Stereocephalus tutus, Lambe, 1902

Lambe L. M., 1902, New genera and species from the Belly River Series (mid-Cretaceous), Geological Survey of Canada Contributions to Canadian Palaeontology 3, pp. 25-81 : 55-57

publication ID

https://doi.org/10.5281/zenodo.3233762

DOI

https://doi.org/10.5281/zenodo.4583897

persistent identifier

https://treatment.plazi.org/id/03BAEA64-B52E-4055-70E0-FD09FA33D990

treatment provided by

Jeremy

scientific name

Stereocephalus tutus
status

 

Stereocephalus tutus . Sp. nov.

Plate XI View PLATE XI , plate XII, figs. 1, 2, 3, 4 and 5 View PLATE XII , and plate XXI, figs. 6, 7 and 8 View PLATE XXI View PLATE XXI .

The speeimen of Which views from above, from the side and from below are given on plates XI and XII, represents part of the plate-protected cranium of a herbivorous dinosaur, that is, apparently, quite distinct from any hitherto described.

With the head was found a transverse series of coössified sharply keeled scutes which will be described farther on.

The part of the head preserved is strongly convex transversely, but only moderately so from front to back. Goôssified plates cover the whole of the upper surface and are continued down on the vertical sides. They are arranged with a certain amount of bilateral symmetry, are quite small at the centre and toward the back, but are larger in front and very much more so on the sides. They are for the most part irregularly five or six sided, with rather undulatory surfaces that are marked by an irregular, raised, structural cross-hatching, feebly suggestive of the surface markings of the plates of Nodosaurus textilis, Marsh. Small vascular openings and grooves are also numerous on the surface. The edges of the plates are as a rule angular and sometimes raised. Each plate has its limit defined by a deep circumscribing furrow, so that although they are coôssified and form a continuous surface covering to the head, they do not lose their individuality. A rounded node, or an incipient keel is noticed on some of the plates.

The removal of sandstone from the lower surface of the specimen revealed the bones of the palatal region ( plate XII View PLATE XII . fig. 2). The interpretation of these elements are as indicated by the letters. The back ends, only, of the palatines (P) are seen, meeting the pterygoids in a suture indicated at “ s. From here the latter bones (pt.) extend backward on either side of interpterygoid vacuities (v.). The ridge (pb.) represents the presphenoid and basisphenoid elements; it is bent posteriorly to one side in the specimen, which has been subjected to considerable pressure from above and is somewhat crushed behind.

From this intel'pretation of the bones of the palate it would appear that the part of the armature preserved covers the upper part of the head near the union of the nasals With the frontals. No indication of the 01'bits can be detected and it is probable that they were placed far forward in the head.

Ãfeasurevnents.
    M.
Antero-posterior diameter of speeimen.   ‘ 250
Greatest transverse diameter.   ' 210
Height of centre of upper surface above the level.   1225
\Vidth of interpterygoid vacuities K' about. ‘ 040
Maximum thickness of cranial armature. . about about ' 016
fllezısurenıents of transverse series of scutes.  
  M
Height of apex of median keel above the level. 190
Height of centre of inner surface of arch above the level. 125
Width of inner spread of arch below ' 236
Average height of apices of keels above inner surface of arcli ' 072
Basal breadth of the seutes (Nos. 2 and 4) on either sidc of the median one. ' 075
'Basal length of same. 143
Thickness of bone on which the scutes rest, about. ' 010

Belly River series, Red Deer river, 1897.

The tooth shown in fig. 12, is of the Stegosaurían type. It differs from those, of the Red Deer river district, referred to the two species of Palœoscincus, and is about twice as large as those of P. costatus. 1 t is figured here with the idea that it may eventually prove to belong to S. tutus. It was collected below Berry creek, on Red Deer river, in 1901.

A spinous dermal plate of massive proportions, fig. 13, A and B, is referred to this species on account of its similarity, in structure and surface markings, to the postcranial keeled scutes described above. This specimen was collected in 1897. Another large plate similar in general proportions to the above and nearly as large, as Well as numerous others of different sizes and of a variety of shapes, were collected in 1901.

Kingdom

Animalia

Phylum

Chordata

Class

Reptilia

Order

Dinosauria

Family

Stegosauridae

Genus

Stereocephalus

Loc

Stereocephalus tutus

Lambe L. M. 1902
1902
Loc

S. tutus

Lambe 1902
1902
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