[1] 包慧娟,李振山,王 涛.沙漠化地区可持续发展的概念模型[J].地理科学,2007,27(2):173~176. [2] 郭绍礼.西辽河流域沙漠化土地的形成和演变[J].自然资源,1980,(4):46~52. [3] 胡孟春.全新世科尔沁沙地环境演变的初步研究[J].干旱区资源与环境,1989,(3):51~58. [4] 刘新民,赵哈林,赵爱芬.科尔沁沙地风沙环境与植被[M].北京:科学出版社,1996. [5] 裘善文.论科尔沁沙地的形成与演变[J].地理科学,1989,9(4):317~328. [6] 董光荣,金 炯,李保生,等.科尔沁沙地沙漠化的几个问题——以南部地区为例[J].中国沙漠,1994,14(1):1~9. [7] 裘善文,李取生,夏玉梅.东北平原西部沙地古土壤与全新世环境变迁[J].第四纪研究,1992,(3):224~232. [8] Zhao H,Lu Y C,Yin J H.Optical dating of Holocene sand dune activities in the Horqin sand-fields in Inner Mongolia,China,using the SAR protocol[J].Quaternary Geochronology,2007,(2):29-33. [9] 任国玉.科尔沁沙地东南缘近3000年来植被演化与人类活动[J].地理科学,1999,19(1):42~48. [10] 任鸿昌,吕永龙,杨 萍,等.科尔沁沙地土地沙漠化的历史与现状[J].中国沙漠,2004,24(5):544~547. [11] 何 忠,周 杰,赖忠平,等.石英光释光测年揭示的晚第四纪毛乌素沙地演化[J].第四纪研究,2009,29(4):744~754. [12] 贾耀锋,黄春长,庞奖励,等.关中盆地西部黄土剖面年代序列及其记录的成壤环境演变[J].地理科学,2010,30(3): 458~464. [13] Murray A S,Wintle A G.Luminescence dating of quartz using an improved sinle-aliquot regenerative-dose protocol[J].Radiation Measurements,2000,32:57-73. [14] Roberts H M,Duller G A T.Standardised growth curves for optical dating of sediment using multiple-grain aliquots[J].Radiation Measurements,2004,38:241-252. [15] Lai Z P,Zller L,Fuchs M,et al.Alpha efficiency determination for OSL of quartz extracted from Chinese loess[J].Radiation Measurements,2008,43:767-770. [16] Aitken M J.Introduction to Optical Dating[M].Oxford:Oxford University Press,1998. [17] Li S H,Sun J M,Zhao H.Optical dating of dune sands in the northeastern deserts of China[J].Palaeogeograghy,Palaeoclimatology,Palaeoecology,2002,181:419-429. [18] Yang X P,Rost K T,Lehmkuhl F,et al.The evolution of dry lands in northern China and in Republic of Mongolia since the Last Glacial Maximum[J].Quaternary International,2004,118-119:69-85. [19] Li Y Y,Willis K J,Zhou L P,et al.The impact of ancient civilization on the northeastern Chinese landscape:palaeoecological evidence from the Western Liaohe River Basin,Inner Mongolia[J].The Holocene,2006,16(8):1109-1121. [20] Wang Y J,Cheng H,Edwards R L,et al.The Holocene Asian monsoon links to solar changes and North Atlantic climate[J].Science,2005,308:854-857. [21] Chambers F M,Mauquoy D,Brain S A,et al.Globally synchronous climate change 2800 years ago:Proxy data from peat in South America[J].Earth and Planetary Science Letters,2007,253:439-444. [22] 胡金明,崔海亭,李宜垠.西辽河流域全新世以来人地系统演变历史的重建[J].地理科学,2002,22(5):535~542. [23] Liu H Y,Xu L H,Cui H T.Holocene history of desertification along the woodland-steppe border in northern China[J].Quaternary Research,2002,57:259-270. [24] 刘鸿雁,李宜垠.半干旱区气候变化和人类活动的孢粉指示[J].古生物学报,2009,48(2):211~221. [25] 李月丛,许清海,阳小兰,等.中国草原区主要群落类型花粉组合特征[J].生态学报,2005,25(3):555~564. [26] Sun J M,Li S H,Han P,et al.Holocene environmental changes in the central Inner Mongolia,based on single-aliquot-quartz optical dating and multi-proxy study of dune sands[J].Palaeogeograghy,Palaeoclimatology,Palaeoecology,2006,233:51-62. [27] 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:L21716,1-4. [28] Zhou Y L,Lu H Y,Mason J A,et al.Optically stimulated luminescence dating of aeolian sand in the Otindag dune field and Holocene climate change[J].Science in China Series D-Earth Sciences,2008,51(6):837-847. [29] Sun J M. Origin of aeolian sand mobilization during the past 2 300 years in the Mu Us desert,China[J].Quaternary Research,2000,53:78-88. |