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Remote coral reefs can sustain high growth potential and may match future sea-level trends

Climate-induced disturbances are contributing to rapid, global-scale changes in coral reef ecology. As a consequence, reef carbonate budgets are declining, threatening reef growth potential and thus capacity to track rising sea-levels. Whether disturbed reefs can recover their growth potential and h...

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Autores principales: Perry, Chris T., Murphy, Gary N., Graham, Nicholas A. J., Wilson, Shaun K., Januchowski-Hartley, Fraser A., East, Holly K.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4680928/
https://www.ncbi.nlm.nih.gov/pubmed/26669758
http://dx.doi.org/10.1038/srep18289
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author Perry, Chris T.
Murphy, Gary N.
Graham, Nicholas A. J.
Wilson, Shaun K.
Januchowski-Hartley, Fraser A.
East, Holly K.
author_facet Perry, Chris T.
Murphy, Gary N.
Graham, Nicholas A. J.
Wilson, Shaun K.
Januchowski-Hartley, Fraser A.
East, Holly K.
author_sort Perry, Chris T.
collection PubMed
description Climate-induced disturbances are contributing to rapid, global-scale changes in coral reef ecology. As a consequence, reef carbonate budgets are declining, threatening reef growth potential and thus capacity to track rising sea-levels. Whether disturbed reefs can recover their growth potential and how rapidly, are thus critical research questions. Here we address these questions by measuring the carbonate budgets of 28 reefs across the Chagos Archipelago (Indian Ocean) which, while geographically remote and largely isolated from compounding human impacts, experienced severe (>90%) coral mortality during the 1998 warming event. Coral communities on most reefs recovered rapidly and we show that carbonate budgets in 2015 average +3.7 G (G = kg CaCO(3) m(−2) yr(−1)). Most significantly the production rates on Acropora-dominated reefs, the corals most severely impacted in 1998, averaged +8.4 G by 2015, comparable with estimates under pre-human (Holocene) disturbance conditions. These positive budgets are reflected in high reef growth rates (4.2 mm yr(−1)) on Acropora-dominated reefs, demonstrating that carbonate budgets on these remote reefs have recovered rapidly from major climate-driven disturbances. Critically, these reefs retain the capacity to grow at rates exceeding measured regional mid-late Holocene and 20th century sea-level rise, and close to IPCC sea-level rise projections through to 2100.
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spelling pubmed-46809282015-12-18 Remote coral reefs can sustain high growth potential and may match future sea-level trends Perry, Chris T. Murphy, Gary N. Graham, Nicholas A. J. Wilson, Shaun K. Januchowski-Hartley, Fraser A. East, Holly K. Sci Rep Article Climate-induced disturbances are contributing to rapid, global-scale changes in coral reef ecology. As a consequence, reef carbonate budgets are declining, threatening reef growth potential and thus capacity to track rising sea-levels. Whether disturbed reefs can recover their growth potential and how rapidly, are thus critical research questions. Here we address these questions by measuring the carbonate budgets of 28 reefs across the Chagos Archipelago (Indian Ocean) which, while geographically remote and largely isolated from compounding human impacts, experienced severe (>90%) coral mortality during the 1998 warming event. Coral communities on most reefs recovered rapidly and we show that carbonate budgets in 2015 average +3.7 G (G = kg CaCO(3) m(−2) yr(−1)). Most significantly the production rates on Acropora-dominated reefs, the corals most severely impacted in 1998, averaged +8.4 G by 2015, comparable with estimates under pre-human (Holocene) disturbance conditions. These positive budgets are reflected in high reef growth rates (4.2 mm yr(−1)) on Acropora-dominated reefs, demonstrating that carbonate budgets on these remote reefs have recovered rapidly from major climate-driven disturbances. Critically, these reefs retain the capacity to grow at rates exceeding measured regional mid-late Holocene and 20th century sea-level rise, and close to IPCC sea-level rise projections through to 2100. Nature Publishing Group 2015-12-16 /pmc/articles/PMC4680928/ /pubmed/26669758 http://dx.doi.org/10.1038/srep18289 Text en Copyright © 2015, Macmillan Publishers Limited http://creativecommons.org/licenses/by/4.0/ This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/
spellingShingle Article
Perry, Chris T.
Murphy, Gary N.
Graham, Nicholas A. J.
Wilson, Shaun K.
Januchowski-Hartley, Fraser A.
East, Holly K.
Remote coral reefs can sustain high growth potential and may match future sea-level trends
title Remote coral reefs can sustain high growth potential and may match future sea-level trends
title_full Remote coral reefs can sustain high growth potential and may match future sea-level trends
title_fullStr Remote coral reefs can sustain high growth potential and may match future sea-level trends
title_full_unstemmed Remote coral reefs can sustain high growth potential and may match future sea-level trends
title_short Remote coral reefs can sustain high growth potential and may match future sea-level trends
title_sort remote coral reefs can sustain high growth potential and may match future sea-level trends
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4680928/
https://www.ncbi.nlm.nih.gov/pubmed/26669758
http://dx.doi.org/10.1038/srep18289
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