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首页> 外文期刊>Journal of South American earth sciences >Presence of the extinct sawfish, Onchosaurus (Neoselachii, Sclerorhynchiformes) in the Late Cretaceous of Peru with a review of the genus
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Presence of the extinct sawfish, Onchosaurus (Neoselachii, Sclerorhynchiformes) in the Late Cretaceous of Peru with a review of the genus

机译:秘鲁白垩纪晚期灭绝的锯fish,甲龙(Neoselachii,Sclelorhynchiformes)的存在及一个属的回顾

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摘要

In this paper we report the first Peruvian record of the extinct giant sclerorhynchiform sawfish, Onchosaurus pharao. The single specimen consists of a characteristic rostral spine, which was recovered from nodular limestone in the West-Peruvian Trough of the central Andean Basin, close to the city of Cajamarca. The fossil-bearing strata belong to the lower part of the Celendin Formation, which is of middle-late Coniacian age. This specimen is the first Coniacian record of Onchosaurus pharao and constitutes the third known record of this sclerorhynchiform taxon in South America filling previous gaps in the stratigraphic and geographic distribution of this species. A review of the distribution patterns of both species assigned to Onchosaurus reveals that the genus originated in circum-Equatorial, tropical waters and subsequently dispersed along different pathways south- and northwards. Based on its palaeogeographic distribution and the size of the rostral spines, both Onchosaurus spp. are considered large, bottom-dwelling sclerorhynchiforms primarily inhabiting shallow marine, near-coastal environments. The palaeogeographic distribution nevertheless indicates that they were powerful swimmers and able to cross wide, open marine distances. The reason for the disappearance of Onchosaurus in the Campanian remains unknown. In the early Maastrichtian, Dalpiazia seemingly replaced Onchosaurus ecologically. However, we hypothesize that the different histologies of rostral spines of Onchosaurus and Dalpiazia are of minor taxonomic importance. Dalpiazia thus might represent a derived onchosaur rather than a distinct taxon.
机译:在本文中,我们报告了秘鲁第一个灭绝的巨型巩膜纲锯鱼Onchosaurus pharao记录。单个标本由特征性的表层脊柱组成,该表层脊柱是从安第斯盆地中部西秘鲁海槽中靠近卡哈马卡市的球状石灰岩中回收的。含化石的地层属于塞伦丁组的下部,属于中晚期柯尼西亚时代。该标本是Onchosaurus pharao的第一个科尼亚纪记录,构成了南美该巩膜纲类群的第三个已知记录,填补了该物种地层和地理分布的先前空白。对分配给甲龙的两个物种的分布模式的回顾表明,该属起源于环赤道热带水域,并随后沿不同的路径向南和向北分散。根据其古地理分布和鸟嘴棘的大小,这两种Onchosaurus spp。被认为是大型的,底部居住的巩膜纲,主要栖息在浅海,近沿海环境中。尽管如此,古地理分布表明他们是强有力的游泳者,能够跨越广阔的海洋距离。坎帕尼亚人甲龙消失的原因仍然未知。在早期的马斯特里赫特时代,达尔皮亚兹岛似乎在生态上取代了甲龙。然而,我们假设甲龙和达皮亚古猿的喙棘的不同组织学在分类学上的重要性不大。因此,Dalpiazia可能代表衍生的甲龙而不是独特的分类群。

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