Descriptive anatomy and three-dimensional reconstruction of the skull of the tetrapod Eoherpeton watsoni Panchen, 1975 from the Carboniferous of Scotland

IF 0.9 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY Earth and Environmental Science Transactions of the Royal Society of Edinburgh Pub Date : 2024-02-02 DOI:10.1017/s175569102300018x
Laura B. PORRO, Elizabeth MARTIN-SILVERSTONE, Emily J. RAYFIELD
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Abstract

The early tetrapod Eoherpeton watsoni is known from the mid- to late Carboniferous (late Viséan to Namurian, approximately 346–313 Ma) of Scotland. The holotype is made up of a nearly complete but crushed skull with postcranial fragments. The skull anatomy of Eoherpeton was first described over 40 years ago; however, many details are obscured due to deformation of the specimen, including internal bone surfaces, the palatal bones and dentition, and suture morphology. Most phylogenetic analyses place Eoherpeton as an embolomere/reptilomorph on the lineage leading to amniotes, making it a key taxon for understanding anatomical changes during the fish-tetrapod transition. In this paper, we scanned the holotype using micro-computed tomography and digitally prepared the specimen. Based on these data, we present a revised description of the skull, including sutural morphology, that supplements and amends previous descriptions. New anatomical findings include the presence of a previously unknown tooth-bearing vomer, additional information on the shape of the basipterygoid processes and jaw joint, the ability to visualise the full extent of the pterygoid, and confirmation of the arrangement of the coronoid series. We also note the size of the pterygoid flange, which is larger than previously described for Eoherpeton. The pterygoid flange is widely considered to be characteristic of amniotes and serves as the origin of the medial pterygoideus muscle. The differentiation of the adductor muscles and appearance of medial pterygoideus are thought to have permitted a static pressure bite in amniotes, potentially resulting in greater bite forces and increased dietary range. Thus, the presence and extent of the pterygoid flange in Eoherpeton suggests this feature (and associated changes in feeding mechanism) may have evolved earlier than previously thought. Finally, the skull was digitally repaired and retrodeformed to create a new, hypothetical three-dimensional reconstruction of the skull of Eoherpeton.
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苏格兰石炭纪四足动物 Eoherpeton watsoni Panchen(1975 年)头骨的描述性解剖和三维重建
早期四足动物Eoherpeton watsoni产于苏格兰石炭纪中晚期(晚维西期至纳穆里亚期,约346-313Ma)。主模式由一个几乎完整但被压碎的头骨和颅后碎片组成。Eoherpeton 的头骨解剖学在 40 多年前首次被描述;然而,由于标本变形,许多细节都模糊不清,包括内部骨骼表面、腭骨和牙齿以及缝合线形态。大多数系统发育分析都将Eoherpeton作为栓皮动物/爬行动物的一种,位于羊膜动物的前缘,因此它是了解鱼类向四足动物过渡期间解剖结构变化的一个关键类群。在本文中,我们使用微型计算机断层扫描技术扫描了主模式,并对标本进行了数字化处理。基于这些数据,我们对头骨进行了修订描述,包括缝合线形态,对之前的描述进行了补充和修正。新的解剖学发现包括一个以前未知的带齿犁膜的存在、关于翼下突和下颌关节形状的更多信息、翼状突全部范围的可视化能力以及冠状突排列的确认。我们还注意到翼状突缘的大小,它比之前描述的Eoherpeton更大。翼缘被广泛认为是羊膜动物的特征,是翼内侧肌的起源。翼内肌的分化和翼内侧肌的出现被认为允许羊膜动物进行静态压力咬合,从而可能导致更大的咬合力和更大的饮食范围。因此,Eoherpeton 翼缘的存在和范围表明,这一特征(以及相关的进食机制变化)的进化可能早于之前的设想。最后,对头骨进行了数字修复和逆变形,以创建一个新的、假定的 Eoherpeton 头骨三维重建模型。
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来源期刊
CiteScore
2.00
自引率
0.00%
发文量
21
期刊介绍: Earth and Environmental Science Transactions (formerly Transactions of the Royal Society of Edinburgh: Earth Sciences) is a general earth sciences journal publishing a comprehensive selection of substantial peer-reviewed research papers, reviews and short communications of international standard across the broad spectrum of the Earth and its surface environments. The journal prides itself on the quality of its graphics and photographic reproduction. The Editors are keen to encourage interdisciplinary papers and Transactions also publishes occasional special symposia and invited volumes of specific interest. We are currently in the process of digitising the archive of RSE Publications, and the archive of the Transactions, dating back to 1788, will be available from the back issues link on this site.
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