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Lichenometric dating and the nature of the excavation of the Huashan Grottoes, East China

机译:华东华山石窟的地衣测年与发掘性质

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The present study aims to identify the timing of the Huashan Grottoes' excavations using the lichenometric dating method. A total of 96 maximum inscribed circle diameters of Rhizocarpon geographicum growing on the ancient architectures and the walls of entrances are measured in the Huashan Grottoes area of southern Anhui, East China. The results show that the period of the grottoes' excavation is estimated to be 450-335 yr BP, or the middle and late Ming Dynasty (1552-1667 AD). The lichenometric dating results are also validated by a lithologic comparison of the grottoes and the surrounding ancient architectures, as well as by the studies on the historical documents and the fragments of ancient porcelain in the grottoes. Furthermore, we infer that the excavation of the inner grottoes might have lasted till the Qing Dynasty (1636-1912 AD), because the lichens chosen for dating are mainly at the grottoes' entrances. The wider significance of this work is that it demonstrates, for the first time, lichenometric dating can be applied in the historical studies on the ancient architectures in East China with a relatively warm and humid climate.
机译:本研究旨在利用地层测年法确定华山石窟开挖的时间。在中国东部安徽南部的华山石窟地区,测量了在古代建筑和入口壁上生长的地理根瘤菌的最大内切圆直径,共计96个。结果表明,石窟的开挖时期估计为450-335年BP,即明代中晚期(公元1552-1667年)。地衣测年的结果还通过对石窟与周围古代建筑的岩性比较以及对石窟中的历史文献和古代瓷器碎片的研究得到证实。此外,我们推断内部石窟的发掘可能一直持续到清朝(公元1636-1912年),因为选择进行约会的地衣主要在石窟的入口处。这项工作的更广泛的意义在于,它首次证明了地衣法测年法可以用于对华东地区具有相对温暖和潮湿气候的古代建筑的历史研究。

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