[1] THOMPSON R,OLDFIELD F. Environmental magnetism[M]. London:Allen&Unwin,1986:1-227.[2] ROBINSON S G. The late Pleistocene palaeoclimatic record of North Atlantic deep-sea sediments revealed by mineral magnetic measurements[J]. Physics of Earth and Planetary Interiors, 1986,(42):22-57.[3] THOMPSON R,BLOEMENDAL J,DEARING J A,et al. Environmental applications of magnetic measurements[J]. Science, 1980,(207):481-486.[4] LIU S Z,DENG C L,XIAO J L et al. High-resolution enviromagnetic records of the last deglaciation from Dali Lake,Inner Mongolia[J]. Palaeogeography,Palaeoclimatology,Palaeoecology, 2016,(454):1-11.[5] 申洪源,贾玉连,郭峰. 内蒙古黄旗海湖泊沉积物磁化率特征 及其环境意义[J]. 干旱区地理,2010,33(2):151-157.[SHEN Hongyuan,JIA Yulian,GUO Feng. Characteristics and environmental significance of the magnetic susceptibility in sediment of Huangqihai Lake,Inner Mongolia,China[J]. Arid Land Geography, 2010,33(2):151-157.][6] CHEN F H,LIU J B,XU Q H et al. Environmental magnetic studies of sediment cores from Gonghai Lake:implications for monsoon evolution in North China during the late glacial and Holocene[J]. Journal of Paleolimnology,2013,(49):447-464.[7] HELLER F,LIU T S. Magnetism of Chinese loess deposits[J]. Geophysical Journal of the Royal Astronomical Society,1984, (77):125-141.[8] KUKLA G,HELLER F,MING L X et al. Pleistocene climates in China dated by magnetic susceptibility[J]. Geology,1988, (16):811-814.[9] LIU T S,DING Z L. Chinese loess and the paleomoonsoon[J]. Annual Review of Earth and Planetary Sciences,1998,(26): 111-145.[10] LIU Q S,DENG C L,TORRENT J et al. Review of recent developments in mineral magnetism of the Chinese loess[J]. Quaternary Science Reviews,2007,(26):368-385.[11] LIU X M,HESSE P,Rolph T et al. Properties of magnetic mineralogy of Alaskan loess:evidence for pedogenesis[J]. Quaternary International,1999,(62):93-102.[12] HELLER F,LIU T S. Magnetostratigraphical dating of loess deposits in China[J]. Nature,1982,(300):431-433.[13] CHEN F H,BLOEMENDAL J,WANG J M,et al. High-resolution multi-proxy climate records from Chinese loess,evidence for rapid climatic changes over the last 75 kyr[J]. Palaeogeography Palaeoclimatology Palaeoecology,1997,(130):323-335.[14] DING Z L,DERBYSHIRE E,YANG S L et al. Stacked 2.6-Ma grain size record from the Chinese loess based on five sections and correlation with the deep-sea delta O-18 record[J]. Paleoceanography, 2002,17(3).[15] LANCI L,HIRT A M,LOWRIE W,et al. Mineral-magnetic record of late Quaternary climatic changes in a high Alpine lake[J]. Earth Planetary Science Letters,1999,(170):49-59.[16] HU S Y,DENG C L,APPEL E,et al. Environmental magnetic study on lacustrine sediments[J]. Chinese Science Bulletin, 2002,(47):613-616.[17] TUDRYN A,TUCHOLKA P,GIBERT E,et al. A late Pleistocene and Holocene mineral magnetic record from sediments of Lake Aibi,Dzungarian Basin,NW China[J]. Journal of Paleolimnology, 2010,44(1):109-121.[18] DEARING J A. Magnetic susceptibility[M]// WALDEN J, OLDFIELD F,SMITH J,eds. Environmental magnetism:a practical guide No.6. London:Quaternary Research Association, 1999:35-62.[19] ROBERTS A P,PIKE C R,VEROSUB K L. First-order reversal curve diagrams:a new tool for characterizing the magnetic properties of natural samples[J]. Journal of Geophysical Researchatmospheres, 2000,(105):28461-28475.[20] GEISS C E,BANERJEE S K. A multi-parameter rock magnetic record of the last glacial-interglacial paleoclimate from southcentral Illinois,USA[J]. Earth Planetary Science Letters,1997, (152):203-216.[21] 许英勤. 新疆博斯腾湖地区全新世以来的孢粉组合与环境[J]. 干旱区地理,1998,21(2):43-49.[XU Yingqin. The assemblage of Holocene spore pollen and its environment in Bosten Lake area Xinjiang[J]. Arid Land Geography,1998,21(2): 43-49.][22] 张英,夏敦胜,赵瑞瑞,等. 新疆博斯腾湖湖滨沉积物的磁学特 征及其环境意义[J]. 海洋地质与第四纪地质,2013,(4):93- 102.[ZHANG Ying,XIA Dunsheng,ZHAO Ruirui,et al. Magnetic propertites of the lakeshore sediments of the Bosten Lake, Xinjiang,China and their environmental implications[J]. Marine Geology & Quaternary Geology,2013,(4):93-102.][23] 黄小忠,陈发虎,肖舜,等. 新疆博斯腾湖沉积物粒度的古环境 意义初探[J]. 湖泊科学,2008,20(3):291-297.[HUANG Xiaozhong, CHEN Fahu,XIAO Shun,et al. Primary study on the environmental significances of grain-size changes of the Lake Bosten sediments[J]. Journal of Lake Sciences,2008,20(3): 291-297.][24] 范育新,赵晖,陈发虎,等. 博斯腾湖湖泊沉积物光释光年代测 量[J]. 第四纪研究,2007,27(4):568-575.[FAN Yuxin,ZHAO Hui,CHEN Fahu,et al. OSL dating of lacustrine sediments from Lake Bosten[J]. Quaternary Sciences,2007,27(4):568-575.][25] 张成君,曹洁,类延斌,等.中国新疆博斯腾湖全新世沉积环境 年代学特征[J]. 沉积学报,2004,22(3):494-499.[ZHANG Chengjun,CAO Jie,LEI Yanbin,et al. The chronological characteristics of Bosten Lake Holocene sediment environment in Xinjiang, China[J]. Acta Sedimentologica Sinica,2004,22(3): 494-499.][26] 钟巍,舒强. 南疆博斯腾湖近12.0 ka BP以来古气候与古水文 状况的变化博斯腾湖全新世湖相沉积相碳酸盐稳定同位素与 古气候的初步研究[J]. 海洋与湖沼,2001,32(2):213-220.[ZHONG Wei,SHU Qiang. Palaeoclimatic and Palaeohydrologic oscillations since about 12.0 ka BP at Bosten Lake,southern Xinjiang[J]. Oceanologia Et Limnologia Sinica,2001,32(2): 213-220.][27] MISCHKE S and WUNNEMANN B. The Holocene salinity history of Bosten Lake(Xinjiang,China)inferred from ostracod species assemblages and shell chemistry:possible palaeoclimatic implications[J]. Quaternary International,2006,(154):100- 112.[28] 张成君,郑绵平,ALEXANDER P,等. 博斯腾湖碳酸盐和同位 素组成的全新世古环境演变高分辨记录及与冰川活动的响应[J]. 地质学报,2007,81(12):1658-1671.[ZHANG Chengjun, ZHENG Mianping,ALEXANDER Prokopenko,et al. The plaeoenvironmental variation from the high-resolution record of the Holocene sediment carbonate andisotopic composition in Bosten Lake and responding to glacial activity[J]. Acta Geologica Sinica,2007,81(12):1658-1671.][29] 张家武,王君兰,郭小燕,等. 博斯腾湖全新世岩芯沉积物碳酸 盐氧同位素气候意义[J]. 第四纪研究,2010,30(6):1078- 1087.[ZHANG Jiawu,WANG Junlan,GUO Xiaoyan et al. Paleoclimatic significance of oxygen isotope composition of carbonates from a sediment core at Bosten Lake,Xinjiang,China[J]. Quaternary International,2010,30(6):1078-1087.][30] WUNNEMANN B,CHEN F H,RIEDEL F,et al. Holocene lake deposits of Bosten lake,southern Xinjiang,China[J]. Chinese Science Bulletin,2003,48(14):1429-1432.[31] WUNNEMANN B,MISCHKE S,CHEN F H. A Holocene sedimentary record from Bosten Lake,China[J]. Palaeogeography, Palaeoclimatology,Palaeoecology,2006,234(2):223-238.[32] 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.[CHEN Fahu,HUANG Xiaozhong, YANG Meilin,et al. Westerly dominated Holocene climate model in arid central Asia:case study on Bosten Lake,Xinjiang,China[J]. Quaternary Sciences,2006,26:881-887.][33] 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.[CHEN Fahu,HUANG Xiaozhong,ZHANG Jiawu, et al.Humid little ice age in arid central Asia documented by Bosten Lake,Xinjiang,China[J]. Science in China Series(D), Earth Sciences,2007,37(1):77-85.][34] 郭召杰,张志诚,钱祥麟,等. 新疆焉耆盆地构造特征及其石油 地质意义[J]. 石油实验地质,1998,20(3):205-209.[GUO Shaojie,ZHANG Zhicheng,QIAN Xianglin,et al. The structural styles and their role in hydrocarbon accumulation of the Yanqi Basin,NW China[J]. Experimental Petroleum Geology,1998, 20(3):205-209.][35] 王苏民,窦鸿身. 中国湖泊志[M]. 北京:科学出版社,1998: 345-346.[WANG Sumin,DOU Hongshen. China Lake Blog[M]. Beijing:Science Press,1998:345-346.][36] 程其畴. 博斯腾湖研究[M]. 南京:河海大学出版社,1995:1-7.[CHENG Qichou. Bosten Lake Research[M]. Nanjing:Hohai University Press,1995:1-7.][37] 刘丽梅,赵景峰,张建平,等. 近50 a 博斯腾湖逐年水量收支估 算与水平衡分析[J]. 干旱区地理,2013,36(1):33-40.[LIU Limei,ZHAO Jingfeng,ZHANG Jianping et al. Water balance of Lake Bosten using annual water-budgets method for the past 50 years[J]. Arid Land Geography,2013,36(1):33-40.][38] 李吉均. 中国西北地区晚更新世以来环境变迁模式[J]. 第四纪 研究,1990,(3):197-204.[LI Jijun. The patterns of environmental changes since late Pleistocene in Northwestern China[J]. Quaternary Sciences,1990,(3):197-204.][39] 石培宏,杨太保,田庆春,等. 靖远黄土-古土壤色度变化特征 分析及古气候意义[J]. 兰州大学学报(自然科学版),2012,48 (2):15-23.[SHI Peihong,YANG Taibao,TIAN Qingchun,et al. Chroma characteristics in the loess-paleosol at Jingyuan section and its signification to paleocliamete[J]. Journal of Lanzhou University(Natural Sciences),2012,48(2):15-23.][40] 曹洁,张家武,张成君,等. 青藏高原北缘哈拉湖近800 年来湖 泊沉积及其环境意义[J]. 第四纪研究,2007,27(1):100-107.[CAO Jie,ZHANG Jiawu,ZHANG Chengjun,et al. Environmental changes during the past 800 years recorded in lake sediments from Hala Lake on the Northern Tibetan Plateau[J]. Quaternary International,2007,27(1):100-107.][41] 罗超,杨东,彭子成,等. 新疆罗布泊地区近3.2 万年沉积物的 气候环境记录[J]. 第四纪研究,2007,27(1):114-121.[LUO Chao,YANG Dong,PENG Zicheng,et al. Climatic and environmental records in the sediment of the Luobei Billabong in Lop Nur,Xinjiang in recent 32 ka[J]. Quaternary International, 2007,27(1):114-121.][42] 刘青松,邓成龙. 磁化率及其环境意义[J]. 地球物理学报, 2009,52(4):1041-1048.[LIU Qingsong,DENG Chenglong. Magnetic susceptibility and its environmental significances[J]. Chinese Journal of Geophysics,2009,52(4):1041-1048.][43] WU D,ZHOU A F,LIU J B,et al. Changing intensity of human activity over the last 2,000 years recorded by the magnetic characteristics of sediments from Xingyun Lake,Yunnan,China[J]. Journal of Paleolimnology,2014,(53):47-60.[44] LIU Q S,BANERJEE S K,JACKSON M J,et al. New insights into partial oxidation model of magnetite and thermal alteration of magnetic mineralogy of the Chinese loess in air[J]. Geophysical Journal International,(158):506-514.[45] TORRES M A,WEST A J,LI G J. Sulphide oxidation and carbonate dissolution as a source of CO2 over geological timescales[J]. Nature,2014,507:346-349.[46] 成艾颖,余俊清,高春亮,等. 湖泊沉积物微量元素ICP-AES与 XRF分析方法和相关性研究[J]. 光谱学与光谱分析,2013,33 (7):1949-1952[. CHENGAiying,YU Junqing,GAO Chunliang, et al. Study on trace elements of lake sediments by ICP-AES and XRF core scanning[J]. Spectroscopy and Spectral Analysis, 2013,33(7):1949-1952.][47] HELMKE J P,SCHULZ M,BAUCH H A. Sediment-color record from the Northeast Atlantic reveals patterns of millennial- scale climate variability during the past 500,000 years[J]. Quaternary Research,2002,(57):49-57.[48] JI J,SHEN J,BALSAM W,et al. Asian monsoon oscillations in the northeastern Qinghai-Tibet Plateau since the late glacial as interpreted from visible reflectance of Qinghai Lake sediments[J]. Earth and Planetary Science Letters,2005,233(1):61-70.[49] CHEN F,YU Z C,YANG M,et al. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history[J]. Quaternary Science Reviews,2008, (27):351-364.[50] HUANG X Z,CHEN F H,FAN Y X,et al. Dry late-glacial and early Holocene climate in arid central Asia indicated by lithological and palynological evidence from Bosten Lake,China[J]. Quaternary International,2009,(194):19-27. |