河南登封方家沟遗址的埋藏学观察

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英文篇名：The Taphonomy Observation of the Fangjiagou Site,Dengfeng 作者：林壹 英文作者：Lin Yi; 关键词：方家沟遗址 ; 埋藏学 ; 沟状遗迹 ; 活动面 英文关键词：Fangjiagou site;;taphonomy;;ditch-shaped feature;;living floor 中文刊名：ZYWW 英文刊名：Cultural Relics of Central China 机构：郑州大学历史学院; 出版日期：2018-12-20 出版单位：中原文物 年：2018 期：No.204 基金：郑州中华之源与嵩山文明研究会重大项目“东亚现代人起源——以嵩山地区为中心的研究”(课题编号:DZ-3);; 中国博士后科学基金项目“登封方家沟旧石器时代遗址出土脉石英石制品的微痕分析”(资助编号:2018M632788)的阶段性成果 语种：中文; 页：ZYWW201806009 页数：8 CN：06 ISSN：41-1012/K 分类号：64-70+131

摘要

河南登封方家沟遗址的旧石器时代文化遗存主要埋藏于距今约5—3万年的河漫滩相堆积中,其中最重要的发现是沟状遗迹G1,多数遗物出土于该层位。根据地层观察和遗物分布情况推断G1边界代表了原生的堆积间界面;而从遗物保存状况、产状、尺寸构成等情况综合考察,遗物应未经流水等自然力的强烈改造;结合石器拼合与空间分析,G1的壁和底应代表了古人类一次活动事件所依托的古地面。
        The Fangjiagou site is located at Dengfeng city,Henan Province. The Paleolithic stratigraphicsequence consists mainly of floodplain deposits dating to about 50-30 ka BP. It is important that a ditch-shaped feature(named G1) was identified and most artifacts are buried in such shallow depressions.According to the observation of stratum and distribution of artifacts, it is inferred that the G1 boundaryshould be the original interface, rather than the result of secondary deposition. Based on the comprehensiveinvestigation of artifacts, including condition of preservation, occurrence and size composition, thearchaeological materials were not heavily transformed by natural forces such as flowing water. Combined withlithic refitting and spatial patterning,we conclude that the wall and bottom of G1 should be a living floorwhich an ancient occupation was based on.

引文

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