Cited by 349Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisPaleontology and Stratigraphy of Fossils

The stable Cr isotope inventory of solid Earth reservoirs determined by double spike MC-ICP-MS

Schoenberg, R., Zink, S., Staubwasser, M., von Blanckenburg, F.·2008·Chemical Geology

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Crossref · 10.1016/j.chemgeo.2008.01.009

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33 of 33 references verified0 citation errors · 0 not checkable

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  • Carbonates and oxic siliciclastic sediments make up a relatively small part of the oceanic Cr sink, and their Cr isotope compositions are not expected to be strongly fractionated relative to the oceanic pool.

    “carbonates and oxic siliciclastic sediments are thought to account for a relatively small fraction of the Cr sink flux in the oceanic Cr budget, and the Cr isotope compositions of these facies are not expected to be strongly fractionated relative to the oceanic pool”

    From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Schoenberg et al., 2008

  • Cr isotopes were measured on a Neptune Plus MC-ICP-MS at Yale following the analytical protocol of Schoenberg et al. (2008) and Reinhard et al. (2014).

    “Chromium isotopes were measured on a Neptune Plus (Thermo-Finnigan) MC-ICP-MS at Yale University according to the analytical protocol of (Schoenberg et al., 2008;Reinhard et al., 2014).”

    From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Schoenberg et al., 2008

  • The three-step separation protocol ensured complete removal of Fe, Ti and V to avoid isobaric interferences on Cr isotopes.

    “The following protocol included three separation steps (Schoenberg et al., 2008;Reinhard et al., 2014) that ensured complete removal of Fe, Ti and V during chemical separation in order to avoid major isobaric interferences of 54 Fe, 50 Ti and 50 V on Cr isotopes.”

    From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Schoenberg et al., 2008

  • BHVO-2 gave δ53Cr -0.12 ± 0.09‰ (n = 25), similar to published BHVO-1 values.

    “The δ 53 Cr value for BHVO-2 is -0.12 ±0.09 ‰ (n=25), which is similar to published values in the literature for BHVO-1 (a geostandard collected at the same location as BHVO-2; Schoenberg et al., 2008)”

    From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Schoenberg et al., 2008

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Authors
Schoenberg, R., Zink, S., Staubwasser, M., & von Blanckenburg, F.
Affiliations
Leibniz University Hannover (DE)
Corresponding author
Schoenberg, R.
Venue
Chemical Geology
Publisher
Elsevier BV
Published
2008-04
Volume
249
Issue
3-4
Pages
294-306
ISSN
0009-2541 (ISSN-L)
OpenAlex
W1985317544
Cited by
349
References
33
Citations by year
2026: 8 · 2025: 17 · 2024: 20 · 2023: 17 · 2022: 25 · 2021: 44 · 2020: 19 · 2019: 30 · 2018: 30 · 2017: 24 · 2016: 26 · 2015: 16 · 2014: 14 · 2013: 19 · 2012: 14
FWCI
7.84
Type
journal article
Language
en
Open access
closed
Locations
  • Chemical Geology (publishedVersion)
  • Kölner Universitäts PublikationsServer (Universität zu Köln) (acceptedVersion)
  • Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion)
Funders
Deutsche Forschungsgemeinschaft
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
mantle xenoliths, ultramafic rocks, chromite, chromitite, crocoite, lead chromate, chromium oxidation state, isotope fractionation, Bushveld Complex, Great Dyke

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