School of Earth Sciences, University of Bristol, Life Sciences Building, 24 Tyndall Avenue, Bristol BS8 1TQ, UK; School of Biological Sciences, University of Bristol, Life Sciences Building, 24 Tyndall Avenue, Bristol BS8 1TQ, UK.
School of Earth Sciences, University of Bristol, Life Sciences Building, 24 Tyndall Avenue, Bristol BS8 1TQ, UK; Department of Geology and Geophysics, Yale University, 210 Whitney Ave., New Haven, Connecticut 06511, USA.
Curr Biol. 2019 Mar 4;29(5):881-888.e1. doi: 10.1016/j.cub.2019.01.052. Epub 2019 Feb 21.
Amiskwia sagittiformis Walcott 1911 is an iconic soft-bodied taxon from the Burgess Shale [1-3]. It was originally interpreted as a chaetognath [1], but it was later interpreted as a pelagic nemertean [2] or considered of uncertain affinity [3]. Part of this ambiguity is due to direct comparisons with members of the crown groups of extant phyla [4] and a lack of clarity regarding the systematic position of chaetognaths, which would allow for assessing character polarity in the phylum with respect to outgroups. Here, we show that Amiskwia preserves a bilaterally arranged set of head structures visible in relief and high reflectivity. These structures are best interpreted as jaws situated within an expanded pharyngeal complex. Morphological studies have highlighted a likely homology between bilateral and chitinous jaw elements in gnathiferans and chaetognaths [5], which is congruent with a shared unique Hox gene that suggests a close relationship between Gnathifera and Chaetognatha [6]. Molecular phylogenetic studies have recently found gnathiferans to be a deep branch of Spiralia and Chaetognaths either a sister group to Spiralia [7] or forming a clade with gnathiferans [6, 8]. Our phylogenetic analyses render Gnathifera paraphyletic with respect to Chaetognatha, and we therefore suggest that Amiskwia is best interpreted as a stem chaetognath, but crown gnathiferan.
Amiskwia sagittiformis Walcott 1911 是伯吉斯页岩中具有标志性的软体动物化石[1-3]。它最初被解释为长尾目生物[1],但后来被解释为漂浮纽形动物[2]或被认为亲缘关系不确定[3]。这种模糊性部分是由于与现存门的冠群成员进行了直接比较[4],以及长尾目动物的系统位置不明确,这使得人们无法评估该门相对于外群的特征极性。在这里,我们表明 Amiskwia 保存了一套双侧排列的头部结构,这些结构在浮雕和高反射率中可见。这些结构最适合解释为位于扩展咽复杂结构内的颚。形态学研究强调了在有颚类和长尾目动物中双侧和几丁质颚元素之间可能存在同源性[5],这与一个独特的 Hox 基因一致,表明有颚类和长尾目动物之间存在密切关系[6]。最近的分子系统发育研究发现,有颚类是螺旋动物和长尾目动物的一个深分支[7],或者与有颚类形成一个分支[6,8]。我们的系统发育分析表明,有颚类相对于长尾目动物是并系的,因此我们建议将 Amiskwia 最好解释为一个原始的长尾目动物,但冠有颚类。