The Ecology and Biogeography of Athrotaxis D. Don
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Blue Tier Reserve Background Report 2016File
Background Report Blue Tier Reserve www.tasland.org.au Tasmanian Land Conservancy (2016). The Blue Tier Reserve Background Report. Tasmanian Land Conservancy, Tasmania Australia. Copyright ©Tasmanian Land Conservancy The views expressed in this report are those of the Tasmanian Land Conservancy and not the Federal Government, State Government or any other entity. This work is copyright. It may be reproduced for study, research or training purposes subject to an acknowledgment of the sources and no commercial usage or sale. Requests and enquires concerning reproduction and rights should be addressed to the Tasmanian Land Conservancy. Front Image: Myrtle rainforest on Blue Tier Reserve - Andy Townsend Contact Address Tasmanian Land Conservancy PO Box 2112, Lower Sandy Bay, 827 Sandy Bay Road, Sandy Bay TAS 7005 | p: 03 6225 1399 | www.tasland.org.au Contents Acknowledgements ................................................................................................................................. 1 Acronyms and Abbreviations .......................................................................................................... 2 Introduction ............................................................................................................................................ 3 Location and Access ................................................................................................................................ 4 Bioregional Values and Reserve Status .................................................................................................. -
(Athrotaxoideae, Cupressaceae) from the Upper Cretaceous Raritan Formation, New Jersey, USA
Botany A new species of Athrotaxites (Athrotaxoideae, Cupressaceae) from the Upper Cretaceous Raritan Formation, New Jersey, USA. Journal: Botany Manuscript ID cjb-2016-0061.R1 Manuscript Type: Article Date Submitted by the Author: 19-May-2016 Complete List of Authors: Escapa, Ignacio; CONICET-MEF, Paleobotany Gandolfo, Maria;Draft Cornell University, Department of Plant Biology Crepet, William; Cornell University, Department of Plant Biology Nixon, Kevin; Cornell University, L.H. Bailey Hortorium, Plant Biology Section, School of Integrative Plant Science, Cornell University Keyword: Cupressaceae, Athrotaxites, Cretaceous, Raritan Formation, New Jersey https://mc06.manuscriptcentral.com/botany-pubs Page 1 of 39 Botany A new species of Athrotaxites (Athrotaxoideae, Cupressaceae) from the Upper Cretaceous Raritan Formation, New Jersey, USA. Ignacio H. Escapa, Maria A. Gandolfo, William L. Crepet, and Kevin C. Nixon I. H. Escapa. CONICET, Museo Paleontológico Egidio Feruglio, Avenida Fontana 140, 9100 Trelew, Chubut, Argentina. M. A Gandolfo, W. L. Crepet and K. C. Nixon. L.H. Bailey Hortorium, Plant Biology Section, School of Integrative Plant Science, Cornell University, Ithaca, New York Corresponding author: Ignacio Escapa (e-mail: [email protected]) Draft https://mc06.manuscriptcentral.com/botany-pubs Botany Page 2 of 39 Abstract. A new species of anatomically preserved Cupressaceae is described from the Upper Cretaceous Raritan Formation (New Jersey, USA). The fossils are charcolified isolated ovuliferous complexes that were studied by means of a combination of MEB images and Micro-CT, allowing the observation of morphological and anatomical characters. Each ovuliferous complex bears 3-4 anatropous winged seeds, disposed in one row on a thin medial part of the adaxial side of the ovuliferous complex. -
Museum of Economic Botany, Kew. Specimens Distributed 1901 - 1990
Museum of Economic Botany, Kew. Specimens distributed 1901 - 1990 Page 1 - https://biodiversitylibrary.org/page/57407494 15 July 1901 Dr T Johnson FLS, Science and Art Museum, Dublin Two cases containing the following:- Ackd 20.7.01 1. Wood of Chloroxylon swietenia, Godaveri (2 pieces) Paris Exibition 1900 2. Wood of Chloroxylon swietenia, Godaveri (2 pieces) Paris Exibition 1900 3. Wood of Melia indica, Anantapur, Paris Exhibition 1900 4. Wood of Anogeissus acuminata, Ganjam, Paris Exhibition 1900 5. Wood of Xylia dolabriformis, Godaveri, Paris Exhibition 1900 6. Wood of Pterocarpus Marsupium, Kistna, Paris Exhibition 1900 7. Wood of Lagerstremia parviflora, Godaveri, Paris Exhibition 1900 8. Wood of Anogeissus latifolia , Godaveri, Paris Exhibition 1900 9. Wood of Gyrocarpus jacquini, Kistna, Paris Exhibition 1900 10. Wood of Acrocarpus fraxinifolium, Nilgiris, Paris Exhibition 1900 11. Wood of Ulmus integrifolia, Nilgiris, Paris Exhibition 1900 12. Wood of Phyllanthus emblica, Assam, Paris Exhibition 1900 13. Wood of Adina cordifolia, Godaveri, Paris Exhibition 1900 14. Wood of Melia indica, Anantapur, Paris Exhibition 1900 15. Wood of Cedrela toona, Nilgiris, Paris Exhibition 1900 16. Wood of Premna bengalensis, Assam, Paris Exhibition 1900 17. Wood of Artocarpus chaplasha, Assam, Paris Exhibition 1900 18. Wood of Artocarpus integrifolia, Nilgiris, Paris Exhibition 1900 19. Wood of Ulmus wallichiana, N. India, Paris Exhibition 1900 20. Wood of Diospyros kurzii , India, Paris Exhibition 1900 21. Wood of Hardwickia binata, Kistna, Paris Exhibition 1900 22. Flowers of Heterotheca inuloides, Mexico, Paris Exhibition 1900 23. Leaves of Datura Stramonium, Paris Exhibition 1900 24. Plant of Mentha viridis, Paris Exhibition 1900 25. Plant of Monsonia ovata, S. -
Vegetation Benchmarks Rainforest and Related Scrub
Vegetation Benchmarks Rainforest and related scrub Eucryphia lucida Vegetation Condition Benchmarks version 1 Rainforest and Related Scrub RPW Athrotaxis cupressoides open woodland: Sphagnum peatland facies Community Description: Athrotaxis cupressoides (5–8 m) forms small woodland patches or appears as copses and scattered small trees. On the Central Plateau (and other dolerite areas such as Mount Field), broad poorly– drained valleys and small glacial depressions may contain scattered A. cupressoides trees and copses over Sphagnum cristatum bogs. In the treeless gaps, Sphagnum cristatum is usually overgrown by a combination of any of Richea scoparia, R. gunnii, Baloskion australe, Epacris gunnii and Gleichenia alpina. This is one of three benchmarks available for assessing the condition of RPW. This is the appropriate benchmark to use in assessing the condition of the Sphagnum facies of the listed Athrotaxis cupressoides open woodland community (Schedule 3A, Nature Conservation Act 2002). Benchmarks: Length Component Cover % Height (m) DBH (cm) #/ha (m)/0.1 ha Canopy 10% - - - Large Trees - 6 20 5 Organic Litter 10% - Logs ≥ 10 - 2 Large Logs ≥ 10 Recruitment Continuous Understorey Life Forms LF code # Spp Cover % Immature tree IT 1 1 Medium shrub/small shrub S 3 30 Medium sedge/rush/sagg/lily MSR 2 10 Ground fern GF 1 1 Mosses and Lichens ML 1 70 Total 5 8 Last reviewed – 2 November 2016 Tasmanian Vegetation Monitoring and Mapping Program Department of Primary Industries, Parks, Water and Environment http://www.dpipwe.tas.gov.au/tasveg RPW Athrotaxis cupressoides open woodland: Sphagnum facies Species lists: Canopy Tree Species Common Name Notes Athrotaxis cupressoides pencil pine Present as a sparse canopy Typical Understorey Species * Common Name LF Code Epacris gunnii coral heath S Richea scoparia scoparia S Richea gunnii bog candleheath S Astelia alpina pineapple grass MSR Baloskion australe southern cordrush MSR Gleichenia alpina dwarf coralfern GF Sphagnum cristatum sphagnum ML *This list is provided as a guide only. -
Edition 2 from Forest to Fjaeldmark the Vegetation Communities Highland Treeless Vegetation
Edition 2 From Forest to Fjaeldmark The Vegetation Communities Highland treeless vegetation Richea scoparia Edition 2 From Forest to Fjaeldmark 1 Highland treeless vegetation Community (Code) Page Alpine coniferous heathland (HCH) 4 Cushion moorland (HCM) 6 Eastern alpine heathland (HHE) 8 Eastern alpine sedgeland (HSE) 10 Eastern alpine vegetation (undifferentiated) (HUE) 12 Western alpine heathland (HHW) 13 Western alpine sedgeland/herbland (HSW) 15 General description Rainforest and related scrub, Dry eucalypt forest and woodland, Scrub, heathland and coastal complexes. Highland treeless vegetation communities occur Likewise, some non-forest communities with wide within the alpine zone where the growth of trees is environmental amplitudes, such as wetlands, may be impeded by climatic factors. The altitude above found in alpine areas. which trees cannot survive varies between approximately 700 m in the south-west to over The boundaries between alpine vegetation communities are usually well defined, but 1 400 m in the north-east highlands; its exact location depends on a number of factors. In many communities may occur in a tight mosaic. In these parts of Tasmania the boundary is not well defined. situations, mapping community boundaries at Sometimes tree lines are inverted due to exposure 1:25 000 may not be feasible. This is particularly the or frost hollows. problem in the eastern highlands; the class Eastern alpine vegetation (undifferentiated) (HUE) is used in There are seven specific highland heathland, those areas where remote sensing does not provide sedgeland and moorland mapping communities, sufficient resolution. including one undifferentiated class. Other highland treeless vegetation such as grasslands, herbfields, A minor revision in 2017 added information on the grassy sedgelands and wetlands are described in occurrence of peatland pool complexes, and other sections. -
Lssn 0811-5311 DATE - SEPTEMBER 19 87
lSSN 0811-5311 DATE - SEPTEMBER 19 87 "REGISTERD BY AUSTRALIA POST -, FTlBL IC AT ION LEADER : Peter Hind, 41 Miller stredt, Mt. Druitt 2770 SECRETARY : Moreen Woollett, 3 Curriwang Place, Como West 2226 HON. TREASURER: Margaret Olde, 138 Fmler ~oad,Illaong 2234 SPORE BANK: Jenny Thompson, 2a Albion blace, Engadine 2233 Dear Wers, I First the good ws. I ?hanks to the myme&- who pdded articles, umrmts and slides, the book uhichwe are produehg thraqh the Pblisw Secticm of S.G.A.P. (NSFi) wted is nearing c~np3etion. mjblicatio~lshkmger, Bill Payne has proof copies and is currm'tly lt-dhg firral co-m. !€his uill be *e initial. volume in ghat is expeckd to be a -1ete reference to &~~txalirrnferns and is titled "The Australian Fern Series 1". It is only a smll volm~hi&hcrpefully can be retailed at an afford& le price -b the majority of fern grcw ers. Our prl3 Emtion differs -Em maq rrgard&gr' b mks b-use it is not full of irrelevant padding, me -is has been on pm3uci.q a practical guide to tihe cultivation of particular Aus&dlian native ferns, There is me article of a technical nature based rm recent research, but al-h scientific this tm has been x ritten in simple tmm that would be appreciated by most fern grm ers, A feature of the beis the 1- nuher of striking full =lour Uus.hratims. In our next Wsletterge hope to say more &opt details of phlicatim EOODIA SP . NO. 1 - CANIF On the last page of this Newsletter there is d photo copy of another unsual and apparently attractive fern contributed by Queensland member Rod Pattison. -
Kosipe Revisited
Peat in the mountains of New Guinea G.S. Hope Department of Archaeology and Natural History, Australian National University, Canberra, Australia _______________________________________________________________________________________ SUMMARY Peatlands are common in montane areas above 1,000 m in New Guinea and become extensive above 3,000 m in the subalpine zone. In the montane mires, swamp forests and grass or sedge fens predominate on swampy valley bottoms. These mires may be 4–8 m in depth and up to 30,000 years in age. In Papua New Guinea (PNG) there is about 2,250 km2 of montane peatland, and Papua Province (the Indonesian western half of the island) probably contains much more. Above 3,000 m, peat soils form under blanket bog on slopes as well as on valley floors. Vegetation types include cushion bog, grass bog and sedge fen. Typical peat depths are 0.5‒1 m on slopes, but valley floors and hollows contain up to 10 m of peat. The estimated total extent of mountain peatland is 14,800 km2 with 5,965 km2 in PNG and about 8,800 km2 in Papua Province. The stratigraphy, age structure and vegetation histories of 45 peatland or organic limnic sites above 750 m have been investigated since 1965. These record major vegetation shifts at 28,000, 17,000‒14,000 and 9,000 years ago and a variable history of human disturbance from 14,000 years ago with extensive clearance by the mid- Holocene at some sites. While montane peatlands were important agricultural centres in the Holocene, the introduction of new dryland crops has resulted in the abandonment of some peatlands in the last few centuries. -
Alpine Sphagnum Bogs and Associated Fens
Alpine Sphagnum Bogs and Associated Fens A nationally threatened ecological community Environment Protection and Biodiversity Conservation Act 1999 Policy Statement 3.16 This brochure is designed to assist land managers, owners and occupiers to identify, assess and manage the Alpine Sphagnum Bogs and Associated Fens, an ecological community listed under Australia’s national environment law, the Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act). The brochure is a companion document to the listing advice which can be found at the Australian Government’s Species Profile and Threats Database (SPRAT). Please go to the Alpine Sphagnum Bogs and Associated Fens ecological community profile in SPRAT, then click on the ‘Details’ link: www.environment.gov.au/cgi-bin/sprat/public/publiclookupcommunities.pl • The Alpine Sphagnum Bogs and Associated Fens ecological community is found in small pockets in the high country of Tasmania, Victoria, New South Wales and the Australian Capital Territory. • The Alpine Sphagnum Bogs and Associated Fens ecological community can usually be defined by the presence or absence of sphagnum moss. • Long term conservation and restoration of this ecological community is essential in order to protect vital inland water resources. • Implementing favourable land use and management practices is encouraged at sites containing this ecological community. Disclaimer The contents of this document have been compiled using a range of source materials. This document is valid as at August 2009. The Commonwealth Government is not liable for any loss or damage that may be occasioned directly or indirectly through the use of or reliance on the contents of the document. © Commonwealth of Australia 2009 This work is copyright. -
Plant Life of Western Australia
INTRODUCTION The characteristic features of the vegetation of Australia I. General Physiography At present the animals and plants of Australia are isolated from the rest of the world, except by way of the Torres Straits to New Guinea and southeast Asia. Even here adverse climatic conditions restrict or make it impossible for migration. Over a long period this isolation has meant that even what was common to the floras of the southern Asiatic Archipelago and Australia has become restricted to small areas. This resulted in an ever increasing divergence. As a consequence, Australia is a true island continent, with its own peculiar flora and fauna. As in southern Africa, Australia is largely an extensive plateau, although at a lower elevation. As in Africa too, the plateau increases gradually in height towards the east, culminating in a high ridge from which the land then drops steeply to a narrow coastal plain crossed by short rivers. On the west coast the plateau is only 00-00 m in height but there is usually an abrupt descent to the narrow coastal region. The plateau drops towards the center, and the major rivers flow into this depression. Fed from the high eastern margin of the plateau, these rivers run through low rainfall areas to the sea. While the tropical northern region is characterized by a wet summer and dry win- ter, the actual amount of rain is determined by additional factors. On the mountainous east coast the rainfall is high, while it diminishes with surprising rapidity towards the interior. Thus in New South Wales, the yearly rainfall at the edge of the plateau and the adjacent coast often reaches over 100 cm. -
Alternative Translation Initiation Codons for the Plastid Maturase Matk: Unraveling the Pseudogene Misconception in the Orchidaceae Michelle M
Barthet et al. BMC Evolutionary Biology (2015) 15:210 DOI 10.1186/s12862-015-0491-1 RESEARCH ARTICLE Open Access Alternative translation initiation codons for the plastid maturase MatK: unraveling the pseudogene misconception in the Orchidaceae Michelle M. Barthet1,2* , Keenan Moukarzel3, Kayla N. Smith1, Jaimin Patel3 and Khidir W. Hilu3 Abstract Background: The plastid maturase MatK has been implicated as a possible model for the evolutionary “missing link” between prokaryotic and eukaryotic splicing machinery. This evolutionary implication has sparked investigations concerning the function of this unusual maturase. Intron targets of MatK activity suggest that this is an essential enzyme for plastid function. The matK gene, however, is described as a pseudogene in many photosynthetic orchid species due to presence of premature stop codons in translations, and its high rate of nucleotide and amino acid substitution. Results: Sequence analysis of the matK gene from orchids identified an out-of-frame alternative AUG initiation codon upstream from the consensus initiation codon used for translation in other angiosperms. We demonstrate translation from the alternative initiation codon generates a conserved MatK reading frame. We confirm that MatK protein is expressed and functions in sample orchids currently described as having a matK pseudogene using immunodetection and reverse-transcription methods. We demonstrate using phylogenetic analysis that this alternative initiation codon emerged de novo within the Orchidaceae, with several reversal events at the basal lineage and deep in orchid history. Conclusion: These findings suggest a novel evolutionary shift for expression of matK in the Orchidaceae and support the function of MatK as a group II intron maturase in the plastid genome of land plants including the orchids. -
Tasmania - from the Wet West to the Dry East
This collection is maintained with the assistance of the Tasmania - from the wet west to the dry east. Regional Branch of the Australian Plant Society. Influences on the development of the Tasmanian plant mix Montane moorland and cool oceanic heathland When Gondwana existed as a super Geology of Tasmania Vegetation Map of Tasmania The Tasmanian highland vegetation developed in isolation from the Australian Alps. Even during ice continent, Australia and Tasmania, Africa, ages, hundreds of kilometres of lowland vegetation separated the two high altitude environments. South America, New Zealand and Antarctica shared many plant families and some Montane plants have to cope with wide temperature fluctuations, with periods of below 0°C and Genera. exposure to winds. Cold may be prolonged if the ground freezes. Plants may be blanketed by snow or BASS STRAIT the mountains by cloud. Snowmelt or clear weather can cause intense rays of light, resulting in high For example, the protea family has members temperature. Wind or sun can dry the plant and soil. in all those land masses except Antarctica. The Southern Africa panel covers the protea family more fully. Plants require moisture and warmth. Small hard leaves offer Tasmania was the last land mass to break protection from the drying away from Antarctica. The opening of the effects of sun and wind. Low gap between these land masses allowed the ocean to circulate growth avoids wind. Branches around Antarctica, cooling the earth’s climate and so locking up grow close together to shelter vast quantities of water as ice. the parts of each plant. -
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.