Symmoriiform sharks from the Pennsylvanian of Nebraska

Authors

  • Michał Ginter University of Warsaw, Faculty of Geology, Żwirki i Wigury 93, PL-02-089 Warsaw

Keywords:

Symmoriiformes, Microfossils, Carboniferous, Indian Cave Sandstone, USA Midcontinent

Abstract

The Indian Cave Sandstone (Upper Pennsylvanian, Gzhelian) from the area of Peru, Nebraska, USA, has yielded numerous isolated chondrichthyan remains and among them teeth and dermal denticles of the Symmoriiformes Zangerl, 1981. Two tooth-based taxa were identified: a falcatid Denaea saltsmani Ginter and Hansen, 2010, and a new species of Stethacanthus Newberry, 1889, S. concavus sp. nov. In addition, there occur a few long, monocuspid tooth-like denticles, similar to those observed in Cobelodus Zangerl, 1973, probably representing the head cover or the spine-brush complex. A review of the available information on the fossil record of Symmoriiformes has revealed that the group existed from the Late Devonian (Famennian) till the end of the Middle Permian (Capitanian).

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Published

2018-09-30