Jorge Hernández-Lozano, Carlos A Garita-Alvarado, Roberto Munguía-Steyer, Marco A Garduño-Sánchez, Claudia Patricia Ornelas-García
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引用次数: 0
摘要
Astyanax mexicanus为研究平行进化提供了一个独特的模型,其穴居形式至少产生于两个不同的地表品系。在这里,我们通过四个表型数据集研究了这两个适应穴居的品系的重复进化:(i) 分体数据;(ii) 生态形态学数据;以及(iii) 头部和(iv) 前颌骨形状的几何形态计量数据。此外,我们还评估了这些表型与其系统发育历史的关联。洞穴生态型的某些性状显示了跨系平行进化的证据,如上颌牙齿数增加、侧线鳞片数减少、前颌骨上升过程变短等。几何形态计量数据显示,洞穴和地表种群的头型存在表型差异梯度,Sierra de El Abra和地表种群之间的差异最大,而地表种群和危地马拉山洞及米科斯山洞之间的差异较小。与地表种群杂交的洞穴种群(如米科斯)与地表生态型的重叠程度最大。前下颌骨的形状也有类似的分化梯度,但洞穴和地表生态型之间的分化较弱。这些洞穴特征重复演化的证据强调了环境对洞穴生态型演化的选择性压力的重要性。
Parallel phenotypic evolution of two independent cavefish lineages of Astyanax mexicanus (De Filippi, 1854) (Characiformes: Characidae)
Astyanax mexicanus offers a unique model for studying parallel evolution, with cave-dwelling forms arising from at least two distinct surface lineages. Here, we examined repeated evolution in the two cave-adapted lineages across four phenotypic datasets: (i) meristic data; (ii) ecomorphological data; and geometric morphometric data for (iii) head and (iv) premaxillary bone shape. Additionally, we assessed the association of these phenotypes with their phylogenetic history. Certain traits exhibited evidence of parallel evolution for the cave ecotype across lineages, such as increased maxillary tooth count, reduced lateral line scale count, and shorter ascending process of the premaxillary bone. Geometric morphometric data showed a phenotypic divergence gradient in head shape between cave and surface populations, with the strongest divergence between Sierra de El Abra and surface populations and with less differentiation between surface populations and caves from Sierra de Guatemala and Micos. Cave populations that hybridize with surface populations (e.g. Micos) displayed the greatest overlap with the surface ecotype. There was a similar divergence gradient for premaxillary bone shape, but with weaker differentiation between cave and surface ecotypes. This evidence of repeated evolution in several cave traits emphasizes the significance of selective pressures exerted by the environment on the evolution of cave ecotypes.