人类学学报 ›› 2023, Vol. 42 ›› Issue (03): 381-389.doi: 10.16359/j.1000-3193/AAS.2023.0008

• 简报/发掘报告 • 上一篇    下一篇

黄河中游山西吉县冯家坡遗址发掘简报

宋艳花(), 申如梦   

  1. 山西大学考古文博学院, 太原030006
  • 收稿日期:2022-03-24 修回日期:2022-10-31 出版日期:2023-06-15 发布日期:2023-06-13
  • 作者简介:宋艳花,教授,主要从事旧石器时代考古学研究。E-mail: songyanhuahan@163.com
  • 基金资助:
    国家重点研发计划项目(2020YFC1521500);国家社科基金重点项目(20AKG001);中国科学院战略性先导科技专项(XDB26000000)

A preliminary report of test excavation at the Fengjiapo site, Jixian, Shanxi Province

SONG Yanhua(), SHEN Rumeng   

  1. School of Archaeology and Museology, Shanxi University, Taiyuan 030006
  • Received:2022-03-24 Revised:2022-10-31 Online:2023-06-15 Published:2023-06-13

摘要:

冯家坡遗址是山西吉县境内黄河中游一级阶地的一处旧石器向新石器时代过渡阶段的遗址。2021年,在面积3 m2、厚约0.15 m的地层中,我们发掘出342件石制品和130件动物骨骼。石制品原料以石英岩为主,其他为燧石、石英、砂岩和变质岩;类型包括石核、石片、断块(片)、碎屑、细石叶和石器;石器类型丰富,中有刮削器,尖状器、石锥、端刮器、砍砸器和研磨石等;另外,还有使用过的石片和断片;打片和加工以锤击法为主,也使用了压制法,未见砸击技术。动物骨骼破碎,且多被钙质裹覆;只能辨识出鹿科和牛科动物的牙齿碎片;有4件碎骨表面尚保留清晰切割痕迹。遗物中较多的碎屑,表明未经较远距离搬运,属于原地埋藏。文化层中动物骨骼AMS 14C测年数据约11.5~10.7 kaBP cal,正好处于新仙女木冰阶后的气候迅速回暖期。

关键词: 黄河, 冯家坡, 旧石器, 细石器, 旧-新石器时代

Abstract:

The Fengjiapo site (36°14′59.96″N, 110°28′37.15″E; 484.63 m above sea level) is an open-air Paleo-Neolithic site located along the middle Yellow River, about 1500 m west of Fengjiapo village, Jixian County, Shanxi Province, North China. It was salvaged excavated in March 2021. The 3 m2 excavation area features a 0.15 m thick Palaeolithic cultural layer dated 11.5~10.7 kaBP cal, above which is 2.5 m thick Western Zhou Dynasty deposition with pottery shards. Three-dimensional measurements were not recorded during the excavation. A total of 472 Palaeolithic objects, including 342 lithic artifacts(72.46%) and 130 animal bones (27.54%) were densely and irregularly distributed in the very top of the mealy sand layer in Layer 5, but also scattered in layers 4 and 3. The cultural layers featured a “core and flake” industry (recently referred to as “flake and shatter”) along with microblades. Stone raw materials are mainly quartzite(n=210; 61.40%) with some flint (n=86; 25.15%), sandstone (n=33; 9.65%), and quartz (n=13; 3.80%) that were all easily available along the riverside. Lithics consisted cobbles (n=1; 0.29%), cores (n=5; 1.46%), flakes (n=108; 31.58%), chunks (n=127; 37.13%), chips (n=84; 24.56%), microblades (n=4; 1.17%), and tools (n=13; 3.80%), such as a chopping tool, point, end-scraper, drilling tool, and grinding stone, and eight scrapers. Assemblages were dominated by flakes, chunks and chips produced by hard or soft hammer percussion, also including microblade technology, with no evidence for anvil (bipolar) percussion. Several flakes and chunks were used with clear microwear observed along used edges. Usewear analyses showed main functions connected with cutting, scraping and grinding, with further studies planned. Debitage indicated in situ human activities of tool making and using and with many chips, which indicated little transport.
All animal bones were broken into pieces, with nearly half (57/130) affected by fire, turning black or gray. Two large mammal genera, Cervidae and Bovidae, were identified based on diagnostic teeth. Most bones were covered in calcareous concretion, but parallel and superimposed cutting marks were observed on the surface of four bone fragments. Two bone samples collected from Layer 5 and one from Layer 3 were dated by Accelerator Mass Spectrometry (AMS) at Peking University with radiocarbon dates ca. 11.5~10.7 kaBP cal, just at the beginning of the Holocene when it warmed rapidly.
The Fengjiapo site is a newly found open air site along the Middle Yellow River during the Palaeo-Neolithc transitional stage. The high amount of debitage, expedient tools, used pieces, and less well-retouched tools indicate it was a temporary camp for tool making, animal cooking, and grinding activities. The clear depositional sequence and dates make the site comparable to those along the Middle Yellow River, and ongoing environmental analysis will help expand our knowledge of human activities from the Palaeolithic to Neolithic.

Key words: Yellow River, Fengjiapo, Paleolithic, Microlithic, Paleo-Neolithc

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