4.4 Article

Causations of phylogeographic barrier of some rocky shore species along the Chinese coastline

Journal

BMC EVOLUTIONARY BIOLOGY
Volume 15, Issue -, Pages -

Publisher

BMC
DOI: 10.1186/s12862-015-0387-0

Keywords

Freshwater discharge; Rocky shore species; Life history; Ocean current; Population structure; Substrate

Funding

  1. National Natural Science Foundation of China [41476115 41276126]
  2. National Basic Research Program of China [2013CB956504]
  3. Nature Science funds for Distinguished Young Scholars of Fujian Province, China [2011 J06017]
  4. Fundamental Research Funds for the Central Universities
  5. Program for New Century Excellent Talents in University of Fujian Province
  6. Program for New Century Excellent Talents in University

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Background: 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). Results: Analysis of molecular variance and pairwise FST 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, similar to 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. Conclusions: 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.

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