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Water 2014, 6(1), 59-67; doi:10.3390/w6010059
Abstract: Deep-water ecosystems are characterized by relatively low carbonate concentration values and, due to ocean acidification (OA), these habitats might be among the first to be exposed to undersaturated conditions in the forthcoming years. However, until now, very few studies have been conducted to test how cold-water coral (CWC) species react to such changes in the seawater chemistry. The present work aims to investigate the mid-term effect of decreased pH on calcification of the two branching CWC species most widely distributed in the Mediterranean, Lophelia pertusa and Madrepora oculata. No significant effects were observed in the skeletal growth rate, microdensity and porosity of both species after 6 months of exposure. However, while the calcification rate of M. oculata was similar for all colony fragments, a heterogeneous skeletal growth pattern was observed in L. pertusa, the younger nubbins showing higher growth rates than the older ones. A higher energy demand is expected in these young, fast-growing fragments and, therefore, a reduction in calcification might be noticed earlier during long-term exposure to acidified conditions.
Due to the absorption by the ocean of a major part of the anthropogenic CO2 emitted to the atmosphere, the pH of global surface waters has already dropped by 0.1 units since the pre-industrial era [1,2,3]. In the case of the Mediterranean Sea, this pH decrease seems to have been greater than in the global ocean  and this area is actually considered one of the most sensitive regions to Ocean Acidification (OA) during the forthcoming years [5,6,7,8]. On the other hand, it is expected that zones characterized by naturally low carbonate concentration values such as high-latitude and deep-water ecosystems will be amongst the first to experience undersaturated conditions [9,10,11].
This would be the case of cold-water coral (CWC) communities, which are found in areas characterised by very low aragonite saturation state values (ΩA) [12,13]. Therefore, studies evaluating the potential impact of OA on CWC populations are essential to determine the future of one of the most complex deep-sea habitats in the Mediterranean Sea.
However, unlike the numerous experiments with tropical or temperate corals, where OA has been suggested to have diverse ecological and physiological impacts [14,15,16,17,18], the responses of CWC to OA remain largely unexplored, with the few available studies showing contrasting results. For instance, the first short-term studies based on short incubations (between 24 h and 1 week-long) conducted on specimens of Lophelia pertusa and Madrepora oculata, found a reduction in the calcification rate ranging from 30% to 56% when the pH was dropped between 0.1 and 0.3 units [13,19,20]. On the contrary, in the most recent short-term (between 24 h and 21 days) and in the two medium-term experiments (between 6 months and 9 months) conducted to date with the same species, no effects were observed when rearing corals at pH values similar to those expected by the end of the century [13,20,21,22]. Thus, despite the different results observed in the first short-term experiments, the outcomes so far from medium-term experiments evidence that some CWC species could be well adapted to possible changes in the chemical conditions of seawater. It is important to remark that, in these previous studies on possible effects of OA in the development of CWC, coral growth was exclusively assessed through measurements of calcification, with no studies so far reporting on possible effects on coral skeletal microdensity or porosity.
In this context, we investigated the mid-term effect (6 months) of OA on the calcification rate, skeleton microdensity and porosity of two CWC species inhabiting deep Mediterranean waters, the branching corals L. pertusa and M. oculata. In this work, we compare our results with the two previous similar studies published with the same CWC species. We anticipate also possible long-term responses of these organisms based on experiments assessing the effect of OA on other Mediterranean corals, both temperate and CWC species.
2. Materials and Methods
2.1. Specimen Collection and Experimental Setup
Colonies of L. pertusa and M. oculata were collected at 250 m depth in the Cap de Creus canyon (NW Mediterranean Sea) in July 2006 and September 2007 by means of the ROV “Phantom HD2 + 2” and the submersible “JAGO” (GEOMAR) respectively, on board of the Research Vessel “García del Cid”. Coral specimens were kept in aquaria with 50 μm filtered running natural seawater at salinity of 38, temperature of 12 °C and in complete darkness as described by Olariaga et al., . A mixed diet including frozen Cyclops, Mysis and Artemia (Ocean Nutrition ™) were supplied 5 days a week. At the beginning of the experiment, 24 nubbins of L. pertusa (2–5 polyps) and 36 of M. oculata (8–20 polyps) were selected and randomly distributed and incubated together into six 30 litres aquaria subject to two pH treatments (8.10 and 7.81 for control and acidified conditions, respectively; 3 replicates per treatment). See Bramanti et al.  for further details on the experimental setup. Discrete analyses of total alkalinity (TA) by potentiometric titration [25,26] and seawater pH by spectrophotometry  were carried out periodically. The rest of the carbonate system parameters were calculated using the CO2calc software (v1.0.30 USGS).
2.2. Skeletal Measurements
Skeletal growth of all coral nubbins was assessed every two months by means of the buoyant weight technique [28,29], using a 0.1 mg resolution balance (Mettler Toledo AB204 SFACT) and a YSI-30M probe to monitor temperature and salinity. The net buoyant weight (BW) of the corals was transformed to dry weight (DW) using the specific value of the aragonite skeleton density for each species previously determined (see below). To evaluate possible differences between the pH treatments, data were normalized with respect to the skeletal DW of the nubbins at the beginning of each sampling period. Calcification rates were calculated using an exponential growth function and results are expressed as mg of CaCO3 increase per gram and day.
One nubbin of each species and aquarium was randomly selected at the end of the experiment to estimate specific skeleton microdensity and porosity following the technique described in Bucher et al., . Coral nubbins were dipped in sodium hypochlorite during 2 days to remove the organic matter and washed with distilled water afterwards. BW and DW of each sample were recorded before and after the inclusion in molten paraffin wax. In both cases, the BW was measured in distilled water at 20 °C with specific gravity of ~1.00 g cm–3.
2.3. Statistical Analysis
A one-way ANOVA was used to examine differences between treatments in skeleton microdensity and porosity. Repeated-measures two-way ANOVA was used to test potential variations in skeletal growth rates between treatments and aquaria over time (aquarium was considered as a random factor nested within treatment). Normality and homoscedasticity were examined using the Kolmogorov-Smirnov and Levene tests, respectively. Statistical analyses were performed using JMP 9.0.1 (SAS Institute Inc., Cary, NC, USA).
3. Results and Discussion
The seawater CO2 system conditions of both treatments were constrained by periodical pHT and TA laboratory measurements and results are shown in Table 1 (all values are expressed as mean ± SD). In the control treatment, pHT and TA (8.092 ± 0.022 pH units and 2540 ± 13 μmol kg−1, respectively) were comparable to those observed in the sampling area at similar depths during a cruise carried out in 2011 (8.084 ± 0.017 pH units and 2559 ± 16 μmol kg−1, respectively). The calculated χCO2 (mole fraction of CO2 in dry air) and ΩA values were 389 ± 24 ppm and 2.8 ± 0.1, respectively. For the acidified treatment, a decrease of pHT of ~0.3 units (7.808 ± 0.031 pH units) at similar TA values (2541 ± 12 μmol kg−1) caused an increase in χCO2 up to 821 ± 61 ppm and a decrease of ΩA to 1.6 ± 0.1. Temperature and salinity remained constant throughout the experiment (12.3 ± 0.3 °C and 37.6 ± 0.1, respectively). Undersaturation conditions with respect to the aragonite were not reached at any time.
|Control||8.092 ± 0.022||2540 ± 13||37.6 ± 0.1||12.3 ± 0.3|
|(8.061 − 8.112)||(2521 − 2551)||(37.5 − 37.8)||(11.9 − 12.5)|
|High-CO2||7.808 ± 0.031||2541 ± 12||37.6 ± 0.1||12.3 ± 0.2|
|(7.787 − 7.854)||(2524 − 2551)||(37.5 − 37.7)||(12.0 − 12.5)|
|Control||384 ± 23||389± 24||2286 ± 16||15.4 ± 0.9||2087 ± 20||184 ± 7||4.3 ± 0.2||2.8 ± 0.1|
|High-CO2||809 ± 61||821 ± 61||2420 ± 18||32.4 ± 2.6||2283 ± 21||105 ± 7||2.5 ± 0.2||1.6 ± 0.1|
Notes: pHT = pH in total scale; TA = total alkalinity (μmol/kg-SW); Sal = salinity; T = temperature (°C); pCO2 = partial pressure of CO2 of air in equilibrium with seawater (ppm); χCO2 = mole fraction of CO2 in dry air (ppm); DIC = dissolved inorganic carbon (μmol/kg-SW); [CO2]aq = CO2 concentration in seawater (μmol/kg-SW); [HCO3−] = bicarbonate ion concentration (μmol/kg-SW); [CO32−] = carbonate ion concentration (μmol/kg-SW); ΩC = saturation state of seawater with respect to calcite; ΩA = saturation state of seawater with respect to aragonite.
Regarding skeletal measurements, microdensity and porosity for L. pertusa were 2.81 ± 0.01 g cm−3 and 53.3 ± 2.5%, respectively and for M. oculata 2.78 ± 0.01 g cm−3 and 42.0 ± 1.8%, respectively (mean ± SE, N = 6). No significant differences between treatments were observed in microdensity or in porosity at the end of the experiment, neither for L. pertusa (ANOVA, F1,5 = 0.978, p = 0.396 and ANOVA, F1,5 = 0.733, p = 0.440, respectively) nor for M. oculata (ANOVA, F1,5 = 0.492, p = 0.522 and ANOVA, F1,5 = 1.727, p = 0.259, respectively). Mean calcification rate of L. pertusa reared under control conditions was double than M. oculata (2.040 and 0.922 mg CaCO3 g−1 day−1, respectively). These growth rates are comparable to those previously measured on the same CWC species using different techniques [19,20,21,22]. However, the average growth rate of L. pertusa observed in the experiment of Form and Riebesell  was about one order of magnitude lower than in previous works, probably due to the lower incubation temperature used by these authors (7.5 °C) compared to other studies (between 10 and 13 °C). No significant differences between treatments were observed among the different sampling times for both species (ANOVA, F4,18 = 0.110, p = 0.739 for L. pertusa and F4,30 = 0.138, p = 0.406 for M. oculata; Figure 1a,b). Our results are in accordance with two previous mid-term studies assessing the effects of OA on these same species, where no differences were observed after 6 months in L. pertusa  or 9 months of exposure in L. pertusa and M. oculata . This suggests that, at least at mid-term, CWC are able to counteract the a priori more negative environment that lowered-pH oceans should create for calcifying organisms. Regarding possible effects of time on calcification, in contrast with changes observed by Maier et al. , no significant differences were detected neither for L. pertusa (ANOVA, F2,17 = 0.052, p = 0.649) nor for M. oculata (ANOVA, F2,29 = 0.614, p = 0.254) throughout the present experiment.
However, it is important to remark that a different growth pattern was observed between both species depending on the initial size of the nubbins. While all specimens of M. oculata showed similar growth rates (calcification rates measured for the whole duration of the experiment), a correlation between the calcification rate and the initial weight of the fragments was observed in L. pertusa (Figure 1c), where smaller nubbins exhibited greater calcification rates than those with a higher initial weight. This kind of species-specific response could be probably due to the different kind of fragments used for each species. Most of the L. pertusa nubbins used in our experiment had 2 to 3 polyps per nubbin, being assumable that a lower initial weight could be generally related to smaller and, therefore, younger polyps. In contrast, given to the smaller size of M. oculata polyps, each nubbin had to include between 8 and 20 polyps in order to detect potential changes by means of the BW technique. As a result, it was not possible to assess the different growth between small and large polyps in this species, given the coexisting combination of polyps in our selected nubbins, including nubbins with many small polyps with nubbins with few large polyps. At the end, the growth vs. initial nubbin weight plot (Figure 1c) in this species displayed similar growth rates for all fragments, though this result was not fully informative given these circumstances.
A similar growth pattern to that showed in this work by the Mediterranean L. pertusa has been previously described in L. pertusa from the North Atlantic  as well as in Desmophyllum dianthus from the Mediterranean . In both studies, the reduction in calcification rate was greater in fast-growing young polyps compared to the larger and older ones. In other Mediterranean coral species such as the temperate Cladocora caespitosa and Oculina patagonica, the faster growing colonies were more affected by a decrease in pH , although in this study, the intraspecific genetic variability could be key in explaining the wide variety of responses observed. In any case, the regulation of the internal pH at the site of calcification has been described as an energy demanding process [33,34,35], and under lowered-pH conditions, it is expected that the energetic requirements for calcifying should be greater in coral fragments showing faster growth rates. Therefore, further studies conducted through even longer experimental time and focusing on young polyps could provide a better understanding of the threats that future OA will pose for CWC species, due to their role in maintaining the structure of the reef and their apparently higher sensitivity to acidified conditions.
Our data show a low sensitivity of L. pertusa and M. oculata to near future acidification in the Mediterranean Sea at mid-term. No apparent pH-driven effects were observed in the skeletal growth rate, microdensity and porosity of both species compared to control conditions after 6 months of exposure. However, we found a high intraspecific variability in the calcification rate among different colony fragments of L. pertusa, with small (and younger) nubbins showing faster skeletal growth rates. As has been observed recently with both temperate and CWC species, fragments showing higher growth rates are likely to show also greater sensitivity to low pH conditions and it is essential to include them in future long-term experiments to better understand the community-level response to OA.
We wish to thank Alejandro Olariaga and Maximino Delgado (ZAE, ICM) for their technical assistance and to the crew of the RV García del Cid and the JAGO team (GEOMAR, Kiel). This research was supported by the European Project HERMIONE (grant agreement number 226354), the Spanish Government (MINECO) projects ACDC (CTM2009-08849/MAR) and MANIFEST (CTM2012-32017) and by the Marine Biogeochemistry and Global Change research group (Generalitat de Catalunya, 2009SGR142). JM was funded by a FPI studentship (BES-2007-16537) and AG by an I3P studentship (I3P-BPD2005) from the Spanish Government.
Conflicts of Interest
The authors declare no conflict of interest.
- Gattuso, J.P.; Hansson, L. Ocean Acidification: Background and History. In Ocean Acidification; Gattuso, J.P., Hansson, L., Eds.; Oxford University Press: Oxford, UK, 2011; pp. 1–20. [Google Scholar]
- Khatiwala, S.; Tanhua, T.; Mikaloff-Fletcher, S.; Gerber, M.; Doney, S.C.; Graven, H.D.; Gruber, N.; McKinley, G.A.; Murata, A.; Ríos, A.F.; et al. Global ocean storage of anthropogenic carbon. Biogeosciences 2013, 10, 2169–2191. [Google Scholar] [CrossRef]
- Orr, J.C.; Fabry, V.J.; Aumont, O.; Bopp, L.; Doney, S.C.; Feely, R.A.; Gnanadesikan, A.; Gruber, N.; Ishida, A.; Joos, F.; et al. Anthropogenic ocean acidification over the twenty-first century and its impact on calcifying organisms. Nature 2005, 437, 681–686. [Google Scholar] [CrossRef]
- Touratier, F.; Goyet, C. Impact of the Eastern Mediterranean Transient on the distribution of anthropogenic CO2 and first estimate of acidification for the Mediterranean Sea. Deep Sea Res. Part I Oceanogr. Res. Pap. 2011, 58, 1–15. [Google Scholar] [CrossRef]
- Schneider, A.; Wallace, D.W.R.; Körtzinger, A. Alkalinity of the Mediterranean sea. Geophys. Res. Lett. 2007, 34, 1–5. [Google Scholar]
- Schneider, A.; Tanhua, T.; Körtzinger, A.; Wallace, D.W.R. High anthropogenic carbon content in the eastern Mediterranean. J. Geophys. Res. 2010. [Google Scholar] [CrossRef]
- Touratier, F.; Goyet, C. Decadal evolution of anthropogenic CO2 in the northwestern Mediterranean Sea from the mid-1990s to the mid-2000s. Deep Sea Res. Part I Oceanogr. Res. Pap. 2009, 56, 1708–1716. [Google Scholar] [CrossRef]
- Calvo, E.; Simó, R.; Coma, R.; Ribes, M.; Pascual, J.; Sabatés, A.; Gili, J.M.; Pelejero, C. Effects of climate change on Mediterranean marine ecosystems: The case of the Catalan Sea. Clim. Res. 2011, 50, 1–29. [Google Scholar] [CrossRef]
- Guinotte, J.M.; Orr, J.C.; Cairns, S.S.; Freiwald, A.; Morgan, L.; George, R. Will human-induced changes in seawater chemistry alter the distribution of deep-sea scleractinian corals? Front. Ecol. Environ. 2006, 4, 141–146. [Google Scholar] [CrossRef]
- Steinacher, M.; Joos, F.; Frölicher, T.L.; Plattner, G.K.; Doney, S.C. Imminent ocean acidification in the Arctic projected with the NCAR global coupled carbon cycle-climate model. Biogeosciences 2009, 6, 515–533. [Google Scholar] [CrossRef]
- Yamamoto, A.; Kawamiya, M.; Ishida, A.; Yamanaka, Y.; Watanabe, S. Impact of rapid sea-ice reduction in the Arctic Ocean on the rate of ocean acidification. Biogeosciences 2012, 9, 2365–2375. [Google Scholar] [CrossRef]
- Thresher, R.; Tilbrook, B.; Fallon, S.J.; Wilson, N.C.; Adkins, J. Effects of chronic low carbonate saturation levels on the distribution, growth and skeletal chemistry of deep-sea corals and other seamount megabenthos. Mar. Ecol. Prog. Ser. 2011, 442, 87–99. [Google Scholar] [CrossRef]
- Form, A.U.; Riebesell, U. Acclimation to ocean acidification during long-term CO2 exposure in the cold-water coral Lophelia pertusa. Glob. Chang. Biol. 2012, 18, 843–853. [Google Scholar] [CrossRef]
- Doney, S.C.; Fabry, V.J.; Feely, R.A.; Kleypas, J.A. Ocean Acidification: The other CO2 problem. Ann. Rev. Mar. Sci. 2009, 1, 169–192. [Google Scholar] [CrossRef]
- Ries, J.B.; Cohen, A.L.; McCorkle, D.C. Marine calcifiers exhibit mixed responses to CO2-induced ocean acidification. Geology 2009, 37, 1131–1134. [Google Scholar] [CrossRef]
- Pelejero, C.; Calvo, E.; Hoegh-Guldberg, O. Paleo-perspectives on ocean acidification. Trends Ecol. Evol. 2010, 25, 332–344. [Google Scholar] [CrossRef]
- Wicks, L.; Roberts, J.M. Benthic invertebrates in a high-CO2 world. Oceanogr. Mar. Biol. Annu. Rev. 2012, 50, 127–188. [Google Scholar]
- Parker, L.; Ross, P.; Connor, W.; Pörtner, H.; Scanes, E.; Wright, J. Predicting the response of molluscs to the impact of ocean acidification. Biology 2013, 2, 651–692. [Google Scholar] [CrossRef]
- Maier, C.; Hegeman, J.; Weinbauer, M.G. Calcification of the cold-water coral Lophelia pertusa under ambient and reduced pH. Biogeosciences 2009, 6, 1671–1680. [Google Scholar] [CrossRef]
- Maier, C.; Watremez, P.; Taviani, M.; Weinbauer, M.G.; Gattuso, J.P. Calcification rates and the effect of ocean acidification on Mediterranean cold-water corals. Proc. R. Soc. Lond. B. Biol. Sci. 2012, 279, 1716–1723. [Google Scholar] [CrossRef]
- Maier, C.; Schubert, A.; Berzunza-Sánchez, M.M.; Weinbauer, M.G.; Watremez, P.; Gattuso, J.P. End of the century pCO2 levels do not impact calcification in Mediterranean cold-water corals. PLoS One 2013, 8. [Google Scholar] [CrossRef]
- Hennige, S.J.; Wicks, L.C.; Kamenos, N.A.; Bakker, D.; Findlay, H.S.; Dumousseaud, C.; Roberts, J.M. Short-term metabolic and growth responses of the cold-water coral Lophelia pertusa to Ocean Acidification. Deep Sea Res. Part II Top. Stud. Oceanogr. 2013. [Google Scholar] [CrossRef]
- Olariaga, A.; Gori, A.; Orejas, C.; Gili, J.M. Development of an autonomous aquarium system for maintaining deep corals. Oceanography 2009, 22, 44–45. [Google Scholar] [CrossRef]
- Bramanti, L.; Movilla, J.; Guron, M.; Calvo, E.; Gori, A.; Dominguez-Carrió, C.; Grinyó, J.; López-Sanz, A.; Martínez-Quintana, A.; Pelejero, C.; et al. Detrimental effects of Ocean Acidification on the economically important Mediterranean red coral (Corallium rubrum). Glob. Chang. Biol. 2013, 19, 1897–1908. [Google Scholar] [CrossRef]
- Perez, F.F.; Fraga, F. A precise and rapid analytical procedure for alkalinity determination. Mar. Chem. 1987, 21, 169–182. [Google Scholar] [CrossRef]
- Perez, F.F.; Rios, A.F.; Rellán, T.; Alvarez, M. Improvements in a fast potentiometric seawater alkalinity determination. Ciencias Mar. 2000, 26, 463–478. [Google Scholar]
- Clayton, T.D.; Byrne, R.H. Spectrophotometric seawater pH measurements: Total hydrogen ion concentration scale calibration of m-cresol purple and at-sea results. Deep Sea Res. I 1993, 40, 2115–2129. [Google Scholar] [CrossRef]
- Jokiel, P.L.; Maragos, J.E.; Franzisket, L. Coral Growth: Buoyant Weight Technique. In Coral Reef: Research Methods; Stoddart, D.R., Johannes, R.E., Eds.; United Nations Educational Scientific and Cultural Organization: Paris, France, 1978; pp. 529–541. [Google Scholar]
- Davies, P.S. Short-term growth measurements of corals using an accurate buoyant weighing technique. Mar. Biol. 1989, 101, 389–395. [Google Scholar] [CrossRef]
- Bucher, D.; Harriott, V.J.; Roberts, L.G. Skeletal micro-density, porosity and bulk density of acroporid corals. J. Exp. Mar. Bio. Ecol. 1998, 228, 117–136. [Google Scholar] [CrossRef]
- Movilla, J.; Orejas, C.; Calvo, E.; Gori, A.; López-Sanz, A.; Grinyó, J.; Dominguez-Carrió, C.; Pelejero, C. Differential response of two Mediterranean cold-water coral species to ocean acidification. Coral Reefs 2013. submitted. [Google Scholar]
- Movilla, J.; Calvo, E.; Pelejero, C.; Coma, R.; Serrano, E.; Fernández-Vallejo, P.; Ribes, M. Calcification reduction and recovery in native and non-native Mediterranean corals in response to ocean acidification. J. Exp. Mar. Bio. Ecol. 2012, 438, 144–153. [Google Scholar] [CrossRef]
- Al-Horani, F.A.; Al-Moghrabi, S.M.; de Beer, D. The mechanism of calcification and its relation to photosynthesis and respiration in the scleractinian coral Galaxea fascicularis. Mar. Biol. 2003, 142, 419–426. [Google Scholar]
- Cohen, A.L.; Holcomb, M. Why corals care about ocean acidification: Uncovering the mechanism. Oceanography 2009, 22, 118–127. [Google Scholar] [CrossRef]
- Allemand, D.; Tambutté, É.; Zoccola, D.; Tambutté, S. Coral Calcification, Cells to Reefs. In Coral Reefs: An Ecosystem in Transition; Dubinsky, Z., Stambler, N., Eds.; Springer: Heidelberg, Germany, 2011; pp. 119–150. [Google Scholar]
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