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  4. 岩石圈演化国家重点实验室
Uplift of the Hengduan Mountains on the southeastern margin of the Tibetan Plateau in the late Miocene and its paleoenvironmental impact on hominoid diversity

文献类型：期刊论文

作者Li, Shihu5,6; Ji, Xueping1,7; Harrison, Terry2; Deng, Chenglong5; Wang, Shiqi3; Wang, Lirui4; Zhu, Rixiang5
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2020-09-01
卷号553页码:14
ISSN号0031-0182
关键词Hominoid Uplift of the Tibetan Plateau Paleoclimate Magnetostratigraphy Aridification Indian monsoon
DOI10.1016/j.palaeo.2020.109794
英文摘要The southeastern margin of the Tibetan Plateau has a number of well-known Late Miocene localities that have yielded fossil hominoids belonging to Lufengpithecus and Khoratpithecus. These localities provide critical evidence about the evolutionary history of hominoids, including their response to environmental changes associated with uplift of the Tibetan Plateau. Here we present magnetostratigraphic dating of the Baoshan hominoid locality in Yunnan, southwestern China, which, based on preliminary biochronological evidence, was previously assumed to be the youngest known Miocene hominoid locality in Eurasia. Paleomagnetic investigations yield three normal and three reversed magnetozones, which can be best correlated, in conjunction with biostratigraphic constraints, to Chrons C3n.4n to C3Ar. The Baoshan hominoid is derived from a horizon correlated with the lowest part of C3r, having an estimated age of similar to 6.0 Ma. This indicates that the Baoshan hominoid is slightly younger than L. cf. lufengensis from Zhaotong, dated to similar to 6.2 Ma, and L. lufengensis from Lufeng, dated to similar to 6.9-6.2 Ma. Our results, coupled with previously published magnetochronology, indicate that hominoids occurred in Southeast Asia from the latest Middle Miocene to the terminal Miocene (similar to 13-6 Ma). The period after 6 Ma coincides with the uplift of the Hengduan Mountains, especially the Gaoligong Mountain. We propose that the Late Miocene uplift of these N-S oriented mountains on the southeastern margin of the Tibetan Plateau created a barrier to the warm and moist Indian monsoon from the west, and this led to a cooler and drier climate in the southeastern margin of the Tibetan Plateau. This paleoenvironmental change potentially had a profound impact on the diversity of the hominoid community in southwestern China and Southeast Asia.
WOS关键词PALEOMAGNETIC CONSTRAINTS ; SOUTHWESTERN CHINA ; NORTHERN THAILAND ; YUANMOU BASIN ; TAXONOMIC STATUS ; YUNNAN PROVINCE ; WESTERN YUNNAN ; DALI BASIN ; SHEAR ZONE ; PLEISTOCENE
资助项目National Natural Science Foundation[41888101] ; National Natural Science Foundation[41690112] ; Strategic Priority Research Program of Chinese Academy of Sciences[XDB26000000] ; Royal Society-K.C.Wong Newton International Fellowship ; International Partnership Program of the Chinese Academy of Sciences[GJHZ1776]
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
出版者ELSEVIER
WOS记录号WOS:000543433100009
资助机构National Natural Science Foundation ; National Natural Science Foundation ; National Natural Science Foundation ; National Natural Science Foundation ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; National Natural Science Foundation ; National Natural Science Foundation ; National Natural Science Foundation ; National Natural Science Foundation ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; National Natural Science Foundation ; National Natural Science Foundation ; National Natural Science Foundation ; National Natural Science Foundation ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; National Natural Science Foundation ; National Natural Science Foundation ; National Natural Science Foundation ; National Natural Science Foundation ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Strategic Priority Research Program of Chinese Academy of Sciences ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; Royal Society-K.C.Wong Newton International Fellowship ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences ; International Partnership Program of the Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/97165]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Li, Shihu; Deng, Chenglong
作者单位1.Yunnan Univ, Yunnan Key Lab Earth Syst Sci, Kunming 650500, Yunnan, Peoples R China
2.NYU, Ctr Study Human Origins, Dept Anthropol, 25 Waverly Pl, New York, NY 10003 USA
3.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
4.Baoshan Inst Cultural Rel, Baoshan 678000, Yunnan, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
6.Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YQ, England
7.Yunnan Cultural Rel & Archaeol Inst, Kunming 650118, Yunnan, Peoples R China
推荐引用方式
GB/T 7714		 Li, Shihu,Ji, Xueping,Harrison, Terry,et al. Uplift of the Hengduan Mountains on the southeastern margin of the Tibetan Plateau in the late Miocene and its paleoenvironmental impact on hominoid diversity[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2020,553:14.
APA Li, Shihu.,Ji, Xueping.,Harrison, Terry.,Deng, Chenglong.,Wang, Shiqi.,...&Zhu, Rixiang.(2020).Uplift of the Hengduan Mountains on the southeastern margin of the Tibetan Plateau in the late Miocene and its paleoenvironmental impact on hominoid diversity.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,553,14.
MLA Li, Shihu,et al."Uplift of the Hengduan Mountains on the southeastern margin of the Tibetan Plateau in the late Miocene and its paleoenvironmental impact on hominoid diversity".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 553(2020):14.

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来源：地质与地球物理研究所

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