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
mm.
Length of animal, as preserved 18
Length of skull 6.5
Posterior width of skull 5.5
Length of side of skull 6.5
Diameter of orbit 65
Interorbital width 2
Length of tooth 0.25
Length of vertebra 1.45
Width of vertebra 35
Length of humerus 2.25
Distal width of humerus 35
CHAPTER XV.
THE MICROSAURIAN FAMILY STEGOPIDÆ, FROM THE COAL MEASURES OF OHIO.
=Family STEGOPIDÆ Moodie, 1909.=
Moodie, Jour. Geol., XVII, No. 1, 79, 1909.
The chief family characters are the large lacrimal, unknown in other
species of Coal Measures Amphibia, the central position of the orbits, the
general form of the skull, and the peculiar, short, divaricate horns from
the squamosal. If an intertemporal element is present in the skull, which
is suggested as a possibility, the family is further distinct. The type
species is Stegops divaricata Cope from the Linton, Ohio, Coal Measures.
The group seems to be distinct and has no immediate allies, being confined
to the American Coal Measures.
=Genus STEGOPS Moodie, 1909.=
Moodie, Jour. Geol., XVII, 79, 1909.
Type: _Stegops divaricata_ Cope.
This genus has been erected for the reception of the peculiar form
described by Cope as _Ceraterpeton divaricatum_, but there are good
reasons why the form can not be retained in the genus. The position of
the orbits in Stegops (plate 25, fig. 3) is different from _Ceraterpeton_
and the muzzle is rounded, not truncate as in the latter form. The horns
are of a different type and there is no indication of the tabulare
protuberance which is present in _Ceraterpeton_. The sculpturing of the
cranial elements is also distinctive in the present form, consisting of
radiating grooves and ridges; the cranium of _Ceraterpeton_ appears to be
but slightly sculptured. There is no lateral projection from the border of
the skull in Stegops, as there is in the other genus. The structure of the
skull of _Ceraterpeton_ is practically unknown, except in a very general
way, although Andrews (8) was able to make out some of the elements and to
trace the lateral-line canals. A structural comparison is thus impossible,
but on the basis of form alone there are good generic distinctions. The
present genus is apparently distinct from other genera in the presence
of an intertemporal, but additional material will be required before
a satisfactory determination is possible. The genus _Diceratosaurus_
of Jaekel (347) is distinct in the arrangement of the elements of the
cranium, the general form of the skull, and in the two known species of
_Diceratosaurus_ the orbits are located well anteriorly, but in Stegops
they are in the median transverse line of the cranium. The genus _Stegops_
is distinct from _Eoserpeton_ in the smaller size of the prosquamosal,
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