C isotopic variations in the lower-middle Frasnian (lower Upper Devonian) of the Rudny Altai
2015
We conducted isotope–geochemical studies of the Upper Devonian of the Rudny Altai.
Whole-rock carbon isotope analyses of the studied section represented by carbonate
fore-reef facies reveal a negative excursion at the base of punctata Zone. When compared to conodont biofacies turnovers and the Upper Devonian events chart,
the new data have demonstrated a synchronism between the negative excursion and the coeval
decline in conodont biodiversity corresponding to the Middlesex anoxic event of the
Frasnian Stage of the Upper Devonian.
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