Spatial Distribution of Species Diversity of Clavarioid Mycobiota in West Siberia

The results of a 20-year study of the spatial distribution of clavarioid mycobiota in the West Siberian Plain (WSP) are discussed. The species structure has been studied on two scales: regional (an area of 100000 km²) and local (100 km²). In the studied area, 121 species of clavarioid fungi are found. The patterns of spatial variability of species diversity on the plain are revealed. On the regional scale, the maximum species richness of fungi is observed in hemiboreal forests (104 species); on the local scale it ranges from the middle boreal to hemiboreal (54.3–54.5 species). With the increasing pessimality of the hydrothermal regime, the number of species decreases sharply on both scales in the direction of the tundra and steppes. The study of the distribution of diversity among the localities reveals changes not only along the latitudinal gradient, but also in the longitude sectors: in the forest zone, the richest localities are located on the western and eastern edges of the plain, while in the extensive marshy areas in the center the number of species is lower (p < 0.05). A map of the spatial distribution of species diversity for the local scale is constructed. The correspondence of the spatial distribution of the studied fungi group to a global latitudinal gradient is discussed. The main abiotic factors forming a variety of the studied group of fungi in the region are revealed.     

Zonal types of host-parasite complexes of arthropods and small mammals in a flat part of Western Siberia

Within a flat part of Western Siberia distribution of the small mammals and parasitic arthropods connected with them is accompanied by formation zonal host-parasite complexes dated for corresponding landscape zones or subzones: tundra complex dated for a tundra zone; forest complex dated for a forest zone (including subzones northern taiga, middle taiga, southern taiga and subtaiga); forest-steppe complex dated for a northern forest-steppe subzone; steppe complex dated for a southern forest-steppe subzone and steppe. Parasitic specificity of each type of a complex is defined by arthropods of different systematical and ecological groups: a tundra complex is defined by epizoite gamasid mites (Mesostigmata), forest and forest-steppe complexes is defined by tick (Ixodides) and fleas (Siphonaptera), steppe complex is defined by fleas and nidicolous gamasid mites.     

Zonal types of host-parasite complexes of arthropods and small mammals in the west Siberian Plain

Comparative analysis of the composition, population structure, and landscape distribution of small mammals and associated parasitic arthropods was performed for the plain part of West Siberia. Four main zonal complexes were distinguished, corresponding to different landscape zones or subzones: tundra, forest, forest-steppe (the northern forest-steppe subzone), and steppe (the southern forest-steppe subzone and steppes). The parasite specificity of each complex is defined by different systematic and ecological groups of arthropods: the tundra complex is defined by epizoic gamasid mites (Acari: Parasitiformes: Mesostigmata), the forest and forest-steppe complexes are defined by ticks (Acari: Parasitiformes: Ixodides) and fleas (Insecta: Siphonaptera), and the steppe complex is defined by fleas and nidicolous gamasid mites.     

Species composition and pattern of fish distribution in Siberia

At the end of the first half of the 20th century, 61 species and subspecies of fish, including one invader (bleak Alburnus alburnus) and 17 species—endemics of Baikal—were reported for Siberia (Berg, 1933, 1949). At the present time, in rivers, lakes, and reservoirs of Siberia, 96 fish species and subspecies are described, of which 80 are aboriginal and 16 are invaders; 33 species are endemics of Baikal. Each landscapegeographic zone of Siberia has its specific ichthyofauna: in rivers and lakes of the south of Siberia, species of boreal piedmont complex dominate; in water bodies of the steppe, forest-steppe, taiga, and southern parts of the forest-steppe zone boreal plain dominates; in the zone of tundra, arctic freshwater dominates; and in Baikal, the most part (35) of species belongs to the Baikal autochtonous complex. Most researchers, as before, distinguish in Siberia two ichthyogeographic sites—West Siberian and East Siberian—that enter the Arctic Province of the Circumpolar subregion of the Holarctic region. Baikal is considered in the rank of the suboblast of the Holarctic.     

Recent drought stress leads to growth reductions in Larix sibirica in the western Khentey,Mongolia

Trends in air temperature and precipitation in the forest‐steppe ecotone of the western Khentey, northern Mongolia were studied and related to stem increment and shoot water relations in Mongolia's most common tree species, Siberian larch (Larix sibirica). The area has been subject to a significant increase of summer temperature and a decrease of summer precipitation during the last 47 years. Tree‐ring width series from >400 larch trees show a strongly decreasing annual increment since the 1940s. The onset of this decrease is independent of the age of the trees and, therefore, can be attributed to the increasing aridity in the 20th century. Simultaneously to the declining annual increment, regeneration of Siberian larch decreased as well; today regeneration is virtually lacking in the larch forests on mountain slopes of the western Khentey. Measurements of shoot water potentials during the growing season exhibited daily minimum water potentials close to the point of zero turgor for extended periods. The drought stress indicated by these results is in line with the current low annual increment. Trees in the forest interior were more severely stressed and grow more slowly than trees at the forest line to steppe. This is attributable to the recent increase in aridity, as the stand density and probably also the trees themselves in the forest interior are adapted to moister conditions, whereas the trees at the forest edge have always been exposed to a more extreme microclimate. The progressing increase in aridity during the 21st century that is predicted for the western Khentey, suggests a future decline of larch forests. A widespread increase of aridity predicted for most parts of the Mongolian forest belt, suggests even a supra‐regional decline of larch.     

Interpretation of the last‐glacial vegetation of eastern‐central Europe using modern analogues from southern Siberia

Aim Interpretation of fossil pollen assemblages may benefit greatly from comparisons with modern palynological and vegetation analogues. To interpret the full‐ and late‐glacial vegetation in eastern‐central Europe we compared fossil pollen assemblages from this region with modern pollen assemblages from various vegetation types in southern Siberia, which presumably include the closest modern analogues of the last‐glacial vegetation of central Europe. Location Czech and Slovak Republics (fossil pollen assemblages); Western Sayan Mountains, southern Siberia (modern pollen assemblages). Methods Eighty‐eight modern pollen spectra were sampled in 14 vegetation types of Siberian forest, tundra and steppe, and compared with the last‐glacial pollen spectra from seven central European localities using principal components analysis. Results Both full‐ and late‐glacial pollen spectra from the valleys of the Western Carpathians (altitudes 350–610 m) are similar to modern pollen spectra from southern Siberian taiga, hemiboreal forest and dwarf‐birch tundra. The full‐glacial and early late‐glacial pollen spectra from lowland river valleys in the Bohemian Massif (altitudes 185–190 m) also indicate the presence of patches of hemiboreal forest or taiga. Other late‐glacial pollen spectra from the Bohemian Massif suggest an open landscape with steppe or tundra or a mosaic of both, possibly with small patches of hemiboreal forest. Main conclusions Our results are consistent with the hypothesis that during the full glacial and late glacial, the mountain valleys of the north‐western Carpathians supported taiga or hemiboreal forest dominated by Larix, Pinus cembra, Pinus sylvestris and Picea, along with some steppic or tundra formations. Forests tended to be increasingly open or patchy towards the west (Moravian lowlands), gradually passing into the generally treeless landscape of Bohemia, with possible woodland patches in locally favourable sites.     

Polymorphism of Mitochondrial DNA in Population of Siberian Tatars from Barabinsk Forest Steppe

The analysis of mtDNA polymorphism was carried out in the population of Siberian Tatars from the Barabinsk forest steppe living on the territory of Novosibirsk oblast (N = 199). As a result of the analysis of HVS I and HVS II nucleotide sequence, 101 haplotypes that refer to 22 mtDNA haplogroups were detected. The population of Baraba Tatars is represented by both East Eurasian (38.7%) and West Eurasian mtDNA lines (61.3%). H, T, U5, and J haplogroups prevail among West Eurasian haplogroups; C, D, G, M, and A haplogroups prevail among East Eurasian ones. According to the index of genetic diversity, Tatars from the Barabinsk forest steppe (0.9141) are the closest to Kazakhs (0.9108), Bashkirs (0.9165), and Tobol-Irtysh Tatars (0.9104). The greatest statistically significant interpopulation differences (F_ST) were detected between all studied samples; the smallest interpopulation differences were detected between all Tatar samples, as well as between Tatars and Komi, Mansi, Udmurts, Kazakhs, Chuvashes, and Bashkirs. The haplogroup H is the most common in populations that we studied. In the present study, was registered the haplotype 16126–16294 with the frequency of 4% (T cluster) previously found only in Caucasians. High frequency of haplogroups U4, U5, and H in the gene pool of Baraba Tatars brings them together not only with Samoyeds but also with Finno-Ugric populations. The highest intrapopulation genetic diversity was detected in Tatars from the Barabinsk forest steppe, Tobol-Irtysh Tatars, Kazakhs, and Bashkirs. The presence of the haplogroup B in the mitochondrial DNA genetic pool of Siberian Tatars brings them together with Turks that came from regions of Altai and Central Kazakhstan and inhabited the Western Siberian forest steppe in the 6th–9th centuries. The haplogroup U7, which is typical of populations of Jordan, Kuwait, Iran, and Saudi Arabia, could also have entered the territory of residence of Siberian Tatars in the middle of second millennium BC, when Iranian-speaking tribes entered Siberia.     

Immunosuppression of insects by the venom of <Emphasis Type="Italic">Habrobracon hebetor</Emphasis> increases the sensitivity of bait method for the isolation of entomopathogenic fungi from soils

We evaluated the susceptibility of Galleria mellonella larvae immunosuppressed by the venom of Habrobracon hebetor to soil entomopathogenic ascomycetes with the use of bait method. It was found that the sensitivity of the modified method was significantly (by almost 200 times) increased as compared with the standard procedure, which provided the isolation of fungi when their abundance was extremely low. Envenomated larvae were more susceptible to the entomopathogenic but not saprotrophic fungi. We presented results of isolation of the entomopathogenic fungi from soils in different climatic zones (from the forest tundra to the steppe) using an improved procedure.     

Ecology of a steppe-tundra gradient in interior Alaska

Abstract. Subarctic steppe is currently restricted in interior Alaska and the Yukon Territory to steep, south-facing river bluffs. Paleoecological and biogeographic evidence suggests that some steppe taxa may have been more widespread during the Full-Glacial. We examined factors controlling the distribution of steppe taxa on an elevation gradient across a steppetundra ecotone; such analyses may help define potential Full-Glacial distributions of these taxa. Multivariate analyses suggest that species can be divided into four spatially distinct groups, but individualistic species distributions create considerable overlap among these groups. The steppe-tundra ecotone comprises a broad zone of mixing between steppe taxa and drought-tolerant alpine tundra taxa, followed by an abrupt shift to alpine shrub tundra. The transition from low steppe to tundra vegetation is primarily associated with a gradient of decreasing soil temperature. The more abrupt transition from mixed steppe-tundra to alpine shrub tundra vegetation is primarily associated with changes in soil depth and soil moisture. Variation in vegetation within steppe is associated with gradients in soil phosphorus and moisture. Greenhouse experiments on drought tolerance of two steppe and two tundra taxa suggest that the individualistic distribution of species along the ecotone is partly a function of physiological differences among species. Our analyses of vegetation-environment relationships support the hypothesis that some components of the steppe community could have been more widespread during the colder Full-Glacial.     

Spatial-typological structure and mapping of reptile population of West Siberia

West Siberian reptiles were studied on the basis of the materials collected in forest, forest-steppe, and steppe zones of the Ob’ region during 12 years. Their abundance in certain biotopes has been determined. The relationship between the heterogeneity of reptile community and basic structure-forming environmental factors has been estimated, and a map of population of this faunal class was compiled.     

Holarctic phylogeography of the tundra shrew (Sorex tundrensis) based on mitochondrial genes

A range‐wide phylogeographic study of the tundra shrew (Sorex tundrensis) was performed using cytochrome b and cytochrome oxidase I (COI) mitochondrial genes. The results based on 121 specimens from 42 localities demonstrate that the tundra shrew is divided into five main mitochondrial DNA phylogenetic lineages with largely parapatric distribution. In addition to a single Nearctic clade (Alaska) four Palearctic clades are identified: Western (Northen Urals, Kazakhstan, South‐West Siberia), Eastern (from East Transbaikalia and the Middle Amur to Chukotka), South Central (Central Siberia, the Altai, the Dzhungarian Alatau) and North Central (Northern Siberia, Central Yakutia). Date estimates obtained by use of a molecular clock corrected for potential rate decay suggest Late Pleistocene age for the most recent common ancestor of all contemporary tundra shrew populations. Relatively high genetic divergence between phylogroups (0.95–1.6%) indicates that the observed phylogeographic structure was initiated by historical events that predated the Last Glacial Maximum. We assume that, being more cold‐ and arid‐tolerant, tundra shrew underwent expansion during an early cold phase of the Last Glacial and spread through its recent range earlier than most of other Siberian red‐toothed shrews. Comparative phylogeographic analysis of Siberian shrews and rodents suggests that evolutionary histories of species associated with azonal or open habitats show important differences compared to forest species. © 2010 The Linnean Society of London, Biological Journal of the Linnean Society, 2010, 101 , 721–746.     

Invasion of Siberian Pine Populations in Mountain Tundra in the Northern Urals

A new method for determining the upper forest border (UFB) as the border of the “root-closed” stand and regrowth as its potential vanguard is proposed. The mass dispersal of Pinus sibirica populations by the nutcracker (Nucifraga caryocatactes) in the UFB ecotone in the Northern Urals (Pavdinskii Kamen’ and Tretii Bugor Mountain) from the middle-mountain taiga to the mountain forest tundra and tundra at a distance reaching 1 km is found. It is done based on the original reconstruction method of the dynamics of population number in P. sibirica annual seedlings and on an analysis of their relations with the dynamics of the seed bearing and population number of the nutcracker. The trustworthy consortive relations of the number of Pinus sibirica generations in the mountain forested tundra and tundra zones, with its seed bearing and nutcracker number in the previous year in the middle-mountain taiga zone, are found. A significant increase, 3.7 times, in the number of seedling generations during the last 49 years is found in connection with the increase in the summer air temperature in the subarctic to 2.0°C. A hypothesis of the formation of the united genetic metapopulation of P. sibirica in the forest–tundra mountain ecotone zone as a consequence of its seed ornitochory from the highly different populations is formulated. A forecast of the mosaic formation of the vanguard “thin forests” in 20–25 years and the root-closed curtains of the forest in 40–50 years in the mountain tundra of the Northern Urals at the current rate of the rise in temperature is made.     

A phytogeographic analysis of birch woodlands in the southern part of West Siberia

A minimum variance cluster analysis of 87 species of vascular plants occurring in south Siberian birch woodlands, based on their total distribution ranges, grouped them into 9 phytogeographic elements. The main distribution patterns of each element are illustrated by means of maps obtained by automatic mapping programs, showing the joint occurrence of the species of each element on a world scale. The results indicate a predominance of Eurasiatic-temperate taxa. The south Siberian birch woodlands can be considered as the easternmost extensions of the European deciduous forest belt, which in Siberia is compressed between the taiga biome in the north and the steppe biome in the south. The marginal position of Siberian Betula stands is reflected by the persistence of plants which are ecologically marginal with respect to true forest vegetation; most of the Eurasiatic species are typical, in Europe, of forest-meadows and forest-margins.     

A study on the vegetation in the east side of Helan Mountain

This paper analyzed the vegetation data obtained from a field survey conducted in the East Side of Helan Mountain, China, to reveal the features of mountainous vegetation growing in a transitional zone between the steppe and desert regions. Detrended correspondence analysis (DCA) was applied to the process of analysis, to clarify the spatial variation of floristic composition of the vegetation in the lower mountain range.The preliminary results obtained from the analysis are: (1) There are 53 vegetation formations existing in the area, following the China's criteria of vegetation classification system. (2) Those vegetation types compose a vertical vegetation spectrum in the East Side of Helan Mountain due to the climatic gradient caused by elevation variation. The spectrum consists of 4 zones. They are, from the foot up to the peak in turn, mountain steppe zone, mountain open forest and steppe zone, mountain coniferous forest zone, and alpine bush and meadow zone. The mountain coniferous forest zone can be further divided into two subzones: Pine forest subzone and Spruce forest subzone. (3) Most of the vegetation types show clear xeromorphic features due to the base zone of the vertical vegetation spectrum lying in the arid region of China. (4) The distribution of vegetation types and flora is sensitive and susceptible to the moisture condition that the vertical vegetation spectrum has quite different expressions between northern and southern exposures. (5) Floristic composition of the vegetation shows a northern temperate feature. The families that are rich in species in the area include Gramineae, Compositae, Leguminosae, Chenopodiaceae, Rosaceae and others, most of which are abundant in herbaceous species. (6) The variation of the ecological conditions from the north to the south also leads to the differentiation of vegetation and its floristic composition in the area. (7) The broad-leaved forest can not form a forest zone in the vertical vegetation spectrum. This may be a special characteristic of the spectrum sitting on a transitional zone between the steppe and desert regions.     

The spatial organization of winter bird communities in the East European and West Siberian plains

The main trends in the territorial changes in winter bird communities and the environmental factors determining them were analyzed based on long-term counts in the East European and West Siberian plains. These trends are reduced to a decline in the winter avian complexes (in the number of species and individuals) in the north- and eastward directions and with a decrease in the degree of sheltering and feed reserves in the habitats associated with reduction in afforestation. The specific regional features of winter East European avian complexes are the larger number of species and individuals in the nemoral forest, forest-steppe, and steppe landscapes, and inland water bodies as compared with the West Siberian avian complexes, as well as an increased influence of the degree of development and agricultural transformation of landscapes.     

Spatial patterns of total and available N and P at alpine treeline

Background and aims

Vegetation can have direct and indirect effects on soil nutrients. To test the effects of trees on soils, we examined the patterns of soil nutrients and nutrient ratios at two spatial scales: at sites spanning the alpine tundra/subalpine forest ecotone (ecotone scale), and beneath and beyond individual tree canopies within the transitional krummholz zone (tree scale).

Methods

Soils were collected and analyzed for total carbon (C), nitrogen (N), and phosphorus (P) as well as available N and P on Niwot Ridge in the Colorado Rocky Mountains.

Results

Total C, N, and P were higher in the krummholz zone than the forest or tundra. Available P was also greatest in the krummholz zone while available N increased from the forest to the tundra. Throughout the krummholz zone, total soil nutrients and available P were higher downwind compared to upwind of trees.

Conclusions

The krummholz zone in general, and downwind of krummholz trees in particular, are zones of nutrient accumulation. This pattern indicates that the indirect effects of trees on soils are more important than the direct effects. The higher N:P ratios in the tundra suggest nutrient dynamics differ from the lower elevation sites. We propose that evaluating soil N and P simultaneously in soils may provide a robust assay of ecosystem nutrient limitation.     

末次冰期以来北海道、萨哈林岛及亚洲东北部落叶松林演变史

萨哈林岛（库叶岛）和北海道的末次冰期沉积丰富的落叶松花粉,为了搞清楚落叶松花粉百分比和实际森林密度的关系,我们系统地分析了从苔原,森林苔原以及泰加林的表土样品,根据孢粉资料恢复了两个岛屿3万年以来的植被和气候,两个岛上3万年前后 以云杉与落叶松共生的森林为主,松和冷杉现在比现代相对较冷和干的气候条件下,萨哈林在末次冰盛期的草原和泰加林主要由落叶松和松组成,和现在西伯利亚东北部的泰加林相似,在北海道末次冰盛期的草原和泰加林主要由落叶松,松以及云杉组成,气候更加干冷,在新仙女木期森林苔原分布到中萨哈林岛,而北海道的草原和泰加林以落叶松为主,气候可能比末次冰盛期还要冷,在1万年前两个岛的落叶松含量都开始下降,6000年前在北海道消失,萨哈林岛的落叶松则残存至今。     

Where do the treeless tundra areas of northern highlands fit in the global biome system: toward an ecologically natural subdivision of the tundra biome

According to some treatises, arctic and alpine sub‐biomes are ecologically similar, whereas others find them highly dissimilar. Most peculiarly, large areas of northern tundra highlands fall outside of the two recent subdivisions of the tundra biome. We seek an ecologically natural resolution to this long‐standing and far‐reaching problem. We studied broad‐scale patterns in climate and vegetation along the gradient from Siberian tundra via northernmost Fennoscandia to the alpine habitats of European middle‐latitude mountains, as well as explored those patterns within Fennoscandian tundra based on climate–vegetation patterns obtained from a fine‐scale vegetation map. Our analyses reveal that ecologically meaningful January–February snow and thermal conditions differ between different types of tundra. High precipitation and mild winter temperatures prevail on middle‐latitude mountains, low precipitation and usually cold winters prevail on high‐latitude tundra, and Scandinavian mountains show intermediate conditions. Similarly, heath‐like plant communities differ clearly between middle latitude mountains (alpine) and high‐latitude tundra vegetation, including its altitudinal extension on Scandinavian mountains. Conversely, high abundance of snowbeds and large differences in the composition of dwarf shrub heaths distinguish the Scandinavian mountain tundra from its counterparts in Russia and the north Fennoscandian inland. The European tundra areas fall into three ecologically rather homogeneous categories: the arctic tundra, the oroarctic tundra of northern heights and mountains, and the genuinely alpine tundra of middle‐latitude mountains. Attempts to divide the tundra into two sub‐biomes have resulted in major discrepancies and confusions, as the oroarctic areas are included in the arctic tundra in some biogeographic maps and in the alpine tundra in others. Our analyses based on climate and vegetation criteria thus seem to resolve the long‐standing biome delimitation problem, help in consistent characterization of research sites, and create a basis for further biogeographic and ecological research in global tundra environments.     

On the Distribution of <Emphasis Type="Italic">Pleurozium schreberi</Emphasis> (Bryophyta,Hylocomiaceae) in the East European Plain and Eastern Fennoscandia

Pleurozium schreberi is one of the most common moss species in the forest area. It is dominant in the moss layer of blueberry and wood sorrel forests. It can occur in small quantities in almost all types of forests (even in bogs). It is also a typical component of the moss layer in tundra. The article considers the distribution of Pleurozium schreberi in the East European Plain and Eastern Fennoscandia. On the basis of literature sources on the occurrence of the species in different regions (according to point data), a model map of species distribution using the kriging-method has been created. The overlaying of the model map on the maps of spatial distribution of climatic parameters and vegetation zones in this area has revealed that the biogeographical preferences of the species. P. schreberi is characterized by its highest distribution in the forest zone. It often occurs here and represents a phytocenotically active species. The occurrence of Pleurozium schreberi dramatically decreases in the transition from the forest to the steppe zone, where it is a rather rare species, growing exclusively in pine and birch pegs. This species disappears in the open steppe. From the steppe zone to the south, the occurrence of Pleurozium schreberi gradually decreases with increase in summer temperatures and decrease in precipitation and with forest disappearance. In the north, where the species is highly active, its range abruptly ends on the coast of the Arctic Ocean. This pattern of distribution of Pleurozium schreberi is associated both with cenotic preferences and with climate: it becomes rare in regions with summer temperatures higher than +23°C and annual precipitation of less than 400 mm.     

Community of wood-destroying fungi as a reflection of the structure and state of a forest

A new approach to the analysis of fungal communities is proposed, with the purpose of indication of the state of ecosystems. The approach is based on the dialectical unity of the parts and the whole, abstraction and concreteness in the light of modern notions of the fractal character of the objective reality. Exemplified by Panholarctic mycocomplex of birch, it is shown that the biota of wood-destroyed fungi is a fractal, the structure of which is an integral reflection of the structure of forest stand developing under different conditions, which is confirmed by the reproducibililty of taxation indices of the stand in the fractal-matrix analysis of groups of wood-destroying fungi. The proposed formulas were tested for the latitudinal-zonal and topological range of forests and can be considered not only as an illustration of the surprising integrity of the universe but also used in ecological activities.