1 Zachos J, Pagani M, Sloan L et al. Trends, rhythms, and aberrations in global climate: 65Ma to present. Science, 2001, 292 (5517): 686~693
[2]
2 Cerling T E, Wang Y, Quade J. Expansion of C4 ecosystems as indicator of global ecological change in the Late Miocene. Nature, 1993, 361 (6410): 344~345
[3]
13 孙继敏, 朱日祥. 天山北麓晚新生代沉积及其新构造与古环境指示意义. 第四纪研究, 2006, 26 (1): 14~19 Sun Jimin, Zhu Rixiang. Cenozoic deposits in the northern Tianshan Mountains and its implications for neotectonics and environmental changes. Quaternary Sciences, 2006, 26 (1): 14~19
15 Molnar P, England P. Late Cenozoic uplift of mountain range sand global climate change: Chicken or egg? Nature, 1990, 346 (6279): 29~34
[6]
16 Sun J M, Xu Q H, Huang B C. Late Cenozoic magnetochronology and paleoenvironmental changes in the northern foreland basin of the Tianshan Mountains. Journal of Geophysical Research, 2007, 112 : B04107, doi: 10.1029/2006JB004653
[7]
17 Tang Z H, Ding Z L, White P D et al. Late Cenozoic Central Asian drying inferred from a palynological record from the northern Tianshan. Earth and Planetary Science Letters, 2011, 302 (3): 439~447
[8]
18 Sun J M, Zhang Z Q. Palynological evidence for the Mid-Miocene climatic optimum recorded in Cenozoic sediments of the Tianshan Range, Northwestern China. Global and Planetary Change, 2008, 64 (1): 53~68
[9]
19 阎 顺. 新疆玛纳斯地区上新世孢粉组合及其意义. 干旱区地理, 1985, 8 (2): 29~34 Yan Shun. Palynological composition and its significant of Pliocene in Manasi, Xinjiang.Arid Land Geography, 1985, 8 (2): 29~34
[10]
20 阎 顺, 许英勤. 天山北麓平原区晚第三纪晚期-更新世的孢粉组合及环境变迁. 新疆地质, 1988, 6 (2): 59~65 Yan Shun, Xu Yingqin. Spore-pollen association and environmental evolution in northern piedment plain of Tianshan Mountain from Late Neogene to Pleistocene. Xinjiang Geology, 1988, 6 (2): 59~65
[11]
21 张金起, 刘 斌, 陈旭光等. 新疆艾比湖东南缘K3孔晚新生代环境演化. 现代地质, 2009, 23 (6): 1012~1021 Zhang Jinqi, Liu Bin, Chen Xuguang et al. Environmental evolution at the drilling hole K3 in the southeast margin of Ebinur Lake, Xinjiang in Late Cenozoic. Geoscience, 2009, 23 (6): 1012~1021
[12]
32 Sun X J, Wang P X. How old is the Asian monsoon system? —Palaeobotanical records from China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2005, 222 (3): 181~222
[13]
42 脱世博, 方小敏, 宋春晖等. 青藏高原东北部西宁盆地晚渐新世-早中新世沉积物岩石磁学特征及其古环境意义. 第四纪研究, 2013, 33 (5): 829~838 Tuo Shibo,Fang Xiaomin,Song Chunhui et al. Rock magnetic characteristics of the Late Oligocene to Early Miocene sediments in the Xining Basin, northeastern Tibetan Plateau. Quaternary Sciences, 2013, 33 (5): 829~838
[14]
43 常秋芳,常 宏. 罗布泊Ls2孔近7.1Ma以来沉积物的环境磁学研究. 第四纪研究, 2013, 33 (5): 876~888 Chang Qiufang,Chang Hong. The environmental magnetism study of core Ls2 in Lop Nur, Tarim since 7.1Ma. Quaternary Sciences, 2013, 33 (5): 876~888
[15]
44 Zhuang G S, Hourigan J K, Koch P L et al. Isotopic constraints on intensified aridity in Central Asia around 12Ma. Earth and Planetary Science Letters, 2011, 312 (1): 152~163
[16]
45 Zhang Z, Wang H, Guo Z et al. What triggers the transition of palaeoenvironmental patterns in China, the Tibetan Plateau or the Paratethys Sea retreat? Palaeogeography, Palaeoclimatology, Palaeoecology, 2007, 245 (3): 317~331
[17]
3 Cerling T E, Harris J M, MacFadden B J et al. Global vegetation change through the Miocene-Pliocene boundary. Nature, 1997, 389 (6647): 153~158
[18]
4 An Z S, Kutzbach J E, Prell W L et al. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan Plateau since Late Miocene times. Nature, 2001, 411 (6833): 62~66
[19]
5 Zheng H B, Powell C McA, Read D K et al. Late Miocene and Mid-Pliocene enhancement of the East Asian monsoon as viewed from the land and sea. Global and Planetary Change, 2004, 41 (3): 147~155
[20]
6 Ségalen L, Lee-Thorp J A, Cerling T. Timing of C4 grass expansion across sub-Saharan Africa. Journal of Human Evolution, 2007, 53 (5): 549~559
[21]
7 Mosbrugger V, Utescher T, Dilcher D L. Cenozoic continental climatic evolution of Central Europe. Proceedings of the National Academy of Sciences, 2005, 102 (42): 14964~14969
[22]
8 新疆维吾尔自治区地质矿产局. 新疆维吾尔自治区区域地质志. 北京: 地质出版社, 1993.1~50 Bureau of Geology and Mineral Resources of Xinjiang Uygur Autonomous Region. Regional Geology of Xinjiang Uygur Autonomous Region. Beijing: Geological Publishing House, 1993. 1~50
[23]
9 中国地层编辑委员会. 中国地层典(第三系). 北京: 地质出版社, 1999. 163 China Stratigraphical Editorial Committee. Stratigraphy of China (Tertiary).Beijing: Geological Publishing House, 1999. 163
[24]
10 Peng X L. Positions and stratigraphical control of the Cenozoic mammalian fossils in the Junggar Basin of Xinjiang. Vertebrate PalAsiatica, 1975, 13 : 185~189
[25]
11 Fu B H, Lin A M, Kano K et al. Quaternary folding of the eastern Tianshan, Northwest China. Tectonophysics, 2003, 369 (1): 79~101
[26]
12 Sun J M, Zhu R X, Bowler J. Timing of the Tianshan Mountains uplift constrained by magnetostratigraphic analysis of molasse deposits. Earth and Planetary Science Letters, 2004, 219 (3~4): 239~253
[27]
22 阎 顺. 新疆库车盆地第三纪孢粉化石及其所反映的自然环境. 新疆地理, 1983, 4 : 18~26 Yan Shun. Tertiary spore-pollen fossil and natural environment in Kuche Basin, Xinjiang. Xinjiang Geography, 1983, 4 : 18~26
[28]
23 金小赤, 王大宁, 柳永清等. 新疆库车库尔哈剖面两个新生代孢粉组合的时代和环境意义. 地质通报, 2002, 21 (12): 823~833 Jin Xiaochi, Wang Daning, Liu Yongqing et al. Two Cenozoic palynological assemblages of the Kurha section, Kuqa, Xinjiang and their age and environmental significance. Geological Bulletin of China, 2002, 21 (12): 823~833
[29]
24 Zhang Z Q, Sun J M. Palynological evidence for Neogene environmental change in the foreland basin of the southern Tianshan Range, Northwestern China. Global and Planetary Change, 2011, 75 (1): 56~66
[30]
25 阎 顺, 许英勤. 新疆塔克拉玛干沙漠中两个钻孔的孢粉分析及其意义. 新疆地质, 1990, 8 (4): 342~350 Yan Shun, Xu Yingqin. Analysis of pollen from two drill holes in Taklimakan Desert of Xinjiang and its significance.Xinjiang Geology, 1990, 8 (4): 342~350
[31]
26 Hao H, Ferguson D K, Chang H et al. Vegetation and climate of the Lop Nur area, China, during the past 7 million years. Climatic Change, 2012, 113 (2): 323~338
[32]
27 Sun J M, Zhang L Y, Deng C L et al. Evidence for enhanced aridity in the Tarim Basin of China since 5.3Ma. Quaternary Science Reviews, 2008, 27 (9): 1012~1023
[33]
28 杜 鹃, 洪汉烈, 张克信等. 新疆其木干剖面中新世-上新世沉积物粘土矿物特征及其古气候指示意义. 生态学杂志, 2010, 29 (5): 923~932 Du Juan, Hong Hanlie, Zhang Kexin et al. Clay mineralogy and its palaeoclimatic indicative significance of Miocene-Pliocene sediments in Qimugan of Xinjiang. Chinese Journal of Ecology, 2010, 29 (5): 923~932
[34]
29 Wang D N, Sun X Y, Zhao Y N. Palynoflora from Late Cretaceous to Tertiary in some regions of Qinghai and Xinjiang. Review of Palaeobotany and Palynology, 1990, 65 (1): 95~104
[35]
30 肖爱芳, 黎敦朋, 张汉军等. 新疆库木库里盆地渐新-上新统孢粉组合特征与古气候演变. 陕西地质, 2003, 21 (1): 36~44 Xiao Aifang, Li Dunpeng, Zhang Hanjun et al. Climate evolution and compositional features of sporopollen in the Oligocene-Pliocene series of the Kumukuli Basin in Xinjiang. Geology of Shaanxi, 2003, 21 (1): 36~44
[36]
31 Guo Z T, Ruddiman W F, Hao Q Z. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 2002, 416 (6877): 159~163
[37]
33 Wang P, Clemens S, Beaufort I. Evolution and variability of the Asian monsoon system: State of the art and outstanding issues. Quaternary Science Reviews, 2005, 24 (5): 595~629
[38]
34 Li F J, Rousseau D D, Wu N Q et al. Late Neogene evolution of the East Asian monsoon revealed by terrestrial mollusk record in western Chinese Loess Plateau: From winter to summer dominated sub-regime. Earth and Planetary Science Letters, 2008, 274 (3): 439~447
[39]
35 Yao Y F, Bruch A, Mosbrugger V et al. Quantitative reconstruction of Miocene climate patterns and evolution in Southern China based on plant fossils. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 304 (3): 291~307
[40]
36 郭正堂,彭淑贞,郝青振等. 晚第三纪中国西北干旱化的发展及其与北极冰盖形成演化和青藏高原隆升的关系. 第四纪研究, 1999, (6):556~567 Guo Zhengtang, Peng Shuzhen, Hao Qingzhen et al. Late Tertiary development of aridification in Northwestern China: Link with the Arctic ice-sheet formation and Tibetan uplifts. Quaternary Sciences, 1999, (6):556~567
[41]
37 安芷生, 张培震, 王二七等. 中新世以来我国季风-干旱环境演化与青藏高原的生长. 第四纪研究, 2006, 26 (5) : 678~693 An Zhisheng, Zhang Peizhen, Wang Erchie et al. Changes of the monsoon-arid environment in China and growth of the Tibetan Plateau since the Miocene. Quaternary Sciences, 2006, 26 (5) : 678~693
[42]
38 卢德源, 李秋生, 高 锐等. 横跨天山的人工爆炸地震剖面. 科学通报, 2000, 45 (9): 982~987 Lu Deyuan, Li Qiusheng, Gao Rui et al. A deep seismic sounding profile across the Tianshan Mountains. Chinese Science Bulletin, 2000, 45 (22): 2100~2106
[43]
39 张培震. 天山及其前陆盆地的晚新生代构造变形. 科学通报, 2003, 48 (24): 2249~2250 Zhang Peizhen.Late Cenozoic tectonic deformation in the Tianshan Mountain and its foreland basins. Chinese Science Bulletin, 2004, 49 (4):311~313
[44]
40 Miao Y F, Herrmann M, Wu F L et al. What controlled Mid-Late Miocene long-term aridification in Central Asia?—Global cooling or Tibetan Plateau uplift: A review. Earth-Science Reviews, 2012, 112 (3): 155~172
[45]
41 方小敏,吴福莉,韩文霞等. 上新世-第四纪亚洲内陆干旱化过程——柴达木中部鸭湖剖面孢粉和盐类化学指标证据. 第四纪研究,2008, 28 (5):874~882 Fang Xiaomin,Wu Fuli,Han Wenxia et al.Plio-Pleistocene drying process of Asian inland——Sporopollen and salinity records from Yahu section in the central Qaidam Basin. Quaternary Sciences, 2008, 28 (5):874~882
