| [1]Chen J,Li G,Yang J,et al.Nd and Sr isotopic characteristics of Chinese deserts:Implications for the provenances of Asian dust[J].Geochimica et Cosmochimica Acta,2007,71:3904-3914.[2]Kapp P,Pelletier J D,Rohrmann A,et al.Wind erosion in the Qaidam basin,central Asia:Implications for tectonics,paleoclimate,and the source of the Loess Plateau[J].GSA Today,2011,21(4/5):4-10.[3]Pullen A,Kapp P,McCallister A T,et al.Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications[J].Geology,2011,39:1031-1034.[4]Bowler J M,Chen K Z,Yuan B Y.Systematic variations in loess source areas:Evidence from Qaidam and Qinghai Basins,Western China[M]//Liu T S.Aspects of Loess Research.Beijing:China Ocean Press,1987:39-51.[5]Li G J,Chen J,Ji J F,et al.Natural and anthropogenic sources of East Asian dust[J].Geology,2009,37:727-730.[6]An F Y,Ma H Z,Wei H C,et al.Distinguishing aeolian signature from lacustrine sediments of the Qaidam Basin in northeastern Qinghai-Tibetan Plateau and its palaeoclimatic implications[J].Aeolian Research,2012,4:17-30.[7]曾永年,冯兆东,曹广超.末次冰期以来柴达木盆地沙漠形成与演化[J].地理学报,2003,58(3):452-457.[8]王俊达,王三学.察尔汗盐湖地区几个第四纪剖面的观察与风成沉积的初探[M]//中国科学院盐湖研究所.青海柴达木盆地晚新生代地质环境变化.北京:科学出版社,1986:152-156.[9]钟德才.柴达木盆地古沙丘的初步研究[M]//中国科学院盐湖研究所.青海柴达木盆地晚新生代地质环境变化.北京:科学出版社,1986:100-103.[10]辛彦林.柴达木盆地盐湖中的风成砂[J].中国沙漠,1995,15(3):252-255.[11]Chen K Z,Bowler J M.Preliminary study on sedimentary characteristics and evolution of palaeoclimate of Qarhan Salt Lake in Qaidam Basin[J].Scientia Sinica (Series B),1985,28(11):1218-1231.[12]Chen K Z,Bowler J M.Late plestocene evolution of salt lakes in the Qaidam Basin,Qinghai province,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1986,54:87-104.[13]Zeng Y N,Ma H Z,Sha Z J,et al.The record of Younger Drays event in eolian sand deposit in Qaidam Basin[J].Chinese Geographical Science,1999,9:92-95.[14]郝永萍,方小敏,奚晓霞,等.柴达木盆地东缘晚更新世气候变化的(古)土壤发生记录[J].地理科学,1998,18(3):249-254.[15]曾永丰.柴达木盆地东部环境演化对古文化的影响[J].干旱区资源与环境,2006,20(2):61-64.[16]Owen L A,Finkel R C,Ma H Z,et al.Late Quaternary landscape evolution in the Kunlun Mountains and Qaidam Basin,Northern Tibet:A framework for examining the links between glaciation,lake level changes and alluvial fan formation[J].Quaternary International,2006,154/155:73-86.[17]Chen Y X,Li Y K,Zhang Y,et al.Late Quaternary deposition and incision sequences of the Golmud River and their environmental implications[J].Quaternary International,2011,236:48-56.[18]牛光明,强明瑞,宋磊,等.5 000 a来柴达木盆地东南缘风成沉积记录的冬季风演化[J].中国沙漠,2010,30(5):29-37.[19]Yu L P,Lai Z P.OSL chronology and palaeoclimatic implications of aeolian sediments in the Qaidam Basin of the northeastern Qinghai-Tibetan Plateau[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2012,337/338:120-129.[20]Liu X J,Lai Z P,Madsen D,et al.Lake level variations of Qinghai Lake in northeastern Qinghai-Tibetan Plateau since 3.7 ka based on OSL dating[J].Quaternary International,2011,236:57-64.[21]Lu H Y,Zhao C F,Mason J,et al.Holocene climate changes revealed by Aeolian deposits from the Qinghai Lake area (northeastern Qinghai-Tibetan Plateau) and possible forcing mechanisms[J].The Holocene,2011,21:297-304.[22]Sun J M,Li S H,Muhs D R,et al.Loess sedimentation in Tibet:provenance,processes,and link with Quaternary glaciations[J].Quaternary Science Reviews,2007,26:2265-2280.[23]徐树建,王涛.蓬莱黄土剖面光释光年代学及其沉积特征研究[J].中国沙漠,2011,31(2):295-301.[24]Liu X J,Lai Z P,Yu L P,et al.Luminescence chronology of aeolian deposits from the Qinghai Lake area in the Northeastern Qinghai-Tibetan Plateau and its palaeoenvironmental implications[J].Quaternary Geochronology,2012,10:37-43.[25]Sun Y J,Lai Z P,Long H,et al.Quartz OSL dating of archaeological sites in Xiao Qaidam Lake of the NE Qinghai-Tibetan Plateau and its implications for palaeoenvironmental changes[J].Quaternary Geochronology,2010,5:360-364.[26]白旸,王乃昂,何瑞霞,等.巴丹吉林沙漠湖相沉积的探地雷达图像及光释光年代学证据[J].中国沙漠,2011,31(4):842-847.[27]Lai Z P,Wintle A G.Locating the boundary between the Pleistocene and the Holocene in Chinese loess using luminescence[J].The Holocene,2006,16:893-899.[28]Lai Z P,Wintle A G,Thomas D S G.Rates of dust deposition between 50 ka and 20 ka revealed by OSL dating at Yuanbao on the Chinese Loess Plateau[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2007,248:431-439.[29]Roberts H M.Assessing the effectiveness of the double-SAR protocol in isolating a luminescence signal dominated by quartz[J].Radiation Measurements,2007,42:1627-1636.[30]Lai Z P,Brückner H.Effects of feldspar contamination on equivalent dose and the shape of growth curve for OSL of silt-sized quartz extracted from Chinese loess[J].Geochronometria,2008,30:49-53.[31]Murray A S,Wintle A G.Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol[J].Radiation Measurement,2000,32:57-73.[32]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.[33]Prescott J R,Hutton J T.Cosmic ray contributions to dose rates for luminescence and ESR dating:Large depths and long-term time variations[J].Radiation Measurements,1994,23:497-500.[34]Murray A S,Wintle A G.The single aliquot regenerative dose protocol:Potential for improvements in reliability[J].Radiation Measurements,2003,37:377-381.[35]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.[36]Lai Z P.Testing the use of an OSL standardized growth curve (SGC) for De determination on quartz from the Chinese Loess Plateau[J].Radiation Measurements,2006,41:9-16.[37]Lai Z P,Brückner H,Zller L,et al.Existence of a common growth curve for silt-sized quartz OSL of loess from different continents[J].Radiation Measurements,2007,42:1432-1440.[38]Lancaster N.Development of linear dunes in the southwestern Kalahari,Southern Africa[J].Journal of Arid Environments,1998,14:233-244.[39]Cohen T J,Nanson G C,Larsen J R,et al.Late Quaternary aeolian and fluvial interactions on the Cooper Creek Fan and the association between linear and source-bordering dunes,Strzelecki Desert,Australia[J].Quaternary Science Reviews,2010,29:455-471.[40]朱震达,吴正,刘恕,等.中国沙漠概论[M].北京:科学出版社,1980.[41]刘东生等.黄土与环境[M].北京:科学出版社,1985.[42]Yang X P,Scuderi L,Paillou P,et al.Quaternary environmental changes in the drylands of China-a critical review[J].Quaternary Science Reviews,2011,30:3219-3233.[43]Huang Q,Cai B Q,Yu J Q.The 14C age and cycle of sedimentation of some saline lakes on the Qinghai-Xizang Plateau[J].Chinese Science Bulletin,1981,26:66-70.[44]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,2008,27:867-879.[45]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,2005,136:131-140.[46]Lister G,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.[47]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,2007,52:539-544.[48]Ji J F,Shen J,Balsam W,et al.Asian monsoon oscillations in the northeastern Qinghai Tibet Plateau since the late glacial interpreted from visible reflectance of Qinghai Lake sediments[J].Earth and Planetary Science Letters,2005,233:61-70.[49]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.[50]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.[51]邵雪梅,王树芝,徐岩,等.柴达木盆地东北部3500年树轮定年年表的初步建立[J].第四纪研究,2007,27(4):477-485.[52]邵雪梅,梁尔源,黄磊,等.柴达木盆地东北部过去1 427 a的降水变化重建[J].气候变化研究进展,2006,2(3):122-126.[53]邵雪梅,黄磊,刘洪滨,等.树轮记录的青海德令哈地区千年降水变化[J].中国科学(D辑),2004,34(2):145-153.[54]Liu K B,Yao Z J,Tompson L G.A pollen record of Holocene climate changes from the Dunde ice cap,Qinghai-Tibetan Plateau[J].Geology,1998,26(2):135-138.[55]周爱锋.晚全新世苏干湖纹层沉积及其环境记录[D].兰州:兰州大学,2007.[56]刘禹,安芷生,马海州,等.青海都兰地区公元850年以来树轮记录的降水变化及其与北半球气温的联系[J].中国科学(D辑),2006,36(5):461-471.[57]刘禹,安芷生,Linderholm H W,等.青藏高原中东部过去2 485年以来温度变化的树轮记录[J].中国科学(D辑),2009,39(2):166-176.[58]康兴成,Graumlich L J,Sheppard P R.青海都兰地区1 835 a年轮序列的建立和初步分析[J].科学通报,1997,42(10):1089-1091.[59]Zheng B X,Jiao K Q,Li S J,et al.New progress about chronological studies of Quaternary glaciation in Qingha-Xizang plateau[J].Chinese Science Bulletin,1990,36:482-486.[60]王宗太.天山中段及祁连山东段小冰期以来的冰川及环境[J].地理学报,1991,46(2):160-167. |
2013, Vol. 33 
