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Black shale deposition during Toarcian super-greenhouse driven by sea level

Abstract:

One of the most elusive aspects of the Toarcian oceanic anoxic event (T-OAE) is the paradox between carbon isotopes that indicate intense global primary productivity and organic carbon burial at a global scale, and the delayed expression of anoxia in Europe. During the earliest Toarcian, no black shales were deposited in the European epicontinental seaways, and most organic carbon enrichment of the sediments postdated the end of the overarching positive trend in the carbon isotopes that chara...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.5194/cp-9-2703-2013

Authors


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Department:
Earth Sciences
Fabrice Minoletti More by this author
Pierre Pellenard More by this author
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Grant:
NE/H015523/1
Funding agency for:
Project
Publisher:
European Geosciences Union Publisher's website
Journal:
Climate of the Past
Volume:
9
Pages:
2703-2712
Publication date:
2013-03-12
Acceptance date:
2013-05-11
DOI:
EISSN:
1814-9332
ISSN:
1814-9324
Language:
English

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