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更新世期间,两极地衣长松萝向南半球扩张。

Pleistocene expansion of the bipolar lichen Cetraria aculeata into the Southern hemisphere.

机构信息

Abt. Botanik und Molekulare Evolutionsforschung, Senckenberg Forschungsinstitut und Naturmuseum, Frankfurt am Main, Germany.

出版信息

Mol Ecol. 2013 Apr;22(7):1961-83. doi: 10.1111/mec.12210. Epub 2013 Feb 12.

Abstract

Many boreal and polar lichens occupy bipolar distributional ranges that frequently extend into high mountains at lower latitudes. Although such disjunctions are more common among lichens than in other groups of organisms, the geographic origin of bipolar lichen taxa, and the way and time frame in which they colonized their ranges have not been studied in detail. We used the predominantly vegetative, widespread lichen Cetraria aculeata as a model species. We surveyed the origin and history of its bipolar pattern using population genetics, phylogenetic and genealogical reconstruction methods. Cetraria aculeata originated in the Northern Hemisphere and dispersed southwards during the Pleistocene. The genetic signal suggests a Pleistocene dispersive burst in which a population size expansion concurred with the acquisition of a South-American range that culminated in the colonization of the Antarctic.

摘要

许多北方和极地地衣占据了两极分布范围,这些范围经常延伸到低纬度的高山地区。尽管这种不连续现象在地衣中比在其他生物群中更为常见,但两极地衣分类群的地理起源以及它们殖民其范围的方式和时间框架尚未得到详细研究。我们使用广泛分布的地衣,即主要为营养体的Cetraria aculeata 作为模式物种。我们使用种群遗传学、系统发育和系统发育重建方法来调查其两极模式的起源和历史。Cetraria aculeata 起源于北半球,并在更新世期间向南扩散。遗传信号表明,在更新世扩散爆发期间,种群规模扩大与获得南美的范围相吻合,最终导致南极的殖民化。

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