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      The upper temperature and hypoxia limits of Atlantic salmon ( Salmo salar) depend greatly on the method utilized

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          ABSTRACT

          In this study, Atlantic salmon were: (i) implanted with heart rate ( f H) data storage tags (DSTs), pharmacologically stimulated to maximum f H, and warmed at 10°C h −1 (i.e. tested using a ‘rapid screening protocol’); (ii) fitted with Doppler ® flow probes, recovered in respirometers and given a critical thermal maximum (CT max) test at 2°C h −1; and (iii) implanted with f H DSTs, recovered in a tank with conspecifics for 4 weeks, and had their CT max determined at 2°C h −1. Fish in respirometers and those free-swimming were also exposed to a stepwise decrease in water oxygen level (100% to 30% air saturation) to determine the oxygen level at which bradycardia occurred. Resting f H was much lower in free-swimming fish than in those in respirometers (∼49 versus 69 beats min −1) and this was reflected in their scope for f H (∼104 versus 71 beats min −1) and CT max (27.7 versus 25.9°C). Further, the Arrhenius breakpoint temperature and temperature at peak f H for free-swimming fish were considerably greater than for those tested in the respirometers and given a rapid screening protocol (18.4, 18.1 and 14.6°C; and 26.5, 23.2 and 20.2°C, respectively). Finally, the oxygen level at which bradycardia occurred was significantly higher in free-swimming salmon than in those in respirometers (∼62% versus 53% air saturation). These results: highlight the limitations of some lab-based methods of determining f H parameters and thermal tolerance in fishes; and suggest that scope for f H may be a more reliable and predictive measure of a fish's upper thermal tolerance than their peak f H.

          Abstract

          Summary: Heart rate responses to environmental challenges in free-swimming salmon are different from those measured using more invasive techniques. This has important implications for predicting the susceptibility of fishes to climate change.

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          Most cited references126

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          Ecology. Physiology and climate change.

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            Climate change affects marine fishes through the oxygen limitation of thermal tolerance.

            A cause-and-effect understanding of climate influences on ecosystems requires evaluation of thermal limits of member species and of their ability to cope with changing temperatures. Laboratory data available for marine fish and invertebrates from various climatic regions led to the hypothesis that, as a unifying principle, a mismatch between the demand for oxygen and the capacity of oxygen supply to tissues is the first mechanism to restrict whole-animal tolerance to thermal extremes. We show in the eelpout, Zoarces viviparus, a bioindicator fish species for environmental monitoring from North and Baltic Seas (Helcom), that thermally limited oxygen delivery closely matches environmental temperatures beyond which growth performance and abundance decrease. Decrements in aerobic performance in warming seas will thus be the first process to cause extinction or relocation to cooler waters.
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              Marine heatwaves under global warming

              Marine heatwaves (MHWs) are periods of extreme warm sea surface temperature that persist for days to months1 and can extend up to thousands of kilometres2. Some of the recently observed marine heatwaves revealed the high vulnerability of marine ecosystems3-11 and fisheries12-14 to such extreme climate events. Yet our knowledge about past occurrences15 and the future progression of MHWs is very limited. Here we use satellite observations and a suite of Earth system model simulations to show that MHWs have already become longer-lasting and more frequent, extensive and intense in the past few decades, and that this trend will accelerate under further global warming. Between 1982 and 2016, we detect a doubling in the number of MHW days, and this number is projected to further increase on average by a factor of 16 for global warming of 1.5 degrees Celsius relative to preindustrial levels and by a factor of 23 for global warming of 2.0 degrees Celsius. However, current national policies for the reduction of global carbon emissions are predicted to result in global warming of about 3.5 degrees Celsius by the end of the twenty-first century16, for which models project an average increase in the probability of MHWs by a factor of 41. At this level of warming, MHWs have an average spatial extent that is 21 times bigger than in preindustrial times, last on average 112 days and reach maximum sea surface temperature anomaly intensities of 2.5 degrees Celsius. The largest changes are projected to occur in the western tropical Pacific and Arctic oceans. Today, 87 per cent of MHWs are attributable to human-induced warming, with this ratio increasing to nearly 100 per cent under any global warming scenario exceeding 2 degrees Celsius. Our results suggest that MHWs will become very frequent and extreme under global warming, probably pushing marine organisms and ecosystems to the limits of their resilience and even beyond, which could cause irreversible changes.

                Author and article information

                Contributors
                Journal
                J Exp Biol
                J Exp Biol
                JEB
                The Journal of Experimental Biology
                The Company of Biologists Ltd
                0022-0949
                1477-9145
                15 September 2023
                26 September 2023
                26 September 2023
                : 226
                : 18
                : jeb246227
                Affiliations
                Department of Ocean Sciences, Memorial University of Newfoundland and Labrador , St John's, NL, Canada, A1C 5S7
                Author notes
                [* ]Authors for correspondence ( r.sandrelli@ 123456mun.ca , kgamperl@ 123456mun.ca )

                Competing interests

                The authors declare no competing or financial interests.

                Author information
                http://orcid.org/0000-0001-5433-5058
                http://orcid.org/0000-0002-9852-4819
                Article
                JEB246227
                10.1242/jeb.246227
                10560559
                37622446
                36289167-ad06-4778-b744-3d04a0c23e47
                © 2023. Published by The Company of Biologists Ltd

                This is an Open Access article distributed under the terms of the Creative Commons Attribution License ( https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution and reproduction in any medium provided that the original work is properly attributed.

                History
                : 1 June 2023
                : 17 August 2023
                Funding
                Funded by: Natural Sciences and Engineering Research Council of Canada, http://dx.doi.org/10.13039/501100000038;
                Award ID: 2016-0448
                Funded by: Memorial University of Newfoundland, http://dx.doi.org/10.13039/501100005616;
                Categories
                Research Article

                Molecular biology
                ctmax,thermal tolerance,heart rate,hypoxia tolerance,data loggers,bradycardia
                Molecular biology
                ctmax, thermal tolerance, heart rate, hypoxia tolerance, data loggers, bradycardia

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