Araeoscelidia
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Araeoscelidia or Araeoscelida is a clade of extinct
diapsid Diapsids ("two arches") are a clade of sauropsids, distinguished from more primitive eureptiles by the presence of two holes, known as temporal fenestrae, in each side of their skulls. The group first appeared about three hundred million years a ...
reptiles superficially resembling lizards, extending from the Late Carboniferous to the Early
Permian The Permian ( ) is a geologic period and System (stratigraphy), stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last ...
. The group contains the genera '' Araeoscelis'', ''Petrolacosaurus'', the possibly aquatic ''Spinoaequalis'', and less well-known genera such as ''Kadaliosaurus'' and ''Zarcasaurus''. This clade is considered to be the sister group to all (currently known) later diapsids.


Description

Araeoscelidians were small animals (less than one meter in length) looking somewhat like lizards, though they are only distantly related to true lizards. They differ from other, earlier sauropsids by their slender limbs, their elongated tail, and of course by the presence of two Skull#Temporal Fenestra, temporal openings, the feature defining the
diapsid Diapsids ("two arches") are a clade of sauropsids, distinguished from more primitive eureptiles by the presence of two holes, known as temporal fenestrae, in each side of their skulls. The group first appeared about three hundred million years a ...
condition. In '' Araeoscelis'', only the upper temporal opening remains, thus resulting in a derived euryapsid condition.


Genera

Araeoscelidia includes well-known genera such as '' Araeoscelis'' Williston 1910, ''Petrolacosaurus'' Lane 1945 and ''Spinoaequalis'', known from virtually complete skeletons. ''Zarcasaurus'', ''Aphelosaurus'' and ''Kadaliosaurus'' belong to this clade, but are known only from post-cranial remains and a mandible fragment for ''Zarcasaurus''. The genus ''Dictybolos'' has been included in Araeoscelidia by Olson (1970) but this inclusion has been criticized e.g. by Evans (1988), especially since Olson also included distantly related groups such as Protorosaurus, protorosaurs and mesosaurs. New specimens have been discovered in Oklahoma, United States but so far lack a scientific description.


Phylogeny

Phylogenetic relationships: The majority of phylogenetic studies recover araeoscelidians as Basal (phylogenetics), basal diapsids; however, Simões ''et al.'' (2022) recover them as Crown group#Stem groups, stem-amniotes instead, as the sister group to the clade including Captorhinidae and ''Protorothyris archeri''.


Stratigraphic and geographic distribution

Araeoscelidia are known from the Late Carboniferous in the United States (''Petrolacosaurus'', ''Spinoaequalis'') to the Early Permian in France (''Aphelosaurus''), Germany (''Kadaliosaurus'') and the United States (''Dictybolos'', ''Zarcasaurus'', ''Araeoscelis''). Apart from araeoscelidans, only one other diapsid is known before the Lopingian, Late Permian: ''Orovenator'' from the Early Permian of Oklahoma.


References


Further reading

* * * * * * * * * * * * * * * * * * * {{Taxonbar, from=Q136663 Prehistoric diapsids Pennsylvanian first appearances Cisuralian extinctions Taxa named by Samuel Wendell Williston Fossil taxa described in 1913