Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast

Detalhes bibliográficos
Autor(a) principal: Salvaterra,André da Silva
Data de Publicação: 2017
Outros Autores: Santos,Rosangela Felício dos, Salaroli,Alexandre Barbosa, Figueira,Rubens Cesar Lopes, Mahiques,Michel Michaelovitch de
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Brazilian Journal of Geology
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000400693
Resumo: ABSTRACT: In this paper, we present new evidence regarding a Marine Isotope Stage 3 (MIS3) transgression on the south-eastern Brazilian coast (Baixada Santista coastal plain). Data collected from a Standard Penetration Test (SPT) drilling reveal the occurrence of myxohaline sediments between cal BP 45,000 and 41,000. A deeper sequence, which shows a clear transition from terrestrial to a myxohaline environment, was associated with MIS5e. Organic and inorganic proxies have been used to recognize the variations on the terrestrial/myxohaline/marine deposits, as well as to infer about climate and energy of the depositional environment. Environmental change, which could correspond to a sea-level peak or the occurrence of drier conditions, was recognized between 43,000 and 42,000 cal BP. The results reinforce the need for future works on MIS3 variability on the South American Atlantic coast.
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spelling Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coastMarine Isotope Stage 3Late Pleistocenesea-levelABSTRACT: In this paper, we present new evidence regarding a Marine Isotope Stage 3 (MIS3) transgression on the south-eastern Brazilian coast (Baixada Santista coastal plain). Data collected from a Standard Penetration Test (SPT) drilling reveal the occurrence of myxohaline sediments between cal BP 45,000 and 41,000. A deeper sequence, which shows a clear transition from terrestrial to a myxohaline environment, was associated with MIS5e. Organic and inorganic proxies have been used to recognize the variations on the terrestrial/myxohaline/marine deposits, as well as to infer about climate and energy of the depositional environment. Environmental change, which could correspond to a sea-level peak or the occurrence of drier conditions, was recognized between 43,000 and 42,000 cal BP. The results reinforce the need for future works on MIS3 variability on the South American Atlantic coast.Sociedade Brasileira de Geologia2017-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000400693Brazilian Journal of Geology v.47 n.4 2017reponame:Brazilian Journal of Geologyinstname:Sociedade Brasileira de Geologia (SBGEO)instacron:SBGEO10.1590/2317-4889201720170057info:eu-repo/semantics/openAccessSalvaterra,André da SilvaSantos,Rosangela Felício dosSalaroli,Alexandre BarbosaFigueira,Rubens Cesar LopesMahiques,Michel Michaelovitch deeng2017-12-19T00:00:00Zoai:scielo:S2317-48892017000400693Revistahttp://bjg.siteoficial.ws/index.htmhttps://old.scielo.br/oai/scielo-oai.phpsbgsede@sbgeo.org.br||claudio.riccomini@gmail.com2317-46922317-4692opendoar:2017-12-19T00:00Brazilian Journal of Geology - Sociedade Brasileira de Geologia (SBGEO)false
dc.title.none.fl_str_mv Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
title Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
spellingShingle Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
Salvaterra,André da Silva
Marine Isotope Stage 3
Late Pleistocene
sea-level
title_short Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
title_full Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
title_fullStr Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
title_full_unstemmed Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
title_sort Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
author Salvaterra,André da Silva
author_facet Salvaterra,André da Silva
Santos,Rosangela Felício dos
Salaroli,Alexandre Barbosa
Figueira,Rubens Cesar Lopes
Mahiques,Michel Michaelovitch de
author_role author
author2 Santos,Rosangela Felício dos
Salaroli,Alexandre Barbosa
Figueira,Rubens Cesar Lopes
Mahiques,Michel Michaelovitch de
author2_role author
author
author
author
dc.contributor.author.fl_str_mv Salvaterra,André da Silva
Santos,Rosangela Felício dos
Salaroli,Alexandre Barbosa
Figueira,Rubens Cesar Lopes
Mahiques,Michel Michaelovitch de
dc.subject.por.fl_str_mv Marine Isotope Stage 3
Late Pleistocene
sea-level
topic Marine Isotope Stage 3
Late Pleistocene
sea-level
description ABSTRACT: In this paper, we present new evidence regarding a Marine Isotope Stage 3 (MIS3) transgression on the south-eastern Brazilian coast (Baixada Santista coastal plain). Data collected from a Standard Penetration Test (SPT) drilling reveal the occurrence of myxohaline sediments between cal BP 45,000 and 41,000. A deeper sequence, which shows a clear transition from terrestrial to a myxohaline environment, was associated with MIS5e. Organic and inorganic proxies have been used to recognize the variations on the terrestrial/myxohaline/marine deposits, as well as to infer about climate and energy of the depositional environment. Environmental change, which could correspond to a sea-level peak or the occurrence of drier conditions, was recognized between 43,000 and 42,000 cal BP. The results reinforce the need for future works on MIS3 variability on the South American Atlantic coast.
publishDate 2017
dc.date.none.fl_str_mv 2017-12-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000400693
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892017000400693
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/2317-4889201720170057
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv Sociedade Brasileira de Geologia
publisher.none.fl_str_mv Sociedade Brasileira de Geologia
dc.source.none.fl_str_mv Brazilian Journal of Geology v.47 n.4 2017
reponame:Brazilian Journal of Geology
instname:Sociedade Brasileira de Geologia (SBGEO)
instacron:SBGEO
instname_str Sociedade Brasileira de Geologia (SBGEO)
instacron_str SBGEO
institution SBGEO
reponame_str Brazilian Journal of Geology
collection Brazilian Journal of Geology
repository.name.fl_str_mv Brazilian Journal of Geology - Sociedade Brasileira de Geologia (SBGEO)
repository.mail.fl_str_mv sbgsede@sbgeo.org.br||claudio.riccomini@gmail.com
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