Atmospheric oxygenation caused by a change in volcanic degassing pressure - Nature
- ️Arndt, Nicholas T.
- ️Wed Oct 12 2011
Buick, R. When did oxygenic photosynthesis evolve? Phil. Trans. R. Soc. Lond. B 363, 2731–2743 (2008)
Campbell, I. H. & Allen, C. M. Formation of supercontinents linked to increases in atmospheric oxygen. Nature Geosci. 1, 554–558 (2008)
Kasting, J. F., Eggler, D. H. & Raeburn, S. P. Mantle redox evolution and the oxidation state of the Archean atmosphere. J. Geol. 101, 245–257 (1993)
Holland, H. D. Volcanic gases, black smokers, and the Great Oxidation Event. Geochim. Cosmochim. Acta 66, 3811–3826 (2002)
Canil, D. Vanadium in peridotites, mantle redox and tectonic environments: Archean to present. Earth Planet. Sci. Lett. 195, 75–90 (2002)
Li, Z. X. A. & Lee, C. T. A. The constancy of upper mantle fO2 through time inferred from V/Sc ratios in basalts. Earth Planet. Sci. Lett. 228, 483–493 (2004)
Farquhar, J. et al. Isotopic evidence for Mesoarchaean anoxia and changing atmospheric sulphur chemistry. Nature 449, 706–709 (2007)
Canfield, D. E., Habicht, K. S. & Thamdrup, B. The Archean sulphur cycle and the early history of atmospheric oxygen. Nature 288, 658–661 (2000)
Farquhar, J., Bao, H. & Thiemans, M. Atmospheric influence of Earth’s earliest sulfur cycle. Science 289, 756–758 (2000)
Zahnle, K. J., Claire, M. W. & Catling, D. C. The loss of mass-independent fractionation in sulfur due to a Paleoproterozoic collapse of atmospheric methane. Geobiology 4, 271–283 (2006)
Halevy, I., Johnston, D. T. & Schrag, D. P. Explaining the structure of the Archean mass-independent sulfur isotope record. Science 329, 204–207 (2010)
Kump, L. R. & Barley, M. E. Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago. Nature 448, 1033–1036 (2007)
Butterfield, D. A. et al. Seafloor eruptions and evolution of hydrothermal fluid chemistry. Phil. Trans. R. Soc. Lond. A 355, 369–386 (1997)
Kump, L. R. & Seyfried, W. E. Hydrothermal Fe fluxes during the Precambrian: effect of low oceanic sulfate concentrations and low hydrostatic pressure on the composition of black smokers. Earth Planet. Sci. Lett. 235, 654–662 (2005)
Carmichael, I. S. E. The redox states of basic and silicic magmas: a reflection of their source regions? Contrib. Mineral. Petrol. 106, 129–141 (1991)
Gaillard, F. & Scaillet, B. The sulfur content of volcanic gases on Mars. Earth Planet. Sci. Lett. 279, 34–43 (2009)
Oppenheimer, C., Scaillet, B. & Martin, R. S. Sulfur degassing from volcanoes: source conditions, surveillance, plume chemistry and Earth system impacts. Rev. Mineral. Geochem. 73, 363–421 (2011)
Aiuppa, A. et al. H2S fluxes from Mt. Etna, Stromboli and Vulcano (Italy) and implications for the global volcanic sulfur budget. Geochim. Cosmochim. Acta 69, 1861–1871 (2005)
Bickle, M. J. Heat loss from the Earth: a constraint on Archaean tectonics from the relation between geothermal gradients and the rate of heat production. Earth Planet. Sci. Lett. 40, 301–315 (1978)
Sleep, N. H. & Windley, B. F. Archean plate tectonics—constraints and inferences. J. Geol. 90, 363–379 (1982)
Kasting, J. F. & Holm, N. G. What determines the volume of the oceans. Earth Planet. Sci. Lett. 109, 507–515 (1992)
Bounama, C., Franck, S. & von Bloh, W. The fate of the Earth’s ocean. Hydrol. Earth Syst. Sci. 5, 569–575 (2001)
Sandiford, M. & McLaren, S. in Evolution and Differentiation of the Continental Crust (eds Brown, M. & Rushmer, T) 67–92 (Cambridge University Press, 2006)
Arndt, N. T. Why was flood volcanism on submerged continental platforms so common in the Precambrian? Precambr. Res. 97, 155–164 (1998)
Flament, N., Coltice, N. & Rey, P. F. A case for late-Archaean continental emergence from thermal evolution models and hypsometry. Earth Planet. Sci. Lett. 275, 326–336 (2008)
Taylor, S. R. & McLennan, S. M. The Continental Crust: Its Composition and Evolution 1–312 (Blackwell, 1985)
Habicht, K. S., Gade, M., Thamdrup, B., Berg, P. & Canfield, D. E. Calibration of sulfate levels in the Archean ocean. Science 298, 2372–2374 (2002)
Lyons, T. W. & Gill, B. C. Ancient sulfur cycling and oxygenation of the early biosphere. Elements 6, 93–99 (2010)
Scott, C. T. et al. Late Archean euxinic conditions before the rise of atmospheric oxygen. Geology 39, 119–122 (2011)
Claire, M. W., Catling, D. C. & Zahnle, K. J. Biogeochemical modelling of the rise in atmospheric oxygen. Geobiology 4, 239–269 (2006)
Shi, P. F. & Saxena, S. K. Thermodynamic modelling of the C-H-O-S fluid system. Am. Mineral. 77, 1038–1049 (1992)
Morizet, Y., Paris, M., Gaillard, F. & Scaillet, B. C–O–H fluid solubility in haplobasalt under reducing conditions: an experimental study. Chem. Geol. 279, 1–16 (2010)
O'Neill, H. S. C. & Mavrogenes, J. The sulfide saturation capacity and the sulphur content at sulfide saturation of silicate melts at 1400 °C and 1 bar. J. Petrol. 43, 1049–1087 (2002)
Gaillard, F., Schmidt, B. C., Mackwell, S. & McCammon, C. Rate of hydrogen-iron redox exchange in silicate melts and glasses. Geochim. Cosmochim. Acta 67, 2427–2441 (2003)
Kress, V. C. & Carmichael, I. S. E. The compressibility of silicate liquids containing Fe2O3 and the effect of composition, temperature, oxygen fugacity and pressure on their redox states. Contrib. Mineral. Petrol. 108, 82–92 (1991)
Burgisser, A. & Scaillet, B. Redox evolution of degassing magma rising to the surface. Nature 445, 194–197 (2007)
Pommier, A., Gaillard, F. & Pichavant, M. Time-dependent changes of the electrical conductivity of basaltic melts with redox state. Geochim. Cosmochim. Acta 74, 1653–1671 (2010)