Description
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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Metrics Over Time
Publication Details
DOI
Publisher
PANGAEA
Subfield
Plant Science
Field
Agricultural and Biological Sciences
Domain
Life Sciences
Confidence Score
98%
Source
Open Alex
Keywords
DEPTH, sediment/rockAbies nordmannianaAcerAlnusArtemisiaBetulaBoraginaceaeBotrychium lunariaCampanulaCarpinus betulusCarpinus orientalisCaryophyllaceaeCastanea sativaCerealia-typeChenopodiaceaeCichoriumCirsiumCompositaeConvolvulaceaeCorylusCyperaceaeDaphneDipsacaceaeDryopterisEquisetumFagus orientalisGeraniaceaeGramineaeHuperzia selagoIndeterminable: unknownIridaceaeJuglans regiaJuniperusLabiataeLeguminosaeLiliaceaeLycopodium undifferentiatedOnagraceaePicea orientalisPinusPlantaginaceaePlumbaginaceaePolygonaceaePolypodiaceae undifferentiatedPteridium undifferentiatedQuercusRanunculaceaeSalixSaxifragaceaeSorbusSphagnumTaraxacumTiliaUlmusUmbelliferaeValerianaVeronicaHand auger (drill)