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Reef PDF. In Email

By: Rebecca Evered, Curriculum & Content Director, Greenspeak International

ReefA reef is a rock, sandbar or other feature that lies just below the water’s surface. Most reefs form by geological processes, but coral makes the best-known reefs Biotic (living) reefs take a second name due to their position in relation to the land. They may be called barrier, fringing or atoll reefs. Barrier reefs form a hard wall around an island protecting the shore from the ocean, while a fringing reef is a reef that is attached to an island. An atoll is a ring reef with no land close by. The reef front (ocean side) is a rougher area, with a lot of wave action whereas the lagoon inside will be calmer.

The Great Barrier Reef is the largest coral reef in the world, made up of over 2,900 individual reefs and 900 islands. It is over 3,000 km (1,600 miles) long. The reef is located in the Coral Sea off the coast of Queensland in northeast Australia. It is so big that it can be seen from space, and is listed as one of the seven natural wonders of the world.

The reef has a very high level of biodiversity and is home to many endemic (not found anywhere else) organisms. Over 30 species of marine mammal have been recorded, (including dolphins, whales and dugongs) as well as 6 species of turtle, 215 species of marine bird, 17 species of seas snake, innumerable fish, mollusks (shelled invertebrates) and even some salt-water crocodiles near the islands.

Four hundred species of corals, both hard and soft are found on the reef. The majority of these breed in mass spawning events that are controlled by warmer sea temperatures of spring and summer, the moon cycle and day lengths. Reefs in the inner Great Barrier Reef spawn during the week after the full moon in October, but the outer reefs spawn in November and December.

A large part of the reef is protected by the Great Barrier Reef Marine Park, which helps to limit human impacts, such as over-fishing and tourism. Other environmental pressures to the reef include water quality from chemicals used on the land (such as fertilizers), climate change accompanied by mass coral bleaching from rising sea temperatures, and outbreaks of the introduced crown-of-thorns starfish.

References
Belfield, Sarah (2002). "Great Barrier Reef: no buried treasure" Geoscience Australia (Australian Government). http://www.ga.gov.au/ Retrieved on 14-7-2009
Bowen, James; Bowen, Margarita (2002). The Great Barrier Reef : history, science, heritage. Cambridge: Cambridge University Press
Department of the Environment and Heritage. "Review of the Great Barrier Reef Marine Park Act 1975" http://www.deh.gov.au/coasts/publications/gbr-marine-park-act.html. Retrieved on 2 November 2006.
Great Barrier Reef Marine Park Authority (2004). "Environmental Status: Marine Mammals" The State of the Great Barrier Reef Report - latest updates. http://www.gbrmpa.gov.au/corp_site/info_services/publications/sotr/latest_updates/marine_mammals. Retrieved on 13-6-2009
Hopley, David; Smithers, Scott G.; Parnell, Kevin E. (2007). The geomorphology of the Great Barrier Reef : development, diversity, and change. Cambridge : Cambridge University Press.
Mather, P.; Bennett, I., ed (1993). A Coral Reef Handbook: A Guide to the Geology, Flora and Fauna of the Great Barrier Reef (3rd ed.). Chipping North: Surrey Beatty & Sons Pty Ltd
Shears N.T. (2007) Biogeography, community structure and biological habitat types of subtidal reefs on the South Island West Coast, New Zealand. Science for Conservation 281. p 53. Department of Conservation, New Zealand.
UNEP World Conservation Monitoring Centre (1980). "Protected Areas and World Heritage - Great Barrier Reef World Heritage Area" Department of the Environment and Heritage http://www.unep-wcmc.org/protected_areas/data/wh/gbrmp.html. Retrieved on 14-7-2009
Image from http://planetsave.com/files/2008/02/great-barrier-reef.jpg
 

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