First report of hybodont shark from the Toarcian Rosso Ammonitico Formation of Umbria-Marche Apennine Polino area, Terni, Central Italy)

M. Romano, P. Citton, A. Cipriani, S. Fabbi
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引用次数: 14

Abstract

In this contribution we present the first material referable to hybodont shark from the Rosso Ammonitico Formation (Umbria-Marche-Sabina Palaeogeographic Domain). Two teeth were recovered isolated within Toarcian red marly-limestone (Bifrons Zone). The best-preserved tooth is characterized by a general structure well in accord with the classic crushing dentition typical of hybodont sharks within the Subfamily Acrodontinae. The gently domed occlusal surface of the tooth does not show any trace of occlusal crest and of wrinkles, and is characterized by densely pitted, finely reticulated ornamentation. The available characters allow a conservative classification of the material at the genus level as Asteracanthus sp. The best-preserved tooth can be referred to the most mesial area of the first row of lateral teeth, using as a reference the holotype of Asteracanthus medius. The new material represents the earliest evidence of Asteracanthus and the second one from the whole Northern Apennines (Central Italy), throwing new light on the dispersal of the genus on the Jurassic Tethys.
意大利中部Terni Umbria-Marche Apennine Polino地区Toarcian Rosso amonitico组下颚鲨首次报道)
在这篇文章中,我们提出了来自翁布里亚-马尔切-萨比纳古地理域Rosso amonitico组的首个可参考的下颚鲨材料。2颗牙齿分离于托塔西亚红泥灰岩(Bifrons带)中。保存最完好的牙齿的总体结构与肩齿亚科下齿鲨典型的典型碾压牙列非常吻合。牙齿的咬合表面呈轻微的圆丘状,没有任何牙嵴和皱纹的痕迹,其特征是密集的凹坑,精细的网状纹饰。现有的特征允许在属水平上保守地将材料分类为Asteracanthus sp.保存最完好的牙齿可以指第一排侧齿的最内侧区域,使用Asteracanthus medius的全型作为参考。新材料代表了Asteracanthus最早的证据,也是来自整个亚平宁山脉北部(意大利中部)的第二个证据,为该属在侏罗纪特提斯的分布提供了新的线索。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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