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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/3D53QH2
Repositóriodpi.inpe.br/plutao/2012/11.28.17.35.15   (acesso restrito)
Última Atualização2013:02.07.17.27.22 (UTC) marciana
Repositório de Metadadosdpi.inpe.br/plutao/2012/11.28.17.35.16
Última Atualização dos Metadados2018:06.05.00.02.10 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1016/j.revpalbo.2012.08.007
ISSN0034-6667
Rótulolattes: 0307721738107549 4 FrançaCoPeRoSmGu:2012:ImClAn
Chave de CitaçãoFrançaFrCoPeRoGuSm:2012:ImClAn
TítuloThe last mangroves of Marajó Island Eastern Amazon: Impact of climate and/or relative sea-level changes
ProjetoFAPESPA (104/2008); FAPESP (03615-5/2007).
Ano2012
MêsNov.
Data de Acesso13 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho2724 KiB
2. Contextualização
Autor1 França, Marlon C.
2 Francisquini, Mariah I.
3 Cohen, Marcelo Cancela Lisboa
4 Pessenda, Luiz Carlos Ruiz
5 Rossetti, Dilce de Fátima
6 Guimarães, José Tasso F
7 Smith, Clarisse B.
Identificador de Curriculo1
2
3
4
5 8JMKD3MGP5W/3C9JGTQ
Grupo1
2
3
4
5 DSR-OBT-INPE-MCTI-GOV-BR
Afiliação1 Coastal Dynamics Laboratory, Post-Graduate Program in Geology and Geochemistry, Federal University of Pará, Av. Perimentral 2651, Terra Firme, CEP: 66077-530, Belém (PA), Brazil
2 Center for Nuclear Energy in Agriculture (CENA), University of São Paulo
3 Coastal Dynamics Laboratory, Post-Graduate Program in Geology and Geochemistry, Federal University of Pará, Av. Perimentral 2651, Terra Firme, CEP: 66077-530, Belém (PA), Brazil
4
5 Instituto Nacional de Pesquisas Espaciais (INPE)
6 Coastal Dynamics Laboratory, Post-Graduate Program in Geology and Geochemistry, Federal University of Pará, Av. Perimentral 2651, Terra Firme, CEP: 66077-530, Belém (PA), Brazil
7 Coastal Dynamics Laboratory, Post-Graduate Program in Geology and Geochemistry, Federal University of Pará, Av. Perimentral 2651, Terra Firme, CEP: 66077-530, Belém (PA), Brazil
Endereço de e-Mail do Autor1
2
3 mcohen@ufpa.br
4 Center for Nuclear Energy in Agriculture (CENA), University of São Paulo, 13400-000, Piracicaba (SP), Brazil
5 rossetti@dsr.inpe.br
Endereço de e-Mailrossetti@dsr.inpe.br
RevistaReview of Palaeobotany and Palynology
Volume187
NúmeroArticle in Press
Páginas50-65
Nota SecundáriaB3_BIOTECNOLOGIA B1_ECOLOGIA_E_MEIO_AMBIENTE B1_GEOCIÊNCIAS
Histórico (UTC)2012-11-28 23:06:32 :: lattes -> marciana :: 2012
2012-11-30 17:26:30 :: marciana -> administrator :: 2012
2013-01-20 15:55:13 :: administrator -> marciana :: 2012
2013-02-07 17:27:22 :: marciana -> administrator :: 2012
2018-06-05 00:02:10 :: administrator -> marciana :: 2012
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-ChaveAmazon coast
climate
holocene
palynology
sea level
vegetation
ResumoThe dynamics, over the last 7500. years, of a mangrove at Marajó Island in northern Brazil were studied by pollen and sedimentary facies analyses using sediment cores. This island, located at the mouth of the Amazon River, is influenced by riverine inflow combined with tidal fluctuations of the equatorial Atlantic Ocean. Herbaceous vegetation intermingled with rainforest dominates the central area of the island, while várzea is the main vegetation type along the littoral. In particular, the modern northeastern coastal zone is covered by a mosaic of dense rainforest, herbaceous vegetation, mangroves, várzea, and restinga. The integration of pollen data and facies descriptions indicates a tidal mud flat colonized by mangroves in the interior of Marajó Island between ~. 7500. cal. yr BP and ~. 3200. cal. yr BP. During the late Holocene, mangroves retracted to a small area (100-700. m in width) along the northeastern coastal plain. Mangrove expansion during the early and mid Holocene was likely caused by the post-glacial sea-level rise which, combined with tectonic subsidence, led to a rise in tidal water salinity. Salinity must have further increased due to low river discharge resulting from increased aridity during the early and mid Holocene. The shrinking of the area covered by mangrove vegetation during the late Holocene was likely caused by the increase in river discharge during the late Holocene, which has maintained relatively low tidal water salinity in Marajó Island. Tidal water salinity is relatively higher in the northeastern part of the island than in others, due to the southeast-northwest trending current along the littoral. The mixing of marine and riverine freshwater inflows has provided a refuge for mangroves in this area. The increase in flow energy during the last century is related to landward sand migration, which explains the current retraction of mangroves. These changes may indicate an increased exposure to tidal influence driven by the relative sea-level rise, either associated with global fluctuations or tectonic subsidence, and/or by an increase in river water discharge.
ÁreaSRE
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > The last mangroves...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Grupo de Usuáriosadministrator
lattes
marciana
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
DivulgaçãoWEBSCI; PORTALCAPES.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress readergroup rightsholder schedulinginformation secondarydate session shorttitle sponsor subject targetfile tertiarymark tertiarytype typeofwork url
7. Controle da descrição
e-Mail (login)marciana
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