Runoff of Onega paleo-lake in late-glacial period: paleolimnological data

Authors

  • Orlov, A. V. 1, 2
  • Subetto, D. A. 1, 2
  • Potakhin, M. S. 2
  • Beliaev, P. Yu. 2, 3
    • 1 Herzen State Pedagogical University of Russia, Nab. Moyki 48, St. Petersburg, 191186, Russia
    2 Northern Water Problems Institute, Karelian Research Centre of the RAS, Aleksander Nevsky st. 50, Petrozavodsk, 185030, Republic of Karelia, Russia
    3 A.P. Karpinsky VSEGEI, Sredniy Prospekt V.O 74, St. Peterburg, 199106, Russia

DOI:

https://doi.org/10.31951/2658-3518-2020-A-4-469

Keywords:

paleolimnoligy, lithology, lake-bottom sediments, glacial reservoir, Late Glacial period, Holocene, Onega lake

Abstract

Bottom sediments of the small relict lakes Regozero, Chernoe, Anashkino, Rzhanoe and other bear important information about a history of Lake Paleo-Onega in the LGM-Holocene transition. We studied the core 4m from bottom sediments of Lake Rzhanoe. The aim of the study was to test the hypothesis that there was an outflow canal from Lake Paleo-Onega in the LGM-Holocene transition.

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Published

2020-08-27

Issue

2020: №4 (SI:Paleo2020)

Section

Articles

License

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