Mw. Caldwell, On the aquatic squamate Dolichosaurus longicollis Owen, 1850 (Cenomanian, Upper Cretaceous), and the evolution of elongate necks in Squamates, J VERTEBR P, 20(4), 2000, pp. 720-735
The marine squamate, Dolichosaurus longicollis, from the Upper Cretaceous (
Cenomanian) Chalk deposits of southeast England is redescribed. The elongat
e neck of D. longicollis is produced by an increased number of cervical ver
tebrae. Cervical peduncles are elongate, curved and are nor fused to the hy
papophyses. There is no scapulocoracoid fenestra, the coracoid is not emarg
inated, and the scapula and coracoid are not fused. The splenial and angula
r articulate in a ball-and-socket joint similar to that of mosasaurs and Co
niasaurus crassidens. The forelimb and pectoral girdle elements show eviden
ce of reduction as compared to the pelvic girdle and rearlimb. Cladistic an
alysis of six mosasaur taxa, three 'aigialosaur' taxa. Coniasaurus crasside
ns. Coniasaurus gracilodens. and D. longicollis. using 66 characters, found
27 most parsimonious cladograms (MPCs): 122 steps: C.I. 0.648: H.I. 0.352:
R.I. 0.669. A Strict Consensus Tree found support for the monophyly of the
Mosasauridae and Aigialosauridae; sister-group relationships between conia
saurs. Dolichosaurus. Aigialosauridae and Mosasauridae are an unresolved po
lytomy. A Majority Rule Consensus Tree finds Dolichosaurus as sistergroup t
o (C. crassidens, C. gracilodens (Aigialosauridae (Mosasauridae))) in nine
(33%) of the MPCs. Lack of support for a more inclusive Dolichosauridae com
posed of Dolichosaurus + (C. crassidens, C. gracilodens) is attributed to t
he incompleteness of the fossil remains of these three taxa. Presence/absen
ce of a pectoral girdle currently defines the presence/absence of a neck. T
his definition is insufficient and hypapophyses are found more informative
regarding taxic differences and transformational scenarios. The paleobiolog
y of Dolichosaurus is reconstructed as similar to coniasaurs. nothosaurs, a
nd modern sea snakes.