The silicon and oxygen isotope compositions of Precambrian cherts: A record of oceanic paleo-temperatures?
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δ30Si values for IFs are systematically lower than those of similar-aged cherts that are not associated with IFs.
“δ 30 Si values for IFs are systematically lower than those of similar-aged cherts that are not associated with IFs (Marin-Carbonne et al., 2014)”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Marin-Carbonne et al., 2014
Trace element contents might also help separate primary from secondary signals in cherts.
“Trace element abundances themselves may also help resolve primary versus secondary signals preserved in cherts (Baldwin et al. 2011;Marin-Carbonne et al., 2014).”
From Trace elements at the intersection of marine biological and geochemical evolution (2016) · cites this paper as Marin-Carbonne et al., 2014
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“They are relevant in valuing the significance of Si isotopes of Precambrian cherts as a potential record of paleo-ocean temperatures (see Marin-Carbonne et al., 2014 for a recent review), particularly if the cherts formed by direct abiotic chemical precipitation from saturated seawater or…”
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Perspectives on the Origin of Biological Homochirality on Earth
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Triple silicon isotope insights into the formation of Precambrian cherts
Sun, H.-X., Chaussidon, M., Robert, F., Tian, S., Deng, Z., & Moynier, F. (2023) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2023.118069 · Cited by 19 · see citing works
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Fluid inclusion analysis of silicified Palaeoarchaean oceanic crust – A record of Archaean seawater?
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Variations of Stable Isotope Ratios in Nature
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“Similar to previous studies (Marin-Carbonne et al., 2014; Oster et al., 2017), we find that most low-water cherts and quartz have the same IMF.”
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Linge, K. L., Bédard, L. P., Bugoi, R., Enzweiler, J., Jochum, K. P., Kilian, R., Liu, J., Marin‐Carbonne, J., Merchel, S., Munnik, F., et al. (2017) · Geostandards and Geoanalytical Research · doi:10.1111/ggr.12200 · Cited by 12 · see citing works
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Deciphering the source of banded iron formations in the North China Craton
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Silicon Isotope Fractionation in Maize and its Biogeochemical Significance
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The Archean–Hadean Earth: Modern paradigms and ancient processes
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Primary microfossiliferous chert in the Aptian Barra Velha Formation
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“As a result, the fluid becomes progressively enriched in 30 Si (De La Rocha et al ., 2000; Ding et al ., 2004; Georg et al ., 2006; Chakra-barti et al ., 2012; Marin-Carbonne et al ., 2014, and references therein).”
Oxygen isotope analysis of fossil organic matter by secondary ion mass spectrometry
Tartèse, R., Chaussidon, M., Gurenko, A. A., Delarue, F., & Robert, F. (2016) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2016.02.035 · Cited by 9 · see citing works
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“…from temperature-dependent hydrothermal fluxes have positive correlations between oxygen and silicon isotopic compositions, the mass balance equation has been suggested based on variations of silicon isotopes from Precambrian cherts (Robert and Chaussidon, 2006; Marin-Carbonne et al., 2014).”
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Isotope Fractionation Processes of Selected Elements
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Silicon and oxygen isotope fractionation in a silicified carbonate rock
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“…especially under non-equilibrium conditions proposed for the formation of Precambrian chert (van den Boorn et al. 2007; Boorn et al. 2010 ), and that the opal-A to micro-crystalline quartz transition is accompanied by a δ 30 Si decrease of some 3‰ (Marin-Carbonne et al. 2014 ; Geilert et al. 2016).”
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“Next, dissolution- precipitation reactions resulted in the transformation of Opal-CT to microcrystalline quartz (Knauth, 1994; Marin-Carbonne et al., 2014).”
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“Another source could be direct precipitation from silica- rich seawater (Ledevin et al., 2019; Maliva & Siever, 1989), which could be expected for ancient Precambrian basins (Marin- Carbonne et al., 2014).”
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The Case for a Hot Archean Climate and its Implications to the History of the BiospherePreprint
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“…to be more complicated than argued by Robert and Chaussidon (2006), with numerous papers since this publication having discussed this isotopic record (van den Boorn et al., 2009; Heck et al., 2011; Marin et al., 2010; Marin-Carbonne et al., 2012, 2014; Geilert et al., 2014; Stefurak et al., 2015).”
BackgroundMethod
- Authors
- Marin-Carbonne, J., Robert, F., & Chaussidon, M.
- Affiliations
- Laboratoire de Minéralogie & Cosmochimie du Muséum (FR)
- Centre National de la Recherche Scientifique (FR)
- Venue
- Precambrian Research
- Publisher
- Elsevier BV
- Published
- 2014-07
- Volume
- 247
- Pages
- 223-234
- ISSN
- 0301-9268 (ISSN-L)
- OpenAlex
- W2034769266
- Cited by
- 157
- References
- 84
- Citations by year
- 2026: 12 · 2025: 14 · 2024: 13 · 2023: 15 · 2022: 10 · 2021: 14 · 2020: 14 · 2019: 10 · 2018: 12 · 2017: 14 · 2016: 10 · 2015: 16 · 2014: 2
- FWCI
- 9.38
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Precambrian Research (publishedVersion)
- HAL (submittedVersion)
- Funders
- Agence Nationale de la Recherche (ANR-11-IDEX-0005, ANR-10-LABX-0023)
- Labex UnivEarthS
- 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 › Geophysics › Geological and Geochemical Analysis
- Keywords
- chert, silicon isotopes, oxygen isotopes, Precambrian, chert origin, diagenesis, trace element composition
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