Ribera Ignacio, Nilsson Anders N, Vogler Alfried P
Department of Entomology, The Natural History Museum, Cromwell Road, London SW7 5BD, UK.
Mol Phylogenet Evol. 2004 Mar;30(3):545-62. doi: 10.1016/S1055-7903(03)00224-0.
The Agabinae, with more than 350 species, is one of the most diverse lineages of diving beetles (Dytiscidae). Using the mitochondrial genes 16S rRNA and cytochrome oxidase I we present a phylogenetic analysis based on 107 species drawn mostly from the four main Holarctic genera. Two of these genera (Ilybius and Ilybiosoma) are consistently recovered as monophyletic with strong support, Platambus is never recovered as monophyletic, and Agabus is found paraphyletic with respect to several of the species groups of Platambus. Basal relationships among the main lineages are poorly defined, although within each of them relationships are in general robust and very consistent across the parameter space, and in agreement with previous morphological analyses. In each of the two most diverse lineages (Ilybius and Agabus including part of Platambus) there is a basal split between Palearctic and Nearctic clades, estimated to have occurred in the late Eocene. The Palearctic clade in turn splits into a Western Palearctic clade and a clade containing mostly Eastern Palearctic species, and assumed to be ancestrally Eastern Palearctic but with numerous transitions to a Holarctic or Nearctic distribution. These results suggest an asymmetry in the colonization routes, as there are very few cases of transcontinental range expansions originating from the Nearctic or the Western Palearctic. According to standard clock estimates, we do not find any transcontinental shift during the Pliocene, but numerous speciation events within each of the continental or subcontinental regions.
沼梭亚科有350多种,是龙虱科(豉甲科)中最多样化的谱系之一。我们利用线粒体基因16S rRNA和细胞色素氧化酶I,对主要来自全北区四个主要属的107个物种进行了系统发育分析。其中两个属(沼梭属和沼梭体属)始终被强烈支持为单系类群,扁龙虱属从未被恢复为单系类群,而沼梭属相对于扁龙虱属的几个物种组而言是并系的。主要谱系之间的基部关系定义不明确,尽管在每个谱系中,关系总体上是稳健的,并且在参数空间中非常一致,并且与先前的形态学分析一致。在两个最多样化的谱系(沼梭属和包括部分扁龙虱属的沼梭属)中,古北区和新北区分支之间都有一个基部分裂,估计发生在始新世晚期。古北区分支又分为西古北区分支和一个主要包含东古北区物种的分支,假定其祖先为东古北区,但有许多向全北区或新北区分布的转变。这些结果表明定殖路线存在不对称性,因为源自新北区或西古北区的跨大陆范围扩张情况非常少。根据标准时钟估计,我们在上新世期间没有发现任何跨大陆转移,但在每个大陆或次大陆区域内有许多物种形成事件。