1983
DOI: 10.1016/0022-0981(83)90165-x
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Monitoring of coral reefs with linear transects: A study of storm damage

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Cited by 62 publications
(28 citation statements)
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“…Its value is 1.0 when the surface is flat and increases with surface irregularity or relief. Analogous methods have been used in studies on coral reef heterogeneity (Wellington 1982, Rogers et al 1983.…”
Section: Methodsmentioning
confidence: 99%
“…Its value is 1.0 when the surface is flat and increases with surface irregularity or relief. Analogous methods have been used in studies on coral reef heterogeneity (Wellington 1982, Rogers et al 1983.…”
Section: Methodsmentioning
confidence: 99%
“…However, it is difficult to ''scale up'' the implications of such studies to a spatial scale that is ecologically relevant to both understanding population drivers of coral reef communities, and management of marine systems. At broad scales, ecological processes on coral reefs occur against a backdrop of abiotic influences such as storms, cyclones, pollution, sedimentation, and climate change impacts, which can cause significant changes to coral reefs (Rogers et al 1983, Hughes 1994, Hughes et al 2003, Wenger et al 2012, Woolsey et al 2012. Coral reefs continue to be at risk from an ever increasing number of such threats, which could affect coral reef organisms at multiple trophic levels.…”
Section: Top-down Effects In Complex Systems: the Case For Reefsmentioning
confidence: 99%
“…The consistent patterns found in this study from four locations encompassing a large area and latitudinal range suggest that these patterns are likely to occur broadly across the GBR, however the likelihood of trophic effects occurring may differ amongst individual reefs and in part this may relate to temporal organismal trajectories relating to other impacts. The Great Barrier Reef and other reef systems are under threat from a myriad of stressors such as cyclones, nutrient runoff and sedimentation, and climate change impacts, all of which can have a strong effect on habitats and fish assemblages (Rogers et al 1983, Hughes 1994, Hughes et al 2003, De'ath et al 2012, Wenger et al 2012. The current state of reefs is actually the net result of a time series of events as reefs are subjected to perturbations, and decline or recover.…”
Section: Management Implicationsmentioning
confidence: 99%
“…The partial death or damage to these shaIIow-water corals was possibly due to a series of strong hurricanes impacting St. John's reefs during the past 20 years or to possible epizootic events (see below). All else being equal, large storm waves have a greater impact in shallow reefs by breaking branching corals, dislodging or toppling boulder corals, or scouring thin coral tissues (Rogers et al, 1983;Edmonds and Witman, 1991;Rogers et al, 1991;Nemeth and Sladek Nowlis, 2001). The shallow St. John sites also contained higher densities of &i7~IiflTllui.UIn;a pattern-of reColon"1zationfhat is typlcal throughofit the Uaribbe (Nemeth, personal observation) following its die-off in the early 1980's (Lessios, 1988).…”
Section: Ssionmentioning
confidence: 99%