Abstract
Oxygen and carbon isotope analyses of planktonic and benthic foraminifera from five Norwegian Sea sediment cores demonstrate that the Norwegian Sea was an active area of deep water formation not only during full interglacial conditions (isotopic stages 1 and 5e) but also during the early part of the glaciation (isotope stages 4 and 5a–5d).
As sinking of surface water to the depth is linked to its cooling during winter, the Norwegian Sea deep water temperature was close to the freezing point during the time intervals 0–8 kyr B.P. and 65–128 kyr B.P.. Consequently the oxygen isotope record of this period is a record of the global sea water ∂18O variations due to the growth and decay of continental ice sheets.
A complete record of the global sea water ∂18O variations during the last climatic cycle has been established by piecing the stacked Norwegian Sea benthic record of stages 1, 4, and 5 with the benthic record of Pacific core V 19–30 for glacial stages 2 and 3. The resulting record may be used to extract either the temperature signal present in benthic records from other oceanic basins or the variations in surface hydrology recorded by the oxygen isotope variations of planktonic foraminifera.
C.F.R. Contribution N° 870.
Preview
Unable to display preview. Download preview PDF.
References
Bard, E., M. Arnold, J. Duprat, J. Moyes, and J.C. Duplessy, Reconstruction of the last deglaciation: Deconvolved records of ∂180 profiles, micropaleontological variations and accelerator mass spectrometric 14C dating, Climate Dynamics, 1, 101–112, 1987.
Belanger, P.E., Paleo-oceanography of the Norwegian Sea during the past 130,000 years: coccolithophorid and foraminiferal data, Boreas, 11, 29–36, 1982.
Belanger, P.E., and S.S. Streeter, Distribution and ecology of benthic foraminifera in the Norwegian-Greenland sea, Mar. Micropal, 5, 401–428, 1980.
Blanc, P.L. and J.C. Duplessy, The deep water circulation during the Neogene and the impact of the Messinian salinity crisis, Deep Sea Res., 29, 1391–1414, 1983.
Boyle, E.A. and L.D. Keigwin, Deep circulation of the North Atlantic over the last 200,000 years: Geochemical evidence, Science, 218, 784–787, 1982.
Chappell J. and N.J. Shackleton, Oxygen isotopes and sea level, Nature, 324, 137–140, 1986
Dodge, E.D., R.G. Fairbanks, L.K. Benninger, and F. Maurasse, Pleistocene sea level from raised coral reefs of Haiti, Science, 219, 1423–1425, 1983.
Duplessy, J.C., Isotope studies, in Climatic Change, edited by J. Gribbin, Cambridge University Press, Cambridge, 46–67, 1978.
Duplessy, J.C., Circulation des eaux profondes nord atlantiques au cours du dernier cycle climatique, Bull. Inst. Géol. Bassin d'Aquitaine, 31, 379–391, 1982.
Duplessy, J.C., C. Lalou, and A.C. Vinot, Differential isotopic fractionation in benthic foraminifera and paleotemperature reassessed, Science, 168, 250–251, 1970.
Duplessy, J.C., L. Chenouard, and F. Vila, Weyl's theory of glaciation supported by isotopic study of Norwegian core K-11, Science, 188, 1208–1209, 1975.
Duplessy, J.C., J. Moyes and C. Pujol, Deep water formation in the North Atlantic Ocean during the last ice age, Nature, 286, 479–482, 1980.
Duplessy, J.C., G. Delibrias, J.L. Turon, C. Pujol, and J. Duprat, Deglacial warming of the northeastern Atlantic ocean: correlation with the paleoclimatic evolution of the european continent, Palaeogeogr., Palaeoclimat., Palaeoecol., 35, 121–144, 1980.
Duplessy, J.C. and N.J. Shackleton, Response of global deep-water circulation to the Earth's climatic change 135,000–107,000 years ago, Nature, 316, 500–507, 1985.
Duplessy, J.C., M. Arnold, P. Maurice, E. Bard, J. Duprat and J. Moyes, Direct dating of oxygen-isotope record of the last deglaciation by C-14 accelerator mass spectrometry, Nature, 320, 350–352, 1986.
Duplessy, J.C., N.J. Shackleton, R.K. Matthews, W. Prell, W.F. Ruddiman, M. Caralp, and C.H. Hendy, 13C record of benthic foraminifera in the last interglacial ocean: Implications for the carbon cycle and the global deep water circulation, Quat. Res., 21, 225–243, 1984.
Duplessy, J.C., N. J. Shackleton, R. Fairbanks, L. Labeyrie, D. Oppo and N. Kallel, Deep water source variations during the last climatic cycle and their impact of the global deep water circulation, Paleoceanography (submitted), 1987.
Emiliani, C., Pleistocene Temperatures, J. Geol., 63, 538–578, 1955.
Holtedahl, H., Geology and paleontology of Norwegian sea bottom cores, J. Sed. Petrol., 29, 16–29, 1959.
Imbrie, J., J.D. Hays, D.G. Martinson, A. Mc Intyre, A. Mix, J. J. Morley, N. Pisias, W. Prell, and N.J. Shackleton, The orbital theory of Pleistocene climate: Support from a revised chronology of the late marine ∂180 record, in Milankovitch and Climate edited by A. Berger et al., D. Reidel, Hingam, Mass., 1984
Jansen, E., H.P. Sejrup, T. Fjaeran, M. Hald, H. Holtedahl and O. Skarbo, Late Weichselian paleoceanography of the southeastern Norwegian Sea, Norsk Geologisk Tidsskrift, 63, 117–146, 1983
Kellogg, T.B., Late Quaternary climatic changes: evidence from cores from Norwegian and Greenland Seas, Geol. Soc. Am. Memoir, 145, 77–110, 1976.
Kellogg, T.B., Paleoclimatology and paleo-oceanography of the Norwegian and Greenland seas: Glacial-interglacial contrasts, Boreas, 9, 115–137, 1980.
Kellogg, T.B., N.J. Shackleton, and J.C. Duplessy, Planktonic foraminiferal and oxygen isotopic stratigraphy and paleoclimatology of Norwegian sea deep sea cores, Boreas, 7, 61–73, 1978.
Labeyrie, L.D. and J.C. Duplessy, Changes in the oceanic C13/C12 ratio during the last 140,000 years: high latitude surface water records, Palaeogeogr., Palaeoclimatol., Palaeoecol., 50, 217–240, 1985.
Labeyrie, L. D., J.C. Duplessy, and P.L. Blanc, Deep water formation and temperature variations over the last 125,000 years, Nature, 327, 477–482, 1987.
Mackensen, A., H.P. Sejrup, and E. Jansen, The distribution of living benthic foraminifera on the continental slope and rise off southwest Norway, Mar. Micropal., 9, 275–306, 1985.
Mix, A. and R.G. Fairbanks, North Atlantic surface-ocean control of Pleistocene deep ocean circulation, Earth Planet. Sci. Lett., 73, 231–243, 1985.
Paterne, M., F. Guichard, J. Labeyrie, P.Y. Gillot and J.C. Duplessy, Tyrrhenian sea tephrochronology of the oxygen-isotope record for the past 60,000 years, Mar. Geol., 72, 259–285, 1986.
Reid, J.L. and R.L. Lynn, On the influence of the Norwegian-Greenland and Weddell seas upon the bottom waters of the Indian and Pacific oceans, Deep Sea Res., 18, 1063–1088, 1971.
Sarnthein, M., H. Erlenkeuser, R. von Grafenstein, and C. Schroeder, Stable-isotope stratigraphy for the last 750,000 years: "Meteor" core 13519 from the eastern equatorial Atlantic, Meteor Forschungergebnisse, Reihe C, 38, 9–24, 1984.
Savitzky, A. and J. E. Golay, Smoothing and differenciation of data by simplified least squares procedure, Anal. Chem., 36, 1627–1639, 1964.
Sejrup, H.P., E. Jansen, H. Herlenkeuser, and H. Holtedahl, New faunal and isotopic evidence of the late Weichselian-Holocene oceanographic changes in the Norwegian Sea, Quat. Res., 21, 74–84, 1984.
Shackleton, N.J., Attainment of isotopic equilibrium between ocean water and the benthonic foraminifer genus Uvigerina: isotopic changes in the ocean during the last glacial, Colloque International du Centre National de la Recherche Scientifique, N° 219, 203–210, 1974.
Shackleton, N.J., Carbon-13 in Uvigerina: Tropical rainforest history and the equatorial Pacific carbonate dissolution cycle, in The Fate of fossil fuel CO2 in the Oceans, edited by N. R. Anderson and A. Malahoff, pp 401–428, Plenum, New York, 1977.
Shackleton, N.J., and M.B. Cita, Oxygen and carbon isotope stratigraphy of benthic foraminifera at site 397: Detailed history of climatic change during the late Neogene, Initial Reports of the Deep Sea Drilling Project, 47, 433–445, 1979.
Shackleton, N.J., J. Imbrie, and M. Hall, Oxygen and Carbon isotope record of east Pacific core V 19–30: Implications for the formation of deep water in the Late Pleistocene North Atlantic, Earth and Planet. Sci. Lett., 65, 233–244, 1983.
Shackleton, N.J. and N. D. Opdyke, Oxygen isotope and paleomagnetic stratigraphy of equatorial Pacific core V28-238: Oxygen isotope temperatures and ice-volumes on a 105 year and a 106 year scale, Quat. Res., 3, 39–55, 1973.
Streeter, S.S., P.E. Belanger, T.B. Kellogg, and J.C. Duplessy, Late Pleistocene paleo-oceanography of the Norwegian-Greenland Sea: Benthic foraminiferal evidence, Quat. Res., 18, 72–90, 1982.
Zahn, R., K. Winn, and M. Sarnthein, Benthic foraminiferal ∂13C and accumulation rates of organic carbon: Uvigerina peregrina group and Cibicidoides wuellerstorfi, Paleoceanography, 1, 27–42, 1986.
Author information
Authors and Affiliations
Editor information
Rights and permissions
Copyright information
© 1988 Springer-Verlag
About this paper
Cite this paper
Duplessy, J.C., Labeyrie, L., Blanc, P.L. (1988). Norwegian sea deep water variations over the last climatic cycle: Paleo-oceanographical implications. In: Wanner, H., Siegenthaler, U. (eds) Long and Short Term Variability of Climate. Lecture Notes in Earth Sciences, vol 16. Springer, Berlin, Heidelberg. https://doi.org/10.1007/BFb0046591
Download citation
DOI: https://doi.org/10.1007/BFb0046591
Published:
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-18843-8
Online ISBN: 978-3-540-38836-4
eBook Packages: Springer Book Archive