Prosotherium

Last updated

Prosotherium
Temporal range: Late Oligocene (Deseadan)
~29–21  Ma
Propachyrucos ameghinorum.jpg
Skeleton of Prosotherium
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Notoungulata
Family: Hegetotheriidae
Subfamily: Pachyrukhinae
Genus: Prosotherium
Ameghino, 1897
Type species
Prosotherium garzoni
Ameghino, 1897
Species
  • P. garzoniAmeghino, 1897
Synonyms
List
  • Prosotherium triangulidensAmeghino, 1897
  • Prosotherium robustumAmeghino, 1897
  • Prosotherium quartumAmeghino, 1901
  • Propachyrucos ameghinorumSimpson, 1945
  • Propachyrucos simpsoniChaffee, 1952

Prosotherium is an extinct genus of hegetotheriid notoungulate. It lived during the Late Oligocene (between ~29-24 Ma), and its fossilized remains were found in South America. [1]

Contents

Description

This animal was similar to rabbits, in aspect and in size. Its hind legs were particularly long.

Crania

Its crania was light and thin, notably in the posterior part. The tympanic part of the temporal bone was particularly developed, even more than its relative Pachyrukhos , and it is probable that its auricle was quite large, similar to the ears of a hare. The maxilla and the mandible were high and deep ; the mandible had a subtle coronoid process. The teeth were characterized by incisors pointing inward, molars and premolars covered by a thin layer of dental cementum, generally on the outside part of the upper teeth and on the inside part of the lower teeth. [1]

Postcranial skeleton

The humerus was large and thin, like the ulna and radius. Metacarpals and phalanges indicates that the hand was small and delicate. The pelvis was elongated, slender and lightly build, while the femur was equipped of a small head separated from the main bone. The femur was even longer than in Pachyrukhos, and had a small trochanter curiously pushed back in the posterior part. Contrary to Pachyrukhos, the tibia and fibula were completely separated. The talus bone was likewise characteristic, with the trochlear nerve extant covering entirely the dorsal part of the bone, and a low and flat condylar crest. The calcaneus was relatively small, with an articulated facet for the cuboid bone slightly concave and occupying the entire distal part of the bone. The metatarsal was robust and shorter than in Pachyrukhos. The distal phalanx was high and narrow, flattening and widening towards the terminal part. [1]

Classification

The genus Prosotherium was first described in 1897 by Florentino Ameghino, over fossilized remains discovered in Patagonia in Late Oligocene terrains. The type species is Prosotherium garzoni, and Ameghino described in this same paper P. triangulidens, which was a bit larger than the type species, as well as P. robustum. [2] P. quartum, a fourth species, was described in 1901 by Ameghino. [3] Only the first name is still considered valid. [1]

Prosotherium was a member of the Hegetotheriidae, a clade of light, rodent-like or hare-like Notoungulata. Prosotherium was a member of the Pachyrukhinae subfamily comprising several hare-like genera. It is possible that Prosotherium was an ancestral form or a close relative of Paedotherium , more specialized.

Paleobiology

The Late Oligocene terrains of Patagonia present at least three genera of hegetotheres with hypsodont teeth : Prosotherium, Propachyrucos and Medistylus , the latter of which is sometimes considered an interatheriid. This implies a strict repartition of ecological niches among the Oligocene hegetotheres, but also reflects the remarkable evolutionary radiation of rodent-like ungulates during the Cenozoic of South America, and suggest environmental differences between the fauna of Patagonia and the fauna of Uruguay and Bolivia, where those animals were absent. [4]

Related Research Articles

<i>Pyrotherium</i> Extinct genus of mammals

Pyrotherium is an extinct genus of South American ungulate, of the order Pyrotheria, that lived in what is now Argentina and Bolivia, during the Late Oligocene. It was named Pyrotherium because the first specimens were excavated from an ancient volcanic ash deposit. Fossils of the genus have been found in the Deseado and Sarmiento Formations of Argentina and the Salla Formation of Bolivia.

<i>Paedotherium</i> Extinct genus of notoungulates

Paedotherium is an extinct, potentially paraphyletic genus of Notoungulate, belonging to the family Hegetotheriidae, composed of small-sized, rodent or lagomorph-like South American ungulates. Four species are unambiguously recognized, from the Late Miocene to the Pleistocene of Argentina, and from the late Miocene of Bolivia and Chile.

<i>Tremacyllus</i> Extinct genus of notoungulates

Tremacyllus is an extinct genus of hegetotheriids. It lived from the Late Miocene to the Late Pleistocene and its fossilized remains were discovered in South America.

Propyrotherium is an extinct genus of mammals, belonging to the order Pyrotheria. It lived during the Late Eocene, in what is now South America.

Proadiantus(Ameghino, 1897) is an extinct genus of adianthid litoptern. It lived during the Late Oligocene, in what is today South America. It consists of only 1 species, Proadiantus excavatus.

Medistylus is an extinct genus of pachyrukhine hegetotheriid. It lived in Argentina during the Late Oligocene. Medistylus is known from its upper teeth and isolated skulls, however, its lower dentition is currently unknown. Its fossilized remains were found at the Cabeza Blanca and Las Cascadas localities of the Sarmiento Formation in Chubut Province of Argentina.

Eohyrax is an extinct genus of Notoungulate, belonging to the suborder Typotheria. It lived during the Middle Eocene, and its remains were discovered in South America.

Propachyrucos is an extinct genus of hegetotheriid notoungulate. It lived from the Late Oligocene to the Early Miocene, in what is today South America.

<i>Isotemnus</i> Extinct genus of notoungulates

Isotemnus is an extinct genus of notoungulate belonging to the family Isotemnidae. It lived from the Late Paleocene to the Middle Eocene of what is now Argentina.

Pleurostylodon is an extinct genus of notoungulate belonging to the family Isotemnidae. It lived during the Middle Eocene, in what is now Argentina.

Eurygenium is an extinct genus of notoungulate belonging to the family Notohippidae. It lived during the Late Oligocene in what is today South America.

<i>Morphippus</i> Extinct genus of notoungulates

Morphippus is an extinct genus of notohippid notoungulate that lived during the Middle to Late Oligocene in what is now South America.

Acoelodus is an extinct genus of placental mammal, belonging to the order Notoungulata. The genus was first described by Florentino Ameghino in 1897. Its fossilized remains were discovered in Casamayoran terrains from Argentine Patagonia.

Ancylocoelus is an extinct genus of mammal, belonging to the order Notoungulata. It lived during the Late Oligocene, in what is today Argentina, in South America.

Archaeopithecus is an extinct genus of Notoungulate, belonging to the suborder Typotheria. It lived during the Middle Eocene, in what is today Argentina.

Oldfieldthomasia is an extinct genus of Notoungulate, probably related to the suborder Typotheria. It lived during the Middle Eocene, in what is today South America.

Argyrohyrax is an extinct genus of interatheriid notoungulate that lived during the Late Oligocene, of what is now Argentina and Bolivia.

<i>Notopithecus</i> Extinct genus of notoungulates

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.

Hegetotheriopsis is an extinct genus of hegetotheriid notoungulate. It lived from the Late Oligocene to the Early Miocene, and its fossilized remains are found in Argentina.

<span class="mw-page-title-main">Sarmiento Formation</span> Geologic formation in Chubut Province, Argentina

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.

References

  1. 1 2 3 4 F. D. Seoane, S. R. Juñent, and E. Cerdeño. 2017. Phylogeny and paleobiogeography of Hegetotheriidae (Mammalia, Notoungulata). Journal of Vertebrate Paleontology 37(1):e1278547:1-13
  2. F. Ameghino. 1897. Mammiféres crétacés de l’Argentine (Deuxième contribution à la connaissance de la fauna mammalogique de couches à Pyrotherium) [Cretaceous mammals of Argentina (second contribution to the knowledge of the mammalian fauna of the Pyrotherium Beds)]. Boletin Instituto Geografico Argentino 18(4–9):406-521
  3. F. Ameghino. 1901. Notices préliminaires sur des ongulés nouveaux des terrains crétacés de Patagonie [Preliminary notes on new ungulates from the Cretaceous terrains of Patagonia]. Boletin de la Academia Nacional de Ciencias de Córdoba 16:349-429
  4. Reguero, Marcelo A.; Dozo, María Teresa; Cerdeño, Esperanza (2007). "A poorly known rodentlike mammal (Pachyrukhinae, Hegetotheriidae, Notoungulata) from the Deseadan (Late Oligocene) of Argentina. Paleoecology, biogeography, and radiation of the rodentlike ungulates in South America". Journal of Paleontology. 81 (6): 1301–1307. Bibcode:2007JPal...81.1301R. doi:10.1666/05-100.1. ISSN   0022-3360. S2CID   55259241.