FIRST RECORD OF A MOSASAUR FROM IOWA
The Mosasauridae were a family of extinct marine reptiles that eventually had a global distribution in the later Mesozoic, and lived between 99 and 65 million years ago. They are well known from the inland sea that existed in the Mesozoic of central North America, with many species being found in the great plains, primarily the genera Clidastes, Tylosaurus and Platecarpus.
The vertebrae were identified through comparison with other mosasaur fossils and it conformed favorably with plioplatecarpine caudal vertebrae, which are distinctive in having sockets where the chevrons would attach instead of the chevrons being fused to the vertebrae. From only 3 fused caudal vertebrae it is not possible to identify the exact genus or species, but in looking at the 3 genera that are well known from the time neither Tylosaurus nor Platecarpus had fused chevrons.
Since the load of rock was from a quarry the specific rock unit it came from is yet to be determined, however The bedrock lithology at the locality where the fossil was quarried is either the Dakota and Windrow formations or the Fort Benton Group according to the geological maps that have been consulted.