Arctic Hare (Lepus Arcticus Bangsii)
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Camouflage in the Arctic
24 1 Characters 2 23 22 3 4 21 Learning from Arctic Animals Adapting to Freezing Temperatures Most people are familiar with a green and brown camouflage The animals of the Arctic Circle adapt, or change, to pattern. But did you know the US Marine Corps developed a survive the cold, harsh winters. When the SNOW camouflage pattern to wear in snowy regions of the world? temperatures drop and snow falls, many animals in The pattern is called Disruptive Overwhite. It has a white the Arctic must change their summer fur to a winter background with gray digital shapes on nylon fabric. In addition, the nylon is lightweight, blocks wind, and repels the rain or snow. coat. Their food choices also change depending on The garments, such as shirts, pants, and jackets, do more than what is available in the snow-covered tundra, the assist with camouflage. In fact, they also help keep a person’s coldest of all habitats on Earth. body temperature comfortable with special features such as zippers, flaps, or drawstrings. Today, people can purchase these garments in many stores all over the world. 20 5 Changing Colors with the Seasons The fur of some Arctic animals changes from the woodland colors of the fall to pure white like winter snow. If they kept their woodland colors, these Arctic animals would stand out in the white snow and they would be unprotected. So, their fur must change to white. As a result, the animals can hide in the snow from their enemies and search safely for food. -
The Hitch-Hiker Is Intended to Provide Information Which Beginning Adult Readers Can Read and Understand
CONTENTS: Foreword Acknowledgements Chapter 1: The Southwestern Corner Chapter 2: The Great Northern Peninsula Chapter 3: Labrador Chapter 4: Deer Lake to Bishop's Falls Chapter 5: Botwood to Twillingate Chapter 6: Glenwood to Gambo Chapter 7: Glovertown to Bonavista Chapter 8: The South Coast Chapter 9: Goobies to Cape St. Mary's to Whitbourne Chapter 10: Trinity-Conception Chapter 11: St. John's and the Eastern Avalon FOREWORD This book was written to give students a closer look at Newfoundland and Labrador. Learning about our own part of the earth can help us get a better understanding of the world at large. Much of the information now available about our province is aimed at young readers and people with at least a high school education. The Hitch-Hiker is intended to provide information which beginning adult readers can read and understand. This work has a special feature we hope readers will appreciate and enjoy. Many of the places written about in this book are seen through the eyes of an adult learner and other fictional characters. These characters were created to help add a touch of reality to the printed page. We hope the characters and the things they learn and talk about also give the reader a better understanding of our province. Above all, we hope this book challenges your curiosity and encourages you to search for more information about our land. Don McDonald Director of Programs and Services Newfoundland and Labrador Literacy Development Council ACKNOWLEDGMENTS I wish to thank the many people who so kindly and eagerly helped me during the production of this book. -
2005 08 26 Department of Environment and Conservation
2005 08 26 Department of Environment and Conservation Environmental Assessment Division ENVIRONMENTAL ASSESSMENT BULLETIN Environment and Conservation Minister Tom Osborne has announced the following event relative to Part 10 Environmental Assessment of the Environmental Protection Act. UNDERTAKING RELEASED: Port aux Basques to Belle Isle (Appalachian) Hiking Trail (Reg. 1194) Proponent: International Appalachian Trail NL Chapter Inc. The Minister has released the Appalachian Hiking Trail from further environmental assessment review subject to the following conditions: • The attached overview map (titled: Amended July 2005) will be the final route for the Appalachian Trail. • The following trail routings must be implemented: • Cape John (Cape Anguille) - the existing Cormack Trail (located along the coast) must be used. • Highlands of St. John - the alternate route shown on maps 15(I & III) must be used instead of maps 15(A-C). • Cloud River - the alternate route shown on map 15(II) has a four kilometre section moved to the north. • Mare Cove - the route shown on map 16(A) is not to be used. • The Parks and Natural Areas Division and the Wildlife Division must be consulted prior to final route selection and trail construction through: The Arches Provincial Park; Sir Richard Squires Memorial Provincial Park; Main River Canadian Heritage River Waterway Park; Table Mountain International Biological Program Site; and, the Serpentine Lake / Lewis Hills Public Reserve areas. • The Wildlife Division must be consulted prior to trail construction through Newfoundland pine marten critical habitat, areas with endangered rare plants, and caribou calving grounds. • Gender equity provisions be included when tendering contracts and advertising positions, and gender equity be considered when awarding contracts and hiring workers. -
Revised Distribution of an Alaskan Endemic, the Alaska Hare (Lepus Othus), with Implications for Taxonomy, Biogeography, and Climate Change
50 ARTICLE Revised distribution of an Alaskan endemic, the Alaska Hare (Lepus othus), with implications for taxonomy, biogeography, and climate change Michelle M. Cason, Andrew P. Baltensperger, Travis L. Booms, John J. Burns, and Link E. Olson Abstract: The Alaska Hare (Lepus othus Merriam 1900) is the largest lagomorph in North America but remains one of the most poorly studied terrestrial mammals on the con- tinent. Its current distribution is restricted to western Alaska south of the Brooks Range, but historical accounts from north of the Brooks Range (the North Slope) have led to confusion over its past, present, and predicted future distributions. To determine if L. othus occurs or historically occurred on the North Slope, we surveyed museum collections, vetted observa- tional accounts, and produced a spatial distribution model based on the resulting georefer- enced records. We located a historic specimen long presumed lost that suggests the occurrence of L. othus on the North Slope as recently as the late 1800s. We also uncovered evidence of L. othus and (or) Mountain Hare (Lepus timidus Linnaeus 1758) on several islands in the Bering Sea, raising the possibility of recurring gene flow between these closely related species across seasonal ice connecting Asia and North America. While our results paint a more complete picture of the current distribution of L. othus, persistent uncertainties surrounding its taxonomic status and potential northward range shift onto lands reserved for oil and gas development call for additional study. For personal use only. Key words: Alaska Hare, Arctic Hare, Lepus othus, Mountain Hare, North Slope. Résumé : Le lièvre d’Alaska (Lepus othus Merriam 1900) est le plus grand lagomorphe en Amérique du Nord mais il demeure un des mammifères terrestres du continent qui n’a aiment pas fait l’objet d’études. -
(STAR Humber-Bay of Islands) Final Report October 2019
Strategic Regional Tourism Plan City of Corner Brook, Bay of Islands and Lower Humber Region (STAR Humber-Bay of Islands) Final Report October 2019 COMMITTEE MEMBERS Co-Chairs • Stelman Flynn, Marble Zip Tours • Craig Borden, Rugged Edge Core Committee Members • Annette George, City of Corner Brook • Glenda Simms, City of Corner Brook • Allan Kendall, Appalachian Chalets + RV’s • Robert Murphy, Legion/Ambassadors • Nora Fever, Corner Brook Port Authority • Richard Wells, Marble Mountain • Darren Martin, Marblewood Inn/Yield Communications • Rob Thomas, Saltbox Restaurant • Laura Watton, Humber Valley Resort • Darren Park, Four Season Tours • Tara Saunders, Qalipu Nation • Lexie McKenzie, Go Western Ex-Offico • Mark Tierney, ACOA • Paul Taylor, TCII Study Team: Tract Consulting • Neil Dawe • Corrina Dawe • Kevin Clarke • Mike Stolte TABLE OF CONTENTS Project Purpose and Process ................................................................................................................................................................................ 1 Environmental Scan ............................................................................................................................................................................................. 5 Our Region ........................................................................................................................................................................................................................................... 6 Our Tourism Sector ............................................................................................................................................................................................................................. -
Western Newfoundland Forest – Serpentine Range Subregion
ECOREGION Forest Barren Tundra Western Newfoundland Forest Bog Serpentine Range subregion NF 1 ne of the largest Hills area. While the entire Western Newfoundland 1 Oecoregions on the island Forest ecoregion ranges from very hilly to 2 of Newfoundland, the mountainous, the Serpentine Range subregion is at a Western Newfoundland the mountainous end of the spectrum. In fact, the Forest includes more than Lewis Hills boast the highest peak on the Island at 810 one million hectares in the metres above sea level, while the barren mountain 3 western portion of the Island. It stretches from the tops of the Tablelands and Blow Me Down Mountains Codroy Valley in the south to Bonne Bay in the north are visible when looking westward from Corner Brook. and extends from the west coast inland, including 4 much of the Long Range Mountains. The steepness with which the mountains of Its neighbouring ecoregions are the Maritime the Serpentine Range rise from the surrounding Barrens to the south, the Long Range Barrens and terrain results in talus in many areas. Other unusual 5 Central Newfoundland Forest to the east, and the geographic formations, such as solifluction terraces Northern Peninsula Forest and Long Range Barrens and stone polygons, are formed along some of these to the north. Local variation in the geology of the slopes. 6 Western Newfoundland Forest ecoregion has This subregion is also characterized by an affected its geography and biology, and has abundance of serpentine rock in its mountains and led to this ecoregion being divided into six plateaus, which in turn contributes to conditions that 7 subregions. -
World Distribution of the European Rabbit (Oryctolagus Cuniculus)
1 The Evolution, Domestication and World Distribution of the European Rabbit (Oryctolagus cuniculus) Luca Fontanesi1*, Valerio Joe Utzeri1 and Anisa Ribani1 1Department of Agricultural and Food Sciences, Division of Animal Sciences, University of Bologna, Italy 1.1 The Order Lagomorpha to assure essential vitamin uptake, the digestion of the vegetarian diet and water reintroduction The European rabbit (Oryctolagus cuniculus, (Hörnicke, 1981). Linnaeus 1758) is a mammal belonging to the The order Lagomorpha was recognized as a order Lagomorpha. distinct order within the class Mammalia in Lagomorphs are such a distinct group of 1912, separated from the order Rodentia within mammalian herbivores that the very word ‘lago- which lagomorphs were originally placed (Gidely, morph’ is a circular reference meaning ‘hare- 1912; Landry, 1999). Lagomorphs are, however, shaped’ (Chapman and Flux, 1990; Fontanesi considered to be closely related to the rodents et al., 2016). A unique anatomical feature that from which they diverged about 62–100 million characterizes lagomorphs is the presence of years ago (Mya), and together they constitute small peg-like teeth immediately behind the up- the clade Glires (Chuan-Kuei et al., 1987; Benton per-front incisors. For this feature, lagomorphs and Donoghue, 2007). Lagomorphs, rodents and are also known as Duplicidentata. Therefore, primates are placed in the major mammalian instead of four incisor teeth characteristic of clade of the Euarchontoglires (O’Leary et al., 2013). rodents (also known as Simplicidentata), lago- Modern lagomorphs might be evolved from morphs have six. The additional pair is reduced the ancestral lineage from which derived the in size. Another anatomical characteristic of the †Mimotonidae and †Eurymilydae sister taxa, animals of this order is the presence of an elong- following the Cretaceous-Paleogene (K-Pg) bound- ated rostrum of the skull, reinforced by a lattice- ary around 65 Mya (Averianov, 1994; Meng et al., work of bone, which is a fenestration to reduce 2003; Asher et al., 2005; López-Martínez, 2008). -
Appendix Lagomorph Species: Geographical Distribution and Conservation Status
Appendix Lagomorph Species: Geographical Distribution and Conservation Status PAULO C. ALVES1* AND KLAUS HACKLÄNDER2 Lagomorph taxonomy is traditionally controversy, and as a consequence the number of species varies according to different publications. Although this can be due to the conservative characteristic of some morphological and genetic traits, like general shape and number of chromosomes, the scarce knowledge on several species is probably the main reason for this controversy. Also, some species have been discovered only recently, and from others we miss any information since they have been first described (mainly in pikas). We struggled with this difficulty during the work on this book, and decide to include a list of lagomorph species (Table 1). As a reference, we used the recent list published by Hoffmann and Smith (2005) in the “Mammals of the world” (Wilson and Reeder, 2005). However, to make an updated list, we include some significant published data (Friedmann and Daly 2004) and the contribu- tions and comments of some lagomorph specialist, namely Andrew Smith, John Litvaitis, Terrence Robinson, Andrew Smith, Franz Suchentrunk, and from the Mexican lagomorph association, AMCELA. We also include sum- mary information about the geographical range of all species and the current IUCN conservation status. Inevitably, this list still contains some incorrect information. However, a permanently updated lagomorph list will be pro- vided via the World Lagomorph Society (www.worldlagomorphsociety.org). 1 CIBIO, Centro de Investigaça˜o em Biodiversidade e Recursos Genéticos and Faculdade de Ciˆencias, Universidade do Porto, Campus Agrário de Vaira˜o 4485-661 – Vaira˜o, Portugal 2 Institute of Wildlife Biology and Game Management, University of Natural Resources and Applied Life Sciences, Gregor-Mendel-Str. -
Portage Pond Subregion NF 1 H E C E N T R a L Named After Portage Pond, Which Lies at the Heart 2 T Newfoundland Forest of the Subregion
ECOREGION Forest Barren Tundra Central Newfoundland Forest Bog Portage Pond subregion NF 1 h e C e n t r a l named after Portage Pond, which lies at the heart 2 T Newfoundland Forest of the subregion. 2 ecoregion covers about Although summer temperatures are higher c 28,000 km2 of the central in this ecoregion than elsewhere on the Island, and northeastern third of they are not as high in the Portage Pond subregion 3 the island of Newfoundland. The Central as in the North-central subregion. Warm summer Newfoundland Forest has the most typically temperatures, and its location east of the Long boreal forests of all the Island's ecoregions, and Range Mountains, make this subregion — and all 4 its climate is the most continental. On of the ecoregion — one of the driest on the average, the highest summer and lowest Island. Not surprisingly, this leads to a large 5 winter temperatures on the Island occur number of forest fires. Only the North-central in this ecoregion, which also has the subregion experiences more fires. least amount of wind and fog. Bogs are common in the Portage 6 The mountain forests and P o n d s u b r e g i o n , a n d a r e bogs that make up the 1,493.2 distinguished from those of the km² Portage Pond subregion n e i g h b o u r i n g W e s t e r n 7 extend over a small south- Portage Pond Newfoundland Forest by the western portion of the subregion absence of some plants — in Central Newfoundland particular, dwarf huckleberry and 8 Forest. -
Quaternary Studies in Newfoundland: a Short Review C
Document generated on 09/29/2021 12:22 a.m. Atlantic Geology Quaternary Studies in Newfoundland: A Short Review C. M. Tucker Volume 12, Number 2, August 1976 URI: https://id.erudit.org/iderudit/ageo12_2rep02 See table of contents Publisher(s) Maritime Sediments Editorial Board ISSN 0843-5561 (print) 1718-7885 (digital) Explore this journal Cite this article Tucker, C. M. (1976). Quaternary Studies in Newfoundland: A Short Review. Atlantic Geology, 12(2), 61–13. All rights reserved © Maritime Sediments, 1976 This document is protected by copyright law. Use of the services of Érudit (including reproduction) is subject to its terms and conditions, which can be viewed online. https://apropos.erudit.org/en/users/policy-on-use/ This article is disseminated and preserved by Érudit. Érudit is a non-profit inter-university consortium of the Université de Montréal, Université Laval, and the Université du Québec à Montréal. Its mission is to promote and disseminate research. https://www.erudit.org/en/ 61 QUATERNARY STUDIES IN NEWFOUNDLAND: A SHORT REVIEW C.M. TUCKER Department of Geography, McMaster University, Hamilton, Ontario, L8S 4K1 INTRODUCTION portion of the remaining marine drift and left the island with its present contours. During the past century and a half, a consider- After the raising of the great North-East able body of knowledge has been amassed on the and South-East ranges, first coast-ice Quaternary epoch of Newfoundland. Until recently, flowed East and. West and afterwards the studies were of a reconnaissance nature, generally glaciers followed in a similar deviation, incidental to bedrock mapping projects or regional and thus perhaps the origin of the boulders, prospecting. -
A Home for Nature: Protected Areas Plan for the Island of Newfoundland
A Home for Nature Protected Areas Plan for the Island of Newfoundland Acknowledgements This Protected Areas Plan for the Island of Newfoundland is the result of over 25 years of science advice, conservation planning, reserve site selection and assessment, resource industry assessments, discussions and negotiations. Although the process was lengthy and challenging, citizens should feel confident that the result is a well-considered and balanced contribution to sustainability of our province: for our environmental, economic and social well-being. The Wilderness and Ecological Reserves Advisory Council would like to acknowledge and thank all those who had a hand in development of the Plan: the Protected Areas Association; the Natural Areas System Plan Committee (1995-1996); the Natural Areas Plan Conflict Resolution Committee (2002-2003); the Western Newfoundland Model Forest; the Natural Areas System Plan Working Group (2006-2008); the Natural Areas System Plan Deputy Minister Steering Committee; past members of the Wilderness and Ecological Reserves Advisory Council; interdepartmental ad hoc committees (2000-2019) and staff from provincial government departments representing tourism, municipalities, forestry, mining, Indigenous affairs, environment and wildlife, that worked so hard over the years to bring this Plan forward. Finally, WERAC would like to thank all the people of Newfoundland and Labrador who have been involved in the establishment of our province’s existing wilderness and ecological reserves. Citation: Wilderness and Ecological Reserves Advisory Council. A Home for Nature: Protected Areas Plan for the Island of Newfoundland. 2020. Available in alternate format upon request. The maps in this document are for illustrative purposes only. Front Cover/Back Cover Arches Provincial Park i Highlands of St. -
Lagomorphs: Pikas, Rabbits, and Hares of the World
LAGOMORPHS 1709048_int_cc2015.indd 1 15/9/2017 15:59 1709048_int_cc2015.indd 2 15/9/2017 15:59 Lagomorphs Pikas, Rabbits, and Hares of the World edited by Andrew T. Smith Charlotte H. Johnston Paulo C. Alves Klaus Hackländer JOHNS HOPKINS UNIVERSITY PRESS | baltimore 1709048_int_cc2015.indd 3 15/9/2017 15:59 © 2018 Johns Hopkins University Press All rights reserved. Published 2018 Printed in China on acid- free paper 9 8 7 6 5 4 3 2 1 Johns Hopkins University Press 2715 North Charles Street Baltimore, Maryland 21218-4363 www .press .jhu .edu Library of Congress Cataloging-in-Publication Data Names: Smith, Andrew T., 1946–, editor. Title: Lagomorphs : pikas, rabbits, and hares of the world / edited by Andrew T. Smith, Charlotte H. Johnston, Paulo C. Alves, Klaus Hackländer. Description: Baltimore : Johns Hopkins University Press, 2018. | Includes bibliographical references and index. Identifiers: LCCN 2017004268| ISBN 9781421423401 (hardcover) | ISBN 1421423405 (hardcover) | ISBN 9781421423418 (electronic) | ISBN 1421423413 (electronic) Subjects: LCSH: Lagomorpha. | BISAC: SCIENCE / Life Sciences / Biology / General. | SCIENCE / Life Sciences / Zoology / Mammals. | SCIENCE / Reference. Classification: LCC QL737.L3 L35 2018 | DDC 599.32—dc23 LC record available at https://lccn.loc.gov/2017004268 A catalog record for this book is available from the British Library. Frontispiece, top to bottom: courtesy Behzad Farahanchi, courtesy David E. Brown, and © Alessandro Calabrese. Special discounts are available for bulk purchases of this book. For more information, please contact Special Sales at 410-516-6936 or specialsales @press .jhu .edu. Johns Hopkins University Press uses environmentally friendly book materials, including recycled text paper that is composed of at least 30 percent post- consumer waste, whenever possible.