Fig. 1
From: The interplay between regeneration and scavenging fluxes drives ocean iron cycling
Study area. The southern part of the CLIVAR P16S line in the south Pacific Ocean, on a backdrop of water age (years) from the OCIM model averaged over the intermediate water isopycnal layers (σ0 = 26.8–27.2). The individual stations used in this analysis are marked with red crosses
