The biodiversity of the Kaikōura region is the variety and variability of life within the land area of the Kaikōura District in New Zealand, and the ocean out to the territorial limit. The region has a diverse landscape ranging from a rugged sea coastline to high mountains. These landforms are shaped by ongoing tectonic movement and seismic activity. The waters offshore are particularly rich in marine life as a result of the convergence of two ocean currents, and the ocean canyon that creates deep water close inshore. The ocean environment offshore from Kaikōura is fundamental to much of the biodiversity in the region.
The economy of the Kaikōura District and township relies to a significant extent on the visitors who come to experience the biodiversity of the local region. Tourism represents around 25% of the GDP of the Kaikōura District.
Geography Land environment The geography of the Kaikōura region is characterized by a diverse landscape ranging from a rugged sea coastline to high mountains rising to . These landforms have been shaped by ongoing fault activity, creating diverse landscapes like alpine ranges, limestone hills, floodplains, and rocky cliffs. The stretch of coastline stretching roughly between the mouths of the Conway and Waiau Toa / Clarence Rivers is generally known as the Kaikōura coast. This coast is unusual for the east of the South Island, as there is very little coastal plain, with the Seaward Kaikōura Range, a branch of the Southern Alps, rising straight from the ocean in places.
The climate of this zone is strongly influenced by the Kaikōura Ranges and Southern Alps to the west. Summer temperatures can be warm, particularly when hot dry northwesterly winds blow over the Alps, although summer temperatures are often reduced by a cool sea breeze from the northeast. Long dry spells can occur, and mean annual rainfall is low. Cold southwesterly winds are more frequent during winter. Winters are cold and frosts can occur.
Ocean environment
The ocean environment offshore from Kaikōura is fundamental to much of the biodiversity in the region. The Kaikōura Canyon is a submarine canyon located southwest of the Kaikōura Peninsula. It is a southern branch of the Hikurangi Trough that extends northwards up New Zealand's eastern coast. The canyon descends into deep water and merges into an ocean channel system that can be traced for hundreds of kilometres across the deep ocean floor. At the head of the canyon, the depth of water is around , but it drops rapidly to and continues down to around deep where it meets the Hikurangi Channel. The canyon has been described as a "biodiversity hotspot", where upwelling of currents from the deep ocean provide feeding grounds along the Kaikōura coast and in offshore waters for a diverse range of seabirds and marine mammals. Studies of the Kaikōura Canyon have found that it is a highly productive ecosystem with 10 to 100 times the density of marine life found in other deep sea habitats. Sperm whales can be seen close to the coast south of the Kaikōura Peninsula, because the deep water of the Kaikōura Canyon is only off the shoreline at Goose Bay. A major Subantarctic Surface Water (SAW) current moves north up the coast of the South Island, coming inshore near Kaikōura during summer but being deflected by a northerly subtropical current during winter and early spring; this flow reversal is correlated with changes in the diving and feeding behaviour of sperm whales.
The town owes its origin to richness of marine life in the ocean, since it developed as a centre for the whaling industry. The name Kaikōura means 'meal of crayfish' (kai – food/meal, kōura – crayfish) and the crayfish industry still plays a role in the economy of the region. However, Kaikōura has now become a popular tourist destination, mainly for whale watching and swimming with or near dolphins.
Human impact Archaeological investigations of the Wairau Bar on the coast approximately north of Kaikōura suggest that this site was part of the first era of colonisation of New Zealand, around 1288–1300 CE. Wairau Bar is a rare example in New Zealand of an early East Polynesian settlement clustered around a central point, and is described as "the type-site of the earliest phase of New Zealand’s prehistory". The Kaikōura coastline was probably visited or occupied around that time. Fire has been a major factor in changing the environment of the Kaikōura region since the time of occupation. In particular, from around the 1860s clearance of land by European settlers has involved repeated burning of high country to enable grazing of sheep.
Protected areas
Protected areas on land The Ka Whata Tu O Rakihouia Conservation Park covers part of the Seaward Kaikōura Range between Kaikōura and Clarence. The area of the park is , representing 43% of the total land area of the Kaikōura District (. The main breeding colony of the endangered Hutton's shearwater is located in the headwaters of the Kowhai River. The area of the colony is protected as the Mount Uwerau Nature Reserve. This is a strict nature reserve of within the Ka Whata Tu o Rakihouia Conservation Park where no public access is permitted.
Kowhai Bush, a reserve on the banks of the Kowhai River and about inland from the Kaikōura Peninsula, has been an important locality for studies of native forest birds. The bush is flat, with a uniform canopy-height. It attracted attention from the New Zealand Wildlife Service in the 1970s, because the bush had an accessible population of South Island robins. These were studied to obtain information that could help with conservation of the endangered Chatham Island black robin. Then, in years and decades following, various post-graduate students from Canterbury University conducted field-work for their post-graduate theses at Kowhai Bush, with the nearby university field station (Edward Percival Marine Laboratory) providing logistical support. The species studied have included riflemen, pīpipi, New Zealand fantails, South Island robins, grey warblers and shining cuckoos.
Blue Duck Scientific Reserve is a scientific reserve, located around north of Kaikōura. It is one of the largest mixed podocarp forests that remain along the entire east coast of the South Island. The importance of the forest was formally recognised in 1903, when was gazetted as a reserve.
The Ō Tamakura Historic Reserve, formerly known as the Goose Bay-Omihi Scenic Reserve, lies to the south of Goose Bay. It contains a coastal forest of beech and podocarps, and adjoins the Ote Makura Scenic Reserve.
Marine protected areas An incorporated society, Te Korowai o Te Tai o Marokura, Kaikōura Coastal Marine Guardians (Te Korowai) was formed in 2005 to develop use and protection strategies and actions for the Kaikōura coast. The work of the society led to the passing of the Kaikōura (Te Tai o Marokura) Marine Management Act in August 2014. This Act established the Kaikōura marine management area, including a new marine reserve, sanctuaries and protections for whales and fur seals, and established new fishing regulations. It also recognised taiapure (traditional Māori fishing grounds which include areas of special cultural or spiritual significance).
The Hikurangi Marine Reserve is a marine reserve off the Kaikōura coast, covering an area of south of the township, and including part of the Kaikōura canyon. The reserve was established in 2014, and is the largest and deepest marine reserve adjacent to any of New Zealand's three main islands. No fishing, harvesting or mining is allowed in the reserve.
The Kaikōura (Te Tai o Marokura) Marine Management Act 2014 established the Te Rohe o Te Whānau Puha Whale Sanctuary covering , and extending north and south of the Kaikōura Peninsula and out to sea, to provide additional protection for marine mammals in this area.
Faunal diversity
Marine mammals A wide variety of marine mammals can be seen in the Kaikōura region, including whales, dolphins, and New Zealand fur seals. The Marine Mammals Protection Act 1978 provides legal protection for these animals, and regulations set conditions that govern human behaviour in the vicinity of marine mammals. Permits are required for commercial tourist operations associated with marine mammals.
New Zealand fur seals The New Zealand fur seal (Arctocephalus forsteri) is found in temperate latitudes around New Zealand and Australia. From the time of arrival of Māori, fur seals were hunted for food. By the time of arrival of Europeans, the breeding range of fur seals was limited to southern parts of the South Island. Large scale commercial harvesting of seals for their skins led to the collapse of the population around the southern parts of New Zealand and outlying islands. The sealing industry closed in 1894.
By the 1950s, fur seals were reported in surveys of the Kaikōura coast, but there was no breeding observed. Fur seals eventually received full legal protection in 1978 with the passing of the Marine Mammals Protection Act. Populations increased significantly, and breeding was reported in the Kaikōura region from around 1990. One of the main breeding areas in the Kaikōura District is north of Kaikōura town at Ōhau Point, where exponential growth of 32% per annum was recorded between 2002 and 2005, and 25% per annum between 2006 and 2009. Fur seals also breed around the Kaikōura Peninsula, and south of the peninsula at Riley’s Lookout / Panau Island. Although accused of impacting commercial fisheries, a 30-year study of the Kaikōura fur seals showed they mostly ate octopus, arrow squid, lanternfish, barracouta, hoki, and āhuru, most of which are not commercial species.
Prior to the 2016 Kaikōura earthquake, a waterfall pool in Ōhau Stream, close to Ōhau Point, was a popular visitor attraction where baby fur seals could be observed in the pool and stream. The section of State Highway 1 at Ōhau Point was badly damaged in the earthquake, and the track to the waterfall pool was closed because of rock falls. In the rebuild of the highway following the earthquake, a car park and lookout was constructed at Ōhau Point where travellers can observe fur seals on the seaward side of the road.
Whales Sperm whales (Physetar macrocephalus) can be observed all year round, most days coming within 10 km of Kaikōura. Sperm whales are deep-water feeders, usually at depths of 1,000 m and up to 3,200 m. The productive cold water upwelling along the Hikurangi Trench is pushed to the surface just off Riley's Rock, a landmark named after Barney Riley, who was a spotter in the early Kaikōura whaling industry and knew this feature marked a whale feeding area.
Stomach contents of over 150 whales caught in the 1960s revealed most of their diet was medium-sized squid, and the rest fish—only one beak from a giant squid was recovered.
A sperm whale's feeding routine consists of 40-minute dives with ten-minute rests in between, during which they are easily observed from boats. Whale watching is a popular tourist attraction for Kaikōura, and an important contributor to the local economy; the town owes its economic resurgence to the presence of sperm whales close to shore.
Adult sperm whales are segregated by sex: nursery groups of females and calves are not found as far south as Kaikōura, so all the sperm whales seen at Kaikōura are males. A survey in 1995 determined two thirds of them were adolescents (aged 10–20), and the rest 25 years or older. Over two hundred individuals have been identified from patterns of nicks and marks on their tail flukes. By 2002, around 80 sperm wales were present in any one summer or winter, some returning repeatedly for years; one first recorded in 1992 was still visiting in July 2006.