Porites lutea is a species of stony coral in the family Poritidae. It is found growing in very shallow water on reefs in the Indo-Pacific region. It sometimes forms "microatolls" in the intertidal zone and these massive structures have been used to study trends in sea levels and sea water temperature.
| Porites lutea | |
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| Porites lutea off Réunion | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Cnidaria |
| Class: | Hexacorallia |
| Order: | Scleractinia |
| Family: | Poritidae |
| Genus: | Porites |
| Species: | P. lutea
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| Binomial name | |
| Porites lutea | |
| Synonyms[2] | |
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Description
editPorites lutea forms massive, smooth, hemispherical mounds or helmet-shaped colonies up to 4 m (13 ft) across. The corallites have thin walls and are closely packed, some 1 to 1.5 mm (0.04 to 0.06 in) in diameter. In contrast to Porites lobata, the corallites are well-filled with skeletal elements, including five tall pali near the centre. The colour of this coral is usually cream or yellow, but other bright colours sometimes occur in shallow-water habitats.[3]
Distribution and habitat
editPorites lutea is native to the tropical Indo-Pacific region. Its range extends from Madagascar and the east coast of Africa to Malaysia, Indonesia, the Philippines, Japan and northern and eastern Australia. It occurs on back reef margins, in lagoons and on fringing reefs. It is a common species, often occurring with Porites australiensis and Porites lobata.[3]
Ecology
editThis coral can form "microatolls" in the intertidal zone; these are disc-shaped mounds with dead coral material at the top and living material round the perimeter which continues to grow sideways.[4] Sometimes these structures remain as fossil microatolls in which no living polyps survive but the colony morphology is retained.[4] Fossil microatolls of Porites lutea, combined with precise dating of individual annual growth rings using the uranium–thorium dating method, allows these structures to be used to determine past relative changes in sea-level.[5] Their use for this purpose on reefs in the South China Sea has shown that during the period 7000–6550 years before 2000, the sea level was about 170 to 220 centimetres (67 to 87 in) higher than now, with four or more cycles of fluctuations.[5]
In Yemen, the non-native, invasive, encrusting red sponge Clathria aceratoobtusa grows over the surface of the coral, at the rate of about 1 cm (0.4 in) per month, smothering and killing it. A thin white line of dead tissue separates the healthy coral tissues from the advancing sponge.[6]
Sometimes fragments of Porites lutea become detached from colonies. These may remain alive and end up further down the reef slope, or moved to a new location by currents or waves; in this way new colonies or even new reefs may form in locations unsuitable for larval settlement.[7]
Research
editThe growth rate of corals is influenced by environmental conditions; massive corals lay down a band of calcium carbonate each year, and the thickness of the band indicates the rate of growth. Researchers in Indonesia have studied the growth rate of Porites lutea and correlated it with the El Niño phenomenon. Growth rates were higher on windward slopes with greater wave action, and lower on lee slopes with less water movement. Rates were at their highest in 1992, when the sea temperature was about 28 °C (82 °F), and at their lowest in 1998 when it was 29.6 °C (85.3 °F). The correlation between water temperature and growth rate was complex, but in general growth rates of the coral were lower when the coral was stressed by higher water temperatures.[8]
Exposure of Porites lutea to increased concentration of iron causes bleaching through loss of symbiotic zooxanthellae; however the effect is less marked in corals previously exposed to raised levels of iron, suggesting the development of tolerance to the metal.[9]
References
edit
- ^ Sheppard, A.; Fenner, D.; Edwards, A.; Abrar, M.; Ochavillo, D. (2014). "Porites lutea". IUCN Red List of Threatened Species. 2014: e.T133082A54191180. doi:10.2305/IUCN.UK.2014-1.RLTS.T133082A54191180.en. Retrieved 19 November 2021.
- ^ a b Hoeksema, Bert (2020). "Porites lutea Milne Edwards & Haime, 1851". WoRMS. World Register of Marine Species. Retrieved 26 September 2020.
- ^ a b "Porites lutea". Corals of the World. Retrieved 26 September 2020.
- ^ a b Smithers, Scott (2011). "Microatoll". Microatolls. Encyclopedia of Earth Sciences Series. Springer. pp. 691–696. doi:10.1007/978-90-481-2639-2_111. ISBN 978-90-481-2638-5. Retrieved 27 September 2020.
{{cite book}}:|work=ignored (help) - ^ a b Ke-Fu Yu; Jian-Xin Zhao; Terry Done; Te-Gu Chen (2009). "Microatoll record for large century-scale sea-level fluctuations in the mid-Holocene". Quaternary Research. 71 (3): 354–360. Bibcode:2009QuRes..71..354Y. doi:10.1016/j.yqres.2009.02.003. S2CID 129728718.
- ^ Ashok, A.M.; Calcinai, B.; Edward, J.K.P. (2020). "The coral-killing red sponge Clathria (Microciona) aceratoobtusa (Porifera: Demosponigiae) invades various coral communities of Gulf of Mannar Marine National Park, southeast India". The European Zoological Journal. 87 (1): 1–11. doi:10.1080/24750263.2019.1708486.
- ^ Highsmith, Raymond C. (1980). "Passive colonization and asexual colony multiplication in the massive coral Porites lutea Milne Edwards & Haime". Journal of Experimental Marine Biology and Ecology. 47 (1): 55–67. doi:10.1016/0022-0981(80)90137-9.
- ^ Zamania, Neviaty P.; Arman, Ali; Lalang (2016). "The growth rate of coral Porites lutea relating to the El Niño phenomena at Tunda Island, Banten Bay, Indonesia". Procedia Environmental Sciences. 33: 505–511. doi:10.1016/j.proenv.2016.03.103.
- ^ Harland, A.D.; Brown, B.E (1989). "Metal tolerance in the scleractinian coral Porites lutea". Marine Pollution Bulletin. 20 (7): 353–357. doi:10.1016/j.proenv.2016.03.103.