Juvenile roach were always more abundant in the less modified section (BPS) of the river than in the other sections (RES and TAIL). While the original primary river channel was directly impacted by the flash flood, no significant difference in otolith shape was observed before or after the flash flood. Our results suggest that this part of the reach provides refuge habitats used by fish during high flow events.
K E Y W O R D SCyprinidae, flood event, Lower Rhône River, otolith morphometry
| INTRODUCTIONThe channelisation and regulation of large rivers have severely impacted fluvial morphology and processes by changing natural hydrological and sedimentary regimes which contribute to the high ecological value of large floodplains (Bravard & Petts, 1996;Poff et al., 1997). The length and habitat heterogeneity of riverine ecotones have been reduced (Schiemer, Zalewski, & Thorpe, 1995;Tockner & Stanford, 2002) and the spatial and temporal patterns of hydrological connectivity have been highly altered (Pringle, 2003;Ward & Stanford, 1995). Populations of highly mobile organisms like fish, which use distinct habitats during their life cycle, have been seriously affected.Major changes in fish assemblages in large European rivers such as the Danube (Balon, Crawford, & Lelek, 1986; Holcik, 1988), the Rhine (Cazemier, 1988;Lelek, 1989) or the Rhône (Pattee, 1988;Persat, 1988) resulted from the 19th century river straightening, the channelisation and the construction of successive diversion dams (mainly during the 20th century) which have created new artificial environments. On the Rhône River, a typical hydropower scheme includes a reservoir (RES) created by the diversion dam built on the upper part of the river, a canal which redirects the main river flow to a power plant, and a bypassed old river that spans for several kilometres. Typically, the tailrace (TAIL) and the bypassed sections (BPS) converge in the downstream RES formed by next diversion dam (see Figure 1). Most of the time, the BPS receives a low minimum instream flow and overflows occur at the dam when river discharge exceeds the capacity of the hydropower plant. However, these released flows (discharge from the dam) are generally lower than the initial discharge prior to the