Communications Earth & Environment (Sep 2024)

Ocean acidification does not prolong recovery of coral holobionts from natural thermal stress in two consecutive years

  • Kerri L. Dobson,
  • Christopher P. Jury,
  • Robert J. Toonen,
  • Rowan H. McLachlan,
  • Jeremy C. Williams,
  • Andréa G. Grottoli

DOI
https://doi.org/10.1038/s43247-024-01672-5
Journal volume & issue
Vol. 5, no. 1
pp. 1 – 16

Abstract

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Abstract Under predicted future ocean conditions, corals will experience frequent and intense thermal stress events while simultaneously being exposed to chronic ocean acidification. Yet, some corals will likely be more resistant and/or resilient to these predicted conditions than others and may be critical to reef persistence in the future. Following natural thermal stress in two consecutive years (2014 and 2015), we evaluated the effects of feeding and simulated ocean acidification on the physiological recovery of Montipora capitata and Porites compressa sourced from Kāneʻohe Bay and Waimānalo Bay, Hawaiʻi. Following the 2014 thermal stress event, simulated ocean acidification did not slow recovery of the holobiont and feeding enhanced recovery. However, feeding did not decrease susceptibility to the 2015 thermal stress event, and simulated ocean acidification did not increase susceptibility. Recovery strategies employed between species and between sites clearly differed, highlighting that coral reef restoration and management should consider species-level and site-specific vulnerabilities. Overall, our findings call attention to the immediate threat which ocean warming presents, the lack of additional stress to the holobiont from ocean acidification, the importance of heterotrophy in coral resilience, and the potential significance of additional local biotic stressors (i.e., predator outbreaks) for coral resiliency under annual thermal stress.