Liu Xingyue, Hayashi Fumio, Yang Ding
Department of Entomology, China Agricultural University, Beijing, 100193, China.
Department of Biology, Tokyo Metropolitan University, Minamiosawa 1-1, Hachioji, Tokyo, 192-0397, Japan.
Cladistics. 2015 Feb;31(1):18-49. doi: 10.1111/cla.12071. Epub 2014 Feb 7.
Sialidae (alderflies) is a family of the holometabolous insect order Megaloptera, with ca. 75 extant species in eight genera distributed worldwide. Alderflies are a group of "living fossils" with a long evolutionary history. The oldest fossil attributed to Sialidae dates back to the Early Jurassic period. Further, the global distribution of modern-day species shows a remarkably disjunctive pattern. However, due to the rareness of most species and scarcity of comprehensive taxonomic revisions, the phylogeny of Sialidae remains largely unexplored, and the present classification system is in great need of renewal. Here we reconstruct the first phylogeny for Sialidae worldwide based on the most comprehensive sampling and broadest morphological data ever presented for this group of insects. All Cenozoic alderflies belong to a monophyletic clade, which may also include the Early Jurassic genus †Dobbertinia, and the Late Jurassic genus †Sharasialis is their putative sister taxon. Two subfamilies of Sialidae are proposed, namely †Sharasialinae subfam. nov. and Sialidinae. Austrosialis is the sister of all other extant genera, an assemblage which comprises three monophyletic lineages: the Stenosialis lineage, the Ilyobius lineage, and the Sialis lineage. The revised classification of Sialidae is composed of 12 valid genera and 87 valid species. Ilyobius and Protosialis are recognized as valid generic names, while Nipponosialis is treated as a synonym of Sialis. Reconstruction of the ancestral area proposes a global distribution of alderflies in Pangaea before their diversification. The generic diversification of alderflies might have occurred before the breakup of Pangaea, but the divergence of some lineages or genera was probably promoted by the splitting of this supercontinent.
泥蛉科(泥蛉)是全变态昆虫广翅目下的一个科,在全球八个属中约有75个现存物种。泥蛉是一类具有悠久进化历史的“活化石”。归因于泥蛉科的最古老化石可追溯到早侏罗世时期。此外,现代物种的全球分布呈现出显著的间断分布模式。然而,由于大多数物种稀有且缺乏全面的分类修订,泥蛉科的系统发育在很大程度上仍未得到探索,目前的分类系统亟需更新。在此,我们基于有史以来针对这类昆虫所呈现的最全面采样和最广泛形态学数据,重建了全球首个泥蛉科系统发育。所有新生代泥蛉都属于一个单系类群,其中可能还包括早侏罗世的†多贝廷尼亚属,晚侏罗世的†沙拉西亚利斯属是其假定的姐妹分类单元。提出了泥蛉科的两个亚科,即†沙拉西亚利纳亚科(新亚科)和泥蛉亚科。澳泥蛉属是所有其他现存属的姐妹属,这一组合包括三个单系谱系:窄泥蛉谱系、溪泥蛉谱系和泥蛉谱系。泥蛉科的修订分类由12个有效属和87个有效种组成。溪泥蛉属和原泥蛉属被确认为有效属名,而日本泥蛉属被视为泥蛉属的同义词。祖先分布区的重建表明,泥蛉在泛大陆多样化之前曾在全球分布。泥蛉的属多样化可能在泛大陆分裂之前就已发生,但一些谱系或属的分化可能是由这个超级大陆的分裂所推动的。