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北美淡水鱼 Pylodictis olivaris 串联重复线粒体 DNA D 环区域的地理变异。

Geographic variation within a tandemly repeated mitochondrial DNA D-loop region of a North American freshwater fish, Pylodictis olivaris.

机构信息

Department of Biological Sciences, University of Tulsa, 800 S. Tucker Dr., OK 74104, USA.

出版信息

Gene. 2014 Mar 15;538(1):63-8. doi: 10.1016/j.gene.2014.01.020. Epub 2014 Jan 15.

DOI:10.1016/j.gene.2014.01.020
PMID:24440244
Abstract

The present study reports the distribution of a 35-bp mitochondrial DNA (mtDNA) D-loop tandemly repeated sequence in the populations of a North American freshwater catfish, Pylodictis olivaris, and the important role of a past geological event in the phylogeographic pattern of this species. A total of 330 individuals of flathead catfish, representing 34 drainages throughout the species' native range in the United States, were collected. While more than 70% of individuals sampled from the Southeastern Gulf Coast drainages were characterized by the presence of a 35-bp mtDNA D-loop tandem repeat proximal to the 5' end, more than 95% of samples from the Mississippi River and its tributaries, as well as from the drainages of the Southwest Gulf Coast region, lack this tandem repeat. Concomitantly, phylogenetic analyses revealed the existence of two distinct matrilineal lineages (lineage I and II) of P. olivaris, which were estimated to have diverged from a common ancestor sometime between 0.70 and 2.05myr ago. While one lineage is comprised of samples from the Mississippi River and its tributaries and rivers draining to the Southwest Gulf Coast, the other lineage is comprised of samples from the Southeastern Gulf Coast drainages. Each lineage also has two sub-lineages, which also showed geographic specificity.

摘要

本研究报告了北美淡水鲶鱼 Pylodictis olivaris 群体中 35-bp 线粒体 DNA(mtDNA)D 环串联重复序列的分布,以及过去地质事件在该物种的系统地理格局中的重要作用。总共采集了 330 条扁头鲶鱼个体,代表了美国原产范围内 34 个流域。虽然在东南部墨西哥湾沿岸流域采集的个体中,有超过 70%的个体具有靠近 5'端的 35-bp mtDNA D 环串联重复,但在密西西比河及其支流以及西南墨西哥湾沿岸流域采集的样本中,超过 95%的样本缺乏这种串联重复。同时,系统发育分析揭示了 P. olivaris 的两个不同的母系谱系(谱系 I 和 II)的存在,它们被估计是在 0.70 到 2.05 百万年前从一个共同的祖先分化而来。一个谱系由密西西比河及其支流和西南墨西哥湾沿岸流域的样本组成,而另一个谱系则由东南部墨西哥湾沿岸流域的样本组成。每个谱系也有两个亚谱系,也具有地理特异性。

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