title: The power of reflection in the creative process of making a new site-specific dance work.

authors: Cheesman, Sue

abstract: This article focuses on feedback given by dancers and invited critical peers as part of my choreographic process for creating a new site-specific dance work Curiously Quirky Invasion,  from  March  to  May  2014  in  the  grounds  of  the  University  of  Waikato, Kirikiriroa Hamilton, Aotearoa New Zealand. In particular I focus on an analysis of the feedback, and interrogate the complex ideas and multiple dialogues generated from the ways dancers and peers responded to what they had seen and experienced in the work. More specifically I examine how these responses filtered through my reflections, influenced  and  affected  my  pedagogical  practice  and  the  development  of  the choreography going forward,and how meaningful engagement with this feedback was embraced  in  relation to  the  development  of  this  site-based  dance.  Finally,  the surprises  and  sense  of  empowerment  this  feedback  engendered  will  be  highlighted,concluding with how this translated into the final dance piece.

text: The power of reflection in the creative process of making a new site-specific dance work. This article focuses on feedback given by dancers and invited critical peers as part of my choreographic process for creating a new site-specific dance work Curiously Quirky Invasion,  from  March  to  May  2014  in  the  grounds  of  the  University  of  Waikato, Kirikiriroa Hamilton, Aotearoa New Zealand. In particular I focus on an analysis of the feedback, and interrogate the complex ideas and multiple dialogues generated from the ways dancers and peers responded to what they had seen and experienced in the work. More specifically I examine how these responses filtered through my reflections, influenced  and  affected  my  pedagogical  practice  and  the  development  of  the choreography going forward,and how meaningful engagement with this feedback was embraced  in  relation to  the  development  of  this  site-based  dance.  Finally,  the surprises  and  sense  of  empowerment  this  feedback  engendered  will  be  highlighted,concluding with how this translated into the final dance piece.

year: 2020

title: Interactions of calcium and other metal ions with caldolysin, the thermostable proteinase from Thermus aquaticus strain T351.

authors: Khoo, T.C.

subjects: biology

abstract: Caldolysin, the extracellular proteinase from the extreme thermophile Thermus aquaticus strain T351, is stabilized by Ca2+. A variety of metal ions were able to substitute for Ca2+. Most were unable to confer as much stability as Ca2+, with the exception of the lanthanide ions, which increased the half-life at 95 degrees C from 1 h to more than 4 h. Results from a variety of separation methods indicated that caldolysin binds 6 Ca2+ ions/molecule of enzyme. The presence of non-linear Ca2+ titration plots, and the removal of 4 Ca2+ ions/molecule by treatment with a cationic ion-exchange gel suggested that caldolysin possesses at least two different types of Ca2+-binding sites, with different affinities. Average binding constants of the two types of binding sites were 2.8 X 10(4)M-1 (for the low-affinity sites) and 7.5 X 10(5) M-1 (for the high-affinity sites). The total Ca2+-binding free energy for caldolysin was shown to be greater than for either thermolysin or Bacillus subtilis neutral proteinase. It appears that the higher thermostability of caldolysin is due to the presence of 6 Ca2+ ions rather than 4 Ca2+ ions/molecule.

text: Interactions of calcium and other metal ions with caldolysin, the thermostable proteinase from Thermus aquaticus strain T351. Caldolysin, the extracellular proteinase from the extreme thermophile Thermus aquaticus strain T351, is stabilized by Ca2+. A variety of metal ions were able to substitute for Ca2+. Most were unable to confer as much stability as Ca2+, with the exception of the lanthanide ions, which increased the half-life at 95 degrees C from 1 h to more than 4 h. Results from a variety of separation methods indicated that caldolysin binds 6 Ca2+ ions/molecule of enzyme. The presence of non-linear Ca2+ titration plots, and the removal of 4 Ca2+ ions/molecule by treatment with a cationic ion-exchange gel suggested that caldolysin possesses at least two different types of Ca2+-binding sites, with different affinities. Average binding constants of the two types of binding sites were 2.8 X 10(4)M-1 (for the low-affinity sites) and 7.5 X 10(5) M-1 (for the high-affinity sites). The total Ca2+-binding free energy for caldolysin was shown to be greater than for either thermolysin or Bacillus subtilis neutral proteinase. It appears that the higher thermostability of caldolysin is due to the presence of 6 Ca2+ ions rather than 4 Ca2+ ions/molecule.

year: 1984

title: Two-step human−environmental impact history for northern New Zealand linked to late-Holocene climate change

authors: Newnham, Rewi M.

subjects: New Zealand

abstract: Following resolution of a long-standing debate over the timing of the initial settlement of New Zealand from Polynesia (late 13th century), a prevailing paradigm has developed that invokes rapid transformation of the landscape, principally by fire, within a few decades of the first arrivals. This model has been constructed from evidence mostly from southern and eastern regions of New Zealand, but a more complicated pattern may apply in the more humid western and northern regions where forests are more resilient to burning. We present a new pollen record from Lake Pupuke, Auckland, northern New Zealand, that charts the changing vegetation cover over the last 1000 years, before and after the arrival of people. Previous results from this site concurred with the rapid transformation model, although sampling resolution, chronology and sediment disturbance make that interpretation equivocal. Our new record is dated principally by tephrochronology together with radiocarbon dating, and includes a cryptotephra deposit identified as Kaharoa tephra, a key marker for first settlement in northern New Zealand. Its discovery and stratigraphic position below two Rangitoto-derived tephras enables a clearer picture of environmental change to be drawn. The new pollen record shows an early phase (step 1) of minor, localised forest clearance around the time of Kaharoa tephra (c. 1314 AD) followed by a later, more extensive deforestation phase (step 2) commencing at around the time of deposition of the Rangitoto tephras (c. 1400‒1450 AD). This pattern, which needs to be corroborated from other well-resolved records from northern New Zealand, concurs with an emerging hypothesis that the ‘Little Ice Age’ had a significant impact on pre-European Māori with the onset of harsher conditions causing a consolidation of populations and later environmental impact in northern New Zealand.

text: Two-step human−environmental impact history for northern New Zealand linked to late-Holocene climate change Following resolution of a long-standing debate over the timing of the initial settlement of New Zealand from Polynesia (late 13th century), a prevailing paradigm has developed that invokes rapid transformation of the landscape, principally by fire, within a few decades of the first arrivals. This model has been constructed from evidence mostly from southern and eastern regions of New Zealand, but a more complicated pattern may apply in the more humid western and northern regions where forests are more resilient to burning. We present a new pollen record from Lake Pupuke, Auckland, northern New Zealand, that charts the changing vegetation cover over the last 1000 years, before and after the arrival of people. Previous results from this site concurred with the rapid transformation model, although sampling resolution, chronology and sediment disturbance make that interpretation equivocal. Our new record is dated principally by tephrochronology together with radiocarbon dating, and includes a cryptotephra deposit identified as Kaharoa tephra, a key marker for first settlement in northern New Zealand. Its discovery and stratigraphic position below two Rangitoto-derived tephras enables a clearer picture of environmental change to be drawn. The new pollen record shows an early phase (step 1) of minor, localised forest clearance around the time of Kaharoa tephra (c. 1314 AD) followed by a later, more extensive deforestation phase (step 2) commencing at around the time of deposition of the Rangitoto tephras (c. 1400‒1450 AD). This pattern, which needs to be corroborated from other well-resolved records from northern New Zealand, concurs with an emerging hypothesis that the ‘Little Ice Age’ had a significant impact on pre-European Māori with the onset of harsher conditions causing a consolidation of populations and later environmental impact in northern New Zealand.

year: 2018