Evidence for rapid climate change in North America during the latest Paleocene thermal maximum: oxygen isotope compositions of biogenic phosphate from the Bighorn Basin (Wyoming)-Reference-Cited by-同舟云学术

Evidence for rapid climate change in North America during the latest Paleocene thermal maximum: oxygen isotope compositions of biogenic phosphate from the Bighorn Basin (Wyoming)

Published:1998-07 Issue:1-2 Volume:160 Page:193-208
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Fricke Henry C.,Clyde William C.,O'Neil James R.,Gingerich Philip D.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference43 articles.

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5. L.D. Stott, A. Sinha, M. Thiry, M.P. Aubry, W.A. Bergen, 1996. The transfer of 13C changes from the ocean to the terrestrial biosphere across the Paleocene/Eocene boundary: criteria for terrestrial–marine correlations, in: R.W.O. Knox, R.M. Corfield and R.E. Dunay (Eds.), Correlations of the Early Paleogene in Northwest Europe. Geol. Soc. London Spec. Publ., pp. 381–399.

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