globalchange  > 影响、适应和脆弱性
DOI: 10.1111/gcb.12336
论文题名:
The Eocene climate of China, the early elevation of the Tibetan Plateau and the onset of the Asian Monsoon
作者: Wang Q.; Spicer R.A.; Yang J.; Wang Y.-F.; Li C.-S.
刊名: Global Change Biology
ISSN: 13541013
出版年: 2013
卷: 19, 期:12
起始页码: 3709
结束页码: 3728
语种: 英语
英文关键词: Asian Monsoon ; China ; Co-existence approach ; Eocene ; Isogram map ; Quantitative palaeoclimate reconstruction ; Tibetan Plateau
Scopus关键词: climate effect ; climate variation ; coexistence ; Eocene ; fossil record ; mapping ; monsoon ; paleoclimate ; paleoenvironment ; paleotemperature ; palynology ; precipitation (climatology) ; reconstruction ; China ; Qinghai-Xizang Plateau ; rain ; article ; Asian Monsoon ; China ; climate ; climate change ; co-existence approach ; Eocene ; fossil ; isogram map ; quantitative palaeoclimate reconstruction ; Tibetan Plateau ; Asian Monsoon ; China ; co-existence approach ; Eocene ; isogram map ; quantitative palaeoclimate reconstruction ; Tibetan Plateau ; China ; Climate ; Climate Change ; Fossils ; Rain
英文摘要: Eocene palynological samples from 37 widely distributed sites across China were analysed using co-existence approach to determine trends in space and time for seven palaeoclimate variables: Mean annual temperature, mean annual precipitation, mean temperature of the warmest month, mean temperature of the coldest month, mean annual range of temperature, mean maximum monthly precipitation and mean minimum monthly precipitation. Present day distributions and observed climates within China of the nearest living relatives of the fossil forms were used to find the range of a given variable in which a maximum number of taxa can coexist. Isotherm and isohyet maps for the early, middle and late Eocene were constructed. These illustrate regional changing patterns in thermal and precipitational gradients that may be interpreted as the beginnings of the modern Asian Monsoon system, and suggest that the uplift of parts of the Tibetan Plateau appear to have taken place by the middle to late Eocene. © 2013 John Wiley & Sons Ltd.
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被引频次[WOS]:25   [查看WOS记录]     [查看WOS中相关记录]
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/62271
Appears in Collections:影响、适应和脆弱性

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作者单位: State Key Laboratory of Systematic and Evolutionary Botany, Institute of Botany, Chinese Academy of Sciences, Beijing, 100093, China; Beijing Radiation Center, Beijing, 100875, China; College of Life Sciences, Liaoning Normal University, Dalian, 116029, China; Department of Earth Sciences, Centre for Earth, Planetary, Space and Astronomical Research, The Open University, Milton Keynes, ML 76 AA, United Kingdom

Recommended Citation:
Wang Q.,Spicer R.A.,Yang J.,et al. The Eocene climate of China, the early elevation of the Tibetan Plateau and the onset of the Asian Monsoon[J]. Global Change Biology,2013-01-01,19(12)
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