title: Ecological modernization versus sustainable development: the case of genetic modification regulation in New Zealand

authors: Wright, Jeanette Marie

subjects: ecological modernization

abstract: Ecological modernization and sustainable development are the two dominant paradigms in environmental policy. This paper assesses the implications of competing understandings of ecological modernization and sustainable development using the case of genetic modification regulation in New Zealand. Although the New Zealand regulatory framework embraces the symbolic language of sustainability, it ultimately adheres to a narrow notion of ecological modernization. By adopting a technically driven risk management process and a diluted precautionary approach, alongside limiting public input into decision-making on genetic modification, it undercuts its commitment to sustainable development definitionally and procedurally. Analysis of the New Zealand biotechnology policy regulatory framework, which consists of the Hazardous Substances and New Organisms (HSNO) Act and the Environmental Risk Management Authority (ERMA), shows how institutionalization of a narrow conception of ecological modernization can preempt real commitment to sustainable development.

text: Ecological modernization versus sustainable development: the case of genetic modification regulation in New Zealand Ecological modernization and sustainable development are the two dominant paradigms in environmental policy. This paper assesses the implications of competing understandings of ecological modernization and sustainable development using the case of genetic modification regulation in New Zealand. Although the New Zealand regulatory framework embraces the symbolic language of sustainability, it ultimately adheres to a narrow notion of ecological modernization. By adopting a technically driven risk management process and a diluted precautionary approach, alongside limiting public input into decision-making on genetic modification, it undercuts its commitment to sustainable development definitionally and procedurally. Analysis of the New Zealand biotechnology policy regulatory framework, which consists of the Hazardous Substances and New Organisms (HSNO) Act and the Environmental Risk Management Authority (ERMA), shows how institutionalization of a narrow conception of ecological modernization can preempt real commitment to sustainable development.

year: 2009

title: Recent occurrence of Cylindrospermopsis raciborskii, in Waikato lakes of New Zealand.

authors: Ryan, E.F.

subjects: Cyanobacteria

abstract: Cylindrospermopsis raciborskii is a toxin-producing species of cyanobacteria that in autumn 2003 was recorded for the first time in three shallow (max. depth ≤5 m) Waikato lakes and a hydro-electric dam on the Waikato River, New Zealand. It formed water blooms at densities >100 000 cells/ml in Lakes Waahi and Whangape. Net rates of population growth >0.2 day-1 were recorded for C. raciborskii in Lakes Ngaroto, Waahi, and Karapiro, based on comparisons of low numbers (detection of <10>cells/ml) from initial samples and its presence at bloom densities (>15 000 cells/ml) in the subsequent sample "x"-"y" days later. C. raciborskii may be well adapted to rapid proliferation in the Waikato lakes, which are eutrophic to hypertrophic, with high light attenuation, and where nitrogen (N) fixation may provide it with a competitive advantage over non-nitrogen fixing algae under N-limited conditions.

text: Recent occurrence of Cylindrospermopsis raciborskii, in Waikato lakes of New Zealand. Cylindrospermopsis raciborskii is a toxin-producing species of cyanobacteria that in autumn 2003 was recorded for the first time in three shallow (max. depth ≤5 m) Waikato lakes and a hydro-electric dam on the Waikato River, New Zealand. It formed water blooms at densities >100 000 cells/ml in Lakes Waahi and Whangape. Net rates of population growth >0.2 day-1 were recorded for C. raciborskii in Lakes Ngaroto, Waahi, and Karapiro, based on comparisons of low numbers (detection of <10>cells/ml) from initial samples and its presence at bloom densities (>15 000 cells/ml) in the subsequent sample "x"-"y" days later. C. raciborskii may be well adapted to rapid proliferation in the Waikato lakes, which are eutrophic to hypertrophic, with high light attenuation, and where nitrogen (N) fixation may provide it with a competitive advantage over non-nitrogen fixing algae under N-limited conditions.

year: 2003-10-01

title: The marine reservoir effect in the Southern Ocean: an evaluation of extant and new R values and their application to archaeological chronologies

authors: Petchey, Fiona

subjects: ∆R

abstract: The last phase of human colonisation of the south-west Pacific occurred around the 12th Century AD amongst the islands of the subtropical and temperate zones of the Southern Ocean (i.e., Norfolk Island, the Kermadec Islands, New Zealand and the Chatham Islands) (Fig. 1). Archaeological evidence indicates that initial colonisation of the region was rapid, possibly taking less than 100 years. Unfortunately, the chronology of these events has been largely reliant on charcoal radiocarbon determinations that have not been successful in delineating these changes. This paper investigates the use of marine shell for radiocarbon dating as an alternative to charcoal, with specific focus on variation in the marine 14C reservoir (specifically the ∆R) of Raoul Island (Kermadec Islands), Norfolk Island and Chatham Island (Fig. 2). Results from known-age, pre-AD 1950 shellfish indicate that ∆R values south of the South Pacific Convergence Zone are low compared to those recorded for islands within the South Pacific generally (Fig. 1) (see Petchey et al.in press). An average ∆R value of –19 ± 13 14C yr is recorded for Raoul Island and –49 ± 10 14C yr for Norfolk Island. These values are attributed to heightened absorption of atmospheric CO2 in this region. Extant published ∆R information from New Zealand (Fig. 2A) also suggests a low average ∆R value for these southern waters, but the range of values indicates that considerable variability is possible because of the complex interplay of currents around the New Zealand coastline. In contrast, results from Chatham Island are more variable and much higher (average ∆R = 134 ± 83 14C yr). Stable oxygen and carbon isotope data support the hypothesis that these ∆R values are caused by upwelling and mixing of 14C-depleted water along the Chatham Rise. Comparison of marine and charcoal 14C determinations from archaeological sites on Raoul Island support, within the limits of the available data, the ∆R values obtained, but further analysis is required to establish the stability of this value over time.

text: The marine reservoir effect in the Southern Ocean: an evaluation of extant and new R values and their application to archaeological chronologies The last phase of human colonisation of the south-west Pacific occurred around the 12th Century AD amongst the islands of the subtropical and temperate zones of the Southern Ocean (i.e., Norfolk Island, the Kermadec Islands, New Zealand and the Chatham Islands) (Fig. 1). Archaeological evidence indicates that initial colonisation of the region was rapid, possibly taking less than 100 years. Unfortunately, the chronology of these events has been largely reliant on charcoal radiocarbon determinations that have not been successful in delineating these changes. This paper investigates the use of marine shell for radiocarbon dating as an alternative to charcoal, with specific focus on variation in the marine 14C reservoir (specifically the ∆R) of Raoul Island (Kermadec Islands), Norfolk Island and Chatham Island (Fig. 2). Results from known-age, pre-AD 1950 shellfish indicate that ∆R values south of the South Pacific Convergence Zone are low compared to those recorded for islands within the South Pacific generally (Fig. 1) (see Petchey et al.in press). An average ∆R value of –19 ± 13 14C yr is recorded for Raoul Island and –49 ± 10 14C yr for Norfolk Island. These values are attributed to heightened absorption of atmospheric CO2 in this region. Extant published ∆R information from New Zealand (Fig. 2A) also suggests a low average ∆R value for these southern waters, but the range of values indicates that considerable variability is possible because of the complex interplay of currents around the New Zealand coastline. In contrast, results from Chatham Island are more variable and much higher (average ∆R = 134 ± 83 14C yr). Stable oxygen and carbon isotope data support the hypothesis that these ∆R values are caused by upwelling and mixing of 14C-depleted water along the Chatham Rise. Comparison of marine and charcoal 14C determinations from archaeological sites on Raoul Island support, within the limits of the available data, the ∆R values obtained, but further analysis is required to establish the stability of this value over time.

year: 2008