[1] Jin H L,Dong G R,Su Z Z,et al.Reconstruction of the spatial patterns of desert/loess boundary belt in North China during the Holocene[J].Chinese Science Bulletin,2001,46(12):969-974.
[2] Li S H,Sun J.Optical dating of Holocene dune sands from the Hulun Buir Desert,northeastern China[J].Holocene,2006,16(3):457-462.
[3] Sun J M,Li S H,Han P,et al.Holocene environment changes in the central inner Monglia,based on the signle-aliquot-quartz optical dating and muti-proxy study of dune sands[J].Palaeogeography Palaeoclimatology Palaeoecology,2006,233:51-62.
[4] Yang L H,Wang T,Zhou J,et al.OSL chronology and possible forcing mechanisms of dune evolution in the Horqin dunefield in northern China since the Last Glacial Maximum[J].Quaternary Research,2012,78:185-196.
[5] Lu H Y,Yi S W,Xu Z W,et al.Chinese deserts and sand fields in Last Glacial Maximum and Holocene Optimum[J].Chinese Science Bulletin,2013,58(23):1-9.
[6] 牛东风,李保生,王丰年,等.微量元素记录的毛乌素沙漠全新世气候波动——以萨拉乌苏流域DGS1层段为例[J].沉积学报,2015,33(4):735-743.
[7] 曹红霞,张云翔,岳乐平,等.毛乌素沙地全新世地层粒度组成特征及古气候意义[J].沉积学报,2003,21(3):482-486.
[8] 黄昌庆,冯兆东,马玉贞,等.巴汗淖孢粉记录的全新世环境变化[J].兰州大学学报:自然科学版,2009,45(4):7-12.
[9] Li S H,Sun J,Li B.Holocene environmental changes in central Inner Mongolia revealed by luminescence dating of sediments from the Sala Us River valley[J].Holocene,2012,22(4):397-404.
[10] 徐志伟,鹿化煜,弋双文,等.末次盛冰期和全新世大暖期毛乌素沙地的空间变化[J].第四纪研究,2013,33(2):218-227.
[11] Liu B,Jin H L,Sun L Y,et al.Holocene moisture change revealed by the Rb/Sr ratio of aeolian deposits in the southeastern Mu Us Desert,China[J].Aeolian Research,2014,13:109-119.
[12] An Z,Kukla G J,Porter S C,et al.Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years[J].Quaternary Research,1991,36(1):29-36.
[13] 刘秀铭,刘东生.中国黄土磁性矿物特征及其古气候意义[J].第四纪研究,1993,13(3):281-287.
[14] 旺罗,刘东生,韩家懋,等.中国第四纪黄土环境磁学研究进展[J].地球科学进展,2000,15(3):335-341.
[15] 安芷生,王俊达,李华梅.洛川黄土剖面的古地磁研究[J].地球化学,1977(4):239-249.
[16] Heller F,Liu T S.Magnetostratigraphical dating of loess deposits in China[J].Nature,1982,300:431-433.
[17] Kukla G,An Z S.Loess stratigraphy in central China[J].Palaeogeography Palaeoclimatology Palaeoecology,1989,72:203-225.
[18] Zhou W J,Donahue D J,Porter S C,et al.Variability of monsoon climate in East Asia at the end of the Last Glaciation[J].Quaternary Research,1996,46:219-229.
[19] 刘冰,靳鹤龄,孙忠.近6 ka以来科尔沁沙地东部气候变化记录[J].中国沙漠,2011,31(6):1398-1405.
[20] 赵景波.黄土地层中的CaCO3与环境[J].沉积学报,1993,11(1):136-142.
[21] 高尚玉,董光荣,李保生,等.萨拉乌苏河地区地层中CaCO3和易溶盐含量变化与气候环境[J].干旱区资源与环境,1988,2(4):41-48.
[22] 罗开利,李保生,祝一志,等.150 ka B.P.以来萨拉乌苏河流域的CaCO3旋回[J].地理科学,2002,22(6):683-688.
[23] 施雅风,孔昭宸,王苏民,等.中国全新世大暖期的气候波动与重要事件[J].中国科学:B辑,1992,22(12):1300-1308.
[24] 鲁瑞洁,王亚军,张登山.毛乌素沙地15 ka以来气候变化及沙漠演化研究[J].中国沙漠,2010,30(2):273-277.
[25] Xiao J,Xu Q,Nakamura T,et al.Holocene vegetation variation in the Daihai Lake region of north-central China[J].Quaternary Science Reviews,2004,23:1669-1679.
[26] Gong Z J,Li S H,Sun J M,et al.Environmental changes in Hunshandake (Otindag) sandy land revealed by optical dating and multi-proxy study of dune sands[J].Journal of Asian Earth Sciences,2013,76:30-36.
[27] 刘冰,靳鹤龄,孙忠.中晚全新世科尔沁沙地演化与气候变化[J].中国沙漠,2013,33(1):77-86.
[28] 许清海,肖举乐,中村俊夫,等.全新世以来岱海盆地植被演替和气候变化的孢粉学证据[J].冰川冻土,2004,26(1):73-80.
[29] 许清海,孔昭宸,陈旭东,等.鄂尔多斯东部4000余年来的环境与人地关系的初步探讨[J].第四纪研究,2002,22(2):105-112.
[30] 刘宇航,夏敦胜,金明,等.阿拉善地区湖泊岩芯磁性特征记录的全新世环境变化[J].中国沙漠,2012,32(4):929-937.
[31] Jia F F,Lu R J,Gao S Y,et al.Holocene aeolian activities in the southeastern Mu Us Desert,China[J].Aeolian Research,2015,19:267-274.
[32] Sun A Z,Feng Z D.Holocene climatic reconstructions from the fossil pollen record at Qigai Nuur in the southern Mongolian Plateau[J].Holocene,2013,23(10):1391-1402.
[33] Huang C C,Jie Z,Pang J L,et al.A regional aridity phase and its possible cultural impact during the Holocene Megathermal in the Guanzhong Basin,China[J].Holocene,2000,10(1):135-142.
[34] 董光荣,陈惠忠,王贵勇,等.150 ka以来中国北方沙漠、沙地演化和气候变化[J].中国科学:B辑,1995,25(12):1303-1312.
[35] Lu H Y,Miao X D,Zhou Y L,et al.Late Quaternary aeolian activity in the Mu Us and Otindag dune fields (north China) and lagged response to insolation forcing[J].Geophysical Research Letters,2005,32(21):365-370.
[36] Wang L,Li J J,Lu H Y,et al.The East Asian winter monsoon over the last 15,000 years:its links to high-latitudes and tropical climate systems and complex correlation to the summer monsoon[J].Quaternary Science Reviews,2012,32:131-142.
[37] Hu C Y,Henderson G M,Huang J H,et al.Quantification of Holocene Asian monsoon rainfall from spatially separated cave records[J].Earth & Planetary Science Letters,2008,266:221-232.
[38] Gergana Y,Nowaczyk N R,Jens M,et al.Influence of the intertropical convergence zone on the East Asian monsoon[J].Nature,2007,445:74-77.
[39] 许清海,肖举乐,中村俊夫,等.孢粉资料定量重建全新世以来岱海盆地的古气候[J].海洋地质与第四纪地质,2003,23(4):99-108.
[40] Berger A,Loutre M F.Insolation values for the climate of the last 10 million years[J].Quaternary Science Reviews,1991,10:297-317.
[41] 方修琦,孙宁.降温事件:4.3 ka BP岱海老虎山文化中断的可能原因[J].人文地理,1998,13(1):71-76.
[42] Zhao Y,Yu Z C,Chen F H,et al.Vegetation response to Holocene climate change in monsoon-influenced region of China[J].Earth-Science Reviews,2009,97:242-256.
[43] Bond G,Bonani G.A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates[J].Science,1997,278:1257-1266.