geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2844Research ArticleНаучные сообщенияShort communicationsПроявление эоловых процессов в плейстоцене на юге Западной Сибири и их геоморфологические последствияPleistocene eolian processes in southern West Siberia and their geomorphic consequencesИлларионовА. Г.IllarionovA. G.Удмуртский государственный университетРоссия19891012202203Геоморфология6571Copyright © Илларионов А.Г., 20222022Илларионов А.Г.Illarionov A.G.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/2844

Several stages of the eolian morphogenesis are distinguished; the youngest one is dated back to the Pleistocene-Holocene boundary, older one- about 15,000 years ago, and the third - at the beginning of the Karginsk (mid-Late Pleistocene) interstadial. Still earlier phases of eolian processes can be traced in sequences of loess and similar deposits. Stages of eolian morphogenesis and loess sedimentation are supposed to correspond to certain regime of the atmospheric circulation.

Several stages of the eolian morphogenesis are distinguished; the youngest one is dated back to the Pleistocene-Holocene boundary, older one- about 15,000 years ago, and the third - at the beginning of the Karginsk (mid-Late Pleistocene) interstadial. Still earlier phases of eolian processes can be traced in sequences of loess and similar deposits. Stages of eolian morphogenesis and loess sedimentation are supposed to correspond to certain regime of the atmospheric circulation.

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The authors declare that there are no conflicts of interest present.