Plant matter decomposition in the upper timberline ecotone of the Polar Urals

A relatively high biological activity of soils has been revealed at the upper timberline in the Polar Urals. The role of the altitudinal gradient as a factor of destruction process has distinctly manifested itself upon comparing decomposition rates of flowering plant foliage and herbaceous plant roots in the forest and in the tundra. The qualitative composition of decomposing plant matter has also proved to play a significant role. The soil moisture regime of the ecotope is the leading factor of the destruction process.     

Distribution of plants differing in attitude toward thermal conditions in communities of the timberline ecotone on Mount Iremel’, the Southern Urals

Specific features in the distribution of plant species differing in their attitude toward thermal conditions have been studied in communities of the present-day timberline ecotone on Mount Iremel’ in the Southern Urals. It has been shown that the distribution of such species is characterized by significant spatial nonuniformity. Elevation above sea level, local conditions in habitats located at the same altitudinal level, and specific features of mountain slopes account for 13–84, 5–30, and 0.4–14% of the total variance of test parameters, respectively. The abundance of plants changes nonlinearly along the altitudinal gradient, whereas changes in the species diversity of different plant groups have an almost linear pattern. Marked differences between plant communities with respect to the proportions of species differently responding to changes in thermal conditions have been revealed on all slopes in the upper part of the timberline ecotone, upon transition from the slopes proper to the plateau-like areas of intermontane depressions.     

Climatic dependence of the Late Holocene dynamics of tree species cenotypes in the intrazonal ecotone of Eastern Sayan forests

A comprehensive study of paleobotanical materials collected in the northern part of the Eastern Sayan was performed, including botanical analysis of peat, palynological and carpological analysis, and radiocarbon dating. The results provided a basis for reconstructing in detail the spatiotemporal distribution of ecocenotic complexes and corresponding paleoclimate types and calculating quantitative gradients of heat and moisture supply in the Late Holocene, beginning from 3500 ka.     

Altitudinal and horizontal shifts of the upper boundaries of open and closed forests in the Polar Urals in the 20th century

In the Polar Urals (the Rai-Iz massif and Mounts Tchernaya and Malaya Tchernaya), altitudinal and horizontal shifts of the upper boundary of open and closed larch forests in the 20th century have been studied. Spatiotemporal parameters of these shifts have been assessed with the aid of the ARC/INFO geographic information system (ESRI Inc., United States), using our original large-scale geobotanical maps showing the distribution of different types of forest-tundra communities in the early 1910s and 2000s. The results show that tree vegetation has been actively expanding to higher elevations over the past 90 years. On average, the upper boundaries of open and closed forests have ascended 26 and 35 m and shifted horizontally 290 and 520 m, respectively. These shifts have been conditioned by climate warming and increasing humidity observed since the 1920s.     

Indicatory aspect of the geographic analysis of plant communities with respect to floristic composition on mountain slopes differing in exposure (the Polar Urals)

Latitudinal geographic groups of vascular plant, moss, and lichen species included in tundra communities and lower vegetation layers of larch forest and open forest have been analyzed with respect to their distribution according to different altitudinal levels and slopes differing in exposure. Prevailing plant groups have been identified. The results were compared with corresponding data on the composition of plant communities in the neighboring flatland area (Kharp Research Station).