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-Reference-Cited by-同舟云学术

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

Published:2015-09 Issue:2 Volume:28 Page:888-897
ISSN:1342-937X
Container-title:Gondwana Research
language:en
Short-container-title:Gondwana Research

Author:

Davydov Vladimir I.,Biakov Alexander S.

Funder

NSF

Russian Foundation for Basic Research

Publisher

Elsevier BV

Subject

Geology

Reference67 articles.

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4. Permian rock sequences of the Balygychan Uplift;Biakov,2004

5. Permian bivalve mollusks of Northeast Asia;Biakov;Journal of Asian Earth Sciences,2006

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