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...
Κύριοι συγγραφείς: | Schlanger, S, Arthur, M, Jenkyns, H, Scholle, P |
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Μορφή: | Journal article |
Γλώσσα: | English |
Έκδοση: |
1987
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Παρόμοια τεκμήρια
Παρόμοια τεκμήρια
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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.
ανά: Schlanger, S, κ.ά.
Έκδοση: (1987) -
STRATIGRAPHIC AND PALEO-OCEANOGRAPHIC SETTING OF ORGANIC CARBON-RICH STRATA DEPOSITED DURING CENOMANIAN-TURONIAN OCEANIC ANOXIC EVENT
ανά: Schlanger, S, κ.ά.
Έκδοση: (1983) -
The Cenomanian-Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation
ανά: Arthur, M, κ.ά.
Έκδοση: (1987) -
The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.
ανά: Arthur, M, κ.ά.
Έκδοση: (1987) -
Carbon-isotope stratigraphy recorded by the Cenomanian-Turonian Oceanic Anoxic Event: correlation and implications based on three key localities
ανά: Tsikos, H, κ.ά.
Έκδοση: (2004)