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Late Glacial and Holocene changes in vegetation cover and climate in southern Siberia derived from a 15 kyr long pollen record from Lake Kotokel

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Academic year: 2020

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Fig. 1. Simplified maps of northern Eurasiaarea (A), the Lake Baikal region (B) and the Lake Kotokel (52◦47′ N, 108◦07′ E, 458 m a.s.l.) study (C), showing locations of the analysed core KTK1 (a star) and other sites with published quantitative palaeoclimatic records from theregion (triangles).
Fig. 2. Simplified pollen percentage diagram of the KTK1 core from Lake Kotokel. Pollen analyst E
Fig. 3. Local pollen assemblages zones (A) and time series of individual vegetation types (biomes) dominating in the study area since 15 kyrBP (B), along with the qualitative characteristics of vegetation (C), and quantitative changes in woody cover percentages (D) derived fromthe KTK1 pollen record, plotted along the time axis.
Fig. 4. Summary chart showing a comparison of three climatic variables (A–C): annual precipitation (Pann) and mean temperatures of thewarmest (Tw) and coldest month (Tc) derived from the KTK1 pollen record (dashed lines indicate most probable values and smoothed linesare three-point moving averages shown for each reconstructed variable), along with oxygen isotope records from the stalagmite D4, DonggeCave, China, as indicator of the Pacific (summer) monsoon intensity (D), and from the GISP2 ice core, as indicator of the North Atlantictemperature change (E), plotted along the time axis.

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