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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3NNKKGB
Repositorysid.inpe.br/mtc-m21b/2017/04.19.13.54   (restricted access)
Last Update2017:07.20.19.34.04 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2017/04.19.13.54.23
Metadata Last Update2018:06.04.02.27.24 (UTC) administrator
DOI10.1017/RDC.2016.107
ISSN0033-8222
Citation KeyRossettiCohePess:2017:VeChSo
TitleVegetation change in southwestern amazonia (Brazil) and relationship to the late pleistocene and holocene climate
Year2017
MonthFeb.
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size1858 KiB
2. Context
Author1 Rossetti, Dilce de Fátima
2 Cohen, Marcelo C. L.
3 Pessenda, Luiz C. R.
Resume Identifier1 8JMKD3MGP5W/3C9JGTQ
Group1 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade Federal do Pará (UFPA)
3 Universidade de São Paulo (USP)
Author e-Mail Address1 dilce.rossetti@inpe.br
JournalRadiocarbon
Volume59
Number1
Pages69-89
Secondary MarkA1_INTERDISCIPLINAR A1_ANTROPOLOGIA_/_ARQUEOLOGIA A2_GEOCIÊNCIAS A2_ENGENHARIAS_II A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I B1_ASTRONOMIA_/_FÍSICA
History (UTC)2017-04-19 13:54:56 :: simone -> administrator :: 2017
2017-06-26 03:35:04 :: administrator -> simone :: 2017
2017-07-20 19:34:05 :: simone -> administrator :: 2017
2018-06-04 02:27:24 :: administrator -> simone :: 2017
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsCarbon isotopes
Climate
Late Pleistocene-Holocene
Sedimentary dynamics
Southwestern Amazonia
Vegetation
AbstractThe Late Quaternary climate in Amazonia is an issue still open to debate, with hypotheses varying from alternate dry and wet episodes to stable climate with undisturbed rainforest. We approach this question using δ13C, C/N, and, to a lesser extent, δ15N from deposits derived from four cores, with the results combined with published pollen data from two of these cores. These data were analyzed within the context of radiocarbon dating, which revealed ages ranging from 42.8-41.8 to 2.3-2.2 cal ka BP. Fluvial channel and floodplain deposits with freshwater phytoplankton recorded a trend of wet climate with dry episodes before ~40 cal ka BP, followed by humid and cold climate until the Last Glacial Maximum, with intensified aridity towards the end of the Late Pleistocene. Peaks of increased contributions in C4 land plants in the mid-to late Holocene were not synchronous and have no correspondence with Amazonian Holocene dry episodes, being due to sedimentary processes related to fluvial dynamics during the establishment of herbaceous fields on abandoned depositional sites. Thus, the climate remained wet in the Holocene, which would have favored the expansion of the Amazonian rainforest as we see today.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Vegetation change in...
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4. Conditions of access and use
Languageen
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/mtc-m21/2012/07.13.14.44.37 5
sid.inpe.br/bibdigital/2013/09.13.21.11 3
DisseminationWEBSCI
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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