title: Relationship between meteoric ¹⁰Be and NO₃⁻ concentrations in soils along Shackleton Glacier, Antarctica

authors: Diaz, Melisa A.

abstract: Outlet glaciers that flow through the Transantarctic Mountains (TAM) experienced changes in ice thickness greater than other coastal regions of Antarctica during glacial maxima. As a result, ice-free areas that are currently exposed may have been covered by ice at various points during the Cenozoic, complicating our understanding of ecological succession in TAM soils. Our knowledge of glacial extent on small spatial scales is limited for the TAM, and studies of soil exposure duration and disturbance, in particular, are rare. We collected surface soil samples and, in some places, depth profiles every 5 cm to refusal (up to 30 cm) from 11 ice-free areas along Shackleton Glacier, a major outlet glacier of the East Antarctic Ice Sheet. We explored the relationship between meteoric ¹⁰Be and NO₃⁻ in these soils as a tool for understanding landscape disturbance and wetting history and as exposure proxies. Concentrations of meteoric ¹⁰Be spanned more than an order of magnitude across the region (2.9×10⁸ to 73×10⁸ atoms g⁻¹) and are among the highest measured in polar regions. The concentrations of NO₃⁻ were similarly variable and ranged from ∼ μg g⁻¹ to 15 mg g⁻¹. In examining differences and similarities in the concentrations of ¹⁰Be and NO₃⁻ with depth, we suggest that much of the southern portion of the Shackleton Glacier region has likely developed under a hyper-arid climate regime with minimal disturbance. Finally, we inferred exposure time using ¹⁰Be concentrations. This analysis indicates that the soils we analyzed likely range from recent exposure (following the Last Glacial Maximum) to possibly >6 Myr. We suggest that further testing and interrogation of meteoric ¹⁰Be and NO₃⁻ concentrations and relationships in soils can provide important information regarding landscape development, soil evolution processes, and inferred exposure durations of surfaces in the TAM.

text: Relationship between meteoric ¹⁰Be and NO₃⁻ concentrations in soils along Shackleton Glacier, Antarctica Outlet glaciers that flow through the Transantarctic Mountains (TAM) experienced changes in ice thickness greater than other coastal regions of Antarctica during glacial maxima. As a result, ice-free areas that are currently exposed may have been covered by ice at various points during the Cenozoic, complicating our understanding of ecological succession in TAM soils. Our knowledge of glacial extent on small spatial scales is limited for the TAM, and studies of soil exposure duration and disturbance, in particular, are rare. We collected surface soil samples and, in some places, depth profiles every 5 cm to refusal (up to 30 cm) from 11 ice-free areas along Shackleton Glacier, a major outlet glacier of the East Antarctic Ice Sheet. We explored the relationship between meteoric ¹⁰Be and NO₃⁻ in these soils as a tool for understanding landscape disturbance and wetting history and as exposure proxies. Concentrations of meteoric ¹⁰Be spanned more than an order of magnitude across the region (2.9×10⁸ to 73×10⁸ atoms g⁻¹) and are among the highest measured in polar regions. The concentrations of NO₃⁻ were similarly variable and ranged from ∼ μg g⁻¹ to 15 mg g⁻¹. In examining differences and similarities in the concentrations of ¹⁰Be and NO₃⁻ with depth, we suggest that much of the southern portion of the Shackleton Glacier region has likely developed under a hyper-arid climate regime with minimal disturbance. Finally, we inferred exposure time using ¹⁰Be concentrations. This analysis indicates that the soils we analyzed likely range from recent exposure (following the Last Glacial Maximum) to possibly >6 Myr. We suggest that further testing and interrogation of meteoric ¹⁰Be and NO₃⁻ concentrations and relationships in soils can provide important information regarding landscape development, soil evolution processes, and inferred exposure durations of surfaces in the TAM.

year: 2021

title: Bioerosion on shore platforms developed in the Waitemata Formation, Auckland

authors: Healy, Terry R.

subjects: Auckland

abstract: Bioerosion - the removal of lithic substrate by the erosive activities of living organisms- has not previously been discussed for New Zealand shore platforms. This paper aims at drawing attention to bioerosion as a process active in shore platform development. Detailed reference is made to bioerosion occurring on the alternating sandstones and siltstones of the Waitemata Formation found outcropping on the coastline around Auckland. In this area several facets of shore platform morphology may be attributed to the direct effects of boring and browsing marine organisms. A classification of animals causing bioerosion, based on mechanism of erosion, is presented, and the geomorphic significance of the various groups discussed.

text: Bioerosion on shore platforms developed in the Waitemata Formation, Auckland Bioerosion - the removal of lithic substrate by the erosive activities of living organisms- has not previously been discussed for New Zealand shore platforms. This paper aims at drawing attention to bioerosion as a process active in shore platform development. Detailed reference is made to bioerosion occurring on the alternating sandstones and siltstones of the Waitemata Formation found outcropping on the coastline around Auckland. In this area several facets of shore platform morphology may be attributed to the direct effects of boring and browsing marine organisms. A classification of animals causing bioerosion, based on mechanism of erosion, is presented, and the geomorphic significance of the various groups discussed.

year: 1968

title: Kei ō tātou ringa te rongoa? Is the remedy already at hand?
The assertion and application of tikanga as a valid and credible response to contemporary issues.

authors: Taitoko, Mikaere

subjects: tikanga

abstract: This thesis examines the notion that tikanga is well positioned to address issues confronting Māori and other indigenous groups who strive to achieve self-determination and the freedom to be and to do.  This work is inspired by the late John Te Rangi-āniwaniwa Rangihau’s statement, “Ko te rongoā kei roto i ō tātau ringa” (1987, p. 24), which promotes the notion that through culture and identity Māori already have within their grasp the answers to contemporary matters of import in te ao Māori.  This thesis inverts that statement and presents it as a question querying whether indeed the remedy is at hand and, if so, could tikanga and cultural identity be that remedy.  To that end this study deliberately sets out to examine if the rongoa of self-determination, power and freedom can be achieved by the assertion and application of Māori ways of being and doing, that is to say by exercising tikanga.
Understanding notions of tikanga, sovereignty, and indigeneity is pivotal to this study as is articulating the notion of third space.  This thesis argues that these four notions are interconnected when considering ideas of self-determination for disempowered groups.  A case study forms a large part of this work and focuses on an indigenous group operating from a pre-contact tupuna worldview and based on He Whakaputanga o te Rangatiratanga o Nu Tireni 1835/Declaration of Independence of New Zealand 1835.  This particular group was chosen because it presented as being a point of intersect for the four notions of tikanga, sovereignty, indigeneity and the third space.
This thesis argues that whilst tikanga is a powerful mechanism for determining and rationalising ways of being and doing it has less to offer at a pragmatic level when it comes to effecting change in the status quo.  However, when overlaid with the third space lens new perspectives can be enunciated and new opportunities detected which in turn can lead to determining new actions.  Through this study it becomes clear that the assertion and application of tikanga contributes to, but on its own is not, the whole answer.

text: Kei ō tātou ringa te rongoa? Is the remedy already at hand?
The assertion and application of tikanga as a valid and credible response to contemporary issues. This thesis examines the notion that tikanga is well positioned to address issues confronting Māori and other indigenous groups who strive to achieve self-determination and the freedom to be and to do.  This work is inspired by the late John Te Rangi-āniwaniwa Rangihau’s statement, “Ko te rongoā kei roto i ō tātau ringa” (1987, p. 24), which promotes the notion that through culture and identity Māori already have within their grasp the answers to contemporary matters of import in te ao Māori.  This thesis inverts that statement and presents it as a question querying whether indeed the remedy is at hand and, if so, could tikanga and cultural identity be that remedy.  To that end this study deliberately sets out to examine if the rongoa of self-determination, power and freedom can be achieved by the assertion and application of Māori ways of being and doing, that is to say by exercising tikanga.
Understanding notions of tikanga, sovereignty, and indigeneity is pivotal to this study as is articulating the notion of third space.  This thesis argues that these four notions are interconnected when considering ideas of self-determination for disempowered groups.  A case study forms a large part of this work and focuses on an indigenous group operating from a pre-contact tupuna worldview and based on He Whakaputanga o te Rangatiratanga o Nu Tireni 1835/Declaration of Independence of New Zealand 1835.  This particular group was chosen because it presented as being a point of intersect for the four notions of tikanga, sovereignty, indigeneity and the third space.
This thesis argues that whilst tikanga is a powerful mechanism for determining and rationalising ways of being and doing it has less to offer at a pragmatic level when it comes to effecting change in the status quo.  However, when overlaid with the third space lens new perspectives can be enunciated and new opportunities detected which in turn can lead to determining new actions.  Through this study it becomes clear that the assertion and application of tikanga contributes to, but on its own is not, the whole answer.

year: 2013