Cortés-Ortiz L, Bermingham E, Rico C, Rodríguez-Luna E, Sampaio I, Ruiz-García M
School of Biological Sciences, University of East Anglia, UK.
Mol Phylogenet Evol. 2003 Jan;26(1):64-81. doi: 10.1016/s1055-7903(02)00308-1.
We take advantage of the broad distribution of howler monkeys from Mexico to Argentina to provide a historical biogeographical analysis on a regional scale that encompasses the entire Neotropics. The phylogenetic relationships among 9 of the 10 recognized Alouatta species were inferred using three mitochondrial and two nuclear genes. The nuclear gene regions provided no phylogenetic resolution among howler monkey species, and were characterized by very low levels of sequence divergence between Alouatta and the Ateles outgroup. The mtDNA genes, on the other hand, produced a well-resolved phylogeny, which indicated that the earliest split among howler monkeys separated cis- and trans-Andean clades. Eight monophyletic mtDNA haplotype clades were identified, representing six named species in South America, including Alouatta seniculus, Alouatta sara, Alouatta macconelli, Alouatta caraya, Alouatta belzebul, and Alouatta guariba, and two in Mesoamerica, Alouatta pigra and Alouatta palliata. Molecular clock-based estimates of branching times indicated that contemporary howler monkey species originated in the late Miocene and Pliocene, not the Pleistocene. The causes of Alouatta diversification were more difficult to pin down, although we posit that the initial cis-, trans-Andean split in the genus was caused by the late Miocene completion of the northern Andes. Riverine barriers to dispersal and putative forest refuges can neither be discounted nor distinguished as causes of speciation in many cases, and one, the other or both have likely played a role in the diversification of South American howler monkeys. Finally, we estimated the separation of Mesoamerican A. pigra and A. palliata at 3Ma, which corresponds to the completion date of the Panama Isthmus promoting a role for this earth history event in the speciation of Central American howler monkeys.
我们利用吼猴从墨西哥到阿根廷的广泛分布,在涵盖整个新热带界的区域尺度上进行历史生物地理学分析。利用三个线粒体基因和两个核基因推断了10种已知吼猴属物种中9种的系统发育关系。核基因区域在吼猴物种之间没有提供系统发育分辨率,其特征是吼猴属与蜘蛛猴外类群之间的序列分歧水平非常低。另一方面,线粒体DNA基因产生了一个分辨率良好的系统发育树,这表明吼猴最早的分化将安第斯山脉以东和以西的分支分开。鉴定出了八个单系线粒体DNA单倍型分支,代表了南美洲的六个指名物种,包括红吼猴、黄臂吼猴、麦氏吼猴、褐吼猴、鬃毛吼猴和圭亚那吼猴,以及中美洲的两个物种,中美吼猴和白喉吼猴。基于分子钟的分支时间估计表明,当代吼猴物种起源于中新世晚期和上新世,而非更新世。吼猴多样化的原因更难确定,尽管我们推测该属最初的安第斯山脉以东和以西的分化是由安第斯山脉北部在中新世晚期形成所导致的。在许多情况下,河流扩散障碍和假定的森林避难所都不能被排除或区分是物种形成的原因,其中一个、另一个或两者都可能在南美洲吼猴的多样化过程中发挥了作用。最后,我们估计中美洲的中美吼猴和白喉吼猴在300万年前分离,这与巴拿马地峡的形成时间相对应,表明这一地球历史事件在中美洲吼猴的物种形成中起到了作用。