Vegetation and climate of the central and northern Qinghai-Xizang plateau from the Middle Jurassic to the end of the Paleogene inferred from palynology
文献类型:期刊论文
作者 | Li, Jianguo (李建国)1,2; Wu, Yixiao3,4; Batten, David J.5,6; Lin, Miaoqin3,4 |
刊名 | JOURNAL OF ASIAN EARTH SCIENCES |
出版日期 | 2019-05-15 |
卷号 | 175页码:35-48 |
ISSN号 | 1367-9120 |
关键词 | Palaeovegetation Palaeoelevation Indian-eurasian Collision Mesozoic Cenozoic Palynostratigraphy |
DOI | 10.1016/j.jseaes.2018.08.012 |
英文摘要 | The collision between India and Eurasia and the subsequent uplift of the Qinghai-Xizang plateau region of the Eurasian continent during the latest Mesozoic and Cenozoic had a significant environmental impact on the region. Understanding the vegetation of both palaeocontinents prior to the collision is crucial for interpreting the evolution of their floras and climatic changes during this period. The composition of the vegetation and climate of the plateau from the Middle Jurassic until the end of the Oligocene are inferred herein from the composition of 14 palynofloras and compared with other regions of China. The palynofloras are similar to those of eastern and northwestern parts of China but bear their own unique features brought about by differing climatic influences. Overall, a warm-hot, arid-semi-arid climate prevailed over the plateau during most of the period from the Middle Jurassic until the end of the Cretaceous. The climate cooled and humidity increased in the Paleogene, and especially during the Oligocene. The long-term climatic change in the Qinghai-Xizang plateau region of the Eurasian continent during the Middle Jurassic-Paleogene that is indicated by the miospore assemblages is broadly comparable to the isotope-based SST (sea-surface temperature) changes that have been identified. It is apparent that climatic changes on a global scale were primarily responsible for controlling the composition and distribution of the vegetation on the plateau; no monsoon features are detectable in the northwestern interior of China. A maximum estimation of 2890 m surface palaeoelevation is inferred for the central and northern plateau during the Oligocene based on vegetation analysis, which is lower than previous estimations based on oxygen isotope and coexistence analyses. The elevation of the southern part of the study area, i.e. the area south of the Gandise Mountains, was low, close to sea-level. |
WOS关键词 | India-asia Collision ; Tibetan Plateau ; Cretaceous Palynofloras ; Tectonic Evolution ; Lunpola Basin ; Late-eocene ; Paleoclimate ; Uplift ; Age ; Paleocene |
资助项目 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDA20070202] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB26000000] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB03010103] ; National Natural Science Foundation of China[41688103] ; National Natural Science Foundation of China[41872004] |
WOS研究方向 | Geology |
语种 | 英语 |
出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
WOS记录号 | WOS:000464298500003 |
资助机构 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China |
源URL | [http://ir.nigpas.ac.cn/handle/332004/15759] |
专题 | 中国科学院南京地质古生物研究所 南京地质古生物研究所_其他 |
通讯作者 | Li, Jianguo (李建国) |
作者单位 | 1.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, 39 East Beijing Rd, Nanjing 210008, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Ctr Excellence Life & Paleoenvironm, 39 East Beijing Rd, Nanjing 210008, Peoples R China 3.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, 39 East Beijing Rd, Nanjing 210008, Peoples R China 4.Univ Sci & Technol China, 96 Jinzhai Rd, Hefei 230026, Anhui, Peoples R China 5.Aberystwyth Univ, Dept Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales 6.Univ Manchester, Sch Earth Atmospher & Environm Sci, Oxford Rd, Manchester M13 9PL, Lancs, England |
推荐引用方式 GB/T 7714 | Li, Jianguo ,Wu, Yixiao,Batten, David J.,et al. Vegetation and climate of the central and northern Qinghai-Xizang plateau from the Middle Jurassic to the end of the Paleogene inferred from palynology[J]. JOURNAL OF ASIAN EARTH SCIENCES,2019,175:35-48. |
APA | Li, Jianguo ,Wu, Yixiao,Batten, David J.,&Lin, Miaoqin.(2019).Vegetation and climate of the central and northern Qinghai-Xizang plateau from the Middle Jurassic to the end of the Paleogene inferred from palynology.JOURNAL OF ASIAN EARTH SCIENCES,175,35-48. |
MLA | Li, Jianguo ,et al."Vegetation and climate of the central and northern Qinghai-Xizang plateau from the Middle Jurassic to the end of the Paleogene inferred from palynology".JOURNAL OF ASIAN EARTH SCIENCES 175(2019):35-48. |
入库方式: OAI收割
来源:南京地质古生物研究所
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