THE SOUTHERN BRAZILIAN SHELF: GENERAL CHARACTERISTICS, QUATERNARY EVOLUTION AND SEDIMENT DISTRIBUTION


Autoria(s): MAHIQUES, Michel Michaelovitch de; SOUSA, Silvia Helena de Mello e; FURTADO, Valdenir Veronese; TESSLER, Moyses Gonsalez; TOLEDO, Felipe Antonio de Lima; BURONE, Leticia; FIGUEIRA, Rubens Cesar Lopes; KLEIN, Daniel Andreas; MARTINS, Cristina Celia; ALVES, Daniel Pavani Vicente
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

20/10/2012

20/10/2012

2010

Resumo

Extending from latitude 34 degrees S to 22 degrees S the Southern Brazilian shelf constitutes the only part of the Brazilian shelf with a subtropical to temperate environment. The studies on the different geological aspects of the area began in the 1960`s and have recently been reassessed after studies related to the determination of the Economic Exclusive Zone. In terms of morphology, the Southern Brazilian shelf may be divided into three sectors, the Sao Paulo Bight, the Florianopolis-Mostardas Sector and the Rio Grande Cone, characterized by conspicuous differences in terms of geological determining factors, bathymetry, declivities and the presence of canyons and channels. Despite the existence of hundreds of radiocarbon datings the sea level changes curve of southern Brazil during the Last Glacial Cycle is still a matter of debate. A recent controversy on the Middle and late Holocene sea level changes curve raised the question of the amplitude of the oscillations which occurred in the period. Also, a few but relatively consistent radiocarbon datings suggest the occurrence of a high sea level during Isotope Stage 3. In terms of sedimentary cover the Southern Brazilian shelf exhibits a very strong hydrodynamic control, both latitudinal and bathymetrical. The sector southward from 25 degrees S is characterized by the influence of the plume of water carrying sediments originating from the Rio de La Plata. Actually its presence is conspicuous up to 28 degrees S, with the area between this latitude and 25 degrees S constituting a transitional zone. In terms of bathymetry the outer shelf is marked by the ""floor-polisher"" effect of the Brazil Current, which is responsible for the maintenance of a relict facies in areas deeper than 100 meters.

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Fundacao de Amparo a Pesquisa do Estado de Sao Paulo (Fapesp)

Conselho de Desenvolvimento Cientifico e Tecnologico (CNPq)

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Identificador

BRAZILIAN JOURNAL OF OCEANOGRAPHY, v.58, Special Issue, p.25-34, 2010

1679-8759

http://producao.usp.br/handle/BDPI/30336

http://apps.isiknowledge.com/InboundService.do?Func=Frame&product=WOS&action=retrieve&SrcApp=EndNote&UT=000281689400004&Init=Yes&SrcAuth=ResearchSoft&mode=FullRecord

Idioma(s)

eng

Publicador

INST OCEANOGRAFICO, UNIV SAO PAULO

Relação

Brazilian Journal of Oceanography

Direitos

closedAccess

Copyright INST OCEANOGRAFICO, UNIV SAO PAULO

Palavras-Chave #Continental shelf #Sedimentation #Sea level changes #Last glacial cycle #SEA-LEVEL CURVES #CANANEIA REGIONS #HOLOCENE #EASTERN #PARANAGUA #EMPHASIS #STATE #Marine & Freshwater Biology #Oceanography
Tipo

article

original article

publishedVersion