NING XIUREN, CHAI FEI, XUE HUI, et al. Physical- biological oceanographic coupling influencing phytoplankton and primary production in the South China Sea [J]. Journal of Geophysical Research, 2004, 109: C10005.LIU K K, CHAO S Y, SHAW P T, et al. Monsoon-forced chlorophyll distribution and primary production in the South China Sea: observations and a numerical study [J]. Deep Sea Research Ⅰ, 2002, 49(8): 1387-1412.RAGUENEAU O, TREGUER P, LEYNAERT A, et al. A review of the Si cycle in the modern ocean: recent progress and missing gaps in the application of biogenic opal as a paleoproductivity proxy [J]. Global and Planetary Change, 2000, 26(4): 317-365.PAYTAN A, GRIFFITH E M. Marine barite: Recorder of variations in ocean export Productivity [J]. Deep Sea Research II, 2007, 54(5-7): 687-705.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 [J]. Organic Geochemistry, 2006, 37(1): 72-97.HE JUAN, ZHAO MEIXUN, LI LI, et al. Biomarker evidence of relatively stable community structure in the northern South China Sea during the last glacial and Holocene [J]. Terrestrial, Atmospheric and Oceanic Sciences, 2008, 19(4): 377-387.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: 中国地质大学学报, 2008, 33(6): 793-799.HU JIANFANG, PENG PING’AN, JIA GUODONG, 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): 1197-1204.ZHAO MEIXUN, HUANG C, WANG C, et al. A millennial-scale UK'37 sea-surface temperature record from the South China Sea (8°N) over the last 150 kyr: Monsoon and sea-level influence [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2006, 236(1-2): 39-55.SHIAU L, YU P, WEI K. Sea surface temperature, productivity, and terrestrial flux variations of the south-eastern south china sea over the past 800000 years(IMAGESMD972142) [J]. Terrestrial, Atmospheric and Oceanic Sciences, 2008, 19(4): 363-376.HU JIANFANG, PENG PING’AN, CHIVAS A R. Molecular biomarker evidence of origins and transport of organic matter in sediments of the Pearl River estuary and adjacent South China Sea [J]. Applied Geochemistry, 2009, 24(9): 1666-1676.赵美训, 赵晓晨, 陈建芳, 等. 南海表层沉积物生物标志物的分布特征及古生产力重建意义[J]. 热带海洋学报, 2009, 28(3): 45-53.MEYERS P A. Organic geochemical proxies of paleoceanographic, paleolimnologic, and paleoclimatic processes [J]. Organic Geochemistry, 1997, 27(5-6): 213-250.WAKEHAM S G, PETERSON M L, HEDGES J I, et al. Lipid biomarker fluxes in the Arabian Sea, with a comparison to the equatorial Pacific Ocean [J]. Deep-Sea Research II, 2002, 49: 2265-2301.HERNANDEZ M T, MILLS R A, PANCOST R D. Algal biomarkers in surface waters around the Crozet Plateau [J]. Organic Geochemistry, 2008, 39(8):1051-1057.GONG G, LIU K K, LIU C T, et al. The chemical hydrography of the South China Sea west of Luzon and a comparison with the West Philippine Sea [J]. Terrestrial, Atmospheric and Oceanic Sciences, 1992, 3(4): 587-602.WANG HUI, JIN QIHUA, GAO SHAN. A preliminary study on the response of marine primary production to monsoon variations in the South China Sea [J]. Acta Oceanologica Sinica, 2008, 27(5): 21-35.赵焕庭. 珠江河口演变[M]. 北京: 海洋出版社, 1990: 1-357.SHAW P T, CHAO S Y. Surface circulation in the South China Sea [J]. Deep Sea Research I, 1994, 41(11-12): 1663-1683.WANG DONGXIAO, HONG BO, GAN JIANPING, et al. Numerical investigation on propulsion of the counter-wind current in the northern South China Sea in winter [J]. Deep Sea Research I, 2010, 57(10): 1206-1221. DONG LIXIAN, SU JILAN, LAI A W, et al. Seasonal variation and dynamics of the Pearl River plume [J]. Continental Shelf Research, 2004, 24(16): 1761-1777.GAN JIANPING, LI LI, WANG DONGXIAO, et al. Interaction of a river plume with coastal upwelling in the northeastern South China Sea [J]. Continental Shelf Research, 2009, 29(4): 728-740.乐凤凤, 孙军, 宁修仁, 等. 2004年夏季中国南海北部的浮游植物[J]. 海洋与湖沼, 2006, 37(3): 238-248.孙军, 宋书群, 乐凤凤, 等. 2004年冬季南海北部浮游植物[J]. 海洋学报, 2007, 29: 132-145.郝锵, 宁修仁, 刘诚刚, 等. 南海北部初级生产力遥感反演及其环境调控机制[J]. 海洋学报, 2007, 29(3): 58-68.陈纪新, 黄邦钦, 刘媛, 等. 应用特征光合色素研究东海和南海北部浮游植物的群落结构[J]. 地球科学进展, 2006, 21(7): 738-746.HUANG BANGQIN, HU JUN, XU HONGZHOU, et al. Phytoplankton community at warm eddies in the northern South China Sea in winter 2003/2004 [J]. Deep Sea Research II, 2010, 57: 1792–1798.CHEN Y L L, CHEN H Y, KARL D M, et al. Nitrogen modulates phytoplankton growth in spring in the South China Sea [J]. Continental Shelf Research, 2004, 24: 527-541.HUANG BANGQIN, LAN WENLU, CAO ZHENRUI, et al. Spatial and temporal distribution of nanoflagellates in the northern South China Sea [J]. Hydrobiologia, 2008, 605(1):143-157.YIN KEDONG, QIAN PEIYUAN, WU M C S, et al. Shift from P to N limitation of phytoplankton growth across the Pearl River estuarine plume during summer [J]. Marine Ecology Progress Series, 2001, 221: 17-28.DAI MINHAN, ZHAI WEIDONG, CAI WEIJUN, et al. Effects of an estuarine plume-associated bloom on the carbonate system in the lower reaches of the Pearl River estuary and the coastal zone of the northern South China Sea [J]. Continental Shelf Research, 2008, 28(12): 1416-1423.XUE HUIJIE, CHAI FEI, XU DANYA, et al. Characteristics and seasonal variation of the coastal currents in the South China Sea [J]. Oceanography in China, 2001, 13: 64-75.SU JILAN. Overview of the South China Sea circulation and its influence on the coastal physical oceanography outside the Pearl River Estuary [J]. Continental Shelf Research, 2004, 24(16): 1745-1760.NITANI H. Beginning of the Kuroshio [J]. Kuroshio: Physical Aspects of the Japan Current, 1972: 129-163.SHAW P. The seasonal variation of the intrusion of the Philippine Sea water into the South China Sea [J]. Journal of Geophysical Research, 1991, 96(C1): 821-827.LI LI, POHLMANN T. The South China Sea warm-core ring 94S and its influence on the distribution of chemical tracers [J]. Ocean Dynamics, 2002, 52(3): 116-122.QIU DAJUN, HUANG LIANGMIN, ZHANG JIANLIN, et al. Phytoplankton dynamics in and near the highly eutrophic Pearl River Estuary, South China Sea [J]. Continental Shelf Research, 2010, 30(2): 177-186.EGGE J K. Are diatoms poor competitors at low phosphate concentrations? [J]. Journal of Marine Systems, 1998, 16(3-4): 191-198.RICHARDSON K. Harmful or exceptional phytoplankton blooms in the marine ecosystem, advances in marine biology [M]. London: Academic Press, 1997: 301-385.XU JIE, YIN KEDONG, HE LEI, et al. Phosphorus limitation in the northern South China Sea during late summer: Influence of the Pearl River [J]. Deep Sea Research I, 2008, 55: 1330-1342.YIN KEDONG, SONG XIUXIAN, SUN JUN, et al. Potential P limitation leads to excess N in the pearl river estuarine coastal plume [J]. Continental Shelf Research, 2004, 24(16): 1895-1907.WANG ZHAOHUI, QI YUZAO, CHEN JUFENG, et al. Phytoplankton abundance, community structure and nutrients in cultural areas of Daya Bay, South China Sea [J]. Journal of Marine Systems, 2006, 62(1-2): 85-94.RIEGMAN R, STOLTE W, NOORDELOOS A, et al. Nutrient uptake and alkaline phosphatase (EC 3 : 1 : 3 : 1) activity of Emiliania huxleyi (Prymnesiophyceae) during growth under N and P limitation in continuous cultures [J]. Journal of Phycology, 2000, 36(1): 87-96.CHISHOLM S W. Phytoplankton size [M] // FALKOWSKI P G, WOODHEAD A D. Primary productivity and biogeochemical cycles in the sea. New York: Plenum Press, 1992: 213-237. |