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Molybdenum-isotope chemostratigraphy and paleoceanography of the Toarcian Oceanic Anoxic Event (Early Jurassic)

Abstract:

Molybdenum (Mo)-isotope chemostratigraphy of organic-rich mudrocks has been a valuable tool for testing the hypothesis that the Toarcian Oceanic Anoxic Event (T-OAE, Early Jurassic, ~183 Ma) was characterized by the spread of marine euxinia (and organic-matter burial) at a global scale. However, the interpretation of existing Mo-isotope data for the T-OAE (from Yorkshire, Cleveland Basin, U.K.) is equivocal. In this study, three new Mo-isotope profiles are presented: from Dotternhausen Quarry...

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Publication status:
Published
Peer review status:
Peer reviewed
Version:
Publisher's version

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Publisher copy:
10.1002/2016PA003048

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Department:
Oxford, MPLS, Earth Sciences
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Department:
Oxford, MPLS, Earth Sciences
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Department:
Oxford, MPLS, Earth Sciences
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Department:
Oxford, MPLS, Earth Sciences
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Shell Global Solutions International B.V. More from this funder
Publisher:
American Geophysical Union Publisher's website
Journal:
Paleoceanography Journal website
Volume:
32
Issue:
8
Pages:
813-829
Publication date:
2017-06-27
Acceptance date:
2017-06-22
DOI:
EISSN:
1944-9186
ISSN:
0883-8305
Pubs id:
pubs:701828
URN:
uri:2032bbb2-12df-4d83-956c-1110d388af55
UUID:
uuid:2032bbb2-12df-4d83-956c-1110d388af55
Local pid:
pubs:701828

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