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Disturbance and the Dynamics of Coral Cover on the Great Barrier Reef (1995–2009)

Coral reef ecosystems worldwide are under pressure from chronic and acute stressors that threaten their continued existence. Most obvious among changes to reefs is loss of hard coral cover, but a precise multi-scale estimate of coral cover dynamics for the Great Barrier Reef (GBR) is currently lacki...

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Autores principales: Osborne, Kate, Dolman, Andrew M., Burgess, Scott C., Johns, Kerryn A.
Formato: Texto
Lenguaje:English
Publicado: Public Library of Science 2011
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3053361/
https://www.ncbi.nlm.nih.gov/pubmed/21423742
http://dx.doi.org/10.1371/journal.pone.0017516
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author Osborne, Kate
Dolman, Andrew M.
Burgess, Scott C.
Johns, Kerryn A.
author_facet Osborne, Kate
Dolman, Andrew M.
Burgess, Scott C.
Johns, Kerryn A.
author_sort Osborne, Kate
collection PubMed
description Coral reef ecosystems worldwide are under pressure from chronic and acute stressors that threaten their continued existence. Most obvious among changes to reefs is loss of hard coral cover, but a precise multi-scale estimate of coral cover dynamics for the Great Barrier Reef (GBR) is currently lacking. Monitoring data collected annually from fixed sites at 47 reefs across 1300 km of the GBR indicate that overall regional coral cover was stable (averaging 29% and ranging from 23% to 33% cover across years) with no net decline between 1995 and 2009. Subregional trends (10–100 km) in hard coral were diverse with some being very dynamic and others changing little. Coral cover increased in six subregions and decreased in seven subregions. Persistent decline of corals occurred in one subregion for hard coral and Acroporidae and in four subregions in non-Acroporidae families. Change in Acroporidae accounted for 68% of change in hard coral. Crown-of-thorns starfish (Acanthaster planci) outbreaks and storm damage were responsible for more coral loss during this period than either bleaching or disease despite two mass bleaching events and an increase in the incidence of coral disease. While the limited data for the GBR prior to the 1980's suggests that coral cover was higher than in our survey, we found no evidence of consistent, system-wide decline in coral cover since 1995. Instead, fluctuations in coral cover at subregional scales (10–100 km), driven mostly by changes in fast-growing Acroporidae, occurred as a result of localized disturbance events and subsequent recovery.
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spelling pubmed-30533612011-03-18 Disturbance and the Dynamics of Coral Cover on the Great Barrier Reef (1995–2009) Osborne, Kate Dolman, Andrew M. Burgess, Scott C. Johns, Kerryn A. PLoS One Research Article Coral reef ecosystems worldwide are under pressure from chronic and acute stressors that threaten their continued existence. Most obvious among changes to reefs is loss of hard coral cover, but a precise multi-scale estimate of coral cover dynamics for the Great Barrier Reef (GBR) is currently lacking. Monitoring data collected annually from fixed sites at 47 reefs across 1300 km of the GBR indicate that overall regional coral cover was stable (averaging 29% and ranging from 23% to 33% cover across years) with no net decline between 1995 and 2009. Subregional trends (10–100 km) in hard coral were diverse with some being very dynamic and others changing little. Coral cover increased in six subregions and decreased in seven subregions. Persistent decline of corals occurred in one subregion for hard coral and Acroporidae and in four subregions in non-Acroporidae families. Change in Acroporidae accounted for 68% of change in hard coral. Crown-of-thorns starfish (Acanthaster planci) outbreaks and storm damage were responsible for more coral loss during this period than either bleaching or disease despite two mass bleaching events and an increase in the incidence of coral disease. While the limited data for the GBR prior to the 1980's suggests that coral cover was higher than in our survey, we found no evidence of consistent, system-wide decline in coral cover since 1995. Instead, fluctuations in coral cover at subregional scales (10–100 km), driven mostly by changes in fast-growing Acroporidae, occurred as a result of localized disturbance events and subsequent recovery. Public Library of Science 2011-03-10 /pmc/articles/PMC3053361/ /pubmed/21423742 http://dx.doi.org/10.1371/journal.pone.0017516 Text en Osborne et al. http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are properly credited.
spellingShingle Research Article
Osborne, Kate
Dolman, Andrew M.
Burgess, Scott C.
Johns, Kerryn A.
Disturbance and the Dynamics of Coral Cover on the Great Barrier Reef (1995–2009)
title Disturbance and the Dynamics of Coral Cover on the Great Barrier Reef (1995–2009)
title_full Disturbance and the Dynamics of Coral Cover on the Great Barrier Reef (1995–2009)
title_fullStr Disturbance and the Dynamics of Coral Cover on the Great Barrier Reef (1995–2009)
title_full_unstemmed Disturbance and the Dynamics of Coral Cover on the Great Barrier Reef (1995–2009)
title_short Disturbance and the Dynamics of Coral Cover on the Great Barrier Reef (1995–2009)
title_sort disturbance and the dynamics of coral cover on the great barrier reef (1995–2009)
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3053361/
https://www.ncbi.nlm.nih.gov/pubmed/21423742
http://dx.doi.org/10.1371/journal.pone.0017516
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