The Coal Measures Amphibia of North AmericaMoodie, Roy Lee
Science
The Coal Measures Amphibia of North America
Moodie, Roy Lee
Amphibians, Fossil -- North America; Paleontology -- Carboniferous; Paleontology -- North America
Our knowledge of the genus is confined to the skull. The genus was
established for certain members of the genus Tuditanus and other forms
which have been recently described. The species of the genus are: _E.
radiatus_ Cope type, _E. tabulatus_ Cope, _E. tuberculatus_ Moodie,
_E. obtusus_ Cope, _E. minutus_ Moodie, _E. acutirostris_ Moodie, _E.
sculptilis_ Moodie. All of the species are from the Linton, Ohio, Coal
Measures, with the exception of _E. sculptilis_ and _E. minutus_, which
are from the Cannelton, Pennsylvania, slates.
The position of the genus as to family is a little uncertain, since family
characters are not yet well understood among the Carboniferous forms on
account of the lack of information as to the structure of the animals. If
we take the absence of the ventral scutellæ as a family character, the
genus will be in the family Tuditanidæ, but the evidence on this point is
negative. For the present we may place the genus only provisionally in the
family Tuditanidæ. The arrangement will undoubtedly require revision later.
=Erpetosaurus radiatus Cope, 1874.=
Cope, Trans. Amer. Phil. Soc., XV, p. 273, 1874.
Cope, Geol. Surv. Ohio, II, pt. II, pp. 394-395, pl. xxvii, fig. 1;
pl. xxxiv, fig. 3; text-fig. 10, 1875.
Moodie, Bull. Amer. Mus. Nat. Hist., XXVI, p. 348, pl. lxii, fig. 1,
1909.
Type: Specimen No. 8600 G, American Museum of Natural History. Locality
and horizon: Linton, Ohio, Coal Measures. (Plate 25, fig. 1.) Cope
originally described this species from a portion of a skull. He (123)
characterized the form as follows:
"The marked character of this form is seen in the very anterior
position of the orbits and the contraction of the muzzle. The orbits
are large and are separated by a little more than their own diameter;
their posterior border is in front of a line measuring the anterior
third of the length to the supraoccipital crest, and nearly to the
line marking the fourth of the length to the quadrate region. The
posterior outline of the skull is deeply concave, the quadrate angle
projecting beyond the occipital condyles."
The base of the specimen is broken and there is no place for the occipital
condyles. Unless the specimen has been mutilated since Cope studied it,
the occipital condyles are not present.
The restoration of the skull given in figure 22, B varies but little from
that given by Cope in 1875. The elements are practically as he represented
them.
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