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首页> 外文期刊>Quaternary International >Chronology and formation processes of the Middle to Upper Palaeolithic deposits of Ifri n'Ammar using multi-method luminescence dating and micromorphology
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Chronology and formation processes of the Middle to Upper Palaeolithic deposits of Ifri n'Ammar using multi-method luminescence dating and micromorphology

机译:利用多方法发光测年和微观形态学研究伊夫里n'mmar中至上古石器时代的年代学和形成过程

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摘要

The existence of an early Upper Palaeolithic culture at the transition from the Middle Palaeolithic to the Upper Palaeolithic in North African cave sites is currently under debate. We studied Ifri n'Ammar in North-East Morocco, which is one of the oldest settlement sites of anatomically modern humans (AMH) in the Maghreb and contains several sediment layers which are attributed to Middle and Upper Palaeolithic occupations. In order to investigate processes of sediment accumulation and postdepositional alteration, we studied thin sections from these levels. According to micromorphological analysis, aeolian input considerably contributed to sediment accumulation and postdepositional mixing by bioturbation occurred. We compared multiple and single-grain quartz and multiple-grain feldspar luminescence dating of three samples from corresponding sediment layers to achieve a comprehensive chronology. The single-grain dose distributions scatter strongly and the source of the scatter is unclear. We used an arithmetic mean to calculate the equivalent doses. Archaeological evidence and age control from radiocarbon dating was essential to interpret the data. Quartz and feldspar multiple-grain luminescence ages are between 15 and 80 ka. The central part of the profile shows an intermediate accumulation, which lacks specified lithic artefacts. This supports the idea of an occupational gap between Middle and Upper Palaeolithic layers. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:在北非洞穴遗址从中旧石器时代过渡到上旧石器时代的过渡时期,早期的旧旧石器时代文化的存在目前正在争论中。我们研究了摩洛哥东北部的Ifri n'Ammar,它是马格里布(Manhreb)解剖学现代人类(AMH)的最古老的定居点之一,其中包含几个沉积层,这些沉积层归因于中,旧石器时代的占领。为了研究沉积物堆积和沉积后蚀变的过程,我们从这些水平研究了薄片。根据微观形态学分析,风沙输入极大地促进了沉积物的积累,并发生了生物扰动引起的沉积后混合。我们比较了来自相应沉积层的三个样品的多粒和单粒石英以及长粒长石发光年代,以实现全面的年代学。单粒剂量分布强烈散布,散布的来源尚不清楚。我们使用算术平均值来计算等效剂量。放射性碳测年的考古证据和年龄控制对于解释数据至关重要。石英和长石的多晶粒发光年龄为15至80 ka。轮廓的中央部分显示出中间堆积,缺少特定的石器物。这支持了旧石器时代中期和上层之间的职业鸿沟的想法。 (C)2017爱思唯尔有限公司和INQUA。版权所有。

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  • 来源
    《Quaternary International》 |2018年第20期|89-102|共14页
  • 作者单位

    Univ Cologne, Inst Geog, Albertus Magnus Pl, D-50923 Cologne, Germany;

    Univ Cologne, Inst Geog, Albertus Magnus Pl, D-50923 Cologne, Germany;

    Inst Natl Sci Archeol & Patrimoine, Rabat, Morocco;

    Univ Cologne, Inst Geog, Albertus Magnus Pl, D-50923 Cologne, Germany;

    Neanderthal Museum, Talstr 300, D-40822 Mettmann, Germany;

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