The molecular phylogeny of cirrate octopods (Cephalopoda: Octopoda: Cirrata) using COI and 16S sequences

Tristan Joseph Verhoeff
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Abstract

Contrasting accounts of taxonomic relationships between finned octopod (Octopoda: Cirrata) taxa complicate species identification and generate nomenclatural instability. A comprehensive analysis based on both 16S and COI mitochondrial gene phylogenies is presented, using all currently accepted genera and approximately 27 putative species (including type species for all genera excepting Grimpoteuthis). The goal of this is to stabilise the concepts of genera and families and identify areas needing further systematic research. Four well supported clades are consistent with families Cirroteuthidae, Cirroctopodidae, Grimpoteuthididae, and Opisthoteuthidae across both 16S and COI phylogenies. Family Stauroteuthidae resolves as a sister clade to Cirroteuthidae in some analyses of the COI gene. Combined molecular and morphological similarities suggest that the Cirrata comprises two superfamily level clades, for which Cirroteuthoidea (for Cirroteuthidae and Stauroteuthidae) and Opisthoteuthoidea (for Cirroctopodidae, Grimpoteuthididae, and Opisthoteuthidae) are proposed. The paraphyletic Cirrothauma (Cirroteuthidae) contains at least three species, while within the Grimpoteuthididae, Cryptoteuthis and Luteuthis form clades within a paraphyletic Grimpoteuthis clade, indicating a need for further taxonomic assessment. Intra-clade structure within Opisthoteuthis is better resolved with COI than 16S data. At least one potentially undescribed Opisthoteuthis occurs in the northwestern Pacific, and northeastern Pacific specimens are tentatively referred to O. bruuni, representing a significant range expansion. Lastly, using the dates of fossil stem-Octobrachians and fossil cirrates for approximate calibration, a timetree estimated from COI gene data suggests that these cirrate families and most cirrate genera arose within the Late Cretaceous, possibly as part of the Mesozoic marine revolution, between 124−62 million years ago.
利用 COI 和 16S 序列研究卷须章鱼(头足纲:章鱼目:卷须科)的分子系统发育
关于有鳍章鱼(章鱼纲:Cirrata)类群之间分类学关系的不同说法使物种鉴定变得复杂,并造成命名的不稳定性。本文基于 16S 和 COI 线粒体基因系统发生进行了全面分析,使用了目前公认的所有属和约 27 个推定种(包括除 Grimpoteuthis 以外所有属的模式种)。这样做的目的是稳定属和科的概念,并确定需要进一步系统研究的领域。在 16S 和 COI 系统发育中,Cirroteuthidae 科、Cirroctopodidae 科、Grimpoteuthididae 科和 Opisthoteuthidae 科有四个支持良好的支系。在某些 COI 基因分析中,Stauroteuthidae 科与 Cirroteuthidae 科为姊妹支系。结合分子和形态学的相似性,Cirrata 包括两个超科一级的支系,即 Cirroteuthoidea(Cirroteuthidae 和 Stauroteuthidae)和 Opisthoteuthoidea(Cirroctopodidae、Grimpoteuthididae 和 Opisthoteuthidae)。Cirrothauma(Cirroteuthidae)旁支系至少包含三个物种,而在 Grimpoteuthididae 中,Cryptoteuthis 和 Luteuthis 在 Grimpoteuthis 旁支系中形成支系,这表明需要进一步的分类评估。与 16S 数据相比,COI 数据能更好地解析 Opisthoteuthis 的支系内结构。至少有一种可能未被描述的 Opisthoteuthis 出现在西北太平洋,而东北太平洋的标本被暂定为 O. bruuni,这表明其分布范围显著扩大。最后,利用茎八腕类化石和卷须类化石的年代进行近似校准,根据 COI 基因数据估算的时间树表明,这些卷须科和大多数卷须属出现在晚白垩世,可能是中生代海洋革命的一部分,时间在距今 1.24-62 亿年之间。
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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