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 amphibian nature of the species having thus been established,
it remains to give a detailed account of its skeletal anatomy, with
comparative references to such other ancient forms as are available.
Little can be said of the vertebral column, since only the molds of a few
vertebræ remain, and these are so obscured by a closely adherent pellicle
of carbonaceous material that their form can not be distinctly discerned.
They are high, with relatively broad neural spines. There are no ribs
preserved. The pelvis is obscured, but it is possible to determine the
presence of an elongate ilium and an ischium. The leg of the left side
is the best preserved of all the elements, and it is to this that our
attention will be confined. The opposite leg is not so complete, yet all
the long bones and a part of the tarsus are preserved with sufficient
clearness to corroborate the findings of the left side.
The femur, as has been stated, is reptilian in appearance. This is due
to the well-rounded articular surfaces, as though the endochondrium were
well developed, and to the large development of the greater and lesser
trochanters, which are quite prominent, though these are distorted and
depressed in fossilization. The bone is stout and well built and its form
suggests an active habit of life. The tibia and fibula are separate, and
do not otherwise have sufficiently noteworthy characters to call for a
special description in this place, except to note an unusual anterior
crest on the tibia. To the lower ends of these bones articulate the first
row of tarsal elements, the tibiale, intermedium, and fibulare. The tarsus
is composed of 9 elements arranged in 3 rows. The proximal row is composed
of the tibiale, the intermedium, and the fibulare. On the edge of the
tibiale there lies a portion of one of the caudal vertebræ, so that the
form of this tarsal element is slightly obscured. The intermedium is a
small, rounded element lying between the larger elements. The fibulare is
rectangular and projects a considerable distance out from the tibia, but
articulates directly with the large lateral distal tarsal. The centrale
is triangular in form and is opposed directly by the tibiale and tarsalia
1 to 3. The phalanges are robust in appearance. The entire foot gives
one the impression of a very broad structure. The ungual phalanges were
apparently bluntly clawed.
CHAPTER XXIII.
SUPPOSED MICROSAURIAN SPECIES OF UNCERTAIN RELATIONSHIP.
The following three species are so unusual and so incompletely known that
they can not be considered with any of the above families: _Brachydectes
newberryi_ Cope, Linton, Ohio; _Amblyodon problematicum_ Dawson, Nova
Scotia; _Proterpeton gurleyi_ Moodie, Danville, Illinois.
=Genus BRACHYDECTES Cope, 1868.=
Cope, Proc. Phila. Acad. Nat. Sci., 1868, p. 214.
Cope, Trans. Am. Phil. Soc., 1868, p. 14.
Cope, Geol. Surv. Ohio, II, pt. II, p. 388, 1875, pl. xxvii, fig. 2.
Type: _Brachydectes newberryi_ Cope.
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