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      Acute and chronic cold exposure differentially affect cardiac control, but not cardiorespiratory function, in resting Atlantic salmon (S almo salar)

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          Abstract

          No studies have examined the effects of cold temperatures (∼0–1 °C) on in vivo cardiac function and control, and metabolism, in salmonids. Thus, we examined: 1) how acclimation to 8 °C vs. acclimation (>3 weeks) or acute exposure (8-1 °C at 1 °C h −1) to 1 °C influenced cardiorespiratory parameters in resting Atlantic salmon; and 2) if/how the control of cardiac function was affected. Oxygen consumption ( ˙MO2 ) and cardiac function [i.e., heart rate ( f H) and cardiac output ( ˙Q) ] were 50% lower in the acutely cooled and 1 oC-acclimated salmon as compared to 8 °C fish, whereas stroke volume (V S) was unchanged. Intrinsic f H was not affected by whether the fish were acutely exposed or acclimated to 1 °C (values ∼51, 24 and 21 beats min −1 in 8 and 1 °C-acclimated fish, and 8-1 °C fish, respectively), and in all groups f H was primarily under adrenergic control/tone (cholinergic tone 13–18%; adrenergic tone 37–70%). However, β-adrenergic blockade resulted in a 50% increase in V S in the 1 oC-acclimated group, and this was surprising as circulating catecholamine levels were ∼1–3 nM in all groups. Overall, the data suggest that this species has a limited capacity to acclimate to temperatures approaching 0 °C. However, we cannot exclude the possibility that cardiac and metabolic responses are evoked when salmon are cooled to ∼ 0–1 °C, and that this prevented further declines in these parameters (i.e., they ‘reset’ quickly). Our data also provide further evidence that V S is temperature insensitive, and strongly suggest that changes in adrenoreceptor mediated control of venous pressure/capacitance occur when salmon are acclimated to 1 °C.

          Highlights

          • No data exist on in vivo salmonid cardiorespiratory function at ∼ 0–1 °C.

          • Acute exposure vs. acclimation to 1 °C generally had similar effects.

          • Heart rate, cardiac output and oxygen consumption at 1 °C were ∼50% of those at 8 °C.

          • Stroke volume and tissue oxygen extraction did not change between 8 and 1 °C.

          • Salmon are stressed, and rely primarily on cardiac adrenergic tone at 1 °C.

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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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            Longer and more frequent marine heatwaves over the past century

            Heatwaves are important climatic extremes in atmospheric and oceanic systems that can have devastating and long-term impacts on ecosystems, with subsequent socioeconomic consequences. Recent prominent marine heatwaves have attracted considerable scientific and public interest. Despite this, a comprehensive assessment of how these ocean temperature extremes have been changing globally is missing. Using a range of ocean temperature data including global records of daily satellite observations, daily in situ measurements and gridded monthly in situ-based data sets, we identify significant increases in marine heatwaves over the past century. We find that from 1925 to 2016, global average marine heatwave frequency and duration increased by 34% and 17%, respectively, resulting in a 54% increase in annual marine heatwave days globally. Importantly, these trends can largely be explained by increases in mean ocean temperatures, suggesting that we can expect further increases in marine heatwave days under continued global warming.
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              Declining oxygen in the global ocean and coastal waters

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                Author and article information

                Contributors
                Journal
                Curr Res Physiol
                Curr Res Physiol
                Current Research in Physiology
                Elsevier
                2665-9441
                17 March 2022
                2022
                17 March 2022
                : 5
                : 158-170
                Affiliations
                [1]Dept. of Ocean Sciences, Memorial University of Newfoundland and Labrador, St. John's, NL, A1C 5S7, Canada
                Author notes
                []Corresponding author. Dept. of Ocean Sciences, 0 Marine Lab Road, Memorial University of Newfoundland and Labrador, St. John's, NL. A1C 5S7. Canada. kgamperl@ 123456mun.ca
                Article
                S2665-9441(22)00014-1
                10.1016/j.crphys.2022.03.002
                8960890
                35359619
                943e405c-42a6-4250-85b6-eef7e610f342
                © 2022 The Authors

                This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).

                History
                : 27 September 2021
                : 19 February 2022
                : 14 March 2022
                Categories
                Articles from the special issue: Environment and the Heart, edited by Holly Shiels, Todd Gillis, Erica Eliason, Elena Fabbri and Denis Abramochkin

                acclimation,cold,temperature,cardiorespiratory physiology,metabolism,haematology,stress

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