“…Plio‐Pleistocene) climate oscillations is of great utility for understanding the evolution of organisms and their future response to anthropogenic climate change (Bálint et al, ; Comes & Kadereit, ; Espíndola et al, ; Haywood et al, ; Hewitt, ; Lawing & Polly, ; Myers, Stigall, & Lieberman, ). Spatially explicit palaeo‐climatic data have provided important insights into macroecology (Bálint et al, ; Couvreur et al, ; Kissling, Blach‐Overgaard, Zwaan, & Wagner, ; Rakotoarinivo et al, ), macroevolution (Meseguer et al, ), palaeobiology (Myers et al, ), systematics (Frajman et al, ; Younger et al, ), biogeography (Benítez‐Benítez, Escudero, Rodríguez‐Sánchez, Martín‐Bravo, & Jiménez‐Mejías, ; Espíndola et al, ; Silva, Antonelli, Lendel, Moraes, & Manfrin, ; Wang et al, ), palaeophylogeography (Lawing & Polly, ; Lawing, Polly, Hews, & Martins, ; Rödder et al, ) and conservation (Alsos, Alm, Normand, & Brochmann, ). However, such palaeo‐climatic data are currently restricted to a few time periods (e.g.…”