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The geochemistry of redox sensitive trace metals in sediments
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“Cr appears to have a shorter residence time (~9 kyr; Reinhard et al., 2013) than other redox-sensitive trace elements with tractable isotopic systems such as U and Mo (~800 kyr and ~400 kyr; Morford and Emerson, 1999;Dunk et al., 2002).”
From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Morford and Emerson, 1999
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Chappaz, A., Lyons, T., Gregory, D., Reinhard, C., Gill, B. C., Li, C., & Large, R. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2013.10.028 · Cited by 157
Extensive marine anoxia during the terminal Ediacaran Period
Zhang, F., Xiao, S., Kendall, B., Romaniello, S. J., Cui, H., Meyer, M., Gilleaudeau, G. J., Kaufman, A. J., & Anbar, A. D. (2018) · Science Advances · doi:10.1126/sciadv.aan8983 · Cited by 180
Nameroff, T. J., Calvert, S. E., & Murray, J. W. (2004) · Paleoceanography · doi:10.1029/2003pa000912 · Cited by 179
Metadata
- Authors
- Morford, J. L., & Emerson, S.
- Affiliations
- University of Washington (US)
- Corresponding author
- Morford, Jennifer L.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1999-06
- Volume
- 63
- Issue
- 11-12
- Pages
- 1735-1750
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2055862951
- Cited by
- 1,215
- References
- 96
- Citations by year
- 2026: 51 · 2025: 69 · 2024: 56 · 2023: 81 · 2022: 83 · 2021: 93 · 2020: 78 · 2019: 70 · 2018: 51 · 2017: 49 · 2016: 63 · 2015: 59 · 2014: 37 · 2013: 50 · 2012: 33
- FWCI
- 14.29
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- 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 › Oceanography › Marine Plankton and Biogeochemistry
- Keywords
- redox-sensitive trace metals, sediment redox conditions, manganese reduction, sulfate reduction, vanadium, molybdenum, uranium, rhenium, cadmium, ocean anoxia, paleo-oxygenation, Arabian Sea
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