首页> 外文期刊>Journal of vertebrate paleontology >Otoliths in situ in the stem teleost Cavenderichthys talbragarensis (Woodward, 1895), otoliths in coprolites, and isolated otoliths from the Upper Jurassic of Talbragar, New South Wales, Australia
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Otoliths in situ in the stem teleost Cavenderichthys talbragarensis (Woodward, 1895), otoliths in coprolites, and isolated otoliths from the Upper Jurassic of Talbragar, New South Wales, Australia

机译:在斯特鲁斯·斯托克斯(Woodward,1895)中,奥斯特里斯,奥特洛岩,新南威尔士州,新南威尔士州塔布拉加的右侧右右右侧,奥特洛斯科斯(Woodward,1895),和孤立的右侧

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摘要

Cavenderichthys talbragarensis (Woodward, 1895) is a common signature freshwater stem teleost in the Upper Jurassic of Australia. Our discovery of numerous otoliths in the Talbragar Fish Bed establishes Cavenderichthys as only the second known Jurassic teleost and the third known stem teleost with otoliths in situ and provides an important calibration point for the interpretation of isolated Mesozoic otoliths. It corroborates the low degree of morphological diversification of stem teleost otoliths. The abundance of otoliths (isolated, in coprolites and in situ) allows the mapping of ontogenetic effects and of intraspecific variability for the first time in attributable stem teleost otoliths. Here, we describe 284 otoliths, mostly from Cavenderichthys. Otoliths in situ in Cavenderichthys document the presence of sagitta, lapillus, and asteriscus. Three other, much rarer otolith types were also found that have a teleost otolith pattern more primitive than that of Leptolepidiformes; the origin of these is unknown, but it is likely that they stem from pholidophoriform fishes of the family Archaeomenidae. If confirmed, this otolith pattern would provide a further highly diagnostic and synapomorphic character to define teleosts at the level of the Leptolepidiformes and above. Different mineral replacement processes in fossils from the Talbragar Fish Bed aided us in finding many otoliths, particularly otoliths in situ. Given their abundance and distinct preservation, it is surprising that otoliths in the Talbragar Fish Bed have not been recognized before.
机译:Caventichthys Talbragarensis(Woodward,1895)是澳大利亚上部侏罗纪的共同签名淡水茎。我们发现瓦尔布加尔鱼床中众多右侧右侧的偏乐力,仅仅是第二种已知的侏罗纪的TeactoST和第三次已知的茎电视与右侧的原位建立了Caventsichthys,并为解释分离的中生型偏离偏离偏离others提供了一个重要的校准点。它证实了茎Textost ottoliths的低程度的形态多样化。偏乐(分离在群体和原位)的丰度允许在可归因的茎Textost Otoliths中首次绘制Ontogency效应和内部变异性。在这里,我们描述了284个Otoliths,主要来自Caventichththys。在Caventsichthys原位原位记录了射击,莱帕里斯和星星的存在。另外三种罕见的偏靠类型也发现,具有远紧靠极端的右侧模式比乳胶脂肌肉更重要;这些起源是未知的,但它们可能源于古尼尼西亚群族的素质鱼类鱼类。如果确认,这种Otolith模式将提供进一步高度诊断和突触突变性的特征,以在Leptolepiformes及以上的水平下定义Teactosts。来自瓦拉加尔鱼床的化石中的不同矿物替代过程帮助我们找到了许多右侧,特别是Otoliths原位。鉴于他们丰富和独特的保存,令人惊讶的是,塔布拉加鱼床中的欧特里斯之前没有被认可。

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