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1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentifierJ8LNKAN8RW/3D53QH5
Repositorydpi.inpe.br/plutao/2012/11.28.17.35.18   (restricted access)
Last Update2013:02.07.17.14.26 (UTC) marciana
Metadata Repositorydpi.inpe.br/plutao/2012/11.28.17.35.19
Metadata Last Update2018:06.05.00.02.10 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.1016/j.quascirev.2012.08.019
ISSN0277-3791
Labellattes: 0307721738107549 4 CohenPBRFGFS:2012:HoPaHi
Citation KeyCohenPBRFGFS:2012:HoPaHi
TitleHolocene palaeoenvironmental history of the Amazonian mangrove belt
ProjectCNPq (Project 562398/ 2008-2), FAPESPA (Project 104/2008), and FAPESP (Project 03615-5/2007).
Year2012
MonthNov.
Access Date2024, Apr. 18
Secondary TypePRE PI
Number of Files1
Size753 KiB
2. Context
Author1 Cohen, Marcelo Cancela Lisboa
2 Pessenda, Luiz Carlos Ruiz
3 Behling, Hermann
4 Rossetti, Dilce de Fátima
5 França, Marlon Carlos
6 Guimarães, José Tasso Felix
7 Friaes, Yuri
8 Smith, Clarisse Beltrão
Resume Identifier1
2
3
4 8JMKD3MGP5W/3C9JGTQ
Group1
2
3
4 DSR-OBT-INPE-MCTI-GOV-BR
Affiliation1 Laboratory of Coastal Dynamics, Programa de Pós-Graduação em Geologia e Geoquímica, Instituto de Geociências, Universidade Federal do Pará (UFPA), Rua Augusto Correa 01, 66075-110 Belém, PA, Brazil
2 Centro de Energia Nuclear na Agricultura (CENA), 13400-000 Piracicaba, SP, Brazil
3 Department of Palynology and Climate Dynamics, Albrecht-von-Haller-Institute for Plant Sciences, University of Göttingen, Untere Karspüle 2, 37073 Göttingen, Germany
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5
6 Laboratory of Coastal Dynamics, Programa de Pós-Graduação em Geologia e Geoquímica, Instituto de Geociências, Universidade Federal do Pará (UFPA), Rua Augusto Correa 01, 66075-110 Belém, PA, Brazil
7 Laboratory of Coastal Dynamics, Programa de Pós-Graduação em Geologia e Geoquímica, Instituto de Geociências, Universidade Federal do Pará (UFPA), Rua Augusto Correa 01, 66075-110 Belém, PA, Brazil
8 Laboratory of Coastal Dynamics, Programa de Pós-Graduação em Geologia e Geoquímica, Instituto de Geociências, Universidade Federal do Pará (UFPA), Rua Augusto Correa 01, 66075-110 Belém, PA, Brazil
Author e-Mail Address1 mcohen@ufpa.br
2
3
4 rossetti@dsr.inpe.br
e-Mail Addressrossetti@dsr.inpe.br
JournalQuaternary Science Reviews
Volume55
Number8
Pages50-58
Secondary MarkA1_CIÊNCIAS_BIOLÓGICAS_I A1_GEOCIÊNCIAS A1_INTERDISCIPLINAR
History (UTC)2012-11-28 23:06:32 :: lattes -> marciana :: 2012
2013-01-17 14:26:52 :: marciana -> administrator :: 2012
2013-01-20 15:55:14 :: administrator -> marciana :: 2012
2013-02-07 17:14:26 :: 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
KeywordsAmazonia
C/N
carbon and nitrogen
climatic changes
palynology
isotopes
sea level
vegetation
water
AbstractWetland dynamic in the northern Brazilian Amazon region during the Holocene was reviewed using palynological, carbon and nitrogen isotopes records, and C/N ratio previously published. The integration of 72 radiocarbon dates recorded in 34 sediment cores sampled along the marine and fluvial littoral, and mainly influenced by the Amazon River, reveals that marine influence and mangrove vegetation were wider than today on the mouth of Amazon River between >8990-8690 and 2300-2230 cal yr BP, forming a continuous mangrove belt along the northern Brazilian Amazon littoral. The establishment of this mangrove strip is a direct consequence of the marine incursion caused by post-glacial sea-level rise possibly associated with tectonic subsidence during the Early and Middle Holocene. In the Late Holocene, in areas influenced by the Amazon River discharge, the mangroves were replaced by freshwater vegetation, and the coast morphology evolved from an estuarine dominated into a rectilinear coast due to coastal progradation. Nevertheless, the marine-influenced littoral, which is currently dominated by mangroves and salt-marsh vegetation, has persistently had brackish water vegetation over tidal mud flats throughout the entire Holocene. Likely, the fragmentation of this continuous mangrove line during the Late Holocene was caused by the increase of river freshwater discharge associated to the change from dry into wet climates in the Late Holocene. This caused a significant decrease of tidal water salinity in areas near the mouth of Amazon River. These changes in the Amazon discharge are probably associated with dry and wet periods in the northern Amazon region during the Holocene.
AreaSRE
Arrangementurlib.net > Fonds > Produção anterior à 2021 > DIDSR > Holocene palaeoenvironmental history...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
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Languageen
User Groupadministrator
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Visibilityshown
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Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
DisseminationWEBSCI; PORTALCAPES; COMPENDEX.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
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