The genus
Cerorhinca evolved in the North Pacific, apparently in the mid-late
Miocene. Although today only one species remains, it used to be much more diverse, both in number of species and in distribution. Fossils have been found as far south as
Baja California. The first record of the clade from the Atlantic Ocean was reported by Smith et al. (2007) and suggests that the biogeographic history of
Cerorhinca is more complex than previously thought. Known prehistoric species are: • Dubious auklet,
Cerorhinca dubia L. H. Miller, 1925 (Late Miocene of San Barbara County, USA) •
Cerorhinca minor Howard, 1971 (Late Miocene/Early Pliocene of Cedros Island, Mexico) •
Cerorhinca reai Chandler, 1990 (San Diego Late Pliocene, North American Southwest) •
Cerorhinca aurorensis N. A. Smith, 2011, a
nomen nudum, only published in a PhD dissertation (Yorktown Formation Late Pliocene, North Carolina, USA) •
Cerorhinca sp. (Early Pliocene, Southeastern Woodlands)
Bill fluorescence Since rhinoceros auklets are monogamous and highly social, the species depend heavily on physical characteristics of the other species in order to choose a lifetime mate. The prominent horn on the bill of breeding rhinoceros auklet is one evolutionary byproduct of this behavior. The bill has fluorescent characteristics when viewed under ultraviolet light. Several bird species are able to detect cues through UV light, which supports the claim that this fluorescence is also meant for breeding purposes. While the upper and lower mandible give off fluorescence as well, this phenomenon is most prominent in the horn. There is no evidence for disparity of fluorescence between sexes, however, the amount of fluorescence does vary between individual auks. ==References==