The paper generalizes the sub-fossil insect data from the 29 localities dated by the Late Pleistocene and Holocene, situated in the Northern part of West Siberia Plain and adjacent territories (the Urals and Bolshezemelskaya tundra). Based on the paleontological data, we try to reconstruct the development of entomofaunas during the Late Pleistocene and Holocene (130 thousand years ago). The dynamics of insect faunas corresponds to the main stages of development of the natural communities of this region, reconstructed on the basis of paleobotanical data. In particular, we described sub-fossil insect faunas with warm climate markers (such as ground beetles Trechus secalis ) for the Last (Eemian) interglacial period (130-115 thousand years ago). It is possible that some boreal beetle species ( Cychrus caraboides , Chlaenius costualtus ) changed their areas northwards in comparison with their modern distribution. Subsequent cooling (until the beginning of the Holocene, about 10 thousand years ago) caused the occurrence of cryophilic (arctic, tundra and subarctic) insects. During the Maximum of the Last glaciation (from 20 to 17 thousand years ago) these complexes reflected severe cold and dry climatic conditions. Insect assemblages from the Holocene layers of alluvial and boggy genesis show similarities with modern insect faunas from these territories. We found boreal species (xylobionts and forest duff inhabitants) in the same Holocene sediments associated with the remains of sub-fossil wood. These species are not found in modern insect communities of the Southern Yamal. These data correspond to the advancing northwards woody vegetation during the Holocene climatic optimum (6-5 thousand years ago). The sub-fossil insect data were compared with the results of paleobotanical studies, as well as with modern insect faunas from this area.
nasekomye, istoriya faun, pozdniy pleystocen, golocen, Zapadnaya Sibir', Ural
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