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Bull. Geol. Soc. Am. Vol. 46, 1935, Pl. 33
BULL. GEOL. SOC. AM. VOL. 46, 1935, PL. 33 F ig u r e 2. E a stern F a ce o f t h e Q uarry DUNDEE-ANDERDON CONTACT IN SIBLEY QUARRY Downloaded from http://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/46/3/425/3415212/BUL46_3-0425.pdf by guest on 01 October 2021 BULLETIN OF THE GEOLOGICAL SOCIETY CfF A M E R IC A VOL. 46, PP. 428-462, PLS. 33-39, 1 FIG. MARCH 31. 1935 PROCEEDINGS OF THE PALEONTOLOGICAL SOCIETY STRATIGRAPHY AND PALEONTOLOGY OF THE DUNDEE LIMESTONE OF SOUTHEASTERN MICHIGAN* BY CHARLES FERNANDO BASSETT (Presented before the Paleontological Society, December SO, 193S) CONTENTS Page Introduction............................................................................................................. 425 Statement of the problem................................................................................ 425 Acknowledgments............................................................................................. 427 Stratigraphy of the Dundee limestone................................................................... 427 Distribution....................................................................................................... 427 Previous classification...................................................................................... 427 Description of sections..................................................................................... 428 Sibley quarry............................................................................................. 428 Christiancy or Macon quarry................................................................. -
Cambrian Ordovician
Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation. -
Middle Devonian Formations in the Subsurface of Northwestern Ohio
STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 SCIENTIFIC AND TECHNICAL STAFF OF THE OHIO DIVISION OF GEOLOGICAL SURVEY ADMINISTRATIVE SECTION Horace R. Collins, State Geologist and Di v ision Chief David K. Webb, Jr., Geologist and Assistant Chief Eleanor J. Hyle, Secretary Jean S. Brown, Geologist and Editor Pauline Smyth, Geologist Betty B. Baber, Geologist REGIONAL GEOLOGY SECTION SUBSURFACE GEOLOGY SECTION Richard A. Struble, Geologist and Section Head William J. Buschman, Jr., Geologist and Section Head Richard M. Delong, Geologist Michael J. Clifford, Geologist G. William Kalb, Geochemist Adriaan J anssens, Geologist Douglas L. Kohout, Geologis t Frederick B. Safford, Geologist David A. Stith, Geologist Jam es Wooten, Geologist Aide Joel D. Vormelker, Geologist Aide Barbara J. Adams, Clerk· Typist B. Margalene Crammer, Clerk PUBLICATIONS SECTION LAKE ERIE SECTION Harold J. Fl inc, Cartographer and Section Head Charles E. Herdendorf, Geologist and Sectwn Head James A. Brown, Cartographer Lawrence L. Braidech, Geologist Donald R. Camburn, Cartovapher Walter R. Lemke, Boat Captain Philip J. Celnar, Cartographer David B. Gruet, Geologist Aide Jean J. Miller, Photocopy Composer Jean R. Ludwig, Clerk- Typist STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY Horace R. Collins, Chief Report of Investigations No. 78 MIDDLE DEVONIAN FORMATIONS IN THE SUBSURFACE OF NORTHWESTERN OHIO by A. Janssens Columbus 1970 GEOLOGY SERVES OHIO CONTENTS Page Introduction . 1 Previous investigations .. .. .. .. .. .. .. .. .. 1 Study methods . 4 Detroit River Group . .. .. .. ... .. ... .. .. .. .. .. .. .. ... .. 6 Sylvania Sandstone .......................... -
Ordovician Land Plants and Fungi from Douglas Dam, Tennessee
PROOF The Palaeobotanist 68(2019): 1–33 The Palaeobotanist 68(2019): xxx–xxx 0031–0174/2019 0031–0174/2019 Ordovician land plants and fungi from Douglas Dam, Tennessee GREGORY J. RETALLACK Department of Earth Sciences, University of Oregon, Eugene, OR 97403, USA. *Email: gregr@uoregon. edu (Received 09 September, 2019; revised version accepted 15 December, 2019) ABSTRACT The Palaeobotanist 68(1–2): Retallack GJ 2019. Ordovician land plants and fungi from Douglas Dam, Tennessee. The Palaeobotanist 68(1–2): xxx–xxx. 1–33. Ordovician land plants have long been suspected from indirect evidence of fossil spores, plant fragments, carbon isotopic studies, and paleosols, but now can be visualized from plant compressions in a Middle Ordovician (Darriwilian or 460 Ma) sinkhole at Douglas Dam, Tennessee, U. S. A. Five bryophyte clades and two fungal clades are represented: hornwort (Casterlorum crispum, new form genus and species), liverwort (Cestites mirabilis Caster & Brooks), balloonwort (Janegraya sibylla, new form genus and species), peat moss (Dollyphyton boucotii, new form genus and species), harsh moss (Edwardsiphyton ovatum, new form genus and species), endomycorrhiza (Palaeoglomus strotheri, new species) and lichen (Prototaxites honeggeri, new species). The Douglas Dam Lagerstätte is a benchmark assemblage of early plants and fungi on land. Ordovician plant diversity now supports the idea that life on land had increased terrestrial weathering to induce the Great Ordovician Biodiversification Event in the sea and latest Ordovician (Hirnantian) -
76-9949 CHAPEL, James David, 1948- PETROLOGY and DEPOSITIONAL HISTORY of DEVONIAN CARBONATES in OHIO
76-9949 CHAPEL, James David, 1948- PETROLOGY AND DEPOSITIONAL HISTORY OF DEVONIAN CARBONATES IN OHIO. The Ohio State University, Ph.D., 1975 Geology Xerox University Microfilms,Ann Arbor, Michigan 48106 PETROLOGY AND EEPOSITIONAL HISTORY OF. DEVONIAN CARBONATES IN OHIO DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Chio State University bY Janes David Chapel, B.A, * * * * * The Ohio State University Reading Coirmittee: Approved Ey Professor Charles H. Summerson Professor Kenneth 0. Stanley //?//? Professor James W. Collinson v Adviser Department of Geology and Mineralogy ACKNOWIEDGMENTS ivy deepest thanks go to Dr. C. H. Summerson for his guidance and encouragement during the course of the research and for his critical reading of several drafts of the manuscript. I also wish to thank Dr. J. W. Collinson and Dr. K. 0. Stanley for their discussion and criticism of material presented in this dissertation. Special thanks go to Mr. A. Janssens of the Ohio Division of Geological Survey who discussed stratigraphic problems with the author on several occasions and provided access to unpublished stratigraphic data. I am especially indebted to the owners and officials of numerous stone companies who permitted me to study the sections in their quarries and who, in some cases, provided access to drill cores. In this regard \ special thanks are. extended to Mr. B. Mascn of the Prance Stone Company and Mr. R. Annesser of the National lime and Stone Company without whose cooperation and assistance this study would have been impossible. I also acknowledge financial support provided by the Friends of Ortcr. -
Detroit River Group in the Michigan Basin
GEOLOGICAL SURVEY CIRCULAR 133 September 1951 DETROIT RIVER GROUP IN THE MICHIGAN BASIN By Kenneth K. Landes UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Washington, D. C. Free on application to the Geological Survey, Washington 25, D. C. CONTENTS Page Page Introduction............................ ^ Amherstburg formation................. 7 Nomenclature of the Detroit River Structural geology...................... 14 group................................ i Geologic history ....................... ^4 Detroit River group..................... 3 Economic geology...................... 19 Lucas formation....................... 3 Reference cited........................ 21 ILLUSTRATIONS Figure 1. Location of wells and cross sections used in the study .......................... ii 2. Correlation chart . ..................................... 2 3. Cross sections A-«kf to 3-G1 inclusive . ......................;.............. 4 4. Facies map of basal part of Dundee formation. ................................. 5 5. Aggregate thickness of salt beds in the Lucas formation. ........................ 8 6. Thickness map of Lucas formation. ........................................... 10 7. Thickness map of Amherstburg formation (including Sylvania sandstone member. 11 8. Lime stone/dolomite facies map of Amherstburg formation ...................... 13 9. Thickness of Sylvania sandstone member of Amherstburg formation.............. 15 10. Boundary of the Bois Blanc formation in southwestern Michigan. -
Ocean Circulation As a Driver for Changes in Ocean Chemistry in the Middle Ordovician of Argentina
University of Tennessee, Knoxville TRACE: Tennessee Research and Creative Exchange Doctoral Dissertations Graduate School 5-2018 Ocean Circulation as a Driver for Changes in Ocean Chemistry in the Middle Ordovician of Argentina Miles Anthony Henderson University of Tennessee, [email protected] Follow this and additional works at: https://trace.tennessee.edu/utk_graddiss Recommended Citation Henderson, Miles Anthony, "Ocean Circulation as a Driver for Changes in Ocean Chemistry in the Middle Ordovician of Argentina. " PhD diss., University of Tennessee, 2018. https://trace.tennessee.edu/utk_graddiss/4885 This Dissertation is brought to you for free and open access by the Graduate School at TRACE: Tennessee Research and Creative Exchange. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of TRACE: Tennessee Research and Creative Exchange. For more information, please contact [email protected]. To the Graduate Council: I am submitting herewith a dissertation written by Miles Anthony Henderson entitled "Ocean Circulation as a Driver for Changes in Ocean Chemistry in the Middle Ordovician of Argentina." I have examined the final electronic copy of this dissertation for form and content and recommend that it be accepted in partial fulfillment of the equirr ements for the degree of Doctor of Philosophy, with a major in Geology. Linda C. Kah, Major Professor We have read this dissertation and recommend its acceptance: Christopher M. Fedo, Jill M. Mikucki, Andrew D. Steen, Colin D. Sumrall Accepted for the Council: Dixie L. Thompson Vice Provost and Dean of the Graduate School (Original signatures are on file with official studentecor r ds.) Ocean Circulation as a Driver for Changes in Ocean Chemistry in the Middle Ordovician of Argentina A Dissertation Presented for the Doctor of Philosophy Degree The University of Tennessee, Knoxville Miles Anthony Henderson May 2018 Copyright © 2018 by Miles Anthony Henderson All rights reserved. -
PREFACE a Graduate Thesis Often Represents a Student's First Attempt at Reporting Extensively on a Specific Research Problem
PREFACE A graduate thesis often represents a student's first attempt at reporting extensively on a specific research problem. The results are seldom published and those unpublished, too often are little known or used. Nevertheless, many if not most of them are sources of potentially significant information. The purpose of this circular is to compile a handy reference to this field of geologic information. Most thesis titles pertain to Michigan and surrounding Great Lakes. However, a few titles were included from adjacent states where this information may be useful in interpreting Michigan geology. The list is organized by author, each thesis assigned a number, cross-referenced to the subject index inside rear cover. The information was gathered primarily by canvassing collegiate geology departments, without whose cooperation this circular would not have been possible. The earliest thesis reported was written in 1895. Revisions are contemplated so any comments or additional data suggested will be appreciated. Prof. B. John Chronic, University of Colorado, has compiled "Bibliography of Theses in Geology" containing over 11,000 titles. University Microfilms, Ann Arbor, Michigan has been microfilming Ph.D. theses since 1938, listed monthly in "Dissertation Abstracts". Ph.D. Geological Survey theses titles appear in the monthly "Abstracts of North CIRCULAR 7 American Geology", U.S. Geological Survey. Lansing Edward A. Kirkby, Geologist INDEX TO MICHIGAN GEOLOGIC THESES May, 1967 Geological Survey Division by E. A. Kirkby Petrography and Petrology (including insoluble residues, petrofabrics, and sediments): Lansing 1967 14, 15, 25, 27, 30, 50, 56, 57, 58, 68, 69, 73, 74, 76, 79, 80, 82, 84, 89, 91, 93, 94, 106, 107, 108, 113, STATE OF MICHIGAN 118, 123, 126, 132, 133, 134, 135, 137, 140, 143, George Romney, Governor 146, 151, 156, 171, 176, 184, 185, 188, 198, 200, DEPARTMENT OF CONSERVATION 216, 218, 224, 226, 227, 237, 243, 246, 253, 259, Ralph A. -
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 -
Stratigraphic Lexicon for Michigan
Stratigraphic Lexicon for Michigan AUTHORS Paul A. Catacosinos David B. Westjohn [Professor Emeritus, United States Geological Survey Delta College [Associate Professor (Adjunct), University Center, MI 48710] Michigan State University] 1001 Martingale Lane SE 6520 Mercantile Way #6 Albuquerque, NM 87123-4305 Lansing, MI 48911 William B. Harrison, III Mark S. Wollensak, CPG Professor, Department of Geosciences EarthFax Engineering, Inc. Western Michigan University 15266 Ann Drive Kalamazoo, MI 49008 Bath, MI 48808 Robert F. Reynolds Reynolds Geological, L.L.C. 504 Hall Blvd. Mason, MI, 48854 Bulletin 8 Lansing, Michigan, 2001 Geological Survey Division and the Michigan Basin Geological Society State of Michigan John Engler, Govenor Michigan Department of Environmental Quality Russell J. Harding, Director MDEQ Geological Survey Division, P O Box 30256, Lansing, MI 48909-7756 On the Internet @ HTTP://W WW .DEQ.STATE.MI.US/GSD Printed by Authority of Act 451, PA 1994 as amended The Michigan Department of Environmental Quality (MDEQ) will not discriminate Total number of copies printed ........... 1,000 against any individual or group on the basis of race, sex, religion, age, national origin, Total cost: .................................... $2,500.00 color, marital status, disability or political beliefs. Directed questions or concerns to the Cost per copy: ..................................... $2.50 MDEQ Office of Personnel Services, P.O. Box 30473, and Lansing, MI 48909 Page 2 - - Stratigraphic Lexicon for Michigan DEDICATION The authors gratefully dedicate this volume to the memories of Helen M. Martin and Muriel Tara Straight. This volume would not have been possible without their monumental reference work Bulletin 50, An Index of Helen Melville Martin Michigan Geology published by the Michigan Geological Survey in 1956. -
Index to the Geologic Names of North America
Index to the Geologic Names of North America GEOLOGICAL SURVEY BULLETIN 1056-B Index to the Geologic Names of North America By DRUID WILSON, GRACE C. KEROHER, and BLANCHE E. HANSEN GEOLOGIC NAMES OF NORTH AMERICA GEOLOGICAL SURVEY BULLETIN 10S6-B Geologic names arranged by age and by area containing type locality. Includes names in Greenland, the West Indies, the Pacific Island possessions of the United States, and the Trust Territory of the Pacific Islands UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 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.G. - Price 60 cents (paper cover) CONTENTS Page Major stratigraphic and time divisions in use by the U.S. Geological Survey._ iv Introduction______________________________________ 407 Acknowledgments. _--__ _______ _________________________________ 410 Bibliography________________________________________________ 410 Symbols___________________________________ 413 Geologic time and time-stratigraphic (time-rock) units________________ 415 Time terms of nongeographic origin_______________________-______ 415 Cenozoic_________________________________________________ 415 Pleistocene (glacial)______________________________________ 415 Cenozoic (marine)_______________________________________ 418 Eastern North America_______________________________ 418 Western North America__-__-_____----------__-----____ 419 Cenozoic (continental)___________________________________ -
A Darriwilian (Middle Ordovician) Bivalve-Dominated Molluscan Fauna from the Stairway Sandstone, Amadeus Basin, Central Australia
A Darriwilian (Middle Ordovician) bivalve-dominated molluscan fauna from the Stairway Sandstone, Amadeus Basin, central Australia KRISTIAN G. JAKOBSEN, GLENN A. BROCK, ARNE T. NIELSEN, and DAVID A.T. HARPER Jakobsen, K.G., Brock, G.A., Nielsen, A.T., and Harper, D.A.T. 2016. A Darriwilian (Middle Ordovician) bivalve-domi- nated molluscan fauna from the Stairway Sandstone, Amadeus Basin, central Australia. Acta Palaeontologica Polonica 61 (4): 897–924. A bivalve-dominated molluscan fauna is described from the Darriwilian (Middle Ordovician) Stairway Sandstone, Amadeus Basin, central Australia. The fauna comprises 16 species of bivalves and rostroconchs plus six gastropod species which are treated under open nomenclature. Two new bivalves, Sthenodonta paenesymmetrica sp. nov. and Modiolopsis pojetai sp. nov., are described. The relatively low-diverse molluscan fauna constitutes around 62% of the total benthic macrofauna. Approximately 75% of the molluscs comprise bivalves, especially nuculoids, which were biogeographically restricted to low latitudes during the Ordovician. The molluscan assemblage displays a very high degree of endemism at species level, though the bivalve Sthenodonta eastii also occurs in the Georgina Basin farther to the northeast. This indicates a possible marine connective seaway between the Georgina and Amadeus basins during the Darriwilian. Nuculites, Cyrtodonta, and Modiolopsis are cosmopolitan and previously reported from North China, Avalonia, and Southern Gondwana. Key words: Mollusca, Bivalvia, endemicity, biodiversity, Ordovician, Darriwilian, Central Australia. Kristian G. Jakobsen [[email protected]], Geological Museum, Natural History Museum of Denmark, University of Co- penhagen, Øster Voldgade 5–7, DK-1350 Copenhagen, Denmark; and Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia; current address: Ministry of Mineral Resources, Government of Green- land, Imaneq 1A, 201, GL-3900 Nuuk, Greenland.