[1] |
Field C B,BehrenfeldM J,Randerson,J T,et al.Primary production of the biosphere:Integrating terrestrial and oceanic components[J].Science,1998,281:237-240.
Google Scholar
|
[2] |
Falkowski P G.The biogeochemistry of primary productivity in the sea[J].Treastise of Geochemistry,2003,682:185-213.
Google Scholar
|
[3] |
Falkowski P G,Barber R T,Smetacek V.Biogeochemical controls and feedbacks on ocean primary production[J].Science,1998,281:200-206.
Google Scholar
|
[4] |
李丽,汪品先.大洋"生物泵"-海洋浮游植物生物标志物[J].海洋地质与第四纪地质,2004,24(4):73-79.
Google Scholar
[LI Li,WANG Pinxian.Marine "bio-pump":biomarker of marine phytoplankton[J].Marine Geology and Quaternary Geology, 2004,24(4):73-79.]
Google Scholar
|
[5] |
张前前,唐晓静,王修林,等.脂类生物标志物在海洋环境中的应用与研究进展[J].中国海洋大学学报,36(3):381-385.[ZHANG Qianqian,TANG Xiaojing,WANG Xiulin,et al.Research progress in applications of lipid biomarkers in the marine environment[J].Periodical of Ocean University of China,2006
Google Scholar
, 36(3):381-385.]
Google Scholar
|
[6] |
Yan X H,Ho C R,Zheng Q, et al.Temperature and size varibilities of the Western Pacific Warm Pool[J].Science, 1992, 258:1643-1645.
Google Scholar
|
[7] |
Webster P J,Magana V O,Palmer T N,et al.Monsoons:Processes,predictability and the prospects for prediction[J].Journal of Oceanography,1998,103(29):14451-14510.
Google Scholar
|
[8] |
Mackey D J,Higgins H W,Mackey M D,et al.Algal class abundances in the western equatorial Pacific:Estimation from HPLC measurements of chloroplast pigments using CHEMTAX[J].Deep-Sea Research I,1998,45:1441-1468.
Google Scholar
|
[9] |
Kawahata N A,Gagan M G.Seasonal change in foraminifera production in the western Equatorial Pacific warm pool:evidence from sediment trap experiment[J].Deep-Sea Research Ⅱ,2002,49:2783-2800.
Google Scholar
|
[10] |
Le Borgne R,Feely R A,Mackey D J.Carbon fluxes in the equatorial Pacific:a synthesis of the JGOFS programme[J].Deep-Sea Research Ⅱ,2002,49:2425-2442.
Google Scholar
|
[11] |
Christian J R, Murtugudde R, Ballabrera-Poy J, et al. A ribbon of dark water:phytoplankton blooms in the meanders of the Pacific north equatorial countercurrent[J].Deep-Sea Research Part Ⅱ,2004,51:209-228.
Google Scholar
|
[12] |
Ryan J P,Ueki I,Chao Y,et al.Western Pacific modulation of large phytoplankton blooms in the central and eastern equatorial Pacific[J].Journal of Geophysical Research,2006,111,G02013:0148-0227.
Google Scholar
|
[13] |
Messié M,Radenac M H. Seasonal variability of the surface chlorophyll in the western tropical Pacific from SeaWiFS data[J].Deep-Sea Research I,2006,53:1581-1600.
Google Scholar
|
[14] |
Yamasaki M,Sasaki A,Oda M,et al.Western equatorial Pacific planktic foraminifera fluxes and assemblages during a La Nina year 1999[J].Marine Micropaleontology,2008,66:304-319.
Google Scholar
|
[15] |
Takahashi K,Onodera J,Katsurada Y.Relationship between time-series diatom fluxes in the central and western equatorial Pacific and ENSO-associated migrations of the western Pacific Warm Pool[J].Deep-Sea Research I,2009,56:1298-1318.
Google Scholar
|
[16] |
Wang X J,Behrenfeld M,Le B R,et al.Regulation of phytoplankton carbon to chlorophyll ratio by light,nutrients and temperature in the equatorial Pacific Ocean:a basin-scale model[J].Biogeosciences,2009,6:391-404.
Google Scholar
|
[17] |
Gordon A L,Fine R A.Pathways of water between the Pacific and Indian oceans in the Indonesian seas[J].Nature,1996, 379:146-149.
Google Scholar
|
[18] |
李丽,王慧,汪品先.南海北部17937岩心四万年来古环境变化的分子有机地球化学记录[J].地球科学,2008,33(6):793-798.
Google Scholar
[LI Li, WANG Hui, WANG Pinxian. Molecular organic geochemical record of paleoenvironmental changes of Core 17937 in northern South China Sea since 40 ka[J].Earth Science-Journal of China University of Geosciences,2008,33(6):793-798.]
Google Scholar
|
[19] |
Volkman J K,Barrett S M,Blackburn S,et al.Microalgal biomarkers:a review of recent research developments[J].Organic Geochemistry,1998,29:1163-1179.
Google Scholar
|
[20] |
丁玲,赵美训.生物标志物重建浮游植物生产力及群落结构研究进展[J].地球科学进展,2010,25(9):981-989.
Google Scholar
[DING Lin, ZHAO Meixun.Applications of biomarkers for reconstructing phytoplankton productivity and community structure changes[J].Advances in Earth Science,2010,25(9):981-989.]
Google Scholar
|
[21] |
刘杰,李丽,贺娟.南海海域浮游植物分布特征及研究进展[J].海洋地质与第四纪地质,2010,30(3):133-142.
Google Scholar
[LIU Jie,LI Li,HE Juan.Recent advances on characterization of the phytoplanktonic distribution in the South China Sea[J].Marine Geology and Quaternary Geology,2010,30(3):133-142.]
Google Scholar
|
[22] |
Behrenfeld M O,Malley R,Siegel D, et al.Climate-driven trends in contemporary ocean productivity[J].Nature,2006, 444:752-755.
Google Scholar
|
[23] |
Martin J H.Glacial-interglacial CO2 change:The iron hypothesis[J].Paleoceanography,1990,5(1):1-13.
Google Scholar
|
[24] |
张武昌,孙松.铁假说和HNLC海区的现场铁加富实验[J].地球科学进展,2002,17:612-615.[ZHANG Wuchang, SUN Song.Iron hypothesis and the in situ iron fertilization experiments in the HNLC regions[J].Advances in Earth Sciences,2002
Google Scholar
,17:612-615.]
Google Scholar
|
[25] |
李宏亮,陈建芳.HNLC海区间现场加铁实验的比较[J].东海海洋,2005,23:24-32.[LI Hongliang, CHEN Jianfang.A comparison of in-situ iron enrichment experiments in the three HNLC regions[J].Donghai Marine Science,2005
Google Scholar
,23:24-32.]
Google Scholar
|
[26] |
Dai L,Weng C Y.A survey on pollen dispersal in the western Pacific Ocean and its paleoclimatological significance as a proxy for variation of the Asian winter monsoon[J].Science China-Earth Sciences,2011,54(2):249-258.
Google Scholar
|
[27] |
Pinckney J,Paerl H,Tester P,et al.The role of nutrient loading and eutrophication in estuarine ecology[J]. Environmental Health Perspectives,2001,109:699-706.
Google Scholar
|
[28] |
Gong G-Ch,Wen Y-H,Wang B-W,et al.Seasonal variation of chlorophyll a concentration,primary production and environmental conditions in the subtropical East China Sea[J].Deep-Sea Research Ⅱ,2003,50:1219-1236.
Google Scholar
|
[29] |
Pea M A,MarlonR L,Cullen J J.New production in the warm waters of the tropical Pacific Ocean[J].Journal of Geophysical Research,1994,99:14255-14268.
Google Scholar
|
[30] |
Abe K.Apparent biological fractionation between Cd and PO4 in the surface waters of the equatorial Pacific Ocean[J].Marine Chemistry,2005,96:347-358.]
Google Scholar
|
[31] |
Mackey D J,O'Sullivan J E,Watson R J.Iron in the western Pacific:a riverine or hydrothermal source for iron in equatorial undercurrent[J].Deep-Sea Research I,2002,49:877-893.
Google Scholar
|
[32] |
Matsumoto K,Furuya K,Kawano T.Association of picophytoplankton distribution with ENSO events in the equatorial Pacific between 145°E and 160°W[J].Deep-Sea Research I,2004,51:1851-1871.
Google Scholar
|
[33] |
Takeda S,Ramaiah N,Miki M,et al.Biological and chemical characteristics of high-chlorophyll,low-temperature water observed near the Sulu Archipelago[J].Deep-Sea Research Ⅱ,2007,54:81-102.
Google Scholar
|
[34] |
Miki M,Ramaiah N,Takeda S,et al.Phytoplankton dynamics associated with the monsoon in the Sulu Sea as revealed by pigment signature[J].Journal of Oceanography,2008,4:663-73.
Google Scholar
|
[35] |
Furuya K,Hayashi M,Yabushita Y,et al.Phytoplankton dynamics in the East China Sea in spring and summer as revealed by HPLC-derived pigment signatures[J].Deep-Sea Research Ⅱ,2003,50:367-387.
Google Scholar
|
[36] |
Chen Y L,Chen H-Y,David M,Karl M.Nitrogen modulates phytoplankton growth in spring in the South China Sea Takahashi[J].Continental Shelf Research,2004,24:527-541.
Google Scholar
|
[37] |
Tanaka Y,Kawahata H.Seasonal occurrence of coccoliths in sediment traps from West Caroline Basin,equatorial West Pacific Ocean[J].Marine Micropaleontology,2001,43:273-284.
Google Scholar
|