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中美洲枫香(枫香科)的系统地理学:北美的中新世广泛温带森林(或云雾林)的幸存者?

Phylogeography of Liquidambar styraciflua (Altingiaceae) in Mesoamerica: survivors of a Neogene widespread temperate forest (or cloud forest) in North America?

机构信息

Departamento de Biología Evolutiva, Instituto de Ecología, A.C. Xalapa, Veracruz, 91070, México ; Red de Biodiversidad y Sistemática, Centro Regional del Bajío, Instituto de Ecología, A.C. Pátzcuaro, Michoacán, 61600, México.

Departamento de Biología Evolutiva, Instituto de Ecología, A.C. Xalapa, Veracruz, 91070, México.

出版信息

Ecol Evol. 2014 Feb;4(4):311-28. doi: 10.1002/ece3.938. Epub 2014 Jan 10.

Abstract

We investigate the genetic variation between populations of the American sweetgum (Liquidambar styraciflua), a tree species with a disjunct distribution between northeastern Texas and Mexico, by analyzing sequences of two chloroplast DNA plastid regions in Mesoamerica. Our results revealed phylogeographical structure, with private haplotypes distributed in unique environmental space at either side of the Trans-Mexican Volcanic Belt, and a split in the absence of gene flow dating back ca. 4.2-1.4 million years ago (MYA). Species distribution modeling results fit a model of refugia along the Gulf and Atlantic coasts but the present ranges of US and Mesoamerican populations persisted disjunct during glacial/interglacial cycles. Divergence between the US and Mesoamerican (ca. 8.4-2.8 MYA) populations of L. styraciflua and asymmetrical gene flow patterns support the hypothesis of a long-distance dispersal during the Pliocene, with fragmentation since the most recent glacial advance (120,000 years BP) according to coalescent simulations and high effective migration rates from Mesoamerica to the USA and close to zero in the opposite direction. Our findings implicate the Trans-Mexican Volcanic Belt as a porous barrier driving genetic divergence of L. styraciflua, corresponding with environmental niche differences, during the Pliocene to Quaternary volcanic arc episode 3.6 MYA, and a Mesoamerican origin of populations in the USA.

摘要

我们通过分析中美洲两个叶绿体 DNA 质地区域的序列,研究了具有不连续分布的美国枫香树(Liquidambar styraciflua)种群之间的遗传变异。我们的研究结果揭示了系统地理学结构,特有单倍型分布在特文斯墨西哥火山带两侧独特的环境空间中,并且存在约 420 万至 140 万年(MYA)前的无基因流分裂。物种分布模型的结果符合海湾和大西洋沿岸避难所的模型,但美国和中美洲种群的当前范围在冰期/间冰期循环期间一直是不连续的。美国和中美洲(约 840 万至 280 万年)枫香树种群之间的分化和不对称的基因流模式支持上新世长距离扩散的假说,自最近一次冰川推进(12 万年前)以来发生了断裂,根据合并模拟和从中美洲到美国的高有效迁移率接近零,而从美国到中美洲的反向迁移率接近零。我们的研究结果表明,特文斯墨西哥火山带是一个多孔屏障,在 360 万年至第四纪火山弧事件期间,导致枫香树的遗传分化,这与上新世至第四纪的环境生态位差异相对应,并且美国的种群起源于中美洲。

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