Fielding Bradford Meek
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Crinoidea, Echinodermata) from Poland
Title: Uncovering the hidden diversity of Mississippian crinoids (Crinoidea, Echinodermata) from Poland Author: Mariusz A. Salamon, William I. Ausich, Tomasz Brachaniec, Bartosz J. Płachno, Przemysław Gorzelak Citation style: Salamon Mariusz A., Ausich William I., Brachaniec Tomasz, Płachno Bartosz J., Gorzelak Przemysław. (2020). Uncovering the hidden diversity of Mississippian crinoids (Crinoidea, Echinodermata) from Poland. "PeerJ" Vol. 8 (2020), art. no e10641, doi 10.7717/peerj.10641 Uncovering the hidden diversity of Mississippian crinoids (Crinoidea, Echinodermata) from Poland Mariusz A. Salamon1, William I. Ausich2, Tomasz Brachaniec1, Bartosz J. Pªachno3 and Przemysªaw Gorzelak4 1 Faculty of Natural Sciences, Institute of Earth Sciences, University of Silesia in Katowice, Sosnowiec, Poland 2 School of Earth Sciences, Ohio State University, Columbus, OH, United States of America 3 Faculty of Biology, Institute of Botany, Jagiellonian University in Kraków, Cracow, Poland 4 Institute of Paleobiology, Polish Academy of Sciences, Poland, Warsaw, Poland ABSTRACT Partial crinoid crowns and aboral cups are reported from the Mississippian of Poland for the first time. Most specimens are partially disarticulated or isolated plates, which prevent identification to genus and species, but regardless these remains indicate a rich diversity of Mississippian crinoids in Poland during the Mississippian, especially during the late Viséan. Lanecrinus? sp. is described from the late Tournaisian of the D¦bnik Anticline region. A high crinoid biodiversity occurred during late Viséan of the Holy Cross Mountains, including the camerate crinoids Gilbertsocrinus? sp., Platycrinitidae Indeterminate; one flexible crinoid; and numerous eucladid crinoids, including Cyathocrinites mammillaris (Phillips), three taxa represented by partial cups left in open nomenclature, and numerous additional taxa known only from isolated radial plates, brachial plates, and columnals. -
Palaeoecology and Taphonomy of a Fossil Sea Floor, in the Carboniferous Limestone of Northern England Stephen K
Palaeoecology and taphonomy of a fossil sea floor, in the Carboniferous Limestone of northern England Stephen K. Donovan Abstract: Death assemblages preserved on bedding planes - fossil ‘sea floors’ - are important palaeontological sampling points. A fossil sea floor from Salthill Quarry (Mississippian), Clitheroe, Lancashire, preserves a mixture of crinoid debris with rarer tabulate corals and has yielded a rich diversity of palaeoecological information. Identifiable crinoids includeGilbertsocrinus sp. and a platycrinitid, associated with columnals/ pluricolumnals, brachials/arms and a basal circlet, crinoid-infesting tabulate corals such as Cladochonus sp. and Emmonsia parasitica (Phillips), and the spoor of a pit-forming organism. Long pluricolumnals showing sub-parallel orientations suggest a current azimuth; one coral is silicified with the mineral beekite. Biotic interactions between ancient organisms Studies of fossil bedding planes and the include the obvious, the subtle and the problematic palaeontological associations preserved thereon are not (Boucot 1990). Obvious associations include the currently in vogue in palaeontology, where the database direct evidence provided by cephalopod hooks (=prey) is currently more important than the unique specimen; preserved in the stomachs of predatory ichthyosaurs it may be that bedding planes are currently more (Pollard, 1968), and intergrowths of Pliocene corals, important as sources of information to sedimentologists bryozoans and barnacles (Harper, 2012). Subtle and ichnologists. Perhaps -
Bivalvia, Late Jurassic) from South America
Author's personal copy Pala¨ontol Z DOI 10.1007/s12542-016-0310-z RESEARCH PAPER Huncalotis, an enigmatic new pectinoid genus (Bivalvia, Late Jurassic) from South America 1 2 Susana E. Damborenea • He´ctor A. Leanza Received: 29 September 2015 / Accepted: 16 March 2016 Ó Pala¨ontologische Gesellschaft 2016 Abstract The extensive outcrops of the Late Jurassic– orientated at right angles to the shell margins. A few speci- Early Cretaceous Vaca Muerta Formation black shales and mens were found on the outside of large calcareous con- marls in the Neuque´n Basin have yielded very few bivalves, cretions within black shales; these are often articulated, and these are not well known. The material described here complete shells, which preserve the original convexity of the was collected in central Neuque´n, from late Tithonian cal- valves. In some cases these articulated shells seem to be careous levels within the black shales, between beds with associated with large ammonite shells, suggesting an epi- Substeueroceras sp. and with Argentiniceras noduliferum byssate (possibly also pseudoplanktonic) lifestyle. (Steuer). The material is referred to the new genus Huncalotis and to the new species H. millaini. The strongly Keywords Late Tithonian Á Neuque´n Basin Á Vaca inequivalve shells, the ligamental area with a triangular Muerta Formation Á Argentina Á Peru Á Bivalvia Á slightly prosocline resilifer, the right valve with ctenolium Pectinoidea Á Pectinidae and a very deep byssal notch, and the lack of radial orna- mentation make the shell of this new genus strikingly similar Kurzfassung Die reichlich zutage tretenden Schwarz- to the Triassic pectinid Pleuronectites. -
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--.-------.- ___________________ -
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. -
SGSI 7 013-034 Amler.Indd 13 11-11-10 08:47 14 Amler
Late Devonian (Frasnian) bivalves from the Nocedo Formation – the results of Wilhelm Kegel’s 1927 field trip to northern Spain Michael R.W. Amler Amler, M.R.W. Late Devonian (Frasnian) bivalves from the Nocedo Formation – the results of Wil- helm Kegel’s 1927 field trip to northern Spain. Scripta Geologica Special Issue, 7: 13-34, 9 figs., Leiden, December 2010. Michael R.W. Amler, Department für Geo- und Umweltwissenschaften, Sektion Geologie, and Geo- Biocenter Munich, Ludwig-Maximilians-Universität München, Luisenstr. 37, D-80333 München, Ger- many ([email protected]), and Institut für Geologie und Paläontologie im Fachbereich Geographie der Philipps-Universität Marburg, Hans-Meerwein-Str., D-35032 Marburg, Germany ([email protected]). Key words — Bivalvia, Rhenish Facies, Nocedo Formation, Frasnian, Cantabrian Mountains, Iberia, Wilhelm Kegel. During a field trip to the Peña-Corada Unit of the southernmost Esla region of the Cantabrian Moun- tains in 1927, the German stratigrapher Wilhelm Kegel sampled brachiopods and bivalves from a section in the Laoz valley near La Ercina. The stratigraphic position is believed to be part of the No- cedo Formation of Frasnian age. This fauna includes poorly preserved steinkerns of a near-shore bi- valve fauna that was prepared for publication including labels and proposed names, but never pub- lished. The fauna represents only a very small and random part of the former community. But as in- formation on Frasnian bivalves is scarce, the few specimens add important information on the distri- bution and palaeogeographic occurrence of near-shore, that is, Rhenish Facies bivalves within the south Laurussian – Rheic Ocean Realm. -
Geology of the Cayuga Lake Basin New York State
I GEOLOGY OF THE CAYUGA LAKE BASIN NEW YORK STATE GEOLOGICAL ASSOCIATION 31 sT ANNUAL MEETING CORNELL UNIVERSITY, MAY 8-9» 1959 GEOLOGY OF THE CAYUGA LAKE BASIN A Guide for the )lst Annual Field Meeting of the New York State Geological Association prepared by Staff and Students of the Department of Geolqgy Cornell Universit,y ".080 We must especially collect and describe all the organic remains of our soil, if we ever want to speculate with the smallest degree of probabilit,r on the formation, respective age, and history of our earth .. " ------ C. S. Rafinesque, 1818 Second (Revised) Edition Ithaca, New York May, 1959 PREFACE Ten years have passed since Cornell was host to the New York state Geological Association. In the intervening yearllf we have attended the annual meetings and field trips at other places with pleasure and profit. Therefore, we take this opportunity to express our appreciation and thanks to all of those who have made theBe meetings possible. We not ~ welcome you to Cornell and the classic cayuga Lake Basin, but we sincerely hope you will en ja,y and profit by your brief excursions with us. This guide is a revision of one prepared for the 1949 annual meeting. Professor John W.. Wells assumed most of the responsi bility for its preparation, ably assisted by Lo R. Fernow, Fe M. Hueber and K.. No Sachs, Jro Without their efforts in converting ideas into diagrams and maps this guide book would have been sterile. we hope that before you leave us, you will agree with Louis Agassiz, who said in one of his lectures during the first year of Cornell, "I was never before in a single locality where there is presented so much ma. -
The Texan Permian and Its Mesozoic Types of Fossils.. .1891
WHITE, C.A. ...The Texan Permian and its Mesozoic types of fossils.. .1891. I*- b37(245 ¥58 jj DEPARTMENT OP THE INTERIOR OF THK UNITED STATES GEOLOGICAL SURVEY No. 77 THE TEXAN PERMIAN AND ITS MESOZOIC TYPES OF FOSSILS WASHINGTON GOVERNMENT PRINTING OFFICE 1891 LIBRARY CATALOGUE SLIPS. United States, Department of the interior. (U. S. geological survey). Department of the interior |- | Bulletin | of the | United States | geological survey | mo. 77 | [Seal of the department] | Washington \ government printing office | 1891 Second title: United States geological survey | J. W. Powell, director | | The Texau Permian | and its | Mesozoio types of fossils | by | Charles A. White | [Vignette] | Washington | government printing office | 1891 8°. 5lpp. 4 pi. White (Charles A.). United States geological survey | J.W. Powell, director | The Texau Permian | audits | Mesozoic types of fossils | by | Charles A. White | [Vignette] | Washington | government printing office | 1891. 8«. 5t pp. 4 pi. [UNITED STATES. Department of the interior. (U. S. geological survey). Bulletin 77.] United States geological survey J. W. Powell, director | | The Texan Permian | and its | Mesozoic types of fossils | by | Charles A. White | [Vignette] | Washingto:a | government printing office | 1891 8". 5lpp. 4 pi. [UNITED STATES. Department <tf the interior. (U. S. geological survey). Bnlletin 77.] A.D'VBRTISEMKN'T. [Bulletin No. 77.] The publications of the United States Geological Survey are issued in accordance with the statute approved March 3, 1879, which declares that "Thepublicationsof tb.eGeological Survey shall consist of the annual report of operations, geological and economic maps illustrating the resources and classification of the lauds, and reports upon general and economic geology and paleontology. -
Epibionts on Upper Eifelian Crinoid Columnals from the Holy Cross Mountains, Poland
Epibionts on upper Eifelian crinoid columnals from the Holy Cross Mountains, Poland EDWARD GŁUCHOWSKI Głuchowski, E. 2005. Epibionts on upper Eifelian crinoid columnals from the Holy Cross Mountains, Poland. Acta Palaeontologica Polonica 50 (2): 315–328. Most of 378 upper Eifelian crinoid columnals collected from the lower part of Skały Beds in the Holy Cross Mountains display traces of borings produced by endobionts, but only approximately 20% of them show traces of epibionts. These infested crinoids are represented by 5 stem−based species: Tantalocrinus scutellus, Schyschcatocrinus creber, Gilbertso− crinus vetulus, Pentagonostipes petaloides, and Cycloocetocrinus sp. They were fouled by 19 species of suspension−feed− ing epibionts, including saccamminid foraminiferans, rugose and tabulate corals, cyrtinitid and productid brachiopods, “ctenostome bryozoans”, “cyclostome bryozoans”, cystoporate bryozoans, and rhabdomesid? bryozoans, crinoids, and organisms of uncertain affinities. The majority of these epibionts were opportunistic commensals colonizing living cri− noids, and only some utilized dead crinoids as hard substrate for attachment. At least some of these epibionts seem to have settled selectively on particular crinoid host species. Key words: Epibionts, crinoids, host−selectivity, Skały Beds, Eifelian, Holy Cross Mountains. Edward Głuchowski [[email protected]], Wydział Nauk o Ziemi, Uniwersytet Śląski, ul. Będzińska 60, PL−41−200 Sosnowiec, Poland. Introduction Geological setting Many modern and ancient marine hard substratum commu− The Grzegorzowice−Skały section is situated in the eastern nities have been documented by numerous authors (for re− part of the Bodzentyn Syncline in the Łysogóry region of view, see Taylor and Wilson 2003). These hard substrata in− the Holy Cross Mountains. Investigations of Lower and clude sedimentary hardgrounds and rock clasts, as well as the Middle Devonian strata in this section have a long history skeletons of living and dead organisms. -
Predation, Resistance, and Escalation in Sessile Crinoids
Predation, resistance, and escalation in sessile crinoids by Valerie J. Syverson A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology) in the University of Michigan 2014 Doctoral Committee: Professor Tomasz K. Baumiller, Chair Professor Daniel C. Fisher Research Scientist Janice L. Pappas Professor Emeritus Gerald R. Smith Research Scientist Miriam L. Zelditch © Valerie J. Syverson, 2014 Dedication To Mark. “We shall swim out to that brooding reef in the sea and dive down through black abysses to Cyclopean and many-columned Y'ha-nthlei, and in that lair of the Deep Ones we shall dwell amidst wonder and glory for ever.” ii Acknowledgments I wish to thank my advisor and committee chair, Tom Baumiller, for his guidance in helping me to complete this work and develop a mature scientific perspective and for giving me the academic freedom to explore several fruitless ideas along the way. Many thanks are also due to my past and present labmates Alex Janevski and Kris Purens for their friendship, moral support, frequent and productive arguments, and shared efforts to understand the world. And to Meg Veitch, here’s hoping we have a chance to work together hereafter. My committee members Miriam Zelditch, Janice Pappas, Jerry Smith, and Dan Fisher have provided much useful feedback on how to improve both the research herein and my writing about it. Daniel Miller has been both a great supervisor and mentor and an inspiration to good scholarship. And to the other paleontology grad students and the rest of the department faculty, thank you for many interesting discussions and much enjoyable socializing over the last five years. -
Proquest Dissertations
INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from tfie original or copy submitled. Thus, some ttiesis 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 t>leedthrough, sut)standard margins, and improper alignment can adversely affect reproduction. In the unlikely event tfiat the autfior did not send UMI a complete manuscript and there are missing pages, tfrese will be noted. Also, if unautfiorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced t>y sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Photographs included in tfie original manuscript have been reproduced xerographically in this copy. Higher quality 6" x 9" black and white photographic prints are available for any ptwtographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. Bell & Howell Information and teaming 300 North zeeb Road, Ann Arbor, Ml 4810B>1346 USA 800-521-0600 UMI* PALEONTOLOGY AND PALEOECOLOGY OF THE NADA MEMBER OF THE BORDEN FORMATION (LOWER MISSISSIPPIAN) IN EASTERN KENTUCKY DISSERTATION Presented in Partial Fullfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Aiguo Li, M.S. ***** The Ohio State University 2000 Dissertation Committee: Dr.