Amphicticeps Temporal range: Early Oligocene, | |
---|---|
![]() | |
Holotype skull of Amphicticeps shackelfordi | |
Scientific classification ![]() | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Mammalia |
Order: | Carnivora |
Family: | † Amphicynodontidae |
Genus: | † Amphicticeps Matthew & Granger, 1924 |
Type species | |
†Amphicticeps shackelfordi Matthew & Granger, 1924 | |
Other species | |
|
Amphicticeps is an extinct genus of small, weasel-like carnivoran mammal. It lived in Mongolia during the Oligocene. The genus was erected in 1924 for the species A. shackelfordi on the basis of a well-preserved skull. Historically, the systematic position of this genus has been problematic until more specimens were described decades later. [1]
The type specimen of Amphicticeps shackelfordi (AMNH 19010) is an almost complete skull. It was discovered during the 1922 field season of the Central Asiatic Expeditions around 2 miles southwest of the Loh campsite in Övörkhangai Province, Mongolia. This locality is part of the Oligocene-aged Hsanda Gol Formation. Though several other jaw elements were also collected, these were not figured or assigned to Amphicticeps in the original description as they could not be firmly associated with the type skull. [1] During the 1994 field season of the Mongolian Academy of Sciences and the American Museum of Natural History joint expeditions, a naturally associated set of lower and upper jaws of A. shackelfordi was found, and the previously known jaw elements can now be confidently assigned to this species. [2]
In addition to the type species, two more species of Amphicticeps were described by Wang et al. in 2005:
A. dorog is currently known exclusively from teeth and jaw elements found in the top of the Tatal Member of the Hsanda Gol Formation, Mongolia. The type specimen (MAE SG.9194) is a fragment of the right maxilla with premolars and molars, and several additional fragments of rami and maxillae are assigned to this species. The specific name is a Mongolian word for 'badger'. This species is believed to be an intermediate form between the less-derived A. shackelfordi and more derived A. makhchinus based on the size and characters of its teeth. [2]
The least-known of the three species, A. makhchinus is known only from the holotype specimen (MAE 93–213) consisting of a right maxillary fragment with preserved teeth. The specimen was collected from the Tatal Member of the Hsanda Gol Formation, Mongolia. The specific name is a Mongolian word meaning 'meat-eater' or 'carnivore', as tooth features indicate this species was the most hypercarnivorous species in the genus. Based on the premolar labial length, A. makhchinus is the largest known species of the Amphicticeps genus, being 32% larger than A. shackelfordi and 16% larger than A. dorog. [2]
Amphicticeps was a small-sized mammal, with the type skull of A. shackelfordi (the smallest species) measuring 8.7 cm from nasal tip to inion. The skull is strongly-built for a carnivoran of this size, with a broad and short rostrum, and moderately-sized canine teeth. The first upper molar has a postprotocrista, enlarged parastyle and no lingual notch on the entoconid crest. The second upper molar is lingually positioned and reduced, and the third upper molar is either very reduced entirely lost. The upper fourth premolar has a carnassial notch and the suprameatal fossa is shallow, these features being primitive compared to the condition seen mustelids. [2]
The classification of Amphicticeps has historically been problematic. In their initial description of the genus, Matthew and Granger (1924) suggested it to be a "highly progressive miacid" rather than placing it in any existing carnivoran family. [1] Later authors have assigned it to Arctoidea based on dental or cranial features. Schmidt-Kittler (1981) noted the basicranium to have features matching arctoids, and deemed it not to belong in Musteloidea due to its shallow suprameatal fossa and the form of its molars, thus regarding it to be a "basal arctoid" that emerged before the development of Musteloidea. [3] Hunt (1996) proposed that Amphicticeps may belong in the family Amphicynodontidae, a classification which was followed by Wang and Qiu (2003). [4] [5]
Wang et al. (2005) conducted a phylogenetic analysis finding Amphicticeps to be a basal ursoid, being the earliest-diverging member of the clade containing it, Amphicynodon , Ursidae and Phocoidea. The cladogram results of their phylogenetic analyses are displayed in the cladogram below: [2]
In their description of Eoarctos , Wang et al. (2023) conducted a phylogenetic analysis recovering Amphicticeps as the earliest-diverging pinniped. Their results are shown in the cladogram below: [6]
| ||||||||||||||||||||||||||||||||||||||||||||||
All known species of Amphicticeps hail from the Hsanda Gol Formation, which is dated to around 33.4 to 31 million years ago (early Oligocene). This formation is believed to have been deposited in an open, semiarid steppe environment with playa lakes and ephemeral rivers. [7] In this habitat, Amphicticeps lived alongside a wide variety of small mammals including various rodents, the leporid Desmatolagus , and the erinaceid Palaeoscaptor . [8] [9] Sympatric predators included several species of Hyaenodon , the stenoplesictids Shandgolictis and Asiavorator , the feliforms Nimravus and Palaeogale , the amphicynodontid Amphicynodon and the didymoconids Didymoconus and Ergilictis . [10] The largest animal living alongside Amphicticeps in this formation was Paraceratheriumtransouralicum, a giant hornless rhinocerotoid. [11]
Proailurus is an extinct felid genus that lived in Europe and Asia approximately 25-30.8 million years ago in the Late Oligocene and Miocene. Fossils have been found in Mongolia, Germany, and Spain.
Andrewsarchus is an extinct genus of ungulate that lived during the Middle Eocene in China. It contains two species, A. mongoliensis and A. crassum. It was formerly placed in the families Mesonychidae or Arctocyonidae, but is now the sole member of a distinct family, Andrewsarchidae. Only known from a largely complete skull as well as isolated teeth, it is notable for being estimated as the largest terrestrial, carnivorous mammal, but that status has been disputed.
Ailuridae is a family in the mammal order Carnivora. The family consists of the red panda and its extinct relatives.
Creodonta is a former order of extinct carnivorous placental mammals that lived from the early Paleocene to the late Miocene epochs in North America, Europe, Asia and Africa. Originally thought to be a single group of animals ancestral to the modern Carnivora, this order is now usually considered a polyphyletic assemblage of two different groups, the Oxyaenids and the Hyenodonts, not a natural group. Oxyaenids are first known from the Palaeocene of North America, while hyaenodonts hail from the Palaeocene of Africa.
Hyaenodon ("hyena-tooth") is an extinct genus of carnivorous placental mammals from extinct tribe Hyaenodontini within extinct subfamily Hyaenodontinae, that lived in Eurasia and North America from the middle Eocene, throughout the Oligocene, to the early Miocene.
Carnassials are paired upper and lower teeth modified in such a way as to allow enlarged and often self-sharpening edges to pass by each other in a shearing manner. This adaptation is found in carnivorans, where the carnassials are the modified fourth upper premolar and the first lower molar. These teeth are also referred to as sectorial teeth.
Tsaganomys altaicus is an extinct species of rodent from Asia, and the only species in the genus Tsaganomys.
The Tsaganomyidae are an extinct family of rodents from Asia. It contains three genera. Tsaganomyids are generally considered to be related to the Hystricognathi. Members of Tsaganomyidae were fossorial (digging) rodents that probably used their incisor teeth to dig like some living mole rats.
Parictis is an extinct arctoid belonging to the family Subparictidae.
Ursoidea is a superfamily of arctoid carnivoran mammals that includes the families Subparictidae, Amphicynodontidae, and Ursidae. The last family includes the extant lineages of bears, as well as the extinct Hemicyoninae and Ursavinae.
Gobicyon is an extinct genus of large-sized carnivoran mammals, belonging to the Amphicyonidae, that was discovered in China, Mongolia, and Serbia, and lived during the Middle Miocene epoch. Despite only being known from rather fragmentary remains, recent discoveries showcase that it was an aberrant member of the subfamily Haplocyoninae, with adaptions towards bone-crushing similar to those of a hyaena.
Asiavorator is an extinct genus of civet-like carnivoran belonging in the family Stenoplesictidae. It was endemic to Asia and lived during the Eocene and Oligocene epochs.
The Irdin Manha Formation is a geological formation from the Eocene located in Inner Mongolia, China, a few kilometres south of the Mongolian border.
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.
Maddenia is an extinct genus of astrapothere, meridiungulate herbivore mammals characterised by its large tusks and the development of proboscis, endemic of South America. This genus was discovered in an outcrop near to the Lake Colhué Huapi in the place La Cantera, in the Chubut Province, in Argentina, in sediments corresponding to the Sarmiento Formation, that dates of the Late Oligocene.
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.
Amphicynodontidae is a probable clade of extinct arctoids. While some researchers consider this group to be an extinct subfamily of bears, a variety of morphological evidence links amphicynodontines with pinnipeds, as the group were semi-aquatic otter-like mammals. In addition to the support of the pinniped–amphicynodontine clade, other morphological and some molecular analyses support bears being the closest living relatives to pinnipeds. According to McKenna and Bell (1997) Amphicynodontinae are classified as stem-pinnipeds in the superfamily Phocoidea. Fossils of these mammals have been found in Europe, North America and Asia. Amphicynodontines should not be confused with Amphicyonids (bear-dogs), a separate family of Carnivora which is a sister clade to arctoids within the caniforms, but which may be listed as a clade of extinct arctoids in older publications.
Eoarctos is an extinct genus of arctoid carnivorans, known from the latest Eocene to early Oligocene of North Dakota and Nebraska. It is known from several remains, the most notable of which is the almost perfectly preserved skeleton of a large male. It was comparable in build and size to a fisher or small raccoon, with an estimated body mass of 4.3 kg, and possessed a variety of features that indicate a mix of terrestrial and scansorial locomotion. Its most notable feature is its unique dentition, with its massive premolars and hypocarnivorous molars, as well as its robust mandible, indicating that it consumed hard-shelled prey, possibly making it the oldest molluscivorous carnivoran known.
Alagtsavbaatar is an extinct species of carnivorous cat-like carnivoran belonging to the infraorder Aeluroidea. It was endemic to Asia, with all known specimens being found in Mongolia, and lived during the late Eocene epoch. It is a monotypic genus, with the type and only known species being A. indigenus, and is named after the Alag Tsav locality where its remains were first discovered.
Didymoconus is an extinct genus of mammal that lived during the early Oligocene epoch. It was endemic to Asia, and its fossils have been found in Mongolia, China and Kazakhstan. It is the type genus of the Didymoconidae, a family of eutherian mammals with uncertain taxonomic affinities.
{{cite journal}}
: CS1 maint: numeric names: authors list (link)