Gomphotherium

Most species of Gomphotherium were similar in size to the Asian elephant, with G. productum (known from a 35-year-old male) measuring tall and weighing . The largest species G. steinheimense, known from a complete 37-year-old male found in Mühldorf, Germany, measured up to tall and weighed . and lower tusks Gomphotherium, like most basal elephantimorphs, had an elongated lower jaw (with the elongation specifically being the fused front-most part, the mandibular symphysis) which bore tusks. Species of Gomphotherium are defined by their conservative molar morphology, which includes "trilophed intermediate molars, third molars with three to four loph(id)s, and pretrite half-loph(id)s typically with anterior and posterior accessory conules that form trefoil-patterned enamel loops with wear (simple molar crowns with no accessory conules on the posttrite side of the crown)". It has been suggested that like other long-jawed elephantimorphs, that the trunk was relatively short in comparison to living elephants, probably not reaching much further than the tips of tusks on the lower jaw. == Ecology ==

Most species of Gomphotherium are inferred to have been browsers or mixed feeders, but specimens of G. steinheimense from China are suggested to have been grazers. Gomphotherium, like other elephantimorphs with long lower jaws, is thought to have used its tusks on the lower jaw to cut through vegetation while it was being held in place by the trunk, which likely had a high level of flexibility similar to living elephants. Its feeding strategy is suggested to have been relatively unspecialised, unlike some other contemporary long-jawed elephantimorphs such as Choerolophodon or the amebelodontid Platybelodon. A 2026 study analyzed the chemical composition of teeth of Gomphotherium angustidens from the Miocene (Langhian) strata from Quinta da Farinheira of Portugal, providing evidence of seasonal changes in its diet and probable evidence of geophagia during fixed times of the year.. == Evolution ==

Gomphotherium likely originated in Africa during the late Oligocene-early Miocene. The oldest remains of Gomphotherium are known from Africa, dating to approximately 19.5 million years ago. Gomphotherium migrated into Eurasia across the "Gomphotherium land bridge" approximately 19 million years ago. Gomphotherium underwent rapid evolution after its arrival in Eurasia, reaching its peak diversity during the Early-Middle Miocene. Gomphotherium first arrived in North America during the mid-Miocene, approximately 16-15 million years ago, and is suggested to be ancestral to later New World gomphothere genera, such as Cuvieronius, Stegomastodon and Rhynchotherium. Asian populations of Gomphotherium are suggested to have been ancestral to Sinomastodon. Gomphotherium became extinct in northern China during the Middle Miocene around 13 million years ago. The youngest remains attributed to Gomphotherium in Africa date to around 13-10 million years ago. The last European species of Gomphotherium became extinct at the beginning of the Late Miocene, around the start of MN9, approximately 10 million years ago. The last Gomphotherium species disappeared from North America at the beginning of the Pliocene, approximately 5 million years ago. ==Taxonomy==

Species , Texas. At the AMNH. Over a dozen species of Gomphotherium are considered valid, with over 30 junior synonyms proposed for these taxa. • G. hannibali Welcomme, 1994 Europe, Early Miocene • G. annectens (Matsumoto, 1925) Japan, Early Miocene • G. cooperi (Osborn, 1932) Asia, Early Miocene • G. sylvaticum Tassy, 1985 Europe, Early Miocene • G. libycum (Fourtau, 1918) Egypt, Early Miocene • G. inopinatum (Borissiak and Belyaeva, 1928) China, late Early Miocene-Early middle Miocene • G. mongoliense (Osborn, 1924) Mongolia, late Early Miocene-Early middle Miocene • G. angustidens (Cuvier, 1817) (type) Europe, Middle Miocene • G. subtapiroideum (Schlesinger, 1917) Europe, Early-Middle Miocene • G. tassyi Wang, Li, Duangkrayom, Yang, He & Chen, 2017 China, Middle Miocene • G. browni (Osborn, 1926) Pakistan, Middle Miocene • G. steinheimense (Klahn, 1922) Europe, China, Middle-Late Miocene • G. productum (Cope, 1874) North America, Middle Miocene-Early Pliocene • G. pyrenaicum (Lartet, 1859) Europe, Middle Miocene Phylogeny after Wang et al., 2017 }} }}}}}}}}}}}}}}}}}}}}|label1=Elephantiformes}} == References ==