Patriofelis
Patriofelis is an extinct genus of carnivorous placental mammals from the extinct subfamily Oxyaeninae within the extinct family Oxyaenidae, which lived from the early to middle Eocene, during the Bridgerian stage of NALMA. The first remains were discovered in 1869 by geologist Ferdinand Vandeveer Hayden, and the genus was named the following year by Joseph Leidy. Over the next few decades, additional specimens would be named from the same locality, many assigned to genera of their own or to separate species within Patriofelis. Now, only two are recognised: Patriofelis ulta, the type species, from the lower Bridger Formation and the Huerfano Formation of Colorado, and P. ferox, from the lower Bridger and lower Washakie Formations of Wyoming and Colorado, and the Clarno Formations at the John Day Fossil Beds National Monument, Oregon.
Patriofelis is the largest oxyaenid to preserve postcranial fossils. P. ulta, the smaller species, has been estimated at around, while the larger P. ferox has been estimated at. Patriofelis had a skull around the same size as of that of a lion, though shorter and broader in a way often likened to otters. A semi-aquatic lifestyle has been suggested for Patriofelis, though there are aspects of its anatomy which make this very unlikely. Its backbone was stiffened by bony structures which projected from its vertebrae, inhibiting the usual mammalian swimming method, in which the spine undulates up and down. Originally it was suggested to be a turtle specialist, though its teeth were not adapted for crushing, but rather for slicing. While some older sources reported that Patriofelis had limited arm flexibility, recent studies have shown that its forearms were capable of a great degree of pronation and supination. Though there are various hypotheses for how Patriofelis lived, the most likely is that it was a terrestrial ambush predator which hunted by grappling its prey.
Patriofelis was among the top predators of at least some localities, competing with certain crocodilians and with mesonychids. During the early to middle Eocene, much of North America was covered in wet subtropical forest and marshland, and Patriofelis was present in geologic formations corresponding to both of these environments. It has been suggested that the extinction of the genus, along with other oxyaenids, corresponded with a shift in available habitat, as the end of the Eocene was marked by a period of cooling and drying which led to the replacement of dense, swampy, forests to more temperate open forests.
History
Early history
Some time in 1869, geologist Ferdinand Vandeveer Hayden recovered a pair of partial mandibular rami from strata belonging to the Bridger Formation. These bones were later catalogued as USNM V105. In a March 1870 publication in the Proceedings of the Philadelphia Academy, palaeontologist Joseph Leidy described the jaw scientifically, making it the holotype of a new genus and species, Patriofelis ulta. He believed that P. ulta was an early member of Felidae, the cat family, hence its name. Two years later, in August 1872, Othniel Charles Marsh described the remains of a "gigantic Carnivore" from the same locality, to which he assigned the name Limnofelis ferox. Marsh's specimen consisted of skull material, vertebrae, and "other less important parts of the skeleton". Marsh also described a second species, L. latidens, from an upper premolar from the same locality.In the summer of 1879, Jacob Lawson Wortman discovered teeth and limb bones from another specimen. These remains came to the attention of Edward Drinker Cope, who, in 1880, gave them the binomial name of Protopsalis tigrinus. In 1892, Wortman suggested a second Protopsalis, P. leidyanus, based on remains in the Princeton Collection. Two years later, Wortman published a paper discussing the osteology of Patriofelis ulta. He determined that the other taxa could be rendered junior synonyms, as there was no convincing evidence in the form of diagnostic traits that they were different taxa. Several other species have been described which have been consistently synonymised, leaving only P. ferox and P. ulta as valid species.
Two relatively complete specimens of Patriofelis have been discovered in the interim, both in 1953. The first of these served as the foundation of a 1957 paper on P. ulta
Classification
Patriofelis is a member of the family Oxyaenidae, which is in turn part of the order Oxyaenodonta. Oxyaenids were at one point considered members of a larger order, Creodonta, alongside hyaenodonts. More recent papers have not supported the monophyly of creodonts, and the link between the two is predicated largely on the presence of a blade on the metastyle of the first molar, a trait present in many eutherians.Description
Size
Patriofelis is the largest oxyaenid from which postcranial remains are known. Wortman suggested that its overall body size was roughly equal to that of a black bear, though was working under the assumption of felid affinities. The type species, of Patriofelis, P. ulta, was the smaller species, weighing at least. In a 2010 publication, Michael Morlo, Gregg F. Gunnell, and Doris Nagel provided general body mass estimates for both Patriofelis species of. In a 2024 paper, Mark S. Juhn and colleagues used a scaling method proposed by Van Valkenburgh in 1990, wherein the size of the largest lower molar was used in a regression analysis, to calculate the body sizes of various extinct mammalian predators, listing their mass estimates in their supplemental materials. Using this method they obtained a body mass of for P. ulta, and a larger body mass of for the larger P. ferox.Skull
The skull of Patriofelis ulta described by Wortman was roughly the same size as that of a lion. He noted that it was fairly short, broad and low, and he likened it to the skulls of seals, though his initial restoration was inaccurate in that it depicted the skull as higher than it actually would have been. Charles Lewis Gazin noted that not only was the modification of its skull more extreme than how Wortman had depicted it, but it was superficially akin to that of an otter. The premaxilla in P. ulta was fairly reduced, forming a narrow rim of bone along the anterior margin of the maxilla. The maxillae were fairly short when viewed from the side, although their nasal processes were very long, extending posteriorly over the lacrimal bones. The nasals of P. ulta were broad anteriorly, tapering posteriorly and widening yet again around the sutures between the maxillae and frontals, after which they once again tapered. The frontals were broad anteriorly and tapered posteriorly. The parietals were long and slender, supporting a fairly well-developed sagittal crest. P. ultaBrain endocast
The brain anatomy of P. ulta is known in part from an endocast. Its cerebellum was fairly large, with a thickly walled cavity, and was not at all covered by the cerebral lobes. As in many Palaeogene mammalian carnivores, the cerebral cavity had at least two longitudinal convolutions. It is not certain if a crucial sulcus was present.Dentition
The dental formula of Patriofelis is uncertain, though was rendered by Gazin as. Its teeth were very robust in comparison to other oxyaenid teeth, and have been variously compared to those of felids, or to those of hyaenids. The upper incisors were fairly simple, with the medial pair being smaller than the lateral pair. The lateral pair were far larger and were somewhat caniniform. The true upper canines were very robust, with deep roots. They were oval-shaped in cross section, as opposed to being sabrelike or laterally compressed, and in the specimen studied by Gazin they had been blunted by wear. In 1900, Henry Fairfield Osborn noted that oxyaenid cheek teeth bore adaptations for slicing and for cutting into bone, such as the loss of the talonid, as in felids. True bone-crushing is unlikely, at least in Patriofelis, as P. ultaPostcranial skeleton
Patriofelis had seven cervical vertebrae, of which five are known from UMNH VP 550. In both species, all of the vertebrae beyond the axis had robust transverse processes. The sixth cervical vertebra is long and angled more ventrally than in modern carnivorans. No neural spines are known from P. ulta, although those of P. ferox were decently large, and it is likely the same is true of both species. Beyond the neck, PatriofelisThe limbs of Patriofelis, particularly its forelimbs, were fairly short and robust. The deltopectoral crest of the humerus was "immensely developed", extending two-thirds down the length of the humeral shaft. Regressions found the humeri of Patriofelis to have been more robust than any felid. In the case of P. ferox, the scar on the deltoid of the deltopectoral crest was located more distally than a felid of comparable size. The bones of the forearm were extremely robust, especially the ulna. The ulna had a very robust, medially angled olecranon; it and the semilunar notch account for about a third of the bone's total length, longer than that of carnivorans. Though some have interpreted the morphology of the radius as a sign that Patriofelis was capable only of limited arm rotation, it is likely that it was capable of a strong degree of both pronation and supination. The metacarpals were short and robust, arranged and angled in such a way that the feet would likely have been splayed in life, and the same is true of the hind feet. Each digit was tipped in thick, blunt claws. The ilium of Patriofelis was fairly small compared to the ischium and pubis, and was trihedral in cross-section due to the presence of a pronounced ridge running along its lateral surface. The acetabulum was fairly shallow. The trochanteric fossa of the femur was deep, extending quite far down the posterior part of the bone. The distal portion of the femur is not known, so the full extent of the fossa is not certain, though it exceeds what is seen in carnivorans. The tibia is slender in comparison to the femur, though is still fairly robust. It bore a prominent cnemial crest, larger than that of Oxyaena. The proximal end of the fibula is characterised by a very robust interosseous crest. The patellas of Patriofelis were similar to those of carnivorans, being generally teardrop-shaped. The calcaneum was fairly robust and generally resembled that of carnivorans with a plantigrade gait, one where the entire foot, including the heel, was pressed flat on the ground while walking. The metatarsals were relatively short and were quite homogenous in length, although the first was shorter than the others and the third was longer.
Palaeobiology
J. L. Wortman initially suggested that Patriofelis was a semi-aquatic, otter-like predator, one which might have specialised in hunting turtles. Henry Fairfield Osborn disagreed with this assessment, arguing in 1900 that it was an arboreal predator which behaved similarly to cats. William Diller Matthew in 1909 disagreed with both ideas, as its short limbs and blunt claws would have made it more suited for hunting on the ground. In their 2022 reassessment of PatriofelisPalaeoecology
Patriofelis lived in North America during the Bridgerian North American Land Mammal Age, or NALMA. Fossils of both species have been found in formations in Wyoming, Colorado, and Oregon.One of the environments Patriofelis inhabited, the depositional environment for the so-called Nut Beds of the Clarno Formation, is the most biodiverse assemblage of fossil flora yet recorded, preserving 66 genera and 76 species of trees and around 173 species of plants overall. Some of the Nut Beds flora is known exclusively from wood, though other plants are known from additional material. Overall there is great floral overlap between the Nut Beds and modern environments, with hamamelidaceans, rosaceans, and pinaceans being known, among others. The reconstructed palaeoenvironment of the Clarno Formation indicates that Patriofelis would have inhabited wet, semitropical forested ecosystems, of the sort which covered much of North America during the early-middle Eocene.
Patriofelis is also known from the Black Forks Member, the lower member of the Bridger Formation, which preserves an environment which alternated between marshlands with braided streams and vast yet shallow lakes. It also preserves the same kind of semitropical forest as the Clarno Formation. Both species of Patriofelis are recorded in the Bridger Formation, although only P. ulta is known from the lower portion. Also known from the Black Forks Member are catfish, salamanders, frogs, varanid lizards, boas, turtles, several crocodilians, the primates Anaptomorphus, Notharctus, Omomys, Trogolemur, Smilodectes, and Uintasorex, the tillodonts Trogosus and Tillodon, the pholidotans Metacheiromys and Tetrapassalus mckennai, various rodents in the families Cylindrodontidae, Paramyidae, and Sciuravidae, the mesonychids Harpagolestes and Mesonyx, the hyaenodonts Limnocyon, Sinopa, Thinocyon, and Tritemnodon, the oxyaenodont Machaeroides, the carnivorans Miacis, Oodectes, Palaearctonyx, Uintacyon, Viverravus, and Vulpavus, the hyopsodont Hyopsodus, the dinoceratan Bathyopsis, the equid Orohippus, the brontotheres Limnohyops and Palaeosyops, the helaletid Helaletes, the hyrachyid Hyrachyus, the dichobunids Antiacodon and Microsus, and the helohyid Helohyus.
In a 2019 thesis, Anne E. Kort noted that Patriofelis would have been among the top predators, alongside crocodilians and perhaps the mesonychids, of the environments it inhabited. However, compared to Patriofelis, mesonychids had dentition more adapted for scavenging, were more cursorial, and had a boarder distribution.