MODELING SUBSISTENCE and DEMOGRAPHIC CHANGE in LATE-HOLOCENE OCCUPATIONS of HOUSEPIT 54 at the BRIDGE RIVER SITE (Eerl4), MID-FRASER, B.C
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Mammals of the California Desert
MAMMALS OF THE CALIFORNIA DESERT William F. Laudenslayer, Jr. Karen Boyer Buckingham Theodore A. Rado INTRODUCTION I ,+! The desert lands of southern California (Figure 1) support a rich variety of wildlife, of which mammals comprise an important element. Of the 19 living orders of mammals known in the world i- *- loday, nine are represented in the California desert15. Ninety-seven mammal species are known to t ':i he in this area. The southwestern United States has a larger number of mammal subspecies than my other continental area of comparable size (Hall 1981). This high degree of subspeciation, which f I;, ; leads to the development of new species, seems to be due to the great variation in topography, , , elevation, temperature, soils, and isolation caused by natural barriers. The order Rodentia may be k., 2:' , considered the most successful of the mammalian taxa in the desert; it is represented by 48 species Lc - occupying a wide variety of habitats. Bats comprise the second largest contingent of species. Of the 97 mammal species, 48 are found throughout the desert; the remaining 49 occur peripherally, with many restricted to the bordering mountain ranges or the Colorado River Valley. Four of the 97 I ?$ are non-native, having been introduced into the California desert. These are the Virginia opossum, ' >% Rocky Mountain mule deer, horse, and burro. Table 1 lists the desert mammals and their range 1 ;>?-axurrence as well as their current status of endangerment as determined by the U.S. fish and $' Wildlife Service (USWS 1989, 1990) and the California Department of Fish and Game (Calif. -
Complement Fixation Tests for Murine Typhus
ice under glass seal. The animals' brains were Complement Fixation Tests removed for tissue infectivity tests and were also stored on dry ice. Tests of the tissues of For Murine Typhus serologically reactive animals and pools of their fleas aided in evaluating the significance of low On Small Mammals titers. Blood samples were obtained by cardiac By RUTH KEATON, B.S. puncture soon after capture of the animals. BILLIE JO NASH, B.A. Serums were separated aseptically and were J. N. MURPHY, JR., M.A., M.S.P.H. kept at ice-box temperature until examination. J. V. IRONS, Sc.D. Serums were inactivated 30 minutes immedi- ately before testing at 56° C. Each serum was subjected to a quantitative complement tT HE IMPORTANCE of commensal rats fixation test employing endemic typhus rick- and their fleas in the epidemiology of en- ettsiae. A slight modification of the pro- demic typhus was well establislhed in 1931 (1,2). cedure described by Brigham and Bensgton Following Dyer's report (3) on the experi- (11) was used. The result was recorded as mental infection of the woodchuck, meadow reactive when a 3 + or greater reaction was ob- mouse, and whitefooted mouse with endemic tained with satisfactory controls at a 1: 20 or tvphus, Brigham (4, 5) indicated that many greater dilution of serum. species of rodents and other mammals were ap- When a serum was reactive, the correspond- parently susceptible to endemic typhus. Spar- ing brain suspension was emulsified and inocu- row (6) recovered a strain of endemic typhus lated individually into hamsters for evidence of rickettsiae in the house mouse (.Mus musodus), typhus. -
Paleontological Resources of the Upper and Middle San Pedro Valley
Paleontological Resources of the Upper and Middle San Pedro Valley Robert D. McCord Arizona Museum of Natural History Geological setting Regional extension causing block faulting – creation of the Basin and Range ~15Ma Poorly developed drainage results in lakes in valley bottom ?-3.4 Ma Drainage develops with flow to north, marshes, ponds and lakes significant from time to time Early Pleistocene Saint David Formation ? – 3.4 million lakes, few fossils Well developed paleomagnetic timeframe – a first for terrestrial sediments! Succession of faunas from ~3 to 1.5 Ma Blancan to ? Irvingtonian NALMA Plants diatoms charophytes Equisetum (scouring rush) Ostracoda (aquatic crustaceans) Cypridopsis cf. vidua Limnocythere cf. staplini Limnocythere sp. Candona cf. renoensis Candona sp. A Candona sp. B ?Candonlella sp. ?Heterocypris sp. ?Cycloypris sp. Potamocypris sp. Cyprideis sp. Darwinula sp. Snails and a Clam Pisidium casertanum (clam) Fossaria dalli (aquatic snail) Lymnaea caperata (aquatic snail) Lymnaea cf. elodes (aquatic snail) Bakerilymnaea bulimoides (aquatic snail) Gyraulus parvus (aquatic snail) Promenetus exacuous (aquatic snail) Promenetus umbilicatellus (aquatic snail) Physa virgata (aquatic snail) Gastrocopta cristata (terrestrial snail) Gastrocopta tappaniana (terrestrial snail) Pupoides albilabris (terrestrial snail) Vertigo milium (terrestrial snail) Vertigo ovata (terrestrial snail) cf. Succinea (terrestrial snail) Deroceras aenigma (slug) Hawaila minuscula (terrestrial snail) Fish and Amphibians indeterminate small fish Ambystoma tigrinum (tiger salamander) Scaphiopus hammondi (spadefoot toad) Bufo alvarius (toad) Hyla eximia (tree frog) Rana sp. (leopard frog) Turtles and Lizards Kinosternon arizonense (mud turtle) Terrapene cf. ornata (box turtle) Gopherus sp. (tortoise) Hesperotestudo sp. (giant tortoise) Eumeces sp. (skink) “Cnemidophorus” sp. (whiptail lizard) Crotaphytus sp. (collared lizard) Phrynosoma sp. (horned lizard) Sceloporus sp. -
Reconstruction of Mid Wisconsin Environments in Southern New Mexico
Articles Arthur H. Harris Reconstruction of Mid Wisconsin Environments in Southern New Mexico Abundant vertebrate remains from two mid-Wisconsin cave deposits in New Mexico allow reconstruction of paleoenvironments. Dry Cave lies in southeastern New Mexico, U-Bar Cave in the extreme southwest (Figure 1). Both sites are in the ecotone between woodland and Chihuahuan Desert vegetations. During the mid Wisconsin, both had vertebrate species indicative of woodland, but otherwise differed greatly. Dry Cave had winter temperatures milder than those at the site today, but otherwise the climate was similar to that now found some 450 km to the north. Except for taxa allowed into the area by mild winters, extralimital forms occur in nearby highland woodlands or in northeastern New Mexico. U-Bar Cave probably lacked winter freezes, had cool summers, and had precipitation more evenly distributed than now. Taxa now as distant as the Great Basin occurred together with species from the nearer highlands. Relatively warm summers and retention of seasonal patterns of precipitation at Dry Cave in contrast to cool summers and decreased seasonality of precipitation at U-Bar Cave produced more extreme biotic differences between the sites than is the case now. Whether this was due to different contemporaneous climatic regimes or to chronological differences between the faunas is uncertain. The last major subdivision of the Pleistocene Epoch is the Wisconsin Age. Between ice advances in the early Wisconsin, terminating around 60 000 B.P., and a major renewal of glacial activity in the late Wisconsin, commencing around 32 000 to 27 000 B. P., there was a long span of less severe climatic conditions, the mid Wisconsin (see Bradley 1985 for age estimates). -
Pack Rats (Neotoma Spp.): Keystone Ecological Engineers?
Journal of Arid Environments 74 (2010) 1450e1455 Contents lists available at ScienceDirect Journal of Arid Environments journal homepage: www.elsevier.com/locate/jaridenv Pack rats (Neotoma spp.): Keystone ecological engineers? Walter G. Whitford a, Yosef Steinberger b,* a USDA-ARS Jornada Experimental Range, MSC 3JER, New Mexico State University, Las Cruces, NM 88003, USA b The Mina & Everard Goodman, The Mina & Everard Goodman Faculty of Life Sciences, Bar-Ilan University, Ramat-Gan 52900, Israel article info abstract Article history: The potential role of two species of pack rats (Neotoma albigula and Neotoma micropus) as keystone Received 8 December 2009 ecological engineers was examined by estimating the species diversity of invertebrates living in the nest Received in revised form middens, and nitrogen mineralization rates in soils associated with the middens. Although pack-rat 15 April 2010 middens in tarbush (Flourensia cernua) shrublands were smaller than those in creostebush (Larrea tri- Accepted 21 May 2010 dentata) shrublands, they housed a higher abundance and diversity of arthropods. The Neotoma spp. Available online 15 June 2010 middens were an important microhabitat for crickets (Gryllus sp.), wolf spiders (Lycosa spp.), and lycid beetle larvae (Lycidae) in all of the shrub habitats. There were five arthropod taxa that occupied all Keywords: Habitat middens in the creosote-bush shrubland, and 12 arthropod taxa that occupied all middens in the tarbush fi Mineralization shrubland. Soils associated with pack-rat middens had signi cantly higher soil organic-matter content Species diversity than reference soils. Nitrogen mineralization was significantly higher in soils associated with pack-rat Stick nest middens than in reference soils. -
Effects of Pleistocene Environmental Changes on the Distribution and Community Structure of the Mammalian Fauna of Mexico
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/220048614 Effects of Pleistocene environmental changes on the distribution and community structure of the mammalian fauna of Mexico Article in Quaternary Research · May 2010 DOI: 10.1016/j.yqres.2010.02.006 CITATIONS READS 51 350 3 authors: Gerardo Ceballos Joaquin Arroyo-Cabrales Universidad Nacional Autónoma de México Instituto Nacional de Antropología e Historia 285 PUBLICATIONS 9,624 CITATIONS 252 PUBLICATIONS 1,903 CITATIONS SEE PROFILE SEE PROFILE Eduardo Ponce Universidad Nacional Autónoma de México 15 PUBLICATIONS 146 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Peces del Estado de México View project Placement of Myotis planiceps within the Myotis phylogeny View project All content following this page was uploaded by Gerardo Ceballos on 01 May 2019. The user has requested enhancement of the downloaded file. Quaternary Research 73 (2010) 464–473 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres Effects of Pleistocene environmental changes on the distribution and community structure of the mammalian fauna of Mexico Gerardo Ceballos a, Joaquín Arroyo-Cabrales b,⁎, Eduardo Ponce a a Instituto de Ecología, UNAM, Apdo. Postal 70-275; México D.F. 04510, Mexico b Subdirección de Laboratorios y Apoyo Académico, INAH, Moneda # 16, Col. Centro, 06060 México, D.F, Mexico article info abstract Article history: Biological communities in Mexico experienced profound changes in species composition and structure as a Received 22 June 2008 consequence of the environmental fluctuations during the Pleistocene. Based on the recent and fossil Available online 7 April 2010 Mexican mammal checklists, we determine the distribution, composition, diversity, and community structure of late Pleistocene mammalian faunas, and analyze extinction patterns and response of individual Keywords: species to environmental changes. -
The Archive of Place 00Front.Qxd 4/27/2007 6:48 AM Page Ii
00front.qxd 4/27/2007 6:48 AM Page i The Archive of Place 00front.qxd 4/27/2007 6:48 AM Page ii The Nature | History | Society series is devoted to the publication of high-quality scholarship in environmental history and allied fields. Its broad compass is signalled by its title: nature because it takes the natural world seriously; history because it aims to foster work that has temporal depth; and society because its essential concern is with the interface between nature and society, broadly conceived. The series is avowedly interdisciplinary and is open to the work of anthropologists, ecologists, historians, geographers, literary scholars, political scientists, sociologists, and others whose interests resonate with its mandate. It offers a timely outlet for lively, innovative, and well-written work on the interaction of people and nature through time in North America. General Editor: Graeme Wynn, University of British Columbia Claire Elizabeth Campbell, Shaped by the West Wind: Nature and History Tina Loo, States of Nature: Conserving Canada’s Wildlife in the Twentieth Century Jamie Benidickson, The Culture of Flushing: A Social and Legal History of Sewage John Sandlos, Hunters at the Margin: Native People and Wildlife Conservation in the Northwest Territories James Murton, Creating a Modern Countryside: Liberalism and Land Resettlement in British Columbia 00front.qxd 4/27/2007 6:48 AM Page iii The Archive of Place Unearthing the Pasts of the Chilcotin Plateau . UBC Press • Vancouver • Toronto 00front.qxd 4/27/2007 6:48 AM Page iv © UBC Press All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, without prior written permission of the publisher, or, in Canada, in the case of photocopying or other reprographic copying, a licence from Access Copyright (Canadian Copyright Licensing Agency), www.accesscopyright.ca. -
SFU Library Thesis Template
Bedrock Structural Influences on River Morphology by Michael J. Curran BA, Colorado College, 2013 Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Geography Faculty of Environment © Michael Curran 2020 SIMON FRASER UNIVERSITY Spring 2020 Copyright in this work rests with the author. Please ensure that any reproduction or re-use is done in accordance with the relevant national copyright legislation. Approval Name: Michael Curran Degree: Master of Science Title: Bedrock Structural Influences on River Morphology Examining Committee: Chair: Rosemary Collard Assistant Professor Jeremy G. Venditti Senior Supervisor Professor John J. Clague Supervisor Professor Emeritus Doug Stead Supervisor Professor Allison Pfeiffer External Examiner Assistant Professor Department of Geology Western Washington University Date Defended/Approved: April 16, 2020 ii Abstract Bedrock rivers largely set the pace for landscape evolution in unglaciated terrain and yet little is known about what controls their morphologies. I examine the role that geologic structure plays in the alignment and morphology of bedrock canyons at different scales. At the watershed scale, I examine the striking alignment of the Fraser River with the Fraser River Fault zone and its largely unmapped secondary fault structures. I explore how large sediment inputs affect bedrock canyons alignment and their morphological characteristics. At the reach scale, I investigate how geological structure influences bedrock canyon width. I find that width constrictions coincide with dominant sub- horizontal joint sets whereas widenings coincide with dominant sub-vertical joint sets. I consider this in the context of sequential constrictions and widenings and propose a conceptual model where sub-vertical jointing makes canyon walls more susceptible to failure due to river undercutting than horizontal jointing. -
Northwest Anthropological Research Notes
ISSN 1538-2834 JOURNAL OF NORTHWEST ANTHROPOLOGY A Collection of Papers from the Journal of Northwest Anthropology Associated with Traditional Indigenous Resources Part 2: Aquatic Spring 2011 Electronic Edition JOURNAL OF NORTHWEST ANTHROPOLOGY FORMERLY NORTHWEST ANTHROPOLOGICAL RESEARCH NOTES EDITORS Roderick Sprague Darby C. Stapp Deward E. Walker, Jr. South Fork Press Richland, WA University of Colorado ASSOCIATE EDITORS C. Melvin Aikens (University of Oregon), Haruo Aoki (University of California), Virginia Bevert (Yakama Tribe), Don E. Dumond (University of Oregon), Don D. Fowler (University of Nevada), Raymond D. Fogelson (University of Chicago), Rodney Frey (University of Idaho), Ronald Halfmoon (Lapwai), Tom F. S. McFeat (University of Toronto), and Jay Miller (Lushootseed Research). Julia G. Longenecker Operations Manager Kara N. Powers Editorial Assistant Diana C. Stapp Editorial Assistant Composed by South Fork Press, Moscow; Printed by Copy Court, Moscow; Bound by Arts & Crafts, Oakesdale. Missing issue claim limit 18 months. For back issues and catalogue of prices contact Coyote Press, P O Box 3377, Salinas, CA 93912. <http://www.californiaprehistory.com>. POLICY Journal of Northwest Anthropology, published semiannually by NARN, Inc. a non-profit organization in Richland, Washington, is a refereed journal and welcomes contributions of professional quality dealing with anthropological research in northwestern North America. Regular issues are published semiannually with additional memoirs issued as funds are available. Theoretical and interpretive studies and bibliographic works are preferred, although highly descriptive studies will be considered if they are theoretically significant. The primary criterion guiding selection of papers will be how much new research they can be expected to stimulate or facilitate. SUBSCRIPTIONS The subscription price is $40.00 U.S. -
The Reproductive Biology of Steelhead (Oncorhynchus Mykiss) in the Bridge and Seton Rivers, As Determined by Radio Telemetry 1996/97 and 1998/99
The Reproductive Biology of Steelhead (Oncorhynchus mykiss) in the Bridge and Seton Rivers, As Determined by Radio Telemetry 1996/97 and 1998/99 Prepared for: The Ministry of Environment, Lands & Parks Fisheries Branch, Southern Interior Region 1259 Dalhousie Dr. Kamloops, BC V2C 5Z5 Prepared by: Stacy Webb, Robert Bison, Al Caverly and Jim Renn Abstract The 1996/97 and 1998/99 studies of the spawning migrations of Bridge and Seton River steelhead were part of a larger study investigating the migration behaviour and stock composition of interior Fraser River steelhead. Steelhead were radio-tagged in the fall of 1996 and 1998 in the Lower Fraser River and in the winter/spring of 1997 and 1999 in the Middle Fraser River. Tagging effort was concentrated at the Seton/Fraser River confluence during the winter/spring captures, specifically to study Bridge and Seton River steelhead. A total of 15 steelhead were tracked during the 1997 spawning season and 18 steelhead were tracked during the 1999 spawning season in the Bridge and Seton watersheds. Immigration into the Seton and Bridge Rivers started around the middle of April and finished during the second week of May. Immigration into the Bridge and Seton Rivers in 1999 occurred primarily during the last two weeks of April. Spawning in the Bridge and Seton watersheds in 1997 started during the second week of May and ended around the middle of June. Spawning in the Bridge and Seton watersheds in 1999 occurred a little earlier, starting during the second week of April and finishing during the first week of June. -
2004 Southern Salmon Fishery Post - Season Review
2004 Southern Salmon Fishery Post - Season Review PART ONE FRASER RIVER SOCKEYE REPORT 2004 Southern Salmon Fishery Post - Season Review PART ONE FRASER RIVER SOCKEYE REPORT March 2005 TABLE OF CONTENTS Preface ..............................................................................................................................................i History and Organization of Review and Committee.....................................................................1 Pre-Season, In-Season, Mission and Post-Season Estimates...........................................................7 Catch Monitoring...........................................................................................................................15 Effects of High Water Temperature on Fraser River Sockeye in 2004 .........................................19 Fishing Gear Impacts ....................................................................................................................29 Enforcement...................................................................................................................................33 Management and Budget ..............................................................................................................43 Recommendations of 1992, 1994 and 2002 Sockeye Management Review Panels: Themes, Lessons, Actions................................................................................49 General Conclusions in Summary ................................................................................................61 -
Xwísten COMMUNITY PROFILE
XWÍSTEN COMMUNITY PROFILE MAY 2013 ISSUE #1 • FEBRUARY 2013 Xwísten The smiling people NXwísten The foamy waters after the rapids II Contents INTRODUCTION . 1. What is Xwísten’s Community Profile? 1 What is the Xwísten Comprehensive Community Plan? 2 OUR PEOPLE AND CULTURE . 5. History 5 Culture and Language 7 Population and Demographics 8 OUR COMMUNITY . 11. Education 11 Health and Wellness 14 Housing 17 Safety and Security 21 Social Development and Elders 23 GOVERNANCE AND ADMINISTRATION . .25 Elected Leadership 25 Band Administration 25 Xwísten Organization 26 OUR ECONOMY . .29 . Employment and Jobs 29 Economic Development Initiatives 30 OUR LAND AND RESOURCES . .33 . Our Lands 33 Land and Resource Management 34 APPENDIX. 37 Additional Details on Educational Programming 37 Xwísten Community Profile III IV Introduction Introduction What is Xwísten’s Community Profile? This Community Profile provides a ‘snap shot’ of current conditions in our community. It is meant to provide a starting point for preparing the Xwísten Comprehensive Community Plan. In addition to looking at what is happening now in our community, this profile provides some direction on areas that we may need to pay special attention to in our Comprehensive Community Plan. Most of all, it is meant to share information with members on how we are doing and to help get discussions going about where we want to go as a community and how. The profile has been organized into five sections: Our People and Culture – History, Culture and Language, Population and Demographics Our Community – Education, Health and Wellness, Housing, Safety and Security, Social Development Our Government – Leadership and Governance, Band Administration, Band Financial Health Our Economy – Employment and Jobs, Economic Development Initiatives Our Land – Our Land and Resources, Land Use Planning In each of these sections, we looked for trends so we can start thinking about how we can build on our strengths (the positive trends) and address our weaknesses (the negative trends).