4.0 Article

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

期刊

BRAZILIAN JOURNAL OF GEOLOGY
卷 47, 期 4, 页码 693-702

出版社

SOC BRASILEIRA GEOLOGIA
DOI: 10.1590/2317-4889201720170057

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Marine Isotope Stage 3; Late Pleistocene; sea-level

资金

  1. Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [303132/2014-0]
  2. University of Sao Paulo

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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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