首页> 外文期刊>Journal of Mammalian Evolution >Protungulatum, Confirmed Cretaceous Occurrence of an Otherwise Paleocene Eutherian (Placental?) Mammal
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Protungulatum, Confirmed Cretaceous Occurrence of an Otherwise Paleocene Eutherian (Placental?) Mammal

机译:Protungulatum,已确认是白垩纪的古新世Eutherian(胎盘?)哺乳动物

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Neither pre-Cenozoic crown eutherian mammals (placentals) nor archaic ungulates ("condylarths") are known with certainty based on the fossil record. Herein we report a new species of the Paleocene archaic ungulate ("condylarth") Protungulatum from undisputed Late Cretaceous aged rocks in Montana USA based on an isolated last upper premolar, indicating rare representatives of these common early Tertiary mammals appeared in North America a minimum of 300 k years before the extinction of non-avian dinosaurs. The other 1200 mammal specimens from the locality are characteristic Late Cretaceous taxa. This discovery overturns the current hypothesis that archaic ungulates did not appear in North America until after the Cretaceous/Tertiary (K/T) boundary and also suggests that other reports of North American Late Cretaceous archaic ungulates may be correct. Recent studies, including ours, cannot determine whether Protungulatum does or does not belong to the crown clade Placentalia.
机译:基于化石记录,既不确定前新生代冠伊瑟尔哺乳动物(胎盘)也不是古有蹄类动物(“ con”)。本文中,我们根据一个孤立的最后上前磨牙,报道了美国蒙大拿州无争议的晚白垩纪老岩石中的新世古有蹄类动物(“ con”)原毛虫,这表明这些常见的第三纪哺乳动物的稀有代表在北美最少出现了。非禽类恐龙灭绝前的30万年。该地区的其他1200个哺乳动物标本是晚白垩世特色类群。这一发现推翻了目前的假设,即有蹄类有蹄类动物直到白垩纪/第三纪(K / T)边界之后才出现在北美,并且也表明北美晚白垩纪有蹄类有蹄类动物的其他报道可能是正确的。最近的研究,包括我们的研究,无法确定Protungulatum是否属于或不属于冠部植物Placentalia。

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