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DOI | 10.1017/qua.2021.15 |
Chronological and rock magnetic constraints on the transition of the Quaternary paleoclimate in the western Qaidam Basin, NE Tibetan Plateau | |
Zhang, Weilin; Li, Tao; Fang, Xiaomin; Zhang, Tao; Yan, Maodu; Zan, Jinbo; Yang, Yibo; Khatri, Dhan Bahadur | |
通讯作者 | Zhang, WL (通讯作者) |
发表日期 | 2021 |
ISSN | 0033-5894 |
EISSN | 1096-0287 |
起始页码 | 170 |
结束页码 | 181 |
卷号 | 104 |
英文摘要 | A closed Quaternary saline paleolake, currently still a lake and named Dalangtan after one of its largest sub-basins, has widely distributed sediments in the western Qaidam Basin, NE Tibetan Plateau. Lacustrine salt minerals and fine sediments from this paleolake provide an environmental record for investigating paleoclimatic evolution in the Asian interior. However, detailed continuous Pliocene-Quaternary paleoclimatic records are broadly lacking from the NE Tibetan Plateau owing to poor exposure of the outcrops in section. For this study, we performed a detailed magnetostratigraphic dating and rock magnetic analysis on a 590-m-long core from the SG-5 borehole in the western Qaidam Basin. The results demonstrate that the lacustrine sediments in the SG-5 borehole were deposited more than similar to 3.0 Ma. Saline minerals began to increase at 1.2 Ma, and the magnetic susceptibility (chi) also changed at that time; the percentage frequency-dependent magnetic susceptibility was relatively low and uniform throughout the whole core. These observations, combined with the chi, pollen, salt ion, and grain-size records from other boreholes, indicate that the western Qaidam Basin and the greater Asian interior had a significant climate transition at 1.2 Ma during an extreme drought. |
关键词 | MIDPLEISTOCENE CLIMATE TRANSITIONALTYN-TAGH FAULTNORTHERN-HEMISPHEREDEFORMATION HISTORYSECTION RESTORATIONEURASIAN CLIMATESOUTHERN ASIAICE VOLUMECORE SG-1EVOLUTION |
英文关键词 | Magnetostratigraphy; Rock magnetism; Paleoclimate; Quaternary paleolake; Western Qaidam Basin |
语种 | 英语 |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000720829800014 |
来源期刊 | QUATERNARY RESEARCH
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来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260208 |
推荐引用方式 GB/T 7714 | Zhang, Weilin,Li, Tao,Fang, Xiaomin,et al. Chronological and rock magnetic constraints on the transition of the Quaternary paleoclimate in the western Qaidam Basin, NE Tibetan Plateau[J]. 中国科学院青藏高原研究所,2021,104. |
APA | Zhang, Weilin.,Li, Tao.,Fang, Xiaomin.,Zhang, Tao.,Yan, Maodu.,...&Khatri, Dhan Bahadur.(2021).Chronological and rock magnetic constraints on the transition of the Quaternary paleoclimate in the western Qaidam Basin, NE Tibetan Plateau.QUATERNARY RESEARCH,104. |
MLA | Zhang, Weilin,et al."Chronological and rock magnetic constraints on the transition of the Quaternary paleoclimate in the western Qaidam Basin, NE Tibetan Plateau".QUATERNARY RESEARCH 104(2021). |
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