首页> 外文期刊>Journal of Archaeological Science >Decorated prehistoric pottery from Castello di Annone (Piedmont, Italy): Archaeometric study and pilot comparison with coeval analogous finds
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Decorated prehistoric pottery from Castello di Annone (Piedmont, Italy): Archaeometric study and pilot comparison with coeval analogous finds

机译:装饰的史前陶器(来自意大利皮埃蒙特的Castello di Annone):考古学研究和先验比较与类似的发现

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Prehistoric pottery decorated with incisions or impressions filled with white and seldom coloured inlays is well documented in the archaeological literature, but the related in-depth archaeometric studies are sporadic. 43 decorated ceramic shards, dating from the Neolithic to the Bronze Age, and an Iron Age fibula from the archaeological site of Castello di Annone (Piedmont, North-Western Italy) were analysed with FTIR, Raman and XRPD for characterization of the ornamental pigments forming these inlays. Few white components were used as fillers, namely talc and bone ash (hydroxyapatite - Bone White), often as a mixture and seldom accompanied by other pigments (i.e. kaolinite and presumably secondary calcite). Comparison with freshly-heated biogenic hydroxyapatite proved that ancient Bone White pigment was calcined at about 900°C. Such a process was kept separate from pottery firing as these white mixtures show absence of talc degradation by-products and sporadic presence of kaolinite, implying these ceramics were decorated only after firing in furnace. Actual presence of fluorapatite in bone ash could allow dating with the Fluorine Method, but lack of fluorine detection with SEM-EDS causes such an attempt to be impracticable so far. A pilot comparative study with a restricted but representative group (11) of coeval finds from other sites of Piedmont suggests that while recurrence of talc prevails in Castello di Annone from the Neolithic throughout the Bronze age, massive use of bone ash (Bone White) becomes widespread in the close Iron Age settlements, possibly consequent to a more efficient handling of its production technology.
机译:在考古文献中已充分记录了史前制的带有刻痕或压痕的装饰陶器,上面印有白色且很少着色的镶嵌物,但相关的深入考古研究是零星的。用FTIR,拉曼和XRPD分析了43个装饰的陶瓷碎片(从新石器时代到青铜器时代)和一个来自Castello di Annone(意大利西北皮埃蒙特)考古现场的铁器时代腓骨,以表征装饰性颜料的形成。这些镶嵌物。很少有白色成分被用作填充剂,即滑石粉和骨灰(羟基磷灰石-骨白),通常作为混合物使用,很少与其他颜料(即高岭石和可能的方解石)伴生。与新鲜加热的生物羟基磷灰石的比较证明,古老的骨白颜料在约900°C下煅烧。由于这些白色混合物显示出滑石降解副产物的缺乏和高岭石的零星存在,因此该过程与陶器的烧成分开保持,这意味着这些陶瓷仅在炉中烧成后才进行装饰。骨灰中氟磷灰石的实际存在可以用氟方法进行年代测定,但是到目前为止,缺乏用SEM-EDS进行氟检测的尝试是不可行的。一项比较有限的具有代表性的皮埃蒙特古迹研究组(11)的先导比较研究表明,尽管在整个青铜时代,新石器时代的Castello di Annone流行滑石,但大量使用骨灰(骨白)在铁器时代附近定居点广泛分布,可能是由于更有效地处理了其生产技术。

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