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Published byMaurice French Modified over 9 years ago
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Invertebrate marine animal A polyp that begins to form an exoskeleton ◦ CO 2 & Ca in the water to make calcium carbonate (CaCO 3 ) aka limestone Sessile – immobile Form colonies
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Coral atolls 1 st proposed by Charles Darwin ◦ HMS Beagle (Nov 1835 – Apr 1836) Supported and modified by 2 geologists ◦ James Daly ◦ Reginald Dana
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1. Oceanic volcano emerges from sea surface and forms an island ◦ Colonized by reef-building corals
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2. Growth of corals forms a fringing reef around the island ◦ Fringing reef – coral structure attached to the mainland or continental islands Island begins to sink slowly Coral growth continues
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3. Island continues to sink Barrier reef forms with lagoon around reef and island ◦ Barrier reef - reef separated from a mainland or island shore by a deep channel or lagoon
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4. Island eventually disappears below sea surface Atoll - consists of a ring of small islands Shallow lagoon in center
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Fringing reef can take 10,000 years to form Atolls up to 30 my Coral – tan and purple
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Data from deep drilling on coral atolls ◦ Bikini Atoll (Pacific Ocean) ◦ As depth of corals increased, age of corals also increased ◦ Fossil corals dated 50 myo and found 1200 m deep Grown on underlying volcanic rock ◦ Shallow corals found at deep depths!
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Darwin (1842) produced 1 st map of distribution of corals 3 main types: ◦ Fringing barrier reefs, barrier reefs, atolls
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Conditions required: ◦ Temperature range =16 ⁰C – 35 ⁰C Optimum range = 23 ⁰C - 25 ⁰C ◦ Water clarity Clear water (less turbid) without silt Silt reduces light penetration which inhibits photosynthesis of symbiotic zooxanthellae in coral tissues (90% nutrients provided) Depth – rapid growth occurs within 20 m from surface ◦ Salinity ◦ Substrate – surface on which plant/animals live Basaltic rocks of seamounts
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http://m.youtube.com/#/watch?feature=yout u.be&v=35ilnGM9EnU&desktop_uri=%2Fwatc h%3Fv%3D35ilnGM9EnU%26feature%3Dyoutu. be http://m.youtube.com/#/watch?feature=yout u.be&v=35ilnGM9EnU&desktop_uri=%2Fwatc h%3Fv%3D35ilnGM9EnU%26feature%3Dyoutu. be
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Zooxanthellae in Coral Polyp
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Zooxanthellae: Symbiodinium microadriacticum
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A Solitary Coral Polyp
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Colonial Coral Polyps
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Benefits to the Algal Symbiont Zooxanthellae gets a place to live Receive chemical wastes from animal metabolism (CO 2 & NH 3 ). Surrounding animal tissues can concentration substantial amounts of ultraviolet light absorbing compounds.
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Benefits to the Coral Host Higher rates of calcification (skeleton deposition). Receive DOM & O 2 Removal of chemical wastes from animal metabolism (CO 2 & NH 3 ). Receive chemicals that absorb damaging ultraviolet light (Micosporine-like amino acids (MAAs)).
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What’s going on here?
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Distribution of Coral Reef Communities
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Shoreline protection from erosion - ◦ Dissipates/absorbs energy of waves Benefits include protection of ◦ Coastal properties ◦ Ecosystems ◦ Costs to provide breakwaters – constructed structures for protection from erosion ◦ Anchorage of boats
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Coral Gardens Fiji (Pacific Ocean) Coral Gardens Fiji (Pacific Ocean) Egypt (Red Sea) Egypt (Red Sea) Baja Baja
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