Castro-Astor Ivandy N, Cracraft Joel, Tello José G, Alves Maria Alice S, Mauck William M, Aleixo Alexandre, Duca Charles, Carnaval Ana Carolina
Department of Biology, City College of New York and Biology Program at CUNY Graduate Center City University of New York New York City New York USA.
Department of Ornithology American Museum of Natural History New York City New York USA.
Ecol Evol. 2024 Dec 9;14(12):e70587. doi: 10.1002/ece3.70587. eCollection 2024 Dec.
We combined mitochondrial DNA sequence data and paleoclimatic distribution models to document phylogeographic patterns and investigate the historical demography of two manakins, and , as well as to explore connections between Amazonia and the Atlantic Forest. ND2 sequences of (75 individuals, 24 sites) and (196, 77) were used in Bayesian inference and maximum likelihood analyses. We estimated mitochondrial nucleotide diversity, employed statistical tests to detect deviations from neutral evolution and constant population sizes, and used species distribution modeling to infer the location of suitable climate for both species under present-day conditions, the Last Glacial Maximum (LGM), and the Last Interglacial Maximum (LIG). Mitochondrial sequence data from indicate one Amazonian and one Atlantic Forest haplogroup. In , we recovered a highly supported and differentiated Atlantic Forest haplogroup embedded within a large Southern Amazonian clade. Genetic and taxonomic structure in Amazonia differs widely between these two species; older has a more marked genetic structure and taxonomic differentiation relative to the younger . Both species have similar genetic patterns in the Atlantic Forest. Paleoclimatic distribution models suggest connections between southwestern Amazonia and the southern Atlantic Forest during the LIG, but not between eastern Amazonia and the northeastern Atlantic Forest, as suggested by previous studies. This indicates that multiple corridors, and at different locations, may have been available over the Pliocene and Pleistocene between these two regions.
我们结合线粒体DNA序列数据和古气候分布模型,以记录系统发育地理格局,研究两种侏儒鸟(物种1和物种2)的历史种群动态,并探索亚马逊地区与大西洋森林之间的联系。物种1(75个个体,24个地点)和物种2(196个个体,77个地点)的ND2序列用于贝叶斯推断和最大似然分析。我们估计了线粒体核苷酸多样性,采用统计检验来检测偏离中性进化和恒定种群大小的情况,并使用物种分布模型来推断在当今条件、末次盛冰期(LGM)和末次间冰期盛期(LIG)下这两个物种适宜气候的位置。来自物种1的线粒体序列数据表明有一个亚马逊单倍群和一个大西洋森林单倍群。在物种2中,我们在一个大型的亚马逊南部分支中发现了一个得到高度支持且分化的大西洋森林单倍群。亚马逊地区这两个物种的遗传和分类结构差异很大;相对于较年轻的物种2,较古老的物种1具有更显著的遗传结构和分类分化。这两个物种在大西洋森林中具有相似的遗传模式。古气候分布模型表明,在末次间冰期盛期,亚马逊西南部与大西洋森林南部之间存在联系,但与先前研究表明的不同,亚马逊东部与大西洋森林东北部之间没有联系。这表明在更新世和上新世期间,这两个地区之间可能在不同位置存在多条通道。