Lösse und Paläoböden der letzten Kaltzeit im mediterranen Raum

Karl Brunnacker
Deposits and structure of loess profiles from the mediterranean region are discussed and interpreted as climate indicators of the last glacial period. For want of precise stratigraphic points we move step by step from the middle-European periglacial-region to the south. The zone, characterized by winterrain, has not changed during the last glacial period. Near by the northern border of that zone in the south-east of Europe relics for the temperate warm middle-European flora and fauna...