| 水洞沟遗址的环境与地层 |
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| 引用本文： | 周昆叔,胡继兰.水洞沟遗址的环境与地层[J].人类学学报,1988(3). |
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| 作者姓名： | 周昆叔 胡继兰 |
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| 作者单位： | 中国科学院地质研究所
(周昆叔)，内蒙古地质局实验室(胡继兰) |
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| 摘 要： | 水洞沟第四纪地层可与萨拉乌苏河组上段对比。水洞沟遗址包含有新石器和旧石器晚期文化,其旧石器晚期文化发生在距今20,000多年至10,000多年间的黄土状粉砂土中,即发生在末次冰期主冰期的干冷环境下,比发育在距今约35,000—50,000年间的萨拉乌苏河旧石器文化为晚。
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| 关 键 词： | 水洞沟 孢粉分析 环境 地层 |
ENVIRONMENT AND STRATIGRAPHY AT THE SHUIDONGGOU SITE |
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| Zhou Kunshu.ENVIRONMENT AND STRATIGRAPHY AT THE SHUIDONGGOU SITE[J].Acta Anthropologica Sinica,1988(3). |
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| Authors: | Zhou Kunshu |
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| Abstract: | The Shuidonggou site is 30 km northeast to Lingwu county in the Ningxia Hui Autono-mous Region. Neolithic and Late Paleolithic remains were found at this site.
The results of field investigation, chronological research and sporo-pollen analysis show that the Quaternary of Shuidouggou could be correlated with the upper Salawusu river forma-tion. The Late Paleolithic culture is dated to 20-10 thousand years BP. and under dry and cold climate of Pleniglacial of Last glacial. |
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| Keywords: | Shuidonggou Sporo-pollen Analysis Environment Stratigraphy |
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