Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland

Danuta J. MICHCZYŃSKA et al.


The central part of Europe during the last cold stage was occupied by permafrost and twice invaded by the Scandinavian ice sheet, but about 70% of time was taken by transitional phases of continuous fluctuations of permafrost, which are reflected especially in type and thickness of slope, fluvial and aeolian deposits

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