Fish teeth and other remains from the British Cretaceous contain abundant e
vidence for post-mortem colonization by endolithic organisms. The borings a
re here recognized as occurring in three morphotypes, including a flask-sha
ped form not previously recorded. There is strong evidence to suggest that
each of these boring types shows a strong preference for a particular subst
rate histology. The damage and destruction of vertebrate remains by microbo
rings is here considered to exert a major taphonomic conrol on microvertebr
ate assemblages. The relationships between the intensity of colonization of
vertebrate material by endolithic organisms and palaeoenvironment have imp
lications for using these bone microborings as palaeoenvironmental indicato
rs.