Pollen profile AMTKEL, Amtkel, Georgia

The rock mass of fluvial and fluvioglacial deposits of the Late Holocene has been studied at the altitude of 1830 m a.s.l. using the palynologic, carpologic, geomorphologic, and geochronologic methods. It was ascertained that in the mid-Subatlantic period the area of the present-day beech elfin wood...

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Bibliographic Details
Main Authors: Kvavadze, Eliso V, Rukhadze, L P, Tretyak, P R, Petrenko, L V
Format: Dataset
Language:English
Published: PANGAEA 1987
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.738965
https://doi.org/10.1594/PANGAEA.738965
Description
Summary:The rock mass of fluvial and fluvioglacial deposits of the Late Holocene has been studied at the altitude of 1830 m a.s.l. using the palynologic, carpologic, geomorphologic, and geochronologic methods. It was ascertained that in the mid-Subatlantic period the area of the present-day beech elfin woodland was occupied by a belt of alpine meadows. Thus, the lower border of alpine meadows ran 370-400 m lower than the recent level, pointing to a rather significant cooling of the climate that occurred from ca 2nd cent. A.D.