The Anatomy of the Bark of Libocedrus in New Zealand
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The Correspondence of Julius Haast and Joseph Dalton Hooker, 1861-1886
The Correspondence of Julius Haast and Joseph Dalton Hooker, 1861-1886 Sascha Nolden, Simon Nathan & Esme Mildenhall Geoscience Society of New Zealand miscellaneous publication 133H November 2013 Published by the Geoscience Society of New Zealand Inc, 2013 Information on the Society and its publications is given at www.gsnz.org.nz © Copyright Simon Nathan & Sascha Nolden, 2013 Geoscience Society of New Zealand miscellaneous publication 133H ISBN 978-1-877480-29-4 ISSN 2230-4495 (Online) ISSN 2230-4487 (Print) We gratefully acknowledge financial assistance from the Brian Mason Scientific and Technical Trust which has provided financial support for this project. This document is available as a PDF file that can be downloaded from the Geoscience Society website at: http://www.gsnz.org.nz/information/misc-series-i-49.html Bibliographic Reference Nolden, S.; Nathan, S.; Mildenhall, E. 2013: The Correspondence of Julius Haast and Joseph Dalton Hooker, 1861-1886. Geoscience Society of New Zealand miscellaneous publication 133H. 219 pages. The Correspondence of Julius Haast and Joseph Dalton Hooker, 1861-1886 CONTENTS Introduction 3 The Sumner Cave controversy Sources of the Haast-Hooker correspondence Transcription and presentation of the letters Acknowledgements References Calendar of Letters 8 Transcriptions of the Haast-Hooker letters 12 Appendix 1: Undated letter (fragment), ca 1867 208 Appendix 2: Obituary for Sir Julius von Haast 209 Appendix 3: Biographical register of names mentioned in the correspondence 213 Figures Figure 1: Photographs -
Supporting Information
Supporting Information Mao et al. 10.1073/pnas.1114319109 SI Text BEAST Analyses. In addition to a BEAST analysis that used uniform Selection of Fossil Taxa and Their Phylogenetic Positions. The in- prior distributions for all calibrations (run 1; 144-taxon dataset, tegration of fossil calibrations is the most critical step in molecular calibrations as in Table S4), we performed eight additional dating (1, 2). We only used the fossil taxa with ovulate cones that analyses to explore factors affecting estimates of divergence could be assigned unambiguously to the extant groups (Table S4). time (Fig. S3). The exact phylogenetic position of fossils used to calibrate the First, to test the effect of calibration point P, which is close to molecular clocks was determined using the total-evidence analy- the root node and is the only functional hard maximum constraint ses (following refs. 3−5). Cordaixylon iowensis was not included in in BEAST runs using uniform priors, we carried out three runs the analyses because its assignment to the crown Acrogymno- with calibrations A through O (Table S4), and calibration P set to spermae already is supported by previous cladistic analyses (also [306.2, 351.7] (run 2), [306.2, 336.5] (run 3), and [306.2, 321.4] using the total-evidence approach) (6). Two data matrices were (run 4). The age estimates obtained in runs 2, 3, and 4 largely compiled. Matrix A comprised Ginkgo biloba, 12 living repre- overlapped with those from run 1 (Fig. S3). Second, we carried out two runs with different subsets of sentatives from each conifer family, and three fossils taxa related fi to Pinaceae and Araucariaceae (16 taxa in total; Fig. -
An Unusual Plant Community on Some Westland Piedmont Moraines, by G. Rennison and J. L. Brock, P
223 AN UNUSUAL PLANT COMMUNITY ON SOME SOUTH WESTLAND PIEDMONT MORAINES by G. Rennison* and J.L. Brockf In South Westland there is an extensive area of piedmont moraines lying between the sea and the western scarp of the Southern Alps, and bounded by the Waiho River to the north and the Cook River to the south (Fig. 1). In the main the existing vegetation is podocarp-broadleaf forest, but with small pockets of a plant community which has definite alpine affinities. From the air these show up as light-coloured areas against the dark forest, and occupy areas of infertile terrace. For an explanation of their occurrence an outline of the recent geological history is pertinent. Late Pleistocene History of the Moraines Approximately two thirds of the moraines are mapped as Okarito Formation and the rest as Moana Formation (Warren, 1967; Fig. 2). Both were formed during the advance of the Otira Glaciation, the Okarito Formation being correlated with the Kumara-2 and early Kumara-3 advance, and the Moana Formation with the later Kumara-3 advance (Suggate, 1965). The Okarito Formation may also include remnants of moraines formed by the earlier Waimea Glaciation. From radio-carbon dating, Suggate suggests that the early Kumara-3 advance commenced approximately 16,000 years before present (BP). The late Kumara-3 advance commenced approximately 1,500 years later (14,500 BP) and resulted in the Fox and Franz Josef Glaciers being extended beyond the present coastline, with an extensive lateral moraine complex being formed along the periphery of the Okarito Formation. Vegetation Development on the Moraines The following is an outline of the possible mode of vegetation development on these piedmont moraines: 1. -
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26 AvailableNew on-lineZealand at: Journal http://www.newzealandecology.org/nzje/ of Ecology, Vol. 38, No. 1, 2014 Simulating long-term vegetation dynamics using a forest landscape model: the post-Taupo succession on Mt Hauhungatahi, North Island, New Zealand Timothy Thrippleton1*, Klara Dolos1, George L. W. Perry2,3, Jürgen Groeneveld3,4 and Björn Reineking1 1Biogeographical Modelling, BayCEER, University of Bayreuth, Universitätsstr. 30, 95447 Bayreuth, Germany 2School of Biological Sciences, The University of Auckland, Private Bag 92019, Auckland 1142, New Zealand 3School of Environment, The University of Auckland, Private Bag 92019, Auckland 1142, New Zealand 4Department of Ecological Modelling, Helmholtz Centre for Environmental Research – UFZ, Permoserstr. 15, 04318 Leipzig, Germany *Corresponding author (Email: [email protected]) Published online: 1 November 2013 Abstract: Forest dynamics in New Zealand are shaped by catastrophic, landscape-level disturbances (e.g. volcanic eruptions, windstorms and fires). The long return-intervals of these disturbances, combined with the longevity of many of New Zealand’s tree species, restrict empirical investigations of forest dynamics. In combination with empirical data (e.g. palaeoecological reconstructions), simulation modelling provides a way to address these limitations and to unravel complex ecological interactions. Here we adapt the forest landscape model LandClim to simulate dynamics across the large spatio-temporal scales relevant for New Zealand’s forests. Using the western slope of Mt Hauhungatahi in the central North Island as a case study, we examine forest succession following the Taupo eruption (c. 1700 cal. years BP), and the subsequent emergence of elevational species zonation. Focusing on maximum growth rate and shade tolerance we used a pattern-oriented parameterisation approach to derive a set of life-history parameters that agree with those described in the ecological literature. -
1992 New Zealand Botanical Society President: Dr Eric Godley Secretary/Treasurer: Anthony Wright
NEW ZEALAND BOTANICAL SOCIETY NEWSLETTER NUMBER 28 JUNE 1992 New Zealand Botanical Society President: Dr Eric Godley Secretary/Treasurer: Anthony Wright Committee: Sarah Beadel, Ewen Cameron, Colin Webb, Carol West Address: New Zealand Botanical Society C/- Auckland Institute & Museum Private Bag 92018 AUCKLAND Subscriptions The 1992 ordinary and institutional subs are $14 (reduced to $10 if paid by the due date on the subscription invoice). The 1992 student sub, available to full-time students, is $7 (reduced to $5 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 28 (June 1992). 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 28 February of each year for that calendar year. Existing subscribers are sent an invoice with the December Newsletter for the next year's 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 September 1992 issue (Number 29) is 28 August 1992. Please forward contributions to: Ewen Cameron, Editor NZ Botanical Society Newsletter C/- Auckland Institute & Museum Private Bag 92018 AUCKLAND Cover illustration Mawhai (Sicyos australis) in the Cucurbitaceae. Drawn by Joanna Liddiard from a fresh vegetative specimen from Mangere, Auckland; flowering material from Cuvier Island herbarium specimen (AK 153760) and the close-up of the spine from West Island, Three Kings Islands herbarium specimen (AK 162592). -
The Evolution of Cavitation Resistance in Conifers Maximilian Larter
The evolution of cavitation resistance in conifers Maximilian Larter To cite this version: Maximilian Larter. The evolution of cavitation resistance in conifers. Bioclimatology. Univer- sit´ede Bordeaux, 2016. English. <NNT : 2016BORD0103>. <tel-01375936> HAL Id: tel-01375936 https://tel.archives-ouvertes.fr/tel-01375936 Submitted on 3 Oct 2016 HAL is a multi-disciplinary open access L'archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destin´eeau d´ep^otet `ala diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publi´esou non, lished or not. The documents may come from ´emanant des ´etablissements d'enseignement et de teaching and research institutions in France or recherche fran¸caisou ´etrangers,des laboratoires abroad, or from public or private research centers. publics ou priv´es. THESE Pour obtenir le grade de DOCTEUR DE L’UNIVERSITE DE BORDEAUX Spécialité : Ecologie évolutive, fonctionnelle et des communautés Ecole doctorale: Sciences et Environnements Evolution de la résistance à la cavitation chez les conifères The evolution of cavitation resistance in conifers Maximilian LARTER Directeur : Sylvain DELZON (DR INRA) Co-Directeur : Jean-Christophe DOMEC (Professeur, BSA) Soutenue le 22/07/2016 Devant le jury composé de : Rapporteurs : Mme Amy ZANNE, Prof., George Washington University Mr Jordi MARTINEZ VILALTA, Prof., Universitat Autonoma de Barcelona Examinateurs : Mme Lisa WINGATE, CR INRA, UMR ISPA, Bordeaux Mr Jérôme CHAVE, DR CNRS, UMR EDB, Toulouse i ii Abstract Title: The evolution of cavitation resistance in conifers Abstract Forests worldwide are at increased risk of widespread mortality due to intense drought under current and future climate change. -
West Takaka Hill Country
WEST TAKAKA HILL-COUNTRY ECOSYSTEM NATIVE PLANT RESTORATION LIST Foothills between the Waingaro and Pariwhakaoho Rivers, including the Onahau and Little Onahau River headwaters, mid-branches of Waikoropupu River; foothills between Locality: Waingaro and Anatoki Rivers and extending to the coast around Takaka River mouth, including Waitapu Hill. Low relief hill country extending from sea-level to 500m altitude with moderately steeply incised streams. On granite substrate, ridges often broad with headwater basins and some Topography: impeded drainage, otherwise well-drained, moderately steep to very steep slopes and bluffs throughout. Very infertile sandy, clayey and stony acidic loams which have been strongly leached; Soils and Geology: overlying quartz schist and granite substrates. Soils extensively eroded in places. Moderate to moderately high sunshine hours. Moderate annual temperature range, most Climate: extreme inland and ameliorated near the coast. Frosts moderate to moderately severe. Rainfall from 2000mm near the coast to 2800mm inland. Coastal influence: Directly west of Takaka River mouth up to ½ km inland, and Waitapu Hill. All once covered in tall forest except on the steepest slopes. Mixed podocarp-broadleaf- beech forest, especially rimu and hard beech with mountain tōtara, miro, yellow pine, silver Original Vegetation: pine, western toatoa, northern rātā, black beech, quintinia, kāmahi and toro. Gullies with kāhikatea, pukatea and mixed broadleaved species. Generally a good cover of native vegetation remains although original forest now confined to small pockets in gullies and on steep hillslopes. Human Modification: Extensively burnt in the past and all gentle topography logged, mainly for rimu. Now commonly succeeded by mānuka shrublands. Exotic pines widespread. -
New Zealand Plants in Australian Gardens Stuart Read (Updated 27/5/2018)
New Zealand Plants in Australian Gardens Stuart Read (updated 27/5/2018) Abstract: (11.6.2013): Raised in a large New Zealand garden full of native trees, plant lover Stuart Read was perhaps hard-wired to notice kiwi plants in Australian gardens. Over time he's pieced together a pattern of waves of fashion in their planting and popularity, reflecting scientific and horticultural expansionism, commercial and familial networks and connections across the Tasman. Stuart will examine a range of NZ plants found in old and younger Australian gardens, try to tease out some of the means by which they got here and why they remain popular. No cabbage, This constellation of asterisks Slaps and rustles Its tough tatters In the brisk breeze; Whispers of times past And ancient histories (Barbara Mitcalfe’s poem, ‘Ti Kouka’ (cabbage tree) catches well the distinctive skyline profile of this ubiquitous New Zealand export (in Simpson, 2000, 213) Introduction / overview New Zealand gardens have been introduced to and cultivated in Australian gardens from early in their ‘discovery’, trade and exchanges between the two colonies. Australian and other explorers, botanists, nurserymen, New Zealand settlers and others searched New Zealand’s coasts and bush, bringing plants into cultivation, export and commerce from early in the settlement’s colonization. New Zealand plants have had their ‘vogue’ periods, including as: A) - Economic plants (various timbers, kauri gum for shellacs and jewellery; flax for fibre, rope, cloth; greens for scurvy; poroporo for the contraceptive ‘the pill’); B) - Exotic ornamental imports into Australian gardens and beyond to English and European conservatories (and some warmer, southern) gardens and parks; C) - Depicted or carved as subjects of botanical and other artworks, commercial commodities. -
Tongariro National Park New Zealand
TONGARIRO NATIONAL PARK NEW ZEALAND In 1993 Tongariro became the first property to be inscribed on the World Heritage List as a Cultural Landscape. The mountains at the heart of the Park have cultural and religious significance for the Maori people and symbolize the spiritual links between this community and its environment. The Park has active and extinct volcanoes, a wide range of ecosystems from the once nationwide Podocarp- broadleaf rainforest to subalpine meadows and some spectacular landscapes. COUNTRY New Zealand NAME Tongariro National Park MIXED NATURAL & CULTURAL WORLD HERITAGE SERIAL SITE 1988: Inscribed on the World Heritage List under Natural Criteria vii and viii (UNESCO, 1998) 1993: Extended as a Cultural Landscape under Cultural Criterion vi. STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] IUCN MANAGEMENT CATEGORY II National Park BIOGEOGRAPHICAL PROVINCE Neozealandia (7.01.02) GEOGRAPHICAL LOCATION A mountain massif in the south centre of North Island almost midway between Auckland and Wellington. A small outlier, 3 km north of the main park, separated from it by Lake Rotoaira lies just south-southwest of the town of Turangi and Lake Taupo. The Park is bounded on the west by a main railway and on the north by a main road, lying between 38° 58' to 39° 35' S and 175° 22’ to 175° 48' E. DATES AND HISTORY OF ESTABLISHMENT 1887: 2,630ha of the central volcanic area gifted by deed to the government by Paramount Chief TeHeuheu Tukino of the Ngati Tuwharetoa people; 1894: The summits of Tongariro, Ngauruhoe and Ruapehu became the nation's first National Park; gazetted in 1907 (25,213ha); 1922: The land area increased to 58,680 ha under the Tongariro National Park Act; between 1925 and 1980 the Park area was increased several times; 1975: The outlying Pihanga Scenic Reserve added (5,129ha); 1980: The National Park Act passed, providing the Park’s legal and administrative structure (DLS, 1986); 1993: Extended as the first UNESCO Cultural Landscape. -
NORFOLK RD NURSERY LTD PLANT LIST 2020 131 Norfolk Road,Carterton 5791 Phone: 06 370 2328 Mob: 027 634 7441 Email: [email protected] Price [ GST Exclusive ]
NORFOLK RD NURSERY LTD PLANT LIST 2020 131 Norfolk Road,Carterton 5791 Phone: 06 370 2328 Mob: 027 634 7441 Email: [email protected] Price [ GST exclusive ] ** O/S meaning out of stock Botanical Name Common Name RTB .5L 1L 2.5L PB8 PB12 PB18 COMMERCIAL NATIVES - CAN BE ORDERED BY EMAIL OR OVER THE PHONE (SMALL GRADES) LOW-COST BULK QUANTITIES COMPETITIVE WHOLE SALE PRICE ECO SOURCED WAIRARAPA INDIGENOUS PLANTS SEE NON-COMMERCIAL LIST FOR LARGER GRADES Coprosma acerosa sand coprosma 3.21 7.39 O/S Coprosma areolata bush edge coprosma 7.39 Coprosma 'Autumn haze' 3.21 Coprosma crassifolia O/S Coprosma grandifolia kanono 3.21 7.39 Coprosma kirkii 3.21 7.39 Coprosma lucida shining karamu 5.65 O/S Coprsosma microcarpa O/S Coprosma pedicillata O/S Coprosma propinqua mingimingi 7.39 Coprosma Red Rocks 7.39 O/S Coprosma repens taupata 3.21 Coprosma rigida stiff karamu 7.39 Coprosma robusta karamu 2.6 Coprosma rugosa needle coprosma 3.21 7.39 O/S Coprosma tenuicaulis O/S Coprosma virescens 7,39 Cordyline australis cabbage tree; ti kouka 3.21 7.39 Corokia 'Blue Grey' 7.39 Corokia buddleioides korokio taranga 3.91 O/S Corokia cotoneaster korokio 7.39 Corokia macrocarpa hokotaka 7.39 Corokia x virgata hybrid corokia 7.39 Corokia ' Frosted Chocolate' 3.91 7.39 Corokia 'Genty's Green' 3.91 7.39 Corokia 'Grey Ghost' 7.39 Dacrycarpus dacrydioides kahikatea, white pine 3.21 7.39 Dodonaea viscosa akeake - Green 7.39 Dodonaea viscosa 'Purpurea' akeake - Red Griselinia littoralis Broadway mint 3.91 7.39 Griselinia 'Canterbury' 7.39 Griselinia littoralis -
1 Supporting Information Supplementary Methods the Main Purposes of Use of Wild Animal and Plant Species Recorded in the Red
1 Supporting information 2 3 Supplementary Methods 4 5 The main purposes of use of wild animal and plant species recorded in the Red List 6 7 We investigated the prevalence of different purposes of use from the use and trade information. 8 Because completing the Use and Trade classification scheme is not mandatory for Red List 9 assessors, we investigated the prevalence of Use and Trade coding to decide which species 10 groups to include in our analyses. We selected taxonomic groups for inclusion based on the 11 following criteria: i) >40% of all extant, data sufficient species, LC species and threatened 12 species have at least one purpose of use coded (thus selecting taxonomic groups with high 13 prevalence of use); and / or ii) the proportion of LC species with at least one purpose of use code 14 falls above or within the range of the proportion of species with Use and Trade coding across the 15 other Red List categories (thus also selecting taxonomic groups where use and trade may be 16 relatively low, but use and trade in LC species is coded to a similar level as that of species in 17 other RL categories). This limited our dataset to the following taxonomic groups which have 18 adequate recording of use and trade: birds, amphibians, reptiles, cycads, conifers and dicots from 19 the terrestrial group; and corals, bony fishes, crustaceans and cone snails from the aquatic species 20 group (Table S4). We excluded mammals, cephalopods and cartilaginous fishes as meeting 21 neither criteria i) nor ii), i.e. -
Telopea · Escholarship.Usyd.Edu.Au/Journals/Index.Php/TEL · ISSN 0312-9764 (Print) · ISSN 2200-4025 (Online)
Volume 6(4): 541-562 T elopea Publication Date: 1 July 1996 . , . _ . neRoyal dx.doi.org/io.775i/teiopeai9963023 Journal ot Plant Systematics “ 2 ™ plantnet.rbgsyd.nsw.gov.au/Telopea · escholarship.usyd.edu.au/journals/index.php/TEL · ISSN 0312-9764 (Print) · ISSN 2200-4025 (Online) Mabberley, Plant introduction and hybridisation in colonial NSW 541 Plant introduction and hybridisation in colonial New South Wales: the work of John Carne Bidwill, Sydney's first director D.J. Mabberley Abstract Mabberley, D.J. (Department of Plant Sciences, University of Oxford, Oxford 0X 1 3PN; and Rijksherbarium, University of Leiden) 1996. Plant introduction and hybridisation in colonial New South Wales: the work of John Carne Bidwill, Sydney's first director. Telopea 6(4): 541-562. A brief biography of J.C. Bidwill, the first Director of the Sydney Gardens, based in part on previously unpublished manuscript sources preserved at Royal Botanic Gardens Kew and in the Mitchell Library Sydney, is presented. Bidwill's scientific impact is assessed and there is an appendix of plants named after him; the hitherto unplaced Bidwillia is perhaps referable to Trachyandra (Asphodelaceae). Introduction 'He is, besides being an excellent botanist, a man of general science, a very skillful horticulturist' — William Macarthur on J.C. Bidwill, 17 September 1847 (Macarthur Papers 37(B) Sir William Macarthur Letterbook 4 viii 1844-7 vi 1850 f. 296, A2933-2 Mitchell Library). In celebrating Lawrie Johnson, here his interest in the history of botany, it is perhaps of some value to examine the career of one of his predecessors as Director of the Sydney Gardens — the first holder of that title, John Carne Bidwill (1815-1853) — as it highlights a number of features of nineteenth-century colonial life and attitudes.