[1]姜修洋,李志忠,陈秀玲,等.新疆伊犁河谷风沙沉积晚全新世孢粉记录与气候变化[J].中国沙漠,2011,31(4):855-861.[2]鲁瑞洁,王亚军,张登山.毛乌素沙地15 ka以来气候变化及沙漠演化研究[J].中国沙漠,2010,30(2):273-277.[3]蔡茂堂,魏明建.洛川地区倒数第二次间冰期气候变化研究[J].中国沙漠,2009,29(3):536-543.[4]Meyers P A.Organic geochemical proxies of paleoceanographic,paleolimnologic and paleoclimatic processe[J].Organic Geochemistry,1997,27(5-6):213-250.[5]Meyers P A,Lallier-Verges E.Lacustrine sedimentary organic matter records of Late Quaternary paleoclimates[J].Journal of Paleolimnology,1999,21:345-372.[6]Li Y,Wang N,Cheng H,et al.Holocene environmental change in the marginal area of the Asian monsoon:A record from Lake Zhuye,NW China[J].Boreas,2009,38:349-361.[7]萧家仪,吕海波,周卫健,等.末次盛冰期以来江西大湖花粉植被与环境演变[J].中国科学(D辑):地球科学,2007,37(6):789-797.[8]马春梅,朱诚,郑朝贵,等.中国东部山地泥炭高分辨率腐殖化度记录的晚冰期以来气候变化[J].中国科学(D辑):地球科学,2008,38(9):1078-1091.[9]中国科学院《中国自然地理》编辑委员会.中国自然地理:气候[M].北京:科学出版社,1984:1-30.[10]赵松乔.中国综合自然地理区划的一个新方案[J].地理学报,1983,38(1):1-10.[11]陈隆亨,曲耀光.河西地区水土资源及其开发利用[M].北京:科学出版社,1992:6-46.[12]黄大燊.甘肃植被[M].兰州:甘肃科学技术出版社,1997:163-176.[13]郭承录,李发明.石羊河流域生态系统存在的问题及治理对策[J].中国沙漠,2010,30(3):608-613.[14]张可新,刘普幸,霍华丽,等.石羊河流域近50 a来日照时数的时空变化特征分析[J].中国沙漠,2011,31(2):517-520.[15]冯绳武.民勤绿洲的水系演变[J].地理学报,1963,29(3):241-249.[16]李并成.猪野泽及其历史变迁考[J].地理学报,1993,48(1):55-59.[17]Pachur H J,Wunnemann B,Zhang H C.Lake evolution in the Tengger Desert,Northwest China,during the last 40 000 years[J].Quaternary Reasearch,1995,44:171-180.[18]Zhang H C,Ma Y Z,Li J J,et al.Palaeolake evolution and abrupt climate changes during last glacial period in NW China[J].Geophysical Research Letters,2001,28:3203-3206.[19]Zhang H C,Peng J L,Ma Y Z,et al.Late Quaternary palaeolake levels in Tengger Desert,NW China[J].Palaeogeography,Palaeoclimatology,Palaeoecology 2004,211:45-48.[20]王乃昂,李卓仑,程弘毅,等.阿拉善高原晚第四纪高湖面与大湖期的再探讨[J].科学通报,2011,56(17):1367-1377.[21]李育,王乃昂,李卓仑.河西猪野泽沉积物有机地化指标之间的关系及古环境意义[J].冰川冻土,2011,33(2):334-340.[22]Faegri K,Kaland P E,Krzywinski K.Textbook of Pollen Analysis[M].New York:Blackwell,1989:69-89.[23]Wang J Q,Liu J L.Amino acids and stable carbon isotope distributions in Taihu Lake,China,over the last 15 000 years,and their palaeoecological implications[J].Quaternary Research,2000,53:223-228.[24]Digerfeldt G,Olsson S,Sandgren P.Reconstruction of lake-level changes in lake Xinias,central Greece,during the last 40 000 years[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2000,158:65-82.[25]Krishnamurthy R V,Bhattacharya S K.Palaeoclimatic changes deduced from 13C/12C and C/N ratios of Karewa lake sediments India[J].Nature,1986,323:150-152.[26]Wagner B,Melles M,Hahne J.Holocene climate history of Geographical Socienty,East Greenland-evidence from lake sediments[J].Palaeogeography,Palaeoclimateology,Palaeoecology,2000,160:45-68.[27]Bowen R.Isotopes and Climates[M].London:Elsevier Applied Science,1991:128-131.[28]Tieszen L L,Boutton T W.Stable carbon isotopes in terrestrial ecosystem research[M]//Rundel P W,Ehleringer J R,Nagy K A.Stable Isotopes in Ecological Research.New York:Springer-Verlag,1989:167-195.[29]Wang G A,Han J M,Zhou L P.The relationship between carbon isotope ratios of C3 plants and average annual temperature in Northwest China[J].Geology in China,2002,29(1):55-57.[30]王国安,韩家懋.C3植物碳同位素在旱季和雨季中的变化[J].海洋地质与第四纪地质,2001,21:43-47.[31]刘贤赵.中国北方农牧交错带C3草本植物δ13C与温度的关系及其对水分利用效率的指示 [J].生态学报,2011,31(1):123-136. |