Abstract

Establishing the dates for the origin and main diversification events in the phylogeny of Ascomycota is among the most crucial remaining goals in understanding the evolution of Fungi. There have been several analyses of divergence times in the fungal tree of life in the last two decades, but most have yielded contrasting results for the origin of the major lineages. Moreover, very few studies have provided temporal estimates for a large set of clades within Ascomycota. We performed molecular dating to estimate the divergence times of most of the major groups of Ascomycota. To account for paleontological uncertainty, we included alternative fossil constraints as different scenarios to enable a discussion of the effect of selection of fossils. We used data from 6 molecular markers and 121 extant taxa within Ascomycota. Our various ‘relaxed clock’ scenarios suggest that the origin and diversification of the Pezizomycotina occurred in the Cambrian. The main lineages of lichen–forming Ascomycota originated at least as early as the Carboniferous, with successive radiations in the Jurassic and Cretaceous generating the diversity of the main modern groups. Our study provides new information about the timing of the main diversification events in Ascomycota, including estimates for classes, orders and families of both lichenized and non–lichenized Ascomycota, many of which had not been previously dated.

Highlights

  • Molecular dating, or the use of DNA sequences to estimate divergence times in phylogenetic trees, is rapidly developing into one of the most exciting applications of phylogenetic systematics [1]

  • Sources of error in the calibration process include the incompleteness of the fossil record, erroneous fossil age estimates, and erroneous placements of fossils on phylogenetic trees [19]

  • Different methods deal with uncertainty associated with the phylogenetic position of fossil calibration points [20,21,22]

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Summary

Introduction

The use of DNA sequences to estimate divergence times in phylogenetic trees, is rapidly developing into one of the most exciting applications of phylogenetic systematics [1]. Different methods have been developed to handle rate heterogeneity [7], some of which attempt to relax the molecular clock assumption by allowing the rate to vary across the tree [8,9,10,11]. These relaxed–clock methods offer greater flexibility in modelling evolutionary events and in incorporating calibrations, which has resulted in a recent discussion about how to calibrate divergence time estimates [11,12,13,14,15,16]. By allowing calibrating information to be represented in the form of parametric distributions, this approach offers a high degree of flexibility to incorporate a time scale into a phylogenetic analysis [16]

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