首页> 外文期刊>Journal of vertebrate paleontology >Calcified cartilage in the paired fins of the osteostracan Escuminaspis laticeps (Traquair 1880), from the Late Devonian of Miguasha (Quebec, Canada), with a consideration of the early evolution of the pectoral fin endoskeleton in vertebrates
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Calcified cartilage in the paired fins of the osteostracan Escuminaspis laticeps (Traquair 1880), from the Late Devonian of Miguasha (Quebec, Canada), with a consideration of the early evolution of the pectoral fin endoskeleton in vertebrates

机译:考虑到脊椎动物胸鳍鳍内骨骼的早期进化,来自米瓜沙晚期泥盆纪(加拿大魁北克)的成骨骨棘Escuminaspis laticeps(Traquair 1880)成对鳍的钙化软骨

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摘要

Patches of spherulitic calcified cartilage are described inside the paired fins of the osteostracan Escuminaspis laticeps from the Upper Devonian of Miguasha, Canada, thereby confirming Belles-Isles interpretation of these patches as evidence for paired fin endoskeleton. The distribution of these calcified cartilage patches suggests that the osteostracan paired fin endoskeleton was a single cartilaginous plate located in the lateral half of the fin, and was thus not made up of separate radials. This morphology resembles that of the endoskeletal disc of the embryonic and larval pectoral fin of piscine gnathostomes, prior to its decomposition into radials, and may mirror the general condition for the clade that includes osteostracans and gnathostomes.
机译:球形钙化软骨斑块描述于加拿大米瓜沙上泥盆统的成骨strastic Escuminaspis laticeps的成对鳍中,从而证实了Belles-Isles对这些斑块的解释,作为成对鳍内骨骼的证据。这些钙化的软骨斑块的分布表明,成骨骨水泥配对的鳍鳍内骨骼是位于鳍鳍外侧的单个软骨板,因此不是由单独的radial骨组成。这种形态类似于鱼咬骨鱼类的胚胎和幼虫胸鳍的椎间盘椎间盘,在分解成放射状之前,可能反映了包括骨吸虫和咬骨鱼类的进化枝的一般状况。

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