Coral bleaching

Information about Coral bleaching

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Two images of the Great Barrier Reef showing that the warmest water (top picture) coincides with the coral reefs (lower picture), setting up conditions that can cause coral bleaching.


Coral bleaching refers to the loss of color of corals due to stress-induced expulsion of symbiotic unicellular algae. The corals that form the structure of the great reef ecosystems of tropical seas depend on a symbiotic relationship with photosynthesizing unicellular algae called zooxanthellae that live within their tissues. Zooxanthellae give coral its particular coloration, depending on the clade living within the coral. Under stress, corals may expel their zooxantheallae, which leads to a lighter or completely white appearance, hence the term "bleached".

Coral bleaching is a vivid sign of corals responding to stress, which can be induced by any of: Some of these factors are anthropogenic, while others occur naturally.

Once bleaching begins, corals tend to continue to bleach even if the stressor is removed. If the coral colony survives, it often requires weeks to months for the remaining symbiont population to reach a normal density. Following bleaching, corals may be recolonised by the same species of zooxanthellae, or by a different species. Different types of zooxanthellae respond differently to environmental conditions and may be more resistant to coral bleaching than other species. Some corals are known to host multiple clades of zooxanthellae within an individual coral. [3]. Ability to withstand stress and bleaching and ability to recover from a bleaching event varies greatly across coral species. Large massive corals, such as Porites lobata is able to withstand extreme temperature shocks, while fragile branching corals, such as Acropora spp. are far more susceptible to dying following a bleaching event. Recent research has also shown that corals consistently exposed to low levels of stress may in fact be more resistant to bleaching. Factors that protect against mass coral bleaching are bleaching resistance, coral tolerance, reef recovery. Due to the patchy nature of bleaching, local climatic conditions such as shade or a stream of cooler water can reduce the risk of bleaching. Also, the health and genetics of both the coral and its zooxanthellae can influence the risk of bleaching.[4]

Other reef creatures have symbiotic zooxanthellae, which they may also expel under stressful conditions. Bleaching stress is also exhibited by soft corals, giant Tridacna clams and some sponges.

The Great Barrier Reef along the northeast coast of Australia suffered two mass coral bleaching events in the summers of 1998 and 2002. While most reef areas recovered with relatively low levels of coral death, some locations suffered severe damage, with up to 90% of corals killed.

Other coral reef provinces have been permanently damaged by warm sea temperatures, most severely in the Indian Ocean. Up to 90% of coral cover has been lost in the Maldives, Sri Lanka, Kenya and Tanzania and in the Seychelles.

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Bioerosion (coral damage) such as this may be caused by coral bleaching.[5]

Pathogen infection

In 1996, Kushumaro, et al. [6] reported that the agent for the coral bleaching in the Red Sea was an infectious bacteria attacking the symbiotic algae. The agent has been later identified as Vibrio shiloi. The pathogen is infectious only during warm periods; therefore, global warming would increase the occurrence of conditions that promote the spread of infection.

During the summer of 2003, coral reefs in the Red Sea appeared to gain resistance to the pathogen, and further infection was not observed [7]. The main hypothesis for the emerged resistance is probiotic: inside the symbiotic communities of bacteria living with the corals. One species capable of lysing V. shiloi has gained prominence. This hypothetical bacteria has not yet been identified.

Notes and references

1. ^ REEF ‘AT RISK IN CLIMATE CHANGE’. Retrieved on 2007-07-12.
2. ^ The Starving Ocean: Mass Coral Bleaching
3. ^ The Future of Coral Reefs by Nancy Knowlton. Retrieved on 2007-03-02.
4. ^ (2006) A Reef Manager’s Guide to Coral Bleaching. Townsville, Australia: Great Barrier Reef Marine Park Authority,. 1 876945 40 0. 
5. ^ Ryan Holl (17 April 2003). papers/Bioerosion.htm Bioerosion: an essential, and often overlooked, aspect of reef ecology. Iowa State University. Retrieved on 2006-11-02.
6. ^ Kusushumaro et al. Bacterial infection and coral bleaching, Nature 380:396 (1996)
7. ^ Reshef et al, The coral probiotic hypothesis Env Microbiolgy, 8:2066 (2006)

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Corals are marine animals from the class Anthozoa and exist as small sea anemone-like polyps, typically in colonies of many identical individuals. The group includes the important reef builders that are found in tropical oceans, which secrete calcium carbonate to form a hard
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microorganism (also spelled as microrganism) or microbe is an organism that is microscopic (too small to be seen by the human eye). The study of microorganisms is called microbiology.
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phytoplankton — provide the food base for most marine food chains. In very high densities (so-called algal blooms) these algae may discolor the water and outcompete or poison other life forms.
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Corals are marine animals from the class Anthozoa and exist as small sea anemone-like polyps, typically in colonies of many identical individuals. The group includes the important reef builders that are found in tropical oceans, which secrete calcium carbonate to form a hard
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Coral reefs are aragonite structures produced by living organisms, found in shallow, tropical marine waters with little to no nutrients in the water. High nutrient levels such as that found in runoff from agricultural areas can harm the reef by encouraging the growth of algae.
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ecosystem is a natural unit consisting of all plants, animals and micro-organisms in an area functioning together with all the non-living physical factors of the environment.
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Symbiodinium

Zooxanthellae (IPA: /ˌzoʊoʊzænˈθɛli/) are golden-brown intracellular endosymbionts of various marine animals and protozoa, especially anthozoans.
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Global warming refers to the increase in the average temperature of the Earth's near-surface air and oceans in recent decades and its projected continuation.

The global average air temperature near the Earth's surface rose 0.74 ± 0.18 °C (1.33 ± 0.
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Zooplankton are the heterotrophic (or detritivorous) component of the plankton that drift in the water column of oceans, seas, and bodies of fresh water. The name is derived from the Greek terms, ζῴον
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Alcyonacea

Suborders

Alcyoniina
Calcaxonia
Holaxonia
Protoalcyonaria
Scleraxonia
Stolonifera

The Alcyonacea, or the soft corals are an order of corals which do not produce calcium carbonate skeletons.
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T. gigas

Binomial name
Tridacna gigas
Linnaeus, 1758

The giant clam (Tridacna gigas) or traditionally, pa’ua, is the largest living bivalve mollusc.
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Porifera
Grant in Todd, 1836

Classes
Calcarea
Hexactinellida
Demospongiae
The sponges or poriferans (from Latin "pore" and "to bear") are animals of the phylum Porifera. Porifera translates to "Pore-bearer".
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Reference 154
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Managing authorities: Great Barrier Reef Marine Park Authority, Queensland Parks and Wildlife Service, Queensland Fisheries
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