| Coral reefs of the Solomon Islands | |
| Location: | Pacific Ocean |
| Archipelago: | Solomon Islands archipelago |
| Total Islands: | 6 main islands and more than 986 smaller islands |
| Major Islands: | Choiseul, the New Georgia Islands, Santa Isabel, Malaita, Makira (San Cristobal), Guadalcanal. |
| Country: | Solomon Islands |
The Coral reefs of the Solomon Islands consists of six major islands and over 986 smaller islands,[1] in Oceania, to the east of Papua New Guinea and northwest of Vanuatu. The Solomon Islands lie between latitudes 5° and 13°S, and longitudes 155° and 169°E. The distance between the westernmost and easternmost islands is about 1500km (900miles). The Santa Cruz Islands are situated north of Vanuatu and are especially isolated at more than 200km (100miles) from the other islands. The Solomon Islands (the Solomons) has the 22nd largest Exclusive Economic Zone of 1589477km2 of the Pacific Ocean.
The Solomons has a rich and diverse marine life, including coral reefs and seagrass meadows. The islands are part of the Coral Triangle, the region of the western Pacific with the World's greatest diversity of corals and coral reef species. The recognizable reef systems in the Solomons are: fringing reef, patch reef, barrier reef, atoll reefs and lagoon environment.[1] The baseline survey of marine biodiversity in 2004,[2] [3] identified the Solomons as having the second highest diversity of corals in the World, second only to the Raja Ampat Islands in eastern Indonesia.[4]
The Coral reefs of the Solomons make up nearly 6750km2 of total coral reef area.[5] There are 113 Locally Managed Marine Areas (LMMA) containing an estimated 155 no-take zones in the Solomons. The largest LMMA, with a contiguous 13km (08miles) no-take zone, is on Tetepare Island.[6]
More than 90% of inshore coastal areas, reefs and islets in the Solomons are owned and managed under the customary marine tenure system, under which family units, clans, or tribes have rights to access and use marine resources. This kinship group ownership system is recognised under the Solomon Islands Constitution.[7] The methods of management of marine resources under the customary marine tenure system include limited entry, closed seasons, closed areas, size limits, species prohibitions and restrictions on the use of fishing equipment.[7] The success or failure of conservation efforts on coral reefs largely depends on the attitudes of the communities owning them.[8]
See also: Protected areas of Solomon Islands.
A total 12 offshore sites and 53 inshore sites have been identified as Key Biodiversity Areas (KBAs) - areas of high biodiversity and conservation.[9] The highest-scoring sites were Marovo Lagoon and the Arnavon Community Marine Conservation Area.[9] The offshore sites are Roncador Reef, Ontong Java Atoll, Tikopia, and Vanikoro, an island in the Santa Cruz group.[9]
KBAs include:
The Solomon Islands are located at the edge of the Solomon Sea Plate, the Pacific Plate and other oceanic tectonic plates. These autochthonous geological systems have tilted to push up and create some of islands, and some of islands are volcanic in origin.[11] [12]
The coral reefs are developed by the carbonate-based skeletons of a variety of animals and algae. Slowly, over time, the reefs have built up to the surface in oceans.[13] Coral reefs are found in shallow, warm salt water. The sunlight filters through clear water and allows microscopic organisms to live and reproduce. Coral reefs are composed of tiny, fragile animals known as coral polyps. Coral reefs are significantly important because of the biodiversity, and are at risk from the detrimental effects of human action and inaction, such as overfishing; and heightened levels of nutrients in the water due to pollution from human waste, which feeds the growth of Macroalgae species (seaweed).
The coral reefs of the Solomons are predominantly fringing reefs, although Ontong Java Atoll and Sikaiana, are examples of coral atolls. Long submerged barrier reefs are uncommon in Solomons,[14] although there are some examples, including in the Reef Islands, a line of four reefs stretches westwards for 21km (13miles) while the Great Reef, which is further north, is about 25km (16miles) long.[8]
The fringing reefs of the Solomons are found off the mountainous volcanic islands of the Solomon Islands archipelago, which includes Choiseul, the Shortland Islands, the New Georgia Islands, Santa Isabel, the Russell Islands, the Florida Islands, Tulagi, Malaita, Maramasike, Ulawa, Owaraha (Santa Ana), Makira (San Cristobal), and the main island of Guadalcanal. Bougainville Island is the largest island in the archipelago, while it is geographically part of the Solomon Islands archipelago, it is politically an autonomous region of Papua New Guinea. The volcanic islands with fringing reefs include the remote, tiny outliers, Tikopia, Anuta, and Fatutaka.[8]
The largest coral reef systems in the Solomons are located where large lagoons are protected by raised or semi-submerged barrier reefs or by raised limestone islands, such as, Marovo Lagoon and Roviana Lagoon (on the southern side of New Georgia Island.[8] There are some large lagoon complexes are that are protected by volcanic islands, raised islands, sand cays, or barrier reefs. Examples of such as reefs are (1) Marau Sound in the eastern part of Guadalcanal; (2) Lau Lagoon on the northeast coast of Malaita; (3) in the vicinity of Vangunu in southeastern New Georgia; (4) in Gizo, on Vonavona island, and the lagoon of New Georgia; (5) along the northeastern coast of Choiseul; (6) on both sides of Manning Strait between Choiseul and Santa Isabel Island; (7) and adjacent to the Shortland Islands near Bougainville.[14]
Sikaiana (formerly called the Stewart Islands) is a small atoll 212km (132miles) northeast of Malaita is almost 14km (09miles) in length and its lagoon, known as Te Moana, is totally enclosed by the coral reef. Sikaiana is an example of a coral atoll formed from an oceanic volcano, with a coral reef growing around the shore of the volcano and then, over several million years, the volcano becomes extinct, eroded and subsided completely beneath the surface of the ocean. The reef and the small coral islets on top of it are all that is left of the original island, and a lagoon has taken the place of the former volcano. For the atoll to persist, the coral reef must be maintained at the sea surface, with coral growth matching any relative change in sea level (subsidence of the island or rising oceans).[15] On the atolls, an annular reef rim surrounds the lagoon, and may include natural reef channels.[16]
Rennell has a land area of 660km2 that is about 80km (50miles) long and 14km (09miles) wide. It is the second largest raised coral atoll in the world.[17] Rennell Island is an example of a reef island also formed from an oceanic volcano that has a completely closed rim of dry land, with the remnants of a lagoon that has no direct connection to the open sea.
The Marovo lagoon is the second largest saltwater lagoon in the World at 700km2. Huvadhu Atoll in the Maldives is the largest saltwater lagoon at 3152km2. Marovo lagoon is surrounded by Vangunu Island and Nggatokae Island, both extinct volcanic islands, at . It is part of the New Georgia Islands, which are located to the northwest of Guadalcanal and is protected by a double barrier reef system.
The volcanic island of Malaita includes, on the northwest coast, the Langa Langa Lagoon and the Lau Lagoon on the northeast coast. The Langa Langa Lagoon or Akwalaafu, is NaNkm (-2,147,483,648miles). The Lau Lagoon is more than 35km (22miles) long and contains about 60 artificial islands built on the reef.[18] [19] [20] The people of the Lau Lagoon continue to live on the reef islands.[21] [19] [20]
See also: List of corals of the Solomon Islands.
The baseline survey of marine biodiversity in 2004,[22] identified 494 coral species, including nine potentially new species and extended the known range of 122 coral species to include the Solomons.[23] The 2004 survey also recorded 1,019 species of reef fish, of which 47 were species range extensions.[24]
There are 3 species of pearl oysters: Black-lip oyster (Pinctada margaritifera), White-lip oyster (Pinctada maxima), and Pteria penguin.[25] [26]
Six species of giant clam (Tridacna) occur: Tridacna crocea; Hippopus hippopus; Tridacna squamosa; Tridacna maxima; Tridacna derasa (southern giant clam or Smooth giant clam); and Tridacna gigas, which can grow to 1m (03feet).[10] These giant clams have been overharvested and restrictions now protect the resource for local subsistence use only. Only farmed shells are allowed to be marketed commercially.[8] [25]
Erect coralline algae (red algae), and Halimeda (green macroalgae) was commonly found throughout the Solomons, particularly at depths deeper than 15 meters.[10]
Reef sites and lagoons within Western Province were surveyed in 2014 near Gizo, Munda, Marovo Lagoon and Nono Lagoon, both located in the New Georgia Islands. These areas had an average Live Coral Cover (LCC) ranging from 18 to 49%. The sites with the highest LCC in the Western Province and second highest in the Solomons were on the exposed side of the fringing reef near Marovo Lagoon measuring an average of 49% LCC. The exposed side of the fringing reef of Marovo Lagoon had an average of 38% LCC. The sites with the lowest live coral cover were found near Munda with an average of 18% LCC.[10] The exposed side of the fringing reef of Marovo Lagoon was dominated by Acropora, followed by Porites, Montipora, Millepora, and Echinopora. Munda was dominated by Acropora, followed by Porites, Montipora and Agariciidae.[10]
Nono Lagoon had an average overall LCC of 32%; with individual sites ranging from 20% to 50% LCC. The lagoon floor cover included leather corals, sponges, and other soft corals such as (Sinularia and Sacrophotons). The algal community within Nono Lagoon was dominated by crustose coralline algae which accounted for 47% of the total algae observed, with the next most dominant algae being turf algae accounting for 29% of the total algae.[10]
The coral diversity in the Western Province was evenly spread among common reef-building genera including Porites, Acropora, Montipora, Pocillopora, Pocillopora, Turbinaria and Millepora (hydrocorals). Isopora was one of the most abundant coral genera in the reefs off Gizo.[10]
Reef sites within Temotu Province were surveyed in 2014 around the Reef Islands, Utupua, Vanikoro and Tinakula and were identified as having some of the highest coral diversity when compared to the other sites surveyed in the Solomons. The Reef Islands are small, uplifted coral islands with an average of 31% LCC. These reefs have the highest percentage of erect coralline algae of all the areas surveyed in the Solomons and are abundant with Halimeda (green macroalgae) that accounted for 38% of the total algae measured. Crown-of-thorns starfish (Acanthaster planci), were found on the reefs in numbers that indicated an active outbreak was occurring.[10] Vanikoro and Utupua are both small atolls found within the Temotu province that had relatively high live coral cover ranging from 42% to 44% respectively. Utupua had an average of 38 of algae of its reefs present, dominated by erect coralline algae 44% coverage of the reef system. Tinakula had lower levels of live coral cover as the volcano of Tinakula had erupted in 2012 so that there was an essentially new reef system beginning to form around the half of the island's reef that was damaged in the eruption. The Reef Islands and Utupua were dominated by Acropora and Porites. Tinakula was dominated by Acropora, Porites, Montipora and Millepora.[10] Vanikoro was also dominated by crustose coralline algae at 32%, however, there was a notable amount of erect coralline algae, particularly Halimeda, accounting for 21% of the total algae observed. A total of 40 different genera were observed at Vanikoro, which was dominated by Acropora, followed by Porites.[10]
Reef sites and lagoons within Isabel Province were surveyed in 2014 around Kerehikapa and Sikopo within the boundaries of the Arnavon Community Marine Conservation Area, as well as the area around Malakobi, which lies outside the conservation area. The site at Kerehikapa had an average of 51% LCC, which was the highest average live coral cover of all areas surveyed in the Solomons. One site had the highest overall with 69% LCC. Algae accounted for an average of 30% around Kerehikapa and was composed predominately of crustose coralline algae and turf algae. Kerehikapa was dominated by Acropora, followed by Porites. These two dominant genera accounted for over 40% of the coral observed at this site.[10]
Sikopo had only 30% LCC when compared to Kerehikapa with significant amounts of coral rubble and very little reef structure, which may have been damage caused by the tsunami that struck Isabel Province in April 2007. The dominant genera around Sikopo were Acropora and Montipora, with Cyphastrea at greater levels as compared to other regions of the Solomons.[10] The survey outside of the conservation area at Malakobi identified live coral cover ranged drastically from 8-45%. The average algal cover of 52% was evenly spread among crustose coralline algae, erect coralline algae, macroalgae and turf algae. Malakobi was dominated by Acropora, Isopora and Porites.[10]
The reefs in the Solomons are exposed to the effects of pollution and over-utilisation of the reef resources by the residents of the islands,[5] and are facing detrimental effects on them due to a variety of factors that are the consequence of Climate Change such as: bleaching; an increased number of destructive tropical cyclones and the potential threat of ocean acidification that would be the result of a lowered pH of ocean waters caused by increased carbon dioxide emissions into the atmosphere, which results in more CO2 dissolving into the ocean.
There are a variety of human activities that are threats to reefs and marine ecosystems, including: Blast fishing using dynamite; the harvesting of coral for lime production for betel nut chewing; mining of corals for construction purposes (e.g., building of seawalls and other structures); and fishing of species that are important in maintaining the functioning of the reef ecosystem.[8] The forms of pollution include: sewage and waste from houses or factories, such as the processing of fish; sedimentation from run-off following removal of trees through logging in the forests; and plastics and other non-degradable refuse entering the ocean.[1] [14] [27] [28]
There was a 36-month bleaching event on the reefs of the Solomons in 2014–2017.[6] The bleaching was a consequence of an increase in ocean temperatures that happened during the El Niño events. Bleaching events can alter the community composition of coral reefs by changing the relative abundance of corals based on the susceptibility of different species of corals to bleaching-induced mortality. Branching corals such as Acropora (staghorn corals), which tend to be more susceptible to bleaching-induced mortality.[6]
Bleaching is a process that expels the photosynthetic algae from the corals' "stomachs" or polyps.[29] This algae is called zooxanthellae. It is vital to the reef's life because it provides the coral with nutrients; it is also responsible for the color.[30] The process is called bleaching because when the algae is ejected from the coral reef the animal loses its pigment. Zooxanthella densities are continually changing; bleaching is an extreme example of what naturally happens.[31]
Surveys in 2016 identified that the reefs around New Georgia Island and Kolombangara Island in Western Province had substantially survived the thermal anomalies that caused extensive coral bleaching in other parts of the Indo-Pacific as the result of heat stress when water temperatures were recorded as high as 30C, even down as far as 25m (82feet) during an El Niño event.[32]
The survey of reefs in 2018 at 13 sites in the Western Province, and at 4 islands (Mbabanga, Tetepare, Uepi, Gatokae) in the New Georgia Islands, concluded that reef-building capacity (percentage cover of reef building organisms: hard corals and coralline algae), as the indicator of the resilience of reefs to large-scale disturbances, was high across the sites.[6] The average percent cover of active reef builders at these sites in Western Province (44.6%) was comparable to that of remote uninhabited islands in the Central Pacific (45.2%), and substantially greater than inhabited islands (27.3%) in the same region.[6] The conclusion reached was that the surveyed reefs in the Western Province remain healthy and functional in the face of recent global and local stressors. The conclusion was that the relatively healthy status of the reefs likely reflects local variation in seawater temperature and low levels of bleaching stress.[6]
However, in January 2021, the reefs around Marovo Lagoon including the Zaira Resource Management Area on the western coast of Vangunu Island, and New Georgia Island were reported as suffering a widespread coral bleaching event.[32]