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Map of the Garonne River basin indicating the position of the sampling stations and the location of the major cities. 

Map of the Garonne River basin indicating the position of the sampling stations and the location of the major cities. 

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Dissolved nutrient and chlorophyll-a concentrations were monitored on 17 occasions and at 16 sites in the Garonne River (France). Concentrations of dissolved inorganic nitrogen (DIN) and soluble reactive phosphorus (SRP) increased about threefold downstream of the urban area of Toulouse. Chlorophyll-a concentrations increased concomitantly with DIN...

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... a catchment of 57,000 km 2 , the Garonne River basin is the third largest river basin in France after the Rhone and Seine (Fig. 1). The Garonne River is a shal- low river (generally <2 m) and has a high flow velocity, even in its lower reaches (~0.4 m s -1 ). This high flow velocity prevents planktonic algae to attain a high bio- mass (Améziane et al. 2003). Due to an important frac- tion of hard substrates in the river bed, turbidity of the Garonne River is low ...
Context 2
... INTRODUCTION During the 20 th Century, N and P inputs into rivers around the world have increased dramatically as a result of intensive agriculture and industrial and municipal waste water discharges (Meybeck 1982). Increased concentrations of N and P are often accompanied by an increase in algal biomass or eutrophication. In rivers, the effects of eutrophication may be moderate because phytoplankton development is limited by short water retention times rather than inorganic nutrient concentrations. Nevertheless, many studies in different river basins have demonstrated a positive relation between N and P enrichment and algal biomass (e.g., Biggs & Close 1989; Basu & Pick 1996; Van Nieuwenhuyse & Jones 1996; Lohman et al . 1999). N and P have received much attention in eutrophication studies because they are essential nutrients for all phytoplankton groups and because their concentrations are strongly influenced by human activities. Si is only required by a few algal groups and Si concentrations are not directly influenced by human activities. Therefore, Si has historically received much less attention. The predominant source of dissolved silica (DSi) is the natural weathering of silicate minerals (Tréguer et al . 1995). The only significant human source of Si consists of metasilicates, of which small amounts are used in deter- gents and fertiliser. Nevertheless, recent estimates have shown that anthropogenic Si inputs may amount to 6% of total Si inputs in a river basin (Sferratore et al . 2006). The most important algal group that requires Si are the diatoms, who need large amounts of Si for the construc- tion of their cell wall. Compared to other algal groups, diatoms are adapted to low-light conditions (because of the pigment fucoxanthin) and to a turbulent water column (because of their high cell density). Therefore, diatoms are often a dominant component of the phytoplankton of the turbulent and turbid lower reaches of rivers (e.g., Garnier et al . 1995). They are also important primary producers in the shallower, upper reaches of rivers, where they are a dominant component of the phytobenthos. Because of the importance of diatoms in river ecosystems, primary producers have a potentially strong influence on Si concentrations. Due to anthropogenic inputs of N and P, Si:N and Si:P ratio's have decreased in many rivers worldwide (Turner et al . 2003; Billen & Garnier 2007). When Si:N and Si:P ratio's are low, diatom production becomes limited by Si and total consumption of Si increases (Conley et al . 1993). Diatoms convert dissolved Si to biogenic Si or opal, which has a low remineralisation rate and easily accumulates in sediments. Therefore, Si consumption in rivers by diatoms may result in an increased retention of Si and a reduced export of Si to coastal ecosystems. Lower Si inputs in coastal waters have been shown to have an adverse effect on diatom production and to favour nuisance algae over diatoms (Humborg et al . 1997; Ittekkot et al . 2000; Cugier et al . 2005). Most studies on Si retention in river basins have focused on retention of Si in lakes or reservoirs in river basins (e.g., Conley et al . 2000). These studies have shown that production of diatoms in reservoirs or lakes and subsequent burial of biogenic Si in sediments results in reduced dissolved Si transport to coastal sys- tems (e.g., Conley et al . 2000; Humborg et al . 2000), although some of these claims have been refuted by more recent studies (Teodoru et al. 2006). Few studies have investigated the consequences of eutrophication on Si consumption in the river itself. Using an ecosystem model, Billen et al . (2001) demonstrated that increased anthropogenic N and P inputs resulted in increased retention of Si in the Seine River basin over the last 50 years. Here we present monitoring data from the Garonne River that suggest that N and P inputs from the city of Toulouse result in increased consumption of dissolved Si by algae. 2. METHODS With a catchment of 57,000 km 2 , the Garonne River basin is the third largest river basin in France after the Rhone and Seine (Fig. 1). The Garonne River is a shallow river (generally <2 m) and has a high flow velocity, even in its lower reaches (~0.4 m s -1 ). This high flow velocity prevents planktonic algae to attain a high biomass (Améziane et al . 2003). Due to an important frac- tion of hard substrates in the river bed, turbidity of the Garonne River is low compared to other lowland rivers, with suspended matter concentrations usually being below 50 mg L -1 (Coynel et al . 2004). This low turbidity combined with a shallow depth allows diatom biofilms to develop on the river bed (Eulin & Le Cohu 1998; Teissier et al . 2002; Améziane et al . 2003; Boulêtreau et al . 2006). Diatom biofilms regularly detach when their biomass is high and are then mixed into the water column (Boulêtreau et al . 2006). Diatoms from these biofilms make up about half of the cell numbers in phytoplankton samples of the Garonne River (Améziane et al . 2003). Both planktonic and biofilm diatoms may consume Si in the Garonne River. The catchment of the Garonne River is predomi- nantly agricultural and contains only one major urban area, Toulouse. The urban area of Toulouse is situated at the confluence of the Garonne and Ariège rivers and has approximately 1 million inhabitants. The largest tributary of the Garonne River downstream of Toulouse is the Tarn River. In contrast to the Garonne River, the Tarn River has no major urban areas in its catchment. The reservoir of Malause is situated at the confluence of the Garonne and Tarn rivers. The Malause reservoir is a large reservoir with a relatively shallow depth (area: 420 ha, mean depth: 3.6 m). The main goal of this study was to evaluate eutrophication caused by the urban area of Toulouse and the resulting impact on dissolved Si concentrations. Water samples were collected at 16 sites upstream and downstream of the city of Toulouse on 17 occasions between July 1992 to September 1993. Sampling occasions were selected to cover high-discharge as well as low-discharge periods. Water was collected using a bucket from bridges or from the river bank, as close as possible to the centre of the main channel. Temperature was measured in the field using a WTW 96 probe. For determination of chlorophyll- a concentration, a known volume of water was filtered through a GF/C filter. Chlorophyll- a was extracted in boiling ethyl alcohol and quantified spectrophotometrically (Marker et al . 1980). For determination of dissolved nutrients, water was filtered through GF/F filters and stored at 4 °C until analy- sis (within 48 hours). Nitrate, nitrite and silica concentrations were measured with a Technicon autoanalyser. Nitrite was determined using the diazotation method, nitrate was determined by cadmium reduction into nitrite and dissolved silica (DSi) was determined by the ammonium molybdate method (APHA 1985). Ammo- nium was measured spectrophotometrically by the indophenol blue method according to Scheiner (1976). Solu- ble reactive phosphorus (SRP) was determined spectrophotometrically with the molybdate and malachite green method (Motomizu et al . 1983). Dissolved inorganic nitrogen (DIN) was calculated as the sum of ammonium, nitrate and nitrite. Determination of solid par- ticulate matter (SPM) concentrations was performed by filtration using dry pre-weighed filters (Whatman GF/F, 0.7 μm). Daily discharge data for the Garonne (at Ver- dun) and Tarn (at Moissac) rivers were provided by water authorities (DIREN Midi-Pyrenees and CA des Coteaux de Gascogne HYDRO-MEDD/DE). 3. RESULTS Discharge of the Garonne and Tarn rivers upstream of their confluence in the Malause reservoir is shown in figure 2. The Garonne River had a high discharge in late autumn to early winter as well as in spring. Discharge of the Tarn River was comparable to that of the Garonne River in summer and autumn but it was slightly higher than that of the Garonne River in winter and lower in spring. In winter, temperature was below 10 °C throughout the river section under investigation (Fig. 3). In summer, temperature was below 18 °C at the most upstream station sampled but increased up to 28 °C downstream of the confluence of the Garonne and Ariège rivers. SPM concentrations were generally low (<40 mg L -1 ) during the low flow periods in winter to early spring and summer (Fig. 3). Peaks in SPM concentrations were observed during the autumn floods along the entire river section and in late spring in the section downstream of the confluence of the Tarn with the Garonne River. DIN concentrations increased from <1 mg L -1 upstream of Toulouse to >2 mg L -1 downstream of Toulouse (Fig. 4) and concentrations were lower during high discharge periods in winter. SRP concentrations were usually <10 μg L -1 upstream of Toulouse (Fig. 4). Only in late summer 1993, higher SRP were measured upstream of Toulouse. Downstream of Toulouse, SRP increased to >20 μg L -1 . Downstream of the confluence between the Tarn and Garonne rivers, SRP decreased again by ...

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