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. 2020 Nov 1;7:184. doi: 10.1038/s41438-020-00407-9

Fig. 6. Paleoelevation and paleovegetation of the Upper Eocene (~36 Ma BP) and the last Quaternary glaciation (~70–10 ka BP) for two types of mountain ranges studied based on previous studies.

Fig. 6

The potential migration path and evolutionary history of Chrysanthemum and its allies was proposed based on comprehensive analysis of present-day (this study) and ancient topography and vegetation