Marko Peter B, Zaslavskaya Nadezhda I
School of Life Sciences, University of Hawai'i at Mānoa, Honolulu, Hawai'i, United States of America.
National Scientific Center of Marine Biology, Far Eastern Branch, Russian Academy of Sciences, Vladivostok, Russian Federation.
PeerJ. 2019 Nov 4;7:e7987. doi: 10.7717/peerj.7987. eCollection 2019.
The demographic history of a species can have a lasting impact on its contemporary population genetic structure. Northeastern Pacific (NEP) populations of the rocky shore gastropod have very little mitochondrial DNA (mtDNA) sequence diversity and show no significant population structure despite lacking dispersive planktonic larvae. A contrasting pattern of high mtDNA diversity in the northwestern Pacific (NWP) suggests that may have recently colonized the NEP from the NWP via stepping-stone colonization through the Aleutian-Commander Archipelago (ACA) following the end of the last glacial 20,000 years ago. Here, we use multi-locus sequence data to test that hypothesis using a combination of descriptive statistics and population divergence modeling aimed at resolving the timing and the geographic origin of NEP populations. Our results show that NEP populations share a common ancestor with a population of on the Kamchatka Peninsula ∼46,900 years ago and that NEP populations diverged from each other ∼21,400 years ago. A more recent population divergence between Kamchatka and NEP populations, than between Kamchatka and other populations in the NWP, suggests that the ACA was the most probable dispersal route. Taking into account the confidence intervals for the estimates, we conservatively estimate that arrived in the NEP between 107,400 and 4,100 years ago, a range of dates that is compatible with post-glacial colonization of the NEP. Unlike other congeners that are relatively abundant in the Pleistocene fossil record of the NEP, only one report of exists from the NEP fossil record. Although broadly consistent with the molecular data, the biogeographic significance of these fossils is difficult to evaluate, as the shells cannot be distinguished from the closely-related congener .
一个物种的种群历史会对其当代种群遗传结构产生持久影响。东北太平洋(NEP)多岩石海岸的腹足类动物种群线粒体DNA(mtDNA)序列多样性极低,且尽管缺乏能扩散的浮游幼虫,但种群结构并无显著差异。与之形成对比的是,西北太平洋(NWP)呈现出高mtDNA多样性的模式,这表明该物种可能在2万年前末次冰期结束后,通过阿留申-指挥官群岛(ACA)的踏脚石式殖民,从西北太平洋最近才殖民到东北太平洋。在此,我们使用多位点序列数据,通过描述性统计和种群分化建模相结合的方法来检验这一假设,旨在确定东北太平洋种群的起源时间和地理来源。我们的结果表明,东北太平洋种群在约46900年前与堪察加半岛的一个种群拥有共同祖先,且东北太平洋种群彼此之间在约21400年前发生了分化。堪察加半岛和东北太平洋种群之间的种群分化时间,比堪察加半岛与西北太平洋其他种群之间的分化时间更近,这表明阿留申-指挥官群岛是最有可能的扩散路线。考虑到估计值的置信区间,我们保守估计该物种在107400至4100年前到达东北太平洋,这一日期范围与东北太平洋的冰期后殖民情况相符。与在东北太平洋更新世化石记录中相对丰富的其他同属物种不同,东北太平洋化石记录中该物种仅有一份报告。尽管这些化石在很大程度上与分子数据一致,但由于其贝壳无法与亲缘关系密切的同属物种区分开来,因此这些化石的生物地理学意义难以评估。