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首页> 外文期刊>Anais da Academia Brasileira de Ciências >A new Xenacanthiformes shark (Chondrichthyes, Elasmobranchii) from the Late Paleozoic Rio do Rasto Formation (Paraná Basin), Southern Brazil
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A new Xenacanthiformes shark (Chondrichthyes, Elasmobranchii) from the Late Paleozoic Rio do Rasto Formation (Paraná Basin), Southern Brazil

机译:来自巴西南部晚古生代里约多拉斯托组(帕拉纳盆地)的一条新的Xenacanthiformes鲨鱼(Chondrichthyes,Elasmobranchii)

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摘要

The Brazilian records on Xenacanthiformes include teeth and cephalic spines from the Parnaíba, Amazonas and Paraná basins. This work describes a new species of Xenacanthidae, collected in an outcrop of Serrinha Member of Rio do Rasto Formation (Wordian to Wuchiapingian), Paraná Basin, municipality of Jacarezinho, State of Paraná. The teeth of the new species are two or three-cuspidated and the aboral surface show a smooth concavity and one rounded basal tubercle. The coronal surface presents one semispherical and subcircular coronal button, and also two lateral main cusps and one central (when present) with less than one fifth of the size of the lateral cusps in the labial portion. The lateral cusps are asymmetric or symmetric, rounded in transversal section, lanceolate in longitudinal section, devoid of lateral carinae and lateral serrations, and with few smooth cristae of enameloid. In optical microscope the teeth show a trabecular dentine (osteodentine) base, while the cusps are composed by orthodentine, and the pulp cavities are non-obliterated by trabecular dentine. The fossil assemblage in the same stratigraphical level and in the whole Rio do Rasto Formation indicates another freshwater record for xenacanthid sharks.
机译:巴西关于Xenacanthiformes的记录包括来自Parnaíba,Amazonas和Paraná盆地的牙齿和头棘。这项工作描述了一种新的Xenacanthidae物种,收集在Paraná州Jacarezinho市Paraná盆地Rio do Rasto组的Serrinha成员露头(Wordian至Wuchiapingian)露头。新物种的牙齿有两个或三个尖齿,并且基部表面显示出平滑的凹面和一个圆形的基底结节。冠状表面具有一个半球形和亚圆形的冠状纽扣,并且还具有两个侧向主瓣和一个中央(当存在时),其小于唇部的侧向瓣的尺寸的五分之一。侧尖不对称或对称,横向切圆,纵切面披针形,没有侧突和侧锯齿,很少有光滑的of骨cr。在光学显微镜下,牙齿呈小梁状的牙本质(osteodentine)基部,而牙尖由原牙本质组成,而牙髓腔则不会被小梁状的牙本质所遮盖。在相同的地层水平和整个里奥·多·拉斯托形成的化石组合表明,塞纳坎西德鲨鱼有另一个淡水记录。

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