2017
DOI: 10.1007/s10963-017-9110-y
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Mass Migration and the Polynesian Settlement of New Zealand

Abstract: This paper 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. We show that the rapid appearance of a strong archaeological signature in the early 14th century AD is the result of a mass migration event, not the… Show more

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Cited by 73 publications
(67 citation statements)
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References 51 publications
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“…Even under a scenario where moa density is double our upper estimate, extinction can occur with a small initial human population (n = 100), human population growth rates of 4-5% and offtake rates of less than five individuals per person per year. There is considerable uncertainty over the size of the founding Polynesian population in New Zealand (Murray-McIntosh et al 1998, Whyte et al 2005, Walter et al 2017. Our results show the size of the initial human population has a strong effect on the offtake rates required for moa extinction; with a founding population of 500 people, lower human population growth rates and offtake rates are sufficient to drive moa to extinction within the timeframe estimated by Perry et al (2014) (Fig.…”
Section: Extinction Processesmentioning
confidence: 76%
“…Even under a scenario where moa density is double our upper estimate, extinction can occur with a small initial human population (n = 100), human population growth rates of 4-5% and offtake rates of less than five individuals per person per year. There is considerable uncertainty over the size of the founding Polynesian population in New Zealand (Murray-McIntosh et al 1998, Whyte et al 2005, Walter et al 2017. Our results show the size of the initial human population has a strong effect on the offtake rates required for moa extinction; with a founding population of 500 people, lower human population growth rates and offtake rates are sufficient to drive moa to extinction within the timeframe estimated by Perry et al (2014) (Fig.…”
Section: Extinction Processesmentioning
confidence: 76%
“…Specht (2002) notes that this colonisation period in other regions of the Pacific was associated with pulses of large obsidian blocks being imported to new sites and expediently reduced, while later periods saw less material being imported and more conservative reduction. Walter et al (2010Walter et al ( , 2017 identify a similar proxy in the Austronesianspeaking colonisation of New Zealand. The implications of the present lithic analysis and the lack of dramatic change through time are (1) that we are not seeing the first colonisation mode because the sites excavated do not represent the earliest pulse of Bel colonisation from the east, or (2) there was no major change because the area was already populated on the mainland and the Bel were already geared towards subsistence trading, with established trading links all along the northeast coast.…”
Section: Coastal Mobility and Lithic Supply Linesmentioning
confidence: 92%
“…Both regions and cultural groups provide examples of long-term relationships to place. Māori migrated to Aotearoa from Polynesian islands by oceangoing canoes around 700 years ago (Wilmshurst et al 2008, Tapsell 2014, Walter et al 2017) and quickly established themselves across the previously unpopulated lands. Across the Pacific, the West Coast of Canada is inhabited by many culturally distinct First Nations (hereafter Coastal Peoples) who have inhabited the region since time before memory (at least 14,000 years according to archeological surveys; Muckle and Gauvreau 2017).…”
Section: Place-based Peoples In Aotearoa (New Zealand) and West Coastmentioning
confidence: 99%