Evidence of an Marine Isotope Stage 3 transgression at the Baixada Santista, south-eastern Brazilian coast
Autor(a) principal: | |
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Data de Publicação: | 2017 |
Outros Autores: | , , , |
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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Brazilian Journal of Geology |
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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 |
_version_ |
1752122398822367232 |