Ocean currents magnify upwelling and deliver nutritional subsidies to reef-building corals during El Niño heatwaves

Author:

Fox Michael D.123ORCID,Guillaume-Castel Robin45ORCID,Edwards Clinton B.6ORCID,Glanz J.6ORCID,Gove Jamison M.7ORCID,Green J. A. Mattias5ORCID,Juhlin E.6,Smith Jennifer E.6ORCID,Williams Gareth J.5ORCID

Affiliation:

1. Division of Biological and Environmental Science and Engineering, King Abdullah University of Science and Technology (KAUST), Thuwal, Saudi Arabia.

2. Marine Science Program, KAUST, Thuwal, Saudi Arabia.

3. Red Sea Research Center, KAUST, Thuwal, Saudi Arabia.

4. LEGOS, Université de Toulouse, CNES, CNRS, Toulouse, France.

5. School of Ocean Sciences, Bangor University, Anglesey LL59 5AB, UK.

6. Center for Marine Biodiversity and Conservation, Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA.

7. National Oceanic and Atmospheric Administration, Pacific Islands Fisheries Science Center, Honolulu, HI, USA.

Abstract

Marine heatwaves are triggering coral bleaching events and devastating coral populations globally, highlighting the need to identify processes promoting coral survival. Here, we show that acceleration of a major ocean current and shallowing of the surface mixed layer enhanced localized upwelling on a central Pacific coral reef during the three strongest El Niño–associated marine heatwaves of the past half century. These conditions mitigated regional declines in primary production and bolstered local supply of nutritional resources to corals during a bleaching event. The reefs subsequently suffered limited post-bleaching coral mortality. Our results reveal how large-scale ocean-climate interactions affect reef ecosystems thousands of kilometers away and provide a valuable framework for identifying reefs that may benefit from such biophysical linkages during future bleaching events.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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