Abstract

Abstract Copper distribution and speciation were determined at stations P4 and P26 along Line P as part of a GEOTRACES Process Study in the Northeast Pacific, at depths between 10 and 1400 m. Two ligand classes (L 1 and L 2 ) were detected at both stations: the stronger L 1 ligand pool with log K' Cu2+L1 15.0–16.5 and the weaker L 2 ligand pool with log K' Cu2+L2 11.6–13.6. The L 1 class bound on average 94% of dCu, with the ratio between L 1 and dCu constant and close to unity (1.15 = [L 1 ]:[dCu]). The concentrations of total ligands exceeded those of dCu at all depths, buffering Cu 2+ concentrations ([Cu 2+ ]) to femtomolar levels (i.e. pCu 14.1–15.7). Measurements using cathodic stripping voltammetry also identified natural copper-responsive peaks, which were attributed to thiourea- and glutathione-like thiols (TU and GSH, respectively), and Cu-binding humic substances (HS Cu ). Concentrations of TU, GSH and HS Cu were determined by standard addition of model compounds in an attempt to identify Cu-binding ligands. HS Cu concentrations were generally higher at P26 than at P4, consistent with a marine origin of the humic material. Overall, HS Cu contributed to 1–27% of the total L concentration (L T ) and when combined with the two thiols contributed to up to 32% of L T . This suggests other ligand types are responsible for the majority of dCu complexation in these waters, such as other thiols. Some potential candidates for detected, but unidentified, thiols are cysteine, 3-mercaptopropionic acid and 2-mercaptoethanol, all of which bind Cu. Significant correlation between the concentrations of TU-like thiols and L 1 , along with the high log K' Cu2+L1 values, tentatively suggest that the electrochemical TU-type peak could be part of a larger, unidentified, high-affinity Cu compound, such as a methanobactin or porphyrin, with a stronger binding capability than typical thiols. This could imply that chalkophores may play a greater role in oceanic dCu complexation than previously considered.

Highlights

  • Complexation by natural organic ligands (L) controls the speciation of biogenic metals in seawater (Bruland et al, 2014)

  • Our work suggests that Cu is strongly complexed by two ligands throughout the water column at both P4 and P26 in this HNLC region

  • The remaining dCu was bound by a weaker ligand class, which was generally found at much higher concentrations than L1

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Summary

Introduction

Complexation by natural organic ligands (L) controls the speciation of biogenic metals in seawater (Bruland et al, 2014). Bound Cu is less bioavailable, and less toxic, than free Cu2+. Free Cu2+ at pM levels can be toxic to cyanobacteria (Brand et al, 1986) but potentially growth-limiting to some archaea that have a greater Cu requirement (Amin et al, 2013). Cu tolerances and requirements vary among phytoplankton species and phylogenetic classes, as well as between coastal and oceanic strains of the same genus (Annett et al, 2008; Peers et al, 2005). Cu complexation with natural organic ligands depends on the ligand concentrations and the complex stability (conditional stability constant, K'Cu2+L). Log K′ Cu2+L values in the literature are typically subdivided into two classes (L1 and L2), with log K'Cu2+L1 around 13–16 and log

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