INSECTS 1 Insects: Native 10 Defoliators 10 Douglas-Fir Tussock Moth
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Membership 2005: Year in Review
ESA Newsletter Information for the Members of the Entomological Society of America MARCH 2006 • VOLUME 29, NUMBER 3 Membership 2005: Year in Review By Chris Stelzig, Director of Membership we get too far into the year, I wanted to fin- not withstanding, this is a great, inexpensive and Marketing ish the update on 2005. way to get general feedback from you on a Sections and Branches—The Pacific wide range of topics. Headquarters uses this For the first time since 1992, ESA posted Branch saw the most growth when we com- data for planning purposes. In the Member- two back-to-back years of membership pare 2004 to 2005 with a 12% increase in ship Toolbox on the website (http://www. growth. This is a milestone, especially when membership. Only the Southeastern Branch entsoc.org/membership/toolbox/support_ coupled with the fact that just five years ago saw an actual decline, and that was merely esa/survey.htm), you will find a list of all our we were losing members by the hundreds by one person (a case in point to say that active surveys and an invitation to partici- every year and our funds were quickly dry- EVERY membership renewal is important!). pate in one. ing up. You’ve heard me say “Strength in Section B saw the largest growth last year, Performance—About 80% of members Numbers” for nearly five years now. The leaping more than 10%. who responded felt that they were satisfied reason for this is that membership is the Membership Types—As I mentioned with performance from ESA headquarters. -
Forest Insect Conditions in the United States 1966
FOREST INSECT CONDITIONS IN THE UNITED STATES 1966 FOREST SERVICE ' U.S. DEPARTMENT OF AGRICULTURE Foreword This report is the 18th annual account of the scope, severity, and trend of the more important forest insect infestations in the United States, and of the programs undertaken to check resulting damage and loss. It is compiled primarily for managers of public and private forest lands, but has become useful to students and others interested in outbreak trends and in the location and extent of pest populations. The report also makes possible n greater awareness of the insect prob lem and of losses to the timber resource. The opening section highlights the more important conditions Nationwide, and each section that pertains to a forest region is prefaced by its own brief summary. Under the Federal Forest Pest Control Act, a sharing by Federal and State Governments the costs of surveys and control is resulting in a stronger program of forest insect and disease detection and evaluation surveys on non-Federal lands. As more States avail themselves of this financial assistance from the Federal Government, damage and loss from forest insects will become less. The screening and testing of nonpersistent pesticides for use in suppressing forest defoliators continued in 1966. The carbamate insecticide Zectran in a pilot study of its effectiveness against the spruce budworm in Montana and Idaho appeared both successful and safe. More extensive 'tests are planned for 1967. Since only the smallest of the spray droplets reach the target, plans call for reducing the spray to a fine mist. The course of the fine spray, resulting from diffusion and atmospheric currents, will be tracked by lidar, a radar-laser combination. -
Insects That Feed on Trees and Shrubs
INSECTS THAT FEED ON COLORADO TREES AND SHRUBS1 Whitney Cranshaw David Leatherman Boris Kondratieff Bulletin 506A TABLE OF CONTENTS DEFOLIATORS .................................................... 8 Leaf Feeding Caterpillars .............................................. 8 Cecropia Moth ................................................ 8 Polyphemus Moth ............................................. 9 Nevada Buck Moth ............................................. 9 Pandora Moth ............................................... 10 Io Moth .................................................... 10 Fall Webworm ............................................... 11 Tiger Moth ................................................. 12 American Dagger Moth ......................................... 13 Redhumped Caterpillar ......................................... 13 Achemon Sphinx ............................................. 14 Table 1. Common sphinx moths of Colorado .......................... 14 Douglas-fir Tussock Moth ....................................... 15 1. Whitney Cranshaw, Colorado State University Cooperative Extension etnomologist and associate professor, entomology; David Leatherman, entomologist, Colorado State Forest Service; Boris Kondratieff, associate professor, entomology. 8/93. ©Colorado State University Cooperative Extension. 1994. For more information, contact your county Cooperative Extension office. Issued in furtherance of Cooperative Extension work, Acts of May 8 and June 30, 1914, in cooperation with the U.S. Department of Agriculture, -
3.7.10 Curculioninae Latreille, 1802 Jetzt Beschriebenen Palaearctischen Ceuthor- Rhynchinen
Curculioninae Latreille, 1802 305 Schultze, A. (1902): Kritisches Verzeichniss der bis 3.7.10 Curculioninae Latreille, 1802 jetzt beschriebenen palaearctischen Ceuthor- rhynchinen. – Deutsche Entomologische Zeitschrift Roberto Caldara , Nico M. Franz, and Rolf 1902: 193 – 226. G. Oberprieler Schwarz, E. A. (1894): A “ parasitic ” scolytid. – Pro- ceedings of the Entomological Society of Washington 3: Distribution. The subfamily as here composed (see 15 – 17. Phylogeny and Taxonomy below) includes approx- Scudder, S. H. (1893): Tertiary Rhynchophorous Coleo- ptera of the United States. xii + 206 pp. US Geological imately 350 genera and 4500 species (O ’ Brien & Survey, Washington, DC. Wibmer 1978; Thompson 1992; Alonso-Zarazaga Stierlin, G. (1886): Fauna insectorum Helvetiae. Coleo- & Lyal 1999; Oberprieler et al. 2007), provisionally ptera helvetiae , Volume 2. 662 pp. Rothermel & Cie., divided into 34 tribes. These are geographically Schaffhausen. generally restricted to a lesser or larger degree, only Thompson, R. T. (1973): Preliminary studies on the two – Curculionini and Rhamphini – being virtually taxonomy and distribution of the melon weevil, cosmopolitan in distribution and Anthonomini , Acythopeus curvirostris (Boheman) (including Baris and Tychiini only absent from the Australo-Pacifi c granulipennis (Tournier)) (Coleoptera, Curculion- region. Acalyptini , Cionini , Ellescini , Mecinini , idae). – Bulletin of Entomological Research 63: 31 – 48. and Smicronychini occur mainly in the Old World, – (1992): Observations on the morphology and clas- from Africa to the Palaearctic and Oriental regions, sifi cation of weevils (Coleoptera, Curculionidae) with Ellescini, Acalyptini, and Smicronychini also with a key to major groups. – Journal of Natural His- extending into the Nearctic region and at least tory 26: 835 – 891. the latter two also into the Australian one. -
Lunar Crater Volcanic Field (Reveille and Pancake Ranges, Basin and Range Province, Nevada, USA)
Research Paper GEOSPHERE Lunar Crater volcanic field (Reveille and Pancake Ranges, Basin and Range Province, Nevada, USA) 1 2,3 4 5 4 5 1 GEOSPHERE; v. 13, no. 2 Greg A. Valentine , Joaquín A. Cortés , Elisabeth Widom , Eugene I. Smith , Christine Rasoazanamparany , Racheal Johnsen , Jason P. Briner , Andrew G. Harp1, and Brent Turrin6 doi:10.1130/GES01428.1 1Department of Geology, 126 Cooke Hall, University at Buffalo, Buffalo, New York 14260, USA 2School of Geosciences, The Grant Institute, The Kings Buildings, James Hutton Road, University of Edinburgh, Edinburgh, EH 3FE, UK 3School of Civil Engineering and Geosciences, Newcastle University, Newcastle, NE1 7RU, UK 31 figures; 3 tables; 3 supplemental files 4Department of Geology and Environmental Earth Science, Shideler Hall, Miami University, Oxford, Ohio 45056, USA 5Department of Geoscience, 4505 S. Maryland Parkway, University of Nevada Las Vegas, Las Vegas, Nevada 89154, USA CORRESPONDENCE: gav4@ buffalo .edu 6Department of Earth and Planetary Sciences, 610 Taylor Road, Rutgers University, Piscataway, New Jersey 08854-8066, USA CITATION: Valentine, G.A., Cortés, J.A., Widom, ABSTRACT some of the erupted magmas. The LCVF exhibits clustering in the form of E., Smith, E.I., Rasoazanamparany, C., Johnsen, R., Briner, J.P., Harp, A.G., and Turrin, B., 2017, overlapping and colocated monogenetic volcanoes that were separated by Lunar Crater volcanic field (Reveille and Pancake The Lunar Crater volcanic field (LCVF) in central Nevada (USA) is domi variable amounts of time to as much as several hundred thousand years, but Ranges, Basin and Range Province, Nevada, USA): nated by monogenetic mafic volcanoes spanning the late Miocene to Pleisto without sustained crustal reservoirs between the episodes. -
Estimated Potentiometric Surface of the Death Valley Regional Groundwater Flow System, Nevada and California by Michael T
U.S. Department of the Interior Prepared in cooperation with the Scientific Investigations Report 2016-5150 U.S. Geological Survey Bureau of Land Management, National Park Service, U.S. Department of Energy National Nuclear Security Administration Sheet 1 (Interagency Agreement DE–AI52–01NV13944), and Office of Civilian Radioactive Waste Management (Interagency Agreement DE–AI28–02RW12167), U.S. Fish and Wildlife Service, and Nye County, Nevada 650000 115° 117° 550000 116° 600000 118° 450000 500000 San Antonio Mts Monte Cristo Range Monitor Range Big Smokey Stone Valley Cabin Grant Range Valley Railroad 1600 Tonopah Valley Quinn Canyon Range Reveille Range 38° 38° Lincoln County Reveille Valley 4200000 4200000 Esmeralda County 1700 1500 1800 1500 Cactus Penoyer Valley Goldfield 00 00 16 Flat 16 (Sand Spring Worthington Range Hill Valley) Nye County 1600 Cactus Range Clayton Valley Stonewall Montezuma Range Flat Kawich Range Timpahute Range Hiko Range Kawich Fish Lake Valley 1700 1500 Gold Valley North Pahranagat Range 1600 Flat Palmetto Mts 1400 Stonewall 1400 4150000 4150000 1500 Mtn 1600 1500 East Pahranagat Range Pahranagat Range 1300 Magruder Mtn Tikaboo Valley Belted Range EmigrantValley Groom Range Last Chance Range 1500 Slate Ridge 1200 1300 Eureka Valley 1200 Pahute 1100 Black Mesa 1100 Mtn 1000 Gold Rainier Eleana 1500 Range Mtn Stonewall Mesa 1000 White Mts Pass Desert Range 900 Halfpint Range Shoshone Yucca 800 Grapevine Mts Flat 1300 Timber Mtn 1500 Sarcobatus Mtn 700 4100000 4100000 1700 Flat 37° 37° 1400 Desert 1600 Valley -
Superposed Compressional and Extensional Strain in Lower Paleozic Rocks of the Northwestern Grant Range, Nevada
AN ABSTRACT OF THE THESIS OF Phyllis A. Camilleri for the degree of Master ofScience in Geology presented on December 15, 1988. Title: Superposed Compressional and Extensional Strain in Lower Paleozoic Rocks in the Northwestern Grant Range, Nevada Redacted for Privacy Abstract approved: Karen Lund The Grant Range, in east-central Nevada, isa north-east trending range bounded on the west bya west-dipping normal fault system. Rocks within therange record a complex polyphase Mesozoic ductile compressional and Cenozoic brittle extensional deformational history. The northwestern Grant Range exposes deformed, regionally metamorphosed and unmetamorphosed, Cambrian to Mississippian carbonate and clastic strata, and minor Tertiary granitic and andesitic dikes. Cambrian and Ordovician rocks are ductilely strained and metamorphosed. Metamorphic grade decreases stratigraphically upwards, generally commensurate with the degree of ductile strain. Two Mesozoic compressional events are recorded in the rocks of the northwestern Grant Range. The first event produced mesoscopic, east-vergent folds with spaced axial-planar cleavage. These folds were overprinted by small-scale, west-vergent thrust faults and folds of the second event. Regional metamorphism began during the first folding event, but outlasted deformation. Static metamorphism was followed by west-vergent deformation, which marked the end of metamorphism. The compressional structures may have been part of an east-vergent anticline or the hanging wall of an east-vergent thrust fault. Ductile Mesozoic compressional structures and fabrics are cut by an arched, imbricate stack of Cenozoic low-angle normal faults of a more brittle character. The low-angle normal faults omit stratigraphic section, and each successively structurally higher fault is generally younger than the one below it. -
STATE of NEVADA Brian Sandoval, Governor
STATE OF NEVADA Brian Sandoval, Governor DEPARTMENT OF WILDLIFE Tony Wasley, Director GAME DIVISION Brian F. Wakeling, Chief Mike Cox, Big Game Staff Biologist Pat Jackson, Carnivore Staff Biologist Cody McKee, Elk Staff Biologist Cody Schroeder, Mule Deer Staff Biologist Peregrine Wolff, Wildlife Health Specialist Western Region Southern Region Eastern Region Regional Supervisors Mike Scott Steve Kimble Tom Donham Big Game Biologists Chris Hampson Joe Bennett Travis Allen Carl Lackey Pat Cummings Clint Garrett Kyle Neill Cooper Munson Matt Jeffress Ed Partee Kari Huebner Jason Salisbury Jeremy Lutz Kody Menghini Tyler Nall Scott Roberts Cover photo credit: Mike Cox This publication will be made available in an alternative format upon request. Nevada Department of Wildlife receives funding through the Federal Aid in Wildlife Restoration. Federal Laws prohibit discrimination on the basis of race, color, national origin, age, sex, or disability. If you believe you’ve been discriminated against in any NDOW program, activity, or facility, please write to the following: Diversity Program Manager or Director U.S. Fish and Wildlife Service Nevada Department of Wildlife 4401 North Fairfax Drive, Mailstop: 7072-43 6980 Sierra Center Parkway, Suite 120 Arlington, VA 22203 Reno, Nevada 8911-2237 Individuals with hearing impairments may contact the Department via telecommunications device at our Headquarters at 775-688-1500 via a text telephone (TTY) telecommunications device by first calling the State of Nevada Relay Operator at 1-800-326-6868. NEVADA DEPARTMENT OF WILDLIFE 2017-2018 BIG GAME STATUS This program is supported by Federal financial assistance titled “Statewide Game Management” submitted to the U.S. -
Geology and Resources of Fluorine in the United States
Geology and Resources of Fluorine in the United States GEOLOGICAL SURVEY PROFESSIONAL PAPER 933 COVER PHOTOGRAPHS 1. Asbestos ore 8. Aluminum ore, bauxite, Georgia 1 2 3 4 2. Lead ore, Balmat mine, N . Y. 9. Native copper ore, Keweenawan 5 6 3. Chromite-chromium ore, Washington Peninsula, Mich. 4. Zinc ore, Friedensville, Pa. 10. Porphyry molybdenum ore, Colorado 7 8 5. Banded iron-formation, Palmer, 11. Zinc ore, Edwards, N. Y. Mich. 12. Manganese nodules, ocean floor 9 10 6. Ribbon asbestos ore, Quebec, Canada 13. Botryoidal fluorite ore, Poncha Springs, Colo. 11 12 13 14 7. Manganese ore, banded rhodochrosite 14. Tungsten ore, North Carolina Geology and Resources of Fluorine in the United States Edited by DANIEL R. SHAWE With sections by D. R. SHAWE, R. E. VAN ALSTINE, R. G. WORL, A. V. HEYL, R. D. TRACE, R. L. PARKER, W. R. GRIFFITTS, C. L. SAINSBURY, and J. B. CATHCART GEOLOGICAL SURVEY PROFESSIONAL PAPER 933 An evaluation of the geochemistry, geographic distribution, and geologic environments of fluorine, and descriptions of major United States fluorine mineral deposits UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 76-600061 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02901-4 APPRAISAL OF MINERAL RESOURCES Continuing appraisal of the mineral resources of the United States is conducted by the U.S. Geological Survey in accordance with the provisions of the Mining and Minerals Policy Act of 1970 (Public Law 91-631, Dec. -
Geology of the Southern Reveille Range, Nye County, Nevada
UNLV Theses, Dissertations, Professional Papers, and Capstones 5-2008 Geology of the southern Reveille Range, Nye County, Nevada Matthew Alan McKelvey University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geology Commons, Stratigraphy Commons, and the Volcanology Commons Repository Citation McKelvey, Matthew Alan, "Geology of the southern Reveille Range, Nye County, Nevada" (2008). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1447. http://dx.doi.org/10.34917/3434676 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. GEOLOGY OF THE SOUTHERN REVEILLE RANGE, NYE COUNTY, NEVADA by Matthew Alan McKelvey Bachelor of Science Austin Peay State University 2001 A thesis submitted in partial fulfillment of the requirements for the Master Degree of Science in Geoscience Department of Geoscience -
Molecular Phylogenetics of the Superfamily Curculionoidea (Insecta: Coleoptera)
Molecular Phylogenetics of the Superfamily Curculionoidea (Insecta: Coleoptera) Conrad Paulus Dias Trafford Gillett A thesis submitted in fulfilment of the requirements for the degree of Doctor of Philosophy University of East Anglia Norwich, Norfolk, England March 2014 © This copy of the thesis has been supplied on condition that anyone who consults it is understood to recognise that its copyright rests with the author and that use of any information derived there-from must be in accordance with current UK Copyright Law. In addition, any quotation or extract must include full attribution. 1 Molecular Phylogenetics of the Superfamily Curculionoidea (Insecta: Coleoptera) Conrad Paulus Dias Trafford Gillett March 2014 Thesis abstract This thesis examines higher-level evolutionary history within the superfamily Curculionoidea, the most speciose family-level taxon, which includes beetles commonly known as weevils. This is achieved using a phylogenetic approach incorporating the largest datamatrix yet employed for weevil molecular systematics, and includes an investigation into the prospect of obtaining short phylogenetically informative amplicons from archival museum specimens. Newly obtained DNA sequence data is analysed from a variety of mitochondrial and nuclear loci, including 92 mitogenomes assembled through the approach of next-generation sequencing of pooled genomic DNA. The resulting trees are used to test previous morphological- and molecular-based hypotheses of weevil relationships and classification schemes. Mitogenomic-derived trees reveal topologies that are highly congruent with previous molecular studies, but that conflict with some morphological hypotheses. Strong nodal support strengthens inferences into the relationships amongst most weevil families and suggests that the largest family, the Curculionidae, is monophyletic, if the subfamily Platypodinae is excluded. -
Coleoptera: Curculionidae1
Pacific Insects Monograph 27: 225-259 10 November 1971 ENTOMOLOGY OF THE AUCKLANDS AND OTHER ISLANDS SOUTH OF NEW ZEALAND: COLEOPTERA: CURCULIONIDAE1 By G. Kuschel2 Abstract: This is a supplementary report to that published on the Curculionidae from Auckland, Campbell, Antipodes, and Snares Islands (no species are known from Bounty or Macquarie) and is based on some 2000 additional specimens collected during further trips to the islands. The native fauna now contains 17 genera and 35 species belonging to 9 subfamilies; 4 genera (23.53%) and 21 species (60.0%) being endemic. All genera and species have their closest relatives in the New Zealand mainland. A significant fact is that none of the true wood borers, flower dwellers, or leaf miners is endemic, and that the larvae of all the endemic species live either in the soil (76.33%) or in decaying plants (23.67%). Further discussions on the composition of the fauna are presented. The fauna is also compared with that of other cold-temperate areas of the southern hemisphere. Apart from a general key to the genera, separate keys to the species are given for the Aucklands, Campbell, and the Snares. A few nomenclatural changes were necessary after an examination of some type material previously not available. INTRODUCTION Since the last paper on the subantarctic weevil fauna was published (Kuschel 1964) further parties to several islands have obtained some 2000 additional specimens which included four new species. I had the opportunity of participating in trips to Adams I, South of Auckland I, Campbell I, and Antipodes I. My primaiy object was to find out a little more about the environmental con ditions and feeding habits of each species as well as to gather large amounts of leaf litter, swards, mats, and cushion plants for the extraction of the ground and soil fauna, and some wood samples for rearing the wood borers and their associates.