Beech (Nothofagus) Silviculture in the South Island
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NEWSLETTER NUMBER 84 JUNE 2006 New Zealand Botanical Society
NEW ZEALAND BOTANICAL SOCIETY NEWSLETTER NUMBER 84 JUNE 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 September 2006 issue is 25 August 2006 Please post contributions to: Joy Talbot 17 Ford Road Christchurch 8002 Send email contributions to [email protected] or [email protected]. Files are preferably in MS Word (Word XP or earlier) or saved as RTF or ASCII. -
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. -
Dieback in New Zealand Nothofagus Forests!
Pacific Science (1983), vol. 37, no. 4 © 1984 by the University of Hawaii Press. All rights reserved Dieback in New Zealand Nothofagus Forests! J. A. WARDLE 2 and R. B. ALLEN 2 ABSTRACT: Dieback has been observed in New Zealand Nothofagus forests for some time, and a number of causal factors have been recognized. Some understanding of the effects of dieback on forest structure has been gained in a study of events after snowfalls had caused partial damage to an area of mountain beech forest. The results of this study are used to interpret the structure of beech forests elsewhere in New Zealand. Nothofagus FORESTS in New Zealand are branch ofthe Rakaia River in inland Canter generally associated with mountain environ bury. These forests, which clothe the upper ments and are consequently subjected to valley between 650 m altitude and the sub frequent disturbance, often ofclimatic origin. alpine timberline at about 1350 m, cover an The effects of these are usually local and area of 5000-6000 ha. The forest is simple contained, but sometimes a relatively minor monotypic Nothofagus solandri var. cliffort event may predispose the forest to damage by ioides (Hook. f.) Poole (mountain beech) and other, often biotic, agents causing extensive there are virtually no other tree species dieback of the forest canopy. As yet, there is (Figure 1). little information on the long-term effect of Two hundred and seventeen permanent 2 canopy dieback on forest structure or on the plots, each 400 m , were established through characteristics that make one stand vulner out the Harper forests during the 1970-1971 able and another not. -
Nothofagus, Key Genus of Plant Geography, in Time
Nothofagus, key genus of plant geography, in time and space, living and fossil, ecology and phylogeny C.G.G.J. van Steenis Rijksherbarium, Leyden, Holland Contents Summary 65 1. Introduction 66 New 2. Caledonian species 67 of and Caledonia 3. Altitudinal range Nothofagus in New Guinea New 67 Notes of 4. on distribution Nothofagus species in New Guinea 70 5. Dominance of Nothofagus 71 6. Symbionts of Nothofagus 72 7. Regeneration and germination of Nothofagus in New Guinea 73 8. Dispersal in Nothofagus and its implications for the genesis of its distribution 74 9. The South Pacific and subantarctic climate, present and past 76 10. The fossil record 78 of in time and 11. Phylogeny Nothofagus space 83 12. Bi-hemispheric ranges homologous with that of Fagoideae 89 13. Concluding theses 93 Acknowledgements 95 Bibliography 95 Postscript 97 Summary Data are given on the taxonomy and ecology of the genus. Some New Caledonian in descend the lowland. Details the distri- species grow or to are provided on bution within New Guinea. For dominance of Nothofagus, and Fagaceae in general, it is suggested that this. Some in New possibly symbionts may contribute to notes are made onregeneration and germination Guinea. A is devoted a discussion of which to be with the special chapter to dispersal appears extremely slow, implication that Nothofagus indubitably needs land for its spread, and has needed such for attaining its colossal range, encircling onwards of New Guinea the South Pacific (fossil pollen in Antarctica) to as far as southern South America. Map 1. An is other chapter devoted to response ofNothofagus to the present climate. -
Functional Plant Biology
Functional Plant Biology Contents Volume 34 Issue 2 2007 Review: Stable oxygen isotope composition of plant Barbour has made a substantial contribution to the fields of tissue: a review isotope theory and biochemical physiology, for which she was Margaret M. Barbour 83–94 awarded the New Zealand Society of Plant Biologists’ Outstanding Physiologist award 2006. This paper provides a concise review of the latest mechanistic understanding of stable isotope effects that control the oxygen isotope composition of plant organic material, and describes some of the applications of measurements of oxygen isotope composition of plants. Hypothesis: Air embolisms exsolving in the transpiration A hypothesis derived from Bernoulli’s Theorem that air content water – the effect of constrictions in the xylem pipes of the xylem should decrease sharply at sunrise is confirmed in a Martin J. Canny, Jed P.Sparks, Cheng X. Huang time domain reflectrometry record of the wood of Pinus over and Michael L. Roderick 95–111 125 summer days. The authors use similar reasoning to explain declining flow of water perfused through detached plant organs, and departures from Poiseuille’s Law. Contrasting responses by respiration to elevated CO2 in This study addresses the question of whether elevated CO2 intact tissue and isolated mitochondria concentrations directly inhibit mitochondrial respiration in plants, Dan Bruhn, Joseph T. Wiskich and and advances our understanding of the regulation of mitochondrial Owen K. Atkin 112–117 electron transport. The authors measured the redox poise of the ubiquinone pool in mitochondria titrated with increasing concentrations of CO2 to identify the point at which elevated CO2 – concentration inhibits respiration. -
An Early Paleogene Pollen and Spore Assemblage from the Sabrina Coast, East Antarctica
Palynology ISSN: 0191-6122 (Print) 1558-9188 (Online) Journal homepage: https://www.tandfonline.com/loi/tpal20 New species from the Sabrina Flora: an early Paleogene pollen and spore assemblage from the Sabrina Coast, East Antarctica Catherine Smith, Sophie Warny, Amelia E. Shevenell, Sean P.S. Gulick & Amy Leventer To cite this article: Catherine Smith, Sophie Warny, Amelia E. Shevenell, Sean P.S. Gulick & Amy Leventer (2019) New species from the Sabrina Flora: an early Paleogene pollen and spore assemblage from the Sabrina Coast, East Antarctica, Palynology, 43:4, 650-659, DOI: 10.1080/01916122.2018.1471422 To link to this article: https://doi.org/10.1080/01916122.2018.1471422 Published online: 12 Dec 2018. Submit your article to this journal Article views: 116 View related articles View Crossmark data Citing articles: 1 View citing articles Full Terms & Conditions of access and use can be found at https://www.tandfonline.com/action/journalInformation?journalCode=tpal20 PALYNOLOGY 2019, VOL. 43, NO. 4, 650–659 https://doi.org/10.1080/01916122.2018.1471422 New species from the Sabrina Flora: an early Paleogene pollen and spore assemblage from the Sabrina Coast, East Antarctica Catherine Smitha, Sophie Warnyb, Amelia E. Shevenella, Sean P.S. Gulickc and Amy Leventerd aCollege of Marine Science, University of South Florida, St. Petersburg, FL, USA; bDepartment of Geology and Geophysics and Museum of Natural Science, Louisiana State University, Baton Rouge, LA, USA; cInstitute of Geophysics and Department of Geological Sciences, University of Texas at Austin, Austin, TX, USA; dDepartment of Geology, Colgate University, Hamilton, NY, USA ABSTRACT KEYWORDS Palynological analyses of 13 samples from two sediment cores retrieved from the Sabrina Coast, East Paleocene; Eocene; Aurora Antarctica provide rare information regarding the paleovegetation within the Aurora Basin, which Basin; Sabrina Coast; East today is covered by the East Antarctic Ice Sheet. -
Eastern Takaka Hills and High Terraces Plant Lists
EASTERN TAKAKA HILLS & HIGH TERRACES ECOSYSTEM NATIVE PLANT RESTORATION LIST Hills, valleys and high terraces regularly scattered from Tarakohe southwards to East Takaka and extending westward to Motupipi Hill and Black Birch Hill north-west of Locality: Takaka township. Backed in the east by the steep marble and granite of slopes the Pikikiruna Range. Scattered outliers also on west side of Takaka River from Hamama to Upper Takaka. Discrete areas of low relief, rolling to moderately steep hill country up to 130m high near the coast and 200m high furthest inland at Upper Takaka. Topography: Hill slopes often capped with high terraces, especially at East Takaka. Terraces trending and gently dipping to the north-west. Hills drained by incised, low-volume, low to moderate-gradient streams. Hill country and terrace side-slopes comprising mudstones and calcareous siltstones, or quartz sandstones and conglomerates with thin coal seams. Underlying moderately to strongly leached sandy, silty and clayey loams of low to medium fertility. Soils often Soils and eroded. Usually adjoining areas of limestone. Terraces comprise soils of moderately Geology: strongly leached, low fertility sandy loams and loess overlying weathered, coarse outwash gravels especially of gabbro, marble. A thin iron pan has resulted in impeded drainage and soil gleying. High sunshine hours; frosts mild to moderate; mild annual temperatures and warm Climate: summers. Rainfall 1500mm at the coast to 2400mm inland. Droughts infrequent. Coastal Mostly confined to Motupipi Hill, but also hills between Tarakohe and Clifton up to ½ km influence: inland. Hill slopes dominated by rimu, hard beech, black beech, tītoki and northern rātā on drier ridges and slopes, with kāhikatea, pukatea, nikau and mixed broadleaved species in Original gullies. -
The Neogene Biota of the Transantarctic Mountains
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Related Publications from ANDRILL Affiliates Antarctic Drilling Program 2007 The Neogene biota of the Transantarctic Mountains A. C. Ashworth North Dakota State University, [email protected] A. R. Lewis North Dakota State University, [email protected] D. R. Marchant Boston University, [email protected] R. A. Askin [email protected] D. J. Cantrill Royal Botanic Gardens, [email protected] See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/andrillaffiliates Part of the Environmental Indicators and Impact Assessment Commons Ashworth, A. C.; Lewis, A. R.; Marchant, D. R.; Askin, R. A.; Cantrill, D. J.; Francis, J. E.; Leng, M. J.; Newton, A. E.; Raine, J. I.; Williams, M.; and Wolfe, A. P., "The Neogene biota of the Transantarctic Mountains" (2007). Related Publications from ANDRILL Affiliates. 5. https://digitalcommons.unl.edu/andrillaffiliates/5 This Article is brought to you for free and open access by the Antarctic Drilling Program at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Related Publications from ANDRILL Affiliates by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors A. C. Ashworth, A. R. Lewis, D. R. Marchant, R. A. Askin, D. J. Cantrill, J. E. Francis, M. J. Leng, A. E. Newton, J. I. Raine, M. Williams, and A. P. Wolfe This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/ andrillaffiliates/5 U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Extended Abstract.071 The Neogene biota of the Transantarctic Mountains A. -
Reconstructing Leaf Area from Fragments: Testing Three Methods Using a Fossil Paleogene Species
RESEARCH ARTICLE Reconstructing leaf area from fragments: testing three methods using a fossil paleogene species Agathe Toumoulin1,2,4 , Lutz Kunzmann1 , Karolin Moraweck1, and Lawren Sack3 Manuscript received 23 March 2020; revision accepted 9 September PREMISE: Fossil leaf traits can enable reconstruction of ancient environments and climates. 2020. Among these, leaf size has been particularly studied because it reflects several climatic 1 Senckenberg Natural History Collections Dresden, Königsbrücker forcings (e.g., precipitation and surface temperature) and, potentially, environment Landstrasse 159, Dresden 01109, Germany characteristics (e.g., nutrient availability, local topography, and openness of vegetation). 2 Aix Marseille University, CNRS, IRD, INRA, Coll France, However, imperfect preservation and fragmentation can corrupt its utilization. We provide CEREGE, Technopole Arbois, 13545 Cedex 04, Aix-en-Provence BP80, France improved methodology to estimate leaf size from fossil fragments. 3 UCLA Ecology and Evolutionary Biology, 621 Charles E. Young METHODS: We apply three methods: (1) visually reconstructing leaf area based on taxon- Drive South, Box 951606, Los Angeles, CA 90095-1606, USA specific gross morphology; (2) estimating intact leaf area from vein density based on a 4 Author for correspondence (e-mail: [email protected]) vein scaling relationship; and (3) a novel complementary method, determining intact leaf Citation: Toumoulin, A., L. Kunzmann, K. Moraweck, and L. Sack. length based on the tapering of the midvein in the fragment. We test the three methods 2020. Reconstructing leaf area from fragments: testing three methods using a fossil paleogene species. American Journal of Botany 107(12): for fossils of extinct Eotrigonobalanus furcinervis (Fagaceae) from two lignite horizons of the 1786–1797. -
SILVICULTURAL NOTES on NOTHOFAGUS MENZIESII. by T
transport is not, except in a very few cases, possible, and in most cases the nature of the timber does not lend itself to this method even if suitable rivers were available. It would seem that the small unit must continue in the saw milling industry of the Dominion and that any general aggregation into large units is of very doubtful wisdom. SILVICULTURAL NOTES ON NOTHOFAGUS MENZIESII. By T. T. C. BIRCH. Regeneration A problem, of primary importance in the silvicultural management of silver-beech {Nothofagus Menziesii) is to devise a practical method of introducing regeneration into those portions of the forest which are overmature and unproductive. A very considerable proportion of Southland silver-beech forest is composed of an upper storey of overmature seed-bearers, a lower or middle storey of Elaeocarpus Hookerianus, Suttonia australis, Pitto sporum eugenioides, Carpodetus serratus, Coprosma spp., tree ferns, and other shrubs and small trees, whilst the forest floor is character ised by a dense and often pure covering of the fern Blechnum discolor, on a deep bed of organic debris. Under such conditions silver-beech regeneration is absent, and it is evident that this has been the position for many decades. Either fertile seed is not reaching the forest floor or alternatively the condition of the soil is unfavourable for beech regeneration. In an endeavour to find an answer to the first alternative, several small samples of leaf mould containing silver-beech mast were col lected in September, 1935, from beneath typical over-mature trees in the Woodlaw forest. The litter containing mast was sown thinly on three boxes of soil, watered periodically and kept beneath partial shade. -
Quercus and Lithocarpus
"Uqog"Vjqwijvu"qp"Gxqnwvkqpct{"cpf"Rj{nqigpgvke" Perspectives in the Oaks - Quercus and Lithocarpus J. Smartt and R.J. White, School of Biological Sciences, University of Southampton, United Kingdom Introduction - the family Hcicegcg Cp"korqtvcpv"lwuvkÞecvkqp"hqt"ectt{kpi"qwv"gzrgtkogpvcn"vczqpqoke"uvwfkgu"qp" c"nctig"itqwr"uwej"cu"vjg"qcmu"ku"vjg"dgnkgh"vjcv"vjgug"ecp"jgnr"vq"tguqnxg"fkhÞewnvkgu" cpf"codkiwkvkgu"yjkej"vjg"encuukecn"vczqpqoke"crrtqcejgu"ecppqv0"Vjg"qcmu"ctg"c" widely distributed and species-rich group with a complex evolutionary history, and it is therefore helpful to view our present perceptions of the oaks particularly in the dtqcfgt"eqpvgzv"qh"vjg"hcokn{"vq"yjkej"vjg{"dgnqpi0 The Fagaceae is not a large family; there are ten recognised genera (Nixon, 3;:;+0"Fagus - the beeches, Nothofagus - the southern beeches, Castanea - the chestnuts, Castanopsis and Chrysolepis - the chinkapins and two genera of oaks, Lithocarpus and Quercus. In terms of species richness, the oak genera are by far vjg"nctiguv0"Ecowu"*3;58/3;76+."kp"jgt"oqpwogpvcn"yqtm"Les Chenes, recognises 279 species of Lithocarpus and 430 of Quercus. In addition, there are 3 very small genera containing rare and possibly relict species, namely Trigonobalanus, Co- lombobalanus and Formanodendron0""Vjg"pwodgt"qh"urgekgu"ujg"tgeqipkugf"kp"vjg" other genera is 8 in Fagus, 12 in Nothofagus, 7 in Castanea and 27 in Castanopsis0 Although the actual number of species recognised by different authorities varies, vjgug"Þiwtgu"kpfkecvg"tgncvkxg"urgekgu"tkejpguu0"Qp"vjku"dcuku."qcmu"eqpuvkvwvg"vjg" -
REVIEW Wind Damage and Response in New Zealand Forests
MARTIN,Available on-line OGDEN: at: http://www.nzes.org.nz/nzje FOREST WIND DAMAGE: A REVIEW 295 REVIEW Wind damage and response in New Zealand forests: a review Timothy. J. Martin* and John Ogden School of Geography and Environmental Science, The University of Auckland, Private Bag 92019, Auckland, New Zealand. * Author for correspondence. Current address: Wildland Consultants Ltd, PO Box 303-376, North Harbour, Auckland 0751 (E-mail: [email protected]) Published on-line: 13 November 2006 ___________________________________________________________________________________________________________________________________ Abstract: The literature on wind damage in New Zealand forests is reviewed to investigate how abiotic and biotic factors influence damage severity, damage type, and forest recovery. Winds that damage forests tend to result from extra-tropical depressions or from topographically enhanced westerly air flows. Severe wind damage can occur when wind speeds exceed c. 110 km/hr, although investigating the relationship between damage and wind speeds is difficult, as gusts, for which speed is usually unrecorded, are important. Damage is often quantified by estimates of area affected, with some authors detailing the size and species of damaged trees within a given area. Key abiotic factors that influence damage patterns are topographical position,edaphic conditions, and disturbance history. Important biotic factors are tree height, tree health, position of the tree within the stand, and species. Damage type (uprooting or breakage) is primarily controlled by canopy position and rooting depth. Forest responses to wind damage include sprouting, recruitment, release, and suppression, with the dominant mode of forest recovery being strongly influenced by the severity of damage, and the species composition of the stand.