The family Aplodontiidae also known as Aplodontidae, Haplodontiidae or Haploodontini is traditionally classified as the sole extant family of the suborder Protrogomorpha. It may be the sister family of the Sciuridae. There are fossils from the Oligocene until Miocene in Asia, from Oligocene in Europe and from the Oligocene until the present in North America, where there is the only living species: the mountain beaver.
Hystricomorpha is a term referring to families and orders of rodents which has had many definitions throughout its history. In the broadest sense, it refers to any rodent with a hystricomorphous zygomasseteric system. This includes the Hystricognathi, Ctenodactylidae, Anomaluridae, and Pedetidae. Molecular and morphological results suggest the inclusion of the Anomaluridae and Pedetidae in Hystricomorpha may be suspect. Based on Carleton & Musser 2005, these two families are discussed here as representing a distinct suborder Anomaluromorpha.
Pseudoltinomys is a prehistoric rodent that lived approximately 30 million years ago, during the Oligocene epoch. It outwardly resembles a gerbil, but may have been related to kangaroo rats or may represent an early offshoot of rodents with no modern relatives.
Eomys is an extinct genus of eomyid rodent from the late Oligocene of France, Germany, Spain, and possibly Turkey. The species Eomys quercyi is the earliest known gliding rodent.
Quercygale is an extinct genus of placental mammals from the clade Carnivoraformes, that lived in Europe during the early to late Eocene.
Corbarimys cezannei, formerly Pseudoparamys cezannei, is a species of extinct rodent in family Ischyromyidae. It is named after French Post-Impressionist painter Paul Cézanne.
Duerotherium is an extinct genus of Palaeogene artiodactyls known only from the Iberian Peninsula during the Middle Eocene, which contains one species D. sudrei. It, like other members of the Anoplotheriidae, was endemic to Western Europe. The anoplotheriine was described from a left fragment of a maxilla from the Mazaterón Formation of the Duero Basin in 2009. Its dentition is mostly typical of the Anoplotheriinae but differs by an elongated plus triangular 3rd upper premolar and very specific traits of the molars. It is thought to have been part of an endemic faunal assemblage that evolved within the Iberian Peninsula by the Middle Eocene, where climates were subtropical.
Palaeochiropterygidae is a family of extinct bats. It was originally erected by the Swiss naturalist Pierre Revilliod in 1917 after discoveries of Palaeochiropteryx fossils from the Messel Pit of Germany. Palaeochiropterygidae was merged into Archaeonycteridae by Kurten and Anderson in 1980, but modern authorities specializing in bat fossils maintain the distinction between the two. It was classified to the unranked clade Microchiropteramorpha by Smith et al. in 2007.
This paleomammalogy list records new fossil mammal taxa that were described during the year 2012, as well as notes other significant paleomammalogy discoveries and events which occurred during that year.
This paleomammalogy list records new fossil mammal taxa that were described during the year 2013, as well as notes other significant paleomammalogy discoveries and events which occurred during that year.
Cainotheriidae is an extinct family of artiodactyls known from the Late Eocene to Middle Miocene of Europe. They are mostly found preserved in karstic deposits.
The Quercy Phosphorites Formation is a geologic formation and lagerstätte in Occitanie, southern France. It preserves fossils dated to the Paleogene period, or MP16 to MP28 zones of the European land mammal age classification, ranging from approximately 38 to 25 Ma.
Necromantis is an extinct genus of bat that lived during the Eocene. Its fossils are found in the Quercy Phosphorites Formation of France and the Djebel Chambi in Tunisia. Specimens of Necromantis are notable for their large size and specialization towards a predatory lifestyle.
Dichodon is an extinct genus of Palaeogene artiodactyls belonging to the family Xiphodontidae. It was endemic to Western Europe and lived from the middle Eocene up to the earliest Oligocene. The genus was first erected by the British naturalist Richard Owen in 1848 based on dental remains from the fossil beds in Hordle, England. He noticed similar dentitions to contemporary artiodactyls like those of the Anoplotheriidae and Dichobunidae and references the name of the genus Dichobune. Eventually, it was found to be more closely related to Xiphodon and now includes 11 species, although one of them may be synonymous.
Robiatherium is an extinct genus of Palaeogene artiodactyls containing one species R. cournovense. The genus name derives from the locality of Robiac in France where some of its fossil were described plus the Greek θήρ/therium meaning "beast" or "wild animal". It was known only from the middle Eocene and, like other anoplotheriids, was endemic to Western Europe. The genus was erected by Jean Sudre in 1988 for a species originally attributed to the xiphodont genus Paraxiphodon in 1978. Robiatherium had dentitions typical of the subfamily Anoplotheriinae, differing from other genera by specific differences in the molars. It is one of the earliest-appearing anoplotheriine species in the fossil record as well as the earliest to have appeared in Central Europe.
Haplomeryx is an extinct genus of Palaeogene artiodactyls belonging to the family Xiphodontidae. It was endemic to Western Europe and lived from the middle Eocene up to the earliest Oligocene. Haplomeryx was first established as a genus by the German naturalist Max Schlosser in 1886 based on a molar tooth set from Quercy Phosphorites deposits. Three additional species were erected and classified to the xiphodontid genus while one other species, first recognized in 1822, was tentatively classified to it and remains unresolved in affinity.
Reinomys is an extinct genus of Palaeogene rodents of unclear affinities belonging to the infraorder Theridomorpha. The genus and its only known species Reinomys rhomboides were both named by the French palaeontologists Monique Vianey-Liaud and Laurent Marivaux in 2021 based on some lower molars from the French locality of Avenay that dates back to the later early Eocene. It is diagnosed as being similar in size to another basal rodent Sparnacomys but differing based on specific traits of the tooth surfaces and cusps.
Auroremys is an extinct genus of Palaeogene rodents belonging to the theridomorph family Pseudosciuridae. The type and only species Auroremys subita was first named by Bernard Comte et al. in 2012 as belonging to the ischyromyid genus Ailuravus before it was eventually reclassified to its own genus by French palaeontologists Monique Vianey-Liaud and Laurent Marivaux in 2021.
Idicia is an extinct genus of Palaeogene rodents belonging to the family Theridomyidae. The genus and its sole species Idicia vidalenci were both named by Monique Vianey-Liaud et al. in 2024 based on some holotype dentition from the French locality of Lavergne, dating to the middle Eocene. It was named in honor of Dominique Vidalenc, who discovered the holotype material. It is diagnosed as being a medium-sized and brachyodont (low-crowned) theridomyid with various specific morphologies of its cuspids. A wide range of other faunas were recovered form Lavergne along with Idicia such as the herpetotheriid Peratherium, nyctithere Saturninia, omomyid Necrolemur, carnivoraforme Quercygale, tapirulid Tapirulus, and the palaeothere Palaeotherium.
Theridomorpha is an extinct clade of Palaeogene rodents that were endemic to western Europe and lived from the early Eocene to the late Oligocene. It is proposed to belong to the suborder Ischyromyiformes, of which the Gliridae is the sole surviving family, and contains the families Euromyidae, Masillamyidae, Theridomyidae, and Pseudosciuridae. Theridomorphs had wide variations in both their tooth crown heights and their surface patterns, namely bunodont, lophodont, or selenodont dentitions. Whereas Eocene species had brachyodont, or low-crowned, to slightly hypsodont (higher-crowned) dentitions, Oligocene species tended to have more semi-hypsodont dentitions. Theridomorphs ranged in size from small field mice at 50 g (1.8 oz) to muskrats at 1 kg (2.2 lb).
