Southwest Atlantic water mass evolution during the last deglaciation

Paleoceanography

Volumn 30, Issue 5, 2015, Pages 477-494

  Lund, D C ^a   Tessin, A C ^b   Hoffman, J L ^b   Schmittner, A ^c  

^a UNIVERSITY OF CONNECTICUT   (United States)

^b UNIVERSITY OF MICHIGAN   (United States)

^c OREGON STATE UNIVERSITY   (United States)

Author keywords

carbon dioxide; deglaciation; South Atlantic; stable isotopes

Indexed keywords

ABYSSAL ZONE; ATMOSPHERIC CHEMISTRY; CARBON DIOXIDE; HEINRICH EVENT; LAST DEGLACIATION; OCEANIC CIRCULATION; PALEOCLIMATE; SEDIMENT CORE; WATER MASS;

ATLANTIC OCEAN; ATLANTIC OCEAN (SOUTHWEST);

EID: 84922423191     PISSN: 08838305     EISSN: 19449186     Source Type: Journal    
DOI: 10.1002/2014PA002657     Document Type: Article

References (60)

1. Adkins, J. F., K. McIntyre, and, D. P. Schrag, (2002), The salinity, temperature, and delta O-18 of the glacial deep ocean, Science, 298 (5599), 1769-1773.
2. Anderson, R. F., S. Ali, L. I. Bradtmiller, S. H. H. Nielsen, M. Q. Fleisher, B. E. Anderson, and, L. H. Burckle, (2009), Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2, Science, 323 (5920), 1443-1448.
3. Angulo, R. J., M. C. de Souza, P. J. Reimer, and, S. K. Sasaoka, (2005), Reservoir effect of the southern and southeastern Brazilian coast, Radiocarbon, 47 (1), 67-73.
4. Broecker, W. S., (1982), Ocean chemistry during glacial time, Geochim. Cosmochim. Acta, 46 (10), 1689-1705.
5. Burke, A., and, L. F. Robinson, (2012), The Southern Ocean's role in carbon exchange during the last deglaciation, Science, 335 (6068), 557-561.
6. Clark, P. U., A. S. Dyke, J. D. Shakun, A. E. Carlson, J. Clark, B. Wohlfarth, J. X. Mitrovica, S. W. Hostetler, and, A. M. McCabe, (2009), The Last Glacial Maximum, Science, 325 (5941), 710-714.
7. 2 reservoir purging signal, Quat. Sci. Rev., 30 (15-16), 1875-1882.
8. 2 in the western Atlantic Ocean, Paleoceanography, 20, PA1017, doi: 10.1029/2004PA001021.
9. 2 between the last glaciation and Holocene, Paleoceanography, 3, 317-341, doi: 10.1029/PA003i003p00317.
10. Cutler, K. B., R. L. Edwards, F. W. Taylor, H. Cheng, J. Adkins, C. D. Gallup, P. M. Cutler, G. S. Burr, and, A. L. Bloom, (2003), Rapid sea-level fall and deep-ocean temperature change since the last interglacial period, Earth Planet. Sci. Lett., 206 (3-4), 253-271.
11. Dokken, T. M., and, E. Jansen, (1999), Rapid changes in the mechanism of ocean convection during the last glacial period, Nature, 401 (6752), 458-461.
12. 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 the global deep water circulation, Paleoceanography, 3, 343-360.
13. Elderfield, H., J. Yu, P. Anand, T. Kiefer, and, B. Nyland, (2006), Calibrations for benthic foraminiferal Mg/Ca paleothermometry and the carbonate ion hypothesis, Earth Planet. Sci. Lett., 250 (3-4), 633-649.
14. Gebhardt, H., M. Sarnthein, P. M. Grootes, T. Kiefer, H. Kuehn, F. Schmieder, and, U. Rohl, (2008), Paleonutrient and productivity records from the subarctic North Pacific for Pleistocene glacial terminations I to V, Paleoceanography, 23, PA4212, doi: 10.1029/2007PA001513.
15. Gherardi, J. M., L. Labeyrie, S. Nave, R. Francois, J. F. McManus, and, E. Cortijo, (2009), Glacial-interglacial circulation changes inferred from Pa-231/Th-230 sedimentary record in the North Atlantic region, Paleoceanography, 24, PA2204, doi: 10.1029/2008PA001696.
16. Herguera, J. C., T. Herbert, M. Kashgarian, and, C. Charles, (2010), Intermediate and deep water mass distribution in the Pacific during the Last Glacial Maximum inferred from oxygen and carbon stable isotopes, Quat. Sci. Rev., 29 (9-10), 1228-1245.
17. Hoffman, J. L., and, D. C. Lund, (2012), Refining the stable isotope budget for Antarctic Bottom Water: New foraminiferal data from the abyssal southwest Atlantic, Paleoceanography, 27, PA1213, doi: 10.1029/2011PA002216.
18. Kallel, N., L. D. Labeyrie, A. Juilletleclerc, and, J. C. Duplessy, (1988), A deep hydrological front between intermediate and deep-water masses in the glacial Indian Ocean, Nature, 333 (6174), 651-655.
19. Keigwin, L. D., and, E. A. Boyle, (2008), Did North Atlantic overturning halt 17,000years ago?, Paleoceanography, 23, PA1101, doi: 10.1029/2007PA001500.
20. Key, R. M., A. Kozyr, C. L. Sabine, K. Lee, R. Wanninkhof, J. L. Bullister, R. A. Feely, F. J. Millero, C. Mordy, and, T. H. Peng, (2004), A global ocean carbon climatology: Results from Global Data Analysis Project (GLODAP), Global Biogeochem. Cycles, 18, GB4031, doi: 10.1029/2004GB002247.
21. Lippold, J., J. Grutzner, D. Winter, Y. Lahaye, A. Mangini, and, M. Christl, (2009), Does sedimentary Pa-231/Th-230 from the Bermuda Rise monitor past Atlantic Meridional Overturning Circulation?, Geophys. Res. Lett., 36, L12601, doi: 10.1029/2009GL038068.
22. Lund, D. C., J. F. Adkins, and, R. Ferrari, (2011a), Abyssal Atlantic circulation during the Last Glacial Maximum: Constraining the ratio between transport and vertical mixing, Paleoceanography, 26, PA1213, doi: 10.1029/2010PA001938.
23. Lund, D. C., A. C. Mix, and, J. Southon, (2011b), Increased ventilation age of the deep northeast Pacific Ocean during the last deglaciation, Nat. Geosci., 4, 771-774.
24. Marcott, S. A., et al., (2011), Ice-shelf collapse from subsurface warming as a trigger for Heinrich events, Proc. Natl. Acad. Sci. U.S.A., 108 (33), 13,415-13,419.
25. Marshall, J., and, K. Speer, (2012), Closure of the meridional overturning circulation through Southern Ocean upwelling, Nat. Geosci., 5, 171-180.
26. McManus, J. F., R. Francois, J. M. Gherardi, L. D. Keigwin, and, S. Brown-Leger, (2004), Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes, Nature, 428 (6985), 834-837.
27. 2 concentrations over the last glacial termination, Science, 291 (5501), 112-114.
28. 2 in the Taylor Dome, Dome C and DML ice cores, Earth Planet. Sci. Lett., 224 (1-2), 45-54.
29. Oppo, D. W., and, W. B. Curry, (2012), Deep Atlantic circulation during the Last Glacial Maximum and deglaciation, Nat. Educ. Knowl., 3 (10), 1.
30. Oppo, D. W., and, R. G. Fairbanks, (1989), Carbon isotope composition of tropical surface water during the past 22,000 years, Paleoceanography, 4, 333-351, doi: 10.1029/PA004i004p00333.
31. 18O data tell us about Atlantic circulation during Heinrich Stadial 1?, Paleoceanography, doi: 10.1002/2014PA002667.
32. Ostermann, D. R., and, W. B. Curry, (2000), Calibration of stable isotopic data: An enriched delta O-18 standard used for source gas mixing detection and correction, Paleoceanography, 15, 353-360, doi: 10.1029/1999PA000411.
33. Parrenin, F., V. Masson-Delmotte, P. Kohler, D. Raynaud, D. Paillard, J. Schwander, C. Barbante, A. Landais, A. Wegner, and, J. Jouzel, (2013), Synchronous change of atmospheric CO2 and Antarctic temperature during the last deglacial warming, Science, 339 (6123), 1060-1063.
34. Peck, V. L., I. R. Hall, R. Zahn, H. Elderfield, F. Grousset, S. R. Hemming, and, J. D. Scourse, (2006), High resolution evidence for linkages between NW European ice sheet instability and Atlantic meridional overturning circulation, Earth Planet. Sci. Lett., 243 (3-4), 476-488.
35. Praetorius, S. K., J. F. McManus, D. W. Oppo, and, W. B. Curry, (2008), Episodic reductions in bottom-water currents since the last ice age, Nat. Geosci., 1 (7), 449-452.
36. Reimer, P. J., et al., (2013), Intcal13 and marine13 radiocarbon age calibration curves 0-50,000 years cal BP, Radiocarbon, 55 (4), 1869-1887.
37. Rickaby, R. E. M., and, H. Elderfield, (2005), Evidence from the high-latitude North Atlantic for variations in Antarctic Intermediate water flow during the last deglaciation, Geochem. Geophys. Geosyst., 6, Q05001, doi: 10.1029/2004GC000858.
38. Robinson, L. F., J. F. Adkins, L. D. Keigwin, J. Southon, D. P. Fernandez, S. L. Wang, and, D. S. Scheirer, (2005), Radiocarbon variability in the western North Atlantic during the last deglaciation, Science, 310 (5753), 1469-1473.
39. Ruhlemann, C., S. Mulitza, G. Lohmann, A. Paul, M. Prange, and, G. Wefer, (2004), Intermediate depth warming in the tropical Atlantic related to weakened thermohaline circulation: Combining paleoclimate data and modeling results for the last deglaciation, Paleoceanography, 19, PA1025, doi: 10.1029/2003PA000948.
40. Schlitzer, R., (2000), Ellectronic atlas of WOCE hydrographic and tracer data now available, Eos Trans. AGU, 81 (5), 45-45, doi: 10.1029/00EO00028.
41. 2 rise from ice cores, Science, 336 (6082), 711-714.
42. Schmittner, A., and, D. C. Lund, (2015), Early deglacial Atlantic overturning decline and its role in atmospheric CO2 rise inferred from carbon isotopes (δ13C), Clim. Past, 1, 135-152, doi: 10.5194/cp-11-135-2015.
43. Shakun, J. D., P. U. Clark, F. He, S. A. Marcott, A. C. Mix, Z. Y. Liu, B. Otto-Bliesner, A. Schmittner, and, E. Bard, (2012), Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation, Nature, 484 (7392), 49-54.
44. Sigman, D. M., and, E. A. Boyle, (2000), Glacial/interglacial variations in atmospheric carbon dioxide, Nature, 407 (6806), 859-869.
45. Slowey, N. C., and, W. B. Curry, (1995), Glacial-interglacial differences in circulation and carbon cycling within the upper western North-Atlantic, Paleoceanography, 10, 715-732, doi: 10.1029/95PA01166.
46. Sortor, R. N., and, D. C. Lund, (2011), No evidence for a deglacial intermediate water Delta C-14 anomaly in the SW Atlantic, Earth Planet. Sci. Lett., 310 (1-2), 65-72.
47. Southon, J., A. L. Noronha, H. Cheng, R. L. Edwards, and, Y. J. Wang, (2012), A high-resolution record of atmospheric C-14 based on Hulu Cave speleothem H82, Quat. Sci. Rev., 33, 32-41.
48. Spero, H. J., and, D. W. Lea, (2002), The cause of carbon isotope minimum events on glacial terminations, Science, 296 (5567), 522-525.
49. Stern, J. V., and, L. E. Lisiecki, (2013), North Atlantic circulation and reservoir age changes over the past 41,000 years, Geophys. Res. Lett., 40, 3693-3697, doi: 10.1002/grl.50679.
50. Stuiver, M., and, H. G. Ostlund, (1980), Geosecs Atlantic radiocarbon, Radiocarbon, 22, 1-24.
51. Tessin, A. C., and, D. C. Lund, (2013), Isotopically depleted carbon in the mid-depth South Atlantic during the last deglaciation, Paleoceanography, 28, 296-306, doi: 10.1002/palo.20026.
52. Thompson, W. G., and, S. L. Goldstein, (2006), A radiometric calibration of the SPECMAP timescale, Quat. Sci. Rev., 25 (23-24), 3207-3215.
53. Thornalley, D. J. R., I. N. McCave, and, H. Elderfield, (2010), Freshwater input and abrupt deglacial climate change in the North Atlantic, Paleoceanography, 25, PA1201, doi: 10.1029/2009PA001772.
54. Thornalley, D. J. R., S. Barker, W. S. Broecker, H. Elderfield, and, I. N. McCave, (2011), The deglacial evolution of North Atlantic deep convection, Science, 331, 202-205.
55. 2 rise, Clim. Past, 7 (3), 771-800.
56. Veres, D., et al., (2012), The Antarctic ice core chronology (AICC2012): An optimized multi-parameter and multi-site dating approach for the last 120 thousand years, Clim. Past Discuss., 8, 6011-6049.
57. Waelbroeck, C., L. C. Skinner, L. Labeyrie, J. C. Duplessy, E. Michel, N. V. Riveiros, J. M. Gherardi, and, F. Dewilde, (2011), The timing of deglacial circulation changes in the Atlantic, Paleoceanography, 26, PA3213, doi: 10.1029/2010PA002007.
58. Yu, J. M., W. S. Broecker, H. Elderfield, Z. D. Jin, J. McManus, and, F. Zhang, (2010), Loss of carbon from the deep sea since the Last Glacial Maximum, Science, 330 (6007), 1084-1087.
59. Zahn, R., and, A. Stuber, (2002), Suborbital intermediate water variability inferred from paired benthic foraminiferal Cd/Ca and delta C-13 in the tropical West Atlantic and linking with North Atlantic climates, Earth Planet. Sci. Lett., 200 (1-2), 191-205.
60. Zahn, R., J. Schonfeld, H. R. Kudrass, M. H. Park, H. Erlenkeuser, and, P. Grootes, (1997), Thermohaline instability in the North Atlantic during meltwater events: Stable isotope and ice-rafted detritus records from core SO75-26KL, Portuguese margin, Paleoceanography, 12, 696-710, doi: 10.1029/97PA00581.