Figure 5 in Genetic homogeneity in a Pontocaspian crested newt species (Triturus karelinii) suggests recent isolation of its three allopatric range sections

Figure 5. Species distribution model for Triturus karelinii projected on climate layers for the present, the mid-Holocene (mid-Holo, ∼6 Ka), the Last Glacial Maximum (LGM, ∼22 Ka) and the Last Interglacial (∼130 Ka). For the mid-Holocene and the Last Glacial Maximum projections on data layers based on the CCSM4 (CCSM) and MIROC-ESM (MIROC) model are shown. Warmer colours reflect a higher predicted suitability.