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Fossil Rodent Burrows in Frozen Late Pleistocene Beds of the Kolyma Lowland

机译:化石啮齿动物在科里马低地的晚更新世晚期的冰层中钻洞

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摘要

The structure and contents of fossil rodent burrows dated 28-32 ka from the frozen Late Pleistocene ice-loess beds of the Kolyma Lowland (northern Yakutia) were studied. The examination of paleoecological material (plants, fruits and seeds, insects, bones, hair, etc ) allowed the reconstruction of environmental conditions for extinct rodents. Their characteristic features included an arid and severe climate, a small depth of inhabited strata, and a wide distribution of disturbed habitats with pioneerand steppe vegetation in areas with relatively flat topography typical of the study region. Comparative analysis of the structure and contents of fossil and present-day suslik burrows provided detailed data on the differences between natural conditionsin local habitats of the Kolyma Lowland in the Holocene and Pleistocene.
机译:研究了科利马低地(北雅库特)的晚更新世冰冻黄土层中28-32 ka的化石啮齿动物洞穴的结构和内容。对古生态材料(植物,水果和种子,昆虫,骨头,头发等)的检查使灭绝啮齿动物的环境条件得以重建。它们的特征包括干旱和严峻的气候,较小的居住地层以及受干扰的生境的广泛分布,这些生境分布在研究区域典型地势相对平坦的地区,具有先驱和草原植被。对化石和当前的苏式洞穴的结构和含量的比较分析,提供了关于全新世和更新世科雷马低地当地栖息地自然条件之间差异的详细数据。

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