Record details

Title
    Palynological Studies from the Ochozská Cave and from the Šošůvka Part of the Sloupsko-Šošůvská Cave (Moravian Karst)
Statement of responsibility
    Nela Doláková
Other titles
    Upper Pleistocene and Holocene Climatic Variations (Variant.)
Author
    Doláková, Nela
Language
    anglicky
Source title - serial
    Geolines
Vol./nr.
    Vol. 11
Pages
    p. 172-174
Year
    2000
Notes
    1 obr., 13 bibl.
    il.
    Zkr. název ser.: Geolines (Praha)
Subject group
    jeskyně
    kvartér
    kvartér Českého masivu
    paleoekologie
    paleoklimatologie
    palynologie
    speleotém
Geographical name
    ČR-Morava
    Moravský kras
    Ochoz u Brna (Brno-venkov)
    Sloup (Blansko)
    Šošůvka (Blansko)
Keyword
    Cave
    Karst
    Moravian
    Ochozská
    Palynological
    Sloupsko-Šošůvská
    Studies
    Šošůvka
Abstract (in english)
   From the Ochozská Cave the samples from the two profiles were studied. The lower parts of the profiles contained representants of the heliophilous cold steppes (Helianthemus, Thalictrum, Selaginella selaginoides, Ephedra), cold resistent wood plants (Pinus, Betula, Salix) and hydrophilous plants and alges (Cyperaceae, Botryococcus, Pediastrum). These belong most likely to the one cold phase of the Late Glacial. In the upper part of the profiles high amounts of the gemus Tilia and of the family Polypodiaceae were found. This accumulation was probably caused by special conditions during the sedimentation and it is probably of the Early Holocene age. From the Šošůvka Cave individual samples were studied. They contained above all the steppe elements (Thalictrum, Galium, Centaurea, Asteraceae, Ranunculaceae, Daucaceae, Poaceas) and a small amount of the trees pollen (Pinus silvestris, P. cembra, Betula, Tilia, Alnus).
   Some samples contain cold elements (Selaginella selaginoides, Botrychium), other warmer ones (Teucrium, Scabiosa). Their age are still not determined. The sediments from the Kůlna cave are dated archeologically. Their palynospectra are similar to the inner part of the Šošůvka cave and they may be used for comparison with the above mentioned ones
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    28. 3. 2008
Import date
    8. 8. 2012