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High resolution stratigraphy at the Cenomanian/Turonian boundary and the timing of paleoceanographic events

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6649789
The Cenomanian/Turonian (Mid-Cretaceous) boundary interval is a time of widespread deposition of organic carbon-rich sediments, marked enrichment of deltaC/sup 13/ measured in carbonates and quite dramatic plankton extinctions. Calcareous nannofossil biostratigraphy has been studied in boundary sections from Arizona, Colorado, Manitoba, DSDP Sites 549 and 551 and several sections from Italy. A consistent set of twelve first and last appearance datum levels have been determined yielding a resolution of approximately 100,000 years. This stratigraphy allows a precise comparison of the timing of the various black shale layers in DSDP and European land section and the carbon isotopic shift as observed in the Western Interior Basin. The single black shale horizons found at DSDP Sites 549 and 551 appear to be exactly contemporaneous with those at the Cismon and Monte Petrano sections of Italy. Nannofossils observed in the black shale at Site 549 indicate that it was deposited shortly prior to the carbon isotopic shift. This timing supports the conclusion of other studies that the carbon shift was a direct result of massive organic carbon removal from the oceanic system. The authors stratigraphic study also indicates that the black shales record an anoxic event in the latest Cenomanian which lasted approximately 100,000 years. The oceanic carbon reservoir, however, required three times this duration to return to its steady state.
Research Organization:
Scripps Institution of Oceanography, La Jolla, CA (USA)
OSTI ID:
6649789
Report Number(s):
CONF-8510489-
Conference Information:
Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Journal Volume: 17
Country of Publication:
United States
Language:
English