Chronology of the glaciation of the Southern Black Forest after the Late Pleistocene glaciation maximum

在更新世晚期，中欧低山脉的最高区域暂时被较小的冰盖和冰川覆盖。黑森林南部的冰川作用主要集中在黑森林的最高海拔（Feldberg：1493 m）及其周边地区。根据以往的年龄测定，晚更新世冰川在大多数低山脉的最大值落在海洋同位素阶段2（30-15 ka），但很少有人知道的时间冰川消退。该项目的目的是全面重建南部黑森林最后一次冰川消退的年表。这应该能够得出结论，在晚更新世中欧上空的大气环流。

During the Late Pleistocene, the highest regions of the low mountain ranges of Central Europe were temporarily covered by smaller ice caps and glaciers. The glaciation of the southern Black Forest was mainly concentrated on the highest elevation of the Black Forest (Feldberg: 1493 m), and the surrounding region. According to previous age determinations, the late Pleistocene glaciation maxima in most of the low mountain ranges fall into marine isotope stage 2 (30-15 ka), but little is known about the timing of deglaciation. The aim of the project is a comprehensive reconstruction of the chronology of the last deglaciation of the southern Black Forest. This should enable conclusions to be drawn about the atmospheric circulation over Central Europe during the late Pleistocene.