Calcitic and aragonitic otoconia from the Japanese red-bellied newt, C
ynops pyrrhogaster, were examined using an atomic force microscope. Th
e surface structure of both otoconial polymorphs consisted of arrays o
f elements approximately 50 nm in diameter. Elements were generally ro
und and were separated by shallow depressions of no more than 20 nm. T
he elements are suggested to be single crystals of calcium carbonate.
The relationship of these observations to theories of otoconial genesi
s is discussed.