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Parallelodon multiliratus Girty 1909

Abstract

Parallelodon multiliratus Girty, 1909 Original source Girty (1909b): 39, pl. 3 figs 4, 4a, 5. Type stratum and age “Caney shale”; Kinderhookian? to Chesterian?, Middle Mississippian, Carboniferous (boundaries not clear). Type locality “Atoka quadrangle (station 2089), Tishomingo quadrangle (station 2085)”; the localities are further detailed in the appendix as: “ Atoka quadrangle, NE. 1/4 SE. 1/4 sec. 35, T. 2 S., R. 8 E. Caney shale (near top of chert)” and “ Tishomingo quadrangle, ravine a short distance (one-eighth mile) west of Viola ”; Oklahoma, United States of America. Type material Syntypes (USNM PAL 120754, 120742) are stored at the Smithsonian National Museum of Natural History, Paleobiology Collection, Washington, D.C. Remarks Mentioned by Aleksandri-Sadova (1965) and Hoare et al. (1989).

Authors 3

  1. University of Cologne

    Affiliation as printed

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

  2. 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. 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

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