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Interrelationships of Late Neogene Elephantoids: New evidence from the Middle Awash Valley, Afar, Ethiopia

Identifieur interne : 00A755 ( Main/Exploration ); précédent : 00A754; suivant : 00A756

Interrelationships of Late Neogene Elephantoids: New evidence from the Middle Awash Valley, Afar, Ethiopia

Auteurs : Jon E. Kalb [États-Unis] ; David J. Froehlich [États-Unis]

Source :

RBID : ISTEX:A1D5E3A7B0AEA81E9008530C352128ED00BCE496

Descripteurs français

English descriptors

Abstract

Abstract: As the most diverse collection of Elephantoidea from one area and a single stratigraphic sequence, fossils from the Middle Awash Valley, Ethiopia, add significantly to our current knowledge of the morphology and systematic phylogeny of late Neogene proboscideans. Abundant specimens of the late surviving “gomphothere” (in the informal sense), Anancus, reveal two species, an earlier more plesiomorphic form in our cladistic analysis and a later, more derived form. The former is tetralophodont on the M2 and is similar to the poorly preserved A. kenyensis from Kenya; also this earlier form is likely to be the immediate ancestor of a more derived tetralophodont Anancus from South Africa. In turn, these two species are clearly ancestral to pentalophodont sister taxa, one from North Africa (A. petrocchii) and a second from the Middle Awash. Both the South African and Ethiopian derived Anancus are apparently new species. All known African genera of the family Elephantidae are also present in the Middle Awash including the three “stegomorphs”, Stegotetrabelodon, Stegodibelodon and Stegodon, all of which form a monophyletic group with the subfamily, Elephantinae, comprising Primelephas, Loxodonta, Mammuthus, and Elephas. In our cladistic analysis, the stegomorphs form a series of paraphyletic taxa that are clearly plesiomorphic to the more widely known elephantines. Finally, the abundant Middle Awash elephants add to our belief that the loxodonts and the remaining elephants (Primelephas, Mammuthus, Elephas) form separate clades that are sister groups to one another.

Url:
DOI: 10.1016/S0016-6995(95)80068-9


Affiliations:


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Le document en format XML

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<div type="abstract" xml:lang="en">Abstract: As the most diverse collection of Elephantoidea from one area and a single stratigraphic sequence, fossils from the Middle Awash Valley, Ethiopia, add significantly to our current knowledge of the morphology and systematic phylogeny of late Neogene proboscideans. Abundant specimens of the late surviving “gomphothere” (in the informal sense), Anancus, reveal two species, an earlier more plesiomorphic form in our cladistic analysis and a later, more derived form. The former is tetralophodont on the M2 and is similar to the poorly preserved A. kenyensis from Kenya; also this earlier form is likely to be the immediate ancestor of a more derived tetralophodont Anancus from South Africa. In turn, these two species are clearly ancestral to pentalophodont sister taxa, one from North Africa (A. petrocchii) and a second from the Middle Awash. Both the South African and Ethiopian derived Anancus are apparently new species. All known African genera of the family Elephantidae are also present in the Middle Awash including the three “stegomorphs”, Stegotetrabelodon, Stegodibelodon and Stegodon, all of which form a monophyletic group with the subfamily, Elephantinae, comprising Primelephas, Loxodonta, Mammuthus, and Elephas. In our cladistic analysis, the stegomorphs form a series of paraphyletic taxa that are clearly plesiomorphic to the more widely known elephantines. Finally, the abundant Middle Awash elephants add to our belief that the loxodonts and the remaining elephants (Primelephas, Mammuthus, Elephas) form separate clades that are sister groups to one another.</div>
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