Protorosaurus (from , 'earlier' and , 'lizard')
Description
Protorosaurus grew up to in length, and was a slender, lizard-like animal, vaguely resembling a
monitor lizard, with long legs and a long neck.
History
Protorosaurus was one of the first fossil reptiles to be described, being initially described in Latin in 1710 by from a specimen found in
Thuringia in Germany, who considered the animal to be a crocodile, and most similar to the
Nile crocodile (
C. niloticus).
[ Spener CM. 1710. Disquisitio de crocodilo in lapide scissili expresso, aliisque Lithozois Miscellanea Berolinensia ad incrementum scientiarum ex scriptis Societati Regiae Scientiarum exhibitis 1:92-110] Over a century later, in publications in 1830 and 1832 Hermann von Meyer recognised
Protorosaurus as distinct extinct reptile and gave it a formal species description, dedicating an extensive
monograph to it in 1856. In 1871 Thomas Henry Huxley erected the clade
Protorosauria, with
Protorosaurus as the only member.
The German specimens were found in the
Kupferschiefer a widespread unit of Late Permian (likely
Wuchiapingian) age.
In 1914, a new ceratopsian dinosaur found by Lawrence Lambe was again given the name Protorosaurus (in this sense meaning "before Torosaurus"). When Lambe found that the name had already been used for the early archosauromorph, he renamed his ceratopsian Chasmosaurus.
In 1870, a new species, Protorosaurus huxleyi was described from a railway cutting near Middridge in County Durham in northern England, in sediments belonging to the Marl Slate, a unit that is equivalent to the Kupferschiefer, however it was later shown that this specimen was not Protorosaurus, and it was subsequently placed in the new genus Adelosaurus.
In 1993, a specimen of Protorosaurus was described from Quarrington Quarry also in County Durham, in sediments of the Marl Slate. This skeleton included fragments of the skull that had not previously been known.
Paleobiology
Stomach contents of a specimen of
Protorosaurus show the presence of numerous ovules of the locally common
Voltziales conifer
Ullmannia frumentaria, which was unexpected given its unspecialised dentiton of conical and unserrated teeth, which were assumed to represent a predatory lifestyle. Along with the coniferous ovules, several rounded pebbles were found in the body cavity, these may have functioned as
gastroliths.
Classification
Protorosaurus has been suggested to be closely related to
Czatkowiella from the Early Triassic of Poland,
but the remains of
Czatkowiella are fragmentary and mixed in with those of other reptiles, so it is possible that the taxon is a chimaera.
In a comprehensive analysis of "Protorosauria" in 2021,
Protorosaurus was consistently recovered as the earliest diverging member of
Archosauromorpha.
The cladogram below follows an analysis by Ezcurra (2016), and highlights the position of Protorosaurus among other early archosauromorph reptiles.
Paleoenvironment
The Kupferschiefer and equivalent Marl Slate is a marine unit that forms part of the
Zechstein, a sequence of rocks formed on the edge of the Zechstein Sea, a large inland shallow sea that existed in Northern Europe during the Late Permian. The environment at the time of deposition is considered to have been semi-arid. The terrestrial flora of the Zechstein is dominated by conifers, with seed ferns also being common, while
Taeniopteris,
Ginkgoales and
Equisetidae are rare. Other terrestrial vertebrates found in the Kupfershiefer and lower Zechstein include the gliding
Weigeltisauridae reptiles
Weigeltisaurus and
Glaurung, the
pareiasaur Parasaurus, the
cynodont Procynosuchus, and indeterminate
Captorhinidae,
, and
Dissorophoidea Temnospondyli.
