A method to date rock engravings using luminescence – tested at Murujuga, Western Australia

IF 1.7 2区 地球科学 Q3 GEOGRAPHY, PHYSICAL
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Abstract

Rock engravings are globally ubiquitous, provide evidence for symbolic behaviours, and demonstrate connections to country and the desire to communicate with other humans. However, rock engravings have proven difficult to date. The development of luminescence rock surface dating approaches has the potential to address this deficiency in applicable dating techniques. Specifically, luminescence rock surface exposure dating methods can be used to tell how long a rock surface has been exposed to sunlight, thus providing a potential avenue to date rock engravings. Here, we present results from laboratory and field bleaching experiments from the Murujuga rock art complex in Western Australia. Four major art-bearing lithologies are petrographically characterised and tested for useable luminescence signals. Three bleaching experiments are conducted: two in the laboratory and one at the study area. The gabbro and microgranite lithologies are shown to be bleachable and show potential for rock surface burial dating. The microgranite can be used to accurately estimate exposure duration over the timescales tested in all experiments, demonstrating promising potential to date rock engravings.
利用发光法确定岩刻年代的方法--在西澳大利亚穆鲁朱加进行了测试
岩刻在全球无处不在,为象征性行为提供了证据,并展示了与国家的联系以及与其他人类交流的愿望。然而,事实证明岩刻很难确定其年代。发光岩石表面测年方法的开发有可能解决适用测年技术的这一不足。具体来说,发光岩石表面暴露年代测定方法可以用来确定岩石表面暴露在阳光下的时间,从而为岩石雕刻的年代测定提供了一个潜在的途径。在此,我们展示了西澳大利亚穆鲁朱加岩画群的实验室和实地漂白实验结果。我们对四种主要的岩画岩性进行了岩相表征,并测试了可用的发光信号。进行了三次漂白实验:两次在实验室,一次在研究区。结果表明辉长岩和微花岗岩岩性是可漂白的,并显示出岩石表面埋藏年代测定的潜力。微花岗岩可用于准确估算所有实验中测试的时间尺度上的暴露持续时间,显示出对岩石雕刻进行年代测定的巨大潜力。
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来源期刊
Quaternary Geochronology
Quaternary Geochronology 地学-地球化学与地球物理
CiteScore
4.40
自引率
22.20%
发文量
130
审稿时长
20 weeks
期刊介绍: Quaternary Geochronology is an international journal devoted to the publication of the highest-quality, peer-reviewed articles on all aspects of dating methods applicable to the Quaternary Period - the last 2.6 million years of Earth history. Reliable ages are fundamental to place changes in climates, landscapes, flora and fauna - including the evolution and ecological impact of humans - in their correct temporal sequence, and to understand the tempo and mode of geological and biological processes.
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