Cited by 537Paleontology and Stratigraphy of FossilsGeochemistry and Elemental AnalysisMarine and coastal ecosystems

Paleoceanographic applications of trace-metal concentration data

Algeo, Thomas J., Rowe, Harry·2012·Chemical Geology

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Crossref · 10.1016/j.chemgeo.2011.09.002

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98 of 98 references verified0 citation errors · 0 not checkable

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  • Primary paleo-productivity can be inferred from trace element enrichments tied to organic carbon burial, which are enhanced under anoxic conditions.

    “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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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 and coastal ecosystems
Keywords
trace metals, paleoceanography, anoxic basins, eustasy, oceanic anoxic events, redox conditions, trace metal cycling

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