Integrated stratigraphy of the Paleocene-Eocene thermalmaximum in the New Jersey Coastal Plain : Toward understanding the effects of global warming in a shelf environment

@inproceedings{Stassen2012IntegratedSO,
  title={Integrated stratigraphy of the Paleocene-Eocene thermalmaximum in the New Jersey Coastal Plain : Toward understanding the effects of global warming in a shelf environment},
  author={Peter Stassen and Ellen Thomas and Robert P. Speijer},
  year={2012}
}
[1] 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 Eocene Manasquan Formation. We integrate new and published stable isotope, biostratigraphic, lithostratigraphic and ecostratigraphic records, constructing a detailed time frame for the PETM along a… CONTINUE READING
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