Continental weathering and climatic changes inferred from clay mineralogy and paired carbon isotopes across the early to middle Toarcian in the Paris Basin
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 relativel...
| Main Authors: | , |
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| Format: | Journal article |
| Language: | English |
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Elsevier
2014
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