Lakhuti-IV – A new site of the early Palaeolithic in Central Asia (Tajikistan)

Pub Date : 2023-09-01 DOI:10.1016/j.ara.2023.100466
Anton Anoikin , Petr Sosin , Andrei Rybalko , Tura Khudjageldiev , Abdullo Sharipov , Asliddin Karayev , Ekaterina Kulakova , Olga Meshcheryakova , Olga Tokareva , Redzhep Kurbanov
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Abstract

Opening of series of sites of Loess Palaeolithic in Central Asia, found within a different levels of loess-palaeosol sequences of Tajikistan, was a great step in understanding history of hominin dispersal in Eurasia. The highest density of Loessic Palaeolithic sites is recorded in the Khovaling Loess Plateau. In 2021 a Russian-Tajik geoarchaeological expedition carried out an archaeological survey and discovered an area rich in stone artefacts,  concentrated in pedocomplexes 5, which was excavated and called Lakhuti-IV. All archaeological material at the Lakhuti-IV site was associated with pedocomplex 5, consisting of two well developed palaeosols reflecting different climatic phases of the interglacial period. The stratigraphic occurrence and the typological characteristics of the assemblage indicate a single industry. Several knapping technologies are recorded in the primary knapping: radial, slice and simple parallel. From the existing geochronological data for the Khovaling Loess Plateau, cultural layer of Lakhuti-IV is correlated with MIS 13 (∼0.5 Ma). A distinctive feature of Lakhuti-IV, and one which distinguishes it from the entire assemblages of the Palaeolithic sites in the Khovaling Loess Plateau, is the high concentration of artefacts. Another unique feature of the site is that here, for the first time in the Loessic Palaeolithic of Central Asia artefacts are found in several distinct cultural horizons within the same pedocomplex, i.e., within the same climatic warm period.

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中亚(塔吉克斯坦)旧石器时代早期新遗址拉库提- iv
在塔吉克斯坦不同层次的黄土-古土壤序列中发现的一系列中亚黄土旧石器时代遗址的开放,是了解欧亚大陆人族扩散历史的重要一步。黄土旧石器时代遗址密度最高的地区是霍瓦岭黄土高原。2021年,俄罗斯-塔吉克地质考古考察队进行了一次考古调查,发现了一个石质文物丰富的地区,集中在儿童建筑群中,被挖掘出来并称为Lakhuti-IV。Lakhuti-IV遗址的所有考古材料都与土壤复合体5有关,该复合体由两个发育良好的古土壤组成,反映了间冰期不同的气候阶段。该组合的地层产状和类型特征表明其为单一工业。在初级压扣中有几种压扣技术:径向压扣、切片压扣和简单平行压扣。从Khovaling黄土高原现有的年代学资料来看,Lakhuti-IV的文化层与MIS 13 (~ 0.5 Ma)相关。拉胡提- iv的一个显著特征,也是将其与黄土高原霍瓦岭旧石器时代遗址的整个组合区分开来的一个特征,是人工制品的高度集中。该遗址的另一个独特之处在于,在中亚黄土旧石器时代,在同一土壤复合体内,即在同一气候温暖时期,首次在几个不同的文化视野中发现了人工制品。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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