“…Pelagic marine food web processes establish a concentration gradient in organic matter from the sunlit surface to the ocean's depths that is driven by the downward flux of organic carbon from the surface to the ocean interior, known as the biological carbon pump (BCP) (Michaels and Silver, 1988;Ducklow et al, 2001;Boyd et al, 2019). The complexity of oceanic food webs directly influences both the amount and composition (e.g., phytoplankton cells, zooplankton fecal pellets, dissolved organic carbon (DOC), aggregates) of carbon that contributes to export (Carlson et al, 1994;Durkin et al, 2016;Guidi et al, 2016;McCave, 1975;Passow & Alldredge, 1995;Rynearson et al, 2013;Serra-Pompei et al, 2022;Steinberg & Landry, 2017;Turner, 2015). The links and losses within food webs influence the magnitude and strength of key export pathways within the BCP including sinking of individual phytoplankton cells, sinking aggregates, fecal pellets, and active vertical migration (Nowicki et al, 2022;Siegel et al, 2023).…”