Coelurosauravus elivensis

A small Malagasy reptile with a membrane supported by long rods that were not extensions of its ribs or limbs.

Coelurosauravus elivensis gliding between trees in a Late Permian Madagascar landscape
The patagial rods and grasping limbs follow fossils; the membrane outline, colour and glide path are reconstructed.

Coelurosauravus elivensis was a small reptile from the Late Permian of Madagascar, famous for long bony rods that supported a membrane along the sides of its body. Those rods were separate from the ribs and forelimbs, creating a gliding surface unlike the wings of birds or bats. A recent redescription of the referred skeleton also found strong features for clinging to tree trunks and an extra bone segment in the fifth finger. Together, the fossils support an animal adapted to climbing and gliding, but they do not preserve the membrane's full outline or measure its performance. The profile belongs in the other fossil reptile catalogue.

Quick facts

Scientific nameCoelurosauravus elivensis Piveteau, 1926
GroupWeigeltisauridae, within Neodiapsida
AgeLate Permian
FormationLower Sakamena Formation, Madagascar
Key anatomyLong dermal rods supported a lateral gliding membrane
LocomotionClimbing and gliding are supported; exact performance is unknown
Related genusWeigeltisaurus is a distinct genus from Germany
Evidence guide

What can the fossils tell us?

The patagial bones are distinct from ribs and limb elements

The bones establish a skeletal support system. The membrane's thickness, trailing edge and aerodynamic performance are not preserved.

A Malagasy fossil with a long history

Jean Piveteau named Coelurosauravus elivensis in 1926 from fossils collected in southwestern Madagascar. The remains come from the Lower Sakamena Formation and include several flattened skeletons, some with bones preserved in three dimensions. A 2022 redescription examined all specimens previously referred to the species, adding detail to the trunk, limbs and unusual membrane-supporting rods.

The family Weigeltisauridae includes other small Permian reptiles with lateral gliding structures. In older literature, the German Weigeltisaurus was sometimes grouped within Coelurosauravus. Current anatomical comparisons distinguish the Malagasy C. elivensis from Weigeltisaurus jaekeli, which comes from a different fossil fauna and continent.

Rods outside the ribs

Long, slender bones called patagials extend from the sides of the trunk. They are not elongated ribs and do not form part of the forelimb. Their arrangement provided a frame for a skin membrane, or patagium, that could spread laterally. This is a distinct solution from the limb-supported wings of birds and bats and from the rib-supported gliding membrane of living Draco lizards.

Fossils preserve the bony supports more clearly than the membrane itself. Its exact rear edge and tension are uncertain, so the silhouette in a reconstruction is not a direct tracing of a complete soft-tissue fossil. The bones show a structure capable of supporting a broad surface; they do not provide a measured glide distance or descent angle.

A grasping hand and a tree-clinging body

The postcranial study describes features in the shoulder, forearm, pelvis and fingers that resemble those of animals adapted to cling to vertical surfaces. The fifth finger of the hand has an additional phalanx in weigeltisaurids where this region is preserved. The researchers suggested that the elongated digit could have helped grip the membrane or adjust its tension, drawing a comparison with the living gliding lizard Draco.

That proposed action is a functional hypothesis, not a behaviour caught in stone. The extra phalanx is directly observable; how it contacted the membrane is inferred. Taken with the limb anatomy, it supports habitual life in trees more strongly than a picture of an animal launching from open ground.

What “gliding” means here

Weigeltisaurids are widely regarded as the earliest vertebrates known with skeletal features for gliding. The term describes a controlled descent using a membrane, rather than powered flight. No fossil records the aerodynamic forces acting on Coelurosauravus, and the exact membrane area, mass distribution and launch height cannot be measured from the preserved rods alone.

The Late Permian Period forests and seasonal landscapes provide a plausible setting for moving between trunks, but the formation's rocks do not preserve a particular glide path. Small sharp teeth are compatible with feeding on invertebrates, yet there are no associated stomach contents to confirm a species-specific diet.

Keeping the reconstruction tied to evidence

The skull, limbs, extra finger segment and patagial rods are fossil anatomy. A full body outline uses comparisons with related reptiles, and the membrane surface uses additional inference. Colour, skin pattern and social displays are not preserved. These uncertainties do not weaken the discovery: they show precisely how an unusual locomotor system can be inferred from skeletal parts.

Coelurosauravus was not a dinosaur and was not a flying lizard in the modern taxonomic sense. It belonged to an extinct diapsid branch and evolved a gliding apparatus independently. Its place beside other extinct lineages in the catalogue is a navigational choice, while its fossil anatomy tells a distinctive story of climbing and aerial descent.

Frequently asked questions

Could Coelurosauravus fly under its own power?

No evidence shows powered flight. Its membrane-supporting rods are interpreted as a gliding apparatus for controlled descent.

What held up its gliding membrane?

Long patagial rods along the body supported the membrane; they were not extensions of the ribs or arms.

Did the extra finger bone control the membrane?

Researchers proposed that it may have helped grip or tension the membrane, but the fossil does not preserve the hand using it.

Was Coelurosauravus the same as Weigeltisaurus?

No. They were related weigeltisaurids from different regions and are treated as distinct genera.