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Paraves

Paraves is a of maniraptoran theropod dinosaurs within the larger group , phylogenetically defined as the stem-based taxon comprising all coelurosaurs more closely related to Passer domesticus (the ) than to Oviraptor philoceratops or Ornithomimus edmontonicus . This encompasses the immediate relatives of birds and modern Aves, including the subclades Deinonychosauria (which contains Dromaeosauridae and Troodontidae) and Avialae, marking a critical evolutionary branch in the transition from non-avian dinosaurs to birds. Notable taxa include Deinonychus antirrhopus, Velociraptor mongoliensis, Troodon formosus, Microraptor zhaoianus, Sinornithosaurus millenii, and Archaeopteryx lithographica, alongside over 11,000 extant bird species (as of 2025) . Paraves originated in the and persisted for over 160 million years into the present, with fossils primarily from formations such as the Djadokhta in and the Jehol Group in . Key synapomorphies defining the include pennaceous feathers on the body and limbs, fused parietals, an L-shaped scapulocoracoid, a symmetrical , and modifications for enhanced mobility, such as a longer than the . These features reflect adaptations toward powered flight, with basal paravians like exhibiting "four-winged" gliding capabilities via elongated feathers on all limbs, while avialans show further refinements like asymmetrical vanes and reduced tails. The evolutionary significance of Paraves lies in its role as the nexus for avian origins, bridging non-avian theropods and modern through innovations in , skeletal pneumatization, and body size reduction—spanning four orders of magnitude in mass over approximately 15 million years. Phylogenetic analyses, incorporating up to 111 taxa and 474 morphological characters, consistently recover Paraves as a monophyletic group sister to oviraptorosaurs or therizinosauroids within , supported by at least 12 unambiguous synapomorphies . Numerous non-avian paravian are known, providing a rich fossil record that illuminates feather evolution, predatory behaviors, and the ecological radiation of feathered dinosaurs across , , and .

Anatomy

Skeletal structure

Paraves is characterized by several key skeletal features distinguishing it from more basal maniraptorans, including a large promaxillary , a T-shaped lacrimal, a lateral posteriorly expanding longitudinal groove on the dentary, manual IV-2 shorter than IV-1, a short with distally located obturator process and posterodistal process, and an extensible pedal II-2. These traits support the of the encompassing deinonychosaurians and avialans. A recent study on the cranial of Anchiornis huxleyi provides additional details on , highlighting features transitional to conditions. The furcula, or wishbone, in Paraves exhibits a distinctive boomerang-shaped morphology, often U-shaped with short, broad, and dorsoventrally expanded clavicular rami that are nearly symmetrical and sometimes pneumatic, as observed in taxa like Buitreraptor (MPCA 245) and Velociraptor mongoliensis. This structure articulates medially with the scapulocoracoid complex and serves to stabilize the shoulder girdle by providing robust attachment sites for flight-related muscles, such as the m. pectoralis, thereby enhancing forelimb excursion during locomotion or aerial behaviors. Cranial features of Paraves include a flexible quadrate with a dorsally displaced triangular process, enabling prokinetic movement, and a large that is vertically oriented with a broadly rounded anterior formed by the lacrimal and nasal. These adaptations facilitate kinetic movement by allowing independent flexion of the rostrum relative to the braincase, a that originated basally within Paraves and supported enhanced feeding efficiency through improved mobility and reduced mass. In the , Paraves display with serrated teeth of varying sizes, such as larger first and second premaxillary teeth compared to posterior ones, exemplified by antirrhopus (YPM 2505) with 15 maxillary, 4 premaxillary, and 16 dentary teeth where posterior denticles are nearly twice as large as anterior ones. The typically number 10–11, providing elongated and flexible necks for greater maneuverability, as seen across taxa like Sinovenator and Mei. A derived trait within avialans, the , involves fusion of the distal caudal vertebrae into a single structure, as documented in basal forms like Confuciusornis sanctus (IVPP V11374), which anchors tail feathers and marks an for aerodynamic control.

Forelimbs and wings

The forelimbs of paravians exhibit significant elongation relative to the hindlimbs, a key adaptation for aerial locomotion, with the manual digits particularly extended to support feather anchorage. In basal paravians such as Anchiornis and Microraptor, digits II and III are notably lengthened, forming the primary structural base for attaching flight feathers, while digit I remains shorter and more claw-like. This configuration allows for a broadened wing surface, with primary remiges anchoring primarily along digits II and III, enhancing stability during gliding or flapping. Pennaceous feathers covering the paravian arms form asymmetrical vanes critical for generating , consisting of a central rachis from which barbs extend, interconnected by barbules with hooklets that create a cohesive, airfoil-like structure. In paravians, these feathers evolved asymmetrical vanes at the clade's base, with the leading-edge vane narrower than the trailing edge to optimize and reduce during aerial maneuvers. The rachis provides rigidity, while the barbule arrangements ensure vane integrity under aerodynamic stress, as seen in the densely packed barbs of feathers that form broad, planar surfaces. The in paravians features specialized adaptations for expansive motion, including a strut-like that articulates firmly with the to transmit forces efficiently during wing beats. The is elongated, often forming an L-shaped complex with the , which positions the laterally and subvertically, permitting a wide range of anteroposterior and elevational movements essential for powered or . These features, observed in taxa like and , support enhanced mobility compared to more basal theropods. Wing loading in paravians varies, with estimated to have relatively low values enabling potential powered flight, in contrast to non-avialan paravians like suited more for . This reflects differences in wing proportions and body size across the clade. Fossil evidence from exemplifies these traits, with exceptionally preserved imprints revealing four-winged configurations where primaries (~10 asymmetrical remiges) and secondaries (~17–21 symmetrical feathers) form layered, V-shaped wings for , supported by soft tissues like the propatagium. These imprints show close-vaned structures curving medioposteriorly, indicating aerodynamic refinement for controlled .

Hindlimbs and pedal features

The hindlimbs of paravians exhibit specialized adaptations for agile and predation, with the pes (foot) displaying a subarctometatarsalian or fully arctometatarsalian condition in which metatarsal III is pinched proximally between metatarsals II and IV, reducing the overall foot width while enhancing rigidity and efficiency. This configuration, observed in troodontids and dromaeosaurids, allows for a more streamlined stride during rapid movement, with metatarsal III often comprising a significant portion of length relative to the and . In microraptorines and unenlagiines, the condition is subarctometatarsalian, providing transitional flexibility between broader theropod feet and the more compact avian . Recent studies highlight diversity in feathering among early paravians, including asymmetrical vanes on leg feathers in , contributing to four-winged gliding. A hallmark feature of deinonychosaurian paravians is the enlarged, recurved ungual on pedal digit II, forming the iconic sickle claw that is hypertrophied relative to other pedal unguals and held retracted off the ground during locomotion via a hyperextensible metatarsophalangeal joint. This claw, strongly curved and falciform, measures several centimeters in length in taxa like Deinonychus and Velociraptor, enabling powerful grasping during predatory strikes. Fossil evidence indicates the presence of a keratinous sheath extending the functional length and sharpness of the ungual, as preserved organic material on pedal phalanges in specimens such as Rahonavis ostromi and basal paravians shows immunoreactivity consistent with beta-keratin composition. The in paravians is notably reduced, adopting a splint-like that tapers distally and attaches closely to the , contributing to enhanced leg stability by buttressing the tibia's lateral surface without bearing significant weight. In dromaeosaurids such as and Unenlagia, the fibula's midshaft diameter is less than one-fifth that of the , and it lacks extensive contact with the calcaneum, reflecting lightweight adaptations for speed. This reduction, combined with proximal fusion of the astragalus and calcaneum to the in many paravians, optimizes force transmission during bipedal strides. The pubic boot, a distal expansion of the pubis forming a sub-triangular or spatulate structure, is present in several paravian clades including unenlagiids, microraptorines, and anchiornithines, potentially providing anchorage for abdominal musculature involved in posture and locomotion. In these taxa, the boot projects posteriorly and supports the retroverted pubis characteristic of maniraptorans, though its role in reproductive efficiency remains speculative without direct evidence of associated soft tissues. Fossil specimens of Deinonychus antirrhopus, such as those from the Cloverly Formation, reveal a hyperextensible ankle joint facilitated by the mesotarsal articulation between the tibia and proximal tarsals, allowing extreme dorsiflexion of the foot during raptorial maneuvers. Musculoskeletal modeling of the Deinonychus hindlimb demonstrates that this configuration, combined with the arctometatarsal pes, maximizes leverage for slashing or pinning strikes, with the ankle's flexibility enabling rapid deployment of the sickle claw.

Size and body plan variation

Paraves exhibit a broad range of body sizes, from diminutive forms like Anchiornis huxleyi, which measured approximately 0.5 meters in length and weighed under 1 kg, to larger dromaeosaurids such as , reaching up to 7 meters in length and around 500 kg. Body plan proportions vary significantly across the , particularly in tail morphology, where non-avialan paravians typically possess long, flexible tails comprising over half the total body length for balance and maneuverability, in contrast to the shortened, stiffened pygostylian tails of avialans that support feathered fans for aerodynamic control. Allometric scaling influences physiological traits, with smaller paravians displaying indicative of higher , such as dense vascularization and rapid deposition rates in cortical bone, compared to larger relatives with slower lines suggesting more moderate . Troodontids exemplify encephalization variation, possessing brains with an approximately five times greater than that of other theropods, reflecting expanded cerebral regions relative to body size despite their generally small stature. Evidence of intraspecific body plan variation comes from growth series in fossils of , where multiple specimens reveal ontogenetic shifts in limb proportions and feather development, indicating flexibility in size and morphology during individual development.

Classification

Taxonomic history

The taxonomic history of Paraves reflects a progression from fragmented understandings of theropod dinosaurs to a cohesive phylogenetic framework, driven by key fossil discoveries and cladistic analyses. In the mid-20th century, non-avialan theropods like dromaeosaurids were often viewed as primitive or distantly related to birds, with limited resolution in their placement among coelurosaurs. This changed with John H. Ostrom's 1969 description of antirrhopus from the Early of Montana, where he recognized its unusual features—such as the enlarged sickle-shaped claw and bird-like skeletal proportions—and classified it within , elevating awareness of maniraptoran diversity. Ostrom's subsequent work in the further bridged birds and theropods. His 1976 analysis of emphasized osteological similarities to , including the , pelvic structure, and forelimb morphology, proposing that represented an early avian derivative of small coelurosaurian dinosaurs closely allied with dromaeosaurs. This revived the dinosaur-bird hypothesis, challenging earlier views that separated birds from reptiles. The formal establishment of Paraves came in 1998, when Paul C. Sereno defined it as a stem-based encompassing all maniraptorans more closely related to Neornithes than to Oviraptor philoceratops, thereby uniting (bird-like theropods including ), , and on the basis of shared traits like reduced manual digits and enhanced arm mobility. Prior nomenclature, such as 's 1986 stem-based definition of (all dinosaurs closer to birds than to ), had partially overlapped with this concept but focused more narrowly on ornithurine descendants; Sereno's Paraves provided a broader, explicit framework for the avian radiation. In a 2001 honoring Ostrom, and Kevin de Queiroz refined avian terminology, redefining to include all dinosaurs with feathered wings adapted for flapping flight and their descendants, while distinguishing it from the more inclusive Paraves to avoid conflating flight origins with deeper theropod affinities. The early 2000s brought transformative fossil evidence from China, led by Xu Xing, that solidified Paraves' . Discoveries of feathered non-avialan theropods, such as the four-limbed glider Microraptor zhaoianus in 2000 and additional "four-winged" dromaeosaurids in 2003, revealed pennaceous s, aerodynamic adaptations, and skeletal features aligning closely with avialans, confirming the 's shared integumentary and locomotor traits beyond Europe and . Ongoing debates centered on enigmatic taxa like , known from specimens such as Epidexipteryx (described in 2008). Initially placed outside due to their elongated third finger and membranous wing structures, phylogenetic analyses in the and beyond have debated their position, with some recovering them within Paraves as basal avialans based on shared paravian synapomorphies like presence and impressions, while others suggest affinities outside the clade or with oviraptorosaurs; expanded datasets incorporating Chinese fossils continue to show instability as of 2025.

Phylogenetic position

Paraves represents a derived within the maniraptoran theropods, positioned as the sister group to in the broader framework of , a subdivision of . This relationship is consistently recovered in large-scale cladistic analyses incorporating hundreds of morphological characters across theropod , emphasizing Paraves' role in the transition toward avian dinosaurs. The is defined as a stem-based including all maniraptorans closer to Neornithes than to Oviraptor philoceratops (Sereno, 1998), though some studies use a node-based definition as the most inclusive group containing , , and excluding oviraptorosaurs. Phylogenetic trees derived from parsimony-based analyses depict Paraves diverging into two primary lineages: , which encompasses (e.g., , ) and (e.g., Mei, ), and , which includes basal forms such as alongside more crownward groups like and (modern birds and their close relatives). Diagnostic synapomorphies uniting Paraves include the enlargement and robustification of the alular digit (manus digit I), which supports enhanced manual dexterity and potential aerodynamic function; the development of uncinate processes on the dorsal ribs, aiding in thoracic stabilization during locomotion or flight; and the presence of a secondary , a cranial opening associated with lightweight skull construction. Additional shared features encompass a retroverted pubis in derived members, contributing to a more avian-like pelvic girdle, and large, posteriorly projecting axial epipophyses on the vertebrae for enhanced neck mobility. These characters are scored in matrices that resolve Paraves with strong clade support, such as Bremer indices of 3 and jackknife values indicating low collapse potential in reduced consensus trees. Quantitative support for Paraves' monophyly and internal topology is robust in seminal datasets; for instance, Brusatte et al. (2015) report bootstrap values of 80–90% for the Paraves node and its major subclades in time-calibrated analyses of theropod , reflecting consistent recovery across 230 taxa and 457 despite variations in . Updates in subsequent studies, including those incorporating new paravian fossils up to 2025, maintain this topology with similar high support (e.g., >70% bootstrap for ). Controversies persist regarding the exact placement of certain paravian taxa, such as Pyroraptor olympius, which fragmentary remains have led some analyses to position as a basal dromaeosaurid within , while others suggest closer avialan affinities due to inferred flight-related traits; however, most comprehensive matrices favor its inclusion in with moderate support (Bremer index ~2).

Included taxa

Paraves encompasses several major subgroups, each characterized by distinct morphological features that reflect their adaptations and evolutionary roles within the . The primary divisions include , , and various basal paravians. Avialae comprises and all modern birds (Aves), along with numerous extinct stem-group members such as enantiornithines from the . This is defined by key synapomorphies including the presence of a —a fused terminal caudal vertebra that supports tail feathers—and a strut-like bone that enhances shoulder girdle stability for flight-related functions. Its diversity spans from stem-birds like , known from deposits, to highly diverse forms like enantiornithines, which dominated avifaunas with over 80 described species exhibiting varied body sizes and ecological niches. Deinonychosauria includes the families and , representing non-avialan paravians specialized for predatory lifestyles. , exemplified by mongoliensis from , features cursorial adaptations such as elongated hindlimbs with a raptorial sickle claw on pedal digit II, enabling agile terrestrial hunting. , including Mei long from , is distinguished by enhanced cranial flexibility, evidenced by kinetic skull elements like a mobile quadratojugal joint, which likely facilitated precise prey manipulation and supported their relatively large brains relative to body size. Basal paravians form a paraphyletic assemblage of early-diverging members outside the crown clades, highlighting the transitional diversity within Paraves. , such as huxleyi from , are recognized for their four-winged body plan with pennaceous feathers on both fore- and hindlimbs, suggesting gliding capabilities in arboreal or forested environments. , including Yi qi from , exhibit arboreal climbing adaptations, notably an elongated third manual digit that may have supported patagial membranes for or scanningorial ; their exact within or relative to Paraves remains debated. Approximately 50 non-avian paravian have been described, underscoring the clade's extensive radiation, with approximately 70% originating from to deposits in , particularly the Yanliao and Jehol biotas of northeastern . This Asian concentration reflects exceptional Lagerstätten preservation that has revealed feathered specimens and informed phylogenetic reconstructions. Groups like , including oviraptorids, are excluded from Paraves based on phylogenetic analyses showing they lack core paravian synapomorphies such as the enlarged forelimbs with elongated manual digits and the hyperextensible pedal digit II, instead aligning with more basal maniraptorans in broader theropod trees.

Evolutionary history

Origins and early diversification

Paraves likely originated in the , with phylogenetic analyses indicating a divergence from other maniraptorans around 170 Ma, coinciding with an acceleration in body size miniaturization that characterized the early evolution of the . This miniaturization trend among maniraptorans, reaching body sizes under 1 kg in basal paravians, may have been driven by predation pressures or adaptations to forested environments, as evidenced by the warm, humid ecosystems of the Yanliao Biota where early paravians are preserved. The earliest potential fossil records of Paraves come from Anchiornis-like forms in the of northeastern , dated to approximately 160 Ma, representing the oldest known specimens of the . Ghost lineages inferred from cladistic analyses extend the inferred stem age of Paraves to about 170 Ma, filling gaps in the fossil record prior to the radiation of coelurosaurs following recovery from the end-Triassic extinction. Early diversification of Paraves occurred by the , with taxa radiating into arboreal, aerial, and terrestrial niches, facilitated by anatomical innovations such as elongated forelimbs and feathered appendages. This radiation is exemplified by the presence of protofeather-like structures in contemporaneous non-paravian dinosaurs like from around 160 Ma, suggesting a broader coelurosaurian experimentation with integumentary coverings that supported niche expansion in forested habitats. Molecular clock estimates place the crown-group divergence of Paraves between 170 and 160 Ma, aligning with the post-Triassic coelurosaur explosion and initial Pangaean distribution before continental breakup restricted later biogeography to primarily Laurasian realms.

Fossil record overview

The fossil record of Paraves is primarily known from exceptional Lagerstätten that preserve delicate structures such as feathers and soft tissues, with the in standing out as a key (~150 Ma) site. This fine-grained , formed in anoxic lagoonal environments, has yielded multiple specimens of Archaeopteryx, including the renowned Berlin specimen (Humboldt Museum HMN MB.AV.101), which features a nearly complete articulated with impressions of primary and other integumentary details. Similarly, the (~125 Ma) in Province, , represents another pivotal deposit of and lacustrine sediments that facilitated the preservation of feathered paravians, such as the dromaeosaurid millenii, whose (IVPP V12719) includes filamentous integument covering much of the body. Beyond these Asian and European hotspots, notable discoveries include the dromaeosaurid antirrhopus from the Cloverly Formation in , , with specimen AMNH 3015—a partial but informative collected in the 1960s—providing early insights into paravian skeletal robustness despite lacking soft-tissue preservation. Other significant sites encompass the in , which has produced over 200 specimens of the anchiornithine Anchiornis huxleyi with detailed plumage, and the in , yielding troodontids and dromaeosaurids in eolian dune settings. Preservation in these deposits favors small-bodied, feathered taxa due to the fine-grained, low-energy sedimentary environments of lakes and lagoons, which inhibit decay and scavenging, leading to an overrepresentation of arboreal or volant forms while undersampling larger, terrestrial paravians. Discovery trends show a marked increase since the , with a majority of paravian specimens originating from , particularly , where lagerstätten like Yixian have contributed to the description of dozens of new species, fundamentally reshaping understandings of paravian diversity. However, significant gaps persist, including scant records from the —prior to the oldest known fossils—where paravians likely originated but direct fossils are rare, and the , limited mostly to isolated unenlagiine finds , , such as Unenlagia comahuensis and the recently described Diuqin lechiguanae from the Santonian (~85 Ma).

Temporal distribution

Paraves first appeared in the fossil record during the Middle to , spanning approximately 160–145 million years ago (Ma), with early basal forms such as Aurornis xui from the of northeastern representing some of the oldest known members of the . This period is characterized by small, feathered paravians exhibiting transitional features between non-avialan theropods and more derived birds. In , the (~155–145 Ma) has preserved incomplete paravian fossils, including elements attributed to Hesperornithoides miessleri, indicating an early presence of the group in Laurasian continental deposits. Following this initial emergence, Paraves underwent significant diversification during the (~145–100 Ma), reaching a peak in abundance and morphological variety within the of northeastern , dated to approximately 130–120 Ma, where exceptionally preserved specimens reveal advanced feathering and flight-related adaptations in taxa like microraptorines and early avialans. The (~100–66 Ma) saw continued paravian presence, particularly among larger dromaeosaurids such as Dakotaraptor steini from the of , (~68–66 Ma), highlighting the persistence of non-avialan forms until the end of the . Non-avialan paravians abruptly vanished at the Cretaceous-Paleogene (K-Pg) boundary (~66 Ma), an event linked to the Chicxulub asteroid impact and associated environmental disruptions, including and climate shifts. In contrast, avian paravians—stem-birds and early crown-group representatives—persisted through the K-Pg mass extinction, with fossil evidence showing their survival in reduced numbers immediately following the event, while crown-group birds underwent rapid post-extinction diversification during the Paleogene.

Paleobiology

Locomotion and flight capabilities

Paravians exhibited a spectrum of locomotor strategies, ranging from quadrupedal gliding in basal forms to cursorial running in dromaeosaurids and powered flapping in avialans, reflecting biomechanical adaptations for diverse environments. Basal paravians like Microraptor utilized a four-winged planform, with elongated feathered forelimbs and hindlimbs forming a biplane-like configuration that facilitated stable gliding. Computer simulations of Microraptor flight performance indicate this morphology was adapted for undulatory "phugoid" gliding between trees, allowing controlled descent with lateral body movements for maneuvering. Physical models tested in wind tunnels have estimated a lift-to-drag ratio of 4.1:1 for Microraptor gui, corresponding to glide angles averaging 13.7° and enabling efficient aerial travel over moderate distances. Dromaeosaurids demonstrated pronounced adaptations suited to terrestrial sprinting, characterized by elongated hindlimbs with tibia-to-femur length ratios of approximately 1.2–1.3, which enhanced stride efficiency and agility. These proportions, observed in taxa such as and , correlate with biomechanical correlates of superior running ability, including reduced body mass relative to leg length and a posture. Limb scaling and trackway analyses infer maximum speeds up to 40 km/h for mid-sized dromaeosaurids like , allowing rapid pursuit across open terrains. The transition to powered flight in avialans involved enhanced shoulder girdle mobility, permitting greater wing excursion during the downstroke to generate propulsive force. In basal avialans, the glenoid fossa's orientation and furcula-scapula articulation allowed abduction and depression of the humerus, optimizing power output from the pectoralis muscle. Muscle attachment scars on the sternum and coracoid, such as those for the pectoralis major, indicate substantial leverage for depressing the wing, with reconstructed musculature suggesting this configuration could produce aerodynamic forces comparable to early flapping in modern birds. Locomotor strategies varied between arboreal and terrestrial niches within Paraves. Scansoriopteryx, an arboreal scansoriopterygid, possessed a short, stiffened that likely functioned as a prop for balance and support during trunk , analogous to woodpecker tails, facilitating ascent along vertical surfaces with its elongated manual digits. In contrast, troodontids exhibited terrestrial adaptations, including elongated metatarsals forming an arctometatarsal pes that enhanced foot flexibility and spring-like for leaping and rapid maneuvers over ground. These long metatarsals, combined with a nimble hallux, supported bounding gaits in pursuit or evasion scenarios. Biomechanical models have elucidated flight performance in early avialans like . Wind tunnel experiments on physical wing models demonstrate lift coefficients approaching 1.2 during downstroke simulations, highlighting the role of asymmetric feather vanes and wing camber in generating sufficient lift for short bursts of powered flight or controlled glides from elevated starts. These analyses underscore how subtle morphological features, such as alula-like structures, mitigated stall risks and improved aerodynamic efficiency.

Diet and predatory adaptations

Members of Paraves, particularly deinonychosaurs, possessed ziphodont adapted for slashing , featuring laterally compressed, recurved crowns with fine serrations that facilitated efficient tearing of prey tissues. These serrations typically exhibited densities of 5-10 per millimeter, enhancing the cutting efficiency during predation. In avialans, dentition evolved toward more versatile forms, with some taxa developing broader crowns and grinding occlusal surfaces suited to processing a wider range of foods beyond strict carnivory. Predatory behaviors in paravians included cooperative strategies, as evidenced by bonebeds containing multiple individuals alongside disarticulated skeletons, suggesting group hunting or scavenging of large herbivores. The iconic sickle-shaped on pedal digit II of dromaeosaurids served primarily to pin and restrain struggling prey, with biomechanical analyses estimating it could exert forces up to approximately 500 N to secure victims during attacks. These adaptations complemented agile locomotion, enabling effective pursuit and capture. Cranial kinesis provided key predatory advantages, with flexible jaw mechanisms allowing expansive gapes of up to 80° to engulf larger or more agile prey items. In troodontids, —where the upper jaw flexed relative to the braincase—further enhanced this capability, permitting rapid and precise strikes in low-light or confined environments. Dietary habits varied across Paraves, reflecting ecological diversification. Small avialans such as displayed omnivorous tendencies, with fossilized gut contents preserving intact seeds from fruits, indicating consumption of plant material alongside animal prey for . Piscivory characterized certain avialans, including , whose conical teeth and robust jaws were specialized for grasping and consuming in settings. Stable isotope analyses of paravian fossils, particularly δ¹³C values, reveal mixed terrestrial and aquatic dietary signals in some taxa, underscoring opportunistic foraging strategies that bridged habitats.

Reproduction and growth

Paraves laid elongated, hard-shelled eggs measuring approximately 10-15 cm in length, arranged in ovoid clutches of up to 24 eggs, with a calcite-based microstructure consisting of a mammillary inner layer and a squamatic outer layer similar to that of modern birds. Nesting evidence from troodontids includes clutches of over 20 eggs arranged in concentric rings, partially buried in substrate, suggesting brooding behavior with direct body contact for incubation. In oviraptorids, close relatives of paravians, multiple specimens preserve adults in a brooding with wings folded over the clutch and head tucked under a wing, consistent with thermoregulatory incubation; associated embryos exhibit advanced development, including curled postures indicative of late-stage . Bone histology in paravians reveals rapid, avian-like growth characterized by fibrolamellar tissue, with von Bertalanffy growth constants (k) of 0.3-0.5 per year, enabling small taxa such as troodontids and dromaeosaurids to reach skeletal maturity in 1-2 years. Evidence for in paravians includes behaviors inferred from nest-associated troodontid specimens. Medullary , indicating calcium mobilization for formation in gravid females, has been identified in close relatives such as oviraptorids; however, brooding adults preserved on nests lack medullary , implying paternal in some cases. Debates on hatchling development center on evidence for precociality, with troodontid nests showing no crushed s or trampling traces, and well-ossified embryonic skeletons suggesting high mobility at hatching rather than altricial dependence.

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