Geochemical indication of the Holocene climatic changes in sediments of Bolshoi Bagan Lake, Southern West Siberia

Authors

  • Maltsev, A.E. 1
  • Krivonogov, S.K. 1
  • Miroshnichenko, L.V. 1
  • Leonova, G.A. 1
  • Smolentseva, E.N. 2
  • Shavekin, A.S. 1
  • Solotchin, P.A. 1
    • 1 Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Science, Academician Koptyug ave., 3, Novosibirsk, 630090, Russia
    2 Institute of Soil Science and Agrochemistry, Siberian Branch of the Russian Academy of Science, Academician Lavrentiev ave., 8/2, Novosibirsk, 630090, Russia

DOI:

https://doi.org/10.31951/2658-3518-2022-A-4-1485

Keywords:

bottom sediments, geochemistry, saline lake, Holocene, paleoclimate

Abstract

Our study of the Holocene sediments of shallow saline Lake Bolshoy Bagan located revealed the following stages of the lake evolution: (I) Appearance and maturing of the lake 9.1–5.8 ka BP; (II) rise in water level 5.8–2.3 ka BP; and  (III) shallowed lake 2.3–0 ka BP.

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Published

2022-09-02

Issue

2022: №4 (SI:Paleo2022)

Section

Articles

License

Creative Commons License
This work is distributed under the Creative Commons Attribution-NonCommercial 4.0 International License.