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Climatic Changes in the Arctic Regions of Eastern Siberia over the Last Millenium according to the Lithological–Geochemical Data on Bottom Sediments of Peyungda Lake (Krasnoyarsk Krai, Evenkia)

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Abstract

Scanning micro-X-ray fluorescence analysis with synchrotron radiation was applied to obtain the depth-variation profiles of element compositions of banded clays in Peyungda Lake (Krasnoyarsk krai, Evenkia) located 30 km southwest of the epicenter of the Tunguska event (1908). The age model was confirmed by a dated layer of anomalous thickness related to the fall and explosion of the Tunguska Cosmic Body (TCB). The variations in the element content in dated core layers were compared with the instrumental meteorological observation data over the last century. The regional average annual temperature and element compositions of the coeval bottom sediments (transfer function) were found to be interrelated. The approximation of the transfer function to the sampling depth of the sedimentary section made it possible to reconstruct the air temperature in the studied region over the past 1000 years. The average annual temperature reconstructions in the study area compared with the global temperature reconstructions in the Arctic region for the same period made it possible to reveal general trends and extreme values.

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Funding

Preparation of solid specimens (T.I. Markovich and V.S. Novikov), micro-XRF-SI (Ya.V. Rakshun, F.A. Darin, and D.S. Sorokoletov) of bottom sediment samples, varve chronology, age modeling (A.V. Darin and V.S. Novikov), and transfer function construction and reconstructions (V.V. Babich) were carried out under a State Assignment of the Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences (project no. 122041400214-9). Bottom sediment sampling and data analysis (D.Yu. Rogozin and A.V. Meydus) were supported by the Russian Science Foundation (grant no. 22-17-00185).

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Authors and Affiliations

  1. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, 630058, Novosibirsk, Russia

    A. V. Darin, V. S. Novikov, V. V. Babich & T. I. Markovich

  2. Institute of Biophysics, Siberian Branch, Russian Academy of Sciences, 660036, Krasnoyarsk, Russia

    D. Yu. Rogozin &  A. G. Degermendzhi

  3. Astafiev Krasnoyarsk State Pedagogical University, 660049, Krasnoyarsk, Russia

    A. V. Meydus

  4. Budker Institute of Nuclear Physics, Siberian Branch, Russian Academy of Sciences, 630090, Novosibirsk, Russia

    Ya. V. Rakshun, F. A. Darin & D. S. Sorokoletov

Authors
  1. A. V. Darin
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  2. D. Yu. Rogozin
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  3. V. S. Novikov
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  4. A. V. Meydus
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  5. V. V. Babich
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  6. T. I. Markovich
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  7. Ya. V. Rakshun
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  8. F. A. Darin
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  9. D. S. Sorokoletov
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  10. A. G. Degermendzhi
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Corresponding author

Correspondence to A. V. Darin.

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Translated by E. Maslennikova

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Darin, A.V., Rogozin, D.Y., Novikov, V.S. et al. Climatic Changes in the Arctic Regions of Eastern Siberia over the Last Millenium according to the Lithological–Geochemical Data on Bottom Sediments of Peyungda Lake (Krasnoyarsk Krai, Evenkia). Dokl. Earth Sc. (2024). https://doi.org/10.1134/S1028334X23603012

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  • DOI: https://doi.org/10.1134/S1028334X23603012

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