塞纳特拉
新近纪
生物
犰狳
中新世晚期
属
新生代
古生物学
航程(航空)
甲壳
动物
生态学
甲壳动物
材料科学
构造盆地
复合材料
作者
Daniel Barasoain,Rodrigo L. Tomassini,Sofía I. Quiñones,Laureano R. González Ruiz,Ricardo A. Bonini,Alfredo E. Zurita
标识
DOI:10.1093/zoolinnean/zlae124
摘要
Abstract Within armadillos, two clades are currently recognized: Chlamyphoridae and Dasypodidae. Major evolutionary processes of Chlamyphoridae are linked to the main environmental and climatic events that occurred in South America in the Cenozoic. More precisely, the Euphractinae reached a high diversity concomitant with the cooling period of the Late Miocene–Pliocene. One of the largest euphractines is Macrochorobates, which includes the species M. scalabrinii and M. chapalmalensis, differentiated by minor details on the osteoderms of the dorsal carapace. This genus had a wide distribution, with records in Late Miocene–Pliocene deposits of different regions of Argentina. Here we describe and compare new specimens of M. scalabrinii, which represent the most complete material known so far. Our comparative analysis strongly suggests that M. chapalmalensis represents a junior synonym of M. scalabrinii. This way, the biochron of M. scalabrinii would range from the Late Miocene to the Late Pliocene. Additionally, anatomical comparisons and cladistic analysis show that Macrochorobates and Macroeuphractus (another Late Neogene large euphractine) share some cranial characters, not observable in other armadillos; therefore, we propose that Macrochorobates scalabrinii could have had intermediate carnivorous diets between more generalist taxa such as Euphractus and the specialized carnivory proposed for Macroeuphractus.
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