title: Closing geographical distances: The value of a New Zealand perspective on the admission policy of a Native Hawaiian School

authors: Hemi, Keakaokawai Varner

subjects: Racial discrimination

abstract: This article examines the legal narratives evident in the American federal court decision in Doe v Kamehameha Schools (Kamehameha).' The article first describes the historical development of everyone/ no-one, someone and Indigenous equality narratives and their particular impact on the narration of Indigenous peoples in the law. It then examines how the opinions of the United States Ninth Circuit Court of Appeals in this case exhibit significant narrative confusion and distrust about the relationship between Indigenous identity and equality, with the Ninth Circuit interpreting the Native Hawaiian schools' preference for Native Hawaiian students as either reverse racial discrimination or an exception to the general rule of homogeneity and anonymity. For comparison, the article then examines similar equality narratives in New Zealand law, which reveal few legal challenges to admission policies which, either explicitly or implicitly, prefer Maori and demonstrate a narrative complementarity between equality and Indigenous identity. The article recognises that, while complementarity could clarify the narrative issues in Kamehameha for future American federal courts, it also provides the opportunity for New Zealand to pause and reflect. Ultimately, the article advocates a weaving of equality narratives across geographical distances.

text: Closing geographical distances: The value of a New Zealand perspective on the admission policy of a Native Hawaiian School This article examines the legal narratives evident in the American federal court decision in Doe v Kamehameha Schools (Kamehameha).' The article first describes the historical development of everyone/ no-one, someone and Indigenous equality narratives and their particular impact on the narration of Indigenous peoples in the law. It then examines how the opinions of the United States Ninth Circuit Court of Appeals in this case exhibit significant narrative confusion and distrust about the relationship between Indigenous identity and equality, with the Ninth Circuit interpreting the Native Hawaiian schools' preference for Native Hawaiian students as either reverse racial discrimination or an exception to the general rule of homogeneity and anonymity. For comparison, the article then examines similar equality narratives in New Zealand law, which reveal few legal challenges to admission policies which, either explicitly or implicitly, prefer Maori and demonstrate a narrative complementarity between equality and Indigenous identity. The article recognises that, while complementarity could clarify the narrative issues in Kamehameha for future American federal courts, it also provides the opportunity for New Zealand to pause and reflect. Ultimately, the article advocates a weaving of equality narratives across geographical distances.

year: 2016

title: Social deprivation in New Zealand

authors: Harcourt, Brian James

subjects: Deprivation

abstract: The purpose of the thesis was to better understand the phenomenon of social deprivation, world-wide and in particular in New Zealand. Social deprivation has been defined in many ways with multiple surrogates used to ‘measure’ its prevalence. The aim of this research was to provide examples of the lived experiences of social deprivation.

Social constructivist and interpretive lenses were used to portray the voices of those living in deprivation, as well as those people tasked to assist them. A narrative case study approach was employed with participants from Whānau Ora. This social and health initiative offered a holistic approach to assistance in contrast to the usual State agencies operating in a silo fashion, with separate agencies providing for different aspects of social deprivation such as housing, employment, mental health and other services. The approach of Whānau Ora is to support clients’ needs holistically and encourage people to develop their own plans for self- improvement. Navigators help people develop their plans and assist in their interactions with the various State agencies whose services they require. This approach allowed a better understanding of ways to overcome people’s feelings of powerlessness and desperation.

The findings from the study lead to suggestions for the application of evidence-based, complementary, integrated assistance programmes rather than having segregated public service agencies acting independently. The recommendations are simple yet require profound changes in public service operations when attempting to ameliorate or prevent social deprivation among citizens.

text: Social deprivation in New Zealand The purpose of the thesis was to better understand the phenomenon of social deprivation, world-wide and in particular in New Zealand. Social deprivation has been defined in many ways with multiple surrogates used to ‘measure’ its prevalence. The aim of this research was to provide examples of the lived experiences of social deprivation.

Social constructivist and interpretive lenses were used to portray the voices of those living in deprivation, as well as those people tasked to assist them. A narrative case study approach was employed with participants from Whānau Ora. This social and health initiative offered a holistic approach to assistance in contrast to the usual State agencies operating in a silo fashion, with separate agencies providing for different aspects of social deprivation such as housing, employment, mental health and other services. The approach of Whānau Ora is to support clients’ needs holistically and encourage people to develop their own plans for self- improvement. Navigators help people develop their plans and assist in their interactions with the various State agencies whose services they require. This approach allowed a better understanding of ways to overcome people’s feelings of powerlessness and desperation.

The findings from the study lead to suggestions for the application of evidence-based, complementary, integrated assistance programmes rather than having segregated public service agencies acting independently. The recommendations are simple yet require profound changes in public service operations when attempting to ameliorate or prevent social deprivation among citizens.

year: 2019

title: Stratigraphy and sedimentology of Pliocene limestones, Wairoa district, northern Hawke's Bay

authors: Jiang, Zichun (Jared)

subjects: Pliocene limestones

abstract: This project documents the sedimentary geology of a shallow-marine, limestone-bearing Pliocene succession (Mangaheia Group; up to 1.5 km thick) within the Wairoa Syncline, northern Hawke’s Bay. The primary focus is three cool-water “Te Aute type” limestone units in the succession – the early Opoitian age Opoiti Limestone (5-10 m thick), the late Opoitian age Whakapunake Limestone (30-100m thick) and the Waipipian age Tahaenui Limestone (10-30 m thick) – that form locally spectacular outcrops in the Wairoa district. Lithostratigraphically, the limestones are given formational status while the encasing siliciclastic sandstones and mudstones are lumped into a newly defined Wairoa Formation which can be informally classified as A, B, C or D depending on position with respect to the three limestone formations. Three field lithofacies groups – limestone (L), sandstone (S) and mudstone (M) – are erected, and variability within these groups is recognised by subdivision into three lithofacies types, L1-3, S1-3 and M1-3. The massive Opoiti Limestone (35-65% CaCO₃; L3 and S2) comprises poorly sorted, variably sandy, barnacle, epifaunal bivalve and locally brachiopod debris well-cemented by low-Mg calcite (LMC) (micro)sparite and micrite. Opoiti Limestone is a bioclastic quartzofeldspathic arenite to biosparrudite, occasionally dolomite-bearing. Occasional calcite infilled biomoulds are testament to former aragonite molluscan skeletons. Opoiti Limestone unconformably overlies Wairoa Formation A (2-200 m thick), and grades up into differentially cemented mudstone of Wairoa Formation B (700-800 m thick) which is unconformably overlain by Whakapunake Limestone. The late Opoitian Whakapunake Limestone (up to 85% CaCO₃; L1, L2 and S1) comprises (cross) bedded and differentially cemented interbeds of fossiliferous and more siliciclastic-rich facies. The limestones are typically poorly sorted bivalve-barnacle biomicrite to biosparrudite cemented by variable amounts of fringe and later equant LMC (micro)spar, sometimes including abundant zoned stoichiometric dolomite rhombohedra. Fabrics are moderately open to tight with some conspicuous limonitised glauconite. Whakapunake Limestone passes conformably up into massive calcareous mudstone of Wairoa Formation C (latest Opoitian; >10 m thick). A shallow angular unconformity separates the Whakapunake Limestone and/or Wairoa Formation C from the overlying well-cemented flaggy Tahaenui Limestone (50-80% CaCO₃; L1), a bivalve-barnacle biosparite to biosparrudite with some neomorphosed former aragonite skeletons and a moderately open fabric. In this limestone early formed dull luminescent isopachous fringing cements (host specific) precede variable pore occlusion by dirty LMC (micro)spar and/or micrite. 
The three limestone formations accumulated on the eastern side of a narrow forearc basin seaway (Ruataniwha Strait) within the Hikurangi subduction complex atop and about antiform upthrust ridges in an active convergent margin setting. Tectonics was the main control on the location and mainly lensoidal geometry of the limestone units, while Pliocene glacioeustatic sea-level fluctuations played a secondary role. Cross-bedded and interbedded limestonesandstone facies attest to deposition under the influence of strong tidal flows and repeated storm events that produced high-energy hydraulic conditions and reworking of variably mixed terrigenous-skeletal sands in the shallow (<30 m) seaway during Pliocene. Redeposition down flank from antiform summits provided accommodation space for sediment build-up.
The calcite dominated cool-water skeletal make-up of these limestones, combined with their relatively shallow burial depths (150-700 m), has resulted in them retaining significant macroporosity (up to 20%). Consequently, as well as having application as a lime or hard rock resource they also have reservoir potential for hydrocarbons in the subsurface.

text: Stratigraphy and sedimentology of Pliocene limestones, Wairoa district, northern Hawke's Bay This project documents the sedimentary geology of a shallow-marine, limestone-bearing Pliocene succession (Mangaheia Group; up to 1.5 km thick) within the Wairoa Syncline, northern Hawke’s Bay. The primary focus is three cool-water “Te Aute type” limestone units in the succession – the early Opoitian age Opoiti Limestone (5-10 m thick), the late Opoitian age Whakapunake Limestone (30-100m thick) and the Waipipian age Tahaenui Limestone (10-30 m thick) – that form locally spectacular outcrops in the Wairoa district. Lithostratigraphically, the limestones are given formational status while the encasing siliciclastic sandstones and mudstones are lumped into a newly defined Wairoa Formation which can be informally classified as A, B, C or D depending on position with respect to the three limestone formations. Three field lithofacies groups – limestone (L), sandstone (S) and mudstone (M) – are erected, and variability within these groups is recognised by subdivision into three lithofacies types, L1-3, S1-3 and M1-3. The massive Opoiti Limestone (35-65% CaCO₃; L3 and S2) comprises poorly sorted, variably sandy, barnacle, epifaunal bivalve and locally brachiopod debris well-cemented by low-Mg calcite (LMC) (micro)sparite and micrite. Opoiti Limestone is a bioclastic quartzofeldspathic arenite to biosparrudite, occasionally dolomite-bearing. Occasional calcite infilled biomoulds are testament to former aragonite molluscan skeletons. Opoiti Limestone unconformably overlies Wairoa Formation A (2-200 m thick), and grades up into differentially cemented mudstone of Wairoa Formation B (700-800 m thick) which is unconformably overlain by Whakapunake Limestone. The late Opoitian Whakapunake Limestone (up to 85% CaCO₃; L1, L2 and S1) comprises (cross) bedded and differentially cemented interbeds of fossiliferous and more siliciclastic-rich facies. The limestones are typically poorly sorted bivalve-barnacle biomicrite to biosparrudite cemented by variable amounts of fringe and later equant LMC (micro)spar, sometimes including abundant zoned stoichiometric dolomite rhombohedra. Fabrics are moderately open to tight with some conspicuous limonitised glauconite. Whakapunake Limestone passes conformably up into massive calcareous mudstone of Wairoa Formation C (latest Opoitian; >10 m thick). A shallow angular unconformity separates the Whakapunake Limestone and/or Wairoa Formation C from the overlying well-cemented flaggy Tahaenui Limestone (50-80% CaCO₃; L1), a bivalve-barnacle biosparite to biosparrudite with some neomorphosed former aragonite skeletons and a moderately open fabric. In this limestone early formed dull luminescent isopachous fringing cements (host specific) precede variable pore occlusion by dirty LMC (micro)spar and/or micrite. 
The three limestone formations accumulated on the eastern side of a narrow forearc basin seaway (Ruataniwha Strait) within the Hikurangi subduction complex atop and about antiform upthrust ridges in an active convergent margin setting. Tectonics was the main control on the location and mainly lensoidal geometry of the limestone units, while Pliocene glacioeustatic sea-level fluctuations played a secondary role. Cross-bedded and interbedded limestonesandstone facies attest to deposition under the influence of strong tidal flows and repeated storm events that produced high-energy hydraulic conditions and reworking of variably mixed terrigenous-skeletal sands in the shallow (<30 m) seaway during Pliocene. Redeposition down flank from antiform summits provided accommodation space for sediment build-up.
The calcite dominated cool-water skeletal make-up of these limestones, combined with their relatively shallow burial depths (150-700 m), has resulted in them retaining significant macroporosity (up to 20%). Consequently, as well as having application as a lime or hard rock resource they also have reservoir potential for hydrocarbons in the subsurface.

year: 2011