“…Indeed, the available fossil record suggests a more intricate historical biogeography for Kalotermitidae, characterized by considerable past extinctions, consistent with the fact that most organisms that have ever lived are today extinct and so historical biogeographic patterns must always be tempered by a consideration of significant extinction. Extinction events are at minimum evidenced by at least four groups of Kalotermitidae: 1) Electrotermes is the first unambiguous kalotermitid fossil from the Palearctic realm represented by ∼49–41 million-year-old fossils (Nel and Bourguet, 2006), and predating our oldest estimates of Palearctic kalotermitids (Figure 1 and S4); 2) Huguenotermes , an extinct genus allied to modern Cryptotermes , which appeared in the Palearctic at least by 35 Mya (Engel and Nel, 2015), while there are no modern native species of Cryptotermes or related genera in the Palearctic realm; 3) a wholly unique fauna of kalotermitids from the Miocene of Zealandia which may have diverged from other Kalotermitidae when Zealandia separated from Australia in the Late Cretaceous, and then become extinct as the landmasses of Zealandia became submerged during the Neogene, necessitating more recent recolonization of modern New Zealand (Engel and Kaulfuss, 2017); and 4) the oldest kalotermitid fossils of Proelectrotermes (a genus also represented in 41 Ma Baltic amber of the Palearctic realm), Kachinitermes , and Kachinitermopsis from the ∼99 million year old Kachin amber (Engel et al, 2007b), substantially predating our estimates of the oldest Oriental kalotermitids (53 Mya, 47–60 Mya 95% HPD, node 7 in Figure 1). These last three are possible representative of the kalotermitid stem group, but the others are crown-Kalotermitidae.…”