The approximately 20,000-year-old Great Barrier Reef offers an example of how coral reefs formed on continental shelves. 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. Corals that rely on zooxanthellae can die when the water becomes too deep for their symbionts to adequately photosynthesize, due to decreased light exposure. 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. ![]() Barrier reefs and atolls do not usually form complete circles but are broken in places by storms. 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. 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. Where the bottom is rising, fringing reefs can grow around the coast, but coral raised above sea level dies. As the subsidence continues, the fringing reef becomes a barrier reef and ultimately an atoll reef.Ī fringing reef can take ten thousand years to form, and an atoll can take up to 30 million years. A fringing reef forms around an extinct volcanic island as the island and ocean floor subside. Darwin set out a sequence of three stages in atoll formation. He theorized that uplift and subsidence of Earth's crust under the oceans formed the atolls. In The Structure and Distribution of Coral Reefs, Charles Darwin set out his theory of the formation of atoll reefs, an idea he conceived during the voyage of the Beagle. Others have tectonic origins where plate movements lifted the deep ocean floor. The majority of these islands are volcanic in origin. Coral reefs are also found in the deep sea away from continental shelves, around oceanic islands and atolls. Reefs that rose too slowly could become drowned, without sufficient light. As communities established themselves, the reefs grew upwards, pacing rising sea levels. Most coral reefs are less than 10,000 years old. Most coral reefs were formed after the Last Glacial Period when melting ice caused sea level to rise and flood continental shelves. See also: Fringing reef, Atoll, and The Structure and Distribution of Coral Reefs The annual global economic value of coral reefs has been estimated at anywhere from US$30–375 billion (19 estimates) to US$2.7 trillion (a 2020 estimate) to US$9.9 trillion (a 2014 estimate). Ĭoral reefs deliver ecosystem services for tourism, fisheries and shoreline protection. They are under threat from excess nutrients (nitrogen and phosphorus), rising ocean heat content and acidification, overfishing (e.g., from blast fishing, cyanide fishing, spearfishing on scuba), sunscreen use, and harmful land-use practices, including runoff and seeps (e.g., from injection wells and cesspools). 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.Ĭoral reefs have declined by 50% since 1950, partly because they are sensitive to water conditions. Coral reefs flourish in ocean waters that provide few nutrients. 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, including fish, mollusks, worms, crustaceans, echinoderms, sponges, tunicates and other cnidarians. Sometimes called rainforests of the sea, shallow coral reefs form some of Earth's most diverse ecosystems. Coral reefs first appeared 485 million years ago, at the dawn of the Early Ordovician, displacing the microbial and sponge reefs of the Cambrian. ![]() Most reefs grow best in warm, shallow, clear, sunny and agitated water. Unlike sea anemones, corals secrete hard carbonate exoskeletons that support and protect the coral. Most coral reefs are built from stony corals, whose polyps cluster in groups.Ĭoral belongs to the class Anthozoa in the animal phylum Cnidaria, which includes sea anemones and jellyfish. Reefs are formed of colonies of coral polyps held together by calcium carbonate. A coral reef is an underwater ecosystem characterized by reef-building corals.
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |