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Pinacosaurus

Pinacosaurus is a of basal ankylosaurine dinosaur belonging to the family , characterized by its heavily armored , low-slung quadrupedal build, and a distinctive used for . This herbivorous ornithischian measured approximately 5 meters in length and weighed up to 2,000 kilograms, with a wide, triangular featuring a for cropping and osteoderms covering much of its and . Known from the stage of the , approximately 81 to 75 million years ago, fossils of Pinacosaurus have been primarily discovered in and , including notable juvenile specimens that suggest gregarious behavior among young individuals. The type species, Pinacosaurus grangeri, and P. mephistocephalus, were first described by Charles W. Gilmore in 1933 based on a partial from the in Mongolia's . Subsequent discoveries, such as a nearly complete juvenile (IGM 100/1014) from the Ukhaa Tolgod locality, reveal ankylosaurid synapomorphies including two pairs of osteodermal "horns" on the quadratojugals and squamosals, as well as a premaxillary edge not continuous with the maxillary row. These specimens highlight Pinacosaurus as a basal ankylosaurine, with a position in the phylogeny that informs the stepwise evolution of tail clubs in the group. Anatomically, Pinacosaurus possessed a robust adapted for a , with grinding in the and dentary, and no premaxillary teeth. Its armor included polygonal osteoderms along the back and a terminating in a knob formed by fused osteoderms, representing an early development of this defensive structure that enveloped the end in specimens. Juvenile forms show incomplete fusion of dermal ossifications, indicating ontogenetic changes, while adult reconstructions suggest a narrower relative to more derived ankylosaurids. Fossils from formations like Bayan Mandahu in further demonstrate variability in features such as paranasal apertures and antorbital fossae. Pinacosaurus occupied arid, dune-rich environments in what is now , coexisting with other dinosaurs such as theropods and ceratopsians. The abundance of juvenile skeletons preserved together points to possible social grouping in early life stages, a less commonly observed in other ankylosaurs. As a basal member of Ankylosaurinae, it provides critical insights into the diversification of armored dinosaurs, bridging earlier thyreophorans and more advanced forms like Euoplocephalus and Ankylosaurus.

Discovery and naming

History of discovery

The initial discovery of Pinacosaurus took place in 1923 during the Third Central Asiatic Expedition of the to Mongolia's . Paleontologist Walter W. Granger located the specimen (AMNH 6523), a partial comprising a taphonomically distorted skull, mandible, atlas, axis, and fragmentary postcranial elements, at the (Bayn Dzak) site in the Djadokhta Formation. In 1933, Charles W. Gilmore named the taxon Pinacosaurus grangeri in recognition of Granger's contributions, designating the AMNH 6523 material as the in his description published in American Museum Novitates. Further AMNH expeditions in the late and early recovered additional fragmentary specimens from the Djadokhta Formation, establishing the site's importance for ankylosaur fossils. The Soviet-Mongolian Paleontological Expedition, active from 1969 to 1970, unearthed dozens of mostly juvenile skeletons at the Alag Teer locality in the equivalent Alagteeg Formation, forming a dense bonebed indicative of mass mortality events possibly triggered by sandstorms or flash floods, with specimens often preserved in disarticulated clusters. Chinese paleontological efforts from the 1970s through the 1990s, including collaborations like the Canada-China Dinosaur Project, yielded over a dozen additional skeletons—predominantly juveniles—from the Bayan Mandahu Formation in Inner Mongolia, where taphonomic evidence suggests similar rapid burial in aeolian or fluvial settings. These efforts have resulted in more than two dozen known Pinacosaurus skeletons across the Djadokhta, Alagteeg, and Bayan Mandahu formations, underscoring the genus's relative abundance among ankylosaurs. As of 2025, several undescribed juvenile specimens persist in institutional collections, supporting continued curatorial and descriptive work.

Species and synonyms

The genus Pinacosaurus was established by Charles W. Gilmore in 1933, with the P. grangeri diagnosed primarily by a low nasal boss, weakly developed pyramidal squamosal horns, a large premaxillary , and a quadrate that is not co-ossified with the paroccipital process. The (AMNH 6523) consists of a dorsoventrally crushed but nearly complete skull and lower jaw, along with the atlas, axis, and associated osteoderms, collected from the Djadokhta Formation at Shabarakh Usu (), . A second species, P. mephistocephalus, was named in 1999 by Pascal Godefroit and colleagues based on a subadult (IMM 96BM3/1), comprising a nearly complete, articulated preserving the , much of the postcranium, dermal armor, and , from the in , . Its validity as a distinct species remains debated; in 2010, suggested it was a junior of P. grangeri, while a 2012 analysis by Robert V. Hill supported its separation based on cranial features. This species is distinguished from P. grangeri by more pronounced cranial ornamentation, including elongate squamosal horns that project posteriorly beyond the occiput, a straighter lacrimal, and differences in the narial region such as fewer accessory openings (four pairs total versus five pairs in P. grangeri). Several taxa have been recognized as junior synonyms of P. grangeri. These include Syrmosaurus disparoserratus (Maleev, 1952), based on fragmentary armor from the Djadokhta Formation, and Syrmosaurus viminicaudus (Maleev, 1952), known from caudal vertebrae and armor also from ; both were later synonymized due to overlapping diagnostic features with the holotype of P. grangeri. Additionally, P. ninghsiensis (Young, 1935), described from a partial in , , was reduced to a upon recognition of its conspecificity with P. grangeri. Referral of Bayan Mandahu specimens to Pinacosaurus has involved some debate, with early assignments to nodosaurids like later reclassified to P. grangeri or P. mephistocephalus based on ankylosaurid synapomorphies such as the narial openings and armor patterns. No additional species have been formally recognized since , though undescribed material from ongoing Gobi expeditions continues to inform taxonomic reviews.

Description

Size and general features

Pinacosaurus was a medium-sized ankylosaurid, with adults estimated to attain a length of approximately 5 . Scaling from subadult and juvenile specimens indicates that younger individuals ranged from 1.3 to 2.5 in length. Body mass for adults is estimated at around 1 to 2 tonnes. The general build of Pinacosaurus was low-slung and flat-bodied, earning it the name meaning "plank lizard," with a broad pelvic and short, robust limbs supporting quadrupedal . This compact form was adapted for low-level among . Distinguishing morphological traits include keeled osteoderms covering the back and flanks, an armored cap formed by fused dermal bones, and the absence of osteoderms on the belly. Adults possessed a small , which was less developed or absent in juveniles. Compared to relatives such as and , Pinacosaurus was smaller and more gracile, with a less robust .

Skull

The of Pinacosaurus is triangular in view and measures approximately 30 cm in length in adults. It features fused nasal and lacrimal bones that contribute to a low boss along the , with the quadrate bones oriented vertically to facilitate efficient closure. The narial region exhibits species-specific variations, with P. grangeri possessing five external nares per side in a complex, fenestrated arrangement interpreted as related to , while P. mephistocephalus has three such nares. Ornamentation includes low, rounded squamosal horns and asymmetrical bosses on the prefrontal and postorbital regions, with the dorsal surface covered by numerous small osteoderms known as caputegulae. The consists of acrodont teeth with leaf-shaped crowns, numbering about 14–17 per , adapted for shearing tough vegetation as evidenced by their multiple cusps; wear patterns on the crowns further indicate a grinding component to feeding. Sensory features include large orbits, up to 45 mm wide, suggesting enhanced , and a possible pit for Jacobson's organ in the vomeronasal region, potentially aiding olfaction.

Postcranial skeleton and armor

The postcranial of Pinacosaurus is characterized by a robust axial column adapted for a quadrupedal stance. The vertebral series includes low neural spines that contribute to the animal's low-slung profile. In individuals, sacral occurs, incorporating multiple vertebrae into a reinforced for enhanced pelvic stability. The reflects the quadrupedal locomotion of Pinacosaurus, with forelimbs significantly shorter than the hindlimbs. The is notably robust, featuring a prominent deltopectoral that supports powerful musculature. The manus retains five digits in a pentadactyl configuration, though with reduced phalangeal counts compared to more basal ornithischians, facilitating weight distribution. The features broad ilia that flare outward, providing a wide base for stability during movement. The consists of 20–25 caudal vertebrae, distally stiffened and terminating in a defensive in subadult and adult specimens. This is formed by a handle of 4–6 osteoderms encasing the distal vertebrae, topped by 3–4 enlarged osteoderms that create a bulbous striking surface. Dermal armor dominates the postcranial , arranged in transverse bands of keeled osteoderms measuring 5–10 in along the neck, back, and tail, offering layered protection against predation. A distinctive pelvic shield arises from fused plates over the hips, reinforcing the ventral-lateral region, while the absence of ventral armor leaves the underbelly relatively exposed. Ontogenetic changes are evident in the postcrania, particularly in armor and tail structures. Juvenile specimens display smoother, less developed osteoderms and lack a fully formed , with these features maturing through fusion and enlargement in subadults and adults.

Classification and phylogeny

Taxonomic history

Pinacosaurus was first described and named by Charles W. Gilmore in 1933, based on a nearly complete juvenile (AMNH 6523), lower jaws, and fragmentary postcranial elements from the Djadokhta Formation at Bayn Dzak (Shabarakh Usu), ; Gilmore assigned it to the family , but highlighted the absence of a in the as a potential nodosaurid-like trait attributable to its immature ontogenetic stage. By the mid-20th century, additional specimens prompted re-evaluations that solidified its ankylosaurid affinities, with W. P. Coombs's 1978 analysis emphasizing similarities in armor patterning and leaf-shaped teeth to other genera like . A brief consideration of subfamily placement within Ankylosaurinae followed from these dental and osteodermal comparisons. In the 1990s and 2000s, revisions by Walter P. Coombs confirmed as a definitive ankylosaurid through comparative analysis of postcranial armor and tail structures across Asian specimens. The 1999 description of a possible second species, P. mephistocephalus, from the in —distinguished by unique narial openings and paired prefrontal horns—further supported its ankylosaurine status within , although its validity as a distinct species has been debated, with some researchers considering it a synonym of P. grangeri or an ontogenetic variant. Since 2010, Pinacosaurus has maintained a stable classification in , with phylogenetic placements consistently recovering it as a basal ankylosaurine. Studies in 2023 on new juvenile material, including an ossified from a Mongolian specimen, reinforced this by demonstrating ankylosaurid-specific traits such as fused osteoderms and the lack of nodosaurid features like prominent lateral scutes or .

Phylogenetic analyses

Phylogenetic analyses consistently place Pinacosaurus within as an early-diverging member of Ankylosaurinae, often as the sister to a comprising more derived ankylosaurines such as Gobisaurus and Shamosaurus. This positioning is supported by shared traits including keeled along the body and narial fenestrae that contribute to the complex nasal passages typical of ankylosaurids. A seminal cladistic analysis by Burns et al. (2011), incorporating juvenile specimens, utilized a matrix of 23 taxa and 66 morphological characters (50 cranial and 16 postcranial/) to recover Pinacosaurus as the most basal ankylosaurine, highlighting its primitive features relative to later Asian forms. This study emphasized synapomorphies such as the posterior embayment of nasal ornamentation and unenclosed paranasal apertures, which distinguish it from outgroups while affirming its ankylosaurine affinities. Subsequent work, including revisions incorporating ontogenetic data from additional juvenile material, has reinforced this basal placement within Ankylosaurinae, scoring approximately 65 characters to confirm relationships among Asian taxa. Key synapomorphies linking Pinacosaurus to other Asian ankylosaurids include asymmetrical squamosal horns that project laterally from the skull, thecodont dentition featuring low-crowned, leaf-shaped teeth suited for abrasive vegetation, and a primitive morphology featuring polygonal osteoderms arranged in a knob-and-hammer configuration. These features underscore its role as a transitional form in ankylosaurine evolution. It is distinguished from the by the presence of a tail club and a fused pelvic shield formed by coalesced osteoderms, which are absent in nodosaurids. Debates persist regarding finer relationships, with some analyses suggesting a closer affinity to derived Asian genera like based on similarities in armor patterning, such as the arrangement of keeled scutes. However, the broader consensus from multiple matrices maintains Pinacosaurus in a basal position within Ankylosaurinae, with no significant revisions reported as of 2025.

Paleobiology

Diet and feeding

Pinacosaurus was a herbivorous that functioned as a low-level , primarily consuming tough, low-growing such as ferns, cycads, and horsetails in its Late Asian habitat. microwear in related basal ankylosaurines reveals steep wear facets and scratches indicative of from silica-rich , supporting a diet dominated by these fibrous, abrasive rather than softer materials. The feeding mechanism of Pinacosaurus involved a pincer-like at the anterior for cropping , complemented by a battery of over 60 small, leaf-shaped arranged in a single row for shearing and grinding. Its pleurokinetic enabled side-to-side motion, facilitating precise and palinal (rearward) grinding to process tough matter efficiently. A , supported by a complex hyobranchial apparatus including robust paraglossalia, likely aided in manipulating and positioning food within the before mastication. Digestion in Pinacosaurus lacked evidence of gastroliths, unlike some other herbivorous dinosaurs, but its expanded gut region suggests reliance on microbial to break down fibrous , analogous to processes in large herbivores. As a quadrupedal low browser, Pinacosaurus occupied a niche that minimized with taller herbivores like hadrosaurs, potentially allowing selective feeding on fruits or softer growth in localized oases amid its dune-dominated landscape.

Growth and ontogeny

The fossil record of Pinacosaurus is dominated by juvenile and subadult specimens, with over two dozen partial to complete skeletons documented, the majority representing individuals under half the estimated adult body length. These young individuals typically measure around 1–2 meters in length, as seen in assemblages from sites such as Bayan Mandahu in China and Alag Teeg and Ukhaa Tolgod in Mongolia. Bone histology from ankylosaur long bones, including those referable to Pinacosaurus, reveals an ontogenetic series characterized by early deposition of woven-fibered bone indicative of relatively rapid initial growth, transitioning to parallel-fibered bone with poorer vascularization in later stages, suggesting a deceleration toward maturity. This pattern aligns with broader ankylosaur growth curves, where juveniles exhibit high metabolic rates during the first few years before slowing. Developmental changes in Pinacosaurus are evident in the and armor. Juvenile specimens, such as IGM 100/1014 from Ukhaa Tolgod, display unfused cranial sutures and secondary dermal ossifications that remain loosely attached to the roof, particularly along the and temporal regions, with osteoderms appearing smooth and underdeveloped. The is rudimentary in these early stages, consisting of small, unfused osteoderms rather than the robust, fused structure inferred for adults through comparison with more mature ankylosaurines. Extrapolation from these features indicates that fusion of armor and cranial elements progressed during subadulthood, enhancing structural integrity for defense. The abundance of juvenile Pinacosaurus in mass bonebeds points to gregarious among young individuals. At Alag Teeg, nearly 100 skeletons—predominantly immature—were preserved in close proximity, often with articulated lower limbs in upright positions, suggesting group mortality events in dune environments. Similar clustering at Ukhaa Tolgod, including multiple partial skeletons in life positions, supports the formation of herds or groups, potentially involving to protect vulnerable juveniles from predators. Taphonomic evidence from these sites indicates rapid burial in aeolian sands, preserving evidence of social aggregation without significant post-mortem transport. No fully adult Pinacosaurus skeletons are preserved, likely due to preservation bias favoring smaller, more numerous juveniles or rarer longevity in adults, though subadulthood appears to have been reached after several years of . A histological analysis of ankylosaur bones, including implications for Asian taxa like Pinacosaurus, confirms a determinate growth strategy, with extensive remodeling and lines of arrested growth marking the transition to slower deposition and skeletal maturity, addressing prior gaps in understanding ankylosaur .

Vocalization and senses

A 2023 study examining the hyolaryngeal apparatus of the grangeri specimen IGM 100/3186 identified an ossified consisting of cricoid and arytenoid elements, marking the first such preservation in a non-avian . This structure features a firm yet kinetic cricoid-arytenoid , akin to the of , which likely enabled closed-mouth vocalizations such as chirps, hisses, or croaks for intra-species signaling rather than the open-mouthed roars typical of larger theropods. The 's role appears to have been in modulating airflow and enhancing acoustic communication, potentially for coordination, displays, or territorial interactions, drawing parallels to sound production in modern like parrots or passerines. Subsequent research in 2025 on the neornithischian Pulaosaurus qinglong uncovered a second ossified in a non-avian , reinforcing that such specialized vocal structures evolved within ornithischians and were not unique to Pinacosaurus but remained rare among known specimens. Juveniles, often preserved in gregarious assemblages indicative of , may have employed these calls for predator evasion or social cohesion within herds. However, inferences remain limited to this single Pinacosaurus specimen, with no direct audio reconstructions possible due to the absence of soft tissues. Beyond vocalization, Pinacosaurus exhibited sensory adaptations suited to its herbivorous lifestyle. The skull's large external nares and extensive nasal passages suggest a well-developed sense of olfaction for detecting or environmental cues during . A possible , inferred from a ventral , may have aided in chemosensory detection of pheromones or chemical signals. Preserved sclerotic rings in related ornithischians indicate diurnal , with eye morphology adapted for daytime activity rather than low-light conditions. There is no evidence for specialized senses like electroreception, consistent with the anatomy of other non-aquatic ornithischians.

Paleoenvironment and paleoecology

Geological formations

Fossils of Pinacosaurus are primarily known from the in the of southern , which dates to the stage of the . The formation consists predominantly of eolian sandstones deposited in desert dune environments interspersed with intermittent fluvial channels and ephemeral ponds. These sedimentary facies reflect a dynamic landscape of wind-blown dunes modified by occasional water flow, with no evidence of volcanic activity influencing deposition. Taphonomic evidence indicates that Pinacosaurus specimens, including articulated skeletons, were preserved in cross-bedded sands and structureless sandslide deposits, likely due to rapid from floods, dune collapses, or sandstorms. The arid paleoclimate featured seasonal , supporting sparse in riparian zones along intermittent rivers, while interdune areas remained largely barren. Age constraints for the formation are based on and , placing it at approximately 75–71 million years ago. Specimens of Pinacosaurus also occur in the of , , a stratigraphic equivalent to the and likewise of age. This unit comprises fluvial and lacustrine deposits with and eolian sands, signifying localized wetter oases amid a broader semi-arid setting. Fossils, often small- to medium-sized and including juveniles, are typically embedded in eolian layers as autochthonous assemblages, preserved following events such as sandstorms that concentrated remains in low-energy interdune areas. Stratigraphically, the Djadochta Formation correlates with the lower portions of the overlying Nemegt Formation and similar horizons elsewhere in the Gobi Basin, including the Alag Teer locality where undescribed Pinacosaurus material has been recovered from fluvial mudstones.

Fauna and interactions

Pinacosaurus inhabited a diverse Late Cretaceous ecosystem in the Gobi Desert region, sharing its environment with a variety of sympatric taxa in the Djadochta Formation of Mongolia. Key co-occurring dinosaurs included the ceratopsian Protoceratops andrewsi, the oviraptorid Oviraptor philoceratops, and the dromaeosaurid Velociraptor mongoliensis, reflecting a community dominated by small- to medium-sized herbivores and carnivores adapted to arid conditions. In the correlative Bayan Mandahu Formation of Inner Mongolia, China, Pinacosaurus coexisted with additional taxa such as the dromaeosaurid Linheraptor exquisitus, indicating similar faunal assemblages across these formations. Predatory interactions likely involved dromaeosaurids, with evidence of theropod bite marks reported on ankylosaur osteoderms in general, suggesting scavenging or attempted predation on armored herbivores like Pinacosaurus. The of Pinacosaurus, formed by fused osteoderms at the tail's end, has been interpreted as a defensive capable of delivering impactful strikes against small theropods. Although direct evidence for intraspecific use exists in other ankylosaurids, the structure's role in deterring agile predators such as Velociraptor aligns with the absence of larger tyrannosaurids in these ecosystems. Competition for resources occurred among low-browsing herbivores, with Pinacosaurus potentially overlapping in dietary niche with , both targeting tough, low-lying vegetation in a resource-scarce arid landscape; however, dental analyses indicate some partitioning based on plant toughness. Crocodylomorphs, such as from the , may have engaged in scavenging of Pinacosaurus remains, contributing to taphonomic patterns in bonebeds. Bonebeds of multiple Pinacosaurus individuals, often preserved in close proximity and life positions, provide strong evidence for gregarious behavior, suggesting structures that facilitated collective defense against predators. No direct fossil evidence exists for in Pinacosaurus, but amber inclusions demonstrate infestations on other dinosaurs, implying similar ectoparasite burdens for armored taxa via ecological analogy. The Djadochta Formation's ecosystem lacked top-down control from large apex predators like tyrannosaurids, with predation pressure primarily from smaller dromaeosaurids and oviraptorids in an arid, eolian-dominated environment of dunes and oases. This setting favored survival of heavily armored herbivores such as , whose osteoderms and low-slung posture provided protection amid sparse vegetation and episodic sandstorms.

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