Over 180 extinct members of Proboscidea have been described. The earliest members of Proboscidea like Eritherium are known from the Paleocene of Africa, around 60 million years ago, the earliest proboscideans were much smaller than living elephants, with Eritherium having a body mass of around 3–8 kilograms (6.6–17.6 lb). By the late Eocene, some members of Proboscidea like Barytherium had reached considerable size, with an estimated mass of around 2 tonnes, while others like Moeritherium are suggested to have been semi-aquatic.
A major event in proboscidean evolution was the collision of Afro-Arabia with Eurasia, during the Early Miocene, around 18-19 million years ago allowing proboscideans to disperse from their African homeland across Eurasia, and later, around 16-15 million years ago into North America across the Bering Land Bridge. Proboscidean groups prominent during the Miocene include the deinotheres, along with the more advanced elephantimorphs, including mammutids (mastodons), gomphotheres, amebelodontids (which includes the "shovel tuskers" like Platybelodon), choerolophodontids and stegodontids. Around 10 million years ago, the earliest members of the family Elephantidae emerged in Africa, having originated from gomphotheres. The Late Miocene saw major climatic changes, which resulted in the decline and extinction of many proboscidean groups such as amebelodontids and choerolophodontids. The earliest members of modern genera of Elephantidae appeared during the latest Miocene-early Pliocene around 6-5 million years ago. The elephantid genera Elephas (which includes the living Asian elephant) and Mammuthus (mammoths) migrated out of Africa during the late Pliocene, around 3.6 to 3.2 million years ago.
The following cladogram is based on endocasts.
Over the course of their evolution, proboscideans experienced a significant increase in body size. Some members of the families Deinotheriidae, Mammutidae, Stegodontidae and Elephantidae are thought to have exceeded modern elephants in size, with shoulder heights over 4 metres (13 ft) and masses over 10 tonnes (22,000 lb), with average fully grown males of the mammutid "Mammut" borsoni having an estimated body mass of 16 tonnes (35,000 lb), making it one the largest and perhaps the largest land mammal ever, with a fragmentary specimen of the Indian elephant species Palaeoloxodon namadicus only known from a partial femur being speculatively estimated in the same study to have possibly reached a body mass of 22 tonnes (49,000 lb). As with other megaherbivores, including the extinct sauropod dinosaurs, the large size of proboscideans likely developed to allow them to survive on vegetation with low nutritional value. Their limbs grew longer and the feet shorter and broader. The feet were originally plantigrade and developed into a digitigrade stance with cushion pads and the sesamoid bone providing support, with this change developing around the common ancestor of Deinotheriidae and Elephantiformes. Members of Elephantiformes and Deinotheriidae have retracted nasal regions of the skull indicating the development of a trunk.
The skull grew larger, especially the cranium, while the neck shortened to provide better support for the skull. The increase in size led to the development and elongation of the mobile trunk to provide reach. The number of premolars, incisors and canines decreased. The cheek teeth (molars and premolars) became larger and more specialised. In Elephantiformes, the second upper incisor and lower incisor were transformed into ever growing tusks on the upper and lower jaws, while in Deinotheriidae there are only tusks on the lower jaw. The tusks are proportionally heavy for their size, being primarily composed of dentine. In primitive proboscideans, a band of enamel covers part of the tusk surface, though in many later groups including modern elephants the band is lost, with elephants only having enamel on the tusk tips of juveniles. The upper tusks were initially modest in size, but from the Late Miocene onwards proboscideans developed increasingly large tusks, with the longest ever recorded tusk being 5.02 metres (16.5 ft) long belonging to the mammutid "Mammut" borsoni found in Greece, with some mammoth tusks likely weighing over 200 kilograms (440 lb). The lower tusks are generally smaller than the upper tusks, but could grow to large sizes in some species, like in Deinotherium (which lacks upper tusks), where they could grow over 1.5 metres (4.9 ft) long, the amebelodontid Konobelodon has lower tusks 1.61 metres (5.3 ft) long, with the longest lower tusks ever recorded being from the primitive elephantid Stegotetrabelodon which are around 2.2 metres (7.2 ft) long.
The molar teeth changed from being replaced vertically as in other mammals to being replaced horizontally in the clade Elephantimorpha. While early Elephantimorpha generally had lower jaws with an elongated mandibular symphysis at the front of the jaw with well developed lower tusks/incisors, from the Late Miocene onwards, many groups convergently developed brevirostrine (shortened) lower jaws with vestigial or no lower tusks. Elephantids are distinguished from other proboscideans by a major shift in the molar morphology to parallel lophs rather than the cusps of earlier proboscideans, allowing them to become higher crowned (hypsodont) and more efficient in consuming grass.
It has been suggested that members of Elephantimorpha, including mammutids, gomphotheres, and stegodontids, lived in herds like modern elephants. Analysis of remains of the American mastodon (Mammut americanum) suggest that like modern elephants, that herds consisted of females and juveniles and that adult males lived solitarily or in small groups, and that adult males periodically engaged in fights with other males during periods similar to musth found in living elephants. These traits are suggested to be inherited from the last common ancestor of elephantimorphs, with musth-like behaviour also suggested to have occurred in gomphotheres. All elephantimorphs are suggested to have been capable of communication via infrasound, as found in living elephants. Deinotheres may have also lived in herds, based on tracks found in the Late Miocene of Romania. Over the course of the Neogene and Pleistocene, various members of Elephantida shifted from a browse-dominated diet towards mixed feeding or grazing.
Below is a taxonomy of proboscidean genera as of 2019.
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