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Abstract
The article presents the results of a collective analysis of 181 radiocarbon and 38 luminescence dating results from the time range 50–11.7 cal kBP for samples originating in fluvial sedimentary environment in Łódź region (central Poland), south of the last glacial maximum (LGM) line. Four sites were selected for a general of fluvial deposits and the obtained dating results Struga Żłobnicka, Parchliny, Warenka, and Swędów regions. Based on the summed probability density function (PDF) curves, the study demonstrates the response of the fluvial sedimentary environment to events of overregional scale. The collective analysis of the radiocarbon age determinations from the Łódź region allows for observing the correlation between local environmental changes and large-scale changes recorded in the NGRIP core. The warming periods Greenland interstadials (GI)-3, GI-4, and GI-5.1, the cooling event GI-1b within the warming GI-1, as well as the transition between GI-1a and Greenland stadials (GS)-1, were most prominently recorded in the PDF curves. The collective analysis of the luminescence age determinations reflects a change in the river valleys, expressed by a strong aggradation during the cold maximum of the studied period.
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1 University of Łódź, Faculty of Geographical Sciences, Department of Geology and Geomorphology, Narutowicza 88, 90-139 Łódź, Poland
2 Silesian University of Technology, Institute of Physics - CSE, Division of Geochronology and Environmental Isotopic Research, Konarskiego 22B, 44-100 Gliwice, Poland
3 Polish Geological Institute - National Research Institute, Holy Cross Branch of Jan Czarnocki in Kielce, Zgoda 21, 25-378 Kielce, Poland
4 University of Wrocław, Institute of Geography and Regional Development, Cybulskiego 34, 50-205 Wrocław, Poland