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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  ( SCI-EXPANDED收录)   被引量:17

文献类型:期刊文献

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

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

作者:Zhuang Yanpei[1];Jin Haiyan[1,2];Li Hongliang[1];Chen Jianfang[1,2];Wang Bin[1];Chen Fajin[3];Bai Youcheng[1];Lu Yong[1];Tian Shichao[1]

机构:[1]State Ocean Adm, Inst Oceanog 2, Lab Marine Ecosyst & Biogeochem, Hangzhou 310012, Zhejiang, Peoples R China;[2]State Ocean Adm, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou 310012, Zhejiang, Peoples R China;[3]Guangdong Ocean Univ, Coll Ocean & Meteorol, Zhanjiang 524088, Peoples R China

年份:2014

卷号:33

期号:6

起止页码:103

中文期刊名:Acta Oceanologica Sinica

外文期刊名:ACTA OCEANOLOGICA SINICA

收录:SCI-EXPANDED(收录号:WOS:000336422900013)、CSTPCD、、Scopus(收录号:2-s2.0-84905445247)、WOS、CSCD、CSCD2013_2014

基金:Foundation item: The National Natural Science Foundation of China under contract Nos 41276198, 41076135 and 41003036; the Scientific Research Fund of Second Institute of Oceanography, SOA under contract Nos JG1323 and JG1023; the Chinese Polar Environment Comprehensive Investigation and Assessment Programs under contract Nos 20130403 and 20130304.

语种:英文

中文关键词:pigment;phytoplankton community structure;CHEMTAX;northern Bering Sea shelf;subsurface cold pool

外文关键词:pigment; phytoplankton community structure; CHEMTAX; northern Bering Sea shelf; subsurface cold pool

中文摘要: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 2160 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 9214 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.

外文摘要: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 mu g/m(2) and 477 to 5 535 mu g/m(2), respectively. Moreover, a diatom bloom was identified at Sta. BB06 with the standing stock of Fuco up to 9 214 mu g/m(3). 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 contribution to Chl a of 80% and 12%, respectively, followed by chlorophytes, dinoflagellates, and cryptophytes. Diatoms 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.

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