Mar Rey-Solé, C. Ionescu, M. Ciută, M. Mureșan-Pop, V. Simon
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引用次数: 0
Abstract
The present archaeometric study focuses on a set of archaeological siliceous lithic tools that are assigned to the early Vinča culture period (Vinča A and Vinča B1). They were found in several pit-houses at Limba-Oarda de Jos (SW Transylvania, Romania), an open settlement that has been dated to 5,405-5,310 cal. BCE, a period in the Middle Neolithic. A total of 322 retouched tools and débitage pieces were typologically and macroscopically investigated. From these, 20 pieces were analyzed by polarized light optical microscopy (OM) and 10 pieces were analyzed by Fourier-transform infrared spectroscopy (FTIR) in order to identify compositional characteristics, define the petrographic type, and establish the spectral fingerprint of each material.
Four petrographic types were discriminated: radiolarite, chert, fossiliferous chert, and siliceous limestone. Mineralogically, the tools primarily consist of a mass of microquartz and fibrous microquartz (called also ‘chalcedony’) associated with radiolarians remnants (in radiolarites); fossil shell fragments (in the fossiliferous chert); and limestone components, such as ooliths and pellets (in the siliceous limestone). All samples show distinct FTIR bands, most of which are assigned to microquartz, quartz, and fibrous microquartz. The deconvolution of the FTIR spectra in the 950-1300 cm-1 domain reveals the contribution of several other phases, such as calcite and clay minerals.
The results support the assumption that the tools made of chert, fossiliferous chert, and siliceous limestone were produced at the site from nodules that probably originated from the Upper Jurassic chert-bearing limestone that crops out nearby in the Trascău Mts. The tools made of radiolarite were most likely brought to the site as finished products from the Trascău Mts.
目前的考古研究集中在一套考古硅质石器工具上,这些工具被分配到早期vin a文化时期(vin a a和vin a B1)。它们是在Limba-Oarda de Jos(罗马尼亚特兰西瓦尼亚西南部)的几个坑屋中发现的,这是一个开放的定居点,可以追溯到公元前5405 - 5310 cal. BCE,新石器时代中期。对322个修饰工具和修饰件进行了类型学和宏观研究。利用偏光光学显微镜(OM)和傅里叶变换红外光谱(FTIR)对其中的20块进行了分析,以确定每种材料的成分特征,确定岩石类型,并建立光谱指纹图谱。划分出4种岩相类型:放射石、燧石、石质燧石和硅质灰岩。矿物学上,这些工具主要由大量微石英和纤维微石英(也称为“玉髓”)组成,与放射虫残留物(在放射虫岩中)有关;化石壳碎片(在化石燧石中);和石灰石成分,如鲕粒和颗粒(在硅质石灰石)。所有样品都显示出明显的FTIR波段,其中大部分属于微石英、石英和纤维微石英。在950-1300 cm-1区域的反褶积显示了方解石和粘土矿物等其他相的贡献。研究结果支持这样一种假设,即燧石、燧石化石和硅质石灰岩制成的工具,可能是在该地点从上侏罗统含燧石的石灰岩中产生的结核中产生的,这些石灰岩可能来自附近的特拉斯库拉乌Mts。放射石制成的工具很可能是作为特拉斯库拉乌Mts的成品被带到该地点的。