中国黄土及其古气候意义
摘要
黄土高原是古气候环境的历史藏在自然界用密码写就的一本本"秘岌"之一。黄土高原的黄土——古土壤序列对研究古气候变化具有重要意义。通过黄土——古土壤的交替出现,来研究古气候的变化旋回。研究发现黄土的颜色、粒度等与古气候变化存在一定的关系。
引文
[1]刘东生.黄土与环境[J].西安交通大学学报(社会科学版),2002,22(4):1-6.
[2]何柳,孙有斌,安芷生.中国黄土颜色变化的控制因素和古气候意义[J].地球化学,2010,39(5):1-9.
[3]Ji Junfeng,Balsam W,Chen Jun.Mineralogic and climatic interpretations of the Luochuan Loess section(China)based on diffuse reflectance spectrophotometry[J]. Quatern Res,2001,56(1):23-30.
[4]季峻峰,陈骏,Balsam W,刘连文,陈,赵良,周玮.黄土剖面中赤铁矿和针铁矿的定量分析与气候干湿变化研究[J].第四纪研究,2007,27(2):221-229.
[5]高万一,林本海,孙东怀.黄土反射光谱研究与气候波动[M].刘东生,安芷生.黄土·第四纪地质·全球变化(第三集).北京:科学出版社,1992:92-100.
[6] Chen Jun,Ji Junfeng,Balsam W,Chen Yang,Liu Lianwen,An Zhisheng.Characterization of the Chinese loess-paleosol stratigraphy by whiteness measurement[J]. Palaeogeogr Palaeoclimatol Palaeoecol,2002,183(3/4):287-297.
[7]Yang Shi-ling,Ding Zhong-li.Color reflectance of Chinese loess and its implications for climate gradient changes during the last two glacial-interglacial cycles[J]. Geophys Res Lett,2003,30(20),2058,doi:10.1029/2003GL018346.
[8]Yang Shengli,Fang Xiaomin,Li Jijun,An Zhisheng,ChenShiyue,Fukusana H. Transformation functions of soil color and climate[J].Sci China(D),2001,44(suppl 1):218-226.
[9]Porter S C.High-resolution paleoclimatic information from Chinese eolian sediments based on grayscale intensity profiles[J].Quatern Res,2000,53(1):70-77.
[10]Fang Xiaomin,Ono Y,Fukusawa H,Pan Baotian,Li Jijun,Guan Donghong,Oi K,Tsukamoto S,Torii M,Mishima T.Asian summer monsoon instability during the past 60,000 years:Magnetic susceptibility and pedogenic evidence from the western Chinese Loess Plateau[J].Earth Planet Sci Lett,1999,168(3/4):219-232.
[11]陈,陈骏,季峻峰,刘连文,鹿化煜.陕西洛川黄土剖面的白度参数及其古气候意义[J].地质论评,2002,48(1):38-43.
[2]何柳,孙有斌,安芷生.中国黄土颜色变化的控制因素和古气候意义[J].地球化学,2010,39(5):1-9.
[3]Ji Junfeng,Balsam W,Chen Jun.Mineralogic and climatic interpretations of the Luochuan Loess section(China)based on diffuse reflectance spectrophotometry[J]. Quatern Res,2001,56(1):23-30.
[4]季峻峰,陈骏,Balsam W,刘连文,陈,赵良,周玮.黄土剖面中赤铁矿和针铁矿的定量分析与气候干湿变化研究[J].第四纪研究,2007,27(2):221-229.
[5]高万一,林本海,孙东怀.黄土反射光谱研究与气候波动[M].刘东生,安芷生.黄土·第四纪地质·全球变化(第三集).北京:科学出版社,1992:92-100.
[6] Chen Jun,Ji Junfeng,Balsam W,Chen Yang,Liu Lianwen,An Zhisheng.Characterization of the Chinese loess-paleosol stratigraphy by whiteness measurement[J]. Palaeogeogr Palaeoclimatol Palaeoecol,2002,183(3/4):287-297.
[7]Yang Shi-ling,Ding Zhong-li.Color reflectance of Chinese loess and its implications for climate gradient changes during the last two glacial-interglacial cycles[J]. Geophys Res Lett,2003,30(20),2058,doi:10.1029/2003GL018346.
[8]Yang Shengli,Fang Xiaomin,Li Jijun,An Zhisheng,ChenShiyue,Fukusana H. Transformation functions of soil color and climate[J].Sci China(D),2001,44(suppl 1):218-226.
[9]Porter S C.High-resolution paleoclimatic information from Chinese eolian sediments based on grayscale intensity profiles[J].Quatern Res,2000,53(1):70-77.
[10]Fang Xiaomin,Ono Y,Fukusawa H,Pan Baotian,Li Jijun,Guan Donghong,Oi K,Tsukamoto S,Torii M,Mishima T.Asian summer monsoon instability during the past 60,000 years:Magnetic susceptibility and pedogenic evidence from the western Chinese Loess Plateau[J].Earth Planet Sci Lett,1999,168(3/4):219-232.
[11]陈,陈骏,季峻峰,刘连文,鹿化煜.陕西洛川黄土剖面的白度参数及其古气候意义[J].地质论评,2002,48(1):38-43.