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New data on age and conditions of buried organic-rich sediments formation in the Nentral Ob River

机译:临床博河埋藏有机沉积物的年龄和条件的新数据

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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 Th-230/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.
机译:本文介绍了Gyttja矿床的综合性地理学研究,从位于Kolpashevo镇的ob河右岸的洪水平台上方的露台上。 根据Th-230 / U约会,Gyttja的年龄可以在110-95 Kyr的范围内。 孢子花粉分析的结果表明,在云杉的主导地位,在云杉中间Taiga森林景观的广泛分布期内形成了Gyttja矿床; 气候条件与现代人相似。 这些事件可能在MIS-5C期间或在Kazantsevo中间批峡地区结束时发生在鸿沟时间。

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