title: Maori participation in higher education: Tainui graduates from the University of Waikato, 1992 to 1997

authors: Tiakiwai, Sarah-Jane

abstract: This thesis is an examination of what factors contribute to the success of Maori who participate in higher education. The thesis is informed by the experiences of nine Tainui tribal members who received scholarships from the Tainui Maori Trust Board and who graduated from the University of Waikato between 1992 and 1997. 

The thesis addresses two questions: what factors contributed to the success of Tainui graduates at the University of Waikato? What effect did programmes, policies and initiatives offered by the University of Waikato and the Tainui Maori Trust Board have on the academic success of Tainui graduates at the University of Waikato? 

There are three main components to the thesis: a brief history of the University of Waikato and an examination of three documents (University of Waikato Charter 1991; Paetawhiti, the strategic plan 1993; Academic Audit Unit report 1997) and how they pertain to Maori; a history of the Tainui Maori Trust Board and an examination of the Tainui Education Strategy (1986, 1991), its review (1993) and scholarship programmes; and a study and analysis of the experiences of nine Tainui graduates from the University of Waikato. 

Argued from an eclectic theoretical and methodological position, drawing from indigenous and western theories and research practices that emphasise a kaupapa Maori and tribal approach, the thesis identifies multiple factors that have contributed to the success of the Tainui graduates. These factors include family and parental support, mentoring, the role of finances, institutional support, and identity. 

The thesis finds through examination of the documents, that the policies, initiatives and programmes of the Tainui Maori Trust Board and the University of Waikato have ambiguous and at times conflicting aims and objectives in regard to Maori participation and graduation from higher education. The thesis also finds that the experiences of the graduates reveal that neither the Tainui Maori Trust Board nor policies relating to Maori at the University of Waikato played significant roles in the success of the Tainui graduates. Rather, the thesis finds that the success of the graduates is largely borne by their own efforts, which reflect western notions of success, but which also reinforce their identity as Maori, and as Tainui tribal members. 

The thesis suggests that both the Tainui Maori Trust Board and the University of Waikato review their relationships with their tribal and Maori members (respectively), and recommendations are made to help develop a greater awareness of the contribution that both organisations can make to the success of Maori university students.

text: Maori participation in higher education: Tainui graduates from the University of Waikato, 1992 to 1997 This thesis is an examination of what factors contribute to the success of Maori who participate in higher education. The thesis is informed by the experiences of nine Tainui tribal members who received scholarships from the Tainui Maori Trust Board and who graduated from the University of Waikato between 1992 and 1997. 

The thesis addresses two questions: what factors contributed to the success of Tainui graduates at the University of Waikato? What effect did programmes, policies and initiatives offered by the University of Waikato and the Tainui Maori Trust Board have on the academic success of Tainui graduates at the University of Waikato? 

There are three main components to the thesis: a brief history of the University of Waikato and an examination of three documents (University of Waikato Charter 1991; Paetawhiti, the strategic plan 1993; Academic Audit Unit report 1997) and how they pertain to Maori; a history of the Tainui Maori Trust Board and an examination of the Tainui Education Strategy (1986, 1991), its review (1993) and scholarship programmes; and a study and analysis of the experiences of nine Tainui graduates from the University of Waikato. 

Argued from an eclectic theoretical and methodological position, drawing from indigenous and western theories and research practices that emphasise a kaupapa Maori and tribal approach, the thesis identifies multiple factors that have contributed to the success of the Tainui graduates. These factors include family and parental support, mentoring, the role of finances, institutional support, and identity. 

The thesis finds through examination of the documents, that the policies, initiatives and programmes of the Tainui Maori Trust Board and the University of Waikato have ambiguous and at times conflicting aims and objectives in regard to Maori participation and graduation from higher education. The thesis also finds that the experiences of the graduates reveal that neither the Tainui Maori Trust Board nor policies relating to Maori at the University of Waikato played significant roles in the success of the Tainui graduates. Rather, the thesis finds that the success of the graduates is largely borne by their own efforts, which reflect western notions of success, but which also reinforce their identity as Maori, and as Tainui tribal members. 

The thesis suggests that both the Tainui Maori Trust Board and the University of Waikato review their relationships with their tribal and Maori members (respectively), and recommendations are made to help develop a greater awareness of the contribution that both organisations can make to the success of Maori university students.

year: 2001

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: Modern life at high temperatures

authors: Daniel, Roy M.

subjects: biology

abstract: A variety of micro-organisms are now known which grow optimally above 65°C, and are defined as extreme thermophiles. As might be expected they are found in both natural and artificial hot environments. Until comparatively recently the upper optimum temperature for the growth of any living organism was about 85°C. Then in 1982 Stetter described an organism, isolated from the hot sea floor of a submarine solfatara field, which grew optimally at 105°C. Since then several other organisms have been found with optimum growth temperatures at 100"C or above and a few are capable of growth at 110*C (e.g. Huber et al., 1987; Fiala and Stetter, 1986; Zillig et al., 1987; Stetter et al., 1990).

text: Modern life at high temperatures A variety of micro-organisms are now known which grow optimally above 65°C, and are defined as extreme thermophiles. As might be expected they are found in both natural and artificial hot environments. Until comparatively recently the upper optimum temperature for the growth of any living organism was about 85°C. Then in 1982 Stetter described an organism, isolated from the hot sea floor of a submarine solfatara field, which grew optimally at 105°C. Since then several other organisms have been found with optimum growth temperatures at 100"C or above and a few are capable of growth at 110*C (e.g. Huber et al., 1987; Fiala and Stetter, 1986; Zillig et al., 1987; Stetter et al., 1990).

year: 1992