Towards timing and stratigraphy of the Bronze Age burial mound royal tomb (Königsgrab) of Seddin (Brandenburg, northeastern Germany)

Moritz Nykamp, Jacob Hardt, P. Hoelzmann, J. May, T. Reimann
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引用次数: 1

Abstract

Abstract. This study uses an integrated multi-method geoarcheological and geochronological approach to contribute to the understanding of the timing and stratigraphy of the monumental burial mound royal tomb (Konigsgrab) of Seddin. We show that the hitherto established radiocarbon-based terminus post quem time frame for the construction of the burial mound of 910–800 BCE is supported by optically stimulated luminescence (OSL) dating. The radiocarbon samples were obtained from a substrate directly underneath the burial mound which supposedly represents the late glacial/Holocene soil that was buried below the structure. We use sedimentological (grain-size analyses) and geochemical analyses (element analyses, carbon, pH, and electric conductivity determinations) to reassess and confirm this hypothesis. In addition to the burial age associated with the last anthropogenic reworking during construction of the burial mound, the OSL dating results provide new insights into the primary deposition history of the original substrates used for the structure. In combination with regional information about the middle and late Quaternary development of the environment, our data allow us to provide a synoptic genetic model of the landscape development and the multiphase stratigraphy of the royal tomb of Seddin within the Late Bronze Age cultural group “Seddiner Gruppe” of northern Germany. Based on our initial experiences with OSL dating applied to the sediments of a burial mound – to the best of our knowledge the first attempt in Europe – we propose a minimal invasive approach to obtain datable material from burial mounds and discuss related opportunities and challenges.
德国东北部勃兰登堡塞丁(Seddin)青铜时代墓葬丘(Königsgrab)的年代与地层研究
摘要本研究采用综合的多方法地质考古和地质年代学方法,有助于了解塞丁纪念性墓葬(Konigsgrab)的时间和地层。我们表明,迄今为止建立的基于放射性碳的终点后队列时间框架为公元前910-800年的墓丘的建设提供了光学激发发光(OSL)测年的支持。放射性碳样本是从埋藏土堆正下方的基质中获得的,该土堆被认为代表了埋在该结构下方的晚冰期/全新世土壤。我们使用沉积学(粒度分析)和地球化学分析(元素分析,碳,pH值和电导率测定)来重新评估和确认这一假设。除了与最后一次人为改造有关的埋藏年龄外,OSL测年结果还为该结构所用的原始基质的原始沉积历史提供了新的见解。结合有关环境中晚期发展的区域信息,我们的数据使我们能够提供德国北部晚青铜器时代文化群体“Seddiner grouppe”中Seddin皇家墓的景观发展和多阶段地层学的概观成因模型。根据我们将OSL定年法应用于埋葬丘沉积物的初步经验(据我们所知,这是欧洲的第一次尝试),我们提出了一种最小侵入性的方法,从埋葬丘中获取可测定的材料,并讨论了相关的机遇和挑战。
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