[1]IPCC.Climate Change 2007:The Physical Science Basis.Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change[M].Cambridge:Cambridge University Press,2007.[2]Arimoto R.Eolian dust and climate:Relationships to sources,tropospheric chemistry,transport and deposition[J].Earth-Science Reviews,2001,54(1):29-42.[3]Harrison S P,Kohfeld K E,Roelandt C,et al.The role of dust in climate changes today,at the last glacial maximum and in the future[J].Earth-Science Reviews,2001,54(1):43-80.[4]Kohfeld K E,Harrison S P.DIRTMAP:The geological record of dust[J].Earth-Science Reviews,2001,54(1):81-114.[5]Jickells T D,An Z S,Andersen K K,et al.Global iron connections between desert dust,ocean biogeochemistry,and climate[J].Science,2005,308(5718):67-71.[6]Maher B A,Prospero J M,Mackie D,et al.Global connections between aeolian dust,climate and ocean biogeochemistry at the present day and at the last glacial maximum[J].Earth-Science Reviews,2010,99:61-97.[7]Liu T S.Loess and Environment[M].Beijing:China Ocean Press,1985:1-234.[8]An Z S,Liu T S,Lu Y C,et al.The long-term paleomonsoon variation recorded by the loess paleosol sequence in central China[J].Quaternary International,1990,(7/8):91-95.[9]Liu T S,Ding Z L.Stepwise coupling of monsoon circulations to global ice volume variations during the late Cenozoic[J].Global and Planetary Change,1993,7:119-130.[10]Ding Z L,Yu Z W,Rutter N W,et al.Towards an orbital time scale for Chinese loess deposits[J].Quaternary Science Reviews,1994,13:39-70.[11]Ding Z L,Liu T S,Rutter N W,et al.Ice-volume forcing of East Asian winter monsoon variationsin the past 800 000 years[J].Quaternary Research,1995,44:149-159.[12]Sun D H,Shaw J,An Z S,et al.Magnetostratigraphy and paleoclimatic interpretation of a continuous 7.2 Ma Late Cenozoic eolian sediments from the Chinese Loess Plateau[J].Geophysical Research Letters,1998,25(1):85-88.[13]Xiao J L,An Z S,Liu T S,et al.East Asia monsoon variation during the last 130 000 years:Evidence from the Loess Plateau of Central China and lake Biwa of Japan[J].Quaternary Science Reviews,1999,18(1):147-157.[14]An Z S.The history and variability of the East Asian paleomonsoon climate[J].Quaternary Science Reviews,2000,19(1-5):171-187.[15]Guo Z T,Ruddiman W F,Hao Q Z,et al.Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J].Nature,2002,416:159-163.[16]Tsoar H,Pye K.Dust transport and the question of desert loess formation[J].Sedimentology,1987,34:139-153.[17]Pye K.Aeolian Dust and Dust Deposits[M].London:Academic Press,1987.[18]Sun D H,Bloemendal J,Rea D K,et al.Bimodal grain-size distribution of Chinese loess,and its palaeoclimatic implications[J].Catena,2004,55:325-340.[19]Sun D H.Monsoon and westerly circulation changes recorded in the late Cenozoic aeolian sequences of Northern China[J].Global and Planetary Change,2004,41:63-80.[20]Sun D H,Su R X,Bloemendal J,et al.Grain-size and accumulation rate records from Late Cenozoic aeolian sequences in northern China:Implications for variations in the East Asian winter monsoon and westerly atmospheric circulation[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2008,264:39-53.[21]肖舜,陈发虎,强明瑞,等.青海苏干湖表层沉积物粒度分布模式与大气粉尘记录[J].地理学报,2007,62(11):1153-1164.[22]Sun D H,Su R X,Li Z J,et al.The ultrafine component in Chinese loess and its variation over the past 7.6 Ma:Implications for the history of pedogenesis[J].Sedimentology,2010 (in press)[23]Derbyshire E,Meng X M,Kemp R A.Provenance,transport and characteristics of modern aeolian dust in western Gansu Province,China,and interpretation of the Quaternary loess record[J].Journal of Arid Environments,1998,39:497-516.[24]肖舜.晚全新世苏干湖高分辨率风尘记录研究[D].兰州:兰州大学,2010.[25]肖洪浪,张继贤,李金贵.腾格里沙漠东南缘降尘粒度特征和沉积速率[J].中国沙漠,1997,17(2):127-132.[26]杨前进.沙尘暴沉降物的粒度特征及其环境意义[J].中国沙漠,2004,24(1):47-50.[27]李晋昌,董治宝,王训明.中国北方东部地区春季降尘量及其环境意义[J].中国沙漠,2008,28(2):195-201.[28]梁云,刘新春,何清,等.新疆春夏季大气降尘分析[J].中国沙漠,2008,28(5):992-995.[29]刘新春,钟玉婷,王敏仲,等.塔里木盆地大气降尘变化特征及影响因素分析[J].中国沙漠,2010,30(4):954-960.[30]Udden J A.Mechanical composition of clastic sediments[J].Bulletin of the Geological Society of America,1914,25:655-744.[31]Wentworth C K.A scale of grade and class terms for clastic sediments[J].Journal of Geology,1922,30:377-392.[32]Friedman G M,Sanders J E.Principles of Sedimentology[M].New York:Wiley,1978.[33]Sun D H,Bloemendal J,Rea D K,et al.Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments,and numerical partitioning of the sedimentary components[J].Sedimentary Geology,2002,152:263-277.[34]Sun D H,Chen F H,Bloemendal J,et al.Seasonal variability of modern dust over the Loess Plateau of China[J].Journal of Geophysical Research,2003,108(D21):AAC 3-1~3-10.[35]鹿化煜,安芷生.前处理方法对黄土沉积物粒度测量影响的实验研究[J].科学通报,1997,42(23):96-101.[36]Uno I,Eguchi K,Yumimoto K,et al.Asian dust transported one full circuit around the globe[J].Nature Geoscience,2009,2(8):557-560.[37]张德二.历史时期“雨土”现象剖析[J].科学通报,1982,(5):294-297. |