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. 2019 Apr 17;10:812. doi: 10.3389/fmicb.2019.00812

FIGURE 3.

FIGURE 3

Chronogram and estimated divergence times of Sanghuangporus generated by molecular clock analysis using the two concatenated datasets (ITS+nrLSU and EF1-α+RPB1+RPB2) dataset. The chronogram was obtained using the Ascomycota–Basidiomycota divergence time of 582 Mya as the calibration point. The calibration point and objects of this study are marked in the chronogram. The geological time scale is in millions of years ago (Mya).