河南贾湖遗址考古地层分析  

Archaeological Stratum Study on the Jiahu Neolithic Site in Henan province

作　　者：凡小盼[1] 秦颍[2] 姚政权 

机构地区：[1]重庆中国三峡博物馆,重庆400015 [2]中国科学院研究生院科技史与科技考古系,安徽合肥230026 [3]安徽省考古研究所,安徽合肥230061

出　　处：《江汉考古》2011年第1期101-108,共8页Jianghan Archaeology

基　　金：国家自然科学基金重点项目(10135050);国家文博类基金(2001042)资助

摘　　要：贾湖遗址是属于裴李岗文化的一个重要遗址,是目前所见的中原地区年代最早的新石器时代遗址。本文主要通过贾湖遗址T107B和T43两个剖面样品的粒度分析和地球化学元素分析来推测当时的环境;并以该遗址为例,尝试利用地球化学多元统计分析进行考古探方之间层位关系对比的可行性。分析表明贾湖地区新石器时代考古地层主要代表了一种洪积,及局部的洼地沼泽相沉积(即顶积层),且新石器时代早期气候较为湿热,晚期则向干旱方向转化。The Jiahu Site is the earliest Neolithic site at present in the Central Plain belonging to the Peiligang Culture. This paper studies researches the environment of that time firstly, according to the granularity analyses and element analyses of samples collected from archaeological strata in the section of excavated pit 107B and T43, and then tries to use using the content of chemical element of the earth to compare with the layers of different excavated pits and establish the relationship between of them. It suggests that the Neolithic sediments at Jiahu is mainly composed of the alluvial deposits mixed with part of fluvial sediment. The climate during the early Neolithic was warm and moist and tended to gradually dry and cool during the later period.

关 键 词：贾湖 粒度 元素分析 环境考古 

分 类 号：K871.13[历史地理—考古学及博物馆学]