RÉSUMÉLa réponse de juvéniles de saumon aux fortes baisses de niveau caractéristiques de l'étiage n'est pas bien connue. Trois expériences ont été menées en fin d'été dans un ruisseau artificiel comportant des séries de 3 biefs (10 m x 3 m) constitués d'amont en aval de séquences d'habitat radier, plat, profond. En eau profonde, les tacons ne réagissent pas aux baisses de niveau et de débit. Dans les eaux peu profondes, ils réduisent leur activité, en particulier alimentaire, et dans des conditions critiques, une partie de la population se déplace vers la plus proche zone profonde. Les autres s'enfouissent dans le substrat. Après la montée du débit, une partie des dévalants retourne dans l'habitat radier.
INFLUENCE OF DEWATERING ON MOVEMENTS AND DISTRIBUTION OF SALMON PARR {SALMO SALAR L.) IN RELATION TO HABITAT CHARACTERISTICS IN AN EXPERIMENTAL STREAM.
ABSTRACTThe response of Atlantic salmon parr to major decreases in water levels, typical of summer low flows, is not well documented. Three experiments were conducted in an artificial stream designed with séquences of riffle, flat, and pool habitat, each habitat in a section 10 m long by 3 m wide. In deeper water, parr did not respond to water level or flow decrease. In shallow water, they reduced activity, particularly feeding, and in critical conditions a portion of the population moved into deeper water. The remainder of the parr buried themselves into the gravel. After flow increase, some of the downstream moving parr returned to the riffle habitat.
INTRODUCTIONIn Spring, after émergence from the redd, fry of Atlantic salmon (SaImo salar L.) disperse in the nursery habitat. This dispersai, which may be extensive, lasts for a few weeks, but after early dispersion the salmon juvéniles are supposed to be sedentary at least until October (SAUNDERS & GEE, 1969 ;BEALL et al., 1994a). Changes in water conditions often occur during the summer months, usually with a period of low flows in mid to late summer. Reduced flows resuit in lower current velocity and depth, decreased availability of habitat and higher températures. According to BINNS & EISERMAN (1979), if the average late summer stream flow falls below 10-15 % of the yearly average, trout populations cannot be supported. Occasionnally in streams with dense populations of salmonids, there may be brief but drastic decreases of discharge which cause dewatering of riffles and reduce the stream to a succession of isolated pools.Reactions of salmon parr to thèse changes are not well documented. LINDROTH (1955) noted that salmonid fry tended to move downstream after a decrease in water flow. SAUNDERS & GEE (1969) observed the movement of parr into the nearest pool during a
INFLUENCE DE FORTES VARIATIONS DE NIVEAU EN ÉTIAGE SUR LES MOUVEMENTS ET LA DISTRIBUTION DE SAUMONS ATLANTIQUES JUVENILES (SALMO SALAR L.) EN FONCTION DE L'HABITAT DANS UN RUISSEAU EXPÉRIMENTAL.