古生代全头鱼属(软骨鱼目,蜗齿目)和从牙齿到牙板的过渡

IF 0.5 4区 地球科学 Q4 GEOLOGY Scottish Journal of Geology Pub Date : 2022-06-22 DOI:10.1144/sjg2021-016
W. Itano
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引用次数: 0

摘要

球粒陨石Psephodus Morris和Roberts的遗骸,1862年,主要由孤立的齿板组成。该属的范围从晚泥盆纪(法门阶)到晚密西西比纪(谢尔普霍夫阶)。最完整的标本是模式种P.magnus的一组部分铰接的牙齿和齿板,来自苏格兰拉纳克郡东基尔布赖德的早期谢尔普霍夫阶。在东基尔布赖德标本的Lophodus样和Helodus样牙齿的基部边缘存在一排微小的节。这将这些牙齿与典型的类洛弗杜斯和类赫洛杜斯的牙齿区分开来。与单纯Helodus一样,Psephodus的一些标本显示出不同程度的牙齿从同一个唇口方向的锉刀融合到齿板中。然而,与单纯赫洛多斯不同的是,一些Psephodus标本显示了近距离分离的齿板融合成一个更大的齿板,每个齿板代表一个融合的齿锉。Psephodus跨越泥盆纪-石炭纪边界,可能是其他密西西比全头动物的祖先,如Cochliodus或Chondrechelys,其齿列由几个只有很少或没有单独牙齿的齿板组成。阿加西斯的艺术家丁克尔的一幅未发表的水彩画描绘了五个齿板,可以被指定为P.magnus的同型。指定了一个细纹Psephodus crenulatus的选择型。
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The Palaeozoic genus Psephodus (Chondrichthyes, Cochliodontiformes) and the transition from teeth to tooth plates in holocephalians
Remains of the chondrichthyan Psephodus Morris and Roberts, 1862, consist mainly of isolated tooth plates. The genus has a range from Late Devonian (Famennian) to Late Mississippian (Serpukhovian). The most complete specimen is a partially articulated set of teeth and tooth plates of the type species, P. magnus, from the early Serpukhovian of East Kilbride, Lanarkshire, Scotland. A row of minute nodes is present along the basal margins of the Lophodus-like and Helodus-like teeth of the East Kilbride specimen. This distinguishes these teeth from typical Lophodus-like and Helodus-like teeth. As in Helodus simplex, some specimens of Psephodus display varying degrees of fusion of teeth from the same labiolingually oriented file into tooth plates. However, unlike Helodus simplex, some specimens of Psephodus display fusion of mesiodistally separated tooth plates, each representing a fused tooth file, into a larger tooth plate. Psephodus, which crosses the Devonian-Carboniferous boundary, may be ancestral to other Mississippian holocephalians, such as Cochliodus or Chondrenchelys, in which dentitions consist of a few tooth plates with only few, or no, separate teeth. An unpublished watercolour by Agassiz's artist Dinkel depicts five tooth plates, which can be designated as syntypes of P. magnus. A lectotype for Psephodus crenulatus is designated.
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来源期刊
Scottish Journal of Geology
Scottish Journal of Geology 地学-地质学
CiteScore
1.70
自引率
0.00%
发文量
10
审稿时长
>12 weeks
期刊介绍: Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.
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