基因谱系与北美东部古排水盆地:双线真螈物种复合体蝾螈的系统地理学与物种形成
Gene lineages and eastern North American palaeodrainage basins: phylogeography and speciation in salamanders of the Eurycea bislineata species complex.
作者信息
Kozak Kenneth H, Blaine Russell A, Larson Allan
机构信息
Department of Biology, Washington University, Saint Louis, MO 63130, USA.
出版信息
Mol Ecol. 2006 Jan;15(1):191-207. doi: 10.1111/j.1365-294X.2005.02757.x.
Contemporary North American drainage basins are composites of formerly isolated drainages, suggesting that fragmentation and fusion of palaeodrainage systems may have been an important factor generating current patterns of genetic and species diversity in stream-associated organisms. Here, we combine traditional molecular-phylogenetic, multiple-regression, nested clade, and molecular-demographic analyses to investigate the relationship between phylogeographic variation and the hydrogeological history of eastern North American drainage basins in semiaquatic plethodontid salamanders of the Eurycea bislineata species complex. Four hundred forty-two sequences representing 1108 aligned bases from the mitochondrial genome are reported for the five formally recognized species of the E. bislineata complex and three outgroup taxa. Within the in-group, 270 haplotypes are recovered from 144 sampling locations. Geographic patterns of mtDNA-haplotype coalescence identify 13 putatively independent population-level lineages, suggesting that the current taxonomy of the group underestimates species-level diversity. Spatial and temporal patterns of phylogeographic divergence are strongly associated with historical rather than modern drainage connections, indicating that shifts in major drainage patterns played a pivotal role in the allopatric fragmentation of populations and build-up of lineage diversity in these stream-associated salamanders. More generally, our molecular genetic results corroborate geological and faunistic evidence suggesting that palaeodrainage connections altered by glacial advances and headwater erosion occurring between the mid-Miocene and Pleistocene epochs explain regional patterns of biodiversity in eastern North American streams.
当代北美流域是由以前孤立的水系组合而成的,这表明古水系的破碎化和融合可能是导致当前与溪流相关生物的遗传和物种多样性模式形成的一个重要因素。在这里,我们结合传统的分子系统发育、多元回归、嵌套分支和分子人口统计学分析,来研究北美东部流域水文地质历史与半水生无肺螈科双行螈属复合体的系统地理学变异之间的关系。我们报告了双行螈属复合体五个正式认可物种和三个外类群分类单元的442个序列,这些序列代表了线粒体基因组中1108个比对碱基。在类群内部,从144个采样地点获得了270个单倍型。线粒体DNA单倍型合并的地理模式识别出13个假定独立的种群水平谱系,这表明该类群目前的分类法低估了物种水平的多样性。系统地理学分歧的时空模式与历史而非现代的水系联系密切相关,这表明主要水系模式的转变在这些与溪流相关的蝾螈种群的异域性破碎化和谱系多样性积累中起到了关键作用。更普遍地说,我们的分子遗传学结果证实了地质和动物区系证据,表明中新世中期到更新世时期冰川前进和源头侵蚀导致的古水系联系变化解释了北美东部溪流生物多样性的区域模式。