Dating of late Pleistocene glaciations in Mediterranean key sites

冰川推进的年代测定是在晚更新世寒冷时期重建地中海规模的山地气候的重要贡献。这样的重建可以追踪水汽从地中海中部盆地向北部和东部的输送。在东南欧，这项初步研究的主要目标地区，到目前为止几乎没有冰雹矿床的年代学。目标区的冰雹矿床缺乏局部和区域相关性。因此，通过测定宇宙成因的Be的方法，需要一个强有力的冰雹矿床的地层框架。在南喀尔巴鄂中部横断面的试验性实地研究中，当地的冰川序列被采样，这表明与全新世早期相比，最后一次冰盛期来自南方的水汽平流更强。对项目KU 1298/13的审查建议进行一项类似的试验性研究，并设想在保加利亚的里拉山进行这项研究。与科西嘉岛的乌尔面晚期样品(项目KU1298/7-3)相似，来自南喀尔巴山区的提纯石英样品已准备好用于目标制备，但缺乏外部测量资金，特此请求。

Dating of glacial advances is an important contribution for the reconstruction of Mediterranean-scale mountain climate during cold spells of the Late Pleistocene. Such reconstructions allow tracking of moisture transport from the central Mediterranean basin towards the north and east. In southeastern Europe, the main target region of this pilot study, almost no chronology of moraine deposits exist so far. The moraine deposits in the target regions are lacking both local and regional correlation. Thus, a robust stratigraphic framework for moraine deposits by means of dating cosmogenic Be is required. During a pilot field study in a cross section of the central South Carpathians, local moraine successions have been sampled which indicate a stronger moisture advection from the south during the Last Glacial Maximum, as compared to the early Holocene. A similar pilot study is recommended by review of project KU 1298/13 and envisaged in the Rila massiv of Bulgaria. Purified quartz samples from the South Carpathians are ready for target preparation, similar to late Wuermian samples from Corsica (project KU1298/7-3), for which funding external measurements is lacking and requested herewith.