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The white sea level change and glacioisostatic land uplift during the Holocene near the Settlement of Kuzema, North Karelia Region

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Abstract

This paper contains lithostratigraphic and chronometric (radiocarbon dating) data on one of the regions on the Karelian coast of the White Sea obtained in the course of investigation of sedimentary sections from recent lake basins, which were separated at different times from the sea due to uplift of the glacioisostatic crust of the Earth. They were used as a basis for stratigraphic subdivision of marine and fresh water sediments and for reconstruction of the White Sea coast level change during the Late Pleistocene-Holocene near the Settlement of Kuzema, Karelia.

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Authors and Affiliations

  1. Geological Institute, Kola Scientific Center, Russian Academy of Sciences, Apatity, Murmansk Region, Russia

    V. V. Kolka & O. P. Korsakova

  2. Geological Institute, Karelian Scientific Center, Russian Academy of Sciences, Petrozavodsk, Russia

    T. S. Shelekhova & N. B. Lavrova

  3. St. Petersburg State University, St. Petersburg, Russia

    Kh. A. Arslanov

Authors
  1. V. V. Kolka
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  2. O. P. Korsakova
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  3. T. S. Shelekhova
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  4. N. B. Lavrova
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  5. Kh. A. Arslanov
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Corresponding author

Correspondence to V. V. Kolka.

Additional information

Original Russian Text © V.V. Kolka, O.P. Korsakova, T.S. Shelekhova, N.B. Lavrova, Kh.A. Arslanov, 2012, published in Doklady Akademii Nauk, 2012, Vol. 442, No. 2, pp. 263–267.

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Kolka, V.V., Korsakova, O.P., Shelekhova, T.S. et al. The white sea level change and glacioisostatic land uplift during the Holocene near the Settlement of Kuzema, North Karelia Region. Dokl. Earth Sc. 442, 139–143 (2012). https://doi.org/10.1134/S1028334X12010151

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  • DOI: https://doi.org/10.1134/S1028334X12010151

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