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鄱阳湖湿地水质空间分异及影响因素研究
作者: 吴燕平  来源:江西师范大学 年份:2016 文献类型 :学位论文
描述:鄱阳湖湿地水质空间分异及影响因素研究
鄱阳湖湿地水质空间分异及影响因素研究
作者: 吴燕平  来源:江西师范大学 年份:2016 文献类型 :学位论文
描述:鄱阳湖湿地水质空间分异及影响因素研究
鄱阳湖鲶鱼人工繁殖及苗种培育技术研究
作者: 姚毅  来源:南昌大学 年份:2016 文献类型 :学位论文
描述:鄱阳湖鲶鱼人工繁殖及苗种培育技术研究
人类活动对鄱阳湖流域侵蚀产沙与输沙的影响
作者: 熊梦雅  来源:江西师范大学 年份:2016 文献类型 :学位论文
描述:人类活动对鄱阳湖流域侵蚀产沙与输沙的影响
鄱阳湖流域主要河道入湖污染物通量研究
作者: 贾娟娟  来源:南昌大学 年份:2016 文献类型 :学位论文
描述:鄱阳湖流域主要河道入湖污染物通量研究
长江、赣江、鄱阳湖鲢遗传多样性和群体遗传结构分析
作者: 于悦  来源:华中农业大学 年份:2016 文献类型 :学位论文
描述:长江、赣江、鄱阳湖鲢遗传多样性和群体遗传结构分析
鄱阳湖典型洲滩湿地水分垂向运移过程研究
作者: 林欢  来源:中国科学院大学 年份:2016 文献类型 :学位论文
描述:鄱阳湖典型洲滩湿地水分垂向运移过程研究
鄱阳湖枯水期子湖泊营养级关系研究
作者: 张欢  来源:中国科学院大学 年份:2016 文献类型 :学位论文
描述:鄱阳湖枯水期子湖泊营养级关系研究
鄱阳湖星子站水位62变化规律分析
作者: 刘恋 曾繁翔 付志强  来源:人民长江 年份:2016 文献类型 :期刊
描述:鄱阳湖星子站水位62变化规律分析
鄱阳湖流域史前人类遗址时空分布及其环境响应
作者: 徐佳佳 贾玉连 马春梅 朱诚 吴立 李育远 王鑫浩  来源:地理学报(英文版) 年份:2016 文献类型 :期刊 关键词: expanded  northward  geographic  records  环境响应  鄱阳湖流域  climatic  ancient  Holocene  southeast 
描述:The temporal-spatial geographic distribution of archaeological sites and its feature between 10.0–2.8 ka BP(ka BP= thousands of years before 0 BP, where “0 BP” is defined as the year AD 1950) were determined, based on GIS spatial analysis in the Poyang Lake Basin. The relationship between geographic distribution of sites of different periods under subsistence existence of ancient civilizations, climate and environmental change was investigated. The results revealed numerous archaeological sites of the Neolithic Age(10.0–3.6 ka BP). The sites were mainly located in the northern part of the Poyang Lake Basin, a hilly and mountainous area with many river terraces suitable for the development of human civilization. The number of archaeological sites rapidly increased during the Shang and Zhou dynasties(3.6–2.8 ka BP) and spread widely on the floodplains of the middle and lower reaches of Ganjiang River and onto the west, south, and southeast beach areas of the Poyang Lake. Holocene records of climate change suggested that it was possible that climate fluctuations had a great impact on human evolution in the study area. Before 3.6 ka BP, westward and northward expansion of Neolithic cultures in the Poyang Lake watershed occurred under the background of climate amelioration(becoming warmer and wetter). The ancient people lived in the hilly areas with high elevation. The simple mode of a fishing and gathering economy was mostly suited to this area in the early Neolithic Age. The scope of human activities was expanded and cultural diversity developed in the late Neolithic Age. However, with population growth and increasing survival pressure in a dry-cold climatic stage after 3.6 ka BP, this simple living mode had to be abandoned, and various forms of economy, the majority being agriculture, were developed on flood plains of the lower reaches of numerous rivers around Poyang Lake. This promoted flourishing of the Bronze culture of South China.
全文:The temporal-spatial geographic distribution of archaeological sites and its feature between 10.0–2.8 ka BP(ka BP= thousands of years before 0 BP, where “0 BP” is defined as the year AD 1950) were determined, based on GIS spatial analysis in the Poyang Lake Basin. The relationship between geographic distribution of sites of different periods under subsistence existence of ancient civilizations, climate and environmental change was investigated. The results revealed numerous archaeological sites of the Neolithic Age(10.0–3.6 ka BP). The sites were mainly located in the northern part of the Poyang Lake Basin, a hilly and mountainous area with many river terraces suitable for the development of human civilization. The number of archaeological sites rapidly increased during the Shang and Zhou dynasties(3.6–2.8 ka BP) and spread widely on the floodplains of the middle and lower reaches of Ganjiang River and onto the west, south, and southeast beach areas of the Poyang Lake. Holocene records of climate change suggested that it was possible that climate fluctuations had a great impact on human evolution in the study area. Before 3.6 ka BP, westward and northward expansion of Neolithic cultures in the Poyang Lake watershed occurred under the background of climate amelioration(becoming warmer and wetter). The ancient people lived in the hilly areas with high elevation. The simple mode of a fishing and gathering economy was mostly suited to this area in the early Neolithic Age. The scope of human activities was expanded and cultural diversity developed in the late Neolithic Age. However, with population growth and increasing survival pressure in a dry-cold climatic stage after 3.6 ka BP, this simple living mode had to be abandoned, and various forms of economy, the majority being agriculture, were developed on flood plains of the lower reaches of numerous rivers around Poyang Lake. This promoted flourishing of the Bronze culture of South China.
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