4.6 Article

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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ESTUARINE COASTAL AND SHELF SCIENCE
卷 61, 期 1, 页码 137-149

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ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
DOI: 10.1016/j.ecss.2004.04.010

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estuaries; hypoxia; microalgae; nutrients; picoplankton; seasonal; south Florida

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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. Watercolumn chlorophyll a concentrations reached up to 29 mug 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. (C) 2004 Elsevier Ltd. All rights reserved.

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