Investigators' Annual Reports Yellowstone
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Developing a Genetic Manipulation System for the Antarctic Archaeon, Halorubrum Lacusprofundi: Investigating Acetamidase Gene Function
www.nature.com/scientificreports OPEN Developing a genetic manipulation system for the Antarctic archaeon, Halorubrum lacusprofundi: Received: 27 May 2016 Accepted: 16 September 2016 investigating acetamidase gene Published: 06 October 2016 function Y. Liao1, T. J. Williams1, J. C. Walsh2,3, M. Ji1, A. Poljak4, P. M. G. Curmi2, I. G. Duggin3 & R. Cavicchioli1 No systems have been reported for genetic manipulation of cold-adapted Archaea. Halorubrum lacusprofundi is an important member of Deep Lake, Antarctica (~10% of the population), and is amendable to laboratory cultivation. Here we report the development of a shuttle-vector and targeted gene-knockout system for this species. To investigate the function of acetamidase/formamidase genes, a class of genes not experimentally studied in Archaea, the acetamidase gene, amd3, was disrupted. The wild-type grew on acetamide as a sole source of carbon and nitrogen, but the mutant did not. Acetamidase/formamidase genes were found to form three distinct clades within a broad distribution of Archaea and Bacteria. Genes were present within lineages characterized by aerobic growth in low nutrient environments (e.g. haloarchaea, Starkeya) but absent from lineages containing anaerobes or facultative anaerobes (e.g. methanogens, Epsilonproteobacteria) or parasites of animals and plants (e.g. Chlamydiae). While acetamide is not a well characterized natural substrate, the build-up of plastic pollutants in the environment provides a potential source of introduced acetamide. In view of the extent and pattern of distribution of acetamidase/formamidase sequences within Archaea and Bacteria, we speculate that acetamide from plastics may promote the selection of amd/fmd genes in an increasing number of environmental microorganisms. -
The Newsletter of the CMC Pikes Peak Group
August 2017 | No. 237 The Newsletter of the CMC Pikes Peak Group Member Contributions BARR CAMP RENOVATION COMPLETED LA PLATA TRIP, JUNE 24 By Dean Waits By David Kuenzli L-R: Dan Hildebrand, Andrea Torske, William Musser, Robin Mino, Brad Sherman, Krista Scott, and Barbara Newsome. Trip leader David Kuenzli behind the camera. If you’ve recently hiked to Barr Camp you would have noticed a lot of new construction activity. A new foundation was GOOSE CREEK TRAIL – SHAFT HOUSE TRIP, JULY 1 installed under the log cabin structure Fred Barr completed in By Carol Schmitz 1924, along with a new composite porch and some new bridges that now allow the caretakers to safely retrieve supplies from the Mountain View storage. The project has now been completed. Your Pikes Peak Group helped preserve and renovate this historical icon by making a $1,000 donation. If you haven’t made a trip to either spend the night or just for the exercise, it’s a wonderful six-mile adventure. L-R: Gary Marx, Barb Gutow, Jo Anne Peterson, Erika Lefstad (Denver group), Sherry Scott, Carol Schmitz (leader), Susan Gerdes, Bryan Scott. 1 Welcome New PPG Members! Your PPG Council Jonathan Huang Matthew Triplett Taylor Lindsey Samuel Woods Chair – Collin Powers Jo Anne Peterson 719-963-0653, [email protected] Past Chair – Rick Keetch 719-634-1165, [email protected] Summer 2017 Stewardship Schedule ARCPro Co-Directors – Collin Powers 719-685-2470, [email protected]; Scott Kime, 719-235-0939, This summer the CMC has four stewardship projects scheduled in [email protected] coordination with the Pike National Forest. -
Microbial (Per)Chlorate Reduction in Hot Subsurface Environments
Microbial (Per)chlorate Reduction in Hot Subsurface Environments Martin G. Liebensteiner Thesis committee Promotor Prof. Dr Alfons J.M. Stams Personal chair at the Laboratory of Microbiology Wageningen University Co-promotor Dr Bart P. Lomans Principal Scientist Shell Global Solutions International B.V., Rijswijk Other members Prof. Dr Willem J.H. van Berkel, Wageningen University Prof. Dr Mike S.M. Jetten, Radboud University Nijmegen Prof. Dr Ian Head, Newcastle University, UK Dr Timo J. Heimovaara, Delft University of Technology This research was conducted under the auspices of the Graduate School for Socio-Economic and Natural Sciences of the Environment (SENSE) Microbial (Per)chlorate Reduction in Hot Subsurface Environments Martin G. Liebensteiner Thesis submitted in fulfi lment of the requirements for the degree of doctor at Wageningen University by the authority of the Rector Magnifi cus Prof. Dr M.J. Kropff, in the presence of the Thesis Committee appointed by the Academic Board to be defended in public on Friday 17 October 2014 at 4 p.m. in the Aula. Martin G. Liebensteiner Microbial (Per)chlorate Reduction in Hot Subsurface Environments 172 pages. PhD thesis, Wageningen University, Wageningen, NL (2014) With references, with summaries in Dutch and English ISBN 978-94-6257-125-9 TABLE OF CONTENTS Chapter 1 General introduction and thesis outline 7 Chapter 2 Microbial redox processes in deep subsurface environments 23 and the potential application of (per)chlorate in oil reservoirs Chapter 3 (Per)chlorate reduction by the hyperthermophilic -
Highwood Mountains Range Analysis Project Area on Those Resources Affected by Implementation
United States Department of Agriculture Environmental Forest Service Assessment 2015 Highwood Mountains Range Judith Ranger District, Lewis and Clark National Forest Cascade, Choteau and Judith Basin Counties, Montana For More Information Contact: Lewis and Clark National Forest Judith Ranger District Standford, Montana www.fs.fed.us/r1/lewisclark/projects 406-566-2292. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TTY). To file a complaint of discrimination, write to USDA, Director, Office of Civil Rights, 1400 Independence Avenue, SW., Washington, DC 20250-9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TTY). USDA is an equal opportunity provider and employer. Environmental Assessment Table of Contents Introduction ...................................................................................................................................................4 Location of the Proposed Project Area ..........................................................................................................4 -
Yellowstone National Park Geologic Resource Evaluation Scoping
Geologic Resource Evaluation Scoping Summary Yellowstone National Park This document summarizes the results of a geologic resource evaluation scoping session that was held at Yellowstone National Park on May 16–17, 2005. The NPS Geologic Resources Division (GRD) organized this scoping session in order to view and discuss the park’s geologic resources, address the status of geologic maps and digitizing, and assess resource management issues and needs. In addition to GRD staff, participants included park staff and cooperators from the U.S. Geological Survey and Colorado State University (table 1). Table 1. Participants of Yellowstone’s GRE Scoping Session Name Affiliation Phone E-Mail Bob Volcanologist, USGS–Menlo Park 650-329-5201 [email protected] Christiansen Geologist/GRE Program GIS Lead, NPS Tim Connors 303-969-2093 [email protected] Geologic Resources Division Data Stewardship Coordinator, Greater Rob Daley 406-994-4124 [email protected] Yellowstone Network Supervisory Geologist, Yellowstone Hank Heasler 307-344-2441 [email protected] National Park Geologist, NPS Geologic Resources Bruce Heise 303-969-2017 [email protected] Division Cheryl Geologist, Yellowstone National Park 307-344-2208 [email protected] Jaworowski Katie Geologist/Senior Research Associate, 970-586-7243 [email protected] KellerLynn Colorado State University Branch Chief, NPS Geologic Resources Carol McCoy 303-969-2096 [email protected] Division Ken Pierce Surficial Geologist, USGS–Bozeman 406-994-5085 [email protected] Supervisory GIS Specialist, Yellowstone Anne Rodman 307-344-7381 [email protected] National Park Shannon GIS Specialist, Yellowstone National Park 307-344-7381 [email protected] Savage Monday, May 16, involved a welcome to Yellowstone National Park and an introduction to the Geologic Resource Evaluation (GRE) Program, including status of reports and digital maps. -
Foundation Document Overview Yellowstone National Park Wyoming, Montana, Idaho
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Yellowstone National Park Wyoming, Montana, Idaho Contact Information For more information about the Yellowstone National Park Foundation Document, contact: [email protected] or 307-344-7381 or write to: Superintendent, Yellowstone National Park, PO Box 168, Yellowstone National Park, WY 82190-0168 Park Description Yellowstone became the world’s first national park on March This vast landscape contains the headwaters of several major 1, 1872, set aside in recognition of its unique hydrothermal rivers. The Firehole and Gibbon rivers unite to form the Madison, features and for the benefit and enjoyment of the people. which, along with the Gallatin River, joins the Jefferson to With this landmark decision, the United States Congress create the Missouri River several miles north of the park. The created a path for future parks within this country and Yellowstone River is a major tributary of the Missouri, which around the world; Yellowstone still serves as a global then flows via the Mississippi to the Gulf of Mexico. The Snake resource conservation and tourism model for public land River arises near the park’s south boundary and joins the management. Yellowstone is perhaps most well-known for its Columbia to flow into the Pacific. Yellowstone Lake is the largest hydrothermal features such as the iconic Old Faithful geyser. lake at high altitude in North America and the Lower Yellowstone The park encompasses 2.25 million acres, or 3,472 square Falls is the highest of more than 40 named waterfalls in the park. miles, of a landscape punctuated by steaming pools, bubbling mudpots, spewing geysers, and colorful volcanic soils. -
Bedrock Geology of the Southern Part of Tom Miner Basin Park and Gallatin Counties Montana
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1969 Bedrock geology of the southern part of Tom Miner Basin Park and Gallatin counties Montana Stanley Glenn Todd The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Todd, Stanley Glenn, "Bedrock geology of the southern part of Tom Miner Basin Park and Gallatin counties Montana" (1969). Graduate Student Theses, Dissertations, & Professional Papers. 6080. https://scholarworks.umt.edu/etd/6080 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. ss’i'S ' In presenting this thesis in partial fulfillment of the require^ ments for an advanced degree at Mont.' "a State University, I agree that the Library shall make it freely available for inspection. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by my major professor, or, in his absence, by the Director of Libraries, It is understood that any copying or publica tion of this thesis for financial gain shall not be allowed without mjr written permission. signature Date n ^ . S, ______________ -
COPYRIGHTED MATERIAL COPYRIGHTED I
Avalanche Campground (MT), 66 Big Horn Equestrian Center (WY), Index Avenue of the Sculptures (Billings, 368 MT), 236 Bighorn Mountain Loop (WY), 345 Bighorn Mountains Trail System INDEX A (WY), 368–369 AARP, 421 B Bighorn National Forest (WY), 367 Absaroka-Beartooth Wilderness Backcountry camping, Glacier Big Red (Clearmont, WY), 370 (MT), 225–227 National Park (MT), 68 Big Red Gallery (Clearmont, WY), Academic trips, 44–45 Backcountry permits 370 Accommodations, 413–414 Glacier National Park (MT), Big Salmon Lake (MT), 113 best, 8–10 54–56 Big Sheep Creek Canyon (MT), 160 for families with children, 416 Grand Teton (WY), 325 Big Sky (MT), 8, 215–220 Active vacations, 43–52 Yellowstone National Park Big Sky Brewing Company AdventureBus, 45, 269 (MT—WY), 264 (Missoula, MT), 93 Adventure Sports (WY), 309, 334 Backcountry Reservations, 56 Big Sky Candy (Hamilton, MT), 96 Adventure trips, 45–46 Backcountry skiing, 48 Big Sky Golf Course (MT), 217 AdventureWomen, 201–202 Backroads, 45, 46 Big Sky Resort (MT), 216–217 Aerial Fire Depot and Baggs (WY), 390 Big Sky Waterpark (MT), 131 Smokejumper Center (Missoula, Ballooning, Teton Valley (WY), Big Spring (MT), 188 MT), 86–87 306 Big Spring Creek (MT), 187 Air tours Bannack (MT), 167, 171–172 Big Timber Canyon Trail (MT), 222 Glacier National Park (MT), 59 Bannack Days (MT), 172 Biking and mountain biking, 48 the Tetons (WY), 306 Barry’s Landing (WY), 243 Montana Air travel, 409, 410 Bay Books & Prints (Bigfork, MT), Big Sky, 216 Albright Visitor Center 105 Bozeman, 202 (Yellowstone), 263, 275 -
Polygonaceae of Alberta
AN ILLUSTRATED KEY TO THE POLYGONACEAE OF ALBERTA Compiled and writen by Lorna Allen & Linda Kershaw April 2019 © Linda J. Kershaw & Lorna Allen This key was compiled using informaton primarily from Moss (1983), Douglas et. al. (1999) and the Flora North America Associaton (2005). Taxonomy follows VAS- CAN (Brouillet, 2015). The main references are listed at the end of the key. Please let us know if there are ways in which the kay can be improved. The 2015 S-ranks of rare species (S1; S1S2; S2; S2S3; SU, according to ACIMS, 2015) are noted in superscript (S1;S2;SU) afer the species names. For more details go to the ACIMS web site. Similarly, exotc species are followed by a superscript X, XX if noxious and XXX if prohibited noxious (X; XX; XXX) according to the Alberta Weed Control Act (2016). POLYGONACEAE Buckwheat Family 1a Key to Genera 01a Dwarf annual plants 1-4(10) cm tall; leaves paired or nearly so; tepals 3(4); stamens (1)3(5) .............Koenigia islandica S2 01b Plants not as above; tepals 4-5; stamens 3-8 ..................................02 02a Plants large, exotic, perennial herbs spreading by creeping rootstocks; fowering stems erect, hollow, 0.5-2(3) m tall; fowers with both ♂ and ♀ parts ............................03 02b Plants smaller, native or exotic, perennial or annual herbs, with or without creeping rootstocks; fowering stems usually <1 m tall; fowers either ♂ or ♀ (unisexual) or with both ♂ and ♀ parts .......................04 3a 03a Flowering stems forming dense colonies and with distinct joints (like bamboo -
Map Showing Geology, Structure, and Geophysics of the Central Black
U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the SCIENTIFIC INVESTIGATIONS MAP 2777 U.S. GEOLOGICAL SURVEY SOUTH DAKOTA SCHOOL OF MINES AND TECHNOLOGY FOUNDATION SHEET 2 OF 2 Pamphlet accompanies map 104°00' 103°30' 103°00' 104°00' 103°30' 103°00' ° ° EXPLANATION FOR MAPS F TO H 44 30' 44°30' EXPLANATION 44 30' 44°30' EXPLANATION Spearfish Geologic features 53 54 Tertiary igneous rocks (Tertiary and post-Tertiary Spearfish PHANEROZOIC ROCKS 90 1 90 sedimentary rocks not shown) Pringle fault 59 Tertiary igneous rocks (Tertiary and post-Tertiary Pre-Tertiary and Cretaceous (post-Inyan Kara sedimentary rocks not shown) Monocline—BHM, Black Hills monocline; FPM, Fanny Peak monocline 52 85 Group) rocks 85 Sturgis Sturgis Pre-Tertiary and Cretaceous (post-Inyan Kara A Proposed western limit of Early Proterozoic rocks in subsurface 55 Lower Cretaceous (Inyan Kara Group), Jurassic, Group) rocks 57 58 60 14 and Triassic rocks 14 Lower Cretaceous (Inyan Kara Group), Jurassic, B Northern extension (fault?) of Fanny Peak monocline and Triassic rocks Paleozoic rocks C Possible eastern limit of Early Proterozoic rocks in subsurface 50 Paleozoic rocks Precambrian rocks S Possible suture in subsurface separating different tectonic terranes 89 51 89 2 PRECAMBRIAN ROCKS of Sims (1995) 49 Contact St 3 G Harney Peak Granite (unit Xh) Geographic features—BL, Bear Lodge Mountains; BM, Bear Mountain; Fault—Dashed where approximately located G DT DT, Devils Tower 48 B Early Proterozoic rocks, undivided Anticline—Showing trace of axial surface and 1 St Towns and cities—B, Belle Fourche; C, Custer; E, Edgemont; HS, Hot direction of plunge. -
Description of the Fort Benton Quadrangle
DESCRIPTION OF THE FORT BENTON QUADRANGLE. INTRODUCTION. steeply inclined sides. In the center of the range of the throat of a volcano, the dikes which radiate heat and cold, varying greatly, of course, with the the limestones and other stratified rocks are hori from these centers of activity, and the loose mate altitude. The annual rainfall is from 13 to 20 General relations. The Fort Benton quad zontal, or nearly so, while on the flanks structure of rials and lava flows of which the cones Structure_. , of. inches, being greatest in the mountains; June and rangle extends in longitude from 110° to 111° of the mountains they are sharply BheuLMoun- were built. The sedimentary strata October are the rainy months. The snowfall is and in latitude from 47° to 48°. It is inclined and dip away from the moun through which the volcanoes broke up heavy and the mountain tracts are well watered. 69.25 miles Ions; from north to south. extent°ofan tains to the lower plains country. The horizontal and upon which their materials accumulated are, Agriculture is therefore confined to the foothills . quadrangle. 47.36 miles wide, and contains 3272.7 attitude is well shown in the rocks of Belt Park, over most of the area, nearly horizontal or inclined and stream bottoms, except where irrigation is square miles. It includes part of Choteau, the whereas farther north the mountain masses near gently to the north. These rocks belong entirely possible. northwest corner of Fergus, and the eastern part Monarch are formed of blocks of tilted limestones to the Cretaceous system, and denudation has Culture. -
Population Viability of Arctic Grayling in the Gibbon River, Yellowstone National Park
North American Journal of Fisheries Management 30:1582–1590, 2010 [Article] Ó Copyright by the American Fisheries Society 2010 DOI: 10.1577/M10-083.1 Population Viability of Arctic Grayling in the Gibbon River, Yellowstone National Park 1 AMBER C. STEED* Montana Cooperative Fishery Research Unit and Department of Ecology, Montana State University, Post Office Box 173460, Bozeman, Montana 59717, USA ALEXANDER V. ZALE U.S. Geological Survey, Montana Cooperative Fishery Research Unit, and Department of Ecology, Montana State University, Post Office Box 173460, Bozeman, Montana 59717, USA TODD M. KOEL Fisheries and Aquatic Sciences Program, Yellowstone Center for Resources, Post Office Box 168, Yellowstone National Park, Wyoming 82190, USA STEVEN T. KALINOWSKI Department of Ecology, Montana State University, Post Office Box 172460, Bozeman, Montana 59717, USA Abstract.—The fluvial Arctic grayling Thymallus arcticus is restricted to less than 5% of its native range in the contiguous United States and was relisted as a category 3 candidate species under the U.S. Endangered Species Act in 2010. Although fluvial Arctic grayling of the lower Gibbon River, Yellowstone National Park, Wyoming, were considered to have been extirpated by 1935, anglers and biologists have continued to report catching low numbers of Arctic grayling in the river. Our goal was to determine whether a viable population of fluvial Arctic grayling persisted in the Gibbon River or whether the fish caught in the river were downstream emigrants from lacustrine populations in headwater lakes. We addressed this goal by determining relative abundances, sources, and evidence for successful spawning of Arctic grayling in the Gibbon River.