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Oxygen-Isotope Analyses and Pleistocene Ice Volumes1

Published online by Cambridge University Press:  20 January 2017

Alan C. Mix  and
William F. Ruddiman
Alan C. Mix
Affiliation:
Lamont-Doherty Geological Observatory, Palisades, New York 10964 USA, and Department of Geological Sciences, Columbia University, New York, New York 10027
William F. Ruddiman
Affiliation:
Lamont-Doherty Geological Observatory, Palisades, New York 10964 USA, and Department of Geological Sciences, Columbia University, New York, New York 10027
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Abstract

The oxygen-isotope record from fossil foraminifera in deep-sea sediments is commonly used as a proxy for global ice volume. The linkage between δ18O and ice volume, however, is probably nonlinear. We have developed a simple numerical model of the isotopic response of the oceans to ice-volume change. The major features it simulates are (1) the changing mean isotopic composition of snow as a function of ice volume (colder snow temperatures forced by climate change and higher-elevation accumulation areas imply more negative mean δ18O); (2) the nonequilibrium isotopic composition of ice sheets (the past history of an ice sheet is integrated into its mean isotopic composition, which introduces a lag of isotopic “ice volume,” i.e., the measured δ18O record, scaled to ice-volume units, behind true ice volume); (3) selective preservation of isotopically more negative (colder, higher-latitude) ice (this geographic effect can selectively amplify or dampen the isotopic response to the ice-volume signal). We illustrate the response of our model to simple hypothetical ice-volume transitions of ice growth and ice decay. Sensitivity tests are illustrated for all model parameters. The results suggest that oxygen-isotope records reproduce the general patterns of ice-volume change fairly accurately. The foraminiferal isotope record, however, may misrepresent the true amplitude of the ice-volume signal and lag true ice volume by 1000 to 3000 yr.

Type
Research Article
Information
Quaternary Research , Volume 21 , Issue 1 , January 1984 , pp. 1 - 20
Copyright
University of Washington

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Footnotes

Lamont-Doherty Geological Observatory Contribution No. 3517.

References

Andrews, J.T., Mahaffy, M.A. (1976). Growth rates of the Laurentide Ice Sheet and sea-level lowering (with emphasis on the 115,000 B.P. sea-level low) Quaternary Research 6, 167–183 CrossRefGoogle Scholar
Barkov, N.I., Gordienko, F.G., Korotkevich, E.S., Kotlyakov, V.M. (1977). The isotopic analysis of ice cores from Vostok Station (Antarctica), to the depth of 950 meters Isotopes and Impurities in Snow and Ice. Proceedings of the Grenoble Symposium August, 1975 I.A.H.S. Publication No. 118 382–387 Google Scholar
Berger, A.L. (1978). Long-term variations of caloric insolation resulting from the earth's orbital elements Quaternary Research 9, 139–167 CrossRefGoogle Scholar
Birchfield, G.E., Weertman, J. (1978). A note on the spectral response of a model continental ice sheet Journal of Geophysical Research 83, No. C-8 4123–4125 CrossRefGoogle Scholar
Birchfield, G.E., Weertman, J., Lunde, A.T. (1981). A paleoclimate model of northern hemisphere ice sheets Quaternary Research 15, 126–142 CrossRefGoogle Scholar
Bloom, A.L., Broecker, W.S., Chappell, J.M.A., Matthews, R.K., Mesolella, K.J. (1974). Quaternary sea level fluctuations on a tectonic coast: New 230Th/234U dates from the Huon Peninsula, New Guinea Quaternary Research 4, 185–205 Google Scholar
Boulton, G.S. (1979). A model of Weichselian glacier variation in the North Atlantic region Boreas 8, 373–395 CrossRefGoogle Scholar
Brinkman, W.A.R., Barry, R.G. (1972). Palaeoclimatological aspects of the synoptic climatology of Keewatin, Northwest Territories, Canada Palaeogeography, Palaeoclimatology, and Palaeoecology 11, 77–91 CrossRefGoogle Scholar
Broecker, W.S. (1975). Floating glacial ice caps in the Arctic Ocean Science 188, 1116–1118 CrossRefGoogle ScholarPubMed
Broecker, W.S. (1978). The cause of glacial to interglacial climatic change Evolution of Planetary Atmospheres and Climatology of the Earth Centre National d'Etudes Spatales Nice, France 165–177 Google Scholar
Buchardt, B., Fritz, P. (1980). Environmental isotopes as environmental and climatological indicators Fritz, P., Fontes, J.Ch., Handbook of Environmental Isotope Geochemistry Vol. 1, Elsevier Amsterdam 473–504 “The Terrestrial Environment, A”Google Scholar
Budd, W.F. (1981). The importance of ice sheets in long term changes of climate and sea level Sea Level, Ice, and Climatic Change, Proceedings of the Canberra Symposium December, 1979 I.A.H.S. Publication No. 131 441–471 Google Scholar
Budd, W.F., Smith, I.N. (1981). The growth and retreat of ice sheets in response to orbital radiation changes Sea Level, Ice, and Climatic Change. Proceedings of the Canberra Symposium December, 1979 I.A.H.S. Publication No. 131 369–409 Google Scholar
Calder, N. (1974). Arithmetic of ice ages Nature (London) 252, 216–218 CrossRefGoogle Scholar
Chappell, J. (1974). Relationships between sea levels, 18O variations, and orbital perturbations, during the past 250,000 years Nature (London) 252, 199–202 CrossRefGoogle Scholar
Clausen, H.B., Dansgaard, W., Nielsen, J.O., Clough, J.W. (1979). Surface accumulation on Ross Ice Shelf Antarctic Journal of the United States 14, 5 68–72 Google Scholar
Craig, H. (1965). The measurement of oxygen isotope paleotemperatures Tongiorgi, E., Stable Isotopes in Oceanic Studies and Paleotemperatures. Third SPOLETO Conference on Nuclear Geology Consiglio Nazionale della Ricerche, Laboratorio di Geologia Nucleare Pisa 161–182 Google Scholar
Curray, J.R. (1965). Late Quaternary history, continental shelves of the United States Wright, H.E., Frey, D.C., The Quaternary of the United States Princeton Univ. Press Princeton, N.J 723–735 Google Scholar
Dansgaard, W. (1964). Stable isotopes in precipitation Tellus 16, 436–468 Google Scholar
Dansgaard, W., Johnsen, S.J., Clausen, H.B., Gundestrup, N. (1973). Stable isotope glaciology Meddelelser om Groenland 197, 1–53 Google Scholar
Dansgaard, W., Tauber, H. (1969). Glacier oxygen-18 content and Pleistocene ocean temperatures Science 166, 499–502 Google Scholar
Denton, G.H., Hughes, T.J. (1981). The Last Great Ice Sheets Wiley New York Google Scholar
Dillon, W.P., Oldale, R.N. (1978). Late Quaternary sea-level curve: Reinterpretation based on glaciotectonic influence Geology 6, 56–60 Google Scholar
Dodge, R.E., Fairbanks, R.G., Benninger, L.K., Maurasse, F. (1983). Pleistocene sea levels from raised coral reets of Haiti Science 219, 1423–1425 CrossRefGoogle Scholar
Duplessy, J.-C., Moyes, J., Pujol, C. (1980). Deep water formation in the North Atlantic Ocean during the last ice age Nature (London) 286, 479–482 CrossRefGoogle Scholar
Emiliani, C. (1955). Pleistocene temperatures Journal of Geology 63, 538–578 Google Scholar
Epstein, S., Buchsbaum, H.A., Lowenstam, H.A., Urey, H.C. (1953). Revised carbonate-water isotopic temperature scale Geological Society of America Bulletin 64, 1315–1325 CrossRefGoogle Scholar
Eriksson, E. (1968). Air-ocean-icecap interactions in relation to climatic fluctuations and glaciation cycles Meteorological Monographs 8, no. 30 68–92 Google Scholar
Ewing, M., Donn, W.L. (1956). A theory of ice ages Science 123, 1061–1066 Google Scholar
Fairbanks, R.G., Matthews, R.K. (1978). The marine oxygen isotope record in Pleistocene coral, Barbados, West Indices Quaternary Research 10, 181–196 Google Scholar
Flint, R.F. (1943). Growth of the North American Ice Sheet during the Wisconsin age Geological Society of America Bulletin 54, 325–362 Google Scholar
Flint, R.F. (1971). Glacial and Quaternary Geology Wiley New York Google Scholar
Flohn, H.H. (1974). Background of a geophysical model of the initiation of the next glaciation Quaternary Research 4, 385–404 CrossRefGoogle Scholar
Fritz, P., Anderson, T.W., Lewis, Cf.M. (1975). Late-Quaternary climatic trends and history of Lake Erie from stable isotope studies Science 190, 267–269 Google Scholar
Hanshaw, B.B., Winograd, I.J., Pearson, F.J. Jr. (1980). Stable isotope studies of subglacially precipitated carbonates and of ancient ground water: Paleoclimatic implications Jacoby, G.C., Proceedings of the International Meeting on Stable Isotopes in Tree-Ring Research United States Department of Energy 102–104 Google Scholar
Harmon, R.S., Schwarez, H.P. (1981). Changes of 2H and 18O enrichment of meteoric water and Pleistocene glaciation Nature (London) 290, 125–128 CrossRefGoogle Scholar
Hays, J.D. (1978). A review of the Late Quaternary climatic history of Antaretic seas van Zinderen Bakker, E.M., Antarctic Glacial History and World Palaeoenvironments Balkena Rotterdam 57–71 Google Scholar
Hays, J.D., Imbrie, J., Shackleton, N.J. (1976). Variations in the Earth's orbit: Pacemaker of the ice ages Science 194, 1121–1132 CrossRefGoogle ScholarPubMed
Hillaire-Marcel, C. (1981). Paleo-oceanographie isotopique des mers post-glaciaires du Quebec Palaeogeography, Palaeoclimatology, and Palaeoecology 35, 63–119 Google Scholar
Hillaire-Marcel, C., Soucy, J.-M., Cailleux, A. (1979). Analyse isotopique de concretions sous-glaciaires de l'indlandsis laurentidien et teneur en oxygene 18 de la glace Canadian Journal of Earth Sciences 16, 1494–1498 CrossRefGoogle Scholar
Hooke, R.LeB., Clausen, H. (1982). Wisconsin and Holocene δ18O variations, Barnes Ice Cap, Canada Geological Society of America Bulletin 93, 784–789 Google Scholar
Imbrie, J., Imbrie, J.Z. (1980). Modeling the climatic response to orbital variations Science 207, 943–953 Google Scholar
International Atomic Energy Agency (IAEA), (1981). Statistical treatment of environmental isotope data in precipitation technical report series No. 206 IAEA Vienna Google Scholar
Ives, J.D., Andrews, J.T., Barry, R.G. (1975). Growth and decay of the Laurentide Ice Sheet and comparisons with Fenno-Scandinavia Naturwissenschaften 62, 118–125 CrossRefGoogle Scholar
Kato, K., Watanabe, O., Satow, K. (1978). Oxygen isotopic composition of the surface snow in Mizuho Plateau Ishida, J., Glaciological Studies on Mizuho Plateau, East Antarctica, 1969–1975. Memoirs of the National Institute of Polar Research. 245–254 special issue No. 7, TokyoGoogle Scholar
Koerner, R.M. (1979). Accumulation, ablation, and oxygen isotope variations on the Queen Elizabeth Islands ice caps, Canada Journal of Glaciology 22, 25–41 CrossRefGoogle Scholar
Lamb, H.H., Woodroffe, A. (1970). Atmospheric circulation during the last ice age Quaternary Research 1, 29–58 Google Scholar
Loewe, F. (1971). Considerations on the origin of the Quaternary Ice Sheet of North America Arctic and Alpine Research 3, 331–344 Google Scholar
Lorius, C., Merlivat, L., Hageman, R. (1969). Variation in the mean deuterium content of precipitations in Antarctica Journal of Geophysical Research 74, no. 28 7027–7031 Google Scholar
Lorius, C., Merlivat, L., Jouzel, J., Pourchet, M. (1979). A 30,000 year isotope climatic record from Antarctic ice Nature (London) 280, 644–648 CrossRefGoogle Scholar
Mahaffy, M. (1976). A three-dimensional numerical model of ice sheets: Tests on the Barnes Ice Cap, Northwest Territories Journal of Geophysical Research 81, no. 6 1059–1066 Google Scholar
Menard, H.W., Smith, S.M. (1966). Hypsometry of ocean basin provinces Journal of Geophysical Research 71, no. 18 4305–4325 Google Scholar
Milankovitch, M. (1941). Kanon der Erdbestrahlung und seine Andwendung auf das Eiszeitproblem Royal Serbian Academy Special Publication 133, BelgradeGoogle Scholar
Milliman, J.D., Emery, K.O. (1968). Sea levels during the past 35,000 years Science 162, 1121–1123 Google Scholar
Morgan, V.I. (1982). Antarctic Ice Sheet surface oxygen isotope values Journal of Glaciology 28, 315–323 CrossRefGoogle Scholar
Moser, H., Stichler, W. (1980). Environmental isotopes in ice and snow Fritz, P., Fontes, J.Ch., Handbook of Environmental Isotope Geochemistry Vol. 1, Elsevier Amsterdam 142–178 “The Terrestrial Environment, A.”Google Scholar
Nye, J.F. (1959). The motion of ice sheets and glaciers Journal of Glaciology 3, 493–507 Google Scholar
Olausson, E. (1965). Evidence of climatic changes in North Atlantic deep-sea cores, with remarks on isotopic paleotemperature analysis Progress in Oceanography 3, 221–252 CrossRefGoogle Scholar
Olaussen, E. (1981). On the isotopic composition of late Cenozoic sea water Geografiska Annaler 63A, 3–4 Google Scholar
Paterson, W.S.B. (1972). Laurentide Ice Sheet: Estimated volumes during late Wisconsin Review of Geophysics and Space Physics 10, no. 4 885–917 Google Scholar
Paterson, W.S.B. (1981). The Physics of Glaciers Pergamon Oxford Google Scholar
Pollard, D. (1978). An investigation of the astronomical theory of ice ages using a simple climate-ice sheet model Nature (London) 272, 233–235 CrossRefGoogle Scholar
Pollard, D. (1980). A simple parameterization for ice sheet ablation rate Tellus 32, 384–388 Google Scholar
Pollard, D., Ingersoll, A.P., Lockwood, J.G. (1980). Response of a zonal climate-ice sheet model to the orbital perturbations during the Quaternary ice ages Tellus 32, 301–319 Google Scholar
Ruddiman, W.F., McIntyre, A. (1981). Oceanic mechanisms for amplification of the 23,000-year ice-volume cycle Science 212, 617–627 CrossRefGoogle ScholarPubMed
Ruddiman, W.F., McIntyre, A. (1982). Severity and speed of Northern Hemisphere glaciation pulses. The limiting case? Geological Society of America Bulletin 93, 1273–1279 2.0.CO;2>CrossRefGoogle Scholar
Ruddiman, W.F., and McIntyre, A. (in press). Ice-age thermal response and climatic role of the surface Atlantic Ocean, Geological Society of America Bulletin .Google Scholar
Shackleton, N.J. (1967a). The Measurement of Palaeotemperatures in the Quaternary Era Ph.D. thesis University of Cambridge Google Scholar
Shackleton, N.J. (1967b). Oxygen isotope analyses and Pleistocene temperatures, re-assessed Nature (London) 215, 15–17 Google Scholar
Shackleton, N.J. (1977). The oxygen isotope stratigraphic record of the late Pleistocene Philosophical Transactions Royal Society of London Series B 280, 169–182 Google Scholar
Urey, H.C. (1947). The thermodynamic properties of isotopic substances Journal of the Chemical Society 169–182 Google Scholar
Veeh, H.H., Veevers, J.J. (1970). Sea level at −175 m off the Great Barrier Reef 13,600 to 17,000 years ago Nature (London) 226, 536–537 Google Scholar
Weertman, J. (1964). Rate of growth or shrinkage of nonequilibrium ice sheets Journal of Glaciology 5, 145–158 Google Scholar
Weertman, J. (1976). Milankovitch solar radiation variation and ice age ice sheet sizes Nature 261, 17–20 Google Scholar
Weyl, P.K. (1968). The role of the oceans in climatic change: A theory of the ice ages Meteorological Monographs 8, no. 30 37–62 Google Scholar
Williams, D.F., Moore, W.S., Fillon, R.H. (1981). Role of glacial Arctic Ocean ice shelves in Pleistocene oxygen isotope and sea level records Earth and Planetary Science Letters 56, 157–166 Google Scholar
Williams, L.D. (1978). Ice-sheet initiation and climatic influence of expanded snow cover in Arctic Canada Quaternary Research 10, 141–149 Google Scholar
Williams, L.D. (1979). An energy balance model of potential glacierization of Northern Canada Arctic and Alpine Research 11, no. 4 443–456 Google Scholar
Woodruff, F., Savin, S.M., Douglas, R.G. (1981). Miocene stable isotope record: A detailed Pacific deep ocean study and its paleoclimatic implications Science 212, 665–668 CrossRefGoogle ScholarPubMed
Yapp, C.J., Epstein, S. (1977). Climatic implications of D/H ratios of meteroric water over North America (9500–22,000 B.P.) as inferred from ancient wood cellulose C-H hydrogen Earth and Planetary Science Letters 34, 333–350 Google Scholar