CHAPTER X.

ORDER CAUDATA DUMÉRIL, 1806. COAL MEASURES TO RECENT.

Naked-skinned, elongate, tailed salamanders, mud-puppies, efts, newts,

etc. External gills present or absent in adult condition, but always

present in young. Limbs short, with usually 4 digits on hand and 5 on

foot, but this is subject to much difference. Limbs never very stout.

Carpus and tarsus cartilaginous. Skull roof without the postparietal,

postorbital, and supratemporal. Skull elements never ornamented and

never cut by the lateral-line canals. Vertebræ consisting of a single

element; ribs short, attached to an elongate transverse process.

Caudal ribs seldom present. Parietal foramen lacking. No ventral

armature. Fresh-water inhabitants.

=Suborder PROTEIDA Cope, 1868.=

This order agrees generally with the Caudata, but presents one most

important feature of difference in the presence of the opisthotic. It is

this point which gives the Proteida its intermediate position between

the extinct amphibians and the recent species, and seems to indicate a

connecting line from the Coal Measures down to the present. The structure

of the hyobranchial arches sustains this view.

The hyoid apparatus differs from that of other adult Caudata and resembles

that of their larvæ in having three epibranchials, instead of one only.

The second basibranchial is also connected with the first, which is

not the case with the other Caudata. Three extinct genera are placed

tentatively in this suborder.

=Family COCYTINIDÆ Cope, 1875.=

Cope, Bull. U. S. Nat. Mus., No. 1, p. 12, 1875.

The present family, as here defined, includes the forms whose structure

seems to ally them with the modern salamanders. The character on which

most dependence is placed is that of the branchial apparatus, lacking

in _Hyphasma_. The forms are all incompletely known and the family will

doubtless require revision on acquisition of additional material. Three

genera, each with a single species, are:

_Cocytinus gyrinoides_ Cope. Linton, Ohio, Coal Measures. Based on the

ventral impression of the skull, with the well-developed branchial

apparatus.

_Erierpeton branchialis_ Moodie. Mazon Creek, Illinois, shales. Based

on impression of mandibles and branchial apparatus.

_Hyphasma lævis_ Cope. Linton, Ohio, Coal Measures. Based on

incomplete and obscure amphibian body, lacking limbs.

=Genus COCYTINUS Cope, 1871.=

Cope, Proc. Am. Phil. Soc., 1871, 177.

Cope, Geol. Surv. Ohio, II, pt. II, 360, 1875.

Type: Cocytinus gyrinoides Cope.

Vertebræ and ribs osseous; teeth on the premaxillary bone, none on the

maxillary; hyoid elements largely developed, an axialhyal with basihyal

on each side, closely united with the corresponding ceratohyal, at the

end of which is an element in the position of a stylohyal; hæmal or

basibranchials 3, the anterior 2, each supporting i pleural branchihyal,

and the third supporting one also, the first hæmal branchihyal on the

inner side of the ceratohyal, approaching the median line, and with

elongate pleural element.

The reference by Cope of this genus to the Caudata is one of the most

interesting facts connected with the Paleozoic Amphibia. He says: "The

present genus is, then, to be referred to the neighborhood of _Amphiuma_

and _Protonopsis_, but forming the type of another family" (123). He

regards the branchial apparatus as being more fish-like than that of any

of the modern genera. It is possible that _Cocytinus gyrinoides_ was a

larval branchiate and consequently aquatic form. It should be more fully

compared with _Erierpeton branchialis_ from the Mazon Creek shales when

better known, as well as with _Hyphasma lævis_ from the Linton locality.

All three of these forms are included, provisionally, under the Cocytinidæ.

=Cocytinus gyrinoides Cope.=

Cope, Proc. Am. Phil. Soc., XII, p. 177, 1871.

Cope, Trans. Am. Phil. Soc., p. 278, 1874.

Cope, Geol. Surv. Ohio, II, pt. II, pp. 364-365, pl. xxxix, fig. 4,

1875.

Type: Specimen No. 8613 G, American Museum of Natural History.

Horizon and locality: Linton, Ohio, Coal Measures.

[Illustration: Fig. 16. Obverse of _Cocytinus gyrinoides_ Cope, from

the Coal Measures of Ohio. × 2. _pmx_, premaxillæ: _mx_, maxilla; _m_,

mandible; _ah_, axialhyal; _h_, basal branchihyal; _ch_, ceratohyal; _bv_,

hæmal branchihyal; _b, bII, bIII, bIIII_, pleural branchihyals.]

Two specimens of this interesting amphibian are known, one of them fairly

complete (No. 2564, Am. Mus. Nat. Hist.). The type specimen consists

of the inferior bones of the cranium in a fairly complete state of

preservation, with the muzzle and its teeth; also 8 anterior vertebræ,

with their short recurved ribs.

The condition of the hyal elements in the type specimen is as follows: the

hæmal elements of the first branchial arch are partially concealed on both

sides of the ceratohyal. An expanded truncate face for attachment to the

axial element is visible on both sides, but the body of the bone is flat

and presents the edge of the specimen.

The first pleural element proceeds from just behind the axialhyal; it

is longer than the other pleural elements. A slender bone is visible

extending from the space between the ceratohyal and mandibular angle;

it may, therefore, pertain to the suspensorium of the jaw as well as to

that of the hyiod arch, or be squamosal as well as stylohyal. The second

hæmal bone is slender, but with an enlarged axial extremity; that of the

right side is not so well preserved as to be safely determined. The third

hæmal elements are the smallest, and originate immediately in front of the

occipital condyles and diverge outwards and backwards. They are little

curved, subcylindric, and slightly expanded at the extremities.

Of the pleural elements the first and second are little curved and the

first is marked by a pit or foramen on the under side near the distal end,

which is clearly visible on both sides of the specimen. The third and

fourth pleurals are more curved and the outer ends slightly expanded and

directed backwards.

[Illustration: MOODIE PLATE 6

_Dendrerpeton acadianum_ Owen. Mandibles, parts of anterior

extremities, humerus, etc. Nearly natural size. Erect tree, Coal formation

South Joggins, Nova Scotia. Photograph by Dawson, published through the

courtesy of Dr. Arthur Willey. Original specimen in the British Museum of

Natural History.]

The obverse of the specimen (fig. 16) shows that the anterior axialhyal

is wedge-shaped. The lateral basihyals are massive. The second hæmal

branchihyal is dilated, fan-shaped distally, and supports two pleural

elements. The muzzle projects over the lower jaw and was rather broadly

truncate. The premaxillary teeth are cylindric and 6 in number on each

side. The maxillary bone is represented by a lamina at each lateral

extremity of the premaxillary. The mandibular rami are very stout, as

are also the ceratohyals. The vertebræ have possessed some apophyses,

apparently keel-shaped diapophyses. The ribs are slightly curved.

Measurements of the Type.

mm.

Length of specimen 32

Length of skull 12

Posterior width of skull 11

Length of premaxilla 5

Length of mandible 10

Length of axialhyal 3

Length of postbranchial 4

Width of vertebra 1

Length of vertebra 3

Length of rib 6

The other specimen of this species (fig. 16_a_) is interesting in having

40 consecutive vertebræ preserved, and 19 pairs of ribs attached in their

natural relations to the skull and hyal elements. There are a few hyal

elements preserved, but nothing is added to our previous knowledge. The

ribs are quite as in the type specimen, as are also the vertebræ. The

animal was apparently a slender, eel-shaped amphibian comparing favorably

with the modern _Amphiuma_ in this respect. There are no indications of

limbs or limb girdles.

Fig. 16_a_. Nearly complete specimen of _Cocytinus gyrinoides_ Cope, from

the Coal Measures of Linton, Ohio. Original in the American Museum of

Natural History. × 0.95.

Measurements (No. 2564, American Museum of Natural History).

mm.

Length of entire specimen 113

Length of skull 15

Width of head posterior 15.5

Length of vertebra 2

Length of rib 4

=Genus ERIERPETON Moodie.=

Moodie, Kans. Univ. Sci. Bull., VI, No. 2, p. 328, 1912.

Type: _Erierpeton branchialis_ Moodie.

The generic characters are found, first of all, in the presence of

hyobranchial arches which indicate its relationship to the formerly

described _Cocytinus gyrinoides_ Cope, from Ohio. The only other known

extinct genera of Caudata which possess, or at least have preserved, the

hyobranchial arches are the Jurassic _Hylæobatrachus_ from Belgium and

Lysorophus from the Permian of Texas. The present form is widely distinct

from both of these genera in the shape of the mandible and the form and

arrangement of the hyobranchial bars. The genus _Erierpeton_ finds its

closest ally in _Cocytinus_, in the family Cocytinidæ, which possibly

belongs in the order Caudata and the suborder Proteida of Cope.

=Erierpeton branchialis Moodie.=

Moodie, Kans. Univ. Sci. Bull., VI, No. 2, pp. 329-330, pl. 1, fig. 3;

pl. 2, fig. I, 1912.

Type: Specimen No. 801 (222) 5, Yale University, Museum.

Horizon and locality: Mazon Creek shales, near Morris, Illinois.

The amphibian remains designated by the above name consist of a distinct

mandible and some rather indefinite body impressions (plate 3, fig.

4). Three elongate impressions occur between the rami of the mandibles

(fig. 15, A), which, I suppose, must represent hyoid bones belonging to

the hyobranchial arches. The lateral elements are paired and the median

impression is straight and lies between the paired impressions of the

hyoids. The paired portions probably represent the hypohyals or hypohyals

plus the ceratohyals, and the unpaired portion of the first basibranchial,

according to the nomenclature of Wiedersheim (Comparative Anatomy of

Vertebrates, 1897, p. 86). If the impressions have been correctly

interpreted the present specimen is of very great interest, since it is

the first evidence we have of the hyobranchial arches in the Amphibia

of Mazon Creek, and the second in the Carboniferous of North America.

Dawson doubtfully identified (216) some elements of the Joggins Amphibia

as hyoids, but was uncertain as to their position. Cope described fully

the well-developed hyobranchial apparatus of _Cocytinus gyrinoides_ (123)

from the Coal Measures of Ohio. Among other Paleozoic Amphibia Williston

(614) has described branchial arches in the peculiar form _Lysorophus

tricarinatus_ Cope, from the Permian of Texas.

The form of the impression of the mandible in the present specimen is

unlike anything known to the writer among other Carboniferous or later

Amphibia. The rami are long, slender, deep, slightly curved, and pointed

anteriorly. The anterior symphysis was not a complete sutural union, but

was occupied partly by cartilage or other connective tissue.

There are no definite traces of the appendicular skeleton. The traces of

the body (fig. 15, A) indicate an elongated, rather slender animal, but

further than this nothing can be said in regard to its structure.

The occurrence of a typically caudate form in the Carboniferous is

unusual and complicates still further our understanding of the origin and

relationships of the early Amphibia.

Measurements of the Type.

mm.

Length of entire impression 50

Length of mandible along median line 10

Width of mandibular ramus 9

Length of basibranchial 2.5

Width of basibranchial 0.75

Length of hypohyal 2.4

Width of hypohyal 1.5

=Genus HYPHASMA Cope, 1875.=

Cope, Proc. Acad. Sci. Phil., p. 16, 1875.

Cope, Geol. Surv. Ohio, II, pt. II, p. 387, 1875.

Type: _Hyphasma lævis_ Cope.

"Vertebræ osseous, the posterior dorsals, and probably the caudals,

furnished with fan-like neural spines; limbs unknown--(?) wanting.

Thoracic shields present. Ventral armature, consisting of rhomboidal

scuta, forming packed rows arranged in chevrons, directed backwards, on

top of which are the usual rod-like scales arranged in packed chevrons,

with the angle directed forward.

"The general appearance of the type of this genus is that of a Ptyonius,

but the ventral armature is different from anything observed in the known

genera of this group. The larger external scuta are like those of the

species of Colosteus (Sauropleura), but their series have a different

direction. The inner chevrons are those of many other genera" (123).

=Hyphasma lævis Cope.=

Cope, Proc. Acad. Sci. Phil., p. 16, 1875.

Cope, Geol. Surv. Ohio., 11, pt. II, p. 387, pl. 37, fig. 4, 1875.

Type: Specimen No. 9023 (in counterpart), American Museum of Natural

History.

Horizon and locality: Linton, Ohio, Coal Measures.

"In the only known specimen the vertebræ have low and squarely

truncate neural spines near the head, and some distance anterior to

the tail they are quite conspicuous and delicately line-grooved.

The body is slender and probably limbless. The thoracic scuta are

large and close to the head; the median is produced at both ends,

but chiefly anteriorly while the lateral are narrow; all are without

sculpture The head is seen from below. The mandibular rami are not so

slender as in most species of _Ptyonius_, but are rather stout. They

are a little incurved distally, so that the form of the muzzle is

somewhat narrowed, but not produced. The teeth are not visible. Ten

rows of the outer layer of scuta in 0.005 m." (123).

The specimen is very indistinctly preserved and the characters given

by Cope can not all be made out. It is puzzling to see just on what

he bases his conclusion. It is possible that the specimen is a poorly

preserved _Ptyonius_. The outlines of the vertebræ are so indistinct that

I am uncertain about them. In certain lights there appear to be regular

impressions which resemble the spines of the vertebræ of Ptyonius, but

they are doubtful. The skull appears totally distinct from any known

species of _Ptyonius_, but it is very imperfect. The condition of the

pectoral elements is very uncertain and I can not be sure that what Cope

described as thoracic "scuta" are such. The interclavicle, however, is

clearly preserved as a diamond-shaped structure. It is almost smooth, with

a few faint radiating lines near the base. It measures 5 mm. in greatest

breadth by 8 mm. in length.

Measurements of the Type.

mm.

Length of specimen as preserved 64

Length of skull 15

Greatest width of skull 8

Width of body 8

Length of 7 cervical vertebræ 15

Length of median thoracic scuta 10

Width of same 4

Width of clavicle 2

Length of mandibular ramus 12

The Coal Measures Amphibia of North America · 第 4 / 19 章