Fossils and Their Value
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Type and Figured Fossils in the Worthen Collection at the Illinois
s Cq&JI ^XXKUJtJLI 14oGS: CIR 524 c, 2 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY Lois S. Kent GEOLOGICAL ILLINOIS Illinois Department of Energy and Natural Resources, STATE GEOLOGICAL SURVEY DIVISION CIRCULAR 524 1982 COVER: This portrait of Amos Henry Worthen is from a print presented to me by Worthen's great-grandson, Arthur C. Brookley, Jr., at the time he visited the Illinois State Geological Survey in the late 1950s or early 1960s. The picture is the same as that published in connection with the memorial to Worthen in the appendix to Vol. 8 of the Geological Survey of Illinois, 1890. -LSK Kent, Lois S., Type and figured fossils in the Worthen Collection at the Illinois State Geological Survey. — Champaign, III. : Illinois State Geological Survey, 1982. - 65 p. ; 28 cm. (Circular / Illinois State Geological Survey ; 524) 1. Paleontology. 2. Catalogs and collections. 3. Worthen Collection. I. Title. II. Series. Editor: Mary Clockner Cover: Sandra Stecyk Printed by the authority of the State of Illinois/1982/2500 II I IHOI'.MAII '.I 'II Of.ir.AI MIHVI y '> 300 1 00003 5216 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY Lois S. Kent | CIRCULAR 524 1982 ILLINOIS STATE GEOLOGICAL SURVEY Robert E. Bergstrom, Acting Chief Natural Resources Building, 615 East Peabody Drive, Champaign, IL 61820 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY CONTENTS Acknowledgments 2 Introduction 2 Organization of the catalog 7 Notes 8 References 8 Fossil catalog 13 ABSTRACT This catalog lists all type and figured specimens of fossils in the part of the "Worthen Collection" now housed at the Illinois State Geological Survey in Champaign, Illinois. -
United States
DEPARTMENT OF THE INTERIOR BULLETIN OF THE UNITED STATES ISTo. 146 WASHINGTON GOVERNMENT Pit IN TING OFFICE 189C UNITED STATES GEOLOGICAL SURVEY CHAKLES D. WALCOTT, DI11ECTOK BIBLIOGRAPHY AND INDEX NORTH AMEEICAN GEOLOGY, PALEONTOLOGY, PETEOLOGT, AND MINERALOGY THE YEA.R 1895 FEED BOUGHTON WEEKS WASHINGTON Cr O V E U N M K N T P K 1 N T I N G OFFICE 1890 CONTENTS. Page. Letter of trail smittal...... ....................... .......................... 7 Introduction.............'................................................... 9 List of publications examined............................................... 11 Classified key to tlio index .......................................... ........ 15 Bibliography ............................................................... 21 Index....................................................................... 89 LETTER OF TRANSMITTAL DEPARTMENT OF THE INTEEIOE, UNITED STATES GEOLOGICAL SURVEY, DIVISION OF GEOLOGY, Washington, D. 0., June 23, 1896. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for the year 1895, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 1 BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINER ALOGY FOR THE YEAR 1895. By FRED BOUGHTON WEEKS. INTRODUCTION. The present work comprises a record of publications on North Ameri can geology, paleontology, petrology, and mineralogy for the year 1895. It is planned on the same lines as the previous bulletins (Nos. 130 and 135), excepting that abstracts appearing in regular periodicals have been omitted in this volume. Bibliography. The bibliography consists of full titles of separate papers, classified by authors, an abbreviated reference to the publica tion in which the paper is printed, and a brief summary of the con tents, each paper being numbered for index reference. -
New Data on Carboniferous Crinoids from the Moscow Region*
Zoosymposia 7: 91–100 (2012) ISSN 1178-9905 (print edition) www.mapress.com/zoosymposia/ ZOOSYMPOSIA Copyright © 2012 · Magnolia Press ISSN 1178-9913 (online edition) New data on Carboniferous crinoids from the Moscow Region* GEORGE V. MIRANTSEV1,2 & SERGEY V. ROZHNOV1 1 A.A. Borissiak Paleontological Institute, Russian Academy of Sciences, Moscow, Russia 2 Corresponding author, E-mail: [email protected] *In: Kroh, A. & Reich, M. (Eds.) Echinoderm Research 2010: Proceedings of the Seventh European Conference on Echinoderms, Göttingen, Germany, 2–9 October 2010. Zoosymposia, 7, xii + 316 pp. Abstract Despite more than 150 years of study of crinoids from the Moscow Region there are numerous undescribed taxa from well-known localities as well as others from poorly known localities. In recent years, through the acquisition of new collections as well as new discoveries, the holdings of Carboniferous crinoids of the Paleontological Institute, Russian Academy of Science have been greatly increased. This has allowed a more detailed study of the faunas, which is in pro- gress. Among the crinoids in the collection there are representatives of the family Pirasocrinidae Moore & Laudon, 1943, that are abundant in the Pennsylvanian of the USA, and previously unknown in the Carboniferous of the Moscow Region, as well as representatives of the genera Allosocrinus Strimple, 1949, Cibolocrinus Weller, 1909 and Elibatocrinus Moore, 1940, also previously unknown in the Moscow Region. There is also the first recognized Pennsylvanian member of the family Taxocrinidae Angelin, 1878. The stratigraphic distribution of the most common crinoids from the Carboniferous of the Moscow Region is compiled. The crinoid faunas that characterize the Upper Carboniferous Substages are described. -
Pleistocene, Mississippian, & Devonian Stratigraphy of The
64 ANNUAL TRI-STATE GEOLOGICAL FIELD CONFERENCE GUIDEBOOK Pleistocene, Mississippian, & Devonian Stratigraphy of the Burlington, Iowa, Area October 12-13, 2002 Iowa Geological Survey Guidebook Series 23 Cover photograph: Exposures of Pleistocene Peoria Loess and Illinoian Till overlie Mississippian Keokuk Fm limestones at the Cessford Construction Co. Nelson Quarry; Field Trip Stop 4. 64th Annual Tri-State Geological Field Conference Pleistocene, Mississippian, & Devonian Stratigraphy of the Burlington, Iowa, Area Hosted by the Iowa Geological Survey prepared and led by Brian J. Witzke Stephanie A. Tassier-Surine Iowa Dept. Natural Resources Iowa Dept. Natural Resources Geological Survey Geological Survey Iowa City, IA 52242-1319 Iowa City, IA 52242-1319 Raymond R. Anderson Bill J. Bunker Iowa Dept. Natural Resources Iowa Dept. Natural Resources Geological Survey Geological Survey Iowa City, IA 52242-1319 Iowa City, IA 52242-1319 Joe Alan Artz Office of the State Archaeologist 700 Clinton Street Building Iowa City IA 52242-1030 October 12-13, 2002 Iowa Geological Survey Guidebook 23 Additional Copies of this Guidebook May be Ordered from the Iowa Geological Survey 109 Trowbridge Hall Iowa City, IA 52242-1319 Phone: 319-335-1575 or order via e-mail at: http://www.igsb.uiowa.edu ii IowaDepartment of Natural Resources, Geologial Survey TABLE OF CONTENTS Pleistocene, Mississippian, & Devonian Stratigraphy of the Burlington, Iowa, Area Introduction to the Field Trip Raymond R. Anderson ............................................................................................................................ -
Geologic Literature of New Mexico by Thomas Peltier Wootton
STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO SCHOOL OF MINES STATE BUREAU OF MINES AND MINERAL RESOURCES E. H. WELLS President and Director BULLETIN NO. 5 Geologic Literature of New Mexico By Thomas Peltier Wootton SOCORRO, N. M. 1930 NEW MEXICO SCHOOL OF MINES STATE BUREAU OF MINES AND MINERAL RESOURCES E. H. WELLS President and Director BULLETIN NO. 5 Geologic Literature of New Mexico By Thomas Peltier Wootton SOCORRO, N. M. 1930 CONTENTS Page The New Mexico Bureau of Mines and Mineral Resources ............................. 3 Board of regents ........................................................................... 4 Officers of the board ..................................................................... 4 Publications ...................................................................................... 4 Introduction .................................................................................................. 5 Plan and scope of bibliography ................................................................... 5 Acknowledgments ............................................................................... 5 How publications may be obtained ....................................................... 6 Abbreviations used ........................................................................... 7 Serials ................................................................................................. 8 Part I. Bibliography ........................................................................ 13 Part II. Index ................................................................................ -
North American Geology, Paleontology Petrology, and Mineralogy
Bulletin No. 221 Series G, Miscellaneous, 25 DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY PETROLOGY, AND MINERALOGY FOR BY 3FJRJEJD BOUGHHXCMV WEEKS WASHINGTON @QVEE,NMENT PRINTING OFFICE 1 9 0 3 O'Q.S. Pago. Letter of transrnittal...................................................... 5 Introduction...............................:............................. 7 List of publications examined............................................. 9 Bibliography............................................................. 13 Addenda to bibliographies for previous years............................... 124 Classified key to the index................................................ 125 Index................................................................... 133 £3373 LETTER OF TRANSMITTAL. DEPARTMENT OF THE INTERIOR, UNITED STATES GEOLOGICAL SURVEY, Washington, D. C., October 20, 1903. SIR: I have the honor to transmit herewith the manuscript) of a bibliography and index of North American geology, paleontology, petrology, and mineralogy for the year 1902, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 5 BIBLIOaRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINERALOGY FOR THE YEAR 1902. By FRED BOUGHTON WEEKS. INTRODUCTION. The arrangement of the material of the Bibliography and Index for 1902 is similar to that adopted for the previous publications (Bulletins Nos. 130, 135, 146, 149, 156, 162, 172, 188, 189, and 203). Several papers that should have been entered in the previous bulletins are here recorded, and the date of publication is given with each entry. Bibliography. The bibliography consists of full titles of separate papers, arranged alphabetically by authors' names, an abbreviated reference to the publication in which the paper is printed, and a brief description of the contents, each r>aper being numbered for index reference. -
Classification of Echinoderms
CLASSIFICATION OF ECHINODERMS The members of the phylum Echinodermata are known to mankind since ancient times. Echinoderms were first given the status of a distinct group by Bruguiere in 1791. Echinoderms are bilaterally symmetrical (in larval stage) or pentamerous radially symmetrical (in adults) having mesodermal calcareous ossicles as exoskeleton, enterocoelom, water-vascular system and without distinct head. But H. B. Fell (1948, 1965), the authority on echinoderm taxonomy of Harvard University, USA, rejected the older classification as it was an artificial one because it was on the basis of mode of existence. The scheme of classification presented in this book (4th ed.), largely based on the classification plan outlined by Edward E. Ruppert and Robert D. Barnes (1994, 6th ed.). Classification with Characters: A. Subphylum Homalozoa (Mid- Cambrian —Devonian): Features: 1. Extinct, irregular, palaeozoic. 2. Carpoids (resembling crinoids but laterally compressed giving the evidence of a bilateral symmetry). Example: Enoploura. B. Subphylum Crinozoa: Features: 1. Radially symmetrical echinoderms with a globoid or cup-shaped theca and brachioles or arms. 2. Mostly attached, with oral surface directed upward. This subphylum includes the fossil eocrinoids, cystoids and the fossil and living crinoids. 1. Class Eocrinoidea (Early Cambrian to Ordovician): Features: 1. The oldest extinct crinoids. 2. They were stalked or stalk-less, with an enclosed theca. 3. The upper or oral end contained five ambulacra and five to many brachioles. Example: Mimocystites. 2. Class Cystidea (Ordovician—Silurian): Features: 1. The well-known group of extinct echinoderms. 2. They have vase-like bodies which remain fixed with the substratum directly or through a stalk. -
Phylogenetic Taxonomy and Classification of the Crinoidea (Echinodermata)
Journal of Paleontology, 91(4), 2017, p. 829–846 Copyright © 2017, The Paleontological Society 0022-3360/17/0088-0906 doi: 10.1017/jpa.2016.142 Phylogenetic taxonomy and classification of the Crinoidea (Echinodermata) David F. Wright,1,* William I. Ausich,1 Selina R. Cole,1 Mark E. Peter,1 and Elizabeth C. Rhenberg2 1School of Earth Sciences, 125 South Oval Mall, Ohio State University, Columbus, OH 43210, USA 〈[email protected]〉, 〈[email protected]〉, 〈[email protected]〉, 〈[email protected]〉 2Department of Geology, Earlham College, 801 National Road West, Richmond, IN 47374, USA 〈[email protected]〉 Abstract.—A major goal of biological classification is to provide a system that conveys phylogenetic relationships while facilitating lucid communication among researchers. Phylogenetic taxonomy is a useful framework for defining clades and delineating their taxonomic content according to well-supported phylogenetic hypotheses. The Crinoidea (Echinodermata) is one of the five major clades of living echinoderms and has a rich fossil record spanning nearly a half billion years. Using principles of phylogenetic taxonomy and recent phylogenetic analyses, we provide the first phylogeny-based definition for the Clade Crinoidea and its constituent subclades. A series of stem- and node-based defi- nitions are provided for all major taxa traditionally recognized within the Crinoidea, including the Camerata, Disparida, Hybocrinida, Cladida, Flexibilia, and Articulata. Following recommendations proposed in recent revisions, we recog- nize several new clades, including the Eucamerata Cole 2017, Porocrinoidea Wright 2017, and Eucladida Wright 2017. In addition, recent phylogenetic analyses support the resurrection of two names previously abandoned in the crinoid taxonomic literature: the Pentacrinoidea Jaekel, 1918 and Inadunata Wachsmuth and Springer, 1885. -
Systematics and Evolutionary Paleoecology of Crinoids from the St
Graduate Theses, Dissertations, and Problem Reports 2010 Systematics and evolutionary paleoecology of crinoids from the St. Louis Limestone (Mississippian, Meramecian) of the Illinois Basin Lewis Anderson Cook West Virginia University Follow this and additional works at: https://researchrepository.wvu.edu/etd Recommended Citation Cook, Lewis Anderson, "Systematics and evolutionary paleoecology of crinoids from the St. Louis Limestone (Mississippian, Meramecian) of the Illinois Basin" (2010). Graduate Theses, Dissertations, and Problem Reports. 3083. https://researchrepository.wvu.edu/etd/3083 This Dissertation is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Dissertation in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Dissertation has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. Systematics and Evolutionary Paleoecology of Crinoids from the St. Louis Limestone (Mississippian, Meramecian) of the Illinois Basin Lewis Anderson Cook Dissertation submitted to the College of Arts and Sciences at West Virginia University in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geology Thomas Kammer, Ph.D., Chair William Ausich, Ph.D. Richard Smosna, Ph.D. Helen Lang, Ph.D. -
Carboniferous Geology and Biostratigraphy of the Appalachian Basin
Carboniferous Geology and Biostratigraphy of the Appalachian Basin Edited by Stephen F. Greb and Donald R. Chesnut Jr. Kentucky Geological Survey James C. Cobb, State Geologist and Director University of Kentucky, Lexington Carboniferous of the Appalachian and Black Warrior Basins Edited by Stephen F. Greb and Donald R. Chesnut Jr. Special Publication 10 Series XII, 2009 Our Mission Our mission is to increase knowledge and understanding of the mineral, energy, and water resources, geologic hazards, and geology of Kentucky for the benefit of the Commonwealth and Nation. Earth Resources—Our Common Wealth www.uky.edu/kgs Technical Level General Intermediate Technical © 2009 University of Kentucky For further information contact: Technology Transfer Officer Kentucky Geological Survey 228 Mining and Mineral Resources Building University of Kentucky Lexington, KY 40506-0107 ISSN 0075-5613 Contents Foreward ...................................................................................................................................................................1 1: Introduction Donald R. Chesnut Jr. and Stephen F. Greb ............................................................................................3 2: Carboniferous of the Black Warrior Basin Jack C. Pashin and Robert A. Gastaldo ..................................................................................................10 3: The Mississippian of the Appalachian Basin Frank R. Ettensohn ....................................................................................................................................22 -
Crinoid Stalk Flexibility: Theoretical Predictions and Fossil Stalk Postures
Crinoid stalk flexibility: theoretical predictions and fossil stalk postures TOMASZ K. BAUMILLER AND WILLIAM I. AUSICH Baurniller, T.K. &Ausich, W.I. 1996 07 15: Crinoid stalk flexibility: theoretical predictions and LETHAIA fossil stalk postures. Lethaia, Vol. 29, pp. 47-59. Oslo. ISSN 0024-1 164. Flexibilities in Lower Mississippian crinoid stalks were inferred from preserved postures and shown not to conform with predictions of a cantilever beam model. Flexibilities were not cor- related with hard-part characters such as stalk diameter, stalk length, or columnal height. The lack of correspondence between the predictions of the cantilever model and observed flexibili- ties implies that the niost likely control of stalk flexibility is the ligament, more specifically, its non-constant, mutable properties. Although a few Lower Mississippian crinoids, such as (21- bertsocrinus, Plntycrinites, and Camptocrinus, have enhanced flexibility achieved by radical modifications of columnal facet morphology, this study has failed to identify any general mor- phological characters that consistently predict flexibility. It appears that skeletal morphology is a poor guide to stalk flexibility; mutable collagenous tissue is the key. OCrinciideci, inphonomy, constructional morphology, Lower Carboniferous, connective tissues. Tomasz K. Baumiller, Museum ofPaleontology and Department of Geological Sciences, University ofMichigan, Ann Arbor, MI 48109-1079, USA; William I. Ausich [[email protected], Department of Geological Sciences, The Ohio State University, Columbus, Ohio 43210, USA; 14th December, 1994; revised 23rd September, 1995. Crinoid stalks are morphologically diverse. Columnals ibility differences have been inferred for fossil stalks, no have a variety of sizes, shapes, facet topographies, lumen general rules for factors controlling flexibility have sizes, and lumen shapes (Moore et ul. -
Carboniferous Echinoderm Zonation in the Appalachian Basin, Eastern USA
Wong, Th. E. (Ed.): Proceedings of the XVth International Congress on Carboniferous and Permian Stratigraphy. Utrecht, the Netherlands, 10–16 August 2003. Royal Netherlands Academy of Arts and Sciences Carboniferous echinoderm zonation in the Appalachian Basin, eastern USA F.R. Ettensohn 1,W.I.Ausich2,T.W.Kammer3, W.K. Johnson 1 & D.R. Chesnut, Jr. 4 1 Department of Earth & Environmental Sciences, University of Kentucky, Lexington, KY 40506, USA; e-mail: [email protected] 2 Department of Geological Sciences, Ohio State University, Columbus, OH 43210, USA 3 Department of Geology and Geography, West Virginia University, Morgantown, WV 26506, USA 4 Kentucky Geological Survey, University of Kentucky, Lexington, KY 40506, USA Abstract The Carboniferous was a period of major echinoderm evolution, especially during Mississippian (Early Car- boniferous) time when crinoids, blastoids, and echinoids increased dramatically in abundance and diversity. The high degree of structural organization and distinctive morphologies of echinoderms make them ideal zonal indicators, and for parts of the Appalachian Basin Mississippian section, they provide greater biostratigraphic resolution than do conodonts or foraminifera. The occurrence of various echinoderm groups in time and space, however, is clearly related to the tectonic and sedimentologic differentiation of the Appalachian Basin through time. By Early Mississippian time on the Laurussian continent, most echinoderms had already made the shift to clastic-rich environments, which predominated in the basin until Middle Mississippian time. Although present, well-preserved Kinderhookian, Osagean, and Meramecian echinoderms are rare in the Appalachian Basin, and most are endemic forms with little diagnostic value. Echinoderms did, however, become especially abundant in the succeeding, late Middle and early Late Mississippian (Late Meramecian–Middle Chesterian), carbonate-rich seas, and it is for this time interval that biostratigraphic resolution, based especially on crinoids and blastoids, is best.