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首页> 外文期刊>Journal of Systematic Palaeontology >A new salamandrid amphibian from the Middle Miocene of Hungary and its phylogenetic relationships
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A new salamandrid amphibian from the Middle Miocene of Hungary and its phylogenetic relationships

机译:匈牙利中新世中新的sal虫两栖动物及其系统发育关系

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摘要

A fossil salamandrid, Carpathotriton matraensis gen. et sp. nov., from the Astaracian (Middle Miocene, MN 7) localities of Matraszolos 1 and 2 (Northern Hungary, Nograd County) is described. Within newts, Carpathotriton is diagnosed by a combination of primitive and derived characters including a premaxillary-frontal contact, a well-developed fronto-squamosal arch, low supraorbital crest and weak sculpture on the frontal surface. Referred material comprises abundant cranial, vertebral and appendicular skeletal elements that exhibit limited morphological variation of mainly allometric nature. The dentary of Carpathotriton is unique in displaying a prominent dental parapet with an extremely short tooth row and a relatively long toothless posterior ramus. The quadrate is provided with an extuberant anterolateral process that may be a homoplasy with some members of the Tylototriton group. Trunk vertebrae of Carpathotriton have extremely high neural spines with some enlargement on their dorsal margin similar to some Recent Eastern Asiatic salaman-drids and the Oligocene newt Archaeotriton. The available fossil record suggests that Carpathotriton never extended into the western Paratethys area, but might have had a wider distribution in the central and eastern Paratethys region, surviving up to late Astaracian times (MN 7 + 8). Taphonomic setting of the Matraszolos localities indicates that Carpathotriton matraensis was closely associated with aquatic environments.
机译:化石sal,carpathotriton matraensis gen。等。参考文献11,描述了来自Matraszolos 1和2(匈牙利北部,诺格拉德县)的阿斯塔拉契人(中新世中期,MN 7)。在new中,通过结合原始和衍生特征(包括上颌前-额叶接触,发达的额额-方弓,眶上and低和额叶表面较弱的雕塑)诊断出卡氏弧菌。所指材料包括丰富的颅骨,椎骨和阑尾骨骼元素,这些元素表现出有限的形态学变化,主要是异速生长。 Carpathotriton的牙齿独特之处在于显示出突出的护齿栏,其齿排非常短,后牙无齿相对较长。该方体具有突出的前外侧突,可能与Tylototriton组的某些成员呈同型。 Carpathotriton的主干椎骨具有极高的神经棘,其背缘有些增大,类似于最近的一些东亚地区的salaman-drids和渐新世的Arch Archaeotriton。现有的化石记录表明,喀尔巴阡藻从未延伸到西部的帕拉特斯地区,但可能在帕拉特斯的中部和东部地区分布更广,幸存下来直到阿斯塔拉西亚时代(MN 7 + 8)。 Matraszolos地点的音速设置表明,喀尔巴阡藻与水生环境密切相关。

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