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Paleoceanographic applications of trace-metal concentration data
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“The latter may be inferred from trace element enrichments that are intimately associated with organic carbon burial fluxes, which are in turn favored under anoxic depositional conditions (e.g., Ni, Cu, Zn, Cd; Tribovillard et al, 2006;Algeo and Rowe, 2012).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Algeo and Rowe, 2012
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Metadata
- Authors
- Algeo, T. J., & Rowe, H.
- Affiliations
- University of Cincinnati (US)
- The University of Texas at Arlington (US)
- Corresponding author
- Algeo, Thomas J.
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2012-09
- Volume
- 324-325
- Pages
- 6-18
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2074831421
- Cited by
- 537
- References
- 100
- Citations by year
- 2026: 33 · 2025: 45 · 2024: 52 · 2023: 51 · 2022: 45 · 2021: 54 · 2020: 50 · 2019: 52 · 2018: 38 · 2017: 30 · 2016: 40 · 2015: 20 · 2014: 18 · 2013: 3 · 2012: 6
- FWCI
- 6.00
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- Funders
- National Science Foundation
- University of Cincinnati
- 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
- trace metals, paleoceanography, anoxic basins, eustasy, oceanic anoxic events, redox conditions, trace metal cycling
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