Arsenic and phosphorus are biochemically very similar, and hence arsenate (As 5+ ) is toxic by interfering with the energy metabolism, in particular during P limitation. However, many phytoplankton detoxify As by reducing arsenate to arsenite (As 3+ ), and/or methylating it to mono and dimethyl As. Such As detoxification becomes operative in oligotrophic waters when phosphate concentrations are below those for As; therefore, we evaluated the potential use of these detoxification products as indicators of P limitation by measuring As speciation during the US GEOTRACES North Atlantic transect. The distribution of As 3+ concentrations in surface waters is similar to that of N : P ratios and alkaline phosphatase activity (APA), two conventional proxies for P-limitation. As 3+ concentrations have a very similar relationship to phosphate as APA to phosphate, and therefore indicate the potential of As 3+ as proxy for P-limitation. From the relationship to phosphate we derived threshold values of As 3+ concentration to indicate moderate and extreme P-limitation. We then applied these threshold values to assess P-limitation with high horizontal resolution in the North Atlantic, improving on the contradictory assessments using the conventional proxies. Our new evaluation is consistent with the general concept that the North Atlantic is moderately to extremely limited in phosphate.Arsenic and phosphorus are biochemically very similar, so that phytoplanktonic uptake of arsenate (As 5+ ) induces toxic effects due to its substitution in the adenotriphosphate (ATP) cycle, effectively decoupling the energy metabolism (Lehninger 1975). Many phytoplankton species evolved different strategies to ameliorate the toxic effects of As 5+ , including reduction to arsenite (As 3+ ) and methylation to monomethyl-(MMAs) and dimethylarsenic (DMAs). These detoxification products are less harmful and easier to excrete (Andreae and Klumpp 1979;Sanders and Riedel 1993;Hellweger et al. 2003). Hellweger et al. (2003) proposed a mechanistic model with a limited methylation capacity due to slower kinetics compared with the preceding reduction. Such capacity may be exceeded during luxury P uptake because the chances of taking up As 5+ increase with higher rates of P uptake. Hellweger et al. (2003) proposed that exceeding methylation capacity leads to the excretion of the reduced As 3+ . Surface waters of oligotrophic central gyres have particularly high As : P ratios, with As 5+ concentrations in a range of 10-15 nmol L 21 (Cutter et al. 2001;Cutter and Cutter 2006), while phosphate is typically within a range of 0.2-10 nmol L 21 (Wu et al.