Parallelodon depressus Hyde 1953

Abstract

Parallelodon depressus Hyde, 1953 Original source Hyde (1953): 299. Type stratum and age “sandstone in the Allensville member of the Logan formation”; earliest Osagean (upper Tournaisian), Mississippian, Carboniferous (Matchen & Kammer 2006). Type locality Rushville, Ohio, United States of America. Type material Specimens are stored at Ohio State University, O.S.U. No. 19671. Driscoll (1965: 100, pl. 16 figs 4–5) figured the holotype and paratype and synonymised the species with P. marshallensis (Winchell, 1862). He considered the other specimens as not belonging to Parallelodon.

Authors 3

1. Julia C. Friedel

   University of Cologne

   Affiliation as printed

   Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49 a, 50674 Cologne, Germany

2. Thomas A. Neubauer Aachen Department of Earth and Environmental Sciences

   Ludwig-Maximilians-Universität München · Bavarian Natural History Collections · Naturalis Biodiversity Center · Bayerische Staatssammlung für Paläontologie und Geologie

   Affiliation as printed

   SNSB - Bavarian State Collection for Palaeontology and Geology, Richard-Wagner-Strasse 10, 80333 Munich, Germany. & Department of Earth and Environmental Sciences, Palaeontology & Geobiology, Ludwig-Maximilians-Universität München, Richard-Wagner-Str. 10, 80333 Munich, Germany. & Naturalis Biodiversity Center, Darwinweg 2, 2333 CR Leiden, The Netherlands

3. Michael R. W. Amler

   University of Cologne · Philipps University of Marburg

   Affiliation as printed

   Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49 a, 50674 Cologne, Germany. & Department of Geography, Philipps-Universität Marburg, Deutschhausstr. 10, 35032 Marburg, Germany