Chapter M
Fore-and-aft diameter of crown ·010
Transverse diameter of crown ·007
Vertical height of crown
Crocodilus clavis, Cope.
U. S. Geol. Survey of Terrs. 1872, p. 612.
This species is indicated by the remains of a crocodilian larger than _Crocodilus Elliotii_, but very different from it. The pitting of the dermal scutes, and of all the cranial bones, is deeper than in any other of the Bridger crocodilians in our possession, and very strongly resembles that in _Alligator mississippiensis_.
The _mandible_ has a long symphysis, and the alveolar border shows the sudden deep depression just behind it, which is so marked in the ordinary alligator. The rami, however, do not diverge at such an open angle. The jaw is very stout, and is deeper and thinner than in _Crocodilus Elliotii_; and is of about the same proportionate thickness, but deeper than in the alligator. The splenial ends obtusely, and approaches the symphysis somewhat more closely than in the alligator, but does not enter into its formation. The teeth are stout and obtusely conical, not striate, and implanted very close together; they exhibit about the same alternation of size as do those of the alligator. What appears to be the canine is small; it is preceded by a much smaller, and succeeded by a slightly smaller tooth. The dermal scutes are quadrate in shape; they are deeply and irregularly pitted, and have a low but distinct longitudinal keel; they are suturally united by their lateral borders.
CHELONIA.
The Bridger beds have yielded a great abundance and variety of land, marsh, and fresh-water chelonians. They present much variation of form and size; and, owing to the great pressure in the strata, scarcely any two specimens of the same species are alike; occasionally, however, an undistorted specimen is obtained.
The most abundant remains of turtles are those of a species of the recent genus _Emys_, which are found in all the beds, and are, perhaps, the commonest fossils of the basin. The genera _Trionyx_ and _Hadrianus_ (_Testudo_, Leidy) follow next in order.
HADRIANUS, Cope.
Resembles _Testudo_ in form, but has two analscuta, as have most _Emydidæ_.
Hadrianus allabiatus, Cope.
U. S. Geol. Survey of Territories, 1872, p. 630.
Represented by two ungual phalanges which resemble the claws of _Testudo_, but are proportionately shorter, broader, and not so pointed at the ends. They are oval in section, both longitudinally and transversely; the articular faces are deep and subinferior.
From Henry's Fork.
Hadrianus octonarius, Cope.
Geol. Survey of Terrs., 1872. p 630.
Represented by the right humerus of a large individual.
This bone is intermediate in character between the corresponding bones of _Testudo_ and _Emys_. The head is longer and narrower than in the former genus; it is implanted on a short, distinct neck, and is strongly convex in both directions. The articular surface extends to the base of the internal tuberosity. The tuberosities, especially the external one, are very large and thick. The external rises above the head, and resembles that of _Emys_ in shape. The fossa separating the tuberosities is comparatively narrow. The shaft is much like that of _Emys_, but is somewhat more strongly curved; not so much, however, as in _Testudo_, and the distal end is not so much flattened. The anconeal fossa is wider and deeper than in either genus. The trochlea is broad, and divided by an obscure groove into a small and convex radial face, and a nearly plane (transversely) ulnar face. The condyles are prominent and rugose.
Found near Dry Creek.
EMYS.
Emys wyomingensis, Leidy.
Cont. to Ex. Vert. Fauna, p. 140.
Represented by six perfect shells from Cottonwood and Dry Creeks, and Henry's Fork, and a shoulder girdle from Cottonwood Creek, which is provisionally referred to this species.
This species, when adult, was upward of a foot in length, and in the composition of the shell, number of scutes, etc., resembled the living species of the genus.
_The Shoulder Girdle_ has the form characteristic of the _Emydidæ_, but presents some peculiarities. The scapula is short, not being as long as the coracoid, and is not so straight or cylindrical as is usual in _Emys_; but is compressed, and somewhat recurved, and tapers towards the upper extremity, which is marked by a smooth rounded facet for the cartilaginous supra-scapula. The precoracoid is long, sub-cylindrical at its origin, but becomes broad and flat distally; at the extremity it is longitudinally striated. The proximal end is flexed forward at an obtuse angle, and is expanded to form the long suture with the scapula and coracoid. It contributes considerably to the glenoid cavity. The coracoid is remarkably long, and after leaving the sutures with the other elements of the girdle, becomes very broad and thin. This is most marked distally. The anterior border is thickened, and the bone is slightly concave on both surfaces.
The three parts of the shoulder girdle are united by distinct bony symphyses; they differ from some of the modern species, in which there is only a ligamentous union between the coracoid and the other parts. It presents a further difference in the long and slender neck which is formed by the flexing of the precoracoid, and in the shallow and subcircular glenoid cavity. The short scapula and long coracoid would indicate a species with a low, broad carapace, as was probably the case in _E. wyomingensis_, though much difficulty has been experienced in determining this point, owing to the distortion of the specimens.
_Measurements._
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Palæontological Report of the Princeton Scientific Expedition of 1877Chapter M
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