AI Article Synopsis

  • Coral reefs globally face pressures from various stressors, with hard coral cover loss being a significant concern, but specific estimates for the Great Barrier Reef (GBR) are currently absent.
  • Monitoring from 47 reefs over 1300 km showed that overall coral cover remained stable at an average of 29% from 1995 to 2009, with some regions experiencing increases and others declines in coral cover.
  • Factors such as crown-of-thorns starfish outbreaks and storm damage caused more coral loss than mass bleaching or disease, yet fluctuations in coral cover were mainly due to changes in fast-growing Acroporidae and localized disturbances rather than a systemic decline since 1995.

Article Abstract

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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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3053361PMC
http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0017516PLOS

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