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DOI10.1073/PNAS.2012647117
A Middle Eocene lowland humid subtropical “Shangri-La” ecosystem in central Tibet
Su T.; Spicer R.A.; Wu F.-X.; Farnsworth A.; Huang J.; Del Rio C.; Deng T.; Ding L.; Deng W.-Y.-D.; Huang Y.-J.; Hughes A.; Jia L.-B.; Jin J.-H.; Li S.-F.; Liang S.-Q.; Liu J.; Liu X.-Y.; Sherlock S.; Spicer T.; Srivastava G.; Tang H.; Valdes P.; Wang T.-X.; Widdowson M.; Wu M.-X.; Xing Y.-W.; Xu C.-L.; Yang J.; Zhang C.; Zhang S.-T.; Zhang X.-W.; Zhao F.; Zhou Z.-K.
发表日期2021
ISSN00278424
起始页码32989
结束页码32995
卷号117期号:52
英文摘要Tibet’s ancient topography and its role in climatic and biotic evolution remain speculative due to a paucity of quantitative surface-height measurements through time and space, and sparse fossil records. However, newly discovered fossils from a present elevation of ∼4,850 m in central Tibet improve substantially our knowledge of the ancient Tibetan environment. The 70 plant fossil taxa so far recovered include the first occurrences of several modern Asian lineages and represent a Middle Eocene (∼47 Mya) humid subtropical ecosystem. The fossils not only record the diverse composition of the ancient Tibetan biota, but also allow us to constrain the Middle Eocene land surface height in central Tibet to ∼1,500 ± 900 m, and quantify the prevailing thermal and hydrological regime. This “Shangri-La”–like ecosystem experienced monsoon seasonality with a mean annual temperature of ∼19 °C, and frosts were rare. It contained few Gondwanan taxa, yet was compositionally similar to contemporaneous floras in both North America and Europe. Our discovery quantifies a key part of Tibetan Paleogene topography and climate, and highlights the importance of Tibet in regard to the origin of modern Asian plant species and the evolution of global biodiversity. © 2020 National Academy of Sciences. All rights reserved.
英文关键词Biodiversity; Fossil; Monsoon; Tibetan Plateau; Topography
语种英语
scopus关键词article; biodiversity; climate; Europe; flora; fossil; Lutetian; nonhuman; North America; quantitative analysis; seasonal variation; Tibet; topography
来源期刊Proceedings of the National Academy of Sciences of the United States of America
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/179626
作者单位CAS Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, 666303, China; Center of Plant Ecology, Core Botanical Gardens, Chinese Academy of Sciences, Mengla, 666303, China; University of Chinese Academy of Sciences, Beijing, 100049, China; School of Environment, Earth and Ecosystem Sciences, Open University, Milton Keynes, MK7 6AA, United Kingdom; Key Laboratory of Vertebrate Evolution and Human Origins, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, 100044, China; Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Beijing, 100101, China; School of Geographical Sciences, Cabot Institute, University of Bristol, Bristol, BS8 1TH, United Kingdom; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, 100101, China; Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chines...
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Su T.,Spicer R.A.,Wu F.-X.,等. A Middle Eocene lowland humid subtropical “Shangri-La” ecosystem in central Tibet[J],2021,117(52).
APA Su T..,Spicer R.A..,Wu F.-X..,Farnsworth A..,Huang J..,...&Zhou Z.-K..(2021).A Middle Eocene lowland humid subtropical “Shangri-La” ecosystem in central Tibet.Proceedings of the National Academy of Sciences of the United States of America,117(52).
MLA Su T.,et al."A Middle Eocene lowland humid subtropical “Shangri-La” ecosystem in central Tibet".Proceedings of the National Academy of Sciences of the United States of America 117.52(2021).
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