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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Biology
Like other reef-building corals, the polyps of Porites corals have microscopic algae (zooxanthellae) living within their tissues. Through photosynthesis, these symbiotic algae produce energy-rich molecules that the coral polyps can use as nutrition. In return, the coral provides the zooxanthellae with protection and access to sunlight (3). Porites colonies also commonly house a wide variety of other fauna (3). The majority of corals are hermaphrodite, and thus colonies possess both male and female reproductive organs. However, Porites corals have separate male and female colonies. With a few exceptions, fertilization is internal and therefore depends on free-swimming sperm from male colonies reaching the polyps of female colonies. The fertilised eggs then develop into larvae within the female polyp's body cavity (2). When released, the larvae settle quickly close to the parent colony. Whilst this means that, unlike spawning corals, the coral is not easily dispersed, brooding corals have the advantage of their young settling in an environment that has already proved suitable for successful reproduction (3). Most of the spherical and hemispherical Porites species are tolerant of sedimentary environments, partly because they protect themselves with a thick film of mucous (3).
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Description
Porites corals form some of the largest of all coral colonies, with some reaching an incredible eight metres in height (2). The growth rate of Porites coral is very slow, perhaps only nine millimetres a year, therefore these giant colonies may be up to 1,000 years old, putting them among the oldest life forms on earth (2). Coral colonies are composed of many individual coral polyps, which are basically anemone-like animals that secrete a skeleton. The many polyps of a colony are joined together at the base of their skeletons (3). The colonies of Porites corals may form flat, branching, spherical or hemispherical structures; some hemispherical colonies may be over five meters across (3). The coral polyps possess tentacles which, in most species, are extended only at night, when they give the coral a furry appearance (2).
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Comprehensive Description
Biology: Skeleton
More info
| Author | Skeleton? | Mineral or Organic? | Mineral | Percent Magnesium |
|---|---|---|---|---|
| Veron and Pichon, 1982 | YES | MINERAL | ARAGONITE |
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Distribution
Range Description
This species has been recorded from the Red Sea, the southwest and northern Indian Ocean, the central Indo-Pacific, west, north and east Australia, South-east Asia, southern Japan and the South China Sea, the oceanic West Pacific, the central and eastern Pacific, the Hawaiian Islands and Johnston Atoll.
It also occurs in the Eastern Tropical Pacific region, and has been reported from Sámara, Costa Rica (Cortés and Murillo 1985, Cortés and Guzmán 1998, Cortés and Jiménez 2003). However, when P. rus was discovered at Sámara, the colonies (i.e., approximately 102 according to Glynn 1997) were bleached and since then P. rus has not been recorded from Sámara nor anywhere else in the Eastern Tropical Pacific region (Glynn 1997, Cortés and Guzmán 1998, Glynn and Ault 2000). Glynn (1997) and Glynn and Ault (2000) reported this species as Regionally Extinct in the Eastern Tropical Pacific.
It also occurs in the Eastern Tropical Pacific region, and has been reported from Sámara, Costa Rica (Cortés and Murillo 1985, Cortés and Guzmán 1998, Cortés and Jiménez 2003). However, when P. rus was discovered at Sámara, the colonies (i.e., approximately 102 according to Glynn 1997) were bleached and since then P. rus has not been recorded from Sámara nor anywhere else in the Eastern Tropical Pacific region (Glynn 1997, Cortés and Guzmán 1998, Glynn and Ault 2000). Glynn (1997) and Glynn and Ault (2000) reported this species as Regionally Extinct in the Eastern Tropical Pacific.
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Aldabra, Chagos, East Africa, Indo-Pacific, Madagascar, Mauritius, Red Sea, 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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Physical Description
Diagnostic Description
Description
Colonies may reach several metres across. They consist of mixtures of small plates and twisted projections, some projections developing into short, stout branches. The surface of the coral is covered with ridges which run between rows of calices. Calices themselves are minute (less than 1 mm diameter). Colours are usually basically brown or pale brown, but yellow colonies are also common, with strong pink colours also sometimes seen, some with blue edges to branches are plates (Sheppard, 1998). Colonies are laminar or contorted anastomosing branches and columns. Corallites are very small. They are separated into groups by ridges which characteristically converge towards each other forming flame-shaped patterns. Colour: pale cream or yellow, or dark bluish-brown, often with pale branch tips. Abundance: usually uncommon but occurs in a wide range of habitats (Veron, 1986). Distinguished by its extremely small calices (<0.6 mm). Open water colonies encrusting to massive, usually with a wrinkled surface; those in more hidden locations with a smooth surface. Colour: brown, pale grey or bright yellowish-green. Habitat: shallow sheltered reefs (Richmond, 1997).
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Veron, J.E.N. (1986). Corals of Australia and the Indo-Pacific. Angus & Robertson Publishers, London.
http://www.marinespecies.org/aphia.php?p=sourcedetails&id=5874
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Type Information
Holotype for Porites (Synaraea) hawaiiensis Vaughan, 1907
Catalog Number: USNM 21624
Collection: Smithsonian Institution, National Museum of Natural History, Department of Invertebrate Zoology
Preparation: Dry
Collector(s): W. Brigham
Locality: Oahu Island, Kalihi Harbor, Hawaii, United States, North Pacific Ocean
Catalog Number: USNM 21624
Collection: Smithsonian Institution, National Museum of Natural History, Department of Invertebrate Zoology
Preparation: Dry
Collector(s): W. Brigham
Locality: Oahu Island, Kalihi Harbor, Hawaii, United States, North Pacific Ocean
- Holotype: Vaughan. 1907. Bull. U.S. Nat. Mus. 59: 216-217, pl.91, fig.2.
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Ecology
Habitat
Habitat and Ecology
Habitat and Ecology
Systems
This species is found in shallow reef environments. It is a common coral in the Indo-Pacific, which is especially successful in shallow reef areas. Branched colonies often form large tracts along the reef front, while massive and encrusting species thrive at more exposed sites. (Wood 1983). P. rus is commonly found from 1 to 11 m, rarely from 12 to 20 m, in the South China Sea and Gulf of Siam (Titlyanov and Titlyanova 2002).
At Sámara, Costa Rica, P. rus was found on exposed rocky outcrops (Cortés pers. comm.).
At Sámara, Costa Rica, P. rus was found on exposed rocky outcrops (Cortés pers. comm.).
Systems
- Marine
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Depth range based on 1158 specimens in 1 taxon.
Water temperature and chemistry ranges based on 1093 samples.
Environmental ranges
Depth range (m): 0 - 80.5
Temperature range (°C): 25.235 - 28.981
Nitrate (umol/L): 0.015 - 1.204
Salinity (PPS): 33.068 - 35.637
Oxygen (ml/l): 4.495 - 4.780
Phosphate (umol/l): 0.067 - 0.351
Silicate (umol/l): 0.900 - 6.846
Graphical representation
Depth range (m): 0 - 80.5
Temperature range (°C): 25.235 - 28.981
Nitrate (umol/L): 0.015 - 1.204
Salinity (PPS): 33.068 - 35.637
Oxygen (ml/l): 4.495 - 4.780
Phosphate (umol/l): 0.067 - 0.351
Silicate (umol/l): 0.900 - 6.846
Note: this information has not been validated. Check this *note*. Your feedback is most welcome.
Water temperature and chemistry ranges based on 1093 samples.
Environmental ranges
Depth range (m): 0 - 80.5
Temperature range (°C): 25.235 - 28.981
Nitrate (umol/L): 0.015 - 1.204
Salinity (PPS): 33.068 - 35.637
Oxygen (ml/l): 4.495 - 4.780
Phosphate (umol/l): 0.067 - 0.351
Silicate (umol/l): 0.900 - 6.846
Graphical representation
Depth range (m): 0 - 80.5
Temperature range (°C): 25.235 - 28.981
Nitrate (umol/L): 0.015 - 1.204
Salinity (PPS): 33.068 - 35.637
Oxygen (ml/l): 4.495 - 4.780
Phosphate (umol/l): 0.067 - 0.351
Silicate (umol/l): 0.900 - 6.846
Note: this information has not been validated. Check this *note*. Your feedback is most welcome.
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Depth range based on 7 specimens in 1 taxon.
Water temperature and chemistry ranges based on 7 samples.
Environmental ranges
Depth range (m): 3 - 30
Temperature range (°C): 25.146 - 28.049
Nitrate (umol/L): 0.009 - 0.089
Salinity (PPS): 34.340 - 34.939
Oxygen (ml/l): 4.597 - 4.813
Phosphate (umol/l): 0.113 - 0.130
Silicate (umol/l): 1.279 - 1.484
Graphical representation
Depth range (m): 3 - 30
Temperature range (°C): 25.146 - 28.049
Nitrate (umol/L): 0.009 - 0.089
Salinity (PPS): 34.340 - 34.939
Oxygen (ml/l): 4.597 - 4.813
Phosphate (umol/l): 0.113 - 0.130
Silicate (umol/l): 1.279 - 1.484
Note: this information has not been validated. Check this *note*. Your feedback is most welcome.
Water temperature and chemistry ranges based on 7 samples.
Environmental ranges
Depth range (m): 3 - 30
Temperature range (°C): 25.146 - 28.049
Nitrate (umol/L): 0.009 - 0.089
Salinity (PPS): 34.340 - 34.939
Oxygen (ml/l): 4.597 - 4.813
Phosphate (umol/l): 0.113 - 0.130
Silicate (umol/l): 1.279 - 1.484
Graphical representation
Depth range (m): 3 - 30
Temperature range (°C): 25.146 - 28.049
Nitrate (umol/L): 0.009 - 0.089
Salinity (PPS): 34.340 - 34.939
Oxygen (ml/l): 4.597 - 4.813
Phosphate (umol/l): 0.113 - 0.130
Silicate (umol/l): 1.279 - 1.484
Note: this information has not been validated. Check this *note*. Your feedback is most welcome.
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Porites corals can be found in a wide range of coral reef environments. Many Porites species are very common in shallow water, and most species are tolerant of areas where sediment accumulates (3).
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Molecular Biology and Genetics
Molecular Biology
Barcode data: Porites rus
The following is a representative barcode sequence, the centroid of all available sequences for this species.

There are 4 barcode sequences available from BOLD and GenBank. Below is a sequence of the barcode region Cytochrome oxidase subunit 1 (COI or COX1) from a member of the species. See the BOLD taxonomy browser for more complete information about this specimen and other sequences.
Download FASTA File
There are 4 barcode sequences available from BOLD and GenBank. Below is a sequence of the barcode region Cytochrome oxidase subunit 1 (COI or COX1) from a member of the species. See the BOLD taxonomy browser for more complete information about this specimen and other sequences.
TTTGGGATTGGGGCAGGTATGCTCGGTACAGCTTTC---AGTATGTTAATAAGATTAGAGCTCTCGGCTCCGGGGGCTATGTTAGGAGAC---GATCATCTTTATAATGTAATTGTTACAGCACACGCTTTTATTATGATCTTTTTTTTGGTTATGCCAGTGATGATAGGGGGATTTGGGAATTGGTTGGTTCCATTA---TATATTGGGGCACCTGATATGGCTTTCCCACGGCTTAATAACATTAGTTTTTGGCTGTTGCCCCCTGCTTTAATATTGTTATTAGGTTCTGCTTTTGTTGAACAAGGGGCGGGTACCGGATGAACGGTTTATCCTCCTCTATCTAGCATTCAGGCCCATTCTGGTGGGGCGGTGGATATG---GCTATTTTTAGTCTCCATTTAGCTGGGGTGTCCTCGATTTTGGGTGCAATGAATTTTATAACAACTATATTTAATATGAGGGCCCCTGGGCTAACGTTGAATAGAATGCCCTTATTTGTGTGGTCTATCTTGATCACTGCTTTTTTATTATTATTGTCTTTGCCCGTATTAGCGGGG---GCCATAACCATGCTTTTAACGGACAGAAACTTTAATACTACTTTCTTTGATCCTGCAGGGGGAGGAGATCCGATTTTATTTCAA
-- end --
-- end --
Download FASTA File
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Statistics of barcoding coverage: Porites rus
Barcode of Life Data Systems (BOLDS) Stats
Public Records: 4
Specimens with Barcodes: 4
Species With Barcodes: 1
Public Records: 4
Specimens with Barcodes: 4
Species With Barcodes: 1
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Genomic DNA is available from 1 specimen with morphological vouchers housed at Queensland Museum
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Genomic DNA is available from 20 specimens with morphological vouchers housed at National Institute of Water and Atmospheric Research, Wellington
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Conservation
Conservation Status
IUCN Red List Assessment
Red List Category
LC
Least Concern
Red List Criteria
Version
3.1
Year Assessed
2008
Assessor/s
Sheppard, A., Fenner, D., Edwards, A., Abrar, M. & Ochavillo, D.
Reviewer/s
Livingstone, S., Polidoro, B. & Smith, J. (Global Marine Species Assessment)
Contributor/s
Justification
The most important known threat for this species is extensive reduction of coral reef habitat due to a combination of threats. Specific population trends are unknown but population reduction can be inferred from estimated habitat loss (Wilkinson 2004). Although this species has likely been lost from the Eastern Tropical Pacific portion of its range, in the Indo-Pacific region, this species is very widespread, and common within its range, has a low susceptibility to bleaching, and therefore is likely to be more resilient to habitat loss and reef degradation because of an assumed large effective population size that is highly connected and/or stable with enhanced genetic variability. Therefore, the estimated habitat loss of 20% from reefs already destroyed within its range is the best inference of population reduction since it may survive in coral reefs already at the critical stage of degradation (Wilkinson 2004). This inference of population reduction over three generation lengths (30 years) does not meet the threshold of a threat category and this species is Least Concern. However, because of predicted threats from climate change and ocean acidification it will be important to reassess this species in 10 years or sooner, particularly if the species is also observed to disappear from reefs currently at the critical stage of reef degradation.
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Trends
Population
Population
Population Trend
This species is common in the Indo-Pacific portion of its range, and may be a dominant species in a wide range of habitats. In a study of 11 areas in the Philippines, three in Malaysia, two in Indonesia, and one each in Madagascar, Rodrigues, Andamans, Papua New Guinea, Australia, New Caledonia, Fiji, American Samoa and Hawaii, the species was present at 79% of the sites surveyed (Fenner pers. comm.).
In the Eastern Tropical Pacific region, P. rus is possibly extinct.
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 more resilient to some of the threats faced by corals and therefore population decline is estimated using the percentage of destroyed reefs only (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 of 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.
In the Eastern Tropical Pacific region, P. rus is possibly extinct.
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 more resilient to some of the threats faced by corals and therefore population decline is estimated using the percentage of destroyed reefs only (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 of 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
Porites species are heavily collected for the aquarium trade. In Indonesia, the catch quota for this genus is 55,500 per year.
The genus is not particularly susceptible to bleaching, but is more prone to disease than many other corals. Coral disease has emerged as a serious threat to coral reefs worldwide and is 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 Great Barrier Reef 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.
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. In addition to global climate change, corals are also threatened by a number of localized threats. 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.
The genus is not particularly susceptible to bleaching, but is more prone to disease than many other corals. Coral disease has emerged as a serious threat to coral reefs worldwide and is 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 Great Barrier Reef 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.
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. In addition to global climate change, corals are also threatened by a number of localized threats. 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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Porites corals face the many threats that are impacting coral reefs globally. It is estimated that 20 percent of the world's coral reefs have already been effectively destroyed and show no immediate prospects of recovery, and 24 percent of the world's reefs are under imminent risk of collapse due to human pressures. These human impacts include poor land management practices that are releasing more sediment, nutrients and pollutants into the oceans and stressing the fragile reef ecosystem. Over fishing has 'knock-on' effects that results in the increase of macro-algae that can out-compete and smother corals, and fishing using destructive methods physically devastates the reef. A further potential threat is the increase of coral bleaching events, as a result of global climate change (4). The predatory starfish, Acanthaster planci, or 'crown-of-thorns starfish', feeds on a wide range of coral species. For little understood reasons, outbreaks of this starfish occur at regular intervals, and large numbers of starfish can have devastating effects on the reef. They can eat so much that they can kill most of the living coral in a region, which may take the reef up to fifteen years to fully recover (5). Due to the exceptionally slow growth rate of Porites corals, these species may not be able to fully recover in the time before the next starfish outbreak, and thus may be sent into a period of prolonged decline (6). An additional potential threat arises from collection for the coral trade. Porites is one of four genera that constitute the majority of the dead coral trade, for ornaments and jewellery. Live Porites are also collected at a lower level for the aquarium industry, and has previously been traded for biomedical purposes. This trade, which probably supplied a specialised market for the use of coral in bone grafts, peaked in 1992 but has since declined to extremely low levels (7).
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Management
Conservation Actions
Conservation Actions
All corals are listed on CITES Appendix II. Parts of this species distribution fall within several Marine Protected Areas within its range.
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.
Having timely access to national-level trade data for CITES analysis reports would be valuable for monitoring trends this species. The species is targeted by collectors for the aquarium trade and fisheries management is required for the species, e.g., Marine Protected Areas, quotas, size limits, etc. Consideration of the suitability of species for aquaria should also be included as part of fisheries management, and population surveys should be carried out to monitor the effects of harvesting.
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.
Having timely access to national-level trade data for CITES analysis reports would be valuable for monitoring trends this species. The species is targeted by collectors for the aquarium trade and fisheries management is required for the species, e.g., Marine Protected Areas, quotas, size limits, etc. Consideration of the suitability of species for aquaria should also be included as part of fisheries management, and population surveys should be carried out to monitor the effects of harvesting.
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Conservation
Porites corals are listed on Appendix II of the Convention on International Trade in Endangered Species (CITES), which means that trade in this species should be carefully regulated (1). Indonesia and Fiji have export quotas for Porites corals (1). Porites corals will form part of the marine community in many marine protected areas (MPAs), which offer coral reefs a degree of protection, and there are many calls from non-governmental organisations for larger MPAs to ensure the persistence of these unique and fascinating ecosystems (4).
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