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Trace element content of sedimentary pyrite as a new proxy for deep-time ocean–atmosphere evolution
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In the citing paper
“Furthermore, Archean marine sediments have low concentrations of elements that enter rivers during oxidative continental weathering (68–70).”
From The Archean atmosphere (2020) · cites this paper as [69]
In the citing paper
“Under more oxic conditions first observed in the Cryogenian and continuing to develop into the Cambrian-Ordovician (Large et al., 2014;Sperling et al., 2015;Sahoo et al., 2016), the models of Saito et al. (2003) indicated that Fe and Mn concentrations in seawater would have been drawn down to modern levels as the result of oxide mineral precipitation.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Large et al. (2014) also provided an assessment of the importance of pyrite versus matrix trace element incorporation, sulfide recrystallization, and the location in the water column or sediment where pyrite forms, which suggest the record is favorable to recording seawater signatures; a result further supported by several additional studies (Gregory et al., 2014;Large et al., 2015;Mukherjee and”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Pyrite (FeS2) can form in sediments contemporaneous with deposition or during early diagenesis, and it may therefore incorporate trace element signatures characteristic of seawater (see Large et al., 2014).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Large et al. (2014) presented a suite of Ni analyses in sedimentary to early diagenetic pyrite that mirrored the observed temporal trend in Ni/Fe ratios observed in IF.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Interestingly, the first-order trends in Ni abundances observed in the IF record (Fig. 6) are also recorded in sedimentary pyrite.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“An observation that supports this assertion is the high Ni and Co values observed in pyrites in the Late Permian (Large et al., 2014), in which case the Ni and Co may be associated with the Siberian traps volcanism and Permian mass extinction”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Large et al. (2014) further noted a correlation between Ni and Co in the pyrite record, and suggested that this may be tied to the emplacement and subsequent erosion of large igneous provinces.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“However, the syngenetic and early diagenetic pyrite record for Co presented by Large et al. (2014) indicates a steadier decline in Co levels from 3 Ga to present.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“They argued that Cr should be sourced from ultramafic rocks similar to Ni and Co, and that this decrease may reflect a decrease in the abundance of the source”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Large et al. (2014) attributed a decrease in Cr concentrations, from the Archean to the Proterozoic (Fig. 9), as reflective of a change in source availability.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Large et al. (2014) also investigated Cr and Mo concentrations in sedimentary pyrite and found patterns consistent with the dominance of anoxic settings in the Proterozoic from 2.15 to 0.7 Ga, with euxinic settings more prevalent between 1.2 and 0.8 Ga.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“They attribute this rise to enhanced oxidative weathering of U-rich granites.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“In their analyses of syngenetic and early diagenetic pyrite, Large et al. (2014) showed a temporal trend in Se with several small peaks at 3.0 and 2.4 Ga, along with a Paleoproterozoic to Mesoproterozoic perturbation between 1800-1300 Ma, and finally a rise in the Neoproterozoic to Phanerozoic.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Large et al. (2014) further suggested that this trend in Se may be used as a paleoproxy for tracking oxygenation.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“laser ablation analyses of black shale matrices by Large et al. (2014) seem to show an increase in U during the Mesoproterozoic, with a peak between 1.4 to 1.7 Ga”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“Overall, it appears that the black shale record for V mirrors that of Mo, and is relatively consistent with Neoproterozoic enrichments seen in the pyrite record (Large et al., 2014).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al., 2014
In the citing paper
“A similar trend is observed in the pyrtie record as presented by Large et al. (2014), however, some variability in the Phanerozoic is observed in the pyrite record that is not present in the IF record.”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al. (2014)
In the citing paper
“similar to the shale matrix record of Large et al. (2014)”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Large et al. (2014)
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Metadata
- Authors
- Large, R. R., Halpin, J. A., Danyushevsky, L. V., Maslennikov, V. V., Bull, S. W., Long, J. A., Gregory, D. D., Lounejeva, E., Lyons, T. W., Sack, P. J., McGoldrick, P. J., & Calver, C. R.
- Affiliations
- University of Tasmania (AU)
- Flinders University (AU)
- University of California, Riverside (US)
- Yukon Geological Survey (CA)
- Corresponding author
- Large, Ross R.
- ORCID
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2014-03
- Volume
- 389
- Pages
- 209-220
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W1969023317
- Cited by
- 545
- References
- 71
- Citations by year
- 2026: 46 · 2025: 59 · 2024: 45 · 2023: 56 · 2022: 54 · 2021: 47 · 2020: 66 · 2019: 45 · 2018: 39 · 2017: 36 · 2016: 18 · 2015: 26 · 2014: 8
- FWCI
- 19.65
- Type
- journal article
- Language
- en
- Open access
- green
- figshare.com
- Licence
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- eCite Digital Repository (University of Tasmania) (submittedVersion)
- Figshare (submittedVersion, cc-by)
- Funders
- ARC Centre of Excellence (CE0561595)
- AMIRA (P923)
- 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 › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- sedimentary pyrite, trace elements, black shales, seawater chemistry, Great Oxidation Event, ocean anoxia, large igneous provinces, continental erosion, Precambrian, Proterozoic, Archean, seawater nutrients, selenium, molybdenum, uranium, nickel, cobalt, Cryogenian, paleo-oxygenation
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