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An enigmatic crocodyliform tooth from the bauxites of western Hungary suggests hidden mesoeucrocodylian diversity in the Early Cretaceous European archipelago

机译:匈牙利西部铝土矿中的一种神秘的鳄形牙齿表明在欧洲早白垩世群岛中隐藏着的中古鳄类多样性

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摘要

Background. The Cretaceous of southern Europe was characterized by an archipelago setting with faunas of mixed composition of endemic, Laurasian and Gondwanan elements. However, little is known about the relative timing of these faunal influences. The Lower Cretaceous of East-Central Europe holds a great promise for understanding the biogeographic history of Cretaceous European biotas because of the former proximity of the area to Gondwana (as part of the Apulian microcontinent). However, East-Central European vertebrates are typically poorly known from this time period. Here, we report on a ziphodont crocodyliform tooth discovered in the Lower Cretaceous (Albian) Alsopere Bauxite Formation of Olaszfalu, western Hungary. Methods. The morphology of the tooth is described and compared with that of other similar Cretaceous crocodyliforms. Results. Based on the triangular, slightly distally curved, constricted and labiolingually flattened crown, the small, subequal-sized true serrations on the carinae mesially and distally, the longitudinal fluting labially, and the extended shelves along the carinae lingually the tooth is most similar to some peirosaurid, non-baurusuchian sebecosuchian, and uruguaysuchid notosuchians. In addition, the paralligatorid Wannchampsus also possesses similar anterior teeth, thus the Hungarian tooth is referred here to Mesoeucrocodylia indet. Discussion. Supposing a notosuchian affinity, this tooth is the earliest occurrence of the group in Europe and one of the earliest in Laurasia. In case of a paralligatorid relationship the Hungarian tooth would represent their first European record, further expanding their cosmopolitan distribution. In any case, the ziphodont tooth from the Albian bauxite deposit of western Hungary belongs to a group still unknown from the Early Cretaceous European archipelago and therefore implies a hidden diversity of crocodyliforms in the area.
机译:背景。欧洲南部的白垩纪以群岛环境为特征,其动物群由地方,劳拉和贡瓦南元素组成。但是,关于这些动物影响的相对时间知之甚少。由于该地区以前靠近冈瓦纳(属于阿普利亚微大陆的一部分),因此中欧下白垩统对了解白垩纪欧洲生物区系的生物地理历史具有广阔的前景。但是,从这一时期开始,中东欧的脊椎动物通常鲜为人知。在这里,我们报道在匈牙利西部Olaszfalu的下白垩统(阿尔比亚)Alsopere铝土矿层中发现的一条ziphodont鳄形牙齿。方法。描述了牙齿的形态并将其与其他类似的白垩纪鳄形牙齿进行比较。结果。基于三角形的,略向远端弯曲的,收缩的和唇舌扁平的冠状结构,小而近等长的真齿锯齿状的近中,远端,沿唇的纵向凹槽和沿舌突的延伸齿架与某些牙齿最相似peirosaurid,非baurusuchian sebecosuchian和uruguaysuchid notosuchians。另外,旁齿的Wannchampsus也具有相似的前牙,因此匈牙利牙在此处称为中性法齿科。讨论。假定这种牙齿具有亲切关系,这是该群体最早出现在欧洲,也是最早出现在劳拉西亚的一种。如果是近亲关系,匈牙利的牙齿将代表他们的第一个欧洲记录,从而进一步扩大其国际化分布。无论如何,来自匈牙利西部Albian铝土矿床的ziphodont牙齿属于早白垩世欧洲群岛仍不为人所知的一群,因此暗示该地区的鳄形动物具有隐藏的多样性。

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