Environment Labidosaurikos specimens have been found in Permian red beds of North American. The alternative sedimentation indicates the environment
Labidosaurikos inhabited were the margins of the aquatic reservoirs that were plentiful in these areas during early Permian time Morphology of the dentition shows the tooth plate teeth are relatively small isodonts and have wear facets usually characteristic of grinding. However this would require propalinal jaw motion. Striations on the wear facets of the teeth can normally be used to determine jaw motion however they are not present on
Labidosaurikos was secondary non-dental evidence is required. The ability of the quadrate to slide antero-posteriorly over the
articular propaliny however the holotype skull provided by Stovall had damaged the articulating surface. Propaliny is evident two other captorhinids, one called
Moradisaurus shares membership in the subfamily Moradisaurinae with
Labidosaurikos. The morphology of the articular for
Moradisaurus does indicate
Labidosaurikos may have been capable of propaliny because articular fragments show great similarity to
Moradisaurus than more basal captorhinids. Other osteological evidence for herbivorous feeding via propaliny in
Labidosaurikos is vaulted skull roof, a feature that is significantly different from
Labidosaurus, Captorhinus, and other more basal captorhinids. This feature is reflected by a posterior expansion of the occipital flange of the
squamosal, suggesting muscle fibers originate in the
mandible. These muscle fibers would insert into the
coronoid process at an angle of 45 degrees to horizontal forming an arrangement that supports the lower jaw being drawn posteriorly thus enabling propaliny. ==Discovery and classification==