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Synapsida

Synapsida is a diverse of vertebrates defined by the presence of a single —a large opening in the behind each eye socket that facilitates jaw muscle attachment—encompassing all living mammals and their extinct relatives, which originated around 320 million years ago in the Late period. This group represents one of the two primary lineages diverging from early amniotes, the other being (which includes reptiles and birds), and synapsids were the dominant large terrestrial vertebrates during the Late Carboniferous and Permian periods, occupying diverse ecological niches from carnivorous predators to herbivorous grazers. Early synapsids, often referred to as pelycosaurs, featured sprawling gaits, ectothermic physiologies, and sprawling postures similar to modern reptiles, exemplified by sail-backed forms like . Later subgroups, known as therapsids, emerged in the Permian and exhibited progressive mammal-like traits, including more upright postures, differentiated teeth, and evidence of endothermy, with advanced cynodonts in the evolving features such as secondary palates and mammalian joints that contributed to the origin of true mammals by the Late or Early Jurassic. Synapsids survived the Permian-Triassic mass extinction— the most severe in Earth's history—through adaptable lineages, leading to multiple radiations and the eventual dominance of mammals in the and eras, with over 6,000 extant species today displaying traits like , , and metabolism that trace back to synapsid innovations. Despite their "mammal-like reptile" moniker, synapsids are not s but a separate branch, with evolutionary transitions such as the reconfiguration of bones into (forming the and ) marking key adaptations for enhanced hearing and mastication in mammalian descendants.

Taxonomy and Classification

Cladistic Definition and Phylogeny

Synapsida is defined cladistically as the monophyletic consisting of the last common ancestor of Mammaliaformes and all of its descendants, encompassing all mammals and their extinct relatives closer to mammals than to sauropsids. This is diagnosed by key synapomorphies in the , including a single lateral positioned low behind the orbit, with the postorbital and squamosal bones excluded from the temporal roof, and the reflected lamina of the angular bone forming the ventral margin of the . These features distinguish synapsids from other amniotes and mark the origin of the group around 318 million years ago during the Late , when the synapsid-sauropsid divergence occurred near the base of Amniota. The phylogenetic framework of Synapsida features basal stem synapsids, often referred to as pelycosauromorphs or non-therapsid synapsids, which include groups like , , and , representing the earliest diverging lineages after the split from sauropsids. More derived within Synapsida is the clade Therapsida, which encompasses all synapsids more closely related to mammals, including Anomodontia, , and the mammalian stem group Cynodontia leading to . This structure reflects a progressive nesting toward mammalian traits, with therapsids emerging in the Early Permian and dominating terrestrial ecosystems thereafter. The modern consensus on synapsid phylogeny emerged from the cladistic revolution of the , pioneered by analyses like Reisz's 1986 systematic revision of basal synapsids, which established and basic branching patterns using morphological characters from fossils. Subsequent refinements integrated additional fossil discoveries, such as those from the Karoo Basin, and molecular data from living mammals to calibrate divergence times and resolve deeper nodes, confirming Synapsida's position as the to within Amniota.

Historical Linnaean Approaches

In traditional , synapsids were classified as a subgroup of reptiles under the class Reptilia, commonly termed "mammal-like reptiles" owing to their intermediate skeletal and dental features between typical reptiles and mammals. This placement reflected early 19th-century views that emphasized shared reptilian traits like sprawling limbs and ectothermy while noting progressive mammalian affinities in later forms. Early hierarchical schemes distinguished basal and advanced groups, with Edward Drinker Cope establishing the order Pelycosauria in 1878 for primitive synapsids, including sail-backed sphenacodonts like , characterized by robust skulls and predatory adaptations but lacking advanced mammalian traits. In 1889, Harry Govier Seeley proposed the order Theromorpha to group more derived forms with mammal-like skull structures, such as differentiated teeth and enlarged temporal openings, positioning them as a transitional category within Reptilia. These orders exemplified the Linnaean focus on morphological grades rather than strict ancestry, treating pelycosaurs as basal "reptilian" stock and theromorphs as progressively "mammalian." Robert Broom formalized Therapsida as a subclass in , elevating advanced mammal-like forms (including gorgonopsians and cynodonts) above pelycosaurs in the and underscoring an from primitive to sophisticated morphologies. This subclass encompassed taxa with features like a secondary and upright , critiqued later for rendering Pelycosauria paraphyletic since therapsids arose from within pelycosaur-grade synapsids. Broom's framework, built on South African Permian fossils, dominated early 20th-century classifications but faced challenges for implying linear progression over branching . The shift from Linnaean to cladistic approaches accelerated in the 1970s and 1980s, with seminal works like those of Robert R. Reisz (1980) and Thomas S. Kemp (1982) demonstrating the of Synapsida as a distinct lineage separate from Reptilia, rendering "mammal-like reptiles" obsolete. In contemporary paleontological practice, "synapsid" denotes the full encompassing all non-reptilian including mammals, while "therapsid" persists informally for mammal-proximate non-mammalian forms to retain descriptive utility in fossil descriptions, despite ongoing debates over nomenclatural precision.

Major Subgroups and Nomenclature

Synapsida encompasses a diverse array of extinct and extant clades, with mammals as the sole surviving lineage. The major subgroups are organized cladistically into basal forms and more derived branches, reflecting successive outgroups to the mammalian stem. Basal synapsids include , a of primarily aquatic or semi-aquatic carnivores from the Late , with elongate skulls and paddle-like limbs, represented by genera like Ophiacodon from North American deposits. , another basal from the Late to Middle Permian, consists of primarily herbivorous forms characterized by robust skulls, leaf-shaped teeth for grinding vegetation, and barrel-shaped bodies adapted for a ; representative genera include Casea and , known from North American deposits. The clade Pelycosauromorpha comprises more advanced non-therapsid synapsids, with as its principal subgroup, including , , and the derived Therapsida. , within , features distinctive sail-like dorsal spines supported by elongated neural spines, possibly for or display, as seen in from the Early Permian of and . , known from the Late to Middle Permian, consists of carnivorous forms with deep skulls, serrated teeth, and robust limbs suited for terrestrial predation; , famous for its , exemplifies this group as an in Permian swamp ecosystems. Therapsida represents the mammalian stem lineage, diversifying in the Permian and , and is divided into several major subclades: (basal carnivores with primitive jaw mechanics), (thick-skulled herbivores and carnivores like Tapinocephalus), Anomodontia (predominantly herbivorous, including dicynodonts such as with beak-like jaws and tusks), (sabre-toothed carnivores akin to big cats), (small to medium predators with mammalian-like structures), and Cynodontia (leading to mammals, featuring advanced and endothermy indicators in forms like ). Nomenclature within Synapsida has seen revisions, particularly regarding varanopids (Varanopidae), a group of agile, lizard-like forms from the Late Carboniferous to Middle Permian. Traditionally placed as basal synapsids or stem-amniotes, 2010s phylogenetic analyses debated their affinity, with some studies positioning them outside Synapsida due to diapsid-like features, while others, incorporating cranial and postcranial data, confirmed them within Eupelycosauria as successive outgroups to Sphenacodontia and Therapsida; a 2019 analysis of new Oklahoma material reinforced their synapsid status, emphasizing the need for additional fossils to resolve uncertainties. In Anomodontia, nomenclature controversies surround dicynodont extinction timelines; while long thought to end in the Late Carnian, 2018-2019 revisions based on Polish faunas (e.g., Lisowicia) extended survival into the Late Triassic (Rhaetian), challenging but not overturning end-Triassic extinction models; a controversial 2002 report of a possible relic in Australian Cretaceous rocks remains unconfirmed by recent studies. These debates underscore ongoing refinements in synapsid phylogeny, driven by integrated morphological and stratigraphic data.

Anatomy and Physiology

Skull Structure and Temporal Fenestra

The synapsid skull is defined by a single temporal opening, the infratemporal , which represents a key synapomorphy distinguishing Synapsida from other clades such as diapsids with their dual fenestrae. This originates in the Late and persists throughout synapsid evolution, including in modern mammals, where it accommodates the . In basal synapsids, the overall architecture resembles the condition of early amniotes, featuring a relatively solid temporal region with fewer perforations, but the infratemporal fenestra emerges as a novel opening bounded dorsally by the postorbital and squamosal bones and ventrally by the jugal and quadratojugal. Over evolutionary time, synapsid skulls underwent progressive simplification, including reduction in the number of dermal bones and partial loss of exposure for elements like the quadrate, which became more internalized compared to the superficial positioning in basal forms. The infratemporal fenestra itself forms through the separation of dermatocranial sutures rather than within a single bone, facilitating biomechanical adaptations for terrestrial feeding. Functionally, this opening enables the expansion and low-angle insertion of jaw adductor muscles, such as the temporalis and masseter precursors, thereby increasing bite force without requiring excessive skull doming. This structural innovation correlates with enhanced anterior biting capabilities, as seen in the stress distributions modeled for early synapsid crania. In more derived synapsids like therapsids, the often enlarges to support further , with pronounced temporal arches developing to counter tensile stresses during mastication. For instance, in the Permian sphenacodontid , the robust skull features a laterally expansive infratemporal fenestra that underscores the shift toward dominant anterior bite mechanics in predatory lifestyles. These variations highlight the 's role in accommodating diverse feeding strategies while maintaining the core synapsid cranial plan.

Dentition and Feeding Adaptations

Early synapsids exhibited a homodont dentition characterized by uniform, conical, unicuspid teeth adapted primarily for grasping and piercing prey, as seen in basal forms like sphenacodontids such as Dimetrodon. These teeth were simple in morphology, with minimal size or shape variation along the jaw, reflecting a faunivorous lifestyle in Carboniferous and early Permian environments. The evolution of heterodonty marked a significant advancement in synapsid , beginning in the Permian with therapsids that developed differentiated types, including incisor-like , enlarged canines, and multicuspid postcanines resembling premolars and molars. This progression allowed for more versatile feeding strategies, with therapsids independently evolving additional cusps on up to three times across lineages. In advanced cynodonts, heterodonty further refined, featuring occluding molars with complex shearing surfaces that enhanced processing of tougher foods, approaching the mammalian condition. Specialized dental adaptations reflected dietary diversification among therapsids; for instance, herbivorous dicynodonts often reduced marginal teeth in favor of a keratinous , retaining prominent for cropping or , as evidenced by histological studies of tusk development in taxa like . In contrast, carnivorous gorgonopsians possessed serrated canines and postcanines with dentine-enamel serrations for efficient tearing of flesh, enabling them to dominate as apex predators in Permian ecosystems. Tooth replacement patterns also evolved progressively, with basal synapsids displaying polyphyodonty—continuous replacement throughout life—via ankylosed attachment to the jawbone, as observed in sphenacodonts like . Therapsids showed transitional states with prolonged ligamentous (gomphotic) attachment, reducing replacement frequency, while advanced cynodonts such as and Diademodon approached the diphyodont condition of mammals, featuring two generations of teeth and permanent gomphosis for durability. This shift, driven by heterochronic changes like , supported more efficient long-term feeding in increasingly mammalian-like forms.

Jaw Mechanics and Musculature

In basal synapsids such as pelycosaurs, the joint consisted of the quadrate and articular bones, enabling a wide gape suitable for capturing prey but providing limited for precise biting. This supported primarily vertical jaw motion, with adductor musculature dominated by a single temporalis-like muscle inserting on a modest coronoid process of the dentary, resulting in relatively weak bite forces compared to later forms. Therapsids exhibited significant advancements in jaw mechanics, including enlargement of the , which accommodated expanded temporalis and emerging masseter muscles for greater and force generation. In advanced therapsids, the raised coronoid enhanced the moment arm of the adductor muscles, allowing for improved stabilization of prey during feeding, while the masseter began to develop as a distinct layer inserting laterally on the angular . These changes facilitated a shift toward more efficient mastication, though the primary joint remained quadrate-articular. The transition to cynodonts marked the emergence of the dentary-squamosal joint, which progressively replaced the quadrate-articular articulation, with the quadrate reducing to form the incus and the articular becoming the malleus in the mammalian middle ear. This reconfiguration, evident in forms like Thrinaxodon, allowed for transverse jaw motion and precise occlusion, supported by further expansion of the temporalis and masseter muscles via the enlarged temporal fenestra. Functionally, these adaptations increased bite efficiency and enabled complex chewing, benefiting from heterodont dentition for varied food processing.

Secondary Palate Development

The secondary palate in synapsids is a bony structure that separates the nasal and oral cavities, enabling independent function of respiration and feeding. This feature is absent in basal synapsids, such as pelycosaurs and early therapsids, where the nasal and oral passages remain connected. Its origin traces to the late Permian in non-mammalian therapsids, with the earliest evidence appearing in forms like the biarmosuchian Promoschorhynchus platyrhinus, where incipient choanal crests and medial bony processes begin to form a partial barrier. The development involves contributions from the , , and bones, which project medially to create a shelf-like extension, often supplemented by vomerine elements in early stages. In early therapsids, such as some dinocephalians and dicynodonts, the secondary remains incomplete, consisting of short, perforated shelves with prominent choanae (posterior nasal openings) positioned anteriorly. For instance, in certain dicynodonts like Kawingasaurus fossilis, the portion features large foramina, allowing limited communication between cavities while providing . By the , this structure becomes more robust and elongated in cynodonts, such as Procynosuchus delaharpe, where the and fuse to form a near-complete bony , marking a key transition toward mammalian conditions. This progressive closure is linked to enhanced reinforcement, as the distributes masticatory stresses across the . The primary function of the secondary palate is to permit breathing during feeding or drinking, as air can flow through the nasal passages uninterrupted by oral contents—a critical for active terrestrial lifestyles. In advanced forms, it also facilitates the warming and humidification of inhaled air via contact with vascularized nasal turbinals, aiding physiological efficiency. These developments in non-mammalian therapsids represent a precursor to the fully ossified of mammals, where the structure supports additional behaviors like suckling in neonates.

Integument, Skin, and Sensory Features

The of basal synapsids, such as those in the and Early Permian, consisted primarily of scaly akin to that of reptiles, with epidermal scales providing protection and possibly aiding in . Skin impressions preserved in Early Permian trackways, including those attributed to synapsids like Dimetropus makers, reveal rectangular or on the limbs, , and tail, indicating a non-overlapping, tuberculate texture.00574-3) In caseids, the earliest detailed soft-tissue preservation from the Early Permian of shows a similar scaly without osteoderms, though dermal bony plates may have occurred sporadically in related basal forms for armor-like reinforcement. Evidence for glandular structures in basal synapsid is sparse, but impressions suggest the presence of simple apocrine-like glands associated with scales, precursors to more complex mammalian skin derivatives. Fur evolved as a transformative feature in synapsids, marking the shift toward mammalian and sensory capabilities, with the transition from scaly to pilose occurring gradually in . -like filaments reported in Late Permian coprolites from localities were initially interpreted as evidence of early , but subsequent analyses identified them as probable debris or fungal hyphae rather than true . Definitive first appears in the fossil record during the to among advanced cynodonts, where skin impressions show a mix of scales and follicles; for instance, the exhibits dermal patterns with small pits suggestive of whisker-like vibrissae emerging amid scales. By the , mammaliaforms such as display clear impressions of dense underfur and guard hairs across the body, confirming pelage as a fully developed insulating cover. Sensory adaptations in synapsid evolved alongside , enhancing tactile and environmental in nocturnal or burrowing lifestyles. In advanced therapsids, including therocephalians and probainognathian cynodonts, enlarged infraorbital foramina and associated nerve canals in the indicate the presence of whisker follicles, enabling mechanoreception for in low-light conditions. These vibrissae likely originated as specialized rooted in deep dermal follicles, with the expansions providing neural support for heightened sensitivity. Mammary glands, as specialized skin-derived structures from ectodermal tissues linked to hair follicles, are inferred to have arisen in early Jurassic mammaliaforms, though direct fossils are lacking; indirect evidence includes correlated soft-tissue impressions and genetic markers like MSX2 expression in related lineages, suggesting nutrient-secreting glands for offspring care. Certain synapsids developed specialized skin extensions for locomotion, exemplified by patagia in haramiyidan mammaliaforms. euharamiyidans such as Vilevolodon and Maiopatagium possessed broad membranes of furred skin stretched between elongated limbs and the body, supported by a and styliform bones, facilitating arboreal over forest canopies. These patagia, covered in fine guard hairs, represent convergent adaptations with modern mammals and highlight the diversity of skin-based locomotor structures in early mammaliaforms. Color patterns in synapsid pelage, inferred from morphology in and fossils, were predominantly dark and monotonous, with eumelanosomes indicating gray-brown hues for amid leaf litter. Phaeomelanosomes, responsible for reddish tones, appear rarely, suggesting limited pigmentation diversity until the radiation of crown mammals.

Metabolic and Thermoregulatory Traits

Synapsids exhibit a progressive evolutionary shift from ectothermic to endothermic metabolic strategies, marking a key physiological divergence from other amniotes. Basal synapsids, such as pelycosaurs, are inferred to have been ectothermic based on their sprawling limb posture, which limited efficient heat retention, and evidence of slow bone growth rates from histological analysis of long s showing laminar or parallel-fibered bone tissue with low . This ectothermy likely supported a low metabolic rate, akin to modern reptiles, allowing energy conservation in the variable climates of the late and early Permian periods. In contrast, advanced synapsids, particularly therapsids, display anatomical adaptations indicative of emerging endothermy. Therapsids possessed nasal turbinates—complex bony or cartilaginous structures within the —that facilitated warming and humidifying inhaled air, a essential for conserving and minimizing respiratory water loss in endotherms. Similarly, cynodont therapsids, closer to mammals, show high vascularity in their long bones, with extensive Haversian canals suggesting rapid blood flow to support elevated metabolic demands. These features collectively point to a higher , enabling sustained activity and potentially nocturnal or high-latitude lifestyles. Bone histology further underscores this metabolic transition through shifts in growth patterns. Early synapsids like pelycosaurs formed slow-growing, avascular bone, but by the late Permian, non-mammalian therapsids developed fibrolamellar bone—a highly vascularized associated with rapid, uninterrupted growth and high in modern endotherms. In advanced cynodonts, such as those from the , evidence from oxygen isotopes and suggests elevated body temperatures of around 30–34°C, indicating emerging endothermy with internal generation supplementing environmental sources. A 2022 study using estimated body temperatures of approximately 34°C in non-mammalian mammaliamorphs from the , supporting a stepwise toward full endothermy in mammals. This thermoregulatory evolution unfolded gradually, with initial signs of elevated appearing in Permian therapsids through enhanced respiratory efficiency and , culminating in fully endothermic, mammalian-like physiology by the period in true mammals. Ancillary traits, such as insulating in cynodonts and the secondary in therapsids, complemented these metabolic advancements by aiding heat retention and efficient , respectively.

Evolutionary History

Origins and Early Diversification in the Carboniferous

Synapsids originated through the divergence of the lineage from sauropsids during the Late , approximately 310–319 million years ago (mya), marking the initial split within crown-group amniotes. This event occurred amid the diversification of early tetrapods following , a period of sparse fossil preservation from about 360 to 345 mya that obscured initial amniote evolution. The earliest known synapsid body fossils date to around 312 mya, represented by small, lizard-like forms such as Protoclepsydrops haplous from the Joggins Formation in , , which exhibit primitive features including a single lower in the for enhanced jaw musculature. These basal synapsids were adapted to swampy, coal-forming environments of the equatorial Euramerica , preying on and smaller tetrapods in ecosystems. The most basal synapsid clade, Ophiacodontidae, emerged in the Late Carboniferous and persisted into the Early Permian, characterized by elongated snouts, robust limbs, and piscivorous or insectivorous diets suited to wetland habitats. Genera like Ophiacodon and Archaeothyris (the latter known primarily from Early Permian deposits but with roots in Late Carboniferous ancestry) were typically under 2 meters in length, with slender bodies resembling modern lizards and teeth adapted for grasping slippery prey. Fossil evidence from sites such as the Joggins Formation includes not only Protoclepsydrops but also trackways attributable to basal synapsids, indicating quadrupedal locomotion in humid, forested lowlands. These early forms established the synapsid clade through key innovations like the temporal fenestra, which supported stronger bite forces compared to contemporary anapsid amniotes. Early diversification of synapsids was driven by the post-Romer's Gap of terrestrial ecosystems, where increased oxygen levels and abundant prey facilitated the occupation of carnivorous niches previously dominated by stem-amniotes. By the late Westphalian stage (around 315–311 mya), synapsids had begun to split into lineages like ophiacodontids and the more herbivorous-leaning caseids, such as Eocasea martini from the Late Pennsylvanian of , reflecting adaptive shifts toward varied feeding strategies in swamps. This initial laid the groundwork for synapsid dominance in later periods, with assemblages from preserving a snapshot of this transitional alongside early diadectomorphs and other amniotes.

Permian Dominance and Key Lineages

The Permian period marked a peak in synapsid diversification, with pelycosaurian-grade forms radiating prominently in the Early Permian () across equatorial regions of Pangea, achieving up to approximately 40 genera by the Kungurian stage. Pelycosaurs occupied diverse ecological niches, including apex predation and herbivory; for instance, Dimetrodon (), a macro-carnivore reaching lengths of 3-4 meters, featured elongated neural spines forming a dorsal sail likely used for through solar absorption and radiative cooling. Similarly, Edaphosaurus (), an early terrestrial with comparable sail structures, utilized specialized grinding dentition for processing vegetation, exemplifying the group's adaptation to plant-based diets. Therapsids emerged in the late Kungurian and underwent rapid radiation following at the Kungurian-Roadian boundary, supplanting pelycosaurs as the dominant synapsids by the Middle Permian (). Early therapsid lineages included dinocephalians, robust forms such as Titanophoneus potens (Anteosauridae), which attained sizes up to 6 meters and served as top carnivores with powerful jaws for bone-crushing predation. Concurrently, dicynodonts within Anomodontia diversified as herbivores, evolving reduced with keratinous beaks for cropping vegetation, which supported their proliferation into over 60 species by the early and enabled exploitation of varied plant resources. Synapsids exerted profound ecological influence as the predominant terrestrial vertebrates in both Gondwanan and Laurasian faunas, numerically and taxonomically dominating Permian assemblages, with therapsids alone comprising a substantial portion—often exceeding 50 species in peak assemblages—of known genera. This dominance underscored their roles in trophic webs, from predation to herbivory, shaping community structures amid increasing and floral shifts. The extinction event, approximately 260 million years ago, imposed selective pressures that curtailed pelycosaurian diversity, reducing species counts from 59 in the early to just 2 by its close, effectively ending their prominence while sparing higher clades. experienced an initial diversity dip but rebounded swiftly, with anomodonts like dicynodonts proving resilient and setting the stage for their continued success.

Triassic Transitions to Mammal-like Forms

The Permian-Triassic extinction event, occurring approximately 252 million years ago, devastated terrestrial vertebrate communities, with around 70% of families lost, yet certain synapsids rapidly recolonized post-extinction ecosystems. , a , emerged as a quintessential "disaster taxon," dominating ( stage, ~252–251 Ma) faunas across Pangea, including sites in , , and . Its success stemmed from ecological versatility, including a generalist herbivorous diet, burrowing behavior, and developmental plasticity that enabled rapid growth in harsh, fluctuating environments, as evidenced by bone histology showing woven and parallel-fibered tissues indicative of fast life histories. By the mid- (, ~251–247 Ma), assemblages comprised up to 95% of vertebrate fossils in some localities, facilitating initial ecosystem recovery before declining as diversity rebounded. Amid this recovery, lineages streamlined, with gorgonopsians and therocephalians representing the final non-cynodont . Gorgonopsians, apex predators of the Late Permian, persisted sparingly into the (–Early , ~252–242 Ma) in regions like the Karoo Basin of and the Buntsandstein of , but their populations dwindled due to competition and environmental instability. Similarly, therocephalians, small carnivorous forms, survived into the (, ~242–237 Ma) in Gondwanan deposits from and , exhibiting skeletal features like reduced postcranial that hinted at transitional physiologies, though they ultimately failed to diversify further. In contrast, cynodonts began emerging prominently from the mid-Triassic onward, with basal forms like Galesaurus appearing in the (~250 Ma) and radiating into diverse ecological roles by the . Advanced cynodonts, such as from the Early Triassic Lystrosaurus Assemblage Zone (~248 Ma), displayed early signs of endothermy, inferred from stable oxygen isotope analyses (δ¹⁸Oₚ values ranging from -3.9‰ to +2.1‰ in co-occurring taxa) indicating elevated body temperatures and improved compared to Permian ancestors. These transitions coincided with notable shifts in body size and habitat preferences among cynodonts, driven by competitive pressures from rising groups. Advanced cynodonts underwent a pattern of size reduction, with body mass estimates for 29 eucynodont species spanning 0.009 kg (e.g., Kuehneotherium) to over 123 kg (e.g., Aleodon), but showing a shift toward lower evolutionary rates of size increase in prozostrodontian lineages by the (~237–227 Ma). This miniaturization, peaking in disparity during the before declining due to extinctions of larger forms, likely represented a plesiomorphic small-bodied state rather than paedomorphic evolution, allowing persistence in underutilized niches. Many occupied nocturnal or habitats to evade diurnal s, supported by brain reconstructions of revealing enlarged olfactory bulbs (18–26% of endocast length) and moderate encephalization quotients (0.16–0.38), enhancements suited for low-light sensory reliance on and touch via whisker-like structures. Such adaptations, including a secondary and refined mechanics, underscored their proto-mammalian trajectory. By the (~237–201 Ma), non-mammalian synapsid lineages had largely vanished, leaving only mammaliaforms as persistent survivors. Dicynodonts like faded by the , though other dicynodonts persisted until the , while gorgonopsians and therocephalians disappeared entirely by the , and many non-mammaliaform lineages succumbed to ecological replacement by dinosaurs around 225 Ma, though specialized groups like tritylodontids endured into the as the sole non-mammaliaform legacy alongside morganucodontids. This pruning set the stage for the cynodont-mammal continuum, with small-bodied forms like tritylodontids and morganucodontids enduring into the .

Mesozoic Survival and Cenozoic Mammalian Radiation

During the Era, non-mammalian synapsids persisted beyond the , with lineages such as tritylodontid cynodonts surviving into the , as evidenced by fossils like Bienotheroides wucaiensis from the in , representing one of the last known non-mammaliaform synapsids. However, the fossil record of cynodonts exhibits significant gaps during the and periods, particularly around the Jurassic- transition, where non-mammaliaform remains are scarce and largely restricted to , underscoring the need for further paleontological to clarify their decline. Early mammaliaforms, such as those in the family Morganucodontidae, bridged this interval, appearing in the and extending into the , with specimens like a newly described morganucodontan from the Upper displaying dental variations that highlight their adaptive persistence. Amidst dinosaur dominance, Mesozoic mammals and mammaliaforms remained small and ecologically marginalized, typically shrew-like in size—often under 100 grams—and occupying niches as insectivores or omnivores, which limited their body size expansion until the Cretaceous-Paleogene (K-Pg) boundary approximately 66 million years ago. Groups like multituberculates originated in the around 160 million years ago and diversified through the , achieving notable success with over 150 genera and adapting to herbivorous diets using specialized teeth. Similarly, s began diversifying in the , with fossils from and a 2023 discovery of the first South American monotreme, Patagorhynchus pascuali, from the indicating an extensive Gondwanan radiation into semiaquatic and burrowing lifestyles before the K-Pg extinction. These traits, including intermediate metabolic rates between reptiles and modern mammals as seen in , likely aided their survival in niche roles alongside larger reptiles. Recent 2025 studies using adaptive landscapes and fossil analyses indicate that the transition to upright posture in synapsids occurred later than previously thought, with early forms retaining sprawling gaits similar to reptiles until advanced therapsids. The K-Pg mass extinction event, which eradicated non-avian dinosaurs, triggered a profound radiation of surviving mammals in the , with placentals and marsupials rapidly achieving dominance through adaptive expansions into vacant ecological niches. Placentals underwent explosive diversification in the and Eocene, exemplified by radiations into aquatic forms like cetaceans (whales) and aerial specialists like chiropterans (bats), filling marine, terrestrial, and volant habitats previously unoccupied by synapsids. Marsupials similarly radiated, particularly in and , evolving diverse morphologies such as gliding possums and herbivorous wombats, though they were later outcompeted by placentals in many regions. This post-extinction burst increased mammalian fourfold within the first million years, establishing the modern mammalian fauna. Recent discoveries have illuminated these Mesozoic transitions, with the 2011 description of Juramaia sinensis from the of (~160 million years ago) identifying it as the earliest known eutherian and pushing back the placental-marsupial divergence. In the 2020s, finds such as two new Jurassic mammaliaforms (Shenshoua and Sinobaatar) from have revealed early dental and innovations, while a 2024 shuotheriid species and a 2025 tritylodontid from the Jurassic further fill gaps in mammaliaform and non-mammalian synapsid diversity, refining our understanding of pre-Cretaceous evolution.

Phylogenetic Relationships

Position Within Amniota

Synapsida and together comprise the crown group Amniota, defined as the of these two clades and all of its descendants. Molecular clock analyses using genome-wide datasets estimate the common ancestor of crown-group Amniota lived approximately 319 million years ago (Ma; 95% confidence interval: 308.5–334.7 Ma) during the , though recent fossil trackway evidence suggests an earlier origin by ~359–354 Ma in the Early . This divergence marks the basal split within Amniota, with Synapsida leading to mammals and encompassing reptiles and birds. Evidence for Synapsida as the sister clade to includes shared synapomorphies of , such as the amniotic egg, which encloses the in a protective fluid-filled sac and allows fully terrestrial reproduction independent of aquatic environments. estimates further support this relationship, with a median age of ~319 Ma, consistent with the earliest records of derived amniotes now extended into the Early by trackway discoveries. Controversies surrounding parareptiles, once considered a separate , have reinforced Synapsida's position as the to a more inclusive . For instance, recent phylogenetic analyses place families like Millerettidae as stem-sauropsids or close sisters to crown-group diapsids such as , integrating former parareptiles into and excluding them from a basal position relative to Synapsida. Fossil calibrations for the amniote tree often draw on early taxa like , a Viséan-stage (approximately 338 Ma) from the Early that exhibits -like features and is positioned as potentially basal to Synapsida or the broader stem in some analyses. This placement helps constrain the minimum age of the Synapsida-Sauropsida divergence and aligns with the origins of amniote diversification, now supported by even earlier trackway evidence.

Interrelationships Among Synapsid Groups

The interrelationships among synapsid groups are primarily resolved through cladistic analyses of morphological characters, revealing a basal of non-therapsid synapsids ("pelycosaurs") succeeded by the more mammal-like therapsids. Basal branching patterns position as the to a comprising and Therapsida, with representing an early offshoot within this structure. This topology is supported by comprehensive meta-analyses integrating hundreds of morphological matrices, which confirm the of (including sphenacodontians and edaphosaurids) as more closely related to Therapsida than to ophiacodontids or caseasaurs. Within , sphenacodontians form a basal sister to Therapsida, as evidenced by shared cranial features like enlarged temporal fenestrae in early therapsids. Within Therapsida, occupies the basalmost position, followed by a branching pattern that unites Anomodontia and as successive sister clades. itself comprises as the basal subclade, with Cynodontia (including therocephalians in some resolutions) as its , a relationship bolstered by shared postcranial traits such as more erect limb postures. Anomodontia, encompassing herbivorous forms like dicynodonts, branches off prior to the diversification of theriodonts, supported by dental specializations absent in gorgonopsians. These interrelationships are derived from large-scale phylogenetic datasets emphasizing and skeletal , with integrations from Permian localities providing critical calibration. Cynodontia exhibits a progressive hierarchy toward mammalian features, with Epicynodontia (including taxa like and Galesaurus) forming a basal leading to . Within , represents an intermediate characterized by advanced auditory structures, directly ancestral to , which includes the earliest near-mammalian forms with differentiated teeth and secondary elements. Haramiyidans, known from and fossils, are positioned as early members of crown Mammalia, potentially within or sister to , based on multituberculate-like and inferred arboreal adaptations. This cynodont phylogeny is reinforced by high-resolution 3D imaging of cranial fossils, highlighting evolutionary trends in and . These resolved topologies stem from morphological matrices, such as those compiled in meta-phylogenetic syntheses incorporating over 260 datasets, which prioritize cranial and postcranial characters while accounting for stratigraphic and biogeographic constraints. For instance, a 2017 study on interrelationships utilized expanded matrices to refine placements within Therapsida, integrating new data to resolve polytomies in earlier analyses. Cladograms generated from such methods consistently depict as a series of nested monophyletic groups, with discoveries periodically refining branch supports but upholding the core structure.

Uncertainties and Recent Discoveries

One persistent uncertainty in synapsid phylogeny concerns the placement of varanopids, which have been debated as either basal synapsids or stem-sauropsids (s). Recent analyses using scans of cranial endocasts from multiple varanopid specimens, including Varanops brevirostris and Heleosaurus scholtzi, reveal neurosensory features such as an ossified and maxillary canal morphology that align closely with other early synapsids rather than sauropsids, supporting their position as the earliest-diverging synapsids. However, a 2020 morphological study proposed a diapsid affinity based on postcranial traits, and preliminary 2024 analyses suggest some varanopid taxa may nest within sauropsids, highlighting ongoing topological instability at the base of Amniota. Advances in dicynodont have revised timelines for their , addressing gaps in diversity. Prior estimates from 2003 posited dicynodont survival into the based on fragments, but reexamination identified these as bones, limiting their range to the . The 2019 discovery of bojani in Norian-Rhaetian deposits of extends undisputed dicynodont persistence into the (~210-201 Ma), representing the youngest known member of the group and contradicting earlier views of their decline by the (~240 Ma). This ~9-ton with erect limbs indicates dicynodonts coexisted with early dinosaurs as large megaherbivores, filling ecological roles previously attributed solely to archosaurs. Jurassic cynodont records remain sparse, particularly for non-mammalian forms, creating gaps in understanding the transition to mammals. The Yanliao Biota (Middle-Late Jurassic, ~164-157 Ma) in northeastern China has yielded new mammaliaform fossils since 2023, including the euharamiyidan Mirusodens caii, a skeletal specimen preserving soft tissues that elucidates allotherian dental and locomotor evolution. Updated radiometric dating of Yanliao strata in 2023 constrains the biota to 164-157 Ma, aligning it with the diversification of crown-group mammals and highlighting rapid ecological shifts among cynodonts toward insectivory and arboreality. These finds underscore the underrepresentation of Mesozoic non-mammalian cynodonts outside Laurasia, with few post-Triassic Gondwanan examples, emphasizing the need for broader sampling to resolve mammal origins. A major 2025 discovery has recalibrated the timeline of early evolution: trackways attributed to crown-group s from the Snowy Plains Formation in (~359–354 Ma, Early ) and Silesia, (~330–323 Ma), push back the inferred origin of the Synapsida-Sauropsida split by at least 35–40 million years compared to prior records. This evidence suggests crown Amniota existed much earlier in the , prompting reconciliation with estimates around 319 Ma and highlighting potential ghost lineages or calibration needs in phylogenetic models. Methodological innovations have begun resolving basal synapsid ambiguities. High-resolution and imaging of Permian specimens, such as those from Orobates and , have revealed neurosensory adaptations like enlarged trigeminal canals, informing phylogenetic placements and behavioral inferences since the early 2020s. Integrated morphological phylogenies incorporating postcranial data, as in 2024 analyses of origins, recover more stable trees for basal groups but highlight in therocephalians, advancing beyond earlier partition-based conflicts. Although phylogenomic approaches remain limited for extinct basal taxa due to DNA preservation issues, calls persist for intensified excavations in Gondwanan deposits, where synapsid diversity is poorly documented compared to , to test Laurasian-origin hypotheses for therapsids.

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