Lustmann J, Shteyer A
J Dent Res. 1981 Aug;60(8):1386-95. doi: 10.1177/00220345810600080101.
Ultrastructural morphology of 16 salivary calculi was studied by means of transmission and scanning electron microscopy. The external surface was mostly globular or coarse, and on high magnifications and features could be divided into four main groups: a) amorphic calcified deposits covering extensive areas, b) other areas covered with crystals in a variety of arrangements, c) heavy accumulations of calcified rod-like and filamentouslike microorganisms, and d) platelet crystals in juxtaposition to calcified microorganisms in several areas. In most calculi the split area was found to be laminated. It is suggested that microorganisms have an important role in the formation and growth of salivary calculi.
通过透射电子显微镜和扫描电子显微镜研究了16颗涎石的超微结构形态。其外表面大多呈球形或粗糙状,在高倍放大下其特征可分为四大类:a)覆盖大片区域的无定形钙化沉积物;b)其他区域覆盖着各种排列的晶体;c)钙化的杆状和丝状微生物大量聚集;d)在几个区域中与钙化微生物并列的血小板晶体。在大多数结石中,裂隙区域被发现是分层的。提示微生物在涎石的形成和生长中起重要作用。