Journal article
The Cenomanian-Turonian Oceanic Anoxic Event, I. Stratigraphy and distribution of organic carbon-rich beds and the marine δ13C excursion
- Abstract:
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Marine strata deposited during late Cenomanian and early Turonian time display lithological, faunal, and geochemical characteristics which indicate that significant parts of the world ocean were periodically oxygen deficient. At, or very close to, the Cenomanian-Turonian boundary, between 90.5 and 91.5 million years ago, oxygen deficiencies were particularly marked over a period of less than 1 my. This short-lived episode of oceanic oxygen deficiency has been termed the Cenomanian-Turonian 'O...
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Authors
- Journal:
- Geological Society Special Publication More from this journal
- Volume:
- 26
- Issue:
- 1
- Pages:
- 371-399
- Publication date:
- 1987-01-01
- DOI:
- ISSN:
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0305-8719
- Language:
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English
- Pubs id:
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pubs:205612
- UUID:
-
uuid:c27e7cfc-71e4-43b6-be8b-0fd1b9db86a7
- Local pid:
-
pubs:205612
- Source identifiers:
-
205612
- Deposit date:
-
2012-12-19
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- Copyright date:
- 1987
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