“…While the exact consequences of the prehistoric and historic megafauna range contractions and extinctions for vegetation structure and ecosystem function are poorly known, several studies point to widespread major effects: South American savannas are estimated to have been much more open, like the African savannas (Doughty, Faurby, & Svenning, 2016a), Great Britain had more open vegetation in the Last Interglacial than in the Early Holocene (Sandom, Ejrnaes, et al, 2014b), grassy ecosystem fire activity increased with grazer extinction severity globally (Karp et al, 2021), megafauna extinction in northern Australia led to increased wildfires and a subsequent shift from mixed savanna to fire-tolerant sclerophyll vegetation (Rule et al, 2012), and vegetation changes have been coupled with megafauna losses in North America (Gill et al, 2009). Furthermore, large and cascading ecosystem effects of large herbivores are also evident in the few areas where well-developed wild herbivore faunas still exist (Ripple et al, 2015), for example extirpation of large herbivores in Mozambique led to an expansion in the alien woody species Mimosa pigra and herbivore reintroductions decreased it back to pre-extirpation levels (Guyton et al, 2020), the re-establishment of bison numbers in Yellowstone National Park is limiting woody plant density (Beschta et al, 2020), long-term elephant impact in African savannas decreases tree density (Gordon et al, 2021) and vegetation height (Davies et al, 2018) while increasing vegetation height variability (Davies et al, 2018), and exclosure experiments in temperate forests have shown that saplings have a hard time escaping the pressure from large herbivores under closed forest canopy as well as in canopy gaps (Churski et al, 2017). From this body of knowledge, it is obvious that large herbivores play a major role in shaping ecosystem structure and functions, with important implications for ecosystem restoration (Donlan et al, 2006;Ripple et al, 2015).…”