vyys Tom 2 -伊兹玛河谷的多层考古遗址

A. Volokitin, N. Volokitina
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引用次数: 0

摘要

第一个多层清晰分层遗址vyys Tom 2在伊兹马河流域被研究,伊兹马河是Pechora河最大的左支流(东欧平原北部)。文化遗迹位于露台海岬的沉积物中,高10米。该遗址于2003年被发现;挖掘工作分别于2010-2011年、2015年和2017年进行。文化有四个层次。第一层文化层放置在当代森林土壤中。在这一层中发现了保存完好的陶瓷器皿碎片。然而,它们的形状和装饰的典型特点使这一层可以追溯到早期铁器时代(公元前6 - 3世纪)的Ananyino文化末期。第二层文化层放置在距当代建筑表面0.3-0.5米深的棕色壤土中。燧石文物并不多。火石的热处理,薄双面的生产,以及大的烧痕是新石器时代蜂窝陶瓷的典型特征。第三和第四文化层位于冲积土层的薄腐殖质砂壤土中,距离当代地表>2米深。它是低冲积平原冲积物,具有高沉积速率。第3层沉积年代分别为7720±100 BP (GIN-15331)、7800±90 BP (GIN-14593)、8510±70 BP (LU-7289)和8685±30 BP (IGANams-5991),第4层沉积年代分别为8540±70 BP (GIN-14594)、8690±90 BP (LU-7288)和8700±30 BP (IGANams-5992)。沉积物的高堆积率表明,第三文化层的时间为7720±100 BP和7800±90 BP。第三层和第四层营地的存在间隔了大约10年。在这些层中,发现了壁炉、赭石痕迹、动物遗骸和石制品,包括一套用于加工骨头的啄食磨具,以及大型板岩抛光工具的薄片(第三层),以及大型点、岩心(包括岩心烧伤)、抛光轴及其碎片(第四层)。我们区分相似性清单的第三和第四文化层。所用原料显示两层均存在页岩和绿帘石。赭石的存在,以及壁炉的位置一个比另一个高,也证实了第三层和第四层中石器时代遗址存在的时间间隔很短。从vyys Tom 2遗址和Parch中石器文化遗址中发现的中石器时代石业的一些相似之处说明了它们之间的相互关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Vylys Tom 2 – A Multilayered Archaeological Site in the Valley of the Izhma River
The first multilayered clearly stratified site Vylys Tom 2 was studied in the valley of the Izhma River, the largest left tributary of the Pechora River (north of the East European Plain). Cultural remains are located in the sediments of the terrace’s promontory, which is 10 m high. The site is discovered in 2003; excavations were done in 2010–2011, 2015, 2017. Four cultural layers are distinguished. The first cultural layer is placed in contemporary forest soil. Badly preserved fragments of ceramic vessels are found in this layer. Nevertheless, typical peculiarities of their forms and ornament allow to date this layer to the end of Ananyino culture of Early Iron Age (VI–III century BC). The second cultural layer is placed in brown loam at 0.3–0.5 m depth from contemporary day surface. Flint artifacts are not numerous. Heat treatment of flint, thin bifaces production, and large burins are typical for the Neolithic with pit-comb ceramics. The third and fourth cultural layers are placed in thin humus sandy loam of alluvial soil strata and found at >2 m depth from contemporary day surface. It is low floodplain alluvium with a high sedimentation rate. The third layer has been dated to 7720±100 BP (GIN-15331), 7800±90 BP (GIN-14593), 8510±70 BP (LU-7289), and 8685±30 BP (IGANams-5991), while the obtained dates for the fourth layer are 8540±70 BP (GIN-14594), 8690±90 BP (LU-7288), and 8700±30 BP (IGANams-5992). The high rate of accumulation of sediments shows that the dates 7720±100 and 7800±90 BP from the third cultural layer are rejuvenated. And there is about 10 years between the existence of camp sites of the third and fourth layers. In these layers, fireplaces, traces of ocher, faunal remains, and stone products are noted, including a set of peckingabrasive stone tools for processing bone, and flakes from large slate polished tools (third layer), as well as large points, cores (including core-burins), polished axes and their fragments (fourth layer). We distinguish similarity the inventories of the third and fourth cultural layers. The used raw materials show the presence of shale and epidosite in both layers. The presence of ocher, the location of the hearths one above the other also confirm the short time interval between the existence of the Mesolithic sites of the third and fourth layers. Some similarities in the stone industry of the Mesolithic layers from the site of Vylys Tom 2 and the sites of Parch Mesolithic culture speak of their interrelations.
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