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The Schistes Carton — the Lower Toarcian of the Paris Basin
1995The Schistes Carton was deposited within an epicontinental sea during the falciferum zone (early Toarcian), during a period of approximately 500 000 years. Available data suggest that deposition occurred under oxygen-depleted conditions. These shales typically obtain thicknesses between 10 and 20 m, with maximum values in excess of 50 m. The shales are
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Global organic carbon burial during the Toarcian oceanic anoxic event: Patterns and controls
Earth-Science Reviews, 2022David B Kemp +2 more
exaly

