Wang Jie, Tsang Ling Ming, Dong Yun-Wei
State Key Laboratory of Marine Environmental Science, College of Marine and Earth Sciences, Xiamen University, Xiamen, China.
Marine Biodiversity and Global Change Laboratory, Xiamen University, Xiamen, China.
BMC Evol Biol. 2015 Jun 15;15:114. doi: 10.1186/s12862-015-0387-0.
Substrate, ocean current and freshwater discharge are recognized as important factors that control the larval dispersal and recruitment of intertidal species. Life history traits of individual species will determine the differential responses to these physical factors, and hence resulting in contrasting phylogeography across the same biogeographic barrier. To determine how these factors affect genetic structure of rocky shore species along the China coast, a comparative phylogeographic study of four intertidal and subtidal species was conducted using mitochondrial and nuclear DNA by combining new sequences from Siphonaria japonica with previously published sequences from three species (Cellana toreuma, Sargassum horneri and Atrina pectinata).
Analysis of molecular variance and pairwise ΦST revealed significant genetic differences between the Yellow Sea (YS) and the other two marginal seas (East China Sea, ECS and South China Sea, SCS) for rocky-shore species (S. japonica, C. toreuma, S. horneri), but not for muddy-shore species Atrina pectinata. Demographic history analysis proved that the population size of all these four species were persistent though the Last Glacial Maximum (LGM, ~20 ka BP). Migration analysis revealed that gene flow differentiated northward and southward migration for these four species. However, the inferred direction of gene flow using alternatively mitochondrial or nuclear markers was contradictory in S. japonica.
It is concluded that there is a phylogeographical break at the Yangtze River estuary for the rocky shore species and the causation of the barrier is mainly due to the unsuitable substratum and freshwater discharge. All four intertidal and subtidal species appear to have persisted through the LGM in China, indicating the lower impact of LGM on intertidal and subtidal species than generally anticipated. The imbalanced gene flow between YS and ESCS groups for these four species could be explained by historical refugia. The discordance between mitochondrial and nuclear markers in the MIGRATE analysis of S. japonica prove the importance of employing multi-locus data in biogeographic study. Climate change, land reclamation and dam construction, which are changing substrate and hydrological conditions around Yangtze River estuary, will consequently affect the biogeographic pattern of intertidal species.
底物、洋流和淡水排放被认为是控制潮间带物种幼体扩散和补充的重要因素。单个物种的生活史特征将决定其对这些物理因素的不同反应,从而导致在相同生物地理屏障上形成截然不同的系统地理学格局。为了确定这些因素如何影响中国沿海岩岸物种的遗传结构,我们结合日本笠贝的新序列和先前发表的三个物种(龟足、铜藻和栉江珧)的序列,利用线粒体和核DNA对四种潮间带和潮下带物种进行了比较系统地理学研究。
分子方差分析和成对ΦST分析表明,岩岸物种(日本笠贝、龟足、铜藻)在黄海与其他两个边缘海(东海和南海)之间存在显著的遗传差异,但泥岸物种栉江珧不存在这种差异。种群历史分析证明,在末次盛冰期(约20 ka BP)期间,这四个物种的种群数量都保持稳定。迁移分析表明,这四个物种的基因流在南北方向上存在差异。然而,在日本笠贝中,使用线粒体或核标记推断的基因流方向是相互矛盾的。
得出结论,长江口对于岩岸物种存在系统地理学间断,其屏障的形成主要是由于不合适的底物和淡水排放。所有四种潮间带和潮下带物种在中国似乎都在末次盛冰期期间存活下来,这表明末次盛冰期对潮间带和潮下带物种的影响比一般预期的要小。这四个物种在黄海和东海-南海组之间的基因流不平衡可以用历史避难所来解释。在日本笠贝的MIGRATE分析中,线粒体和核标记之间的不一致证明了在生物地理学研究中使用多基因座数据的重要性。气候变化、围垦和大坝建设正在改变长江口周围的底物和水文条件,这将进而影响潮间带物种的生物地理格局。