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首页> 外文期刊>Neues Jahrbuch fur Geologie und Palaontologie. Abhandlungen >A Devonian phoebodont shark tooth from a Lower Cretaceous karst fill
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A Devonian phoebodont shark tooth from a Lower Cretaceous karst fill

机译:下白垩纪喀斯特充填的泥盆纪p骨鲨齿

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The Sauerland mountain ridge in NW Germany is well known for its high number of caves and fissures, which are developed within Devonian reef limestones. Several karst events took place in geological history and the resulting cavities were often refilled by sediment. One of these karst fissures near Balve in the Remscheid-Altena Anticline contains sediments of Barremian to Aptian age with fossil remains of fish, turtles, crocodiles, pterosaurs, dinosaurs, and mammals. Among them, a single, extraordinarily preserved, minuscule shark tooth is indistinguishable in its preservation from the Cretaceous fossils. Nevertheless, several characters, such as an orolingual button on the surface of its base clearly identify it as the tooth of Phoebodus sophiae, an ancient shark taxon approximately 255 million years older than the Cretaceous vertebrate remains in the karst fissure. It is the first unambiguous evidence of the Phoebodus type species in Germany.
机译:德国西北部的Sauerland山脊以其大量的洞穴和裂隙而闻名,这些洞穴和裂隙是在泥盆纪珊瑚礁石灰岩中形成的。地质历史上发生了几次喀斯特事件,由此产生的空洞经常被沉积物所填充。雷姆沙伊德-阿尔滕纳背斜Balve附近的这些喀斯特裂隙之一包含巴雷米亚至Aptian时代的沉积物,以及鱼类,乌龟,鳄鱼,翼龙,恐龙和哺乳动物的化石遗骸。其中,单个极少保存的小鲨鱼牙齿在保存方面与白垩纪化石没有区别。然而,一些字符,例如其基部表面上的口音按钮清楚地将其标识为Phoebodus sophiae的牙齿,Phoebodus sophiae是一种古老的鲨鱼类群,比白垩纪脊椎动物存在约2.55亿年,仍然存在于岩溶裂隙中。这是德国Phoebodus型物种的第一个明确证据。

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