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. 2018 May 25;18:75. doi: 10.1186/s12862-018-1194-1

Fig. 5.

Fig. 5

Modelled climatically suitable areas for the Euphrates poplar in China at different times: (a) the present; (b) the last interglacial (LIG: c. 130 Ka BP); (c) the last glacial maximum (LGM: c. 21 Ka BP) under the Model for Interdisciplinary Research on Climate (MIROC) model; (d) the LGM under the Community Climate System Model (CCSM), and (e) the Pliocene (3 Ma BP). The logistic value of habitat suitability is shown according to the color-scale bars. The map was downloaded from China’s national fundamental geographic information system