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New data on the Middle Quaternary peat bogs in the Pechora River basin

https://doi.org/10.52349/0869-7892_2024_97_41-60

Abstract

The supposed marine nature of authigenic gypsum mineralization, first discovered on exposed dry surfaces of the Middle Quaternary peat bogs, and on the woody debris contained in them, is discussed. Peat bogs protrude from the lower part of the erosional cliffs on the Pechora River near the village Rodionovo, on the Vertny River (right tributary of the Pechora River), and in the Lodmashchelya area on the Seyda River (tributary of the Usa River). The similarity of «paleogypsum» with gypsum grown on modern wood that has been in the sea for a long time allows us to assert that sea water is conserved in peat bogs. Lists of flora and beetles first discovered in the Lodmashchelya peat bog are provided.

About the Authors

V. A. Zharkov
Interdepartmental Stratigraphic Committee, Commission on the Neogene System (ISC)
Russian Federation

Zharkov Vladimir Arsenievich – Mining Engineer-geologist

Syktyvkar, Komi Republic, 167000



E. V. Zinoviev
Institute of Plant and Animal Ecology of the Ural Branch of the Russian Academy of Sciences (IPAE UB RAS)
Russian Federation

Zinoviev Evgeniy Vitalievich – Doctor of Biological Sciences, Leading Researcher

202 Ul. 8 Marta, Ekaterinburg, 620144



A. S. Shuyskiy
Institute of Geology of Komi Science Centre of the Ural Branch of the Russian Academy of Sciences (IG Komi SC UB RAS)
Russian Federation

Shuyskiy Alexandr Sergeevich – Junior Researcher

54 Ul. Pervomayskaya, Syktyvkar, Komi Republic, 167982



T. V. Yakubovskaya
Institute of Geology of the «Research and Production Center for Geology» (IG «RPC for Geology»)
Belarus

Yakubovskaya Tatiana Vasilievna – Candidate of Geological and Mineralogical Sciences, Associate Professor, Leading Researcher

7 Ul. Akademika Kuprevicha, Minsk, 220141



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Review

For citations:


Zharkov V.A., Zinoviev E.V., Shuyskiy A.S., Yakubovskaya T.V. New data on the Middle Quaternary peat bogs in the Pechora River basin. Regional Geology and Metallogeny. 2024;(97):41-60. (In Russ.) https://doi.org/10.52349/0869-7892_2024_97_41-60

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