National Report on the Implementation of the Ramsar Convention on Wetlands
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NOTORNIS QUARTERLY JOURNAL of the Ornithological Society of New Zealand Volume Sixteen, Number Two, lune, 1969 NOTICE TO CONTRIBUTORS Contributions should be type-written, double- or treble-spaced, with a wide margin, on one side of the paper only. They should be addressed to the Editor, and are accepted o?, condition that sole publication is being offered in the first instance to Notornis." They should be concise, avoid repetition of facts already published, and should take full account of previous literature on the subject matter. The use of an appendix is recommended in certain cases where details and tables are preferably transferred out of the text. Long contributions should be provided with a brief summary at the start. Reprints: Twenty-five off-prints will be supplied free to authors, other than of Short Notes. When additional copies are required, these will be produced as reprints, and the whole number will be charged to the author by the printers. Arrangements for such reprints must be made directly between the author and the printers, Te Rau Press Ltd., P.O. Box 195, Gisborne, prior to publication. Tables: Lengthy and/or intricate tables will usually be reproduced photographically, so that every care should be taken that copy is correct in the first instance. The necessity to produce a second photographic plate could delay publication, and the author may be called upon to meet the additional cost. nlastrutions: Diagrams, etc., should be in Indian ink, preferably on tracing cloth, and the lines and lettering must be sufficiently bold to allow of reduction. Photographs must be suitable in shape to allow of reduction to 7" x 4", or 4" x 3f". -
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The Late Quaternary Geomorphology of the Lower Manawatu
Copyright is owned by the Author of the thesis. Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only. The thesis may not be reproduced elsewhere without the permission of the Author. THE LATE QUATERNARY GEOMORPHOLOGY OF THE LOWER MANAWATU A thesis presented in partial fulfilment of the requirements for the Degree of Master of Arts in Geography at Massey University by PATRICK ALAN HESP 1975 ABSTRACT The geomorphology of the present Lower Manawa tu floodplain and the valleys that exit at the margin of the floodplain, is presented. An introduction to the geology and geomorphology of the study area is given, and previous studies are reported where relevant. Two types of tributary valleys have been recognised in the study area. These valleys have been cut into the Tokomaru Marine Terrace. The first type recognised are predominantly gravel-floored, box-shaped valleys with headwaters in the Tararua Ranges. The second and major type recognised are box-shaped valleys without gravel floors. The first type have been formed by normal fluvial processes, while the second type were originally V-shaped, and have been infilled by estuarine sedimentation processes. The latter occurred as a direct result of the Flandrian Transgression. The morphology of the Tokoma ru Marine Terrace margin is examined, and it is concluded that the margin is predominantly river-cut. The Manawatu floodplain was originally an estuary. As the Flandrian Transgression began the lower reaches of the Manawatu and eventually the Oroua Rivers were drowned. As the Transgression progressed, the Lower Manawatu became an estuary. -
New Zealand's Fresh Waters: Values, State, Trends and Human Impacts
OFFICE OF THE PRIME MINISTER’S CHIEF SCIENCE ADVISOR Professor Sir Peter Gluckman, KNZM FRSNZ FMedSci FRS Chief Science Advisor New Zealand’s fresh waters: Values, state, trends and human impacts 12 April 2017 Office of the Prime Minister’s Chief Science Advisor PO Box 108-117, Symonds Street, Auckland 1150, New Zealand Telephone: +64 9 923 6318 Website: www.pmcsa.org.nz Email: [email protected] ACKNOWLEDGMENTS This set of reports is the result of a lengthy collaborative effort initiated and guided by Sir Peter Gluckman, the Prime Minister’s Chief Science Advisor (PMCSA). Development of the technical report was led by Dr Bryce Cooper, working with Drs Clive Howard-Williams, Scott Larned and John Quinn of the freshwater team at the National Institute of Water and Atmospheric Research (NIWA), and the Office of the PMCSA. Coordination of the project and preparation of the summary report was led by Dr Anne Bardsley of the Office of the PMCSA, in close collaboration with Dr Ken Hughey, Chief Science Advisor for the Department of Conservation, and Dr David Wratt, Departmental Science Advisor for the Ministry for the Environment. We gratefully acknowledge the input of the following reviewers: David Hamilton, University of Waikato Ken Taylor, AgResearch; Our Land and Water National Science Challenge Roger Young, Cawthron Institute Brett Eaton, University of British Columbia Neil Deans, Ministry for the Environment Wes Patrick, Ministry for the Environment Joanne Perry, Department of Conservation Adam Tipper, Stats NZ We also thank Kristiann Allen -
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Hydrology.Wetland Restoration. a Handbook for New Zealand Freshwater Systems
CHAPTER 7 HYDROLOGY DAVE CAMPBELL CONTENTS INTRODUCTION 1 UNDERSTANDING HYDROLOGICAL PROCESSES IN WETLANDS 1.1 Peatlands and hydrology 1.1.1 Peat decomposition 2 HUMAN IMPACTS ON HYDROLOGICAL REGIMES 3 RESTORING YOUR WETLAND 3.1 Developing a Wetland Restoration Plan 3.1.1 Mapping 3.2 Determining wetland type 3.3 Understanding the site 3.3.1 Reference wetland hydrology 3.3.2 Wetland restoration site hydrology 3.4 Setting realistic goals and objectives 3.4.1 Keeping it legal 4 TIPS FOR RESTORING WETLAND HYDROLOGY 5 MONITORING 5.1 Locating monitoring points 5.2 Dipwells, piezometers and reference points 5.3 Monitoring frequency 5.4 The von Post Peat Decomposition Index 6 REFERENCES AND FURTHER READING 6.1 Useful websites SECTION TWO: ACTION ON THE GROUND CHAPTER 7 HYDROLOGY 75 HYDROLOGY WETLAND RESTORATION: A HANDBOOK FOR NZ FRESHWATER SYSTEMS HYDROLOGY DAVE CAMPBELL When applied to wetlands, the science of hydrology a downstream location, either as surface water is concerned with how the storage and movement in streams or groundwater that may emerge in of water into and out of a wetland affects the plants seepages or springs. Wetlands often occur in and animals, and the soils on which they grow. the lower parts of catchments where there is an Most wetland scientists agree that the single most excess of water input so that the water table is important factor determining both wetland type permanently or seasonally close to the ground and function is hydrology. Consequently, changes surface. This includes valley bottoms, low-lying in hydrology are the leading causes of wetland areas alongside streams and rivers, and down degradation or destruction. -
2031 Auckland/Waikato Fish & Game 15
SPORTS FISH AND GAME MANAGEMENT PLAN FOR AUCKLAND/WAIKATO FISH AND GAME REGION 2021 – 2031 AUCKLAND/WAIKATO FISH & GAME 156 BRYMER RD, RD 9, HAMILTON PH: 07 849 1666 [email protected] www.fishandgame.org.nz Contents: PART 1 BACKGROUND AND RESOURCE SUMMARY How To Use this Plan ...................................................................................................................... 5 1.1. Operation of Plan .................................................................................................................... 5 1.2. Plan Review ............................................................................................................................. 5 1.3. Organisational management .................................................................................................. 5 2. Introduction .................................................................................................................................... 6 2.1. Fish and Game New Zealand ................................................................................................... 6 2.2. The Auckland/Waikato Fish and Game ................................................................................... 6 3. Legal Context................................................................................................................................... 9 3.1. Conservation Act 1987 ............................................................................................................ 9 3.2. Wildlife Act 1953 .................................................................................................................... -
Resilient Wetlands Research Programme Update 7: July 2017 to June 2018
Resilient Wetlands Research Programme Update 7: July 2017 to June 2018 Bev Clarkson, Dave Campbell, Yvonne Taura, Chris Tanner Overview Our Resilient Wetlands research programme is funded by the Strategic Science Investment Fund (SSIF) Crown Research Institutes from the Ministry of Business, Innovation and Employment's Science and Innovation Group (previously ‘core’ funding). The following update summarises the major outputs and successes between July 2017 and June 2018. O tu Wharekai wetlands relatively resilient to N-loading in the short term. Our 3-year fertiliser (N, P) experiment in a montane fen to determine the vulnerability of natural wetlands to agricultural inputs has now been completed. Olivia Burge led the data analysis and write-up of the journal paper, which has just been submitted. The catchment, on the foothills of the Southen Alps, is largely intact, with very low atmospheric nitrogen inputs. We found little evidence of community-level change after 3 years of nutrient addition, aside from increasing dominance in cover of the most abundant canopy species and decreases in species richness, in the highest N treatment (both nitrate-N and ammonium-N) plots. Species richness decreases were due to losses of both native and exotic species. Further work is required to assess the longer-term resilience of New Zealand wetlands to agricultural losses of N and P, the impacts of which have largely gone unstudied. Final harvesting of a total of 8 replicated plots each of Schoenus (left), Carex (right), and Chionochloa (not shown) communities at O Tu Wharekai after 3 years fertilization with either nitrate-N, ammonium-N and phosphate-P alone or in combination. -
Manawatū-Whanganui Regional Climate Change Risk Assessment
Manawatū-Whanganui Regional Climate Change Risk Assessment Prepared for Horizons Regional Council Prepared by Tonkin & Taylor Ltd Date September 2021 Job Number 1014266.V1.0 Document Control Manawatū-Whanganui Regional Climate Change Risk Assessment Version 1.0 published 02 September 2021 Prepared by: Gemma Bishop Morgan Lindsay Ben Simms Alex Cartwright Reviewed by: Alex Cartwright Approved by: Peter Cochrane Sections of this report have been technically reviewed by: Manea Sweeney, James Hughes, Roger MacGibbon and Alex Cartwright. This report was prepared in collaboration with Councils of the Manawatū-Whanganui Region. Distribution Horizons Regional Council 1 PDF copy Tonkin & Taylor Ltd (FILE) 1 electronic copy Table of contents 1 Introduction 3 2 Framework, method and approach 4 2.1 Framework 4 2.2 Method (assessing risk) 7 2.3 Approach 7 3 Summary of climate change for the region 9 4 Summary of climate change risks 12 4.1 District summaries 15 5 Te Ao Tūroa | Natural world 19 5.1 Biodiversity and ecology 20 5.2 Biosecurity 25 5.3 Natural landscapes 28 5.4 Freshwater ecosystems 32 6 Hauora | Wellbeing 35 6.1 Health 35 6.2 Public spaces 39 6.3 Location, quality and availability of housing 42 6.4 Social capital 46 7 Business 51 7.1 Commerce: commercial buildings and manufacturing 52 7.2 Fast moving consumer goods (FMCGs) 53 7.3 Livestock and animal welfare 55 7.4 Productivity of land 61 7.5 Tourism 65 8 Infrastructure 70 8.1 Water supply 71 8.2 Stormwater 76 8.3 Wastewater 79 8.4 Flood management schemes 83 8.5 Energy 87 8.6 Telecommunication -
(Anarhynchus Frontalis) at the Manawatu River Estuary, North Island, New Zealand
118 Notornis, 2007, Vol. 54: 118-119 0029-4470 © The Ornithological Society of New Zealand, Inc. SHORT NOTE Wrybills (Anarhynchus frontalis) at the Manawatu River Estuary, North Island, New Zealand IAN ARMITAGE 50 Ranui Terrace, Tawa, Wellington 5028, New Zealand [email protected] The ‘sandspit’ on the True Right bank of the In Jan, wrybills should be moving north from Manawatu River, in Foxton Beach Village, (175°14’E the breeding grounds on the eastern braided rivers 40°30’S) is a significant roosting site for migratory of the South I to wintering areas on the northern and resident waders, gulls, terns, pied stilts harbours. The brevity of the flock’s visit to the (Himantopus himantopus), royal spoonbills (Platalea ‘sandspit’ area in the Manawatu River estuary regia), shags, ducks, and other birds. The ‘sandspit’ suggests that the birds were on migration, although is 2-5 ha, depending on the state of the tide, c.1 km the value of a 10 min rest during a flight of several from the Tasman Sea, It is surrounded on 3 sides by hundred km would seem to be slight. It is, of course, the main course of the river and by tidal flats, and unknown how long the flock had been flying before as well as this natural isolation, it is protected as a it visited the Manawatu River estuary, nor how far a “bird sanctuary” by local bye-laws. wrybill can fly without resting, but my observation On 14 Jan 2006, I observed a flock of 29 wrybills suggests that the migration may not be made non- (Anarhynchus frontalis) arrive on the ‘sandspit’, rest stop. -
GROWTH STRATEGY TE RAUTAKI WHAKATIPU 2050 Contents
HAURAKI DISTRICT GROWTH STRATEGY TE RAUTAKI WHAKATIPU 2050 Contents 3 Foreword | Kuku Whakataki 4 Overview | Tirohanga whānaui 5 SECTION 1: DISTRICT PROFILE | KŌRERO A ROHE 6 Demographic Trends 9 Existing Development 9 Capacity for Growth 10 Summary of Development Constraints and Opportunities 11 Treaty Settlements 12 Infrastructure 15 Natural Features 17 Historic Heritage 18 Natural Hazards 22 SECTION 2: GROWTH STRATEGY | TE RAUTAKI WHAKATIPU 23 Key Principles for Growth 24 Strategic Direction for Growth 33 Future Capacity Analysis 34 SECTION 3: IMPLEMENTATION | TE WHAKATINANATANGA 35 Implementation actions and timeframes 37 ATTACHMENTS LISTS OF FIGURES 6 Table 1: District and Town Population Projections 7 Table 2: District Dwellings Projections 7 Table 3: District Rating Units Projections 7 Diagram 1: Industry proportion of GDP, 2018 7 Table 4: Biggest contribution to economic growth 2008 - 2018 8 Table 5: Industries which created most jobs, 2008-2018 9 Table 6: Potential development of existing zones 10 Diagram 2: Land availability for expected residential and business development growth - 30 years 10 Diagram 3: Summary of main development contraints and opportunities for the District over the next 30 years 19 Table 7: Natural Hazard Risk Assessment * 24 Map 1 Strategic direction for growth 27 Map 2: Existing and growth areas of Waihi 29 Map 3: Existing and growth areas of Paeroa 31 Map 4: Existing and growth areas of Ngatea 33 Table 8: Development Capacity 35 Table 9: Implementation Actions and Timeframes (Short term = 1-5 years, Medium term = 5-15 years, Long term = 15-30 years) 38 Table 10: “Refined” Hauraki hazards risk evaluation (See Appendix 6 for key) 2 Foreword | Kuku Whakataki The future looks bright in the Hauraki District. -
New Zealand's Fresh Waters
OFFICE OF THE PRIME MINISTER’S CHIEF SCIENCE ADVISOR Professor Sir Peter Gluckman, KNZM FRSNZ FMedSci FRS Chief Science Advisor New Zealand’s fresh waters: Values, state, trends and human impacts 12 April 2017 Office of the Prime Minister’s Chief Science Advisor PO Box 108-117, Symonds Street, Auckland 1150, New Zealand Telephone: +64 9 923 6318 Website: www.pmcsa.org.nz Email: [email protected] ACKNOWLEDGMENTS This set of reports is the result of a lengthy collaborative effort initiated and guided by Sir Peter Gluckman, the Prime Minister’s Chief Science Advisor (PMCSA). Development of the technical report was led by Dr Bryce Cooper, working with Drs Clive Howard-Williams, Scott Larned and John Quinn of the freshwater team at the National Institute of Water and Atmospheric Research (NIWA), and the Office of the PMCSA. Coordination of the project and preparation of the summary report was led by Dr Anne Bardsley of the Office of the PMCSA, in close collaboration with Dr Ken Hughey, Chief Science Advisor for the Department of Conservation, and Dr David Wratt, Departmental Science Advisor for the Ministry for the Environment. We gratefully acknowledge the input of the following reviewers: David Hamilton, University of Waikato Ken Taylor, AgResearch; Our Land and Water National Science Challenge Roger Young, Cawthron Institute Brett Eaton, University of British Columbia Neil Deans, Ministry for the Environment Wes Patrick, Ministry for the Environment Joanne Perry, Department of Conservation Adam Tipper, Stats NZ We also thank Kristiann Allen