“…Living vegetation can directly affect GHG fluxes by moderating the influence of climate on CO 2 uptake through growth, in addition to moderating CO 2 and CH 4 release through differences in plant physiology between PFTs, which affect decomposition and gas transport (Greenup, Bradford, McNamara, Ineson, & Lee, 2000). However, PFT can also indirectly affect C fluxes through differences in the quality and quantity of rhizodeposits and plant litter entering the soil (De Deyn, Cornelissen, & Bardgett, 2008; Dieleman, Branfireun, & Lindo, 2017), which influence the abiotic and biotic properties of peat (Chronakova, Barta, Kastovska, Urbanova, & Picek, 2019; Robroek et al, 2015; Robroek et al, 2016; Ward, Bardgett, McNamara, & Ostle, 2009). Separating the direct and indirect effects of living and decomposing plants on peatland C dynamics is complex and has received little attention (Armstrong et al, 2015; Kuiper, Mooij, Bragazza, & Robroek, 2014; Wiedermann, Kane, Potvin, & Lilleskov, 2017).…”