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DOI10.1029/2020GL087741
Late Miocene Climate Cooling Contributed to the Disappearance of Hominoids in Yunnan Region; Southwestern China
Li P.; Zhang C.; Kelley J.; Deng C.; Ji X.; Jablonski N.G.; Wu H.; Fu Y.; Guo Z.; Zhu R.
发表日期2020
ISSN 0094-8276
卷号47期号:11
英文摘要The relationship between long-sequence climate change and Miocene hominoid evolution in the Yunnan region of southwestern China has recently received some attention, partly because this region has been regarded as a “refugium” for hominoids at the end of the Miocene. Here, we carry out a high-resolution reconstruction of climate evolution in the Zhaotong Basin of Yunnan through the late Miocene to Pliocene using chemical weathering indices and other proxies. The results reveal gradual cooling within generally warm and humid conditions from 8.8–6.2 Ma; three more marked cooling episodes from 6.2–5.0 Ma; cool and humid conditions from 5.0–2.8 Ma; finally, cold and humid conditions from 2.8–2.62 Ma. The evidence is compatible with a scenario in which terminal Miocene cooling episodes within a prevailing warm and humid climate, and associated changes in vegetation, may have been critical factors in the disappearance of hominoids from this region. ©2020. American Geophysical Union. All Rights Reserved.
英文关键词Weathering; Chemical weathering; Climate cooling; Critical factors; High-resolution reconstruction; Humid conditions; Long sequences; Warm and humid climates; Warm and humid conditions; Climate change; chemical weathering; climate conditions; climate variation; cooling; episodic event; hominid; humid tropics; Miocene; Pliocene; proxy climate record; reconstruction; refugium; warming; China; Yunnan; Zhaotong; Hominoidea; Homo
语种英语
来源期刊Geophysical Research Letters
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/170314
作者单位Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, China; CAS Center for Excellence in Life and Paleoenvironment, Beijing, China; College of Earth Science and Engineering, Shandong University of Science and Technology, Qingdao, China; Institute of Human Origins and School of Human Evolution and Social Change, Arizona State University, Tempe, AZ, United States; Department of Human Evolutionary Biology, Harvard University, Cambridge, MA, United States; State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China; Department of Paleoanthropology, Yunnan Institute of Cultural Relics and Archaeology, Kunming, China; Joint Research Center for Human Evolution and Environmental Changes of Yunnan, Zhaotong, China; Department of Anthropology, The Pennsylvania State University...
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Li P.,Zhang C.,Kelley J.,et al. Late Miocene Climate Cooling Contributed to the Disappearance of Hominoids in Yunnan Region; Southwestern China[J],2020,47(11).
APA Li P..,Zhang C..,Kelley J..,Deng C..,Ji X..,...&Zhu R..(2020).Late Miocene Climate Cooling Contributed to the Disappearance of Hominoids in Yunnan Region; Southwestern China.Geophysical Research Letters,47(11).
MLA Li P.,et al."Late Miocene Climate Cooling Contributed to the Disappearance of Hominoids in Yunnan Region; Southwestern China".Geophysical Research Letters 47.11(2020).
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