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安徽宣城第四纪红土剖面的全氧化铁含量及其古环境意义
引用本文:李小平,夏应菲.安徽宣城第四纪红土剖面的全氧化铁含量及其古环境意义[J].地质学刊,1998,22(3):182-185.
作者姓名:李小平  夏应菲
作者单位:中国科学院南京土壤研究所土壤圈物质循环开放实验室,南京师范大学地理科学学院
摘    要:对宣城第四纪红土剖面的研究表明,全氧化铁含量能够较好地指示中国南方第四纪气候的波动。与北方黄土古土壤序列相比,宣城剖面的全氧化铁明显较高,指示了南方地区更强的风化成壤作用。

关 键 词:全氧化铁  第四纪  红土化  安徽宣城

Total Iron Content of Quaternary Laterite Profile and Its Paleoenvironmental Significance in Xuancheng of Anhui Province
Li Xiaoping Xia Yingfei Yang Hao Institute of Soil Science,Academia Sinic,Nanjing,.Total Iron Content of Quaternary Laterite Profile and Its Paleoenvironmental Significance in Xuancheng of Anhui Province[J].Jiangsu Geology,1998,22(3):182-185.
Authors:Li Xiaoping Xia Yingfei Yang Hao Institute of Soil Science  Academia Sinic  Nanjing  
Institution:Li Xiaoping 1 Xia Yingfei 2 Yang Hao 1 1 Institute of Soil Science,Academia Sinica,Nanjing,210008 2 Department of Geography,Nanjing Normal University,Nanjing,210097
Abstract:As a large environmental section in the Eastern Hemisphere, PEPII covers the laterization areas in the Southern part of the Country. It studies mainly different paleoclimatic records, specially continental records in the section. Various laterite successions are an important carrier of continental paleoenvironmental records in China. The study of Quaternary laterization profile in Xuancheng, Anhui Province shows that the paleoclimatic fluctuation in South China during Quaternary can be clearly described by the total iron oxide. Compared with the succession of loesspaleosol series in North China, the content of total iron oxide of Xuancheng profile is much higher. It refers that the sediments from Southern area of China have undergone a stronger weathering since it deposited. Furthermore, the curve of total iron oxide in Xuancheng profile coincides with the oxygen isotope of V28 238 core.
Keywords:Total  iron  oxide  Quaternary  Laterization  Xuancheng    Anhui
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