title: Sedimentation And Hydrodynamics of Whitianga Estuary

authors: Reeve, Glen M.D

subjects: Hydrodynamics

abstract: Whitianga Estuary is a bayhead barrier type estuary located on the east of the Coromandel Peninsula, North Island, New Zealand. The catchment has undergone many land-use changes since pre-European settlement. In some areas of the catchment land-use has changed from native forest to grasslands to forestry and back to pasture. These changes in catchment land-use all contribute to increased sedimentation into the estuary. Development of the estuary itself has also occurred in recent times. Much growth has been focussed around the estuary due to Whitianga town-ship having a large boating community, and includes a 170 berth marina and wharf situated at
the tidal inlet entrance to the estuary. These, and the extensive canal development engineering works can have substantial impacts on the
sedimentation regime, and may modify tidal circulation, flushing, and sediment deposition within the estuary.

The principle aim of this research is to assess hydrodynamics and sedimentation of the estuary for future management and development purposes, and also to model different scenarios in order to determine the most cost effective, and least obtrusive design for a proposed boat-ramp and
approach channel near the marina.

To determine sedimentation rates, sediment cores from four locations were collected to depths of 1 m. Coring locations were chosen based on
preliminary model run results, selecting areas that appeared to be long-term sediment sinks of a stable nature. Cores were divided into 10 mm sections and prepared for 210Pb dating and heavy metal analysis, to make an assessment of the vertical sedimentation rates. Recent sedimentation rates were found to be as high as 9 mm/yr post-1950s and past sedimentation rates
as high as 30 mm/yr pre-1950s. The use of heavy metal analysis for dating proved difficult as the background levels of the conservative elements used to normalise results varied, making the geochemical analysis approach inappropriate.

As bathymetry is one of the most important aspects of modelling, a large amount of surveying was undertaken for this study. LiDAR, singlebeam data, and recent rectified aerial photographs were interpreted for the creation of a
bathymetric grid file to be used for hydrodynamic modelling of the estuary.

The 3DD numerical model was used to determine tidal flows and current velocities. From this initial hydrodynamic model a particle-tracking model was created to determine sediment transport pathways within the estuary. From the initial 20 m model it was then possible to create a number of nested model grids for the purpose of determining the best practice scenario for the
creation of a proposed boat ramp and associated approach channel near the harbour entrance. Hydrodynamic results suggest that residual circulation in Whitianga Estuary is nearly in balance, with a low ebb tidal domination present. Particle tracking results suggest that sediment entrained and carried into and within the estuary will accumulate on the intertidal flats. Sediment
transport modelling indicates that the impact of a proposed boat-ramp will result in sedimentation of the dredged approach channel due to reductions in residual and tidal velocities.

text: Sedimentation And Hydrodynamics of Whitianga Estuary Whitianga Estuary is a bayhead barrier type estuary located on the east of the Coromandel Peninsula, North Island, New Zealand. The catchment has undergone many land-use changes since pre-European settlement. In some areas of the catchment land-use has changed from native forest to grasslands to forestry and back to pasture. These changes in catchment land-use all contribute to increased sedimentation into the estuary. Development of the estuary itself has also occurred in recent times. Much growth has been focussed around the estuary due to Whitianga town-ship having a large boating community, and includes a 170 berth marina and wharf situated at
the tidal inlet entrance to the estuary. These, and the extensive canal development engineering works can have substantial impacts on the
sedimentation regime, and may modify tidal circulation, flushing, and sediment deposition within the estuary.

The principle aim of this research is to assess hydrodynamics and sedimentation of the estuary for future management and development purposes, and also to model different scenarios in order to determine the most cost effective, and least obtrusive design for a proposed boat-ramp and
approach channel near the marina.

To determine sedimentation rates, sediment cores from four locations were collected to depths of 1 m. Coring locations were chosen based on
preliminary model run results, selecting areas that appeared to be long-term sediment sinks of a stable nature. Cores were divided into 10 mm sections and prepared for 210Pb dating and heavy metal analysis, to make an assessment of the vertical sedimentation rates. Recent sedimentation rates were found to be as high as 9 mm/yr post-1950s and past sedimentation rates
as high as 30 mm/yr pre-1950s. The use of heavy metal analysis for dating proved difficult as the background levels of the conservative elements used to normalise results varied, making the geochemical analysis approach inappropriate.

As bathymetry is one of the most important aspects of modelling, a large amount of surveying was undertaken for this study. LiDAR, singlebeam data, and recent rectified aerial photographs were interpreted for the creation of a
bathymetric grid file to be used for hydrodynamic modelling of the estuary.

The 3DD numerical model was used to determine tidal flows and current velocities. From this initial hydrodynamic model a particle-tracking model was created to determine sediment transport pathways within the estuary. From the initial 20 m model it was then possible to create a number of nested model grids for the purpose of determining the best practice scenario for the
creation of a proposed boat ramp and associated approach channel near the harbour entrance. Hydrodynamic results suggest that residual circulation in Whitianga Estuary is nearly in balance, with a low ebb tidal domination present. Particle tracking results suggest that sediment entrained and carried into and within the estuary will accumulate on the intertidal flats. Sediment
transport modelling indicates that the impact of a proposed boat-ramp will result in sedimentation of the dredged approach channel due to reductions in residual and tidal velocities.

year: 2008

title: Medios compositivos y nuevas formas de experiencia perceptiva en la poesía experimental española actual

authors: Lopez-Fernandez, Laura

abstract: La naturaleza híbrida y heterogénea de los modos poéticos experimentales —poéticas no versificadas y no declamatorias— constituye un rasgo distintivo de este macrogénero, el cual requiere para un mejor entendimiento un marco teórico apropiado y una revisión de las nociones convencionales de lírica, representación y discursividad. En este estudio se revisan estas nociones dentro del contexto poético español del siglo XXI y se presenta un nuevo modo de acercamiento a estas textualidades alteradas donde se subraya la no linealidad, los lenguajes no verbales y la tecnología como herramientas integrales en el proceso de creación y descodificación de estos múltiples modos compositivos.

text: Medios compositivos y nuevas formas de experiencia perceptiva en la poesía experimental española actual La naturaleza híbrida y heterogénea de los modos poéticos experimentales —poéticas no versificadas y no declamatorias— constituye un rasgo distintivo de este macrogénero, el cual requiere para un mejor entendimiento un marco teórico apropiado y una revisión de las nociones convencionales de lírica, representación y discursividad. En este estudio se revisan estas nociones dentro del contexto poético español del siglo XXI y se presenta un nuevo modo de acercamiento a estas textualidades alteradas donde se subraya la no linealidad, los lenguajes no verbales y la tecnología como herramientas integrales en el proceso de creación y descodificación de estos múltiples modos compositivos.

year: 2014

title: Ahumoana tawhito (ancient aquaculture): The translocation of  toheroa (Paphies ventricosa) and other marine species by Māori

authors: Taikato, Vanessa Rona

subjects: Mātauranga

abstract: Throughout time, humans have cultivated and translocated plants and animals. Ancient mariculture (the cultivation of marine species) often leaves little trace of human agency. Consequently, the extent to which mariculture was used in the distant past largely remains a mystery. In Aotearoa (New Zealand), Māori have a long history of translocating and cultivating terrestrial and freshwater species. Increasingly, it is becoming apparent that the translocation of marine species is a resource management tool that has been utilized by Māori for hundreds of years. Research into the population genetic structure of a large surf clam endemic to Aotearoa, the toheroa (Paphies ventricosa), has led to the hypothesis that Māori have undertaken long-distance transport and translocation of this shellfish during the earlier phases of Māori occupation within Aotearoa. Specifically, this “translocation hypothesis” suggests that Māori successfully transported toheroa from the West Coast of Te ika-a-Māui (the North Island) to the South Coast of Te Waipounamu (the South Island) thereby explaining the unique and disjunct distribution pattern of this taonga (treasured) species. This thesis weaves together knowledge from multiple disciplines to test the toheroa translocation hypothesis, explore technologies used by Māori and reclaim traditional knowledge regarding resource management. 

An examination of archaeological databases revealed a record that was not consistent with toheroa being endemic to Murihiku (southern South Island). On the west coast of Te Ika-a-Māui, 968 midden records were identified of which 40% either contained or consisted entirely of toheroa. In contrast, along the South Coast of Murihiku (Southland, Te Waipounamu), 122 midden records were examined, of which only 6.5% contained toheroa. Toheroa were not a major component of any of these middens. Toheroa were also absent from a natural shell deposit within Murihiku that pre-dates human arrival to Aotearoa. The general absences of toheroa in all but a few southern middens lends itself to the notion that toheroa did not occur there naturally, but were introduced by Māori at a later date. 

An examination of anthropological, historical and traditional knowledge was conducted to explore the human elements of toheroa translocation. Specifically, I wanted to better understand the reasons why early-Māori might have wanted to translocate toheroa, as well as the capacity and opportunities they would have had to undertake such long-distance transport of live bivalves. The movement of iwi from the north to the south is a concept steeped in kōrero tuku iho (oral history) and is referred to many times in ethnohistorical and contemporary literature. This included the very first movements of Polynesian explorers north to south, as well as multiple accounts of expeditions and southward migrations by Māori originating from the north. Toheroa were an important resource for the earliest occupants of northern regions in Aotearoa and this is evident in the prominence of toheroa in northern Māori culture. Interestingly, while they are a taonga of southern Māori today, toheroa are conspicuously absent in the narratives, whakataukī (proverbs) and whakapapa (genealogy) of Murihiku (Southland). This could be explained by a later introduction of toheroa to the area, leading to less time and opportunity of the resource to shape southern Māori identity. While toheroa may not have been endemic to the south, there was ample opportunity for them to be relocated, either through trade, or as part of a southward migration. Archaeological records of industrial stone, such as obsidian, provide evidence for trade between northern and southern Māori as early as the 14th century. It is clear that people who had come from or were closely connected to northern Māori have occupied the southern most areas of Aotearoa, in the earliest phases of the prehistoric sequence. 
While it is apparent that the opportunity for shellfish translocation existed, the suitability of toheroa for relocation was unknown. This would depend on their ability to cope with and combat stressors (such as hypoxia, bacterial proliferation, starvation and desiccation) associated with such a journey. Respiration rates, morphometric indices, behavioural responses and physiological responses to these stressors were measured in a series of in situ experiments. Toheroa displayed an overall physiological robustness to lack of oxygen and food and, when held in seawater and treated with antibiotics, toheroa were able to switch to anaerobiosis and survive for extended periods of time (more than two weeks). The primary causes of health deterioration were found to be bacterial proliferation (of particular prevalence when held in anoxic water) and desiccation. These are risks that could easily have been mitigated during a translocation journey.

The pōhā, a natural kelp bag fashioned from the large brown alga Durvillaea spp., is a southern Māori technology said to have been used in the translocation and re-seeding of toheroa and other shellfish species, prehistorically. An important first step in understanding this technology was to review the traditional knowledge associated with pōhā and of rimurapa (southern Bull Kelp) from which pōhā are constructed. The literature contained a variety of information covering prehistoric practices to contemporary management of this natural resource as well as details of its wide and varied uses. Interestingly, contemporary use of pōhā and rimurapa has included translocation and restoration of seagrass in Te Waipounamu. 

While there are many historical references to pōhā being used for translocating shellfish, the details of exactly how they were used are missing, both in the literature and in the memories of traditional practitioners of pōhā with whom I have been lucky enough to speak with. Consequently, the final component of this thesis explored the biochemical and bacterial implications of holding live toheroa in pōhā. I found that the photosynthetic blades of the algae were able to replenish dissolved oxygen consumed by the toheroa during respiration. Furthermore, it was clear that the microbiome associated with pōhā, or the secondary metabolites released by pōhā, influenced the bacterial community to which toheroa were exposed when held within the algal bags. From these experiments, it appears unlikely that pōhā were used in the manner employed in this experiment (filled with seawater and left to stagnate) as this resulted in the rapid deterioration of the pōhā bags. However, the biochemical and bacterial results that were found, have direct implications for the functionality of pōhā and the toheroa held within. While possibly not the main vessel in which toheroa were translocated, kōrero tuku iho about the use of pōhā in shellfish re-seeding, suggest that raw pōhā may have been the last link in the chain of shellfish translocation by providing protection while acclimating to a new area. 

The research I have undertaken for this thesis is novel and it contributes to our growing understanding of indigenous resource management in Aotearoa. While I have not been able to determine definitively whether toheroa in the south are solely a consequence of Māori translocation, the evidence presented here is consistent with that hypothesis. The experiments undertaken here are the first of their kind for toheroa, and they highlight how the complex nature of surf clam physiology and behaviour would play into their cultivation, either in ancient or contemporary contexts. This thesis reclaims traditional knowledge regarding the management of two taonga species (toheroa and rimurapa) and highlights several possible avenues for future research. Furthermore, this research demonstrates how academic knowledge and indigenous knowledge can be interwoven, to attempt to unravel the mysteries of the past and to pave the way for the future.

text: Ahumoana tawhito (ancient aquaculture): The translocation of  toheroa (Paphies ventricosa) and other marine species by Māori Throughout time, humans have cultivated and translocated plants and animals. Ancient mariculture (the cultivation of marine species) often leaves little trace of human agency. Consequently, the extent to which mariculture was used in the distant past largely remains a mystery. In Aotearoa (New Zealand), Māori have a long history of translocating and cultivating terrestrial and freshwater species. Increasingly, it is becoming apparent that the translocation of marine species is a resource management tool that has been utilized by Māori for hundreds of years. Research into the population genetic structure of a large surf clam endemic to Aotearoa, the toheroa (Paphies ventricosa), has led to the hypothesis that Māori have undertaken long-distance transport and translocation of this shellfish during the earlier phases of Māori occupation within Aotearoa. Specifically, this “translocation hypothesis” suggests that Māori successfully transported toheroa from the West Coast of Te ika-a-Māui (the North Island) to the South Coast of Te Waipounamu (the South Island) thereby explaining the unique and disjunct distribution pattern of this taonga (treasured) species. This thesis weaves together knowledge from multiple disciplines to test the toheroa translocation hypothesis, explore technologies used by Māori and reclaim traditional knowledge regarding resource management. 

An examination of archaeological databases revealed a record that was not consistent with toheroa being endemic to Murihiku (southern South Island). On the west coast of Te Ika-a-Māui, 968 midden records were identified of which 40% either contained or consisted entirely of toheroa. In contrast, along the South Coast of Murihiku (Southland, Te Waipounamu), 122 midden records were examined, of which only 6.5% contained toheroa. Toheroa were not a major component of any of these middens. Toheroa were also absent from a natural shell deposit within Murihiku that pre-dates human arrival to Aotearoa. The general absences of toheroa in all but a few southern middens lends itself to the notion that toheroa did not occur there naturally, but were introduced by Māori at a later date. 

An examination of anthropological, historical and traditional knowledge was conducted to explore the human elements of toheroa translocation. Specifically, I wanted to better understand the reasons why early-Māori might have wanted to translocate toheroa, as well as the capacity and opportunities they would have had to undertake such long-distance transport of live bivalves. The movement of iwi from the north to the south is a concept steeped in kōrero tuku iho (oral history) and is referred to many times in ethnohistorical and contemporary literature. This included the very first movements of Polynesian explorers north to south, as well as multiple accounts of expeditions and southward migrations by Māori originating from the north. Toheroa were an important resource for the earliest occupants of northern regions in Aotearoa and this is evident in the prominence of toheroa in northern Māori culture. Interestingly, while they are a taonga of southern Māori today, toheroa are conspicuously absent in the narratives, whakataukī (proverbs) and whakapapa (genealogy) of Murihiku (Southland). This could be explained by a later introduction of toheroa to the area, leading to less time and opportunity of the resource to shape southern Māori identity. While toheroa may not have been endemic to the south, there was ample opportunity for them to be relocated, either through trade, or as part of a southward migration. Archaeological records of industrial stone, such as obsidian, provide evidence for trade between northern and southern Māori as early as the 14th century. It is clear that people who had come from or were closely connected to northern Māori have occupied the southern most areas of Aotearoa, in the earliest phases of the prehistoric sequence. 
While it is apparent that the opportunity for shellfish translocation existed, the suitability of toheroa for relocation was unknown. This would depend on their ability to cope with and combat stressors (such as hypoxia, bacterial proliferation, starvation and desiccation) associated with such a journey. Respiration rates, morphometric indices, behavioural responses and physiological responses to these stressors were measured in a series of in situ experiments. Toheroa displayed an overall physiological robustness to lack of oxygen and food and, when held in seawater and treated with antibiotics, toheroa were able to switch to anaerobiosis and survive for extended periods of time (more than two weeks). The primary causes of health deterioration were found to be bacterial proliferation (of particular prevalence when held in anoxic water) and desiccation. These are risks that could easily have been mitigated during a translocation journey.

The pōhā, a natural kelp bag fashioned from the large brown alga Durvillaea spp., is a southern Māori technology said to have been used in the translocation and re-seeding of toheroa and other shellfish species, prehistorically. An important first step in understanding this technology was to review the traditional knowledge associated with pōhā and of rimurapa (southern Bull Kelp) from which pōhā are constructed. The literature contained a variety of information covering prehistoric practices to contemporary management of this natural resource as well as details of its wide and varied uses. Interestingly, contemporary use of pōhā and rimurapa has included translocation and restoration of seagrass in Te Waipounamu. 

While there are many historical references to pōhā being used for translocating shellfish, the details of exactly how they were used are missing, both in the literature and in the memories of traditional practitioners of pōhā with whom I have been lucky enough to speak with. Consequently, the final component of this thesis explored the biochemical and bacterial implications of holding live toheroa in pōhā. I found that the photosynthetic blades of the algae were able to replenish dissolved oxygen consumed by the toheroa during respiration. Furthermore, it was clear that the microbiome associated with pōhā, or the secondary metabolites released by pōhā, influenced the bacterial community to which toheroa were exposed when held within the algal bags. From these experiments, it appears unlikely that pōhā were used in the manner employed in this experiment (filled with seawater and left to stagnate) as this resulted in the rapid deterioration of the pōhā bags. However, the biochemical and bacterial results that were found, have direct implications for the functionality of pōhā and the toheroa held within. While possibly not the main vessel in which toheroa were translocated, kōrero tuku iho about the use of pōhā in shellfish re-seeding, suggest that raw pōhā may have been the last link in the chain of shellfish translocation by providing protection while acclimating to a new area. 

The research I have undertaken for this thesis is novel and it contributes to our growing understanding of indigenous resource management in Aotearoa. While I have not been able to determine definitively whether toheroa in the south are solely a consequence of Māori translocation, the evidence presented here is consistent with that hypothesis. The experiments undertaken here are the first of their kind for toheroa, and they highlight how the complex nature of surf clam physiology and behaviour would play into their cultivation, either in ancient or contemporary contexts. This thesis reclaims traditional knowledge regarding the management of two taonga species (toheroa and rimurapa) and highlights several possible avenues for future research. Furthermore, this research demonstrates how academic knowledge and indigenous knowledge can be interwoven, to attempt to unravel the mysteries of the past and to pave the way for the future.

year: 2021