Contrasting sulfur geochemistry and Fe/Al and Mo/Al ratios across the last oxic-to-anoxic transition in the Cariaco Basin, Venezuela
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Unlike iron formations, black shales have modern analogues-the Cariaco Basin and Black Sea-that can help explain how ancient counterparts formed and took up trace metals.
“A significant advantage of the black shale record over the IF archives is that examples from modern settings, such as the Cariaco Basin and the Black Sea (e.g., Lyons and Berner, 1992;Lyons et al., 2003;Algeo and Lyons, 2006;Scott et al., 2008;2013;Reinhard et al., 2013b), can be used as analogues to understand the processes underpinning the formation and the pathways of trace metal uptake for the”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Lyons et al., 2003
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- Authors
- Lyons, T. W., Werne, J. P., Hollander, D. J., & Murray, R. W.
- Affiliations
- University of Missouri (US)
- Northwestern University (US)
- Boston University (US)
- Corresponding author
- Lyons, Timothy W
- Venue
- Chemical Geology
- Publisher
- Elsevier BV
- Published
- 2003-04
- Volume
- 195
- Issue
- 1-4
- Pages
- 131-157
- ISSN
- 0009-2541 (ISSN-L)
- OpenAlex
- W2104296040
- Cited by
- 432
- References
- 120
- Citations by year
- 2026: 12 · 2025: 18 · 2024: 25 · 2023: 25 · 2022: 22 · 2021: 31 · 2020: 27 · 2019: 29 · 2018: 13 · 2017: 16 · 2016: 22 · 2015: 24 · 2014: 20 · 2013: 20 · 2012: 19
- FWCI
- 11.43
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Chemical Geology (publishedVersion)
- 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
- Cariaco Basin, euxinia, pyrite sulfur isotopes, Fe/Al ratio, iron scavenging, siliciclastic input, organic carbon, Late Pleistocene, postglacial sea-level rise, Black Sea
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