Biomarker and compound-specific isotope records across the Toarcian CIE at the Dormettingen section in SW Germany
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The Toarcian oceanic anoxic event (T-OAE) is associated with a prominent negative carbon isotope excursion (CIE; ~ 183 million years (Myr)). About 10-m-thick organic matter-rich sediments accumulated during the T-OAE in the Southwest German Basin (SWGB). Rock-... ...
