2009
DOI: 10.1016/j.ecss.2009.05.022
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Particulate suspended matter concentrations in the Bahía Blanca Estuary, Argentina: Implication for the development of phytoplankton blooms

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Cited by 73 publications
(48 citation statements)
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“…On the contrary, it is expected that the turbidity reaches maximum values in spring and summer, when stronger winds blow and maximum significant wave heights are found, producing resuspension and, consequently, an increase of suspended particulate matter (SPM) [71]. Furthermore, in the Bahí a Blanca Estuary, maximum (minimum) SPM concentrations were observed during spring (winter) [72], which is expected to influence zone 1A.…”
Section: Discussionmentioning
confidence: 99%
“…On the contrary, it is expected that the turbidity reaches maximum values in spring and summer, when stronger winds blow and maximum significant wave heights are found, producing resuspension and, consequently, an increase of suspended particulate matter (SPM) [71]. Furthermore, in the Bahí a Blanca Estuary, maximum (minimum) SPM concentrations were observed during spring (winter) [72], which is expected to influence zone 1A.…”
Section: Discussionmentioning
confidence: 99%
“…growth became inhibited at *150 lEm -2 s -1 under laboratory conditions (Popovich and Gayoso 1999). In addition, seasonal variability in water turbidity was not noticed in previous years (Popovich and Marcovecchio 2008) whereas in 2007, the winter phytoplankton bloom (dominated by Chaetoceros sp.1) occurred when water transparency increased as a consequence of significant shifts in wind effect (Guinder et al 2009). Similarly, in the Narragansett Bay (USA), changes in the phytoplankton annual pattern over the last 50 years (i.e.…”
Section: Underwater Light Conditionsmentioning
confidence: 96%
“…In temperate lakes (Reynolds 2006), oceans (Longhurst 1995) and coastal basins (Longhurst 1995;Li et al 2010), a secondary bloom in autumn is often fuelled by transport of nutrientrich deep waters to the surface as stratification is eroded by surface cooling and convective mixing. Further, in turbid estuaries where phytoplankton is controlled by light availability, winter blooms can be triggered by increasing solar penetration caused by a reduction of suspended sediments owing to low river inflow or reduced wind stress (Guinder et al 2009). Similar to the unimodal patterns, these bimodal patterns are highly variable and secondary blooms may not appear regularly.…”
Section: Annual Cycles Of Phytoplankton Biomassmentioning
confidence: 99%