Lophelia

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Lophelia
Lophelia spec.jpg
CITES Appendix II (CITES)
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Cnidaria
Class: Hexacorallia
Order: Scleractinia
Family: Caryophylliidae
Genus: Lophelia
Milne-Edwards & Haime, 1849
Species:
L. pertusa
Binomial name
Lophelia pertusa
Lophelia worldmap 372.jpg
Known range (NOAA)
Synonyms   [1]
  • Dendrosmilia nomlandiDurham & Barnard, 1952
  • Lophelia californicaDurham, 1947
  • Lophelia prolifera(Pallas, 1766)
  • Lophohelia affinisPourtalès, 1868
  • Lophohelia prolifera
  • Lophohelia prolifera f. brachycephalaMoseley, 1881
  • Lophohelia prolifera f. gracilisDuncan, 1873
  • Lophohelia subcostataMilne-Edwards & Haime, 1850
  • Lophohelia tubulosaStuder, 1878
  • Madrepora pertusaLinnaeus, 1758
  • Madrepora proliferaPallas, 1766

Lophelia pertusa, the only species in the genus Lophelia, [2] [3] 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. [4] 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. [5]

Contents

Biology

Lophelia pertusa Lophelia figure 1 600.jpg
Lophelia pertusa

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. [6] 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. [7]

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. [7] 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 budding new polyps, with living ones emerging around the outer edges of deceased coral. Coral colonies reproduce asexually through fragmentation. Each colony is gendered, engaging in sexual reproduction by releasing sperm or oocytes into the sea. The larvae, which do not feed but rely on their yolk reserves, drift with plankton for weeks. Upon settling on the seabed, they undergo metamorphosis, developing into polyps capable of initiating new colonies. [7]

New polyps grow on the outer edges when Lophelia pertusa experiences budding or regeneration. Lophelia pertusa NOAA.jpg
New polyps grow on the outer edges when Lophelia pertusa experiences budding or regeneration.

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. [8] These reefs are ancient, with a growth rate of around 1 mm per year.

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. [9]

L. pertusa are considered to be opportunistic feeders since they feed on particles of organic matter that have been broken down. [10] 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.

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 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. [5]

The primary threats arise from the devastation of reefs caused by the use of heavy deep-sea trawl nets, specifically aimed at catching redfish or grenadiers. These nets, equipped with heavy metal "doors" to keep the net open, and a "footline" fitted with large metal "rollers," are dragged across the seabed, inflicting severe damage on coral. Given the slow growth rate of coral, this practice is unlikely to be sustainable in the long term.

A squat lobster living on a Lophelia reef Lophelia fauna 600.jpg
A squat lobster living on a Lophelia reef

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. [11]

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. [11] 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. [12]

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, [13] 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, [14] although recent studies have shown this to be a common occurrence, with 13 of 14 North Sea oil rigs examined having L. pertusa colonies. [15] 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". [16]

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. [17]

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. [18]

Ecological significance

L. pertusa in its ecological environment. Expl0006 - Flickr - NOAA Photo Library.jpg
L. pertusa in its ecological environment.

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. [19]

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. [9]

Range

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. [20]

Related Research Articles

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Corals are colonial marine invertebrates within the class Anthozoa of the phylum Cnidaria. They typically form compact colonies of many identical individual polyps. Coral species include the important reef builders that inhabit tropical oceans and secrete calcium carbonate to form a hard skeleton.

<span class="mw-page-title-main">Coral reef</span> Outcrop of rock in the sea formed by the growth and deposit of stony coral skeletons

A coral reef is an underwater ecosystem characterized by reef-building corals. Reefs are formed of colonies of coral polyps held together by calcium carbonate. Most coral reefs are built from stony corals, whose polyps cluster in groups.

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<span class="mw-page-title-main">Anthozoa</span> Class of cnidarians without a medusa stage

Anthozoa is a class of marine invertebrates which includes the sea anemones, stony corals and soft corals. Adult anthozoans are almost all attached to the seabed, while their larvae can disperse as part of the plankton. The basic unit of the adult is the polyp; this consists of a cylindrical column topped by a disc with a central mouth surrounded by tentacles. Sea anemones are mostly solitary, but the majority of corals are colonial, being formed by the budding of new polyps from an original, founding individual. Colonies are strengthened by calcium carbonate and other materials and take various massive, plate-like, bushy or leafy forms.

<span class="mw-page-title-main">Scleractinia</span> Order of Hexacorallia which produce a massive stony skeleton

Scleractinia, also called stony corals or hard corals, are marine animals in the phylum Cnidaria that build themselves a hard skeleton. The individual animals are known as polyps and have a cylindrical body crowned by an oral disc in which a mouth is fringed with tentacles. Although some species are solitary, most are colonial. The founding polyp settles and starts to secrete calcium carbonate to protect its soft body. Solitary corals can be as much as 25 cm (10 in) across but in colonial species the polyps are usually only a few millimetres in diameter. These polyps reproduce asexually by budding, but remain attached to each other, forming a multi-polyp colony of clones with a common skeleton, which may be up to several metres in diameter or height according to species.

<span class="mw-page-title-main">Alcyonacea</span> Order of octocorals that do not produce massive calcium carbonate skeletons

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References

  1. ↑ Bert Hoeksema (2011). "Lophelia pertusa (Linnaeus, 1758)". WoRMS. World Register of Marine Species . Retrieved 27 March 2012.
  2. ↑ Stephen Cairns & Bert Hoeksema (2011). "Lophelia Milne-Edwards & Haime, 1849". WoRMS. World Register of Marine Species . Retrieved March 26, 2012.
  3. ↑ 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.
  4. ↑ C. Michael Hogan. 2011. Alboran Sea. eds. P. Saundry & C. J. Cleveland. Encyclopedia of Earth. National Council for Science and the Environment. Washington DC
  5. 1 2 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. Bibcode:1999IRH....84..315R. doi:10.1002/iroh.199900032. ISSN   1434-2944.
  6. ↑ 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. Bibcode:1999IRH....84..315R. doi:10.1002/iroh.199900032. ISSN   1434-2944.
  7. 1 2 3 Shaw, E.; Sussman, S. (2014). "Lophelia pertusa". Animal Diversity Web. Retrieved 27 June 2017.
  8. ↑ 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.
  9. 1 2 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.
  10. ↑ 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.
  11. 1 2 "Deep Water Corals". coris.noaa.gov. Archived from the original on February 21, 2010. Retrieved August 29, 2009.
  12. ↑ 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.
  13. ↑ 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. Bibcode:2003JMBUK..83..897W. doi:10.1017/S0025315403008014h. S2CID   85598319.
  14. ↑ Bell, Niall; Smith, Jan (1999-12-09). "Coral growing on North Sea oil rigs" (PDF). Nature. 402 (6762): 601. Bibcode:1999Natur.402..601B. doi:10.1038/45127. S2CID   4401771 . Retrieved 2022-05-13.
  15. ↑ 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. Bibcode:2006MarPB..52..549G. doi:10.1016/j.marpolbul.2005.10.002. PMID   16300800. INIST   17830117.
  16. ↑ "Oil rig home to rare coral". BBC News. 8 December 1999. Retrieved 14 September 2017.
  17. ↑ 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.
  18. ↑ 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.
  19. ↑ 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.
  20. ↑ 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.[ citation needed ]
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