Number of the records: 1  

Sur, a former late-glacial and Holocene lake at the westernmost margin of the Carpathians

  1. 1.
    0397874 - ÚACH 2014 RIV CZ eng J - Journal Article
    Petr, L. - Žáčková, P. - Matys Grygar, Tomáš - Píšková, Anna - Křížek, M. - Treml, V.
    Sur, a former late-glacial and Holocene lake at the westernmost margin of the Carpathians.
    Preslia. Roč. 85, č. 3 (2013), s. 239-263. ISSN 0032-7786. E-ISSN 0032-7786
    Institutional support: RVO:61388980
    Keywords : Geochemistry * Geomorphology * Multi-proxy reconstruction * Palaeobotany * Palaeolimnology * Pannonia
    Subject RIV: DD - Geochemistry
    Impact factor: 2.778, year: 2013

    There is a unique palaeolimnological record of the late-glacial and Holocene periods in the former lake Šúr near Bratislava in western Slovakia. The aim of this study was to reconstruct the development of the environment in the locality of the lake, including the gradual infilling of the lake. We reconstructed the development of the lake environment by combining results of a geochemical analysis with analyses of diatoms and plant macrofossils.We also carried out a pollen analysis to assess the changes in the surrounding terrestrial vegetation. The results reveal how the character of the lake has changed over time. At the peak of the glacial period, water flowed through the lake and deposited sand there. Later on the flowofwater through the lake ceased and a vast oligotrophic lake developed. During the Holocene, the lake gradually became eutrophic. The pollen record contains evidence of the occurrence of woody species of broad-leaved forest in the late-glacial period in the Carpathians and of the expansion of mixed forests of Fagus and Carpinus in the Holocene around 4500 BP. The development of the vegetation in the locality of lake Šúr is more similar to that at localities in Hungary than those situated north and west of the Western Carpathians.
    Permanent Link: http://hdl.handle.net/11104/0225479

     
     
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.