Martinelli Agustín G, Ezcurra Martín D, Fiorelli Lucas E, Escobar Juan, Hechenleitner E Martín, von Baczko M Belén, Taborda Jeremías R A, Desojo Julia B
Sección Paleontología de Vertebrados, CONICET-Museo Argentino de Ciencias Naturales "Bernardino Rivadavia", Buenos Aires, Argentina.
Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Buenos Aires, Argentina.
Anat Rec (Hoboken). 2024 Apr;307(4):818-850. doi: 10.1002/ar.25388. Epub 2024 Jan 29.
The Chañares Formation (Ischigualasto-Villa Unión Basin) is worldwide known by its exquisitely preserved fossil record of latest Middle-to-early Late Triassic tetrapods, including erpetosuchids, "rauisuchians," proterochampsids, gracilisuchids, dinosauromorphs, pterosauromorphs, kannemeyeriiform dicynodonts, and traversodontid, chiniquodontid and probainognathid cynodonts, coming from the Tarjadia (bottom) and Massetognathus-Chanaresuchus (top) Assemblage Zones of its lower member. Regarding cynodonts, most of its profuse knowledge comes from the traditional layers discovered by Alfred Romer and his team in the 1960s that are now enclosed in the Massetognathus-Chanaresuchus Assemblage Zone (AZ). In this contribution we focus our study on the probainognathian cynodonts discovered in levels of the Tarjadia Assemblage Zone. We describe a new chiniquodontid cynodont with transversely broad postcanine teeth (Riojanodon nenoi gen. et sp. nov.) which is related to the genus Aleodon. In addition, the specimen CRILAR-Pv 567 previously referred to cf. Aleodon is here described, compared, and included in a phylogenetic analysis. It is considered as an indeterminate Aleodontinae nov., a clade here proposed to included chiniquodontids with transversely broad upper and lower postcanines, by having a cuspidated sectorial labial margin and a lingual platform that is twice broader than a lingual cingulum. Cromptodon mamiferoides, from the Cerro de Las Cabras Formation (Cuyo Basin), was also included in the phylogenetic analysis and recovered as an Aleodontinae. The new cynodont and the record of Aleodontinae indet. reinforce the faunal differentiation between the Tarjadia and Massetognathus-Chanaresuchus Assemblage Zones, in the lower member of the Chañares Formation, and inform on the diverse chiniquodontid clade with both sectorial and transversely broad postcanine teeth.
查尼亚雷斯组(伊斯基瓜拉斯托 - 比利亚联盟盆地)以其保存极为精美的晚三叠世中期至晚期早期四足动物化石记录而闻名于世,这些化石包括鳄蜥类、“劳氏鳄类”、原鳄龙类、纤肢鳄类、恐龙形类、翼龙形类、卡氏兽形二齿兽类,以及来自其下部成员的塔尔贾迪亚(底部)和马塞托鳄 - 查纳雷鳄(顶部)组合带的横齿龙类、奇尼瓜齿兽类和原颌兽类犬齿兽。关于犬齿兽,其大部分丰富知识来自阿尔弗雷德·罗默及其团队在20世纪60年代发现的传统地层,这些地层现在包含在马塞托鳄 - 查纳雷鳄组合带(AZ)中。在本论文中,我们将研究重点放在塔尔贾迪亚组合带地层中发现的原颌兽类犬齿兽上。我们描述了一种新的奇尼瓜齿兽类犬齿兽,其犬齿后齿横向宽阔(内诺里奥哈诺龙,新属新种),它与阿莱奥齿兽属有关。此外,之前被归为阿莱奥齿兽属未定种的标本CRILAR - Pv 567在此进行描述、比较,并纳入系统发育分析。它被认为是一种未定的阿莱奥齿兽亚科新属,这里提出的一个分支,包括上下犬齿后齿横向宽阔的奇尼瓜齿兽类,其特点是有一个具尖的扇形唇缘和一个比舌侧齿带宽两倍的舌侧平台。来自拉斯卡布拉斯山组(库约盆地)的似哺乳克伦普托齿兽也被纳入系统发育分析,并被归为阿莱奥齿兽亚科。这种新的犬齿兽和未定的阿莱奥齿兽亚科记录加强了查尼亚雷斯组下部成员中塔尔贾迪亚组合带和马塞托鳄 - 查纳雷鳄组合带之间的动物群分化,并为具有扇形和横向宽阔犬齿后齿的多样奇尼瓜齿兽类分支提供了信息。