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中尺度涡影响下的南海西部活性铝分布
引用本文:刘甲星,周林滨,谭烨辉,王琼,胡子峰,李佳俊,姜歆,柯志新.中尺度涡影响下的南海西部活性铝分布[J].海洋学报(英文版),2017,36(6):95-103.
作者姓名:刘甲星  周林滨  谭烨辉  王琼  胡子峰  李佳俊  姜歆  柯志新
作者单位:中国科学院南海海洋研究所中国科学院热带海洋生物资源与生态重点实验室, 广东 广州 510301;中国科学院南海海洋研究所广东省应用海洋生物学重点实验室, 广东 广州 510301;中国科学院大学, 北京 100049,中国科学院南海海洋研究所中国科学院热带海洋生物资源与生态重点实验室, 广东 广州 510301;中国科学院南海海洋研究所广东省应用海洋生物学重点实验室, 广东 广州 510301,中国科学院南海海洋研究所中国科学院热带海洋生物资源与生态重点实验室, 广东 广州 510301;中国科学院南海海洋研究所广东省应用海洋生物学重点实验室, 广东 广州 510301,中国科学院南海海洋研究所中国科学院热带海洋生物资源与生态重点实验室, 广东 广州 510301;中国科学院南海海洋研究所广东省应用海洋生物学重点实验室, 广东 广州 510301;中国科学院大学, 北京 100049,中国科学院南海海洋研究所中国科学院热带海洋生物资源与生态重点实验室, 广东 广州 510301;中国科学院南海海洋研究所广东省应用海洋生物学重点实验室, 广东 广州 510301;中国科学院大学, 北京 100049,中国科学院南海海洋研究所中国科学院热带海洋生物资源与生态重点实验室, 广东 广州 510301;中国科学院南海海洋研究所广东省应用海洋生物学重点实验室, 广东 广州 510301;中国科学院大学, 北京 100049,中国科学院南海海洋研究所中国科学院热带海洋生物资源与生态重点实验室, 广东 广州 510301;中国科学院南海海洋研究所广东省应用海洋生物学重点实验室, 广东 广州 510301;中国科学院大学, 北京 100049,中国科学院南海海洋研究所中国科学院热带海洋生物资源与生态重点实验室, 广东 广州 510301;中国科学院南海海洋研究所广东省应用海洋生物学重点实验室, 广东 广州 510301
基金项目:The Strategic Priority Research Program of the Chinese Academy of Sciences under contract No. XDA11020305; the National Basic Research Program (973 program) of China under contract No. 2015CB452903; the Special Fund for Agro-scientific Research in the Public Interest under contract No. 201403008; the National Project of Basic Sciences and Technology under contract No. 2017FY201404; the National Natural Science Foundation of China under contract Nos 41506150 and 41276162.
摘    要:To understand the distribution of aluminum(Al) under the influence of mesocale eddies in the western South China Sea(SCS), sea level anomaly, geostrophic current, environmental parameters and reactive Al were investigated in the western SCS in August 2013. The highest reactive Al concentration((180±64) nmol/L) was observed in the surface waters, indicating a substantial atmospheric input. Vertically, the reactive Al decreased from the surface high concentration to the subsurface minima at the depth of chlorophyll a(Chl a) maxima and then increased again with depth at most of the stations. The average concentration of reactive Al in the upper 100 m water column was significantly lower in the cyclonic eddy((137±6) nmol/L) as compared with that in the noneddy waters((180±21) nmol/L). By contrast, the average concentrations of Chl a and silicate in the upper 100 m water column were higher in the cyclonic eddy and lower in the anticyclonic eddy. There was a significant negative correlation between the average concentrations of reactive Al and Chl a in the upper 100 m water column. The vertical distribution of reactive Al and the negative correlation between reactive Al and Chl a both suggest that the reactive Al in the upper water column was significantly influenced by biological removal processes. Our results indicate that mesoscale eddies could regulate the distribution of reactive Al by influencing the primary production and phytoplankton community structure in the western SCS.

关 键 词:活性铝  中尺度涡  叶绿素a  生物清除  浮游植物  初级生产力  南海西部
收稿时间:2016/3/7 0:00:00
修稿时间:2016/6/30 0:00:00

Distribution of reactive aluminum under the influence of mesoscale eddies in the western South China Sea
LIU Jiaxing,ZHOU Linbin,TAN Yehui,WANG Qiong,HU Zifeng,LI Jiajun,JIANG Xin and KE Zhixin.Distribution of reactive aluminum under the influence of mesoscale eddies in the western South China Sea[J].Acta Oceanologica Sinica,2017,36(6):95-103.
Authors:LIU Jiaxing  ZHOU Linbin  TAN Yehui  WANG Qiong  HU Zifeng  LI Jiajun  JIANG Xin and KE Zhixin
Institution:Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;University of Chinese Academy of Sciences, Beijing 100049, China,Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China,Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China,Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;University of Chinese Academy of Sciences, Beijing 100049, China,Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;University of Chinese Academy of Sciences, Beijing 100049, China,Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;University of Chinese Academy of Sciences, Beijing 100049, China,Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;University of Chinese Academy of Sciences, Beijing 100049, China and Key Laboratory of Tropical Marine Bio-resources and Ecology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
Abstract:To understand the distribution of aluminum (Al) under the influence of mesocale eddies in the western South China Sea (SCS), sea level anomaly, geostrophic current, environmental parameters and reactive Al were investigated in the western SCS in August 2013. The highest reactive Al concentration ((180±64) nmol/L) was observed in the surface waters, indicating a substantial atmospheric input. Vertically, the reactive Al decreased from the surface high concentration to the subsurface minima at the depth of chlorophyll a (Chl a) maxima and then increased again with depth at most of the stations. The average concentration of reactive Al in the upper 100 m water column was significantly lower in the cyclonic eddy ((137±6) nmol/L) as compared with that in the non-eddy waters ((180±21) nmol/L). By contrast, the average concentrations of Chl a and silicate in the upper 100 m water column were higher in the cyclonic eddy and lower in the anticyclonic eddy. There was a significant negative correlation between the average concentrations of reactive Al and Chl a in the upper 100 m water column. The vertical distribution of reactive Al and the negative correlation between reactive Al and Chl a both suggest that the reactive Al in the upper water column was significantly influenced by biological removal processes. Our results indicate that mesoscale eddies could regulate the distribution of reactive Al by influencing the primary production and phytoplankton community structure in the western SCS.
Keywords:reactive aluminum  mesoscale eddy  chlorophyll a  biological removal  phytoplankton  primary production  western South China Sea
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