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In general, the evolution of fluvial systems in Central-Eastern Europe reflects the main phases of climatic changes during the period of 60–8 ka cal BP registered in Greenland ice cores and their isotopic 18O curves. The Greenland isotope curve shows many more wiggles and stages than the fluvial record of the same time, especially during the Interpleniglacial phase. In Central-Eastern Europe, we observe...
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