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We describe the penultimate glacial – last interglacial transition from the one of the numerous palaeolake successions in central Poland, which have yielded many documented Eemian and Early Weichselian floral records. In the new profile, Parchliny 2016, the lacustrine deposits were analysed lithologically, botanically, zoologically, and geochemically, providing new data that illustrate the environmental transition from the Late Saalian (MIS 6a) to the Eemian interglacial (MIS 5e). Five phases of palaeolake development have been distinguished. The first phase was related to the rapid melting of a dead ice block buried in the tills to form a lake. The second phase documented a Late Saalian initial succession, with the dominance of open steppe communities (Stadial 1), followed by a third phase with gradual increasing density of vegetation, the spread of boreal forests (Zeifen interstadial) and further increase in open communities and the retreat of pine (Kattegat stadial). The fourth phase reflected the beginning of Eemian interglacial by the expansion of pioneering birch-pine and purely birch forests and an increasing proportion of deciduous trees, including oak (Vth phase). Diatom, cladoceran and geochemical studies indicate at least two stages of lake development. The first stage (Late Saalian) was of an open lake (2–4 m deep), in relatively cold conditions and nutrient-poor water with the lowest amounts of organic carbon and nitrogen. The second stage (Eemian interglacial), shows warmer, shallower conditions in which the lake’s primary production increased, the water was well oxygenated, and there were more trophic levels.
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art. no. 31
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Bibliogr. 133 poz., fot., rys., tab., wykr.
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- University of Warsaw, Institute of Geology, Żwirki and Wigury 93, 02-089 Warszawa, Poland
- University of Łódz, Department of Geology and Geomorphology, Narutowicza 88, 90-139 Łódź, Poland
autor
- University of Wrocław, Institute of Geography and Regional Development, Plac Uniwersytecki 1, 50-137 Wrocław, Poland
autor
- University of Wrocław, Institute of Geological Sciences, Cybulskiego 34, 50-205 Wrocław, Poland;
- Polish Academy of Sciences, Institute of Geological Sciences, Twarda 51/55, 00-818 Warszawa, Poland
autor
- Pomeranian University in Słupsk, Institute of Biology and Earth Sciences, Partyzantów 27, 76-200 Słupsk, Poland
autor
- Adam Mickiewicz University in Poznań, Biogeochemistry Research Unit, Krygowskiego 10, 61-680 Poznań, Poland
autor
- University of Wrocław, Faculty of Biological Sciences, Department of Plant Developmental Biology, Kanonia 6/8, 50-328 Wrocław, Poland
autor
- Wroclaw University of Environmental and Life Sciences, Department of Botany and Plant Ecology, Plac Grunwaldzki 24a, 50-328 Wrocław, Poland
autor
- Polish Geological Institute – National Research Institute, Holy Cross Branch, Zgoda 21, 25-953 Kielce, Poland
autor
- University of Wrocław, Institute of Geography and Regional Development, Plac Uniwersytecki 1, 50-137 Wrocław, Poland
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Uwagi
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-2899d006-1cef-4c2d-912c-a80615d23bba