Phylogenetic relationships of the western North American cyprinid genus Richardsonius, with an overview of phylogeographic structure

被引:23
|
作者
Houston, Derek D. [1 ]
Shiozawa, Dennis K. [2 ]
Riddle, Brett R. [1 ]
机构
[1] Univ Nevada, Sch Life Sci, Las Vegas, NV 89154 USA
[2] Brigham Young Univ, Dept Biol, Provo, UT 84602 USA
关键词
Biogeography; Clinostomus; Cyprinidae; Drainage history; Iotichthys; Lahontan redside shiner; Redside shiner; FRESH-WATER FISHES; PACIFIC-NORTHWEST; EVOLUTIONARY RELATIONSHIPS; MOLECULAR SYSTEMATICS; MITOCHONDRIAL; 12S; SHALLOW HISTORY; BIOGEOGRAPHY; ACTINOPTERYGII; IDAHO; HYPOTHESES;
D O I
10.1016/j.ympev.2009.10.017
中图分类号
Q5 [生物化学]; Q7 [分子生物学];
学科分类号
071010 ; 081704 ;
摘要
Diversification of many North American taxa, including freshwater fishes, has been heavily influenced by the effects of complex geological and climatic events throughout the Cenozoic that have significantly altered the landscape. Here, we employ an array of phylogenetic analyses using a multiple gene tree approach to address several questions regarding the phylogenetic relationships of the North American cyprinid genus Richardsonius and two other closely related genera, Clinostomus and Iotichthys. We also use divergence time estimates generated using fossil calibrations to qualitatively assess the phylogeographic implications of evolution within the group. Mitochondrial and nuclear DNA sequences show a sister relationship between Iotichthys and Richardsonius, with Clinostomus being sister to an Iotichthys-Richardsonius clade, hence the currently recognized sister relationship between Clinostomus and Richardsonius is not supported. These genera appear to be monophyletic lineages, and sister species within genera appear to be reciprocally monophyletic. The two species within the genus Richardsonius both exhibit phylogeographic structure that is worthy of further investigation. Divergence time estimates between genera and species are Miocene or Pliocene in age, and divergence between phylogroups within species occurred in the late Pliocene to Pleistocene. These splits coincide with documented geological and climatic events. (C) 2009 Elsevier Inc. All rights reserved.
引用
收藏
页码:259 / 273
页数:15
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