Taylor John W, Berbee Mary L
Department of Plant and Microbial Biology, University of California, Berkeley 94720-3102, USA.
Mycologia. 2006 Nov-Dec;98(6):838-49. doi: 10.3852/mycologia.98.6.838.
The collection of papers in this issue of Mycologia documents considerable improvements in taxon sampling and phylogenetic resolution regarding the Fungal Tree of Life. The new data will stimulate new attempts to date divergences and correlate events in fungal evolution with those of other organisms. Here, we review the history of dating fungal divergences by nucleic acid variation and then use a dataset of 50 genes for 25 selected fungi, plants and animals to investigate divergence times in kingdom Fungi. In particular, we test the choice of fossil calibration points on dating divergences in fungi. At the scale of our analysis, substitution rates varied without showing significant within-lineage correlation, so we used the Langley-Fitch method in the R8S package of computer programs to estimate node ages. Different calibration points had a dramatic effect on estimated divergence dates. The estimate for the age of the Ascomycota/Basidiomycota split was 1808000000 y ago when calibrated assuming that mammals and birds diverged 300000000 y ago, 1489000000 y ago when calibrated assuming that the 400000000 y old fungal fossil Paleopyrenomycites devonicus represents Sordariomycetes and approximately 400000000 y ago when calibrated assuming 206000000 y ago for the plant eudicot/monocot divergence. An advantage of a date of approximately 400000000 y ago for the Ascomycota/Basidiomycota divergence is that the radiation of fungi associated with land plants would not greatly precede the earliest land plant fossils. Acceptance of approximately 400000000 y ago for the Ascomycota/Basidiomycota split would require that P. devonicus be considered a deeply branching Ascomycota. To improve on current estimates of divergence times, mycologists will require calibration points from within groups of fungi that share similar substitution rates. The most useful calibration is likely to depend on the discovery and description of continuous records of fossil fungi, or their spores, that show recognizable shifts in morphology.
本期《真菌学》中的论文集记录了在真菌生命树的分类群采样和系统发育分辨率方面取得的显著进展。新数据将激发新的尝试,以确定分歧时间,并将真菌进化中的事件与其他生物的事件联系起来。在这里,我们回顾了通过核酸变异确定真菌分歧时间的历史,然后使用一个包含25种选定真菌、植物和动物的50个基因的数据集来研究真菌界的分歧时间。特别是,我们测试了在确定真菌分歧时间时化石校准点的选择。在我们的分析尺度上,替换率各不相同,没有显示出明显的谱系内相关性,因此我们使用计算机程序R8S包中的Langley-Fitch方法来估计节点年龄。不同的校准点对估计的分歧日期有显著影响。当假设哺乳动物和鸟类在3亿年前分歧时进行校准时,子囊菌门/担子菌门分裂的年龄估计为18亿年前;当假设4亿年前的真菌化石古双囊菌属代表粪壳菌纲时进行校准时,为14.89亿年前;当假设双子叶植物/单子叶植物分歧时间为2.06亿年前进行校准时,约为4亿年前。子囊菌门/担子菌门分歧时间约为4亿年前的一个优势是,与陆地植物相关的真菌辐射不会大大早于最早的陆地植物化石。接受子囊菌门/担子菌门分裂时间约为4亿年前,将需要把古双囊菌属视为一个分支较深的子囊菌门。为了改进当前对分歧时间的估计,真菌学家将需要来自具有相似替换率的真菌群体内部的校准点。最有用的校准可能取决于发现和描述化石真菌或其孢子的连续记录,这些记录显示出形态上可识别的变化。