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DOI | 10.1029/2020GL087741 |
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
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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... |
推荐引用方式 GB/T 7714 | 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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