“…Phytoplankton incorporate P by direct assimilation of DIP (Cembella et al 1984, Chróst & Overbeck 1987, González-Gil et al 1998. In marine waters, the pool of DOP can comprise 25 to 80% of the dissolved P pool (Hoppe 2003, Suzumura et al 2012, though not all of it is biologically available (Karl & Bjorkman 2002), When DIP concentrations are depleted, phytoplankton may use reservoirs of DOP, like sugar phosphates and esters, for P deficiencies (Jackson & Williams 1985, Cotner & Wetzel 1992, Yamaguchi et al 2006. There is evidence to suggest that DOP compounds such as phosphomonoesters and less-labile phosphonates play an important role in phytoplankton (Dyhr man & Haley 2006, Dyhrman & Ruttenberg 2006, though the production of P-cleaving enzymes is more energetically costly than incorporation of DIP (Me seck et al 2009).…”