Abstract

This article presents the results of a comprehensive geochronological study of gyttja deposits from a section of a terrace above a floodplain located on the right bank of the Ob River near the town of Kolpashevo. According to the 230Th/U dating, the age of the gyttja could be dated in the range of 110–95 kyr. The results of spore–pollen analysis suggest that the gyttja deposit was formed in the period of a wide distribution of middle taiga forest landscapes with the dominance of spruce; the climatic conditions were similar to modern ones. These events probably took place in the interstadial time during MIS-5c or at the end of Kazantsevo interglacial period.

Original languageEnglish
Pages (from-to)370-379
Number of pages10
JournalContemporary Problems of Ecology
Volume10
Issue number4
DOIs
Publication statusPublished - 1 Jul 2017

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Scopus subject areas

  • Environmental Science(all)

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