晚第四纪湖泊沉积物盐类与碎屑矿物反相关关系的沉积学解释
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摘要
湖泊沉积物中矿物组合是古气候环境研究的敏感性指标之一,充分认识湖泊沉积物中各类矿物组合类型、沉积过程,对正确解释矿物学指标有重要意义.我国晚第四纪湖泊沉积记录中,盐类矿物与碎屑矿物含量普遍存在反相关关系,影响了矿物组合作为气候指标的解释和应用.从地球科学的角度正确理解这种关系,可以为湖泊动力学以及古气候环境定量研究提供重要的科学依据.选择甘肃民勤盆地石羊河下游终端湖猪野泽不同位置5个全新世剖面,在明确湖泊沉积物来源、搬运方式和沉积动力机制的基础上,研究了以碳酸盐矿物为主的盐类矿物含量与粒度指标之间的关系.结果表明:猪野泽各剖面砂层富含的中砂、细砂沉积物主要是来自于巴丹吉林沙漠和腾格里沙漠的风成砂;水动力作用主导了湖相沉积层200μm以下沉积物的沉积,风力作用对20~70μm粉砂组分沉积也有所贡献.同时,猪野泽湖相沉积层中高含量的碳酸盐主要来自于流水搬运,湖相沉积层位200μm以下的粉砂和极细砂是碳酸盐的主要富集区.综上所述,干旱区湖泊沉积物中盐类矿物含量与其沉积过程密切相关,盐类矿物在全球变化研究中的应用要建立在充分研究其沉积动力机制的基础上.
Mineral assemblages in lake sediments are sensitive indicators of palaeoclimates,whose types anddeposit processes have important significances to interpretations of mineralogical proxies. The ubiquitous inverse correlation between saline minerals and detrital minerals in the Late Quaternary lake sediments has disturbed the interpretation and application of mineral assemblages as a paleoclimate proxy. A correct understanding of the relationship from the perspective of earth sciences can provide important scientific basis for hydrodynamics of lake and quantitative research of palaeoclimate. In this paper,five sections from different positions of Zhuye Lake( Sections QTH01,QTH02,XQ,SKJ and JTL) were chosen to conduct a comparative study on saline mineral contents and grain sizes in order to make clear the sedimentary models of saline minerals and detrital mineralsunder different hydrodynamic conditions. The results revealed that in the aeolian layers,sediments above200 μm mainly are aeolian sands from the Badain Jaran Desert and the Tengger Desert. In lake sediments,wind force slightly contributes to the deposition of silt between 20 μm and 70 μm,but silt and sand under 200 μm are dominated by hydrodynamic effect,and carbonate mineral enriches in this grain size interval. Meanwhile,sedimentary processes of saline mineral showdifferent patterns under different sedimentary conditions. Sedimentary environment at Sections QTH01 and QTH02 was stationary,and carbonate content was significantly high;Section XQ had strong hydrodynamic condition. At the same time,Sections SKJ and JTL were far away from the estuary,and carbonate content was relatively low. Sedimentary environment at Sections QTH01,QTH02 and XQ were dominated by runoff, where there was high value of carbonate content in the lake sediments corresponding to a finer average grain size; Sections SKJ and JTL were influenced by local environment,so the high value of carbonate content was corresponding to coarse particles. Above all,saline mineral contents in lake sediments of arid areas were closely related to the sedimentary process; therefore,the application of the saline minerals in global change research should be established on the basis of the full study of the sedimentary dynamic mechanism.
Mineral assemblages in lake sediments are sensitive indicators of palaeoclimates,whose types anddeposit processes have important significances to interpretations of mineralogical proxies. The ubiquitous inverse correlation between saline minerals and detrital minerals in the Late Quaternary lake sediments has disturbed the interpretation and application of mineral assemblages as a paleoclimate proxy. A correct understanding of the relationship from the perspective of earth sciences can provide important scientific basis for hydrodynamics of lake and quantitative research of palaeoclimate. In this paper,five sections from different positions of Zhuye Lake( Sections QTH01,QTH02,XQ,SKJ and JTL) were chosen to conduct a comparative study on saline mineral contents and grain sizes in order to make clear the sedimentary models of saline minerals and detrital mineralsunder different hydrodynamic conditions. The results revealed that in the aeolian layers,sediments above200 μm mainly are aeolian sands from the Badain Jaran Desert and the Tengger Desert. In lake sediments,wind force slightly contributes to the deposition of silt between 20 μm and 70 μm,but silt and sand under 200 μm are dominated by hydrodynamic effect,and carbonate mineral enriches in this grain size interval. Meanwhile,sedimentary processes of saline mineral showdifferent patterns under different sedimentary conditions. Sedimentary environment at Sections QTH01 and QTH02 was stationary,and carbonate content was significantly high;Section XQ had strong hydrodynamic condition. At the same time,Sections SKJ and JTL were far away from the estuary,and carbonate content was relatively low. Sedimentary environment at Sections QTH01,QTH02 and XQ were dominated by runoff, where there was high value of carbonate content in the lake sediments corresponding to a finer average grain size; Sections SKJ and JTL were influenced by local environment,so the high value of carbonate content was corresponding to coarse particles. Above all,saline mineral contents in lake sediments of arid areas were closely related to the sedimentary process; therefore,the application of the saline minerals in global change research should be established on the basis of the full study of the sedimentary dynamic mechanism.
引文
[1]Jin Zhangdong.Composition,origin and environmental interpretation of minerals in lake sediments and recent progress[J].Journal of Earth Sciences and Environment,2011,33(1):38-48.[金章东.湖泊沉积物的矿物组成、成因、环境指示及研究进展[J].地球科学与环境学报,2011,33(1):38-48.]
[2]Lerman A.Lake:chemistry,geology,physics[M].Berlin:Springer,1978.
[3]Hakanson L,Jansson M.Principles of lake sedimentology[M].Berlin:Springer,1983.
[4]Jin Zhangdong,Wang Sumin,Shen Ji,et al.Chemical weathering since the Little Ice Age recorded in lake sediments:a highresolution proxy of past climate[J].Earth Surface Processes and Landforms,2001,26(7):775-782.
[5]Last W M,Smol J P.Tracking environmental change using lake sediments[M].Dordrecht,the Netherlands:Kluw er Academic Publishers,2001.
[6]Jin Zhangdong,Wu Yanhong,Zhang Xiaohui,et al.Role of Late Glacial to M id-Holocene climate in catchment w eathering in the central Tibetan Plateau[J].Quaternary Research,2005,63(2):161-170.
[7]Wu Yanhong,Li Shijie,Xia Weilan.Element geochemistry of lake sediment from Gourenco Lake,Kekexili,Qinghai-Xizang Plateau and its significance for climate variation[J].Journal of Earth Sciences and Environment,2004,26(3):64-68.[吴艳宏,李世杰,夏威岚.可可西里苟仁错湖泊沉积物元素地球化学特征及其环境意义[J].地球科学与环境学报,2004,26(3):64-68.]
[8]Crowley J K.Mapping playa evaporite minerals aviris data:A first report from Death Valley,California[J].Remote Sensing of Environment,1993,44(2/3):337-356.
[9]Bryant R G,Sellwood B W,Millington A C,et al.Marine-like potash evaporite formation on a continental playa:case study from Chottel Djerid,southern Tunisia[J].Sedimentary Geology,1994,90(3):269-291.
[10]Yao Bo,Liu Xingqi,Wang Yongbo,et al.Late Holocene climatic changes revealed by mineralogical records from lacustrine core KS-2006 from Lake Kusai in the Hoh Xil area,northern Tibetan Plateau[J].Lake Sciences,2011,23(6):903-909.[姚波,刘兴起,王永波,等.可可西里库赛湖KS-2006孔矿物组成揭示的青藏高原北部晚全新世气候变迁[J].湖泊科学,2011,23(6):903-909.]
[11]Rhodes T E,Gasse F,Lin R F,et al.A Late Pleistocene-Holocene lacustrine record from Lake M anas,Zunggar(northern Xinjiang,w estern China)[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1996,120(1):105-121.
[12]Wei K,Gasse F.Oxygen isotopes in lacustrine carbonates of West China revisited:implications for post glacial changes in summer monsoon circulation[J].Quaternary Science Review s,1999,18(12):1315-1334.
[13]Chen Jing'an,Wan Guojiang,Chen Zhenlou,et al.Chemical elements in sediments of Lake Erhai and palaeoclimate evolution[J].Geochemica,1999,28(6):562-570.[陈敬安,万国江,陈振楼,等.洱海沉积物化学元素与古气候演化[J].地球化学,1999,28(6):562-570.]
[14]Chen Jing'an,Wan Guojiang,Wang Fushun,et al.A study on modern lake sedimentary carbon environmental records[J].Science in China(Series D),2002,45(10):875-884.[陈敬安,万国江,汪福顺,等.湖泊现代沉积物碳环境记录研究[J].中国科学(D辑),2002,32(1):73-80.]
[15]Zheng Mianping.Salt lake resources and eco-environment in China[J].Acta Geologica Sinica,2010,84(11):1613-1622.[郑绵平.中国盐湖资源与生态环境[J].地质学报,2010,84(11):1613-1622.]
[16]Zheng Dazhong,Zheng Ruofeng.Material sources and prospecting indicators of potassium deposits[J].Journal of Salt Lake Research,2006,14(4):9-17.[郑大中,郑若锋.论钾盐矿床的物质来源和找矿指示[J].盐湖研究,2006,14(4):9-17.]
[17]Zheng Xiyu.Sedimentary features of sylvite-nitrate in Lake Wuzunbulake[J].Journal of Salt Lake Research,2000,8(1):41-45.[郑喜玉.乌尊布拉克湖硝酸钾盐沉积特征[J].盐湖研究,2000,8(1):41-45.]
[18]Sun Qing,Chu Guoqiang,Li Shengqiang,et al.Long chain ketene in sulfate type salt lake and its paleoenvironment significance[J].Chinese Science Bulletin,2004,49(19):2082-2086.[孙青,储国强,李圣强,等.硫酸盐型盐湖中的长链烯酮及古环境意义[J].科学通报,2004,49(17):1789-1792.]
[19]Morton A C,Hallsworth C.Identifying provenance-specific features of detrital heavy mineral assemblages in sandstones[J].Sedimentary Geology,1994,90(3):241-256.
[20]Frihy O E,Lotfy M F,Komar P D.Spatial variations in heavy minerals and patterns of sediment sorting along the Nile Delta,Egypt[J].Sedimentary Geology,1995,97(1):33-41.
[21]Morton A C,Hallsworth C.Processes controlling the composition of heavy mineral assemblages in sandstones[J].Sedimentary Geology,1999,124(1):3-29.
[22]Ruhl K W,Hodges K V.The use of detrital mineral cooling ages to evaluate steady state assumptions in active orogens:An example from the central Nepalese Himalaya[J].Tectonics,2005,24(4).doi:10.1029/2004TC001712.
[23]Hallsworth C R,Morton A C,Claou-Long J,et al.Carboniferous sand provenance in the Pennine Basin,UK:constraints from heavy mineral and detrital zircon age data[J].Sedimentary Geology,2000,137(3):147-185.
[24]Chen Lirong.Sedimentary mineralogy in China sea[M].Beijing:China Ocean Press,2008:22-30.[陈丽蓉.中国海沉积矿物学[M].北京:海洋出版社,2008:22-30.]
[25]Wang Zhongbo,Yang Shouye,Li Rihui,et al.Detrital mineral composition of the sediments from Huanghe and its hydrodynamic environmental constraints[J].M arine Geology&Quaternary Geology,2010,30(4):78-90.[王中波,杨守业,李日辉,等.黄河水系沉积物碎屑矿物组成及沉积动力环境约束[J].海洋地质与第四纪地质,2010,30(4):78-90.]
[26]Biscaye P E.Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans[J].Geological Society of America Bulletin,1965,76(7):803-832.
[27]Singer A.The paleoclimatic interpretation of clay minerals in sediments:a review[J].Earth-Science Review s,1984,21(4):251-293.
[28]Yuretich R,Melles M,Sarata B,et al.Clay minerals in the sediments of Lake Baikal:a useful climate proxy[J].Journal of Sedimentary Research,1999,69(3):588-596.
[29]Dong Zhiwen,Ren Jiawen,Qin Dahe,et al.Chemistry characteristics and environmental significance of snow deposited on the Laohugou Glacier No.12,Qilian M ountains[J].Journal of Glaciology and Geocryology,2013,35(2):327-335.[董志文,任贾文,秦大河,等.祁连山老虎沟12号冰川积雪化学特征及环境意义[J].冰川冻土,2013,35(2):327-335.]
[30]Tang Yanjie,Jia Jianye,Xie Xiande.Environment significance of clay minerals[J].Earth Science Frontiers,2002,9(2):337-344.[汤艳杰,贾建业,谢先德.黏土矿物的环境意义[J].地学前缘,2002,9(2):337-344.]
[31]Mueller A D,Anselmetti F S,Ariztegui D,et al.Late Quaternary palaeoenvironment of northern Guatemala:evidence from deep drill cores and seismic stratigraphy of Lake Petén Itzá[J].Sedimentology,2010,57(5):1220-1245.
[32]Xue Jibin,Zhong Wei.Holocene climate change recorded by lacustrine sediments in Barkol Lake and its regional comparison[J].Quaternary Sciences,2008,28(4):610-620.[薛积彬,钟巍.新疆巴里坤湖全新世环境记录及区域对比研究[J].第四纪研究,2008,28(4):610-620.]
[33]Zhang Chengjun,Zheng Mianping,Prokopenko A,et al.The palaeoenvironmental variation from the high-resolution record of the Holocene sediment carbonate and isotopic composition in Bosten Lake and responding to glacial activity[J].Acta Geologica Sinica,2007,81(12):1658-1671.[张成君,郑绵平,Prokopenko A,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.]
[34]Li Bingxiao,Cai Biqin,Liang Qingsheng.Depositional characteristics of Aydingkol Lake in Turpan depression[J].Chinese Science Bulletin,1989,34(18):1551-1555.[李秉孝,蔡碧琴,梁青生.吐鲁番盆地艾丁湖沉积特征[J].科学通报,1989,34(8):608-610.]
[35]Ji Lei,Xia Weilan,Xiang Liang,et al.Mineral composition and sedimentation rate of surficial sediments in Hulun Lake,Inner M ongolia[J].Lake Sciences,1994,6(3):227-232.[吉磊,夏威岚,项亮,等.内蒙古呼伦湖表层沉积物的矿物组成和沉积速率[J].湖泊科学,1994,6(3):227-232.]
[36]Shen Ji,Wang Sumin,Zhu Yuxin,et al.Quantitative reconstruction of the lake w ater paleotemperature of Daihai Lake,Inner M ongolia,China and its significance in paleoclimate[J].Science in China(Series D),2002,45(9):792-800.[沈吉,王苏民,朱育新,等.内蒙古岱海古水温定量恢复及其古气候意义[J].中国科学(D辑),2001,31(12):1017-1023.]
[37]Chen Fahu,Zhu Yan,Li Jijun,et al.Abrupt Holocene changes of the Asian monsoon at millenial and centennial scales:Evidence from lake sediment document in M inqin Basin,NW China[J].Chinese Science Bulletin,2001,46(23):1942-1947.[陈发虎,朱艳,李吉均,等.民勤盆地湖泊沉积记录的全新世千百年尺度夏季风快速变化[J].科学通报,2001,46(23):1414-1419.]
[38]Li Rongquan.Lakes and environmental changes in Inner Mongolia Plateau[M].Beijing:Beijing Normal University Press,1990.[李容全.内蒙古高原湖泊与环境变迁[M].北京:北京师范大学出版社,1990.]
[39]Zheng Xiyu,Zhang Minggang,Dong Jihe.Salt lake in Inner M ongolia[M].Beijing:Science Press,1992.[郑喜玉,张明刚,董继和.内蒙古盐湖[M].北京:科学出版社,1992.]
[40]Gasse F,Arnold M,Fontes J C,et al.A 13 000-year climate record from w estern Tibet[J].Nature,1991,353(6346):742-745.
[41]Liu Xingqi,Dong Hailiang,Rech J A,et al.Evolution of Chaka Salt Lake in NW China in response to climatic change during the Latest Pleistocene-Holocene[J].Quaternary Science Review s,2008,27(7):867-879.
[42]Feng Shengwu.The evolution of the drainage system of the Minqin oasis[J].Acta Geographica Sinica,1963,29(3):241-249.[冯绳武.民勤绿洲的水系演变[J].地理学报,1963,29(3):241-249.]
[43]Li Bingcheng.A study on the Zhuye Lake and its historical evolution[J].Acta Geographica Sinica,1993,48(1):55-59.[李并成.猪野泽及其历史变迁考[J].地理学报,1993,48(1):55-59.]
[44]Zhu Yan,Xie Yaowen,Cheng Bo,et al.Pollen transport in the Shiyang River drainage[J].Chinese Science Bulletin,2003,48(14):1499-1506.[朱艳,程波,陈发虎,等.石羊河流域现代孢粉传播研究[J].科学通报,2004,49(1):15-21.]
[45]Zhao Y,Yu Z,Chen F,et al.Holocene vegetation and climate change from a lake sediment record in the Tengger Sandy Desert,northw est China[J].Journal of Arid Environment,2008,72:2054-2064.
[46]Li Yu,Wang Nai'ang,Cheng Hongyi,et al.Holocene environmental change in the marginal area of the Asian monsoon:a record from Zhuye Lake,NW China[J].Boreas,2009,38:349-361.
[47]Li Yu,Wang Nai'ang,Li Zhuolun,et al.Holocene palynological records and their responses to the controversies of climate system in the Shiyang River drainage basin[J].Chinese Science Bulletin,2011,56(2):161-172.[李育,王乃昂,李卓仑,等.石羊河流域全新世孢粉记录及其对气候系统响应争论的启示[J].科学通报,2011,55(10):1669-1678.]
[48]Editorial Board of Physical Geography of China,Chinese Academy of Sciences.China's natural geography and climate[M].Beijing:Science Press,1984:1-30.[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.]
[49]Chen F H,Yu Z C,Yang M L,et al.Holocene moisture evolution in arid central Asia and its out-of-phase relationship w ith Asian monsoon history[J].Quaternary Science Review s,2008,27:351-364.
[50]Guo Xiaoyin,Chen Fahu,Xie Yaowen,et al.A study on modeling the terminal lake of Shiyang River Drainage Basin under the natural conditions[J].Journal of Natural Resources,1999,14(4):94-97.[郭晓寅,陈发虎,颉耀文,等.自然条件下石羊河终闾湖泊模拟研究[J].自然资源学报,1999,14(4):94-97.]
[51]Zhao Qiang.Environmental change of Shiyang River drainage basin since the Last Deglaciation[D].Lanzhou:Lanzhou University,2005.[赵强.石羊河流域末次冰消期以来环境变化研究[D].兰州:兰州大学,2005.]
[52]Wei Wei,Shi Peiji,Yang Wangming,et al.Spatial distribution of land surface temperature in Shiyang River basin based on M ODIS data[J].Journal of Glaciology and Geocryology,2013,35(1):57-64.[魏伟,石培基,杨旺明,等.基于MODIS数据的石羊河流域地表温度空间格局[J].冰川冻土,2013,35(1):57-64.]
[53]Chen Longhen,Qu Yaoguang.Water and soil resources and its exploitation and utilization in Hexi area[M].Beijing:Science Press,1992:6-46.[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.]
[54]Zhang Kecun,Qu Jianjun,Ma Zhonghua.Environmental characteristics of sandstorm in M inqin county in recent 50 years[J].Journal of Desert Research,2004,24(3):257-260.[张克存,屈建军,马中华.近50 a来民勤沙尘暴的环境特征[J].中国沙漠,2004,24(3):257-260.]
[55]Long Hao,Wang Nai'ang,Ma Haizhou,et al.Eolian activity and environment evolution history recorded by the Qingtu Lake,NW Tengger Desert[J].Acta Sedimentologica Sinica,2007,25(4):626-631.[隆浩,王乃昂,马海州,等.腾格里沙漠西北缘湖泊沉积记录的区域风沙特征[J].沉积学报,2007,25(4):626-631.]
[56]Zhao Q,Wang N A,Li X M.Lacustrine strata sedimentology and lake-level history in ancient Zhuyeze Lake since the Last Deglaciation[J].Frontiers of Earth Science in China,2008,2(2):199-208.
[57]Long H,Lai Z P,Wang N A,et al.Holocene climate variations from Zhuyeze terminal lake records in East Asian monsoon margin in arid northern China[J].Quaternary Research,2010,74(1):46-56.
[58]Li Y,Wang N A,Li Z L,et al.Reworking effects in the Holocene Zhuye Lake sediments:A case study by pollen concentrates AM S14C dating[J].Science China:Earth Sciences,2012,55(10):1669-1678.
[59]Long Hao.Mid-Holocene climate variation from lake evidences of east Asian monsoon margin areas[D].Lanzhou:Lanzhou University,2006.[隆浩.季风边缘区全新世中期气候变化的古湖泊记录[D].兰州:兰州大学,2006.]
[60]Pye K.Aeolian dust and dust deposits[M].London:Academic Press,1987:29-62.
[61]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(3/4):263-277.
[62]Ren Mingda,Wang Nailiang.Introduction to the modern sedimentary environment[M].Beijing:Science Press,1985:1-4.[任明达,王乃梁.现代沉积环境概论[M].北京:科学出版社,1985:1-4.]
[63]Zhao Qiang,Wang Nai'ang,Cheng Hongyi,et al.Grain-size characteristics of Qingtu lake sediments and its paleaoenvironment explanation[J].Arid Land Geography,2003,26(1):2-6.[赵强,王乃昂,程弘毅,等.青土湖沉积物粒度特征及其古环境意义[J].干旱区地理,2003,26(1):2-6.]
[64]Sun Donghuai,An Zhisheng,Su Ruixia,et al.Grain size numerical partitioning of the sedimentary components and its applications[J].Progress in Natural Science,2001,11(3):269-276.[孙东怀,安芷生,苏瑞侠,等.古环境中沉积物粒度组分分离的数学方法及其应用[J].自然科学进展,2001,11(3):269-276.]
[65]Sun Donghuai,Lu Huayu,Rea D,et al.Bimode grain-size distribution of Chinese loess and its paleoclimate implication[J].Acta Sedimentologica Sinica,2000,18(3):327-335.[孙东怀,鹿化煜,Rea D,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.]
[66]Campell C.Late Holocene lake sedimentology and climate change in southern Alberta,Canada[J].Quaternary Research,1997,49(1):96-101.
[67]Chen Jing'an,Wan Guojiang,Zhang D D,et al.Environmental records of lacustrine sediments in different time scales:Sediment grain size as an example[J].Science in China(Series D),2004,47(10):954-960.[陈敬安,万国江,张峰,等.不同时间尺度下的湖泊沉积物环境纪录:以沉积物粒度为例[J].中国科学(D辑),2003,33(6):563-568.]
[68]Wang Junbo,Zhu Liping.Grain-size characteristics and their paleo-environmental significance of Chen Co Lake sediments in southern Tibet[J].Progress in Geography,2002,21(5):459-467.[王君波,朱立平.藏南沉错沉积物的粒度特征及其古环境意义[J].地理科学进展,2002,21(5):459-467.]
[69]Sun Qianli,Zhou Jie,Xiao Jule.Grain-size characteristics of lake Daihai sediments and its palaeoenvironment significance[J].M arin Geology&Quaternary Geology,2001,21(1):93-95.[孙千里,周杰,肖举乐.岱海沉积物粒度特征及其古环境意义[J].海洋地质与第四纪地质,2001,21(1):93-95.]
[70]Sun Yongchuan,Li Huisheng.The sedimentary facies and sedimentary environment of clastic rocks[M].Beijing:Geological Publishing House,1986:65-81.[孙永传,李惠生.碎屑岩沉积相和沉积环境[M].北京:地质出版社,1986:65-81.]
[71]Chen Fahu,Wu Wei,Holmes J A,et al.A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau,Inner M ongolia,China[J].Chinese Science Bulletin,2003,48(14):1401-1410.
[72]Zhang Liang,Zhang Qiang,Feng Jianying,et al.A study of atmospheric w ater cycle over the Qilian M ountains(I):Variation of annual w ater vapor transport[J].Journal of Glaciology and Geocryology,2014,36(5):1079-1091.[张良,张强,冯建英,等.祁连山地区大气水循环研究(I):空中水汽输送年际变化分析[J].冰川冻土,2014,36(5):1079-1091.]
[73]Zhang Xiao'e,Shen Zhibao,Zhang Guangyu,et al.Remote mineral aerosols in Westeries and their contributions to the Chinese loess[J].Science in China(Series D),1996,39(2):134-143.
[74]Li Enju.A comparative study of sediments characteristics between the Badain Jaran Desert and Tengger Desert[D].Xi'an:Shaanxi Normal University,2001.[李恩菊.巴丹吉林沙漠与腾格里沙漠沉积物特征的对比研究[D].西安:陕西师范大学,2001.]
[75]Li Zhuolun,Wang Nai'ang,Li Yu,et al.The salinity change and its environmental significance in Huahai Lake,Heixi Corridor,Northw est China during the early-middle Holocene[J].Journal of Glaciology and Geocryology,2013,35(6):1481-1489.[李卓仑,王乃昂,李育,等.河西走廊花海古湖泊早、中全新世湖水盐度变化及其环境意义[J].冰川冻土,2013,35(6):1481-1489.]
[2]Lerman A.Lake:chemistry,geology,physics[M].Berlin:Springer,1978.
[3]Hakanson L,Jansson M.Principles of lake sedimentology[M].Berlin:Springer,1983.
[4]Jin Zhangdong,Wang Sumin,Shen Ji,et al.Chemical weathering since the Little Ice Age recorded in lake sediments:a highresolution proxy of past climate[J].Earth Surface Processes and Landforms,2001,26(7):775-782.
[5]Last W M,Smol J P.Tracking environmental change using lake sediments[M].Dordrecht,the Netherlands:Kluw er Academic Publishers,2001.
[6]Jin Zhangdong,Wu Yanhong,Zhang Xiaohui,et al.Role of Late Glacial to M id-Holocene climate in catchment w eathering in the central Tibetan Plateau[J].Quaternary Research,2005,63(2):161-170.
[7]Wu Yanhong,Li Shijie,Xia Weilan.Element geochemistry of lake sediment from Gourenco Lake,Kekexili,Qinghai-Xizang Plateau and its significance for climate variation[J].Journal of Earth Sciences and Environment,2004,26(3):64-68.[吴艳宏,李世杰,夏威岚.可可西里苟仁错湖泊沉积物元素地球化学特征及其环境意义[J].地球科学与环境学报,2004,26(3):64-68.]
[8]Crowley J K.Mapping playa evaporite minerals aviris data:A first report from Death Valley,California[J].Remote Sensing of Environment,1993,44(2/3):337-356.
[9]Bryant R G,Sellwood B W,Millington A C,et al.Marine-like potash evaporite formation on a continental playa:case study from Chottel Djerid,southern Tunisia[J].Sedimentary Geology,1994,90(3):269-291.
[10]Yao Bo,Liu Xingqi,Wang Yongbo,et al.Late Holocene climatic changes revealed by mineralogical records from lacustrine core KS-2006 from Lake Kusai in the Hoh Xil area,northern Tibetan Plateau[J].Lake Sciences,2011,23(6):903-909.[姚波,刘兴起,王永波,等.可可西里库赛湖KS-2006孔矿物组成揭示的青藏高原北部晚全新世气候变迁[J].湖泊科学,2011,23(6):903-909.]
[11]Rhodes T E,Gasse F,Lin R F,et al.A Late Pleistocene-Holocene lacustrine record from Lake M anas,Zunggar(northern Xinjiang,w estern China)[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1996,120(1):105-121.
[12]Wei K,Gasse F.Oxygen isotopes in lacustrine carbonates of West China revisited:implications for post glacial changes in summer monsoon circulation[J].Quaternary Science Review s,1999,18(12):1315-1334.
[13]Chen Jing'an,Wan Guojiang,Chen Zhenlou,et al.Chemical elements in sediments of Lake Erhai and palaeoclimate evolution[J].Geochemica,1999,28(6):562-570.[陈敬安,万国江,陈振楼,等.洱海沉积物化学元素与古气候演化[J].地球化学,1999,28(6):562-570.]
[14]Chen Jing'an,Wan Guojiang,Wang Fushun,et al.A study on modern lake sedimentary carbon environmental records[J].Science in China(Series D),2002,45(10):875-884.[陈敬安,万国江,汪福顺,等.湖泊现代沉积物碳环境记录研究[J].中国科学(D辑),2002,32(1):73-80.]
[15]Zheng Mianping.Salt lake resources and eco-environment in China[J].Acta Geologica Sinica,2010,84(11):1613-1622.[郑绵平.中国盐湖资源与生态环境[J].地质学报,2010,84(11):1613-1622.]
[16]Zheng Dazhong,Zheng Ruofeng.Material sources and prospecting indicators of potassium deposits[J].Journal of Salt Lake Research,2006,14(4):9-17.[郑大中,郑若锋.论钾盐矿床的物质来源和找矿指示[J].盐湖研究,2006,14(4):9-17.]
[17]Zheng Xiyu.Sedimentary features of sylvite-nitrate in Lake Wuzunbulake[J].Journal of Salt Lake Research,2000,8(1):41-45.[郑喜玉.乌尊布拉克湖硝酸钾盐沉积特征[J].盐湖研究,2000,8(1):41-45.]
[18]Sun Qing,Chu Guoqiang,Li Shengqiang,et al.Long chain ketene in sulfate type salt lake and its paleoenvironment significance[J].Chinese Science Bulletin,2004,49(19):2082-2086.[孙青,储国强,李圣强,等.硫酸盐型盐湖中的长链烯酮及古环境意义[J].科学通报,2004,49(17):1789-1792.]
[19]Morton A C,Hallsworth C.Identifying provenance-specific features of detrital heavy mineral assemblages in sandstones[J].Sedimentary Geology,1994,90(3):241-256.
[20]Frihy O E,Lotfy M F,Komar P D.Spatial variations in heavy minerals and patterns of sediment sorting along the Nile Delta,Egypt[J].Sedimentary Geology,1995,97(1):33-41.
[21]Morton A C,Hallsworth C.Processes controlling the composition of heavy mineral assemblages in sandstones[J].Sedimentary Geology,1999,124(1):3-29.
[22]Ruhl K W,Hodges K V.The use of detrital mineral cooling ages to evaluate steady state assumptions in active orogens:An example from the central Nepalese Himalaya[J].Tectonics,2005,24(4).doi:10.1029/2004TC001712.
[23]Hallsworth C R,Morton A C,Claou-Long J,et al.Carboniferous sand provenance in the Pennine Basin,UK:constraints from heavy mineral and detrital zircon age data[J].Sedimentary Geology,2000,137(3):147-185.
[24]Chen Lirong.Sedimentary mineralogy in China sea[M].Beijing:China Ocean Press,2008:22-30.[陈丽蓉.中国海沉积矿物学[M].北京:海洋出版社,2008:22-30.]
[25]Wang Zhongbo,Yang Shouye,Li Rihui,et al.Detrital mineral composition of the sediments from Huanghe and its hydrodynamic environmental constraints[J].M arine Geology&Quaternary Geology,2010,30(4):78-90.[王中波,杨守业,李日辉,等.黄河水系沉积物碎屑矿物组成及沉积动力环境约束[J].海洋地质与第四纪地质,2010,30(4):78-90.]
[26]Biscaye P E.Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans[J].Geological Society of America Bulletin,1965,76(7):803-832.
[27]Singer A.The paleoclimatic interpretation of clay minerals in sediments:a review[J].Earth-Science Review s,1984,21(4):251-293.
[28]Yuretich R,Melles M,Sarata B,et al.Clay minerals in the sediments of Lake Baikal:a useful climate proxy[J].Journal of Sedimentary Research,1999,69(3):588-596.
[29]Dong Zhiwen,Ren Jiawen,Qin Dahe,et al.Chemistry characteristics and environmental significance of snow deposited on the Laohugou Glacier No.12,Qilian M ountains[J].Journal of Glaciology and Geocryology,2013,35(2):327-335.[董志文,任贾文,秦大河,等.祁连山老虎沟12号冰川积雪化学特征及环境意义[J].冰川冻土,2013,35(2):327-335.]
[30]Tang Yanjie,Jia Jianye,Xie Xiande.Environment significance of clay minerals[J].Earth Science Frontiers,2002,9(2):337-344.[汤艳杰,贾建业,谢先德.黏土矿物的环境意义[J].地学前缘,2002,9(2):337-344.]
[31]Mueller A D,Anselmetti F S,Ariztegui D,et al.Late Quaternary palaeoenvironment of northern Guatemala:evidence from deep drill cores and seismic stratigraphy of Lake Petén Itzá[J].Sedimentology,2010,57(5):1220-1245.
[32]Xue Jibin,Zhong Wei.Holocene climate change recorded by lacustrine sediments in Barkol Lake and its regional comparison[J].Quaternary Sciences,2008,28(4):610-620.[薛积彬,钟巍.新疆巴里坤湖全新世环境记录及区域对比研究[J].第四纪研究,2008,28(4):610-620.]
[33]Zhang Chengjun,Zheng Mianping,Prokopenko A,et al.The palaeoenvironmental variation from the high-resolution record of the Holocene sediment carbonate and isotopic composition in Bosten Lake and responding to glacial activity[J].Acta Geologica Sinica,2007,81(12):1658-1671.[张成君,郑绵平,Prokopenko A,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.]
[34]Li Bingxiao,Cai Biqin,Liang Qingsheng.Depositional characteristics of Aydingkol Lake in Turpan depression[J].Chinese Science Bulletin,1989,34(18):1551-1555.[李秉孝,蔡碧琴,梁青生.吐鲁番盆地艾丁湖沉积特征[J].科学通报,1989,34(8):608-610.]
[35]Ji Lei,Xia Weilan,Xiang Liang,et al.Mineral composition and sedimentation rate of surficial sediments in Hulun Lake,Inner M ongolia[J].Lake Sciences,1994,6(3):227-232.[吉磊,夏威岚,项亮,等.内蒙古呼伦湖表层沉积物的矿物组成和沉积速率[J].湖泊科学,1994,6(3):227-232.]
[36]Shen Ji,Wang Sumin,Zhu Yuxin,et al.Quantitative reconstruction of the lake w ater paleotemperature of Daihai Lake,Inner M ongolia,China and its significance in paleoclimate[J].Science in China(Series D),2002,45(9):792-800.[沈吉,王苏民,朱育新,等.内蒙古岱海古水温定量恢复及其古气候意义[J].中国科学(D辑),2001,31(12):1017-1023.]
[37]Chen Fahu,Zhu Yan,Li Jijun,et al.Abrupt Holocene changes of the Asian monsoon at millenial and centennial scales:Evidence from lake sediment document in M inqin Basin,NW China[J].Chinese Science Bulletin,2001,46(23):1942-1947.[陈发虎,朱艳,李吉均,等.民勤盆地湖泊沉积记录的全新世千百年尺度夏季风快速变化[J].科学通报,2001,46(23):1414-1419.]
[38]Li Rongquan.Lakes and environmental changes in Inner Mongolia Plateau[M].Beijing:Beijing Normal University Press,1990.[李容全.内蒙古高原湖泊与环境变迁[M].北京:北京师范大学出版社,1990.]
[39]Zheng Xiyu,Zhang Minggang,Dong Jihe.Salt lake in Inner M ongolia[M].Beijing:Science Press,1992.[郑喜玉,张明刚,董继和.内蒙古盐湖[M].北京:科学出版社,1992.]
[40]Gasse F,Arnold M,Fontes J C,et al.A 13 000-year climate record from w estern Tibet[J].Nature,1991,353(6346):742-745.
[41]Liu Xingqi,Dong Hailiang,Rech J A,et al.Evolution of Chaka Salt Lake in NW China in response to climatic change during the Latest Pleistocene-Holocene[J].Quaternary Science Review s,2008,27(7):867-879.
[42]Feng Shengwu.The evolution of the drainage system of the Minqin oasis[J].Acta Geographica Sinica,1963,29(3):241-249.[冯绳武.民勤绿洲的水系演变[J].地理学报,1963,29(3):241-249.]
[43]Li Bingcheng.A study on the Zhuye Lake and its historical evolution[J].Acta Geographica Sinica,1993,48(1):55-59.[李并成.猪野泽及其历史变迁考[J].地理学报,1993,48(1):55-59.]
[44]Zhu Yan,Xie Yaowen,Cheng Bo,et al.Pollen transport in the Shiyang River drainage[J].Chinese Science Bulletin,2003,48(14):1499-1506.[朱艳,程波,陈发虎,等.石羊河流域现代孢粉传播研究[J].科学通报,2004,49(1):15-21.]
[45]Zhao Y,Yu Z,Chen F,et al.Holocene vegetation and climate change from a lake sediment record in the Tengger Sandy Desert,northw est China[J].Journal of Arid Environment,2008,72:2054-2064.
[46]Li Yu,Wang Nai'ang,Cheng Hongyi,et al.Holocene environmental change in the marginal area of the Asian monsoon:a record from Zhuye Lake,NW China[J].Boreas,2009,38:349-361.
[47]Li Yu,Wang Nai'ang,Li Zhuolun,et al.Holocene palynological records and their responses to the controversies of climate system in the Shiyang River drainage basin[J].Chinese Science Bulletin,2011,56(2):161-172.[李育,王乃昂,李卓仑,等.石羊河流域全新世孢粉记录及其对气候系统响应争论的启示[J].科学通报,2011,55(10):1669-1678.]
[48]Editorial Board of Physical Geography of China,Chinese Academy of Sciences.China's natural geography and climate[M].Beijing:Science Press,1984:1-30.[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.]
[49]Chen F H,Yu Z C,Yang M L,et al.Holocene moisture evolution in arid central Asia and its out-of-phase relationship w ith Asian monsoon history[J].Quaternary Science Review s,2008,27:351-364.
[50]Guo Xiaoyin,Chen Fahu,Xie Yaowen,et al.A study on modeling the terminal lake of Shiyang River Drainage Basin under the natural conditions[J].Journal of Natural Resources,1999,14(4):94-97.[郭晓寅,陈发虎,颉耀文,等.自然条件下石羊河终闾湖泊模拟研究[J].自然资源学报,1999,14(4):94-97.]
[51]Zhao Qiang.Environmental change of Shiyang River drainage basin since the Last Deglaciation[D].Lanzhou:Lanzhou University,2005.[赵强.石羊河流域末次冰消期以来环境变化研究[D].兰州:兰州大学,2005.]
[52]Wei Wei,Shi Peiji,Yang Wangming,et al.Spatial distribution of land surface temperature in Shiyang River basin based on M ODIS data[J].Journal of Glaciology and Geocryology,2013,35(1):57-64.[魏伟,石培基,杨旺明,等.基于MODIS数据的石羊河流域地表温度空间格局[J].冰川冻土,2013,35(1):57-64.]
[53]Chen Longhen,Qu Yaoguang.Water and soil resources and its exploitation and utilization in Hexi area[M].Beijing:Science Press,1992:6-46.[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.]
[54]Zhang Kecun,Qu Jianjun,Ma Zhonghua.Environmental characteristics of sandstorm in M inqin county in recent 50 years[J].Journal of Desert Research,2004,24(3):257-260.[张克存,屈建军,马中华.近50 a来民勤沙尘暴的环境特征[J].中国沙漠,2004,24(3):257-260.]
[55]Long Hao,Wang Nai'ang,Ma Haizhou,et al.Eolian activity and environment evolution history recorded by the Qingtu Lake,NW Tengger Desert[J].Acta Sedimentologica Sinica,2007,25(4):626-631.[隆浩,王乃昂,马海州,等.腾格里沙漠西北缘湖泊沉积记录的区域风沙特征[J].沉积学报,2007,25(4):626-631.]
[56]Zhao Q,Wang N A,Li X M.Lacustrine strata sedimentology and lake-level history in ancient Zhuyeze Lake since the Last Deglaciation[J].Frontiers of Earth Science in China,2008,2(2):199-208.
[57]Long H,Lai Z P,Wang N A,et al.Holocene climate variations from Zhuyeze terminal lake records in East Asian monsoon margin in arid northern China[J].Quaternary Research,2010,74(1):46-56.
[58]Li Y,Wang N A,Li Z L,et al.Reworking effects in the Holocene Zhuye Lake sediments:A case study by pollen concentrates AM S14C dating[J].Science China:Earth Sciences,2012,55(10):1669-1678.
[59]Long Hao.Mid-Holocene climate variation from lake evidences of east Asian monsoon margin areas[D].Lanzhou:Lanzhou University,2006.[隆浩.季风边缘区全新世中期气候变化的古湖泊记录[D].兰州:兰州大学,2006.]
[60]Pye K.Aeolian dust and dust deposits[M].London:Academic Press,1987:29-62.
[61]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(3/4):263-277.
[62]Ren Mingda,Wang Nailiang.Introduction to the modern sedimentary environment[M].Beijing:Science Press,1985:1-4.[任明达,王乃梁.现代沉积环境概论[M].北京:科学出版社,1985:1-4.]
[63]Zhao Qiang,Wang Nai'ang,Cheng Hongyi,et al.Grain-size characteristics of Qingtu lake sediments and its paleaoenvironment explanation[J].Arid Land Geography,2003,26(1):2-6.[赵强,王乃昂,程弘毅,等.青土湖沉积物粒度特征及其古环境意义[J].干旱区地理,2003,26(1):2-6.]
[64]Sun Donghuai,An Zhisheng,Su Ruixia,et al.Grain size numerical partitioning of the sedimentary components and its applications[J].Progress in Natural Science,2001,11(3):269-276.[孙东怀,安芷生,苏瑞侠,等.古环境中沉积物粒度组分分离的数学方法及其应用[J].自然科学进展,2001,11(3):269-276.]
[65]Sun Donghuai,Lu Huayu,Rea D,et al.Bimode grain-size distribution of Chinese loess and its paleoclimate implication[J].Acta Sedimentologica Sinica,2000,18(3):327-335.[孙东怀,鹿化煜,Rea D,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.]
[66]Campell C.Late Holocene lake sedimentology and climate change in southern Alberta,Canada[J].Quaternary Research,1997,49(1):96-101.
[67]Chen Jing'an,Wan Guojiang,Zhang D D,et al.Environmental records of lacustrine sediments in different time scales:Sediment grain size as an example[J].Science in China(Series D),2004,47(10):954-960.[陈敬安,万国江,张峰,等.不同时间尺度下的湖泊沉积物环境纪录:以沉积物粒度为例[J].中国科学(D辑),2003,33(6):563-568.]
[68]Wang Junbo,Zhu Liping.Grain-size characteristics and their paleo-environmental significance of Chen Co Lake sediments in southern Tibet[J].Progress in Geography,2002,21(5):459-467.[王君波,朱立平.藏南沉错沉积物的粒度特征及其古环境意义[J].地理科学进展,2002,21(5):459-467.]
[69]Sun Qianli,Zhou Jie,Xiao Jule.Grain-size characteristics of lake Daihai sediments and its palaeoenvironment significance[J].M arin Geology&Quaternary Geology,2001,21(1):93-95.[孙千里,周杰,肖举乐.岱海沉积物粒度特征及其古环境意义[J].海洋地质与第四纪地质,2001,21(1):93-95.]
[70]Sun Yongchuan,Li Huisheng.The sedimentary facies and sedimentary environment of clastic rocks[M].Beijing:Geological Publishing House,1986:65-81.[孙永传,李惠生.碎屑岩沉积相和沉积环境[M].北京:地质出版社,1986:65-81.]
[71]Chen Fahu,Wu Wei,Holmes J A,et al.A mid-Holocene drought interval as evidenced by lake desiccation in the Alashan Plateau,Inner M ongolia,China[J].Chinese Science Bulletin,2003,48(14):1401-1410.
[72]Zhang Liang,Zhang Qiang,Feng Jianying,et al.A study of atmospheric w ater cycle over the Qilian M ountains(I):Variation of annual w ater vapor transport[J].Journal of Glaciology and Geocryology,2014,36(5):1079-1091.[张良,张强,冯建英,等.祁连山地区大气水循环研究(I):空中水汽输送年际变化分析[J].冰川冻土,2014,36(5):1079-1091.]
[73]Zhang Xiao'e,Shen Zhibao,Zhang Guangyu,et al.Remote mineral aerosols in Westeries and their contributions to the Chinese loess[J].Science in China(Series D),1996,39(2):134-143.
[74]Li Enju.A comparative study of sediments characteristics between the Badain Jaran Desert and Tengger Desert[D].Xi'an:Shaanxi Normal University,2001.[李恩菊.巴丹吉林沙漠与腾格里沙漠沉积物特征的对比研究[D].西安:陕西师范大学,2001.]
[75]Li Zhuolun,Wang Nai'ang,Li Yu,et al.The salinity change and its environmental significance in Huahai Lake,Heixi Corridor,Northw est China during the early-middle Holocene[J].Journal of Glaciology and Geocryology,2013,35(6):1481-1489.[李卓仑,王乃昂,李育,等.河西走廊花海古湖泊早、中全新世湖水盐度变化及其环境意义[J].冰川冻土,2013,35(6):1481-1489.]