Developmental osteology of Ictalurus punctatus and Noturus gyrinus (Siluriformes: Ictaluridae) with a discussion of siluriform bone homologies

IF 2.4 2区 生物学 Q1 ZOOLOGY
Kole M. Kubicek
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引用次数: 3

Abstract

Abstract The skeleton of Siluriformes is characterized by several autapomorphies, including secondary absence, extreme modification, and purported fusion of several ossifications. Although well documented in adults, information on skeletal development in catfishes is relatively sparse and typically focused on particular regions of the skeleton (e.g., Weberian apparatus). To further our understanding of the siluriform skeleton, I document the development of the entire skeleton in two ictalurid species, Ictalurus punctatus (channel catfish) and Noturus gyrinus (tadpole madtom) from five days pre-hatch to adult. I reexamine the homologies of bones previously hypothesized to represent compound elements in catfishes as well as an additional element only known to occur in some ictalurids. Development of the skeleton is complete in I. punctatus at 22.4 mm SL and almost complete in N. gyrinus (except dorsal- and anal-fin distal radials) at 14.1 mm SL. No signs of ontogenetic fusion were observed in any of the purported compound elements. Previous hypotheses of the homology of these elements and of additional ossifications are reviewed in light of developmental information obtained herein. No dermal parietal component is present at any stage in the so-called parieto-supraoccipital. The bone is the supraoccipital which ossifies from two lateral centers of ossification which later fuse, rather than from a median center. The ‘posttemporo-supracleithrum’ originates from a single center of ossification and represents the supracleithrum. The posttemporal is present in ictalurids and many other catfishes as a canal-bearing bone between the supracleithrum and the pterotic, a bone sometimes identified as the extrascapular. The extrascapular is missing in catfishes. Ictalurids have an additional dermal bone above the posttemporal, which is either an independently ossifying fragment of the posttemporal or a neoformation restricted to some members of this family. The single chondral bone of the pectoral girdle originates from a single center of ossification that represents the coracoid. The scapula is missing in catfishes. Dorsal-fin distal radial 2 is absent in catfishes and the foramen of dorsal-fin spine 2 is formed from modifications to the base of the fin-ray itself. Unlike loricarioid catfishes, the urohyal of ictalurids originates solely as an ossification of the sternohyoideus tendons. The anteriormost infraorbital element ossifies from a single center of ossification around the infraorbital sensory canal and represents the lacrimal. The antorbital is missing in catfishes. Finally, skeletal development of I. punctatus is compared to that available for other otophysans, including the cypriniforms Danio rerio and Enteromius holotaenia and the characiform Salminus brasiliensis.
斑尾鹬和灰尾鹬的发育骨学研究(鲇形目:尾鹬科)——兼论尾鹬类骨同源性
摘要志留形目的骨骼具有几种自变形特征,包括次生缺失、极端修饰和几种骨化的融合。尽管在成年鱼身上有充分的记录,但关于鲶鱼骨骼发育的信息相对较少,通常集中在骨骼的特定区域(例如韦伯氏器)。为了进一步加深我们对siluriform骨骼的理解,我记录了两种ictalulid物种的整个骨骼从孵化前五天到成年的发育过程,这两种物种分别是斑点伊卡龙(海峡鲶鱼)和灰尾蟾蜍(蝌蚪)。我重新检查了以前假设代表鲶鱼中复合元素的骨骼同源性,以及一种仅出现在某些黄疸中的额外元素。在22.4 mm SL的P.punctatus中骨骼发育完全,在14.1 mm SL的N.gyrinus(背鳍和臀鳍远端桡侧除外)中骨骼发育几乎完全。在任何所谓的复合元素中都没有观察到个体发生融合的迹象。根据本文获得的发育信息,回顾了先前关于这些元素同源性和额外骨化的假设。在所谓的顶-枕上区的任何阶段都不存在真皮-顶叶成分。骨是枕上骨,它从两个外侧骨化中心骨化,这些骨化中心后来融合,而不是从中央骨化。“后颞上韧带”起源于一个骨化中心,代表韧带上韧带。颞后棘突作为一种带管的骨存在于棘突上和翼突之间,有时被认为是肩胛骨外。鲶鱼缺少肩胛外肌。Ictalurids在时态后上方有一个额外的真皮骨,它要么是时态后的独立骨化片段,要么是仅限于该家族某些成员的新形成物。胸带的单个软骨骨来源于代表珊瑚礁的单个骨化中心。鲶鱼的肩胛骨不见了。鲶鱼的背鳍远侧桡侧2不存在,并且背鳍棘2的孔是由鳍射线本身的基部的修饰形成的。与懒虫类鲶鱼不同,黄疸的尿透明仅起源于胸骨舌骨肌腱的骨化。最前面的眶下元件从眶下感觉管周围的单个骨化中心骨化,代表泪道。鲶鱼中缺少眶内突。最后,将点状隐尾蠊的骨骼发育与其他耳膜虫的骨骼发育进行了比较,这些耳膜虫包括塞浦路斯型的Danio rerio和Enteromius holotaenia以及特征型的Salminus brasiliensis。
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来源期刊
CiteScore
4.00
自引率
19.00%
发文量
42
审稿时长
>12 weeks
期刊介绍: Research fields covered by VERTEBRATE ZOOLOGY are ta‍xo‍no‍my, mor‍pho‍logy, an‍at‍omy, phy‍lo‍ge‍ny (mo‍le‍cu‍lar and mor‍pho‍lo‍gy-based), hi‍sto‍ri‍cal bio‍geo‍gra‍phy, and pa‍lae‍on‍to‍lo‍gy of ver‍te‍bra‍tes.
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