STABLE CARBON ISOTOPE (Δ13CCARB AND Δ13CORG) EVIDENCE OF THE TOARCIAN OCEAN ANOXIC EVENT FROM CENTRAL ITALY: EVIDENCE FOR A GLOBALLY MIXED TETHYS SEA.
We sampled 28 lime mudstone hand samples from the Marne Del Monte Serrone Formation of the Colle d'Orlando section in central Italy (Umbria region) to identify whether the T-OAE is preserved in these rocks. This 65-m-thick measured section comprises marly limestone and shale facies, with a thin (<30-cm-thick) black shale preserved in the lower part of the measured interval. Bulk carbonate (δ13Ccarb) and bulk organic matter (δ13Corg) were sampled for chemostratigraphic correlation as the palaeontologic record here is not well constrained. Hand samples were drilled on fresh surfaces to obtain sufficient powder for isotopic analysis. We observe a clearly defined δ13Ccarb increase from 0‰ to ~3.5‰. However, the δ13Corg record is less clearly defined, but δ13Corg values increase from ~ -30‰ to -26‰ at the peak of the excursion. The magnitudes of these results are similar to published studies, suggesting that these sections deposited in well-connected basins that were able to freely exchange with the global reservoir. Future work will analyze the same samples to generate a sulfur isotopic record, from carbonate-associated sulfate and pyrite, to better characterize the global to regional expression of this geochemical perturbation.