5-Year Review Short Form Summary
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Taxonomic Overview of the Greater Fritillary Genus Speyeria Scudder
INSECTA MUNDI A Journal of World Insect Systematics 0090 Taxonomic overview of the greater fritillary genus Speyeria Scudder and the atlantis hesperis species complexes, with species accounts, type images, and relevant literature (Lepidoptera: Nymphalidae) James C. Dunford McGuire Center for Lepidoptera and Biodiversity Florida Museum of Natural History, University of Florida PO Box 112710, Gainesville, FL 326112710, USA Date of Issue: September 26, 2009 CENTER FOR SYSTEMATIC ENTOMOLOGY, INC., Gainesville, FL James C. Dunford Taxonomic overview of the greater fritillary genus Speyeria Scudder and the atlantis hesperis species complexes, with species accounts, type images, and relevant literature (Lepidoptera: Nymphalidae) Insecta Mundi 0090: 174 Published in 2009 by Center for Systematic Entomology, Inc. P. O. Box 141874 Gainesville, FL 326141874 U. S. A. http://www.centerforsystematicentomology.org/ Insecta Mundi is a journal primarily devoted to insect systematics, but articles can be published on any nonmarine arthropod taxon. Manuscripts considered for publication include, but are not limited to, systematic or taxonomic studies, revisions, nomenclatural changes, faunal studies, book reviews, phylo genetic analyses, biological or behavioral studies, etc. Insecta Mundi is widely distributed, and refer- enced or abstracted by several sources including the Zoological Record, CAB Abstracts, etc. As of 2007, Insecta Mundi is published irregularly throughout the year, not as quarterly issues. As manuscripts are completed they are published and given an individual number. Manuscripts must be peer reviewed prior to submission, after which they are again reviewed by the editorial board to insure quality. One author of each submitted manuscript must be a current member of the Center for System- atic Entomology. -
BEFORE the SECRETARY of the INTERIOR Petition to List the Preble's Meadow Jumping Mouse (Zapus Hudsonius Preblei) As a Distinc
BEFORE THE SECRETARY OF THE INTERIOR Petition to List the Preble’s Meadow Jumping Mouse (Zapus hudsonius preblei) as a Distinct Population Segment under the Endangered Species Act November 9, 2017 Petitioners: Center for Biological Diversity Rocky Mountain Wild Acknowledgment: Conservation Intern Shane O’Neal substantially contributed to drafting of this petition. November 9, 2017 Mr. Ryan Zinke CC: Ms. Noreen Walsh Secretary of the Interior Mountain-Prairie Regional Director Department of the Interior U.S. Fish and Wildlife Service 18th and C Street, N.W. 134 Union Boulevard, Suite 650 Washington, D.C. 20240 Lakewood, CO 80228 [email protected] Dear Mr. Zinke, Pursuant to Section 4(b) of the Endangered Species Act (“ESA”), 16 U.S.C. §1533(b), Section 553(3) of the Administrative Procedures Act, 5 U.S.C. § 553(e), and 50 C.F.R. §424.14(a), the Center for Biological Diversity and Rocky Mountain Wild hereby formally petitions the Secretary of the Interior, through the United States Fish and Wildlife Service (“FWS”, “the Service”) to list the Preble’s meadow jumping mouse (Zapus hudsonius preblei) as a distinct population segment. Although the Preble’s meadow jumping mouse is already currently listed as a subspecies, this petition is necessary because of a petition seeking to de-list the Preble’s meadow jumping mouse (“jumping mouse”, “Preble’s”), filed by the Pacific Legal Foundation on behalf of their clients (PLF 2017), arguing that the jumping mouse no longer qualifies as a subspecies. Should FWS find this petition warrants further consideration (e.g. a positive 90-day finding), we are submitting this petition to ensure that the agency simultaneously considers listing the Preble’s as a distinct population segment of the meadow jumping mouse. -
Denudation History and Internal Structure of the Front Range and Wet Mountains, Colorado, Based on Apatite-Fission-Track Thermoc
NEW MEXICO BUREAU OF GEOLOGY & MINERAL RESOURCES, BULLETIN 160, 2004 41 Denudation history and internal structure of the Front Range and Wet Mountains, Colorado, based on apatitefissiontrack thermochronology 1 2 1Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM 87801Shari A. Kelley and Charles E. Chapin 2New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM 87801 Abstract An apatite fissiontrack (AFT) partial annealing zone (PAZ) that developed during Late Cretaceous time provides a structural datum for addressing questions concerning the timing and magnitude of denudation, as well as the structural style of Laramide deformation, in the Front Range and Wet Mountains of Colorado. AFT cooling ages are also used to estimate the magnitude and sense of dis placement across faults and to differentiate between exhumation and faultgenerated topography. AFT ages at low elevationX along the eastern margin of the southern Front Range between Golden and Colorado Springs are from 100 to 270 Ma, and the mean track lengths are short (10–12.5 µm). Old AFT ages (> 100 Ma) are also found along the western margin of the Front Range along the Elkhorn thrust fault. In contrast AFT ages of 45–75 Ma and relatively long mean track lengths (12.5–14 µm) are common in the interior of the range. The AFT ages generally decrease across northwesttrending faults toward the center of the range. The base of a fossil PAZ, which separates AFT cooling ages of 45– 70 Ma at low elevations from AFT ages > 100 Ma at higher elevations, is exposed on the south side of Pikes Peak, on Mt. -
Species Status Assessment Report New Mexico Meadow Jumping Mouse (Zapus Hudsonius Luteus)
Species Status Assessment Report New Mexico meadow jumping mouse (Zapus hudsonius luteus) (photo courtesy of J. Frey) Prepared by the Listing Review Team U.S. Fish and Wildlife Service Albuquerque, New Mexico May 27, 2014 New Mexico Meadow Jumping Mouse SSA May 27, 2014 EXECUTIVE SUMMARY This species status assessment reports the results of the comprehensive status review for the New Mexico meadow jumping mouse (Zapus hudsonius luteus) (jumping mouse) and provides a thorough account of the species’ overall viability and, conversely, extinction risk. The jumping mouse is a small mammal whose historical distribution likely included riparian areas and wetlands along streams in the Sangre de Cristo and San Juan Mountains from southern Colorado to central New Mexico, including the Jemez and Sacramento Mountains and the Rio Grande Valley from Española to Bosque del Apache National Wildlife Refuge, and into parts of the White Mountains in eastern Arizona. In conducting our status assessment we first considered what the New Mexico meadow jumping mouse needs to ensure viability. We generally define viability as the ability of the species to persist over the long-term and, conversely, to avoid extinction. We next evaluated whether the identified needs of the New Mexico meadow jumping mouse are currently available and the repercussions to the subspecies when provision of those needs are missing or diminished. We then consider the factors that are causing the species to lack what it needs, including historical, current, and future factors. Finally, considering the information reviewed, we evaluate the current status and future viability of the species in terms of resiliency, redundancy, and representation. -
Wildlife Regulation
Province of Alberta WILDLIFE ACT WILDLIFE REGULATION Alberta Regulation 143/1997 With amendments up to and including Alberta Regulation 148/2013 Office Consolidation © Published by Alberta Queen’s Printer Alberta Queen’s Printer 5th Floor, Park Plaza 10611 - 98 Avenue Edmonton, AB T5K 2P7 Phone: 780-427-4952 Fax: 780-452-0668 E-mail: [email protected] Shop on-line at www.qp.alberta.ca Copyright and Permission Statement Alberta Queen's Printer holds copyright on behalf of the Government of Alberta in right of Her Majesty the Queen for all Government of Alberta legislation. Alberta Queen's Printer permits any person to reproduce Alberta’s statutes and regulations without seeking permission and without charge, provided due diligence is exercised to ensure the accuracy of the materials produced, and Crown copyright is acknowledged in the following format: © Alberta Queen's Printer, 20__.* *The year of first publication of the legal materials is to be completed. Note All persons making use of this consolidation are reminded that it has no legislative sanction, that amendments have been embodied for convenience of reference only. The official Statutes and Regulations should be consulted for all purposes of interpreting and applying the law. (Consolidated up to 148/2013) ALBERTA REGULATION 143/97 Wildlife Act WILDLIFE REGULATION Table of Contents Interpretation and Application 1 Establishment of certain provisions by Lieutenant Governor in Council 2 Establishment of remainder by Minister 3 Interpretation 4 Interpretation for purposes of the Act 5 Exemptions and exclusions from Act and Regulation 6 Prevalence of Schedule 1 7 Application to endangered animals Part 1 Administration 8 Terms and conditions of approvals, etc. -
Rocky Mountain Birds: Birds and Birding in the Central and Northern Rockies
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Zea E-Books Zea E-Books 11-4-2011 Rocky Mountain Birds: Birds and Birding in the Central and Northern Rockies Paul A. Johnsgard University of Nebraska - Lincoln, [email protected] Follow this and additional works at: https://digitalcommons.unl.edu/zeabook Part of the Ecology and Evolutionary Biology Commons, and the Poultry or Avian Science Commons Recommended Citation Johnsgard, Paul A., "Rocky Mountain Birds: Birds and Birding in the Central and Northern Rockies" (2011). Zea E-Books. 7. https://digitalcommons.unl.edu/zeabook/7 This Book is brought to you for free and open access by the Zea E-Books at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Zea E-Books by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. ROCKY MOUNTAIN BIRDS Rocky Mountain Birds Birds and Birding in the Central and Northern Rockies Paul A. Johnsgard School of Biological Sciences University of Nebraska–Lincoln Zea E-Books Lincoln, Nebraska 2011 Copyright © 2011 Paul A. Johnsgard. ISBN 978-1-60962-016-5 paperback ISBN 978-1-60962-017-2 e-book Set in Zapf Elliptical types. Design and composition by Paul Royster. Zea E-Books are published by the University of Nebraska–Lincoln Libraries. Electronic (pdf) edition available online at http://digitalcommons.unl.edu/zeabook/ Print edition can be ordered from http://www.lulu.com/spotlight/unllib Contents Preface and Acknowledgments vii List of Maps, Tables, and Figures x 1. Habitats, Ecology and Bird Geography in the Rocky Mountains Vegetational Zones and Bird Distributions in the Rocky Mountains 1 Climate, Landforms, and Vegetation 3 Typical Birds of Rocky Mountain Habitats 13 Recent Changes in Rocky Mountain Ecology and Avifauna 20 Where to Search for Specific Rocky Mountain Birds 26 Synopsis of Major Birding Locations in the Rocky Mountains Region U.S. -
Appendices for Small Mammal Report
Appendix 1. Small Mammals in the Muskwa-Kechika Management Area This list includes only species actually recorded (museum specimens and observational records from published and unpublished sources) in the Muskwa-Kechika Management Area. Small mammals that probably occur in the MKMA but have not been verified from actual documented records are listed in Appendix 2. Scientific names, English common names, and species codes are based on the RIC standards (Ministry of Environment, Lands and Parks 2000). ORDER INSECTIVORA: Insectivores FAMILY SORICIDAE: Shrews Sorex cinereus Kerr Common Shrew (M-SOCI) Sorex hoyi Baird Pygmy Shrew (M-SOHO) Sorex monticolus Merriam Dusky Shrew (M-SOMO) Sorex palustris Richardson Common Water Shrew (M-SOPA) ORDER CHIROPTERA: Bats FAMILY VESPERTILIONIDAE: Vespertilionid Bats Myotis lucifugus (Le Conte) Little Brown Myotis (M-MYLU) ORDER LAGOMORPHA: Lagomorphs FAMILY LEPORIDAE: Hares and Rabbits Lepus americanus Erxleben Snowshoe Hare (M-LEAM) ORDER RODENTIA: Rodents FAMILY SCIURIDAE: Squirrels Glaucomys sabrinus (Shaw) Northern Flying Squirrel (M-GLSA) Marmota caligata (Eschscholtz) Hoary Marmot (M-MACA) Marmota monax (Linnaeus) Woodchuck (M-MAMO) Spermophilus parryii (Richardson) Arctic Ground Squirrel (M-SPPA) Tamias minimus Bachman Least Chipmunk (M-TAMI) Tamiasciurus hudsonicus (Erxleben) Red Squirrel (M-TAHU) FAMILY CASTORIDAE: Beavers Castor canadensis Kuhl Beaver (M-CACA) FAMILY MURIDAE: Murids SUBFAMILY ARVICOLINAE: Voles and Lemmings Clethrionomys gapperi (Vigors) Southern Red-backed Vole (M-CLGA) Clethrionomys -
New Mexico Meadow Jumping Mouse (Zapus Hudsonius Luteus)
New Mexico Meadow Jumping Mouse (Zapus hudsonius luteus) 5-Year Review: Summary and Evaluation U.S. Fish and Wildlife Service New Mexico Ecological Services Field Office Albuquerque, New Mexico January 30, 2020 1 5-YEAR REVIEW New Mexico meadow jumping mouse (Zapus hudsonius luteus) 1.0 GENERAL INFORMATION 1.1 Listing History Species: New Mexico meadow jumping mouse (Zapus hudsonius luteus) Date listed: June 10, 2014 Federal Register citations: • June 10, 2014. Determination of Endangered Status for the New Mexico Meadow Jumping Mouse Throughout Its Range (79 FR 33119) • March 16, 2016. Designation of Critical Habitat for the New Mexico Meadow Jumping Mouse; Final Rule ( 81 FR 14263) Classification: Endangered 1.2 Methodology used to complete the review: In accordance with section 4(c)(2) of the Endangered Species Act of 1973, as amended (Act), the purpose of a 5-year review is to assess each threatened species and endangered species to determine whether its status has changed and it should be classified differently or removed from the Lists of Threatened and Endangered Wildlife and Plants. The U.S. Fish and Wildlife Service (Service) recently evaluated the biological status of the New Mexico meadow jumping mouse to update the original 2014 Species Status Assessment (SSA) report (Service 2014). The original SSA report supported the listing of the species as endangered in 2014 and the designation of critical habitat in 2016 within eight separate geographical management areas (GMAs). The updated SSA report (Service 2020) contains the scientific basis that the Service is using to inform this 5-year review, guiding future research projects that will answer key questions about the life history and ecology of the species, and supporting further recovery planning and implementation. -
Lakamie Basin, Wyoming
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY GEORGE OTIS SMITH, DIRECTOR BULLETIN 364 GEOLOGY AND MINERAL RESOURCES OF THE LAKAMIE BASIN, WYOMING A PRELIMINARY REPORT BY N. H. DARTON AND C. E. SIEBENTHAL WASHINGTON GOVERNMENT PRINTING OFFICE 1909 CONTENTS. Page. Introduction............................................................. 7 Geography ............................................................... 8 Configuration........................................................ 8 Drainage ............................................................ 9 Climate ............................................................. 9 Temperature...................................................... 9 Precipitation..................................................... 10 Geology ................................................................. 11 Stratigraphy.......................................................... 11 General relations........................../....................... .11 Carboniferous system............................................. 13 Casper formation......................... .................... 13. General character........................................ 13 Thickness ............................................... 13 Local features............................................ 14 Erosion and weathering of limestone slopes ................ 18 Paleontology and age..................................... 19 Correlation .............................................. 20 Forelle limestone............................................ -
A Publication of the Wyoming Native Plant Society
Castilleja A Publication of the Wyoming Native Plant Society Mar 2004, Volume 23, No. 1 www.uwyo.edu/wyndd/wnps/wnps_home.htm Adventures in Laramie-Peak-Land By Hollis Marriott What does it take to convert a middle- aged construction worker with a big 4-WD pickup truck into a field botanist looking for rare plants? “Impossible!” you are probably thinking to yourself. But strange things can happen in the land of the Laramie Batholith and the Central Metamorphic Complex. The Laramie columbine, Aquilegia laramiensis, is endemic to the Laramie Mountains in southeast Wyoming. It was discovered by Aven Nelson in 1895 on a botanizing trip on and around Laramie Peak. The flowers of this little columbine are nodding, and are borne among the leaves. They have greenish-white to lavender sepals, and cream to lavender petals with spurs less than 10 mm long. Prior to the 2003 field season, Aquilegia laramiensis was known from just 12 sites, two of which were considered historical without precise location data. Most were in the northern part of the Laramie Mountains, in the vicinity of Laramie Peak. The columbine also occurs on Ragged Top Mountain about 60 miles to the south, and Char Delmatier found it roughly halfway Aquilegia laramiensis, by Isobel Nichols between Laramie Peak and Ragged Top in In this issue: 1993. Most of the known populations were Living floras – keeping score of score-keepers . 3 growing on granite rocks. The columbine Physaria vitulifera status in Wyoming . 5 appeared to be rare, but those in the know Invasive species and CBM development . -
Pennsylvanian and Associated Rocks in Wyomin
Pennsylvanian and Associated Rocks in Wyomin By WILLIAM W. MALLORY SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 5S4-G A regional study of the extent, thickness, lit ho logy, and stratigraphic relations of the Tensleep, Ams- den, Casper, and Fountain Formations, with em phasis on origin,paleogeography, and paleotectonic implications UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1967 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract. _________________________________________ Gl Casper Formation._________________________________ G17 Introduction. ______________________________________ 1 Fountain Formation._______________________________ 18 Location and extent of the area. _ _________________ 1 Minnelusa and Hartville Formations __________________ 18 Scope and objectives. ___________________________ 1 Morgan Formation and Weber Sandstone-_____________ 20 Previous work and acknowledgments. ____________ 2 Rocks of Morrow age in the Minnelusa, Hartville, Casper, Methods of study. _____________________________ 2 and Morgan Formations..___________-_-_--______-_ 20 Tectonic setting of the Middle Rocky Mountain region in Tensleep Sandstone._____-____________------------__ 21 Pennsylvanian time.. _ ____________________________ 3 Lithology and thickness.___-_-____-------_______ 21 Definition of the Pennsylvanian System -
The Rocky Mountain Front, Southwestern USA
The Rocky Mountain Front, southwestern USA Charles E. Chapin, Shari A. Kelley, and Steven M. Cather New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801, USA ABSTRACT northeast-trending faults cross the Front thrust in southwest Wyoming and northern Range–Denver Basin boundary. However, Utah. A remarkable attribute of the RMF is The Rocky Mountain Front (RMF) trends several features changed from south to north that it maintained its position through multi- north-south near long 105°W for ~1500 km across the CMB. (1) The axis of the Denver ple orogenies and changes in orientation from near the U.S.-Mexico border to south- Basin was defl ected ~60 km to the north- and strength of tectonic stresses. During the ern Wyoming. This long, straight, persistent east. (2) The trend of the RMF changed from Laramide orogeny, the RMF marked a tec- structural boundary originated between 1.4 north–northwest to north. (3) Structural tonic boundary beyond which major contrac- and 1.1 Ga in the Mesoproterozoic. It cuts style of the Front Range–Denver Basin mar- tional partitioning of the Cordilleran fore- the 1.4 Ga Granite-Rhyolite Province and gin changed from northeast-vergent thrusts land was unable to penetrate. However, the was intruded by the shallow-level alkaline to northeast-dipping, high-angle reverse nature of the lithospheric fl aw that underlies granitic batholith of Pikes Peak (1.09 Ga) faults. (4) Early Laramide uplift north of the RMF is an unanswered question. in central Colorado.