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Lord Howe Island is located approximately 700 km east of Australia and 1,350 km northwest of New Zealand (31 S, 159E) on the submerged Lord Howe Rise. It is a 10 km long crescent-shaped remnant of a huge shield volcano that was formed about 6.9 million years ago as the Australian plate moved over a stationary hotspot (McDougall et al. 1981). The volcano has now eroded into Lord Howe Island, the tiny islets of the Admiralty Group, and Ball’s Pyramid, an islet now separated from Lord Howe Island by 21 km of water. There are two main peaks on the southern end of Lord Howe Island, Mt. Gower (875 m) and Mt. Lidgbird (777 m). The climate is humid-subtropical, with a mean annual rainfall of 1,717 mm (Mueller Dombois and Fosberg 1998). This rainfall is spread evenly throughout the year and enables the island to support a lush rainforest. Lord Howe Island is largely covered with rainforest, although there are areas of scrub, grassland, and clearings in the lowlands and on the cliffs. The lowland rain forest is divided into five types by Mueller-Dombois and Fosberg (1998): Drypetes-Cryptocarya, Cleistocalyx-Chionanthus, mixed broadleaf, Howea forsterana or H. belmoreana palm forest, and pandan forest (Pandanus forsteri). Cryptocarya gregsonii and the palm Hedyscepe canterburyana dominate the submontane forest. The understory is rich with ferns, tree-ferns (Cyathea spp.) and mosses. Canopy dieback occurs in this forest and is thought to be a natural phenomenon related to cohort senescence. On the upper reaches of Mt. Gower and Mt. Lidgbird, there is true cloud forest, dominated by Zygogynum howeanum and Dracophyllum fitzgeraldii. This stunted, gnarled forest is an important haven for the endemic Lord Howe woodhen (Gallirallus sylvestris), and is used as a breeding ground by Providence petrels (Pterodoma solandri). In general, the forests of Lord Howe Island show strong affinities with the flora of Australia, New Caledonia, and, to a lesser extent, New Zealand.
Due in part to its long isolation, the flora and fauna of Lord Howe Island show a high degree of endemism. Of the 241 native species of vascular plants, 105 are endemic species (DEST/ERIN 1995). There are 5 endemic plant genera: Negria, Lordhowea, and the palms Hedyscepe, Howea, and Lepidorrhachis (Rodd and Pickard 1983). At least 16 of the endemic plant species are considered rare, endangered or vulnerable, and many have extremely restricted ranges: the endemic Chionochloa conspicua is known from a single clump on Mount Lidgbird. There are currently 129 native and introduced bird species in the islands, 27 of which breed regularly on Lord Howe (Davey 1986). Nine of the original 15 native landbird species have gone extinct, including 7 endemic species.There are four extant endemic landbirds, including two species and two subspecies: the relatively abundant Lord Howe white-eye (Zosterops tephropleurus), the Lord Howe Island woodhen, Lord Howe Island golden whistler (Pachycephala pectoralis contempta), and the Lord Howe Island currawong (Strepera graculina crissalis). The woodhen was reduced to 25 individuals in the 1970s, but an intensive management program has boosted the population to more than 220 individuals (Miller and Kingston 1980). Seabirds use the islands as well, and one of the few known breeding grounds of the Providence petrel is in the cloud forest of Lord Howe Island. Approximately half of the world’s population of flesh-footed shearwater (Puffinus carneipes hullianus) breeds on the Island, and Lord Howe Island has the greatest concentration of red-tailed tropicbird (Phaethon rubricauda). Twelve other species of seabird also breed on the island. Not surprisingly, there is only one native mammal, the large forest bat (Eptesicus sagittula), and two native reptiles, a skink (Oligosoma lichenigera VU) (Hilton-Taylor 2000) and a gecko (Phyllodactylus guentheri), both of which may be extinct on the main island due to the effects of introduced predators (WCMC 1996). There are, however, many endemic invertebrate taxa in the subtropical forests, ranging from land snails to flies and earthworms. Of the 100 spider taxa described from Lord Howe, up to 50 percent are thought to be endemic. It is also worth noting that Lord Howe Island boasts the southernmost coral reef of any Pacific island, and that 4 percent of its fish taxa are shared only with Norfolk Island. Lord Howe’s geographical isolation led to the development of its unique flora and fauna. It also resulted in its persistence, in that the island was not settled until the early 19th century and has never supported a large human population. Only 10 percent of the land area has been cleared for human use, and an additional 20 percent of native vegetation has been disturbed by introduced animals, including cattle, feral sheep, goats, pigs, and rats. Most of the island is still forested, and 75 percent of the land area was declared a Natural World Heritage Site in 1982. The management of Lord Howe’s biological and cultural heritage is entrusted to the Lord Howe Island Board, which has been responsible for successfully eradicating goats from the islands and decimating feral pig populations. Efforts to control other introduced species such as rats, mice, and a variety of weeds are ongoing. The removal of feral animals has resulted in the recovery of forest understory on Lord Howe Island. Although most of Lord Howe Island is now protected, continued vigilance is needed to prevent the introduction and naturalization of exotic species. Introduced predators have had a devastating effect of the endemic land fauna, and introduced weeds are invading the islands and displacing native species. Continued control of existing exotics is an integral step in promoting the recovery of Lord Howe Island’s many threatened species (Davey 1986).
Includes the ‘Lord Howe Island’ EBA (Stattersfield et al. 1998). Part of ‘Norfolk and Lord Howe Islands’ CPD.
Australian National Parks and Wildlife Service. 1981. Nomination of the Lord Howe Island Group for inclusion in the World Heritage List. New South Wales Government, Sydney. Davey, A. 1986. Plan of management: Lord Howe Island Permanent Park Preserve. New South Wales National Parks and Wildlife Service, Sydney. DEST/ERIN. 1995. Lord Howe Island Group. Managed Area Report. Department of the Environment, Australia. Disney, H.J. and Smithers, C.N. 1972. The Distribution of Terrestrial and Freshwater Birds on Lord Howe Island, in comparison with Norfolk Island. The Australian Zoologist 17(1). Hilton-Taylor, C. 2000. 1998. The IUCN 2000 Red List of Threatened Species. IUCN, Gland, Switzerland and Cambridge, United Kingdom. McDougall, I., Embleton, B.J.J., and Stone, D.B. 1981. Origin and evolution of Lord Howe Island. Southwest Pacific Ocean: Journal of the Geological Society of Australia, 28: 155-176. Miller, B. and Kingston, T. 1980. Lord Howe Island Woodhen. Endangered Species of New South Wales. National Parks and Wildlife Service.
Mueller-Dombois, D. and F. R. Fosberg. 1998. Vegetation of the tropical Pacific islands. Springer-Verlag, New York, Inc. Recher, H.F. and Clark, S.S. 1974. A biological survey of Lord Howe Island with recommendations for the conservation of the island's wildlife. Biological Conservation 6(4): 263-273. Stattersfield, A. J., M. J. Crosby, A. J. Long, and D. C. Wedge. 1998. Endemic Bird Areas of the World. Priorities for biodiversity conservation. BirdLife Conservation Series No. 7. BirdLife International, Cambridge, United Kingdom. WCMC. 1996. Lord Howe Island Group. WCMC Database of Protected Areas. http://www.wcmc.org.uk/protected_areas/data/wh/lordhowe.html. viewed on August 24, 2001. Reviewed by: For more general information on this ecoregion, go to the WildWorld version of this description. All text by World Wildlife Fund © 2001 | |