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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/3R3TR32
Repositorysid.inpe.br/mtc-m21c/2018/05.07.19.21   (restricted access)
Last Update2018:05.07.19.21.36 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2018/05.07.19.21.36
Metadata Last Update2020:12.07.21.11.37 (UTC) administrator
DOI10.1016/j.jsames.2018.04.006
ISSN0895-9811
Citation KeyLorentePOBRGCOMFFBM:2018:11ReDe
TitleAn 11,000-year record of depositional environmental change based upon particulate organic matter and stable isotopes (C and N) in a lake sediment in southeastern Brazil
Year2018
MonthJuly
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size3196 KiB
2. Context
Author 1 Lorente, Flávio Lima
 2 Pessenda, Luiz Carlos Ruiz
 3 Oboh-Ikuenobe, Francisca
 4 Buso Junior, Antonio Alvaro
 5 Rossetti, Dilce de Fátima
 6 Giannini, Paulo César Fonseca
 7 Cohen, Marcelo Cancela Lisboa
 8 Oliveira, Paulo Eduardo de
 9 Mayle, Francis Edward
10 Francisquini, Mariah Izar
11 França, Marlon Carlos
12 Bendassolli, José Albertino
13 Macario, Kita
Resume Identifier 1
 2
 3
 4
 5 8JMKD3MGP5W/3C9JGTQ
Group 1
 2
 3
 4
 5 DIDSR-CGOBT-INPE-MCTIC-GOV-BR
Affiliation 1 Centro de Energia Nuclear em Agricultura (CENA)
 2 Centro de Energia Nuclear em Agricultura (CENA)
 3 Missouri University of Science and Technology
 4 Centro de Energia Nuclear em Agricultura (CENA)
 5 Instituto Nacional de Pesquisas Espaciais (INPE)
 6 Universidade de São Paulo (USP)
 7 Universidade Federal do Pará (UFPA)
 8 Universidade de São Paulo (USP)
 9 University of Reading
10 Centro de Energia Nuclear em Agricultura (CENA)
11 Instituto Federal do Pará (IFPA)
12 Centro de Energia Nuclear em Agricultura (CENA)
13 Universidade Federal Fluminense (UFF)
Author e-Mail Address 1
 2
 3
 4
 5 dilce.rossetti@inpe.br
JournalJournal of South American Earth Sciences
Volume84
Pages373-384
Secondary MarkA1_INTERDISCIPLINAR A1_GEOGRAFIA A2_GEOCIÊNCIAS A2_ENGENHARIAS_III A2_CIÊNCIAS_AGRÁRIAS_I B1_ODONTOLOGIA B1_MEDICINA_II B1_CIÊNCIAS_AMBIENTAIS B1_BIODIVERSIDADE B1_ANTROPOLOGIA_/_ARQUEOLOGIA B2_QUÍMICA B2_MATERIAIS B2_CIÊNCIAS_BIOLÓGICAS_I B3_ASTRONOMIA_/_FÍSICA C_ENGENHARIAS_II
History (UTC)2018-05-07 19:21:36 :: simone -> administrator ::
2018-05-07 19:21:36 :: administrator -> simone :: 2018
2018-05-07 19:24:30 :: simone -> administrator :: 2018
2020-12-07 21:11:37 :: administrator -> simone :: 2018
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsHolocene
Organic matter
Stable isotopes
Paleoenvironment
Palynofacies
AbstractThe aim of this paper is to reconstruct an 11,000-year history of depositional environmental change in southeastern Brazil, based upon the integration of particulate organic matter and stable isotope (C and N) data from a 136-cm sediment core from Lake Canto Grande. These proxies are used to explore the evolution of terrestrial and marine influence on the lake. Isotopic (δ13C: −27.87 to −31.9; δ15N: −0.074.9) and elemental (total organic carbon - TOC: 0.58%37.19%; total nitrogen - TN: 0.08%1.73%; C/N: 0.3 to 54.7) values recorded in Lake Canto Grande suggest that the sedimentary organic matter was derived from mostly C3 land plants and freshwater phytoplankton. Particulate organic matter and cluster analyses distinguished four associations characterized by the predominance of amorphous organic matter, followed by phytoclasts and palynomorphs. These results indicate two different phases of lake evolution. The first phase (136 - 65 cm; ∼10,943 cal yr. B.P. to ∼8529 cal yr. B.P.) is recorded by sand layers interbedded with mud, which contain amorphous organic matter (AOM, 4559%) and phytoclasts (opaques - OP: 618%; non-opaques NOP: 1723%) which indicate a floodplain area. The second phase (650 cm; ∼8529 cal yr. B.P. to ∼662 cal yr. B.P.) comprises mud, AOM (6886%) and palynomorphs (PAL, 816%) related to lake establishment comparable to modern conditions. Thus, characterizing particulate organic matter, in combination with stable isotopes, proved to be invaluable proxies for lacustrine paleoenvironmental change through the Holocene.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > An 11,000-year record...
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4. Conditions of access and use
Languageen
Target Filelorente_11.pdf
User Groupsimone
Reader Groupadministrator
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
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 2
DisseminationWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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