Acclimatization of a coral-dinoflagellate mutualism at a CO2 vent.

Ocean acidification caused by shifts in ocean carbonate chemistry resulting from increased atmospheric CO₂ concentrations is threatening many calcifying organisms, including corals. Here we assessed autotrophy vs heterotrophy shifts in the Mediterranean zooxanthellate scleractinian coral Balanophyllia europaea acclimatized to low pH/high pCO₂ conditions at a CO₂ vent off Panarea Island (Italy). Dinoflagellate endosymbiont densities were higher at lowest pH Sites where changes in the distribution of distinct haplotypes of a host-specific symbiont species, Philozoon balanophyllum, were observed. An increase in symbiont C/N ratios was observed at low pH, likely as a result of increased C fixation by higher symbiont cell densities. δ¹³C values of the symbionts and host tissue reached similar values at the lowest pH Site, suggesting an increased influence of autotrophy with increasing acidification. Host tissue δ¹⁵N values of 0‰ strongly suggest that diazotroph N₂ fixation is occurring within the coral tissue/mucus at the low pH Sites, likely explaining the decrease in host tissue C/N ratios with acidification. Overall, our findings show an acclimatization of this coral-dinoflagellate mutualism through trophic adjustment and symbiont haplotype differences with increasing acidification, highlighting that some corals are capable of acclimatizing to ocean acidification predicted under end-of-century scenarios. Low seawater pH impacts trophic dynamics in corals, increasing symbiont density and autotrophic/heterotrophic ratios and varying dinoflagellate haplotypes under ocean acidification. [ABSTRACT FROM AUTHOR]