Paleoceanographic Model of Neogene Phosphorite Deposition, U.S. Atlantic Continental Margin

The Neogene stratigraphic section of the southeastern U.S. continental shelf-coastal plain system is characterized by (i) a series of major regional phosphogenic episodes; (ii) a strong spatial relationship between the structural or topographic framework and phosphate deposition; and (iii) distinct...

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Bibliographic Details
Published in:Science (American Association for the Advancement of Science) Vol. 223; no. 4632; pp. 123 - 131
Main Author: Riggs, Stanley R.
Format: Journal Article
Language:English
Published: United States The American Association for the Advancement of Science 13-01-1984
American Association for the Advancement of Science
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Summary:The Neogene stratigraphic section of the southeastern U.S. continental shelf-coastal plain system is characterized by (i) a series of major regional phosphogenic episodes; (ii) a strong spatial relationship between the structural or topographic framework and phosphate deposition; and (iii) distinct cyclical and regional patterns of deposition of the terrigenous, carbonate, and phosphate lithofacies. The complex depositional patterns are explained by a paleoceanographic model based upon the interaction of glacial eustatic sea-level fluctuations, associated changes in climate, and the dynamics of the Gulf Stream in response to the bathymetric configurations of the continental margin during the past 20 million years.
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ISSN:0036-8075
1095-9203
DOI:10.1126/science.223.4632.123