The Different Climatic Response of Pedogenic Hematite and Ferrimagnetic Minerals: Evidence from Particle-Sized Modern Soils over the Chinese Loess Plateau
Xinbo Gao1,2, Qingzhen Hao1,2, Wang Luo1,2, Frank Oldfield3, Jan Bloemendal3, Chenglong Deng2,4, Yang Song5, Junyi Ge2,6, Haibin Wu2,7, Bing Xu1,2, Fengjiang Li1,2, Long Han1,2, Yu Fu1,2 and Zhengtang Guo2,7, (1)Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China, (2)University of Chinese Academy of Sciences, Beijing, China, (3)School of Environmental Sciences, University of Liverpool, Liverpool, United Kingdom, (4)State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, beijing, China, (5)State Key Laboratory of Urban and Regional Ecology, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing, China, (6)Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijng, China, (7)Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China
