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  • Atomic absorption spectrometry (AAS); Cadmium; Cast number; Climate - Biogeochemistry Interactions in the Tropical Ocean; CTD/Rosette; CTD-RO; DEPTH, water; Event label; GOFLO; Go-Flo bottles; LATITUDE; LONGITUDE; M77/3; M77/3_011-1; M77/3-CTD50; M77/4; M77/4_078; M77/4-CTD12; M77/4-CTD18; M77/4-CTD19; M77/4-CTD23; M77/4-CTD3; M77/4-CTD35; M77/4-CTD4; M77/4-CTD44; M77/4-CTD45; M77/4-CTD48; M77/4-CTD50; M77/4-CTD52; M77/4-CTD53; M77/4-CTD63; M77/4-CTD64; Meteor (1986); Sample code/label; SFB754; Standard deviation; Station label; δ114/110Cd; ε-114/110 Cd  (1)
  • dissolved trace metals  (1)
  • GEOTRACES
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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Xie, Ruifang C; Rehkämper, Mark; Grasse, Patricia; van de Flierdt, Tina; Frank, Martin; Xue, Zichen (2019): Isotopic evidence for complex biogeochemical cycling of Cd in the eastern tropical South Pacific. Earth and Planetary Science Letters, 512, pp.134-146, https://doi.org/10.1016/j.epsl.2019.02.001
    Publication Date: 2024-07-19
    Description: The depth profiles of Cd isotopes display high δ114/110Cd at the surface and decreasing δ114/110Cd with increasing water depth, consistent with preferential utilization of lighter Cd isotopes during biological uptake in the euphotic zone and subsequent remineralization of the sinking biomass. In the surface and subsurface ocean, seawater displays similar δ114/110Cd signatures of 0.47 ±0.23‰ to 0.82 ±0.05‰ across the entire eastern tropical South Pacific despite highly variable Cd concentrations between 0.01 and 0.84 nmol/kg. This observation, best explained by an open system steady-state fractionation model, contrasts with previous studies of the South Atlantic and South Pacific Oceans, where only Cd-deficient waters have a relatively constant Cd isotope signature. For the subsurface to about 500 m depth, the variability of seawater Cd isotope compositions can be modeled by mixing of remineralized Cd with subsurface water from the base of the mixed layer. In the intermediate and deep eastern tropical South Pacific (〉500 m), seawater [Cd] and δ114/110Cd appear to follow the distribution and mixing of major water masses. We identified modified AAIW of the ETSP to be more enriched in [Cd] than AAIW from the source region, whilst both water masses have similar δ114/110Cd. A mass balance estimate thus constrains a δ114/110Cd of between 0.38‰ and 0.56‰ for the accumulated remineralized Cd in the ETSP. Nearly all samples show a tight coupling of Cd and PO4 concentrations, whereby surface and deeper waters define two distinct linear trends. However, seawater at a coastal station located within a pronounced plume of H2S, is depleted in [Cd] and features significantly higher δ114/110Cd. This signature is attributed to the formation of authigenic CdS with preferential incorporation of lighter Cd isotopes. The process follows a Rayleigh fractionation model with a fractionation factor of α114/110Cd(seawater-CdS)=1.00029. Further deviations from the deep Cd-PO4 trend were observed for samples with O2〈10μmol/kg and are best explained by in situ CdS precipitation within the decaying organic matter even though dissolved H2S was not detectable in ambient seawater.
    Keywords: Atomic absorption spectrometry (AAS); Cadmium; Cast number; Climate - Biogeochemistry Interactions in the Tropical Ocean; CTD/Rosette; CTD-RO; DEPTH, water; Event label; GOFLO; Go-Flo bottles; LATITUDE; LONGITUDE; M77/3; M77/3_011-1; M77/3-CTD50; M77/4; M77/4_078; M77/4-CTD12; M77/4-CTD18; M77/4-CTD19; M77/4-CTD23; M77/4-CTD3; M77/4-CTD35; M77/4-CTD4; M77/4-CTD44; M77/4-CTD45; M77/4-CTD48; M77/4-CTD50; M77/4-CTD52; M77/4-CTD53; M77/4-CTD63; M77/4-CTD64; Meteor (1986); Sample code/label; SFB754; Standard deviation; Station label; δ114/110Cd; ε-114/110 Cd
    Type: dataset
    Format: text/tab-separated-values, 656 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-01-21
    Description: Upwelling of subsurface waters injects macronutrients (fixed N, P, and Si) and micronutrient trace metals (TMs) into surface waters supporting elevated primary production in Eastern Boundary Upwelling Regions. The eastern South Atlantic features a highly productive shelf sea transitioning to a low productivity N‐Fe (co)limited open ocean. Whilst a gradient in most TM concentrations is expected in any off‐shelf transect, the factors controlling the magnitude of cross‐shelf TM fluxes are poorly constrained. Here, we present dissolved TM concentrations of Fe, Co, Mn, Cd, Ni, and Cu within the Benguela Upwelling System from the coastal section of the GEOTRACES GA08 cruise. Elevated dissolved Fe, Co, Mn, Cd, Ni, Cu and macronutrient concentrations were observed near shelf sediments. Benthic sources supplied 2.22 ± 0.99 μmol Fe m−2 day−1, 0.05 ± 0.03 μmol Co m−2 day−1, 0.28 ± 0.11 μmol Mn m−2 day−1 and were found to be the dominant source to shallow shelf waters compared to atmospheric depositions. Similarly, off‐shelf transfer was a more important source of TMs to the eastern South Atlantic Ocean compared to atmospheric deposition. Assessment of surface (shelf, upper 200 m) and subsurface (shelf edge, 200–500 m) fluxes of Fe and Co indicated TM fluxes from subsurface were 2–5 times larger than those from surface into the eastern South Atlantic Ocean. Under future conditions of increasing ocean deoxygenation, these fluxes may increase further, potentially contributing to a shift toward more extensive regional limitation of primary production by fixed N availability.
    Description: Key Points: Shelf sediments release redox‐sensitive trace metals (TMs) to overlying oxygen‐depleted waters in the Benguela Upwelling System. Sediment‐derived TMs are upwelled and laterally transported constituting a major source to shelf waters and to the eastern South Atlantic. Subsurface fluxes of dissolved Fe and Co from the shelf edge play an important role in supplying Fe and Co to the eastern South Atlantic.
    Description: China Scholarship Council, CSC http://dx.doi.org/10.13039/501100004543
    Description: GEOMAR and German Research Foundation
    Description: German DFG
    Description: German Research Foundation
    Description: https://doi.pangaea.de/10.1594/PANGAEA.947275
    Keywords: ddc:551 ; dissolved trace metals ; Benguela Upwelling Systems ; fluxes ; Eastern Boundary Upwelling Systems Regions
    Language: English
    Type: doc-type:article
    Location Call Number Limitation Availability
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