The Geology of New Zealand
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Quaternaryaustralasia
Volume 24 | Number 2 | July 2007 Quaternary AUSTRALASIA • MICROFOSSILS IN THE FLINDERS RANGES • NEW ZEALAND GLACIATION • AUSTRALIAN-CHINESE QUATERNARY CONNECTIONS • CARBON ISOTOPE VARIABILITY IN AUSTRALIAN GRASSES Volume 24 | Number 2 | July 2007 | ISSN 0811–0433 Quaternary AUSTRALASIA 1 Editorial, President’s Pen Feature Article 2 Professor Liu Tungsheng: Australian-Chinese Quaternary connections JIM BOWLER, WITH INTRODUCTION BY DONALD WALKER Research Articles 11 A reconnaissance study of glaciation on the Owen Massif, northwest Nelson, New Zealand OLIVIA HYATT, JAMES SHULMEISTER, CHRIS SMART 19 Late Pleistocene environments in the Flinders Ranges, Australia: Preliminary evidence from microfossils and stable isotopes PETER GLASBY, MARTIN WILLIAMS, DAVID MCKIRDY, REX SYMONDS, ALLAN CHIVAS 29 Carbon isotope discrimination by C3 pasture grasses along a rainfall gradient in South Australia: Implications for palaeoecological studies DONALD PATE, EVELYN KRULL Meeting Reports 34 Southern Connection Conference, Adelaide PETER KERSHAW COVER The cover photograph shows late 37 ANZGG Rivers Workshop, Canberra and Kioloa KATHRYN AMOS, RACHEL NANSON Pleistocene fine deposits unconformably overlying Proterozoic Rocks of the Brachina 40 International Young Scientists’ Global Change Conference and Earth System formation in the Flinders Ranges. This Science Partnership’s Open Science Conference, Beijing, China JOËLLE GERGIS section forms the basis for microfossil and 43 Plant Macrofossil Workshop, Adelaide JOHN TIBBY stable isotope studies discussed in the research paper by Peter Glasby and others in Book Reviews this issue. (Photo: David Haberlah) 44 John Merrick et al.: Evolution and biogeography of Australasian vertebrates BELOW Oblique aerial view of the coarse- REVIEWED BY RICHARD GILLESPIE grained sand beach ridges at Cowley Beach, 44 Chris Johnson: Australia’s mammal extinctions 100km south of Cairns. -
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 -
Geocene Auckland Geoclub Magazine Number 23, July 2020
Geocene Auckland GeoClub Magazine Number 23, July 2020 Editor: Jill Kenny CONTENTS Instructions on use of hyperlinks last page 26 A CURIOUS CASE OF RIVERBED POTHOLES IN Michael Coote, Kent Xie 2 – 6 WEST AUCKLAND GRANITE FLUTING, BASINS AND TAFONE ON Lee Sawyer, Ken Smith, 7 – 10 SOUTHERN STEWART ISLAND Bruce W. Hayward EVIDENCE FOR TUFFS AT MANGAWHAI HEADS Garry Carr 11 – 13 EXHUMED LAVA CAVE AT KERIKERI, NORTHLAND Bruce W. Hayward 14 – 15 A RECORD OF THE DISTINCTIVE BRYOZOAN GENUS Seabourne Rust 16 – 18 RETELEPRALIA FROM THE EARLY MIOCENE WAITIITI FORMATION OF NORTHLAND, NEW ZEALAND IHUMATAO ROAD END FOSSIL FOREST Bruce W. Hayward, 19 – 21 Maureen Burke RAFTS OF PLEISTOCENE SEDIMENT IN Bruce W. Hayward 22 – 25 PUPUKE VOLCANO LAVA FLOWS Corresponding authors’ contact information 26 Geocene is a periodic publication of Auckland Geology Club, a section of the Geoscience Society of New Zealand’s Auckland Branch. Contributions about the geology of New Zealand (particularly northern New Zealand) from members are welcome. Articles are lightly edited but not refereed. Please contact Jill Kenny [email protected] 1 A CURIOUS CASE OF RIVERBED POTHOLES IN WEST AUCKLAND Michael Coote Map and photographs by Kent Xie Natural rock potholes at Woodside Reserve, Swanson two or more underlying, often oblique potholes, totalling During the COVID-19 lockdown period, local exercise up to about 1 m in depth in the biggest example. was promoted as official government policy. This situation encouraged the authors to look up maps for local The majority of the potholes were filled with water, but walkways, rights-of-way and reserves not previously most were above the water level of the stream. -
Mt Owen Guidelines Page 1 of 13 Version 6-10
New Zealand Speleological Society Guidelines for Caving and Camping on the Mount Owen Massif: A Guide for Local and Overseas Cavers Occasional publication number 14 NZSS Mt Owen Guidelines Page 1 of 13 Version 6-10 Contents Acknowledgement ..................................................................................................................................... 3 Copyright ...................................................................................................................................... 3 Amendments ................................................................................................................................ 3 Summary ................................................................................................................................................... 3 Caving in NZ ............................................................................................................................................. 4 Liaison with New Zealand Speleological Society (NZSS) ........................................................... 4 NZ Caving Ethics ......................................................................................................................... 4 Caving Style ................................................................................................................................. 5 Rigging Style ................................................................................................................................ 5 Cave Conservation ..................................................................................................................... -
Nelson Tramping Club High Mis-Adventure
Nelson Tramping Club December 2018 Newsletter of the NELSON TRAMPING CLUB Founded 1934, Nelson, New Zealand www.nelsontrampingclub.org.nz EDITORIAL COMMENT that you never do a multi-day, off-track, solo High mis-Adventure tramp on a long weekend in the Tasman region during summer afternoons. Especially if you’re a Did you realise that you are living in a hot spot for man aged 50–64, like myself. tramping fatalities? The Tasman region is the second most dangerous in NZ, according to MSC’s recent What shall I do, to avoid becoming a statistic? report, A Walk In The Park. Short of swapping my boots for a set of golf clubs … or doing DOC’s great walks on Google Diving into the scary statistics, it’s a miracle I am Earth … I will need to relocate to Northland, still standing. For starters, I do lots of solo tramping, where there’s little chance of falling off anything (a necessary evil of being a semi-pro landscape higher than a sand dune. I’ll need to join a photographer). Of the 57 trampers who perished group that does mid-week day walks in winter. during the past decade, 21 were men alone. Oh, and I’ll require a sex-change. “Solo trampers (that’s me) … were disproportionately Ray Salisbury high among men (me) tramping in the Tasman Area Idioter (me again).” Indeed, of the 10 local fatalities from 2007-2017… • 80% were male • 70% were tramping solo • 70% of these tragedies occurred during December and February • 35% of local trampers involved in SAR call-outs were aged 50–64 • Nearly 60% of deaths happened on multi-day expeditions From this analysis, it appears I have a target on my back; the proverbial clock is ticking; I gamble with my limbs or my life each time I lace up my boots. -
Download the Intentions Wilder Spots
Nelson Tramping Club March 2016 Newsletter of the NELSON TRAMPING CLUB Founded 1934, Nelson, New Zealand www.nelsontrampingclub.org.nz PRESIDENT’s PIECE : Keep your powder dry No cotton – Cotton underwear and tee-shirts quickly absorb rainwater and sweat, are slow to A couple of recent trips in the hills provided dry and provide little insulation. Hypothermia can me with some reminders of the pleasures and follies arise under mild conditions, especially with wind. of our wonderful pursuit. Here are a few gems of The core body is the key to keeping the extremities wisdom that I have gathered from these trips and warm. Make sure you use wool or synthetic layers, others. I offer them in the spirit of instruction, not even in summer, as these provide some insulation destruction. Some of the follies are my own; others when damp. And carry some spares. by tramping friends who shall remain nameless. Tenting – it is a challenge to keep gear dry in It is axiomatic that some of our trips will be wet conditions including the making or breaking conducted in less than ideal weather. Even careful of camp. Modern nylon tents with flies do not prior study of weather maps cannot preclude all risk generally leak much if in good condition. But care of wind and rain for multi-day trips. I believe an and discipline are essential so tracking of water unduly cautious approach to trip planning detracts into the tent and gear is minimised. A pack cover from the totality of our experience in the hills. The is excellent, so the wet pack can stay outside the changeable New Zealand climate indeed offers tent. -
The Mid-Cenozoic Challenger Rift System of Western New Zealand and Its Implications for the Age of Alpine Fault Inception
The mid-Cenozoic Challenger Rift System of western New Zealand and its implications for the age of Alpine fault inception PETER J. J. KAMP Department of Earth Sciences, University of Waikato, Hamilton, 2001, New Zealand ABSTRACT finger-like re-entrants of the Late Cretaceous New Caledonia basin and Bounty Trough, which both protrude into the subcontinent. The objective Analysis of the structure and sedimentary geology of western of this paper is to document evidence for another rift system, of Eocene- New Zealand has identified a middle Eocene to early Miocene conti- Oligocene age, named here the "Challenger Rift System," which trended nental rift system, 1,200 km long and 100-200 km wide, named here north-south through western New Zealand from the Norfolk basin to the the "Challenger Rift System." Four phases of rift development oc- Solander Trough (Fig. 1). This rift, by dissecting the subcontinent, induced curred: (1) infra-rift subsidence, (2) active axial trough subsidence, (3) subsidence of its most interior parts. It also indicates that the foundering expanded rift subsidence involving collapse of the rift shoulders, and was associated with at least two periods of rifting, one in the Late Creta- (4) incipient sea-floor spreading. The spatial and temporal distribution ceous and another in the mid-Cenozoic. of these phases identifies a North Island and a South Island rift seg- The Challenger Rift System is named after the Challenger Plateau, a ment and shows that rifting propagated toward the center of the rift shallowly submerged portion of the New Zealand subcontinent (Law- from both ends. -
Mineral, Coal and Petroleum Resources: Production,Exploration and Potential
2.3 MINERAL, COAL AND PETROLEUM RESOURCES MINERAL, COAL AND PETROLEUM RESOURCES: PRODUCTION, EXPLORATION AND POTENTIAL Anthony B. Christie1, Richard G. Barker2 1 GNS Science, PO Box 30-368, Lower Hutt 5040, New Zealand 2 Consulting Geologist, PO Box 54-094, The Marina, Bucklands Beach, Auckland 2144, New Zealand ABSTRACT: New Zealand has been a signifi cant producer of minerals and coal since early European settlement in the mid-19th century, and of hydrocarbons since 1970. Current production consists of oil, gold and silver, high quality (bituminous) coal, ironsand and specialised industrial minerals such as halloysite china clay for export, and a range of minerals and rocks for domestic use that are fundamental to New Zealand’s economy and infrastructure. The latter include aggregate for road making and construction (concrete aggregate and cement), coal for use by industry and electricity generation, and limestone for agriculture, cement making, and industry. Small quantities of diatomite, dolomite, perlite, pumice, serpentinite, and zeolite are also produced mainly for domestic markets. Other commodities that have been produced in the past include antimony, chromium, copper, lead, manganese, mercury, phosphate, platinum, sulphur, tin, tungsten, and zinc. New Zealand has well-documented potential for the discovery of a wide range of minerals and of petroleum, both onshore and offshore. Exploration is essential for converting this resource potential to wealth-creating assets. The resource-related industries are signifi cant economic contributors, but New Zealand’s resource potential remains to be realised. Mineral resources are created by natural processes and are generally described as non-renewable, implying they are fi nite, but many minerals (metals in particular) have been produced for several thousand years. -
The Last Interglacial Sea-Level Record of Aotearoa New Zealand (Aotearoa)
The last interglacial sea-level record of Aotearoa New Zealand (Aotearoa) Deirdre D. Ryan1*, Alastair J.H. Clement2, Nathan R. Jankowski3,4, Paolo Stocchi5 1MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany 5 2School of Agriculture and Environment, Massey University, Palmerston North, New Zealand 3 Centre for Archeological Science, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, Australia 4Australian Research Council (ARC) Centre of Excellence for Australian Biodiversity and Heritage, University of Wollongong, Wollongong, Australia 10 5NIOZ, Royal Netherlands Institute for Sea Research, Coastal Systems Department, and Utrecht University, PO Box 59 1790 AB Den Burg (Texel), The Netherlands Correspondence to: Deirdre D. Ryan ([email protected]) Abstract: This paper presents the current state-of-knowledge of the Aotearoa New Zealand (Aotearoa) last interglacial (MIS 5 sensu lato) sea-level record compiled within the framework of the World Atlas of Last Interglacial Shorelines (WALIS) 15 database. Seventy-seven total relative sea-level (RSL) indicators (direct, marine-, and terrestrial-limiting points), commonly in association with marine terraces, were identified from over 120 studies reviewed. Extensive coastal deformation around New Zealand has prompted research focused on active tectonics, which requires less precision than sea-level reconstruction. The range of last interglacial paleo-shoreline elevations are resulted in a significant range of elevation measurements on both the North Island (276.8 ± 10.0 to -94.2 ± 10.6 m amsl) and South Island (173.1165.8 ± 2.0 to -70.0 ± 10.3 m amsl) and 20 prompted the use of RSL indicators tohave been used to estimate rates of vertical land movement; however, indicators in many instances lackk adequate description and age constraint for high-quality RSL indicators. -
4.2.6 Desired Outcome for Hokitika Place Section 4.2.6 Describes What the Hokitika Place Will Be Like in 2020 If the Direction of This CMS Is Followed
The Mäwhera Place provides opportunities for recreational sports fishing, whitebaiting, game bird, deer, chamois, goat and pig hunting. See also Chapter 3.5 Authorised Uses of Public Conservation Lands Chapter 3.6 People’s Benefit and Enjoyment 4.2.6 Desired Outcome for Hokitika Place Section 4.2.6 describes what the Hokitika Place will be like in 2020 if the direction of this CMS is followed. See also Chapter 4.1 Desired outcome for the Conservancy 4.2.6.1 Place description The Hokitika Place extends from the Taramakau River in the north to the Waitaha River catchment in the south and inland to the crest of the Southern Alps Kä Tiritiri o te Moana (Maps 16-17). Part of Arthur’s Pass National Park is located within this Place (see Map 16). Hokitika is split in two both geologically and ecologically by the Alpine Fault, which lies about 20 km west of the crest of the Main Divide. East of the fault, the schist mountains and valleys are rugged and broken, and a large portion is protected as public conservation land. West of the fault the geology is more complex, landscapes extensively modified and public conservation lands fragmented. This Place is the historic heart of the West Coast Te Tai o Poutini ’s pounamu trade and is the scene of gold mining, forestry and farming industries - particularly dairying. Hokitika is the largest town (population of 3,700 as at 2010). 4.2.6.2 Arthur’s Pass National Park in 2020 Arthur’s Pass National Park straddles the Main Divide of the Southern Alps Kä Tiritiri o te Moana . -
Maori Cartography and the European Encounter
14 · Maori Cartography and the European Encounter PHILLIP LIONEL BARTON New Zealand (Aotearoa) was discovered and settled by subsistence strategy. The land east of the Southern Alps migrants from eastern Polynesia about one thousand and south of the Kaikoura Peninsula south to Foveaux years ago. Their descendants are known as Maori.1 As by Strait was much less heavily forested than the western far the largest landmass within Polynesia, the new envi part of the South Island and also of the North Island, ronment must have presented many challenges, requiring making travel easier. Frequent journeys gave the Maori of the Polynesian discoverers to adapt their culture and the South Island an intimate knowledge of its geography, economy to conditions different from those of their small reflected in the quality of geographical information and island tropical homelands.2 maps they provided for Europeans.4 The quick exploration of New Zealand's North and The information on Maori mapping collected and dis- South Islands was essential for survival. The immigrants required food, timber for building waka (canoes) and I thank the following people and organizations for help in preparing whare (houses), and rocks suitable for making tools and this chapter: Atholl Anderson, Canberra; Barry Brailsford, Hamilton; weapons. Argillite, chert, mata or kiripaka (flint), mata or Janet Davidson, Wellington; John Hall-Jones, Invercargill; Robyn Hope, matara or tuhua (obsidian), pounamu (nephrite or green Dunedin; Jan Kelly, Auckland; Josie Laing, Christchurch; Foss Leach, stone-a form of jade), and serpentine were widely used. Wellington; Peter Maling, Christchurch; David McDonald, Dunedin; Bruce McFadgen, Wellington; Malcolm McKinnon, Wellington; Marian Their sources were often in remote or mountainous areas, Minson, Wellington; Hilary and John Mitchell, Nelson; Roger Neich, but by the twelfth century A.D. -
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JANUARYHIGHLIGHTS | KOTITĀTEA 2017 Royal Society Te Apārangi EXPLORE DISCOVER SHARE Royal Society Te Apārangi I HIGHLIGHTS 2017 01 HIGHLIGHTS 2017 02 JANUARY | KOTITĀTEA HIGHLIGHTS 2017 23 JUNE PIPIRI Matariki and the Pleiades: our world from different lights Launch of New Zealand ORCID Hub Students attend overseas science and technology opportunities CONTENTS Alumni series launched Innovative technology to detect OCTOBER WHIRINGA-Ā-NUKU disease-causing bacteria 46 Accelerating research careers with Progress for biosystematics and Rutherford Discovery Fellowships taxonomy 2017 New Zealand Research Honours JULY HŌNGONGOI 05 OUR YEAR IN REVIEW 30 Climate change will disrupt many Cutting-edge information for MPs factors that contribute to our health JANUARY KOTITĀTEA He waka eke noa: Mentoring in the 06 Aotearoa research community Researchers recognised for Drones to support search and sustained research excellence rescue Bilingual approach for Primary Science Conference Highly promising researchers awarded fellowships and FEBRUARY HUITĀNGURU scholarships 08 AUGUST HERETURIKŌKĀ Valuing nature in a human- 34 Great Kiwi Research, Sharing dominated world 150 Women in 150 Words Women’s Discoveries Making the Science Teaching Talk it up – should New Zealand Leadership Programme more develop a national languages NOVEMBER WHIRINGA-Ā-RANGI culturally responsive policy? 56 Diverse topics important for New Better engagement with Māori Marsden Fund investment plan Zealand supported by the Marsden researchers released and discussed Fund 150th Anniversary