洞头海域网采浮游植物的月际变化
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国家海洋局第二海洋研究所 国家海洋局海洋生态系统与生物地球化学重点实验室 杭州,国家海洋局第二海洋研究所 国家海洋局海洋生态系统与生物地球化学重点实验室 杭州,国家海洋局第二海洋研究所 国家海洋局海洋生态系统与生物地球化学重点实验室 杭州,国家海洋局第二海洋研究所 国家海洋局海洋生态系统与生物地球化学重点实验室 杭州,国家海洋局第二海洋研究所 国家海洋局海洋生态系统与生物地球化学重点实验室 杭州,国家海洋局第二海洋研究所 国家海洋局海洋生态系统与生物地球化学重点实验室 杭州,浙江省海洋水产养殖研究所 温州,国家海洋局第二海洋研究所 国家海洋局海洋生态系统与生物地球化学重点实验室 杭州;浙江省海洋水产养殖研究所 温州

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国家重点基础研究发展规划项目(2010CB428903);海洋公益性行业科研专项(200805069,201305009,2013418009);浙江省自然科学基金(Y5110131);浙江省海水养殖重点科技创新团队项目(2010R50025);国家自然科学科学基金(41176142,41206103);中国博士后科学基金(20110491828)和国家海洋局第二海洋研究所基本科研业务费专项(JG1222,JT0806)


Monthly variation of net-phytoplankton composition in Dongtou Island
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Key Laboratory of Marine Ecosystem and Biogeochemistry,Second Institute of Oceanography,Key Laboratory of Marine Ecosystem and Biogeochemistry,Second Institute of Oceanography,Key Laboratory of Marine Ecosystem and Biogeochemistry,Second Institute of Oceanography,Key Laboratory of Marine Ecosystem and Biogeochemistry,Second Institute of Oceanography,Key Laboratory of Marine Ecosystem and Biogeochemistry,Second Institute of Oceanography,Key Laboratory of Marine Ecosystem and Biogeochemistry,Second Institute of Oceanography,Zhejiang Mariculture Research Institute,Key Laboratory of Marine Ecosystem and Biogeochemistry,Second Institute of Oceanography;China;Zhejiang Mariculture Research Institute;China

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    摘要:

    通过2010年8月至2011年7月对洞头海域网采浮游植物的逐月调查,共鉴定出浮游植物5门187种,主要由硅藻(143种)和甲藻(40种)组成,金藻、绿藻和蓝藻偶有检出。全年共发现20种优势种,其中硅藻16种,甲藻3种,蓝藻1种。浮游植物丰度、种类数、Shannon-Wiener指数(H')和Pielou均匀度指数(J)月变化均较大。典范对应分析(CCA)显示,影响浮游植物群落的主要因子为溶解硅(DSi)、溶解无机氮(DIN)、氮磷比(N:P)、溶解无机磷(DIP)、硅磷比(Si:P)、盐度和温度。台湾暖流、闽浙沿岸流和瓯江径流也是影响本海域浮游植物变化的重要因素:6-9月,台湾暖流影响较大,调查海域外海暖水性种类增多;其他各月闽浙沿岸流和瓯江径流影响较大,调查海域既有近岸低盐种类,也有半咸水、淡水种类。结合历史数据分析表明,近30年来洞头海域营养盐结构已经发生较大变化,表现为硝酸盐浓度急剧升高,由1981-1982年的12.89 μmol/L升至2010-2011年的52.63 μmol/L,N:P由19.1:1升至51.8:1。同时浮游植物群落也有较大改变,表现为浮游植物细胞丰度的增加(由5.8×105 个/m3上升至39.2×106 个/m3)和优势种的更替(由圆筛藻Coscinodiscus spp.向骨条藻Skeletonema spp.演替)。

    Abstract:

    As the basic status and function in marine food chains, phytoplankton plays an important role in dynamics of material and energy fluxes. Dongtou Island (121°10'E, 27°50'N), located at the southeast coast of Zhejiang Province, is the confluence of the Wenzhou Bay and Yueqing Bay mouths. The development of water eutrophication and frequent occurrence of harmful algae blooms (HABs) events at some sea area of Dongtou Island have been observed in recent years. However, report about the relationships between the environmental factors and the phytoplankton community at sea area of Dongtou Island is rare. To understand the response of phytoplankton to environmental changes, an annual investigation was carried out at the northeast sea area of Dongtou Island.
    Seven net-phytoplankton samples were collected from the studied area once a month during August 2010 to July 2011 for understanding the monthly variation of phytoplankton and the relationship between the community structures and the environmental factors. A total of 5 phyla and 187 species were identified, including 143 diatom species, 40 dinoflagellate species and other 4 taxonomic (Chrysophyta, Cyanophyta and Chlorophyta) species. Twenty dominant species consisted of 16 diatom species, 3 dinoflagellate species and 1 Cyanophyta were observed all year round. The monthly phytoplankton community parameters (abundance, species number, Shannon-Wiener diversity and Pielou evenness) varied greatly. Canonical correspondence analysis (CCA) indicated that the DSi, DIN, N:P, DIP, Si:P, salinity and temperature were the main factors influencing the phytoplankton community. Compared to diatoms, dinoflagellate had a stronger response to the P concentration. The growth of dinoflagellate species was enhanced when the P concentration increased. The phytoplankton composition was also profoundly controlled by the Taiwan Warm Current (TWC), Fujian-Zhejiang Coastal Current (FZCC), and runoff from Oujiang River (OR). From July to September, warm-water species such as Cerataulina pelagic, Chaetoceros pseudocurvisetus and C. distans increased significantly as the TWC intruded (with the salinity of 29.8-30.1). In other months, the phytoplankton composition was mainly influenced by the FZCC and OR runoff. Consequently, all the coastal (with the salinity of 26.8-28.6), brackish and freshwater phytoplankton species such as Prorocentrum triestinum, Ditylum brightwellii, Pediastrum duplex var. echinatum and Synedra sp. increased clearly. Since 1980's, the environmental conditions at the studied area had changed obviously: concentrations of NO3--N dramaticly increased from 12.89 μmol/L in 1981-1982 to 52.63 μmol/L in 2010-2011; and N:P ratio also increased from 19.1:1 in 1981-1982 to 51.8:1 in 2010-2011. The structure of phytoplankton community has also experienced obvious variation since 1980. The cells abundance increased from 5.8×105 cells/m3 in 1981-1982 to 39.2×106 cells/m3 in 2010-2011, and dominant species (Coscinodiscus spp. was replaced by Skeletonema spp.) of phytoplankton were also changed a lot.

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朱旭宇,黄伟,曾江宁,江志兵,杜萍,廖一波,张鹏,陈全震.洞头海域网采浮游植物的月际变化.生态学报,2013,33(11):3351~3361

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