The dental system of †Kazanichthys viatkensis (Actinopterygii, Acrolepididae) from the middle Permian of European Russia: palaeobiological and palaeoecological inferences

IF 2.3 2区 地球科学 Q1 PALEONTOLOGY
A. Bakaev, Z. Johanson, A. Leblanc
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引用次数: 0

Abstract

Among ray‐finned fishes (Actinopterygii), the crushing, durophagous feeding strategy first evolved in the early Carboniferous period, with the †Eurynotiformes possessing dentitions with single layers of partially to fully fused blunt teeth. In the †‘Platysomidae’ (Permian), a new form of crushing dentition evolved (phyllodonty), in which multiple layers of superimposed crushing teeth developed intraosseously, within the jaw. The phyllodont durophagous dentition is also recovered from later‐occurring taxa originating mainly in the Mesozoic, such as the †Bobastraniiformes, the neopterygians †Pycnodontiformes and Ginglymodi, and in the teleost group †Phyllodonta. By comparison, †Kazanichthys viatkensis, an actinopterygian from the middle Permian of European Russia, is characterized by a third, putatively durophagous dentition, with anterior conical teeth and closely packed molariform teeth on the buccal dental plates (a potential similarity with eurynotiforms). Whereas the conical teeth are similar to those of basal actinopterygians, the molariform teeth superficially resemble teeth of some teleosts (Characiformes, Tetraodontiformes), but are unique among known fossil and living Actinopterygii in being crowned by anastomosing, sharp apical ridges. Teeth are ankylosed to the jaw and acrodont in implantation. There is neither evidence of plicidentine, nor cavities corresponding to intraosseous crypts. Most replacement teeth formed extraosseously, differing from the phyllodont dentition, but similar to several more phylogenetically basal actinopterygians. The dental system morphologically resembles recent Sparidae (Teleostei; Perciformes), possibly indicating a similar trophic adaptation. Based on these comparisons and patterns of wear, we propose that †K. viatkensis was a generalist durophagous feeder, with the ability to switch prey types with its unique and complex dentition.
俄罗斯欧洲地区中二叠纪Kazanichthys viatkensis(放线翼目,Acrolepididae)的牙齿系统:古生物学和古生态学推论
在射线鳍鱼类(放射线鳍科)中,咬碎、硬食的捕食策略最早在石炭纪早期进化,Eurynotiformes具有单层部分融合到完全融合的钝齿。在Platysomidae(二叠纪)中,进化出了一种新的破碎齿列(phyllodonty),在颌骨内的骨内发育了多层叠加的破碎齿。在主要起源于中生代的较晚发生的类群中,如†Bobastraniiformes, neopterygians†Pycnodontiformes和Ginglymodi,以及硬骨鱼类群†Phyllodonta中也发现了硬骨鱼的硬食性牙齿。相比之下,来自俄罗斯欧洲地区二叠纪中期的Kazanichthys viatkensis,其特征是具有第三个牙列,推测为硬食性牙列,其牙板上有前锥形牙齿和紧密排列的磨牙状牙齿(可能与eurynotiforms相似)。虽然锥形牙齿与基生放光鳍鱼的牙齿相似,但磨牙状牙齿表面类似于某些硬骨鱼(特指,四齿形目)的牙齿,但在已知的化石和现存放光鳍鱼中是独特的,它们有吻合的尖脊。植牙时,牙齿与下颌和牙尖紧密相连。没有证据表明有外翻,也没有与骨内隐窝相应的空腔。大多数替代牙是在骨外形成的,不同于叶状齿的牙列,但与一些系统发育上更接近的基底放线齿类相似。牙齿系统在形态上类似于最近的无毛蛛科(Teleostei;表现形动物),可能表明类似的营养适应。基于这些比较和磨损模式,我们提出†K。Viatkensis是一种多面手的硬食性捕食者,凭借其独特而复杂的牙齿能够转换猎物类型。
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来源期刊
Papers in Palaeontology
Papers in Palaeontology PALEONTOLOGY-
CiteScore
4.50
自引率
4.30%
发文量
55
期刊介绍: Papers in Palaeontology is the successor to Special Papers in Palaeontology and a journal of the Palaeontological Association (www.palass.org). The journal is devoted to the publication of papers that document the diversity of past life and its distribution in time and space. Papers in Palaeontology is devoted to the publication of papers that document the diversity of past life and its distribution in time and space. As a sister publication to Palaeontology its focus is on descriptive research, including the descriptions of new taxa, systematic revisions of higher taxa, detailed biostratigraphical and biogeographical documentation, and descriptions of floras and faunas from specific localities or regions. Most contributions are expected to be less than 30 pp long but longer contributions will be considered if the material merits it, including single topic parts. The journal publishes a wide variety of papers on palaeontological topics covering: palaeozoology, palaeobotany, systematic studies, palaeoecology, micropalaeontology, palaeobiogeography, functional morphology, stratigraphy, taxonomy, taphonomy, palaeoenvironmental reconstruction, palaeoclimate analysis, biomineralization studies.
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