人类学学报 ›› 2001, Vol. 20 ›› Issue (03): 229-237.

• 人类学学报 • 上一篇    下一篇

洛南盆地旧石器遗址地层划分及年代研究

王社江,黄培华   

  • 出版日期:2001-09-15 发布日期:2001-09-15

Stratigraphy and TL dating of Paleolithic sites in the Luonan Basin, southern Shannxi, China

WANG She-jiang , HUANG Pei-hua   

  • Online:2001-09-15 Published:2001-09-15

摘要: 1995— 1999年 ,在秦岭东部山区的洛南盆地发现 5 0处旷野类型旧石器地点 ,并对花石浪龙牙洞洞穴遗址进行发掘 ,获得大量旧石器材料。本文对洛南盆地旧石器遗址地层进行了划分及对比研究 ,并进行了热释光 (TL)测年数据分析。从地层对比及所测 5个样品结果判断 ,龙牙洞及二级阶地地层年代属中更新世中晚期 (Q22— 3 ) ,与北京直立人洞穴堆积层相当 ,绝对年代距今 2 5— 5 0万年左右 ,属旧石器时代早期。

关键词: 地层划分; 热释光年代; 旧石器遗址; 洛南盆地

Abstract: The Huashilang Longyadong Cave site along with open-air sites of Paleolithic were identified for the first time, and then excavated and investigated during 1995-1999 in the Luonan Basin, Luonan county, Shaanxi province, China.More than 2 000 stone artifacts were collected from the 50 open-air sites and about 20 species animal fossils along with 65000 artifacts were excavated from the Longyadong cave. This paper provides a preliminary study of site formation of lithic-stratigraphy in their geological context as well as results of TL dating.
Supported by relationship of the 8 strata, three cultural periods were divided in the Longyadong cave site.In the first period, humans lived in the river bank; In the second period, they lived in the cave and on the terrace, the climate was dry and cold; The third period was a main deposit time in the Longyadong cave site, most artifacts and ash layers were identified in this period, the climate was warm and moist.After that time, no hominid remains were identified.
The five samples of the TL dates (three from the cave site and the other two from the Zhoupo open-air site 95LP07)place the site into the middle to late period of the Middle Pleistocene (Q2 2—3). The three samples in the Longyadong cave site were collected from the third middle period of the inner cave and the upper layer of the outer cave.The two TL dates from inner cave are 356.6 ±17.8ka and 273.9 ±13.7ka respectively, and another from the outer cave is 210.5 ±10.5ka.It is suggested that the early hominids left this site about 250ka ago because no cultural remains were found both in the inner cave and the upper layer of the slope deposits of the outer cave.The other two samples from upper layer of the Zhoupo site are 251.05 ±12.5ka and 182.8 ±9.1ka respectively.
Compared the TL dates with the stratigraphic data of Zhou-koudian Peking Man site, loess depos- its in the Shaanxi Luochuan, the red earth in Anhui and deep-sea records, the dates of the sites we are dealing with in this article are in range of about 500-250 ka, which is in the same timeframe of Zhoukoudian Peking Man site.Therefore, culturally the sites can be suggested to be Early Paleolithic.

Key words: Stratigraphy; TL Dating; Paleolithic; Luonan Basin