“…On the other hand, 18:0, 18:2ω6, 18:4ω3, 20:4ω6 and 22:6ω3 displayed only moderate enrichment ( Table 2) (Viso & Marty 1993, St. John & Lund 1996, Dalsgaard et al 2003, it is likely that the increase in δ 13 C in settled fish reflects increased reliance on epiphytic or benthic diatoms. Moreover, 15:0 is often used as a bacterial biomarker (Bec et al 2003, Dalsgaard et al 2003, Jaschinski et al 2008, and its enriched δ 13 C values suggest the benthic origin of the bacterial carbon on which settled fish rely, probably by ingesting sediment directly. The particularly high mean δ 13 C values of 14:0, 15:0, 16:0 and 16:1ω7 in the 20-30 mm fish (-7.6 to -10.9 ‰ for 14:0 and 16:0, respectively, in NLs) were close to the bulk δ 13 C values of macroalgae (Table 2, Fig.…”