A new species of Coniasaurus, from the Lower Chalk Formation (Upper Cretace
ous: Lower to Middle Cenomanian) of southeast England, is described. The ty
pe and only specimen preserves the right and left maxilla, frontal,? squamo
sal?, parietal, partial right and left pterygoids, right septomaxilla, part
ial right and left vomeropalatines, four articulated dorsal vertebrae, seve
ral fragmentary ribs, and the left scapula and coracoid. The maxilla and ve
rtebrae of the new species are similar in form to equvialent elements from
the genotype, Coniasaurus crassidens Owen, 1850. However, significant diffe
rences are found in maxillary tooth morphology, the number of maxillary tee
th, and the length of the maxilla. In Coniasaurus, sp. nov., in contrast to
the genotype, the maxilla is shorter and slightly more robust, the ascendi
ng process of the maxilla is taller (but lower as compared to other squamat
es), the crowns of the maxillary teeth are swollen and blunt-tipped, not bu
lbous, and without lateral sulci. Cladistic analysis of six mosasaur taxa,
three 'aigialosaur' taxa, Coniasaurus crassidens, and Coniasaurus, sp. nov.
(73 characters, 11 taxa in total) found 52 shortest cladograms (137 steps;
CI 0.650; HI 0.350). A Strict Consensus Tree found the genus Coniasaurus t
o be monophyletic in air cladograms; the six mosasaur taxa also formed a mo
nophyletic group nested higher in the cladogram. However, basal relationshi
ps between coniasaurs, the three aigialosaur taxa (Aigialosaurus dalmaticus
, Aigialosaurus [=Opetiosaurus] buccichi, Carsosaurus marchesetti), and the
mosasaur clade were unresolved. A Majority Rule Consensus tree found that
in 58% of the cladograms, coniasaurs are the sister-group to a clade compos
ed of mosasaurs and aigialosaurs. Previous suggestions of aigialosaur parap
hyly cannot be verified or refuted by this analysis, however, coniasaurs ar
e a basal clade within the larger clade containing mosasaurs and aigialosau
rs.