Physiological responses of rainbow trout Salmo gairdneri exposed to plastic lake inlet and outlet stream waters

1986 ◽  
Vol 30 (3-4) ◽  
pp. 687-694 ◽  
Author(s):  
H. H. Harvey ◽  
J. M. McArdle
1980 ◽  
Vol 88 (1) ◽  
pp. 109-132
Author(s):  
D. G. McDONALD ◽  
H. HŌBE ◽  
C. M. WOOD

The physiological responses of 1- to 2-year-old rainbow trout to low pH are dependent on the environmental calcium concentration. Trout, maintained for 5 days in moderately hard water ([Ca2+] = 1·6–2·7 m-equiv/1) at a mean pH of 4·3, developed a major blood acidosis but exhibited only a minor depression in plasma ion levels. In acidified soft water ([Ca2+] = 0·3 m-equiv/1), only a minor acidosis occurred, but plasma ion levels fell and there were substantially greater mortalities. Lethal bioassays performed on fingerling trout over a range of pH levels (3·0–4·8) revealed an important influence of external [Ca2+] on resistance to acid exposure. Terminal physiological measurements on adult fish succumbing to low pH in soft water indicate the singular importance of iono-regulatory failure as the toxic mechanism of action under these circumstances.


1962 ◽  
Vol 19 (2) ◽  
pp. 201-270 ◽  
Author(s):  
T. G. Northcote

The marked differences in response to water current, exhibited by juvenile rainbow trout migrating into Loon Lake from its outlet and inlet streams, were studied both in the field and in experimental laboratory apparatus. All available evidence argued against genetically discrete outlet and inlet stocks, each maintaining different innate responses to water current. Difference in water temperature between streams was shown, in field and laboratory experiments, to regulate direction of juvenile trout migration through action on behaviour associated with downstream movement, maintenance of position and upstream movement.In laboratory experiments with cool (5 and 10 °C) flowing water, recently emerged fry rarely made contact with the stream bottom in darkness and exhibited much more downstream movement than in warm (> 14 °C) water. In cool streams of the Loon Lake system (daily mean consistently < 13 °C) large numbers of recently emerged fry moved downstream in darkness. Laboratory experiments indicated that combination of cool water (10 °C) and long day length (16 hours) induced downstream movement of fingerlings. In the field, fingerlings moved downstream largely in late spring and summer in cool streams of the Loon Lake system.In laboratory experiments with warm (15 and 20 °C) flowing water, recently emerged fry made frequent contact with the stream bottom in darkness and exhibited much less downstream movement than in cool (10 °C) water. In the warm outlet stream (daily mean in summer usually > 15 °C) recently emerged fry maintained position in darkness. Laboratory experiments suggested that short day length (8 hours) may facilitate maintenance of position exhibited by fingerlings in streams during late autumn and winter.Upstream movement of fry recorded in the field and tested in the laboratory was most pronounced in warm water (> 14 °C). Fingerlings subjected to rapid 5–degree (C) increases in water temperature in an experimental stream exhibited an immediate increase in upstream movement. Upstream movement in summer of large fry and fingerlings occurred only in the warm outlet stream; daily periodicity of upstream movement was positively correlated with sharp rises in water temperature.Evidence examined from four other widely separated stream systems indicated an environmental control of migration in juvenile rainbow trout similar to that demonstrated in the Loon Lake stream system. Possible mechanisms and interaction of factors controlling migratory patterns between and within streams are discussed. Significance of the predominant role played by temperature is considered.


1962 ◽  
Vol 19 (2) ◽  
pp. 173-200 ◽  
Author(s):  
G. F. Hartman ◽  
T. G. Northcote ◽  
C. C. Lindsey

Rainbow trout (Salmo gairdneri) entering and leaving inlet and outlet spawning streams were trapped and marked during three years. Spawners entered the outlet stream at approximately the same time each year despite considerable differences in time of lake ice breakup. Spawners entered the inlet stream 3 to 5 weeks later than outlet spawners and at water temperatures several degrees higher. The inlet spawning run was later in years when disappearance of lake ice was delayed. Comparative statistics are presented on size, sex ratio, survival and diel movement of spawners in both streams. Effects of several types of marking were compared; removal of adipose fins produced much lower mortality than tagging with Petersen discs. In the outlet stream an inverse correlation existed between number of spawners and survival, condition, and length of stay of spawners in the stream. Factors which may be responsible for differences in timing of spawning migrations are discussed.


1979 ◽  
Vol 83 (1) ◽  
pp. 193-202
Author(s):  
R. N. BATH ◽  
F. B. EDDY

Physiological responses of rainbow trout (mean weight 13.3 g) to sudden changes in salinity were investigated. An initial period lasting about 8 h was characterized by increased drinking and an increase in plasma and body ions. Fish failed to survive more than 2 days in full strength sea water but in two-thirds sea water there were few mortalities and adaptation was complete in 7–10 days. During this period there were gradual physiological changes resulting in normal plasma ion concentrations but significantly increased body ionic content. The intracellular concentrations of muscle chloride showed the greatest increase.


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