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Thrinaxodon
Thrinaxodon
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Thrinaxodon
Temporal range: Early Triassic, 251–247 Ma
Fossil of T. liorhinus in National Museum of Natural History
Diagram of skull in lateral view
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Clade: Synapsida
Clade: Therapsida
Clade: Cynodontia
Clade: Epicynodontia
Family: Thrinaxodontidae
Watson & Romer, 1956
Genus: Thrinaxodon
Seeley, 1894
Type species
Thrinaxodon liorhinus
Seeley, 1894

Thrinaxodon is an extinct genus of cynodonts which lived in what are now South Africa and Antarctica during the Early Triassic. The genus contains a single species, T. liorhinus.

Similar to other therapsids, Thrinaxodon adopted a semi-sprawling posture, an intermediary form between the sprawling position of basal tetrapods and the more upright posture present in current mammals.[1] Thrinaxodon is prevalent in the fossil record, and one of the specimens represent the oldest known record of burrowing behavior among cynodonts.[2]

Description

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Restoration

Thrinaxodon was a small synapsid roughly the size of a fox.[2] Allometric study of its skull suggests that Thrinaxodon was an omnivore.[3] It was capable of and reliant on tympanic hearing similar to hearing of extant mammals, as evidenced by the examination of its mandibular ear bones and soft-tissue eardrum based on finite element analyses.[4]

Skull

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The nasals of Thrinaxodon are pitted with a large number of foramina. The nasals narrow anteriorly and expand anteriorly and articulate directly with the frontals, pre-frontals and lacrimals; however, there is no interaction with the jugals or the orbitals. The maxilla of Thrinaxodon is also heavily pitted with foramina.[5] The arrangement of foramina on the snout of Thrinaxodon resembles that of lizards, such as Tupinambis, and also bears a single large infraorbital foramen.[5][6] As such, Thrinaxodon would have had non-muscular lips like those of lizards, not mobile, muscular ones like those of mammals.[5] Without the infraorbital foramen and its associated facial flexibility, it is unlikely that Thrinaxodon would have had whiskers.[6][7]

On the skull roof of Thrinaxodon, the fronto-nasal suture represents an arrow shape instead of the general transverse process seen in more primitive skull morphologies. The prefrontals, which are slightly anterior and ventral to the frontals exhibit a very small size and come in contact with the post-orbitals, frontals, nasals and lacrimals. More posteriorly on the skull, the parietals lack a sagittal crest. The cranial roof is the narrowest just posterior to the parietal foramen, which is very nearly circular in shape. The temporal crests remain quite discrete throughout the length of the skull. The temporal fenestra have been found with ossified fasciae, giving evidence of some type of a temporal muscle attachment.[5]

The upper jaw contains a secondary palate which separates the nasal passages from the rest of the mouth, which would have given Thrinaxodon the ability to breathe uninterrupted, even if food had been kept in its mouth. This adaptation would have allowed the Thrinaxodon to mash its food to a greater extent, decreasing the amount of time necessary for digestion. The maxillae and palatines meet medially in the upper jaw developing a midline suture. The maxillopalatine suture also includes a posterior palatine foramen. The large palatal roof component of the vomer in Thrinaxodon is just dorsal to the choana, or interior nasal passages. The pterygoid bones extend in the upper jaw and enclose small interpterygoid vacuities that are present on each side of the cultriform processes of the parasphenoids. The parasphenoid and basisphenoid are fused, except for the most anterior/dorsal end of the fused bones, in which there is a slight separation in the trabecular attachment of the basisphenoid.[5]

The skull of specimen AMNH 5630 in the American Museum of Natural History, from South Africa

The otic region is defined by the regions surrounding the temporal fenestrae. Most notable is evidence of a deep recess that is just anterior to the fenestra ovalis, containing evidence of smooth muscle interactions with the skull. Such smooth muscle interactions have been interpreted to be indicative of the tympanum and give the implications that this recess, in conjunction with the fenestra ovalis, outline the origin of the ear in Thrinaxodon. This is a new synapomorphy as this physiology had arisen in Thrinaxodon and had been conserved through late Cynodontia. The stapes contained a heavy cartilage plug, which was fit into the sides of the fenestra ovalis; however, only one half of the articular end of the stapes was able to cover the fenestra ovalis. The remainder of this pit opens to an "un-ossified" region which comes somewhat close to the cochlear recess, giving one the assumption that inner ear articulation occurred directly within this region.[5]

The skull of Thrinaxodon is an important transitional fossil which supports the simplification of synapsid skulls over time. The most notable jump in bone number reduction had occurred between Thrinaxodon and Probainognathus, a change so dramatic that it is most likely that the fossil record for this particular transition is incomplete. Thrinaxodon contains fewer bones in the skull than that of its pelycosaurian ancestors.[8]

Dentition

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Data on the dentition of Thrinaxodon liorhinus was compiled by use of a micro CT scanner on a large sample of Thrinaxodon skulls, ranging between 30 and 96 mm (1.2 and 3.8 in) in length. These dentition patterns are similar to that of Morganucodon, allowing one to make the assumption that these dentition patterns arose within Thrinaxodontidae and extended into the records of early Mammalia. Adult T. liorhinus assumes the dental pattern of the four incisors, one canine and six postcanines on each side of the upper jaw. This pattern is reflected in the lower jaw by a dental formula of three incisors, one canine and seven or eight postcanines on each side of the lower jaw. With this formula, one can make a small note that in general, adult Thrinaxodon contained anywhere between 44 and 46 total teeth.[9]

Upper incisors in T. liorhinus assume a backwards directed cusp, being curved and pointed at their most distal point, and becoming broader and rounder as they reach their proximal insertion point into the premaxilla. The fourth upper incisor is roughly homologous with a small canine tooth in form, but is positioned too far anteriorly to be a functional canine - thus ruling it out as an instance of convergent evolution. Lower incisors possess a very broad base, which is progressively reduced, heading distally towards the tip of the tooth. The lingual face of the lower incisors is most often concave while the labial face is often convex, and these lower incisors are oriented anteriorly, except in some cases for the third lower incisor, which can assume a more dorsoventral orientation. The incisors are, for the most part, single functional teeth encompassing a broad, cone-like morphology. The canines of T. liorhinus possess small dorsoventrally-directed facets on their surfaces, which appear to be involved with occlusion (dentition alignment in upper- and lower jaw closure). Each canine possesses a replacement canine located within the jaw, posterior to the existing canine, neither of the replacement or functional canine teeth possess any serrated margins only the small facets. It is important to note that the lower canine is directed almost vertically (dorsoventrally) while the upper canine is directed slightly anteriorly.[9]

Fossil in CosmoCaixa Barcelona

The upper and lower postcanines in T. liorhinus share some common features but also vary quite a fair amount in comparison to one another. The first postcanine (just posterior to the canine) is most often smaller than the other postcanines and is most often bicuspid. Including the first postcanine, if any of the other postcanines are bicuspid, then it is safe to assume that the posterior accessary cusp is present and that that tooth will not have any cingular or labial cusps. If, however, the tooth is tricuspid, then there is a chance of cingular cusps developing, if this occurs then the anterior cusp will be the first to appear and will be the most pronounced cusp. In the upper postcanines, there should be no occurrence of any teeth possessing more than three cusps, and there is no occurrence of any labial cusps on the upper postcanines. The majority of upper postcanines in the juvenile Thrinaxodon are bicuspid, while only one of these upper teeth are tricuspid. The upper postcanines of an intermediate (between juvenile and adult) Thrinaxodon are all tricuspid with no labial or cingular cusps. The adult upper postcanines retain the intermediate physiologies and possess only tricuspid teeth; however, it is possible for cingular cusps to develop in these adult teeth. The ultimate (posterior-most) upper canine is often the smallest of all canines in the entire jaw system. Little data is known of the juvenile and intermediate forms of the lower postcanines in Thrinaxodon, but the adult lower postcanines all possess multiple (any value more than three) cusps as well as the only appearance of labial cusps. Some older specimens have been found that possess no multiple-cups lower canines, possibly a response to old age or teeth replacement.[9]

Thrinaxodon shows one of the first occurrences of replacement teeth in cynodonts. This was discerned by the presence of replacement pits, which are situated lingual to the functional tooth in the incisors and postcanines. While a replacement canine does exist, more often than not it is not erupted and the original functional canine remains.[9]

Histology

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Vertebrae and ribs of specimen AMNH 9516 in the American Museum of Natural History, from Antarctica

The bone tissue of Thrinaxodon consists of fibro-lamellar bone, to a varying degree across all the separate limbs, most of which develops into parallel-fibred bone tissue towards the periphery. Each of the bones contains a large abundance of globular osteocyte lacunae which radiate a multitude of branched canaliculi. Ontogenetically early bones - mostly consisting of fibro-lamellar tissue - possessed a large amount of vascular canals. These canals are oriented longitudinally within primary osteons that contain radial anastomoses. Regions consisting mostly of parallel-fibred bone tissue contain few simple vascular canals, in comparison to the nearby fibro-lamellar tissues. Parallel-fibred peripheral bone tissue are indicative that bone growth began to slow, and they bring about the assumption that this change in growth was due to the age of the specimen in question. Combine this with the greater organization of osteocyte lacunae in the periphery of adult T. liorhinus, and we approach the assumption that this creature grew very quickly in order to reach adulthood at an accelerated rate. Before Thrinaxodon, ontogenical patterns such as this had not been seen, establishing the idea that reaching peak size rapidly was an adaptively advantageous trait that had arisen with Thrinaxodon.[10]

Within the femur of Thrinaxodon, there is no major region of the bone that is made of parallel-fibred tissues; however, there is a small ring of parallel-fibred bone within the mid-cortex. The remainder of the femur is made of fibro-lamellar tissue; however, the globular osteocyte lacunae become much more organized and the primary osteons assume less vasculature than many other bones as you begin to approach the subperiosteal surface. The femur contains very few bony trabeculae. The humerus differs from the femur in many regards, one of which being that there is a more extensive network of bony trabeculae in the humerus near the meduallary cavity of the bone. The globular osteocyte lacunae become more flattened as you get closer and closer to the midshaft of the humerus. While the vasculature is present, the humerus contains no secondary osteons. The radii and ulnae of Thrinaxodon represent roughly the same histological patterns. In contrast to the humerii and femora, the parallel-fibred region is far more distinct in the distal bones of the forelimb. The medullary cavities are surrounded by multiple layers of very poorly vascularized endosteal lamellar tissue, along with very large cavities near the medullary cavity of the metaphyses.[10]

Discovery and naming

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Two South African specimens preserved together

Thrinaxodon was originally discovered in the Lystrosaurus Assemblage Zone of the Beaufort Group of South Africa. The genoholotype, BMNH R 511, was in 1887 described by Richard Owen as the plesiotype of Galesaurus planiceps.[11] In 1894 it was by Harry Govier Seeley made a separate genus with as type species Thrinaxodon liorhinus. Its generic name was taken from the Ancient Greek for "trident tooth", thrinax and odon. The specific name is Latinised Greek for "smooth-nosed".

Thrinaxodon was initially believed to be isolated to that region. Other fossils in South Africa were recovered from the Normandien and Katberg Formations.[12] It had not been until 1977 that additional fossils of Thrinaxodon had been discovered in the Fremouw Formation of Antarctica. Upon its discovery there, numerous experiments were done to confirm whether or not they had found a new species of Thrinaxodontidae, or if they had found another area which T. liorhinus called home. The first experiment was to evaluate the average number of pre-sacral vertebrae in the Antarctic vs African Thrinaxodon. The data actually showed a slight difference between the two, in that the African T. liorhinus contained 26 presacrals, while the Antarctic Thrinaxodon had 27 pre-sacrals. In comparison to other cynodonts, 27 pre-sacrals appeared to be the norm throughout this sub-section of the fossil record. The next step was to evaluate the size of the skull in the two different discovery groups, and in this study they found no difference between the two, the first indication that they may in fact be of the same species. The ribs were the final physiology to be cross-examined, and while they portrayed slight differences in the expanded ribs, against one another, the most important synapomorphy remained consistent between the two, and that was that the intercostal plates overlapped with one another. These evaluations led to the conclusion that they had not found a new species of Thrinaxodontidae, but yet they had found that Thrinaxodon occupied two different geographical regions, which today are separated by an immense expanse of ocean. This discovery was one of many to support the idea of a connected land mass, and that during the early Triassic, Africa and Antarctica must have been linked in some way, shape or form.[13]

Classification

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Reconstructed jaw adductor musculature

Thrinaxodon belongs to the clade Epicynodontia, a subdivision of the greater clade Cynodontia. Its closest relative based on phylogenetic analyses is Platycraniellus.[14]

Theriodontia

Paleobiology

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Ontogeny

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There appear to be nine cranial features that successfully separate Thrinaxodon into four ontogenetic stages. The paper denotes that in general, the Thrinaxodon skull increased in size isometrically, except for four regions, one of which being the optic region. Much of the data assumes that the length of the sagittal crest increased at a greater rate in relation to the rest of the skull. The posterior sagittal crest to appear in an earlier ontogenetic stage than the more anterior crest had, and in conjunction with the dorsal deposition of bone, a unified sagittal crest had developed rather than having a single suture span the entire length of the skull.[3]

The bone histology of Thrinaxodon indicates that it most likely had very rapid bone growth during juvenile development, and much slower development throughout adulthood, giving rise to the idea that Thrinaxodon reached peak size very early in its life.[10]

There is strong evidence that juvenile Thrinaxodon were cared for by their parents, as evidenced by fossilised aggregations of adults with multiple juvenile individuals of a similar size, likely indicating these juveniles were the same age and belonged to the same clutch.[15]

Posture

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The posture of Thrinaxodon is an interesting subject, because it represents a transition between the sprawling behavior of the more lizard-like pelycosaurs and the more upright behavior found in modern, and many extinct, Mammalia. In cynodonts such as Thrinaxodon, the distal femoral condyle articulates with the acetabulum in a way that permits the hindlimb to present itself at a 45-degree angle to the rest of the system. This is a large difference in comparison to the distal femoral condyle of pelycosaurs, which permits the femur to be parallel with the ground, forcing them to assume a sprawling-like posture.[1] More interesting is that there is an adaptation that has only been observed within Thrinaxodontidae, which allows them to assume upright posture, similar to that of early Mammalia, within their burrows.[2] These changes in posture are supported by the physiological changes in the torso of Thrinaxodon. Such changes as the first appearance of a segmented rib compartment, in which Thrinaxodon expresses both thoracic and lumbar vertebrae. The thoracic segment of the vertebrae contain ribs with large intercostal plates that most likely assisted with either protection or supporting the main frame of the back. This newly developed arrangement allowed for the appropriate space for a diaphragm, however, without proper soft tissue records, the presence of a diaphragm is purely speculative.[16]

Burrowing

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CT image of specimen in burrow

Thrinaxodon has been identified as a burrowing cynodont by numerous discoveries in preserved burrow hollows. There is evidence that the burrows are in fact built by the Thrinaxodon to live in them, and they do not simply inhabit leftover burrows by other creatures. Due to the evolution of a segmented vertebral column into thoracic, lumbar and sacral vertebrae, Thrinaxodon was able to achieve flexibilities that permitted it to comfortably rest within smaller burrows, which may have led to habits such as aestivation or torpor. This evolution of a segmented rib cage suggests that this may have been the first instance of a diaphragm in the synapsid fossil record; however, without the proper soft tissue impressions this is nothing more than an assumption.[16][2]

3D reconstruction of a Thrinaxodon liorhinus skeleton found in the same burrow with a Broomistega amphibian (synchrotron imaging)[17]

The earliest discovery of a burrowing Thrinaxodon places the specimen found around 251 million years ago, a time frame surrounding the Permian–Triassic extinction event. Much of these fossils had been found in the flood plains of South Africa, in the Karoo Basin. This behavior had been seen at a relatively low occurrence in the pre-Cenozoic, dominated by therapsids, early-Triassic cynodonts and some early Mammalia. Thrinaxodon was in fact the first burrowing cynodont that has been found, showing similar behavioral patterns to that of Trirachodon. The first burrowing vertebrate on record was the dicynodont synapsid Diictodon, and it is possible that these burrowing patterns had passed on to the future cynodonts due to the adaptive advantage of burrowing during the extinction. The burrow of Thrinaxodon consists of two laterally sloping halves, a pattern that has only been observed in burrowing non-mammalian Cynodontia. The changes in vertebral/rib anatomy that arose in Thrinaxodon permit the animals to a greater range of flexibility, and the ability to place their snout underneath their hindlimbs, an adaptive response to small living quarters, in order to preserve warmth and/or for aestivation purposes.[2]

A Thrinaxodon burrow contained an injured temnospondyl, Broomistega. The burrow was scanned using a synchrotron, a tool used to observe the contents of the burrows in this experiment, and not damage the intact specimens. The synchrotron revealed an injured rhinesuchid, Broomistega putterilli, showing signs of broken or damaged limbs and two skull perforations, most likely inflicted by the canines of another carnivore. The distance between the perforations was measured in relation to the distance between the canines of the Thrinaxodon in question, and no such relation was found. Therefore, we may assume that the temnospondyl found refuge in the burrow after a traumatic experience and the T. liorhinus allowed it to stay in its burrow until they both ultimately met their respective deaths. Interspecific shelter sharing is a rare anomaly within the fossil record; this T. liorhinus shows one of the first occurrences of this type of behavior in the fossil record, but it currently is unknown if the temnospondyl inhabited the burrow before or after the death of the nesting Thrinaxodon.[18]

See also

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References

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Thrinaxodon liorhinus is an extinct species of small, carnivorous cynodont therapsid that lived during the period, approximately 251 million years ago, shortly after the Permian-Triassic mass extinction. Known primarily from the Assemblage Zone of the Basin in and similar deposits in , it measured about 50 cm in length and weighed roughly 1-2 kg, comparable to a modern house cat. This basal cynodont is notable for its transitional features between reptiles and mammals, including a well-developed secondary bony and a double occipital condyle, as well as evidence of burrowing behavior that likely contributed to its survival in a recovering . With over two dozen well-preserved specimens documented, Thrinaxodon provides critical insights into the early radiation of synapsids and the origins of mammalian traits. Its diet consisted of small , , and other prey, supported by a featuring sharp incisors, prominent canines, and multi-cusped postcanines adapted for piercing and shearing. The inhabited warm, temperate environments with seasonal rainfall and flooding, possibly wooded swamplands, where its adaptations—such as robust forelimbs with high torsion and strong pronator muscles—enabled it to dig burrows for shelter and possibly . Evolutionary studies highlight Thrinaxodon's role as a link between Late Permian procynodonts and more advanced mammaliamorphs, with cranial morphology showing ontogenetic changes like the development of a transverse nasal-frontal suture and increased ossification in adults. Bone tissue analysis reveals fibrolamellar bone indicative of rapid juvenile growth rates, transitioning to slower parallel-fibered bone in maturity, suggesting ectothermic to mesothermic metabolic shifts and determinate growth patterns akin to those in mammals. Additionally, its presence across Gondwanan continents underscores the biogeographic connections before continental drift, aiding reconstructions of early Mesozoic paleogeography.

Description

Skull

The skull of Thrinaxodon liorhinus is elongated and narrow, with adult specimens reaching basal lengths of up to 96 mm, though total skull length typically measures around 8-10 cm from the premaxillary tip to the . This shape reflects a transitional morphology between reptilian synapsids and mammals, characterized by a developing secondary formed primarily by the maxillae and , which partially separates the nasal passages from the oral cavity, remaining open along the midline, and extends posteriorly to near the level of the last postcanine teeth. The secondary includes a long incisivum anteriorly and is perforated by small posterior palatal foramina approximately 2 mm in length, enhancing respiratory efficiency during mastication—a feature absent in more basal therapsids but retained and refined in advanced cynodonts. Key cranial elements include two pairs of temporal fenestrae: a lateral bordered by the postorbital, squamosal, and jugal, and an infratemporal fenestra below the , both accommodating expanded adductor musculature such as the temporalis, which originated from an spanning the fenestrae. The braincase is enlarged relative to basal cynodonts, with the occupying about 42% of the total length and featuring a prominent that represents the widest region of the , indicating early encephalization trends toward mammalian levels; however, ventral remains incomplete, leaving gaps between the basisphenoid and basioccipital. The postorbital bar is reduced and slender in adults, formed by the postorbital and jugal bones with partial overlap from the prefrontal, while the are robust and laterally flared, broader in presumed males to support larger masseter muscles. Sensory structures emphasize enhanced visual capabilities, with large orbits (slower-growing relative to the snout during ) positioned for partially forward-facing eyes that likely supported , their anterior walls formed by the extending to the third upper postcanine. A small pineal , approximately 4 mm long and oval-shaped, perforates the midline between the frontals and parietals on the skull roof, possibly housing a organ. The jaw articulates at a shallow within a of the squamosal , where the quadrate fits loosely but stably, bridging reptilian quadrate-squamosal joints toward the mammalian dentary-squamosal configuration through a developing reflected lamina on the angular process. Interorbital width is constricted relative to the broader temporal region in mid-sized adults.

Dentition

Thrinaxodon exhibited heterodont dentition, characterized by distinct tooth types adapted for different functions in feeding. The incisors were simple, sharp, and conical, suited for nipping and grasping prey, while the canines were enlarged and piercing, facilitating the capture and dispatch of small animals. Postcanine teeth were multi-cusped, featuring a main sectorial cusp accompanied by smaller accessory cusps and a lingual cingular collar, enabling shearing of food items. The dental formula in adult Thrinaxodon liorhinus averaged 4/3 incisors, 1/1 canines, and 6/7–8 postcanines (upper/lower), though variation occurred across individuals and ontogenetic stages. Tooth replacement followed an alternating pattern, with postcanines showing posterior-to-anterior waves in the and evidence of up to three replacements per locus in juveniles; this process slowed in adults, where anterior postcanines were often not replaced, leading to a reduction in tooth row length over time. Incisors underwent sequential replacement, more frequent in medium-sized individuals, while canines showed dual replacement sites in small juveniles. Jaw mechanics in Thrinaxodon featured limited occlusion, with lower postcanines positioned lingually to the uppers and lacking consistent contact between opposing teeth, a condition linked to the alternating replacement pattern that prevented fixed alignment. This arrangement represented an early stage in the of mammalian , with multi-cusped postcanines serving as precursors to tribosphenic dentition through enhanced shearing capabilities. Tooth morphology and sectorial postcanines indicate a carnivorous diet incorporating insectivory and consumption of small vertebrates, supported by the sharp, gripping incisors and canines alongside shearing postcanines. Wear patterns, including striations on postcanine surfaces, further suggest processing of tough, fibrous foods mixed with softer prey items.

Postcranial skeleton

The postcranial skeleton of Thrinaxodon exhibits transitional features between reptilian and mammalian conditions, particularly in its axial and appendicular elements, which supported a semi-sprawling while allowing enhanced flexibility for locomotion and potential burrowing activities. The vertebral column comprises approximately 26–27 presacral vertebrae, typically divided into seven cervical, 13 thoracic, and seven , reflecting a regional differentiation that improved axial mobility compared to more basal synapsids. are reduced to thin, platelike structures with minimal overlap and a small hemicircular near the tuberculum, reducing interference with movement. The region demonstrates increased flexibility through robust yet non-synostosed , interlocking costal plates, and imbrication that permits lateral flexure and undulation, facilitating agile body movements. The limb girdles show adaptations toward a more upright posture. The lacks a distinct process, with a high narrow that enhances stability and supports the deltoideus musculature, though it remains underdeveloped relative to later cynodonts. The ilium is elongated, with a thin, moderately expanded that contacts up to five sacral vertebrae and exhibits anterodorsal expansion to accommodate , indicating a shift from sprawling to a more parasagittal stance. In the , the retains a primitive entepicondylar for the passage of nerves and vessels, while the itself is robust with a distinct shaft; the is similarly sturdy, featuring a bulbous head and moderate expansion, both contributing to efficiency in a semi-sprawling configuration where limbs splay at approximately 45 degrees from the body axis. The manus follows a phalangeal of 2-3-4-4-3, characteristic of non-mammalian therapsids, with elongated proximal phalanges supporting grasping and capabilities. The is notably narrow, formed by closely spaced thoracic ribs with imbricating costal plates that create a medial channel, enhancing structural integrity without excessive rigidity. are absent, a condition typical of advanced cynodonts that distinguishes them from earlier reptiles and allows greater ventral flexibility. This arrangement, combined with an enlarged muscle system and gradual zygapophyseal reorientation, improves thoracic mobility, permitting expanded respiratory excursions and lateral bending essential for burrowing adaptations. Ontogenetic changes in limb proportions, such as relative elongation of the and in juveniles, further underscore the skeleton's developmental plasticity.

Geological context

Stratigraphy

Thrinaxodon fossils are primarily known from the Assemblage Zone (LAZ) of the Beaufort Group in the Basin of , which forms part of the Tarkastad Subgroup and encompasses the upper Palingkloof Member and lower Katberg Formation. This zone represents the earliest ( stage) terrestrial deposits, immediately following the Permian- boundary dated to approximately 251.9 Ma. of ash beds within the lower LAZ, using U-Pb CA-ID-TIMS on zircons, yields ages around 252.24 ± 0.11 Ma near the base, confirming the zone's position spanning the latest Permian into the early , though Thrinaxodon occurrences are confined to post-boundary strata. The genus appears in floodplain mudstones and siltstones characteristic of the LAZ, which indicate low-energy depositional environments with periodic flooding and rubified paleosols suggesting a warmer, possibly more arid post-extinction. Many specimens, including articulated skeletons, are preserved in these fine-grained sediments, often within structures that highlight the animal's habits and rapid post-extinction recolonization of habitats. Thrinaxodon co-occurs with the eponymous dicynodont in these assemblages, underscoring its role in the initial wave of terrestrial vertebrate recovery. Although some early cynodont referrals extend into the overlying Cynognathus Assemblage Zone, Thrinaxodon itself is restricted to the LAZ, representing a short-lived genus that persisted for approximately 1-2 million years after the Permian . This brief temporal range aligns with the lower LAZ's estimated duration in the early , before faunal turnover led to more diverse assemblages.

Geographic distribution

Thrinaxodon fossils are primarily known from the Karoo Basin in , where over 100 specimens have been collected, making it one of the most abundantly represented basal cynodonts in the Early Triassic record of . These finds occur across multiple localities within the basin, highlighting its prevalence in post-extinction recovery faunas of the southern supercontinent. In contrast, Antarctic discoveries are far scarcer, with approximately 16 specimens recovered from the Fremouw Formation in the , representing some of the highest paleolatitude (around 70° S) remains from the . Confirmed Thrinaxodon fossils are restricted to and , underscoring the genus's distribution across the southern during the , spanning areas now separated by approximately 10,000 km due to . In sites, Thrinaxodon constitutes a notable component of small assemblages, comprising up to 3% of overall specimens in the declivis Assemblage Zone but potentially higher locally in cynodont-rich horizons. Elsewhere, such as in , it is rarer, reflecting either lower preservation potential or patchier distribution in high-latitude environments. This pattern informs reconstructions of continental configurations, illustrating how Thrinaxodon contributed to the recolonization of diverse Gondwanan landscapes following the end-Permian mass extinction.

Discovery and nomenclature

Initial finds

The first fossils attributable to Thrinaxodon were collected in during the late 19th century from the Karoo Basin. In 1887, described a partial (BMNH R 511) as a plesiotype of the cynodont Galesaurus planiceps, collected from deposits near in the . Harry Govier Seeley recognized the distinctiveness of this material in 1894 and erected the genus Thrinaxodon with the species T. liorhinus, distinguishing it from Galesaurus based on cranial features such as the elongated and reduced temporal fenestrae. In 1911, provided a detailed description of the structure in cynodont reptiles, including a specimen he referred to as Galesaurus planiceps, emphasizing its mammalian-like features such as the secondary and ; this material was later synonymized with Thrinaxodon liorhinus. Key early 20th-century specimens included isolated and partial skeletons from surface prospecting in outcrops, often exposed in workings of the Beaufort Group. By , and others collected additional material, including well-preserved that formed the basis for subsequent anatomical studies. Articulated skeletons emerged from South African excavations in the mid-20th century, notably during the 1947 African Expedition, which yielded multiple complete individuals from nodule-bearing horizons in the Assemblage Zone near , providing insights into postcranial anatomy. Further digs in the , led by institutions like the South African Museum, uncovered clusters of associated skeletons, highlighting Thrinaxodon's abundance in post-extinction recovery faunas. Collection methods typically involved manual surface prospecting and careful extraction from weathered exposures, preserving delicate bones in fine-grained shales. Expeditions to Antarctica in the 1970s expanded the known distribution of Thrinaxodon, with partial skeletons discovered in the Fremouw Formation of the Transantarctic Mountains during U.S. Geological Survey field seasons. These finds, including limb elements and vertebrae from sites like Graphite Peak, confirmed a bipolar Gondwanan range and were collected via systematic prospecting in remote nunataks under harsh polar conditions. In recent decades, modern techniques such as high-resolution CT scanning have been applied to key specimens, revealing internal cranial anatomy like the braincase and inner ear structures that were previously inaccessible without destructive preparation.

Etymology and species

The genus name Thrinaxodon derives from the Greek words thrinax, meaning or three-pronged tool, and odon, meaning , referring to the trident-like structure of the postcanine teeth. The name was coined by Harry Govier Seeley in 1894 to describe a new cynodont based on cranial material from the Basin of . The is T. liorhinus, originally described by Seeley in 1894 based on the skull (BMNH R. 511), with a detailed description provided by Sidney H. Haughton in 1924. This is known from numerous specimens, primarily from , representing a small, carnivorous cynodont approximately 40–50 cm in length. Antarctic fossils from the Fremouw Formation, initially considered potentially distinct, have been referred to T. liorhinus following revisions that emphasized morphological consistency across Gondwanan deposits. Early taxonomic work led to the referral of several related taxa to Thrinaxodon, including species previously classified under Pachygenelus and Galesaurus, due to similarities in cranial and dental features. However, 1970s revisions, notably by Van Heerden (1976), resolved many junior synonyms (such as Nythosaurus larvatus and Glochinodon gracilis) as ontogenetic variants or conspecific with T. liorhinus, solidifying its status as the sole valid South African species. Material from the Upper Santa Maria Formation of was originally named as a second species, T. brasiliensis, in 1987, but was reclassified in 2001 as the type species of the distinct genus Prozostrodon due to differences in postcranial proportions, dental morphology, and phylogenetic position.

Classification

Position within Cynodontia

Thrinaxodon is classified within the family Thrinaxodontidae, a group of basal epicynodont cynodonts that represents an early divergence near the base of . This family is characterized by several key synapomorphies that distinguish it from earlier cynodonts, including the development of a complete osseous secondary formed by the maxillae and , an expanded with a deepened masseteric fossa for enhanced jaw musculature, and a reduced contribution of the squamosal to the , reflecting progressive mammalianization of the skull. These features position Thrinaxodontidae as the sister clade to , the more crownward group encompassing advanced non-mammaliaform cynodonts and . Recent phylogenetic analyses using 3D imaging technologies, such as those by Pusch et al. (2024), recover Thrinaxodon in a with Nanictosaurus and Platycraniellus, outside , highlighting the instability of early cynodont interrelationships but affirming its basal epicynodont position through shared derived traits like postcanine occlusion. Earlier cladograms, such as those in Hopson and Kitching (2001), depict Thrinaxodon as a basal form before the eucynodont radiation, supported by 96 cranial and dental characters across 32 taxa. More recent studies, including Huttenlocker and Sidor (2020) using 111 characters from 25 therapsids, reinforce this placement, often showing polytomies among epicynodonts where Thrinaxodon clusters with other basal forms in strict consensus trees. Within Gondwanan Early Triassic deposits, Thrinaxodon is coeval with close relatives such as Platycraniellus, which shares similar basal epicynodont affinities and temporal distributions in South African and strata. Platycraniellus, in particular, often emerges as a direct sister taxon to Thrinaxodon or to in cladograms, underscoring the familial cohesion of Thrinaxodontidae.

Evolutionary significance

Thrinaxodon represents a crucial transitional form in the evolution of synapsids toward , exhibiting early precursors to mammalian dental replacement patterns. In Thrinaxodon, postcanine teeth are replaced in a manner that foreshadows diphyodonty, with successors emerging directly beneath predecessors in a caudal-to-rostral sequence, contrasting with the replacement of more basal synapsids and approaching the single juvenile-to-adult replacement seen in early mammals. Additionally, microtomographic analyses of its indicate the absence of ossified turbinal structures, suggesting that if present, non-ossified precursors supported away from primary respiratory airflow, indicating an evolutionary shift toward specialized sensory capabilities in cynodonts. Thrinaxodon's configuration further underscores this transition, with the quadrate and articular bones still integrated into the jaw mechanism but showing incipient detachment and enlargement of the , facilitating the dual role of mastication and audition that fully separates in . Following the Permian-Triassic mass extinction, Thrinaxodon played a pivotal role in the recovery of terrestrial vertebrate faunas, becoming one of the most abundant small-bodied carnivores in the earliest Lystrosaurus Assemblage Zone of the Basin, where it contributed to the rebound of cynodont diversity amid low overall taxonomic richness. Its persistence across the extinction boundary, from late Permian to deposits in and , highlights adaptive strategies that enabled survival and proliferation in post-extinction ecosystems characterized by environmental instability. This abundance provides critical insights into the delayed recovery phase, where Thrinaxodon-like forms helped repopulate niches vacated by larger herbivores and predators. Comparatively, Thrinaxodon shares advanced jaw adductor musculature with early mammaliaforms like , including an expanded masseter and temporalis complex that enhanced bite efficiency through increased , yet it retained reptilian traits such as a sprawling limb posture that limited terrestrial agility compared to the more upright stance of later forms. These shared cranial features, such as the reconfiguration of adductor origins onto the dentary, illustrate a where mammalian innovations in feeding mechanics preceded full locomotor shifts. In contemporary research, Thrinaxodon serves as a model for investigating the onset of endothermy in synapsids, with histology and growth patterns suggesting partial metabolic elevation that supported activity in variable post-extinction climates, bridging ectothermic therapsids and fully endothermic mammals. Its well-preserved has also informed studies on sensory evolution, revealing enlarged olfactory bulbs and pathways that prefigure mammalian enhancements in chemosensation and somatosensation.

Paleobiology

Growth and ontogeny

Thrinaxodon liorhinus exhibited significant size variation throughout its , with basal lengths (BSL) ranging from approximately 30 mm in juveniles to 96 mm in adults, based on a growth series of 68 cranial specimens. Total body in adults reached about 50 cm, while juveniles were roughly 37% of adult size. growth occurred primarily through rapid periosteal deposition of fibro-lamellar tissue in early stages, transitioning to slower parallel-fibred in outer cortices of larger elements, indicating sustained but decelerating expansion. Ontogenetic shifts were prominent in cranial morphology and . Juvenile skulls (BSL ≤ 42 mm) featured bicuspid and tricuspid upper postcanines with cingular cusps, paired interpterygoid vacuities, and an inverted V-shaped nasal-frontal suture; these transitioned in subadults and adults to monocuspid postcanines, absent vacuities (by BSL ≥ 56 mm), a transverse nasal-frontal suture, and development of sagittal and occipital crests (starting at BSL ≥ 42 mm and ≥ 61 mm, respectively). Tooth replacement patterns also varied: incisors replaced more slowly in immatures (BSL ≤ 56 mm) but accelerated in adults (BSL ≥ 75 mm), while canines showed faster replacement in early juveniles (BSL ≤ 42 mm) and slower rates later. These changes reflect positive in the snout, , and temporal regions, with negative in orbits. Growth rates were rapid during early , as evidenced by fibro-lamellar deposition, but slowed with age, potentially coinciding with ; lines of arrested growth (LAGs) were generally absent, except for a single annulus in one near-adult , suggesting minimal disruption from seasonal environmental stresses, possibly due to burrowing . microstructure displayed inter-elemental variation, with faster growth in propodials than epipodials. Evidence for in Thrinaxodon is unconfirmed, with no clear differences in canine size or other traits observed across specimens, including paired associations; variation in features like development appears individualistic rather than dimorphic.

Locomotion and posture

Thrinaxodon exhibited a quadrupedal inferred from its postcranial , with limb postures transitional between those of earlier sprawling therapsids and more advanced mammalian forms. The forelimbs adopted a semi-sprawling configuration, characterized by abduction of the and limited protraction, while the hindlimbs were more upright, approaching a parasagittal alignment that enhanced locomotor efficiency. Recent analyses confirm high lateroflexion in the anterior vertebral column but reduced in the posterior, supporting transitional flexibility; possible eucynodont trackways from ~247 Ma suggest quadrupedal s. Skeletal mechanics indicate that humeral rotation in Thrinaxodon was restricted to approximately 45–60 degrees, constraining mobility compared to fully sprawling reptiles but allowing greater stability during movement. This intermediate posture is evidenced by the morphology of the and humeral head, which supported a crouched stance with the elbows directed posteriorly. Rare ichnofossils attributable to early cynodonts, including possible Thrinaxodon-like forms, suggest a quadrupedal walking pattern, though direct trackways for Thrinaxodon remain scarce. The vertebral column of Thrinaxodon featured moderate spinal flexibility, with an arched thoracic region providing stability during locomotion and a that likely aided in balance by counteracting lateral shifts in body mass. This configuration represents an evolutionary intermediate: fully sprawling postures in proterosuchids relied on extensive lateral undulation, whereas advanced cynodonts evolved more rigid, parasagittal s for faster, energy-efficient travel. Ontogenetically, juvenile specimens show proportionally longer limbs that may have facilitated initial improvements in stability.

Burrowing behavior

Thrinaxodon liorhinus exhibits a lifestyle inferred from multiple articulated skeletons preserved within burrow casts from sediments of the Basin, . These taphonomic structures, dating to approximately 251 million years ago, consist of partial casts featuring a terminal living chamber connected to a narrower access shaft, with vaulted ceilings and double-sloping floors often infilled by fine-grained sandstones from flood events. The curled-up posture of the skeletons, showing signs of post-mortem , indicates that individuals died while using these burrows as refuges. Anatomical features support active burrowing behavior, including robust forelimbs with skeletal configurations transitional between reptilian sprawling and mammalian parasagittal postures, enabling effective excavation. Low parallel ridges observed on the sides and ceilings of casts represent scratch marks from , while the absence of such marks on floors suggests during occupation. These adaptations allowed Thrinaxodon to construct or modify burrows, with preserved systems up to approximately 35 cm in length. Ecologically, these burrows likely served solitary or family groups for predator avoidance and amid the harsh post-Permian-Triassic environment, as evidenced by aggregations including adults with juveniles preserved together. Such behavior may have contributed to Thrinaxodon's survival, with multiple juveniles found in shared burrow systems suggesting possible .

Physiological adaptations

histology in Thrinaxodon reveals a predominance of fibro-lamellar bone tissue with highly vascularized canals, particularly in juveniles, indicating rapid early growth rates that slowed in adulthood. This tissue type, characterized by woven-parallel complexes and longitudinally oriented vascular canals in larger individuals, supports elevated metabolic rates consistent with partial endothermy, as such microstructures are associated with sustained high-energy demands in synapsids. Lines of arrested growth (LAGs) are generally absent or infrequent, suggesting uninterrupted growth unaffected by strong seasonal constraints, further aligning with physiological traits bridging reptilian and mammalian patterns. Sensory evolution in Thrinaxodon is evidenced by enlarged olfactory bulbs in endocranial reconstructions, which occupy a significant portion of the cavity and indicate enhanced olfaction for detecting prey or environmental cues in low-oxygen post-extinction settings. The features prolific trigeminal canal branching with up to 16 , concentrated rostrally, suggesting advanced facial tactile sensitivity possibly via proto-whisker pads that transmitted sensory information to the . Additionally, the exhibits an intermediate morphology with a gracile structure, ovoid , and variable crura, representing a transitional stage in middle ear evolution from inertial to impedance-matching hearing systems seen in mammals. Respiratory traits in Thrinaxodon include inferences of a proto-diaphragm derived from musculature, enabling more efficient pulmonary ventilation than in earlier synapsids, as supported by the differentiation of thoracic and regions in the vertebral column. Broad, overlapping with specialized attachments facilitated this thoraco-abdominal separation, allowing expanded capacity and improved gas exchange during the oxygen-poor atmosphere. Thermoregulation in Thrinaxodon likely involved burrow-sharing behaviors for buffering environmental extremes, as evidenced by articulated skeletons preserved in communal burrows, which would have stabilized body temperature in fluctuating post-Permian climates. Fur-like insulation is inferred but debated, based on cranial foramina patterns suggesting whisker-bearing pelage, though direct skin impressions are absent; metabolic rates, estimated from bone vascularity, were elevated approximately 2-4 times above reptilian baselines, aiding heat retention.

References

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