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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >Hominin distribution in glacial-interglacial environmental changes in the Qinling Mountains range, central China
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Hominin distribution in glacial-interglacial environmental changes in the Qinling Mountains range, central China

机译：中国中部秦岭山脉冰川间环境变化的母亲分布

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The Qinling Mountain Range (QMR) in central China encompasses innumerable Paleolithic sites. The hominin settlement in the QMR is comparable with that in the Nihewan Basin in northern China. The recorded information on the loess deposition in the QMR include both hominin remains and environmental changes. Since 2004, geological, geomorphological, archaeological, and chronological investigations were conducted by our team. By systematically using luminescence, paleomagnetic, and Al-26/Be-10 burial dating methods to obtain age controls, and by correlating the pedostratigraphy and magnetic susceptibility of the Luochuan loess section, we established the loess-paleosol sequence and chronology of the lithic artifact levels for 35 Paleolithic sites and spots in the QMR. This work remarkable found shifts from glacial-to interglacial-driving hominin settlement patterns. During the stage between 1.2 and 0.7 Ma, large drying events, such as L15 (MIS 38) and L9 (MIS 22, 23 and 24), may have driven hominin migrations when the Loess Plateau was depopulated; moreover, the southern QMR was a glacial refugium. During the stage after similar to 0.60 Ma, the contrasts between glacial and interglacial scales are the greatest; furthermore, longer and warmer humid interglacial environments were dominant. S5 (MIS 13, 14, 15) and S1 (MIS 5) interglacial periods provided the optimal environments for hominin settlement and dispersal. On the basis of investigations, we also found that the hominin settlement is relatively continuous from similar to 1.20 Ma to similar to 0.05 Ma in the QMR. The human occupation of the QMR decreased considerably after similar to 0.05 Ma, probably because of changes in climate and human adaptations. (C) 2018 Elsevier Ltd. All rights reserved.
机译：中部秦岭山脉（QMR）包括无数旧石器时代的遗址。 QMR中的Hominin解决方案与中国北方尼河盆地的北方河流盆地相当。关于QMR中黄土沉积的记录信息包括Hominin遗骸和环境变化。自2004年以来，我们的团队进行地质，地貌，考古和年表调查。通过系统地使用发光，古磁石和AL-26 / BE-10墓葬数据来获得年龄控制，并通过将洛川黄土部分的女性化学和磁化率相关，我们建立了岩石工件的黄土 - 古溶胶序列和年表35个古石英网站和QMR中斑点的水平。这项工作的显着发现从冰川到中间钎焊的主体沉降模式转移。在1.2和0.7 mA之间的阶段，当黄土高原分开时，大量干燥事件如L15（MIS 38）和L9（MIS 22,23和24），可能已经驱动了Hominin迁移;此外，南方QMR是一种冰川避难所。在类似于0.60 mA之后的阶段，冰川和中间爆垢之间的对比是最大的;此外，更长，更温暖的潮湿的潮湿的中间爆炸性环境占主导地位。 S5（MIS 13,14,15）和S1（MIS 5）中间尖端为宿主和分散提供最佳环境。在调查的基础上，我们还发现，在QMR中，同性恋沉降与类似于1.20 mA相似的同样为0.05 mA。在类似于0.05 mA的情况下，QMR对QMR的人类占用可能是由于气候和人类适应的变化。 （c）2018年elestvier有限公司保留所有权利。

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