“…While transient trampling effects of these ungulates may be subtle in comparison to past Pleistocene megafauna, their ability to locally drive graminoid‐moss state transitions accompanied by shifts in ecosystem and soil processes and albedo has been reported, especially for Old World reindeer (Forbes & Kumpula, 2009; Olofsson et al., 2004; van der Wal, 2006). Indeed, much of the complex vegetation and ecosystem responses to herbivores in tundra may be driven by trampling either alone or in concert with defoliation and fertilization that alone usually do not recreate the observed changes in vegetation or ecosystem processes caused by ungulate presence (Egelkraut et al., 2020; Falk et al., 2014, 2015; Olofsson, 2009). In tundra, climate warming is rapidly shifting species pools, altering biogeochemical cycles (Abbott et al., 2016; IPCC, 2014; Meredith et al, 2019) and changing the populations and behaviour of ungulates (Cuyler et al., 2020; Mallory & Boyce, 2017; Mysterud, 2013; Uboni et al., 2016).…”