Zhou Weihua, Gao Jie, Liao Jianzu, Shi Ronggui, Li Tao, Guo Yajuan, Long Aimin
Key Laboratory of Tropical Marine Bio-resources and Ecology, and Guangdong Provincial Key Laboratory of Applied Marine Biology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China.
Tropical Marine Biological Research Station in Hainan, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Sanya, China.
PLoS One. 2016 Dec 1;11(12):e0167630. doi: 10.1371/journal.pone.0167630. eCollection 2016.
In recent decades, increasing frequency and intensity of saltwater intrusion in the Modaomen Channel has threatened the freshwater supply in the surrounding cities of the Pearl River Estuary, and ulteriorly changed the environmental conditions of the estuarine waters. Phytoplankton biomass, primary production (PP) and species composition, as well as hydrological and chemical parameters were examined along a downstream transect in the Modaomen Channel during neap tide (NT) and spring tide (ST), when a strong saltwater intrusion event occurred in late September, 2011. A total of 46 species phytoplankton were identified, including Bacillariophyta (25 species), Dinoflagellate (14 species), Chlorophyta (4 species), Cyanophyta (2 species) and Euglenozoa (1 species). The dominant species were shifted from freshwater diatoms (e.g., Melosira granulata and Melosira granulata var. angustissima) in the upper reaches to saline water diatoms (e.g., Skeletonema costatum and Coscinodiscus sp.) in the river mouth. Generally, phytoplankton density, biomass (chl-a) and PP decreased from the upper to lower reaches along the channel, and were significantly higher in NT than those of ST. There was a shift from large-sized phytoplankton (>20 μm) in the upper reaches to relative small-sized cells (5-20 μm) in the lower reaches. Compared to NT, low discharge and flow velocity, coupled with strong easterly winds during ST specially aggravated saltwater intrusion further to the upstream (~50 km from the estuary). The intruded saltwater diluted nutrients, N/P ratios, chl-a, and phytoplankton abundances, and thereby led to a decline in PP during ST.
近几十年来,磨刀门水道咸潮入侵频率和强度不断增加,威胁着珠江口周边城市的淡水供应,并进而改变了河口海域的环境条件。在2011年9月下旬发生强烈咸潮入侵事件的小潮(NT)和大潮(ST)期间,沿着磨刀门水道下游断面,对浮游植物生物量、初级生产力(PP)和物种组成,以及水文和化学参数进行了调查。共鉴定出46种浮游植物,包括硅藻门(25种)、甲藻门(14种)、绿藻门(4种)、蓝藻门(2种)和眼虫藻门(1种)。优势种从上游的淡水硅藻(如颗粒直链藻和窄隙直链藻变种)转变为河口的咸水硅藻(如中肋骨条藻和圆筛藻属)。总体而言,浮游植物密度、生物量(叶绿素a)和PP沿水道从上游到下游逐渐降低,且小潮时显著高于大潮。存在从上游大型浮游植物(>20μm)到下游相对小型细胞(5-20μm)的转变。与小潮相比,大潮期间低流量和流速,再加上强劲的东风,特别加剧了咸潮向上游的入侵(距离河口约50公里)。入侵的咸水稀释了营养物质、氮磷比、叶绿素a和浮游植物丰度,从而导致大潮期间PP下降。