[1] Fallon S J, White J C, McCulloch M T. Porites corals as recorders of mining and environmental impacts: Misima Island, Papua New Guinea[J]. Geochimia et Cosmochimica Acta, 2002,66(1):45-62.
[2] Cobb K M, Charles C D, Cheng Hai, et al. U/Th-dating living and young fossil corals from the central tropical Pacific[J]. Earth and Planetary Science Letters,2003,210(1/2):91-103.
[3] Kilbourne K H,Quinn T M,Taylor F W. A fossil coral perspective on western tropical Pacific climate/350ka[J]. Paleoceanography, 2004,19 (1), doi:10.1029/2003PA000944.
[4] Weber J N. Incorporation of strontium into reef coral skeletal carbonate[J]. Geochimica et Cosmochimica Acta,1973,37:2 173-2 190.
[5] Fallon S J, McCulloch M T, Alibert C.Examining water temperature proxies in Porites corals from the Great Barrier Reef: A cross-shelf comparison[J]. Coral Reefs,2003,22(8):389-404
[6] Broecker W S, Peng T H. Tracers in the Sea[M]. New York:Lamont-Doherty Geological Observatory,Columbia University, 1982.
[7] Mitsuguchi T, Matsumoto E, Abe O, et al. Mg/Ca thermometry in coral skeletons[J]. Science, 1996, 274(5 289):961-963.
[8] Min G R, Edwards R L, Taylor F W, et al. Annual cycles of U/Ca in coral skeletons and U/Ca thermometry[J]. Geochimica et Cosmochimica Acta,1995, 59(10):2 025-2 042.
[9] Amiel A J, Friedman G M, Miller D S. Distribution and nature of incorporation of trace elements in modern aragonitic corals[J]. Sedimentology,1973,20:47-64.
[10] Walls R A, Ragland P C, Crisp E L. Experimental and natural early diagenetic mobility of Sr and Mg in biogenic carbonates[J]. Geochimica et Cosmochimica Acta,1997,41:1 731-1 737.
[11] Kinsman D J J, Holland H D.The co-precipitation of cations with CaCO3. IV. The co-precipitation of Sr2+ with aragonite between 16 and 96℃[J]. Geochimica et Cosmochimica Acta,1969,33:1-17.
[12] Swart P K. The strontium, magnesium and sodium composition of recent scleractinian coral skeletons as standards for palaeoenvironmental analysis[J]. Palaeogeogr Palaeoclimatol Palaeoecol,1981,34:115-136.
[13] Swart P K, Hubbard J A E B.Uranium in scleractinian coral skeletons[J]. Coral Reefs,1982,1:13-19.
[14] Beck J W, Edwards R L, Ito E, et al. Sea-surface temperature from coral skeletal strontium/calcium ratios[J]. Science,1992, 257:644-647.
[15] Wei Gangjian, Sun Min, Li Xianhua, et al. Mg/Ca, Sr/Ca and U/Ca ratios of a porites coral from Sanya Bay, Hainan Island, South China Sea and their relationships to sea surface temperature[J]. Palaeo,2000,162(1/2):59-74.
[16] Schrag D P. Rapid analysis of high-precision Sr/Ca ratios in corals and other marine carbonates[J]. Paleoceanography,1999,14(2):97-102.
[17] Tudhope A W, Chilcott C P, McCulloch M T, et al. Variability in the El Niño Southern Oscillation through a glacial-interglacial Cycle [J]. Science, 2001,291(5 508):1 511-1 517.
[18] Cobb K M, Charles C D, Cheng H, et al. El Niño/Southern Oscillation and tropical Pacific climate during the last millennium [J]. Nature, 2003, 424(6 946): 271-276.
[19] McCulloch M T, Gagan M K, Mortimer G E, et al. A high-resolution Sr/Ca and δ18O coral record from the Great Barrier Reef, Australia, and the 1982-1983 El Niño [J]. Geochimica et Cosmochimica Acta,1994, 58:2 747-2 754.
[20] Ren L, Linsley B K, Wellington G M, et al. Deconvolving the 18O seawater component from subseasonal coral δ18O and Sr/Ca at Rarotonga in the southwestern subtropical Pacific for the period 1726 to 1997[J]. Geochimica et Cosmochimica Acta,2003,67(9):1 609-1 621.
[21] Druffel E M. Pulses of rapid ventilation in the north Atlantic surface ocean during past century[J]. Science,1997,275(5 305):1 454-1 457.
[22] Guilderson T P, Schrag D P. Abrupt shift in subsurface temperatures in the tropical pacific associated with changes in El Niño[J]. Science,1998,281(5 374):240-243.
[23] H nisch B,Hemming N G,Grottoli A G,et al. Assessing scleractinian corals as recorders for paleo-pH: Empirical calibration and vital effects[J]. Geochimica et Cosmochimica Acta,2004, 68(18):3 675-3 685.
[24] Liu Weiguo, Peng Zicheng, Xiao Yingkai, et al. Boron isotopic composition of corals from South China Sea and their environmental significance[J]. Geochimica,1999,28(6):534-541. [刘卫国,彭子成,肖应凯,等.南海珊瑚礁硼同位素组成及其环境意义[J].地球化学,1999,28(6):534-541.]
[25] Wyndham T, McMulloch M, Fallon S, et al. High-resolution coral records of rare Earth elements in coastal seawater:Biogeochemical cycling and a new environmental proxy[J]. Geochimica et Cosmochimica Acta,2004,68(9):2 067-2 080.
[26] Akagi T, Hashimoto Y, F-F Fu, et al. Variation of the distribution coefficients of rare earth elements in modern coral-lattices:Species and site dependencies[J].Geochimica et Cosmochimica Acta,2004,68(10):2 265-2 273.
[27] David C P. Heavy metal concentrations in growth bands of corals: A record of mine tailings input through time (Marinduque Island, Philippines)[J]. Marine Pollution Bulletin,2003, 46 (2) :187-196.
[28] Peng Zicheng, He Xuexian, Zhang Zhaofeng, et al. Correlation of coral fluorescence with nearshore rainfall and runoff in Hainan Island, South China Sea[J]. Progress in Natural Science, 2002,12(1):41-44.
[29] Nie Baofu, Chen Tegu, Liang Meitao, et al. The Relationship Between Reef Coral and Environmental Changes of Nansha Islands and Adjacent Regions[M].Beijing:Science Press,1997:53.[聂宝符,陈特固,梁美桃,等.南沙群岛及其邻近礁区造礁珊瑚与环境变化的关系[M].北京:科学出版社,1997:53.]
[30] Yu Kefu, Zhao Jianxin, Liu Tungsheng, et al. High-frequency winter cooling and reef coral mortality during the Holocene climatic optimum[J]. Earth and Planetary Science Letters,2004,224(1/2):143-155.
[31] Bagnato S, Linsley B K, Howe S S. Evaluating the use of the massive coral Diploastrea heliopora for paleoclimate reconstruction[J]. Paleoceanography,2004,19(1), doi:PA1032.10.1029/2003PA000935.
[32] Sarnthein M, Kennett J P, Allen J R M, et al. Decadal-to-millennial-scale climate variability-chronology and mechanisms: Summary and recommendations[J].Quaternary Science Reviews,2002,21:1 121-1 128.
[33] Linsley B K, Wellington G M, Schrag D P. Decadal sea surface temperature variability in the subtropical south pacific from 1726 to 1997 A.D[J].Science, 2000, 290(5 494):1 145-1 148.
[34] Felis T, Lohmann G, Kuhnert H, et al. Increased seasonality in Middle East temperatures during the last interglacial period[J]. Nature,2004,429(6 988):164-168.
[35] Schrag D P, Linsley B. Corals, chemistry, and climate [J]. Science,2002, 296(5 566):277-278.
[36] de Villiers S D, Nelson B K, Chivas A R. Biological controls on coral Sr/Ca and δ18O recnstructions of sea surface temperature[J]. Science,1995,269:1 247-1 249.
[37] Mitsuguchi T, Matsumoto E, Uchida T. Mg/Ca and Sr/Ca ratios of Porites coral skeleton: Evaluation of the effect of skeletal growth rate[J].Coral Reefs,2003,22(8):381-388.
[38] Weber J N. Incorporation of strontium into reef coral skeletal carbonate[J]. Geochimica et Cosmochimica Acta, 1973, 37:2 173-2 190.
[39] Smith S V, Buddemeier R W, Redalje R C, et al. Strontium-calcium thermometry in coral skeletons[J]. Science, 1979,204:404-407.
[40] Marshall J F, McMulloch M T. An assessment of the Sr/Ca ratio in shallow water hermatypic corals as a proxy for sea surface temperature[J]. Geochimica et Cosmochimica Acta, 2002, 66(18):3 263-3 280.
[41] Cohen A L, Owens K E, Layne G D, et al. The effect of algal symbionts on the accuracy of Sr/Ca paleotemperatures from coral[J].Science,2002,296(5 566):331-333.
[42] de Villiers S D. Seawater strontium and Sr/Ca variability in the Atlantic and Pacific oceans [J]. Earth and Planetary Science Letters, 1999,171(4):623-634.
[43] Grottoli A G. Effect of light and brine shrimp on skeletal δ13C in the Hawaiian coral Porites compressa: A tank experiment[J]. Geochimica et Cosmochimica Acta,2002,66(11):1 955-1 967.
[44] Hendy E J, Gagan M K, Alibert C, et al. Abrupt decrease in tropical sea surface salinity at end of Little Ice Age[J]. Science,2002,295(5 559):1 511-1 514.
[45] Watanabe T, Winter A, Oba T. Seasonal changes in sea surface temperature and salinity during the Little Ice Age in the Caribbean Sea deduced from Mg/Ca and 18O/16O ratios in corals[J]. Marine Geology,2001,173(1/4):21-35.
[46] Gagan M K, Ayliffe L K, Hopley D, et al. Temperature and surface-ocean water balance of the mid-Holocene tropical western pacific [J]. Science,1998, 279(5 343):1 014-1 018.
[47] Stoll H M, Schrag D P. Effects of Quaternary sea level cycles on strontium in seawater[J]. Geochim et Cosmochim Acta,1998,62(7):1 107-1 118.
[48] McCulloch M T, Tudhope A W, Esat T M, et al. Coral record of equatorial sea-surface temperatures during the Penultimate Deglaciation at Huon Peninsula[J]. Science, 1999,283(5 399):202-222.
[49] Clement A C, Seager R, Cane M A. Suppression of El Niño during the mid-Holocene by changes in the Earth’s orbit[J].Paleoceanography,2000,15(6): 731-737.
[50] Rittenour T M,Brigham-Grette J,Mann M E. El Niño-Like climate teleconnections in New England during the Late Pleistocene[J].Science,2000,288(5 468):1 039-1 042.
[51] Zebiak E, Cane M A. A model El Niño /Southern Oscillation[J]. Monthly Weather Review, 1987, 115:2 262-2 278.
[52] Cane M A. The evolution of El Niño, past and future[J]. Earth and Planetary Science Letters, 2005, 230(3/4):227-240.
[53] Torrence C, Webster P. Interdecadal changes in the ENSO-monsoon system[J]. Journal Climate,1999,12(8):2 679-2 690.
[54] Charles C D, Hunter D E, Fairbanks R G. Interaction between the ENSO and the Asian monsoon in a coral record of tropical climate [J]. Science, 1997,277(5 328):925-928.
[55] Cole J E, Dunbar R B, McClanahan T R, et al. Tropical pacific forcing of decadal SST variability in the western Indian ocean over the past two centuries[J]. Science, 2000,287(5 453): 617-619.
[56] Charles C D, Cobb K, Moore M D, et al. Monsoon-tropical ocean interaction in a network of coral records spanning the 20th century[J]. Marine Geology,2003,201(1/3):207-222.
[57] Evans M N, Fairbanks R G, Rubenstone J L. The thermal oceanographic signal of El Niño reconstructed from a Kiritimati Island coral[J]. Journal of Geophysical Research, 1999,104(C6):13 409-13 421.
[58] Urban F E, Cole J E, Overpeck J T. Influence of mean climate change on climate variability from a 155-year tropical Pacific coral record[J]. Nature, 2000,407(6 781): 989-993.
[59] Pfeiffer M, Dullo W-C, Eisenhauer A. Variability of the Intertropical Convergence Zone recorded in coral isotopic records from the central Indian Ocean (Chagos Archipelago)[J]. Quaternary Research 2004,61(3):245-255.
[60] Kumar K K, Rajagopalan B, Cane M A. On the weakening relationship between the Indian Monsoon and ENSO[J]. Science,1999,284(5 423):2 156-2 159.
[61] Wang B, An S-I. Why the properties of El Niño changed during the late 1970s[J]. Geophysical Research Letters, 2001,28(19):3 709- 3 712.
[62] Guilderson T P, Schrag D P. Abrupt shift in subsurface temperatures in the tropical pacific associated with changes in El Niño[J]. Science, 1998,281(5 374):240-243.
[63] Peng Zicheng, Chen Tegu, Nie Baofu,et al. Coral δ18O records as an indictor of winter monsoon intensity in the South China Sea[J]. Quaternary Research,2003,59(3):285-292.
[64] Watanabe T, Winter A, Oba T. Seasonal changes in sea surface temperature and salinety during the Little Ice Age in the Caribbean Sea deduced from Mg/Ca and 18O/16O ratios in corals[J]. Marine Geology,2001,173(1/4):21-35.
[65] Bec N L, Juillet-Leclerc A, Corre`ge T, et al. A coral δ18O record of ENSO driven seas surface salinity variability in Fiji (south-western tropical Pacific)[J]. Geophysical Research Letter, 2000,27(23):3 897-3 900.
[66] Wang Pinxian. Earth system science in China Quo Vadis?[J]. Advances in Earth Science,2003,18(6):837-851.[汪品先.我国的地球系统科学研究向何处去[J].地球科学进展,2003,18(6):837-851.]
[67] Sun Yali, Sun Min, Wei Gangjian, et al. Strontium contents of a Porites coral from Xisha Island, South China Sea: A proxy for sea-surface temperature of the 20th century[J]. Paleoceanography,2004,19(2), doi:PA2004.10.1029/2003PA000959.
[68] Ge Quansheng, Zheng Jingyun, Man Zhimin, et al. Key points on temperature change of the past 2000 years in China[J]. Progress in Natural Science, 2004,14(4):449-450.[葛全胜,郑景云,满志敏,等.过去2000年中国温度变化研究的几个问题[J]. 自然科学进展,2004,14(4):449-450.]
[69] Wang Pinxian. The role of west pacific marginal seas in glacial aridification of China:A preliminary study[J]. Quaternary Sciences,1995,(1):32-42.[汪品先.西太平洋边缘海对我国冰期干旱化影响的初步探讨[J]. 第四纪研究,1995,(1):32-42.]
[70] Dennis C. Coral reveals ancient origins of human genes[J]. Nature,2003,426(6 968):744-746.
[71] Karlson R H, Cornell H V, Hughes T P, et al. Coral communities are regionally enriched along an oceanic biodiversity gradient[J].Nature, 2004, 429(6 994):867-870 .
[72] Liu Yi, Peng Zicheng, Chen Tegu, et al. A new way of investigating red tides—Reconstructing paleo-environment from reef corals[J]. Ziran Zazhi,2004,26(3):141-144.[刘羿,彭子成,陈特固,等.一种研究赤潮的新途径——珊瑚古环境法的探讨[J].自然杂志,2004,26(3):141-144.]
[73] Gong Yiming, Li Baohua, Si Yuanlan, et al. Late Devonian red tide and mass extinction[J]. Chinese Science Bulletin,2002,47(7):554-560.[龚一鸣,李保华, 司远兰,等.晚泥盆赤潮与生物集群绝灭[J].科学通报,2002,47(7):554-560.]
[74] Su Jilan, Tang Qisheng. A new direction for China’s research on marine ecosystems [J]. Advances in Earth Science, 2005,20(2):139-143.[苏纪兰,唐启升.我国海洋生态系统基础研究的发展—国际趋势和国内需要[J].地球科学进展,2005,20(2):139-143.]
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