人类学学报 ›› 2003, Vol. 22 ›› Issue (02): 139-144.

• 人类学学报 • 上一篇    下一篇

江西新余旧石器地点的埋藏环境与时代

房迎三,李徐生,杨达源   

  • 出版日期:2003-06-15 发布日期:2003-06-15

Paleoenvironmental and chronlogical analyses of the Daguling Paleolithic Locality, Xinyu Xity,Jiangxi Pronvince

FANG Ying-san; LI Xu-sheng; YANG Da-yuang   

  • Online:2003-06-15 Published:2003-06-15

摘要: 本文通过对江西新余打鼓岭旧石器地点及邻近地区沉积物的系统采样分析和石英电镜扫描观察,探讨其沉积学特征和环境意义,提出打鼓岭含石制品的中、上部沉积物为风尘堆积,性质与北方典型黄土和长江下游土状堆积相似,石制品应为原生就地埋藏。用光释光法试测打鼓岭中、上部2个沉积物样品,年代分别为36.1±2.6ka和64.2±4.9ka,表明石制品时代相当于旧石器晚期或稍早一些

关键词: 旧石器;埋藏环境;光释光测年;新余;江西

Abstract: The Daguling Paleolithic locality is situated at the second terrace of the Yuanshui River, a branch of the Ganjiang River in the Xinyu City, Jiangxi Province. More than 40 stone artifacts were collected from the site in 1997, which exhibit close affiliation with the Laterite Paleolithic Culture in South China. The representative deposit section at the site contains loess-like silty clay of more than 10 m thick. Through analyzing the granulometric, chemical composition and heavy mineral elements of the deposits and observing the surface characteristics of quartz grains by electron microscope, it is concluded that the deposits are aeolian, and the Xinyu loess was deposited in a climatic condition warmer and wetter than that of the loess of northern China and the Xiashu Loess in lower reaches of the Yangtze River. The OSL dating results indicate that the ages of the upper and middle part the deposits are 36. 1 ±2. 6 ka and 64. 2 ±4. 9 ka, respectively. Therefore, it is concluded that the Daguling cultural horizon is formed during the Upper Paleolithic.

Key words: Paleolithic; Taphonomic environment; OSL dating; Daguling; Jiangxi