Ecology of Brown Bear (Ursus Arctos)
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MINNESOTA MUSTELIDS Young
By Blane Klemek MINNESOTA MUSTELIDS Young Naturalists the Slinky,Stinky Weasel family ave you ever heard anyone call somebody a weasel? If you have, then you might think Hthat being called a weasel is bad. But weasels are good hunters, and they are cunning, curious, strong, and fierce. Weasels and their relatives are mammals. They belong to the order Carnivora (meat eaters) and the family Mustelidae, also known as the weasel family or mustelids. Mustela means weasel in Latin. With 65 species, mustelids are the largest family of carnivores in the world. Eight mustelid species currently make their homes in Minnesota: short-tailed weasel, long-tailed weasel, least weasel, mink, American marten, OTTERS BY DANIEL J. COX fisher, river otter, and American badger. Minnesota Conservation Volunteer May–June 2003 n e MARY CLAY, DEMBINSKY t PHOTO ASSOCIATES r mammals a WEASELS flexible m Here are two TOM AND PAT LEESON specialized mustelid feet. b One is for climb- ou can recognize a ing and the other for hort-tailed weasels (Mustela erminea), long- The long-tailed weasel d most mustelids g digging. Can you tell tailed weasels (M. frenata), and least weasels eats the most varied e food of all weasels. It by their tubelike r which is which? (M. nivalis) live throughout Minnesota. In also lives in the widest Ybodies and their short Stheir northern range, including Minnesota, weasels variety of habitats and legs. Some, such as badgers, hunting. Otters and minks turn white in winter. In autumn, white hairs begin climates across North are heavy and chunky. Some, are excellent swimmers that hunt to replace their brown summer coat. -
Fall 2017 Vol
International Bear News Tri-Annual Newsletter of the International Association for Bear Research and Management (IBA) and the IUCN/SSC Bear Specialist Group Fall 2017 Vol. 26 no. 3 Sun bear. (Photo: Free the Bears) Read about the first Sun Bear Symposium that took place in Malaysia on pages 34-35. IBA website: www.bearbiology.org Table of Contents INTERNATIONAL BEAR NEWS 3 International Bear News, ISSN #1064-1564 MANAGER’S CORNER IBA PRESIDENT/IUCN BSG CO-CHAIRS 4 President’s Column 29 A Discussion of Black Bear Management 5 The World’s Least Known Bear Species Gets 30 People are Building a Better Bear Trap its Day in the Sun 33 Florida Provides over $1 million in Incentive 7 Do You Have a Paper on Sun Bears in Your Grants to Reduce Human-Bear Conflicts Head? WORKSHOP REPORTS IBA GRANTS PROGRAM NEWS 34 Shining a Light on Sun Bears 8 Learning About Bears - An Experience and Exchange Opportunity in Sweden WORKSHOP ANNOUNCEMENTS 10 Spectacled Bears of the Dry Tropical Forest 36 5th International Human-Bear Conflict in North-Western Peru Workshop 12 IBA Experience and Exchange Grant Report: 36 13th Western Black Bear Workshop Sun Bear Research in Malaysia CONFERENCE ANNOUNCEMENTS CONSERVATION 37 26th International Conference on Bear 14 Revival of Handicraft Aides Survey for Research & Management Asiatic Black Bear Corridors in Hormozgan Province, Iran STUDENT FORUM 16 The Andean Bear in Manu Biosphere 38 Truman Listserv and Facebook Page Reserve, Rival or Ally for Communities? 39 Post-Conference Homework for Students HUMAN BEAR CONFLICTS PUBLICATIONS -
Species Assessment for the Humboldt Marten (Martes Americana Humboldtensis)
Arcata Fish and Wildlife Office Species Assessment for the Humboldt Marten (Martes americana humboldtensis) R. Hamlin, L. Roberts, G. Schmidt, K. Brubaker and R. Bosch Photo credit: Six Rivers National Forest Endangered Species Program U.S. Fish and Wildlife Service Arcata Fish and Wildlife Office 1655 Heindon Road Arcata, California 95521 (707) 822-7201 www.fws.gov/arcata September 2010 i The suggested citation for this report is: Hamlin, R., L. Roberts, G. Schmidt, K. Brubaker and R. Bosch 2010. Species assessment for the Humboldt marten (Martes americana humboldtensis). U.S. Fish and Wildlife Service, Arcata Fish and Wildlife Office, Arcata, California. 34 + iv pp. ii Table of Contents INTRODUCTION ................................................................................................................ 1 BIOLOGICAL INFORMATION .......................................................................................... 1 Species Description ................................................................................................... 1 Taxonomy.................................................................................................................. 1 Life History ............................................................................................................... 4 Reproduction .................................................................................................. 5 Diet ................................................................................................................ 5 Home Range -
Coptis Trifolia Conservation Assessment
CONSERVATION ASSESSMENT for Coptis trifolia (L.) Salisb. Originally issued as Management Recommendations December 1998 Marty Stein Reconfigured-January 2005 Tracy L. Fuentes USDA Forest Service Region 6 and USDI Bureau of Land Management, Oregon and Washington CONSERVATION ASSESSMENT FOR COPTIS TRIFOLIA Table of Contents Page List of Tables ................................................................................................................................. 2 List of Figures ................................................................................................................................ 2 Summary........................................................................................................................................ 4 I. NATURAL HISTORY............................................................................................................. 6 A. Taxonomy and Nomenclature.......................................................................................... 6 B. Species Description ........................................................................................................... 6 1. Morphology ................................................................................................................... 6 2. Reproductive Biology.................................................................................................... 7 3. Ecological Roles ............................................................................................................. 7 C. Range and Sites -
A Trip to Alaska's Brooks Range Is the Trip of a Lifetime. You’Ll See Herds of Caribou Migrating Like They Have for Thousands of Years
Hunt ID: AK-GBearMooseCaribou-Rifle-Kotzebue-AKO-Wayne A trip to Alaska's Brooks Range is the trip of a lifetime. You’ll see herds of caribou migrating like they have for thousands of years. If you feel comfortable you can take an outfitted semi-guided Caribou Hunt for the largest member of the caribou family, the barren ground caribou. Grizzly bear are often seen splashing after salmon in the river or foraging for berries on the tundra. Moose and other wildlife, including black bears, wolverine, and wolves are seen not far from camp often. He has been hunting in this area for over 40 years and guiding for over 20 years. His son’s adult sons assist with running the camp and guiding. They have both grown up hunting in the area and pride themselves with providing you a hunt of a life time. The enormous size of the big game animals has much to do with their location so far north they must have hung bulk to withstand the long cold winter. The camp is located above the Arctic Circle, in the Squirrel River Valley of the western Brooks Range. Clients fly into the Inupiaq village of Kotzebue where they board small bush planes for the 80 mile trip to the hunting area. Base camps consist of comfortable free standing Hansen Weatherport tents with cots and heaters, including a shower tent. The main tent is a cooking area and gathering point for discussing the days hunt. Cooking is provided by the staff using a modern 4 burner gas stove with oven. -
The Thermal State of Permafrost in Canada – Results from the International Polar Year
The Thermal State of Permafrost in Canada – Results from the International Polar Year Sharon L. Smith 1, Antoni G. Lewkowicz 2, Christopher R. Burn 3, Michel Allard 4 & Jennifer Throop 2 1Geological Survey of Canada, Natural Resources Canada, Ottawa, Ontario, Canada 2Department of Geography, University of Ottawa, Ottawa, Ontario, Canada 3Department of Geography and Environmental Studies, Carleton University, Ottawa, Ontario, Canada 4Centre d’études nordiques, Université Laval, Ste-Foy, Québec, Canada ABSTRACT A snapshot of permafrost thermal state in northern Canada during the International Polar Year was developed with ground temperature measurements from about 170 boreholes. The measurements span a wide range of ecoclimate and geological conditions and are at various elevations. Ground temperatures within the discontinuous permafrost zone are generally above -2°C and range to as low as -15°C in the continuous zone. Permafrost temperatures have generally increased across northern Canada for the past several decades, with greater warming rates occurring north of tree line. Consequently the spatial diversity of permafrost thermal conditions is decreasing over time. RÉSUMÉ Un instantané de l’état thermique du pergélisol dans le nord du Canada au cours de l’Année polaire internationale a été élaboré en utilisant les mesures des températures au sol obtenues d’environ 170 puits. Les mesures couvraient une vaste gamme de conditions écoclimatiques et géologiques et diverses élévations. Les températures au sol au sein de la zone discontinue de pergélisol étaient généralement supérieures à -2°C et descendaient jusqu’à -15°C dans la zone continue. Les températures du pergélisol ont généralement augmenté dans tout le nord du Canada au cours des dernières décennies, les taux de réchauffement les plus marqués étant survenus au nord de la ligne des arbres. -
Wildlife Protection Guidelines for Alaska
Wildlife Protection Guidelines for Alaska Alaska Regional Response Team, Wildlife Protection Committee Revision 5 – August 2012 2018 Administrative Update Revision 5 – August 2012 Administrative Update: March 2018 1 Table of Contents I. Introduction ........................................................................................................................... G-5 A. Background G-5 B. Objectives ........................................................................................................................... G-5 C. Scope of Wildlife Protection Guidelines for Alaska ............................................................... G-6 1. Geographic Area ............................................................................................................. G-6 2. Wildlife Resources .......................................................................................................... G-8 3. Wildlife Resource Agencies ............................................................................................. G-8 D. Committee Organization and Development of Guidelines ................................................... G-8 1. Committee Organization ................................................................................................. G-8 2. Development of Guidelines ............................................................................................ G-9 E. Relationship to National Planning Requirements and Guidance .......................................... G-9 F. Procedures for Revisions and -
I. 1. the Influence of Permafrost on Northern Development
I. 1. THE INFLUENCE OF PERMAFROST ON NORTHERN DEVELOPMENT INTRODUCTION The expansion of settlement from man's early home in the fertile, friendly and protected river valleys of the Middle East has been marked by conquest of one natural obstacle after another. Broad seas, hot, dry deserts, mountain ranges and dense forests each in their turn arrested his progress until new techniques were devised and perfected, and became common knowledge. His invasion of the tropical rainforests was delayed by diseases, and his ventures into the far north - what Stefansson has termed "The .Northward Course of Empire" (1) - were handicapped by severe cold and snow, and by the heavy ice which impeded and damaged his ships. In his long and frequently frustrated efforts to make a home in even the remotest parts of the earth, man has encountered, and eventually learned to deal with, an enormous variety of natural hazards. Perennially frozen ground in the polar regions is one of his most recent natural obstacles. It has become of major importance only in the past few decades, although its existence has long been known. Alexander Mackenzie mentioned it and Jules Verne wrote a novel (2) based in part on it, while the quick-frozen mammoths of Siberia have been a cause of wonder for generations. How was it that such a widespread phenomenon, covering about one-half of Canada and almost as great a proportion of the Soviet Union, should nevertheless have attracted so little attention that until a few years ago it even lacked a commonly accepted English name and is only now being honoured in Canada by a national symposium ? The world population map demonstrates that man has as yet barely reached in any numbers the southern limit of that one-fifth of the land surface underlain by permafrost. -
Moose Hunters in - Southwest Alaska a Better Opportunity to Evaluate Antlers
280 AN EVALUATION OF TROPHY MOOSE MANAGEMENT ON THE ALASKA PENINSULA Christian A. Smith, Alaska Dept. of Fish and Game, King Salmon, Alaska James B. Faro, Alaska Dept. of Fish and Game, Anchorage, Alaska Nicholas C. Steen, Alaska Dept. of Fish and Game, King Salmon, Alaska '" Abstract: an experimental trophy management program was initiated on the Alaska Peninsula in 1976 with the imple mentation of a regulation requiring that all harvested bull moose (AZaes aZaes gigas) have antlers with at least a 50 inch spread. The regulation was designed to protect bulls under 5 years of age, to test the capability of hunters to comply with minimum size requirements, and to determine the potential for maintaining trophy class bulls in the population through this approach. The first two objectives have been accomplished. Nearly 70 - percent of the harvested bulls have been 5 or more years old and only 4 percent of the bulls taken were illegal. Adequate survey data are not available to determine current proportions of trophy bulls in the herd. In view of the declining nature of the population and increasing frequency - of 5 year olds in the kill, however, it seems likely that current harvests may be curtailing recruitment beyond age 5. Although this may not further affect average trophy size, availability of trophy class animals could eventually be - limited to the size of the 5 year old cohort. The moose population of the central Alaska Peninsula, Game Management - Unit 9E, appears to have established via i11111igration southwest from the Naknek River drainage in the early 1930's (Faro 1969). -
Article Is Available On- Rise Derived from Satellite Imagery, Nat
The Cryosphere, 15, 1845–1862, 2021 https://doi.org/10.5194/tc-15-1845-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Spatially and temporally resolved ice loss in High Mountain Asia and the Gulf of Alaska observed by CryoSat-2 swath altimetry between 2010 and 2019 Livia Jakob1, Noel Gourmelen1,2,3, Martin Ewart1, and Stephen Plummer4 1Earthwave Ltd, Edinburgh, EH9 3HJ, UK 2School of GeoSciences, University of Edinburgh, Edinburgh, EH8 9XP, UK 3IPGS UMR 7516, Université de Strasbourg, CNRS, Strasbourg, 67000, France 4European Space Agency, ESA-ESTEC, Noordwijk, 2201 AZ, the Netherlands Correspondence: Livia Jakob ([email protected]) Received: 25 June 2020 – Discussion started: 27 July 2020 Revised: 23 February 2021 – Accepted: 26 February 2021 – Published: 14 April 2021 Abstract. Glaciers are currently the largest contributor to sea HMA ice loss is sustained until 2015–2016, with a slight de- level rise after ocean thermal expansion, contributing ∼ 30 % crease in mass loss from 2016, with some evidence of mass to the sea level budget. Global monitoring of these regions gain locally from 2016–2017 onwards. remains a challenging task since global estimates rely on a variety of observations and models to achieve the required spatial and temporal coverage, and significant differences re- main between current estimates. Here we report the first ap- 1 Introduction plication of a novel approach to retrieve spatially resolved elevation and mass change from radar altimetry over entire Glaciers store less than 1 % of the mass (Farinotti et al., 2019) mountain glaciers areas. We apply interferometric swath al- and occupy just over 4 % of the area (RGI Consortium, 2017) timetry to CryoSat-2 data acquired between 2010 and 2019 of global land ice; however their rapid rate of mass loss has over High Mountain Asia (HMA) and in the Gulf of Alaska accounted for almost a third of the global sea level rise dur- (GoA). -
Brown Bear Conservation Action Plan for Europe
Chapter 6 Brown Bear Conservation Action Plan for Europe IUCN Category: Lower Risk, least concern CITES Listing: Appendix II Scientific Name: Ursus arctos Common Name: brown bear Figure 6.1. General brown bear (Ursus arctos) distribution in Europe. European Brown Bear Action Plan (Swenson, J., et al., 1998). 250 km ICELAND 250 miles Original distribution Current distribution SWEDEN FINLAND NORWAY ESTONIA RUSSIA LATVIA DENMARK IRELAND LITHUANIA UK BELARUS NETH. GERMANY POLAND BELGIUM UKRAINE LUX. CZECH SLOVAKIA MOLDOVA FRANCE AUSTRIA SWITZERLAND HUNGARY SLOVENIA CROATIA ROMANIA BOSNIA HERZ. THE YUGOSL. FEDER. ANDORRA BULGARIA PORTUGAL ITALY MACEDONIA SPAIN ALBANIA TURKEY GREECE CYPRUS 55 Introduction assumed to live in southwestern Carinthia, representing an outpost of the southern Slovenian population expanding In Europe the brown bear (Ursus arctos) once occupied into the border area with Austria and Italy (Gutleb 1993a most of the continent including Scandinavia, but since and b). The second population is located in the Limestone about 1850 has been restricted to a more reduced range Alps of Styria and Lower Austria and comprises 8–10 (Servheen 1990), see Figure 6.1. individuals; it is the result of a reintroduction project started by WWF-Austria in 1989. In addition to these populations, the Alps of Styria and Carinthia and to a lesser Status and management of the extent also of Salzburg and Upper Austria, are visited by brown bear in Austria migrating individuals with increasing frequency. A third Georg Rauer center of bear distribution is emerging in northwestern Styria and the bordering areas of Upper Austria (Dachstein, Distribution and current status Totes Gebirge, and Sengsengebirge) where, since 1990, 1–3 bears have been present almost continuously (Frei, J., At present, there are just a few brown bears living in Bodner, M., Sorger, H.P. -
New Late Carboniferous Heritschioidinae (Rugosa) from the Kuiu Island Area and Brooks Range, Alaska
Geologica Acta, Vol.12, Nº 1, March 2014, 29-52 DOI: 10.1344/105.000002074 New Late Carboniferous Heritschioidinae (Rugosa) from the Kuiu Island area and Brooks Range, Alaska J. FEDOROWSKI1 C.H. STEVENS2 E. KATVALA3 1Institute of Geology, Adam Mickiewicz University Makow Polnych 16, PL-61-606, Poznan, Poland. E-mail: [email protected] 2Department of Geology, San Jose Unversity San Jose, California 95192, USA. E-mail: [email protected] 3Department of Geology, University of Calgary Calgary, Canada. E-mail: [email protected] ABS TRACT Three new species of the genus Heritschioides, i.e., H. alaskensis sp. nov., H. kuiuensis sp. nov., and H. splendidus sp. nov., and Kekuphyllum sandoense gen. et sp. nov. from the northeastern Kuiu Island area and nearby islets, part of Alexander terrane in southeastern Alaska, and Heritschioides separatus sp. nov. from the Brooks Range, Alaska, are described and illustrated. The three new fasciculate colonial coral species from the Kuiu Island area, collected from the Moscovian Saginaw Bay Formation, are phylogenetically related to those of probable Bashkirian age in the Brooks Range in northern Alaska as shown by the presence of morphologically similar species of Heritschioides. These corals from both areas also are related to one species in the Quesnel terrane in western Canada. Kekuphyllum sandoense from the Saginaw Bay Formation of the Kuiu Island area is the only cerioid-aphroid species within the Subfamily Heritschioidinae described so far. The complete early ontogeny of a protocorallite is for the first time described here on a basis of H. kuiuensis sp. nov. and compared to the hystero-ontogeny in order to show similarities and differences in those processes.