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更新世冰川作用与新西兰一种蜗牛——新西兰泥蜗的系统地理学结构有关。

Pleistocene glaciation is implicated in the phylogeographical structure of Potamopyrgus antipodarum, a New Zealand snail.

作者信息

Neiman Maurine, Lively Curtis M

机构信息

Department of Biology, Indiana University, 1001 E. Third Street, Bloomington, IN 47405, USA.

出版信息

Mol Ecol. 2004 Oct;13(10):3085-98. doi: 10.1111/j.1365-294X.2004.02292.x.

Abstract

Pleistocene glaciation has been identified as an important factor shaping present-day patterns of phylogeographical structure in a diverse array of taxa. The purpose of this study was to use mitochondrial sequence data to address whether Pleistocene glaciation is also a major determinant of phylogeographical patterns in Potamopyrgus antipodarum, a freshwater snail native to New Zealand. We found that haplotypes were separated by no more than 3.7% sequence divergence, and major genetic divisions tended to occur on a north-south axis. These data fit the predictions of the hypothesis that isolation of P. antipodarum in glacial refugia at the northern and southern tip of the South Island of New Zealand during the Pleistocene glaciation underlies the present-day phylogeographical structure. Because sexual P. antipodarum occasionally produce asexual offspring, we also used these data to show that the appearance of asexuality is not phylogeographically constrained. This means that the maintenance of sex in P. antipodarum cannot be wholly due to limited contact between sexual and asexual lineages and must instead be linked to a selective advantage of sexual reproduction.

摘要

更新世冰川作用被认为是塑造当今各类生物地理结构模式的一个重要因素。本研究的目的是利用线粒体序列数据,探讨更新世冰川作用是否也是新西兰本土淡水蜗牛新西兰泥蜗生物地理模式的主要决定因素。我们发现,单倍型之间的序列差异不超过3.7%,主要的遗传分化倾向于发生在南北轴线上。这些数据符合这样一种假设的预测,即在更新世冰川作用期间,新西兰泥蜗在新西兰南岛南北两端的冰川避难所中隔离,构成了当今的生物地理结构。由于有性的新西兰泥蜗偶尔会产生无性后代,我们还利用这些数据表明,无性生殖的出现不受生物地理学的限制。这意味着,新西兰泥蜗有性生殖的维持不能完全归因于有性和无性谱系之间有限的接触,而必须与有性生殖的选择优势相关联。

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