PALEVOPRIM
UMR 7262 CNRS & UP

Laboratoire Paléontologie
Evolution Paléoécosystèmes
Paléoprimatologie
Université de Poitiers

Janvier 2025 : publication PaleorXiv

New data on morphological evolution and dietary adaptations of Elephas recki from the Plio-Pleistocene Shungura Formation (Lower Omo Valley, Ethiopia)

The abundant and diverse proboscideans are essential terrestrial megaherbivores for studying morphological adaptations and reconstructing paleoenvironments in Africa. This new study of the lineage of Elephas recki from the Plio-Pleistocene deposits of the Shungura Formation aimed at investigating further the interplay between morphological and behavioral adaptations within proboscideans. For this, we used the most complete and well-preserved third molars of the series for characterizing morphological changes, while describing dietary behavior by applying mesowear angle analysis to all identifiable cheek teeth. Biometric character changes indicated that evolutionary change was not a gradual, progressive trend through the Shungura sequence deposition. Rather, we observed a complex trend involving sudden changes. The mesowear angle analysis suggested that Elephas recki from the Shungura Formation had consistently grazing dietary habits throughout its evolution, except for some slight tendencies of mixed browse/graze diet in certain time intervals. We therefore did not observe any correlation between morphological change and feeding preferences over two million years. This delay between the acquisition of the observed diet and purportedly consequent morphological changes questions the classical interpretations of factors at play in this evolutionary sequence.

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Fig. 2. – Measurements acquired from teeth of Elephas recki from the Shungura Formation. A, measurements involved in the calculation of the hypsodonty index (HI); B, measurement of the enamel thickness (ET) on sketched occlusal surface of molar plates; C, measurements of mesowear angles (dentin valley angle, in white on the sketch) between ridge of enamel bands (in black) plates of a molar.

Références

Bedane T. G., Mackaye H. T., Boisserie J.-R. 2025 – New data on morphological evolution and dietary adaptations of Elephas recki from the Plio-Pleistocene Shungura Formation (Lower Omo Valley, Ethiopia) – PaleorXiv qexuf, ver. 4 – DOI: 10.31233/osf.io/qexuf

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