Coral Reefs What is coral? It’s a living organism! It is an invertebrate Cnidaria!! Sun Coral Polyps Where Can You Find Coral Reefs? Coral is found all over the world: Tropical Temperate Only tropical corals build reefs Coral reefs around the world Coral Builds Reefs? The animal portion of the reef is called a polyp The polyp absorbs calcium carbonate out of the water The calcium carbonate is used to build the reef Coral are Cnidarians Soft bodied Carnivorous Stinging tentacles arranged in a circle around their mouth Radial symmetry Cnidarians Usually two life stages: Polyp Medusa Anatomy of Coral The coral polyps build a calcium carbonate cup called a corallite to live in Coral has stinging cells called nematocysts Stinging Cells Nematocysts help coral catch food They also help protect the coral When the cell is stimulated, it releases a sharp barb The barb will fire and catch the food and bring it back towards the mouth Coral and Zooxanthella (algae) Symbiotic relationship Zooxanthella is an algae that lives in the skin of coral Coral provides protection Zooxanthella provides food and color! Coral is Picky Very specific habitats: Temperature: 73-75F Depth: Less than 80 ft to 230 feet Salinity: Normal salt levels (35ppt) Light: Zooxanthellae need light to survive Sedimentation: Being covered with silt interferes with photosynthesis Desiccation: being exposed to air. The corals will die if exposed too long Key Concepts Coral reefs are primarily found in tropical clear water, usually at depths of 60 meters or less. The three major types of coral reefs are fringing reefs, barrier reefs, and atolls. Both physical and biological factors determine the distribution of organisms on a reef. © 2006 Thomson-Brooks Cole Key Concepts Stony corals are responsible for the large colonial masses that make up the bulk of a coral reef. Reef-forming corals rely on symbiotic dinoflagellates called “zooxanthellae” to supply nutrients and to produce an environment suitable for formation of the coral skeleton. Coral reefs are constantly forming and breaking down. © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Key Concepts The most important primary producers on coral reefs are symbiotic zooxanthellae and turf algae. Coral reefs are oases of high productivity in nutrient-poor tropical seas. © 2006 Thomson-Brooks Cole World of Coral Reefs Coral reefs are highly productive, but occur in nutrient-poor waters This is made possible by the symbiotic relationship between coral animals and zooxanthellae © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Coral Animals Coral nutrition symbiotic zooxanthellae supply 90% of nutritional needs of stony coral coral polyp provides a suitable habitat and nutrients, absorbed directly through the animal’s tissues zooxanthellae remove CO2 and produce O2 need of zooxanthellae for sunlight limits the depths to which stony corals can grow © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Coral Animals Coral nutrition (continued) corals as predators small animals paralyzed by the nematocysts are passed into the digestive cavity © 2006 Thomson-Brooks Cole Coral Animals Coral nutrition (continued) other sources of nutrition corals can feed off bacteria living in their tissues, which feed on dissolved organic matter directly from the water © 2006 Thomson-Brooks Cole Coral Reef Types Fringing reefs border islands or continental landmasses © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Coral Reef Types Barrier reefs are similar to fringing reefs but separated from the landmass and fringing reef by lagoons or deepwater channels © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Coral Reef Types Atolls, usually elliptical, arise out of deep water and have a centrally-located lagoon © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Reef Structure Reef front or forereef—portion of the reef that rises from the lower depths of the ocean to a level just at or just below the surface of the water, on the seaward side © 2006 Thomson-Brooks Cole Reef Structure Reef crest—the highest point on the reef and the part that receives the full impact of wave energy Reef flat or back reef—portion behind the reef crest © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Coral Reef Distribution Major factors influencing distribution: temperature – corals do best at 23-25o C light availability – photosynthetic zooxanthellae need light sediment accumulation – can reduce light and clog feeding structures salinity wave action – moderate wave action brings in oxygenated seawater, removes sediment that could smother coral polyps duration of air exposure – can be deadly © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Coral Reef Ecology Coral provides: foundation for reef food webs shelter for resident organisms Reefs form a complex 3-dimensional habitat for many beautiful and strange creatures © 2006 Thomson-Brooks Cole Coral Reef Community Sponges and cnidarians sessile organisms, though anemones can move if necessary filter feed; anemones also paralyze and consume small fishes and crustaceans Annelids sessile filter feeders include featherduster and Christmas tree worms fireworms are mobile predators palolo worms burrow through and weaken coral and usually deposit feed © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Coral Reef Community Crustaceans shrimps, crabs and lobsters vary from parasites to active hunters Molluscs gastropods eat algae from coral surfaces giant clams are filter feeders, but also host symbiotic zooxanthellae octopus and squid are active predators © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Coral Reef Community Echinoderms feather stars, sea urchins, brittle stars, sea stars, and sea cucumbers filter feed, scavenge, or eat sediment Reef fishes most prominent and diverse inhabitant diverse food sources, including detritus, algae, sponges, coral, invertebrates, other fish © 2006 Thomson-Brooks Cole Species Interactions on Coral Reefs Competition among corals fast-growing, branching corals grow over slower- growing, encrusting or massive corals and deny them light slower-growing corals extend stinging filaments from their digestive cavity to kill faster-growing corals fast-growing corals can also sting and kill using long sweeper tentacles with powerful nematocysts © 2006 Thomson-Brooks Cole Species Interactions on Coral Reefs Competition among corals (continued) slower-growing corals are more tolerant of shade, and can grow at greater depths as a result… fast-growing, branching corals on many reefs dominate upper, shallower portions larger, slower-growing corals dominate deeper portions © 2006 Thomson-Brooks Cole Species Interactions on Coral Reefs Competition between corals and other reef organisms sponges, soft corals and algae can overgrow stony corals and smother them algae outcompete corals at shallow depths unless grazers control the algae growth © 2006 Thomson-Brooks Cole Species Interactions on Coral Reefs Effect of grazing grazing of larger, fleshier seaweeds permits competitively inferior filamentous forms or coralline algae to persist herbivory decreases with depth damselfish form territories where they exclude grazers and permit abundant algal growth provides habitat for small invertebrates overgrows corals; fast-growing, branching corals are most successful near damselfish © 2006 Thomson-Brooks Cole Coral Reef Ecology Coral reefs - marine habitats with greatest diversity/abundance of fishes Seems to defy competitive exclusion principle, which suggests that no 2 species can occupy the same niche 60-70% of reef fishes are general carnivores about 15% are coral algae grazers or omnivorous © 2006 Thomson-Brooks Cole Threats to Coral Reefs Effect of physical changes on the health of coral reefs hurricanes and typhoons topple and remove coral formations El Niño Southern Oscillation (ENSO) changes winds, ocean currents, temperatures, rainfall and atmospheric pressure over large areas of tropical and subtropical areas can cause massive storms © 2006 Thomson-Brooks Cole Threats to Coral Reefs Coral bleaching a phenomenon by which corals expel their symbiotic zooxanthellae most often associated with warming of the ocean water by or global warming if the stress is not too severe, corals may regain zooxanthellae and recover if the stress is prolonged, corals may fail to regain zooxanthellae and die © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Threats to Coral Reefs Human impact on coral reefs overfishing may occur human-sewage bacteria cause white pox nutrient-rich runoff (eutrophication) increases algal growth, which covers and smothers corals e.g. Kane’ohe Bay in Hawaii © 2006 Thomson-Brooks Cole Evolutionary Adaptations of Reef Dwellers Role of color in reef organisms color for concealment and protection countershading disruptive coloration camouflage (bright colors in reef environment) © 2006 Thomson-Brooks Cole © 2006 Thomson-Brooks Cole Evolutionary Adaptations of Reef Dwellers Role of color in reef organisms other types of camouflage body shape warning coloration other roles of color defending territories mating rituals © 2006 Thomson-Brooks Cole Evolutionary Adaptations of Reef Dwellers Symbiotic relationships on coral reefs cleaning symbioses cleaner wrasses, gobies, etc. feed on parasites of larger fishes cleaning organisms set up a cleaning station Other symbiotic relationships clownfishes and anemones conchfish and the queen conch gobies and snapping shrimp crustaceans and anemones © 2006 Thomson-Brooks Cole Coral Reefs http://tools.coralreef.org/content/ objects/view.acs?object_id=545 http://ourworld.compuserve.com/homepages/ mccarty_and_peters/coral/C-intro.htm Importance of Coral Reefs 0.2% of world’s oceans Habitat for 1/3 of marine fishes Habitat for tens of thousands of other animals The rainforests of the oceans Importance of Coral Reefs PROTECTION TO COASTLINES ECONOMIC RESOURCES BIODIVERSITY NATURAL BEAUTY Importance of Coral Reefs PROTECTION TO COASTLINES absorb energy of ocean waves reduce erosion of shoreline storm damage flooding Importance of Coral Reefs ECONOMIC RESOURCES Fisheries for food Fisheries for jobs Tourism Building materials Aquarium trade Importance of Coral Reefs BIODIVERSITY The rainforests of the sea Genetic diversity Pharmaceuticals Importance of Coral Reefs NATURAL BEAUTY http://sustainableseas.noaa.gov/missions/ florida2/background/coralspawning.html $375 billion in environmental goods and services Reefs at Risk 1998 (http://www.wri.org/powerpoints/reefswww/sld011.htm Caribbean reef values (annual net benefits in 2000) Fisheries: $310 million Dive tourism: $2.1 billion Shoreline protection: $0.7-2.2 billion Total: $4.1-4.6 billion REEFS WORLDWIDE ARE THREATENED • 11% of reefs have been lost • 16% of reefs severely damaged • ~60% of studied reefs threatened by human activities • No pristine reefs left CARIBBEAN REEFS DECLINING • 1970s: ~50% coral cover • Present: ~10% coral cover • =80% reduction in coral cover over last 30 years Gardner et al. 2003 Science 301: 958-960 Threats to coral and coral reefs: 1) Natural 2) Anthropogenic – of human origin Natural disturbances that affect corals and coral reefs? • Hurricanes • Tsunamis • Volcanoes • Earthquakes • Predators & competitors • Bleaching • Pathogens Hurricanes Physical damage •Smothering •Freshwater poisoning http://www.nhc.noaa.gov/ 1989hugo.html •Destruction of other ecosystems upon which coral reefs depend Tsunamis Physical damage •Erosion •Possible disruption of reproduction and recruitment Volcanoes Depends upon where volcano occurs •Heat •smothering and sedimentation http://volcano.und.nodak.edu/vwdocs/ current_volcs/montserrat/montserrat.html Earthquakes Little direct impact •Indirect impacts -triggers tsunamis -coastal landslides Predators crown of thorns starfish snails parrotfish butterflyfish http://www.aims.gov.au/pages/reflib/ cot-starfish/pages/cot-q07.html http://www.sanctuaries.nos.noaa.gov/pgallery/pgflower/living/fg_living.html Competitors algae http://catbert.er.usgs.gov/african_dust/algae.html Loss of zooxanthellae causes higher than usual ocean temperature sharp changes in salinity heavy UV light exposure http://ourworld.compuserve.com/homepages/ mccarty_and_peters/coral/Bleach.htm http://orbit-net.nesdis.noaa.gov/orad/coral_bleaching_index.html Pathogens Diseases on the rise new pathogens (8+) land pathogens (Aspergillus) occurring at all depths More susceptible when stressed http://ourworld.compuserve.com/ homepages/mccarty_and_peters/ coral/Bbd.htm Anthropogenic threats to coral reefs: •Overfishing •Development •Mining and dredging •Recreation Overfishing Ecological imbalance http://www.photolib.noaa.gov/r eef/reef2570.htm http://tools.coralreef.org/content/objects/view.acs?object_id=545 Overfishing Ecological imbalance http://catbert.er.usgs.gov/african_dust/events.html Overfishing • Destructive fishing practices http://oceanworld.tamu.edu/stud ents/coral/coral5.htm http://www.wri.org/indictrs/rrcyanid.htm Development Sediment smothering Freshwater input Pollutants & nutrients (sewage, pesticides, fertilizer, heavy metals, pathogens) Development http://www.wcmc.org.uk/marine/data/co ral_mangrove/coral.danger.html http://ourworld.compuserve.com/homepages/ mccarty_and_peters/coral/c-intro.htm Development http://www.sanctuaries.nos.noaa.gov/scied/science/habitat/influences.html Mining for construction materials and dredging Destruction of reef structure stirs up sediment Recreation Anchors, boats, flippers, hands, feet •Kill animal tissue •Skeleton breakage http://www.sanctuaries.nos.noaa.gov/scied/science/ habitat/influences.html Global climate change Reduced reef building Increase in frequency and intensity of hurricanes Increases in bleaching Increased in disease
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