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直布罗陀海峡的系统发育地理学印记与地中海西部第四纪气候波动:以大白齿鼩(Crocidura russula)为例(哺乳纲:鼩鼱科)

Phylogeographical footprints of the Strait of Gibraltar and Quaternary climatic fluctuations in the western Mediterranean: a case study with the greater white-toothed shrew, Crocidura russula (Mammalia: Soricidae).

作者信息

Cosson Jean-François, Hutterer Rainer, Libois Roland, Sarà Maurizio, Taberlet Pierre, Vogel Peter

机构信息

Centre de Biologie et Gestion des Populations, INRA UMR 1062, Campus International de Baillarguet, CS 30016, 34988 Montferrier/Lez cedex, France.

出版信息

Mol Ecol. 2005 Apr;14(4):1151-62. doi: 10.1111/j.1365-294X.2005.02476.x.

Abstract

We used mitochondrial cyt b sequences to investigate the phylogenetic relationships of Crocidura russula (sensu lato) populations across the Strait of Gibraltar, western Europe, Maghreb, and the Mediterranean and Atlantic islands. This revealed very low genetic divergence between European and Moroccan populations. The application of a molecular clock previously calibrated for shrews suggested that the separation of European from Moroccan lineages occurred less than 60 000 bp, which is at least 5 million years (Myr) after the reopening of the Strait of Gibraltar. This means that an overwater dispersal event was responsible for the observed phylogeographical structure. In contrast, genetic analyses revealed that Moroccan populations were highly distinct from Tunisian ones. According to the molecular clock, these populations separated about 2.2 million years ago (Ma), a time marked by sharp alternations of dry and humid climates in the Maghreb. The populations of the Mediterranean islands Ibiza, Pantelleria, and Sardinia were founded from Tunisian populations by overwater dispersal. In conclusion, overwater dispersal across the Strait of Gibraltar, probably assisted by humans, is possible for small terrestrial vertebrates. Moreover, as in Europe, Quaternary climatic fluctuations had a major effect on the phylogeographical structure of the Maghreb biota.

摘要

我们利用线粒体细胞色素b序列来研究地中海小家鼠(广义)种群在直布罗陀海峡、西欧、马格里布以及地中海和大西洋诸岛之间的系统发育关系。这揭示了欧洲和摩洛哥种群之间极低的遗传差异。应用先前为鼩鼱校准的分子钟表明,欧洲和摩洛哥谱系的分离发生在不到6万年前,这至少是在直布罗陀海峡重新开通后的500万年。这意味着一次跨水扩散事件导致了观察到的系统地理结构。相比之下,遗传分析表明摩洛哥种群与突尼斯种群高度不同。根据分子钟,这些种群大约在220万年前分离,这一时期马格里布地区气候干湿交替剧烈。地中海的伊维萨岛、潘泰莱里亚岛和撒丁岛的种群是由突尼斯种群通过跨水扩散形成的。总之,对于小型陆生脊椎动物来说,在可能由人类协助的情况下,跨直布罗陀海峡进行跨水扩散是可能的。此外,与欧洲一样,第四纪气候波动对马格里布生物群的系统地理结构产生了重大影响。

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