Environmental evolution of the south shore of Kandalaksha Bay, as indicated by the study of bottom sediments from small lakes

Authors

  • Shelekhova T.S. 1
  • Lavrova N.B. 1
    • 1 Institute of Geology, Karelian Research Centre, Russian Academy of Sciences, Pushkinskaya St., 11, Petrozavodsk, 185910, Karelia, Russia

DOI:

https://doi.org/10.31951/2658-3518-2024-A-4-665

Keywords:

Holocene, bottom sediments, pollen analysis, diatom analysis, White Sea

Abstract

Environmental changes on the south shore of Kandalaksha Bay in Holocene time were reconstructed by analyzing the data obtained by palynological and 14C methods. Diatom complexes of marine, freshwater and transition facies are described. The possible application of pollen indicators for a better understanding of the genesis of sediments is discussed.

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Published

2024-08-26

Issue

2024: №4 (SI:Paleo2024)

Section

Articles

License

Copyright (c) 2024 Limnology and Freshwater Biology

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

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