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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3QAT57E
Repositorysid.inpe.br/mtc-m21b/2018/01.04.14.53   (restricted access)
Last Update2018:01.04.14.53.52 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21b/2018/01.04.14.53.52
Metadata Last Update2021:01.02.22.17.20 (UTC) administrator
DOI10.1016/j.quascirev.2017.12.005
ISSN0277-3791
Citation KeyCrivellariCKHPZZSMHAOM:2018:InAmFr
TitleIncreased Amazon freshwater discharge during late Heinrich Stadial 1
Year2018
MonthFeb.
Access Date2024, May 17
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size2525 KiB
2. Context
Author 1 Crivellari, Stefano
 2 Chiessi, Cristiano Mazur
 3 Kuhnert, Henning
 4 Häggi, Christoph
 5 Portilho-Ramos, Rodrigo da Costa
 6 Zeng, Jing-Ying
 7 Zhang, Yancheng
 8 Schefuß, Enno
 9 Mollenhauer, Gesine
10 Hefter, Jens
11 Alexandre, Felipe
12 Oliveira, Gilvan Sampaio de
13 Mulitza, Stefan
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12 8JMKD3MGP5W/3C9JHBE
Group 1
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12 DIDOP-CGCPT-INPE-MCTIC-GOV-BR
Affiliation 1 Universidade Federal de São Paulo (UNIFESP)
 2 Universidade de São Paulo (USP)
 3 University of Bremen
 4 University of Bremen
 5 Universidade Federal de São Paulo (UNIFESP)
 6 University of Bremen
 7 University of Bremen
 8 University of Bremen
 9 Alfred Wegener Institute for Polar and Marine Research
10 Alfred Wegener Institute for Polar and Marine Research
11 Instituto Nacional de Pesquisas Espaciais (INPE)
12 Instituto Nacional de Pesquisas Espaciais (INPE)
13 University of Bremen
Author e-Mail Address 1
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12 gilvan.sampaio@inpe.br
JournalQuaternary Science Reviews
Volume181
Pages144-155
Secondary MarkA1_INTERDISCIPLINAR A1_GEOCIÊNCIAS A1_CIÊNCIAS_AGRÁRIAS_I C_CIÊNCIAS_BIOLÓGICAS_I
History (UTC)2018-01-04 14:53:52 :: simone -> administrator ::
2018-01-04 14:53:52 :: administrator -> simone :: 2018
2018-01-04 14:57:58 :: simone -> administrator :: 2018
2021-01-02 22:17:20 :: administrator -> simone :: 2018
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsHeinrich Stadial 1
Amazon Basin
Continental precipitation
Planktonic foraminifera
Lipid biomarkers
AbstractThe temporal succession of changes in Amazonian hydroclimate during Heinrich Stadial 1 (HS1) (ca. 1814.7 cal ka BP) is currently poorly resolved. Here we present HS1 records based on isotope, inorganic and organic geochemistry from a marine sediment core influenced by the Amazon River discharge. Our records offer a detailed reconstruction of the changes in Amazonian hydroclimate during HS1, integrated over the basin. We reconstructed surface water hydrography using stable oxygen isotopes (δ18O) and Mg/Ca-derived paleotemperatures from the planktonic foraminifera Globigerinoides ruber, as well as salinity changes based on stable hydrogen isotope (δD) of palmitic acid. We also analyzed branched and isoprenoid tetraether concentrations, and compared them to existing bulk sediment ln(Fe/Ca) data and vegetation reconstruction based on stable carbon isotopes from n-alkanes, in order to understand the relationship between continental precipitation, vegetation and sediment production. Our results indicate a two-phased HS1 (HS1a and HS1b). During HS1a (1816.9 cal ka BP), a first sudden increase of sea surface temperatures (SST) in the western equatorial Atlantic correlated with the slowdown of the Atlantic Meridional Overturning Circulation (AMOC) and the associated southern hemisphere warming phase of the bipolar seesaw. This phase was also characterized by an increased delivery of terrestrial material. During HS1b (16.914.8 cal ka BP), a decrease in terrestrial input was, however, associated with a marked decline of seawater δ18O and palmitic acid δD. Both isotopic proxies independently indicate a drop in sea surface salinity (SSS). A number of records under the influence of the North Brazil Current, in contrast, indicate increases in SST and SSS resulting from a weakened AMOC during HS1. Our records thus suggest that the expected increase in SSS due to the AMOC slowdown was overridden by a two-phased positive precipitation anomaly in Amazonian hydroclimate.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDOP > Increased Amazon freshwater...
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4. Conditions of access and use
Languageen
Target Filecrivellari_increased.pdf
User Groupsimone
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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/43SQKNE
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.49.24 3
sid.inpe.br/bibdigital/2021/01.02.22.14 2
DisseminationWEBSCI; PORTALCAPES; COMPENDEX.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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