Dataset: Vanadium concentrations and isotope compositions of seawater samples collected from the South Atlantic Ocean (2010 UK GEOTRACES cruise GA10/D357 Leg 1) and the Black Sea (2013 MedBlack GEOTRACES cruise leg 2, 64PE373, R/V Pelagia)

ValidatedFinal no updates expectedDOI: 10.26008/1912/bco-dmo.957165.1Version 1 (2025-04-01)Dataset Type:Cruise Results

Principal Investigator: Jeremy D. Owens (Florida State University - National High Magnetic Field Lab)

Co-Principal Investigator: Sune G. Nielsen (Woods Hole Oceanographic Institution)

Student: Siqi Li (Florida State University - National High Magnetic Field Lab)

BCO-DMO Data Manager: Shannon Rauch (Woods Hole Oceanographic Institution)


Project: Fingerprinting and Calibrating Low Oxygen Conditions Using Vanadium Isotopes (Vanadium Isotopes)


Abstract

These data include vanadium concentrations and isotope compositions of seawater samples from the South Atlantic Ocean (collected during the UK GEOTRACES cruise GA10/D357 Leg 1) and the shallow water columns in the Black Sea (collected during the leg 2 of the MedBlack GEOTRACES cruises, 64PE373, R/V Pelagia). The resin column chromatography method is utilized to purify vanadium. The vanadium concentrations were measured with the Agilent 7500ce Inductively Coupled Plasma Mass Spectrometry (ICP-MS)...

Show more

Collection protocols for the South Atlantic Ocean seawater samples (Owens et al., 2017): a "trace metal-clean" titanium rosette with a PTFE-coated CTD system was used and deployed using a plasma rope to collect the seawater samples. Seawater samples were filtered through 0.2-micrometer (μm) filter capsules and transferred into 1-liter (L) HDPE bottles in a trace metal clean container. Then seawater samples were acidified at WHOI (Woods Hole Oceanographic Institution) to pH ~2 using concentrated distilled HCl.

Collection protocols for the Black Sea seawater samples (Cruise Report 64PE373 on RV Pelagia): an ultra-clean titanium CTD system was deployed to collect the seawater samples. The collected seawater was filtered with 0.2 μm Sartobran 300 filter cartridges (Sartorius) and acidified on board to pH ~2 with Baseline grade Seastar HCl. (See: https://www.geotraces.org/ga04-2/)

Here we describe the general protocols for chemical procedures. The in-lab column chromatography procedures to pre-concentrate and purify seawater vanadium (V) for concentration and isotope composition measurement are described in detail in Li et al. (under review). The chemical reagents utilized were trace-metal clean.

For seawater V concentration measurement, the column chromatography utilizing Bio-rad AG 50W-X12 cation resin was used to pre-concentrate V (Li et al., under review). The acidified seawater samples (pH ~2) were doped with H2O2 solution to contain 2% H2O2 before being loaded onto the resin column. Vanadium was yielded with weakly acidic H2O2 solution (0.01 M HCl + 2% H2O2) with the matrix metal elements being retained on the resin.

For seawater V isotope composition measurement, a four-column chromatography (Wu et al., 2019) was used to pre-concentrate and purify seawater V. Details of further improvements on this column chromatography method have been described in Li et al. (under review). The pre-cleaned Hitachi Nobias Chelate PA-1 resin and Bio-rad AG1-X8 anion resin were utilized to pre-concentrate and purify seawater V. The first column utilized Nobias Chelate PA-1 resin. Seawater samples were buffered to pH at 6.0 ± 0.1 with acetic acid and ammonia solutions before being loaded onto the column. Then V was yielded with 3 M HNO3. The following three columns utilized Bio-rad AG1-X8 anion resin to further purify seawater V, and the yielded V from the previous column was redissolved in 0.01 M HCl + 2% H2O2 solution before being loaded onto the column. Then, clean the resin column after the complete dripping of the sample solution using 0.01M HCl + 2% H2O2. Finally, V was yielded with 6M HCl and 2M HNO3.

The artificial seawater standards SW Matrix-AA and SW Matrix-BDH were made as in-lab standards for isotope composition measurement. The matrix elutes of two seawater samples were yielded after the first Nobias resin column and were separately doped with pure V solution standards, ~900 nanograms (ng) AA-V (SW Matrix-AA) and ~900 ng BDH V (SW Matrix-BDH). The two artificial seawater standards were processed parallelly with seawater samples with the same chemical procedures.


Related Datasets

No Related Datasets

Related Publications

Results

Li, S., Nielsen, S.G, & Owens, J.D. (under review, 2025) Global cycling of vanadium isotopes from multiple ocean water masses and a restricted euxinic basin.
Methods

Brophy, C., Clancy, V., Willie, S., & Yang, L. (2012). NASS-6: Seawater reference material for trace metals (Version 1). National Research Council of Canada. https://doi.org/10.4224/CRM.2012.NASS-6
Methods

Conway, T. M., John, S. G., & Lacan, F. (2016). Intercomparison of dissolved iron isotope profiles from reoccupation of three GEOTRACES stations in the Atlantic Ocean. Marine Chemistry, 183, 50–61. doi:10.1016/j.marchem.2016.04.007
Methods

Horner, T. J., Kinsley, C. W., & Nielsen, S. G. (2015). Barium-isotopic fractionation in seawater mediated by barite cycling and oceanic circulation. Earth and Planetary Science Letters, 430, 511–522. doi:10.1016/j.epsl.2015.07.027
Methods

Nielsen, S. G., Owens, J. D., & Horner, T. J. (2016). Analysis of high-precision vanadium isotope ratios by medium resolution MC-ICP-MS. Journal of Analytical Atomic Spectrometry, 31(2), 531–536. doi:10.1039/c5ja00397k