Lophelia pertusa
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| Lophelia pertusa | ||||||||||||||
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| Lophelia pertusa (Linnaeus, 1758) |
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Dendrosmilia nomlandi |
Lophelia pertusa is a species of cold-water coral which grows in the deep waters throughout the North Atlantic ocean. L. pertusa reefs are home to a diverse community, however the species is extremely slow growing and may be harmed by destructive fishing practices, or oil exploration and extraction.
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[edit] Biology
Lophelia pertusa is a reef building, deep water coral, which is unusual for its lack of zooxanthellae - the symbiotic algae which lives inside most tropical reef building corals. Lophelia lives between 80 m to over 3000 m depth, but most commonly between 200 m to 1000 m depth, where there is no sunlight, and a temperature range from about 12 °C to 4 °C. As a coral, it represents a colonial organism, which consists of many individuals. New polyps live and build upon the calcium carbonate skeletal remains of previous generations. Living coral ranges in colour from white to orange-red. Unlike most tropical corals, the polyps are not interconnected by living tissue. Radiocarbon dating indicates that some Lophelia reefs in the waters off North Carolina may be 40,000 years old, with individual living coral bushes as much as 1,000 yrs old.
The coral reproduces by budding off new polyps and by producing free-living planktonic larvae which float in the water until they find a suitable surface to attach to and grow on.
Lophelia reefs can grow to 35 m high, be hundreds of metres wide, and the largest recorded reef measures 13 km, off the Lofoten Islands, Norway. When this is seen in terms of a growth rate of around 1 mm per year, the great age of these reefs becomes apparent.
Polyps at the end of branches feed by extending their tentacles and straining plankton from the seawater. The spring bloom of phytoplankton and subsequent zooplankton blooms, provide the main source of nutrient input to the deep sea. This rain of dead plankton is visible on photographs of the seabed and stimulates a seasonal cycle of growth and reproduction in Lophelia. This cycle is recorded in patterns of growth, and can be studied to investigate climatic variation in the recent past.
[edit] Conservation status
L. pertusa was listed under CITES Appendix II in January 1990, meaning that the United Nations Environmental Programme recognizes that this species is not necessarily currently threatened with extinction but that it may become so in the future. CITES is technically a means of restricting international trade in endangered species, which is not a major threat to the survival of L. pertusa. The OSPAR Commission for the protection of the marine environment of the North-East Atlantic have recognised Lophelia pertusa reefs as a threatened habitat in need of protection.
Main threats come from destruction of reefs by heavy deep-sea trawl nets, targeting redfish or grenadiers. The heavy metal "doors" which hold the mouth of the net open, and the "footline", which is equipped with large metal "rollers", are dragged along the sea bed, and have a highly damaging effect on the coral. Because the rate of growth is so slow, it is unlikely that that this practice will prove to be sustainable.
In recent years, environmental organisations such as Greenpeace have argued that exploration for oil on the north west continental shelf slopes of Europe should be curtailed due to the possibility that is it damaging to the Lophelia reefs - conversely, Lophelia has recently been observed growing on the legs of oil installations.[1]
[edit] Ecological significance
Lophelia beds create a specialised habitat favoured by some species of deep water fishes. Surveys have recorded conger eels, sharks, groupers and hake. The invertebrate community consists of brittle stars, molluscs, amphipods and crabs. High densities of smaller fish such as hatchetfish and lanternfish have been recorded in the waters over Lophelia beds, indicating they may be important prey items for the larger fish below.
[edit] Range
L. pertusa has been reported from Anguilla, Bahamas, Bermuda, Brazil, Canada, Cape Verde, Colombia, Cuba, Ecuador, France, French Southern Territories, Greece, Grenada, Iceland, India, Ireland, Italy, Jamaica, Japan, Madagascar, Mexico, Montserrat, Norway, Portugal, Puerto Rico, Saint Helena, Saint Kitts and Nevis, Saint Vincent and the Grenadines, Senegal, South Africa, United Kingdom, United States of America, U.S. Virgin Islands and Wallis and Futuna Islands.[2]
[edit] Notes
- ^ P. Whomersley and G.B. Picken (2003). Long-term dynamics of fouling communities found on offshore installations in the North Sea. Journal of the Marine Biological Association of the UK 83: 897-901.
- ^ As reported by CITES and the UNEP, and as such, is incomplete, and affected by development of marine science in that country, and effort put into surveying for it.
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