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首页> 外文期刊>E&G: Quaternary Science Journal >New data from the Middle Palaeolithic Cotencher cave (Swiss Jura): site formation, environment, and chronology
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New data from the Middle Palaeolithic Cotencher cave (Swiss Jura): site formation, environment, and chronology

机译:来自中古石器时代的Cotencher洞穴(瑞士汝拉州)的新数据:场地形成,环境和年代

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Cotencher cave is one of the oldest Palaeolithic sites of Switzerland and is known for its rich faunaland Mousterian artefacts, the latter suggesting one or several passages of Neanderthal hunter–gatherertribes. This interdisciplinary study summarises novel data concerning site formation processes and anthropic attendance of the site. While the lithic artefacts indicate tool production at the site, the faunalremains do not yield any evidence of a link to human occupation. The sedimentary sequence permitsus to unravel several important environmental changes that occurred during the Late Pleistocene. Thepresence of a local glacier around 70 ka (Marine Isotope Stage, MIS 4) is revealed followed by ice-freeconditions characterised by alternating soil formation processes and landscape destabilisation duringMIS 3. Solifluction processes suggesting recurrent frozen ground were responsible for the displacements of part of the artefacts and faunal remains. Evidence of local glacier development around 36 kais related to the particular geomorphological conditions of the studied region and shed new light onthe complexity of glacier dynamics. The recognition and dating of recurrent hostile glacier landscapesmight contribute to understanding the reasons for the Middle and Upper Palaeolithic attendance hiatuses known in the studied region.
机译:Cotencher洞穴是瑞士最古老的旧石器时代遗址之一,以其丰富的动物区穆斯特手工艺品而闻名,后者暗示着尼安德特人的狩猎者-采集者部落中的一个或几个通道。这项跨学科研究总结了有关站点形成过程和站点的人类出勤率的新数据。虽然石器物表明现场有工具生产,但动物区系遗迹并未提供任何与人类占领有关的证据。沉积层序揭示了晚更新世期间发生的一些重要环境变化。结果表明,在70 ka(海洋同位素阶段,MIS 4)附近存在局部冰川,其次是无冰条件,其特征是MIS 3期间土壤形成过程交替变化和景观不稳定。人工制品和动物遗骸。 36 kais附近的局部冰川发育的证据与所研究区域的特定地貌条件有关,并为冰川动力学的复杂性提供了新的思路。经常性敌对冰川景观的识别和年代测定可能有助于了解研究区域中上古旧石器时代出勤中断的原因。

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