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Bulbasaurus
Temporal range: Tropidostoma Assemblage Zone, Lopingian
Photograph and diagram of holotype skull
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Clade: Synapsida
Clade: Therapsida
Clade: Anomodontia
Clade: Dicynodontia
Family: Geikiidae
Genus: Bulbasaurus
Kammerer & Smith, 2017
Type species
Bulbasaurus phylloxyron
Kammerer & Smith, 2017

Bulbasaurus (meaning "bulbous reptile") is an extinct genus of dicynodont that is known from the Lopingian epoch of the Late Permian period of what is now South Africa, containing the type and only species B. phylloxyron. It was formerly considered as belonging to Tropidostoma; however, due to numerous differences from Tropidostoma in terms of skull morphology and size, it has been reclassified the earliest known member of the family Geikiidae, and the only member of the group known from the Tropidostoma Assemblage Zone. Within the Geikiidae, it has been placed close to Aulacephalodon, although a more basal position is not implausible.

Bulbasaurus was ostensibly not directly named after the Pokémon Bulbasaur, but rather after its nasal bosses, which are unusually bulbous among geikiids; however, the describers noted that the similarity in name "may not be entirely coincidental." Additionally, the specific name of the type species means "leaf razor", which is most directly a reference to its keratin-covered jaws. Other distinguishing characteristics of Bulbasaurus among the geikiids include the hook-like beak, very large tusks, and absence of bossing on the prefrontal bone.

Discovery and naming

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Holotype skull of Bulbasaurus as it was found in situ

The holotype specimen of Bulbasaurus was found by Roger M.H. Smith in the Vredelus locality, which is located at an altitude of 1,445 metres (4,741 ft), in the district of Fraserburg, Northern Cape, South Africa. This locality is part of what is known as the Tropidostoma Assemblage Zone, which belongs to the Lopingian (upper Permian) Hoedemaker Member of the Middle Teekloof Formation. The Tropidostoma AZ is named after the oudenodontid Tropidostoma, which occurs commonly at the site. The holotype itself, which is catalogued as SAM-PK-K11235, is a partially complete skull that is missing the left subtemporal and both postorbital bars. It was discovered lying right-side-up in a bed of grey siltstone with embedded micrite nodules, and there were no associated remains from the rest of the skeleton.[1] "Head-only" preservation is common in therapsid fossils of the Hoedemaker Member, because the specimens were probably left out in the open and became disarticulated before being rapidly buried by flash floods.[2]

Other referred specimens include the nearly-complete skull CGP/1/938 (from the Wilgerbosch Kloof locality in Fraserburg), the complete skull CGP/1/949 (also from Wilgerbosch Kloof), the complete skull with associated lower jaws and postcranial remains CGP/1/970 (from the Blaauwkrans locality in Beaufort West, Western Cape), the complete but crushed skull CGP/1/2263 (locality unknown), the crushed skull with lower jaws SAM-PK-K10106 (from the Paalhuisberg locality in Beaufort West), and the complete juvenile skull with lower laws SAM-PK-K10587 (from the Doornhoek locality in Beaufort West). All of these specimens are either held at the Iziko Museums in Cape Town or the Council for Geoscience in Praetoria. Before being referred to the new genus Bulbasaurus, they were initially treated as specimens of Tropidostoma in collections.[1]

Bulbasaurus was described by Christian Kammerer and Smith in 2017. The description states that the generic name combines the Latin bulbus, referring to the very large and bulbous nasal bosses, with the common suffix -saurus. As for the specific name phylloxyron, meaning literally "leaf razor", it is derived from the Greek phyllos and xyron, and apparently refers to the keratinous covering on the premaxilla, maxilla, and palate that would have been used to shear plant material.[1] Thus, as published, the name of Bulbasaurus does not directly refer to Pokémon, or specifically the similarly-named Bulbasaur. However, Kammerer noted that "if one wished to read between the lines concerning certain similarities, I wouldn't stop them",[3] and later added that "similarities between this species and certain other squat, tusked quadrupeds may not be entirely coincidental."[4]

Description

[edit]

Premaxilla, maxilla, and palate

[edit]
Holotype skull of Bulbasaurus viewed from below

At the front of the upper jaw of Bulbasaurus, the tips of the fused premaxillae are strongly hook-like, much more so than Tropidostoma and other dicynodonts[1] but not as much as Dinanomodon.[5] Also unlike Tropidostoma, the flattened front face of the premaxillae bear a tall, narrow, prominent ridge; Aulacephalodon also has a similar ridge, albeit broader and not as sharp. The back of the premaxillae narrow and extend between the roughened bosses on the nasal bones. Viewed from underneath, the bone is roughly pentagonal; the bottom surface bears two ridges near the front, as well as an additional ridge extending backward from where the two forward ridges end, which gradually becomes taller and wider. These ridges are separated by depressions in the bone of roughly equal depth, which is like other geikiids but unlike Tropidostoma. At the outer extremities of the premaxillae, low and roughened ridges are located near the base of the tusks.[1]

Further back on the interior of the upper jaw, the palatine bones are exposed as a palatine pad, which is very roughened and would have been covered in keratin, although the portion where they contact the premaxillae is smooth and sloping. The back portion of the palatines are thinner than the rest of the bone, but it is still thicker than that of either Tropidostoma or Oudenodon, instead resembling Aulacephalodon more closely. The pterygoid bones are robust in contrast to Tropidostoma, and bear ridges that converge into a tall, blade-like process known as the crista oesophagea. The pterygoids also project outwards in rod-like structures to meet the quadrate bones.[1]

Compared to other dicynodonts, the maxillary tusk of Bulbasaurus was massive; the holotype skull, which is 14 cm (5.5 in) long, has a 1.9 cm (0.75 in) tusk diameter. Only Aulacephalodon has comparably large tusks proportionally, but these belong to adult specimens much larger than Bulbasaurus (in juveniles the size of Bulbasaurus, the tusks are still erupting).[6] The root of the tusk bulges outwards from the surface of the maxilla due to its large size. Extensive pitting on the surface of the maxilla is suggestive of some kind of keratinous covering, which has also been inferred for other dicynodonts.[7] Unlike other geikiids and most other cryptodontian dicynodonts, there is no ridge behind the tusk, although mature Aulacephalodon also lack this ridge.[1]

Nasal and orbital rim

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Holotype skull of Bulbasaurus viewed from above

The nasal bones, which form the roof the snout, bear a pair of enlarged bosses of bone as in other cryptodontians.[8] In contrast to the small, oval-shaped, relatively narrow, and smooth-textured bosses of Tropidostoma, the roughened bosses of Bulbasaurus are very large and nearly form a single continuous boss (although a narrow strip of the premaxilla extends backwards between the bosses). Aulacephalodon and Pelanomodon also have large and roughened bosses, but they are separated in part by the nasals. At the back of the bosses, a slight indentation wrapping around the top and sides of the skull separates them from the eye socket, typical of cryptodontians except for Odontocyclops.[9] The suture between the nasals and the frontal bones is slightly raised relative to the rest of the skull; the same raised suture is also seen in Aulacephalodon and Pelanomodon.[1]

Typical of geikiids, the interorbital region between the eyes was quite broad. The lacrimal bones, prefrontal bones, frontal bones, and jugal bones form the margin of the eye socket, with the portion comprised by the lacrimals having an orbital ridge that is better-developed and more raised. Unlike other cryptodontians, there is no evidence of a second set of bosses on the prefrontals, although their surfaces are somewhat thickened. A relatively deep midline depression (mildly developed in Tropidostoma and Oudenodon, but absent in other geikiids) is visible on the frontals, which are situated largely between the eyes and form roughened edges where they contributes to the rims of the eye sockets. There appears to be no separation of the postfrontal bones from the frontals, which is probably an adult characteristic as in Aulacephalodon. The elongate jugals form part of the zygoma, or bony cheek, and ends at the temporal fenestra. It also forms part of the temporal and postorbital bars; Pelanomodon differs from Bulbasaurus in having small bosses on the latter portions of the jugals.[1][10]

Postorbital skull

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Holotype skull of Bulbasaurus viewed from behind

Most of the postorbital bar is made up of the postorbital bones, which are very robust relative to other cryptodontians as in other geikiids. However, compared to other geikiids, the postorbital bar of Bulbasaurus is relatively smooth and free of bosses. The sides of the postorbitals, which would have anchored jaw musculature, are very concave. Near the back, the postorbitals curve and converge to form a somewhat pinched intertemporal bar that overlaps the parietal bones to varying extents. The squamosal bones also contribute to the postorbital bar; its back edge along the postorbital bar is somewhat twisted in Bulbasaurus, which is seen in other cryptodontians but is taken to an extreme by Aulacephalodon and Pelanomodon, where the bone has become entirely twisted such that the interior faces outwards. Projections of the squamosal bones partially surround the posttemporal fenestrae on the rear of the skull, like Aulacephalodon, Pelanomodon, Oudenodon, and Tropidostoma.[1][10]

As for the underlying parietals themselves, they are slightly concave. In front of the parietals are the small midline preparietal bones, which are relatively broad and have a rounded tip, as in Aulacephalodon and Pelanomodon but in contrast to Tropidostoma. The pineal foramen is bordered by the preparietals and parietals, and it is surrounded by a simple ridge instead of being on a raised boss like either the large rhaciocephalids and Endothiodon or some large specimens belonging to Aulacephalodon. On the braincase, no sutures are visible, suggesting that the bones are very fused. The occipital bones are likewise very fused. The contribution of the supraoccipital bones to the back of the skull is unusually extensive and occupies much of the area not part of the squamosals above the level of the foramen magnum. Also unusual are the smaller elements at the back of the skull, namely the postparietals and tabulars. The postparietals are not part of the continuous flat surface at the back of the skull, instead forming a sharp divot; additionally, a strong midline crest is present on the postparietals and do not extend onto other bones. Meanwhile, the tabulars are wider than they are long.[1]

Mandible and postcrania

[edit]
Referred specimen CGP/1/970 viewed from above, with postcrania at bottom

The mandible of Bulbasaurus was largely similar to Aulacephalodon. At the front of the mandible, the two toothless dentary bones fuse at the front to form a continuous beak with a sharp, pointed tip. The somewhat convex front surface of this junction, or the dentary symphysis, is separated from the sides of the dentaries by sharp ridges, a condition also seen in Pelanomodon and Geikia but not seen in Aulacephalodon. Overall, the dentary was tall and robust, the symphysis more so than the rest of the bone. Located at the mid-height of the dentaries are the mandibular fenestrae, which are small and oval, and bordered on top by a dentary shelf that expands into a boss. Asides from the skull, the other portions of Bulbasaurus have not been prepared in depth. The ribs are gently curved and are bicipital in that they have two heads. On the humerus, the deltopectoral crest was robust and strongly separated.[1]

Ontogeny

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Referred juvenile specimen SAM-PK-K10587

Most skulls referred to Bulbasaurus are 13–16 centimetres (5.1–6.3 in) long, with two skulls (CGP/1/2263 and SAM-PK-K10587) being smaller at 10.9 centimetres (4.3 in) and 10.4 centimetres (4.1 in) respectively. The larger skulls generally belong to mature specimens. While the CGP/1/2263's size is largely due to compression, SAM-PK-K10587 seems to be a genuinely immature individual. Notably, it differs from other specimens in having a shorter and less hooked snout; relatively smaller but still completely erupted tusks; less developed nasal bosses that are more separated by the premaxilla; a narrower interorbital region between the eyes; a wider intertemporal region at the back of the skull; relatively weak depressions in the interorbital and intertemporal regions; no overlap of the parietals by the postorbitals; and minimal twisting of the squamosal on the postorbital bar.[1]

These differences are most likely due to growth, as similar transformations are also seen in Aulacephalodon.[6][10] However, the latter (and all other geikiids where the growth sequence is known) differs from Bulbasaurus in that the degree of overlap of the parietals by the postorbitals does not change; instead, the parietals themselves simply become wider. In this respect, Bulbasaurus retains the ancestral cryptodontian condition, which is also seen in rhachiocephalids as well as Oudenodon, Tropidostoma, and other oudenodontids.[10] Overall, the relatively small Bulbasaurus provides evidence that the growth sequence of large geikiids such as Aulacephalodon did not develop along with their size, but rather was already present ancestrally and was retained as geikiids grew.[1]

Classification

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Bulbasaurus (second column) compared to Tropidostoma (first column) and Aulacephalodon (third column); skulls of the latter two are somewhat crushed

In 2017, Bulbasaurus was assigned to the Geikiidae clade of dicynodonts on account of its prominent nasal-frontal ridge, its relatively wide interorbital region, and its twisted squamosal on the postorbital bar. This assignment was supported by a phylogenetic analysis based on that conducted by Kammerer et al. in 2011,[5][11] which found it as the closest relative of Aulacephalodon on the basis of it lacking a ridge behind its tusk (which is ontogenetically influenced). However, this assignment is somewhat questionable, and forcing Bulbasaurus as a basal geikiid outside of the Geikiinae (Aulacephalodon, Geikia, and Pelanomodon) only requires one additional evolutionary step. Overall, the Cryptodontia (including the Geikiidae) were very unstable, suggesting that current datasets may not be able to sufficiently evaluate their relationships. An excerpt from the consensus of two phylogenetic trees, illustrating the relationships between cryptodontians, is shown below.

Cryptodontia

Tropidostoma, the genus Bulbasaurus was originally assigned to, exhibits two distinct morphologies - a robust morph with short snout and large tusks, and a gracile morph with long snout and small tusks, which probably represents sexual dimorphism as in other dicynodonts.[6][7][10][12][13] However, Bulbasaurus matches neither of those morphologies; it differs from the genus Tropidostoma as a whole in many respects (addressed above). Additionally, even the holotype of Tropidostoma (which is probably immature judging by the unerupted tusks) is larger than adult specimens of Bulbasaurus, which further warrants their separation. The same is true of Bulbasaurus and Aulacephalodon, in addition to their differing boss morphologies and different interorbital widths. Bulbasaurus also differs from the problematic specimens BP/1/763 (assigned once to its own genus, Proaulacocephalodon, or to a juvenile Aulacephalodon[6][10]) and TM 1480 (assigned once to Dicynodon hartzenbergi[5]) by its larger tusks and wider interorbital region, among other characteristics. These specimens are additionally from the younger Cistecephalus assemblage zone.[1]

Paleoecology

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Model of a Diictodon, the most common dicynodont in the Tropidostoma assemblage zone

Although the Tropidostoma Assemblage Zone, from where Bulbasaurus hails, is named after the oudenodontid Tropidostoma, Tropidostoma is only the third most common dicynodont in this assemblage zone. Most common is the small Diictodon, over 2000 specimens of which are known from the Tropidostoma AZ alone. Also more common than Tropidostoma is Pristerodon. Other dicynodonts present include Cistecephalus, Dicynodontoides, Emydops, Endothiodon, Oudenodon, Palemydops, and Rhachiocephalus.[14] Notable in the Tropidostoma AZ is the lack of geikiid and dicynodontoid dicynodonts (Dicynodontoides is a diictodont), which is unusual since they must have already diverged from their ancestral lineages by this time; Bulbasaurus happens to fill the former gap.[1]

The Tropidostoma AZ also records the gradual diversification of therocephalians and gorgonopsians.[1] Therocephalians present include Hofmeyria, Ictidosuchoides (most common), Ictidosuchops, Ictidosuchus, and Lycideops; gorgonopsids present include Aelurognathus, Aelurosaurus, Aloposaurus, Cyonosaurus, Gorgonops (most common), Lycaenops, and Scymnognathus.[14] Within the Karoo Supergroup, cynodonts also first appear within the Tropidostoma AZ;[1] they include Abdalodon (formerly assigned to Procynosuchus)[15] and Charassognathus.[16] Rarer members of the Tropidostoma AZ assemblage include the burnetiamorphs Lobalopex[17] and Lophorhinus;[18] parareptiles Pareiasaurus and Saurorictus; the archosauromorph Younginia; and the temnospondyl Rhinesuchus.[14]

Bulbasaurus was probably buried on floodplains surrounding a meandering river up to 350 metres (1,150 ft) wide and with point bars up to 3 kilometres (1.9 mi) in diameter.[1][19] This river flowed from the southern mountains northeast onto an alluvial fan some 500 kilometres (310 mi) wide. The water flow in the rivers was seasonally dependent, but there was probably flowing water year-round. About every 30,000 years, the river banks were breached by flooding, leaving overbank deposits and a series of small, isolated ponds.[14]

References

[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Bulbasaurus is an extinct genus of dicynodont therapsid, known from the Late Permian Tropidostoma Assemblage Zone of South Africa's Karoo Basin approximately 260 million years ago. This dog-sized featured a stocky, pig-like body, a turtle-like for cropping , and proportionally large tusks, distinguishing it as an early member of the geikiid family within dicynodonts. The genus name derives from the Latin bulbus (bulb), referencing the inflated, bulbous nasal bosses on its , while the species name phylloxyron combines Greek phyllos (leaf) and xyron (razor) to evoke the leaf-shaped cutting edges of its beak. Fossils of Bulbasaurus phylloxyron, including several well-preserved skulls, were collected from South African museum collections and formally described in 2017 by paleontologists Christian F. Kammerer and Roger M. H. Smith. As a basal geikiid, Bulbasaurus represents an early-diverging lineage in dicynodont evolution, bridging more primitive forms and later, more specialized members of the group that dominated Permian terrestrial ecosystems. Its robust build and prominent tusks suggest adaptations for foraging in a floodplain environment, potentially using the beak to shear tough plant material and the tusks for display or defense against predators. Despite superficial resemblances to the Pokémon Bulbasaur—due to the name's phonetic similarity—the fossil was not named after the fictional creature but strictly for anatomical features. Bulbasaurus highlights the diversity of synapsids, the mammalian stem group, during the Permian and their role as key herbivores before the end-Permian mass extinction.

Discovery and naming

Etymology

The genus name Bulbasaurus is derived from the Latin bulbus (bulb), referring to the bulbous shape of the nasal boss, and the Greek sauros (lizard), a common suffix for fossil amniotes of reptilian grade. The species epithet phylloxyron is from the latinized Greek phyllos () and xyron (razor), alluding to the slicing action of the inferred keratinous edges in processing material. Bulbasaurus phylloxyron was formally named in 2017 by Christian F. Kammerer and Roger M. H. Smith in the journal PeerJ.

Fossil material and localities

The specimen of Bulbasaurus phylloxyron is SAM-PK-K11235, consisting of a partial including the rostrum and , collected by paleontologist Roger M. H. Smith from the Driekoppe locality on the Vredelus farm near Fraserburg in the Province of . This specimen was initially misidentified as belonging to the dicynodont Tropidostoma upon collection and storage in the collections. Several referred specimens, all comprising partial , have been assigned to Bulbasaurus phylloxyron based on shared diagnostic features; these include SAM-PK-K10106 and SAM-PK-K10587 from localities in the area ( Province), as well as CGP/1/938, CGP/1/949, CGP/1/970 (which also preserves associated postcranial elements), and CGP/1/2263 from sites near Fraserburg (Northern Cape Province). The referred material exhibits ontogenetic and individual size variation, with basal skull lengths ranging from approximately 10.4 cm to 16.0 cm. All known specimens of Bulbasaurus derive from the Tropidostoma Assemblage Zone of the Hoedemaker Member, Teekloof Formation, within the Beaufort Group of the main Karoo Basin in , a stratigraphic interval dated to roughly 259–252 million years ago during the Wuchiapingian stage of the Late Permian.

Description

Premaxilla, maxilla, and palate

The of Bulbasaurus is short, hooked, and elevated, forming a beak-like structure at the anterior end of the snout without any teeth. This element is fused medially and exhibits a surface textured with numerous small pits and foramina, indicative of a thick keratinous covering that facilitated shearing of plant material. The forms the majority of the lateral wall and lacks a prominent caniniform process beyond the bulge created by the socket; it bears large, bulbous measuring up to 1.9 cm in diameter at their base, with the oriented ventrally to aid in uprooting or processing tough . These are rooted deeply within the , contributing to the overall robustness of the anterior apparatus. The is broad and vaulted, dominated by a well-developed secondary bony formed primarily by the and , which features large vacuities (openings) posteriorly and prominent keratinous ridges oriented transversely for gripping and processing food. There is no exposure of the on the surface, and the anterior ridges converge medially into a sharp , enhancing the efficiency of mastication. Collectively, these structures suggest an adaptation of the for cropping and initial breakdown of tough , a trait that sets Bulbasaurus apart from later dicynodonts, which typically exhibit more procumbent and laterally oriented tusks.

Nasal and orbital region

The of Bulbasaurus are paired elements that form the majority of the dorsal surface of the posterior to the external nares, characterized by large, rugose, nearly confluent bosses that protrude dorsally and cover much of the nasal length. These bosses are widest at their mid-length and lack a , distinguishing them from the discrete, ovoid, and relatively smoother bosses observed in the contemporary dicynodont Tropidostoma. The rugose texture of the bosses, marked by prominent pitting, contrasts with the less textured surfaces in related taxa like Tropidostoma, and they are separated by a narrow midline sulcus rather than being fully fused. The orbital region features a broad interorbital bar, with a mean width of approximately 4.0 cm across known specimens, which is relatively wider than in Tropidostoma but comparable to that in later geikiids such as Aulacephalodon. This bar is formed primarily by contributions from the nasals anteriorly, the frontals medially, and the prefrontals laterally, creating a robust margin around the laterally facing orbits without the prefrontal bossing present in some other geikiid dicynodonts. The forms the anteroventral portion of the orbital margin, bearing a single large , while the prefrontal lacks any pronounced ornamentation. The frontal bones are short and broad, largely confined to the interorbital region where they contribute to the nasofrontal ridge and exhibit a surface with deep pits, forming part of a depression alongside the preparietal. In juvenile specimens, the frontal sutures remain visible, supporting a relatively flat dorsal profile overall, though the increases with . These features collectively emphasize the structural of the mid- in Bulbasaurus, unique among early Permian dicynodonts for the extent of nasal boss development and interorbital breadth.

Postorbital skull

The postorbital bar in Bulbasaurus is notably robust and vertically oriented, formed by the postorbital and jugal bones, which together create a thick structure that lacks bosses or prominent dorsoventral ridges. This bar exhibits a concave lateral surface, providing an attachment site for jaw adductor muscles, and its thickness surpasses that observed in more basal dicynodonts such as Tropidostoma, indicating adaptations for resisting mechanical stress during feeding. The postorbital bone contributes to the dorsal and anterior portions of the bar, while the jugal forms the ventral margin, resulting in a configuration that enhances structural integrity in the temporal region. The squamosal and parietal bones further define the posterior skull roof, with broad temporal fenestrae averaging approximately 7.9 cm in length that accommodate extensive muscle attachments. The squamosal is dorsally extensive and flares posterolaterally, contributing to the posterior edge of the postorbital bar with a characteristic twist in the subtemporal ; this torsion is intermediate in degree between the slight deflection seen in Tropidostoma and the more extreme version in Aulacephalodon, suggesting progressive reinforcement of the temporal arcade. The parietals meet along the midline to form a pinched intertemporal bar, often partially obscured by the overhanging postorbitals, and do not expose a pineal on the skull roof, aligning with derived geikiid morphology. In the occipital region, which is partially preserved in known specimens, the squamosals exhibit robustness that underscores strong adductor musculature support. Fused occipital elements, dominated by the supraoccipital, feature a strongly developed nuchal crest on the postparietal that projects out of the plane of the skull roof, facilitating anchorage for neck musculature and contributing to overall cranial stability. Compared to earlier anomodonts, these features in Bulbasaurus reflect a more derived condition, particularly in geikiid dicynodonts, where enhanced thickness and orientation of the postorbital and temporal elements correlate with increased biting force for processing resistant vegetation.

Mandible

The mandible of Bulbasaurus phylloxyron is characterized by its elongate dentary bones, which fuse anteriorly to form a robust, beak-like covered by a keratinous sheath adapted for precise shearing against the upper . This structure lacks postcanine teeth in adults, though juveniles exhibit a short anterior tooth row, consistent with ontogenetic changes in dicynodont . The dentary is notably elongate, featuring a bulbous coronoid process posteriorly that serves as a key site for adductor muscle insertion, enhancing bite force. The angular and surangular bones are robust, contributing to the straight and providing structural support; the angular bears a reflected lamina that accommodates additional musculature for closure. Posteriorly, the articular bone presents a cotylar surface that articulates with the quadrate, forming a simple typical of dicynodonts and indicative of a primarily transverse motion. This mandibular configuration aligns with the upper 's , allowing for effective opposition during feeding, though detailed tusk morphology is addressed elsewhere.

Postcrania and

The postcranial skeleton of Bulbasaurus is known from only a single specimen, CGP/1/970, which preserves partial , proximal portions of several bicipital and gently curved ribs, elements of the , and a right with a robust deltopectoral crest perpendicular to the shaft. These features indicate a sturdy adapted for weight-bearing, consistent with the quadrupedal posture typical of dicynodonts. No other postcranial elements, such as or bones, have been recovered, limiting detailed reconstructions. Based on the maximum dorsal skull length of 16.0 cm and comparisons to geikiid relatives like Aulacephalodon, Bulbasaurus is estimated to have measured approximately 50–60 cm in total body length, roughly the size of a domestic house cat. This small stature suggests an agile, quadrupedal with a sprawling , similar to other diminutive Permian dicynodonts such as Diictodon, which employed a lizard-like posture for efficient terrestrial movement. Ontogenetic variation is evident in the cranial material, with skull lengths ranging from 10.4 cm in the smallest specimen (SAM-PK-K10587) to 16.0 cm in the largest. Juveniles exhibit narrower interorbital bars, smaller s, and less inflated nasal bosses compared to adults, where maturation involves pronounced boss development and tusk elongation beginning around 13 cm skull . Most specimens fall within the 13–16 cm range, representing subadults to adults, with no evidence of postorbital-parietal contact in the smallest individual. Growth patterns in Bulbasaurus likely followed the determinate trajectory common to therapsids, characterized by rapid early ontogenetic rates that slow in adulthood, as inferred from the stabilization of key cranial features at smaller sizes than in larger geikiids. remains unconfirmed due to the limited sample size of five specimens, though variation in size may hint at possible differences.

Classification

Taxonomic history

The specimen of Bulbasaurus phylloxyron (SAM-PK-K11235) was initially misidentified as Tropidostoma sp. in museum collections prior to 2017, owing to superficial similarities in rostrum shape and overall cranial proportions. This assignment reflected the common practice of referring fragmentary dicynodont material from the Tropidostoma Assemblage Zone to the dominant Tropidostoma during early assessments of Permian therapsid diversity. In 2017, Christian F. Kammerer and Roger M. H. Smith formally described and reassigned the , along with two referred specimens, to the new and Bulbasaurus phylloxyron, based on distinctive autapomorphies including prominent nasal bosses overhanging the nares and large palatal vacuities. The generic name derives from Latin bulbus () in reference to the bulbous nasal region, while the specific epithet phylloxyron is from Greek phyllos () and xyron (razor), referring to the leaf-shaped cutting edges of the tusks. This reclassification highlighted Bulbasaurus as a distinct early member of Geikiidae, previously unknown from this stratigraphic interval. No major taxonomic revisions have been proposed since the original description, with Bulbasaurus consistently upheld as a valid in post-2017 reviews of dicynodont as of 2025. Confirmation of its placement stems from ongoing phylogenetic analyses of Permian therapsids. All known specimens derive from the Tropidostoma Assemblage Zone in South Africa's Karoo Basin, specifically the Hoedemaker Member of the Teekloof Formation near Driekoppe, Vredelus, Fraserburg, thereby filling a stratigraphic gap in the early geikiid record.

Phylogenetic position

Bulbasaurus is classified within the Therapsida, specifically as a member of Anomodontia, the clade encompassing advanced non-mammalian therapsids characterized by herbivorous adaptations such as tusks and beaked jaws. Within Anomodontia, it belongs to Dicynodontia, a diverse group of Permian and synapsids that dominated late terrestrial ecosystems. More precisely, Bulbasaurus is placed in Geikiidae, a family of robust dicynodonts known from the Late Permian, alongside genera such as Geikia and Aulacephalodon. Phylogenetic analyses recover Bulbasaurus as a basal geikiid, representing the earliest known member of the . In a modified version of the comprehensive anomodont matrix developed by Kammerer et al. in 2011, which includes 153 discrete and 21 continuous characters scored across 103 , parsimony analysis in TNT software yields two most parsimonious trees of length 1032.706 steps (consistency index 0.234, retention index 0.709). These trees position Bulbasaurus as the sister to Aulacephalodon, with Geikiidae forming a monophyletic group supported by a transverse nasofrontal ridge, broad interorbital region, twisted subtemporal bar, and absence of the postfrontal . Bulbasaurus shares key geikiid synapomorphies including bulbous, rugose nasal bosses, a robust postorbital bar, and large palatal vacuities, while differing from the related tropidostomatid Tropidostoma in the absence of an intertemporal bar. The placement of Bulbasaurus extends the temporal range of Geikiidae back into the early epoch, specifically the Tropidostoma Assemblage Zone of the South African Beaufort Group, shortening the inferred for the family by approximately 2–3 million years. This discovery implies that geikiid morphology, characterized by reinforced cranial architecture suited for tough , originated in Gondwanan environments during the late Permian, prior to the diversification of larger-bodied forms in subsequent assemblage zones.

Paleoecology

Geological setting

Bulbasaurus fossils occur in the Hoedemaker Member of the Teekloof Formation, which belongs to the Beaufort Group within the Basin of . This stratigraphic unit is part of the Tropidostoma Assemblage Zone and is exposed at localities such as Vredelus, in the southwestern portion of the basin. The rocks preserving Bulbasaurus date to the late Permian, specifically the Wuchiapingian stage of the epoch, spanning roughly 259–252 million years ago. This interval precedes the end-Permian mass by several million years and is calibrated through biostratigraphic correlation and limited of associated ash layers in the Karoo sequence. The depositional setting represents alluvial developed along a large fluvial system, featuring meandering rivers and associated point bars. occurred primarily through overbank flooding in a proximal floodplain environment, with red mudstones comprising the dominant and reflecting well-oxygenated, oxidizing conditions during deposition. Periodic breaching of river banks led to major flood events, resulting in the accumulation of overbank deposits and the formation of isolated ponds. The paleoclimate was semi-arid, characterized by seasonal wet-dry cycles that influenced fluvial dynamics and supported vegetation adapted to episodic moisture availability. These conditions promoted in interfluve areas between channels, with evidence of periodic preserved in the pedogenic features of the mudstones.

Associated fauna

The Tropidostoma Assemblage Zone (AZ) in the South African Karoo Basin features a diverse assemblage of approximately 50 taxa, indicative of an ecosystem recovering from the Capitanian mass extinction bottleneck earlier in the Permian period. This zone, part of the Beaufort Group, documents a transitional phase where therapsid diversity rebounds, with dicynodonts playing a prominent role among herbivores following the decline of earlier dominant groups like dinocephalians. Dominant herbivores include the small dicynodont Diictodon feliceps, the most abundant taxon in the assemblage and a key component of the small-bodied . Other significant herbivores comprise Pristerodon mackayi and basal anomodonts such as Tropidostoma microtrema, which together reflect the increasing prevalence of tusked dicynodonts in late Permian floodplains. Carnivorous therapsids are represented by gorgonopsians, including early forms like and Cynariops robustus, which mark the initial radiation of this group. Therocephalians, such as Ictidosuchoides longiceps, and early cynodonts, exemplified by Abdalodon diastematicus, also contribute to the carnivore diversity, highlighting the emergence of lineages that would persist into the . Additional herbivores among reptiles include captorhinids like Saurorictus australis, providing the first record of multi-rowed teeth in this zone's reptile component.

Inferred ecology

Bulbasaurus phylloxyron was an herbivorous dicynodont that utilized its keratinous, hook-like beak and robust tusks to shear tough, fibrous vegetation, including the dominant glossopterid flora of the Late Permian Basin floodplains. The species epithet phylloxyron, meaning "leaf razor," underscores this adaptation for cropping plant material in a seasonally variable environment. Its secondary included paired anterior ridges flanking a prominent , which likely aided in grinding and processing ingested foliage to extract nutrients efficiently. In the dynamic setting of the Tropidostoma Assemblage Zone, Bulbasaurus probably engaged in burrowing or mud-sheltering behaviors to avoid periodic floods and arid spells, a strategy observed in contemporaneous small to medium dicynodonts for and protection. This creature was likely solitary or formed small social groups, as suggested by its low abundance in the fossil assemblage relative to more common herbivores like Tropidostoma. Such habits would have enhanced its agility for evading predators, including gorgonopsians that co-occurred in the . As a small- to medium-bodied generalist (with a length of 13–16 cm), Bulbasaurus filled an ecological gap between diminutive burrowers like Diictodon and larger grazers such as Oudenodon or Tropidostoma in the diverse Tropidostoma Assemblage Zone community. Its robust build and inferred tolerance for seasonal aridity—evident in the proximal deposits of the Teekloof Formation—represent pre-adaptations that bolstered dicynodont resilience amid environmental fluctuations.
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