Rock magnetic record of late Neogene red clay sediments from the Chinese Loess Plateau and its implications for East Asian monsoon evolution | |
Song, Yougui1; Fang, Xiaomin2; Chen, Xiuling3; Torii, Masayuki4; Ishikawa, Naoto5; Zhang, Maosheng6; Yang, Shengli7; Chan, Hong1 | |
通讯作者 | Song, Yougui(ygsong@loess.llqg.ac.cn) |
2018-12-01 | |
发表期刊 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY |
ISSN | 0031-0182 |
卷号 | 510页码:109-123 |
摘要 | The Quaternary loess-paleosol and underlying Neogene red clay sequences on the Chinese Loess Plateau (CLP) contain a remarkable continental record of past East Asian monsoon changes and aridification of the Asian interior. While monsoon variability during the Quaternary is reasonably well understood, the evolution and dynamics of the monsoon during the Neogene are still debated. The rock magnetism of aeolian sediments is a well-established tool for reconstructing the palaeoclimatic history of Asia. Here, we present a rock magnetic record from Late Neogene red clay sediments of the Chaona section in the central CLP. The results indicate that the main magnetic minerals in the red clay are magnetite, maghemite, hematite and goethite, similar to the overlying Quaternary loess-palaeosol sequences. The high-resolution rock magnetic record, combined with the results of other proxies, demonstrate a stepwise intensification of the summer monsoon and a progressive enhancement of the winter monsoon in East Asia during the Late Neogene. Based on the results, the climatic evolution of East Asia can be divided into three intervals: Interval III, from 8.1 to 6.8 Ma, is characterized by a cool, dry climate with a relatively weak East Asian Summer Monsoon (EASM) and East Asian Winter Monsoon (EAWM); Interval II, from 6.8 to 4.3 Ma, is characterized by cool/warm cycles; and Interval I, from 4.3 to 2.8/2.6 Ma, was warm and humid, and within which the EASM strengthened rapidly and the EAWM fluctuated considerably, with an increasing trend. We infer that before 4.3 Ma the variations of both the EASM and EAWM were closely related to global cooling and that the intensified EASM during the late Pliocene was primarily caused by tectonic events, including the gradual closure of the Panama Seaway and the uplift of the Tibetan Plateau, rather than by global cooling. |
关键词 | Late Miocene Pliocene Global cooling Tectonic events Magnetic minerals |
DOI | 10.1016/j.palaeo.2017.09.025 |
关键词[WOS] | LATE CENOZOIC UPLIFT ; ANTARCTIC ICE-SHEET ; GRAIN-SIZE RECORDS ; LATE MIOCENE ; TIBETAN PLATEAU ; PALEOCLIMATIC SIGNIFICANCE ; SUMMER MONSOON ; MODERN SOILS ; LIUPAN-SHAN ; LOESS/PALAEOSOL SEQUENCES |
收录类别 | SCI ; SCI |
语种 | 英语 |
资助项目 | Natural Science Foundation of China (NSFC)[41290253] ; Natural Science Foundation of China (NSFC)[41572162] ; Natural Science Foundation of China (NSFC)[41472147] ; Xi'an Centre of Geological Survey, CGS[[2017]0438] ; International partnership Program of Chinese Academy of Sciences (CAS)[132B61KYS20160002] ; Scientific and Technological Innovation Team of CAS[CAS Renzi (2013)47] |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
项目资助者 | Natural Science Foundation of China (NSFC) ; Xi'an Centre of Geological Survey, CGS ; International partnership Program of Chinese Academy of Sciences (CAS) ; Scientific and Technological Innovation Team of CAS |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
WOS记录号 | WOS:000452585100011 |
出版者 | ELSEVIER SCIENCE BV |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.ieecas.cn/handle/361006/14487 |
专题 | 古环境研究室 |
通讯作者 | Song, Yougui |
作者单位 | 1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Shaanxi, Peoples R China 2.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China 3.Fujian Normal Univ, Coll Geog Sci, Inst Geog, Fuzhou 350007, Fujian, Peoples R China 4.Okayama Univ Sci, Fac Informat, Okayama 7000005, Japan 5.Kyoto Univ, Grad Sch Human & Environm Studies, Kyoto 6068501, Japan 6.Minist Land & Resources China, Xian Ctr Geol Survey, Key Lab Geohazard Loess Area, Xian 710054, Shaanxi, Peoples R China 7.Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Lanzhou 730000, Gansu, Peoples R China |
推荐引用方式 GB/T 7714 | Song, Yougui,Fang, Xiaomin,Chen, Xiuling,et al. Rock magnetic record of late Neogene red clay sediments from the Chinese Loess Plateau and its implications for East Asian monsoon evolution[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2018,510:109-123. |
APA | Song, Yougui.,Fang, Xiaomin.,Chen, Xiuling.,Torii, Masayuki.,Ishikawa, Naoto.,...&Chan, Hong.(2018).Rock magnetic record of late Neogene red clay sediments from the Chinese Loess Plateau and its implications for East Asian monsoon evolution.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,510,109-123. |
MLA | Song, Yougui,et al."Rock magnetic record of late Neogene red clay sediments from the Chinese Loess Plateau and its implications for East Asian monsoon evolution".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 510(2018):109-123. |
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