2015
DOI: 10.1017/s0016756814000703
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C isotopic variations in the lower–middle Frasnian (lower Upper Devonian) of the Rudny Altai

Abstract: 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 o… Show more

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Cited by 7 publications
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“…Among the many unique geological sites of the Altai, one should take note of the Devonian reefs [25,27,28]. They are covered only marginally in the famous PARED database [29], although their consideration can be important to better understand the shift from reef abundance in the Early-Middle Devonian to their decline at the Devonian-Carboniferous transition [30].…”
Section: Introductionmentioning
confidence: 99%
“…Among the many unique geological sites of the Altai, one should take note of the Devonian reefs [25,27,28]. They are covered only marginally in the famous PARED database [29], although their consideration can be important to better understand the shift from reef abundance in the Early-Middle Devonian to their decline at the Devonian-Carboniferous transition [30].…”
Section: Introductionmentioning
confidence: 99%