“…Konno (utakonno@mail.sci.hokudai.ac.jp) total fixed nitrogen is predominantly controlled by the total influx of fixed nitrogen through N 2 fixation and by the total efflux of fixed nitrogen through denitrification (Codispoti et al, 2001;Brandes and Devol, 2002;Deutsch et al, 2004). However, the estimated values of both fluxes obtained in different studies are highly variable (e.g., Wada et al, 1975;Liu, 1979;Codispoti and Christensen, 1985;Gruber and Sarmiento, 1997;Codispoti et al, 2001;Brandes and Devol, 2002;Capone and Knapp 2007;Naqvi et al, 2008). Earlier estimates have revealed the efflux of 95 ± 20 Tg N yr −1 through sedimentary denitrification (Gruber and Sarmiento, 1997) and the influx of 110 ± 40 Tg N yr −1 through oceanic N 2 fixation (Codispoti et al, 2001).…”