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Homalocephale
Homalocephale
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Homalocephale
Temporal range: Late Cretaceous, Maastrichtian
Mounted holotype in the Mongolian Natural History Museum, 2002
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Dinosauria
Clade: †Ornithischia
Clade: †Pachycephalosauria
Family: †Pachycephalosauridae
Genus: †Homalocephale
Maryanska & Osmolska, 1974
Species:
†H. calathocercos
Binomial name
†Homalocephale calathocercos
Maryanska & Osmolska, 1974

Homalocephale (from Greek ὁμαλός, homalos, "even", and κεφαλή, kephalē, "head") is a genus of pachycephalosaurid dinosaur that lived during the Late Cretaceous period of what is now the Nemegt Formation, Mongolia. The genus was described in 1974 by Halszka Osmólska and Teresa Maryańska, and consists of a single species, H. calathocercos. Though Homalocephale has been regarded as a synonym (and juvenile form) of Prenocephale, juvenile specimens of the latter indicate that they were distinct. Homalocephale was 1.8 m (5.9 ft) long and possibly an omnivore.

Discovery

[edit]
Skeletal diagram of the holotype

The type species, H. calathocercos, was described from an incomplete skull and postcranial material (holotype MPC-D 100/1201) from the Nemegt locality of the Nemegt Formation. The specimen has large openings on the top of the skull, a distinct frontoparietal suture, low and long infratemporal fenestrae, and a large, round eye socket. The forehead is notably rough, with multiple nodules on the lateral and posterior sides of the squamosal bone. Paleontologists concluded that the specimen was an adult, despite the fact that the sutures are discernible and that it had a flat skull (a juvenile trait in many pachycephalosaurid species).[1]

In 2010, a study by Nick Longrich and colleagues suggested that flat-headed pachycephalosaurs were just juvenile forms of dome-headed adults, a view also supported by the earlier analysis of Horner and Goodwin in 2009. Longrich and colleagues suggested that Homalocephale is actually the juvenile or sub-adult stage of Prenocephale mainly based on the lack of a dome and being discovered in the same locality (Nemegt) as the latter.[2]

David C. Evans and team in 2018 reported juvenile specimens of Prenocephale from the Nemegt Formation, noting a relatively linear growth in this pachycephalosaur characterized by a rounded dome. This differs from the flat skull of Homalocephale and given that even juvenile Prenocephale possessed a rather rounded dome, both taxa should be regarded as separate.[3]

Description

[edit]
Life restoration

Homalocephale was about 1.8 m (5.9 ft) long.[4] Unlike other definitely adult pachycephalosaurs (though similar to probable juvenile specimens referred to Dracorex and Goyocephale), Homalocephale sported a flat, wedge-shaped skull roof. Nonetheless, the surface of the skull was fairly thickened.[1]

Classification

[edit]
Cast of the holotype skull

Below is a cladogram from Evans et al. (2013).[5]

Pachycephalosauria

Paleobiology

[edit]
Two Homalocephale with Saurolophus herd behind

Homalocephale is also noted for having an unusually broad pelvis and some have suggested that the width served to protect vital organs from harm during flank-butting. Others think that they were for giving birth to live young, instead of laying eggs.[6] Homalocephale also had rather long legs, indicating a fast-moving gait.[7]

See also

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References

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Sources

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[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia

Homalocephale

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Homalocephale is a of small, bipedal, herbivorous ornithischian in the family Pachycephalosauridae, characterized by its distinctive flat skull roof and thick cranial bones. Known from a single , H. calathocercos, it lived during the period, approximately 72 to 68 million years ago, in what is now the of . The was named for its "even head" (from Greek homalos, meaning level, and kephalē, meaning head), reflecting the unique non-domed structure of its skull, which contrasts with the rounded domes typical of many other pachycephalosaurids. The type specimen, a nearly complete including the and extensive postcrania such as , ribs, , and hind limbs, was discovered in the and described by paleontologists Teresa Maryańska and Halszka Osmólska in 1974. This specimen, cataloged as GI SPS 100/51, measures about 1.5 meters (4.9 feet) in length, with estimates suggesting a weight of around 40-50 kilograms, making Homalocephale one of the smaller members of its family. Key anatomical features include a flat, thickened roof with visible sutures, large supratemporal fenestrae, a broad , and a rigid reinforced by a "" of ossified tendons starting from the 12th caudal , which may have aided in stability during bipedal locomotion. Homalocephale is classified within the suborder , a group of marginocephalians known for their thickened roofs, possibly used for display or intraspecific , though the flat head of Homalocephale suggests differences in behavior or ontogeny compared to domed relatives like . It coexisted with other dinosaurs in the , such as the pachycephalosaurid Prenocephale prenes, from which it is distinguished by cranial and postcranial traits, including tooth wear patterns and vertebral structure; its relationship to Prenocephale remains debated, with some suggesting Homalocephale represents a juvenile stage. Recent analyses support its validity as a separate , though its flat may indicate a juvenile or paedomorphic condition rather than primitive adult features relative to more derived pachycephalosaurids.

Discovery and Naming

Discovery

The specimen of Homalocephale calathocercos, currently designated MPC-D 100/1201 (originally cataloged as G.I. No. SPS 100/51), was unearthed during the Polish-Mongolian Paleontological Expeditions conducted in the early 1970s, specifically in 1971. This discovery occurred in the at the Nemegt locality within the of southern . The expeditions, which began in 1963 and continued through the 1970s, systematically explored Upper Cretaceous deposits in the region, yielding numerous fossils alongside this pachycephalosaurid material. The preserved elements include an incomplete roof (lacking mandibles, nasals, anterior frontals, supraorbitals, prefrontals, and the right jugo-maxillar arch), two sternal plates, ten posterior dorsal vertebrae with associated , six sacral vertebrae, 29 postsacral vertebrae with caudal , the right ilium, a left ilium fused with the proximal portion of the right , the left , distal ends of the left and right and , the left astragalus, the right metatarsal II, and numerous free caudal tendons. These remains represent a partial , providing key insights into the dinosaur's cranial and postcranial from the Upper (late to ) , a fluvial and lacustrine depositional environment contemporaneous with taxa such as Tarbosaurus bataar and Saurolophus angustirostris. Although the skull roof exhibits a notably flat morphology, the specimen was interpreted as an based on the fusion of the sacral vertebrae and other neurocentral sutures in the preserved axial elements, indicating skeletal maturity. This assessment contrasted with the more domed skulls typical of other pachycephalosaurids, prompting its initial distinction within the group. The was formally described and named by Polish paleontologists Teresa Maryańska and Halszka Osmólska in their seminal 1974 published in Acta Palaeontologica Polonica, where they erected the suborder and positioned H. calathocercos as a representative .

Etymology and Taxonomy

The genus name Homalocephale derives from words homalos (ἁμαλός), meaning "even" or "flat," and kephalē (κεφαλή), meaning "head," in reference to the notably flat dorsal surface of the roof. The species epithet calathocercos combines kalathos (κάλαθος), meaning "basket," and kerkos (κερκός), meaning "tail," alluding to the distinctive basket-like arrangement of the chevron bones enclosing the caudal vertebrae. The genus Homalocephale and its H. calathocercos were formally established in 1974 by paleontologists Teresa Maryańska and Halszka Osmólska, based on the specimen (an incomplete and partial postcrania) recovered from the Upper of . This description positioned Homalocephale as the second recognized Asian pachycephalosaurid genus, distinct from the contemporaneous Prenocephale prenes described in the same publication. In 2006, Robert M. Sullivan proposed synonymizing Homalocephale with Prenocephale, interpreting the flat-headed morphology of H. calathocercos as representative of a juvenile ontogenetic stage rather than a valid adult . This drew on the shared provenance in the and similarities in non-cranial anatomy, suggesting that dome formation occurred later in growth. The proposed synonymy was refuted in 2011 by David C. Evans and colleagues, who documented consistent morphological differences between the holotypes of H. calathocercos and P. prenes, including distinct patterns of cranial ornamentation (e.g., node distribution on the squamosals and parietals), structure, and , despite comparable body sizes. Subsequent analysis in 2018 by Evans, Ryan, and colleagues reinforced this distinction through examination of new juvenile Prenocephale specimens, which exhibited incipient dome development and ornamentation patterns absent in Homalocephale, confirming the latter's validity as a separate . As of 2025, Homalocephale remains a monospecific genus, with H. calathocercos as its sole valid species and no additional taxa recognized within it.

Anatomy

Skull

The skull of Homalocephale calathocercos is characterized by a flat, wedge-shaped roof lacking the pronounced dome seen in other pachycephalosaurs such as Pachycephalosaurus wyomingensis, with the dorsal surface forming a nearly horizontal plane that slopes gently anteriorly. This configuration results in a low-profile cranium adapted for potential lateral impacts rather than direct frontal collisions. The dorsal surface of the skull roof is markedly thickened, featuring a rough texture ornamented with vascular grooves, deep peripheral pits, and irregular node-like thickenings that provide structural , possibly for resisting impacts. The squamosals exhibit broad, flat flanges along their posterolateral and posterior margins, adorned with moderate accessory nodes arranged in linear series, contributing to the overall ornamentation of the parietosquamosal bar. Similarly, the postorbitals extend medially toward the supratemporal fenestrae and bear horn-like projections that integrate into the flat cranial roof, enhancing the lateral profile without elevating the overall height. Internally, the braincase reveals features indicative of a relatively large for a of comparable size, including extensive in the orbital region and elongated olfactory bulbs that suggest an enhanced compared to more basal ornithischians. The holotype skull has a greatest width of 138 mm and height of 118 mm.

Postcrania

The postcranial skeleton of Homalocephale calathocercos is known from the specimen (MPC-D 100/1201, formerly GI SPS 100/51), which includes elements from the axial column, girdles, and limbs, allowing for reconstructions of overall . The total body length is estimated at approximately 1.5 meters, with a body mass of around 45 kg, derived from scaling measurements of the preserved and comparisons to related pachycephalosaurids like Prenocephale prenes. The hind limbs exhibit gracile proportions indicative of adaptations, featuring an elongated measuring 218 mm in length that curves slightly inward with a weakly pendant fourth positioned proximally for enhanced muscle leverage. The is similarly elongated relative to the , with a strongly broadened distal end (transverse width of 57.5–59.5 mm) that articulates with a tetradactyl pes, where metatarsals II and III reach lengths of 95 mm and 99.5 mm, respectively; these features suggest efficient terrestrial locomotion suited to open environments. The is notably broad and basket-shaped, characterized by expanded ilia (right ilium length 230 mm) that project horizontally with a medial bearing dorsal striations for muscle or attachment, and a highly reduced pubis nearly excluded from the , which is deeply enclosed by the ilium and . This configuration likely accommodated increased pelvic musculature volume, potentially aiding in extension or supporting a spacious . The caudal vertebrae feature a unique "basket" structure formed by ossified tendons and chevron bones, starting from the 12th caudal vertebra and extending along the distal portion of the tail, with fusiform elements up to 10 mm in diameter arranged in a zig-zag pattern to limit lateral and vertical mobility while providing rigidity and protection. This myorhabdoid ossification, a synapomorphy of , contributes to the species' etymological reference to a "basket-tailed" form. Preserved dorsal vertebrae (10 posterior examples) and ribs indicate a relatively flexible spine compared to more robust pachycephalosaurids like , with amphicoelous centra, low neural spines, and bicapitate ribs (lengths up to 83 mm) that articulate via tongue-and-groove zygapophyses, allowing limited dorsoventral movement while maintaining overall stability; long, rod-like caudal ribs on proximal caudals further broaden the body outline.

Classification and Phylogeny

Historical Classification

Homalocephale was initially described and classified within the family Pachycephalosauridae by Teresa Maryańska and Halszka Osmólska in 1974, based on a partial and postcranial elements from the Upper of ; they noted its distinctive flat skull roof differing from the domed forms typical of other pachycephalosaurids. This placement emphasized its position as a small-bodied ornithischian with node-like cranial ornamentation, large supratemporal fenestrae, and a relatively complete postcranium, distinguishing it from contemporaneous Asian taxa like Prenocephale. During the and , Homalocephale was often assigned to the Homalocephalinae (or family Homalocephalidae as proposed by Dong in 1977), to accommodate flat-headed Asian pachycephalosaurids such as Homalocephale and Goyocephale, in contrast to the domed Pachycephalinae; this division was based on skull roof morphology and was supported in descriptions of new Mongolian material. However, by the late and into the early , taxonomic reviews began to synonymize or reject such subfamilies, arguing they lacked robust synapomorphies and reflected ontogenetic variation rather than distinct clades; Homalocephale was increasingly viewed amid debates on Asian pachycephalosaur diversity, with analyses highlighting its primitive cranial features relative to more derived North American forms. A 2013 phylogenetic analysis by David C. Evans and colleagues refined Homalocephale's position as a derived pachycephalosaurid, closely related to fully domed taxa like Prenocephale and pachycephalosaurines, rather than a basal ; this study emphasized its distinction from contemporaneous North American taxa through temporal precedence and cranial details, supporting the idea that flat-headed forms may represent juvenile stages without altering its generic validity. Prior to 2018, synonymy proposals, such as those by Nicholas R. Longrich and colleagues in 2010, suggested Homalocephale might represent a juvenile or sexual dimorph of Prenocephale based on shared Mongolian provenance and morphological overlap; these were resolved as separate genera in subsequent ontogenetic studies, confirming Homalocephale's unique cranial ornamentation and maturity indicators.

Phylogenetic Position

Homalocephale is firmly placed within the family Pachycephalosauridae as a derived pachycephalosaurid, based on multiple cladistic analyses utilizing morphological character matrices focused on cranial features. In a 2013 analysis incorporating 50 characters across 16 pachycephalosaurian taxa, Homalocephale groups closely with other Asian forms such as Goyocephale and Prenocephale, forming a more derived than and basal taxa like , which branches as the sister to all other pachycephalosaurs. Subsequent matrices, including an expanded dataset in Evans et al. (2018) with additional specimens, reinforce this positioning, recovering Homalocephale as the sister taxon to Prenocephale or a broader Asian clade that excludes earlier North American lineages. Key synapomorphies supporting Homalocephale's placement include the presence of flat squamosal flanges with reduced ornamentation and vascularized nodes on the skull roof, which distinguish it from more basal pachycephalosaurs lacking such derived cranial vascular patterns while aligning it with advanced Asian pachycephalosaurids. These features indicate a specialized adaptation within the group, consistent with its position in simplified cladograms where Homalocephale branches after basal forms like but prior to fully domed pachycephalosaurines. A phylogenetic analysis of the Chinese taxon Sinocephale bexelli, using a modified matrix from prior studies, further supports Homalocephale as part of a derived Asian , positioning it as a to Prenocephale within a that includes other Mongolian forms. As a derived Asian pachycephalosaur, Homalocephale represents a lineage that diverged from North American pachycephalosaurids around 80 million years ago during the , coinciding with biogeographic separation across . Recent discoveries, such as the early Mongolian pachycephalosaur Zavacephale rinpoche (2025), extend the group's origins but do not alter the stability of Homalocephale's position, as it remains un-reclassified amid new Chinese and Mongolian specimens that reinforce rather than disrupt existing Asian-derived topologies.

Paleobiology

Locomotion and Speed

Homalocephale, as a small bipedal ornithischian, possessed gracile proportions consistent with adaptations that supported efficient bipedal locomotion and maneuverability. The - ratio in pachycephalosaurs, where the exceeds the in length, indicates potential for agile dodging rather than sustained high-speed pursuits, differing from the elongated tibiae typical of more theropods. Biomechanical analyses using Alexander's formula, which scales speed estimates from relative stride length and hip height derived from limb dimensions, suggest that small bipedal dinosaurs like Homalocephale could achieve top speeds of 25–40 km/h during short bursts. This range aligns with the capabilities of similarly sized extinct and extant runners, emphasizing over endurance. The elongated metatarsals and phalanges in pachycephalosaur hindlimbs enabled rapid initial , advantageous for navigating open terrains inferred from the Nemegt Formation's . A stiff reinforced by ossified caudal tendons provided counterbalance and stability during quick directional changes, while the vertebral column allowed some flexibility for overall postural adjustments. These locomotor traits parallel evasion strategies in modern analogs such as the pronghorn antelope, which relies on bursts of speed and sharp turns to evade predators in open habitats.

Diet and Feeding

Homalocephale is inferred to have been primarily herbivorous, potentially with omnivorous tendencies, based on its cranial and dental features adapted for processing plant material and possibly small . The maxillary teeth are low-crowned and roughly leaf-shaped, featuring a strong medial ridge on the lingual surface flanked by additional anterior and posterior ridges, with the posterior edge coarsely serrated; these teeth lack a dental battery and exhibit extensive wear on the lingual side, forming a near-continuous horizontal plane across the tooth row for cropping and initial breakdown of . This morphology suggests suitability for low , such as leaves, fruits, seeds, twigs, stems, and bark from and angiosperms, with the worn surfaces indicating grinding or crushing of tough, fibrous items. Jaw mechanics in pachycephalosaurs like Homalocephale involved primarily orthal (up-and-down) motion at the craniomandibular joint, coupled with slight long-axis rotation of the mandibular rami to enable limited lateral movement during occlusion, facilitating mastication of plant matter without the complex shearing seen in carnivorous reptiles. The absence of significant propalinal (fore-aft) motion and the presence of undeflected dentaries with uneven tooth rows point to simple puncture-crushing actions, where much food processing likely occurred in the gut rather than the mouth, consistent with a diet emphasizing low-energy oral preparation. The overall low posterior bite forces further support adaptation to softer or less resistant foods, such as fruits and , rather than highly fibrous or abrasive requiring powerful occlusion. As a small-bodied ornithischian, Homalocephale probably foraged at low heights, restricted to under 1 meter above the ground in its floodplain environment, potentially overlapping with other small herbivores in accessing ground-level browse. The triangular, ridged teeth with serrations may have also permitted opportunistic consumption of , aligning with broader pachycephalosaurid feeding inferred from dental wear patterns and .

Reproduction and Growth

The flat skull of Homalocephale is interpreted as an trait rather than a juvenile feature, supported by ontogenetic analyses indicating that cranial dome formation in related pachycephalosaurs like Prenocephale begins early in development, precluding Homalocephale from representing a juvenile stage of a domed . Recent studies have resolved earlier debates, confirming Homalocephale as a valid, distinct representing an form with primitive features. This distinction is reinforced by the unique cranial ornamentation pattern in Homalocephale, including pronounced nodes along the squamosal, which aligns with mature morphology rather than transitional juvenile forms. The broad of Homalocephale, notably wider than in many contemporaneous ornithischians, has been hypothesized to facilitate either or the laying of large eggs, potentially accommodating an expanded birth canal for head-first delivery of with proportionally large heads—a possibly linked to the robust cranial observed across pachycephalosaurs. This pelvic morphology may have provided structural support during , contrasting with narrower-hipped relatives and suggesting specialized reproductive strategies in flat-headed forms. Recent analyses of pachycephalosaur growth indicate that was achieved prior to the completion of somatic growth, with cranial dome development serving as a key indicator of reproductive readiness in domed taxa; analogous patterns in flat-headed Homalocephale likely involved similar precocious maturation, where nodes signaled adulthood. from related pachycephalosaurs reveals fibrolamellar tissue indicative of rapid early growth, transitioning to slower rates in maturity. Growth patterns in Homalocephale are inferred to reflect determinate growth typical of ceratopsians and ornithopods, with external annuli marking annual increments in long bones.

Paleoecology

Geological Formation

The , the primary stratigraphic unit yielding fossils of Homalocephale, is a deposit located in the Nemegt Basin of the , southern . It dates to the stage, approximately 72–68 million years ago, and forms part of the extensive continental sedimentary sequences of the region. The formation reaches a minimum thickness of 235 meters and conformably overlies the older Baruungoyot Formation, with the two units interfingering over at least 23 meters in some sections, indicating a gradual environmental transition. Sedimentologically, the consists predominantly of light gray to tan sandstones and mudstones, reflecting a fluvial and with meandering rivers, ephemeral lakes, and paludal settings. Channel-fill sandstones, comprising over 80% of the , record southwest-flowing rivers approximately 6 meters deep and 75 meters wide, while overbank mudstones and sheetflood deposits indicate periodic flooding and progradation from southeastern sources. These features point to a dynamic where supply increased due to tectonic uplift, leading to southeastward progradation of fluvial tongues up to 4 kilometers long. The paleoclimate of the was warm and humid, with seasonal rainfall that fostered forested vegetation along river courses and supported a lush, diverse . This wetter regime, inferred from the abundance of fine-grained overbank deposits and lack of extensive eolian features, marked a shift from the semi-arid conditions of the underlying Baruungoyot Formation. Taphonomically, Homalocephale fossils and other vertebrate remains in the are commonly concentrated in channel lags within sandstone units, suggesting post-mortem transport by fluvial currents before final burial. This process often resulted in disarticulated and abraded bones, with the richest assemblages occurring in the interfingering zone with the Baruungoyot Formation, where rapid preserved a mix of aquatic and terrestrial taxa.

Associated Fauna

The Nemegt Formation of , where fossils of Homalocephale have been recovered, preserves a diverse assemblage of vertebrates, including numerous taxa that co-occurred in a fluvial and floodplain environment. Theropod dinosaurs dominate the carnivorous guild, with tyrannosaurids such as bataar representing apex predators, alongside oviraptorosaurians like Nemegtomaia and , troodontids including , ornithomimids such as and Anserimimus, and smaller forms like alvarezsaurids and dromaeosaurids (). Ornithischian herbivores include hadrosaurs like Saurolophus angustirostris and Barsboldia sicinskii, therizinosaurs such as and , ankylosaurids including Tarchia and , and other marginocephalians including the pachycephalosaurid Prenocephale prenes. Beyond dinosaurs, the Nemegt fauna encompasses a multitaxon ecosystem with aquatic and semi-aquatic reptiles, such as turtles and crocodylomorphs (Paralligator), as well as fish, birds, and small mammals, reflecting a humid, riverine habitat supportive of varied ecological niches. No direct fossil evidence documents interactions between Homalocephale and these contemporaries, but ecological inferences suggest that large theropods like Tarbosaurus may have preyed on juvenile Homalocephale, while adult individuals, as mid-sized browsers, likely competed for low vegetation with hadrosaurs such as Saurolophus. Homalocephale's inferred agility and speed would have aided in evading predators within this dynamic community. Recent discoveries in 2025, including the new pachycephalosaur Zavacephale rinpoche from the Early Cretaceous Khuren Dukh Formation in Mongolia's Gobi Desert, highlight expanding diversity of the group in Asian formations, though no new taxa have been added directly to the Nemegt assemblage.

References

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