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Effects of an oceanic anoxic event on the stable carbon isotopic composition of Early Toarcian carbon

By J.S. Sinninghe Damsté, S. Schouten, H.M.E. van Kaam-Peters and M. Schoell

Abstract

The early Toarcian transgression is marked by the occurrence of organic carbon-rich shales in large parts of western Europe and in other parts of the world

Topics: Aardwetenschappen, organic carbon, black shale deposition, negative isotopic excursion
Year: 2000
OAI identifier: oai:dspace.library.uu.nl:1874/4290
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