Chronostratigraphy of the Cheremoshnik key section (Yaroslavl Volga region) based on new geochronological, palynological, and paleosol data


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Resumo

According to radiochemical and biostratigraphic studies of the buried peat layer in the Cheremoshnik key section on the East European plain, the first age dating of this peat was obtained and its assignment to the Mikulino interglacial was confirmed. The Th/U isotope age data obtained for the peat horizon allow us to state with confidence that it was formed during the MIS5e. It was found that a variety of signs, including the lithological characteristics of dated layers and climatic indexes, is evidence that the Cheremoshnik site and Borisoglebsk upland occurred in the periglacial zone during MIS3–MIS2.

Sobre autores

A. Rusakov

Institute of Earth Sciences

Autor responsável pela correspondência
Email: a.rusakov@spbu.ru
Rússia, St. Petersburg

A. Nikonov

Institute of Physics of the Earth

Email: a.rusakov@spbu.ru
Rússia, Moscow, 123995

L. Savelieva

Institute of Earth Sciences

Email: a.rusakov@spbu.ru
Rússia, St. Petersburg

A. Simakova

Geological Institute

Email: a.rusakov@spbu.ru
Rússia, Moscow, 109017

F. Maksimov

Institute of Earth Sciences

Email: a.rusakov@spbu.ru
Rússia, St. Petersburg

V. Kuznetsov

Institute of Earth Sciences

Email: a.rusakov@spbu.ru
Rússia, St. Petersburg

M. Korkka

Institute of Earth Sciences

Email: a.rusakov@spbu.ru
Rússia, St. Petersburg

V. Savenko

Institute of Earth Sciences

Email: a.rusakov@spbu.ru
Rússia, St. Petersburg

A. Starikova

Institute of Earth Sciences

Email: a.rusakov@spbu.ru
Rússia, St. Petersburg


Declaração de direitos autorais © Pleiades Publishing, Ltd., 2017

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