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This paleomammalogy list records new fossil mammal taxa that were described during the year 2010, as well as notes other significant paleomammalogy discoveries and events which occurred during that year.
Name | Status | Authors | Age | Unit | Location | Notes | Images |
---|---|---|---|---|---|---|---|
Valid |
| Early Cretaceous | Western Siberia | ||||
Valid |
| Pleistocene | A marsupial belonging to the family Dasyuridae, a species of Antechinus . | ||||
Valid |
| Pleistocene | A marsupial belonging to the family Dasyuridae, a species of Antechinus . | ||||
Valid |
| Early Oligocene | A member of Didelphimorphia belonging to the superfamily Peradectoidea and the family Caroloameghiniidae. The type species is C. cristata. | ||||
Valid |
| Early Oligocene | A member of Microbiotheria, a species of Clenia. | ||||
Valid |
| Early Oligocene | A member of Microbiotheria, a species of Eomicrobiotherium. | ||||
Valid |
| Early Oligocene | A member of Argyrolagoidea of uncertain phylogenetic placement. The type species is E. verticalis. | ||||
Valid |
| Oligo-Miocene | A bandicoot. | ||||
Valid |
| Aptian/Albian | |||||
Valid |
| Early Oligocene | A member of Bonapartheriiformes, a species of Hondonadia. | ||||
Valid |
| Early Oligocene | A member of Bonapartheriiformes, a species of Hondonadia. | ||||
Valid |
| Early Oligocene | A member of Bonapartheriiformes, a species of Hondonadia. | ||||
Valid |
| Bathonian | A tegotheriid docodont. The type species is H. yaomingi. | ||||
Valid |
| Lower Aptian | An amphidontid 'eutriconodont'. The type species is J. liaoningensis. | ||||
Valid |
| Aptian/Albian | An albionbaatarid multituberculate. | ||||
Valid |
| Early Oligocene | A member of Argyrolagoidea of uncertain phylogenetic placement, a species of Klohnia. | ||||
Valid |
| Plio-Pleistocene | A marsupial belonging to the subfamily Zygomaturinae; a new genus for "Euowenia" robusta De Vis (1891). | ||||
Valid |
| Late Eocene to early Oligocene | A member of Polydolopiformes. The type species is K. mayoi (Odreman Rivas, 1978); genus also includes K. abanicoi (Flynn and Wyss, 1999) and K. mckennai (Flynn and Wyss, 2004), as well as new species K. fissuratus and K. maximus. | ||||
Valid |
| Late Cretaceous | A metatherian, a species of Leptalestes. | ||||
Valid |
| Probably middle Miocene | Riversleigh World Heritage Area | A marsupial belonging to the family Phascolarctidae (a relative of the koala). | |||
Valid |
| Late Oligocene | A marsupial belonging to the family Phascolarctidae (a relative of the koala). | ||||
Valid |
| Oxfordian | An amphitheriid, a species of Nanolestes. | ||||
Valid |
| Upper Cretaceous | A neoplagiaulacid multituberculate. The type species is N. occultus. | ||||
Valid |
| Miocene | Pinturas Formation | A marsupial belonging to the group Microbiotheria. | |||
Valid |
| Late Cretaceous | A multituberculate, a species of Paracimexomys. | ||||
Valid |
| Late Cretaceous | A neoplagiaulacid multituberculate. The type species is P. nelsoni. | ||||
Valid |
| Late Cretaceous | A cimolomyid multituberculate. The type species is P. carpenteri. | ||||
Valid |
| Middle Jurassic (Callovian) | A basal docodont. A new genus for "Shuotherium" kermacki Sigogneau-Russell, 1988. | ||||
Valid |
| Collón Curá Formation | A member of the family Thylacosmilidae. The type species is P. goini. | ||||
Valid |
| Early Oligocene | A member of Polydolopimorphia belonging to the suborder Hatcheriformes and the family Glasbiidae. The type species is P. ambiguus. | ||||
Valid |
| Early Oligocene | A member of Palaeothentidae, a species of Pilchenia. | ||||
Valid |
| Early Oligocene | A member of Palaeothentidae, a species of Pilchenia. | ||||
Valid |
| Early Oligocene | A member of Argyrolagoidea of uncertain phylogenetic placement. The type species is P. aberrans. | ||||
Valid |
| Early Oligocene | A member of Bonapartheriiformes, a species of Rosendolops. | ||||
Valid |
| Bathonian | A simpsonodontid docodont. | ||||
Valid |
| Oxfordian | A eleutherodontid allotherian. | ||||
Name | Status | Authors | Age | Unit | Location | Notes | Images |
---|---|---|---|---|---|---|---|
Valid |
| Aptian | An early eutherian | ||||
Valid |
| A gundi. | |||||
Valid |
| Baringo Basin | A relative of the okapi. Its type species is A. leakeyi. | ||||
Valid |
| Eocene | An early member of Anthropoidea. | ||||
Valid |
| Early Miocene | A tragulid ruminant. | ||||
Valid |
| Probably Pleistocene | An oryzomyine rodent. The type species is A. donovani; genus also includes A. praeuniversitatis. | ||||
Valid |
| Early Oligocene | A ctenodactyloid rodent. The species is A. neimongolensis. | ||||
Valid |
| Early Eocene | |||||
Valid |
| Early Miocene | A eumyarionine cricetid. The species is A. sihongensis. | ||||
Valid |
| Early Eocene | A primate of uncertain phylogenetic placement, a species of Altanius. | ||||
Valid |
| A murid rodent belonging to the subfamily Gerbillinae. The type species is A. grandis. | |||||
Junior synonym? |
| Late Oligocene | A lagomorph, a species of Amphilagus. Considered to be a probable junior synonym of Amphilagus antiquus by Fostowicz-Frelik (2016). [27] | ||||
Valid |
| Early Eocene | A member of Apatemyidae. | ||||
Valid |
| Oligocene (Rupelian) | |||||
Valid |
| Eocene | Creechbarrow Limestone Formation | An early bat. | |||
Valid |
| Early Eocene | A member of Arctocyonidae. | ||||
Valid |
| Early Pleistocene | Dmanisi locality | A large-sized deer. | |||
Valid |
| A squirrel belonging to the tribe Xerini, a relative of the Barbary ground squirrel. | |||||
Valid |
| Late Tertiary to Early Quaternary | One of the youngest known australopithecines to date. | ||||
Valid |
| Early Oligocene | An armadillo. The type species is "Meteutatus" rigidus Ameghino (1902); genus also includes "Meteutatus" tinguiririquensis Carlini et al. (2009), as well as new species Barrancatatus maddeni. | ||||
Valid |
| Late Hemphillian (Late Miocene) | Species:
| ||||
Valid |
| Middle Eocene | A shrew-like mammal, a species of Batodonoides. | ||||
Valid |
| Early Oligocene | A member of Leptictida. The type species is B. longinares; genus also includes B. latidens. | ||||
Valid |
| Early Pleistocene | |||||
Valid |
| Late Miocene (Huayquerian) | A euphractine armadillo related to Eutatus , a species of Chasicotatus. | ||||
Valid |
| Late Miocene (Huayquerian) | A euphractine armadillo related to Eutatus , a species of Chasicotatus. | ||||
Valid |
| Early Pliocene | Langebaanweg locality | A golden mole, a species of Chrysochloris . | |||
Valid |
| Early Pliocene | Langebaanweg locality | A golden mole, a species of Chrysochloris . | |||
Valid |
| Miocene (Colhuehuapian) | A rodent belonging to the family Eocardiidae. | ||||
Valid |
| Miocene | A rodent. | ||||
Valid |
| Early Miocene | |||||
Valid |
| Late Pliocene | Uquía Formation | A tuco-tuco. | |||
Valid |
| Middle Pliocene | An alcelaphine bovid. Its type species is Damalborea elisabethae. | ||||
Valid |
| Miocene | An anourosoricini soricidae. The type species is D. vandermeuleni. | ||||
Valid |
| Middle Eocene | A basal carnivoramorphan. | ||||
Valid |
| Late Cretaceous (Maastrichtian) | Deccan Intertrappean Beds | ||||
Valid |
| Early Miocene | |||||
Valid |
| Early Miocene | |||||
Valid |
| Miocene | A member of Talpidae. | ||||
Valid |
| Miocene | A member of Talpidae. | ||||
Valid |
| Early Miocene | An aletomerycine palaeomerycid. The type species is D. simonsi. | ||||
Valid |
| Early Eocene | |||||
Valid |
| Eocene (Ypresian) | |||||
Valid |
| Eocene | |||||
Valid |
| early Late Eocene (early Priabonian) | A hyracoid. The type species is D. patnaiki. | ||||
Valid |
| Earliest Priabonian | The oldest known afrosoricid. | ||||
Valid |
| Early Pleistocene | A relative of the Ryukyu long-tailed giant rat. | ||||
Valid |
| Early Pliocene (Zanclean) | A small rorqual | ||||
Valid |
| Eocene (Irdinmanhan) | A rodent of uncertain phylogenetic placement. The type species is D. dolus. | ||||
Valid |
| Early Oligocene | An octodontoid rodent of uncertain phylogenetic placement. The type species is D. verai. | ||||
Valid |
| Middle Torrejonian | A primitive paromomyid plesiadapiform. | ||||
Valid |
| Early Eocene | A primitive myodont rodent. The species is E. combinatus. | ||||
Valid |
| Late Paleocene | A member of Mixodectidae. | ||||
Valid |
| A rodent related to the maned rat. The type species is F. heissigi. | |||||
Valid |
| Eocene | A rodent belonging to the family Remyidae. The type species is F. russelli. | ||||
Valid |
| Early Oligocene | A rodent belonging to the group Hystricognathi. | ||||
Valid |
| Late Oligocene | A cricetid rodent, a species of Geringia. | ||||
Valid |
| earliest Eocene | A miacid carnivoran. | ||||
Valid |
| Middle Miocene | A primitive cavioid rodent. | ||||
Valid |
| Late Paleocene | |||||
Valid |
| A gundi. The type species is H. deserta. | |||||
Valid |
| Oligocene | |||||
Valid |
| Pleistocene | Identification of H. gautengensis was based on partial skulls, several jaws, teeth and other bones found at various times at the Caves. It emerged over 2 million years ago and died out approximately 600,000 years ago, and is believed to have arisen earlier than Homo habilis. | ||||
Valid |
| Early Pliocene | A member of Leporidae belonging to the subfamily Archaeolaginae. | ||||
Valid |
| Early Miocene | An early catarrhine of uncertain affinity. The type species is I. alekileki. | ||||
Valid |
| earliest Late Miocene | A cetotheriid whale. The type species is J. shimizui. | ||||
Valid |
| earliest late Eocene | An anomaluroid rodent. | ||||
Valid |
| Early Miocene | An early catarrhine of uncertain affinity. The type species is K. akisimia. | ||||
Valid |
| Eocene | |||||
Valid |
| Early Miocene | A galago. | ||||
Valid |
| Miocene | A new name for Kotadasiren gracilis Das & Basu, 1994 (nomen nudum). The type species is Kutchisiren cylindrica. | ||||
Valid |
| Late Oligocene | A cricetid rodent, a species of Leidymys. | ||||
Valid |
| Late Miocene (Huayquerian) | A mylodontid. The type species is L. sprechmanni. | ||||
Valid |
| Miocene | A physeteroid whale. The type species is L. melvillei. | ||||
Valid |
| Late Miocene | |||||
Valid |
| Miocene (Colhuehuapian) | A rodent belonging to the family Eocardiidae. | ||||
Valid |
| Pliocene to Pleistocene | A relative of the African wild dog. | ||||
Valid |
| An octodontoid rodent. The type species is M. gregoriana. | |||||
Valid |
| Middle Eocene | A notharctid adapiform. The type species is Mazateronodon endemicus. | ||||
Valid |
| Early Miocene | A New World monkey related to Homunculus patagonicus and members of the genus Soriacebus . The type species is M. almendrae. | ||||
Valid |
| Late Eocene | An armadillo. The type species is M. ingens. | ||||
Valid |
| Late Oligocene | |||||
Valid |
| Late Hemphillian (Late Miocene) | Species: Metaliomys sevierensis | ||||
Valid |
| Early Eocene | Originally described as a species of Miacis , [23] subsequently transferred to the genus Gracilocyon. [86] | ||||
Valid |
| Middle Eocene | |||||
Valid |
| A free-tailed bat, a species of Mormopterus . | |||||
Valid |
| Early Pliocene | A member of Caprinae. | ||||
Valid |
| Early Eocene | A member of Erinaceomorpha belonging to the family Amphilemuridae. | ||||
Valid |
| Eocene (Priabonian) | Birket Qarun Formation | A primate of uncertain phylogenetic placement. The type species is N. aenigmaticus. | |||
Valid |
| Late Pleistocene to Holocene | A shrew, a species of Notiosorex . | ||||
Valid |
| A shrew, a species of Notiosorex. | |||||
Valid |
| Middle Pliocene | A species of Nyctereutes (a relative of the raccoon dog). | ||||
Valid |
| Pleistocene | A pika. | ||||
Valid |
| Early Miocene | A dipodid rodent. | ||||
Valid |
| Late Oligocene | An eomyid rodent, a species of Orelladjidaumo. | ||||
Valid |
| Late Oligocene | A cricetid rodent, a species of Paciculus. | ||||
Valid |
| Lower Willwood Formation | |||||
Valid |
| Oligocene | A notohippid notoungulate. The type species is P. canterensis; genus also includes P. dukei. | ||||
Valid |
| Eocene | A rodent belonging to the family Phiomyidae. | ||||
Valid |
| Late Miocene (Tortonian) | Sediments of the Stirone River | A parabalaenopterine balaenopterid. The type species is P. quarantellii. | |||
Valid |
| early or middle Pleistocene | A prehistoric pilot whale (Family Delphinidae). The type species is P. hoekmani | ||||
Valid |
| Early Eocene | |||||
Valid |
| Paleocene | A cyriacotheriid pantodont. Species:
| ||||
Valid |
| Early Miocene | |||||
Valid |
| Pliocene | A member of Lagomorpha, a species of Prolagus . | ||||
Valid |
| Eocene | A rodent belonging to the family Phiomyidae. | ||||
Valid |
| Eocene | |||||
Valid |
| Rupelian | The youngest known afrosoricid. | ||||
Valid |
| Miocene | A rhinoceros, a new genus for "Dicerorhinus" leakeyi (Hooijer, 1966). | ||||
Valid |
| Oligocene | A catarrhine primate. The species was named S. hijazensis. | ||||
Sadypus minutus [34] | Valid |
| Early Oligocene | ||||
Valid |
| A murid rodent belonging to the subfamily Murinae. The type species is S. misrensis. | |||||
Valid |
| Oligocene | |||||
Valid |
| Late Eocene | An anomalure. The type species is S. minutus. | ||||
Valid |
| Middle Miocene | |||||
Valid |
| A hamster. | |||||
Valid |
| Early Miocene | A dipodid rodent. | ||||
Valid |
| Early Eocene | A rodent belonging to the family Paramyidae and the subfamily Microparamyinae. | ||||
Valid |
| ||||||
Valid |
| Eocene to early Oligocene | A rodent belonging to the family Phiomyidae. The type species is "Phiomys" lavocati Wood (1968); genus also includes new species T. libycus. | ||||
Valid |
| Eocene | A member of Oligopithecidae. The type species is T. parvus. | ||||
Valid |
| Early Pleistocene | A tapir. | ||||
Valid |
| Early Miocene | |||||
Valid |
| Early Oligocene | An octodontoid rodent of uncertain phylogenetic placement. The type species is V. mazzonii; genus might also include Vallehermosomys? merlinae. | ||||
Valid |
| Early Eocene | A member of Viverravidae. | ||||
Valid |
| Early Eocene | A rodent related to the gundis. The type species is Y. zhoui. | ||||
Protypotherium is an extinct genus of notoungulate mammals native to South America during the Oligocene and Miocene epochs. A number of closely related animals date back further, to the Eocene. Fossils of Protypotherium have been found in the Deseadan Fray Bentos Formation of Uruguay, Muyu Huasi and Nazareno Formations of Bolivia, Cura-Mallín and Río Frías Formations of Chile, and Santa Cruz, Salicas, Ituzaingó, Aisol, Cerro Azul, Cerro Bandera, Cerro Boleadoras, Chichinales, Sarmiento and Collón Curá Formations of Argentina.
Cramauchenia is an extinct genus of litoptern South American ungulate. Cramauchenia was named by Florentino Ameghino. The name has no literal translation. Instead, it is an anagram of the name of a related genus Macrauchenia. This genus was initially discovered in the Sarmiento Formation in the Chubut Province, in Argentina, and later it was found in the Chichinales Formation in the Río Negro Province and the Cerro Bandera Formation in Neuquén, also in Argentina, in sediments assigned to the SALMA Colhuehuapian, as well as the Agua de la Piedra Formation in Mendoza, in sediments dated to the Deseadan. In 1981 Soria made C. insolita a junior synonym of C. normalis. A specimen of C. normalis was described in 2010 from Cabeza Blanca in the Sarmiento Formation, in sediments assigned to the Deseadan SALMA.
Eomyidae is a family of extinct rodents from North America and Eurasia related to modern day pocket gophers and kangaroo rats. They are known from the Middle Eocene to the Late Miocene in North America and from the Late Eocene to the Pleistocene in Eurasia. Eomyids were generally small, but occasionally large, and tended to be squirrel-like in form and habits. The family includes the earliest known gliding rodent, Eomys quercyi.
The Divisaderan age is a South American land mammal age, covering a period of geologic time within the Middle and Late Eocene epochs of the Paleogene. It follows the Mustersan age and is followed by the Tinguirirican age.
The Tinguirirican age is a period of geologic time within the Late Eocene and Early Oligocene epochs of the Paleogene, used more specifically within the SALMA classification in South America. It follows the Divisaderan and precedes the Deseadan age.
The Deseadan age is a period of geologic time within the Oligocene epoch of the Paleogene to the Early Miocene epoch of the Neogene, used more specifically within the SALMA classification of South America. It follows the Tinguirirican and precedes the Colhuehuapian age.
Astrapotheriidae is an extinct family of herbivorous South American land mammals that lived from the Late Eocene to the Middle Miocene 37.71 to 15.98 million years ago. The most derived of the astrapotherians, they were also the largest and most specialized mammals in the Tertiary of South America. There are two sister taxa: Eoastrapostylopidae and Trigonostylopidae.
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.
This paleomammalogy list records new fossil mammal taxa that were described during the year 2011, as well as notes other significant paleomammalogy discoveries and events which occurred during that year.
Groeberiidae is a family of strange non-placental mammals from the Eocene and Oligocene epochs of Patagonia, Argentina and Chile, South America. Originally classified as paucituberculate marsupials, they were suggested to be late representatives of the allothere clade Gondwanatheria. However, the relationship of the type genus, Groeberia, to Gondwanatheria has been firmly rejected by other scholars.
The Agua de la Piedra Formation is a Late Oligocene geologic formation of the Malargüe Group that crops out in the southernmost Precordillera and northernmost Neuquén Basin in southern Mendoza Province, Argentina.
Ernestokokenia is an extinct genus of mammal, belonging to the Didolodontidae. It lived during the Early Eocene and the Middle Eocene, and its fossils were discovered in South America.
Notopithecus is an extinct genus of Notoungulate, belonging to the suborder Typotheria. It lived from the Middle to the Late Eocene and its fossilized remains were discovered in South America.
The Sarmiento Formation, in older literature described as the Casamayor Formation, is a geological formation in Chubut Province, Argentina, in central Patagonia, which spans around 30 million years from the mid-Eocene to the early Miocene. It predominantly consists of pyroclastic deposits, which were deposited in a semi-arid environment. It is divided up into a number of members. The diverse fauna of the Sarmiento Formation, including a variety of birds, crocodilians, turtles and snakes, also includes many mammals such as South American native ungulates as well as armadillos, and caviomorph rodents.
The Chichinales Formation is a geological formation in Río Negro Province, Argentina which dates from the Late Oligocene to the Early Miocene, around 23 to 17.5 million years ago. It predominantly consists of pyroclastic deposits, which were deposited in a semi-arid environment. It is divided up into a number of members. The diverse fauna of the Chichinales Formation, including a variety of turtles and birds, also includes many mammals such as South American native ungulates as well as armadillos, and caviomorph rodents.
Australoprocta is an extinct genus of dasyproctid rodent that lived during the Early Miocene of what is now Argentina. Fossils of this genus have been found in the Chichinales and Sarmiento Formations of Argentina.
Perimys is an extinct genus of neoepiblemid rodent that lived from the Early to Late Miocene in what is now South America. Fossils have been found in the Cerro Bandera, Cerro Boleadoras, Ituzaingó, Santa Cruz, and Sarmiento Formations of Argentina, and the Galera, Santa Cruz and Río Frías Formations of Chile.
Proargyrohyrax is an extinct genus of interatheriine notoungulates that lived from the Early to Middle Oligocene in what is now Argentina. Fossils of this genus have been found in the Sarmiento Formation of Argentina.
Eoviscaccia is an extinct genus of chinchillid rodent that lived during the Early Oligocene (Tinguirirican) to the Early Miocene (Colhuehuapian) in what is now South America. Fossils of this genus have been found in the Cerro Bandera, Chichinales, Fray Bentos, and Sarmiento Formations of Argentina, the Salla Formation of Bolivia, and the Abanico Formation of Chile.