自然杂志 ›› 2016, Vol. 38 ›› Issue (4): 248-252.doi: 10.3969/j.issn.0253-9608.2016.04.003

• 专题综述 • 上一篇    下一篇

黄河流域新石器文化的空间扩张及其影响因素

董广辉,刘峰文,杨谊时,王琳,陈发虎   

  1. ①兰州大学资源环境学院西部环境教育部重点实验室,兰州 730000;②华侨大学建筑学院,福建 厦门 361021
  • 收稿日期:2016-06-12 出版日期:2016-08-25 发布日期:2016-09-05
  • 作者简介:陈发虎:中国科学院院士,研究方向:气候环境变化、环境考古和干旱区地理研究
  • 基金资助:

    国家自然科学基金(41271218、41401224)和兰州大学中央高校基本科研业务费专项资金(lzujbky-2015-k09)资助

Cultural expansion and its influencing factors during Neolithic period in the Yellow River valley, northern China

DONG Guanghui, LIU Fengwen, YANG Yishi, WANG Lin, CHEN Fahu   

  1. ①Key Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China; ②School of Architecture, Huaqiao University, Xiamen 361021, Fujian Province, China
  • Received:2016-06-12 Online:2016-08-25 Published:2016-09-05

摘要:

黄河流域的新石器文化的发展为中华文明起源奠定了重要的基础。考古资料显示黄河流域新石器文化的发展主要经历了三个阶段:前仰韶时期(9 000~7 000 BP,BP表示距今年代,这里指距1950年)遗址数量少且分散;仰韶时期(7 000~5 000 BP)遗址数量显著增加,分布范围扩张至黄河及支流谷地;龙山时期(5 000~4 000 BP)遗址分布空间进一步扩张至丘陵地带。对比古气候和农业考古研究进展,显示黄河流域新石器时代粟黍农业的发展是推动文化扩张的主要动力,气候变
化则在此过程中起到了促进作用。

关键词: 中国北方, 新石器时代, 粟黍农业, 狩猎采集, 气候变化

Abstract:

The development of Neolithic cultures in the Yellow River valley promoted the emergence of Chinese ancient civilization. Three phases of the temporal-spatial variation of Neolithic culture evolution can be decerned based on archaeological survey, the distribution range of Neolithic sites was mainly limited to foothills during the pre-Yangshao period (9 000~7 000 BP), which widely expanded to the valleys of the Yellow River and its tributaries during the Yangshao period (7 000~5 000 BP), and further extended to hilly areas during the Longshan period (5 000~4 000 BP). With the comparison to the results of palaeoclimate and archaeometry studies, we argue that the spatial expansion of Neolithic cultures was primarily facilitated by the development of millet-based agriculture in the Yellow River valley, which was further affected by the climate changes.