The Marine Science Institute, University of the Philippines, Diliman, Quezon City 1101, Philippines.
Mol Ecol. 2010 Oct;19(20):4520-34. doi: 10.1111/j.1365-294X.2010.04803.x. Epub 2010 Sep 28.
Historical isolation during Pleistocene low sea level periods is thought to have contributed to divergence among marine basin populations across the Coral Triangle. In the Philippine archipelago, populations in the South China Sea, Sulu Sea-inland seas, and Philippine Sea-Celebes Sea basins might have been partially isolated. Meanwhile, present-day broadscale oceanographic circulation patterns suggest connectivity between these basins. To evaluate hypotheses regarding the influence of historical and contemporary factors on genetic structure, phylogeographic patterns based on mitochondrial control region sequences for a reef-associated fish, Siganus fuscescens, were analysed. Three distinct lineages were recovered. One lineage was identified as the morphologically similar species Siganus canaliculatus, while two lineages are monophyletic with S. fuscescens. Clade divergence and demographic expansion in S. fuscescens occurred during the Pleistocene. A strong signal of latitudinal structure was detected (Φ(CT) = 0.188), driven by marked differences in clade distribution: one clade is widely distributed (clade A), while a second clade (clade B) has a restricted northern distribution. Regional structure of clade A is consistent with the basin isolation hypothesis (Φ(CT) = 0.040) and suggests isolation of the South China Sea (Φ(CT) = 0.091). Fine-scale structure was observed in the South China Sea and south Philippine Sea, while Sulu Sea and inland seas were unstructured. Genetic structure across multiple spatial scales (archipelagic, regional, and fine-scale within basins) suggests the influence of vicariant barriers and contemporary limits to gene flow in S. fuscescens that may be influenced by oceanographic circulation, geographical distance between available habitats, and latitudinal temperature differences.
历史上的更新世海平面低位时期的隔离被认为是导致珊瑚三角区各海洋盆地种群分歧的原因之一。在菲律宾群岛,南海、苏禄海内陆海和菲律宾海-西里伯斯海盆地的种群可能部分隔离。与此同时,当今广泛的海洋环流模式表明这些盆地之间存在连通性。为了评估历史和当代因素对遗传结构的影响假设,基于与珊瑚礁相关的鱼类 Siganus fuscescens 的线粒体控制区序列的系统地理学模式进行了分析。共发现了三个不同的谱系。一个谱系被鉴定为形态相似的物种 Siganus canaliculatus,而另外两个谱系与 S. fuscescens 是单系的。S. fuscescens 的支系分歧和种群扩张发生在更新世。检测到强烈的纬度结构信号(Φ(CT) = 0.188),这是由支系分布的显著差异驱动的:一个支系分布广泛(支系 A),而第二个支系(支系 B)分布范围狭窄且偏北。支系 A 的区域结构与盆地隔离假说一致(Φ(CT) = 0.040),表明南海(Φ(CT) = 0.091)的隔离。在南海和菲律宾南部海域观察到支系 A 的精细结构,而苏禄海和内陆海则没有结构。多个空间尺度(群岛、区域和盆地内的精细尺度)的遗传结构表明,地理距离、可用栖息地之间的地理距离和纬度温度差异等因素可能影响了 S. fuscescens 中的隔离障碍和当代基因流动限制。