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  • Print publication year: 2015
  • Online publication date: February 2015

14 - Volcanic emissions: short-term perturbations, long-term consequences and global environmental change

from Part Three - Modes of volcanically induced global environmental change


Andres, R.J. and Kasgnoc, A.D. (1998). A time-averaged inventory of subaerial volcanic sulfur emissions. Journal of Geophysical Research, 103, 25251–25261.
Berner, R.A., Lasaga, A.C. and Garrels, R.M. (1983). The carbonate–silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years. American Journal of Science, 283, 641–683.
Black, B.A., Elkins-Tanton, L.T., Rowe, M.C. and PeateI.U. (2012). Magnitude and consequences of volatile release from the Siberian Traps. Earth and Planetary Science Letters, 317 –318, 363–373.
Blake, S., Self, S., Sharma, K. and Sephton, S. (2010). Sulfur release from the Columbia River Basalts and other flood lava eruptions constrained by a model of sulfide saturation. Earth and Planetary Science Letters, 299, 328–338.
Bray, J.R. (1977). Pleistocene volcanism and glacial initiation. Science, 197, 251–254.
Brown, R.J., Blake, S., Dondre, N.R., Phadnis, V.M. and Self, S. (2011). ‘A’ā lava flows in the Deccan Volcanic Province, India, and their significance for the nature of continental flood basalt eruptions. Bulletin of Volcanology, 73, 737–752.
Bryan, S.E., Peate, I.U., Peate, al. (2010). The largest volcanic eruptions on Earth. Earth-Science Reviews, 102, 207–229
Burton, M.R., Sawyer, G.M. and Granieri, D. (2013). Deep carbon emissions from volcanoes. Reviews in Mineralogy & Geochemistry, 75, 323–354.
Carr, M.J., Saginor, I., Alvarado, al. (2007). Element fluxes from the volcanic front of Nicaragua and Costa Rica. Geochemistry Geophysics Geosystems, 8, Q06001.
Cather, S.M., Dunbar, N.W., McDowell, F.W., McIntosh, W.C. and Scholle, P.A. (2009). Climate forcing by iron fertilization from repeated ignimbrite eruptions: the icehouse–silicic large igneous province (SLIP) hypothesis. Geosphere, 5, 315–324.
Chesner, C.A. and Luhr, J.F. (2010). A melt inclusion study of the Toba Tuffs, Sumatra, Indonesia. Journal of Volcanology and Geothermal Research, 197, 259–278.
Crisp, J.A. (1984). Rates of magma emplacement and volcanic output. Journal of Volcanology and Geothermal Research, 20, 177–211.
Delmelle, P., Stix, J., Baxter, P.J., Garcia-Alvarez, J. and Barquero, J. (2002). Atmospheric dispersion, environmental effects and potential health hazard associated with the low-altitude gas plume of Masaya volcano, Nicaragua. Bulletin of Volcanology, 64, 423–434.
de Silva, S.L. and Gosnold, W.D. (2007). Episodic construction of batholiths: insights from the spatiotemporal development of an ignimbrite flare-up. Journal of Volcanology and Geothermal Research, 167, 320–335.
Edmond, J.M. and Huh, Y. (2003). Non-steady state carbonate recycling and implications for the evolution of atmospheric P-CO2. Earth and Planetary Science Letters, 216, 125–139.
Gaillard, F., Scaillet, B. and Arndt, N.T. (2011). Atmospheric oxygenation caused by a change in volcanic degassing pressure. Nature, 478, 229–232.
Ganino, C. and Arndt, N.T. (2009). Climate changes caused by degassing of sediments during the emplacement of large igneous provinces. Geology, 37, 323–326.
Gerlach, T.M. (2011). Volcanic versus anthropogenic carbon dioxide. EOS, Transactions AGU, 92, 201–202.
Gerlach, T.M., Westrich, H.R. and Symonds, R.B. (1996). Preeruption vapor in magma of the climactic Mount Pinatubo eruption: source of the giant stratospheric sulfur dioxide cloud. In Fire and Mud: Eruptions and Lahars of Mount Pinatubo, Philippines, ed. C.G. Newhall and R.S. Punongbayan,University of Washington Press, 415–433.
Glazner, A.F., Manley, C.R., Marron, J.S. and Rojstaczer, S. (1999). Fire or ice: anticorrelation of volcanism and glaciation in California over the past 800,000 years. Geophysical Research Letters, 26, 1759–1762.
Gorman, P.J., Kerrick, D.M. and Connolly, J.A.D. (2006). Modeling open system metamorphic decarbonation of subducting slabs. Geochemistry Geophysics Geosystems, 7, Q04007.
Halmer, M.M., Schmincke, H.U. and Graf, H.F. (2002). The annual volcanic gas input into the atmosphere, in particular into the stratosphere: a global data set for the past 100 years. Journal of Volcanology and Geothermal Research, 115, 511–528.
Holland, H.D. (2002). Volcanic gases, black smokers, and the Great Oxidation Event. Geochimica et Cosmochimica Acta, 66, 3811–3826.
Holland, H.D. (2009). Why the atmosphere became oxygenated: a proposal. Geochimica et Cosmochimica Acta, 73, 5241–5255.
Huybers, P. and Langmuir, C. (2009). Feedback between deglaciation, volcanism, and atmospheric CO2. Earth and Planetary Science Letters, 286, 479–491.
Johnston, F.K.B., Turchyn, A.V. and Edmonds, M. (2011). Decarbonation efficiency in subduction zones: implications for warm Cretaceous climates. Earth and Planetary Science Letters, 303, 143–152.
Jones, G.S., Gregory, J.M., Stott, P.A., Tett, S.F.B. and Thorpe, R.B. (2005). An AOGCM simulation of the climate response to a volcanic super-eruption. Climate Dynamics, 25, 725–738.
Jull, M. and McKenzie, D. (1996). The effect of deglaciation on mantle melting beneath Iceland. Journal of Geophysical Research, 101, 21815–21828.
Kasting, J.F. and Catling, D. (2003). Evolution of a habitable planet. Annual Review of Astronomy and Astrophysics, 41, 429–463.
Kent, D.V. and Muttoni, G. (2008). Equatorial convergence of India and early Cenozoic climate trends. Proceedings of the National Academy of Sciences, 105, 16065–16070.
Krueger, A.J., Walter, L.S., Bhartia, al. (1995). Volcanic sulfur dioxide measurements from the total ozone mapping spectrometer instruments. Journal of Geophysical Research, 100, 14,057–14,076.
Kutterolf, S., Freundt, A. and Perez, W. (2008). Pacific offshore record of Plinian arc volcanism in Central America: 2. Tephra volumes and erupted masses. Geochemistry Geophysics Geosystems, 9, Q02S02.
Lipman, P.W. (2007). Incremental assembly and prolonged consolidation of Cordilleran magma chambers: evidence from the Southern Rocky Mountain volcanic field. Geosphere, 3, 42–70.
Lund, D.C. and Asimow, P.D. (2011). Does sea level influence mid-ocean ridge magmatism on Milankovitch timescales?Geochemistry Geophysics Geosystems, 12, Q12009.
Maclennan, J., Jull, M., McKenzie, D., Slater, L. and Gronvold, K. (2002). The link between volcanism and deglaciation in Iceland. Geochemistry Geophysics Geosystems, 3, 1062–1087.
Marks, L., Keiding, J., Wenzel, al. (2014). F, Cl, and S concentrations in olivine-hosted melt inclusions from mafic dikes in NW Namibia and implications for the environmental impact of the Paraná–Etendeka Large Igneous Province. Earth and Planetary Science Letters, 392, 39–49.
Marty, B. and Tolstikhin, I.N. (1998). CO2 fluxes from mid-ocean ridges, arcs and plumes. Chemical Geology, 145, 233–248.
Mason, B.G., Pyle, D.M. and Oppenheimer, C. (2004a). The size and frequency of the largest eruptions on Earth. Bulletin of Volcanology, 66, 735–748.
Mason, B.G., Pyle, D.M., Dade, W.B. and Jupp, T. (2004b). Seasonality of volcanic eruptions. Journal of Geophysical Research, 109, B04206.
Mather, T.A., Pyle, D.M. and Oppenheimer, C. (2003). Tropospheric volcanic aerosol. AGU Geophysical Monograph, 139, 189–212.
McCormickM.P., Thomason, L.W. and Trepte, C.R. (1995). Atmospheric effects of the Mt. Pinatubo eruption. Nature, 373, 399–404.
McGuire, W.J., Howarth, R.J., Firth, al. (1997). Correlation between rate of sea-level change and frequency of explosive volcanism in the Mediterranean. Nature, 389, 473–476.
Miller, G.H., Geirsdóttir, Á., Zhong, al. (2012). Abrupt onset of the Little Ice Age triggered by volcanism and sustained by sea-ice/ocean feedbacks. Geophysical Research Letters, 39, L02708.
Moretti, R., Papale, P. and Ottonello, G. (2003). A model for the saturation of C–O–H–S fluids in silicate melts. Geological Society of London Special Publication, 213, 81–101.
Nakada, M. and Yokose, H. (1992). Ice-age as a trigger of active quaternary volcanism and tectonism. Tectonophysics, 212, 321–329.
Nowell, D.A.G., Jones, M.C. and Pyle, D.M. (2006). Episodic Quaternary volcanism in France and Germany. Journal of Quaternary Science, 21, 645–675.
Oppenheimer, C. (2002). Limited global change due to the largest known Quaternary eruption, Toba ~ 74 kyr BP?Quaternary Science Reviews, 21, 1593–1609.
Oppenheimer, C. (2003). Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (Indonesia) 1815. Progress in Physical Geography, 27, 230–259.
Pagli, C. and Sigmundsson, F. (2008). Will present day glacier retreat increase volcanic activity? Stress induced by recent glacier retreat and its effect on magmatism at the Vatnajokull ice cap, Iceland. Geophysical Research Letters, 35, L09304.
Parks, M.M., Caliro, S., Chiodini, al. (2013). Distinguishing contributions to diffuse CO2 emissions in volcanic areas from magmatic degassing and thermal decarbonation using soil gas 222Rn–δ13C systematics: application to Santorini volcano, Greece. Earth and Planetary Science Letters, 377 –378, 180–190.
Paterson, S.R., Okaya, D., Memeti, V., Economos, R. and Miller, R.B. (2011). Magma addition and flux calculations of incrementally constructed magma chambers in continental margin arcs: combined field, geochronologic, and thermal modeling studies. Geosphere, 7, 1439–1468.
Petraglia, M., Ditchfield, P., Jones, S., Korisettar, R. and Pal, J.N. (2012). The Toba volcanic super-eruption, environmental change and hominin occupation history in India over the last 140,000 years. Quaternary International, 258, 119–134.
Pyle, D.M. (1995). Mass and energy budgets of explosive volcanic eruptions. Geophysical Research Letters, 22, 563–566.
Pyle, D.M., Beattie, P.D. and Bluth, G.J.S. (1996). Sulphur emissions to the stratosphere from explosive volcanic eruptions. Bulletin of Volcanology, 57, 663–671.
Pyle, D.M. and Mather, T.A. (2003). The importance of volcanic emissions in the global atmospheric mercury cycle. Atmospheric Environment, 37, 5115–5124.
Rampino, M.R., Self, S. and Fairbridge, R.W. (1979). Can rapid climatic change cause volcanic eruptions?Science, 206, 826–829.
Robock, A., Ammann, C.M., Oman, al. (2009). Did the Toba volcanic eruption of similar to 74 ka BP produce widespread glaciation?Journal of Geophysical Research, 114, D10107.
Robock, A. (2000). Volcanic eruptions and climate. Reviews of Geophysics, 38, 191–219.
Roth, R. and Joos, F. (2012). Model limits on the role of volcanic carbon emissions in regulating glacial–interglacial CO2 variations. Earth and Planetary Science Letters, 329, 141–149.
Scaillet, B. and Macdonald, R. (2006). Experimental and thermodynamic constraints on the sulphur yield of peralkaline and metaluminous silicic flood eruptions. Journal of Petrology, 47, 1413–1437.
Scaillet, B. and Pichavant, M. (2003). Experimental constraints on volatile abundances in arc magmas and their implications for degassing processes. Geological Society of London Special Publication, 213, 23–52.
Schaefer, L. and Fegley, B. (2007). Outgassing of ordinary chondritic material and some of its implications for the chemistry of asteroids, planets, and satellites. Icarus, 186, 462–483.
Self, S., Gertisser, R., Thordarson, T., Rampino, M.R. and Wolff, J.A. (2004). Magma volume, volatile emissions, and stratospheric aerosols from the 1815 eruption of Tambora. Geophysical Research Letters, 31, L20608.
Self, S., Widdowson, M., Thordarson, T. and Jay, A.E. (2006). Volatile fluxes during flood basalt eruptions and potential effects on the global environment: a Deccan perspective. Earth and Planetary Science Letters, 248, 518–532.
Self, S., Blake, S., Sharma, K., Widdowson, M. and Sephton, S. (2008). Sulfur and chlorine in Late Cretaceous Deccan magmas and eruptive gas release. Science, 319, 1654–1657.
Sigvaldason, G.E., Annertz, K. and Nilsson, M. (1992). Effect of glacier loading/deloading on volcanism: postglacial volcanic production rates of the Dyngjufjöll area, central Iceland. Bulletin of Volcanology, 54, 385–392.
Sobolev, S.V., Sobolev, A.V., Kuzmin, al. (2011). Linking mantle plumes, large igneous provinces and environmental catastrophes. Nature, 477, 312–316.
Stoiber, R.E., Williams, S.N. and Huebert, B. (1987). Annual contribution of sulfur dioxide to the atmosphere by volcanoes. Journal of Volcanology and Geothermal Research, 33, 1–8.
Syracuse, E.M. and Abers, G.A. (2006). Global compilation of variations in slab depth beneath arc volcanoes and implications. Geochemistry Geophysics Geosystems, 7, Q05017.
Tang, Q., Zhang, M., Li, C., Yu, M. and Li, L. (2013). The chemical compositions and abundances of volatiles in the Siberian large igneous province: constraints on magmatic CO2 and SO2 emissions into the atmosphere. Chemical Geology, 339, 84–91.
Thordarson, T. and Self, S. (1996). Sulfur, chlorine and fluorine degassing and atmospheric loading by the Roza eruption, Columbia River Basalt Group, Washington, USA. Journal of Volcanology and Geothermal Research, 74, 49–73.
Timmreck, C., Graf, H-F., Lorenz, al. (2010). Aerosol size confines climate response to volcanic super-eruptions. Geophysical Research Letters, 37, L24705.
Timmreck, C., Graf, H.F., Zanchettin, al. (2012). Climate response to the Toba super-eruption: regional changes. Quaternary International, 258, 30–44.
Völker, D., Kutterolf, S. and Wehrmann, H. (2011). Comparative mass balance of volcanic edifices at the southern volcanic zone of the Andes between 33 °S and 46 °S. Journal of Volcanology and Geothermal Research, 205, 114–129.
Wallmann, P.C., Mahood, G.A. and Pollard, D.D. (1988). Mechanical models for correlation of ring-fracture eruptions at Pantelleria, Strait of Sicily, with glacial sea-level drawdown. Bulletin of Volcanology, 50, 327–339.
Wallmann, K. (2001). Controls on the Cretaceous and Cenozoic evolution of seawater composition, atmospheric CO2 and climate. Geochimica et Cosmochimica Acta, 65, 3005–3025.
Watt, S.F.L., Pyle, D.M. and Mather, T.A. (2013). The volcanic response to deglaciation: evidence from glaciated arcs and a reassessment of global eruption records. Earth-Science Reviews, 122, 77–102.
Westrich, H.R. and Gerlach, T.M. (1992). Magmatic gas source for the stratospheric SO2 cloud from the June 15, 1991, eruption of Mount Pinatubo. Geology, 20, 867–870.
White, S.M., Crisp, J.A. and Spera, F.J. (2006). Long-term volumetric eruption rates and magma budgets. Geochemistry Geophysics Geosystems, 7, Q03010.
Zielinski, G.A. (2000). Use of paleo-records in determining variability within the volcanism–climate system. Quaternary Science Reviews, 19, 417–438.