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Silurian Rugose Corals of the Central and Southwest Great Basin
Silurian Rugose Corals of the Central and Southwest Great Basin GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 Silurian Rugose Corals of the Central and Southwest Great Basin By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 A stratigraphic-paleontologic investigation of rugose corals as aids in age detern2ination and correlation of Silurian rocks of the Great Basin with those of other regions UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600082 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price $2.15 (paper cover) Stock Number 2401-00363 CONTENTS Page Page Abstract--------------------------------------------------------------------------- 1 Systematic and descriptive palaeontology-Continued Introduction -------------------------------------------------------------------- 1 Family Streptelasmatidae-Continued Purpose and scope of investigation------------------------------- 1 Dalmanophyllum ------------------------------------------------- 32 History of investigation ---------------------------------------------- 1 Family Stauriidae ------------------------------------------------------- 32 Methods of study------------------------------------------------------- 2 Cyathoph y llo ides-------------------------------------------------- 32 Acknowledgments------------------------------------------------------- 4 Palaeophyllum -
Contents List of Illustrations LETTER OF
STATE OF MICHIGAN Plate IV. A. Horizontal and oblique lamination, Sylvania MICHIGAN GEOLOGICAL AND BIOLOGICAL SURVEY Sandstone......................................................................27 Plate IV. B. Stratification and lamination, in sand dune, Dune Publication 2. Geological Series 1. Park, Ind.........................................................................28 THE MONROE FORMATION OF SOUTHERN Plate V. Sand grains, enlarged 14½ times ............................31 MICHIGAN AND ADJOINING REGIONS Plate VI. Desert sand grains, enlarged 14½ times ................31 by Plate VII. Sylvania and St. Peter sand grains, enlarged 14½ A. W. Grabau and W. H. Sherzer times. .............................................................................32 PUBLISHED AS PART OF THE ANNUAL REPORT OF THE BOARD OF GEOLOGICAL AND BIOLOGICAL SURVEY FOR Figures 1909. Figure 1. Map showing distribution of Sylvania Sandstone. 25 LANSING, MICHIGAN WYNKOOP HALLENBECK CRAWFORD CO., STATE Figure 2. Cross bedding in Sylvania sandstone ....................27 PRINTERS Figure 3. Cross bedding on east wall of Toll’s Pit quarry ......28 1910 Figure 4. Cross bedding shown on south wall of Toll’s Pit quarry.............................................................................28 Contents Figure 5. Cross bedding on south wall of Toll’s Pit quarry in Sylvania sandstone. .......................................................28 Letter of Transmittal. ......................................................... 1 Figure 6. Cross bedding shown on south wall -
V/ New Cretaceous and Tertiary Decapod Crustaceans from Western
SCi^y^lfi^^ f-euyj^w/«v/ Bulletin of the Mizunami Fossil Museum, no. 28 (2001), p. 173-210, 19 figs., 3 tables. New Cretaceous and Tertiary decapod crustaceans from western North America Carrie E. Schweitzer and Rodney M. Feldmann Department of Geology, Kent State University, Kent, OH 44242, U.S.A. <[email protected]> and <[email protected]> Abstract Several new decapod crustaceans have been recovered from Cretaceous and Tertiary rocks of west- em North America. New species include Palaeastacus trisulcatus, Glyphea micheleae, Hoploparia tshudyi, Ctenocheles hokoensis, Callianopsis ? inornatus, Palaeopentacheles? starri, Eucorystes platys, Archaeopus lunicarina, Brecanclawu rathbunae gen. nov. amd sp. nov., Pagurus malloryi, Paguristes hokoensis. One new combination has resulted from this work, Paguristes subaequalis comb. nov. (Rathbun, 1926). Family level diagnostic characters of the chelae are given for each paguroid family; chelae are the only portion of paguroid decapods commonly preserved in the fossil record. Palaeopentacheles and Eucorystes appear to have had north polar distributions, and Glyphea and Palaeastacus have bipolar or amphitropical distributions, corroborating the patterns observed by Schweitzer (2001) for Cretaceous and Tertiary decapods of the North Pacific rim. Key words: Cretaceous, Cenozoic, Decapoda, North America Introduction much of that material was made available to us for study. Their collections were supplemented by those of geologists The history of study of fossil decapod crustaceans on the working in Alaska, often under the auspices of the U. S. west coast of North America has been disjunct. Several Geological Survey or petroleum companies. Numerous studies in the latter part of the lO"" Century and the early papers, cited in the work to follow, have resulted from the 20* Century resulted in the recognition of fossil decapods study of this material. -
University of Michigan University Library
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL.23, NO.5, p. 81-91, (4 pls.) JUNE 19, 1970 CORALS OF THE TRAVERSE GROUP OF MICHIGAN PART 13, HEXAGONARIA ERWIN C. STUMM MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Director: ROBERTV. KESLING The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collection in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals upon request. A list of the separate papers may also be obtained. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48104. VOLS.2-22. Parts of volumes may be obtained if available. Price lists available upon inquiry. 1. The rodents from the Hagerman local fauna, Upper Pliocene of Idaho, by Richard J. Zakrzewski. Pages 1-36, with 13 text-figures. 2. A new brittle-star from the Middle Devonian Arkona Shale of Ontario, by Robert V. Kesling. Pages 37-51, with 6 plates and 2 text-figures. 3. Phyllocarid crustaceans from the Middle Devonian Silica Shale of northwestern Ohio and southeastern Michigan, by Erwin C. Stumm and Ruth B. Chilman. Pages 53-71, with 7 plates and 4 text-figures. 4. Drepanaster wrighti, a new species of brittle-star from the Middle Devonian Arkona Shale of Ontario, by Robert V. Kesling. Pages 73-79, with 2 plates. -
Basal Metazoans - Dirk Erpenbeck, Simion Paul, Michael Manuel, Paulyn Cartwright, Oliver Voigt and Gert Worheide
EVOLUTION OF PHYLOGENETIC TREE OF LIFE - Basal Metazoans - Dirk Erpenbeck, Simion Paul, Michael Manuel, Paulyn Cartwright, Oliver Voigt and Gert Worheide BASAL METAZOANS Dirk Erpenbeck Ludwig-Maximilians Universität München, Germany Simion Paul and Michaël Manuel Université Pierre et Marie Curie in Paris, France. Paulyn Cartwright University of Kansas USA. Oliver Voigt and Gert Wörheide Ludwig-Maximilians Universität München, Germany Keywords: Metazoa, Porifera, sponges, Placozoa, Cnidaria, anthozoans, jellyfishes, Ctenophora, comb jellies Contents 1. Introduction on ―Basal Metazoans‖ 2. Phylogenetic relationships among non-bilaterian Metazoa 3. Porifera (Sponges) 4. Placozoa 5. Ctenophora (Comb-jellies) 6. Cnidaria 7. Cultural impact and relevance to human welfare Glossary Bibliography Biographical Sketch Summary Basal metazoans comprise the four non-bilaterian animal phyla Porifera (sponges), Cnidaria (anthozoans and jellyfishes), Placozoa (Trichoplax) and Ctenophora (comb jellies). The phylogenetic position of these taxa in the animal tree is pivotal for our understanding of the last common metazoan ancestor and the character evolution all Metazoa,UNESCO-EOLSS but is much debated. Morphological, evolutionary, internal and external phylogenetic aspects of the four phyla are highlighted and discussed. SAMPLE CHAPTERS 1. Introduction on “Basal Metazoans” In many textbooks the term ―lower metazoans‖ still refers to an undefined assemblage of invertebrate phyla, whose phylogenetic relationships were rather undefined. This assemblage may contain both bilaterian and non-bilaterian taxa. Currently, ―Basal Metazoa‖ refers to non-bilaterian animals only, four phyla that lack obvious bilateral symmetry, Porifera, Placozoa, Cnidaria and Ctenophora. ©Encyclopedia of Life Support Systems (EOLSS) EVOLUTION OF PHYLOGENETIC TREE OF LIFE - Basal Metazoans - Dirk Erpenbeck, Simion Paul, Michael Manuel, Paulyn Cartwright, Oliver Voigt and Gert Worheide These four phyla have classically been known as ―diploblastic‖ Metazoa. -
AR 1904 Part 1
REPORT PART I. THE PREORDOVICIAN OF THE BY STATE BOARD OF GEOLOGICAL SURVEY A. C. LANE AND A. E. SEAMAN OF MICHIGAN REVISED AND ENLARGED FROM AN ARTICLE IN THE JOURNAL FOR THE YEAR 1908 OF GEOLOGY, VOL. XV, NO. 7, OCT.-NOV., 1907. GEOLOGY INTRODUCTION. ALFRED C. LANE STATE GEOLOGIST It is not as easy to summarize the section of Michigan as, for instance, a compact state like Iowa. For one MAY 18, 1910 thing the state is so spread out that, turned around by its southeast corner on the map, it would reach beyond BY AUTHORITY New York into the Atlantic Ocean, and turned around by LANSING, MICHIGAN its northwest corner, would extend to Hudson's Bay and WYNKOOP HALLENBECK CRAWFORD CO., STATE PRINTERS into the Dakotas. Again it includes within its borders 1909 representatives of probably the oldest land masses, NOTES which have been frequently, if not continuously, above ON THE sea level ever since they were first elevated. The GEOLOGICAL SECTION geological succession may therefore be expected to be interspersed with beds laid down on land and in lakes OF MICHIGAN fresh and salt, and seas like the Caspian and Black, by FOR stream and wind, as well as wave. GEOLOGISTS, TEACHERS AND DRILLERS Part I includes the pre-Trenton rocks which even the drill has not reached in the Lower Peninsula. Contents In preparing these notes the state geologist had assistance from Professor Seaman of the College of PART I. THE PREORDOVICIAN..................................... 1 Mines as to the older rocks to such an extent that it may PART II. -
Iii Silurian Fauna
III SILURIAN FAUNA By AUGUST F. FOERSTE THE SILURIAN FAUNA OF KENTUCKY By AUGUST F. FOERSTE THE SOURCE AND AFFINITIES OF THE SILURIAN FAUNAS In prehistoric times the North American continent was invaded by oceanic faunas from various directions. The tilting of the continent toward the south permitted the invasion of oceanic faunas from the Gulf of Mexico, and tilting toward the east, permitted invasions from the North Atlantic. There have been invasions also from the Arctic and Pacific. Some of these invasions extended far inland. Some from the Gulf of Mexico spread northward along the Mississippi embayment as far as the southern part of Canada, and some from the North Atlantic reached Ohio and Kentucky. As far as known, none of the invasions from the Arctic or Pacific reached Kentucky. In most Silurian faunas, the brachiopod element predominates. Three of the southern invasions—the Brassfield, Osgood, and Waldron—are characterized by the abundance of bryozoans, in addition to the brachiopods. The Brassfield and Waldron contain also a considerable number of gastropods, pelecypods, cephalopods, and trilobites, all of which are relatively scarce in the Osgood and Louisville. In the Osgood, on the contrary, there are numerous cystids, though almost all of these were described originally under the single generic name Holocystites. The Waldron is characterized by the considerable variety of crinoids. In the Laurel and Louisville bryozoans are rare. The Laurel is now characterized by numerous species of crinoids, a considerable number of which show affinities with crinoids occurring in Gotland and England. Possibly these invaded the American continent from some North Atlantic source. -
Upper Carboniferous Corals from the Nagaiwa Series, Southern Kitakami Mountains, N.E
Title Upper Carboniferous Corals from the Nagaiwa Series, Southern Kitakami Mountains, N.E. Japan Author(s) Minato, Masao; Kato, Makoto Citation Journal of the Faculty of Science, Hokkaido University. Series 4, Geology and mineralogy, 16(2-3), 43-119 Issue Date 1974-11 Doc URL http://hdl.handle.net/2115/36031 Type bulletin (article) File Information 16(2-3)_43-120.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP 43 UPPER CARBONIFEROUS CORALS FROM THE NAGAIWA SERIES, SOUTHERN KITAKAMI MOUNTAINS, N.E. JAPAN by Masao MINATo and Makoto KATo (With 7 Text-figures and 16 Plates) (Contribution from the Department of Geology and Mineralogy, Faculty of Science, Hokkaido University, No. 1373) Introduction In the southern Kitakami Mountains, N. E. Japan, rich limestone resources have been found to develop within Palaeozoic sequence ranging from Silurian to Permian, At present mainly Permian limestones are extensively quarried for cement industry. l414s'E ''4iG"OEisi Kamaishi !.YOMOGIeArAN. city N't"1-isABUKURAIS--."N".i:,gf,;,lr"EFi.SN,sA{s:trt/I,P,,T,O,,8,Aei4eeONtMARU' MAT5UBi IWSumita-cho .gpt"taq..dipt'`ta"'.-h.3s" 1d .t'N')Sanriku- e5ErAMAit t,'N.Noi""'"'INKo)gtUiueosAwA'N.N--s.×N.lkMAGOE -". cho - s, Ohfunato City yuKisArvAN. `', >" Rikuzen±akada "k city d . b 39ON-i " ,N. xg -v"ptxY"N-x gNk 9>+ MIYAGIPREF. O510km Fig. 1. The Southern Kitakami Mountains, showing chief localities wherein coral-bearing Nagaiwa series occurs. 44 M, MtNATo and M, KATo In old days, Palaeozoic limestones in Japan were considered exclusively of Permian age, thus were assumed to bear fusulinids. -
U.S. Government Publishing Office Style Manual
Style Manual An official guide to the form and style of Federal Government publishing | 2016 Keeping America Informed | OFFICIAL | DIGITAL | SECURE [email protected] Production and Distribution Notes This publication was typeset electronically using Helvetica and Minion Pro typefaces. It was printed using vegetable oil-based ink on recycled paper containing 30% post consumer waste. The GPO Style Manual will be distributed to libraries in the Federal Depository Library Program. To find a depository library near you, please go to the Federal depository library directory at http://catalog.gpo.gov/fdlpdir/public.jsp. The electronic text of this publication is available for public use free of charge at https://www.govinfo.gov/gpo-style-manual. Library of Congress Cataloging-in-Publication Data Names: United States. Government Publishing Office, author. Title: Style manual : an official guide to the form and style of federal government publications / U.S. Government Publishing Office. Other titles: Official guide to the form and style of federal government publications | Also known as: GPO style manual Description: 2016; official U.S. Government edition. | Washington, DC : U.S. Government Publishing Office, 2016. | Includes index. Identifiers: LCCN 2016055634| ISBN 9780160936029 (cloth) | ISBN 0160936020 (cloth) | ISBN 9780160936012 (paper) | ISBN 0160936012 (paper) Subjects: LCSH: Printing—United States—Style manuals. | Printing, Public—United States—Handbooks, manuals, etc. | Publishers and publishing—United States—Handbooks, manuals, etc. | Authorship—Style manuals. | Editing—Handbooks, manuals, etc. Classification: LCC Z253 .U58 2016 | DDC 808/.02—dc23 | SUDOC GP 1.23/4:ST 9/2016 LC record available at https://lccn.loc.gov/2016055634 Use of ISBN Prefix This is the official U.S. -
Publication 38. Geological Series 32 OIL and GAS FIELDS of MICHIGAN
STATE OF MICHIGAN CHAPTER IV. Historical Geology ................................37 DEPARTMENT OF CONSERVATION Difficulties in tracing the evolution of the synclinal George E. Hogarth, Director basin.............................................................................37 GEOLOGICAL SURVEY DIVISION Paleozoic Era ...............................................................37 R. A. Smith, State Geologist Cambrian Period.................................................... 37 Lake Superior Time....................................................37 Publication 38. Geological Series 32 Ordovician Period .................................................. 37 OIL AND GAS FIELDS OF MICHIGAN Ozarkian Time............................................................37 Canadian Time...........................................................37 A DISCUSSION OF DEPOSITIONAL AND STRUCTURAL St. Peter Time ............................................................37 FEATURES OF THE MICHIGAN BASIN Trenton-Black River Time ..........................................38 Decorah Time.............................................................38 BY ROBERT B. NEWCOMBE Cincinnatian Time ......................................................38 Silurian Period ....................................................... 38 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE Cataract Time.............................................................38 REQUIREMENTS FOR THE DEGREE OF DOCTOR OF Niagaran Time............................................................38 -
Canada Archives Canada Published Heritage Direction Du Branch Patrimoine De I'edition
THE BURGESS SHALE: A CAMBRIAN MIRROR FOR MODERN EVOLUTIONARY BIOLOGY by Keynyn Alexandra Ripley Brysse A thesis submitted in conformity with the requirements for the degree of Doctor of Philosophy Institute for the History and Philosophy of Science and Technology University of Toronto © Copyright by Keynyn Alexandra Ripley Brysse (2008) Library and Bibliotheque et 1*1 Archives Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-44745-1 Our file Notre reference ISBN: 978-0-494-44745-1 NOTICE: AVIS: The author has granted a non L'auteur a accorde une licence non exclusive exclusive license allowing Library permettant a la Bibliotheque et Archives and Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par Plntemet, prefer, telecommunication or on the Internet, distribuer et vendre des theses partout dans loan, distribute and sell theses le monde, a des fins commerciales ou autres, worldwide, for commercial or non sur support microforme, papier, electronique commercial purposes, in microform, et/ou autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in et des droits moraux qui protege cette these. this thesis. Neither the thesis Ni la these ni des extraits substantiels de nor substantial extracts from it celle-ci ne doivent etre imprimes ou autrement may be printed or otherwise reproduits sans son autorisation. -
Review of Fossil Collections in Scotland Scotland South Scotland South
Detail of Permian footprints Chelichnus duncani in sandstone from Dumfries and Galloway. Dumfries Museum and Camera Obscura. © Dumfries and Galloway Council Museums Service Review of Fossil Collections in Scotland Scotland South Scotland South Dumfries Museum and Camera Obscura (Dumfries and Galloway Council) Sanquhar Tolbooth Museum (Dumfries and Galloway Council) Stranraer Museum (Dumfries and Galloway Council) Gem Rock Museum Newton Stewart Museum Tweeddale Museum (Live Borders) Hawick Museum (Live Borders) 1 Dumfries Museum and Camera Obscura (Dumfries and Galloway Council) Collection type: Local authority Accreditation: 2018 The Observatory, Rotchell Road, Dumfries, DG2 7SW Contact: [email protected] Location of collections The original Museum was located in a windmill dating from the late 1700s, preserved in the 1830s by the newly-formed Dumfries and Maxwelltown Astronomical Society for use as an observatory. An extension built in the 1860s added a large gallery and mezzanine level with further gallery and storage space added in the 1980s. Collections are onsite in displays and a main storeroom. Size of collections 1,000-1,200 fossils. Onsite records Information is in an Adlib CMS database transcribed from several previous electronic systems and various paper documents, such as MDA and other index card systems, Gift Books, Accession Registers, free text catalogues, inventories and listings. Fossils are catalogued with other geological material as a series of numbered boxes with a list compiled in the 1980s by James Williams (1944- 2009). An online catalogue is available at: https://dgc-web.adlibhosting.com/home but does not yet contain fossil entries. Collection highlights 1. Permian vertebrate trackways from Locharbriggs and Corncockle quarries linked to Reverend Henry Duncan (1774-1846) and former curator Alfred Truckell (1919-2007).