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
The canals have been described in all known orders of fossil Amphibia
and the system is found likewise in all the living orders, including the
Gymnophiona, which have "a strong line of lateral sense-organs" (Gadow).
In the Branchiosauria, the earliest of the true Amphibia (Euamphibia)
and ancestral to the modern Caudata, the lateral-line system is known
on the tails of two genera (462, 478) from the Mazon Creek, Illinois,
shales--_Micrerpeton_ and _Eumicrerpeton_. The system as there defined
has been fully discussed in the description of the anatomical details of
the species, to which reference may be made for further data (pp. 52-60).
Suffice it to say here that the system of sense-organs there preserved
is identical with that of the larval _Necturus_; the lines arising as a
_median_ from the tip of the tail and a _dorsal_ springing from the median
at a distance of a few millimeters from the tip of the tail. The lines are
more evident on account of the fact that the lateral-line sense-organs
were located under specialized pigmented scales. The significance of the
close similarity between the arrangement of the lateral-line systems on
the tail of Necturus, _Micrerpeton_, and _Eumicrerpeton_ is doubtless of
genetic (459) importance, indicating the origin of the caudate Amphibia
from the Branchiosauria by a degenerative or recessive evolution in other
structural characters. This system of sense-organs has been described in
no other branchiosaurian.
The Microsauria (458) are exceedingly interesting in possessing a very
peculiar type of lateral-line system. It is known in a few forms and in
one specimen especially well (_Erpetosaurus tabulatus_) (fig. 22, G). In
this species, which is represented by a single imperfect skull, there are
evidences of a nearly complete lateral-line system of canals and pits.
The occipital cross-commissure is represented on the posterior border
of the skull by a row of elongate pits such as Andrews described for
_Ceraterpeton_ (8). I fail to find in American species the pores described
by Andrews. The temporal canal forms with the jugal canal a complete ring,
much as it is in _Trematosaurus_, only in _Erpetosaurus tabulatus_ the
temporal canal does not touch the tabulare. I think there are indications
of a connection of the temporal canal with the supraorbital. The temporal
canal cuts the supratemporal, the squamosal, and jugal. The jugal canal
lies for the most part on the supratemporal and quadratojugal, and joins
the infraorbital on the jugal. A portion only of the infraorbital canal
is preserved. There is also a portion of the supraorbital canal. It seems
not to be connected with the temporal canal, although there is a possible
indication of this connection. The supraorbital crosses the frontal,
prefrontal, and a part of the nasal. The squamosal element is peculiar
in _Erpetosaurus tabulatus_ in that it is excluded from the parietal by
the extension of the tabulare and postorbital. This condition is found in
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