[1]An Z S,Porter S C,Kutzbach J E,et al.Asynchronous Holocene optimum of the East Asian monsoon[J].Quaternary Science Reviews,2000,19(8):743-762. [2]He Y,Theakstone W H,Zhang Z L,et al.Asynchronous Holocene climatic change across China[J].Quaternary Research,2004,61:52-63. [3]Hong Y T,Hong B,Lin Q H,et al.Correlation between Indian Ocean summer monsoon and North Atlantic climate during the Holocene[J].Earth and Planetary Science Letters,2003,211:371-380. [4]Hong Y T,Hong B,Lin Q H,et al.Inverse phase oscillations between the East Asian and Indian Ocean summer monsoons during the last 12000 years and paleo-El Nin[J].Earth and Planetary Science Letters,2005,231:337-346. [5]Hong Y T,Hong B,Lin Q H,et al.Synchronous climate anomalies in the western North Pacific and North Atlantic regions during the last 14 000 years[J].Quaternary Science Reviews,2009,28:840-849. [6]Jiang W Y,Guo Z T,Sun X J,et al.Reconstruction of climate and vegetation changes of Lake Bayanchagan (Inner Mongolia):Holocene variability of the East Asian monsoon[J].Quaternary Research,2006,65:411-420. [7]Jung S J A,Davies G R,Ganssen G M,et al.Synchronous Holocene sea surface temperature and rainfall variations in the Asian monsoon system[J].Quaternary Science Reviews,2004,23:2207-2218. [8]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. [9]陈发虎,黄小忠,杨美临,等.亚洲中部干旱区全新世气候变化的西风模式——以新疆博斯腾湖记录为例[J].第四纪研究,2006,26(6):881-887. [10]Yancheva G,Nowaczyk N R,Mingram J,et al.Influence of the intertropical convergence zone on the East Asian monsoon[J].Nature,2007,445:74-77. [11]叶玮.北疆地区全新世气候波动与水热组合特点[J].中国沙漠,2000,20(2):185-191. [12]薛积彬,钟巍,赵引娟,等.东疆北部全新世气候不稳定的湖泊沉积记录[J].中国沙漠,2008,28(4):648-656. [13]陈少勇,郭江勇,韩通,等.中国西北干旱半干旱区近46 a秋季气候变暖分析[J].中国沙漠,2009,29(3):544-550. [14]史玉光,孙照渤.新疆大气可降水量的气候特征及其变化[J].中国沙漠,2008,28(3):519-525. [15]辛渝,毛炜峄,李袁鹏,等.新疆不同季节降水气候分区及变化趋势[J].中国沙漠,2009,29(5):948-959. [16]王涛.干旱区绿洲化、荒漠化研究的进展与趋势[J].中国沙漠,2009,29(1):1-9. [17]罗传秀,郑卓,盘安定,等.新疆地区表土孢粉分布规律及其植被关系研究[J].干旱区地理,2007,30(4):536-543. [18]张 芸,孔昭宸,倪 健,等.新疆草滩湖湿地4550年以来的孢粉记录和环境演变[J].科学通报,2008,53(2):306-316. [19]冯晓华,阎顺,倪健,等.新疆北部平原湖泊记录的晚全新世湖面波动及环境变化[J].科学通报,2006,51(S1):49-55. [20]阎顺,穆桂金,孔昭宸,等.天山北麓晚全新世环境演变及其人类活动的影响[J].冰川冻土,2004,26(4):403-410. [21]鞠远江,刘耕年.孢粉记录揭示的4 000 a BP来乌鲁木齐河源区气候环境变化[J].冰川冻土,2004,26(2):166-170. [22]陈发虎,黄小忠,张家武,等.新疆博斯腾湖记录的亚洲内陆干旱区小冰期湿润气候研究[J].中国科学(D辑),2007,37(1):77-85. [23]叶 玮,袁玉江.新疆伊犁地区现代气候特征与300年来的干湿变化规律[J].中国沙漠,1999,19(2):97-103. [24]阎顺,许英勤.新疆阿勒泰地区表土孢粉组合[J].干旱区研究,1989,1:26-33. [25]孙湘君,杜乃秋,翁成郁,等.新疆玛纳斯湖盆周围近14 000年以来的古植被古环境[J].第四纪研究,1994,3:239-248. [26]姚檀栋,秦大河,田立德,等.青藏高原2 ka来温度与降水变化——古里雅冰芯记录[J].中国科学(D辑),1996,26(4):348-353. [27]Yang B,Braeuning A,Shi Y F,et al.Evidence for a late Holocene warm and humid climate periodand environmental characteristics in the arid zones of northwest China during 2.2~1.8 kyr BP[J].Journal of Geophysical Research,2004,109:1-10. [28]Yang X P,Zhu Z D,Jaekel D,et al.Late Quaternary palaeoenvironment change and landscape evolution along the Keriya River,Xinjiang,China:the relationship between high mountain glaciation and landscape evolution in foreland desert regions[J].Quaternary International,2002,(97-98):155-166. |