嵊山水域中肋骨条藻赤潮发生过程主导因子分析
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摘要: 嵊山位于我国长江口、杭州湾的长江三角洲浅海大陆边缘,系长江口赤潮多发区[1]的东北部(30°45'27"N,122°48'15"E),是我国最东侧的一个居民岛.该岛地处中纬度,周围海域北面受制于黄海冷水团,东南接纳外海暖水,西面濒临长江径流的季节影响,生态环境复杂多变,时常有赤潮发生[1-3].
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洪君超等.长江口外及邻近海区赤潮多发区的分析与探讨.暨南大学学报(赤潮研究专刊),1989,90-50 洪君超等.长江口赤潮多发区的一次中肋骨条藻赤潮现象观察.海洋环境科学,1992,11(3):75-79 蒋晓山等.长江口赤潮多发地区夜光藻赤潮发生过程分析.暨南大学学报,1992,13(3);139-138 安达六郎.赤潮生物01分类学研究.三重县水产学报纪要,1972,9(1):46 Boto K G,Dissolved oxygen and pH relationships in northern australian mangrove waterways.Limnol,Oceanogr.,1981,26(5):1176-1179 Furras M J,Cyclonic disturbance and phytoplankton bloom in a tropical shelf ecosystem:RED TIDES.Biology,Environmental Science and Toxicology,Elsevier Science Publishers,New York,273-276 Masao K.Algal growth potential and the limiting nutrient in Mikawa Bay.J.of Oceanogr.Soc,of Japan,1984,40(5):391-396 Yamoch S.Nutrient factors involved in controlling the growth of red tide flagellates Prorocentrum micans,Eutreptiella sp,and Chtattonella mirana in Osaka Bay.Bull.Plankton Soc,Japan,1984,31(12);97-106 Cochlan W P.Seasonal study of uptake and regeneration of nitrogen on the Scotian Shelf.Continental Shelf Research,1986,5(5);555-557 Blasco D.Effect of ammonium on the regulation of nitrate assimilation in natural phytoplankton populations.J.Ex p.Mar.Biol.Ecol.,1982,61(2),157-168 -
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