Galesaurus

Galesaurus (from the Greek roots for 'weasel' and 'lizard') was a prehistoric carnivorous therapsid that lived between the Induan and the Olenekian age in what is now South Africa. It was incorrectly classified as a dinosaur by Sir Richard Owen in 1859.
Notably, "Galesaurus" was mentioned in the first issue of Nature in 1869, where T. H. Huxley expressed confidence that it would eventually be shown to be a dinosaur. However, current opinion is that it was not a dinosaur and belongs to a mammal-like group called Cynodonts.
Description.
The largest "Galesaurus" skull discovered is roughly long. Larger remains indicate that an adult "Galesaurus" is roughly long. Cynodonts, including "Galesaurus," are believed to have had sprawling postures.
Examination of "Galesaurus" reveals two distinct morphs, a gracile and a robust morph. The main differences between the two morphs lie in the pectoral and pelvic girdles, as well as subtle differences in the fore and hind limbs. The morphological differences may be due to sexual dimorphism, ontogeny, or the presence of two subspecies.
Skull.
The skull of "Galesaurus" is generally wide and low, the widest part being the region of the zygomatic arches. The snout is blunt.
The nasal bones of "Galesaurus" are unusually large, they are constricted in the middle and extend over the anterior of the nostrils. A sheet of bone forms the septomaxilla that lines the floor of the naris and extends backwards between the nasal and maxilla. The skull has a septomaxillary foramen. The maxilla makes up a significant section of the lateral wall of the snout and contacts the lacrimal and jugal posteriorly. Formina perforates the maxilla, especially in the area of the canine. Two large foramina, above the fifth and sixth postcanines, are present. The ascending process of the premaxilla dorsally overlaps the nasal. The anterior of the ascending process has a small opening call the anterior premaxillary foramen.
"Galesaurus" has large, pentagonal shaped lacrimals with a flat outer surface. A fossa is present medial to the crista lacrimalis. This fossa is connected by two canals, one above the other, to the lacrimonasal canal that opens into the nasal cavity. The prefrontals extend halfway along the border of the lacrimals until they meet the postorbitals at the middle of the upper border of the orbits, forming the upper orbital margin. As in other cynodonts, the frontal is excluded from the orbital margin by the prefrontal and postorbital.
Dentition.
The upper teeth of "Galesaurus" are located on the alveolar ridges of the premaxilla and maxilla. Palatal teeth are absent in "Galesaurus". The first postcanine of "Galesaurus" only has one cusp, while the other postcanine teeth are flattened and have two curved cusps. The second tooth contains a long anterior cusp and a short posterior cusp. The base of the incisors is wide, though the crown tapers to a point. The canines and postcanines have been pushed to the outer rim of the maxilla, allowing the lower teeth enough room to lie medially to the upper teeth when the jaw is closed. Postcanine tooth replacement is believed to have occurred throughout life.
The maxilla forms a large portion of the lateral wall of the snout. It is composed of a corpus, frontal process, zygomatic process, palatal process, and alveolar process. The corpus is long, inconspicuous, and encloses the sinus maxillaris cavity. The sinus maxillaris opens into the nasal cavity dorsal to the secondary palate and anterior to the palatine. It extends anteriorly, and continues to narrow until the cavity ends below the posterior elongation of the roots of the canine. This cavity is hypothesized to have served as the cynodont equivalent to the mammalian canalis alveolaris. There are two large foramina in the maxilla, above the fifth and sixth postcanines.
Discovery and naming.
The first "Galesaurus" specimen was originally discovered in the Karoo Basin of South Africa and described by the naturalist Sir Richard Owen in 1859. Owen named the specimen "Galesaurus planiceps", but incorrectly classified "Galesaurus" as a new species of dinosaur. Owen assumed that "Galesaurus" was reptilian because its skull resembled "Rhopalodon", a synapsid that had also been misclassified as a dinosaur. Despite classifying "Galesaurus" as a dinosaur, Owen noted that "Galesaurus" was remarkably mammal-like. Owen's "Galesaurus" type specimen was considerably crushed and the teeth were poorly preserved. Only recently have articulated skeletons of "Galesaurus" been found, whose well-preserved postcranial bones yield a better understanding of Galesaurus morphology; it is now considered to be a cynodont.
Other "Galesaurus planiceps" fossils that were initially identified as "Glochinodon detinens" in 1916 and "Glochinodontoides gracilis" in 1924 were synonymized subjectively with "Galesaurus planiceps" in 1972.
Classification.
"Galesaurus" is a member of the clade Epicynodontia, which is within the infraorder Cynodontia, the ancestor group of all mammals. "Galesaurus" is also a member of the family "Galesauridae," which includes the closest relatives of "Galesaurus, Cynosaurus" and "Progalesaurus."
Paleobiology.
Locomotion.
During cynodont locomotion, the axial skeleton is unlikely to have flexed and extended in the sagittal plane as it does in mammals. Instead, cynodonts are believed to moved by lateral undulation, the typical axial movement of reptiles. The imbricating coastal plates in cynodonts may be analogous to the expanded ribs in certain edentates, which may represent musculoskeletal adaptation to adopt a more characteristically mammalian posture by lifting the trunk off the ground. Cynodonts are also believed to have had propulsive movements in the humerus, which are typical in mammal locomotion. The presence of both reptile and mammal features in cynodont locomotion is indicative of a transition between the two classes.
Comparison of "Galesaurus" to "Thrinaxodon".
"Galesaurus" is often compared with "Thrinaxodon", a more derived basal cynodont, because "Thrinaxodon" is the best known of all the "Epicynodonts". "Galesaurus" and "Thrinaxodon" are also very similar in morphology, are both from the early Triassic, and are both found in the Karoo Basin in South Africa. Though "Galesaurus" and "Thrinaxodon" are similar in appearance, they have a number of differences in their skulls. In "Galesaurus," the zygomatic arch height has positive allometry, which indicates that older individuals of "Galesaurus" had larger and more developed masseter muscles than in Thrinaxodon. The development of the angulation of the zygomatic arch in the adult "Galesaurus" indicates that the superficial masseter muscle also became more developed in comparison to "Thrinaxodon". Timing of the development of the posterior sagittal crest occurs later in "Galesaurus" than it does in "Thrinaxodon". The posterior sagittal crest develops in "Thrinaxodon" in the late juvenile stage, while it only appears in the adult stage of "Galesaurus." While all adult "Thrinaxodon" develop an anterior sagittal crest, the structure is absent in most "Galesaurus" specimens. The absence of the anterior sagittal crest indicates that the anterior fibers of the temporalis muscle not as developed in "Galesaurus" as they were in "Thrinaxodon." Skull width, which indicates lateral expansion of the zygomatic arches, varies between "Galesaurus" and "Thrinaxodon. Galesaurus" has a positively allometric skull width, while skull width in isometric in "Thrinaxodon." This indicates that "Galesaurus" had a more developed adductor musculature. When taking the differences in adductor musculature and the large medial shift of the mandible within the temporal fenestra, it is hypothesized that "Galesaurus" had highly developed masseters. The external occipital crest of "Galesaurus" increased during growth, though it was absent in juvenile "Thrinaxodon," and poorly developed in the adults. The size of the external occipital crest indicates enlarged, stronger nuchal muscles in "Galesaurus," but relatively weaker nuchal muscles in "Thrinaxodon. Galesaurus" also had a larger maximum skull size than "Thrinaxodon." The presence of comparatively thicker peripheral lamellar tissue in "Thrinaxodon" and excelerated ontogenetic development of the posterior sagittal crest suggests that "Galesaurus" reached sexual maturity later than "Thrinaxodon."
During ontogeny, both "Galesaurus" and "Thrinaxodon" undergo changes in posterior projection of the postorbital, posterior sagittal crest, and external occipital crest. Ontogenetic changes that were unique to "Galesaurus" include a large shift in the relative position of the mandible within the temporal fenestra, a change in the ectocranial morphology of the nasal-nasal suture, fusion of the exocciptal with three surrounding occipital bones, and development of sexual dimorphism in adults. In contrast, the ontogenetic changes that were unique to "Galesaurus" include the presence of an interpterygoid vacuity in small juveniles, change in the ectocranial trace of the frontal-parietal suture, the changing shape of the parietal foramen, and obliteration of the posterior parietal-parietal suture.