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The Putorana Plateau (Krasnoyarsk Territory, Russia) is one of the largest mountainous regions of subarctic Eurasia. Studies of aquatic ecosystems of this are far from complete. In particular, microcrustaceans (Cladocera и Copepoda) of the Putorana Plateau are poorly investigated, although they are one of the main components of meiobenthic and zooplanktonic communities and a target for monitoring of the anthropogenic influence and climate change. An open question is a biogeographical status of the crustacean fauna of the plateau. Additionally, it is unknown which environmental factors significantly affect benthic and planktonic crustacean assemblages? Based on the samples collected in tundra and forest tundra ponds in the western and central parts of the plateau, analysis of the composition of crustacean fauna and factors regulating the assemblage structure was performed. In total, 36 Cladocera and 24 Copepoda species were found. Of these, 23 taxa are new for the region, and four are new to science. Species richness of Copepoda is higher in the central part and on the western slopes of the plateau than in foothills, while number of the Cladocera species in contrast decreases in mountainous areas. Variations in meiobenthic assemblages are due to the research area, type of water supply and less affected by altitude above sea level. For planktonic assemblages the size of the water body and, to a lesser degree, by macrophytes species composition was significant. Almost 12.8% of microcrustacean species of the Putorana Plateau can be attributed to glacial relics. Crustacean fauna of the Putorana Plateau has a high species richness and distinguishes significantly from the fauna of both western and eastern regions of the Arctic. The specifics of faunal composition of the region are connected to the climatic features of Middle Siberia and the retaining of the Pleistocene fauna in some glacial refugia. [ABSTRACT FROM AUTHOR]

The intraspecific structure of major populations of the walleye pollock Theragra chalcogramma from the northwestern part of the Bering Sea was studied. Specimens from Navarin, Olyutor and Shirshov shoals were sampled in the 2001 spawning season. Preliminary cluster analysis (TREECON) of PCR-RAPD data revealed the existence of cluster with low level of bootstrap support, which generally corresponds to geographic localization of the shoals. Processing of microsatellite sequence data (loci Tch12, Tch14, Tch15 and Tch18) with GENEPOP demonstrated the deviation from HWE and differentiation between the samples. The value of the inter-population variance (Fst = 0.02) corresponded to published data on marine stocks, which were subject to high levels of gene flow. The Shirshov group was found to be equidistant from the Navarin and Olyutor groups, with the genetic distance between the latter two being significantly less. Analysis of the microsatellite loci inferred disparities in their selective capacities. Loci Tch12 and Tch15 are found to be highly homozygous with low levels of polymorphism. Tch12 clearly follows the '3 band' pattern. Tch15 shows sign of linkage disequilibrium. Comparison of Fst values for the loci with the mean standardized variance f0 suggests that Tch12 is under pressure of disruptive selection, while Tch15 is rather neutral and Tch14 and Tch18 are under the influence of balance selection. Also a discussion is conducted in the context of undeterminate group migration. [ABSTRACT FROM AUTHOR]