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Analysis of mammalian species composition has been performed for eight archaeological sites on the Ustyurt plateau. They date to the range from the middle Subboreal to the middle Subatlantic. The modern species composition of large mammals formed by the end of the Middle Holocene (Subboreal 2) and did not change until the early 20th century. The ungulate species composition and ratio on the plateau showed geographical variation and changed over time. Boars were always rare or absent in the north of Ustyurt. The structure of the ungulate fauna in the north of Ustyurt changed over time. Onager numbers in this area increased and saiga numbers decreased in the middle of the Late Holocene. Significant geographical differences in the structure of ungulate fauna were recorded in the middle of the Late Holocene. The numbers of onagers, goitered gazelles, and argali were higher, whereas the numbers of saigas were lower in the south of Ustyurt than in the north.

Enamel macro- and microstructure has been studied in the teeth of Merck's rhinoceros (Stephanorhinus kirchbergensis Jäger, 1839), woolly rhinoceros (Coelodonta antiquitatis Blumenbach, 1799), and rhinoceroses from the Tetyukhinskaya (44°35' N, 135°36' E) and Sukhaya (43°09' N, 131°28' E) caves in southern Primorye. The teeth from the caves were identified as the teeth of Merck's rhinoceros. Radiocarbon dating and accompanying animal species enabled the dating of Merck's rhinoceros remains to the Late Pleistocene (marine isotope stages 5-2). These finds mark the extreme eastern boundary of the Merck's rhinoceros species range in the Late Pleistocene. The living range reached the Pacific Ocean coast during a certain time interval within this epoch. This was due to the abundance of tree and shrub vegetation in the area during the Late Pleistocene.

The study deals with a new sample of the mammalian fossils from the Pleistocene deposits of the Ignatievskaya Cave in Southern Urals (54°53' N, 57°46' E). Among the rodent fossils, the teeth of red squirrel (Sciurus vulgaris) and forest dormouse (Dryomys nitedula) have been identified. The enamel differentiation quotient (SDQ) of the water vole teeth matches the Arvicola terrestris species from locations of the end of Middle and Late Pleistocene (oxygen isotope stages, OIS 6 and OIS 5-2, respectively). The high SDQ value for the water vole and the presence of the squirrel and dormouse in the fauna allow dating the finding near the end of the Middle Pleistocene and beginning of the Late Pleistocene (OIS 6 and OIS 5e, respectively). The widespread open and forest landscapes were inhabited by this fauna.

The paper gives the experience in introducing a new disinfection method based on the relationships between the saprophytic microflora of a complex of antigenic slime organisms and most pathogenic microorganisms to neutralize waste waters of the Kazanorgsintez production association. This method makes it possible to prevent all side effects of chlorination, to improve the sanitary state of a water object, and to optimize self-purification processes; and its introduction into practice can yield considerable economic benefits. This method meets the current hygienic and ecological requirements and aims at rationally using natural resources and protecting human health.