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

Orlov, A. V.; Subetto, D. A.; Potakhin, M. S.; Beliaev, P. Yu.

doi:10.31951/2658-3518-2020-A-4-469

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

Авторы

Orlov, A. V. ^{1, 2}
Subetto, D. A. ^{1, 2}
Potakhin, M. S. ²
Beliaev, P. Yu. ^{2, 3}

DOI:

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

Ключевые слова:

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

Аннотация

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.