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11th ICRS Abstract book - Nova Southeastern University

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12-27<br />

Interaction Between Fishing And Bleaching On Kenyan Coral Reefs Moderated By<br />

Disturbance History<br />

Emily DARLING* 1 , Tim MCCLANAHAN 2 , Isabelle CÔTÉ 1<br />

1 Simon Fraser <strong>University</strong>, Burnaby, BC, Canada, 2 Wildlife Conservation Society, Bronx,<br />

NY<br />

Coral reef ecosystems are affected by many stressors. The possibility these stressors<br />

interact synergistically causes conservation concern, but such non-linear effects remain<br />

untested in nature. We examined the independent and interactive effects of two stressors,<br />

fishing and bleaching, on coral community structure using a 16-year time series of<br />

monitoring data from Kenyan reefs. While both fishing and a mass coral bleaching event<br />

in 1998 decreased hard coral cover, these stressors did not interact synergistically to<br />

accelerate coral decline. Instead, fishing and bleaching interacted antagonistically.<br />

Following 1998, hard coral cover on unfished reefs declined 74% (relative to prebleaching<br />

cover) compared to 48% on fished reefs. Multivariate community analyses<br />

suggest that the non-synergistic interaction between fishing and bleaching may be<br />

explained by changes in coral community structure associated with fishing history. Prior<br />

to 1998, unfished reefs had diverse coral assemblages (dominated by branching Acropora<br />

and plating Montipora) that were not resistant to the 1998 bleaching event. In contrast,<br />

fished reefs, composed primarily of massive and branching Porites, were both more<br />

resistant to and recovered more quickly from bleaching. Decades of fishing pressure thus<br />

appears to have favoured low-diversity disturbance-tolerant coral communities. By<br />

contrast, unfished reefs may be refugia for high-diversity disturbance-sensitive<br />

communities. We suggest that disturbance history, community susceptibility, and tradeoffs<br />

between diversity and resilience can moderate interactions between multiple<br />

stressors and may be important factors determining resilience to future large-scale<br />

climate events.<br />

12-28<br />

Great Barrier Reef Coral Communities: Resilient in the 1980s but Struggling in the<br />

2000s<br />

Terry DONE* 1 , Lyndon DEVANTIER 2 , Emre TURAK 2 , Mary WAKEFORD 2 , Abbi<br />

MCDONALD 2 , Craig JOHNSON 3<br />

1 Australian Institute of Marine Science, Townsville, Qld, Australia, 2 Australian Institute<br />

of Marine Science, Townsville, 4810, Qld, Australia, 3 <strong>University</strong> of Tasmania, Hobart,<br />

Australia<br />

Coral communities were monitored using photography and video at 30 Great Barrier Reef<br />

study sites in the period 1980 – 2005. At Pandora Reef in the 1980s, regional elevation of<br />

land-based nutrients did not prevent spectacular recovery of coral cover and diversity<br />

following a sequence of environmental disturbances in the 1970s. There was high coral<br />

mortality in some habitats in the 1998 bleaching, and the standing dead corals were then<br />

flattened by a 2000 cyclone. Degree of impact and extent of recovery was related to<br />

marked differences around the reef in benthic species composition and relative<br />

abundance, notably fleshy algae, soft corals, poritids and acroporids. Relative paucity of<br />

larval derived recruits and viable fragments in 2005 suggests the strong coral population<br />

resilience of the 1980s will not be repeated in the short term, especially reflecting<br />

regional paucity in Acropora broodstock. At a small (32 m2) site at Lizard Island there<br />

were three acute disturbance events followed by good coral recovery and no tendency for<br />

phase-shift: 1982- a combination of coral bleaching and Crown-of-Thorns starfish; 1990 -<br />

cyclone waves and 1996 - Crown-of-Thorns starfish. However beyond 1996,<br />

observations and modeling using Johnson’s Compete © Cellular Automaton model<br />

suggest the area may be subject to annual chronic background mortality. The apparent<br />

retardation of coral recovery may be exacerbated by projected reduced intervals between<br />

disturbances associated with global climate change. However hopefully recovery<br />

prospects will be improved as region-wide benefits of improved GBR-wide management<br />

introduced in 2004 take effect: i.e. an eightfold increase in the area of no take protected<br />

areas, and the initiation of actions to improved coastal water quality.<br />

Oral Mini-Symposium 12: Reef Resilience<br />

106

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