Effects of an oceanic anoxic event on the stable carbon isotopic composition of Early Toarcian carbon
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Publication date
2000
Authors
Sinninghe Damsté, J.S.
Schouten, S.
Kaam-Peters, H.M.E. van
Schoell, M.
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Document Type
Article
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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.
Keywords
organic carbon, black shale deposition, negative isotopic excursion