近代鱼鳞中羟基磷灰石的变化

J. Nemliher, T. Kallaste, I. Puura
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引用次数: 2

摘要

. 用x射线衍射分析研究了近代鲨鱼、鳐鱼和硬鱼鳞片中磷灰石的矿物学。所研究的鱼鳞均由不同晶格参数的羟基磷灰石组成。近代鳐鱼和硬鱼鳞片中的磷灰石晶格参数范围为a=9.44-9.46 апа,与近代脊椎动物骨骼中的磷灰石晶格参数相当。鲨鳞磷灰石晶格参数a = 9.40 ~ 9.41, c = 6.87 ~ 6.88,与近代舌形腕足类壳中的磷灰石较为接近。不同的晶格参数反映了化学成分的差异,首先是羟基、氟和碳酸盐阴离子的含量。从进化的角度来看,现代鱼类高级分类群之间的这些差异具有重要意义,并对化石脊椎动物骨骼的矿物学解释具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
HYDROXYAPATITE VARIETIES IN RECENT FISH SCALES
. Mineralogy of apatite in the scales of Recent sharks, rays, and teleosts was studied using X-ray diffraction analysis. All the studied fish scales are composed of hydroxyapatite with different lattice parameters. The apatite in the scales ofRecent rays and teleosts has lattice parameters within the range of a=9.44-9.46 апа с = 6.87-6.88, which is comparable to the apatite in Recent vertebrate bones. The shark scale apatite has lattice parameters a = 9.40-9.41 and c = 6.87-6.88, closer to the apatite in Recent lingulate brachiopod shells. The distinct lattice parameters reflect differences in the chemical composition, first of all, in the content of hydroxyl, fluorine, and carbonate anions. These differences between the higher taxa of Recent fishes are significant from an evolutionary perspective and have implications to the interpretation of the mineralogy of fossil vertebrate skeletons.
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