Corresponding autor: vguinder@criba.edu.ar Hydrological processes such as advection, resuspension, estuarine circulation, internal waves, tidal stirring, vertical mixing and stratification are the main physical forces affecting the phytoplankton distribution in estuaries (DENMAN; GARGETT, 1983; CLOERN et al., 1989; CUSHING 1989; DE JONGE; VAN BEUSEKOM, 1992). Vertical and horizontal transport of phytoplankton in coastal areas could be induced by winds, water mass intrusions from the open sea, turbulence, freshwater inflow and tides (CLOERN et al., 1989; LI; SMAYDA, 2001; BRUNET; LIZON, 2003; HAGY III et al., 2005; POPOVICH; MARCOVECCHIO, 2008; POPOVICH et al., 2008b) and these sorts of transport are related to biomass accumulation and dispersion. Many studies have revealed intratidal variations in phytoplankton dynamics (e.g. DEMERS; LEGENDRE, 1979; DEMERS et al., 1986; DUSTAN; PINCKNEY, 1989; BRUNET; LIZON, 2003) and even differences in biomass between micro and macrotidal estuaries (MONBET, 1992). Moreover, phytoplankton patchiness in estuaries has been associated with the physical influence of tides (DUSTAN; PINCKNEY, 1989). In estuaries characterized by high-tidal energy, a steady phytoplankton composition over short time periods might be expected owing to the intense mixing processes continuously occurring in the water column. However, heterogeneous distributions of phytoplankton cells in the water column on different temporal and spatial scales have been observed (e.g. CUSHING, 1989; BRUNET; LIZON, 2003). Many studies have used the biomass (estimated by the chlorophyll a concentration) as the main intrinsic property to describe the phytoplankton community dynamics during tidal cycles (DENMAN, 1977; FRECHETTE; LEGENDRE, 1982, CLOERN et al., 1989; DUSTAN; PINCKNEY, 1989; MONBET 1992), without taking into consideration the species-specific patterns related to these regular short-time events. Hence, studies based only on phytoplankton biomass variability throughout tidal cycles may overlook the short-term temporal changes in the species composition. The Bahia Blanca Estuary constitutes a mesotidal system with a semidiurnal cycle, the tides being the single most important input of energy (PERILLO; PICCOLO, 1991; PERILLO et al., 2004). The temporal and spatial dynamics of the phytoplankton in the estuary have been extensively studied (GAYOSO, 1998, 1999; POPOVICH; MARCOVECCHIO, 2008; POPOVICH et al. 2008a, 2008b) but none of these works has considered the short-term variability associated with the tidal cycle. The main goal of this study was to describe the temporal phytoplankton and physico-chemical dynamics over a short-time period at a fixed station under strong tidal influence. This study presents the first integrated description of daily phytoplankton-community dynamics together with physical and chemical variables in the Bahia Blanca Estuary. Beside its local relevance, it is also a contribution to the understanding of the short-term variability in estuaries characterized by high tidal energy. Bahia Blanca is a coastal plain estuary (38°45´S; 62°22´W) on the Atlantic coast of Argentina (Fig. 1). Tidal currents are reversible with maximum surface velocities of about 1.3 m s
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