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Climate-Volcanism Feedback and the Toba Eruption of ∼74,000 Years Ago

Published online by Cambridge University Press:  20 January 2017

Michael R. Rampino  and
Stephen Self
Michael R. Rampino
Affiliation:
Earth Systems Group, Department of Applied Science, New York University, New York, New York 10003; and NASA, Goddard Institute for Space Studies, New York, New York 10025
Stephen Self
Affiliation:
Department of Geology and Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, Hawaii 96822
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Abstract

A general feedback between volcanism and climate at times of transition in the Quaternary climate record is suggested, exemplified by events accompanying the Toba eruption (∼74,000 yr ago), the largest known late Quaternary explosive volcanic eruption. The Toba paroxysm occurred during the δ18O stage 5a-4 transition, a period of rapid ice growth and falling global sea level, which may have been a factor in creating stresses that triggered the volcanic event. Toba is estimated to have produced between 1015 and 1016 g of fine ash and sulfur gases lofted in co-ignimbrite ash clouds to heights of at least 32 ± 5 km, which may have led to dense stratospheric dust and sulfuric acid aerosol clouds. These conditions could have created a brief, dramatic cooling or "volcanic winter," followed by estimated annual Northern Hemisphere surface-temperature decreases of ∼3° to 5°C caused by the longer-lived aerosols. Summer temperature decreases of ⩾10°C at high northern latitudes, adjacent to regions already covered by snow and ice, might have increased snow cover and sea-ice extent, accelerating the global cooling already in progress. Evidence for such climate-volcanic feedback, following Milankovitch periodicities, is found at several climatic transitions.

Type
Research Article
Information
Quaternary Research , Volume 40 , Issue 3 , November 1993 , pp. 269 - 280
Copyright
University of Washington

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References

Acharyya, S. K. (1993). The Toba ash-bed marker from the Indian subcontinent: Its implications on correlation of Late Pleistocene alluvial conditions and assessment of paleoclimatic conditions. Quaternary Research 40, 10–19.CrossRefGoogle Scholar
Barnola, J. M. Raynaud, D. Korotkevich, Y. S., and Lorius, C. (1987). Vostok ice core provides 160,000 year record of atmospheric CO2. Nature 329, 408–414.CrossRefGoogle Scholar
Barry, R. C. Andrews, J. T., and Mahaffy, M. A. (1975). Continental ice sheets: Conditions for growth. Science 190, 979–981.CrossRefGoogle Scholar
Berger, A. L. (1978a). Long-term variations of daily insolation and Quaternary climatic changes. Journal of the Atmospheric Sciences 35, 2362–2367.2.0.CO;2>CrossRefGoogle Scholar
Berger, A. L. (1978b). Long-term variations of caloric insolation resulting from the Earth’s orbital elements. Quaternary Research 9, 139–167.CrossRefGoogle Scholar
Berger, A. L. (1984). Accuracy and frequencies stability of the Earth’s orbital elements during the Quaternary. In “Milankovitch and Climate, Parts 1 and 2” (Berger, A. L. et al., Eds.), pp. 3–40. Reidel, Dordrecht.Google Scholar
Bjork, S. Ingolfsson, O. Haflidason, H. Hallsdottir, M., and Anderson, N. J. (1992). Lake Torfadalsvatn: A high resolution record of the North Atlantic ash zone I and the last glacial-interglacial environ-mental changes in Iceland. Boreas 21, 15–22.CrossRefGoogle Scholar
Bradley, R. S., and England, J. (1978a). Recent climatic fluctuations of the Canadian high Arctic and their significance for glaciology. Arctic and Alpine Research 10, 715–731.CrossRefGoogle Scholar
Bradley, R. S., and England, J. (1978b). Volcanic dust in influence on glacier mass balances at high latitudes. Nature 271, 736–738.CrossRefGoogle Scholar
Bray, J. R. (1977). Pleistocene volcanism and glacial initiation. Science 197, 251–254.CrossRefGoogle ScholarPubMed
Broecker, W. S., and Denton, G. H. (1990). The role of ocean-atmosphere reorganizations in glacial cycles. Quaternary Science Reviews 9, 305–341.CrossRefGoogle Scholar
Busacca, A. J. Nelstead, K. T. McDonald, E. V., and Purser, M. D. (1992). Correlation of distal tephra layers in loess in the channeled scabland and palouse of Washington state. Quaternary Research 37, 281–303.CrossRefGoogle Scholar
Caldeira, K., and Rampino, M. R. (1992). Mount Etna CO2 may affect climate. Nature 355, 401–402.CrossRefGoogle Scholar
Caress, M. (1985). “Volcanology of the Younger Toba Tuff, Sumatra.” Unpublished Masters dissertation, University of Hawaii at Manoa.Google Scholar
Carey, S. N. Sigurdsson, H., and Sparks, R. S. J. (1989). Experimental studies of particle-laden plumes. Journal of Geophysical Research 93, 15314–15328.CrossRefGoogle Scholar
Chappell, J., and Shackleton, N. J. (1986). Oxygen isotopes and sea level. Nature 324, 137–140.CrossRefGoogle Scholar
Chesner, C. A. Rose, W. I. Deino, A. Drake, R., and Westgate, J. A. (1991). Eruptive history of Earth’s largest Quaternary caldera (Toba, Indonesia) clarified. Geology 19, 200–203.2.3.CO;2>CrossRefGoogle Scholar
Dawson, A. (1991). “Ice Age Earth: Late Quaternary Geology and Climate,” pp. 180–198. Rutledge, London.Google Scholar
DeAngelis, M. Barkov, N. I., and Petrov, V. N. (1987). Aerosol concentrations over the last climatic cycle (160 ka) from an Antarctic core. Nature 325, 318–321.CrossRefGoogle Scholar
Deblonde, G., and Peltier, W. R. (1990). A model of late Pleistocene ice sheet growth with realistic geography and simplified cryodynamics and geodynamics. Climate Dynamics 5, 103–110.CrossRefGoogle Scholar
Dehn, J. Farell, J. W., and Schmincke, H.-U. (1991). Neogene tephro-chronology from Site 758 on Northern Ninetyeast Ridge: Indonesian arc volcanism of the past 5 Ma. Proceedings of the Ocean Drilling Program, Scientific Results 121, 273–295.Google Scholar
Devine, J. D. Sigurdsson, H. Davis, A. N., and Self, S. (1984). Estimates of sulfur and chlorine yield to the atmosphere from volcanic eruptions and potential climatic effects. Journal of Geophysical Research 89, 6309–6325.CrossRefGoogle Scholar
Dobran, F. Neri, A., and Macedonio, G. (1992). “Numerical Simulation of Collapsing Volcanic Columns.” Volcanic Simulation Group Report No. 92–2. Gruppo Nazionale per la Volcanologia, Pisa.Google Scholar
Fichefet, T. Tricot, C Berger, A. Gallee, H., and Marsiat, I. (1989). Climatic studies with a coupled atmosphere-upper-ocean-ice-sheet model. Philosophical Transactions of the Royal Society of London, Series A329, 249–261.Google Scholar
Fierstein, J., and Nathanson, M. (1992). Another look at the calculation of fallout tephra volumes. Bulletin of Volcanology 54, 233–254.CrossRefGoogle Scholar
Gilmour, I. Wolbach, W. S., and Anders, E. (1990). Early environmental effects of the terminal Cretaceous impact. Geological Society of America Special Paper 247, 383–390.CrossRefGoogle Scholar
Guiot, J. (1990). Methodology of the last climatic cycle reconstruction in France from pollen data. Palaeogeography, Palaeoclimateology, Palaeoecology 80, 49–69.CrossRefGoogle Scholar
Guiot, J. Pons, A. de Beaulieu, J. L., and Reille, M. (1989). A 140,000-year continental climate reconstruction from two European pollen records. Nature 338, 309–313.CrossRefGoogle Scholar
Heinrich, H. (1988). Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130,000 years. Quaternary Research 29, 142–152.CrossRefGoogle Scholar
Hofmann, D. J. (1987). Perturbations of the global atmosphere associated with El Chichón volcanic eruption of 1982. Reviews of Geophysics 25, 743–759.CrossRefGoogle Scholar
Ives, J. D. Andrews, J. T., and Barry, R. G. (1975). Growth and decay of the Laurentide Ice Sheet and comparisons with Fenno-Scandinavia. Naturwissenschaften 62, 118–125.CrossRefGoogle Scholar
Jacoby, G. C. Ivanciu, I. S., and Ulan, L. D.(1988). A 263-year record of summer temperature for northern Quebec reconstructed from tree-ring data and evidence of a major climatic shift in the early 1800’s. Palaeogeography, Palaeoclimatology, Palaeoecolology 64, 69–78.CrossRefGoogle Scholar
Jaupart, Cand Allégre, C. J. (1991). Gas content, eruption rate and instabilities of eruption regime in silicic volcanoes. Earth and Planetary Science Letters 102, 413–429.CrossRefGoogle Scholar
Jouzel, J., et at. (1987). Vostok ice core: A continuous isotope temperature record over the last climatic cycle (160,000 years). Nature 329, 403–418.CrossRefGoogle Scholar
Kennett, J. P., and Thunell, R. C. (1975). Global increase in Quaternary explosive volcanism. Science 187, 497–503.CrossRefGoogle ScholarPubMed
Koerner, R. M., and Fisher, D. A. (1985). In “Late Quaternary Environments: Eastern Canadian Arctic, Baffin Bay and West Greenland” (Andrews, J. T., Ed.), pp. 309–327. Allen and Unwin, London.Google Scholar
Koyaguchi, T., and Tokuno, M. (in press). Origin of the giant eruption cloud of Pinatubo, June 15, 1991. Journal of Volcanology and Geo-thermal Research. Google Scholar
Ledbetter, M. T., and Sparks, R. S. J. (1979). Duration of large-magnitude explosive eruptions deduced from graded bedding in deep-sea ash layers. Geology 7, 240–244.2.0.CO;2>CrossRefGoogle Scholar
Legrand, M. R. Delmas, R. J., and Charlson, R. J. (1988). Climate forcing implications from Vostok ice-core sulphate data. Nature 334, 418–420.CrossRefGoogle Scholar
Loewe, F. (1971). Considerations of the origin of the Quaternary Ice Sheet of North America. Arctic and Alpine Research 3, 331–334.CrossRefGoogle Scholar
Manabe, S., and Bryan, K. Jr. (1985). CO2-induced change in a coupled ocean atmosphere model and its paleoclimatic implications. Journal of Geophysical Research 90, 11689–11707.CrossRefGoogle Scholar
Mangerud, J., et al. (1984). A younger Dryas ash bed in western Norway, and its possible correlations with tephra in cores from the Norwegian Sea and the North Atlantic. Quaternary Research 21, 85–104.CrossRefGoogle Scholar
Martinson, D. G., et al. (1987). Age dating and the orbital theory of the Ice Ages: Development of a high-resolution 0 to 300,000-year chro-nostratigraphy. Quaternary Research 7, 1–29.CrossRefGoogle Scholar
Matteucci, G. (1989). Orbital forcing in a stochastic resonance model of the Late-Pleistocene climatic variations. Climate Dynamics 3, 179–190.CrossRefGoogle Scholar
Matthews, R. K. (1969). Tectonic implication of glacio-eustatic sea level fluctuations. Earth and Planetary Science Letters 5, 459–462.CrossRefGoogle Scholar
Nakada, M., and Yokose, H. (1992). Ice age as a trigger of active Quaternary volcanism and tectonism. Tectonophysics 212, 321–329.CrossRefGoogle Scholar
Ninkovich, D., and Shackleton, N. J. (1975). Distribution, stratigraphic position, and age of ash layer “L”, in the Panama Basin. Earth and Planetary Science Letters 27, 20–34.CrossRefGoogle Scholar
Ninkovich, D. Shackleton, N. J. Abdel-Monem, A. A. Obradovich, J. A., and Izett, G. (1978). K-Ar age of the late Pleistocene eruption of Toba, north Sumatra. Nature 276, 574–577.CrossRefGoogle Scholar
Norddahl, H., and Haflidason, H. (1992). The Skógar Tephra, a Younger Dryas marker in North Iceland. Boreas 21, 23–41.CrossRefGoogle Scholar
Oerlemans, J. (1988). Simulation of historic glacier variations with a simple climate-glacier model. Journal of Glaciology 34, 333.CrossRefGoogle Scholar
Oglesby, R. J. (1990). Sensitivity of glaciation to initial snow cover, CO2, snow albedo, and oceanic roughness in the NCAR CCM. Climate Dynamics 4, 219–235.CrossRefGoogle Scholar
Palais, J. M., and Sigurdsson, H. (1989). Petrologic evidence of volatile emissions from major historic and pre-historic volcanic eruptions. American Geophysical Union, Geophysical Monograph 52, 32–53.Google Scholar
Pallister, J. S. Hoblitt, R. P., and Reyes, A. G. (1992). A basalt trigger for the 1991 eruptions of Pinatubo volcano? Nature 356, 426–428.CrossRefGoogle Scholar
Paterae, M., and Guichard, F. (1993). Triggering of volcanic pulses in the Campanian area, South Italy, by periodic deep magma influx. Journal of Geophysical Research 98, 1861–1873.CrossRefGoogle Scholar
Paterne, M. Labeyrie, J. Guichard, F. Mazaud, A., and Maitre, F. (1990). Fluctuations of the Campanian explosive volcanic activity (South Italy) during the past 190,000 years as determined by marine tephrochronology. Earth and Planetary Science Letters, 98, 166–174.CrossRefGoogle Scholar
Paterne, M. Labeyrie, J. Guichard, F. Mazaud, A., and Maitre, F. (1991). “Fluctuations of the Campanian Explosive Volcanic Activity (South Italy) during the Past 190,000 Years as Determined by Marine Tephrochronology,” p. 6. IAVCEI, Programs and Abstracts, XX General Assembly, Vienna, IUGG.Google Scholar
Pinto, J. P. Turco, R. P., and Toon, O. B. (1989). Self-limiting physical and chemical effects in volcanic eruption clouds. Journal of Geophysical Research 94, 11165–11174.CrossRefGoogle Scholar
Porter, S. C. (1986). Pattern and forcing of Northern Hemisphere glacier variations during the last millennium. Quaternary Research 26, 27–48.CrossRefGoogle Scholar
Rampino, M, R., and Self, S. (1982). Historic eruptions of Tambora (1815), Krakatau (1883), and Agung (1963), their stratospheric aerosols, and climatic impact. Quaternary Research 18, 127–143.CrossRefGoogle Scholar
Rampino, M. R., and Self, S. (1992). Volcanic winter and accelerated glaciation following the Toba super-eruption. Nature 359, 50–52.CrossRefGoogle Scholar
Rampino, M. R. Self, S., and Fairbridge, R. W. (1979). Can rapid climatic change cause volcanic eruptions? Science 206, 826–829.CrossRefGoogle ScholarPubMed
Rampino, M. R. Self, S., and Stothers, R. B. (1988). Volcanic winters. Annual Reviews of Earth and Planetary Science 16, 73–99.CrossRefGoogle Scholar
Riehle, J. R. Mann, D. H. Peteet, D. M. Engstrom, D. R. Brew, D. A., and Meyer, C. E. (1992). The Mount Edgecumbe tephra deposits, a marker horizon in southeastern Alaska near the Pleistocene-Holocene boundary. Quaternary Research 37, 183–202.CrossRefGoogle Scholar
Rind, D. Peteet, D., and Kukla, G. (1989). Can Milankovitch orbital variations initiate the growth of ice sheets in a general circulation model? Journal of Geophysical Research 94, 12851–12871.CrossRefGoogle Scholar
Rind, D. (1991). The paleorecord: How useful is it in testing models for future climatic prediction? In “Global Changes of the Past” (Bradley, R. S., Ed.), pp. 397–420. UCAR/Office for Interdisciplinary Earth Studies, Boulder.Google Scholar
Rose, W. I., and Chesner, C. A. (1987). Dispersal of ash in the great Toba eruption, 75 Ka. Geology 15, 913–917.2.0.CO;2>CrossRefGoogle Scholar
Rose, W. I., and Chesner, C. A. (1990). Worldwide dispersal of ash and gases from earth’s largest known eruption: Toba, Sumatra, 75 Ka. Global and Planetary Change 89, 269–275.CrossRefGoogle Scholar
Ruddiman, W. F. (1977a). North Atlantic ice-rafting: A major change at 75,000 years before the present. Science 196, 1208–1211.CrossRefGoogle Scholar
Ruddiman, W. F. (1977). Late Quaternary deposition of ice-rafted sand in the subpolar North Atlantic (lat. 40° to 65°N). Geological Society of America Bulletin 88, 1813–1827.2.0.CO;2>CrossRefGoogle Scholar
Ruddiman, W. F., and Mclntyre, A. (1979). Warmth of the subpolar North Atlantic Ocean during northern hemisphere ice-sheet growth. Science 204, 173–175.CrossRefGoogle ScholarPubMed
Ruddiman, W. F. McIntyre, A. Niebler-Hunt, V., and Durazzi, J. T. (1980). Oceanic evidence for the mechanism of rapid northern hemisphere glaciation. Quaternary Research 13, 33–64.CrossRefGoogle Scholar
Saltzman, B. (1982). Stochastically-driven climatic fluctuations in the sea-ice, ocean temperature, CO2 feedback system. Tellus 34, 97–112.CrossRefGoogle Scholar
Sancetta, C Imbrie, J. Kipp, N. G. McIntyre, A., and Ruddiman, W. F. (1972). Climatic record in North Atlantic deep-sea core V23-82: Comparison of the last and present interglacials based on quantitative time series. Quaternary Research 2, 363–367.CrossRefGoogle Scholar
Sejrup, H. P. (1989). Quaternary tephrachronology on the Iceland Plateau, north of Iceland. Journal of Quaternary Science 4, 109–114.CrossRefGoogle Scholar
Sigvaldason, G. Annerts, K., and Nilsson, M. (1992). Effect of glacier loading/deloading on volcanism: Postglacial volcanic production rate of the Dyngjufjöll area, central Iceland. Bulletin Volcanologique 54, 385–392.CrossRefGoogle Scholar
Sioholm, J. Sejrup, H. P., and Furnes, H. (1991). Quaternary volcanic ash zones on the Iceland Plateau, southern Norwegian Sea. Journal of Quaternary Science 6, 159–173.Google Scholar
Smit, J. van Eijden, , and Troelstra, S. R. (1991). Analysis of the Australasian microtektite event, the Toba Lake event, and the Creta-ceous/Paleogene boundary, Eastern Indian Ocean. Proceedings of the Ocean Drilling Program, Scientific Results 121, 489–503.Google Scholar
Sparks, R. S. J. Moore, J. G., and Rice, C. J. (1986). The initial giant umbrella cloud of the May 18, 1980, explosive eruption of Mount St. Helens. Journal of Volcanology and Geothermal Research 28, 257.CrossRefGoogle Scholar
Sparks, R. S. J., and Walker, G. P. L. (1977). The significance of vitric-enriched airfall ashes associated with crystal-rich igrumbrites. Journal of Volcanology and Geothermal Research 2, 329.CrossRefGoogle Scholar
Stothers, R. B. (1984a). Mystery cloud of AD 536. Nature 307, 344–345.CrossRefGoogle Scholar
Stothers, R. B. (1984b). The great Tambora eruption in 1815 and its aftermath. Science 224, 1191–1198.CrossRefGoogle ScholarPubMed
Stothers, R. B. Wolff, J. A. Self, S., and Rampino, M. R. (1986). Basaltic fissure eruptions, plume heights, and atmospheric aerosols. Geophysical Research Letters 13, 725–728.CrossRefGoogle Scholar
Streeter, S. S., and Shackleton, N. J. (1979). Paleocirculation of the deep North Atlantic: 150,000-year record of benthic foraminifera and oxygen-18. Science 203, 168–171.CrossRefGoogle ScholarPubMed
Turco, R. P. Toon, O. B. Ackerman, T. P. Pollack, J. B., and Sagan, C. (1990). Climate and smoke: An appraisal of nuclear winter. Science 247, 166–176.CrossRefGoogle ScholarPubMed
Westrich, H. R., and Gerlach, T. M. (1992). Magmatic gas source for the stratospheric SO2 cloud from the June 15, 1991, eruption of Mt. Pinatubo. Geology 20, 867–871.2.3.CO;2>CrossRefGoogle Scholar
Wigley, T. M. L. (1991). Climate variability on the 10-100-year time scale: Observations and possible causes. In “Global Changes of the Past” (Bradley, R. S., Ed.), pp. 83–101. UCAR/Office for Interdisciplinary Earth Studies, Boulder.Google Scholar
Williams, J. (1975). The influence of snowcover on the atmospheric circulation and its role in climatic change: An analysis based on results from the NCAR Global Circulation Model. Journal of Applied Meteorology 14, 137–152.2.0.CO;2>CrossRefGoogle Scholar
Williams, L. D. (1979). An energy balance model of potential glacier-ization of northern Canada. Arctic and Alpine Research 11, 443–456.CrossRefGoogle Scholar
Wilson, C. (1985). The Little Ice Age on Eastern Hudson/James Bay: The summer weather and climate at Great Whale, Port George and Eastmain, 1814 to 1821, as derived from Hudson’s Bay Company records. Syllogeus 55, 147–1990.Google Scholar
Woillard, G., and Mook, W. G. (1982). Carbon-14 dates of Grande Pile: Correlation of land and sea chronologies. Science 215, 159–161.CrossRefGoogle ScholarPubMed
Woods, A. W. (1988). The thermodynamics and fluid dynamics of eruption columns. Bulletin Volcanologique 50, 169–191.CrossRefGoogle Scholar
Woods, A. W., and Kienle, J. (in press). The dynamics and thermodynamics of volcanic clouds: Theory and observations from the April 15 and April 21, 1990 eruptions of Redoubt, Alaska. Journal of Volca-nology and Geothermat Research. Google Scholar
Woods, A. W. M., and Wohletz, K. H. (1991). Dimensions and dynamics of co-ignimbrite eruption columns. Nature 350, 225–227.CrossRefGoogle Scholar