Rapid transient changes in northeast Atlantic deep water ventilation age across Termination I

Paleoceanography

Volumn 19, Issue 2, 2004, Pages

  Skinner, L C ^a   Shackleton, N J ^a  

^a UNIVERSITY OF CAMBRIDGE   (United Kingdom)

Author keywords

Termination I; Thermohaline circulation; Ventilation age

Indexed keywords

CLIMATE CHANGE; DEEP WATER; FORAMINIFERA; LAST DEGLACIATION; PALEOCEANOGRAPHY; PALEOCLIMATE; QUATERNARY; RADIOCARBON DATING; THERMOHALINE CIRCULATION; VENTILATION;

ATLANTIC OCEAN; ATLANTIC OCEAN (NORTHEAST);

FORAMINIFERA;

EID: 4544270903     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/2003PA000983     Document Type: Article

References (54)

1. 14C and the record of deep water paleoventilation ages, Paleoceanography, 12(3), 337-344.
2. Adkins, J. F., H. Cheng, E. A. Boyle, E. R. M. Druffel, and R. L. Edwards (1998), Deep-sea coral evidence for rapid change in ventilation of the deep North Atlantic 15,400 years ago, Science, 280, 725-728.
3. 14C ages measured in planktonic foraminifera: Paleoceanographic implications, Paleoceanography, 3(6), 635-645.
4. 14C dating, Clim. Dyn., 1, 101-112.
5. 14 C accelerator mass spectrometry, Nature, 328, 791-794.
6. 14C time-scale over the past 30,000 years using mass spectrometric U-Th ages from Barbados corals, Nature, 345, 405-409.
7. 14C gradient during the Younger Dryas climatic event, Earth Planet. Sci. Lett., 126, 275-287.
8. 14C ages of corals: An updated database including samples from Barbados, Mururoa and Tahiti, Radiocarbon, 40(3), 1085-1092.
9. 14C concentration during the last glacial period, Science, 292, 2453-2458.
10. Bjorck, S., N. Koc, and G. Skog (2003), Consistently large marine reservoir ages in the Norwegian Sea during the Last Deglaciation, Quat. Sci. Rev., 22, 429-435.
11. Boyle, E. A. (2000), Is ocean circulation linked to abrupt stadial/interstadial transitions?, Quat. Sci. Rev., 19, 255-272.
12. Boyle, E. A., and L. D. Keigwin (1987), North Atlantic thermohaline circulation during the last 20,000 years linked to high latitude surface temperature, Nature, 330, 35-40.
13. Broecker, W. S. (1998), Palaeocean circulation during the last deglaciation: A bipolar seesaw?, Paleoceanography, 13, 119-121.
14. Broecker, W. S., and T. H. Peng (1982), Tracers in the Sea, 690 pp., Lahmont-Doherty Earth Observ., Palisades, N. Y.
15. Broecker, W. S., A. Mix, M. Andree, and H. Oeschger (1984), Radiocarbon measurements on coexisting benthic and planktonic foraminifera shells: Potential for reconstructing ocean ventilation times over the past 20,000 years, Nucl. Instrum. Methods Phys. Res. Sect. B, 5, 331-339.
16. Broecker, W. S., T. H. Peng, S. Trumbore, G. Bonani, and W. Wolfli (1990), The distribution of radiocarbon in the glacial ocean, Global Biogeochem. Cycles, 4, 103-117.
17. Charles, C. D., J. Lynch-Stieglitz, U. S. Ninneman, and R. G. Fairbanks (1996), Climate connections between the hemispheres revealed by deep sea sediment core/ice core correlations, Earth Planet. Sci. Lett., 142, 19-42.
18. Clark, P. U., J. X. Mitrovica, G. A. Milne, and M. E. Tamisca (2002a), Sea-level fingerprinting as a direct test for the source of global meltwater pulse IA, Science, 295, 2438-2441.
19. Clark, P. U., N. G. Pisias, T. F. Stocker, and A. J. Weavers (2002b), The role of the thermohaline circulation in abrupt climate change, Nature, 415, 863-869.
20. 2 between the last glaciation and the Holocene, Paleoceanography, 3(3), 317-341.
21. Delaygue, G., T. F. Stocker, F. Joos, and G.-K. Plattner (2003), Simulation of atmospheric radiocarbon during abrupt oceanic circulation changes: Trying to reconcile models and reconstructions, Quat. Sci. Rev., 22, 1647-1658.
22. Duplessy, J.-C., N. J. Shackleton, R. G. Fairbanks, L. Labeyrie, D. Oppo, and N. Kallel (1988), Deep water source variations during the last climatic cycle and their impact on global deep water circulation, Paleoceanography, 3, 343-360.
23. Ganachaud, A., and C. Wunsch (2000), Improved estimates of global ocean circulation, heat transport and mixing from hydrographic data, Nature, 408, 453-457.
24. Goldstein, S. J., D. W. Lea, S. Chakraborty, M. Kashgarian, and M. T. Murrell (2001), Uranium-series and radiocarbon geochronology of deep-sea corals: Implications for Southern Ocean ventilation rates and the oceanic carbon cycle, Earth Planet. Sci. Lett., 193, 167-182.
25. 5-year time resolution, J. Geophys. Res., 102, 26,455-26,470.
26. Hanebuth, T., K. Stattegger, and P. M. Grootes (2000), Rapid flooding of the Sunda Shelf: A late-glacial sea-level record, Science, 288, 1033-1035.
27. Hughen, K., J. T. Overpeck, S. J. Lehman, M. Kashgarian, J. Southon, L. C. Peterson, R. Alley, and D. M. Sigman (1998a), Deglacial changes in ocean circulation from an extended radiocarbon calibration, Nature, 391, 65-68.
28. 14C calibration data set for the last deglaciation based on marine varves, Radiocarbon, 40(1), 483-494.
29. Hughen, K., J. R. Southon, S. J. Lehmann, and J. T. Overpeck (2000), Synchronous radiocarbon and climate shifts during the last deglaciation, Science, 290, 1951-1954.
30. 14C activity and global carbon cycle changes over the past 50,000 years, Science, 33, 22-27.
31. 16O ice core records and North Atlantic foraminifera profiles: A comparison with U/Th coral data, Radiocarbon, 40(1), 495-504.
32. Kienast, M., T. J. J. Hanebuth, C. Pelejero, and S. Steinke (2003), Synchroneity of meltwater pulse 1a and the Bolling-Allerod warming: New evidence from the South China Sea, Geology, 31(1), 67-70.
33. Kitagawa, H., and J. van der Plicht (2000), Atmospheric radiocarbon calibration beyond 11,900 cal BP from Lake Suigetsu sediments, Radiocarbon, 42(3), 369-380.
34. Knorr, G., and G. Lohmann (2003), Southern Ocean origin for the resumption of Atlantic thermohaline circulation during deglaciation, Nature, 424, 532-536.
35. 14C during the last 50 kyr, Earth Planet. Sci. Lett., 200, 177-190.
36. Meese, D. A., A. J. Gow, R. B. Alley, G. A. Zielinski, P. M. Grootes, M. Ram, K. C. Taylor, P. A. Mayewski, and J. F. Bolzan (1997), The Greenland Ice Sheet Project 2 depth-age scale: Methods and results, J. Geophys. Res., 102, 26,411-26,423.
37. 14C content of marine shells: Evidence for variability in coastal upwelling off Portugal during the Holocene, Isotope techniques in the study of past and current environmental changes in the hydrosphere and the atmosphere, Int. Atom. Energy Ag., Vienna.
38. 14C records, Nature, 408, 567-570.
39. 14C records, Nature, 408, 567-570.
40. Schroder-Ritzrau, A., A. Mangini, and M. Lomitschka (2003), Deep-sea corals evidence periodic reduced ventilation in the North Atlantic during the LGM/Holocene transition, Earth Planet. Sci. Lett., 216, 399-410.
41. Shackleton, N. J., J.-C. Duplessy, M. Arnold, P. Maurice, M. A. Hall, and J. Cartlidge (1988), Radiocarbon age of last glacial Pacific deep water, Nature, 335(6192), 708-711.
42. Shackleton, N. J., M. A. Hall, and E. Vincent (2000), Phase relationships between millennial-scale events 64,000-24,000 years ago, Paleoceanography, 15(6), 565-569.
43. Siani, G., M. Paterne, E. Michel, R. Sulpizio, A. Sbrana, M. Arnold, and G. Haddad (2001), Mediterranean sea surface radiocarbon reservoir age changes since the last glacial maximum, Science, 294, 1917-1920.
44. Sikes, E. L., C. R. Samson, T. P. Guilderson, and W. R. Howard (2000), Old radiocarbon ages in the southwest Pacific Ocean during the last glacial period and deglaciation, Nature, 405, 555-559.
45. dw indicating deep-water source variations in the northeast Atlantic, 0-34 cal ka BP, Geochem. Geophys. Geosyst., 4(12), 1098, doi:10.1029/2003GC000585.
46. Stocker, T. F., and D. G. Wright (1996), Rapid changes in ocean circulation and atmospheric radiocarbon, Paleoceanography, 11(6), 773-795.
47. 14C, Radiocarbon, 40(1), 359-366.
48. Stocker, T. F., D. G. Wright, and W. S. Broecker (1992), The influence of high latitude surface forcing on the global thermohaline circulation, Paleoceanography, 7, 529-542.
49. Stuiver, M., and H. G. Ostlund (1980), GEOSECS Atlantic radiocarbon, Radiocarbon, 22(1), 1-24.
50. Stuiver, M., P. J. Reimer, and T. F. Braziunas (1998), High-precision radiocarbon age calibration for terrestrial and marine samples, Radiocarbon, 40(3), 1127-1151.
51. Voelker, A. H. L., P. M. Grootes, M.-J. Nadeau, and M. Sarnthein (2000), Radiocarbon levels in the Iceland Sea from 25-53 kyr and their links to the Earth's magnetic field intensity, Radiocarbon, 42(3), 437-452.
52. Waelbroeck, C., J.-C. Duplessy, E. Michel, L. Labeyrie, D. Paillard, and J. Duprat (2001), The timing of the last deglaciation in North Atlantic climate records, Nature, 412, 724-727.
53. Weaver, A. J., O. A. Saenko, P. U. Clark, and J. X. Mitrovica (2003), Meltwater pulse 1A from Antarctica as a trigger for the Bolling-Allerod warm interval, Science, 299, 1709-1713.
54. Wunsch, C. (2003), Determining paleoceanographic circulations, with emphasis on the Last Glacial Maximum, Quat. Sci. Rev., 22, 371-385.