The Cambridge natural history, Vol. 08 (of 10)Gadow, Hans
Science
The Cambridge natural history, Vol. 08 (of 10)
Gadow, Hans
Animals
The orbital region of the primitive cranium remains cartilaginous, but
further forward the cranial cavity is closed by the unpaired sphenethmoid,
which forms a ring round the anterior portion of the brain-cavity, hence
called "os en ceinture" by some anatomists. The frontals and parietals fuse
into one pair of fronto-parietal bones, and these again can fuse together
in the middle line; as in Aglossa and _Pelobates_. The palatal portion of
the palato-quadrate cartilage is complete, reaching forwards to the sides
of the ethmoid region. The curved arch, formed by this cartilage, is
covered by the following bones: (1) the quadrato-jugal, reduced to a thin
splint which connects the quadrate and squamosal with the posterior end of
the maxilla; (2) the pterygoid, always strong, extending from the distal
inner corner of the quadrate to the maxilla, sometimes also to the
palatine, and with a broad, median process to the parasphenoid, this
process covering ventrally most of the otic region; (3) the palatines,
which vary considerably in shape and size; they are placed transversely and
meet in the middle line; in _Bombinator_ and _Pelodytes_ they are absent.
The quadrates are directed transversely and backwards, in conformity with
the wide gape of the mouth. The squamosal is always well developed,
covering the whole of the quadrate on its outer side; it has a forwardly
directed process which ends freely in _Rana_, meets a corresponding process
of the maxilla and forms a bony arch with it in _Discoglossus_,
_Pelobates_, and others, or {29}is scarcely developed at all, for instance
in _Bufo_. In _Pelobates cultripes_ the squamosal is very wide and forms a
junction with the fronto-parietals, thus producing a broad bridge across
the temporal fossa.
The nasal bones are large and meet in the middle line. Frequently they
leave a space between them and the diverging anterior portion of the
fronto-parietals, through which gap appears part of the dorsal surface of
the ethmoid cartilage. A fontanelle between the frontals occurs in most
Hylidae, many Cystignathidae, some few Bufonidae, in _Pelodytes_ amongst
the Pelobatidae, and in the Discoglossidae.
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