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ARTICLES

Evolution of Protanancus (Proboscidea, Mammalia) in East Asia

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Article: e881830 | Received 29 Nov 2012, Accepted 31 Dec 2013, Published online: 23 Jan 2015
 

ABSTRACT—

Interspecific competition and species replacement explain many evolutionary successions, but these processes are difficult to test. According to recent paleontological research, amebelodontines were predominant proboscideans in faunas of the early to middle Miocene of East Asia. In addition to the abundant Platybelodon, other amebelodontines are known, but they have been largely neglected by researchers. Here we describe two species of Protanancus, Pr. tobieni and Pr. brevirostris, sp. nov., from China. The former was present during the middle Miocene in Tongxin and Qin’an and was previously attributed to Amebelodon or Serbelodon; the latter was present during the early Miocene in the Linxia Basin. Cladistic analysis indicates that the two species appear to represent primitive members of Protanancus. However, the phylogenetic relationship among Protanancus, Platybelodon, and Amebelodon remains unresolved because of their strong parallel evolution. Our study suggests intensive competition between Protanancus and Platybelodon based on similarities in their mandibular morphologies and dental microwear patterns, with the former genus disappearing from East Asia by the late middle Miocene. This scenario is supported by a mechanical model, in which lower tusks with dentinal tubules, as occur in Platybelodon, show greater resistance to the adverse effects of both a heavy load and abrasion than those with concentric laminae, present in Protanancus. The model aids in interpreting the evolution of the inner structure of the lower tusks of amebelodontines, which may have provided a competitive advantages for these species.

http://zoobank.org/urn:lsid:zoobank.org:pub:4D33BD71-CB05-4058-B9DD-337060B0B7CB

SUPPLEMENTAL DATA——Supplemental materials are available for this article for free at www.tandfonline.com/UJVP

ACKNOWLEDGMENTS

We thank P. Tassy, U. Göhlich, M. Pickford, Z.-X. Qiu, G.-F. Chen, and Y. Wang for their advice and discussions; J. Ye for stratigraphic work; and D. Liu, C.-H. Zeng, W. He, and S.-Q. Chen for specimens preparation. We also thank the reviewers H. Saegusa and G. Markov and editor J. Theodor for their generous advice. This work was supported by the National Basic Research Program of China (grant no. 2012CB821900), the Chinese Academy of Sciences (grant no. XDB03020104), and the National Natural Science Foundation of China (grant nos. 41372001, 41430102).

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