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Molluscan and Vertebrate Successions from the Veľká Drienčanská Cave

Here we present a biostratigraphy of entrance deposits in the Veľká Drienčanská Cave based on molluscan and vertebrate successions in correlation with prehistoric pottery records. This corresponds to the final Last Glacial – Holocene time-span and reflects the following environmental history: the coexistence of open-country and woodland snail communities throughout the whole succession documents the persistence of high-diversity karsts parkland since the Late Glacial up to present, which has been supported by human activities since the Neolithic occupation. However, the molluscan succession shows a general agreement with the standard mid-European developmental pattern. The molluscan evidence is confirmed by vertebrate fossil finds.