Geochemical Environment Evolution of Human Cultural Sites in North China
Received date: 2012-07-24
Revised date: 2012-08-28
Online published: 2012-10-10
In the evolutionary history of the Earth, Quaternary is the times of human birth, development and expansion and its formation geological products has recorded the rich environment information. Weathering index CIA, Fe2O3/FeO, Fe/Mn, etc., chemical parameters of Hebei Province Quaternary lithostratigraphics (Nihewan group, Chicheng group, Malan group, Qian’an group), may serve as the average annual temperature, annual rainfall and other climatic factors similar proxy. In the stream sediments of the location of the human cultural heritage sites in North China, mercury, tin, gold and other metal concentrations reach the higher stage with the evolution of human civilization. The results show that in order to adapt to changing natural geography environment (cold, drought) human being have to make technological innovation, resulting in the advances in the civilization as farming, industrial revolution and modern information industry. But at the same time, geological environment has also led to manmade pollution, maybe even to global warming.
Key words： Cultural ecology model; Environmental change; Geochemistry; Human sites; North China
Gong Jinzhong . Geochemical Environment Evolution of Human Cultural Sites in North China[J]. Advances in Earth Science, 2012 , 27(10) : 1153 -1160 . DOI: 10.11867/j.issn.1001-8166.2012.10.1153
[1]Zhou Mulin, Liu Yourui, Chen Ming, et al. The Quaternary System of China[M]. Beijing:Geological Publishing House, 1988：64-85.[周慕林，刘佑睿，陈明,等.中国的第四系[M].北京：地质出版社，1988：64-85.]
[2]Zhang Lansheng.Research of Environment Evolution[M].Beijing:Science Press，1992:5-9.[张兰生.环境演变研究[M].北京：科学出版社，1992:5-9.]
[3]Gu Zhaoyan, Han Jiamao, Liu Dongsheng. Quaternary loess geochemistry studies progress[J].Quaternary Research，2000，20(1):42.[顾兆炎，韩家懋，刘东生.中国第四纪黄土地球化学研究进展[J].第四纪研究，2000,20(1):42.]
[4]Zhao Zhenhua. Geochemistry Principle of Trace Element[M]. Beijing:Science Press，1997:158-159,178,191.[赵振华.微量元素地球化学原理[M].北京：科学出版社，1997:158-159，178，191.]
[5]Bureau of Geology Mineral Resoures of Hebei Province.Regional Geology of Hebei Province,Beijing Mumicipality and Tianjin Mumicipality[M].Beijing:Geological Publishing House,1989:276-299.[河北省地质矿产局.河北省北京市天津市区域地质志[M].北京：地质出版社，1989:276-299.]
[6]Wendy Ashmore, Robert J.Sharer. Discovering Our Past: A Brief Introduction to Archaeology[M]. McGraw-Hill Companies Inc.,2006:127,182-192.[温迪·安西莫，罗伯特·夏尔著，沈梦蝶译.发现我们的过去——简明考古学导论[M].上海:上海社会科学院出版社，2007:127,182-192.]
[7]Wang Zhikun, Ning Fuzheng,Fu Qiaoling,et al.An evaluation of status of soil heavy metal pollution in Luoyang City propre[J].Geophysical and Geochemical Exploration, 2008，32(4):415.[王志坤，宁富政，付巧玲,等.洛阳城区土壤重金属污染现状评价[J].物探与化探，2008，32(4):415.]
[8]Gong Jinzhong, Li Guangping. Geochemical environmental characteristics of China’s seven ancient capitals[J]. Geology in China, 2009,36(5):1 160-1 161.[宫进忠，李广平.中国七大古都的地球化学环境特征[J].中国地质，2009,36(5):1 160-1 161.]
[9]Zhao Shiyu, Zhou Shangyi. Introdution of Chinese Cultural geography[M].Taiyuan: Shanxi Education Publishing House,1991:65-66.[赵世瑜，周尚意.中国文化地理概说[M].太原：山西教育出版社，1991:65-66.]
[10]Zhibin Zhang, Huidong Tian，Bernard Cazelles,et al. Periodic climate cooling enhanced natural disasters and wars in China during AD 10-1900[J]. Proceedings of the Royal Society, Series B: Biological Sciences,doi:10.1098/rspb.2010.0890.
/
| 〈 |
|
〉 |
甘公网安备62010202000687
