Protypotherium
Protypotherium | |
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Fossil of P. australe. Exhibit in the National Museum of Nature and Science, Tokyo, Japan | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Class: | Mammalia |
Order: | †Notoungulata |
Family: | †Interatheriidae |
Subfamily: | †Interatheriinae |
Genus: | †Protypotherium Ameghino 1882 |
Type species | |
†Protypotherium antiquum Moreno 1882
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Species | |
Synonyms | |
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Protypotherium is an extinct genus of
The
Taxonomy
Protypotherium was a typical representative of the Interatheriidae, a group of typotherian notoungulates with rodent-like appearances, usually with slender forms. The genus has a wide stratigraphic and geographic distribution, around 29 million years. Fossils assigned to Protypotherium have been found in numerous localities in Argentina, Bolivia, Chile, and Uruguay.[1][2][3][4] The oldest occurrence of Protypotherium dates back to the Late Oligocene (Deseadan) Fray Bentos Formation of Uruguay.[5]
The genus Protypotherium was first described in 1882 by Florentino Ameghino, based on fossil remains found in the Ituzaingó Formation in Entre Ríos Province, Argentina, in soils dating from the Late Miocene. The type species is Protypotherium antiquum. Another well-known species is P. australe, also from the Santa Cruz Formation,[6] but several other species have been attributed to this genus, such as P. altum, P. attenuatum, P. claudum, P. colloncurensis, P. diastematum, P. distinctum, P. endiadys, P. minutum, P. praerutilum, and P. sinclairi,[7] all found in various localities in Argentina in Lower and Middle Miocene deposits. A species from Chile, P. concepcionensis was described in 2019.[8]
Protypotherium was a rather specialized member of the interatheriids, akin to the bizarre Miocochilius; these two forms, according to a 2017 study, formed a
The following cladogram of the Interatheriinae is based on Vera et al. 2017, showing the position of Protypotherium.[9]
Interatheriinae |
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Species
The following species of Protypotherium have been described:[10]
- P. altum Ameghino 1891
- P. antiquum Ameghino 1882
- P. attenuatum Ameghino 1887
- P. australe Moreno 1882
- P. claudum Ameghino 1889
- P. colloncurensis Vera et al. 2017[9]
- P. diastematum Ameghino 1891
- P. distinctum Cabrera & Kraglievich 1931
- P. endiadys Roth 1898
- P. minutum Cabrera & Kraglievich 1931
- P. praerutilum Ameghino 1887
- P. sinclairi Kramarz et al. 2015[7]
- P. concepcionensis Solórzano et al. 2019
Description
Protypotherium was slightly larger than a rabbit, measuring about 40 centimetres (1.3 ft) in length. The body and legs as well as the tail of this animal were relatively long, while its neck was short. It probably resembled a rodent, possessing slender limbs with four, digitigrade clawed feet.[11] Its rat-like skull contained a set of 44 unspecialized teeth.
From the shape of its claws, Protypotherium would have been adept at digging and likely took over the burrows of other animals.[12]
Skull and dentition
The skull of Protypotherium was about halfway up the cranial vault, was slightly descending in the anterior part; the posterior part, on the other hand, lowered abruptly, in contrast to similar forms such as
The
The upper incisors of Protypotherium are characterized by a three-layered schmelzmuster represented by outer radial enamel. The prism diameter is ~6 μm. The Hunter-Schreger bands are thin (20–50 μm thick) and oblique. The interprismatic matrix forms closed coats near the outer enamel service and interrow sheets near the enamel dentine junction, and is intermediate to modified in the Hunter-Schreger bands. Lower incisors of Protypotherium are characterized by a one-layered schmelzmuster with Hunter-Schreger bands. Prism diameter is ~6 μm. Hunter-Schreger Bands are generally oblique and steady, even if they present a low decussation on both sections and are less discernible on some transverse sections. The interprismatic matrix forms closed coats in the entire thickness, but it is also slightly anastomosing near the enamel dentine junction. The thickness of its dentition suggest that it was a grazer, eating mainly grass.[14]
Protypotherium has euhypsodont (well high-crowned) premolars and molars, and
Compared with the related Interatherium and Cochilius, Protypotherium had well-differentiated third and fourth premolars compared to molars, and numerous other dental features. In contrast to Miocochilius, moreover, Protypotherium possessed the canine-shaped lower first premolar and shorter lower third molar.[9]
Regarding the species Protypotherium sinclairi, it can be distinguished from other species of Protypotherium by its dentition, with all teeth having a thick cementum covering. The third and fourth premolar both have a shorter anteroposterior diameter of the talonid than the trigonid, while the first and second premolars are short and non-molariform. The teeth of this species are smaller than those of P. australe, but larger than those of P. praerutilum and P. attenuatum, all of which are Santacrucian in age. The posterior lower premolars show proportionally larger buccolingual diameter of the talonid than those in the Santacrucian species.[2]
Postcranial skeleton
The skeleton of Protypotherium is well known, especially regarding the species Protypotherium australe. Fifteen dorsal
The
The
Paleobiology
Protypotherium was mainly a herbivore, but it is possible that Protypotherium fed occasionally on carrion as well. The legs clearly show robust nail phalanges, thanks to which the animal could dig burrows or modify those abandoned by other animals.[12]
A 2021 study concerning numerous fossils of the teeth of various species of Protypotherium showed that there is a trend in the preservation of tooth pattern, increase in size and decrease in number of species over time. This could be correlated with a global trend of cooling temperatures, indicating a deterioration of paleoenvironmental conditions during the Miocene. There also appears to have been a latitude shift in the distributional range of these animals: from Lower Miocene Patagonia to northern areas of South America towards the end of the Miocene.[4]
Paleoenvironment
Fossils of Protypotherium have been found in various fossiliferous stratigraphic units in South America. Several specimens come from the
In the Chichinales Formation, which is known for its local mammal fauna, Protypotherium would have coexisted with
The Sarmiento Formation has provided a wide assemblage of mammals, consisting of pyroclastic deposits in an arid desert environment.[26] Among these mammals were the astrapotheres Astrapotherium and Parastrapotherium,[27] the fellow notoungulates Argyrohippus,[28] Cochilius, Colpodon,[29] Interatherium and Pachyrukhos,[3] the litopterns Cramauchenia,[30] Lambdaconus, Paramacrauchenia, Proheptaconus,[31] Prolicaphrium,[32] Pternoconius,[33][34][35] Tetramerorhinus[3] and Theosodon,[36] the xenarthrans Hapaloides, Holomegalonyx, Nematherium, Peltephilus, Proeutatus, Proschismotherium, Prozaedyus, Stegotherium, and Stenotatus,[37] the metatherians Acyon, Acrocyon, Arctodictis, Borhyaena, Cladosictis, Palaeothentes, and Sipalocyon,[38] the rodents Acarechimys[25] Acaremys,[39] Caviocricetus,[40] Eosteiromys, Eoviscaccia,[41] Hypsosteiromys, Neoreomys,[42] Paradelphomys,[40] Parasteiromys, Perimys, Prospaniomys, Prostichomys, Protacaremys, Protadelphomys, Sarremys and Soriamys,[43][44][45][46][47][48] and the primates Homunculus, Mazzonicebus and Tremacebus.[49][50][51] The late-surviving meridiolestidan Necrolestes was also present.[38]
Multiple species of Protypotherium lived during the Early Miocene in the Santa Cruz Formation of Argentina, which preserves mostly a coastal environment, but also forested and grassland regions.[52] The area had little rainfall, so forests developed around lakes and rivers, giving Santa Cruz a diverse environment. During the Miocene, the climate was similar to those of the coasts of Chile with semi-temperate forests and oceanic winds. Grasslands began spreading into Argentina during the Miocene, though much of inner Patagonia was still arid with small rainforests in between. Large, herbivorous, South American ungulates such as the astrapothere Astrapotherium, the toxodont notoungulates Adinotherium, Homalodotherium and Nesodon shared the niche of low browsers, along with the litopterns Adianthus,[31] Anisolophus, Diadiaphorus, Tetramerorhinus, Theosodon, and Thoatherium,[53][54][55][16][56][57] with the rabbit-like interatheres such as Interatherium and the hegetotheres Hegetotherium and Pachyrukhos being frugivorous.[58][59][60] Both mammalian and avian carnivores inhabited the area, the largest being the phorusrhacid Phorusrhacos. Marsupials also lived in the region, including the large carnivorous sparassodonts Borhyaena and the smaller sparassodonts Acyon, Cladosictis, and Sipalocyon. Xenarthrans in the Santa Cruz Formation were fairly common, such as the ground sloths Analcimorphus, Analcitherium, Eucholoeops,[61] Hapalops, Hyperleptus, Nematherium, Megalonychotherium, Planops, Prepotherium, Schismotherium, Trematherium, and Xyophorus,[62][63] and the armadillos Cochlops, Eucinepeltus, Proeutatus, Propalaehoplophorus, Prozaedyus, Stegotherium, and Stenotatus.[64][16] In addition, fossils of rodents, such as Acarechimys, Acaremys, Adelphomys, Eocardia, Neoreomys, Perimys, Pliolagostomus, Prolagostomus,[65] Schistomys, Scleromys, Spaniomys, and Stichomys are also known.[66] There were also primates found in the formation, such as Carlocebus and Homunculus.[67][68]
The Collón Curá Formation and the Colloncuran age of South America represent a time when more open environments with reduced plant covering predominated, similar to
The Collón Curá Formation of Argentina has provided a wide assemblage of mammals, including at least 24 taxa such as the
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External links
- Media related to Protypotherium at Wikimedia Commons