[1] Zhang Lansheng,Fang Xiuqi,Ren Guoyu. Global Change[M]. Beijing:Higher Education Press,2001. 1-341.[张兰生,方修琦,任国玉. 全球变化[M]. 北京:高等教育出版社,2001.1-341.] [2] Cheng Hai. The mutation study of global climate:Argue or act?[J]. Chinese Science Bulletin,2004,49(13):1 339-1 344. [3] Schwartz P, Randall D. “Abrupt climate change,” report prepared by Global Business Network (GBN) for the Department of Defense[EB/OL]. http:∥www.gbn.org/ArticleDisplayServlet.srv?aid= 26231,2005. [4] Lyell C. Principles of Geology, Being An Attempt to Explain the Former Changes of the Earth's Surface by Reference to Causes Now in Operation[M].London: John Murray,1830. [5] Agassiz L. Tudes Sur Les Glaciers[M]. Neuch Tel:Privately Published, 1840. [6] Savin S. The history of the Earth's surface temperature during the past 100 million years[J]. Annual Reviews of Earth and Planetary Science,1977,5:318-355. [7] Savin S. Stable isotopes in climatic reconstructions[A]. In: Berger W H, Crowell J C ,eds. Climate in Earth History[C]. Washington:National Academy Press, 1982. 164-171. [8] Douglas R, Woodruff F. Deep sea benthic foraminifera[A]. In: Emiliani C ,ed. The Sea. Vol 7, The Oceanic Lithosphere[C]. New York: John Wiley, 1981.1 233-1 327. [9] Moore T C, Pisias N G, Keigwin L D. Cenozoic variability of oxygen isotopes in benthic foraminifera[A]. In: Berger W H, Crowell J C,eds. Climate in Earth History[C]. Washington:National Academy Press, 1982.172-181. [10] Miller K G, Fairbanks R G, Mountain G S. Tertiary oxygen isotope synthesis, sea level history, and continental margin erosion[J]. Paleoceanography,1987,2:1-19. [11] Wolfe J A. Tertiary climates and floristic relationships at high latitudes in the Northern Hemisphere [J]. Palaeogeogr Palaeoclimatol Palaeoecol,1980,30:313-323. [12] Wolfe J A, Poore R Z. Tertiary marine and non marine trends[A]. In: Berger W H, Crowell J C,eds. Climate in Earth History[C]. Washington:National Academy Press, 1982.154-158. [13] Wolfe J A. Climatic, floristic and vegetational changes near the Eocene Oligocene boundary in North America[A]. In: Prothero D R, Berggren W A,eds. Eocene Oligocene Climate and Biotic Evolution[C]. Princeton:Princeton University Press,1992.421-436. [14] Wolfe J A. Distribution of major vegetational types during the Tertiary[A]. In: Sundquist E T, Broecker W S,eds. The Carbon Cycle and Atmospheric CO2: Natural Variations Archaean to Present[C].Washington: American Geophysical Union, 1985. 357-375. [15] Heinrich H. Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130 000 years[J]. Quaternary Research, 1988, 29: 142-152. [16] Dansgaard W, Johnsen S J, Clausen H B, et al. Evidence for general instability of past climate from a 250 kyr ice core record[J]. Nature, 1993, 364: 218-220. [17] Bond G, Broecker W, Johnsen S, et al. Correlations between climate records from North Atlantic sediments and Greenland ice[J]. Nature, 1993, 365: 143 147. [18] Broecker W S, Andree W, Wolfi H, et al. The chronology of the last deglaciation: Implication to the cause of the Younger Dryas event[J]. Paleoceanography, 1988, 3: 1 19. [19] Pestiaux P, Mersch I V D, Berger A, et al. Paleocclimatic variability at frequencies ranging from 1 cycle per 10,000 years to 1 cycle per 1000 years: Evidence for nonlinear behavior of the Climate system[J]. Climate Change, 1988, 12: 9-13. [20] Keigwin L D, Jones G A, Lehman S J, et al. Deglacial meltwater discharge, North Atlantic deep circulation and abrupt climate change[J]. Journal of Geophysical Research, 1991, 96(C6): 16 811-16 826. [21] Hughen K A, Overpeck J T, Peterson L C, et al. Rapid climate changes in the tropical Atlantic region during the last deglaciation[J]. Nature, 1996, 380: 51-54. [22] Peterson L C, Haug G H, Hughen K A, et al. Rapid changes in the hydrologic cycle of the Tropical Atlantic during the Last Glacial[J]. Science, 2000, 290: 1 947 1-951. [23] Liu D S, Guo Z T. Geological environments in China and global change[A]. In: An Z S,ed. An Corpus of Liu Dongsheng[C].Beijing: Science Press, 1997.192-202. [24] Porter S C, An Z S. Correlation between climate events in the North Atlantic and China during the last glaciation[J]. Nature, 1995,375: 305-308. [25] Guo Z T, Liu T S, Fedoroff N, et al. Climate extremes in Loess of China coupled with the strength of deep water formation in the North Atlantic[J]. Global and Planetary Change, 1998, 18:113-128. [26] Thompson L G, Yao T D, Davis M E, et al. Tropical cimate instability: The last glacial cycle from a Qinghai Tibetan ice core[J]. Science,1997, 276: 1 821-1 825. [27] Thompson L G, Thompson M E, Sowers T A, et al. A 25000 year tropical climate history from Bolivian ice cores[J]. Science,1998, 282: 1 858-1 864.[28] Zachos J,Pagani M, Sloan L, et al. Trends, rhythms, and aberrations in global climate 65 Ma to present[J].Science,2001,292:686-699. [29] Tang Maocang, Zhu Deqin, Gao Xiaoqing. Review and prospect of the research of Earth system's evolution[J]. Advances in Earth Science,2004,19(1):55 62. [ 汤懋苍,朱德琴,高晓清. 地球系统演化原因研究的回顾与展望[J].地球科学进展,2004,19(1):55-62.] [30] Hay W W, Emanuel Soeding Robert M D,Christopher N W. The Late Cenozoic uplift climate change paradox [J]. International Journal of Earth Sciences,2002,91:746-774. [31] Ruddiman W F, Prell W L. Introduction to the uplift climate connection[A]. In: Ruddiman W F,ed. Tectonic Uplift and Climate Change[C]. New York:Plenum Press, 1997.3-15. [32] Raymo M E, Ruddiman W F. Tectonic forcing of late Cenozoic climate[J]. Nature,1992,359:117-122. [33] Li J J,Fang X M. Uplift of Tibetan Plateau and environmental Changes[J]. Chinese Science Bulletin, 1999,44(23):2 117-2 124. [34] Molnar P, England P. Late Cenozoic uplift of mountain ranges and global climate change: Chicken or egg?[J]. Nature,1990,346:29-34. [35] Ouyang Ziyuan,Wang Shijie,Xiao Zhifeng, et al. Palaeoenvironmental and palaeoclimate catastarophe induced by Cenozoic bolideimpact eventa [J].Quaternary Sciences,1995,(4):324-330.[欧阳自远,王世杰,肖志峰,等. 新生代地外物体撞击事件诱发的古气候环境灾变[J]. 第四纪研究,1995,(4):324-330.] [36] France Lanord C, Derry L. Organic carbon burial forcing of the carbon cycle from Himalayan erosion[J]. Nature,1997,390:65-67. [37] Quade J,Cerling T E,Brwman J R. Development of Asia monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan[J]. Nature,1989,342:162-166. [38] Shi Yafeng,Li Jijun,Li Bingyuan. Late Cenozoic Uplift of Tibetan Plateau and Environmental Changes[M]. Guangzhou:Guangdong Science and Technology Press,1998.[施雅风,李吉均,李炳元. 青藏高原晚新生代隆升与环境变化[M]. 广州:广东科学技术出版社,1998.] [39] Barron E J, Washington W M. The role of geographic variables in explaining paleoclimates: Results from Cretaceous climate model simulations[J]. Journal of Geophysical Research,1984,89:1 267- 1 279. [40] Tang Maocang, Guo Weidong. The great ice age cycles associated with the variation of the atmospheric heat engine efficiency[J] . Science in China ( D),1998 ,28 (3) :284-288.[汤懋苍,郭维栋.大冰期成因的大气热机效率变化说[J].中国科学D辑,1998 ,28 (3) :284-288.] [41] Schwarzacher W. The identification and analysis of stratification cycles[J]. Paleoceanography,1987,2:79-95. [42] Muller R A, MacDonald G J.〖KG1〗Glacial cycles and astronomical forcing[J]. Science,1997,277:215-218. [43] Chamberlin T C. An attempt to frame a working hypothesis of the cause of glacial periods on an atmospheric basis[J]. Journal of Geophysical Research,1899,7:545-787. [44] Broecker W S. The end of the present interglacial: How and when?[J]. Quaternary Science Reviews,1998, 17: 689-694. [45] Peter U C,Richard B A,David P. Northern hemisphere ice sheet influences on global climate change[J].Science,1999,286:1 104- 1 111. [46] Peter U C,Shawn J M,Garry K C,et al.Freshwater forcing of abrupt climate change during the last glaciation[J].Science,2001,299:283-287. [47] Pagani M, Arthur M A, Freeman K H. Miocene evolution of atmospheric carbon dioxide[J]. Paleoceanography,1999,14:273-292. [48] Pagani M, Freeman K H, Arthur M A. Miocene atmospheric CO2- levels and the expansion of C4 grasses[J]. Science,1999,285:876-879. [49] Pearson P N, Palmer M R. Declining atmospheric carbon dioxide in the last sixty million years[J]. Nature,2000,406:695 699. [50] Veizer J, Godderis Y, Franξois L M. Evidence for decoupling of atmospheric CO2 and global climate during the Phanerozoic eon[J]. Nature,2000,408:698-701. [51] EPICA Community Members. Eight glacial cycles from an Antarctic ice core[J].Nature,2004,429:623-628. [52] Clement A C, Cane M A, Seager R. An orbitally driven tropical source for abrupt climate change[J]. Journal of Climate, 2001, 14:2 369-2 375. [53] Stott L, Poulsen C, Lund S, et al. Super ENSO and global climate oscillations at millennial time scales[J]. Science, 2002, 297: 222-226. [54] Visser K, Thunell R, Stott L. Magnitude and timing of temperature change in the indo Pacific warm pool during deglaciation[J]. Nature,2003, 421: 152-155. [55] Friis C E,Lassen K. Length of the solar cycle: An indicator of solar activity closely associated with climate[J]. Science,1991,245:698. [56] Xu Jinghua. Sun,climate and nation's great migration[J]. Science in China(D),1998,28(4):365-384. [57] Tang Maocang, Liu Yanxiang,Guo Weidong. Climatic condition and Chinese history (1):SCL and Chinese climate[J]. Plateau Meteorlogy,2001,20(4):368-373.[汤懋苍,柳艳香,郭维栋. 天时、气候与中国历史上:黑子周长与中国气候[J]. 高原气象,2001,20(4):368-373.] [58] Gao Xiaoqing, Tang Mancang, Zhu Deqin. Some thoughts on climate system and earth system [J]. Chinese Journal of Geophysical, 2004 ,47(2) :364-368. [高晓清,汤懋苍,朱德琴. 关于气候系统与地球系统的若干思考[J].地球物理学报,2004 ,47(2) :364-368.] [59] Svensmark H. Cosmic rays and Earth’s climate[J]. Space Science Review,2000,93:155-166. [60] Marsh N, Svensmark H. Cosmic rays, clouds, and climate[J]. Space Science Review,2000,94:375-380. [61] Martin J H. Glacial interglacial CO2- change: The iron hypothesis[J]. Paleoceanography,1990,5:1-13. [62] Boyd P W, Watson A J, Law C S, et al. A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization[J]. Nature,2000,407:695-702. [63] Coale K H,Johnson K S, Stout P M, et al. A massive phytoplankton bloom induced by an ecosystem scale iron fertilization experiment in the equatorial Pacific Ocean[J]. Nature,1996,383:495-501. [64] Abraham E R,Law C S, Boyd P W, et al. Importance of stirring in the development of an iron fertilized phytoplankton bloom[J]. Nature,2000,407:727-730. [65] Watson A J, Bakker D C E, Ridgwell A J, et al. Effect of iron supply on Southern Ocean CO2- uptake and implications for glacial atmospheric CO2-[J]. Nature,2000,407:730-733. [66] Ridgwell A J, Maslin M A,Watson A J. Reduced effectiveness of terrestrial carbon sequestration due to an antagonistic response of ocean productivity[J]. Geophysical Research Letter,2002,29,10.1029/2001GL014304. [67] Zhuang Guoshun, Guo Jinghua, Yuan Hui, et al. Coupling and feedback between iron and sulphue in air sea exchange[J].Chinese Science Bulletin, 2003,48(11):1 080-1 086. [68] Fang Xiaomin,Han Yongxiang,Ma Jinghui,et al. Dust storms and loess accumulation on the Tibetan Plateau: A case study of dust event on 4 March 2003 in Lhasa[J]. Chinese Science Bulletin, 2004,49(9): 953-960. [69] Wu Guanjian, Yao Tandong, Thompson L G, et al. Microparticle record in the Guliya ice core and its comparison with polar records since the last interglacial[J]. Chinese Science Bulletin, 2004, 49(6): 607-611. [70] Thomas J C. Causes of climate change over the past 1000 years[J]. Science,2000,289:270-277. [71] Petit J R, Jouzel J, Raynaud, D, et al. Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica [J]. Nature, 1999,399:429-436. |