Fossil molluscan successions from ca 450 sites provide evidence of the paleo-environmental history of the Czech Republic and Slovakia during the Quaternary. They not only reflect the Quaternary cycle of warm and cold phases but also a number of various events, such as the impact of the cold oscillation at 8,2 ky BP or the detailed reconstruction in time and space of the habitat patchwork in areas where other fossils are sparse or absent, particularly in karstlands, in the full scale of elevations. and Vojen Ložek.