盘龙城遗址商代灰坑的土壤微形态观察  

Observation of Soil Micromorphology of Shang Dynasty Pit at Panlongcheng site

作　　者：李春霞 张海[1] 庄奕杰[2] LI Chunxia;ZHANG Hai;ZHUANG Yijie(Beijing 100872;London,UK WC1H 0PY)

机构地区：[1]北京大学考古文博学院,北京100871 [2]伦敦大学学院考古系,伦敦WC1H OPY

出　　处：《江汉考古》2024年第5期125-132,共8页Jianghan Archaeology

基　　金：中国国家留学基金委(CSC)“2022年国家建设高水平大学公派研究生项目”资助(证书编号202206010173)。

摘　　要：本研究对盘龙城遗址王家嘴、杨家湾北坡两个地点灰坑内堆积进行了土壤微形态观察。通过薄片观察,我们确定研究涉及的灰坑均为倾倒废弃堆积的场所,但因所处功能区不同,坑内堆积在包含物和土壤发育程度上均存在差别。王家嘴居址区内的H15、H16包含物杂,杨家湾北坡H63坑内堆积来自周边祭祀遗迹,其包含物以与燃烧相关的红烧土和炭屑为主,且土壤发育程度稍高,指示其低于居址区灰坑的使用频率。此外,薄片中观察到的细碎动物骨骼以及可能与灰烬相关的迹象为后续工作提供了重要线索。This study conducted soil micromorphological observations of the deposits in the ash pits at two locations,Wangjiazui and the northern slope of Yangjiawan,within the Panlongcheng site.Through thin-section analysis,we determined that the ash pits examined were sites of discarded waste accumulation;however,differences in the contents and soil development levels were observed due to their distinct functional areas.The H15 and H16 pits in the Wangjiazui residential area contained diverse materials.In contrast,pit H63 on the northern slope of Yangjiawan had deposits primarily associated with nearby ritual sites,dominated by burnt clay and charcoal fragments,indicating a slightly higher level of soil development and suggesting a lower frequency of use compared to the ash pits in the residential area.Additionally,fragmented animal bones and possible ash-related indicators observed in the thin sections provide important clues for future research.

关 键 词：盘龙城遗址 土壤微形态 灰坑 废弃堆积 微观考古 

分 类 号：K871.3[历史地理—考古学及博物馆学]