MAGNETO-MINERALOGICAL ANOMALIES AT THE PLEISTOCENE-HOLOCENE BOUNDARY IN LAKE SEDIMENTS OF NORTHEASTERN RUSSIA

P. S. Minyuk; Минюк П. С.; D. K. Pozhidaeva; Пожидаева Д. К.; O. T. Sotskaya; Соцкая О. Т.; V. V. Akinin; Акинин В. В.; M. A. Morozova; Морозова М. А.

doi:10.31857/S2686739723600182

MAGNETO-MINERALOGICAL ANOMALIES AT THE PLEISTOCENE-HOLOCENE BOUNDARY IN LAKE SEDIMENTS OF NORTHEASTERN RUSSIA

Authors: Minyuk P.S.¹, Pozhidaeva D.K.¹, Sotskaya O.T.¹, Akinin V.V.¹, Morozova M.A.¹
Affiliations:
1. N.A. Shilo North-East Interdisciplinary Scientific Research Institute, Far-Eastern Branch of the Russian Academy of Sciences
Issue: Vol 510, No 2 (2023)
Pages: 194-200
Section: LITHOLOGY
Submitted: 14.10.2023
Published: 01.06.2023
URL: https://bakhtiniada.ru/2686-7397/article/view/135774
DOI: https://doi.org/10.31857/S2686739723600182
EDN: https://elibrary.ru/UKKFMJ
ID: 135774

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Abstract

The results of the study of lake sediments in the North-East of Russia are presented. The reasons for the abnormally high values of magnetic susceptibility in the transition layers from the Late Pleistocene to the Holocene are considered. The magnetic fraction of Lake Grand sediments is represented by detrital titanomagnetites and magnetites. In the sediments of the Gryazevoye, Sosednee, Vodorazdelnoye, and Sapog lakes, high values of magnetic susceptibility are due to autigenic iron sulfides, mainly greigite. The data obtained do not confirm the well-known assumption about the presence of an impact event at the boundary of the Pleistocene and Holocene.

Keywords

Late Pleistocene, Holocene, lake sediments, North-East of Russia, magnetic susceptibility, iron sulfides, greigite

References

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