Prodeinotherium

''Prodeinotherium'' is an extinct representative of the family Deinotheriidae that lived in Africa, Europe, and Asia in the early and middle Miocene. ''Prodeinotherium'', meaning "before terrible beast", was first named in 1930, but soon after, the only species in it, ''P. hungaricum'', was reassigned to ''Deinotherium''. During the 1970s, however, the two genera were once again separated, with ''Prodeinotherium'' diagnosed to include ''Deinotherium bavaricum'' (=''P. hungaricum''), ''Deinotherium hobleyi'', and ''Deinotherium pentapotamiae'', which were separated based on geographic location. The three species are from Europe, Africa, and Asia, respectively. However, because of usage of few characters to separate them, only one species, ''P. bavaricum'', or many more species, including ''P. cuvieri'', ''P. orlovii'', and ''P. sinense'' may be possible.

''Prodeinotherium'' is one of three genera of the Deinotheriidae, the others being ''Chilgatherium'' from Africa, and ''Deinotherium'' from Europe, Africa, and Asia. ''Chilgatherium'' preceded ''Prodeinotherium'', while ''Deinotherium'' succeeded it. ''P. hobleyi'' was the first species of ''Prodeinotherium'', and it migrated into Asia and Europe before evolving into ''P. pentapotamiae'' and then ''P. bavaricum''. ''Prodeinotherium'' lived for the Early Miocene and Middle Miocene before being replaced by ''Deinotherium''. The deinotheriids are an early branch of proboscideans, although more derived than ''Barytherium'' and ''Moeritherium''.

All deinotheres were large animals that evolved to be even larger, and many features are shared throughout the group. ''Prodeinotherium'' and ''Deinotherium'' both had large, downcurved tusks on the lower jaw, but none on the upper jaw. This could have been used to grasp food while the tusks moved branches out of the way. ''Prodeinotherium'' was slightly smaller than ''Deinotherium'', yet much larger than more primitive proboscideans. All ''Prodeinotherium'' species were similar in size, ranging from tall and weighing about .

Description

''Prodeinotherium'' was the size of the present Asian elephant, about at the shoulders, but differing from elephants by lacking upper tusks and instead possessing downward-facing lower tusks. In appearance and many characters, it was like ''Deinotherium'', but differed in being of smaller size, having shorter fore limbs, and also in various details in the shape and form of the teeth.Sanders, W. J., Kappelman, J. & Rasmussen, D. T., 200
New large-bodied mammals from the late Oligocene site of Chilga, Ethiopia. ''Acta Palaeontologica Polonica''
Vol. 49, no.3, pp. 365–392 A potentially adult female specimen of ''P. bavaricum'' is estimated to be tall and weigh , while an adult male measured tall and was about . The earliest species ''P. hobleyi'' was estimated at similar tall and . ''Prodeinotherium hobleyi'' was larger and more specialised than its Oligocene predecessor ''Chilgatherium''. It flourished for several millions of years, before being replaced in the middle Miocene by the much larger ''Deinotherium''.

''Prodeinotherium'' is distinguished from ''Deinotherium'' from multiple features, including possessing a different dental formula of 003/103 and 0023/1023; M2-3 with an ornamentation; the rostrum turns down parallel to the mandibular symphysis; the rostrum and external nares narrow; the swelling of the preorbital is close to the orbit; the roof of the skull is longer and wider than in ''Deinotherium''; the articulation between the neck vertebrae and skull is more upturned; the skeleton is graviportally adapted; the scapula has a prominent spine and a stout acromion and metacromion; and the carpal bones and tarsal bones are narrow, but not dolichopodous.

Deinotheres such as ''Prodeinotherium'' have a muscle attachment for a trunk-like structure. However, instead of an elephant-like trunk, the appendage was more muscular and similar to a tapirs snout. Within the evolution of Deinotheriidae, the paired "tongs" arrangement consisting of upper and lower incisors possessed by earlier Proboscideans was lost.

''P. bavaricum'', fossils of which come from the Upper Freshwater Molasse, is the most well-studied species of ''Prodeinotherium'', with multiple features shared among all specimens, not necessarily to the exclusion of other species. Some of these features include "small size, generally simple dental structure, less enamel plication and crenulation, ... thus the valleys of the premolars are well separated, slender teeth, bicuspid mesial lophid in P3 (the cuspids are distinct but more compressed against each other than in P. hobleyi), and clear mesial projection (“preprotolophide”) in P3; sometimes is bicuspid." Other features noted earlier in 1957 include "the mesial lophid of P3 is well separated into two cuspids, the mesial projection of P3 is well developed and often bicuspid, and the base of the protoconid in P3 is longer than that of the metaconid." ''P. hobleyi'' differs in morphology from ''P. bavaricum'' mostly in these P3 characteristics.

All deinothere mandibles have the same basic anatomy, with a downturned symphysis, and lower incisors. Most differences of deinothere genera are in the P3 tooth morphology and dimensions of the mandible and teeth. Measurements of the mandible have shown that the curve of the jaw is relative to the length of the jaw; a longer jaw means a stronger curve. A distinguishing feature of ''Prodeinotherium'' is that the area at the base of the curve in the jaw is flat, while a depression is seen in all specimens of ''Deinotherium''.

Taxonomy and evolution

''Prodeinotherium'' lived during the Early Miocene and Middle Miocene, about 19.0 to 18.0 million years ago (Mya). ''Prodeinotherium'' likely evolved from ''Chilgatherium'', or the common ancestor of the two genera. The earliest remains of ''Prodeinotherium'' come from Kenya, where two deposits preserving the genus date to 22.5 and 19.5 Mya according to one 1978 study. The same study found that fossils from Uganda date to 20.0 Mya. However, more recent studies (from 1988, 1991, and 2002) find that the deposits date to >17.9, 19.5, and 17.0 Mya, respectively. After evolving in Africa, ''Prodeinotherium'' spp. likely migrated into Asia and then Europe with the formation of the " ''Gomphotherium'' land bridge". ''Prodeinotherium'' may have gone extinct around 15.5 Mya, based on the last known fossils from the Arabian Peninsula. ''P. hobleyi'' was the first species to evolve, followed soon after ''P. pentapotamiae'' and then ''P. bavaricum'' around the same time. These species are from Africa, Europe, and South Asia, respectively. ''Prodeinotherium'' was replaced in Asia by ''Deinotherium indicum'', in Europe by ''D. giganteum'', and in Africa by ''D. bozasi''.

Deinotheres are quite controversial with regards to the systematics. Many species have been named, yet major studies by Harris and Huttunen find that only three species in each genus are valid, based on distribution and smaller details. Within ''Prodeinotherium'', the species found valid by these authors include ''P. bavaricum'', ''P. pentapotamiae'', and ''P. hobleyi''. Many descriptions of new species of deinotheres are based upon limited material compared to only a small number of the species. Thus, many species of deinotheres are no longer valid. In addition to invalid species, ''Prodeinotherium'' has on occasion been synonymized with ''Deinotherium''. Species of ''Prodeinotherium'' found to be valid by multiple studies include ''P. cuvieri'', ''P. sinense'', and ''P. orlovii''. In a study 2011 analyzed the mandibles of multiple genera in a phylogenetic analysis. Their results are shown below:

History of discovery

''Deinotherium bavaricum'' was originally mentioned in a paper by Christian Erich Hermann von Meyer in 1831. However, his first description of the material came in 1833, in which he also created the new species ''Dinotherium bavaricum'', the accidental change in genus spelling making it a ''lapsus calami''. The material known is the lectotype P3, in the Bayerische Staatssammlung für Paläontologie und historische Geologie, selected from a group of specimens (a syntype) from Bavaria. Meyer compared the tooth to the material of ''Deinotherium gigantium'', and found enough features to distinguish it as a separate species. Most deinotheres were lumped into ''Deinotherium'' until the studies of Harris, who concluded that morphology separated them into two genera, ''Prodeinotherium'' and ''Deinotherium''. As the earliest description of a small deinothere in Europe, ''P. bavaricum'' became the type species of ''Prodeinotherium''. ''Prodeinotherium'' was named in 1830 by Ehik, and its name is derived from ''pro'' – "before" ''Deinotherium'' – "terrible beast".

Another early description of ''Prodeinotherium'' is that of Kaup (1832). He described teeth previously assigned to '' Tapir gigantesque'', finding them to be a new deinothere. Kaup assigned these to ''Dinotherium cuvieri'', using size to distinguish it from ''D. giganteum''. However, the size, morphology, and distribution match that of ''P. bavaricum'', thus the latter became the senior synonym. Later in 1836, Lartet described yet another deinothere that eventually became ''P. bavaricum''. This new species was named ''Deinotherium secondarium'', for teeth from France. Lartet published no description, and did not mention this species in later works. Huttunen showed that the distribution of ''D. secondarium'' was within that of ''P. bavaricum'', thus considered the two species likely synonymous. Later, Ehik (1930) described the genus and the new species ''Prodinotherium hungaricum'', misspelling the genus name. The species was known from a jaw with teeth and some post cranial elements. This material was from Királd, and was destroyed, but casts of it remain in the Hungarian Natural History Museum. Diagnosed by dental features, and post cranial morphology, the specimen was later found similar to specimens from elsewhere in Europe, which were assigned to ''P. bavaricum''. Harris found ''P. hungaricum'' to be a synonym of ''P. bavaricum'', a conclusion followed by Huttunen. ''P. petenyii'' was described in 1989 by Vörös, who found it to differ from all other ''Prodeinotherium'' species. From Hungary, the material includes a jaw with teeth. The tooth morphology is very similar to that of ''P. bavaricum'', and although the species has the unique feature of tusks that do not curve down and instead project forwards, Huttunen considered it a synonym of ''P. bavaricum''.

In 1868, Hugh Falconer's notes from before his death were published, including the description of material that he labelled ''Dinotherium pentapotamiae''. This was from the Sewalik of India, he noted that the teeth were possibly the same as ''D. indium'', but were within the range of a midsized individual. This presumption as ''D. indium'' was based on the possibility that ''D. giganteum'' was the only species of ''Deinotherium'' in Europe, and the variation of individuals of '' Mastodon longirostris'' within a population. This species was later reassigned to ''Prodeinotherium'', distinct from ''D. indicum''.

The African species, ''P. hobleyi'', was first described in 1911 by Charles William Andrews. The species was from East Africa, and was named ''Dinotherium hobleyi''. Andrews described these remains, which included a mandible with teeth, a calcaneum, a patella, and other indeterminable fragments, shipped to him by C.W. Hobley. It was compared to ''Dinotherium cuvieri'', and although they were similar, the minor differences and geographical separation were enough for Andrews to create a new species. This species was later reassigned to ''Prodeinotherium'', as the only species from Africa.

''P. sinense'' was described in 2007 as a late species of ''Prodeinotherium''; it was described by Qui ''et al.'', and is known from dental material and jaw. It was first found in 2005, in Gansu, China. It is of a Late Miocene age, thus is younger than other ''Prodeinotherium'' species. That study also found that the material of ''P. hungaricum'' is distinct from ''P. bavaricum''. A study in 2010 by Vergiev & Markow noted that the teeth are quite similar to those of ''Deinotherium'', and based on these features and age the species was thought to either be a species in between ''Prodeinotherium'' and ''Deinotherium'', or belonging to the latter genus.

Early depictions of deinotheres such as ''Prodeinotherium'' were scientifically incorrect. Before postcranial material was known, the genera were considered to be rhinos, giant tapirs, sirenians, whales, and marsupials. However, with postcranial material came the proposal of an elephantine relation. However, early depictions of deinotheres were too elephantine, practically only with the addition of lower tusks. These restorations were inaccurate, because they showed the lower lip directly beneath the trunk, with the tusks projecting from the "chin". According to a 2001 study, the tusks more likely projected above the lip, which followed the curvature of the jaw down. Another inaccuracy is likely the length of the trunks. Having a long, elephantine trunk was thought of as unlikely by multiple authors, including Harris and the 2001 study. Besides the large opening often associated with a trunk, the general skull structure makes it unlikely for the trunk to be elongated. The upper tusks, retained in all more derived proboscideans, were likely lost so that the upper lip could directly manipulate the food of ''Prodeinotherium''.

Paleobiology

''Prodeinotherium'' was a herbivorous organism. Based on the known distribution of fossils, ''Prodeinotherium'' could only survive along the coast in closed forests. Rodents and fish may have lived in the same environment or region as ''Prodeinotherium''. In Europe, fossils of ''Gomphotherium'' have been found alongside those of ''Prodeinotherium'', showing that the genera likely ate different plants.

Deinotheres were browsers, meaning they ate plants above ground level. Deinotheres possibly ate specific dicots. These could be found in closed woodland forests. The way they chewed their food was probably similar to that of modern tapirs, with the front teeth being used to crush the food, while the second and third molars have a strong vertical shearing action, with little lateral movement. This chewing action differs from both that of gomphotheres (lateral grinding) and elephants (horizontal shearing). Deinothere molars show little wear, indicating a diet of soft, nongritty, forest vegetation, with the down-turned lower tusks being used for stripping bark or other vegetation. The supports for the tusks used in feeding is also based on the fact that juveniles have a different tusk morphology, which is consistent on them likely possessing a slightly different diet or feeding strategy. The trunks of deinotheres were likely similar to a tapirs, which could have been used for grasping plant matter and moving it to where the tongue could manipulate it.

References

External links

Phenomena: The largest Beast to walk the Earth
discussing the size and weight estimates of Larramendi (2015).

{{Taxonbar, from=Q2048802

Deinotheriids
Miocene proboscideans
Langhian genus extinctions
Prehistoric placental genera
Miocene mammals of Africa
Miocene mammals of Asia
Miocene mammals of Europe
Aquitanian genus first appearances
Fossil taxa described in 1930