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Instability of the environment at the end of the Eemian Interglacial as illustrated by the isopollen maps for Poland

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EN
Abstrakty
EN
Many terrestrial pollen profiles from Poland (and a few pollen records from other parts of Central Europe) show the end of the last interglacial (Eemian, MIS 5e) to have been characterized by climatic and environmental instability. This is expressed by a strong, rapid cooling in the middle part of the pine phase ending this interglacial (E7 regional pollen assemblage zone), and then a re-warming at the very end of this phase, immediately before the transition to the glacial conditions of the last glaciation (Vistulian, Weichselian, MIS 5d). We have characterized the regional distribution of these climatic fluctuations in Poland on the basis of isopollen maps prepared for the Eemian Interglacial based on palynological data from 31 Polish pollen profiles. These maps show unequivocally that the intra-interglacial cooling at the end of the Eemian Interglacial was a transregional phenomenon, which was reflected very clearly by a temporary openness of vegetation across the whole of Poland. It was associated with a distinct decrease in pine forest areas and an increase in birch forests and open communities of cold steppe type with a domination of Artemisia. The pronounced climate and environment instability during the last phase of the Eemian Interglacial may be consistent with it being a natural phenomenon, characteristic of transitional stages. Taking into consideration the currently observed global warming, coinciding with a natural cooling trend, the study of such transitional stages is important for understanding the underlying processes of climate change.
Rocznik
Strony
225--237
Opis fizyczny
Bibliogr. 112 poz., rys., tab.
Twórcy
  • University of Białystok, Department of Botany, Institute of Biology, Ciołkowskiego 1J, 15-425 Białystok, Poland
  • Polish Geological Institute - National Research Institute, Carpathian Branch, Skrzatów 1, 31-560 Kraków, Poland
autor
  • Polish Academy of Sciences, Władysław Szafer Institute of Botany, Lubicz 46, 31-512 Kraków, Poland
autor
  • Maria Skłodowska-Curie University, Department of Geoecology and Palaeogeography, Faculty of Earth Sciences and Spatial Management, Kraśnicka 2cd, 20-718 Lublin, Poland
autor
  • AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, al. A. Mickiewicza 30, 30-059 Kraków, Po land
autor
  • University of Łódź, Department of Geomorphology, Institute of Earth Sciences, Narutowicza 88, 90-139 Łódź, Poland
autor
  • University of Białystok, Department of Botany, Institute of Biology, Ciołkowskiego 1J, 15-425 Białystok, Poland
autor
  • Adam Mickiewicz University, Department of Biogeography and Palaeoecology, Institute of Geoecology and Geoinformation, Dzięgielowa 27, 61-680 Poznań, Poland
autor
  • University of Warsaw, Departmentof Climate Geology, Institute of Geology, Żwirkii Wigury 93, 02-089 Warszawa, Poland
  • University of Wrocław, Laboratory of Palaeobotany, Department of Stratigraphical Geology, Institute of Geological Sciences, Cybulskiego 30, 50-205 Wrocław, Poland
autor
  • University of Silesia, Department of Fundamental Geology, Faculty of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland
  • University of Silesia, Department of Fundamental Geology, Faculty of Earth Sciences, Będzińska 60, 41-200 Sosnowiec, Poland
autor
  • Polish Geological Institute - National Research Institute, Rakowicka 4, 00-975 Warszawa, Poland
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Uwagi
Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-2a5de6f3-7792-4c62-987b-640c7c301772
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