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Variation in palaeo-shorelines explains contemporary population genetic patterns of rocky shore species

机译:古海岸线的变化解释了岩石海岸物种的当代种群遗传模式

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摘要

Processes driving and maintaining disjunct genetic populations in marine systems are poorly understood, owing to a lack of evidence of hard barriers that could have shaped patterns of extant population structure. Here, we map two genetically divergent lineages of an obligate rocky shore fish, Clinus cottoides, and model sea-level change during the last 110 000 years to provide the first evidence of a vicariant event along the southern coastline of Africa. Results reveal that lowered sea levels during glacial periods drastically reduced rocky intertidal habitat, which may have isolated populations in two refugia for at least 40 000 years. Contemporary coastal dynamics and oceanography explain secondary contact between lineages. This scenario provides an explanation for the origin of population genetic breaks despite a lack of obvious present-day geographical barriers and highlights the need for including palaeo-oceanography in unravelling extant population patterns.
机译:由于缺乏关于可能形成现存种群结构模式的硬障碍的证据,人们很少了解驱动和维持海洋系统中分离的遗传种群的过程。在这里,我们绘制了两个遗传上各不相同的多岩石海岸鱼类科林斯科托斯的血统,并模拟了过去11万年来的海平面变化,以提供非洲南部海岸线上的维多利亚时代事件的第一个证据。结果表明,冰川期的海平面降低大大减少了潮间带岩石栖息地,这可能使两个避难所中的孤立种群至少生存了4万年。当代的沿海动力学和海洋学解释了世系之间的次要联系。尽管目前没有明显的地理障碍,但这种情况为人口遗传断裂的起源提供了解释,并突显了在揭示现有人口格局中包括古海洋学的必要性。

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