Peatlands cover 25%-30% of the boreal zone and are an important component of both regional and global carbon cycle dynamics (Wieder et al., 2006). However, industrial activities for resource extraction in these areas have led to an extensive network of linear disturbances known as seismic lines. In fact, there is an estimated 345,000 km (disturbing an area of ∼1,900 km 2 ) of seismic lines crossing peatlands in the province of Alberta, Canada alone (Strack et al., 2019). These linear clearings can be between 1.5 and 10 m wide, creating a dense grid across the landscape. These lines are cleared using a combination of tree removal and soil disturbance/compaction, altering hydrological conditions (Braverman & Quinton, 2015), vegetation communities (Echiverri et al., 2020) and ecosystem functions such as carbon exchange (Dabros et al., 2018;