Fig. 3From: Influence of Pleistocene climate fluctuations on the demographic history and distribution of the critically endangered Chinese pangolin (Manis pentadactyla)Species distribution models for the Chinese pangolin. a to (d) are the potential suitable areas in the current and historical (Mid-Holocene [MH], 5–7.5 ka, last glacial maximum [LGM], ~ 21 ka, and the last interglacial [LIG], 120–140 ka) times, respectively. Colours indicate the probability of occurrence as predicted by MAXENT [23]Back to article page