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Continental weathering and climatic changes inferred from clay mineralogy and paired carbon isotopes across the early to middle Toarcian in the Paris Basin

Abstract:

Lower Toarcian strata (Lower Jurassic) have been extensively studied with a view to understanding the oceanographic, climatic and biological processes that drove the Earth’s system into an Oceanic Anoxic Event (OAE). For this time period, the evolution of the European marine seaways is now relatively well constrained owing to multiple geochemical studies, but investigations regarding climatic trends in the continental realm remain sparse. In the present study, we test the clay mineralogy as a...

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Publication status:
Published
Peer review status:
Peer reviewed
Version:
Author's Original

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Publisher copy:
10.1016/j.palaeo.2014.02.007

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Institution:
University of Oxford
Department:
Mathematical,Physical & Life Sciences Division
Role:
Author
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Institution:
Université de Bourgogne
Role:
Author
Publisher:
Elsevier B.V. Publisher's website
Journal:
Palaeogeography, Palaeoclimatology, Palaeoecology Journal website
Volume:
399
Pages:
385-393
Publication date:
2014-04-05
DOI:
ISSN:
0031-0182
URN:
uuid:9422efde-caab-46da-8998-e3b4f56d5040
Local pid:
ora:8564

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