| Parachleuastochoerus Temporal range: | |
|---|---|
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Mammalia |
| Order: | Artiodactyla |
| Family: | Suidae |
| Genus: | † Parachleuastochoerus Golpe-Posse, 1972 |
| Species | |
| |
Parachleuastochoerus was an extinct genus of even-toed ungulates that existed during the Miocene in Europe. [1] [2] [3] It was a smaller descendant of the Conohyus genus, with narrower cheek teeth and reduced premolars. [4]
P. steinheimensis fed on roots, as indicated by 87Sr/86Sr, δ18OCO3, and δ13C values sourced from its dental enamel. [5]
Hemicyon, also known as the "dog-bear", is an extinct genus of hemicyonine bear, which probably originated in Eurasia but was found in Europe, Asia and North America during the Miocene epoch, existing for approximately 16 to 13 mya. Hemicyon is the best-known genus in the Hemicyoninae, a subfamily intermediate between bears and their Caniform ancestors but most often classified as bears. Hemicyonid bears should not be confused with Amphicyonids (bear-dogs), which are their own separate family of carnivores.
Stirtonia is an extinct genus of New World monkeys from the Middle Miocene. Its remains have been found at the Konzentrat-Lagerstätte of La Venta in the Honda Group of Colombia. Two species have been described, S. victoriae and the type species S. tatacoensis. Synonyms are Homunculus tatacoensis, described by Ruben Arthur Stirton in 1951 and Kondous laventicus by Setoguchi in 1985. The genus is classified in Alouattini as an ancestor to the modern howler monkeys.
The Laventan age is a period of geologic time within the Middle Miocene epoch of the Neogene, used more specifically within the SALMA classification in South America. It follows the Colloncuran and precedes the Mayoan age.
The Huayquerian age is a period of geologic time within the Late Miocene epoch of the Neogene, used more specifically within the SALMA classification. It follows the Chasicoan and precedes the Montehermosan age.
Chelonoidis is a genus of turtles in the tortoise family erected by Leopold Fitzinger in 1835. They are found in South America and the Galápagos Islands, and formerly had a wide distribution in the West Indies.
The Pisco Formation is a geologic formation located in Peru, on the southern coastal desert of Ica and Arequipa. The approximately 640 metres (2,100 ft) thick formation was deposited in the Pisco Basin, spanning an age from the Late Miocene up to the Early Pliocene, roughly from 9.6 to 4.5 Ma. The tuffaceous sandstones, diatomaceous siltstones, conglomerates and dolomites were deposited in a lagoonal to near-shore environment, in bays similar to other Pacific South American formations as the Bahía Inglesa and Coquimbo Formations of Chile.
Cainochoerinae was a subfamily of even-toed ungulates that existed during the Miocene and Pliocene in Asia and Africa.
Albanohyus was an extinct genus of even-toed ungulates which lived during the Miocene in Eurasia and possibly Africa.
Cainochoerus was an extinct genus of even-toed ungulates which lived during the Miocene and Pliocene in Africa. Fossils have been found in Kenya, Ethiopia and South Africa.
Hyotheriinae was a subfamily of even-toed ungulates that existed during the Miocene and Pliocene in Europe, Asia, and Africa.
Aureliachoerus was an extinct genus of suids that existed during the Miocene in Europe.
Nguruwe was an extinct genus of even-toed ungulates that existed during the Miocene in Africa. It was formerly considered a member of the subfamily Listriodontinae, but has since been placed in Hyotheriinae.
Xenohyus was an extinct genus of suids that existed during the Miocene in Europe.
Sivachoerus was an extinct genus of even-toed ungulates that existed during the Miocene in Europe.
Tetraconodon was an extinct genus of even-toed ungulates that existed during the middle and late Miocene in Asia.
Hippopotamodon is a genus of extinct suid even-toed ungulates that existed during the Miocene to the Pleistocene in Europe and Asia.
Korynochoerus is an extinct genus of even-toed ungulates that existed during the Miocene in Europe and Asia Minor.
Microstonyx was an extinct genus of suid that existed during the Miocene in Asia and Europe.
Miocallicebus is an extinct genus of New World monkeys from the Middle Miocene. Its remains have been found at the Konzentrat-Lagerstätte of La Venta in the Honda Group of Colombia. The type species is Miocallicebus villaviejai.
Boreostemma is an extinct genus of glyptodonts from northern South America. Fossils assigned to the genus were first described as belonging to Asterostemma from southern South America, but have been placed in the new genus Boreostemma by Carlini et al. in 2008. The type species is B. pliocena. Fossils of Boreostemma have been found in the Honda Group of Colombia, in Peru and Venezuela.
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