“…These two hypotheses (H2 and H3) are based on the insight that tropical communities have higher spatial turnover than their temperate counterparts due-in part-to less variable environmental conditions and longer evolutionary history in the absence of major ice ages at lower latitudes (Alahuhta et al, 2020;Janzen, 1967;Smith et al, 2020). Similarly, we predicted (H4) that contemporary climate would explain a substantial variation in the composition of freshwater plant ecoregions (Alahuhta et al, 2020;Alahuhta et al, 2021;Chappuis et al, 2012;García-Girón et al, 2020a;Heino, 2011;Heino, 2020b;Iversen et al, 2021), with topography, Pleistocene Ice Age legacies, human footprint, water alkalinity, availability of inland waterbodies and the surface area of individual regions playing supplementary role (Chappuis et al, 2014;Iversen et al, 2019;Lacoul & Freedman, 2006;Murphy et al, 2019Murphy et al, , 2020. This hypothesis originates from the latitudinal diversity gradient and Rapoport's rule, which posit that species occurring at lower latitudes, which have lower climatic seasonality and longer evolutionary legacies, are thermal specialists with narrower ranges (Currie et al, 2004), resulting also in higher species richness in and around the Tropics (Alahuhta et al, 2021;Murphy et al, 2019).…”