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. 2017 Apr 20;17:102. doi: 10.1186/s12862-017-0948-5

Fig. 3.

Fig. 3

Chronogram and estimated divergence times of Laetiporus generated from molecular clock analysis using the ITS + nrLSU + nrSSU and EF-1α + RPB2 datasets. A chronogram obtained using the Ascomycota–Basidiomycota divergence time of 582 Mya as the calibration point is shown. The calibration point and objects of this study are marked in the chronogram. The lineages in the Polyporales are highlighted in green. The geological time scale is in millions of years ago (Mya)