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Unique Biochemical and Mineral Composition of Whale Ear Bones

1Department of Geology and Geophysics, University of Wyoming, 1000 East University Avenue 3006, Laramie, Wyoming 82071; 2Department of Anatomy and Neurobiology, Northeast Ohio Medical University, Rootstown, Ohio 44272; 3Program in Ecology, University of Wyoming, 1000 East University Avenue 3622, Laramie, Wyoming 82071; 4Department of Wildlife Management, North Slope Borough, Barrow, Alaska 99753; 5Biology Department, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543; and Department of Otology and Laryngology, Harvard Medical School, Boston, Massachusetts 02114

Cetaceans are obligate aquatic mammals derived from terrestrial artiodactyls. The defining characteristic of cetaceans is a thick and dense lip (pachyosteosclerotic involucrum) of an ear bone (the tympanic). This unique feature is absent in modern terrestrial artiodactyls and is suggested to be important in underwater hearing. Here, we investigate the mineralogical and biochemical properties of the involucrum, as these may hold clues to the aquatic adaptations of cetaceans. We compared bioapatites (enamel, dentine, cementum, and skeletal bone) of cetaceans with those of terrestrial artiodactyls and pachyosteosclerotic ribs of manatees (Sirenia). We investigated organic, carbonate, and mineral composition as well as crystal size and crystallinity index. In all studied variables, bioapatites of the cetacean involucrum were intermediate in composition and structure between those of tooth enamel on the one hand and those of dentine, cementum, and skeletal bone on the other. We also studied the amino acid composition of the cetacean involucrum relative to that of other skeletal bone. The central involucrum had low glycine and hydroxyproline concentrations but high concentrations of nonessential amino acids, unlike most bone samples but similar to the tympanic of hippos and the (pachyosteosclerotic) ribs of manatees. These amino acid results are evidence of rapid bone development. We hypothesize that the mineralogical and amino acid composition of cetacean bullae differs from that of other bone because of (1) functional modifications for underwater sound reception and (2) structural adaptations related to rapid ossification.