Joint South-Central and North-Central Sections, both conducting their 41st Annual Meeting (11–13 April 2007)
Paper No. 30-7
Presentation Time: 10:40 AM-11:00 AM

TELYCHIAN (LLANDOVERY, SILURIAN) CONODONTS FROM A NEW STRATIGRAPHIC UNIT IN THE CHIMNEYHILL SUBGROUP, WEST CARNEY HUNTON FIELD, NORTH-CENTRAL OKLAHOMA

BADER, Jeremy D., Geosciences, Texas Tech University, 325 Science Building, Lubbock, TX 79409, styxfan24@yahoo.com, BARRICK, James E., Dept. of Geosciences, Texas Tech Univ, Lubbock, TX 79409-1053, and DERBY, James R., Geological Consultant, P.O. Box 178, Leonard, OK 74043

Twenty-eight cores from the West Carney Hunton Field (Logan and Lincoln Counties, Oklahoma) yielded late Llandovery (Silurian) conodont faunas from the Chimneyhill Subgroup of the Hunton Group. Five cores yielded late Llandovery (Telychian) conodonts from a previously unknown stratigraphic unit that lies between the Cochrane (Aeronian) and Clarita (Wenlock) formations. The main part of the field is a reef-dominated carbonate shoal consisting of reef facies in the Cochrane and lagoonal facies in both the Cochrane and the new Telychian unit. The lagoonal facies is a complex of pentamerid brachiopod mounds flanked by crinoid-, brachiopod- and/or coral-dominated grainstones. The Telychian lagoonal facies fauna includes Pterospathodus a. amorphognathoides, Pt. a. lennarti, Pt. a. angulatus, Pt. celloni, Ozarkodina p. polinclinata, Ozarkodina p. estonica, Aspelundia fluegeli and Asp. expansa. Species of Pterospathodus and Ozarkodina allow recognition of the Telychian Pt. eopennatus through Pt. a. amorphognathoides zones of Mannik, which are based on sections in the Baltic region. Distally two cores in nodular shaly limestones, dolostones, and shale yield deeper water faunas containing Aulacognathus bullatus, Aul. kuehni, Aul. latus, and Oulodus sigmoideus. We recognize three successive biozones based on species of Aulacognathus (Aul. bullatus, Aul. kuehni, and Aul. latus). The lack of Pterospathodus in the deeper water fauna makes it difficult to correlate this fauna to the lagoonal facies and to the standard Silurian conodont zonation. The occurrence of Pt. a. amorphognathoides at the top of the deeper water cores and the presence of Oz. polinclinata in the lagoonal facies indicates they are contemporaneous. Many of the species of these Telychian faunas have been found previously only as elements reworked into Late Silurian strata, but the strata from which they originated were unknown.

Joint South-Central and North-Central Sections, both conducting their 41st Annual Meeting (11–13 April 2007)
General Information for this Meeting
Session No. 30
Pander Society Symposium—Mixed-Up Conodonts: Extracting Useful Information and Solving Geologic Puzzles Using Stratigraphic Leaks and Redeposited Faunas
Kansas Union, University of Kansas: Woodruff Auditorium
8:10 AM-12:00 PM, Friday, 13 April 2007

Geological Society of America Abstracts with Programs, Vol. 39, No. 3, p. 62

© Copyright 2007 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.