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Chronology of the last ice sheet decay on the southern Baltic area based on dating of glaciofluvial and ice-dammed lake deposits

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Abstrakty
EN
The paper presents the results of the first OSL dating of glaciofluvial and ice-marginal lake sediments which occur between end moraines of the Słupsk Bank and the Polish coast. The sand and gravel of glaciofluvial deltas on the Słupsk Bank were deposited most likely during a period from 14.3 ±1.2 to 16.6 ±1.4 ka ago. The deposition of silty-sandy sediments of the ice-marginal lake is dated at 14.51 ±0.81 and 14.6 ±1.4 ka years. Likewise, dates ranging from 13.74 ±0.84 to 16.70 ±1.1 ka obtained from low sandy ridges, related to the southern range of the ice-marginal lake in the Gardno-Łeba Lowland, indicate the most likely timing of their deposition. It can be concluded that a short stop of the ice sheet on the Słupsk Bank took place approximately 15.2 ka ago, which could be correlated with the position of the ice sheet front in central Skåne and in northern Lithuania at that time. Older and younger results were also obtained, except the dates mentioned above. The older ages show little sunlight exposure of sediments during their deposition. The younger dates indicate a marine origin of the sediments and show that some parts of glaciofluvial sediments were redeposited and exposed to sunlight at a later stage, most probably when dead-ice blocks were melting.
Rocznik
Strony
193--208
Opis fizyczny
Bibliogr. 64 poz., fot., mapa, rys., tab., wykr.
Twórcy
  • Polish Geological Institute - National Research Institute, Branch of Marine Geology, Kościerska 5, 80-328 Gdańsk, Poland
  • Silesian University of Technology, Institute of Physics – Centre for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland
  • Silesian University of Technology, Institute of Physics – Centre for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland
  • Polish Geological Institute - National Research Institute, Branch of Marine Geology, Kościerska 5, 80-328 Gdańsk, Poland
autor
  • Polish Geological Institute - National Research Institute, Branch of Marine Geology, Kościerska 5, 80-328 Gdańsk, Poland
  • Polish Geological Institute - National Research Institute, Branch of Marine Geology, Kościerska 5, 80-328 Gdańsk, Poland
autor
  • Silesian University of Technology, Institute of Physics – Centre for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland
  • Polish Geological Institute - National Research Institute, Branch of Marine Geology, Kościerska 5, 80-328 Gdańsk, Poland
  • Silesian University of Technology, Institute of Physics – Centre for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland
  • Silesian University of Technology, Institute of Physics – Centre for Science and Education, Konarskiego 22B, 44-100 Gliwice, Poland
  • Polish Geological Institute - National Research Institute, Branch of Marine Geology, Kościerska 5, 80-328 Gdańsk, Poland
  • Polish Geological Institute - National Research Institute, Branch of Marine Geology, Kościerska 5, 80-328 Gdańsk, Poland
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Uwagi
Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-8bfb5cd4-60d6-4728-bd3b-0ed6259b9149
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