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Middle to Late Pleistocene human habitation in the western Nefud Desert, Saudi Arabia

机译:沙特阿拉伯内弗德沙漠中的中更新世晚期

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The Nefud Desert is crucial for resolving debates concerning hominin demography and behaviour in the Saharo-Arabian belt. Situated at the interface between the Mediterranean Westerlies and African Monsoonal climate systems, the Nefud lies at the centre of the arid zone crossed by Homo sapiens dispersing into Eurasia and the edges of the southernmost known extent of the Neanderthal range. In 2013, the Palaeodeserts Project conducted an intensive survey of the western Nefud, to: (1) evaluate Pleistocene population dynamics in this important region of the Saharo-Arabian belt and (2) contribute towards understanding early modern human range expansions and interactions between different hominin species. Thirteen Lower and Middle Palaeolithic sites were discovered in association with palaeolake basins. One of the sites, T'is al Ghadah, may feature the earliest Middle Palaeolithic assemblage of Arabia. Preliminary analyses show that the Lower and Middle Palaeolithic sites discovered display diverse technological characteristics, indicating that the Nefud was important for population turnovers and exchanges throughout the Pleistocene. Periodic environmental amelioration appears to have attracted hominin incursions into the region, and subsequent ephemeral occupations structured around lakes and, to a lesser extent, raw material sources. However, differences between the Lower and Middle Palaeolithic sites are indicative of greater mobility during the later Pleistocene. A rarity of formal tools, but strong similarities in lithic production techniques, are also suggestive of demographic affinities across the Nefud during the Pleistocene, and perhaps beyond. These preliminary results support the view that the Arabian Peninsula was a critically important region of southwest Asia during the Late Pleistocene, in which demographic responses to climatic amelioration may have structured connectivity across the Saharo-Arabian belt, the Levant and as far as India. (C) 2014 Elsevier Ltd and INQUA. All rights reserved.
机译:内夫德沙漠对于解决有关萨哈罗-阿拉伯带人均人口学和行为的辩论至关重要。 Nefud位于地中海西风和非洲季风气候系统之间的交界处,位于干旱地区的中心,被分布到欧亚大陆的智人横渡,是尼安德特人山脉最南端的边缘。 2013年,古生物学项目对尼夫德西部进行了深入调查,以:(1)评价这一重要的萨哈罗-阿拉伯带地区的更新世种群动态,(2)有助于了解早期现代人类范围的扩展以及不同人类之间的相互作用人种。与古湖盆相关的13处下古和中古石器时代遗址被发现。 T'is al Ghadah是其中一处遗址,可能是阿拉伯最早的中古石器时代遗址。初步分析表明,所发现的旧石器时代中期和中期遗址显示出不同的技术特征,这表明,纳弗德对整个更新世的人口周转和交流很重要。周期性的环境改善似乎吸引了人参入侵,并随后在湖泊周围以及在较小程度上围绕原材料来源进行了短暂的占领。然而,下旧石器时代遗址与中旧石器时代遗址之间的差异表明,晚更新世时期的活动性更大。很少有形式化的工具,但在石器生产技术上有很强的相似性,这也暗示了在更新世期间乃至更远的整个纳富德的人口亲和力。这些初步结果支持这样一种观点,即阿拉伯半岛是晚更新世期间西南亚的一个至关重要的地区,在该地区,人口对气候改善的反应可能在整个萨哈罗-阿拉伯带,黎凡特和印度一直具有结构性的联系。 (C)2014 Elsevier Ltd和INQUA。版权所有。

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