Middle Jurassic continental biota and paleolandscape in the Dubinino locality (Sharypovo area, Krasnoyarsk krai)


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Abstract

On the basis of the lithological-facies analysis, it was established that deposits of the Upper Itat Subformation, comprising the Dubinino locality of the Middle Jurassic flora and insects (Sharypovo district, Krasnoyarsk krai), accumulated in alluvial and lacustrine and, to a lesser extent, floodplain environments (floodplain and alluvial fan facies). The occurrence of remains of insects, macroremains of flora, spores, and pollen allowed us to make a paleoreconstruction of an area with a strongly dissected relief: continental fresh-water reservoir (lake) with varying degree of overflow, surrounded by hills covered with gymnospermous and ginkgo forests.

About the authors

S. V. Ivantsov

Tomsk State University

Author for correspondence.
Email: stepan_ivantsov@mail.ru
Russian Federation, pr. Lenina 36, Tomsk, 634050

L. I. Bystritskaya

Tomsk State University

Email: stepan_ivantsov@mail.ru
Russian Federation, pr. Lenina 36, Tomsk, 634050

S. A. Krasnolutskii

Sharypovo Museum of History and Regional Studies

Email: stepan_ivantsov@mail.ru
Russian Federation, mkr. 6, Sharypovo, Krasnoyarsk Krai, 662320

K. P. Lyalyuk

Tomsk State University

Email: stepan_ivantsov@mail.ru
Russian Federation, pr. Lenina 36, Tomsk, 634050

A. O. Frolov

Institute of the Earth’s Crust, Siberian Branch

Email: stepan_ivantsov@mail.ru
Russian Federation, ul. Lermontova 128, Irkutsk, 664033

A. S. Alekseev

Tomsk State University

Email: stepan_ivantsov@mail.ru
Russian Federation, pr. Lenina 36, Tomsk, 634050

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