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