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The Holocene loess-soil sequence on the Chinese Loess Plateau constitutes an excellent record of evolution of soil formation, monsoonal climate, eolian dust accumulation and influences of arable farming of over 8000 years. A high-resolution soil profile on the Zhouyuan loess tableland to the west of Xi'an was studied using particle-size analysis, measurement of magnetic susceptibility, total Fe, TOC...
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