1. Identity statement | |
Reference Type | Journal Article |
Site | plutao.sid.inpe.br |
Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identifier | J8LNKAN8RW/3D53QH5 |
Repository | dpi.inpe.br/plutao/2012/11.28.17.35.18 (restricted access) |
Last Update | 2013:02.07.17.14.26 (UTC) marciana |
Metadata Repository | dpi.inpe.br/plutao/2012/11.28.17.35.19 |
Metadata Last Update | 2018:06.05.00.02.10 (UTC) administrator |
Secondary Key | INPE--PRE/ |
DOI | 10.1016/j.quascirev.2012.08.019 |
ISSN | 0277-3791 |
Label | lattes: 0307721738107549 4 CohenPBRFGFS:2012:HoPaHi |
Citation Key | CohenPBRFGFS:2012:HoPaHi |
Title | Holocene palaeoenvironmental history of the Amazonian mangrove belt |
Project | CNPq (Project 562398/ 2008-2), FAPESPA (Project 104/2008), and FAPESP (Project 03615-5/2007). |
Year | 2012 |
Month | Nov. |
Access Date | 2024, Apr. 19 |
Secondary Type | PRE PI |
Number of Files | 1 |
Size | 753 KiB |
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2. Context | |
Author | 1 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 Identifier | 1 2 3 4 8JMKD3MGP5W/3C9JGTQ |
Group | 1 2 3 4 DSR-OBT-INPE-MCTI-GOV-BR |
Affiliation | 1 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 Address | 1 mcohen@ufpa.br 2 3 4 rossetti@dsr.inpe.br |
e-Mail Address | rossetti@dsr.inpe.br |
Journal | Quaternary Science Reviews |
Volume | 55 |
Number | 8 |
Pages | 50-58 |
Secondary Mark | A1_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 |
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3. Content and structure | |
Is the master or a copy? | is the master |
Content Stage | completed |
Transferable | 1 |
Content Type | External Contribution |
Version Type | publisher |
Keywords | Amazonia C/N carbon and nitrogen climatic changes palynology isotopes sea level vegetation water |
Abstract | Wetland 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. |
Area | SRE |
Arrangement | urlib.net > Fonds > Produção anterior à 2021 > DIDSR > Holocene palaeoenvironmental history... |
doc Directory Content | access |
source Directory Content | there are no files |
agreement Directory Content | there are no files |
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4. Conditions of access and use | |
Language | en |
User Group | administrator lattes marciana |
Visibility | shown |
Archiving Policy | denypublisher denyfinaldraft24 |
Read Permission | deny from all and allow from 150.163 |
Update Permission | not transferred |
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5. Allied materials | |
Next Higher Units | 8JMKD3MGPCW/3ER446E |
Dissemination | WEBSCI; PORTALCAPES; COMPENDEX. |
Host Collection | dpi.inpe.br/plutao@80/2008/08.19.15.01 |
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6. Notes | |
Empty Fields | alternatejournal 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 |
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7. Description control | |
e-Mail (login) | marciana |
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