Species belonging to the genera Alexandrium and Gymnodinium are amongst the dinoflagellates that regularly cause massive coastal phytoplankton blooms along Mediterranean beaches.These episodes encompass a variety of factors favouring bloom development, including near-shore nutrient enrichment, enhanced growth and low water renewal.During the summer of 2003 the development of a bloom was monitored at 2 nearby beaches, Peguera and Santa Ponça, located at the head of Santa Ponça Bay (Mallorca).Both sites are under the influence of the same physical regime -which is mainly wind-forced -and present relatively high inorganic nutrient concentrations for Mediterranean waters during summer (mean dissolved inorganic nitrogen > 1.2 μM and PO 4 > 0.18 μM).Total dinoflagellate abundance exhibited a similar trend at both beaches, with remarkable outbursts in late June (> 8 × 10 6 cells l -1 ).Water exchange calculations, based on 3D numerical modeling, yielded low average renewal rates at both sites (< 0.08 d -1 ), and cell growth estimations suggested a significant increase in the specific growth rates during the blooming season associated with the seasonal temperature variation.We postulate that both the increased growth rates and the low wind-induced water renewal times are complementary factors and are of key relevance to the modulation of these blooms.Diagnostic analyses using a simple phytoplanktonzooplankton (PZ ) model allowed us to observe the effect of growth rate and water renewal on bloom dynamics, and to identify a threshold condition for bloom occurrence.
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Basterretxea et al. (2007) studied this question.
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