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Journal of Paleontology 91(6):1228–1243
pseudodont sea turtle not directly ancestral to any of the living forms. Probably the evolutionary center of living cheloniid turtles was in the Indo-Pacific region, where the oldest turtle convincingly referable to the crown cheloniids has been repor- ted from lower Miocene strata along the eastern margin of the Pacific basin (Brinkman, 2009). This conclusion also is sup- ported by the fact that the most basal of the living cheloniid sea turtles, N. depressus, occurs only in the vicinity of Australia, and there is no evidence that it ever was present in any other part of the world ocean (Zangerl et al., 1988). By early in the Pliocene, four of the five living cheloniid
genera (Caretta, Chelonia, Eretmochelys, and Lepidochelys) had migrated into the North Atlantic basin (Dodd and Morgan, 1992). Even so, Trachyaspis lardyi continued to persist there well into the Pliocene despite the arrival of these new competi- tors (Zug, 2001). It is possible that it persisted in this region entirely through the Pliocene, because T. lardyi is known to have persisted into the late Pliocene in Italy (Villa and Raineri, 2015). By the Pleistocene, however, T. lardyi apparently was extinct, and the sea turtle fauna of the North Atlantic basin took on its present complexion.
Acknowledgments
The authors would like to thank J. ParhamandW. Joyce for their thorough review of this paper and their excellent suggestions for its improvement.A special note of thanks also is due to W. Joyce for running a phylogenetic analysis for us using TNT.Without his generous help, this paper could not have reached fruition.
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