Morris Ashley B, Ickert-Bond Stefanie M, Brunson D Burke, Soltis Douglas E, Soltis Pamela S
Department of Biology, University of South Alabama, Mobile, AL 36688, USA.
Mol Ecol. 2008 Sep;17(17):3889-900. doi: 10.1111/j.1365-294X.2008.03875.x. Epub 2008 Jul 24.
Eastern North American plant biogeography has traditionally focused on two primary issues: (i) the location of temperate Pleistocene refugia and their proximity to the southern margin of the ice sheet during the last glacial maximum, and (ii) the origin of the temperate element of northern Latin America. While numerous population genetic and phylogeographical studies have focused on the first issue, few (if any) have considered the second. We addressed these issues by surveying 117 individuals from 24 populations of Liquidambar styraciflua (American sweetgum; Altingiaceae) across the southeastern USA, eastern Mexico, and Guatemala, using more than 2200 bp of chloroplast DNA sequence data. To specifically address the issue of timing, we estimated intraspecific divergence times on the basis of multiple fossil-based calibration points, using taxa from Altingiaceae (Liquidambar and Altingia) and Hammamelidaceae (Hamamelis) as outgroups. More than half of the sampled localities exhibited multiple haplotypes. Remarkably, the greatest variation was observed within the USA, with Mexico and Guatemala sharing widespread haplotypes with Texas, Mississippi, Kentucky, Ohio, and northern Virginia. This lack of differentiation suggests shared ancestral polymorphisms, and that the genetic signal we observed is older than the disjunction itself. Our data provide support for previously proposed hypotheses of Pleistocene refugia in peninsular Florida and along the eastern Atlantic, but also for deeper divergences (approximately 8 million years ago) within the USA. These patterns reflect a dynamic biogeographical history for eastern North American trees, and emphasize the importance of the inclusion of a temporal component in any phylogeographical study.
传统上,北美东部植物生物地理学主要关注两个主要问题:(i)温带更新世避难所的位置以及它们在末次盛冰期时与冰盖南缘的距离,以及(ii)拉丁美洲北部温带成分的起源。虽然众多的种群遗传学和系统地理学研究都集中在第一个问题上,但很少有研究(如果有的话)考虑第二个问题。我们通过对来自美国东南部、墨西哥东部和危地马拉的24个北美枫香(金缕梅科)种群的117个个体进行调查,使用超过2200 bp的叶绿体DNA序列数据来解决这些问题。为了具体解决时间问题,我们基于多个基于化石的校准点估计种内分歧时间,使用金缕梅科(枫香属和蕈树属)和金缕梅科(金缕梅属)的分类群作为外类群。超过一半的采样地点呈现出多种单倍型。值得注意的是,在美国境内观察到的变异最大,墨西哥和危地马拉与得克萨斯州、密西西比州、肯塔基州、俄亥俄州和弗吉尼亚州北部共享广泛分布的单倍型。这种缺乏分化表明存在共同的祖先多态性,并且我们观察到的遗传信号比分布间断本身更古老。我们的数据为先前提出的佛罗里达半岛和沿大西洋东部存在更新世避难所的假设提供了支持,但也为美国境内更深层次的分歧(约800万年前)提供了支持。这些模式反映了北美东部树木动态的生物地理历史,并强调了在任何系统地理学研究中纳入时间成分的重要性。