Pennsylvanian Conodont Localities in Northeastern Ohio By

Total Page:16

File Type:pdf, Size:1020Kb

Pennsylvanian Conodont Localities in Northeastern Ohio By DIVISION OF GEOLOGICAL SURVEY GUIDEBOOK NO. 3 PENNSYLVANIAN CONODONT LOCALITIES IN NORTHEASTERN OHIO BY GLEN K. MERRILL Prepared for annua I meeting of the PANDER SOCIETY in cooperation with THE GEOLOGICAL SOCIETY OF AMERICA NORTH-CENTRAL SECTION 8TH ANNUAL MEETING KENT, OHIO MAY 8-11. 1974 ®NATillAL llESOOllCES STATE OF OHIO DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL SURVEY John J. Gilligan, Governor William B. Nye, Director Horace R. Collins. Chief SCIENTIFIC AND TECHNICAL STAFF OF THE DIVISION OF GEOLOGICAL SURVEY 0IEPARTMENT IJ NATURAL RESOURCES ADMINISTRATIVE SECTION Horace R. Collins, MS, State Geologist and Division Chief Jean Simmons Brown, MS, Geologist and Editor William J. Buschman, Jr., BS, Administrative Geologist Merrianne Hackathorn, BS, Geologist and Assistant Editor Michael C. Hansen, MS, Geologist Edwin F. Helser, BS, Administrative Assistant Madge E. Rodgers, BS, Geologist Pauline Smyth, MS, Geologist Eleanor J. Hyle, Secretary Jacquelene Connolly, Clerk-Typist Donna M. Schrappe, Clerk-Typist REGIONAL GEOLOGY SECTION SUBSURFACE GEOLOGY SECTION Richard A. Struble, PhD, Geologist and Section Head Adriaan Janssens, PhD, Geologist and Section Head Richard W. Carlton, PhD, Geologist Michael J. Clifford, MS, Geologist Michael L. Couchot, MS, Geologist Jeffrey B. Hermann, BS, Geologist Richard M. DeLong, MS, Geologist Ronald D. Stieglitz, PhD, Geologist David S. Fullerton, PhD, Geologist James Wooten, Geologist Aide Gerald H. Groenewold, PhD, Geologist Barbara J. Adams, Clerk Joseph R. Hatch, PhD, Geochemist B. Margalene Crammer, Clerk Donald 0. Johnson, PhD, Geologist Jeff L. Reese, BS, Geologist David A. Stith, MS, Geologist Robert G. Van Horn, MS, Geologist Joel D. Vormelker, MS, Geologist Geochemistry laboratory LAKE ERIE SECTION Donald L. Streib, PhD, Geochemist in charge George Botoman, MS, Geologist Charles H. Carter, PhD, Geologist and Section Head Norman F. Knapp, PhD, Chemist Donald J. Benson, MS, Geologist E. Lorraine Partlow, Laboratory Technician Walter R. Lemke, Boat Captain Donald E. Guy, Jr., BA, Geologist Aide Dale L. Liebenthal, Geologist Aide Lynn M. Gerold, Clerk-Typist WATER INVENTORY SECTION Alfred C. Walker, BS, Geologist and Section Head Herbert B. Eagon, Jr., BS, Geologist Leonard J. Harstine, BS, Research Associate Glenn W. Hartzell, BS, Geologist PUBLICATIONS SECTION Anthony R. Rudnick, BS, Geologist James J. Schmidt, BS, Geologist Harold J. Flint, Cartographer and Section Head David S. Ziegler, BA, Geologist James A. Brown, Cartographer Lloyd C. Flower, Technician Donald R. Camburn, Cartographer Otha B. Furlough, Technician Philip J. Celnar, BFA, Cartographer Donald M. Henry, Technician James E. Hairston, Cartographer V. Ruth Haldeman, Geologist Aide Leslie R. Lewis, BF A, Cartographer Jane Kellermeyer, Clerk-Typist Jean J. Miller, Photocopy Composer STATE OF OHIO John J. Gi II igan, Governor DEPARTMENT OF NATURAL RESOURCES William B. Nye, Director DIVISION OF GEOLOGICAL SURVEY Horace R. Collins. Chief Guidebook No. 3 PENNSYLVANIAN CONODONT LOCALITIES IN NORTHEASTERN OHIO by Glen K. Merrill Columbus 1974 ------~------------------"' .::::: GEOLOGY SERVES OHIO ~ CONTENTS Page Trip at a glance .... .... .. .... ... .... ...... ...... .. .. ...... .... .... ...... .. .... .... .. .... .. .. .......... .... ... .... ...... .. .... 1 Geologic setting .... ......... ... .... ... .... .. .. .... ... .... .. .... ........ .... .... .... .... .......... .... .... .... ........ ...... 1 General .............................................................................................................................. 1 Topographic maps ................ ............ ............ .......... .......... .... ............................................ 2 Road log............................................................................................................................ 3 Stop lA - Grindstone Run, Lowellville, Ohio ............................................................ 4 Lowellville Limestone .... ........ ............ ................ .......... .................... .......... ................ 4 Lower Mercer Limestone ............ ................ .................................. .............................. 5 Upper Mercer Limestone ................ ............................ ........ ........ .... ............................ 5 Stop lB - quarry at Lowellville Rod and Gun Club .................................................. 6 Vanport Limestone...................................................................................................... 6 Stop 2 - in bed of Yellow Creek, Poland, Ohio ...................................... .................... 6 Lower Mercer Limestone .. ........ .... .... .... .... .... ........ .... ...... .... .... ...... .. ...... .... ...... ............ 6 Stop 3 - along old U.S. 30 west of Cannon's Mill...................................................... 9 Brush Creek Member.................................................................................................... 9 Stop 4 - along Ohio Rte. 45 west of Round Knob ...................................................... 10 Cambridge Member ...................................................................................................... 10 Stop 5 - along Ohio Rte. 213 at Yellow Creek.......................................................... 11 Washingtonville Shale ................................................................................................ 11 Stop 6 - road and railroad cuts near Broadacre ......................................................... ., 13 Ames Limestone ........ .................................. ................ .... ........ ........ ............ .......... ...... 13 Stop 7 - hilltop west of Bowerston.............................................................................. 14 Ames Limestone.......................................................................................................... 14 Stop 8 - New Philadelphia road cut ...................................... .... .......................... .......... 17 Putnam Hill Limestone .... ................ .. ............ .. .......... .. .. .... .... .... ........ .... .... ................ 17 Lower Clarion Shale .... .. .. ............ .. .... .... ........ .... .... .... .... .... .... ...... .... ............ .... .... ...... .. 17 Vanport Limestone and Chert.................................................................................... 17 Upper Clarion Shale .... ................................................................................................ 18 Occurrences of Pennsylvanian conodonts in eastern Ohio: a brief summary.......... 19 Phylogenetic and biostratigraphic summary .............................................................. 19 N eognathodus ...... ........ ........ ...... ...... .......... .. .......... .... ............ .... ...... .... .... ........ ........ .. 19 ldiognathodus-Streptognathodus ................ .......................... .................................... 21 Cavusgnathus .......... .. .. .... .... .... .... ... .......... ...... ...... .... .... .... .... .... .... .... .... .... ................ 22 Anchignathodus ..... .... ... .. ........ .... ...... .... .... ........ .... .... .... .... .... ...... .................... .......... 22 ''Spathognathodus'' .................................................................................................. 22 Zona ti on .... .... .... ........ .... ...... .. .......... ............ .... ...... ...... .. .. .... .......... .... ..... ... .... ............ 22 Lithostratigraphic and paleoecologic summary .......... ................................................ 23 Acknowledgments.............................................................................................................. 24 References cited .... ........ ...... .. ...... .......... ............ .. .. ........ ........ ...... ...... ...... .... .... ...... ........ .. 24 FIGURES 1. Route map .................................................................................................................... 1 2. Composite columnar section at Stops lA and lB ........ ........ .......... .......................... 5 3. Columnar section at Stop 5 .................................... ................................ ...... .............. 12 4. Graphic portrayal of conodont data at Stop 8 .......................................................... 16 5. Schematic summary of conodont occurrences in Pennsylvanian rocks of east- ern Ohio ............................................................................................................ 20 iii CONTENTS TABLES 1. Generalized stratigraphic relationships between the various marine beds in the Pennsylvanian of Ohio .............................................................................. 21 2. List of taxa with associates and occurrences ........ ................................................ 23 PLATES 1. Conodonts from the Putnam Hill, Upper Mercer, Lower Mercer, and Lowellville Members........................................................ Following page 25 2. Conodonts from the Ames, Cambridge, Brush Creek, Washing- tonville, and Vanport Members .............................................. Following page 25 iv PENNSYLVANIAN CONODONT LOCALITIES IN NORTHEASTERN OHIO by Glen K. Merrill THE TRIP AT A GLANCE ing northward until in the region around Youngstown, Ohio, it is nearly east-west. As we follow the trip Purpose: To acquaint the participant with
Recommended publications
  • CONODONT BIOSTRATIGRAPHY and ... -.: Palaeontologia Polonica
    CONODONT BIOSTRATIGRAPHY AND PALEOECOLOGY OF THE PERTH LIMESTONE MEMBER, STAUNTON FORMATION (PENNSYLVANIAN) OF THE ILLINOIS BASIN, U.S.A. CARl B. REXROAD. lEWIS M. BROWN. JOE DEVERA. and REBECCA J. SUMAN Rexroad , c.. Brown . L.. Devera, 1.. and Suman, R. 1998. Conodont biostrati graph y and paleoec ology of the Perth Limestone Member. Staunt on Form ation (Pennsy lvanian) of the Illinois Basin. U.S.A. Ill: H. Szaniawski (ed .), Proceedings of the Sixth European Conodont Symposium (ECOS VI). - Palaeont ologia Polonica, 58 . 247-259. Th e Perth Limestone Member of the Staunton Formation in the southeastern part of the Illinois Basin co nsists ofargill aceous limestone s that are in a facies relati on ship with shales and sandstones that commonly are ca lcareous and fossiliferous. Th e Perth conodo nts are do minated by Idiognathodus incurvus. Hindeodus minutus and Neognathodu s bothrops eac h comprises slightly less than 10% of the fauna. Th e other spec ies are minor consti­ tuents. The Perth is ass igned to the Neog nathodus bothrops- N. bassleri Sub zon e of the N. bothrops Zo ne. but we were unable to co nfirm its assignment to earliest Desmoin esian as oppose d to latest Atokan. Co nodo nt biofacies associations of the Perth refle ct a shallow near- shore marine environment of generally low to moderate energy. but locali zed areas are more variable. particul ar ly in regard to salinity. K e y w o r d s : Co nodo nta. biozonation. paleoecology. Desmoinesian , Penn sylvanian. Illinois Basin. U.S.A.
    [Show full text]
  • 03-Alekseev and Goreva (Neognathodus).P65
    Lucas, S.G., et al. eds., 2013, The Carboniferous-Permian Transition. New Mexico Museum of Natural History and Science, Bulletin 60. 1 THE CONODONT NEOGNATHODUS BOTHROPS MERRILL, 1972 AS THE MARKER FOR THE LOWER BOUNDARY OF THE MOSCOVIAN STAGE (MIDDLE PENNSYLVANIAN) ALEXANDER S. ALEKSEEV1 AND NATALIA V. GOREVA 2 1 Department of Paleontology, Geological Faculty, Moscow State University, Russia, email: aaleks@geol. msu.ru; 2 Geological institute of Russian Academy of Science, Moscow, Russia, email: [email protected] Abstract—The Moscovian Stage constitutes the Middle Pennsylvanian Series of the Carboniferous System, but a biostratigraphic marker and GSSP for it have not yet been designated. The exact position of the Moscovian boundary cannot be defined properly because in the type area the basal Vereian unconformably overlies the Mississippian limestone or the alluvial and lagoonal Aza Formation of the uppermost Bashkirian. The Task Group to establish a GSSP close to the existing Bashkirian-Moscovian boundary suggested several potential markers among foraminifers and conodonts, but the search for a marker near traditional base of the global Moscovian Stage has stalled. It may be more productive to search for FADs in the lower Moscovian, above the traditional base, to designate the lower boundary of the stage. Relatively rich Vereian and Kashirian conodont assemblages have been recovered from the southwest Moscow Basin, as well as from the Oka-Tsna Swell. The most complete information on the distribution of conodonts in the Vereian- Kashirian boundary interval was obtained from the Yambirno section (Oka-Tsna Swell). The greatest change in conodont assemblages does not occur near the level of the traditional base of the Moscovian, but stratigraphically higher.
    [Show full text]
  • Conodonts in Ordovician Biostratigraphy
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Archivio istituzionale della ricerca - Università di Modena e Reggio Emilia 1 Conodonts in Ordovician biostratigraphy STIG M. BERGSTRÖM AND ANNALISA FERRETTI Conodonts in Ordovician biostratigraphy The long time interval after Pander’s (1856) original conodont study can in terms of Ordovician conodont biostratigraphic research be subdivided into three periods, namely the Pioneer Period (1856-1955), the Transition Period (1955-1971), and the Modern Period (1971-Recent). During the pre-1920s, the few published conodont investigations were restricted to Europe and North America and were not concerned about the potential use of conodonts as guide fossils. Although primarily of taxonomic nature, the pioneer studies by Branson & Mehl, Stauffer, and Furnish during the 1930s represent the beginning of the use of conodonts in Ordovician biostratigraphy. However, no formal zones were introduced until Lindström (1955) proposed four conodont zones in the Lower Ordovician of Sweden, which marks the end of the Pioneer Period. Because Lindström’s zone classification was not followed by similar work outside Baltoscandia, the time interval up to the late 1960s can be regarded as a Transition Period. A milestone symposium volume, entitled ‘Conodont Biostratigraphy’ and published in 1971, 2 summarized much new information on Ordovician conodont biostratigraphy and is taken as the beginning of the Modern Period of Ordovician conodont biostratigraphy. In this volume, the Baltoscandic Ordovician was subdivided into named conodont zones whereas the North American Ordovician succession was classified into a series of lettered or numbered Faunas. Although most of the latter did not receive zone names until 1984, this classification has been used widely in North America.
    [Show full text]
  • Preliminary Geologic Map of the Baird Mountains and Part of the Selawik Quadrangles, Alaska By
    preliminary Geologic Map of the Baird Mountains and part of the Selawik Quadrangles, Alaska by S.M. Karl, J.A. Dumoulin, Inyo Ellersieck, A.G. Harris, and J.M. Schmidt Open-File Report 89-551 This map is preliminary and has not been reviewed for conformity with the North American stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Table Contents ~ntroduction.......................................... 1 Stratigraphic Framework .................................1 Structural Framework ....................................4 Acknowledgments .......................................6 Unit Descriptions ......................................6 Kc ............................................. 6 KJm .............................................6 JPe .............................................7 ~zb................ '. ... ., ,....................... 8 Mzg ............................................10 MzPzi ..........................................10 MZPZ~.......................................... 11 PMC ............................................12 PD1 ............................................12 Mk0 ............................................12 M1 .............................................13 MDue ...........................................14 Mlt ............................................15 Mk .............................................15 MD1 ............................................16 MDe ............................................16 MD~...........................................
    [Show full text]
  • Six Charts Showing Biostratigraphic Zones, and Correlations Based on Conodonts from the Devonian and Mississippian Rocks of the Upper Mississippi Valley
    14. GS: C.2 ^s- STATE OF ILLINOIS DEPARTMENT OF REGISTRATION AND EDUCATION SIX CHARTS SHOWING BIOSTRATIGRAPHIC ZONES, AND CORRELATIONS BASED ON CONODONTS FROM THE DEVONIAN AND MISSISSIPPIAN ROCKS OF THE UPPER MISSISSIPPI VALLEY Charles Collinson Alan J. Scott Carl B. Rexroad ILLINOIS GEOLOGICAL SURVEY LIBRARY AUG 2 1962 ILLINOIS STATE GEOLOGICAL SURVEY URBANA 1962 CIRCULAR 328 I I co •H co • CO <— X c = c P o <* CO o CO •H C CD c +» c c • CD CO ft o e c u •i-CU CD p o TJ o o co CO TJ <D CQ x CO CO CO u X CQ a p Q CO *» P Mh coc T> CD *H O TJ O 3 O o co —* o_ > O p X <-> cd cn <d ^ JS o o co e CO f-l c c/i X ex] I— CD co = co r CO : co *H U to •H CD r I .h CO TJ x X CO fc TJ r-< X -P -p 10 co C => CO o O tJ CD X5 o X c c •> CO P <D = CO CO <H X> a> s CO co c %l •H CO CD co TJ P X! h c CD Q PI CD Cn CD X UJ • H 9 P CD CD CD p <D x c •—I X Q) p •H H X cn co p £ o •> CO o x p •>o C H O CO "P CO CO X > l Ct <-c . a> CD CO X •H D. CO O CO CM (-i co in Q.
    [Show full text]
  • Catalog of Type Specimens of Invertebrate Fossils: Cono- Donta
    % {I V 0> % rF h y Catalog of Type Specimens Compiled Frederick J. Collier of Invertebrate Fossils: Conodonta SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY NUMBER 9 SERIAL PUBLICATIONS OF THE SMITHSONIAN INSTITUTION The emphasis upon publications as a means of diffusing knowledge was expressed by the first Secretary of the Smithsonian Institution. In his formal plan for the Insti­ tution, Joseph Henry articulated a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This keynote of basic research has been adhered to over the years in the issuance of thousands of titles in serial publications under the Smithsonian imprint, com­ mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Annals of Flight Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Studies in History and Technology In these series, the Institution publishes original articles and monographs dealing with the research and collections of its several museums and offices and of profes­ sional colleagues at other institutions of learning. These papers report newly acquired facts, synoptic interpretations of data, or original theory in specialized fields. These publications are distributed by mailing lists to libraries, laboratories, and other in­ terested institutions and specialists throughout the world. Individual copies may be obtained from the Smithsonian Institution Press as long as stocks are available.
    [Show full text]
  • Sequence Biostratigraphy of Carboniferous-Permian Boundary
    Brigham Young University BYU ScholarsArchive Theses and Dissertations 2019-07-01 Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin Joshua Kerst Meibos Brigham Young University Follow this and additional works at: https://scholarsarchive.byu.edu/etd Part of the Physical Sciences and Mathematics Commons BYU ScholarsArchive Citation Meibos, Joshua Kerst, "Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin" (2019). Theses and Dissertations. 7583. https://scholarsarchive.byu.edu/etd/7583 This Thesis is brought to you for free and open access by BYU ScholarsArchive. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin Joshua Kerst Meibos A thesis submitted to the faculty of Brigham Young University in partial fulfillment of the requirements for the degree of Master of Science Scott M. Ritter, Chair Brooks B. Britt Sam Hudson Department of Geological Sciences Brigham Young University Copyright © 2019 Joshua Kerst Meibos All Rights Reserved ABSTRACT Sequence Biostratigraphy of Carboniferous-Permian Boundary Strata in Western Utah: Deciphering Eustatic and Tectonic Controls on Sedimentation in the Antler-Sonoma Distal Foreland Basin Joshua Kerst Meibos Department of Geological Sciences, BYU Master of Science The stratal architecture of the upper Ely Limestone and Mormon Gap Formation (Pennsylvanian-early Permian) in western Utah reflects the interaction of icehouse sea-level change and tectonic activity in the distal Antler-Sonoma foreland basin.
    [Show full text]
  • VOLUME 33 December 2017
    VOLUME 33 December 2017 Volume 33 Table of Contents EXECUTIVE’S COLUMN…………………………………………………………………..…….. 2 OBITUARY……………………………………………………………………………………..…5 SCCS REPORTS………………………………………………………………………………….7 ANNUAL REPORT TO ICS FOR 2016-2017…………………………………………………..….7 TASK GROUP REPORTS FOR 2016-2017 AND WORK PLANS FOR 2017 FISCAL YEAR………….11 Report of the task group to establish a GSSP close to the existing Viséan-Serpukhovian boundary…………11 Report of the task group to establish a GSSP close to the existing Bashkirian-Moscovian boundary………16 Report of the task group to establish the Moscovian-Kasimovian and Kasimovian-Gzhelian boundaries…....18 SCCS DOCUMENTS (CONTRIBUTIONS BY MEMBERS)…………………………………...……21 SHALLOW-WATER SIPHONODELLIDS AND DEFINITION OF THE DEVONIAN-CARBONIFEROUS BOUNDARY…………………………………………………………………………………….21 REPORT FOR PROGRESS FOR 2017 ACTIVITIES IN THE CANTABRIAN MOUNTAINS, SPAIN AND THE AMAZONAS BASIN, BRAZIL……………………………………………...………………26 TAXONOMIC AND STRATIGRAPHIC PROBLEMS CONCERNING THE CONODONTS LOCHRIEA SENCKENBERGICA NEMIROVSKAYA, PERRET & MEISCHNER, 1994 AND LOCHRIEA ZIEGLERI NEMIROVSKAYA, PERRET & MEISHCNER, 1994-CONSEQUENCES FOR DEFINING THE VISÉAN- SERPUKHOVIAN BOUNDARY………………………………………………………………………………...28 PROGRESS ON THE VISÉAN-SERPUKHOVIAN BOUNDARY IN SOUTH CHINA AND GERMANY……………………………………………………………………………………..35 POTENTIAL FOR A MORE PRECISE CORRELATION OF THE BASHKIRIAN AMMONOID AND FORAMINIFERAL ZONES IN THE SOUTH URALS…………………………………………..……42 CHEMOMETRICS AND CARBONIFEROUS MEDULLOSALEAN FRONDS: IMPLICATIONS FOR CARBONIFEROUS PHYTOSTRATIGRAPHY…………………………………………………...…45
    [Show full text]
  • Conodont Faunas from Portugal and Southwestern Spain
    v. d. Boogaard, Middle Devonian conodonts from Portugal, Scripta Geol. 13 (1972) 1 Conodont faunas from Portugal and southwestern Spain Part 1. A Middle Devonian fauna from near Montemor-o-Novo M. van den Boogaard Van den Boogaard, M. Conodont faunas from Portugal and southwestern Spain. Part 1. A Middle Devonian fauna from near Montemor-o-Novo. - Scripta Geol., 13: 1-11, 6 figs., 1 pl., Leiden, December 1972. Conodonts of Couvinian age are recorded from limestone beds incorporated in a sedimentary sequence which was previously considered to be Late Devonian or Early Carboniferous in age. M. van den Boogaard, Rijksmuseum van Geologie en Mineralogie, Hooglandse Kerkgracht 17, Leiden, The Netherlands. Introduction 1 Geological setting 4 Comments on the faunas 4 Stratigraphie results 8 References 9 Introduction The stratigraphy of the Palaeozoic rocks of southern Portugal and southwestern Spain is still not well known in detail, one of the reasons being the scarcity of fossils. Therefore conodonts obtained from local limestone lenses have given welcome information (Höllinger, 1959; van den Boogaard, 1963). Occasionally, new outcrops of limestone have been encountered by geologists presently at work in that region, and during the last few years I have received several samples of these limestones for investigation. Since further limestone outcrops may be dis- covered and samples thereof sent to me, and since there is no stratigraphical control, I decided to publish the results separately but under the general heading 2 v. d. Boogaard, Middle Devonian conodonts from Portugal, Scripta Geol. 13 (1972) Fig. 1. Map showing the locality of Pedreira da Engenharia (= P.E.).
    [Show full text]
  • Proceedings of the Indiana Academy of Science 83
    Proceedings of the Indiana Academy of Science 83 (1993) Volume 102 p. 83-91 CONODONTS FROM COAL BALLS IN THE SPRINGFIELD COAL MEMBER OF THE PETERSBURG FORMATION (DESMOINESIAN, PENNSYLVANIAN) IN SOUTHERN INDIANA Carl B. Rexroad Indiana Geological Survey 611 North Walnut Grove Bloomington, Indiana 47405 ABSTRACT: A well-preserved and moderately diverse conodont faunule was recovered from five coal balls in the Springfield Coal Member of the Petersburg Formation from Peabody Coal Com- pany's Eby Pit, Lynnville Mine, in Warrick County, Indiana. The presence of Neognathodus roundyi and the other species recorded in this study is compatible with the middle Desmoinesian age of the Springfield. Idioprioniodus conjunctus is the most ecologically diagnostic of the conodonts and suggests organic-rich, quiet water with a low pH, which in turn suggests that the conodonts lived in a salt-water marsh bordered on one side by coal swamps and on another by near-normal marine waters. Apparently coal balls had multiple origins, and the origin of the conodont-bearing ones is uncertain. INTRODUCTION Because marine fossils are commonly associated with plant fossils in some coal balls, it is not surprising that conodonts have been reported from them. A half-dozen well-pre- served conodonts from Pennsylvanian coal balls from three different States were figured by Mamay and Yochelson (1962), but no other conodonts were figured; therefore, the overall conodont content in coal balls is unknown. To better understand the distribution of conodonts and their paleoecologic impor- tance in coal balls, samples were processed from coal balls of the middle Desmoinesian Springfield Coal Member of the Petersburg Formation from the Eby Pit of Peabody Coal Company's Lynnville Mine (SW'/4 , SWA, NE'A, Sec.
    [Show full text]
  • Biostratigraphic Problems of Morrowan and Derryan (Atokan) Strata in the Pennsylvanian System of Western United States
    Biostratigraphic problems of Morrowan and Derryan (Atokan) strata in the Pennsylvanian System of western United States D. L. DUNN Gulf Research and Development Company, H.T.S.C., P.O. Box 36506, Houston, Texas 77036 ABSTRACT CONODONT ZONES Although both foraminiferal and conodont zonations have been Lane and Straka (1974) proposed a conodont zonation (Fig. 1) proposed for Lower and Middle Pennsylvanian strata, the current for Arkansas and Oklahoma utilizing slightly different terminology state of the art indicates that several proposed Morrowan cono- from that proposed by Lane and others (1971). They did not rec- dont zones and one important Derryan(?) fusulinid zone (21) and ognize the Streptognathodus expansus—S. suberectus, the the ranges of several important associated conodonts and Idiognathodus humerus—I. sinuosis, and the Streptognathodus fusulinids are in question. The conodont zones in question are the parvus—Adetognathus spathus Zones proposed earlier (Dunn, Gnathodus girtyi simplex, the Streptognathodus expansus-S. sub- 1970b), apparently because they did not believe these zones to be erectus, the Idiognathodus humerus—I. sinuosis, and the adequately documented in northeastern Oklahoma (Lane and Streptognathodus parvus— Adetognathus spathus Zones of Dunn Straka, 1974, p. 31). Lane and Straka (1974) have failed to recog- and the Idiognathodus sinuosis, I. klapperi, and 1. convexus nize the significance of some of the most important upper Mor- Zones of Lane and Straka. The conodonts whose ranges are in rowan index fossils now known — namely, those of the first and question are Gnathodus girtyi simplex, Rhachistognathus, third zones cited above — and, consequently, have demonstrated muricatus, Declinognathodus noduliferus, Adetognathus spathus, inconsistency in the correlation of Morrowan strata and in the Neognathodus bassleri bassleri, and Idiognathoides convexus.
    [Show full text]
  • BIASES in INTERPRETATION of the FOSSIL RECORD of CONODONTS by MARK A
    [Special Papers in Palaeontology, 73, 2005, pp. 7–25] BETWEEN DEATH AND DATA: BIASES IN INTERPRETATION OF THE FOSSIL RECORD OF CONODONTS by MARK A. PURNELL* and PHILIP C. J. DONOGHUE *Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK; e-mail: [email protected] Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK; e-mail: [email protected] Abstract: The fossil record of conodonts may be among and standing generic diversity. Analysis of epoch ⁄ stage-level the best of any group of organisms, but it is biased nonethe- data for the Ordovician–Devonian interval suggests that less. Pre- and syndepositional biases, including predation there is generally no correspondence between research effort and scavenging of carcasses, current activity, reworking and and generic diversity, and more research is required to bioturbation, cause loss, redistribution and breakage of ele- determine whether this indicates that sampling of the cono- ments. These biases may be exacerbated by the way in which dont record has reached a level of maturity where few genera rocks are collected and treated in the laboratory to extract remain to be discovered. One area of long-standing interest elements. As is the case for all fossils, intervals for which in potential biases and the conodont record concerns the there is no rock record cause inevitable gaps in the strati- pattern of recovery of different components of the skeleton graphic distribution of conodonts, and unpreserved environ- through time. We have found no evidence that the increas- ments lead to further impoverishment of the recorded ing abundance of P elements relative to S and M elements spatial and temporal distributions of taxa.
    [Show full text]