New data contradict the mosasaur-bite hypothesis for the origin of hol
es seen in Placenticeras ammonites from the Late Cretaceous Pierre Sha
le and Bearpaw Formation of the western interior of North America. Obs
ervations of a limpet-infested Placenticeras ammonite and of several P
lacenticeras specimens with radular scratch marks reveal that the limp
ets dwelled on floating ammonites, and their homing activity produced
circular depressions. When altered during diagenesis, the depressions
mimic tooth punctures. Crushing experiments on fresh Nautilus shells u
sing a mosasaur robot show that mosasaur bites could not have produced
holes resembling those in the fossils. Furthermore, sectioning of ''b
itten'' ammonites reveals that sepia are sometimes intact under the ho
les, an observation irreconcilable,vith penetration by a tooth. We pre
sent an alternative interpretation that the alleged ''bite marks'' in
Placenticeras ammonites are really limpet home scars that were altered
after burial. While predation of mosasaurs on ammonites remains a pos
sibility, it would have to be demonstrated by other criteria. Our find
ings do not support mosasaur-ammonoid coevolution in the Late Cretaceo
us.