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首页> 外文期刊>Molecular phylogenetics and evolution >Origin, diversification, and systematics of the New Zealand skink fauna (Reptilia: Scincidae)
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Origin, diversification, and systematics of the New Zealand skink fauna (Reptilia: Scincidae)

机译:新西兰石龙动物区系的起源,多样性和系统化(Reptilia:Scincidae)

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The diverse scincid lizard fauna of the largely submerged subcontinent of Zealandia (which incorporates New Zealand, New Caledonia, Lord Howe Island, Norfolk Island, and the Chatham Islands) forms a monophyletic lineage within the Eugongylus group of skinks. We use 4062 bp of mitochondrial (ND2, ND4, Cytochrome b, 12SrRNA, 16SrRNA) and nuclear (Rag-1) DNA sequence data to recover a molecular phylogeny for the New Zealand skink fauna, and investigate the origin and diversification of skinks in New Zealand. Our phylogeny includes 32 of the 33 extant described New Zealand skink species (Cyclodina and Oligosoma), the Lord Howe Island skink (C. lichenigera), and representatives from several New Caledonian genera. Neighbour-joining, Maximum Parsimony, Maximum Likelihood, and Bayesian phylogenetic analyses are used to demonstrate that the New Zealand skink species form a single monophyletic lineage, with C. lichenigera representing a closely related sister lineage to the New Zealand radiation. Our relaxed molecular clock analyses indicate that skinks colonised New Zealand in the early Miocene (16-22.6 mya), shortly after the 'Oligocene drowning' event (~25 mya). We propose that skinks reached New Zealand from New Caledonia via long-distance overwater dispersal, with C. lichenigera persisting on volcanic islands along the Lord Howe Rise and Norfolk Ridge. Eight major genetic clades are evident within the New Zealand skink fauna, with the divergences among these clades during the early to mid-Miocene resulting in distinct open habitat, forest, and coastal radiations. Subsequent diversification in the late Miocene-Pliocene appears to coincide with tectonic activity along the Alpine Fault and the uplift of the Southern Alps. We were unable to resolve the phylogenetic affinities of O. suteri, New Zealand's only native oviparous skink. We use the phylogeny and topology tests to resolve several taxonomic issues and assess the taxonomic status of several suspected undescribed taxa. We complete a generic revision for the New Zealand skink fauna, placing C. lichenigera and all native New Zealand species into a single genus.
机译:在很大程度上被淹没的西兰西亚次大陆(其中包括新西兰,新喀里多尼亚,豪勋爵岛,诺福克岛和查塔姆群岛)的多样奇特蜥蜴动物群在石龙子Eugongylus群内形成了单系谱系。我们使用4062 bp的线粒体(ND2,ND4,细胞色素b,12SrRNA,16SrRNA)和核(Rag-1)DNA序列数据来恢复新西兰石龙动物区系的分子系统发育,并研究新的石龙鱼的起源和多样性西兰。我们的系统进化论包括33种现存描述的新西兰石龙子物种(Cyclodina和Oligosoma)中的32种,豪勋爵岛的石龙子(C. lichenigera)以及几个新喀里多尼亚属的代表。邻域连接,最大简约,最大似然和贝叶斯系统发育分析被用来证明新西兰的石龙子物种形成了单一的单系谱系,地衣梭菌代表了与新西兰辐射密切相关的姐妹谱系。我们轻松的分子钟分析表明,在“渐新世溺水”事件(〜25 mya)发生后不久,石龙子在中新世早期(16-22.6 mya)定居于新西兰。我们建议,石龙子通过长途水上扩散从新喀里多尼亚到达新西兰,而地衣梭菌在沿豪勋爵山和诺福克岭的火山岛上持续存在。在新西兰的石龙类动物群中,有八种主要的遗传进化枝是显而易见的,在中新世早期至中期,这些进化枝之间存在差异,从而导致明显的开放栖息地,森林和沿海辐射。中新世-上新世晚期的随后多样化似乎与沿阿尔卑斯断裂和南阿尔卑斯山隆升的构造活动相吻合。我们无法解析新西兰唯一的原生卵生石龙子O. suteri的系统亲缘关系。我们使用系统发育和拓扑测试来解决几个分类问题,并评估几个可疑未描述分类单元的分类状态。我们完成了对新西兰石龙动物的通用修订,将地衣梭菌和所有新西兰本土物种归为一个属。

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