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Redox cycling of rare earth elements in the suboxic zone of the Black Sea
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“suboxic and anoxic waters lack significant negative Ce(SN) anomalies due to reductive dissolution of settling Mn(IV)-Fe(III)-oxyhydroxide particles (German et al., 1991; Byrne and Sholkovitz, 1996)”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as German et al., 1991
In the citing paper
“the ratio of light to heavy REEs markedly increases across redox boundaries due to reductive dissolution of Mn(IV)-Fe(III)-oxyhydroxides (German et al., 1991; Byrne and Sholkovitz, 1996)”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as German et al., 1991
In the citing paper
“depletion of light REE+Y develops in oxygenated waters owing to preferential removal of LREE versus HREE onto Mn(IV)-Fe(III)-oxyhydroxides and other particle-reactive surfaces”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as German et al., 1991
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Self-citationUnexpected changes in the oxic/anoxic interface in the Black Sea
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Martins, P. L. G., Toledo, C. L. B., Silva, A. M., Chemale, F., Archer, C., & de Assis, L. M. (2021) · Gondwana Research · doi:10.1016/j.gr.2021.09.008 · Cited by 12
Metadata
- Authors
- German, C. R., Holliday, B. P., & Elderfield, H.
- Affiliations
- University of Cambridge (GB)
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1991-12
- Volume
- 55
- Issue
- 12
- Pages
- 3553-3558
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2075585431
- Cited by
- 371
- References
- 26
- Citations by year
- 2026: 22 · 2025: 26 · 2024: 26 · 2023: 20 · 2022: 28 · 2021: 21 · 2020: 20 · 2019: 23 · 2018: 24 · 2017: 12 · 2016: 24 · 2015: 15 · 2014: 9 · 2013: 11 · 2012: 4
- FWCI
- 6.23
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Topics
- 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
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine Plankton and Biogeochemistry
- Keywords
- rare earth elements, redox cycling, suboxic zone, Black Sea, manganese oxide, iron oxide, anoxic basins
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
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