Palaeogale Temporal range: | |
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Lateral view of Bunaelurus (=Palaeogale) from Matthew 1902 | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Mammalia |
Order: | Carnivora |
Suborder: | Feliformia |
Family: | † Palaeogalidae |
Genus: | † Palaeogale von Meyer 1846, p. 474 |
Species [1] | |
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Synonyms | |
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Palaeogale is an extinct genus of carnivorous mammal known from the Late Eocene, Oligocene, and Early Miocene of North America, Europe, and Eastern Asia. A small carnivore often associated with the mustelids, Palaeogale might have been similar to living genets, civets, and linsangs.
The ancestry of Palaeogale remains enigmatic. The genus appears in Europe 32 Ma, after the Grande Coupure, but 35-36 Ma-old (Chadronian NALMA) specimens from Pipestone Springs, Montana, are the oldest known. [2] Palaeogale survived until the late Early Miocene of Europe and the early Early Miocene of East Asia. [3]
Morlo & Nagel 2007 noted that the Palaeogale specimens found in Mongolia are the most plesiomorphic (p1 double-rooted, m2 relatively large, very small overall size) and that the genus probably originated there and migrated to Europe and North America. [3]
Palaeogale was the size of a small mustelid but had a hypercarnivorous dentition and its taxonomic position remains enigmatic. Its dental morphology includes both mustelid (reduced m2) and feliform (slit-like carnassial notch, loss of metaconid on m2, presence of parastyle on P4) features, and Palaeogale is typically placed in Carnivora incertae sedis . [4] [5]
The body mass of Palaeogale sectoria, one of the smallest species, has been estimated to much less than a kilo based on teeth sizes. It was probably semifossorial. [6] P. sanguinarius is slightly larger than P. dorothiae and probably equivalent in age. [5]
When von Meyer 1846 named the genus Palaeogale and two species (P. pulchella and P. fecunda), he only gave a very vague description of these taxa. Gervais 1848 described a related species, Mustela minuta, which Schlosser 1888 [7] thought identical and named Palaeogale minuta, a name that has remained accepted for the type species. [8]
Simpson 1946 wrote that when Cope 1873 described the North American species Bunaelurus lagophagus, he distinguished the genus from the European Plesiogale (=Palaeogale in part) based on differences in M2. Simpson, however, thought this molar was "very closely similar" in both genera and synonymized Cope's genus with Palaeogale. [9] Matthew 1902 described a skull which he referred to Cope's genus "Bunaelurus". The skull was found without lower jaws (on which all Bunaelurus specimens were based), but Matthew argued that the correspondence in horizon and size made the "identification reasonably safe." He nevertheless described it as a "Palaeogale with a minute second molar still retained." [9] [10]
Species | Time span | Size | Dental morphology |
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P. sectoria | Late Eocene, Early Oligocene | Medium | M2 and p1 retained |
P. minuta | Late Oligocene, Early Miocene | Smallest | M2 and p1 lost |
P. hyaenoides | Miocene | Medium | |
P. dorothiae | Late Oligocene, Early Miocene | Largest |
de Bonis 1981 synonymized the then described Palaeogale species from Europe and North America into four taxa based on age occurrence, size difference, presence of M2, and loss of p1. Two species from Mongolia (P. ulysses and P. parvula) described by Matthew & Granger 1924 were synonymized by Simpson 1946 [11] who argued that the smaller individuals most likely were female and the larger male members of the same species, like in modern mustelids. [4]
Flynn & Galiano 1982 created the infraorder Aeluroida to accommodate Palaeogale, Ictidopappus , and Feloidea and argued that these taxa share some derived dental features not present in other feliforms, and retain some primitive dental features that have been modified in other feliforms. [12] Flynn & Galiano, however, placed Ictidopappus as incertae sedis within this infraorder, [13] and pointed out that the grouping of Palaeogale and the Viverravidae in the superfamily Viverravoidea was a hypothetical arrangement. [14]
Baskin 1998 accepted Palaeogale as closely related to the family Viverravidae but, because it does not share any "unambiguous synapomorphies with either Feliformia or Caniformia", should be considered incertae sedis within Carnivora (together with Stenogale , another very small carnivoran.) [5]
Carnivora is an order of placental mammals that have specialized in primarily eating flesh, whose members are formally referred to as carnivorans. The order Carnivora is the fifth largest order of mammals, comprising at least 279 species.
Amphicyonidae is an extinct family of terrestrial carnivorans belonging to the suborder Caniformia. They first appeared in North America in the middle Eocene, spread to Europe by the late Eocene, and further spread to Asia and Africa by the early Miocene. They had largely disappeared worldwide by the late Miocene, with the latest recorded species at the end of the Miocene in Africa. They were among the first carnivorans to evolve large body size. Amphicyonids are colloquially referred to as "bear-dogs".
Caniformia is a suborder within the order Carnivora consisting of "dog-like" carnivorans. They include dogs, bears, raccoons, and mustelids. The Pinnipedia are also assigned to this group. The center of diversification for the Caniformia is North America and northern Eurasia. Caniformia stands in contrast to the other suborder of Carnivora, the Feliformia, the center of diversification of which was in Africa and southern Asia.
Nimravidae is an extinct family of carnivorans, sometimes known as false saber-toothed cats, whose fossils are found in North America and Eurasia. Not considered to belong to the true cats, the nimravids are generally considered closely related and classified as a distinct family in the suborder Feliformia. Fossils have been dated from the Middle Eocene through the Late Miocene epochs, spanning about 33.2 million years.
Ailuridae is a family in the mammal order Carnivora. The family consists of the red panda and its extinct relatives.
Viverravidae is an extinct monophyletic family of mammals from extinct superfamily Viverravoidea within the clade Carnivoramorpha, that lived from the early Palaeocene to the late Eocene in North America, Europe and Asia. They were once thought to be the earliest carnivorans and ancestral to extant ones, but now are placed outside the order Carnivora based on cranial morphology as relatives to extant carnivorans.
Eupleridae is a family of carnivorans endemic to Madagascar and comprising 10 known living species in seven genera, commonly known as euplerids, Malagasy mongooses or Malagasy carnivorans. The best known species is the fossa, in the subfamily Euplerinae. All species of Euplerinae were formerly classified as viverrids, while all species in the subfamily Galidiinae were classified as herpestids.
Phlaocyon is an extinct genus of the Borophaginae subfamily of canids native to North America. It lives from the Early Oligocene to the Early Miocene epoch 33.3–16.3 Mya, existing for approximately 17.3 million years. It is closely related to Cynarctoides.
The John Day Formation is a series of rock strata exposed in the Picture Gorge district of the John Day River basin and elsewhere in north-central Oregon in the United States. The Picture Gorge exposure lies east of the Blue Mountain uplift, which cuts southwest–northeast through the Horse Heaven mining district northeast of Madras. Aside from the Picture Gorge district, which defines the type, the formation is visible on the surface in two other areas: another exposure is in the Warm Springs district west of the uplift, between it and the Cascade Range, and the third is along the south side of the Ochoco Mountains. All three exposures, consisting mainly of tuffaceous sediments and pyroclastic rock rich in silica, lie unconformably between the older rocks of the Clarno Formation below and Columbia River basalts above.
Feliformia is a suborder within the order Carnivora consisting of "cat-like" carnivorans, including cats, hyenas, mongooses, viverrids, and related taxa. Feliformia stands in contrast to the other suborder of Carnivora, Caniformia.
Ursoidea is a superfamily of arctoid carnivoran mammals that includes the families Subparictidae, Amphicynodontidae, and Ursidae which the last family includes the extant lineages of bears as well the extinct Hemicyoninae and Ursavinae. The interrelationships of ursoids has had slight arrangements. In the past it was thought the extinct Amphicyonidae were stem-bears based on morphological analysis of the ear region, though the most recent publications on early amphicyonids suggests they were basal caniforms. The amphicynodontids are sometimes classified as either a subfamily of bears, a paraphyletic assemblage of early bears, or even stem-pinnipeds. The subparictids were previously classified as amphicynodontine/ids. The hemicyonines have been occasionally reclassified as a separate family.
Enhydrocyon is an extinct genus of bone crushing canid which inhabited North America during the Oligocene and Early Miocene, 30.8—20.4 Ma, existing for approximately 11 million years.
Pristinictis is an extinct genus of placental mammals from extinct subfamily Didymictinae within extinct family Viverravidae, that lived in North America during middle Paleocene.
Stenoplesictidae is the name of a polyphyletic family of extinct civet-like feliforms.
Ysengrinia is an extinct genus of carnivoran in the family Amphicyonidae (beardogs), which lived in Europe, Asia, and North America during the Early Miocene. It was also reported from Egypt and Namibia, but this material has been reassigned to other genera of beardogs.
Arctoidea is a clade of mostly carnivorous mammals which include the extinct Hemicyonidae (dog-bears), and the extant Musteloidea, Pinnipedia, and Ursidae (bears), found in all continents from the Eocene, 46 million years ago, to the present. The oldest group of the clade is the bears, as their CMAH gene is still intact. The gene became non-functional in the common ancestor of the Mustelida. Arctoids are caniforms, along with dogs (canids) and extinct bear dogs (Amphicyonidae). The earliest caniforms were superficially similar to martens, which are tree-dwelling mustelids. Together with feliforms, caniforms compose the order Carnivora; sometimes Arctoidea can be considered a separate suborder from Caniformia and a sister taxon to Feliformia.
Phlaocyon annectens is an extinct species of the genus Phlaocyon, belonging to the subfamily Borophaginae and tribe Phlaocyonini, a canid endemic to central and western North America from the Late Oligocene to Early Miocene living 24.6—20.8 mya and existed for approximately 4.2 million years.
Phlaocyon latidens is an extinct species of the genus Phlaocyon, belonging to the subfamily Borophaginae and tribe Phlaocyonini, a canid which inhabited northwestern North America from the Late Oligocene to Miocene living 33.3–20.6 mya and existed for approximately 12.7 million years.
Hyaenodonta is an extinct order of hypercarnivorous placental mammals of clade Pan-Carnivora from mirorder Ferae. Hyaenodonts were important mammalian predators that arose during the early Paleocene in Europe and persisted well into the late Miocene.
Amphictis was an extinct genus of ailurid that existed from the Late Oligocene to the Middle Miocene with fossils found in Eurasia and North America with a total of nine described species. The interrelationships of the different species as well as their relationship to the other ailurids is not fully understood. Usually Amphictis is classified in the basal monotypic subfamily Amphictinae, but there is not certain as the genus could potentially be a paraphyletic with the Oligocene species A. borbonica being a potential sister taxon to the ancestor of the subfamily Ailurinae, while a Middle Miocene clade consisting of an anagenesis line from A. prolongata–to–A. wintershofensis–to–A. cuspida being closer to the ancestry of the now extinct Simocyoninae. This is due to the nature of their plesiomorphic nature of their anatomy.
Media related to Palaeogale at Wikimedia Commons