Location and General Description
Christmas Island is located 360 km south of Jakarta, Indonesia at 100 S and 1050 E. The 137 km2 island is the peak of an ancient volcano rising 5000 m from the ocean floor. While it’s volcanic origin is mostly hidden under a thick crust of porous coralline limestone and phosphate-rich soil, the underlying basalt is exposed in a few places allowing the accumulation of surface water. As sea levels have changed, limestone has been deposited and eroded resulting in a series of stepped terraces rising to an inland plateau 250-300 m high. Undercut cliffs dominate much of the island’s coastline except for a few beaches around the northeast. The climate is tropical with temperatures between 23-290 C and a constant humidity of 80-90% (Gray 1981). Over 2000 mm of rain falls on the island, mostly during the northwest monsoon between December to April (Stoddart 1971).
Christmas Island forests are dominated by Indo-Malaysian and Melanesian tree species that form a dense evergreen canopy supporting a diverse epiphyte community, but with little understory vegetation (Du Puy 1993). During the dry season some deciduous species drop their foliage exposing the understory to more light (Du Puy 1993). In areas with deep soil, the canopy reaches 30-40 m with emergents growing to 50 m. The most common tree canopy species are: Planchonella nitida, Syzygium nervosum, Tristiropsis acutangula, Inocarpus fagifer, and Hernandia ovigera. The understory is dominated by two endemic species: the palm Arenga listeri and the tree-like Pandanus elatus (Du Puy 1993). The forest floor is almost bare of leaf litter, seeds, or seedlings because they are quickly consumed by the approximately 100 million red crabs (Gecarcoidea natalis) found in the forest (Green 1997). In total there are 237 native and 174 introduced plant species on the island, and most of the introduced species are restricted to disturbed sites (Du Puy 1993).
The Cocos Islands are located 1000 km southwest of western Java, Indonesia at 120 S and 960 E. The ecoregion consists of two separate island groups: 1.1 km2 North Keeling Island is about 25 km north of the main horseshoe-shaped atoll of 30 islands. Each island group sits atop a volcanic seamount in the Vening Meinesz chain (Telford 1993). As the seamounts have subsided downward, reef-building has maintained land near the sea surface such that the coral rock is built up 0.5-1.0 km thick over the igneous base (Telford 1993). However, coral growth has not always kept pace with changes in sea level and all land in the islands was submerged as recently as 4000 BP (Woodroffe et al. 1990). Currently, the highest point is atop a 9 m sand dune and soils are based mostly on coral, guano, and pumice washed ashore after volcanic eruptions nearby. The southern islands encircle a large lagoon that ranges in depth from 1 m in the southern end to 15 m in the north. The islands are tropical with mean daily temperatures ranging from 26-280 C. Southeast trade winds are fairly constant with an average rainfall of over 2100 mm falling predominantly between January and September when cyclones also occur (Falkland 1994).
While almost all natural forests in the Cocos southern atoll have been replaced with coconut plantation or other introduced species, the vegetation on North Keeling Island remains fairly intact and is probably representative of the flora that used to exist throughout the island group. Pisonia grandis forest up to 25 m tall dominates sheltered areas with low numbers of Laportea aestuans, Canavalia cathartica, and Erythrina variegata. In more exposed areas strand forest is dominated by coconut (Cocos nucifera), Calophyllum inophyllum, Argusia argentea, Cordia subcordata and an endemic pandanus subspecies (Pandanus tectorius cocosensis), with Scaevola taccada, Suriana maritime, and Hibiscus tiliaceus present as shrubs (Telford 1993). Herbfields dominated by Stenotaphrum micranthum, Lepturus repens, and Ipomoea pes-capreae are present at the tops of numerous ocean beaches (Williams 1994). Most plant species in the Cocos Islands are widespread species from Pacific and Indian Ocean strand communities (Telford 1993, Williams 1994).
With individual weights up to 500 grams (1 lb.), densities of 1.2 – 2.6 crabs/m2, and biomass up to 1454 kg per hectare (O’Dowd and Lake 1991, Green 1997) red crabs (Gecarcoidea natalis) are the most striking feature of Christmas Island forests. The crabs live in the understory of rainforest where humidity is high enough to prevent desiccation. They excavate burrows 40-100 cm long and live a solitary existence feeding on leaf litter, fruit, and seeds. Their densities are so high that most fruit and seeds are removed and consumed within 12 hours of falling to the ground (O’Dowd and Lake 1991) and the forest floor is often completely clear of plant matter (Du Puy 1993). At the beginning of the wet season, usually in November or December, all adult crabs leave their burrows and spend 9-18 days migrating to coastal locations (Hicks 1985). They mate near the sea, in burrows excavated by males, lay eggs in the ocean, and then return to the forest (Hicks 1985).
For such a small island, Christmas Island supports a large number of endemic species and subspecies of animal and plant including one of the rarest owls in the world, the Christmas Island hawk owl (Ninox natalis), Christmas Island frigatebird (Fregata andrewsi), the endangered Abbott’s booby (Papasula abbotti), Christmas Island imperial pigeon (Ducula whartoni), and the Christmas Island white-eye (Zosterops natalis) (Du Puy 1993, Hill and Lill 1998). All but three endemic species are still present. The extinction of the endemic rat, Rattus maclari, around 1900 was caused by hybridization with introduced Rattus rattus and disease (Pickering and Norris 1996). Two of 16 endemic plant species have also disappeared. There are also another 16 species of land crab present in low densities, including a large population of coconut crabs (Birgus latro).
Although the Cocos Islands are the most isolated tropical islands in the Indian Ocean their isolation has not resulted in high levels of endemism. This is probably the result of the submergence of all land in the islands within the last 4000 years and frequent catastrophic cyclones that inundate much of the land (Woodroffe and Berry 1994). They support 121 vascular plant species, including 57 introduced species, and at least 14 seabird species. The only two forest birds are an endemic subspecies of the buff-banded rail (Rallus phillippensis andrewsi) and the Christmas Island white-eye (Zosterops natalis) which was introduced between 1885-1900 (Stokes et al. 1984). The Cocos Islands support at least 9 species of terrestrial crab including the coconut crab (Birgus latro) and the Christmas Island red crab (Gecarcoidea natalis), introduced earlier this century. Terrestrial crabs only occur in significant numbers on North Keeling Island where they quickly consume fruit, seeds, seedlings, and leaf litter keeping the forest floor open (Telford 1993, Morgan 1994).
The majority of Christmas Island’s forest is intact and protected in a national park that covers 63% of the island including almost all of the western half of the island with a smaller isolated section on the east coast (Du Puy 1993). Forest habitat outside the national park is highly fragmented between phosphate-mined areas, human settlements, and roads (Shepherd 1994) but still provides some habitat for threatened birds (Yorkston and Green 1997, Hill and Lill 1998)
The flora and fauna of the Cocos southern atoll islands has been completely modified since human settlement in the 1800’s with overexploitation resulting in the disappearance of most terrestrial species. Most forest has been replaced with coconut plantation. Only the uninhabitated North Keeling Island supports significant tracts of tall and strand forest and has relatively large populations of the endangered buff-banded rail, red-footed boobies (Sula sula) and native land crabs (Stokes et al. 1984, Telford 1993, Morgan 1994). Seabird breeding colonies throughout the Cocos Islands supported immense numbers of birds before human settlement (Gibson-Hill 1949), but today only North Keeling supports seabirds and these are endangered by egg poaching and shooting by hunting parties from the south (Stokes 1984).
Types and Severity of Threats
Phosphate mining has been and continues to be the major threat on Christmas Island. Clearing of forest and removal of soil before 1987 resulted in the destruction of 25% of the Abbott’s booby’s nesting habitat and 15% of the adult population (Shepherd 1994). Mined areas either remain bare or are colonized by introduced plant species and the increased wind turbulence in these areas decreases nest success for boobies (Hill and Lill 1998). Mining is now restricted to processing of existing stockpiles of soil, but future forest clearing in areas outside the national park could have detrimental effects on endemic species. The Australian government is currently attempting to rehabilitate mining areas by replacing some soil and outplanting mostly native tree seedlings (Australian National Parks and Wildlife Service 1986) although, at a rate of 10 hectares/year, it will be some time before forest is restored to all mined areas in the national park (Shepherd 1994). Red crab populations appear to be unaffected by introduced mammalian predators or massive automobile-related mortality (Hicks 1985) and will likely to continue as a spectacular feature of Christmas Island into the foreseeable future.
While cyclones will continue to have a dramatic and unpredictable impact on the native flora and fauna of North Keeling Island of the Cocos group, poaching and human activity will persist as the most overriding threat. A formal moratorium protecting seabirds was made by the Australian government and Cocos Island residents, but this has failed to stop poachers from destroying thousands of adults and nests through the 1980’s and 1990’s (Stokes 1994). There is some hope that local conservation education, more active patrolling, cat and rat control, and reserve declaration called for in the Australian National Parks and Wildlife Service action plan for North Keeling will go some way toward protecting this last wild piece of the Cocos Islands, but the island’s future is by no means certain (Stokes 1994).
Justification of Ecoregion Delineation
Christmas and Cocos Islands are isolated oceanic islands in the Indian Ocean. This isolation has resulted in a significant rate of endemism on Christmas Island. This has not been the case for the Cocos Islands. However, these islands typify atoll ecosystems throughout the Indian and Pacific Oceans to the extent that Charles Darwin provided the basis for his theory on coral reef and atoll development- which still holds today- based on a visit to Cocos in 1836 (Darwin 1842).
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Prepared by: Tim Male
Reviewed by: In process