New U-Pb dates show a Paleogene origin for the modern Asian biodiversity hot spots
文献类型：期刊论文
| 作者 | Linnemann, U.; Su, T.; Kunzmann, L.; Spicer, R. A.; Ding, W. -N.; Spicer, T. E. V.; Zieger, J.; Hofmann, M.; Moraweck, K.; Gaertner, A. |
| 刊名 | GEOLOGY
 |
| 出版日期 | 2018 |
| 卷号 | 46期号:1页码:3-6 |
| ISSN号 | 0091-7613 |
| DOI | 10.1130/G39693.1 |
| 文献子类 | Article |
| 英文摘要 | Yunnan, in southwestern China, straddles two of the world's most important biodiversity hot spots (i.e., a biogeographic region that is both a reservoir of biodiversity and threatened with destruction) and hosts more than 200 fossiliferous sedimentary basins documenting the evolutionary history of that biodiversity, monsoon development, and regional elevation changes. The fossil biotas appear modern and have been assumed to be mostly Miocene in age. Dating has been by cross-correlation using palynology, magnetostratigraphy, and lithostratigraphy because numerical radiometric ages are lacking. Here we report the first unequivocal early Oligocene age (33-32 Ma) of a section in the Luhe Basin (25.141627 degrees N, 101.373840 degrees E, 1890 m above mean sea level), central Yunnan, based on U-Pb zircon dates of unreworked volcanic ash layers in a predominantly lacustrine succession hosting abundant plant and animal fossils. This section, located in Luhe town, is correlated with an adjacent section in the Luhe coal mine previously assigned to the upper Miocene based on regional lithostratigraphic comparison. Our substantially older age for the Luhe town section calls into question previous estimates for the surface uplift and climate history of the area, and the age of all other correlative basins. The modernization of the biota similar to 20 m.y. earlier than previously thought overturns existing concepts of vegetation history in southwestern China, and points to Paleogene modernization of the biota in Yunnan and associated Asian biodiversity hot spots. |
| 学科主题 | Geology |
| 出版地 | BOULDER |
| 电子版国际标准刊号 | 1943-2682 |
| WOS关键词 | MIOCENE ; YUNNAN ; EVOLUTION ; MARGIN ; CLIMATE ; CHINA ; PALEOALTIMETRY ; GEOCHEMISTRY ; TAXODIACEAE ; VEGETATION |
| 语种 | 英语 |
| WOS记录号 | WOS:000418589600001 |
| 出版者 | GEOLOGICAL SOC AMER, INC |
| 资助机构 | National Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [U1502231, 4161101253] ; Chinese Academy of Scientists (CAS) [QYZDB-SSW-SMC016] ; Youth Innovation Promotion Association, CAS [2017439] |
| 源URL | [http://ir.ibcas.ac.cn/handle/2S10CLM1/20552]  |
| 专题 | 植被与环境变化国家重点实验室 |
| 作者单位 | 1.[Gerdes, A. 2.[Ding, W. -N. 3.Spicer, T. E. V.] Chinese Acad Sci, Inst Bot, 20 Nanxincun, Beijing 100093, Peoples R China 4.[Spicer, R. A. 5.[Spicer, R. A.] Open Univ, Walton Hall,Kents Hill, Milton Keynes MK7 6AA, Bucks, England 6.Zhou, Z. -K.] Chinese Acad Sci, Xishuangbanna Trop Bot Garden, Key Lab Trop Forest Ecol, Menglun 666303, Yunnan, Peoples R China 7.Huang, J. 8.Tang, H. 9.Li, S. -F. 10.Ding, W. -N. |
| 推荐引用方式 GB/T 7714 | Linnemann, U.,Su, T.,Kunzmann, L.,et al. New U-Pb dates show a Paleogene origin for the modern Asian biodiversity hot spots[J]. GEOLOGY,2018,46(1):3-6. |
| APA | Linnemann, U..,Su, T..,Kunzmann, L..,Spicer, R. A..,Ding, W. -N..,...&Zhou, Z. -K..(2018).New U-Pb dates show a Paleogene origin for the modern Asian biodiversity hot spots.GEOLOGY,46(1),3-6. |
| MLA | Linnemann, U.,et al."New U-Pb dates show a Paleogene origin for the modern Asian biodiversity hot spots".GEOLOGY 46.1(2018):3-6. |
入库方式： OAI收割
来源：植物研究所
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