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作 者:刘子琳[1] 陈忠元[2] 周蓓锋[1] 张涛[1] 丁涛[1]
机构地区:[1]国家海洋局第二海洋研究所国家海洋局海洋动力过程与卫星海洋学重点实验室,浙江杭州310012 [2]国家海洋局第二海洋研究所国家海洋局第二海洋研究所区域海洋学重点实验室,浙江杭州310012
出 处:《东海海洋》2004年第4期17-23,共7页Donghai Marine Science
基 金:国家海洋局海洋动力过程与卫星海洋学重点实验室资助项目(200201)
摘 要:2002年10~11月在15°00′~27°40′N,121°30′~131°00′E的吕宋岛、台湾岛和琉球群岛以东的西北太平洋副热带环流区设测站121个,观测了该区表层和水柱中的叶绿素a质量浓度分布和光合浮游生物粒级结构。结果表明,观测海区秋季叶绿素a的质量浓度较低,变化幅度较小,变幅范围为0.039~0.271μg/dm3。台湾岛至琉球群岛以东的北部测区平均叶绿素a质量浓度高于吕宋岛以东的南部测区。叶绿素a含量的垂直分布在真光层内随深度的增加而增大,在真光层以下却随深度增加而降低。表层水的光合浮游植物细胞丰度较低,并以小粒径的硅藻占优势,细胞丰度约为103个/dm3。粒度分级结果表明,Pico级份的光合浮游生物占绝对优势(86%),Nano级份次之(11%),大细胞的Net级份所占比例最小(3%),呈现出微微型光合浮游生物在寡营养海区居重要地位的状况。The size-fractionated chlorophyll a concentration was surveyed in the subtropical circle area of the northwest Pacific Ocean, which is in the area east of Ryukyu Islands chain, Taiwan Island and Luzon Island (15°00′~27°40′N, 121°30′~131°00′E) during the autumn 2002. The results showed that chlorophyll a concentration in the surface water was 0.039~0.271μg/dm^3,with an average value of 0.090±0.047μg/dm^3 in autumn;the chlorophyll a concentration in the northern area east of Islands Chain was higher than that in the southern surveyed area;the vertical distribution of chlorophyll a concentration was rather uniform; the chlorophyll a concentration in the surface water was lower,increasing with depths upon the euphotic layer and decreasing with depth under the euphotic zone until 200 m depth. The size-fractionated chlorophyll a concentration showed that the contribution of picoplankton was predominated (86%), the contributions of nanoplankton and netplankton accounted for 11% and 3% respectively;the abundance of phytoplankton in the surface water was 10~3cell/dm^3, and the small grain size diatoms were predominant.It suggested that the picoplankton was the most important group contributed to the chlorophyll a concentration in the surveyed sea area.
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