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首页> 外文期刊>Quaternary geochronology >~(230)Th/U chronology of a paleolithic site at Xinglong Cave in the three-Gorge region of south China
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~(230)Th/U chronology of a paleolithic site at Xinglong Cave in the three-Gorge region of south China

机译:华南三峡地区兴隆洞古岩质遗址的〜(230)Th / U年代学

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Xinglong Cave, containing four human teeth, numerous mammalian fossils, stone artifacts and a Stegodon tusk with intentional and seemingly grouped engravings, is one of the most significant archaic Homo sapiens sites in south China, located 95 km south of Fengjie County, in Chongqing. In an attempt to constrain the age of the human relics, calcitic flowstone deposits with a significant detrital component were dated by U-Th methods using a leachate scheme. Total sample digestion MC-ICPMS dating was used to assess the reliability of the leachate technique. Six calcite samples from horizons beneath and above the fossil-bearing layer were dated. We obtained ages of 130 ± 9.1, 124 ± 11, 135 ± 12 and 127 ± 11 ka for the flowstones above the fossil layer with a weighted mean of 128.9 ± 5.2 ka. Two flowstone samples gave MC-ICPMS dates between 128.3 ± 3.3 and 152.4 ± 25.3 ka with an assumed detrital component to correct for the initial ~(230)Th, which are consistent with results obtained using the L/ L regression data from layer U-4 within uncertainty. All errors herein quoted at the 2s level. Ages determined for the flowstone underlying the fossil-bearing layer were 221 ± 29 to 189 ± 19 ka with a weighted mean age of 199 ± 16 ka. These results are stratigraphically consistent within error limits and show that the cave was occupied by Fengjie Man within the time range of ~200 to ~130 ka. These new Useries ages of flowstones in association with human teeth and an engraved stegodon tusk at the Xinglong Cave site provide valuable geochronologic information for the study of the origin of modern humans in East Asia and earliest human art.
机译:兴隆洞是重庆市奉节县以南95公里的华南地区最重要的古朴智人遗址之一,其中有四颗人类牙齿,许多哺乳动物化石,石器和一个剑齿象牙,上面刻有故意和看似成组的雕刻。为了限制人类文物的年龄,采用渗滤液方案通过U-Th方法对具有重要碎屑成分的钙质流石沉积物进行了测年。使用总样品消解MC-ICPMS测年法评估渗滤液技术的可靠性。在含化石层之下和之上的地平线上标出了六个方解石样品。对于化石层上方的流石,我们获得的年龄为130±9.1、124±11、135±12和127±11 ka,加权平均值为128.9±5.2 ka。两个流石样品的MC-ICPMS日期在128.3±3.3和152.4±25.3 ka之间,并具有假定的碎屑成分以校正初始〜(230)Th,这与使用来自U-层的L / L回归数据获得的结果一致4在不确定范围内。本文中所有错误均以2s级引用。化石层下面的流石测定的年龄为221±29至189±19 ka,加权平均年龄为199±16 ka。这些结果在误差范围内在地层上是一致的,并且表明该洞穴在〜200至〜130 ka的时间范围内被奉节人占领。这些新的乌尼族时代的流石与人类的牙齿以及在兴隆洞遗址上刻制的剑齿象牙相关,为研究东亚现代人类起源和最早的人类艺术提供了宝贵的年代学信息。

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