“…The Indian plate, the land portion of which comprises the Indian subcontinent, was part of the Gondwanan supercontinent 150 million years ago (Ma) (Jokat et al 2003), before separating from Africa 130-110 Ma (Morley 2003, Lomolino et al 2017, then Madagascar and the Seychelles 99-66 Ma (Ashton and Gunatilleke 1987, Plummer et al 1998, Lomolino et al 2017, and then drifting northwards and colliding with Eurasia 55-42 Ma (Ashton andGunatilleke 1987, Briggs 2003). Dramatic climatic shifts during its northward journey resulted in the loss of many endemic plant lineages (Morley 1998(Morley , 2000(Morley , 2003, but the region might have played a key role in the diversification of species-rich plant families in Asia, such as Dipterocarpaceae and Zingiberaceae (e.g., Karanth 2006, Ashokan et al, 2022 as the recipient of long-distance dispersals (e.g., Zhao et al 2022); the site of rapid in situ radiations (e.g., Surveswaran et al 2021) and as 'a biogeographical raft' (Zhao et al 2022). Certainly, biotic exchanges following collision with Eurasia would have had profound effects on the composition of the flora of that region (e.g., Mani 1974, Conti et al 2002, Karanth 2006, Sen et al 2019, but most biogeographic studies involving the Indian plate have focused on animals, with plants examined only rarely (e.g., Sen et al 2019, Zhao et al 2022.…”