Latoplatecarpus: a plioplatecarpine mosasaur from the Campanian sea

A new genus emerged when researchers tested whether familiar Platecarpus fossils belonged to one evolutionary branch.

Latoplatecarpus willistoni swimming through the Late Cretaceous Western Interior Seaway
The skull and body proportions follow described mosasaur fossils. Skin, colour, soft fins and the exact position in the seaway are reconstructed.

Latoplatecarpus is a plioplatecarpine mosasaur from the Campanian seas of North America. Konishi and Caldwell named it in 2011 while revising a group of fossils long assigned to Platecarpus. The type species, L. willistoni, is based on a substantially preserved skull and associated bones from Manitoba. The same study transferred L. nichollsae into the genus, though later analyses have continued to test whether the two species form one natural group. Its history makes Latoplatecarpus a useful case in the marine reptile catalogue for seeing how new comparisons can alter a familiar fossil classification.

Quick facts

Scientific nameLatoplatecarpus Konishi & Caldwell, 2011
GroupSquamata, Mosasauridae, Plioplatecarpinae
Named speciesL. willistoni; L. nichollsae was referred in the original revision
AgeLower to middle Campanian, Late Cretaceous
Type localityPembina Member of the Pierre Shale, Manitoba, Canada
Type materialSkull and jaws with associated parts of the skeleton
Main evidenceCranial and postcranial characters assessed in a phylogenetic analysis
Main limitThe genus composition and assignment of incomplete specimens remain testable
Evidence guide

What the fossils establish

The holotype preserves much of the skull and jaws, with associated vertebral and shoulder material

The type does not preserve an entire skeleton or soft-tissue outline.

A genus separated from a broad Platecarpus

The name Latoplatecarpus was introduced in a 2011 systematic revision by Takuya Konishi and Michael Caldwell. The authors reassessed plioplatecarpine mosasaurs using a character matrix rather than relying on one conspicuous bone. Their analysis included 97 morphological characters and proposed two new genera. For Latoplatecarpus, they named L. willistoni and recombined the previously named species Plioplatecarpus nichollsae.

The holotype of L. willistoni, TMP 84.162.01, comes from the Pembina Member of the Pierre Shale in Manitoba. It preserves a nearly complete skull and lower jaws together with part of the skeleton. Such associated material is more informative than an isolated tooth because several regions can be compared in one individual. It still leaves gaps: the fossil does not preserve every vertebra, a complete tail, or the skin and fin outline.

The species name honours Samuel Williston, whose early work helped organise the study of North American mosasaurs. The genus name signals its relationship to Platecarpus, but the new classification did not mean that all older identifications had immediately been resolved. Some incomplete remains assigned to related genera continue to require comparisons against overlapping characters.

What the skull contributes to classification

Mosasaur skulls contain many useful features in the palate, braincase, quadrate and tooth-bearing bones. Konishi and Caldwell compared these regions across a broad sample and recovered a different arrangement from a simple, expansive Platecarpus. In their analysis, L. willistoni occupied a position near the base of a group that also included Platecarpus tympaniticus. Those placements describe the result of a particular dataset and method; later character sampling can change the branching pattern.

The original genus included L. nichollsae, a species previously placed in Plioplatecarpus. The two species are not represented by identical material, so any contrast between them must distinguish observed differences from missing anatomy. Follow-up phylogenetic work has revised character scores in plioplatecarpines, reinforcing the need to test the placement rather than treat a 2011 classification as a final verdict.

A marine predator, with limits on the life reconstruction

The teeth are conical and suited to gripping prey that could slip from a jaw. Together with the skull and mosasaur body plan, they support a marine predator. Fish and other marine vertebrates are plausible prey, but the type specimen does not preserve its last meal. Nearby fossils describe the Western Interior Seaway ecosystem, not a species-specific diet by themselves.

Mosasaurs propelled themselves chiefly with the muscular tail and its fin, while the limbs were transformed into paddles. This broader anatomical pattern makes a fully marine lifestyle clear. The tail fin's living shape, exact swimming speed, skin colour and hunting sequence cannot be read directly from the Latoplatecarpus holotype. Reconstructions borrow comparisons from better-preserved mosasaurs and should be understood as models.

The safest account is therefore specific about what is known: a Campanian plioplatecarpine named from a substantial Manitoba skull, placed among related mosasaurs through comparative anatomy, and originally understood to include two species. Its classification is stronger than a guess from one tooth, but the boundaries of the genus remain open to future testing.

Frequently asked questions

When did Latoplatecarpus live?

Its named material is from the Campanian Stage of the Late Cretaceous, including the Pembina Member in Manitoba.

Why was the genus separated from Platecarpus?

A 2011 analysis compared many skull and skeleton characters and found that fossils assigned to the broad older genus represented distinct lineages.

Which species were included?

The original revision named L. willistoni and transferred L. nichollsae into Latoplatecarpus. Their grouping can be tested as new evidence is analysed.

What did it eat?

Its conical teeth support gripping animal prey, but the type fossil does not preserve stomach contents that identify a particular meal.