FIRST OCCURRENCE OF THE TEIID LIZARD PENETEIUS FROM THE LATEST CRETACEOUS NAASHOIBITO MEMBER, KIRTLAND FORMATION, SAN JUAN BASIN, NEW MEXICO

T. Williamson, A. Weil
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引用次数: 2

Abstract

Three Teeth from the Naashoibito Member, Kirtland Formation can be referred to the unusual teiid lizard Peneteius . Specimens NMMNH P-36544, P-41223, and P-41224 were recovered by screen washing from NMMNH locality 4005. The locality 4005 has also yielded isolated teeth mammals including the Lancian index taxon Essonodon browni , dinosaurs, crocodilians, and other squamates. P-41223 represents an isolated lower tooth, P-36544 and P-41224 are upper teeth. Isolated osteoderms (P-36543) from locality 4005 may also belong to the same taxon. The Naashoibito Member Peneteius teeth closely resemble the teeth of P. aquilonius , from the late Maastrichtian Hell Creek Formation of Montana. Peneteius is also known from the late Maastrichtian of Montana and the Campanian of Utah and Texas. Peneteius has teeth with a more complicated structure than is known for any other lizard. They are convergent on the molariform cheek teeth of mammals. It was a relatively small lizard with an estimated snout to vent length of about 80 mm and may have had an insectivorous diet. Its mammal-like teeth may have allowed it to orally process food more efficiently than other lizards.
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新墨西哥州圣胡安盆地kirtland组晚白垩世naashoibito段首次发现的尖蜥
来自Kirtland组Naashoibito成员的三颗牙齿可以指的是不寻常的蜥蜴Peneteius。标本NMMNH P-36544、P-41223和P-41224通过筛洗从NMMNH 4005区回收。在4005号地点还发现了独立的有牙齿的哺乳动物,包括兰西亚指数分类单元褐Essonodon browni、恐龙、鳄鱼和其他有鳞动物。P-41223为孤立的下牙,P-36544和P-41224为上牙。来自4005地区的分离骨真皮(P-36543)也可能属于同一分类群。Naashoibito成员Peneteius的牙齿与蒙大拿州马斯特里赫特地狱溪组晚期的P. aquilonius的牙齿非常相似。Peneteius也因蒙大拿州的马斯特里赫特人以及犹他州和德克萨斯州的坎帕尼亚人而闻名。佩涅提乌斯的牙齿结构比其他任何蜥蜴都要复杂。它们会聚在哺乳动物的臼齿状颊齿上。这是一种相对较小的蜥蜴,据估计鼻子到排气口的长度约为80毫米,可能以食虫为食。它像哺乳动物一样的牙齿可能使它比其他蜥蜴更有效地口服食物。
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FIRST OCCURRENCE OF THE TEIID LIZARD PENETEIUS FROM THE LATEST CRETACEOUS NAASHOIBITO MEMBER, KIRTLAND FORMATION, SAN JUAN BASIN, NEW MEXICO THE VERTEBRATE FAUNA OF THE UPPER CRETACEOUS (EARLY CAMPANIAN) MENEFEE FORMATION, NORTHWESTERN NEW MEXICO CAMPANIAN (LATE CRETACEOUS) SELACHIAN FAUNA FROM THE CLIFF HOUSE SANDSTONE NEAR CUBA, NEW MEXICO COMPARATIVE STRATIGRAPHY OF THE DAKOTA SANDSTONE ACROSS THE PICURIS–PECOS FAULT SYSTEM SOUTH OF LAMY, NEW MEXICO: DEFINITIVE EVIDENCE OF LARAMIDE STRIKE-SLIP MAP OF SURFICIAL GEOLOGIC MATERIALS OF NEW MEXICO NEARS COMPLETION
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