Castro Mariela C, Goin Francisco J, Ortiz-Jaureguizar Edgardo, Vieytes E Carolina, Tsukui Kaori, Ramezani Jahandar, Batezelli Alessandro, Marsola Júlio C A, Langer Max C
Laboratório de Paleontologia, FFCLRP, Universidade de São Paulo, Ribeirão Preto-SP 14040-901, Brazil.
División Paleontología Vertebrados, Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque S/N°, B1900FWA La Plata, Argentina.
R Soc Open Sci. 2018 May 30;5(5):180482. doi: 10.1098/rsos.180482. eCollection 2018 May.
In the last three decades, records of tribosphenidan mammals from India, continental Africa, Madagascar and South America have challenged the notion of a strictly Laurasian distribution of the group during the Cretaceous. Here, we describe a lower premolar from the Late Cretaceous Adamantina Formation, São Paulo State, Brazil. It differs from all known fossil mammals, except for a putative eutherian from the same geologic unity and , from the Maastrichtian of India. The incompleteness of the material precludes narrowing down its taxonomic attribution further than Tribosphenida, but it is larger than most coeval mammals and shows a thin layer of parallel crystallite enamel. The new taxon helps filling two major gaps in the fossil record: the paucity of Mesozoic mammals in more northern parts of South America and of tribosphenidans in the Cretaceous of that continent. In addition, high-precision U-Pb geochronology provided a post-Turonian maximal age (≤87.8 Ma) for the type stratum, which is overlain by the dinosaur-bearing Marília Formation, constraining the age of the Adamantina Formation at the site to late Coniacian-late Maastrichtian. This represents the first radioisotopic age for the Bauru Group, a key stratigraphic unit for the study of Cretaceous tetrapods in Gondwana.
在过去三十年里,来自印度、非洲大陆、马达加斯加和南美洲的三楔齿兽类哺乳动物化石记录,对该类群在白垩纪严格局限于劳亚大陆分布的观点提出了挑战。在此,我们描述了一枚来自巴西圣保罗州晚白垩世阿达曼蒂纳组的下前磨牙。它与所有已知的化石哺乳动物不同,除了来自同一地质单元以及印度马斯特里赫特阶的一种假定真兽类。材料的不完整性使得我们无法将其分类归属进一步限定在三楔齿兽目之外,但它比大多数同期哺乳动物更大,并且具有一层薄的平行微晶釉质。这个新分类单元有助于填补化石记录中的两个主要空白:南美洲更北部地区中生代哺乳动物化石的匮乏,以及该大陆白垩纪三楔齿兽类化石的缺失。此外,高精度铀铅年代测定法为该类型地层提供了一个晚土伦阶最大年龄(≤8780万年),该地层之上覆盖着含恐龙的马里利亚组,从而将该地点阿达曼蒂纳组的年龄限制在科尼亚克晚期至马斯特里赫特晚期。这代表了包鲁群的首个放射性同位素年龄,包鲁群是冈瓦纳白垩纪四足动物研究的关键地层单元。