Intermittent anoxia : reconciliation of a Jurassic black shale with its biofacies

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Intermittent anoxia : reconciliation of a Jurassic black shale with its biofacies
 
Sinninghe Damsté, J.S.; Kenig, F.; Hudson, J.; Popp, B.N.
(2004) Geology, volume 32, issue 5, pp. 421 - 424
(Article)
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.
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Keywords: Green sulfur bacteria, Biofacies, Oxford Clay Formation, Anoxia, Isorenieratane, Peterborough Member
DOI: https://doi.org/10.1130/G20356.1
ISSN: 0091-7613
Publisher: Geological Society of America
 
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