“理解语境而非成分”:从地质考古的角度评价Mayurbhanj旧石器时代

Krishnendu Polley, K. Chakraborty, Shubhrakanti Baul
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引用次数: 0

摘要

印度出土的第一个较低旧石器时代(阿舍利)遗址位于奥里萨邦Mayurbahnj地区的Burhabalang河谷。这表明Mayurbhanj Acheulean遗址群已经被史前考古学家扫描了很长一段时间。然而,遗憾的是,尽管有多位学者对布尔哈巴郎河谷的实河床进行了近一个世纪的研究,但至今尚未对其进行详细的研究。本文对奥里萨邦巴里帕达镇附近的布尔哈巴朗河流域的阿舍利文物床的性质和起源模式进行了探讨。本研究采用地质考古学的方法,对该地区几个阿舍利遗址的各种地貌、岩性属性等物理特征进行研究和比较。此外,还试图了解该地区阿舍利人工制品承载层的赋存性质以及这些承载层的起源方式。研究结果表明,在更新世中期,在更为湿润的季风气候的影响下,可能沉积了带有布哈巴郎河谷铁质层的阿舍利人工制品。也许史前人类带着阿舍利的人工制品在这个地区的河谷中漫步,而此时正是含铁沉积或铁精矿沉积的时期。在较晚的时间里,由于气候更加干燥,在铁质沉积物的顶部形成了含铁硬壳,现在在硬壳层中发现了阿舍利人工制品。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
“Understanding Context rather than Component”: An Assessment of Mayurbhanj Palaeoliths from a Geo-Archaeological Perspective
The first Lower Palaeolithic (Acheulean) sites ever excavated in India are located in the Burhabalang river valley of the Mayurbahnj district of Orissa. It reveals that the Mayurbhanj Acheulean site complex has been under the scanner of prehistoric archaeologists for a long period. However, it is unfortunate to say that, despite being studied for nearly one century by several scholars, the implementiferous beds of the Burhabalang River valley have not been studied in detail till now. The present article brings forward an attempt to fathom the nature and the mode of origin of the Acheulean artifact-bearing beds of the Burhabalang river valley near Baripada town of Orissa. In this study approach of geo-archaeology is adopted to study and compare physical features like various geomorphological and lithological attributes of several Acheulean sites of this region. Besides, an attempt is made to understand the nature of occurrence of Acheulean artifact bearing-beds of this region and the mode of origin of these implementiferous beds too. Results of this study reveal that probably Acheulean artifacts bearing ferricrete horizons of the Burhabalang river valley were deposited some time during the middle Pleistocene, under the influence of a much more humid monsoonal climate. Perhaps prehistoric humans with Acheulean artifacts roamed in the river valleys of this region when deposition of ferruginous sedimentation or ferricrete was taking place. During the later time under the influence of a much drier climate ferruginous duricrust developed at the top of ferricrete sediments and Acheulean artifacts are now found deposited in the hard duricrust horizon.
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