Coral reef

Marine habitats
Blue Linckia Starfish.JPG
Biodiversity of a coral reef

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.

Coral belongs to the class Anthozoa in the animal phylum Cnidaria, which includes sea anemones and jellyfish. Unlike sea anemones, corals secrete hard carbonate exoskeletons that support and protect the coral. Most reefs grow best in warm, shallow, clear, sunny and agitated water.

Often called "rainforests of the sea", shallow coral reefs form some of Earth's most diverse ecosystems. They occupy less than 0.1% of the world's ocean area, about half the area of France, yet they provide a home for at least 25% of all marine species,[1][2][3][4] including fish, mollusks, worms, crustaceans, echinoderms, sponges, tunicates and other cnidarians.[5] Coral reefs flourish in ocean waters that provide few nutrients. They are most commonly found at shallow depths in tropical waters, but deep water and cold water coral reefs exist on smaller scales in other areas.

Coral reefs deliver ecosystem services for tourism, fisheries and shoreline protection. The annual global economic value of coral reefs is estimated between US$30–375 billion.[6][7] Coral reefs are fragile, partly because they are sensitive to water conditions. They are under threat from excess nutrients (nitrogen and phosphorus), rising temperatures, oceanic acidification, overfishing (e.g., from blast fishing, cyanide fishing, spearfishing on scuba), sunscreen use[8] overuse and harmful land-use practices, including runoff and seeps (e.g., from injection wells and cesspools).[9][10][11]

Formation

Most coral reefs were formed after the last glacial period when melting ice caused sea level to rise and flood continental shelves. Most coral reefs are less than 10,000 years old. As communities established themselves, the reefs grew upwards, pacing rising sea levels. Reefs that rose too slowly could become drowned, without sufficient light.[12] Coral reefs are found in the deep sea away from continental shelves, around oceanic islands and atolls. The majority of these islands are volcanic in origin. Others have tectonic origins where plate movements lifted the deep ocean floor.

In The Structure and Distribution of Coral Reefs,[13] Charles Darwin set out his theory of the formation of atoll reefs, an idea he conceived during the voyage of the Beagle. He theorized that uplift and subsidence of the Earth's crust under the oceans formed the atolls.[14] Darwin set out a sequence of three stages in atoll formation. A fringing reef forms around an extinct volcanic island as the island and ocean floor subsides. As the subsidence continues, the fringing reef becomes a barrier reef and ultimately an atoll reef.

Darwin predicted that underneath each lagoon would be a bedrock base, the remains of the original volcano. Subsequent research supported this hypothesis. Darwin's theory followed from his understanding that coral polyps thrive in the tropics where the water is agitated, but can only live within a limited depth range, starting just below low tide. Where the level of the underlying earth allows, the corals grow around the coast to form fringing reefs, and can eventually grow become a barrier reef.

A fringing reef can take ten thousand years to form, and an atoll can take up to 30 million years.[15]

Where the bottom is rising, fringing reefs can grow around the coast, but coral raised above sea level dies. If the land subsides slowly, the fringing reefs keep pace by growing upwards on a base of older, dead coral, forming a barrier reef enclosing a lagoon between the reef and the land. A barrier reef can encircle an island, and once the island sinks below sea level a roughly circular atoll of growing coral continues to keep up with the sea level, forming a central lagoon. Barrier reefs and atolls do not usually form complete circles, but are broken in places by storms. Like sea level rise, a rapidly subsiding bottom can overwhelm coral growth, killing the coral and the reef, due to what is called coral drowning.[16] Corals that rely on zooxanthellae can die when the water becomes too deep for their symbionts to adequately photosynthesize, due to decreased light exposure.[17]

The two main variables determining the geomorphology, or shape, of coral reefs are the nature of the substrate on which they rest, and the history of the change in sea level relative to that substrate.

The approximately 20,000-year-old Great Barrier Reef offers an example of how coral reefs formed on continental shelves. Sea level was then 120 m (390 ft) lower than in the 21st century.[18][19] As sea level rose, the water and the corals encroached on what had been hills of the Australian coastal plain. By 13,000 years ago, sea level had risen to 60 m (200 ft) lower than at present, and many hills of the coastal plains had become continental islands. As sea level rise continued, water topped most of the continental islands. The corals could then overgrow the hills, forming cays and reefs. Sea level on the Great Barrier Reef has not changed significantly in the last 6,000 years.[19] The age of living reef structure is estimated to be between 6,000 and 8,000 years.[20] Although the Great Barrier Reef formed along a continental shelf, and not around a volcanic island, Darwin's principles apply. Development stopped at the barrier reef stage, since Australia is not about to submerge. It formed the world's largest barrier reef, 300–1,000 m (980–3,280 ft) from shore, stretching for 2,000 km (1,200 mi).[21]

Healthy tropical coral reefs grow horizontally from 1 to 3 cm (0.39 to 1.18 in) per year, and grow vertically anywhere from 1 to 25 cm (0.39 to 9.84 in) per year; however, they grow only at depths shallower than 150 m (490 ft) because of their need for sunlight, and cannot grow above sea level.[22]

Material

As the name implies, coral reefs are made up of coral skeletons from mostly intact coral colonies. As other chemical elements present in corals become incorporated into the calcium carbonate deposits, aragonite is formed. However, shell fragments and the remains of coralline algae such as the green-segmented genus Halimeda can add to the reef's ability to withstand damage from storms and other threats. Such mixtures are visible in structures such as Eniwetok Atoll.[23]

Other Languages
Afrikaans: Koraalrif
العربية: شعاب مرجانية
asturianu: Petón de coral
azərbaycanca: Mərcan rifi
Bân-lâm-gú: San-ô͘-chiau
башҡортса: Мәрйен рифтары
беларуская: Каралавыя рыфы
български: Коралов риф
bosanski: Koralni greben
čeština: Korálový útes
dansk: Koralrev
Deutsch: Korallenriff
eesti: Korallrahu
Esperanto: Korala rifo
føroyskt: Korallriv
français: Récif corallien
한국어: 산호초
hrvatski: Koraljni greben
Bahasa Indonesia: Terumbu karang
íslenska: Kóralrif
Basa Jawa: Terumbu karang
ქართული: მარჯნის რიფი
kaszëbsczi: Rafa
Kreyòl ayisyen: Resif koray
latviešu: Koraļļu rifs
lietuvių: Koralinis rifas
македонски: Корален гребен
Bahasa Melayu: Terumbu karang
Nederlands: Koraalrif
日本語: サンゴ礁
norsk: Korallrev
norsk nynorsk: Korallrev
occitan: Arrecife
oʻzbekcha/ўзбекча: Marjon riflari
ਪੰਜਾਬੀ: ਮੂੰਗਾ ਚਟਾਨ
Papiamentu: Ref di koral
português: Recife de coral
română: Recif de corali
සිංහල: කොරල් පර
Simple English: Coral reef
slovenčina: Koralový útes
slovenščina: Koralni greben
српски / srpski: Корални гребен
srpskohrvatski / српскохрватски: Koraljni greben
svenska: Korallrev
Türkçe: Mercan resifi
українська: Кораловий риф
Tiếng Việt: Rạn san hô
吴语: 珊瑚礁
粵語: 珊瑚礁
中文: 珊瑚礁