Abstract
Coastal marine systems are characterized by high levels of primary production that result in diel oxygen fluctuations from undersaturation to supersaturation. Constant normoxia, or 100% oxygen saturation, is therefore rare. Since the thermal sensitivity of invertebrates is directly linked to oxygen availability, we hypothesized that (i) the metabolic response of coastal marine invertebrates would be more sensitive to thermal stress when exposed to oxygen supersaturation rather than 100% oxygen saturation and (ii) natural diel fluctuation in oxygen availability rather than constant 100% oxygen saturation is a main driver of the thermal response. We tested the effects of oxygen regime on the metabolic rate, and haemocyanin and lactate levels, of velvet crabs (Necora puber) and blue mussels (Mytilus edulis), under rising temperatures (up to 24°C) in the laboratory. Oxygen supersaturation and photosynthetically induced diel oxygen fluctuation amplified animal metabolic thermal response significantly in both species, demonstrating that the natural variability of oxygen in coastal environments can provide considerable physiological benefits under ocean warming. Our study highlights the significance of integrating ecologically relevant oxygen variability into experimental assessments of animal physiology and thermal response, and predictions of metabolic performance under climate warming. Given the escalating intensity and frequency of climate anomalies, oxygen variation caused by coastal vegetation will likely become increasingly important in mitigating the effects of higher temperatures on coastal fauna.
Keywords: oxygen supersaturation, marine invertebrates, macroalgae, thermal response, ocean warming refugia, climate change
1. Introduction
Climate warming is a critical driver of worldwide ocean deoxygenation, having resulted in an overall loss of 1–2% of dissolved oxygen since the mid-twentieth century [1,2]. Global temperature rise not only reduces oxygen solubility in water, but also increases the oxygen requirements of ectotherms [3]. Although coastal waters conform to this trend, they often exhibit particularly high levels of primary production and can act as refugia from a combination of oxygen depletion and high temperatures and also from long-term oxygen depletion [4]. This effect occurs over large spatial scales because, typically, productive coastal systems are interconnected, allowing them to form a mosaic of favourable habitats. The activity of primary producers can cause dynamic and dramatic shifts in the environmental conditions of coastal waters, namely pH [5], CO2 [6] and, more recently, their role in generating significant diurnal and seasonal fluctuations in oxygen has been revealed [7]. As a result, productive coastal waters exhibit oxygen supersaturation on a daily basis [8], while at night the cessation of photosynthesis and plant respiration cause concentrations to plummet as low as 10% [7].
A large number of ecologically and economically important marine species, from micro- to mega-fauna, have evolved in, or in close association with, coastal environments that are characterized by diel oxygen fluctuations, spending at least part of their life cycle in shallow waters [9–11]. It is well known that productive marine coastal habitats can provide shelter from predation and are frequently used as nursery habitats as well as feeding grounds for adults [12,13]. But in addition, the generation of hyperoxic conditions in such habitats has other advantages. Oxygen supersaturation can reduce exposure to pathogens [14] and enhance resistance to marine pollutants [15,16] and is also associated with increased clutch size in marine invertebrates [17]. The mechanistic link between oxygen availability and thermal tolerance has been described by Pörtner [18]. More recently, the association between oxygen supersaturation and thermal sensitivity has been explored, with evidence that exposure to oxygen supersaturation can improve the ability of marine animals to extract oxygen from water [7] and improve aerobic capacity during warming [19].
When driven by primary production, oxygen supersaturation is generally coupled on a diel basis with undersaturation, or hypoxia. This cyclical switch from undersaturation (during the night) to oxygen supersaturation (during the day) reflects the actual conditions experienced by the majority of aquatic animals living in productive marine systems [20]. While effects of oxygen supersaturation and, to a greater extent, undersaturation (e.g. impacts on the early development, behaviour, growth and survival of marine animals [21–23]) are well known, to our knowledge no studies have addressed the effects of the diel fluctuations of oxygen saturation. Rather, typically experimental designs consider oxygen levels to be stable at whichever of these extremes was studied.
To gain a more realistic understanding of the potential consequences of ocean warming and heatwaves for species' survival, it is necessary to address the question of how naturally occurring diel fluctuation of dissolved oxygen affects the responses of coastal animals to warming. Metabolic rates are widely used as a proxy for this, since animals tend to avoid reduced fitness or even mortality by maintaining aerobic performance and fulfilling the oxygen demand induced by increased metabolism [24,25]. We addressed this question by testing two hypotheses: (i) that thermal response of metabolism is altered when animals are exposed to oxygen supersaturation rather than 100% oxygen saturation (experiment 1) and (ii) that natural diel fluctuation in oxygen availability induced by primary producers rather than constant 100% oxygen saturation is the main driver of the thermal response of coastal invertebrates (experiment 2).
2. Methods
The study was carried out during November–December 2019 at the St Abbs Marine Station research facility on the east coast of Scotland (55°53′52″ N, 2°7′44″ E). The oxygen and temperature conditions in the algae beds at the study site (from the period October–December 2019) were recorded with a PME miniDOT dissolved oxygen and temperature logger and light sensor (ONSET HOBO - UA-002-08) (electronic supplementary material, figure S1).
(a) . Animal collection and experimental set-up
Two model coastal invertebrates were selected as study species: Necora puber (Linnaeus, 1767) (velvet crab) and Mytilus edulis (Linnaeus, 1758) (blue mussel) (figure 1a,b). Similar-sized animals were collected: crabs at St Abbs (carapace width 80–120 mm) and mussels at Musselburgh, 40 miles farther north (shell length 50–60 mm). All specimens used in experiments appeared healthy, with no signs of shell or carapace damage. Mussels were hand-collected and crabs (only male specimens to avoid possible confounding effects of sex) were provided by local fishermen. Fouling was removed from mussel shells to avoid any interference with respiration measurements. Animals were acclimated in the laboratory under natural light/dark conditions (due to a Perspex roof) and ambient temperature seawater for 14 days prior to the experiments (approx. 10 h light: 14 h dark, 9–11°C, 100–104% oxygen saturation, salinity: 34.23–34.38 ppt). The two species were kept in separate flow-through fibreglass tanks. Crabs were kept in a 973 l tank and provided with a shelter to reduce stress. Mussels were held fully submerged in a 550 l tank. Crabs were provided a diet of either cooked mussels, or fish, or squid every 2–4 days. Mussels were fed algae (Nannochloropsis sp.) ad libitum at the start of the acclimation period and were subsequently allowed to filter natural sea water.
Figure 1.
(a) Velvet crab (Necora puber), (b) blue mussels (Mytilus edulis) and (c,d) bladderwrack (Fucus vesiculosis). Photos: (a) J.M. Booth, (b) E. Chapman, (c,d) C. Rochas. (Online version in colour.)
Two experiments (oxygen supersaturation and diel oxygen fluctuation—details below) were performed in a photoperiod- and temperature-controlled room, using separate treatment aquaria (110 l) for each experiment filled with ambient UV-treated seawater (salinity: 34.23–34.38 ppt). All aquaria were equipped with a PME miniDOT dissolved oxygen and temperature logger and light sensor (ONSET HOBO - UA-002-08). Water temperature in each aquarium was controlled with two thermometers (Aquastar, Germany) and two heating rods (Aquastar, Germany) connected to a control system (IKS Aquastar, Germany).
Oxygen was supplied to tanks either in the form of an air bubbler (100% oxygen saturation) or via the photosynthetic activity of macroalgae (oxygen supersaturation treatment and diel oxygen fluctuation treatment). Fresh, fertile macroalgae (figure 1c,d), Fucus vesiculosis (Linnaeus, 1753) (bladderwrack), was collected on the first day of the experiment in Coldingham Bay (0.5 km south of St Abbs harbour) and rinsed in UV-treated seawater to remove epibionts, and the same wet weight of algae (2 kg, measured on a balance) was added to each aquarium allocated to the oxygen supersaturation treatment (Experiment 1) and the diel oxygen fluctuation treatment (Experiment 2). Two water pumps (Q116 aquarium pump, 320 l h−1) ensured circulation of oxygen within each aquarium for all treatments. LED growth lamps (KINGBO, 400–760 nm full spectrum) were set up over each aquarium, including the 100% oxygen saturation treatments, to promote algal photosynthesis (light intensity was recorded as 5000 lx ±500 in both experiments). Lastly, mussels (in a protective cage, to avoid disturbance from crabs) and crabs (free-swimming) were added to each treatment aquarium. Algae and aquarium brushes provided shelter for individual crabs to prevent aggressive intraspecific behaviour.
(b) . Experiment 1—thermal response under constant oxygen supersaturation
This experiment was performed to test the effect of naturally occurring oxygen supersaturation on the respiration and thermal response of metabolism of the two coastal invertebrates, using primary producers as the source of oxygen supersaturation. Animals were acclimated in treatment aquaria (see above) under 100% oxygen saturation (air bubbler) or oxygen supersaturation (algae), and both treatments were under permanent light conditions at ambient temperature (9°C) for 24 h, before animals were transferred to Perspex custom-made respirometry chambers equipped with an oxygen sensor spot glued to the inner wall. Prior to being transferred to the chambers, animals were cleaned with sterile seawater to help remove epibionts and microorganisms. Animals were acclimated for 12 h in the respirometry chambers, under light conditions, to recover from handling stress, at treatment oxygen levels (i.e. oxygen supersaturation (160% saturation) or 100% saturation), supplied by flow-through water from their respective treatment aquaria using pumps (Eheim, Germany), before starting a temperature ramp of 1°C per hour (following [7], [26]) from 9–24°C. Oxygen consumption (hereafter referred to as MO2 in the Methods and Results) was recorded using intermittent respirometry at 9°C, 14°C, 19°C and 24°C for each animal in each treatment (n = 8, i.e. eight respiration chambers with one mussel each and eight chambers with one crab each for 100% oxygen saturation and oxygen supersaturation). MO2 was measured by connecting each closed chamber, via an optical fibre, to a single-channel oxygen transmitter Fibox (Microx) 4 (PreSens, Regensburg, Germany). To avoid disturbance to animals, chambers were covered in dark foil and positioned so that the optical fibre could be connected without subjecting animals to visual stimuli or movement. MO2 was calculated as the linear decline in oxygen saturation in chambers. During measurements, while chambers were closed, oxygen saturation was not allowed to drop below 10% of the saturation level of the corresponding treatment; the duration of measurement was approximately 30 s. All tubes and connectors were rinsed with bleach (10%) and UV-treated filtered seawater between each experimental run to remove any microorganisms that could affect oxygen consumption measurements. An empty chamber provided a control for microbial respiration at each temperature (following Fusi et al. [26]), which was found to account for less than 0.4% of animal oxygen consumption.
After measuring MO2 at 24°C, animals were carefully removed from their chambers. Haemolymph, approximately 200 µl, was extracted from crabs from the arthrodial membrane at the base of a fifth walking leg with a 25-gauge needle for measurement of haemocyanin concentration [27]. Haemocyanin concentrations were calculated by diluting 10 µl haemolymph with 990 µl chilled oxygenated buffer (Tris-HCl Buffer pH 7.4 50 mM), before reading absorbance spectrophotometrically (Helios Epsilon, Thermo Fisher Scientific; 335 nm wavelength; [28]), three times for each sample. Haemocyanin concentration was calculated following Harris & Andrews [29], using the molar extinction coefficient E1cm mM = 17.26. Handling time from removing the animal from the chamber to completing haemolymph extraction was kept to 60 s. In order to obtain the internal volume of each respiration chamber, animals were weighed, and their volume calculated by means of water displacement in a graduated cylinder before release. No deaths were recorded during acclimation, experiments or handling.
(c) . Experiment 2—thermal response under diel oxygen fluctuation
This experiment was performed to test the effect of diel oxygen fluctuation on the respiration and thermal response of metabolism of the two coastal marine invertebrates. For this second experiment, we exposed one set of animals (n = 16 mussels and n = 16 crabs) to diel oxygen fluctuation (achieved with the use of a growth lamp set to a 12 h : 12 h light : dark cycle, and setting the room lighting to the same cycle) in aquaria with macroalgae, and another set of animals (n = 16 mussels and n = 16 crabs) exposed to constant 100% oxygen saturation provided only with an air bubbler but no algae (electronic supplementary material, figure S2). Animals were exposed to their respective treatments for 6 days prior to measurements, and the experiment was replicated at 9°C, 16°C and 21°C using new animals for each temperature (i.e. a total of 48 of each crabs and mussels). For the treatment tanks at 16°C and 21°C, animals were gradually acclimated to the higher temperatures at a warming rate of 0.5°C per hour. The room temperature was initially maintained at 9°C and subsequently increased to mirror that of the experimental temperature. The oxygen levels in the diel oxygen fluctuation tank varied between 30% and 180% during the experiment, and in the 100% saturation tanks oxygen levels were 100% (±4%; electronic supplementary material, figure S3). Every 2 days, half of the aquarium water was replaced with fresh UV-treated seawater, first heated to the correct temperature, to ensure animals and oxygen levels were not detrimentally affected by a build-up of urea (pH was monitored daily) or a loss of nutrients hindering photosynthesis.
As for Experiment 1, animals were transferred to respirometry chambers and allowed to recover from disturbance for 12 h prior to measurements, and conditions in the chambers were identical to those in the respective treatment tanks, with a water pump continuously circulating water between the tanks and chambers. MO2 was measured, as described above, at the beginning of the light phase of the diel cycle after overnight (12 h) acclimation in individual respiration chambers, at the point where oxygen saturation levels were identical between the two treatments, i.e. 100% oxygen saturation. After measuring MO2 for each individual animal, chambers were kept closed and MO2 was recorded every 2 min as oxygen decreased in each chamber to 5–10% saturation in order to calculate the critical oxygen pressure, the partial oxygen pressure below which oxygen consumption significantly declines, hereafter referred to as PO2crit.
Haemocyanin and lactate were measured from the haemolymph of the eight crabs which were not placed in the respirometry chambers from each treatment and temperature after the 6-day acclimation to diel oxygen fluctuation. Haemolymph could not be taken from the same animals used for MO2 measurements because these individuals were used for the measurement of PO2crit. Haemocyanin was measured following the protocol described above. Lactate concentration was measured using a drop of venous haemolymph (extracted as described above), following Giomi et al. [7] with a Lactate Pro 2 Analyser (www.lactatepro.com.au).
(d) . Statistical analysis
PO2crit was calculated by plotting MO2 against PO2, using a piecewise linear regression function in SigmaPlot v. 11, then calculating the breakpoint (following Giomi et al. [7]).
To test MO2 under oxygen supersaturation, an analysis of covariance was performed using a linear mixed model (lme4) to test the effects of the factors ‘Temperature’ (as our continuous explanatory variable) and ‘Treatment’ (fixed, 2 levels: 100% oxygen saturation, oxygen supersaturation) with MO2 as our response variable. Individual ID was included as a random factor in the mixed model to account for the non-independence of repeated measures across the temperature ramp.
A one-way ANOVA was used to test the effect of ‘Treatment’ (fixed, two levels) on the dependent variable haemocyanin at 24°C (crabs only). To explore thermal response under oxygen diel fluctuation, an analysis of covariance was used to test the effects of ‘Temperature’ (as our continuous explanatory variable) and the factor ‘Treatment’ (fixed, two levels: constant 100% oxygen saturation, diel oxygen fluctuation) on the response variables MO2, PO2crit, haemocyanin (crabs only) and lactate (crabs only). Prior to statistical testing, normality and homogeneity of variances of the data were confirmed using the Shapiro–Wilk's and Levene's tests, respectively. All statistical tests were performed in R (R Studio v. 1.1.463).
3. Results
In both experiments, a significant interaction between temperature and treatment was observed in the majority of cases. In general, oxygen treatment significantly affected the variables tested at intermediate to high temperatures, but not at low temperatures.
(a) . Experiment 1—thermal response of metabolism under constant oxygen supersaturation
Crab oxygen consumption (MO2) was affected by a significant temperature × oxygen treatment interaction (second polynomial regression analysis, F2,58 = 4.11, p < 0.05; electronic supplementary material, table S1). Overall crab MO2 was highest at 14°C and 19°C, and at these two intermediate temperatures, individual crabs exposed to oxygen supersaturation had a significantly higher MO2 than those exposed to 100% oxygen saturation (figure 2a). Mussel MO2 was found to be affected by a significant temperature × oxygen treatment interaction (second polynomial regression analysis, F2,58 = 19.94, p < 0.0001; electronic supplementary material, table S1). The same pattern was observed as for crabs, with overall MO2 highest at 14°C and 19°C and individuals exposed to oxygen supersaturation had a significantly higher MO2 than those exposed to 100% oxygen saturation at these temperatures (figure 2b).
Figure 2.
Oxygen consumption (MO2) by (a) Necora puber and (b) Mytilus edulis over a temperature ramp from 9°C to 24°C under 100% oxygen saturation (red) and constant oxygen supersaturation (blue). Data represent MO2 in µmol per gram wet weight per hour. (Online version in colour.)
Crabs produced significantly higher levels of haemocyanin at 24°C when exposed to oxygen supersaturation than 100% oxygen saturation (figure 3; one-way ANOVA, F1,14 = 31.53, p < 0.0001; electronic supplementary material, table S1).
Figure 3.

Haemocyanin concentrations in Necora puber haemolymph after a temperature ramp from 9°C to 24°C under 100% oxygen saturation (red) and constant oxygen supersaturation (blue). Asterisks represent significant differences between the treatments (p < 0.05). (Online version in colour.)
(b) . Experiment 2: thermal response of metabolism under diel oxygen fluctuation
Crab and mussel oxygen consumption (MO2) were both significantly affected by a temperature × oxygen treatment interaction (second polynomial regression analysis, F2,41 = 6.41, p < 0.01 and F2,42 = 6.82, p < 0.01, respectively; electronic supplementary material, table S2). When exposed to diel fluctuation in oxygen, both crabs and mussels had significantly higher MO2 at 16°C and 21°C, compared to animals exposed to constant 100% oxygen saturation (figure 4a,b).
Figure 4.
Oxygen consumption (MO2) by (a) Necora puber and (b) Mytilus edulis and PO2crit in (c) Necora puber and (d) Mytilus edulis at 9°C, 16°C and 24°C under 100% oxygen saturation (red) diel oxygen fluctuation (O2 DF, blue) after 6 days exposure to treatment. Data represent MO2 in µmol per gram wet weight per hour. (Online version in colour.)
Due to the switch to anaerobic metabolism at 21°C, PO2crit was analysed for the temperatures below this, i.e. 9°C and 16°C. Crab PO2crit was significantly affected by a temperature × oxygen treatment interaction (linear model, F1,28 = 53.29, p < 0.0001; electronic supplementary material, table S2). At 16°C, crabs exposed to diel oxygen fluctuation had a significantly lower PO2crit than those exposed to constant 100% oxygen saturation (figure 4c). Mussel PO2crit was unaffected by either temperature or oxygen fluctuation or their interaction (figure 4d).
Crab lactate was significantly affected by a temperature × oxygen treatment interaction (linear model, F1,44 = 127.49, p < 0.001; electronic supplementary material, table S2); those exposed to diel fluctuation in oxygen had significantly lower lactate concentrations at 16°C and 21°C than crabs exposed to constant 100% oxygen saturation (figure 5a). Lactate could not be detected in mussel haemolymph.
Figure 5.
(a) Lactate and (b) haemocyanin concentration in Necora puber haemolymph at 9°C, 16°C and 24°C under 100% oxygen saturation (red) and diel oxygen fluctuation (O2 DF, blue) after 6 days exposure to treatment. (Online version in colour.)
Crab haemocyanin was also significantly affected by a temperature × oxygen treatment interaction (linear model, F1,44 = 6.33, p < 0.05; electronic supplementary material, table S2). Crabs exposed to diel fluctuation in oxygen had significantly higher haemocyanin levels at 21°C than crabs exposed to constant 100% oxygen saturation (figure 5b; Tukey p-pht, p < 0.001).
4. Discussion
Primary producer communities in shallow coastal waters offer several crucial ecosystem services to their associated animal communities. They provide a pH-controlled environment that can mitigate the effects of ocean acidification [30] and reduce pathogen activity through the production of biocides [14]. Here, we show that natural diel oxygen fluctuation and oxygen supersaturation due to photosynthesis drive changes in the sensitivity of ectotherm metabolic rate to temperature. Our findings highlight that the current experimental standards may be biased by the fact that animals are typically tested under ecologically unrealistic constant oxygen levels, while oxygen availability is actually highly variable, especially in productive coastal areas.
Ectotherms commonly sustain aerobic metabolism when faced with thermal stress, thus meeting the increased oxygen demand induced by heat [24,25,31]. Natural levels of oxygen at the Scottish study location can reach around 160% saturation due to photosynthesis (electronic supplementary material, figure S1). In our experiments, blue mussels and velvet crabs experiencing such levels of oxygen supersaturation showed increased metabolic rates under warming compared to animals in the absence of algae and experiencing constant oxygen levels at around 100% saturation (Experiment 1). Importantly, significant differences between oxygen treatments appeared as temperatures rose above 9°C, with increased metabolic rate in the study species recorded only under relatively high temperatures (beyond 14°C). Both mussels and crabs were able to maximize their metabolic activity under oxygen supersaturation at these temperatures, while no effect on animal metabolic rate was seen at low temperatures (9°C). Tropical animals kept under constant oxygen supersaturation showed a similar response when exposed to higher than ambient temperatures [7].
We found that exposure to diel fluctuation in the oxygen environment, including extremes of oxygen supersaturation and undersaturation, modified the metabolic performance of crabs at elevated temperatures by increasing rates of oxygen uptake (MO2, Experiment 2). Crabs exposed to diel oxygen fluctuation had a lower PO2crit than those exposed to 100% oxygen saturation at 16°C, indicating a more efficient ability to extract dissolved oxygen at a lower environmental oxygen tension. While at 9°C animals could largely sustain oxygen metabolic demands, 16°C represented a rarely encountered condition for these temperate crabs. Water in this region only reaches this temperature on a few hot summer days (Marine Scotland, https://data.marine.gov.scot/dataset/scottish-coastal-observatory-st-abbs-site). Although our study was performed on animals acclimated to colder winter temperatures, and experimental timing may have underestimated the thermal sensitivity of these species, qualitative responses to temperature would likely be comparable in the warmer summer months as has been demonstrated for tropical species inhabiting warm environments [7].
Our measurements of haemocyanin and lactate levels likewise indicate an increased metabolic response to temperature under conditions of oxygen supersaturation (Experiment 1) and diel oxygen fluctuation (Experiment 2). Haemocyanin is the oxygen-carrying protein in a number of crustaceans and molluscs and critical for normal physiological function [32]. Environmental factors affect haemocyanin concentrations in blue crabs (Callinectus sapidus), with low salinity and oxygen undersaturation causing a decrease in haemocyanin [32]. In another crustacean, the Norway lobster (Nephrops norvegicus), the extent to which oxygen undersaturation resulted in an increase in haemocyanin was crucially dependent on both initial haemocyanin levels, so that individuals which had an initially high haemocyanin level showed no change, or even a decrease in haemocyanin [33]. This decrease was linked to energy allocation, i.e. haemocyanin is regulated to the minimum level required for successful respiratory gas transport so that the energy required for protein synthesis may be allocated to more essential processes than the production of an excess of haemocyanin [34]. A relationship between thermal tolerance and haemolymph oxygen transport was also found in the eurythermal crab Carcinus maenas [27], providing evidence that oxygen storage by haemocyanin has an increasingly important role in sustaining cardiac performance under warming by enhancing aerobic metabolism and increasing thermal tolerance. In our study, velvet crab haemocyanin was unaffected at temperatures that these animals naturally experience in the field. At average temperatures, and in fully oxygenated seawater, portunid crabs rely on the oxygen dissolved in haemolymph alone [27]. In cases where we observed an increase in haemocyanin concentration during oxygen supersaturation, or diel oxygen fluctuation, we interpret this as a molecular mechanism to increase the oxygen scavenging efficiency of the whole system.
Lactate is a stress marker in many invertebrates and is commonly used as an indicator of anaerobic respiration resulting from hypoxic conditions [35], thermal stress [7,36] or the combination of the two [37]. High levels of lactate indicate that an animal is relying increasingly on anaerobic metabolism, likely associated with more stressful conditions [38]. We found that velvet crabs exposed to constant 100% oxygen saturation at temperatures elevated above ambient, specifically 16°C and 21°C, displayed significantly higher lactate levels than those exposed to diel oxygen fluctuation. As with the results for metabolic rate, this clearly indicates that these crabs experience less physiological stress at higher temperatures under conditions of cyclical diel oxygen fluctuation in water from under- to over-saturation.
Mussel metabolic rates were affected by temperature and/or oxygen level in a similar manner to those of crabs. However, in contrast with the crabs, mussel PO2crit was unaffected by either temperature or oxygen treatment. The ability of these sedentary animals to close their shells for extended periods, depressing their metabolism or relying on anaerobic pathways, provides an alternative strategy for coping with low-oxygen availability, for example, during low tide, from that of highly active species, such as crabs, which strive to maintain their metabolic rates [18]. Oxygen saturation levels of 20% have been previously found to have no effect on the resting metabolic rate of blue mussels from the southern Baltic Sea, but did affect gaping activity [39]. Mussels have evolved under highly variable oxygen conditions in which regular submersion and emersion are superimposed on diel fluctuations in oxygen tension, and a constant oxygen environment is not a natural setting for them. Although constant 100% oxygen saturation is not detrimental to mussels, as demonstrated in the vast majority of studies adopting steady rearing conditions, diel oxygen fluctuation led to a larger scope of metabolic rate, which in turn determines a more efficient capacity for thermal response [18]. To our knowledge, this important aspect is not incorporated into published studies based on conditions of 100% oxygen saturation.
Animals living in marine habitats exhibiting high primary productivity have evolved in an inherently dynamic environment, particularly in terms of oxygen availability, and many species, including those in our study, have evolved in close association with primary producers under these fluctuating environmental conditions. These animals are physiologically adapted to cope with the predictable variability in their environment [10,18,20]; critically, their metabolic performance is tailored to oxygen variation, resulting from changing temperature and levels of photosynthesis. We demonstrate that assessments of animal physiology and thermal response under warming should account for ecologically relevant oxygen variability rather than employing a stable experimental oxygen level, but studies so far have not done so [20].
Coastal animals are adapted to persist in a naturally variable environment, having evolved strategies to exploit predictable environmental change and mechanisms to anticipate future expected changes [40]. We suggest that the species investigated in our study, and likely the majority of coastal ectotherms, normally exploit predictable daily oxygen supersaturation to cope with nightly oxygen undersaturation. However, the environment is being altered at an unusual rate due to anthropogenic activity, compromising feedback mechanisms, and the ability of communities to adapt to different fluctuation regimes remains overlooked [40]. Interestingly, the importance of behavioural and evolutionary mechanisms involved in the plasticity of species' thermal tolerance is unrelated to latitude or thermal seasonality, and it has been proposed that in cases where species are limited in their behavioural thermoregulation, greater plasticity in physiological traits will be favoured [41], it is possible that exposure to environmental fluctuations contributes to this.
The intensified response of coastal fauna to higher temperatures driven by oxygen supersaturation mediated by primary producers for parts of the day shown here is foreseen to become increasingly important under future climate change. While primary producers will have their own specific responses to ocean warming and acidification, it is likely that coastal habitats such as seagrasses, kelp forests, mangroves and coral reefs will be important as refugia in which oxygen variation can drive the metabolic performance of animals in a changing world. Upwelling areas have already been identified as climate refugia for marine macroalgae [42], as these areas show comparatively lower trends of warming. The thermal response of plants and animals results from the complex interaction of several factors, beyond temperature alone. Here, we demonstrate that the provision, and resultant variability, of oxygen by primary production are important drivers of the thermal responses of coastal animals. By producing periodic oxygen supersaturation, coastal primary producers sustain the increasing metabolic demand of animals under warming, and are therefore likely to have an increasingly important effect on both permanent residents and transient animals that use these habitats as nursery sites under climate warming (e.g. [43]). This makes the loss of macrophytes through ocean heatwaves and long-term warming [44], which will increase with further ocean warming, detrimental to the associated biota [45]. The disappearance of diverse communities of macroalgae in coastal waters is a threat to biodiversity not only through habitat loss [46,47], but also through reduced oxygen variability and the effects of this on animal thermal responses.
Supplementary Material
Acknowledgements
The authors thank Kevin Scott, Adam Houghton, Blair Easton and Petra Harsanyi from the St Abbs Marine Station for advice and logistical support, and fishermen and volunteers for assistance collecting animals and algae. We are also grateful to W. Verberk and an anonymous reviewer for their useful suggestions to improve the final version of the manuscript.
Contributor Information
J. M. Booth, Email: jen.marie.booth@gmail.com.
M. Fusi, Email: m.fusi@napier.ac.uk.
Data accessibility
The data are provided in the electronic supplementary material [48].
Authors' contributions
J.M.B.: conceptualization, data curation, formal analysis, investigation, methodology, project administration, writing-original draft, writing-review and editing; M.F.: conceptualization, data curation, formal analysis, investigation, methodology, writing-original draft, writing-review and editing; F.G.: conceptualization, formal analysis, writing-review and editing; E.C.N.C.: data curation, writing-review and editing; K.D.: conceptualization, funding acquisition, project administration, resources, supervision, writing-review and editing; C.D.M.: conceptualization, funding acquisition, supervision, writing-original draft, writing-review and editing
All authors gave final approval for publication and agreed to be held accountable for the work performed therein.
Competing interests
We declare we have no competing interests.
Funding
This work is based upon research supported by the National Research Foundation of South Africa (grant no. 64801) and by Edinburgh Napier University (Research Excellence Grant Scheme, School of Applied Sciences).
References
- 1.Schmidtko S, Stramma L, Visbeck M. 2017. Decline in global oceanic oxygen content during the past five decades. Nature 542, 335-339. ( 10.1038/nature21399) [DOI] [PubMed] [Google Scholar]
- 2.Limburg KE, Breitburg D, Swaney DP, Jacinto G. 2020. Primer ocean deoxygenation: a primer. One Earth 2, 24-29. ( 10.1016/j.oneear.2020.01.001) [DOI] [Google Scholar]
- 3.Breitburg D, et al. 2018. Declining oxygen in the global ocean and coastal waters. Science 359, 46. ( 10.1126/science.aam7240) [DOI] [PubMed] [Google Scholar]
- 4.Cloern JE, et al. 2016. Human activities and climate variability drive fast-paced change across the world's estuarine–coastal ecosystems. Glob. Chang. Biol. 22, 513-529. ( 10.1111/gcb.13059) [DOI] [PubMed] [Google Scholar]
- 5.Cornwall CE, Hepburn CD, Mcgraw CM, Currie KI, Pilditch CA, Hunter KA, Boyd PW, Hurd CL, Boyd PW, Hurd CL. 2013. Diurnal fluctuations in seawater pH influence the response of a calcifying macroalga to ocean acidification. Proc. R. Soc. B 280, 20132201. ( 10.1098/rspb.2013.2201) [DOI] [PMC free article] [PubMed] [Google Scholar]
- 6.Shaw EC, Mcneil BI, Tilbrook B, Matear R. 2013. Anthropogenic changes to seawater buffer capacity combined with natural reef metabolism induce extreme future coral reef CO2 conditions. Glob. Chang. Biol. 19, 1632-1641. ( 10.1111/gcb.12154) [DOI] [PubMed] [Google Scholar]
- 7.Giomi F, Barausse A, Duarte CM, Booth J, Agusti S, Saderne V, Anton A, Daffonchio D, Fusi M. 2019. Oxygen supersaturation protects coastal marine fauna from ocean warming. Sci. Adv. 5, eaax1814. ( 10.1126/sciadv.aax1814) [DOI] [PMC free article] [PubMed] [Google Scholar]
- 8.Craig H, Hayward T. 1987. Oxygen supersaturation in the ocean: biological versus phyical contributions. Science 235, 199-202. ( 10.1126/science.235.4785.199) [DOI] [PubMed] [Google Scholar]
- 9.Hendriks IE, Duarte CM, Alvarez M. 2010. Vulnerability of marine biodiversity to ocean acidification: a meta-analysis. Estuar. Coast Shelf Sci. 86, 157-164. ( 10.1016/j.ecss.2009.11.022) [DOI] [Google Scholar]
- 10.Harley CDG, Hughes AR, Kristin M, Miner BG, Sorte CJB, Carol S. 2006. The impacts of climate change in coastal marine systems. Ecol. Lett. 9, 228-241. ( 10.1111/j.1461-0248.2005.00871.x) [DOI] [PubMed] [Google Scholar]
- 11.Sievers M, et al. 2019. The role of vegetated coastal wetlands for marine megafauna conservation. TREE 34, 807-817. [DOI] [PubMed] [Google Scholar]
- 12.Mumby PJ, et al. 2003. Mangroves enhance the biomass of coral reef fish communities in the Caribbean. Nature 158, 533-536. [DOI] [PubMed] [Google Scholar]
- 13.Sheaves M, Baker R, Nagelkerken I, Connolly RM. 2015. True value of estuarine and coastal nurseries for fish: incorporating complexity and dynamics. Estuaries Coasts 38, 401-414. ( 10.1007/s12237-014-9846-x) [DOI] [Google Scholar]
- 14.Lamb JB, Water JAJM, Van de Bourne DG, Altier C, Hein MY, Fiorenza EA, Abu N, Jompa J, Harvell CD. 2017. Seagrasses ecosystems reduce exposure to bacterial pathogens of humans, fishes and invertebrates. Science 355, 731-733. ( 10.1126/science.aal1956) [DOI] [PubMed] [Google Scholar]
- 15.Limatola N, Bertocci I, Chun JT, Musco L, Munari M, Danovaro R, Santella L. 2020. Oxygen supersaturation mitigates the impact of the regime of contaminated sediment reworking on sea urchin fertilization process. Mar. Env. Res. 158, 104951. ( 10.1016/j.marenvres.2020.104951) [DOI] [PubMed] [Google Scholar]
- 16.Chiarore A, et al. 2020. Sea urchin chronicles. The effect of oxygen super-saturation and marine polluted sediments from Bagnoli-Coroglio Bay on different life stages of the sea urchin Paracentrotus lividus. Mar. Environ. Res. 159, 104967. ( 10.1016/j.marenvres.2020.104967) [DOI] [PubMed] [Google Scholar]
- 17.Lardies MA, Fernández M. 2002. Effect of oxygen availability in determining clutch size in Acanthina monodon. Mar. Ecol. Prog. Ser. 239, 139-146. ( 10.3354/meps239139) [DOI] [Google Scholar]
- 18.Pörtner H. 2010. Oxygen- and capacity-limitation of thermal tolerance: a matrix for integrating climate-related stressor effects in marine ecosystems. J. Exp. Biol. 213, 881-893. ( 10.1242/jeb.037523) [DOI] [PubMed] [Google Scholar]
- 19.Mcarley TJ, Sandblom E, Herbert NA. 2021. Fish and hyperoxia—from cardiorespiratory and biochemical adjustments to aquaculture and ecophysiology implications. Fish Fish. 22, 324-355. ( 10.1111/faf.12522) [DOI] [Google Scholar]
- 20.Kroeker KJ, Bell LE, Toy JA, Donham EM, Hoshijima U, Norton EW. 2020. Ecological change in dynamic environments: accounting for temporal environmental variability in studies of ocean change biology. Glob. Chang. Biol. 26, 54-67. ( 10.1111/gcb.14868) [DOI] [PubMed] [Google Scholar]
- 21.Cadiz L, Ernande B, Quazuguel P, Servili A, Mazurais D. 2018. Moderate hypoxia but not warming conditions at larval stage induces adverse carry-over effects on hypoxia tolerance of European sea bass (Dicentrarchus labrax) juveniles. Mar. Environ. Res. 138, 28-35. ( 10.1016/j.marenvres.2018.03.011) [DOI] [PubMed] [Google Scholar]
- 22.Diaz RJ, Neubauer RJ, Schaffner LC, Pihl L, Baden SP. 1992. Continuous monitoring of dissolved oxygen in an estuary experiencing periodic hypoxia and the effect of hypoxia on macrobenthos and fish. In Marine coastal eutrophication (eds Vollenweider RA, Marchetti R, Viviani R), pp. 1055-1068. Amsterdam, The Netherlands: Elsevier Science. [Google Scholar]
- 23.Chan HY, et al. 2008. Prolonged exposure to low dissolved oxygen affects early development and swimming behaviour in the gastropod Nassarius festivus (Nassariidae). Mar. Biol. 153, 735-743. ( 10.1007/s00227-007-0850-6) [DOI] [Google Scholar]
- 24.Pörtner HO, Knust R. 2007. Climate change affects marine fishes through the oxygen limitation of thermal tolerance. Science 315, 95-97. ( 10.1126/science.1135471) [DOI] [PubMed] [Google Scholar]
- 25.Schulte PM. 2015. The effects of temperature on aerobic metabolism: towards a mechanistic understanding of the responses of ectotherms to a changing environment. J. Exp. Biol. 218, 1856-1866. ( 10.1242/jeb.118851) [DOI] [PubMed] [Google Scholar]
- 26.Fusi M, Giomi F, Babbini S, Daffonchio D, McQuaid CD, Porri F, Cannicci S. 2015. Thermal specialization across large geographical scales predicts the resilience of mangrove crab populations to global warming. Oikos 124, 784-795. ( 10.1111/oik.01757) [DOI] [Google Scholar]
- 27.Giomi F, Pörtner H. 2013. A role for haemolymph oxygen capacity in heat tolerance of eurythermal crabs. Front. Physiol. 4, 1-12. ( 10.3389/fphys.2013.00110) [DOI] [PMC free article] [PubMed] [Google Scholar]
- 28.Scott K, Harsanyi P, Lyndon AR. 2018. Baseline measurements of physiological and behavioural stress markers in the commercially important decapod Cancer pagurus (L). J. Exp. Mar. Biol. Ecol. 507, 1-7. ( 10.1016/j.jembe.2018.07.001) [DOI] [Google Scholar]
- 29.Harris RRT, Andrews MB. 2005. Physiological changes in the Norway lobster Nephrops norvegicus (L.) escaping and discarded from commercial trawls on the West Coast of Scotland 1. Body fluid volumes and haemolymph composition after capture and during recovery. J. Exp. Mar. Biol. Ecol. 320, 179-193. ( 10.1016/j.jembe.2004.12.029) [DOI] [Google Scholar]
- 30.Hendriks IE, Olsen YS, Ramajo L, Basso L, Moore TS, Howard J, Duarte CM. 2014. Photosynthetic activity buffers ocean acidification in seagrass meadows. Biogeosciences 11, 333-346. ( 10.5194/bg-11-333-2014) [DOI] [Google Scholar]
- 31.Sokolova IM, Frederich M, Bagwe R, Lannig G, Sukhotin AA. 2012. Energy homeostasis as an integrative tool for assessing limits of environmental stress tolerance in aquatic invertebrates. Mar. Environ. Res. 79, 1-15. ( 10.1016/j.marenvres.2012.04.003) [DOI] [PubMed] [Google Scholar]
- 32.Engel DW. 1993. Hemocyanin concentrations in marine crustaceans as a function of environmental conditions. Mar. Ecol. Prog. Ser. 93, 235-244. ( 10.3354/meps093235) [DOI] [Google Scholar]
- 33.Spicer I, Baden P. 2001. Environmental hypoxia and haemocyanin between-individual variability in Norway lobsters Nephrops norvegicus (L.). Mar. Biol. 139, 727-734. ( 10.1007/s002270100591) [DOI] [Google Scholar]
- 34.Baden SP, Hajansson CL, Spicer J. 2003. Between-individual variation in haemocyanin concentrations in the Norway lobster Nephrops norvegicus following exposure to hypoxia and manganese. Mar. Biol. 143, 267-273. ( 10.1007/s00227-003-1082-z) [DOI] [Google Scholar]
- 35.Durand F, Devillers N, Lallier H. 2000. Nitrogen excretion and changes in blood components during emersion of the subtidal spider crab Maia squinado (L.). Comp. Biochem. Physiol. Part A Mol. Integr. Physiol. 127, 259-271. ( 10.1016/S1095-6433(00)00253-1) [DOI] [PubMed] [Google Scholar]
- 36.Verberk WCEP, Sommer U, Davidson RL, Viant MR. 2013. Anaerobic metabolism at thermal extremes: a metabolomic test of the oxygen limitation hypothesis in an aquatic insect. Integr. Comp. Biol. 53, 609-619. ( 10.1093/icb/ict015) [DOI] [PMC free article] [PubMed] [Google Scholar]
- 37.Giomi F, Raicevich S, Giovanardi O, Pranovi F, Di Muro P, Beltramini M. 2008. Catch me in winter! Seasonal variation in air temperature severely enhances physiological stress and mortality of species subjected to sorting operations and discarded during annual fishing activities. Hydrobiologia 606, 195-202. ( 10.1007/s10750-008-9336-x) [DOI] [Google Scholar]
- 38.Hsia C,AS, Lambertz M, Perry S, Maina J. 2013. Evolution of air breathing: oxygen homeostasis and the transitions from water to land and sky. Compr. Physiol. 3, 849-915. [DOI] [PMC free article] [PubMed] [Google Scholar]
- 39.Jakubowska M, Normant M. 2015. Metabolic rate and activity of blue mussel Mytilus edulis trossulus under short-term exposure to carbon dioxide-induced water acidification and oxygen deficiency. Mar. Freshw. Behav. Physiol. 48, 37-41. ( 10.1080/10236244.2014.986865) [DOI] [Google Scholar]
- 40.Palumbi SR, et al. 2009. Managing for ocean biodiversity to sustain marine ecosystem services. Front. Ecol. Environ. 7, 204-211. ( 10.1890/070135) [DOI] [Google Scholar]
- 41.Bernhardt JR, Connor MIO, Sunday JM, Gonzalez A, Bernhardt JR. 2020. Life in fluctuating environments. Phil. Trans. R. Soc. B 375, 20190454. ( 10.1098/rstb.2019.0454) [DOI] [PMC free article] [PubMed] [Google Scholar]
- 42.Gunderson AR, Stillman JH. 2015. Plasticity in thermal tolerance has limited potential to buffer ectotherms from global warming. Proc. R. Soc. B 282, 20150401. ( 10.1098/rspb.2015.0401) [DOI] [PMC free article] [PubMed] [Google Scholar]
- 43.Lourenco CR, Zardi GI, McQuaid CD, Serrao EA, Pearson GA, Jacinto R, Nicastro KR. 2016. Upwelling areas as climate change refugia for the distribution and genetic diversity of a marine macroalga. J. Biogeogr. 43, 1595-1607. ( 10.1111/jbi.12744) [DOI] [Google Scholar]
- 44.Lilley RJ, Unsworth RKF. 2014. Atlantic cod (Gadus morhua) benefits from the availability of seagrass (Zostera marina) nursery habitat. Glob. Ecol. Conserv. 2, 367-377. ( 10.1016/j.gecco.2014.10.002) [DOI] [Google Scholar]
- 45.Nicastro KR, Zardi GI, Teixeira S, Neiva J, Serrão EA, Pearson GA. 2013. Shift happens: trailing edge contraction associated with recent warming trends threatens a distinct genetic lineage in the marine macroalga Fucus vesiculosus. BMC Biol. 11, 6. ( 10.1186/1741-7007-11-6) [DOI] [PMC free article] [PubMed] [Google Scholar]
- 46.Arias-Ortiz A, et al. 2018. A marine heat wave drives massive losses from the world's largest seagrass carbon stocks. Nat. Clim. Chang. 8, 338. ( 10.1038/s41558-018-0096-y) [DOI] [Google Scholar]
- 47.Duarte CM, et al. 2020. Rebuilding marine life. Nature 580, 39-51. ( 10.1038/s41586-020-2146-7) [DOI] [PubMed] [Google Scholar]
- 48.Booth JM, Fusi M, Giomi F, Chapman ECN, Diele K, McQuaid CD. 2021. Data from: Diel oxygen fluctuation drives the thermal response and metabolic performance of coastal marine ectotherms. Figshare. [DOI] [PMC free article] [PubMed]
Associated Data
This section collects any data citations, data availability statements, or supplementary materials included in this article.
Data Citations
- Booth JM, Fusi M, Giomi F, Chapman ECN, Diele K, McQuaid CD. 2021. Data from: Diel oxygen fluctuation drives the thermal response and metabolic performance of coastal marine ectotherms. Figshare. [DOI] [PMC free article] [PubMed]
Supplementary Materials
Data Availability Statement
The data are provided in the electronic supplementary material [48].




