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A global event with a regional character: the Early Toarcian Oceanic Anoxic Event in the Pindos Ocean (northern Peloponnese, Greece)

Alternative title:
Toarcian Oceanic Anoxic Event in the Pindos Ocean
Abstract:

The early Toarcian (Early Jurassic, ca 183 Ma) was characterized by an Oceanic Anoxic Event (T-OAE), primarily identified by the presence of globally distributed approximately coeval black organic-rich shales. This event corresponded with relatively high marine temperatures, mass extinction, and both positive and negative carbon-isotope excursions. Because most studies of the T-OAE have taken place in northern European and Tethyan palaeogeographic domains, there is considerable controversy as...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1017/S0016756811000082

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Institution:
National University of Athens
Department:
Department of Geology and Geoenvironment
Role:
Author
More by this author
Institution:
National University of Athens
Department:
Department of Geology and Geoenvironment
Role:
Author
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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
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Institution:
Université Claude Bernard Lyon 1
Role:
Author
Publisher:
Cambridge University Press Publisher's website
Journal:
Geological Magazine Journal website
Volume:
148
Issue:
4
Pages:
619–631
Publication date:
2011-06-01
DOI:
EISSN:
1469-5081
ISSN:
0016-7568
Language:
English
Keywords:
Subjects:
UUID:
uuid:86f3ce50-9371-470b-a924-c5e27012e1e9
Local pid:
ora:6579
Deposit date:
2012-11-26

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