Insights Into the Biogeochemical Cycling of Iron, Nitrate, and Phosphate Across a 5,300 km South Pacific Zonal Section (153°E-150°W)

Iron, phosphate, and nitrate are essential nutrients for phytoplankton growth, and hence, their supply into the surface ocean controls oceanic primary production. Here we present a GEOTRACES zonal section (GP13; 30-33 degrees S, 153 degrees E-150 degrees W) extending eastward from Australia to the oligotrophic South Pacific Ocean gyre outlining the concentrations of these key nutrients. Surface dissolved iron concentrations are elevated at >0.4 nmol L-1 near continental Australia (west of 165 degrees E) and decreased eastward to <= 0.2 nmol L-1 (170 degrees W-150 degrees W). The supply of dissolved iron into the upper ocean (<100 m) from the atmosphere and vertical diffusivity averaged 11 +/- 10 nmol m(-2) d(-1). In the remote South Pacific Ocean (170 degrees W-150 degrees W), atmospherically sourced iron is a significant contributor to the surface dissolved iron pool with average supply contribution of 23 +/- 17% (range 3% to 55%). Surface water nitrate concentrations averaged 5 +/- 4 nmol L-1 between 170 degrees W and 150 degrees W, while surface water phosphate concentrations averaged 58 +/- 30 nmol L-1. The supply of nitrogen into the upper ocean is primarily from deeper waters (24-1647 mu mol m(-2) d(-1)) with atmospheric deposition and nitrogen fixation contributing <1% to the overall flux along the eastern part of the transect. The deep water N:P ratio averaged 14.5 +/- 0.5 but declined to <1 above the deep chlorophyll maximum (DCM) indicating a high N:P assimilation ratio by phytoplankton leading to almost quantitative removal of nitrate. The supply stoichiometry for iron and nitrogen relative to phosphate at and above the DCM declines eastward leading to two biogeographical provinces: one with diazotroph production and the other without diazotroph production. Plain Language Summary Iron, phosphate, and nitrate are essential nutrients for phytoplankton growth and hence their supply into the surface ocean controls phytoplankton growth. We present a 5,300 km zonal section extending from Australia into the South Pacific Ocean relating to iron, nitrate, and phosphate. We find that the supply of these nutrients into the surface ocean defines that biogeographical distribution of phytoplankton groups.