Iron is an essential micronutrient for marine life, and its distribution across the world ocean is mostly driven by its complexation by a fraction of the dissolved organic matter pool called iron-binding ligands. This dataset includes the concentration and conditional stability constant of dissolved iron-binding ligands of samples collected during the U.S. GEOTRACES GP17-ANT cruise. This cruise was aiming to investigate the distribution of trace metals and dependent variables in the Amundsen Sea...
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Sample Collection:
This work was funded by the U.S. National Science Foundation and the samples collected on the U.S. GEOTRACES GP17-ANT cruise in the Amundsen Sea onboard the RVIB Nathaniel B. Palmer from November 28, 2023 until January 28, 2024 (cruise ID NBP24-01). Water column sampling was accomplished with a trace-metal clean towed fish (Mellett and Buck, 2020) and a rosette equipped with 12-liter (L) GO-Flo bottles (General Oceanics; Cutter et al., 2017). The seawater was filtered inline through 0.2-micrometer (µm) (Pall Acropak) capsule filters, collected in acid-clean Milli-Q conditioned 500 milliliter (mL) fluorinated high-density polyethylene (FLPE; Nalgene) bottles, and stored frozen at -20 degrees Celsius (°C) immediately after collection and until analysis (e.g., Buck et al., 2018) if not analyzed within the next 24 hours following collection. 27 full-depth profiles were collected for iron-binding ligands (398 samples).
Analysis of iron-binding ligands:
The samples were prepared and analyzed onboard following an established method (Rue and Bruland, 1995; Buck et al. 2007, 2012; Mahieu et al. 2024). The samples were thawed overnight at room temperature in the dark prior to analysis if not analyzed fresh. Aliquots of 10 milliliters (mL) of sample were placed in 16 conditioned tubes (50 mL, MetalFree, Labcon) and spiked with 50 microliters (µL) of a 1.5 M borate acid (99 + %, Thermo Scientific) in 0.4 molar (M) ammonium (Optima, Fisher Chemical) buffer for a final pH of 8.2. The aliquots were then spiked with iron standard (prepared by dilution of atomic absorption spectrometry grade, AA; Fisher Chemical in 0.024 M trace metal grade HCl) for final concentration of 0, 0, 0.1, 0.25, 0.5, 0.75, 1, 1.5, 2, 2.5, 3, 4, 5, 7.5, 10 and 15 nanomolar (nM) in each 10 mL of sample. After at least 2 hours of equilibration, the tubes were spiked with 50 µL of a 5 millimolar (mM) salicylaldoxime (98 + %, TCI America) solution made in methanol (LC/MS Grade Optima, Fisher Chemical) for a final concentration of 25 micromolar (µM) and left to equilibrate for at least 15 minutes before analysis.
Each aliquot was analyzed after being placed in a fluorinated ethylene propylene (FEP) cell originally manufactured by Princeton Applied Research, on a controlled mercury growth electrode (CGME) from BioAnalytical Systems, Inc. (BASi) set on drop size 14 in Static Mercury Drop Electrode (SMDE) mode and equipped with a platinum wire counter electrode, a chloride/silver chloride reference electrode, and commercially available quadruple-distilled elemental mercury (Bethlehem Apparatus) as working electrode. The CGME was controlled by an Epsilon Ɛ2 electrochemical analyzer (BASi; 2 systems were used simultaneously). The following parameters were applied through the software EpsilonEC (BASi): analysis with differential pulse adsorptive cathodic stripping voltammetry (DP-AdCSV), deposition at +0.05 volts (V) while stirring, 15 seconds of equilibration (no stirring), stripping from 0 to -0.85 V with a 6 millivolt (mV) step, 50 mV amplitude, 35 milliseconds (ms) pulse width and 200 ms pulse period (Mahieu et al., 2024).
The height of the reduction peak was determined using an automated procedure presented and tested by Mahieu et al. (2024). Briefly, the 4th derivative of the scan was produced through the software ECDSoft (Omanović and Branica, 1998), and the peak height defined with a linear baseline using adaptive scan mode. The peak heights were then compiled in a custom-made Excel spreadsheet, and the data fitted on the software ProMCC (Omanović et al., 2015) using complete complexation fitting model and considering a detection of αAL of 79 (e.g., Buck et al., 2007).
Mahieu, L., Buck, K. N., Bundy, R. M. (2026). Dissolved iron-binding ligand concentrations and conditional stability constants from field samples collected on US GEOTRACES GP17-ANT cruise NBP24-01 on RVIB Palmer in the Amundsen Sea from Nov 2023 to Jan 2024. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2026-03-17 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/994890 [access date]
Terms of Use
This dataset is licensed under Creative Commons Attribution 4.0.
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