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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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Atmospheric sulfur rearrangement 2.7 billion years ago: Evidence for oxygenic photosynthesis
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Primary Productivity Was Limited by Electron Donors Prior to the Advent of Oxygenic Photosynthesis
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“Assuming a volcanic SO2 outgassing flux of ~10 11 moles/year (Ono et al., 2003), sulfur could fuel at most only about 4 × 1010 moles carbon fixed per year, less than 2% of the estimate for H2-fueled productivity.”
BackgroundHalevy, I. (2013) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1213148110 · Cited by 89
Finding a Second Sample of Life on Earth
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“However, the accumulation of atmospheric oxygen was a slow process, and to reach levels that would interfere with organic synthesis would be unlikely to have occurred before about 3 Gyr (Catling and Zahnle, 2002; Ono et al., 2003).”
Biological regulation of atmospheric chemistry en route to planetary oxygenation
Izon, G., Zerkle, A. L., Williford, K. H., Farquhar, J., Poulton, S. W., & Claire, M. W. (2017) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1618798114 · Cited by 86
“Consequently, it seems that the dominant sulfur source for pyrite formation over the examined interval was elemental sulfur, inferred to carry a positive Δ(33)S (7, 18, 25).”
BackgroundLithofacies control on multiple-sulfur isotope records and Neoarchean sulfur cycles
Ono, S., Kaufman, A. J., Farquhar, J. D., Sumner, D. Y., & Beukes, N. J. (2008) · Precambrian Research · doi:10.1016/j.precamres.2008.10.013 · Cited by 86
Self-citationSteadman, J. A., Large, R. R., Meffre, S., Olin, P., Danyushevsky, L. V., Gregory, D. D., Belousov, I. A., Lounejeva, E., Ireland, T. R., & Holden, P. N. (2015) · Economic Geology · doi:10.2113/econgeo.110.5.1157 · Cited by 86
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“These data likely result from mixing with elemental sulfur and 34S-enriched seawater sulfate (e.g., Ono et al., 2003; Kamber and Whitehouse, 2007).”
BackgroundChemical and biological evolution of early Earth: Constraints from banded iron formations
Ohmoto, H., Watanabe, Y., Yamaguchi, K. E., Naraoka, H., Haruna, M., Kakegawa, T., Hayashi, K., & Kato, Y. (2006) · Geological Society of America eBooks · doi:10.1130/2006.1198(17 · Cited by 86
Large sulfur isotope fractionations associated with Neoarchean microbial sulfate reduction
Zhelezinskaia, I., Kaufman, A. J., Farquhar, J. D., & Cliff, J. (2014) · Science · doi:10.1126/science.1256211 · Cited by 91
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Multiple sulfur isotopes of sulfides from sediments in the aftermath of Paleoproterozoic glaciations
Papineau, D., Mojzsis, S. J., Coath, C. D., Karhu, J. A., & McKeegan, K. D. (2005) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2005.07.005 · Cited by 82
“30‰ (Farquhar et al., 2000; Hu et al., 2003; Mojzsis et al., 2003; Ono et al., 2003), which stands in contrast with almost all sulfides and sulfates younger than 2.”
BackgroundRoerdink, D. L., Mason, P. R. D., Farquhar, J. D., & Reimer, T. (2012) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2012.03.020 · Cited by 80
Atmospherically-derived mass-independent sulfur isotope signatures, and incorporation into sediments
Lyons, J. R. (2009) · Chemical Geology · doi:10.1016/j.chemgeo.2009.03.027 · Cited by 77
LaFlamme, C. K., Jamieson, J. W., Fiorentini, M. L., Thébaud, N., Caruso, S., & Selvaraja, V. (2018) · Gondwana Research · doi:10.1016/j.gr.2018.02.005 · Cited by 78
The Geologic History of Seawater
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Czaja, A. D., Johnson, C. M., Beard, B. L., Eigenbrode, J. L., Freeman, K. H., & Yamaguchi, K. E. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.01.032 · Cited by 76
“…of excess sulfate (Partridge et al., 2008), which suggests relatively high levels of O2 in at least the upper water column, consistent with temporal S isotope (Bottomley et al., 1992; Yamaguchi, 2002; Ono et al., 2003; Kaufman et al., 2007) and N isotope (Godfrey and Falkowski, 2009) trends.”
BackgroundInfluentialSelf-citationThe Great Oxidation Event Transition
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Self-citationAvailability of O 2 and H 2 O 2 on Pre-Photosynthetic Earth
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“SO2 outgassing was fixed at 3.5 108 cm 2 s 1, or *9.4 1010 mol/yr, following Ono et al. (2003).”
BackgroundInfluentialSelf-citationTransient surface ocean oxygenation recorded in the ∼2.66-Ga Jeerinah Formation, Australia
Koehler, M. C., Buick, R., Kipp, M. A., Stüeken, E. E., & Zaloumis, J. (2018) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1720820115 · Cited by 72
“S1) and ∼128 m of predominantly black shales from the Jeerinah Formation that were sampled at 1-m resolution.”
BackgroundInfluentialProtracted oxygenation of the Proterozoic biosphere
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“Combined with a growing inventory of chemical data suggesting that locally oxygenated environments may have occurred nearly 200 million years prior to the GOE (Ono et al. 2003; Anbar et al. 2007; Kaufman et al. 2007; Frei et al. 2009; Reinhard et al. 2009), our view of the GOE changes dramatically.”
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“, 2003) suggests either no homogenization or only localized homogenization (Ono et al., 2003).”
BackgroundInfluentialWilliford, K. H., Ushikubo, T., Lepot, K., Kitajima, K., Hallmann, C., Spicuzza, M. J., Kozdon, R., Eigenbrode, J. L., Summons, R. E., & Valley, J. W. (2015) · Geobiology · doi:10.1111/gbi.12163 · Cited by 69
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“5 Ga Western Australia (9, 13, 35, 36, 39), filled yellow circles; 2.”
BackgroundInfluentialSyverson, D. D., Ono, S., Shanks, W. C., & Seyfried, W. E. (2015) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2015.06.022 · Cited by 65
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Buhn, B. M., Santos, R. V., Dardenne, M. A., & de Oliveira, C. G. (2012) · Chemical Geology · doi:10.1016/j.chemgeo.2012.04.003 · Cited by 63
Gregory, D. D., Large, R., Halpin, J., Steadman, J., Hickman, A., Ireland, T., & Holden, P. (2015) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2014.10.023 · Cited by 62
Ding, X., Ripley, E. M., Shirey, S. B., & Li, C. (2012) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2012.04.029 · Cited by 63
Tectonic controls on atmospheric, climatic, and biological evolution 3.5–2.4Ga
Lowe, D. R., & Tice, M. M. (2007) · Precambrian Research · doi:10.1016/j.precamres.2007.04.008 · Cited by 65
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Oxidative sulfide dissolution on the early Earth
Reinhard, C. T., Lalonde, S. V., & Lyons, T. W. (2013) · Chemical Geology · doi:10.1016/j.chemgeo.2013.10.006 · Cited by 60
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Anaerobic methanotrophy and the rise of atmospheric oxygen
Catling, D. C., Claire, M. W., & Zahnle, K. J. (2007) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2007.2047 · Cited by 57
“Models show that both low levels of oxygen and a sufficiently high abundance of methane are required for insoluble S8 to be a significant photochemical product of the ancient anoxic atmosphere (Ono et al. 2003; Zahnle et al. 2006).”
BackgroundOrganic sulfur was integral to the Archean sulfur cycle
Fakhraee, M., & Katsev, S. (2019) · Nature Communications · doi:10.1038/s41467-019-12396-y · Cited by 62
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High-precision analysis of multiple sulfur isotopes using NanoSIMS
Hauri, E. H., Papineau, D., Wang, J., & Hillion, F. (2015) · Chemical Geology · doi:10.1016/j.chemgeo.2015.11.013 · Cited by 56
Geologic and Geochemical Constraints on Earth's Early Atmosphere
Farquhar, J., Zerkle, A. L., & Bekker, A. (2014) · Treatise on Geochemistry · doi:10.1016/b978-0-08-095975-7.01304-8 · Cited by 53
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Co-evolution of primitive methane-cycling ecosystems and early Earth’s atmosphere and climate
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Cabral, A. R., Creaser, R. A., Nägler, T. F., Lehmann, B., Voegelin, A. R., Belyatsky, B. V., Pašava, J., Gomes, A. A. S., Galbiatti, H. F., Böttcher, M. E., et al. (2013) · Chemical Geology · doi:10.1016/j.chemgeo.2013.08.041 · Cited by 52
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“2554 anomaly of most Archean sedimentary rocks is characterized by Δ33S/δ34S~1 and Δ36S/Δ33S~ 0.9 [Farquhar et al., 2000; Ono et al., 2003] (solid grey line in Figures 8a and 8b, respectively).”
BackgroundInfluentialEvidence for pervasive petroleum generation and migration in 3.2 and 2.63 Ga shales
Rasmussen, B. (2005) · Geology · doi:10.1130/g21316.1 · Cited by 49
An ab initio study of the low-lying electronic states of S3
Peterson, K. A., Lyons, J. R., & Francisco, J. S. (2006) · The Journal of Chemical Physics · doi:10.1063/1.2222367 · Cited by 50
Thomazo, C., Nisbet, E. G., Grassineau, N. V., Peters, M., & Strauss, H. (2013) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2013.06.036 · Cited by 49
“Methanotrophs oxidize methane utilizing a wide variety of oxidants (oxygen, nitrate, sulfate, and Mn–Fe oxides) and methanotrophy in the Archean did not involve significant quantities of free oxygen as evidenced by the presence of sizeable MIF-S in this study and elsewhere (Ono et al., 2003; Kaufman et al., 2007; Thom…”
BackgroundHazen, R. M., Downs, R. T., Kah, L. C., & Sverjensky, D. A. (2013) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2013.75.4 · Cited by 51
“…in the 2.5 Ga Pronto paleosols (Murakami et al. 2001); (3) the absence of Fe3+ hydroxides in paleosols older than 2.3 Ga (Rye et al. 1995; Holland and Rye 1997); and (4) mass-independent fractionation of sulfur isotopes (e.g., Farquhar et al. 2000, 2007; Ono et al. 2003; Papineau et al. 2007).”
BackgroundInfluentialWacey, D., Noffke, N., Cliff, J., Barley, M., & Farquhar, J. D. (2014) · Precambrian Research · doi:10.1016/j.precamres.2014.12.012 · Cited by 48
“of MIF signatures from the atmosphere to the surface (Pavlov and Kasting, 2002; Ono et al., 2003; Halevy et al., 2010).”
BackgroundRoerdink, D. L., Mason, P. R. D., Whitehouse, M. J., & Brouwer, F. M. (2016) · Precambrian Research · doi:10.1016/j.precamres.2016.05.007 · Cited by 50
“1.0 (Farquhar et al., 2000) and D 33 S/ d 34 S = 0.90 (Ono et al., 2003).”
InfluentialMurakami, T., Sreenivas, B., Sharma, S. D., & Sugimori, H. (2011) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2011.04.023 · Cited by 49
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False Negatives for Remote Life Detection on Ocean-Bearing Planets: Lessons from the Early Earth.
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Multiple-sulfur isotope effects during photolysis of carbonyl sulfide
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Self-citationSedimentary sulfur isotopes and Neoarchean ocean oxygenation
Fakhraee, M., Crowe, S. A., & Katsev, S. (2018) · Science Advances · doi:10.1126/sciadv.1701835 · Cited by 44
“Seawater sulfate was assumed to carry no MIF signal (D(33)SSO4 = 0) in benchmark simulations, but the model was also run for an alternative set of values (D(33)SSO4 = −7‰) (9).”
BackgroundHarman, C. E., Pavlov, A. A., Babikov, D., & Kasting, J. F. (2018) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2018.05.041 · Cited by 44
Self-citationOxygen and sulfur isotope fractionation during sulfide oxidation by anoxygenic phototrophic bacteria
Brabec, M. Y., Lyons, T. W., & Mandernack, K. W. (2011) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2011.12.008 · Cited by 44
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“4 Ga) sedimentary and diagenetic sulfur minerals (sulfides and sulfates; Ono et al., 2003).”
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Elemental sulfur aerosol-forming mechanism
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Multiple-Sulphur Isotope Biosignatures
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Self-citationPapineau, D., & Mojzsis, S. J. (2006) · Geobiology · doi:10.1111/j.1472-4669.2006.00083.x · Cited by 41
Earliest Seafloor Hydrothermal Systems on Earth: Comparison with Modern Analogues
Golding, S. D., Duck, L. J., Young, E., Baublys, K. A., Glikson, M., & Kamber, B. S. (2010) · Springer eBooks · doi:10.1007/978-90-481-8794-2_2 · Cited by 40
“6a) at odds with compositions expected to result from atmospheric photolysis of volcanic gases with 193-nm UV radiation, which may reflect different atmospheric conditions (Farquhar and Wing 2003; Ono et al. 2003; Bao et al. 2007).”
BackgroundInfluentialFehr, M. A., Rehkämper, M., Halliday, A. N., Wiechert, U., Hattendorf, B., Günther, D., Ono, S., Eigenbrode, J. L., & Rumble, D., III (2005) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2005.04.020 · Cited by 39
Self-citationIzon, G., Luo, G., Uveges, B. T. I., Beukes, N. J., Kitajima, K., Ono, S., Valley, J. W., Ma, X., & Summons, R. E. (2022) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.2025606119 · Cited by 39
“S1, S4, S7 and S9), and, those that do, are separated from the Rooihoogte Formation by hundreds of kilometers and some 200 million years (24, 41).”
BackgroundSelf-citationReconciling discrepant minor sulfur isotope records of the Great Oxidation Event
Uveges, B. T. I., Izon, G., Ono, S., Beukes, N. J., & Summons, R. E. (2023) · Nature Communications · doi:10.1038/s41467-023-35820-w · Cited by 40
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“Ono et al. (2003) also predicted a SO 2 pressure dependence on the S 8 / H 2 SO 4 ratio, which they attributed to the increased S atom requirement to form S 8 over H 2 SO 4 .”
InfluentialVelivetskaya, T. A., Ignatiev, A. V., Yakovenko, V. V., & Vysotskiy, S. V. (2019) · Rapid Communications in Mass Spectrometry · doi:10.1002/rcm.8528 · Cited by 39
Mission to Planet Earth: The First Two Billion Years
Stüeken, E. E., Som, S. M., Claire, M. W., Rugheimer, S., Scherf, M., Sproß, L., Tosi, N., Ueno, Y., & Lammer, H. (2020) · Space Science Reviews · doi:10.1007/s11214-020-00652-3 · Cited by 39
Rodriguez, M. G., Hagemann, S. G., LaFlamme, C. K., & Fiorentini, M. L. (2018) · Mineralium Deposita · doi:10.1007/s00126-018-0828-y · Cited by 36
Montinaro, A., Strauß, H., Mason, P. R. D., Roerdink, D. L., Münker, C., Schwarz‐Schampera, U., Arndt, N., Farquhar, J. D., Beukes, N. J., Gutzmer, J., et al. (2015) · Precambrian Research · doi:10.1016/j.precamres.2015.06.008 · Cited by 37
“Conclusions based solely on the ı 34 S record include (i) an unfractionated sulfur isotope signature in magmatic rocks (Clark and Fritz, 1997; Ono et al., 2003; Seal, 2006), (ii) slightly positive ı 34 S values in hydrothermal precipitates reflecting a mixture between an unfractionated juvenile…”
Mishima, K., Yamazaki, R., Satish-Kumar, M., Ueno, Y., Hokada, T., & Toyoshima, T. (2017) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2017.02.007 · Cited by 35
Muller, É., Philippot, P., Rollion‐Bard, C., Cartigny, P., Assayag, N., Marin‐Carbonne, J., Mohan, M. R., & Sarma, D. S. (2017) · Precambrian Research · doi:10.1016/j.precamres.2017.04.029 · Cited by 35
Volcanically modulated pyrite burial and ocean–atmosphere oxidation
Olson, S. L., Ostrander, C. M., Gregory, D. D., Roy, M., Anbar, A. D., & Lyons, T. W. (2018) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2018.11.015 · Cited by 34
Young, S. A., Loukola-Ruskeeniemi, K., & Pratt, L. M. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.02.004 · Cited by 35
Anomalous sulfur isotopes trace volatile pathways in magmatic arcs
Selvaraja, V., Fiorentini, M. L., LaFlamme, C. K., Wing, B. A., & Bui, T.-H. (2017) · Geology · doi:10.1130/g38853.1 · Cited by 35
Hiebert, R. S., Bekker, A., Houlé, M. G., Wing, B. A., & Rouxel, O. J. (2016) · Mineralium Deposita · doi:10.1007/s00126-016-0644-1 · Cited by 34
“…by sulfate-reducing bacteria that resulted in a horizontal shift in seawater sulfate composition (red oval) to higher δ34S values (fields are after Ono et al. 2003) Significance of negative δ56Fe values in exhalite and graphitic argillite Negative, and highly variable, δ56Fe values are…”
BackgroundResultGalić, A., Mason, P. R. D., Mogollón, J. M., Wolthers, M., Vroon, P. Z., & Whitehouse, M. J. (2016) · Chemical Geology · doi:10.1016/j.chemgeo.2016.12.006 · Cited by 33
Provenance and Geochemical Variations in Shales of the Mesoarchean Witwatersrand Supergroup
Nwaila, G. T., Frimmel, H. E., & Minter, W. E. L. (2017) · The Journal of Geology · doi:10.1086/692329 · Cited by 33
Proterozoic Atmospheric Oxygen
Canfield, D. E. (2014) · Treatise on Geochemistry · doi:10.1016/b978-0-08-095975-7.01308-5 · Cited by 32
Glombitza, C., Putman, L. I., Rempfert, K. R., Kubo, M. D. Y., Schrenk, M. O., Templeton, A. S., & Hoehler, T. M. (2021) · Communications Earth & Environment · doi:10.1038/s43247-021-00157-z · Cited by 30
Kresse, C., Lobato, L. M., Hagemann, S. G., & Silva, R. C. F. E. (2018) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2018.05.012 · Cited by 28
Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation
LaFlamme, C. K., Fiorentini, M. L., Lindsay, M., & Bui, T. H. (2018) · Nature Communications · doi:10.1038/s41467-018-06691-3 · Cited by 30
Abundance, Notation, and Fractionation of Light Stable Isotopes
Criss, R. E., & Farquhar, J. (2008) · Reviews in Mineralogy and Geochemistry · doi:10.2138/rmg.2008.68.3 · Cited by 29
Coupled-cluster study of the electronic structure and energetics of tetrasulfur, S4
Matus, M. H., Dixon, D. A., Peterson, K. A., Harkless, J. A. W., & Francisco, J. S. (2007) · The Journal of Chemical Physics · doi:10.1063/1.2774973 · Cited by 29
Biogeochemical cycles of sulfur and nitrogen in the Archean ocean and atmosphere
Shen, Y., Pinti, D. L., & HASHIZUME, K. (2006) · Geophysical monograph · doi:10.1029/164gm19 · Cited by 27
“Recent isotopic measurements of the stable isotopes δ33S and δ36S from Precambrian sulfides and sulfates show anomalous massindependent fractionation signature [Farquhar et al., 2000; Bekker et al., 2004; Ono et al., 2003; Mojzsis et al., 2003].”
BackgroundLyons, J. R. (2008) · Advances in quantum chemistry · doi:10.1016/s0065-3276(07)00205-5 · Cited by 28
Kinetics of Decomposition of Thiocyanate in Natural Aquatic Systems
Kurashova, I., Halevy, I., & Kamyshny, A. (2017) · Environmental Science & Technology · doi:10.1021/acs.est.7b04723 · Cited by 28
Saitoh, M., Ueno, Y., Matsu’ura, F., Kawamura, T., Isozaki, Y., Yao, J., Ji, Z., & Yoshida, N. (2016) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2016.12.009 · Cited by 26
“Coupled with photochemical experiments, this method has shed light on the characteristic sulfur cycle in the Archean atmosphere (e.g., Ono et al., 2003; Ueno et al., 2008, 2009, 2015).”
MethodCaruso, S., Fiorentini, M. L., Champion, D. C., Lu, Y., Ueno, Y., & Smithies, R. H. (2022) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2022.03.023 · Cited by 26
Sulphur cycling in a Neoarchaean microbial mat
Meyer, N. R., Zerkle, A. L., & Fike, D. A. (2017) · Geobiology · doi:10.1111/gbi.12227 · Cited by 25
“They correlated different pyrite phases with the Archaean reference array (Ono et al., 2003) and suggested nodular and layered pyrite had S- isotope signatures most consistent with MSR.”
MethodInfluentialSchwarzenbach, E. M., Gill, B. C., & Johnston, D. T. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2017.12.006 · Cited by 25
Guy, B. M., Ono, S., Gutzmer, J., Lin, Y., & Beukes, N. J. (2014) · Mineralium Deposita · doi:10.1007/s00126-014-0518-3 · Cited by 26
“The relatively large negative δ34S values (down to −6.2‰) and small negative Δ33S anomalies (∼−0.4‰) are indicative of microbial sulfate reduction (Ono et al. 2003; Farquhar et al. 2013), and probably reflect elevated concentrations of sulfate in fluvial channels, ephemeral ponds and interchannel…”
BackgroundInfluentialSelf-citation
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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