Sedimentation-driven Element Cycling
Sedimentation-Driven Element Cycling is a geochemical framework that describes the systematic redistribution and transformation of chemical elements within Earth's surface environments through the processes of erosion, transport, deposition, and diagenesis, distinguishing it from other biogeochemical cycles by emphasizing physical sedimentation as the primary mechanism controlling elemental fluxes and storage in sedimentary systems.
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207
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2017–2026
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Global distribution of sediment-hosted metals controlled by craton edge stability
Mark Hoggard, Karol Czarnota, Fred Richards et al. · Nature Geoscience · 2020 · 213 citations
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Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
2 publications · 126 citations
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United States Geological Survey
Reston, United States
4 h-index
11 publications
569 citations
University of Bremen
Bremen, Germany
3 h-index
9 publications
375 citations
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
3 h-index
8 publications
492 citations

GEOMAR Helmholtz Centre for Ocean Research Kiel
Kiel, Germany
3 h-index
4 publications
136 citations

Chinese Academy of Sciences
Beijing, China
3 h-index
20 publications
790 citations
Planetary Science Institute
Tucson, United States
3 h-index
5 publications
1K citations
Oregon State University
Corvallis, United States
3 h-index
6 publications
350 citations
University of Chinese Academy of Sciences
Beijing, China
3 h-index
13 publications
513 citations
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6 publications · 778 citations
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4 publications · 936 citations
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4 publications · 121 citations
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