Projecting coral responses to intensifying marine heatwaves under ocean acidification

• Published in: Global Change Biology
• Main Authors: Klein, Shannon, Geraldi, Nathan, Anton Gamazo, Andrea, Schmidt-Roach, Sebastian, Ziegler, Maren, Cziesielski, Maha Joana, Martin, Cecilia, Rädecker, Nils, Frölicher, Thomas L., Mumby, Peter J., Pandolfi, John M., Suggett, David J., Voolstra, Christian R., Aranda, Manuel, Duarte, Carlos M.
• Other Authors: Biological and Environmental Science and Engineering (BESE) Division, Marine Science Program, Red Sea Research Center (RSRC), Reef Genomics Lab, Department of Animal Ecology & Systematics Justus Liebig University Heinrich-Buff-Ring 26-32 IFZ D-35392 Giessen Germany, Climate and Environmental Physics Physics Institute University of Bern Bern Switzerland, Oeschger Centre for Climate Change Research University of Bern Bern Switzerland, Marine Spatial Ecology Lab School of Biological Sciences The University of Queensland St. Lucia, Brisbane QLD 4072 Australia, Australian Research Council Centre of Excellence for Coral Reef Studies School of Biological Sciences The University of Queensland St. Lucia, Brisbane QLD 4072 Australia, University of Technology Sydney Climate Change Cluster Faculty of Science Sydney NSW 2007 Australia, Department of Biology University of Konstanz Konstanz 78457 Germany
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Wiley 2021
• Subjects: Ocean acidification
• Online Access: http://hdl.handle.net/10754/670419; https://doi.org/10.1111/gcb.15818

Over this century, coral reefs will run the gauntlet of climate change as marine heatwaves (MHWs) become more intense and frequent, and ocean acidification (OA) progresses. However, we still lack a quantitative assessment of how, and to what degree, OA will moderate the responses of corals to MHWs as they intensify throughout this century. Here, we first projected future MHW intensities for tropical regions under three future greenhouse gas emissions scenarios (RCP2.6, RCP4.5, and RCP8.5) for the near-term (2021-2040), mid-century (2041-2060), and late-century (2081-2100). We then combined these MHW intensity projections with a global dataset of 1,788 experiments to assess coral attribute performance and survival under the three emissions scenarios for the near term, mid-century, and late century in the presence and absence of OA. Although warming and OA had predominately additive impacts on the coral responses, the contribution of OA in affecting most coral attribute responses was minor relative to the dominant role of intensifying MHWs. However, the addition of OA led to greater decreases in photosynthesis and survival under intermediate and unrestricted emissions scenarios for the mid and late century than if intensifying MHWs were considered as the only driver. These results indicate that the role OA in affecting coral responses to intensifying MHWs temperatures is specific to the coral attribute examined and the extremity of temperatures tested. Specifically, intensifying MHWs and OA will cause increasing instances of coral bleaching and substantial declines in coral productivity, calcification, and survival within the next two decades under the low and intermediate emissions scenarios. These projections suggest that corals must rapidly adapt or acclimatize to projected ocean conditions to persist, which is far more likely under a low emissions scenario and with increasing efforts to manage reefs to enhance resilience.