中国黄土高原中部南佐考古遗址受热材料的多重发光测年法

IF 2.6 1区 地球科学 Q1 ANTHROPOLOGY Journal of Archaeological Science Pub Date : 2024-05-24 DOI:10.1016/j.jas.2024.106005
Daobin Tang , Xiangjun Liu , Guanghui Dong , Jianye Han , Xiaoning Zhang , Kartika Goswami , Xianjiao Ou
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引用次数: 0

摘要

南佐是中国黄土高原中部一处重要的新石器时代考古遗址。该遗址对了解中华文明的起源和发展非常重要,但却缺乏一个强有力的年代框架。本次研究首次使用各种发光测年技术对南召考古遗址主发掘区附近剖面上两种不同类型的受热材料(陶器和烧土)进行了测年。这些技术包括对烧土样本和陶器进行单颗粒(SG)石英 OSL 和 K 长石后红外激发(pIRIR)测年,以及利用岩石表面发光技术(RSL)对陶片进行 pIRIR 测年。通过将 SG 石英、钾长石和陶片的年代与同一文化层的放射性碳(14C)年代进行比较,研究了发光测年的可靠性。结果表明,两件粗陶器的 SG 石英 OSL 和 K 长石 pIRIR225 年龄估计值与 14C 年龄一致,但陶片(NZ22-CPS150)的年龄估计值明显偏小,主要原因是等效剂量(De)估计不足。此外,虽然粗陶片的 De 随深度变化很大,但钾含量与 De 之间没有明显的相关性。μ-XRF扫描显示,粗陶片的钾含量不均匀。相反,细陶显示出均匀的钾含量分布和与 14C 年龄一致的年龄估计。因此,与粗陶片相比,细陶片更适合进行 pIRIR 测定。与 SG K 长石相比,混合矿物中的 De 值被低估是造成切片年代被低估的主要原因,而 K 长石的粒度和 K 含量的变化仅起次要作用。因此,通过将 14C 年龄与陶器的发光年龄相整合,可以推断南左遗址的人类活动发生在距今约 5100 至 4500 年之间,这与南左遗址主断面获得的 14C 年龄相吻合。目前的工作进一步得出结论,单颗粒发光测年法对于陶器是可靠的。研究建议优先使用钾(K)含量相对均匀的材料,利用陶片进行 pIRIR 测定。
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Multiple luminescence dating on heated materials at the nanzuo archaeological site, central Chinese Loess Plateau

Nanzuo is a key Neolithic archaeological site in the central Chinese Loess Plateau (CCLP). The site is important for understanding the origin and development of the Chinese civilization, yet, it lacks a robust chronological framework. The current work, for the first time, dates two different types of heated materials (pottery and burnt soil) from a profile near the main excavation of the Nanzuo archaeological site using various luminescence dating techniques. These techniques included single grain (SG) quartz OSL and K-feldspar post-infrared infrared-stimulated (pIRIR) dating for burnt soil samples and pottery, and pIRIR dating for pottery slices using the rock surface luminescence technique (RSL). The reliability of luminescence dating was investigated by comparing SG quartz, K-feldspar and pottery slice ages with radiocarbon (14C) ages obtained from the same cultural layer. The results show that the SG quartz OSL and K-feldspar pIRIR225 age estimates of the two coarse potteries are consistent with the 14C ages, however, the age estimates of the pottery slice (NZ22-CPS150) are significantly younger, which is primarily explained by underestimation in equivalent doses (De). Moreover, it is noted that while there is a considerable variation in the De of coarse pottery slices with depth, no significant correlation is observed between K- content and De. Heterogeneous K content was revealed by μ-XRF scanning on coarse pottery slices. Conversely, fine pottery displayed homogeneous K-content distribution and age estimates consistent with the 14C ages. Thus fine pottery slices are suggested to be more suitable for pIRIR dating relative to coarse pottery slices. The underestimation of De values in mixed minerals is observed as the primary reason for underestimated slice ages compared to SG K-feldspar, with grain size of K-feldspar and K content variation playing only a minor role. Therefore, by integrating the 14C ages with the luminescence ages of the pottery, it is inferred that human occupation of the Nanzuo site occurred around 5100 to 4500 years ago, which aligns with the 14C ages obtained from the main section of the Nanzuo site. The current work further concludes that the single-grain luminescence dating method is reliable for pottery. The study recommends to prioritize materials characterized by relatively uniform potassium (K) content for pIRIR dating using pottery slices.

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来源期刊
Journal of Archaeological Science
Journal of Archaeological Science 地学-地球科学综合
CiteScore
6.10
自引率
7.10%
发文量
112
审稿时长
49 days
期刊介绍: The Journal of Archaeological Science is aimed at archaeologists and scientists with particular interests in advancing the development and application of scientific techniques and methodologies to all areas of archaeology. This established monthly journal publishes focus articles, original research papers and major review articles, of wide archaeological significance. The journal provides an international forum for archaeologists and scientists from widely different scientific backgrounds who share a common interest in developing and applying scientific methods to inform major debates through improving the quality and reliability of scientific information derived from archaeological research.
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