New insights into Archean sulfur cycle from mass-independent sulfur isotope records from the Hamersley Basin, Australia
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Pyrite in the S-MIF interval carries distinct S-MIF signals, with Δ33S reaching as high as +8‰ and Δ36S/Δ33S ratios centering around −0.98, characteristic of the Neoarchean array.
“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]
The Δ36S/Δ33S slope of −0.9 is widespread in Neoarchean sedimentary rocks and interpreted to be of atmospheric origin.
“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]
For simplicity, the model did not explicitly model different kinetics for different forms of sulfur that are likely present in the Archean oceans.
“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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“Recent multiple-sulfur isotope studies have been fueled by a discovery of anomalous S and S abundances in Archean sulfate and sulfide minerals that reflect unique atmospheric sulfur chemistry in an early anoxic atmosphere (Farquhar et al., 2000a; Ono et al., 2003; Mojzsis et al., 2003).”
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“Past studies of non-mass dependent and mass dependent sulfur isotope records of sedimentary pyrite have placed important constraints on the biogeochemical cycle of sulfur and the evolution of ocean chemistry during the rise in atmospheric oxygen (Cameron 1982; Farquhar et al. 2000, 2007; Mojzsis et al. 2003; Ono et al…”
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ResultSelf-citationSulfate was a trace constituent of Archean seawater
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“…also has a long heritage of being used to study photochemistry in nonhazy atmospheres ( e.g. , Kasting and Donahue, 1980; Pavlov and Kasting, 2002; Ono et al. , 2003; Segura et al. , 2003, 2005, 2007, 2010; Zahnle et al. , 2006; Grenfell et al. , 2007; Catling et al. , 2010; Domagal-Goldman et…”
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“Ono et al. (2003) consider 3.5 × 108, 1 × 109, and 3.5 × 109 cm−2 s−1 for their low, medium and high volcanic fluxes, respectively.”
BackgroundResultInfluentialA Late Archean Sulfidic Sea Stimulated by Early Oxidative Weathering of the Continents
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“3A), which is in agreement with previous multiple sulfur isotope studies of Neoarchean successions (Kaufman et al., 2007; Ono et al., 2003), as well as the products of ultraviolet (UV) photolysis experiments with SO 2 in the absence of oxygen (Farquhar and Wing, 2003).”
Spectral Evolution of an Earth‐like Planet
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Late Archean rise of aerobic microbial ecosystems
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Self-citationSulphur isotope evidence for an oxic Archaean atmosphere
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Self-citationA 200-million-year delay in permanent atmospheric oxygenation
Poulton, S. W., Bekker, A., Cumming, V. M., Zerkle, A. L., Canfield, D. E., & Johnston, D. T. (2021) · Nature · doi:10.1038/s41586-021-03393-7 · Cited by 243 · see citing works
A bistable organic-rich atmosphere on the Neoarchaean Earth
Zerkle, A. L., Claire, M. W., Domagal-Goldman, S. D., Farquhar, J., & Poulton, S. W. (2012) · Nature Geoscience · doi:10.1038/ngeo1425 · Cited by 239 · see citing works
““Ono et al., 2003”, (in blue) refers to the proposed explanation for the Archean reference line 14 .”
Geological constraints on the origin of oxygenic photosynthesis
Farquhar, J., Zerkle, A. L., & Bekker, A. (2011) · Photosynthesis Research · doi:10.1007/s11120-010-9594-0 · Cited by 223 · see citing works
“The threshold for the opening of this pathway was constrained to be approximately 10 PAL (10 bar) (Pavlov and Kasting 2002), but is sensitive to the concentration of atmospheric sulfur (Ono et al. 2003) 24 Photosynth Res (2011) 107:11–36”
BackgroundInfluentialS-33 constraints on the seawater sulfate contribution in modern seafloor hydrothermal vent sulfides
Ono, S., Shanks, W. C., Rouxel, O. J., & Rumble, D., III (2006) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2006.11.017 · Cited by 226 · see citing works
“Ono et al.(2007) GCA 71, 1170-1182 S-33 constraints on the hydrothermal vent sulfides”
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Stolper, D., Revsbech, N., & Canfield, D. (2010) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1013435107 · Cited by 185 · see citing works
Farquhar, J., Wu, N., Canfield, D. E., & Oduro, H. (2010) · Economic Geology · doi:10.2113/gsecongeo.105.3.509 · Cited by 212 · see citing works
Biogeochemical modelling of the rise in atmospheric oxygen
CLAIRE, M. W., CATLING, D. C., & ZAHNLE, K. J. (2006) · Geobiology · doi:10.1111/j.1472-4669.2006.00084.x · Cited by 200 · see citing works
“Analyses that show the presence of massindependent fractionation (MIF) of sulfur isotopes in Archean rocks (Farquhar et al., 2000; Farquhar & Wing, 2003; Ono et al., 2003; Zahnle et al., 2006) provide to many observers convincing evidence that the Archean atmosphere was globally weakly reducing.”
BackgroundOrganic haze, glaciations and multiple sulfur isotopes in the Mid-Archean Era
Domagal-Goldman, S. D., Kasting, J. F., Johnston, D. T., & Farquhar, J. (2008) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2008.01.040 · Cited by 204 · see citing works
Self-citationShen, Y., Farquhar, J. D., Masterson, A. L., Kaufman, A. J., & Buick, R. (2009) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2009.01.018 · Cited by 205 · see citing works
“…and rd. Plotted here are data for North Pole sulfate analyzed here (black filled circular symbols), s (black unfilled symbols), Mesoarchean samples (grey unfilled squares), Neoarchean (grey et al. (2006), Ono et al. (2003), Mojzsis et al. (2003), Papineau et al. (2007), Kamber and al.”
BackgroundIron and carbon isotope evidence for microbial iron respiration throughout the Archean
Craddock, P. R., & Dauphas, N. (2011) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.12.045 · Cited by 196 · see citing works
“The primarymechanism for oxidation of Fe(II)aq in an Archean ocean that was purportedly anoxic (Canfield et al., 2000; Farquhar et al., 2000; Kasting, 1987; Ono et al., 2003; Pavlov and Kasting, 2002), is uncertain.”
BackgroundAn iron shuttle for deepwater silica in Late Archean and early Paleoproterozoic iron formation
Fischer, W. W., & Knoll, A. H. (2006) · Geological Society of America Bulletin · doi:10.1130/b26328.1 · Cited by 196 · see citing works
“…rock-based proxies suggest that very little if any O 2 was present in the atmosphere or oceans (atmospheric O 2 mixing ratio << 10 −5 ) (Rye and Holland, 1998; Rasmussen and Buick, 1999; Farquhar et al., 2000; Pavlov and Kasting, 2002; Ono et al., 2003; Bekker et al., 2004; Frimmel, 2005).”
BackgroundMethane and climate during the Precambrian era
KASTING, J. (2005) · Precambrian Research · doi:10.1016/j.precamres.2005.03.002 · Cited by 190 · see citing works
Self-citationSulfur isotope measurement of sulfate and sulfide by high-resolution MC-ICP-MS
Craddock, P. R., Rouxel, O. J., Ball, L. A., & Bach, W. (2008) · Chemical Geology · doi:10.1016/j.chemgeo.2008.04.017 · Cited by 191 · see citing works
“…fractionation of S isotopes in late Archean sedimentary sulfides (Jeerinah Formation; Table 4) is consistent with previous studies suggesting sulfate reduction at low sulfate concentrations (Canfield et al., 2000) due to low levels of atmospheric oxygen (Farquhar et al., 2000; Ono et al., 2003).”
BackgroundPalaeoproterozoic Supercontinents and Global Evolution
Reddy, S. M., Mazumder, R., Evans, D. A. D., & Collins, A. S. (2009) · Cited by 181 · see citing works
Mass-Independent Sulfur Isotopic Compositions in Stratospheric Volcanic Eruptions
Baroni, M., Thiemens, M. H., Delmas, R. J., & Savarino, J. (2007) · Science · doi:10.1126/science.1131754 · Cited by 178 · see citing works
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“Positive correlations between Δ(33)S anomalies and δ(34)S values recorded in pyrites have been interpreted to represent a photolytic signal, without further modification by other fractionation processes (45).”
Palaeoproterozoic supercontinents and global evolution: correlations from core to atmosphere
Reddy, S. M., & Evans, D. A. D. (2009) · Geological Society London Special Publications · doi:10.1144/sp323.1 · Cited by 167 · see citing works
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“…that substantial Mass Independent Fractionation (MIF) of sulfur isotopes is restricted to the time interval before ~2.3 Ga argues for an anoxic atmosphere at that time (Farquhar, 2000; Pavlov and Kasting, 2002; Mojzsis et al., 2003; Ono et al., 2003; Bekker et al., 2004; Farquhar et al., 2007).”
BackgroundInfluentialThe Great Oxidation Event preceded a Paleoproterozoic “snowball Earth”
Warke, M. R., Rocco, T. D., Zerkle, A. L., Lepland, A., Prave, A. R., Martin, A. P., Ueno, Y., Condon, D. J., & Claire, M. W. (2020) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.2003090117 · Cited by 161 · see citing works
Anomalous Fractionations of Sulfur Isotopes During Thermochemical Sulfate Reduction
Watanabe, Y., Farquhar, J. D., & Ohmoto, H. (2009) · Science · doi:10.1126/science.1169289 · Cited by 159 · see citing works
Hessler, A. M., & Lowe, D. R. (2006) · Precambrian Research · doi:10.1016/j.precamres.2006.08.008 · Cited by 153 · see citing works
Eigenbrode, J. L., Freeman, K. H., & Summons, R. E. (2008) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2008.06.037 · Cited by 150 · see citing works
Self-citationPathways for Neoarchean pyrite formation constrained by mass-independent sulfur isotopes
Farquhar, J. D., Cliff, J., Zerkle, A. L., Kamyshny, A., Poulton, S. W., Claire, M. W., Adams, D. T., & Harms, B. (2013) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1218851110 · Cited by 153 · see citing works
Evidence for Paleoproterozoic cap carbonates in North America
BEKKER, A., KAUFMAN, A., KARHU, J., & ERIKSSON, K. (2005) · Precambrian Research · doi:10.1016/j.precamres.2005.03.009 · Cited by 147 · see citing works
“, 2002, 2004), suggesting that immediately before the oldest Paleoproterozoic glaciation the atmosphere became more oxidizing than in the latest Neoarchean (Farquhar et al., 2000; Ono et al., 2003).”
Electrons, life and the evolution of Earth's oxygen cycle
Falkowski, P. G., & Godfrey, L. V. (2008) · Philosophical Transactions of the Royal Society B: Biological Sciences · doi:10.1098/rstb.2008.0054 · Cited by 144 · see citing works
“Data from Hayes et al. (1983), Sano & Pillinger (1990), Pinti & Hashizume (2001), Hu et al. (2003), Mosjzsis et al. (2003), Ono et al. (2003, 2006), Jia & Kerrich (2004), Bekker et al. (2004), Johnston et al. (2005), Papineau et al. (2005), Ohmoto et al. (2006) and Kaufman et al. (2007). passive…”
Palaeoclimates: The first two billion years
Kasting, J. F., & Ono, S. (2006) · Philosophical Transactions of the Royal Society B Biological Sciences · doi:10.1098/rstb.2006.1839 · Cited by 144 · see citing works
“5 to 8.2‰) for older rock formations (figure 6; Farquhar et al. 2000; Mojzsis et al. 2003; Ono et al. 2003).”
BackgroundInfluentialSelf-citationWhat caused the rise of atmospheric O2?
Kasting, J. F. (2013) · Chemical Geology · doi:10.1016/j.chemgeo.2013.05.039 · Cited by 144 · see citing works
“In particular, the idea that sulfur was less mobile, and therefore less available, in the Archean has been emphasized by many different authors (e.g., Walker and Brimblecombe, 1985; Ono et al., 2003; Canfield et al., 2006).”
BackgroundUeno, Y., Johnson, M. S., Danielache, S. O., Eskebjerg, C., Pandey, A., & Yoshida, N. (2009) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0903518106 · Cited by 144 · see citing works
“The predicted positive 33S of the sulfate is incompatible with the geological record suggesting Archean seawater sulfate would have had negative 33S values (1, 3, 7, 10).”
BackgroundInfluentialExplaining the Structure of the Archean Mass-Independent Sulfur Isotope Record
Halevy, I., Johnston, D. T., & Schrag, D. P. (2010) · Science · doi:10.1126/science.1190298 · Cited by 141 · see citing works
Contributions to late Archaean sulphur cycling by life on land
Stüeken, E. E., Catling, D. C., & Buick, R. (2012) · Nature Geoscience · doi:10.1038/ngeo1585 · Cited by 137 · see citing works
Did life originate from a global chemical reactor?
Stüeken, E. E., Anderson, R. E., Bowman, J. S., Brazelton, W. J., Colangelo-Lillis, J. R., Goldman, A. D., Som, S. M., & Baross, J. A. (2013) · Geobiology · doi:10.1111/gbi.12025 · Cited by 130 · see citing works
“For example, UV photolysis of volcanogenic SO2 and H2S is thought to have produced a mixture of SO2, H2S, S 0 and H2SO4 (Farquhar et al., 2001; Ono et al., 2003), which could have acted as important oxidation or reduction species for protometabolisms.”
BackgroundThe age of Rubisco: the evolution of oxygenic photosynthesis
Nisbet, E. G., Grassineau, N. V., Howe, C. J., Abell, P. I., Regelous, M., & Nisbet, R. E. R. (2007) · Geobiology · doi:10.1111/j.1472-4669.2007.00127.x · Cited by 128 · see citing works
“The bulk of the δ34S signal is likely to be from microbial processes (Ono et al., 2003; for discussion of older sulphur record see Ohmoto et al., 1993, 2001).”
BackgroundInfluentialHofmann, A., Bekker, A., Rouxel, O. J., Rumble, D., III, & Master, S. (2009) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2009.07.008 · Cited by 127 · see citing works
“Alternatively, the covariation in δ34S and Δ33S values could reflect a combination of mass-dependent and nonmass dependent isotope effects, as suggested by Ono et al. (2003), Ueno et al. (2008), and Shen et al. (2009).”
BackgroundMultiple sulfur isotopes monitor fluid evolution of an Archean orogenic gold deposit
LaFlamme, C. K., Sugiono, D., Thébaud, N., Caruso, S., Fiorentini, M. L., Selvaraja, V., Jeon, H., Voute, F., & Martin, L. A. J. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2017.11.003 · Cited by 127 · see citing works
Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event
Philippot, P., Ávila, J. N., Killingsworth, B. A., Tessalina, S. G., Baton, F., Caquineau, T., Muller, É., Ernesto Pecoits, A., Cartigny, P., Lalonde, S. V., et al. (2018) · Nature Communications · doi:10.1038/s41467-018-04621-x · Cited by 123 · see citing works
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Frontiers of stable isotope geoscience
Eiler, J. M., Bergquist, B., Bourg, I., Cartigny, P., Farquhar, J., Gagnon, A., Guo, W., Halevy, I., Hofmann, A., Larson, T. E., et al. (2014) · Chemical Geology · doi:10.1016/j.chemgeo.2014.02.006 · Cited by 121 · see citing works
“Earth's surface in H2SO4 and S8 aerosols as well as in the residual SO2 (e.g., Farquhar et al., 2000a, 2001; Pavlov and Kasting, 2002; Ono et al., 2003; Zahnle et al., 2006).”
BackgroundOno, S. (2017) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-060115-012324 · Cited by 119 · see citing works
Self-citationMicro‐scale sulphur isotope evidence for sulphur cycling in the late Archean shallow ocean
Kamber, B. S., & Whitehouse, M. J. (2006) · Geobiology · doi:10.1111/j.1472-4669.2006.00091.x · Cited by 120 · see citing works
“The most negative ∆33S of −2.5‰ reported to date is from c. 2.6 Gyr Carrawine Dolomite sulphides (Ono et al., 2003), implied to have formed from H2SO4-derived sulphate.”
BackgroundInfluentialTrace Element Content of Pyrite from the Kapai Slate, St. Ives Gold District, Western Australia
Gregory, D. D., Large, R. R., Bath, A. B., Steadman, J. A., Wu, S., Danyushevsky, L. V., Bull, S. W., Holden, P. N., & Ireland, T. R. (2016) · Economic Geology · doi:10.2113/econgeo.111.6.1297 · Cited by 119 · see citing works
A Chronostratigraphic Division of the Precambrian
Kranendonk, M. J. V., Contributors, Altermann, W., Beard, B. L., Hoffman, P. F., Johnson, C. M., Kasting, J. F., Melezhik, V. A., Nutman, A. P., Papineau, D., et al. (2012) · Elsevier eBooks · doi:10.1016/b978-0-444-59425-9.00016-0 · Cited by 120 · see citing works
Self-citationHoffman, P. F. (2013) · Chemical Geology · doi:10.1016/j.chemgeo.2013.04.018 · Cited by 116 · see citing works
The Pale Orange Dot: The Spectrum and Habitability of Hazy Archean Earth
Arney, G., Domagal-Goldman, S. D., Meadows, V., Wolf, E. T., Schwieterman, E. W., Charnay, B., Claire, M. W., Hébrard, É., & Trainer, M. G. (2025) · Figshare · Cited by 117 · see citing works
Evolution of the oceanic sulfur cycle at the end of the Paleoproterozoic
Johnston, D. T., Poulton, S. W., Fralick, P. W., Wing, B. A., Canfield, D. E., & Farquhar, J. D. (2006) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2006.08.001 · Cited by 115 · see citing works
Thomazo, C., Pinti, D. L., Busigny, V., Ader, M., HASHIZUME, K., & Philippot, P. (2009) · Comptes Rendus Palevol · doi:10.1016/j.crpv.2009.02.003 · Cited by 116 · see citing works
Long-term sedimentary recycling of rare sulphur isotope anomalies
Reinhard, C. T., Planavsky, N. J., & Lyons, T. W. (2013) · Nature · doi:10.1038/nature12021 · Cited by 113 · see citing works
“Parameter values for the reference case were chosen to approximately satisfy known constraints on: (1) the overall size of the crustal sulphur reservoir(53,81,99,100); (2) the residence time of sulphur as it cycles through the exogenic system(87,101); (3) the fraction of overall sulphur input derived from the rapidly…”
Coupled Fe and S isotope variations in pyrite nodules from Archean shale
Marin‐Carbonne, J., Rollion‐Bard, C., Bekker, A., Rouxel, O. J., Agangi, A., Cavalazzi, B., Wohlgemuth‐Ueberwasser, C. C., Hofmann, A., & McKeegan, K. D. (2014) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2014.02.009 · Cited by 112 · see citing works
“Elemental sulfur is highly insoluble and less amenable to biological processes; as a result, most of it is transferred to sediments as solid S (Ono et al., 2003).”
BackgroundModeling the signature of sulfur mass-independent fractionation produced in the Archean atmosphere
Claire, M. W., Kasting, J. F., Domagal-Goldman, S. D., Stüeken, E. E., Buick, R., & Meadows, V. S. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2014.06.032 · Cited by 108 · see citing works
“Compared to models without a photosynthetic O2 source (Pavlov and Kasting, 2002; Ono et al., 2003), SO2 is also a quantitatively significant exit channel, with positive D33S in SO2 delivered to the surface by a combination of wet and dry deposition.”
BackgroundMethodResultInfluentialSelf-citationReactive Oxygen Species: Radical Factors in the Evolution of Animal Life
Taverne, Y. J. H. J., Merkus, D., Bogers, A. J. J. C., Halliwell, B. B., Duncker, D. J., & Lyons, T. W. (2018) · BioEssays · doi:10.1002/bies.201700158 · Cited by 110 · see citing works
Sulfur cycling at the Mid-Atlantic Ridge: A multiple sulfur isotope approach
Peters, M., Strauß, H., Farquhar, J. D., Ockert, C., Eickmann, B., & Jost, C. L. (2009) · Chemical Geology · doi:10.1016/j.chemgeo.2009.09.016 · Cited by 112 · see citing works
Holland, H. D. (2005) · Economic Geology · doi:10.2113/gsecongeo.100.8.1489 · Cited by 110 · see citing works
Whitehouse, M. J. (2012) · Geostandards and Geoanalytical Research · doi:10.1111/j.1751-908x.2012.00188.x · Cited by 112 · see citing works
“The development of an oxygenated atmosphere in the Palaeoproterozoic at ca. 2.3 Ga effectively shut down the mass-independent fractionation process (Farquhar and Wing 2003), but the signature provides an important tracer of the evolution and distribution of early sulfur reservoirs (Ono et al. 2003).”
BackgroundInfluentialOno, S., Beukes, N. J., & Rumble, D., III (2008) · Precambrian Research · doi:10.1016/j.precamres.2008.10.012 · Cited by 108 · see citing works
Self-citationOno, S., Whitehill, A. R., & Lyons, J. R. (2013) · Journal of Geophysical Research Atmospheres · doi:10.1002/jgrd.50183 · Cited by 103 · see citing works
“…older than 2.4 Giga years ago (Ga) commonly show signatures of sulfur isotope mass-independent fractionation (S-MIF), anomalous isotope compositions that deviate from the mass-dependent scaling law of isotope fractionation [e.g., Farquhar et al., 2000a; Pavlov and Kasting, 2002; Ono et al., 2003].”
BackgroundInfluentialEarth's atmosphere – Hadean to early Proterozoic
Shaw, G. H. (2008) · Geochemistry · doi:10.1016/j.chemer.2008.05.001 · Cited by 83 · see citing works
Variations in atmospheric sulphur chemistry on early Earth linked to volcanic activity
Philippot, P., van Zuilen, M. A., & Rollion‐Bard, C. (2012) · Nature Geoscience · doi:10.1038/ngeo1534 · Cited by 108 · see citing works
Two coexisting sulfur metabolisms in a ca. 3400 Ma sandstone
Wacey, D., McLoughlin, N., Whitehouse, M. J., & Kilburn, M. R. (2010) · Geology · doi:10.1130/g31329.1 · Cited by 104 · see citing works
Ono, S. (2006) · South African Journal of Geology · doi:10.2113/gssajg.109.1-2.97 · Cited by 104 · see citing works
Self-citationEarth's First Redox Revolution
Ostrander, C. M., Johnson, A. C., & Anbar, A. D. (2021) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-072020-055249 · Cited by 101 · see citing works
Multiple oscillations in Neoarchaean atmospheric chemistry
Izon, G., Zerkle, A. L., Zhelezinskaia, I., Farquhar, J., Newton, R. J., Poulton, S. W., Eigenbrode, J. L., & Claire, M. W. (2015) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2015.09.018 · Cited by 99 · see citing works
“3A), closely approximating both the general Neoarchaean reference array (−0.90; Ono et al., 2003) and those reported from GKF01 (−0.96; Zerkle et al., 2012).”
BackgroundInfluentialSelf-citationWilliford, K. H., Kranendonk, M. J. V., Ushikubo, T., Kozdon, R., & Valley, J. W. (2011) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2011.07.010 · Cited by 108 · see citing works
Thomazo, C., Ader, M., Farquhar, J. D., & Philippot, P. (2009) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2008.12.036 · Cited by 99 · see citing works
Whitehill, A. R., Xie, C., Hu, X., Xie, D., Guo, H., & Ono, S. (2013) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1306979110 · Cited by 98 · see citing works
Self-citationTurnstiles and bifurcators: The disequilibrium converting engines that put metabolism on the road
Branscomb, E., & Russell, M. J. (2013) · Biochimica et Biophysica Acta (BBA) - Bioenergetics · doi:10.1016/j.bbabio.2012.10.003 · Cited by 105 · see citing works
Neoarchaean seawater sulphate concentrations from sulphur isotopes in massive sulphide ore
Jamieson, J. W., Wing, B. A., Farquhar, J. D., & Hannington, M. D. (2012) · Nature Geoscience · doi:10.1038/ngeo1647 · Cited by 100 · see citing works
Ono, S., Wing, B. A., Rumble, D., III, & Farquhar, J. D. (2005) · Chemical Geology · doi:10.1016/j.chemgeo.2005.08.005 · Cited by 97 · see citing works
Self-citationMass‐independent fractionation of sulfur isotopes by isotope‐selective photodissociation of SO2
Lyons, J. R. (2007) · Geophysical Research Letters · doi:10.1029/2007gl031031 · Cited by 96 · see citing works
“Comparing these values to the maximum D33S measured in pyrites, which are 8–10% [Ono et al., 2003; Kamber and Whitehouse, 2007], and neglecting dilution by non-MIF sulfate, suggests pSO2 10 ppb during generation of the largest S-MIF signatures, or about 100 times the present-day global SO2…”
BackgroundBao, H., Rumble, D., III, & Lowe, D. R. (2007) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2007.05.032 · Cited by 94 · see citing works
False Negatives for Remote Life Detection on Ocean-Bearing Planets: Lessons from the Early Earth
Reinhard, C. T., Olson, S. L., Schwieterman, E. W., & Lyons, T. W. (2017) · Astrobiology · doi:10.1089/ast.2016.1598 · Cited by 93 · see citing works
“When interpreted in the context of photochemical models (Pavlov and Kasting, 2002; Ono et al., 2003; Zahnle et al., 2006; Ueno et al., 2009), the presence of these isotopic anomalies implies a ground-level atmospheric pO2 value that was below 10 -5 times the present atmospheric level (PAL) and more likely below *10 PA…”
BackgroundJohnston, D. T., Farquhar, J. D., HABICHT, K. S., & Canfield, D. E. (2008) · Geobiology · doi:10.1111/j.1472-4669.2008.00171.x · Cited by 94 · see citing works
“Kaufman et al. (2007) used a framework presented in Ono et al. (2003) suggesting that the sulphur reaching sedimentary environments carried an atmospheric isotope signature of 33λMt.”
Method
- 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 › Geophysics › 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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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 ›
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