Reconstruction of paleogeographic conditions in the Late Glacial-Holocene in Central Karelia based on comprehensive analysis of sediments from the lake Yuzhnoe Haugilampi
https://doi.org/10.31857/S0869607121060070
Abstract
The results of diatom, palynological and radiocarbon analyses have shown that bottom sediments have been accumulating in the lake Yuzhnoe Haugilampi for the last 13–12 000 cal. years. Terrigenous sediments (sand, clay) formed in the lake in the Late Glacial Period and organic sediments (gyttia) began to form in Pre-Boreal time. The vegetation reconstructions of the area cover the period from Younger Dryas until present. After the retreat of the glacier of the last Valdai glaciation, periglacial vegetation (Artemisia-Chenopodiaceae), tundra and forest-tundra birch communities spread over the study area. In Pre-Boreal, tundra and forest-tundra vegetation had been changed by birch open forests. Later, in the Boreal period, middle taiga pine forests reached their maximum development. In Atlantic period, middletaiga forests were replaced by south-taiga pine and spruce forests with thermophilic species. The forests began to acquire a middle-taiga character in the Late Holocene. In the Late Glacial Period, no diatom flora evolved in the lake. Sediments from that period contain the scarce, possibly redeposited valves of marine diatoms and small quantities of pioneer epiphytes and bottom species. In the Pre-Boreal period, a rather scarce diatom complex (regarding the abundance and diversity of species) developed in the lake, represented by pioneer forms typical for many northern water bodies: Ellerbeckia arenaria, Pseudostaurosira brevistriata, etc. The mass vegetation of diatoms began in the Boreal Period. The dynamics of the development of the lake from the Younger Dryas to the Subboreal time is traced.
About the Authors
T. S. Shelekhova
Institute of Geology, Karelian Research Centre, Russian Academy of Sciences
Russian Federation
Russian Federation
N. B. Lavrova
Institute of Geology, Karelian Research Centre, Russian Academy of Sciences
Russian Federation
Russian Federation
D. A. Subetto
Herzen State Pedagogical University of Russia
Russian Federation
Russian Federation
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For citations:
Shelekhova T.S., Lavrova N.B., Subetto D.A. Reconstruction of paleogeographic conditions in the Late Glacial-Holocene in Central Karelia based on comprehensive analysis of sediments from the lake Yuzhnoe Haugilampi. Proceedings of the Russian Geographical Society. 2021;153(6):73-89. (In Russ.) https://doi.org/10.31857/S0869607121060070
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