[1] 朱震达,吴正,刘恕,等.中国沙漠概论[M].北京:科学出版社:1980.
[2] Yang X,Scuderi L,Paillou P,et al.Quaternary environmental changes in the drylands of China-a critical review[J].Quaternary Science Reviews,2011,30(23):3219-3233.
[3] Wang N A,Li Z L,Cheng H Y,et al.High lake levels on Alxa Plateau during the Late Quaternary[J].Chinese Science Bulletin,2011,56(17):1799-1808.
[4] Yang X.Landscape evolution and precipitation changes in the Badain Jaran Desert during the last 30 000 years[J].Chinese Science Bulletin,2000,45(11):1042-1047.
[5] Yang X,Scuderi L A.Hydrological and climatic changes in deserts of China since the late Pleistocene[J].Quaternary Research,2010,73(1):1-9.
[6] Zhang H C,Peng J L,Ma Y Z,et al.Late quaternary palaeolake levels in Tengger Desert,NW China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2004,211(1):45-58.
[7] 陈建生,赵霞,汪集旸,等.巴丹吉林沙漠湖泊钙华与根状结核的发现对研究湖泊水补给的意义[J].中国岩溶,2005,23(4):277-282.
[8] 春喜,陈发虎,范育新,等.乌兰布和沙漠的形成与环境变[J].中国沙漠,2007,27(6):927-931
[9] 高尚玉,陈渭南,靳鹤龄,等.全新世中国季风区西北缘沙漠演化初步研究[J].中国科学:B辑,1993.
[10] 徐志伟,鹿化煜,赵存法,等.库姆塔格沙漠地表物质组成,来源和风化过程[J].地理学报,2010,65(1):53-64.
[11] 谢静,丁仲礼.中国东北部沙地重矿物组成及沙源分析[J].中国科学:D辑,2007,37(8):1065-1072.
[12] Nesbitt H W,Young G M.Petrogenesis of sediments in the absence of chemical weathering:effects of abrasion and sorting on bulk composition and mineralogy[J].Sedimentology,1996,43(2):341-358.
[13] 马宁,王乃昂,朱金峰,等.巴丹吉林沙漠周边地区近50 a来气候变化特征[J].中国沙漠,2011,31(6):1541-1547.
[14] Li Z,Wang N,Li Y,et al.Runoff simulations using water and energy balance equations in the lower reaches of the Heihe River,northwest China[J].Environmental Earth Sciences,2013,70(1):1-12.
[15] 朱金峰,王乃昂,陈红宝,等.基于遥感的巴丹吉林沙漠范围与面积分析[J].地理科学进展,2010,29(9):1087-1094.
[16] 马宁,王乃昂,李卓仑,等.1960-2009 年巴丹吉林沙漠南北缘气候变化分析[J].干旱区研究,2011,28(2):242-250.
[17] 马宁,王乃昂,赵力强,等.巴丹吉林沙漠腹地降水事件后的沙山蒸发观测[J].科学通报,2014,59(7):615-622.
[18] 王乃昂,马宁,陈红宝,等.巴丹吉林沙漠腹地降水特征的初步分析[J].水科学进展,2013,24(2):153.
[19] Yang X,Ma N,Dong J,et al.Recharge to the inter-dune lakes and Holocene climatic changes in the Badain Jaran Desert,western China[J].Quaternary Research,2010,73(1):10-19.
[20] 陆莹,王乃昂,李贵鹏,等.巴丹吉林沙漠湖泊水化学空间分布特征[J].湖泊科学,2010,22(5):774-782.
[21] 来婷婷,王乃昂,黄银洲,等.2002年腾格里沙漠湖泊季节变化研究[J].湖泊科学,2012,24(6):957-964.
[22] 陈立.应用地球化学方法探究巴丹吉林沙漠地下水源[D].兰州:兰州大学,2012.
[23] 丁贞玉,马金珠,何建华.腾格里沙漠西南缘地下水水化学形成特征及演化[J].干旱区地理,2009,32(6):948-957.
[24] 李鸿娟.吉兰泰盆地地下水化学特征及氟污染风险评价[D].西安:长安大学,2013.
[25] Jaillard B,Guyon A,Maurin A F.Structure and composition of calcified roots,and their identification in calcareous soils[J].Geoderma,1991,50(3):197-210.
[26] Košir A.Microcodium revisited:root calcification products of terrestrial plants on carbonate-rich substrates[J].Journal of Sedimentary Research,2004,74(6):845-857.
[27] Wright V P.Paleosols in shallow marine carbonate sequences[J].Earth-Science Reviews,1994,35(4):367-395.
[28] Wright V P,Platt N H,Marriott S B,et al.A classification of rhizogenic(root-formed) calcretes,with examples from the Upper Jurassic-Lower Cretaceous of Spain and Upper Cretaceous of southern France[J].Sedimentary Geology,1995,100(1):143-158.
[29] Gocke M,Pustovoytov K,Kühn P,et al.Carbonate rhizoliths in loess and their implications for paleoenvironmental reconstruction revealed by isotopic composition:δ 13C,14 C[J].Chemical Geology,2011,283(3):251-260.
[30] 任美锷.中国自然地理纲要[M].北京:商务印书馆,1992.
[31] Li Z L,Wang N A,Cheng H Y,et al.Formation and environmental significance of Late Quaternary calcareous root tubes in the deserts of the Alashan Plateau,Northwest China[J].Quaternary International,2015,372:167-174.
[32] Chen F H,Fan Y X,Chun X,et al.Preliminary research on Megalake Jilantai-Hetao in the arid areas of China during the Late Quaternary[J].Chinese Science Bulletin,2008,53(11):1725-1739.
[33] Zhao H,Li G,Sheng Y,et al.Early middle Holocene lake-desert evolution in northern Ulan Buh Desert,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2012,331:31-38.