Pilot Studies of the Unique Highland Palsa Mire in Western Sayan (Tuva Republic, Russian Federation)

Author:

Kirpotin Sergey N.,Kvasnikova Zoia N.,Potapova Sophia A.,Volkova Irina I.,Volkov Igor V.ORCID,Pyak Andrei I.,Byzaakay Arisiya A.,Kolesnichenko Larisa G.,Lushchaeva Inna V.,Khovalyg Aldynay O.,Kuzhevskaia Irina V.,Chursin Vladislav V.,Peregon Anna M.

Abstract

In contrast to the well-studied West Siberian sector of frozen bogs in the Russian Arctic, the frozen mound bogs (so-called “palsas”) on the highlands of Southern Siberia have not yet been studied, but they are suspected to be even more sensitive to ongoing climate change. This article provides the pilot study on palsa mire Kara-Sug in the highland areas of Western Sayan mountain system, Tuva Republic. The study focuses on the current state of palsa mire and surrounding landscapes, providing wide range of ecological characteristics while describing ongoing transformations of natural landscapes under a changing climate. The study used a variety of field and laboratory methods: the integrated landscape-ecological approach, the study of peat deposits, geobotanical analysis, and modern analysis of the chemical composition of water, peat, and soils. The study shows that highland palsa mires are distinguished by their compactness and high variety of cryogenic landforms leading to high floristic and ecosystem diversity compared with lowland palsa mires. This information brings new insights and contributes to a better understanding of extrazonal highland palsa mires, which remain a “white spot” in the global environmental sciences.

Funder

Russian Science Foundation

Ministry of Science and Higher Education of the Russian Federation

RFBR

EU project INTERACT II GA

Publisher

MDPI AG

Subject

Atmospheric Science,Environmental Science (miscellaneous)

Reference78 articles.

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3. Effects of Climate Change on the Distribution and Development of Palsa Peatlands: Background and Suggestions for a National Monitoring Project;Hoofgard,2003

4. The Origin of Palsas

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