Palynological characteristic of the series of lacustrine and paludal deposites of the Holocene in the headwaters of the Zakan River (Western Caucasus).

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Kvavadze et al. 1994: Palynological studies of the deposits of the Luganski bog situated at an altitutde of 2428 m have shown that glacial lakes repeatedly emerged there during the Holocene. They used to exist for rather a long time during the Atlantic. More shortterm lake basins reappeared at the very end of the Subboreal period and during the climatic optimums 1000 BP and 400-500 BP.

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Kvavadze, Eliso V; Efremov, Yurii Y; Bukreeva, G V; Akatov, V V (1994): Palynological characteristic of the series of lacustrine and paludal deposites of the Holocene in the headwaters of the Zakan River (Western Caucasus). Bulletin of the Georgian National Academy of Sciences, 150, 177-184, hdl:10013/epic.37430.d001

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