The Cenomanian-Turonian Oceanic Anoxic Event, I. Stratigraphy and distribution of organic carbon-rich beds and the marine δ13C excursion

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...

תיאור מלא

מידע ביבליוגרפי
Main Authors:	Schlanger, S, Arthur, M, Jenkyns, H, Scholle, P
פורמט:	Journal article
שפה:	English
יצא לאור:	1987

פריטים דומים

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