Limnoscelis (/limˈnäsələ̇s/, meaning "marsh footed") is an extinct genus of large diadectomorph tetrapods from the Late Carboniferous to early Permian of western North America. It includes two species: the type species Limnoscelis paludis from New Mexico, and Limnoscelis dynatis from Colorado, both of which are thought to have lived concurrently. No specimens of Limnoscelis are known from outside of North America. Limnoscelis was carnivorous, and likely semiaquatic, though it may have spent a significant portion of its life on land. Limnoscelis had a combination of derived amphibian and primitive reptilian features, and its placement relative to Amniota has significant implications regarding the origins of the first amniotes.

The type species Limnoscelis paludis was collected by the fossil hunter David Baldwin between 1877 and 1880 from the El Cobre Canyon beds of the Cutler Formation, New Mexico. Baldwin was collecting fossils in service of the paleontologist Othniel Charles Marsh during the bone wars. Although Marsh would describe several specimens from Baldwin's collections, many fossils, including Limnoscelis paludis, would be deposited without description at the Peabody Museum of Natural History at Yale College for several decades.

Limnoscelis paludis was finally described in 1911 by the paleontologist Samuel Wendell Williston, who discovered three specimens of the genus in the Yale Peabody Museum collections. These included one relatively complete articulated specimen which included the skull (the holotype, YPM 811), and two less-complete post-cranial skeletons (MCZ 1947 and MCZ 1948, formerly YPM 819 and YPM 809 respectively). Williston named the fossil Limnoscelis paludis, referencing the marsh-like environment that he hypothesized Limnoscelis might have inhabited. In 1912, Williston described the discovery of an additional specimen, collected by himself at the same locality as the previous specimens.

More Limnoscelis fossils were collected between 1966 and 1973 by the paleontologist Peter P. Vaughn from the Sangre de Cristo Formation in Colorado, which would later be attributed to the species Limnoscelis dynatis. Vaughn, however, did not initially recognize these materials as belonging to Limnoscelis, instead attributing several fossil elements to the Rhachitomi or the Anthracosauria. The presence of Limnoscelis at the locality was finally recognized upon the collection of more fossils from the genus, which would amount to three disarticulated specimens (the holotype CM 47653, and paratypes CM 47651 and CM 47652). These fossils, particularly the holotype, were referenced as representing the genus Limnoscelis in several publications. However, the fossils themselves were not recognized as their own species until paleontologists David S. Berman and Stuart S. Sumida described the fossils in 1990. They designated the new species as Limnoscelis dynatis, with “dynatis” being derived from the Greek dynatos meaning “strong” or “powerful”, referencing the genus’ capability as a “formidable predator”.

The skeleton of Limnoscelis was relatively large, with Limnoscelis paludis measuring 7 feet (around 2 meters) long. Portions of the skeleton are poorly ossified, with many cartilaginous elements.

Limnoscelis had a relatively elongated skull, with a narrow snout and wider posterior region. Its teeth were conical and labyrinthodont, with infolding of enamel and dentin. Limnoscelis had particularly well-developed incisors, peaking in size at the anterior maxilla, similar to the placement of the canine tooth of many derived synapsids. This tooth morphology has been used to infer that Limnoscelis was a carnivore. The mandible of Limnoscelis was well-built, with large processes for jaw muscle attachment, indicating that it had a powerful bite. In addition to its premaxillary, maxillary, and dentary teeth, Limnoscelis had additional palatal teeth on transverse flanges of its pterygoid. These flanges consisted of an anterior row of smaller blunt denticles, and a posterior row of larger teeth, with neither having labyrinthodont infolding. The pterygoid of Limnoscelis articulated with the basisphenoid. The occipital region of Limnoscelis was relatively flat, similar to that of some basal synapsids. Limnoscelis had a single occipital condyle. Limnoscelis had an anapsid skull fenestration pattern, lacking temporal fenestrae. However, the supratemporal of Limnoscelis has been pushed posteriorly and ventrally, creating a “line of weakness” between the supratemporal, postorbital, and squamosal bones. This “line of weakness” has been proposed to be a precursor to the synapsid temporal fenestra, although this hypothesis has been challenged.

Limnoscelis had 26 presacral vertebrae. These vertebrae had swollen neural arches, and amphicoelous notochordal centra. The vertebrae of Limnoscelis were typically longer than they were wide, but varied in size and shape throughout the vertebral column, along with neural spine height. Limnoscelis had a multipartite atlas and axis complex, with a ventral anterior process of the axis intercentrum articulating with that of the atlas. Limnoscelis had single headed ribs, though they might have had cartilaginous caps to allow the passage of the vertebral artery between the capitulum and tubercle of each rib. Limnoscelis had two sacral vertebrae, a feature shared with amniotes, though the second sacral vertebra is reduced compared to the first.

The pectoral girdle of Limnoscelis consisted of a single interclavicle, with paired clavicles, scapulocoracoids, and cleithra on its right and left sides. The cleithrum was small and possibly vestigial, indicating further ossification of the scapulocoracoid. Limnoscelis may also have had cartilaginous extensions above the scapolocoracoid, compensating for this reduction in size. The scapulocoracoid of Limnoscelis had two fused coracoid elements, which it shares with a number of basal amniotes, but which differentiates Limnoscelis from its fellow diadectomorphs (which only had a single coracoid). The ilium of Limnoscelis possessed an iliac shelf, a low ridge extending anteroposteriorly across the dorsal ilium, a synapomorphy of the Diadectomorpha. The forelimbs and hindlimbs of Limnoscelis were short and robust, giving the animal a low sprawling posture. It had a phalangeal formula of 2-3-4-5-3 for the manus, and a formula of 2-3-4-5-4 for the pes, which it shared with basal amniotes. Originally, it was thought that Limnoscelis possessed two proximal tarsals, consisting of the fibulare and a preaxial element comprising a fused tibiale and intermedium. However, subsequent analyses have cast doubt on this assessment, instead proposing that the two preserved proximal tarsals are the fibulare and intermedium, and that Limnoscelis possessed an unfused tibiale along with these elements. The absence of the tibiale has been attributed either to poor preservation (possibly due to being cartilaginous), or to being displaced and misidentified as one of the distal tarsals. This differs from other diadectomorphs in the family Diadectidae, which possessed an astragalus consisting of a fused tibiale, intermedium, and proximal centrale, similar (and possibly homologous) to the astragalus or talus bone found in amniotes.