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Hydrothermal Fe fluxes during the Precambrian: Effect of low oceanic sulfate concentrations and low hydrostatic pressure on the composition of black smokers
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“Moreover, the elevated temperatures of water-rock reactions in the Archaean and the low concentration of marine sulfate (which affect the Eh of hydrothermal fluids, as well as limit near-vent precipitation of iron sulfides) suggest that dissolved Fe(II) in hydrothermal effluents may have been orders of magnitude greater than today (e.g., Kump and Seyfried, 2005).”
From Iron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history (2017) · cites this paper as Kump and Seyfried, 2005
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The rise of oxygen in Earth's early ocean and atmosphere
Lyons, T. W., Reinhard, C. T., & Planavsky, N. J. (2014) · Nature · doi:10.1038/nature13068 · Cited by 2,810
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“Neoproterozoic iron formations are interbedded with glacial deposits, but it is unlikely that Snowball Earth conditions alone led to their deposition (e.g., Kump and Seyfried, 2005).”
BackgroundFerruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
Canfield, D. E., Poulton, S. W., Knoll, A. H., Narbonne, G. M., Ross, G., Goldberg, T., & Strauss, H. (2008) · Science · doi:10.1126/science.1154499 · Cited by 789
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The Iron Biogeochemical Cycle Past and Present
Raiswell, R., & Canfield, D. E. (2012) · Geochemical Perspectives · doi:10.7185/geochempersp.1.1 · Cited by 756
“Lee Kump of Penn State has taken this idea further and has modelled the circumstances under which sulphide could have been released from the oceans to the atmosphere (Kump et al., 2005).”
BackgroundA Stratified Redox Model for the Ediacaran Ocean
Li, C., Love, G. D., Lyons, T. W., Fike, D. A., Sessions, A. L., & Chu, X. (2010) · Science · doi:10.1126/science.1182369 · Cited by 673
Serpentinization as a source of energy at the origin of life
RUSSELL, M. J., HALL, A. J., & MARTIN, W. (2010) · Geobiology · doi:10.1111/j.1472-4669.2010.00249.x · Cited by 527
“…oceanic spreading centers, thermostated just above 400 C by the thermodynamic properties of salt water, emitted micromolar concentrations of Fe, Zn, Mn, Co, Ni and Cu to the ocean (Jupp & Schultz, 2000; Douville et al., 2002; Kump & Seyfried, 2005; Zerkle et al., 2005; Konhauser et al., 2009).”
BackgroundIron formations: A global record of Neoarchaean to Palaeoproterozoic environmental history
Konhauser, K. O., Planavsky, N. J., Hardisty, D. S., Robbins, L. J., Warchola, T. J., Haugaard, R., Lalonde, S. V., Partin, C. A., Oonk, P. B. H., Tsikos, H., et al. (2017) · Earth-Science Reviews · doi:10.1016/j.earscirev.2017.06.012 · Cited by 537
“Furthermore, assuming that the iron was hydrothermally derived, there must have been a crash, potentially to Archaean levels, of the marine sulfate reservoir, which would have fostered iron-rich rather than sulfide-rich hydrothermal fluids (Kump and Seyfried, 2005).”
BackgroundInfluentialPlanavsky, N. J., Bekker, A., Rouxel, O. J., Kamber, B. S., Hofmann, A., Knudsen, A. C., & Lyons, T. W. (2010) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2010.07.021 · Cited by 522
Widespread iron-rich conditions in the mid-Proterozoic ocean
Planavsky, N. J., McGoldrick, P., Scott, C. T., Li, C., Reinhard, C. T., Kelly, A. E., Chu, X., Bekker, A., Love, G. D., & Lyons, T. W. (2011) · Nature · doi:10.1038/nature10327 · Cited by 505
Ernst, R. E., & Youbi, N. (2017) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2017.03.014 · Cited by 470
Canfield, D. E., Rosing, M. T., & Bjerrum, C. (2006) · Philosophical Transactions of the Royal Society B: Biological Sciences · doi:10.1098/rstb.2006.1906 · Cited by 417
“Kump & Seyfried (2005) have argued that because they were hotter, mid-ocean ridge systems on the early Earth would have risen higher into the oceans, venting at shallower depths than at present.”
BackgroundInfluentialSpatial variability in oceanic redox structure 1.8 billion years ago
Poulton, S. W., Fralick, P. W., & Canfield, D. E. (2010) · Nature Geoscience · doi:10.1038/ngeo889 · Cited by 406
“The data available at present are entirely consistent with euxinia being prevalent in shallower marine settings and becoming less widespread and persistent with time, although a gradual decrease in hydrothermal Fe inputs relative to S through the Proterozoi”
BackgroundIncreased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago
Kump, L. R., & Barley, M. E. (2007) · Nature · doi:10.1038/nature06058 · Cited by 403
Self-citationA palaeogeographic context for Neoproterozoic glaciation
Hoffman, P. F., & Li, Z. (2009) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2009.03.013 · Cited by 390
“Fe-rich waters would be possible if H2S production was low because 366 of diminished input of SO4 from the glaciated continents (Raiswell and Canfield, 1999) 367 and because of lowered S:Fe ratios in hydrothermal vent fluids due to the fall in 368 hydrostatic pressure resulting from glacioeustatic drawdown (Kump and S…”
BackgroundInfluentialAtmospheric oxygenation caused by a change in volcanic degassing pressure
Gaillard, F., Scaillet, B., & Arndt, N. (2011) · Nature · doi:10.1038/nature10460 · Cited by 353
Decoupling photochemical Fe(II) oxidation from shallow-water BIF deposition
Konhauser, K. O., Amskold, L., Lalonde, S. V., Posth, N. R., Kappler, A. A., & Anbar, A. D. (2007) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2007.03.026 · Cited by 303
“could then foster the release of highly reduced, Fe(II)-rich hydrothermal fluids [18] directly to the upper ocean (e.”
BackgroundA Late Archean Sulfidic Sea Stimulated by Early Oxidative Weathering of the Continents
Reinhard, C. T., Raiswell, R., Scott, C., Anbar, A. D., & Lyons, T. W. (2009) · Science · doi:10.1126/science.1176711 · Cited by 287
Anoxygenic photosynthesis modulated Proterozoic oxygen and sustained Earth's middle age
Johnston, D. T., Wolfe-Simon, F., Pearson, A., & Knoll, A. H. (2009) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0909248106 · Cited by 329
“2) and an increase in the proportional input of Fe to S into the ocean (53, 54).”
BackgroundIron Formations: Their Origins and Implications for Ancient Seawater Chemistry
Bekker, A., Planavsky, N. J., Krapež, B., Rasmussen, B., Hofmann, A., Slack, J. F., Rouxel, O. J., & Konhauser, K. O. (2013) · Elsevier eBooks · doi:10.1016/b978-0-08-095975-7.00719-1 · Cited by 292
A key role for green rust in the Precambrian oceans and the genesis of iron formations
Halevy, I., Alesker, M., Schuster, E. M., Popovitz‐Biro, R., & Feldman, Y. (2017) · Nature Geoscience · doi:10.1038/ngeo2878 · Cited by 254
Tosca, N. J., Guggenheim, S., & Pufahl, P. K. (2016) · Geological Society of America Bulletin · doi:10.1130/b31339.1 · Cited by 241
Neoproterozoic glaciation in the Earth System
Fairchild, I. J., & Kennedy, M. J. (2007) · Journal of the Geological Society · doi:10.1144/0016-76492006-191 · Cited by 244
“Kump & Seyfried (2005) showed that the Fe/S ratio of hydrothermal fluids increases at lower hydrostatic pressure and so could be influenced by low sea level during glaciation, implicating this, together with low oceanic sulphate, as a possible way of explaining the return of Banded Iron Formation…”
BackgroundThe Continuing Puzzle of the Great Oxidation Event
Sessions, A. L., Doughty, D. M., Welander, P. V., Summons, R. E., & Newman, D. K. (2009) · Current Biology · doi:10.1016/j.cub.2009.05.054 · Cited by 244
“Fluxes of reduced Fe and S from the mantle, mainly at volcanoes and midocean ridges, would also have been larger on the ancient Earth and presumably limited (or prevented) the accumulation of O2 [23–25].”
BackgroundDruschel, G. K., Emerson, D., Sutka, R. L., Suchecki, P., & Luther, G. W. (2008) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2008.04.035 · Cited by 225
The Origin and Nature of Life on Earth: The Emergence of the Fourth Geosphere
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Johnston, D. T., Poulton, S. W., Dehler, C., Porter, S., Husson, J., Canfield, D. E., & Knoll, A. H. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2009.11.059 · Cited by 216
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
“A further refinement of the declining volcanic flux model involves an enhanced Archean flux of both H2 and hydrothermal cations (Fe2+) venting from mid-ocean ridges (Kump & Seyfried, 2005).”
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
“The ultimate source of Fe is commonly linked to increased regional or global, seafl oor basaltic volcanism (e.g., Isley, 1995; Barley et al., 1997; Isley and Abbott, 1999; Barley et al., 2005), or changes in the composition of midocean-ridge hydrothermal systems (Kump and Seyfried, 2005).”
BackgroundSpatio-temporal distribution and tectonic settings of the major iron deposits in China: An overview
Zhang, Z., Hou, T., Santosh, M., Li, H., Li, J., Zhang, Z., Song, X., & Wang, M. (2013) · Ore Geology Reviews · doi:10.1016/j.oregeorev.2013.08.021 · Cited by 190
“The oxygenation of the atmosphere and the development of sufidic deep ocean by 1.8 Ga ago led to the cessation of BIF deposition (e.g., Canfield, 1998; Fairchild and Kennedy, 2007; Kump and Seyfried, 2005).”
BackgroundInfluentialCox, G. M., Halverson, G. P., Minarik, W. G., Heron, D. P. L., Macdonald, F. A., Bellefroid, E. J., & Strauss, J. V. (2013) · Chemical Geology · doi:10.1016/j.chemgeo.2013.08.002 · Cited by 187
“Kump and Seyfried (2005) showed that lower sulfate levels haa considerable affect on the Fe concentration of hydrothermal fluids which become fayalite-pyrrohhotite-magnetite buffered rather than anhydrite-magnetite buffered, with a resulting increase in the concentration of Fe in…”
BackgroundBasta, F. F., Maurice, A. E., Fontboté, L., & Favarger, P. ‐. (2011) · Precambrian Research · doi:10.1016/j.precamres.2011.03.011 · Cited by 183
Signatures of early microbial life from the Archean (4 to 2.5 Ga) eon
Lepot, K. (2020) · Earth-Science Reviews · doi:10.1016/j.earscirev.2020.103296 · Cited by 189
“In particular, Fe 2+ was fed into seawater by hydrothermal vents and basaltic eruptions, and probably more so than H 2 S (Foriel et al., 2004; Kump and Seyfried, 2005), so that ferruginous water likely dominated the Archean (Fig.”
On the coevolution of Ediacaran oceans and animals
Shen, Y., Zhang, T., & Hoffman, P. F. (2008) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0802168105 · Cited by 170
“Conclusions Low oceanic sulfate concentrations during the Proterozoic have been documented by S-isotopic records of pyrite (50–52, 60, 61), trace sulfate (69–72), calculations of the Proterozoic hydrothermal fluid compositions (73), and measurements of multiple S-isotopes on trace sulfate in Proterozoic carbonate (74).”
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Biomass recycling and Earth’s early phosphorus cycle
Kipp, M. A., & Stüeken, E. E. (2017) · Science Advances · doi:10.1126/sciadv.aao4795 · Cited by 157
Fe isotope and trace element geochemistry of the Neoproterozoic syn-glacial Rapitan iron formation
Halverson, G. P., Poitrasson, F., Hoffman, P. F., Nédélec, A., Montel, J.-M., & Kirby, J. K. (2011) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2011.06.021 · Cited by 159
“Iron accumulation may have been enhanced by increased iron concentrations in hydrothermal fluids due to low seawater sulfate concentrations and glacioeustatic depressurization of midocean ridges (Kump and Seyfried, 2005).”
On the antiquity of metalloenzymes and their substrates in bioenergetics
Nitschke, W., McGlynn, S. E., Milner-White, E. J., & Russell, M. J. (2013) · Biochimica et Biophysica Acta (BBA) - Bioenergetics · doi:10.1016/j.bbabio.2013.02.008 · Cited by 152
“derived from magmatically driven hot acidic springs at ~400 °C [61,65,79,87].”
BackgroundCauses and consequences of mid-Proterozoic anoxia: CAUSES OF MID-PROTEROZOIC ANOXIA
Derry, L. A. (2015) · Geophysical Research Letters · doi:10.1002/2015gl065333 · Cited by 147
What caused the rise of atmospheric O2?
Kasting, J. F. (2013) · Chemical Geology · doi:10.1016/j.chemgeo.2013.05.039 · Cited by 144
“Using methods from Kump and Seyfried (2005), they estimated that f ≅ 1.5 for Archean hydrothermal vents.”
BackgroundMethodInfluentialDeposition of 1.88-billion-year-old iron formations as a consequence of rapid crustal growth
Rasmussen, B., Fletcher, I. R., Bekker, A., Muhling, J. R., Gregory, C. J., & Thorne, A. M. (2012) · Nature · doi:10.1038/nature11021 · Cited by 140
Molybdenum isotope constraints on the extent of late Paleoproterozoic ocean euxinia
Kendall, B., Gordon, G. W., Poulton, S. W., & Anbar, A. D. (2011) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2011.05.019 · Cited by 136
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 139
The Alkaline Solution to the Emergence of Life: Energy, Entropy and Early Evolution
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The inevitable journey to being
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“Upon exhalation, the alkaline and reduced hydrothermal fluids at approximately 1008C interacted with the acidulous, somewhat oxidized, ocean [122] to precipitate porous inorganic mounds [123–125].”
BackgroundBiologically induced initiation of Neoproterozoic snowball-Earth events
Tziperman, E., Halevy, I., Johnston, D. T., Knoll, A. H., & Schrag, D. P. (2011) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1016361108 · Cited by 122
“However, given the lower sulfate concentration in the Neoproterozoic, the hydrothermal Fe2þ concentration is expected to have been much higher (34).”
BackgroundRasmussen, B., Krapež, B., Muhling, J. R., & Suvorova, A. (2015) · Geology · doi:10.1130/g36309.1 · Cited by 115
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
The Geologic History of Seawater
Lowenstein, T. K., Kendall, B., & Anbar, A. D. (2013) · Elsevier eBooks · doi:10.1016/b978-0-08-095975-7.00621-5 · Cited by 117
Snowball Earth ocean chemistry driven by extensive ridge volcanism during Rodinia breakup
Gernon, T., Hincks, T. K., Tyrrell, T., Rohling, E. J., & Palmer, M. R. (2016) · Nature Geoscience · doi:10.1038/ngeo2632 · Cited by 111
Highly alkaline, high-temperature hydrothermal fluids in the early Archean ocean
Shibuya, T., Komiya, T., Nakamura, K., Takai, K., & Maruyama, S. (2010) · Precambrian Research · doi:10.1016/j.precamres.2010.08.011 · Cited by 112
Niches of the pre‐photosynthetic biosphere and geologic preservation of Earth's earliest ecology
SLEEP, N. H., & BIRD, D. K. (2007) · Geobiology · doi:10.1111/j.1472-4669.2007.00105.x · Cited by 117
Spence, G. H., Heron, D. P. L., & Fairchild, I. J. (2016) · Sedimentology · doi:10.1111/sed.12261 · Cited by 105
“A positive feedback on Fe/S ratios is found at ocean ridges where enhanced Fe release from hydrothermal systems is expected when sulphate levels (or sea-levels) drop (Kump & Seyfried, 2005).”
BackgroundGreen Rust: The Simple Organizing ‘Seed’ of All Life?
Russell, M. J. (2018) · Life · doi:10.3390/life8030035 · Cited by 101
“s noted, green rust ould have been precipitated fro iron derived ulti ately fro high te perature acidic springs [142].”
BackgroundInfluentialThe rise of oxygen and siderite oxidation during the Lomagundi Event
Bachan, A., & Kump, L. R. (2015) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1422319112 · Cited by 96
“Delivery of ferrous iron from terrestrial settings would have ceased under a high-O2 atmosphere, and hydrothermal inputs of reduced iron would have likely diminished in an ocean bearing appreciable quantities of sulfate (26).”
BackgroundSelf-citationStern, R. J., Mukherjee, S. K., Miller, N. R., Ali, K. A., & Johnson, P. R. (2013) · Precambrian Research · doi:10.1016/j.precamres.2013.07.015 · Cited by 102
“…the global re-appearance of BIF in Neoproterozoic time: (1) the Snowball Earth Hypothesis (SEH) of Hoffman et al. (2002); (2) the Zipper Rift Model of Eyles and Januszczak (2004); (3) the Stagnant Basin model of Knoll et al. (1996); and (4) the Fall in Sea Level model of Kump and Seyfried (2005).”
BackgroundMethodThe biogeochemistry of ferruginous lakes and past ferruginous oceans
Swanner, E. D., Lambrecht, N., Wittkop, C. A., Harding, C., Katsev, S., Torgeson, J. M., & Poulton, S. W. (2020) · Earth-Science Reviews · doi:10.1016/j.earscirev.2020.103430 · Cited by 104
Iron-Sulfide-Bearing Chimneys as Potential Catalytic Energy Traps at Life's Emergence
Mielke, R. E., Robinson, K. J., White, L. M., McGlynn, S. E., McEachern, K., Bhartia, R., Kanik, I., & Russell, M. J. (2011) · Astrobiology · doi:10.1089/ast.2011.0667 · Cited by 99
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The Great Oxygenation Event as a consequence of ecological dynamics modulated by planetary change
Olejarz, J. W., Iwasa, Y., Knoll, A. H., & Nowak, M. A. (2021) · Nature Communications · doi:10.1038/s41467-021-23286-7 · Cited by 90
Tsikos, H., Matthews, A., Erel, Y., & Moore, J. M. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2010.07.032 · Cited by 91
Photoferrotrophy, deposition of banded iron formations, and methane production in Archean oceans
Thompson, K. J., Kenward, P. A., Bauer, K. W., Warchola, T. J., Gauger, T., Martinez, R. E., Simister, R. L., Michiels, C., Llirós, M., Reinhard, C. T., et al. (2019) · Science Advances · doi:10.1126/sciadv.aav2869 · Cited by 95
“The effect of seawater sulfate concentrations on the Fe(II) concentration in lower-temperature, off-axis hydrothermal fluids appears less pronounced, and so we conservatively consider off-axis hydrothermal Fe(II) concentrations equivalent to today (~0.75 mmol kg −1 ) ( 42 ).”
InfluentialEvolution of the structure and impact of Earth’s biosphere
Planavsky, N. J., Crowe, S. A., Fakhraee, M., Beaty, B., Reinhard, C. T., Mills, B. J. W., Holstege, C., & Konhauser, K. O. (2021) · Nature Reviews Earth & Environment · doi:10.1038/s43017-020-00116-w · Cited by 102
Li, C., Planavsky, N. J., Love, G. D., Reinhard, C. T., Hardisty, D. S., Feng, L., Bates, S. M., Huang, J., Zhang, Q., Chu, X., et al. (2014) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2014.12.005 · Cited by 87
“Alternatively, the end of major IF deposition may have been linked to changes in hydrothermal fluid Fe-tosulfide ratios (e.g., Kump and Seyfried, 2005; Planavsky et al., 2011) and the overall fluxes of those fluids to the ocean (Isley and Abbott, 1999; Bekker et al., 2010).”
BackgroundBiogeochemical Transformations in the History of the Ocean
Lenton, T. M., & Daines, S. J. (2016) · Annual Review of Marine Science · doi:10.1146/annurev-marine-010816-060521 · Cited by 80
Kendall, B., Anbar, A. D., Kappler, A. A., & Konhauser, K. O. (2012) · Wiley eBooks · doi:10.1002/9781118280874.ch6 · Cited by 80
“Modified from Langmuir (1997).”
Cheng, M., Li, C., Chen, X., Zhou, L., Algeo, T. J., Ling, H.-F., Feng, L.-J., & Jin, C.-S. (2018) · Precambrian Research · doi:10.1016/j.precamres.2017.12.007 · Cited by 77
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A theoretical prediction of chemical zonation in early oceans (>520 Ma)
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Hoffman, P. F., Macdonald, F. A., & Halverson, G. P. (2011) · Geological Society London Memoirs · doi:10.1144/m36.5 · Cited by 76
“High degrees of continental ice cover and consequent large sea-level falls favour Fe over S in ocean waters because of reduced riverine sulphate supply and higher Fe/S in deep-sea hydrothermal vent fluids, respectively (Canfield & Raiswell 1999; Kump & Seyfried 2005).”
BackgroundThe Great Oxidation Event Transition
Catling, D. C. (2013) · Elsevier eBooks · doi:10.1016/b978-0-08-095975-7.01307-3 · Cited by 80
Black smokers and density currents: A uniformitarian model for the genesis of banded iron-formations
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Huang, J., Chu, X., Jiang, G., Feng, L., & Chang, H. (2011) · Journal of the Geological Society · doi:10.1144/0016-76492010-132 · Cited by 73
Hoffman, P. F. (2005) · South African Journal of Geology · doi:10.2113/108.4.557 · Cited by 70
Effect of paleoseawater composition on hydrothermal exchange in midocean ridges
Antonelli, M. A., Pester, N. J., Brown, S. T., & DePaolo, D. J. (2017) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1709145114 · Cited by 71
“This result may be important for understanding hydrothermal circulation during the Archean and Proterozoic, when seawater [SO4] may have been especially low (12, 56, 57).”
BackgroundProducts of the iron cycle on the early Earth
Tosca, N. J., Jiang, C. Z., Rasmussen, B., & Muhling, J. R. (2019) · Free Radical Biology and Medicine · doi:10.1016/j.freeradbiomed.2019.05.005 · Cited by 71
“Such low pressures are thought to have been more common in mid-ocean ridge systems developed during the Archean when higher heat flow led to shallower depths to the magma chamber [86,89,90].”
BackgroundInfluentialDesign, Fabrication, and Test of a Hydrothermal Reactor for Origin-of-Life Experiments
Mielke, R. E., Russell, M. J., Wilson, P. R., McGlynn, S. E., Coleman, M. L., Kidd, R. D., & Kanik, I. (2010) · Astrobiology · doi:10.1089/ast.2009.0456 · Cited by 68
“These transition metals, dissolved as clusters or occurring as nanoparticles in the early oxygen-free carbonic ocean, were ultimately derived from much hotter (360–4008C) acidic submarine springs (Douville et al., 2002; Kump and Seyfried, 2005).”
Hodel, F., Macouin, M., Triantafyllou, A., Carlut, J., Berger, J., Rousse, S., Ennih, N., & Trindade, R. I. F. (2017) · Precambrian Research · doi:10.1016/j.precamres.2017.08.005 · Cited by 69
Effects of primitive photosynthesis on Earth’s early climate system
Ozaki, K., Tajika, E., Hong, P. K., Nakagawa, Y., & Reinhard, C. T. (2018) · Nature Geoscience · doi:10.1038/s41561-017-0031-2 · Cited by 65
Shibuya, T., Russell, M. J., & Takai, K. (2015) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2015.11.021 · Cited by 66
Soderman, C., Matthews, S., Shorttle, O., Jackson, M. G., Ruttor, S., Nebel, O., Turner, S., Beier, C., Millet, M., Widom, E., et al. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.09.033 · Cited by 65
Extraterrestrial demise of banded iron formations 1.85 billion years ago
Slack, J. F., & Cannon, W. F. (2009) · Geology · doi:10.1130/g30259a.1 · Cited by 63
Baldwin, G. J., Turner, E. C., & Kamber, B. S. (2012) · Canadian Journal of Earth Sciences · doi:10.1139/e11-066 · Cited by 62
Anoxic photochemical oxidation of siderite generates molecular hydrogen and iron oxides
Kim, J. D., Yee, N., Nanda, V., & Falkowski, P. G. (2013) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1308958110 · Cited by 62
“Further, assuming an Fe–H2S ratio of ∼12:1 and an iron concentration of ∼50 mmol Fe/kg (28, 29), we estimate the iron flux to the entire Archean ocean to have been ∼4.”
BackgroundInfluentialMacdonald, F. A., Strauss, J. V., Rose, C. V., Dudás, F. Ö., & Schrag, D. P. (2010) · American Journal of Science · doi:10.2475/09.2010.05 · Cited by 59
Branscomb, E., & Russell, M. J. (2018) · BioEssays · doi:10.1002/bies.201700182 · Cited by 59
Wang, C., Konhauser, K. O., & Zhang, L. (2015) · Economic Geology · doi:10.2113/econgeo.110.6.1515 · Cited by 59
“…to promote the formation of giant BIFs, or that marine sulfate levels were high enough so that the sulfide produced during bacterial sulfate reduction exceeded the hydrothermal Fe(II) supply, with the result that iron sulfides precipitated instead of iron oxides (see Kump and Seyfried, 2005).”
BackgroundA seawater throttle on H 2 production in Precambrian serpentinizing systems
Tutolo, B. M., Seyfried, W. E., & Tosca, N. J. (2020) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1921042117 · Cited by 64
Self-citationDepositional setting of Algoma-type banded iron formation
Gourcerol, B., Thurston, P. C., Kontak, D. J., Côté-Mantha, O., & Biczok, J. (2016) · Precambrian Research · doi:10.1016/j.precamres.2016.04.019 · Cited by 61
“…it appears that calcite (rather than anhydrite) and igneous plagioclase precipitated due to extremely low sulfate concentration in the seawater (Kump and Seyfried, 2005) suggesting that CO2 concentration in the Archean hydrothermal fluid was high enough to precipitate calcite compared to…”
BackgroundAngerer, T., Hagemann, S. G., Walde, D. H. G., Halverson, G. P., & Boyce, A. J. (2016) · Precambrian Research · doi:10.1016/j.precamres.2016.01.002 · Cited by 61
“If fluid flow rates were intense enough, possibly accommodated by 611 glacioeustatic pressurization and depressurization (Kump and Seyfried, 2005), these processes 612 may effectively contribute to the metal fertilization.”
BackgroundMcGlynn, S. E., Kanik, I., & Russell, M. J. (2012) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2011.0211 · Cited by 57
Paleontology of Earth's Mantle
Sleep, N. H., Bird, D. K., & Pope, E. C. (2012) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-092611-090602 · Cited by 54
“By convention, the standard reference ratio is a meteorite; hence the δ values for the mantle are approximately 0; δ34S of arc volcanics is ∼6 (Alt 1995, Kump & Seyfried 2005).”
BackgroundWang, X., Wan, Y., Hu, W., Chou, I., Cao, J., Wang, X., Wang, M., & Li, Z. (2016) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2016.03.001 · Cited by 52
Iron isotope biogeochemistry of Neoproterozoic marine shales
Kunzmann, M., Gibson, T. M., Halverson, G. P., Hodgskiss, M. S. W., Bui, T. H., Carozza, D. A., Sperling, E. A., Poirier, A., Cox, G. M., & Wing, B. A. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2017.04.003 · Cited by 51
“…ocean, hydrothermal iron must have been a much more important iron source due to anoxic and sulfate-poor conditions (e.g., Derry and Jacobsen, 1990; Kump and Seyfried, 2005; Holland, 2006), which allowed the build-up of a significant ferrous seawater reservoir as indicated by the deposition of BIF…”
BackgroundIron: Life’s primeval transition metal
Johnson, J. E., Present, T. M., & Valentine, J. S. (2024) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.2318692121 · Cited by 52
Kou, C., Zhang, Z., Santosh, M., Huang, H., & Zhu, J. (2017) · Gondwana Research · doi:10.1016/j.gr.2017.05.016 · Cited by 46
Hydrothermal vent fluid-seawater mixing and the origins of Archean iron formation
Tosca, N. J., & Tutolo, B. M. (2023) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2023.05.002 · Cited by 49
Yang, X.-Q., Zhang, Z.-H., Duan, S.-G., & Zhao, X.-M. (2015) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2015.03.024 · Cited by 42
Types and geological characteristics of iron deposits in China
Li, H., Li, L., Yang, X., & Cheng, Y. (2014) · Journal of Asian Earth Sciences · doi:10.1016/j.jseaes.2014.11.003 · Cited by 44
Russell, M. J., & Ponce, A. (2020) · Life · doi:10.3390/life10110291 · Cited by 46
Metadata
- Authors
- Kump, L. R., & Seyfried, W. E.
- Affiliations
- Pennsylvania State University (US)
- University of Minnesota (US)
- Corresponding author
- Kump, Lee R.
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2005-07
- Volume
- 235
- Issue
- 3-4
- Pages
- 654-662
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2011437871
- Cited by
- 221
- References
- 54
- Citations by year
- 2026: 2 · 2025: 13 · 2024: 19 · 2023: 9 · 2022: 10 · 2021: 13 · 2020: 12 · 2019: 11 · 2018: 9 · 2017: 20 · 2016: 11 · 2015: 14 · 2014: 5 · 2013: 13 · 2012: 11
- FWCI
- 4.90
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- Funders
- NASA Astrobiology Institute
- 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 › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
- Keywords
- black smokers, iron flux, seawater sulfate, hydrogen sulfide, banded iron formations, oxidative weathering, Snowball Earth, eustatic sea-level fall, hydrostatic pressure, mid-ocean ridge basalt
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