Holocene environmental history on the eastern slope of the Polar Ural Mountains, Russia

• Published in: Boreas
• Main Authors: JANKOVSKÁ, VLASTA, ANDREEV, ANDREI A., PANOVA, NATA K.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2006
• Subjects: palsa; permafrost; Tundra; ural mountains
• Online Access: http://dx.doi.org/10.1111/j.1502-3885.2006.tb01171.x; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.2006.tb01171.x; https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.2006.tb01171.x

The Holocene environmental history of the eastern slope of the Polar Ural Mountains has been reconstructed using pollen, spores, algae and other microfossils from the Chernaya Gorka palsa section (67°05'N, 65°21'E, 170 m a.s.l.). An initial oligotrophic lake was formed at the study site c . 9800–9500 14 C yr BP Although tundra communities dominated the vegetation in the area, birch and larch trees might have grown at lower elevations. Dry and disturbed soil habitats also occurred around the lake. Algae (mostly Pediastrum and Botryococcus ) started to expand in the lake as climate gradually improved after c . 9500 14 C yr BP. However, the role of mosses (mostly Calliergon and Drepanocladus ) was most important for the infilling of the lake basin. Increased temperatures and subsequent improvement of hydrological conditions resulted in vegetation changes: stands of willows developed rapidly and the role of tree birch in the local vegetation increased. The lake was completely filled at c . 8600 14 C yr BP. Peat accumulation started with Bryales mosses and, later, Sphagnum became dominant. Stands of Larix, Picea and Betula became well developed during the Boreal climate optimum. Tree birch began to spread into the tundra. Different Bryales mosses formed peat c . 8000–6500 14 C yr BP. Cyperaceae later became the main peat‐forming element. Dense spruce canopies with Larix sibirica and Betula pubescens surrounded the study site during the Atlantic period, pointing to the warmest climate during the Holocene. Summer temperatures might have been up to 3–4°C higher than today. However, a decline of spruce and an increase of birch around 6700–6300 14 C yr BP may reflect some climate deterioration. There are no dated deposits younger than 6000 14 C yr BP. It is assumed that Subboreal climate deterioration resulted in the development of permafrost and formation of the palsa at the site. The deposits, now protruding above the surrounding terrain, were eroded by wind, water and cryogenic processes.