DOCSLIB.ORG

Information to Users

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Information to Users INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back of the book. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. UMI University Microfilms International A Beil & Howell Information Company 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA 313/761-4700 800/521-0600 Order Number 9211255 Paleoecology and paleoenvironmental analysis of the Upper Greenbrier Group (Upper Mississippian): West Virginia and western Maryland WulfF, Julie Iris, Ph.D. The Ohio State University, 1991 UMI 300 N. Zeeb Rd. Ann Aibor, MI 48106 PALEOECOLOGY AND PALEOENVIRONMENTAL ANALYSIS OF THE UPPER GREENBRIER GROUP (UPPER MISSISSIPPIAN): WEST VIRGINIA AND WESTERN MARYLAND DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy In the Graduate School of The Ohio State University by Julie Iris Wulff, B.S., M.S. The Ohio State University 1991 Dissertation Committee: Approved by Loren E. Babcock James W. Coilinson William I. Ausich, Adviser Terry J. Wilson Department of Geological Sciences Copyright by Julie Iris Wulff 1991 To Danielle Rose ACKNOWLEDGEMENTS No dissertation can be completed without the help of numerous people. I thank my advisor and friend, Dr. William I. Ausich, for his endless supply of advice, encouragement, ideas, good humor and, at times, financial support; Steven Riddle, my office mate and friend, for countless hours of discussion (not always dissertation reiatedi), study help and moral support; my fellow classmates, ail too many to mention, and the staff of the Department of Geological Sciences, in particular, Helen Hayes, Sue Shipley and Mary Hill. This study was field intensive and could not have been carried out without the help of field assistants Brenda Lord Lasorsa, Barbara Schwimmer, Bill Ausich, Kelly Beattiey Grant, Mike Grant, Rob Corzatt, Ralph Bentley, Matt Karrer, Doug Ricketts, Bob Janosy and Elizabeth Ausich. Dr. James Krug, of Aiderson, West Virginia, generously lent us the use of his turn of the century Victorian home while we were working in the area. The following people allowed us access to their quarries: Mr. Mike Hale and Mr. Steve Hinebaugh - Browning’s Deep Creek Quarry; Mr. Paul Schockey, Maryland Department of Transportation - Sang Run Quarry; Mr. C. K. Meadows - Kenton-Meadows Quarry; Mr. Patrick Adamson - Kermit Butcher Quarry; Mr. William Ryder - R. & R. Quarry; Ms. Diana Slater and Mr. Larry Simmons, Seneca Quarries - Slaty Fork Quarry; Acme Limestone Quarry and Mr. and Mrs. John E. Lane of Buckeye, WV. Financial support was provided by the Appalachian Basin industrial Associates Fund and Friends of Orton Hail, both administered through the Department of Geological Sciences, Shell Oil Company, Arco Oil Company, and a Graduate Student Alumni Research Award. Photographic assistance was provided by Beth Ann Daye and Bill Ausich. Drafting assistance was provided by Karen Tyler. I thank my parents, Jerry and Helene Wulff, for their continued support and understanding throughout yet another degree. Finally, I thank my husband and best friend, Eric Greenfield, who has only known me as a student. I am done, its finished, thanks for putting up with me through thick and thin. Lets get on with the rest of our iivesi III VITA March 31, 1959. ....................... Born - Chicago, Illinois 1982 B.S.,University of Illinois, Urbana, Illinois - Secondary Education, Physical Sciences 1986 ................................ M.S., University of Illinois, Chicago, Illinois - Geological Sciences PUBLICATIONS Wulff, J. I. 1986. Ordination of paleocommunities in the Lodgepole Limestone of Central Montana. (Abstr.). IN The Geological Society of America, North-central section, 20th annual meeting. Abstracts with Programs, 18(4):331. Riddle, S. W., J. I. Wulff & W. I. Ausich. 1987. Biomechanics of flexibility in the Gilbertsocrinus column. Sixth International Echinoderm Conference. Abstr., 101. Riddle, S. W., J. I. Wulff & W. I. Ausich. 1988. Biomechanics and stereomic microstructure of the Gilbertsocrinus tuberosus column. IN Proceedings of the Victoria International Echinoderm Conference. Balkema Press, Rotterdam. Wulff, J. I. 1989a. Biostratinomy of Archimedes ; Use in paleoenvironmental interpretation. (Abstr.). IN The Geological Society of America, North-central section, 23rd annual meeting. Abstracts with Programs, 21(4):53. Wulff, J. I. 1989b. Ecophenotypic variability in Spirifer pellaensis. (Abstr.). IN The Geological Society of America, 101st annual meeting, St. Louis, November, 1989. Abstracts with Programs, 21 (6). Wulff, J. I. 1990a. Morphometries of Spirifer pellaensis; how many species are there? Second International Brachiopod Congress, University of Otago, Dunedin, New Zealand, February, 1990. Abstr., 103. Wulff, J. I. 1990b. An Upper Mississippian reef in southern West Virginia. (Abstr.) IN The Geological Society of America, North- Central section, 24th annual meeting. Abstracts with Programs, 22(5). Wulff, J. I. 1990c. Biostratinomic use of Archimedes in paleoenvironmental interpretation. Palaios, 5:160-166. IV Wulff, J. I. 1990d. Tracking faunal and faciès changes across an uplift within a foreland basin. (Abst.). The Geological Society of America, 102nd annual meeting, Dallas, November, 1990. Abstracts with Programs, p. 62. Wulff, J. I. 1991. Intraspecific morphologic variability in Spirifer pellaensis. Greenbrier Group, (Upper Mississippian/Lower Carboniferous) USA. pp. 49-56 IN MacKinnon, D. et al., (eds.), Brachiopods Through Time. Balkema Press, Rotterdam. Wulff, J. I. & W. I. Ausich. 1991. Paleosols in the Greenbrier Group of central West Virginia: Evidence for extreme shallowing in the Greenbrier Sea. (Abst.). The Geological Society of America, North-Central section, 25th annual meeting. Wulff, J. I. & W. I. Ausich. 1989. Growth of the xenomorphic crinoid column (Taxocrinus, Late Mississippian). Journal of Paleontology, 63:657-661. Wulff, J. I., S. W. Riddle & W. I. Ausich. 1988. Columnal insertion and column growth in a Mississippian flexible crinoid. (Abstr.). IN The Geological Society of America, North-central section, 22nd annual meeting. Abstracts with Programs, 20(5): 395. Fields of Study Major Field: Goelogical Sciences Minor Field: Paleoecology and Paleoenvironmental Analysis TABLE OF CONTENTS DEDICATION ........................................................................................................................... i i ACKNOWLEDGEMENTS .......................................................... i ü VITA ...................................... iv LIST OF TABLES • • ................................................................................. - - - ix LIST OF FIGURES .............................................................................................................. x CHAPTER PAGE I. Introduction ........................ 1 M e th o d s ...................................................................................... 2 History & Geoiogic Setting of the Greenbrier G roup......................... ............................................ 4 Paieogeography & Tectonic Setting ...................................... 12 II. Sedimentology and Facies Anaiysis.................................................. 21 Introduction .................................................................................. 21 Interpretation of Lithofacies .................................................. 23 Region 1 - Garrett Co., Maryland.......................................... 25 Interpretation-Region 1 .............................................................. 43 Region 2 - North-central West Virginia....................................... 54 Interpretation-Region 2 . .................................................. 83 Region 3 - Southeastern West Virg in ia............................... 84 Interpretation-Region 3 .................................... 112 Regional Synthesis.................................................................. 116 Facies Relationships.................................................................. 119 III. Autecology . 125 Brachiopods • • ■ Bryozoans.................................... 142 Echinoderms .............................................................................. 149 Trilobite ..................................................................................... 153
Load more

Recommended publications
  • Triassic Gastropods of the Southern Qinling Mountains, China
    SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY • NUMBER 92 Triassic Gastropods of the Southern Qinling Mountains, China Jinnan Tong and Douglas H. Erwin Smithsonian Institution Press Washington, D.C. 2001 ABSTRACT Tong, Jinnan, and Douglas H. Erwin. Triassic Gastropods of the Southern Qinling Mountains, China. Smithsonian Contributions to Paleobiology, number 92,47 pages, 11 figures, 6 plates, 5 tables, 2001. Forty-eight species in 27 genera of gastropods, including 14 new species and one new genus, are described from early- to middle-Triassic (Scythian- to Ladinian-aged) rocks from the southern Qinling Mountains of Gansu and Sichuan provinces, China. This report expands the knowledge of the biogeographic distribution of gastropods during the recovery from the end-Permian mass extinction. The new taxa include Tongweispira sichuanensis, new genus and new species, and the following new species: Ananias guojiashanensis, Worthenia extendia, Gosseletinal dangchangensis, Zygites laevigatus, Trochotoma {Discotoma) gansuensis, Cheilotomona acutocarinata, Naticopsis (Dicosmos) compressus, Naticopsis (Dicosmos) sichuanensis, Naticopsis? ribletella, Neritopsis planoplicatus, Platychilina sinen­ sis, Platychilina obliqua, and Omphaloptycha gansuensis. OFFICIAL PUBLICATION DATE is handstamped in a limited number of initial copies and is recorded in the Institution's annual report, Annals of the Smithsonian Institution. SERIES COVER DESIGN: The trilobite Phacops rana Green. Library of Congress Cataloging-in-Publication Data Tong, Jinnan. Triassic gastropods
    [Show full text]
  • Foster Et Al., 2017A.Pdf
    Provided by the author(s) and University College Dublin Library in accordance with publisher policies. Please cite the published version when available. Title A silicified Early Triassic marine assemblage from Svalbard Authors(s) Foster, William J.; Danise, Silvia; Twitchett, Richard J. Publication date 2016-11-10 Publication information Journal of Systematic Palaeontology, 15 (10): 851-877 Publisher Taylor & FrancisNatural Environment Research Council (NERC) grant [NE/I005641] Item record/more information http://hdl.handle.net/10197/10921 Publisher's statement This is an Open Access article distributed under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Publisher's version (DOI) 10.1080/14772019.2016.1245680 Downloaded 2021-10-01T07:17:08Z The UCD community has made this article openly available. Please share how this access benefits you. Your story matters! (@ucd_oa) © Some rights reserved. For more information, please see the item record link above. Journal of Systematic Palaeontology, 2016 http://dx.doi.org/10.1080/14772019.2016.1245680 A silicified Early Triassic marine assemblage from Svalbard William J. Fostera,b,c*, Silvia Daniseb,d and Richard J. Twitchettc aJackson School of Geosciences, University of Texas, Austin, TX 78712, USA; bEarth Sciences, Plymouth University, Plymouth, PL4 8AA, UK; cDepartment of Earth Sciences, Natural History Museum, London, SW7 5BD, UK; dDepartment of Geology, University of Georgia, Athens, GA 30602, USA (Received 7 December 2015; accepted 31 August 2016) Understanding how the marine biosphere recovered from the late Permian mass extinction event is a major evolutionary question.
    [Show full text]
  • Carboniferous Formations and Faunas of Central Montana
    Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa­ tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________
    [Show full text]
  • Revision of Some of Girty's Invertebrate Fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma Introduction by MACKENZIE GORDON, JR
    Revision of Some of Girty's Invertebrate Fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma Introduction By MACKENZIE GORDON, JR. Corals By WILLIAM J. SANDO Pelecypods By JOHN POJETA, JR. Gastropods By ELLIS L. YOCHELSON Trilobites By MACKENZIE GORDON, JR. Ostracodes By I. G. SOHN GEOLOGICAL SURVEY PROFESSIONAL PAPER 606-A, B, C, D, E, F Papers illustrating and describing certain of G. H. Girty' s invertebrate fossils from the Fayetteville Shale UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 70-650224 For sale by the Superintendent of Documents, U.S. Government Printing Office Washing.ton, D.C. 20402 CONTENTS [The letters in parentheses preceding the titles are those used to designate the chapters] Page (A) Introduction, by Mackenzie Gordon, Jr _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 1 (B) Corals, by William J. Sando__________________________________________________________________________________ 9 (C) Pelecypods, by John Pojeta, Jr _____ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 15 (D) Gastropods, by Ellis L.
    [Show full text]
  • Mississippian Cephalopods of Northern and Eastern Alaska
    Mississippian Cephalopods of Northern and Eastern Alaska By MACKENZIE GORDON, JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 283 Descr9tions and illustrations of nautiloids and ammonoids and correlation of the assemblages with European Carbonferous goniatite zones UNITED STATES GOVERNMENT PRINTING OF,FICE, WASHINGTON : 1957 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1.50 (paper cover) CONTENTS Pane Page 1 Stratigraphic and geographic distribution-Continued Introduction - - - - - - .. - - - - ... - - - - - - - - - - - - .. - - - - - - - - - - - - - 1 Brooks Range-Continued Previous work-------------------------------------- 1 Kiruktagiak River basin--Chandler Lake area- - Composition of the cephalopod fauna ------------------ 2 Siksikpuk River basin ------- ---------- ------ Stratigraphic and geographic distribution of the cepha- Anaktuvuk River basin _------------..-..------ lopods------------------------------------------- Nanushuk River basin ...................... - Brooks Range---------------------------------- Echooka River basin --------- ----- - Cape Lisburne region ------- -- --- --------- - - - Eagle-Circle district ---__ _ -___ _- --- --- - - ---- - -- - - Lower Noatak Rlver basin -----------------..- Age and correlation of the cephalopod-bearing beds- ---- Western De Long Mountains_--__----- .------ Mississippian cephalopod-collecting localities in Alaska- -
    [Show full text]
  • 02 Inside Front Cover
    156 JAMES HALL’S (1856) ROSTROCONCHS? VOL. 106 James Hall’s (1856) Rostroconchs from the Mississippian of Indiana and Illinois1 RICHARD D. HOARE, Department of Geology, Bowling Green State University, Bowling Green, OH 43403 ABSTRACT. Hall (1856) described without illustrations six species of the rostroconch Conocardium in his study of the fauna of the Salem Limestone in Indiana and the Warsaw Shale in Illinois. The species represent five genera, two of which are new, Leptoconocardium and Kyoconocardium. Other species represent the genera Hippocardia Brown, 1843; Oxyprora Hoare, Mapes, and Yancey, 2002; and Diedrorynchus Hoare and Peck, 2005. OHIO J SCI 106 (4):156-163, 2006 INTRODUCTION have reduced the outer shell layer so that fine orna- In a continuing study of Upper Paleozoic rostro- mentation is often obliterated or poorly preserved. The conchs it was thought useful to locate and examine the ornamentation may not show up when the specimens Mississippian (Meremecian) specimens described by Hall are coated for photography, but is visible when un- (1856) from the Salem Limestone in Indiana and the coated or when slightly wet. Many of the fossils in the Warsaw Shale in Illinois. This study would compliment Salem Limestone are coated with a banded, oolitic-like those made from the Mississippian in Ohio (Hyde 1953; coating which may hide the ornamentation. Remnants of Hoare 1990, 2004) and West Virginia (Hoare and Peck the larval shell are present on some specimens. 2005). The purposes of this study are: 1) to redescribe All of the specimens are small, ranging in length from and photographically illustrate Hall’s specimens; 2) to 2.3 mm to 12.0 mm.
    [Show full text]
  • The Carboniferous Evolution of Nova Scotia
    Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The Carboniferous evolution of Nova Scotia J. H. CALDER Nova Scotia Department of Natural Resources, PO Box 698, Halifax, Nova Scotia, Canada B3J 2T9 Abstract: Nova Scotia during the Carboniferous lay at the heart of palaeoequatorial Euramerica in a broadly intermontane palaeoequatorial setting, the Maritimes-West-European province; to the west rose the orographic barrier imposed by the Appalachian Mountains, and to the south and east the Mauritanide-Hercynide belt. The geological affinity of Nova Scotia to Europe, reflected in elements of the Carboniferous flora and fauna, was mirrored in the evolution of geological thought even before the epochal visits of Sir Charles Lyell. The Maritimes Basin of eastern Canada, born of the Acadian-Caledonian orogeny that witnessed the suture of Iapetus in the Devonian, and shaped thereafter by the inexorable closing of Gondwana and Laurasia, comprises a near complete stratal sequence as great as 12 km thick which spans the Middle Devonian to the Lower Permian. Across the southern Maritimes Basin, in northern Nova Scotia, deep depocentres developed en echelon adjacent to a transform platelet boundary between terranes of Avalon and Gondwanan affinity. The subsequent history of the basins can be summarized as distension and rifting attended by bimodal volcanism waning through the Dinantian, with marked transpression in the Namurian and subsequent persistence of transcurrent movement linking Variscan deformation with Mauritainide-Appalachian convergence and Alleghenian thrusting. This Mid- Carboniferous event is pivotal in the Carboniferous evolution of Nova Scotia. Rapid subsidence adjacent to transcurrent faults in the early Westphalian was succeeded by thermal sag in the later Westphalian and ultimately by basin inversion and unroofing after the early Permian as equatorial Pangaea finally assembled and subsequently rifted again in the Triassic.
    [Show full text]
  • Mississippian and Pennsylvanian Fossils of the Albuquerque Country Stuart A
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/12 Mississippian and Pennsylvanian fossils of the Albuquerque country Stuart A. Northrop, 1961, pp. 105-112 in: Albuquerque Country, Northrop, S. A.; [ed.], New Mexico Geological Society 12th Annual Fall Field Conference Guidebook, 199 p. This is one of many related papers that were included in the 1961 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States.
    [Show full text]
  • Chickasaw National Recreation Area Geologic Resources Inventory Report
    National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Chickasaw National Recreation Area Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2015/1008 ON THIS PAGE Sunset over Lake of the Arbuckles in Chickasaw National Recreation Area. National Park Service photograph. ON THE COVER A collage of features at Chickasaw National Recreation Area. Clockwise from upper left: waterfall on Travertine Creek; Lincoln Bridge (built in 1909 to connect the town of Sulphur to mineral springs south of Travertine Creek); Vendome Well (the largest artesian well in Oklahoma when drilled in 1922); Buffalo Spring (freshwater from the spring flows into Travertine Creek). National Park Service photographs. Chickasaw National Recreation Area Geologic Resources Inventory Report Natural Resource Report NPS/NRSS/GRD/NRR—2015/1008 John P. Graham Colorado State University Research Associate National Park Service Geologic Resources Division Geologic Resources Inventory PO Box 25287 Denver, CO 80225 August 2015 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate comprehensive information and analysis about natural resources and related topics concerning lands managed by the National Park Service. The series supports the advancement of science, informed decision-making, and the achievement of the National Park Service mission.
    [Show full text]
  • United States National Museum Bulletin 262
    SMITHSONIAN INSTITUTION MUSEUM O F NATURAL HISTORY For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C., 20402 - Price 70 cents UNITED STATES NATIONAL MUSEUM BULLETIN 262 Catalog of the Type Specimens of Invertebrate Fossils LOUIS R. PURNELL Part I: Paleozoic Cephalopoda SMITHSONIAN INSTITUTION PRESS WASHINGTON, D.C. 1968 Publications of the United States National Museum The scientific publications of the United States National Museum in- clude two series, Proceedings of the United States National Museum and United States National Museum Bulletin. In these series are published original articles and monographs dealing with the collections and work of the Museum and setting forth newly ac- quired facts in the field of anthropology, biology, geology, history, and technology. Copies of each publication are distributed to libraries and scientific organizations and to specialists and others interested in the various subjects. The Proceedings, begun in 1878, are intended for the publication, in separate form, of shorter papers. These are gathered in volumes, octavo in size, with the publication date of each paper recorded in the table of contents of the volume. In the Bulletin series, the first of which was issued in 1875, appear longer, separate publications consisting of monographs (occasionally in several parts) and volumes in which are collected works on related sub- jects. Bulletins are either octavo or quarto in size, depending on the the needs of the presentation. Since 1902, papers relating to the botanical collections of the Museum have been published in the Bulletin series under the heading Contributions from the United States National Herbarium.
    [Show full text]
  • TREATISE ONLINE Number 48
    TREATISE ONLINE Number 48 Part N, Revised, Volume 1, Chapter 31: Illustrated Glossary of the Bivalvia Joseph G. Carter, Peter J. Harries, Nikolaus Malchus, André F. Sartori, Laurie C. Anderson, Rüdiger Bieler, Arthur E. Bogan, Eugene V. Coan, John C. W. Cope, Simon M. Cragg, José R. García-March, Jørgen Hylleberg, Patricia Kelley, Karl Kleemann, Jiří Kříž, Christopher McRoberts, Paula M. Mikkelsen, John Pojeta, Jr., Peter W. Skelton, Ilya Tëmkin, Thomas Yancey, and Alexandra Zieritz 2012 Lawrence, Kansas, USA ISSN 2153-4012 (online) paleo.ku.edu/treatiseonline PART N, REVISED, VOLUME 1, CHAPTER 31: ILLUSTRATED GLOSSARY OF THE BIVALVIA JOSEPH G. CARTER,1 PETER J. HARRIES,2 NIKOLAUS MALCHUS,3 ANDRÉ F. SARTORI,4 LAURIE C. ANDERSON,5 RÜDIGER BIELER,6 ARTHUR E. BOGAN,7 EUGENE V. COAN,8 JOHN C. W. COPE,9 SIMON M. CRAgg,10 JOSÉ R. GARCÍA-MARCH,11 JØRGEN HYLLEBERG,12 PATRICIA KELLEY,13 KARL KLEEMAnn,14 JIřÍ KřÍž,15 CHRISTOPHER MCROBERTS,16 PAULA M. MIKKELSEN,17 JOHN POJETA, JR.,18 PETER W. SKELTON,19 ILYA TËMKIN,20 THOMAS YAncEY,21 and ALEXANDRA ZIERITZ22 [1University of North Carolina, Chapel Hill, USA, [email protected]; 2University of South Florida, Tampa, USA, [email protected], [email protected]; 3Institut Català de Paleontologia (ICP), Catalunya, Spain, [email protected], [email protected]; 4Field Museum of Natural History, Chicago, USA, [email protected]; 5South Dakota School of Mines and Technology, Rapid City, [email protected]; 6Field Museum of Natural History, Chicago, USA, [email protected]; 7North
    [Show full text]
  • Appendices (3.601Mb)
    University of Plymouth PEARL https://pearl.plymouth.ac.uk 04 University of Plymouth Research Theses 01 Research Theses Main Collection 2015 Palaeoecology of the late Permian mass extinction and subsequent recovery Foster, William J. http://hdl.handle.net/10026.1/5467 Plymouth University All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. Appendix 2.1: Balaton Highlands and Bükk Mountains Investigated sites. The Permian-Triassic succession of Balaton Highlands comprises part of the ALCAPA megaunit (Kóvacs and Haas, 2010) and is represented by Permian fluvial red sandstones and Triassic shallow marine rocks. The Lower Triassic succession in the Balaton Highlands is divided into four formations: the Kóveskál Dolomite Formation, Arács Marl Formation, Hidegkút Formation and Csopak Marl Formation (Figure A2.1). These formations paraconformably overlay the Permian Baltonfelvidék Formation and are capped by the Middle Triassic Aszòfo Dolomite Formation (Haas et al., 2012). Field visits (June 2012) to the Balaton Highlands (Figure A2.2) recorded 5m of the Kóveskál Formation at Balatonfüred; 15m at Balataonálmadi; and 1m of the Csopak Marl Formation at the Sóly section. Broglio Loriga et al. (1990) studied the biostratigraphy of the entire succession, but their data, were acquired from a trench that is no longer exposed (János Haas, pers. comm.) and their collections were not available for study (Renato Posenato, pers.
    [Show full text]