A 14.7 Ka record of earth surface processes from the arid‐monsoon transitional zone of China |
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| Authors: | Selvaraj Kandasamy Shengqian Chen Chengling Xie Qiaomei Chen Baozhi Lin Kaifeng Yu Qinghai Xu Victor M Velasco Fahu Chen |
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| Affiliation: | 1. State Key Laboratory of Marine Environmental Science and Department of Geological Oceanography, Xiamen University, Xiamen, P. R. China;2. Key Laboratory of Western China's Environmental Systems (Ministry of Education), Lanzhou University, Lanzhou, P. R. China;3. Department of Geography, RWTH Aachen University, Aachen, Germany;4. Institute of Nihewan Archaeology Research, College of Resources and Environment, Hebei Normal University, Shijiazhuang, P. R. China;5. Instituto de Geofísica, Universidad Nacional Autónoma de México, Ciudad Universitaria, México, Mexico |
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| Abstract: | The stability of Earth's critical zone is intimately linked with erosion, weathering and vegetation type and density. Therefore, it affects global biogeochemical processes which in turn affect the global climate by absorbing and reflecting solar radiation, and by altering fluxes of heat, water vapour, carbon dioxide and other trace gases through various feedback mechanisms. However, there is a lack of knowledge about how Earth's critical zone processes have changed over time and their link with past monsoon variability, especially in Asia. The study of lake sediments, which contain a suite of inorganic elemental and isotopic proxies, may facilitate the understanding of the Earth's critical zone processes on millennial timescales. Here we reconstruct the history of erosion–weathering–vegetation interactions since ~14.7 ka using geochemical records from a radiocarbon‐dated sediment core from Lake Gonghai in the monsoon‐arid transitional zone of north China. Detrital (Al, Ti, K, Rb) and authigenic (Ca, Sr) elemental records reveal distinct, millennial‐scale, late deglacial‐Holocene erosion and weathering patterns and transitions with the former (latter) elements showing higher (lower) values in warm intervals and vice versa. Chemical Index of Alteration (CIA) molar, a humidity proxy, suggests low humidity during the late deglacial ~11.5–14.7 ka, high humidity during the early‐mid Holocene ~11.5–3.2 ka, and intermediate humidity during the late Holocene interval since ~3.2 ka. The results of cross‐spectral analysis and comparison of our records with other climate reconstructions also suggest a pattern of orbitally‐phased humidity changes in north China. Overall, our results provide evidence for the solar‐forcing of Earth's surface processes in mid‐latitude China under natural climatic conditions. Copyright © 2017 John Wiley & Sons, Ltd. |
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| Keywords: | Earth's critical zone Earth's surface processes arid‐monsoon transitional China Holocene last deglaciation |
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