Lithic and Conodont Succession of Silurian Strata, Batesville District, Arkansas

Abstract

Research Article| August 01, 1969 Lithic and Conodont Succession of Silurian Strata, Batesville District, Arkansas WILLIAM W CRAIG WILLIAM W CRAIG Department of Earth Sciences, Louisiana State University, New Orleans, Louisiana Search for other works by this author on: GSW Google Scholar GSA Bulletin (1969) 80 (8): 1621–1628. https://doi.org/10.1130/0016-7606(1969)80[1621:LACSOS]2.0.CO;2 Article history received: 06 Dec 1968 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation WILLIAM W CRAIG; Lithic and Conodont Succession of Silurian Strata, Batesville District, Arkansas. GSA Bulletin 1969;; 80 (8): 1621–1628. doi: https://doi.org/10.1130/0016-7606(1969)80[1621:LACSOS]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract In ascending order the Cason Shale consists of phosphatic sandstone and shale, oölitic limestone, pelmatozoan limestone, and sandy, calcareous shale containing abundant ellipsoidal algal growths. Conodonts from these units and the overlying St. Clair and Lafferty Limestones indicate the occurrence of Bereich I and the celloni-Zone, amorphognathoides-Zone, sagittus-Zone, and siluricus-Zone of Walliser's (1964) European conodont zonation. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.