Hafner John C, Upham Nathan S
J Biogeogr. 2011 Jun;38(6):1077-1097. doi: 10.1111/j.1365-2699.2010.02472.x.
The rodent genus Microdipodops (kangaroo mice) includes two sand-obligate endemics of the Great Basin Desert: M. megacephalus and M. pallidus. The dark kangaroo mouse, M. megacephalus, is distributed throughout the Great Basin and our principal aims were to formulate phylogenetic hypotheses for this taxon and make phylogeographical comparisons with its congener. LOCATION: The Great Basin Desert of western North America. METHODS: DNA sequence data from three mitochondrial genes were examined from 186 individuals of M. megacephalus, representing 47 general localities. Phylogenetic inference was used to analyse the sequence data. Directional analysis of phylogeographical patterns was used to examine haplotype sharing patterns and recover routes of gene exchange. Haplotype-area curves were constructed to evaluate the relationship between genetic variation and distributional island size for M. megacephalus and M. pallidus. RESULTS: Microdipodops megacephalus is a rare desert rodent (trapping success was 2.67%). Temporal comparison of trapping data shows that kangaroo mice are becoming less abundant in the study area. The distribution has changed slightly since the 1930s but many northern populations now appear to be small, fragmented, or locally extinct. Four principal phylogroups (the Idaho isolate and the western, central and eastern clades) are evident; mean sequence divergence between phylogroups for cytochrome b is c. 8%. Data from haplotype sharing show two trends: a north-south trend and a web-shaped trend. Analyses of haplotype-area curves reveal significant positive relationships. MAIN CONCLUSIONS: The four phylogroups of M. megacephalus appear to represent morphologically cryptic species; in comparison, a companion study revealed two cryptic lineages in M. pallidus. Estimated divergence times of the principal clades of M. megacephalus (c. 2-4 Ma) indicate that these kangaroo mice were Pleistocene invaders into the Great Basin coincident with the formation of sandy habitats. The north-south and web patterns from directional analyses reveal past routes of gene flow and provide evidence for source-sink population regulation. The web pattern was not seen in the companion study of M. pallidus. Significant haplotype-area curves indicate that the distributional islands are now in approximate genetic equilibrium. The patterns described here are potentially useful to conservation biologists and wildlife managers and may serve as a model for other sand-obligate organisms of the Great Basin.
啮齿动物小更格卢鼠属(更格卢鼠)包括大盆地沙漠的两种沙地专性特有种:巨颅更格卢鼠和苍白更格卢鼠。深色更格卢鼠,即巨颅更格卢鼠,分布于整个大盆地,我们的主要目的是构建该分类单元的系统发育假说,并与其同属物种进行系统地理学比较。地点:北美西部的大盆地沙漠。方法:从代表47个一般地点的186只巨颅更格卢鼠个体中检测了来自三个线粒体基因的DNA序列数据。使用系统发育推断来分析序列数据。系统地理模式的定向分析用于检查单倍型共享模式并恢复基因交换路线。构建单倍型 - 面积曲线以评估巨颅更格卢鼠和苍白更格卢鼠的遗传变异与分布岛屿大小之间的关系。结果:巨颅更格卢鼠是一种稀有的沙漠啮齿动物(捕获成功率为2.67%)。捕获数据的时间比较表明,更格卢鼠在研究区域的数量正在减少。自20世纪30年代以来分布略有变化,但现在许多北部种群似乎规模较小、破碎化或局部灭绝。四个主要的系统发育类群(爱达荷分离种群以及西部、中部和东部分支)很明显;细胞色素b的系统发育类群之间的平均序列分歧约为8%。单倍型共享数据显示出两种趋势:南北趋势和网状趋势。单倍型 - 面积曲线分析揭示了显著的正相关关系。主要结论:巨颅更格卢鼠的四个系统发育类群似乎代表形态上难以区分的物种;相比之下,一项配套研究揭示了苍白更格卢鼠中的两个隐性谱系。巨颅更格卢鼠主要分支的估计分歧时间(约200 - 400万年前)表明,这些更格卢鼠是更新世时期侵入大盆地的,与沙地栖息地的形成同时发生。定向分析中的南北和网状模式揭示了过去的基因流动路线,并为源 - 汇种群调节提供了证据。在苍白更格卢鼠的配套研究中未发现网状模式。显著的单倍型 - 面积曲线表明,分布岛屿现在处于近似的遗传平衡状态。这里描述的模式可能对保护生物学家和野生动物管理者有用,并可能作为大盆地其他沙地专性生物的一个模型。