Chattopadhyay Balaji, Garg Kritika M, Gwee Chyi Yin, Edwards Scott V, Rheindt Frank E
Department of Biological Sciences, National University of Singapore, 117543, Singapore, Republic of Singapore.
Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, 02138, MA, USA.
BMC Evol Biol. 2017 Sep 1;17(1):210. doi: 10.1186/s12862-017-1047-3.
Pleistocene climatic fluctuations are known to be an engine of biotic diversification at higher latitudes, but their impact on highly diverse tropical areas such as the Andes remains less well-documented. Specifically, while periods of global cooling may have led to fragmentation and differentiation at colder latitudes, they may - at the same time - have led to connectivity among insular patches of montane tropical habitat with unknown consequences on diversification. In the present study we utilized ~5.5 kb of DNA sequence data from eight nuclear loci and one mitochondrial gene alongside diagnostic morphological and bioacoustic markers to test the effects of Pleistocene climatic fluctuations on diversification in a complex of Andean tyrant-flycatchers of the genus Elaenia.
Population genetic and phylogenetic approaches coupled with coalescent simulations demonstrated disparate levels of gene flow between the taxon chilensis and two parapatric Elaenia taxa predominantly during the last glacial period but not thereafter, possibly on account of downward shifts of montane forest habitat linking the populations of adjacent ridges. Additionally, morphological and bioacoustic analyses revealed a distinct pattern of character displacement in coloration and vocal traits between the two sympatric taxa albiceps and pallatangae, which were characterized by a lack of gene flow.
Our study demonstrates that global periods of cooling are likely to have facilitated gene flow among Andean montane Elaenia flycatchers that are more isolated from one another during warm interglacial periods such as the present era. We also identify a hitherto overlooked case of plumage and vocal character displacement, underpinning the complexities of gene flow patterns caused by Pleistocene climate change across the Andes.
更新世气候波动是高纬度地区生物多样性分化的一个驱动力,但其对安第斯山脉等生物多样性极高的热带地区的影响,记录尚不充分。具体而言,全球变冷时期可能导致了寒冷纬度地区的生物片段化和分化,但与此同时,也可能导致了山地热带栖息地岛屿状斑块之间的连通性,而这对生物多样性分化的影响尚不清楚。在本研究中,我们利用来自8个核基因座和1个线粒体基因的约5.5 kb DNA序列数据,以及诊断性形态学和生物声学标记,来测试更新世气候波动对埃拉尼亚属安第斯霸鹟复合体生物多样性分化的影响。
群体遗传学和系统发育方法,再加上溯祖模拟,表明在末次冰期期间,智利霸鹟分类单元与两个邻域分布的埃拉尼亚分类单元之间的基因流水平不同,但此后则不然,这可能是由于连接相邻山脊种群的山地森林栖息地向下迁移所致。此外,形态学和生物声学分析揭示了两个同域分布的分类单元白枕霸鹟和苍白霸鹟在颜色和鸣声特征上存在明显的性状替换模式,其特点是缺乏基因流。
我们的研究表明,全球变冷时期可能促进了安第斯山地埃拉尼亚霸鹟之间的基因流,而在当前这样的温暖间冰期,它们彼此之间的隔离程度更高。我们还发现了一个迄今为止被忽视的羽毛和鸣声性状替换案例,这突显了更新世气候变化在安第斯山脉造成的基因流模式的复杂性。