Abstract Clark, Catherine Margaret

Total Page:16

File Type:pdf, Size:1020Kb

Abstract Clark, Catherine Margaret ABSTRACT CLARK, CATHERINE MARGARET. Genetic diversity and phylogeography in a Tasmanian rainforest conifer (Lagarostrobos franklinii (Hook f.) Quinn Podocarpaceae. (Under the direction of Dr. Ronald Sederoff and Dr. Thomas Wentworth). Genetic variation in Huon pine (Lagarostrobos franklinii), a Tasmanian rainforest conifer, was estimated using several marker systems and two spatial scales. Genealogy based methods were used to infer population history of eight Huon pine stands based on chloroplast DNA variation. Chloroplast nucleotide diversity (π) was low (0.00093± 0.00006) in a multilocus haplotype generated by three universal chloroplast primers (trnS-trnT, trnD-trnT, psbC-trnS). Five haplotypes were identified; two were€ widely distributed but the most frequently occurring haplotype was found only in trees in the western portion of the range. Genetic differentiation among populations was significant and showed a high degree of structure (GST = 0.26077 p ≤ 0.00001). Pairwise comparisons between populations revealed significant structure between the southeastern and northwestern watersheds and significant isolation€ by distance€ ( p ≤ 0.0220). Nucleotide variation was also assessed in segments of three nuclear genes, 4Cl (4- € coumarate: coenzyme A ligase), ITS2 (intergenic spacer region of ribosomal DNA) and G3pdh (glyceraldehyde 3-phosphate dehydrogenase). A total of 1,154 base pairs were sequenced from 79 individuals (158 alleles) representing seven geographic locations. Estimates of nucleotide diversity (π = 0.00089 ± 0.00007) and theta (θ) (0.00061 ± 0.00031) were low for the combined loci and similar to chloroplast estimates. There was a higher level of variation at the 4Cl locus (π = 0.00167 ± 0.00014) associated with recombination. Nucleotide diversity for nuclear loci was highest in the subalpine Mt. Read population, previously described as a putative clonal stand. Population differentiation (FST = 0.0130) was lower than estimated in chloroplast DNA, or in a previous allozyme investigation (FST = 0.095). Multilocus genotypes based on RAPD markers (random amplified polymorphic DNA) were generated to further investigate genetic diversity in the Huon pine stand at Mt. Read. DNA was analyzed from 63 trees from Mt. Read and genetic diversity compared to 33 Huon pine samples from a wide geographic range. Twelve random decanucleotide primers amplified a total of 35 alleles. Only three of the alleles (8.6%) from the Mt. Read population were polymorphic in contrast to 18 (51.4%) polymorphic alleles in the reference population. Gene diversity at Mt. Read (0.0316 ± 0.1061) was six-fold lower than that found in the reference sample (0.1973 ± 0.2112). Only four unique DNA fingerprints were revealed at Mt. Read and these were spatially clustered in the stand. Each of the 33 isolates in the wide geographic sample exhibited a unique genotype. The three marker systems of this study, along with a previous allozyme survey, are concordant in indications of a low level of diversity in a Southern Hemisphere conifer. The low level of nucleotide diversity, star-like phylogeny and haplotype distribution of chloroplast DNA suggest that Huon pine has experienced a series of population bottlenecks and colonization events from refugial areas. This is congruent with paleoecological data that suggest that there were major refugial areas on the western coast of Tasmania in addition to small, isolated refugia in other portions of the current range. The low level of variation found in nuclear loci is also compatible with a history of demographic events related to Pleistocene and Holocene environmental variability and long-term range reduction. The limited genetic variation in the Mt. Read population may be related to minimal gene flow into this stand due to geographic isolation, and extensive vegetative reproduction in a harsh environment. For my mother, Jo Graham Clark Herlinger, and for Ernie Retzel and Ken Garrard ii BIOGRAPHY Catherine M. Clark was born in Pasadena, Texas and grew up and attended school in Houston, Texas. After graduating from Daeflower Free School, she left Houston on a bicycle and ended up in the Santa Cruz Mountains of California. After several cross-country moves, Catherine moved to Boone, North Carolina in 1978 to attend Appalachian State University and received a B.S. in 1984 from the Biology Naturalist program. After completing course work at Appalachian State University, she took an extended trip to Mexico. Some of the experiences of this trip led to a decision to pursue an education in the health care field. After graduating from Wake Technical College with an Associate Degree in Nursing in 1985 she worked as a Registered Nurse for ten years in gerontology, student health, chemical dependency treatment and for the American Red Cross. Catherine then decided to return to studying plant biology and returned to school at North Carolina State University. She received a Master’s degree in Botany from North Carolina State University in 1998, based on the study of chloroplast microsatellite variation in North American Abies. She then continued her graduate education in a Ph.D. program, co-majoring in Botany and Forestry at North Carolina State University. iii ACKNOWLEDGEMENTS It is a great privilege to pursue an extended educational program. The support, guidance and friendship of family, friends and professional colleagues have made it possible for me to complete this degree. I would like to first thank the members of my committee for their examples of scholarship, education and leadership: Dr. Ron Sederoff, Dr. Tom Wentworth, Dr. Henry Amerson and Dr. Bruce Weir. A number of sources of financial support and recognition have made my graduate program possible including; an EPA STAR Graduate Fellowship, Department of Forestry Fellowship, Preparing the Professoriate Fellowship, Namkoong Family Graduate Fellowship, The American Chestnut Foundation and a National Science Foundation Small Grant for Exploratory Research. Members of the Forest Biotechnology Group provided technical assistance with molecular markers. In particular, I am grateful to Dr. Henry Amerson, Saul Garcia, Dr. Arthur Johnson, Dr. David Remington, Dr. Alexander Myburg, and Dr. Ying-Hsuan Sun. Jerri Johnson, secretary for the Forest Biotechnology Group and Sue Vitello, Graduate Program secretary for the Botany Department, provided administrative assistance. Thanks to Dr. Ignazio Carbone of the NCSU Plant Pathology Department who provided assistance with data analysis. The people and agencies of Tasmania were very gracious in facilitating my field collections. Mick Brown of Forestry Tasmania provided assistance with field collections. Tasmanian Parks and Wildlife provided information on location of Huon pine populations and facilitated the issuance of sample permits. Dr. Greg Jordan of the Plant Biology iv Department, University of Tasmania assisted with information on the paleohistory of Huon pine and in finding a field assistant for sample collection. Penny Brodrib was a wonderful, resourceful and knowledgeable field assistant. Georgina Davies was my initial contact in Tasmania and provided names of several contacts that were vital to the success of the field collections. Dr. Alison Shapcott shared her knowledge of her previous population genetic survey of Huon pine. Dr. Rosanne D’Arrigo of the Tree Ring Laboratory at Lamont-Doherty Earth Observatory first approached members of the Forest Biotechnology Group about working with Huon pine. She and Dr. Ed Cook, also of the Tree Ring Laboratory, collaborated on a subsequent grant proposal involving this species and I am grateful for their assistance with the project. I am also grateful to Dr. Remy Petit and Dr. Antoine Kremer of INRA for hosting me in their lab at Pierroton, France to study DNA extraction from wood specimens. Finally, I owe very special thanks to both Ernie Retzel and Ken Garrard, two people that have had an extraordinary impact on my life. They provided exceptional support that made it possible for me to complete this program. v TABLE OF CONTENTS LIST OF TABLES...............................................................................................................ix LIST OF FIGURES .............................................................................................................xi PREFACE.............................................................................................................................1 Literature Cited.....................................................................................................................9 CHAPTER 1: CHLOROPLAST DNA PHYLOGEOGRAPHY IN A TASMANIAN ENDEMIC CONIFER (LAGAROSTROBOS FRANKLINII (HOOK F.) QUINN) PODOCARPACEAE ..........................................................................................................20 Abstract ..............................................................................................................................21 Introduction ........................................................................................................................23 Study species...........................................................................................................26 Materials and Methods........................................................................................................29 Sample collection ....................................................................................................29 DNA extraction, PCR amplification and sequencing................................................29
Recommended publications
  • West Coast Land Use Planning Strategy
    " " " " " " " " " !"#$%&'(#$%&')*&+,%,(*-%)#"%.,(**+*/%#$0($"/1%" " #".$"23"0%4567% " " " " " " " " " " " " " " " " " " " " " " " " " " " Prepared for West Coast Council" " By:" ႛ Integrated Planning Solutions; ႛ Essential Economics; and ႛ Ratio Consultants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
    [Show full text]
  • Mount Lyell Abt Railway Tasmania
    Mount Lyell Abt Railway Tasmania Nomination for Engineers Australia Engineering Heritage Recognition Volume 2 Prepared by Ian Cooper FIEAust CPEng (Retired) For Abt Railway Ministerial Corporation & Engineering Heritage Tasmania July 2015 Mount Lyell Abt Railway Engineering Heritage nomination Vol2 TABLE OF CONTENTS BIBLIOGRAPHIES CLARKE, William Branwhite (1798-1878) 3 GOULD, Charles (1834-1893) 6 BELL, Charles Napier, (1835 - 1906) 6 KELLY, Anthony Edwin (1852–1930) 7 STICHT, Robert Carl (1856–1922) 11 DRIFFIELD, Edward Carus (1865-1945) 13 PHOTO GALLERY Cover Figure – Abt locomotive train passing through restored Iron Bridge Figure A1 – Routes surveyed for the Mt Lyell Railway 14 Figure A2 – Mount Lyell Survey Team at one of their camps, early 1893 14 Figure A3 – Teamsters and friends on the early track formation 15 Figure A4 - Laying the rack rail on the climb up from Dubbil Barril 15 Figure A5 – Cutting at Rinadeena Saddle 15 Figure A6 – Abt No. 1 prior to dismantling, packaging and shipping to Tasmania 16 Figure A7 – Abt No. 1 as changed by the Mt Lyell workshop 16 Figure A8 – Schematic diagram showing Abt mechanical motion arrangement 16 Figure A9 – Twin timber trusses of ‘Quarter Mile’ Bridge spanning the King River 17 Figure A10 – ‘Quarter Mile’ trestle section 17 Figure A11 – New ‘Quarter Mile’ with steel girder section and 3 Bailey sections 17 Figure A12 – Repainting of Iron Bridge following removal of lead paint 18 Figure A13 - Iron Bridge restoration cross bracing & strengthening additions 18 Figure A14 – Iron Bridge new
    [Show full text]
  • Evolution of the Female Conifer Cone Fossils, Morphology and Phylogenetics
    DEPARTMENT OF BIOLOGICAL AND ENVIRONMENTAL SCIENCES EVOLUTION OF THE FEMALE CONIFER CONE FOSSILS, MORPHOLOGY AND PHYLOGENETICS Daniel Bäck Degree project for Bachelor of Science with a major in Biology BIO602, Biologi: Examensarbete – kandidatexamen, 15 hp First cycle Semester/year: Spring 2020 Supervisor: Åslög Dahl, Department of Biological and Environmental Sciences Examiner: Claes Persson, Department of Biological and Environmental Sciences Front page: Abies koreana (immature seed cones), Gothenburg Botanical Garden, Sweden Table of contents 1 Abstract ............................................................................................................................... 2 2 Introduction ......................................................................................................................... 3 2.1 Brief history of Florin’s research ............................................................................... 3 2.2 Progress in conifer phylogenetics .............................................................................. 4 3 Aims .................................................................................................................................... 4 4 Materials and Methods ........................................................................................................ 4 4.1 Literature: ................................................................................................................... 4 4.2 RStudio: .....................................................................................................................
    [Show full text]
  • 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).
    [Show full text]
  • Methods for Measuring Frost Tolerance of Conifers: a Systematic Map
    Review Methods for Measuring Frost Tolerance of Conifers: A Systematic Map Anastasia-Ainhoa Atucha Zamkova *, Katherine A. Steele and Andrew R. Smith School of Natural Sciences, Bangor University, Bangor LL57 2UW, Gwynedd, UK; [email protected] (K.A.S.); [email protected] (A.R.S.) * Correspondence: [email protected] Abstract: Frost tolerance is the ability of plants to withstand freezing temperatures without unrecov- erable damage. Measuring frost tolerance involves various steps, each of which will vary depending on the objectives of the study. This systematic map takes an overall view of the literature that uses frost tolerance measuring techniques in gymnosperms, focusing mainly on conifers. Many different techniques have been used for testing, and there has been little change in methodology since 2000. The gold standard remains the field observation study, which, due to its cost, is frequently substituted by other techniques. Closed enclosure freezing tests (all non-field freezing tests) are done using various types of equipment for inducing artificial freezing. An examination of the literature indicates that several factors have to be controlled in order to measure frost tolerance in a manner similar to observation in a field study. Equipment that allows controlling the freezing rate, frost exposure time and thawing rate would obtain results closer to field studies. Other important factors in study design are the number of test temperatures used, the range of temperatures selected and the decrements between the temperatures, which should be selected based on expected frost tolerance of the tissue and species. Citation: Atucha Zamkova, A.-A.; Steele, K.A.; Smith, A.R.
    [Show full text]
  • Podocarpus Has a fleshy Enlarged Stem with the Seed Capsule Attached
    Some members of the Podocarpaceae It now seems as if the general lock down is being eased across the country and I am looking to do other things than write these notes which seemed helpful eleven weeks ago but hopefully soon will not be so. Not quite a bakers dozen but one more than a S.I. preferred unit. Also I must get on with the June FACTT Newsletter which I like to think is as eagerly awaited as these notes. This note is about a family, members of which are found in fossils of Gondwana times and now in those countries which formed the original landmass and some other countries. Podocarpus has a fleshy enlarged stem with the seed capsule attached. It is easy to see the possibility of birds spreading the seeds, unlike Nothofagus where the seed is less likely to be spread widely one would think. Regarding the movement of continents it needs to be mentioned that a million is a very large number. If, as Australia is presently doing, a landmass moves 70mm a year in just 1 million years; a short period of time in geological terms; the distance traveled is 70km. Australia is moving so fast in fact that GPS can’t keep up. Some people think that taxonomists fall into two broad categories - Lumpers and Splinters. Lumpers tend to say -Well the species are so similar they are in fact one. Splitters on the other hand tend to the view that the fine details represent sufficient differences to recognise they are different species.
    [Show full text]
  • Discovery of Van Diemen's Land in 1642 with Notes on the Localities Mentioned in Tasman's Journal of the Voyage
    ( No. 80.) 1891. PARLIAMENT OF TASMANIA. DISCOVERY OF ·VAN DIEMEN'S LAND . IN 1642 :. WITH NOTES ON THE LOCALITIES MENTIONED IN TASlVIAN'S JOURNAL OF THE VOYAGE. Presented to both Houses of Parliament by His Excellency's Command .. THE D'ISCO'VERY OF VAN D'lEMEN~s LAND IN 1642; WI'£H NOTES ON THE LOC .A.LITIES :MENTION E,n IN TASMAN'S JOURNAL OF THE VOYAGE. BY JAMES BAOKHOUSE WALKER ABEL J anszoon Tasman was unquestionably one of East Indies published in 1726, gave a inore extended the greatest, if not the greatest, of the navigators between account, illustrated by copies of Tasman's maps and Magellan, who in the early years of the 16th century sketches. But the joumal itself remained practically first crossed the Pacific Ocean, and Cook, who in the unknown until a copy of it and of the original sketches latter years of the 18th practically opened Oceania and and charts was discovered in London in 1776 and pur­ Austrnlia to Europe. chased for half a guinea. This MS. aftei:wards came Little is known of Tasman's personal history, except into the possession of Sir Joseph Banks, and he employed that he was born about the year 1602, at Hoorn on the the Rev. C. G. Waide, a Dutch clergyman living in Zuyder Zee, a seaport which produced many another London," to make a translation of it. Thirty years later hardy navigator. Tasman has made familiar in our seas the substance of this translation was printed by Dr. the name of one of these fellow townsmen, the Cornelis­ Burney in his "History of Discovery in the South Sea," zoon Schouten, who in 1616 doubled the Cape, :softerwards published in J 814.
    [Show full text]
  • The Philosophers' Tale
    1 Photo: Ollie Khedun Photo: THE VISION THE CONCEPT THE PROPOSAL The Philosophers’ Tale is The West Coast Range consists The Next Iconic Walk – The of 6 mountains on a north south Philosophers’ Tale 2019 proposal more than just an iconic walk, ridge. The ridge is trisected by the – Chapter One: Owen, takes it is made up of a series of Lyell Highway (between Mt Lyell people on a journey over 28km in iconic walks to be developed and Mt Owen) and the King River 3 days and 2 nights experiencing Gorge (between Mt Huxley and Mt mountain peaks, incredible views, over a period of time. There Jukes). This makes for three distinct button grass plains, cantilever are an abundance of coastal regions, each with their own part platforms and suspension bridges walks – the Overland Track to play in telling the bigger story. over deep river gorges down into All areas have been impacted cool temperate rainforest, majestic is now mature, and people by mining exploration or other waterfalls along the tranquil King are looking for the next development in the past 100 years. River on the incredible West Coast of Tasmania. With the option to option – The Philosophers’ The area is naturally divided into finish via train, hi-rail, raft, kayak, four zones, or in story telling Tale is just that. People will helicopter or jet boat, making it a parlance, ‘Chapters’. The Chapters be drawn locally and across truly unforgettable experience. (outlined on page 8), let’s call them the globe to experience these Owen, Jukes, Lyell and Tyndall lead View West Coast video iconic walks, returning time easily to the staged construction of any proposed track works.
    [Show full text]
  • Geochemical Journal, Vol. 50 (No. 2), Pp. 197-210, 2016
    Geochemical Journal, Vol. 50, pp. 197 to 210, 2016 doi:10.2343/geochemj.2.0405 Geochemistry of Late Cambrian-Early Ordovician fluvial to shallow marine sandstones, western Tasmania, Australia: Implications for provenance, weathering, tectonic settings, and chemostratigraphy S. A. MAHMUD,1* S. NASEEM,2 M. HALL1 and KHALID A. ALMALKI3 1School of Earth, Atmosphere and Environment, Monash University, Clayton, VIC 3800, Australia 2Department of Geology, University of Karachi, Pakistan 3King Abdulaziz City for Science and Technology, Saudi Arabia (Received March 3, 2015; Accepted November 5, 2015) A geochemical study of the Late Cambrian-Early Ordovician sandstones exposed in the West Coast Range, Tasmania, Australia, was carried out to develop an understanding of the provenance and tectonic settings. The average composition of these sandstones displayed high SiO2 (92.72%), moderate Al2O3 (3.34%) and Fe2O3 (1.71%), low K2O (0.90%) and MgO (0.15%), and very low CaO and Na2O (<0.01%) concentrations. The sandstones were mainly classified as quartzarenite, and some samples were classified as sublitharenite. Tectonic discrimination diagrams based on major and trace elements suggest passive margin settings. Provenance diagram (Al2O3 vs. TiO2) revealed that the Owen Group was derived from a silica-rich source. The average chemical index of alteration (CIA) was 78.45, indicating that the source area suffered severe weathering due to persistent warm and humid climate. High amounts of rare earth elements (REE) and strong negative anomalies on the chondrite-normalized REE pattern indicate an oxidizing deposition environment. The trace element chemostratigraphy reflects sharp contrasts in concentrations, distinguishing the unconformity between the lower and upper sequences and also shows the effect of alteration assemblages.
    [Show full text]
  • TWWHA Wilderness Value Assessment 2015.Pdf
    Tasmanian Wilderness World Heritage Area Assessment of Wilderness Value Stage 2: Entire TWWHA Martin Hawes & Roger Ling September 2015 TWWHA Wilderness Value Assessment Stage 2: Entire TWWHA Summary Two computer-based methodologies, the National Wilderness Inventory (NWI) methodology and a revised version of this, were used to assess wilderness value across the Tasmanian Wilderness World Heritage Area (TWWHA) and contiguous wild areas based on input geodata that was (mostly) current in 2015. The results were used to assess the current status of wilderness across the region and the changes in wilderness value relative to the results of similar studies undertaken in 1995 and 2005. The 2015 results were broadly similar to those obtained in 2005, although substantial losses due to post-2005 roading were observed in several areas, particularly the Counsel River area. Gains in wilderness value due to the closure, downgrading or revegetation of roads and vehicle tracks were observed in the area west of Macquarie Harbour, the middle Hansons River area and the area north of Victoria Pass. Numerous apparent changes (mainly losses) in wilderness value were observed due the inclusion in the 2015 data set of features such as residences and areas of disturbed land that were overlooked in the 2005 analysis. Comparison using the NWI methodology of current wilderness value with the results obtained in 1995 revealed numerous gains and losses, some of which had already been observed in 2005. Substantial gains in wilderness value, mostly due to the closure, downgrading or revegetation of roads and vehicle tracks, were observed in the area southwest of Macquarie Harbour, Moores Valley, Alma Valley, the northern half of the Jane River Track and Little Fisher Valley.
    [Show full text]
  • Tassie's Trees Black Peppermint - Eucalyptus Gum-Top Stringy Bark - Eucalyptus Amygdalina Delegatensis
    Tassie's Trees Black peppermint - Eucalyptus Gum-top stringy bark - Eucalyptus amygdalina delegatensis Black peppermint is a tree of the more open This impressive gum tree is one of the giants of forests that can grow up to 30 metres tall. It can Tasmanian forests and can reach heights of up to be found mostly in the drier areas of Tasmania, 90 metres. This tree is the dominant forest species often in association with white gum and silver that grow in the cooler, higher altitude areas. It is wattle. This species is only found in Tasmania. one of the ash group of eucalypts which include swamp gum and stringy bark. White gum - Eucalyptus viminalis Silver wattle - Acacia dealbata White gum is a tree with many forms. It can grow Silver wattle is a distinctive tree or large shrub of to over 90 metres tall in the Evercreech forests the wattle family. It is widely distributed near Fingal in the north east, but it is usually throughout eucalypt forests and woodlands in found growing among black peppermint in drier eastern Australia. The tree can easily be identified eucalypt forests. White gum is a major species in by its blue-green feathery foliage and yellow the open woodlands of Tasmania. flowers during spring. It is more valued for horticultural uses than for its timber. Tassie's Trees Native Laurel - Anopterus King Billy pine - Athrotaxis glandulosus selaginoides More an understorey shrub rather than a canopy Although related to the famous redwoods of tree, this endemic species is wide-spread in wet California, the King Billy pine is only a medium eucalypt forests and rainforest up to 1200m above sized tree, usually between 25 and 30 metres sea level.
    [Show full text]
  • The Ecology and Conservation of Bryophytes in Tasmanian Wet Eucalypt Forest
    The ecology and conservation of bryophytes in Tasmanian wet eucalypt forest Perpetua A. M. Turner B.Sc. (Hons) Submitted in fulfilment of the requirements of the degree of Doctor of Philosophy School of Geography and Environmental Studies University of Tasmania Hobart July 2003 Declaration This thesis contains no material that has been accepted for the award of any other degree or diploma in any tertiary institution and, to the best of my knowledge and belief, the thesis contains no material previously published or written by another person, except where due reference is made in the text. Perpetua A.M. Turner (nee Blanks) 11th July 2003 Authority of Access This thesis may be made available forloan. Copying of any part of this thesis is prohibited fortwo years fromthe date this statement was signed; after that time limited copying is permitted in accordance with the Copyright Act 1968. Perpetua A.M. Turner (nee Blanks) 11 th July 2003 11 Abstract The aim of this study was to determine the factors that affect bryophyte richness and species composition in wet eucalypt forest, including old growth and forest disturbed by wildfire or silvicultural practice. Approximately one third of the total bryophyte flora for Tasmania was recorded in old growth mixed forest, with more liverwort than moss species found. Bryophyte species composition was significantly different between groups of sites of forest from the northwest, central and southern areas of the state. Mean annual temperature, altitude, rainfall of the driest month and aspect were most significant in predicting variation in bryophyte species composition. The use of vascular plants as surrogates for the conservation ofbryophyte species was examined.
    [Show full text]