Trilophosaurus buettneri

A Late Triassic archosauromorph with broad three-cusped cheek teeth, known from rich Texas and Arizona fossil beds.

Trilophosaurus buettneri feeding among Late Triassic plants in Texas
The broad skull and three-cusped teeth are based on fossils; posture and plant setting are reconstructed.

Trilophosaurus buettneri was a Late Triassic archosauromorph from the Dockum and Chinle successions of the southwestern United States. E. C. Case named it in 1928 from UMMP 2338, then interpreted as a fragment of lower jaw. A 2024 re-examination using high-resolution images and a 3D model identified the type as an incomplete maxilla instead. Hundreds of later bones and partial skeletons reveal broad, three-cusped cheek teeth suited to processing plants. A proposed climbing lifestyle remains debated because limb and claw proportions do not give an uncomplicated arboreal signal. Its corrected type and distinctive dentition make it a notable entry in the other fossil reptile catalogue.

Quick facts

Scientific nameTrilophosaurus buettneri Case, 1928
GroupTrilophosauridae, Allokotosauria
AgeLate Triassic; known occurrences span multiple biochronological intervals
LocalitiesDockum Group and Chinle Formation, Texas and Arizona
HolotypeUMMP 2338, incomplete right maxilla
Cheek teethBroad crowns with three labiolingually aligned cusps
Known materialHundreds of bones and several partial skeletons
DietPlant processing supported by dental form; exact menu unknown
Evidence guide

What can the fossils tell us?

High-resolution re-examination identifies UMMP 2338 as an incomplete maxilla

The correction changes which side and jaw the bone represents; it does not change the species name.

A type fossil reidentified after nearly a century

E. C. Case named Trilophosaurus buettneri in 1928 from UMMP 2338, a small jaw fragment from Crosby County, Texas. Because the fossil was incomplete and no other specimens of the animal were then known, it was interpreted as part of a lower jaw. Rountrey and colleagues revisited the specimen in 2024 with high-resolution photographs and a digital three-dimensional model. Its anatomy identifies it as an incomplete right maxilla, part of the upper jaw.

The change matters because the tooth row can now be compared in the correct orientation with better fossils. It does not create a new species or invalidate the name. The name-bearing piece remains a fragment, but hundreds of later specimens from the Dockum Group and Chinle Formation supply a much fuller picture. Each referral still needs diagnostic features; abundance does not make every isolated bone equally informative.

Three cusps across each broad cheek tooth

The genus is named for the three principal cusps on its cheek teeth. In T. buettneri, the crowns are broad from the cheek side to the tongue side and short from front to back. The three cusps form a crushing and grinding surface rather than the blade-like edge of a meat-slicing tooth. The tooth row was suited to processing plant matter, and wear patterns add evidence about repeated contact.

Dental shape supports herbivory, but it cannot identify a specific leaf, seed or stem. Nor should Trilophosaurus be called a dinosaur: it was an unusual archosauromorph outside Dinosauria. Researchers have proposed different positions for trilophosaurids within the archosauromorph family tree, and those placements depend on the characters and taxa included in each analysis.

Many bones, several species and variable anatomy

Later collections include hundreds of isolated remains and several more complete skeletons. They show that the animal was medium-sized, with a long body and limbs, though estimates of total length are reconstructions from incomplete skeletons rather than a direct measurement of one intact fossil. The related species T. jacobsi is distinguished using combinations of tooth and skeletal traits, so an isolated tooth should not be assigned by its three cusps alone.

Growth and wear affect what individual bones look like. A large fossil sample can reveal variation unavailable from the holotype, but it may also combine different ages, body sizes and preservation histories. Good taxonomic work tests several anatomical features together and keeps uncertain referrals separate.

Did Trilophosaurus climb?

An arboreal interpretation has been proposed from skeletal features, including limb proportions and claws. Later discussion questioned whether those features indicate climbing: the limbs are not a simple match for specialised climbers, and the claws are laterally compressed rather than broadened for digging. The evidence has not established habitual tree climbing. At most, the hypothesis invites tests against functional anatomy and a wider range of living comparisons.

The fossil beds formed in Late Triassic continental environments of what is now Texas and Arizona. Different localities and stratigraphic levels span substantial time; they should not be collapsed into one scene. The fossils support a distinctive plant-processing archosauromorph with a corrected upper-jaw type and a rich but partly disarticulated record. Skin, colour, social life and an exact gait remain unknown.

Frequently asked questions

Was the Trilophosaurus type a lower jaw?

No. A 2024 re-examination identified UMMP 2338 as an incomplete right maxilla, or upper-jaw bone.

Why is it called Trilophosaurus?

Its cheek teeth have three principal cusps across each broad crown.

Was Trilophosaurus a dinosaur?

No. It was an archosauromorph reptile outside Dinosauria.

Could it climb trees?

Climbing has been proposed, but limb and claw anatomy do not settle the question; habitual arboreal behaviour remains uncertain.