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首页> 外文期刊>Evolution: International Journal of Organic Evolution >INTRASPECIFIC PHYLOGEOGRAPHY OF NORTH AMERICAN HIGHLAND FISHES - A TEST OF THE PLEISTOCENE VICARIANCE HYPOTHESIS
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INTRASPECIFIC PHYLOGEOGRAPHY OF NORTH AMERICAN HIGHLAND FISHES - A TEST OF THE PLEISTOCENE VICARIANCE HYPOTHESIS

机译:北美高地鱼类的种内显微照相-更新世相变假说的一项试验

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摘要

The highland fish fauna of eastern North America consists of Appalachian and Ozark centers of endemism separated by the intervening Glacial Till plains. Clades within these areas are more closely related phylogenetically to each other than to clades occurring in the intervening formerly glaciated region, suggesting that the Pleistocene glaciations fragmented a widespread highland region and its associated fauna. Alternatively, it is possible that these faunal assemblages predate the glaciations or that recent dispersals may have been more important than vicariance in determining faunal compositions. We examined the relationships among mitochondrial DNA (mtDNA) haplotypes within five clades of highland fishes, each with a distribution suggestive of a Pleistocene vicariance event. Darters of the subgenera Litocara and Odontopholis have distributions and mtDNA relationships that are consistent with the Pleistocene integration and burial of the Teays-Mahomet valley, a major drainage of the early Pleistocene. The distribution and mtDNA relationships among subspecies of Erimystax dissimilis are not consistent with Pleistocene vicariance, but relationships among Appalachian haplotypes are consistent with the late Pleistocene integration of the modern Ohio River system. Both Cottus carolinae and the Fundulus catenatus species group have representatives in the Mobile basin consistent with pre-Pleistocene divergences. Three haplotype clusters were found in C. carolinae, corresponding to the Appalachian, Ozark, and upper Kanawha River populations. However, Appalachian and Ozark F. catenatus populations are paraphyletic with respect to each other. This, coupled with a relatively low degree of sequence divergence, suggests that no long-term barriers to gene flow exist for C. carolinae and F. catenatus. These three distinct phylogeographic patterns indicate that Pleistocene vicariance is not the only explanation for the Appalachian-Ozark distribution of highland fish communities. [References: 54]
机译:北美东部的高原鱼类区系由阿巴拉契亚和奥扎克地方性中心组成,中间由冰川耕种平原隔开。这些区域内的进化枝在系统发育上彼此之间的联系比与之前的冰川时期的进化枝之间的亲缘关系更为紧密,这表明更新世冰川将一个广阔的高原地区及其相关动物区分开了。或者,这些动物群可能早于冰川时期,或者在确定动物群组成方面,最近的散布可能比变异更为重要。我们检查了5个高地鱼类进化枝中线粒体DNA(mtDNA)单倍型之间的关系,每种分布都暗示了更新世的迁徙事件。 Litocara和Odontopholis属的突进者具有分布和mtDNA关系,与早更新世的主要排水区Teays-Mahomet山谷的更新世整合和埋葬相一致。 rim草亚种间亚种间的分布和mtDNA关系与更新世的变异不一致,但阿巴拉契亚单体型之间的关系与现代俄亥俄河系统的更新世晚期整合一致。卡特斯卡罗莱纳州科和底孔雀科物种组在移动盆地中都具有代表,这与前更新世前的发散一致。在卡罗莱纳州发现了三个单体型簇,分别对应于阿巴拉契亚,奥扎克和卡纳瓦哈河上游种群。但是,阿巴拉契亚和Ozark catenatus种群彼此之间是共生的。这,加上相对较低的序列差异,表明C. carolinae和F. catenatus不存在长期的基因流动障碍。这三种不同的系统地理学模式表明,更新世的变化并不是高原鱼类群落的阿巴拉契亚-欧扎克分布的唯一解释。 [参考:54]

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