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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3J33G2B
Repositorysid.inpe.br/mtc-m21b/2015/02.24.17.39   (restricted access)
Last Update2015:02.24.17.39.38 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2015/02.24.17.39.38
Metadata Last Update2018:06.04.02.55.16 (UTC) administrator
DOI10.1016/j.catena.2015.02.005
ISSN0341-8162
Citation KeyFrançaACCRPLFBGF:2015:MuEvTr
TitleA multi-proxy evidence for the transition from estuarine mangroves to deltaic freshwater marshes, Southeastern Brazil, due to climatic and sea-level changes during the late Holocene
Year2015
MonthMay
Access Date2024, May 18
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size2755 KiB
2. Context
Author 1 França, Marlon C.
 2 Alves, Igor Charles C.
 3 Castro, Darciléa Ferreira
 4 Cohen, Marcelo C. L.
 5 Rossetti, Dilce de Fátima
 6 Pessenda, Luiz C. R.
 7 Lorente, Flávio L.
 8 Fontes, Neuza Araújo
 9 Buso Junior, Antônio Álvaro
10 Giannini, Paulo César Fonseca
11 Francisquini, Mariah Izar
Resume Identifier 1
 2
 3
 4
 5 8JMKD3MGP5W/3C9JGTQ
Group 1
 2
 3 DSR-OBT-INPE-MCTI-GOV-BR
 4
 5 DSR-OBT-INPE-MCTI-GOV-BR
Affiliation 1 Universidade Federal do Pará (UFPA)
 2 Universidade Federal do Pará (UFPA)
 3 Instituto Nacional de Pesquisas Espaciais (INPE)
 4 Universidade Federal do Pará (UFPA)
 5 Instituto Nacional de Pesquisas Espaciais (INPE)
 6 Universidade de São Paulo (USP)
 7 Universidade de São Paulo (USP)
 8 Universidade Federal do Pará (UFPA)
 9 Universidade de São Paulo (USP)
10 Universidade de São Paulo (USP)
11 Universidade de São Paulo (USP)
Author e-Mail Address 1 marlon.franca@fpa.edu.br
 2
 3 darcicastro@yahoo.com.br
 4
 5 rossetti@dsr.inpe.br
JournalCatena
Volume128
Pages155-166
Secondary MarkA1_ENGENHARIAS_I A1_GEOGRAFIA A2_GEOCIÊNCIAS A2_CIÊNCIAS_AGRÁRIAS_I A2_ENGENHARIAS_III A2_SOCIOLOGIA B2_QUÍMICA B2_CIÊNCIAS_BIOLÓGICAS_I B3_ASTRONOMIA_/_FÍSICA C_ZOOTECNIA_/_RECURSOS_PESQUEIROS
History (UTC)2015-02-24 17:39:38 :: simone -> administrator ::
2018-06-04 02:55:16 :: administrator -> simone :: 2015
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsCarbon and nitrogen isotopes
Diatoms
Holocene
Palynology
Sea-level changes
Southeastern Brazil
AbstractThe present study investigates a paleo-estuary at the Doce River Delta, southeastern Brazil, through a multi-proxy approach that links palynology, diatoms, sedimentology and geochemistry analyses (i.e., Total C, Total N, δ13C and δ15N). These analyses, temporally synchronized with five radiocarbon ages, revealed environmental changes from marine to continental over the last ∼ 7550 years. The studied sedimentary succession recorded the upward transition from estuarine channel (until ~ 7550 cal yr BP) to estuarine central basin (>~ 7550 to ~ 5250 cal yr BP) deposits, the latter containing increased mangrove vegetation, marine and marine/brackish water diatoms. The range of geochemical values (δ13C = − 30− 10, δ15N = 2 − 8 and C/N = 440) also indicate marine/estuarine organic matter and C3 terrestrial plants to that time interval. A following period recorded two phases: lake/ria (~ 5250 to ~ 400 cal yr BP) and fluvial channel (~ 400 cal yr BP until modern age). During this stage, mangroves were replaced by trees/shrubs and herbs/grasses due to the disconnection with the marine realm. As a result, the corresponding sediments contain only organic matter sourced from freshwater and C3 terrestrial plants (δ13C = − 29− 26, δ15N = 0 − 8 and C/N = 1045). The equilibrium between fluvial sediment supply and relative sea-level changes during the Holocene controlled the morphologic and vegetation changes in the studied littoral. The estuary became established during the early Holocene as a resulted of a eustatic sea-level rise, when the fluvial sediment supply to the coast was relatively lower due to a dry period. However, during the late Holocene, the climatic force was more significant to the development of coastal morphology due to a wet period that caused an increase in sandy sediment supply to coastal system. Then, the increase of fluvial discharge associated to a relative sea-level fall caused a marine regression and shrinkage of mangroves during the late Holocene. The evaluation of mangrove dynamics according to climatic and sea-level changes mainly during the late Holocene is essential for the understanding of their survival ability under future scenarios, with a probable accelerated sea-level rise and intensification of extreme climatic events in southeastern Brazil for the next century.
AreaSRE
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > A multi-proxy evidence...
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4. Conditions of access and use
Languageen
Target FileFranca_multi.pdf
User Groupadministrator
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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
Mirror Repositoryurlib.net/www/2011/03.29.20.55
Next Higher Units8JMKD3MGPCW/3ER446E
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.44.37 1
DisseminationWEBSCI; PORTALCAPES; SCOPUS.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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