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Sedimentary patterns across the Paleocene-Eocene boundary in the Atlantic and Gulf Coastal Plains of the United States

Bulletin - Societe Belge de Geologie
By:  and 

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Abstract

Fossiliferous clay and sand belonging to calcareous nannofossil Zones NP 9 (latest Paleocene) and NP 10 (earliest Eocene) are widespread in the US Gulf and Atlantic Coastal Plains. Although the thickness of Zone NP 9-NP 10 strata is several times greater in the eastern Gulf Coastal Plain than in the Atlantic Coastal Plain, the hiatus that usually is present between these two zones in inner neritic strata is of longer duration in the Gulf Coast. Although 6 sequences are found in Zones NP 10-NP 11 in both the Atlantic and Gulf Coastal Plains, the number of sequences in each NP zone differs in the 2 areas. There is continuous deposition across the Zone NP 9-NP 10 boundary only in the northern Atlantic Coastal Plain, where middle to outer neritic deposits record the presence of several latest Paleocene (upper Zone NP 9) events that occurred at approximately 55.2 Ma.

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Publication type Article
Publication Subtype Journal Article
Title Sedimentary patterns across the Paleocene-Eocene boundary in the Atlantic and Gulf Coastal Plains of the United States
Series title Bulletin - Societe Belge de Geologie
Volume 103
Issue 3-4
Year Published 1994
Language English
Publisher Societe Belge de Geologie
Contributing office(s) Eastern Geology and Paleoclimate Science Center
Description 29 p.
First page 237
Last page 265
Country United States
Other Geospatial Atlantic Coastal Plain, Gulf Coastal Plain
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