Assessing tiger distributions through the Late Pleistocene can provide insight to the evolutionary histories of currently recognized tiger subspecies. If global tiger ranges have been continuous, and not sufficiently isolated through glacial or interglacial periods, then there should be fewer subspecies than those currently recognized. This paper uses a phylogeographic approach, by modelling tiger distributions for the present day and the Last Glacial Maximum using a maximum entropy framework. Models of the present day and the Last Glacial Maximum have been used to represent interglacial and glacial conditions for the Late Pleistocene respectively; especially with regard to the environmental conditions before and after the ~73ka super-eruption of Toba on the Island of Sumatra. Using models based on 9 bioclimatic variables, tiger range is continuous from the Indian Subcontinent to northeast Siberia during present day conditions. Last Glacial Maximum distributions are reduced to a core, southern area of the Indian Subcontinent and Southeast Asia. The 73ka volcanic eruption of Toba may have reinforced the separation of mainland and Island tigers by drastically reducing tiger populations to southern China and the Islands of Java and Bali. These findings support a growing number of geographic, genetic and morphological studies which call for a reduction in subspecies based on a lack of evidence for their unique evolutionary histories. A single mainland subspecies and a single Sunda Island subspecies is proposed by this study.