Reconstructing the vegetation of forest and alpine-steppe landscapes in the southwestern part of Tuva since the Late Glacial period till the present |
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| Affiliation: | 1. Department of Physical Geography and Geoecology, Charles University in Prague, Faculty of Science, Albertov 6, 128 42 Praha 2, Czech Republic;2. Laboratoire Image, Ville, Environnement, UMR 7362, CNRS/ Université de Strasbourg, 3, rue de l''Argonne, 67083 Strasbourg Cedex, France;3. Department for Landscape Protection and Environmental Geography, University of Debrecen, Egyetem tér 1, P. O. Box 9, H-4010 Debrecen, Hungary;4. Institute of Ecology and Botany, Centre for Ecological Research, Inst Ecol & Bot. Hung Acad. Sci., Alkotmány 2-4, 2163 Vácrátót, Hungary;5. Paléotime, 6173 rue Jean Séraphin Archard-Picard, 38250 Villard-de-Lans, France;6. ANTEA Archéologie, 11 rue de Zurich, 68442 Habsheim, France;7. Institute of Archaeology of Academy of Science of the Czech Republic, Letenská 4, 11801 Praha 1, Czech Republic;1. University of East Anglia, School of Environmental Sciences, Norwich Research Park, Norwich NR4 7TJ, UK;2. HYDEA S.p.A., Via del Rosso Fiorentino 2/g, 50142 Florence, Italy;1. University of Marburg, Institute of Prehistoric Archaeology, Biegenstrasse 11, Marburg, Germany;2. University of Cologne, Institute of Geography, Cologne, Germany;1. Institute of Biological, Environmental and Rural Sciences, Aberystwyth University, Penglais, Aberystwyth SY23 3DA, UK;2. School of Environment, Natural Resources and Geography, Bangor University, Bangor LL57 2UW, UK;3. Institute of Forest Ecology, University of Natural Resources and Life Sciences, 1190 Vienna, Austria;1. Laboratory of Mineralogy and Petrology (Luminescence Research Group), Department of Geology and Soil Science, Ghent University, Krijgslaan 281 (S8), B-9000 Gent, Belgium;2. Department of Earth Sciences, Faculty of Earth and Life Sciences, Vrije Universiteit Amsterdam, The Netherlands |
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| Abstract: | On the basis of the spore-pollen, lithological and radiocarbon analysis of sediments from two lakes lying on a high-mountain plateau in the southwestern part of Tuva, the changes in vegetation, climate and landscapes have been reconstructed from 14645 years ago till the present. |
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