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Canton Island typifies the isolated coral atolls dotting the Pacific Ocean. The Structure and Distribution of Coral Reefs, Being the first part of the geology of the voyage of the Beagle, under the command of Capt. Fitzroy, R.N. during the years 1832 to 1836, was published in 1842 as Charles Darwin's first monograph, and set out his theory of the formation of coral reefs and atolls.
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. [1] 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 ...
Spur and groove formations are a geomorphic feature of many coral reefs. They are ridges of reef formed by coral ("spurs") separated by channels ("grooves") which often have sediment or rubble bed. Spur and groove formations vary in their size and distribution worldwide but are a common feature on many forereefs of fringing reefs , barrier ...
While it covers only 1.6% of the planet's oceanic area, the region has 76% of all known coral species in the world. As a habitat for 52% of Indo-Pacific reef fishes and 37% of the world's reef fishes, it contains the greatest diversity of coral reef fishes in the world [17] More than 3,000 species of bony fish are distributed over more than 90% of the Coral Triangle.
Coral reef at Nusa Lembongan, Bali, Indonesia Pamalican island with surrounding reef, Sulu Sea, Philippines A reef surrounding an islet Reefs off Vanatinai Island in the Louisiade Archipelago. A reef is a ridge or shoal of rock, coral, or similar relatively stable material lying beneath the surface of a natural body of water. [1]
The fringing reef becomes a barrier reef for the reason that the outer part of the reef maintains itself near sea level through biotic growth, while the inner part of the reef falls behind, becoming a lagoon because conditions are less favorable for the coral and calcareous algae responsible for most reef growth.
The part of the Coral Triangle's coral reef area that lies within the Philippines ranges from 10,750 square kilometers (4,150 sq mi) to 33,500 square kilometers (12,900 sq mi). It contains over 500 species of scleractinian or stony corals, and at least 12 endemic coral species. [10]
Diagram showing a coral polyp, its corallite, coenosarc and coenosteum Up : zoom on the skeletal cup of an Astrangia coral; Down : view of the skeleton of the whole colony, showing all the coralittes. A corallite is the skeletal cup, formed by an individual stony coral polyp, in which the polyp sits and into which it