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1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentifierJ8LNKAN8RW/3D53QH2
Repositorydpi.inpe.br/plutao/2012/11.28.17.35.15   (restricted access)
Last Update2013:02.07.17.27.22 (UTC) marciana
Metadata Repositorydpi.inpe.br/plutao/2012/11.28.17.35.16
Metadata Last Update2018:06.05.00.02.10 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.1016/j.revpalbo.2012.08.007
ISSN0034-6667
Labellattes: 0307721738107549 4 FrançaCoPeRoSmGu:2012:ImClAn
Citation KeyFrançaFrCoPeRoGuSm:2012:ImClAn
TitleThe last mangroves of Marajó Island Eastern Amazon: Impact of climate and/or relative sea-level changes
ProjectFAPESPA (104/2008); FAPESP (03615-5/2007).
Year2012
MonthNov.
Access Date2024, May 02
Secondary TypePRE PI
Number of Files1
Size2724 KiB
2. Context
Author1 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.
Resume Identifier1
2
3
4
5 8JMKD3MGP5W/3C9JGTQ
Group1
2
3
4
5 DSR-OBT-INPE-MCTI-GOV-BR
Affiliation1 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
Author e-Mail Address1
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
e-Mail Addressrossetti@dsr.inpe.br
JournalReview of Palaeobotany and Palynology
Volume187
NumberArticle in Press
Pages50-65
Secondary MarkB3_BIOTECNOLOGIA B1_ECOLOGIA_E_MEIO_AMBIENTE B1_GEOCIÊNCIAS
History (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. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsAmazon coast
climate
holocene
palynology
sea level
vegetation
AbstractThe 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.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > The last mangroves...
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Languageen
User Groupadministrator
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
DisseminationWEBSCI; PORTALCAPES.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
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