In the northern South Island, the area northern Te Wai Pounamu (NTWP) is defined appropriate to a regional investigation of pre-European culture change. It is argued that the Maori sequence of this region is relevant to a range of interpretative problems in New Zealand�s archaeological past. Preparatory to this investigation, the international and New Zealand literature on culture change is reviewed. Two primary investigative foci of change are identified in NTWP; subsistence economy and stone tool manufacturing technology. A chronological scheme of Early, Middle and Late Periods based on firmly dated ecological events and/or independent radiocarbon ages is defined so as to order the archaeological data without recourse to unproven scenarios of cultural change and association. The Early Period subsistence economy is assessed in some detail. An Early Period settlement focus is documented along the eastern Tasman Bay coast in proximity to meta-argillite sources. Early Period midden remains suggest that several genera of seal and moa were exploited, and that people were fishing in eastern Tasman Bay during the warmer months of the year. From the Early Period fishhook assemblages of Tasman Bay, manufacturing change is inferred related to the increasing scarcity of moa bone over time. It is argued that lower Early Period settlement of the larger northern South Island was focused on the north-eastern coast to Rangitoto (D�Urville Island), while NTWP was characterized by smaller stone working communities operating in summer. In contrast, moa-free middens in Awaroa Inlet and Bark Bay of the western Tasman Bay granite coast present a physical dominance of Paphies australis, and finfish species suggesting, along with the dearth of Austrovenus stutchburyi, occupation outside of the warmer summer months. These middens also present an absence of seal and a paucity of bird bone, while sharing a robust 15th-16th centuries AD radiocarbon chronology. With the dearth of all bird species from granite coast middens in general, and evidence that the less preferred kokako (Callaeas c. cinerea) was caught during the occupation of Awaroa Inlet N26/214, it is suggested that cultural regulations beyond immediate subsistence needs were also operating at this time. From southern Tasman Bay, the archaeological investigation of the important Appleby site N27/118 suggests that the people associated with the extensive horticultural soils of Waimea West otherwise consumed finfish and estuarine shellfish in (non-summer) season, kiore (Rattus exulans), dog or kuri (Canis familiaris), and several small evidence of Maori tradition, archaeological charcoal, and the approximately 16th century radiocarbon chronology for N27/118 and the associated Appleby gravel borrow pit N27/122 places the advent of extensive Waimea horticulture within the post-moa, lower Middle Period Maori economy. The Haulashore Island archaeological assemblage of south-eastern Tasman Bay with a similar material culture to Appleby is also bereft of seal and any diagnostic moa bone. This Middle Period evidence is considered in a larger comparative perspective, where the absence of seal from 15th-16th centuries Tasman Bay middens is interpreted as a factor of human predation. A secure radiocarbon chronology suggests the convergence of this loss with the diminishment and loss of selected avifauna, and the subsequent advent of large horticultural complexes in the northern South Island compensated for the loss of faunal calories in a seasonally economy and a managed ecology. The evidence of stone tool use is also reviewed in some detail for NTWP, following the definition of an adze typology appropriate to the classification of meta-argillite tools. It is clear that meta-argillite is the dominant material of adze and (non-adze) flake tool manufacture throughout the Maori sequence of NTWP, while granite coast quartz remains generally subdominant. Beyound the apparent loss of the laterally-hafted adze, the evidence of adze change is generally subdominant. Beyond the apparent loss of the laterally-hafted adze, the evidence of adze change is generally reflected in shifting typological proportions, and in new manufacturing technologies and dressing techniques. Functional change may be inferred in the loss over time of large meta-argillite points and blade tools associated respectively with the manufacture of one-piece moa bone fishhooks and moa and seal butchery. The exclusive identification of hammer-dressed adzes with hump backs and steep bevels in Middle Period assemblages is related to the advent of horticultural intensification. More generally, adzes of the upper Early and Middle Periods are increasingly characterized by round sections, while hammer-dressing is employed more frequently and extensively reduced from riverine meta-argillite and recycled banks. Collectively, these changes reflect a developing emphasis on economy and opportunistic exploitation. From this interpretation, and evidence that meta-argillite adze length and the size of high quality Ohana source flakes diminish over time, it is suggested that accessible, high quality and appropriately shaped meta-argillite rock became increasingly scarce through intensive quarry manufacture. In conclusion, the coincidence of diminishing rock and faunal resources over time is related in a speculative anthropological model of culture change. It is proposed that the 14th-16th centuries Maori economy of NTWP, and by implication and inference, many other regions of New Zealand, was characterized by a resource crisis which either precipitated or reinforced a broader trajectory of culture change. It is suggested that influential leadears perceived a linkage in the loss of high quality rock and important subsistence fauna at this time, and that distinctive technologies, institutions and ideologies of Middle Period Maori society were influenced by, and/or developed from, this perception. Finally, it is recommended that the data of an archaeological Maori culture sequence be ordered and tested within a radiocarbon based chronological scheme, rather than the still generally used model of �Archaic� and �Classic� cultural periods. It is also suggested that New Zealand archaeologists should look beyond the functional-ecological imperative to consider more holistic anthropological explanations of change in the pre-European Maori past, with a focus on integrated regional sequences.

The economic impact of frost on agriculture remains a global problem. It is a particular concern for the New Zealand wine industry, where the consequences of an unexpected spring frost can be disastrous. Marlborough is located in the north-eastern corner of the South Island and is the largest grape-growing region in New Zealand. The region is surrounded by complex mountainous terrain that gives rise to extremes of climate, particularly large spatial variations of minimum temperature and the frequent occurrence of spring frost. The high spatial variation of near-surface minimum temperature can lead to under-preparedness among grape growers who rely on accurate frost forecasts as part of their frost mitigation systems. Field campaigns of the 1980’s and 90’s extended the understanding of the physical meteorological processes that affect cooling in complex terrain. More recent modelling efforts continue to refine this knowledge, although much less attention is given to the effects of different cooling processes on near-surface temperature. Agricultural developments in areas of complex terrain would benefit from an increased understanding of the meteorological processes that govern near-surface cooling, as this will help with the local prediction of frost. The spatial variation of near-surface minimum temperatures is first explored by identifying relationships with synoptic weather patterns using the Kidson (2000) synoptic classification scheme. Analysis revealed that Kidson types associated with the largest daily variations in near-surface minimum temperature (T, TNW and H) are not always associated with the occurrence of frost. Frost is more likely to occur during the cooler airflows of Kidson type HW, HNW and SW, or during the settled anticyclonic conditions that follow cooler airflows. The relationship between the spatial variation of near-surface minimum temperature and regional airflow patterns is explored using numerical weather prediction (NWP) modelling. Results indicated that a high σ Tmin around the region is a product of interaction between the region’s complex terrain and ambient meteorology, and it could occur in both settled weather and more dynamic synoptic conditions. A high regional σ Tmin during light ridge top winds could occur as a function of a location’s relative susceptibility to ventilation from thermally-induced drainage winds, and it may also occur as a result of the simultaneous ventilation and stagnation of near-surface air layers as synoptic wind interacts with local topography. The influence of the vertical structure of the nocturnal boundary layer (NBL) on nearsurface minimum temperature was investigated with the University of Canterbury Sonic Detection And Ranging (SODAR). Measurements confirmed the formation of low-level jets (LLJ’s) in the Awatere and Wairau Valleys during settled weather conditions, and that shear-induced turbulence beneath the jets was sufficient to mix warmer air to the surface and increase local temperatures. The process is sufficient to reduce frost risk to some of the region’s upper valleys during clear settled weather. In stronger ridge top winds development of the LLJ’s can be suppressed or eliminated and this was found to reduce shear-induced turbulence near the surface, allowing increased near-surface cooling. While results from this study are of greatest value to the prediction of near-surface minimum temperature and frost in Marlborough, the results could be applied to improved prediction of near-surface minimum temperature in complex terrain around the world. Further research could be directed toward the interaction of synoptic winds with thermally-induced airflows, as the transition zone between these wind systems is believed to govern the temporal and spatial evolution of near-surface stagnation, and this is related to episodes of strong near-surface cooling.

In the northern South Island, the area northern Te Wai Pounamu (NTWP) is defined appropriate to a regional investigation of pre-European culture change. It is argued that the Maori sequence of this region is relevant to a range of interpretative problems in New Zealand�s archaeological past. Preparatory to this investigation, the international and New Zealand literature on culture change is reviewed. Two primary investigative foci of change are identified in NTWP; subsistence economy and stone tool manufacturing technology. A chronological scheme of Early, Middle and Late Periods based on firmly dated ecological events and/or independent radiocarbon ages is defined so as to order the archaeological data without recourse to unproven scenarios of cultural change and association. The Early Period subsistence economy is assessed in some detail. An Early Period settlement focus is documented along the eastern Tasman Bay coast in proximity to meta-argillite sources. Early Period midden remains suggest that several genera of seal and moa were exploited, and that people were fishing in eastern Tasman Bay during the warmer months of the year. From the Early Period fishhook assemblages of Tasman Bay, manufacturing change is inferred related to the increasing scarcity of moa bone over time. It is argued that lower Early Period settlement of the larger northern South Island was focused on the north-eastern coast to Rangitoto (D�Urville Island), while NTWP was characterized by smaller stone working communities operating in summer. In contrast, moa-free middens in Awaroa Inlet and Bark Bay of the western Tasman Bay granite coast present a physical dominance of Paphies australis, and finfish species suggesting, along with the dearth of Austrovenus stutchburyi, occupation outside of the warmer summer months. These middens also present an absence of seal and a paucity of bird bone, while sharing a robust 15th-16th centuries AD radiocarbon chronology. With the dearth of all bird species from granite coast middens in general, and evidence that the less preferred kokako (Callaeas c. cinerea) was caught during the occupation of Awaroa Inlet N26/214, it is suggested that cultural regulations beyond immediate subsistence needs were also operating at this time. From southern Tasman Bay, the archaeological investigation of the important Appleby site N27/118 suggests that the people associated with the extensive horticultural soils of Waimea West otherwise consumed finfish and estuarine shellfish in (non-summer) season, kiore (Rattus exulans), dog or kuri (Canis familiaris), and several small evidence of Maori tradition, archaeological charcoal, and the approximately 16th century radiocarbon chronology for N27/118 and the associated Appleby gravel borrow pit N27/122 places the advent of extensive Waimea horticulture within the post-moa, lower Middle Period Maori economy. The Haulashore Island archaeological assemblage of south-eastern Tasman Bay with a similar material culture to Appleby is also bereft of seal and any diagnostic moa bone. This Middle Period evidence is considered in a larger comparative perspective, where the absence of seal from 15th-16th centuries Tasman Bay middens is interpreted as a factor of human predation. A secure radiocarbon chronology suggests the convergence of this loss with the diminishment and loss of selected avifauna, and the subsequent advent of large horticultural complexes in the northern South Island compensated for the loss of faunal calories in a seasonally economy and a managed ecology. The evidence of stone tool use is also reviewed in some detail for NTWP, following the definition of an adze typology appropriate to the classification of meta-argillite tools. It is clear that meta-argillite is the dominant material of adze and (non-adze) flake tool manufacture throughout the Maori sequence of NTWP, while granite coast quartz remains generally subdominant. Beyound the apparent loss of the laterally-hafted adze, the evidence of adze change is generally subdominant. Beyond the apparent loss of the laterally-hafted adze, the evidence of adze change is generally reflected in shifting typological proportions, and in new manufacturing technologies and dressing techniques. Functional change may be inferred in the loss over time of large meta-argillite points and blade tools associated respectively with the manufacture of one-piece moa bone fishhooks and moa and seal butchery. The exclusive identification of hammer-dressed adzes with hump backs and steep bevels in Middle Period assemblages is related to the advent of horticultural intensification. More generally, adzes of the upper Early and Middle Periods are increasingly characterized by round sections, while hammer-dressing is employed more frequently and extensively reduced from riverine meta-argillite and recycled banks. Collectively, these changes reflect a developing emphasis on economy and opportunistic exploitation. From this interpretation, and evidence that meta-argillite adze length and the size of high quality Ohana source flakes diminish over time, it is suggested that accessible, high quality and appropriately shaped meta-argillite rock became increasingly scarce through intensive quarry manufacture. In conclusion, the coincidence of diminishing rock and faunal resources over time is related in a speculative anthropological model of culture change. It is proposed that the 14th-16th centuries Maori economy of NTWP, and by implication and inference, many other regions of New Zealand, was characterized by a resource crisis which either precipitated or reinforced a broader trajectory of culture change. It is suggested that influential leadears perceived a linkage in the loss of high quality rock and important subsistence fauna at this time, and that distinctive technologies, institutions and ideologies of Middle Period Maori society were influenced by, and/or developed from, this perception. Finally, it is recommended that the data of an archaeological Maori culture sequence be ordered and tested within a radiocarbon based chronological scheme, rather than the still generally used model of �Archaic� and �Classic� cultural periods. It is also suggested that New Zealand archaeologists should look beyond the functional-ecological imperative to consider more holistic anthropological explanations of change in the pre-European Maori past, with a focus on integrated regional sequences.

Contemporary tourism planning recognises that an integrated and sustainable development approach includes the participation of local communities and residents. Success depends on community level capacity for innovation and leadership which are important variables for the creation and implementation of new ideas as part of the development process. The main aim of this research is to determine the capacity of stakeholders to support integration of tourism and aquaculture through development of a themed seafood tourism trail in the Nelson/Marlborough/Golden Bay region of New Zealand as a means to promote sustainable tourism. In 2005 the Marine Farming Association developed and published the “Top of the South Aquaculture and Seafood Trail” as a brochure for tourists to promote a positive image of aquaculture in the region. The Trail integrates local tourism providers, restaurants, accommodation, seafood retail, as well as harvesting and processing businesses (mussel farms) as part of a themed driving route linking several peripheral communities. Themed driving routes are an innovative means for providing destinations with the opportunity to bring tourists and associated economic outcomes to remote locations. There is strong economic dependence on aquaculture and tourism in the region with both industries generating a combined NZ$402 million annually in the Nelson Region alone. The research involved interviews with 22 local stakeholders regarding their perceptions about strengths, weaknesses, threats and opportunities associated with the Trail as part of a mixed method, case study approach. The results show that tourism and aquaculture in the region are well developed, but that there are weaknesses in networking and collaboration within and among industrial sectors. In addition, there are differing perceptions of the aquaculture and tourism industries. The role of the university has been important in building community capacity for research and strategic planning linked to the Trail.

La guerre de Succession d'Espagne, dernière guerre du règne de Louis XIV, est marquée par une série de défaites retentissantes : Blenheim (1704, Bavière), Ramillies et Turin (1706, Brabant et Piémont), Audenarde (1708, Flandre). L’approche qualifiée de « nouvelle histoire-bataille » permet de relativiser la vision traditionnelle qui explique ces défaites par le talent supérieur de John Churchill, duc de Marlborough, et du prince Eugène de Savoie, affrontant des généraux français courtisans et incompétents. Cette approche met l’événement-bataille au centre de l’étude et en aborde tous les aspects : dimensions politique, stratégique et tactique ; logistique ; techniques du combat et expériences ressenties sur le champ de bataille ; onde de choc.On constate que la guerre au début du XVIIIe siècle est à bien des égards limitée : les armées dépendent de leurs sources d’approvisionnement. Eugène et Marlborough, par leur audace et leur talent, accélèrent le rythme des opérations, mais sans renverser cet état de fait : aucune bataille n’est individuellement « décisive » et la guerre de Succession d'Espagne reste une guerre d’attrition. Les batailles sont le lieu d’une expérience du combat singulière, où se voient portées à leur paroxysme l’ensemble des formes d’affrontement et de violence que comporte la guerre de l’époque. Enfin, l’image d’une bataille se dégage lentement. Les courtisans doivent comparer nouvelles officielles, correspondances privées et gazettes pour comprendre ce qui s’est passé. Le roi mène des enquêtes pour déterminer qui a bien agi et qui a démérité. En définitive, c’est aux écrivains et aux artistes de fixer l’image que la postérité aura de ces batailles. / The war of the Spanish Succession is the last war fought by Louis XIV. It begins with a succession of astonishing defeats: Blenheim (Bavaria, 1704), Ramillies and Turin (Brabant and Piedmont, 1706), Audenarde (Flanders, 1708). The method known as “new battle-history” lets us temper the traditional vision, which claims that French have been defeated because their armies where led by courtiers that faced two military geniuses: John Churchill, duke of Marlborough, and Prince Eugene of Savoy. This historiographic approach focuses on the battle as an event, and seeks to treat it in all its dimensions: political, strategic and tactical aspects; logistics; how soldiers fight and what they feel; shock wave.Early eighteenth-century warfare is in many ways limited: armies highly rely on their supply sources. Eugene and Marlborough, thanks to their audacity and their talent, are able to speed up the operations, but without changing the way war is fought. There is no single “decisive” battle: the war of the Spanish Succession remains as a war of attrition. Battles are rare and formidable events where a singular fighting experience takes place; all contemporary kinds of combat and violence are to be observed. The importance of a battle is not immediately obvious. Its image takes time to come out. Versailles’ courtiers need to compare official news, private letters, French or foreign gazettes, in order to understand what happened. The king conducts investigations to identify the generals and units that have served well, and those that have not. In the end, it is writers and artists who are in charge of fixing what image of these battles will be left for posterity.

The North Bank area lies on the north side of the Wairau River, Marlborough, New Zealand, bounded by the Richmond Ranges to the north and the Wairau River to the south. The North Bank is an interactive zone where groundwaters and surface waters from North Bank tributary valleys mix with waters of the Wairau River. This investigation aimed to define the nature and origin of groundwaters of the North Bank area. Stable isotopes of oxygen and hydrogen, along with hydrogeochemistry, were utilised in order to define the spatial extent of the North Bank riparian margin and delineate the Wairau River-groundwater interface. Distinct stable isotopic signatures differentiate ground and surface waters that come from high mountain catchments versus those that arrive more locally at lower altitude. The results gathered by this study demonstrated stable isotopes to be the most powerful forensic tool capable of distinguishing Wairau River water from North Bank tributary groundwater sources. In contrast, hydrogeochemical characteristics of the waters of the North Bank were young and chemically dilute in nature, which made them chemically indistinguishable from waters of the Wairau River. Geomorphological mapping was conducted in order to investigate the relationship between groundwater flow patterns and geomorphology upon the North Bank. Geomorphology, in the form of prominent fluvial terraces, was found to play a role in limiting the extent of Wairau River influence to groundwater to either low-lying Q2 Speargrass Formation, Q1 Rapaura Formation alluvium or the Wairau River channel itself. Aquifer pump testing and water level observation carried out in the Waikakaho Valley revealed a plentiful groundwater resource in the local context. Like other tributary valleys within the North Bank study area, surface water and groundwater were found to be chemically and isotopically linked to one another which points to an interconnected ground and surface water resource, larger than first thought. Driven by recharge by the Waikakaho River, the groundwater resource has development potential, and continued monitoring will further define the hydrogeological system and ensure long term sustainable use.

Geomorphological and paleoseismic studies provide insight into the fault geometry and kinematics of a series of dextral northeast striking faults, including the Porters Pass, Hawdon, Bullock Hill, and Esk faults, in the South Island of New Zealand. These faults show post-glacial offsets that are significantly larger than predicted from co-seismic displacement - surface rupture length regressions derived from empirical relationships. Geomorphological mapping reveals slip rates as high as 9 mm/year for the Hawdon fault and Bullock Hill fault over an expected fault length of c. 140 km. Surface expressions of some parts of the studied faults are obscured by glacial gravels, indicating that blind faults are present in parts of the Sourthern Alps and may be the source for a component of a reported slip deficit in North Canterbury. Concluding from comparing scaling relationship results for the individual faults I hypothesize that the Porters Pass, Hawdon, Bullock Hill and Esk faults are segments of an incipient fault system that stretches from the western tip of the Porters Pass fault to the Hope fault, east of Hanmer Springs. Considering the location, similar strike and dextral deformation mode, I suggest that this 140 km long dextral strike-slip fault system marks the southernmost extension of the Marlborough Fault System resulting from the ongoing southward propagation of the Pacific-Australian plate boundary in New Zealand's South Island.

No description available.

In our ever more populated world, the rapid expansion and intensification of agriculture is driving worldwide biodiversity loss, and the interactions between production landscapes and wildlife conservation are becoming increasingly important. Farming systems depend on ecosystem services such as biological control, while conservationists are calling for the establishment of conservation initiatives in non-preserve landscapes. Despite this, the goals of agriculture and the goals of predator-conservation are rarely mutual. Here, I demonstrate one of the first examples of a mutually beneficial scenario between agriculture and predator conservation. I used, as a case study, a reintroduction project that translocated individuals of the threatened New Zealand falcon (Falco novaeseelandiae) from the hills of Marlborough into vineyards, to determine if predators can survive within an agricultural landscape while simultaneously providing that landscape with biological control services. Examples of vertebrates providing biological control to agriculture are rare. I show that the presence of falcons in vineyards caused an economically important reduction in grape damage worth over US $230/ ha. Falcon presence caused a 78- 83% reduction in the number of introduced European pest birds, which resulted in a 95% reduction in the damage caused by these species. Falcon presence did not cause a reduction in the abundance of the native silvereye (Zosterops lateralis), but did halve the damage caused by this species. To assess the conservation value of the falcon translocations, I used remote videography, direct observations and prey analysis to measure the behavioural changes associated with the relocation of falcons from their natural habitat in the hills and into vineyards. Falcons in vineyard nests had higher nest attendance, higher brooding rates, and higher feeding rates than falcons in hill nests. Additionally, parents in vineyard nests fed their chicks a greater amount of total prey and larger prey items compared to parents in hill nests. I also found an absence of any significant diet differences between falcons in hill and vineyard habitats, suggesting that the latter may be a suitable alternative habitat for falcons. Because reintroduced juvenile falcons were released in areas devoid of adult falcons, it was possible that they were missing essential training normally provided by their parents. I used direct observations to demonstrate that the presence of siblings had similar effects to the presence of parents on the development of juvenile behaviour, with individuals flying, hunting, and playing more often when conspecifics were present. Finally, through the use of artificial nests and remote videography, I identified that falcons nesting in vineyards are likely to suffer lower predation rates. I also found that falcons in vineyards are predated by a less dangerous suite of animals (such as hedgehogs, Erinaceus europaeus, and avian predators), than their counterparts in the hills, which are predated by more voracious species (such as stoats, Mustela erminea, and feral cats, Felis catus). The work presented in this thesis has also added to the current knowledge of New Zealand falcon breeding behaviour, prey preferences, and behavioural development. Although agricultural regions globally are rarely associated with raptor conservation, and the ability of raptors to control the pests of agricultural crops has not been previously quantified, these results suggest that translocating New Zealand falcons into vineyards has potential for both the conservation of this species, and for providing biological control services to agriculture

Much public attention has been given lately to the concept of sustainability, a notion which is increasingly viewed as a desirable goal of viticulture development and environmental management. The emergence of the sustainability concept has seen a concomitant rise in the interest of its measurement. It has been suggested that through the analysis of regulatory and non-regulatory methods, the attainment of how sustainable freshwater use in vineyards can be assessed. Regulation has to date been the policy tool of choice in regards to environmental protection. While regulation is often necessary, non-regulatory approaches may, in some circumstances, serve as useful supplements to an effective regulatory regime. There are a number of stages to achieving the aim of this research. The first is designed at galvanising New Zealand‟s will to stride out down the sustainability road through the development of the sustainable vineyard concept. Investigations into regulatory freshwater policies were undertaken to assess the relative efficacy of such methods in guiding vineyards in sustainable freshwater use. The research then explored the elements of freshwater use as they relate to non-regulatory methods for achieving sustainable environmental outcomes. Qualitative research was undertaken through the instigation of an email questionnaire and semi-structured interviews to provide an understanding of freshwater use in vineyards within Marlborough. The research focuses on the discussion of the methodological considerations which are important in developing a working framework for assessing how vineyards achieve sustainable freshwater use. The ideal properties and characteristics of sustainability are identified and critically examined. An evaluation of the different types of regulatory and non-regulatory policies on freshwater management are considered. Both regulatory and non-regulatory methods were seen to be significant in developing an operational framework, as they are capable of representing the management of freshwater use and sustainability practices in vineyards. It is observed that the policy goal of both regulatory and non-regulatory organisations in achieving sustainable freshwater outcomes generally cannot be attained to the full satisfaction of all the dimensions of sustainability. Rather, sustainable freshwater use could be considered as a „road‟ and not a fixed destination. Along the way, trade-offs and balances have to be made. It is up to individual vineyard managers to weight the various alternatives, with the policy and decision makers providing information upon which rational choices can be based. This research demonstrates the efficacy of regulatory and non-regulatory methods in guiding sustainable environmental outcomes. It appears that the „ideals‟ of policies, as outlined in the literature and data collected, recommend an overall adaptive management approach if achieving sustainable freshwater use is the ultimate goal.