title: New Zealand history is Maori history: Tikanga as the ethical foundation of historical scholarship In Aotearoa New Zealand

authors: Mahuika, Nepia

subjects: Arts & Humanities

abstract: IT SHOULD COME AS NO SURPRISE TO FIND that New Zealand history is Māori history. In 1987 when Tipene O’Regan stated that the ‘the past belongs to all New Zealanders, but first it is ours’, he was drawing attention to New Zealand history’s foundation in Māori history.1 Thinking about New Zealand history as Māori history does not mean denying the histories of European, Asian and Pasifika immigrants, but draws attention to the notion that ‘settler’ aspirations to claim ‘Aotearoa’ as home occur within a much broader narrative of indigenous occupation and struggle.2 Indeed, how can New Zealand history be the story of ‘here’ when it has ‘othered’ indigenous narratives that speak to the heart of what it is to belong in the land of the long white cloud? Yes, New Zealand history is Māori history – and that presents a problem for tangata whenua self-determination. Likewise, for Pākehā, it is an issue because until New Zealand history recognizes and enables the centrality of Māori history it will always fail to articulate the collective ‘us’ that is so often assumed in the discourse of ‘full and final settlement’.3 In its current form it will never be able to ethically or adequately account for the shaping of a New Zealand identity that finds ‘composure’ in the story of how Pākehā became ‘native’ New Zealanders.4 For Māori, these issues are keenly felt, because while New Zealand history has always been about us, it has predominantly been articulated on the colonizers’ terms. In the ‘discursive constructions’ that are New Zealand histories, the indigenous have regularly been culturally appropriated, dislocated and misrepresented.5 Even when Māori have turned their back on the writing of New Zealand history it has been, and will still be, a history of being or becoming ‘native’. Yes, New Zealand history is Māori history – so why does it feel like the story of Pākehā settlers?

text: New Zealand history is Maori history: Tikanga as the ethical foundation of historical scholarship In Aotearoa New Zealand IT SHOULD COME AS NO SURPRISE TO FIND that New Zealand history is Māori history. In 1987 when Tipene O’Regan stated that the ‘the past belongs to all New Zealanders, but first it is ours’, he was drawing attention to New Zealand history’s foundation in Māori history.1 Thinking about New Zealand history as Māori history does not mean denying the histories of European, Asian and Pasifika immigrants, but draws attention to the notion that ‘settler’ aspirations to claim ‘Aotearoa’ as home occur within a much broader narrative of indigenous occupation and struggle.2 Indeed, how can New Zealand history be the story of ‘here’ when it has ‘othered’ indigenous narratives that speak to the heart of what it is to belong in the land of the long white cloud? Yes, New Zealand history is Māori history – and that presents a problem for tangata whenua self-determination. Likewise, for Pākehā, it is an issue because until New Zealand history recognizes and enables the centrality of Māori history it will always fail to articulate the collective ‘us’ that is so often assumed in the discourse of ‘full and final settlement’.3 In its current form it will never be able to ethically or adequately account for the shaping of a New Zealand identity that finds ‘composure’ in the story of how Pākehā became ‘native’ New Zealanders.4 For Māori, these issues are keenly felt, because while New Zealand history has always been about us, it has predominantly been articulated on the colonizers’ terms. In the ‘discursive constructions’ that are New Zealand histories, the indigenous have regularly been culturally appropriated, dislocated and misrepresented.5 Even when Māori have turned their back on the writing of New Zealand history it has been, and will still be, a history of being or becoming ‘native’. Yes, New Zealand history is Māori history – so why does it feel like the story of Pākehā settlers?

year: 2015

title: A discontinuous ca. 80 ka record of Late Quaternary environmental change from Lake Omapere, Northland, New Zealand

authors: Newnham, Rewi M.

subjects: Last Glacial

abstract: We present an integrated record of environmental change from Lake Omapere, Northland, New Zealand, based on palaeolimnological analysis of a 7-m-long core and eight adjunct cores spanning part of the last 80 calendar (cal.) ka. The chronology was developed using tephrochronology, palaeomagnetism and radiocarbon dating together with climato- and palyno-stratigraphy. Two of 14 tephra layers in the cores provide markers for correlating the record with other New Zealand climato-stratigraphic sequences, deep-sea cores and the global marine isotope record. Pollen, diatom, palaeomagnetic, sedimentologic and pigment analyses show that Lake Omapere, currently 2 m deep, has had a discontinuous history. Occupying a shallow basin perched partly within old basalt lavas, the initial (alkaline) lake formed towards the end of MIS 5a at ca. 80 cal. ka, presumably because of blockage of local drainage of a swampy alluvial floodplain, inundating peat deposits and forest trees, including kauri (Agathis australis). The lake filled rapidly to a level 1–2 m above that at present. Such filling was probably unrelated to climate but a subsequent phase of variable but generally falling lake levels and increasing dystrophy may have been climatically controlled, commencing during MIS 4 and culminating in periods early in MIS 3 when the lake became swampy or dry. Conditions of non-deposition (or non-preservation) obtained for most of the period after ca. 55 cal. ka (Rotoehu Ash) until formation of the modern lake approximately 600–700 cal. years ago or soon after, as indicated by the presence of Tephra-1, identified in part as Kaharoa Tephra (AD 1314), near the top of the core. The modern lake originated possibly through damming of the western outlet as a consequence of accelerated erosion accompanying earliest Polynesian deforestation, an interpretation supported by Maori oral tradition.
The pollen record indicates that beech Nothofagus (presumably N. truncata) was much more common in Northland during the Last Glacial, and that for this region the relative abundance of Nothofagus vs. Agathis pollen serves as a better indicator of cooler versus warmer intervals during the Quaternary than the ratio of tree to non-tree pollen. However, it seems likely that moisture balance was a more critical factor than temperature in vegetation composition and distribution, particularly during the LGM, and the long periods of hiatus may also be linked to a drier climate than present. Correlation coefficients between the pollen curves confirm that several tree species (Halocarpus bidwillii, H. biformis and Phyllocladus alpinus), previously palynologically concealed within generic taxonomic groups, occurred about two degrees latitude further north and at a much lower altitude than their current limits during cooler or drier phases of the Last Glacial. A temperature depression in Northland of 4 °C at various times during the Last Glacial is inferred from these range expansions. Nevertheless, the persistence of widespread forest cover suggests that the late Pleistocene climate of Northland was less severe than for most of the rest of New Zealand and strengthens the argument for a heightened temperature gradient across northern New Zealand during the Last Glacial.

text: A discontinuous ca. 80 ka record of Late Quaternary environmental change from Lake Omapere, Northland, New Zealand We present an integrated record of environmental change from Lake Omapere, Northland, New Zealand, based on palaeolimnological analysis of a 7-m-long core and eight adjunct cores spanning part of the last 80 calendar (cal.) ka. The chronology was developed using tephrochronology, palaeomagnetism and radiocarbon dating together with climato- and palyno-stratigraphy. Two of 14 tephra layers in the cores provide markers for correlating the record with other New Zealand climato-stratigraphic sequences, deep-sea cores and the global marine isotope record. Pollen, diatom, palaeomagnetic, sedimentologic and pigment analyses show that Lake Omapere, currently 2 m deep, has had a discontinuous history. Occupying a shallow basin perched partly within old basalt lavas, the initial (alkaline) lake formed towards the end of MIS 5a at ca. 80 cal. ka, presumably because of blockage of local drainage of a swampy alluvial floodplain, inundating peat deposits and forest trees, including kauri (Agathis australis). The lake filled rapidly to a level 1–2 m above that at present. Such filling was probably unrelated to climate but a subsequent phase of variable but generally falling lake levels and increasing dystrophy may have been climatically controlled, commencing during MIS 4 and culminating in periods early in MIS 3 when the lake became swampy or dry. Conditions of non-deposition (or non-preservation) obtained for most of the period after ca. 55 cal. ka (Rotoehu Ash) until formation of the modern lake approximately 600–700 cal. years ago or soon after, as indicated by the presence of Tephra-1, identified in part as Kaharoa Tephra (AD 1314), near the top of the core. The modern lake originated possibly through damming of the western outlet as a consequence of accelerated erosion accompanying earliest Polynesian deforestation, an interpretation supported by Maori oral tradition.
The pollen record indicates that beech Nothofagus (presumably N. truncata) was much more common in Northland during the Last Glacial, and that for this region the relative abundance of Nothofagus vs. Agathis pollen serves as a better indicator of cooler versus warmer intervals during the Quaternary than the ratio of tree to non-tree pollen. However, it seems likely that moisture balance was a more critical factor than temperature in vegetation composition and distribution, particularly during the LGM, and the long periods of hiatus may also be linked to a drier climate than present. Correlation coefficients between the pollen curves confirm that several tree species (Halocarpus bidwillii, H. biformis and Phyllocladus alpinus), previously palynologically concealed within generic taxonomic groups, occurred about two degrees latitude further north and at a much lower altitude than their current limits during cooler or drier phases of the Last Glacial. A temperature depression in Northland of 4 °C at various times during the Last Glacial is inferred from these range expansions. Nevertheless, the persistence of widespread forest cover suggests that the late Pleistocene climate of Northland was less severe than for most of the rest of New Zealand and strengthens the argument for a heightened temperature gradient across northern New Zealand during the Last Glacial.

year: 2004

title: Investigating regional house price convergence in the United States: Evidence from a pair-wise approach

authors: Holmes, Mark J.

subjects: panel data

abstract: In this paper we examine long-run house price convergence across US states using a novel econometric approach advocated by Pesaran (2007) and Pesaran et al. (2009). Our empirical modelling strategy employs a probabilistic test statistic for convergence based on the percentage of unit root rejections among all state house price differentials. Using a sieve bootstrap procedure, we construct confidence intervals and find evidence in favour of convergence. We also conclude that speed of adjustment towards long-run equilibrium is inversely related to distance.

text: Investigating regional house price convergence in the United States: Evidence from a pair-wise approach In this paper we examine long-run house price convergence across US states using a novel econometric approach advocated by Pesaran (2007) and Pesaran et al. (2009). Our empirical modelling strategy employs a probabilistic test statistic for convergence based on the percentage of unit root rejections among all state house price differentials. Using a sieve bootstrap procedure, we construct confidence intervals and find evidence in favour of convergence. We also conclude that speed of adjustment towards long-run equilibrium is inversely related to distance.

year: 2011