“…Climatically and edaphically homogeneous landscapes may support structurally and floristically distinct biomes, raising the question as to what determines the boundaries between them ( Bond, Midgley & Woodward, 2003 ; Hoffmann et al, 2012 ; Butler et al, 2014 ; Coetzee, Bond & Wigley, 2015 ; Cowling & Potts, 2015 ; Cramer et al, 2019 ). In landscapes dominated by fire-prone vegetation such as savannas, grasslands and heathlands, fire regime effects have been invoked to explain the boundaries between fire-prone and fire-avoiding biomes, for example Afrotemperate forest patches in Cape fynbos shrublands ( Manders, 1990 ; Geldenhuys, 1994 ; Cowling & Potts, 2015 ; Bond, Midgley & Woodward, 2003 ) and rainforest patches in savanna and grassland ( Hoffmann et al, 2009 ; Murphy & Bowman, 2012 ; Becket et al, 2022 ). The coastal dunes of the Cape Floristic Region (CFR) are an interesting case in this regard, since they can support three biomes, namely dune forest, subtropical dune thicket (hereafter “dune thicket”) and dune fynbos, each of which experiences different fire regimes as determined by topographically-induced fire protection and species-specific flammability properties ( Pierce & Cowling, 1991 ; Cowling & Potts, 2015 ; Msweli et al, 2020 ; Cowling & Hoffman, 2021 ).…”