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新生代东亚地形、水系与生物地理演变——第三届地球系统科学大会拾翠

DOI: 10.11867/j.issn.1001-8166.2014.11.1280, PP. 1280-1286

Keywords: 新生代,亚洲,构造—,地貌,生物地理

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Abstract:

新生代期间,亚洲及周边地区地球深部过程与地表环境发生了一系列重大变革。印度板块—欧亚板块碰撞和太平洋板块俯冲驱动下的构造—地貌过程,导致青藏高原隆升、亚洲东部岩石圈伸展减薄、西太平洋边缘海扩张,并最终塑造了现今的宏观地形地貌和水系格局。这一系列构造地貌过程与新生代全球气候变冷、西风环流与亚洲季风环流重组、生物地理演变之间存在紧密的关联,成为地球科学领域重大前沿与热点课题,是开展地球深部与浅表过程、地球表层各圈层之间相互作用研究的重要切入点。

References

[1]  Pinxian. Deformation of Asia and global cooling: Searching links climate and tectonics[J]. Quaternary Science, 1998, 3: 213-221.[汪品先. 亚洲形变与全球变冷——探索气候与构造的关系[J]. 第四纪研究, 1998, 3: 213-221.]
[2]  P, Xu Z, Roger F, et al. Oblique stepwise rise and growth of the Tibet Plateau[J]. Science, 2001, 294: 1 671-1 677.
[3]  P, Kapp P, Gehrels G. Paleocene-Eocene foreland basin evolution in the Himalaya of southern Tibet and Nepal: Implications for the age of initial India-Asia collision[J]. Tectonics, 2014, 33, doi:10.1002/2014TC003522.
[4]  Xiumian, An Wei, Wang Jian’gang. Basin evolution in the Yarlung Zangbo Suture: From Tethyan subduction to Indian-Asian collision[C]\\ Abstract of the Third Conference on Earth System Science.Shanghai, 2014.[胡修棉, 安慰, 王建刚. 横过雅鲁藏布缝合带的沉积盆地演化: 从特提斯俯冲到印亚大陆碰撞[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[5]  Peizhen, Zhang Huiping, Zheng Wenjun. Cenozoic tectonic evolution of East Asia[C]\\ Abstract of the Third Conference on Earth System Science. Shanghai, 2014.[张培震, 张会平, 郑文俊. 东亚大陆新生代构造演化[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[6]  Junliang, Song Bowen, Zhang Kexin. Magnetostratigraphy of Dahonggou section in Qaidam Basin[C]\\ Abstract of the Third Conference on Earth System Science.Shanghai, 2014.[季军良, 宋博文, 张克信. 柴达木盆地东北部大红沟剖面新生代磁性地层与构造隆升[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[7]  E, Kirby E, Furlong K, et al. Two-phase growth of high topography in eastern Tibet during the Cenozoic[J]. Nature Geoscience, 2012, 5: 640-645.
[8]  C, Zhao X, Lippert P. Constraints on the early uplift history of the Tibetan Plateau[J]. Proceedings of the National Academy of Sciences, 2008, 105(13): 4 987-4 992.
[9]  K, Wang G, Ji J, et al. Paleogene-Neogene stratigraphic realm and sedimentary sequence of the Qinghai-Tibet Plateau and their response to uplift of the plateau[J]. Science in China (Series D), 2010, 53(9): 1 271-1 294.
[10]  Guodong, Ma Yongjia, Sun Jimin. Paleoaltitude of Lunpola Basin at Qoligocene/Miocene boundary[C]\\ Abstract of the Third Conference on Earth System Science.Shanghai, 2014.[贾国东, 马永嘉, 孙继敏. 渐新世—中新世之交青藏高原伦坡拉盆地的古高度[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[11]  Yan, Fang Xiaomin, Tian Xi, et al. Stable isotope paleohypsometry in southern Tibetan Plateau[C]\\ Abstract of the Third Conference on Earth System Science.Shanghai, 2014.[白艳, 方小敏, 田茜, 等.青藏高原南部稳定同位素高度计[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[12]  Chunfeng, Lin Jian, Denise Kulhanek. Evolution of oceanic lithosphere of South China Sea: New results from IODP 349[C]\\ Abstract of the Third Conference on Earth System Science. Shanghai, 2014.[李春峰, 林间, Denise Kulhanek. 南海大洋岩石圈演化与沉积环境变迁——IODP 349航次新成果[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[13]  Ping, Zheng Hongbo, Chen Jun. Cenozoic exhumation of Huangling anticline: Sedimentary evidence from western Jianghan Basin[C]\\ Abstract of the Third Conference on Earth System Science.Shanghai, 2014.[王平, 郑洪波, 陈军. 黄陵背斜的新生代剥露——来自江汉盆地西缘的沉积记录[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[14]  J, Zhao D. High-resolution mantle tomography of China and surrounding regions[J]. Journal of Geophysical Research, 2006, 111: B09305, doi:10.1029/2005JB004066.
[15]  M E, Ruddiman W F. Tectonic forcing of late Cenozoic climate[J]. Nature, 1992, 359: 117-122.
[16]  Milliman, Katherine Farnsworth. River Discharge to the Coastal Ocean: A Global Synthesis[M]. Cambridge: Cambridge University Press, 2011.
[17]  Mengying, Zheng Hongbo, Bookhagen Bodo, et al. Controls on erosion intensity in the Yangtze River Basin tracked by detrital U-Pb zircon dating[J]. Earth-Science Reviews, 2014, 136: 121-140.
[18]  Meie, Bao Haosheng, Han Tongchun, et al. The geomorphology of the Jinshajiang valley of northwest Yunnan and problems associated with river capture[J]. Acta Geographica Sinica, 1959, 25(2): 135-155.[任美锷, 包浩生, 韩同春.云南西北部金沙江河谷地貌与河流袭夺问题[J]. 地理学报, 1959, 25(2): 135-155.]
[19]  J J, Xie S Y, Kuang M S, et al. Geomorphic evolution of the Yangtze gorges and the time of their formation[J]. Geomorphology, 2001, 41: 125-136.
[20]  H B, Clift P, Wang P, et al. Pre-Miocene birth of the Yangtze River[J]. Proceedings of the National Academy of Sciences, 2013, 110(19): 7 529-7 960.
[21]  Hongbo, Wang Ping, He Mengying. Birth of the Yangtze River: Tectonic and geomorphic processes[C]\\ Abstract of the Third Conference on Earth System Science.Shanghai, 2014.[郑洪波, 王平, 何梦颖. 长江的诞生——构造与地貌过程[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[22]  W F. Tectonic Uplift and Climatic Change[M]. New York: Plenum Press, 1997.
[23]  Xiaomin, Sun Jimin, Xu Zhifang. Continental weathering in western China and uplift of Tibetan Plateau[C]\\ Abstract of the Third Conference on Earth System Science.Shanghai, 2014.[方小敏, 孙继敏, 许志方. 中国西部大陆剥蚀风化与青藏高原隆升[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[24]  Zihua, Huang Baochun, Ding Zhongli. Pollen record of Kuche area in Tarim Basin during Oligocene[C]\\ Abstract of the Third Conference on Earth System Science.Shanghai, 2014.[唐自华, 黄宝春, 丁仲礼.塔里木盆地库车地区渐新世以来的孢粉记录[C]\\ 第三届地球系统科学大会摘要. 上海, 2014.]
[25]  X J, Wang P X. How old is the Asian monsoon? Palaeobotanical constraints from China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 222: 181-222.
[26]  G, Fluteau F, Besse J. Effect of orogeny, plate motion and landesea distribution on Eurasian climate change over the past 30 million years[J]. Nature, 1997, 386: 788-795.
[27]  R, Dupont-Nivet G, Houben A, et al. Late Eocene sea retreat from the Tarim Basin (west China) and concomitant Asian paleoenvironmental change[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 299: 385-398.
[28]  J, Pagani M, Sloan L, et al. Trends, rhythms, and aberrations in global climate 65 Ma to present[J]. Science, 2001, 292: 686-693.
[29]  Z, Ruddiman W F, Hao Q, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J]. Nature, 2002, 416: 159-163.
[30]  T, Halliday A, Rea D. Cenozoic evolution of Asian climate and sources of Pacific seawater Pb and Nd derived from eolian dust of sediment core LL44-GPC3[J]. Paleoceanography, 2002, 17(3): 1-31, doi:10.1029/2001PA000673.
[31]  Y, Cerling T E, MacFadden B. Fossil horses and carbon isotopes: New evidence for Cenozoic dietary, habitat, and ecosystem changes in North America[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1994, 107: 269-279.
[32]  J, Cerling T E. Expansion of C4 grasses in the Late Miocene of northern Pakistan: Evidence from stable isotopes in paleosols[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1995, 115: 91-116.
[33]  M, Kingston J, Marino B. Carbon isotopic evidence for the emergence of C4 plants in the Neogene from Pakistan and Kenya[J]. Nature, 1994, 367: 162-164.
[34]  Y, Deng T. A 25-Ma record of paleodiet and environmental change from carbon and oxygen isotopes in mammalian tooth enamel and paleosols from the NE margin of the Tibetan Plateau[J]. Earth and Planetary Science Letters, 2005, 236: 322-338.
[35]  C F, Wang Y, Deng T, et al. C4 expansion in the central Inner Mongolia during the latest Miocene and early Pliocene[J]. Earth and Planetary Science Letters, 2009, 287: 311-319.
[36]  C F, Wang Y, Li Q, et al. Diets and environments of late Cenozoic mammals in the Qaidam Basin, Tibetan Plateau: Evidence from stable isotopes[J]. Earth and Planetary Science Letters, 2012, 333/334: 70-82.
[37]  T, Wang X M, Fortelius M, et al. Out of Tibet: Pliocene woolly rhino suggests high-plateau origin of Ice Age megaherbivores[J]. Science, 2011, 333: 1 285-1 288.
[38]  Z J, Wang X M, Slater G J, et al. Himalayan fossils of the oldest known pantherine establish ancient origin of big cats[J]. Proccedings of the Royal Society B, 2014, 281, doi.org/10.1098/rspb.2013: 2686.
[39]  X M, Tseng Z J, Li Q, et al. From ‘third pole’ to north pole: A Himalayan origin for the arctic fox[J]. Proccedings of the Royal Society B, 2014, 281, doi.org/10.1098/rspb.2014: 0893.[JP]
[40]  Tao. Tibetan origin of Quaternary Ice Age fauna and its northward spreading[C]\\ Abstract of the Third Conference on Earth System Science. Shanghai, 2014.[邓涛. 第四纪冰期动物群的青藏高原起源及其在全北界的扩散[C]\\ 第三届地球系统科学大会摘要.上海, 2014.]
[41]  Xiaohong, Liu Junlai, Ren Shoumai. Influence of Tibetan Plateau uplift on tectonic-geomorphology, climate and migration of ancient humen[C]\\ Abstract of the Third Conference on Earth System Science. Shanghai, 2014.[葛肖虹, 刘俊来, 任收麦. 青藏高原隆升对我国构造—地貌形成、气候环境变迁与古人类迁徙的影响[C]\\ 第三届地球系统科学大会摘要. 上海, 2014.]
[42]  Q M, Meyer M, Gao X, et al. DNA analysis of an early modern human from Tianyuan Cave, China[J]. Proceedings of the National Academy of Sciences, 2013, 110: 2 223-2 227.

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