The features of peat-accumulation process at the southern slope of the Great Vasyugan Bog

摘要: The peat-forming process of the southern margin taiga zone in West Siberia depends on climatic fluctuations, which have an effect peat stratigraphy and chemical composition peat. It is shown that contemporary warming does not interrupt bog formation, due to lateral flooding by water came from adjoining peatlands periodical waterlogging floodplain depressions during years excessive supply.