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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/3R8F6FL
Repositorysid.inpe.br/mtc-m21c/2018/06.04.16.06   (restricted access)
Last Update2018:06.04.16.06.37 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2018/06.04.16.06.37
Metadata Last Update2020:12.07.21.11.46 (UTC) administrator
DOI10.1017/RDC.2017.62
ISSN0033-8222
Citation KeySilvaCoheRossPess:2018:DiSeCh
TitleDid sea-level changes affect the brazilian amazon forest during the holocene?
Year2018
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size1208 KiB
2. Context
Author1 Silva, Mayra Nina Araújo
2 Cohen, Marcelo C. L.
3 Rossetti, Dilce de Fátima
4 Pessenda, Luiz C. R.
Resume Identifier1
2
3 8JMKD3MGP5W/3C9JGTQ
Group1
2
3 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
Affiliation1 Universidade Federal do Pará (UFPA)
2 Universidade Federal do Pará (UFPA)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade de São Paulo (USP)
Author e-Mail Address1
2
3 dilce.rossetti@inpe.br
JournalRadiocarbon
Volume60
Number1
Pages91-112
Secondary MarkA1_INTERDISCIPLINAR A1_ANTROPOLOGIA_/_ARQUEOLOGIA A2_GEOCIÊNCIAS A2_ENGENHARIAS_II A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I B1_ASTRONOMIA_/_FÍSICA
History (UTC)2018-06-04 16:08:40 :: simone -> administrator :: 2018
2020-12-07 21:11:46 :: administrator -> simone :: 2018
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsAmazonia
Branco River
climate
Holocene
palynology
sea level
AbstractIn order to contribute to the discussion of Holocene climate changes, four sediment cores were collected from the northern Brazilian Amazonia lowland. These cores were studied through pollen analysis and sedimentary features, and the results were discussed within a chronological framework provided by radiocarbon dating. The cores were sampled from fluvial terraces representative of channel, floodplain/lake and crevasse splay deposits formed since the mid-Holocene. The pollen samples derive from floodplain/lake deposits and the pollen grains are mainly composed by families Moraceae, Euphorbiaceae, Caesalpiniaceae, Fabaceae, Rubiaceae, Melastomataceae, Combretaceae, Sapindaceae, Poaceae, Cyperaceae, Aizoaceae, Apiaceae and genus Sebastiana. The pollen data suggest no significant vegetation changes in the study area for the past 48084886 cal yr BP. This led to proposing stable climatic conditions since at least the middle Holocene. Such a finding is contrary to the occurrence of a dry period during the middle Holocene. The stabilization of the relative sea level about 6000 cal yr BP along the northern Brazilian littoral may have influenced the water table, and favored the establishment and maintenance of Amazonian lowland forest during the mid- and late Holocene. In addition, this process may have attenuated the impact of that dry period in areas under most fluvial influence.
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Arrangementurlib.net > DIDSR > Did sea-level changes...
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4. Conditions of access and use
Languageen
Target Filesilva_did.pdf
User Groupsimone
Reader Groupadministrator
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Visibilityshown
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/bibdigital/2013/09.13.21.11 4
sid.inpe.br/mtc-m21/2012/07.13.14.44.37 1
DisseminationWEBSCI
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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