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成对的鳍和体节侧缘的演化。

Evolution of paired fins and the lateral somitic frontier.

机构信息

Department of Palaeontology, Natural History Museum, Cromwell Road, London, United Kingdom.

出版信息

J Exp Zool B Mol Dev Evol. 2010 Jul 15;314(5):347-52. doi: 10.1002/jez.b.21343.

Abstract

Recent research on the evolutionary origins of the paired fins (pectoral and pelvic, evolving into the four tetrapod limbs) has focused on genetic, developmental, and fossil evidence. However, a combined synthesis of this evidence has largely been lacking. In living animals, identification of dorsal and ventrolateral zones of fin-producing competence, the distinction between primaxial and abaxial regions separated by the lateral somitic frontier, and the recognition that fin developmental mechanisms could have been co-opted from unpaired to paired fins can be used to evaluate vertebrate fin evolution, including fossil forms. These fossil taxa dominate early vertebrate history and possess an unusually wide variety of fin or fin-like structures; establishing homologies with the paired fins of jawed vertebrates has been challenging, in part owing to the absence of supporting girdles in most jawless vertebrates. An evolutionary scenario is proposed where these fin-like structures develop from somites, in the same manner as dorsal, unpaired fins. Girdles and the paired fins of osteostracans and jawed vertebrates develop from lateral plate mesoderm when the lateral somitic frontier and the abaxial region of the body evolve.

摘要

最近对成对鳍(胸鳍和腹鳍,进化为四肢)的进化起源的研究集中在遗传、发育和化石证据上。然而,这种证据的综合综合在很大程度上是缺乏的。在现存动物中,识别鳍产生能力的背侧和腹外侧区、由侧体节边界隔开的原轴和背轴区域之间的区别,以及认识到鳍发育机制可能已经从不成对鳍被共同进化到成对鳍,可以用于评估包括化石形式在内的脊椎动物鳍的进化。这些化石类群主导着早期脊椎动物的历史,并拥有异常广泛的各种鳍或鳍状结构;与有颌脊椎动物的成对鳍建立同源关系具有挑战性,部分原因是大多数无颌脊椎动物缺乏支持带。提出了一个进化情景,其中这些类似鳍的结构从体节发育而来,与背侧、不成对的鳍一样。当体节边界和身体的背轴区域进化时,硬骨鱼类和有颌脊椎动物的带和成对鳍由侧板中胚层发育而来。

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