Section 2: Objectives and Policies
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Quarterly Bulletin of The Ornithological Society of New Zealand Volume 7, Number Seven :January l 958 NOTORNIS In continuation of New Zealand Bird Notes BULLETIN OP THE ORNITHOLOGICAL SOCIETY OF NEW ZBALAND (Incorporated) Registered with the G.P.O., Wellington, as a Magazine Edited by R. B. SIBSON, King's College, Auckland S.E.7 Annual Subscription, 10/- (Juniors, 5/-); Endowment Membership, Cl; Life Membership, E10 (for members over thirty years of age). OFFICERS, 1957 - 58 President - MR P. C. BULL, Lower Hutt. North Island Vice-President - MR E. G. TURBOTT, Christchurcb South Island Vice-President - MRS L. E. WALKER, Dunedin Editor- MR R. B. SIBSON, King's College, Auckland S.E.7 Treasurer - MR H. R. McKENZIE, North Road, Clevedon Secretary - MR G. R. WILLIAMS, Wildlife Division, Department of Internal Affairs, Wellington MRS 0. SANSOM, Invercargill; DR R. A. FALLA, Wellington; MR J. C. DAVENPORT, Auckland Contents of Volume 7, Number 7 : January 1958 Some Notes on Muttonbirding in the North Island- W. J. Phillipps 189 Classified Summarised Notes .................................... 191 Annual Locality Reports for Firth of Thames and Manukau Harbour 201 Obituary: W. R. B. Oliver ....................................205 Short Notes mentioning: S.I. Pied Oystercatcher, White-faced Heron, Spotted Shag, Barn Owl, Spur-winged Plover, Crested Grebe, 'Red- legged ' Herons, Myna in !;.I., Bush-hawk, Weka ................ 206 Review8 .................................................... 2 11 Notices. XIIth International Ornithological Congress ............ 212 Nest Records Scherne Publications for sale Donations NOTORNI S VOLUME SEVEN NUMBER SEVEN : JANUARY NINETEEN FIFTY-EIGHT SOME NOTES ON MUTTONBIRDIING IN THE NORTH ISLAND By W. 1. PHILLIPPS During the period 1919- 1924 odd notes were collected on the occurrence of muttonbirds breeding on Mount Pihanga not far from Lake Rotoaira. -
Circulation and Mixing in Greater Cook Strait, New Zealand
OCEANOLOGICA ACTA 1983- VOL. 6- N" 4 ~ -----!~- Cook Strait Circulation and mixing Upwelling Tidal mixing Circulation in greater Cook S.trait, Plume Détroit de Cook Upwelling .New Zealand Mélange Circulation Panache Malcolm J. Bowrnan a, Alick C. Kibblewhite b, Richard A. Murtagh a, Stephen M. Chiswell a, Brian G. Sanderson c a Marine Sciences Research Center, State University of New York, Stony Brook, NY 11794, USA. b Physics Department, University of Auckland, Auckland, New Zealand. c Department of Oceanography, University of British Columbia, Vancouver, B.C., Canada. Received 9/8/82, in revised form 2/5/83, accepted 6/5/83. ABSTRACT The shelf seas of Central New Zealand are strongly influenced by both wind and tidally driven circulation and mixing. The region is characterized by sudden and large variations in bathymetry; winds are highly variable and often intense. Cook Strait canyon is a mixing basin for waters of both subtropical and subantarctic origins. During weak winds, patterns of summer stratification and the loci of tidal mixing fronts correlate weil with the h/u3 stratification index. Under increasing wind stress, these prevailing patterns are easily upset, particularly for winds b1owing to the southeasterly quarter. Under such conditions, slope currents develop along the North Island west coast which eject warm, nutrient depleted subtropical water into the surface layers of the Strait. Coastal upwelling occurs on the flanks of Cook Strait canyon in the southeastern approaches. Under storm force winds to the south and southeast, intensifying transport through the Strait leads to increased upwelling of subsurface water occupying Cook Strait canyon at depth. -
Flora of New Zealand Mosses
FLORA OF NEW ZEALAND MOSSES BRACHYTHECIACEAE A.J. FIFE Fascicle 46 – JUNE 2020 © Landcare Research New Zealand Limited 2020. Unless indicated otherwise for specific items, this copyright work is licensed under the Creative Commons Attribution 4.0 International licence Attribution if redistributing to the public without adaptation: "Source: Manaaki Whenua – Landcare Research" Attribution if making an adaptation or derivative work: "Sourced from Manaaki Whenua – Landcare Research" See Image Information for copyright and licence details for images. CATALOGUING IN PUBLICATION Fife, Allan J. (Allan James), 1951- Flora of New Zealand : mosses. Fascicle 46, Brachytheciaceae / Allan J. Fife. -- Lincoln, N.Z. : Manaaki Whenua Press, 2020. 1 online resource ISBN 978-0-947525-65-1 (pdf) ISBN 978-0-478-34747-0 (set) 1. Mosses -- New Zealand -- Identification. I. Title. II. Manaaki Whenua-Landcare Research New Zealand Ltd. UDC 582.345.16(931) DC 588.20993 DOI: 10.7931/w15y-gz43 This work should be cited as: Fife, A.J. 2020: Brachytheciaceae. In: Smissen, R.; Wilton, A.D. Flora of New Zealand – Mosses. Fascicle 46. Manaaki Whenua Press, Lincoln. http://dx.doi.org/10.7931/w15y-gz43 Date submitted: 9 May 2019 ; Date accepted: 15 Aug 2019 Cover image: Eurhynchium asperipes, habit with capsule, moist. Drawn by Rebecca Wagstaff from A.J. Fife 6828, CHR 449024. Contents Introduction..............................................................................................................................................1 Typification...............................................................................................................................................1 -
Taranaki-Whanganui Conservation Board Notice of Appeal
To The ReGistrar of the HiGh Court at WellinGton and To The Respondent and To The Applicant and To Other submitters This document notifies you that: 1 The appellant, being the Taranaki-WhanGanui Conservation Board (Conservation Board), will move the HiGh Court at WellinGton by way of appeal against the decision of the majority decision of the decision making committee of the Environmental Protection Authority (DMC), dated 3 AuGust 2017, public notice #EEZ000011, in which a marine consent and marine discharge consent was granted to Trans-Tasman Resources Limited (TTRL). The Application and Decision 2 TTRL applied for marine consents and marine discharge consents to enable it to mine iron sands in the South Taranaki BiGht, 22-36km offshore (Application). Up to 50 million tonnes of seabed material could be mined and processed each year, for up to 35 years. 3 The Environmental Protection Authority (EPA) made its decision on the application through its DMC (Decision). The DMC’s Decision was split. Two of the DMC’s members considered that the consents should be refused. They took the view that: … overall the localised adverse environmental effects on the Patea Shoals and tangata whenua existing interests are unacceptable, and are not avoided, remedied or mitigated by the conditions imposed. We also have concerns reGardinG uncertainty and the adequacy of environmental protection within the coastal marine area (CMA).1 4 However, the Chair held the castinG vote, and exercised it in favour of granting consent. Accordingly, the “majority decision” was to grant consent. 5 The DMC made its Decision on 3 August 2017. -
Aquatic Ecology of Lake Rotokare, Taranaki, and Options for Restoration
Aquatic ecology of Lake Rotokare, Taranaki, and options for restoration 2013 ERI report number 14 A report prepared for the Rotokare Scenic Reserve Trust by Brendan J. Hicks, Dudley G. Bell, Ian Duggan, Susie Wood1 and Grant Tempero Environmental Research Institute School of Science Faculty of Science and Engineering University of Waikato, Private Bag 3105 Hamilton 3240, New Zealand 1Cawthron Institute, Private Bag 2, Nelson 7042, New Zealand 2 Table of contents Executive summary ................................................................................................................................. 5 Introduction ............................................................................................................................................ 7 Methods .................................................................................................................................................. 9 Water quality ...................................................................................................................................... 9 Conductivity and Secchi disc depth ................................................................................................ 9 Dissolved oxygen ............................................................................................................................. 9 Dissolved nutrients ......................................................................................................................... 9 Fish ................................................................................................................................................... -
Blue Whale Ecology in the South Taranaki Bight Region of New Zealand
Blue whale ecology in the South Taranaki Bight region of New Zealand January-February 2016 Field Report March 2016 1 Report prepared by: Dr. Leigh Torres, PI Assistant Professor; Oregon Sea Grant Extension agent Department of Fisheries and Wildlife, Marine Mammal Institute Oregon State University, Hatfield Marine Science Center 2030 SE Marine Science Drive Newport, OR 97365, U.S.A +1-541-867-0895; [email protected] Webpage: http://mmi.oregonstate.edu/gemm-lab Lab blog: http://blogs.oregonstate.edu/gemmlab/ Dr. Holger Klinck, Co-PI Technology Director Assistant Professor Bioacoustics Research Program Oregon State University and Cornell Lab of Ornithology NOAA Pacific Marine Environmental Laboratory Cornell University Hatfield Marine Science Center 159 Sapsucker Woods Road 2030 SE Marine Science Drive Ithaca, NY 14850, USA Newport, OR 97365, USA Tel: +1.607.254.6250 Email: [email protected] Collaborators: Ian Angus1, Todd Chandler2, Kristin Hodge3, Mike Ogle1, Callum Lilley1, C. Scott Baker2, Debbie Steel2, Brittany Graham4, Philip Sutton4, Joanna O’Callaghan4, Rochelle Constantine5 1 New Zealand Department of Conservation (DOC) 2 Oregon State University, Marine Mammal Institute 3 Bioacoustics Research Program, Cornell Lab of Ornithology, Cornell University 4 National Institute of Water and Atmospheric Research, Ltd. (NIWA) 5 University of Auckland, School of Biological Sciences Research program supported by: The Aotearoa Foundation, The National Geographic Society Waitt Foundation, The New Zealand Department of Conservation, The Marine Mammal Institute at Oregon State University, The National Oceanographic and Atmospheric Administration’s Cooperative Institute for Marine Resources Studies (NOAA/CIMRS), Greenpeace New Zealand, OceanCare, Kiwis Against Seabed Mining, and an anonymous donor. -
Retrieval of Suspended Sediment Concentration in Near-Shore Coastal Waters Using MODIS Data
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. Retrieval of suspended sediment concentration in near-shore coastal waters using MODIS data A thesis presented in partial fulfilment of the requirements for the degree of Master of Philosophy In Earth Science At Massey University, Palmerston North New Zealand Di Zhou 2012 1 Abstract: This study focuses on using remote sensing satellite data to retrieve water suspended sediment concentration (SSC) of near-shore coastal waters. Aqua/Terra Satellite MODIS 250m data of the south-western coast of the North Island, New Zealand was used. Two methods of analysis are used in this study to obtain an SSC map; non-liner optimisation and quasi-analytical. The non-linear optimisation method was used to fit an exponential function between reflectance and SSC, with SSC replaced by a linear relationship between SSC and reflectance in the near infrared domain. The optimisation result was used to convert Aqua/Terra MODIS images to SSC maps. The quasi-analytical method, a backscattering coefficient at 645nm is first derived from Aqua/Terra MODIS 250m Band 1 data using a quasi-analytical algorithm after applying a simple atmospheric correction routine. An empirical relationship was derived from laboratory experiments. Finally SSC maps were obtained by applying the empirical relationship to convert the backscattering coefficient to SSC. 2 Acknowledgements I would firstly like to thank my supervisor Mike Tuohy for his time and thoughtful advice throughout the preparation of this thesis. -
Appendix C – Geotechnical Assessment
Appendix C – Geotechnical Assessment Whanganui District Council Mill Road Structure Plan Geotechnical Assessment October 2017 Table of contents 1. Introduction ............................................................................................................................... 3 1.1 Introduction ..................................................................................................................... 3 1.2 Scope of this report ......................................................................................................... 3 1.3 General Site Setting ........................................................................................................ 3 2. Published Geological Information .............................................................................................. 4 2.1 Geology .......................................................................................................................... 4 2.2 Earthquakes .................................................................................................................... 5 2.3 Known Active Faults ........................................................................................................ 6 2.4 Liquefaction Susceptibility ............................................................................................... 6 2.5 Slope Stability ................................................................................................................. 6 2.6 Site Sub-Soil Class ......................................................................................................... -
Seabed Mining (KASM), Posted a Facebook Page Inviting People to Turn up at the Stadium When Hearings Began
MINING MINEFIELD A company called Trans-Tasman Resources is having a second go at setting up a world-first project to mine iron ore from the seabed off South Taranaki’s coast. The company (TTR) has spent a decade and about $70 million to hone its case for Environmental Protection Authority (EPA) consent to take more than a billion tonnes of iron- bearing sand off the sea floor over 25 or so years. The process – which will return 90 percent of what’s extracted back to the seabed - will bring in about $400 million a year in off-shore ore sales, with our government getting about $6 million in annual royalties. The project is expected to increase Taranaki’s gross domestic product by about $220 million a year (half that of Methanex) and create about 300 jobs. Sound like a good deal? Somewhere between 13,733 and about 17,000 people (the total is disputed) don’t think so. Many people living in South Taranaki and further afield, local iwi, most of the fishing industry, and a close-neighbour oil company are worried about what it might do to the environment and local communities. That uncertainty has prompted their representative organisations and many individuals to fight the company to the bitter end. The case will be a precedent-setter under the Exclusive Economic Zone (EEZ) Act. Environmentalists don’t like the law, partly because it excludes climate change-causing emissions as grounds for objection, and partly because they reckon it’s the National government’s way of opening up our 200 kilometre-wide continental shelf to big overseas business. -
Temporal and Spatial Lags Between Wind, Coastal Upwelling, and Blue Whale Occurrence Dawn R
www.nature.com/scientificreports OPEN Temporal and spatial lags between wind, coastal upwelling, and blue whale occurrence Dawn R. Barlow1*, Holger Klinck2,3, Dimitri Ponirakis2, Christina Garvey4 & Leigh G. Torres1 Understanding relationships between physical drivers and biological response is central to advancing ecological knowledge. Wind is the physical forcing mechanism in coastal upwelling systems, however lags between wind input and biological responses are seldom quantifed for marine predators. Lags were examined between wind at an upwelling source, decreased temperatures along the upwelling plume’s trajectory, and blue whale occurrence in New Zealand’s South Taranaki Bight region (STB). Wind speed and sea surface temperature (SST) were extracted for austral spring–summer months between 2009 and 2019. A hydrophone recorded blue whale vocalizations October 2016-March 2017. Timeseries cross-correlation analyses were conducted between wind speed, SST at diferent locations along the upwelling plume, and blue whale downswept vocalizations (D calls). Results document increasing lag times (0–2 weeks) between wind speed and SST consistent with the spatial progression of upwelling, culminating with increased D call density at the distal end of the plume three weeks after increased wind speeds at the upwelling source. Lag between wind events and blue whale aggregations (n = 34 aggregations 2013–2019) was 2.09 ± 0.43 weeks. Variation in lag was signifcantly related to the amount of wind over the preceding 30 days, which likely infuences stratifcation. This study enhances knowledge of physical-biological coupling in upwelling ecosystems and enables improved forecasting of species distribution patterns for dynamic management. A central pursuit of ecology is to decipher and understand the complex relationships between biological organ- isms and their physical environment. -
North Island 1
Wetlands to visit in the North Island 1. Te Werahi, Northland 2. Lake Ohia, Northland You can start your journey of magical wetlands near the Lake Ohia is an other-worldly place of charred stumps and !1 northern tip of New Zealand in a remote but highly natural gumland scrub that casts a strange sort of magic over you. and scenic landscape. Te Werahi is a good stopping place on The area was once an ancient kauri forest, then a lake that was your way to or back from Cape Reinga. From the road, you will subsequently drained in the 1900s for gum digging, exposing !2 Kaitaia ! see a large freshwater wetland system, which has three raupō a maze of 30,000-year-old kauri stumps. It is now an important swamps linked by narrow sandy streams. It is an important site habitat for rare ferns, mosses and orchids. Lake Ohia is an for wetland birds such as Australasian bitterns/matuku, grey ephemeral lake that usually dries out in summer and is wet in ducks, grey teals/tētē, NZ shovelers/kuruwhengi, pied stilts/ winter. Whangarei !3 ! 4 poaka, pied shags and little shags. Dargaville ! Places to explore Places to explore The Gumhole Reserve Walk is a 10 min loop through mānuka !5 The wetland can be accessed scrub and passes a series of holes excavated by gum diggers. via boardwalks down the Many of the holes are deep so keep to the track. Throughout Twilight–Te Werahi Loop the walk you’ll find information about the history of the site ! Auckland track. -
Benthic Flora and Fauna of the Patea Shoals Region, South Taranaki Bight
Benthic flora and fauna of the Patea Shoals region, South Taranaki Bight Prepared for Trans-Tasman Resources Ltd October 2013 (Updated November 2015) Authors/Contributors: J. Beaumont, T.J. Anderson, A.B. MacDiarmid For any information regarding this report please contact: Tara J. Anderson NIWA Nelson +64-3-545 7746 National Institute of Water & Atmospheric Research Ltd 301 Evans Bay Parade, Greta Point Wellington 6021 Private Bag 14901, Kilbirnie Wellington 6241 New Zealand Phone +64-4-386 0300 Fax +64-4-386 0574 NIWA Client Report No: WLG2012-55 Report date: October 2013 NIWA Project: TTR11301 © All rights reserved. This publication may not be reproduced or copied in any form without the permission of the copyright owner(s). Such permission is only to be given in accordance with the terms of the client’s contract with NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. Whilst NIWA has used all reasonable endeavours to ensure that the information contained in this document is accurate, NIWA does not give any express or implied warranty as to the completeness of the information contained herein, or that it will be suitable for any purpose(s) other than those specifically contemplated during the Project or agreed by NIWA and the Client. 30 November 2015 12.33 p.m. Contents Executive summary ............................................................................................................. 9 1 Introduction ............................................................................................................ 12 1.1 Background ............................................................................................................. 12 1.1.1 Iron ore and seabed extraction ............................................................... 12 1.2 Previous research on the benthic fauna of the South Taranaki Bight .................... 13 1.3 NIWA’s brief ...........................................................................................................