Conodonts Frorn the Genesee Formation in Western New York

Total Page:16

File Type:pdf, Size:1020Kb

Conodonts Frorn the Genesee Formation in Western New York ·U.S: BUREAu Of MINES P.O. BOX 550 IUNEAU, AlASK} OQ9( ' Conodonts frorn the Genesee Formation in Western New York GEOLOGICAL SURVEY PROFESSIONAL PAPER 1032-B \ Conodonts from the Genesee Formation in Western New York By JOHN W. HUDDLE, assisted by JOHN E. REPETSKI STRATIGRAPHY AND CONODONTS OF THE GENESEE FORMATION (DEVONIAN) IN WESTERN AND CENTRAL NEW YORK GEOLOGICAL SURVEY PROFESSIONAL PAPER 1032-B Conodonts from the Genesee Formatz"on z"n western New York, first descrz"bed by G.]. Hz"nde z"n 1879 and W. L. Bryant z·n 1921, are redescrz"bed, and the b£ostrat£graph£c zones are determz"ned UNITED STATES GOVERNMENT PRINTING OFFICE,WASHINGTON 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secreta·ry GEOLOGICAL SURVEY Doyle G. Frederick, Acting Director Library of Congress Cataloging in Publication Data Huddle, John Warfield, 1907-1975 Conodonts from the Genesee Formation in western New York. (Stratigraphy and conodonts of the Genesee Formation (Devonian) in western and central New York) (Geological Survey professional paper ; 1032-B) Bibliography: p. Supt. of Docs. No.: I 19.16:1032-B 1. Conodonts. 2. Paleontology-Devonian. 3. Paleontology-New York (State) I. Title. II. Series. III. Series: United States. Geological Survey. Professional paper ; 1032-B. QE899.H83 557.3'08s [562] 77-608125 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 FOREWORD After John Huddle's death in late November 1975, I was asked to serve as author's representative in the completion of this report. In September 1975, Huddle had completed. the posttechnical review copy of his manuscript and had forwarded it for U.S. Geological Survey publica­ tion approval. I received the edited manuscript in September 1976, for review of accuracy of taxonomy and of technical matters and details noted by the Survey editors and by myself. My contribution consisted of checking for, and correcting where necessary, objective errors in the manuscript. In making necessary changes, I relied on Huddle's most recent worksheets, notes, and notes on specimen slides as much as possible in order to preserve the integrity of his work. No changes were made in subjective matters of taxonomy or of interpretation. Throughout my efforts on this paper, I have tried to avoid making any changes that would have affected Huddle's substance or style, so that this published report would be as· much as possible John Huddle's original work. John E. Repetski U.S. Geological Survey Washington, D.C. 1/12/77 III . I CONTENTS Page Page Abstract B1 Biostratigraphy-Continued Application of conodont zo11ation to New York Introduction -------------------------------------­ 1 Purpose of the investigation ------------------ 1 formations-Continued Age of the Penn Yan Shale Member of the Fieldvvork -----------------------------------­ 2 Laboratory preparation ----------------------- 2 Genesee Formation --------------------­ B15 Previous vvork ------------------------------­ 2 Age of the Williams Brook Coquinite Member of Ithaca facies of Caster (1933) ------­ 15 Acknovvledgtnents ----------------------------- 3 Age of the Genundevva Limestone Member Occurrence of conodonts in the Genesee· Formation -­ 3 3 of the Genesee Formation --------------­ 16 Distribution and abundance -------------------­ Age of the Crosby Sandstone Member of the Revvorked conodonts, lag concentrates, and un- Standish Formation as used by Torrey and 3 conformities -------------------------------- 16 9 others (1932) -------------------------­ Facies distribution ---------------------------- Age of the West River Shale Member of the 9 Biostratigraphy ---------------------------------­ Genesee Formation ---------------------- 16 Ammonoid zonation --------------------------­ 9 Systematic paleontology of conodonts ---------­ 16 Conodont zonation ---------------------------­ 9 Multielement versus element taxonomy ----­ 16 Polygnathus varcus Zone -----------------­ 11 Why element taxonomy is used in this report 18 Schmidtognathus hermanni-Polygnathus cri- Locality numbers and type depository ------ 18 status Zone ----------------------------- 12 Description of genera and spec·ies -------------­ 19 Polygnathus asymmetricus Zone ----------- 12 Platform and blade elements -------------­ 19 Problems in using the European range zon.es Platform elements -------------------­ 19 12 in vvestern Nevv York ------------------­ Blade elements ----------------------­ 33 Sequence of first appearances in the N evv Ozarkodinan elements --------------------­ 34 York Genesee Formation ---------------­ 13 Neoprioniodontan elements ---------------­ 39 Application of conodont zonation to Nevv York Hindeodellan elements --------------------­ 41 formations --------------------------------­ 14 Ligonodinan elements --------------------­ 44 Age of the Windom Member. of the Moscovv Lonchodinan elements --------------------- 45 Shale and th.e Tully Limestone ---------­ 14 Locality list -------------------------------------­ 47 Age of the Geneseo Shale Member and asso- References cited ---------------------------------- 57 ciated beds of the Genesee Formation __ _ 14 Index -------------------------~------------------ 63 ILLUSTRATIONS [Plates 1-31 following index] PLATE 1-3. Ancyrodella. 4, 5. Icriodus. 6. Palmatolepis? and Polygnathus. 7-17. Polygnathus. 18. Polygnathus and N othognathella. 19. Prioniodina, Polygnathus, Spathognathodus, Pandorinellina, and Synprioniodina. 20. Bryantodus and Ozarkodina. 21. Bryantodus. 22. Bryantodus and Ozarkodina. 23. N eoprioniodus and Synprioniodina. 24. H indeodella. 25. Hindeodella and Angulodus. 26. Bryantodus, Angulodus, Ozarkodina, and Enantiognathus. 27. Enantiognathus and Ligonodina. 28. Ligonodina and Prioniodina. 29. Bryantodus, Prioniodina, Lonchodina, ·and Trichonodella. 30. Prioniodina, Lonchodina, Trichonodella, and Bryantodus?. 31. Bryantodus, Lonchodina, and Prioniodina. v VI CONTENTS Page PLATE 32. Diagram showing the sequential appearance of conodont species in the basal beds of the Genesee For- mation ---------------------------------------------------------------------------------In pocket FIGURE 1. Stratigraphy and conodont zonation of the Belgian Frasnian stratotype section ------------------- Bll TABLES Page TABLE 1. Occurrence of conodonts by species, sample number, and stratigraphic units ----------------·---- In pocket 2. Range chart of conodont :species by first ap·pea.rances ---------------------------------------------- B4 3. Occurrence, from west to east for each member, of conodonts in samples of the Windom Member of the Moscow Shale and the Tully Limestone ------------------------------------------------------ 6 4. Occurrence, from west to east, of platform and blade conodonts in the Leicester Marcasite Member of Moscow Formation of Sutton (1951) and the North Evans Limestone of Rickard (1964) ------- 7 5. Early Late Devonian ammonoid zonation in Europe and New York -------------------------------- 9 6. Comparison of European and North American conodont zonation --------------------------------- 10 STRATIGRAPHY AND CONODONTS OF THE GENESEE FORl\tiATION (DEVONIAN) IN \VESTERN AND CENTRAL NE\V YORK CONODONTS FROM THE GENESEE FORMATION IN WESTERN NEW YORK By JoHN W. HuDDLE/ assisted by JoHN E. REPETSKI ABSTRACT erence section in North America and with the cor­ Conodonts from the Genesee Formation in western New relation of these rocks with Upper Devonian rocks York were first described by G. J. Hinde in 1879, and cono­ in other areas. These studies were intended to aid donts from the "conodont bed" (North Evans Limestone of in the search for oil and gas in New York, Pennsyl­ Rickard, 1964) were desc·ribed by W. L. Bryant in 1921. vania, and Ohio. Many new species and genera were named in these reports, and a multielement species was proposed by Hinde. Taxo­ This study of the conodont faunas of the Genesee nomic revision, redescription, and improved illustrations of Formation in western New York was carried out these species are given in the present report, which also from 1956 to 1959 by W. H. Hass in cooperation documents the ranges of conodonts in the classic New York with a study of the physical stratigraphy of the Devonian section and relates their ranges to the occurrence formation by Wallace de Witt, Jr., and G. W. Colton. of ammonoids. Sixty-eight element sp,ecies of conodonts are described, including one new species, Polygnathus collieri, I continued the study of the conodonts after 1962. and three new subspecies, Polygnathus rhenanus marijae, P. The sequence of first appearances of conodont asymmetricus unilabius, and P. dubius frons. species in New York does not correspond to that of the standard European ~onodont ~onation; the zona­ INTRODUCTION tion of Klapper and others (1971) for North Amer- PURPOSE OF THE INVESTIGATION ica is used here for the conodont zones near the Chapter A of this Professional Paper (de Witt boundary between the Middle and Upper Devonian. and CoUon, 1978) is the report of work done by Conodont zo~e,~ ne~r this boundary need revision, U.S. Geological Survey parties under the direction but such revisiOn IS not done here. The boundary of James F. Pepper as part of a study of the origin I between the Middle and Upper Devonian is not dis­ and occurrence of black petroliferous shales. Field cussed here because i.t is not de,finable in central parties began measuring sections and mapping in I and ~estern New York until international agree- 1947: More than 400 sections were measured in I ment IS reach:d
Recommended publications
  • The Unique Devonian of Immouzer-Du-Kandar (Middle Atlas Basement) – Biostratigraphy, Faunas, and Facies Development
    Aboussalam & al. Devonian of Immouzer-du-Kandar The unique Devonian of Immouzer-du-Kandar (Middle Atlas basement) – biostratigraphy, faunas, and facies development ZHOR SARAH ABOUSSALAM, RALPH THOMAS BECKER, JULIA RICHTER, SVEN HARTENFELS, AHMED EL HASSANI & STEPHAN EICHHOLT Fig. 1: View (from the hill at Douar Ahmed-ben-Mellouk) on Devonian exposures of Immouzer-du-Kandar (hill rising from Chabat el Jenanet, Sections C2 and C3 of CYGAN et al. 1990), our Section C4, with outcrop of the lower Emsian conglomerate (Chabat Jenanet Formation) along and above the track, faulted upper Emsian to lower Givetian limestones in the lower slope (new Ahmed-ben-Mellouk Formation), the reef breccia forming a small terrace ca. 2/3 upwards, and the Famennian upper slope (new Chabat el Hallouf Formation, Section C5) towards the top. The slope to the left (NNE) is occupied by Triassic red beds. Section numbers are marked in circles. 1. Introduction Mesozoic Middle Atlas, with the best and most important outcrops in the tectonic window The Middle Atlas divides the Moroccan (“boutonnière”) at Immouzer-du-Kandar, ca. Meseta into the Western and Eastern Meseta, 40 km S of Fès. The wooded Jebel Kandar to which differ strongly in the Devonian in terms the SW is a more than 1600 m high mountain of facies and synsedimentary structural built of Jurassic strata (Fig. 2). Fossiliferous geology (e.g., overviews of EL HASSANI & Ordovician to Lower Carboniferous BENFRIKA 1995, 2000). There is restricted formations crop out to the NW, from Dour knowledge of the Palaeozoic basement of the Rouda towards the SE, the Chabat el Jenanet, Hassan II Academy of Science and Technology Frontiers in Science and Engineering - Vol.
    [Show full text]
  • Download This PDF File
    Acta Geologica Polonica, Vol. 50 (2000), No. 1, pp. 67-97 Revision of ammonoid biostratigraphy in the Frasnian (Upper Devonian) of the Southern Timan (Northeast Russian Platform) R. THOMAS BECKER1, MICHAEL R. HOUSE2, VLADIMIR V. MENNER3 & N. S. OVNATANOVA4 1 Museum für Naturkunde der Humboldt-Universität zu Berlin, Invalidenstr. 43, D-10115 Berlin, Germany. E-mail: [email protected] 2 School of Ocean and Earth Science, Southampton Oceanography Centre, European Way, Southampton, SO 14 3ZH, U.K. 3 Institute of Geology and Exploitation of Combustible Fuel, Fersman 50, Moscow 117312, Russian Federation 4 All-Russia Research Geological Oil Prospecting Institute, Shosse Entuziastov 36, Moscow 105819, Russian Federation ABSTRACT: BECKER, R.T., HOUSE, M.R., MENNER, V.V. & OVNATANOVA, N.S. (2000). Revision of ammonoid biostratig- raphy in the Frasnian (Upper Devonian) of the Southern Timan (Northeast Russian Platform). Acta Geologica Polonica, 50 (1), 67-97, Warszawa. New field work in outcrops of the Ukhta Region (Southern Timan) together with the re-exanimation of former collections allows a detailed revision of the ammonoid zonation in one of the classical Frasnian regions of Russia. There is a total of 47 species, 18 of which are new or recorded for the first time from the region. The latter applies to representatives of Linguatornoceras, Phoenixites, Aulatornoceras s.str. and Acantho- clymenia. New taxa are Chutoceras manticoides n.gen. n.sp. and Linguatornoceras yudinae n.sp. In the Ust’yarega Formation regional Hoeninghausia nalivkini, Timanites keyserlingi and Komioceras stuckenber- gi Zones can be recognized which correlate with the international Frasnian divisions UD I-B/C.
    [Show full text]
  • G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine
    DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY GEOLOGY OF THE CRAIG QUADRANGLE, ALASKA By G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine Open-File Report 83-91 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and strati graphic nomenclature Menlo Park, California 1983 Geology of the Craig Quadrangle, Alaska By G. D. Eberlein, Michael Churkin, Jr., Claire Carter, H. C. Berg, and A. T. Ovenshine Introduction This report consists of the following: 1) Geologic map (1:250,000) (Fig. 1); includes Figs. 2-4, index maps 2) Description of map units 3) Map showing key fossil and geochronology localities (Fig. 5) 4) Table listing key fossil collections 5) Correlation diagram showing Silurian and Lower Devonian facies changes in the northwestern part of the quadrangle (Fig. 6) 6) Sequence of Paleozoic restored cross sections within the Alexander terrane showing a history of upward shoaling volcanic-arc activity (Fig. 7). The Craig quadrangle contains parts of three northwest-trending tectonostratigraphic terranes (Berg and others, 1972, 1978). From southwest to northeast they are the Alexander terrane, the Gravina-Nutzotin belt, and the Taku terrane. The Alexander terrane of Paleozoic sedimentary and volcanic rocks, and Paleozoic and Mesozoic plutonic rocks, underlies the Prince of Wales Island region southwest of Clarence Strait. Supracrustal rocks of the Alexander terrane range in age from Early Ordovician into the Pennsylvanian, are unmetamorphosed and richly fossiliferous, and aopear to stratigraphically overlie pre-Middle Ordovician metamorphic rocks of the Wales Group (Eberlein and Churkin, 1970).
    [Show full text]
  • An Examination of the Devonian Bedrock and Overlying Pleistocene Sediments at Messerly & Morgan Quarries, Blackhawk County, Iowa
    FromFFrroomm OceanOOcceeaann tottoo Ice:IIccee:: AnAAnn examinationeexxaammiinnaattiioonn ofooff thetthhee DevonianDDeevvoonniiaann bedrockbbeeddrroocckk andaanndd overlyingoovveerrllyyiinngg PleistocenePPlleeiissttoocceennee sedimentssseeddiimmeennttss ataatt MesserlyMMeesssseerrllyy &&& MorganMMoorrggaann Quarries,QQuuaarrrriieess,, BlackBBllaacckk HawkHHaawwkk County,CCoouunnttyy,, IowaIIoowwaa Geological Society of Iowa ______________________________________ April 24, 2004 Guidebook 75 Cover photograph : University of Northern Iowa Professor and field trip leader Dr. Jim Walters points to a stromatoporoid-rich bed in the Osage Springs Member of the Lithograph City Formation at the Messerly Quarry, the first stop of this field trip From Ocean to Ice: An examination of the Devonian bedrock and overlying Pleistocene sediments at Messerly & Morgan Quarries, Blackhawk County, Iowa prepared and led by: James C. Walters Department of Earth Science University of Northern Iowa Cedar Falls, IA 50614 John R. Groves Department of Earth Science University of Northern Iowa Cedar Falls, IA 50614 Sherman Lundy 4668 Summer St. Burlington IA 52601 with contributions by: Bill J. Bunker Iowa Geological Survey Iowa Department Natural Resources Iowa City, Iowa 52242-1319 Brian J. Witzke Iowa Geological Survey Iowa Department Natural Resources Iowa City, Iowa 52242-1319 April 24, 2004 Geological Society of Iowa Guidebook 75 i ii Geological Society of Iowa TABLE OF CONTENTS From Ocean to Ice: An examination of the Devonian bedrock and overlying Pleistocene
    [Show full text]
  • Evidence for the Presence of the Global Late Devonian Kellwasser
    СПИСАНИЕ НА БЪЛГАРСКОТО ГЕОЛОГИЧЕСКО ДРУЖЕСТВО, год. 80, кн. 3, 2019, с. 113–115 REVIEW OF THE BULGARIAN GEOLOGICAL SOCIETY, vol. 80, part 3, 2019, p. 113–115 Национална конференция с международно участие „ГЕОНАУКИ 2019“ National Conference with international participation “GEOSCIENCES 2019” Evidence for the presence of the global Late Devonian Kellwasser Event in the Berende section (Parchar Formation, Western Bulgaria) Доказателства за присъствие на глобалното къснодевонско събитие Kellwasser в разрез Беренде (Пърчарска свита, Западна България) Iliana Boncheva1, Valeri Sachanski1,2, Polina Andreeva1, Stoyan Tanatsiev2 Илияна Бончева1, Валери Сачански1,2, Полина Андреева1, Стоян Танациев2 1 Geological Institute, Bulgarian Academy of Sciences, Acad. G. Bonchev str., bl. 24, 1113 Sofia, Bulgaria; E-mails: [email protected]; [email protected]; [email protected] 2 University of Mining and Geology “St. Ivan Rilski”, 1 Prof. Boyan Kamenov str., Studentski Grad, 1700 Sofia, Bulgaria; E-mails: [email protected]; [email protected] Keywords: Late Kellwasser Event, Frasnian/Famennian boundary, conodonts, Western Bulgaria. Introduction Spassov, 1985; Boncheva, Yanev, 1993; Boncheva et al., 2015). The Frasnian–Famennian mass extinction is strati- Tsarichina section (Svoge Unit). According graphically associated with the famous Kellwas- to previous studies, the turbiditic accumulation in ser Event (cf., Buggisch, 1991; McGhee, 1996). It the Svoge Unit starts in Givetian, when siliciclas- is one of the largest Phanerozoic mass extinction tic and cherty rocks were deposited (Katina Forma- events that affects most of the global tropical ma- tion). Later, during the Late Devonian, a deposition rine ecosystems (e.g., Sandberg et al., 1988; Mor- of thick flysch succession of conglomerates, sand- row, 2000).
    [Show full text]
  • Calcium Stable Isotopes Place Devonian Conodonts As First Level Consumers V
    Calcium stable isotopes place Devonian conodonts as first level consumers V. Balter, J.E. Martin, T. Tacail, G. Suan, Sabrina Renaud, Catherine Girard To cite this version: V. Balter, J.E. Martin, T. Tacail, G. Suan, Sabrina Renaud, et al.. Calcium stable isotopes place Devonian conodonts as first level consumers. Geochemical Perspectives Letters, European Assoication of Geochemistry, 2019, 10, pp.36-39. 10.7185/geochemlet.1912. hal-02112869 HAL Id: hal-02112869 https://hal.archives-ouvertes.fr/hal-02112869 Submitted on 27 Apr 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. © 2019 The Authors Published by the European Association of Geochemistry Calcium stable isotopes place Devonian conodonts as first level consumers V. Balter1*, J.E. Martin1, T. Tacail2, G. Suan1, S. Renaud3, C. Girard4 Abstract doi: 10.7185/geochemlet.1912 Conodont animals are an extinct group of jawless vertebrates whose hard parts, also known as conodont elements, represent the earliest evidence of a mineralised skeleton in the vertebrate lineage. Conodont elements are interpreted as parts of a feeding apparatus, which together with the presence of eyes and microwear patterns, support the controversial hypothesis that conodont animals were macrophagous predators and/or scavengers.
    [Show full text]
  • Taxonomic Note Palmatolepis Spallettae, New Name for a Frasnian
    Journal of Paleontology, 91(3), 2017, p. 578 Copyright © 2017, The Paleontological Society 0022-3360/15/0088-0906 doi: 10.1017/jpa.2017.21 Taxonomic Note Palmatolepis spallettae, new name for a Frasnian conodont species Gilbert Klapper,1 Thomas T. Uyeno,2 Derek K. Armstrong,3 and Peter G. Telford4 1Department of Earth and Planetary Sciences, Northwestern University, Evanston, Illinois 60208, USA 〈[email protected]〉 2Emeritus, Geological Survey of Canada, 3303-33rd St NW, Calgary, Alberta, T2L 2A7, Canada 〈[email protected]〉 3Ontario Geological Survey, 933 Ramsey Road, Sudbury, Ontario, P3E 6B5, Canada 4Departmental Associate, Department of Palaeobiology, Royal Ontario Museum, 100 Queen’s Park, Toronto, Ontario, M5S 2C6, Canada R. Thomas Becker and Sven Hartenfels of the Westfälische (Klapper et al., 2004, p. 375); this is the preferred zonal Wilhelms-Universität, Münster, Germany, have kindly terminology used in that paper, as well as was formalized by informed us that the name Palmatolepis nodosa (Klapper et al., Klapper and Kirchgasser (2016). 2004, p. 381) based on a Frasnian conodont species from northern Ontario is preoccupied. An earlier name, Palmatolepis References marginifera nodosus, was established by Xiong (1983, p. 313) based on a Famennian conodont subspecies from southwest Klapper, G., and Kirchgasser, W.T., 2016, Frasnian Late Devonian conodont China. Species and subspecies within the same genus are biostratigraphy in New York: graphic correlation and taxonomy: Journal of coordinate for the purposes of homonymy. Nor does it prevent Paleontology, v. 90, p. 525–554. Klapper, G., Uyeno, T.T., Armstrong, D.K., and Telford, P.G., 2004, Conodonts homonymy that Xiong used a masculine ending for his of the Williams Island and Long Rapids formations (Upper Devonian, subspecies, as it is automatically corrected to a feminine ending Frasnian–Famennian) of the Onakawana B Drillhole, Moose River Basin, to agree with the gender of the genus name.
    [Show full text]
  • Conodont Biostratigraphy and Paleoecology of The
    CONODONT BIOSTRATIGRAPHY AND PALEOECOLOGY OF THE LOWER DEVONIAN HELDERBERG GROUP OF VIRGINIA by Elizabeth G. Cook Thesis submitted to the Graduate Faculty of the Virginia Polytechnic Institute and State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in Geological Sciences APPROVED: Dr. C. G. Tillman, Chairman -------------~-""'\-----7----- --------------------~-~------- Dr. W. D.)Lowry Dr. J. F. Read May, 1981 Blacksburg, Virginia ACKNOWLEDGEMENTS I thank Dr. Tillman for proposing the problem and for continued help and encouragement during the research and writing of the thesis. Dr. J. F. Read and W. D. Lowry offered constructive criticism of the ' ' manuscript. Thanks are also due to William Seaton for assistance with some of the sampling and to Gordon Love for assistance with the photography. I also acknowledge financial support from the Department of Geological Sciences at Virginia Polytechnic Institute and State University. E. G. C. ii TABLE OF CONTENTS Page ACKNOWLEDGEMENTS ii LIST OF FIGURES vi LIST OF TABLES vii INTRODUCTION • 1 LOCATION OF SECTIONS 3 METHODS 5 STRUCTURAL SETTING • 7 STRATIGRAPHY • 8 Introduction • 8 Previous Work 8 Description of Formations in the Study Area 10 Keyser Formation • • 10 New Creek Limestone 12 Healing Springs Sandstone 12 Corriganville Limestone 13 Licking Creek Formation 13 Regional Correlation 14 DEPOSITIONAL ENVIRONMENTS 17 Introduction • • 17 Keyser Formation 17 Laminated limestone lithofacies 17 Nodular limestone lithofacies 20 Cross-stratified sand lithofacies 22 iii Page Shale lithofacies 23 Deeper water facies 23 Swmnary of Keyser facies in the study area • 24 New Creek Limestone 24 Healing Springs Sandstone 25 Corriganville Limestone 26 Licking Creek Formation 26 Cherry Run Member 26 Little Cove Member .
    [Show full text]
  • Conodont Stratigraphy of a Highly Tectonised Silurian-Devonian Section in the San Basilio Area (SE Sardinia, Italy)
    Bollettino della Societa Paleontologica Italiana 40 (3), 2001 ISSN 0375-7633 Modena, Dicembre 2001 Conodont stratigraphy of a highly tectonised Silurian-Devonian section in the San Basilio area (SE Sardinia, Italy) Carlo CORRADINI F rancesco LEONE Alfredo Loi Enrico SERPAGLI Dipartimento del Museo di Paleobiologia Dipartimento di Scienze della Terra Dipartimento del Museo di Paleobiologia e dell'Orto Botanico Universita di Cagliari e dell'Orto Botanico Universidt di Modena e Reggio Emilia Universita di Modena e Reggio Emilia KEYWORDS- Conodonts, Biostratigraphy, Tectonics, Silurian, Devonian, SE Sardinia. ABSTRACT- Several conodont species belonging to five "late Silurian biozones (Ancoradella ploeckensis, Polygnathoides siluricus, Ozarkodina crispa, Ozarkodina remscheidensis, Oulodus elegans detortus) and four Early and Late Devonian biozones (delta, pesavis, kitabicus-excavatus and Late rhenana) allow a better interpretation of stratigraphy and tectonics of the San Basilio area in western Gerrei. Frasnian sediments are documented for the first time in SE Sardinia. RIASSUNTO- [Stratigrafia a conodonti di una sezione forremente tettonizzata di eta Siluriano-Devoniano nell'area di San Basilio (Sardegna SE)] - Grazie alla biostratigrafia a conodonti viene interpretata la complessa tettonica di una sezione nell'area di San Basilio (Sardegna sud-orientale) e viene ricostruita la successione originaria. Sono documentate cinque biozone a conodonti del Siluriano superiore (Ancoradella eioeckensis, Polygnathoides siluricus, Ozarkodina crispa,
    [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]
  • Upper Devonian Depositional and Biotic Events in Western New York
    MIDDLE- UPPER DEVONIAN DEPOSITIONAL AND BIOTIC EVENTS IN WESTERN NEW YORK Gordon C. Baird, Dept. of Geosciences, SUNY-Fredonia, Fredonia, NY 14063; D. Jeffrey Over, Dept. of Geological Sciences, SUNY-Geneseo, Geneseo, NY 14454; William T. Kirch gasser, Dept. of Geology, SUNY-Potsdam, Potsdam, NY 13676; Carlton E. Brett, Dept. of Geology, Univ. of Cincinnati, 500 Geology/Physics Bldg., Cincinnati, OH 45221 INTRODUCTION The Middle and Late Devonian succession in the Buffalo area includes numerous dark gray and black shale units recording dysoxic to near anoxic marine substrate conditions near the northern margin of the subsiding Appalachian foreland basin. Contrary to common perception, this basin was often not stagnant; evidence of current activity and episodic oxygenation events are characteristic of many units. In fact, lag deposits of detrital pyrite roofed by black shale, erosional runnels, and cross stratified deposits of tractional styliolinid grainstone present a counter intuitive image of episodic, moderate to high energy events within the basin. We will discuss current-generated features observed at field stops in the context of proposed models for their genesis, and we will also examine several key Late Devonian bioevents recorded in the Upper Devonian stratigraphic succession. In particular, two stops will showcase strata associated with key Late Devonian extinction events including the Frasnian-Famennian global crisis. Key discoveries made in the preparation of this field trip publication, not recorded in earlier literature,
    [Show full text]