Vandenberghe J, Renssen H, Huissteden K, et al. Penetration of Atlantic westerly winds into Central and East Asia[J]. Quaternary Science Reviews, 2006, 25(17/18):2380-2389.
[2]
Zhao Y, Yu Z C, Chen F H. Spatial and temporal patterns of Holocene vegetation and climate changes in arid and semi-arid China[J]. Quaternary International, 2009, 194(1/2):6-18.
[3]
Thompson L G, Mosley-Thompson E, Davis M E, et al. Holocene-Late Pleistocene climatic ice core records from Qinghai-Tibetan Plateau[J]. Science, 1989, 246(4929):474-477.
[4]
Feng Z D, Thompson L G, Mosley-Thompson E, et al. Temporal and spatial variations of climate in China during the last 10 000 years[J]. The Holocene, 1993, 3(2):174-180.
[5]
D'Arrigo R D, Jacoby G C, Pederson N, et al. Mongolian tree-rings, temperature sensitivity and reconstructions of Northern Hemisphere temperature[J]. The Holocene, 2000, 10(6):669-672.
[6]
Jacoby G C, D'Arrigo R D, Davaajamts T. Mongolian tree rings and 20th-century warming[J]. Science, 1996, 273(5276):771-773.
[7]
Li J J, Feng Z D, Tang L Y. Late Quaternary monsoon patterns on the Loess Plateau of China[J]. Earth Surface Processes and Landforms, 1988, 13(2):125-135.
[8]
鹿化煜, 安芷生, 刘洪滨, 等. 洛川黄土记录的最近2500ka东亚冬夏季风变化周期[J]. 地质论评, 1998, 44(5):553-558. [Lu Huayu, An Zhisheng, Liu Hongbin, et al. Periodicity of East Asian winter and summer monsoon variation during the past 2500 ka recorded by loess deposits at Luochuan on the central Chinese Loess Plateau[J]. Geological Review, 1998, 44(5):553-558.]
[9]
丁仲礼, 余志伟. 第四纪时期东亚季风变化的动力机制[J]. 第四纪研究, 1995, 2(1):63-74. [Ding Zhongli, Yu Zhiwei. Forcing mechanisms of paleomonsoons over East Asia[J]. Quaternary Sciences, 1995, 2(1):63-74.]
[10]
于学峰, 周卫健, Franzen L G, 等. 青藏高原东部全新世冬夏季风变化的高分辨率泥炭记录[J]. 中国科学(D 辑):地球科学, 2006, 36(2):182-187. [Yu Xuefeng, Zhou Weijian, Franzen L G, et al. High-resolution peat records for Holocene monsoon history in the eastern Tibetan Plateau[J]. Science China (Seri. D):Earth Sciences, 2006, 36(2):182-187.]
[11]
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(7182):1090-1093.
[12]
Wang Y J, Cheng H, Edwards R L, et al. The Holocene Asian Monsoon:links to solar changes and North Atlantic climate[J]. Science, 2005, 308(5723):854-857.
[13]
Chen F H, Yu Z C, Yang M L, et al. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history[J]. Quaternary Science Reviews, 2008, 27(3/4):351-364.
[14]
Feng Z D, An C B, Wang H B. Holocene climatic and environmental changes in the arid and semi-arid areas of China:a review[J]. The Holocene, 2006, 16(1):119-130.
[15]
Li Y, Wang N, Cheng H Y, et al. Holocene environmental change in the marginal area of the Asian monsoon:a record from Zhuye Lake, NW China[J]. Boreas, 2009, 38(2):349-361.
[16]
Liang E Y, Liu X H, Yuan Y J, et al. The 1920s drought recorded by tree rings and historical documents in the semi-arid and arid areas of northern China[J]. Climatic Change, 2006, 79(3/4):403-432.
[17]
Ma Z, Fu C. Interannual characteristics of the surface hydrological variables over the arid and semi-arid areas of northern China[J]. Global and Planetary Change, 2003, 37(3):189-200.
[18]
吴建国, 吕佳佳. 气候变化对我国干旱区分布及其范围的潜在影响[J]. 环境科学研究, 2009, 22(2):199-206. [Wu Jianguo, Lü Jiajia. Potential effect of climate change on the distribution and range of arid regions[J]. Research of Environmental Sciences, 2009, 22(2):199-206.]
[19]
An C B, Feng Z D, Barton L. Dry or humid? Mid-Holocene humidity changes in arid and semi-arid China[J]. Quaternary Science Reviews, 2006, 25(3/4):351-361.
[20]
李育, 王乃昂, 李卓仑, 等. 石羊河流域全新世孢粉记录及其对气候系统响应争论的启示[J]. 科学通报, 2011, 56(2):161-173. [Li Yu, Wang Nai'ang, Li Zhuolun, et al. Holocene palynological records and their responses to the controversies of climate system in the Shiyang River drainage basin[J]. Chinese Science Bulletin, 2011, 56(2):161-173.]
[21]
Zhao Y, Yu Z C, Zhao W W. Holocene vegetation and climate histories in the eastern Tibetan Plateau:controls by insolation-driven temperature or monsoon-derived precipitation changes?[J]. Quaternary Science Reviews, 2011, 30(9/10):1173-1184.
[22]
Wen R L, Xiao J L, Chang Z G, et al. Holocene precipitation and temperature variations in the East Asian monsoonal margin from pollen data from Hulun Lake in northeastern Inner Mongolia, China[J]. Boreas, 2010, 39(2):262-272.
[23]
An Z S, Porter S C, Kutzbach J E, et al. Asynchronous Holocene optimum of the East Asian monsoon[J]. Quaternary Science Reviews, 2000, 19(8):743-762.
[24]
He Y, Theakstone W H, Zhang Z L, et al. Asynchronous Holocene climatic change across China[J]. Quaternary Research, 2004, 61(1):52-63.
[25]
Shao X H, Wang Y J, Cheng H, et al. Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ18O record from Shennongjia in Central China[J]. Chinese Science Bulletin, 2006, 51(2):221-228.
[26]
Ma Z G, Fu C B, Dan L. Decadal variations of arid and semi-arid boundary in China[J]. Chinese Journal of Geophysics, 2005, 48(3):574-581.
[27]
Yang J P, Ding Y J, Chen R S, et al. The interdecadal fluctuation of dry and wet climate boundaries in China in recent 50 years[J]. Acta Geographica Sinica, 2002, 57(6):655-661.
[28]
张兰生, 史培军, 侯乐峰. 中国北方季风尾闾区全新世不同时期降水变化及其区域分异规律研究[M]//张兰生. 中国生存环境历史演变规律研究. 北京:海洋出版社, 1993:147-154. [Zhang Lansheng, Shi Peijun, Hou Lefeng. Research on precipitation change and its distributive pattern of monsoon edge area in northern China during Holocene[M]//Zhang Lansheng. Research on Historical Evolution Law of Living Environment in China. Beijing:Ocean Press, 1993:147-154.]
[29]
张成君, 郑绵平, Prokopenko A, 等. 博斯腾湖碳酸盐和同位素组成的全新世古环境演变高分辨记录及与冰川活动的响应[J]. 地质学报, 2007, 81(12):1658-1671. [Zhang Chengjun, Zheng Mianping, Prokopenko A, et al. The palaeoenvironmental variation from the high-resolution record of the Holocene sediment carbonate and isotopic composition in Bosten Lake and responding to glacial activity[J]. Acta Geologica Sinica, 2007, 81(12):1658-1671.]
[30]
薛积彬, 钟巍. 新疆巴里坤湖全新世环境记录及区域对比研究[J]. 第四纪研究, 2008, 28(4):610-620. [Xue Jibin, Zhong Wei. Holocene climate change recorded by lacustrine sediments in Barkol Lake and its regional comparison[J]. Quaternary Sciences, 2008, 28(4):610-620.]
[31]
李秉孝, 蔡碧琴, 梁青生. 吐鲁番盆地艾丁湖沉积特征[J]. 科学通报, 1989, 34(8):608-610. [Li Bingxiao, Cai Biqin, Liang Qingsheng. Sedimentary characteristics of Aydingkol Lake in Turpan Basin[J]. Chinese Science Bulletin, 1989, 34(8):608-610.]
[32]
沈吉, 王苏民, 朱育新, 等. 内蒙古岱海古水温定量恢复及其古气候意义[J]. 中国科学(D 辑):地球科学, 2001, 31(12):1017-1023. [Shen Ji, Wang Sumin, Zhu Yuxin, et al. Quantitative reestablishment palaeo-water temperature of Daihai Lake, Inner Mongolia[J]. Science China (Seri. D):Earth Sciences, 2001, 31(12):1017-1023.]
[33]
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. [Chen Fahu, Zhu Yan, Li Jijun, et al. Abrupt Holocene changes of the Asian monsoon at millennial- and centennial scales:evidence from lake sediment document in Minqin Basin, NW China[J]. Chinese Science Bulletin, 2001, 46(17):1414-1419.]
[34]
李容全. 内蒙古高原湖泊与环境变迁[M]. 北京:北京师范大学出版社, 1990. [Li Rongquan. Lakes and Environmental Changes in Inner Mongolia Plateau[M]. Beijing:Beijing Normal University Press, 1990.]
[35]
郑喜玉, 张明刚, 董继和. 内蒙古盐湖[M]. 北京:科学出版社, 1992. [Zheng Xiyu, Zhang Minggang, Dong Jihe. Salt Lake in Inner Mongolia[M]. Beijing:Science Press, 1992.]
[36]
Gasse F, Arnold M, Fontes J C, et al. A 13, 000-year climate record from western Tibet[J]. Nature, 1991, 353(6346):742-745.
[37]
Morinaga H, Itota C, Isezaki N, et al. Oxygen-18 and carbon-13 records for the last 14, 000 years from Lacustrine carbonates of Siling-Co (Lake) in the Qinghai-Tibetan Plateau[J]. Geophysical Research Letters, 1993, 20(24):2909-2912.
[38]
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):地球科学, 2004, 34(6):582-589. [Shen Ji, Liu Xingqi, Matsumoto R, et al. A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake[J]. Science China (Seri. D):Earth Sciences, 2004, 34(6):582-589.]
[39]
Madsen D B, Ma H Z, Rhode D, et al. Age constraints on the late Quaternary evolution of Qinghai Lake, Tibetan Plateau[J]. Quaternary Research, 2008, 69(2):316-325.
[40]
Liu X J, Lai Z P, Fan Q S, et al. Timing for high lake levels of Qinghai Lake in the Qinghai-Tibetan Plateau since the last interglaciation based on quartz OSL dating[J]. Quaternary Geochronology, 2010, 5(2/3):218-222.
[41]
Liu X Q, Dong H L, Rech J A, et al. Evolution of Chaka Salt Lake in NW China in response to climatic change during the Latest Pleistocene-Holocene[J]. Quaternary Science Reviews, 2008, 27(7/8):867-879.
[42]
孙小虹. 罗布泊盐湖盐类矿物特征、成因与成钾作用[D]. 北京:中国地质科学院, 2013. [Sun Xiaohong. Characteristics and genesis of salt minerals, and potash formation in the Lop Nur playa[D]. Beijing:Chinese Academy of Geological Sciences, 2013.]
[43]
Sarg J F. The sequence stratigraphy, sedimentology, and economic importance of evaporite-carbonate transitions:a review[J]. Sedimentary Geology, 2001, 140(1/2):9-34.
[44]
Sinha R, Raymahashay B C. Evaporite mineralogy and geochemical evolution of the Sambhar Salt Lake, Rajasthan, India[J]. Sedimentary Geology, 2004, 166(1/2):59-71.
[45]
Crowley J K. Mapping playa evaporite minerals with AVIRIS data:A first report from Death Valley, California[J]. Remote Sensing of Environment, 1993, 44(2/3):337-356.
[46]
Bryant R G, Sellwood B W, Millington A C, et al. Marine-like potash evaporite formation on a continental playa:case study from Chott el Djerid, southern Tunisia[J]. Sedimentary Geology, 1994, 90(3/4):269-291.
[47]
王云飞. 青海湖、岱海的湖泊碳酸盐化学沉积与气候环境变化[J]. 海洋与湖沼, 1993, 24(1):31-35. [Wang Yunfei. Lacustrine carbonate chemical sedimentation and climatic-environmental evolution—a case study of Qinghai Lake and Daihai Lake[J]. Oceanologia Et Limnologia Sinica, 1993, 24(1):31-35.]
[48]
Rhodes T E, Gasse F, Lin R F, et al. A Late Pleistocene-Holocene lacustrine record from Lake Manas, Junggar (northern Xinjiang, western China)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1996, 120(1/2):105-121.
[49]
Wei K, 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(12):1315-1334.
[50]
陈敬安, 万国江, 陈振楼, 等. 洱海沉积物化学元素与古气候演化[J]. 地球化学, 1999, 28(6):562-570. [Chen Jing'an, Wan Guojiang, Chen Zhenlou, et al. Chemical elements in sediments of Lake Erhai and palaeoclimate evolution[J]. Geochemica, 1999, 28(6):562-570.]
[51]
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):地球科学, 2002, 32(l):73-80. [Chen Jing'an, Wan Guojiang, Wang Fushun, et al. A study on modern lake sedimentary carbon environmental records[J]. Science China(Seri. D):Earth Sciences, 2002, 32(l):73-80.]
[52]
郑喜玉, 张明刚, 徐昶, 等. 中国盐湖志[M]. 北京:科学出版社, 2002:3-29. [Zheng Xiyu, Zhang Minggang, Xu Chang, et al. Chinese Salt Lakes[M]. Beijing:Science Press, 2002:3-29.]
[53]
郑绵平, 赵元艺, 刘俊英. 第四纪盐湖沉积与古气候[J]. 第四纪研究, 1998(4):297-307. [Zheng Mianping, Zhao Yuanyi, Liu Junying. Quaternary saline lake deposition and paleoclimate[J]. Quaternary Sciences, 1998(4):297-307.]
[54]
Wang N A, Zhang J M, Cheng H Y, et al. The age of formation of the mirabilite and sand wedges in the Hexi Corridor and their paleoclimatic interpretation[J]. Chinese Science Bulletin, 2003, 48(14):1439-1445.
[55]
刘成林, 陈永志, 陈伟十, 等. 罗布泊盐湖更新世晚期沉积钙芒硝包裹体特征及古气候意义探讨[J]. 矿物学报, 2006, 26(1):94-98. [Liu Chenglin, Chen Yongzhi, Chen Weishi, et al. Studies of fluid inclusions in glauberite of middle upper Pleistocene strata and their paleoclimatic significance in Lop Nur salty lake, Xinjiang, NW China[J]. Acta Mineralogica Sinica, 2006, 26(1):94-98.]
[56]
孙青, 储国强, 李圣强, 等. 硫酸盐型盐湖中的长链烯酮及古环境意义[J]. 科学通报, 2004, 49(17):1789-1792. [Sun Qing, Chu Guoqiang, Li Shenqiang, et al. Long chain ketene in sulfate type salt lake and its paleo-environment significance[J]. Chinese Science Bulletin, 2004, 49(17):1789-1792.]
[57]
郑绵平. 中国盐湖资源与生态环境[J]. 地质学报, 2010, 84(11):1613-1622. [Zheng Mianping. Salt lake resources and eco-environment in China[J]. Acta Geologica Sinica, 2010, 84(11):1613-1622.]
[58]
郑大中, 郑若锋. 论钾盐矿床的物质来源和找矿指示[J]. 盐湖研究, 2006, 14(4):9-17. [Zheng Dazhong, Zheng Ruofeng. Material sources and prospecting indicators of potassium deposits[J]. Journal of Salt Lake Research, 2006, 14(4):9-17.]
[59]
郑喜玉. 乌尊布拉克湖硝酸钾盐沉积特征[J]. 盐湖研究, 2000, 8(1):41-45. [Zheng Xiyu. Sedimentary features of sylvite nitrate in Lake Wuzunbulake[J]. Journal of Salt Lake Research, 2000, 8(1):41-45.]
[60]
Li Y, Wang N A, Chen H B, et al. Tracking millennial-scale climate change by analysis of the modern summer precipitation in the marginal regions of the Asian monsoon[J]. Journal of Asian Earth Sciences, 2012, 58:78-87.
[61]
王可丽, 江灏, 赵红岩. 西风带与季风对中国西北地区的水汽输送[J]. 水科学进展, 2005, 16(3):432-438. [Wang Keli, Jiang Hao, Zhao Hongyan. Atmospheric water vapor transport from westerly and monsoon over the Northwest China[J]. Advances in Water Science, 2005, 16(3):432-438.]
[62]
李万莉, 王可丽, 傅慎明, 等. 区域西风指数对西北地区水汽输送及收支的指示性[J]. 冰川冻土, 2008, 30(1):34-38. [Li Wanli, Wang Keli, Fu Shenming, et al. The interrelationship between regional westerly index and the water vapor budget in Northwest China[J]. Journal of Glaciology and Geocryology, 2008, 30(1):34-38.]
[63]
赵松乔. 中国综合自然地理区划的一个新方案[J]. 地理学报, 1983, 38(1):1-10. [Zhao Songqiao. A new scheme for comprehensive physical regionalization in China[J]. Acta Geographica Sinica, 1983, 38(1):1-10.]
丁宏伟, 张举. 河西走廊地下水水化学特征及其演化规律[J]. 干旱区研究, 2005, 22(1):24-28. [Ding Hongwei, Zhang Ju. Goechemical properties and evolution of groundwater beneath the Hexi Corridor, Gansu Province[J]. Arid Zone Research, 2005, 22(1):24-28.]
[67]
白福, 杨小荟. 河西走廊黑河流域地下水化学特征研究[J]. 西北地质, 2007, 40(3):105-110. [Bai Fu, Yang Xiaohui. Hydrochemical characteristics of groundwater of the Heihe Basin in the Hexi Corridor, Gansu Province[J]. Northwestern Geology, 2007, 40(3):105-110.]
[68]
赵强. 石羊河流域末次冰消期以来环境变化研究[D]. 兰州:兰州大学, 2005. [Zhao Qiang. Environment changes of the Shiyang River Drainage since the Last Deglaciation[D]. Lanzhou:Lanzhou University, 2005.]
[69]
陈隆亨, 曲耀光. 河西地区水土资源及其合理开发利用[M]. 北京:科学出版社, 1992:6-46. [Chen Longhen, Qu Yaoguang. Water and Soil Resources and Its Exploitation and Utilization in Hexi Area[M]. Beijing:Science Press, 1992:6-46.]
[70]
张克存, 屈建军, 马中华. 近50a来民勤沙尘暴的环境特征[J]. 中国沙漠, 2004, 24(3):257-260. [Zhang Kecun, Qu Jianjun, Ma Zhonghua. Environmental characteristics of sandstorm in Minqin county in recent 50 years[J]. Journal of Desert Research, 2004, 24(3):257-260.]
[71]
冯绳武. 民勤绿洲的水系演变[J]. 地理学报, 1963, 29(3):241-249. [Feng Shengwu. The evolution of the drainage system of the Minchin oasis[J]. Acta Geographica Sinica, 1963, 29(3):241-249.]
[72]
李并成. 猪野泽及其历史变迁考[J]. 地理学报, 1993, 48(1):55-59. [Li Bingcheng. A study on the Zhuye Lake and its historical evolution[J]. Acta Geographica Sinica, 1993, 48(1):55-59.]
[73]
隆浩. 季风边缘区全新世中期气候变化的古湖泊记录[D]. 兰州:兰州大学, 2006. [Long Hao. Mid-Holocene climate variation from lake evidence of East Asian monsoon margin areas[D]. Lanzhou:Lanzhou University, 2006.]
[74]
朱艳, 程波, 陈发虎, 等. 石羊河流域现代孢粉传播研究[J]. 科学通报, 2004, 49(1):15-21. [Zhu Yan, Cheng Bo, Chen Fahu, et al. Spread of modern pollen in the Shiyang River drainage basin[J]. Chinese Science Bulletin, 2004, 49(1):15-21.]
[75]
Zhao Y, Yu Z, Chen F, et al. Holocene vegetation and climate change from a lake sediment record in the Tengger Sandy Desert, northwest China[J]. Journal of Arid Environments, 2008, 72(11):2054-2064.
[76]
Long H, Lai Z P, Wang N A, et al. Holocene climate variations from Zhuyeze terminal lake records in East Asian monsoon margin in arid northern China[J]. Quaternary Research, 2010, 74(1):46-56.
[77]
李育, 王乃昂, 李卓仑, 等. 河西走廊盐池晚冰期以来沉积地层变化综合分析——来自夏季风西北缘一个关键位置的古气候证据[J]. 地理学报, 2013, 68(7):933-944. [Li Yu, Wang Nai'ang, Li Zhuolun, et al. Comprehensive analysis of lake sediments in Yanchi Lake of Hexi Corridor since the late glacial[J]. Acta Geographica Sinica, 2013, 68(7):933-944.]
[78]
李育, 王乃昂, 许清海, 等. 中国北方第四纪孢粉提取方法研究[J]. 沉积学报, 2007, 25(1):124-130. [Li Yu, Wang Naiang, Xu Qinghai, et al. Investigation of Quarternary pollen and spores extraction methods in North China[J]. Acta Sedimentologica Sinica, 2007, 25(1):124-130.]
李明慧, 易朝路, 方小敏, 等. 柴达木西部钻孔盐类矿物及环境意义初步研究[J]. 沉积学报, 2010, 28(6):1213-1228. [Li Minghui, Yi Chaolu, Fang Xiaomin, et al. Evaporative minerals of the upper 400m sediments in a core from the Western Qaidam Basin, Tibet[J]. Acta Sedimentologica Sinica, 2010, 28(6):1213-1228.]
[81]
李恩菊. 巴丹吉林沙漠与腾格里沙漠沉积物特征的对比研究[D]. 西安:陕西师范大学, 2011. [Li Enju. A comparative study of sediments characteristics between the Badain Jaran Desert and Tengger Desert[D]. Xi'an:Shanxi Normal University, 2011.]
[82]
Pye K. Aeolian Dust and Dust Deposits[M]. London:Academic Press, 1987:29-62.
[83]
大连理工大学无机化学教研室. 无机化学[M]. 北京:高等教育出版社, 2001:154-172. [Staff Room of Inorganic Chemistry, Dalian University of Technology. Inorganic Chemistry[M]. Beijing:Higher Education Press, 2001:154-172.]
[84]
Warren J K. Evaporite Sedimentology:Importance in Hydrocarbon Accumulation[M]. Englewood Cliffs, N. J.:Prentice Hall, 1989:1-37.
[85]
Lea D W, Pak D K, Peterson L C, et al. Synchroneity of tropical and high-latitude Atlantic temperatures over the last glacial termination[J]. Science, 2003, 301(5638):1361-1364.
[86]
Rasmussen S O, Andersen K K, Svensson A M, et al. A new Greenland ice core chronology for the last glacial termination[J]. Journal of Geophysical Research:Atmospheres (1984-2012), 2006, 111(D6):D06102, doi:10.1029/2005JD006079.
[87]
Berger A, Loutre M F. Insolation values for the climate of the last 10 million years[J]. Quaternary Science Reviews, 1991, 10(4):297-317.
[88]
杨文光, 郑洪波, 谢昕, 等. 南海北部陆坡沉积记录的全新世早期夏季风极强事件[J]. 第四纪研究, 2008, 28(3):425-430. [Yang Wenguang, Zheng Hongbo, Xie Xin, et al. East Asian summer monsoon maximum records in Northern South China Sea during the Early Holocene[J]. Quaternary Sciences, 2008, 28(3):425-430.]
[89]
Shen J, Liu X Q, Wang S M, et al. Palaeoclimatic changes in the Qinghai Lake area during the last 18, 000 years[J]. Quaternary International, 2005, 136(1):131-140.
[90]
Liu X Q, Shen J, Wang S M, et al. Southwest monsoon changes indicated by oxygen isotope of ostracode shells from sediments in Qinghai Lake since the late Glacial[J]. Chinese Science Bulletin, 2007, 52(4):539-544.
[91]
Fleitmann D, Burns S J, Mudelsee M, et al. Holocene forcing of the Indian monsoon recorded in a stalagmite from southern Oman[J]. Science, 2003, 300(5626):1737-1739.
[92]
Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China[J]. Earth and Planetary Science Letters, 2005, 233(1/2):71-86.
[93]
Wang R L, Scarpitta S C, Zhang S C, et al. Later Pleistocene/Holocene climate conditions of Qinghai-Xizhang Plateau (Tibet) based on carbon and oxygen stable isotopes of Zabuye Lake sediments[J]. Earth and Planetary Science Letters, 2002, 203(1):461-477.
[94]
Morrill C, Overpeck J T, Cole J E, et al. Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet[J]. Quaternary Research, 2006, 65(2):232-243.
[95]
Yancheva G, Nowaczyk N R, Mingram J, et al. Influence of the intertropical convergence zone on the East Asian monsoon[J]. Nature, 2007, 445(7123):74-77.
[96]
Zhu L P, Zhen X L, Wang J B, et al. A ~30, 000-year record of environmental changes inferred from Lake Chen Co, Southern Tibet[J]. Journal of Paleolimnology, 2009, 42(3):343-358.
[97]
安芷生, Porter S C, 吴锡浩, 等. 中国中、东部全新世气候适宜期与东亚夏季风变迁[J]. 科学通报, 1993, 38(14):1302-1305. [An Zhisheng, Potter S C, Wu Xihao, et al. The Holocene climatic optimum and East Asian monsoon transition in east and central China [J]. Chinese Science Bulletin, 1993, 38(14):1302-1305.]
[98]
Ko？ N, Jansen E, Haflidason H. Paleoceanographic reconstructions of surface ocean conditions in the Greenland, Iceland and Norwegian seas through the last 14 ka based on diatoms[J]. Quaternary Science Reviews, 1993, 12(2):115-140.
[99]
Birks C J A, Ko？ N. A high-resolution diatom record of late-Quaternary sea-surface temperatures and oceanographic conditions from the eastern Norwegian Sea[J]. Boreas, 2002, 31(4):323-344.
[100]
Dahl-Jensen D, Mosegaard K, Gundestrup N, et al. Past temperatures directly from the Greenland ice sheet[J]. Science, 1998, 282(5387):268-271.
[101]
Li Y, Morrill C. Multiple factors causing Holocene lake-level change in monsoonal and arid central Asia as identified by model experiments[J]. Climate Dynamics, 2010, 35(6):1119-1132.
[102]
Jin L Y, Chen F H, Morrill C, et al. Causes of early Holocene desertification in arid central Asia[J]. Climate Dynamics, 2012, 38(7/8):1577-1591.
[103]
Xiao J L, Xu Q H, Nakamura T, et al. Holocene vegetation variation in the Daihai Lake region of north-central China:a direct indication of the Asian monsoon climatic history[J]. Quaternary Science Reviews, 2004, 23(14/15):1669-1679.
[104]
Herzschuh U. Palaeo-moisture evolution in monsoonal Central Asia during the last 50, 000 years[J]. Quaternary Science Reviews, 2006, 25(1/2):163-178.
