Australian Institute of Marine Science

Australian Institute of Marine Science

 
 

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Highlights

Climate change and the Great Barrier Reef

While the GBR has been identified as the best-protected and best-managed coral reef ecosystem in the world, it is still vulnerable to the global ‘enhanced greenhouse’ phenomenon. Although average water temperatures of the GBR have increased only 0.5°C since the late 1800s, the GBR suffered major bleaching events in 1998 and 2002 linked to unusually warm waters in summer.

Bleaching thresholds vary along the GBR but the threshold for coral mortality is approximately 1°C higher than the bleaching point.

 Hydrodynamic processes play an important role and have been shown to make some areas consistently cooler and therefore less susceptible to bleaching. An understanding of this spatial variation using satellite sea surface temperature (SST) data (in collaboration with NOAA) enables scientists to predict areas most at risk of warming and possible bleaching.

Studies on massive coral cores from inshore and mid-shelf reefs revealed growth hiatuses coinciding with major bleaching events in 1998 and 2002. These appear unprecedented in coral growth histories over the past several centuries. Some coral species may be able to respond to warmer waters by changing their algal symbionts to more thermally tolerant species. This is being tested as the possible cause for this change in growth associated with the bleaching events.

Investigations are being conducted into the capacity of corals to acclimatise to warmer water. Some colonies possess the ability to change the balance of zooxanthellae type in their tissues, leading to inceased thermal tolerance.

Investigations are being conducted into the capacity of corals to acclimatise to warmer water. Some colonies possess the ability to change the balance of zooxanthellae type in their tissues, leading to inceased thermal tolerance.
Photo: R. Berkelmans

Modelling of future impacts suggest that a 1-3°C increase in GBR water temperatures, predicted for the end of this century, would result in ~80-100% bleaching of the GBR, compared with ~50% in 1998 and 2002. To maintain current levels of hard coral cover on the GBR corals would need to increase their heat tolerance limits by 0.1°C per decade. Even with adaptation, this may not help them acclimatise fast enough to match the most conservative projected temperature rise.

 

November 20, 2005