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Coupled ESR and U-series dating of early Pleistocene Gigantopithecus faunas at Mohui and Sanhe Caves, Guangxi, southern China

机译:中国南部广西墨会和三合洞的早更新世巨猿科动物区系的ESR和U系列耦合测年

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摘要

Several caves of the Guangxi Zhuang Autonomous Region, southern China, have delivered Gigantopithecus blacki remains, an extinct Pleistocene giant ape, in association with abundant mammalian faunas. To determine their geological ages, fossil teeth from Mohui and Sanhe Caves were dated using the coupled ESR/U-series method. The teeth from Mohui Cave gave age estimates of 1.69 +/- 0.22 Ma and 1.29 +/- 0.11 Ma. The Sanhe Cave samples had age estimates ranging from 910 +/- 200 ka to 600 +/- 150 ka with error weighted mean ages of 890 +/- 130 ka and 720 +/- 90 ka for the layers 5 and 4, respectively. Our results and previous paleomagnestism data place the Gigantopithecus fauna at Mohui Cave between Olduvai and Jaramillo subchrons and suggest that it was coeval with Chuifeng, Longgupo and Liucheng assemblages. The Sanhe fauna is younger, of late early Pleistocene age, and can be dated to the period between Jaramillo subchron and B/M boundary. (C) 2015 Elsevier B.V. All rights reserved.
机译:中国南方的广西壮族自治区的几个山洞已经运送了已灭绝的更新世巨猿黑巨猿(Gigantophitothecus blacki),并饲养了丰富的哺乳动物。为了确定其地质年龄,使用结合的ESR / U系列方法确定了磨合洞和三河洞的化石牙齿。来自莫会洞的牙齿的年龄估计为1.69 +/- 0.22 Ma和1.29 +/- 0.11 Ma。三河溶洞样品的年龄估算范围为910 +/- 200 ka至600 +/- 150 ka,第5层和第4层的误差加权平均年龄分别为890 +/- 130 ka和720 +/- 90 ka。我们的研究结果和先前的古动物学资料将巨嘴鸟科动物区系置于Olduvai和Jaramillo次世代之间的Mohui洞穴中,表明它与Chuifeng,Longgupo和Liucheng组合处于同一时期。三河动物区系较年轻,处于更新世晚期晚期,可以追溯到Jaramillo次纪与B / M边界之间的时期。 (C)2015 Elsevier B.V.保留所有权利。

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