| 肖阳，李凤全*，王天阳，朱丽东，叶玮.长江下游新石器时代遗址的空间分布特征[J].海南师范大学学报自科版,2018,31(3):338-345 |
| 长江下游新石器时代遗址的空间分布特征 |
| The Spatial Distribution Characteristics of the Neolithic Sites in the Lower Reaches of Yangtze River |
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| DOI：10.12051/j.issn.1674-4942.2018.03.014 |
| 中文关键词: 长江下游 新石器时代遗址 空间自相关 空间分布 |
| 英文关键词: Yangtze River neolithic sites spatial autocorrelation spatial distribution |
| 基金项目:国家自然科学基金项目(41572345）；浙江省自然科学基金项目（LY16D010001） |
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| 中文摘要: |
| 基于泰森多边形、空间自相关及核密度估计等方法，研究了长江下游新石器时代遗址
的空间分布规律及特征。结果表明：（1）不同文化遗址均呈现出聚集分布特征，但存在单核与多核
的差异。马家浜文化遗址主要集聚在太湖的东、西部，以草鞋山、骆驼墩遗址群最为密集；崧泽文化
遗址集聚于太湖东、东北部，以草鞋山遗址群最为密集；良渚文化遗址主要集聚在太湖南部、东部，
以余杭—良渚遗址群最为密集；马桥文化遗址主要集聚在太湖东部和西南部，以上海西部的马桥、
湖州—长兴、海宁—海盐一带的遗址群最为集中。马家浜至崧泽时期遗址呈多核心特征，崧泽至良
渚时期遗址由多核变为单核，马桥时期遗址聚集区重现多核心特征。（2）随着气候、地貌、社会结
构的演变，遗址密集区的分布趋势、连续性及密度相应变化。遗址密集区分布呈现出由太湖东、西
部先向太湖东、南部，再向太湖南部，最后向太湖东、西南部发展的趋势。遗址聚集区的连续性和密
度在马家浜、崧泽、良渚时期逐渐增强，而马桥时期遗址密集区的连续性和密度较良渚时期有所下
降。研究结果对研究人地关系具有一定的参考借鉴意义。 |
| 英文摘要: |
| Based on the methods of thiessen polygons, spatial autocorrelation and nuclear density estimation, the spatial
distribution and characteristics of Neolithic sites in the lower reaches of the Yangtze River was studied. The results showed
that: (1) all different cultural sites showed agglomeration distribution characteristics, but there were differences between sin⁃
gle - core and multi - core. Majiabang cultural sites were mainly distributed in the east and west of Taihu Lake. The Caoxie
mountain and Luotuodun sites were the most densely. Songze cultural sites were clustered in the east and northeastern parts
of Taihu Lake, with the most densest sites of Qingpu - Songze and Caoxie mountain. Liangzhu cultural sites were mainly clus⁃
tered in the southern and east of Tai Lake, and the Yuhang - Liangzhu sites were most densest. Maqiao cultural sites were
mainly concentrated in the east and southwest of Taihu Lake, the sites in the west of Shanghai, Huzhou - Changxing, Hain⁃
ing - Haiyan are the most concentrated. During the period from Majiabang to Songze, the sites were characterized by multiple
cores. The sites changed from the multi - nucleus to the single - nucleus during the Songze to Liangzhu period. The sites of the
Maqiao period reappeared multi - core features. (2) With the evolution of climate, geomorphology and social structure, the dis⁃
tribution of sites concentrated areas, continuity and density also showed the evolution. The distribution of the sites showed
the trend from the east and west to the east and south of Taihu Lake, then to the south of Taihu Lake, and finally to the east
and southwest of Taihu Lake. The continuity and density of the site gradually increased from the periods of Majiabang, Songze and Liangzhu. However, the continuity and density of the sites in concentrated areas during the Maqiao period have de⁃
clined compared with the Liangzhu period. This paper is of certain reference significance to the study of human - land rela⁃
tions. |
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