Glendonites in the Aptian Stage (Lower Cretaceous) of Western Siberia

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Resumo

The first occurrence of glendonite (calcite pseudomorph after cold-water mineral ikaite) was described from the Aptian Stage (Tanopcha Formation) of Western Siberia. The review of Aptian-Albian glendonite record in other regions of the world is provided, and the significance of these occurrences for clarifying the climate of the terminal part of the Early Cretaceous is discussed. Aptian glendonites from the North-East of Russia are figured.

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Sobre autores

M. Rogov

Geological Institute of the Russian Academy of Sciences; Saint-Petersburg State University

Email: rogov@ginras.ru
Moscow, Russia; Saint-Petersburg, Russia

A. Fedorova

Saint-Petersburg branch of All-Russian Research Geological Oil Institute

Email: rogov@ginras.ru
Saint-Petersburg, Russia

O. Kochubey

Saint-Petersburg branch of All-Russian Research Geological Oil Institute

Email: rogov@ginras.ru
Saint-Petersburg, Russia

K. Vasileva

Geological Institute of the Russian Academy of Sciences; Saint-Petersburg State University

Email: rogov@ginras.ru
Moscow, Russia; Saint-Petersburg, Russia

I. Panchenko

Geological Institute of the Russian Academy of Sciences; JSC MiMGO

Email: rogov@ginras.ru
Moscow, Russia; Moscow, Russia

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