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A new archaic homodont toothed cetacean (Mammalia, Cetacea, Odontoceti) from the early Miocene of Peru

机译:秘鲁中新世早期的一种新的古胡齿齿鲸科动物(哺乳动物,鲸科动物,Odontoceti)

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摘要

Apart from a few exceptions, extant odontocetes (toothed cetaceans) exhibit a roughly homodont dentition. The transition from basilosaurid-like double-rooted cheek teeth with accessory denticles to single-rooted conical teeth occurred during the late Oligocene-early Miocene. At that time, several clades of now extinct, homodont and predominantly long-snouted odontocetes appeared in the fossil record. Among them, members of the genera Argyrocetus Lydekker, 1893 and Macrodelphinus Wilson, 1935, from the early Miocene of the Northeast Pacific and Argentina, were tentatively attributed to the family Eurhinodelphinidae. However, due to the fragmentary state of the specimens, unambiguous apomorphies of the family could not be detected. Based on two well-preserved skulls with associated mandibular elements, discovered in early Miocene layers of the Chilcatay Formation (Pisco Basin, Peru), we report on a new genus and species of long-snouted homodont odontocete, Chilcacetus cavirhinus n. gen., n. sp. Characterized by, among others, the presence of alveoli on the anterior premaxillary portion of the rostrum, the lack of a lateral groove on the rostrum, anterodorsally elevated nasals, a possibly autapomorphic cavity between nasals and mesethmoid in the posterior wall of the bony nares, a high temporal fossa, and the absence of ankylosis along the mandibular symphysis, C. cavirhinus n. gen., n. sp. does not fit in any of the known odontocete families, but shares several morphological features with Argyrocetus spp. and Macrodelphinus. Our phylogenetic analysis, based on 77 characters for 35 odontocete taxa, suggests the existence of an early Miocene Eastern Pacific long-snouted homodont odontocete clade (with an hypothetical South Atlantic member, the poorly known Argyrocetus patagonicus Lydekker, 1893), distinct from the only superficially similar eoplatanistids and eurhinodelphinids. Furthermore, our consensus tree indicates an early branching of this new clade compared to other homodont odontocete lineages. Unfortunately, the results of the cladistic analysis presented here are not well supported; a reappraisal of Argyrocetus and Macrodelphinus is needed to more clearly define the new clade and bolster its phylogentic position.
机译:除了少数例外,现存的齿形齿(齿状鲸类)显示出大致的齿齿状。在晚渐新世-中新世早期,发生了从具龙的类龙牙似的双根颊齿到单根圆锥形牙齿的过渡。当时,化石记录中出现了几条现已灭绝的,纯齿的和主要是长鼻齿的齿形牙齿。其中,来自东北太平洋和阿根廷中新世早期的Argyrocetus Lydekker属和1893年的Macrodelphinus Wilson属暂时被归因于Eurhinodelphinidae科。但是,由于标本的碎片状态,无法检测到该家族的明确无性。基于在奇尔卡塔伊组(秘鲁皮斯科盆地)的中新世早期层中发现的两个保存完好的具有相关下颌骨元素的头骨,我们报道了一种长鼻homo齿牙形石的新属和种,即奇尔卡西特斯cavirhinus n。 gen。,n。 sp。其特征是,在上颌骨前前部分上存在肺泡,在上颌骨上没有侧向凹槽,鼻腔前部升高,鼻腔后壁与鼻窦之间的可能是类异形腔,颞窝高,沿下颌骨联合体没有强直,C。cavirhinus。 gen。,n。 sp。不适合于任何已知的牙形突科,但与Argyrocetus spp具有一些形态特征。和Macrodelphinus。我们的系统发育分析基于35个齿状齿类群的77个字符,表明存在早中新世东太平洋的长齿型齿状齿形进化枝(有一个假设的南大西洋成员,鲜为人知的Argyrocetus patagonicus Lydekker,1893年),与唯一表面相似的eoplatanistids和eurhinodelphinids。此外,我们的共识树表明该新进化枝与其他同齿牙本质谱系相比早分支。不幸的是,这里介绍的分类分析的结果没有得到很好的支持。需要重新评估Argyrocetus和Macrodelphinus,以更清楚地定义新进化枝并增强其系统发育位置。

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