Late Holocene vegetation history of the Western Caucasus inferred from high-resolution pollen record from Lake Karakel

Авторы: Chepurnaya A.A., Novenko E.Y., Aleksandrin M.Y.
Журнал: Limnology and Freshwater Biology
Номер: 4
Год издания: 2022
Издательство: Лимнологический институт Сибирского отделения Российской академии наук
Местоположение издательства: Иркутск
Первая страница: 1408
Последняя страница: 1411
DOI: 10.31951/2658-3518-2022-a-4-1408
Аннотация: The paper presents a new paleoecological evidence for the last 2200 years based on highresolution pollen record and detail radiocarbon dating, obtained from Lake Karakel (Teberda Rivervalley, Western Caucasus). The obtained results showed that vegetation changes from 2200 to stage1200 cal, yr BP occurred under a climate warming and increase of humidity. The Medieval ClimaticAnomaly-MCA (ca. 1200-880 cal. yr BP) was characterized in this region by the predominance ofbroadleaved forests. The MCA was followed by a cold interval of the Little Ice Age (ca. 880-120 calyr BP) that marked by expansion of pine, spruce and fir forests to the lower altitude the present time.
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