Bagley Justin C, Heming Neander M, Gutiérrez Eliécer E, Devisetty Upendra K, Mock Karen E, Eckert Andrew J, Strauss Steven H
Plant Evolutionary Genomics Laboratory Department of Biology Virginia Commonwealth University Richmond VA USA.
Departamento de Zoologia Instituto de Ciências Biológicas Universidade de Brasília Brasília Brazil.
Ecol Evol. 2020 Apr 23;10(11):4609-4629. doi: 10.1002/ece3.6214. eCollection 2020 Jun.
is the widest-ranging tree species in North America and an ecologically important component of mesic forest ecosystems displaced by the Pleistocene glaciations. Using phylogeographic analyses of genome-wide SNPs (34,796 SNPs, 183 individuals) and ecological niche modeling, we inferred population structure, ploidy levels, admixture, and Pleistocene range dynamics of , and tested several historical biogeographical hypotheses. We found three genetic lineages located mainly in coastal-Cascades (cluster 1), east-slope Cascades-Sierra Nevadas-Northern Rockies (cluster 2), and U.S. Rocky Mountains through southern Canadian (cluster 3) regions of the range, with tree graph relationships of the form ((cluster 1, cluster 2), cluster 3). Populations consisted mainly of diploids (86%) but also small numbers of triploids (12%) and tetraploids (1%), and ploidy did not adversely affect our genetic inferences. The main vector of admixture was from cluster 3 into cluster 2, with the admixture zone trending northwest through the Rocky Mountains along a recognized phenotypic cline (Utah to Idaho). Clusters 1 and 2 provided strong support for the "stable-edge hypothesis" that unglaciated southwestern populations persisted in situ since the last glaciation. By contrast, despite a lack of clinal genetic variation, cluster 3 exhibited "trailing-edge" dynamics from niche suitability predictions signifying complete northward postglacial expansion. Results were also consistent with the "inland dispersal hypothesis" predicting postglacial assembly of Pacific Northwestern forest ecosystems, but rejected the hypothesis that Pacific-coastal populations were colonized during outburst flooding from glacial Lake Missoula. Overall, congruent patterns between our phylogeographic and ecological niche modeling results and fossil pollen data demonstrate complex mixtures of stable-edge, refugial locations, and postglacial expansion within . These findings confirm and refine previous genetic studies, while strongly supporting a distinct Pacific-coastal genetic lineage of quaking aspen.
是北美分布范围最广的树种,也是被更新世冰川作用取代的中生森林生态系统的重要生态组成部分。利用全基因组单核苷酸多态性(34796个单核苷酸多态性,183个个体)的系统发育地理分析和生态位建模,我们推断了该树种的种群结构、倍性水平、混合情况和更新世范围动态,并检验了几个历史生物地理学假设。我们发现三个遗传谱系,主要位于沿海-喀斯喀特山脉(聚类1)、喀斯喀特山脉东坡-内华达山脉-北落基山脉(聚类2)以及美国落基山脉至加拿大南部(聚类3)的分布区域,树形图关系为((聚类1, 聚类2), 聚类3)。种群主要由二倍体(86%)组成,但也有少量三倍体(12%)和四倍体(1%),倍性并未对我们的遗传推断产生不利影响。混合的主要载体是从聚类3到聚类2,混合区域沿着一条公认的表型渐变群(从犹他州到爱达荷州)向西北穿过落基山脉。聚类1和聚类2为“稳定边缘假说”提供了有力支持,即未受冰川影响的西南种群自上一次冰川作用以来一直原地留存。相比之下,尽管缺乏渐变的遗传变异,但聚类3从生态位适宜性预测中表现出“后缘”动态,表明其在冰期后完全向北扩张。结果也与“内陆扩散假说”一致,该假说预测了西北太平洋森林生态系统的冰期后组装,但拒绝了太平洋沿岸种群在米苏拉冰川湖爆发洪水期间被殖民的假说。总体而言,我们的系统发育地理和生态位建模结果与化石花粉数据之间的一致模式表明,该树种内部存在稳定边缘、避难所位置和冰期后扩张的复杂混合情况。这些发现证实并完善了先前的遗传研究,同时有力地支持了颤杨独特的太平洋沿岸遗传谱系。