浙江田螺山遗址古盐度及其环境背景同河姆渡文化演化的关系
收稿日期: 2008-11-26
修回日期: 2009-03-25
网络出版日期: 2009-07-25
基金资助
国家科技支撑计划项目 (2006BAK21B02); 国家自然科学基金课题 (40671016); 国家重点基础发展研究计划 (2003CB415201); 北京大学考古研究中心课题
Paleosalinity in Tianluoshan Site and the Relation between Hemudu Culture and Its Environmental Background
Received date: 2008-11-26
Revised date: 2009-03-25
Online published: 2009-07-25
Supported by
National Science and Technology Supporting Project, No.2006BAK21B02; National Natural Science Foundation of China, No.40671016; National Key and Basic Development Research Project of China, No.2003CB415201; Program of Archeological Research Center of Peking University
李明霖1, 莫多闻1, 孙国平2, 周昆叔3, 毛龙江4 . 浙江田螺山遗址古盐度及其环境背景同河姆渡文化演化的关系[J]. 地理学报, 2009 , 64(7) : 807 -816 . DOI: 10.11821/xb200907005
Paleosalinity of Tianluoshan Site is reestablished by mensurations and analyses of clay mineral, boron, strontium, barium, after sampling in a profile of Tianluoshan Site. The relative sea level changes are discussed according to the lab results. It turns out that there are at least three time periods of relative sea-level highstand not only before but also during and after Hemudu Culture in Tianluoshan Site. Based on previous researches and through studying several environmental elements comprehensively, the characteristics of environmental background and their relationships between human activities and development of Hemudu Culture are systematically discussed.
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