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Journal articles on the topic 'Central Otago'

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Author: Grafiati

Published: 4 June 2021

Last updated: 29 January 2023

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1

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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2

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 this variability was the accumulated number of growing degree-days. Insecticide sprays target midge larvae, but are timed against the second and third peaks of adult emergence. Variations in the timing of these peaks annually and across the main pipfruit growing regions, mean that specific insecticide timing recommendations are necessary each year for each region.

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3

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 iconic status epitomised by the "Southern Man" stereotype. This places Central Otago deep in the psyche of the nation. With this goes a unique and significant set of conditions under which farming must take place. Not only does the region have the biophysical challenges of soils, water and climate to contend with, but a wider set of values, often imposed from elsewhere. Fifty years after that first conference we remain challenged. What are the opportunities in front of us and how should we best accommodate the challenge of maintaining a viable enterprise and at the same time, respecting the intense public and customer interest in our use of land and livestock? Central Otago and the associated high country of the Lakes district and McKenzie basin can be divided into three farming types. These are the valley floor irrigable type, the flat and downland dryland regions, and the high country. Each of these has challenges that are at times unique, but often overlap with problems faced in other regions.

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4

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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5

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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6

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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7

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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8

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 the economic growth of the district and seeks to create a thriving economy that will be attractive to business and residents alike. Two key principles that underpin the LTP are sustainability and affordability, with the definition of sustainability being "… development that meets the needs of the present without compromising the ability of future generations to meet their own needs."

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9

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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10

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 and 14.8 t DM/ha in Year 3. There were no annual DM responses to any of the three fertilisers applied regardless of the rate of application. Despite the control mean annual herbage P concentrations being within the optimum range of 0.20-0.25% the application of P fertiliser significantly increased the P concentrations (P

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11

Barker, Shaun L. L. "Pseudotachylyte-generating faults in Central Otago, New Zealand." Tectonophysics 397, no. 3-4 (March 2005): 211–23. http://dx.doi.org/10.1016/j.tecto.2004.12.005.

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12

Pole, Mike. "Early miocene floras from Central Otago, New Zealand." Journal of the Royal Society of New Zealand 19, no. 2 (June 1989): 121–25. http://dx.doi.org/10.1080/03036758.1989.10426442.

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13

Walker, Susan, William G. Lee, and Geoffrey M. Rogers. "The woody vegetation of Central Otago, New Zealand." New Zealand Journal of Botany 42, no. 4 (September 2004): 589–612. http://dx.doi.org/10.1080/0028825x.2004.9512914.

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14

Attfield, B., and D. Anderson. "Remote microscopy diagnostics for preclearance export of apricots grown in Central Otago." New Zealand Plant Protection 68 (January 8, 2015): 440. http://dx.doi.org/10.30843/nzpp.2015.68.5842.

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Central Otago growers wishing to export apricots to Australia are required to have fruit graded packed and inspected by a registered packhouse as part of the Offshore PreClearance Inspection Programme As part of this programme an Australian government inspector is brought to Central Otago by the industry for approximately 6 weeks to carry out fruit inspections in the packhouse specifically targeting insect interceptions Any insects found in the 600 fruit sampled from each lot inspected (0530 pallets) are brought to Plant Food Research Clyde where a technician prepares the specimen for remote microscopy diagnostics (RMD) RMD enables sameday insect identification by experts from the Plant Health and Environment Laboratory Ministry for Primary Industries Christchurch A camera mounted on a compound or stereo microscope relays images in real time via the internet enabling the specimen to be manipulated by the technician in Clyde for identification by qualified staff in Christchurch Previously insect identification took approximately 3 days as specimens were sent by courier from Central Otago to a certified laboratory in Auckland RMD real time saving equates to less fruit spoilage and less disruption to transport systems awaiting shipments to be cleared

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15

Mortensen, James K., J. Anthony Coote, David Craw, and Douglas J. MacKenzie. "Early Jurassic felsic and associated mafic meta-igneous rocks in Otago Schist, Central Otago, New Zealand." New Zealand Journal of Geology and Geophysics 61, no. 2 (April 3, 2018): 237–46. http://dx.doi.org/10.1080/00288306.2018.1464032.

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16

Wakelin, J. "WATER CONSERVATION LANDSCAPING: A CENTRAL OTAGO PLANTING EXPERIENCE©." Acta Horticulturae, no. 1014 (December 2013): 41–43. http://dx.doi.org/10.17660/actahortic.2013.1014.7.

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17

YEATS, ROBERT S. "Tectonic map of Central Otago based on Landsat imagery." New Zealand Journal of Geology and Geophysics 30, no. 3 (August 1987): 261–71. http://dx.doi.org/10.1080/00288306.1987.10552621.

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18

McLaren, Gillian F. "Phenology of oystershell scaleQuadraspidiotus ostreaeformis(Curtis) in Central Otago." New Zealand Journal of Crop and Horticultural Science 17, no. 3 (July 1989): 215–19. http://dx.doi.org/10.1080/01140671.1989.10428035.

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19

Walker, Susan, William G. Lee, and Geoffrey M. Rogers. "Pre‐settlement woody vegetation of Central Otago, New Zealand." New Zealand Journal of Botany 42, no. 4 (September 2004): 613–46. http://dx.doi.org/10.1080/0028825x.2004.9512915.

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20

Markley, Michelle, and Basil Tikoff. "Geometry of the folded Otago peneplain surface beneath Ida valley, Central Otago, New Zealand, from gravity observations." New Zealand Journal of Geology and Geophysics 46, no. 3 (September 2003): 449–56. http://dx.doi.org/10.1080/00288306.2003.9515020.

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21

Adams, C. J., and J. I. Raine. "Age of Cretaceous silicic volcanism at Kyeburn, Central Otago, and Palmerston, eastern Otago, South Island, New Zealand." New Zealand Journal of Geology and Geophysics 31, no. 4 (October 1988): 471–75. http://dx.doi.org/10.1080/00288306.1988.10422144.

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22

Redpath, S. P., A. Wilson, L. E. Jamieson, N. E. M. Page-Weir, M. J. Griffin, A. Chhagan, and B. Hamilton. "Postharvest management of New Zealand flower thrips on export apricots using ethyl formate." New Zealand Plant Protection 67 (January 8, 2014): 103–8. http://dx.doi.org/10.30843/nzpp.2014.67.5758.

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New Zealand flower thrips (NZFT Thrips obscuratus) is the most abundant pest on New Zealand apricots at harvest and is a quarantine pest for apricot export markets Ethyl formate (EF) is a Generally Recognised As Safe (GRAS) compound being investigated treatments against NZFT and their impact on apricot fruit quality in shipping containers NZFT adults and larvae on apricots were treated in field bins of apricots in a 282 m3 in Hawkes Bay and Central Otago respectively In Hawkes Bay the treatments resulted in 100 mortality of NZFT adults and larvae In Central Otago the treatments resulted in 100 mortality of NZFT adults and 98100 larval mortality Export grade apricot cultivars expressed no adverse effects on quality to this concentration of EFCO2

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23

McLaren, G. F., J. A. Fraser, and J. E. Grant. "POLLINATION COMPATIBILITY OF APRICOTS GROWN IN CENTRAL OTAGO, NEW ZEALAND." Acta Horticulturae, no. 384 (December 1995): 385–90. http://dx.doi.org/10.17660/actahortic.1995.384.61.

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24

Worthy, T. H., A. J. D. Tennyson, C. Jones, J. A. McNamara, and B. J. Douglas. "Miocene waterfowl and other birds from central Otago, New Zealand." Journal of Systematic Palaeontology 5, no. 1 (January 2007): 1–39. http://dx.doi.org/10.1017/s1477201906001957.

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25

Hayes, A. J., G. F. McLaren, and J. A. Fraser. "Developmenting a preliminary model predicting thrips movement into central Otago nectarines." Proceedings of the New Zealand Plant Protection Conference 52 (August 1, 1999): 45–49. http://dx.doi.org/10.30843/nzpp.1999.52.11584.

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26

McLaren, G. F., D. M. Suckling, A. M. El-Sayed, B. T. Hislop, and T. F. S. Jones. "Multiple species mating disruption of leafrollers in cherries in Central Otago." New Zealand Plant Protection 66 (January 8, 2013): 132–37. http://dx.doi.org/10.30843/nzpp.2013.66.5564.

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Mating disruption for leafrollers has been conducted on a commercial scale using a single multispecies pheromone dispenser on contiguous blocks of cherries in Central Otago for 4 years Pheromone trap and packhouse results were collected from isolated untreated (654 ha) and pheromonetreated cherry orchard areas (764 ha) in the Cromwell district In untreated cherry orchards catches of light brown apple moth (Epiphyas postvittana) were exceptionally high (38 males/trap/day) with lower catches of Planotortrix octo (025 males/ trap/day) Catches of both species were strongly disrupted in the treated areas reducing E postvittana to 00036 moths/trap/day and P octo to nil Trap catches of both species have increased steadily over 5 years (2008/09 to 20012/13) in blocks not using mating disruption Packhouse results showed that all of the fruit inspected from both treated and untreated areas were free of leafroller infestations in 2012/13 Insecticide use in the pheromonetreated areas was reduced by one application compared with the areas without pheromone

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27

Fraser, K. W. "Emergence behaviour of rabbits,Oryctolagus cuniculus, in Central Otago, New Zealand." Journal of Zoology 228, no. 4 (December 1992): 615–23. http://dx.doi.org/10.1111/j.1469-7998.1992.tb04459.x.

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28

Morgan, R. K. "Chemotypic Characteristics of Thymus vulgaris L. in Central Otago, New Zealand." Journal of Biogeography 16, no. 5 (September 1989): 483. http://dx.doi.org/10.2307/2845110.

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29

Pearson, C. "Extent and tectonic significance of the Central Otago shear-strain anomaly." New Zealand Journal of Geology and Geophysics 33, no. 2 (April 1990): 295–301. http://dx.doi.org/10.1080/00288306.1990.10425687.

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30

Stirling, M. W. "Peneplain modification in an alpine environment of Central Otago, New Zealand." New Zealand Journal of Geology and Geophysics 34, no. 2 (June 1991): 195–201. http://dx.doi.org/10.1080/00288306.1991.9514457.

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31

McLaren, Gillian F. "Control of oystershell scaleQuadraspidiotus ostreaeformis(Curtis) on apples in Central Otago." New Zealand Journal of Crop and Horticultural Science 17, no. 3 (July 1989): 221–27. http://dx.doi.org/10.1080/01140671.1989.10428036.

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32

McLaren, G. F., and D. M. Suckling. "Pheromone trapping of orchard lepidopterous pests in Central Otago, New Zealand." New Zealand Journal of Crop and Horticultural Science 21, no. 1 (March 1993): 25–31. http://dx.doi.org/10.1080/01140671.1993.9513742.

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33

Clark, Geoffrey R., Peter Petchey, Matthew S. McGlone, and Peter Bristow. "Faunal and floral remains from Earnscleugh Cave, Central Otago, New Zealand." Journal of the Royal Society of New Zealand 26, no. 3 (September 1996): 363–80. http://dx.doi.org/10.1080/03014223.1996.9517515.

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34

Pole, M. S., A. M. Holden, and J. D. Campbell. "Fossil legumes from the Manuherikia Group (Miocene), Central Otago, New Zealand." Journal of the Royal Society of New Zealand 19, no. 3 (September 1989): 225–28. http://dx.doi.org/10.1080/03036758.1989.10427178.

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35

Walker, Susan, J. Bastow Wilson, and Alan F. Mark. "Seasonal changes in semi‐arid vegetation of Central Otago, New Zealand." New Zealand Journal of Botany 37, no. 3 (September 1999): 479–93. http://dx.doi.org/10.1080/0028825x.1999.9512647.

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36

Harris, A. C. "A specimen ofCizara ardeniae(Lepidoptera: Sphingidae) captured at Naseby, Central Otago." New Zealand Entomologist 13, no. 1 (January 1990): 38–39. http://dx.doi.org/10.1080/00779962.1990.9722588.

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37

Patrick, Brian H., Hamish J. H. Patrick, and Robert J. B. Hoare. "Review of the endemic New Zealand genus Arctesthes Meyrick (Lepidoptera, Geometridae, Larentiinae), with descriptions of two new range-restricted species." Alpine Entomology 3 (May 29, 2019): 121–36. http://dx.doi.org/10.3897/alpento.3.33944.

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The genus Arctesthes Meyrick (Geometridae: Larentiinae: Xanthorhoini), endemic to the South Island of New Zealand, is revised. Four species are recognised, including two new species, as follows: Arctesthescatapyrrha (Butler, 1877), A.siris (Hudson, 1908), A.titanicasp. nov. and A.avatarsp. nov. All except A.catapyrrha are restricted to subalpine and alpine localities. Adults and genitalia are fully described and illustrated for all species; larvae of A.catapyrrha are also briefly described and illustrated. Only Arctesthescatapyrrha is widespread; A.siris is restricted to a few mountain ranges of Central Otago; A.titanica is only known from two wetland localities in the Von Valley of the Otago Lakes district, and A.avatar is only known from a few wetlands in a restricted area of north-west Nelson. The two new species are considered of very high priority for conservation.

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38

Fahey, Barry D. "Weathering Pit Development in the Central Otago Mountains of Southern New Zealand." Arctic and Alpine Research 18, no. 3 (August 1986): 337. http://dx.doi.org/10.2307/1550891.

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39

Youngson, J. H., and D. Craw. "Evolution of placer gold deposits during regional uplift, central Otago, New Zealand." Economic Geology 90, no. 4 (July 1, 1995): 731–45. http://dx.doi.org/10.2113/gsecongeo.90.4.731.

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40

McLaren, G. F., J. A. Fraser, and D. G. Lynch. "An evaluation of sulphur for brown rot control in Central Otago stonefruit." Proceedings of the New Zealand Plant Protection Conference 49 (August 1, 1996): 32–36. http://dx.doi.org/10.30843/nzpp.1996.49.11406.

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41

Markley, Michelle, and Richard J. Norris. "Structure and neotectonics of the Blackstone Hill Antiform, Central Otago, New Zealand." New Zealand Journal of Geology and Geophysics 42, no. 2 (June 1999): 205–18. http://dx.doi.org/10.1080/00288306.1999.9514840.

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42

Hawke, DJ, and KA Hunter. "Dissolved trace metal speciation in the Manuherikia River, Central Otago, New Zealand." Marine and Freshwater Research 43, no. 6 (1992): 1381. http://dx.doi.org/10.1071/mf9921381.

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The inorganic speciation of the trace metals Cu, Ni, Cd, Zn and Pb has been calculated for the pristine, subalpine Manuherikia River. Temperature, pH, ionic strength and major-ion composition were found to be important controls on the free-ion activity of trace metals. Metal -CO3-2 species were the most important complexes for Pb, Cu and Ni. The metal-HCO3- species was most important for Cd, and Zn was intermediate. Ni, Zn and Cd were present mainly as the free divalent ion, whereas Pb (up to 81% complexed) and Cu (up to 70% complexed) were strongly affected by ionic interactions. Free-ion activities of Cu2+ and Pb2+ were essentially constant along the length of the river despite significant increases in total dissolved-metal concentrations. Thus, for these metal ions, total dissolved concentrations are a poor indicator of biological availability.

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43

McGlone, M. S., A. F. Mark, and D. Bell. "Late Pleistocene and Holocene vegetation history, Central Otago, South Island, New Zealand." Journal of the Royal Society of New Zealand 25, no. 1 (March 1995): 1–22. http://dx.doi.org/10.1080/03014223.1995.9517480.

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44

Pole, Mike. "Plant macrofossils from the Foulden Hills Diatomite (Miocene), Central Otago, New Zealand." Journal of the Royal Society of New Zealand 26, no. 1 (March 1996): 1–39. http://dx.doi.org/10.1080/03014223.1996.9517503.

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45

Gibson, R., A. Hewitt, G. Sparling, and O. Bosch. "Vegetation change and soil quality in central Otago tussock grasslands, New Zealand." Rangeland Journal 22, no. 2 (2000): 190. http://dx.doi.org/10.1071/rj0000190.

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46

Wearing, C. Howard, Kate Colhoun, Bernie Attfield, and Ross R. Marshall. "Phenology and management of noctuids attacking apple in Central Otago, New Zealand." New Zealand Entomologist 33, no. 1 (February 2010): 55–67. http://dx.doi.org/10.1080/00779962.2010.9722192.

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47

Németh, Károly. "Calculation of long-term erosion in Central Otago, New Zealand, based on erosional remnants of maar/tuff rings." Zeitschrift für Geomorphologie 47, no. 1 (March 19, 2003): 29–49. http://dx.doi.org/10.1127/zfg/47/2003/29.

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48

Wearing, C. H. "Resistance of Planotortrix octo to organophosphate insecticides in Dumbarton, central Otago." Proceedings of the New Zealand Plant Protection Conference 48 (January 8, 1995): 40–45. http://dx.doi.org/10.30843/nzpp.1995.48.11542.

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49

Ridl, R. N., M. C. Villenueve, D. H. Bell, and D. F. Macfarlane. "Mineralogical control on the intact strength of schist in Central Otago, New Zealand." IOP Conference Series: Earth and Environmental Science 833, no. 1 (August 1, 2021): 012037. http://dx.doi.org/10.1088/1755-1315/833/1/012037.

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50

Rosin, Christopher, Angga Dwiartama, Darryl Grant, and Debbie Hopkins. "Using provenance to create stability: State-led territorialisation of Central Otago as assemblage." New Zealand Geographer 69, no. 3 (November 25, 2013): 235–48. http://dx.doi.org/10.1111/nzg.12024.

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