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Titlebook: Long Continental Records from Lake Baikal; Kenji Kashiwaya (Professor) Book 2003 Springer Japan 2003 Holozän.Insolation.Lacustrine records

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Paleoclimate Records from the Lake Baikal Sediments and Lava Formations of the South Baikal Volcanicres, which contain almost no diatoms around the Matuyama/Gauss paleomagnetic reversal boundary. The glacial clay layers are interpreted as being linked with the growth of young mountain ranges around Lake Baikal, where glaciers could develop at a height of 2000m or more. This cooling phase is coinci
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Paleoenvironmental Changes in the Eurasian Continental Interior during the Last 12 Million Years Deroic acids, .-C. and .-C., reflects the fact that the dominant plants of the Lake Baikal basin were . spp., . spp., . spp., etc. Normal-C. alkane is mainly attributed to conifers and herbaceous plants, and has increased from 1 Myr ago to the present. C. stanol/sterol ratios suggest that the lake bott
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