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首页> 外文期刊>Acta Palaeontologica Polonica >New dryolestidan mammal from the Hauterivian-Barremian transition of the Iberian Peninsula
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New dryolestidan mammal from the Hauterivian-Barremian transition of the Iberian Peninsula

机译:伊比利亚半岛上特韦尔-巴里米亚过渡期的新的dryolestidan哺乳动物

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摘要

Crusafontia amoae sp. nov. (Dryolestida, Stem Cladotheria) is represented by two isolated upper molars (M4 or M5 and M6 or M7) from the terminal Hauterivian-basal Barremian (Early Cretaceous) of the El Castellar Formation (Galve, Spain). The molars have a deep ectoflexus, a distinct metacone, a continuous metacrista, and an antero-lingually placed paracone. They differ from the molars of the other species of the genus, Crusafontia cuencana, by their larger size, by their outsized parastyle, by the pointed lingual slope of the paracone, their more symmetrical appearance with a deep ectoflexus in occlusal view, and the well-developed metacone. Revision of three isolated teeth previously attributed to Crusafontia cuencana suggests that instead of being upper premolars belonging to Crusafontia cuencana they in fact belong to Pocamus pepelui, of the stem cladotherian superorder Zatheria, probably "peramuran". As such, the stem Cladotheria record from the Early Cretaceous of the Iberian Peninsula is composed of two dryolestids (Crusafontia amoae and Crusafontia cuencana) and one zatherian (Pocamus pepelui).
机译:十字花科植物十一月(Dryolestida,茎克拉德)以El Castellar岩层(西班牙加尔维)的末胡特里夫基底巴雷米亚(早白垩世)的两个孤立的上臼齿(M4或M5和M6或M7)为代表。臼齿有一个深的外弯肌,一个独特的后圆锥形,一个连续的后圆锥形,和一个前舌旁放置的副圆锥形。它们与其他属的臼齿不同,它们的体型更大,它们的体形较大,副锥的舌尖斜度更大,它们的对称外观以及在咬合点上的深外弯肌以及井开发的metacone。对先前归因于Crusafontia cuencana的三颗孤立牙齿的修订表明,它们实际上并非属于Crusafontia cuencana的上前磨牙,而是属于茎锁骨科超人Zatheria的Pocamus pepelui,可能是“ peramuran”。因此,伊比利亚半岛早白垩纪的克拉德索尔茎记录由两种石ol科动物(Crusafontia amoae和Crusafontia cuencana)和一个z草科(Pocamus pepelui)组成。

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