Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing
文献类型：期刊论文
| 作者 | An, ZS; Wang, SM; Wu, XH; Chen, MY; Sun, DH; Liu, XM; Wang, FB; Li, L; Sun, YB; Zhou, WJ |
| 刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
 |
| 出版日期 | 1999-06-01 |
| 卷号 | 42期号:3页码:258-271 |
| 关键词 | Late Cenozoic eolian deposits of Loess Plateau Great Glaciation in the Northern Hemisphere East Asian monsoon evolution Qinghai-Xizang Plateau uplift |
| ISSN号 | 1006-9313 |
| 通讯作者 | An, ZS() |
| 英文摘要 | On the basis of a newly-constructed record of magnetic susceptibility (SUS) and the depositional rate change of eolian loess-red clay sequences in the last 7.2 Ma BP from the Loess Plateau, together with a comparison of a record of delta(18)O values from the equatorial East Pacific Ocean and eolian Quartz nux variations from the North Pacific Ocean, the evolutionary process of the Late Cenozoic Great Glaciation in the Northern Hemisphere can be divided into three stages: the arrival stage around 7.2-3.4 Ma BP, the initial stage at shout 3.4-2.6 Ma BP, and the Great Ice Age since 2.6 Ma BP. The evolution of the East Asian monsoon is characterized by paired winter and summer monsoons, and it is basically composed of the initial stage of weak winter and summer monsoons, the transitional stage of simultaneous increase in intensity of winter and summer monsoons, and the prevailing stage of strong winter and weak summer monsoons, or weak winter and strong summer monsoons. The Late Cenozoic global tectonic uplift, particularly the Qinghai-Xizang Plateau uplift and the associated CO2 concentration variation, controls the cooling processes of the onset of Great Glaciation and the long-term changes of East Asian monsoom climate in the Northern Hemisphere to a large extent. The accelerating uplift of the Qinghai-Xizang Plateau between 3.4 and 2.6 Ma BP provided an important driving force to global climiatic change. |
| 收录类别 | SCI |
| WOS关键词 | SOUTHERN ASIA ; AMERICAN WEST ; EVOLUTION ; CLIMATE ; BASIN ; HIMALAYA ; HISTORY |
| WOS研究方向 | Geology |
| WOS类目 | Geosciences, Multidisciplinary |
| 语种 | 英语 |
| WOS记录号 | WOS:000081744900005 |
| 出版者 | SCIENCE PRESS |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2556641 |
| 专题 | 寒区旱区环境与工程研究所 |
| 通讯作者 | An, ZS |
| 作者单位 | 1.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Xian 710054, Peoples R China 2.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China 3.Chinese Acad Sci, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China 4.Macquarie Univ, Sydney, NSW 2109, Australia 5.Nanjing Univ, Dept Geog, Nanjing 210008, Peoples R China 6.Chinese Acad Sci, Lanzhou Inst Plateau Atmospher Phys, Lanzhou 730000, Peoples R China 7.NW Univ Xian, Dept Geol, Xian 710069, Peoples R China 8.Chinese Acad Sci, Lanzhou Inst Desert, Lanzhou 730000, Peoples R China |
| 推荐引用方式 GB/T 7714 | An, ZS,Wang, SM,Wu, XH,et al. Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,1999,42(3):258-271. |
| APA | An, ZS.,Wang, SM.,Wu, XH.,Chen, MY.,Sun, DH.,...&Qiang, XK.(1999).Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,42(3),258-271. |
| MLA | An, ZS,et al."Eolian evidence from the Chinese Loess Plateau: the onset of the Late Cenozoic Great Glaciation in the Northern Hemisphere and Qinghai-Xizang Plateau uplift forcing".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 42.3(1999):258-271. |
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来源：寒区旱区环境与工程研究所
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