Changes in the Distribution of Broadleaf Tree Species in the Central Part of the Southern Urals since the 1970s

Russian Journal of Ecology - Changes in the distribution of broadleaf tree species—Tilia cordata Mill., Quercus robur L., Acer platanoides L., and Ulmus glabra Huds.—in the central part...     

Low-frequency variability of storms in the northern Black Sea and associated processes in the ocean–atmosphere system

Monthly anomalies of stormy wind–wave heights and return periods are evaluated using secular routine observations in the coastal zone of the northern Black Sea. It is shown that wind–wave anomalies in this region are characterized by high-amplitude quasi-periodical variability with typical timescale of about 50 years. This timescale is determined by temporal variability of the coupled ocean–atmosphere system and coincides with periodicity of Atlantic Multidecadal Oscillation. Atmospheric re-analysis data show that cyclonic activity over the Black Sea basin intensifies when North Atlantic is relatively cold and meridional forms of atmospheric circulation are more frequent in the North Atlantic-Eurasian region. This leads to generation of more frequent Black Sea storm events and enhanced recurrence of extreme waves and results in profound (and mostly negative) environmental consequences. When North Atlantic is relatively warm and meridional forms of atmospheric circulation are less frequent in the North Atlantic-Eurasian region, environmental conditions in the Black Sea region are calmer. Thus, statistics of dangerous events can be wrongly estimated even if relatively long-term (~30 years) time series are considered and interdecadal variability of wind–wave anomalies must be taken into account when the risk assessment is accomplished.     

Assessment of vegetation β-diversity on the basis of syntaxonomy

Using the example of vegetation in four specially protected natural areas in the Southern Urals, it has been shown that its β-diversity can be estimated in two ways: from the number of syntaxa ranking from the class to the association and from the syntaxonomic spectrum, i.e., the ratio between associations of different classes. The second approach is more informative and better reflects the diversity of vegetation.     

Analysis of trends in the formation of species richness of plant communities using syntaxonomy and ecological scales

On the basis of syntaxonomy of primary forests in the Southern Ural region, an analysis of trends in the formation of their species diversity has been performed in regard to heat supply, soil moisture, and general soil richness. The roles of environmental factors have been estimated using Landolt’s scales. The results have shown that communities of forest classes Querco-Fagetea, Brachypodio-Betuletea, and Vaccinio-Piceetea differ in the trends of changes in species richness along gradients of the above factors. In communities of all these classes, species richness depends primarily on heat supply, with soil richness being the second most important factor.