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首页> 外文期刊>Journal of Archaeological Science >Two independent methods for dating rock art: Age determination of paint and oxalate layers at Eagle Cave, TX
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Two independent methods for dating rock art: Age determination of paint and oxalate layers at Eagle Cave, TX

机译:鹰洞,TX的两种独立方法:鹰洞涂料和草酸层

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摘要

This study demonstrates a novel approach to overcoming challenges associated with obtaining reliable radio-carbon dates for rock paintings. Using two independent methods, we obtained ages for Pecos River style paintings at Eagle Cave in Langtry, Texas. The first method employed plasma oxidation to isolate organic carbon directly from the paint layer for accelerator mass spectrometry C-14 measurement. The second method treated mineral accretion layers with phosphoric acid to isolate calcium oxalate for plasma oxidation cleaning, com-bustion, and C-14 measurement to obtain minimum and maximum ages for the paintings. Radiocarbon dates for the paintings are statistically indistinguishable, with a weighted average of 3280 ? 70 years BP calibrated to 1740-1420 cal BC (3690-3370 cal BP) at 2 sigma (95.4%) probability. Radiocarbon assays obtained for the overlying accretion layers are younger and underlying accretion layers are older. The chronological stratigraphy of the accretion and paint layers supports the validity of both dating methods. With accurate and reliable dating methods, rock paintings in the region can be studied alongside excavated cultural deposits to provide a more complete understanding of this hunter-gather society. These methods for dating rock paintings can be applied to many rock art provinces around the world.
机译:这项研究展示了一种新的方法,可以克服与获得可靠的岩画放射性碳数据相关的挑战。使用两种独立的方法,我们获得了德克萨斯州朗特里的鹰洞佩科斯河风格绘画的年代。第一种方法是利用等离子体氧化直接从油漆层中分离出有机碳,用于加速器质谱仪C-14测量。第二种方法是用磷酸处理矿物沉积层,分离草酸钙,用于等离子体氧化清洗、燃烧和C-14测量,以获得绘画的最小和最大年龄。这些画的放射性碳年代在统计上无法区分,加权平均数为3280?70年血压以2西格玛(95.4%)的概率校准至1740-1420 cal BC(3690-3370 cal BP)。上覆吸积层的放射性碳分析结果较年轻,下伏吸积层较老。沉积层和油漆层的年代地层学支持这两种年代测定方法的有效性。通过准确可靠的年代测定方法,可以对该地区的岩画和挖掘出的文化沉积物进行研究,从而更全面地了解这个猎人聚集的社会。这些测定岩画年代的方法可以应用于世界各地的许多岩画省份。

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