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首页> 外文期刊>Quaternary International >Settlement distribution and its relationship with environmental changes from the Paleolithic to Shang-Zhou period in Liyang Plain, China
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Settlement distribution and its relationship with environmental changes from the Paleolithic to Shang-Zhou period in Liyang Plain, China

机译:Li阳平原旧石器时代至商州时期的聚落分布及其与环境变化的关系

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摘要

With increasing collaboration between archeology and natural sciences, research on past human-environment interactions has received more attention in recent years. This paper uses nineteen radiocarbon and OSL dates from three profiles to explore environmental evolution of the Liyang Plain, investigate the spatial and temporal distributions of archaeological sites from the Paleolithic Age to the Shang-Zhou period and discuss relationships between human cultures and environmental changes. The results show that Paleolithic sites are mainly distributed in surrounding mountainous and hilly areas, changing to the plain in the late Paleolithic Age. Climatic cooling during the Last Glacial Maximum did not cause severe damage to the regional vegetation and ecosystem, which allowed the continuous development of the late Paleolithic culture in the Liyang Plain. Suitable environmental conditions and progression of human activities facilitated rice cultivation in the early Holocene, and rice agriculture as an important food resource provided a solid material foundation for social development. The number of archaeological sites increased continuously and their distribution expanded considerably into eastern low-lying plain areas during the Neolithic Age. These trends reversed in the late Shijiahe culture, and social development did not recover until the Shang-Zhou period. Variation of site distribution in the Liyang Plain was primarily influenced by hydrological and geomorphological changes as well as climate change. However, it might also have been affected by broader regional political situations, especially during the Shang-Zhou period.
机译:随着考古学与自然科学之间日益紧密的合作,近年来对人类与环境相互作用的研究受到了越来越多的关注。本文利用三个剖面的19种放射性碳和OSL数据来探索the阳平原的环境演变,调查从旧石器时代到商周时期的考古遗址的时空分布,并讨论人类文化与环境变化之间的关系。结果表明,旧石器时代遗址主要分布在周围的山地和丘陵地区,在旧石器时代后期转变为平原。最后一次冰期末期的气候降温并未对区域植被和生态系统造成严重破坏,这使得the阳平原晚期旧石器时代文化得以持续发展。适宜的环境条件和人类活动的发展促进了全新世早期的水稻种植,水稻农业作为重要的粮食资源,为社会发展奠定了坚实的物质基础。在新石器时代,考古遗址的数量不断增加,分布范围大大扩展到东部低洼平原地区。这些趋势在晚期石家河文化中得到了扭转,直到商周时期社会发展才恢复。 the阳平原站点分布的变化主要受水文和地貌变化以及气候变化的影响。但是,它也可能受到更广泛的地区政治局势的影响,尤其是在商代时期。

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  • 来源
    《Quaternary International》 |2014年第13期|29-36|共8页
  • 作者单位

    Laboratory for Earth Surface Process, Ministry of Education, College of Urban and Environmental Sciences, Peking University, No. 5 Yiheyuan Road, Haidian District, Beijing 100871, China;

    Laboratory for Earth Surface Process, Ministry of Education, College of Urban and Environmental Sciences, Peking University, No. 5 Yiheyuan Road, Haidian District, Beijing 100871, China;

    College of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China;

    Laboratory for Earth Surface Process, Ministry of Education, College of Urban and Environmental Sciences, Peking University, No. 5 Yiheyuan Road, Haidian District, Beijing 100871, China;

    Hunan Provincial Institute of Cultural Relics and Archaeology, Changsha 410008, China;

    Geological Survey of Canada-Atlantic, P.O. Box 1006, Dartmouth, NS B2Y 4A2, Canada;

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