Paleoenvironment conditions of the bottom sediment formation in the small lake depressions on the Pomorsky coast of the White Sea

New lithological, palinological and chronological data obtained through the study of bottom sediments from four small lake depressions on the Pomor Coast, Onega Bay, White Sea are presented. The integrated study of bottom sediments from lakes lying at different elevations in the northeastern part of...

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Bibliographic Details
Published in:Proceedings of the Karelian Research Centre of the Russian Academy of Sciences
Main Authors: Vasili Kolka, Olga Korsakova, Nadezhda Lavrova
Format: Article in Journal/Newspaper
Language:English
Russian
Published: Karelian Research Centre of the Russian Academy of Sciences 2015
Subjects:
bottom sediments
lithology
pollen analysis
late glacial
holocene
pomor coast
white sea
Science
Q
Onega
White Sea
karelian
Onega Bay
Online Access:https://doi.org/10.17076/lim70
https://doaj.org/article/1da79f3339db4b9b986fe0301e038569
Description
Summary:New lithological, palinological and chronological data obtained through the study of bottom sediments from four small lake depressions on the Pomor Coast, Onega Bay, White Sea are presented. The integrated study of bottom sediments from lakes lying at different elevations in the northeastern part of the Sumozersky moraine complex and the White Sea lowland allowed to establish the time and features of their deposition, to distinguish the palaeoclimatic stages in the development of the environment on the Karelian Coast of the White Sea during the Late Glacial and Holocene.

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