Where Māori Came From and When They Arrived in New Zealand
Few peoples on earth have an origin story as well attested, as recently dated, and as scientifically dramatic as Māori. The ancestors of every Māori living today crossed thousands of kilometres of empty ocean to reach the last large landmass on the planet ever to be settled by humans. They came late, they came on purpose, and when they arrived they walked into a Pleistocene relic, a country still ruled by giant flightless birds and the world’s largest eagle. What follows sets out, in as much detail as the current evidence allows, who those ancestors were, where they began their long migration, what route they followed across the Pacific, when they finally reached these shores, in how many waves they came, and what they encountered when they did.
It is a story that runs from the rice-growing villages of Neolithic Taiwan to a windy gravel bar in Marlborough, and it has been pieced together by archaeologists, geneticists, linguists, oral historians, palaeoecologists, volcanologists, and the descendants of the voyagers themselves. The evidence does not always agree at the edges, and where it disagrees that will be said plainly. But the broad outline is now firmer than at any point in the past century, and it is a remarkable thing to be able to tell.
The Deep Origin
To understand where Māori came from, you have to begin a very long way from New Zealand, in latitudes Māori ancestors had not seen for thousands of years by the time their waka first nosed into Hokianga or Wairau. The story does not start in Hawaiki. It starts in Taiwan.
Genetics, linguistics, and archaeology converge on a striking conclusion. The deep ancestry of all Polynesian peoples, including Māori, traces back to the indigenous peoples of Taiwan, with that ancestry stretching back about 5,000 years as part of the larger group of Austronesian peoples. Language-evolution studies and mitochondrial DNA evidence suggest that most Pacific populations originated from Taiwanese indigenous peoples around 5,200 years ago. These Austronesian ancestors moved south to the Philippines, where they settled for some time. From there, some eventually sailed southeast, skirting the northern and eastern fringes of Melanesia along the coasts of Papua New Guinea and the Bismarck Islands to the Solomon Islands, where they again settled, leaving shards of their Lapita pottery behind and picking up a small amount of Melanesian DNA. From there, some migrated down to the western Polynesian islands of Samoa and Tonga.
The Austronesian language family that grew out of this Taiwanese root is now the second largest in the world by geographic spread. It runs from Madagascar off the coast of Africa to Rapa Nui (Easter Island) off the coast of South America, encompassing more than a thousand languages, of which te reo Māori is one of the youngest branches. The deep linguistic kinship is unmistakable. The Māori word for five, rima, is lima in Samoan, lima in Tagalog spoken in the Philippines, and lima in Malagasy spoken in Madagascar. The word for eye, karu or mata in Māori, sits in a tight cousinage with mata across hundreds of Pacific tongues.
The next great archaeological signature of this expansion is the Lapita cultural complex, named after a site in New Caledonia where its distinctive dentate-stamped pottery was first identified. The Lapita people were originally from Taiwan and other regions of East Asia. They were highly mobile seaborne explorers and colonists who had established themselves on the Bismarck Archipelago northeast of New Guinea by 2000 BCE. Beginning about 1600 BCE they spread to the Solomon Islands, they had reached Fiji, Tonga, and the rest of western Polynesia by 1000 BCE, and they had dispersed to Micronesia by 500 BCE. The decorated pots they left behind, broadly similar in vessel form and design from the Bismarcks all the way east to Tonga and Samoa, are the fingerprint of an extraordinary maritime expansion.
In Tonga and Samoa the Lapita people paused. Lapita culture spread into previously uninhabited areas of Remote Oceania, reaching its eastern-most extent in the Tongan and Samoan archipelagos around 2900 to 2750 years before present. There, in the western Polynesian heartland, the elaborate dentate stamping on their pots gradually fell away and was replaced by undecorated wares that archaeologists call Polynesian Plainware. Lapita pottery production appears to have stopped in Samoa by about 2,800 years ago and in Tonga by about 2,000 years ago. This transition is generally taken to mark the emergence of Ancestral Polynesian society, the cultural matrix from which all later Polynesian peoples descend.
For roughly fifteen hundred years after that Tonga and Samoa pause, the eastern Pacific remained empty of human beings. This long stay in western Polynesia is sometimes called the Long Pause, and it is one of the most interesting silences in the prehistory of the world. During those centuries the population of Tonga, Samoa, and the surrounding islands grew, the language family that linguists call Proto-Polynesian developed its characteristic vocabulary and grammar, and the canoe technology, agricultural systems, and navigational knowledge that would later carry people across the world’s largest ocean were perfected.
When the eastern movement finally resumed it did so with extraordinary speed. Some island-hopped eastward, all the way from Ontong Java in the Solomons to the Society Islands of Tahiti and Raʻiātea (once called Havai’i, or Hawaiki). From there, a succession of migrant waves colonised the rest of eastern Polynesia as far as Hawaiʻi in the north, the Marquesas Islands and Rapa Nui (Easter Island) in the east, and lastly New Zealand in the far south. The genetic legacy of this journey is striking. Analysis by Kayser et al. (2008) discovered that only 21 per cent of the Māori-Polynesian autosomal gene pool is of Melanesian origin, with the rest (79 per cent) being of East Asian origin. The brief sojourn in the Bismarcks and Solomons left a small but real Melanesian imprint on the Polynesian genome, but the dominant signal is unmistakably East Asian, written in the DNA of every Māori today.
It is worth pausing on what this all means. Māori are not, as some early European writers fancifully suggested, the remnant of some lost Israelite tribe or a wandering band from South America. They are the southernmost branch of an enormous Austronesian family that began farming rice on Taiwanese hillsides in the late Stone Age and worked its way, generation by generation and island by island, across half the globe. By the time Polynesians stood on the shore of a Tahitian beach looking south into the empty ocean, they were already the inheritors of one of the longest continuous voyaging traditions humanity has ever produced.
Hawaiki and the Last Leg
In Māori tradition the homeland from which the founding waka set out is called Hawaiki. The same word, with small variations, runs through the Polynesian world. It is Havaiʻi in Tahitian, ʻAvaiki in Cook Islands Māori, Savaiʻi in Samoan, and Hawaiʻi in Hawaiian, where it became the name of the largest island in the chain. Hawaiki, in Polynesian folklore, is the original home of the Polynesians, before dispersal across Polynesia. It also features as the underworld in many Māori stories.
Where in the real world was Hawaiki? The answer depends on which Hawaiki you mean, because the word operates on more than one level. In some traditions Hawaiki is perceived to be a physical place from which the Māori people first emerged before arriving in New Zealand. Others associate it with certain compass points, particularly the east, or regard it as an actual island located somewhere in Polynesia. Yet others believe that Hawaiki can be found in New Zealand. All these traditions and versions represent Hawaiki as a special place full of mystical power and regenerating force, the source and origin of life itself.
For the proximate Hawaiki, the place from which the founding waka actually sailed, the convergent evidence points to central East Polynesia, almost certainly the Society Islands and the Cook Islands, with the Southern Cooks and the leeward Society Islands as the most likely staging grounds. Researchers think Hawaiki is a real place, the traditionally important island of Raʻiātea in the Leeward Society Islands (in French Polynesia), which, in the local dialect, was called Havai’i. Raʻiātea was the great religious centre of central East Polynesia, home to the marae of Taputapuātea, which functioned as a kind of pan-Polynesian sanctuary and from which voyaging canoes set out for distant islands. The name Taputapuātea was carried south to New Zealand by the founding waka and survives as a place name in several parts of the country.
Some Māori traditions and some scholars place Hawaiki more specifically in the Southern Cook Islands, particularly Rarotonga. The artist and scholar James Tylor, drawing on a strand of New Zealand Māori thought, writes that for New Zealand Māori people, the actual physical place of Hawaiki is ‘Avaiki Nui (The Cook Islands). Linguistic evidence supports this central East Polynesian location. The Māori language is most closely related to Cook Islands Māori and to the Tahitic group of Polynesian languages, sharing innovations not found in Samoan, Tongan, or Hawaiian. The genetic signal from human remains at the founding settlement of Wairau Bar in Marlborough is consistent with an East Polynesian source population, though it points to a heterogeneous founder group rather than a single home island.
The most likely picture, integrating all of this evidence, is that the immediate Hawaiki of Māori tradition was not one island but a region. The founding canoes drew their crews and provisions from a network of related communities scattered across the Society and Cook Islands, perhaps with some involvement of the Australs and the Marquesas, and they set out from this region in the closing decades of the thirteenth century, riding the seasonal weather windows that briefly made the southern voyage feasible.
The voyage south was not, on any account, a casual drift. Lying in a band of prevailing westerly winds far south of the tropics, New Zealand presented a severe challenge to Polynesian navigators. A good way to reach the country was to sail with easterly tail winds across the top of an anti-clockwise rotating high-pressure system. Early summer, before the cyclone season, is an ideal time to make the journey. Two replica canoes, Hōkūleʻa and Hawaiki nui, did just this in November 1985. The strategy required navigators to sail south-west on a particular weather pattern, slipping across the latitudes where the trade winds give way to the westerlies, and to be confident that something solid lay at the end of the run. Exploring canoes may have followed migrating birds, as told in Māori tradition. The long-tailed cuckoo comes to New Zealand from tropical Polynesia in October, and shearwaters would have been observed flying south in September. People would have known that land lay in that direction, but not how far away it was.
The vessels they sailed in were waka hourua, double-hulled voyaging canoes capable of carrying dozens of people along with the cuttings, seed, and live animals needed to start a new colony. Polynesian wayfinding was used for thousands of years to enable long voyages across the open Pacific. Polynesians made contact with nearly every island within the vast Polynesian Triangle, using outrigger canoes or double-hulled canoes. The double-hulled canoes were two large hulls, equal in length, and lashed side by side. The space between the paralleled canoes allowed for storage of food, hunting materials, and nets when embarking on long voyages. Twentieth century replicas, most famously the Hawaiian Hōkūleʻa and the New Zealand-built Te Aurere, have demonstrated that such craft can cross thousands of nautical miles using only the sun, stars, swells, winds, and bird behaviour as guides. Te Aurere was the first waka hourua in modern times to sail back from Aotearoa New Zealand to the Cook Islands (1992), a key link in the migration path of the Polynesian settlers who came here about 800 years ago.
The navigators who guided these craft worked from a discipline now partially reconstructed but still incompletely understood. In the Pacific, prevailing north- and south-easterly trade winds pushed up swells that remained constant for long periods. Navigators kept their canoes at the same angle to these swells. Sudden changes in canoe motion indicated that it had changed course. To avoid veering off course, a rope was trailed behind the canoe, and if a wave suddenly jarred the vessel, the rope remained true to the original line of travel. Some navigators also lined up their canoe with wind direction, using pennants tied to the mast and rigging as guides. They read the rising and setting points of named stars, the colour of clouds piled over invisible islands, the flight paths of land-resting seabirds returning to roost at dusk, and the deep ocean swells that fan out in predictable patterns from distant landmasses. The Micronesian master navigator Mau Piailug, who taught the modern revival of these skills, summarised the discipline simply. “I have no fear when I am at sea because I have faith in the words of the ancestors. This faith is what we call courage. With this courage you can travel anywhere in the world and not get lost. Because I have faith in the words of my ancestors, I am a navigator. I learned these words when I was a young boy in my father’s canoe.”
When They Came
For most of the twentieth century, the standard textbook answer for when Māori arrived in New Zealand was somewhere between 800 and 1000 AD. That answer is now known to be wrong by several centuries. The chronology of settlement has been one of the most actively debated questions in New Zealand archaeology and the evidence has shifted dramatically since the 1990s.
The current best estimate, supported by multiple independent lines of evidence, places the main settlement in the very late thirteenth or early fourteenth century, with the bulk of the founding population arriving over a relatively short window of decades rather than centuries. Recent discoveries in New Zealand archaeology have overturned long-held views about our past, and especially about the date of Māori settlement. New dating methods now show that the settlement of these islands by Polynesian ancestors of Māori occurred only around 1300 AD, not 800 AD as previously thought. This discovery effectively halved what was already a short pre-contact history, meaning that the dramatic changes to the way of life of the first settlers of New Zealand took place much faster than existing models allowed.
The crucial breakthroughs came from refining radiocarbon dating techniques and from looking at material that records human arrival with very tight resolution. The Pacific rat, Rattus exulans or kiore, was carried to New Zealand by Polynesian settlers and could not have arrived any other way. By radiocarbon dating the bones of the earliest kiore and the gnaw-marks they left on seeds, researchers could fix the moment when humans first stepped ashore. The answer was consistent. The earliest reliable kiore-gnawed seeds and earliest kiore bones cluster tightly around 1280 to 1300 AD.
A second independent line of evidence comes from a volcano. Mount Tarawera in the Bay of Plenty erupted in the early fourteenth century, laying down a layer of ash, the Kaharoa Tephra, across much of the upper North Island. The Kaharoa eruption occurred at Mt Tarawera in the winter of 1314 AD plus or minus 12 years, dated by counting the rings on a piece of celery pine killed by the blast. This rhyolitic eruption from Tarawera Volcano in AD 1314 provides an important datum because Polynesian artefacts first occur above this ash layer. Below the ash, almost nothing of human origin. Above it, an explosion of charcoal, burnt stumps, archaeological sites, and artefacts. The ash is a knife-edge boundary between an empty country and an inhabited one.
A third line of evidence comes from the vegetation itself. Lake sediment cores from the North and South Islands show a sudden, sustained spike in charcoal particles and a collapse in forest pollen at almost exactly the same time. The forests that had stood undisturbed for tens of thousands of years began to burn, on a continental scale, in the late thirteenth and early fourteenth centuries.
A fourth line, from the archaeology of human settlement itself, agrees. The Wairau Bar site in Marlborough is the most thoroughly studied early settlement in the country and is widely regarded as a founding-phase village. Radiocarbon dates indicate that Wairau Bar was inhabited during the earliest settlement of New Zealand, around the end of the 13th century AD. Covering at least 11 hectares, Wairau Bar is best known for its numerous burials and rich assemblage of grave goods, which include artefacts of Archaic East Polynesian type, such as distinctive jewellery, as well as the eggs and bones of the extinct flightless moa. The artefacts at Wairau Bar are not a New Zealand culture, they are a tropical East Polynesian culture, sitting incongruously on a southern beach. The people buried there grew up somewhere else and ended their lives here.
A fifth line, from oral tradition, is also broadly consistent. This scenario is also consistent with a much debated third line of evidence, traditional genealogies (whakapapa) which point to 1350 AD as a probable arrival date for many of the founding canoes (waka) from which many Māori trace their descent. Working back from the present at roughly twenty-five years a generation, the foundational ancestors named in the canoe traditions sit comfortably in the late 1200s and 1300s. This is a genuinely independent calibration, gathered for entirely different reasons by entirely different people, and it lands within decades of the radiocarbon and tephra dates.
The synthesis of all of this evidence is clean and now widely accepted. The most recent synthesis of archaeological and genetic evidence concludes that, whether or not some settlers arrived before the Tarawera eruption, the main settlement period was in the decades after it, somewhere between 1320 and 1350 CE, possibly involving a coordinated mass migration. Some researchers leave open the possibility of a small earlier exploratory presence in the late 1200s, perhaps the historical kernel of Kupe traditions, but the demographic settlement, the moment when New Zealand became a populated country rather than a place humans had touched, falls in the first half of the fourteenth century.
A note on the “mass migration” framing is worth making here, because it is one of the more interesting recent shifts in the field. For most of the late twentieth century, archaeologists tended to picture settlement as a slow trickle of small founding parties followed by gradual demographic growth. Recent work reintroduces the concept of mass migration into debates concerning the timing and nature of New Zealand’s settlement by Polynesians. Upward revisions of New Zealand’s chronology show that the appearance of humans on the landscape occurred extremely rapidly, and that within decades settlements had been established across the full range of climatic zones. The rapid appearance of a strong archaeological signature in the early 14th century AD is the result of a mass migration event, not the consequence of gradual demographic growth out of a currently unidentified earlier phase of settlement. Mass migration is not only consistent with the archaeological record but is supported by recent findings in molecular biology and genetics. It also opens the door to a new phase of engagement between archaeological method and indigenous Māori and Polynesian oral history and tradition.
What this means in plain language is that the founding population of New Zealand was probably not a few dozen castaways. It was hundreds, perhaps low thousands, of people, arriving on multiple voyages over a few decades, organised enough to seed settlements from Northland to Foveaux Strait inside a few generations. While archaeological research has refined the timeframe that the first waka might have landed on Aotearoa sands, from 1000 years ago to 750, we can thank mtDNA evidence for transforming our understanding of the number of colonists that came. The figure has jumped dramatically from between 70 and 90 women to many hundreds, and perhaps even more than 1000. This is not a story of accidental drift. It is a story of deliberate, large-scale, coordinated colonisation, undertaken by people who knew what they were doing and what they were looking for.
How Many Waves
The question of how many waves of migration brought Māori to New Zealand has been debated for more than a century, and along the way it has produced one of the most influential and most thoroughly debunked stories in New Zealand history. To understand the current view, you have to know where the older view came from and why it is no longer believed.
For most of the twentieth century, the standard story taught in New Zealand schools was the so-called Great Fleet. According to this account, the Polynesian explorer Kupe discovered an uninhabited New Zealand in around 925 AD, returned home to tell of it, and centuries later, in 1350 AD, a fleet of seven named canoes set out together from central Polynesia and arrived in New Zealand to found the iwi we know today. Smith used the Fornander method and combined disparate traditions from various parts of New Zealand and other parts of Polynesia to derive the “Great Fleet” hypothesis. Through an examination of the genealogies of various tribes, he came up with a set of precise dates for the Great Fleet and the explorers that he and others posited as having paved the way for the fleet. Smith’s account went as follows. In 750 CE the Polynesian explorer Kupe discovered an uninhabited New Zealand. Then in 1000–1100 CE, the Polynesian explorers Toi and Whātonga visited New Zealand, and found it inhabited by a primitive, nomadic people known as the Moriori. Finally, in 1350 CE a ‘great fleet’ of seven canoes, Aotea, Kurahaupō, Mataatua, Tainui, Tokomaru, Te Arawa and Tākitimu, all departed from the Tahitian region at the same time, bringing the people now known as Māori to New Zealand.
This story, in something like the form just summarised, was repeated in school journals, museum displays, and government publications for the better part of seventy years. The problem is that almost none of it survives contact with the actual evidence.
The Great Fleet narrative was the work of the colonial-era ethnologist Stephenson Percy Smith, working with the Māori scholar Hoani Te Whatahoro Jury, in the late 1800s and early 1900s. Smith obtained details about places in Rarotonga and Tahiti during a visit in 1897, while Jury provided information about Māori canoes in New Zealand. Smith then ‘cut and pasted’ his material, combining several oral traditions into new ones. The historian Rawiri Taonui has put the criticism more bluntly, calling the result a falsification produced by stitching together disparate iwi traditions into a single national myth. The Great Fleet scenario won general acceptance, its adherents including the respected Māori ethnologist Te Rangi Hīroa (Sir Peter Buck), and it was taught in New Zealand schools. However, it was effectively demolished during the 1960s by the ethnologist David Simmons, who showed that it derived from an incomplete and indiscriminate study of Māori traditions as recorded in the 19th century. Simmons also suggests that some of these “migrations” may actually have been journeys within New Zealand.
Simmons’s critique, set out in detail across the 1960s and 1970s, was devastating. He went back to the original nineteenth century manuscripts and the recorded whaikōrero of Māori elders and found that the great fleet of seven canoes setting off together from Raiatea did not exist in the old manuscripts nor in the whaikōrero of learned men. Bits and pieces there were. Kupe was and is known, in the traditions of the Hokianga, Waikato, East Coast and South Island, but the genealogies given did not tally with those given by S. Percy Smith. The stories given by Smith were a mixture of differing tribal tradition. In other words the whole tradition as given by Smith was Pākehā, not Māori. Learned men of the same tribe make no mention of this story and there are no waiata celebrating their deeds. Tribal origin canoes are well known to the tribes belonging to them, but none of them talk as Smith did of six large sea-going canoes setting out together from Raiatea.
What the actual iwi traditions describe is something quite different and much richer. It was once believed that the ancestors of Māori came to New Zealand in a single ‘great fleet’ of seven canoes. We now know that many canoes made the perilous voyage from Polynesia. Through stories passed down the generations, tribal groups trace their origins to the captains and crew of more than 40 legendary vessels, from Kurahaupō at North Cape to Uruao in the South Island. Rich in conflict and drama, and blending history and symbolism, these canoe traditions form a founding narrative for Māori New Zealanders.
The waka named in tribal traditions arrived at different times, from different places, and made landfall at different points around the country. Tainui made landfall in the Bay of Plenty before working its way up the Coromandel coast, into the Hauraki Gulf, and eventually to Kāwhia on the west coast, where its crew settled and seeded the iwi of the Tainui confederation. Te Arawa came in to the Bay of Plenty under the captaincy of Tama-te-kapua and gave its name to the iwi of Rotorua and the surrounding inland country. Mātaatua landed at Whakatāne. Aotea, captained by Turi, came down the west coast of the North Island and settled at Pātea, where Kupe was said to have planted karaka seeds long before. Kurahaupō broke up at sea and its crew were distributed across several waka. Tākitimu followed the east coast south, naming features as it went, before its remains were said to have been turned to stone in Southland as the Takitimu Mountains. Tokomaru landed in north Taranaki. Horouta worked the East Coast. Ngātokimatawhaorua, the canoe of Nukutawhiti, came into the Hokianga and seeded the Ngāpuhi peoples of the north. Uruao made it to the South Island. Many others are remembered in regional traditions.
These canoes do not arrive together. They are not even all from the same place. Recent research appears to confirm that the “Great Fleet” of Māori tradition is a myth coined by European Māori-phils in the generation after the Maori Wars. The myth, which arose out of popular scholastic attempts to systematise conflicting tribal arrival-traditions, gained wide acceptance owing to its simplicity. A re-examination of the legends shows that, far from there having been a large fleet of canoes, those which reached New Zealand came at irregular intervals during the 300 or so years following Kupe.
The current best picture, integrating tradition and archaeology, is therefore something like this. The proper answer to “how many waves” is “many”, spread across a relatively concentrated period of probably less than a century, beginning in the late 1200s and continuing through the 1300s and into the 1400s. There is no single founding fleet. There is no neat sequence of three migrations. There is, instead, a pulse of voyaging, drawing on multiple home communities in central East Polynesia, sending dozens of canoes south on the seasonal weather windows, with most of those canoes arriving inside the first few generations of the colonisation period and the trickle slowing to almost nothing by the early 1400s.
After about 1450 the voyaging effectively stopped. New Zealand’s connection to the wider Polynesian world fell silent. The original Polynesian settlers discovered the country on deliberate voyages of exploration, navigating by making use of prevailing winds and ocean currents, and observing the stars. The navigator credited in some traditions with discovering New Zealand is Kupe. Some time later the first small groups arrived from Polynesia. Now known as Māori, these tribes did not identify themselves by a collective name until the arrival of Europeans, when, to mark their distinctiveness, the name Māori, meaning ‘ordinary’, came into use. Although New Zealand has abundant clay deposits, Māori people did not make pottery. The absence of pottery is itself a clue. The new arrivals came from a pottery-making tradition (Lapita and its descendants), but in New Zealand the craft was abandoned within a generation or two, probably because the colder climate killed the tropical crops that had been stored in pots and the cooking technology shifted to the earth oven.
The discontinuation of the long-distance voyaging is one of the more poignant facts of New Zealand history. The same techniques that brought the founding canoes here did not, on any scale, return Māori to Hawaiki. New Zealand became its own world.
A handful of figures stand out from the canoe traditions and deserve a note of their own. The first is Kupe, whom many iwi credit as the original discoverer of Aotearoa. He was born in the geographically uncertain Māori homeland of Hawaiki, to a father from Rarotonga and a mother from Raiatea, between 23 and 40 generations ago, and probably spoke a Māori proto-language similar to Cook Islands Māori or Tahitian. The story of his voyage, in the version most commonly told, has him pursuing a giant octopus, Te Wheke-a-Muturangi, that had been raiding his fishing grounds in Hawaiki. The wheke belonged to Kupe’s rival Muturangi, and Kupe chased it across the Pacific until he ran it down in the waters between the North and South Islands of New Zealand.
The name of the country itself comes from this voyage. It is said that his wife, Kuramārōtini, devised the name of Ao-tea-roa (‘long white cloud’) on seeing the North Island for the first time. Like Māui before him, Kupe’s arrival is a foothold in the land for Māori. His adventures took place predominantly in the south Wairarapa, Cook Strait and Northland regions. Kupe is associated with place names from Hokianga in the far north, where he first made landfall, to Wellington and the Marlborough Sounds, where he fought and killed the wheke. Most traditions name his canoe Matawhaorua or Matahorua, although some say these were different canoes. In all of them he is credited with “dividing the land” or “cutting the land in half”, a reference to his journeying through Raukawa Moana (Cook Strait) as he explored the coastline.
What is unusual about Kupe in the iwi traditions is that, in most accounts, he did not stay. He returned to Hawaiki, told his people of the new land, and never came back. The very last thing he is said to have declared, on departing the Hokianga, was “e kore e hokianga mai”, “I shall never return,” and from that statement, in the traditional account, the harbour took its name.
There are, importantly, regional differences in how Kupe is remembered. The three regions where the Kupe traditions are strongest are Heretaunga (Hawkes Bay), Raukawa Moana and Te Tai ō Aorere (Cook Strait and Tasman Bay) and Te Tai Tokerau (Northland). Some Northland traditions place Kupe as a contemporary of, but slightly older than, Nukutawhiti, the ancestor of Ngāpuhi, rather than as a figure from centuries earlier. The “hundreds of years before the canoes” version of Kupe was largely a creation of Smith’s synthesising work and is not a reliable feature of the original iwi accounts. In the iwi accounts that pre-date Smith, Kupe is a contemporary, or near-contemporary, of the other founding ancestors. This sits comfortably with the radiocarbon evidence that puts all of the founding-period activity in a relatively narrow window of decades.
The waka named in iwi tradition are not, on the modern reading, neat sequential waves. They are individual journeys, undertaken across a few generations, each remembered in detail by the descendants of those who travelled aboard. The iwi who descend from Tainui, Te Arawa, Mātaatua, Tākitimu, Aotea, Tokomaru, Kurahaupō, Horouta, Ngātokimatawhaorua and the rest do not see themselves as branches of a single founding event. They see themselves as the descendants of many founding events, related but distinct, each with its own history and its own ancestors.
What Was Already Here
When Māori ancestors stepped ashore in the early 1300s, the country they walked into was unlike anywhere else on earth. New Zealand had been geographically isolated for around eighty million years, ever since it broke away from the supercontinent of Gondwana. In that long isolation, in the absence of any land mammals other than three species of small bat, the islands had filled with birds. Birds occupied the niches that mammals occupied elsewhere. They became the grazers, the browsers, the predators, and the scavengers. They lost their wings, grew to extraordinary sizes, and evolved into forms that have no parallel anywhere else.
The dominant herbivores of the country, the closest thing it had to deer or cattle or kangaroos, were the moa. Before the arrival of humans, the moa’s only predator was the massive Haast’s eagle. New Zealand had been isolated for 80 million years and had few predators before human arrival, meaning that not only were its ecosystems extremely vulnerable to perturbation by outside species, but also the dominant herbivores in New Zealand’s forest, shrubland, and subalpine ecosystems until the arrival of the Māori, were hunted only by Haast’s eagle. These included nine species of moa that ranged in size from the turkey-sized small bush moa to the 250 kg giant moa. The largest moa, the South Island giant moa, Dinornis robustus, stood up to 3.6 metres tall when fully extended and could weigh more than a fully grown red deer. The smallest, the bush moa, was about the size of a turkey. They were flightless, they had no wings at all, not even vestigial bones, and they lived in habitats from coastal forest to high alpine tussock.
Above the moa flew the largest eagle the world has ever known. At the top of the food chain was the extinct Haast’s eagle, Harpagornis moorei. H. moorei (10–15 kg, 2–3 m wingspan) was 30%–40% heavier than the largest extant eagle (the harpy eagle, Harpia harpyja), and hunted moa up to 15 times its weight. In a dramatic example of morphological plasticity and rapid size increase, H. moorei was very closely related to one of the world’s smallest extant eagles, which is one-tenth its mass. This spectacular evolutionary change illustrates the potential speed of size alteration within lineages of vertebrates, especially in island ecosystems. Haast’s eagle was an apex predator capable of striking moa weighing 200 kilograms or more, killing them with the impact of its dive. Some palaeontologists have speculated, on the basis of the eagle’s size and Māori oral references to a giant raptor, that it would have been capable of killing a child. There is no archaeological evidence that it ever did, but the eagle’s anatomy makes the possibility uncomfortably plausible. The Māori names pouākai and hōkioi, both linked in tradition to a great bird now lost, are usually identified with this species.
The forests below were full of other birds now extinct or critically endangered. The huia, with its sexually dimorphic beak (the male’s short and chisel-like, the female’s long and curved) and its glossy black tail tipped with white. The piopio, an endemic thrush. The South Island kōkako and its surviving North Island cousin. The takahē, a large flightless rail thought extinct for half a century until its rediscovery in the Murchison Mountains in 1948. The kiwi, in five species, snuffling through the leaf litter at night. The kākāpō, a large flightless nocturnal parrot that climbs trees and booms its mating call from carved bowls in hilltops. The weka, the pūkeko, the kererū. The forest floor was densely populated with ground-foraging insectivores, and the canopy thrummed with nectar feeders.
Around the coast, the seas were thick with marine life. The coast and marine environment supported large populations of seabirds, seals and whales. Fur seals and sea lions hauled out on beaches the length of both islands. Southern right whales calved in sheltered bays from the Bay of Islands to Foveaux Strait. Elephant seals, now confined almost entirely to the subantarctic islands, may have been more widespread on the mainland coast. The skies above the open ocean were dense with seabirds whose like is hard to imagine today, vast colonies of petrels and shearwaters and albatrosses on every offshore island and many headlands of the mainland.
There were three species of native frog of an extremely ancient lineage, frogs that do not croak and that hatch from the egg as miniature adults rather than as tadpoles. There were the tuatara, the only surviving member of the order Rhynchocephalia, a reptile lineage that diverged from snakes and lizards over 220 million years ago and has otherwise been extinct since the time of the dinosaurs. There were several species of geckos and skinks. There were giant insects, including the enormous wētā punga, fist-sized crickets that filled the role taken on continents by rats and mice. There were no land snakes. There were no land mammals other than two species of bat. There were no land predators larger than a hawk.
The vegetation that supported all of this was a temperate rainforest of extraordinary antiquity. From 65 million years ago, the landmass was inhabited by species that were originally from Gondwana. Some of them were beech trees, ferns, kiwi, moa, tuatara, and wētā. The forests of the cool south were dominated by southern beech, Nothofagus, a Gondwanan genus shared with the temperate forests of Patagonia and Tasmania. The warmer north grew a podocarp-broadleaf forest of kauri, rimu, tōtara, mataī, miro, kahikatea, pūriri, and tawa, draped with vines, perched with epiphytes, and full of tree ferns. The wetlands were forests of kahikatea standing in shallow water. The coasts grew pōhutukawa and karaka. The alpine zones above the bushline supported a flora as endemic and unusual as the fauna, with cushion plants, vegetable sheep, and the giant Mount Cook lily.
This was the country Māori ancestors stepped into. There was nothing else here. The clear archaeological consensus is that there was no pre-Polynesian human population. No credible evidence exists of pre-Māori settlement of New Zealand. On the other hand, compelling evidence from archaeology, linguistics, and physical anthropology indicates that the first settlers migrated from Polynesia and became the Māori. The various claims that have circulated in popular literature over the years, of Celts, Phoenicians, Egyptians, Sri Lankans, or assorted other pre-Māori arrivals, have not survived scrutiny. The structures and artefacts variously offered as proof have, on examination, turned out to be either natural geological features or post-1840 European constructions. A feature that has been put forward as evidence of pre-Polynesian settlers is the Kaimanawa Wall, which some claim is a remnant of ancient human construction that the Māori could not have built because they did not build with stone in such a way. The wall formation was inspected by an archaeologist and a geologist. Neither saw evidence of a human origin and they concluded the formation is a natural ignimbrite outcrop formed 330,000 years ago.
The other version of the pre-Māori claim, that there was an earlier “Moriori” people in New Zealand whom Māori displaced, was a Victorian-era fabrication closely tied to the Great Fleet myth and to colonial-era arguments that Māori were themselves only the latest of a sequence of conquering races. The Moriori are real, but they are the descendants of people who left mainland New Zealand for the Chatham Islands in the fifteenth century and developed a distinctive culture there. They were never a separate pre-Māori people on the mainland. We will return to them shortly.
The Founding Generations
The first generations to live in New Zealand are known to archaeologists as the Archaic phase, sometimes called Archaic East Polynesian, sometimes called the moa-hunter culture. Early Māori history is often divided into two periods, the Archaic period (c. 1300 to c. 1500) and the Classic period (c. 1500 to c. 1769). Archaeological sites such as Wairau Bar show evidence of early life in Polynesian settlements in New Zealand. Many crops the settlers brought from Polynesia did not grow well in the colder New Zealand climates. However, many native bird and marine species were hunted or collected for food, with some birds hunted to extinction.
The cultural toolkit of the Archaic was unmistakably tropical East Polynesian. The fishing hooks, adzes, ornaments, and burial practices found at Wairau Bar and contemporary sites have direct parallels in the Society Islands, the Cook Islands, and the Marquesas. The first New Zealanders were, materially and culturally, Polynesians who had not yet had time to become anything else. They wore the same kinds of necklaces, used the same kinds of fish hooks, and arranged their dead in the same kinds of burials as their cousins on tropical islands thousands of kilometres to the north.
The land itself, however, was an unfamiliar problem. The crops the founding canoes had brought (taro, yam, gourd, paper mulberry, and most importantly the South American sweet potato, kūmara) were tropical plants. They struggled and largely failed in the colder New Zealand climate. Coconut, a Polynesian staple, simply would not grow. Breadfruit could not survive at all. The pig and the chicken, both standard Polynesian domesticates, did not make it across the long voyage south or did not survive the early years. The dog, the kurī, did, and so did the kiore, the Pacific rat, but everything else had to be replaced from local resources.
What the country offered instead was meat on a scale tropical Polynesians had never seen. The moa were the obvious resource. They were big, slow, calorific, defenceless against humans, and they had no behavioural repertoire for evading a primate predator because they had never had to develop one. The first New Zealanders ate moa systematically, and the archaeological signature of that exploitation is enormous. Estimates of the number of individual moa remains in 1,200 open ovens and middens surveyed in the vicinity of the Waitaki River mouth during the 1930s range from 29,000 to 90,000.
A site at the mouth of the Waitaki River in the South Island is the largest moa-hunting station ever found. Waitaha Māori ventured deep into the remote interior to harvest moa, transporting them down the river on rafts (mōkihi) made from raupō and flax. Over 1200 ovens for cooking moa flesh were excavated at the Waitaki River mouth, the biggest moa-hunter archaeological site in New Zealand.
The moa did not last. The latest and now generally accepted view is that, as part of the greater Quaternary ‘overkill’, an extremely low-density population of first New Zealand settlers wiped out the entire population of moa on the islands in a period of less than 150 years, which would coincide with 1400 to 1450 CE. This rapid megafaunal extinction is evidenced by high-quality radiocarbon dates on moa remains from natural and archaeological sites. The moa had relatively low reproduction rates and older ages of sexual maturity, making them vulnerable to extinction via predation. A recent collaborative analysis of ancestral sayings suggests that early Māori used the moa as a metaphor for extinction, e.g. ‘lost as the moa is lost’, similar to the English phrase ‘dead as a dodo’.
The phrase kua ngaro i te ngaro o te moa, “lost as the moa is lost”, entered Māori proverbial speech as a way of describing something gone forever. Moa extinction occurred within 100 years of human settlement of New Zealand, primarily because of overhunting. The word moa is a Polynesian term for domestic fowl. The name was not in common use among the Māori by the time of European contact, likely because the bird it described had been extinct for some time. Nevertheless, knowledge was passed down through traditional stories and proverbs.
The disappearance of the moa took the Haast’s eagle with it, since the eagle had no other prey base sufficient to support a bird of its size. The fur seal colonies on the North Island and the upper South Island were largely driven into extinction or pushed into refuges in the deep south. Ground-nesting bird colonies collapsed. Many species of duck, rail, and goose, evolved in the absence of mammalian predators, were driven to extinction by hunting and by predation from the kiore. Forests that had stood since the last ice age were burned to clear land for kūmara cultivation and to drive game. The human signature on the New Zealand environment, in the first two centuries of occupation, was as drastic as anything humans have ever done to a previously unpeopled landscape.
In response to the collapse of the megafauna and to the cooling that came with the Little Ice Age from around 1450, the founding culture changed. People moved away from the southern moa-hunting bases. Permanent settlements concentrated in the warmer north, where kūmara could be grown reliably and stored through the winter in carefully constructed pits. The diet shifted to a broader base of fish, shellfish, fern root, kūmara, taro, and small forest birds. The material culture diverged steadily from its tropical origins. New tools, new ornaments, new building styles emerged. Pottery, never very developed in the founding generation, disappeared entirely. By around 1500, what archaeologists call the Classic Māori period had taken shape.
The Classic Māori World
The Classic Māori culture that developed from around 1500 onwards was unmistakably the product of the New Zealand environment. Factors that operated in the transition to the Classic period (the culture at the time of European contact) include a significantly cooler period from 1500, and the extinction of the moa and of other food species. The Classic period is characterised by finely made pounamu (greenstone) weapons and ornaments, elaborately carved war canoes and wharenui (meeting houses). Māori lived in autonomous settlements in extended hapū groups descended from common iwi ancestors. The settlements had farmed areas and food sources for hunting, fishing and gathering. Fortified pā were built at strategic locations due to occasional warfare over wrongdoings or resources, and this practice varied over different locations throughout New Zealand, with more populations in the far north. In the course of a few centuries, the growing population led to competition for resources and an increase in warfare and an increased frequency of fortified pā.
Settlement clustered most heavily in the warmer parts of the country, north of a line through about Banks Peninsula. The South Island, particularly its colder and wetter parts, remained sparsely populated by tribal groups (Waitaha, Ngāti Mamoe, and later Ngāi Tahu) who relied more heavily on seasonal mobility, on muttonbirding and fishing, and on the trade in pounamu (greenstone) extracted from the rivers of the West Coast. Pounamu became one of the most valuable items in the Māori economy, traded the length of the country for its hardness and beauty, used for adzes, weapons, and ornaments including the iconic hei tiki.
The political unit of the Classic Māori world was the hapū, a kinship group descending from a named ancestor and operating with substantial autonomy under the leadership of a rangatira. Hapū combined into larger iwi confederations, and individual people could trace lineage to multiple iwi through their parents and grandparents. Land was held collectively by the hapū. Authority was based on whakapapa, on demonstrated ability, and on the spiritual concept of mana, a quality of effective presence in the world that flowed from one’s ancestors and that could be enhanced or diminished by one’s own actions.
Warfare was a regular feature of life. The fortified pā, hilltop or headland settlements protected by terraces, palisades, and ditches, became one of the defining features of the New Zealand landscape. Archaeological evidence indicates that Māori began constructing pā around AD 1500, coinciding with population expansion and the intensification of inter-group conflict following initial settlement in the 13th–14th centuries. Radiocarbon dating of palisade posts and associated features from sites across New Zealand supports this timeline, with fortifications appearing in response to resource pressures from growing communities reliant on kūmara cultivation and territorial control. Prior to this, early Māori settlements consisted of unfortified kāinga, reflecting a period of exploration and adaptation without widespread defensive needs.
Pā are mainly in the North Island of Aotearoa New Zealand, north of Lake Taupō. Most pā sites are found in the North Island, especially north of Lake Taupō. Over 5,000 pā sites have been found and studied. No pā have been found from the very early days when Polynesian-Māori settlers first arrived in the lower South Island. Similar types of fortified settlements can be found in other parts of central Polynesia, like Fiji, Tonga, and the Marquesas Islands.
The construction of pā was a significant labour investment, sometimes representing months or years of communal earthworking. The ditches and ramparts of the largest sites are still visible from the air across much of the upper North Island, hundreds of years after they were last defended. They speak to a society in which competition for fertile land, productive fishing grounds, and prestige was intense and sometimes violent, but also one in which collective effort could be mobilised on a substantial scale.
By the time the first Europeans arrived in the seventeenth and eighteenth centuries, the Māori population was probably somewhere between 100,000 and 200,000 (estimates vary considerably), distributed across dozens of iwi and hundreds of hapū, occupying a country whose every harbour, river mouth, headland, and forest was named, known, and accounted for in whakapapa.
The Chathams and the Moriori
A footnote to the main story, though an important and often misunderstood one, concerns the Chatham Islands and the Moriori. The Chathams (Rēkohu in the Moriori language, Wharekauri in te reo Māori) lie about 800 kilometres east of the New Zealand mainland. They are the easternmost outpost of the broader settlement of Aotearoa.
The Moriori are the first settlers of the Chatham Islands. They are Polynesians who came from the New Zealand mainland by at least about 1500 AD, and possibly around the mid-15th century. The settlers’ culture diverged from mainland Māori, and they developed a distinct Moriori language, mythology, artistic expression and way of life.
The point that bears emphasising, because the older literature got it badly wrong, is that the Moriori are not pre-Māori. They are not a separate or earlier people. They share the same ancestry and the same founding population as mainland Māori, and their language is more closely related to te reo Māori than to any other Polynesian language. The Moriori are descended from the East Polynesians who settled New Zealand and from whom the Māori also descended. A group of New Zealand Polynesians migrated from mainland New Zealand to the Chatham Islands. Traditions of Moriori genealogy and some features of artefacts suggest that some arrivals may have come directly to the Chatham Islands from East Polynesia. The Chathams are no further from Rarotonga than the Coromandel coast is, and it is possible that they were settled separately during the Polynesian exploration of the South Pacific, with most of the immigrants coming from New Zealand later. It is clear from artefacts and linguistic evidence that the final migration was from New Zealand.
Once on Rēkohu, the Moriori found a colder and harsher environment than even southern New Zealand. The kūmara would not grow there. Their economy turned to fishing, sealing, fowling (especially albatross harvesting on offshore islets), and the gathering of fern root and karaka berries. The population grew to around 2,000 across nine tribes and developed its own distinctive culture, including the famous Nunuku’s Law, a covenant of non-violence introduced by the chief Nunuku-whenua in the sixteenth century after a period of inter-tribal conflict.
The story of how the older “pre-Māori Moriori” myth came about is itself a chapter in the misuse of history. Based on the writing of Percy Smith and Elsdon Best from the late 19th century, theories grew up that the Māori had displaced a more primitive pre-Māori population of Moriori (sometimes described as a small-statured, dark-skinned race of possible Melanesian origin) in mainland New Zealand, and that the Chatham Island Moriori were the last remnant of this earlier race. These theories also favoured the supposedly more recent and more technically able Māori. This was used to justify racist stereotyping, colonisation, and conquest by cultural “superiors”. From the view of European settlers this served the purpose of undermining the notion of the Māori as the indigenous people of New Zealand, making them just one in a progression of waves of migration and conquest by increasingly more civilised people.
The myth was discredited by professional anthropologists across the twentieth century, but it lingered in popular consciousness and in school curricula for decades. The Moriori themselves suffered terribly when in 1835 two Taranaki iwi, Ngāti Mutunga and Ngāti Tama, displaced from their own homeland during the Musket Wars, invaded the Chathams aboard a British whaling vessel. The Moriori, holding to Nunuku’s Law, did not fight back. The result was one of the worst genocides, by proportional toll, in recorded history. The injustice was eventually formally acknowledged by the Crown. In February 2020, the New Zealand government signed a treaty with tribal leaders, giving them rights enshrined in law and the Moriori people at large an apology for the past actions of Māori and European settlers.
The Moriori today number a few thousand, a culture and a people in active revival.
The South American Question and Other Contacts
A final piece of the puzzle, often overlooked in the standard story, concerns the eastern boundary of Polynesian voyaging and what it tells us about the wider context of Māori arrival.
The kūmara, the sweet potato that Māori brought with them on the founding canoes and that became the most important cultivated staple in the New Zealand diet, is not a Polynesian plant. It is South American. Ipomoea batatas was domesticated in the western Andes thousands of years ago. Its presence in pre-European Polynesian agriculture, all the way from Hawaiʻi to New Zealand, is one of the best-supported pieces of evidence for direct human contact between Polynesia and the Americas before Columbus.
Its presence in precontact archaeological sites scattered throughout Polynesia has long been considered as direct evidence for prehistoric contact between Polynesia and America. The lexical similarity between terms for sweet potato in Polynesian languages (“kuumala” and its derivatives) and the terms for this plant (“kumara,” “cumar,” or “cumal”) found among Quechua speakers of northwestern South America supports the hypothesis that humans introduced sweet potato from South America to Polynesia.
Recent genetic research provides strong support for the tripartite hypothesis, notably concerning the Kumara line, the pre-Columbian diffusion of sweet potatoes from South America (the Peru–Ecuador area) into Polynesia. The Polynesian word kumara and its variants almost certainly derive from the Quechua cumar or cumal, a borrowing that requires direct human contact between Polynesian voyagers and South American populations sometime before 1300 AD.
The implications are significant. The Polynesian voyaging tradition that brought Māori ancestors to New Zealand also reached, at some point, the western coast of South America, picked up the sweet potato, and brought it back. Whether the contact was a single Polynesian round trip or a more sustained interaction, and whether any South American crews ever travelled westward, is unresolved. But the fact of the contact itself is now well established by genetics, by linguistics, and by archaeological dating of kūmara remains in eastern Polynesia. Analysis of historically collected samples seemingly confirms the hypothesis that kumara lineages were introduced to the eastern Pacific by Polynesian voyagers, which archaeological evidence indicates occurred by approximately A.D. 1200 to 1300.
The kūmara that Māori grew at Pātea and Kāwhia and Hauraki, and that was carried as far south as the Otago coast in carefully built storage pits, is a direct living link to that ancient encounter on the South American shore. By about 1300 CE, the first human settlers had transferred ancestral Ipomoea batatas cultivation to the new country, and it remained a staple of the Māori economy until the introduction of the European white potato transformed New Zealand horticulture in the nineteenth century.
There were no further outside contacts with Aotearoa, after the closing of the long voyaging tradition around 1450, until the Dutch navigator Abel Tasman sighted the West Coast of the South Island in December 1642. Tasman’s brief and bloody encounter with Ngāti Tūmatakōkiri at what he named Murderers Bay (now Golden Bay) ended without him ever setting foot on land. He sailed on, naming the country Staten Landt in the belief it might be connected to a similarly named landmass off South America, before Dutch cartographers later renamed it Nieuw Zeeland. It would be another 127 years before James Cook’s Endeavour arrived in 1769 and the country’s long isolation from the wider world finally ended.
By that point Māori had been alone in Aotearoa for around fourteen generations. The country they presented to Cook and his crew, with its carved meeting houses, its terraced pā, its painted canoes, its complex kinship system and rich oral literature, was a Polynesian civilisation utterly distinct from any other, the southernmost flowering of the great Austronesian expansion that had begun in Taiwan five thousand years before.
A Story Still Being Written
The deep ancestry of Māori traces, through the Lapita pottery makers of the western Pacific, to the Austronesian-speaking peoples of Neolithic Taiwan around 5,000 years ago. Their immediate ancestors paused in western Polynesia, in Tonga and Samoa, for roughly 1,500 years, and then resumed an eastward expansion that took them through the Cook and Society Islands and from there, around the late 1200s and early 1300s, on the final southward run to Aotearoa. The voyage was deliberate, undertaken in double-hulled waka hourua by skilled navigators using a sophisticated body of practical knowledge about stars, swells, winds, and birds. Hawaiki, the homeland from which the founding canoes set out, was almost certainly a region in central East Polynesia, with Raʻiātea in the leeward Society Islands and the Southern Cook Islands as the strongest single candidates.
The arrival came late, by world standards. New Zealand was the last large landmass on earth to be settled by humans, and by the time the founding canoes made landfall, agriculture had been practised in the Middle East for around nine thousand years and the cathedrals of medieval Europe were already standing.
The number of waves was many, not three and not seven. The old Great Fleet story is a Victorian fabrication built by stitching together fragments of inconsistent regional traditions into a single neat narrative. The actual iwi traditions describe more than forty named waka, arriving at different times across a few generations, from different parts of central East Polynesia, making landfall at different places around the country. The bulk of the founding population probably arrived in a relatively concentrated pulse between about 1280 and 1350, and the long-distance voyaging effectively ceased by around 1450, leaving Māori isolated in their new country for the next three centuries until European contact.
What was here when they came was a country eighty million years out of step with the rest of the world. Nine species of moa, the largest of them taller than a horse, browsed forests of beech and podocarp. Haast’s eagle, the largest the world has ever known, hunted them from above. The seas teemed with fur seals, whales, and seabird colonies whose like is hard to imagine today. There were no land mammals other than three species of bat. There were no people. The first New Zealanders walked into an ecosystem that had never seen a primate, never seen fire used as a tool, and never seen a snare. They transformed it inside two centuries. The moa were gone within a hundred years of arrival. Vast tracts of forest burned. The fur seal colonies of the upper coast collapsed. The country that emerged from this transformation, a land of pā and kūmara gardens and pounamu trade routes and tribal histories carved into the meeting house walls, was an entirely new thing, a Polynesian civilisation in temperate latitudes, the southernmost branch of the Austronesian family tree.
The story is still being written. New radiocarbon dates refine the chronology by a year or two with each passing season. New ancient DNA studies trace the founding population back to specific home islands in Polynesia. New excavations turn up new founding-period sites and reshape our understanding of where the first generations lived and what they ate. Mātauranga Māori, the body of traditional knowledge held by iwi and hapū, is being brought into closer dialogue with scientific archaeology in ways that enrich both, after a century in which they were too often treated as rivals.
What does seem unlikely to change is the broad outline. A long Austronesian expansion. A fifteen-hundred-year pause in Tonga and Samoa. A late, fast colonisation of the eastern Pacific. A final southward pulse to Aotearoa around the turn of the fourteenth century. Many waka, not one fleet. A pristine country full of giant birds. A culture that became uniquely its own in a few centuries of isolation. That is the story the evidence currently tells, and it is, in its actual detail, more remarkable than the simpler stories that came before it.
What’s your take on Māori origins? Did you grow up with the Great Fleet story in school? Tell us in the comments.