Journal of the RNZIH
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The New Zealand Rain Forest: a Comparison with Tropical Rain Forest! J
The New Zealand Rain Forest: A Comparison with Tropical Rain Forest! J. W. DAWSON2 and B. V. SNEDDON2 ABSTRACT: The structure of and growth forms and habits exhibited by the New Zealand rain forest are described and compared with those of lowland tropical rain forest. Theories relating to the frequent regeneration failure of the forest dominants are outlined. The floristic affinities of the forest type are discussed and it is suggested that two main elements can be recognized-lowland tropical and montane tropical. It is concluded that the New Zealand rain forest is comparable to lowland tropical rain forest in structure and in range of special growth forms and habits. It chiefly differs in its lower stature, fewer species, and smaller leaves. The floristic similarity between the present forest and forest floras of the Tertiary in New Zealand suggest that the former may be a floristically reduced derivative of the latter. PART 1 OF THIS PAPER describes the structure The approximate number of species of seed and growth forms of the New Zealand rain plants in these forests is 240. From north to forest as exemplified by a forest in the far north. south there is an overall decrease in number of In Part 2, theories relating to the regeneration species. At about 38°S a number of species, of the dominant trees in the New Zealand rain mostly trees and shrubs, drop out or become forest generally are reviewed briefly, and their restricted to coastal sites, but it is not until about relevance to the situation in the study forest is 42°S, in the South Island, that many of the con considered. -
Dynamics of Even-Aged Nothofagus Truncata and N. Fusca Stands in North Westland, New Zealand
12 DYNAMICS OF EVEN-AGED NOTHOFAGUS TRUNCATA AND N. FUSCA STANDS IN NORTH WESTLAND, NEW ZEALAND M. C SMALE Forest Research Institute, Private Bag, Rotorua, New Zealand H. VAN OEVEREN Agricultural University, Salverdaplein 11, P.O. Box 9101, 6700 HB, Wageningen, The Netherlands C D. GLEASON* New Zealand Forest Service, P.O. Box 138, Hokitika, New Zealand and M. O. KIMBERLEY Forest Research Institute, Private Bag, Rotorua, New Zealand (Received for publication 30 August, 1985; revision 12 January 1987) ABSTRACT Untended, fully stocked, even-aged stands of Nothofagus truncata (Col.) Ckn. (hard beech) or N. fusca (Hook, f.) Oerst. (red beech) of natural and cultural origin and ranging in age from 20 to 100 years, were sampled using temporary and permanent plots on a range of sites in North Westland, South Island, New Zealand. Changes in stand parameters with age were quantified in order to assess growth of these stands, and thus gain some insight into their silvicultural potential. Stands of each species followed a similar pattern of growth, with rapid early height and basal area increment. Mean top height reached a maximum of c. 27 m by age 100 years. Basal area reached an equilibrium of c. 41 m2/ha in N. truncata and 46 m2/ha in N. fusca as early as age 30 years. Nothofagus truncata stands had, on average, a somewhat lower mean diameter at any given age than N. fusca stands, and maintained higher stockings. Both species attained similar maximum volume of c. 460 m3/ha at age 100 years. Keywords: even-aged stands; stand dynamics; growth; Nothofagus truncata; Nothofagus fusca. -
Mt Taranaki Summit Climb Brochure
Getting there Plan and prepare It is important to plan and prepare New Plymouth your trip and be well equipped. Before Mt Taranaki you go, know the Outdoor Safety Code 0510 ¥3A 5 simple rules to help you stay safe: Kilometres Summit Climb ¥3 1. Plan your trip: Check the DOC Oakura Visitor Centre for updated track Egmont Village Nga hīkoi o Mounga Taranaki conditions. Inglewood 2. Tell someone responsible where ¥45 Egmont National Park Okato you are going and your estimated return time. oad See www.adventuresmart.org.nz. Egmont R nt ¥ National Park mo 3 3. Be aware of the weather: Check Trampers heading up the Eg weather forecasts before you go on Translator Road. Photo: T. Weston. Mt Taranaki North Egmont/ 0900 999 24 or www.metservice.com. Summit Climb Waiwhakaiho 4. Know your limits: Mountaineering experience is required Mt Taranaki or Egmont for this track in snow and ice conditions. 5. Take sufficient supplies Further information • Map and compass • Waterproof raincoat and trousers For park information, hut tickets, and Konini Lodge bookings: • Sturdy tramping/hiking boots Taranaki / Egmont National Park Visitor Centre (North Egmont) • Warm clothing, gloves and hat (Open daily) • Sunhat, sunglasses, sunscreen Egmont Road Inglewood • First aid kit Phone: (06) 756 0990 • Food and 2–3 L of water (no water available on the track) E-mail: [email protected] • Cellphone/mountain radio/personal locator beacon (hire from Taranaki / Egmont National Park Visitor Centre) • Walking poles (optional) CK Check, Clean, Dry E • Putties/gaiters (optional) H C Stop the spread of didymo and other L C E freshwater pests. -
Will You Survive the Next Eruption? Before The
AN EXHIBITION EXPLORING A HYPOTHETICAL ERUPTION OF MT. TARANAKI WILL YOU SURVIVE THE NEXT ERUPTION? Mount Taranaki or Mount Egmont is a The last major eruption of Taranaki occurred stratovolcano of alternating layers of lava around 1755, and it is estimated that the flows and ash deposits. It stands at 2,518m volcano has erupted over 160 times in the last in Egmont National Park and is the second 36,000 years. There are no indications that highest mountain in the North Island. It Mt. Taranaki is about to erupt, however, its is the dominant landmark towering over a unbroken geological history of activity tells us district of fertile, pastoral land with a bounty it will in the future. of resources ranging from oil to iron-sand to Mt. Taranaki is well monitored by the groundwater. GeoNet project, and dormant volcanoes like Mt. Taranaki is part of a volcanic chain that Taranaki almost always demonstrate unrest includes the Kaitake and Pouakai Ranges, before an eruption starts, with warning Paritutu, and the Sugar Loaf islands. periods likely to range between days to months. BEFORE THE ERUPTION Find out about the volcanic risk in your community. Ask your local council about emergency plans and how they will warn you of a volcanic eruption. ICAO AVIATION VOLCANO NEW ZEALAND VOLCANIC ALERT LEVEL SYSTEM COLOUR CODE Volcanic Alert Level Volcanic Activity Most Likely Hazards Volcano is in normal, non- Major volcanic eruption Eruption hazards on and beyond volcano* eruptive state or, a change 5 from a higher alert level: Moderate volcanic eruption Eruption hazards on and near volcano* GREEN Volcanic activity is considered 4 to have ceased, and volcano reverted to its normal, non- ERUPTION 3 Minor volcanic eruption Eruption hazards on and near vent* eruptive state. -
Ecology of Hard Beech (Nothofagus Truncata) in Southern Outlier Stands
A. F. MARK and W. G. LEE 97 Botany Department, University of Otago, P.O. Box 56, Dunedin, New Zealand. Botany Division, D.S.I.R., Private Bag, Dunedin, New Zealand. ECOLOGY OF HARD BEECH (NOTHOFAGUS TRUNCATA) IN SOUTHERN OUTLIER STANDS IN THE HAAST ECOLOGICAL DISTRICT, SOUTH WESTLAND, NEW ZEALAND Summary: Vegetation and habitat descriptions are given for sites that span the very limited environmental range of southern outlier stands of hard beech (Nothofagus truncata). These are on well-drained, north to northwest aspect slopes at 44 oS in South Westland, 260km south of the species' previously assumed southern limit. Size class distributions and diameter growth rates of hard beech stems indicate that it is competing effectively with podocarp and broadleaved species, including the two other beeches present. Of the three local species (mountain beech - N. solandri var. cliffortioides and silver beech - N. menziesii), only hard beech showed a significant relationship between stem diameter and age, though diameter growth rates were generally similar among the three species. The erratic distribution of the three local beech species in the Haast and adjacent Paringa Ecological Districts is discussed in relation to possible glacial refugia. The scientific and conservation values of the outlier stands are emphasised. Keywords: Nothofagus truncata; Nothofagus biogeography; hard beech forest; tree age-size relations; glacial refugia; South Westland, New Zealand. Introduction June (1977) briefly described the forest The unexpected recent discovery of hard beech communities associated with hard beech as ranging (Nothofagus truncata) at five lowland localities near 'from tall forest where Dacrydium cupressinum', the Arawata and Waiatoto Rivers in the Haast Metrosideros umbellata, Nothofagus menziesii, N. -
CDEM Group Plan for Taranaki 2018-2023
Civil Defence Emergency Management Group Plan for Taranaki 2018-2023 Te Mahere Rōpū Tauira a Taranaki Civil Defence Emergency Management 2018-2023 Taranaki Civil Defence Emergency Management Group Te Rākau Whakamarumaru Ki Taranaki July 2018 Civil Defence Emergency Group Plan for Taranaki This Civil Defence Emergency Management Group Plan for Taranaki was prepared by the Taranaki Civil Defence Emergency Management Group pursuant to the requirements of the Civil Defence Emergency Management Act 2002 and any subsequent amendments. The Civil Defence Emergency Management Plan for Taranaki was approved by the Taranaki Civil Defence Emergency Management Group on 19 June 2018, to take effect on 19 June 2018 and remain in force until 18 June 2023. DATED at ___________ this ____________ day of ____________, 2018 SIGNED by the following members of the Taranaki Civil Defence Emergency Management Group: SIGNED for and on behalf of _____________________________________ STRATFORD DISTRICT COUNCIL Signature _____________________________________ Print Name SIGNED for and on behalf of _____________________________________ SOUTH TARANAKI DISTRICT COUNCIL Signature _____________________________________ Print Name SIGNED for and on behalf of _____________________________________ NEW PLYMOUTH DISTRICT COUNCIL Signature _____________________________________ Print Name SIGNED for and on behalf of _____________________________________ TARANAKI REGIONAL COUNCIL Signature _____________________________________ Print Name Foreword I am very pleased to present the Taranaki Civil Defence Emergency Management Plan 2018- 2023, the third for the Taranaki CDEM Group. Recent regional and national events have continued to remind us that our region is vulnerable to geological, climatic, and technological disruptions. This Plan sets out how we seek to address the exposure, by enhancing our ability to prepare and to cope. The Civil Defence Emergency Management sector (CDEM) is in the process of transformation in Taranaki. -
TARANAKI AS ONE—Taranaki Tāngata Tū Tahi 144 New Final Draft # 1507200
Indigenous forest once made up much of the land cover in the region. Biodiversity on land Biodiversity on land, or terrestrial biodiversity, includes the plants, animals and ecosystems that are based on land. The arrival of humans radically changed New Zealand’s indigenous biodiversity. Introduced animals have preyed on or competed with native species, or degraded their habitat. Exotic plants also became widespread as settlement progressed. Natural ecosystems and indigenous species have also been affected by human activities such as land development and clearing of native vegetation. A number of Council programmes are helping to protect forest remnants and control pests to encourage indigenous terrestrial biodiversity in the region. We work alongside private landowners, providing practical initiatives to protect and enhance biodiversity on private land. To ensure we are protecting significant habitats in the region adequately, we also monitor the condition of prioritised ecosystems and biodiversity sites across the region. Our pest control operations focus on controlling introduced animals and plants that threaten prioritised biodiversity sites. As a result, the condition of significant biodiversity sites across the region is generally good or very good. ‘The arrival of humans Forty percent of Taranaki’s land area is currently in indigenous radically changed New forest and shrubland. Whilst the region’s native forest has Zealand’s indigenous greatly reduced since the arrival of humans, Taranaki compares well to the rest of New Zealand, which has about 24% native biodiversity.’ forest cover. It is estimated that since the arrival of humans, around 60% of Taranaki’s indigenous forest and shrubland has been cleared, particularly on the intensively farmed ring plain and coastal terraces. -
Dawson Falls and East Egmont Walks
Other tracks Dogs Dogs and other pets are not allowed in Egmont York Road Loop Track Dawson Falls National Park, even inside vehicles. 3 hr (return) This family friendly historic walk begins at the end of York and East Road, just north of Midhirst on State Highway 3. It follows the Further information path of an old railway line. This forest walk has interpretation For park information, hut tickets, Konini Lodge bookings: Egmont Walks panels about the areas history and wildlife, and passes many Taranaki/Egmont National Park Visitor Centre interesting relics. (North Egmont) Nga hīkoi o Mounga Taranaki Track categories (Open daily) Egmont Road Egmont National Park Choose the type of track that most suits the skills and abilities Inglewood of your party. Phone: (06) 756 0990 Easy access short walk: suitable for people of all E-mail: [email protected] abilities, wheelchairs and children’s buggies. Dawson Falls Visitor Centre Short walk: well formed, easy walking for up to an hour. (limited opening hours - check website) Manaia Road Walking track: well formed easy walks from a few Kaponga minutes to a day. Phone: (027) 443 0248 Tramping track: mostly unformed but have track E-mail: [email protected] directional markers, poles or cairns. Route: unformed, suitable only for people with high level backcountry skills and experience. Check, Clean, Dry CK Plan and prepare E H C Stop the spread of didymo and other L C It is important to plan and prepare your trip and be well E freshwater pests. A Y N R equipped. Before you go, know the Outdoor Safety Code – D Remember to Check, Clean, Dry all items 5 simple rules to help you stay safe: before entering, and when moving 1. -
A Selected Bibliography of Pohutukawa and Rata (1788-1999)
[Type text] Preface Stephanie Smith, an experienced librarian and Rhodes Scholar with specialist skills in the development of bibliographies, was a wonderful partner for Project Crimson in the production of this comprehensive bibliography of pohutukawa and rata. Several years ago the Project Crimson Trust recognized the need to bring together the many and diverse references to these national icons for the benefit of researchers, conservationists, students, schools and the interested public. We never imagined the project would lead to such a work of scholarship, such a labour of love. Stephanie, like others who embrace the cause rather than the job, has invested time and intellect far beyond what was ever expected, and provided us with this outstanding resource. I urge all users to read the short introduction and gain some of the flavour of Stephanie’s enthusiasm. Project Crimson would also like to acknowledge the contribution of Forest Research library staff, in particular Megan Gee, for their help and support throughout the duration of this project. Gordon Hosking Trustee, Project Crimson February 2000 INTRODUCTION: THE LIVING LIBRARY [The] world around us is a repository of information which we have only begun to delve into. Like any library, once parts are missing, it is incomplete but, unlike a library, once our books (in this instance biological species) are lost they cannot be replaced. - Catherine Wilson and David Given, Threatened Plants of New Zealand. ...right at their feet they [Wellingtonians] have one of the most wide-ranging and fascinating living textbooks of botany in the country. Well - selected pages anyway. Many of the pages were ripped out by zealous colonisers, and there are now some big gaps. -
Volcanic Activity (Including Lava Flows, Debris Flows
Clarkson, B.D. & Clarkson, B.R. (2010). Pattern and process of vegetation change (succession) in recent volcanic landscapes of New Zealand and Hawaii. In Proceedings of the international symposium “Plants and Volcanoes”, Yamanashi Institute of Environmental Sciences, Fuji-Yoshida September 9-11th, 2010. 60pp. Pattern and process of vegetation change (succession) in recent volcanic landscapes of New Zealand and Hawaii Bruce D. Clarkson ([email protected]), Centre for Biodiversity and Ecology Research, University of Waikato, Private Bag 3105, Hamilton, New Zealand Beverley R. Clarkson ([email protected]), Landcare Research, Private Bag 3127, Hamilton, New Zealand Introduction Volcanic activity (including lava flows, debris flows and tephra eruptions) is a regular feature of many landscapes of the North Island of New Zealand and the Hawaiian archipelago. Over the last 35 years, we have been using a combination of the chronosequence and direct monitoring methodologies (Clarkson 1998; Walker et al. 2010) to research the pattern and process of vegetation change (succession) in these landscapes. The following account summarizes pattern and process from our main study sites (Fig. 1): Whakaari (White Island), Rangitoto Island, Mt Tarawera, Mt Ngauruhoe, Mt Ruapehu, and Mt Taranaki in New Zealand and Mauna Loa in Hawaii. Most of this information is taken from our previous publications (see References) and the references contained therein. New information on Rangitoto Island Metrosideros excelsa patch dynamics and updated (2005) species statistics for White Island have been included. The main focus of this account is forest development following significant eruptions. White Island (Whakaari) White Island (Whakaari) is a 238 ha island volcano (highest point 321 m a.s.l.) located 50 km north of North Island mainland in the Bay of Plenty. -
Introductory Statement
Introductory Statement DIETER MUELLER-DOMBOIS THE PAPERS PUBLISHED in this issue were presented in a symposium with the theme Canopy Dieback and Dynamic Processes in Pacific Forests, which was held at the 15th Pacific Science Congress in Dunedin, New Zealand, 1-12 February 1983. Co-organizers were D. R. McQueen (Botany Department, Victoria University of Wellington, New Zealand) and D. Mueller-Dombois (Department of Botany, University ofHawaii at Manoa, Honolulu). The history goes back to 1981, when my wife and I spent a sabbatical of research and travel in Australia, the Melanesian Islands, and New Zealand. One of the objectives was to look for forests with canopy dieback similar to that found in the Hawaiian Metrosideros rain forest ecosystem (Mueller Dombois 1980). This dieback is characterized by monospecific canopy stands, in Hawaii represented by M. polymorpha, that are losing or have lost their foliage more or less simultaneously as if they were deciduous tree stands. The spatial pattern of dieback is patchy, but patch sizes vary from less than a hectare to over 10 ha and their boundaries often coincide with major soil boundaries. No obviously violent perturbations, such as fire, hurricanes, land slides, or floods are directly involved in this foliage loss and mortality phe nomenon, although violent perturbations may be indirectly involved. A number of such forests with dieback stands were seen, most notably Nothofagus pullei dieback stands on Mt. Giluwe in Papua New Guinea, Eucalyptus deglupta dieback stands in tropical humid lowland rain forests on the island of New Britain, and Nothofagus solandri var. cliffortioides and Metrosideros umbellata-Weinmannia racemosa dieback stands on New Zea land's South Island. -
The Essential Role of Tree-Fern Trunks in the Regeneration of Weinmannia Tinctoria in Rain Forest on Reunion,´ Mascarene Archipelago
Journal of Tropical Ecology (2007) 23:487–492. Copyright © 2007 Cambridge University Press doi:10.1017/S026646740700418X Printed in the United Kingdom The essential role of tree-fern trunks in the regeneration of Weinmannia tinctoria in rain forest on Reunion,´ Mascarene Archipelago Geraldine´ Derroire∗†, Laurent Schmitt∗, Jean-Noel¨ Riviere` ∗, Jean-Michel Sarrailh† and Jacques Tassin‡1 ∗ CIRAD, UMR 53, 7 chemin de l’IRAT, 97410 Saint-Pierre, Reunion,´ France † ENGREF, 14 rue Girardet, CS 14216, 54042 Nancy Cedex, France ‡ CIRAD, UPR 37, Campus International de Baillarguet, TA 10/D, 34398 Montpellier Cedex 5, France (Accepted 30 March 2007) Abstract: The regeneration processes and the spatial distribution of the shade-intolerant Weinmannia tinctoria seedlings in the south of Reunion´ were investigated, with a special focus on the role of tree-ferns in seedling establishment. Mature individuals and seedling patches of Weinmannia tinctoria, and also tree-ferns, were mapped on two 1-ha rain-forest plots. Weinmannia tinctoria has hemi-epiphytic behaviour since seedlings were generally located on plant supports (99.6%). Regeneration was better on a support than on the ground, and germination tests showed that seeds were light-stimulated. Tall tree-ferns (Cyathea spp.) were suitable supports. Cyathea glauca and C. excelsa were more suitable supports than C. borbonica. Weinmannia tinctoria establishment complies with the facilitation model of succession and is dependent on tree-ferns. Resum´ e:´ La reg´ en´ eration´ et la distribution spatiale des semis de Weinmannia tinctoria,espece` intolerante´ a` l’ombre, ont et´ e´ etudi´ ees´ dans le sud de La Reunion.´ Nous nous sommes interess´ es´ au roleˆ des fougeres` arborescentes sur l’emergence´ de plantules.