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首页> 外文期刊>Geomorphology >Records of human occupation from Pleistocene river terrace and aeolian sediments in the Arneiro depression (Lower Tejo River, central eastern Portugal)
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Records of human occupation from Pleistocene river terrace and aeolian sediments in the Arneiro depression (Lower Tejo River, central eastern Portugal)

机译:在Arneiro凹陷(葡萄牙中东部的下特茹河)的更新世河流阶地和风成沉积物中人类被占领的记录

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In the uppermost reach of the Lower Tejo River (eastern central Portugal), where the river crosses two quartzite ridges that separate the Rodao (upstream) and Arneiro (downstream) depressions, Palaeolithic artefacts have been recovered from three lower river terrace levels and a cover unit of aeolian sands. This paper presents data on the discovery of archaeological artefacts from the terrace levels and the aeolian sands that can be linked to Middle and Upper Palaeolithic industries from new field sites at Tapada do Montinho and Castelejo. The archaeological data when placed in a geomorphological, sedimentary and chronological framework, contribute new information on the understanding of human occupation in western Iberia during cold~ climate episodes of the last 62 to 12 ka; and especially during the cooler and driest conditions that occurred between 32 and 12 ka, when the climate favoured aeolian sediment transport. In the Lower Tejo River, the integration of absolute age datasets with archaeological, geomorphological and sedimentary data indicate that in westernmost Iberia the first appearance of artefacts in river terrace sediments suggests that the earliest marker for human occupation dates from the lower Acheulian (Lower Palaeolithic), probably corresponding to an age of ~340 ka. Data also suggest, for the first time, that Acheulian lithic industries were replaced by Middle Palaeolithic ones (namely the Levallois stone knapping technique) by ~160 ka (~MIS6). Middle Palaeolithic industries were later replaced by Upper Palaeolithic industries at 32 ka. The post 32 ka period, dominated by aeolian sediment transport, is related to the onset of cold~dry climate conditions which resulted in low river flow discharges, floodplain exposure and reworking by NW winds. This cold~ dry period is coeval with the disappearance of Megafauna and associated Neanderthal communities, and the replacement of the Middle Palaeolithic industries by Upper Palaeolithic ones in this westernmost part of Europe.
机译:在下特茹河(葡萄牙中部东部)的最上游,该河穿过两条石英岩山脊,分隔了Rodao(上游)和Arneiro(下游)洼地,从三个较低的河阶和覆盖层中恢复了旧石器时代的文物。风沙的单位。本文介绍了有关从阶地和风沙中发现的考古文物的数据,这些风沙可以与Tapada do Montinho和Castelejo的新油田现场的中,上古石器时代的产业联系起来。将考古数据放在地貌,沉积和时间顺序框架中,为了解最近62至12 ka的寒冷至气候事件期间伊比利亚西部的人类占领提供了新的信息。特别是在32到12 ka之间最凉爽和最干燥的条件下,当时气候有利于风沙沉积物的运输。在下特茹河中,绝对年龄数据集与考古,地貌学和沉积数据的整合表明,在伊比利亚最西端,河阶阶沉积物中的人工制品首次出现表明,人类占领的最早标记可追溯到阿彻留纪(下古石器时代) ,可能对应于约340 ka的年龄。数据还首次表明,以约160 ka(〜MIS6)的程度将阿彻勒石器时代的工业替换为中古石器时代的工业(即Levallois石绑技术)。中古石器时代的工业后来被32 ka的上古石器时代的工业所取代。后32 ka时期以风沙沉积为主导,与寒冷到干燥的气候条件的发生有关,这导致河流流量减少,洪泛区暴露和西北风的影响。在这个寒冷〜干燥的时期,与欧洲最西端的巨型动物群和相关的尼安德特人群落的消失,以及上古石器时代的工业取代了旧石器时代的工业相伴。

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