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Episodic reductions in bottom-water currents since the last ice age

Nature Geoscience volume 1, pages 449–452 (2008)Cite this article

Abstract

Past changes in the freshwater balance of the surface North Atlantic Ocean are thought to have influenced the rate of deep-water formation, and consequently climate1,2. Although water-mass proxies are generally consistent with an impact of freshwater input on meridional overturning circulation3, there has been little dynamic evidence to support this linkage. Here we present a 25,000 year record of variations in sediment grain size from south of Iceland, which indicates vigorous bottom-water currents during both the last glacial maximum and the Holocene period. Together with reconstructions of North Atlantic water-mass distribution, vigorous bottom currents suggest a shorter residence time of northern-source waters during the last glacial maximum, relative to the Holocene period. The most significant reductions in flow strength occur during periods that have been associated with freshening of the surface North Atlantic. The short-term deglacial oscillations in bottom current strength are closely coupled to changes in Greenland air temperature, with a minimum during the Younger Dryas cold reversal and a maximum at the time of rapid warming at the onset of the Holocene. Our results support a strong connection between ocean circulation and rapid climate change.

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Figure 1: Schematic map of the North Atlantic circulation32 with the location of ODP Site 984 (61∘25′ N, 24∘04′ W, 1.65 km).
Figure 2: The δ18O of benthic foraminifera plotted on an inverted axis with the sediment-size data from Site 984.
Figure 3: GISP2 Greenland ice core δ18O record34 plotted with grain size and carbon isotopes from Site 984.

References

  1. Broecker, W. S. & Denton, G. H. The role of ocean–atmosphere reorganizations in glacial cycles. Geochim. Cosmochim. Acta 53, 2465–2501 (1989).

    Article  Google Scholar 

  2. Manabe, S. & Stouffer, R. J. Simulation of abrupt climate change induced by freshwater input to the North Atlantic Ocean. Nature 378, 165–167 (1995).

    Article  Google Scholar 

  3. Boyle, E. A. & Keigwin, L. North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature. Nature 330, 35–40 (1987).

    Article  Google Scholar 

  4. Worthington, L. V. On the North Atlantic Circulation (John Hopkins Press, Baltimore/London, 1976).

    Google Scholar 

  5. Duplessy, J. C. et al. Deepwater source variations during the last climatic cycle and their impact on global deepwater circulation. Paleoceanography 3, 343–360 (1988).

    Article  Google Scholar 

  6. Oppo, D. W. & Lehman, S. J. Mid-depth circulation of the subpolar North Atlantic during the last glacial maximum. Science 259, 1148–1152 (1993).

    Article  Google Scholar 

  7. Sarnthein, M. et al. Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography 9, 209–267 (1994).

    Article  Google Scholar 

  8. Curry, W. B. & Oppo, D. W. Glacial water mass geometry and the distribution of d13C of SCO2 in the western Atlantic Ocean. Paleoceanography 20, PA1017 (2005).

    Article  Google Scholar 

  9. LeGrand, P. & Wunsch, C. Constraints from paleotracer data on the North Atlantic circulation during the last glacial maximum. Paleoceanography 10, 1011–1045 (1995).

    Article  Google Scholar 

  10. McCave, I. N., Manighetti, B. & Beveridge, N. A. S. Circulation in the glacial North Atlantic inferred from grain-size measurements. Nature 374, 149–152 (1995).

    Article  Google Scholar 

  11. McCave, I. N., Manighetti, B. & Robinson, S. G. Sortable silt and fine sediment size/composition slicing: Parameters for palaeocurrent speed and palaeoceanography. Paleoceanography 10, 593–610 (1995).

    Article  Google Scholar 

  12. McCave, I. N. & Hall, I. R. Size sorting in marine muds; processes, pitfalls, and prospects for paleoflow-speed proxies. Geochem. Geophys. Geosyst. 7, 37 (2006).

    Article  Google Scholar 

  13. Bianchi, G. & McCave, I. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland. Nature 397, 515–517 (1999).

    Article  Google Scholar 

  14. Duplessy, J. C., Moyes, J. & Pujol, C. Deep water formation in the North Atlantic Ocean during the last ice age. Nature 286, 479–482 (1980).

    Article  Google Scholar 

  15. Kroopnick, P. The distribution of 13C in the Atlantic Ocean. Earth Planet. Sci. Lett. 49, 469–484 (1980).

    Article  Google Scholar 

  16. Bond, G. C. et al. Evidence for massive discharges of icebergs into the Northern Atlantic ocean during the last glacial period. Nature 360, 245–249 (1992).

    Article  Google Scholar 

  17. Ruddiman, W. F. & McIntyre, A. The North Atlantic Ocean during the last deglaciation. Palaeogeogr. Palaeoclimatol. Palaeoecol. 35, 145–214 (1981).

    Article  Google Scholar 

  18. Broecker, W. S. et al. Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode. Nature 341, 318–321 (1989).

    Article  Google Scholar 

  19. Tarasov, L. & Peltier, W. R. Arctic freshwater forcing of the Younger Dryas cold reversal. Nature 435, 662–665 (2005).

    Article  Google Scholar 

  20. Firestone, R. et al. Evidence for an extraterrestrial impact 12,900 years ago that contributed to the megafaunal extinctions and the Younger Dryas cooling. Proc. Natl Acad. Sci. 104, 16016–16021 (2007).

    Article  Google Scholar 

  21. Kennett, J. P., Becker, L. & West, A. Triggering of the Younger Dryas cooling by extraterrestrial impact. Eos Trans. AGU Joint Assembly Supplement 88, PP41A-05 (2007).

    Google Scholar 

  22. Alley, R. B. et al. Holocene climatic instability: A prominent, widespread event 8,200 yr ago. Geology 25, 483–486 (1997).

    Article  Google Scholar 

  23. Yu, E.-F., Francois, R. & Bacon, M. P. Similar rates of modern and last-glacial ocean thermohaline circulation inferred from radiochemical data. Nature 379, 689–694 (1996).

    Article  Google Scholar 

  24. McManus, J. F., Francois, R., Gherardi, J., Keigwin, L. D. & Brown-Leger, S. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature 428, 824–837 (2004).

    Article  Google Scholar 

  25. Gherardi, J.-M. et al. Evidence from the Northeastern Atlantic basin for variability in the rate of the meridional overturning circulation through the last deglaciation. Earth Planet. Sci. Lett. 240, 710–723 (2005).

    Article  Google Scholar 

  26. Came, R. E., Oppo, D. W. & McManus, J. F. Amplitude and timing of salinity and temperature variability in the high-latitude North Atlantic. Geology 35, 315–318 (2007).

    Article  Google Scholar 

  27. Ellison, C. R. W., Chapman, M. R. & Hall, I. R. Surface and deep ocean interactions during the cold climate event 8,200 years ago. Science 312, 1929–1932 (2006).

    Article  Google Scholar 

  28. Hall, I. R., Bianchi, G. & Evans, J. R. Centennial to millennial scale Holocene climate–deep water linkage in the North Atlantic. Quat. Sci. Rev. 23, 1529–1536 (2004).

    Article  Google Scholar 

  29. Rohling, E. J. & Pälike, H. Centennial-scale climate cooling with a sudden cold event around 8,200 years ago. Nature 434, 975–979 (2005).

    Article  Google Scholar 

  30. Barber, D. C. et al. Forcing of the cold event 8,200 years ago by catastrophic draining of Laurentide lakes. Nature 400, 344–348 (1999).

    Article  Google Scholar 

  31. Bard, E. et al. The North Atlantic atmosphere–sea surface 14C gradient during the Younger Dryas climatic event. Earth Planet. Sci. Lett. 126, 275–287 (1994).

    Article  Google Scholar 

  32. McCartney, M. S., Curry, R. G. & Bezdek, H. F. North Atlantic’s transformation pipeline chills and redistributes subtropical water. Oceanus 39, 19–23 (1996).

    Google Scholar 

  33. Bianchi, G., Hall, I. R., McCave, I. & Joseph, L. Measurement of the sortable silt current speed proxy using the Sedigraph 5100 and Coulter Multisizer IIe: precision and accuracy. Sedimentology 46, 1001–1014 (1999).

    Article  Google Scholar 

  34. Grootes, P. M., Stuiver, M., White, J. W. C., Johnsen, S. & Jouzel, J. Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores. Nature 366, 552–554 (1993).

    Article  Google Scholar 

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Acknowledgements

This study was improved by assistance and technical support from M. Jeglinski.

Support for this research was provided in part by the US-NSF, the WHOI-OCCI and the Comer Science and Research Foundation.

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Authors and Affiliations

  1. Geology and Geophysics Department, Woods Hole Oceanographic Institution, MS 23, Woods Hole, Massachusetts 02543, USA

    Summer K. Praetorius, Jerry F. McManus, Delia W. Oppo & William B. Curry

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  1. Summer K. Praetorius
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  2. Jerry F. McManus
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  3. Delia W. Oppo
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  4. William B. Curry
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Correspondence to Summer K. Praetorius.

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Praetorius, S., McManus, J., Oppo, D. et al. Episodic reductions in bottom-water currents since the last ice age. Nature Geosci 1, 449–452 (2008). https://doi.org/10.1038/ngeo227

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