|
Similarities and differences
between
cold-water and warm-water coral reefs
| Cold-Water Coral Reefs | Warm-Water
Coral Reefs [1] |
|
| Distribution |
Global - potentially in all seas and at all latitudes |
Global - in sub-tropical and tropical seas between 30ΊN and 30ΊS |
| Number of states, countries and territories with corals |
41 so far |
109 |
| Coverage |
Unknown - but studies to date indicate that global coverage of cold-water coral reefs could equal, or even exceed, that of warm-water reefs |
284,300 km2 |
| Country with highest coral reef coverage |
Unknown the total amount of reefs in Norwegian waters alone was roughly estimated to cover at least 2,000 km2 |
|
| Largest reef complex |
Unknown so
far, the Rψst Reef (100 km2) discovered in 2002 in northern
|
Great Barrier
Reef (more than 30,000 km2), |
| Temperature range |
4Ί 13Ί C |
20Ί - 29Ί C |
| Salinity range |
32 38.8 |
33 36 |
| Depth range |
40 beyond 1,000m |
0 up to 100 m |
| Nutrition |
Uncertain, but likely suspended organic matter and zooplankton |
Suspended organic matter and photosynthesis |
| Symbiotic algae |
No |
Yes |
| Growth rate |
4 25 mm / year |
Up to 150 mm / year |
| Number of reef building coral species |
Few - only 6 primary species. |
Around 800 |
| Reefs composition |
Mostly composed of one or few coral species |
Mostly composed of numerous coral species |
| Age of living reefs |
Up to 8,000 years |
6,000 9,000 years |
| Status |
Unknown but most reefs studied so far show signs of physical damage. Some reefs in the NE Atlantic have been lost completely due to bottom trawling. |
30% irreversibly damaged, another 30% at severe risk of being lost in the next 30 years |
| Rate of Regeneration / recovery |
Unknown - slow growth rate indicates that if regeneration / recovery is possible at all, it might take decades to centuries for a damaged reef to regain its ecological function |
Slow (years to decades) - in most cases, regeneration / recovery will lead to reduced coral diversity, a shift in coral species composition, or even a change from a coral to an algae dominated ecosystem especially where humans impacts are evident |
| Main natural and climate change induced threats |
Unknown climate change could a.o. cause changes in current systems which could affect food supply in deeper waters. |
Increased episodes of higher than normal sea temperatures leading to more widespread and lethal coral bleaching |
| Main threats from human activities |
|
|
| Ecological importance |
Reefs provide habitat, feeding grounds, recruitment and nursery functions for a range of deep-water organisms, including commercial fish species. The number of species depending on or associated with these reefs, and their full ecological importance/value, is still unknown. |
An estimated 1 million plant and animal species are associated with warm water coral reefs. There are approximately 4000 coral reef fish species (Ό of all marine fish species). |
| Socio-economic importance |
Unknown but initial observations suggest importance for local fisheries, including coastal line / net fisheries and deep-water fisheries (especially around seamounts) |
Reefs provide coastal protection and a source of livelihood for more than 1 billion people. The net potential benefits provided reefs are estimated at US$ 30 billion / year. |
| International awareness and attention |
Increased over the last 2-3 years. |
Increasing over the last 1-2 decades, especially after bleaching events in the 90s, with more than 100 non- and intergovernmental organisations engaged in work on warm-water reefs. |
[1] Data on warm-water coral reefs taken from: World Atlas of Coral Reefs (Spalding et al. 2001), Corals of the World (Veron, 2000), The Economics of Worldwide Coral Reef Degradation (Cesar et al. 2003), Life and Death of Coral Reefs (Birkeland, 1997), Status of Coral Reefs of the World 2002 (Wilkinson, C. 2002). |
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