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...
Հիմնական հեղինակներ: | Schlanger, S, Arthur, M, Jenkyns, H, Scholle, P |
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Ձևաչափ: | Journal article |
Լեզու: | English |
Հրապարակվել է: |
1987
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Նմանատիպ նյութեր
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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.
: Schlanger, S, և այլն
Հրապարակվել է: (1987) -
STRATIGRAPHIC AND PALEO-OCEANOGRAPHIC SETTING OF ORGANIC CARBON-RICH STRATA DEPOSITED DURING CENOMANIAN-TURONIAN OCEANIC ANOXIC EVENT
: Schlanger, S, և այլն
Հրապարակվել է: (1983) -
The Cenomanian-Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation
: Arthur, M, և այլն
Հրապարակվել է: (1987) -
The Cenomanian- Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organic-matter production and preservation.
: Arthur, M, և այլն
Հրապարակվել է: (1987) -
Carbon-isotope stratigraphy recorded by the Cenomanian-Turonian Oceanic Anoxic Event: correlation and implications based on three key localities
: Tsikos, H, և այլն
Հրապարակվել է: (2004)