两种长距燧石示踪剂的ED-XRF和LA-ICP-MS地球化学表征。对比利牛斯山脉(欧洲西南部)抹大拉时期人类迁移的影响

Marta Sánchez de la Torre, François‐Xavier Le Bourdonnec, S. Dubernet, B. Gratuze, Xavier Mangado, J. Fullola
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引用次数: 14

摘要

摘要/ ABSTRACT摘要:我们对比利牛斯山两个裸露的燧石组进行了地球化学表征,并在视觉和微观尺度上表现出相似的特征:Montgaillard复理燧石组和montsaun燧石组。在马格达莱尼亚比利牛斯山脉的几个遗址中发现了两种类型的燧石,它们具有相同的结构和微古生物学特征。我们面对的是一种长距离燧石类型,其地球化学特征对于了解示踪剂的来源至关重要。利用能量色散x射线荧光(ED-XRF)和激光烧蚀电感耦合等离子体质谱(LA-ICP-MS)进行了分析。结果表明,尽管在主、微量元素方面获得了相似的数据,但在微量元素方面却存在差异。在地球化学水平上建立两种地层之间的差异,可以确定在Parco洞穴(Alòs de Balaguer, Spain)的马格达莱期水平上发现的这种燧石类型的起源。结果表明,在旧石器时代晚期,在比利牛斯山脉有长期的石器原料流通,因此,人类的流动性。
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The geochemical characterization of two long distance chert tracers by ED-XRF and LA-ICP-MS. Implications for Magdalenian human mobility in the Pyrenees (SW Europe)
ABSTRACT We geochemically characterize two chert formations outcropping in the Pyrenees and presenting similar characteristics at the visual and microscopic scale: The Montgaillard flysch cherts and the Montsaunès cherts. Cherts presenting identical textural and micropalaeontological features as both types have been found in several Magdalenian Pyrenean sites. We are face to a long distance chert type whose geochemical characterization is essential for knowing where the tracer comes from. Analyses have been done using Energy-dispersive X-ray fluorescence (ED-XRF) and laser ablation inductively-coupled plasma mass spectrometry (LA-ICP-MS). Results show that despite obtaining similar data concerning major and minor elements, differences have been observed regarding trace elements. The establishment of differences between both formations at the geochemical level has allowed specifying the origin of this chert type recovered at the Magdalenian levels of Parco Cave (Alòs de Balaguer, Spain). Results demonstrate long lithic raw material circulation and thus, human mobility in the Pyrenees during the Upper Palaeolithic.
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