Intermittent anoxia : reconciliation of a Jurassic black shale with its biofacies
Publication date
2004
Authors
Sinninghe Damsté, J.S.
Kenig, F.
Hudson, J.
Popp, B.N.
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Document Type
Article
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Abstract
Isorenieratane is ubiquitous in the organic, carbon-rich Peterborough Member (Callovian, UK) of the Oxford Clay Formation, indicating a temporal overlap of the euphotic and sulphidic zone in the water column.
Keywords
Green sulfur bacteria, Biofacies, Oxford Clay Formation, Anoxia, Isorenieratane, Peterborough Member