Bavarisaurus macrodactylus was a small squamate from the Late Jurassic lithographic limestones of Bavaria. Its fossils preserve skull bones, a long tail and four slender limbs with notably elongated digits. A lizard skeleton inside the famous Compsognathus specimen was once assigned to Bavarisaurus, but a later anatomical revision gave that animal a separate name, Schoenesmahl dyspepsia. Both belong in the ancient lizard and snake catalogue, but only the second is directly documented as food for the dinosaur.
Quick facts
| Scientific name | Bavarisaurus macrodactylus |
|---|---|
| Group | Lepidosauria, Squamata |
| Age | Late Jurassic, Tithonian |
| Locality | Solnhofen archipelago, Bavaria, Germany |
| Material | Skulls and postcranial remains |
| Length | Several tens of centimetres; exact value varies by specimen |
| Likely food | Small invertebrates, inferred from teeth and size |
| Important correction | The lizard inside Compsognathus is Schoenesmahl, not Bavarisaurus |
What can the fossils tell us?
Thin bones are difficult to read in compressed limestone; preparation and cracks can obscure or imitate sutures.
Missing or bent tail tips and the method used to measure a slab affect any single total-length figure.
A 2017 reassessment identified it as Schoenesmahl, a separate ardeosaurid, rather than Bavarisaurus.
No stomach contents, trackways or soft tissues establish exact prey, speed or climbing behaviour.
Name and history of study
The genus name refers to Bavaria, where the fossils were found. The species epithet macrodactylus means “long-fingered.” Early material was described in the nineteenth century, before the anatomy and relationships of fossil lizards were understood in the modern sense. Susan Evans reassessed the genus in 1994 after new skull material became available.
Solnhofen limestone compresses very thin bones into fine slabs. Sutures can disappear beneath the rock, and fractures can resemble boundaries between skull bones. Additional material helped clarify the temporal region, palate and jaws. A lizard skull is not a set of obvious plates; interpreting it requires comparing contacts and proportions across specimens.
The same limestone system is famous for Archaeopteryx, pterosaurs, fishes and marine invertebrates. Shared preservation in Solnhofen does not imply close ancestry. Archaeopteryx was a feathered avialan, whereas Bavarisaurus was a squamate reptile.
What the skeleton shows
Known material includes cranial and postcranial bones. The body was elongated, the tail formed a substantial portion of its length, and all four limbs were relatively slender. The long digits explain the species epithet and may have helped the animal gain purchase on uneven surfaces. They do not by themselves demonstrate a specialised tree-climbing lifestyle.
The skull had the arrangement of an early lizard, but it should not be treated as a copy of a modern gecko or skink. Researchers compare the temporal arches, contacts among the frontal and parietal bones, palate and jaw. Those features help place a fossil on the squamate family tree, yet missing or compressed parts can change which characters are visible.
Small teeth were suited to seizing small prey rather than slicing large pieces or grinding vegetation. The exact diet remains unknown. No securely identified stomach contents belong to Bavarisaurus, so insects and other small invertebrates are plausible prey based on anatomy, not a recovered menu.
Size, tail and locomotion
The total length was several tens of centimetres, including the tail. A single precise figure would hide differences among specimens and uncertainty created by missing tail tips. Measuring along a curved slab also gives a different result from restoring a straightened body line.
The tail likely helped with balance during movement. Tail shedding cannot be confirmed from a long tail alone: fossil evidence for autotomy requires characteristic fracture planes in the vertebrae. Likewise, long fingers may have helped with climbing, gripping or moving across irregular ground, but no trackway records the animal's exact gait.
A cautious reconstruction is a small terrestrial lizard able to use low vegetation and rocky surfaces. A fully arboreal posture, extraordinary speed or a specific escape manoeuvre would go beyond the skeleton. The animal's small size and delicate bones also help explain why such land vertebrates are less common in the fossil record than large dinosaurs.
The lizard inside Compsognathus
A small lizard skeleton lies inside the abdominal region of the Compsognathus longipes holotype. For decades it was identified as Bavarisaurus macrodactylus, producing the popular account that this exact lizard was the dinosaur's last meal. In 2017, Jack Conrad re-examined the bones and found differences in the frontal-parietal suture, paired parietal bones and the direction of the parietal processes.
A phylogenetic analysis identified the swallowed animal as a distinct ardeosaurid, later named Schoenesmahl dyspepsia. The gut content still directly shows that Compsognathus swallowed a small lizard. It does not show that it ate Bavarisaurus. This distinction separates a real predator-prey observation from an outdated identification.
The correction matters to both profiles. Bavarisaurus should not inherit anatomy from the swallowed skeleton, and Schoenesmahl has its own name and diagnosis. The two Bavarian lizards lived in a similar island setting, but a possible encounter is not the same as a direct fossil link.
Squamate relationships and Solnhofen habitat
Bavarisaurus belongs to Squamata, the reptile group that contains living lizards and snakes. Its exact position within early squamate branches has varied among analyses. It is useful as evidence of Jurassic squamate diversity, but it is not known as the direct ancestor of any modern family.
Solnhofen slabs also limit comparisons. Compression can flatten the skull and shift delicate elements, while preparation may expose different surfaces in different specimens. A character that seems absent may instead be hidden or broken, so placement depends on features that can be checked across the available material. This helps explain why analyses have placed Bavarisaurus near different early squamate branches. The disagreement does not erase its identity as a squamate; it marks uncertainty about how early lizard lineages diverged. No proposed position makes it the direct ancestor of a living family.
During the Tithonian, the Solnhofen region was a chain of carbonate islands and shallow lagoons near the Tethys Sea. Some lagoons had restricted water exchange and conditions near the bottom that slowed scavenging and decay. Land animals could be carried into the water by storms or runoff, so the place of burial does not make Bavarisaurus aquatic.
The surrounding archipelago included vegetation, terrestrial arthropods, small reptiles, dinosaurs and pterosaurs, with fishes and cephalopods in the water. Those neighbours give environmental context, not proof of a particular meal. No eggs or nest series establish reproduction; colour, scale pattern, social behaviour, daily activity and migration are also unknown.
Frequently asked questions
Was Bavarisaurus a dinosaur?
No. It was a small squamate reptile, within the broader group that includes living lizards and snakes.
When did Bavarisaurus live?
It lived during the Tithonian age of the Late Jurassic in what is now Bavaria, Germany.
Was the lizard inside Compsognathus a Bavarisaurus?
No. A 2017 reassessment identified it as the separate ardeosaurid Schoenesmahl dyspepsia.
What did Bavarisaurus eat?
Small teeth and body size are consistent with small invertebrate prey, but no direct gut contents establish a specific diet.

