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A reevaluation of the oceanic uranium budget for the Holocene
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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 Dunk et al., 2002
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Metadata
- Authors
- Dunk, R. M., Mills, R. A., & Jenkins, W. J.
- Affiliations
- University of Southampton (GB)
- Corresponding author
- Dunk, R.M
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2002-10
- Volume
- 190
- Issue
- 1-4
- Pages
- 45-67
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2026367284
- Cited by
- 341
- References
- 143
- Citations by year
- 2026: 16 · 2025: 12 · 2024: 18 · 2023: 24 · 2022: 22 · 2021: 28 · 2020: 24 · 2019: 16 · 2018: 24 · 2017: 22 · 2016: 21 · 2015: 13 · 2014: 9 · 2013: 14 · 2012: 9
- FWCI
- 7.91
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- ePrints Soton (University of Southampton) (submittedVersion)
- Funders
- Natural Environment Research Council
- 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 › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
- Keywords
- Holocene, groundwater discharge, aeolian dust, uranium isotopes, biogenic carbonates, hydrothermal alteration, seafloor weathering, glacial-interglacial cycles, salt marshes, mangrove sediments
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