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环地中海物种毁灭材小蠹(Tomicus destruens Woll.)(鞘翅目:小蠹科)的系统发育地理结构及历史

Phylogeographic structure and past history of the circum-Mediterranean species Tomicus destruens Woll. (Coleoptera: Scolytinae).

作者信息

Horn A, Roux-Morabito G, Lieutier F, Kerdelhue C

机构信息

Université d'Orléans, Laboratoire de Biologie des Ligneux et des Grandes Cultures UPRES EA 1207, France.

出版信息

Mol Ecol. 2006 May;15(6):1603-15. doi: 10.1111/j.1365-294X.2006.02872.x.

DOI:10.1111/j.1365-294X.2006.02872.x
PMID:16629814
Abstract

Phylogeographic studies are often focused on temperate European species with relict footholds in the Mediterranean region. Past climatic oscillations usually induced range contractions and expansions from refugial areas located in southern Europe, and spatial distribution of genetic diversity show that northward expansions were usually pioneer-like. Actually, few studies have focused on circum-Mediterranean species, which probably were not influenced in the same way by climatic oscillations. We present the phylogeography of the bark beetle Tomicus destruens, which is restricted to the whole Mediterranean basin and the Atlantic coasts of North Africa and Portugal. We systematically sequenced 617 bp of the mitochondrial genes COI and COII for 42 populations (N = 219). Analysis revealed 53 haplotypes geographically structured in two clades, namely eastern and western clades, that diverged during the Pleistocene. A contact zone was identified along the Adriatic coast of Italy. Interestingly, we found contrasting levels of genetic structure within each clade. The eastern group was characterized by a significant phylogeographic pattern and low levels of gene flow, whereas the western group barely showed a spatial structure in haplotype distribution. Moreover, the main pine hosts were different between groups, with the Aleppo-brutia complex in the east and the maritime pine in the west. Potential roles of host species, climatic parameters and geographical barriers are discussed and the phylogeographic patterns are compared to classical models of postglacial recolonization in Europe.

摘要

系统发育地理学研究通常聚焦于在地中海地区拥有残留栖息地的温带欧洲物种。过去的气候振荡通常导致分布范围从位于南欧的避难区域收缩和扩张,而遗传多样性的空间分布表明向北的扩张通常类似先锋扩散。实际上,很少有研究关注环地中海物种,它们可能未受到气候振荡的相同影响。我们展示了树皮甲虫毁灭齿小蠹(Tomicus destruens)的系统发育地理学,该物种分布局限于整个地中海盆地以及北非和葡萄牙的大西洋沿岸。我们对42个种群(N = 219)的线粒体基因COI和COII的617 bp进行了系统测序。分析揭示了53个单倍型,在地理上形成两个分支,即东部和西部支系,它们在更新世期间分化。在意大利亚得里亚海沿岸确定了一个接触带。有趣的是,我们在每个支系中发现了不同程度的遗传结构。东部群体具有显著的系统发育地理格局和低水平的基因流,而西部群体在单倍型分布上几乎没有显示出空间结构。此外,两个群体的主要松树寄主不同,东部是阿勒颇松 - 布鲁蒂亚松复合体,西部是海岸松。讨论了寄主物种、气候参数和地理障碍的潜在作用,并将系统发育地理格局与欧洲冰期后重新定殖的经典模型进行了比较。

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