The DOI matches its Crossref record; 70 of the 71 references it cites were found in a registry or an index.
Trace element content of sedimentary pyrite as a new proxy for deep-time ocean–atmosphere evolution
Open accessOverview
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
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)
Citations
Cites
Trace metals as paleoredox and paleoproductivity proxies: An update
Tribovillard, N., Algeo, T. J., Lyons, T., & Riboulleau, A. (2006) · Chemical Geology · doi:10.1016/j.chemgeo.2006.02.012 · Cited by 4,201
Self-citationAssembly, configuration, and break-up history of Rodinia: A synthesis
Li, Z., Bogdanova, S., Collins, A. S., Davidson, A., Waele, B. D., Ernst, R. E., Fitzsimons, I. C. W., Fuck, R. A., Gladkochub, D. P., Jacobs, J., et al. (2007) · Precambrian Research · doi:10.1016/j.precamres.2007.04.021 · Cited by 3,522
87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater
Veizer, J., Ala, D., Azmy, K., Bruckschen, P., Buhl, D., Bruhn, F., Carden, G. A. F., Diener, A., Ebneth, S., Godderis, Y., et al. (1999) · Chemical Geology · doi:10.1016/s0009-2541(99)00081-9 · Cited by 2,694
A Neoproterozoic Snowball Earth
Hoffman, P. F., Kaufman, A. J., Halverson, G. P., & Schrag, D. P. (1998) · Science · doi:10.1126/science.281.5381.1342 · Cited by 2,693
The Chemical Evolution of the Atmosphere and Oceans
Holland, H. D. (1984) · doi:10.1515/9780691220239 · Cited by 1,836
The oxygenation of the atmosphere and oceans
Holland, H. D. (2006) · Philosophical Transactions of the Royal Society B: Biological Sciences · doi:10.1098/rstb.2006.1838 · Cited by 1,535
(2009) · Developments in sedimentology · doi:10.1016/s0070-4571(09)06212-8 · Cited by 1,334
A new model for Proterozoic ocean chemistry
Canfield, D. E. (1998) · Nature · doi:10.1038/24839 · Cited by 1,243
The size distribution of framboidal pyrite in modern sediments: An indicator of redox conditions
Wilkin, R. T., Barnes, H. L., & Brantley, S. L. (1996) · Geochimica et Cosmochimica Acta · doi:10.1016/0016-7037(96)00209-8 · Cited by 1,195
Proterozoic Ocean Chemistry and Evolution: A Bioinorganic Bridge?
Anbar, A. D., & Knoll, A. H. (2002) · Science · doi:10.1126/science.1069651 · Cited by 1,191
Research works printed but not linked: 1
- Baldwin, 1985, Compaction curves, Am. Assoc. Pet. Geol. Bull., 69, 622
Cited by
Sorted by citations
Orogenic gold: Common or evolving fluid and metal sources through time
Goldfarb, R. J., & Groves, D. I. (2015) · Lithos · doi:10.1016/j.lithos.2015.07.011 · Cited by 1,073
Catling, D. C., & Zahnle, K. J. (2020) · Science Advances · doi:10.1126/sciadv.aax1420 · Cited by 568
A re-assessment of elemental proxies for paleoredox analysis
Algeo, T. J., & Liu, J. (2020) · Chemical Geology · doi:10.1016/j.chemgeo.2020.119549 · Cited by 556
Trace Element Content of Sedimentary Pyrite in Black Shales
Gregory, D. D., Large, R., Halpin, J., Baturina, E. L., Lyons, T., Wu, S., Danyushevsky, L., Sack, P., Chappaz, A., Maslennikov, V., et al. (2015) · Economic Geology · doi:10.2113/econgeo.110.6.1389 · Cited by 468
Self-citationA holistic model for the origin of orogenic gold deposits and its implications for exploration
Groves, D. I., Santosh, M., Deng, J., Wang, Q., Yang, L., & Zhang, L. (2019) · Mineralium Deposita · doi:10.1007/s00126-019-00877-5 · Cited by 429
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
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
