Overview
Brief Summary
Biology
zooxanthellate
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UNESCO-IOC Register of Marine Organisms
http://www.marinespecies.org/aphia.php?p=sourcedetails&id=1318
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Comprehensive Description
Biology: Skeleton
More info
| Author | Skeleton? | Mineral or Organic? | Mineral | Percent Magnesium |
|---|---|---|---|---|
| Veron, 2000 | YES | MINERAL | ARAGONITE | |
| Yabe and Sugiyama, 1941 | YES | MINERAL | ARAGONITE | |
| Cairns, Hoeksema, and van der Land, 1999 | YES | MINERAL | ARAGONITE |
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Distribution
Range Description
In the Indo-West Pacific, this species is found in the Red Sea, the southwest and central Indian Ocean, the central Indo-Pacific, southern Japan and the South China Sea, eastern Australia, the oceanic west Pacific, the central Pacific, the Hawaiian Islands and Johnston Atoll.
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Aldabra, Chagos, Indo-West Pacific, Madagascar, Mauritius, Mozambique, Reunion, Rodriguez, Seychelles
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UNESCO-IOC Register of Marine Organisms
http://www.marinespecies.org/aphia.php?p=sourcedetails&id=1318
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Sheppard, C.R.C. (1998). Corals of the Indian Ocean: a taxonomic and distribution database for coral reef ecologists
http://www.marinespecies.org/aphia.php?p=sourcedetails&id=6092
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Fauré, G. (1977). Annotated checklist of the corals in the Mascarene Archipelago, Indian Ocean. Atoll Research Bulletin 203: 1-26
http://www.marinespecies.org/aphia.php?p=sourcedetails&id=5899
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Sheppard, C.R.C. (1981). The Reef and Soft-substrate coral fauna of Chagos, Indian Ocean.
http://www.marinespecies.org/aphia.php?p=sourcedetails&id=6031
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Sheppard, C.R.C. (1987). [Pichon]
http://www.marinespecies.org/aphia.php?p=sourcedetails&id=5879
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Sheppard, C.R.C. (1987). [Best; Boshof]
http://www.marinespecies.org/aphia.php?p=sourcedetails&id=5878
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Ecology
Habitat
Habitat and Ecology
Habitat and Ecology
Systems
This species is found on reef slopes and on vertical walls. The maximum size is 20 cm. This species is found from 10-20 m.
Systems
- Marine
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Depth range based on 44 specimens in 1 taxon.
Water temperature and chemistry ranges based on 34 samples.
Environmental ranges
Depth range (m): 0 - 43
Temperature range (°C): 24.763 - 28.810
Nitrate (umol/L): 0.032 - 0.526
Salinity (PPS): 34.254 - 35.222
Oxygen (ml/l): 4.362 - 4.996
Phosphate (umol/l): 0.083 - 0.265
Silicate (umol/l): 1.178 - 6.608
Graphical representation
Depth range (m): 0 - 43
Temperature range (°C): 24.763 - 28.810
Nitrate (umol/L): 0.032 - 0.526
Salinity (PPS): 34.254 - 35.222
Oxygen (ml/l): 4.362 - 4.996
Phosphate (umol/l): 0.083 - 0.265
Silicate (umol/l): 1.178 - 6.608
Note: this information has not been validated. Check this *note*. Your feedback is most welcome.
Water temperature and chemistry ranges based on 34 samples.
Environmental ranges
Depth range (m): 0 - 43
Temperature range (°C): 24.763 - 28.810
Nitrate (umol/L): 0.032 - 0.526
Salinity (PPS): 34.254 - 35.222
Oxygen (ml/l): 4.362 - 4.996
Phosphate (umol/l): 0.083 - 0.265
Silicate (umol/l): 1.178 - 6.608
Graphical representation
Depth range (m): 0 - 43
Temperature range (°C): 24.763 - 28.810
Nitrate (umol/L): 0.032 - 0.526
Salinity (PPS): 34.254 - 35.222
Oxygen (ml/l): 4.362 - 4.996
Phosphate (umol/l): 0.083 - 0.265
Silicate (umol/l): 1.178 - 6.608
Note: this information has not been validated. Check this *note*. Your feedback is most welcome.
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Conservation
Conservation Status
IUCN Red List Assessment
Red List Category
VU
Vulnerable
Red List Criteria
A4ce
Version
3.1
Year Assessed
2008
Assessor/s
Hoeksema, B., Rogers, A. & Quibilan, M.
Reviewer/s
Livingstone, S., Polidoro, B. & Smith, J. (Global Marine Species Assessment)
Contributor/s
Justification
This species is widespread and uncommon throughout its range. However, it is susceptible to bleaching, disease, crown-of-thorns starfish predation, and extensive reduction of coral reef habitat due to a combination of threats. Specific population trends are unknown but population reduction can be inferred from declines in habitat quality based on the combined estimates of both destroyed reefs and reefs at the critical stage of degradation within its range (Wilkinson 2004). Its threat susceptibility increases the likelihood of being lost within one generation in the future from reefs at a critical stage. Therefore, the estimated habitat degradation and loss of 35% over three generation lengths (30 years) is the best inference of population reduction and meets the threshold for Vulnerable under Criterion A4c. It will be important to reassess this species in 10 years time because of predicted threats from climate change and ocean acidification.
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Trends
Population
Population
Population Trend
This is an uncommon species.
There is no species specific population information available for this species. However, there is evidence that overall coral reef habitat has declined, and this is used as a proxy for population decline for this species. This species is particularly susceptible to bleaching, disease, and other threats and therefore population decline is based on both the percentage of destroyed reefs and critical reefs that are likely to be destroyed within 20 years (Wilkinson 2004). We assume that most, if not all, mature individuals will be removed from a destroyed reef and that on average, the number of individuals on reefs are equal across its range and proportional to the percentage destroyed reefs. Reef losses throughout the species' range have been estimated over three generations, two in the past and one projected into the future.
The age of first maturity of most reef building corals is typically three to eight years (Wallace 1999) and therefore we assume that average age of mature individuals is greater than eight years. Furthermore, based on average sizes and growth rates, we assume that average generation length is 10 years, unless otherwise stated. Total longevity is not known, but likely to be more than ten years. Therefore any population decline rates for the Red List assessment are measured over at least 30 years. Follow the link below for further details on population decline and generation length estimates.
There is no species specific population information available for this species. However, there is evidence that overall coral reef habitat has declined, and this is used as a proxy for population decline for this species. This species is particularly susceptible to bleaching, disease, and other threats and therefore population decline is based on both the percentage of destroyed reefs and critical reefs that are likely to be destroyed within 20 years (Wilkinson 2004). We assume that most, if not all, mature individuals will be removed from a destroyed reef and that on average, the number of individuals on reefs are equal across its range and proportional to the percentage destroyed reefs. Reef losses throughout the species' range have been estimated over three generations, two in the past and one projected into the future.
The age of first maturity of most reef building corals is typically three to eight years (Wallace 1999) and therefore we assume that average age of mature individuals is greater than eight years. Furthermore, based on average sizes and growth rates, we assume that average generation length is 10 years, unless otherwise stated. Total longevity is not known, but likely to be more than ten years. Therefore any population decline rates for the Red List assessment are measured over at least 30 years. Follow the link below for further details on population decline and generation length estimates.
Population Trend
Unknown
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Threats
Major Threats
In general, the major threat to corals is global climate change, in particular, temperature extremes leading to bleaching and increased susceptibility to disease, increased severity of ENSO events and storms, and ocean acidification.
Coral disease has emerged as a serious threat to coral reefs worldwide and a major cause of reef deterioration (Weil et al. 2006). The numbers of diseases and coral species affected, as well as the distribution of diseases have all increased dramatically within the last decade (Porter et al. 2001, Green and Bruckner 2000, Sutherland et al. 2004, Weil 2004). Coral disease epizootics have resulted in significant losses of coral cover and were implicated in the dramatic decline of acroporids in the Florida Keys (Aronson and Precht 2001, Porter et al. 2001, Patterson et al. 2002). In the Indo-Pacific, disease is also on the rise with disease outbreaks recently reported from the Great Barrier Reef (Willis et al. 2004), Marshall Islands (Jacobson 2006) and the northwestern Hawaiian Islands (Aeby 2006). Increased coral disease levels on the GBR were correlated with increased ocean temperatures (Willis et al. 2007) supporting the prediction that disease levels will be increasing with higher sea surface temperatures. Escalating anthropogenic stressors combined with the threats associated with global climate change of increases in coral disease, frequency and duration of coral bleaching and ocean acidification place coral reefs in the Indo-Pacific at high risk of collapse.
Localized threats to corals include fisheries, human development (industry, settlement, tourism, and transportation), changes in native species dynamics (competitors, predators, pathogens and parasites), invasive species (competitors, predators, pathogens and parasites), dynamite fishing, chemical fishing, pollution from agriculture and industry, domestic pollution, sedimentation, and human recreation and tourism activities.
The severity of these combined threats to the global population of each individual species is not known.
Coral disease has emerged as a serious threat to coral reefs worldwide and a major cause of reef deterioration (Weil et al. 2006). The numbers of diseases and coral species affected, as well as the distribution of diseases have all increased dramatically within the last decade (Porter et al. 2001, Green and Bruckner 2000, Sutherland et al. 2004, Weil 2004). Coral disease epizootics have resulted in significant losses of coral cover and were implicated in the dramatic decline of acroporids in the Florida Keys (Aronson and Precht 2001, Porter et al. 2001, Patterson et al. 2002). In the Indo-Pacific, disease is also on the rise with disease outbreaks recently reported from the Great Barrier Reef (Willis et al. 2004), Marshall Islands (Jacobson 2006) and the northwestern Hawaiian Islands (Aeby 2006). Increased coral disease levels on the GBR were correlated with increased ocean temperatures (Willis et al. 2007) supporting the prediction that disease levels will be increasing with higher sea surface temperatures. Escalating anthropogenic stressors combined with the threats associated with global climate change of increases in coral disease, frequency and duration of coral bleaching and ocean acidification place coral reefs in the Indo-Pacific at high risk of collapse.
Localized threats to corals include fisheries, human development (industry, settlement, tourism, and transportation), changes in native species dynamics (competitors, predators, pathogens and parasites), invasive species (competitors, predators, pathogens and parasites), dynamite fishing, chemical fishing, pollution from agriculture and industry, domestic pollution, sedimentation, and human recreation and tourism activities.
The severity of these combined threats to the global population of each individual species is not known.
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Management
Conservation Actions
Conservation Actions
All corals are listed on CITES Appendix II. Parts of the species’ range fall within Marine Protected Areas.
Recommended measures for conserving this species include research in taxonomy, population, abundance and trends, ecology and habitat status, threats and resilience to threats, restoration action; identification, establishment and management of new protected areas; expansion of protected areas; recovery management; and disease, pathogen and parasite management. Artificial propagation and techniques such as cryo-preservation of gametes may become important for conserving coral biodiversity.
Recommended measures for conserving this species include research in taxonomy, population, abundance and trends, ecology and habitat status, threats and resilience to threats, restoration action; identification, establishment and management of new protected areas; expansion of protected areas; recovery management; and disease, pathogen and parasite management. Artificial propagation and techniques such as cryo-preservation of gametes may become important for conserving coral biodiversity.
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