Paleocirculation of the southwestern Atlantic.

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Abstract

The Cenozoic history of the abyssal circulation of the SW Atlantic is punctuated by tectonically or climatically controlled 'threshold' events, triggered by the changing geophysical boundary conditions associated with plate tectonic development of the basins.-from Author

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APA

Johnson, D. A. (1983). Paleocirculation of the southwestern Atlantic. Initial Reports DSDP, Leg 72, Santos, Brazil, 977–994. https://doi.org/10.2973/dsdp.proc.72.152.1983

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