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洞穴沉积物的光释光测年研究——以中国东北小孤山史前遗址为例

Optically stimulated luminescence dating of cave deposits at the Xiaogushan prehistoric site, northeastern China.

机构信息

Laboratory for Earth Surface Processes, Department of Geography, Peking University, Beijing 100871, China.

出版信息

J Hum Evol. 2010 Nov;59(5):514-24. doi: 10.1016/j.jhevol.2010.05.008. Epub 2010 Aug 17.

Abstract

The Xiaogushan cave site is one of the most important prehistoric sites in North China. The stone and bone artifacts found in the cave are similar to European contemporaneous artifacts. Cave deposits consist of five layers that have been dated from 46,353 ± 1179 to 4229 ± 135 cal. yr BP, using radiocarbon dating techniques on charcoal and bone samples collected from Layers 2-5. In this paper, optically stimulated luminescence (OSL) techniques were applied to date six samples taken from Layers 1-3. The luminescence properties of the fine-grained and coarse-grained quartz extracts indicate that the materials are suitable for OSL dating using a single-aliquot regeneration-dose (SAR) protocol. The OSL ages obtained are broadly consistent with the stratigraphy and the associated calibrated radiocarbon ages. The dating results show that the cave was first occupied by humans about 70 ka. The human occupation of the cave may be related to climate change. An occupation hiatus is inferred to between ∼ 17 to ∼ 10 ka. The stone and bone artifacts found in Layers 2 and 3 may indicate the Middle to Upper Paleolithic transitions in the region.

摘要

小孤山洞穴遗址是华北最重要的史前遗址之一。洞穴中发现的石器和骨器与欧洲同期的文物相似。洞穴沉积物由五层组成,使用从第 2 层到第 5 层采集的木炭和骨骼样本的放射性碳测年技术,其年代可追溯到 46353±1179 到 4229±135 cal. yr BP。本文应用光释光(OSL)技术对取自第 1-3 层的 6 个样本进行了年代测定。细粒和粗粒石英提取物的发光性质表明,这些材料适合使用单剂量再生(SAR)协议进行 OSL 定年。获得的 OSL 年龄与地层学和相关的放射性碳校准年龄基本一致。定年结果表明,洞穴最初是在约 70ka 前被人类占据的。洞穴的人类居住可能与气候变化有关。推断在约 17 到约 10ka 之间存在一个居住中断。在第 2 层和第 3 层发现的石器和骨器可能表明该地区处于中更新世到上新世的过渡时期。

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