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New insights into Archean sulfur cycle from mass-independent sulfur isotope records from the Hamersley Basin, Australia
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“The pyrite in the S-MIF interval (below the pink band in Fig. 2) carries distinct S-MIF signals, with Δ33S reaching as high as +8‰ and the Δ36S/Δ33S ratios centering around −0.98, which is characteristic of the Neoarchean array (Fig. 3) (30, 43).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [30]
In the citing paper
“This is also supported by the Δ36S/Δ33S slope of −0.9, which is widespread in Neoarchean sedimentary rocks and interpreted to be of atmospheric origin (9, 25, 30, 43).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [30]
In the citing paper
“For simplicity, we did not explicitly model different kinetics for different forms of sulfur (for example, thiosulfate, S8, or sulfate) that are likely present in the Archean oceans (1, 30).”
From Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago (2016) · cites this paper as [30]
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Total Pressure Dependence of Sulfur Mass‐Independent Fractionation by SO2Photolysis
Endo, Y., Danielache, S. O., & Ueno, Y. (2018) · Geophysical Research Letters · doi:10.1029/2018gl080730 · Cited by 23
“489 logical records can be reproduced, whereas above 100 kPa of pTotal, the observed large Δ33S values (Δ33S > +14‰) cannot be produced by mixing between the photoproduct and normal MDF source of sulfur at surface (Ono et al., 2003).”
BackgroundComputational refinement of the puzzling red tetrasulfur chromophore in ultramarine pigments
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Tracking Water‐Rock Interaction at the Atlantis Massif (MAR, 30°N) Using Sulfur Geochemistry
Liebmann, J., Schwarzenbach, E. M., Früh‐Green, G. L., Boschi, C., Rouméjon, S., Strauß, H., Wiechert, U., & John, T. (2018) · Geochemistry Geophysics Geosystems · doi:10.1029/2018gc007813 · Cited by 23
“…on the analyses of the traditional 34S/32S ratio as a tracer for Earth systems processes, whereas interest in measuring ratios of the less abundant 33S and 36S isotopes was limited to the study of extraterrestrial materials (Farquhar et al., 2000) and Archean sedimentary rocks (Ono et al., 2003).”
BackgroundKrull-Davatzes, A. E., Byerly, G. R., & Lowe, D. R. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.05.014 · Cited by 23
Hou, K., Ma, X., Li, Y., Liu, F., & Han, D. (2018) · Journal of Geochemical Exploration · doi:10.1016/j.gexplo.2018.11.005 · Cited by 21
Mesoarchaean Gold Mineralisation in the Barberton Greenstone Belt: A Review
Agangi, A., Hofmann, A., Eickmann, B., & Marin‐Carbonne, J. (2019) · Regional geology reviews · doi:10.1007/978-3-319-78652-0_7 · Cited by 21
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Marti, A. M., Fox‐Powell, M. G., Cousins, C. R., Macey, M. C., & Zerkle, A. L. (2022) · Journal of the Geological Society · doi:10.1144/jgs2021-134 · Cited by 22
“This process has already been observed in late Archaean rocks, revealing trends that reflect S-MIF signals were overprinted by S-cycling microorganisms (Ono et al., 2003; Zerkle et al., 2021).”
BackgroundMechanisms and climatic-ecological effects of the Great Oxidation Event in the early Proterozoic
Luo, G., Zhu, X., Wang, S., Zhang, S., & Jiao, C. (2022) · Science China Earth Sciences · doi:10.1007/s11430-021-9934-y · Cited by 20
“4 Ga indeed reflect a rise of pO2 to >10 −5 PAL, as temporary low Δ(33)S values also exist in Archean strata (Ono et al., 2003).”
BackgroundInfluentialGrosch, E. G., & McLoughlin, N. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.06.035 · Cited by 20
Intercomparison measurements of two 33S-enriched sulfur isotope standards
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Liebmann, J., Spencer, C. J., Kirkland, C. L., Bucholz, C. E., Xia, X., Martin, L. A. J., Kitchen, N., & Shumlyanskyy, L. V. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2021.05.045 · Cited by 21
“A similar scenario has been suggested to be responsible for the negative d34S values and positive D33S values of pyrite in the Archean upper Mount McRae Shale in the Hamersley Basin, Western Australia (Ono et al., 2003; Kaufman et al., 2007).”
BackgroundLiu, P., Harman, C. E., Kasting, J. F., Hu, Y., & Wang, J. (2019) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2019.115767 · Cited by 20
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Quadruple sulfur isotopic fractionation during pyrite desulfidation to pyrrhotite
Liu, L., Mavrogenes, J., Holden, P. N., & Ireland, T. R. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.01.024 · Cited by 18
Tracing the Early Emergence of Microbial Sulfur Metabolisms
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The Sedimentary Sulfur System: Biogeochemistry and Evolution through Geologic Time
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Ohmoto, H., Runnegar, B. N., Kump, L. R., Fogel, M. L., Kamber, B. S., Anbar, A. D., Knauth, P., Lowe, D. R., Sumner, D. Y., & Watanabe, Y. (2008) · Astrobiology · doi:10.1089/ast.2008.0257 · Cited by 20
“…under O 2 poor or O 2 rich atmosphere (Farquhar and Wing, 2003; Ohmoto et al ., 2006b) or by the UV photolysis of volcanic SO 2 in an O 2 poor atmosphere, as suggested by many investigators who have used multiple sulfur isotopes (Farquhar et al ., 2000; Far-quhar and Wing, 2003; Ono et al ., 2003).”
Multiple sulfur isotope signature of early Archean oceanic crust, Isua (SW-Greenland)
Siedenberg, K., Strauß, H., & Hoffmann, J. E. (2016) · Precambrian Research · doi:10.1016/j.precamres.2016.07.002 · Cited by 18
Zhao, Y., Zhang, Y., & Sun, R. (2021) · Atmospheric Research · doi:10.1016/j.atmosres.2020.105447 · Cited by 18
Liu, C., & Li, W. (2019) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2019.12.027 · Cited by 17
“Except for some photochemical or organo-chemical reactions of certain elements (e.g., S, Thiemens, 1999; Farquhar et al., 2000; Ono et al., 2003; Hg, Bergquist and Blum, 2007; Sherman et al., 2010; Point et al., 2011), most of isotopes in terrestrial conditions demonstrate mass-dependent behavior (Johnson et al.”
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Rodiouchkina, K., Rodushkin, I., Goderis, S., & Vanhaecke, F. (2022) · Analytica Chimica Acta · doi:10.1016/j.aca.2022.340744 · Cited by 16
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Decoupling of Neoarchean sulfur sources recorded in Algoma-type banded iron formation
Diekrup, D., Hannington, M. D., Strauß, H., & Ginley, S. (2018) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2018.02.022 · Cited by 17
Quadruple sulfur isotope biosignatures from terrestrial Mars analogue systems
Marti, A. M., Fox‐Powell, M. G., Stüeken, E. E., Rocco, T. D., Galloway, T., Osinski, G. R., Cousins, C. R., & Zerkle, A. L. (2021) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2021.06.007 · Cited by 16
Hiebert, R. S., Bekker, A., Houlé, M. G., & Rouxel, O. J. (2018) · Precambrian Research · doi:10.1016/j.precamres.2018.04.004 · Cited by 16
An isotopic analysis of ionising radiation as a source of sulphuric acid
Enghoff, M. B., Bork, N., Hattori, S., Meusinger, C., Nakagawa, M., Pedersen, J. O. P., Danielache, S. O., Ueno, Y., Johnson, M. S., Yoshida, N., et al. (2012) · Atmospheric chemistry and physics · doi:10.5194/acp-12-5319-2012 · Cited by 15
“NMD signatures have been found in atmospheric sulphate aerosols (Baroni et al., 2007; Pavlov et al., 2008) and Archean rock samples (Farquhar et al., 2000a; Ono et al., 2003; Ueno et al., 2008; Bao et al., 2007).”
BackgroundCaruso, S., Fiorentini, M. L., Hollis, S. P., LaFlamme, C. K., Baumgartner, R. J., Steadman, J. A., & Savard, D. (2018) · Precambrian Research · doi:10.1016/j.precamres.2018.08.012 · Cited by 16
Maynard, J. B., Sutton, S. J., Rumble, D., III, & Bekker, A. (2013) · Chemical Geology · doi:10.1016/j.chemgeo.2013.09.011 · Cited by 15
“Measurements of MIF-S have now been applied not only to a number of sulfidebearing rocks, mostly marine shales and carbonates (e.g. Mojzsis et al., 2003; Ono et al., 2003; Johnston et al., 2006; Papineau et al., 2007; Johnston, 2011;Williford et al., 2011), but also to marine hydrothermal systems (Jamieson et al.”
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House, C. H. (2009) · Methods in Molecular Biology · doi:10.1007/978-1-60327-853-9_8 · Cited by 18
Teles, G. D. S., Chemale, F., Ávila, J. N., Ireland, T. R., Dias, A. N. C., Cruz, D. C. F., & Constantino, C. J. L. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.01.035 · Cited by 14
Euxinia in the Neoarchean: The starting point for early oxygenation in a Brazilian Craton
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VUV pressure-broadening in sulfur dioxide
Lyons, J. R., Herde, H., Stark, G., Blackie, D., Pickering, J. C., & de Oliveira, N. (2018) · Journal of Quantitative Spectroscopy and Radiative Transfer · doi:10.1016/j.jqsrt.2018.02.013 · Cited by 14
Kopf, S., & Ono, S. (2012) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2012.02.008 · Cited by 15
Self-citationWeathering model for the quantification of atmospheric oxygen evolution during the Paleoproterozoic
Yokota, K., Kanzaki, Y., & Murakami, T. (2013) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2013.03.015 · Cited by 14
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Gallagher, M., Whitehouse, M. J., & Kamber, B. S. (2017) · Geobiology · doi:10.1111/gbi.12234 · Cited by 12
“, SO2 and/or H2SO4 (Δ 33S <0), both of which are rained out to the hydrosphere and subsequently delivered to the ocean and sediments (Farquhar et al., 2001; Ono et al., 2003).”
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A thermodynamic chemical reaction network drove autocatalytic prebiotic peptides formation
Bao, P., He, Y., Li, G., Zhang, H., & Xiao, K. (2022) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2022.03.004 · Cited by 13
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“However, a very distinct record of mass-independent sulphur isotopes exists [7, 26, 48, 52 ], thereby pointing to an atmospheric oxygen abundance of <10 −5 PAL [57].”
BackgroundTriple Oxygen Isotope Analysis of Methanesulfonate Using the SO 3 – Fragment in ESI-Orbitrap-MS
Hong, Y., Zhu, L., Crocker, D. R., et al. (2025) · Analytical Chemistry · doi:10.1021/acs.analchem.5c01382 · Cited by 11
Structure changes of nanocrystalline mackinawite under hydrothermal conditions
Sano, Y., Kyono, A., Yoneda, Y., Isaka, N., Takagi, S., & Yamamoto, G.-I. (2020) · Journal of Mineralogical and Petrological Sciences · doi:10.2465/jmps.190903 · Cited by 11
“This biological sulfur cycle called ‘sulfur cycle’ is one of the most essential elemental cycles at the Earth’s surface (Kellogg et al., 1972; Ono et al., 2003; Fike et al., 2015).”
BackgroundPeng, Z., Wang, C., Poulton, S. W., Tong, X., Konhauser, K. O., & Zhang, L. (2022) · Economic Geology · doi:10.5382/econgeo.4920 · Cited by 11
Archaean asteroid impacts, banded iron formations and MIF-S anomalies: A discussion
Glikson, A. Y. (2009) · Icarus · doi:10.1016/j.icarus.2009.11.024 · Cited by 11
Reactivity of Electronically Excited SO2 with Alkanes
Kroll, J. A., Frandsen, B. N., Rapf, R. J., Kjaergaard, H. G., & Vaida, V. (2018) · The Journal of Physical Chemistry A · doi:10.1021/acs.jpca.8b04643 · Cited by 11
From minerals to metabolisms: Evidence for life before oxygen from the geological record
Johnson, J. E. (2019) · Free Radical Biology and Medicine · doi:10.1016/j.freeradbiomed.2019.01.047 · Cited by 14
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Ranjan, S., Abdelazim, K., Lozano, G. G., Mandal, S., Zhou, C. Y., Kufner, C. L., Todd, Z. R., Sahai, N., & Sasselov, D. D. (2023) · AGU Advances · doi:10.1029/2023av000926 · Cited by 12
“However, early Earth may have featured less SO 2 outgassing due to lower concentrations of recycled oceanic sulfate (Harman, Pavlov, et al., 2018), or due to higher magmatic degassing pressures (Gaillard et al., 2011), though this is debated (Brounce et al., 2017; Korenaga, 2021).”
BackgroundVelivetskaya, T. A., Ignatiev, A. V., & Yakovenko, V. V. (2020) · Geochemistry International · doi:10.1134/s0016702920110105 · Cited by 10
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Sulfur mass-independent fractionation during SO2 photolysis in low-temperature/pressure atmospheres
Endo, Y., Sekine, Y., & Ueno, Y. (2022) · Chemical Geology · doi:10.1016/j.chemgeo.2022.121064 · Cited by 8
Multiple Sulfur Isotopic Evidence for Sulfate Formation in Haze Pollution
Han, X., Dong, X., Liu, C., Wei, R., Lang, Y., Strauß, H., & Guo, Q. (2023) · Environmental Science & Technology · doi:10.1021/acs.est.3c05072 · Cited by 9
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Multiple Sulfur Isotope Records of the 3.22 Ga Moodies Group, Barberton Greenstone Belt
Saitoh, M., Nabhan, S., Thomazo, C., Olivier, N., Moyen, J., Ueno, Y., & Marin‐Carbonne, J. (2020) · Geosciences · doi:10.3390/geosciences10040145 · Cited by 9
“9, termed the Archean Reference Array (ARA) [45], which is not recognized in our dataset.”
BackgroundInfluentialBosco‐Santos, A., Gilhooly, W., de Melo-Silva, P., Fouskas, F., Bouyon, A., Motta, J. G., Baldim, M. R., Fabricio-Silva, W., Philippot, P., & OLIVEIRA, E. P. D. (2021) · Geoscience Frontiers · doi:10.1016/j.gsf.2021.101250 · Cited by 9
“Small ranges inD33S that expanded into larger fractionations leading up to the Great Oxygenation Event (GOE; 2.45–2.2 Ga) are disproportionately represented by sequences from the Kaapvaal and Pilbara Cratons.”
BackgroundInfluentialTeles, G. D. S., Chemale, F., Ávila, J. N., & Ireland, T. R. (2021) · Geoscience Frontiers · doi:10.1016/j.gsf.2021.101252 · Cited by 9
Theca2.74 Ga Mopoke Member, Kylena Formation: a marine incursion into the northern Fortescue Group?
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“…for providing insights into the composition of the Archean atmosphere based on stable carbon and multiple sulfur isotopes (e.g. Pavlov et al. 2001; Ono et al. 2003; Eigenbrode & Freeman 2006; Thomazo et al. 2009), for insights into Archean microbial communities from stromatolites (e.g. Walter…”
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“…sulfate got thermochemically (TSR) or bacterially (BSR) reduced and precipitated as sedimentary sulfides, or as evaporitic or exhalative sulfides in cherts, banded iron formation (BIF), and volcanogenic massive sulfide (VMS) reservoirs (e.g., Canfield 2001; Ono et al. 2003; Farquhar et al. 2013).”
InfluentialMacdonald, J. E., Sugden, P. J., Dumont, M., Szilas, K., Glorie, S., Simpson, A. D., Gilbert, S., Burke, A., & Stüeken, E. E. (2024) · Geobiology · doi:10.1111/gbi.12595 · Cited by 8
“…sulfur species (SO 2 and H 2 S, initial ∆ 33 S = 0; Siedenberg et al., 2016) are injected into the atmosphere, where they undergo photolysis generating a MIF signal that is carried by the major products, S 8 (∆ 33 S > 0) and H 2 SO 4 (∆ 33 S < 0) (Claire et al., 2014; Ono et al., 2003).”
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Multiple sulfur isotopes evidence deep intra-slab transport of sulfate-rich fluids
Genot, I., Angiboust, S., & Cartigny, P. (2024) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2024.05.025 · Cited by 8
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Archean Asteroid Impacts on Earth
Krull-Davatzes, A. E., Goderis, S., & Simonson, B. M. (2018) · Elsevier eBooks · doi:10.1016/b978-0-444-63901-1.00008-3 · Cited by 8
Deposition of sulfate aerosols with positive Δ33S in the Neoarchean
Paris, G., Fischer, W. W., Johnson, J. E., Webb, S. M., Present, T. M., Sessions, A. L., & Adkins, J. F. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.06.028 · Cited by 9
“Unusual sulfur isotope compositions have been observed in Archean sedimentary rocks until their disappearance from the rock record in early Proterozoic time associated with the Great Oxygenation Event (Farquhar et al., 2000; Ono et al., 2003; Guo et al., 2009; Johnston, 2011; Luo et al., 2016; Philippot et al., 2018).”
BackgroundMineralogical Co‐Evolution of the Geosphere and Biosphere
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Kinetic factors control trace element and isotope zoning in Archean pyrite corona nodules
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Simon, L., Lécuyer, C., Martineau, F., & Robert, F. (2011) · Central European Geology · doi:10.1556/ceugeol.54.2011.1-2.8 · Cited by 7
“Sulfur species in Precambrian seawater were both in reduced and oxidized states as suggested by the high variability of sulfur isotope ratios of both sulfides and sulfates in Precambrian rocks older than 2.4 Ga (Farquhar et al. 2000; Farquhar and Wing 2003; Ono et al. 2003).”
BackgroundInfluentialSensitivity of mass-independent Sn isotope fractionation to UV radiation and magnetic fields
She, J.-X., Li, W., Zhang, S., Gu, C., Chen, X., Zheng, H., Xu, C., & Liu, W. (2025) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.2504065122 · Cited by 6
“Sn - MIF signatures may also be archived via adsorption onto clay minerals ( 41 , 42 ) in shales or sequestration within sulfide phases (e.g., stannite), mirroring sulfur MIF preservation pathways ( 43 , 44 ).”
Coldebella, B., LaFlamme, C. K., Malta, I. S., Guilmette, C., Barré, G., Beaudoin, G., Martin, L. A. J., & Savard, D. (2025) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2024.12.027 · Cited by 6
Vysotskiy, S. V., Velivetskaya, T. A., Ignatiev, A. V., Slabunov, A. I., & Асеева, А. В. (2022) · Minerals · doi:10.3390/min12091143 · Cited by 8
Kumar, P., & Poirier, B. (2019) · Molecular Physics · doi:10.1080/00268976.2019.1567850 · Cited by 6
Liu, L., Ireland, T. R., Holden, P. N., Ávila, J. N., Vasconcelos, P. M., & Mavrogenes, J. (2021) · Contributions to Mineralogy and Petrology · doi:10.1007/s00410-021-01788-3 · Cited by 6
Microbial sulphur-cycling and atmospheric signatures in the 2.52 Ga Gamohaan Formation, South Africa
McLoughlin, N., Li, M., Wacey, D., Martin, L. A. J., Shen, Y., & Beukes, N. J. (2022) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2022.117941 · Cited by 6
Faint Young Sun, Planetary Paleoclimates and Varying Fundamental Constants
Tomaschitz, R. (2005) · International Journal of Theoretical Physics · doi:10.1007/s10773-005-1492-4 · Cited by 7
“(Kasting, 1989). Further circumstantial evidence for a warm Archean Earth is the 34 S depletion in sediments dated back to 2.6 − 3.5 Gyr, possibly caused by sulfurreducing bacteria in 30 − 50 ◦ C oceans ( Ohmoto and Felder, 1987; Habicht et al., 2002; Ono et al., 2003).”
BackgroundInfluentialBond Dissocation and Conformational Energetics of Tetrasulfur: A Quantum Monte Carlo Study
Harkless, J. A. W., & Francisco, J. S. (2008) · The Journal of Physical Chemistry A · doi:10.1021/jp076376h · Cited by 6
Poulson, S. R. (2004) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.1754 · Cited by 6
The Evolution of the Sedimentary Sulfur Cycle
Rickard, D. T. (2012) · Developments in sedimentology · doi:10.1016/b978-0-444-52989-3.00017-9 · Cited by 6
Origin and Evolution of Atmospheres
Visconti, G. (2021) · Springer eBooks · doi:10.1007/978-3-030-74713-8_1 · Cited by 6
The Identification and Interpretation of Microbial Biogeomagnetism
Kopp, R. E. (2007) · CaltechTHESIS (California Institute of Technology) · doi:10.7907/83r3-vb23 · Cited by 8
Runge, E., Vulpius, S., Herwartz, D., Pack, A., Brachmann, C., & Noack, L. (2025) · Geo-Bio Interfaces · doi:10.1180/gbi.2025.10003 · Cited by 6
“Between about 2.7 and 2.5 Ga a pronounced MIF-S spike is observed coinciding with the GOE (Farquhar, 2000; Mojzsis et al. , 2003; Ono et al. , 2003; Hu et al. , 2003; Bekker et al. , 2004; Whitehouse et al. , 2005; Papineau et al. , 2005; Jamieson et al. , 2006; Ohmoto et al. , 2006a; Ono et al. ,…”
InfluentialVysotskiy, S. V., Velivetskaya, T. A., Ignatiev, A. V., Kuleshevich, L. V., & Slabunov, A. I. (2022) · Russian Geology and Geophysics · doi:10.2113/rgg20214413 · Cited by 5
Sulphur tales from the early Archean world
Montinaro, A., & Strauß, H. (2016) · International Journal of Astrobiology · doi:10.1017/s1473550415000531 · Cited by 5
“Experimental work revealed a minor change in the minor sulphur isotopes related to elemental sulphur disproportionation with an increase in Δ36S and a decrease in Δ33S compared with the reactant sulphur (Farquhar et al. 2003; Johnston et al. 2005, 2007), while for bacterial sulphate reduction a slight increase in Δ33S…”
BackgroundInfluentialVysotskiy, S. V., Игнатьев, А. В., Levitskii, V. I., Velivetskaya, T. A., Асеева, А. В., Levitskiy, I. V., & Мехоношин, А. С. (2019) · Russian Geology and Geophysics · doi:10.15372/rgg2019062 · Cited by 5
Chen, M., Huang, Z., Campbell, I. H., Sambridge, M., & Ávila, J. N. (2021) · Chemical Geology · doi:10.1016/j.chemgeo.2021.120640 · Cited by 5
Calcitized evaporites in the Mesoproterozoic Atar and El Meriti Groups, Mauritania, Africa
Manning‐Berg, A., Goodman, E. E., & Kah, L. C. (2023) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2023.111974 · Cited by 5
Diverse sources of sulfur in Archean ore deposits of the southwest Yilgarn Craton, Western Australia
Duuring, P., & González-Álvarez, I. (2025) · Mineralium Deposita · doi:10.1007/s00126-025-01386-4 · Cited by 4
Sulfur recombination: A direct approach
Koots, R., Brown, G. E., & Pérez‐Ríos, J. (2024) · The Journal of Chemical Physics · doi:10.1063/5.0222273 · Cited by 6
An analysis of Δ36S/Δ33S dependence on definitions of sulfur mass-independent fractionation
Endo, Y., Chen, M., & Claire, M. W. (2024) · Chemical Geology · doi:10.1016/j.chemgeo.2024.122157 · Cited by 4
Ueno, Y., Danielache, S. O., & Yoshida, N. (2015) · Origins of Life and Evolution of Biospheres · doi:10.1007/s11084-015-9447-0 · Cited by 4
“In the anoxic atmosphere, the SO2 remaining after photolysis and the photolysis products could be finally transformed into sulfate and elemental sulfur aerosols, respectively (Ono et al. 2003).”
BackgroundLi, Y., Hou, K., Defang, W., & Yue, G. (2008) · Acta Geologica Sinica - English Edition · doi:10.1111/j.1755-6724.2008.tb00595.x · Cited by 4
Metadata
- Authors
- Ono, S., Eigenbrode, J. L., Pavlov, A. A., Kharecha, P., Rumble, D., Kasting, J. F., & Freeman, K. H.
- Affiliations
- Carnegie Institution for Science (US)
- Pennsylvania State University (US)
- University of Colorado Boulder (US)
- Corresponding author
- Ono, Shuhei
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2003-08
- Volume
- 213
- Issue
- 1-2
- Pages
- 15-30
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W1988435801
- Cited by
- 363
- References
- 65
- Citations by year
- 2026: 13 · 2025: 7 · 2024: 12 · 2023: 8 · 2022: 18 · 2021: 17 · 2020: 15 · 2019: 19 · 2018: 22 · 2017: 18 · 2016: 13 · 2015: 10 · 2014: 14 · 2013: 24 · 2012: 22
- FWCI
- 14.66
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- Pennsylvania State University
- University of Colorado
- National Science Foundation (EAR-0125096, EAR-0073831)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Keywords
- Hamersley Basin, pyrite sulfur, sulfide sulfur, UV photolysis, early atmosphere, microbial sulfur metabolism, mass-dependent fractionation
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