Author
Listed:
- Chris T. Perry
(University of Exeter)
- Lorenzo Alvarez-Filip
(Universidad Nacional Autónoma de México)
- Nicholas A. J. Graham
(Lancaster University)
- Peter J. Mumby
(University of Queensland)
- Shaun K. Wilson
(Conservation and Attractions, Kensington
University of Western Australia)
- Paul S. Kench
(The University of Auckland)
- Derek P. Manzello
(Atlantic Oceanographic and Meteorological Laboratory, NOAA)
- Kyle M. Morgan
(Nanyang Technological University)
- Aimee B. A. Slangen
(Utrecht University)
- Damian P. Thomson
(University of Western Australia)
- Fraser Januchowski-Hartley
(2UMR 248 MARBEC/UMR250 ENTROPIE, UM2-CNRS-IRD-IFREMER-UM1, Université Montpellier 2)
- Scott G. Smithers
(James Cook University)
- Robert S. Steneck
(University of Maine)
- Renee Carlton
(Khaled bin Sultan Living Oceans Foundation)
- Evan N. Edinger
(Memorial University
Memorial University)
- Ian C. Enochs
(Atlantic Oceanographic and Meteorological Laboratory, NOAA
University of Miami)
- Nuria Estrada-Saldívar
(Universidad Nacional Autónoma de México)
- Michael D. E. Haywood
(Queensland, Bioscience Precinct)
- Graham Kolodziej
(Atlantic Oceanographic and Meteorological Laboratory, NOAA
University of Miami)
- Gary N. Murphy
(University of Exeter)
- Esmeralda Pérez-Cervantes
(Universidad Nacional Autónoma de México)
- Adam Suchley
(Universidad Nacional Autónoma de México)
- Lauren Valentino
(Atlantic Oceanographic and Meteorological Laboratory, NOAA
University of Miami)
- Robert Boenish
(University of Maine, School of Marine Sciences)
- Margaret Wilson
(University of California, Santa Barbara)
- Chancey Macdonald
(James Cook University
James Cook University)
Abstract
Sea-level rise (SLR) is predicted to elevate water depths above coral reefs and to increase coastal wave exposure as ecological degradation limits vertical reef growth, but projections lack data on interactions between local rates of reef growth and sea level rise. Here we calculate the vertical growth potential of more than 200 tropical western Atlantic and Indian Ocean reefs, and compare these against recent and projected rates of SLR under different Representative Concentration Pathway (RCP) scenarios. Although many reefs retain accretion rates close to recent SLR trends, few will have the capacity to track SLR projections under RCP4.5 scenarios without sustained ecological recovery, and under RCP8.5 scenarios most reefs are predicted to experience mean water depth increases of more than 0.5 m by 2100. Coral cover strongly predicts reef capacity to track SLR, but threshold cover levels that will be necessary to prevent submergence are well above those observed on most reefs. Urgent action is thus needed to mitigate climate, sea-level and future ecological changes in order to limit the magnitude of future reef submergence.
Suggested Citation
Chris T. Perry & Lorenzo Alvarez-Filip & Nicholas A. J. Graham & Peter J. Mumby & Shaun K. Wilson & Paul S. Kench & Derek P. Manzello & Kyle M. Morgan & Aimee B. A. Slangen & Damian P. Thomson & Frase, 2018.
"Loss of coral reef growth capacity to track future increases in sea level,"
Nature, Nature, vol. 558(7710), pages 396-400, June.
Handle:
RePEc:nat:nature:v:558:y:2018:i:7710:d:10.1038_s41586-018-0194-z
DOI: 10.1038/s41586-018-0194-z
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Cited by:
- Lauren T. Toth & Curt D. Storlazzi & Ilsa B. Kuffner & Ellen Quataert & Johan Reyns & Robert McCall & Anastasios Stathakopoulos & Zandy Hillis-Starr & Nathaniel Hanna Holloway & Kristen A. Ewen & Clay, 2023.
"The potential for coral reef restoration to mitigate coastal flooding as sea levels rise,"
Nature Communications, Nature, vol. 14(1), pages 1-13, December.
- Edwin A. Hernández-Delgado & Ricardo Laureano, 2024.
"Bringing Back Reef Fish: Sustainable Impacts of Community-Based Restoration of Elkhorn Coral ( Acropora palmata ) in Vega Baja, Puerto Rico (2008–2023),"
Sustainability, MDPI, vol. 16(14), pages 1-41, July.
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