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Dating archaeological sites in an arid environment: A multi-method case study in the Negev Highlands, Israel

机译:在干旱环境中约会考古遗址:以色列内盖夫高地的多方法案例研究

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Archaeological surveys of the Negev Highlands show that the settlement history of this arid environment oscillated widely over time. This observation is almost entirely based on scant sherd assemblages from surveys, with only a few chronometric ages from one or two archaeological features at a given site. The reasons for the scarcity of chronometric ages include insufficient attention to radiocarbon dating in past research, low amounts of datable organic material for radiocarbon dating and issues related to low rate of site accumulation, and incomplete preservation of activity remains. In order to overcome these problems, we present here the results of a detailed chronometric radiocarbon and optically stimulated luminescence (OSL) dating study exploring the development of Negev archaeological sites in the third millennium BCE. The study included micromorphological analyses to aid identification of sedimentological and post -depositional processes at the studied sites. At Nahal Boger 66, one of many small Negev third millennium BCE sites, seven radiocarbon ages were determined from archaeological contexts that suggest repeated discontinuous activity throughout the Early Bronze (EB) and early part of the Intermediate Bronze Age (IBA) (c. 3300-2350 BCE). At Ein Ziq -one of a few large sites in the region seven samples were dated; they show a very short period of activity in the beginning of the IBA (c. 2450-2200 BCE). OSL age determinations at this site provided evidence for the rapidity of site burial by sediment accumulation. Also, OSL ages from secure depositional contexts verified via micromorphology are in agreement with those obtained by radiocarbon dating. Taken together, the results provide new systematic evidence for the timing of EB IBA activity in the arid Negev Highlands. (C) 2017 Elsevier Ltd. All rights reserved.
机译:内盖夫高地的考古调查表明,这种干旱环境的定居历史随着时间的流逝而广泛波动。这项观察几乎完全基于调查中稀疏的羊群组合,在给定地点只有一个或两个考古特征的年代计时年龄。计时年代稀缺的原因包括:过去的研究中对放射性碳测年的关注不足,用于放射性碳测年的数据量低的有机材料以及与站点积累速率低有关的问题以及活动的保存不完全。为了克服这些问题,我们在这里介绍详细的计时放射性碳和光激发发光(OSL)测年研究的结果,探索公元前三千年内盖夫考古遗址的发展。该研究包括微观形态分析,以帮助识别研究地点的沉积学和沉积后过程。在纳哈尔·伯格(Nahal Boger 66),这是内盖夫第三千年的许多小型站点之一,根据考古背景确定了七个放射性碳年龄,这表明整个早期青铜时代(EB)和中级青铜时代早期(IBA)的重复不连续活动(约3300年)公元前-2350年)。在Ein Ziq-该地区几个大地点中的一个,已标出了七个样本。它们在IBA(约公元前2450-2200年)开始时显示出非常短的活动时间。该地点OSL年龄的确定为沉积物堆积而埋葬现场的速度提供了证据。而且,通过微观形貌验证的来自安全沉积环境的OSL年龄与通过放射性碳测年获得的年龄一致。两者合计,结果为干旱的内盖夫高地EB IBA活动的时间提供了新的系统证据。 (C)2017 Elsevier Ltd.保留所有权利。

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