“…Selection of POM particles is based on their size, quality, and composition, and some benthic consumers with high δ 13 C values may have selected for ice algal-derived POM. Based on the slow turnover time in Arctic benthic consumer tissues (McMahon et al, 2006;Kaufman et al, 2008;Weems et al, 2012) and the low benthic organism δ 13 C seasonal variability ( o1‰) recorded in previous Arctic studies (Dunton et al, 1989;Kedra et al, 2012;Legezynska et al, 2012;Søreide et al, 2013;Carroll et al, 2014) and in this study, isotopic enrichment from ice-algal ingestion should be measurable even months after the ice-algal deposition. Similar reliance of Arctic benthic communities on sea-ice diatoms through tight sympagic-benthic coupling has been reported for the Svalbard Archipelago (Søreide et al, 2013).…”