Maximum clade credibility chronogram for the major groups of Ascomycota.
The chronogram is the result from the BEAST analysis of Scenario 4. Each node represents the mean divergence time estimate and bars show their associated 95% credibility interval. Numbers corresponding to dated groups shown in Table 3 are written above the nodes.

Maximum clade credibility chronogram for the major groups of Ascomycota. The chronogram is the result from the BEAST analysis of Scenario 4. Each node represents the mean divergence time estimate and bars show their associated 95% credibility interval. Numbers corresponding to dated groups shown in Table 3 are written above the nodes.

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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 t...

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... We identified two examples of HGT within ascomycete fungi where the same elements have recently generated introns among highly divergent lineages (Fig. 3A). Xylaria and Lasiodiplodia last shared a common ancestor approximately 350 MYA (29,30). Nonetheless, each species' genome contains an introner family with 83.8% sequence similarity across the complete 134bp sequence between elements found in either lineage ( Fig. 3B; table S4). ...
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... It has been widely used and it is still used in dating the fungal tree of life 26 . However, whether it is basal to the Ascomycota or nested within the subphylum Pezizomycotina is contentious and its position varies depending on the studies and data used leading to strikingly different age estimates for the same divergence events (e.g., 26,[64][65][66][67][68][69]. For example, Lücking et al. 66 considered using this fossil to calibrate three alternative positions in the Ascomycota tree: origin of Sordariomycetes, divergence of Pezizomycotina, and origin of Pezizomycotina. ...
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... The broader basal region distally tapered to a short or cylindrical beak with or without a dark thickened tip [123] . The species was found from Iceberg Bay formation at Kanguk Peninsula, Axel Heiberg Island and Northwest Territories, Canada with an estimated age during the late Palaeocene or early Eocene (40.4-58.7 MYA) [123] . However, the link between P. alternariatus and Alternaria has not yet been confirmed due to Alternaria being variable in shape, size and septation of conidium and was shown to be a species complex [11][12][13][14]22,55,123] . ...
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... The species was referred to Alternaria in forming muriform, ovoid to obclavate, rostrate, pale brown to brown conidia, arising singly or in clusters, with transverse septa more prominent and thicker than the longitudinal or oblique septa. The broader basal region distally tapered to a short or cylindrical beak with or without a dark thickened tip [123] . The species was found from Iceberg Bay formation at Kanguk Peninsula, Axel Heiberg Island and Northwest Territories, Canada with an estimated age during the late Palaeocene or early Eocene (40.4-58.7 MYA) [123] . ...
... The broader basal region distally tapered to a short or cylindrical beak with or without a dark thickened tip [123] . The species was found from Iceberg Bay formation at Kanguk Peninsula, Axel Heiberg Island and Northwest Territories, Canada with an estimated age during the late Palaeocene or early Eocene (40.4-58.7 MYA) [123] . However, the link between P. alternariatus and Alternaria has not yet been confirmed due to Alternaria being variable in shape, size and septation of conidium and was shown to be a species complex [11][12][13][14]22,55,123] . ...