Abstract

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 Ponca, located at the head of Santa Ponca Bay (Mallorca). Both sites are under the influence of the same physical regime — which is mainly wind-forced — and present relatively high inorganic nutrient con- centrations for Mediterranean waters during summer (mean dissolved inorganic nitrogen > 1.2 μM and PO4 > 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 esti- mations 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 phytoplankton- zooplankton (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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