Cretaceous Oceanic Anoxic Events: Causes and Consequences
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 deposit...
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| Format: | Journal article |
| Language: | English |
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Netherlands Journal of Geosciences Foundation
1976
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