Cited by 341Geochemistry and Elemental AnalysisPaleontology and Stratigraphy of FossilsGroundwater and Isotope Geochemistry

A reevaluation of the oceanic uranium budget for the Holocene

Dunk, R.M, Mills, R.A, Jenkins, W.J·2002·Chemical Geology

Integrity signals

Registry

Crossref · 10.1016/s0009-2541(02)00110-9

Cites

136 of 136 references verified0 citation errors · 0 not checkable

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  • Cr has a shorter residence time, about 9 kyr, than U and Mo, about 800 kyr and 400 kyr.

    “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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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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