Expansion of Dust Provenance and Aridification of Asia Since similar to 7.2 Ma Revealed by Detrital Zircon U-Pb Dating
文献类型：期刊论文
| 作者 | Zhang, Hanzhi1,2; Lu, Huayu1,2; Stevens, Thomas3; Feng, Han1; Fu, Yu1,4; Geng, Junyan1,4; Wang, Hanlin1 |
| 刊名 | GEOPHYSICAL RESEARCH LETTERS
 |
| 出版日期 | 2018-12-28 |
| 卷号 | 45期号:24页码:13437-13448 |
| ISSN号 | 0094-8276 |
| DOI | 10.1029/2018GL079888 |
| 英文摘要 | The relative importance of global cooling and Tibetan Plateau uplift in driving the aridification of Asia during the late Cenozoic is debated, largely due to the lack of appropriate proxy indicators. Here we address this problem by investigating changes in the source of Chinese loess and Red Clay, which is directly controlled by changes in the extent and distribution of the arid zone of Asia and the intensity of the East Asian winter monsoon, using zircon U-Pb dating of 27 levels in a near-continuous eolian sedimentary sequence in southern Chinese Loess Plateau. The results show that source regions expanded stepwise at similar to 7.2, similar to 2.6, 1.2-0.9Ma, and at the Last Glacial Maximum. These changes were synchronous with global cooling and ice cover expansion in the Northern Hemisphere, suggesting that the drivers of aridification of the Asian interior were intimately related to global cooling in the late Cenozoic. Plain Language Summary The arid and semiarid regions of Central Asia are one of the most important dust sources on Earth. Dust emitted from these regions is deposited in the Chinese Loess Plateau, the North Pacific Ocean, and even in Greenland, with broad environmental impacts. Although there is evidence that the drying of the Asian interior occurred gradually over several tens of million years, the driving factor remains unclear. Here we investigate the evolution of the sediment sources of the Chinese Loess Plateau and find that the changes in the source regions of wind-blown sediment were synchronous with global cooling since similar to 7.2 Ma. This indicates that the long-term aridification of the Asian interior was most likely driven by global cooling. |
| WOS关键词 | CHINESE LOESS PLATEAU ; LA-ICP-MS ; RED CLAY DEPOSITS ; NORTHERN TIBETAN PLATEAU ; PORPHYRY MO DEPOSIT ; GRAIN-SIZE ; QILIAN MOUNTAINS ; TRACE-ELEMENT ; TIANSHUI AREA ; PHASED UPLIFT |
| 资助项目 | National Natural Science Foundation of China[41690111] ; National Key Research and Development Program of China[2016YFA0600503] ; National Key Research and Development Program of China[2016YFE0109500] ; Fundamental Research Funds for the Central Universities |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000456404600029 |
| 出版者 | AMER GEOPHYSICAL UNION |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/90205]  |
| 专题 | 地质与地球物理研究所_其他部门 |
| 通讯作者 | Lu, Huayu |
| 作者单位 | 1.Nanjing Univ, Sch Geog & Ocean Sci, Nanjing, Jiangsu, Peoples R China 2.Jiangsu Collaborat Innovat Ctr Climate Change, Nanjing, Jiangsu, Peoples R China 3.Uppsala Univ, Dept Earth Sci, Uppsala, Sweden 4.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Hanzhi,Lu, Huayu,Stevens, Thomas,et al. Expansion of Dust Provenance and Aridification of Asia Since similar to 7.2 Ma Revealed by Detrital Zircon U-Pb Dating[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(24):13437-13448. |
| APA | Zhang, Hanzhi.,Lu, Huayu.,Stevens, Thomas.,Feng, Han.,Fu, Yu.,...&Wang, Hanlin.(2018).Expansion of Dust Provenance and Aridification of Asia Since similar to 7.2 Ma Revealed by Detrital Zircon U-Pb Dating.GEOPHYSICAL RESEARCH LETTERS,45(24),13437-13448. |
| MLA | Zhang, Hanzhi,et al."Expansion of Dust Provenance and Aridification of Asia Since similar to 7.2 Ma Revealed by Detrital Zircon U-Pb Dating".GEOPHYSICAL RESEARCH LETTERS 45.24(2018):13437-13448. |
入库方式： OAI收割
来源：地质与地球物理研究所
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