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    中国百强科技报刊

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    Volume 50 Issue 5
    May  2025
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    Article Navigation >  Earth Science  > 2025  >  50(5): 2055-2071
    Wang Sikai, Zhang Yuzhu, Wang Ninglian, Huang Chunchang, Zhu Yan, Huang Xiaoling, Jin Yao, Cao Pengpeng, Xiao Qili, Chen Dou, 2025. Relationship between the Transition of Longshan Culture-Erlitou Culture and the Hydro-Climate in the Luoyang Basin. Earth Science, 50(5): 2055-2071. doi: 10.3799/dqkx.2023.155
    Citation: Wang Sikai, Zhang Yuzhu, Wang Ninglian, Huang Chunchang, Zhu Yan, Huang Xiaoling, Jin Yao, Cao Pengpeng, Xiao Qili, Chen Dou, 2025. Relationship between the Transition of Longshan Culture-Erlitou Culture and the Hydro-Climate in the Luoyang Basin. Earth Science, 50(5): 2055-2071. doi: 10.3799/dqkx.2023.155
    shu

    Relationship between the Transition of Longshan Culture-Erlitou Culture and the Hydro-Climate in the Luoyang Basin

    doi: 10.3799/dqkx.2023.155
    • 1.

      Shaanxi Key Laboratory of Earth Surface System and Environmental Carrying Capacity, College of Urban and Environmental Sciences, Northwest University, Xi'an 710127, China

    • 2.

      School of Geography and Tourism, Shaanxi Normal University, Xi'an 710062, China

    • Received Date: 2023-05-19
      Available Online: 2025-06-06
    • Publish Date: 2025-05-25
      Abstract
    • In order to understand the relationship between the transformation of Longshan culture to Erlitou culture in the Luoyang basin and the hydrological climate, in this paper it collects and analyzes the location and scale information of the settlements (quantity, grade and the largest settlement area) in the two cultural periods, the Holocene paleoclimate records and the paleoflood events at ca. 4 000 a BP. The results show follows. (1) During the Longshan Culture period (4 900-4 000 a BP), the scale of settlements grew, which may be closely related to the stable and suitable climate in the late Middle Holocene. In the turning stage of Longshan Culture to Erlitou Culture (4 000-3 750 a BP), the 4 200 a BP climatic event triggered extreme floods in the basin, which destroyed many settlements and prompted residents to move to the surrounding highlands or other places. (2) During the Erlitou Culture period (3 750-3 500 a BP), the extreme floods did not occur again, the superior geographical location and geomorphic conditions in the basin provided a broad space for large-scale agricultural production and settlement construction. The results are of great significance for exploring the relationship between the evolution of Longshan Culture-Erlitou Culture in Luoyang basin and the hydrological climate.

       

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