Journal article icon

Journal article

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 ...

Expand abstract
Publication status:
Published
Peer review status:
Peer reviewed
Version:
Publisher version

Actions


Access Document


Files:

Authors


More by this author
Institution:
University of Oxford
Department:
Oxford, MPLS, 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
URN:
uuid:0921605b-4793-43df-889d-7b896790de62
Source identifiers:
81969
Local pid:
pubs:81969

Terms of use


Metrics


Views and Downloads






If you are the owner of this record, you can report an update to it here: Report update to this record

TO TOP