首页> 外文期刊>Estuarine Coastal and Shelf Science >Intra-annual variability of water quality and phytoplankton in the North Fork of the St. Lucie River Estuary, Florida (USA): a quantitative assessment
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Intra-annual variability of water quality and phytoplankton in the North Fork of the St. Lucie River Estuary, Florida (USA): a quantitative assessment

机译:美国佛罗里达州圣露西河河口北叉水质和浮游植物的年内变化:定量评估

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摘要

Water quality and phytoplankton were examined within the North Fork of the St. Lucie River Estuary, Florida (USA) from March 2000 to March 2001. Alterations in water-quality parameters and phytoplankton assemblages mirrored salinity regimes resulting from the 'wet'/'dry' seasonality of south Florida. Salinity was greatest during the 'dry', winter months whereas water temperature and nitrogen and phosphorus concentrations were greatest during the 'wet', summer months. A seasonal dissimilarity in phytoplankton occurred; cell abundance of cyanobacterial picoplankton (Synechocystis sp., Synechococcus sp.) and a diatom (Skeletonema costatum (Greville) Cleve) and cell carbon of a dinoflagellate (Gyrodinium sp.) and S. costatum were greatest during summer whereas abundance of chrysophytes (Chrysochromulina parva Lackey, Chromulina sp.) and carbon of dinoflagellates (Gymnodinium spp., Heterocapsa rotundata (Lohmann) Hansen) and a diatom (Cyclotella sp.) were greatest during winter. Water-column chlorophyll a concentrations reached up to 29 μg L~(-1) and were negatively associated with salinity. Diatom chlorophyll comprised the majority and at times, greater than 90% of the total chlorophyll a. Picoplanktonic cyanobacteria comprised up to 5% and 1.4% of total phytoplankton carbon and chlorophyll a, respectively throughout the estuary; as such, its impact on overall assemblage rate processes and system-level function appeared minimal. Sediment and whole-water incubations confirmed the presence of heterotrophic dinoflagellates within the estuary. Dissolved oxygen concentrations did not correspond with total chlorophyll a concentrations and salinity, indicating that hypoxia within bottom waters during summer was not solely attributable to phytoplankton biomass or water-column stratification but likely, a result of multiple, interacting physical/chemical and biological factors.
机译:2000年3月至2001年3月,在美国佛罗里达州圣露西河河口北叉内检查了水质和浮游植物。水质参数和浮游植物组合的变化反映了“干” /“干”导致的盐度变化佛罗里达州南部的季节性。在冬季的“干燥”月份,盐度最大,而在夏季的“潮湿”月份,水温,氮和磷的浓度最大。浮游植物出现季节性差异;夏季,蓝藻微微浮游生物(Synechocystis sp。,Synechococcus sp。)和硅藻(Skeletonema costatum(Greville)Cleve)的细胞丰度和单鞭毛酸盐(Gyrodinium sp。)和肋骨链球菌的细胞碳在夏季最高,而金藻(Chrysochromate)(Chrysochromus)丰富在冬季,parva Lackey,Chromulina sp。)和鞭毛藻(Gymnodinium spp。,Heptocapsa rotundata(Lohmann)Hansen)和硅藻(Cyclotella sp。)的碳含量最高。水柱叶绿素a的浓度高达29μgL〜(-1),与盐度呈负相关。硅藻叶绿素占总叶绿素a的大部分,有时甚至超过90%。整个河口的浮游蓝藻分别占浮游植物总碳和叶绿素a的5%和1.4%。因此,它对整体装配速度过程和系统级功能的影响似乎很小。沉积物和全水培养证实了河口内存在异养鞭毛藻。溶解氧浓度与总叶绿素a浓度和盐度不符,这表明夏季底部水域内的缺氧不仅是由于浮游植物生物量或水柱分层引起的,而且可能是多种相互作用的物理/化学和生物学因素共同作用的结果。

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