| [1] Ｗang Pinxian.Paleoceanography[J].Advances in Earth Science,1994,9(4):94-96.［汪品先.古海洋学[J].地球科学进展,1994,9(４):94-96.］
[2] Jian Zhimin.ODP and global change (II)―Studying quaternary past global change from the view of sea[J].Advances in Earth Science,1995,10(3):267-272.[翦知湣.大洋钻探与全球变化（二）——从海洋角度研究第四纪古全球变化[J].地球科学进展,1995,10(3):267-272.]
[3] Jian Zhimin,Huang Wei.Rapid climate change and high resolution deep-sea sedimentary records[J].Advances in Earth Science,2003,18(5):673-680.[翦知湣,黄维.快速气候变化与高分辨率的深海沉积记录[J].地球科学进展,2003,18(5):673-680.]
[4] Bond G,Showers W,Cheseby M,et al.A pervasive milliannial-scale cycle in North Atlantic Holocene and Glacial climate[J].Science,1997,278:1 257-1 266.
[5] Porter S C,An Z S.Correlation between climate events in the North Atlantic and China during the last glaciation[J].Nature,1995,375:305-308.
[6] Yao Tandong,Shi Yafeng,Qin Dahe,et al.A research of climate change inferred from Guliya ice core since the last interglobal stage[J].Science in China(D),1997,27(5):447-452.[姚檀栋,施雅风,秦大河,等.古里雅冰芯中末次间冰期以来的气候变化纪录研究[J].中国科学D辑,1997,27(5):447-452.]
[7] O’Brien S R,Mayewski P A,Meeker L D,et al.Complexity of Holocene climate as reconstructed from a Greenland ice core[J].Science,1995,270:1 962-1 964.
[8] GRIP members.Climate instability during the last interglacial period recorded in the GRIP ice core[J].Nature,1993,364:203-207.
[9] Xie Shucheng,Liang Bin,Guo Jianqiu,et al.Biomarkers and the related global change[J].Quaternary Science,2003,23(5):521-528.[谢树成,梁斌,郭建秋,等.生物标志化合物与相关的全球变化[J].第四纪研究,2003,23(5):521-528.]
[10] Lu Yuehan,Sun Yongge,Weng Huanxin.Lacustrine sediments as a record of changes of regional climate and environment[J].Geochimica,2004,33(1):20-28.[卢粤晗,孙永革,翁焕新.湖泊沉积有机质的地球化学纪录与古气候环境重建[J].地球化学,2004,33(1):20-28.]
[11] Chen Jianfang.New geochemical proxies in paleoceanography studies[J].Advances in Earth Science,2002,17(3):402-410.[陈建芳.古海洋研究中的地球化学新指标[J].地球科学进展,2002,17(3):402-410.]
[12] Meng Xianwei,Du Dewen,Liu Zhenxia, et al.Molecular biomarker records of paleoceanphraphic environment change in the East Sea for the last 35,000 years[J].Science in China(D),2001,31(8):691-696.[孟宪伟,杜德文,刘振夏,等.东海近3.5万年来古海洋环境变化的分子生物标志物纪录[J].中国科学D辑,2001,31(8):691-696.]
[13] Lu Bing,Chen Ronghua,Wang Zipan,et al.Ocean environment change in the Bering Sea over the past 100 years—Evidences from the molecular fossil[J].Science in China(D),2004,34(4):367-374.[卢冰,陈荣华,王自磐,等.亚北极白令海近百年海洋环境变化——来自分子化石的证据[J].中国科学D辑,2004,34(4):367-374.]
[14] Villanueva J,Grimalt J O,Cortijo E,et al.A biomarker approach to the organic matter deposited in the North Atlantic during the last climatic cycle[J].Geochimica et Cosmochimica Acta,1997,61(21):4 633-4 646.
[15] Schefub E,Versteegh G J M,Jansen J H F,et al.Lipid biomarkers as major source and preservation indicators in SE Atlantic surface sediments[J].Deep Sea Research,2004,51(9):1 199-1 228.
[16] Muri G,Wakeham S G,Pease T K,et al.Evaluation of lipid biomarkers as indicators of changes in organic matter delivery to sediments from Lake Planina,a remote mountain lake in NW Slovenia[J].Organic Geochemistry,2004,35(10):1 083-1 093.
[17] Zhang Zhaohui,Zhao Meixun,Yang Xiangdong,et al.A hydrocarbon biomarker record for the last 40 kyr of plant input to Lake Heqing,southwestern China[J].Organic Geochemistry,2004,35(5):595-613.
[18] Xie Shucheng,Chen Fahu,Wang Zhiyuan,et al.Lipid distributions in loess-paleosol sequences from northwest China[J].Organic Geochemistry,2003,34(8):1 071-1 079.
[19] Duan Yi.Compositional features of lipid compounds in sediments from Gannan Marsh,China[J].Geochemica,2002,31(6):525-531.[段毅.甘南沼泽沉积脂类生物标志物化合物的组成特征[J].地球化学,2002,31(6):525-531.]
[20] Pancost R D,Baas M,Geel B V,et al.Biomarkers as proxies for plant inputs to peats:An example from a sub-boreal ombrotropic bog[J].Organic Geochemistry,2002,33(7):675-690.
[21] Hayes J M, Preeman K H,Popp B N,et al.Compound-specific isotopic analyses:A novel tool for reconstruction of ancient biogeochemical process[J].Advances in Organic Geochemsity,1989,16:1 115-1 128.
[22] Hayes J M.Factors controlling C13 contents of sedimentary organic compounds:principles and evidence[J].Marine Geology,1993,113(1):111-125.
[23] Zhou Yunlong.Plant Bioology[M].Beijing: Higher Education Press, 1999.198-201.[周云龙.植物生物学[M].北京:高等教育出版社,1999.198-201.]
[24] Wang Guoan.Application of stable carbon isotope for paleoenvironmental research [J].Quaternaty Sciences,2003,23(5):471-484.[王国安.稳定同位素在第四纪古环境研究中的应用[J].第四纪研究,2003,23(5):471-484.]
[25] Niu Shuli,Jiang Gaoming,Li Yonggeng.Environmental regulations of C3 and C4 plants[J].Ａcta Ecologica Sinica,2004,24(2):308-314.[牛书丽,蒋高明,李永庚.C3和C4植物的环境调控[J].生物学报,2004,24(2):308-314.]
[26] Pancost R D, Boot C S. The papaeoclimatic utility of terrestrial biomarkers in marine sediments[J]. Marine Chemistry, 2004,92:239-261.
[27] Huang Y S,Street-Perrott F A,Perrott R A,et al.Glacial-interglacial environmental changes inferred from molecular and compounds-specific δ13C analyses of sediments from Scared Lake,Mt. Kenya[J].Geochimica et Cosmochimica Acta,1999,63(9):1 383-1 404.
[28] Cerling T E,Harris J M,Bruce J,et al.Global vegetation change through the Miocene/Pliocene boundary[J].Nature,1997,389:153-158.
[29] Pagani M,Freeman K H,Arthur M A.Late Miocene atmospheric CO2 concentrations and the expansion of C4 grasses[J].Science,1999,285:876-879.[30] Huang Y S,Street-Perrott F A,Metcalfe S E,et al.Climate change as the dominant contral on glacial-interglacial variations in C3 and C4 plant abundance[J].Science,2001,293:1 647-1 651.
[31] Neunlist S, Rodier C, Liopiz P. Isotopic biogeochemistry of the lipids in recent sediments of Lake Bled(Slovenia) and Baldeggersee(Switzerland)[J]. Organic Geochmistry, 2002, 33:1 183-1 195.
[32] Bird I M,Summmons R E,Gagan M K,et al.Terrestrial vegetation change inferred from n-alkance δ13C analyses in the marine environment[J].Geochimica et Cosmochimica Acta,1995,59(13):2 853-2 857.
[33] Hu J F,Peng P A,Jia G D,et al.Biological markers and their carbon isotopes as an approach to the paleoenvironmental reconstruction of Nansha area, South China Sea during the last 30 ka[J].Organic Geochemistry,2002,33(10):1 197-1 204.
[34] Freeman K H,Colarusso L A.Molecular and isotopic records of C4 grassland expansion in the late Miocene[J].Geochimica et Cosmochimica Acta,2001,65(9):1 439-1 454.
[35] Zhao Meixun,Eglinton G,Simon K,et al.Marine and terrestrial biomarker records for the last 35,000 years at ODP site 658C off NW Africa[J].Organic Geochemistry,2000,31(9):919-930.
[36] Huang Y S,Dupont L,Sarnthein M,et al.Mapping of C4 plant input from North West Africa into North East Atlantic sediment[J].Geochimica et Cosmochimica Acta,2000,64(20):3 505-3 513.
[37] Hughen K A, Eglinton T L, Xu L, et al. Abrupt tropical vegetation response to rapid climate changes[J]. Science, 2004, 304:1 955-1 958.
[38] Bird M I,Giresse P,Chivas A R.The effect of savanna vegetation on the carbon-isotope composition of sediment from the Sanga river,Cameroon[J].Limnol Oceanogr,1994,43(1):143-146.
[39] Bird M I,Giresse P,Ngos S.A seasonal cycle in the carbon-isotope composition of organic carbon in the Sanaga river,Cameroon[J].Limnology and Oceanography,1998,43(1):143-146.
[40] Gordon E S, Goni M A. Sources and distribution of terrigenous organic matter delivered by the Atchafalaya River to sediments in the northern Gulf of Mexico[J]. Geochimica et Cosmochimica Acta, 2003,67 (13): 2 359-2 375.
[41] Hooghiemstra H.Changes of major wind belts and vegetation zones in NW Africa 20,000-5,000 yr BP. as deduced from a marine pollen record near Cap Blanc[J].Review of Palaeobotany and palynology,1988,55(2):101-140.
[42] Jasper J P, Hayes J M.Reconstruction of paleoceanic pCO2 levels from the carbon isotopic compositions of sedimentary biogenic components[A]. In: Carbon Cycling in the Glacial Ocean: Constraints on the Ocean`s Role in Global change[C].NATO ASI Series,1994,17(2):323-341.
[43] Meng Xianwei,Du Dewen,Han Yibing.Long chain Alkenones and its carbon isotope:A new tool for assessment of abrupt climatic change during Quaternary[J].Journal of Oceanography of Huanghai & Bohai Seas,2000,18(1):66-73.[孟宪伟,杜德文,韩贻兵.第四纪气候突变研究的新工具长链不饱和酮及其碳同位素[J].黄渤海海洋,2000,18(1):66-73.]
[44] Marlowe I T,Brassell S C,Eglinton G,et al.Long chain unsaturated ketones and esters in living algae and marine sediment[J].Organic Geochemistry,1984,6:135-141.
[45] Burkhardt S,Riebesell U,Zondervan I.Effects of growth rate, CO2 concentration, and sell size on the stable carbon isotope fractionation in marine phytoplankton[J].Geochimica et Cosmochimica Acta,1999,63(22):3 729-3 741.
[46] Schoell M,Schouten S,Sinninghe D J S,et al.A molecular organic carbon record of Miocene climate[J].Science,1994,263:1 122-1 125.
[47] Duan Yi,Wang Zhiping.Isotopic composition and probable organic resource of long-chain individual alkanes from the Nansha Sea[J].Science Bulletion,2001,46:2 003-2 006.[段毅,王智平.南沙海洋沉积单体长链正构烷烃成因的碳同位素证据[J].科学通报,2001,46:2 003-2 006.]
[48] Amo M,Minagawa M.Sedimentary record of marine and terrigenous organic matter delivery to the Shatsky Rise, western North Pacific, over the last 130 kyr[J].Organic Geochemistry,2003,34(9):1 299-1 312.
[49] Mark P,Freeman K H,Arthur M A.Isotope analyses of molecular and total organic carbon from Miocene sediments[J].Geochimica et Cosmochimica Acta,2000,64(1):37-49.
[50] Duan Yi,Song Jinming,Zhang Hui.A study of biologic individual lipid carbon isotopic composition in the Nansha Sea[J].Science in China(D),2003,33:889-894.[段毅,宋金明,张辉.南沙海区生物单体脂类碳同位素研究[J].中国科学D辑,2003,33:889-894.]
[51] Li Hui,Wang Shengzhong,Leng Xuetian.Progresses in organic geochemical researches on lipids of mires[J].Wetland Science,2004,2(1):172-178.[李辉,王升忠,冷雪天.泥炭沼泽有机地球化学研究进展[J].湿地科学,2004,2(1):172-178.]
[52] Ficken K J,Barber K E,Eglinton G.Lipid biomarker, δ13C and plant macrofossil stratigraphy of a Soottish montane peat bog over the last two millennia[J].Organic Geochemistry,1998,28(3):217-237.
[53] Nott C J,Xie S,Avsejs L A,et al.N-alkane distributions in ombrotropic mire as indicators of vegetation change related to climatic variation[J].Organic Geochmistry,2000,31(3):231-235.
[54] White J W C,Clais P,Figge R A,et al.A high resolution record of atmospheric CO2 content from carbon isotopes in peat[J].Nature,1994,367:153-156.[55] Xie Shucheng,Yi Yi,Liang Bin,et al.Paleoclimate implication from compound specific δ13C and δD of molecular fossils in peat deposits[J].Bulletin of Mineralogy,Petrology and Geochemistry,2003,22(1):8-13.[谢树成,易轶,梁斌, 等.泥炭分子化石单体碳氢同位素的古气候意义[J].矿物岩石地球化学通报,2003,22(1):8-13.]
[56] Schse D, Gleixner G. Hydrogen isotope ratios of recent lacustrine sedimentary n-alkanes record modern climate variability [J]. Geochimica et Cosmochimica Acta, 2004, 68(23): 4 877-4 889. |