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Synapsida

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Synapsida
Synapsida
Nobu Tamura Max Bellomio Roman Uchytel Dmitry Bogdanov Fir0002 John and Karen, r · Public domain · source
NameSynapsida
Fossil rangeCarboniferous–Present (as mammals)
TaxonClade
AuthoritySee paleontological literature
Subdivision ranksMajor groups
Subdivision* Pelycosauria (traditional grade) * Therapsida * Cynodontia * Mammalia

Synapsida

Synapsida are a major clade of amniotes originating in the Late Carboniferous that gave rise to mammals. They include a broad array of extinct Permian and Mesozoic taxa and the extant Mammalia; their history spans interactions with contemporaneous groups such as Sauropsida, Archosauria, and Theropoda. Synapsid evolution influenced terrestrial ecosystems through the Permian–Triassic extinction event, the rise of Dinosaurs, and the eventual dominance of Mammals.

Evolutionary history

Synapsid origins trace to Carboniferous assemblages studied by paleontologists like Edward Drinker Cope and Othniel Charles Marsh, with early members appearing in faunas alongside Eryops and Dimetrodon-grade forms. The early diversification of pelycosaur-grade synapsids paralleled contemporaneous radiations of Anapsida-referenced taxa and later transitions to therapsids occurred during the Guadalupian and Lopingian epochs, influencing communities that included Gorgonopsia, Thrinaxodon-containing assemblages, and Dicynodontia. Major turnover during the Permian–Triassic extinction event reshaped synapsid diversity, allowing cynodonts and other clades to persist into the Triassic, coexisting with Cynognathus and early archosaurs associated with formations like the Karoo Basin and Ischigualasto Formation.

Anatomy and physiology

Synapsid defining traits include a single temporal fenestra bounded by the postorbital and squamosal bones, a feature compared and contrasted with fenestration in Diapsida and Anapsida-described taxa. Cranial and postcranial modifications—such as differentiated dentition in taxa like Thrinaxodon, expansion of the secondary palate in therocephalians, and limb posture shifts seen in Gorgonopsia reconstructions—reflect transitions in feeding and locomotor strategies. Respiratory and metabolic inferences derive from studies of turbinate-like structures in derived cynodonts and bone histology compared with work by researchers affiliated with institutions like the Smithsonian Institution and Natural History Museum, London. Physiological trends toward endothermy and parental care are inferred from comparisons to extant Monotremata, Marsupialia, and Eutheria.

Classification and taxonomy

Traditional classification divided early synapsids into pelycosaurs and therapsids, with modern cladistics favoring monophyletic groupings such as Therapsida and Cynodontia. Important taxonomic revisions have been published by paleontologists working at institutions including the American Museum of Natural History, the University of Chicago, and the University of California, Berkeley. Higher-level taxa associated with synapsids include Caseidae, Ophiacodontidae, Sphenacodontidae, Galesauridae, and Probainognathia. Mammaliaformes and crown Mammalia occupy terminal positions in modern phylogenies discussed at conferences like the Society of Vertebrate Paleontology meetings.

Paleobiology and ecology

Synapsids occupied diverse ecological roles from apex predators like sphenacodontids to herbivorous dicynodonts influencing Triassic flora such as Glossopteris and Lycopodiophyta-dominated communities. Paleoenvironments containing synapsids include permian rift basins, floodplain deposits in the Karoo Basin, and Triassic continental strata of China and Argentina. Isotopic and microwear analyses conducted by researchers from University of Bristol and Harvard University inform on diet, thermoregulation, and seasonal behaviors, while nest site inferences draw on comparisons with extant Monotremata and fossil nests reported from formations studied by teams at the Field Museum.

Fossil record and notable genera

The synapsid fossil record is rich, with notable genera represented in museum collections worldwide: early pelycosaurs like Dimetrodon, Sphenacodon, and Edaphosaurus; therapsid groups exemplified by Gorgonops, Inostrancevia, Lystrosaurus, Dicynodon, and Cistecephalus; cynodonts including Thrinaxodon, Cynognathus, Procynosuchus, Morganucodon, and Exaeretodon; and mammaliaforms such as Eozostrodon and Docodon. Key fossil-bearing localities include the Georgian (Caucasus) deposits yielding Inostrancevia, the Karoo Basin with Lystrosaurus beds, the Chinle Formation, and the Ischigualasto Formation containing early dinosaur-synapsid faunal lists. Iconic specimens are curated at institutions such as the Natural History Museum, Vienna, Royal Ontario Museum, and Museo Paleontológico Egidio Feruglio.

Transition to mammals

The synapsid-to-mammal transition involves staged acquisition of mammalian traits: heterodont dentition, precise occlusion, enlargement of the dentary, reduction of post-dentary bones leading to the middle ear, development of the secondary palate, and probable shifts toward endothermy and lactation. Key fossil taxa illuminating this transition include Morganucodon, Hadrocodium, Tritylodon, and Sinoconodon, with pivotal work produced by researchers at the University of Cambridge and Yale University. Debates over timing and tempo reference events such as the Triassic-Jurassic extinction event and are informed by discoveries from China's Liaoning Province, Portugal, and North America.

Category:Prehistoric synapsids