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WANG Lei,HUANG Hao,AN Lina,THOHA Hikmah,BONG Chuiwei,XIAO Wupeng,GU Haifeng.Comparison of photosynthetic pigments and phytoplankton assemblages in two types of coastal regions in Southeast Asia-Indonesian Throughflow and river estuary[J].Acta Oceanologica Sinica,2018,37(12):18-27
东南亚近岸海区浮游植物光合色素和群落组成—印度尼西亚贯穿流和吉兰丹河口区的比较研究
Comparison of photosynthetic pigments and phytoplankton assemblages in two types of coastal regions in Southeast Asia-Indonesian Throughflow and river estuary
投稿时间:2017-06-15  
DOI:10.1007/s13131-018-1284-3
中文关键词:  浮游植物  光合色素  蓝碧海峡  吉兰丹河口
英文关键词:phytoplankton  pigment  Lembeh Strait  Kelantan River Estuary
基金项目:The National Key R&D Program of China under contract Nos 2017YFC0604902 and 2017YFC1405101; the China-Indonesia Maritime Cooperation Fund Project "China-Indonesia Bitung Ecological Station Establishment"; the China-ASEAN Maritime Cooperation Fund and HICoE-MOHE Grant IOES-2014.
作者单位E-mail
王磊 自然资源部第三海洋研究所, 厦门 361005, 中国  
黄浩 自然资源部第三海洋研究所, 厦门 361005, 中国 huanghao@tio.org.cn 
安丽娜 自然资源部第三海洋研究所, 厦门 361005, 中国  
THOHA Hikmah 印度尼西亚科学研究院海洋研究中心, 雅加达 14430, 印度尼西亚  
BONG Chuiwei 海洋与地球科学学院, 马来亚大学, 吉隆坡 50603, 马来西亚
生物科学学院, 马来亚大学, 吉隆坡 50603, 马来西亚 
 
肖武鹏 滨海湿地生态系统教育部重点实验室, 厦门 361102, 中国  
顾海峰 自然资源部第三海洋研究所, 厦门 361005, 中国  
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中文摘要:
      于2016年7月和8月期间,在印度尼西亚蓝碧海峡和马来西亚吉兰丹河口区分别采集了水样用于分析浮游植物光合色素和群落组成的空间变化。利用高效液相色谱结合CHEMTAX软件检测浮游植物光合色素,确定叶绿素a生物量和群落组成。结果显示,蓝碧海峡表层海水叶绿素a浓度较低,在0.580~0.682μg/L之间,平均值为0.620±0.039 μg/L。然而,叶绿素a浓度在吉兰丹河口区表层海水波动较大,浓度在0.299~3.988μg/L之间,平均值为0.922±0.992 μg/L。在吉兰丹河口区,底层叶绿素a浓度明显高于表层,变动范围为0.704~2.352 μg/L,平均值1.493±0.571 μg/L。叶绿素b、玉米黄素和岩藻黄素是蓝碧海峡含量最丰富的三种色素。两个研究区域浮游植物群落组成存在着明显差别。在蓝碧海峡,青绿藻(26.48%±0.83%)和聚球藻(25.73%±4.13%)贡献了约50%的叶绿素a浓度,其次是硅藻(20.49%±2.34%)和定鞭藻-8型(15.13%±2.42%)。吉兰丹河口区表层海水主要以硅藻为优势(58.53%±18.44%),其次为聚球藻(27.27±14.84%)和青绿藻(7.00%±4.39%);底层水体与表层近似,硅藻、聚球藻和青绿藻分别贡献了64.89%±15.29%,16.23%±9.98% and 8.91%±2.62%的叶绿素a浓度。浮游植物群落组成的这种差别表明,蓝碧海峡水体主要是寡营养盐的西太平洋水,可能主要受到上行效应的控制;而吉兰丹河口区由于营养盐的补充,硅藻优势度明显,可能主要受到微型浮游动物摄食微微型浮游植物的下行效应调控其浮游植物群落结构。
英文摘要:
      Water samples were collected in order to study the spatial variation of photosynthetic pigments and phytoplankton community composition in the Lembeh Strait (Indonesia) and the Kelantan River Estuary (Malaysia) during July and August 2016, respectively. Phytoplankton photosynthetic pigments were detected using high performance liquid chromatography combining with the CHEMTAX software to confirm the Chl a biomass and community composition. The Chl a concentration was low at surface in the Lembeh Strait, which it was 0.580-0.682 μg/L, with the average (0.620±0.039) μg/L. Nevertheless, the Chl a concentration fluctuated violently at surface in the Kelantan River Estuary, in which the biomass was 0.299-3.988 μg/L, with the average (0.922±0.992) μg/L. The biomass at bottom water was higher than at surface in the Kelantan River Estuary, in which the Chl a concentration was 0.704-2.352 μg/L, with the average (1.493±0.571) μg/L. Chl b, zeaxanthin and fucoxanthin were three most abundant pigments in the Lembeh Strait. As a consequence, phytoplankton community composition was different in the two study areas. In the Lembeh Strait, prasinophytes (26.48%±0.83%) and Synechococcus (25.73%±4.13%) occupied ~50% of the Chl a biomass, followed by diatoms (20.49%±2.34%) and haptophytes T8 (15.13%±2.42%). At surface water in the Kelantan River Estuary, diatoms (58.53%±18.44%) dominated more than half of the phytoplankton biomass, followed by Synechococcus (27.27%±14.84%) and prasinophytes (7.00%±4.39%). It showed the similar status at the bottom water in the Kelantan River Estuary, where diatoms, Synechococcus and prasinophytes contributed 64.89%±15.29%, 16.23%±9.98% and 8.91%±2.62%, respectively. The different phytoplankton community composition between the two regions implied that the bottom up control affected the phytoplankton biomass in the Lembeh Strait where the oligotrophic water derived from the West Pacific Ocean. The terrigenous nutrients supplied the diatoms growing, and pico-phytoplankton was grazed through top down control in the Kelantan River Estuary.
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