人类学学报 ›› 2020, Vol. 39 ›› Issue (03): 392-403.doi: 10.16359/j.cnki.cn11-1963/q.2018.0038cstr: 32091.14.j.cnki.cn11-1963/q.2018.0038

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日本北海道地区细石叶技术研究概述

岳健平1,2,3,4(), 王晗5, 加藤真二6   

  1. 1.中国科学院脊椎动物演化与人类起源重点实验室,中国科学院古脊椎动物与古人类研究所,北京 100044
    2.中国科学院生物演化与环境卓越创新中心,北京 100044
    3.中国科学院大学,北京 100049
    4.中国科学院资源地层学与古地理学重点实验室,中国科学院南京地质古生物研究所,南京 10008
    5.东北大学文学研究科考古学研究室,仙台 9808576
    6.奈良文化财研究所,奈良 6308577
  • 收稿日期:2018-03-14 修回日期:2018-06-14 出版日期:2020-08-15 发布日期:2020-08-31
  • 作者简介:岳健平(1992-),男,湖南人,博士研究生,主要从事旧石器时代考古学研究。Email: yuejianpingivpp@163.com
  • 基金资助:
    中国科学院战略性先导科技专项B类(XDB26000000);国家自然科学基金项目(41672024);中国科学院资源地层学与古地理学重点实验室开放课题(2017KF04)

An overview of studies on microblade technology in Hokkaido, Japan

YUE Jianping1,2,3,4(), WANG Han5, KATO Shinji6   

  1. 1. Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044
    2. CAS Center for Excellence in Life and Paleoenvironment, Beijing 100044
    3. University of Chinese Academy of Sciences, Beijing 100049
    4. Key Laboratory of Economic Stratigraphy and Palaeogeography, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008
    5. Department of Archaeology of Graduate School of Arts and Letters, Tohoku University, Sendai 9808576
    6. Nara National Research Institute for Cultural Properties, Nara 6308577
  • Received:2018-03-14 Revised:2018-06-14 Online:2020-08-15 Published:2020-08-31

摘要:

细石叶技术是晚更新世晚期东北亚和西北美新的变革性剥坯技术和适应手段。北海道地区拥有丰富、多样的细石器遗存,相关材料最早可以追溯到距今约2.5万年前,持续了约1.2万年。以北海道具有明显技术复杂性和多样性特点的细石器为材料,学者们基于技术式“阅读”和拼合研究划分出一系列细石核工艺类型和剥坯技法;岛内以楔形细石核为代表的细石器工业传统在不断延续的同时,也表现出明显的阶段性变化,并在一定程度上显示出与气候环境变化较强的相关性。本文对北海道地区晚更新世末次盛冰期以来的气候、环境背景以及细石器的发现与研究历程进行介绍。在此基础上,厘清北海道细石核工艺类型的划分,并对细石器群的阶段性演变进行系统梳理,以期对我国相关研究有所裨益。

关键词: 细石叶技术, 北海道, 旧石器时代晚期, 剥坯技法

Abstract:

Microblade technology represents an important technological innovation and adaptation in northeastern Asia and northwestern America during the Late Pleistocene. Hokkaido, located along the edge of far-eastern Eurasia, contains a rich microlithic sequence that began around 25 thousand years ago and lasted for about 12 thousand years. Based on qualitative technological analysis and refitting, several microlithic debitage methods and microblade core types have been identified in Hokkaido. The regional microlithic sequence is characterized by the continuity of wedge-shaped cores, along with periodic changes that appear to correspond with climatic and environmental shifts. This article provides an overview of the climatic and environmental background of Hokkaido during the Late Pleistocene, and the research history of microlithic technology in the region. On this basis, this paper highlights the nature and differences among microblade debitage methods in Hokkaido and clarifies the development of microlithic industry through time. This overview has implication for our understanding of microlithic technology and Late Pleistocene hunter-gatherer mobility and adaptation in the broader region of far-eastern Asia, including the neighboring area of China.

Key words: Microblade technology, Hokkaido, Upper Paleolithic, Debitage method

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