title: Transcending the personal and political: Provocations

authors: Morrison, Michele

abstract: Each case study in this book stands alone. The leaders portrayed in these narratives, and the authors who collaborated with them in the re-storying of their lived experience, bring unique worldviews and particular theoretical lenses to bear. le is appropriate chat readers should do the same. In this concluding chapter we seek not to prescribe meaning nor constrain interpretation but to highlight three emerging themes: complexity, agency, and action. Rather than summarise each case we select examples that evoke and illustrate the points we wish co make. We consider the implications of complexity, agency, and action for practitioners, policy makers, and the education profession (pre- and in-service). Finally, we conclude with a series of provocations that we hope will ignite passionate debate, professional commitment, and the political will necessary co reach national consensus over what we mean by social justice and how we best go about achieving this.

text: Transcending the personal and political: Provocations Each case study in this book stands alone. The leaders portrayed in these narratives, and the authors who collaborated with them in the re-storying of their lived experience, bring unique worldviews and particular theoretical lenses to bear. le is appropriate chat readers should do the same. In this concluding chapter we seek not to prescribe meaning nor constrain interpretation but to highlight three emerging themes: complexity, agency, and action. Rather than summarise each case we select examples that evoke and illustrate the points we wish co make. We consider the implications of complexity, agency, and action for practitioners, policy makers, and the education profession (pre- and in-service). Finally, we conclude with a series of provocations that we hope will ignite passionate debate, professional commitment, and the political will necessary co reach national consensus over what we mean by social justice and how we best go about achieving this.

year: 2017

title: Connecting with tephras: principles, functioning, and applications of tephrochronology in Quaternary science

authors: Lowe, David J.

abstract: Tephrochronology is a unique method for linking and dating geological, palaeoecological, palaeoclimatic, or archaeological sequences or events. The method relies firstly on stratigraphy and the law of superposition, which apply in any study that connects or correlates deposits from one place to another. Secondly, it relies on characterising and hence identifying or ‘fingerprinting’ tephra layers using either physical properties evident in the field or those obtained from laboratory analysis, including mineralogical examination by optical microscopy or geochemical analysis of glass shards or crystals (e.g., Fe-Ti oxides, ferromagnesian minerals) using the electron microprobe and other tools. Thirdly, the method is enhanced when a numerical age is obtained for a tephra layer by (1) radiometric methods such as radiocarbon, fission-track, U-series, or Ar/Ar dating, (2) incremental dating methods including dendrochronology or varved sediments or layering in ice cores, or (3) age-equivalent methods such as palaeomagnetism or correlation with marine oxygen isotope stages or palynostratigraphy. Once known, that age can be transferred from one site to the next using stratigraphic methods and by matching compositional characteristics, i.e., comparing ‘fingerprints’ from each layer. Used this way, tephrochronology is an age-equivalent dating method.

text: Connecting with tephras: principles, functioning, and applications of tephrochronology in Quaternary science Tephrochronology is a unique method for linking and dating geological, palaeoecological, palaeoclimatic, or archaeological sequences or events. The method relies firstly on stratigraphy and the law of superposition, which apply in any study that connects or correlates deposits from one place to another. Secondly, it relies on characterising and hence identifying or ‘fingerprinting’ tephra layers using either physical properties evident in the field or those obtained from laboratory analysis, including mineralogical examination by optical microscopy or geochemical analysis of glass shards or crystals (e.g., Fe-Ti oxides, ferromagnesian minerals) using the electron microprobe and other tools. Thirdly, the method is enhanced when a numerical age is obtained for a tephra layer by (1) radiometric methods such as radiocarbon, fission-track, U-series, or Ar/Ar dating, (2) incremental dating methods including dendrochronology or varved sediments or layering in ice cores, or (3) age-equivalent methods such as palaeomagnetism or correlation with marine oxygen isotope stages or palynostratigraphy. Once known, that age can be transferred from one site to the next using stratigraphic methods and by matching compositional characteristics, i.e., comparing ‘fingerprints’ from each layer. Used this way, tephrochronology is an age-equivalent dating method.

year: 2013

title: Te Kōtihitihi: Ngā Tuhinga Reo Māori, Putanga 2

authors: Ngāpō, Korohere

abstract: Koinei te katoa o te Putanga 2 o te puka hautaka, Te Kōtihitihi.

text: Te Kōtihitihi: Ngā Tuhinga Reo Māori, Putanga 2 Koinei te katoa o te Putanga 2 o te puka hautaka, Te Kōtihitihi.

year: 2012-05