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3 referências similares encontradas (inclusive a original) buscando em 22 dentre 22 Arquivos.
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3NNKKGB
Repositóriosid.inpe.br/mtc-m21b/2017/04.19.13.54   (acesso restrito)
Última Atualização2017:07.20.19.34.04 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2017/04.19.13.54.23
Última Atualização dos Metadados2018:06.04.02.27.24 (UTC) administrator
DOI10.1017/RDC.2016.107
ISSN0033-8222
Chave de CitaçãoRossettiCohePess:2017:VeChSo
TítuloVegetation change in southwestern amazonia (Brazil) and relationship to the late pleistocene and holocene climate
Ano2017
MêsFeb.
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1858 KiB
2. Contextualização
Autor1 Rossetti, Dilce de Fátima
2 Cohen, Marcelo C. L.
3 Pessenda, Luiz C. R.
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGTQ
Grupo1 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade Federal do Pará (UFPA)
3 Universidade de São Paulo (USP)
Endereço de e-Mail do Autor1 dilce.rossetti@inpe.br
RevistaRadiocarbon
Volume59
Número1
Páginas69-89
Nota SecundáriaA1_INTERDISCIPLINAR A1_ANTROPOLOGIA_/_ARQUEOLOGIA A2_GEOCIÊNCIAS A2_ENGENHARIAS_II A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I B1_ASTRONOMIA_/_FÍSICA
Histórico (UTC)2017-04-19 13:54:56 :: simone -> administrator :: 2017
2017-06-26 03:35:04 :: administrator -> simone :: 2017
2017-07-20 19:34:05 :: simone -> administrator :: 2017
2018-06-04 02:27:24 :: administrator -> simone :: 2017
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-ChaveCarbon isotopes
Climate
Late Pleistocene-Holocene
Sedimentary dynamics
Southwestern Amazonia
Vegetation
ResumoThe Late Quaternary climate in Amazonia is an issue still open to debate, with hypotheses varying from alternate dry and wet episodes to stable climate with undisturbed rainforest. We approach this question using δ13C, C/N, and, to a lesser extent, δ15N from deposits derived from four cores, with the results combined with published pollen data from two of these cores. These data were analyzed within the context of radiocarbon dating, which revealed ages ranging from 42.8-41.8 to 2.3-2.2 cal ka BP. Fluvial channel and floodplain deposits with freshwater phytoplankton recorded a trend of wet climate with dry episodes before ~40 cal ka BP, followed by humid and cold climate until the Last Glacial Maximum, with intensified aridity towards the end of the Late Pleistocene. Peaks of increased contributions in C4 land plants in the mid-to late Holocene were not synchronous and have no correspondence with Amazonian Holocene dry episodes, being due to sedimentary processes related to fluvial dynamics during the establishment of herbaceous fields on abandoned depositional sites. Thus, the climate remained wet in the Holocene, which would have favored the expansion of the Amazonian rainforest as we see today.
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4. Condições de acesso e uso
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Grupo de Leitoresadministrator
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.44.37 5
sid.inpe.br/bibdigital/2013/09.13.21.11 3
DivulgaçãoWEBSCI
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject targetfile tertiarymark tertiarytype url
7. Controle da descrição
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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP5W34M/3FA45DJ
Repositóriosid.inpe.br/mtc-m21b/2013/11.26.16.54.34   (acesso restrito)
Última Atualização2014:04.14.18.10.40 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2013/11.26.16.54.35
Última Atualização dos Metadados2018:06.04.03.14.12 (UTC) administrator
DOI10.2458/azu_js_rc.55.16211
ISSN0033-8222
Rótuloscopus 2013-11
Chave de CitaçãoBusoJrPOGCVORLBSBFGS:2013:LaPlHo
TítuloLate Pleistocene and Holocene vegetation, climate dynamics, and Amazonian Taxa in the Atlantic forest, Linhares, SE Brazil
Ano2013
Data de Acesso16 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1852 KiB
2. Contextualização
Autor 1 Buso Junior, Antonio Alvaro
 2 Pessenda, Luiz Carlos Ruiz
 3 Oliveira, Paulo Eduardo de
 4 Giannini, Paulo César Fonseca
 5 Cohen, Marcelo Cancela Lisboa
 6 Volkmer-Ribeiro, Cecília
 7 Oliveira, Sonia Maria Barros de
 8 Rossetti, Dilce de Fatima
 9 Lorente, Flávio Lima
10 Borotti Filho, Marcos Antonio
11 Schiavo, Jolimar Antonio
12 Bendassolli, José Albertino
13 França, Marlon Carlos
14 Guimarães, José Tasso Felix
15 Siqueira, Geovane Souza
Identificador de Curriculo 1
 2
 3
 4
 5
 6
 7
 8 8JMKD3MGP5W/3C9JGTQ
Grupo 1
 2
 3
 4
 5
 6
 7
 8 DSR-OBT-INPE-MCTI-GOV-BR
Afiliação 1 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
 2 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
 3 São Francisco University, Brazil
 4 Instituto de Geociências da Universidade de São Paulo, Brazil
 5 Federal University of Pará, Brazil
 6 Fundação Zoobotânica do Rio Grande do Sul, Brazil
 7 Instituto de Geociências da Universidade de São Paulo, Brazil
 8 Instituto Nacional de Pesquisas Espaciais (INPE)
 9 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
10 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
11 Universidade Estadual de Mato Grosso do Sul, Brazil
12 Center for Nuclear Energy in Agriculture (CENA/USP), Brazil
13 Instituto de Geociências, Univ. Federal do Pará (UFPA), Brazil
14 Instituto de Geociências, Univ. Federal do Pará (UFPA), Brazil
15 Vale Nature Reserve, Brazil
Endereço de e-Mail do Autor 1 alvaro.buso.jr@gmail.com
 2
 3
 4
 5
 6
 7
 8 rossetti@dsr.inpe.br
Endereço de e-Mailmarcelo.pazos@inpe.br
RevistaRadiocarbon
Volume55
Número2-3
Páginas1747-1762
Nota SecundáriaA1 A1 A1 A2 A2 B1 B1
Histórico (UTC)2018-06-04 03:14:12 :: administrator -> :: 2013
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chaveabundance
climate change
dominance
Holocene
humid environment
Pleistocene
seasonal variation
sediment core
soil profile
vegetation dynamics
Atlantic Forest
Brazil
Espirito Santo
Linhares
filicophyta
ResumoAnalysis of biological proxies in lake sediment and geochemical analysis of soil profiles reveal natural vegetation dynamics, with climate inferences, since the late Pleistocene in a fragment of the pristine lowland Atlantic Forest of southeastern Brazil. Carbon isotopes from soil organic matter and 14C ages from the humin fraction indicate the dominance of C3 plants since ~17,000 cal BP. Palynological analysis of a sediment core indicates the presence of Atlantic Forest vegetation since 7700 cal BP. Changes in the relative abundance of tree ferns and palms suggest the predominance of a humid period from ~7000-4000 cal BP and establishment of the modern seasonal climate at ~4000 cal BP. Data indicate maintenance of the regional forest coverage since the late Pleistocene, corroborating previous suggestions that this region was a forest refuge during less humid periods of the late Pleistocene and Holocene. Some plant taxa with currently divided distributions between Amazonia and the Atlantic Forest colonized the region since at least 7500 cal BP, indicating an earlier connection between Amazonia and Atlantic Forest.
ÁreaSRE
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Idiomaen
Arquivo Alvo16211-23001-5-PB.pdf
Grupo de Usuáriosadministrator
marcelo.pazos@inpe.br
Grupo de Leitoresadministrator
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Visibilidadeshown
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5. Fontes relacionadas
Repositório Espelhoiconet.com.br/banon/2006/11.26.21.31
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Lista de Itens Citandosid.inpe.br/mtc-m21/2012/07.13.14.44.37 6
DivulgaçãoWEBSCI; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
NotasProceedings of the 21st International Radiocarbon Conference
Campos Vaziosalternatejournal archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark month nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url

1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16d.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP7W/395S5HH
Repositóriosid.inpe.br/mtc-m19/2011/02.08.12.16
Última Atualização2011:02.08.12.16.07 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m19/2011/02.08.12.16.07
Última Atualização dos Metadados2018:06.05.04.35.29 (UTC) administrator
Chave SecundáriaINPE--PRE/
Chave de CitaçãoRossettiBGVAMTB:2010:LaPlRe
TítuloThe late Pleistocene-Holocene record of sea level in Northeastern Brazil and its relation to climate, eustasy and tectonics
FormatoOn-line
Ano2010
Data de Acesso16 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho440 KiB
2. Contextualização
Autor1 Rossetti, D
2 Bezerra, F H
3 Góes, A
4 Valeriano, M
5 Andrades Filho, C
6 Millani, J
7 Tatumi, S
8 Brito Neves, B B
Grupo1 DSR-OBT-INPE-MCT-BR
2
3
4 DSR-OBT-INPE-MCT-BR
5 DSR-OBT-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2
3 USP, São Paulo, Brazil
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 FATEC, São Paulo, Brazil
7 FATEC, São Paulo, Brazil
8 USP, São Paulo, Brazil
Nome do EventoMeeting of the Americas.
Localização do EventoFoz Iguaçu
Data8-12 Aug. 2010
Título do LivroProceedings
Histórico (UTC)2011-02-08 12:58:01 :: marciana -> administrator :: 2010
2018-06-05 04:35:29 :: administrator -> marciana :: 2010
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoAB: Late Quaternary deposits in Northeastern Brazil have been scarcely investigated, despite their great relevance to discuss the post-rift evolution of South American passive margin within the context of landform, sea level and tectonic deformation. Sedimentological, stratigraphic and morphological characterization of these deposits led to their distinction from the underlying Early/Middle Miocene Barreiras Formation. Two sedimentary units (PB1 and PB2) were recognized and related, with basis on optically stimulated luminescence (OSL) dating, to the time intervals between 74.8±9.3 and 30.8±6.9 ka, and 8.8±0.9 and 1.8±0.2 ka, respectively. Unit PB1 is exposed discontinuously in the highest topography (usually between 100 m and 150 m), being mostly composed of endured sandstones and breccias either with massive bedding or an abundance of complex styles of ductile and brittle soft sediment deformation structures related to contemporaneous seismic activity. This unit also includes a large volume of non-indured sharply bounded, fining upward massive or stratified conglomerates and sandstones interbedded with mudstones, attributed to fluvial, alluvial and aeolian dune environments. These deposits might include nearshore marine-influenced strata in areas located nearby the modern coastline, as suggested by presence of burrows as Skolithos, Thalassinoides, Planolites, Diplocraterion, and Teichichnus. Unit PB2, composed of sands with massive or dissipation dune structures, occurs continuously, mostly on northeastward dipping tablelands located at altitudes lower than 100 m. The present work focusing on units PB1 and PB2, together referred as Post-Barreiras Sediments, opens a new opportunity to discuss landform, sea level and tectonic history of eastern South American passive margin during the latest Quaternary. Hence, following the Miocene transgression, there was a prolonged period of non-deposition and sub-aerial exposure, which is related to combination of a worldwide low sea level in the Tortonian and tectonic quiescence. Sediment deposition was reactivated during the latest Pleistocene due to tectonic deformation, which created space to accommodate unit PB1 in downthrown faulted blocks and, perhaps, also synclines produced by extension and compression associated with strike-slip tectonic deformation. Although deposition of this unit was simultaneous to the eustatic fall that followed the Penultimate Transgression, punctuated rises superimposed on the overall fall, added to subsidence, would have favored marine deposition in areas located nearby the modern coastline. A renewed phase of deformation would have resulted in newly subsiding areas in the Holocene, promoting deposition of unit PB2 over unit PB1. Although unit PB2 formed during most of the last transgression, except along coastal areas, it has no records of marine sedimentation, suggesting a non-significant rise or reworking of thin transgressive sands by aeolian process. The data presented herein leads to review the evolution of South American passive margin based on assumptions of uniform sedimentation and undeformed planation surfaces over a wide coastal area of Northeastern Brazil.
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Idiomaen
Arquivo Alvocintra.pdf
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marciana
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Repositório Espelhosid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosarchivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor electronicmailaddress isbn issn keywords label lineage mark nextedition notes numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark tertiarytype type url versiontype volume
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