Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.epsl.2020.116312 |
The early Eocene rise of the Gonjo Basin, SE Tibet: From low desert to high forest | |
Xiong, Zhongyu; Ding, Lin; Spicer, Robert A.; Farnsworth, Alexander; Wang, Xu; Valdes, Paul J.; Su, Tao; Zhang, Qinghai; Zhang, Liyun; Cai, Fulong; Wang, Houqi; Li, Zhenyu; Song, Peiping; Guo, Xudong; Yue, Yahui | |
通讯作者 | Ding, L |
来源期刊 | EARTH AND PLANETARY SCIENCE LETTERS |
ISSN | 0012-821X |
EISSN | 1385-013X |
出版年 | 2020 |
卷号 | 543 |
英文摘要 | Views differ on the uplift history of the SE Tibetan Plateau and causal geodynamic mechanisms, yet reliable age-constrained paleoaltimetry in this region could test growth models of the entire plateau. Here we apply carbonate clumped isotope thermometry to well-dated carbonate paleosols and marls in the Gonjo Basin, SE Tibet, to reveal the topographic evolution of the basin. The sedimentary ages of carbonates of the lower and upper Ranmugou Formation are constrained to 54-50 Ma and 44-40 Ma, respectively. The temperature derived from carbonate clumped isotope thermometry indicates the mean annual air temperature (MAAT) of the Gonjo Basin in the early Eocene was similar to 24 degrees C, which is consistent with the warm climate indicated by palm fossils. The MAAT of the basin in the middle Eocene was similar to 7 degrees C, 17 degrees C cooler than in the early Eocene. Carbonate clumped oxygen isotope thermometry-based paleoaltimetry shows the Gonjo Basin experienced a rapid uplift of 3.1 km, from similar to 0.7 km in the early Eocene to similar to 3.8 km in the middle Eocene. This rise explains the marked cooling. As a cause of this rapid rise, and the associated regional climate change transforming the landscape from desert to forest, we invoke crustal deformation and thickening induced by intracontinental subduction between the Lhasa and Qiangtang terranes that comprise the core of the Tibet. (C) 2020 Published by Elsevier B.V. |
英文关键词 | SE Tibetan Plateau clumped isotope paleoelevation Eocene intracontinental subduction |
类型 | Article |
语种 | 英语 |
开放获取类型 | Green Published, Other Gold |
收录类别 | SCI-E |
WOS记录号 | WOS:000540452500001 |
WOS关键词 | QIANGTANG TERRANE ; GEOLOGICAL EVOLUTION ; STABLE-ISOTOPES ; SOUTHERN TIBET ; HIGH-ELEVATION ; PLATEAU ; PALEOCENE ; CLIMATE ; PALEOALTIMETRY ; DELTA-O-18 |
WOS类目 | Geochemistry & Geophysics |
WOS研究方向 | Geochemistry & Geophysics |
来源机构 | 中国科学院青藏高原研究所 ; 中国科学院地质与地球物理研究所 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/324764 |
作者单位 | [Xiong, Zhongyu; Ding, Lin; Zhang, Qinghai; Zhang, Liyun; Cai, Fulong; Wang, Houqi; Li, Zhenyu; Song, Peiping; Guo, Xudong; Yue, Yahui] Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China; [Xiong, Zhongyu] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China; [Spicer, Robert A.; Su, Tao] Chinese Acad Sci, CAS Key Lab Trop Forest Ecol, Xishuangbanna Trop Bot Garden, Mengla 666303, Peoples R China; [Spicer, Robert A.] Open Univ, Sch Environm Earth & Ecosyst Sci, Milton Keynes MK7 6AA, Bucks, England; [Farnsworth, Alexander; Valdes, Paul J.] Univ Bristol, Sch Geog Sci, Univ Rd, Bristol BS8 1SS, Avon, England; [Wang, Xu] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100101, Peoples R China |
推荐引用方式 GB/T 7714 | Xiong, Zhongyu,Ding, Lin,Spicer, Robert A.,et al. The early Eocene rise of the Gonjo Basin, SE Tibet: From low desert to high forest[J]. 中国科学院青藏高原研究所, 中国科学院地质与地球物理研究所,2020,543. |
APA | Xiong, Zhongyu.,Ding, Lin.,Spicer, Robert A..,Farnsworth, Alexander.,Wang, Xu.,...&Yue, Yahui.(2020).The early Eocene rise of the Gonjo Basin, SE Tibet: From low desert to high forest.EARTH AND PLANETARY SCIENCE LETTERS,543. |
MLA | Xiong, Zhongyu,et al."The early Eocene rise of the Gonjo Basin, SE Tibet: From low desert to high forest".EARTH AND PLANETARY SCIENCE LETTERS 543(2020). |
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