Vascular Flora of Love Valley Wildlife Management Area, Love County, Oklahoma

Total Page:16

File Type:pdf, Size:1020Kb

Vascular Flora of Love Valley Wildlife Management Area, Love County, Oklahoma 9 Vascular Flora of Love Valley Wildlife Management Area, Love County, Oklahoma Bruce W. Hoagland Oklahoma Biological Survey and Department of Geography, University of Oklahoma, Norman, OK 73019 Forrest Johnson (deceased) Oklahoma Biological Survey, and Department of Botany and Microbiology, University of Oklahoma, Norman, OK 73019 This article reports the results of an inventory of the vascular plants from the Love Valley Wildlife Management Area in south-central Oklahoma. Three hundred sixty- eight species of vascular plants in 258 genera and 86 families were collected. The most species were collected from the families Asteraceae (54), Poaceae (47), and Fabaceae (35). One hundred six species were annuals, and 241 were perennials. Sixty-nine species of woody plants were present. Thirty-one exotic species were collected representing 8.6% of the flora. One species tracked by the Oklahoma Natural Heritage Inventory was found. This study reports 162 species previously not documented in Love County. © 2004 Okla- homa Academy of Science INTRODUCTION STUDY AREA Biotic inventories are the foundation of con- The LVWMA encompasses 3,134 ha in Love servation biology and biogeographic re- County (Fig. 1; Wyatt 2004). It is located search. This study had two objectives, the along the North Bank of the Red River im- first of which was to fill a gap in floristic mediately upstream from Lake Texoma. The data for south-central Oklahoma. Prior to LVWMA was established in 1969 and is one 1997, the year collecting began for this study, of 64 wildlife management areas maintained 345 species were reported from Love County by the Oklahoma Department of Wildlife (Hoagland 2004). Botanical study of Love Conservation. Latitudinal extent ranges County began on 15 April 1913, when G. W. from 33.72oN to 33.82oN and longitudinal Stevens collected 54 specimens. In addition extent from 97.02oW to 94.14oW. to 1913, peak years for plant collecting in The LVWMA is located within the sub- Love County were 1938 (51 specimens) and tropical humid (Cf) climate zone (Trewartha 1953 (42 specimens; Hoagland 2004). 1968). Summers are warm (mean July tem- The second objective of this study was perature = 27.7oC) and humid, whereas win- to provide a comprehensive floristic inven- ters are relatively short and mild (mean tory and species for resource managers at January temperature = 1.9oC). Mean annual Love Valley Wildlife Management Area precipitation is 105.6 cm, with periodic se- (LVWMA). Such inventories aid resource vere droughts (Oklahoma Climatological managers in locating populations of sensi- Survey 2003). Physiographically, the study tive species and documenting the occur- area is located within the Osage Plains sec- rence of exotic and nuisance species (Barkley tion of the Central Lowlands province (Hunt 2000). Ignorance of the presence of exotic 1974) and the Dissected Coastal Plain prov- species can be detrimental to sensitive spe- ince of Oklahoma (Curtis and Ham 1979). cies and/or exert adverse economic impacts The surface geology is primarily Quaternary (Ertter 2000). silt, sand, and clay, but an outcropping of Proc. Okla. Acad. Sci. 84: pp 9-18 (2004) 10 B.W. HOAGLAND and F. JOHNSON Figure 1: Location of Love Valley Wildlife Management Area and floristic collection sites. Collection sites are denoted as white circles. Cretaceous sandstone is also preset (Branson (2000). Collections also were made ran- and Johnson 1979). Elevation ranges from domly throughout the LVWMA from March 197 m to 243 m. The primary soil associa- through October 1997. Vouchers for species tion at LVWMA is the Miller-Yahola, which exotic to North America were made from is composed of deep, clayeyand loamey soils naturalized populations only, thus exclud- in bottomlands. The Dougherty-Eufaula ing cultivated and ornamental plants. Speci- association occurs on deep sandy soils in mens were processed at the Robert Bebb uplands (Maxwell and Reasoner 1966). The Herbarium of the University of Oklahoma predominant potential vegetation types are (OKL) following standard procedures. Quercus stellata-Q. marilandica forest and Manuals used for specimen identification woodlands, bottomland forests, and included Waterfall (1969), Great Plains Flora tallgrass prairies (Duck and Fletcher 1943). Association (1986), and Diggs et al (1999). These vegetation types are restricted in dis- Origin, either native or introduced, was de- tribution. The majority of bottomland for- termined by using Taylor and Taylor (1991) ests are tilled and planted in crops. Old- and US Department of Agriculture-Natural fields are also a common land cover type at Resources Conservation Service (USDA- LVWMA. NRCS 2004). Nomenclature follows the (USDA-NRCS 2004). Voucher specimens METHODS were deposited at OKL. Eight collection sites were established at RESULTS AND DISCUSSION LVWMA for intensive floristic sampling. Sites were selected following a review of US A total of 368 species of vascular plants in Geological Survey 1:24,000 topographic 86 families and 258 genera were collected at maps and field reconnaissance. The pre- LVWMA (Table 1). Among the an- dominant vegetation association at these giosperms, 78 were monocots, and 276 were sites was classified according to Hoagland dicots. In addition, there were five species Proc. Okla. Acad. Sci. 84: pp 9-18 (2004) VASCULAR FLORA OF LOVE VALLEY WILDLIFE MANAGEMENT AREA 11 Table 1: Summary of floristic collections threatened or endangered species were en- made at Love Valley Wildlife Management countered at LVWMA. Marsilea vestita Area, Love County, Oklahoma.* (G5S1) was the only species tracked by the Oklahoma Natural Heritage Inventory Taxonomic Native Introduced (ONHI; 2004) encountered. (Species are group Species spp. spp. ranked by the ONHI according to level of imperilment at the global [G] and state [S] Equisetophyta 1 1 0 level on a scale of 1-5; with 1 representing a Pteridophyta 5 5 0 species that is imperiled and 5 a species that Coniferophyta 1 1 0 is secure [Groves et al 1995]). Magnoliophyta As a result of this study, 523 species are Magnoliopsida 277 259 18 now known to occur in Love County. A Liliopsida 84 72 12 comparison with the Atlas of the Flora of Total 368 338 30 Oklahoma database (AFO; Hoagland 2004) revealed that of the 361 species reported in * Table format follows Palmer et al (1995). this study, 162 had been previously collected in Love County. However, 164 species re- ported in the AFO database were not col- of ferns, one fern ally, and one gymnosperm. lected in this study. The Asteraceae (54), Poaceae (47), and Fabaceae (35) had the greatest number of The eight collection sites occurred species. The genera Carex (8), Quercus (6), within four vegetation associations. These and Symphyotrichum (6) included the great- associations are described in Hoagland est number of species. One hundred six (2000). A brief description of each follows. species of annuals, 12 biennials, and 241 perennials were in the LVWMA flora. Sixty- Quercus stellata-Q. marilandica-Carya nine species of woody plants were collected: texana forest association 27 trees, 26 shrubs, and 16 woody vines. This association occurred on uplands Thirty-one species (8.6%) from 12 fami- with deep sandy soils and was of limited lies were introduced to North America. The extent. Associated species include Aesculus families with the greatest number of intro- glabra, Cercis canadensis, Helianthus hirsutus, duced species were Poaceae (12) and Juglans nigra, Monarda punctata, Prunus Fabaceae (9). Eighteen of the introduced mexicana, Schizachyrium scoparium, species were annuals, one was biennial, and Symphoricarpos orbiculatus and Viburnum 12 were perennials. The percentage of ex- rufidulum. otic species was low in comparison to re- cently published floristic inventories. At Fraxinus pennsylvanica - Ulmus Keystone Wildlife Management Area, 15% americana forest association of the flora was composed of exotic species, Most common in seasonally flooded 12% at the Chickasaw National Recreation bottomlands along the Red River. Common Area, (Hoagland and Johnson 2001), 9% at associates include Acer negundo, Ampelopsis the Oologah Wildlife Management Area cordata, Boehmeria cylindrica, Celtis laevigata, (Hoagland and Wallick 2003) and Hugo Gleditsia triacanthos, and Morus rubra. Wildlife Management Area (Hoagland and Buthod, forthcoming), and 11% for an inven- Schizachyrium scoparium-Bouteloua tory of Tillman County (Hoagland et al, curtipendula herbaceous association forthcoming). However, both Red Slough This association occurred on upland and Grassy Slough had a much lower per- slopes underlain by Cretaceous sandstone. centage of exotics, 6.6% (Hoagland and Common associated species include Johnson, forthcoming). No federally listed Andropogon gerardii, Artemisia psilostachya, Proc. Okla. Acad. Sci. 84: pp 9-18 (2004) 12 B.W. HOAGLAND and F. JOHNSON Helianthus hirsutus, Krameria lanceolata, REFERENCES Pediomelum cuspidatum, Rhus aromatica, Barkley TM. 2000. Floristic studies in contemporary Symphyotrichum ericoides, and Tridens flavuus. botany. Madroño 47:253-258. Branson CC, Johnson KS. 1979. Generalized geologic map of Oklahoma. In: Johnson KS, Branson CC, Wetland and aquatic vegetation Curtis NM, Ham WE, Harrison WE, Marcher MV, Wetlands were limited to human-made and Roberts JF, editors. Geology and earth re- ponds, a spring, and some seeps. As a re- sources of Oklahoma. Norman (OK): Oklahoma Geological Survey. p 4. sult, it was decided not to classify wetlands Curtis NM, Ham WE. 1979. Geomorphic
Recommended publications
  • Baylor Geological Studies
    BAYLORGEOLOGICA L STUDIES PAUL N. DOLLIVER Creative thinking is more important than elaborate FRANK PH.D. PROFESSOR OF GEOLOGY BAYLOR UNIVERSITY 1929-1934 Objectives of Geological Training at Baylor The training of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of train­ ing geologists at Baylor University are to provide a sound basis of understanding and to foster a truly geological point of view, both of which are essential for continued professional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research in­ cluding that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring ob­ jective attitude and to examine critically all geological concepts and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. Frontis. Sunset over the Canadian River from near the abandoned settlement of Old Tascosa, Texas. The rampart-like cliffs on the horizon first inspired the name "Llano Estacado" (Palisaded Plain) among Coronado's men. THE BAYLOR UNIVERSITY PRESS WACO, TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN NO. 42 Cenozoic Evolution of the Canadian River Basin Paul N. DoUiver BAYLOR UNIVERSITY Department of Geology Waco, Texas Spring 1984 Baylor Geological Studies EDITORIAL STAFF Jean M. Spencer Jenness, M.S., Editor environmental and medical geology O. T. Ph.D., Advisor, Cartographic Editor what have you Peter M. Allen, Ph.D. urban and environmental geology, hydrology Harold H. Beaver, Ph.D.
    [Show full text]
  • Txu-Oclc-2601092.Pdf
    BUREAU OF ECONOMIC GEOLOGY The University of Texas Austin, Texas 78712 l'eter T. Flawn, Director Report of Investigations—No. 51 Relation of Ogallala Formation to the Southern High Plains in Texas By John C. Frye and A. Byron Leonard March 1964 Contents Page Abstract 5 Introduction 5 Regional physiography 8 The Ogallala Formation and the High Plains surface 10 Fossil seeds of the Ogallala Formation 11 Pleistocene dissection of the High Plains margin 14 Abandoned Panther Valley 15 Lake Lomax 17 Fossil molluscan assemblages 18 Conclusions 20 References 20 Index . 24 - Illustrations Figures Page Index of central-western Texas location 1. map showing of profiles and fossil localities . 7 2. Regional profiles in central-western Texas 9 abandoned Panther the 3. Profiles across Lake Lomax and Valley in of and Glasscock counties - 16 Big Spring area Howard, Martin, Plate I. Field views 22 Relation of Ogallala Formation to the Southern High Plains in Texas JOHN C. FRYE 1 and A. BYRON LEONARD^ ABSTRACT Studies along the southern and south- Pliocene and Pleistocene valley is de- scribed of Edwards Plateau eastern borders of the High Plains have across a prong the of outliers of south of and the drainage of demonstrated presence Big Spring, Lake Lomax is de- fossiliferous Ogallala Formation in Borden the late Pleistocene in and Scurry counties and have documented termined to have occurred pre-Bradyan Wisconsinan lime. A the occurrence of Pliocene deposition as far meaningful physio- be- The limit of cannot be drawn southeast as Sterling County. graphic boundary southern limits of the characteristic Ash Hollow seed floras is ex- tween the High Plains and the Edwards Plateau.
    [Show full text]
  • A Biodiversity and Conservation Assessment of the Edwards Plateau Ecoregion
    A Biodiversity and Conservation Assessment of the Edwards Plateau Ecoregion June 2004 © The Nature Conservancy This document may be cited as follows: The Nature Conservancy. 2004. A Biodiversity and Conservation Assessment of the Edwards Plateau Ecoregion. Edwards Plateau Ecoregional Planning Team, The Nature Conservancy, San Antonio, TX, USA. Acknowledgements Jasper, Dean Keddy-Hector, Jean Krejca, Clifton Ladd, Glen Longley, Dorothy Mattiza, Terry The results presented in this report would not have Maxwell, Pat McNeal, Bob O'Kennon, George been possible without the encouragement and Ozuna, Jackie Poole, Paula Power, Andy Price, assistance of many individuals and organizations. James Reddell, David Riskind, Chuck Sexton, Cliff Most of the day-to-day work in completing this Shackelford, Geary Shindel, Alisa Shull, Jason assessment was done by Jim Bergan, Bill Carr, David Singhurst, Jack Stanford, Sue Tracy, Paul Turner, O. Certain, Amalie Couvillion, Lee Elliott, Aliya William Van Auken, George Veni, and David Wolfe. Ercelawn, Mark Gallyoun, Steve Gilbert, Russell We apologize for any inadvertent omissions. McDowell, Wayne Ostlie, and Ryan Smith. Finally, essential external funding for this work This project also benefited significantly from the came from the Department of Defense and the U. S. involvement of several current and former Nature Army Corps of Engineers through the Legacy Grant Conservancy staff including: Craig Groves, Greg program. Without this financial support, many of the Lowe, Robert Potts, and Jim Sulentich. Thanks for critical steps in the planning process might not have the push and encouragement. Our understanding of ever been completed. Thank you. the conservation issues important to the Edwards Plateau was greatly improved through the knowledge and experiences shared by many Conservancy staff including Angela Anders, Gary Amaon, Paul Barwick, Paul Cavanagh, Dave Mehlman, Laura Sanchez, Dan Snodgrass, Steve Jester, Bea Harrison, Jim Harrison, and Nurani Hogue.
    [Show full text]
  • Reconaissance of the Chemical Quality of Surface Waters of The
    ( TEXAS WATER DEVELOPMENT BOARD REPORT 129 RECONNAISSANCE OF THE CHEMICAL QUALITY OF SURFACE WATERS OF THE RED RIVER BASIN, TEXAS By Donald K. Leifeste, James F. Blakey. and Leon S. Hughes Prepared by the U.S GeologH;.1 Su..... ey in c:oope,-"on wIth the TellllS Waler Development Board M~ 1971 TEXAS WATER DEVELOPMENT BOARD W. E. Tinsley, Chairman Marvin Shurbet. Vice Chairman Robert B. Gilmore John H. McCoy Milton T. Potts earl Illig Harry P. Burleigh. EXl!QJtive Director ( Authorization for use or reproduction of any material contained in this publication, i.e., not obtained from other sources, is freely granted without the n«:essity of securing permission therefor. The Board would appreciate acknowledgement of the source of original material so utilized. ( ( Published and distributed bV the Texas Water Development Board ( Post Office Box 13087 Austin, Texas 78711 ( ( ii i :;.oC , ~no <.. ... qa 1)0 lal TABLE OF CONTENTS Pogo ABSTRACT .... _.... INTRODUCTION . 3 RED RIVER DRAINAGE BASIN 3 General Description 3 Population and Municipalities 5 Agricultural and Industrial Development ...............•... 9 Development of Surface·Water Resources . 9 CHEMICAL QUALITY OF THE WATER 9 Chemical·Quality Records ....................••............••......•.. 9 Streamflow Records . 10 Environmental Factors and Their Effects on the Chemical Quality of the Water ...............•...........................•. 10 Geology ..................••.••..••.••..••••...•..•....•••..•...•. 10 Streamflow . 12 Actillities of Man ., 12 Relation of Quality of Water to Use 17 Domestic Use 17 Industrial Use 19 Irrigation .. 19 Geographic Variations In Water Quality ............•.................... 19 Dissolved Solids ... 21 Chloride . 22 Hardness ...........••.••..•••••..•••••..•••••.••••••..•••••.•••.. _ 22 Other Constituents .......•.........•.••••.....•......•......•...••.•. 22 Water Quality in Reservoirs 22 Buffalo Lake . 22 iii TABLE OF CONTENTS IConl'd.) p,.
    [Show full text]
  • Flora of North Central Texas Flora of North Central Texas
    SHINNERS & MAHLER’S FLOR A OF NORTH CENTRAL TEXAS GEORGE M. DIGGSIGGS,, JJR.. BBARNEY L. LIPSCOMBIPSCOMB ROBERT J. O’KENNON D VEGETATIONAL AREAS OF TEXAS MODIFIED FROM CHECKLIST OF THE VASCULAR PLANTS OF TEXAS (HATCH ET AL. 1990). NEARLY IDENTICAL MAPS HAVE BEEN USED IN NUMEROUS WORKS ON TEXAS INCLUDING GOULD (1962) AND CORRELL AND JOHNSTON (1970). 1 PINEYWOODS 2 GULF PRAIRIES AND MARSHEs 3 POST OAK SAVANNAH 4 BLACKLAND PRAIRIES 5 CROSS TIMBERS AND PRAIRIES 6 SOUTH TEXAS PLAINS 7 EDWARDS PLATEAU 8 ROLLING PLAINS 9 HIGH PLAINS 10 TRANS-PECOS, MOUNTAINS AND BASINS D VEGETATIONAL AREAS OF NORTH CENTRAL TEXAS D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D D SHINNERS & MAHLER’S ILLUSTRATED FLORA OF NORTH CENTRAL TEXAS Shinners & Mahler’s ILLUSTRATED FLORA OF NORTH CENTRAL TEXAS IS PUBLISHED WITH THE SUPPORT OF: MAJOR BENEFACTORS: NEW DOROTHEA L. LEONHARDT FOUNDATION (ANDREA C. HARKINS) BASS FOUNDATION ROBERT J. O’KENNON RUTH ANDERSSON MAY MARY G. PALKO AMON G. CARTER FOUNDATION MARGRET M. RIMMER MIKE AND EVA SANDLIN INSTITUTIONAL SUPPORT: AUSTIN COLLEGE BOTANICAL RESEARCH INSTITUTE OF TEXAS SID RICHARDSON CAREER DEVELOPMENT FUND OF AUSTIN COLLEGE OTHER CONTRIBUTORS: PEG AND BEN KEITH FRIENDS OF HAGERMAN NAT IONAL WILDLIFE REFUGE SUMMERLEE FOUNDATION JOHN D.
    [Show full text]
  • Report 360 Aquifers of the Edwards Plateau Chapter 2
    Chapter 2 Conceptual Model for the Edwards–Trinity (Plateau) Aquifer System, Texas Roberto Anaya1 Introduction The passage of Senate Bill 1 in 1997 established a renewed public interest in the State’s water resources not experienced since the drought of the 1950s. Senate Bill 1 of 1999 and Senate Bill 2 of 2001 provided state funding to initiate the development of groundwater availability models for all of the major and minor aquifers of Texas. The development and management of Groundwater Availability Models (GAMs) has been tasked to the Texas Water Development Board (TWDB) to provide reliable and timely information on the State’s groundwater resources. TWDB staff is currently developing a GAM for the Edwards–Trinity (Plateau) aquifer. An essential task in the design of a numerical groundwater flow model is the development of a conceptual model. The conceptual model is a generalized description of the aquifer system that defines boundaries, hydrogeologic parameters, and hydrologic stress variables. The conceptual model helps to compile and organize field data and to simplify the real-world aquifer flow system into a graphical or diagrammatical representation while retaining the complexity needed to adequately reproduce the system behavior (Anderson and Woessner, 1992). The first step in the development of a conceptual model is to delineate the study area and form an understanding of its physical landscape with regard to the physiography, climate, and geology. Another early step also involves the research and investigation of previous aquifer studies. Intermediate steps bring together all of the information for establishing the hydrogeologic setting which consists of the hydrostratigraphy, structural geometry, hydraulic properties, water levels and regional groundwater flow, recharge, interactions between surface water and groundwater, well discharge, and water quality.
    [Show full text]
  • Texas Wildlife Third - Fifth
    Texas Wildlife Third - Fifth Life Science TEKS Third Grade: 3.9A, 3.9B, 3.10A, 3.10B, 3.10C Fourth Grade: 4.9A, 4.9B, 4.10A, 4.10C Fifth Grade: 5.9A, 5.9B, 5.9C, 5.9D, 5.10A Vocabulary amphibian, Big Bend Country, bird, carnivore, coastal, desert, eco-region, ecosystem, endangered, fish, forest, Gulf Coast, habitat, herbivore, Hill Country, invertebrate, landforms, mammal, omnivore, Panhandle Plains, Pineywoods, prairie, precipitation, reptile, reptile, soil, South Texas Plains, swamp, vegetation, vertebrate Pre-Show Activity Pre-Show Lesson: Texas Eco-regions (3 day activity) Post this question on the board: “What do you know about the nine eco-regions in Texas?” Materials: Per class: 9 pieces of large chart paper, Per group: Eco-region map, Eco-region chart and Eco-region map answer key (Appendix A-1), a different colored marker, 8 pieces of computer paper, Internet accessibility Procedure: Part 1 1. Groups will get a map of Texas with the nine eco-regions numbered and a list of the names of the regions. They will try to guess which region goes with each area on the map. To guess, they will place the number of the associated region of the map next to the appropriate region name on the chart (see Appendix A-1). HMNS 3-5 Texas Wildlife Page 1 2. Groups will check their guesses with the answer key to see how many they got right. 3. Hang nine separate chart papers, each with one of the following titles, around the room in a carousel-like arrangement: Region One: Coastal Prairies or Gulf Coastal Plain Region Two: West Gulf Coastal Plain or Piney Woods Region Three: Oaks and Prairies or Grand Prairie and Plains Region Four: Osage Plains (Cross Timbers) Region Five: Rolling Plains Region Six: Pecos and Staked Plains or High Plains Region Seven: Edwards Plateau Region Eight: South Texas Brushlands Region Nine: Chihuahuan Desert and Mexican Mountains in Texas or Trans- Pecos 4.
    [Show full text]
  • Tree Fall Gap Dynamics in the Cross Timbers of Oklahoma
    TREE FALL GAP DYNAMICS IN THE CROSS TIMBERS OF OKLAHOMA By LAXMAN KARKI Bachelor of Science in Biology Tribhuvan University Kathmandu, Nepal 1998 Master of Science in Botany Tribhuvan University Kathmandu, Nepal 2002 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE December, 2007 TREE FALL GAP DYNAMICS IN THE CROSS TIMBERS OF OKLAHOMA Thesis Approved: Dr. Stephen W. Hallgren Thesis Adviser Dr. Rodney Will Dr. Michael W. Palmer Dr. A. Gordon Emslie Dean of the Graduate College ii ACKNOWLEGEMENTS I am grateful to my adviser Dr. Stephen W. Hallgren for his advices, support and encouragement during my study and research. I would like to thank my committee members Dr. Michael W. Palmer and Dr. Rodney Will for their suggestions. I am grateful to Ryan DeSantis, Mauricio Moreno, Ed Lorenzi and Bruce Burton for their help in field data collection. I am grateful to my parents and my wife for their support and encouragement in every step of my life. iii TABLE OF CONTENTS Chapter Page I. INTRODUCTION..........................................................................................1 Background................................................................................................1 Purpose of study ........................................................................................3 II. REVIEW OF LITERATURE……………………………………………………..4 Physical Environment ................................................................................4
    [Show full text]
  • SPRING 1971 Bulletin No. 20 CLIFFORD LEON BYRD
    BAYLOR SPRING 1971 Bulletin No. 20 Origin and History of the Gravel of Central Texas CLIFFORDLEO N BYRD thinking is more important than elaborate FRANK CARNEY, PH.D. OF GEOLOGY BAYLOR UNIVERSITY 1929-1934 Objectives of Geological Training at Baylor The training of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of training geologists at Baylor University are to provide a sound basis of understanding and to foster a truly geological point of view, both of which are essential for continued pro­ fessional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research in­ cluding that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring objective attitude and to examine critically all geological concepts and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. THE BAYLOR UNIVERSITY PRESS WACO, TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN No. 20 Origin and History of the Uvalde Gravel of Central Texas CLIFFORD LEON BAYLOR UNIVERSITY Department of Geology Waco, Texas Spring, 1971 Geological Studies EDITORIAL STAFF Jean M. Spencer, M.S., Editor environmental and medical geology O. T. Hayward, Ph.D., Advisor, Cartographic Editor urban geology and what have you R. L. M.A., Business Manager archeology, geomorphology, vertebrate paleontology James W. Dixon, Jr., Ph.D. stratigraphy, paleontology, structure Walter T. Huang, Ph.D. mineralogy, petrology, metallic minerals Gustavo A. Morales, Ph.D.
    [Show full text]
  • Paleozoic, and It Therefore Seems Most Likely That the Seas in Which These Deposits Were Formed Were Connected with the Missis• Sippi Embayment Through These States
    Paleozoic, and it therefore seems most likely that the seas in which these deposits were formed were connected with the Missis• sippi embayment through these states. PENNSYLVANIAN SYSTEM The entire Pennsylvanian system is well represented in Texas. Rocks of this age are exposed in a great belt extending through north-central Texas from the Red River southward to the Llano uplift, and thence westward and southwestward until concealed by the overlying Permian or Cretaceous. In the Marathon and Soli- tario uplifts, formations of this system again come to the surface. A third region of disconnected exposures is that of the Diablo, Hueco, and Franklin mountains. The formations of these several regions will be separately discussed. Rocks of this system are found underground in north-central Texas west and east of the belt of surface outcrop and also south• west of the Llano uplift. The Pennsylvanian of north-central Texas is connected underground with that of Trans-Pecos Texas and, with the exception of some of the most pronounced highs, underlies much, if not all, of the great Permian basin. The sediments occur under varying facies. In extreme north Texas and the adjacent part of Oklahoma the uppermost part of the Pennsylvanian is of the red bed facies. Southward the red beds grade into normal marine lime• stones and shales. The sandstones and limestones of this system have afforded storage for a very large quantity of oil and gas, which is being produced in north-central Texas. The occurrence of Pennsylvanian in Texas seems to have been first recorded in 1852 by Roemer (1331), who included it under the general term of Carboniferous.
    [Show full text]
  • Stratigraphic Distribution of the Ostracoda of the Conanche (Cretaceous) Series of North Texas
    Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1974 Stratigraphic Distribution of the Ostracoda of the Conanche (Cretaceous) Series of North Texas. Walter Paul Kessinger Jr Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Kessinger, Walter Paul Jr, "Stratigraphic Distribution of the Ostracoda of the Conanche (Cretaceous) Series of North Texas." (1974). LSU Historical Dissertations and Theses. 2613. https://digitalcommons.lsu.edu/gradschool_disstheses/2613 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided io help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image.
    [Show full text]
  • The Osage Plains (Physiographic Area 33) Partners in Flight Bird Conservation Plan
    Partners in Flight Bird Conservation Plan for The Osage Plains (Physiographic Area 33) Partners in Flight Bird Conservation Plan for The Osage Plains (Physiographic Area 33) Version 1.0 6 October 2000 by Jane Fitzgerald, Bill Busby, Mark Howery, Ron Klataske, Dan Reinking, and David Pashley Please address comments to: Jane Fitzgerald PIF Midwest Regional Coordinator 8816 Manchester, suite 135 Brentwood, MO 63144 314-918-8505 e-mail: [email protected] *********************************************** Front cover illustration from ‘All the Birds of North America’ by Jack Griggs, courtesy of HarperCollins publishers. Table of Contents: Executive Summary: ....................................................1 Preface ...............................................................2 Section 1: The planning unit Background ............................................................3 Conservation issues .....................................................4 General conservation opportunities ..........................................7 Section 2: Avifaunal analysis General characteristics ...................................................8 Priority species .........................................................12 Section 3: Habitats and objectives Grasslands: Ecology and conservation status .........................................19 Bird habitat requirements ...............................................22 Population objectives and habitat strategies .................................28 Evaluation of assumptions - research
    [Show full text]