Integrated stratigraphy of the Paleocene-Eocene thermal maximum in the New Jersey Coastal Plain: Toward understanding the effects of globalwarming in a shelf environment

In the New Jersey Coastal Plain, a silty to clayey sedimentary unit (the Marlboro Formation) represents deposition during the Paleocene-Eocene thermal maximum (PETM). This interval is remarkably different from the glauconitic sands and silts of the underlying Paleocene Vincentown and overlying Eocen...

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Bibliographic Details
Published in:Paleoceanography
Main Authors: Stassen, P., Thomas, E.
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
ANW
USA
Online Access:https://www.vliz.be/imisdocs/publications/268925.pdf