2004
DOI: 10.1016/j.ecss.2004.05.007
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Spring phytoplankton of Rı́o de la Plata: a temperate estuary of South America

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Cited by 42 publications
(34 citation statements)
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“…twofold higher at the most polluted area of the estuary. Nonetheless, our estimations are lower than those reported for the freshwater tidal zone (56x10 3 pg C mL -1 ) as well as the mixohaline zone (231x10 3 pg C mL -1 ) of the Río de la Plata estuary (Gómez et al, 2004). The nanophytoplankton biomass, mostly comprised of small diatoms and cyanobacteria, represented a large proportion (84%) of the total phytoplankton biomass.…”
Section: Discussioncontrasting
confidence: 53%
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“…twofold higher at the most polluted area of the estuary. Nonetheless, our estimations are lower than those reported for the freshwater tidal zone (56x10 3 pg C mL -1 ) as well as the mixohaline zone (231x10 3 pg C mL -1 ) of the Río de la Plata estuary (Gómez et al, 2004). The nanophytoplankton biomass, mostly comprised of small diatoms and cyanobacteria, represented a large proportion (84%) of the total phytoplankton biomass.…”
Section: Discussioncontrasting
confidence: 53%
“…We also observed that phytoplankton density was higher at the most polluted area. Nevertheless, our estimation was twentyfold higher than the highest density observed by Gómez et al (2004), three-times higher than that estimated by Gómez and Bauer (1998), and about thirtyfold higher than the average value estimated for the other eleven sites in this study. In contrast, the density was lower in the outer portion of the estuary mouth, where the salinity level was higher.…”
Section: Discussioncontrasting
confidence: 49%
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“…Both studies emphasized the large proportion and long survival of diatoms in rivers compared with lakes. Moreover, other algae such as flagellates (Cloern et al, 1983;De Oliveira and Calheiros, 2000;Gómez et al, 2004), filamentous cyanobacteria (Köhler and Hoeg, 2000), non-diatoms that indicate altered conditions (Mihaljević et al, 2013), are also important. The composition and persistence of potamoplankton assemblages in riverine ecosystems mainly depend on physical (light, water temperature, and turbidity) and hydrological factors (discharge, flow velocity, water level, suspended sediment concentration and water residence time) (Köhler, 1993;Gosselain et al, 1994;Kirk, 1994;Reynolds et al, 1994;Reynolds and Descy, 1996;Train and Rodrigues, 1997;Centis et al, 2010;Salmaso and Zignin, 2010), and resolved silicate concentration (Dortch and Whitledge, 1992;Tavernini et al, 2011).…”
Section: Introductionmentioning
confidence: 99%