scholarly journals Hypoxia during incubation does not affect aerobic performance or haematology of Atlantic salmon (Salmo salar) when re-exposed in later life

2019 ◽  
Vol 7 (1) ◽  
Author(s):  
Andrew T Wood ◽  
Sarah J Andrewartha ◽  
Nicholas G Elliott ◽  
Peter B Frappell ◽  
Timothy D Clark

Abstract Hypoxia in aquatic ecosystems is becoming increasingly prevalent, potentially reducing fish performance and survival by limiting the oxygen available for aerobic activities. Hypoxia is a challenge for conserving and managing fish populations and demands a better understanding of the short- and long-term impacts of hypoxic environments on fish performance. Fish acclimate to hypoxia via a variety of short- and long-term physiological modifications in an attempt to maintain aerobic performance. In particular, hypoxia exposure during early development may result in enduring cardio-respiratory modifications that affect future hypoxia acclimation capacity, yet this possibility remains poorly investigated. We incubated Atlantic salmon (Salmo salar) in normoxia (~100% dissolved oxygen [DO, as percent air saturation]), moderate hypoxia (~63% DO) or cyclical hypoxia (100–25% DO daily) from fertilization until 113 days post-fertilization prior to rearing all groups in normoxia for a further 8 months. At ~11 months of age, subsets of each group were acclimated to hypoxia (50% DO) for up to 44 days prior to haematology, aerobic metabolic rate and hypoxia tolerance measurements. Hypoxia exposure during incubation (fertilization to 113 days post-fertilization) did not affect the haematology, aerobic performance or hypoxia tolerance of juvenile salmon in later life. Juveniles acclimated to hypoxia increased maximum aerobic metabolic rate and aerobic scope by ~23 and ~52%, respectively, when measured at 50% DO but not at 100% DO. Hypoxia-incubated juveniles also increased haematocrit and haemoglobin concentration but did not affect acute hypoxia tolerance (critical oxygen level and DO at LOE). Thus, while Atlantic salmon possess a considerable capacity to physiologically acclimate to hypoxia by improving aerobic performance in low oxygen conditions, we found no evidence that this capacity is influenced by early-life hypoxia exposure.

2017 ◽  
Vol 90 (4) ◽  
pp. 494-501 ◽  
Author(s):  
Andrew T. Wood ◽  
Timothy D. Clark ◽  
Sarah J. Andrewartha ◽  
Nicholas G. Elliott ◽  
Peter B. Frappell

Aquaculture ◽  
2013 ◽  
Vol 388-391 ◽  
pp. 8-13 ◽  
Author(s):  
Dean Basic ◽  
Åshild Krogdahl ◽  
Joachim Schjolden ◽  
Svante Winberg ◽  
Marco A. Vindas ◽  
...  

2021 ◽  
Vol 94 (1) ◽  
pp. 1-11
Author(s):  
Kirt L. Onthank ◽  
Lloyd A. Trueblood ◽  
Taylir Schrock-Duff ◽  
Lydia G. Kore

Aquaculture ◽  
2021 ◽  
pp. 737670
Author(s):  
Lene Moltumyr ◽  
Jonatan Nilsson ◽  
Angelico Madaro ◽  
Tore Seternes ◽  
Fredrik Agerup Winger ◽  
...  

2004 ◽  
Vol 61 (12) ◽  
pp. 2392-2400 ◽  
Author(s):  
Francis Juanes ◽  
Stephen Gephard ◽  
Kenneth F Beland

The Connecticut River historically represented the southernmost extent of the North American range of Atlantic salmon (Salmo salar), but the native population was extirpated 200 years ago by dam construction. An extensive restoration effort has relied upon stock transfers from more northerly rivers, especially the Penobscot River (Maine). Recent work has shown differences in age structure between donor and derivative populations. Here we focus on a related life-history trait, the timing of the adult migration. We examined 23 years of migration timing data collected at two capture locations in the Connecticut River drainage. We found that both dates of first capture and median capture dates have shifted significantly earlier by about 0.5 days·year–1. To conclude whether this is a consequence of local adaptation or a coast-wide effect, we also quantified changes in migration timing of more northerly stocks (in Maine and Canada). We found that the changes in migration timing were not unique to the Connecticut River stock and instead observed coherent patterns in the shift towards earlier peak migration dates across systems. These consistent shifts are correlated with long-term changes in temperature and flow and may represent a response to global climate change.


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