4.3 Article

Biogeography and Historical Demography of the Juan Fernndez Rock Lobster, Jasus frontalis (Milne Edwards, 1837)

期刊

JOURNAL OF HEREDITY
卷 104, 期 2, 页码 223-233

出版社

OXFORD UNIV PRESS INC
DOI: 10.1093/jhered/ess141

关键词

coalescence time; glaciations; Juan Fernndez rock lobster; mesoscale oceanographic activity; phylogeography; skyride plot; southeastern Pacific Ocean

资金

  1. Universidad de Concepcion research grant (DIUC) [207.112.098-1.0]
  2. national fund for scientific and technological development grant [FONDECYT 11080110]
  3. Conservation, Research and Education Opportunities (CREO) program
  4. graduate school of the Universidad de Concepcion

向作者/读者索取更多资源

The genetic structure of present-day populations has been highly affected by glacial periods and physical oceanographic forcing, particularly with respect to species distributions and population gene-flow patterns. We assessed the current genetic composition of the Jasus frontalis population in the southeastern Pacific Islands off the coast of Chile to evaluate their connectivity modulated by contemporary and historic oceanographic processes. Population structure and demographical history for this species were assessed based on classic and Bayesian approaches using 84 sequences of cytochrome oxidase subunit I. In addition, we estimated the time of origin of J. frontalis in the different geographic zones. The analyses show a panmictic population with high gene flow between subcomponents and a lack of genetic structure (F-ST < 0.008). This high gene flow is mainly modulated by mesoscale oceanographic factors such as eddies and meanders. In a historical spatial context, the most probable common ancestor of J. frontalis could have colonized the region around 0.258 million years before present (MYBP), first becoming established in the Juan Fernndez Archipelago and then expanding toward the Desventuradas Islands. The demographic history shows a consistent increase in the effective population size (N-e) starting approximately 0.130 MYBP, which is highly correlated with sea-level changes during the last glacial maximum.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.3
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据