title: Life in a clinical diploma course

authors: Paterson, Keriata

subjects: Maori

abstract: This paper focuses on the author’s experience of a Clinical Diploma programme. The author is a Maori woman who is in her second year of a three year post-graduate Clinical Diploma programme. The paper includes comment on the cultural focus of content, culture conflicts and areas where the programme might be improved for Maori students.

text: Life in a clinical diploma course This paper focuses on the author’s experience of a Clinical Diploma programme. The author is a Maori woman who is in her second year of a three year post-graduate Clinical Diploma programme. The paper includes comment on the cultural focus of content, culture conflicts and areas where the programme might be improved for Maori students.

year: 1993

title: Na Tarimo i whakaari... Ko Rangiwewehi te iwi

authors: Flavell, James William Ben

abstract: Ko ngā kōrero e whai ake nei, he mea kohikohi, he mea tuku mai ki ahau mō te iwi e kiia nei, ko Ngāti Rangiwewehi. Ko te rohe ki te taha raki o te Rotorua-nui-ā-kahumatamomoe to tūrangawaewae, otirā the rohe takahi o te iwi nei, i ngā rā o mua, nā, ahakoa he nui te whenua kua ngaro atu, kei konei tonu te papa kāinga mō tēnei karangatanga o Te Arawa waka, kei konei hoki tōna mauri, tōna mana, tōna wehi.
Ko Ngāti Rangiwehei i ēnei rā, e rite tonu ana ki te tōtara nui. I tipu ake tēnei tōtara i te kākano i ruia i Rangiātea arā, i Hawaiki, i mānu mai ki Aotearoa nei, i puāwai mai, ā, kei te tipu tonu, kei te tuipu tonu.
Nā, kei roto i tēnei rākau, ko ngā kōrero katoa mō te iwi nei, arā ko ngā whakapapa, ko ngā waiata ko ngā karakia, ko ngā pakiwaitara otirā ko ngā āhuatanga katoa e pā ana ki te iwi. Kei konei hoki ko te ira o te tangata e mau nei i ēnei āhuatanga nei.
Ka tae ki te ngahuru, ka heke iho ngā rau rākau ka pirau, ka ngaro. Pēnei i te rākau nei, te hinga te tangata, ka kapohia e te ringa o Aituā, ā, ka ngaro. Ēhara i te mea ko te mauri o te tangata anake te mea e ngaro nei, ēngari, ko ōna mātauranga katoa hoki.
Nā, matemate noa atu ngā koroua me ngākuia e mōhio tūturu ana ki ngā kōrero hōhonu tuku iho a Ngāti Rangiwewehi. Nō reira, ko tāku mahi, he kohi i ēnei kōrero, i mua i te ngaronga tonutanga o ngā kaumātua e ora ana, nei ngaro.
Kua kohia nei e au ngā kōrero katoa ahakoa Māori ahakoa Pākehā, kia kitea ai, kia mārama ake ai ngā momo āhuatanga o tōku iwi.
Ēhara tēnei i te me ngāwari, nō te mea, ko tēnei mea te mātaranga ahakoa he whakapapa rānei, he pakiwaitara rānei, he mea tino tapu ki te Māori, i te ao tawhito, ā, kei te pērā anō hoki i ēnei rā. Kua oti te tārai te tāhū o tēnei tuhituhinga e kore a taea te whakatārewa tēnei tāhū mehemea kāore, ōna pou kāore ōna here e tika ana. Otirā e kore e tū te whare kōreo, te tāhū whakaringa kōereo, mehemea kāore ōna kaupapa whenua, tangata, tae atu ki a Papatūānuku. Nō reira, koia tēnei ka tātaihia ake ngā kupu kōreroa muri ake nei, kia tutuki ai ngā tūmanako ngā wawata, a ngā whakatipuranga, mai, mai, mai i te pō ki ngā kaikōrero me te kaituhi.
E ai ki te iwi, ko Rangiwewehi te tipuna o tēnei iwi te tamaiti a Tawakeheimoa rāua ko Te Aongahoro.
Nā te mea, he karangatanga a Ngāti Rangiwewehi nō Te Arawa waka i hoki atu ai au ki ngā kōrero mō tēnei waka tapu. Tae rawa mai tēnei waka ki tēnei whenua, ka horapa hāere ngā tāngata i te mata o te whenua. I tōna wā, i tae atu ngā tīpuna ke Te Awahou awa, otirā ki te taha raki o Rotorua moana. Mai i taua wā, ka tīmata ngā āhuatanga katoa e pā ana ki tēnei iwi.
Nā, ēhara tēnei tuhinga i te pukapuka hei whakaatu i te tūturutanga o ngā kōrero katoa o Ngāti Rangiwewehi, mā Ngāti Rangiwewehi hei whai atu, ēngari he kōrero kua kohia nei e au i ngā rangatira, i ngā tohunga, i ngā tāngata mōhio, i ngā whāea, i ngā kaumātua me ngā pukapuka a ngā Māori me ngā Pākehā.
He pūtake kōrero noa iho tēnei mō Ngāti Rangiwewehi he tohu whakamaharatanga hoki ki ngā tīpuna, ki ngā mātua kua wehe atu nei ki te pō.

text: Na Tarimo i whakaari... Ko Rangiwewehi te iwi Ko ngā kōrero e whai ake nei, he mea kohikohi, he mea tuku mai ki ahau mō te iwi e kiia nei, ko Ngāti Rangiwewehi. Ko te rohe ki te taha raki o te Rotorua-nui-ā-kahumatamomoe to tūrangawaewae, otirā the rohe takahi o te iwi nei, i ngā rā o mua, nā, ahakoa he nui te whenua kua ngaro atu, kei konei tonu te papa kāinga mō tēnei karangatanga o Te Arawa waka, kei konei hoki tōna mauri, tōna mana, tōna wehi.
Ko Ngāti Rangiwehei i ēnei rā, e rite tonu ana ki te tōtara nui. I tipu ake tēnei tōtara i te kākano i ruia i Rangiātea arā, i Hawaiki, i mānu mai ki Aotearoa nei, i puāwai mai, ā, kei te tipu tonu, kei te tuipu tonu.
Nā, kei roto i tēnei rākau, ko ngā kōrero katoa mō te iwi nei, arā ko ngā whakapapa, ko ngā waiata ko ngā karakia, ko ngā pakiwaitara otirā ko ngā āhuatanga katoa e pā ana ki te iwi. Kei konei hoki ko te ira o te tangata e mau nei i ēnei āhuatanga nei.
Ka tae ki te ngahuru, ka heke iho ngā rau rākau ka pirau, ka ngaro. Pēnei i te rākau nei, te hinga te tangata, ka kapohia e te ringa o Aituā, ā, ka ngaro. Ēhara i te mea ko te mauri o te tangata anake te mea e ngaro nei, ēngari, ko ōna mātauranga katoa hoki.
Nā, matemate noa atu ngā koroua me ngākuia e mōhio tūturu ana ki ngā kōrero hōhonu tuku iho a Ngāti Rangiwewehi. Nō reira, ko tāku mahi, he kohi i ēnei kōrero, i mua i te ngaronga tonutanga o ngā kaumātua e ora ana, nei ngaro.
Kua kohia nei e au ngā kōrero katoa ahakoa Māori ahakoa Pākehā, kia kitea ai, kia mārama ake ai ngā momo āhuatanga o tōku iwi.
Ēhara tēnei i te me ngāwari, nō te mea, ko tēnei mea te mātaranga ahakoa he whakapapa rānei, he pakiwaitara rānei, he mea tino tapu ki te Māori, i te ao tawhito, ā, kei te pērā anō hoki i ēnei rā. Kua oti te tārai te tāhū o tēnei tuhituhinga e kore a taea te whakatārewa tēnei tāhū mehemea kāore, ōna pou kāore ōna here e tika ana. Otirā e kore e tū te whare kōreo, te tāhū whakaringa kōereo, mehemea kāore ōna kaupapa whenua, tangata, tae atu ki a Papatūānuku. Nō reira, koia tēnei ka tātaihia ake ngā kupu kōreroa muri ake nei, kia tutuki ai ngā tūmanako ngā wawata, a ngā whakatipuranga, mai, mai, mai i te pō ki ngā kaikōrero me te kaituhi.
E ai ki te iwi, ko Rangiwewehi te tipuna o tēnei iwi te tamaiti a Tawakeheimoa rāua ko Te Aongahoro.
Nā te mea, he karangatanga a Ngāti Rangiwewehi nō Te Arawa waka i hoki atu ai au ki ngā kōrero mō tēnei waka tapu. Tae rawa mai tēnei waka ki tēnei whenua, ka horapa hāere ngā tāngata i te mata o te whenua. I tōna wā, i tae atu ngā tīpuna ke Te Awahou awa, otirā ki te taha raki o Rotorua moana. Mai i taua wā, ka tīmata ngā āhuatanga katoa e pā ana ki tēnei iwi.
Nā, ēhara tēnei tuhinga i te pukapuka hei whakaatu i te tūturutanga o ngā kōrero katoa o Ngāti Rangiwewehi, mā Ngāti Rangiwewehi hei whai atu, ēngari he kōrero kua kohia nei e au i ngā rangatira, i ngā tohunga, i ngā tāngata mōhio, i ngā whāea, i ngā kaumātua me ngā pukapuka a ngā Māori me ngā Pākehā.
He pūtake kōrero noa iho tēnei mō Ngāti Rangiwewehi he tohu whakamaharatanga hoki ki ngā tīpuna, ki ngā mātua kua wehe atu nei ki te pō.

year: 1986

title: Restiad bog development and nutrient dynamics of the dominant species

authors: Clarkson, Beverley R.

subjects: bog succession

abstract: Vegetation and peat in lowland restiad (dominated by Restionaceae) raised bogs on North Island (Waikato region) and Chatham Island, New Zealand, were sampled to investigate the main environmental controls of pattern and change. Vegetation classification based on a chronosequence of Waikato restiad bogs revealed a sequence from sedges, through Empodisma minus, the main peatforming restiad, to phases dominated by a second restiad, Sporadanthus ferrugineus. The sequence paralleled temporal successional patterns and was used for interpreting plant-nutrient dynamics along a successional gradient. As succession proceeds, von Post (an index of peat decomposition), total P, total N and % ash in peat decrease. Empodisma was considered to be the key species in restiad bog development. It is tolerant of a wide environmental range, establishing early in minerotrophic wetlands to initiate restiad bog development, and persisting through to late ombrotrophic phases. On Chatham Island, the ecological role of Sporadanthus traversii in restiad bog development is similar to Empodisma in Waikato, being the main peat former and occupying a wide environmental range. Peat under S. traversii had significantly higher total N, total K, available P, bulk density and von Post, and lower pH than Waikato peats under S. ferrugineus or Empodisma. This was attributed to a strong oceanic influence and long history of sea-bird nutrient inputs. 
Nutrient responses in the heath and restiad components of the bog were compared by measuring plant ¹⁵N natural abundance across N and P gradients. Heath shrubs revealed considerable isotopic variation (-2.03 to - 15.55 for Leptospermum scoparium), with foliar δ¹⁵N strongly positively correlated with P concentrations in foliage and peat. In contrast, restiad species revealed little isotopic variation, with Empodisma and S. traversii having δ¹⁵N levels around 0‰, and S. ferrugineus being significantly more depleted (mean -4.97‰). The differences in ii isotopic signatures between heath shrubs and restiads were linked to contrasting nutrient demands, acquisition mechanisms, and root morphology. Leptospermum shrubs on low nutrient peats were stunted, with low foliar %P and high N:P ratios, suggesting they were P-limited. The concurrence of δ¹⁵N depletion and %P in plant tissues suggests N fractionation is promoted by P limitation. In contrast, the constancy in δ¹⁵N of the restiad species through the nutrient gradients indicates these may not be P-limited. 
The contrasting δ¹⁵N signatures of co-habiting Empodisma and S. ferrugineus in late successional bogs suggest the species are accessing different sources of N. Empodisma has a thick layer of cluster roots overlying the deeper S. ferrugineus roots, and would be better positioned to intercept aerially derived N. The hypothesis that this root disposition allows Empodisma to preferentially access the primary N input from rainfall was tested using a ¹⁵N-enriched tracer. At plots codominated by Empodisma and S.ferrugineus, 1.6 mmoles m-2 of 99 atom% excess ¹⁵N as (NH4)2S04 was applied to the peat surface, followed by deionised water, simulating a rainfall event of 34 mm. After 5 hours, cores were harvested and analysed for ¹⁵N. Approximately 90% of the recovered isotope was in the upper Empodisma root layer. Seven weeks after tracer application, young shoots of Empodisma were significantly enriched whereas adjacent Sporadanthus shoots were not. The results confirm that species acquire nutrients from different rooting zones, with Empodisma accessing nutrients at the surface from rainfall and S. ferrugineus acquiring nutrients from deeper peat layers. Niche differentiation facilitates species co-existence, which, on a successional time scale, may be a mechanism for slowing the rate of competitive displacement.

text: Restiad bog development and nutrient dynamics of the dominant species Vegetation and peat in lowland restiad (dominated by Restionaceae) raised bogs on North Island (Waikato region) and Chatham Island, New Zealand, were sampled to investigate the main environmental controls of pattern and change. Vegetation classification based on a chronosequence of Waikato restiad bogs revealed a sequence from sedges, through Empodisma minus, the main peatforming restiad, to phases dominated by a second restiad, Sporadanthus ferrugineus. The sequence paralleled temporal successional patterns and was used for interpreting plant-nutrient dynamics along a successional gradient. As succession proceeds, von Post (an index of peat decomposition), total P, total N and % ash in peat decrease. Empodisma was considered to be the key species in restiad bog development. It is tolerant of a wide environmental range, establishing early in minerotrophic wetlands to initiate restiad bog development, and persisting through to late ombrotrophic phases. On Chatham Island, the ecological role of Sporadanthus traversii in restiad bog development is similar to Empodisma in Waikato, being the main peat former and occupying a wide environmental range. Peat under S. traversii had significantly higher total N, total K, available P, bulk density and von Post, and lower pH than Waikato peats under S. ferrugineus or Empodisma. This was attributed to a strong oceanic influence and long history of sea-bird nutrient inputs. 
Nutrient responses in the heath and restiad components of the bog were compared by measuring plant ¹⁵N natural abundance across N and P gradients. Heath shrubs revealed considerable isotopic variation (-2.03 to - 15.55 for Leptospermum scoparium), with foliar δ¹⁵N strongly positively correlated with P concentrations in foliage and peat. In contrast, restiad species revealed little isotopic variation, with Empodisma and S. traversii having δ¹⁵N levels around 0‰, and S. ferrugineus being significantly more depleted (mean -4.97‰). The differences in ii isotopic signatures between heath shrubs and restiads were linked to contrasting nutrient demands, acquisition mechanisms, and root morphology. Leptospermum shrubs on low nutrient peats were stunted, with low foliar %P and high N:P ratios, suggesting they were P-limited. The concurrence of δ¹⁵N depletion and %P in plant tissues suggests N fractionation is promoted by P limitation. In contrast, the constancy in δ¹⁵N of the restiad species through the nutrient gradients indicates these may not be P-limited. 
The contrasting δ¹⁵N signatures of co-habiting Empodisma and S. ferrugineus in late successional bogs suggest the species are accessing different sources of N. Empodisma has a thick layer of cluster roots overlying the deeper S. ferrugineus roots, and would be better positioned to intercept aerially derived N. The hypothesis that this root disposition allows Empodisma to preferentially access the primary N input from rainfall was tested using a ¹⁵N-enriched tracer. At plots codominated by Empodisma and S.ferrugineus, 1.6 mmoles m-2 of 99 atom% excess ¹⁵N as (NH4)2S04 was applied to the peat surface, followed by deionised water, simulating a rainfall event of 34 mm. After 5 hours, cores were harvested and analysed for ¹⁵N. Approximately 90% of the recovered isotope was in the upper Empodisma root layer. Seven weeks after tracer application, young shoots of Empodisma were significantly enriched whereas adjacent Sporadanthus shoots were not. The results confirm that species acquire nutrients from different rooting zones, with Empodisma accessing nutrients at the surface from rainfall and S. ferrugineus acquiring nutrients from deeper peat layers. Niche differentiation facilitates species co-existence, which, on a successional time scale, may be a mechanism for slowing the rate of competitive displacement.

year: 2005