One of the few biological structures visible from space, the Great Barrier Reef stretches over 2,300 km (1,430 miles) and began life about 600,000 years ago. It is home to more than 400 types of coral and 2,000 species of fish.
Corals reefs globally occupy less than 1% of the ocean, but support 25% of all marine life. 30% of all reefs are estimated to be severely damaged, and close to 60% may be lost by 2030.
Hard corals and other organisms which secrete calcium carbonate contribute most to reef building. The reef needs to be structurally strong to cope with differing light and sediment conditions as well as wave and storm power.
Both hard and soft reef-building corals can only exist within a limited range of conditions, needing light and an optimum temperature and salinity range. The ideal conditions for coral reef growth are water temperatures of 26°C to 27°C, and salinity of 36 parts per thousand. If the water is clear, corals can grow to a depth of over 100m. This is reduced to 8m if the water is turbid or cloudy.
Other species living on the reef, such as clams and parrotfish eat corals, contributing to bioerosion, so there is a natural reef cycle of production and destruction.
This cycle can be disturbed by upsetting the ecological balance. The threats to coral reefs include:
Most of the threats above are caused directly or indirectly by human activity.
The Great Barrier Reef has lost half its coral cover since 1985. The loss was due to storm damage (48%), Crown-of-thorns starfish (42%), and bleaching (10%) according to a 2012 study by researchers from the Australian Institute of Marine Science (AIMS).