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Austroraptor

Austroraptor cabazai is a large-bodied unenlagiine dromaeosaurid theropod dinosaur known from the Maastrichtian stage of the Late Cretaceous period in Patagonia, Argentina. The holotype specimen (MML-195), discovered in the Allen Formation at Bajo de Santa Rosa, Río Negro Province, consists of a partial skeleton including portions of the skull (e.g., maxillae, dentaries, frontals), vertebrae, ribs, a right humerus and manual ungual (forelimb elements), a left pubic shaft, and hindlimb bones (e.g., femur, tibia). Measuring approximately 5 meters in length with an estimated body mass of 368–460 kg, it represents the largest known dromaeosaurid from the Southern Hemisphere and the youngest record of a Gondwanan dromaeosaurid. The is characterized by a long, low approximately 80 cm in length, featuring 24 maxillary teeth and 25 dentary teeth that are small, conical, slightly recurved, unserrated, and longitudinally fluted—morphology reminiscent of piscivorous theropods like spinosaurids. Its are notably short, with a measuring 26.2 cm (about 46% the length of the at 56 cm), the shortest relative arm length among known dromaeosaurids, though equipped with a robust manual . The are sturdy, with a of 56.5 cm supporting bipedal locomotion, and the tail is elongated with chevron bones suggesting flexibility. A second specimen (MML-220), including additional and elements from the same locality, confirms these proportions and provides further details on pneumaticity in cranial bones, such as wide recesses in the , lacrimal, and postorbital revealed by scans. Phylogenetically, Austroraptor belongs to , a of South American dromaeosaurids that may represent the sister group to () or a basal subgroup within , highlighting the morphological disparity among Gondwanan paravians. Its discovery underscores the evolutionary radiation of dromaeosaurids in the , distinct from northern relatives like Velociraptor, and contributes to discussions on paravian , including potential adaptations for aquatic prey capture based on cranial features. Named in 2008 by Fernando E. Novas and colleagues, Austroraptor cabazai honors Héctor Cabaza, founder of the Museo Municipal de Lamarque, and combines the Latin "auster" for "south" with "raptor" for "thief", emphasizing its Gondwanan affinity.

Discovery and naming

Discovery history

The specimen of Austroraptor cabazai (MML-195), a partial preserving elements of the , vertebrae, , and limbs, was discovered in December 2002 at the Bajo de Santa Rosa locality (40°03′28″ S, 66°48′03″ W) in the , , , . The specimen, loaned to researchers by local collector Daniel Cabaza and housed at the Museo Municipal de Lamarque (MML), includes the right frontal and postorbital bones, lacrimals, maxillae, dentaries with teeth, right surangular and prearticular, several cervical vertebrae (including the third, fifth, sixth, seventh, and eighth), two dorsal vertebrae (second and fourth), associated and , the right , a manual ungual phalanx from digit III, the left pubic shaft, left , right , astragalus, calcaneum, metatarsal III, and various pedal phalanges. Initial fieldwork in the region, which revealed theropod remains amid eroded outcrops of the Maastrichtian-aged formation, was part of broader surveys documenting vertebrates in northern . The was formally described in by a team led by Fernando E. Novas from the Museo Paleontológico Egidio Feruglio (MPEF), along with Diego Pol, Juan I. Canale, Juan D. Porfiri, and Jorge O. Calvo, who identified it as a novel large-bodied dromaeosaurid based on its distinctive cranial and postcranial features. Preparation of the specimen was conducted by M. Isasi and S. Reuil at MPEF, highlighting collaborative efforts between local museums and paleontological institutions in . The discovery occurred in a semi-arid paleoenvironment where naturally exposed fossil-bearing layers, allowing for the initial recognition of the material as theropod remains during prospecting. A referred specimen (MML-220), consisting of maxilla fragments, isolated teeth, an incomplete dorsal vertebra, caudal vertebrae, and additional postcranial elements such as the right humerus, radii, ulnae, metacarpal I, ischium, pubis, tibia, metatarsals, and pedal phalanges, was collected during a joint expedition in 2008 approximately 20 km east of the holotype site in the same formation. This material, slightly smaller than the holotype and representing an adult individual, was described in 2012 by Philip J. Currie and Ariana Paulina Carabajal, confirming its attribution to A. cabazai through shared morphology in the humerus, metatarsal III, and pedal phalanges. In November 2023, further fieldwork at the holotype quarry yielded an isolated gastralium and right pedal phalanx III-1, which were referred to MML-195 based on comparable size and proportions. Recent osteological analysis in 2025 by Matías J. Motta and Fernando E. Novas incorporated computed tomography (CT) scans of elements from both the holotype and MML-220, revealing internal pneumatic structures in the maxilla and lacrimal, and re-evaluating some fragments (e.g., maxillae from MML-220) as indeterminate while solidifying referrals for others like the right splenial. These updates, based on enhanced preparation and imaging, suggest potential for additional referrals from ongoing excavations in the Allen Formation, though no further complete specimens have been confirmed as of late 2025.

Etymology and taxonomy

The genus name Austroraptor is derived from the Latin australis (southern), in reference to its discovery in southern , combined with raptor (thief or plunderer), alluding to the predatory habits typical of dromaeosaurids. The specific epithet cabazai honors the late Héctor Cabaza, founder of the Museo Municipal de Lamarque in , , where the holotype specimen is housed. Austroraptor cabazai was formally named and described in 2008 by Fernando E. Novas, Diego Pol, Juan I. Canale, Juan D. Porfiri, and Jorge O. Calvo, in a study published in Proceedings of the Royal Society B: Biological Sciences. The holotype (MML-195) comprises a partial skull, vertebrae, ribs, and limb elements collected from the Bajo de Santa Rosa locality in the lower section of the Allen Formation (Maastrichtian stage, approximately 70–66 million years ago), Río Negro Province, Argentina. In its original description, Austroraptor was classified as a member of Dromaeosauridae, nested within the subfamily Unenlagiinae, distinguishing it as one of the largest known Gondwanan dromaeosaurids and providing insights into southern hemisphere theropod evolution. Subsequent phylogenetic analyses have upheld this placement in Unenlagiinae while refining its position as a basal member of the clade, closer to taxa like Unenlagia and Buitreraptor.

Description

Cranial anatomy

The cranial remains of Austroraptor cabazai are primarily known from the specimen (MML 195), which preserves a nearly complete left , fragmentary right , partial right lacrimal, right frontal, right postorbital, left and right dentaries, right surangular, and right quadrate, along with isolated teeth. A referred specimen ( 220) adds fragmentary , dentary fragments, teeth, and a right splenial, providing additional insights into dental and mandibular variation. The is estimated to have measured approximately 80 cm in length, contributing to the animal's overall body length of 5–6 m. The is notably elongated anteroposteriorly but dorsoventrally low, with a length of 39 cm and height of 8.5 cm, yielding a height-to-length of about 21%, which is lower than in most dromaeosaurids. It features a straight ventral margin bearing 24–25 tooth positions, a subtriangular occupying roughly half its length, and a single large, elliptical , representing a reduced antorbital fenestral complex compared to the multiple (including promaxillary) typical of Laurasian dromaeosaurids like . Recent analysis reveals pneumatic features, including a large paranasal recess and three small anterior chambers within the , potentially linked to diverticula invading the . This morphology closely resembles that of the South American unenlagiid but contrasts with the deeper, shorter of basal paravians, suggesting derived elongation possibly influenced by troodontid-like traits. The jugal bone, partially preserved in the holotype, is robust with a prominent crest along its dorsal margin, indicating attachment sites for strong jaw adductor musculature; its suture with the postorbital is tightly interdigitated, and pneumatic invasion is evident in adjacent elements. The right quadrate is robust and dorsoventrally short, with a subtriangular lateral process, a broken pterygoid process, and a smaller lateral condyle relative to the medial one; its near-upright orientation lacks prominent pneumatic foramina, differing from the more slender, pneumatized quadrates of some troodontids, and may support limited prokinetic movement at the joint. Other cranial elements exhibit distinctive pneumaticity and form. The lacrimal is T-shaped and highly pneumatized with five internal recesses, featuring an elongated anterior process, a ventrally curved descending process at approximately 45°, and a unique posterolateral projection; this , including two foramina in a caudal excavation, sets it apart from the straighter, less pneumatized lacrimals of Laurasian dromaeosaurids. The right frontal is subtriangular, tapering rostrally with an anteromedial process comprising about 40% of its length and a deep notch for lacrimal articulation, lacking large pneumatic chambers but showing a straight oblique ridge in the supratemporal depression—traits echoing troodontids while differing from the caudolaterally expanded frontals of typical dromaeosaurids. The postorbital is dorsoventrally elongated with three pneumatic recesses (dorsal, medial, and lateral), lacking a dorsomedial process for frontal contact and exhibiting a quotation mark-like lateral profile, a reduced relative to Laurasian forms. The includes elongate, gracile dentaries with 24–25 alveoli, interdental plates, and an elongated nutrient groove with , alongside a mid-length ; teeth are small, conical, unserrated, and fluted, with anterior and middle teeth showing labiolingual compression and distal torsion up to 37° in the . The surangular features a hook-shaped shelf, wide , and absence of a surangular , while the referred splenial is robust, subtriangular, and dorsoventrally tall with a ventral mylohyoid . These mandibular traits align closely with and basal paravians, highlighting shared unenlagiid specializations such as reduced serrations and enhanced pneumaticity in the skull roof.

Postcranial skeleton

The postcranial skeleton of Austroraptor cabazai is incompletely known from the specimen MML 195 and a referred specimen MML 220, preserving elements of the axial column, , pectoral , , and both fore- and hindlimbs. These remains reveal a robust build consistent with large-bodied paravians, with adaptations for bipedal locomotion. The includes an incomplete in the , which is elongated with low neural spines that suggest enhanced neck flexibility compared to more rigid conditions in basal theropods. Dorsal vertebrae, represented by three partial elements in the and an additional incomplete mid-posterior dorsal in the referred specimen, are robust with well-developed hyposphene-hypantrum articulations that interlock adjacent vertebrae for increased stability along the trunk. Pleurocoels are present in the dorsal centra, indicating pneumatization similar to other unenlagiids. Recent analyses provide detailed descriptions of the sacral vertebrae, comprising at least five fused elements with tall neural spines and robust sacral ribs that anchor the firmly, alongside morphology featuring elongate proximal caudals that taper distally over at least 10 preserved centra (lengths 32–82 mm), further supporting unenlagiid affinities through shared vertebral specializations; the caudals also exhibit pneumatic features with wide internal recesses. The 2025 study additionally describes previously undescribed elements including and more (e.g., possible CV3, CV5, CV9, CV10) with pneumatic fossae. The features a right ilium in the with an elongated preacetabular process that exceeds the postacetabular wing in length, a condition approaching that seen in theropods and contributing to a bird-like profile. The pubis and left are partially preserved, with the pubis showing a straight shaft typical of paravians. Hindlimb elements demonstrate cursorial proportions, with the left of the measuring approximately 600 mm in length and the (from the referred specimen) measuring approximately 600 mm, similar in length to the , accompanied by a reduced that splints the proximally but tapers distally. Metatarsals II–IV are slender and elongate, with the third metatarsal ginglymoid at the distal end, supporting agile terrestrial movement. Forelimb preservation is limited but includes the right (232 mm long in the referred specimen; 265 mm in ), partial (161 mm), , and several phalanges with large, recurved unguals (up to 67 mm), indicating robust but shortened arms relative to the hindlimbs ( ~46% of length). These features align with derived paravian manual morphology, though reduced in size compared to typical dromaeosaurids; the right metacarpal I is confirmed as authentic.

Size and distinguishing traits

Austroraptor cabazai was one of the largest known paravians from , with body length estimates ranging from 5 to 6 meters based on the femur (60 cm long) and comparative scaling with other dromaeosaurids. Weight estimates, derived from volumetric models, originally calculated at 368 kg in 2008 and later refined to approximately 460 kg in 2025 osteological analyses incorporating both known specimens, place it in the range of 300–500 kg overall. The (MML 195) likely represents an individual, inferred from the advanced ontogenetic stage evident in morphology and preserved fusion patterns comparable to the second specimen (MML 220), which is explicitly identified as . No evidence of exists, as the two known specimens exhibit size differences consistent with intraspecific variation rather than sexual differences. Austroraptor cabazai is diagnosed by several autapomorphies, including a highly pneumatized with a strongly rostrally curved descending process and a horizontally flaring caudal process, as well as a postorbital bone lacking a dorsomedial process for articulation with the frontal. Other distinguishing traits include proportionally short and robust forelimbs ( ~46% of length), a low and elongate with small, conical, unserrated teeth, and a narrow pedal II-2. Recent 2025 studies using scans have identified additional unique features, such as pneumatic caudal vertebrae with wide internal recesses.

Classification

Phylogenetic analysis

Austroraptor cabazai was initially placed within , specifically in the subfamily , based on a phylogenetic analysis using an updated version of the dataset from Turner et al. (2007). This analysis employed equally weighted parsimony with software and incorporated both cranial and postcranial synapomorphies, recovering Austroraptor as a member of a monophyletic alongside taxa such as Unenlagia and . Key characters supporting this placement included reduced forelimbs, with the measuring approximately 46% of femoral length, elongated hindlimbs evidenced by a nearly equal in length to the , and features indicative of such as a long, low skull with small conical teeth. A more recent phylogenetic analysis in 2025 incorporated new osteological data from additional specimens and utilized an expanded matrix derived from Pei et al. (2020), comprising over 150 characters across 175 operational taxonomic units. This study applied parsimony analysis using v1.6 software, with bootstrap resampling to assess node support, confirming Austroraptor's position as a basal unenlagiid and reinforcing as the to within . The analysis highlighted Austroraptor's close affinities to Unenlagia comahuensis and Neuquenraptor argentinus, based on shared derived traits such as proportionally short upper limbs relative to elongation. Bootstrap values provided moderate to strong support for the (above 70% at key nodes), underscoring the robustness of this topology despite ongoing debates on paravian interrelationships. The resulting strict consensus depicts Austroraptor as a basal member of , branching near the base of the subfamily alongside Unenlagia and Neuquenraptor, with the broader forming a southern Gondwanan radiation sister to dromaeosaurines. This placement emphasizes the morphological divergence within unenlagiines, where Austroraptor's and specialized cranial features distinguish it while retaining core synapomorphies like the reduced condition. The updated matrix's inclusion of extensive character data, including newly scored postcranial elements, resolved previous ambiguities in southern paravian relationships, supporting Unenlagiinae's with high scores.

Relationship to other dromaeosaurids

Austroraptor cabazai is a member of the , a group of dromaeosaurid theropods characterized by a South American radiation that contrasts with the predominantly Laurasian distribution of other dromaeosaurid lineages, such as eudromaeosaurs. This Gondwanan endemism highlights an isolated evolutionary trajectory for unenlagiines, with fossils primarily from during the . Within , Austroraptor is positioned as a basal , larger than the contemporaneous Unenlagia comahuensis, which measured approximately 3 meters in length, while Austroraptor reached 5–6 meters. It shares a similar body size with the Asian giganteus, estimated at around 5 meters long and 250–350 kilograms, though Austroraptor exhibits distinct adaptations suited to its southern habitat. The evolutionary implications of Austroraptor's position underscore a of size variation among unenlagiines, with some taxa like Austroraptor exhibiting relative to smaller relatives, potentially influenced by on the fragmenting Gondwanan continents. Known from strata approximately 70 million years ago, unenlagiines represent a late divergence from northern dromaeosaurid lineages around 100 million years ago, following the separation of and . Recent analyses in 2025, including a study by Motta et al. that recovered as the to (modern birds and their close relatives), have strengthened support for paravians encompassing unenlagiids as basal avialans rather than strictly within , emphasizing their role in early bird evolution.

Paleobiology

Locomotion and adaptations

Austroraptor cabazai exhibited hindlimb proportions indicative of agile terrestrial locomotion, characterized by a femur-to-tibia ratio near 1:1 and a subarctometatarsalian foot structure similar to that of its relative Buitreraptor, which facilitated efficient cursorial movement on land. These features, combined with elongated metatarsals, suggest the dinosaur was adapted for pursuits in open Patagonian environments. In contrast to many northern dromaeosaurids with elongated s, Austroraptor displayed significant forelimb reduction, with arms notably shorter relative to hindlimb length and bearing robust manual claws suited for close-range rather than slashing or prey at a distance. This represents a departure from the typical "" build, potentially reflecting adaptations for a larger body size where powerful but compact forelimbs aided in subduing prey during terrestrial hunts. Evidence for aquatic adaptations in Austroraptor is primarily from its conical teeth, consistent with semi- hypotheses for unenlagiids involving wading or shallow- . Recent osteological analysis reveals details of tail musculature in Austroraptor, with robust caudal vertebrae and associated attachment sites indicating enhanced lateral stability, likely aiding balance during maneuvers in water or on uneven terrain. Despite retaining paravian traits such as a and possible feather impressions, Austroraptor's large size and robust postcranial skeleton preclude flight capability, positioning it firmly as a ground-dwelling predator.

Diet and behavior

The dentition of Austroraptor cabazai consists of small, conical, unserrated, and fluted teeth, a that closely resembles that of spinosaurids and suggests a focused on piscivory or soft-bodied prey, rather than hard-shelled or heavily armored animals. This carnivorous, non-durophagous feeding strategy is further supported by recent osteological analyses (as of September 2025), which describe the teeth as adapted for grasping and piercing slippery prey, complemented by a long, low skull housing numerous teeth (24–25 maxillary and 24–25 dentary). The robust, dorsoventrally short quadrate and extensive cranial pneumaticity, including large paranasal recesses in the and multiple recesses in the lacrimal, indicate adaptations for rapid jaw closure and a lightweight structure potentially suited to capture or similar elusive prey near water surfaces. Additionally, the short forelimbs may have facilitated maneuvers in environments, aiding in the pursuit of quarry. The claw morphology of A. cabazai features strongly curved manual unguals, particularly on digit III, which were likely used for slashing or securely holding slippery prey during feeding. These adaptations align with a predatory involving close-range interactions with agile, targets, emphasizing precision over brute force. Although pack hunting has been inferred for some dromaeosaurid relatives based on gregarious bonebed assemblages, such behavior in A. cabazai remains speculative with no direct evidence, such as multiple associated individuals. Sensory capabilities, inferred from impressions of cerebral hemispheres, , and bulb in the , suggest enhanced sensory adaptations for detecting prey, potentially active during low-light conditions, though specific nocturnal adaptations are unconfirmed for this .

Paleoecology

Geological context

The represents a key stratigraphic unit in northern , , spanning the mid to early stages and dated to approximately 73–66 Ma based on biostratigraphic evidence from , palynomorphs, and vertebrate assemblages, as well as magnetostratigraphic correlations. This formation belongs to the lower portion of the Malargüe Group and outcrops extensively in , including the Bajo de Santa Rosa locality (approximately 38°50′S, 68°00′W) where the of Austroraptor cabazai was discovered. Although direct is limited, the unit's position above the dated Anacleto Formation (ca. 83–79 Ma) and below the early Roca Formation supports its assignment to the late . Deposited in the northeastern Neuquén Basin, the records a mixed continental-marginal marine system dominated by fluvial and lacustrine sediments, indicative of riverine channels, floodplains, and shallow water bodies. The includes interbedded medium- to fine-grained sandstones, siltstones, claystones, and occasional limestones and evaporites, reflecting low-energy depositional settings with channels, intertidal flats, and shoreface environments influenced by the initial Atlantic ingression. This hybrid setting transitioned from tidally dominated lower sections to wave-influenced upper strata, with clastic inputs from nearby continental sources. Taphonomic preservation in the formation favors rapid burial in sandy channel fills and overbank deposits, as evidenced by disarticulated but associated vertebrate remains embedded in cross-bedded sandstones at sites like Bajo de Santa Rosa. Such conditions minimized transport and , preserving a mix of terrestrial, freshwater, and minor fossils in fine- to medium-grained sediments that suggest episodic high-energy fluvial events. Paleoenvironmental reconstructions indicate a warm, humid with seasonal and flooding, supported by palynological data showing thermophilous elements such as palm-like (e.g., Spinizonocolpites), alongside and ferns indicative of forested floodplains. The presence of freshwater taxa and fluvial features points to dynamic systems prone to periodic inundation, while subtle incursions are inferred from evaporitic layers and rare elasmosaurid remains, reflecting proximity to a low-gradient epicontinental .

Contemporaneous fauna

The of , , hosted a diverse assemblage during the late to early stages of the , including several theropod dinosaurs that coexisted with Austroraptor cabazai. Other theropods included the alvarezsaurid Bonapartenykus ultimus, known from partial skeletal remains indicating a small, specialized or adapted for behaviors, and the medium-sized abelisaurid Niebla antiqua represented by isolated cranial and postcranial elements suggestive of a robust, short-snouted predator potentially occupying an apex niche. Isolated theropod teeth associated with sauropod remains further indicate the presence of additional carnivorous or scavenging theropods, though their exact affinities remain uncertain. Ornithischian dinosaurs were relatively scarce in the Allen Formation compared to saurischians, with ornithopods represented by the hadrosaurid Bonapartesaurus rionegrensis, a medium-sized duck-billed known from well-preserved specimens showing evidence of healed pathologies possibly from intraspecific combat or predation attempts. Sauropod diversity was higher, dominated by saltasaurid titanosaurs such as Aeolosaurus sp., Bonatitan reigi, and Rocasaurus muniozi, which were armored, quadrupedal that likely browsed on floodplain vegetation and may have served as potential prey for large theropods like Austroraptor. Avifauna in the formation included early ornithurine birds, exemplified by Limenavis patagonica, a basal carinate known from fragmentary limb bones that suggest a terrestrial or semi-aquatic lifestyle similar to modern shorebirds, filling a niche as small, agile foragers. No enantiornithine remains have been definitively identified from the , though the overall bird record points to a developing diversity of crown-group avians in southern Gondwanan ecosystems. Potential prey items for Austroraptor encompassed a range of smaller vertebrates, including crocodyliforms such as notosuchians (indeterminate forms with adaptations for terrestrial or semi-aquatic lifestyles), possibly inhabiting rivers and wetlands. Abundant fish taxa, such as teleosts and chondrichthyans, populated the fluvial and lacustrine environments, providing opportunities for piscivory or opportunistic feeding. Smaller reptiles (e.g., turtles like Yaminuechelys gasperinii), amphibians, and early mammals further contributed to the prey base, supporting a in which Austroraptor likely functioned as a mid-tier predator, preying on juveniles of larger herbivores or competing with abelisaurids for carcasses. Marine reptiles like the elasmosaurid Kawanectes lafquenianum indicate occasional marine influence. The ecosystem of the Allen Formation represented a dynamic floodplain community with meandering rivers, seasonal flooding, and forested riparian zones, fostering interactions among these taxa; for instance, theropod bite marks on sauropod bones suggest scavenging or predatory behaviors involving multiple carnivores. Fossil preservation is characterized by isolated finds rather than mass death assemblages, reflecting low-energy depositional settings that favored disarticulated remains over concentrated bone beds. This scattered distribution underscores a stable, low-disturbance paleoenvironment where Austroraptor navigated a balanced trophic structure alongside diverse herbivores and smaller opportunists.

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