CNRS UMR 7205, Muséum National d'Histoire Naturelle, CP 50, Entomologie, 45 Rue Buffon, Paris F-75231, France.
Nature. 2013 Nov 14;503(7475):257-61. doi: 10.1038/nature12629. Epub 2013 Oct 16.
The Eumetabola (Endopterygota (also known as Holometabola) plus Paraneoptera) have the highest number of species of any clade, and greatly contribute to animal species biodiversity. The palaeoecological circumstances that favoured their emergence and success remain an intriguing question. Recent molecular phylogenetic analyses have suggested a wide range of dates for the initial appearance of the Holometabola, from the Middle Devonian epoch (391 million years (Myr) ago) to the Late Pennsylvanian epoch (311 Myr ago), and Hemiptera (310 Myr ago). Palaeoenvironments greatly changed over these periods, with global cooling and increasing complexity of green forests. The Pennsylvanian-period crown-eumetabolan fossil record remains notably incomplete, particularly as several fossils have been erroneously considered to be stem Holometabola (Supplementary Information); the earliest definitive beetles are from the start of the Permian period. The emergence of the hymenopterids, sister group to other Holometabola, is dated between 350 and 309 Myr ago, incongruent with their current earliest record (Middle Triassic epoch). Here we describe five fossils--a Gzhelian-age stem coleopterid, a holometabolous larva of uncertain ordinal affinity, a stem hymenopterid, and early Hemiptera and Psocodea, all from the Moscovian age--and reveal a notable penecontemporaneous breadth of early eumetabolan insects. These discoveries are more congruent with current hypotheses of clade divergence. Eumetabola experienced episodes of diversification during the Bashkirian-Moscovian and the Kasimovian-Gzhelian ages. This cladogenetic activity is perhaps related to notable episodes of drying resulting from glaciations, leading to the eventual demise in Euramerica of coal-swamp ecosystems, evidenced by floral turnover during this interval. These ancient species were of very small size, living in the shadow of Palaeozoic-era 'giant' insects. Although these discoveries reveal unexpected Pennsylvanian eumetabolan diversity, the lineage radiated more successfully only after the mass extinctions at the end of the Permian period, giving rise to the familiar crown groups of their respective clades.
真昆虫(包括内翅类(也称为全变态类)和外翅类)拥有最多的物种,对动物物种多样性做出了巨大贡献。支持它们出现和成功的古生态环境仍然是一个有趣的问题。最近的分子系统发育分析表明,全变态类的最初出现时间范围很广,从中生代泥盆纪(3.91 亿年前)到晚宾夕法尼亚纪(3.11 亿年前),以及半翅目(3.1 亿年前)。在这些时期,古环境发生了巨大变化,全球变冷,绿色森林的复杂性增加。宾夕法尼亚纪冠真昆虫的化石记录仍然明显不完整,特别是因为一些化石被错误地认为是原始全变态类(补充信息);最早的明确甲虫来自二叠纪早期。与它们目前最早的记录(中三叠纪)不一致的是,膜翅目昆虫的姊妹群——长翅目昆虫的出现时间被定在 3.5 亿至 3.09 亿年前。在这里,我们描述了五个化石——一个泥盆纪时代的原始鞘翅目,一个不定目全变态类幼虫,一个原始膜翅目,以及早期的半翅目和石蛃目,均来自莫斯科纪,并揭示了早期真昆虫明显的同时代广泛多样性。这些发现与目前的支系分化假说更为一致。全变态类在西伯利亚纪-莫斯科纪和卡兹米诺纪-格热利纪时期经历了多样化事件。这种分支活动可能与冰川作用导致的干燥显著事件有关,导致欧洲和美洲的煤沼泽生态系统最终消失,这一时期的花卉更替证明了这一点。这些古老的物种体型非常小,生活在古生代“巨型”昆虫的阴影下。尽管这些发现揭示了出乎意料的宾夕法尼亚纪真昆虫多样性,但该谱系只有在二叠纪末期大规模灭绝之后才成功辐射,形成了各自支系熟悉的冠群。