Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC, United States of America.
Sam Noble Oklahoma Museum of Natural History, University of Oklahoma, Norman, OK, United States of America.
PeerJ. 2024 Oct 31;12:e18169. doi: 10.7717/peerj.18169. eCollection 2024.
The superorder Forcipulatacea is a major clade of sea stars with approximately 400 extant species across three orders (Forcipulatida, Brisingida, Zorocallida). Over the past century, the systematics of Forcipulatacea have undergone multiple revisions by various authors, with some considering numerous families such as Asteriidae, Zoroasteridae, Pedicellasteridae, Stichasteridae, Heliasteridae, Labidiasteridae, and Neomorphasteridae, while others recognized only two families (., Asteriidae and Zoroasteridae). Recent molecular analyses have shown the artificial nature of some of these groupings. Notably, four well-supported clades (Zorocallida, Brisingida, Stichasteridae, and Asteriidae) emerged from a synthesis of morphological and molecular evidence. The majority of extinct forcipulatacean species have been placed in modern families. However, many of these fossil species are in need of revision, especially those species placed within the Asteriidae, the largest of all forcipulatacean families.
In light of recent advancements in forcipulatacean systematics, we comprehensively reassess six well-preserved Jurassic forcipulatacean taxa, including the earliest crown-group members from the Hettangian (∼201.4 Ma), and also describe two new Jurassic genera, gen. nov. and gen. nov. We assembled the largest and most comprehensive phylogenetic matrix for this group, sampling 42 fossil and extant forcipulatacean species for 120 morphological characters. To infer phylogenetic relationships and construct an evolutionary timeline for the diversification of major clades, we conducted a Bayesian tip-dating analysis incorporating the fossilized birth-death process. A total of 13 fossil species were sampled in our analysis, including six taxonomically revaluated herein, two recently reappraised species from the Jurassic, and five additional species from the Cretaceous and Miocene.
Contrary to prior assumptions, our results indicate that none of the Jurassic taxa investigated belong to Asteriidae or any other modern families, and instead represent stem-forcipulatids. Furthermore, our phylogenetic results suggest that Asteriidae likely originated during the late Cretaceous. Our findings highlight a greater early diversity within the Forcipulatacea than previously presumed, challenging existing perceptions of the evolutionary history of this significant clade of marine invertebrates.
长腕目是海星的一个主要分支,拥有约 400 种现存物种,分为三个目(长腕海星目、有棘海星目、真蛇尾目)。在过去的一个世纪里,长腕目动物的系统发生学经历了多位作者的多次修订,一些作者认为有许多科,如 Asteriidae、Zoroasteridae、Pedicellasteridae、Stichasteridae、Heliasteridae、Labidiasteridae 和 Neomorphasteridae,而另一些作者只承认两个科(即 Asteriidae 和 Zoroasteridae)。最近的分子分析表明,这些分组中的一些是人为的。值得注意的是,从形态学和分子证据的综合来看,四个支持良好的进化枝(真蛇尾目、有棘海星目、Stichasteridae 和 Asteriidae)出现了。大多数已灭绝的长腕目物种都被归入现代科。然而,许多这些化石物种需要修订,特别是那些被归入 Asteriidae 的物种,这是所有长腕目动物中最大的一个科。
鉴于长腕目系统发生学的最新进展,我们全面重新评估了六个保存完好的侏罗纪长腕目分类群,包括始新世(约 201.4 Ma)最早的冠群成员,还描述了两个新的侏罗纪属, 属。nov. 和 属。nov. 我们为该组组装了最大和最全面的系统发育矩阵,对 42 种化石和现生物种的 120 个形态特征进行了采样。为了推断主要进化枝的系统发育关系和构建进化时间表,我们进行了贝叶斯尖峰定年分析,其中包含化石化的生死过程。我们的分析共采样了 13 个化石物种,包括本文中重新评估的六个分类群、两个最近重新评估的侏罗纪物种以及另外五个来自白垩纪和中新世的物种。
与之前的假设相反,我们的结果表明,研究的侏罗纪分类群没有一个属于 Asteriidae 或任何其他现代科,而是代表长腕目祖先。此外,我们的系统发育结果表明,Asteriidae 可能起源于晚白垩纪。我们的发现强调了长腕目动物在早期的多样性比之前认为的要大,挑战了对这个重要的海洋无脊椎动物类群的进化历史的现有认识。