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3 edition of Organic-walled microphytoplankton of the Sylvan Shale (Richmondian : Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A. found in the catalog.

Organic-walled microphytoplankton of the Sylvan Shale (Richmondian : Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A.

Geoffrey Playford

Organic-walled microphytoplankton of the Sylvan Shale (Richmondian : Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A.

by Geoffrey Playford

  • 249 Want to read
  • 20 Currently reading

Published by Oklahoma Geological Survey in [Norman] .
Written in English

    Subjects:
  • Phytoplankton, Fossil -- Oklahoma -- Arbuckle Mountains,
  • Shale -- Oklahoma -- Arbuckle Mountains,
  • Geology, Stratigraphic -- Ordovician

  • Edition Notes

    Includes bliographical references (p. 39-45) and index.

    StatementGeoffrey Playford, Reed Wicander.
    SeriesBulletin / Oklahoma Geological Survey -- 148, Bulletin (Oklahoma Geological Survey) -- 148.
    ContributionsWicander, Reed, 1946-
    Classifications
    LC ClassificationsQE955 .P53 2006, QE153 .A2 no.148
    The Physical Object
    Paginationiv, 116 p. :
    Number of Pages116
    ID Numbers
    Open LibraryOL16322398M
    LC Control Number2007414147

    Bibliography of Oklahoma Palynology Brian J. Cardott Oklahoma Geological Survey and E.R. Wicander, , Organic-walled micro-phytoplankton from the Lower Devonian (Late Gedinnian) Haragan and Bois d'Arc Formations of Playford, G., and R. Wicander, , Organic-walled microphytoplankton of the Sylvan Shale (Richmondian, Upper. The Palaeozoic rock units mainly, Ghelli, Niur, Padeha, Khoshyeilagh and Mobark formations are well-exposed in the north of Robat-e Gharabil village. out of surface samples were analyzed to determine aged relationships of Ghelli Formation. The samples of Ghelli Formation are dominated by acritarchs (42 species belonging to 23 genera) and chitinozoans (26 species distributing among 15 Author: M. Ghavidel-Syooki, S. Borji.

    American League West by Clendening, John and a great selection of related books, a new Acritarch Genus from the Middle Cambrian Rogersville Shale of Tennessee, USA (Palynology, Volume 5, , pp. ). Organic - Walled Microphytoplankton and Chitinozoans from the Middle Devonian (Givetian) Boyle Dolomite of Kentucky, U.S.A. It is found that the Posedonia shale is comparable to several U.S.A. shale pays in terms of geological and petrophysical attributes (porosity, permeability, thickness, gas, oil and water content water). Therefore, we expect the multi-stage fracturing techniques developed in the U.S.A. to be largely applicable for the Posedonia by: 2.

    mation, a calcareous to silty shale with in-terbedded argillaceous, biofragmental, and fine to medium-grained limestones (ocality 6), in Indiana. SYSTEMATIC PALEONTOLOGY As in our earlier publications on the organic-walled microphytoplankton, taxa are arranged alphabetically. The very recent and rapid ex-pansion of knowledge of this group has shown.   Cengage Learning's HISTORICAL GEOLOGY brings course concepts to life with interactive learning, study, and exam preparation tools along with comprehensive text content for historical geology courses. Adopt the resources that enable your students to purchase the right solution to meet their needs, whether it's a traditional printed text, all digital learning platform, or package that .


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Organic-walled microphytoplankton of the Sylvan Shale (Richmondian : Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A by Geoffrey Playford Download PDF EPUB FB2

Get this from a library. Organic-walled microphytoplankton of the Sylvan Shale (Richmondian: Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A.

[Geoffrey Playford; Reed Wicander]. Systematics and biostratigraphy of the organic-walled microphytoplankton from the Middle Devonian (Givetian) Silica Formation, Ohio, U.S.A (AASP contributions series) [Wicander, Reed] on *FREE* shipping on qualifying offers.

Systematics and biostratigraphy of the organic-walled microphytoplankton from the Middle Devonian (Givetian) Silica Formation. The University of Queensland's institutional repository, UQ eSpace, aims to create global visibility and accessibility of UQ’s scholarly research.

Organic-walled microphytoplankton of the Sylvan Shale (Richmondian: Upper Ordovician), Arbuckle Mountains, southern Oklahoma, by: Home › Organic-walled microphytoplankton of the Sylvan shale (Richmondian: Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A The University of Queensland, Australia Brisbane St Lucia, QLD Organic-walled microphytoplankton of the Sylvan Shale (Richmondian: Upper Ordovician), Arbuckle Mountains, southern Oklahoma, : G.

Playford and R. Wicander. October Bibliography of Sylvan Shale Brian J. Cardott Oklahoma Geological Survey Burruss, R.C., and J.R. Hatch,Geochemistry of oils and hydrocarbon source Organic-walled microphytoplankton of the Sylvan Shale (Richmondian, Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A.: OGS BulletinSize: 12KB.

An abundant, diverse, and well-preserved organic-walled microphytoplankton assemblage is described from the Upper Ordovician Bill's Creek Shale and the lower Stonington Formation (Bay de Noc Member) in the Upper Peninsula of Michigan, U.S.A.

Based on graptolite and conodont evidence, the Bill's Creek Shale and Stonington Formation are Richmondian (=Ashgill) in by: Book. Historical geology: evolution of earth and life through time. Organic-walled microphytoplankton of the Sylvan Shale (Richmondian: Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A.

Playford, G. and Wicander, R. () Organic-walled microphytoplankton of the Sylvan Shale (Richmondian: Upper Ordovician), Arbuckle. organic-walled microfossils in the Sylvan Shale, and the only attempt to describe them systematically. The possibility exists, however, that chitinozoans were encountered in fossil residues of the Sylvan Shale as early as A short publication by Thomas () contains (p.

Organic-walled Microplankton in the Subsurface Ordovician of Northeastern Kansas The Ashgillian Sylvan Shale assemblage is the most similar by comparison with Leiofusa litotes, Baltisphaeridium perclarumOrganic-walled microphytoplankton from the Eden Shale (Upper Ordovician), Indiana, U.S.A.: Palaeontographica, Abteilung B, v.

Organic-walled microphytoplankton of the Sylvan shale (Richmondian: Upper Ordovician), Arbuckle Mountains, southern Oklahoma, U.S.A. Oklahoma Geological Survey BulletinOklahoma Geological Survey Bulletin. i-iv, Organic-Walled Microphytoplankton of the Sylvan Shale (Richmondian: Upper Ordovician), Arbuckle Mountains, Southern Oklahoma, by Geoffrey Playford and Reed Wicander.

pages. Bulletin A synopsis of the Pleistocene vertebrates of Oklahoma, by Kent S. Smith and Richard L. Cifelli. 36 pages, 1 figure, 14 tables. Bulletin Sylvan Shale of Oklahoma (Loeblich, ) which is generally understood to be of Ashgill age, but is rare in the Eden Shale (Caradoc) of Indiana (Colbath, ) and in the type section of the Caradoc Series in Shrop- shire, England (Turner, ).

The common occur- Cited by: other microfossils from the upper Sylvan Shale and Keel Formation (Late Ordovician), Arbuckle Mountains, Oklahoma, USA: Program with Abstracts, Geological Association of Canada and Mineralogical Association of Canada, v. 29, p.

Playford, G., and R. Wicander,Organic-walled microphytoplankton of the SylvanFile Size: 13KB. Wicander, Reed and Playford, Geoffrey () Organic-walled microphytoplankton from the Middle Devonian (Givetian) Gravel Point Formation, Michigan, USA.

Palynology, 41 sup1: doi: / On the evolution of the elastic properties of organic-rich shale upon pyrolysis-induced thermal maturation Adam M.

Allan 1, Anthony C. Clark, Tiziana Vanorio, Waruntorn Kanitpanyacharoen2, and Hans-Rudolf Wenk3 ABSTRACT The evolution of the elastic properties of organic-rich shale as a function of thermal maturity remains poorly Size: 7MB.

An abundant, diverse, and well-preserved organic-walled microphytoplankton assemblage is described from the Upper Ordovician Bill's Creek Shale and the lower Stonington Formation (Bay de Noc.

The Ames structure is an hidden crater located in northwestern Oklahoma (centered at about 36° 15′ N, 98° 12′ W) at km below the surface on top of the Cambro–Ordovician Sylvan shale. THE CHANGING EARTH: EXPLORING GEOLOGY AND EVOLUTION, Sixth Edition, is a member of a rare breed of texts written specifically for courses covering both physical and historical geology but it also stands apart by other measures.

Three interrelated themes (plate tectonics, organic evolution, and geologic time) help students understand that Earth is a complex, integrated, and 5/5(1). Sylvan shale. In West Texas (Permian basin), exposed at surface in Marathon uplift and southeast Marathon basin. Consists of green, waxy, fissile argillite or brown arenaceous shale, weathers pinkish, 20 to 50 feet thick.

Extends, in subsurface, north to Terry and Lynn Counties as greenish-gray shale with disseminated mica and pyrite; contains.

Peter E. Isaacson, "Devonian brachiopods from Northeastern Washington: Evidence for a non-allochthonous terrane and Late Devonian biogeographic update", The Terrane Puzzle: New Perspectives on Paleontology and Stratigraphy from the North American .Geologic unit mapped in Oklahoma: ARDMORE-SHERMAN- "Sylvan," shale, dark-greenish-gray; thickness, 60 to feet.

"Fernvale" and "Viola," limestone, gray, fine- to coarse-grained; thickness, to feet. Occurs in the ARBUCKLE MTNS.Two new species of trilobites from the Middle Devonian silica shale of northwestern Ohio, (Contributions from the Museum of Paleontology, University of Michigan) [Stumm, Erwin Charles] on *FREE* shipping on qualifying offers.

Two new species of trilobites from the Middle Devonian silica shale of northwestern Ohio, (Contributions from the Museum of Paleontology.