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This book contains 25 papers in English and 2 papers in Chinese.

The papers in English are as follows:
● The History and Variability of the East Asian Paleomonsoon Climate
● Asynchronous Holocene Optimum of the East Asian Monsoon
● Evolution of Asian Monsoons and Phased Uplift of the Himalaya-Tibetan Plateau since Late Miocene Times
● A Preliminary Seasonal Precipitation Reconstruction from Tree-ring Stable Carbon Isotopes at Mt. Helan, China, since    AD 1804
● Sensitivity of East Asian Monsoon Climate to the Uplift of the Tibetan Plateau
● Characterization of the Chinese Loess-Paleosol Stratigraphy by Whiteness Measurement
● High Resolution Hematite/Goethite Records from Chinese Loess Sequences for the Last Glacial-Interglacial Cycle: Rapid    Climatic Response of the East Asian Monsoon to the Tropical Pacific
● Be-Susceptibility Model and Quantitative Estimates of Pedogenic Ferromagnetic Material Flux in Chinese Loess
● Holocene Climate Changes over the Desert/Loess Transition of North-Central China
● Twentieth Century Increase of Atmospheric Ammonia Recorded in Mount Qomolangma Ice Core
● The Ion Chemistry of Lakes and Late and Late Holocene Desiccation in the Badain Jaran Desert, Inner Mongolia, China
● Coeval Changes in Grain Size and Sedimentation Rate of Eolian Loess, the Chinese Loess Plateau
● Color Reflectance of Chinese Loess and Its Implications for Climate Gradient Changes during the Last Two Glacial-    Interglacial Cycles
● Cyclic Rapid Warming on Centennial-Scale Revealed by a 2650-Year Stalagmite Record of Warm Season Temperature
● Climate as the Dominant Control on C3 and C4 Plant Abundance in the Loess Plateau: Organic Carbon Isotope Evidence    from the Last Glacial-Interglacal Loess-Soil Sequences
● Sources Regions and Formation of the Loess Sediments on the High Mountain Regions of Northwestern China
● Environmental and Climatic Change as Recorded in Geological Sediments from the Arid to Semi-Arid Zone of China
● Environmental Variability within the Chinese Desert-Loess Transition Zone over the Last 20000 Years
● Terrestrial Evidence for a Spatial structure of Tropical-polar Interconnections during the Younger Dry as Episode
● The Vegetation Characteristics of the ‘Yuan’ area at Yaoxian on the Loess Plateau in China over the Last 12000    Years
● Late Quaternary Evolution and Paleoclimated Western Alashan Plateau, Inner Mongolia, China
● Stable Isotope Records of Plant Cover Change and Monsoon Variation in the Past 2200 Years: Evidence from Laminated    Stalagmites in Beijing, China

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