Squires Et Al 2012

Total Page:16

File Type:pdf, Size:1020Kb

Squires Et Al 2012 Estimating detection probability for Canada lynx Lynx canadensis using snow-track surveys in the northern Rocky Mountains, Montana, USA Author(s): John R. Squires, Lucretia E. Olson, David L. Turner, Nicholas J. DeCesare & Jay A. Kolbe Source: Wildlife Biology, 18(2):215-224. Published By: Nordic Board for Wildlife Research DOI: http://dx.doi.org/10.2981/10-105 URL: http://www.bioone.org/doi/full/10.2981/10-105 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Wildl. Biol. 18: 215-224 (2012) Short communication DOI: 10.2981/10-105 Ó Wildlife Biology, NKV www.wildlifebiology.com Estimating detection probability for Canada lynx Lynx canadensis using snow-track surveys in the northern Rocky Mountains, Montana, USA John R. Squires, Lucretia E. Olson, David L. Turner, Nicholas J. DeCesare & Jay A. Kolbe We used snow-tracking surveys to determine the probability of detecting Canada lynx Lynx canadensis in known areas of lynx presence in the northern Rocky Mountains, Montana, USA during the winters of 2006 and 2007. We used this information to determine the minimum number of survey replicates necessary to infer the presence and absence of lynx in areas of similar lynx density (approximately 2.8 lynx/100 km2) with confidence. The probability of detecting lynx in mountainous habitats that support resident populations was 0.80-0.99 when surveys were conducted on an 838km2 grid with 10 km of search effort per cell. Snow-track surveys were highly successful at detecting the presence of Canada lynx over large landscapes. Two survey replicates established absence of Canada lynx with 95% certainty. The high probability of detection associated with snow-track surveys makes this method useful for documenting populations of Canada lynx in areas where their status is uncertain. Key words: Canada lynx, detection probability, forest carnivores, Lynx canadensis, monitoring, snow-track surveys John R. Squires & Lucretia E. Olson, U.S. Forest Service, Rocky Mountain Research Station, 800 E. Beckwith, Missoula, Montana 59801, USA - e-mail addresses: [email protected] (John R. Squires); [email protected] (Lucretia E. Olson) David L. Turner, U.S. Forest Service, Rocky Mountain Research Station, 860 North 1200 E. Logan, Utah 84321, USA - e- mail: [email protected] Nicholas J. DeCesare, College of Forestry and Conservation, University Of Montana, Missoula, Montana 59812, USA - e- mail: [email protected] Jay A. Kolbe, Montana Fish, Wildlife and Parks, P.O. Box 1288, Seeley Lake, Montana 59868, USA - e-mail: jkolbe@mt. gov Corresponding author: John R. Squires Received 1 October 2010, accepted 2 October 2011 Associate Editor: Aure´lien Besnard Canada lynx Lynx canadensis are federally listed in rare or sensitive species are often based on anecdotal the contiguous United States as a threatened species occurrence data (unverifiable observations or sign; under the Endangered Species Act (U.S. Fish and McKelvey et al. 2008). Using anecdotal data to de- Wildlife Service 2000). Therefore, determining the lineate species occurrence leads to errors of omission presence or absence of lynx across broad landscapes, and commission that result in a misallocation of such as wilderness areas or national forest units, is limited funding and inefficient conservation actions important to conservationists and land managers. (McKelvey et al. 2008). Snow-tracking to detect The presence of carnivores can be especially difficult carnivores is particularly effective because it does not to establish as they are often cryptic, exhibit crepus- require a solicited response from the animal, it do- cular activity patterns and occur at low densities cuments the presence of individuals over a span of across large spatial scales (Wilson & Delahay 2001, several days if snow conditions permit, and it is O’Connell et al. 2006, Kolbe & Squires 2007). generally low cost compared to live-trapping or re- Delineations of current and historical ranges for mote cameras (Reid et al. 1987, Halfpenny et al. Ó WILDLIFE BIOLOGY 18:1 (2012) 215 1997, Foresman & Pearson 1998). Snow-track sur- tions (Squires et al. 2004). In that study, we used veys have been used successfully to determine the computer simulations to model the probability of presence of a variety of carnivore species, including detecting lynx snow-tracks depending on the amount wolverine Gulo gulo, river otter Lutra canadensis,red of search effort. Our goal in this study is to expand on fox Vulpes vulpes and short-tailed weasel Mustela this earlier work by calculating the empirical prob- erminea (Reid et al. 1987, Edelmann & Copeland ability of detecting lynx based on snow-track surveys 1999, Forsey & Baggs 2001, Ulizio et al. 2006, in areas of known presence. We focus on detectability Heinemeyer et al. 2008). However, a chronic weak- within areas occupied by resident populations of lynx ness of monitoring strategies based on snow-tracking rather than in areas occupied by single dispersing is species misidentification. This shortcoming can be individuals to ensure that underlying lynx densities addressed to meet evidentiary standards of species are relevant for conservation. We address the fol- identification by considering the snow-track a lowing two questions: 1) What was the probability of ’collection device’ for obtaining genetic samples detecting lynx with snow-track surveys conducted in (Squires et al. 2004), a method demonstrated to be areas with confirmed resident populations? 2) Given effective for lynx (McKelvey et al. 2006) and other this estimated detection probability, what level of forest carnivores (Ulizio et al. 2006). survey effort would be necessary to infer the absence Monitoring efforts based on snow-track surveys of resident lynx populations with confidence? Based conducted on a standardized survey grid can be used on these results, we offer management recommenda- to delineate local distributions of lynx (Squires et al. tions to optimize survey methods for monitoring lynx 2004). In the Northern Rocky Mountains, Montana, using snow-tracking methodology. USA, delineations of local lynx distributions as de- termined by snow-tracks overlapped the distribution of lynx as estimated by radio-telemetry by 97% Material and methods (Squires et al. 2004). Track counts can also estimate animal population density if track age and estimated We conducted our study in two regions of western daily travel rates are known (Stephens et al. 2006). Montana: the Purcell Mountains in the northwest However, using snow-track surveys to establish corner of the state and the Seeley Lake area, either the presence or absence of species in potential including the Garnet Range, located approximately habitat may be more difficult. Although species 50 km to the southwest (Fig. 1). The boreal forests in presence can be ascertained by a single detection the Seeley Lake area and the Garnet Range are (assuming correct identity), absence is difficult to composed mainly of subalpine fir Abies lasiocarpa establish with statistical certainty. A variety of sta- and Engelmann spruce Picea engelmannii,witha tistical concepts, including occupancy models, spe- smaller component of lodgepole pine Pinus contorta cies distribution models and mark-recapture models, and western larch Larix occidentalis; ponderosa pine provide statistical frameworks for modeling species Pinus ponderosa and Douglas-fir Pseudotsuga men- occurrence across landscapes (Pollock et al. 1990, ziesii were dominant at low elevations. Forests in the McKenzie et al. 2003, Elith et al. 2006). These models Purcell Mountains are similar with the addition of are data intensive and require significant financial western red cedar Thuja plicata and western hemlock and time commitments. Since our primary goal was Tsuga mertensiana in mixed stands. Elevations to provide managers with a relatively accessible ranged from 800 to 2,300 m a.s.l. in the Purcell method of estimating probability of detection and Mountains and from 1,200 to 2,500 m in the Seeley presence/absence of lynx, we chose to use a more Lake area and Garnet Range. tractable model by McArdle (1990) and Reed (1996). During 2006 and 2007, we conducted winter snow- This model uses the estimated probability of detect- track surveys for lynx on a grid of 8 3 8kmsquares ing a given species to determine the number of following Squires et al. (2004). This grid size roughly sampling events necessary to establish presence or equals an average female home range (of 72 km2)for absence with known statistical certainty, and has lynx from southern boreal forests (United States and proven to be effective in determining the number of southern Canada; Aubry et al. 2000, Squires et al. sampling events necessary to detect species that occur 2004). We used VHF-telemetry to verify the presence at different densities (Kery 2002, Jackson et al. 2006). of lynx in our study areas prior to surveys; however, In a previous study, we demonstrated the efficacy the technicians did not know the actual location of of snow-tracking for delineating local lynx distribu- lynx when they conducted their surveys. We selected 216 Ó WILDLIFE BIOLOGY 18:1 (2012) Figure 1. Locations of the survey grids used in the Purcell Mountains, near Libby, Montana, and the Seeley Lake area, near Missoula, Montana.
Recommended publications
  • Montana Forest Insect and Disease Conditions and Program Highlights
    R1-16-17 03/20/2016 Forest Service Northern Region Montata Department of Natural Resources and Conservation Forestry Division In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. Additionally, program information may be made available in languages other than English. To file a program discrimination complaint, complete the USDA Program Discrimination Complaint Form, AD-3027, found online at http://www.ascr.usda.gov/complaint_filing_cust.html and at any USDA office or write a letter addressed to USDA and provide in the letter all of the information requested in the form. To request a copy of the complaint form, call (866) 632-9992. Submit your completed form or letter to USDA by: (1) mail: U.S.
    [Show full text]
  • Harry Butler Has Been Taken Into Custody for Violation of Donlan Law
    people,of Montana, out of the great­ hearted generosity that has ever char­ acterized them, respond as liberally as may be possible in this emergency for- the relief of suffering that is daily becoming more distressing. Contri­ The Scenic theater was practically butions may be made to any member packed to its doors last Friday night of the Montana state board of the at 7:30, one half hour before the ama­Harry Butler Has Been Taken Dilloninto Leads with Thirty-twoAmerican Red Cross, said board1 be­ teur performance began. Twelve num­ ing composed of the followingProposed citizens to Extend the Great bers were presented to an appreciativeCustody for Violation of Names, Wisdom next of this state: Edward J. Bowman, audience, Edward Hoffman receiving Anaconda, treasurer; Henry W. Row-Northern from Moccasin first prize, Miss Belle Holmes second Donlan Law. with Seven ley, Billings, secretary; F. S. Lusk, to the Capital and Miss Ruth Stoller third. The Missoula; T. A. Marlow, Helena; Ken­ SPEECH OF PATTERSON LIKED winner sang a song, little Miss HolmesSECURES VICTIMS WITH NOTES FIRST RAILROAD CASE MONDAY neth McLean, Miles City; W. M recited a poem and Miss Stoller sang Thornton, Great Falls. All fundsGILMORE thus & PITTSBURG LIKELY a song and then gave a fair imitationLuring Missives Will Be Used as received will be promptly remitted to Gives His Views on Roadways and Isof the skirt dance. The latter’s act Considerable Interest Manifested in A Portland Dispatch Says the G. A Interested in Park-to-Park Evidence Against Him in Com- These Cases—Burglary Trial the national treasurer of the Red CrossP.
    [Show full text]
  • 1 OUTREACH Kootenai National Forest Supervisor's Office, Fire and Aviation Management Forestry Technician GS-0462-05 IA Di
    OUTREACH Kootenai National Forest Supervisor’s Office, Fire and Aviation Management Forestry Technician GS‐0462‐05 IA Dispatcher The Northern Region (R1), Kootenai National Forest, Supervisor’s Office, Fire and Aviation Management, GS‐0462‐05, position. Duty station is Libby, MT. This is a permanent seasonal 13/13 position. The results of the outreach will help determine the area of consideration for the vacancy announcement. Interested applicants are requested to respond utilizing the Employee Outreach Database. For Forest Service applicants the database is located in ConnectHR. For external applicants this may be accessed by an internet search for FS Outreach or the following link https://fsoutreach.gdcii.com/Outreach. Duties This position serves as a Fire Dispatcher located in an interagency (Forest Service and Montana Department of Natural Resources dispatch center. The center is responsible primarily for wildland fire preparedness and suppression support activities and may assist with all‐risk incidents as needed or directed. Work schedule may include weekends with days off during the week. Incumbent serves as a dispatcher, receiving, filling, and tracking resources requests for fire and other emergency incidents. Follows established procedures to perform a variety of technical duties common to the dispatch of personnel, equipment, aircraft and/or supplies according to 1 pre‐defined plans or in a response to resource orders from the field. Incumbent initiates requests to higher organizational levels for additional resources as needed. Collects, processes, collates and submits incident information to support fire operations (e.g. fire reports smoke permits, spot weather forecasts, prescribed fire burn requests). Processes and interprets weather information (e.g.
    [Show full text]
  • Geologic Map of the Line Point Quadrangle, Boundary County Idaho, and Lincoln County, Montana
    IDAHO GEOLOGICAL SURVEY IDAHOGEOLOGY.ORG IGS DIGITAL WEB MAP 150 MONTANA BUREAU OF MINES AND GEOLOGY MBMG.MTECH.EDU MBMG OPEN FILE 623 white graded or nongraded argillite tops. Conspicuous bar code-like REFERENCES patterns in the middle, formed by alternating dark and light siltite, persist regionally (Huebschman, 1973) and have been used as markers for correla- GEOLOGIC MAP OF THE LINE POINT QUADRANGLE, BOUNDARY COUNTY, IDAHO, AND tion by Cominco (Hamilton and others, 2000). Siltite and argillite couplets, Anderson, H.E., and D.W. Davis, 1995, U-Pb geochronology of the Moyie sills, with dark, less commonly light tops, have even and parallel, uneven, wavy Purcell Supergroup, southeastern British Columbia: Implications for the or undulating lamination. Rusty nature of outcrop is due to weathering of Mesoproterozoic geological history of the Purcell (Belt) basin: Canadian CORRELATION OF MAP UNITS abundant sulfides, commonly pyrrhotite. Dominant lamination style and Journal of Earth Sciences, v. 32, no. 8, p. 1180-1193. LINCOLN COUNTY, MONTANA concentration of sulfides vary between members. Quartzite in 2-20 dm beds Anderson, H.E., and W.D. Goodfellow, 2000, Geochemistry and isotope chem- Alluvial and Colluvium and Glacial and Related Deposits is light weathering, averages about 60 percent quartz, 20 percent plagio- istry of the Moyie sills: Implications for the early tectonic setting of the Lacustrine Deposits Mass Wasting Deposits clase, with the rest mostly white micas and 5 percent biotite (Cressman, Mesoproterozoic Purcell basin, in J.W. Lydon, Trygve Höy, J.F. Slack, and 1989). Previous mapping in this area and to the east by Cressman and Harri- M.E.
    [Show full text]
  • The Purcell Lava Glacier National Park, Montana
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY The Purcell Lava Glacier National Park, Montana by Robert G. McGimsey 1 Open-File Report 85-0543 1985 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editoral standards and stratigraphic nomenclature Denver, Colorado CONTENTS Page LIST OF FIGURES.......................................................... iii LIST OF TABLES........................................................... vii ABSTRACT................................................................. 1 ACKNOWLEDGMENTS.......................................................... 2 CHAPTER I. INTRODUCTION..................................................... 3 Purpose of Investigation....................................... 3 Location and Geologic Setting.................................. 3 Previous Work.................................................. 4 Field and Laboratory Methods................................... 5 II. DIVISION AND DESCRIPTION OF FACIES............................... 6 Introduction................................................... 6 Pillow Lava Facies............................................. 6 Two-Dimensional Pillow Exposures............................. 7 Three-Dimensional Pillow Exposures........................... 9 Isolated- and Broken-Pillow Breccia.......................... 9 Coalesced Pillows and the Upper Contact...................... 10 Hyaloclastite Breccia........................................ 10 Intercalated Sediment.......................................
    [Show full text]
  • Glacier National Park Geologic Resource Evaluation Report
    National Park Service U.S. Department of the Interior Geologic Resources Division Denver, Colorado Glacier National Park Geologic Resource Evaluation Report Glacier National Park Geologic Resource Evaluation Geologic Resources Division Denver, Colorado U.S. Department of the Interior Washington, DC Table of Contents List of Figures .............................................................................................................. iv Executive Summary ...................................................................................................... 1 Introduction ................................................................................................................... 3 Purpose of the Geologic Resource Evaluation Program ............................................................................................3 Geologic Setting .........................................................................................................................................................3 Glacial Setting ............................................................................................................................................................4 Geologic Issues............................................................................................................. 9 Economic Resources..................................................................................................................................................9 Mining Issues..............................................................................................................................................................9
    [Show full text]
  • Geologic Map of the Curley Creek Quadrangle, Boundary County
    IDAHO GEOLOGICAL SURVEY IDAHOGEOLOGY.ORG DIGITAL WEB MAP 148 MONTANA BUREAU OF MINES AND GEOLOGY MBMG.MTECH.EDU MBMG OPEN FILE 625 CORRELATION OF MAP UNITS Ravalli Group STRUCTURE GEOLOGIC MAP OF THE CURLEY CREEK QUADRANGLE, BOUNDARY COUNTY, IDAHO, AND The Ravalli Group that crosses the northeast quadrant of the map is only Alluvial and Colluvium and Glacial and Related Deposits slightly thicker than documented to the southeast (Cressman and Harrison, The major structure in this quadrangle is the Moyie fault. It is characterized Lacustrine Deposits Mass Wasting Deposits 1986) and south-southwest (Burmester and others, 2007). Although cosets regionally as an east-vergent thrust and juxtaposes older rocks on the west QalQQar lm Qt Qcg Qglc Holocene of thick sets of quartzite used to define the Revett elsewhere (Hayes, 1983; (hanging wall) against younger rocks on the east, consistent with this LINCOLN COUNTY, MONTANA Hayes and Einaudi, 1986) are rarely observed, Revett is mapped on the east interpretation. However, strata of the hanging and foot walls face each Quaternary side of the Sylvanite anticline, Fig. 1, (Cressman and Harrison, 1986) and Qgl Qgo Qg Qgt Qgk Pleistocene other, giving the impression that the fault occupies a syncline. Support for a correlated with the middle Creston north of the border where copper-silver- synclinal fold geometry comes from existence of a slightly east-verging, cobalt mineralization is similar to that in the Revett to the south (Hartlaub, southward-plunging syncline west of the Moyie fault south of the map, 1 1 1 1 2 Intrusive Rocks 2009). Revett mapped here as the swath of quartzite-rich strata below more Fig.1, (Miller and Burmester, 2004) and an open, northward-plunging Roy M.
    [Show full text]
  • Cabinet-Yaak Grizzly Bear Recovery 2016 Research and Monitoring Progress Report
    CABINET-YAAK GRIZZLY BEAR RECOVERY AREA 2016 RESEARCH AND MONITORING PROGRESS REPORT PREPARED BY WAYNE F. KASWORM, THOMAS G. RADANDT, JUSTIN E. TEISBERG, ALEX WELANDER, MICHAEL PROCTOR, AND HILARY COOLEY 2017 UNITED STATES FISH AND WILDLIFE SERVICE GRIZZLY BEAR RECOVERY COORDINATOR'S OFFICE UNIVERSITY OF MONTANA, MAIN HALL ROOM 309 MISSOULA, MONTANA 59812 (406) 243-4903 1 This annual report is cumulative and represents data collected since the inception of this monitoring program in 1983. New information collected or made available to this study is incorporated, reanalyzed, and summarized annually. Information in this report supersedes previous reports. Please obtain permission prior to citation. Cite this report as follows: Kasworm, W. F., T. G. Radandt, J.E. Teisberg, A. Welander, M. Proctor, and H. Cooley. 2017. Cabinet-Yaak grizzly bear recovery area 2016 research and monitoring progress report. U.S. Fish and Wildlife Service, Missoula, Montana. 101 pp. ABSTRACT Sixteen grizzly bears were monitored with radio collars during portions of 2016. Research monitoring included seven females (three adults and four subadults) and nine males (five adults and four subadults) in the Cabinet-Yaak ecosystem (CYE). Two bears of these bears were from the Cabinet Mountains (1 subadult male and 1 subadult female) and part of the augmentation program. Grizzly bear monitoring and research has been ongoing in the Cabinet Mountains since 1988 and in the Yaak River since 1986. Sixty-eight resident bears have been captured and monitored through telemetry in the two areas from 1986-2016. Research in the Cabinet Mountains indicated that only a small population remained as of 1988.
    [Show full text]
  • Mesoproterozoic–Early Cretaceous Provenance and Paleogeographic Evolution of the Northern Rocky Mountains
    Mesoproterozoic–Early Cretaceous provenance and paleogeographic evolution of the Northern Rocky Mountains: Insights from the detrital zircon record of the Bridger Range, Montana, USA Chance B. Ronemus†, Devon A. Orme, Saré Campbell, Sophie R. Black, and John Cook Department of Earth Sciences, Montana State University, P.O. Box 173480, Bozeman, Montana 59717-3480, USA ABSTRACT Jurassic detritus into the foreland basin to rels et al., 1996, 2011; Gehrels and Ross, 1998; dominate by the Early Cretaceous. Park et al., 2010; Laskowski et al., 2013). These The Bridger Range of southwest Montana, ancient sources may consist of first-cycle grains USA, preserves one of the most temporally INTRODUCTION derived from Precambrian basement provinces extensive sedimentary sections in North or more recent magmatism. However, zircons America, with strata ranging from Meso- Sedimentary rocks in the Bridger Range of are more commonly sourced from erosion and proterozoic to Cretaceous in age. This study southwest Montana, USA, record the Mesopro- recycling of previously deposited sedimentary presents new detrital zircon geochronologic terozoic–Mesozoic history of sedimentation in rock (e.g., Schwartz et al., 2019). data from eight samples collected across this this region of North America, with Mesopro- The evolution of sedimentary provenance is mountain range. Multidimensional scaling terozoic to Cretaceous stratigraphy exposed as strongly influenced by tectonic factors (Gehrels, and non-negative matrix factorization sta- a generally eastward dipping homoclinal panel 2014). Tectonic events, such as rifting and moun- tistical analyses are used to quantitatively across the range (Fig. 1). The >8 km of stratig- tain building, trigger drainage reorganization unmix potential sediment sources from these raphy collectively record critical information and uplift new sediment sources.
    [Show full text]
  • WEST KOOTENAY / REVELSTOKE DESTINATION DEVELOPMENT STRATEGY MONASHEE MOUNTAINS Photo: Ryan Creary
    WEST KOOTENAY / REVELSTOKE DESTINATION DEVELOPMENT STRATEGY MONASHEE MOUNTAINS Photo: Ryan Creary DESTINATION BC Seppe Mommaerts MANAGER, DESTINATION DEVELOPMENT Jody Young SENIOR PROJECT ADVISOR, DESTINATION DEVELOPMENT [email protected] KOOTENAY ROCKIES TOURISM Emilie Cayer-Huard INDUSTRY & DESTINATION DEVELOPMENT SPECIALIST 250 427 4838 Ext.206 [email protected] MINISTRY OF TOURISM, ARTS AND CULTURE Amber Mattock DIRECTOR, LEGISLATION AND DESTINATION BC GOVERNANCE 250 356 1489 [email protected] INDIGENOUS TOURISM ASSOCIATION OF BC 604 921 1070 [email protected] WEST KOOTENAY/REVELSTOKE | 2 TABLE OF CONTENTS I. EXECUTIVE SUMMARY .....................................................................1 7. STRATEGY AT A GLANCE ............................................................. 35 a. The West Kootenay/Revelstoke Area — A Distinctive Destination 8. STRATEGIC PRIORITIES ................................................................ 36 b. Destination Development in the West Kootenay/Revelstoke 8.1 Theme 1 — Improve Access, Signage and Infrastructure Area — A Distinctive Direction 8.1.1 Access 8.1.2 Signage II. ACRONYMS .........................................................................................7 8.1.3 Infrastructure 1. FOREWORD AND ACKNOWLEDGEMENTS...........................8 8.2 Theme 2 — Improve Business Operating Conditions 8.3 Theme 3 — Enhance Experiential Quality and Variety 2. INTRODUCING THE STRATEGY .................................................10 8.3.1 Experiential
    [Show full text]
  • Wolverine Ecology and Conservation in the Western United States
    Acta Universitatis Agriculturae Sueciae • 2013:4 No. Thesis Doctoral Doctoral Thesis No. 2013:4 This thesis focuses on wolverine ecology and conservation in the western Doctoral Thesis No. 2013:4 United States. The thesis covers the wolverine’s niche, scale of effective Faculty of Natural Resources and Agricultural Sciences management, and conservation priorities; it also examines the institutional system in place for delivering conservation actions for non-game species like wolverines. The analyses presented include home range size, movement Ecology and Conservation in the Western… Wolverine Wolverine Ecology and Conservation in rates, social organization, density, dispersal, reproductive chronology, habitat the Western United States selection, and connectivity. This thesis provides information that can facilitate recovery and management of this candidate endangered species. Robert Michael Inman Robert Michael Inman received his Master and Bachelor of Science degrees from the University of Tennessee, Department of Forestry, Wildlife and Fisheries. Acta Universitatis Agriculturae Sueciae presents doctoral theses from the Swedish University of Agricultural Sciences (SLU). SLU generates knowledge for the sustainable use of biological natural • Robert Michael Inman • Robert Michael resources. Research, education, extension, as well as environmental monitoring and assessment are used to achieve this goal. Online publication of thesis summary: http://epsilon.slu.se/eindex.html ISSN 1652-6880 ISBN 978-91-576-7761-7 Wolverine Ecology and Conservation in the Western United States Robert Michael Inman Faculty of Natural Resources and Agricultural Sciences Department of Ecology Uppsala Doctoral Thesis Swedish University of Agricultural Sciences Uppsala 2013 Acta Universitatis agriculturae Sueciae 2013:4 Cover: F121 and two cubs of the year in the Gravelly Range of Montana, USA.
    [Show full text]
  • Cabinet-Yaak Grizzly Bear Recovery Area 2019 Research and Monitoring Progress Report
    CABINET-YAAK GRIZZLY BEAR RECOVERY AREA 2019 RESEARCH AND MONITORING PROGRESS REPORT PREPARED BY WAYNE F. KASWORM, THOMAS G. RADANDT, JUSTIN E. TEISBERG, TYLER VENT, ALEX WELANDER, MICHAEL PROCTOR, HILARY COOLEY, AND JENNIFER FORTIN-NOREUS 2020 UNITED STATES FISH AND WILDLIFE SERVICE GRIZZLY BEAR RECOVERY COORDINATOR'S OFFICE UNIVERSITY OF MONTANA, MAIN HALL ROOM 309 MISSOULA, MONTANA 59812 (406) 243-4903 1 This annual report is cumulative and represents data collected, reanalyzed and summarized annually since the inception of this monitoring program in 1983. Information in this report supersedes previous reports. Please obtain permission prior to citation. Cite as follows: Kasworm, W. F., T. G. Radandt, J. E. Teisberg, T. Vent, A. Welander, M. Proctor, H. Cooley and J. Fortin-Noreus. 2020. Cabinet-Yaak grizzly bear recovery area 2019 research and monitoring progress report. U.S. Fish and Wildlife Service, Missoula, Montana. 105 pp. ABSTRACT Twelve grizzly bears were monitored with radio-collars during portions of 2019. Research monitoring included four females (two adults and two subadults) and eight males (three adult and five subadults) in the Cabinet-Yaak Ecosystem (CYE). Two subadult males and a subadult female were from the Cabinet Mountains augmentation program. One adult male bear was collared for conflict management purposes. Grizzly bear monitoring and research has been ongoing in the Cabinet Mountains since 1983 and in the Yaak River since 1986. Eighty-one resident bears were captured and monitored through telemetry in the two areas from 1983–2019. Research in the Cabinet Mountains indicated that only a small population remained as of 1988. Concern over persistence of grizzly bear populations within this area resulted in a pilot program in 1990 that tested population augmentation techniques.
    [Show full text]