Squatinactis caudispinatus Lund and Zangerl, 1974
publication ID |
https://doi.org/ 10.4202/app.00084.2014 |
persistent identifier |
https://treatment.plazi.org/id/251B879F-FFC5-FFB4-FCF0-354608F1F817 |
treatment provided by |
Felipe |
scientific name |
Squatinactis caudispinatus Lund and Zangerl, 1974 |
status |
|
Squatinactis caudispinatus Lund and Zangerl, 1974
Figs. 7G View Fig , 8D View Fig .
Material.—Four teeth from upper Viséan of Cawdor Quarry, Matlock, Derbyshire, England, UK (samples Cawdor 5 and 11); NHMUK PV P73282, NHMUK PV P73286.
Description and remarks.—A few small cladodont teeth (less than 0.5 mm across the base) from Cawdor Quarry are tentatively attributed to S. caudispinatus because of the short base (labio-lingually) provided with two separate, oval orolingual buttons and two basolabial projections, separated by a deep basolabial depression. Some of the teeth are wide (mesio- -distally) and have multicuspid crowns (up to four lateral cusps; Fig. 8B View Fig ), covered on both sides with sub-parallel cristae, and the other have narrower bases ( Fig. 7G View Fig ), fewer cusps and apparently less well developed ornamentation. Similar differences were observed in the material of S. caudispinatus from the Tournaisian of Illinois, USA (Ginter et al. 2010: fig. 73A–F).
Stratigraphic and geographic range.—Articulated specimens from Serpukhovian of Bear Gulch, Montana, USA ( Lund and Zangerl 1974; Lund 1988), Tournaisian of Illinois, USA (Ginter et al. 2010) and South Urals, Russia (Ivanov 1996), upper Viséan of Derbyshire, England (this paper).
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.