose/A-1141-2010; de Almeida Santos, Rudney/AAD-5079-2022; Cruz, Francisco W/G-6059-2012; Vuille, Mathias/O-8128-2019; CHENG, HAI/H-3413-2017	mendes, vinicius ribau/0000-0003-1072-8292; de Almeida Santos, Rudney/0000-0002-1398-1835; Vuille, Mathias/0000-0002-9736-4518; CHENG, HAI/0000-0002-5305-9458; Ampuero Grandez, Angela/0000-0002-1264-9152; Cruz, Francisco/0000-0002-4030-4581; Gregorio de Souza, Jonas/0000-0001-6032-4443; Iriarte, Jose/0000-0002-8155-5360; Azevedo Alves, Vitor/0000-0002-1893-1618	FAPESP [2017/50085-3 PIRE NSF-FAPESP, 2016/02656-9]; CAPES [AUXPE PREMIO 2043/2014]; CLIMATE-PRINT-UFF Project (CAPES) [88887.310301/2018-00]; NSF [OISE-1743738]; CNPq [423573/2018-7, 426258/2016-9]	FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CLIMATE-PRINT-UFF Project (CAPES); NSF(National Science Foundation (NSF)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank A. Barros, Y. Ning and I. Pedron for their support during the stable isotope data acquisition at the University of Sao Paulo and dating analyses at the Xi'an Jiaotong University. We thank A. Auler, S. Carolin, J. Watling, V. Novello and an anonymous reviewer for their suggestions regarding the manuscript. We are grateful to Instituto Brasileiro do Meio Ambiente/Instituto Chico Mendes de Conservacao da Biodiversidade (IBAMA/ICMBio) for permission to collect stalagmite samples. This work was supported by FAPESP (Grants 2017/50085-3 PIRE NSF-FAPESP and 2016/02656-9), CAPES (AUXPE PREMIO 2043/2014 to R.A.S. and Master Fellowship to V.A.), CLIMATE-PRINT-UFF Project (CAPES grant 88887.310301/2018-00), NSF grant OISE-1743738 and CNPq (Grants 423573/2018-7 and 426258/2016-9).	Behling H, 2000, J QUATERNARY SCI, V15, P687, DOI 10.1002/1099-1417(200010)15:7<687::AID-JQS551>3.0.CO;2-6; Blaauw M, 2011, BAYESIAN ANAL, V6, P457, DOI 10.1214/ba/1339616472; Bozrath S. 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J	Aboim, IL; Gomes, DF; Mafalda, PO				Aboim, Igor Lima; Gomes, Doriedson Ferreira; Mafalda Junior, Paulo Oliveira			Phytoplankton response to water quality seasonality in a Brazilian neotropical river	ENVIRONMENTAL MONITORING AND ASSESSMENT			English	Article						Phytoplankton ecology; Functional groups; Jequitinhonha River; Eutrophication	FUNCTIONAL-GROUPS; LAND-USE; EUTROPHICATION; NUTRIENT; DIVERSITY; DOMINANCE; COMMUNITY; GRADIENT; ESTUARY; STREAM	Tropical wet-dry climate seasonality is widely recognized as an important condition to phytoplankton communities' structure in freshwater ecosystems; however, there are few studies in that field in northeast Brazilian rivers. This study aimed to evaluate the influence of water quality seasonal variability over the phytoplankton dynamics and identify seasonality in eutrophication phenomena in a poorly studied neotropical river. Water quality variables and phytoplankton were examined within the Jequitinhonha River lower course, Bahia (Brazil) from 2010 to 2012. A 3-year time series was analyzed for both rainy and dry seasons. Descriptive, inferential, and multivariate analyses (CCA) were performed. Results indicated that chemical oxygen demand, dissolved aluminum, and turbidity were the main factors which influenced phytoplankton community structure and composition. Dry season was favorable for diatoms and Chlorophyceae (chlorophylls) while rainy season was favorable for cyanobacteria. Still, it was revealed that, in dry season, lower values for turbidity, chemical oxygen demand, dissolved aluminum, and dissolved iron were related with an eutrophication phenomenon.	[Aboim, Igor Lima; Mafalda Junior, Paulo Oliveira] Univ Fed Bahia, Lab Plancton LABPLAN, Inst Biol, Rua Barao Jeremoabo S-N,Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Gomes, Doriedson Ferreira] Univ Fed Bahia, Lab Paleoecol EcoPaleo, Inst Biol, Rua Barao Jeremoabo S-N,Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal da Bahia	Aboim, IL (autor correspondente), Univ Fed Bahia, Lab Plancton LABPLAN, Inst Biol, Rua Barao Jeremoabo S-N,Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.	igoraboim@gmail.com	Gomes, Doriedson F./F-8228-2013	Gomes, Doriedson F./0000-0002-1569-8101	VERACEL Papel e Celulose; CAPES-Central de Aperfeicoamento de Pessoal de Ensino Superior, within the Ministerio da Educacao do Brasil [001]	VERACEL Papel e Celulose; CAPES-Central de Aperfeicoamento de Pessoal de Ensino Superior, within the Ministerio da Educacao do Brasil	This research was partially supported by VERACEL Papel e Celulose and was conducted during a scholarship Financed by CAPES-Central de Aperfeicoamento de Pessoal de Ensino Superior-Finance Code 001, within the Ministerio da Educacao do Brasil.	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J	Schettini, CAF; Asp, NE; Ogston, AS; Gomes, VJC; McLachlan, RL; Fernandes, MEB; Nittrouer, CA; Truccolo, EC; Gardunho, DCL				Schettini, Carlos A. F.; Asp, Nils E.; Ogston, Andrea S.; Gomes, Vando J. C.; McLachlan, Robin L.; Fernandes, Marcus E. B.; Nittrouer, Charles A.; Truccolo, Eliane C.; Gardunho, Danilo C. L.			Circulation and fine-sediment dynamics in the Amazon Macrotidal Mangrove Coast	EARTH SURFACE PROCESSES AND LANDFORMS			English	Article						mangroves; tidal circulation; mud dynamics; tropical systems; sediment budget	SUSPENDED SEDIMENT; TURBIDITY MAXIMUM; TRANSPORT; ESTUARY; RIVER; BAY; HYDRODYNAMICS; ASYMMETRY; CURRENTS; FORESTS	The Amazon Macrotidal Mangrove Coast (AMMC) is a large (similar to 7500 km(2)) contiguous mangrove fringe eastwards from the Amazon River mouth. It encompasses dozens of interconnected bays intercalated with mangrove peninsulas. Mud accumulates on the mangrove flats, whereas the bed of the bays and channels is generally sandy. In this study we investigated the circulation, sediment transport and deposition in a central site at one of these mangrove peninsulas. The study was undertaken during the dry period, when there is no influence of the Amazon River plume and minimum local freshwater inflow. Current and suspended-sediment concentration were monitored in a feeder channel on the mangrove flat along a similar to 1000 m section oriented along the peninsula axis. Sediment deposition was also measured on the flat. Our results show there was a strong exchange between the neighboring bays. Channel currents were flood dominant, reaching up to >1 m s(-1), with residual water and sediment transport westwards. Suspended sediment concentration (SSC) in the channel was directly related to velocity magnitude, ranging between 50 and 350 mg L-1. The flat was flooded in a way that indicated the tidal wave evolves westwards, nearly parallel to the AMMC shoreline. Currents on the flats were much slower than those in the channel and showed slight ebb dominance. However, SSC was higher during the flood than ebb, clearly indicating settling during the current deceleration and limited erosion during the following ebb-flow acceleration. The net sediment transport across the section was 60 tons westwards for the period of the experiment (similar to 4 days). The mean deposition rate was 0.006 kg m(-2) s(-1) (or 1.4 kg m(-2) per tide), which was higher than rates from other reported assessments in mangroves. The set of results indicate very large internal sediment reworking in the AMMC. (c) 2019 John Wiley & Sons, Ltd.	[Schettini, Carlos A. F.; Truccolo, Eliane C.] Fed Univ Rio Grande, Inst Oceanog, Ave Italia,Km 8, BR-96201900 Rio Grande, RS, Brazil; [Asp, Nils E.; Gomes, Vando J. C.; Fernandes, Marcus E. B.; Gardunho, Danilo C. L.] Fed Univ Para, Inst Coastal Studies, Belem, Para, Brazil; [Ogston, Andrea S.; McLachlan, Robin L.; Nittrouer, Charles A.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA	Universidade Federal do Rio Grande; Universidade Federal do Para; University of Washington; University of Washington Seattle	Schettini, CAF (autor correspondente), Fed Univ Rio Grande, Inst Oceanog, Ave Italia,Km 8, BR-96201900 Rio Grande, RS, Brazil.	guto.schettini@gmail.com	Asp, Nils/J-6226-2012	Asp, Nils/0000-0002-6468-6158	Brazilian Project Funding Agency (FINEP) [1826/10]; Brazilian National Science Council (CNPq) [401215/2014-8]; Office of Naval Research Global [N62909-14-1-N205]	Brazilian Project Funding Agency (FINEP); Brazilian National Science Council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Office of Naval Research Global(Office of Naval Research)	We thank the Brazilian Project Funding Agency (FINEP, ref. 1826/10), the Brazilian National Science Council (CNPq, ref. #401215/2014-8) and the Office of Naval Research Global (grant number N62909-14-1-N205) for financial support. To the anonymous reviewers in helping to improve the manuscript. We want also to acknowledge Prof. Pedro Souza for lending some of the instruments used in the experiment, and the many students from UFPA/IECOS/Braganca, Paulo Freitas, Elielton Monteiro, Giordana Maciel, Alessandra Braga, Amanda Oliveira, Denise Freitas, Clauber Santiago e Jessica Natalia, for field assistance.	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J	Guzman-Gonzalez, J; Sial, AN; Piovesan, EK; Oliveira, EV; Fambrini, GL				Guzman-Gonzalez, Juliana; Sial, Alcides N.; Piovesan, Enelise Katia; Oliveira, Edison Vicente; Fambrini, Gelson Luis			Paleolimnological reconstruction of a marginal area of Jurassic Capianga Lake, Jatoba Basin, northeast Brazil	JOURNAL OF PALEOLIMNOLOGY			English	Article						Alianca formation; Jatoba Basin; Paleolimnology; Biogenic carbonate; Ostracodes; Stable isotopes	CARBON; OXYGEN; ISOTOPES; PALEOCLIMATE; EASTERN	The Alianca Formation, within the Brazilian Reconcavo-Tucano-Jatoba Rift System, is a succession of Late Jurassic sedimentary rocks that record the maximum flooding surface of shallow Capianga Lake in the Afro-Brazilian Depression, Gondwana. Several aulacogens and drift-marginal Mesozoic basins of eastern Brazil and western Africa recorded the great extensional event that occurred during the early stage of Gondwana break-up. Lithologic, petrographic, micropaleontological and geochemical analyses of lacustrine carbonates collected near the city of Ibimirim, Pernambuco State, were carried out to establish the paleolimnological evolution of a marginal area of Capianga Lake, in the Jatoba Basin. The ostracode fauna, obtained from grainstone and calcareous quartzarenite, is constituted by Theriosynoecum pricei, Theriosynoecum uninodosa, Theriosynoecum quadrinodosum, Reconcavona? jatobaensis and Alicenula? spp. Carbon and oxygen stable isotopes in bulk rock, Theriosynoecum pricei and Alicenula? spp. were measured. Theriosynoecum pricei displays the most negative delta C-13 values, between - 2.1 and - 1.3 parts per thousand. The delta C-13 values obtained from Alicenula? spp. and bulk rock were also negative. The delta O-18 values for Theriosynoecum pricei range from - 10.1 to + 4.1 parts per thousand. Alicenula? spp. show delta O-18 values between - 4.6 and + 5.8 parts per thousand. The bioclastic character of the carbonates and the presence of cross-bedding and ripple marks suggest deposition in a low-energy, low-gradient, ramp-type littoral zone of a shallow, balanced-fill lake. The ostracode association, characteristic of permanent, alkaline, freshwater bodies, corresponds to the Theriosynoecum pricei ostracode biozone, which is of Tithonian age. The lithofacies, along with covariation of delta C-13 and delta O-18, and large delta O-18 fluctuations, suggest that this marginal area of Capianga Lake was characterized by stable hydrological conditions in a closed basin. The delta C-13 values display a slightly narrower range, suggesting oligotrophic to slightly mesotrophic conditions, and holomixis in this marginal area of Capianga Lake.	[Guzman-Gonzalez, Juliana; Piovesan, Enelise Katia] Univ Fed Pernambuco, Appl Micropaleontol Lab LMA, BR-50740540 Recife, PE, Brazil; [Sial, Alcides N.] Univ Fed Pernambuco, Nucleus Geochem Studies Stable Isotope Lab NEG LA, BR-50740530 Recife, PE, Brazil; [Oliveira, Edison Vicente] Univ Fed Pernambuco, Paleontol Lab PALEOLAB, BR-50740530 Recife, PE, Brazil; [Fambrini, Gelson Luis] Univ Fed Pernambuco, Sedimentary Geol Lab LAGESE, BR-50740540 Recife, PE, Brazil	Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal de Pernambuco; Universidade Federal de Pernambuco	Guzman-Gonzalez, J (autor correspondente), Univ Fed Pernambuco, Appl Micropaleontol Lab LMA, BR-50740540 Recife, PE, Brazil.	julitaguzmang@gmail.com; sial@ufpe.br; katiapiovesan@gmail.com; vicenteedi@gmail.com; g_fambrini@yahoo.com	Sial, Alcides/AAD-1901-2021; Oliveira, Édison Vicente/A-8427-2011; Piovesan, Enelise Katia/Q-2953-2017	Piovesan, Enelise Katia/0000-0002-0433-0395; Guzman, Juliana/0000-0001-7898-049X; Oliveira, Edison/0000-0001-6634-5480	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [161599/2014-1, 480275/2012-2]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Funding was provided by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (Grant Nos. 161599/2014-1, 480275/2012-2).	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J	Pires, LN; Dias, FD; Teixeira, LS				Pires, Lais N.; Dias, Fabio de S.; Teixeira, Leonardo Sg			Assessing the internal standardization of the direct multi-element determination in beer samples through microwave-induced plasma optical emission spectrometry	ANALYTICA CHIMICA ACTA			English	Article						Microwave induced plasma optical emission spectrometry; Internal standardization; Beer; Multi-element determination	HYDRIDE-FORMING ELEMENTS; TRACE-ELEMENTS; ATOMIC SPECTROMETRY; DILUTION ANALYSIS; ALCOHOLIC BEVERAGES; INTRODUCTION SYSTEM; PRECIOUS METALS; MIP-OES; CU; PB	An evaluation of different elements (Be, Ga, In, Sc, and Y) as internal standards was performed to determine the content of Al, Ba, Co, Cr, Cu, Fe, Mn, Ni, Sr, Zn, Ca, Mg, Na, K in beer samples through microwave induced plasma optical emission spectrometry. The analytes were determined after simple dilutions of the samples with a 1.0 M nitric acid solution at a 1:4 ratio (sample: acid solution) with the addition of the IS. The analytical performance for each potential IS was established based on the limit of detection, limit of quantification, addition and recovery tests and accuracy obtained in the determination of each analyte. Each analyte responded differently when internal standardization was applied, and as such, the evaluation of each IS is important in the development of the method. In the presence of the recommended internal standard, the limit of detection varied, in mu g L-1, from 0.23 to 4.6 for the microelements and between 10 and 620 for the macroelements. The limit of quantification, in mu g L-1, was between 0.78 and 15.4 and between 30 and 970 for the microelements and macroelements, respectively. The precisions of the measurements, expressed as the relative standard deviation (n = 10; 0.50 and 3.0 mg L-1 of each analyte), were lower than 1.0% for all analytes. The proposed method was applied for the multi-element determination in commercial beer samples and the results were compared with those obtained by inductively coupled plasma optical emission spectrometry after sample digestion. (C) 2019 Elsevier B.V. All rights reserved.	[Pires, Lais N.; Teixeira, Leonardo Sg] Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil; [Dias, Fabio de S.] Univ Fed Reconcavo Bahia, Ctr Ciencias Exatas & Tecnol, Campus Univ Cruz das Almas, BR-44380000 Cruz Das Almas, BA, Brazil; [Teixeira, Leonardo Sg] Univ Fed Bahia, INCT Energia & Ambiente, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil	Universidade Federal da Bahia; Universidade Federal do Reconcavo da Bahia; Universidade Federal da Bahia	Teixeira, LS (autor correspondente), Univ Fed Bahia, Inst Quim, Dept Quim Analit, Campus Univ Ondina, BR-40170115 Salvador, BA, Brazil.	lsgt@ufba.br	Teixeira, Leonardo S G/J-9131-2016; de Souza Dias, Fabio/I-4716-2013	Teixeira, Leonardo S G/0000-0003-0320-8299; 	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) [001]; Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)(Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brasil (CAPES) - Finance Code 001. The authors are also grateful to Fundacao de Amparo a Pesquisa do Estado da Bahia (FAPESB) and Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for providing grants, fellowships and financial support.	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Chim. Acta	DEC 20	2019	1090						31	38		10.1016/j.aca.2019.09.033	http://dx.doi.org/10.1016/j.aca.2019.09.033			8	Chemistry, Analytical	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry	JG3AI	31655643				2023-06-23	WOS:000491946300003
J	Janikian, L; de Almeida, RP; Galeazzi, CP; Tamura, LN; Ardito, JC; Chamani, MAC				Janikian, Liliane; de Almeida, Renato Paes; Galeazzi, Cristiano Padalino; Tamura, Larissa Natsumi; Ardito, Julio Cesar; Carrari Chamani, Marley Antonio			Variability of fluvial architecture in a poorly vegetated Earth: Silurian sheet-braided and meandering ancestor river deposits recorded in northeastern Brazil	TERRA NOVA			English	Article						bar surface orientation; clinoform modelling; Early Paleozoic rivers; meandering ancestors; paleocurrents	PARNAIBA BASIN; EVOLUTION; MODELS; PLANTS	Rivers with little to no influence of vegetation and their implications for the architecture of Early Paleozoic and Precambrian fluvial deposits are an important topic of investigation for both clastic sedimentology and Earth System evolution perspectives. Despite the long-held concept of a dominant style of wide, shallow sheet-braided sandy channels, growing evidence for a great variability of architectural elements in pre-vegetation settings point to the predictable occurrence of other fluvial styles, which are possibly related to areas of low-slope alluvial plains. The present work brings sedimentological descriptions and fluvial style interpretations of Silurian fluvial successions of the Serra Grande Group in northeastern Brazil, developed in a glaciated basin margin (therefore with little to no effect of vegetation). The comparison of the resulting channel body architectures integrated to paleocurrent data and a diffusion-based numerical model enabled the evaluation of the controls on fluvial architecture variability in unvegetated alluvial plains.	[Janikian, Liliane] Univ Fed Sao Paulo, Inst Mar, Santos, SP, Brazil; [de Almeida, Renato Paes; Galeazzi, Cristiano Padalino; Tamura, Larissa Natsumi; Ardito, Julio Cesar; Carrari Chamani, Marley Antonio] Univ Sao Paulo, Inst Geociencias, Sao Paulo, SP, Brazil	Universidade Federal de Sao Paulo (UNIFESP); Universidade de Sao Paulo	Janikian, L (autor correspondente), Univ Sao Paulo, Dept Geofis, Inst Astron Geofis & Ciencias Atmosfer, Rua Matao 1226,Cidade Univ, BR-05508900 Sao Paulo, SP, Brazil.	lijanikian@yahoo.com.br	Galeazzi, Cristiano/AGX-8001-2022; Almeida, Renato/AAF-6705-2020; Janikian, Liliane/P-1218-2015; Almeida, Renato/G-2567-2013	Almeida, Renato/0000-0003-3664-1558; Galeazzi, Cristiano/0000-0001-7285-2884	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo [2016/03091-5, 2017/06874-3]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico [142276/2015-4, 306513/2016-1]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Fundacao de Amparo a Pesquisa do Estado de Sao Paulo(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior; Fundacao de Amparo a Pesquisa do Estado de Sao Paulo, Grant/Award Number: 2016/03091-5 and 2017/06874-3; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, Grant/Award Number: 142276/2015-4 and 306513/2016-1	Almeida RP, 2016, SEDIMENTOLOGY, V63, P609, DOI 10.1111/sed.12230; Bridgland DR, 2014, P GEOLOGIST ASSOC, V125, P503, DOI 10.1016/j.pgeola.2014.11.001; BUTTON A, 1981, EC GEOLOGY ANNIVERSA, V0075, P00686; CAPUTO Mario Vicente, 1984, 33 C BRAS GEOL RIO J, V33, P740; CASSHYAP SM, 1968, J SEDIMENT PETROL, V38, P920; Cotter E., 1978, CANADIAN SOC PETROLE, V5, P361; Cunha F. 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G. F., 1978, FLUVIAL SEDIMENTOLOG; Long DGF, 2011, SOC SEDIMENT GEOL SP, P37; McMahon W. J., 2018, FLUVIAL MEANDERS THE; Miall A. D., 1996, GEOLOGY FLUVIAL DEPO; Paola C, 2000, SEDIMENTOLOGY, V47, P121, DOI 10.1046/j.1365-3091.2000.00006.x; PEMBERTON SG, 1992, SEPM CORE WORKSHOP, V17, P339; Salamon MA, 2018, NEW PHYTOL, V218, P1305, DOI 10.1111/nph.15091; Santos MGM, 2014, SEDIMENTOLOGY, V61, P881, DOI 10.1111/sed.12074; Schumm S. A., 1969, GSA B, V79, P1573; Silva A.J.P., 2003, GEOLOGIA TECTONICA R, P55; Steemans P., 2014, SCIENCE, V324, P352, DOI 10.1126/science.1169659; SWEET IP, 1988, SEDIMENT GEOL, V58, P277, DOI 10.1016/0037-0738(88)90073-5; Syvitski JPM, 2007, J GEOL, V115, P1, DOI 10.1086/509246; Vaz P.T., 2007, B GEOCIE NCIAS PETRO, V15, P253	36	10	10	0	4	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0954-4879	1365-3121		TERRA NOVA	Terr. Nova	JUN	2020	32	3					187	197		10.1111/ter.12446	http://dx.doi.org/10.1111/ter.12446		DEC 2019	11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	LN9HX					2023-06-23	WOS:000503357300001
J	Marangoanha, B; de Oliveira, DC; Dall'Agnol, R				Marangoanha, Bhrenno; de Oliveira, Davis Carvalho; Dall'Agnol, Roberto			The Archean granulite-enderbite complex of the northern Carajas province, Amazonian craton (Brazil): Origin and implications for crustal growth and cratonization	LITHOS			English	Article						Neoarchean enderbite; Mesoarchean granulite; Geochemistry; U-Pb; Lu-Hf; Carajas province	PLASMA-MASS SPECTROMETRY; U-PB GEOCHRONOLOGY; CONTINENTAL-CRUST; HF ISOTOPES; LU-HF; ZIRCON; GEOCHEMISTRY; MAGMATISM; CONSTRAINTS; EVOLUTION	The central portion of the Canaa dos Carajas domain (Ouro Verde area) exhibits a peculiar scenario involving two units of orthopyroxene-bearing sodic rocks: (i) the Mesoarchean Ouro Verde felsic granulite with protolith crystallization and metamorphism ages of 3.05-2.93 Ga and 2.89-2.84 Ga, respectively, and (ii) the Neoarchean Caf enderbite, composed of tonalites, trondhjemites and scarce quartz diorites that crystallized at 2.75-2.73 Ga and show syntectonic character. While the orthopyroxene in the felsic granulites was formed by breakdown of primary biotite during metamorphism, in the enderbitic rocks, this mineral was formed by crystallization of a hot water-poor magma at deep crustal levels. This terrane evolved in three important geodynamic stages: (1) at 3.05-2.93 Ga, TTG crust was generated by partial melting of LILE-enriched basalts in a N-S subduction setting; (2) from 2.89 to 2.84 Ga, in a collisional setting, large volumes of anatectic granites formed and contributed to crustal thickening, which triggered granulite-facies ultrahigh-temperature metamorphism in the TTG crust, forming the Ouro Verde felsic granulite; and (3) in the Neoarchean, at 2.75-2.73 Ga, the lowermost mafic crust was delaminated during crustal thickening, causing crustal underplating followed by partial melting of Mesoarchean mafic granulites, which was responsible for the origin of the enderbitic magma. This area was subjected to a transpressional tectonic regime, leading to the development of plutons (E W-trending) amalgamated linearly and emplaced along ancient suture zones (ductile-brittle transition). Lu-Hf isotope data of magmatic zircon cores from the Mesoarchean felsic granulite show Hf-T-DM2 values of 3.44-3.15 Ga and epsilon Hf(t) values between -1.7 and 3.0, which suggest juvenile sources. The Neoarchean enderbites present Hf-T-DM2 ages of 3.46-3.29 Ga and lower eHf(t) values (between 4.8 and 1.9), which indicate a longer crustal residence time for these rocks. All these findings lead us to consider the central portion of the Canaa dos Carajas domain as exhumed lower crust, and the tectonic juxtaposition of anatectic granites, enderbites and high-grade metamorphic rocks suggests that the Ouro Verde area represents middle and deep exposure levels of the same crust. (C) 2019 Elsevier B.V. All rights reserved.	[Marangoanha, Bhrenno; de Oliveira, Davis Carvalho; Dall'Agnol, Roberto] Univ Fed Para UFPA, IG, GPPG, Rua Augusto Correa 01, BR-66075110 Belem, Para, Brazil; [Marangoanha, Bhrenno; de Oliveira, Davis Carvalho; Dall'Agnol, Roberto] UFPA, IG, PPGG, Belem, Para, Brazil; [Dall'Agnol, Roberto] ITV, Belem, Para, Brazil	Universidade Federal do Para; Universidade Federal do Para; Instituto Tecnologico Vale Desenvolvimento Sustentavel	Marangoanha, B (autor correspondente), Univ Fed Para UFPA, IG, GPPG, Rua Augusto Correa 01, BR-66075110 Belem, Para, Brazil.	bhrenno@ufpa.br; davis@ufpa.br; robdal@ufpa.br		Marangoanha, Bhrenno/0000-0003-0741-5148	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [163874/2014-0, 311388/2016-7, 485806/2013-4, 435552/2018-0, 306108/2014-3]; Fundo de Amparo a Pesquisa do Estado do Para (FAPESPA) [133/2008-0]; Vale/FAPESPA (ICAAF) [053/2011]; INCT program (CNPq/FAPESPA/CAPES/PETROBRAS) [573733/2008-2]; PROPESP (PAPQ)/UFPA; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) [001]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundo de Amparo a Pesquisa do Estado do Para (FAPESPA); Vale/FAPESPA (ICAAF); INCT program (CNPq/FAPESPA/CAPES/PETROBRAS); PROPESP (PAPQ)/UFPA; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES))	We would like to thank C.N. Lamarao and G.T. Marques for providing BSE and CL images obtained at the Laboratorio de Microanalises (UFPA). We are also grateful to K. Sato and A.T. Onoe for assistance during the acquisition of U-Pb SHRIMP data at the Laboratorio de Geologia de Alta Resolucao (USP), and A.R. Alkmim for the help provided during the acquisition of U-Pb LA-SF-ICP-MS and Lu-Hf data at the Laboratorio de Geoquimica IsotOpica (UFOP). The constructive reviews of Jaana Halla and an anonymous reviewer and encouraging editorial input by Michael Roden are gratefully acknowledged. The first author (BM) thanks the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for a doctoral thesis scholarship (Proc. 163874/2014-0). Funding for this project came from CNPq (D.C. Oliveira - Proc. 311388/2016-7, 485806/2013-4 and 435552/2018-0; R. Dall'Agnol - Proc. 306108/2014-3), the Fundo de Amparo a Pesquisa do Estado do Para (FAPESPA; Proc. 133/2008-0), Vale/FAPESPA (ICAAF n. 053/2011), the INCT program (CNPq/FAPESPA/CAPES/PETROBRAS; Proc. 573733/2008-2) and PROPESP (PAPQ)/UFPA. This study was financed in part by the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior - Brazil (CAPES) - Finance Code 001.	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J	Satge, F; Hussain, Y; Xavier, A; Zola, RP; Salles, L; Timouk, F; Seyler, F; Garnier, J; Frappart, F; Bonnet, MP				Satge, Frederic; Hussain, Yawar; Xavier, Alvaro; Zola, Ramiro Pillco; Salles, Leandro; Timouk, Franck; Seyler, Frederique; Garnier, Jeremie; Frappart, Frederic; Bonnet, Marie-Paule			Unraveling the impacts of droughts and agricultural intensification on the Altiplano water resources	AGRICULTURAL AND FOREST METEOROLOGY			English	Article						Climate; Agriculture; Water scarcity; Hydrological drought; Remote sensing	QUINOA PRODUCTION; METAL CONCENTRATION; SOUTHERN BOLIVIA; TRACE-ELEMENTS; CLIMATE-CHANGE; PRECIPITATION; EXPOSURE; VARIABILITY; ACCURACY; TITICACA	During the last decades, agriculture has drastically increased over the South American Andean Plateau (Altiplano), resulting in extensive changes in land cover from native vegetation to essentially Quinoa crop. Along with climatic variability, these land use changes appear as a catalyst in worsening the already existing drought events and water scarcity processes. Hence, understanding their relative contributions to the regional desertification process is crucial for sustainable water-use adaptation, but also is quite ambiguous because of water resource data scarcity over the Altiplano. Therefore, in the present study, an attempt to measure the impact of severe droughts and agricultural intensification on the water resources has been made using remote sensing datasets. The first step was dedicated to the validation of newly released CHIRPS v.2 precipitation and GLEAM v.3 potential evapotranspiration products by comparing their estimates with the results obtained from gauges data. Then, the Standardized Precipitation Index (SPI) was used to describe past hydro-meteorological drought events in terms of their spatial extent, duration, intensity and their impacts on the regional water resources. Finally, the dynamic trends in the spatial extent of the Quinoa crop and the meteorological conditions derived from CHIRPS v.2 and GLEAM v.3 were compared with the Vegetation Condition Index (VCI) and the Total Water Storage (TWS) derived from AVHRR and GRACE data respectively, to observe the respective influence of agriculture and climate variability on the regional hydrological system. A significant increase in Quinoa crop extent is observed from 2001 which corresponds to a significant decrease in regional VCI and TWS. Based on this trend, agriculture appears as a contributing factor in the water scarcity process over the Altiplano. The outcomes of this study will contribute to local decision making for a better water management and hydro-meteorological monitoring system.	[Satge, Frederic; Seyler, Frederique; Bonnet, Marie-Paule] IRD, UMR 228, Espace Dev ESPACE DEV, Montpellier, France; [Hussain, Yawar; Xavier, Alvaro; Salles, Leandro; Garnier, Jeremie] Univ Brasilia UnB, Inst Geociencias, Brasilia, DF, Brazil; [Hussain, Yawar] Univ Brasilia, Dept Engn Civil & Ambiental, Brasilia, DF, Brazil; [Zola, Ramiro Pillco] UMSA, IHH, La Paz, Bolivia; [Timouk, Franck] IRD, GET, UMR 5563, Toulouse, France; [Frappart, Frederic] Univ Toulouse, UPS, UMR 5566, CNES,CNRS,IRD,LEGOS, 14 Ave Edouard Belin, F-31400 Toulouse, France	Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Universidade de Brasilia; Universidade de Brasilia; Universidad Mayor de San Andres; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Toulouse; Universite Toulouse III - Paul Sabatier; Institut de Recherche pour le Developpement (IRD); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Toulouse; Universite Toulouse III - Paul Sabatier; Institut de Recherche pour le Developpement (IRD); Laboratoire d'Etudes en Geophysique et oceanographie spatiales	Satge, F (autor correspondente), Maison Teledetect, 500 Rue Jean Francois Breton, F-34090 Montpellier, France.	frederic.satge@ird.fr	garnier, jeremie/AAK-8470-2021; Seyler, Frédérique/D-5518-2011; Hussain, Yawar/Q-1597-2015	garnier, jeremie/0000-0001-9571-7933; Seyler, Frédérique/0000-0002-3609-7524; Hussain, Yawar/0000-0002-4155-6764; Frappart, Frederic/0000-0002-4661-8274; Salles, Leandro/0000-0002-6056-7055; SATGE, Frederic/0000-0003-3662-6876	Centre National d'Etudes Spatiales (CNES), France; Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brazil; Institut de Recheche pour le Developpement (IRD), France	Centre National d'Etudes Spatiales (CNES), France(Centre National D'etudes Spatiales); Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brazil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Institut de Recheche pour le Developpement (IRD), France	This work was supported by the Centre National d'Etudes Spatiales (CNES), France, in the framework of the HASM project (Hydrology of Altiplano: from Spatial to Modeling); the Institut de Recheche pour le Developpement (IRD), France, and the Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES), Brazil.	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For. Meteorol.	DEC 15	2019	279								107710	10.1016/j.agrformet.2019.107710	http://dx.doi.org/10.1016/j.agrformet.2019.107710			13	Agronomy; Forestry; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Agriculture; Forestry; Meteorology & Atmospheric Sciences	JS3GO					2023-06-23	WOS:000500197400021
J	Sha, LJ; Brahim, YA; Wassenburg, JA; Yin, JJ; Peros, M; Cruz, FW; Cai, YJ; Li, HY; Du, WJ; Zhang, HW; Edwards, RL; Cheng, H				Sha, Lijuan; Brahim, Yassine Ait; Wassenburg, Jasper A.; Yin, Jianjun; Peros, Matthew; Cruz, Francisco W.; Cai, Yanjun; Li, Hanying; Du, Wenjing; Zhang, Haiwei; Edwards, R. Lawrence; Cheng, Hai			How Far North Did the African Monsoon Fringe Expand During the African Humid Period? Insights From Southwest Moroccan Speleothems	GEOPHYSICAL RESEARCH LETTERS			English	Article						African Humid Period; speleothem delta O-18 records; Holocene; abrupt climate change; West African summer monsoon	ATLANTIC OSCILLATION; HOLOCENE CLIMATE; SAHARA; PRECIPITATION; OXYGEN; TERMINATION; VARIABILITY; EVOLUTION; HYDROCLIMATE; MECHANISMS	We present new high-resolution oxygen isotope (delta O-18) records from three NW African speleothems located at 31 degrees N. The present-day rainfall patterns at 31 degrees N in NW Africa are linked to negative winter North Atlantic Oscillation phases. However, on multimillennial time scales, our delta O-18 records, together with other hydroclimate records, provide new evidence of humid conditions during the mid-Holocene, a period that was presumably characterized by arid climate. Thus, the apparent increase in moisture during the mid-Holocene is interpreted better as an increase in summer rainfall. This is most likely linked to the expansion of the West African summer monsoon fringe during the African Humid Period, which terminated in our record abruptly around 4 Kyr BP. The temporospatial difference with speleothem records from N Morocco suggests that the High-Atlas Mountains might have been a topographic barrier to further expansion of the West African summer monsoon fringe into higher latitudes. Plain Language Summary The Holocene African Humid Period in North Africa, characterized by the expansion of vegetation into the Green Sahara, has been linked to the intensification of the West African summer monsoon (WASM). However, the temporospatial pattern of the African Humid Period, especially the northernmost expansion of the WASM, remain a matter of controversy, largely owing to the lack of precisely dated and high-resolution paleoclimatic records. This study presents new highresolution paleoclimate data based on speleothem oxygen isotope records from a key site at 31 degrees N in NW Africa. Our data suggest that the WASM expanded to 31 degrees N in NW Africa during the mid-Holocene and terminated abruptly at 4 Kyr BP.	[Sha, Lijuan; Brahim, Yassine Ait; Cai, Yanjun; Li, Hanying; Du, Wenjing; Zhang, Haiwei; Cheng, Hai] Xi An Jiao Tong Univ, Inst Global Environm Change, Xian, Shaanxi, Peoples R China; [Wassenburg, Jasper A.] Max Planck Inst Chem, Climate Geochem Dept, Mainz, Germany; [Yin, Jianjun] Chinese Acad Geol Sci, Inst Karst Geol, Key Lab Karst Dynam, MNR & Guangxi, Guilin, Peoples R China; [Peros, Matthew] Bishops Univ, Dept Environm & Geog, Sherbrooke, PQ, Canada; [Cruz, Francisco W.] Univ Sao Paulo, Inst Geociencias, Sao Paulo, SP, Brazil; [Cai, Yanjun] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian, Shaanxi, Peoples R China; [Edwards, R. Lawrence; Cheng, Hai] Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA	Xi'an Jiaotong University; Max Planck Society; Chinese Academy of Geological Sciences; Bishops University; Universidade de Sao Paulo; Chinese Academy of Sciences; Institute of Earth Environment, CAS; University of Minnesota System; University of Minnesota Twin Cities	Cheng, H (autor correspondente), Xi An Jiao Tong Univ, Inst Global Environm Change, Xian, Shaanxi, Peoples R China.; Cheng, H (autor correspondente), Univ Minnesota, Dept Earth Sci, Minneapolis, MN 55455 USA.	cheng021@xjtu.edu.cn	Cai, Yanjun/A-9462-2010; Cruz, Francisco W/G-6059-2012; CHENG, HAI/H-3413-2017	Cai, Yanjun/0000-0001-7063-5050; CHENG, HAI/0000-0002-5305-9458; Zhang, Haiwei/0000-0002-0855-1283; Cruz, Francisco/0000-0002-4030-4581	NSFC [41888101, 41472140, 41731174, 41561144003]; U.S. NSF [1702816]; Postdoctoral Science Foundation of China [2018M640971]	NSFC(National Natural Science Foundation of China (NSFC)); U.S. NSF(National Science Foundation (NSF)); Postdoctoral Science Foundation of China(China Postdoctoral Science Foundation)	This work was supported by grants from NSFC (41888101, 41472140, 41731174, and 41561144003), U.S. NSF Grant 1702816, and the Postdoctoral Science Foundation of China (Grant 2018M640971) to Yassine Ait Brahim.	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Res. Lett.	DEC 16	2019	46	23					14093	14102		10.1029/2019GL084879	http://dx.doi.org/10.1029/2019GL084879		DEC 2019	10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	JZ8ZT		Bronze			2023-06-23	WOS:000502462500001
J	Soares, JL; Santos, HP; Brito, AD; Nogueira, AAE; Nogueira, ACR; Amorim, KB				Soares, Joelson L.; Santos, Hudson P.; Brito, Ailton da S.; Nogueira, Anna Andressa E.; Nogueira, Afonso C. R.; Amorim, Kamilla B.			The crustaceans burrow Sinusichnus sinuosus from the Oligocene-Miocene carbonate deposits of eastern Amazonia	ICHNOS-AN INTERNATIONAL JOURNAL FOR PLANT AND ANIMAL TRACES			English	Article						Sinusichnus; carbonate rocks; Oligocene-Miocene; Pirabas Formation; Amazonia	PIRABAS FORMATION; TRACE FOSSIL; DECAPOD CRUSTACEA; STATE; PLATFORM; SYSTEMS	Sinusichnus Gibert 1996 is recorded for the first time in the Oligocene-Miocene Pirabas Formation of Northern Brazil. In these Oligocene-Miocene carbonate deposits, Sinusichnus sinuosus is characterized by horizontal, highly regular sinusoidal burrow systems with T- and H-shaped branching points. The main difference between the S. sinuosus described herein and other occurrences worldwide is the anomalous diameter of the burrows (4 to 10 cm). These trace fossils occur in organic matter-rich, wackestone/packstone and laminated mudstones interbedded with boundstones deposited in an inner carbonate platform paleoenvironment. The exceptional size of the studied S. sinuosus could have been associated to the producer's size, which may be attributed to construction by large crustaceans, similar to fossils found within the Pirabas Formation. Also, the sinusoidal morphology and retrusive spreiten could be a result of the fodinichnial/domichnial behavior.	[Soares, Joelson L.; Santos, Hudson P.; Brito, Ailton da S.; Nogueira, Anna Andressa E.; Nogueira, Afonso C. R.; Amorim, Kamilla B.] Univ Fed Para, Programa Posgrad Geol & Geoquim, Inst Geociencias, Av Augusto Correa 1, BR-66075110 Belem, Para, Brazil	Universidade Federal do Para	Soares, JL (autor correspondente), Univ Fed Para, Programa Posgrad Geol & Geoquim, Inst Geociencias, Av Augusto Correa 1, BR-66075110 Belem, Para, Brazil.	jlsoares@ufpa.br		NOGUEIRA, AFONSO/0000-0002-5225-9255; Brito, Ailton/0000-0001-9224-5563; Soares, Joelson Lima/0000-0003-3683-523X; Borges Amorim, Kamilla/0000-0002-5031-402X	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico; Fundacao Amazonia de Amparo a Estudos e Pesquisas	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao Amazonia de Amparo a Estudos e Pesquisas(Fundacao Amazonia de Amparo a Estudos e Pesquisas (FAPESPA))	This work was supported by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico and Fundacao Amazonia de Amparo a Estudos e Pesquisas.	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J	Amaral-Santos, E; Jelinek, AR; Almeida-Abreu, PA; Genezine, FA				Amaral-Santos, E.; Jelinek, A. R.; Almeida-Abreu, P. A.; Genezine, F. A.			Phanerozoic cooling history of Archean/Paleoproterozoic basement in the southern Espinhaco Range, southeastern Brazil, through apatite fission-track analysis	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Espinhaco Range basement; Quadrilatero Ferrifero; Apatite fission-track thermochronology; Denudation history	SAO-FRANCISCO CRATON; FERRIFERO MINAS-GERAIS; LONG-TERM EVOLUTION; QUADRILATERO-FERRIFERO; DENUDATION HISTORY; CONTINENTAL-MARGIN; THERMOTECTONIC HISTORY; DETRITAL ZIRCON; BASIN; GEOCHRONOLOGY	Apatite fission track thermochronology of basement rocks from the southern Espinhaco Range and Quadrilatero Ferrifero in southeastern Brazil unravels the tectonic history of this portion of the Brazilian Shield. The study area encompasses an Archean and Paleoproterozoic granitoid-gneiss basement, in the southern border of the Sao Francisco Craton, and an Archean to Paleo-Mesoproterozoic sedimentary cover. Apatite fission track ages (AFT) vary from 187 +/- 18 to 91.8 +/- 7.3 Ma and horizontal confined track lengths vary from 9.62 +/- 1.81 mu m to 12.85 +/- 1.35 mu m. Thermal history modeling shows an accelerated cooling episode starting in the Upper Devonian to Early Permian. After this event, quiescence lasted from 115 to 170 Ma. Apatite samples lack evidence of far-field effects from rifting and opening of the South Atlantic Ocean, and also evidence from alkaline and basaltic magmatism emplacement during Mesozoic-Cenozoic. The AFT thermochronometer remained undisturbed during Transminas mafic dyke swarm intrusion. Finally, the last cooling event in the Espinhaco Range-Quadrilatero Ferrifero basement records ascension to surface temperatures due to epeirogeny after new configurations of the Nazca, South American and African plates. A climatic origin for the ascension is supported by accentuated erosion rates, even though a weathering-prone phase is registered in weathering profiles.	[Amaral-Santos, E.; Jelinek, A. R.] Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil; [Almeida-Abreu, P. A.] Univ Fed Vales Jequitinhonha & Mucuri, Ctr Estudos Geociencias ICT, Diamantina, MG, Brazil; [Genezine, F. A.] Inst Pesquisas Energet & Nucl, Ctr Reator Pesquisa, Sao Paulo, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal dos Vales do Jequitinhonha e Mucuri (UFVJM); Comissao Nacional de Energia Nuclear (CNEN); Instituto de Pesquisas Energeticas e Nucleares (IPEN)	Amaral-Santos, E (autor correspondente), Univ Fed Rio Grande do Sul, Inst Geociencias, Av Bento Goncalves 9500, BR-91501970 Porto Alegre, RS, Brazil.	edgar.amaral@ufrgs.br	Almeida-Abreu, Pedro Angelo/AAL-6281-2021; Jelinek, Andrea/ABH-9386-2020	Jelinek, Andrea/0000-0002-7375-5039; do Amaral Santos, Edgar/0000-0003-2751-4987	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -CAPES, Brazil; Conselho Nacional de Desenvolvimento Cientifico e Tecnolegico -CNPq [303184/2017-5]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -CAPES, Brazil(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnolegico -CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The first author thanks Leo Afraneo Hartmann for valuable considerations throughout the writing of this manuscript and Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -CAPES, Brazil, for financial support. 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South Am. Earth Sci.	DEC	2019	96								102352	10.1016/j.jsames.2019.102352	http://dx.doi.org/10.1016/j.jsames.2019.102352			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KB8BX					2023-06-23	WOS:000506715400021
J	Araujo, R; Nogueira, A				Araujo, Raphael; Nogueira, Afonso			Serra Sul diamictite of the Carajas Basin (Brazil): A Paleoproterozoic glaciation on the Amazonian craton	GEOLOGY			English	Article							U-PB GEOCHRONOLOGY; GRAO-PARA GROUP; QUARTZ GRAINS; INTERNAL ARCHITECTURE; SNOWBALL EARTH; ICE; MICROTEXTURES; GEOCHEMISTRY; REACTIVATION; MAGMATISM	This paper reports the discovery of glacial deposits of likely Siderian-Rhyacian age (2.58-2.06 Ga) in South America (Carajas Basin, Brazil), thereby expanding the potential reach of Paleoproterozoic glaciations to the Amazonian craton for the first time. Glacially derived diamictites are stacked within a hitherto unrecognized similar to 600-m-thick siliciclastic succession, here named the Serra Sul Formation. Well-preserved textures, with evidence of glaciotectonism and ice rafting, indicate deposition in a coastal subglacial to glacial-fed submarine fan system, in which the immediately underlying units (banded iron formation and volcanic rock) were the main source and bedrock. The Serra Sul diamictite may be correlated with any of the known Paleoproterozoic glaciations, or with none of them.	[Araujo, Raphael] Geol Survey Brazil, Management Geol & Mineral Resources, Av Perimetral 3645, BR-66095904 Belem, Para, Brazil; [Araujo, Raphael; Nogueira, Afonso] Fed Univ Para, Inst Geosci, R Augusto Correa 01, BR-66075110 Belem, Para, Brazil	Universidade Federal do Para	Araujo, R (autor correspondente), Geol Survey Brazil, Management Geol & Mineral Resources, Av Perimetral 3645, BR-66095904 Belem, Para, Brazil.; Araujo, R (autor correspondente), Fed Univ Para, Inst Geosci, R Augusto Correa 01, BR-66075110 Belem, Para, Brazil.	raphaelneto@ufpa.br		NOGUEIRA, AFONSO/0000-0002-5225-9255	Geological Survey of Brazil (Belem, Brazil); PROPESP/UFPA	Geological Survey of Brazil (Belem, Brazil); PROPESP/UFPA	We thank Sergio Huhn, Fernando Matos, and Luiz Costa of Vale S.A. (Parauapebas, Brazil) for making the drill cores available for the research; the Geological Survey of Brazil (Belem, Brazil) and the PROPESP/UFPA for supporting this work; Werner Truckenbrodt for his constructive comments on an earlier version of the manuscript; and Roberto Araujo Filho and Alexandre Ribeiro for fieldwork assistance. We are also very grateful to Daniel Le Heron, Paul Hoffman, Kari Strand, and an anonymous reviewer for reviewing our manuscript; and to James Schmitt for his editorial work.	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J	Barros, LD; Gorayeb, PSD				Barros, Luisa Dias; de Sousa Gorayeb, Paulo Sergio			Serra do Tapa Ophiolite Suite - Araguaia Belt: Geological characterization and Neoproterozoic evolution (central-northern Brazil)	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Serra do Tapa; Ophiolite; Neoproterozoic; Araguaia Belt	GONDWANA; RODINIA; BASALTS	The Araguaia Belt is a Neoproterozoic collisional orogen located in the northern Tocantins tectonic province, North-central Brazil, being one of the most expressive orogens of West Gondwana. The Serra do Tapa Ophiolite Suite is the most important representative of the ophiolitic bodies of the Araguaia Belt, exposed along the low-grade metamorphic domain of the Belt and extending over 80 km in the N-S direction. It constitutes a set of N-S aligned bodies that represent a disrupted ophiolite special sequence comprising serpentinized peridotites and dunites, massive and pillow basaltic lavas, volcanosedimentary rocks, cherts, jaspilites, and their metamorphic products. The serpentinized rocks have protoliths of mantelic harzburgites and dunites, with relict original protogranular texture partially replaced by pseudomorphic texture after olivine and orthopyroxene, and nonpseudomorphic (replacements). Submarine basaltic flows represent the volcanic succession, overlying serpentinized peridotites. The volcanic succession occurs as homogeneous massive basalts or pillow basalts, and locally volcanoclastic breccias (hyaloclastite). The pillow structure shows zoning, where the core consists of homogeneous massive metabasalt with preserved igneous features whereas pillow outer zone consists of hyalobasalt with quenching textures whose pillow surface is transformed into chlorite-rich rocks that appear fine-grained and related to the metasomatic transformations due to interactions with seawater. Geochemically, the massive metabasalts display a subalkaline-tholeiitic affinity, compatible with Middle Oceanic Ridge Basalts types (MORB). The suite evolution is a testimony of an oceanic stage during the Neoproterozoic of the Araguaia Basin that generated an oceanic lithosphere followed by volcanic activity, the interaction between lava flows and pelitic sediments, and deposition of chemical sedimentary rocks (jaspilites and cherts). Subsequently, the detachment of the oceanic lithosphere and the compressional tectonic evolution of the Araguaia Orogen inverted the sequence leading to the obduction of ophiolite bodies along overthrust and transcurrent faults projecting/thrusting a mass toward the Amazonian Craton. The tectonics was accompanied by regional metamorphism from anchymetamorphism to low greenschist facies conditions. All these processes are related to the evolution of the Brasiliano/Pan-African Cycle of the Araguaia Belt. The Serra do Tapa Ophiolite constitutes a mega-slice of an oceanic crust and marks a phase of lithosphere construction and the early opening of the Araguaia Basin related to the crustal evolution of the Araguaia Belt in the Neoproterozoic (transition Tonian-Ediacaran).	[Barros, Luisa Dias; de Sousa Gorayeb, Paulo Sergio] Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, PPGG IG UFPA, Av Augusto Correa 1, BR-66075110 Belem, Para, Brazil	Universidade Federal do Para	Gorayeb, PSD (autor correspondente), Univ Fed Para, Inst Geociencias, Programa Posgrad Geol & Geoquim, PPGG IG UFPA, Av Augusto Correa 1, BR-66075110 Belem, Para, Brazil.	luisadbars@gmail.com; gorayebp@ufpa.br			Graduate Program in Geology and Geochemistry, Geosciences Institute of the Federal University of Para; "Geosciences Institute of Amazonian" -INCT (GEOCIAM -CNPq/MCT/FAPESPA) [573733/2008-2]; Petrology, geochronology and tectonics of the magmatic rocks of the Araguaia Belt, Neoproterozoic" (CNPq-Universal Project) [427225/2016-7, 130012/2014-9]	Graduate Program in Geology and Geochemistry, Geosciences Institute of the Federal University of Para; "Geosciences Institute of Amazonian" -INCT (GEOCIAM -CNPq/MCT/FAPESPA); Petrology, geochronology and tectonics of the magmatic rocks of the Araguaia Belt, Neoproterozoic" (CNPq-Universal Project)	This study was developed by the research group "Petrology and Crustal Evolution" (CNPq-UFPA), and the Graduate Program in Geology and Geochemistry, Geosciences Institute of the Federal University of Para (PPGG/IG/UFPA). The research was supported by the projects "Geosciences Institute of Amazonian" -INCT (GEOCIAM -CNPq/MCT/FAPESPA, Proc. No. 573733/2008-2), "Petrology, geochronology and tectonics of the magmatic rocks of the Araguaia Belt, Neoproterozoic" (CNPq-Universal Project, Proc. No. 427225/2016-7), and for Master's degree scholarship (CNPq, Proc. No. 130012/2014-9). We are grateful to Iara Maria dos Santos for her support in surveying and interpreting structural data; to Fabio Henrique Garcia Domingos for the review of the manuscript in its initial phase, and to Microanalyses and X-RD Labs of PPGG/UFPA.	Abreu F.A.M., 1994, AN 4 S GEOL AM, P1; Abreu FAM, 1978, AN 30 C BRAS GEOL RE, P539; Almeida F., 1976, B I GEOCIENCIAS USP, V7, P45, DOI DOI 10.11606/ISSN.2316-8978.V7I0P45-80; Almeida F.F.M., 1986, AN 34 C BRAS GEOL GO, V3, P1269; Almeida F.F.M., 1974, C GEOL 28 AN PORT AL, V4, P11; Alvarenga C. J. 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DEC	2019	96								102323	10.1016/j.jsames.2019.102323	http://dx.doi.org/10.1016/j.jsames.2019.102323			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KB8BX					2023-06-23	WOS:000506715400011
J	Campos, MC; Chiessi, CM; Prange, M; Mulitza, S; Kuhnert, H; Paul, A; Venancio, IM; Albuquerque, ALS; Cruz, FW; Bahr, A				Campos, Marilia C.; Chiessi, Cristiano M.; Prange, Matthias; Mulitza, Stefan; Kuhnert, Henning; Paul, Andre; Venancio, Igor M.; Albuquerque, Ana Luiza S.; Cruz, Francisco W.; Bahr, Andre			A new mechanism for millennial scale positive precipitation anomalies over tropical South America	QUATERNARY SCIENCE REVIEWS			English	Article						Quaternary; Paleoclimatology; South America; Inorganic geochemistry; Heinrich Stadials; Precipitation; X-ray fluorescence	ATLANTIC CONVERGENCE ZONE; SEA-SURFACE TEMPERATURE; EL-NINO; CLIMATE; BRAZIL; VARIABILITY; CIRCULATION; VEGETATION; NORTHEAST; DYNAMICS	Continental and marine paleoclimate archives from northwestern and northeastern South America recorded positive precipitation anomalies during Heinrich Stadials (HS). These anomalies have been classically attributed to enhanced austral summer (monsoon) precipitation. However, the lack of marine paleoclimate records off eastern South America as well as inconsistencies between southeastern South American continental and marine records hamper a comprehensive understanding of the mechanism responsible for (sub-) tropical South American hydroclimate response to HS. Here we investigate piston core M125-95-3 collected off eastern South America (10.94 degrees S) and simulate South American HS conditions with a high-resolution version of an atmosphere-ocean general circulation model. Further, meridional changes in precipitation over (sub-) tropical South America were assessed with a thorough compilation of previously available marine paleorecords. Our ln(Ti/Ca) and ln(Fe/K) data show increases during HS6-Younger Dryas. It is the first core off eastern South America and the southernmost from the Atlantic continental margin of South America that unequivocally records HS-related positive precipitation anomalies. Based on our new data, model results and the compilation of available marine records, we propose a new mechanism for the positive precipitation anomalies over tropical South America during HS. The new mechanism involves austral summer precipitation increases only over eastern South America while the rest of tropical South America experienced precipitation increases during the winter, challenging the widely held assumption of a strengthened monsoon. South American precipitation changes were triggered by dynamic and thermodynamic processes including a stronger moisture supply from the equatorial North Atlantic (tropical South Atlantic) in austral winter (summer). (C) 2019 Elsevier Ltd. All rights reserved.	[Campos, Marilia C.; Chiessi, Cristiano M.] Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, SP, Brazil; [Prange, Matthias; Mulitza, Stefan; Kuhnert, Henning; Paul, Andre] Univ Bremen, MARUM Ctr Marine Environm Sci, Bremen, Germany; [Venancio, Igor M.] Natl Inst Space Res INPE, Ctr Weather Forecasting & Climate Studies CPTEC, Cachoeira Paulista, Brazil; [Albuquerque, Ana Luiza S.] Fluminense Fed Univ, Grad Program Geochem, Niteroi, RJ, Brazil; [Cruz, Francisco W.] Univ Sao Paulo, Inst Geoci, Sao Paulo, SP, Brazil; [Bahr, Andre] Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany	Universidade de Sao Paulo; University of Bremen; Instituto Nacional de Pesquisas Espaciais (INPE); Universidade Federal Fluminense; Universidade de Sao Paulo; Ruprecht Karls University Heidelberg	Campos, MC (autor correspondente), Univ Sao Paulo, Sch Arts Sci & Humanities, Sao Paulo, SP, Brazil.	marilia.carvalho.campos@usp.br	Chiessi, Cristiano Mazur/E-1916-2012; Albuquerque, Ana Luiza S/C-5167-2013; Venancio, Igor M/I-5893-2014; Cruz, Francisco W/G-6059-2012; Campos, Marília/AFL-1717-2022; Campos, Marília/AAC-8457-2019	Chiessi, Cristiano Mazur/0000-0003-3318-8022; Albuquerque, Ana Luiza S/0000-0003-1267-6190; Venancio, Igor M/0000-0003-3118-4247; Campos, Marília/0000-0003-0059-9853; Campos, Marília/0000-0003-0059-9853; Cruz, Francisco/0000-0002-4030-4581; Kuhnert, Henning/0000-0001-5242-4495	FAPESP [2016/10242-0, 2018/06790-7, 2018/15123-4]; CAPES [88887.156152/2017-00, 88881.161151/2017-01, 564/2015, 88881.313535/2019-01]; CNPq [406322/2018-0, 302607/2016-1, 422255/2016-5, 302521/2017-8, 429767/2018-8]; Alexander von Humboldt Foundation; DFG Research Center, Cluster of Excellence "The Ocean in the Earth System"; German PalMod initiative (BMBF)	FAPESP(Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (FAPESP)); CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Alexander von Humboldt Foundation(Alexander von Humboldt Foundation); DFG Research Center, Cluster of Excellence "The Ocean in the Earth System"(German Research Foundation (DFG)); German PalMod initiative (BMBF)(Federal Ministry of Education & Research (BMBF))	We thank two anonymous reviewers for their comments and suggestions that improved the manuscript. Logistic and technical assistance was provided by the captain and crew of the R/V Meteor. New data shown herein are archived in Pangaea (doi:10.1594/PANGAEA.905181). M.C. Campos acknowledges the financial support from FAPESP (grants 2016/10242-0 and 2018/06790-7). C.M. Chiessi and A.L. Albuquerque acknowledges the financial support from FAPESP (grant 2018/15123-4), CAPES (grants 564/2015 and 88881.313535/2019-01), CNPq (grants 302607/2016-1, 422255/2016-5, 302521/2017-8 and 429767/2018-8) and the Alexander von Humboldt Foundation. CAPES (grants 88887.156152/2017-00 and 88881.161151/2017-01) and CNPq (grant 406322/2018-0) currently support I.M. Venancio. S. Mulitza, M. Prange, H. Kuhnert and A. Paul were funded through the DFG Research Center, Cluster of Excellence "The Ocean in the Earth System". Support from the German PalMod initiative (BMBF) is also acknowledged. The CCSM3 simulations were performed on the supercomputer of the Norddeutscher Verbund far Hoch-und Hochstleistungsrechnen (HLRN). Sample material was provided by the Core Repository at the Fluminense Federal University, Brazil. This research used data acquired at the XRF Core Scanner Lab at the MARUM -Center for Marine Environmental Sciences, University of Bremen, Germany.	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Sci. Rev.	DEC 1	2019	225								105990	10.1016/j.quascirev.2019.105990	http://dx.doi.org/10.1016/j.quascirev.2019.105990			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	JQ2AS					2023-06-23	WOS:000498754500003
J	Cardoso, AR; Nogueira, ACR; Rabelo, CEN; Soares, JL; Goes, AM				Cardoso, Alexandre Ribeiro; Rodrigues Nogueira, Afonso Cesar; Neri Rabelo, Cleber Eduardo; Soares, Joelson Lima; Goes, Ana Maria			Multi-approach provenance in stratigraphy: Implications for the Upper Mesozoic evolution of the Parnaiba Basin, NE Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Provenance; Stratigraphic positioning; Heavy minerals; Cathodoluminescence; Parnaiba Basin	HEAVY MINERAL ASSEMBLAGES; CRUSTAL STRUCTURE; QUARTZ; CATHODOLUMINESCENCE; SYSTEM; PETROGRAPHY; SANDSTONES; INDICATORS; PROVINCE; SPECTRA	Provenance analyses are highly affected by transport, depositional and diagenetic processes, as well as the grain size chosen for evaluation. In order to avoid misleading data, provenance research requires multi-approach techniques. In this work, a set of widespread methods were applied to investigate a debatable stratigraphic interval in the Parnaiba Basin, northeastern Brazil. Discontinuous exposures and fault displacements result in enigmatic stratigraphic relations in the Mesozoic portion of this basin. This succession consists of the lacustrine sandstones and shales of the Pastos Bons Formation and aeolian sandstones of the Corda Formation, composing the Mearim Group, and fluvial conglomerates and sandstones of the Grajad Formation. The provenance was studied through sandstone petrography, quartz petrography, hot cathodoluminescence and heavy minerals analyses. Sandstones from Mearim Group plotted in recycled orogenic and craton interior fields, whereas quartz petrography and cathodoluminescence constrained predominantly volcanic sources. The heavy minerals assemblages of the lacustrine and aeolian deposits are very similar, whereas the fluvial succession presents texturally immature grains and anomalous high hornblende content. Additionally, ZTR, GZi and RZi indexes are higher for lacustrine and aeolian deposits, and lower for fluvial beds. These data indicate polycyclic minerals and mixed sources for Mesozoic sandstones of the Parnaiba Basin. The Mearim Group presents both volcanic contribution, probably supplied by basalts from the Central Atlantic Magmatic Province (CAMP), and low to medium-grade metapelitic heavy minerals assemblage. Heavy minerals were probably supplied by Neoproterozoic metapelites from the Ceara Central Domain (Ceara Group?), Borborema Province. Conversely, heavy minerals of the Grajad Formation were derived from I-type Brazilian granites, incompatible with the Mearim Group. These data provided new stratigraphic relations for the Mesozoic deposits of the Parnaiba Basin and implications for the evolution of this basin.	[Cardoso, Alexandre Ribeiro; Rodrigues Nogueira, Afonso Cesar; Neri Rabelo, Cleber Eduardo; Soares, Joelson Lima] Fed Univ Para Ufpa, Inst Geociences, Ppgg, BR-66075110 Belem, Para, Brazil; [Cardoso, Alexandre Ribeiro] State Univ Campinas Unicamp, Inst Geosci, Dept Geol & Nat Resources, BR-13083870 Campinas, SP, Brazil; [Goes, Ana Maria] State Univ Sao Paulo, Inst Geosci, BR-05508080 Sao Paulo, Brazil	Universidade Federal do Para; Universidade Estadual de Campinas; Universidade Estadual Paulista	Cardoso, AR (autor correspondente), Fed Univ Para Ufpa, Inst Geociences, Ppgg, BR-66075110 Belem, Para, Brazil.	a229678@dac.unicamp.br	Góes, Ana Maria/M-4518-2017; Cardoso, Alexandre/AAK-3108-2020	Cardoso, Alexandre/0000-0001-7562-6567; NOGUEIRA, AFONSO/0000-0002-5225-9255	National Council for Scientific and Technological Research (CNPq) [CNPq -130823/2017-1]	National Council for Scientific and Technological Research (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET))	We are very grateful to National Council for Scientific and Technological Research (CNPq) for funding this research with a master scholarship (CNPq -130823/2017-1) conceded to the first author and to the Programa de Pos-Graduacao em Geologia e Geoquimica (PPGG) of the Federal University of Para (UFPa). We also thank Raiza Renne and Hudson Santos for hot cathodoluminescence analysis, as well as Everaldo Cunha and Joelma Lobo, who facilitated the heavy minerals separation. Francisco Abrantes Jr., Werner Truckenbrodt and Raphael AraOjo are thanked for helpful suggestions. We also acknowledge the editor Andres Folguera, as well as the careful corrections of M. Sol Raigemborn and an anonymous reviewer that greatly improved an earlier version of this manuscript.	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D., 2001, INTRO IGNEOUS METAMO; ZAlan P., 1991, BOGOTA, V1, P17; Zimmermann S, 2016, GONDWANA RES, V37, P1, DOI 10.1016/j.gr.2016.06.001	68	0	0	2	4	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0895-9811	1873-0647		J S AM EARTH SCI	J. South Am. Earth Sci.	DEC	2019	96								102386	10.1016/j.jsames.2019.102386	http://dx.doi.org/10.1016/j.jsames.2019.102386			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KB8BX					2023-06-23	WOS:000506715400047
J	Cecilio, RO; Dillenburg, SR				Cecilio, R. O.; Dillenburg, S. R.			An ocean wind-wave climatology for the Southern Brazilian Shelf. Part II: Variability in space and time	DYNAMICS OF ATMOSPHERES AND OCEANS			English	Article						Wave modelling; Shoreface; Wave base; Wave gradients; Wave refraction; WW3; SWAN	ENERGY RESOURCE ASSESSMENT; TELECONNECTION PATTERNS; GENERALIZED FROSTS; COASTAL REGIONS; CHINA SEA; PROPAGATION; REANALYSIS; HINDCAST; MODEL; ANDES	Previously validated model results were used to characterize the wave climate over the Southern Brazilian Shelf (SBS). The low mean significant wave height over the western South Atlantic shelves was shown together with examples of cyclone-induced extreme wave fields and other typical wave conditions. The mean offshore spectra showed a bimodal shape with a predominance of S/SSW and ENE/E waves with distinctive interannual rising periods in wave energy density. Along-shelf wave energy gradients were seen near the coast with higher energy located off capes and coastal projections and energy minima between them. A considerable drop in wave energy suggests the 40 m depth as the mean wave base and consequently the lower limit of the SBS shoreface. The upper shoreface mean wave energy density varied abruptly along the shelf in response to differences in bottom declivities. The large and shallow shoreface was responsible for an intense refraction of the waves and hence very small angles of attack. Additionally, it was shown the sheltering effect caused by capes and coastal projections and a remarkable north/south energy asymmetry between them, caused by a windowing on the wave propagation to the shore. Altogether, it was possible to state that bottom friction plays a major role in wave differentiation along the SBS shoreface, thus suggesting that shelf morphology might indeed be more important to generate wave variability than the offshore wave variation itself.	[Cecilio, R. O.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Porto Alegre, RS, Brazil; [Dillenburg, S. R.] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul	Cecilio, RO (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Porto Alegre, RS, Brazil.	rececilio@gmail.com	Dillenburg, Sergio/C-4027-2013	Dillenburg, Sergio/0000-0003-0072-7018	Brazilian Research Council (CNPq - Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)	Brazilian Research Council (CNPq - Conselho Nacional de Desenvolvimento Cientifico e Tecnologico)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors acknowledge the Brazilian Research Council (CNPq - Conselho Nacional de Desenvolvimento Cientifico e Tecnoldgico) for the first author's Doctoral Studentship and for the Research Fellowship granted to Dr. Sergio Dillenburg.	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Atmos. Oceans	DEC	2019	88								101103	10.1016/j.dynatmoce.2019.101103	http://dx.doi.org/10.1016/j.dynatmoce.2019.101103			14	Geochemistry & Geophysics; Meteorology & Atmospheric Sciences; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics; Meteorology & Atmospheric Sciences; Oceanography	JS0WQ					2023-06-23	WOS:000500035600004
J	Cetina, LM; Tassinari, CC; Rodriguez, G; Correa-Restrepo, T				Cetina, L. M.; Tassinari, C. C.; Rodriguez, Gabriel; Correa-Restrepo, T.			Origin of pre-mesozoic xenocrystic zircons in cretaceous sub-volcanic rocks of the northern Andes (Colombia): paleogeographic implications for the region	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Crustal recycling; Zircon xenocrysts; CLIP; Western Cordillera of Colombia; Intra-oceanic subduction zones	CENTRAL CORDILLERA; CONTINENTAL-CRUST; SUBDUCTION INITIATION; TECTONIC EVOLUTION; WESTERN CORDILLERA; OCEANIC PLATEAU; ARC-BASIN; SANTA-FE; GEOCHRONOLOGY; GEOCHEMISTRY	This paper reports the presence of xenocrystic zircons in sub-volcanic rocks (Guarco Andesite and Porphyritic Intrusives units) exposed in the northeast of the Western Cordillera of Colombia (WCC) and provides a new contribution to the understanding of the tectono-magmatic evolution of the area during the Upper Cretaceous associated with the geological history of the Caribbean Large Igneous Province (CLIP). The study area is located in an accretionary terrane constituted by a basement of oceanic affinity (Barroso Formation and San Jose de Urama Diabases unit), amalgamated against the northwestern South American margin and associated with the development of CLIP. The elemental and isotopic geochemical data (with an initial ratio of Sr-87/Sr-86 between 0.70334 and 0.70543 and epsilon(Nd) between + 6.25 and + 7.42) indicate an island arc environment for the formation of sub-volcanic rocks and a mantle wedge source area (and/or the arc itself), which presents subordinate levels of crustal material. U-Pb zircon ages by SHRIMP He and LA-ICP-MS show ages from the Mesoarchean to the Upper Cretaceous, with representative peaks of approximately 2700, 2100, 600 and 90 Ma. The younger age population is interpreted as the crystallization age of the studied rocks and indicates a spatial and temporal relationship with the basement rocks associated with the CLIP. The older zircons are interpreted as xenocrysts coming from terrigenous sediments that were dragged down into the subduction channel (reflecting crustal recycling processes through the mantle in subduction zones). Alternatively, the xenocrystic zircons could have come from the assimilation of crustal sediments that were previously deposited over the primitive arc. We suggest that the source areas of zircon xenocrysts probably are located close to the Arequipa Massif and the Maranon Complex inliers, and close to the ensialic Basement of the Central Cordillera of Colombia (CCCB). Using these source areas and paleogeographic/paleomagnetic models published by other authors, we propose two possible paleogeographic scenarios differentiated by the polarity of the subduction zone.	[Cetina, L. M.; Tassinari, C. C.] Univ Sao Paulo, Geosci Inst, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil; [Rodriguez, Gabriel; Correa-Restrepo, T.] Colombian Geol Survey, Calle 75 79A-51, Medellin, Colombia	Universidade de Sao Paulo	Cetina, LM (autor correspondente), Univ Sao Paulo, Geosci Inst, Rua Lago 562, BR-05508080 Sao Paulo, SP, Brazil.	linacetina0526@usp.br; ccgtassi@usp.br; grodriguez@sgc.gov.co; tcorrea@sgc.gov.co	; Rodriguez, Gabriel/V-2526-2018	Cetina, Lina/0000-0001-6814-480X; Rodriguez, Gabriel/0000-0003-1422-3523	CAPES; CNPq [302962/2010-7]	CAPES(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); CNPq(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	The authors -thank the CAPES program for the master's scholarship given to the first author, the CNPq development agency for the financial support to conduct various analyses through project 302962/2010-7, and the Colombian Geological Service (Medellin Office) for the support in the field and providing various samples and analyses. The authors would like to thank Ryan P. Bresnahan for his help during the final edition of this paper and to the reviewers of the manuscript (Antonio Garcia-Casco and Yamirka Rojas-Agramonte) for their comments and corrections that have allowed us to greatly improve the document.. We also thank the technicians of the CPGeo laboratories, SHRIMP IIe/Mc and the chemical laboratory of SGC, especially Key Sato, Vasco Loiso, John Mauro Castario, Artur Takashi and Liliane Petronilho.	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J	Santos, LCMD; Dantas, EL; Cawood, PA; Lages, GD; Lima, HM; dos Santos, EJ; Caxito, FA				de Lira Santos, Lauro Cezar M.; Dantas, Elton L.; Cawood, Peter A.; Lages, Geysson de A.; Lima, Haroldo M.; dos Santos, Edilton J.; Caxito, Fabricio A.			Early to late Neoproterozoic subduction-accretion episodes in the Cariris Velhos Belt of the Borborema Province, Brazil: Insights from isotope and whole-rock geochemical data of supracrustal and granitic rocks	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Early Neoproterozoic post-orogenic setting; Ediacaran granitic magmatism; Cariris Velhos and Brasiliano orogens; Borborema Province; West Gondwana	ZIRCON U-PB; PLASMA-MASS SPECTROMETRY; EAST-AFRICAN OROGEN; SM-ND ISOTOPE; NE BRAZIL; WEST GONDWANA; PLUTONIC ROCKS; TRANSVERSAL ZONE; TRACE-ELEMENTS; CRUSTAL GROWTH	The Cariris Velhos Belt is an unique domain of the Borborema Province, Brazil, because it presents magmatic and metamorphic lithotectonic associations spanning all the Neoproterozoic. In this study, we investigate the main sources of its major supracrustal sequence (i.e. Sao Caetano Complex) as well as genetic aspects of a later intrusive granitic body, the Sao Pedro Stock. Detrital U-Pb zircon determinations for the supracrustal rocks are characterized by a major peak in the range of 1.0-0.9 Ga, with maximum deposition age at around 0.86 Ga. Minor components are aged at 1.8-1.6 Ga and 2.5 Ga. The Nd isotopic composition for this unit suggest crustal reworking of Meso-to Paleoproterozoic sources as well as inheritance of juvenile mantle material. Whole-rock geochemical data points out to derivation from magmatic arc-related andesites and rhyolites as well as foreland material, and we interpret this sequence as remnant of the Cariris Velhos (1.0-0.9 Ga) post-orogenic basin. The Sao Pedro Stock corresponds to a mostly isotropic intrusion of dominantly granitic composition. U-Pb zircon data from a monzogranitic and a tonalitic samples suggest crystallization ages of ca. 615 +/- 02 Ma and 596 +/- 22 Ma, respectively. Zircon crystals with ages of ca. 981 +/- 29 Ma are interpreted as inherited crystals. Sm-Nd isotopic behavior is similar from samples of the Sao Caetano Complex, whereas overall geochemistry suggests crystallization from high-K talc-alkaline and peraluminous magmas, in addition to trace-element distribution compatible with Cordilleran granites. It is proposed that the Sao Pedro stock were formed in a modern-style subduction zone in later stages of the Brasiliano-Pan African orogeny (0.6-0.5 Ga). Accordingly, we conclude that systematic subduction-accretion episodes took place in this part of West Gondwana from early to late Neoproterozoic times.	[de Lira Santos, Lauro Cezar M.; Dantas, Elton L.] Univ Fed Pemambuco, Dept Geol, Recife, PE, Brazil; [de Lira Santos, Lauro Cezar M.] Univ Brasilia, Inst Geociencias, Brasilia, DF, Brazil; [Cawood, Peter A.] Monash Univ, Sch Earth Atmosphere & Environm, Clayton, Vic, Australia; [Lages, Geysson de A.; dos Santos, Edilton J.] Serv Geol Brasil CPRM, Brasilia, DF, Brazil; [Lima, Haroldo M.] Univ Fed Ceara, Dept Geol, Fortaleza, Ceara, Brazil; [Caxito, Fabricio A.] Univ Fed Minas Gerais, Inst Geociencias, CPMTC, Belo Horizonte, MG, Brazil	Universidade de Brasilia; Monash University; Universidade Federal do Ceara; Universidade Federal de Minas Gerais	Santos, LCMD (autor correspondente), Univ Fed Pemambuco, Dept Geol, Recife, PE, Brazil.	lauromontefalco@gmail.com	de Almeida Lages, Geysson A/C-9314-2014; Dantas, Elton Luiz/AAK-8464-2021; de Lira Santos, Lauro Cézar Montefalco/E-5536-2015; Monteiro Lima, Haroldo/GPG-1946-2022; Caxito, Fabricio A/J-1317-2016	de Almeida Lages, Geysson A/0000-0001-7041-4944; Dantas, Elton Luiz/0000-0002-7954-5059; de Lira Santos, Lauro Cézar Montefalco/0000-0001-6098-1873; Caxito, Fabricio A/0000-0002-0335-3667; Monteiro Lima, Haroldo/0000-0002-9744-7997; Cawood, Peter/0000-0003-1200-3826	Brazilian scientific council (CNPq) [308312/2014-7, 454272/2014-6]; Australian Research Council [FL160100168]; INCT (Estudos tectonicos)	Brazilian scientific council (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Australian Research Council(Australian Research Council); INCT (Estudos tectonicos)	This work is part of the PhD thesis of Lauro Cezar M. de Lira Santos at UnB. The anonymous reviews comments are strongly appreciated. Elton L. Dantas and Fabricio A. Caxito are fellows of the Brazilian scientific council (CNPq, grants 308312/2014-7 and 454272/2014-6, respectively) and acknowledge for the received support. PAC acknowledges support from Australian Research Council grant FL160100168. We also thank INCT (Estudos tectonicos) for supporting this research project.	Affaton P., 1991, W AFRICAN OROGENS CI, P95; Alcantara D. C. B. 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South Am. Earth Sci.	DEC	2019	96								102384	10.1016/j.jsames.2019.102384	http://dx.doi.org/10.1016/j.jsames.2019.102384			22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KB8BX		Green Published			2023-06-23	WOS:000506715400044
J	de Mesquita, NM; Carrino, TA; Neto, JAD				de Mesquita, Nayara Moreira; Carrino, Thais Andressa; de Souza Neto, Joao Adauto			The use of reflectance spectroscopy and the prehnite spectral index to target gold mineralization at the Bonfim polymetallic skarn deposit, Serido Mobile Belt, Borborema Province, Brazil	ORE GEOLOGY REVIEWS			English	Article						Serido Mobile Belt; Bonfim Au-W-Mo skarn; Hydrothermal alteration; Brazil; VNIR-SWIR	GA SAO-JOSE; NE BRAZIL; NORTHEASTERN BRAZIL; CAMPESTRE MASSIF; LUDWIG SKARN; EXPLORATION; NEVADA; YERINGTON; CALCITE	The Serido Mobile Belt hosts numerous mineralized skarns in the Borborema Province, northeastern Brazil. The Bonfun W-Mo-Au-Bi-Te skarn occurs within a Neoproterozoic metasedimentary sequence (Serido Group), within marble and schist lenses, or at the contacts between both. An ASD-FieldSpc (TM) 3 High-Resolution spectrometer was used to characterize the mineralogy of a representative drill core interval (181 m) from the Bonfim deposit, in order to generate the spectral characterization to define the gold mineralization. Skarns are characterized by the presence of diopside, actinolite-tremolite, clinozoisite-zoisite, muscovite and prehnite. Prehnite and epidote constitute the main components of the talc-silicate assemblage associated with late-stage gold mineralization. The diagnostic absorption feature of prehnite at 1478 nm (OH) can be used to identify its presence, and the prehnite index proposed in this case study (a reflectance ratio of 1465 nm/1478 nm) allows highlighting the prehnite enriched sections along the core. Geochemical data show a positive correlation between gold and the presence of a prehnite absorption at 1478 nm. The results suggest that the prehnite spectral signature can be used as a reliable and efficient (rapid) indicator for gold skams, perhaps under geologically similar circumstances to those at Bonfim.	[de Mesquita, Nayara Moreira; Carrino, Thais Andressa; de Souza Neto, Joao Adauto] Univ Fed Pernambuco, Dept Geol, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil	Universidade Federal de Pernambuco	de Mesquita, NM (autor correspondente), Univ Fed Pernambuco, Dept Geol, Av Arquitetura S-N, BR-50740550 Recife, PE, Brazil.	nayara.mesquita@ufpe.br	Carrino, Thais Andressa/AAH-1292-2020; Neto, João Adauto Souza/AAG-6672-2021; Souza Neto, João Adauto/D-6810-2016	Carrino, Thais Andressa/0000-0001-8528-5225; Neto, João Adauto Souza/0000-0002-9870-7113; Souza Neto, João Adauto/0000-0002-9870-7113	National Council for Scientific and Technological Development (CNPq) [312.275/2017-0]; Nosso Senhor do Bonfim Mining Company	National Council for Scientific and Technological Development (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Nosso Senhor do Bonfim Mining Company	The authors would like to thank Nosso Senhor do Bonfim Mining Company, especially geologist Fernanda Muniz and mining specialist Daniele Rodrigues for supporting this study. We also acknowledge the Institute of Geosciences of the University of Campinas, Prof. Dr. Carlos Roberto de Souza Filho, Dr. Rebecca Scafutto and Prof. Dr. Diego Ducart for the use of ASD-FieldSpec'', and the Devices and Nanostructures Laboratory of Federal University of Pernambuco, for providing access to analytical facilities, especially Dr. Edval Santos. N.M. Mesquita and Prof. J.A. Souza Neto thank the National Council for Scientific and Technological Development (CNPq) for providing, respectively, master's scholarship and research grant (process number 312.275/2017-0). We are so grateful to Dr. Daniel Muller and two anonymous reviewers for their valuable contributions to this manuscript.	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Rev.	DEC	2019	115								103192	10.1016/j.oregeorev.2019.103192	http://dx.doi.org/10.1016/j.oregeorev.2019.103192			17	Geology; Mineralogy; Mining & Mineral Processing	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Mineralogy; Mining & Mineral Processing	JU1BI					2023-06-23	WOS:000501412500019
J	de Oliveira, JF; Barboza, EG; Martins, EM; Scarelli, FM				de Oliveira, Julio F.; Barboza, Eduardo G.; Martins, Eduardo M.; Scarelli, Frederico M.			Geomorphological and stratigraphic analysis applied to coastal management	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article							GROUND-PENETRATING RADAR; SOUTHERN BRAZIL; EROSION MANAGEMENT; BARRIER; EVOLUTION; HOLOCENE; SEA; VULNERABILITY; QUATERNARY; DYNAMICS	Many of the current conflicts related to inadequate planning of coastal land use are due to the lack of public knowledge about coastal dynamics. With the objective of supporting Integrated Coastal Management actions and increasing public knowledge, this study presents results obtained from the application of Remote Sensing and Ground Penetrating Radar (GPR) to demonstrate the medium and long term behavior of the Cigana Beach barrier evolution in southern Brazil. The stratigraphic record enables definition of the Holocene retrogradational stacking pattern of the coastal barrier at the study area. On a more recent scale, the average of shoreline changes obtained from the aerial photos of 1938 and 1978 shows a historical erosion trend. The proposed use of the mean high tide line in 1831 to legally designate Federal Lands in coastal areas does not consider coastal dynamics and generates an overlap of public jurisdictions. Due to lack of information on a local scale, and the consequent missing application of coastal management tools for decision-making to resolve land use conflicts, incorporation of the knowledge generated in this work into municipal management instruments is suggested.	[de Oliveira, Julio F.; Barboza, Eduardo G.; Scarelli, Frederico M.] Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil; [Barboza, Eduardo G.] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, Inst Geociencias, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil; [Martins, Eduardo M.] Univ Fed Santa Catarina, Ctr Ciencias Rurais, Dept Ciencias Nat & Sociais, Rod Ulysses Gaboardi,Km 3, Curitibanos, SC, Brazil	Universidade Federal do Rio Grande do Sul; Universidade Federal do Rio Grande do Sul; Universidade Federal de Santa Catarina (UFSC)	de Oliveira, JF (autor correspondente), Univ Fed Rio Grande do Sul, Programa Posgrad Geociencias, Av Bento Goncalves 9500, Porto Alegre, RS, Brazil.	jfogeo@gmail.com; eduardo.barboza@ufrgs.br	Barboza, Eduardo Guimarães/C-7579-2012; Martins, Eduardo Marques/B-5518-2014; Oliveira, Julio Fernandes de/HPF-1935-2023	Barboza, Eduardo Guimarães/0000-0003-2107-6904; Martins, Eduardo Marques/0000-0002-9185-3791; Oliveira, Julio Fernandes de/0000-0001-7758-7434	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) [BEX 8003/14-9]; Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -Brasil (CNPq) [140741/2012-7]; Fundacao de Apoio da Universidade Federal do Rio Grande do Sul -Brasil (FAURGS) [04467 GEO/MUNICIPIO DE JAGUARUNA - IAP 000097]	Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -Brasil (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Fundacao de Apoio da Universidade Federal do Rio Grande do Sul -Brasil (FAURGS)	This study was financed in part by: i) Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior -Brasil (CAPES) -BEX 8003/14-9; ii) Conselho Nacional de Desenvolvimento Cientifico e Tecnologico -Brasil (CNPq) - 140741/2012-7; iii) Fundacao de Apoio da Universidade Federal do Rio Grande do Sul -Brasil (FAURGS) - 04467 GEO/MUNICIPIO DE JAGUARUNA - IAP 000097.	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J	de Oliveira, RS; Nogueira, ACR; Romero, GR; Truckenbrodt, W; Bandeira, JCD				de Oliveira, Rick Souza; Rodrigues Nogueira, Afonso Cesar; Romero, Guilherme Raffaeli; Truckenbrodt, Werner; da Silva Bandeira, Jose Cavalcante			Ediacaran ramp depositional model of the Tamengo Formation, Brazil	JOURNAL OF SOUTH AMERICAN EARTH SCIENCES			English	Article						Cloudina; Tamengo formation; Sedimentary facies; Ediacaran; Carbonate ramp	NEOPROTEROZOIC CARBONATE RAMP; NAMA GROUP; SOUTH-AMERICA; ITAPUCUMI GROUP; ISOTOPE RATIOS; CLYMENE OCEAN; LUCIANOI BEURLEN; FOSSIL CLOUDINA; EARLY EVOLUTION; SHELLY FOSSILS	The Tamengo Formation corresponds to one of the most complete records of Ediacaran carbonate deposits in South America that contains Claudine and Corumbella calcified exoskeletons macroscopic fossils. With the objective of characterizing its paleoenvironment, a total of ten sedimentary facies indicative of a carbonate platform were identified. In the outer ramp region there are massive mudstones, massive marl to claystones, and shales. In the mid-ramp there are facies that are storm-dominated with swaley/hummocky cross-stratified grainstone, tangential cross-bedding grainstone, massive bioclastic grainstone and massive marl to claystone. Lastly, in the inner ramp portion there are massive intraclastic grainstone, massive intraclastic rudstone, massive oolitic grainstone and laminate mudstone/shale rhythmite, and microbial textures are present at the base of the rhythmites, indicative of a back-ramp environment. Faciology data indicate that the Cloudinas inhabited a protected environment between oolitic bars in the inner ramp and back-ramp. These organisms were periodically transported and reworked by waves generated by storms in the mid-ramp and outer ramp zones. The positive values for delta C-13 in carbonates (1,5 to 5,4 parts per thousand) and delta N-15 (between 3,5 and 4,54 parts per thousand) of deposits with Claudine indicate a marine paleoenvironment with shallow, hot, and oxygenated waters with a high productivity of organic matter. In this context, the facies analyses and stratigraphy, aided by C, O, and N isotopes from the Tamengo Formation in outcrops from the Corumbd regions in the southwest of Brazil allows for the reconstruction of an Ediacaran carbonate ramp and inferences about the habitat of Claudine, thus increasing understanding of this important chapter of Earth history.	[de Oliveira, Rick Souza] Univ Fed Oeste Para UFOPA, Inst Engn & Geociencias, Rua Vera Paz S-N, BR-68040255 Santarem, PA, Brazil; [Rodrigues Nogueira, Afonso Cesar; Romero, Guilherme Raffaeli; Truckenbrodt, Werner; da Silva Bandeira, Jose Cavalcante] Univ Fed Para, PPGG, Rua Augusto Correa 01,Caixa Postal 1611, BR-66075110 Belem, Para, Brazil	Universidade Federal do Oeste do Para; Universidade Federal do Para	de Oliveira, RS (autor correspondente), Univ Fed Oeste Para UFOPA, Inst Engn & Geociencias, Rua Vera Paz S-N, BR-68040255 Santarem, PA, Brazil.	rick.oliveira@ufopa.edu.br	OLIVEIRA, Rick/Q-9613-2019	OLIVEIRA, Rick/0000-0001-7439-4944; Raffaeli Romero, Guilherme/0000-0001-9955-0878; NOGUEIRA, AFONSO/0000-0002-5225-9255	Brazilian Research Council for Science and Technology (CNPq) [Universal 481978/2004-6, Universal/CT-Petro -485902/2007/9]; Institute Nacional de Ciencia e Tecnologia de Geociencias da Amazonia (INCT -GEOCIAM); Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior (CAPES); Programa de Pos-Graduaccio em Geologia e Geoquimica da Universidade Federal do Para	Brazilian Research Council for Science and Technology (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ)); Institute Nacional de Ciencia e Tecnologia de Geociencias da Amazonia (INCT -GEOCIAM); Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)(Coordenacao de Aperfeicoamento de Pessoal de Nivel Superior (CAPES)); Programa de Pos-Graduaccio em Geologia e Geoquimica da Universidade Federal do Para	The authors thank the Brazilian Research Council for Science and Technology (CNPq), that financed this research through the projects Universal 481978/2004-6 and Universal/CT-Petro -485902/2007/9, the Institute Nacional de Ciencia e Tecnologia de Geociencias da Amazonia (INCT -GEOCIAM) for support, and the Coordenacdo de Aperfeicoamento de Pessoal de Nivel Superior (CAPES) for the masters research scholarship granted to the first author. Additionally, the authors thank the Programa de Pos-Graduaccio em Geologia e Geoquimica da Universidade Federal do Para (PPGG-UFPA) and Magali Ader of the Laboratoire de Geochimie des Isotopes Stables of Universite de Paris for logistical support. We also thank Professor Dr. Francois Gauthier-Lafaye of the Laboratoire d'Hydrologie et de Geochimie de Strasbourg of Universite de Strasbourg and Dra. Renata Hidalgo for help and valuable discussions during the field campaigns. The authors are grateful to the companies Calcdrio Corumbd Ltda., Itad Cimentos -Votorantim and the management of the Corcal and Laginha quarries for help and the access offered during field work. A special thanks to Prof. Dr. Troy Patrick Beldini of the Universidade Federal do Geste do Pard (UFOPA) and the anonymous reviewers for their careful review and suggestions that greatly improved the final version of the manuscript.	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DEC	2019	96								102348	10.1016/j.jsames.2019.102348	http://dx.doi.org/10.1016/j.jsames.2019.102348			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	KB8BX					2023-06-23	WOS:000506715400018
