最近1.2Ma青藏高原的隆升与东亚地表各圈层的相互作用
|
摘要
地球系统科学是近年来地学研究的热点和趋势之一。地球各圈层间的相互作用是地球系统科学的核心和研究对象。新生代以来地球各圈层相互作用的研究表明，构造运动是各圈层相互作用中的一个重要因素，对地球各圈层相互作用的研究往往是以构造运动作为切入点的。
青藏高原隆升是新生代地质历史上最为重要的构造运动事件，对全球环境变化起着重要的作用。青藏高原隆升过程及其资源环境效应一直是国内外地学界研究的热点问题。青藏高原及其周缘地区是地球表层各圈层相互作用研究的天然实验场。为了深入的认识高原隆升及其环境效应，我们选择了最近1.2Ma以来青藏高原的构造运动及其对东亚地区(主要是我国)环境的影响来探讨地球表层各圈层之间的相互联系。
结合前人的工作和我们最近对青藏高原东缘渭河阶地发育的研究，对最近1.2Ma以来青藏高原的隆升过程进行了一个系统的初步总结。高原最近1.2Ma以来的隆升过程主要经过了“昆黄运动”和“共和运动”。这两次构造运动对东亚地表的其他圈层产生了重要的影响。其中，“昆黄运动”历时较长，可以分为三个亚阶段，分别发生在1.2—1.1Ma，0.9—0.8Ma和0.6Ma。渭河上游河流阶地上覆黄土的磁性地层学研究表明渭河在1.0和0.8Ma发生了强烈下切。从这两级阶地的组成特征，及其和“昆黄运动”的第二阶段存在着时间上的良好吻合等特征，我们认为，渭河上游此时的河流下切代表的地表抬升过程是青藏高原“昆黄运动”在西秦岭地区的区域响应。
对青藏高原东北边缘的祁连山东段中路剖面磁组构的研究是我们进行古大气环流重建研究的工作重点。古风向的代用指标研究显示：1.4Ma以来，祁连山东段地区的古风向存在两个重要的转变时期：一是0.78Ma左右，该区地面主导风向由此前的NW—SE向W—E方向转变；二是古土壤S5(0.5Ma)之后，地面主导风向转为NE—SW。这两次风向的转变和高原在中更新世以来的隆升及全球性的气候变化事件在时间上具有良好的耦合性。这种近地面大气环流的变化很可能是高原隆升和／或气候变化的产物。同时，我们对沙沟剖面的磁组构参数研究揭示出：在西北内陆干旱—半干旱条件下，黄土磁化率指标“失灵”，而受强烈冬季风影响的磁化率各向异性参数(尤其是各向异性度P)却可以较为灵敏的记录环境变化的重要信息。区域和全球气候变化的重要信息都被记录在磁组构参数的变化当中，如250ka区域的强烈干冷化事件和MIS16阶段全球
During past decades, the development of earth science indicates that the environmental conditions of earth, including the climate, are determined by physical, chemical, biological, and human interactions that transform and transport materials and energy. Investigations on the interaction or mechanism between these multiple components of the earth system became a hot issue of geosciences field. The tectonic movement/uplift of the lithosphere, as discussed in many investigations, controlled the global environmental change during the whole Cenozoic period on the 10~5-10~7 years time scale. Given this discussion, the tectonic movement/uplift of lithosphere provides a good opportunity for the research of interaction between the complex earth system components. Specifically, our efforts are paid to the recent 1.2Ma when the environment in China changed dramatically. First, also the dominant change of Chinese environment since 1.2Ma B.P. is the tectonic uplift of the Tibetan Plateau (TP). Hence, this lithosphere change is proved to be the trigger and amplifier of the whole system by previous investigations. However, the advance and detail research are limited.
Well situated at the eastern margin of the Tibetan Plateau, the geomorphology evolvement of the Weihe River is a promising evidence to record the tectonic uplift events of the TP. The magnetostragraphy study of loess deposited on the river terrace indicated that there were at least two dramatic down-cutting events in the Longxi Basin during 1.0-0.8Ma. The analysis of river terrace characters and the temporal coincidence of records in other regions confirm our proposal that these two down-cutting events of Weihe River are tectonic driven. Integrated our results with other intensively studied records in and around the Tibetan Plateau from 1.2Ma; we suggest two tectonic uplift stages of TP with the first one during 1.2-0.6Ma and the second one during 0.2-0.15Ma. Moreover, the first stage can be divided into three sub-stages: l)1.2-1.1Ma, characterized by the down-cutting of the Yellow river in Jishi Gorge, 2)0.9-0.8Ma, the main phase of the tectonic uplift, and 3) 0.6Ma.
Before attempting a systematic discussion of the interactions between lithosphere, atmosphere, hydrosphere, and biosphere of China, the evolution of every sphere since 1.2Ma are considered. The magnetic fabric-based reconstruction of paleowind direction in the northeastern flank of Qilian Mountains reveals the near surface air circulation changes, which are dictated by the East Asian Monsoon, in ~0.78Ma (from NW-SE to W-E) and 0.5Ma (a NE-SW dominant direction established). Time of the first paleowind direction change is temporal related to the end time of the major tectonic uplift of TP casually, which may suggest the affection of tectonic uplift on the atmospheric circulation. Studies on the loess magnetic fabric and magnetic susceptibility (MS) in semi-arid region, such as northeastern flank of Qilian Mountains,
青藏高原隆升是新生代地质历史上最为重要的构造运动事件，对全球环境变化起着重要的作用。青藏高原隆升过程及其资源环境效应一直是国内外地学界研究的热点问题。青藏高原及其周缘地区是地球表层各圈层相互作用研究的天然实验场。为了深入的认识高原隆升及其环境效应，我们选择了最近1.2Ma以来青藏高原的构造运动及其对东亚地区(主要是我国)环境的影响来探讨地球表层各圈层之间的相互联系。
结合前人的工作和我们最近对青藏高原东缘渭河阶地发育的研究，对最近1.2Ma以来青藏高原的隆升过程进行了一个系统的初步总结。高原最近1.2Ma以来的隆升过程主要经过了“昆黄运动”和“共和运动”。这两次构造运动对东亚地表的其他圈层产生了重要的影响。其中，“昆黄运动”历时较长，可以分为三个亚阶段，分别发生在1.2—1.1Ma，0.9—0.8Ma和0.6Ma。渭河上游河流阶地上覆黄土的磁性地层学研究表明渭河在1.0和0.8Ma发生了强烈下切。从这两级阶地的组成特征，及其和“昆黄运动”的第二阶段存在着时间上的良好吻合等特征，我们认为，渭河上游此时的河流下切代表的地表抬升过程是青藏高原“昆黄运动”在西秦岭地区的区域响应。
对青藏高原东北边缘的祁连山东段中路剖面磁组构的研究是我们进行古大气环流重建研究的工作重点。古风向的代用指标研究显示：1.4Ma以来，祁连山东段地区的古风向存在两个重要的转变时期：一是0.78Ma左右，该区地面主导风向由此前的NW—SE向W—E方向转变；二是古土壤S5(0.5Ma)之后，地面主导风向转为NE—SW。这两次风向的转变和高原在中更新世以来的隆升及全球性的气候变化事件在时间上具有良好的耦合性。这种近地面大气环流的变化很可能是高原隆升和／或气候变化的产物。同时，我们对沙沟剖面的磁组构参数研究揭示出：在西北内陆干旱—半干旱条件下，黄土磁化率指标“失灵”，而受强烈冬季风影响的磁化率各向异性参数(尤其是各向异性度P)却可以较为灵敏的记录环境变化的重要信息。区域和全球气候变化的重要信息都被记录在磁组构参数的变化当中，如250ka区域的强烈干冷化事件和MIS16阶段全球
During past decades, the development of earth science indicates that the environmental conditions of earth, including the climate, are determined by physical, chemical, biological, and human interactions that transform and transport materials and energy. Investigations on the interaction or mechanism between these multiple components of the earth system became a hot issue of geosciences field. The tectonic movement/uplift of the lithosphere, as discussed in many investigations, controlled the global environmental change during the whole Cenozoic period on the 10~5-10~7 years time scale. Given this discussion, the tectonic movement/uplift of lithosphere provides a good opportunity for the research of interaction between the complex earth system components. Specifically, our efforts are paid to the recent 1.2Ma when the environment in China changed dramatically. First, also the dominant change of Chinese environment since 1.2Ma B.P. is the tectonic uplift of the Tibetan Plateau (TP). Hence, this lithosphere change is proved to be the trigger and amplifier of the whole system by previous investigations. However, the advance and detail research are limited.
Well situated at the eastern margin of the Tibetan Plateau, the geomorphology evolvement of the Weihe River is a promising evidence to record the tectonic uplift events of the TP. The magnetostragraphy study of loess deposited on the river terrace indicated that there were at least two dramatic down-cutting events in the Longxi Basin during 1.0-0.8Ma. The analysis of river terrace characters and the temporal coincidence of records in other regions confirm our proposal that these two down-cutting events of Weihe River are tectonic driven. Integrated our results with other intensively studied records in and around the Tibetan Plateau from 1.2Ma; we suggest two tectonic uplift stages of TP with the first one during 1.2-0.6Ma and the second one during 0.2-0.15Ma. Moreover, the first stage can be divided into three sub-stages: l)1.2-1.1Ma, characterized by the down-cutting of the Yellow river in Jishi Gorge, 2)0.9-0.8Ma, the main phase of the tectonic uplift, and 3) 0.6Ma.
Before attempting a systematic discussion of the interactions between lithosphere, atmosphere, hydrosphere, and biosphere of China, the evolution of every sphere since 1.2Ma are considered. The magnetic fabric-based reconstruction of paleowind direction in the northeastern flank of Qilian Mountains reveals the near surface air circulation changes, which are dictated by the East Asian Monsoon, in ~0.78Ma (from NW-SE to W-E) and 0.5Ma (a NE-SW dominant direction established). Time of the first paleowind direction change is temporal related to the end time of the major tectonic uplift of TP casually, which may suggest the affection of tectonic uplift on the atmospheric circulation. Studies on the loess magnetic fabric and magnetic susceptibility (MS) in semi-arid region, such as northeastern flank of Qilian Mountains,
引文
1. Albrecht, B. Aerosols, cloud microphysics, and fractional cloudiness. Science, 1989 (245): 1227-1230.
2. Alley R. B, Lawson D. E, Evenson. G. J et al. Stabilizing feedbacks in glacial-bed erosion. Nature, 2003, 424:758-760
3. An Z S, Kukla G, Porter S C, et al. Late Quaternary dust flow on the Chinese Loess Plateau. Catena, 1991, 18: 125-132
4. An zhisheng, John.E.Kutzbach. Warren.Prell et el. Evolution of Asian monsoons and Phased uplift of the Himalaya-Tibetan Plateau since late Miocene times. Nature, 2001,411: 62-66
5. Andrew S. Ackerman, Michael P. Kirkpatrick, David E. Stevens et al. The impact of humidity above stratiform clouds on indirect aerosol climate forcing. Nature, 2004, 432(23/30): 1014-1017
6. Atbogast, Alan F., Daniel R. Muhs, Geochemical and mineralogical evidence from eolian sediments for northwesterly mid-Holocene paleowinds, central Kansas, USA Quaternary International, 2000, 67:107-118
7. Ashkenazy, Yosef Eli Tziperman. Are the 41kyr glacial oscillations a linear response to Milankovitch forcing? Quaternary Science Review, 2004, 23 1879-1890
8. Bains, Santo Richard D. Norris, Richard M. Corfield et al Termination of global warmth at the Palaeocen/Eocene boundary through productivity feedback. Nature, 2000, 407:171-173
9. Balsama W, Junfeng Ji, Jun Chen. Climatic interpretation of the Lunchuan and Lingtai loess sections, China, based on changing iron oxide mineralogy and magnetic susceptibility. Earth and Planetary Research Letters, 2004, 223:335-348
10. Barry, Leon George C, Craig, John Thuburn, Poleward heat transport by the atmospheric heat caging. Nature, 2002, 415:774—777
11. Becquey Sabine, Rainer Gersonde Past hydrographic and climatic changes in the Subantarctic Zone of the South Atlantic -The Pleistocene record from ODP Site 1090 Palaeogeography, Palaeoclimatology, Palaeoecology, 2002,182: 221-239
12. Ben, Richards W.M. Luminescence dating of Quaternary sediments in the Himalaya and High Asia: a practical guide to its use and limitations for constraining the timing of glaciation. Quaternary International, 2000, 65/66:49-61
13. Benn, Douglas Ⅰ, Lewis A. Owen Himalayan glacial sedimentary environments: a framework for reconstructing and dating the former extent of glaciers in high mountains. Quatemery International, 2002, 97/98:3-25
14. Berger, X.S.Li M.F.loutre. Modelling Northern Hemisphere ice volume over the last 3 Ma. Quaternary science review. 1999, 18:1-11
15. Berner, Robert A. Elizabeth K. Berner. Silicate weathering and climate, in:W.F.Ruddiman(Ed.),Tectonic Uplift and Climate Change, Plenum, New York Press, NY, 1997:353-365
16. Bettis, E. Arthur, Daniel R. Muhs, Helen M. Roberts. Last Glacial loess in the conterminous USA. Quaternary Science Reviews 2003, 22:1907-1946
17. Bice, Karen L. Christopher R. Scotese, Dan Seidov, Quantifying the role of geographic change in Cenozoic ocean heat transport using uncoupled atmosphere and ocean models Palaeogeography, Palacoclimatology, Palaeoecology, 2000, 161:295-310
18. Bush, A.B.G, A comparison of simulated monsoon circulations and snow accumulation in Asia during the mid-Holocene and at the Last Glacial Maximum. Global and Planetary Change, 2002. 32:331-347.
19. Bush, A.B.G, Apositive climatic feedback mechanism for Himalayan glaciation. Quaternary International, 2000, 65166, 3-13.
20. Cande, S.C., Kent, D.V., Revised calibration of the geomagnetic polarity timeacales for the late cretaceous and Cenozoic, J. Geophys. Res (D), 1995, (100): 603-609
21. Cane, Mark A, Peter Moiner, Closing of the Indonesian seaway as a precursor to east African aridification mound 3-4 million yeats ago. Nature, 2001, 411: 157-162
22. Carmala N Garzione, David L. Dettman, Jay Quade et al. High times on the Tibetan plateau: Paleoelevation of the Thakkhola graben, Nepal. Geology, 2000, 28 (4): 339-342
23. Chen F H. High-resolution multi-proxy climate records from Chinese loess: evidence for rapid climate changes over the last 75 kyr (J). Paleogeography Paleoclimatology Paleoecology, 1997, 130:323—335
24. Christensen, B.A., J.L. Kalbas, M. Maslin. Paleoclimatic changes in southern Africa during the intensification of Northern Hemisphere glaciation: evidence from ODP Leg 175 Site 1085 Marine. Geology, 2002,180:117-131
25. Clark, Peter U. Richard B. Alley, David Pollard. Northern Hemisphere Ice-Sheet Influences on Global Climate Change Science, 2000, 286:1104-1111
26. Clifford S. Riebe, James W. Kirchner, Darryl E. Granger et al. Strong tectonic and week climatic control of long-term chemical weathering rates. Geology,2001, 29(6): 511-514
27. Crowley, Thomas J. Cycles, Cycles Everywhere, Science, 2002, 295:1473-1474
28. Cui Zhijiu, Chienfu Yang, Gengnian Liu. The Quaternary glaciation of Shesan Mountain in Taiwan and glacial classification in monsoon areas. Quaternary International, 2002, 97/98:147-153
29. Dansgaard, W. S J. Johnsen, H B. Clausen. Evidence for general instability of past climate from a 250-kyr ice-core record. Nature, 1993, 364:218-220
30. DeConto, Robert M. David Pollard, Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO_2. Nature, 2003, 421: 245-249
31. Derbyshire, Edward Loess and the Dust Indicators and Records of Terrestrial and Marine Palaeoenvironments (DIRTMAP) database. Quaternary Science Reviews, 2003, 22:1813-1819
32. Derry, L. A., France-Lanord., Neogene Himalaya weathering history and river ~(87)Sr/~(86)Sr: impact on the marine Sr record. Earth and Planetary Science Letters, 1996, 142:59-74
33. Ding, Z L Derbyshire, S. L. Yang et al, Stacked 2.6-Ma grain size record from the Chinese Loess based on five section and correlation with deep-sea δ~(18)O record, Paleoceangraphy, 2002, 17 (3): 5-1 5-21
34. Ding, Z. L. J. M. Sun, S. L. Yang. Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change. Geochimica et Cosmochimica Acta, 2001, 65 (6): 901-913
35. Elkibbi, Maya Jose A. Rial, An outsider's review of the astronomical theory of the climate: is the eccentricity-driven insolation the main driver of the ice ages? Earth-Science Reviews, 2001, 56:161-177
36. EPICA community members, Eight glacial cycles from an Antarctic ice core. Nature, 2004, 429:623-628
37. Fang, Xiao-Ming Ji-jun Li, Rob Van der Voo. Rock magnetic and grain size evidence for intensified Asian atmospheric circulation since 800,000 years B.P. related to Tibetan uplift. Earth and Planetary Science letters,1999,165:129-144
38. Feng Z.-D, P. Khosbayar Paleosubarctic Eolian environments along the southern margin of the North American Icesheet and the southern margin of Siberia during the Last Glacial Maximum. Palaeogeography, Palaeoclimatology, Palaeoecology. 2004, 212:265- 275
39. Flynn, John J. Michael J. Novacekc, Holly E. Dodson. A new fossil mammal assemblage from the southern Chilean Andes: implications for geology, geochronology, and tectonics. Journal of South American Earth Sciences, 2002:1-18
40. Getty, Stephen R. Yemane A.Smerom, Terrence M.Quinn. Accelerated Pleistocene coral extinction in the Caribbean Basin shown by uranium-lead (U-Pb) dating. Geology, 2001, 29(7): 639-642
41. Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 2002, 416:159～163
42. Guyodo, Yohan Jean-Pierre Valte. Global changes in intensity of the earth's magnetic field during the past 800kyr. Nature, 1999, 399:249-252
43. Handy, R L, Loess distribution by variable winds. Geological Society of American Bulletin, 1976, 87:915-92744. Hang, Gerald H. Andrey Ganopolski, Daniel M. Sigman et al, North Pacific seasonality and the glaciation of North America 2.7 million years ago. Nature, 2005, 433, 821-825
45. Hays, J. D. Variations in Earth's orbit: Pace-maker of Ice Ages. Science,1976, 194:1121
46. Heller, F, liu,T.s. Magnetostratigralhical dating of loess deposits in China. Nature, 1982, 300:431-433
47. Henrich, Ru.diger Karl-Heinz Baumann, Robert Huber. Carbonate preservation records of the past 3 Myr in the Norwegian-Greenland Sea and the northern North Atlantic: implications for the history of NADW production Marine Geology. 2002, 184:17-39
48. Henrik Svensen, Sverre Planke, Anders Malthe-Sφrenssenl, Release of methane from a volcanic basin as a mechanism for initial Eocene global warming nature, 2004, 429:542-545
49. Heslop, D. Langereis. C.G. Dokkers. M.J. a new astronomical timescale for the loess deposition of Northern China. Earth and Planetary Science Letters. 2000,184:125-139
50. Heslop, D., M.J. Dekkers, C.G. Langereis Timing and structure of the mid-Pleistocene transition: records from the loess deposits of northern China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 185:133-143
51. Hess S, Wolfgang, Kuhnt. Neogene and Quaternary paleocenography changes in the southern South China Sea (site 1143): the benthic foraminiferal record. Marine Micropaleontology, 2005, 54:63-87
52. Hopkinson, Charles S. Jr & Joseph J. Vallino. Efficient export of carbon to the deep ocean through dissolved organic matter. Nature, 2005, 433(13): 142-145
53. Hu, Xiaomeng Youli Li, Jinchun Yang. Quaternary Paleolake development in the Fen River Basin, North China. Geomorphology, 2005, 65:1-13
54. Hunt, C. P., S. K. Banerjee, J. M. Hart, P. A. Solheid, E. Oches, W. W. Sun, and T. S. Liu, Rock magnetic proxies of climate changes in the loess-paleosol sequences of the western Loess Plateau of China, Geophys. J. Int., 1995, 123: 232-244
55. Joseph L. H., Rea D. K., Ben A.van der Pluijm. use of grain size and magnetic fabric analyses to distinguish among depositional environments. Paleoceanography, 1998, 13(5): 491-501
56. Kashiwaya, K., Ochial, S., Sakai, H. & Kawai, T. Orbit-related long-term climate cycles revealed in a 12-Myr continental record from Lake Baikal. Nature, 2001, 410: 71-74.
57. Kathryn M. Gregory., Wodzicki, A late Miocene subtropical-dry flora from the northern Altiplano, Bolivia. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 180:331-348
58. Kathryn M. Gregory-Wodziciki, Uplift history of the Central and Northern Andes: A review. Geological Society of American Bulletin. 2000, 112 (7): 1091-1105
59. Kent D.V., Opdyke, N. D., Ewing. M., Climate change in the North Pacific using ice-rafted detritus as a climatic indicator. Geological Society of American Bulletin, 1971, 82:2741-2754
60. Kent D.V., Rio D., Massari F et al., Emergence of Veince during the Pleistocene. Quaternary Science Review, 2002, 21: 1719-1727
61. Kerich, D M. K.Caldeira. Was the Himalayan orogen a climatically significant coupled source and sink for atmospheric CO2 during the Cenozonic? Earth and Planetary science letters, 1999, 173:195-203
62. Kohfeld, K.E S.P. Harrison. Glacial-interglacial changes in dust deposition on the Chinese Loess Plateau. Quaternary Science Review, 2003, 22:1859-1878
63. Kukla, G, Heiler, F, Liu, X.M,. Pleistocene climates in China dated by magnetic susceptibility. Geology, 1988, 16: 811-814.
64. Kump, Lee.R. Reducing uncertainty about carbon dioxide as a climate driver. Nature, 2002, 419:188-190
65. Kutzbach, J.E. Prell, W. L., Ruddiman, W. F. Sensitivity of Eurasian climate to surface uplift of the Tibetan Plateau. Journal of Geology. 1993, 101:177-190
66. Kutzbach, J.E., Guetter, P. J., Ruddiman, W. F., et al. Sensitivity of climate to late Cenozoic uplift in southern Asia and the American West: numerical experiments. Journal of Geophysical Research, 1989, 94:18,393-18,407
67. Lacis, Tegen I, A.A., Fung, I.,. The infuence on climate forcing of mineral aerosols from disturbed soils. Nature, 1996, 380: 419-422.
68. Lagriox, F, and S. K. Banerjee, Paleowind directions from the magnetic fabric if loess profiles in central Alaska. Earth Planet. Sci. Lett., 2002, 195: 99-112.
69. Lagriox, F, and S. K. Banerjee. The regional and temporal significance of primary Aeolian magnetic fabric preserved in Alaskan loess. Earth Planet. Sci. Lett, 2004, 225: 379-395
70. Lamb, Simon Paul Davis. Cenozoic climate change as a possible cause for the rise of the Andes. Nature, 2003, 425: 792-797
71. Lavier, Luc L Michael S.Steckler Frederic Brigaud. Climatic and tectonic control on the Cenozoic evolution of the western Africa Margin. Marine Geology, 2001,178:63-80
72. Li Ji jun, Shiyou Xie, Mingsheng Kuang. Geomorphic evolution of the Yangtze Gorges and the time of their formation. Geomorphology, 2001, 41: 125-135
73. Li Jijun. The environmental effects of the uplift of the Qinghai—Xizang Plateau. Quaternary Science Reviews, 1991, 10: 4792 483.
74. Liu Qingsong,- Subir. K. Banerjee. Michael. J. Jackson et al. Iner-profile correlation of the Chinese loess/paleosol sequences during Marine Oxygen Isotope Stage 5 and indications of pedogenesis. Quaternary Science Review, 2005, 24:195-210
75. Liu X M, Xu.T.C, Liu, T.S, The Chinese loess in Xifeng. II .A study of anisotropy of magnetic susceptibility of loess from Xifeng. Geophysics.J, 1988, 92: 349-353
76. Liu, Xiuming Tim Rolph, Zhisheng An et al. paoleoclimatic significance of magnetic properties on the Red clay underlying the loess and paleosols in China. Paleogeography paleoclimatology, paleoecology, 2003,199: 153-166
77. Maher, Barbara. A., Roy Thompson. Mineral magnetic record of the Chinese loess and paleosols. Geology, 1991, 19: 3-6
78. Manabe, Syukuro Ronald J. Stouffer. Simulation of abrupt climate change induced by freshwater input to the North Atlantic Ocean. Nature, 1995,378:165-167
79. Manabe, Syukuro Theodore B. Terpstra. The effect of mountains on the general circulation of the atmosphere as identified by numerical experiments. Journal of the atmosphere sciences, 1974, 31 (1): 3-41
80. Marincovich, Louie Andrey Yu. Gladenkov. Evidence for an early opening of the Bering Strait. Nature, 1999, 397: 149-151
81. Mason., J.A, E A Natter, H.C. Hobbs. Transport direction of Wisconsin Loess in southeastern Minnesota. Quaternary Research, 1994, 41: 44-51
82. Matalucci R. V., Shelton J. W., and Abdel-Hady M., Grain orientation in Vicksburg loess. Journal of sedimentary petrology, 1969, 39(3): 969-979
83. Miao, Xiaodong Youbin Sun, Huayu Lu et al, Spatial pattern of grain size in the Late Pliocene 'Red Clay' deposits (North China) indicates transport by low-level northerly winds. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004,206: 149-155
84. Mittoni, Giovanni,. Cipriano. Carcano, Eduardo. Garzanti et al, Onset of major Pleistocene glacialtions in the Alps. Geological Society of America, 2003, 31(11):989-992
85. Moberg. A, Dmitry M. Sonechkin, Karin Holmgren. Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature, 2005,433:613-617
86. Nikki M, White, M. Pringle, E. Garzanti et al. Constraints on the exhumation and erosion of the High Himalayan Slab, NW India, from foreland basin deposits. Earth and Planetary Science Letters, 2002,195: 29-44
87. North Greeland Ice Core Project Members. High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature, 2004,431:147-151
88. Owen, Lewis A. Robert C. Finkel, Patrick L. Barnard. Climatic and topographic controls on the style and timing of Late Quaternary glaciation throughout Tibet and the Himalaya defined by ~(10)Be cosmogenic radionuclide surface exposure dating. Quaternary Science Review, 2004,
89. Pearson, Paul N, Martin R, Palmer. Atmospheric carbon dioxide concentration over the past 60 million years. Nature, 2000, 406:696-699
90. Petit, J.R., Briat, M., Royer, A., Ice age aerosol content from east Antarctic ice core samples and past wind strength. Nature, 1981, 293: 391-394.
91. Pickart R. S. Spall M. A, Ribergaard M. H et al. Deep convection in the Irminger sea forced by the greeland tip jet. Nature, 2003, 424:152-156
92. Pincus, R, Baker, M. B. Effect of precipitation on the albedo susceptibility of clouds in the marine boundary layer. Nature, 1994(372): 250-252
93. Porter, Stephen C An Zhisheng. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature, 1995, 375:305-308.
94. Prell, W.L, Kutzbach, J.F,. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution. Nature, 1992, 360: 647-652.
95. Quade, J Cerling T,E, Bowman J, R. Development of Asian monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan, Nature, 1989, 342:163-166
96. Quade, Jay Louis Roe, Peter G. DeCelles, Tank P. Ojha. The Late Neogene ~(87)Sr/~(86)Sr Record of Lowland Himalayan Rivers. Science, 1997, 276:1828-1831
97. Ramos, Victor A. E.O. Cristallini, Daniel J. Perez. The Pampe, an flat-slab of the Central Andes. Journal of south American Earth Science, 2002, 15:59-78
98. Raymo, M.E. Glacial puzzles, science, 1998,281:1467-1468
99. Raymo, M.E. Kerim Nisancioglu. the 41 kyr world: Milankovitch's other unsolved mystery, paleoceanography, 2003, 18(1):11-1-11-6
100. Raymo, M.E. The initiation of North Hemisphere Glaciation. Annu tee.Earth Planet Sci. 1994, 23:353-383
101. Raymo, M.E. W E Ruddiman. Tectonic forcing of late Cenozoic climate. Nature, 1992,359:117-122
102. Raymo, M.E. W.F.Ruddiman, P.N.Froelich. Influence of late Cenozoic mountain building on Ocean geochemical Cycles. Geology, 1988,16:649-653
103. Reguero, Marcelo A. Sergio A. Marenssi, Serglo N. Santillana Antarctic Peninsula and South America (Patagonia) Paleogene terrestrial faunas and environments: biogeographic relationships. Palaeogeography, Palaeoclimatoiogy, Palaeoecology, 2002, 179:189-210
104. Ruddiman, W F Kutzbuch J.E. Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and the American west. Journal of geophysical Research, 1998, 94:18409-18427
105. Ruddiman, W.F. (Ed.), Tectonic Uplift and Climate Change. Plenum, New York Press, NY, 1997.
106. Ruddiman, W.F. M.E. Raymo, D.G. Martinson, B.M. Clement, and J. Backman. Pleistocenen evolution: Northern hemisphere ice sheet and North Atlantic Ocean. Paleoceangraphy, 1989, 4(4): 353-412
107. Ruddiman, William F. Maureen E. Raymo A methane-based time scale for Vostok ice. Quaternary Science Reviews, 2002:1-15
108. Rutherfor, Scott Steven D'Hondt. Early onset and tropical forcing of 100,000- year Pleistocene glacial cycles. Name, 2000:72-74
109. Sangode, S. J. Rohtash Kumar and Sumit K. Ghosh. Application of magnetic fabric studies in anancient fluvial sequence of NW Himalaya. Current Science, 2001, 81 (1): 66-71
110. Schafer, Jorg M. Silvio Tschudi, Zhizhong Zhao. The limited in(?)uence of glaciations in Tibet on global climate over the past 170 000 yr. Earth and Planetary Science Letters, 2002, 194:287-297
111. Schefu, E., Schouton, S., Fred Jansen, J. H. African vegetation controlled by tropical sea surface temperatures in the mid-Pleistocene period. Nature, 2003,422:418-421
112. Schmieder, Frank, Tilo von Dobeneck, Ulrich Bleil. The Mid-Pleistocene climate transition as documented in the deep South Atlantic Ocean: initiation, interim state and terminal event. Earth and Planetary Science Letters, 2000, 179: 539-549
113. Schmittner A. Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation. Nature, 2005,434: 628-633
114. Shackleton N.J The 100,000 ice age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity. Science, 2000, 289: 1897-1902
115. Shackleton, Nicholas John. Neil D Opdyke. Oxygen isotope and palaeomagnetic stratigraphy of Equatorial pacific core v28-238: oxygen isotope temperature and ice volume on a 10~5 year and 10~6 year scale. Quaternary research, 1973,3: 39-55
116. Shi, Y, Ge, Y, Xiaodong, L, Bingyuan, L, Tandong, Y,.Reconstruction of the 30-40 ka B.P. enhanced Indian monsoon climate based on geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 169: 69-83
117. Silva, P.F. F.O. Marques, J.M. Miranda et al. Anisotropy of magnetic susceptibility constraints on Variscan obduction processes in the Braganc, a Massif (NE Portugal). Tectonophysics, 2001,341:95-119
118. Stainforthl, D. A. T.Ainal, C. Christensen. Uncertainty in predictions of the climate response to rising levels of greenhouse gases. Nature, 2005,433(27): 403-406
119. Sun J M, Liu T S. Stratigraphic Evidence for the Uplift of the Tibetan plateau between～1.1 and～0.9 myr ago. Quaternary Research, 2000, 54: 309-320
120. Sun Jimin, Tungsheng Liu. Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments. Earth and Planetary Science Letters. 2000, 180: 287-296
121. Sun Jimin. Source Regions and Formation of the Loess Sediments on the High Mountain Regions of Northwestern China. Quaternary Research, 2002, 58: 341-351
122. Sun jimin, Zhongli Ding, Tungsheng Liu. 580,000-year environmental reconstruction from aeolian deposits at the Mu Us Desert margin, China. Quaternary Science Review, 1999,18: 1351-1364
123. Thibault de Garklel-Thoron, Yair Rosenthall, Franck Bassinot et al. Stable sea surface temperatures in the western Pacific warm pool over the past 1.75million years. Nature, 2005, 433(20): 294-298
124. Tilman, Rost Karl Pleistocene paleoenvironmental changes in the high mountain ranges of central China and adjacent regions. Quaternary International, 2000,65/66: 147-160
125. Treguer, Paul Philippe Pondaven. Silica control of carbon dioxide. Nature, 2002,406:358-359
126. Venz, Kathryn A. David A. Hodell. New evidence for changes in Plio—Pleistocene deep water circulation from Southern Ocean ODP Leg 177 Site 1090. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 182: 197-220
127. Visser, Katherine Robert Thunell, Lowell Stott. Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation. Nature, 2003, 421: 152-155
128. Wallmann, K. et al Controls on the Cretaceous and Cenozoic evolution of seawater composition, atmospheric CO2 and climate. Cosmochimica Acta, 2001,65 (18): 3005-3025,
129. Wang Pinxian, Steven Clemens, Luc Beaufort. Evolution and variability of the Asian monsoon system: state of the art and outstanding issues. Quaternary Science Reviews, 2005, 24: 595-629
130. Wehausen, Rolf Hans-Ju.rgen Brumsack. Astronomical forcing of the East Asian monsoon mirrored by the composition of Pliocene South China Sea sediments, Earth and Planetary Science Letters, 2000, 201: 621-636
131. Winckler, Giaela, Robert F. Anderson, Martin Stute and Peter Schlosser. Does interplanetary dust control 100kyr glacial cycles? Quaternary Science Review, 2004,23: 1873-1878
132. Wood, Richard A. Ann B. Keen, John F. B. Mitchell Changing spatial structure of the thermohaline circulation in response to atmospheric CO_2 forcing in a climate model. Nature, 1999, 399:572-575
133. Wu, Guangjian, Baotian Pan, Qingyu Guan, Dunsheng Xia. Terminations and their correlation with solar insolation in the Northern Hemisphere: a record from a loess section in Northwest China. Palaeogcography, Palaeoclimatology, Palaenecology, 2005, 216: 267-277
134. Yamazaki, Toshitsugu Hirokuni Oda. Oribtal influence on earth's magnetic field: 100,000-year periodicity in inclination. Science, 2002, 295:2435-2438
135. Yokokawa, M., and S. O. Franz. Changes in grain size and magnetic fabric at Blake-Bahama outer ridge during the late Pleistocene (marine isotope stages 8-10). Marine Geology, 2002, 189: 123-144.
136. Zachos, James Mark Pagani, Lisa Sloan et al. Trends. Rhythms and aberration in global climate 65 Ma to present. Science, 2001, 292:686-693
137. Zhang Peizhen, Peter Molnar, William R. Downs.Increased sedimentation rates and grain sizes 2±4 Myr ago due to the infuence of climate change on erosion rates. Nature, 2001, 410:891-897
138. Zhang, X. Y, R. Arimoto, and Z. S. An. Glacial and interglacial patterns for Asian dust transport, Quaternary Science Review, 1999, 18: 811-819.
139. Zhang, Xian Y. R. Arimoto, Zhi S. An. Glacial and interglacial patterns for Asian dust transport. Quaternary Science Review, 1999,18:811-819
140. Zhao, H., Moore, G.W.K., on the relationship between Tibetan snow cover, the Tibetan plateau monsoon and the Indian summer monsoon. Geophysical Research Letters, 2004, 31:14-20
141. Zheng, Hongbo Christopher McAulay.Powell, Zhisheng An et al. Uplift of the northern Tibetan plateau. Geology, 2000,28(8): 715-718
142. Zhou Shangzhe, Jijun Li, Shiqiang Zhang. Quaternary glaciation of the Ballang River Valley, Qilian Shan. Quaternary International, 2002, 97/98:103-110
143. Zhou, L.P, Oldfield, F., Wintle, A.G., Robinson, S.G., Wang, J.T. Partly pedogenic origin of magnetic variations in Chinese loess. Nature, 1990, 36: 737-739.
144. Zhu R X. History of anisotropy of the magnetic susceptibility and its implications: preliminary results along an E-W transect of the Chinese loess plateau. Geophysics Research Abs, 2000, 2:226
145. Zhu, R. X, Q. S. Liu, and M. J. Jackson, Palenenvironmental significance of magnetic fahries in Chinese Lcess-paleosoils since the last interglacial (＜130ka). Earth Planet. Sci. Lett, 2004, 221: 55-69.
146. Zhu, R. X., G. Matasova, A. Kazansky, V. Zykina and J. M. Sun. Rock magnetic record of the last glacial-interglacial cycle from the Kurtak loess section, Southern Siberia. Geophys. J. Int, 2003, 152: 335-343.
147．安芷生，Porter s，ChappelI．J，等．最近130ka洛川黄土堆积序列与格陵兰冰芯记录对比．科学通报，1994，24(39)：2254—2256
148．安芷生，刘晓东．东亚季风气候的历史与变率．科学通报．2000，45(3)：238—249
149．曹家欣，石宁，张建中．晋东南黄土．第四纪研究．1995(2)：123-129
150．陈发虎，张维信．甘青地区的黄土地层学与第四纪冰川问题．科学出版社，1993．
151．陈惠中，金炯，董光荣．全新世古尔班通古特沙漠演化和气候变化．中国沙漠，2001，21(4)：333-339
152．陈杰，卢演俦，丁国瑜等．祁连山西段及酒西盆地地区第四纪构造运动的阶段划分．第四纪研究，1996(3)：263—271
153．陈庆强，李从先，丛友滋．沉积物磁组构与其动力沉积特征对应关系研究．科学通报，1998，43(10)：1106—1109
154．陈云，童国榜，曹家栋等．渭河宝鸡段河谷地貌的构造气候响应．地质力学学报，1999，5(4)：49—56
155．程绍平，邓起东，闵伟．黄河晋陕峡谷河流阶地和鄂尔多斯高原第四纪构造运动．第四纪研究，1998，(3)：238—
156．崔之久，伍永秋，刘耕年．关于“昆仑-黄河运动”．中田科学(D辑)，1998，28(1)：53-59
157．丁仲札，孙继敏，刘东生．联系沙漠—黄土演变过程中耦合关系的沉积学指标．中国科学(D)，1999，29(1)：82-87
158．丁仲礼，孙继敏，刘东生．上新世以来毛乌素沙地的阶段性扩张的黄土—红粘土沉积证据．科学通报，1999， 44(3)：324—326
159．丁仲礼，孙继敏，余志伟等．黄土高原过去130ka以来古气候事件年表．科学通报，1998，43(6)：567-574
160．丁仲礼．晚更新世季风—沙漠系统千年尺度的不规则变化及其机制问题．中国科学(D辑)，1996，26(5)：386-391
161．董光荣，陈惠中，金炯等．塔克拉玛干南缘新生代古风成砂．中国第四纪冰川与环境．科学出版社，1991：164—170
162．董光荣，高尚玉，金炯，李保生．毛乌素沙漠的形成、演变和成因问题．中国科学，1988，6：633—642
163．董光荣，靳鹤龄，王贵勇等．中国沙漠形成演化与气候变化研究．中国科学院院刊，1999，(4)：276—280
164．董光荣，李森，李保生等．中国沙漠形成演化的初步研究．中国沙漠，1991，11(4)：23—32
165．董光荣，王贵勇，陈惠中等．中国沙漠形成、演化与青藏高原隆升的关系．青藏高原与全球变化研讨会论文集．气象出版社，1995：13-28
166．董光荣等．中国沙漠形成演化气候变化与沙漠化研究．海洋出版社，北京，2002
167．范代读，邱桂强，李从先等．东营三角洲的古流向研究．石油学报，2000，21(1)：29—33
168．范淑贤，童国榜，郑宏瑞．山西大同地区0.8M a以来植物群及古气候演化．地质力学学报，1998，4(4)63-68
169．方精云，唐艳鸿，林俊达等．全球生态学-气候变化与生态响应．高等教育出版社．2000：2-5
170．方小敏，陈富斌，施雅风等．甘孜黄土与青藏高原冰冻圈演化．科学通报，1996，41(20)：1865-1867
171．方小敏，李吉均，Rob Van der Voo，西秦岭黄土的形成时代与物源区关系探讨．科学通报，1999，44(7)：779-782
172．方小敏，吕连清，杨胜利等．昆仑山黄土与中国西部沙漠发育和高原隆升．中国科学(D)，2001，31(3)：177-184
173．方小敏，史正涛，杨胜利等．天山黄土和古尔班通古特沙漠发育及北疆干旱化．科学通报，2002，47(7)：540-545
174．方小敏，宋春晖，高军平等．青藏高原东北边缘晚新生代哺乳动物化石的磁性地层学．科学通报，2002，47(23)：1824-1828
175．方小敏．青藏高原东部边缘及邻区马兰黄土成因与来源的初步研究．中国科学，1994，(5)：539-54624
176．关恩威．渭河谷地地貌发育史及有关问题的讨论．中国第四纪研究，1965，4(1)：195～203
177．郭正堂，魏兰英，吕厚远等．晚第四纪风尘物质成分的变化及其环境意义，第四纪研究，1999，1：41-48
178．郭正堂，吴海滨．浅谈固体地球科学与地球系统科学．地球科学进展，2004，19(5)：699-705
179．郭正堂．最后两个冰期黄土记录中的Heinrich型气候节拍．第四纪研究，1996，(1)：21—28
180．韩广，张桂芳．河流演变在科尔沁沙地形成和演化中的作用初探—以科尔沁沙地南部教来河中游沙地为例，中国沙漠，2001，21(2)
181．韩家懋，王国安，刘东生等．C4植物的出现与全球环境变化．地学前缘，2002，9(1)：233-243
182．胡小猛，傅建利，李有利．汾河流域地貌发育对构造运动和气候变化的响应．地理学报，2002，57(3)：317-324
183．胡小猛，杨景春，临汾盆地中更新世中晚期以来的演化历史及成因分析．上海师范大学学报(自然科学版)，2001，30(3)：72—76
184．黄汲清，闵隆瑞．青藏高原的隆起，沙漠和黄土的形成，人类的起源与演化．第四纪研究，1992，(1)：24—28
185．金性春，周祖翼，汪品先．大洋钻探与中国地球科学．同济大学出版社，1995：79-94
186．靳鹤龄，董光荣，刘玉璋等．0.8Ma B．P．以来西藏雅鲁藏布江中游地区沙地演化和气候变化．中国沙漠，1998，18(2)：97—104
187．靳鹤龄，董光荣，苏志珠等．全新世沙漠-黄土边界带空间格局的重建．科学通报，2001，46(7)：538-543
188．靳鹤龄，董光荣，张春来．雅鲁藏布江河谷黄土的沉积特征及成因．中国沙漠．2000，20(1)：14-19
189．雷样义．商州黄土记录的最近六十万年来东秦岭古环境变迁．海洋地质与第四纪地质，1999，19(1)：63-73
190．李保生，李森，王跃等．我国极端干旱区边缘阿羌砂尘堆积剖面的地质年代．地质学报，1998，72(1)：83-92
191．李丰江，邓金宪，温泉波等．长春腰分水岭黄土剖面常量化学元素特征及其气候意义．世界地质，2002，21(1)：53-56
192．李吉均，方小敏，潘保田等．新生代晚期青藏高原强烈隆起及其对周边环境的影响．第四纪研究，2001，21(5)：381-391
193．李吉均，方小敏，马海洲，等．晚新生代黄河上游地貌演化与青藏高原隆起．中国科学(D)，1996，26(4)：316-322
194．李吉均，方小敏．青藏高原的隆起与环境变化研究．科学通报，1998，43(15)：1569-1574
195．李吉均，文世宣，张青松等．青藏高原隆起的时代、幅度和形式的探讨．中国科学，1979，(6)：608-616
196．李军敏，王锡魁，范昌福等．四平杏山黄土堆积的粒度特征及成因探讨．世界地质，2004，23(2)：134—137
197．李萍，李培英，张晓龙等．冲绳海槽沉积物与不同粒级的磁性特征及其与环境的关系．科学通报，2005，50(3)：262-268
198．李徐生，杨达源．镇江下蜀黄土-古土壤序列磁化率特征与环境记录．中国沙漠，2002，1：
199．李永化，张小咏，崔之久等．第四纪泥石流活动期与气候期的阶段性耦合过程．第四纪研究，2002，22(4)：340-348
200．李永昭．青藏高原第四纪冰期序列及其意义．成都理工学院学报，1998，25(2)：304—309
201．李哲，周昆叔，曾贻伟．周原黄土磁化率与Fe~(3+)／Fe~(2+)+Fe~(3+)及铁相对含量间的关系．海洋地质与第四纪地质，1996，16(4)：105—112
202．林海．中国全球变化研究的回顾与展望．地学前缘，2002，9(1)：19-25
203．林年丰，汤洁，卞建民等．东北平原第四纪环境演化与荒漠化问题．第四纪研究，1999(5)：448—455
204．刘百麓，刘小凤，袁道阳等．黄河中上游阶地对青藏高原东北部第四纪构造活动的反映．地震地质，2003，25(1)：133—145
205．刘宝柱，李存先，业治诤等．沉积磁组构在长江三角洲晚第四纪古土壤研究中的应用．海洋地质与第四纪地质，1994，14(2)：55—62
206．刘东生，郑绵平，郭正堂．亚洲季风系统的起源和发展及其与两极冰盖和区域构造运动的时代耦合．第四纪研究，1998，3：194-203
207．刘东生．黄土与环境，科学出版社，北京，1985
208．刘护军，秦岭新生代构造隆升研究．陕西师范大学学报(自然科学版)，2002，30(1)：121-124
209．刘嘉麒，韩家懋．方兴未艾，再创辉煌．2002，第八届全国第四纪学术会议论文摘要
210．刘晓东，焦彦军等．东亚季风气候对青藏高原隆升的敏感性研究．大气科学，2000，24(5)：593-607
211．刘晓东，李力，安芷生等．青藏高原隆升与欧亚内陆及北非的干旱化．第四纪研究，2001，21(2)：114-122
212．刘秀铭，许同春，刘东生．中国黄土磁化率各向异性与成因及其对第四纪研究的意义．中国科学(B辑)，1989，4：441—448
213．吕厚远，韩家懋，吴乃琴等．中国现代土壤磁化率分析及其古气候意义．中国科学(B辑)，1994，24(12)：1290—1297
214．鸟居雅之，福间洁司，苏黎等．黄土—古土壤磁化率述评．海洋地质与第四纪地质，1999，19(3)：83—96
215．潘保田，高红山，李吉均．关于夷平面的科学问题—兼论青藏高原夷平面．地理科学，2002，22(5)：520-526
216．潘保田，李吉均，曹继秀等．化隆盆地地貌演化与黄河发育研究．山地研究，1996，14(3)：153-158
217．潘保田，李吉均，陈发虎等．青藏高原：全球气候变化的驱动机与放大器．Ⅰ新生代气候变化的基本特征，兰州大学学报(自然科学版)，1995，31(3)：120-128
218．潘保田，李吉均，朱俊杰，曹继秀等．青藏高原：全球气候变化的驱动机与放大器．Ⅱ青藏高原隆起的基本过程．兰州大学学报(自然科学版)，1995，31(4)：160-167
219．潘保田，李吉均．青藏高原：全球气候变化的驱动机与放大器：青藏高原隆起对气候变化的影响．兰州大学学报(自然科学版)，1996，32(1)：108-115
220．潘保田，邬光剑，王义祥等．祁连山东段沙沟阶地的年代与成因．科学通报，2000，45(24)：2669-2675
221．潘保田．贵德盆地地貌演化与黄河上游发育研究．干旱区地理，1994，17(3)：3-50
222．潘保田．兰州地区黄土阶地发育与地貌演化．1991．见：中国第四纪冰川与环境，北京：科学出版社
223．潘保田，王均平，高红山等．河南扣马黄河最高级阶地古地磁年代及其对黄河贯通时代的指示．科学通报，2005，50(3)：255-261
224．潘永信，朱日祥．磁组构研究现状．地球物理学进展，1999，13(1)：52—59
225．潘裕生，孔祥儒，钟大赉等．高原岩石圈结构、演化和动力学．In：青藏高原形成演化与发展：孙鸿烈，郑度，广 东科技出版社，1998
226．潘裕生．青藏高原的形成与隆升．地学前缘，1999，6(3)
227．屈建军，郑本兴，俞祁浩．罗布泊东阿奇克谷地雅丹地貌与库姆塔格沙漠形成的关系．中国沙漠，2004，24(3)：294—300
228．施雅风，李吉均，李炳元，潘保田等．高原隆升与环境演化．In：青藏高原形成演化与发展：孙鸿烈，郑度，广东科技出版社，1998：76-78
229．施雅风，郑本兴．青藏高原中东部最大冰期时代高度与气候环境探讨．冰川冻土，1997，17(2)：97-112
230．施雅风．第四纪中期青藏高原冰冻圈的演化及其与全球变化的关系．冰川冻土，1998，20(3)：197-208
231．施雅风．中国第四纪冰期划分改进建议．冰川冻土，2002，24(6)：687—692
232．苏珍，施雅风，郑本兴．贡嘎山第四纪冰川遗迹及冰期划分．地球科学进展，2002，17(5)：639-647
233．孙继敏，丁仲礼，刘东生．50万a来沙漠．黄土边界带的环境演变．干旱区地理，1995，18(4)：2—9
234．孙继敏，丁仲礼，刘东生．黄土与古土壤磁组构测定在重建冬季风风向上的初步应用．科学通报．1995，40(21)：1976-1978
235．孙继敏，刘东生，丁仲礼等，五十万年来毛乌素沙漠的变迁．第四纪研究，1996，(4)：360—367
236．汤懋苍．董文杰等．青藏高原的抬升和夷平过程对气候与环境的影响．高原气象，1997，16(1)：23-29
237．汤懋苍，柳艳香等．青藏高原隆升的深层原因及其环境后果．第四纪研充2001，21(6)：500-507
238．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．地球科学进展，2004，19(1)：55-62
239．汤懋苍．高原季风的形成、演化及振荡特性．见：青藏高原近代气候变化及对环境的影响．广州：广东科技出版社，1998，161～183
240．田勤俭，申旭辉，冯希杰等．渭河盆地断层活动反映的第四纪构造事件初步研究，地震地质，2003，25(1)：146—154
241．童国榜，吴锡浩，陈云等．渭河谷地晚新生代地表环境巨变的孢粉记录．地质力学学报，2000，6(4)：11—18
242．汪品先，田军，成鑫荣．第四纪冰期旋回转型在南沙深海的记录．中国科学，2001，31(10)：793—799
243．汪品先．穿越圈层．横跨时空．地球科学进展，2002，17(3)：311-313
244．汪阳春，柴宗新，刘淑珍等．横断山地区的黄土及意义．山地学报，1999，17(4)：300-305
245．王岸，王国灿，向树元．东昆仑山东段北坡河流阶地发育及其与构造隆升的关系．地球科学—中国地质大学学报，2003，28(6)：675—679
246．王国灿，侯光久，张克信，朱云海．东昆仑东段中更新世以来的成山作用及其动力转换．地球科学—中国地质大学学报，2002，27(1)：4-12
247．王建力，方小敏，张宇田等．青藏高原东北边缘黄土磁化率各向异性揭示古风向的初步研究．兰州大学学报(自然科学版)，1995，31(4)：155-159
248．王克鲁，盛学斌，严富华等．山西洪洞王绪黄土地层划分．地质科学，1997，32(4)：495-505
249．王乃昂，张虎才，曹继秀等．腾格里沙漠南缘武咸黄土剖面磁性地层年代初步研究．兰州大学学报(自然科学版)，1997，33(4)：144-146
250．王苏民，吴锡浩，张振克等．三门古湖沉积记录的环境变迁与黄河贯通东流研究．中国科学(D)，2001，31(9)：760—768
251．王苏民，薛滨．中更新世以来若尔盖盆地环境演化与黄土高原比较研究．中国科学，26(4)：323-328
252．王涛．巴丹吉林沙漠形成演变的若干问题．中国沙漠，1990，10(1)：29-40
253．邬光剑，潘保田，管清玉等．中更新世全球最大冰期与中国沙漠扩张．冰川冻土，2002，24(5)：544-549
254．吴海滨，陈发虎，王建民等．现代风成沉积物磁化率各向异性与风向关系的研究．地球物理学报，1998，41(6)：811-817
255．吴汉宁，岳乐平．风成沉积物磁组构与中国黄土区第四纪风向变化．地球物理学报，1997，40(4)：487-494
256．吴文样，刘东生．更新世中期气候变化与手斧文化扩散．地学前缘，2001，8(2)
257．吴中海，赵希涛，江万等．念青唐古拉山东南麓更新世冰川沉积物年龄测定．冰川冻土，2003，25(3)：273-274
258．吴中海，赵希涛，朱大岗．念青唐古拉山西布冰川区的冰碛层．地球学报，2002，23(4)：343-348
259．伍永秋，崔之久，葛道凯等．青藏高原何时隆升到现代的高度-以昆仑山垭口地区为例．地理科学，1999，19(6)：481-484
260．伍永秋，崔之久，刘耕年等．昆仑山垭口地区的冰期序列．冰川冻土，1999，21(1)：71—76
261．徐孝彬，王建，朱捷等．利用宇生核素测年技术对青藏高原东南部冰蚀面年代的研究．地理科学，2004，24(1)：101-104
262．薛滨，王苏民，王云飞．湖泊深钻揭示的中更新世以来中国环境的区域分异及其与亚洲季风的关系．湖泊科学，1998，10(1)：1-4
263．薛祥熙，李文厚，刘玉林．渭河北迁与秦岭抬升．西北大学学报(自然科学版)，2002，32(5)：451-454
264．阎满存，董光荣，李保生等．腾格里沙漠东南缘沙漠演化的初步研究．中国沙漠，1998，18(2)：111—117
265．颜茂都，方小敏，陈诗越等．青藏高原更新世黄土磁化率和磁性地层与高原重大气候变化事件．中国科学(D辑)，2001，31：182-186
266．杨达源．中国东部的第四纪风尘堆积与季风变迁．第四纪研究，1991，4：354-359
267．姚檀栋．古里雅冰芯氧同位素地层学．第四纪研究，2000，20(2)：165-170
268．于革，王苏民．欧亚大陆湖泊记录和两万年以来大气环流变化．第四纪研究，1998，4：360-367
269．于洪军，韩德亮，初风友．晚更新世末期北方陆架区沙漠-黄土堆积群的初步研究．地质力学学报，1997，3(4)：33-38
270．张鸿义，门国发．塔克拉玛干沙漠腹地第四纪地层划分与环境变迁．新疆地质，2002，20(3)：256—261
271．张力小，宋豫秦．青藏高原的隆起对中国沙漠与沙漠化时空格局的影响．中国人口，资源与环境，2001，11(4)：98—101
272．张拴宏，周显强．磁化率各向异性地学应用综述．地质论评，1999，45(6)：613—620
273．张小曳．亚洲粉尘源区的分布、释放、输送、沉降和黄土堆积．第四纪研究，2001，21(1)：29—40
274．张叶春，李吉均，朱俊杰等．晚新生代金沙江形成时间与过程研究．云南地理环境研究，1998，10(2)：43—48
275．张叶春．长江三峡贯通的时代及意义．西北师大学报(自然科学版)，1995，31(2)：52—56
276．张智勇，于庆文，张克信，顾延生，向树元．黄河上游第四纪河流地貌演化-兼论青藏高原1：25万新生代地质填图地貌演化调查．地球科学，2003，28(6)：621—633
277．张祖陆．渤海莱州湾南岸滨海平原的黄土．海洋学报，1995，17(3)：127—134
278．赵景波，童国榜．秦岭太白盆地黄土地层发育时的古环境．西安地质学院学报，1994，16(1)：64-70
279．赵志军，史正涛，方小敏．祁连山北缘早中更新世新构造运动的地层记录．兰州大学学报(自然科学版)，2001，37(6)：92-98
280．郑本兴．云南玉龙雪山第四纪冰期与冰川演化模式．冰川冻土，2000，22(1)：53—61
281．郑本兴，施雅风．珠穆朗玛峰地区第四纪冰期探讨．见：珠穆朗玛地区科学考察报告(1966—1968)，第四纪地质学．北京：科学出版社，1976
282．郑度，李炳元．青藏高原地理环境研究进展．地理科学，1999，19(4)：295-302
283．郑度，林振耀，张雪芹．青藏高原与全球环境变化研究．地学前缘，2002，9(1)：95-102
284．钟大赉，丁林．青藏高原的隆起过程及其机制探讨．中国科学(D)，1996，26(4)：289-295
285．周尚哲，李吉均，张世强．祁连山摆浪河谷地的冰川地貌与冰期．冰川冻土，2001b，23(2)：131—138
286．周尚哲，李吉均．冰期之青藏高原新研究．地学前缘，2001 a，8(1)：67—75
287．周尚哲，易朝路，施雅风．中国西部MIS12冰期研究．地质力学学报，2001，7(4)：321—327
288．周秀骥．对地球系统科学的几点认识．地球科学进展，2004，19(5)：513-515
289．朱大岗，赵希涛，盂宪刚等．念青唐古拉山中段第四纪冰期划分．地球学报，2002，23(4)：335-342
290．朱俊杰，曹继秀，钟巍等．兰州地区黄河最高阶地与最老黄土堆积的发现及其古地磁年代学的研究．见：青藏项目专家委员会编．青藏高原形成演化、环境变迁与生态系统研究学术论文年刊(1994)．北京：科学出版社：77-90
291．朱日祥，AKazansky，G Matasova，等．西伯利亚南部黄土沉积物的磁学性质．科学通报，2000，45(11)：1200-1205
292．朱照宇．黄河中游河流阶地的形成与水系演化．地理学报，1989，44(4)：429～439
2. Alley R. B, Lawson D. E, Evenson. G. J et al. Stabilizing feedbacks in glacial-bed erosion. Nature, 2003, 424:758-760
3. An Z S, Kukla G, Porter S C, et al. Late Quaternary dust flow on the Chinese Loess Plateau. Catena, 1991, 18: 125-132
4. An zhisheng, John.E.Kutzbach. Warren.Prell et el. Evolution of Asian monsoons and Phased uplift of the Himalaya-Tibetan Plateau since late Miocene times. Nature, 2001,411: 62-66
5. Andrew S. Ackerman, Michael P. Kirkpatrick, David E. Stevens et al. The impact of humidity above stratiform clouds on indirect aerosol climate forcing. Nature, 2004, 432(23/30): 1014-1017
6. Atbogast, Alan F., Daniel R. Muhs, Geochemical and mineralogical evidence from eolian sediments for northwesterly mid-Holocene paleowinds, central Kansas, USA Quaternary International, 2000, 67:107-118
7. Ashkenazy, Yosef Eli Tziperman. Are the 41kyr glacial oscillations a linear response to Milankovitch forcing? Quaternary Science Review, 2004, 23 1879-1890
8. Bains, Santo Richard D. Norris, Richard M. Corfield et al Termination of global warmth at the Palaeocen/Eocene boundary through productivity feedback. Nature, 2000, 407:171-173
9. Balsama W, Junfeng Ji, Jun Chen. Climatic interpretation of the Lunchuan and Lingtai loess sections, China, based on changing iron oxide mineralogy and magnetic susceptibility. Earth and Planetary Research Letters, 2004, 223:335-348
10. Barry, Leon George C, Craig, John Thuburn, Poleward heat transport by the atmospheric heat caging. Nature, 2002, 415:774—777
11. Becquey Sabine, Rainer Gersonde Past hydrographic and climatic changes in the Subantarctic Zone of the South Atlantic -The Pleistocene record from ODP Site 1090 Palaeogeography, Palaeoclimatology, Palaeoecology, 2002,182: 221-239
12. Ben, Richards W.M. Luminescence dating of Quaternary sediments in the Himalaya and High Asia: a practical guide to its use and limitations for constraining the timing of glaciation. Quaternary International, 2000, 65/66:49-61
13. Benn, Douglas Ⅰ, Lewis A. Owen Himalayan glacial sedimentary environments: a framework for reconstructing and dating the former extent of glaciers in high mountains. Quatemery International, 2002, 97/98:3-25
14. Berger, X.S.Li M.F.loutre. Modelling Northern Hemisphere ice volume over the last 3 Ma. Quaternary science review. 1999, 18:1-11
15. Berner, Robert A. Elizabeth K. Berner. Silicate weathering and climate, in:W.F.Ruddiman(Ed.),Tectonic Uplift and Climate Change, Plenum, New York Press, NY, 1997:353-365
16. Bettis, E. Arthur, Daniel R. Muhs, Helen M. Roberts. Last Glacial loess in the conterminous USA. Quaternary Science Reviews 2003, 22:1907-1946
17. Bice, Karen L. Christopher R. Scotese, Dan Seidov, Quantifying the role of geographic change in Cenozoic ocean heat transport using uncoupled atmosphere and ocean models Palaeogeography, Palacoclimatology, Palaeoecology, 2000, 161:295-310
18. Bush, A.B.G, A comparison of simulated monsoon circulations and snow accumulation in Asia during the mid-Holocene and at the Last Glacial Maximum. Global and Planetary Change, 2002. 32:331-347.
19. Bush, A.B.G, Apositive climatic feedback mechanism for Himalayan glaciation. Quaternary International, 2000, 65166, 3-13.
20. Cande, S.C., Kent, D.V., Revised calibration of the geomagnetic polarity timeacales for the late cretaceous and Cenozoic, J. Geophys. Res (D), 1995, (100): 603-609
21. Cane, Mark A, Peter Moiner, Closing of the Indonesian seaway as a precursor to east African aridification mound 3-4 million yeats ago. Nature, 2001, 411: 157-162
22. Carmala N Garzione, David L. Dettman, Jay Quade et al. High times on the Tibetan plateau: Paleoelevation of the Thakkhola graben, Nepal. Geology, 2000, 28 (4): 339-342
23. Chen F H. High-resolution multi-proxy climate records from Chinese loess: evidence for rapid climate changes over the last 75 kyr (J). Paleogeography Paleoclimatology Paleoecology, 1997, 130:323—335
24. Christensen, B.A., J.L. Kalbas, M. Maslin. Paleoclimatic changes in southern Africa during the intensification of Northern Hemisphere glaciation: evidence from ODP Leg 175 Site 1085 Marine. Geology, 2002,180:117-131
25. Clark, Peter U. Richard B. Alley, David Pollard. Northern Hemisphere Ice-Sheet Influences on Global Climate Change Science, 2000, 286:1104-1111
26. Clifford S. Riebe, James W. Kirchner, Darryl E. Granger et al. Strong tectonic and week climatic control of long-term chemical weathering rates. Geology,2001, 29(6): 511-514
27. Crowley, Thomas J. Cycles, Cycles Everywhere, Science, 2002, 295:1473-1474
28. Cui Zhijiu, Chienfu Yang, Gengnian Liu. The Quaternary glaciation of Shesan Mountain in Taiwan and glacial classification in monsoon areas. Quaternary International, 2002, 97/98:147-153
29. Dansgaard, W. S J. Johnsen, H B. Clausen. Evidence for general instability of past climate from a 250-kyr ice-core record. Nature, 1993, 364:218-220
30. DeConto, Robert M. David Pollard, Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO_2. Nature, 2003, 421: 245-249
31. Derbyshire, Edward Loess and the Dust Indicators and Records of Terrestrial and Marine Palaeoenvironments (DIRTMAP) database. Quaternary Science Reviews, 2003, 22:1813-1819
32. Derry, L. A., France-Lanord., Neogene Himalaya weathering history and river ~(87)Sr/~(86)Sr: impact on the marine Sr record. Earth and Planetary Science Letters, 1996, 142:59-74
33. Ding, Z L Derbyshire, S. L. Yang et al, Stacked 2.6-Ma grain size record from the Chinese Loess based on five section and correlation with deep-sea δ~(18)O record, Paleoceangraphy, 2002, 17 (3): 5-1 5-21
34. Ding, Z. L. J. M. Sun, S. L. Yang. Geochemistry of the Pliocene red clay formation in the Chinese Loess Plateau and implications for its origin, source provenance and paleoclimate change. Geochimica et Cosmochimica Acta, 2001, 65 (6): 901-913
35. Elkibbi, Maya Jose A. Rial, An outsider's review of the astronomical theory of the climate: is the eccentricity-driven insolation the main driver of the ice ages? Earth-Science Reviews, 2001, 56:161-177
36. EPICA community members, Eight glacial cycles from an Antarctic ice core. Nature, 2004, 429:623-628
37. Fang, Xiao-Ming Ji-jun Li, Rob Van der Voo. Rock magnetic and grain size evidence for intensified Asian atmospheric circulation since 800,000 years B.P. related to Tibetan uplift. Earth and Planetary Science letters,1999,165:129-144
38. Feng Z.-D, P. Khosbayar Paleosubarctic Eolian environments along the southern margin of the North American Icesheet and the southern margin of Siberia during the Last Glacial Maximum. Palaeogeography, Palaeoclimatology, Palaeoecology. 2004, 212:265- 275
39. Flynn, John J. Michael J. Novacekc, Holly E. Dodson. A new fossil mammal assemblage from the southern Chilean Andes: implications for geology, geochronology, and tectonics. Journal of South American Earth Sciences, 2002:1-18
40. Getty, Stephen R. Yemane A.Smerom, Terrence M.Quinn. Accelerated Pleistocene coral extinction in the Caribbean Basin shown by uranium-lead (U-Pb) dating. Geology, 2001, 29(7): 639-642
41. Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature, 2002, 416:159～163
42. Guyodo, Yohan Jean-Pierre Valte. Global changes in intensity of the earth's magnetic field during the past 800kyr. Nature, 1999, 399:249-252
43. Handy, R L, Loess distribution by variable winds. Geological Society of American Bulletin, 1976, 87:915-92744. Hang, Gerald H. Andrey Ganopolski, Daniel M. Sigman et al, North Pacific seasonality and the glaciation of North America 2.7 million years ago. Nature, 2005, 433, 821-825
45. Hays, J. D. Variations in Earth's orbit: Pace-maker of Ice Ages. Science,1976, 194:1121
46. Heller, F, liu,T.s. Magnetostratigralhical dating of loess deposits in China. Nature, 1982, 300:431-433
47. Henrich, Ru.diger Karl-Heinz Baumann, Robert Huber. Carbonate preservation records of the past 3 Myr in the Norwegian-Greenland Sea and the northern North Atlantic: implications for the history of NADW production Marine Geology. 2002, 184:17-39
48. Henrik Svensen, Sverre Planke, Anders Malthe-Sφrenssenl, Release of methane from a volcanic basin as a mechanism for initial Eocene global warming nature, 2004, 429:542-545
49. Heslop, D. Langereis. C.G. Dokkers. M.J. a new astronomical timescale for the loess deposition of Northern China. Earth and Planetary Science Letters. 2000,184:125-139
50. Heslop, D., M.J. Dekkers, C.G. Langereis Timing and structure of the mid-Pleistocene transition: records from the loess deposits of northern China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 185:133-143
51. Hess S, Wolfgang, Kuhnt. Neogene and Quaternary paleocenography changes in the southern South China Sea (site 1143): the benthic foraminiferal record. Marine Micropaleontology, 2005, 54:63-87
52. Hopkinson, Charles S. Jr & Joseph J. Vallino. Efficient export of carbon to the deep ocean through dissolved organic matter. Nature, 2005, 433(13): 142-145
53. Hu, Xiaomeng Youli Li, Jinchun Yang. Quaternary Paleolake development in the Fen River Basin, North China. Geomorphology, 2005, 65:1-13
54. Hunt, C. P., S. K. Banerjee, J. M. Hart, P. A. Solheid, E. Oches, W. W. Sun, and T. S. Liu, Rock magnetic proxies of climate changes in the loess-paleosol sequences of the western Loess Plateau of China, Geophys. J. Int., 1995, 123: 232-244
55. Joseph L. H., Rea D. K., Ben A.van der Pluijm. use of grain size and magnetic fabric analyses to distinguish among depositional environments. Paleoceanography, 1998, 13(5): 491-501
56. Kashiwaya, K., Ochial, S., Sakai, H. & Kawai, T. Orbit-related long-term climate cycles revealed in a 12-Myr continental record from Lake Baikal. Nature, 2001, 410: 71-74.
57. Kathryn M. Gregory., Wodzicki, A late Miocene subtropical-dry flora from the northern Altiplano, Bolivia. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 180:331-348
58. Kathryn M. Gregory-Wodziciki, Uplift history of the Central and Northern Andes: A review. Geological Society of American Bulletin. 2000, 112 (7): 1091-1105
59. Kent D.V., Opdyke, N. D., Ewing. M., Climate change in the North Pacific using ice-rafted detritus as a climatic indicator. Geological Society of American Bulletin, 1971, 82:2741-2754
60. Kent D.V., Rio D., Massari F et al., Emergence of Veince during the Pleistocene. Quaternary Science Review, 2002, 21: 1719-1727
61. Kerich, D M. K.Caldeira. Was the Himalayan orogen a climatically significant coupled source and sink for atmospheric CO2 during the Cenozonic? Earth and Planetary science letters, 1999, 173:195-203
62. Kohfeld, K.E S.P. Harrison. Glacial-interglacial changes in dust deposition on the Chinese Loess Plateau. Quaternary Science Review, 2003, 22:1859-1878
63. Kukla, G, Heiler, F, Liu, X.M,. Pleistocene climates in China dated by magnetic susceptibility. Geology, 1988, 16: 811-814.
64. Kump, Lee.R. Reducing uncertainty about carbon dioxide as a climate driver. Nature, 2002, 419:188-190
65. Kutzbach, J.E. Prell, W. L., Ruddiman, W. F. Sensitivity of Eurasian climate to surface uplift of the Tibetan Plateau. Journal of Geology. 1993, 101:177-190
66. Kutzbach, J.E., Guetter, P. J., Ruddiman, W. F., et al. Sensitivity of climate to late Cenozoic uplift in southern Asia and the American West: numerical experiments. Journal of Geophysical Research, 1989, 94:18,393-18,407
67. Lacis, Tegen I, A.A., Fung, I.,. The infuence on climate forcing of mineral aerosols from disturbed soils. Nature, 1996, 380: 419-422.
68. Lagriox, F, and S. K. Banerjee, Paleowind directions from the magnetic fabric if loess profiles in central Alaska. Earth Planet. Sci. Lett., 2002, 195: 99-112.
69. Lagriox, F, and S. K. Banerjee. The regional and temporal significance of primary Aeolian magnetic fabric preserved in Alaskan loess. Earth Planet. Sci. Lett, 2004, 225: 379-395
70. Lamb, Simon Paul Davis. Cenozoic climate change as a possible cause for the rise of the Andes. Nature, 2003, 425: 792-797
71. Lavier, Luc L Michael S.Steckler Frederic Brigaud. Climatic and tectonic control on the Cenozoic evolution of the western Africa Margin. Marine Geology, 2001,178:63-80
72. Li Ji jun, Shiyou Xie, Mingsheng Kuang. Geomorphic evolution of the Yangtze Gorges and the time of their formation. Geomorphology, 2001, 41: 125-135
73. Li Jijun. The environmental effects of the uplift of the Qinghai—Xizang Plateau. Quaternary Science Reviews, 1991, 10: 4792 483.
74. Liu Qingsong,- Subir. K. Banerjee. Michael. J. Jackson et al. Iner-profile correlation of the Chinese loess/paleosol sequences during Marine Oxygen Isotope Stage 5 and indications of pedogenesis. Quaternary Science Review, 2005, 24:195-210
75. Liu X M, Xu.T.C, Liu, T.S, The Chinese loess in Xifeng. II .A study of anisotropy of magnetic susceptibility of loess from Xifeng. Geophysics.J, 1988, 92: 349-353
76. Liu, Xiuming Tim Rolph, Zhisheng An et al. paoleoclimatic significance of magnetic properties on the Red clay underlying the loess and paleosols in China. Paleogeography paleoclimatology, paleoecology, 2003,199: 153-166
77. Maher, Barbara. A., Roy Thompson. Mineral magnetic record of the Chinese loess and paleosols. Geology, 1991, 19: 3-6
78. Manabe, Syukuro Ronald J. Stouffer. Simulation of abrupt climate change induced by freshwater input to the North Atlantic Ocean. Nature, 1995,378:165-167
79. Manabe, Syukuro Theodore B. Terpstra. The effect of mountains on the general circulation of the atmosphere as identified by numerical experiments. Journal of the atmosphere sciences, 1974, 31 (1): 3-41
80. Marincovich, Louie Andrey Yu. Gladenkov. Evidence for an early opening of the Bering Strait. Nature, 1999, 397: 149-151
81. Mason., J.A, E A Natter, H.C. Hobbs. Transport direction of Wisconsin Loess in southeastern Minnesota. Quaternary Research, 1994, 41: 44-51
82. Matalucci R. V., Shelton J. W., and Abdel-Hady M., Grain orientation in Vicksburg loess. Journal of sedimentary petrology, 1969, 39(3): 969-979
83. Miao, Xiaodong Youbin Sun, Huayu Lu et al, Spatial pattern of grain size in the Late Pliocene 'Red Clay' deposits (North China) indicates transport by low-level northerly winds. Palaeogeography, Palaeoclimatology, Palaeoecology, 2004,206: 149-155
84. Mittoni, Giovanni,. Cipriano. Carcano, Eduardo. Garzanti et al, Onset of major Pleistocene glacialtions in the Alps. Geological Society of America, 2003, 31(11):989-992
85. Moberg. A, Dmitry M. Sonechkin, Karin Holmgren. Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature, 2005,433:613-617
86. Nikki M, White, M. Pringle, E. Garzanti et al. Constraints on the exhumation and erosion of the High Himalayan Slab, NW India, from foreland basin deposits. Earth and Planetary Science Letters, 2002,195: 29-44
87. North Greeland Ice Core Project Members. High-resolution record of Northern Hemisphere climate extending into the last interglacial period. Nature, 2004,431:147-151
88. Owen, Lewis A. Robert C. Finkel, Patrick L. Barnard. Climatic and topographic controls on the style and timing of Late Quaternary glaciation throughout Tibet and the Himalaya defined by ~(10)Be cosmogenic radionuclide surface exposure dating. Quaternary Science Review, 2004,
89. Pearson, Paul N, Martin R, Palmer. Atmospheric carbon dioxide concentration over the past 60 million years. Nature, 2000, 406:696-699
90. Petit, J.R., Briat, M., Royer, A., Ice age aerosol content from east Antarctic ice core samples and past wind strength. Nature, 1981, 293: 391-394.
91. Pickart R. S. Spall M. A, Ribergaard M. H et al. Deep convection in the Irminger sea forced by the greeland tip jet. Nature, 2003, 424:152-156
92. Pincus, R, Baker, M. B. Effect of precipitation on the albedo susceptibility of clouds in the marine boundary layer. Nature, 1994(372): 250-252
93. Porter, Stephen C An Zhisheng. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature, 1995, 375:305-308.
94. Prell, W.L, Kutzbach, J.F,. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution. Nature, 1992, 360: 647-652.
95. Quade, J Cerling T,E, Bowman J, R. Development of Asian monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan, Nature, 1989, 342:163-166
96. Quade, Jay Louis Roe, Peter G. DeCelles, Tank P. Ojha. The Late Neogene ~(87)Sr/~(86)Sr Record of Lowland Himalayan Rivers. Science, 1997, 276:1828-1831
97. Ramos, Victor A. E.O. Cristallini, Daniel J. Perez. The Pampe, an flat-slab of the Central Andes. Journal of south American Earth Science, 2002, 15:59-78
98. Raymo, M.E. Glacial puzzles, science, 1998,281:1467-1468
99. Raymo, M.E. Kerim Nisancioglu. the 41 kyr world: Milankovitch's other unsolved mystery, paleoceanography, 2003, 18(1):11-1-11-6
100. Raymo, M.E. The initiation of North Hemisphere Glaciation. Annu tee.Earth Planet Sci. 1994, 23:353-383
101. Raymo, M.E. W E Ruddiman. Tectonic forcing of late Cenozoic climate. Nature, 1992,359:117-122
102. Raymo, M.E. W.F.Ruddiman, P.N.Froelich. Influence of late Cenozoic mountain building on Ocean geochemical Cycles. Geology, 1988,16:649-653
103. Reguero, Marcelo A. Sergio A. Marenssi, Serglo N. Santillana Antarctic Peninsula and South America (Patagonia) Paleogene terrestrial faunas and environments: biogeographic relationships. Palaeogeography, Palaeoclimatoiogy, Palaeoecology, 2002, 179:189-210
104. Ruddiman, W F Kutzbuch J.E. Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and the American west. Journal of geophysical Research, 1998, 94:18409-18427
105. Ruddiman, W.F. (Ed.), Tectonic Uplift and Climate Change. Plenum, New York Press, NY, 1997.
106. Ruddiman, W.F. M.E. Raymo, D.G. Martinson, B.M. Clement, and J. Backman. Pleistocenen evolution: Northern hemisphere ice sheet and North Atlantic Ocean. Paleoceangraphy, 1989, 4(4): 353-412
107. Ruddiman, William F. Maureen E. Raymo A methane-based time scale for Vostok ice. Quaternary Science Reviews, 2002:1-15
108. Rutherfor, Scott Steven D'Hondt. Early onset and tropical forcing of 100,000- year Pleistocene glacial cycles. Name, 2000:72-74
109. Sangode, S. J. Rohtash Kumar and Sumit K. Ghosh. Application of magnetic fabric studies in anancient fluvial sequence of NW Himalaya. Current Science, 2001, 81 (1): 66-71
110. Schafer, Jorg M. Silvio Tschudi, Zhizhong Zhao. The limited in(?)uence of glaciations in Tibet on global climate over the past 170 000 yr. Earth and Planetary Science Letters, 2002, 194:287-297
111. Schefu, E., Schouton, S., Fred Jansen, J. H. African vegetation controlled by tropical sea surface temperatures in the mid-Pleistocene period. Nature, 2003,422:418-421
112. Schmieder, Frank, Tilo von Dobeneck, Ulrich Bleil. The Mid-Pleistocene climate transition as documented in the deep South Atlantic Ocean: initiation, interim state and terminal event. Earth and Planetary Science Letters, 2000, 179: 539-549
113. Schmittner A. Decline of the marine ecosystem caused by a reduction in the Atlantic overturning circulation. Nature, 2005,434: 628-633
114. Shackleton N.J The 100,000 ice age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity. Science, 2000, 289: 1897-1902
115. Shackleton, Nicholas John. Neil D Opdyke. Oxygen isotope and palaeomagnetic stratigraphy of Equatorial pacific core v28-238: oxygen isotope temperature and ice volume on a 10~5 year and 10~6 year scale. Quaternary research, 1973,3: 39-55
116. Shi, Y, Ge, Y, Xiaodong, L, Bingyuan, L, Tandong, Y,.Reconstruction of the 30-40 ka B.P. enhanced Indian monsoon climate based on geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology, 2001, 169: 69-83
117. Silva, P.F. F.O. Marques, J.M. Miranda et al. Anisotropy of magnetic susceptibility constraints on Variscan obduction processes in the Braganc, a Massif (NE Portugal). Tectonophysics, 2001,341:95-119
118. Stainforthl, D. A. T.Ainal, C. Christensen. Uncertainty in predictions of the climate response to rising levels of greenhouse gases. Nature, 2005,433(27): 403-406
119. Sun J M, Liu T S. Stratigraphic Evidence for the Uplift of the Tibetan plateau between～1.1 and～0.9 myr ago. Quaternary Research, 2000, 54: 309-320
120. Sun Jimin, Tungsheng Liu. Multiple origins and interpretations of the magnetic susceptibility signal in Chinese wind-blown sediments. Earth and Planetary Science Letters. 2000, 180: 287-296
121. Sun Jimin. Source Regions and Formation of the Loess Sediments on the High Mountain Regions of Northwestern China. Quaternary Research, 2002, 58: 341-351
122. Sun jimin, Zhongli Ding, Tungsheng Liu. 580,000-year environmental reconstruction from aeolian deposits at the Mu Us Desert margin, China. Quaternary Science Review, 1999,18: 1351-1364
123. Thibault de Garklel-Thoron, Yair Rosenthall, Franck Bassinot et al. Stable sea surface temperatures in the western Pacific warm pool over the past 1.75million years. Nature, 2005, 433(20): 294-298
124. Tilman, Rost Karl Pleistocene paleoenvironmental changes in the high mountain ranges of central China and adjacent regions. Quaternary International, 2000,65/66: 147-160
125. Treguer, Paul Philippe Pondaven. Silica control of carbon dioxide. Nature, 2002,406:358-359
126. Venz, Kathryn A. David A. Hodell. New evidence for changes in Plio—Pleistocene deep water circulation from Southern Ocean ODP Leg 177 Site 1090. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 182: 197-220
127. Visser, Katherine Robert Thunell, Lowell Stott. Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation. Nature, 2003, 421: 152-155
128. Wallmann, K. et al Controls on the Cretaceous and Cenozoic evolution of seawater composition, atmospheric CO2 and climate. Cosmochimica Acta, 2001,65 (18): 3005-3025,
129. Wang Pinxian, Steven Clemens, Luc Beaufort. Evolution and variability of the Asian monsoon system: state of the art and outstanding issues. Quaternary Science Reviews, 2005, 24: 595-629
130. Wehausen, Rolf Hans-Ju.rgen Brumsack. Astronomical forcing of the East Asian monsoon mirrored by the composition of Pliocene South China Sea sediments, Earth and Planetary Science Letters, 2000, 201: 621-636
131. Winckler, Giaela, Robert F. Anderson, Martin Stute and Peter Schlosser. Does interplanetary dust control 100kyr glacial cycles? Quaternary Science Review, 2004,23: 1873-1878
132. Wood, Richard A. Ann B. Keen, John F. B. Mitchell Changing spatial structure of the thermohaline circulation in response to atmospheric CO_2 forcing in a climate model. Nature, 1999, 399:572-575
133. Wu, Guangjian, Baotian Pan, Qingyu Guan, Dunsheng Xia. Terminations and their correlation with solar insolation in the Northern Hemisphere: a record from a loess section in Northwest China. Palaeogcography, Palaeoclimatology, Palaenecology, 2005, 216: 267-277
134. Yamazaki, Toshitsugu Hirokuni Oda. Oribtal influence on earth's magnetic field: 100,000-year periodicity in inclination. Science, 2002, 295:2435-2438
135. Yokokawa, M., and S. O. Franz. Changes in grain size and magnetic fabric at Blake-Bahama outer ridge during the late Pleistocene (marine isotope stages 8-10). Marine Geology, 2002, 189: 123-144.
136. Zachos, James Mark Pagani, Lisa Sloan et al. Trends. Rhythms and aberration in global climate 65 Ma to present. Science, 2001, 292:686-693
137. Zhang Peizhen, Peter Molnar, William R. Downs.Increased sedimentation rates and grain sizes 2±4 Myr ago due to the infuence of climate change on erosion rates. Nature, 2001, 410:891-897
138. Zhang, X. Y, R. Arimoto, and Z. S. An. Glacial and interglacial patterns for Asian dust transport, Quaternary Science Review, 1999, 18: 811-819.
139. Zhang, Xian Y. R. Arimoto, Zhi S. An. Glacial and interglacial patterns for Asian dust transport. Quaternary Science Review, 1999,18:811-819
140. Zhao, H., Moore, G.W.K., on the relationship between Tibetan snow cover, the Tibetan plateau monsoon and the Indian summer monsoon. Geophysical Research Letters, 2004, 31:14-20
141. Zheng, Hongbo Christopher McAulay.Powell, Zhisheng An et al. Uplift of the northern Tibetan plateau. Geology, 2000,28(8): 715-718
142. Zhou Shangzhe, Jijun Li, Shiqiang Zhang. Quaternary glaciation of the Ballang River Valley, Qilian Shan. Quaternary International, 2002, 97/98:103-110
143. Zhou, L.P, Oldfield, F., Wintle, A.G., Robinson, S.G., Wang, J.T. Partly pedogenic origin of magnetic variations in Chinese loess. Nature, 1990, 36: 737-739.
144. Zhu R X. History of anisotropy of the magnetic susceptibility and its implications: preliminary results along an E-W transect of the Chinese loess plateau. Geophysics Research Abs, 2000, 2:226
145. Zhu, R. X, Q. S. Liu, and M. J. Jackson, Palenenvironmental significance of magnetic fahries in Chinese Lcess-paleosoils since the last interglacial (＜130ka). Earth Planet. Sci. Lett, 2004, 221: 55-69.
146. Zhu, R. X., G. Matasova, A. Kazansky, V. Zykina and J. M. Sun. Rock magnetic record of the last glacial-interglacial cycle from the Kurtak loess section, Southern Siberia. Geophys. J. Int, 2003, 152: 335-343.
147．安芷生，Porter s，ChappelI．J，等．最近130ka洛川黄土堆积序列与格陵兰冰芯记录对比．科学通报，1994，24(39)：2254—2256
148．安芷生，刘晓东．东亚季风气候的历史与变率．科学通报．2000，45(3)：238—249
149．曹家欣，石宁，张建中．晋东南黄土．第四纪研究．1995(2)：123-129
150．陈发虎，张维信．甘青地区的黄土地层学与第四纪冰川问题．科学出版社，1993．
151．陈惠中，金炯，董光荣．全新世古尔班通古特沙漠演化和气候变化．中国沙漠，2001，21(4)：333-339
152．陈杰，卢演俦，丁国瑜等．祁连山西段及酒西盆地地区第四纪构造运动的阶段划分．第四纪研究，1996(3)：263—271
153．陈庆强，李从先，丛友滋．沉积物磁组构与其动力沉积特征对应关系研究．科学通报，1998，43(10)：1106—1109
154．陈云，童国榜，曹家栋等．渭河宝鸡段河谷地貌的构造气候响应．地质力学学报，1999，5(4)：49—56
155．程绍平，邓起东，闵伟．黄河晋陕峡谷河流阶地和鄂尔多斯高原第四纪构造运动．第四纪研究，1998，(3)：238—
156．崔之久，伍永秋，刘耕年．关于“昆仑-黄河运动”．中田科学(D辑)，1998，28(1)：53-59
157．丁仲札，孙继敏，刘东生．联系沙漠—黄土演变过程中耦合关系的沉积学指标．中国科学(D)，1999，29(1)：82-87
158．丁仲礼，孙继敏，刘东生．上新世以来毛乌素沙地的阶段性扩张的黄土—红粘土沉积证据．科学通报，1999， 44(3)：324—326
159．丁仲礼，孙继敏，余志伟等．黄土高原过去130ka以来古气候事件年表．科学通报，1998，43(6)：567-574
160．丁仲礼．晚更新世季风—沙漠系统千年尺度的不规则变化及其机制问题．中国科学(D辑)，1996，26(5)：386-391
161．董光荣，陈惠中，金炯等．塔克拉玛干南缘新生代古风成砂．中国第四纪冰川与环境．科学出版社，1991：164—170
162．董光荣，高尚玉，金炯，李保生．毛乌素沙漠的形成、演变和成因问题．中国科学，1988，6：633—642
163．董光荣，靳鹤龄，王贵勇等．中国沙漠形成演化与气候变化研究．中国科学院院刊，1999，(4)：276—280
164．董光荣，李森，李保生等．中国沙漠形成演化的初步研究．中国沙漠，1991，11(4)：23—32
165．董光荣，王贵勇，陈惠中等．中国沙漠形成、演化与青藏高原隆升的关系．青藏高原与全球变化研讨会论文集．气象出版社，1995：13-28
166．董光荣等．中国沙漠形成演化气候变化与沙漠化研究．海洋出版社，北京，2002
167．范代读，邱桂强，李从先等．东营三角洲的古流向研究．石油学报，2000，21(1)：29—33
168．范淑贤，童国榜，郑宏瑞．山西大同地区0.8M a以来植物群及古气候演化．地质力学学报，1998，4(4)63-68
169．方精云，唐艳鸿，林俊达等．全球生态学-气候变化与生态响应．高等教育出版社．2000：2-5
170．方小敏，陈富斌，施雅风等．甘孜黄土与青藏高原冰冻圈演化．科学通报，1996，41(20)：1865-1867
171．方小敏，李吉均，Rob Van der Voo，西秦岭黄土的形成时代与物源区关系探讨．科学通报，1999，44(7)：779-782
172．方小敏，吕连清，杨胜利等．昆仑山黄土与中国西部沙漠发育和高原隆升．中国科学(D)，2001，31(3)：177-184
173．方小敏，史正涛，杨胜利等．天山黄土和古尔班通古特沙漠发育及北疆干旱化．科学通报，2002，47(7)：540-545
174．方小敏，宋春晖，高军平等．青藏高原东北边缘晚新生代哺乳动物化石的磁性地层学．科学通报，2002，47(23)：1824-1828
175．方小敏．青藏高原东部边缘及邻区马兰黄土成因与来源的初步研究．中国科学，1994，(5)：539-54624
176．关恩威．渭河谷地地貌发育史及有关问题的讨论．中国第四纪研究，1965，4(1)：195～203
177．郭正堂，魏兰英，吕厚远等．晚第四纪风尘物质成分的变化及其环境意义，第四纪研究，1999，1：41-48
178．郭正堂，吴海滨．浅谈固体地球科学与地球系统科学．地球科学进展，2004，19(5)：699-705
179．郭正堂．最后两个冰期黄土记录中的Heinrich型气候节拍．第四纪研究，1996，(1)：21—28
180．韩广，张桂芳．河流演变在科尔沁沙地形成和演化中的作用初探—以科尔沁沙地南部教来河中游沙地为例，中国沙漠，2001，21(2)
181．韩家懋，王国安，刘东生等．C4植物的出现与全球环境变化．地学前缘，2002，9(1)：233-243
182．胡小猛，傅建利，李有利．汾河流域地貌发育对构造运动和气候变化的响应．地理学报，2002，57(3)：317-324
183．胡小猛，杨景春，临汾盆地中更新世中晚期以来的演化历史及成因分析．上海师范大学学报(自然科学版)，2001，30(3)：72—76
184．黄汲清，闵隆瑞．青藏高原的隆起，沙漠和黄土的形成，人类的起源与演化．第四纪研究，1992，(1)：24—28
185．金性春，周祖翼，汪品先．大洋钻探与中国地球科学．同济大学出版社，1995：79-94
186．靳鹤龄，董光荣，刘玉璋等．0.8Ma B．P．以来西藏雅鲁藏布江中游地区沙地演化和气候变化．中国沙漠，1998，18(2)：97—104
187．靳鹤龄，董光荣，苏志珠等．全新世沙漠-黄土边界带空间格局的重建．科学通报，2001，46(7)：538-543
188．靳鹤龄，董光荣，张春来．雅鲁藏布江河谷黄土的沉积特征及成因．中国沙漠．2000，20(1)：14-19
189．雷样义．商州黄土记录的最近六十万年来东秦岭古环境变迁．海洋地质与第四纪地质，1999，19(1)：63-73
190．李保生，李森，王跃等．我国极端干旱区边缘阿羌砂尘堆积剖面的地质年代．地质学报，1998，72(1)：83-92
191．李丰江，邓金宪，温泉波等．长春腰分水岭黄土剖面常量化学元素特征及其气候意义．世界地质，2002，21(1)：53-56
192．李吉均，方小敏，潘保田等．新生代晚期青藏高原强烈隆起及其对周边环境的影响．第四纪研究，2001，21(5)：381-391
193．李吉均，方小敏，马海洲，等．晚新生代黄河上游地貌演化与青藏高原隆起．中国科学(D)，1996，26(4)：316-322
194．李吉均，方小敏．青藏高原的隆起与环境变化研究．科学通报，1998，43(15)：1569-1574
195．李吉均，文世宣，张青松等．青藏高原隆起的时代、幅度和形式的探讨．中国科学，1979，(6)：608-616
196．李军敏，王锡魁，范昌福等．四平杏山黄土堆积的粒度特征及成因探讨．世界地质，2004，23(2)：134—137
197．李萍，李培英，张晓龙等．冲绳海槽沉积物与不同粒级的磁性特征及其与环境的关系．科学通报，2005，50(3)：262-268
198．李徐生，杨达源．镇江下蜀黄土-古土壤序列磁化率特征与环境记录．中国沙漠，2002，1：
199．李永化，张小咏，崔之久等．第四纪泥石流活动期与气候期的阶段性耦合过程．第四纪研究，2002，22(4)：340-348
200．李永昭．青藏高原第四纪冰期序列及其意义．成都理工学院学报，1998，25(2)：304—309
201．李哲，周昆叔，曾贻伟．周原黄土磁化率与Fe~(3+)／Fe~(2+)+Fe~(3+)及铁相对含量间的关系．海洋地质与第四纪地质，1996，16(4)：105—112
202．林海．中国全球变化研究的回顾与展望．地学前缘，2002，9(1)：19-25
203．林年丰，汤洁，卞建民等．东北平原第四纪环境演化与荒漠化问题．第四纪研究，1999(5)：448—455
204．刘百麓，刘小凤，袁道阳等．黄河中上游阶地对青藏高原东北部第四纪构造活动的反映．地震地质，2003，25(1)：133—145
205．刘宝柱，李存先，业治诤等．沉积磁组构在长江三角洲晚第四纪古土壤研究中的应用．海洋地质与第四纪地质，1994，14(2)：55—62
206．刘东生，郑绵平，郭正堂．亚洲季风系统的起源和发展及其与两极冰盖和区域构造运动的时代耦合．第四纪研究，1998，3：194-203
207．刘东生．黄土与环境，科学出版社，北京，1985
208．刘护军，秦岭新生代构造隆升研究．陕西师范大学学报(自然科学版)，2002，30(1)：121-124
209．刘嘉麒，韩家懋．方兴未艾，再创辉煌．2002，第八届全国第四纪学术会议论文摘要
210．刘晓东，焦彦军等．东亚季风气候对青藏高原隆升的敏感性研究．大气科学，2000，24(5)：593-607
211．刘晓东，李力，安芷生等．青藏高原隆升与欧亚内陆及北非的干旱化．第四纪研究，2001，21(2)：114-122
212．刘秀铭，许同春，刘东生．中国黄土磁化率各向异性与成因及其对第四纪研究的意义．中国科学(B辑)，1989，4：441—448
213．吕厚远，韩家懋，吴乃琴等．中国现代土壤磁化率分析及其古气候意义．中国科学(B辑)，1994，24(12)：1290—1297
214．鸟居雅之，福间洁司，苏黎等．黄土—古土壤磁化率述评．海洋地质与第四纪地质，1999，19(3)：83—96
215．潘保田，高红山，李吉均．关于夷平面的科学问题—兼论青藏高原夷平面．地理科学，2002，22(5)：520-526
216．潘保田，李吉均，曹继秀等．化隆盆地地貌演化与黄河发育研究．山地研究，1996，14(3)：153-158
217．潘保田，李吉均，陈发虎等．青藏高原：全球气候变化的驱动机与放大器．Ⅰ新生代气候变化的基本特征，兰州大学学报(自然科学版)，1995，31(3)：120-128
218．潘保田，李吉均，朱俊杰，曹继秀等．青藏高原：全球气候变化的驱动机与放大器．Ⅱ青藏高原隆起的基本过程．兰州大学学报(自然科学版)，1995，31(4)：160-167
219．潘保田，李吉均．青藏高原：全球气候变化的驱动机与放大器：青藏高原隆起对气候变化的影响．兰州大学学报(自然科学版)，1996，32(1)：108-115
220．潘保田，邬光剑，王义祥等．祁连山东段沙沟阶地的年代与成因．科学通报，2000，45(24)：2669-2675
221．潘保田．贵德盆地地貌演化与黄河上游发育研究．干旱区地理，1994，17(3)：3-50
222．潘保田．兰州地区黄土阶地发育与地貌演化．1991．见：中国第四纪冰川与环境，北京：科学出版社
223．潘保田，王均平，高红山等．河南扣马黄河最高级阶地古地磁年代及其对黄河贯通时代的指示．科学通报，2005，50(3)：255-261
224．潘永信，朱日祥．磁组构研究现状．地球物理学进展，1999，13(1)：52—59
225．潘裕生，孔祥儒，钟大赉等．高原岩石圈结构、演化和动力学．In：青藏高原形成演化与发展：孙鸿烈，郑度，广 东科技出版社，1998
226．潘裕生．青藏高原的形成与隆升．地学前缘，1999，6(3)
227．屈建军，郑本兴，俞祁浩．罗布泊东阿奇克谷地雅丹地貌与库姆塔格沙漠形成的关系．中国沙漠，2004，24(3)：294—300
228．施雅风，李吉均，李炳元，潘保田等．高原隆升与环境演化．In：青藏高原形成演化与发展：孙鸿烈，郑度，广东科技出版社，1998：76-78
229．施雅风，郑本兴．青藏高原中东部最大冰期时代高度与气候环境探讨．冰川冻土，1997，17(2)：97-112
230．施雅风．第四纪中期青藏高原冰冻圈的演化及其与全球变化的关系．冰川冻土，1998，20(3)：197-208
231．施雅风．中国第四纪冰期划分改进建议．冰川冻土，2002，24(6)：687—692
232．苏珍，施雅风，郑本兴．贡嘎山第四纪冰川遗迹及冰期划分．地球科学进展，2002，17(5)：639-647
233．孙继敏，丁仲礼，刘东生．50万a来沙漠．黄土边界带的环境演变．干旱区地理，1995，18(4)：2—9
234．孙继敏，丁仲礼，刘东生．黄土与古土壤磁组构测定在重建冬季风风向上的初步应用．科学通报．1995，40(21)：1976-1978
235．孙继敏，刘东生，丁仲礼等，五十万年来毛乌素沙漠的变迁．第四纪研究，1996，(4)：360—367
236．汤懋苍．董文杰等．青藏高原的抬升和夷平过程对气候与环境的影响．高原气象，1997，16(1)：23-29
237．汤懋苍，柳艳香等．青藏高原隆升的深层原因及其环境后果．第四纪研充2001，21(6)：500-507
238．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．地球科学进展，2004，19(1)：55-62
239．汤懋苍．高原季风的形成、演化及振荡特性．见：青藏高原近代气候变化及对环境的影响．广州：广东科技出版社，1998，161～183
240．田勤俭，申旭辉，冯希杰等．渭河盆地断层活动反映的第四纪构造事件初步研究，地震地质，2003，25(1)：146—154
241．童国榜，吴锡浩，陈云等．渭河谷地晚新生代地表环境巨变的孢粉记录．地质力学学报，2000，6(4)：11—18
242．汪品先，田军，成鑫荣．第四纪冰期旋回转型在南沙深海的记录．中国科学，2001，31(10)：793—799
243．汪品先．穿越圈层．横跨时空．地球科学进展，2002，17(3)：311-313
244．汪阳春，柴宗新，刘淑珍等．横断山地区的黄土及意义．山地学报，1999，17(4)：300-305
245．王岸，王国灿，向树元．东昆仑山东段北坡河流阶地发育及其与构造隆升的关系．地球科学—中国地质大学学报，2003，28(6)：675—679
246．王国灿，侯光久，张克信，朱云海．东昆仑东段中更新世以来的成山作用及其动力转换．地球科学—中国地质大学学报，2002，27(1)：4-12
247．王建力，方小敏，张宇田等．青藏高原东北边缘黄土磁化率各向异性揭示古风向的初步研究．兰州大学学报(自然科学版)，1995，31(4)：155-159
248．王克鲁，盛学斌，严富华等．山西洪洞王绪黄土地层划分．地质科学，1997，32(4)：495-505
249．王乃昂，张虎才，曹继秀等．腾格里沙漠南缘武咸黄土剖面磁性地层年代初步研究．兰州大学学报(自然科学版)，1997，33(4)：144-146
250．王苏民，吴锡浩，张振克等．三门古湖沉积记录的环境变迁与黄河贯通东流研究．中国科学(D)，2001，31(9)：760—768
251．王苏民，薛滨．中更新世以来若尔盖盆地环境演化与黄土高原比较研究．中国科学，26(4)：323-328
252．王涛．巴丹吉林沙漠形成演变的若干问题．中国沙漠，1990，10(1)：29-40
253．邬光剑，潘保田，管清玉等．中更新世全球最大冰期与中国沙漠扩张．冰川冻土，2002，24(5)：544-549
254．吴海滨，陈发虎，王建民等．现代风成沉积物磁化率各向异性与风向关系的研究．地球物理学报，1998，41(6)：811-817
255．吴汉宁，岳乐平．风成沉积物磁组构与中国黄土区第四纪风向变化．地球物理学报，1997，40(4)：487-494
256．吴文样，刘东生．更新世中期气候变化与手斧文化扩散．地学前缘，2001，8(2)
257．吴中海，赵希涛，江万等．念青唐古拉山东南麓更新世冰川沉积物年龄测定．冰川冻土，2003，25(3)：273-274
258．吴中海，赵希涛，朱大岗．念青唐古拉山西布冰川区的冰碛层．地球学报，2002，23(4)：343-348
259．伍永秋，崔之久，葛道凯等．青藏高原何时隆升到现代的高度-以昆仑山垭口地区为例．地理科学，1999，19(6)：481-484
260．伍永秋，崔之久，刘耕年等．昆仑山垭口地区的冰期序列．冰川冻土，1999，21(1)：71—76
261．徐孝彬，王建，朱捷等．利用宇生核素测年技术对青藏高原东南部冰蚀面年代的研究．地理科学，2004，24(1)：101-104
262．薛滨，王苏民，王云飞．湖泊深钻揭示的中更新世以来中国环境的区域分异及其与亚洲季风的关系．湖泊科学，1998，10(1)：1-4
263．薛祥熙，李文厚，刘玉林．渭河北迁与秦岭抬升．西北大学学报(自然科学版)，2002，32(5)：451-454
264．阎满存，董光荣，李保生等．腾格里沙漠东南缘沙漠演化的初步研究．中国沙漠，1998，18(2)：111—117
265．颜茂都，方小敏，陈诗越等．青藏高原更新世黄土磁化率和磁性地层与高原重大气候变化事件．中国科学(D辑)，2001，31：182-186
266．杨达源．中国东部的第四纪风尘堆积与季风变迁．第四纪研究，1991，4：354-359
267．姚檀栋．古里雅冰芯氧同位素地层学．第四纪研究，2000，20(2)：165-170
268．于革，王苏民．欧亚大陆湖泊记录和两万年以来大气环流变化．第四纪研究，1998，4：360-367
269．于洪军，韩德亮，初风友．晚更新世末期北方陆架区沙漠-黄土堆积群的初步研究．地质力学学报，1997，3(4)：33-38
270．张鸿义，门国发．塔克拉玛干沙漠腹地第四纪地层划分与环境变迁．新疆地质，2002，20(3)：256—261
271．张力小，宋豫秦．青藏高原的隆起对中国沙漠与沙漠化时空格局的影响．中国人口，资源与环境，2001，11(4)：98—101
272．张拴宏，周显强．磁化率各向异性地学应用综述．地质论评，1999，45(6)：613—620
273．张小曳．亚洲粉尘源区的分布、释放、输送、沉降和黄土堆积．第四纪研究，2001，21(1)：29—40
274．张叶春，李吉均，朱俊杰等．晚新生代金沙江形成时间与过程研究．云南地理环境研究，1998，10(2)：43—48
275．张叶春．长江三峡贯通的时代及意义．西北师大学报(自然科学版)，1995，31(2)：52—56
276．张智勇，于庆文，张克信，顾延生，向树元．黄河上游第四纪河流地貌演化-兼论青藏高原1：25万新生代地质填图地貌演化调查．地球科学，2003，28(6)：621—633
277．张祖陆．渤海莱州湾南岸滨海平原的黄土．海洋学报，1995，17(3)：127—134
278．赵景波，童国榜．秦岭太白盆地黄土地层发育时的古环境．西安地质学院学报，1994，16(1)：64-70
279．赵志军，史正涛，方小敏．祁连山北缘早中更新世新构造运动的地层记录．兰州大学学报(自然科学版)，2001，37(6)：92-98
280．郑本兴．云南玉龙雪山第四纪冰期与冰川演化模式．冰川冻土，2000，22(1)：53—61
281．郑本兴，施雅风．珠穆朗玛峰地区第四纪冰期探讨．见：珠穆朗玛地区科学考察报告(1966—1968)，第四纪地质学．北京：科学出版社，1976
282．郑度，李炳元．青藏高原地理环境研究进展．地理科学，1999，19(4)：295-302
283．郑度，林振耀，张雪芹．青藏高原与全球环境变化研究．地学前缘，2002，9(1)：95-102
284．钟大赉，丁林．青藏高原的隆起过程及其机制探讨．中国科学(D)，1996，26(4)：289-295
285．周尚哲，李吉均，张世强．祁连山摆浪河谷地的冰川地貌与冰期．冰川冻土，2001b，23(2)：131—138
286．周尚哲，李吉均．冰期之青藏高原新研究．地学前缘，2001 a，8(1)：67—75
287．周尚哲，易朝路，施雅风．中国西部MIS12冰期研究．地质力学学报，2001，7(4)：321—327
288．周秀骥．对地球系统科学的几点认识．地球科学进展，2004，19(5)：513-515
289．朱大岗，赵希涛，盂宪刚等．念青唐古拉山中段第四纪冰期划分．地球学报，2002，23(4)：335-342
290．朱俊杰，曹继秀，钟巍等．兰州地区黄河最高阶地与最老黄土堆积的发现及其古地磁年代学的研究．见：青藏项目专家委员会编．青藏高原形成演化、环境变迁与生态系统研究学术论文年刊(1994)．北京：科学出版社：77-90
291．朱日祥，AKazansky，G Matasova，等．西伯利亚南部黄土沉积物的磁学性质．科学通报，2000，45(11)：1200-1205
292．朱照宇．黄河中游河流阶地的形成与水系演化．地理学报，1989，44(4)：429～439