Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Services Email this article to a friend Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via Google Scholar Google Scholar Articles by Grier, J. W. Articles by Petersen, J. G. Search for Related Content GeoRef GeoRef Citation

Synonymy of the ammonite genus Ponteixites Warren with Rhaeboceras Meek

¹ Department of Biological Sciences, North Dakota State University, Fargo, ND 58102-3400, U.S.A.
² 17648 57th Ave N, Hawley, MN 56549, U.S.A.
³ Black Hills Institute of Geological Research, Inc., 117 Main Street, Hill City, SD 57745, U.S.A.
⁴ 1256 Hammond, Waterloo, IA 50702, U.S.A.

^* Correspondence should be addressed to: james.grier{at}ndsu.edu

The scaphitid ammonite genus Ponteixites Warren, 1934, has remained poorly known and poorly represented in collections up to the present. All previously described specimens of Ponteixites, including the original type specimens, are small and appear to be juveniles. A larger, clearly adult specimen was recently discovered in the Pierre Shale of eastern Montana. If not for the larger size, it would be identified as P. robustus Warren, 1934. A comparison of the new, larger specimen with hundreds of typical, smaller specimens of P. robustus provides evidence for replacing the name Ponteixites with Rhaeboceras Meek, 1876. An alternative interpretation of the large size of the new specimen would be gigantism. However, it is within the size range of other known Rhaeboceras species and has normal scaphite adult characteristics, thus disqualifying it as a candidate for gigantism. The species P. robustus should be renamed R. robustus. Another species, R. coloradoense Cobban, 1987, strongly resembles R. robustus and might be the latter species. The species formerly described as P. gracilis Warren, 1934, is believed either to represent the juvenile stage of another Rhaeboceras species or to be within the range of morphologic variation for R. robustus.

Key Words: ammonite • Cedar Creek • Cobban • gigantism • Montana • Ponteixites • Rhaeboceras • scaphite • suture approximation • synonymy • uncoiling • Pierre Shale