Institute for Ecology, Evolution and Diversity, Biosciences, Goethe-University, Frankfurt am Main, Germany.
Mol Phylogenet Evol. 2010 Jun;55(3):996-1007. doi: 10.1016/j.ympev.2009.11.027. Epub 2009 Dec 6.
The aim of the current study was to gain new insights into the phylogeny, biogeography and evolution of the opisthobranch clade Pleurobranchomorpha. We focused on testing the hypothesis of an Antarctic origin of this clade. The combination of four gene markers (18S rDNA, 28S rDNA, 16S rDNA and CO1) was used to infer a phylogenetic hypothesis of the Pleurobranchomorpha employing Maximum likelihood and Bayesian inference methods. Four methodologically distinct approaches were applied to reconstruct the historical biogeography and dating of the tree was performed via relaxed molecular clock analysis. Phylogenetic analyses supported the monophyly of the Pleurobranchomorpha and their sister group relationship to the Nudibranchia. Monophyly of the main subgroups Pleurobranchaeinae and Pleurobranchinae could not be revealed. Reconstruction of the ancestral area of the Pleurobranchomorpha yielded different possibilities in the diverse analyses. However, the Pleurobranchinae most probably derived from an Antarctic origin. Estimation of divergence times revealed a long credible interval for the Pleurobranchomorpha, whereas the Pleurobranchinae diverged in Early Oligocene and underwent rapid radiation during Oligocene and Early Miocene. Divergence of the Pleurobranchinae into the Antarctic Tomthompsonia and the remaining species in Early Oligocene coincides with two major geological events; namely the onset of glaciation in Antarctica and the opening of the Drake Passage with following formation of the Antarctic Circumpolar Current (ACC). These sudden and dramatic changes in climate probably led to subsequent migration of the last common ancestor of the remaining Pleurobranchinae into warmer regions, while the ACC may have accounted for larval dispersal to the Eastern Atlantic.
本研究旨在深入了解后鳃类 Pleurobranchomorpha 的系统发育、生物地理学和演化。我们专注于检验该类群起源于南极的假说。我们结合了四个基因标记(18S rDNA、28S rDNA、16S rDNA 和 CO1),运用最大似然法和贝叶斯推断法,对 Pleurobranchomorpha 进行了系统发育假设推断。我们采用了四种不同的方法来重建历史生物地理学,并通过放松分子钟分析对树进行了测时。系统发育分析支持后鳃类 Pleurobranchomorpha 的单系性及其与裸鳃目 Nudibranchia 的姊妹群关系。然而,主要亚群 Pleurobranchaeinae 和 Pleurobranchinae 的单系性无法得到揭示。对 Pleurobranchomorpha 祖先区的重建在不同的分析中产生了不同的可能性。然而,Pleurobranchinae 极有可能起源于南极。对 Pleurobranchomorpha 分歧时间的估计显示了一个很长的置信区间,而 Pleurobranchinae 在早渐新世发生分歧,并在渐新世和早中新世经历了快速辐射。Pleurobranchinae 分化为南极的 Tomthompsonia 和早渐新世的剩余物种,与两个主要的地质事件同时发生;即南极洲的冰川作用开始和德雷克海峡的开放,随后形成了南极环极流(ACC)。这些气候的突然和剧烈变化可能导致剩余 Pleurobranchinae 的最后共同祖先随后向温暖地区迁移,而 ACC 可能促成了幼虫向东大西洋的扩散。