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首页> 外文期刊>Historical Biology: an international journal of paleobiology >Palaeoenvironmental and palaeoclimatic reconstruction of the Middle to Late Pleistocene sequence of Scladina Cave (Namur, Belgium) using the small-mammal assemblages
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Palaeoenvironmental and palaeoclimatic reconstruction of the Middle to Late Pleistocene sequence of Scladina Cave (Namur, Belgium) using the small-mammal assemblages

机译:使用小型哺乳动物组合的古群洞穴(Namur,比利时)中间到晚期更新世序列中的古古典族和古尖端重建

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摘要

The habitat weighting, the bioclimatic model methods and the Simpson diversity index are applied to the small-mammals assemblage of Scladina Cave (border between High and Middle Belgium) in order to reconstruct the environmental and climatic fluctuations that are reflected on the Middle to Late Pleistocene sequence of the cave. The small-mammal data analyzed come from two surveys carried out at the entrance of the cave and allow us to identify within the section one cold episode: a dry, cool phase in the upper part of the sequence (probably associated with the MIS 3). The environmental and climatic data show an alternation of open meadows and woodland formations through both sequences, punctuated by peaks in local watery environments together with lower temperatures and higher precipitations rates than at present. Finally, a comparison of the small-mammal fossil assemblage from the studied surveys with the small-mammals assemblage from the Holocene deposits of Scladina Cave shows that layers related with MIS 5 temperate sub-stages (MIS 5c and MIS 5a) present environmental characteristics similar to those prevailing nowadays (a landscape dominated by woodland formations and water streams) in the area surrounding the cave. This is coherent with the available chronostratigraphic datasets on this part of the sequence, suggesting the record of the humid and temperate phases at the beginning of the Late Pleistocene.
机译:栖息地加权,生物基础模型方法和辛普森多样性指数应用于巩膜洞穴的小哺乳动物组合(高中和中间的边界),以重建在中间到晚期中间至晚期中间的环境和气候波动洞穴的序列。分析的小型哺乳动物数据来自洞穴入口处进行的两次调查,并允许我们识别在一个冷情节中:序列的上半部分的干燥,冷却相(可能与MIS 3相关联) 。环境和气候数据通过两个序列显示开放草甸和林地形成的交替,在当地水利环境中的峰值,以及较低的温度和比目前更高的沉淀率。最后,从Scladina洞穴的全新型沉积物的小哺乳动物组合的小哺乳动物化石组合的比较表明,与MIS 5温度分阶段(MIS 5C和MIS 5A)的层数存在类似的层在洞穴周围的地区,现在普遍存在的人(由林地形成和水流主导的景观)。这与序列的这一部分上的可用计时器数据集相干,表明晚熟开始时潮湿和温带阶段的记录。

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