“…Assuming that this hypothesis is true, the number of trophic levels increases from 3 to 4 in the transition from inshore to offshore areas, and the major contributor to the trophic link shifts from BM to PP. Previous isotopic studies that showed systematic landward decreases in δ 13 C and/or δ 15 N for estuarine consumers have suggested a change of food source from algae to terrestrial organic matter (Kikuchi & Wada 1996, Riera & Richard 1996, Doi et al 2005, Kasai & Nakata 2005 or the consumption of PP with differing δ 13 C values, reflecting the source of dissolved inorganic carbon used for photosynthesis (Fry 1999, Piola et al 2006). In our study area, however, such trends were not found, probably due to the more saline environment, where marine-influenced, nutritive primary producers such as PP and BM prevail.…”