奥陶系和志留系Atrypida目成员的系统发育

IF 2.2 2区 地球科学 Q3 EVOLUTIONARY BIOLOGY
B. Gudveig Baarli, Bing Huang, L. Maroja
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引用次数: 1

摘要

腕足动物属于腕足目,起源于中奥陶世,在泥盆纪晚期灭绝。对这一群体进行的进化研究很少。在这里,我们研究它们在志留纪的早期演化。本文对该目所有早期类群的41个性状和70个属进行了系统发育分析。所分析的化石属的地层记录与我们从简约分析中恢复的系统发育非常一致。除了Atrypinae, Idiospirinae和Septatrypidae外,大多数目前公认的亚科和科都可以在分支中确定。这就保证了前者的细分和后两者的重新定义。重新定义了Atrypinae亚科,并分离出一个新的Atrypidae亚科,即Protatrypinae。追踪整个树的特征进化表明,钙化的螺旋体和jugum或jugal过程是所有atrypia成员的特征,除了最基础的分支,Cyclospiridae,它没有钙化的jugum。肋是一种同质性的特征,发生在整个树的许多枝上。darriwilliam时代到Sandbian时代代表了一个快速进化的时代,在这个时代,在原始形态中看到的大多数新的自异形都在进化。该期段是大奥陶纪生物多样化事件(GOBE)的第一个主要阶段。坚固的牙齿、螺旋纹的背向、精致的纹饰和褶边在卡天纪晚期到志留纪早期进化。在最近的Katian进化枝上看到的实心牙齿可能是一个类似的特征。地层树显示了晚奥陶世大灭绝(LOME)和一个可能发生在Aeronian末的事件。这棵树支持了长期以来的假设,即Plectatrypinae是从spirigerinae进化而来的。这进一步表明Tuvaella属可能被归入戴维森总科。同样,重新定义的Atrypinae是Lissatrypidae的姊妹类群,也是系统发育树上的衍生类群。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Phylogeny of the Ordovician and Silurian members of the order Atrypida
Brachiopods belonging to order Atrypida originated in the Middle Ordovician and went extinct in the Late Devonian. Few cladistic studies have been undertaken for this group. Here we investigate their early evolution through Silurian time. We present a parsimony-based phylogenetic analysis of 41 characters and 70 genera representing all the early taxonomic groups within the order. The stratigraphical record of the fossil genera analysed strongly aligns with the phylogeny recovered from our parsimony analysis. Most currently recognized subfamilies and families may be identified within clades, except for the Atrypinae, Idiospirinae, and the Septatrypidae. This warrants subdivision of the former and redefinition of the latter two. The subfamily Atrypinae is redefined, and a new subfamily of the Atrypidae, the Protatrypinae, is split off. Tracing character evolution across the tree indicates that the calcified spiralia and a jugum or jugal processes characterize all members of the Atrypida, except the most basal clade, the Cyclospiridae, which lacks a calcified jugum. Ribs are a homoplasious character, occurring in numerous clades throughout the tree. Darriwillian through Sandbian ages represent times with rapid evolution when most new autapomorphies seen in the atrypides evolved. This interval is the first major part of the Great Ordovician Biodiversification Event (GOBE). Solid teeth, dorsal direction of spiralia, elaborate ornamentation, and frills evolved in the latest Katian into early Silurian time. Solid teeth seen in distantly related clades from latest Katian onwards may be an analogous feature. The Late Ordovician Mass Extinction (LOME) is indicated in the stratigraphical tree together with a possible event at the end of the Aeronian. The tree supports the long-held assumptions that the Plectatrypinae evolved from the Spirigerininae. It further suggests that the genus Tuvaella may be included with the Davidsonioidea. Likewise, the redefined Atrypinae is a sister group of the Lissatrypidae and a derived group in the phylogenetic tree.
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来源期刊
CiteScore
5.30
自引率
7.70%
发文量
31
审稿时长
>12 weeks
期刊介绍: The Journal of Systematic Palaeontology publishes papers that provide novel and impactful results in phylogenetics and systematics and that use these results in ways that significantly advance rigorous analyses of palaeogeography, palaeobiology, functional morphology, palaeoecology or biostratigraphy. Papers dealing with theoretical issues or molecular phylogenetics are also considered if they are of relevance to palaeo-systematists. Contributions that include substantial anatomical descriptions, descriptions of new taxa or taxonomic revisions are welcome, but must also include a substantial systematics component, such as a new phylogeny or a revised higher-level classification. Papers dealing primarily with alpha-taxonomic descriptions, the presentation of new faunal/floristic records or minor revisions to species- or genus-level classifications do not fall within the remit of the journal.
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