Calvo E,Pelejero C,Logan G A et al.Dust-induced changes in phytoplankton composition in the Tasman Sea during the last four glacial cycles.Paleoceanography,2004,19:PA2020,doi:1029/2003PA000992
[2]
Higginson M J,Altabet M A,Murray D W et al.Geochemical evidence for abrupt changes in relative strength of the Arabian monsoons during a stadial/interstadial climate transition.Geochimica et Cosmochimica Acta,2004,68(19):3807~3826
[3]
Lie H J,Cho C H,Lee J H et al.Separation of the Kuroshio water and its penetration the continental shelf west of Kyushu.Journal of Geophysical Research,1998,103(C2):2963~2976
[4]
Zhao Meixun,Mercer J L,Eglinton G et al.Comparative molecular biomarker assessment of phytoplankton paleoproductivity for the last 160 kyr off Cap Blanc,NW Africa.Organic Geochemistry,2006,37(1):72~97
[5]
Stuiver M,Reimer P J,Bard E et al.INTCAL98 radiocarbon age calibration 24000~0 cal.aBP.Radiocarbon,1998,40:1041~1083
[6]
Whatley R,Boomer I.Autochthonous and allochthonous Quaternary ostracoda from Site 893,Santa Barbara Basin.In:Kennett J P,Baldauf J G,Lyle M eds.Proceedings of the Ocean Drilling Program,Scientific Results,1995,146:251~255
[7]
Wei K Y.Leg195 Synthesis:Site 1202--LaLe Quaternary sedimentation and paleoceanography in the Southern Okinawa Troush.In:Shinohara M,Salisbury M H,Richter C eds.Proceedings of the Ocean Drilling Program,Scientific Results,2004,195:1~31
[8]
Brummer G J A.van Eijden A J M."Blue-ocean"palcoproductivity estimates from pelagic carbonate mass accumulation rate.Marine Micropaleontology,1992,19(1~2):99~117
[9]
Zhao Meixun,Dupont L,Eglinton G et al.n-Alkane and pollen reconstruction of terrestrial climate and vegetation for N.W.Africa over the last 160 kyr.Organic Geochemistry,2003,34(1):131~143
[10]
Hsu Shihchieh,Lin Feijan,Jeng Woeilih et al.Observed sediment fluxes in the southwesternmost Okinawa Trough enhanced by episodic events:Flood runoff from Taiwan rivers and large earthquakes.Deep Sea Research Part Ⅰ:Oceanographic Research Papers,2004,51(7):979~997
[11]
Ruddiman W F.Tropical Atlantic terrigenous fluxes since 25,000 yrs B.P.Marine Geology,1997,136(3~4):189~207
[12]
Harris P G,Zhao M,Rosell-Mele A et al.Chlorin accumulation rate as a proxy for Quaternary marine primary productivity.Nature,1996,383:63~65
[13]
Altabet M A.Nitrogen and carbon isotopic tracers of the source and transformation of particles in the deep sea.In:lttekot V,Sch(a)fer P,Honjo S et al.eds.Particle Flux in the Ocean.Hoboken:John Wiley,1996.155~184
[14]
Sheu D D,Jou W C,Chung Y C et al.Geochemical and carbon isotopic characterization of particles collected in sediment traps from the East China Sea continental slope and the Okinawa Trough northeast of Taiwan.Continental Shelf Research,1999,19(2):183~203
[15]
Kao S J,Lin F J,Liu K K.Organic carbon and nitrogen contents and their isotopic compositions in surficial sediments from the East China Sea shelf and the southern Okinawa Troush.Deep Sea Research,Part Ⅱ:Topical Studies in Oceanography,2003,50(6~7):1203~1217
[16]
Martin J H.Fitzwater S E.Iron deficiency limits phytoplankton growth in the north-east Pacific subarctic.Nature,1988,331:341~343
[17]
Price N M.Morel F M M.Cadmium and cobalt substitution for zinc in a marine diatom.Nature,1990,344:658~660
[18]
Mills M M,Ridame C,Davey M et al.Iron and phosphonls co-limit nitrogen fixation in the eastern tropical North Atlantic.Nature,2004,429:292~294
[19]
Wells M L.The level of iron enrichment required to initiate diatom blooms in HNLC waters.Marine Chemistry,2003,82(1~2):101~114
[20]
Milliman J D,Hsueh Y,Hu Dunxin et al.Tidal phase control of sediment discharge from the Yangtze River.Coastal and Shelf Science,1984,19(1):119~128
[21]
Kao S J,Liu K K.Estimating the suspended sediment load by using the historical hydrometric record from the Lanyang-hsi watershed.Terrestrial,Atmospheric and Oceanic Sciences,2000,12(2):401~414
[22]
Bertrand P,Shimmield G,Martinez P et al.The glacial ocean productivity hypothesis:The importance of regional temporal and spatial studies.Marine Geology,1996,130(1~2):1~9
[23]
Yancheva G,Nowaczyk N R,Mingram J et al.Influence of the intertropical convergence zone on the East Asian monsoon.Nature,2007,445:74~77
[24]
Fleitmann D,Bums S J,Mangini A et al.Holocene ITCZ and Indian monsoon dynamics recorded in stalagmites from Oman and Yemen(Socotra).Quaternary Science Reviews,2007,26(1~2):170~188
[25]
Hughen K A,Overpeck J T,Peterson L C et al.Rapid climate changes in the tropical Atlantic region during the last deglaciation.Nature,1996,380:51~54
[26]
Haug G H,Hughen K A,Sigman D M et al.Southward migration of the intertropical convergence zone through the Holocene.Science,2001,293:1304~1308
[27]
Xiang Rong,Sun Youbin,Li Tiegang et al.Paleoenvironmental change in the middle Okinawa Trough since the last deglaciation:Evidence from the sedimentation rate and planktonic foraminiferal record.Palaeogeography,Palaeoclimatology,Palaeoecology,2007,243(3~4):378~393
[28]
Marlowe I T,Brassell S C,Eglinton G et al.Long-chain alkenones and alkyl alkenoates and the fossil coccolith record of marine sediments.Chemical Geology,1990,88(3~4):349~375
[29]
Villanueva L,Grimalt J O,Cortijo E et al.A biomarker approach to the organic matter deposited in the North Atlantic during the last climatic cycle.Geochimica et Cosmochimica Acta,1997,61:4633~4646
[30]
Henriksson A S,Sarnthein M,Eglinton G et al.Dimethylsulfide production variations over the past 200k.y.in the equatorial Atlantic:A first estimate.Geology,2000,28(6):499~502
[31]
Broeeker W S.Peng T H.The causes of the glacial to interglacial atmospheric CO2 change:A polar alkalinity hypothesis.Global Biogeochemical Cycles,1989,3:215~239
[32]
Berger W H.Smetacek V S,Wefer G.Ocean productivity and Palaeoproductivity-An Overview.In:Berger W H,Smeataeek V S.Werer G eds.Productivity of the Ocean:Present and Past.New York:John Wiley and Sons Limited,1989.1~34
[33]
汪品先.气候演变中的冰和碳.地学前缘,2002,9(1):85~93 Wang Pinxian.Ice and carbon in climate evolution.Each Science Frontiers,2002,9(1):85~93
[34]
Anderson R F,Chase Z,Fleisher M Q et al.The Southern Ocean''s biological pump during the Last Glacial Maximum.Deep Sea Research Part Ⅱ:Topical Studies in Oceanography,2002,49(9~10):1909~1938
[35]
Abrantes F.200000 yr diatom records from Atlantic upwelling sites reveal maximum productivity during LGM and a shift in phytoplankton community structure at 185000yr.Earth and Planetary Science Letters,2000,176(1):7~16
[36]
Sarnthein M,Pflaumann U,Ross R et al.Transfer functions to reconstruct ocean paleoproductivity:A comparison.In:Summerhayes C P,Prell W L,Emeis K C eds.Upwelling Systems:Evolution since the Early Miocene.London:Geological Society,1992.411~427
[37]
Meyers P A.Organic geochemical proxies of paleoceanographic,paleolimnologic,and paleoclimatic processes.Organic Geochemistry,1997,27(5):213~250
[38]
Jeng W L.Aliphatic hydrocarbon concentrations in short sediment cores from the southeen Okinawa Troush:Implications for lipid deposition in a complex environment.Continental Shelf Research,2007,27(15):2066~2078
[39]
Cane M A.A role for the tropical Pacific.Seicnce,1998,282:59~61
[40]
Huang Ronghui,Yin Baoyu,Liu Aidi.Intraseasonal variability of the East Asian summer monsoon and its association with the convective activities in the tropical western Pacific.In:Ye D eds.Climate Variability.Beijing:Chinese Meteorological Press,1992.134~155
[41]
(李麦村),吴仪芳,黄嘉佑.中国东部季风降水与赤道东太平洋海温的关系.大气科学,1987,11(4):365~372 (Li Maicun),Wu Yifang,Huang Jiayou.The relationship between the monsoon rainfall over Eastern China and the eastern equatorial Pacific sea surface temperature.Seientia Atmospherica Sinica,1987,11(4):365~372
[42]
汪品先.我国海洋第四纪研究与环境演变中的海陆相互作用.第四纪研究,2001,21(3):218~222 Wang Pinxian.Marine Quaternary research in China and sea-land interaction in environmental changes.Quaternary Sciences,2001,21(3):218~222
[43]
田正隆,龙爱民,陈绍勇.南海古生产力研究进展.海洋科学,2004,28(8):65~71 Tian Zhenglong,Long Aimin,Chen Shaoyong.Review of paleoproductivity research in South China Sea.Marine Sciences,2004,28(8):65~71
[44]
李保华,赵泉鸿,王永吉等.冲绳海槽南部两万年来的浮游有孔虫与古海洋学事件.海洋学报,1997,19(4):90~98 Li Baohua,Zhao Quanhong,Wang Yongji et al.Planktonic foraminifer community and its paleoceanographic implications in the South Okinawa Trough since the last 20,000 years.Acta Oceanologica Sinica,1997,19(4):90~98
[45]
Chang Fengming,Zhuang Lihua,Li Tiegang et al.Radiolarian fauna in surface sediments of the northeastern East China Sea.Marine Micropaleontology,2003,48(3~4):169~204
[46]
刘晓东,安芷生,李小强等.最近18ka中国夏季风气候变迁的数值模拟研究.见:刘东生,安芷生,吴锡浩主编.黄土·第四纪地质·全球变化(第四集).北京:科学出版社,1996.142~150 Liu Xiaodong,An Zhisheng,Li Xiaoqiang et al.A stury on numeric model of summer monsoon climatic change of China in the last 18000 years.In:Liu Tungsheng,An Zhisheng,Wu Xihao eds.Loess,Quaternary Geology and Global Change Part IV.Beijing:Science Press,1996.142~150
[47]
吴文祥,刘东生.4000aB.P.前后东亚季风变迁与中原周围地区新石器文化的衰落.第四纪研究,2004,24(3):278~284 Wu Wenxiang,Liu Tungsheng.Variations in East Asia Monsoon around 4000aB.P.and the collapse of Neolithic cultures around central plain.Quaternary Sciences,2004,24(3):278~284
[48]
Bond G.Kromer B.Beer J et al.Persistent solar influence on North Atlantic climate during the Holocene.Science,2001,294:2130~2136
[49]
Holland G J.Global Guide to Tropical Cyclone Forecasting.Geneva:World Meteorological Organization,1993.1~293
[50]
Ivanochko T S,Ganeshram R S,Brommer G J A et al.Variations in tropical convection as an amplifier of global climate change at the millennial scale.Earth and Planetary Science Letters,2005,235(1~2):302~314
[51]
Gong G C,Shiah F K,Lju K K et al.Spatial and temporal variation of chlorophyll a,primary productivity and chemical hydrography in the southern East China Sea.Continental Shelf Research,2000,20(4~5):411~436