Relevant bibliographies by topics / Central Otago

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Central Otago'

Author: Grafiati
Published: 4 June 2021
Last updated: 29 January 2023

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Journal articles on the topic "Central Otago"

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Clark, R. G., C. J. Mulvaney, D. M. Dodd, R. F. Bishop, and G. A. Walker. "Sheep cobalt deficiency in Central Otago." New Zealand Veterinary Journal 44, no. 1 (February 1996): 37–38. http://dx.doi.org/10.1080/00480169.1996.35930.

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Lo, P. L., and J. T. S. Walker. "Annual and regional variability in adult Dasineura mali (apple leafcurling midge) emergence in New Zealand." New Zealand Plant Protection 70 (August 8, 2017): 131–36. http://dx.doi.org/10.30843/nzpp.2017.70.38.

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Apple leafcurling midge is an important quarantine pest for New Zealand apple exports. Season-long pheromone trapping was conducted in Hawke’s Bay and Nelson from 2004—2017, and from 2012—2017 in Central Otago. Four generations occurred annually in Hawke’s Bay and Nelson and 3—4 in Central Otago. In Hawke’s Bay and Nelson, the timing of each peak varied by about 3—4 weeks between years, while the difference was ~2—3 weeks in Central Otago during fewer years of monitoring. Hawke’s Bay was up to a month earlier than Central Otago for the same peak within individual years. The major factor behind
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Stevens, D. R., and J. P. Garden. "Challenges facing the farmers of Central Otago." Proceedings of the New Zealand Grassland Association 76 (January 1, 2014): 25–28. http://dx.doi.org/10.33584/jnzg.2014.76.2957.

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The Central Otago region, with its cold winters and hot summers, and valley floors with uplift mountains is definitely "a world of difference". At the NZGA conference in Alexandra in 1966 John Hercus stated "Central Otago has a lure which sets it apart from the rest of New Zealand. Its characteristics of geology, topography and climate, its history of occupation and exploitation, its scenery at once forbidding and yet strangely fascinating - these features combine to cast a spell which few who have been exposed, can ever fully escape" (Hercus 1966). The region and its high country have an icon
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Buchanan, L. "APRICOT PRODUCTION IN CENTRAL OTAGO, NEW ZEALAND." Acta Horticulturae, no. 192 (November 1986): 113–22. http://dx.doi.org/10.17660/actahortic.1986.192.19.

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Dawber, K. R., and G. M. Drinkwater. "Windfarm prospects in central Otago, New Zealand." Renewable Energy 9, no. 1-4 (September 1996): 802–5. http://dx.doi.org/10.1016/0960-1481(96)88404-7.

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Mackenzie, D. J., and D. Craw. "Structural and lithological continuity and discontinuity in the Otago Schist, Central Otago, New Zealand." New Zealand Journal of Geology and Geophysics 48, no. 2 (June 2005): 279–93. http://dx.doi.org/10.1080/00288306.2005.9515115.

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Denys, P., C. Pearson, R. Norris, and M. Denham. "A geodetic study of Otago: results of the central Otago deformation network 2004–2014." New Zealand Journal of Geology and Geophysics 59, no. 1 (January 2, 2016): 147–56. http://dx.doi.org/10.1080/00288306.2015.1134592.

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Wills, Barrie J. "Central Otago - Built on gold, growing on grass." Proceedings of the New Zealand Grassland Association 76 (January 1, 2014): 15–23. http://dx.doi.org/10.33584/jnzg.2014.76.2950.

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A warm welcome to our "World of Difference" to all delegates attending this conference - we hope your stay is enjoyable and that you will leave Central Otago with an enhanced appreciation of the diversity of land use and the resilient and growing economic potential that this region has to offer. Without regional wellbeing the national economy will struggle to grow, something Central Government finally seems to be realising, and the Central Otago District Council Long Term Plan 2012-2022 (LTP) signals the importance of establishing a productive economy for the local community which will aid in
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Ashley, P. M., and D. Craw. "Carrick Range Au and Sb mineralisation in Caples Terrane, Otago Schist, Central Otago, New Zealand." New Zealand Journal of Geology and Geophysics 38, no. 2 (April 1995): 137–49. http://dx.doi.org/10.1080/00288306.1995.9514646.

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Smith, L. C., K. D. Trainor, and J. D. Morton. "Nutrient requirements for irrigated lucerne in Central Otago." Proceedings of the New Zealand Grassland Association 76 (January 1, 2014): 97–104. http://dx.doi.org/10.33584/jnzg.2014.76.2966.

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Abstract Two field trials were commenced in September 2000 on newly sown irrigated lucerne near Tarras in Central Otago. The first trial measured the effects of phosphorus (P) (0, 30, 60, 120 kg P/ha) and potassium (K) (0, 50, 100, 200 kg K/ha) fertiliser applications while the second trial determined nitrogen (N) requirements for lucerne establishment. Initial soil test levels (0-75 mm) were pH 5.6, Olsen P 15 μg/ml; quicktest (QT) K 6 and sodium tetra-phenol-boron extractable K (TBK) 3.1. Lucerne production averaged 9.5 t dry matter (DM)/ha in the establishment year, 15.6 t DM/ ha in Year 2
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Dissertations / Theses on the topic "Central Otago"

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Nicol, Ryan Charles Smith. "Hydrogeology of the Cromwell Terrace Aquifer, Central Otago." Thesis, University of Canterbury. Geological Sciences, 2011. http://hdl.handle.net/10092/6431.

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A hydrogeologic model, groundwater chemistry and stable isotopic analysis were used to establish recharge resources and outflows so a water balance could be developed for the Cromwell Terrace Aquifer (CTA) in Central Otago, New Zealand. Increased popularity of the Central Otago region for viticulture, orcharding and tourism, has resulted in an increased demand for water. Groundwater is a viable option to meet this demand for water. The CTA is a single unconfined aquifer contained within a thin veneer of permeable Quaternary glacial outwash gravels that range in thickness between 10 and 50m. T
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Dowsett, O. "'Rural restructuring' : a multi-scalar analysis of the Otago Central Rail Trail." Lincoln University, 2008. http://hdl.handle.net/10182/669.

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‘Rural restructuring’ has frequently been used to indicate the magnitude, and conceptualise the nature, of contemporary change in the countryside. Most notably, concern has focused upon the fundamental changes in economic and social organisation brought about by the increasing leverage of consumption-based activity as a path to rural development. By drawing on the relevant literature, however, I suggest in this thesis that the use of ‘rural restructuring’ as a conceptual framework has been inconsistent. The issue of scale is a case in point with scholars positioning their studies of rural chan
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Carpenter, Lloyd. "Rich in Myth, Gold and Narrative: Aspects of the Central Otago Gold Rush, 1862-2012." Thesis, University of Canterbury. Humanities, 2013. http://hdl.handle.net/10092/8034.

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Abstract 150 years ago, the carefully-planned Presbyterian settlement of Dunedin was torn apart by the discovery that nearly every stream in Otago was laden with gold. The population exploded, adding the accents of Greece, Tipperary, Victoria, California, Guangdong and the King Country to the Scots burr which had been predominant. Almost immediately a myth of identity emerged, typified by goldfields balladeer Charles Thatcher’s ‘Old Identity and New Iniquity’ and boosted by the histrionics of a press enamoured of the romanticised machinations of the Otago goldfields ‘digger’. This popular myth
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Blackwell, Dean. "Community and visitor benefits associated with the Otago Central Rail Trail, New Zealand." Lincoln University, 2002. http://hdl.handle.net/10182/1027.

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Outdoor recreation and heritage resources have the potential to provide a wide range of benefits to individuals, groups of individuals and the economy. An increased knowledge of these benefits can give recreation managers and planners a better understanding of how their actions and decisions regarding a resource may impact upon the visitors and communities that they serve. Placed within a climate of increasing public sector accountability, this information might also prove useful in justifying the allocation of scarce resources to recreation and heritage preservation. Justifying the value that
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Youngson, John Hughan, and n/a. "Physical and chemical processes affecting the formation of alluvial gold deposits in Central Otago, New Zealand." University of Otago. Department of Geology, 2007. http://adt.otago.ac.nz./public/adt-NZDU20071108.160736.

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Alluvial gold placers in Otago and northern Southland occur at several stratigraphic horizons within the Late Cretaceous - Recent sedimentary sequence. The gold is derived ultimately from primary sources in the Otago Schist. Poor correlation between the distribution of placers and that of the known primary deposits reflects repeated recycling of gold in the present drainage network and two precursor networks, each with substantially different architecture. The previous drainage networks were inundated and buried during marine or lacustrine transgression. There has been local addition of first
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Scott, Matthew B., and n/a. "Fine-scale ecology of alpine patterned ground, Old Man Range, Central Otago, New Zealand." University of Otago. Department of Botany, 2007. http://adt.otago.ac.nz./public/adt-NZDU20080130.093120.

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This study is an interdisciplinary ecological study addressing the fine-scale relationships between plants, invertebrates and the environment in an alpine ecosystem. Alpine environments are marked by steep environmental gradients and complex habitat mosaics at various spatial scales. Regular forming periglacial patterned ground landforms on the Old Man Range, Central Otago, South Island, New Zealand present an ideal medium for studying plant-invertebrate-environment relationships due to their partitioning of the landscape into discrete units of contrasting environmental conditions, and the exi
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Bennett, E. R. "Fault growth and landscape development in Central Otago, New Zealand, using in situ cosmogenic isotopes." Thesis, University of Cambridge, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.596565.

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Central Otago in New Zealand is a region dominated by late Tertiary NE trending anticlines which form above buried reverse faults. As the folds uplift, soft Tertiary sediments are rapidly eroded, exposing the underlying basement schist. At the base of the sedimentary cover there is patchy occurrence of hard silica cemented quartz-rich boulders which remain exposed on the schist surface after the overlying sediments are removed. <sup>10</sup>Be and <sup>26</sup>Al accumulate in the quartz within the boulders upon exposure to cosmic radiation. Cosmogenic dating of the boulders provides the means
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Mason, Norman, and n/a. "Functional diversity and ecosystem-level processes in a short-tussock grassland." University of Otago. Department of Botany, 2006. http://adt.otago.ac.nz./public/adt-NZDU20061024.114054.

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Increased functional diversity has been linked to an increase in ecosystem level processes (ELPs), such as productivity, ecosystem reliability and invasion resistance. However, there has been no exact definition of functional diversity and it is not known which indices are appropriate for its measurement. Consequently, continuous indices have rarely been applied in examination of relationships between functional diversity and ELPs and little is known of the mechanisms linking functional diversity to ELPs. This thesis begins by providing an exact definition of functional diversity, identifying
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Brown, Charles Stewart. "Secondary succession in the high-alpine of Central Otago, New Zealand, 25 years following anthropogenic disturbance." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape2/PQDD_0005/MQ59783.pdf.

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Wood, Jamie Russell, and n/a. "Pre-settlement paleoecology of Central Otago�s semi-arid lowlands, with emphasis on the pre-settlement role of avian herbivory in South Island dryland ecosystems, New Zealand." University of Otago. Department of Geology, 2008. http://adt.otago.ac.nz./public/adt-NZDU20080211.142212.

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The vegetation communities that existed in the semi-arid intermontane basins and gorges of Central Otago prior to human settlement ~750 years B.P. are poorly understood. This is because of a lack of fossil evidence and complex restructuring by anthropogenic factors, especially increased fire frequency, and more recently mammalian grazing. There is also little information regarding the effect of the lost fauna on maintaining and structuring presettlement communities, both in Central Otago and throughout the eastern South Island dryland zone. This study aims to provide a clearer understanding of
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Books on the topic "Central Otago"

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Cunningham, Gerald. Central Otago: A special place. North Shore, N.Z: Raupo/Penguin Group, 2009.

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2

Hurst, Tony. The Otago Central Railway: A tribute. 5th ed. Wellington [N.Z.]: Transpress NZ, 2008.

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The Otago Central Railway: A tribute. 5th ed. Wellington [N.Z.]: Transpress NZ, 2008.

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4

Brian, Patrick, ed. Wild Central: Discovering the natural history of Central Otago. Dunedin, N.Z: University of Otago Press, 1999.

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5

Amisfield: Food, wine and stories from Central Otago. Auckland, New Zealand: Random House New Zealand, 2014.

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6

Peter, Andrews. Otago Rail trail guidebook: A comprehensive pictorial guide to travelling the Otago Central Rail trail. 4th ed. Waipiata, Ranfurly, New Zealand: Otagorailtrail.co.nz, 2014.

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7

Cull, Dave. Vineyards on the edge: The story of Central Otago wine. Dunedin, N.Z: Longacre, 2001.

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8

Cunningham, Gerald. Illustrated history of Central Otago and the Queenstown Lakes District. Auckland [N.Z.]: Reed, 2005.

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9

Sullivan, Jim. Old Waipiata: Pictures and stories from a Central Otago railway town. Dunedin [N.Z.]: Rock and Pillar Press, 2008.

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10

Madin, Ian. Geology and neotectonics of the Upper Manuherikia Basin, Central Otago, New Zealand. Lower Hutt, New Zealand: New Zealand Geological Survey, 1988.

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Book chapters on the topic "Central Otago"

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Fountain, Joanna, and Charlotte Thompson. "Wine Tourist’s Perception of Winescape in Central Otago, New Zealand." In Wine Tourism Destination Management and Marketing, 29–44. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-00437-8_3.

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"Working the vines: ni- Vanuatu labour, Central Otago Pinot, and economic development in Vanuatu." In Social, Cultural and Economic Impacts of Wine in New Zealand., 85–99. Routledge, 2014. http://dx.doi.org/10.4324/9780203083161-14.

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Mulvihill, P., and I. Walsh. "Development of a Small Hydroelectric Scheme at Horseshoe Bend, Teviot River, Central Otago, New Zealand." In Comprehensive Renewable Energy, 467–83. Elsevier, 2012. http://dx.doi.org/10.1016/b978-0-08-087872-0.00618-1.

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"The new gold: the role of place and heritage in the marketing of the Central Otago wine region JOANNA FOuNTAIN ANd dAISY dAWSON." In Wine and Identity, 59–72. Routledge, 2014. http://dx.doi.org/10.4324/9780203067604-13.

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Lambert, Tristan H. "Functional Group Protection." In Organic Synthesis. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780190200794.003.0014.

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Alfonso Iadonisi at the University of Naples Federico II developed (Eur. J. Org. Chem. 2013, 3137) a procedure for the selective acetolysis of the perbenzylated sugar 1 to furnish 3 using isopropenyl acetate (2) instead of the more typical and high-boiling acetic anhydride. The (3,4-dimethoxylphenyl)benzyl (DMPBn) protecting group, which is removed (cf. 4 → 5) under acidic conditions in the presence of the cation scavenger 5, was developed (J. Org. Chem. 2013, 78, 5264) by David S. Larsen at the University of Otago as an alternative to the p-methoxybenzyl (PMB) group. Another new hydroxyl-protecting group, the AzDMB group, which can be installed by simple acylation of (7 + 8 → 9) and removed under reductive conditions, was developed by Gijsbert A. van der Marel and Jeroen D.C. Codée of Leiden University. Stefan Grimme at the University of Bonn and Armido Studer at Westfälische-Wilhelms-Universität Münster found (Chem. Sci. 2013, 4, 2177) that NHC precatalyst 11 in the presence of NaH, benzaldehyde, and the oxidant 12 allows for the selective O-acylation of aminoalcohol 10 to 13. The reductive deprotection of benzyl carbamate 14 using the strong organic reductant 15 under photolytic conditions was achieved (Angew. Chem. Int. Ed. 2013, 52, 2239) by John A. Murphy at the University of Strathclyde. Liang-Qiu Lu and Wen-Jing Xiao at Central China Normal University found (Chem. Asian J. 2013, 8, 1090) that mixed imide 17 could be detosylated under visible light photoredox catalysis in the presence of Hantzsch ester 18. Frank Glorius at Westfälische-Wilhelms-Universität Münster developed (Org. Lett. 2013, 15, 1776) a ruthenium-catalyzed procedure for the N-formylation of amine 20 using methanol as the source of the formyl group. Protection of the thymine derivative 22 with a 2-(methoxycarbonyl)ethenyl (MocVinyl) group to produce 23 was developed (J. Org. Chem. 2013, 78, 5832) by Jaume Vilarrasa at the University of Barcelona. Deprotection of the MocVinyl group is readily achieved by treatment with a nucleophilic reagent such as pyrrolidine. Robert H. Grubbs at Caltech demonstrated (Chem. Sci. 2013, 4, 1640) that ether 24 could be demethylated with triethylsilane and potassium t-butoxide at high temperatures.
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Conference papers on the topic "Central Otago"

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Law, Shanna L., Dave Craw, Dave Craw, Cathy Rufaut, Cathy Rufaut, Kat Lilly, and Kat Lilly. "EROSIONAL AND GEOCHEMICAL CONTROLS ON NATURAL REVEGETATION AT AN UNREMEDIATED PLACER GOLD MINE, CENTRAL OTAGO, NEW ZEALAND." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272054.

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