张海鹏,刘维明,赵慧敏,等. 四川省旧石器—青铜器时期遗址空间分布及其影响因素[J]. 海洋地质与第四纪地质,xxxx,x(x): x-xx. DOI: 10.16562/j.cnki.0256-1492.2024031802
引用本文: 张海鹏,刘维明,赵慧敏,等. 四川省旧石器—青铜器时期遗址空间分布及其影响因素[J]. 海洋地质与第四纪地质,xxxx,x(x): x-xx. DOI: 10.16562/j.cnki.0256-1492.2024031802
ZHANG Haipeng,LIU Weiming,ZHAO Huimin,et al. The Paleolithic-Bronze age sites in Sichuan Province: Distribution and influencing factors[J]. Marine Geology & Quaternary Geology,xxxx,x(x): x-xx. DOI: 10.16562/j.cnki.0256-1492.2024031802
Citation: ZHANG Haipeng,LIU Weiming,ZHAO Huimin,et al. The Paleolithic-Bronze age sites in Sichuan Province: Distribution and influencing factors[J]. Marine Geology & Quaternary Geology,xxxx,x(x): x-xx. DOI: 10.16562/j.cnki.0256-1492.2024031802

四川省旧石器—青铜器时期遗址空间分布及其影响因素

The Paleolithic-Bronze age sites in Sichuan Province: Distribution and influencing factors

  • 摘要: 史前遗址作为研究人类文明传承的重要依据,了解其时空分布及影响因素,有助于揭示古人类遗址点选址的规律和人地关系的演变特征。四川省地貌复杂,西部为山地,中部为平原,东部以丘陵为主,研究不同时期遗址的分布,更能揭示不同生业模式下古人类对环境的适应策略。本文利用GIS对收集整理的四川省旧石器至青铜器时期共计151处遗址数据进行空间分析,利用二元逻辑回归建立各时期遗址分布模型,研究了高程、坡度、水系、地貌与遗址分布之间的关系。结果发现:(1)四川省旧石器—青铜器时期遗址分布方向总体由EW向过渡到EN-WS向,核密度值随时间推移逐渐增大,证明遗址分布呈现集聚现象。从旧石器时期至青铜器时期,遗址分布逐渐由分散的多核心布局演化为以成都平原为中心的单核心布局。(2)利用二元逻辑回归建立各时期遗址分布模型,其中距水距离是影响四川省旧石器时期和新石器时期遗址点分布的主要因素,坡度是影响四川省青铜器时期遗址分布的最大诱因。(3)四川省旧石器—青铜器时期,古人类生业模式经历了3次大的变迁。生业模式的变化促使古人类对生存环境做出不同的适应策略。

     

    Abstract: Prehistoric sites are important basis for understanding the inheritance of human civilization, their spatial-temporal distribution, and influencing factors on the formation, thus to reveal the rules of site selection, the evolution of human-land interactions, and the adaptation strategies of remote ancestors under different modes of production. The geomorphology of Sichuan Province is complex: many mountain ranges in the west, vast plains in the central regions (e.g., Chengdu Plain), and hills in the east. GIS was used to analyze the data from 151 sites built during the Paleolithic to Bronze Age, from which the distribution model of the sites in each period was established by using binary logistic regression, and the relationships of elevation, slope, water system, and geomorphology versus the distribution of the sites were explored. Results show that the distribution of these sites shifted from in EW direction to in NE-SW direction, and the kernel density value gradually increased over time, which proves that the distribution of the sites shows the phenomenon of agglomeration. The site distribution gradually evolved from a scattered multi-centered pattern to a single-centered pattern such as shown in the Chengdu Plain. The distribution pattern of the sites in each ancient period was analyzed using binary logistic regression, and we found that the distance from water sources was the main factor on the site selection during the Paleolithic-Neolithic times, and the slope was the major causative factor on site selection during the Bronze Age. During the Paleolithic-Bronze Age, the life style of ancient people underwent three major changes. The changes in subsistence patterns prompted our ancestors to make different adaptive strategies to the living environment.

     

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