年首次确定岩画年代Ẓufār(阿曼苏丹国):低能等离子体氧化放射性碳采样

IF 1.6 3区 地球科学 Q3 GEOGRAPHY, PHYSICAL
Holocene Pub Date : 2022-12-29 DOI:10.1177/09596836221145402
M. Rowe, Jean-Loïc Le Quellec, Shelby A Jones, E. Blinman, C. Welte, F. Duquesnoy, V. Charpentier, A. Al-Mashani, Ali Aḥmed al-Kathiri
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引用次数: 0

摘要

我们成功地在一幅黑色几何岩画的两个样本上测量了四个放射性碳年代,其中一块碎片有可能在Ẓ阿曼苏丹国南部的乌法尔地区。在新墨西哥州圣达菲考古研究办公室的等离子体氧化实验室中提取二氧化碳(CO2),用于岩画样本黑色颜料中粘合剂的放射性碳年代测定。放射性碳含量是在瑞士ETH-Zürich加速器质谱仪MICADAS上测量的。在统计不确定性范围内,获得的日期彼此一致,四个样本的平均日期为1500 ± 35放射性碳年BP。平均日期的日历当量导致日历校准日期范围从五世纪中期到七世纪中期(440–453 CE、478–496 CE和534–646 CE)。这项研究表明,可以确定阿曼杰贝尔·卡拉地区的黑色绘画的年代;这是该地区第一个使用放射性碳年代测定法测年的象形图。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
First dating of a rock painting in Ẓufār (Sultanate of Oman): Low energy plasma oxidation radiocarbon sampling
We successfully measured four radiocarbon dates on two specimens of a black geometric rock painting with a fragment in jeopardy of naturally spalling off in the wall of a rock shelter in the Ẓufār region, in the south of the Sultanate of Oman. Extraction of carbon dioxide (CO2) for radiocarbon dating of the binder in the black pigment of the rock painting specimen was conducted in the plasma oxidation laboratory at the Office of Archeological Studies in Santa Fe, NM. The radiocarbon content was measured on the Swiss ETH-Zürich accelerator mass spectrometer MICADAS. The dates obtained agreed with one another within the statistical uncertainty and the average date of the four samples was 1500 ± 35 radiocarbon years BP. The calendric equivalents of the average date results in calendric calibration date ranges that span the mid-fifth through mid-seventh centuries (440–453 CE, 478–496 CE, and 534–646 CE). This research demonstrates that it is possible to date the black paintings of the Jebel al-Qara’ area of Oman; this is the first pictogram that was dated using radiocarbon dating in the region.
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来源期刊
Holocene
Holocene 地学-地球科学综合
CiteScore
4.70
自引率
8.30%
发文量
106
审稿时长
4 months
期刊介绍: The Holocene is a high impact, peer-reviewed journal dedicated to fundamental scientific research at the interface between the long Quaternary record and the natural and human-induced environmental processes operating at the Earth''s surface today. The Holocene emphasizes environmental change over the last ca 11 700 years.
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