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\u0441\u0442\u0440\u043e\u0435\u043d\u0438\u044f \u042112-\u042121 \u0441 \u0447\u0435\u0442\u043d\u044b\u043c \u043c\u0430\u043a\u0441\u0438\u043c\u0443\u043c \u042116, \u0447\u0442\u043e \u043f\u0440\u0438 \u043f\u043e\u0432\u044b\u0448\u0435\u043d\u043d\u043e\u043c \u0441\u043e\u0434\u0435\u0440\u0436\u0430\u043d\u0438\u0438 \u0433\u043e\u043f\u0430\u043d\u043e\u0432\u044b\u0445 \u0441\u0442\u0440\u0443\u043a\u0442\u0443\u0440 \u043d\u0438\u0437\u043a\u043e\u0439 \u0441\u0442\u0435\u043f\u0435\u043d\u0438 \u0442\u0435\u0440\u043c\u0430\u043b\u044c\u043d\u043e\u0439 \u0437\u0440\u0435\u043b\u043e\u0441\u0442\u0438 (\u0433\u043e\u043f-17(21)-\u0435\u043d\u043e\u0432, \u0433\u043e\u043f-13(18)-\u0435\u043d\u043e\u0432) \u043c\u043e\u0436\u0435\u0442 \u0441\u0432\u0438\u0434\u0435\u0442\u0435\u043b\u044c\u0441\u0442\u0432\u043e\u0432\u0430\u0442\u044c \u043e\u0431 \u0430\u043a\u0442\u0438\u0432\u043d\u043e\u043c \u0440\u0430\u0437\u0432\u0438\u0442\u0438\u043c \u0441\u043e\u043e\u0431\u0449\u0435\u0441\u0442\u0432 \u043c\u0435\u0442\u0430\u043d\u043e\u0442\u0440\u043e\u0444\u043d\u044b\u0445 \u0438 \u0445\u0435\u043c\u043e\u043e\u0440\u0433\u0430\u043d\u043e\u0442\u0440\u043e\u0444\u043d\u044b\u0445 \u043c\u0438\u043a\u0440\u043e\u043e\u0440\u0433\u0430\u043d\u0438\u0437\u043c\u043e\u0432.\n\n[ENG]\nThe detailed research of the dispersed organic matter of Lake Baikal bottom sediments including analysis of hydrocarbon molecular markers \u2013 n-alkanes, isoprenoids, terpanes and polycyclic aromatic hydrocarbons has been carried out. The distribution of homologues of n-alkanes and their ratios in bottom sediments of the Posol bank-2, where mud breccias, gas-hydrates (bottom stations St1GT3, St1GT8) and authigenic carbonates (St1GT3) were detected, has shown an input of the highly transformed organic matter to the surface sediments likely due to the erosion and redeposition of sediments of the last glacial maximum extension age. Molecular composition of dispersed organic matter of the Ostrov site sediments (St3GC4) attested to the normal type of deposition not influenced by migration processes. Increased values of \u042112-\u042121 n-alkanes with an even maximum at \u042116 have been detected in sediments of station St18GC6 collected near the thermogenic methane seep (Kedr mud volcano), and together with the presence of the low transformed hopane structures (hop-17(21)-enes and hop-13(18)-enes) can testify to the methanotrophic and concomitant chemoorganotrophic microorganisms development in sediments.", "subitem_description_type": "Abstract"}]}, "item_3_full_name_183": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "209", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "40241426", "nameIdentifierScheme": "KAKEN - \u7814\u7a76\u8005\u691c\u7d22", "nameIdentifierURI": "https://nrid.nii.ac.jp/ja/nrid/1000040241426/"}], "names": [{"name": "\u5357, \u5c1a\u55e3", "nameLang": "ja"}]}, {"nameIdentifiers": [{"nameIdentifier": "89765", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "50312450", 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