Previous studies have suggested that the inner ear of some benthic species of elasmobranchs contain only exogenous material within their otoconial organs, a unique feature within vertebrates. However, these examinations have not accounted for the possibility of otoconial degeneration or used modern experimental methods to identify the materials present. Both of these issues are addressed in this study using inner ear samples from the adult Port Jackson shark, Heterodontus portusjacksoni. A comparison of the otoconial mass in fixed specimens over short and medium time scales reveals that over those timescales the degeneration of calcium carbonate-based otoconia does not occur and confirms that calcium carbonate-based otoconia are not found within the otoconial organs of H. portusjacksoni. Additionally, microanalysis of the chemical composition and ultrastructure of the otoconial mass using energy dispersive X-ray microanalysis and scanning electron microscopy confirms that the entire otoconial mass is comprised of exogenous silicon dioxide particles, bound within a carbon matrix. This exogenous material is suggested to play an equivalent role to the otoconia found in other species of elasmobranchs, and allows both hearing and vestibular control to occur in benthic sharks that spend their lives foraging within a sandy substrate. Anat Rec, 294:373-378, 2011. V V C 2011 Wiley-Liss, Inc.
Key words: audition; inner ear; otoconia; Heterodontus portusjacksoniThe saccular macula found within the sacculus of the fish inner ear is one of the two maculae thought to be responsible for sound detection in elasmobranchs (Corwin, 1981). This macula is hypothesized to be stimulated in response to sound waves, as a result of a smaller displacement of the dense overlying otoconial mass relative to the displacement of the fish's body (Popper et al., 2003). The elasmobranch otoconial mass is analogous to the otolith of other fish. The elasmobranch otoconial mass is generally comprised of assemblages of otoconia, calcium carbonate monohydrate, calcite, aragonite, or vaterite crystals, bound together by a gelatinous matrix