Suppr超能文献

扩张年代测定法:末次冰盛期后大陆架扩张对海洋物种分子钟的标定。

Expansion dating: calibrating molecular clocks in marine species from expansions onto the Sunda Shelf Following the Last Glacial Maximum.

机构信息

Department of Biological Sciences, Old Dominion University, University of California, Los Angeles, USA.

出版信息

Mol Biol Evol. 2012 Feb;29(2):707-19. doi: 10.1093/molbev/msr227. Epub 2011 Sep 15.

Abstract

The rate of change in DNA is an important parameter for understanding molecular evolution and hence for inferences drawn from studies of phylogeography and phylogenetics. Most rate calibrations for mitochondrial coding regions in marine species have been made from divergence dating for fossils and vicariant events older than 1-2 My and are typically 0.5-2% per lineage per million years. Recently, calibrations made with ancient DNA (aDNA) from younger dates have yielded faster rates, suggesting that estimates of the molecular rate of change depend on the time of calibration, decaying from the instantaneous mutation rate to the phylogenetic substitution rate. aDNA methods for recent calibrations are not available for most marine taxa so instead we use radiometric dates for sea-level rise onto the Sunda Shelf following the Last Glacial Maximum (starting ∼18,000 years ago), which led to massive population expansions for marine species. Instead of divergence dating, we use a two-epoch coalescent model of logistic population growth preceded by a constant population size to infer a time in mutational units for the beginning of these expansion events. This model compares favorably to simpler coalescent models of constant population size, and exponential or logistic growth, and is far more precise than estimates from the mismatch distribution. Mean rates estimated with this method for mitochondrial coding genes in three invertebrate species are elevated in comparison to older calibration points (2.3-6.6% per lineage per million years), lending additional support to the hypothesis of calibration time dependency for molecular rates.

摘要

DNA 变化率是理解分子进化的一个重要参数,因此也是从系统地理学和系统发生学研究中得出结论的基础。海洋物种线粒体编码区的大多数速率校准都是基于化石和地理隔离事件的分歧时间,这些事件的年龄都超过 1-2 百万年,通常每个谱系每百万年的速率为 0.5-2%。最近,使用来自更年轻日期的古 DNA(aDNA)进行的校准得出了更快的速率,这表明分子变化率的估计取决于校准的时间,从瞬时突变率衰减到系统发育替代率。大多数海洋分类群都没有用于最近校准的 aDNA 方法,因此我们使用末次冰期最大值(约 18000 年前)之后海平面上升的放射性测年数据,这导致了海洋物种的大规模种群扩张。我们没有使用分歧时间进行推断,而是使用了一个两时期的合并模型,对数人口增长之前是一个恒定的人口规模,以推断这些扩张事件开始时的突变单位时间。与恒定种群大小、指数或对数增长的简单合并模型相比,该模型具有更好的拟合效果,而且比不吻合分布的估计要精确得多。与更老的校准点相比,这种方法估计的三个无脊椎动物物种线粒体编码基因的平均速率有所提高(每个谱系每百万年 2.3-6.6%),这进一步支持了分子速率校准时间依赖性的假说。

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验