Sampling of hiatal horizons within the Hauterivian part of the Speeton Clay
Formation of north-east England has produced teeth of several species of s
harks and rays, four of which are previously unnamed. One species of shark,
Cretorectolobus doylei sp. nov., and two species of rays, Spathobatis rugo
sus sp. nov. and Dasyatis speetonensis sp. nov., are named, whilst the pres
ence of an indeterminate triakid shark is also noted. Synechodus dubrisiens
is (Mackie) is shown to be a senior synonym of S. michaeli Thies. Although
the dasyatid ray and triakid shark are by far the oldest representatives of
their respective families, the overall composition of the fauna is conside
red to resemble more closely assemblages known from the Jurassic than those
from upper parts of the Cretaceous.