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Phytoplankton composition and its ecological effect in subsurface cold pool of the northern Bering Sea in summer as revealed by HPLC derived pigment signatures

机译:HPLC衍生的色素特征揭示夏季白令海北部表层冷池中的浮游植物组成及其生态效应

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摘要

CHEMTAX analysis of high-performance liquid chromatography (HPLC) pigment was conducted to study phytoplankton community structure in the northern Bering Sea shelf, where a seasonal subsurface cold pool emerges. The results showed that fucoxanthin (Fuco) and chlorophyll a (Chl a) were the most abundant diagnostic pigments, with the integrated water column values ranging from 141 to 2 160 µg/m2 and 477 to 5 535 µg/m2, respectively. Moreover, a diatom bloom was identified at Sta. BB06 with the standing stock of Fuco up to 9 214 µg/m3. The results of CHEMTAX suggested that the phytoplankton community in the northern Bering Sea shelf was dominated by diatoms and chrysophytes with an average relative contribu-tion to Chl a of 80%and 12%, respectively, followed by chlorophytes, dinoflagellates, and cryptophytes. Dia-toms were the absolutely dominant algae in the subsurface cold pool with a relative contribution exceeding 90%, while the contribution of chrysophytes was generally higher in oligotrophic upper water. Additionally, the presence of a cold pool would tend to favor accumulation of diatom biomass and a bloom that occurred beneath the halocline would be beneficial to organic matter sinks, which suggests that a large part of the phytoplankton biomass would settle to the seabed and support a rich benthic biomass.
机译:进行了高效液相色谱(HPLC)颜料的CHEMTAX分析,以研究白令海北部海域浮游植物群落结构,那里出现了季节性的地下冷池。结果表明,岩藻黄质(Fuco)和叶绿素a(Chl a)是最丰富的诊断颜料,水柱的积分值分别为141至2 160 µg / m2和477至5 535 µg / m2。此外,在Sta发现了硅藻绽放。 BB06,Fuco的现有库存量高达9214 µg / m3。 CHEMTAX的结果表明,白令海北部陆架的浮游植物群落以硅藻和温藻为主,对Chla的平均相对贡献分别为80%和12%,其次是绿藻,鞭毛藻和隐藻。直径最大的藻类是地下冷水池中的绝对优势藻类,相对贡献超过90%,而在贫营养的上层水域中,金藻类的贡献通常更高。此外,冷水池的存在将倾向于促进硅藻生物质的积累,而盐湖下方的水华将有利于有机质汇,这表明浮游植物生物质的很大一部分将沉降到海床并支撑海藻。底栖生物量丰富。

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  • 来源
    《海洋学报(英文版)》 |2014年第6期|103-111|共9页
  • 作者单位

    Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of 0ceanography, State 0ceanic Administration, Hangzhou 310012, China;

    Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of 0ceanography, State 0ceanic Administration, Hangzhou 310012, China;

    Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of 0ceanography, State 0ceanic Administration, Hangzhou 310012, China;

    Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of 0ceanography, State 0ceanic Administration, Hangzhou 310012, China;

    Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of 0ceanography, State 0ceanic Administration, Hangzhou 310012, China;

    College of 0cean and Meteorology, Guangdong 0cean University, Zhanjiang 524088, China;

    Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of 0ceanography, State 0ceanic Administration, Hangzhou 310012, China;

    Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of 0ceanography, State 0ceanic Administration, Hangzhou 310012, China;

    Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of 0ceanography, State 0ceanic Administration, Hangzhou 310012, China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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