Zygolophodon
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Through Indian subcontinent
Description
As with other mammutids, the molars have a zygodont morphology. The lower jaw has an elongate mandibular symphysis and bears tusks/incisors. The upper tusks have enamel bands and are untwisted and downward curving, and outwardly diverge from each other. The jaws retained permanent premolar teeth.
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Ecology
Zygolophodon is suggested to have primarily had a browsing-based diet.
Taxonomy
Zygolophodon belongs in the family Mammutidae, whose best known member is the American mastodon (Mammut americanum).
The genus likely originated in Africa. The oldest species is Z. aegyptensis, known from Egypt and Namibia, dating to the late Early Miocene-early Middle Miocene. The species Z. turicensis had a widespread distribution in both Africa (Kenya, Tunisia), Anatolia and Europe, dating to the Early-Late Miocene, with its earliest appearance in Europe being approximately 18-17 million years ago, and last appearance in the region dating to around 7-6 million years ago. The youngest confirmed record of Zygolophodon in Africa dates to around 13 million years ago, based on teeth suggested to belong to Z. turicensis found in Kenya, though a possible younger record is known from the Late Miocene of Algeria.
The species Z. tapiroides (Desmarets, 1822) is considered invalid. The taxonomy of East Asian Zygolophodon is uncertain. Tassy et al. (1988) synonymised many Chinese species with Z. gobiensis (including Z. lufengensis, Z. chinjiensis, Z. nemonguensis, Z. gromovae and Z. jiningensis, as well as Miomastodon tongxiensis), with Z. gobiensis also known from Mongolia, but other authors suggest that at least some of these species may be valid. The species Z. atavus is known from the early Middle Miocene of Kazakhstan. The oldest remains of Zygolophodon on the Indian subcontinent are known from the Bugti Hills of Pakistan, dating to around 19-17 million years ago. The species Z. metachinjiensis is known from the mid-Late Miocene of Pakistan. Zygolophodon has also been reported from western India, dating to the mid Miocene, and other probable remains dating to the Late Miocene, around 10 million years old, representing the youngest mammutids on the Indian subcontinent. An indeterminate species has also been reported from Thailand, of uncertain but probably Late Miocene age.
Zygolophodon entered North America during the latter part of the Early Miocene (during the late Hemingfordian faunal stage), with the oldest record being a partial tooth from Massacre Lake, Nevada, dating to 16.5-16.4 million years ago. Remains of Zygolophodon are known from across western and central North America during the following Barstovian (including Colorado, California, Montana, Oregon, Nebraska, Nevada, Wyoming and Saskatchewan). Z. proavus currently represents the only known North American species of Zygolophodon. The youngest specimens of Z. proavus date to approximately 11-12 million years ago. Mammut is thought to be descended from Zygolophodon. The species "Mammut" borsoni, whose relationship with North American Mammut is controversial, and sometimes placed in Zygolophodon (from which, like North American Mammut, it descended from), is the youngest member of Mammutidae in Eurasia, persisting from the Late Miocene into the Earliest Pleistocene, around 2.5-2 million years ago.
Some authors have suggested placing M. tongxinensis, Z. gobiensis and Z. metachinjiensis within a revived Miomastodon, which was originally described for the North American Miomastodon merriami. Miomastodon is usually treated as a synonym of Zygolophodon (with M. merriami typically considered a synonym of Z. proavus) and other authors have reacted with caution to the proposal.