青藏高原腹地湖泊沉积物记录的中更新世以来的气候变化
|
摘要
青藏高原的形成和隆升对全球气候和环境变化产生了重要的影响和作用,一直以来都是国内外地理学研究的热点之一,普遍认为青藏高原是气候变化的敏感区。可可西里地区地处青藏高原腹地,该区由于受人类活动的干扰较小,大部分地区仍保持原始的自然状态,其特殊的地理位置、地壳结构和自然环境以及特有的生物区系组成等,是研究高原内部气候演化历史以及分析区域气候变化和全球气候变化异同点的理想地点。
文章以可可西里边缘地区106m深钻湖泊岩芯为材料,根据磁性地层学方法建立了BDQ06孔的天文轨道调谐时间标尺,坚实的年代学基础为区域和全球气候对比提供了可能。通过对BDQ06孔沉积物粒度、总有机碳、有机碳同位素组成(δ13Corg)、C/N、磁化率、色度、碳酸盐及其碳、氧同位素(δ13Ccar、δ18Ocar)等多环境指标的分析,重建了可可西里地区中更新世以来古气候古环境演化序列,并将本区气候变化与其它地质记录进行对比,发现它们在冰期-间冰期旋回的尺度上具有很强的相似性,但也存在明显的差异。既表现出与全球气候变化-致的信息,也反映了一定的区域特征。通过粒度特征并结合沉积速率的分析,分辨出中更新世以来青藏高原的3次明显隆升时期,分别为-0.6Ma、0.36Ma和0.16Ma。
功率谱分析显示本区0.9Ma以来气候变化既存在明显的轨道周期,同时也存在一些万年、千年尺度的气候不稳定振荡。同时小波分析显示本区0.9Ma以来不同时段气候变化周期信号强度不同,在约0.78Ma前出现较为显著的41ka周期,它与100ka周期同时出现,结束时伴随着100ka周期的最强功率谱出现,也就是说本区100ka周期在0.9Ma左右就已经出现,直到0.78Ma左右占据了主导优势,到0.58Ma左右100ka周期信号减弱,气候变化周期较为复杂,可能出现多种气候模式的组合。
青藏高原隆升可能对本区气候环境变化产生了重要的影响,昆黄运动(～0.6Ma)使高原隆升到一个临界高度(3000～3500m),导致大气环流发生了一次根本性的转变,由于高原的阻挡使原来爬越高原的西风改为绕流,高空西风波槽增强,扰动加剧。使青藏高原大范围进入冰冻圈,强烈的高原冬季风吹向阿拉伯海,降低海面表层温度,从而又削弱了夏季风。导致高原内部环境出现了明显的变化,表现出暖期不暖的特点,BDQ06孔显示此时气候波动幅度比上一阶段明显降低,各指标都显示出温度比较低。并且此时BDQ06孔各指标小波分析显示出100ka周期信号也受到影响,100ka周期信号变得较弱。说明此时气候变化不仅受到轨道驱动的影响,构造运动对气候产生的影响占有相当的比重,从而使本区气候表现出不规律的变化。0.36Ma的高原隆升可能导致了亚洲冬、夏季风都有加强,但其具体的隆升高度及其意义还有待进一步研究。共和运动(0.16Ma)使高原抬升到现代高度,奠定了现代气候的格局。
Tibet Plateau is one of the most climate-sensitive area, the climate change on Tibet Plateau considered as key issue to understand the paleoclimate system.The formation and uplift of Tibet plateau had profoundly influence on global climate and environmental change. Our study area Hoh Xil which locates on the northwest of Tibet plateau is the biggest national nature reserve of China. The research area is lightly interferred by human activity and takes on nearly original natural state. Therefore, it is an ideal region to investigate regional climate evolution and its relationship with global climate.
We took the106m deep drilling lake material cores in the Hohxil edge area of the region, and adopted tie points derived by matching the observed magnetostratigraphy to the geomagnetic polarity time scale (GPTS), developed an orbital tuned timescale for core BDQ06. The correct chronology was estimated from the experiment, which provides the possibility of comparison between regional and global climate. We analysed multi-proxies, such as the grian size, total orgnic carbon(TOC), Organic carbon isotope(δ13Corg), C/N, magnetic susceptibility, chroma and carbon and oxygen isotopes of carbonate(δ13Ccar、δ18Ocar), and reconstructed the history of evoluitons in palaeoclimate and palaeoenvironment since the Medio-Pleistocene. Furthermore, the climate change of our study area was compared with other geological record, the results indicated that there were very strong similarity with the scale of glacial-interglacial cycle, however there were also obvious regional differences. That is to say, our research area responded to global climate change with regional characteristics. Grain size parameters combined with deposition rate analysis showed there were three periods of markedly tectonic uplift of Qinghai-TibetanPlateau since Mid-Pleistocen,～0.60Ma,0.36Ma and0.16Ma, respectively.
The results of power spectrum analysis revealed that climate evolution not only corresponded to earth orbital cycle, but also presented oscillations in millennium and ten thousand scales during past0.9Ma. Furthermore, the signal intensity of climate evolution cycle exhibited the obvious difference. The climate evolution presented strength41ka cycle, and weakly100ka cycle during0.84～0.78Ma, Strongest100ka cycle power spectrum occurred which was the dominant cycle of climate evolution, and it was not weakened until0.58Ma, when the climate evolution cycle was more complicated. All of these evidences support that100ka cycle exists over the past0.9Ma and it turned to be dominant cycle around0.78Ma.
The uplift of Qinghai-Tibet plateau might have had an important influence on environmental change of study area. In particular, Kunhuang movement (～0.60Ma) drive plateau uplift to a critical height (about3000-3500m), and then the westerly was forced to divert and the aerological west storm tank was enhanced, which led to a fundamental shift of atmospheric circulation. After that, the Qinghai-Tibet plateau walked into cryosphere on a large range and the strong winter monsoon from the plateau blew into the Arabian Sea. Decreaed temperature of sea surface weakened the summer monsoon. As the result, the internal environment of the plateau was characterized by an obvious temperature change, even in the warm period the climate was still cool. The results from BDQ06borehole indicated that the climate fluctuation reduced significantly than that on the early stage, and all the indexes showed the lower temperature. In addition, the wavelet analysis of all the proxies from BDQ06borehole showed that100ka periodic signal was affected and became weaker. Climate change was not only forced by the orbital, but also forced by a quite proportion of the tectonic movement. Our results showed that climate change was very complex and had no explicit law in the study area. The uplift of the plateau at about0.36Ma caused the enhancement of the Asian winter and summer monsoon, but the uplift height and environmental signification still needed further research. Gonghe Movement (～0.16Ma) ultimately made the plateau uplift to the current height, which shaped the modern climate pattern.
文章以可可西里边缘地区106m深钻湖泊岩芯为材料,根据磁性地层学方法建立了BDQ06孔的天文轨道调谐时间标尺,坚实的年代学基础为区域和全球气候对比提供了可能。通过对BDQ06孔沉积物粒度、总有机碳、有机碳同位素组成(δ13Corg)、C/N、磁化率、色度、碳酸盐及其碳、氧同位素(δ13Ccar、δ18Ocar)等多环境指标的分析,重建了可可西里地区中更新世以来古气候古环境演化序列,并将本区气候变化与其它地质记录进行对比,发现它们在冰期-间冰期旋回的尺度上具有很强的相似性,但也存在明显的差异。既表现出与全球气候变化-致的信息,也反映了一定的区域特征。通过粒度特征并结合沉积速率的分析,分辨出中更新世以来青藏高原的3次明显隆升时期,分别为-0.6Ma、0.36Ma和0.16Ma。
功率谱分析显示本区0.9Ma以来气候变化既存在明显的轨道周期,同时也存在一些万年、千年尺度的气候不稳定振荡。同时小波分析显示本区0.9Ma以来不同时段气候变化周期信号强度不同,在约0.78Ma前出现较为显著的41ka周期,它与100ka周期同时出现,结束时伴随着100ka周期的最强功率谱出现,也就是说本区100ka周期在0.9Ma左右就已经出现,直到0.78Ma左右占据了主导优势,到0.58Ma左右100ka周期信号减弱,气候变化周期较为复杂,可能出现多种气候模式的组合。
青藏高原隆升可能对本区气候环境变化产生了重要的影响,昆黄运动(～0.6Ma)使高原隆升到一个临界高度(3000～3500m),导致大气环流发生了一次根本性的转变,由于高原的阻挡使原来爬越高原的西风改为绕流,高空西风波槽增强,扰动加剧。使青藏高原大范围进入冰冻圈,强烈的高原冬季风吹向阿拉伯海,降低海面表层温度,从而又削弱了夏季风。导致高原内部环境出现了明显的变化,表现出暖期不暖的特点,BDQ06孔显示此时气候波动幅度比上一阶段明显降低,各指标都显示出温度比较低。并且此时BDQ06孔各指标小波分析显示出100ka周期信号也受到影响,100ka周期信号变得较弱。说明此时气候变化不仅受到轨道驱动的影响,构造运动对气候产生的影响占有相当的比重,从而使本区气候表现出不规律的变化。0.36Ma的高原隆升可能导致了亚洲冬、夏季风都有加强,但其具体的隆升高度及其意义还有待进一步研究。共和运动(0.16Ma)使高原抬升到现代高度,奠定了现代气候的格局。
Tibet Plateau is one of the most climate-sensitive area, the climate change on Tibet Plateau considered as key issue to understand the paleoclimate system.The formation and uplift of Tibet plateau had profoundly influence on global climate and environmental change. Our study area Hoh Xil which locates on the northwest of Tibet plateau is the biggest national nature reserve of China. The research area is lightly interferred by human activity and takes on nearly original natural state. Therefore, it is an ideal region to investigate regional climate evolution and its relationship with global climate.
We took the106m deep drilling lake material cores in the Hohxil edge area of the region, and adopted tie points derived by matching the observed magnetostratigraphy to the geomagnetic polarity time scale (GPTS), developed an orbital tuned timescale for core BDQ06. The correct chronology was estimated from the experiment, which provides the possibility of comparison between regional and global climate. We analysed multi-proxies, such as the grian size, total orgnic carbon(TOC), Organic carbon isotope(δ13Corg), C/N, magnetic susceptibility, chroma and carbon and oxygen isotopes of carbonate(δ13Ccar、δ18Ocar), and reconstructed the history of evoluitons in palaeoclimate and palaeoenvironment since the Medio-Pleistocene. Furthermore, the climate change of our study area was compared with other geological record, the results indicated that there were very strong similarity with the scale of glacial-interglacial cycle, however there were also obvious regional differences. That is to say, our research area responded to global climate change with regional characteristics. Grain size parameters combined with deposition rate analysis showed there were three periods of markedly tectonic uplift of Qinghai-TibetanPlateau since Mid-Pleistocen,～0.60Ma,0.36Ma and0.16Ma, respectively.
The results of power spectrum analysis revealed that climate evolution not only corresponded to earth orbital cycle, but also presented oscillations in millennium and ten thousand scales during past0.9Ma. Furthermore, the signal intensity of climate evolution cycle exhibited the obvious difference. The climate evolution presented strength41ka cycle, and weakly100ka cycle during0.84～0.78Ma, Strongest100ka cycle power spectrum occurred which was the dominant cycle of climate evolution, and it was not weakened until0.58Ma, when the climate evolution cycle was more complicated. All of these evidences support that100ka cycle exists over the past0.9Ma and it turned to be dominant cycle around0.78Ma.
The uplift of Qinghai-Tibet plateau might have had an important influence on environmental change of study area. In particular, Kunhuang movement (～0.60Ma) drive plateau uplift to a critical height (about3000-3500m), and then the westerly was forced to divert and the aerological west storm tank was enhanced, which led to a fundamental shift of atmospheric circulation. After that, the Qinghai-Tibet plateau walked into cryosphere on a large range and the strong winter monsoon from the plateau blew into the Arabian Sea. Decreaed temperature of sea surface weakened the summer monsoon. As the result, the internal environment of the plateau was characterized by an obvious temperature change, even in the warm period the climate was still cool. The results from BDQ06borehole indicated that the climate fluctuation reduced significantly than that on the early stage, and all the indexes showed the lower temperature. In addition, the wavelet analysis of all the proxies from BDQ06borehole showed that100ka periodic signal was affected and became weaker. Climate change was not only forced by the orbital, but also forced by a quite proportion of the tectonic movement. Our results showed that climate change was very complex and had no explicit law in the study area. The uplift of the plateau at about0.36Ma caused the enhancement of the Asian winter and summer monsoon, but the uplift height and environmental signification still needed further research. Gonghe Movement (～0.16Ma) ultimately made the plateau uplift to the current height, which shaped the modern climate pattern.
引文
Abell P. Oxygen isotope ratios in modern African gastropod shells:a data base for paleoclimalogy[J]. Chem. Geol, Isotope Geosci.1985,58:183-193.
Alley R B. Ice-core evidence of abrupt climate change[J]. Proc Natl Acd Sci USA.1993,97: 1331-1334.
Alley R B, Meese D A, Shuman C A et al. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event[J]. Nature.1993,362:527-529.
An Zhisheng,Sun D,Zhang X et al. Accumulation sequence of Chinese loess and climatic records of Greenland ice core during the last 130 ka[J]. Chinese Science Bulletin.1995,40 (15):1272-1276.
An, Z., Huang, Y., Liu, W., Guo, Z. Multiple expansions of C4 plant biomass in East Asia since 7 Ma coupled with strengthened monsoon circulation[J]. Geology.2005,33:705-708. doi:10.1130/G21423.1
An Z., Kutzbach, J E., Prell, W.L., Porter, S C. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times[J]. Nature.2001,411:62-66.
An,Z.S.,Kukla,G.,Porter,S.C.,Xiao,J.L. Late Quaternary dust flow on the Chinese Loess Plateau[J]. Catena.1991,18:125-132.
Arenas C, Casanova J, Pardo G. Stable-isptope characterization of the Miocence lacustrine systems of Los Monegros (Ebro Basin,Spain):Paleogeographic and paleoclimatic implications[J]. Palaeogeography, Palaeoclimate, Palaeoecology.1997,128:133-155.
Avouac J.P., Dobremez J.F.Bourjot L. Paleoclimatic interpretation of a topgraphic profile across middle Holocene regressive shorelines of Longmu Co(Western Tibet) [J]. Paleogeogr., Paleoclimatol., Paleoecol.1996,120:93-104.
Berger, A., Loutre, M.F. Insolation values for the climate of the last 10 million years[J]. Quat. Sci. Rev.1991,10:297-317.
Berger, A., Loutre, M.F. Intertropical latitudes and precessional and half-precessional cycles[J]. Science.1997,278:1476-1478.
Becker, J., Lourens, L.J., Raymo, M.E. High-frequency climate linkages between the North Atlantic and the Mediterranean during marine oxygen isotope stage 100 (MIS100)[J]. Paleoceanography.2006,21, PA3002, doi:10.1029/2005PA001168
Baker P A, Rigsby C A, Seitzer G O, et al. Tropical climate changes at millennial and orbital timescales on the Bolivian Altiplano[J]. Nature.2001409:698-701.
Berger, W.H., Bickert, T., Jansen, E. The central mystery of the Quaternary Ice Age[J]. Oceanus. 1993,36:53-56.
Berger W.H., Jansen E. Mid-Pleistocene climate shift-The Nansen connection[J]. Geophysical Monograph.1994,84:295-311.
Berger A and Loutre M F. Insolation values for the climate of the last 10 million years[J]. Quaternary Scinese Reciew.1991,10:297-317.
BDP-99 Baikal Drilling Project Members. A new Quaternary record of regional tectonic, sedimentation and paleoclimate changes from drill core BDP-99 at Posolskaya Bank, Lake Baikal[J]. Quat. Int.2005,136:105-121.
Bowen R. Isotopes and Climates[M]. London, New York:Elsevier Applied Science,1990, 75-140.
Burcharott, B., Fritz, P. Environmental isotopes as environmental and climatological indicators [A], in:Handbook of Environmental Isotope Geochemistry[C], Part Ⅰ. eds P. Fritz and J. C. Fontes. Elsevier Scientific Publishers, Amsterdam,1980,478-504.
Campell C. Late Holocene lake sedimentology and climate change in southern Alberta, Canada[J]. Quaternary Research.1997, (49):96-101.
Cande, S.C., Kent, D.V. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic[J]. Geophys. Res.1995,100:6093-6095.
Chen ATC, Lou JY, Wann JK. Preliminary paleoclimatological records from high mountain lakes in Taiwan[J]. TAO.1993,4(3):321-329.
Chen F H, Bloemendaol J, Zhang P Z, et al. An 800 kyr proxy record of climate from lake sediments of the Zoige Basin, eastern Tibetan Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.1999,151(4):307-320.
Chou, C. Land-sea heating contrast in an idealized Asian summer monsoon[J]. Clim. Dynam., 2003,21:11-25.
Clark, P.U., Alley, R.B., Pollard, D. Northern Hemisphere ice-sheet influences on global climate change[J]. Science.1999,286:1104-1111.
Clark, P.U., Archer, D., Pollard, D et al. The Middle Pleistocene Transition:Characteristics, mechanisms, and implications for long-term hanges in atmospheric pCO2[J]. Quat. Sci. Rev., in press.2006.
Clark, P.U., Pisias, N.G., Stocker, T.F., Weaver, A.J., The role of the thermohaline circulation in abrupt climate change[J]. Nature.2002,415:863-869.
Clemens S C, Prell W L. A 350,000 year summer-monsoon multiproxy stack from the Owen Ridge, Northern Arabian Sea[J]. Mar Geol,2003,201:35-51.
Clemens S, Prell W, Murray D, et al. Forcing mechanisms of the Indian Ocean monsoon[J]. Nature.1991,353:720-725.
Craig H. The measurement of oxygen isotope palaeotemperatrue.In:Tongiorgi E. ed. Stable Isotopes in Ocean ographic Studies and Palaeotemperatrue[J]. Cons Naz Rich Lab Geo Nucl, Pisa.1965.161-182.
Cruz FW, Burns S J, Karmann I et al. Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil[J]. Nature.2005,434:63-66.
Dansgaard W, Clausen H B, Gundestrup N, et al. A new Greenland deep ice core[J], Science. 1982,218:1273-1277.
Dansgaard W, Johnsen S J. A flow model and time scale for the ice core from Camp Century, Greenland[J]. J Glaciol.1969,8:215-223.
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.
Dansgaard W, Johnson S, Meller J et al.One thousand centuries of climatic record from Camp Century on the Greenland ice sheet[J]. Science.1969,166:377-381.
Degens E T. Biogeochemistry of stable carbon isotope. In:G Eglinton (eds). Organic geochemistry [M]. Berlin:Springer-Verlag.1969.304-329.
Degens E T, et al. Metabolic fractionation of carbon isotopes in marine plankton:Temperature and respiration experiments[J]. Deep-See Res.1968,15:1-9.
Derbyshire,E.,Kemp,R.A.,Meng,X.M. Variations in loess and palaeosol properties as indicators of palaeoclimatic gradients across the Loess Plateau of Northern China[J]. Quaternary Science Reviews.1995,14:681-697.
Digerfeldt G, Olsson S, Sandgren P. Recons truction of lake level changes in lak e Xinias, central Greece, during the last 40000 years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology. 2000,158:65-82.
Ding, Z.L., Derbyshire, E., Yang, S.L. et al. Stacked 2.6-Ma grain sizerecord from the Chinese loess based on five sections and correlation with the deep-sea δ18O record[J]. Paleoceanography.2002a.17, doi:10.1029/2001PA000725.
Ding, Z.L., Derbyshire, E., Yang, S.L.et al. Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution[J]. Earth Planet. Sci. Lett.2005,237:45-55.
Ding, Z.L., Ranov, V., Yang, S.L. et al. The loess record in southern Tajikistan and correlation with Chinese loess[J]. Earth Planet. Sci. Lett.2002b 200:387-400.
Ding, Z.L., Liu.T.S., Rutter,N, Yu,Z.W. et al. Ice-Volume Forcing of East Asian Winter Monsoon Variations in the Past 800,000 Years[J]. Quaternary Research.1995,44:149-159.
Ding Z L,Ren J Z,Yang S L,et al.Climate instability during the penultimate glaciation:Evidence from two high-resolution loess records,China.Journal of Geophysical Research[J]. B:Solid Earth.1999,104(9):20123-20132.
Ding,Z.L.,Rutter,N.,Liu,T.S.,et al, Climatic correlation between loess and deep sea cores: astronomical approach[A],In Liu,T.S.(eds.),Loess,Environment and Chang,The series of the ⅩⅢINQUA congress[C], Beijing, Science Press,1991,168-186.
Ding,Z.L.,Rutter,N.W.,Liu,T.S.et al. Correlation of Dansgaard-Oeschger cycles between Greenland ice and Chinese Loess[J]. Paleoclimates.1998,4:281-291.
Ding Z L, Yu Z W., Rutter, N.W.et al. Towards an orbital time scale for Chinese loess deposits[J]. Quaternary Scinese Reviews.1994,13:39-70.
Drummond C N, PattersonW P, Walker J C G. Climatic forcing of carbon-oxygen isotopic covariance in temperate-region marl lakes[J]. Geology.1995,23:1031-1034.
E Chongyi, Wang Yong, Yang Taibao. Different responses of different altitudes surrounding Taklimakna Desert to global climate change[J]. Environmental Geology.2009,56(7): 1281-1293.
Emeis K C, A nderson D M, Doo se H et al. Sea surface temperatures and the history of monsoon upwelling in the No rthwest Arabian Sea during the last 500,000 years[J]. Quaternary Research.1995,43(2):355-361.
Emrich, k. et al. Carbon isotope fractionation during the precipitation of calcium carbonate[J]. Earth Planet. Sci. Letts.1970,8:363-371.
EPICA community members. Eight glacial cycles from an Antarctic ice core[J]. Nature,2004,429: 623-629.
Fang, X.-M., Li, J.-J., Van der Voo, R., Rock magnetic and grain size evidence for intensified Asian atmospheric circulation since 800,000 years B.P. related to Tibetan uplift[J]. Earth Planet. Sci. Lett.1999.165:129-144.
Fink, J. Kukla, G. J. Pleistocene climates in central Europe:at least 17 interglacials after the Olducai event[J]. Quaternary Research.1977,7:363-371.
Fontes J.Ch.,Melieres F.,Gibert E.et al.Stable isotope and radiocarbon balances of two Tibetan lakes (Sumxi Co,Longmu Co) from 13,000yr BP[J]. Quat.Sci.Rev.1993,12:875-887.
Fontes,J.C.et al, Holocene environmental changes in Lake Bangong basin(Western Tibet). Part: chronology and stable isotopes of carbonates of a Holocene lacustrine core[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.1996,120:25-47.
Gasse F, ArnoldM, Fontes J C, et al. A 13,000-year climate record from western Tibet[J]. Nature. 1991,353(24):742-745.
Gasse F.et al., Holocene enbironmental changes in Bangong Co badin(Western Tibet).Part4: Discussion and conclusions[J]. Palaeogeography,Palaeoclimatology,Palaeoecology.1996, 120(1-2):79-92.
Gasse F, Fontes J C, Plaziat J C, et al. Biological remains, geochemistry geochemistry and stable isotopes for the reconstruction of environmental and hydrological changes in the Holocene lakes from North Sahara[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.1987,60: 1-46.
Georg J K, Ralph R S, Peter J M. Late Quaternary Temperature Variability in the Bnguela Current System Derived from Alkenones[J]. Quaternary Researh.1999,52:92-103.
Glancarlo G Bmnehi, Nicholas McCave _Holocene perodicity in North Atlantic climate and deep-ocean flow south of lceland[J]. Nature.1999,397:515-517.
Giosan, L., Flood, R.D., Aller, R.C. Paleoceanographic significance of sediment color on western North Atlantic drifts:Ⅰ. Origin of color[J]. Mar. Geol.2002,189:25-41.
Groots P M, Stuive M, White J W et al. Comparison of oxygen isotope record from the GISP2 and GRIP Greenland ice cores[J]. Nature.1993,366:552-554.
GRIP Project Members. Climate instability during the last interglacial period recorded in the GRIP ice core[J]. Nature.1993,364:203-207.
Guiot J, Pons A, Beaulieu J I. et al. A 140 000-year continental climate reconstruction from two European pollen records[J]. Nature.1989,338:309-313.
Guo, Z., Liu, T., Fedoroff, N. Et al. Climate extremes in Loess of China coupled with the strength of deep-water formation in the North Atlantic[J]. Globle Planet. Change.1998,18:113-128.
Guo Z T, Biscaye P, Wei L Y, et al. Summer monsoon variations over the last 1.2Ma from the weathering of loess-soil sequences in China[J]. Geophysical Research Letter.2000,27(12): 1751-1754.
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[J]. Nature.2002,416:159-163.
Gupta S M. Orbital frequencies in radiolarian assemblages of the central Indian Ocean: Implications on the Indian summer monsoon[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.2003,197(1-2):97-112.
Hagelberg, T.K., Bond, G., deMenocal, P. Milankovitch band forcing of sub-Milankovitch climate variability during the Pleistocene[J]. Paleoceanography.1994,9:545-558.
Hailwood, E.A. The role of magnetostratigraphy in the development of geological time scales[J]. Paleoceanography.1989,4:1-18.
Hall, I.R., McCave, I.N., Shackleton, N.J. et al. Intensified deep Pacific inflow and ventilation in Pleistocene glacial times[J]. Nature.2001,412:809-812.
Hays, J D., Imbrie,J., Shackleton, N J. Variations in the Earth's orbit:Pacemaker of the Ice Ages[J]. Science.1976,194:1121-1132.
Heller F,Liu T S. Magnetism of Chinese loess deposit [J]. Journal of Geophysical Research.1984, 77:125-141.
Helmke, J.P., Bauch, H.A., Erlenkeuser, H. Development of glacial and interglacial conditions in the Nordic seas between 1.5 and 0.35 Ma[J]. Quat. Sci. Rev.2003,22:1717-1728.
Heusser LE, Van de Geer.G. Direct correlation of terrestrial and marine palaeoclimatic records from glacial-interglacial cycles-DSDP Site 594 southwest Pacific[J].Quaternary Science Reviews.1994,13:273-282.
Hilton J, Lishman J P, Chapman J S. Mannetic and chemical characterization of a diagenetic mineral formed in the sediments of productive lakes[J]. Chen, Geol.1986,56:325-335.
Hu, S., Goddu, S.R., Appel, E., et al. Palaeoclimatic changes over the past 1 million years derived from lacustrine sediments of Heqing basin (Yunnan, China). Quat. Int.2005,136:123-129.
Huybers, P., Wunsch, C. A depth-derived Pleistocene age model:Uncertainty estimates, sedimentation variability, and nonlinear climate change[J]. Paleoceanography.2004.19, PA1028, doi:10.1029/2002PA000857
Imbrie, J., Berger, A., Boyle, E.A. et al. On the structure and origin of major glaciation cycles 2: The 100,000-year cycle[J]. Paleoceanography.1993,8:699-736.
Imbrie J, Hays J,G, Martinson D G et al. The orbital theory of Pleistocene climate:Support From a revised chronology of the marine δ18O [A]. In:Berger A L, Imebrie J, Hays J et al. eds. Milankovitch and Climate(Part 1)[C].Dordrecht:Reidel Publishing Company,1984,269-305.
IPCC. Climate Change, the Physical Scientific Basis. Working Group I Contribution to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change[C], Cambridge, UK:Cambridge University Press,2007,1009.
James L.B.and Cummins K. Wisconsin Glaciation of the Sierra Nevada (79000-15000yr B1P1) as Recorded by Rock Flour, in Sediments of Owens Lake, California [J] Quaternary Research.2001,1 (55):14-24.
Jansen E The use of stable oxygen and carbon isotope stratigraphy as a dating tool[J]. Quaternary International.1989,1:151-166.
Jan. P, Helmke, Miehael Sehulz, Henning A. Baueh.Sediment—eolor Record from the Northeast Atlantic Reveals Patterns of Millennial-Seale Climate Variability during the Past 500,000 Years[J].Quaternary Researeh.2002,57:49-57.
Jean-Pieere, Bertini A, Leroy S A G et al. Towards the lowering of the Pliocene/Pleistocene boundary to the Gauss-Matuyama reversal[J]. Quaternary International.1997,40:37-42.
Jian, Z.M., Zhao, Q.H., Cheng, X.R. et al. Pliocene-Pleistocene stable isotope and paleoceanographic changes in the northern South China Sea[J]. Palaeogeogr. Palaeoclimatol. Palaeoecol.2003,193:425-442.
Kashiwaya K, Yamanoto A, Fukuyama K. Time Variations of Erosional force and grain size in Pleistocene lake sediments[J]. Quaternary Research.1985,28:61-68.
Kirschvink J L. The least-squares line and plane and the analysis of the paleomagnetic data[J]. Roy Astranom Soc Geophys J.1980,62:699-718.
Krishnamurthy R V, Bhattacharya S K, Sheela K. Palaeoclimatic changes deduced from 13C/12C and C/N ratioS of Karewa lake sediments,India[J].Nature.1986,323:150-152.
Kukla G. Loess stratigraphy of central Europe[A].In After the Australopithecines(edited by K.W. Butzer & G.I.Isaac)[C],Mouton Publishers,The Hague,1975,99-188.
Kukla G. Pleistocene climates in China and Europe cornpared to oxygen isotope record[J]. Palaeoeco,ogy of Africa.1987a,18:37-45.
Kukla G. Loess stratigraphy in central China[J].Quaternary Science Reviews.1987b,6:191-219
Kukla,G.,An,Z.S.Loess stratigraphy in Central China[J].Palaeogeograpby,palaeoclimatology, Palaeoecology.1989,72:203-225.
Kukla G,An Z S,Melice J L,et al.Magnetic susceptibility record of Chinese loess[J].Trans Royal,Soc Edinburgh:Earth Sc.1990,81:263-288.
Kukla G. J.Pleistocene land-sea correlaclon[J].Earth Science Reniew.1977,13:307-374.
Kutzbach J E.Monson climate of the early HOlocene:Climate experiment with the Earth's orbital parameters for 9000 years ago[J].Scinece.1981,214:59-61.
Kutzbach J E,Prell W L,Ruddiman W F.Sensitivity of Eurasian Climate to surface uplift of the Tibetan Plateau[J].J Geol.1993,101:177-190.
Kutzbach J.E.Street-Perrott F.A.Milankovich fbrcing of fluctuations in the level of tropical lakes from 18-0 kyr BP[J].Nature.1985,317:130-134.
Kuzbach J E,Guetter P J,Ruddirlman W F et al.Sensitibity of climate to late Cenozoic uplift in Southem Asia and the Ametican west:numerical expriments[J].J Geophys Res.1989,94: 18393-18407.
Langereis,C.G.,Dekkers,M.J.,de Lange,G.J.,et al.Magnetostratigraphy and astronomical calibration of the last 1.1 Myr from an eastern Mediterranearl piston core and dating of short events in the Brunhes[J].Geophys.J. Int.1997,129:75-94.
Larrasoafia,J.C.,Roberrs,A.P.,Rohling,E.J.,Winklhofer,M.,Wehatlsen,R.Three million years of monsoon vatiability over the nothern Sahara[J].Clim.Dynam.2003,21:689-698.
Lau,K.M.,Weng,H.Climate signal detection using wavelet transform:how to make a time series sing[J].Bull Am.Meteorol.Soc.1995,76.
Laurizen S Anderson P M.Introduction:The last Interglaciation in Artic and Subarctic:time frame,structure and duration[J].Quaternary Research.1995,43:115-116
Lear,C.H.,Elderneld,H.,Wilson,P.A..Cenozoic deep-sea ternperatures and global ice volumes from Mg/Ca in benthic foraminiferal calcite[J].Science.2000,287,269-272.
LengM J,Marshall J D.Palaeoclimate interp retation of stable isotope data ffom lake sediment archives[J].Quaternary Science Review.2004,23:811-831.
Li Jijun et al.Uplift of Qinghai-Xizang(Tibet)Plateau and Global Change[D].Lanzhou: LanZhou University,Press.1995.181-207.
Lisiecki, L.E., Lisiecki, P.A. Application of dynamic programming to the correlation of paleoclimate records[J].Paleoceanography.2002,17,1049,doi:10.1029/2001PA000733.
Lisiecki,L.E.,Raymo,M.E.A Pliocene.Pleistocene stack of 57 globally distributed benthic δ8O records[J].Paleoceanography.2005,20,PA1003,doi:10.1029/2004PA001071.
Lister,G.S.et alLake Qinghai,China:Closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene[J]. Palaeogeograpby, Palaeoclimatology, Palaeoecology.1991.84:141-162.
Lister G S,Kelts K,Chen K Z et al.Lake Qinghai,China:Closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene[J]. Palaeogeography Palaeoclimatology, Palaeoecology,.1991,84:141-162.
Liu,T.S.,Ding,Z.L.,Rutter,N. Comparison of Milanko vitch periods between continental loess and deep sea records over the last 2.5Ma[J]. Quaternary Science Reviews.1999,18:1205-1212.
Liu XD, kutzbach J E, Liu Z et al. The Tibetan Plateau as amplifier of orbital-scale variability of the East Asian monsoon[J]. Geophys Res lett. 2003,30(16):1839 dio:10.1029/2003GL017510
Liu Ze-chun, Wang Yong-jin, Yang Fan, et al. Stratigraphic and geochronology analyses of the quaternary deposits in the three-lake region of qaidam basin[J]. Science in China.1991,34(8): 987-1006.
Liu, Z. Magnetostratigraphy and sedimentologieal derived geoehronology of the Quaternary laeustrine deposits of a 3000m thiek sequence in the central qaidam basin[J]. PalaeogcograPhy, Palaeoclimatology, Palaeoecology,.1998,140:459-473.
Lizhong Yu, Oldfield F, Wu Yushu, et al. Paleoenvironmental imp lications of magnetic measure-ments on sediment core from Kunming basin Southwest China[J]. Journal of Paleoliminology.1990, (3):95-111.
Lorius C, Jouzel J, Ritz C et al. A 15000 year climatic record from Antarctic ice[J]. Nature.1985, 316(6029):591-596.
Lorius C, Merlivat L, Jouzel J. A 30000 year isotope climatic record from Antarctic ice[J]. Nature. 1989,280:644-648.
Lu, HY (Lu, Huayu); Zhao, CF (Zhao, Cunfa); Mason, J (Mason, Joseph);, Holocene climatic changes revealed by aeolian deposits from the Qinghai Lake area (northeastern Qinghai-Tibetan Plateau) and possible forcing mechanisms[J]. HOLOCENE.2011,21 (2):297-304. DOI:10.1177/0959683610378884
Manabe S, Broccoli A J. Mountains and arid climates of middle latitudes[J]. Science.1990,247: 192-194.
Manabe, S., Stouffer, R.J., Century-scale effects of increased atmospheric CO2 on the ocean-atmosphere system[J]. Nature.,1993.364:215-218.
Manabe S, Terpstra T B. The effects of mountains of the general circulation of the atmosphere by numerical experiments[J]. Journal of Atmospheric Science,1974,31:3-42.
Martinson D G, Pisias N G., Hays J D, et al. Age dating and the orbital theory of the ice ages: development of a high resolution 0-300,000 year chronostratigraphy[J]. Quaternary Research. 1987,27:1-29.
Masson-Delmotte V, Jouzel J, Parrenin F B, et al. EPICA Dome C:800000 years of climate and environmental history and relationship with orbital parameters[J]. Fourth Mars Polar Science Conference. Houston:Lunar and Planetary Institute,2006.8108
Mclntyre A, Molfino B. Forcing of Atlantic equatorial and subpolar millennial cycles by precession[J]. Scinece.1996,274:1867-1870.
Mctainsh G H, Nickling W G. Dust deposition and particle size in Mali, West Africa[J]. Catena. 1997,29:307-322.
Morner, N. A. and Lanser, J. P., Gothenburg Magnetic Flip[J]. Nature,1974,251:408-409.
Monnin E, Indermuhle A, Dallenbach A, et al. Atmospheric CO2 concentrations over the last glacial termination[J]. Science.2001,291:112-114.
Mook, W. Carbon 13 in hygrogeological studies. in:Handbook of Environmental Isotope Geochemistry, Part Ⅰ. eds P. Fritz and J. C. Fontes. Elsevier Scientific Publishers[J]. Amsterdam.1980.49-47.
Munsell A H. A Color Notation[M]. Boston.1905.
Narcissi B, Anselm i B. Lithostratigraphy of the 250000 year record of latchstring sediments from the valle di Castilian crater, Roma[J]. Quaternary Science Review.1992,11:353-362.
Niirnberg, D., Tiedemann, R. Environmental change in the Sea of Okhotsk during the last 1.1 million years[J]. Paleoceanography.2004,19, PA4011, doi:10.1029/2004PA001023.
Oldfield F. Environmental Magnetisma Personal Pers Peetive[J]. Quaternary Scinece Rebiews. 1991,10:73-85.
Oppo,D.W.,Fairbanks,R.G.,Gordon,A.C. Late Pleistocene Southern Oceanδ18O variability [J]. Paleoceanography.1990,5:43-54.
Overpeck, J.T., Otto-Bliesner, B., Miller, G.H., et al. Paleoclimatic evidence for future ice-sheet instability and rapid sea-level rise[J]. Science.2006,311:1747-1750.
Pachur H J, Wunnemann B, Zhang H C. Lake evolution in the Tengger Desert, Northwestern China, during the last 40000 Years[J]. Quaternary Research.1995,44:171-180.
Paillard, D.,. The timing of Pleistocene glaciations from a simple multiple-state climate model[J]. Nature.1998,391:378-381.
Paterson W S B, Koerner R M, Fisher D A, et al. An oxygen-isotope climatic record from the Devon Island ice cap, Arctic Cananda[J]. Nature.1977,266:508-511.
Patience A J. Kroom D. Oxygen isotope chronostratigraphy[J]. In Quaternary Dating Metheds-a User's Guide (edited by P. L. Smart & P D Frances)[M], Technical Guide 4, Quaternary Research Association, Cambridge,1991,199-228.
Pearson,F J and Coplen,T B. Stable isotope studies of lake. In:ALerman. ed. Lakes:Chemistry, Geology, Physics [M]. New York:Springerverlag,1978,235-236.
Petit J R, Jouzel J, Raynaud D, et al. Climate and atmospheric history of the past 420000 years from the Vostok ice core, Antarctica[J]. Nature.1999,399:429-436.
Pisias, N.G., Moore Jr., T.C.,The evolution of Pleistocene climate:a time series approach[J]. Earth Planet. Sci. Lett.1981,52:450-458.
Pokras EM, Mix A C. Earthps precession cycle and Quaternary climatic change in tropical Africa[J]. Nature.1987,326:486-487.
Prell, W.L., Oxygen and carbon isotope stratigraphy for the Quaternary of Hole 502B:Ebidence for two modes of isotopic variability[J]. in:W.L. Prell and J.V. Gardner et al. (eds.), Init. Repts.1982,68:455-464.
Ramstein, G., Fluteau, F., Besse, J., Joussaume, S. Effect of orogeny, plate motion and land-sea distribution on Eurasian climate change over the past 30 million years[J]. Nature.1997,386: 788-795.
Raymo M E. Oppo D W. Curru W. The Mid-Pleistocene climate transition:A deep sea carbon isotopic perspective[J]. Paleoceanography.1997,12(4):546-559.
Raymo, M.E., Oppo, D.W., Flower, B.P.et al. Stability of North Atlantic water masses in face of pronounced climate variability during the Pleistocene[J]. Paleoceanography.2004.19, PA2008, doi:2010.1029/2003PA000921
Rea, D.K., Snocks, H., Joseph, L.H. Late Cenozoic eolian deposition in the North Pacific Hemisphere[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,.1998,13:215-224.
Rhodes T.E.,Gasse F.,Ruifen L.et al. A late Pleistocene-Holocene laustrine record from Lake Manas(Northern Xinjiang,western China) [J]. Paleogeogr.,Paleoclimatol.,Paleoecol.1996, 120:105-121.
Rickett, R. D. T.C. Johnsona, E.T. Browna, et al. The Holocene paleolimnology of Lake lssyk-Kul, Kyrgyzstan:trace element and stable isotope composition of ostracodes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.2001,176(1-4):207-227.
Romanek C S, Grossman E L, Morse J W. Carbon isotopes fractionation in synthetic aragonite and calcite:effects of temperatureand precipitation rate[J]. Geochimica et Cosmochima Acta. 1992,56:419-430.
Rossigno-Strick M. African monsoons, an immediate climate response to orbital insolation[J]. Nature,1983,303:46-49.
Rubinson, M., Clayton, R. N. Carbon 13 fraction between aragonite and calcite[J]. Geochim. Cosmochim. Acta.1969,33,997-1002.
Rutherford, S., D'Hondt, S. Early onset and tropical forcing of 100,000-year Pleistocene glacial cycles[J]. Nature.2000,408:72-75.
Sarnthein, M. Winn, K. Jung, S. J.A. et al. Changes in east Atlantic deepwater circulation over the last 30,000 years:eight time slice reconstruction[J]. Paleoceanography,1994,9:209-267.
Savin, S. The history of the Earth's surface temperature during the past 100 million years[J]. Ann. Rev. Earth Planet. Sci.1977,5:319-335.
Scheffer f, Welte E, Zur Ftage der Eisinoxidhydrate im Boden[J]. Chm Erde.1958,19:51-64
SchefuB, E., Schouten, S., Fred Jansen, J.H et al. African vegetation controlled by tropical sea surface temperatures in the mid-Pleistocene period[J]. Nature.2003,422:418-421.
Schefuβ, E., Sinninghe Damste, J.S., Jansen, J.H.F. Forcing of tropical Atlantic sea surface temperatures during the mid-Pleistocene transition[J]. Paleoceanography.2004,19, PA4029, doi:10.1029/2003PA000892.
Schulz M., Mudelsee M. REDFIT:Estimating red-noise directly from unevenly spaced paleoclimatic time series[J]. Computer & Geoscience.2002,28:421-426.
Seiya Nagao, Satoru Nakashima. The factors controlling verticalcolor variations of north Atlantic Maderia Abyssal plain sediments[J]. Marine Geology.1992,109(1-2):83-94.
Shackleton, N.J. & Opdyke, N.D. Atmospheric carbon dioxide, orbital forcing and climate[J]. In The Carbon Cycle and Atmospheric CO2:Natural Variations Archean to Present (edited by E. Sundqvist&W.S.Broecker)[M], American Geophysical Union, Geophysical Monograph. 1985,32:303-317.
Shackleton, N.J., Berger, A., Peltier, W.R. An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677[J]. Trans. R. Soc. Edinb. Earth Sci.1990,81: 251-261.
Shackleton, N.J., Le, J. Mix, A. et al. Carbon isotope records from Pacific surface waters and atmospheric carbon dioxide[J]. Quaternary Science Reviews.1992,11:387-400.
Shackleton, N.J., Hagelberg, T.K., Crowhurst, S.J. Evaluating the success of astronomical tuning: pitfalls of using coherence as a criterion for assessing pre-Pleistocene timescales[J]. Paleoceanography.1995,10:693-967.
Shackleton N J, Opdyke N D. Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238:oxygen isotope temperatures and ice volume on a 105 and 106 year scale[J]. Quaternary Research.1973,3:39-55.
Shackleton N J. The 100 000-Year Ice Age Cycle Identified and Found to Lag Temperature, Carbon Dioxide, and Orbital Eccentricity [J]. Science.2000,289:1897-1902.
Shaeketon N, Opdyke N.Oxygen isotope and palaeomagnetic evidence for early Northern Hemisphere Glaciation[J]. Nature.1977,270:216-219.
Sharma, S.G. Moraa, J. W. Iohnstonb, et al. Stable isotope ratios in swale sequences of Lake Superior a S indicators of climate and lake level fluctuations during the Late Holocene[J] Quaternary Science Reviews.2005,24:1941-1951.
Shen J i, Liu Xingqi, Matsumoto R, et al. Palaeoclimate evolution reflected by highresolution multip roxies in Qinghai Lake since postglacial [J]. Science in China (Series D).2004,34 (6):582-589.
Shen Yongping, et al, Correlation of the ice age and loess deposit sequence in the Mt. Dalijia, Gansu, China[J]. Journal of Lanzhou University. Special issue on international workshop on loess geomorphological processes and harzards,1989,109-119.
Shi Yafeng, Ge Yu, Liu Xiaodong,et al.Reconstruction of the 40-30kaBP enhanced India Monsoon climate based on geogical records from Tibetan Plateau[J]. Paleogeography Paleoclimatology Paleoecology.2001,169(1):69-83.
Singer, B.S., Hoffman, K.A., Chauvin, A., Coe, R.S., Pringle, M.S. Dating transitionally magnetized lavas of the late Matuyama Chron:Toward a new 40Ar/39Ar timescale of reversals and events[J]. J. Geophys. Res.1999,104:679-693.
Smith,B.N,and Epstein S. Two categories of C/C ratios for higher plants[J]. Plant Physiology. 1971,47:380-384.
Smith B N, Epstein S. Two categories of 13C/12C ration for higher plants [J]. Plant Physiology. 1971, (47):380-384.
Soil Survey Staff. Soil Taxonomy—A Bacic System of Soil Classification for Making and Interpreting Soil Surveys[M]. USDA Handbook Number 436. Washington D C:US Gevernment Printing Office,1975.
Steven M Colman. Continental drilling for palaeoclimatic records[C]. PAGES Workshop Report, 1996, Series 96-104
Stuiver M. Oxygen and carbon isotope ratios of freshwater carbonate as climatic indicators[J]. Journal of Geophysics Research.1970,75:5247-5257.
Sun, J., Huang, X. Half-precessional cycles recorded in Chinese loess:response to low-latitude insolation forcing during the last interglaciation[J]. Quat. Sci. Rev.2006,25:1065-1072.
Sun Y B, Chen J, Clemens S C, et al. East Asian monsoon variability over the last seven glacial cycles recorded by a loess sequence from the northwestern Chinese Loess Plateau[J]. Geochem Geophys Geosys.2006,7:Q12Q02, doi:10.1029/2006GC001287
Sun, Y., Clemens, S.C., An, Z., Yu, Z. Astronomical timescale and palaeoclimatic implication of stacked 3.6-Myr monsoon records from the Chinese Loess Plateau[J]. Quat. Sci. Rev.2006, 25:33-48.
Telford, R.J., Heegaard, E., Birks, H.J.B. All age-depth models are wrong:but how badly[J] Quat. Sci.Rev.2004.23:1-5.
Thomson. D.J., SPeetrum Estimation And Harmonie Analysis Proeeedings Of The IEEE[C], 1982,70:1055-1096.
Thompson L G, Yao TD, DaviesM E, et al. Trop ical climate instability:The last glacial cycle from a Qinghai-Tibetan Plateau [J]. Science.1997,276:1821-1825.
Thompson R,Bloemendal J, Dearing J A, et al. Environmental app lications of magnetic measurements[J]. Science.1980,207 (4430):481-861.
Torrenece Christopher, Compo Gilbert P., A Practical guide to wavelet analysis[J]. Bulletin of the American Meteorological Society 1998,79:61-78.
Trenberth K E,Chen S C. Planetary waves kinematically forced by Himalayan orography[J], Journal of the Atmospheric Sciences.1988,45:2934-2948.
Trentesaux A, Recourt P, Roumazeilles V B, et al. Carbonate grain size distribution in hem ipelagic sediments from a laser particle sizer[J]. Journal of Sedimentary Research.2001, 71(5):858-862.
Von Campo,E.&Gasse F. Pollen-and diatom-inferred climatic and hydrological changes in Sumxi Co Basin(western Tibet)since 13,000yr B.P[J].Quaternary Research.1993.39:300-313.
Wang Fubao, Li Shengfeng, Shen Xuhui, et al. Formation, evolution and environmental changes of the Gyirong Basin and up lift of the Himalaya [J]. Science in China (Series D).1996,39 (4):401-409.
Wang Sumin,The record of Younger Dryas event in the lake sediment from Jalai Nur, Inner Mongolia[J]. Chinese Science Bulletin.1994 39(10):831-835.
Wang Sumin, Xue Bin. Environmental evolution of Zoige Basin since 900 kaB. P. and comparison study with Loess Plateau [J]. Science in China (SeriesD),1997,40(3):329-336
Wang Y J, Cheng H, Edwards R L, et al. A higher solution absolute dated late Pleistocene moosoon record from Hulu cave[J]. China.Science.2001,294:2345-2348.
Wang Y J, Cheng H, Edwards R L, et al. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years[J]. Nature.2008,451:1090-1093.
Wei K and Gasse F. Oxygen isotopes in lacustrine carbonates of west China revisited: Implications for Post Glacial changes in summer monsoon circulation[J].Quaternary Science Reviews.1999,18:1315-1334.
Williams D F, Peck J, karabanov E B, et al. Lake Bai kal record of continental climate response to orbital insolation during the past 5 million years[J]. Science.1997,278:1114-1117
Willis, K.J., Kleczkowski, A., Briggs, K.M., Gilligan, C.A., The role of sub-Milankovitch climatic forcing in the initiation of the Northern Hemisphere glaciation[J]. Science.1999,285: 568-571.
Wu J inglu, Wang Sumin, Shi Yafeng, et al. Temperature estimation by oxygen2stable record over the past 200ka in Zoige Basin [J].Science in China (Series D).2000,43 (6):577-586.
Xiao,J.L.,An,Z.S. Three large shifts in East Asian monsoon circulation indicated by loess-paleosol sequences in China and late Cenozoic deposits in Japan[J]. Palaeogeography, Palaeoclimatology, Palaeoecolo.1999,154:179-189.
Xue Bin, Wang Sumin, XiaWeilan, et al. The up lifting and environmental change of Qinghai-Xizang (Tibetan) Plateau in the past 0.9 Ma inferred from core RM of Zoige Basin [J]. Science in China(Series D).1998,41(2):165-170.
Yao Tandong. Abrupt climate change on Tibetan plateau during last interglacial cycle-comparison study of Guliya ice core Greenland ice core [J]. Science in China (Series D).1999,42(4): 358-368.
Yao Tandong, Thomp son L G, Shi Yafeng, et al. Climate variationsince the last interglaciation recorded in the Guliya ice core [J]. Science in China (Series D).1997,40 (6):662-668.
Yao Tandong, Thompson L G. Trends and features of climatic changes in the past 5000 years recorded by the Dunde ice core[J]. Annals of Glaciology.1992,16:21-24.
Yuan D, Cheng H, Edwards R L, et al. Timing, duration, and transitions of the last interglacial Asian Monsoon[J]. Science.2004,304:575-578.
Yu Lizhong, Oldfield F, Wu Yushu, et al. Paleoenvironmental implication of magnetic measure-ments on sediment core from Kunming Basin[J], Southwest China. Journal of Paleolimnology.1990,3:95-111.
Yu L Z, Oldfield, F., et al.. Paleoenvironmental implications of magnetic measurements on sediment core from Kunming Basin, Southwest China[J]. J Paleolimnol.1991,3:95-11.
Zhu Liping, Chen Ling, Li Bingyuan, et al. Environmental changes reflected by the lake sediments of the South Hongshan Lake,Northwest Tibet [J]. Science in China (Series D).2002,45 (5):430-439.
安芷生,肖举乐,张景昭等.季风与最近13万年黄土高原的气候历史[A].见：刘东生主编,黄土、第四纪与环境变化,第二集[c].北京,地质出版社,1991：108-114.
安芷生,李华梅,王俊达.洛川黄土剖面的古地磁学研究[J].地球化学1977,(4)：239-249.
安芷生,Porter S,Kukla等.最近13万年黄土高原季风变迁的磁化率证据[J].科学通报.1990,7：529-532.
安芷生,刘晓东.东亚季风气候的历史与变率[J].群学通报.2000,45(3)：238-249.
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[J].第四纪研究.2006,26(5)：678-692.
安芷生,吴锡浩,汪品先等.最近130ka中国的古季风--Ⅱ古季风变迁[J].中国科学(B辑).1999,11：1209-1215.
安芷生.亚洲季风演化、北半球大冰期的发展与喜马拉雅—青藏高原隆升[J].中国基础科学2001,(8)：9-11.
陈富斌,高生准,陈继良.甘孜黄土剖面磁性地层学初步研究[J].科学通报.1990.35：1600.
陈发虎,朱艳,李吉均等,民勤盆地湖泊沉积记录的全新世千百年尺度夏季风快速变化[J].科学通报.2001,46(17)：1414-1419.
陈发虎,张维信.甘青地区黄土地层和第四届冰川[M].北京：科学出版社.1993.
陈敬安,万国江,王福顺等.湖泊现代沉积物碳环境记录研究[J]中国科学(D辑).2002,32(1)：73-80.
陈敬安,万国江,汪福顺等.湖泊现代沉积物碳环境记录研究[J].中国科学(D辑).2003,2002,32(1)：73-80.
陈敬安,万国江.洱海沉积物化学元素与古气候演化[J].地带化学1999,28：562-570.
陈敬安,万国安,张峰等.不同时间尺度下的湖泊沉积物环境记录[J].中国科学(D辑).2003,33(6)：563-568.
陈诗越,方小敏,王苏民.川西高原甘孜黄土与印度季风演化关系[J].海洋地质与第四纪地质.2002,22(3)：41-46
陈忠.冰消期晚期以来德令哈尕海湖气候环境演变的碳、氧同位素记录[D].博士学位论文.西宁.中国科学院盐湖研究所.2007.
成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京：地质出版社.1978,31-36.
陈晔,袁林旺,周春林,刘泽纯.柴达木盆地第四纪古气候变化在自然伽玛测井曲线上的记录[J].古地理学报.2001,3：29-37.
陈克造,Bowler JM,Kelts K.四万年以来青藏高原的气候变迁[J].第四纪研究.1990,(1)：46-53.
陈克造.柴达木盆地晚更新世盐湖演化[A].见：中国科学院中澳第四纪合作研究组编,中国—澳大利亚第四纪学术讨论会论文集[C].北京：科学出版社.1987,83-91.
陈志明.从青藏高原隆起探讨西藏湖泊生态环境的变迁[J].海洋与湖沼.1981,12(5)：402-410.
曹升庚.土壤颜色的测定和描述—门赛尔土壤比色卡的应用[A].见：土壤分类及土壤地理论文集[C].北京：科学出版社.1985.
崔之久,吴永秋,刘耕年.关于“昆仑—黄河运动”[J].中国科学D辑.1998a,16(1)：53-60
崔之久,高全洲,刘耕年等.夷平面、古岩溶与青藏高原隆起[J].中国科学(D).1996,26(4)：378-385.
崔之久,吴永秋,刘耕年等.昆仑山垭口天然剖面记录[A].青藏高原晚新生代隆升和环境演化仁[M].广州：广东科技出版社.1998b,81-111.
崔之久,伍永秋,葛道凯等.昆仑山垭口地区第四纪环境演变[J].海洋地质与第四纪地质.1999,19(1)：53-62.
丁仲礼,刘东生.中国黄土研究新进展(一)黄土地层[J].第四纪研究.1989(1)：1-9.
丁仲礼,余志伟,刘东生.中国黄土研究新进展(三)时间标尺[J].第四纪研究.1991,(4)：336-348.
丁仲礼,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[J].中国科学(D辑).1999a,29(1)：82-87.
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[J].科学通报.1999b,44(3)：324-326.
鄂崇毅.新疆西风区粉尘研究[D].兰州大学.兰州大学图书馆.2009.
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[J].中国科学(D辑).2001,31：177-184.
方小敏,陈富斌,施雅风等.甘孜黄土与青藏高原冰冻圈演化[J].科学通报.1996,41：1865-1867.
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[J].科学通报.2002,47：540-545.
方小敏,李吉均,Van der Voo, R西秦岭黄土的形成年代及与物源区关系探讨[J].科学通报.1999,44：779-782.
高以信,张林源.青藏高原古土壤演化与高原隆起的关系[A]。见：龚子同主编,土壤环境变化[C].北京：中国科学技术出版社.1992,17-25.
顾兆言,刘嘉麒,袁宝印等.12000年来青藏高原季风变化——色林错沉积地球化学证据[J].科学通报.1993,38(1)：61-64.
郭佳宁.内蒙古宁城中更新世以来黄土磁化率与粒度特征及古环境研究[D],中国地质大学.北京.2009.
郭雪莲,王琪,史基安等.青海湖沉积物有机碳含量与同位素和粒度特征及其古气候意义[J].海洋地质与第四纪地质.2002,229(8)：99-102.
郭正堂,刘东生,Fedoroff N等.约0.85Ma前后黄土高原区季风强度的变化[J].科学通报.1993,38(2)：143-146.
胡东生.青藏高原第四纪湖泊地质环境演变[J].自然杂志.1995a,17(5)：257-261.
胡东生,张京华,徐冰等.青藏高原腹地第四纪地质环境演化的地球动力学机制[J],中国工程群学.2011,(13)：81-88.
胡东生.可可西里地区湖泊演化[J].干旱区地理.1995b,18(1)：60-67.
胡东生.可可西里地区湖泊水体中金富集规律的初步探讨[J].科学通报.1992,(16)：1499-1502.
胡东生,张华京,李炳元等.青藏高原腹地湖泊沉积序列与古气候变化[J].地质学报.2000,74(4)：363-370.
胡东生.可可西里地区湖泊水体地球化学特征[J].泊洋与湖泊.1997,28(2)：153-164.
胡东生,张华京,徐冰等.青藏高原腹地湖泊沉积对第四纪晚期古季风变化的响应[J].干旱区地理.2006,29(8)：483-489.
胡守云,吉磊,王苏民等.呼伦湖地区扎赉诺尔晚第四纪湖泊沉积物的磁化率变化及其影响因素[J].湖泊科学.1995,7(1)：33-40.
胡守云.呼伦湖湖泊沉积物磁化率变化的环境磁学机制[J].中国科学(D辑).1998a,28：334-339.
胡守云,王苏民,Apple E,等.呼伦湖湖泊沉积物磁化率变化的环境磁学机制[J].中国科学(D辑).1998b,28(4)：334-339.
黄赐璇,冯·康波·艾利斯,李拴科.根据孢粉分析论青藏高原西部和北部全新世环境变化[J].微体古生物学报.1996,13(4)：423-432.
黄翡,孙湘君.南海北部ODPI144站更新世(1.05—036Ma)抱粉记录[J].中国科学D(辑).2002,32(11)：914-920.
黄嘉佑.气象中的谱分析[M].气象出版社.1984.
黄汲清,闵隆瑞.青藏高原的隆升,沙漠和黄土的形成,人类的起源与演化[J].第四纪研究.1992,(1)：24-28.
黄孔怒.可可西里地区气候概况[J].青海环境.1989,(1)：28-29.
黄麒,孟昭强,刘海玲等.柴达木盆地查尔汗盐湖区古气候波动模式的初步研究[J].中国群学(B辑).1990,(6)：652-663.
黄小忠,陈发虎,肖舜等.新疆博斯腾湖沉积物粒度的古环境意义初探[J].湖泊科学.2008,20(3)：291-297.
江樟焰,伍永秋,崔之久.“昆仑-黄河运动”与我国自然地理格局的形成[J].北京师范大学学报.2005,41(1)85-88.
贾玉连,施雅风,范云崎.四万年以来青海湖的三期高湖面及其降水量研究[J].湖泊群笋2000,12(3)：182-192.
贾玉连,施雅风,王苏民等.40ka以来青藏高原的4次湖涨期及其形成机制初探[J].中国科学(D辑),2001,31(增刊)：241-251.
蒋庆丰,刘兴起,沈吉.乌伦古湖沉积物粒度特征及其古气候环境意义[J].沉积学报.2006,877-882.
金章东,邹成娟,高南华等.小冰期以来岱海地区的环境变迁与尘暴事件[J].西安工程学院学报.2001,23(4)：6-10.
刘传联.稳定同位素地球化学方法在古湖泊学研究中的应用[A]见：含油盆地古湖泊学研究方法[C]汪品先,刘传联主编,北京：海洋出版社.1993：96-123.
刘椿,刘东生,金增信,等.北京颐和园昆明湖近代沉积物的环境磁学初步研究及意义[J].群学通报.1994,39(21)：1989-1991.
刘东生,郑绵平,郭正堂等.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 的时代偶合性[J].第四纪研究.1998,18(3)：194-20.
刘东生等.黄土与环境[M].北京：科学出版社.1985.
刘东生,丁仲礼.二百五十万年来季风环流与大陆冰量变化的阶段性耦合过程[J].第四纪研究.1992,12(1)：12-23.
刘东生主编,黄土、第四纪与全球变化,第二集[M].北京,地质出版社.108-114.
刘光秀,王睿,李世杰等.西昆仑山甜水海24万年以来生态环境演化的孢粉学证据[J],冰川冻土,1998,20(1)：21-24.
刘光绣,沈永平,张平中等.青藏高原若尔盖地区RH孔800-150ka. B.P.的孢粉记录及古气候意义[J].沉积学报.1994,12(4)：101-109.
刘嘉麒,王文远.第四纪地质定年与地质年表[J].第四纪研究.1997,3：193-202.
刘冬雁,彭莎莎,乔彦松等.青藏高原东南缘甘孜黄土磁化率解释的西南季风演化[J].海洋地质与第四纪地质.2009,29(5)：115-121.
刘晓东,李力,安芷生.青藏高原隆升与欧亚内陆及北非的干旱化[J].第四纪研究.2001,21(2)：114-122.
刘晓东,汤懋苍.青藏高原影响气候的临界高度[A].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(1995).北京：科学出版社孙鸿烈主编,1996,青藏高原的形成演化。上海：社会科学技术出版社.1-369.
刘秀铭,刘东生,John S.中国黄土磁性矿物特征及其古气候意义[J].第四纪研究.1993(3)：282-287.
刘泽纯,陈晔,袁林旺等.应用自然伽玛测井曲线反演2.85Ma B.P来的古气候变化[J].中国科学(D辑).2000,26：316-322.
李才林.江淮平原末次冰消期以来环境变化的钻孔记录[D].南京师范大学.2007.
李长安,殷鸿福,于庆文.东昆仑山构造隆升与水系演化及其发展趋势[J].科学通报.1999,44(2)：211-214.
李炳元.西藏第四纪地质[M].北京：科学出版社.1983,15-130.
李炳元.羌塘高原北部湖泊演化的初步探讨[A]。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)[C].北京：科学出版社.1994,261-266.
李炳元,李吉均等.青藏高原第四纪冰川遗迹分布图[M].北京：科学技术出版社,1991.
李炳元.青藏高原晚新生代隆起于环境变化[M].广州：广东科技出版社,1998.
李炳元,李元芳,孔昭宸等.青海可可西里苟弄错地区近二万年来的环境变化[J].科学通报.1994,39(18)：1727-1728.
李炳元.青海可可西里地区自然环境[M].北京：科学出版社.1996.
李炳元等.青海省地貌图[M].测绘出版社.1988.
李炳元.青海可可西里地区综合科学考察初报[J].山地研究.1990,8(3)：161-166.
李炳元,李吉均.青藏高原第四纪冰川遗迹分布图(1：3000000)[M].科学出版社.1991
李炳元.青藏高原大湖期[J].地埋学报.2000,55(2)：174-182.
李国胜.艾比湖冰消期以来的δ13C记录与突变气候事件研究[J].科学通报.1993,38(22)：2069-2071.
李元芳,张青松,李炳元等.青藏高原西北部17000年以来的介形类及环境演变[J].地理学报.1994,49(1)：46-54.
李元芳,李炳元,王国等.西昆仑山甜水海介形类及其环境[J].湖泊科学.1997,9(3)：223-229.
李吉均,方小敏.青藏高原隆起与环境变化研究[J].科学通报.1998,43(15)：1569-1574.
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[J].中国科学1979(6)：608-616.
李吉均.青藏高原的地貌演化与亚洲季风[J].海洋地质第四纪地质.1999,19(1)：1-9.
李吉均.郑本兴等.西藏冰川[M].科学出版社.北京.1986,251-276.
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[J].中国科.D辑1996,26(4)：316-322.
李吉均,方小敏,潘保田等.新时代晚期青藏高原强烈隆起及其对周边环境的影响[J].第四纪研究.2001,21(5)：381-391.
李世杰,区荣康,朱照宇等.24万年以来西昆仑山甜水海湖岩芯碳酸盐含量与气候演化[J].湖泊群学.1998a,10(2)：58-65.
李世杰,李炳元,朱照宇等.甜水海湖泊钻探岩芯记录[A].1998b.见：施雅风,李吉均,李丙元,1998。青藏高原晚新生代隆起于环境变化[C].广州：广东科技出版社,215-246.
李世杰,王小天,夏威岚等.青藏高原苟鲁错湖泊沉积记录的小冰期气候变化[J].第四纪研究.2004,24(5)：578-584.
李世杰.青藏高原可可西里地区现代冰川发育特征[J].地理科学.1996,16(1)：10-17.
李华梅,王俊达.渤海湾北岸平原钻孔岩心的古地磁研究[J].地球化学.1983,(2)：196-204.
李育,王乃昂,李卓仑等.甘肃石羊河流域猪野泽湖泊沉积物粒度敏感组分与花粉组合关系[J].湖泊科学.2011,23(2)：295-302.
李红春,朱照宇.美国西部Owens湖地球化学记录及其古气候意义[J].第四纪研究.2002,22(6)：578-588.
李徐生,杨达源,韩辉友.皖南风尘堆积—古土壤序列磁化率初步研究[J].安徽师范大学学报(自然科学版).1998,21(1)：64-69.
莱尔曼.A,王苏民等译.湖泊的化学地质学和物理学[M].北京：地质出版社.1989.
雷国良,张虎才,张文翔等.柴达木盆地查尔汗古湖贝壳堤剖面粒度特征及其沉积环境[J].沉积学报.2007,25(2)：274-282.
吕厚远,王苏民,吴乃琴等.青藏高原错鄂湖2.8Ma来的孢粉记录[J].中国群笋(D辑).2001a,31(增刊)：234-240.
吕厚远,顾兆炎,吴乃琴等.海拔高度对青藏高原现代表土有机碳同位素组成的影响[J].第四纪研究.2001b,21(5)：399406.
鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义[J].中国科学(D辑).1998a,28(3)：278-283.
鹿化煜,杨文峰,刘晓东等.轨道调谐建立洛川黄土地层的时间标尺[J].地球物理学报.1998b,41(6)：804-810.
鹿化煜,安芷生,刘洪滨等.洛川黄土记录的最近2500 ka东亚冬夏季风变化周期[J].地质论评.1998c,44(5)：553-558.
卢武长.稳定同位素地球化学[M].成都：成都地质学院.1986.
卢演俦.黄土地层中CaCO3含量变化与更新世气候旋回[J].地质科学.1981,2：122-131.
罗运利,孙湘君,陈怀成.南海北部地区百万年以来的天然火与气候：ODP 1144孔深海沉积中的炭屑记录[J].群学通报.2006,51：942-950.
林振耀,吴洋定.青藏高原水汽输送路径的初步研究[J].地理研究.1990,9(3)：37.
林振耀,吴祥定.青藏高原隆起前后的气候状况[A].见：国科学院青藏高原综合科学考察队,1981青藏高原隆起的幅度和形式问题[C].北京：科学出版社.1981,159-165.
林晓,常浩,李云涛等.青藏高原东缘都江堰湖相沉积MIS3a阶段的快速气候变化记录[J],地球 科学—中国地质大学学报.2010,35(5)：858-866.
马玉贞,曹继秀,李吉均.甘肃临夏塬堡黄土剖面15万年来的孢粉植物群发展及气候演变[A].青藏高原形成演化、环境变迁与生态系统研究[C].北京：科学出版社.1995,103-113.
潘保田,邬光剑,王义祥等。祁连山东段沙沟河阶地的年代与成因[J].科学通报.2000,45：2669-2675.
潘保田.青藏高原全新世的气候与环境变化[A].见,施雅风,李吉均,李炳元编,青藏高原晚新生代隆升与环境变化[J].广州：广东科技出版社.1998,432-436.
庞小朋,韩凤清,吕亚平等.可可西里盐湖及其沉积特征初步研究[J].盐湖研究.2010,18(1)：9-14.
强明瑞,陈发虎,张家武等.2ka来苏干湖沉积碳酸盐稳定同位素记录的气候变化[J].科学通报.2005,50(13)：1385-1393.
乔彦松,郭正堂,郝青振等.皖南风尘堆积-土壤序列的磁性地层学研究及其古环境意义[J].科学通报.2003,48：1465-1469.
钱方,徐树全,陈富斌等.昔格达组磁性地层研究[J].山地研究1984,4(2)：171-179.
沈才明,唐领余,王苏民等.若尔盖盆地RM孔孢粉记录及其年代序列[J].科学通报.2005,50(3)：246-254.
沈吉,张恩楼,夏葳岚.青海湖近千年气候环境变化的湖泊沉积记录[J].第四纪研究.2001,21(6)：508-513.
沈吉,肖海丰,王苏民等.云南鹤庆钻孔揭示的区域气候轨道尺度演化[J].科学通报.2007,52(10)：1168-1173.
沈吉,吕厚远,王苏民等.错鄂孔深钻揭示的青藏高原中部2.8MaB. P.以来环境演化及其对构造事件响应[J].中国科学D辑.2004a,34(4)：359-366.
沈吉,刘兴起, Matsumoto R等.晚冰期以来青海湖沉积物多指标高分辨率的古气候演化[J].中国科学D辑.2004b,34(6)：582-589.
沈吉,汪勇,羊向东等.湖泊沉积记录的区域风沙特征及湖泊演化历史：以陕西红碱淖湖泊为例[J].科学通报.2006,1：87-92.
沈吉,肖海丰,王苏民等.云南鹤庆深钻揭示的区域气候轨道尺度演化[J].科学通报.2007,52：1168-1173.
沈振枢,程果,乐昌硕等.柴达木盆地第四纪含盐地层划分及沉积环境[M].北京：地质出版社.1993.
孙鸿烈,郑度.青藏高原形成演化与发展[M].广州：广东科技出版社.1998.
孙东怀,陈明扬John Shaw等.晚新生代黄土高原风尘堆积序列的磁性地层年代域古气候记录[J].中国科学(D辑).1998,28(1)：79-84.
孙东怀,刘禹,谭明.古环境记录的数字图像分析及应用[J].科学通报.2002,47(21)：1613-1618.
孙广友,罗新正,Turner R E.青藏东北部若尔盖高原全新世泥炭沉积年代学研究[J].沉积学报.2001,19(2)：177-182.
孙湘君,罗运利.南海北部280ka以来深海花粉记录[J].中国科学(D辑).2001,31(10)：846-853.
孙有斌,安芷生.最后4个冰期旋回中国黄土记录的东亚冬季风变化[J].地球科学—中国地质大学学报.2002,27(1)：19-24.
孙千里,周杰,肖举乐.岱海沉积物粒度特征及其古环境意义[J].海洋地质与第四纪地质.2001,21(1)：93-95.
施雅风,汤慰苍,马玉贞.青藏高原二期隆升与亚洲季风孕育关系探讨[J].中国科学(D辑). 1998a,28(3)：263-271.
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：广州科技出版社.1998b,PP419.
施雅风,李吉均,李炳元等.青藏高原隆升与环境演化[A].1998c.见”青藏高原形成演化与发展[C]."(孙鸿烈、郑度,编),pp.98-105.广东科技出版社.广州.
施雅风,李吉均,李炳元等.晚新时代青藏高原隆升与东亚环境变化[J].地理学报.1999a,54：10-21.
施雅风,刘晓东,李炳元等.距今40-30ka青藏高原特强夏季风事件及其与岁差周期关系[J],科学通报.1999b,44(14)：1475-1480.
施雅风,郑本兴,李世杰等.青藏高原中东部最大冰期的时代高度与气候环境探讨[J].冰川冻土.1995,17(2)：97-112.
施雅风,郑本兴.青截高原进入冰冻圈的时代、高度及其对周围地区的影响[A].见孙鸿烈、郑度主编藏高原形成演化、环境变迁与生态系统研究学术论文年刊(1995)[C].北京：科学出版社.1996,136-146.
师育新.兰州“930505”特大尘暴沉积物特征研究[J].沉积学报.1995,13(3)：76-82.
谭红兵,于升松.我国湖泊沉积环境演变研究中元素地球化学的应用现状及发展方向[J].盐湖研究.1999,7(3)：58-65.
唐领余,王睿.青海昆仑山垭口盆地第四纪湖泊沉积孢粉组合及其意义[A].见：中国科学院兰州冰川冻土沙漠研究所集刊,第一号[C].北京：科学出版社.1976,106-119.
汤懋苍,刘晓东.一个新的划分第四纪的标志——高原季风演变的地质环境后果[J].第四纪研究.1995,(1)：82-88.
田军.南海ODP1143站有孔虫稳定同位素揭示的上新世至更新世气候变化[D].博士学位论文.上海：同济大学.2002.
田庆春,杨太保,张述鑫等.青藏高原腹地湖泊沉积物磁化率及其环境意义[J].沉积学报.2011,29(1)：143-150.
藤则雄.根据日本中部琵琶湖深井孢粉资料重建第四纪古植被和古气候及全球占气候对比[J].古生物学报.2003,42(1)：138-147.
吴锡浩.晚新生代青藏高原隆升的阶段和高度[A].见：刘东生,安芷生主编,黄土·第四纪地质·全球变化(三)[C].北京：科学出版社.1992,1-12.
王富葆,韩灰有,阎革等.青藏高原东北部30ka来的古植被与古气候演变序列[J].中国科学(D辑).1996,26(2)：111-117.
王国安.稳定碳同位素在第四纪古环境研究中的应用[J].第四纪研究2003,23(5)：471-484.
王宁,刘卫国,徐黎明等.青藏高原现代湖泊沉积物碳酸盐矿物氧同位素组成特征及影响因素[J]第四纪研究2008,28(4)：591-600.
王苏民.湖泊沉积的信息原理与研究趋势[A].见：张兰生,中国生存环境历史演变规律研究[C],北京：海洋出版社.1993,22-31.
王苏民,张振克.中国湖泊沉积与环境演变研究的新进展[J].群学通报.1999,44(6)：579-587.
王苏民,施雅风,沈吉等.青藏高原东部800ka来古气候与古环境变迁的初步研究[A].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.1994,236-248.
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[J],中国辫学(D辑).1998,26(4)：323-328.
王苏民,施雅风.晚第四纪青海湖演化研究析视和讨论[J].湖泊科学.1992,4(3)：1-9.
王苏民,夏威岚,钱君龙等.若尔盖盆地RM孔的沉积特征与构造-气候演化过程[A].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[C].学术论文年刊,北京：科学出版社.1995.
王苏民,吉磊,羊向东等.呼伦湖—古湖泊学研究[M].合肥：中国科技大学出版社,1995.
王苏民,冯敏.内蒙古岱海湖泊环境变化与东南季风强弱的关系[J].中国科学(B).1991,(7)：759-767.
王心源,吴力,张广胜等.安徽巢湖全新世湖泊沉积物磁化率与粒度组合的变化特征及其环境意义[J].地理科学2008,28(4)：548-553.
王心源,张广胜,张恩楼等.巢湖湖泊沉积记录的早-中全新世环境演化研究[J].科学通报.2008,53(增刊Ⅰ)：132-138.
王绍武.气候系统引论[M].北京：气象出版社.1994,54-59.
王建,黄巧华.2.5 Ma以来柴达木盆地的气候干湿变化特征及其原因[J].地理科学.2002,22：34-38.
王澄海,董安祥,王式功等.青藏高原积雪与西北春节降水的相关特征[J].冰川冻土.2000,22(4)：340-346.
王云飞,王苏民,薛滨等.黄河袭夺若尔盖古湖时代的沉积学依据[J].科学通报.1995,40(8)：273-275.
王永波,刘兴起,羊向东等.可可西里库赛湖揭示的青藏高原北部近4000年来的干湿变化[J].湖泊科学.2008,20(5)：605-612.
王万春,吉利明.有机碳和有机分子碳同位素的地球化学意义[J].地球科学进展.1997,12(5)：74-478.
王赞红.现代尘暴降尘与非尘暴降尘的粒度特征[J].地理学报.2003,58(4)：606-610.
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[J].中国科学D辑:地球科学.2001,31(10)：793-799.
邬光剑.祁连山东段0.8 Ma以来的构造隆升与气候变化[M].博士学位论文,兰州大学.兰州.2001 pp.161.
邬光剑,潘保田,管清玉等.中更新世全球大冰期与中国沙漠扩张[J].冰川冻土.2002,24(5)：544-549.
吴福莉,方小敏,马玉贞等.黄土高原中部1.5 Ma以来古生态环境演化的孢粉记录[J].科学通报.2004.49：99-105.
吴敬禄,刘建军,王苏民.近1500年来新疆艾比湖同位素记录的气候环境演化特征[J].第四纪研究.2004,24(5)：585-590.
吴敬禄,王苏民,潘红玺等.青藏高原东部RM孔140ka以来湖泊碳酸盐同位素记录的古气候特征[J].中国科学(D辑).1997a,27,3：255-259.
吴敬禄,王苏民.青藏高原东部RM孔碳酸盐同位素揭示的末次间冰期气候特征[J].科学通报.1996,41(17)：1601-1604.
吴敬禄.若尔盖盆地RH孔近80万年来δ13Corg气候特征的频谱分析[J].湖泊科学1997b,9(3)：211-216.
吴乃琴,吕厚远等.C3、C4植物及其硅酸体研究的古气候意义[J].第四纪研究.1992,(2)：241-249.
吴艳宏,李世杰,王小天等.青藏高原苟鲁错湖泊沉积记录的小冰期气候变化[J].第四纪研究.2004a,24(5)：578-584.
吴艳宏,王苏民,夏威岚等.青藏高原中部0.2ka来的环境变化[J].中国科学(D辑).200131(增 刊)：264-269.
吴艳宏,王苏民,夏威岚等.1770年以来青藏高原错鄂地区古气候定量恢复[J].海洋地质与第四纪地质.2003,23(4)：115-120.
吴艳宏.青藏高原中部第四纪环境变迁的初步研究[D].中国科学院南京地理与湖泊研究所.2002.
吴艳宏,李世杰.湖泊沉积物色度在短尺度古气候研究中的应用[J].地球科学进展.2004b,19(5)：789-792.
吴瑞金.湖泊沉积物磁化率、频率磁化率的环境意义——以青海湖、岱海近代沉积为例[J].湖泊科学.1993.5(2)：128-135.
吴中海,赵希涛,江万.念青唐古拉山尔南麓更新世冰川沉积物年龄测定[J].冰川冻土.2003,25(3)：272-274.
薛滨,王苏民,夏威岚等.若尔盖RM孔揭示的青藏高原900kaBP以来的隆升与环境变化[J].中国科学(D辑).1997,27(6)：543-547.
薛滨,王苏民,吴艳宏等.若尔盖盆地RM孔揭示的过去14万年古环境[J].湖泊科学.1999,11(3)：206-212.
肖海丰,沈吉,肖霞云.云南鹤庆钻孔揭示的西南季风轨道尺度演化[J].第四纪研究.2006a,26(2)：274-282.
肖海丰,沈吉,肖霞云.云南鹤庆钻盆地2.78Ma以来的环境演化[J].湖泊科学.2006b,18(3)：255-260.
肖海丰,沈吉,肖霞云.鹤庆孔碳酸盐记录与深海δ18O和黄土粒度记录的对比[J].海洋地质与第四纪地质.2006c,26(2)：41-47.
谢又予等.沉积地貌分析[M].北京：海洋出版社.2000.3.
谢远云,李长安,王秋良等.江汉平原江陵湖泊沉积物粒度特征及气候环境意义[J].吉林大学学报(地球科学版).2007,37(3)：570-577.
徐仁,陶君容,孙湘君.希夏邦马峰高山栎化石层的发现及其在植物学和地质学上的意义[J].植物学报.1973,53：263-279.
徐馨,何才华,沈志达.关于中国气候地貌若干问题的探讨[J].贵州师范大学学报(自然科学版).1992,10(2)：1-12.
羊向东,王苏民,Kamenik C,等.藏南沉错钻孔硅藻组合与湖水古盐度定量恢复[J].中国群学D辑.2003,33(2)：163-169.
姚檀栋,王宁练.冰芯研究的过去、现在和未来[J].科学通报.1997a,42(3)：225-230.
姚檀栋,L G Thompson,施雅风等.古里雅冰芯中末次间冰期以来气候变化记录研究[J].中国科笋(D辑).1997b,27(5)：448-452.
姚檀栋,秦大河,田立德等.青藏高原2ka来温度与江水变化—古里雅冰芯记录[J].中国群学(D辑).1996,269(4)：348-353.
姚檀栋.末次冰期青藏高原的气候突变——古里雅冰芯与格陵兰GRIP冰芯对比研究[J].中国科学(D辑).1999,29,175-184.
杨建强,崔之久,易朝路等.云南点苍山冰川湖泊沉积物磁化率的影响因素及其环境意义[J].第四纪研究.2004,24(5)：591-597.
杨前进.沙尘暴沉积物的粒度特征及其环境意义[J].中国沙漠.2004,24(1)：47-50.
杨逸畴,张青松,李吉均等.高原隆起与环境变化[A].见孙鸿烈主编,青藏高原的形成演化[C].上海：上海科学技术出版社.1996,100-1151.
杨胜利.土壤颜色的气候意义[D].兰州：兰州大学资源与环境学院.2001.
杨胜利,方小敏,李吉均等.表土颜色和气候定性至半定量关系研究[J].中国科学(D辑).2001,31(增刊)：175-181.
杨志红,姚檀栋,皇翠兰等.古里雅冰芯中的新仙女木事件记录[J].群学通报.1997,42(18)：1975-1978.
阎满存,羞光荣,李保生等.腾格里沙淇东南缘沙淇演化的初步研究[J].中国沙漠.1998,18(2)：111-117
叶笃正,高由禧著.青藏高原气象学[J].北京：科学出版社.1979.1-278.
易朝路,焦克勤,刘克新等.冰碛物ESR测年与天山鸟鲁木齐河源末次冰期系列[J].冰川冻土.2001,23(4)：389-393.
殷勇,方念乔等.云南中甸纳帕海湖泊沉积物的磁化率及环境意义[J].地理科学.2002,22(4)：143-149.
余俊清,王小燕,李军等.湖泊沉积物有机碳同位素与环境的研究进展[J].湖泊科学.2001,13(1)：72-78.
余素华,朱照字,李炳元等.23万年以来青藏高原甜水海湖岩心铁元素的气候记录刍议[J].海洋地质与第四纪地质.1998,18(3)：63-68.
余志伟,丁仲礼.黄土古气候记录中的100 ka周期与岁差、半岁差周期的非线性耦合关系[J].中国科学(D辑).2003,33：520-528.
于永涛,柴达木盆地西北缘尕斯库勒湖钻孔记录的中更新世气候转型[D].兰州大学：兰州大学图书馆,2006.
袁林旺.柴达木盆地自然伽玛曲线记录的古气候变化信息研究[D].博士学位论文.南京师范大学.南京.2001.pp.130.
赵强,王乃昂,程弘毅等.青土湖沉积物粒度特征及其古环境意义[J].干旱区地理.2003,26(1)：1-5.
赵泉鸿,汪品先.南海第四纪古海洋学研究进展[J].第四纪研究.1999,6：481-501.
赵井东,周尚哲,崔建新等.乌鲁木齐河源冰碛物的ESR测年研究[J].冰川冻土.2002,24(6)：737-743.
张恩楼,沈吉,王苏民等.青海湖近900年来气候环境演化的湖泊沉积记录[J].湖泊科学.2002,14(1)：32-38.
张俊辉.柴达木盆地CH0310钻揭示的中更新世中晚期气候变化[D].兰州大学.兰州.2010.
张林源.青藏高原形成过程与我国新生代气候演变阶段的划分[A].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)[C].北京：科学出版社.1994,267-281.
张建军,杨达源,李徐生.长江中下游地区下蜀黄土磁化率曲线比较研究[J].华东地质学院学报.1999,22(2)：124-129.
张树夫,肖家仪,俞立中等.沉积物矿物磁性测量在古环境研究中的应用[J].地理科学.1991,11(2)：128-139.
张振克,吴瑞金,王苏民.岱海湖泊沉积物频率磁化率对历史时期环境变化的反映[J].地理研究.1998,17(3)：297-302.
张平中,王先彬,陈践发等.青藏高原若尔盖盆地RH孔沉积有机质的δ13C值和氢指数记录[J].中国科学(B辑).1995,25(6)：631-638.
张以茀,郑祥身.青海可可西里地区地质演化[M].北京：科学出版社.1996：9-15.
张成君,陈发虎,施祺等.西北干旱区全新世气候变化的湖泊有机质碳同位素记录——以石羊河流域三角城为例[J].海洋地质与第四纪地质.2000,20(4)：93-97.
张理刚.稳定同位素有地质科学中的应用[M].西安：陕西科学技术出版社.1985.
张彭熹,张保珍.柴达木地区距今三百万年来古气候环境演化的初步研究[J].地理学报.1991,46：327-335.
张彭熹,陈克造,于升松等.柴达木盆地盐湖[M].北京：科学出版社,1987.32-73.
张青松,周耀正,陆祥顺等.现代青藏高原上升速度问题[J].群学通报.1991,36(21)：1820-1824.
郑绵平,刘文高,向军等.论西藏的盐湖[J].地质学报.1983,(2)：184-193.
邹进上.气候学研究—“天、地、生”相互影响问题[M].北京：气象出版社.1989.
周爱锋.晚全新世苏干湖年纹层沉积及其环境变化[D].兰州,兰州大学图书馆.2007.
周才平,欧阳华,王勤学等.青藏高原主要生态系统净初级生产力的估算[J].地理学报.2004,59(1)：74-79.
周廷儒.近三十年来中国第四纪古地理研究的进展[J].地理学报.1979,34(4)：279-292.
周尚哲,李吉均,张世强等.祁连山摆浪河谷地的冰川地貌与冰期[J].冰川冻土.2001,23(2)：131-138.
周尚哲,李吉均.第四纪冰川测年研究新进展[J].冰川冻土.2003,23(6)：660-666.
周卫建,卢雪峰,武振坤等.若尔盖高原全新世气候变化的泥炭记录与加速器放射性碳测年[J].科学通报.2001,46(12)：1040-1044.
中国科学院南京地理与湖泊研究所,等.云南断陷湖泊环境与沉积[M].北京：科学出版社.1989,1-5.
朱芸,陈晔,舒强等.苏北盆地XH1钻孔中更新世以来的彩度指标记录及其气候环境变化[J].海洋地质与第四纪地质.2007,27(2)：23-31.
朱照宇,丁仲礼.中国黄土高原第四纪古气候与新构造演化[M].北京：地质出版社.1994,1-209.
Alley R B. Ice-core evidence of abrupt climate change[J]. Proc Natl Acd Sci USA.1993,97: 1331-1334.
Alley R B, Meese D A, Shuman C A et al. Abrupt increase in Greenland snow accumulation at the end of the Younger Dryas event[J]. Nature.1993,362:527-529.
An Zhisheng,Sun D,Zhang X et al. Accumulation sequence of Chinese loess and climatic records of Greenland ice core during the last 130 ka[J]. Chinese Science Bulletin.1995,40 (15):1272-1276.
An, Z., Huang, Y., Liu, W., Guo, Z. Multiple expansions of C4 plant biomass in East Asia since 7 Ma coupled with strengthened monsoon circulation[J]. Geology.2005,33:705-708. doi:10.1130/G21423.1
An Z., Kutzbach, J E., Prell, W.L., Porter, S C. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times[J]. Nature.2001,411:62-66.
An,Z.S.,Kukla,G.,Porter,S.C.,Xiao,J.L. Late Quaternary dust flow on the Chinese Loess Plateau[J]. Catena.1991,18:125-132.
Arenas C, Casanova J, Pardo G. Stable-isptope characterization of the Miocence lacustrine systems of Los Monegros (Ebro Basin,Spain):Paleogeographic and paleoclimatic implications[J]. Palaeogeography, Palaeoclimate, Palaeoecology.1997,128:133-155.
Avouac J.P., Dobremez J.F.Bourjot L. Paleoclimatic interpretation of a topgraphic profile across middle Holocene regressive shorelines of Longmu Co(Western Tibet) [J]. Paleogeogr., Paleoclimatol., Paleoecol.1996,120:93-104.
Berger, A., Loutre, M.F. Insolation values for the climate of the last 10 million years[J]. Quat. Sci. Rev.1991,10:297-317.
Berger, A., Loutre, M.F. Intertropical latitudes and precessional and half-precessional cycles[J]. Science.1997,278:1476-1478.
Becker, J., Lourens, L.J., Raymo, M.E. High-frequency climate linkages between the North Atlantic and the Mediterranean during marine oxygen isotope stage 100 (MIS100)[J]. Paleoceanography.2006,21, PA3002, doi:10.1029/2005PA001168
Baker P A, Rigsby C A, Seitzer G O, et al. Tropical climate changes at millennial and orbital timescales on the Bolivian Altiplano[J]. Nature.2001409:698-701.
Berger, W.H., Bickert, T., Jansen, E. The central mystery of the Quaternary Ice Age[J]. Oceanus. 1993,36:53-56.
Berger W.H., Jansen E. Mid-Pleistocene climate shift-The Nansen connection[J]. Geophysical Monograph.1994,84:295-311.
Berger A and Loutre M F. Insolation values for the climate of the last 10 million years[J]. Quaternary Scinese Reciew.1991,10:297-317.
BDP-99 Baikal Drilling Project Members. A new Quaternary record of regional tectonic, sedimentation and paleoclimate changes from drill core BDP-99 at Posolskaya Bank, Lake Baikal[J]. Quat. Int.2005,136:105-121.
Bowen R. Isotopes and Climates[M]. London, New York:Elsevier Applied Science,1990, 75-140.
Burcharott, B., Fritz, P. Environmental isotopes as environmental and climatological indicators [A], in:Handbook of Environmental Isotope Geochemistry[C], Part Ⅰ. eds P. Fritz and J. C. Fontes. Elsevier Scientific Publishers, Amsterdam,1980,478-504.
Campell C. Late Holocene lake sedimentology and climate change in southern Alberta, Canada[J]. Quaternary Research.1997, (49):96-101.
Cande, S.C., Kent, D.V. Revised calibration of the geomagnetic polarity timescale for the Late Cretaceous and Cenozoic[J]. Geophys. Res.1995,100:6093-6095.
Chen ATC, Lou JY, Wann JK. Preliminary paleoclimatological records from high mountain lakes in Taiwan[J]. TAO.1993,4(3):321-329.
Chen F H, Bloemendaol J, Zhang P Z, et al. An 800 kyr proxy record of climate from lake sediments of the Zoige Basin, eastern Tibetan Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.1999,151(4):307-320.
Chou, C. Land-sea heating contrast in an idealized Asian summer monsoon[J]. Clim. Dynam., 2003,21:11-25.
Clark, P.U., Alley, R.B., Pollard, D. Northern Hemisphere ice-sheet influences on global climate change[J]. Science.1999,286:1104-1111.
Clark, P.U., Archer, D., Pollard, D et al. The Middle Pleistocene Transition:Characteristics, mechanisms, and implications for long-term hanges in atmospheric pCO2[J]. Quat. Sci. Rev., in press.2006.
Clark, P.U., Pisias, N.G., Stocker, T.F., Weaver, A.J., The role of the thermohaline circulation in abrupt climate change[J]. Nature.2002,415:863-869.
Clemens S C, Prell W L. A 350,000 year summer-monsoon multiproxy stack from the Owen Ridge, Northern Arabian Sea[J]. Mar Geol,2003,201:35-51.
Clemens S, Prell W, Murray D, et al. Forcing mechanisms of the Indian Ocean monsoon[J]. Nature.1991,353:720-725.
Craig H. The measurement of oxygen isotope palaeotemperatrue.In:Tongiorgi E. ed. Stable Isotopes in Ocean ographic Studies and Palaeotemperatrue[J]. Cons Naz Rich Lab Geo Nucl, Pisa.1965.161-182.
Cruz FW, Burns S J, Karmann I et al. Insolation-driven changes in atmospheric circulation over the past 116,000 years in subtropical Brazil[J]. Nature.2005,434:63-66.
Dansgaard W, Clausen H B, Gundestrup N, et al. A new Greenland deep ice core[J], Science. 1982,218:1273-1277.
Dansgaard W, Johnsen S J. A flow model and time scale for the ice core from Camp Century, Greenland[J]. J Glaciol.1969,8:215-223.
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.
Dansgaard W, Johnson S, Meller J et al.One thousand centuries of climatic record from Camp Century on the Greenland ice sheet[J]. Science.1969,166:377-381.
Degens E T. Biogeochemistry of stable carbon isotope. In:G Eglinton (eds). Organic geochemistry [M]. Berlin:Springer-Verlag.1969.304-329.
Degens E T, et al. Metabolic fractionation of carbon isotopes in marine plankton:Temperature and respiration experiments[J]. Deep-See Res.1968,15:1-9.
Derbyshire,E.,Kemp,R.A.,Meng,X.M. Variations in loess and palaeosol properties as indicators of palaeoclimatic gradients across the Loess Plateau of Northern China[J]. Quaternary Science Reviews.1995,14:681-697.
Digerfeldt G, Olsson S, Sandgren P. Recons truction of lake level changes in lak e Xinias, central Greece, during the last 40000 years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology. 2000,158:65-82.
Ding, Z.L., Derbyshire, E., Yang, S.L. et al. Stacked 2.6-Ma grain sizerecord from the Chinese loess based on five sections and correlation with the deep-sea δ18O record[J]. Paleoceanography.2002a.17, doi:10.1029/2001PA000725.
Ding, Z.L., Derbyshire, E., Yang, S.L.et al. Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution[J]. Earth Planet. Sci. Lett.2005,237:45-55.
Ding, Z.L., Ranov, V., Yang, S.L. et al. The loess record in southern Tajikistan and correlation with Chinese loess[J]. Earth Planet. Sci. Lett.2002b 200:387-400.
Ding, Z.L., Liu.T.S., Rutter,N, Yu,Z.W. et al. Ice-Volume Forcing of East Asian Winter Monsoon Variations in the Past 800,000 Years[J]. Quaternary Research.1995,44:149-159.
Ding Z L,Ren J Z,Yang S L,et al.Climate instability during the penultimate glaciation:Evidence from two high-resolution loess records,China.Journal of Geophysical Research[J]. B:Solid Earth.1999,104(9):20123-20132.
Ding,Z.L.,Rutter,N.,Liu,T.S.,et al, Climatic correlation between loess and deep sea cores: astronomical approach[A],In Liu,T.S.(eds.),Loess,Environment and Chang,The series of the ⅩⅢINQUA congress[C], Beijing, Science Press,1991,168-186.
Ding,Z.L.,Rutter,N.W.,Liu,T.S.et al. Correlation of Dansgaard-Oeschger cycles between Greenland ice and Chinese Loess[J]. Paleoclimates.1998,4:281-291.
Ding Z L, Yu Z W., Rutter, N.W.et al. Towards an orbital time scale for Chinese loess deposits[J]. Quaternary Scinese Reviews.1994,13:39-70.
Drummond C N, PattersonW P, Walker J C G. Climatic forcing of carbon-oxygen isotopic covariance in temperate-region marl lakes[J]. Geology.1995,23:1031-1034.
E Chongyi, Wang Yong, Yang Taibao. Different responses of different altitudes surrounding Taklimakna Desert to global climate change[J]. Environmental Geology.2009,56(7): 1281-1293.
Emeis K C, A nderson D M, Doo se H et al. Sea surface temperatures and the history of monsoon upwelling in the No rthwest Arabian Sea during the last 500,000 years[J]. Quaternary Research.1995,43(2):355-361.
Emrich, k. et al. Carbon isotope fractionation during the precipitation of calcium carbonate[J]. Earth Planet. Sci. Letts.1970,8:363-371.
EPICA community members. Eight glacial cycles from an Antarctic ice core[J]. Nature,2004,429: 623-629.
Fang, X.-M., Li, J.-J., Van der Voo, R., Rock magnetic and grain size evidence for intensified Asian atmospheric circulation since 800,000 years B.P. related to Tibetan uplift[J]. Earth Planet. Sci. Lett.1999.165:129-144.
Fink, J. Kukla, G. J. Pleistocene climates in central Europe:at least 17 interglacials after the Olducai event[J]. Quaternary Research.1977,7:363-371.
Fontes J.Ch.,Melieres F.,Gibert E.et al.Stable isotope and radiocarbon balances of two Tibetan lakes (Sumxi Co,Longmu Co) from 13,000yr BP[J]. Quat.Sci.Rev.1993,12:875-887.
Fontes,J.C.et al, Holocene environmental changes in Lake Bangong basin(Western Tibet). Part: chronology and stable isotopes of carbonates of a Holocene lacustrine core[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.1996,120:25-47.
Gasse F, ArnoldM, Fontes J C, et al. A 13,000-year climate record from western Tibet[J]. Nature. 1991,353(24):742-745.
Gasse F.et al., Holocene enbironmental changes in Bangong Co badin(Western Tibet).Part4: Discussion and conclusions[J]. Palaeogeography,Palaeoclimatology,Palaeoecology.1996, 120(1-2):79-92.
Gasse F, Fontes J C, Plaziat J C, et al. Biological remains, geochemistry geochemistry and stable isotopes for the reconstruction of environmental and hydrological changes in the Holocene lakes from North Sahara[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.1987,60: 1-46.
Georg J K, Ralph R S, Peter J M. Late Quaternary Temperature Variability in the Bnguela Current System Derived from Alkenones[J]. Quaternary Researh.1999,52:92-103.
Glancarlo G Bmnehi, Nicholas McCave _Holocene perodicity in North Atlantic climate and deep-ocean flow south of lceland[J]. Nature.1999,397:515-517.
Giosan, L., Flood, R.D., Aller, R.C. Paleoceanographic significance of sediment color on western North Atlantic drifts:Ⅰ. Origin of color[J]. Mar. Geol.2002,189:25-41.
Groots P M, Stuive M, White J W et al. Comparison of oxygen isotope record from the GISP2 and GRIP Greenland ice cores[J]. Nature.1993,366:552-554.
GRIP Project Members. Climate instability during the last interglacial period recorded in the GRIP ice core[J]. Nature.1993,364:203-207.
Guiot J, Pons A, Beaulieu J I. et al. A 140 000-year continental climate reconstruction from two European pollen records[J]. Nature.1989,338:309-313.
Guo, Z., Liu, T., Fedoroff, N. Et al. Climate extremes in Loess of China coupled with the strength of deep-water formation in the North Atlantic[J]. Globle Planet. Change.1998,18:113-128.
Guo Z T, Biscaye P, Wei L Y, et al. Summer monsoon variations over the last 1.2Ma from the weathering of loess-soil sequences in China[J]. Geophysical Research Letter.2000,27(12): 1751-1754.
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[J]. Nature.2002,416:159-163.
Gupta S M. Orbital frequencies in radiolarian assemblages of the central Indian Ocean: Implications on the Indian summer monsoon[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.2003,197(1-2):97-112.
Hagelberg, T.K., Bond, G., deMenocal, P. Milankovitch band forcing of sub-Milankovitch climate variability during the Pleistocene[J]. Paleoceanography.1994,9:545-558.
Hailwood, E.A. The role of magnetostratigraphy in the development of geological time scales[J]. Paleoceanography.1989,4:1-18.
Hall, I.R., McCave, I.N., Shackleton, N.J. et al. Intensified deep Pacific inflow and ventilation in Pleistocene glacial times[J]. Nature.2001,412:809-812.
Hays, J D., Imbrie,J., Shackleton, N J. Variations in the Earth's orbit:Pacemaker of the Ice Ages[J]. Science.1976,194:1121-1132.
Heller F,Liu T S. Magnetism of Chinese loess deposit [J]. Journal of Geophysical Research.1984, 77:125-141.
Helmke, J.P., Bauch, H.A., Erlenkeuser, H. Development of glacial and interglacial conditions in the Nordic seas between 1.5 and 0.35 Ma[J]. Quat. Sci. Rev.2003,22:1717-1728.
Heusser LE, Van de Geer.G. Direct correlation of terrestrial and marine palaeoclimatic records from glacial-interglacial cycles-DSDP Site 594 southwest Pacific[J].Quaternary Science Reviews.1994,13:273-282.
Hilton J, Lishman J P, Chapman J S. Mannetic and chemical characterization of a diagenetic mineral formed in the sediments of productive lakes[J]. Chen, Geol.1986,56:325-335.
Hu, S., Goddu, S.R., Appel, E., et al. Palaeoclimatic changes over the past 1 million years derived from lacustrine sediments of Heqing basin (Yunnan, China). Quat. Int.2005,136:123-129.
Huybers, P., Wunsch, C. A depth-derived Pleistocene age model:Uncertainty estimates, sedimentation variability, and nonlinear climate change[J]. Paleoceanography.2004.19, PA1028, doi:10.1029/2002PA000857
Imbrie, J., Berger, A., Boyle, E.A. et al. On the structure and origin of major glaciation cycles 2: The 100,000-year cycle[J]. Paleoceanography.1993,8:699-736.
Imbrie J, Hays J,G, Martinson D G et al. The orbital theory of Pleistocene climate:Support From a revised chronology of the marine δ18O [A]. In:Berger A L, Imebrie J, Hays J et al. eds. Milankovitch and Climate(Part 1)[C].Dordrecht:Reidel Publishing Company,1984,269-305.
IPCC. Climate Change, the Physical Scientific Basis. Working Group I Contribution to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change[C], Cambridge, UK:Cambridge University Press,2007,1009.
James L.B.and Cummins K. Wisconsin Glaciation of the Sierra Nevada (79000-15000yr B1P1) as Recorded by Rock Flour, in Sediments of Owens Lake, California [J] Quaternary Research.2001,1 (55):14-24.
Jansen E The use of stable oxygen and carbon isotope stratigraphy as a dating tool[J]. Quaternary International.1989,1:151-166.
Jan. P, Helmke, Miehael Sehulz, Henning A. Baueh.Sediment—eolor Record from the Northeast Atlantic Reveals Patterns of Millennial-Seale Climate Variability during the Past 500,000 Years[J].Quaternary Researeh.2002,57:49-57.
Jean-Pieere, Bertini A, Leroy S A G et al. Towards the lowering of the Pliocene/Pleistocene boundary to the Gauss-Matuyama reversal[J]. Quaternary International.1997,40:37-42.
Jian, Z.M., Zhao, Q.H., Cheng, X.R. et al. Pliocene-Pleistocene stable isotope and paleoceanographic changes in the northern South China Sea[J]. Palaeogeogr. Palaeoclimatol. Palaeoecol.2003,193:425-442.
Kashiwaya K, Yamanoto A, Fukuyama K. Time Variations of Erosional force and grain size in Pleistocene lake sediments[J]. Quaternary Research.1985,28:61-68.
Kirschvink J L. The least-squares line and plane and the analysis of the paleomagnetic data[J]. Roy Astranom Soc Geophys J.1980,62:699-718.
Krishnamurthy R V, Bhattacharya S K, Sheela K. Palaeoclimatic changes deduced from 13C/12C and C/N ratioS of Karewa lake sediments,India[J].Nature.1986,323:150-152.
Kukla G. Loess stratigraphy of central Europe[A].In After the Australopithecines(edited by K.W. Butzer & G.I.Isaac)[C],Mouton Publishers,The Hague,1975,99-188.
Kukla G. Pleistocene climates in China and Europe cornpared to oxygen isotope record[J]. Palaeoeco,ogy of Africa.1987a,18:37-45.
Kukla G. Loess stratigraphy in central China[J].Quaternary Science Reviews.1987b,6:191-219
Kukla,G.,An,Z.S.Loess stratigraphy in Central China[J].Palaeogeograpby,palaeoclimatology, Palaeoecology.1989,72:203-225.
Kukla G,An Z S,Melice J L,et al.Magnetic susceptibility record of Chinese loess[J].Trans Royal,Soc Edinburgh:Earth Sc.1990,81:263-288.
Kukla G. J.Pleistocene land-sea correlaclon[J].Earth Science Reniew.1977,13:307-374.
Kutzbach J E.Monson climate of the early HOlocene:Climate experiment with the Earth's orbital parameters for 9000 years ago[J].Scinece.1981,214:59-61.
Kutzbach J E,Prell W L,Ruddiman W F.Sensitivity of Eurasian Climate to surface uplift of the Tibetan Plateau[J].J Geol.1993,101:177-190.
Kutzbach J.E.Street-Perrott F.A.Milankovich fbrcing of fluctuations in the level of tropical lakes from 18-0 kyr BP[J].Nature.1985,317:130-134.
Kuzbach J E,Guetter P J,Ruddirlman W F et al.Sensitibity of climate to late Cenozoic uplift in Southem Asia and the Ametican west:numerical expriments[J].J Geophys Res.1989,94: 18393-18407.
Langereis,C.G.,Dekkers,M.J.,de Lange,G.J.,et al.Magnetostratigraphy and astronomical calibration of the last 1.1 Myr from an eastern Mediterranearl piston core and dating of short events in the Brunhes[J].Geophys.J. Int.1997,129:75-94.
Larrasoafia,J.C.,Roberrs,A.P.,Rohling,E.J.,Winklhofer,M.,Wehatlsen,R.Three million years of monsoon vatiability over the nothern Sahara[J].Clim.Dynam.2003,21:689-698.
Lau,K.M.,Weng,H.Climate signal detection using wavelet transform:how to make a time series sing[J].Bull Am.Meteorol.Soc.1995,76.
Laurizen S Anderson P M.Introduction:The last Interglaciation in Artic and Subarctic:time frame,structure and duration[J].Quaternary Research.1995,43:115-116
Lear,C.H.,Elderneld,H.,Wilson,P.A..Cenozoic deep-sea ternperatures and global ice volumes from Mg/Ca in benthic foraminiferal calcite[J].Science.2000,287,269-272.
LengM J,Marshall J D.Palaeoclimate interp retation of stable isotope data ffom lake sediment archives[J].Quaternary Science Review.2004,23:811-831.
Li Jijun et al.Uplift of Qinghai-Xizang(Tibet)Plateau and Global Change[D].Lanzhou: LanZhou University,Press.1995.181-207.
Lisiecki, L.E., Lisiecki, P.A. Application of dynamic programming to the correlation of paleoclimate records[J].Paleoceanography.2002,17,1049,doi:10.1029/2001PA000733.
Lisiecki,L.E.,Raymo,M.E.A Pliocene.Pleistocene stack of 57 globally distributed benthic δ8O records[J].Paleoceanography.2005,20,PA1003,doi:10.1029/2004PA001071.
Lister,G.S.et alLake Qinghai,China:Closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene[J]. Palaeogeograpby, Palaeoclimatology, Palaeoecology.1991.84:141-162.
Lister G S,Kelts K,Chen K Z et al.Lake Qinghai,China:Closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene[J]. Palaeogeography Palaeoclimatology, Palaeoecology,.1991,84:141-162.
Liu,T.S.,Ding,Z.L.,Rutter,N. Comparison of Milanko vitch periods between continental loess and deep sea records over the last 2.5Ma[J]. Quaternary Science Reviews.1999,18:1205-1212.
Liu XD, kutzbach J E, Liu Z et al. The Tibetan Plateau as amplifier of orbital-scale variability of the East Asian monsoon[J]. Geophys Res lett. 2003,30(16):1839 dio:10.1029/2003GL017510
Liu Ze-chun, Wang Yong-jin, Yang Fan, et al. Stratigraphic and geochronology analyses of the quaternary deposits in the three-lake region of qaidam basin[J]. Science in China.1991,34(8): 987-1006.
Liu, Z. Magnetostratigraphy and sedimentologieal derived geoehronology of the Quaternary laeustrine deposits of a 3000m thiek sequence in the central qaidam basin[J]. PalaeogcograPhy, Palaeoclimatology, Palaeoecology,.1998,140:459-473.
Lizhong Yu, Oldfield F, Wu Yushu, et al. Paleoenvironmental imp lications of magnetic measure-ments on sediment core from Kunming basin Southwest China[J]. Journal of Paleoliminology.1990, (3):95-111.
Lorius C, Jouzel J, Ritz C et al. A 15000 year climatic record from Antarctic ice[J]. Nature.1985, 316(6029):591-596.
Lorius C, Merlivat L, Jouzel J. A 30000 year isotope climatic record from Antarctic ice[J]. Nature. 1989,280:644-648.
Lu, HY (Lu, Huayu); Zhao, CF (Zhao, Cunfa); Mason, J (Mason, Joseph);, Holocene climatic changes revealed by aeolian deposits from the Qinghai Lake area (northeastern Qinghai-Tibetan Plateau) and possible forcing mechanisms[J]. HOLOCENE.2011,21 (2):297-304. DOI:10.1177/0959683610378884
Manabe S, Broccoli A J. Mountains and arid climates of middle latitudes[J]. Science.1990,247: 192-194.
Manabe, S., Stouffer, R.J., Century-scale effects of increased atmospheric CO2 on the ocean-atmosphere system[J]. Nature.,1993.364:215-218.
Manabe S, Terpstra T B. The effects of mountains of the general circulation of the atmosphere by numerical experiments[J]. Journal of Atmospheric Science,1974,31:3-42.
Martinson D G, Pisias N G., Hays J D, et al. Age dating and the orbital theory of the ice ages: development of a high resolution 0-300,000 year chronostratigraphy[J]. Quaternary Research. 1987,27:1-29.
Masson-Delmotte V, Jouzel J, Parrenin F B, et al. EPICA Dome C:800000 years of climate and environmental history and relationship with orbital parameters[J]. Fourth Mars Polar Science Conference. Houston:Lunar and Planetary Institute,2006.8108
Mclntyre A, Molfino B. Forcing of Atlantic equatorial and subpolar millennial cycles by precession[J]. Scinece.1996,274:1867-1870.
Mctainsh G H, Nickling W G. Dust deposition and particle size in Mali, West Africa[J]. Catena. 1997,29:307-322.
Morner, N. A. and Lanser, J. P., Gothenburg Magnetic Flip[J]. Nature,1974,251:408-409.
Monnin E, Indermuhle A, Dallenbach A, et al. Atmospheric CO2 concentrations over the last glacial termination[J]. Science.2001,291:112-114.
Mook, W. Carbon 13 in hygrogeological studies. in:Handbook of Environmental Isotope Geochemistry, Part Ⅰ. eds P. Fritz and J. C. Fontes. Elsevier Scientific Publishers[J]. Amsterdam.1980.49-47.
Munsell A H. A Color Notation[M]. Boston.1905.
Narcissi B, Anselm i B. Lithostratigraphy of the 250000 year record of latchstring sediments from the valle di Castilian crater, Roma[J]. Quaternary Science Review.1992,11:353-362.
Niirnberg, D., Tiedemann, R. Environmental change in the Sea of Okhotsk during the last 1.1 million years[J]. Paleoceanography.2004,19, PA4011, doi:10.1029/2004PA001023.
Oldfield F. Environmental Magnetisma Personal Pers Peetive[J]. Quaternary Scinece Rebiews. 1991,10:73-85.
Oppo,D.W.,Fairbanks,R.G.,Gordon,A.C. Late Pleistocene Southern Oceanδ18O variability [J]. Paleoceanography.1990,5:43-54.
Overpeck, J.T., Otto-Bliesner, B., Miller, G.H., et al. Paleoclimatic evidence for future ice-sheet instability and rapid sea-level rise[J]. Science.2006,311:1747-1750.
Pachur H J, Wunnemann B, Zhang H C. Lake evolution in the Tengger Desert, Northwestern China, during the last 40000 Years[J]. Quaternary Research.1995,44:171-180.
Paillard, D.,. The timing of Pleistocene glaciations from a simple multiple-state climate model[J]. Nature.1998,391:378-381.
Paterson W S B, Koerner R M, Fisher D A, et al. An oxygen-isotope climatic record from the Devon Island ice cap, Arctic Cananda[J]. Nature.1977,266:508-511.
Patience A J. Kroom D. Oxygen isotope chronostratigraphy[J]. In Quaternary Dating Metheds-a User's Guide (edited by P. L. Smart & P D Frances)[M], Technical Guide 4, Quaternary Research Association, Cambridge,1991,199-228.
Pearson,F J and Coplen,T B. Stable isotope studies of lake. In:ALerman. ed. Lakes:Chemistry, Geology, Physics [M]. New York:Springerverlag,1978,235-236.
Petit J R, Jouzel J, Raynaud D, et al. Climate and atmospheric history of the past 420000 years from the Vostok ice core, Antarctica[J]. Nature.1999,399:429-436.
Pisias, N.G., Moore Jr., T.C.,The evolution of Pleistocene climate:a time series approach[J]. Earth Planet. Sci. Lett.1981,52:450-458.
Pokras EM, Mix A C. Earthps precession cycle and Quaternary climatic change in tropical Africa[J]. Nature.1987,326:486-487.
Prell, W.L., Oxygen and carbon isotope stratigraphy for the Quaternary of Hole 502B:Ebidence for two modes of isotopic variability[J]. in:W.L. Prell and J.V. Gardner et al. (eds.), Init. Repts.1982,68:455-464.
Ramstein, G., Fluteau, F., Besse, J., Joussaume, S. Effect of orogeny, plate motion and land-sea distribution on Eurasian climate change over the past 30 million years[J]. Nature.1997,386: 788-795.
Raymo M E. Oppo D W. Curru W. The Mid-Pleistocene climate transition:A deep sea carbon isotopic perspective[J]. Paleoceanography.1997,12(4):546-559.
Raymo, M.E., Oppo, D.W., Flower, B.P.et al. Stability of North Atlantic water masses in face of pronounced climate variability during the Pleistocene[J]. Paleoceanography.2004.19, PA2008, doi:2010.1029/2003PA000921
Rea, D.K., Snocks, H., Joseph, L.H. Late Cenozoic eolian deposition in the North Pacific Hemisphere[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,.1998,13:215-224.
Rhodes T.E.,Gasse F.,Ruifen L.et al. A late Pleistocene-Holocene laustrine record from Lake Manas(Northern Xinjiang,western China) [J]. Paleogeogr.,Paleoclimatol.,Paleoecol.1996, 120:105-121.
Rickett, R. D. T.C. Johnsona, E.T. Browna, et al. The Holocene paleolimnology of Lake lssyk-Kul, Kyrgyzstan:trace element and stable isotope composition of ostracodes[J]. Palaeogeography, Palaeoclimatology, Palaeoecology.2001,176(1-4):207-227.
Romanek C S, Grossman E L, Morse J W. Carbon isotopes fractionation in synthetic aragonite and calcite:effects of temperatureand precipitation rate[J]. Geochimica et Cosmochima Acta. 1992,56:419-430.
Rossigno-Strick M. African monsoons, an immediate climate response to orbital insolation[J]. Nature,1983,303:46-49.
Rubinson, M., Clayton, R. N. Carbon 13 fraction between aragonite and calcite[J]. Geochim. Cosmochim. Acta.1969,33,997-1002.
Rutherford, S., D'Hondt, S. Early onset and tropical forcing of 100,000-year Pleistocene glacial cycles[J]. Nature.2000,408:72-75.
Sarnthein, M. Winn, K. Jung, S. J.A. et al. Changes in east Atlantic deepwater circulation over the last 30,000 years:eight time slice reconstruction[J]. Paleoceanography,1994,9:209-267.
Savin, S. The history of the Earth's surface temperature during the past 100 million years[J]. Ann. Rev. Earth Planet. Sci.1977,5:319-335.
Scheffer f, Welte E, Zur Ftage der Eisinoxidhydrate im Boden[J]. Chm Erde.1958,19:51-64
SchefuB, E., Schouten, S., Fred Jansen, J.H et al. African vegetation controlled by tropical sea surface temperatures in the mid-Pleistocene period[J]. Nature.2003,422:418-421.
Schefuβ, E., Sinninghe Damste, J.S., Jansen, J.H.F. Forcing of tropical Atlantic sea surface temperatures during the mid-Pleistocene transition[J]. Paleoceanography.2004,19, PA4029, doi:10.1029/2003PA000892.
Schulz M., Mudelsee M. REDFIT:Estimating red-noise directly from unevenly spaced paleoclimatic time series[J]. Computer & Geoscience.2002,28:421-426.
Seiya Nagao, Satoru Nakashima. The factors controlling verticalcolor variations of north Atlantic Maderia Abyssal plain sediments[J]. Marine Geology.1992,109(1-2):83-94.
Shackleton, N.J. & Opdyke, N.D. Atmospheric carbon dioxide, orbital forcing and climate[J]. In The Carbon Cycle and Atmospheric CO2:Natural Variations Archean to Present (edited by E. Sundqvist&W.S.Broecker)[M], American Geophysical Union, Geophysical Monograph. 1985,32:303-317.
Shackleton, N.J., Berger, A., Peltier, W.R. An alternative astronomical calibration of the lower Pleistocene timescale based on ODP Site 677[J]. Trans. R. Soc. Edinb. Earth Sci.1990,81: 251-261.
Shackleton, N.J., Le, J. Mix, A. et al. Carbon isotope records from Pacific surface waters and atmospheric carbon dioxide[J]. Quaternary Science Reviews.1992,11:387-400.
Shackleton, N.J., Hagelberg, T.K., Crowhurst, S.J. Evaluating the success of astronomical tuning: pitfalls of using coherence as a criterion for assessing pre-Pleistocene timescales[J]. Paleoceanography.1995,10:693-967.
Shackleton N J, Opdyke N D. Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28-238:oxygen isotope temperatures and ice volume on a 105 and 106 year scale[J]. Quaternary Research.1973,3:39-55.
Shackleton N J. The 100 000-Year Ice Age Cycle Identified and Found to Lag Temperature, Carbon Dioxide, and Orbital Eccentricity [J]. Science.2000,289:1897-1902.
Shaeketon N, Opdyke N.Oxygen isotope and palaeomagnetic evidence for early Northern Hemisphere Glaciation[J]. Nature.1977,270:216-219.
Sharma, S.G. Moraa, J. W. Iohnstonb, et al. Stable isotope ratios in swale sequences of Lake Superior a S indicators of climate and lake level fluctuations during the Late Holocene[J] Quaternary Science Reviews.2005,24:1941-1951.
Shen J i, Liu Xingqi, Matsumoto R, et al. Palaeoclimate evolution reflected by highresolution multip roxies in Qinghai Lake since postglacial [J]. Science in China (Series D).2004,34 (6):582-589.
Shen Yongping, et al, Correlation of the ice age and loess deposit sequence in the Mt. Dalijia, Gansu, China[J]. Journal of Lanzhou University. Special issue on international workshop on loess geomorphological processes and harzards,1989,109-119.
Shi Yafeng, Ge Yu, Liu Xiaodong,et al.Reconstruction of the 40-30kaBP enhanced India Monsoon climate based on geogical records from Tibetan Plateau[J]. Paleogeography Paleoclimatology Paleoecology.2001,169(1):69-83.
Singer, B.S., Hoffman, K.A., Chauvin, A., Coe, R.S., Pringle, M.S. Dating transitionally magnetized lavas of the late Matuyama Chron:Toward a new 40Ar/39Ar timescale of reversals and events[J]. J. Geophys. Res.1999,104:679-693.
Smith,B.N,and Epstein S. Two categories of C/C ratios for higher plants[J]. Plant Physiology. 1971,47:380-384.
Smith B N, Epstein S. Two categories of 13C/12C ration for higher plants [J]. Plant Physiology. 1971, (47):380-384.
Soil Survey Staff. Soil Taxonomy—A Bacic System of Soil Classification for Making and Interpreting Soil Surveys[M]. USDA Handbook Number 436. Washington D C:US Gevernment Printing Office,1975.
Steven M Colman. Continental drilling for palaeoclimatic records[C]. PAGES Workshop Report, 1996, Series 96-104
Stuiver M. Oxygen and carbon isotope ratios of freshwater carbonate as climatic indicators[J]. Journal of Geophysics Research.1970,75:5247-5257.
Sun, J., Huang, X. Half-precessional cycles recorded in Chinese loess:response to low-latitude insolation forcing during the last interglaciation[J]. Quat. Sci. Rev.2006,25:1065-1072.
Sun Y B, Chen J, Clemens S C, et al. East Asian monsoon variability over the last seven glacial cycles recorded by a loess sequence from the northwestern Chinese Loess Plateau[J]. Geochem Geophys Geosys.2006,7:Q12Q02, doi:10.1029/2006GC001287
Sun, Y., Clemens, S.C., An, Z., Yu, Z. Astronomical timescale and palaeoclimatic implication of stacked 3.6-Myr monsoon records from the Chinese Loess Plateau[J]. Quat. Sci. Rev.2006, 25:33-48.
Telford, R.J., Heegaard, E., Birks, H.J.B. All age-depth models are wrong:but how badly[J] Quat. Sci.Rev.2004.23:1-5.
Thomson. D.J., SPeetrum Estimation And Harmonie Analysis Proeeedings Of The IEEE[C], 1982,70:1055-1096.
Thompson L G, Yao TD, DaviesM E, et al. Trop ical climate instability:The last glacial cycle from a Qinghai-Tibetan Plateau [J]. Science.1997,276:1821-1825.
Thompson R,Bloemendal J, Dearing J A, et al. Environmental app lications of magnetic measurements[J]. Science.1980,207 (4430):481-861.
Torrenece Christopher, Compo Gilbert P., A Practical guide to wavelet analysis[J]. Bulletin of the American Meteorological Society 1998,79:61-78.
Trenberth K E,Chen S C. Planetary waves kinematically forced by Himalayan orography[J], Journal of the Atmospheric Sciences.1988,45:2934-2948.
Trentesaux A, Recourt P, Roumazeilles V B, et al. Carbonate grain size distribution in hem ipelagic sediments from a laser particle sizer[J]. Journal of Sedimentary Research.2001, 71(5):858-862.
Von Campo,E.&Gasse F. Pollen-and diatom-inferred climatic and hydrological changes in Sumxi Co Basin(western Tibet)since 13,000yr B.P[J].Quaternary Research.1993.39:300-313.
Wang Fubao, Li Shengfeng, Shen Xuhui, et al. Formation, evolution and environmental changes of the Gyirong Basin and up lift of the Himalaya [J]. Science in China (Series D).1996,39 (4):401-409.
Wang Sumin,The record of Younger Dryas event in the lake sediment from Jalai Nur, Inner Mongolia[J]. Chinese Science Bulletin.1994 39(10):831-835.
Wang Sumin, Xue Bin. Environmental evolution of Zoige Basin since 900 kaB. P. and comparison study with Loess Plateau [J]. Science in China (SeriesD),1997,40(3):329-336
Wang Y J, Cheng H, Edwards R L, et al. A higher solution absolute dated late Pleistocene moosoon record from Hulu cave[J]. China.Science.2001,294:2345-2348.
Wang Y J, Cheng H, Edwards R L, et al. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years[J]. Nature.2008,451:1090-1093.
Wei K and Gasse F. Oxygen isotopes in lacustrine carbonates of west China revisited: Implications for Post Glacial changes in summer monsoon circulation[J].Quaternary Science Reviews.1999,18:1315-1334.
Williams D F, Peck J, karabanov E B, et al. Lake Bai kal record of continental climate response to orbital insolation during the past 5 million years[J]. Science.1997,278:1114-1117
Willis, K.J., Kleczkowski, A., Briggs, K.M., Gilligan, C.A., The role of sub-Milankovitch climatic forcing in the initiation of the Northern Hemisphere glaciation[J]. Science.1999,285: 568-571.
Wu J inglu, Wang Sumin, Shi Yafeng, et al. Temperature estimation by oxygen2stable record over the past 200ka in Zoige Basin [J].Science in China (Series D).2000,43 (6):577-586.
Xiao,J.L.,An,Z.S. Three large shifts in East Asian monsoon circulation indicated by loess-paleosol sequences in China and late Cenozoic deposits in Japan[J]. Palaeogeography, Palaeoclimatology, Palaeoecolo.1999,154:179-189.
Xue Bin, Wang Sumin, XiaWeilan, et al. The up lifting and environmental change of Qinghai-Xizang (Tibetan) Plateau in the past 0.9 Ma inferred from core RM of Zoige Basin [J]. Science in China(Series D).1998,41(2):165-170.
Yao Tandong. Abrupt climate change on Tibetan plateau during last interglacial cycle-comparison study of Guliya ice core Greenland ice core [J]. Science in China (Series D).1999,42(4): 358-368.
Yao Tandong, Thomp son L G, Shi Yafeng, et al. Climate variationsince the last interglaciation recorded in the Guliya ice core [J]. Science in China (Series D).1997,40 (6):662-668.
Yao Tandong, Thompson L G. Trends and features of climatic changes in the past 5000 years recorded by the Dunde ice core[J]. Annals of Glaciology.1992,16:21-24.
Yuan D, Cheng H, Edwards R L, et al. Timing, duration, and transitions of the last interglacial Asian Monsoon[J]. Science.2004,304:575-578.
Yu Lizhong, Oldfield F, Wu Yushu, et al. Paleoenvironmental implication of magnetic measure-ments on sediment core from Kunming Basin[J], Southwest China. Journal of Paleolimnology.1990,3:95-111.
Yu L Z, Oldfield, F., et al.. Paleoenvironmental implications of magnetic measurements on sediment core from Kunming Basin, Southwest China[J]. J Paleolimnol.1991,3:95-11.
Zhu Liping, Chen Ling, Li Bingyuan, et al. Environmental changes reflected by the lake sediments of the South Hongshan Lake,Northwest Tibet [J]. Science in China (Series D).2002,45 (5):430-439.
安芷生,肖举乐,张景昭等.季风与最近13万年黄土高原的气候历史[A].见：刘东生主编,黄土、第四纪与环境变化,第二集[c].北京,地质出版社,1991：108-114.
安芷生,李华梅,王俊达.洛川黄土剖面的古地磁学研究[J].地球化学1977,(4)：239-249.
安芷生,Porter S,Kukla等.最近13万年黄土高原季风变迁的磁化率证据[J].科学通报.1990,7：529-532.
安芷生,刘晓东.东亚季风气候的历史与变率[J].群学通报.2000,45(3)：238-249.
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[J].第四纪研究.2006,26(5)：678-692.
安芷生,吴锡浩,汪品先等.最近130ka中国的古季风--Ⅱ古季风变迁[J].中国科学(B辑).1999,11：1209-1215.
安芷生.亚洲季风演化、北半球大冰期的发展与喜马拉雅—青藏高原隆升[J].中国基础科学2001,(8)：9-11.
陈富斌,高生准,陈继良.甘孜黄土剖面磁性地层学初步研究[J].科学通报.1990.35：1600.
陈发虎,朱艳,李吉均等,民勤盆地湖泊沉积记录的全新世千百年尺度夏季风快速变化[J].科学通报.2001,46(17)：1414-1419.
陈发虎,张维信.甘青地区黄土地层和第四届冰川[M].北京：科学出版社.1993.
陈敬安,万国江,王福顺等.湖泊现代沉积物碳环境记录研究[J]中国科学(D辑).2002,32(1)：73-80.
陈敬安,万国江,汪福顺等.湖泊现代沉积物碳环境记录研究[J].中国科学(D辑).2003,2002,32(1)：73-80.
陈敬安,万国江.洱海沉积物化学元素与古气候演化[J].地带化学1999,28：562-570.
陈敬安,万国安,张峰等.不同时间尺度下的湖泊沉积物环境记录[J].中国科学(D辑).2003,33(6)：563-568.
陈诗越,方小敏,王苏民.川西高原甘孜黄土与印度季风演化关系[J].海洋地质与第四纪地质.2002,22(3)：41-46
陈忠.冰消期晚期以来德令哈尕海湖气候环境演变的碳、氧同位素记录[D].博士学位论文.西宁.中国科学院盐湖研究所.2007.
成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京：地质出版社.1978,31-36.
陈晔,袁林旺,周春林,刘泽纯.柴达木盆地第四纪古气候变化在自然伽玛测井曲线上的记录[J].古地理学报.2001,3：29-37.
陈克造,Bowler JM,Kelts K.四万年以来青藏高原的气候变迁[J].第四纪研究.1990,(1)：46-53.
陈克造.柴达木盆地晚更新世盐湖演化[A].见：中国科学院中澳第四纪合作研究组编,中国—澳大利亚第四纪学术讨论会论文集[C].北京：科学出版社.1987,83-91.
陈志明.从青藏高原隆起探讨西藏湖泊生态环境的变迁[J].海洋与湖沼.1981,12(5)：402-410.
曹升庚.土壤颜色的测定和描述—门赛尔土壤比色卡的应用[A].见：土壤分类及土壤地理论文集[C].北京：科学出版社.1985.
崔之久,吴永秋,刘耕年.关于“昆仑—黄河运动”[J].中国科学D辑.1998a,16(1)：53-60
崔之久,高全洲,刘耕年等.夷平面、古岩溶与青藏高原隆起[J].中国科学(D).1996,26(4)：378-385.
崔之久,吴永秋,刘耕年等.昆仑山垭口天然剖面记录[A].青藏高原晚新生代隆升和环境演化仁[M].广州：广东科技出版社.1998b,81-111.
崔之久,伍永秋,葛道凯等.昆仑山垭口地区第四纪环境演变[J].海洋地质与第四纪地质.1999,19(1)：53-62.
丁仲礼,刘东生.中国黄土研究新进展(一)黄土地层[J].第四纪研究.1989(1)：1-9.
丁仲礼,余志伟,刘东生.中国黄土研究新进展(三)时间标尺[J].第四纪研究.1991,(4)：336-348.
丁仲礼,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[J].中国科学(D辑).1999a,29(1)：82-87.
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[J].科学通报.1999b,44(3)：324-326.
鄂崇毅.新疆西风区粉尘研究[D].兰州大学.兰州大学图书馆.2009.
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[J].中国科学(D辑).2001,31：177-184.
方小敏,陈富斌,施雅风等.甘孜黄土与青藏高原冰冻圈演化[J].科学通报.1996,41：1865-1867.
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[J].科学通报.2002,47：540-545.
方小敏,李吉均,Van der Voo, R西秦岭黄土的形成年代及与物源区关系探讨[J].科学通报.1999,44：779-782.
高以信,张林源.青藏高原古土壤演化与高原隆起的关系[A]。见：龚子同主编,土壤环境变化[C].北京：中国科学技术出版社.1992,17-25.
顾兆言,刘嘉麒,袁宝印等.12000年来青藏高原季风变化——色林错沉积地球化学证据[J].科学通报.1993,38(1)：61-64.
郭佳宁.内蒙古宁城中更新世以来黄土磁化率与粒度特征及古环境研究[D],中国地质大学.北京.2009.
郭雪莲,王琪,史基安等.青海湖沉积物有机碳含量与同位素和粒度特征及其古气候意义[J].海洋地质与第四纪地质.2002,229(8)：99-102.
郭正堂,刘东生,Fedoroff N等.约0.85Ma前后黄土高原区季风强度的变化[J].科学通报.1993,38(2)：143-146.
胡东生.青藏高原第四纪湖泊地质环境演变[J].自然杂志.1995a,17(5)：257-261.
胡东生,张京华,徐冰等.青藏高原腹地第四纪地质环境演化的地球动力学机制[J],中国工程群学.2011,(13)：81-88.
胡东生.可可西里地区湖泊演化[J].干旱区地理.1995b,18(1)：60-67.
胡东生.可可西里地区湖泊水体中金富集规律的初步探讨[J].科学通报.1992,(16)：1499-1502.
胡东生,张华京,李炳元等.青藏高原腹地湖泊沉积序列与古气候变化[J].地质学报.2000,74(4)：363-370.
胡东生.可可西里地区湖泊水体地球化学特征[J].泊洋与湖泊.1997,28(2)：153-164.
胡东生,张华京,徐冰等.青藏高原腹地湖泊沉积对第四纪晚期古季风变化的响应[J].干旱区地理.2006,29(8)：483-489.
胡守云,吉磊,王苏民等.呼伦湖地区扎赉诺尔晚第四纪湖泊沉积物的磁化率变化及其影响因素[J].湖泊科学.1995,7(1)：33-40.
胡守云.呼伦湖湖泊沉积物磁化率变化的环境磁学机制[J].中国科学(D辑).1998a,28：334-339.
胡守云,王苏民,Apple E,等.呼伦湖湖泊沉积物磁化率变化的环境磁学机制[J].中国科学(D辑).1998b,28(4)：334-339.
黄赐璇,冯·康波·艾利斯,李拴科.根据孢粉分析论青藏高原西部和北部全新世环境变化[J].微体古生物学报.1996,13(4)：423-432.
黄翡,孙湘君.南海北部ODPI144站更新世(1.05—036Ma)抱粉记录[J].中国科学D(辑).2002,32(11)：914-920.
黄嘉佑.气象中的谱分析[M].气象出版社.1984.
黄汲清,闵隆瑞.青藏高原的隆升,沙漠和黄土的形成,人类的起源与演化[J].第四纪研究.1992,(1)：24-28.
黄孔怒.可可西里地区气候概况[J].青海环境.1989,(1)：28-29.
黄麒,孟昭强,刘海玲等.柴达木盆地查尔汗盐湖区古气候波动模式的初步研究[J].中国群学(B辑).1990,(6)：652-663.
黄小忠,陈发虎,肖舜等.新疆博斯腾湖沉积物粒度的古环境意义初探[J].湖泊科学.2008,20(3)：291-297.
江樟焰,伍永秋,崔之久.“昆仑-黄河运动”与我国自然地理格局的形成[J].北京师范大学学报.2005,41(1)85-88.
贾玉连,施雅风,范云崎.四万年以来青海湖的三期高湖面及其降水量研究[J].湖泊群笋2000,12(3)：182-192.
贾玉连,施雅风,王苏民等.40ka以来青藏高原的4次湖涨期及其形成机制初探[J].中国科学(D辑),2001,31(增刊)：241-251.
蒋庆丰,刘兴起,沈吉.乌伦古湖沉积物粒度特征及其古气候环境意义[J].沉积学报.2006,877-882.
金章东,邹成娟,高南华等.小冰期以来岱海地区的环境变迁与尘暴事件[J].西安工程学院学报.2001,23(4)：6-10.
刘传联.稳定同位素地球化学方法在古湖泊学研究中的应用[A]见：含油盆地古湖泊学研究方法[C]汪品先,刘传联主编,北京：海洋出版社.1993：96-123.
刘椿,刘东生,金增信,等.北京颐和园昆明湖近代沉积物的环境磁学初步研究及意义[J].群学通报.1994,39(21)：1989-1991.
刘东生,郑绵平,郭正堂等.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 的时代偶合性[J].第四纪研究.1998,18(3)：194-20.
刘东生等.黄土与环境[M].北京：科学出版社.1985.
刘东生,丁仲礼.二百五十万年来季风环流与大陆冰量变化的阶段性耦合过程[J].第四纪研究.1992,12(1)：12-23.
刘东生主编,黄土、第四纪与全球变化,第二集[M].北京,地质出版社.108-114.
刘光秀,王睿,李世杰等.西昆仑山甜水海24万年以来生态环境演化的孢粉学证据[J],冰川冻土,1998,20(1)：21-24.
刘光绣,沈永平,张平中等.青藏高原若尔盖地区RH孔800-150ka. B.P.的孢粉记录及古气候意义[J].沉积学报.1994,12(4)：101-109.
刘嘉麒,王文远.第四纪地质定年与地质年表[J].第四纪研究.1997,3：193-202.
刘冬雁,彭莎莎,乔彦松等.青藏高原东南缘甘孜黄土磁化率解释的西南季风演化[J].海洋地质与第四纪地质.2009,29(5)：115-121.
刘晓东,李力,安芷生.青藏高原隆升与欧亚内陆及北非的干旱化[J].第四纪研究.2001,21(2)：114-122.
刘晓东,汤懋苍.青藏高原影响气候的临界高度[A].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(1995).北京：科学出版社孙鸿烈主编,1996,青藏高原的形成演化。上海：社会科学技术出版社.1-369.
刘秀铭,刘东生,John S.中国黄土磁性矿物特征及其古气候意义[J].第四纪研究.1993(3)：282-287.
刘泽纯,陈晔,袁林旺等.应用自然伽玛测井曲线反演2.85Ma B.P来的古气候变化[J].中国科学(D辑).2000,26：316-322.
李才林.江淮平原末次冰消期以来环境变化的钻孔记录[D].南京师范大学.2007.
李长安,殷鸿福,于庆文.东昆仑山构造隆升与水系演化及其发展趋势[J].科学通报.1999,44(2)：211-214.
李炳元.西藏第四纪地质[M].北京：科学出版社.1983,15-130.
李炳元.羌塘高原北部湖泊演化的初步探讨[A]。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)[C].北京：科学出版社.1994,261-266.
李炳元,李吉均等.青藏高原第四纪冰川遗迹分布图[M].北京：科学技术出版社,1991.
李炳元.青藏高原晚新生代隆起于环境变化[M].广州：广东科技出版社,1998.
李炳元,李元芳,孔昭宸等.青海可可西里苟弄错地区近二万年来的环境变化[J].科学通报.1994,39(18)：1727-1728.
李炳元.青海可可西里地区自然环境[M].北京：科学出版社.1996.
李炳元等.青海省地貌图[M].测绘出版社.1988.
李炳元.青海可可西里地区综合科学考察初报[J].山地研究.1990,8(3)：161-166.
李炳元,李吉均.青藏高原第四纪冰川遗迹分布图(1：3000000)[M].科学出版社.1991
李炳元.青藏高原大湖期[J].地埋学报.2000,55(2)：174-182.
李国胜.艾比湖冰消期以来的δ13C记录与突变气候事件研究[J].科学通报.1993,38(22)：2069-2071.
李元芳,张青松,李炳元等.青藏高原西北部17000年以来的介形类及环境演变[J].地理学报.1994,49(1)：46-54.
李元芳,李炳元,王国等.西昆仑山甜水海介形类及其环境[J].湖泊科学.1997,9(3)：223-229.
李吉均,方小敏.青藏高原隆起与环境变化研究[J].科学通报.1998,43(15)：1569-1574.
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[J].中国科学1979(6)：608-616.
李吉均.青藏高原的地貌演化与亚洲季风[J].海洋地质第四纪地质.1999,19(1)：1-9.
李吉均.郑本兴等.西藏冰川[M].科学出版社.北京.1986,251-276.
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[J].中国科.D辑1996,26(4)：316-322.
李吉均,方小敏,潘保田等.新时代晚期青藏高原强烈隆起及其对周边环境的影响[J].第四纪研究.2001,21(5)：381-391.
李世杰,区荣康,朱照宇等.24万年以来西昆仑山甜水海湖岩芯碳酸盐含量与气候演化[J].湖泊群学.1998a,10(2)：58-65.
李世杰,李炳元,朱照宇等.甜水海湖泊钻探岩芯记录[A].1998b.见：施雅风,李吉均,李丙元,1998。青藏高原晚新生代隆起于环境变化[C].广州：广东科技出版社,215-246.
李世杰,王小天,夏威岚等.青藏高原苟鲁错湖泊沉积记录的小冰期气候变化[J].第四纪研究.2004,24(5)：578-584.
李世杰.青藏高原可可西里地区现代冰川发育特征[J].地理科学.1996,16(1)：10-17.
李华梅,王俊达.渤海湾北岸平原钻孔岩心的古地磁研究[J].地球化学.1983,(2)：196-204.
李育,王乃昂,李卓仑等.甘肃石羊河流域猪野泽湖泊沉积物粒度敏感组分与花粉组合关系[J].湖泊科学.2011,23(2)：295-302.
李红春,朱照宇.美国西部Owens湖地球化学记录及其古气候意义[J].第四纪研究.2002,22(6)：578-588.
李徐生,杨达源,韩辉友.皖南风尘堆积—古土壤序列磁化率初步研究[J].安徽师范大学学报(自然科学版).1998,21(1)：64-69.
莱尔曼.A,王苏民等译.湖泊的化学地质学和物理学[M].北京：地质出版社.1989.
雷国良,张虎才,张文翔等.柴达木盆地查尔汗古湖贝壳堤剖面粒度特征及其沉积环境[J].沉积学报.2007,25(2)：274-282.
吕厚远,王苏民,吴乃琴等.青藏高原错鄂湖2.8Ma来的孢粉记录[J].中国群笋(D辑).2001a,31(增刊)：234-240.
吕厚远,顾兆炎,吴乃琴等.海拔高度对青藏高原现代表土有机碳同位素组成的影响[J].第四纪研究.2001b,21(5)：399406.
鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义[J].中国科学(D辑).1998a,28(3)：278-283.
鹿化煜,杨文峰,刘晓东等.轨道调谐建立洛川黄土地层的时间标尺[J].地球物理学报.1998b,41(6)：804-810.
鹿化煜,安芷生,刘洪滨等.洛川黄土记录的最近2500 ka东亚冬夏季风变化周期[J].地质论评.1998c,44(5)：553-558.
卢武长.稳定同位素地球化学[M].成都：成都地质学院.1986.
卢演俦.黄土地层中CaCO3含量变化与更新世气候旋回[J].地质科学.1981,2：122-131.
罗运利,孙湘君,陈怀成.南海北部地区百万年以来的天然火与气候：ODP 1144孔深海沉积中的炭屑记录[J].群学通报.2006,51：942-950.
林振耀,吴洋定.青藏高原水汽输送路径的初步研究[J].地理研究.1990,9(3)：37.
林振耀,吴祥定.青藏高原隆起前后的气候状况[A].见：国科学院青藏高原综合科学考察队,1981青藏高原隆起的幅度和形式问题[C].北京：科学出版社.1981,159-165.
林晓,常浩,李云涛等.青藏高原东缘都江堰湖相沉积MIS3a阶段的快速气候变化记录[J],地球 科学—中国地质大学学报.2010,35(5)：858-866.
马玉贞,曹继秀,李吉均.甘肃临夏塬堡黄土剖面15万年来的孢粉植物群发展及气候演变[A].青藏高原形成演化、环境变迁与生态系统研究[C].北京：科学出版社.1995,103-113.
潘保田,邬光剑,王义祥等。祁连山东段沙沟河阶地的年代与成因[J].科学通报.2000,45：2669-2675.
潘保田.青藏高原全新世的气候与环境变化[A].见,施雅风,李吉均,李炳元编,青藏高原晚新生代隆升与环境变化[J].广州：广东科技出版社.1998,432-436.
庞小朋,韩凤清,吕亚平等.可可西里盐湖及其沉积特征初步研究[J].盐湖研究.2010,18(1)：9-14.
强明瑞,陈发虎,张家武等.2ka来苏干湖沉积碳酸盐稳定同位素记录的气候变化[J].科学通报.2005,50(13)：1385-1393.
乔彦松,郭正堂,郝青振等.皖南风尘堆积-土壤序列的磁性地层学研究及其古环境意义[J].科学通报.2003,48：1465-1469.
钱方,徐树全,陈富斌等.昔格达组磁性地层研究[J].山地研究1984,4(2)：171-179.
沈才明,唐领余,王苏民等.若尔盖盆地RM孔孢粉记录及其年代序列[J].科学通报.2005,50(3)：246-254.
沈吉,张恩楼,夏葳岚.青海湖近千年气候环境变化的湖泊沉积记录[J].第四纪研究.2001,21(6)：508-513.
沈吉,肖海丰,王苏民等.云南鹤庆钻孔揭示的区域气候轨道尺度演化[J].科学通报.2007,52(10)：1168-1173.
沈吉,吕厚远,王苏民等.错鄂孔深钻揭示的青藏高原中部2.8MaB. P.以来环境演化及其对构造事件响应[J].中国科学D辑.2004a,34(4)：359-366.
沈吉,刘兴起, Matsumoto R等.晚冰期以来青海湖沉积物多指标高分辨率的古气候演化[J].中国科学D辑.2004b,34(6)：582-589.
沈吉,汪勇,羊向东等.湖泊沉积记录的区域风沙特征及湖泊演化历史：以陕西红碱淖湖泊为例[J].科学通报.2006,1：87-92.
沈吉,肖海丰,王苏民等.云南鹤庆深钻揭示的区域气候轨道尺度演化[J].科学通报.2007,52：1168-1173.
沈振枢,程果,乐昌硕等.柴达木盆地第四纪含盐地层划分及沉积环境[M].北京：地质出版社.1993.
孙鸿烈,郑度.青藏高原形成演化与发展[M].广州：广东科技出版社.1998.
孙东怀,陈明扬John Shaw等.晚新生代黄土高原风尘堆积序列的磁性地层年代域古气候记录[J].中国科学(D辑).1998,28(1)：79-84.
孙东怀,刘禹,谭明.古环境记录的数字图像分析及应用[J].科学通报.2002,47(21)：1613-1618.
孙广友,罗新正,Turner R E.青藏东北部若尔盖高原全新世泥炭沉积年代学研究[J].沉积学报.2001,19(2)：177-182.
孙湘君,罗运利.南海北部280ka以来深海花粉记录[J].中国科学(D辑).2001,31(10)：846-853.
孙有斌,安芷生.最后4个冰期旋回中国黄土记录的东亚冬季风变化[J].地球科学—中国地质大学学报.2002,27(1)：19-24.
孙千里,周杰,肖举乐.岱海沉积物粒度特征及其古环境意义[J].海洋地质与第四纪地质.2001,21(1)：93-95.
施雅风,汤慰苍,马玉贞.青藏高原二期隆升与亚洲季风孕育关系探讨[J].中国科学(D辑). 1998a,28(3)：263-271.
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：广州科技出版社.1998b,PP419.
施雅风,李吉均,李炳元等.青藏高原隆升与环境演化[A].1998c.见”青藏高原形成演化与发展[C]."(孙鸿烈、郑度,编),pp.98-105.广东科技出版社.广州.
施雅风,李吉均,李炳元等.晚新时代青藏高原隆升与东亚环境变化[J].地理学报.1999a,54：10-21.
施雅风,刘晓东,李炳元等.距今40-30ka青藏高原特强夏季风事件及其与岁差周期关系[J],科学通报.1999b,44(14)：1475-1480.
施雅风,郑本兴,李世杰等.青藏高原中东部最大冰期的时代高度与气候环境探讨[J].冰川冻土.1995,17(2)：97-112.
施雅风,郑本兴.青截高原进入冰冻圈的时代、高度及其对周围地区的影响[A].见孙鸿烈、郑度主编藏高原形成演化、环境变迁与生态系统研究学术论文年刊(1995)[C].北京：科学出版社.1996,136-146.
师育新.兰州“930505”特大尘暴沉积物特征研究[J].沉积学报.1995,13(3)：76-82.
谭红兵,于升松.我国湖泊沉积环境演变研究中元素地球化学的应用现状及发展方向[J].盐湖研究.1999,7(3)：58-65.
唐领余,王睿.青海昆仑山垭口盆地第四纪湖泊沉积孢粉组合及其意义[A].见：中国科学院兰州冰川冻土沙漠研究所集刊,第一号[C].北京：科学出版社.1976,106-119.
汤懋苍,刘晓东.一个新的划分第四纪的标志——高原季风演变的地质环境后果[J].第四纪研究.1995,(1)：82-88.
田军.南海ODP1143站有孔虫稳定同位素揭示的上新世至更新世气候变化[D].博士学位论文.上海：同济大学.2002.
田庆春,杨太保,张述鑫等.青藏高原腹地湖泊沉积物磁化率及其环境意义[J].沉积学报.2011,29(1)：143-150.
藤则雄.根据日本中部琵琶湖深井孢粉资料重建第四纪古植被和古气候及全球占气候对比[J].古生物学报.2003,42(1)：138-147.
吴锡浩.晚新生代青藏高原隆升的阶段和高度[A].见：刘东生,安芷生主编,黄土·第四纪地质·全球变化(三)[C].北京：科学出版社.1992,1-12.
王富葆,韩灰有,阎革等.青藏高原东北部30ka来的古植被与古气候演变序列[J].中国科学(D辑).1996,26(2)：111-117.
王国安.稳定碳同位素在第四纪古环境研究中的应用[J].第四纪研究2003,23(5)：471-484.
王宁,刘卫国,徐黎明等.青藏高原现代湖泊沉积物碳酸盐矿物氧同位素组成特征及影响因素[J]第四纪研究2008,28(4)：591-600.
王苏民.湖泊沉积的信息原理与研究趋势[A].见：张兰生,中国生存环境历史演变规律研究[C],北京：海洋出版社.1993,22-31.
王苏民,张振克.中国湖泊沉积与环境演变研究的新进展[J].群学通报.1999,44(6)：579-587.
王苏民,施雅风,沈吉等.青藏高原东部800ka来古气候与古环境变迁的初步研究[A].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.1994,236-248.
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[J],中国辫学(D辑).1998,26(4)：323-328.
王苏民,施雅风.晚第四纪青海湖演化研究析视和讨论[J].湖泊科学.1992,4(3)：1-9.
王苏民,夏威岚,钱君龙等.若尔盖盆地RM孔的沉积特征与构造-气候演化过程[A].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[C].学术论文年刊,北京：科学出版社.1995.
王苏民,吉磊,羊向东等.呼伦湖—古湖泊学研究[M].合肥：中国科技大学出版社,1995.
王苏民,冯敏.内蒙古岱海湖泊环境变化与东南季风强弱的关系[J].中国科学(B).1991,(7)：759-767.
王心源,吴力,张广胜等.安徽巢湖全新世湖泊沉积物磁化率与粒度组合的变化特征及其环境意义[J].地理科学2008,28(4)：548-553.
王心源,张广胜,张恩楼等.巢湖湖泊沉积记录的早-中全新世环境演化研究[J].科学通报.2008,53(增刊Ⅰ)：132-138.
王绍武.气候系统引论[M].北京：气象出版社.1994,54-59.
王建,黄巧华.2.5 Ma以来柴达木盆地的气候干湿变化特征及其原因[J].地理科学.2002,22：34-38.
王澄海,董安祥,王式功等.青藏高原积雪与西北春节降水的相关特征[J].冰川冻土.2000,22(4)：340-346.
王云飞,王苏民,薛滨等.黄河袭夺若尔盖古湖时代的沉积学依据[J].科学通报.1995,40(8)：273-275.
王永波,刘兴起,羊向东等.可可西里库赛湖揭示的青藏高原北部近4000年来的干湿变化[J].湖泊科学.2008,20(5)：605-612.
王万春,吉利明.有机碳和有机分子碳同位素的地球化学意义[J].地球科学进展.1997,12(5)：74-478.
王赞红.现代尘暴降尘与非尘暴降尘的粒度特征[J].地理学报.2003,58(4)：606-610.
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[J].中国科学D辑:地球科学.2001,31(10)：793-799.
邬光剑.祁连山东段0.8 Ma以来的构造隆升与气候变化[M].博士学位论文,兰州大学.兰州.2001 pp.161.
邬光剑,潘保田,管清玉等.中更新世全球大冰期与中国沙漠扩张[J].冰川冻土.2002,24(5)：544-549.
吴福莉,方小敏,马玉贞等.黄土高原中部1.5 Ma以来古生态环境演化的孢粉记录[J].科学通报.2004.49：99-105.
吴敬禄,刘建军,王苏民.近1500年来新疆艾比湖同位素记录的气候环境演化特征[J].第四纪研究.2004,24(5)：585-590.
吴敬禄,王苏民,潘红玺等.青藏高原东部RM孔140ka以来湖泊碳酸盐同位素记录的古气候特征[J].中国科学(D辑).1997a,27,3：255-259.
吴敬禄,王苏民.青藏高原东部RM孔碳酸盐同位素揭示的末次间冰期气候特征[J].科学通报.1996,41(17)：1601-1604.
吴敬禄.若尔盖盆地RH孔近80万年来δ13Corg气候特征的频谱分析[J].湖泊科学1997b,9(3)：211-216.
吴乃琴,吕厚远等.C3、C4植物及其硅酸体研究的古气候意义[J].第四纪研究.1992,(2)：241-249.
吴艳宏,李世杰,王小天等.青藏高原苟鲁错湖泊沉积记录的小冰期气候变化[J].第四纪研究.2004a,24(5)：578-584.
吴艳宏,王苏民,夏威岚等.青藏高原中部0.2ka来的环境变化[J].中国科学(D辑).200131(增 刊)：264-269.
吴艳宏,王苏民,夏威岚等.1770年以来青藏高原错鄂地区古气候定量恢复[J].海洋地质与第四纪地质.2003,23(4)：115-120.
吴艳宏.青藏高原中部第四纪环境变迁的初步研究[D].中国科学院南京地理与湖泊研究所.2002.
吴艳宏,李世杰.湖泊沉积物色度在短尺度古气候研究中的应用[J].地球科学进展.2004b,19(5)：789-792.
吴瑞金.湖泊沉积物磁化率、频率磁化率的环境意义——以青海湖、岱海近代沉积为例[J].湖泊科学.1993.5(2)：128-135.
吴中海,赵希涛,江万.念青唐古拉山尔南麓更新世冰川沉积物年龄测定[J].冰川冻土.2003,25(3)：272-274.
薛滨,王苏民,夏威岚等.若尔盖RM孔揭示的青藏高原900kaBP以来的隆升与环境变化[J].中国科学(D辑).1997,27(6)：543-547.
薛滨,王苏民,吴艳宏等.若尔盖盆地RM孔揭示的过去14万年古环境[J].湖泊科学.1999,11(3)：206-212.
肖海丰,沈吉,肖霞云.云南鹤庆钻孔揭示的西南季风轨道尺度演化[J].第四纪研究.2006a,26(2)：274-282.
肖海丰,沈吉,肖霞云.云南鹤庆钻盆地2.78Ma以来的环境演化[J].湖泊科学.2006b,18(3)：255-260.
肖海丰,沈吉,肖霞云.鹤庆孔碳酸盐记录与深海δ18O和黄土粒度记录的对比[J].海洋地质与第四纪地质.2006c,26(2)：41-47.
谢又予等.沉积地貌分析[M].北京：海洋出版社.2000.3.
谢远云,李长安,王秋良等.江汉平原江陵湖泊沉积物粒度特征及气候环境意义[J].吉林大学学报(地球科学版).2007,37(3)：570-577.
徐仁,陶君容,孙湘君.希夏邦马峰高山栎化石层的发现及其在植物学和地质学上的意义[J].植物学报.1973,53：263-279.
徐馨,何才华,沈志达.关于中国气候地貌若干问题的探讨[J].贵州师范大学学报(自然科学版).1992,10(2)：1-12.
羊向东,王苏民,Kamenik C,等.藏南沉错钻孔硅藻组合与湖水古盐度定量恢复[J].中国群学D辑.2003,33(2)：163-169.
姚檀栋,王宁练.冰芯研究的过去、现在和未来[J].科学通报.1997a,42(3)：225-230.
姚檀栋,L G Thompson,施雅风等.古里雅冰芯中末次间冰期以来气候变化记录研究[J].中国科笋(D辑).1997b,27(5)：448-452.
姚檀栋,秦大河,田立德等.青藏高原2ka来温度与江水变化—古里雅冰芯记录[J].中国群学(D辑).1996,269(4)：348-353.
姚檀栋.末次冰期青藏高原的气候突变——古里雅冰芯与格陵兰GRIP冰芯对比研究[J].中国科学(D辑).1999,29,175-184.
杨建强,崔之久,易朝路等.云南点苍山冰川湖泊沉积物磁化率的影响因素及其环境意义[J].第四纪研究.2004,24(5)：591-597.
杨前进.沙尘暴沉积物的粒度特征及其环境意义[J].中国沙漠.2004,24(1)：47-50.
杨逸畴,张青松,李吉均等.高原隆起与环境变化[A].见孙鸿烈主编,青藏高原的形成演化[C].上海：上海科学技术出版社.1996,100-1151.
杨胜利.土壤颜色的气候意义[D].兰州：兰州大学资源与环境学院.2001.
杨胜利,方小敏,李吉均等.表土颜色和气候定性至半定量关系研究[J].中国科学(D辑).2001,31(增刊)：175-181.
杨志红,姚檀栋,皇翠兰等.古里雅冰芯中的新仙女木事件记录[J].群学通报.1997,42(18)：1975-1978.
阎满存,羞光荣,李保生等.腾格里沙淇东南缘沙淇演化的初步研究[J].中国沙漠.1998,18(2)：111-117
叶笃正,高由禧著.青藏高原气象学[J].北京：科学出版社.1979.1-278.
易朝路,焦克勤,刘克新等.冰碛物ESR测年与天山鸟鲁木齐河源末次冰期系列[J].冰川冻土.2001,23(4)：389-393.
殷勇,方念乔等.云南中甸纳帕海湖泊沉积物的磁化率及环境意义[J].地理科学.2002,22(4)：143-149.
余俊清,王小燕,李军等.湖泊沉积物有机碳同位素与环境的研究进展[J].湖泊科学.2001,13(1)：72-78.
余素华,朱照字,李炳元等.23万年以来青藏高原甜水海湖岩心铁元素的气候记录刍议[J].海洋地质与第四纪地质.1998,18(3)：63-68.
余志伟,丁仲礼.黄土古气候记录中的100 ka周期与岁差、半岁差周期的非线性耦合关系[J].中国科学(D辑).2003,33：520-528.
于永涛,柴达木盆地西北缘尕斯库勒湖钻孔记录的中更新世气候转型[D].兰州大学：兰州大学图书馆,2006.
袁林旺.柴达木盆地自然伽玛曲线记录的古气候变化信息研究[D].博士学位论文.南京师范大学.南京.2001.pp.130.
赵强,王乃昂,程弘毅等.青土湖沉积物粒度特征及其古环境意义[J].干旱区地理.2003,26(1)：1-5.
赵泉鸿,汪品先.南海第四纪古海洋学研究进展[J].第四纪研究.1999,6：481-501.
赵井东,周尚哲,崔建新等.乌鲁木齐河源冰碛物的ESR测年研究[J].冰川冻土.2002,24(6)：737-743.
张恩楼,沈吉,王苏民等.青海湖近900年来气候环境演化的湖泊沉积记录[J].湖泊科学.2002,14(1)：32-38.
张俊辉.柴达木盆地CH0310钻揭示的中更新世中晚期气候变化[D].兰州大学.兰州.2010.
张林源.青藏高原形成过程与我国新生代气候演变阶段的划分[A].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)[C].北京：科学出版社.1994,267-281.
张建军,杨达源,李徐生.长江中下游地区下蜀黄土磁化率曲线比较研究[J].华东地质学院学报.1999,22(2)：124-129.
张树夫,肖家仪,俞立中等.沉积物矿物磁性测量在古环境研究中的应用[J].地理科学.1991,11(2)：128-139.
张振克,吴瑞金,王苏民.岱海湖泊沉积物频率磁化率对历史时期环境变化的反映[J].地理研究.1998,17(3)：297-302.
张平中,王先彬,陈践发等.青藏高原若尔盖盆地RH孔沉积有机质的δ13C值和氢指数记录[J].中国科学(B辑).1995,25(6)：631-638.
张以茀,郑祥身.青海可可西里地区地质演化[M].北京：科学出版社.1996：9-15.
张成君,陈发虎,施祺等.西北干旱区全新世气候变化的湖泊有机质碳同位素记录——以石羊河流域三角城为例[J].海洋地质与第四纪地质.2000,20(4)：93-97.
张理刚.稳定同位素有地质科学中的应用[M].西安：陕西科学技术出版社.1985.
张彭熹,张保珍.柴达木地区距今三百万年来古气候环境演化的初步研究[J].地理学报.1991,46：327-335.
张彭熹,陈克造,于升松等.柴达木盆地盐湖[M].北京：科学出版社,1987.32-73.
张青松,周耀正,陆祥顺等.现代青藏高原上升速度问题[J].群学通报.1991,36(21)：1820-1824.
郑绵平,刘文高,向军等.论西藏的盐湖[J].地质学报.1983,(2)：184-193.
邹进上.气候学研究—“天、地、生”相互影响问题[M].北京：气象出版社.1989.
周爱锋.晚全新世苏干湖年纹层沉积及其环境变化[D].兰州,兰州大学图书馆.2007.
周才平,欧阳华,王勤学等.青藏高原主要生态系统净初级生产力的估算[J].地理学报.2004,59(1)：74-79.
周廷儒.近三十年来中国第四纪古地理研究的进展[J].地理学报.1979,34(4)：279-292.
周尚哲,李吉均,张世强等.祁连山摆浪河谷地的冰川地貌与冰期[J].冰川冻土.2001,23(2)：131-138.
周尚哲,李吉均.第四纪冰川测年研究新进展[J].冰川冻土.2003,23(6)：660-666.
周卫建,卢雪峰,武振坤等.若尔盖高原全新世气候变化的泥炭记录与加速器放射性碳测年[J].科学通报.2001,46(12)：1040-1044.
中国科学院南京地理与湖泊研究所,等.云南断陷湖泊环境与沉积[M].北京：科学出版社.1989,1-5.
朱芸,陈晔,舒强等.苏北盆地XH1钻孔中更新世以来的彩度指标记录及其气候环境变化[J].海洋地质与第四纪地质.2007,27(2)：23-31.
朱照宇,丁仲礼.中国黄土高原第四纪古气候与新构造演化[M].北京：地质出版社.1994,1-209.