Two specimens, however, suggest
stronger evidence for attack rather than accidental breakage of elements. These feature a
series of elements with marks that give an arc unlike one of impact, but strongly
resembling the curve of a bite. The first specimen (BMNH P.6924) was excavated by
Alfred Leeds and accessioned by the BM(NH) in 1893 (Liston & Noe 20(4), and consists
of a series of dorsal fin-rays (fig. 9.3A-C). Although, as was Alfred Leeds' usual practice.
they have been washed clean of their clay and so do not have any matrix to indicate their
precise relations when found, a comparable specimen excavated by Henry Keeping
(CAMSM J.46873, fig. 2.3, fig. 4.10) has preserved some matrix that indicates that these
elements were in contact at their broad bases. With this knowledge, the arrangement of the
bones in life can be reconstructed, providing an estimated width of bite of 130mm, with
signs of a tooth impression of 47mm diameter. As far as is known, a bite and tooth this
size in the Oxford Clay sea could only have been made by a pliosaur, the plesiosaurs
having too small a gape (Andrews 1910). A pliosaur tooth of this girth (probably
Liopleurodon) would have a crown of around IOOmm length, with a total length of around
300mm (L. Noe, pers. comm., 51712006). The second specimen to give evidence of the
specific mouth shape of an attacker is BMNH P.62054, a collection of fin-rays (probably
pectoral, but this can only be confirmed or denied once the preparation of the pectoral fins
of PETMG F.174 has been completed) donated by I. Crowson (via D.M. Martill) in July
1985 from the Bunting's Lane borrow pit near Peterborough, believed to be from Bed 12
(Hudson & Martill 1994). A section of this was figured by Martill (I 986b: plate 9C), but
viewing the entire specimen (fig. 9.3d) indicates the constrained arc of the damage, again
suggesting a mouth. Smaller in size, it could be from a plesiosaur as well as a small
pliosaur (Andrews 1913), but it is too broad and curved to have been made by a
crocodilian.