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Cretaceous Oceanic Anoxic Events: Causes and Consequences

Abstract:

Organic carbon-rich sediments are globally developed in pelagic sedimentary sequences of Aptian-Albian and Cenomanian-Turonian age. They formed in a variety of paleo-bathymetric settings including oceanic plateaus and basins, continental margins and shelf seas. The widespread nature of these deposits suggests that they were not strictly controlled by local basin geometry but were a product of ″Oceanic Anoxic Events″ . Interpretation of these events as the result of the interplay of two major ...

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Publication status:
Published
Peer review status:
Peer reviewed

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Publisher:
Netherlands Journal of Geosciences Foundation Publisher's website
Journal:
Geologie en Mijnbouw Journal website
Volume:
55
Issue:
3-4
Pages:
179-184
Publication date:
1976-01-01
Source identifiers:
81969
Language:
English
Keywords:
Subjects:
UUID:
uuid:0921605b-4793-43df-889d-7b896790de62
Local pid:
pubs:81969
Deposit date:
2012-12-19

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