Cited by 108Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisGroundwater and Isotope Geochemistry

A review of mass-dependent fractionation of selenium isotopes and implications for other heavy stable isotopes

Johnson, Thomas M·2004·Chemical Geology

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Crossref · 10.1016/j.chemgeo.2003.11.015

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  • Johnson (2004) noted that microbial reductions yield fractionations less than 5‰, whereas abiotic processes yield fractionations greater than 7.3‰, suggesting that it may be possible to distinguish microbial from abiotic reduction.

    “Johnson (2004) [50] noted that microbial reductions yield fractionations less than 5‰, whereas abiotic processes yield fractionations greater than 7.3‰, suggesting that it may be possible to distinguish microbial from abiotic reduction.”
  • Assimilation by higher plants, Se(IV) oxidation, sorption, and biological volatilization induce little or no isotopic fractionation.

    “Assimilation by higher plants, Se(IV) oxidation, sorption, and biological volatilization induce little or no isotopic fractionation [50].”

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Authors
Johnson, T. M.
Affiliations
University of Illinois Urbana-Champaign (US)
Corresponding author
Johnson, Thomas M
Venue
Chemical Geology
Publisher
Elsevier BV
Published
2004-04
Volume
204
Issue
3-4
Pages
201-214
ISSN
0009-2541 (ISSN-L)
OpenAlex
W2063623510
Cited by
108
References
0
Citations by year
2026: 3 · 2025: 2 · 2024: 1 · 2023: 3 · 2022: 3 · 2021: 4 · 2020: 8 · 2019: 4 · 2018: 7 · 2017: 9 · 2016: 5 · 2015: 9 · 2014: 8 · 2013: 3 · 2012: 4
FWCI
3.38
Type
journal article
Language
en
Open access
closed
Locations
Chemical Geology (publishedVersion)
Funders
Division of Earth Sciences
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
Keywords
selenium isotopes, mass-dependent fractionation, bacterial reduction, wetland sediments, selenium volatilization, selenium sorption, selenium oxidation, redox reactions, source apportionment

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