The upper Bajocian of the Crimean Mountains: Paleogeography and sedimentation conditions from palynological data


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Abstract

Based on the spore-pollen data, the mineral composition of clay rocks, analyzed structures and facies, and a general paleogeographic analysis, the sedimentation conditions and landscapes of islands located during the Late Bajocian in the region of the present-day the Crimean Mountains have been reconstructed. It is shown that the sublatitudinally elongated insular land zone had a width of 30 km, the heights of the islands were no more than 1 km, with steep mudflow-affected northern slopes and with an extensive river system on the southern slopes.

About the authors

J. I. Rostovceva

Department of Geology

Author for correspondence.
Email: paleopen@mail.ru
Russian Federation, Moscow

A. N. Stafeev

Department of Geology

Email: paleopen@mail.ru
Russian Federation, Moscow

T. V. Sukhanova

Department of Geology

Email: paleopen@mail.ru
Russian Federation, Moscow

I. V. Latysheva

Geological Institute of the Russian Academy of Sciences

Email: paleopen@mail.ru
Russian Federation, Moscow

V. L. Kosorukov

Department of Geology

Email: paleopen@mail.ru
Russian Federation, Moscow

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