“…By specifically choosing to develop the edaphic-SDM based on the geomorphological and soil features that inform the microclim data set (Kearney, Isaac, et al, 2014), we were able to calculate microclim estimates across the projection area, including below-ground microclimate. One of the challenges facing studies of SRE flora, especially in highly biodiverse landscapes such as the BIF outcrops of south-western Western Australia (Gibson, Prober, Meissner, & Leeuwen, 2017;Gibson et al, 2010), Table Mountain National Park in South Africa (Helme & Trinder-Smith, 2006), or archipelagos such as New Caledonia (Gâteblé et al, 2019;Kier et al, 2009) is that there may be a large number of SRE species, but they are usually either entirely unique, or a unique clade of closely related species within a taxon. One of the challenges facing studies of SRE flora, especially in highly biodiverse landscapes such as the BIF outcrops of south-western Western Australia (Gibson, Prober, Meissner, & Leeuwen, 2017;Gibson et al, 2010), Table Mountain National Park in South Africa (Helme & Trinder-Smith, 2006), or archipelagos such as New Caledonia (Gâteblé et al, 2019;Kier et al, 2009) is that there may be a large number of SRE species, but they are usually either entirely unique, or a unique clade of closely related species within a taxon.…”