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| 1 | Tibet,the Himalaya,Asian monsoons and biodiversity-In what ways are they related?显示文摘Prevailing dogma asserts that the uplift of Tibet, the onset of the Asian monsoon system and high biodiversity in southern Asia are linked, and that all occurred after 23 million years ago in the Neogene.Here, spanning the last 60 million years of Earth history, the geological, climatological and palaeontological evidence for this linkage is reviewed. The principal conclusions are that: 1) A proto-Tibetan highland existed well before the Neogene and that an Andean type topography with surface elevations of at least 4.5 km existed at the start of the Eocene, before final closure of the Tethys Ocean that separated India from Eurasia. 2) The Himalaya were formed not at the start of the India-Eurasia collision, but after much of Tibet had achieved its present elevation. The Himalaya built against a pre-existing proto-Tibetan highland and only projected above the average height of the plateau after approximately 15 Ma. 3)Monsoon climates have existed across southern Asia for the whole of the Cenozoic, and probably for a lot longer, but that they were of the kind generated by seasonal migrations of the Inter-tropical Convergence Zone. 4) The projection of the High Himalaya above the Tibetan Plateau at about 15 Ma coincides with the development of the modern South Asia Monsoon. 5) The East Asia monsoon became established in its present form about the same time as a consequence of topographic changes in northern Tibet and elsewhere in Asia, the loss of moisture sources in the Asian interior and the development of a strong winter Siberian high as global temperatures declined. 6) New radiometric dates of palaeontological finds point to southern Asia's high biodiversity originating in the Paleogene, not the Neogene. | Robert A. Spicer | 2017 | Plant Diversity2017，39，5： | 30 |
| 2 | Uplift, climate and biotic changes at the Eocene-Oligocene transition in south-eastern Tibet显示文摘The uplift history of south-eastern Tibet is crucial to understanding processes driving the tectonic evolution of the Tibetan Plateau and surrounding areas.Underpinning existing palaeoaltimetric studies has been regional mapping based in large part on biostratigraphy that assumes a Neogene modernization of the highly diverse,but threatened,Asian biota.Here,with new radiometric dating and newly collected plant-fossil archives,we quantify the surface height of part of the south-eastern margin of Tibet in the latest Eocene(~34 Ma)to be^3 km and rising,possibly attaining its present elevation(3.9 km)in the early Oligocene.We also find that the Eocene–Oligocene transition in south-eastern Tibet witnessed leaf-size diminution and a floral composition change from sub-tropical/warm temperate to cool temperate,likely reflective of both uplift and secular climate change,and that,by the latest Eocene,floral modernization on Tibet had already taken place,implying modernization was deeply rooted in the Palaeogene. | Tao Su Robert A. Spicer Shi-Hu Li He Xu Jian Huang Sarah Sherlock Yong-Jiang Huang Shu-Feng Li Li Wang Lin-Bo Jia Wei-Yu-Dong Deng Jia Liu Cheng-Long Deng Shi-Tao Zhang Paul J. Valdes Zhe-Kun Zhou | 2019 | National Science Review2019，6，3： | 16 |
| 3 | Lake geochemistry reveals marked environmental change in Southwest China during the Mid Miocene Climatic Optimum显示文摘中间中新世的气候的最佳(MMCO;~ 15-17 ? 妈) 是标点的短期的气候的温暖的事件之一新生代长期的冷却趋势。因为有这个事件的很少的陆上的记录,大多数我们的理解来自海洋的核心。在这份报告,我们首先介绍修订标明日期的新 palaeomagnetic 数据我们的 400 ? 在 Wenshan (云南) 的 m 厚的湖的节,以前想了晚中新世。这些新数据建议老年, ca。15.2-16.5 ? 妈,与 MMCO 与一致。我们测量了 13 体积有机物上的 C (13 C 器官的碳(TOC ) ,全部的氮(TN ) 和在高度的 C/N 比率取样的 org ), 总数分辨率:(1 ) 重建在湖集水区域的 palaeoenvironmental 变化,并且(2 ) 推断为这些变化负责的机制。我们的结果证明所有四个 geochemical 参数证明一个强壮的环境变化发生在节的中间附近,立即在在 15.97 点的 C5Cn/C5Br 地磁气的颠倒和早 / 中间中新世的边界以后 ? 妈。我们建议环境移动可能由于在气候的一个变化的联合,它变得更凉爽,和在有机物在湖以内骑车的一个变化。这研究提供新卓见进 MMCO 并且证明尽管 MMCO 通常是一个温暖的事件,它也是气候的不稳定性和突然的环境变化的一倍。 | Julie Lebreton-Anberree Shihu Li Shu-Feng Li Robert A. Spicer Shi-Tao Zhang Tao Su Chenglong Deng Zhe-Kun Zhou | 2016 | Science Bulletin2016，61，11： | 8 |
| 4 | Palaeoclimate background of the diverse Eocene floras of South China显示文摘Hainan and Guangdong provinces,located in north tropical area and south subtropical area of China respectively,bear one of the highest levels of biodiversity in China.The modern floras of Hainan and Guangdong are dominated by pantropical and tropical-subtropical taxa and many of their representative families appeared as early as in the Eocene[1].The Eocene,therefore,represents a crucial stage in the formation of the extant flora.However,previously the Eocene floras and vegetation were largely studied in mid- | Jian-Hua Jin Alexei B. Herman Robert A. Spicer Tatiana M. Kodrul | 2017 | Science Bulletin2017，62，22： | 2 |
| 5 | Pollen evidence for an Eocene to Miocene elevation of central southern Tibet predating the rise of the High Himalaya显示文摘 | Xiao-Yan Song Robert A. Spicer Jian Yang Yi-Feng Yao Cheng-Sen Li | 2010 | Palaeogeography, Palaeoclimatology, Palaeoecology2010，，1： | 1 |
| 6 | Pediatric Cardiomyopathy: Importance of Genetic and Metabolic Evaluation显示文摘 | Steven J. Kindel Erin M. Miller Resmi Gupta Linda H. Cripe Robert B. Hinton Robert L. Spicer Jeffrey A. Towbin Stephanie M. Ware | 2012 | Journal of Cardiac Failure2012，，5： | 1 |
| 7 | Pediatric Cardiomyopathy: Importance of Genetic and Metabolic Evaluation显示文摘 | Steven J. Kindel Erin M. Miller Resmi Gupta Linda H. Cripe Robert B. Hinton Robert L. Spicer Jeffrey A. Towbin Stephanie M. Ware | 2012 | Journal of Cardiac Failure2012，，5： | 1 |
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