ORIGINAL RESEARCH article
Sec. Global Change and the Future Ocean
Volume 1 - 2014 | https://doi.org/10.3389/fmars.2014.00062
Impact of ocean acidification and warming on the Mediterranean mussel (Mytilus galloprovincialis)
- 1Sorbonne Universités, Université Pierre et Marie Curie Univ Paris 06, Unité Mixte de Recherche 7093, Laboratoire d'Océanographie de Villefranche, Villefranche/Mer, France
- 2Centre National de la Recherche Scientifique, Unité Mixte de Recherche 7093, Laboratoire d'Océanographie de Villefranche, Observatoire Océanologique, Villefranche/Mer, France
- 3Alfred-Wegener-Institute Helmholtz Zentrum für Polar und Meeresforschung, Am Handelshafen 12, D-27570 Bremerhaven, Germany
- 4Sorbonne Universités, Université Pierre et Marie Curie Univ Paris 06, Unité Mixte de Recherche 8222, Laboratorio de Ecofisiología para la Conservación de Bosques, Observatoire Océanologique, Banyuls/mer, France
- 5Centre National de la Recherche Scientifique, Unité Mixte de Recherche 8222, Laboratorio de Ecofisiología para la Conservación de Bosques, Observatoire Océanologique, Banyuls/mer, France
- 6GeoZentrum Nordbayern, Universität Erlangen-Nürnberg, Erlangen, Germany
- 7German University of Technology in Oman, Halban Campus, Muscat, Sultanate of Oman
- 8Consejo Superior de Investigaciones Científicas, Institut de Ciencies del Mar, Barcelona, Spain
- 9Universitat Autònoma de Barcelona, Institut de Ciència i Tecnologia Ambientals, Barcelona, Spain
- 10Institució Catalana de Recerca i Estudis Avançats, Barcelona, Spain
In order to assess the effects of ocean acidification and warming on the Mediterranean mussel (Mytilus galloprovincialis), specimens were reared in aquarium tanks and exposed to elevated conditions of temperature (+3°C) and acidity (−0.3 pH units) for a period of 10 months. The whole system comprised a factorial experimental design with 4 treatments (3 aquaria per treatment): control, lowered pH, elevated temperature, and lowered pH/elevated temperature. Mortality was estimated on a weekly basis and every 2 months, various biometrical parameters and physiological processes were measured: somatic and shell growth, metabolic rates and body fluid acid-base parameters. Mussels were highly sensitive to warming, with 100% mortality observed under elevated temperature at the end of our experiment in October. Mortality rates increased drastically in summer, when water temperature exceeded 25°C. In contrast, our results suggest that survival of this species will not be affected by a pH decrease of ~0.3 in the Mediterranean Sea. Somatic and shell growth did not appear very sensitive to ocean acidification and warming during most of the experiment, but were reduced, after summer, in the lowered pH treatment. This was consistent with measured shell net dissolution and observed loss of periostracum, as well as uncompensated extracellular acidosis in the lowered pH treatment indicating a progressive insufficiency in acid-base regulation capacity. However, based on the present dataset, we cannot elucidate if these decreases in growth and regulation capacities after summer are a consequence of lower pH levels during that period or a consequence of a combined effect of acidification and warming. To summarize, while ocean acidification will potentially contribute to lower growth rates, especially in summer when mussels are exposed to sub-optimal conditions, ocean warming will likely pose more serious threats to Mediterranean mussels in this region in the coming decades.
During the last 150 years, human activities, through the combustion of fossil fuels (oil, gas, and coal), have led to a dramatic release of carbon dioxide (CO2) to the Earth's atmosphere. The accumulation of CO2 impacts the radiative forcing, thereby warming the atmosphere and the ocean. The surface ocean has warmed from 1971 to 2010 by 0.11°C per decade (Rhein et al., 2013), with maximal rates recorded on average in the coastal zone (0.18°C; Lima and Wethey, 2012). Depending on the future emission scenario, surface ocean temperatures are projected to warm in the top 100 m by about 0.6 to 2.0°C by 2100 (Collins et al., 2013). The oceans are not only absorbing a large amount of increased heat, but also about 25% of anthropogenic CO2 emissions (Le Quéré et al., 2009). This massive CO2 input greatly impacts seawater chemistry, leaving a surface ocean imprint. These changes are referred to as “ocean acidification” (OA) because increased CO2 lowers seawater pH (i.e., increases its acidity). The pH in ocean surface waters has already decreased by 0.1 units since the beginning of the industrial era, equivalent to an increased acidity of 26%. According to recent projections, an additional decrease is expected by 2100, ranging from 0.06 to 0.32 units, equivalent to an increased acidity of 15–110%, depending on the considered emission scenario (Ciais et al., 2013).
The effects of OA on marine organisms have been studied over the past 20 years (Gattuso and Hansson, 2011), with particular attention to organisms producing calcareous structures. Indeed, while decreasing pH levels are expected to have profound impacts on the physiology and metabolism of marine organisms through a disruption of intercellular transport mechanisms (Pörtner et al., 2004), the seawater pH decrease will also lead to a decrease in the concentration of carbonate ions (CO2−3), one of the building blocks of calcium carbonate (CaCO3), and likely alter the ability of calcifying organisms to precipitate CaCO3 (Gazeau et al., 2007). Being both ecologically and economically important species in the coastal zone, the body of literature on mollusks has grown substantially over recent years (see comprehensive review from Gazeau et al., 2013).
To date, very few studies have considered the impacts of OA in synergy with other environmental stressors such as warming, with contrasting results. Moreover, all these studies considered stable pH and/or temperature conditions although large daily and/or seasonal variations in these parameters are common features of coastal sites (Hofmann et al., 2011). For instance, Mackenzie et al. (2014) reported that Atlantic mussels (Mytilus edulis) were not impacted by a decrease of pH by 0.4 units, while these organisms were highly sensitive to a temperature increase of 4°C. In contrast, Duarte et al. (2014) found that the Chilean mussel (Mytilus chilensis) was able to tolerate an increase in temperature of 4°C for 2 months but that shell growth was significantly affected by a decrease in pH of ~0.2–0.3 units. Additive effects of these two stressors have been highlighted in several studies (Talmage and Gobler, 2011; Hiebenthal et al., 2013) although with large variations between species and even developmental stages (Talmage and Gobler, 2011). Finally, Watson et al. (2012) and Ivanina et al. (2013) reported synergistic effects of these two stressors on the survival of the fluted giant clam (Tridacna squamosa), and on the shell hardness of Eastern oysters (Crassostrea virginica), and hard clams (Mercenaria mercenaria). Interestingly, Ivanina et al. (2013) showed that mortality of oysters was ameliorated under a warmer and more acidified scenario as compared to a warmer scenario only.
The Mediterranean mussel (Mytilus galloprovincialis) is one of the most cultivated bivalve species with a global production that has drastically increased in the last 50 years to reach a value of around 1 million tons in 2011, with China and Spain representing the most important producers: ~700,000 and ~200,000 tons, respectively (FAO, 2014). In the Mediterranean Sea, this bivalve is the third-most cultivated species in terms of production, after Seabass and Seabreams. The production is dominated by Italy and Greece with values in 2011 of ~65,000 and ~20,000 tons, respectively. The Spanish production occurs predominantly on the Atlantic coast (i.e., 98%).
In the northwestern Mediterranean Sea, mean maximum summer temperatures have increased by about 1°C between 2002 and 2010 relative to the 1980–2000 average (Marba and Duarte, 2010) and a rapid warming of 2.8 ± 1.1°C is expected by the end of the century (Jorda et al., 2012). In this region, high summer temperature levels already represent a problem for the rearing of mussels and farmers are obliged to sell their product before summer (Ramón et al., 2005). Moreover, the observed mean rate of OA is similar to that in Atlantic subtropical regions (Orr, 2011), with a 0.05–0.14 decrease in seawater pH since the pre-industrial period (Touratier and Goyet, 2011) and projected to decrease by 0.3 units by the end of the century (Orr, 2011). In addition, Mediterranean coastal marine ecosystems are experiencing the synergistic effects of multiple climatic and non-climatic anthropogenic stressors such as chemical contaminants (The Mermex Group, 2011). In order to assess the potential combined effects of OA and warming on the Mediterranean mussel, we performed laboratory experiments in which mussels were exposed to elevated temperature (+3°C) and acidity (−0.3 pH units) in aquaria flushed with ambient seawater and thus against the background of natural variability for a period of 10 months.
Material and Methods
Biological Material and Experimental Set-up
Mussels with a mean shell length of 45 ± 5 mm were collected in the Delta del Ebro (40°35′59″N; 0°41′21″E) in November 2011 and directly brought to the Institute of Marine Science (Barcelona, Spain). Seawater, pumped from a depth of 10 m at proximity of the institute (300 m from the coast), and filtered onto 50 μm, was continuously supplied to four 100 L header tanks at a minimal rate of 50 L h−1. The whole system comprised a factorial experimental design with 4 treatments (control, lowered pH, elevated temperature, and lowered pH/elevated temperature), and 12 experimental aquaria (30 L) with 3 aquaria per treatment. From each header tank, seawater was delivered by gravity to the three experimental aquaria at a rate of ca. 15 L h−1 per aquarium (checked on a weekly basis with a flow meter). A small pump was installed in each aquarium in order to create some water movement. A total of 120 mussels were haphazardly placed in each aquarium. In the perturbation header tanks, pH and temperature were respectively decreased by 0.1 pH units and increased by 1°C/week over 3 weeks, and thereafter maintained at a pH offset of ~ −0.3 and a temperature offset of ~ +3°C for the duration of the experiment (~10 months). The pH offset was controlled by bubbling pure-CO2 in the corresponding header tanks using a continuous pH-stat system (IKS, Karlsbad, Aquastar). pH electrodes from the pH-stat system were inter-calibrated on a weekly basis using a glass combination electrode (Metrohm, electrode plus) calibrated on the total scale using TRIS buffer solutions with a salinity of 35 (provided by A. Dickson, Scripps Institution of Oceanography, San Diego). The +3°C offset was maintained with thermo-resistances (2 × 500 W per header tank) controlled by a COREMA© temperature-regulation system. Twice a day, the seawater flow was stopped and mussels were fed with a commercial mixture of live Nannochloropsis oculata, Phaeodactylum tricornutum and Chlorella (DT's Live Marine Phytoplankton) at a final concentration of ~4% mussel tissue dry weight, close to ingestion rates measured in situ by Galimany et al. (2011) in the area of collection. Mussel average tissue dry weight was estimated at the start of the experiment by weighing 10 randomly selected mussels after 24 h in an oven at 60°C. Food quantity was adjusted in each aquarium based on the remaining number of mussels and considering a constant average tissue dry weight throughout the experiment. Seawater flow was restored once all phytoplankton had been filtered by the mussels (1–2 h). Mortality of the mussels was recorded, dead mussels were removed and aquaria were cleaned on a weekly basis.
Seawater samples for total alkalinity (AT) measurements were collected once a week in the ambient seawater header tank, filtered on GF/F membranes, immediately poisoned with HgCl2 and analyzed within 2 months at the Laboratoire d'Océanographie de Villefranche (France). AT was determined potentiometrically using a Metrohm titrator (Titrando 80), and a glass electrode (Metrohm, electrode plus) calibrated using first NBS buffers (pH 4.0 and pH 7.0, to check that the slope was Nernstian) and then using TRIS buffer solutions (salinity 35, provided by A. Dickson, Scripps Institution of Oceanography, San Diego). Triplicate titrations were performed on 50 mL sub-samples at 25°C and AT was calculated as described by Dickson et al. (2007). Titrations of standard seawater provided by A. Dickson (batch 106) yielded AT values within 2.4 μmol kg−1 of the nominal value (SD = 1.2 μmol kg−1, n = 32). All parameters of the carbonate chemistry were determined from pHT, AT, temperature and salinity using the R package seacarb (Lavigne et al., 2014).
Biometrics and Physiological Measurements
Every 2 months, various biometrical parameters and physiological processes were measured. Shell length, shell weight and fresh weight were monitored on 20 haphazardly pre-labeled mussels per aquarium. Shell weight was measured using the buoyant weight technique (Spencer Davies, 1989). Net calcification, excretion and respiration rates were measured by incubating 3 haphazardly chosen mussels per aquarium in 300 mL respiration chambers for 3 h. Temperature was maintained at the corresponding level for each treatment by plunging the respiration chambers in tanks with flowing experimental seawater. Mussels were not fed for a period of 6 h before the start of the incubations. Blanks containing only seawater were done at the start and at the end of the 10-month exposure and showed that variations of any of the constituents due to microbial processes were less than 0.5% of the variations observed with mussels (data not shown). Respiration rates were estimated as the rate of oxygen concentrations decrease over the 3 h incubations by means of continuous measurements (1 measurement every 5 s) with fiber-optic oxygen microsensors (PreSens©). Oxygen decrease was always linear during the 3 h incubations and concentrations never dropped below 70% of saturation. Before and after the 3 h incubations, pHT was measured with a glass electrode calibrated using TRIS buffers (see above) and seawater was sampled for the measurements of ammonium (NH4) and AT. pHT decrease during the incubations averaged 0.14 ± 0.05. For NH4, 20 mL of seawater were sampled, filtered on 0.2 μm and immediately frozen at −20°C. Measurements were performed within 2 days at the Institute of Marine Science, using an autoanalyzer. For AT, sampling and measurements were performed as described above. Tissue dry weights of the incubated mussels were measured after 24 h in an oven at 60°C and all rates were expressed as per gram of tissue dry weight (g DW). Net calcification rates were calculated based on the observed difference in AT before and after incubation, corrected for the effect of excretion on AT (Wolf-Gladrow et al., 2007), following the equation:
where G are net calcification rates (in μmol CaCO3 g DW−1 h−1), E are excretion rates (in μmol N g DW−1 h−1) and ΔAT are the observed AT changes (in μmol g DW−1 h−1).
Within a maximum of 5 days from the metabolism measurements, an analysis of haemolymph and extrapallial fluid pH and pCO2 was conducted on another batch of mussels (n = 6 individuals) from all four groups, except in October when no measurements were performed. A volume of 0.2–1 mL of haemolymph and extrapallial fluid was sampled using a syringe equipped with cannulas of 0.6 × 30 and 0.6 × 80 mm size, respectively. The body fluids were transferred directly to Eppendorf caps and placed into a thermostated water bath (Lauda R100) set to the temperature determined in the aquaria prior to sampling. Body fluid pH was measured using a micro pH electrode (Mettler) combined with a pH meter (WTW pH 3310) and calibrated to the specific temperature. Fluid pCO2 were determined by calculation (Pörtner et al., 1990, 2010) from measurements of total CO2 in a carbon dioxide analyzer (Corning 965) operating in a linear range from 0.71 to 11.36 mM using a NaHCO3 standard (1 g L−1) for calibration. The sample volume was 0.1 mL. Total CO2 was determined in relation to standard solutions set to similar concentrations to compensate for a potential drift of the sensor.
At the end of the experimental period, shells from live mussels were sampled for quantification of periostracum cover. As all mussels were dead in the elevated temperature aquaria at the end of the experiment, only shells from the control and the lowered pH treatments were analyzed. Five random specimens from each treatment were used for area quantification and valve dimensions (height, width, and inflation) were additionally measured with a digital caliper as secondary control. Visual inspections of these shells showed areas without periostracum, preferentially in the umbo portions of the shells. In order to quantify systematic differences between the two treatments, the outline of periostracum-free areas and of the shell perimeter were redrawn in CorelDraw from scaled high-resolution pictures, placed on a constant reference area of 1441 × 1441 pixel (equivalent to 10 × 10 cm) and converted into black and white images. Pixel count area quantifications were carried out in ImageJ 1.47v (http://imagej.nih.gov/ij/) and periostracum loss (%) is given relative to the total shell area.
Growth rates (shell weight, shell length, and fresh weight) were compared based on the analyses of variance of linear regression models performed with the R software. Regarding mortality, metabolic rates, and acid-base parameters (haemolymph and extrapallial fluid pCO2 and pH), due to the low number of replicates, permutational multivariate analyses of variance (Permanova) were performed using the R package RVAideMemoire (Hervé, 2014) to test for differences between the 4 treatments. These analyses were performed considering two orthogonal fixed factors (pHT and temperature) and one blocking factor (time) over 1000 permutations and a significant effect was considered when p < 0.05. Differences between control and lowered pH treatments in terms of periostracum cover at the end of the experiment was tested using a non-parametric Mann-Whitney test on R, and considered significant at the risk α = 5%.
Environmental parameters to which the mussels were exposed are presented in Figure 1 and Table 1. Weekly averaged temperature naturally varied between ~12 and ~25°C with minimal levels recorded in February and maximal levels reached in August. Temperature was maintained with mean offsets of respectively 2.7 ± 0.6 and 2.6 ± 0.6°C in the lowered pH/elevated temperature and elevated temperature treatments, as compared to the control. pHT was relatively constant in the ambient pH treatments (8.01 ± 0.04 and 8.01 ± 0.06 in the control and elevated temperature treatments, respectively). In the lowered pH treatments, offsets of −0.31 ± 0.08 and −0.30 ± 0.07 were observed in the lowered pH and lowered pH/elevated temperature treatments, respectively. However, as can be seen in Figure 1, the pH regulation was less efficient in summer (July/August) with observed average offsets of −0.40 ± 0.1 and −0.32 ± 0.1 in the lowered pH and lowered pH/elevated temperature treatments, respectively. Notwithstanding, aragonite saturation states differed among treatments with minimal values in the lowered pH/ambient temperature treatment, but seawater remained oversaturated with respect to this mineral in all treatments during the entire experiment.
Figure 1. Variations of weekly averaged (± SD) temperature (upper panel) and pH (pHT, total scale, lower panel) during the 10-month experiment in the four treatments. The vertical dotted line refers to the start of the experiment when offsets of + 3°C and −0.3 pH units have been reached in the corresponding treatments and the vertical black arrows refer to the sampling periods for biometrics and physiological measurements.
Table 1. Parameters of the seawater carbonate chemistry during the 10-month experiment: temperature (Temp, in°C), pH (pHT, total scale), partial pressure of carbon dioxide (pCO2, in μatm), total inorganic carbon concentration (CT, in μmol kg−1), and saturation state of the seawater with respect to aragonite (Ωa), and calcite (Ωc).
Cumulative mortality rates were below 20% for all treatments until the end of June and started to increase abruptly in the elevated temperature treatments when temperature levels reached ~25°C or more (Figure 2). Temperature was the main driver for this increased mortality (Permanova, p < 0.001, n = 38), with no significant effect of pH, either combined, or in isolation (Permanova, p > 0.05, n = 38, in both cases). In the ambient temperature treatments, regardless of the pH level, mortality rates started to increase after August, when temperature levels also reached ~25°C. A mortality of 100% was recorded by the end of the experiment (October) in the elevated temperature treatments, while in ambient temperature treatments mortality was 60%.
Figure 2. Cumulative number of dead mussels as expressed as a percentage of the initial population (120 individuals per aquarium) in the four treatments during the 10-month experiment. Error bars correspond to standard errors (SE; 3 aquaria per treatment: n = 3).
Growth parameters are presented in Figure 3. Cumulated growth in terms of shell length, fresh weight, and shell weight were relatively small with maximum growth by the end of the experiment of 1.4 ± 0.1 mm, 0.9 ± 0.1 g, and 0.20 ± 0.1 g, respectively. Note that, as all mussels exposed to elevated temperature levels were dead before the last sampling period in October, no data are available for these treatments. We applied linear models to describe these data, revealing that growth in shell length and in fresh weight was not affected by lowered pH or elevated temperature (Table 2). In contrast, growth in shell weight was significantly reduced by both of these perturbations, although without cumulative effects. In October, mussel shell weights even decreased in the lowered pH treatment, a decrease that was accompanied by a decrease in fresh weight and shell length (Figure 3).
Figure 3. Cumulative growth in shell length (mm; upper panel), fresh weight (g, central panel) and shell weight (g; lower panel) in the four treatments during the 10-month experiment. Error bars correspond to standard errors (SE; maximum of 20 measures per aquarium, 3 aquaria per treatment: n = 60 in January and decreases with time due to mortality).
Table 2. Analysis of variance of the linear models fitted to the growth of mussels exposed to the four treatments (n = 932; 5 time points, 2 temperature levels, 2 pH levels).
Respiration, excretion and net calcification rates are presented in Figure 4. As no data were collected in October for mussels exposed to elevated temperature levels (no specimen survived), two distinct Permanova tests have been applied: 1) for all treatments and for the period January to July and 2) for ambient temperature treatments (testing only the effect of lowered pH) for the whole experimental period (see Table 3). Respiration rates significantly increased at elevated temperature (Table 3), and with mean values, for the period January/July, of 21.03 ± 3.3 and 24.2 ± 4.8 μmol O2 g DW−1 h−1 in the ambient and increased temperature treatments, respectively. Excretion rates mean values were 3.3 ± 1.0 μmol N g DW−1 h−1 for all treatments and sampling periods and, as for respiration rates, significantly increased at elevated temperature (2.6 ± 0.7 vs. 3.3 ± 0.9 μmol N g DW−1 h−1 in the ambient and increased temperature treatments, respectively, for the period January/July). Excretion of ammonium was responsible, on average, for 63.3 ± 0.2% of the observed AT variations, and confirmed that a correction of the alkalinity anomaly technique was necessary for this species. Net calcification rates significantly decreased in the lowered pH/elevated temperature treatment. Most of the time, net calcification rates were significantly above 0, except in May and July in the lowered pH/elevated temperature treatment and in October in the ambient pH and lowered pH treatments. In October, negative values (net dissolution) were measured in the lowered pH treatment, however as a consequence of the low replication and large associated errors, the difference between ambient and lowered pH treatments were not statistically significant.
Figure 4. Metabolic rates of mussels exposed to the four treatments during the 10-month experiment. Upper panel: respiration rates, central panel: excretion rates and lower panel: net calcification rates. All rates are expressed as per gram of tissue dry weight (g DW) and per hour. Error bars correspond to standard errors (SE; 1 measure per aquarium, 3 aquaria per treatment: n = 3).
Table 3. Results of the permutational multivariate analyses of variance (Permanova) on metabolic rates and haemolymph/extrapallial fluid pH and pCO2 (n = 54; 4 time points, 2 temperature levels, 2 pH levels).
Figure 5 depicts the pH changes in haemolymph and extrapallial fluid from January to July. The analysis of variance showed a significant impact of seawater pH only for haemolymph pH (Table 3), and no impacts of temperature on both fluids in terms of pH. Except for the mean haemolymph pH of the elevated temperature group, pH in haemolymph and extrapallial fluid started with values below 7.4 in all groups. pH values in all groups increased from January to March, but always remained much lower than seawater pH. After March, pH values in both haemolymph and extrapallial fluid decreased over time, with a larger decrease at lowered pH levels. In July, a large difference (~0.16 units) in extracellular pH of the haemolymph had developed between the two normocapnic groups and the two groups under elevated CO2. Figure 6 presents the corresponding changes in pCO2 in the haemolymph and extrapallial fluid of all groups over time. The changes in pCO2 correlate with the observed changes in pH in both haemolymph and extrapallial fluid (Pearson correlation: r = −0.51, n = 96, and r = −0.37, n = 96, respectively). In contrast to extracellular pH, the analysis of variance showed no significant impact of both temperature and pH for the haemolymph fluid in terms of pCO2 and large variability between replicates (Table 3, Figure 6). Temperature appeared as a significant factor with no cumulative effect of pH for extrapallial pCO2 (Table 3).
Figure 5. pH changes in haemolymph and extrapallial fluid of the four treatments from the four sampling campaigns between January and July. Upper panel: haemolymph pH, lower panel: pH of extrapallial fluid. Error bars correspond to standard errors (SE, 6 measures per aquarium, 3 aquaria per treatment: n = 18).
Figure 6. pCO2 (mm Hg) changes in haemolymph and extrapallial fluid of the four treatments from the four sampling campaigns between January and July. Upper panel: haemolymph pCO2, lower panel: pCO2 of extrapallial fluid. Error bars correspond to standard errors (SE, 6 measures per aquarium, 3 aquaria per treatment: n = 18).
All valves showed shell areas free of periostracum at or near the umbo, which may spread from there toward progressively younger shell portions (Figure 7). Pristine periostracum is rather dark-blue to black, while the periostracum free zones are surrounded by a discolored periostracum with a beige taint. Average periostracum loss for the two treatments for which some mussels were still alive at the end of the experiment was 3.9 ± 1.5% in the control and 16.9 ± 6.7% in the lowered pH treatment. Periostracum discoloration was restricted to a narrow fringe around the periostracum free area in the control treatment, but was significantly increased in the lowered pH treatment (Mann-Whitney test, p = 0.002, n = 10), affecting ~2/3 of the shell area.
Figure 7. Visual comparison of periostracum-free areas of the shell in the two experimental treatments at which some mussels were still alive at the end of the experiment (Control: upper panel and lowered pH treatment: lower panel).
In the present work we tested the effects of OA and warming on growth physiology and survival of the Mediterranean mussel (Mytilus galloprovincialis). For the first time, this species has been exposed to pH and temperature levels that are projected for the end of the century by considering constant offsets of −0.3 pH units and +3°C from ambient conditions. Based on these results, there is no doubt that mussels are highly sensitive to a 3°C warming that leads to suboptimal and even lethal temperature levels in summer. Increased mortality rates were recorded in July, when seawater temperature exceeded ~25°C in the elevated temperature treatment. In this treatment, in August and September, seawater reached ~28°C, and all mussels died within few weeks. It must be stressed that increased mortality was also observed in summer (August and September) in the ambient temperature treatment, corresponding to temperature levels around 25°C. Temperature levels of 24–25°C have been identified, for this species, as an upper limit for normal physiological activities (Anestis et al., 2007, 2010) indicating that Mediterranean mussels already live close to their thermal acclimation limits (Anestis et al., 2007). Total mortality of mussels has been observed in Fangar Bay, located in the area where mussels used in the present study were sampled, when seawater temperature reached 28°C for more than 10 days (Ramón et al., 2007). In the last years, farmers from this area have already adapted their marketing strategy to increased summer temperature by selling their product earlier than in the previous years, thus avoiding the period of heat-induced mortalities (Ramón et al., 2005).
In contrast to warming, our results showed that acidification alone did not induce higher mortalities. The effects of CO2 can be twofold in organisms in environments such as intertidal or shallow subtidal zones. By exerting metabolic depression, CO2 can alleviate the level of stress and delay mortality through more efficient exploitation of energy reserves and passive tolerance. This is not corroborated by our results that do not show any significant delay in mortality at lowered pH levels. Conversely, it has been hypothesized that OA, as an additional stressor, can narrow the thermal window of an organism (Pörtner and Farrell, 2008; Pörtner, 2012), by reducing aerobic performance, i.e., the range of active tolerance. This effect would become visible once the passive tolerance range is exploited sooner and faster at high temperature beyond the critical temperature of 25°C. However, again, this was not observed in our study as the earlier onset in mortality at lowered pH and elevated temperature was not statistically significant. This absence of acidification effects on mussel survival is consistent with results reported by Range et al. (2012) who exposed juveniles of M. galloprovincialis to pH offsets of −0.3 and −0.6 for 84 days and also observed no impact on survival. In contrast, Bressan et al. (2014) observed a slight but significant increase in mortality after 6 months of experiment in the northern Adriatic Sea. However, it must be stressed that they exposed mussels to a much larger decrease in pH (0.7) than the one considered in our study. Our results therefore strongly suggest that survival of this species will not be affected by a pH decrease of ~0.3 in the Mediterranean Sea, predicted to occur within the present century.
According to our results, basic metabolic rates were also not impacted by OA alone while, as expected, they increased at elevated temperature. This is consistent with results from another experiment conducted on this species in the north Adriatic Sea (Range et al., 2014) that showed no effect of a pH decrease of 0.7 on both respiration and excretion rates. These results are not in line with the general theory of increased amino-acid metabolism and their decreased use in growth-related protein synthesis, which seems to be a typical response in marine invertebrates during hypercapnic acidosis (Pörtner et al., 1998; Michaelidis et al., 2005; Thomsen and Melzner, 2010). In another experiment conducted on Mediterranean mussels from the Atlantic coast in Portugal, respiration rates appeared again insensitive to acidification (water pH lowered by 0.3 and 0.6 compared to control treatment), but excretion rates increased at lowered levels of seawater pH (Fernandez-Reiriz et al., 2012).
The capacity of mollusks to compensate for changes in acid–base status due to elevated CO2 is believed to be somewhat limited (Melzner et al., 2009). In our experiment, in all groups, patterns of pH and pCO2 changes were similar in haemolymph and extrapallial fluid, confirming that the carbonate saturation status is similar in both body fluids (Thomsen et al., 2010). All groups displayed similar pH changes between spring and summer, however absolute values were different. The lowest extracellular pH values were observed in the elevated CO2 groups, in line with the low capacity of mussel species for extracellular acid base regulation, as previously observed (e.g., Michaelidis et al., 2005; Thomsen et al., 2010). For both body fluids, pH values displayed large seasonal changes in all groups, possibly reflecting shifting set points over time. The up-regulation of pH in spring (March sampling point), observed in all groups, may reflect transition from winter dormancy to enhanced activity, associated with an increase in the capacity for extracellular acid-base regulation, and likely, overall activity. Indeed, mussels reconstitute their energy reserves during the first quarter of the year before undergoing gametogenesis (Lowe et al., 1982). Furthermore, the seawater temperature from March to April was close to the optimum temperature of the species with critical thermal limits close to 25°C (Anestis et al., 2007). Any temperature change outside the optimum range will increase the baseline energy demand of an ectothermic animal and reduce e.g. the growth performance of the organism (oxygen- and capacity-limited thermal tolerance (OCLTT; see Pörtner, 2010). Accordingly, the later sampling points under elevated seasonal temperatures led to a higher baseline energy demand (Guderley and Pörtner, 2010), visible as increased respiration and excretion rates. Moreover, elevated CO2 concentration caused a significant reduction in pH of the haemolymph in July. An exacerbation of uncompensated extracellular acidosis, in addition to the loss of the periostracum, could explain the negative calcification rates measured in October (see thereafter). Unfortunately, high mortality prevented measurements of extracellular pH during this period. The exacerbation of uncompensated extracellular acidosis, as observed in July, suggests a progressive insufficiency in acid-base regulation capacity at elevated temperatures and pCO2 levels, conditions that will prevail in the future high CO2 ocean, affecting the species at the warm end of their distribution range. However, as will be discussed below, the significant decrease of seawater pH in the lowered pH treatment during this summer period could have been also responsible for these lowered compensation capacities and growth.
Somatic and shell growth did not appear highly sensitive to OA and warming during most of the experiment. It must be stressed that growth was very limited and much lower than what can be measured in aquaculture sites in the Mediterranean Sea (i.e., 20–40 mm yr−1; Sarà et al., 1998). Although feeding rates were calculated based on in situ ingestion rates, maintaining mussels in the laboratory is challenging and optimal growth rates could not be reached with a feeding protocol using only a few phytoplankton species. It appears essential, in order to improve risk assessment for the Mediterranean aquaculture industry and for designing related adaptation strategies, to conduct future perturbation experiments, for instance using FOCE systems (Gattuso et al., 2014), directly in the field near aquaculture sites. Net calcification rates as estimated by a modified alkalinity anomaly technique showed positive values under all treatments during most of the experiment, except after summer when negative values (net dissolution) were measured in the lowered pH treatment. The visual analysis of the shells indeed showed that mussels exposed to lowered pH levels had much larger areas of their shells free of periostracum (Figure 7). This organic layer plays the role of shell protection and can be partially lost as a natural result of abrasion from the bivalve's movements. However, our results suggest, in accordance with findings by Rodolfo-Metalpa et al. (2011), that the periostracum is altered when mussels are exposed to lowered pH conditions. For these mussels, calcitic and aragonitic shell layers were then more exposed to the surrounding seawater and consequently more subject to corrosion, partially explaining the observed net dissolution rates and the decrease of shell weight in low pH treatments after summer. This could reduce the resistance of the shell to mechanical damage, enhancing the risk of predation (Reimer and Tedengren, 1996; Aronhime and Brown, 2009) and of damage by storms and associated wave action (Nehls and Thiel, 1993). Furthermore, although no systematic data have been gathered on this aspect, mussels from all aquaria were able to group and attach to each other with their byssus during most of the experiment, while mussels exposed to low pH conditions after summer were unable to do so and it was possible to easily pick them out of the aquarium individually. This could be due to weaker and less extensible byssal threads for mussels maintained at a lowered pH, as shown by O'donnell et al. (2013) on mussels from the US West coast. Weaker byssal threads negatively affect the ability of mussels to attach to substrate, thereby increasing the probability to be displaced due to hydrodynamic forces generated by storms, which is a significant cause of mortality in the field (Carrington et al., 2009).
Although, as already mentioned, growth was limited in our study, lower net calcification rates, and growth under lowered pH levels in summer have been observed and are consistent with Kroeker et al. (2014) who recently reported significant effects of acidification on M. galloprovincialis shell growth after one month exposure at a pH level maintained at an offset of ~ −0.3 as compared to control conditions. However, this study, conducted over a relatively short exposure time and at lower temperature levels than in our experiment, showed that warming (from 14 to 20°C) mitigated this negative acidification effect as a consequence of both physiological (performances such as calcification increase if warming occurs at temperatures below the thermal optimum, Pörtner, 2012) and chemical (pH and saturation states increase with temperature) effects. Such mitigation effects of warming were not be observed during our study that was conducted under higher temperature levels. In contrast, and more in line with our results, a decrease in shell calcification for this species has been shown as a consequence of synergistic impacts of elevated pCO2 and temperature on the same species by Rodolfo-Metalpa et al. (2011). However, based on our experiment, we cannot elucidate if the decrease in net calcification rates and growth as observed after summer is a consequence of lower pH levels during that period (pH offsets of −0.4 vs. −0.3 during the rest of the experiment) or a consequence of a combined effect of acidification and warming as suggested by Rodolfo-Metalpa et al. (2011).
To conclude, this study is the first focused on the combined effects of warming and acidification on the Mediterranean mussel over seasonal exposure time. Our results strongly suggest that ongoing ocean warming and more frequent summer heat waves will be serious threats to this species in the Mediterranean Sea. All in all, OA does not seem to have very serious impacts on this species in this alkaline region although our results suggest lower growth rates, lower acid-base regulation capacities and significant loss of the periostracum cover in summer coinciding with temperatures beyond optimal levels. Based on the present dataset, the question whether decreased growth capacities are due to a combined effect of OA and warming remains however unresolved. More long-term experiments performed at proximity of aquaculture sites and combining these two stressors are still necessary to improve risk assessment for the Mediterranean aquaculture industry and for designing related adaptation strategies.
Conflict of Interest Statement
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
We like to thank Zora Zittier for her help with the body fluid measurements during the sampling in January, Jean-Pierre Gattuso for help with experimental design and Jean-Olivier Irisson for help with statistics. We wish to thank Claudia R. Benitez-Nelson and Emily Carrington for their constructive reviews. This work was funded by the EC FP7 project “Mediterranean Sea Acidification in a changing climate” (MedSeA; grant agreement 265103), the French program PNEC (Programme national environnement côtier; Institut national des sciences de l'univers) and the EC FP7 project “European Project on Ocean Acidification” (EPOCA; grant agreement 211384).
Anestis, A., Lazou, A., Portner, H. O., and Michaelidis, B. (2007). Behavioral, metabolic, and molecular stress responses of marine bivalve Mytilus galloprovincialis during long-term acclimation at increasing ambient temperature. Am. J. Physiol. Regul. Integr. Comp. Physiol. 293, R911–R921. doi: 10.1152/ajpregu.00124.2007
Anestis, A., Pörtner, H. O., Karagiannis, D., Angelidis, P., Staikou, A., and Michaelidis, B. (2010). Response of Mytilus galloprovincialis (L.) to increasing seawater temperature and to marteliosis: metabolic and physiological parameters. Comp. Biochem. Physiol. A 156, 57–66. doi: 10.1016/j.cbpa.2009.12.018
Bressan, M., Chinellato, A., Munari, M., Matozzo, V., Manci, A., Marèeta, T., et al. (2014). Does seawater acidification affect survival, growth and shell integrity in bivalve juveniles? Mar. Environ. Res. 99, 136–148. doi: 10.1016/j.marenvres.2014.04.009
Carrington, E., Moeser, G. M., Dimond, J., Mello, J. J., and Boller, M. L. (2009). Seasonal disturbance to mussel beds: field test of a mechanistic model predicting wave dislodgment. Limnol. Oceanogr. 54, 978–986. doi: 10.4319/lo.2009.54.3.0978
Ciais, P., Sabine, C., Bala, G., Bopp, L., Brovkin, V., Canadell, J., et al. (2013). “Carbon and other biogeochemical cycles,” in Climate Change 2013: the Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, eds T. F. Stocker, D. Qin, G.-K. Plattner, M. Tignor, S. K. Allen, and J. Boschung, et al. (Cambridge; New York: Cambridge University Press), 465–570.
Collins, M., Knutti, R., Arblaster, J., Dufresne, J.-L., Fichefe, T., Friedlingstein, P., et al. (2013). “Long-term climate change: projections, commitments and irreversibility,” in Climate Change 2013: the Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, eds T. F. Stocker, D. Qin, G.-K. Plattner, M. Tignor, S. K. Allen, J. Boschung, et al. (Cambridge; New York: Cambridge University Press), 1029–1136.
Duarte, C., Navarro, J. M., Acuna, K., Torres, R., Manriquez, P. H., Lardies, M. A., et al. (2014). Combined effects of temperature and ocean acidification on the juvenile individuals of the mussel Mytilus chilensis. J. Sea Res. 85, 308–314. doi: 10.1016/j.seares.2013.06.002
Fernandez-Reiriz, M. J., Range, P., Alvarez-Salgado, X. A., Espinosa, J., and Labarta, U. (2012). Tolerance of juvenile Mytilus galloprovincialis to experimental seawater acidification. Mar. Ecol. Prog. Ser. 454, 65–74. doi: 10.3354/meps09660
Galimany, E., Ramón, M., and Ibarrola, I. (2011). Feeding behavior of the mussel Mytilus galloprovincialis (L.) in a Mediterranean estuary: a field study. Aquaculture 314, 236–243. doi: 10.1016/j.aquaculture.2011.01.035
Gattuso, J.-P., Kirkwood, W., Barry, J. P., Cox, E., Gazeau, F., Hansson, L., et al. (2014). Free-ocean CO2 enrichment (FOCE) systems: present status and future developments. Biogeosciences 11, 4057–4075. doi: 10.5194/bg-11-4057-2014
Gazeau, F., Parker, L. M., Comeau, S., Gattuso, J.-P., O'connor, W. A., Martin, S., et al. (2013). Impacts of ocean acidification on marine shelled molluscs. Mar. Biol. 160, 2207–2245. doi: 10.1007/s00227-013-2219-3
Gazeau, F., Quiblier, C., Jansen, J. M., Gattuso, J.-P., Middelburg, J. J., and Heip, C. H. R. (2007). Impact of elevated CO2 on shellfish calcification. Geophys. Res. Lett. 34, L07603. doi: 10.1029/2006GL028554
Hervé, M. (2014). RVAideMemoire: Diverse Basic Statistical and Graphical Functions. Available online at: http://cran.r-project.org/web/packages/RVAideMemoire/index.html
Hiebenthal, C., Philipp, E. E. R., Eisenhauer, A., and Wahl, M. (2013). Effects of seawater pCO2 and temperature on shell growth, shell stability, condition and cellular stress of Western Baltic Sea Mytilus edulis (L.) and Arctica islandica (L.). Mar. Biol. 160, 2073–2087. doi: 10.1007/s00227-012-2080-9
Hofmann, G. E., Smith, J. E., Johnson, K. S., Send, U., Levin, L. A., Micheli, F., et al. (2011). High-frequency dynamics of ocean pH: a multi-ecosystem comparison. PLoS ONE 6:e28983. doi: 10.1371/journal.pone.0028983
Ivanina, A. V., Dickinson, G. H., Matoo, O. B., Bagwe, R., Dickinson, A., Beniash, E., et al. (2013). Interactive effects of elevated temperature and CO2 levels on energy metabolism and biomineralization of marine bivalves Crassostrea virginica and Mercenaria mercenaria. Comp. Biochem. Physiol. Mol. Integr. Physiol. 166, 101–111. doi: 10.1016/j.cbpa.2013.05.016
Kroeker, K. J., Gaylord, B., Hill, T. M., Hosfelt, J. D., Miller, S. H., and Sanford, E. (2014). The role of temperature in determining species' vulnerability to ocean acidification: a case study using Mytilus galloprovincialis. PLoS ONE 9:e100353. doi: 10.1371/journal.pone.0100353
Lavigne, H., Epitalon, J. M., and Gattuso, J.-P. (2014). Seacarb: Seawater Carbonate Chemistry with R. Available online at: http://CRAN.R-project.org/package=seacarb
Mackenzie, C. L., Ormondroyd, G. A., Curling, S. F., Ball, R. J., Whiteley, N. M., and Malham, S. K. (2014). Ocean warming, more than acidification, reduces shell strength in a commercial shellfish species during food limitation. PLoS ONE 9:e86764. doi: 10.1371/journal.pone.0086764
Melzner, F., Gutowska, M. A., Hu, M., and Stumpp, M. (2009). Acid-base regulatory capacity and associated proton extrusion mechanisms in marine invertebrates: an overview. Comp. Biochem. Physiol. Mol. Integr. Physiol. 153A, S80–S80. doi: 10.1016/j.cbpa.2009.04.056
Michaelidis, B., Ouzounis, C., Paleras, A., and Pörtner, H. O. (2005). Effects of long-term moderate hypercapnia on acid-base balance and growth rate in marine mussels Mytilus galloprovincialis. Mar. Ecol. Prog. Ser. 293, 109–118. doi: 10.3354/meps293109
Nehls, G., and Thiel, M. (1993). Large-scale distribution patterns of the mussel Mytilus edulis in the Wadden Sea of Schleswig-Holstein: do storms structure the ecosystem? Netherlands J. Sea Res. 31, 181–187. doi: 10.1016/0077-7579(93)90008-G
Pörtner, H. O. (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. doi: 10.1242/jeb.037523
Pörtner, H.-O. (2012). Integrating climate-related stressor effects on marine organisms: unifying principles linking molecule to ecosystem-level changes. Mar. Ecol. Prog. Ser. 470, 273–290. doi: 10.3354/meps10123
Pörtner, H.-O., Bickmeyer, U., Bleich, M., Bock, C., Brownlee, C., Melzner, F., et al. (2010). “Studies of acid-base status and regulation, p137-166,” in Guide to Best Practices for Ocean Acidification Research and Data Reporting, eds U. Riebesell, V. J. Fabry, L. Hansson, and J.-P. Gattuso (Publications Office of the European Union), 260. Available online at: http://www.epoca-project.eu/index.php/Home/Guide-to-OA-Research/
Pörtner, H.-O., Boutilier, R. G., Tang, Y., and Toews, D. P. (1990). Determination of intracellular pH and pCO2 after metabolic inhibition by fluoride and nitrilotriacetic acid. Respir. Physiol. 81, 255–274. doi: 10.1016/0034-5687(90)90050-9
Pörtner, H. O., Langenbuch, M., and Reipschlager, A. (2004). Biological impact of elevated ocean CO2 concentrations: lessons from animal physiology and earth history. J. Oceanogr. 60, 705–718. doi: 10.1007/s10872-004-5763-0
Ramón, M., Cano, J., Peña, J. B., and Campos, M. J. (2005). Current status and perspectives of mollusc (bivalves and gastropods) culture in the Spanish Mediterranean. Boletin Instituto Español de Oceanografia 21, 361–373.
Ramón, M., Fernandez, M., and Galimany, E. (2007). Development of mussel (Mytilus galloprovincialis) seed from two different origins in a semi-enclosed Mediterranean Bay (NE Spain). Aquaculture 264, 148–159. doi: 10.1016/j.aquaculture.2006.11.014
Range, P., Chícharo, M. A., Ben-Hamadou, R., Piló, D., Fernandez-Reiriz, M. J., Labarta, U., et al. (2014). Impacts of CO2-induced seawater acidification on coastal Mediterranean bivalves and interactions with other climatic stressors. Reg. Environ. Change 14, 19–30. doi: 10.1007/s10113-013-0478-7
Range, P., Piloì, D., Ben-Hamadou, R., ChiìCharo, M. A., Matias, D., Joaquim, S, et al. (2012). Seawater acidification by CO2 in a coastal lagoon environment: effects on life history traits of juvenile mussels Mytilus galloprovincialis. J. Exp. Mar. Biol. Ecol. 424–425, 89–98. doi: 10.1016/j.jembe.2012.05.010
Reimer, O., and Tedengren, M. (1996). Phenotypical improvement of morphological defences in the mussel Mytilus edulis induced by exposure to the predator Asteria rubens. Oikos 75, 383–390. doi: 10.2307/3545878
Rhein, M., Rintoul, S. R., Aoki, S., Campos, E., Chambers, D., Feely, R. A., et al. (2013). “Observations: ocean,” in Climate Change 2013: the Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, eds T. F. Stocker, D. Qin, G.-K. Plattner, M. Tignor, S. K. Allen, J. Boschung, et al. (Cambridge; New York: Cambridge University Press), 255–332.
Rodolfo-Metalpa, R., Houlbrèque, F., Tambutté, E., Boisson, F., Baggini, C., Patti, F. P., et al. (2011). Coral and mollusc resistance to ocean acidification adversely affected by warming. Nat. Clim. Change 1, 308–312. doi: 10.1038/nclimate1200
Sarà, G., Manganaro, A., Cortese, G., Pusceddu, A., and Mazzola, A. (1998). The relationship between food availability and growth in Mytilus galloprovincialis in the open sea (southern Mediterranean). Aquaculture 167, 1–15. doi: 10.1016/S0044-8486(98)00281-6
Talmage, S. C., and Gobler, C. J. (2011). Effects of elevated temperature and carbon dioxide on the growth and survival of larvae and juveniles of three species of Northwest Atlantic bivalves. PLoS ONE 6:e26941. doi: 10.1371/journal.pone.0026941
Thomsen, J., Gutowska, M. A., Saphorster, J., Heinemann, A., Trubenbach, K., Fietzke, J., et al. (2010). Calcifying invertebrates succeed in a naturally CO2-rich coastal habitat but are threatened by high levels of future acidification. Biogeosciences 7, 3879–3891. doi: 10.5194/bg-7-3879-2010
Thomsen, J., and Melzner, F. (2010). Moderate seawater acidification does not elicit long-term metabolic depression in the blue mussel Mytilus edulis. Mar. Biol. 157, 2667–2676. doi: 10.1007/s00227-010-1527-0
Touratier, F., and Goyet, C. (2011). Impact of the Eastern Mediterranean Transient on the distribution of anthropogenic CO2 and first estimate of acidification for the Mediterranean Sea. Deep-Sea Res. I Oceanogr. Res. Papers 58, 1–15. doi: 10.1016/j.dsr.2010.10.002
Watson, S. A., Southgate, P. C., Miller, G. M., Moorhead, J. A., and Knauer, J. (2012). Ocean acidification and warming reduce juvenile survival of the fluted giant clam, Tridacna squamosa. Molluscan Res. 32, 177–180.
Keywords: ocean acidification, ocean warming, Mediterranean mussels, growth, survival, Mediterranean Sea
Citation: Gazeau F, Alliouane S, Bock C, Bramanti L, López Correa M, Gentile M, Hirse T, Pörtner H-O and Ziveri P (2014) Impact of ocean acidification and warming on the Mediterranean mussel (Mytilus galloprovincialis). Front. Mar. Sci. 1:62. doi: 10.3389/fmars.2014.00062
Received: 31 July 2014; Accepted: 03 November 2014;
Published online: 26 November 2014.
Edited by:Robinson W. Fulweiler, Boston University, USA
Reviewed by:Claudia R. Benitez-Nelson, University of South Carolina, USA
Emily Carrington, University of Washington, USA
Copyright © 2014 Gazeau, Alliouane, Bock, Bramanti, López Correa, Gentile, Hirse, Pörtner and Ziveri. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Frédéric Gazeau, Laboratoire d'Océanographie de Villefranche, Centre National de la Recherche Scientifique - Université Pierre et Marie Curie and Unité Mixte de Recherche 7093, 06230 Villefranche-sur-mer, France e-mail: firstname.lastname@example.org