Polar cod (Boreogadus saida) is an important prey species in the Arctic ecosystem, yet its habitat is changing rapidly: climate change, through rising seawater temperatures and CO2 concentrations, is projected to be most pronounced in Arctic waters. This study aimed to investigate the influence of ocean acidification and warming on maximum performance parameters of B. saida as indicators for the species' acclimation capacities under environmental conditions projected for the end of this century. After 4 months at four acclimation temperatures (0, 3, 6, 8°C) each combined with two PCO2 levels (390 and 1170 µatm), aerobic capacities and swimming performance of B. saida were recorded following a Ucrit protocol. At both CO2 levels, standard metabolic rate (SMR) was elevated at the highest acclimation temperature indicating thermal limitations. Maximum metabolic rate (MMR) increased continuously with temperature, suggesting an optimum temperature for aerobic scope for exercise (ASex) at 6°C. Aerobic swimming performance (Ugait) increased with acclimation temperature irrespective of CO2 levels, while critical swimming speed (Ucrit) did not reveal any clear trend with temperature. Hypercapnia evoked an increase in MMR (and thereby ASex). However, swimming performance (both Ugait and Ucrit) was impaired under elevated near-future PCO2 conditions, indicating reduced efficiencies of oxygen turnover. The contribution of anaerobic metabolism to swimming performance was very low overall, and further reduced under hypercapnia. Our results revealed high sensitivities of maximum performance parameters (MMR, Ugait, Ucrit) of B. saida to ocean acidification. Impaired swimming capacity under ocean acidification may reflect reduced future competitive strength of B. saida.
The oceans are currently experiencing a warming trend in parallel with increasing PCO2 levels (Caldeira and Wickett, 2003; IPCC, 2014). These changes are expected to be fastest in Arctic waters due to the high solubility of CO2 in cold waters (Fransson et al., 2009), and an increase in the temperature of Atlantic water masses flowing into the Arctic ocean (Polyakov et al., 2010). This accelerates the decline in sea-ice cover and the freshening of surface waters (McPhee et al., 1998), which, in turn, exacerbates ocean acidification due to decreasing buffer capacities (Steinacher et al., 2009). According to the Representative Concentration Pathway representing business-as-usual CO2 emissions (RCP 8.5), the Arctic is projected to experience a rise in surface temperatures of 4–11°C by the year 2100 compared with the period 1986–2005 (IPCC, 2014). Within the same timeframe, PCO2 levels in the Arctic ocean are projected to rise from 400 µatm to up to 1370 µatm (IPCC, 2014). Warming and potentially other climate change stressors such as ocean acidification appear to be already causing large-scale geographic shifts of marine species (Poloczanska et al., 2014) such as the ongoing borealization of the Arctic (Fossheim et al., 2015), entailing significant effects on the Arctic food chain.
Temperature is considered to be the most important abiotic factor shaping the geographical distribution of aquatic species (Magnuson et al., 1979; Perry et al., 2005; Fossheim et al., 2015) because of its effects on biochemical and physiological processes (Reynolds and Casterlin, 1979; Pörtner and Farrell, 2008). Accordingly, ectotherms tolerate a range of species-specific habitat temperatures that support the functionality of their molecular, cellular and systemic processes (Pörtner and Farrell, 2008). The species' thermal performance window can be understood from the ability of aerobic metabolic capacities to cover higher-than-baseline maintenance costs (Pörtner, 2010), as exemplified by aerobic scope (AS) [maximum metabolic rate (MMR)−standard metabolic rate (SMR)]. Within the thermal window, aerobic scope increases towards a species-specific optimum temperature and decreases rapidly at thermal conditions exceeding the optimum (Pörtner and Farrell, 2008; Farrell, 2016; Pörtner et al., 2017). Thermal performance windows are delimited by upper and lower critical temperatures at which aerobic scope reaches zero, solely supporting a time-limited passive and anaerobic existence (Pörtner and Farrell, 2008). In contrast, maximized aerobic scope at the species-specific optimum temperature implies optimum conditions for the performance of a given activity (Fry, 1947). Assuming that different aerobic activities do not necessarily have identical optimum temperatures, a broad thermal window with maximum aerobic scope covering a wide thermal range implies reduced competition between aerobic activities (Farrell, 2016). Most polar species, however, are adapted and specialized to the low temperatures and low thermal fluctuations of their natural habitat by evolving mechanisms to maintain overall performance along with reduced tolerance to changing abiotic conditions as a trade-off (Pörtner et al., 2000, 2005). Even relatively small increments in temperature can therefore have a tremendous impact on their metabolic demand (Claireaux et al., 2000; Pörtner, 2010) entailing a rise in energy turnover with detrimental consequences for fitness and performance traits e.g. growth, reproduction and swimming capacity (Butler et al., 1992). Despite decreasing performance capacities, the thermal range between peak aerobic scope and upper critical temperature is considered to be a buffer against a future increase in water temperature (Farrell, 2016), for the case where northward distribution shifts triggered by the motivation to preserve organismic performance cannot fully compensate for ocean warming.
aerobic scope of exercise
maximum burst count
total number of bursts
efficiency of maximum swimming performance
rate of oxygen consumption
maximum metabolic rate
ocean acidification and warming
partial pressure of carbon dioxide
standard metabolic rate
critical thermal limit
time between Ugait and Ucrit (‘time spent bursting’)
estimated proportion of anaerobic metabolism between Ugait and Ucrit
maximum swimming speed
transition speed from purely aerobic to partly anaerobic swimming (∼maximum aerobic swimming speed)
highest speed maintained for full time interval
Polar cod (Boreogadus saida, Lepechin 1774), is the most abundant Arctic gadid (Mueter et al., 2016 and references therein) and it is regarded as a key species in Arctic ecosystems (Bain and Sekerak, 1978; Welch et al., 1993; Hop and Gjøsæter, 2013) because of its role as a link between lower and higher trophic levels (Lowry and Frost, 1981; Bradstreet, 1982; Welch et al., 1993). Furthermore, it is the most energy-rich prey organism in the Arctic food chain (Harter et al., 2013). In recent years, the abundance of B. saida has been found to decrease in its southern distribution area in the Barents Sea as a result of rising water temperatures (Eriksen et al., 2015). Throughout its life stages, B. saida prefers different thermal habitats. Spawning takes place in shallow waters above 0°C with a peak period in January and February (Ajiad et al., 2011). Pelagic 0-group B. saida prefer 2.0–5.5°C (Eriksen et al., 2015), while juveniles and non-spawning adults are either ice-associated (Lønne and Gulliksen, 1989) or found in deep water layers below 0°C (Falk-Petersen et al., 1986). A progressive distribution retreat of B. saida, evoked directly or indirectly by climate change, might have profound, cascading ecological consequences. In order to gauge ecosystem impacts caused by rapidly changing abiotic conditions, the assessment of sensitivities and acclimation capacities of key species such as B. saida to future climate scenarios is highly important.
The whole-animal SMR is an important parameter for the assessment of long-term survival because it integrates essential cellular and molecular energetic costs in the inactive organism at the respective environmental conditions (Chabot et al., 2016). Therefore, the SMR of B. saida has been identified over a range of acclimation temperatures in a number of studies (Holeton, 1974; Steffensen et al., 1994; Hop and Graham, 1995; Kunz et al., 2016a). Maximum respiratory performance of B. saida has been studied by Drost et al. (2016); however, aerobic swimming capacity as a fitness parameter has never been quantified in B. saida.
Furthermore, studies investigating performance capacities of B. saida exposed to combined climate drivers such as ocean acidification and warming (OAW) are still scarce. Recent studies investigated growth performance, feed consumption and SMR (Kunz et al., 2016a), laterality and spontaneous activity (Schmidt et al., 2017) and heart mitochondria performance (Leo et al., 2017) in juveniles as well as survival rates, SMR and morphology at hatch in early life stages (Flemming Dahlke, Daniela Storch and H.-O.P., unpublished data) under combined OAW conditions. We hypothesize that traits involving maximum performance will also be affected by ocean acidification, possibly even more so than routine functions, as the former may reflect limits to acclimatization. Therefore, the aim of the present study is to investigate the impact of long-term exposure to projected OAW scenarios on ASex and swimming performance of B. saida in light of its whole-animal acclimation capacities to future Arctic water conditions.
MATERIALS AND METHODS
All procedures reported in the present study were in accordance with the ethical standards of the federal state of Bremen, Germany, and were approved under the reference number 522-27-22/02-00 (113).
B. saida originated from Isfjorden and Kongsfjorden on the west coast of Spitsbergen. They were caught by RV Helmer Hanssen using bottom trawls at a depth of 120 m in January 2013. A fish-lift connected to the trawl (Holst and McDonald, 2000) protected the fish from injuries during trawling. The animals were then kept in the aquaria of Havbruksstasjonen i Tromsø AS (HiT) until April 2013, when they were transported to the laboratories of the Alfred Wegener Institute (AWI) in Bremerhaven.
B. saida specimens were acclimated to different combinations of present and projected future ocean water conditions (temperature: 0, 3, 6, 8°C; PCO2: 390 and 1170 µatm) for approximately 4 months. Each temperature/PCO2 treatment comprised 12 individuals placed in 24 litre aquaria. The PCO2 conditions for each treatment were generated in a common header tank (∼200 litres) which then provided identical conditions in each of the individual tanks. The setting of PCO2 levels was accomplished by equilibration with mixtures of air and CO2 provided by an automated mass flow controller system (4 and 6 channel MFC system, HTK, Hamburg, Germany).
The distribution of individuals between treatments was done randomly. The acclimation to experimental temperatures took place gradually (max. temperature change: 1°C in 24 h), followed by establishing experimental PCO2 conditions within 1 day, as soon as the desired experimental temperatures were reached. Light conditions were maintained at 12 h light:12 h dark throughout the experiment. Each fish was fed ad libitum every fourth day with formulated high-protein feed pellets (Amber Neptun, 5 mm, Skretting AS, Norway). For details on whole-animal parameters throughout the incubation period, see Kunz et al. (2016b).
Temperature, salinity and pH (cross-calibrated to total pH scale) were monitored once to twice a week in triplicate for every treatment in order to verify the stability of PCO2 conditions, as described in Kunz et al. (2016a). The seawater carbonate chemistry was calculated in the program CO2SYS (Lewis and Wallace, 1998) based on the total dissolved inorganic carbon and the pHtot values as listed in table 2 in Kunz et al. (2016a). The full water chemistry raw data of the incubation can be found in Schmidt et al. (2016).
Swimming performance measurements
Two swim tunnels (30 litres; dimension working section: 46.5×13.5×14 cm, Loligo Systems ApS, Denmark) were used simultaneously to determine the swimming performance of B. saida (n=4–6 per treatment), enabling the measurement of up to 6 individuals per day in temperature-controlled rooms. The swim tunnels were supplied with pre-conditioned water from the header tank of the respective incubation treatment. For the time span of the experiment, the water conditions in the tunnels were maintained by permanent aeration with a gas mixture containing the respective CO2 levels. Aeration was maintained in the reservoir tank surrounding the swimming chamber. The swim chamber was kept in open mode to avoid decreasing O2 concentrations as well as temperature and PCO2 fluctuations in the chamber. Permanent seawater exchange between the outer reservoir tank and the swim chamber was established by an aquarium pump (9.2 litres min−1). The desired velocity was translated from a control unit to a propeller in the swim chamber. A uniform velocity profile and a laminar flow were promoted by honeycomb-shaped plastic inserts. A flow sensor (Vane wheel flow sensor FA, Höntzsch Instruments, Waiblingen, Germany) placed in the centre of the working section of the swim tunnel was used to calibrate the water velocity to voltage output from the control unit.
Individual rates of oxygen consumption (ṀO2 in µmol min−1 g−1) were measured at long-term acclimation temperature and PCO2 by automated intermittent flow-through respirometry in a separate experimental set-up, comprising two sets of 6 perspex respiration chambers (1.8 and 2.2 litres). Respiration chambers were submerged as sets of two in common tanks (∼50 litres) with water conditions identical to the respective temperature/PCO2 treatments. Partial water exchanges with pre-conditioned sea water were performed after ∼24 h. A non-transparent plastic wall between the respiration chambers prevented visual contact of the two individuals sharing a common water basin. Aeration of the water surrounding the respiration chambers with the respective air/CO2 mix was maintained throughout the experimental period to ensure oxygen saturation.
The water inside the respiration chambers circulated permanently at constant velocity by aid of an aquarium pump (8.2 litres min−1). A flush pump (5.0 litres min−1) facilitated periodic water exchanges between respirometer and its surrounding. ṀO2 measurement periods of 15 min were alternated with flush periods of 30 min to fully re-establish O2 saturation. The O2 concentration was determined by optical oxygen probes and recorded using a ten-channel oxygen meter (PreSens-Precision Sensing GmbH, Hamburg, Germany; system 1) as well as a four-channel FireStingO2 (Pyro Science GmbH, Aachen, Germany) and two one-channel Fibox 3 systems (PreSens-Precision Sensing GmbH, Hamburg, Germany) (system 2). For the 0% calibration, the oxygen probes were flushed with nitrogen at room temperature. The calibration for 100% O2 was performed in fully aerated water at the respective experimental temperature prior to the measurements of each treatment. Blank measurements to detect bacterial background respiration were recorded following the ṀO2 analyses once at every temperature. In order to minimize potential disturbances, all tanks were covered with opaque plastic sheets.
In the respiration chambers, both MMR and SMR were determined at long-term acclimation temperature and PCO2. To obtain SMR, individuals remained in the chambers for ∼48 h in order to fully recover from exercise in the swim tunnel. The ṀO2 values were calculated using the appropriate constants for O2 solubility in seawater (Boutilier et al., 1984) and normalized to an average fish weight of 25.6 g following Steffensen et al. (1994). After subtraction of bacterial respiration (solely measurable at 8°C), the first 5 min of the slope of the first ṀO2 recording were used to calculate MMR, while the 15% quantile of ṀO2 recordings starting from the second night in the respiration chamber was considered as SMR (Chabot et al., 2016). After respiration measurements, the length of each fish was measured.
Calculations and statistical analysis
In order to further classify anaerobic swimming performance, we analysed both the maximum consecutive number of bursts at one velocity step and the total number of bursts throughout the whole swim trial.
Individuals that displayed physical abnormalities (n=1; 0°C/1170 µatm) or refused to swim (n=2; 0°C/390 µatm, 8°C/1170 µatm) because of lethargic behaviour were excluded from data analysis. Fish that refused to swim for no apparent reason (n=1; 6°C/1170 µatm) were included in the analysis for SMR. Individuals that did not have any burst capacity were excluded from the statistical analysis for Ucrit for comparability reasons.
Statistical analyses were accomplished using R version 3.0.2 (2013). All variables were tested for normal distribution and homoscedasticity with Shapiro–Wilk and Levene tests, respectively. Owing to heteroscedasticity, the data sets for BCtot and TSBanaerob were log and square root transformed, respectively. Following Nalimov tests, one outlier was removed from the variable ASex (3°C/390 µatm; P=0.0111), Ugait (3°C/1170 µatm; P=0.0007), Emax (0°C/390 µatm; P=0.0073) and TSBanaerob (0°C/390 µatm; P=0.0241), respectively. Outlier tests proved inefficient within the one treatment of the variable BCtot (0°C/390 µatm, P=0.0233). Therefore, this treatment was tolerated as false positive during further statistical analysis. Statistical comparisons between treatments were performed for the variables SMR, MMR, ASex, Ugait, Ucrit, Emax, maximum burst count (BCmax), BCtot, TSB and TSBanaerob using two-way ANOVA. In the case of statistically significant differences, a subsequent post hoc Tukey honest significance test was applied. The results of the two-way ANOVA are shown in Table 1, while the results of the Tukey honest significance test between temperature treatments are shown as letters within the figures. Significant differences were assumed using a 5% threshold (P<0.05).
This model was also applied to the data set of 6°C/390 µatm, although the model fit was relatively poor for the data of this treatment (see Table 2 for significance levels). Significant differences in the burst performance between PCO2 treatments were accepted in the case of non-overlapping 95% confidence intervals.
Table 3 provides a summary of the results for respiration measurements and swimming performance. A summary of burst swimming parameters is given in Table 4. In total, four individuals showed no bursting event (6°C/390 µatm, n=1; 6°C/1170 µatm, n=1; 8°C/390 µatm, n=2). For a further three individuals (0°C/390 µatm, n=1; 6°C/390 µatm, n=1; 6°C/1170 µatm, n=1), bursting occurred very close to the critical swimming speed (Ucrit).
The SMR of B. saida showed comparable values at 0, 3 and 6°C, but was significantly higher at 8°C (0°C versus 8°C, P<0.0001; 3°C versus 8°C, P<0.0001; 6°C versus 8°C, P=0.0005). Hypercapnia did not reveal any effect on the SMR of this species (P=0.342) (Fig. 1A). Long-term acclimation to different temperatures had a distinct effect (P=0.0005) on the MMR of B. saida: MMR rose significantly between 0 and 6°C (P=0.0041), where it levelled off (6°C versus 8°C, P=0.9232). At all temperatures but 0°C, MMR was enhanced in high PCO2 treatments compared with control PCO2 treatments (P=0.0322) (Fig. 1B). An overall temperature effect (P=0.0185) was recorded for the aerobic scope of exercise (ASex) after 4 months with a peak observed at 6°C (0°C versus 6°C, P=0.0336). Furthermore, ASex was significantly elevated under high PCO2 conditions (P=0.0059) (Fig. 2).
The transition speed from purely aerobic to partly anaerobic swimming performance (Ugait) increased significantly with long-term acclimation temperature (P=0.0341). The significant difference, nevertheless, refers to an elevated Ugait at the highest (8°C) compared with the lowest acclimation temperature (0°C), indicating an overall modest temperature effect on this parameter. Long-term acclimation at high PCO2 significantly depressed Ugait (P=0.0270; Fig. 3A). An interaction between temperature and PCO2 level was not found for this parameter (P=0.8134). Ucrit did not reveal a significant temperature effect (P=0.2014). Ucrit data, however, indicated a downward trend due to hypercapnia (P=0.0559; Fig. 3B).
The maximum number of bursts, a parameter assumed to reflect the capacity for anaerobic swimming, was highest at 3°C (0°C versus 3°C, P=0.1358; 3°C versus 6°C, P=0.0051; 3°C versus 8°C, P=0.0776). At the same time, the maximum burst count was found to be higher under normocapnia than hypercapnia (P=0.0231). Furthermore, elevated PCO2 shifted mean burst performance at 3°C to lower velocities under hypercapnia (non-overlapping 95% CI; asterisk in Fig. 4). In contrast to the results for maximum number of bursts, neither temperature nor PCO2 affected the total number of bursts significantly. However, a combined effect of temperature and PCO2 level was detected (P=0.0288), mainly evoked by the low number of bursts detected in the treatment at 8°C/1170 µatm. The time between Ugait and Ucrit – hereafter classified as ‘time spent bursting’ (TSB) – revealed a decreasing trend with temperature (P=0.0059), with no apparent PCO2 effect (P=0.8760). The putative contribution of anaerobic metabolism to swimming performance between Ugait and Ucrit (TSBanaerob) was low overall (<3% in 92.9% of individuals) with no apparent influence of temperature or PCO2 (Table 4).
Energetic efficiency of maximum swimming performance (Emax) (Fig. 5) was high at 0°C (0°C versus 3°C, P=0.1161; 0°C versus 6°C, P=0.0128; 0°C versus 8°C, P=0.0210). Although no significant impact of hypercapnia was detected (P=0.1045), Emax was reduced under high PCO2 conditions at all temperatures above 0°C due to the elevated MMR under hypercapnic conditions between 3 and 8°C. Furthermore, Emax showed a significant interaction effect of temperature and PCO2 evoked by a strongly elevated value at 0°C under hypercapnia (0°C/1170 µatm versus 3°C/1170 µatm, P=0.0236; 0°C/1170 µatm versus 6°C/1170 µatm, P=0.0348; 0°C/1170 µatm versus 8°C/1170 µatm, P=0.0155).
The present study aimed to investigate oxygen consumption and exercise capacities of B. saida after long-term acclimation to future OAW conditions in order to estimate the competitive strength of this species under future environmental conditions at PCO2 levels following the RCP8.5 scenario (IPCC, 2014). Our results suggest that enhanced costs visible in elevated MMR under hypercapnic water conditions cause a reduction in maximum swimming capacity.
At comparable temperatures, the SMR obtained in the present study was in the same order of magnitude as published for B. saida (Steffensen et al., 1994, 4.5°C; Drost et al., 2016, 1.0, 3.5, 6.5°C), when applying the ṀO2 units and the weight correction formula of the respective studies. Slight deviations in SMR are likely to be attributable to divergent approaches to determine SMR: when applying the same approach for the determination of SMR as used by Drost et al. (2016) (assuming the lowest ṀO2 recording as SMR) for comparison between both studies, the resulting SMR values of the present study (65, 64 and 78 mg O2 kg−1 h−1 at 0, 3 and 6°C, respectively) are fairly similar to those published by Drost et al. (2016) (∼53, 50 and 76 mg O2 kg−1 h−1 at 1, 3.5 and 6.5°C, respectively). The approach chosen by Drost et al. (2016) was the only method applicable to their particular experimental design. However, Chabot et al. (2016) raised the concern of an underestimation of SMR due to temporal variability within this parameter when only a single ṀO2 measurement is chosen to represent SMR. In order to correct for temporal variability, we preferred to calculate SMR by aid of a quantile approach allowing 15% of the resting ṀO2 values to fall below the actual individual SMR (Dupont-Prinet et al., 2013; Chabot et al., 2016).
The SMRs of B. saida acclimated long-term at 3 and 6°C were similar to those found in the 0°C acclimated individuals. This implies efficient metabolic compensation in the thermal range between 0 and 6°C (Precht, 1958). Metabolic compensation is hypothesized to enable the individual to maintain vital functions independent of environmental temperatures (Precht, 1958). Hop and Graham (1995) detected incomplete compensation in the SMR of B. saida following a 12 day exposure to 2.7°C compared with SMR values obtained in specimens acclimated for 5 months at 0.4°C. Accordingly, the rather short exposure period (12 days) to the elevated temperature was probably insufficient to establish a new physiological steady state and thereby to unfold the full acclimation potential of this species. At 8°C, the SMR of B. saida was significantly elevated, even after 4 months of acclimation, also perceived in a non-significantly reduced growth performance (Kunz et al., 2016a). Mitochondrial plasticity has been identified to be involved in setting the limits of thermal acclimation capacity (e.g. Strobel et al., 2013). Accordingly, the elevated whole-animal SMR at the highest temperature investigated may, at least partly, be attributed to limited acclimation capacities expressed through reduced mitochondrial efficiencies at 8°C shown in cardiac myocytes of the same individuals as used in the present study (Leo et al., 2017). B. saida revealed little capacity to adjust mitochondrial enzyme activities and lipid class compositions in response to warm acclimation above 6°C (Elettra Leo, Martin Graeve, Daniela Storch, H.-O.P. and F.C.M., unpublished data). Accordingly, an enhanced proton leak and an associated decrease in ATP production efficiency evoked by changes in membrane fluidity are suggested to cause the impaired mitochondrial efficiency in B. saida close to its long-term whole-animal upper thermal tolerance limit [pejus temperatures (Tpej) sensu Pörtner et al., 2017; Leo et al., 2017].
Elevated CO2 levels did not influence the SMR of B. saida in the present study in line with findings for the Atlantic cod (Gadus morhua) (3–4 weeks of exposure, Kreiss et al., 2015) and the Antarctic Notothenia rossii (29–36 days of exposure, Strobel et al., 2012), long-term acclimated to moderate PCO2 conditions. This suggests a rather low sensitivity of baseline metabolism to hypercapnia. Accordingly, the resting cardiac mitochondrial respiration of B. saida was not affected by chronically elevated PCO2 (Leo et al., 2017).
Recorded values for MMR are consistent with recently published results for B. saida (Drost et al., 2016). A positive correlation between MMR and environmental temperatures as detected in the present study is well established for diverse teleost species (e.g. Claireaux et al., 2006; Eliason et al., 2011; Clark et al., 2011) along with an increase in cardiorespiratory performance with temperature. Limitations in heart rate and oxygen-carrying capacity are hypothesized to cause a levelling off in MMR at high acclimation temperatures (Pörtner, 2010), as seen in the present study.
The continuous increase in MMR with temperature and the elevated SMR at 8°C result in a peak aerobic scope for exercise (ASex) of B. saida acclimated to 6°C. In line with this observation, growth of B. saida under laboratory conditions was also maximum at 6°C (Kunz et al., 2016a), suggesting a connection between aerobic capacities and growth as well as exercise (Pörtner and Knust, 2007; Pörtner and Farrell, 2008). The optimization of aerobic performance governed by environmental factors is widely recognized to determine a species' spatial and temporal niche (Claireaux and Lagardère, 1999; Pörtner and Farrell, 2008). Nevertheless, fish often inhabit areas with temperatures well below their physiological optimum obtained under artificial ad libitum food situations (Björnsson et al., 2001) indicating that maximum exploitation of aerobic scope is not a precondition for survival (Deutsch et al., 2015; Norin and Clark, 2016). Despite cold-induced reductions in ASex due to lower MMR, B. saida is well adapted to temperatures around 0°C, visible in a high feed conversion efficiency (Kunz et al., 2016a). Likewise, Hop et al. (1997) found assimilation efficiencies at 0°C (average 80%), similar to assimilation capacities detected in stenothermal Antarctic fish. Thus, B. saida likely has an energetic advantage over potential predators and competitors in cold waters. In contrast, when inhabiting waters with their maximum ASex and their optimum temperature for growth (6°C) (Kunz et al., 2016a), a reduced abundance of suitable prey (Fossheim et al., 2015) would probably demand elevated energy fractions for foraging activity, possibly constraining growth and reproduction. Accordingly, during ongoing climate change, polar fish at their southern distribution limits such as B. saida may be especially vulnerable to competition with invading species adapted to higher water temperatures. Among the northwards moving species, capelin (Mallotus villosus), Atlantic cod and haddock (Melanogrammus aeglefinus) represent a potential treat to B. saida. While M. villosus is expected to compete for prey with B. saida during a progressive future habitat overlap (Hop and Gjøsæter, 2013), juvenile G. morhua and M. aeglefinus revealed little dietary overlap with B. saida in habitats where they co-occurred (Renaud et al., 2012). During ongoing climate change, however, adult G. morhua and M. aeglefinus may become increasingly important as predators on B. saida (Renaud et al., 2012). Nevertheless, the distribution of B. saida has already been observed to contract in its southern habitat as a direct result of increasing water temperatures (Eriksen et al., 2015).
In parallel to ASex, both mainly aerobically fuelled steady-state swimming performance (Lurman et al., 2007) (Ugait) and partly anaerobically fuelled Ucrit are known to increase acutely with temperature up to maximum performance before decreasing at temperatures approaching the critical thermal limit (TC,max sensu Farrell, 2016) (e.g. Griffiths and Alderdice, 1972). In the present study, however, Ugait of B. saida showed only a modest increase with acclimation temperature. Ucrit did not reveal any clear trend with long-term acclimation temperature. These results indicate that metabolic compensation processes during warm acclimation as observed for the SMR of B. saida (see above) were also reflected in swimming metabolism for this species. Thus, while Ugait and Ucrit of B. saida showed signs of acclimation throughout the range of investigated temperatures (0–8°C), the SMR of B. saida showed full compensation up to only 6°C attributed to a significant reduction in mitochondrial ATP production efficiency at 8°C compared with lower acclimation temperatures (0, 3 and 6°C) (Leo et al., 2017). The decreasing mitochondrial ATP production efficiency may further contribute to the observed decrease in muscle output efficiency (here expressed as Emax) with acclimation temperature. Based on the reduced mitochondrial efficiencies that translated into organismic limitations, we expect an overall limited capacity of B. saida to acclimate to water conditions higher than 6°C. Similar to indications obtained in our study, Drost et al. (2016), who investigated the thermal acclimation response of B. saida from the Canadian Arctic by measuring cardio-respiratory performance, found that B. saida can acclimate to 6.5°C (highest investigated acclimation temperature). Nevertheless, cardio-respiratory limitations caused a higher sensitivity of 6.5°C-acclimated specimens to acute temperature changes compared with B. saida acclimated to lower temperatures (Drost et al., 2016).
The switch from aerobic to anaerobic metabolism at Ugait is marked by burst-type exercise events (Milligan and Wood, 1986; Lurman et al., 2007). Burst performance is essential during predator–prey interactions (Beamish, 1978), and can only be maintained for short periods. B. saida showed low burst capacity throughout all temperature/PCO2 treatments (Table 4), with a few specimens (n=4 at 6 and 8°C treatments out of in total 42 specimens used in the swimming performance tests) not even displaying any burst behaviour at all. Accordingly, the contribution of anaerobic metabolism to maximum swimming capacity is putatively minor. This phenomenon is in line with observations in other polar species, including Antarctic fishes that revealed low potential for anaerobic glycolysis (e.g. the yellowbelly rockcod Notothenia neglecta, Dunn and Johnston, 1986; the bald notothen Pagothenia borchgrevinki, Davison et al., 1988). Compared with active temperate species, the burst performance of B. saida is several-fold lower (highest maximum burst count for B. saida: 19.5 for 30 s, 3°C versus e.g. European sea bass Dicentrarchus labrax, 23°C; maximum burst count at Ucrit: ∼84 for 30 s, Marras et al., 2010). Furthermore, the stores of the white muscle metabolites ATP and glycogen have been shown to remain independent of acclimation temperature (see review by Kieffer, 2000). Combined with the low level of anaerobically fuelled swimming capacity (0–5.7%), the slightly elevated burst performance (both BCmax and BCtot) of B. saida at 3°C found in the present study is not given much weight. Hence, the moderately active lifestyle of B. saida described by Gradinger and Bluhm (2004) is also mirrored in the low-burst swimming performance, possibly involving a disadvantage during predator avoidance.
The response of aerobic capacities to near-future elevated PCO2 conditions has been found to be strongly species specific (compare review by Esbaugh, 2018), with reduced sensitivities to CO2 suggested for species frequently exposed to natural fluctuations in abiotic conditions (Rummer et al., 2013). The majority of studies did not detect any impact of near-future PCO2 conditions on MMR in a variety of species after chronic exposure (G. morhua, 4 months at 3000 µatm, Melzner et al., 2009; red drum, Sciaenops ocellatus, 14 days at 1000 µatm, Esbaugh et al., 2016; blue rockfish, Sebastes mystinus 16–19 weeks at 750, 1900 and 2800 µatm, Hamilton et al., 2017). In contrast, a reduction of MMR under ocean acidification was found in copper rockfish (Sebastes caurinus) exposed to 1900 µatm CO2 and 10°C for 14–17 weeks (Hamilton et al., 2017). B. saida, however, revealed an elevated MMR under near-future PCO2 conditions (at all temperatures above 0°C), in line with observations in the tropical coral reef fish Acanthochromis polyacanthus (17 days at 950 µatm, Rummer et al., 2013) and the temperate species D. labrax under long-term exposure to realistic PCO2 scenarios (1.5 years, 1500 µatm, Amélie Crespel, Katja Anttila, Pernelle Lelièvre, Patrick Quazuguel, Nicolas Le Bayon, José-Luis Zambonino-Infante, Denis Chabot and G.C., unpublished data). Interestingly, B. saida showed reduced maximum swimming velocities despite elevated MMR. Unfortunately, the studies of Rummer et al. (2013) and Crespel and coworkers (unpublished data) do not report on swimming performance. As a consequence of elevated MMR and reduced swimming performance, Emax was impaired in B. saida under hypercapnia at all temperatures above 0°C. Under control PCO2 conditions, however, swimming performance efficiency was only reduced at acclimation temperatures above 3°C, suggesting a higher thermal sensitivity of MMR under hypercapnia. Nevertheless, Emax has to be considered with care as an unquantifiable oxygen debt may interfere with it (Brett, 1962), which, in turn, is expected to be of little extent due to limited anaerobic capacities implied by a low burst capacity detected in the present study.
To date, physiological mechanisms causing elevated aerobic metabolic costs under moderate PCO2 conditions are not fully understood. Our results suggest that this cost is likely elevated through mechanisms other than exercise and constrains swimming performance (both Ugait and Ucrit) to lower levels under hypercapnia while causing elevated ṀO2 and a consequently higher ASex. One organ potentially being involved in elevated energy demands under high PCO2 conditions is the gill. Kreiss et al. (2015) found branchial ṀO2 per gram gill tissue after long-term acclimation of G. morhua to 2200 µatm remained comparable to values under control PCO2 conditions at 10°C. However, high PCO2 caused an increase in gill soft tissue, resulting in elevated fractions of gill ṀO2 from whole-animal ṀO2 (increase from 5 to 7%) (Kreiss et al., 2015). Nevertheless, the SMR of both G. morhua (Kreiss et al., 2015) and B. saida (present study) remained unaffected under hypercapnia. Yet, potential cascading effects might be amplified during maximum performance causing trade-offs in swimming capacity as seen in B. saida. The results of the present study focusing on whole-animal parameters, however, represent only an ensemble of organismic costs and do not give further insight into the energetic partition of underlying mechanisms.
Hypercapnia-acclimated fish not only showed a shift to anaerobic white muscle reserves at lower swimming speeds (as observed by lower Ugait), but the burst performance was also reduced compared with normocapnia-acclimated fish. Despite a marginal contribution of anaerobic metabolism to the maximum swimming capacities of B. saida, this finding is in line with the overall impairment in maximum performance detected following exposure to elevated PCO2 levels. Hence, aerobic as well as anaerobic exercise capacities appear reduced under high PCO2 scenarios. Thus, hypercapnia has effects on the energy metabolism of B. saida at high and maximum metabolic rates that are not visible at rest (Kunz et al., 2016a).
In conclusion, the present study revealed a strong impact of ocean acidification on maximum performance traits of B. saida. Although elevated PCO2 levels did not significantly impact routine parameters (growth, food consumption, SMR) in this species (Kunz et al., 2016a), trade-offs in energy allocation became visible when the metabolism was operating at maximum performance under hypercapnic conditions. More precisely, long-term acclimation under near-future PCO2 conditions caused reduced swimming capacity of B. saida at higher metabolic costs. Consequently, when translating the present results obtained from a limited number of specimens onto the population level, foraging success and escape response of B. saida during predator encounters might be impaired under future water conditions. Species that are resilient to a broader range of abiotic conditions, such as G. morhua (Melzner et al., 2009), may find it easier to prevail in light of the ongoing borealization and community shifts in the Arctic (Fossheim et al., 2015). Accordingly, the competitive strength of B. saida, and thereby its abundance in this new setting in the waters around Svalbard can be expected to decrease.
We gratefully acknowledge J. Nahrgang for providing B. saida (research program Polarisation no. 214184/F20 funded by the Norwegian Research Council), as well as the crew of RV Helmer Hanssen (University of Tromsø) for animal collection. We would like to thank E. Leo, M. Schmidt, S. Hardenberg and H. Windisch for their support during the realization of the incubation setup and animal maintenance, as well as T. Hirse and S. Berger for technical assistance with the manipulation of CO2 partial pressure. We appreciate the contribution of A. Tillmann, I. Ketelsen, F. V. Moraleda, K. Zanaty, M. Machnik and B. Matthei to the measurements of pH and DIC. Finally, we greatly appreciate the constructive suggestions of the two reviewers.
Conceptualization: K.L.K., H.P., R.K., F.C.M.; Methodology: K.L.K., G.C., F.C.M.; Validation: K.L.K., G.C.; Formal analysis: K.L.K.; Investigation: K.L.K., F.C.M., G.C.; Data curation: K.L.K.; Writing - original draft: K.L.K., F.C.M.; Writing - review & editing: K.L.K., G.C., H.P., R.K., F.C.M.; Supervision: G.C., H.P., R.K., F.C.M.; Project administration: F.C.M.; Funding acquisition: H.P., R.K., F.C.M.
This project was part of the research program BIOACID (Biological Impacts of Ocean Acidification, phase II) funded by the German Bundesministerium für Bildung und Forschung (BMBF; FKZ 03F0655B and FKZ 03F0728B to H.-O.P., R.K. and F.C.M.). K.L.K., H.-O.P., R.K. and F.C.M. acknowledge funding through the PACES (Polar Regions and Coasts in a Changing Earth System) program of the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI). Deposited in PMC for immediate release.
Raw data generated and analyzed during the present study are available in PANGAEA under deposition number 889447 (Kunz et al., 2018).
The authors declare no competing or financial interests.