Coral reef is an underwater ecosystem characterized by reef-building corals.
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Coral reef is an underwater ecosystem characterized by reef-building corals.
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Coral reef belongs to the class Anthozoa in the animal phylum Cnidaria, which includes sea anemones and jellyfish.
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Coral reef theorized that uplift and subsidence of Earth's crust under the oceans formed the atolls.
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Fringing Coral reef, called a shore Coral reef, is directly attached to a shore, or borders it with an intervening narrow, shallow channel or lagoon.
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The surface of the fringe Coral reef generally remains at the same height: just below the waterline.
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Above all, the offshore outer Coral reef edge formed in open water rather than next to a shoreline.
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Coral reef ecosystems contain distinct zones that host different kinds of habitats.
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Each Coral reef is made up of irregular patches of algae, sessile invertebrates, and bare rock and sand.
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Coral reef heads consist of accumulations of individual animals called polyps, arranged in diverse shapes.
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Coral reef polyps do not photosynthesize, but have a symbiotic relationship with microscopic algae of the genus Symbiodinium, commonly referred to as zooxanthellae.
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Coral reef that loses a large fraction of its zooxanthellae becomes white and is said to be bleached, a condition which, unless corrected, can kill the coral.
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However many other organisms living in the reef community contribute skeletal calcium carbonate in the same manner as corals.
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The largest and strongest corals grew in parts of the reef exposed to the most violent surf and corals were weakened or absent where loose sediment accumulated.
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Those settling on the Coral reef include many other species, particularly crustaceans and polychaete worms.
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Coral reef systems provide important habitats for seabird species, some endangered.
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Large-scale systematic study of the Jarvis Island coral community, which experienced ten El Nino-coincident coral bleaching events from 1960 to 2016, found that the reef recovered from almost complete death after severe events.
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Coral reef restoration has grown in prominence over the past several decades because of the unprecedented reef die-offs around the planet.
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Coral reef gardens take advantage of a coral's natural ability to fragment and continuing to grow if the fragments are able to anchor themselves onto new substrates.
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One case study with coral reef restoration was conducted on the island of Oahu in Hawaii.
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Times of maximum reef development were in the Middle Cambrian, Devonian and Carboniferous, owing to order Rugosa extinct corals and Late Cretaceous and all Neogene, owing to order Scleractinia corals.
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