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Ocean acidification partially mitigates the negative effects of warming on the recruitment of the coral, Orbicella faveolata

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Abstract

Ocean acidification and ocean warming constitute major threats to many calcifying reef organisms, including scleractinian corals. The combined effects of these two environmental stressors on the earliest life history stages of reef calcifiers remain poorly studied, particularly for Atlantic corals. Here, we investigate how acidification and warming influence the fertilization success, larval survivorship, and larval settlement of the threatened Atlantic coral, Orbicella faveolata. Gametes and larvae from O. faveolata were subjected to a factorial combination of warming (ambient versus + 1.5 °C) and acidification (ambient versus − 0.2 pH units) projected to occur by the year 2050. O. faveolata individuals were maintained in the same treatments throughout all early life history stages investigated. The fertilization success of O. faveolata was not affected by acidification, warming, or their combination. However, during larval development, warming caused complete mortality and prevented any subsequent settlement. Interestingly, these negative effects of warming were mitigated when combined with ocean acidification, such that both larval survivorship and settlement increased by 41% in the combined treatment relative to the isolated warming treatment. Our research suggests that temperature-induced increases in larval metabolism may be counterbalanced by acidification, which serves to reduce larval metabolism. Notwithstanding, larval survivorship and settlement were still reduced by 50% under combined acidification and warming relative to the ambient treatment, indicating that climate change will continue to serve as major stressor during the early life history stages of corals, jeopardizing the resilience of Caribbean reefs.

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Acknowledgements

The work contributing to this paper has been supported by the US National Science Foundation Project OCE-1538469. This is a contribution #1015 of the Smithsonian Caribbean Coral Reef Ecosystems Program. We thank Zach Foltz, Valerie Paul, and Scott Jones at the Smithsonian Institution for their logistical support and Tom Opishinski for the ocean temperature data. We thank the Belizean Fisheries Department, marine scientific research permit number 000008-17, for allowing us to conduct this research. Finally, we appreciate the helpful comments by the three anonymous reviewers that greatly improved this manuscript. This is contribution #172 from the Center for Coastal Oceans in the Institute of Environment at Florida International University.

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  1. Department of Marine and Environmental Science, Nova Southeastern University, Dania Beach, FL, USA

    Kelly A. Pitts, Joana Figueiredo & Nicole D. Fogarty

  2. Department of Biological Sciences, Institute of the Envrionment, Florida International University, Miami, FL, USA

    Justin E. Campbell

  3. Department of Biology and Marine Biology, Center for Marine Science, University of North Carolina, Wilmington, NC, USA

    Nicole D. Fogarty

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338_2019_1888_MOESM1_ESM.tif

Supplemental Fig. 1 Monthly temperatures (mean ± SE) from the collection site near Carrie Bow Cay (16°48′06.0″N, 88°04′57.9″W) during 2017 (TIFF 24 kb)

338_2019_1888_MOESM2_ESM.tif

Supplemental Fig. 2 Daily temperatures of the survivorship and settlement mesocosms. Bars are color coded by treatment (AMB: ambient; OA: ocean acidification (pH -0.2 units); OW: ocean warming (+ 1.5 °C); OAW: ocean acidification and warming (pH -0.2 units, + 1.5 °C) (TIFF 90 kb)

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Pitts, K.A., Campbell, J.E., Figueiredo, J. et al. Ocean acidification partially mitigates the negative effects of warming on the recruitment of the coral, Orbicella faveolata. Coral Reefs 39, 281–292 (2020). https://doi.org/10.1007/s00338-019-01888-4

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