Lehnert Sarah J, DiBacco Claudio, Jeffery Nicholas W, Blakeslee April M H, Isaksson Jonatan, Roman Joe, Wringe Brendan F, Stanley Ryan R E, Matheson Kyle, McKenzie Cynthia H, Hamilton Lorraine C, Bradbury Ian R
Northwest Atlantic Fisheries Centre Fisheries and Oceans Canada St. John's Newfoundland Canada.
Bedford Institute of Oceanography Fisheries and Oceans Canada Dartmouth Nova Scotia Canada.
Evol Appl. 2018 Jun 28;11(9):1656-1670. doi: 10.1111/eva.12657. eCollection 2018 Oct.
Two genetically distinct lineages of European green crabs () were independently introduced to eastern North America, the first in the early 19th century and the second in the late 20th century. These lineages first came into secondary contact in southeastern Nova Scotia, Canada (NS), where they hybridized, producing latitudinal genetic clines. Previous studies have documented a persistent southward shift in the clines of different marker types, consistent with existing dispersal and recruitment pathways. We evaluated current clinal structure by quantifying the distribution of lineages and fine-scale hybridization patterns across the eastern North American range (25 locations, ~39 to 49°N) using informative single nucleotide polymorphisms (SNPs; = 96). In addition, temporal changes in the genetic clines were evaluated using mitochondrial DNA and microsatellite loci ( = 9-11) over a 15-year period (2000-2015). Clinal structure was consistent with prior work demonstrating the existence of both northern and southern lineages with a hybrid zone occurring between southern New Brunswick (NB) and southern NS. Extensive later generation hybrids were detected in this region and in southeastern Newfoundland. Temporal genetic analysis confirmed the southward progression of clines over time; however, the rate of this progression was slower than predicted by forecasting models, and current clines for all marker types deviated significantly from these predictions. Our results suggest that neutral and selective processes contribute to cline dynamics, and ultimately, highlight how selection, hybridization, and dispersal can collectively influence invasion success.
欧洲绿蟹()的两个基因不同的谱系被独立引入北美东部,第一个在19世纪初,第二个在20世纪末。这些谱系首次在加拿大新斯科舍省东南部(NS)发生二次接触,在那里它们杂交,形成了纬度遗传渐变群。先前的研究记录了不同标记类型的渐变群持续向南移动,这与现有的扩散和补充途径一致。我们通过使用信息性单核苷酸多态性(SNP;=96)量化北美东部范围内(25个地点,约北纬39至49度)谱系的分布和精细尺度的杂交模式,评估了当前的渐变群结构。此外,在15年期间(2000 - 2015年),使用线粒体DNA和微卫星位点(=9 - 11)评估了遗传渐变群的时间变化。渐变群结构与先前的研究一致,表明存在北部和南部谱系,杂交带出现在新不伦瑞克省南部(NB)和新斯科舍省南部之间。在该地区和纽芬兰岛东南部检测到大量的后代杂种。时间遗传分析证实了渐变群随时间向南推进;然而,这种推进速度比预测模型预测的要慢,并且所有标记类型的当前渐变群与这些预测有显著偏差。我们的结果表明,中性和选择性过程促成了渐变群动态,最终突出了选择、杂交和扩散如何共同影响入侵成功。