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152


Journal of Paleontology 91(1):146–161


these divided ridges as taxonomic characters, based on obser- vations of variable twinning of the last ridge crest in the living Australian lungfish (Neoceratodus forsteri). Our survey of post- Triassic ceratodontids of North America suggests that this condition is often absent, or at least extremely rare, in most species. Here, we follow Milner and Kirkland (2006) and attribute taxonomic significance to this feature.


Ceratodus molossus new species Figure 2.2–2.7, Supplemental Data 3–5, Table 1


Holotype.—NCSM 30252, a robust, complete right pterygo- palatine plate with a partial pterygopalatine attached; Late Cretaceous, Mussentuchit Member, Cedar Mountain Forma- tion; 31km south of Emery, Emery County, Utah, U.S.A.


Diagnosis.—A ceratodontid bearing four primary ridge crests on the pterygopalatine plate, with the last being twinned slightly into an exposed ‘chin’ on the posterolabial corner; mesial mar- gin strongly linear. Both pterygopalatine and prearticular plates have a highly obtuse inner angle (ABC exceeding 130°) in combination with a strongly acute C1Cp angle (69–76°) and nearly planar occlusal surfaces, with negligible development of crests. The prearticular plate is characterized by rounded lingual and posterior margins, and a thick but short C1 ridge crest.


Occurrence.—Upper Cretaceous (Cenomanian), Cedar Moun- tain and Naturita formations, Utah, U.S.A. The referred pre- articular specimen (MNA.V.10649) is fromMNAlocality 1067, 2.4km northwest of Cannonville, Garfield County, Utah, U.S. A. The referred pterygopalatine plate (UMNH 16774) is also from the Naturita Formation, near Escalante, Garfield County, Utah, U.S.A.


Description.—The holotype specimen (NCSM 30252) is a large, right pterygopalatine plate with a complete occlusal surface. An additional specimen, very similar to the holotype, is also described here. UMNH 16774 is a large, right pter- ygopalatine plate, complete except for the tip of C1. Both known pterygopalatine plates (Fig. 2.2–2.5) strongly resemble the pterygopalatine plate of Ceratodus robustus (Knight, 1898, fig. 1), particularly in its large size, extreme flattening of the occlusal surface, shallow and rounded notches between ridges (greatest separation is between C1-C2), and squared posterior margin (Kirkland, 1987, pl. 1N; 1998, fig. 3I). These plates differs from C. robustus in having a twinnedCp ridge crest; also, ridge crests are thinner, withC3 andCp ridge crests slightly more distinct (the latter


noticeably shorter than in C. robustus). In addition, the elongate, finger-like C1 ridge crest of the holotype specimen is not observed in C. robustus. The large projection seenonthe mesiolingual border (junction of inner angle) of C. robustus is also present in NCSM 30252 and UMNH 16774, but is broader and does not project as far lingually. The prearticular plate referred to Ceratodus molossus


(MNA.V.10649, Fig. 2.6, 2.7) is complete; one complete and several partial prearticular plates of C. robustus are available for comparison (Kirkland, 1987, plate 1P–T; 1998, fig. 3H, J). MNA.V.10649 is slightly smaller than would be expected for the individual represented by the holotype, NCSM 30252, but it


is morphologically appropriate and would occlude well with the holotype, were it not for minor deformation of the prearticular tooth plate surface (see below). As with the upper plates, the prearticular tooth plate of C. molossus is similar to that of C. robustus, particularly in its massive construction, negligible expression of ridge crests on the occlusal surface, and the shallowness of the notches between ridges. MNA.V.10649 bears four ridges, of which C1 and C2 are widely spaced; the distance between C2-C3 is slightly greater than between C3-Cp, whereas C2-C4 tend to be more closely spaced, with more angulate intervening notches, in C. robustus. In both, the mesial margin differs from other North American species of Ceratodus in being rounded. In C. molossus, this rounded mesial margin is continuous with similarly curved lingual and posterior margins, giving the plate a semilunate shape. The lingual and posterior margins are straighter in C. robustus. TATE 3000 (Kirkland, 1998, fig. 3J), the only complete prearticular plate known for C. robustus, is proportionately more labiolingually expanded (especially on the mesial end, where C1 is particularly broad) than MNA.V.10649, but other specimens of C. robustus suggest variability in proportions of the prearticular plate. Intriguingly, the occlusal surface of MNA.V.10649 is


somewhat bowed, with the central portion being concave; a distinct trough (~4mm wide and 2–3mm deep) runs labiolin- gually across the center. These are readily identified as pathologies, of which a number are known for fossil and living lungfishes; the condition in MNA.V.10649 is closely matched in a specimen of Triassic Ceratodus kaupi (Kemp, 2001, fig. 6B; see also Kemp, 2003).


Etymology.—From molossus (Latin form of Greek Μολοσσfo), after the extinct breed of Greco-Roman fighting dog (De Prisco and Johnson, 1990), named in reference to Bulldog Bench near Cannonville, Utah, U.S.A., where the prearticular specimen (and other lungfish material) was found. The name is also an allusion to the presumed large and powerful feeding apparatus of the species, reminiscent of that of a bulldog or mastiff.


Materials.—Three nearly complete tooth plates, including the holotype: NCSM 30252 (holotype), a right pterygopalatine plate; UMNH 16774, a right pterygopalatine plate; and MNA. V.10649, a right prearticular plate.


Remarks.—With the addition of C. molossus, the already diverse ichthyofauna of the Naturita Formation (see Brinkman et al., 2013) now includes two species of Ceratodus. Ceratodus gustasoni Kirkland, 1987, like C. molossus, has flat, low-crested tooth plates; though represented by a number of specimens, only the lower (prearticular) tooth plate is known. It can be readily distinguished from that of C. molossus in that it is proportio- nately narrower labiolingually, with C1 being elongate and narrow, the crushing surface at the origin of ridge crests more mound-like, the lingual margin straight, and the C2-Cp ridge crests sharply pointed. Ceratodus molossus provides a striking point of contrast with the other recognized Cenomanian species, C. carteri Main, Parris, Grandstaff, and Carter, 2014, from the Woodbine Formation of Texas, which has small, sharply crested tooth plates.


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