A morphological study of vertebral centra in extant species of pike, Esox (Teleostei: Esociformes)

Sinjini Sinha, D. Brinkman, A. Murray
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引用次数: 3

Abstract

            Isolated centra of members of the Esocidae occur frequently in vertebrate microfossil localities of Late Cretaceous and early Paleocene age and are an important source of data on the early history of the family. However, morphological variation along the vertebral column can lead to incorrect interpretations of diversity if they are not recognized. To facilitate the use of centra for interpreting the diversity and distribution of esocids in Cretaceous vertebrate microfossil localities, the variation along the column in five extant species of esocids is described. Comparison with Cretaceous centra referred to the Esocidae allows identification of a series of features in which species of Esox differ from basal members of the family. These include the presence of a mid-ventral groove bordered by a pair of low budges on centra in the anterior end of the column, and antero-lateral processes on the posterior abdominal and anterior caudal centra. These differences provide a basis for recognizing early occurrences of the genus Esox in the fossil record and thus will allow centra to be used to document the timing of origin of the genus.
现存梭子鱼脊椎中心的形态学研究(直骨目:直形目)
在晚白垩世和古新世早期的脊椎动物微化石中,经常发现有棘尾科成员的孤立中心,是研究棘尾科早期历史的重要资料来源。然而,如果不识别,沿着脊柱的形态变化可能导致对多样性的不正确解释。为了便于利用centra解释白垩纪脊椎动物微化石地点的棘虫多样性和分布,本文描述了现存5种棘虫沿柱的变化。将其与白垩纪Esocidae的centra进行比较,可以识别出esocx物种与该家族基础成员不同的一系列特征。这些包括中腹侧沟的存在,其边界是柱前端中央的一对低突起,以及腹后中央和前尾中央的前外侧突。这些差异为在化石记录中认识Esox属的早期出现提供了基础,因此将允许centra用于记录该属的起源时间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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