Department of Biology, Washington University, St. Louis, Missouri, United States of America.
PLoS One. 2007 Aug 22;2(8):e760. doi: 10.1371/journal.pone.0000760.
Phylogenetic and geographic evidence suggest that many parthenogenetic organisms have evolved recently and have spread rapidly. These patterns play a critical role in our understanding of the relative merits of sexual versus asexual reproductive modes, yet their interpretation is often hampered by a lack of detail. Here we present a detailed phylogeographic study of a vertebrate parthenogen, the Australian gecko Heteronotia binoei, in combination with statistical and biophysical modeling of its distribution during the last glacial maximum. Parthenogenetic H. binoei occur in the Australian arid zone and have the widest range of any known vertebrate parthenogen. They are broadly sympatric with their sexual counterparts, from which they arose via hybridization. We have applied nested clade phylogeographic, effective migration, and mismatch distribution analyses to mitochondrial DNA (mtDNA) sequences obtained for 319 individuals sampled throughout the known geographic ranges of two parthenogenetic mitochondrial lineages. These analyses provide strong evidence for past range expansion events from west to east across the arid zone, and for continuing eastward range expansion. Parthenogen formation and range expansion events date to the late Pleistocene, with one lineage expanding from the northwest of its present range around 240,000 years ago and the second lineage expanding from the far west around 70,000 years ago. Statistical and biophysical distribution models support these inferences of recent range expansion, with suitable climatic conditions during the last glacial maximum most likely limited to parts of the arid zone north and west of much of the current ranges of these lineages. Combination of phylogeographic analyses and distribution modeling allowed considerably stronger inferences of the history of this complex than either would in isolation, illustrating the power of combining complementary analytical approaches.
系统发育和地理证据表明,许多单性生殖生物是最近进化而来的,并迅速传播。这些模式在我们理解有性繁殖与无性繁殖模式的相对优势方面起着至关重要的作用,但由于缺乏细节,它们的解释往往受到阻碍。在这里,我们结合末次冰期最大值期间其分布的统计和生物物理建模,对澳大利亚壁虎 Heteronotia binoei 这一种脊椎动物的单性生殖体进行了详细的系统地理研究。单性生殖的 Heteronotia binoei 存在于澳大利亚干旱地区,是已知的任何脊椎动物单性生殖体中分布范围最广的。它们与它们的有性对应物广泛共存,而这些有性对应物是通过杂交产生的。我们应用嵌套分类系统地理、有效迁移和不匹配分布分析,对从已知的两个单性生殖线粒体谱系的地理范围内采集的 319 个个体的线粒体 DNA(mtDNA)序列进行了分析。这些分析为从干旱区西部到东部的过去范围扩张事件提供了强有力的证据,并为持续的向东扩张提供了证据。单性生殖的形成和范围扩张事件发生在更新世晚期,其中一个谱系大约在 24 万年前从其目前范围的西北部扩张,第二个谱系大约在 7 万年前从最西部扩张。统计和生物物理分布模型支持这些对最近范围扩张的推断,在末次冰期最大值期间,最适合的气候条件可能仅限于这些谱系当前范围的北部和西部的干旱区的部分地区。系统地理分析和分布建模的结合,使得对这一复杂历史的推断比任何一种分析方法都要有力得多,这说明了结合互补分析方法的力量。