Articles | Volume 381
https://doi.org/10.5194/piahs-381-13-2019
https://doi.org/10.5194/piahs-381-13-2019
Post-conference publication
 | 
01 Aug 2019
Post-conference publication |  | 01 Aug 2019

Lake sedimentation as an agent of postglacial transformation of interfluves and fluvial landscapes of the Borisoglebsk Upland, Central European Russia

Ekaterina V. Garankina, Vladimir R. Belyaev, Ilya G. Shorkunov, Yuliya V. Shishkina, Pavel V. Andreev, and Elena D. Sheremetskaya

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Proc. IAHS, 381, 37–47, https://doi.org/10.5194/piahs-381-37-2019,https://doi.org/10.5194/piahs-381-37-2019, 2019
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Cited articles

ASTM D 2974-87: Standard Test Methods for Moisture, Ash, and Organic Matter of Peat and Other Organic Soils, USGA Green Section Record, March/April, 31–33, 1993. 
Antonov, S. I.: Pleistocene lacustrine lithomorphogenesis at the southeastern Moscow region limits, in: History of Pleistocene lakes of the Eastern European Plain, Saint Petersburg, Nauka, 282–290, 1998 (in Russian). 
Astakhov, V., Shkatova, V., Zastrozhnov, A., and Chuyko, M.: Glaciomorphological Map of the Russian Federation, Quaternary Int., 420, 4–14, 2016. 
Belyaev, V. R., Semochkina, A. E., Streletskaya, I. D., Lisova, A. D., Garankina, E. V., Shorkunov, I. G., and Lugovoy, N. N.: Relic periglacial features and their impact on modern soil redistribution processes on cultivated slopes of the European Russia, PIAHS, submitted, 2019. 
Garankina, E. V., Belyaev, V. R., Shorkunov, I. G., Andreev, P. V., Verlova, T. A., Shishkina, Yu. Vl., and Bondar, A. I.: Evolution of the Borisoglebsk Upland interfluves over the last 150000 years (Marginal zone of Moscow Glaciation, central part of Russian Plain), in: Practical Geography and XXI Century Challenges. International Geographical Union Thematic Conference, Moscow, Russia, 4–6 June 2018, Conf. Book, Part 1, 180–187, 2018. 
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Short summary
Previously underestimated, lake sedimentation appears to be the leading agent of landscape transformation since the last glaciation at the Borisoglebsk Upland – one of the numerous marginal uplands in the center of the Russian Plain. Investigation of thick laminated surface drifts and associated buried soils and cryogenic features adds new genetic interpretation to the problem of mantle loams formation.