76-9949 CHAPEL, James David, 1948- PETROLOGY and DEPOSITIONAL HISTORY of DEVONIAN CARBONATES in OHIO
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Para Conhecer a Terra: Memórias E Notícias De Geociências No Espaço Lusófono Autor(Es): Lopes, F.C. (Coord.); Andrade, A. I
Para conhecer a Terra: memórias e notícias de Geociências no espaço lusófono Lopes, F.C. (coord.); Andrade, A. I. (coord.); Henriques, M. H. (coord.); Autor(es): Quinta-Ferreira, M. (coord.); Reis, R. Pena dos (coord.); Barata, M. T. (coord.) Publicado por: Imprensa da Universidade de Coimbra URL persistente: URI:http://hdl.handle.net/10316.2/24406 DOI: DOI:http://dx.doi.org/10.14195/978-989-26-0534-0 Accessed : 11-Oct-2021 03:52:55 A navegação consulta e descarregamento dos títulos inseridos nas Bibliotecas Digitais UC Digitalis, UC Pombalina e UC Impactum, pressupõem a aceitação plena e sem reservas dos Termos e Condições de Uso destas Bibliotecas Digitais, disponíveis em https://digitalis.uc.pt/pt-pt/termos. Conforme exposto nos referidos Termos e Condições de Uso, o descarregamento de títulos de acesso restrito requer uma licença válida de autorização devendo o utilizador aceder ao(s) documento(s) a partir de um endereço de IP da instituição detentora da supramencionada licença. Ao utilizador é apenas permitido o descarregamento para uso pessoal, pelo que o emprego do(s) título(s) descarregado(s) para outro fim, designadamente comercial, carece de autorização do respetivo autor ou editor da obra. Na medida em que todas as obras da UC Digitalis se encontram protegidas pelo Código do Direito de Autor e Direitos Conexos e demais legislação aplicável, toda a cópia, parcial ou total, deste documento, nos casos em que é legalmente admitida, deverá conter ou fazer-se acompanhar por este aviso. pombalina.uc.pt digitalis.uc.pt 9 789892 605111 Série Documentos A presente obra reúne um conjunto de contribuições apresentadas no I Congresso Imprensa da Universidade de Coimbra Internacional de Geociências na CPLP, que decorreu de 14 a 16 de maio de 2012 no Coimbra University Press Auditório da Reitoria da Universidade de Coimbra. -
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................................................................. -
OGS 1962 RI-42.Pdf
·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·i i STATE CE OHIO • MICHAEL V. DISALLI, eo-- DD'AU'MEHT CE NATIJl\AL llES<XmCES Ilo IElllEl\T a, EAGON, Dlncllor In'ISION OF GEOLOGICAL SURVEY l\AJ.PH J. KIUIHACEN, Chief Ii I• lo I REPORT OF INVESTIGATIONS NO. 42 LOWER AND MIDDLE DEVONIAN LIMESTONES IN NORTHEASTERN OHIO • I • AND ADJACENT AREAS I i• I ~ ~ By i John W. Dow i II • I • I • I I • i I . • I I COLUMBUS ~ . 1962 I I • • I• I I • • I I ~-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·-· STATE OF OHIO Michael V. DiSalle Governor DEPARTMENT OF NATURAL RESOURCES Herbert B. Eagon Director NATURAL RESOURCES COMMISSION Herbert B. Eagon Lawrence Kimble Byron Frederick Roy M. Kottman Forrest G. Hall Demas L. Sears William Hoyne Myron T.· Sturgeon Joseph E. Hurst DIVISION OF GEOLOGICAL SURVEY Ralph J. Bernhagen Chief The F . J . Heer Printing Company Columbus 16, Ohio 1962 Bound by the State of Ohio ;-·-·-·-·-·-·-·-·-·-~-·-·-·-·-·-·-·-·-·-·-·-·-·-·-·i i• i I ~Of~ I• 0 MICHAEL V. DI SALLE, Governor lo DEPAR1MENT Of NATURAL RESOURCES I HERBERT II. EAGON, Director I DIVISION OF GEOLOGICAL SURVEY RALPH J. BERNHAGEN, Chief • I • I.. I REPORT OF INVESTIGATIONS NO. 42 i i;. ! .I .I I LOWER AND MIDDLE DEVONIAN LIMESTONES . IN NORTHEASTERN OHIO I • AND ADJACENT AREAS .I I• I.. I By i• John W. Dow I ! ! ! I • I • I • .I .I .I I I COLUMBUS • . 1962 I I • . I.. I For sale l::ry Ohio Division of Geological Survey, Columbus, Ohio I • Price 97 cents plus 3 cents tax in Ohio • I ~ ...... _...... ··-.- .- ·-.- .- .- .- .- .- .- .- .- .- .- ._,,. -.- .- .- .- .- .- . BLANK PAGE CONTENTS Page Introduction. 1 Purpose of study 1 Previous studies 1 Methods of investigation. -
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) -
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. -
ART. El Material Tipo De La
Wicander, R. and Playford, G., 2017. Organic-walled microphytoplankton assemblage of the Middle Devonian (Givetian) Arkona, Hungry Hollow and Widder formations, Ontario, Canada: biostratigraphic and palaeogeographic significance . Boletín Geológico y Minero, 128 (4): 839-883 ISSN: 0366-0176 DOI: 10.21701/bolgeomin.128.4.001 Organic-walled microphytoplankton assemblage of the Middle Devonian (Givetian) Arkona, Hungry Hollow and Widder formations, Ontario, Canada: biostratigraphic and palaeogeographic significance R. Wicander (1, 2) and G. Playford (2) (1) Department of Earth and Atmospheric Sciences, Central Michigan University, Mount Pleasant, Michigan, U.S.A. 48859. [email protected] (2) School of Earth and Environmental Sciences, The University of Queensland, Brisbane, Q 4072, Australia. [email protected] ABSTRACT A diverse and abundant organic-walled microphytoplankton assemblage, consisting of 49 species of acri - tarchs, prasinophyte phycomata and chitinozoans, was recovered from a 13.3 m-section of the Middle Devonian (Givetian) Arkona, Hungry Hollow and Widder formations at Hungry Hollow, Ontario, Canada. Close similarity exists between this assemblage and others described previously from the Givetian of North America. Marine palynofloras of comparable age from elsewhere in North America share between 59–96% of the species identified in the present assemblage, thus testifying to its stratigraphic-correlative applicability in a regional context. Species widely occurring in North America and typically Givetian (although not restricted therein) include: Arkonites bilixus, Cymatiosphaera canadense, Diexallophasis simplex, Duvernaysphaera angelae, D. tenuicingulata, Estiastra rhytidoa, Exochoderma arca, Gorgonisphaeridium inflatum, Hapsidopalla chela, Leiofusa pyrena, Muraticavea munifica, Oppilatala sparsa, Palacanthus ledanoisii , Polyedryxium ambitum, Staplinium cuboides, Tyligmasoma alargada, Uncinisphaera acantha, Veryhachium pastoris, Villosacapsula compta and V. -
Biodiversity Patterns Across the Late Paleozoic Ice Age
Palaeontologia Electronica palaeo-electronica.org Biodiversity patterns across the Late Paleozoic Ice Age Barbara Seuss, Vanessa Julie Roden, and Ádám T. Kocsis ABSTRACT The Late Palaeozoic Ice Age (LPIA, Famennian to Wuchiapingian) witnessed two transitions between ice- and greenhouse conditions. These alternations led to drastic alterations in the marine system (e.g., sea-level, habitat size, sea-surface temperature) forcing faunal changes. To reassess the response of the global marine fauna, we ana- lyze diversity dynamics of brachiopod, bivalve, and gastropod taxa throughout the LPIA using data from the Paleobiology Database. Diversity dynamics were assessed regarding environmental affinities of these clades. Our analyses indicate that during the LPIA more taxa had an affinity towards siliciclastic than towards carbonate environ- ments. Deep-water and reefal habitats were more favored while grain size was less determining. In individual stages of the LPIA, the clades show rather constant affinities towards an environment. Those bivalves and brachiopods with an affinity differ in their habitat preferences, indicating that there might have been little competition among these two clades. Origination and extinction rates are similar during the main phase of the LPIA, whether environmental affinities are considered or not. This underlines that the LPIA marine fauna was well adapted and capable of reacting to changing environ- mental and climatic conditions. Since patterns of faunal change are similar in different environments, our study implies that the changes in faunal composition (e.g., diversity loss during the LPIA; strong increase of brachiopod diversity during the Permian) were influenced by the habitat to only a minor degree but most likely by yet unknown abiotic factors. -
The Ohio Journal of Science — Index 1951-1970
THE OHIO JOURNAL OF SCIENCE — INDEX 1951-1970 JANE L. FORSYTH AND CHRISTINE M. GORTA Department of Geology, Bowling Green State University, Bowling Green, Ohio 43403 INTRODUCTION It is almost 20 years since the first General Index to The Ohio Journal of Science, which covered the issues from the beginning (1900) through 1950, was published (Miller, E. M., 1953, published by The Ohio State University and The Ohio Academy of Science). It is time, therefore, for another general index, dealing with issues appearing since 1950. This is that index. Unlike the first index, there is no separate listing of full references by author; rather, this is simply a combining of all the entries from all the yearly indexes from 1951 through 1972. Basically these original entries remain unchanged here, though mistakes found in a few were corrected, and some have been slightly reworded in order to fit better into this multiple listing. Entries relating to book reviews occur only for the years of 1963 through 1970, because book reviews were not included in the earlier indexes. It should also be noted that, though a few of these books represent merely a reprinting of older, out-of-date books, these books are not so identified in the entries in this index. Preparation of this index has been mostly handled by Miss Christine M. Gorta, under the direction of Dr. Jane L. Forsyth, Editor of The Ohio Journal of Science from 1964 to 1973, but others have also contributed to this work—mainly Misses Lauran Boyles and Laura Witkowski—contributers whose efforts are gratefully acknowledged. -
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. -
Permophiles International Commission on Stratigraphy
Permophiles International Commission on Stratigraphy Newsletter of the Subcommission on Permian Stratigraphy Number 66 Supplement 1 ISSN 1684 – 5927 August 2018 Permophiles Issue #66 Supplement 1 8th INTERNATIONAL BRACHIOPOD CONGRESS Brachiopods in a changing planet: from the past to the future Milano 11-14 September 2018 GENERAL CHAIRS Lucia Angiolini, Università di Milano, Italy Renato Posenato, Università di Ferrara, Italy ORGANIZING COMMITTEE Chair: Gaia Crippa, Università di Milano, Italy Valentina Brandolese, Università di Ferrara, Italy Claudio Garbelli, Nanjing Institute of Geology and Palaeontology, China Daniela Henkel, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany Marco Romanin, Polish Academy of Science, Warsaw, Poland Facheng Ye, Università di Milano, Italy SCIENTIFIC COMMITTEE Fernando Álvarez Martínez, Universidad de Oviedo, Spain Lucia Angiolini, Università di Milano, Italy Uwe Brand, Brock University, Canada Sandra J. Carlson, University of California, Davis, United States Maggie Cusack, University of Stirling, United Kingdom Anton Eisenhauer, GEOMAR Helmholtz Centre for Ocean Research Kiel, Germany David A.T. Harper, Durham University, United Kingdom Lars Holmer, Uppsala University, Sweden Fernando Garcia Joral, Complutense University of Madrid, Spain Carsten Lüter, Museum für Naturkunde, Berlin, Germany Alberto Pérez-Huerta, University of Alabama, United States Renato Posenato, Università di Ferrara, Italy Shuzhong Shen, Nanjing Institute of Geology and Palaeontology, China 1 Permophiles Issue #66 Supplement