Hallworth R, Wiederhold M L, Campbell J B, Steyger P S
Department of Otolaryngology-Head and Neck Surgery, University of Texas Health Science Center at San Antonio 78284-7777, USA.
Hear Res. 1995 May;85(1-2):115-21. doi: 10.1016/0378-5955(95)00038-6.
Calcitic and aragonitic otoconia from the Japanese red-bellied newt, Cynops pyrrhogaster, were examined using an atomic force microscope. The surface structure of both otoconial polymorphs consisted of arrays of elements approximately 50 nm in diameter. Elements were generally round and were separated by shallow depressions of no more than 20 nm. The elements are suggested to be single crystals of calcium carbonate. The relationship of these observations to theories of otoconial genesis is discussed.
利用原子力显微镜对日本红腹蝾螈(Cynops pyrrhogaster)的方解石型和文石型耳石进行了研究。两种耳石多晶型的表面结构均由直径约50 nm的元素阵列组成。这些元素通常呈圆形,被不超过20 nm的浅凹陷隔开。这些元素被认为是碳酸钙的单晶。本文讨论了这些观察结果与耳石形成理论的关系。