Milne-Edwards & Haime, 1849
|Known range (NOAA)|
Lophelia pertusa, the only species in the genus Lophelia, is a cold-water coral that grows in the deep waters throughout the North Atlantic ocean, as well as parts of the Caribbean Sea and Alboran Sea. Although L. pertusa reefs are home to a diverse community, the species is extremely slow growing and may be harmed by destructive fishing practices, or oil exploration and extraction.
Lophelia pertusa is a reef building, deep water coral, but it does not contain zooxanthellae, the symbiotic algae which lives inside most tropical reef building corals. Lophelia lives at a temperature range from about 4–12 °C (39–54 °F) and at depths between 80 metres (260 ft) and over 3,000 metres (9,800 ft), but most commonly at depths of 200–1,000 metres (660–3,280 ft), where there is no sunlight.
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; each polyp has up to 16 tentacles and is a translucent pink, yellow or white. Unlike most tropical corals, the polyps are not interconnected by living tissue. Some colonies have larger polyps while others have small and delicate -looking ones. 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 years old.
The colony grows by the budding off of new polyps. Living polyps are present on the edges of dead coral and fragmentation of coral colonies provides one form of asexual reproduction. Each colony is either male or female and sexual reproduction occurs when these liberate sperm and oocytes into the sea. The larvae do not have a feeding stage, but sustain themselves on their yolks and drift with the plankton, possibly for several weeks. When settling on the seabed, they undergo metamorphosis and develop into polyps, which then potentially start new colonies.
Lophelia reefs can grow to 35 m (115 ft) high. The largest recorded Lophelia reef, Røst Reef, measures 3 km × 35 km (1.9 mi × 21.7 mi) and lies at a depth of 300–400 m (980–1,310 ft) 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. They are able to ingest particles of up to 2 cm, and are able to discriminate between food and sediment using their chemoreceptors to differentiate between the two. Growth of polyps depends on environmental factors such as food availability, water quality, and how the water flows.
L. pertusa are considered to be opportunistic feeders since they feed on particles of organic matter that have been broken down.  Hence, 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.
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 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 recognized 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 this practice will prove to be sustainable.
Scientists estimate that trawling has damaged or destroyed 30%–50% of the Norwegian shelf coral area. The International Council for the Exploration of the Sea, the European Commission’s main scientific advisor on fisheries and environmental issues in the northeast Atlantic, recommend mapping and then closing all of Europe’s deep corals to fishing trawlers.
In 1999, the Norwegian Ministry of Fisheries closed an area of 1,000 square kilometres (390 sq mi) at Sula, including the large reef, to bottom trawling. In 2000, an additional area closed, covering about 600 square kilometres (230 sq mi). An area of about 300 square kilometres (120 sq mi) enclosing the Røst Reef closed to bottom trawling in 2002. Bottom trawling leads to siltation or sand deposition, which involves the disturbance of underlying sediments and nutrients. This harmful process destroys and decreases the growth of coral reefs, affecting the expansion of polyp budding.
In recent years, environmental organizations 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, specifically the Brent Spar rig which Greenpeace campaigned to remove. At the time, the growth of L. pertusa on the legs of oil rigs was considered unusual, although recent studies have shown this to be a common occurrence, with 13 of 14 North Sea oil rigs examined having L. pertusa colonies. The authors of the original work suggested that it may be better to leave the lower parts of such structures in place— a suggestion opposed by Greenpeace campaigner Simon Reddy, who compared it to "[dumping] a car in a wood – moss would grow on it, and if I was lucky a bird may even nest in it. But this is not justification to fill our forests with disused cars".
Recovery of damaged L.pertusa will be a slow process not only due to its slow growth rate, but also due to its low rates of colonization and recolonization process. This is because even if L.pertusa produces a dispersive larva, a sediment free surface is required to initiate a new settlement. Moreover, excessive sedimentation and chemical contaminants will negatively impact the larvae, even when they are available in large numbers.
As ocean temperatures continue to rise due to global warming, climate change is another deadly factor that threatens the existence of L. pertusa. Although L. pertusa can survive changes in oxygen levels during periods of hypoxia and anoxia, they are vulnerable to sudden temperature changes. These fluctuations in temperature affect their metabolic rate, which has detrimental consequences regarding their energy input and growth. 
Lophelia beds create a specialized habitat favored by some species of deep water fishes. Surveys have recorded that conger eels, sharks, groupers, hake and the invertebrate community consisting of brittle stars, molluscs, amphipods and crabs reside on these beds. 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.
L. pertusa also forms a symbiosis with polychaete Eunice norvegica. It is suggested that E. norvegica positively influences L.pertusa by forming connecting tubes, which are later calcified, in order to strengthen the reef frameworks. While E. norvegica requires partial consumption of the food obtained by L. pertusa, E. norvegica aids in cleaning the living coral framework and protecting it from potential predators.
Foraminiferans including Hyrrokkin sarcophaga also carry out a parasitic relationship with L. pertusa by attaching to polyps on the coral. Although settlement and reproduction are carried out by H. sarchophaga, this parasitism is not detrimental to the coral.
L. pertusa has been reported from Anguilla, Bahamas, Bermuda, Brazil, Canada, Cape Verde, Colombia, Cuba, Cyprus, Ecuador, Faroe Islands, 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.
- ^ Bert Hoeksema (2011). "Lophelia pertusa (Linnaeus, 1758)". WoRMS. World Register of Marine Species. Retrieved 27 March 2012.
- ^ Stephen Cairns & Bert Hoeksema (2011). "Lophelia Milne-Edwards & Haime, 1849". WoRMS. World Register of Marine Species. Retrieved March 26, 2012.
- ^ Cheryl L. Morrison; Robin L. Johnson; Tim L. King; Steve W. Ross; Martha S. Nizinski (2008). "Molecular assessment of deep-sea scleractinian coral biodiversity and population structure of Lobelia pertusa in the Gulf of Mexico". In Kenneth J. Sulak; Michael Randall; Kirsten E. Luke; April D. Norem; Jana M. Miller (eds.). Characterization of Northern Gulf of Mexico Deepwater Hard Bottom Communities with Emphasis on Lophelia Coral – Lophelia Reef Megafunal Community Structure, Biotopes, Genetics, Microbial Ecology, and Geology (2004–2006) (PDF). United States Geological Survey. pp. 4-1–4-77. USGS Open-File Report 2008-1148.
- ^ C. Michael Hogan. 2011. Alboran Sea. eds. P. Saundry & C. J. Cleveland. Encyclopedia of Earth. National Council for Science and the Environment. Washington DC
- ^ a b Rogers, Alex David (1999). "The Biology ofLophelia pertusa(L. 1758) and Other Deep-Water Reef-Forming Corals and Impacts from Human Activities". International Review of Hydrobiology. 84 (4): 315–406. doi:10.1002/iroh.199900032. ISSN 1434-2944.
- ^ Rogers, Alex David (1999). "The Biology ofLophelia pertusa(L. 1758) and Other Deep-Water Reef-Forming Corals and Impacts from Human Activities". International Review of Hydrobiology. 84 (4): 315–406. doi:10.1002/iroh.199900032. ISSN 1434-2944.
- ^ a b c Shaw, E.; Sussman, S. (2014). "Lophelia pertusa". Animal Diversity Web. Retrieved 27 June 2017.
- ^ Coral reefs in Norway (2002). Large Lophelia pertusa reef discovered off Røst in Lofoten. Archived 2012-08-29 at the Wayback Machine Institute of Marine Research, Norway.
- ^ a b Mortensen, Pål Buhl (April 2001). "Aquarium observations on the deep-water coral Lophelia pertusa (L., 1758) (scleractinia) and selected associated invertebrates". Ophelia. 54 (2): 83–104. doi:10.1080/00785236.2001.10409457. ISSN 0078-5326. S2CID 87985061.
- ^ Strömberg, Susanna M.; Östman, Carina (April 2017). "The cnidome and internal morphology of Lophelia pertusa (Linnaeus, 1758) (Cnidaria, Anthozoa)". Acta Zoologica. 98 (2): 191–213. doi:10.1111/azo.12164. PMC 5363355. PMID 28392575.
- ^ a b "Deep Water Corals". coris.noaa.gov. Archived from the original on February 21, 2010. Retrieved August 29, 2009.
- ^ Fosså, J.H.; Mortensen, P.B.; Furevik, D.M. (2002-03-01). "The deep-water coral Lophelia pertusa in Norwegian waters: distribution and fishery impacts". Hydrobiologia. 471 (1): 1–12. doi:10.1023/A:1016504430684. ISSN 1573-5117. S2CID 40904134.
- ^ Whomersley, P.; Picken, G.B. (October 2003). "Long-term dynamics of fouling communities found on offshore installations in the North Sea". Journal of the Marine Biological Association of the United Kingdom. 83 (5): 897–901. doi:10.1017/S0025315403008014h. S2CID 85598319.
- ^ Bell, Niall; Smith, Jan (1999-12-09). "Coral growing on North Sea oil rigs" (PDF). Nature. 402: 601. Retrieved 2022-05-13.
- ^ Gass, Susan E.; Roberts, J. Murray (May 2006). "The occurrence of the cold-water coral Lophelia pertusa (Scleractinia) on oil and gas platforms in the North Sea: Colony growth, recruitment and environmental controls on distribution". Marine Pollution Bulletin. 52 (5): 549–559. doi:10.1016/j.marpolbul.2005.10.002. PMID 16300800. INIST:17830117.
- ^ "Oil rig home to rare coral". BBC News. 8 December 1999. Retrieved 14 September 2017.
- ^ Rogers, Alex David (1999). "The Biology of Lophelia pertusa (L. 1758) and Other Deep-Water Reef-Forming Corals and Impacts from Human Activities". International Review of Hydrobiology. 84 (4): 315–406. Bibcode:1999IRH....84..315R. doi:10.1002/iroh.199900032.
- ^ Dodds, L. A.; Roberts, J. M.; Taylor, A. C.; Marubini, F. (2007-10-19). "Metabolic tolerance of the cold-water coral Lophelia pertusa (Scleractinia) to temperature and dissolved oxygen change". Journal of Experimental Marine Biology and Ecology. 349 (2): 205–214. doi:10.1016/j.jembe.2007.05.013. ISSN 0022-0981.
- ^ Mueller, Christina E.; Lundälv, Tomas; Middelburg, Jack J.; Oevelen, Dick van (2013-03-11). "The Symbiosis between Lophelia pertusa and Eunice norvegica Stimulates Coral Calcification and Worm Assimilation". PLOS ONE. 8 (3): e58660. Bibcode:2013PLoSO...858660M. doi:10.1371/journal.pone.0058660. ISSN 1932-6203. PMC 3594175. PMID 23536808.
- ^ 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.
Media related to Lophelia pertusa at Wikimedia Commons