Complete mitochondrial genomes and updated divergence time of the two freshwater clupeids endemic to Lake Tanganyika (Africa) suggest intralacustrine speciation.

Leona J M Milec, Maarten P M Vanhove, Fidel Muterezi Bukinga, Els L R De Keyzer, Vercus Lumami Kapepula, Pascal Mulungula Masilya, N'Sibula Mulimbwa, Catherine E Wagner, Joost A M Raeymaekers
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Abstract

Background: The hydrogeological history of Lake Tanganyika paints a complex image of several colonization and adaptive radiation events. The initial basin was formed around 9-12 million years ago (MYA) from the predecessor of the Malagarasi-Congo River and only 5-6 MYA, its sub-basins fused to produce the clear, deep waters of today. Next to the well-known radiations of cichlid fishes, the lake also harbours a modest clade of only two clupeid species, Stolothrissa tanganicae and Limnothrissa miodon. They are members of Pellonulini, a tribe of clupeid fishes that mostly occur in freshwater and that colonized West and Central-Africa during a period of high sea levels during the Cenozoic. There is no consensus on the phylogenetic relationships between members of Pellonulini and the timing of the colonization of Lake Tanganyika by clupeids.

Results: We use short-read next generation sequencing of 10X Chromium libraries to sequence and assemble the full mitochondrial genomes of S. tanganicae and L. miodon. We then use Maximum likelihood and Bayesian inference to place them into the phylogeny of Pellonulini and other clupeiforms, taking advantage of all available full mitochondrial clupeiform genomes. We identify Potamothrissa obtusirostris as the closest living relative of the Tanganyika sardines and confirm paraphyly for Microthrissa. We estimate the divergence of the Tanganyika sardines around 3.64 MYA [95% CI: 0.99, 6.29], and from P. obtusirostris around 10.92 MYA [95% CI: 6.37-15.48].

Conclusions: These estimates imply that the ancestor of the Tanganyika sardines diverged from a riverine ancestor and entered the proto-lake Tanganyika around the time of its formation from the Malagarasi-Congo River, and diverged into the two extant species at the onset of deep clearwater conditions. Our results prompt a more thorough examination of the relationships within Pellonulini, and the new mitochondrial genomes provide an important resource for the future study of this tribe, e.g. as a reference for species identification, genetic diversity, and macroevolutionary studies.

Abstract Image

Abstract Image

Abstract Image

非洲坦噶尼喀湖特有的两种淡水棒足类的全线粒体基因组和更新的分化时间表明它们是湖内物种形成。
背景:坦噶尼喀湖的水文地质历史描绘了一系列殖民和适应性辐射事件的复杂图像。最初的盆地形成于大约900万至1200万年前(MYA),由马拉加拉西-刚果河的前身形成,仅在5-6亿年前,它的子盆地融合产生了今天清澈、深邃的水域。除了众所周知的水螅鱼外,该湖还拥有一个只有两种类的中等进化支,即Stolothrissa tanganicae和Limnothrissa miodon。它们是Pellonulini的成员,Pellonulini是一种羽状鱼类,主要生活在淡水中,在新生代高海平面时期殖民西非和中非。关于Pellonulini成员之间的系统发育关系以及clupeids在坦噶尼喀湖定居的时间,目前还没有达成共识。结果:我们利用10X Chromium文库的短读次测序技术对S. tanganicae和L. miodon的线粒体全基因组进行了测序和组装。然后,我们利用最大似然和贝叶斯推理将它们放入Pellonulini和其他棍棒形式的系统发育中,利用所有可用的全线粒体棍棒形式基因组。我们确定了Potamothrissa obtusirostris是坦噶尼喀沙丁鱼的近亲,并确认了Microthrissa的近亲。我们估计Tanganyika沙丁鱼的分化大约在3.64 MYA [95% CI: 0.99, 6.29],而P. obtusirostris的分化大约在10.92 MYA [95% CI: 6.37-15.48]。结论:这些估计表明,坦噶尼喀沙丁鱼的祖先从一个河流祖先分化而来,并在其形成前后从马拉加拉西-刚果河进入坦噶尼喀原湖,并在深水清澈条件开始时分化为现存的两个物种。我们的研究结果促进了对Pellonulini内部关系的更深入的研究,并且新的线粒体基因组为该部落的未来研究提供了重要的资源,例如作为物种鉴定,遗传多样性和宏观进化研究的参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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