Išuwa在公元前十三世纪末(关于沟槽器的问题)

A. Kosyan
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引用次数: 1

摘要

公元前十三世纪末,在土耳其东部各个地区进行的考古发掘揭示了一个完整的文化断裂,从而标志着青铜时代晚期(LBA)的结束和早期铁器时代(EIA)的兴起。新文化的主要特点是所谓的“沟槽器”的出现,它是在Išuwa境内许多遗址的发掘中出土的,这是一种由赫梯楔形文字文本很好地证明的政治单位。在东部高地不同地区的几个地点也发现了同样的陶器(东部凡湖盆地,Tillehöyük, Lidarhöyük, Erzurum, Iğdır等)。迄今为止,造成这种现象的原因尚不清楚。Ch. Burney和V. Sevin首先假设,至少在幼发拉底河上游流域,从LBA到EIA的转变是外高加索移民的结果。后来,这一假设遭到了其他考古学家的质疑。U. m . ller建议,沟槽器的来源应该在Išuwa上寻找,后来这个地区的一些人口搬到了南部和东南部。为了解决这一问题,作者提到了外高加索及其邻近地区的库拉-阿拉克斯文化人口向西南和南部的迁移,这发生在LBA结束前约2000年,即外高加索早期青铜时代末期(公元前4千年结束)。最有可能的是,这两次迁徙的原因可能是所谓的5.2和3.2千年气候事件的结果。引人注目的是,库拉-阿拉克斯I移民的路线与沟槽器人的路线一致。因此,Ch. Burney和V. Sevin的建议似乎比后来的作者提出的建议更合理。很可能在这两种情况下,我们都要处理外高加索人口群体的大规模迁移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Išuwa towards the end of the XIII century BC (on the problem of the grooved ware)
At the end of the XIII century BC archaeological excavations carried out in various regions of Eastern Turkey have revealed a complete cultural break, thus marking the end of the Late Bronze Age (LBA) and the rise of the Early Iron Age (EIA). The main peculiarity for the new culture is the appearance of the so-called "grooved ware" which was unearthed during the excavations at numerous sites on the territory of Išuwa, a political unit well attested by Hittite cuneiform texts. This same ware is known also from several sites located in different parts of Eastern Highlands (eastern Lake Van basin, Tillehöyük, Lidarhöyük, Erzurum, Iğdır, etc.). To date the causes of this phenomenon are not clear. Ch. Burney and V. Sevin were the first to assume that at least in the case of the Upper Euphrates basin the transition from LBA to EIA was the result of migration from Transcaucasia. Later this as-sumption was cast doubt on by other archaeologists. U. Müller suggested that the source for the grooved ware should be looked for in Išuwa, and that later some population of this region moved to the south and south-east. For the solution to this problem the author refers to the movement of the population of the Kura-Araxes culture of Transcaucasia and neighboring regions to the south-west and south which happened about 2000 years before the end of the LBA, during the termination of the Early Bronze Age I in Transcaucasia (end of the IV millennium BC). Most probably, the causes of both migrations could be the result of the so-called 5.2 and 3.2 kiloyear climatic events. Strikingly, the routes of the Kura-Araxes I migrants coincide with that of the grooved ware people. Thus, the suggestion of Ch. Burney and V. Sevin seem more plausible than the proposals put forward by later authors. Most probably in both cases we deal with significant migrations of Transcaucasian population groups.
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