Record details

Title
    Palynological research in the Šumava Mountains
Statement of responsibility
    Eva Břízová
Other titles
    Palynologický výzkum Šumavy
    Proceedings of The MAB UNESCO's conference Geo-biodiversity of the Bohemian/Bavarian Forest: Trilateral Research, Conservation and Management of the Frontier Mountains (Variant.)
Author
    Břízová, Eva
Language
    česky
Source title - serial
    Silva Gabreta : sborník vědeckých prací ze Šumavy
Vol./nr.
    Roč. 1
Pages
    s. 109-113
Year
    1996
Notes
    2 s.bibl.
    Anglické resumé
    Zkr. název ser.: Silva Gabreta
Subject group
    holocén
    jezero ledovcové
    kvartér Českého masivu
    palynologie
    rašeliniště
    sedimentace lakustrinní
Geographical name
    ČR-Čechy
    Šumava
Keyword
    Mountains
    Palynological
    Research
    Šumava
Abstract (in english)
   Peat bogs are prominent and specific ecosystem in the Šumava Mts. They have an important and exceptional value; they keep recording information about their own recent and ancient past, about the vegetational history and factors of natural environment in the nearby and more distant landscape. This information is obtainable by means of paleobotanical methods, such as the pollen and macroscopic analyses. In the past, scientific studies of the Šumava Mts. were generally scarce, owing to their location in the frontier area. They are also little known palynologically. - Along with the geochemical investigation, pollen analysis of the upper part of Jezerní Mire section (thickness 0.26 m) was carried out, and dated by the newly applied 210 Pb method (VILE & al. 1995).
   Besides studying the peat bog sediments by means of pollen analysis, it was also suitable to apply this method to the lacustrine sediments of the Šumava lakes, i.e., to Černé Lake (Břízová 1991a, b, 1993, 1995; Reissinger 1930, 1931; Řeháková 1991 - diatoms) and Čertovo Lake (Břízová 1991a, b, 1993, 1995; Veselý & al. 1993), the latter sediments being also used for geochemical study (Veselý 1994). Their thickness was 1.15 m and 0.8 m, respectively. The analysed deposits date back to the younger Subatlantic period (Period X - by Firbas 1949, 1952)
Contributor
    Česká geologická služba
Contributor code
    ČGS (UNM)
Source format
    U
Entered date
    20. 2. 2008
Import date
    8. 8. 2012