New Zealand's Native Trees
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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. -
Metrosideros.Pdf
Riding the ice age El Nin˜ o? Pacific biogeography and evolution of Metrosideros subg. Metrosideros (Myrtaceae) inferred from nuclear ribosomal DNA S. D. Wright*†, C. G. Yong*, J. W. Dawson‡, D. J. Whittaker*, and R. C. Gardner* *School of Biological Sciences, University of Auckland, P.B. 92019 Auckland, New Zealand; and ‡School of Biological Sciences, Victoria University, Box 600 Wellington, New Zealand Edited by Peter H. Raven, Missouri Botanical Garden, St. Louis, MO, and approved January 10, 2000 (received for review August 17, 1999) Metrosideros subg. Metrosideros (Myrtaceae) comprises Ϸ26 The very small seeds of Metrosideros require wind speeds of species distributed widely across the Pacific basin. They occur on only 5–19 km per h to be lofted. The seeds can retain viability the ancient Gondwanan landmasses of New Zealand and New in temperatures of Ϫ30°C for at least 6 h and after seawater Caledonia, as well as on the volcanic islands of the remote immersion for more than 1 month (10). Carlquist (1) suggested Pacific, from Melanesia to tropical Polynesia and the Bonin that the more remote taxa had achieved long-distance dispersal Island. Phylogenetic analysis based on nuclear ribosomal DNA to the isolated islands of Oceania on high-altitude jet streams spacer sequences from all named species showed Metrosideros that traverse the tropical Pacific from west to east. The most umbellata of New Zealand as basal in the subgenus, with the recent speculation on the dispersal history of subg. Metrosideros remaining species falling into three monophyletic clades. One (6) points to New Zealand rather than New Caledonia as the includes the seven New Caledonian species together with three landmass of origin and suggests that Samoa is the secondary axis daughters in western Oceania that probably dispersed during of dispersal into remote Polynesia. -
International Review of Environmental History: Volume 5, Issue 1, 2019
TABLE OF CONTENTS Introduction James Beattie 1 Nature’s revenge: War on the wilderness during the opening of Brazil’s ‘Last Western Frontier’ Sandro Dutra e Silva 5 Water as the ultimate sink: Linking fresh and saltwater history Simone M. Müller and David Stradling 23 Climate change: Debate and reality Daniel R. Headrick 43 Biofuels’ unbalanced equations: Misleading statistics, networked knowledge and measured parameters Kate B. Showers 61 ‘To get a cargo of flesh, bone, and blood’: Animals in the slave trade in West Africa Christopher Blakley 85 Providing guideline principles: Botany and ecology within the State Forest Service of New Zealand during the 1920s Anton Sveding 113 ‘Zambesi seeds from Mr Moffat’: Sir George Grey as imperial botanist John O’Leary 129 INTRODUCTION JAMES BEATTIE Victoria University of Wellington; Research Associate Centre for Environmental History The Australian National University; Senior Research Associate Faculty of Humanities, University of Johannesburg This first issue of 2019 speaks to the many exciting dimensions of environmental history. Represented here is environmental history’s great breadth, in terms of geographical scope (Brazil, the Atlantic world, Europe, global, Africa and New Zealand); topics (animal studies, biography, climatological analysis, energy and waste); and temporal span (from the early modern to the contemporary period). The first article, ‘Nature’s revenge: War on the wilderness during the opening of Brazil’s “Last Western Frontier”’, explores the ongoing trope of the frontier and ‘frontiersman’ in the environmental history of twentieth-century Amazonia, Brazil. The author, Sandro Dutra e Silva, does so by skilfully analysing the creation of the heroic image of the road-building engineer Bernardo Sayão, and his deployment by the state to underpin its aims of developing Amazonia. -
Revegetation of the Stockton Coal Mine, Buller©
114 Combined Proceedings International Plant Propagators’ Society, Volume 57, 2007 Revegetation of the Stockton Coal Mine, Buller© Michael Kingsbury Solid Energy New Zealand Limited, P.O. Box 250, Westport Email: [email protected] INTRODUCTION Stockton Coal Mine is situated 25 km north-east of Westport and stretches from 1 km to 5 km from the coast. The 2,200-ha coal mining licence is located within the western sector of the Buller Coal Field on a plateau 400 to 1,100 m above the coastal plain. The opencast mine currently has a disturbed area of 750 ha and is expected to have a footprint of more than 900 ha at end of mine life. Thick seams of generally high quality coal exported for use in thermal, coking, and specialised markets overlies a basement of weathered granite rock. This ma- terial is quarried for mine road aggregate and, due to its phosphate content, is capable of supporting vegetation. Overlying the coal is a thick layer of hard, mas- sive quartz sandstone overburden, which is fragmented by blasting and stripped using 180-tonne excavators. It has poor plant-supporting characteristics, being low in fertility and having low water and nutrient-holding capacity. Remnants of the Kaiata mudstone exist on top of the sandstone and contribute to acid rock drainage through oxidation of sulphide-bearing minerals. Stockton Mine experiences a moist (some would say very moist) temperate cli- mate, which, combined with strong prevailing west/north westerly winds, means extreme weather conditions are common. Annual mean precipitation of 6,500 mm (predominantly as rain) and common, intense rainfall events (e.g., 140 mm in 6 h) produce extreme soil nutrient leaching and, along with severe winter frosts, causes high erosion rates of unprotected soil particles. -
Recent Changes in the Names of New Zealand Tree and Shrub Species
-- -- - Recent changes in the names of New Zealand tree and shrub species - Since the publication of 'Flora of New Zealand' Volume 1 (A- iii) Podocarpus dacydioides Dacrycarpus ducydioides lan 1961),covering indigenous ferns, conifers and dicots, there (iii)Podocarpus ferrugzneus Prumnopitys ferruginea have been major advances in taxonomic research and the clas- Podocarpus spicatus Prumnopitys taxijolia sification of many plant groups revised accordingly. Most of (iv1 Dacrydium cupressinum (unchanged) these changes have been summarised in the Nomina Nova (v)Dacrydium bidwillii Halocarpus bidwillii series published in the New Zealand Journal of Botany (Edgar Dacrydium bijorme Halocarpus bijormis 1971, Edgar and Connor 1978, 1983) and are included in re- Dacrydium kirkii Halocarpus kirkii cent books on New Zealand plants ie.g. Eagle 1982, Wilson (vi)Dacydium colensoi Lagarostrobos colensoi 1982). A number of these name changes affect important (vii)Dacrydium intermediurn Lepidothamnus intermedius forest plants and as several of these new names are now start- Dacrydium laxijolium Lepidotbamnus laxijolius ing to appear in the scientific literature, a list of changes af- (viii)Phyllocladus trichomanoidi~(unchanged) fecting tree and shrub taxa are given here. As a large number Phyllocladus glaucus (unchanged) of the readers of New Zealand Forestry are likely to use Poole Phyllocladus alpinus Phyllocladus aspleniijolius and Adams' "Trees and Shrubs of New Zealand" as their var. alpinus* * main reference for New Zealand forest plants, all the name changes are related to the fourth impression of this book. * It has been suggested that the Colenso name P, cunnin- it is important to realise that not all botanists necessarily ghamii (1884)should take precedence over the later (18891 ark agree with one particular name and you are not obliged to use name (P. -
Plant Charts for Native to the West Booklet
26 Pohutukawa • Oi exposed coastal ecosystem KEY ♥ Nurse plant ■ Main component ✤ rare ✖ toxic to toddlers coastal sites For restoration, in this habitat: ••• plant liberally •• plant generally • plant sparingly Recommended planting sites Back Boggy Escarp- Sharp Steep Valley Broad Gentle Alluvial Dunes Area ment Ridge Slope Bottom Ridge Slope Flat/Tce Medium trees Beilschmiedia tarairi taraire ✤ ■ •• Corynocarpus laevigatus karaka ✖■ •••• Kunzea ericoides kanuka ♥■ •• ••• ••• ••• ••• ••• ••• Metrosideros excelsa pohutukawa ♥■ ••••• • •• •• Small trees, large shrubs Coprosma lucida shining karamu ♥ ■ •• ••• ••• •• •• Coprosma macrocarpa coastal karamu ♥ ■ •• •• •• •••• Coprosma robusta karamu ♥ ■ •••••• Cordyline australis ti kouka, cabbage tree ♥ ■ • •• •• • •• •••• Dodonaea viscosa akeake ■ •••• Entelea arborescens whau ♥ ■ ••••• Geniostoma rupestre hangehange ♥■ •• • •• •• •• •• •• Leptospermum scoparium manuka ♥■ •• •• • ••• ••• ••• ••• ••• ••• Leucopogon fasciculatus mingimingi • •• ••• ••• • •• •• • Macropiper excelsum kawakawa ♥■ •••• •••• ••• Melicope ternata wharangi ■ •••••• Melicytus ramiflorus mahoe • ••• •• • •• ••• Myoporum laetum ngaio ✖ ■ •••••• Olearia furfuracea akepiro • ••• ••• •• •• Pittosporum crassifolium karo ■ •• •••• ••• Pittosporum ellipticum •• •• Pseudopanax lessonii houpara ■ ecosystem one •••••• Rhopalostylis sapida nikau ■ • •• • •• Sophora fulvida west coast kowhai ✖■ •• •• Shrubs and flax-like plants Coprosma crassifolia stiff-stemmed coprosma ♥■ •• ••••• Coprosma repens taupata ♥ ■ •• •••• •• -
Nzbotsoc No 86 Dec 2006
NEW ZEALAND BOTANICAL SOCIETY NEWSLETTER NUMBER 86 DECEMBER 2006 New Zealand Botanical Society President: Anthony Wright Secretary/Treasurer: Ewen Cameron Committee: Bruce Clarkson, Colin Webb, Carol West Address: c/- Canterbury Museum Rolleston Avenue CHRISTCHURCH 8001 Subscriptions The 2006 ordinary and institutional subscriptions are $25 (reduced to $18 if paid by the due date on the subscription invoice). The 2006 student subscription, available to full-time students, is $9 (reduced to $7 if paid by the due date on the subscription invoice). Back issues of the Newsletter are available at $2.50 each from Number 1 (August 1985) to Number 46 (December 1996), $3.00 each from Number 47 (March 1997) to Number 50 (December 1997), and $3.75 each from Number 51 (March 1998) onwards. Since 1986 the Newsletter has appeared quarterly in March, June, September and December. New subscriptions are always welcome and these, together with back issue orders, should be sent to the Secretary/Treasurer (address above). Subscriptions are due by 28th February each year for that calendar year. Existing subscribers are sent an invoice with the December Newsletter for the next years subscription which offers a reduction if this is paid by the due date. If you are in arrears with your subscription a reminder notice comes attached to each issue of the Newsletter. Deadline for next issue The deadline for the March 2007 issue is 25 February 2007 Please post contributions to: Melanie Newfield 17 Homebush Rd Khandallah Wellington Send email contributions to [email protected]. Files are preferably in MS Word (Word XP or earlier) or saved as RTF or ASCII. -
Pollination Drop in Relation to Cone Morphology in Podocarpaceae: a Novel Reproductive Mechanism Author(S): P
Pollination Drop in Relation to Cone Morphology in Podocarpaceae: A Novel Reproductive Mechanism Author(s): P. B. Tomlinson, J. E. Braggins, J. A. Rattenbury Source: American Journal of Botany, Vol. 78, No. 9 (Sep., 1991), pp. 1289-1303 Published by: Botanical Society of America Stable URL: http://www.jstor.org/stable/2444932 . Accessed: 23/08/2011 15:47 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Botanical Society of America is collaborating with JSTOR to digitize, preserve and extend access to American Journal of Botany. http://www.jstor.org AmericanJournal of Botany 78(9): 1289-1303. 1991. POLLINATION DROP IN RELATION TO CONE MORPHOLOGY IN PODOCARPACEAE: A NOVEL REPRODUCTIVE MECHANISM' P. B. TOMLINSON,2'4 J. E. BRAGGINS,3 AND J. A. RATTENBURY3 2HarvardForest, Petersham, Massachusetts 01366; and 3Departmentof Botany, University of Auckland, Auckland, New Zealand Observationof ovulatecones at thetime of pollinationin the southernconiferous family Podocarpaceaedemonstrates a distinctivemethod of pollencapture, involving an extended pollinationdrop. Ovules in all generaof the family are orthotropousand singlewithin the axil of each fertilebract. In Microstrobusand Phyllocladusovules are-erect (i.e., the micropyle directedaway from the cone axis) and are notassociated with an ovule-supportingstructure (epimatium).Pollen in thesetwo genera must land directly on thepollination drop in theway usualfor gymnosperms, as observed in Phyllocladus.In all othergenera, the ovule is inverted (i.e., the micropyleis directedtoward the cone axis) and supportedby a specializedovule- supportingstructure (epimatium). -
Beetles in a Suburban Environment: a New Zealand Case Study. The
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West Coast Crimson Trail
WEST COAST CRIMSON TRAIL The West Coast is the rata capital of New Zealand. In the North, from the Heaphy Track to Greymouth, northern rata often dominates the forest landscape, mainly near the coast and on limestone faces. Huge trees festooned with climbing and perching plants billow above the forest canopy. On higher ground southern rata is scattered on bluffs and through beech forest. Northern rata South of Hokitika in the valleys and slopes of the beech-free main divide, Northern rata (Metrosideros robusta) is one of New Zealand’s tallest flowering trees and grows from southern rata becomes a dominant canopy tree reaching high into the Alps. Hokitika northwards. It usually begins life as an epi- And, in the far South, it forms emergent giants on the flood plains, or gnarled phyte (perching plant) high in the forest’s canopy. groups around the precipitous shores of the fiords. As its roots descend to the ground, the rata smoth- ers its host. Grows to 25m or more in height with a This Crimson Trail is a journey from the north to south on the West coast of trunk up to 2.5m in diameter. Prefers warm moist New Zealand’s South Island. As you travel some 500 kilometres you will see areas such as north-west Nelson and Northland. significant glaciers, wild coastline and large tracts of primeval forest. Northern rata grows from sea level to a maximum of 900m above sea level. Southern rata Southern rata (Metrosideros umbellata) is the most widespread rata, growing throughout New Zealand as well as in the sub-antarctic Auckland Islands. -
New Zealand's Threatened Species Strategy
NEW ZEALAND’S THREATENED SPECIES STRATEGY DRAFT FOR CONSULTATION Toitū te marae a Tāne-Mahuta, Toitū te marae a Tangaroa, Toitū te tangata. If the land is well and the sea is well, the people will thrive. From the Minister ew Zealand’s unique While Predator Free 2050 is the single most significant and Nplants, birds, reptiles ambitious conservation programme in our history, it has to and other animal species be part of a broader range of work if we are to succeed. help us to define who we This draft Threatened Species Strategy is the are as a nation. Familiar Government’s plan to halt decline and restore healthy, emblems include our sustainable populations of native species. The Strategy flightless nocturnal kiwi looks at what steps are needed to restore those species and kākāpō, and the at risk of extinction, and what we should do to prevent silver fern proudly worn others from becoming threatened. by our sportspeople and etched on our war graves We are deliberately using the language of war because we and memorials. are up against invasive enemies that are hard to defeat. If we are to save the creatures we love, we have to eradicate They are our national the predators intent on eating them to extinction. taonga, living treasures found nowhere else on Earth – the unique creations of In response to beech tree seeding ‘mast’ years we have millions of years of geographical isolation. launched the successful Battle for our Birds – pest control on a landscape scale. We have declared a War on Weeds The wildlife on our islands of Aotearoa evolved in a with an annual list of the ‘Dirty Dozen’ to tackle invasive world without teeth, a paradise which for all its stunning plants that are suffocating vast areas of our bush. -
Interactive Effects of Climate Change and Species Composition on Alpine Biodiversity and Ecosystem Dynamics
Interactive effects of climate change and plant invasion on alpine biodiversity and ecosystem dynamics Justyna Giejsztowt M.Sc., 2013 University of Poitiers, France; Christian-Albrechts University, Germany B. Sc., 2010 University of Canterbury, New Zealand A thesis submitted to Victoria University of Wellington in partial fulfilment of the requirements for the degree of Doctor of Philosophy School of Biological Sciences Victoria University of Wellington Te Herenga Waka 2019 i ii This thesis was conducted under the supervision of Dr Julie R. Deslippe (primary supervisor) Victoria University of Wellington Wellington, New Zealand And Dr Aimée T. Classen (secondary supervisor) University of Vermont Burlington, United States of America iii iv “May your mountains rise into and above the clouds.” -Edward Abbey v vi Abstract Drivers of global change have direct impacts on the structure of communities and functioning of ecosystems, and interactions between drivers may buffer or exacerbate these direct effects. Interactions among drivers can lead to complex non-linear outcomes for ecosystems, communities and species, but are infrequently quantified. Through a combination of experimental, observational and modelling approaches, I address critical gaps in our understanding of the interactive effects of climate change and plant invasion, using Tongariro National Park (TNP; New Zealand) as a model. TNP is an alpine ecosystem of cultural significance which hosts a unique flora with high rates of endemism. TNP is invaded by the perennial shrub Calluna vulgaris (L.) Hull. My objectives were to: 1) determine whether species- specific phenological shifts have the potential to alter the reproductive capacity of native plants in landscapes affected by invasion; 2) determine whether the effect of invasion intensity on the Species Area Relationship (SAR) of native alpine plant species is influenced by environmental stress; 3) develop a novel modelling framework that would account for density-dependent competitive interactions between native species and C.