Callistomordax kugleri, Schoch, 2008

Schoch, Rainer R., 2008, A new stereospondyl from the German Middle Triassic, and the origin of the Metoposauridae, Zoological Journal of the Linnean Society 152 (1), pp. 79-113 : 80-84

publication ID

https://doi.org/ 10.1111/j.1096-3642.2007.00363.x

DOI

https://doi.org/10.5281/zenodo.10546283

persistent identifier

https://treatment.plazi.org/id/03DF87F4-FFAF-FFC5-4BB1-F9910FEDF891

treatment provided by

Felipe

scientific name

Callistomordax kugleri
status

sp. nov.

CALLISTOMORDAX KUGLERI SP. NOV.

1985 ‘Metoposaurier-Vorfahr’ Kugler & Bartholomä (1985: 16).

1988 ‘oldest undoubted Morales (1988: 23 a). metoposaurid’

1993 ‘probably a latiscopid’ Hunt (1993: 90).

1998 Almasauridae gen. nov. Schoch & Werneburg sp. nov. (1998: 637).

2000 Almasauridae gen. nov. Schoch & Milner (2000: sp. nov. 120, fig. 85).

Holotype: SMNS 82035 View Materials , a nearly complete skeleton. The skull, exposed in dorsal view, has a length of 137 mm (from tip of premaxilla to back rim of postparietal), and the length of the preserved skeleton is 1. 23 m.

Type horizon: Top of Untere Graue Mergel (Bed 6 of Schoch, 2002a), Lower Keuper (Erfurt Formation), Longobardian (Upper Ladinian), Middle Triassic.

Type locality: Vellberg (Schumann quarry), northern Baden-Württemberg, southern Germany.

Referred material: From type locality: SMNS 90516 View Materials , anterior two-thirds of skeleton with complete skull in dorsal view (153 mm); SMNS 55385 View Materials , isolated, complete skull (148 mm; Figs 2A View Figure 2 , 5 View Figure 5 ); SMNS 90519 View Materials , isolated left humerus ( Fig. 7 D–F View Figure 7 ); SMNS 90520 View Materials , parts of skeleton including well-preserved pectoral and pelvic girdle ( Fig. 7A, B, H, I View Figure 7 ) and crushed skull (145 mm); SMNS 90700 View Materials , articulated skeleton lacking posterior half of tail, but including well-preserved girdles, appendages, and skull (125 mm) in ventral view ( Fig. 7C View Figure 7 ); MHI-K1, a nearly complete postcranial skeleton including one humerus and both hind limbs; MHI-K2, fairly complete, small postcranial skeleton with pectoral girdle; MHI-K3, disarticulated large postcranial skeleton with scapulocoracoid ( Fig. 7G View Figure 7 ), interclavicle, humerus, radius, and ilium; MHI-K4, small skull (95 mm); MHI-K5, slightly disarticulated skull with good snout region (160 mm). From Ummenhofen quarry: SMNS 90506 View Materials , posterior part of trunk, pelvic elements, and hind limb ( Fig. 9 View Figure 9 ). From Kupferzell locality: SMNS 81713 View Materials , isolated articular; SMNS 84115–84118 View Materials , 90521 View Materials , isolated intercentra ( Fig. 8C–L View Figure 8 ); SMNS 84119 View Materials , atlas ( Fig. 8A, B View Figure 8 ) .

Stratigraphic range: Albertibank through Untere Graue Mergel, Lower Keuper (Erfurt Formation), Langobardian, Middle Triassic.

Etymology: In honour of Werner Kugler, private collector of Crailsheim, who found and prepared the first specimen. His general contributions to our understanding of Lower Keuper vertebrates have been outstanding.

Diagnosis: Autapomorphic character states are as follows: (1) frontals co-ossified, with single medial anterior tip and blunt posterior end ( Figs 1A View Figure 1 , 4B View Figure 4 ); (2) pterygoid distinct by very broad and flat quadrate ramus combined with a particularly slender and narrow palatine ramus ( Figs 1B View Figure 1 , 5 View Figure 5 ); (3) subtemporal windows nearly round and wider than the basicranial region ( Fig. 1B View Figure 1 ); (4) anterior palate very short, with vomers and palatines dominated by huge fangs the sockets of which occupy most of the bone surfaces, and minute, obliquely orientated choanae ( Figs 1B View Figure 1 , 5 View Figure 5 ); (5) palatal and symphyseal fangs laterally compressed and keeled; (6) intercentra forming open crescents with high flanks (except when fused to pleurocentra, then giving a disc-shaped compound bone, see Fig. 8C, D View Figure 8 ) with pointed upper ends and a massive, anteroposteriorly elongated ventral portion that has a quadrangular outline ( Fig. 8C–J View Figure 8 ); (7) shaft of cleithrum curved in semilunar fashion ( Fig. 7H, I View Figure 7 ).

Derived characters shared with other taxa:

1. Callistomordax and the Metoposauridae : clavicle extending well posteriorly on interclavicle, with the radial arrangement of the ornament pointing posteromedially.

2. Callistomordax , Rileymillerus , and the Metoposauridae : lacrimal forms small element confined to the anterolateral margin of the orbit [ Bolt & Chatterjee, 2000 regarded this as a lateral exposure of the palatine (LEP), in analogy with dissorophoids].

3. Callistomordax and Almasaurus : cultriform process forms a prominent ventral keel, which rises from a ridge on the anterior portion of the basal plate, and terminates shortly posterior to the point where the parasphenoid is framed by posteromedial processes of the vomers; snout narrow, with the nares in the terminal position and located in close proximity.

Trigonosternum latum: Schmidt (1931) described and named a partial interclavicle from the Lower Keuper of Kölleda in Thuringia ( Germany) as a new genus and species, T. latum , which he referred to the Metoposauridae . Colbert & Imbrie (1956) have argued that the assignment of this fragment to metoposaurids is based on a misinterpretation caused by a wrong orientation of the interclavicle, which is followed here. The type and only specimen is not only indeterminate, but differs from the interclavicle of C. kugleri in ornamentation and overall shape ( Werneburg, 1990; Schoch & Milner, 2000).

Kingdom

Animalia

Phylum

Chordata

Class

Amphibia

Order

Temnospondyli

Family

Trematosauria

Genus

Callistomordax

Loc

Callistomordax kugleri

Schoch, Rainer R. 2008
2008
Loc

C. kugleri

Schoch 2008
2008
Loc

Trigonosternum latum

: Schmidt 1931
1931
Loc

T. latum

: Schmidt 1931
1931
Loc

Metoposauridae

Watson 1919
1919
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