title: The microbial olympics

authors: Youle, Merry

subjects: microbiology

abstract: Every four years, the Olympic Games plays host to competitors who have built on their natural talent by training for many years to become the best in their chosen discipline. Similar spirit and endeavour can be found throughout the microbial world, in which every day is a competition to survive and thrive. Microorganisms are trained through evolution to become the fittest and the best adapted to a particular environmental niche or lifestyle, and to innovate when the 'rules of the game' are changed by alterations to their natural habitats. In this Essay, we honour the best competitors in the microbial world by inviting them to take part in the inaugural Microbial Olympics.

text: The microbial olympics Every four years, the Olympic Games plays host to competitors who have built on their natural talent by training for many years to become the best in their chosen discipline. Similar spirit and endeavour can be found throughout the microbial world, in which every day is a competition to survive and thrive. Microorganisms are trained through evolution to become the fittest and the best adapted to a particular environmental niche or lifestyle, and to innovate when the 'rules of the game' are changed by alterations to their natural habitats. In this Essay, we honour the best competitors in the microbial world by inviting them to take part in the inaugural Microbial Olympics.

year: 2012

title: Geology, History and Stratigraphy of Hydrothermal Eruptions in the Rotorua Geothermal Field

authors: Cody, Ashley Douglas

subjects: Geothermal Hydrothermal eruptions Rotorua

abstract: The study area is the Rotorua geothermal field (RGF), which is located in the southern end of the Rotorua caldera. Distribution of surface geothermal activity, hydrothermal eruption (HE) deposits and craters have been mapped. HE deposits formed in geological, historical and modern times were studied to record and describe their distribution, composition, petrography, lithology and stratigraphy.

Locations of all identified HE sites in the RGF have been plotted and shown on accompanying maps. At Ohinemutu and Sulphur Bay, HE breccias have been preserved only where deposits were subsequently silicified by hot spring outflows. At Whakarewarewa two HE breccias outcrop over about 0.5 km² and are up to 23 m thick. Study of stratigraphic relationships with tephras of known ages has determined one as Holocene (c. 20 ka) and one of Late Pleistocene age (c. 65 ka).

Four HE breccias were studied in detail. The mineral composition, physical description, field characteristics and spatial distribution of HE breccias are described and mapped. Clasts and matrix were examined by XRD analyses of whole (67) and clay fraction separates (16). Silica crystallinity indices (14) were determined by XRD to identify devitrification rates of opaline mineral species. The petrography of 67 breccia clasts and matrix samples were studied, and polished sections showed the only sulphide to be pyrite. Geothermal alteration of all prehistorical HE deposits was of advanced argillic to argillic and one modern day deposit was of sub propylitic epithermal alteration.

Study of a HE deposit formed in Kuirau Park on 26 January 2001 allowed properties and mineral composition to be examined and recorded before rapid oxidation and weathering destroyed its physical and mineral composition. Study of this and other twentieth century HE events confirms that these rapidly decompose to leave little or no recognisable deposit in the geological record.

Descriptions and all known historical records of HEs in the RGF have been collated to provide a comprehensive inventory of maps and appendices of these events. This information will greatly assist statutory authorities with mitigation of risk to lives and property from geothermal hazards as well as aid appropriate land use and emergency services planning.

Hydrothermal eruptions are ongoing in the RGF through time and produce craters 2 - 110m diameter with erupted deposit volumes of 1 - 500,000 m³ that have distributed over <5 m² to >0.5 km². These have occurred throughout at least Late Pleistocene to Holocene times and appear to have been triggered by such events as volcanic eruptions from the adjacent Okataina Volcanic Centre and related abrupt changes to the waterlevels of Lake Rotorua. Frequency and spatial distribution of HEs in historical times suggest human interference with the geothermal system is also a significant influence.

This study has brought together all records of known hydrothermal eruptions and other unusual geothermal disturbances in the Rotorua geothermal field. The information has plotted into GIS for use by statutory authorities and others. Two prehistorical HE deposits in Rotorua city have also been recognised and described for the first time, together with identification of their likely vent locations and possible eruption initiating events.

text: Geology, History and Stratigraphy of Hydrothermal Eruptions in the Rotorua Geothermal Field The study area is the Rotorua geothermal field (RGF), which is located in the southern end of the Rotorua caldera. Distribution of surface geothermal activity, hydrothermal eruption (HE) deposits and craters have been mapped. HE deposits formed in geological, historical and modern times were studied to record and describe their distribution, composition, petrography, lithology and stratigraphy.

Locations of all identified HE sites in the RGF have been plotted and shown on accompanying maps. At Ohinemutu and Sulphur Bay, HE breccias have been preserved only where deposits were subsequently silicified by hot spring outflows. At Whakarewarewa two HE breccias outcrop over about 0.5 km² and are up to 23 m thick. Study of stratigraphic relationships with tephras of known ages has determined one as Holocene (c. 20 ka) and one of Late Pleistocene age (c. 65 ka).

Four HE breccias were studied in detail. The mineral composition, physical description, field characteristics and spatial distribution of HE breccias are described and mapped. Clasts and matrix were examined by XRD analyses of whole (67) and clay fraction separates (16). Silica crystallinity indices (14) were determined by XRD to identify devitrification rates of opaline mineral species. The petrography of 67 breccia clasts and matrix samples were studied, and polished sections showed the only sulphide to be pyrite. Geothermal alteration of all prehistorical HE deposits was of advanced argillic to argillic and one modern day deposit was of sub propylitic epithermal alteration.

Study of a HE deposit formed in Kuirau Park on 26 January 2001 allowed properties and mineral composition to be examined and recorded before rapid oxidation and weathering destroyed its physical and mineral composition. Study of this and other twentieth century HE events confirms that these rapidly decompose to leave little or no recognisable deposit in the geological record.

Descriptions and all known historical records of HEs in the RGF have been collated to provide a comprehensive inventory of maps and appendices of these events. This information will greatly assist statutory authorities with mitigation of risk to lives and property from geothermal hazards as well as aid appropriate land use and emergency services planning.

Hydrothermal eruptions are ongoing in the RGF through time and produce craters 2 - 110m diameter with erupted deposit volumes of 1 - 500,000 m³ that have distributed over <5 m² to >0.5 km². These have occurred throughout at least Late Pleistocene to Holocene times and appear to have been triggered by such events as volcanic eruptions from the adjacent Okataina Volcanic Centre and related abrupt changes to the waterlevels of Lake Rotorua. Frequency and spatial distribution of HEs in historical times suggest human interference with the geothermal system is also a significant influence.

This study has brought together all records of known hydrothermal eruptions and other unusual geothermal disturbances in the Rotorua geothermal field. The information has plotted into GIS for use by statutory authorities and others. Two prehistorical HE deposits in Rotorua city have also been recognised and described for the first time, together with identification of their likely vent locations and possible eruption initiating events.

year: 2003

title: An examination of DHB climate change policy and implementation: Responsiveness to Māori health

authors: Powell, Elisha

abstract: The impacts of climate change have become increasingly evident throughout the world and in Aotearoa. Frequency and intensity of extreme weather events such as flooding, coastal erosion, wildfires, and droughts are notably increasing. Climate-related disasters have devastating effects on human health, as is well documented in literature. These effects include cardiovascular disease, poorer mental health, food insecurity and water borne disease. 

Due to pre-existing health disparities, Māori are particularly vulnerable to the health impacts of climate change. Further, Māori have unique relationships with whenua wherein destruction of the natural environment will have a negative impact on the health of Māori people and communities. The health sector has an obligation to respond to Māori health in a way that honours Māori relationships with the environment and prioritises equitable health outcomes for Māori in climate change policy. 

Although Māori face potentially severe health impacts due to climate change, there is limited literature that considers health sector climate change policy and its responsiveness to Māori health. In an effort to address this gap in literature, this thesis aims to examine whether there is existing District Health Board (DHB) policy focused on implementing institutional responses to climate change. Further, this research seeks to understand the extent to which any identified DHB climate change policy responds to Māori health. 

At the time of study, DHBs were responsible for providing and funding health services throughout Aotearoa. During the late stages of this research, the health sector underwent reform, and two health authorities have replaced DHBs. The implications of this research have important ramifications within the newly established health authorities. A dedicated Māori health authority will provide the health sector with the chance to advance health equity by acting on holistic understandings of health for Māori. These actions would establish health policy that recognises Māori health as fundamentally linked to the environment and therefore uniquely impacted by climate change. 

To achieve the aims of this thesis, two research methods were implemented. Initially, an environmental scan of 17 DHB websites was completed to identify climate change and Māori health policies. This was followed by qualitative interviews with three DHB staff from diverse localities. Additionally, tāngata whenua interviews from the wider research project named Haumanu Hauora, were analysed to ensure Māori understandings of climate change were included in this research (Masters-Awatere et al., 2022). 

Research findings provide insights that point to highly fragmented climate change policies across the health sector. There is a glaring lack of direction in the health sector's response to climate change throughout existing policy. Māori health policies were in place across all DHBs, however, lacked recognition of the interconnection between Māori health and the natural environment, and therefore the impacts of climate change. 

Although policy was fragmented across regions, there is potential to enhance both climate change and Māori health policies by recognising the interconnected nature of Māori health and climate change. This will necessitate a significant change in the health systems policy response to climate change that prioritises mātauranga Māori and addresses the ongoing impacts of colonisation.

text: An examination of DHB climate change policy and implementation: Responsiveness to Māori health The impacts of climate change have become increasingly evident throughout the world and in Aotearoa. Frequency and intensity of extreme weather events such as flooding, coastal erosion, wildfires, and droughts are notably increasing. Climate-related disasters have devastating effects on human health, as is well documented in literature. These effects include cardiovascular disease, poorer mental health, food insecurity and water borne disease. 

Due to pre-existing health disparities, Māori are particularly vulnerable to the health impacts of climate change. Further, Māori have unique relationships with whenua wherein destruction of the natural environment will have a negative impact on the health of Māori people and communities. The health sector has an obligation to respond to Māori health in a way that honours Māori relationships with the environment and prioritises equitable health outcomes for Māori in climate change policy. 

Although Māori face potentially severe health impacts due to climate change, there is limited literature that considers health sector climate change policy and its responsiveness to Māori health. In an effort to address this gap in literature, this thesis aims to examine whether there is existing District Health Board (DHB) policy focused on implementing institutional responses to climate change. Further, this research seeks to understand the extent to which any identified DHB climate change policy responds to Māori health. 

At the time of study, DHBs were responsible for providing and funding health services throughout Aotearoa. During the late stages of this research, the health sector underwent reform, and two health authorities have replaced DHBs. The implications of this research have important ramifications within the newly established health authorities. A dedicated Māori health authority will provide the health sector with the chance to advance health equity by acting on holistic understandings of health for Māori. These actions would establish health policy that recognises Māori health as fundamentally linked to the environment and therefore uniquely impacted by climate change. 

To achieve the aims of this thesis, two research methods were implemented. Initially, an environmental scan of 17 DHB websites was completed to identify climate change and Māori health policies. This was followed by qualitative interviews with three DHB staff from diverse localities. Additionally, tāngata whenua interviews from the wider research project named Haumanu Hauora, were analysed to ensure Māori understandings of climate change were included in this research (Masters-Awatere et al., 2022). 

Research findings provide insights that point to highly fragmented climate change policies across the health sector. There is a glaring lack of direction in the health sector's response to climate change throughout existing policy. Māori health policies were in place across all DHBs, however, lacked recognition of the interconnection between Māori health and the natural environment, and therefore the impacts of climate change. 

Although policy was fragmented across regions, there is potential to enhance both climate change and Māori health policies by recognising the interconnected nature of Māori health and climate change. This will necessitate a significant change in the health systems policy response to climate change that prioritises mātauranga Māori and addresses the ongoing impacts of colonisation.

year: 2025