Startseite Lebenswissenschaften Identifying white spots on the roadmap of Late Pleistocene and Holocene palaeolimnology in Slovakia: Review and future directions
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Identifying white spots on the roadmap of Late Pleistocene and Holocene palaeolimnology in Slovakia: Review and future directions

  • Jaroslav Stoklasa , Daniela Dobríková , Lucia Sochuliaková , Radovan Pipík und Ladislav Hamerlík EMAIL logo
Veröffentlicht/Copyright: 29. Dezember 2017
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Biologia
Aus der Zeitschrift Biologia Band 72 Heft 11

Abstract

Paleolimnological research in the territory of Slovakia has relatively short history with the beginning in the 1990s primarily as a response to the ecological changes in mountain lakes due to air pollution and missing data from the pre-industrial period as well as a need to quantify anthropic impact on the landscape. In the present paper, we reviewed 53 publications, including research papers, monographs, conference abstracts and theses, dealing with aquatic proxies in Holocene lake sediments to identify (1) the location of surveyed sites, (2) proxies used, and (3) the object of the paleolimnological reconstructions. The vast majority (37) of the analysed paleolimnological localities (51) took place in the High Tatra Mountains, focusing on the alpine lakes of glacial origin. The most frequently used biological proxy was Chironomidae remains (44%). In contrast, Cladocera, Ostracoda, loss-on-ignition, molluscs and stable isotopes were used only in 10–12% of studies. Most studies (84%) focused on a simple ecological reconstruction of the past environment, and only 24% of the studies attempted to reconstruct specific ecological variables, properties and processes, such as acidification (10%), temperature (8%) and eutrophication (4%). Only 2% of the studies used molecular techniques. Sixteen out of the 51 cores analysed (i.e., 31%) were dated by radiometric methods. In the end of our review we pinpoint the weaknesses of the local paleolimnological research and sketch possible future directions.

Acknowledgements

The study was co-financed by projects VEGA 1/0664/15, VEGA 2/0056/15 and APVV-15-0292 ’Deglaciation and postglacial climatic evolution recorded in the lake deposits of the High Tatra Mountains’. The projects was also funded by the National Science Centre, Poland, contract no. 2015/19/P/ST10/04048 and the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement No. 665778. We are grateful to Mats Rundgren (Lund University, Sweden) for calibration of the radiometric ages, Peter Bitušík and Tímea Chamutiova (Matej Bel University) for commenting on the manuscript.

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Received: 2017-4-5
Accepted: 2017-10-11
Published Online: 2017-12-29
Published in Print: 2017-11-27

© 2017 Institute of Zoology, Slovak Academy of Sciences

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