Pollen profile LUGAN, Luganskoe, Russia

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 v...

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Bibliographic Details
Main Authors: Efremov, Yurii Y, Kvavadze, Eliso V
Format: Dataset
Language:English
Published: PANGAEA 1995
Subjects:
Abies nordmanniana
Acer
Alnus
Artemisia
Betula
Boraginaceae
Botrychium lunaria
Campanula
Carpinus betulus
Carpinus orientalis
Caryophyllaceae
Castanea sativa
Cerealia-type
Chenopodiaceae
Cichorium
Cirsium
Compositae
Convolvulaceae
Corylus
Cyperaceae
Daphne
DEPTH
sediment/rock
Dipsacaceae
Dryopteris
Equisetum
Fagus orientalis
Geraniaceae
Gramineae
HADR
Hand auger (drill)
Huperzia selago
Indeterminable: unknown
Iridaceae
Juglans regia
Juniperus
Labiatae
Leguminosae
Liliaceae
LUGAN
Luganskoe
Russia
Lycopodium undifferentiated
Onagraceae
Picea orientalis
Pinus
Plantaginaceae
Plumbaginaceae
Polygonaceae
Polypodiaceae undifferentiated
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.739493
https://doi.org/10.1594/PANGAEA.739493
Description
Summary: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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