西北干旱区湖泊碳同位素与环境变化
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摘要
湖泊沉积的碳同位素组成因可记录地质历史时期C_3/C_4植被等环境变化信息,被广泛用于陆地生态系统和全球环境变化研究,在中国西北干旱区湖泊古环境研究中也广为应用.近年来,进一步深入研究的成果,为湖泊碳同位素地球化学所反映的环境意义注入了新的信息,使得我们需要从多方面考虑湖泊碳同位素在环境变化示踪研究中的解释.文章总结了过去几十年来西北干旱区湖泊碳同位素的研究结果,讨论可能存在的湖泊沉积物碳同位素变化机制问题,为更好地将碳同位素地球化学应用于湖泊环境变化研究提供参考.
引文
陈敬安,万国江,汪福顺,黄荣贵,张峰,Zhang D D,Schmidt R.2002.湖泊现代沉积物碳环境记录研究.中国科学D辑:地球科学,32:73-80
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谢树成,梁斌,郭建秋,易轶,Evershed R P,Maddy D,Chambers F M.2003.生物标志化合物与相关的全球变化.第四纪研究,23:521-528
张成君,陈发虎,尚华明,曹洁.2004.中国西北干旱区湖泊沉积物中有机质碳同位素组成的环境意义——以民勤盆地三角城古湖泊为例.第四纪研究,24:88-94
张恩楼,沈吉,夏威岚,朱育新,王苏民.2002.青海湖沉积物有机碳及其同位素的气候环境信息.海洋地质与第四纪地质,22:105-108
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Aichner B,Feakins S J,Lee J E,Herzschuh U,Liu X.2015.Highresolution leaf wax carbon and hydrogen isotopic record of the late Holocene paleoclimate in arid Central Asia.Clim Past,11:619-633
Aichner B,Herzschuh U,Wilkes H,Vieth A,B?hner J.2010b.δDvalues of n-alkanes in Tibetan lake sediments and aquatic macrophytes-A surface sediment study and application to a 16ka record from Lake Koucha.Org Geochem,41:779-790
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An Z,Colman S M,Zhou W,Li X,Brown E T,Jull A J T,Cai Y,Huang Y,Lu X,Chang H,Song Y,Sun Y,Xu H,Liu W,Jin Z,Liu X,Cheng P,Liu Y,Ai L,Li X,Liu X,Yan L,Shi Z,Wang X,Wu F,Qiang X,Dong J,Lu F,Xu X.2012.Interplay between the Westerlies and Asian monsoon recorded in Lake Qinghai sediments since 32 ka.Sci Rep,2:619
Casta?eda I S,Schouten S.2011.A review of molecular organic proxies for examining modern and ancient lacustrine environments.Quat Sci Rev,30:2851-2891
Casta?eda I S,Werne J P,Johnsona T C.2009.Influence of climate change on algal community structure and primary productivity of Lake Malawi(East Africa)from the Last Glacial Maximum to present.Limnol Oceanogr,54:2431-2447
Chen C T A,Lan H C,Lou J Y,Chen Y C.2003.The dry Holocene megathermal in Inner Mongolia.Palaeogeogr Palaeoclimatol Palaeoecol,193:181-200
Chikaraishi Y,Naraoka H.2003.Compound-specificδD-δ13C analyses of n-alkanes extracted from terrestrial and aquatic plants.Phytochemistry,63:361-371
Chu G,Sun Q,Xie M,Lin Y,Shang W,Zhu Q,Shan Y,Xu D,Rioual P,Wang L,Liu J.2014.Holocene cyclic climatic variations and the role of the Pacific Ocean as recorded in varved sediments from northeastern China.Quat Sci Rev,102:85-95
Cranwell P A,Eglinton G,Robinson N.1987.Lipids of aquatic organisms as potential contributors to lacustrine sediments-II.Org Geochem,11:513-527
Doberschütz S,Frenzel P,Haberzettl T,Kasper T,Wang J,Zhu L,Daut G,Schwalb A,M?usbacher R.2014.Monsoonal forcing of Holocene paleoenvironmental change on the central Tibetan Plateau inferred using a sediment record from Lake Nam Co(Xizang,China).J Paleolimnol,51:253-266
Duan Y,Wu Y,Cao X,Zhao Y,Ma L.2014.Hydrogen isotope ratios of individual n-alkanes in plants from Gannan Gahai Lake(China)and surrounding area.Org Geochem,77:96-105
Duan Y,Xu L.2012.Distributions of n-alkanes and their hydrogen isotopic composition in plants from Lake Qinghai(China)and the surrounding area.Appl Geochem,27:806-814
Eglinton G,Calvin M.1967.Chemical fossils.Sci Am,216:32-43
Eglinton G,Hamilton R J.1967.Leaf epicuticular waxes.Science,156:1322-1335
Eglinton T I,Eglinton G.2008.Molecular proxies for paleoclimatology.Earth Planet Sci Lett,275:1-16
Fang J,Wu F,Xiong Y,Li F,Du X,An D,Wang L.2014.Source characterization of sedimentary organic matter using molecular and stable carbon isotopic composition of n-alkanes and fatty acids in sediment core from Lake Dianchi,China.Sci Total Environ,473-474:410-421
Ficken K J,Li B,Swain D L,Eglinton G.2000.An n-alkane proxy for the sedimentary input of submerged/floating freshwater aquatic macrophytes.Org Geochem,31:745-749
Filley T R,Freeman K H,Bianchi T S,Baskaran M,Colarusso L A,Hatcher P G.2001.An isotopic biogeochemical assessment of shifts in organic matter input to Holocene sediments from Mud Lake,Florida.Org Geochem,32:1153-1167
Finlay J C,Kendall C.2007.Stable isotope tracing of temporal and spatial variability in organic matter sources to freshwater ecosystems.In:Michener R,Lajtha K,eds.Stable Isotopes in Ecology and Environmental Science.2nd ed.Oxford:Blackwell Publishing.283-333
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