Where are Coral Reefs Located?
Coral reefs are located in tropical oceans near the equator.
Tropical Oceans are Shown in Green
The largest coral reef is the Great Barrier Reef in Australia.
The second largest coral reef can be found off the coast of Belize, in Central America.
Other reefs are found in Hawaii, the Red Sea, and other areas in tropical oceans.
Types of Coral Reefs
Most reef scientists generally recognize three basic types of coral reefs:
• Atoll - a roughly circular (annular) oceanic reef system surrounding a central lagoon
• Barrier Reef - a reef system that parallel the shore and is separated from it by a wide lagoon that contains at least
some deep portions
• Fringing Reef - a reef system that grow fairly close to (or directly from) the shore, with an entirely shallow lagoon or no
lagoon at all
The three main types of coral reefs: (a) atoll (left), (b) barrier reef (center) Courtesy NASA, and (c) fringing reef (right) © Fotolia.com
The differences between these three main reef types are often quite pronounced in terms of large-scale structural features. Nonetheless, there is often a good deal of similarity between them within a given biogeographic region in terms of dominant species of coral reef fishes, reef-building corals, and other forms of marine life, as well as their ecological interactions within the coral reef biome.
Development of Major Reef Types
The basic coral reef classification scheme described above was first proposed by Charles Darwin, and is still widely used today.
The evolution of the three main types of coral reefs, as first proposed by Charles Darwin
Darwin spent most of his coral reef explorations in the Indo-Pacific region, and viewed the three types of coral reefs he described as simply different stages in the geological 'evolution" of Pacific oceanic islands.
Darwin theorized that fringing reefs began to grow near the shorelines of new islands as ecological conditions became ideal for hard coral growth.
Then, as the island began to gradually subside into the sea, the coral was able to keep pace in terms of growth and remained in place at the sea surface, but farther from shore; it was now a barrier reef. Eventually, the island disappeared below the sea surface, leaving only the ring of coral encircling the central lagoon; an atoll had formed (see diagram, left).
Darwin's general "reef evolution" theory was finally verified for Indo-Pacific reefs in the early 1950s after analyses of the results of deep core drilling at Bikini and Eniwetok Atolls. However, it has also now become apparent that each of these three types of coral reef can, in some instances, also be formed by different processes as well. This is clearly the case with most of the relatively few true atolls that occur among Caribbean coral reefs.
*A Note On Patch Reefs
Numerous patch reefs. © Fotolia
The term "patch reef" is commonly used to refer to comparatively small, isolated outcrops of coral surrounded by sand and/or seagrass (see photo, left). These have sometimes been described as a fourth "coral reef type", but such comparisons are clearly not appropriate.
Patch reefs are microscale reef features common to fringing reefs, atolls and barrier reef systems throughout the world. They are not remotely comparable to, and should not be confused with, the three macroscale types of coral reef systems first described by Darwin and still used in that context today..
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