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DOI10.1016/j.palaeo.2020.109794
Uplift of the Hengduan Mountains on the southeastern margin of the Tibetan Plateau in the late Miocene and its paleoenvironmental impact on hominoid diversity
Li S.; Ji X.; Harrison T.; Deng C.; Wang S.; Wang L.; Zhu R.
发表日期2020
ISSN0031-0182
卷号553
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 ~6.0 Ma. This indicates that the Baoshan hominoid is slightly younger than L. cf. lufengensis from Zhaotong, dated to ~6.2 Ma, and L. lufengensis from Lufeng, dated 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 (~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. © 2020 Elsevier B.V.
英文关键词Aridification; Hominoid; Indian monsoon; Magnetostratigraphy; Paleoclimate; Uplift of the Tibetan Plateau
语种英语
scopus关键词biochronology; community structure; environmental change; environmental effect; fossil record; hominid; magnetostratigraphy; Miocene; monsoon; paleoenvironment; uplift; Baoshan [Shanghai]; Baoshan [Yunnan]; China; Hengduan Mountains; Qinghai-Xizang Plateau; Shanghai; Yunnan; Zhaotong; Hominoidea; Homo
来源期刊Palaeogeography, Palaeoclimatology, Palaeoecology
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/150453
作者单位State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; Lancaster Environment Centre, Lancaster University, Lancaster, LA1 4YQ, United Kingdom; Yunnan Cultural Relics and Archaeology Institute, Kunming, Yunnan 650118, China; Yunnan Key Laboratory of Earth System Science, Yunnan University, Kunming, 650500, China; Center for the Study of Human Origins, Department of Anthropology, New York University, 25 Waverly Place, New York, NY 10003, United States; Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, 100044, China; Baoshan Institute of Cultural Relics, Baoshan, Yunnan 678000, China
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Li S.,Ji X.,Harrison T.,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],2020,553.
APA Li S..,Ji X..,Harrison T..,Deng C..,Wang S..,...&Zhu R..(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.
MLA Li S.,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).
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