Fig. 1: Key relationships across the Southern Ocean.
From: Marine biogenic humic substances control iron biogeochemistry across the Southern Ocean

a Sampling stations are shown superimposed on nitrate concentrations to illustrate the contrasting sites sampled during the Antarctic Circumpolar Expedition (ACE). b Component loading from the Principal Component Analysis for the ACE dataset (0–1000 m, n = 70). This figure represents the relationship between dissolved Fe (DFe, nmol L−1), in situ iron-binding ligands (Fe-L, nmol L−1), the conditional stability constant (log KFe’L), electroactive humic substances (eHS, µg L−1 Suwanee River Fulvic Acid (SRFA) equivalent), hydrolysable carbohydrates (Carb, µg L−1 glucose equivalent) and depth (m). Principal Component (PC) 1 and 2 together explain 64.33% of the dataset. The variances of the data are explained at 77% for depth, 80% for DFe, 81% for Fe-L, 22% for logKFe’L, 53% for Carb, and 75% for eHS. log KFe’L and Carb are not statistically represented.