Acropora (Acropora divaricata)

KingdomAnimalia
PhylumCnidaria
ClassAnthozoa
OrderScleractinia
FamilyAcroporidae
GenusAcropora (1)

Acropora divaricata is classified as Near Threatened (NT) on the IUCN Red List (1) and listed on Appendix II of CITES (2).

A reef-building coral that is flat or sponge-like in appearance, Acropora divaricata is often the dominant coral species in reefs throughout the Indian and west Pacific Oceans. It is a member of a fast-growing group of corals known as the staghorns due to their branching structure. Their speed of growth, however, is balanced by the fragility of some of the structures, as they are easily damaged in storms allowing other coral species a chance of growth. Like other colony-forming corals, colonies of Acropora divaricata  are composed of numerous small polyps, soft-bodied animals related to anemones. Each polyp bears numerous tentacles that direct food into a central mouth, where it is digested in a sac-like body cavity. One of the most remarkable and ecologically important features of stony corals (order Scleractinia) is that the polyps secrete a hard skeleton, called a ‘corallite’, which over successive generations contributes to the formation of a coral reef. The coral skeleton forms the bulk of the colony, with the living polyp tissue comprising only a thin veneer (3). Living colonies of Acropora divaricata are usually dark brown or greenish in colour, but are sometimes light brown or dark blue, with whitish tips on the blunt branches (3) (4).

Acropora divaricata is found in the Indian and Pacific Oceans, ranging from the Red Sea, Gulf of Aden and southwest Indian Ocean, across the northern Indian Ocean to Southeast Asia, Japan and the East China Sea, and the western Pacific Ocean (1).

Throughout its range Acropora divaricata can be found on almost any reef habitat, and is quite often the dominant coral species. It is particularly common on reef fronts and slopes, in lagoons and on fringing reefs. It is found between depths of 5 and 25 metres, with colonies becoming flatter in shape with depth (1).   

Like many corals, staghorn corals have a special symbiotic relationship with algae, called zooxanthellae. The algae gain a safe, stable environment within the coral's tissues, while the coral receives nutrients produced by the algae through photosynthesis. While, on average, zooxanthellate coral can obtain around 70 percent of its nutrient requirements from zooxanthellae photosynthesis, the coral may also feed on zooplankton (3).  

Staghorn corals are reef-building, or hermatypic corals, and are incredibly successful at this task for two main reasons. Firstly, they have light skeletons which allow them to grow quickly and out-compete their neighbouring corals. Secondly, the skeleton, or corallite, of a new polyp, is built by specialised ‘axial’ corallites. These axial corallites form the tips of branches, and as a result, all the corallites of a colony are closely interconnected and can grow in a coordinated manner. By harnessing the sun's energy, staghorn corals are able to grow relatively rapidly and form vast reef structures, but are constrained to live near the water surface (3). 

Staghorn corals reproduce sexually or asexually. Sexual reproduction occurs via the release of eggs and sperm into the water. Streams of pinkish eggs are released from corallites on the sides of branches, to be fertilised by sperm released from other polyps at the same time. The water turns milky from all the eggs and sperm released from thousands of colonies. Some of the resulting larvae settle quickly on the same reef, whilst others may drift around for months, finally settling on reefs hundreds of kilometres away. Asexual reproduction occurs via fragmentation, when a branch breaks off a colony, reattaches to the substrate and grows (3).

With an estimated 20 percent of the world’s coral reefs already destroyed, Acropora divaricata faces many of the threats that are affecting coral reefs globally (5) (6). Worldwide there is increasing pressure on coastal resources resulting from human population growth and development. There has been a significant increase in domestic and agricultural waste in the oceans, poor land-use practices that result in an increase in sediment running on to the reefs, and over-fishing, which can have ‘knock-on’ effects on the reef (5). However, the major threat to corals is global climate change, with the expected rise in ocean temperatures increasing the risk of coral ‘bleaching’, in which the stressed coral expels its zooxanthellae, often resulting in the death of the coral (6). Corals in the genus Acropora are particularly vulnerable to such bleaching events and typically take a long time to recover from them (1). Climate change may also lead to more frequent, severe storms, which can damage reefs, and rising carbon dioxide levels may make the ocean increasingly acidic. Such stresses can also make corals more susceptible to disease, parasites and predators, such as the crown-of-thorns sea star (Acanthaster planci) (5) (6) (7).

In addition to being listed on Appendix II of the Convention on International Trade in Endangered Species (CITES), which makes it an offence to trade this species without a permit, Acropora divaricata also forms part of the reef community in numerous marine protected areas (1) (2). To specifically conserve this coral, recommendations have been made for a raft of studies into various aspects of its biology, population status, habitat and threats to its survival (1).

For further information on the conservation of coral reefs, see:

This information is awaiting authentication by a species expert, and will be updated as soon as possible. If you are able to help please contact:
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  1. IUCN Red List (October, 2010)
    http://www.iucnredlist.org/
  2. CITES (October, 2010)
    http://www.cites.org/
  3. Veron, J.E.N. (2000) Corals of the World. Australian Institute of Marine Science, Townville, Australia.
  4. World Register of Marine Species - Acropora divaricata (October, 2010)
    http://www.marinespecies.org/aphia.php?p=taxdetails&id=207106
  5. Wilkinson, C. (2004) Status of Coral Reefs of the World: 2004. Volume 3. Australian Institute of Marine Science, Townsville, Australia.
  6. Carpenter, K.E. et al. (2008) One-third of reef-building corals face elevated extinction risk from climate change and local impacts. Science, 321: 560-563.
  7. Miththapala, S. (2008) Coral Reefs. Coastal Ecosystems Series (Volume 1). Ecosystems and Livelihoods Group Asia, IUCN, Colombo, Sri Lanka.