“…Similarly, glacier surfaces accumulate organic carbon from biological activity (e.g., in situ primary production) and the deposition of allochthonous organic material from terrestrial or anthropogenic sources (Hood and Berner, 2009;Singer et al, 2012;Stibal et al, 2012). It has been suggested that the allochthonous flux of organic carbon to glacier forefields could increase over the next two centuries due to (1) increased glacier runoff and thus increased flux of organic carbon from glacier surfaces to the pro-glacial zone (Foreman et al, 2007;Hood et al, 2015), (2) a longer residence time of liquid water in the glacial snowpack supporting higher growth and carbon fixation rates of snow algae (Morgan-Kiss et al, 2006;Stibal et al, 2007;Takeuchi et al, 2009;Lutz et al, 2015), (3) the invasion of non-native birds and mammals (Jonsdottir, 2005;Kelly et al, 2010;Miller and Ruiz, 2014;Ware et al, 2014), (4) the invasion of new plant species as human activity and tourism increases (Ware et al, 2014), and (5) an enhanced input of feces-derived organic material to soils from increasing populations of Barnacle Geese, Reindeer herds and other biota in Svalbard in response to climate warming (Michelutti et al, 2009;Moe et al, 2009;Luoto et al, 2015). However, there is considerable uncertainty in predicting the magnitude of future substrate deposition and, to our knowledge, no studies have made direct predictions based on estimations or empirical data.…”