Ambuchanania Leucobryoides
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Northern Fen Communitynorthern Abstract Fen, Page 1
Northern Fen CommunityNorthern Abstract Fen, Page 1 Community Range Prevalent or likely prevalent Infrequent or likely infrequent Absent or likely absent Photo by Joshua G. Cohen Overview: Northern fen is a sedge- and rush-dominated 8,000 years. Expansion of peatlands likely occurred wetland occurring on neutral to moderately alkaline following climatic cooling, approximately 5,000 years saturated peat and/or marl influenced by groundwater ago (Heinselman 1970, Boelter and Verry 1977, Riley rich in calcium and magnesium carbonates. The 1989). community occurs north of the climatic tension zone and is found primarily where calcareous bedrock Several other natural peatland communities also underlies a thin mantle of glacial drift on flat areas or occur in Michigan and can be distinguished from shallow depressions of glacial outwash and glacial minerotrophic (nutrient-rich) northern fens, based on lakeplains and also in kettle depressions on pitted comparisons of nutrient levels, flora, canopy closure, outwash and moraines. distribution, landscape context, and groundwater influence (Kost et al. 2007). Northern fen is dominated Global and State Rank: G3G5/S3 by sedges, rushes, and grasses (Mitsch and Gosselink 2000). Additional open wetlands occurring on organic Range: Northern fen is a peatland type of glaciated soils include coastal fen, poor fen, prairie fen, bog, landscapes of the northern Great Lakes region, ranging intermittent wetland, and northern wet meadow. Bogs, from Michigan west to Minnesota and northward peat-covered wetlands raised above the surrounding into central Canada (Ontario, Manitoba, and Quebec) groundwater by an accumulation of peat, receive inputs (Gignac et al. 2000, Faber-Langendoen 2001, Amon of nutrients and water primarily from precipitation et al. -
Fossil Mosses: What Do They Tell Us About Moss Evolution?
Bry. Div. Evo. 043 (1): 072–097 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.7 Fossil mosses: What do they tell us about moss evolution? MicHAEL S. IGNATOV1,2 & ELENA V. MASLOVA3 1 Tsitsin Main Botanical Garden of the Russian Academy of Sciences, Moscow, Russia 2 Faculty of Biology, Lomonosov Moscow State University, Moscow, Russia 3 Belgorod State University, Pobedy Square, 85, Belgorod, 308015 Russia �[email protected], https://orcid.org/0000-0003-1520-042X * author for correspondence: �[email protected], https://orcid.org/0000-0001-6096-6315 Abstract The moss fossil records from the Paleozoic age to the Eocene epoch are reviewed and their putative relationships to extant moss groups discussed. The incomplete preservation and lack of key characters that could define the position of an ancient moss in modern classification remain the problem. Carboniferous records are still impossible to refer to any of the modern moss taxa. Numerous Permian protosphagnalean mosses possess traits that are absent in any extant group and they are therefore treated here as an extinct lineage, whose descendants, if any remain, cannot be recognized among contemporary taxa. Non-protosphagnalean Permian mosses were also fairly diverse, representing morphotypes comparable with Dicranidae and acrocarpous Bryidae, although unequivocal representatives of these subclasses are known only since Cretaceous and Jurassic. Even though Sphagnales is one of two oldest lineages separated from the main trunk of moss phylogenetic tree, it appears in fossil state regularly only since Late Cretaceous, ca. -
Plant Life MagillS Encyclopedia of Science
MAGILLS ENCYCLOPEDIA OF SCIENCE PLANT LIFE MAGILLS ENCYCLOPEDIA OF SCIENCE PLANT LIFE Volume 4 Sustainable Forestry–Zygomycetes Indexes Editor Bryan D. Ness, Ph.D. Pacific Union College, Department of Biology Project Editor Christina J. Moose Salem Press, Inc. Pasadena, California Hackensack, New Jersey Editor in Chief: Dawn P. Dawson Managing Editor: Christina J. Moose Photograph Editor: Philip Bader Manuscript Editor: Elizabeth Ferry Slocum Production Editor: Joyce I. Buchea Assistant Editor: Andrea E. Miller Page Design and Graphics: James Hutson Research Supervisor: Jeffry Jensen Layout: William Zimmerman Acquisitions Editor: Mark Rehn Illustrator: Kimberly L. Dawson Kurnizki Copyright © 2003, by Salem Press, Inc. All rights in this book are reserved. No part of this work may be used or reproduced in any manner what- soever or transmitted in any form or by any means, electronic or mechanical, including photocopy,recording, or any information storage and retrieval system, without written permission from the copyright owner except in the case of brief quotations embodied in critical articles and reviews. For information address the publisher, Salem Press, Inc., P.O. Box 50062, Pasadena, California 91115. Some of the updated and revised essays in this work originally appeared in Magill’s Survey of Science: Life Science (1991), Magill’s Survey of Science: Life Science, Supplement (1998), Natural Resources (1998), Encyclopedia of Genetics (1999), Encyclopedia of Environmental Issues (2000), World Geography (2001), and Earth Science (2001). ∞ The paper used in these volumes conforms to the American National Standard for Permanence of Paper for Printed Library Materials, Z39.48-1992 (R1997). Library of Congress Cataloging-in-Publication Data Magill’s encyclopedia of science : plant life / edited by Bryan D. -
CHANGES in SOUTHWESTERN TASMANIAN FIRE REGIMES SINCE the EARLY 1800S
Papers and Proceedings o/the Royal Society o/Tasmania, Volume 132, 1998 IS CHANGES IN SOUTHWESTERN TASMANIAN FIRE REGIMES SINCE THE EARLY 1800s by Jon B. Marsden-Smedley (with five tables and one text-figure) MARSDEN-SMEDLEY, ].B., 1998 (31:xii): Changes in southwestern Tasmanian fire regimes since the early 1800s. Pap.Proc. R. Soc. Tasm. 132: 15-29. ISSN 0040-4703. School of Geography and Environmental Studies, University of Tasmania, GPO Box 252-78, Hobart, Tasmania, Australia 7001. There have been major changes in the fire regime of southwestern Tasmania over the past 170 years. The fire regime has changed from an Aboriginal fire regime of frequent low-intensity fires in buttongrass moorland (mostly in spring and autumn) with only the occasional high-intensity forest fire, to the early European fire regime of frequent high-intensity fires in all vegetation types, to a regime of low to medium intensity buttongrass moorland fires and finally to the current regime of few fires. These changes in the fire regime resulted in major impacts to the region's fire-sensitive vegetation types during the early European period, while the current low fire frequency across much of southwestern Tasmania has resulted in a large proportion of the region's fire-adapted buttongrass moorland being classified as old-growth. These extensive areas of old-growth buttongrass moorland mean that the potential for another large-scale ecologically damaging wildfire is high and, to avoid this, it would be better to re-introduce a regime oflow-intensity fires into the region. Key Words: fire regimes, fire management, southwestern Tasmania, Aboriginal fire, history. -
VH Flora Complete Rev 18-19
Flora of Vinalhaven Island, Maine Macrolichens, Liverworts, Mosses and Vascular Plants Javier Peñalosa Version 1.4 Spring 2019 1. General introduction ------------------------------------------------------------------------1.1 2. The Setting: Landscape, Geology, Soils and Climate ----------------------------------2.1 3. Vegetation of Vinalhaven Vegetation: classification or description? --------------------------------------------------3.1 The trees and shrubs --------------------------------------------------------------------------3.1 The Forest --------------------------------------------------------------------------------------3.3 Upland spruce-fir forest -----------------------------------------------------------------3.3 Deciduous woodlands -------------------------------------------------------------------3.6 Pitch pine woodland ---------------------------------------------------------------------3.6 The shore ---------------------------------------------------------------------------------------3.7 Rocky headlands and beaches ----------------------------------------------------------3.7 Salt marshes -------------------------------------------------------------------------------3.8 Shrub-dominated shoreline communities --------------------------------------------3.10 Freshwater wetlands -------------------------------------------------------------------------3.11 Streams -----------------------------------------------------------------------------------3.11 Ponds -------------------------------------------------------------------------------------3.11 -
<I>Sphagnum</I> Peat Mosses
ORIGINAL ARTICLE doi:10.1111/evo.12547 Evolution of niche preference in Sphagnum peat mosses Matthew G. Johnson,1,2,3 Gustaf Granath,4,5,6 Teemu Tahvanainen, 7 Remy Pouliot,8 Hans K. Stenøien,9 Line Rochefort,8 Hakan˚ Rydin,4 and A. Jonathan Shaw1 1Department of Biology, Duke University, Durham, North Carolina 27708 2Current Address: Chicago Botanic Garden, 1000 Lake Cook Road Glencoe, Illinois 60022 3E-mail: [email protected] 4Department of Plant Ecology and Evolution, Evolutionary Biology Centre, Uppsala University, Norbyvagen¨ 18D, SE-752 36, Uppsala, Sweden 5School of Geography and Earth Sciences, McMaster University, Hamilton, Ontario, Canada 6Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, SE-750 07, Uppsala, Sweden 7Department of Biology, University of Eastern Finland, P.O. Box 111, 80101, Joensuu, Finland 8Department of Plant Sciences and Northern Research Center (CEN), Laval University Quebec, Canada 9Department of Natural History, Norwegian University of Science and Technology University Museum, Trondheim, Norway Received March 26, 2014 Accepted September 23, 2014 Peat mosses (Sphagnum)areecosystemengineers—speciesinborealpeatlandssimultaneouslycreateandinhabitnarrowhabitat preferences along two microhabitat gradients: an ionic gradient and a hydrological hummock–hollow gradient. In this article, we demonstrate the connections between microhabitat preference and phylogeny in Sphagnum.Usingadatasetof39speciesof Sphagnum,withan18-locusDNAalignmentandanecologicaldatasetencompassingthreelargepublishedstudies,wetested -
Reimagining the Visitor Experience of Tasmania's Wilderness World
Reimagining the Visitor Experience of Tasmania’s Wilderness World Heritage Area Ecotourism Investment Profile Reimagining the Visitor Experience of Tasmania’s Wilderness World Heritage Area: Ecotourism Investment Profile This report was commissioned by Tourism Industry Council Tasmania and the Cradle Coast Authority, in partnership with the Tasmanian Government through Tourism Tasmania and the Tasmanian Parks and Wildlife Service. This report is co-funded by the Australian Government under the Tourism Industry Regional Development Fund Grants Programme. This report has been prepared by EC3 Global, TRC Tourism and Tourism Industry Council Tasmania. Date prepared: June 2014 Design by Halibut Creative Collective. Disclaimer The information and recommendations provided in this report are made on the basis of information available at the time of preparation. While all care has been taken to check and validate material presented in this report, independent research should be undertaken before any action or decision is taken on the basis of material contained in this report. This report does not seek to provide any assurance of project viability and EC3 Global, TRC Tourism and Tourism Industry Council Tasmania accept no liability for decisions made or the information provided in this report. Cover photo: Huon Pine Walk Corinna The Tarkine - Rob Burnett & Tourism Tasmania Contents Background...............................................................2 Reimagining the Visitor Experience of the TWWHA .................................................................5 -
Ambuchananiaceae
AMBUCHANANIACEAE Rodney D. Seppelt1 Ambuchananiaceae Seppelt & H.A.Crum, Fl. Australia 51: 406 (2006); Seppelt & H.A.Crum, in H.A.Crum & R.D.Seppelt, Contr. Univ. Michigan Herb. 22: 29 (1999), nom. inval. Type: Ambuchanania Seppelt & H.A.Crum Autoicous. Stem cortical cells in a single layer, weakly differentiated from underlying cells, without pores or fibrils; scleroderm lacking. Stem leaves large, imbricate, bordered by 15–20 rows of narrow cells with pitted walls in mid-lamina. Branches erect, dimorphic, short and long, not forming fascicles; branch cortical cells similar to those of the stem. Branch leaves narrower than stem leaves; hyaline cells with rudimentary fibrils on abaxial lower surface; adaxial surface pores simple, solitary, in centre of cell surface on branch leaves, absent on stem leaves; abaxial surface pores simple, forming a pore-like structure at junction of 4 hyaline cells, with ringed pores on walls between 2 hyaline cells, scattered, up to 10 per cell on stem leaves. Chlorophyllose cells of leaves located on adaxial side of hyaline cells (in cross-section). Perichaetia terminal; perigonia lateral, borne immediately below perichaetia; antheridia oblong-ellipsoidal. Formerly, a monotypic family considered endemic to Tasmania, Shaw et al. (2010) added a second genus, Eosphagnum A.J.Shaw. This family differs from Sphagnaceae in the location of the chlorophyllous cells in cross- sections of the leaves, the ringed thickenings found in leaf hyaline cells, and in the elongate antheridia. Eosphagnum, unlike Ambuchanania, conforms to mainstream Sphagnum architecture at the whole plant level. At the molecular level, the two taxa form one of three distinct lineages within the Sphagnopsida (Shaw et al., 2010). -
Appendix 13 Public
BASSLINK INTEGRATED IMPACT ASSESSMENT STATEMENT POTENTIAL EFFECTS OF CHANGES TO HYDRO POWER GENERATION APPENDIX 13: GORDON RIVER PUBLIC USE ASSESSMENT Dr Lorne K. Kriwoken1 June 2001 Prepared for 1. Lecturer, Centre for Environmental Studies, University of Tasmania; GPO Box 252-78, Hobart, Tasmania 7001 Australia Appendix 13: Gordon River Public Use Assessment June 2001 Kriwoken EXECUTIVE SUMMARY The aim of this report is to ascertain the level of existing public use associated with the Gordon River and to make an assessment of how this level of public use may be potentially affected by Basslink. The greatest number of tourist and recreational users are concentrated in the Lower Gordon River corridor, downstream of the Franklin River confluence, in the Tasmanian Wilderness World Heritage Area recreation zone. The major users of this reach of the Gordon River are cruise boats, float planes, rafters, kayakers, ocean kayakers, boaters and recreational fishers. The greatest number of tourists on the Lower Gordon River are the cruise boats with approximately 10,000 tourists per year. Rafters, kayakers, ocean kayakers and boater numbers represent approximately 600 to 800 per year. The number of tourists using float planes to gain access to the Lower Gordon River is approximately 2,000 per year. The number of recreational fishers is approximately 400 per year. The corridor of the Middle Gordon River, from the tailrace to the Franklin River confluence, is a wilderness zone. This reach immediately downstream of the Gordon Power Station is not used by tourists and does not readily support recreational activities. In some rare cases the Middle Gordon River is accessed from the tailrace immediately downstream of the Gordon Power Station or from the Denison River using rafts and/or kayaks. -
Field Guide to the Moss Genera in New Jersey by Keith Bowman
Field Guide to the Moss Genera in New Jersey With Coefficient of Conservation and Indicator Status Keith Bowman, PhD 10/20/2017 Acknowledgements There are many individuals that have been essential to this project. Dr. Eric Karlin compiled the initial annotated list of New Jersey moss taxa. Second, I would like to recognize the contributions of the many northeastern bryologists that aided in the development of the initial coefficient of conservation values included in this guide including Dr. Richard Andrus, Dr. Barbara Andreas, Dr. Terry O’Brien, Dr. Scott Schuette, and Dr. Sean Robinson. I would also like to acknowledge the valuable photographic contributions from Kathleen S. Walz, Dr. Robert Klips, and Dr. Michael Lüth. Funding for this project was provided by the United States Environmental Protection Agency, Region 2, State Wetlands Protection Development Grant, Section 104(B)(3); CFDA No. 66.461, CD97225809. Recommended Citation: Bowman, Keith. 2017. Field Guide to the Moss Genera in New Jersey With Coefficient of Conservation and Indicator Status. New Jersey Department of Environmental Protection, New Jersey Forest Service, Office of Natural Lands Management, Trenton, NJ, 08625. Submitted to United States Environmental Protection Agency, Region 2, State Wetlands Protection Development Grant, Section 104(B)(3); CFDA No. 66.461, CD97225809. i Table of Contents Introduction .................................................................................................................................................. 1 Descriptions -
Notes on the History of Mining and Exploration at Adamsfield
Mineral Resources Tasmania TASMANIA DEVELOPMENT REPORT 1992/20 AND RESOURCES Notes on the history of mining and exploration at Adamsfield by C .A. Bacon Abstract electrodes, electrical breaker points, crucibles, spark plugs and so on. The alloy was also used to make standard Alluvial osmiridium was discovered in the Adams River weights and measures. Iridium oxide was used as a colour valley in 1925, prompting something of a ‘rush’ to the area. (grey-black) in pottery4, 5. In 1929 osmiridium was found in situ in ultramafic rocks in the headwaters of Main Creek. Remnants of the early OTHER TASMANIAN FIELDS hard-rock and alluvial mining activity can be found in the area, although some of the early areas have been reworked Whilst Adamsfield is remembered as Tasmania’s premier by later prospectors. The large open cut was created in the osmiridium field it was not the only, or even the first, place early 1960s. Since that time the area has been explored in which the metal was found and mined. A thriving intermittently; the last recorded production from the field osmiridium industry existed long before the 1925 was 12 ounces in 1968. discovery at Adamsfield. The first recorded occurrence of osmiridium in Tasmania INTRODUCTION was made by the Surveyor-General Sprent on one of his The naturally-occurring alloy known commonly as expeditions through the Western districts in 1876. Sprent ‘osmiridium’ is composed of the metals Osmium (Os) and records the occurrence of ‘palladium’ in the valley of the Iridium (Ir). The scientific name for this alloy is Wilson River on his exploratory chart. -
A Review of Geology and Exploration in the Macquarie Harbour–Elliott Bay Area, South West Tasmania
Mineral Resources Tasmania Tasmanian Geological Survey Tasmania DEPARTMENT of INFRASTRUCTURE, Record 2003/04 ENERGY and RESOURCES Western Tasmanian Regional Minerals Program Mount Read Volcanics Compilation A review of geology and exploration in the Macquarie Harbour–Elliott Bay area, South West Tasmania K. D. Corbett Contents Summary ………………………………………………………………………………… 2 Introduction ……………………………………………………………………………… 3 Scope of study ………………………………………………………………………… 3 Conditions related to working in South West Tasmania …………………………………… 3 Acknowledgements …………………………………………………………………… 4 Major elements of the geology …………………………………………………………… 5 Introduction …………………………………………………………………………… 5 Mesoproterozoic Rocky Cape Group on Cape Sorell ……………………………………… 5 Neoproterozoic rift-related sequences of central Cape Sorell peninsula area ………………… 5 Early Cambrian allochthonous sequences ………………………………………………… 6 Middle Cambrian post-collisional sequences ……………………………………………… 7 Sequences present and their correlation …………………………………………………… 7 Eastern Quartz-Phyric Sequence correlate (Lewis River Volcanics) …………………………… 8 Western Volcano-Sedimentary Sequence (‘Wart Hill Pyroclastics’) …………………………… 8 Andesite-bearing volcano-sedimentary sequences—Noddy Creek Volcanics ………………… 8 Late Cambrian to Ordovician Owen Group and Gordon Group rocks ……………………… 10 Permo-Carboniferous and Jurassic rocks ………………………………………………… 12 Tertiary sedimentary rocks ……………………………………………………………… 12 Outline of proposed tectonic–depositional history ………………………………………… 13 Notes on aeromagnetic features from the WTRMP