Several Recent cetacean species have a near-cosmopolitan dis tribution in the open-ocean, with some taxa rarely venturing near shore (Rice, 1998; Jefferson et al, 2008). In contrast, the fossil record of Cet cea is primarily derived from continental shelf sequences (Fordyce and Muizon, 2001). Rare exceptions to this bias include fragmentary fossils dredged from abyssal plains (Turner, 1880; Eastman, 1903; Roux and Geistdoerfer, 1988), and, rarer still, those from oceanic islands (Estevens and vila, 2007). These sources of fossil Cet cea are important because they have the potential to (1) sample fossil cetacean diversity from otherwise poorly represented oceanic paleoenvironments; and (2) add insights into the past zoogeography and ecology of cetaceans that may not be apparent from neritic shelf assem blages. A significant limitation on the last point is the gener ally poor stratigraphic control associated with dredged cetacean fossils (Bianucci et al., 2007). With such uncertain stratigraphic contexts, the broader significance of open-ocean fossil Cet cea is problematic. Although fossil cetaceans from oceanic islands may be associated with more evidence on geologic age, such de posits have hitherto proved extremely rare: late Miocene-early Pliocene fossils on the Azores in the mid-North Atlantic repre sent the sole pre-Holocene record of Cet cea from oceanic is lands (Estevens and Avila, 2007). The Pacific has been the largest ocean throughout cetacean history and its Rim has produced an excellent fossil record (Fordyce, 2008). Yet until now, none of its ~20,000 oceanic islands (i.e., on oceanic crust) have yielded pre Holocene Cet cea. This note reports the first discovery of a pre-Holocene cetacean from a Pacific oceanic island-a stem physeteroid from the Pleistocene of Nauru, represented by an isolated tooth (NMV P204274) (Figs. 1-2). This new fossil evidence adds to knowl edge of both the spatial and temporal distribution of stem Phy seteroidea.
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