title: Development and application of large interactive display surfaces

authors: Apperley, Mark

abstract: Recent hardware developments have made possible the construction of relatively inexpensive large interactive display surfaces (LIDS). We have built prototype systems with office whiteboard sized displays using off-the-shelf data projectors and pen digitising equipment. Our group is investigating the use of these prototype systems in a variety of situations, including: programming, teaching, and both local and remote meeting support.
The challenge of this research is to provide a style of user interaction in which the computer is an unobtrusive support agent - offering assistance, recording and replaying data - but not distracting from the interaction between people using the system.

text: Development and application of large interactive display surfaces Recent hardware developments have made possible the construction of relatively inexpensive large interactive display surfaces (LIDS). We have built prototype systems with office whiteboard sized displays using off-the-shelf data projectors and pen digitising equipment. Our group is investigating the use of these prototype systems in a variety of situations, including: programming, teaching, and both local and remote meeting support.
The challenge of this research is to provide a style of user interaction in which the computer is an unobtrusive support agent - offering assistance, recording and replaying data - but not distracting from the interaction between people using the system.

year: 2001

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

title: Takuahi: Te oriori mō Tāmaunga-o-te-rangi - Mana atua, mana whenua, mana tangata

authors: Dewes, Mahue

subjects: Takuahi

abstract: E roa nei tātau te Māori nō ngā wā o Hawaiki e tito ana i te waiata, i te haka, i te oriori, i te mōteatea hei waka kawe i ngā kōrero tuku iho ki ngā whakatipuranga hou. He putuputu tonu ngā tūmomo karere, ka raua atu ki roto i wēnei momo titonga waiata a te Māori. Ka whārikihia e ngā tohunga kaitito ngā karere nei mā te reo kīwaha, mā te reo whakataukī, mā te reo auaha hei kura huna. Mei māmā te kimi, ka tohunga katoa ngā Māori. Kai te aroaro o te tuhingaroa nei, ka ketuketu i tētahi o ngā oriori o Ngāti Porou, otiā, nō Te Whānau-a-Hinerupe, ko te oriori mō Tāmaunga-o-te-rangi, nā Te Māperetahi. Mā konei ake e ruku atu ai ki te raparapa i ngā kura huna e whakatauira ana i te mana Atua, mana whenua, mana tangata hei mana ahi kā. Mā tēnā hoki e whakatauira te mana ahi kā, kai a Tama, otiā, hei tauira atu ki ngā uri o Te Whānau-a-Hinerupe i tō rātau ake ahi kā roa ki Te Kawakawa mai Tawhiti. Ko ngā kōrero kua kohingia, he kōrero nō ngā tāngata e mōhio ana ki ngā tūmomo mana, ā, ki ngā kōrero e pā ana ki te oriori nei. Ka iringia wēnei rau kōrero hei whakarākei tonu i te pae tapu o Te Whānau-a-Hinerupe.

text: Takuahi: Te oriori mō Tāmaunga-o-te-rangi - Mana atua, mana whenua, mana tangata E roa nei tātau te Māori nō ngā wā o Hawaiki e tito ana i te waiata, i te haka, i te oriori, i te mōteatea hei waka kawe i ngā kōrero tuku iho ki ngā whakatipuranga hou. He putuputu tonu ngā tūmomo karere, ka raua atu ki roto i wēnei momo titonga waiata a te Māori. Ka whārikihia e ngā tohunga kaitito ngā karere nei mā te reo kīwaha, mā te reo whakataukī, mā te reo auaha hei kura huna. Mei māmā te kimi, ka tohunga katoa ngā Māori. Kai te aroaro o te tuhingaroa nei, ka ketuketu i tētahi o ngā oriori o Ngāti Porou, otiā, nō Te Whānau-a-Hinerupe, ko te oriori mō Tāmaunga-o-te-rangi, nā Te Māperetahi. Mā konei ake e ruku atu ai ki te raparapa i ngā kura huna e whakatauira ana i te mana Atua, mana whenua, mana tangata hei mana ahi kā. Mā tēnā hoki e whakatauira te mana ahi kā, kai a Tama, otiā, hei tauira atu ki ngā uri o Te Whānau-a-Hinerupe i tō rātau ake ahi kā roa ki Te Kawakawa mai Tawhiti. Ko ngā kōrero kua kohingia, he kōrero nō ngā tāngata e mōhio ana ki ngā tūmomo mana, ā, ki ngā kōrero e pā ana ki te oriori nei. Ka iringia wēnei rau kōrero hei whakarākei tonu i te pae tapu o Te Whānau-a-Hinerupe.

year: 2016