“…These remotely sensed acoustic data sets have demonstrated considerable potential to map seabed substrate (e.g., Diesing et al, 2014;Misiuk et al, 2018), single species distributions (e.g., Galparsoro et al, 2009;Brown et al, 2012), macrofaunal assemblage patterns (e.g., Lacharité and Brown, 2019), and seabed landscapes sometimes referred to as "seascape" (e.g., Boström et al, 2011;Shaw et al, 2014) or "benthoscape" maps (Zajac, 2008;Brown et al, 2012). The next step in the evolution of these methods is to develop models to extrapolate biogeochemical processes at the fine/millimeter-tocentimeter scale (Figure 1a) to broader spatial scales (Figure 1b), utilizing spatial data to improve estimates Smeaton and Austin, 2019;Gogina et al, 2020), which is limited primarily by the paucity of remotely sensed acoustic data sets, with less than 9% of the ocean floor currently mapped by these modern, remote sensing systems (Mayer et al, 2018). At global scales, ocean digital elevation models, produced using satellite-gravity models that calibrate the gravity-to-topography ratio using bathymetric soundings (Becker et al, 2009), must rely on considerably coarser data resolution than similar terrestrial models (e.g., Figure 1c).…”