德国西南部巴尔地区和邻近的低山脉之间的考古数据和崩塌沉积物得出的新石器时代定居动态

J. Miera, Jessica Henkner, K. Schmidt, M. Fuchs, T. Scholten, P. Kühn, Thomas Knopf
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引用次数: 11

摘要

摘要本研究将考古数据与来自崩塌沉积物的考古学数据相结合,以推断巴尔地区、黑森林和斯瓦本汝拉之间的新石器时代定居动态。本文回顾了考古研究的现状,并分析了新石器时代遗址的发现过程,从而在这些景观中形成了当前的考古遗址分布。研究区域的土地利用强度使用场地频率与德国南部其他景观进行比较。利用碳的AMS 14C年龄和沉积物的发光年龄来确定崩塌沉积的阶段,并将其解释为人类存在的局部代用物。考古来源的批评表明,新石器时代遗址的分布可能受到诸如侵蚀和风化作用导致的叠加等因素的扭曲,这些因素限制了新石器时代陶器的保存条件。重建新石器时代的沉降动力学是通过补充沉积阶段的考古数据来实现的。研究提供了巴尔地区在整个新石器时代持续使用土地的证据,并确定了斯瓦本汝拉和黑森林的零星土地使用阶段。在新石器时代晚期和晚期,在低山脉地区可以注意到崩塌形成的加剧。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Neolithic settlement dynamics derived from archaeological data and colluvial deposits between the Baar region and the adjacent low mountain ranges, southwest Germany
Abstract. The present study combines archaeological data with archaeopedological data from colluvial deposits to infer Neolithic settlement dynamics between the Baar region, the Black Forest and the Swabian Jura. A review of the state of archaeological research and an analysis of the processes leading to the discovery of the Neolithic sites and thereby the formation of the current archaeological site distribution in these landscapes is presented. The intensity of land use in the study area is compared with other landscapes in southern Germany using site frequencies. Phases of colluvial deposition are dated using AMS 14C ages of charcoals and luminescence ages of sediments and interpreted as local proxies for a human presence. Archaeological source criticism indicates that the distribution of the Neolithic sites is probably distorted by factors such as superimposition due to erosion and weathering effects limiting the preservation conditions for Neolithic pottery. A reconstruction of Neolithic settlement dynamics is achieved by complementing the archaeological data with phases of colluviation. Evidence for a continuous land use in the Baar region throughout the Neolithic is provided and sporadic phases of land use on the Swabian Jura and in the Black Forest are identified. In the late and final Neolithic, an intensification of colluvial formation can be noticed in the low mountain ranges.
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