“…For the AZ, the obvious major refugia are the ancient rocky ranges and plateaus of the Pilbara craton in the west and the Central Ranges in the inland (Figure ; Oliver & McDonald, ; Pepper, Doughty, & Keogh, ; Pepper, Fujita, Moritz, & Keogh, ; Pepper, Ho, Fujita, & Keogh, ). For the MT, major refugia occur in the dissected sandstone plateaus and ranges in the Top End and Kimberley (Potter, Eldridge, Taggart, & Cooper, ; Potter et al, ), as well as karst limestones at the interface of the AZ and MT (Oliver et al, ). Each of these MT refugia has high endemism, and thus, conservation value (Rosauer et al, , ).…”