Acclimatization of a coral-dinoflagellate mutualism at a CO(2) vent

Ocean acidification caused by shifts in ocean carbonate chemistry resulting from increased atmospheric CO(2) concentrations is threatening many calcifying organisms, including corals. Here we assessed autotrophy vs heterotrophy shifts in the Mediterranean zooxanthellate scleractinian coral Balanophy...

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Bibliographic Details
Published in:Communications Biology
Main Authors: Prada, Fiorella, Franzellitti, Silvia, Caroselli, Erik, Cohen, Itay, Marini, Mauro, Campanelli, Alessandra, Sana, Lorenzo, Mancuso, Arianna, Marchini, Chiara, Puglisi, Alessia, Candela, Marco, Mass, Tali, Tassi, Franco, LaJeunesse, Todd C., Dubinsky, Zvy, Falini, Giuseppe, Goffredo, Stefano
Format: Text
Language:English
Published: Nature Publishing Group UK 2023
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Article
Ocean acidification
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC9849335/
https://doi.org/10.1038/s42003-022-04327-3
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Summary:Ocean acidification caused by shifts in ocean carbonate chemistry resulting from increased atmospheric CO(2) 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 pCO(2) conditions at a CO(2) 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. δ(13)C 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 δ(15)N values of 0‰ strongly suggest that diazotroph N(2) 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.

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