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Environmental changes in the Late Glacial and Holocene in the southeast of Belarus

https://doi.org/10.29235/1561-8323-2019-63-5-584-596

Abstract

Communicated by Academician Aleksey V. Matveev

The reconstruction of environmental changes in the southeast of Belarus during the last 14700 cal. BP is based on the results of palynological, radiocarbon, isotope and lithological studies of Lake Staroje deposits. Climatic fluctuations, fires and human activities played a significant role in the transformation of the vegetation cover. The beginning of the lacustrine sedimentation was dated circa 16000 cal. BP. The intensification of erosion processes on the water catchment area was marked by an increase in the mineral material flow into the lake. These events have a positive correlation with the climate cooling and humidity phases in the Late Glacial and Early Holocene, and in the Late Holocene with anthropogenic impact stages. The traces of the episodic human activity were dated to 5800 cal. BP, while the expansion of farming and pasturing areas began at 3000 cal. BP Currently the consequences of human activities (including drainage of bogs) are reflected in the treeless landscapes adjacent to the lake.

About the Authors

Valentina P. Zernitskaya
Bnstitute for Nature Management, National Academy of Sciences of Belarus
Belarus

Zernitskaya Valentina Petrovna - Ph. D. (Geography), Leading researcher.

10, F. Skorina Str., 220114, Minsk



Elena Yu. Novenko
Lomonosov Moscow State University
Russian Federation

Novenko Elena Yurevna - D. Sc. (Geography), Leading researcher.

1, Le-ninskie Gory Str., 119991, Moscow



Migle Stančikaitė
Institute of Geology and Geography, Nature Research Centre
Lithuania

Stancikaite Migle - D. Sc. (Geography), Leading researcher.

2, Akademijos Str., LT-08412, Vilnius



Boris P. Vlasov
Belarusian State University
Belarus

Vlasov Boris Pavlovich - D. Sc. (Geography), Head of the Laboratory.

4, Nezavisimosti Ave., 220030, Minsk



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ISSN 1561-8323 (Print)
ISSN 2524-2431 (Online)