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对欧洲鳀(Engraulis encrasicolus)线粒体DNA变异性的再审视:评估种群结构模型与黑海隔离假说

A second look at mitochondrial DNA variability in European anchovy (Engraulis encrasicolus): assessing models of population structure and the Black Sea isolation hypothesis.

作者信息

Grant W Stewart

机构信息

P.O. Box 240104, Anchorage, AK 99524-0104, USA.

出版信息

Genetica. 2005 Nov;125(2-3):293-309. doi: 10.1007/s10709-005-0717-z.

Abstract

Genetic architectures of marine fishes are generally shallow because of the large potential for gene flow in the sea. European anchovy, however, are unusual among small pelagic fishes in showing large differences among sub-basins and in harbouring two mtDNA phylogroups ('A' & 'B'), representing 1.1-1.85 million years of separation. Here the mtDNA RFLP dataset of Magoulas et al. [1996, Mol. Biol. Evol. 13: 178-190] is re-examined to assess population models accounting for this subdivided population structure and to evaluate the zoogeographical origins of the two major phylogroups. Haplotype and nucleotide diversities are highest in the Ionian Sea and lowest in the Aegean and Black seas. However, this gradient is absent when 'A' and 'B' haplotypes are examined separately. Neither the self-sustaining nor the basin population models adequately describe anchovy population behaviour. Tests for neutrality, mismatch and nested clade analyses are concordant in depicting recent expansions of both phylogroups. Unimodel mismatch distributions and haplotype coalescences dating to the last (Eemian) interglacial ('B') and the Weichselian pleniglacial period ('A') indicate separate colonizations of the Mediterranean Basin. Phylogroup 'A' is unlikely to have arisen through continuous long-term isolation in the Black Sea because of climate extremes from displaced subpolar weather systems during the ice ages. Ancestors of both groups appear to have colonized the Mediterranean from the Atlantic in the late Pleistocene. Hence, zoogeographic models of anchovy in the Mediterranean must also include the eastern (and possibly southern) Atlantic.

摘要

由于海洋中基因流动的潜力巨大,海洋鱼类的遗传结构通常较为简单。然而,欧洲凤尾鱼在小型中上层鱼类中却与众不同,其在不同亚流域间表现出巨大差异,并且拥有两个线粒体DNA系统发育类群(“A”和“B”),这两个类群已经分离了110万至185万年。在此,我们重新审视了马古拉斯等人[1996年,《分子生物学与进化》13: 178 - 190]的线粒体DNA RFLP数据集,以评估能够解释这种细分种群结构的种群模型,并评估这两个主要系统发育类群的动物地理学起源。单倍型和核苷酸多样性在爱奥尼亚海最高,在爱琴海和黑海最低。然而,当分别检查“A”和“B”单倍型时,这种梯度并不存在。自我维持模型和流域种群模型都不能充分描述凤尾鱼的种群行为。中性检验、错配分析和嵌套分支分析在描述两个系统发育类群最近的扩张方面是一致的。单峰错配分布和单倍型合并可追溯到最后一个(伊米亚)间冰期(“B”)和魏克塞尔冰期盛冰期(“A”),这表明地中海盆地是分别殖民的。由于冰期期间极地天气系统位移导致的极端气候,类群“A”不太可能是通过在黑海持续长期隔离而产生的。两个类群的祖先似乎都是在更新世晚期从大西洋殖民到地中海的。因此,地中海凤尾鱼的动物地理学模型也必须包括东大西洋(可能还有南大西洋)。

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