The Ornithosauria: An elementary study of the bones of Pterodactyles made from fossil remains found in the Cambridge Upper Greensand, and arranged in the Woodwardian Museum of the University of CambridgeSeeley, H. G. (Harry Govier)
Science
The Ornithosauria: An elementary study of the bones of Pterodactyles made from fossil remains found in the Cambridge Upper Greensand, and arranged in the Woodwardian Museum of the University of Cambridge
Seeley, H. G. (Harry Govier)
Pterosauria
Nearly every writer on Pterodactyles, who has expressed any opinion
at all, has formed an estimate of his own of their organization. They
have been assigned to almost all possible positions in the vertebrate
province, by great anatomists who all had before them very similar
materials. An account of these views is given by von Meyer in his
monograph of the Pterodactyles of the Lithographic Slate. It will not
be necessary to discuss these conclusions here, for the materials
from the Lithographic Slate and those from the Cambridge Greensand
are so different that no light would be thrown on the organization of
the animals by an exposition of any fallacious inferences from German
specimens. In England they are classed with Reptilia, chiefly through
the influence of the discourse upon them given by Baron Cuvier in his
_Ossemens Fossiles_[A]. It therefore may conduce to a clear view of
the subject to quote in Cuvier's words the passages in that memoir
which have been supposed to establish their position among reptiles. He
says,--"Ayant encore porté mon attention sur le petit os cylindrique
marqué _g_ (i.e. os quadratum) qui va du crâne à l'articulation des
mâchoires, je me crus muni de tout ce qui étoit nécessaire pour classer
ostéologiquement notre animal parmi les reptiles." The exact relations
of the quadrate bone are not seen in either Cuvier's or Goldfuss' or
von Meyer's figures of this Pterodactyle, the P. longirostris; but in
von Meyer's figures of P. crassirostris, P. longicollum, and P. Kochi
it appears to be a free bone articulated to the squamosal and petrosal
region of the skull and with the lower jaw. This is not the case with
either Chelonians or Crocodiles, which have the quadrate bone firmly
packed in the skull; nor is it paralleled even among those lizards
and serpents which have the bone as free; while, on the contrary, it
is characteristic of the whole class of birds. The form of the bone
is not more Lacertian than Avian, while its direct attachment to the
bone of the brain-case finds no parallel among lizards, but is exactly
paralleled in all birds.
[Footnote A: Tome V. Part a, pp. 358, 383. Edition, 1814.]
Cuvier then goes on to say, "Ce n'étoit pas non plus un oiseau,
quoiqu'il eût été rapporté aux oiseaux palmipèdes par un grand
naturaliste[B]." Which position he supports as follows:--
[Footnote B: Blumenbach.]
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