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| Prosthennops | |
|---|---|
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Mammalia |
| Order: | Artiodactyla |
| Family: | Tayassuidae |
| Genus: | † Prosthennops Matthew and Gidley, 1904 |
Prosthennops is a genus of extinct peccaries that lived in North and Central America between the middle Miocene and lower Pliocene (around 15-5 million years ago). [1]
This animal was very similar to present-day peccaries, both in appearance and size. Prosthennops had a shoulder height of about 76 cm. Individuals in the northern part of its range were larger than those in southern Central America.
It possessed a robust skull, with a depressed and elongated snout (but to a lesser extent than other extinct peccaries such as Mylohyus). The orbits were set back on the skull, above the glenoid cavity. The malar/zygomatic bones were prominent like those of African warthogs, developing laterally in massive tubercles.The premaxillary bones were well-developed and bore only two pairs of incisors, of which the second pair was often vestigial.
The fangs were pointed downwards, rather than forwards as in modern boars. The highly developed canines had an elliptical cross-section. The molarisation of the premolars was already very advanced: the second and third premolars were short, with an almost circular outline. The molars were low crowned (brachydonts), covered with a thick layer of enamel and with very simple tubercles.
Fossil finds date to the North American land mammal ages Late Clarendonian and Hemphillian, falling within the Late Miocene. [2] Prosthennops is known from the United States, Mexico, Honduras and Costa Rica. In the Curré Formation in the Costa Rican province of Puntarenas, part of the right mandible, molars, parts of the canines and incisors, and a phalanx have been found to be 5.8 million years old. [3] Prosthennops is found in a 12-million-year-old stratum of the lagerstätten Ashfall Fossil Beds, predating the ash layer.
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Prosthennops co-occurred with other peccaries such as Platygonus and Protherohyus . It was an omnivore, feeding on plants, nuts, roots and small animals.
Prosthennops is a typical member of the taiassuids, widespread in North America during the Miocene. It appears to have been a relatively specialised form, perhaps along the same evolutionary line that later led to the appearance of elongated snouted peccary forms such as Mylohyus.
Ancient Greek σθένος (sthénos, “strength”) — referring to the skull.
The genus Prosthennops was established by Matthew and Gidley in 1904; the type species, Prosthennops serus, had previously been described by Edward Drinker Cope as Dicotyles serus. A number of species, including P. condoni, P. kernensis, P. niobrarensis, P. rex, P. xiphodonticus, P. ziegleri, and P. haroldcooki, have been ascribed to the genus Prosthennops in much of the western United States (but also in Alabama and Mexico). Some of these species, such as P. niobrarensis and P. xiphodonticus, are clearly more derived than the others and indeed resemble today's taiassuids; they are therefore not ascribable to the genus Prosthennops. Donald Prothero asserts that the genus has historically been a wastebasket taxon. [4]
Prosthennops contains the following species: [1]
The species P. haroldcooki has been at the centre of a curious case of misattribution: the teeth on which the species is based were described in 1922 by Henry Fairfield Osborn, who attributed them to an anthropoid primate, the first known in North America. It was then Edwin Colbert, in 1935, who recognised in these teeth a typical representative of the taiassuids, and thus re-attributed the fossils to the genus Prosthennops. [5]
A peccary is a pig-like ungulate of the family Tayassuidae. They are found throughout Central and South America, Trinidad in the Caribbean, and in the southwestern area of North America. They usually measure between 90 and 130 cm in length, and a full-grown adult usually weighs about 20 to 40 kg. They represent the closest relatives of the family Suidae, which contains pigs and relatives. Together Tayassuidae and Suidae are grouped in the suborder Suina within the order Artiodactyla.
Stenomylus is an extinct genus of miniature camelid native to North America that died out around 30 million years ago. Its name is derived from the Greek στενός and μύλος.
The collared peccary is a species of artiodactyl (even-toed) mammal in the family Tayassuidae found in North, Central, and South America. It is the only member of the genus Dicotyles. They are commonly referred to as javelina, saíno, or báquiro, although these terms are also used to describe other species in the family. The species is also known as the musk hog. In Trinidad, it is colloquially known as quenk.
Borophagus is an extinct genus of the subfamily Borophaginae, a group of canids endemic to North America from the Middle Miocene epoch through the Early Pleistocene epoch 12—1.8 Mya.
Epicyon is a large, extinct, canid genus of the subfamily Borophaginae, native to North America. Epicyon existed for about 15 million years from the Hemingfordian age of the Early Miocene, to the Hemphillian of the Late Miocene. Epicyon is the largest known canid of all time, with the type species reaching 2.4 m (7.9 ft) in length, 90 cm (35 in) in shoulder height and approximately 100–125 kg (220–276 lb) in body mass. The largest known humerus specimen belonged to an individual weighing up to 170 kg (370 lb).
Daeodon is an extinct genus of entelodont even-toed ungulates that inhabited North America about 23 to 20 million years ago during the latest Oligocene and earliest Miocene. The type species is Daeodon shoshonensis, described by a very questionable holotype by Cope. Some authors synonymize it with Dinohyus hollandi and several other species, but due to the lack of diagnostic material, this is questionable at best.
Platygonus is an extinct genus of herbivorous peccaries of the family Tayassuidae, endemic to North and South America from the Miocene through Pleistocene epochs, existing for about 10.289 million years. P. compressus stood 2.5 feet tall.
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.
Suinae is a subfamily of artiodactyl mammals that includes several of the extant members of Suidae and their closest relatives – the domestic pig and related species, such as babirusas. Several extinct species within the Suidae are classified in subfamilies other than Suinae. However, the classification of the extinct members of the Suoidea – the larger group that includes the Suidae, the peccary family (Tayassuidae), and related extinct species – is controversial, and different classifications vary in the number of subfamilies within Suidae and their contents. Some classifications, such as the one proposed by paleontologist Jan van der Made in 2010, even exclude from Suinae some extant taxa of Suidae, placing these excluded taxa in other subfamilies.
Brachyhyops is an extinct genus of entelodont artiodactyl mammal that lived during the Eocene Epoch of western North America and southeastern Asia. The first fossil remains of Brachyhyops are recorded from the late Eocene deposits of Beaver Divide in central Wyoming and discovered by paleontology crews from the Carnegie Museum of Natural History during the early 20th century. The type species, Brachyhyops wyomingensis, is based on a single skull and was named by E.H. Colbert in 1937, but was not officially described until 1938. During the latter half of the 20th century, additional specimens from North America have been recorded from Saskatchewan and as far south as Texas, indicating that Brachyhyops had a broad distribution and was well-dispersed throughout western North America.
Aphelops is an extinct genus of hornless rhinocerotids endemic to North America. It lived from the Middle Miocene to the early Pliocene, during which it was a common component of North American mammalian faunas along with Teleoceras.
The Polk County paleontological sites are assemblages of Early Miocene to Late Pleistocene vertebrates occurring in Polk County, Florida, United States.
Platygonus compressus, the flat-headed peccary, is an extinct mammal species from the Tayassuidae family that lived in North and South America during the Pleistocene. It was first described in 1848 by John L. Leconte.
Apeomyoides savagei is a fossil rodent from the Miocene of the United States, the only species in the genus Apeomyoides. It is known from fragmentary jaws and isolated teeth from a site in the early Barstovian, around 15–16 million years ago, of Nevada. Together with other species from scattered localities in the United States, Japan, and Europe, Apeomyoides is classified in the subfamily Apeomyinae of the extinct rodent family Eomyidae. Apeomyines are a rare but widespread group that may have been adapted to a relatively dry habitat.
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Surameryx is an extinct genus of herbivorous even-toed ungulates originally described as belonging to the extinct family Palaeomerycidae. A single species, S. acrensis, was described from the Late Miocene of the Madre de Dios Formation, South America. It was originally interpreted as one of the few northern mammals that entered South America before the Pliocene. However, both its identification as a member of the family Palaeomerycidae and claims about its Miocene age were subsequently challenged.
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