balamutivka村附近的旧石器时代遗址

O. Kononenko, B. Ridush, Yana Popiuk
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摘要

这篇论文涉及了自20世纪50年代以来在切尔诺夫茨州Balamutivka村附近的德涅斯特河右岸发现的旧石器时代材料。最近在这里发现的几个遗址,第一次被详细公布。特别值得注意的是,在村庄附近的洞穴中发现了旧石器时代的燧石人工制品。在Balamutivka和更远的东北部,有许多与第四纪高(10-12)梯田沉积物有关的旧石器时代遗址。由于山体滑坡对梯田及其斜坡的破坏,旧石器时代的燧石人工制品躺在那里的表面。对各自组合的属性分析表明,在旧石器时代中期至晚期,不同技术综合体的定义形式混合在一起。该系列包括收敛型和亚交叉型;绞齿式端刮器、鼻形端刮器;单向和双向亚圆柱形岩心,宽刀片,组合工具-主要是烧刀+刮刀;小型岩心,有一个或两个平台,亚圆柱形和狭窄的工作表面,从那里捕获薄叶片和微叶片;微石(包括«Dufour»,反润饰背衬微石),拉康类型的燃烧(?)。在洞穴中,燧石也不是原地形成的,而是由于水侵蚀和山体滑坡,从阶地表面与松散的阶地沉积物一起形成的。由于洞穴面积小和水文地质状况(周期性洪水),不适合人类或大型食肉动物居住。Balamutivka村是对德涅斯特中部地区旧石器时代进行进一步研究的有趣和有希望的地区。研究地点发现的类型学多样性证明了多层遗址的存在。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
PALAEOLITHIC SITES NEAR THE BALAMUTIVKA VILLAGE
The paper deals with the Palaeolithic materials found on the right bank of the Dniester River, in the vicinity of the Balamutivka Village, Chernivtsi Oblast, since the 1950s. Several sites, which have been recently discovered here, are published in detail for the first time. Particular attention is paid to the finds of Palaeolithic flint artefacts from caves located near the village. Within the Balamutivka and further to the northeast, there are many Palaeolithic sites associated with Quaternary sediments of high (10—12) terraces. Because of the destruction of terraces and their slopes by landslides, the Palaeolithic flint artefacts lie on the surface there. An attribute analysis of the respective assemblages indicates a mixing of defining forms of different techno-complexes of the Middle — the end of the Upper Palaeolithic. In particular, the series includes convergent and sub-cross cores; carinated end-scraper, nosed end-scrapers; uni- and bidirectional sub-cylindrical cores, wide blades, combination tools — mostly burin + scraper; small-sized cores with one or two platforms, sub-cylindrical and narrow working surface, from which thin bladelet and microblade were knapped; microliths (including «Dufour», counter-retouch backing microliths), a Lacan-type burin (?). In the caves, the knapped flints also did not occur in situ but got there from the surface of the terraces together with the loose terrace sediments due to water erosion and landslides. The caves are not suitable for habitation by humans or large predators because of their small size and hydrogeological regime (periodic flooding). The area of Balamutivka Village is interesting and promising for further investigation of the Palaeolithic of the Middle Dniester region. The typological diversity of the finds from the studied locations evidences the presence of multilayer sites.
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