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The Late Pleistocene microvertebrate fauna of the Vaskapu Cave (North Hungary) and its taphonomical, biostratigraphical and palaeoecological implications

机译:瓦斯卡普洞(匈牙利北部)的晚更新世微脊椎动物群,及其在地形学,生物地层学和古生态学方面的意义

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摘要

About 60 years later than the systematic excavation in 1933 carried out by Dr. Mária Mottl and her coworkers,udthe Vaskapu locality in North Hungary was rediscovered by Dr. János Hír. In the following 15udyears, several different field surveys were take place at the site and a rich microvertebrate assemblageudwere found. The aims of the present study were to review the vertebrate fauna (paying particularudattention to the previously poorly studied herpetofauna) and to summarize its taphonomical,udbiostratigraphical and palaeoecological implications. The slightly mixed assemblage with elements ofudthe forest as well as the grassland habitat is interpreted here as the result of a mosaic or quickly shiftingudenvironment left behind a retractive glaciation in the late Würm (namely at the time of the transitionudbetween the Pilisszántóian and Palánkian local biochronological stages around 15 000 years ago).
机译:距离MáriaMottl博士及其同事在1933年进行的系统发掘大约60年之后,JánosHír博士重新发现了匈牙利北部的Vaskapu地区。在随后的15年中,在该地点进行了几次不同的野外调查,发现了丰富的微脊椎动物组合体。本研究的目的是审查脊椎动物区系(特别注意以前对研究不足的Herpetofauna的重视),并总结其在形态学,生物地层学和古生态学方面的意义。与森林以及草地栖息地的元素略有混合的组合在这里被解释为马赛克或快速移动的 udenvironment遗留在Würm晚期的回缩冰川中的结果(即在过渡时期大约1.5万年前的Pilisszántóian和Palánkian局部生物年代学阶段)。

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