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Shringasaurus
Shringasaurus
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Shringasaurus
Temporal range: Middle Triassic, 247–242 Ma
Composite skeleton from the fossils of multiple individuals
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Archosauromorpha
Clade: Crocopoda
Clade: Allokotosauria
Family: Azendohsauridae
Genus: Shringasaurus
Sengupta et al., 2017
Species:
S. indicus
Binomial name
Shringasaurus indicus
Sengupta et al., 2017

Shringasaurus (meaning "horned lizard", from Sanskrit शृङ्ग (śṛṅga), "horn", and Ancient Greek σαῦρος (sauros), "lizard") is an extinct genus of archosauromorph reptile from the Middle Triassic (Anisian) of India. It is known from the type and only known species, S. indicus. Shringasaurus is known from the Denwa Formation in the state of Madhya Pradesh. Shringasaurus was an allokotosaur, a group of unusual herbivorous reptiles from the Triassic, and is most closely related to the smaller and better known Azendohsaurus in the family Azendohsauridae. Like some ceratopsid dinosaurs, Shringasaurus had two large horns over its eyes that faced up and forwards from its skull. Shringasaurus also bears convergent physical similarities to sauropodomorph dinosaurs, such as its long neck, its shoulders and forelimbs, and the shape of its teeth. Shringasaurus possibly occupied a similar ecological niche as a large browsing herbivore before such dinosaurs had evolved.[1][2]

Description

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Skeletal restoration and various bones of Shringasaurus.

Shringasaurus was a large-bodied quadruped, with an estimated body length of 3–4 metres (9.8–13.1 ft). It closely resembles the related Azendohsaurus, with its small, boxy head on a long neck and a large, barrel-shaped body with deep shoulders and ribs, sprawled to semi-sprawled limbs and a short tail. Aside from being notably larger than Azendohsaurus, Shringasaurus is most recognisable for its long curving brow horns, as well as for having a proportionately shorter and thicker neck than other azendohsaurids and much taller neural spines in the neck and over the shoulders.[1]

Skull

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The skull of Shringasaurus is not completely known, but what's preserved indicates that the skull was small and boxy, with a short, deep snout with rounded jaw tips and bony nostrils fused into a single, confluent opening at the front of the snout. This is broadly similar to the completely known skull of Azendohsaurus, but the lower jaw of Shringasaurus has a more conspicuous taper towards the tip compared to the deep, down-turned dentary of the Azendohsaurus.[1][3]

The horns of Shringasaurus closely resemble those seen in ceratopsid dinosaurs, despite azendohsaurids and ceratopsids being totally unrelated to each other. The horns are attached to the frontal bones on the roof of the skull over the eyes, and sit across almost the entire breadth of the skull. They are pointed up and curve forwards from the skull, with slight variation in size and orientation existing among large individuals. Smaller and younger individuals had smaller, more gracile horns, indicating that the horns did not fully develop until the animals were mature. Intriguingly, at least one small specimen lacks horns entirely, whereas another similarly small specimen has small but well developed horns. It is suggested then that Shringasaurus was sexually dimorphic, and that possibly the females lacked horns.[1]

The horns themselves have a rough, grooved texture that implies they were covered with a keratinous sheath of horn in life, also like ceratopsid horns, and so would have likely been longer than the bony cores indicate.[4][5] The bones of the skull beneath the horns are unusually thick, and in the larger individuals the bones of roof of the skull (the nasal, prefrontal, frontal and postfrontal) are fused together on each side.[1]

Speculative reconstruction showing battle-scars made by other Shringasaurus
Life restoration

The teeth of Shringasaurus are low and leaf-shaped (lanceolate) with large denticles on either side, similar in shape to those of Azendohsaurus but lacking the prominent expansion above the root, like the teeth of Pamelaria. Because the skull and jaws are incompletely known, the total tooth count of Shringasaurus is unknown, but like Azendohsaurus it had four teeth in each premaxilla. Shringasaurus also had numerous palatal teeth (though known only from the vomer thus far), and like Azendohsaurus they are uniquely as well developed as the marginal teeth along the edge of the jaw. Like them, they were leaf-shaped and serrated, but in Shringasaurus the palatal teeth are even more lanceolate than the marginal rows.[1] Such palatal teeth are unusual, as most other herbivorous reptiles with them have much simpler, domed palatal teeth, and palatal teeth identical to those of the jaw margins are otherwise only found in the related allokotosaurs Azendohsaurus and Teraterpeton.[3][6]

Skeleton

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Femur, tibia and fibula of Shringasaurus.

The vertebral column is well known in Shringasaurus, including the whole cervical series, various dorsal vertebrae, both sacral vertebrae and some caudal vertebrae. Like other azendohsaurids, the first-through-middle cervical vertebrae are characteristically elongated, giving Shringasaurus a long, raised neck, although it is proportionately shorter than in Azendohsaurus and Pamelaria. The neck is also much taller than in other azendohsaurids, with tall, prominent neural spines. This trend continues into the dorsals of the back, which although are not as long as the cervicals have neural spines twice the height of their centra. The 2nd–5th cervicals of Shringasaurus sport prominent epipophyses, structures for supporting neck musculature. The first twelve dorsals are also marked by various well-defined laminae that bound deep fossae (depressions in the bone), similar to those found on the vertebrae of sauropods. Like Azendohsaurus, Shringasaurus has two sacral vertebrae with well-developed ribs that articulate with the ilia.[1]

The shoulder and forelimb are broadly similar to those of Azendohsaurus, with a tall scapula that is concave along the front with an expanded tip, and an interclavicle with a long paddle-like process on the back and a short forward-pointing process (an unusual feature for archosauromorphs but also found in Azendohsaurus). The coracoid articulates with the scapula to form a glenoid (shoulder socket) that faces out to the sides and back. The humerus is likewise similar, with broad ends and a narrow midshaft, and a very well-developed deltopectoral crest half as long as the whole bone, indicating powerful forelimbs. The ulna, however, can be distinguished by a lower olecranon process below the elbow than in Azendohsaurus.[1]

The hips and hind limbs are very similar to those of Azendohsaurus. The ilium has a prominent, semi-circular process at the front while the rear process is longer and thinner, and the acetabulum (hip socket) is also solid, unlike the perforated hip socket of dinosaurs. The femur is robust and slightly s-shaped, held out to the sides in a sprawl, with a robust tibia and a fibula only half as wide in the lower leg. The foot is typical for early archosauromorphs, including Azendohsaurus.[1]

Discovery and naming

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Shringasaurus is known from a single bone bed of fossils in the upper Denwa Formation, India. The formation is part of the Satpura Gondwana Basin, located in the Hoshangabad district in the state of Madhya Pradesh. The precise age of the Denwa Formation is not known, but vertebrate biostratigraphy has been used to narrow it down to a range in the early Middle Triassic with conflicting opinions on an early or late Anisian age.[7][8] The upper Denwa Formation is characteristically dominated by red mudstones with ribbon-shaped sandstone sheets encased within them.[1] The bonebed itself was preserved in a crevasse splay deposit composed of cross-bedded, dipped sandstone with irregular boundaries that breached along the south edge of an ancient filled river channel. This flooding event was unlikely to be an isolated event, as the size of the crevasse splay suggests multiple phases of flooding that cumulatively buried the remains of the herd.[9]

Maps detailing the location of the Shringasaurus bone bed.

The Shringasaurus bone bed consists of mostly disarticulated bones (although one partial skeleton was found in articulation) scattered within a 5 m X 5 m (25 square metres (270 sq ft)) area of red mudstone with fine, sandy laminations. The bonebed is monodominant, only containing fossils of Shringasaurus, and preserves eight individuals based on the minimum number of unique right femora, left humeri, skull roofs and horns discovered. The specimens also represent a variety of different ontogenetic stages of growth with a wide range of body sizes, from juveniles to adults. Of these individuals, only one or two lacked horns, and it's suggested that the bone bed was taphonomically biased towards the heavier, solidly built skulls of horned individuals while being transported and preserved.[1][9][10]

However, the retention of bones rapidly lost in transport (such as ribs and limb bones), as well as minimal abrasion to many of the bones, indicates they were not transported a great distance after death. Although the bones were later disarticulated after transportation (apart from a single series of six dorsal vertebrae and ribs), they remained in closely associated clusters. They also show little weathering, indicating that most of the bones only remained exposed on the surface for perhaps only 1–3 years, with only a few exposed for longer (3–15 years). The articulated vertebrae, found lowest in the bonebed, was likely buried immediately, while the remaining bones higher in the bonebed were buried by subsequent floods. Similarly, the bones show now signs of trampling or marks from scavenging and plant growth, indicative of their short exposure before burial.[9]

The fossils were excavated and prepared by Professor Saswati Bandyopadhyay, Dhurjati Sengupta and Shiladri Das of the Indian Statistical Institute, Kolkata, where the fossils are also stored. It was then described and named in August 2017 by Sarandee Sengupta and Bandyopadhyay, as well as by Martín D. Ezcurra of the Bernardino Rivadavia Natural Sciences Argentine Museum in Argentina. The holotype specimen, ISIR 780, consists of a partial skull roof including the prefrontal, frontal, postfrontal and parietal bones, along with a pair of large supra-orbital horns. The various other specimens from the bone bed have been designated as paratypes and consist of multiple cranial and postcranial bones from much of the skeleton. The genus was named using the ancient Sanskrit word for "horn", 'Śṛṅga' (शृङ्ग), for the unique horns on its skull, combined with the Ancient Greek σαῦρος (sauros) for "lizard". The specific name indicus is Latin for "Indian", to refer to its country of discovery.[1]

Classification

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Shringasaurus is recognised as a member of the family Azendohsauridae, and as the closest relative of Azendohsaurus itself. The family is typically grouped within the recently recognised clade Allokotosauria, along with the trilophosaurids, as was recovered by Sengupta and colleagues when they described Shringasaurus and analysed its phylogenetic relationships in 2017.[1] Another analysis of archosauromorph relationships in 2019 that used a different dataset from Sengupta et al. (2017)—that of Pritchard et al. (2018)[11]—was updated to include Shringasaurus, and similarly recovered it and Azendohsaurus as each other's closest relatives within Allokotosauria, further supporting an azendohsaurid affinity for Shringasaurus.[12]

The results found by Sengupta and colleagues in 2017 is shown below as an excerpt of the full cladogram, simplified and focused on the relationships of Shringasaurus to other allokotosaurs:[1]

Skull diagram of Azendohsaurus, the closest relative of Shringasaurus.
Crocopoda

Shringasaurus and other azendohsaurids share several features, including confluent nares, leaf-shaped teeth and a long neck, as well as a few other minor details of the skeleton. It is particularly similar to Azendohsaurus in features of the parietals, the lower jaw, shoulder, hip, femur and vertebrae, but can be distinguished by teeth that are not expanded above the roots, the lack of a groove on the inside surface of the maxilla, tall neural spines, and of course the horns.[1]

Palaeobiology

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The Shringasaurus bonebed suggests that it was a gregarious animal that lived in herds. The herd appears to have died in a mass mortality event and was buried in a short span of time, possibly drowned by a breached levee. The bonebed includes juveniles, sub-adults and adults, further suggesting that Shringasaurus lived in mixed-age herds. The herd was also mixed-sex, based on the presence of both purported males and females, although it is unclear if they lived mixed-sex year round or if they only did so during part of the year, namely the breeding season (as observed in domestic sheep and related herbivores where males similarly spar with their horns). The herd was likely congregating around a nearby river channel during a period of environmental stress such as a drought, as occurs in living herbivores and has also been inferred for some dinosaurs.[9]

Function of the horns

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Reconstruction of the skull and horns compared to that of the ceratopsid dinosaur Arrhinoceratops, and a comparison of various horns from different sized individuals, including a possibly female hornless specimen.

The horns of Shringasaurus are its most prominent feature, and so some focus was placed on their role and function in its initial description. Its describers considered its horns to be likely products of sexual selection, not primarily for defence or species recognition (as has been proposed for the head ornaments of dinosaurs).[13] The horns grow notably larger and more robust in large adults, while smaller individuals have shorter and more graceful horns. The possibility that Shringasaurus was sexually dimorphic, with probable females lacking horns, further supports this interpretation. This would be similar to modern horned bovids, but unlike ceratopsid dinosaurs, and indeed other archosauromorphs, which do not appear to have been dimorphic.[1]

Palaeopathology

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One specimen of Shringasaurus is known to have had a pair of malformed vertebrae in its neck. The two cervicals are partially fused together, interpreted as either the result of a birth defect, spondyloarthropathy (a type of arthritis), or possibly a bacterial or fungal disc infection. The vertebrae belonged to a large adult animal, so it is unlikely that the quality of life for the individual was severely affected by the disorder, and it was probably not fatal to the animal. One of the vertebrae also preserves a healed fracture, although the cause for this injury is unknown.[10]

Palaeoecology

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Life restoration

In the upper Denwa Formation, Shringasaurus coexisted with the lungfish Ceratodus sp. and a variety of temnospondyl amphibians, including the capitosaurid Paracyclotosaurus crookshanki, the mastodonsaurid Cherninia denwai, a lonchorhynchine trematosaurid, and a brachyopid. Other terrestrial vertebrates include a large undescribed rhynchosaur and two species of dicynodonts, a mid-sized species similar to Kannemeyeria and a larger species interpreted as similar to Stahleckeria.[1][7][14] The environment is interpreted as representing a dry, semi-arid floodplain with slow moving, anabranching rivers that periodically burst their banks. Rainfall was seasonal, and the environment experienced droughts that dried up ephemeral rivers and ponds.[1][14][15] The large body size of Shringasaurus and its convergent similarity to sauropodomorphs—including its jaws and teeth as well as a superficially similar body shape—suggests that it possibly occupied the role of a large, relatively high-browsing herbivore in its environment.[1]

References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Shringasaurus is a of extinct herbivorous allokotosaurian archosauromorph reptile that lived during the early epoch ( stage, approximately 247 million years ago) in what is now . The type and only recognized species is Shringasaurus indicus, known from partial skeletons including a distinctive bearing large supraorbital horns, which exhibit with males possessing prominent paired horns projecting anterodorsally from above the eyes. This quadrupedal reptile reached a total body length of 3–4 meters, with a long neck, small head, and robust limbs adapted for supporting its herbivorous lifestyle as a primary consumer in its fluvial . The fossils of Shringasaurus indicus were discovered in the upper part of the Denwa Formation within the Satpura Basin, near Tekapar village in the of , . The specimen (ISIR 780) consists of a partial with attached supraorbital horns, while referred specimens include additional cranial elements, vertebrae, ribs, and limb bones from multiple individuals, indicating a bonebed accumulation in red deposits of an anabranching system. The genus was formally described and named in 2017, with "Shringasaurus" deriving from the word śṛṅga (horn) and Greek sauros (lizard), and indicus referring to its Indian provenance; the name highlights its most striking feature, the pair of conical horns ornamented with rugosities and grooves, which are comparable in form to those of later ceratopsid dinosaurs but appeared over 100 million years earlier. Systematically, Shringasaurus is classified within the clade , a group of unusual non-archosauriform archosauromorphs that also includes Azendohsaurus and Pamelaria, and is specifically placed in the family Azendohsauridae as the sister taxon to Azendohsaurus. Phylogenetic analyses support this placement with robust metrics, such as a Bremer support value of 4 for Azendohsauridae, underscoring its position as a stem-archosaur outside the crocodylomorph-dinosaur lineage. Anatomically, the is proportionally small with a short, rounded and confluent external nares, while the postcranium features elongated (about 1.5 times longer than tall) contributing to its long neck, tall neural spines on dorsal vertebrae, and sturdy limb elements suggesting a terrestrial, browsing . The presence of dimorphic horns in adults—absent or reduced in some individuals, presumed females—implies potential use in intrasexual combat or display, broadening the known morphological diversity of Early-Middle tetrapods. As one of the earliest known large herbivorous archosauromorphs, Shringasaurus represents an important evolutionary experiment in reptile diversity, filling an later dominated by dinosaurs and highlighting the of horned structures in unrelated lineages. Its discovery expands understanding of the , a that flourished briefly in the Early to before going extinct by the , demonstrating the rapid radiation of archosauromorphs following the Permian- .

Discovery and naming

Geological context

The fossils of Shringasaurus indicus were recovered from the upper part of the Denwa Formation in the Satpura Basin, , , with the primary locality situated near Tekapar village in the . This stratigraphic unit is assigned to the , specifically the stage (approximately 247–242 million years ago), based on vertebrate that includes the temnospondyl genus Paracyclotosaurus. The of the upper Denwa Formation reflects a semi-arid setting influenced by an anabranching fluvial system, featuring red mudstones as dominant deposits, sandy/muddy heterolithic sheets representing splay events, and isolated ribbon-shaped channel-fill bodies indicative of mixed- to suspended-load sinuous channels. The semi-arid paleoclimate is evidenced by the presence of calcic paleosols and the red coloration of the mudstones, suggesting periodic with seasonal . Globally, the upper Denwa Formation correlates with the late Anisian subzone C of the Cynognathus Assemblage Zone in South Africa and the Ashfield Shale of the Sydney Basin in Australia, highlighting its position within early Middle Triassic Gondwanan terrestrial ecosystems that also hosted contemporaneous taxa such as dicynodonts and temnospondyls.

Fossil discoveries

Fossils of Shringasaurus indicus were first discovered during expeditions conducted by the Indian Statistical Institute in the 1970s and 1980s in the Satpura Gondwana Basin, central India. These efforts targeted the Denwa Formation, yielding disarticulated and partially articulated skeletal remains from a bonebed spanning approximately 25 m². The specimen, ISIR 780, consists of a partial roof including the prefrontal, frontal, postfrontal, and parietal bones, with the supraorbital horns preserved , from an adult individual. Referred specimens, cataloged as ISIR 781–1072, encompass additional cranial elements and extensive postcranial material such as (e.g., ISIR 785–789), limb bones, and elements from at least seven individuals representing various ontogenetic stages. These remains indicate multiple partial skeletons accumulated in a single locality near Tekapar village, . In 2017, an additional specimen featuring fused anterior (ISIR 811–812) was described, providing evidence of vertebral anomalies in Shringasaurus. Taphonomically, the fossils are preserved within red layers of the upper Denwa Formation, consistent with rapid in deposits of an anabranching river system. This preservation suggests minimal post-mortem transport for many elements, though some occurred prior to .

Etymology and validity

Shringasaurus indicus was formally named and described in 2017 by paleontologists Sarandee Sengupta, Martín D. Ezcurra, and Saswati Bandyopadhyay in the journal . The description established it as a new and of allokotosaurian archosauromorph based on material from the Denwa Formation. The name Shringasaurus derives from the word śṛṅga, meaning "horn," combined with the Greek sauros, meaning "lizard," in reference to the distinctive pair of supraorbital horns on the . The specific epithet indicus is Latin for "Indian," honoring the country of discovery. The type locality is situated near Tekapar village in the , , , approximately 50 kilometers from . The , designated ISIR 780, comprises a partial roof including the prefrontal, frontal, postfrontal, and parietal bones, with the supraorbital horns preserved . Since its original description, Shringasaurus indicus has been upheld as a valid and distinct taxon within , with no junior synonyms proposed or alternative generic assignments suggested in subsequent studies.

Description

Overall morphology

Shringasaurus indicus was a large-bodied, quadrupedal archosauromorph that reached an estimated total body length of 3–4 meters in adulthood. Its build was stocky and robust, characterized by a relatively short tail and powerful limbs adapted for supporting its weight on all fours. The animal exhibited herbivorous adaptations, including a proportionally long and muscular that allowed for high browsing on , showing convergence with the body plan of early sauropodomorph dinosaurs. This facilitated access to elevated plant matter in its environment. The general morphology featured tall neural spines on the , which were proportionally taller than those in related taxa and may have contributed to a slight sail-like structure along the neck. Evidence from multiple specimens suggests , with larger supraorbital horns present in presumed males, while some individuals lacked prominent horns, possibly indicating females. Overall, Shringasaurus displayed a distinctive combination of features that set it apart from other early archosauromorphs, emphasizing its role as a primary with specialized anatomical traits for its .

Cranial anatomy

The of Shringasaurus indicus is proportionally small and boxy, with a short, rounded and confluent external nares that fuse into a single opening anteriorly. This configuration contributes to a compact cranial profile adapted for herbivory, where the fused nares likely facilitated efficient during feeding. A defining feature is the pair of prominent supraorbital horns, which project anterodorsally in a sub-conical shape and are almost equal in height to the rest of the in large adult individuals. These bony cores are ornamented with tangential rugosities and grooves, indicating they were sheathed in for enhanced durability and possibly sensory function. The horns exhibit , with some specimens lacking them entirely, suggesting variation between sexes or ontogenetic stages. Dentition in Shringasaurus supports its herbivorous lifestyle, featuring low, leaf-shaped marginal teeth with serrated edges bearing large denticles on both margins for shearing tough . The palatal teeth, including those on the pterygoid and , are similarly formed and bulbous-based, aiding in grinding plant material against the . There are four premaxillary positions, with crowns that are slightly bulbous at the base. The braincase is characterized by a parabasisphenoid with an oblique, anteroventrally slanting main axis, while the orbits are relatively large, bordered mostly by thick prefrontal and postfrontal bones that nearly exclude the frontal from the margin, implying enhanced . This orbital arrangement, combined with the short snout, underscores adaptations for precise foraging in a forested environment. The supraorbital horns of Shringasaurus show convergent morphology with those of ceratopsid dinosaurs, such as Arrhinoceratops brachyops, in their anterodorsal projection and sub-conical form, though arising from distinct phylogenetic lineages.

Postcranial skeleton

The postcranial skeleton of Shringasaurus indicus is characterized by a robust axial column adapted for supporting a quadrupedal body plan, with preserved elements including cervical, dorsal, sacral, and caudal vertebrae. The cervical vertebrae exhibit elongated centra that are approximately 1.5 times longer than tall, contributing to a relatively long neck; at least nine cervicals are indicated by the presence of mammillary processes on the fifth through ninth, and the neural spines are proportionally taller than those in close relatives such as Azendohsaurus madagaskarensis. Epipophyses are present on the second through fifth cervical vertebrae, while the anterior to middle cervicals feature high neural spines that enhance structural support. The dorsal region is robust, comprising 12 vertebrae in the holotype, with anterior dorsal neural spines reaching twice the height of the and all dorsals bearing mammillary processes; these vertebrae display prominent laminae, including paradiapophyseal, posterior centrodiapophyseal, prezygodiapophyseal, spinodiapophyseal, and spinoprezygapophyseal types, underscoring a sturdy thoracic framework. The sacral region consists of two vertebrae, the first slightly longer than the second, both with ribs of similar size, providing a stable articulation with the for in a quadrupedal stance. The features pillar-like limbs suited for weight-bearing, with the strongly constricted at mid-length and a deltopectoral crest extending half the bone's length, indicating robust support. The has a low process, and the is sigmoid in shape with a prominent internal and a distal end broader than the proximal, further emphasizing load-bearing capabilities; the fibular shaft is approximately two times narrower than the tibial shaft, contributing to a sturdy configuration. The astragalus includes separated tibial and fibular facets by a broad non-articular surface, with a fused lateral centrale bearing a broad tibial facet. The pectoral girdle comprises a with a concave anterior margin and moderate distal expansion for enhanced stability, a contributing to a posterolaterally oriented with a short post-glenoid process, a T-shaped interclavicle featuring a short anterior process and long paddle-shaped posterior process, and a constricted near its ventral end. In the pelvic girdle, the ilium has a semi-circular preacetabular process, a longer and dorsoventrally shallower postacetabular process, and a fully closed with a low supraacetabular crest, all supporting quadrupedal locomotion; the pubis forms a transversely broad apron with an extensive plate-like contact to the . The is relatively short, with preserved elements that decrease rapidly in size; the anterior caudals bear mammillary processes and an intercentrum between them, while posterior caudals are less robust. Overall, these postcranial features align with an estimated total body length of 3–4 , reflecting adaptations for a large, herbivorous quadruped.

Phylogenetic analyses

The phylogenetic position of Shringasaurus indicus was first assessed in a comprehensive cladistic incorporating the into a modified dataset derived from prior studies on Permo-Triassic archosauromorphs. This utilized a matrix of 88 taxa ranging from early archosauromorphs to crown-group archosaurs and 620 morphological characters, with 14 new characters added to accommodate Shringasaurus and other allokotosaurs. Employing heuristic parsimony searches in TNT 1.5 software, the study recovered 48 most parsimonious trees of 4,277 steps, placing Shringasaurus indicus as a non-archosauriform crocopod within , specifically as the sister to Azendohsaurus in the clade Azendohsauridae. Support for this placement was provided by several synapomorphies diagnosing and Azendohsauridae, including a hook-shaped dorsal end of the quadrate for the former and, for the latter, confluent external nares, similarly sized leaf-shaped marginal and palatal teeth bearing large denticles, mammillary processes on neural spines of middle-posterior cervical, dorsal, and anterior caudal vertebrae, and hyposphene-hypantrum accessory articulations in those same vertebrae. Branch support metrics indicated moderate stability, with Bremer support values of 2 for and 4 for Azendohsauridae, alongside bootstrap frequencies exceeding 50% for key nodes within . Key anatomical traits coded for Shringasaurus, such as its anterodorsally oriented supraorbital horns and elongated neck (with anterior-middle cervical centra approximately 1.5 times longer than tall), contributed to its resolution near Azendohsaurus. Subsequent phylogenetic analyses have corroborated this positioning. A 2021 study incorporating detailed osteological data from Shringasaurus indicus and related taxa, such as Malerisaurus robinsonae, confirmed Shringasaurus as the sister taxon to both species of Azendohsaurus within azendohsaurid allokotosaurs, supported by 21 synapomorphies (10 cranial and 11 postcranial). This analysis yielded strong branch support, including a Bremer value of 12 and bootstrap frequencies of 93% (both absolute and GC-resampled) for Allokotosauria.

Relationships within Allokotosauria

Shringasaurus indicus is classified within , a of non-archosaurian archosauromorphs that diverged early from the archosaur lineage, encompassing taxa with diverse body plans but unified by shared cranial, girdle, and limb features. Within this group, Shringasaurus belongs to the family Azendohsauridae, characterized by herbivorous adaptations such as leaf-shaped and elongated that facilitate browsing in higher vegetation layers. These synapomorphies distinguish allokotosaurs from contemporaneous carnivorous pseudosuchians like rauisuchians, which possessed serrated, conical teeth suited for predation rather than herbivory. The closest relative of Shringasaurus is Azendohsaurus, known from Middle to Late Triassic deposits in and , forming a sister-taxon relationship supported by shared traits including a hook-shaped quadrate and robust postcranial elements. Azendohsaurus species were smaller, typically measuring around 2–3 meters in length, contrasting with the larger stature of Shringasaurus and highlighting size variation within Azendohsauridae. This positioning underscores the early diversification of herbivorous archosauromorphs in during the ( stage), approximately 242–247 million years ago, shortly after the Permo-Triassic mass extinction. Shringasaurus exemplifies the rapid of specialized ecomorphotypes in southern continents, filling ecological niches as large-bodied herbivores before the dominance of dinosaurian faunas. In terms of size evolution, Shringasaurus attained a peak body length of 3–4 meters among early allokotosaurs, exceeding that of its relatives and possibly reflecting adaptations for intra-specific or partitioning in forested environments.

Palaeobiology

Dietary habits

Shringasaurus indicus is inferred to have been herbivorous based on its , which features leaf-shaped marginal and palatal teeth with prominent serrations and denticles along the edges, adaptations suited for shearing and processing tough vegetation such as ferns, cycads, and other flora. These teeth closely resemble those of early sauropodomorph dinosaurs, another group of herbivorous archosauromorphs, reinforcing the interpretation of a . No gut contents have been preserved in known specimens, leaving as the primary evidence for dietary habits. The relatively long neck, with approximately 1.5 times longer than tall, combined with an elevated and quadrupedal posture, positioned Shringasaurus as a high browser capable of accessing elevated beyond the reach of smaller contemporaneous herbivores. This allowed it to exploit a niche for tall plants in the diverse Gondwanan ecosystems of the early , filling an ecological gap prior to the diversification of sauropodomorph dinosaurs in the . Jaw mechanics, inferred from the relatively small skull compared to its 3–4 meter body length, suggest a weak bite force appropriate for selective browsing and cropping foliage rather than powerful crushing or predatory actions. Stable isotope analyses on similar Triassic herbivorous taxa indicate a diet dominated by C3 plants, consistent with the global prevalence of such during this period, though direct isotopic data from Shringasaurus remains unavailable. As a large primary , Shringasaurus likely functioned as a selective feeder, targeting softer, higher foliage in vegetated settings, contributing to and vegetation control within its habitat.

Horn function and sexual dimorphism

The supraorbital horns of Shringasaurus indicus are robust, unbranched structures projecting from the frontal bones in adult specimens. These horns are interpreted as adaptations primarily for intrasexual combat and display, driven by rather than defense against predators or species recognition. Similar to the horns of ceratopsid dinosaurs and modern bovids, they likely served as weapons in male-male agonistic behaviors to secure access to receptive females, signaling individual quality and dominance. Evidence for is suggested by the variation in horn presence and size among specimens from the same bonebed. While most individuals exhibit well-developed horns, a pair of isolated frontals lacks any horn cores, interpreted as belonging to females or juveniles. In horned specimens, ontogenetic analysis reveals that horn size and robustness increase progressively toward adulthood, indicating growth post-hatching and maturation-linked exaggeration of these structures. This pattern aligns with pressures, where larger horns in presumed males enhance competitive success in or territorial disputes. Comparatively, the horns of Shringasaurus show convergence with those of mammals, such as bovids, and certain like chamaeleonids, where such features function in intraspecific signaling and combat. Behavioral inferences point to group-based interactions, potentially involving territorial displays or lekking systems, though direct evidence is limited to the anatomical correlates observed in the fossils.

Locomotion and pathology

Shringasaurus indicus was an quadruped characterized by a typical of allokotosaurs, with robust limb bones adapted for stability rather than speed. The and exhibit sigmoid curvature and a closed , supporting an upright yet sprawling posture that facilitated slow, deliberate movement suited to a among . Unlike sauropod dinosaurs, its relatively long —evidenced by cervical centra approximately 1.5 times longer than tall—was likely held horizontally or slightly elevated to access mid-level foliage, rather than raised high above the body. Documented pathologies in Shringasaurus fossils are limited but informative. Specimens ISIR 811 and 812 preserve two adjacent anterior that are longitudinally fused, a condition attributed to either congenital malformation (genetic or environmentally induced) or an infectious process, potentially nonspecific spondyloarthropathy. This represents the earliest reported vertebral in an Indian archosauromorph, highlighting that such disorders affected basal members of the group similar to later dinosaurs and modern vertebrates. Among the bonebed assemblage, which includes remains from at least eight individuals, overt are rare, indicating a generally robust and healthy capable of surviving injuries or developmental anomalies. The concentration of multiple skeletons in a confined 25 area suggests gregarious habits, where social grouping may have offered protection from predators and facilitated recovery from injuries, as inferred from the low incidence of lethal pathologies. No skeletal features, such as flattened ribs or modified limb proportions, indicate aquatic adaptations, aligning with its terrestrial herbivorous ecology in a fluvial environment.

Palaeoecology

The upper Denwa Formation, from which Shringasaurus indicus fossils derive, represents a mudstone-dominated fluvial characterized by an anabranching to high-sinuosity meandering river system within a broad alluvial . Red mudstones, often pedoturbated, form the dominant extra-channel deposits, indicating stable s periodically inundated by overbank flows, while ribbon-shaped channel-fill bodies (2–5 m thick) composed of sandy or muddy inclined heterolithic strata reflect limited lateral accretion in sinuous channels. These sedimentary features suggest a low-gradient, low-energy fluvial regime with secondary splays and splay deposits contributing to fine-grained sedimentation. Paleoclimatic evidence points to a influenced by seasonal monsoons, fostering episodic flooding and sediment aggradation on the while allowing for periods of relative that supported in the red mudstones. Vegetation in this environment consisted of conifer-dominated woodlands interspersed with horsetails and ferns, reflecting a typical Gondwanan flora without the presence of angiosperms. Water bodies included perennial rivers, as inferred from sedimentary stability and the preservation of aquatic-adapted taxa, alongside lakes and abandoned channels that could become seasonally stagnant. Shringasaurus fossils occur within fine-grained mudrock horizons associated with crevasse splay deposits adjacent to channel complexes, where disarticulated and partially articulated bones show evidence of short-distance hydraulic transport during events, leading to localized accumulation in low-energy settings. This taphonomic pattern underscores the role of seasonal ing in concentrating remains near active fluvial channels. Regionally, the Denwa Formation accumulated in the Satpura Basin, one of several basins along the eastern margin of during the early stages of Pangea fragmentation in the .

Associated biota and interactions

Shringasaurus indicus coexisted with a diverse assemblage in the upper Denwa Formation of the Satpura Basin, , during the early ( stage, approximately 247 million years ago). This fauna included the Ceratodus sp., multiple temnospondyl amphibians such as Paracyclotosaurus crookshanki, Cherninia denwai, an undescribed brachyopid, and a lonchorhynchine trematosaurid, as well as an indeterminate rhynchosaurid and dicynodonts. These taxa represent a mix of aquatic, semi-aquatic, and terrestrial forms, highlighting a multifaceted with representatives from , amphibians, and synapsids alongside the herbivorous archosauromorph Shringasaurus. As a large-bodied reaching 3–4 meters in length, Shringasaurus likely functioned as a mid-level primary , browsing on in a community dominated by other herbivores like dicynodonts and rhynchosaurs, which may have shared similar dietary niches. The absence of crocodylomorphs or other large carnivorous archosaurs in the known assemblage suggests limited predation pressure on Shringasaurus, and no of predation—such as bite marks on bones—has been reported from the monospecific bonebed preserving a minimum of eight individuals across various ontogenetic stages and sexes, interpreted as a mixed-sex that experienced a likely due to during a in a crevasse splay near a perennial channel, with rapid minimizing post-mortem modification. This structure implies a relatively stable where Shringasaurus could have been a prominent browser, contributing to the trophic dynamics without apparent intense competitive or predatory interactions documented in the fossil record, and suggesting herding behavior. The Denwa Formation's tetrapod assemblage reflects the ongoing recovery and morphological diversification of Gondwanan vertebrates following the end-Permian mass extinction, with exemplifying the experimentation in body plans among early archosauromorphs during this phase of rebuilding. This underscores the as a period of increasing ecological complexity in southern landmasses, where herbivorous reptiles like Shringasaurus helped fill niches left vacant by earlier synapsid dominants.
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