Discovery of shallow-marine biofacies conodonts in a bioherm within the Carboniferous-Permian transition in the Omolon Massif, NE Russia near the North paleo-pole: Correlation with a warming spike in the southern hemisphere - «Национальный агрегатор открытых репозиториев российских университетов» (НОРА)

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Discovery of shallow-marine biofacies conodonts in a bioherm within the Carboniferous-Permian transition in the Omolon Massif, NE Russia near the North paleo-pole: Correlation with a warming spike in the southern hemisphere

Davydov V., Biakov A.

Дата публикации: 2014

Дата публикации в реестре: 2020-03-01T01:08:49Z

Аннотация:

Ключевые слова:
Conodonts, NE Russia, Omolon Massif, Shelly fauna, Uppermost Carboniferous to Permian transition, Warming event

Тип: Article in Press

Источник: SCOPUS1342937X-2014-SID84906650122

Другие версии документа

Discovery of shallow-marine biofacies conodonts in a bioherm within the Carboniferous-Permian transition in the Omolon Massif, NE Russia near the North paleo-pole: Correlation with a warming spike in the southern hemisphere Discovery of shallow-marine biofacies conodonts in a bioherm within the Carboniferous-Permian transition in the Omolon Massif, NE Russia near the North paleo-pole: Correlation with a warming spike in the southern hemisphere Discovery of shallow-marine biofacies conodonts in a bioherm within the Carboniferous-Permian transition in the Omolon Massif, NE Russia near the North paleo-pole: Correlation with a warming spike in the southern hemisphere

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