Sequence of events during the last deglaciation in Southern Ocean sediments and Antarctic ice cores

Paleoceanography

Volumn 17, Issue 4, 2002, Pages 8-1-8-7

  Shemesh, A ^a   Hodell, D ^b   Crosta, X ^a   Kanfoush, S ^b,c   Charles, C ^d   Guilderson, T ^e  

^a WEIZMANN INSTITUTE OF SCIENCE   (Israel)

^b UNIVERSITY OF FLORIDA   (United States)

^c UTICA COLLEGE   (United States)

^d UNIVERSITY OF CALIFORNIA   (United States)

^e LAWRENCE LIVERMORE NATIONAL LABORATORY   (United States)

Author keywords

Biogenic opal; Diatoms; IRD; Last glacial; Southern ocean; Stable isotopes

Indexed keywords

BIOGENIC MATERIAL; ICE CORE; LAST DEGLACIATION; MARINE SEDIMENT; PALEOCEANOGRAPHY; SEDIMENT CORE;

ANTARCTICA; SOUTHERN OCEAN;

BACILLARIOPHYTA; FORAMINIFERA;

EID: 0011709054     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/2000pa000599     Document Type: Article

References (35)

1. Altabet, M. A., and R. Francois, Sedimentary nitrogen isotopic ratio as a recorder for surface ocean nitrate utilization, Global Biogeochem. Cycles, 8(1), 103-116, 1994.
2. Bard, E., M. Arnold, B. Hamelin, N. Tisnerat-Laborde, and G. Cabioch, Radiocarbon calibration by means of mass spectrometric Th- 230/U-234 and C-14 ages of corals: An updates database including samples from Barbados, Mururoa and Tahiti, Radiocarbon, 40(3), 1085-1092, 1998.
3. 2 change: Organic carbon isotope evidences, Global Planet. Change, 16, 25-36, 1998.
4. Blunier, T., et al., Asynchrony of Antarctic and Greenland climate change during the last glacial period, Nature, 394, 739-743, 1998.
5. Broecker, W. S., Ocean chemistry during glacial time, Geochim. Cosmochim. Acta, 46, 1689-1705, 1982.
6. 2 changes, Paleoceanography, 13(4), 352-364, 1998.
7. Burckle, L. H., Diatom distribution and paleoceanographic reconstruction in the Southern Ocean Present and Last Glacial Maximum, Mar. Micropaleontol., 9, 241-261, 1984.
8. Charles, C. D., J. Lynch-Stieglitz, U. S. Ninnemann, and R. G. Fairbanks, Climate connections between the hemispheres revealed by deep sea sediment core/ice core correlation, Earth Planet. Sci. Lett., 142, 19-27, 1996.
9. Crosta, X., J. J. Pichon, and L. H. Burckle, Application of modern analog technique to marine Antarctic diatoms: Reconstruction of the maximum sea ice extent at the Last Glacial Maximum, Paleoceanography, 13(3), 284-297, 1998.
10. Elderfield, H., and R. E. M. Rickaby, Oceanic Cd/P ratio and nutrient utilization in the glacial Southern Ocean, Nature, 405, 305-310, 2000.
11. 2 around the last three glacial terminations, Science, 283, 1712-1714, 1999.
12. 2 concentrations during the last glacial period, Nature, 389, 929-935, 1997.
13. Gersonde, R., and G. Wefer, Sedimentation of biogenic siliceous particles in Antarctic waters from the Atlantic sector, Mar. Micropaleontol., 11, 311-332, 1987.
14. 2 concentration, pH, temperature, and species, Global Biogeochem. Cycles, 8(1), 91-102, 1994.
15. Jouzel, J., et al., The 2-step shape and timing of the last deglaciation in Antarctica, Clim. Dyn., 11, 151-161, 1995.
16. Juillet-Leclere, A., and L. Labeyrie, Temperature dependence of the oxygen isotopic fractionation between diatom silica and water, Earth Planet. Sci. Lett., 84, 69-74, 1987.
17. Kanfoush, S. L., et al., Millennial-scale instability of the Antarctic ice sheet during the last glaciation, Science, 288, 1815-1819, 2000.
18. Labeyrie, L. D., et al., Melting history of Antarctica during the past 60,000 years, Nature, 1986.
19. Labracherie, M., L. D. Labeyrie, and J. E. A. Duprat, The last deglaciation in the Southern Ocean, Paleoceanography, 4, 629-638, 1989.
20. 2 change: The iron hypothesis, Paleoceanography, 5, 1-13, 1990.
21. 2, Global Biogeochem. Cycles, 14(1), 455-475, 2000.
22. Ninnemann, U. S., C. D. Charles, and D. A. Hodell, Origin of global millenial scale climate events: Constraints from the Southern Ocean deep sea sedimentary record, in Mechanisms of Global Climate Change at Millenial Time Scales, Geophys. Monogr. Ser., vol. 112, edited by P. U. Clark, R. S. Webb, and L. D. Keigwin, pp. 99-112, AGU, Washington, D.C., 1999.
23. Petit, J. R., et al., Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica, Nature, 399, 429-436, 1999.
24. Popp, B. N., et al., Effect of phytoplankton cell geometry on carbon isotopic fractionation, Geochim. Cosmochim. Acta, 62(1), 69-77, 1998.
25. 2 as inferred from carbon isotopes in diatoms, Paleoceanography, 15(1), 65-75, 2000.
26. Shemesh, A., L. H. Burckle, and J. D. Hays, Meltwater input to the Southern Ocean during the Last Glacial Maximum, Science, 266, 1542-1544, 1994.
27. Shemesh, A., C. D. Charles, and R. G. Fairbanks, Oxygen isotopes in biogenic silica: Global changes in ocean temperature and isotopic composition, Science, 256, 1434-1436, 1992.
28. Shemesh, A., S. A. Macko, C. D. Charles, and G. H. Rau, Isotopic evidence for reduced productivity in the glacial Southern Ocean, Science, 262, 407-410, 1993.
29. Sigman, D. M., M. A. Altabet, R. Francois, D. C. McCorkle, and J. F. Gaillard, The isotopic composition of diatom-bound nitrogen in the Southern Ocean sediments, Paleoceanography, 14(2), 118-134, 1999.
30. Singer, A. J., and A. Shemesh, Climatically linked carbon isotope variation during the past 430,000 years in Southern Ocean sediments, Paleoceanography, 10(2), 171-177, 1995.
31. Sowers, T., and M. Bender, Climate records covering the last deglaciation, Science, 269, 210-214, 1995.
32. 2 variations, Nature, 404, 171-174, 2000.
33. Stuiver, M., P. J. Reimer, and T. F. Braziunas, High-precision radiocarbon age calibration for terrestrial and marine samples, Radiocarbon, 40(3), 1127-1151, 1998.
34. 2 by ventilation of the ocean's deepest water, Paleoceanography, 14(5), 571-588, 1999.
35. Zielinski, U., R. Gersonde, R. Sieger, and D. Futterer, Quaternary surface water temperature estimations: Calibration of diatom transfer function for the Southern Ocean, Paleoceanography, 13(4), 365-383, 1998.