Benthic foraminifera and Neogene sea level changes in the Pelotas Basin, offshore south Brazil
Author:
Affiliation:
1. Cedar Lodge, UK; The University of the West Indies, Trinidad and Tobago
2. Universidade Federal do Rio Grande do Sul, Brasil
3. Smithsonian Institution, USA
Publisher
FapUNIFESP (SciELO)
Subject
Water Science and Technology,Aquatic Science,Oceanography
Link
http://www.scielo.br/pdf/ocr/v68/2675-2824-ocr-68-e20333.pdf
Reference42 articles.
1. Scaling percentages and distributional patterns of benthic foraminifera with flux rates of organic carbon;ALTENBACH A. V.;Journal of Foraminiferal Research,1999
2. Strontium isotope stratigraphy of the Pelotas Basin;ANJOS-ZERFASS G. S.;Brazilian Journal of Geology,2014
3. Cenozoic synthem stratigraphic architecture of the SE Brazilian shelf and its global eustatic context: evidence from the Pelotas Basin (offshore Brazil);ANJOS-ZERFASS G. S.;Geologos,2013
4. Bioestratigraphia (Foraminiferida) de Sondagem 1-SCS-3B, Plataforma de Florianopolis, Bacia de Pelotas, Brasil;ANJOS G. S.;Revista Brasileira de Paleontologia,2004
5. Widespread Miocene deep-sea hiatuses: Coincidence with periods of global cooling;BARRON J. A.;Geology,1982
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