Ellwood, MichaelBowie, AndrewBaker, AlexGault-Ringold, M.Hassler, Christel S.Law, Cliff S.Maher, WilliamMarriner, AndrewNodder, Scott D.Sander, S.Stevens, C. L.2021-04-272021-04-27Ellwood, M. J., Bowie, A. R., Baker, A., Gault-Ringold, M., Hassler, C., Law, C. S., … Boyd, P. W. (2018). Insights into the biogeochemical cycling of iron, nitrate, and phosphate across a 5,300 km South Pacific zonal section (153°E–150°W). Global Biogeochemical Cycles, 32, 187–207. https://doi.org/10.1002/ 2017GB0057360886-6236http://hdl.handle.net/1885/231040Iron, 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°S, 153°E–150°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°E) and decreased eastward to ≤0.2 nmol L−1 (170°W–150°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°W–150°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°W and 150°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 μmol 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.This research was supported by the New Zealand Foundation for Research, Science and Technology Coasts and Oceans Outcome-Based Investment (COIX0501), and the Australian Research Council Discovery Projects (DP1092892 and DP110100108) and Future Fellowships (FT130100037) programs, University of Tasmania, internal grants to A. R. B. (refs B0018994, B0019024, and L0018934), and University of Technology Sydney Chancellor Fellowship to CSH.application/pdfen-AU© 2018 American Geophysical UnionironnitratephosphateSW Pacific Oceanphytoplankton2018-01-0410.1002/2017GB0057362020-11-23