Seawater redox variations during the deposition of the Kimmeridge Clay Formation, United Kingdom (Upper Jurassic): Evidence from molybdenum isotopes and trace metal ratios-Reference-Cited by-同舟云学术

Seawater redox variations during the deposition of the Kimmeridge Clay Formation, United Kingdom (Upper Jurassic): Evidence from molybdenum isotopes and trace metal ratios

Published:2010-11-12 Issue:4 Volume:25 Page:n/a-n/a
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Pearce Christopher R.¹,Coe Angela L.¹,Cohen Anthony S.¹

Affiliation:

1. Department of Earth and Environmental Sciences, Centre for Earth, Planetary, Space and Astronomical Research; Open University; Walton Hall, Milton Keynes UK

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://www.agu.org/journals/pa/pa1004/2010PA001963/2010PA001963.pdf

Reference83 articles.

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3. Geol. Soc. Spec. Publ.;Ahmadi,1998

4. Can marine anoxic events draw down the trace element inventory of seawater?;Algeo;Geology,2004

5. Mo-total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and palaeohydrographic conditions;Algeo;Paleoceanography,2006

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