Late Glacial vegetation changes in the Kostroma Volga region based on pollen study of Lake Chukhlomskoye bottom sediments
DOI:
https://doi.org/10.31951/2658-3518-2024-A-4-642Keywords:
reconstruction of paleolandscapes, lacustrine sediments, pollen analysis, Final Pleniglacial, Late GlacialAbstract
The article presents the results of a palynological study of Lake Chukhlomskoye bottom sediments. Pollen analysis in combination with the results from 14C and 137Cs dating made it possible to reconstruct the main stages of changes in plant communities in the Kostroma Volga region at the end of the Pleniglacial and during the Late Glacial: 19.5–16.9 cal. ka BP – periglacial steppe, 16.9–14.7 cal. ka BP – birch periglacial forest-steppe, 14.7–12.7 cal. ka BP – spruce and birch-spruce forests and open woods with periglacial-steppe and meadow communities, 12.7–11.7 cal. ka BP – birch periglacial forest-steppe with rare participation of spruce.
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This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
This work is distributed under the Creative Commons Attribution-NonCommercial 4.0 International License.