The Cenomanian-Turonian Oceanic Anoxic Event, I. Stratigraphy and distribution of organic carbon-rich beds and the marine δ13C excursion
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 9...
المؤلفون الرئيسيون: | Schlanger, S, Arthur, M, Jenkyns, H, Scholle, P |
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التنسيق: | Journal article |
اللغة: | English |
منشور في: |
1987
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مواد مشابهة
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The Cenomanian-Turonian Oceanic Anoxic Event, I. Stratigraphy and distribution of organic carbon-rich beds and the Marine delta 13C excursion.
حسب: Schlanger, S, وآخرون
منشور في: (1987) -
STRATIGRAPHIC AND PALEO-OCEANOGRAPHIC SETTING OF ORGANIC CARBON-RICH STRATA DEPOSITED DURING CENOMANIAN-TURONIAN OCEANIC ANOXIC EVENT
حسب: Schlanger, S, وآخرون
منشور في: (1983) -
The Cenomanian-Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation
حسب: Arthur, M, وآخرون
منشور في: (1987) -
The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.
حسب: Arthur, M, وآخرون
منشور في: (1987) -
Carbon-isotope stratigraphy recorded by the Cenomanian-Turonian Oceanic Anoxic Event: correlation and implications based on three key localities
حسب: Tsikos, H, وآخرون
منشور في: (2004)