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New ZealandDavid R. Given38, Alan Saunders39, Dave Towns40, Alan Tennyson41 and Keri Nielson42 New Zealand (Aoteraroa) is the only hotspot that encompasses the entire land area of a developed nation. A piece of Gondwanaland that separated from Australia about 82 million years ago (Sutherland 1999), it now forms an isolated archipelago located some 2 000 km to the southeast of Australia in the southern Pacific Ocean. It covers 270 197 km2, with the three main islands, North Island, South Island, and Stewart Island, making up 90% of the land area. Smaller outliers are the Chatham Islands (963 km2) 800 km east of South Island, the Kermadec Islands (34 km2) to the north, and the Subantarctic Islands to the south (including the Bounty Islands, Antipodes Islands, Campbell Island, Snares Islands, Auckland Islands, and Macquarie Island). Also included here are Lord Howe (14.6 km2) and Norfolk (36.8 km2) islands, both Australian territories. Climate is an important determinant of biotic patterns in New Zealand. The country is strongly influenced by its mid-temperate location, northeast-southwest orientation, and hilly to mountainous topography, with about 75% of the land area above 200-m altitude and reaching a maximum altitude of 3 700 m on Aoraki (Mount Cook). The mountains form a barrier to westerly airflow, resulting in 12 000 mm or more annual rainfall on the western flank of the Southern Alps, one of the highest on Earth, and heavy falls of winter snow. In striking contrast, rainshadow areas east of the Southern Alps can experience as little as 300 mm annually. The Kermadec Islands have a subtropical climate, with warm, moist conditions throughout the year, while the Chatham Islands have a cloudy, humid climate, with cool, wet winters and warm, often dry summers. The southern Subantarctic Islands have a generally windy, cool, temperate-montane climate and relatively low levels of sunshine.
New Zealand has relatively low plant species diversity, with 3 400 species (including 2 300 vascular species and 1 100 liverworts and mosses), but high endemism. At least 1 865 vascular plants are endemic (81%) and an additional 220-440 liverworts and mosses (20%-40%), the exact number for the latter not yet having been determined. In addition, of the estimated 390 plant genera, there are about 35 endemic genera. Some of the more interesting plant species on New Zealand include the endemic fern Loxoma cunninghamii, whose closest living relatives are three species of the genus Loxomopsis from Central America, and the pingao sand sedge, belonging to the endemic monotypic genus Desmoschoenus. There is also a single endemic family, the Ixerbaceae, represented by a single species (I. brexiodes).
Reptiles are represented by 37 species on New Zealand, and all native species are endemic and, remarkably, five of the six genera represented are endemic. The largest terrestrial reptile in this hotspot is the tuatara (Sphenodon spp.), a member of an endemic order (Sphenodontida), and the only case in which an entire reptilian order is endemic to a single country. It was previously thought that only one species, S. punctatus, existed, but a second species, S. guntheri, has now been recognized. These reptiles, superficially resembling iguana lizards, are the last survivors of a group that lived side by side with the dinosaurs and whose heyday was the Triassic Period some 200 million years ago (May 1990). Amphibians and mammals are the two groups of terrestrial vertebrates that are poorly represented. There are only four native frog species, all highly primitive and members of an endemic family, Leiopelmatidae, and genus, Leiopelma, found only on New Zealand. Native mammals on New Zealand number only two, both of them endemic bats, but one, the New Zealand lesser short-tailed bat (Mystacina tuberculata, VU), is the only living representative of an endemic family, Mystacinidae. The hotspot harbors one of the smallest but most distinctive inland fish faunas of any hotspot, with 39 species in 15 genera, and 25 endemic species. This fauna is dominated by members of the family Galaxiidae, a group of coolwater trout-like fishes restricted to the southern tips of South America, Africa, Australia, New Zealand, and a few small islands such as Lord Howe and the Campbell Islands. Of the 51 galaxiid species known worldwide, 19 occur in the hotspot and 16 are restricted to it. A related family, the Retropinnidae or New Zealand smelts, is represented in the hotspot by three endemic species including the only member of the endemic genus Stokellia. A distinctive element of the New Zealand biota is the widespread occurrence of gigantism (Daugherty et al. 1993). Some of the giant forms include the now extinct flightless moas and Haast's eagle among the birds, and also giant insects, myriapods, flatworms, land snails, centipedes, slugs, earthworms, and some plants. The world's heaviest insect, the weta or wingless cricket of Little Barrier Island (Hauturu) weighs up to 70 g and is one of 12 species of Deinacrida, the ancestors of which roamed the Jurassic forests. However, this biodiversity represents only a small percentage of what existed prior to human settlement on these islands. As is the case with many oceanic islands, humans arrived fairly late on New Zealand, with the Maoris first arriving perhaps 700-800 years ago (Ministry for the Environment 1997) and the Europeans in the early part of the nineteenth century. Since then, remarkable species like the giant moas (which reached nearly 3 m in height) and the immense Haast's eagle that preyed on the moas, have gone extinct. Human impact on the pristine ecosystems of New Zealand can be divided into three main categories: predation through hunting, fishing, and gathering; habitat destruction through deforestation, wetland drainage, and ecosystem degradation of various kinds; and, particularly, introduction of alien species, both plant and animal. Since European settlement alone, some 16 land birds, one native bat species, one fish, at least a dozen invertebrates and 10 plants are believed to have gone extinct, while other species such as the tuataras, the stitchbird (Notiomystis cincta, VU), and the North Island saddleback (Philesturnus carunculatus rufusater) survive only on offshore islands. Furthermore, prior to the arrival of humans in New Zealand, indigenous forest covered some 230 000 km2, or about 85% of the country, with the remainder being native grasslands, duneland ecosystems, and wetlands. Today, the forest has been reduced to 62 000 km2, or about 23% of the country, and only about 35 000 km2 (13%) of this is still in more or less pristine condition. Grasslands, on the other hand, have now increased from 10 000–20 000 km2 to more than 140 000 km2, or 52% of the country; however, most of this is grazed or overgrown with introduced grasses, leaving only about 15 000 km2 in more or less pristine condition. Duneland ecosystems, one of the most threatened ecosystem types in the country, are now down to no more than 250 km2. Wetland systems have been especially heavily impacted; once covering perhaps as much as 10 000 km2, or almost 4% of the country, they have now been substantially reduced in extent, with only about 4 000 km2 still remaining in good condition. In terms of natural habitat, then, it is estimated that remaining indigenous habitat in more or less primary condition amounts to 35 000 km2 of forest, 15 000 km2 of native grassland-scrub, 4 000 km2 of wetlands and other aquatic systems, 2 600 km2 of smaller island ecosystems, 1 800 km2 of alpine systems, and about 1 000 km2 of coastal systems, for a total of 59 400 km2 (or 22% of the land surface of the country). The protected area network of the New Zealand Hotspot includes 3 345 protected areas in IUCN categories I to IV, covering around 22% of the hotspot. The additional protected areas in IUCN categories V and VI bring the total surface area of the hotspot under a reasonable level of protection to 27%, a very high percentage by international standards. Comparing this figure with the 59 400 km2 estimated above to remain in more or less pristine condition, it is likely that much of what is left intact in New Zealand is already under some form of protection. In part, this is because a lot of New Zealand is mountainous, and areas like the Southern Alps are protected because the land can't be used for anything else; lowlands, on the other hand, are not nearly as well protected. At least 60 protected areas have been set aside as Nature Reserves or Wildlife Sanctuaries specifically to protect threatened species. These include many of the offshore and outlying islands ranging from the large subantarctic Auckland and Campbell Island groups, Little Barrier (Hauturu), and Kapiti, to the warm temperate Kermadec Islands.
Finally, no discussion on New Zealand would be complete without a word on invasive species, which have contributed to the decline and extinction of many native species in this country. While formal habitat protection is important, active pest management is required if further extinctions are to be avoided. Conservation practitioners in New Zealand have earned an international reputation for their achievements in eradicating invasive mammals from islands and, more recently, controlling animal and plant pests at “mainland” sites. Twelve species of pest mammals and one predatory bird have been successfully eradicated from offshore and oceanic islands in the New Zealand region (Veitch and Bell 1990). Significant recent advances have involved a new capability to eradicate rodents from much larger islands using aerial bait application techniques, and the use of more effective quarantine and contingency procedures to reduce the risks of further invasions. For example, Norway rats (Rattus norvegicus) were recently eradicated from Campbell Island (112 km2), opening the way for important species recovery and ecological restoration objectives. The Department of Conservation is applying a strategy to develop capacity to eradicate different suites of invasive species from further islands and to refine procedures to minimize invasion risks (Cromarty et al. 2002). Important recent progress has also been made in controlling invasive species on the New Zealand “mainland”– sites not surrounded by water, where terrestrial pest invasion rates are higher than on remote islands. Better planned and more consistently supported pest animal and weed control programs have resulted in significant conservation outcomes being recorded (Saunders 2000). < previous section < index > next section >
‹Preface: CEMEX› ‹Preface: Peter A. Seligmann› ‹Preface: Patricio Robles Gil› ‹Foreword: Harrison Ford› ‹Introduction› ‹An Update of Existing Hotspots› ‹Tropical Andes› ‹Tumbes-Chocó-Magdalena› ‹Atlantic Forest› ‹Cerrado› ‹Chilean Winter Rainfall-Valdivian Forests› ‹Mesoamerica› ‹Caribbean Islands› ‹California Floristic Province› ‹Guinean Forests of West Africa› ‹Cape Floristic Region› ‹Succulent Karoo› ‹Madagascar and the Indian Ocean Islands› ‹Mediterranean Basin› ‹Caucasus› ‹Western Ghats and Sri Lanka› ‹Mountains of Southwest China› ‹Sundaland› ‹Wallacea› ‹Philippines› ‹Southwest Australia› ‹New Zealand› ‹New Caledonia› ‹Polynesia-Micronesia› ‹Madrean Pine-Oak Woodlands› ‹Maputaland-Pondoland-Albany› ‹Coastal Forests of Eastern Africa› ‹Eastern Afromontane› ‹Eastern Arc Mountains and Southern Rift› ‹Albertine Rift› ‹Ethiopian Highlands› ‹Horn of Africa› ‹Irano-Anatolian› ‹Mountains of Central Asia› ‹ Himalaya› ‹Indo-Burma› ‹Japan› ‹East Melanesian Islands› ‹Taiwan› ‹Queensland Wet Tropics› ‹References› ‹Addresses› ‹Acknowledgements› ‹Image Captions and Photographer Credits›
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