Kay R F, Johnson D, Meldrum D J
Department of Biological Anthropology and Anatomy, Duke University Medical Center, Durham, North Carolina 27710, USA.
Am J Primatol. 1998;45(4):317-36. doi: 10.1002/(SICI)1098-2345(1998)45:4<317::AID-AJP1>3.0.CO;2-Z.
We report here a new fossil primate from the middle Miocene of Argentina. The material consists of isolated teeth, mandibular fragments, and a talus. The fossils were collected in the Collón Cura formation at Cañadón del Tordillo in Neuquén Province. An age of 15.71 +/- 0.07 Ma has been reported for the Pilcaniyeu Ignimbrite, which lies just below the paleosols in which the fossils were found. This material is thus the youngest occurrence of fossil primates in Argentina (hitherto documented in the Santacrucian and older land mammal ages) but still is older than the middle Miocene platyrrhine primates from La Venta, Colombia, in particular the pitheciins Nuciruptor and Cebupithecia. The material is recognized as a new genus and species of Pitheciinae, Propithecia neuquenensis. The mesiodistally compressed, high-crowned incisors are specialized and similar to species in the tribe Pithecini and to the nonpitheciin Soriacebus (early Miocene, Patagonia). We rule out a phylogenetic relationship to the latter because of differences in molar morphology. Propithecia does, however, fit well into the pattern of pitheciin evolution, being more derived than the middle Miocene pitheciin Nuciruptor but not as much as another middle Miocene taxon, Cebupithecia. As such, this makes Propithecia the oldest taxon that can be confidently placed within this modern New World monkey subfamily. By analogy with the molar structures and diets of extant platyrrhines, Propithecia has a molar structure consistent with a variety of low-fiber diets ranging from fruit and gum to seeds. Its incisors suggest seed-eating in much the same way as extant pitheciins, like Pithecia. The talus resembles that of Callicebus, suggesting arboreal quadrupedal locomotion.
我们在此报告一种来自阿根廷中新世中期的新灵长类化石。材料包括孤立的牙齿、下颌骨碎片和一块距骨。这些化石是在内乌肯省托迪约峡谷的科龙库拉组采集的。据报道,位于发现化石的古土壤层之下的皮尔卡尼约凝灰岩的年龄为1571±7万年。因此,这些材料是阿根廷最年轻的灵长类化石(此前记录于圣克鲁斯期及更古老的陆生哺乳动物时代),但仍比哥伦比亚拉文塔的中新世中期阔鼻猴灵长类动物古老,尤其是僧面猴科的努西鲁ptor和塞布皮西西亚。该材料被确认为僧面猴亚科的一个新属和新种,即内乌肯原僧面猴。近中远中压缩的高冠门齿很特殊,与僧面猴族的物种以及非僧面猴属的索里亚猴(中新世早期,巴塔哥尼亚)相似。由于臼齿形态的差异,我们排除了与后者的系统发育关系。然而,原僧面猴确实很好地符合僧面猴科的进化模式,比中新世中期的僧面猴科努西鲁ptor更进化,但不如另一个中新世中期分类群塞布皮西西亚。因此,这使得原僧面猴成为可以确定归入这个现代新大陆猴亚科的最古老分类群。通过与现存阔鼻猴的臼齿结构和饮食进行类比,原僧面猴的臼齿结构与从水果、树胶到种子等各种低纤维饮食一致。它的门齿表明其以种子为食,方式与现存的僧面猴科动物,如僧面猴属非常相似。距骨类似于伶猴属的距骨,表明其树栖四足运动方式。