[1] 高前兆,李福兴.黑河流域水资源合理开发利用[M].兰州:甘肃科学技术出版社,1991.
[2] Yang X P,Ma N N,Dong J F,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.
[3] 肖生春,肖洪浪.近百年来人类活动对黑河流域水环境的影响[J].干旱区资源与环境,2004,18(3):57-62.
[4] 肖生春,肖洪浪.额济纳地区历史时期的农牧业变迁与人地关系演进[J].中国沙漠,2004,24(4):448-450.
[5] 龚家栋,程国栋,张小由,等.黑河下游额济纳地区的环境演变[J].地球科学进展,2002,17(4):491-496.
[6] 郎丽丽,王训明,哈斯,等.灌丛沙丘形成演化及环境指示意义研究的主要进展[J].地理学报,2012,67(11):1526-1536.
[7] Marston R A.Maneuver-caused wind erosion impacts,south central New Mexico[M]//Nickling W G.Aeolian Geomorphology.Boston,USA:Allen and Unwin,1986:273-290.
[8] Khalaf F I,Misak R,Al-Dousari A.Sedimentological and morphological characteristics of some nabkha deposits in the northern coastal plain of Kuwait,Arabia[J].Journal of Arid Environments,1995,29:267-292.
[9] Lancaster N.Paleoenvironmental implications of fixed dune systems in Southern Africa[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1981,33(4):327-346.
[10] Kocurek G,Lancaster N.Aeolian system sediment state:theory and Mojave Desert Kelso dune field example[J].Sedimentology,1999,46(3):505-515.
[11] Weems S L,Monger H C.Banded vegetation-dune development during the Medieval Warm Period and 20th century,Chihuahuan Desert,New Mexico,USA[J].Ecological Society of America,2012,3(3):1-16.
[12] Wang X M,Zhang C X,Zhang J W,et al.Nebkha formation:implications for reconstructing environmental changes over the past several centuries in the Ala Shan Plateau,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,297:697-706.
[13] Forman S L,Pierson J.Formation of linear and parabolic dunes on the eastern Snake River Plain,Idaho in the nineteenth century[J].Geomorphology,2003,56:189-200.
[14] Ballarini M,Wallinga J,Murray A S,et al.Optical dating of young coastal dunes on a decadal time scale[J].Quaternary Science Reviews,2003,22:1011-1017.
[15] Bailey S D,Wintle A G,Duller G A T,et al.Sand deposition during the last millennium at Aberffraw,Anglesey,North Wales as determined by OSL dating of quartz[J].Quaternary Science Reviews,2001,20:701-704.
[16] 夏训诚,赵元杰,王富葆,等.罗布泊地区红柳沙包年层的环境意义探讨[J].科学通报,2005,50(19):2176-2177.
[17] Wang X M,Xiao H L,Li J C,et al.Nebkha development and its relationship to environmental change in the Alaxa Plateau,China[J].Environmental Geology,2008,56:359-365.
[18] 赵元杰,夏训诚,王富葆,等.罗布泊地区红柳沙包纹层沙粒度特征与环境指示意义[J].干旱区地理,2007,30(6):791-796.
[19] 赵元杰,宋艳,夏训诚,等.近150 年来罗布泊红柳沙包沉积纹层沙物质粒度特征[J].干旱区资源与环境,2009,23(12):103-107.
[20] Lang L L,Wang X M,Hua T,et al.Moisture availability over the past five centuries indicated by carbon isotopes of Tamarix taklamakanensis leaves in a nebkha profile in the Central Taklimakan Desert,NW China[J].Aeolian Research,2013,11:101-108.
[21] 赵元杰,李雪峰.罗布泊红柳沙包沉积纹层有机碳氮含量与气候变化[J].干旱区资源与环境,2011,25(4):149-154.
[22] Wang X M,Wang T,Dong Z B,et al.Nebkha development and its significance to wind erosion and land degradation in semi-arid northern China[J].Journal of Arid Environments,2006,65:129-141.
[23] Pye K.Aeolian Dust and Dust Deposits[M].London,UK:Academic Press,1987:1-256.
[24] 鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义[J].中国科学(D辑),1991,28(3):278-283.
[25] Bronger A,Heinkele T.Mineralogical and clay mineralogical aspects of loess research[J].Quaternary International,1990,7:37-53.
[26] 孙东怀,鹿化煜,David Rea,等.中国黄土粒度的双峰分布及其古气候意义[J].沉积学报,2000,18(3):327-335.
[27] 卢连战,史正涛.沉积物粒度参数内涵及计算方法的解析[J].环境科学与管理,2010,35(6):54-60.
[28] 杜建会,严平,董玉祥.干旱地区灌丛沙堆研究现状与展望[J].2010,65(3):339-350.
[29] 武胜利,李志忠,惠军,等.灌丛沙堆表面压力分布特征的实验研究[J].干旱区地理,2006,29(6):790-796.
[30] Yang X P,Scuderi L,Liu T,et al.Formation of the highest sand dunes on Earth[J].Geomorphology,2011,135:108-116.
[31] Yang X P,Li H W,Arthur C.Large-scale controls on the development of sand seas in northern China[J].Quaternary International,2012,250:74-83.
[32] Kuriyama Y,Mochizuki N,Nakashima T.Influence of vegetation on aeolian sand transport rate from a backshore to foredune at Hasaki,Japan[J].Sedimentology,2005,52:1123-1132.
[33] Trasande L,Landrigan P J,Schechter C.Public health and economic consequences of methyl mercury toxicity to the developing brain[J].Environmental Health Perspectives,2005,113(5):590-596.
[34] 冯新斌,仇广乐,付学吾,等.环境汞污染[J].化学进展,2009,21:436-457.
[35] Sun L G,Yin X B,Liu X D,et al.A 2000-year record of mercury and ancient civilizations in seal hairs from King George Island,West Antarctica[J].Science of the Total Environment,2006,368(1):236-247.
[36] Pyle D M,Mather T A.The importance of volcanic emissions for the global atmospheric mercury cycle[J].Atmospheric Environment,2003,37:5115-5124.
[37] Gustin M S.Are mercury emissions from geologic sources significant?A status report[J].Science of the Total Environment,2003,304(1):153-167.
[38] Gbor P K,Wen D,Meng F,et al.Modeling of mercury emission,transport and deposition in North America[J].Atmospheric Environment,2007,41(6):1135-1149.
[39] Outridge P M,Stern G A,Hamilton P B,et al.Trace metal profiles in the varved sediment of an Arctic lake[J].Geochimica et Cosmochimica Acta,2005,69(20):4881-4894.
[40] Schuster P F,Krabbenhoft D P,Naftz D L,et al.Atmospheric mercury deposition during the last 270 years:A glacial ice core record of natural and anthropogenic sources[J].Environmental Science & Technology,2002,36(11):2303-2310.
[41] 文雪琴,迟清华.中国汞的地球化学空间分布特征[J].地球化学,2007,36(6):621-627.
[42] Pyle D M,Mather T A.The importance of volcanic emission for the global atmospheric mercury cycle[J].Atmospheric Environment,2003,37:5115-5124.
[43] Hylander L D,Meili M.500 years of mercury production:global annual inventory by region until 2000 and associated emissions[J].Science of the Total Environment,2003,304:13-27.
[44] Berg T F,Steinnes E.Atmospheric mercury in Norway:Contributions from different sources[J].Science of the Total Environment,2006,368(1):3-9.
[45] Bethell L.Mining in colonial Spanish America[M]//Bethell L.The Cambridge History of Latin America. Cambridge,UK:Cambridge University Press,1984:105-151.
[46] Nriagu J O.Mercury pollution from the past mining of gold and silver in the Americas[J].Science of the Total Environment,1994,149:167-181.