Rensberger J M, Pfretzschner H U
Department of Geological Sciences, University of Washington, Seattle 98195.
Scanning Microsc. 1992 Jun;6(2):495-508; discussion 508-10.
Astrapotheres, large extinct ungulates of South America, share with rhinoceroses vertical prism decussation in the cheek tooth enamel. The similarity extends beyond merely the direction of the planes of decussation. The vertical decussation in astrapotheres is confined to the inner part of the enamel and has uniformly well-defined zones in which the prism direction differs by nearly 90 degrees and the zones are separated by narrow transitional borders of intermediate prism direction. The outer enamel consists of predominantly occlusally and outwardly directed prisms. Within the outer enamel is a region of horizontally decussating prisms; here the angle of decussation is usually smaller than that of the inner vertically decussating prisms. Except for the horizontal decussation in the outer enamel, these conditions match structures that have been described for rhinocerotoids. These features, together with the similarity in premortem crack direction and gross shape of the cheek teeth, imply that astrapotheres and rhinocerotoids shared essentially the same system of cheek tooth mechanics. However, the microstructure of the canine enamel in the astrapotheres is distinct. The lower canine enamel of the Oligocene Parastrapotherium exhibits a form of vertical decussation modified by a wavelike bending of prism zones, whereas the decussation in the rhinocerotoid canine is horizontal. The lower canine in Parastrapotherium was subjected to different loading conditions, judging from multiple sets of premortem crack directions. The modified vertical decussation would in theory resist cracking under different directions of tensile stresses. This is confirmed by the sinuous paths of cracks that run in directions differing by up to 90 degrees. That diverse stresses were generated in the enamel during life is confirmed by the pattern of premortem cracks in Parastrapotherium. The enamel in the upper canine of a late Miocene astrapothere lacks decussation but may have resisted cracking under varied loading conditions by virtue of a 3-dimensional wavelike bending of the prisms.
箭齿兽是南美洲已灭绝的大型有蹄类动物,其颊齿釉质具有与犀牛相同的垂直棱柱交叉结构。这种相似性不仅体现在交叉平面的方向上。箭齿兽的垂直交叉结构局限于釉质内部,具有均匀清晰的区域,其中棱柱方向相差近90度,这些区域由棱柱方向介于中间的狭窄过渡边界分隔。外层釉质主要由向咬合面和向外方向的棱柱组成。在外层釉质内部有一个水平交叉棱柱的区域;这里的交叉角度通常小于内部垂直交叉棱柱的角度。除了外层釉质中的水平交叉结构外,这些情况与犀类动物所描述的结构相匹配。这些特征,加上生前裂纹方向和颊齿总体形状的相似性,意味着箭齿兽和犀类动物具有基本相同的颊齿力学系统。然而,箭齿兽犬齿釉质的微观结构是独特的。渐新世的副箭齿兽的下犬齿釉质呈现出一种垂直交叉结构,棱柱区域呈波浪状弯曲,而犀类动物犬齿的交叉结构是水平的。从多组生前裂纹方向判断,副箭齿兽的下犬齿承受着不同的加载条件。理论上,这种改良的垂直交叉结构可以抵抗不同方向拉伸应力下的开裂。这一点通过裂纹蜿蜒路径得到证实,这些裂纹方向相差可达90度。副箭齿兽生前釉质中产生多种应力这一点通过其生前裂纹模式得到证实。中新世晚期箭齿兽上犬齿的釉质没有交叉结构,但可能通过棱柱的三维波浪状弯曲在不同加载条件下抵抗开裂。