Skip to main content

Thank you for visiting nature.com. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser (or turn off compatibility mode in Internet Explorer). In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript.

  • Letter
  • Published:

Subtropical iceberg scours and meltwater routing in the deglacial western North Atlantic

Abstract

Abrupt centennial-to-millennial shifts in Northern Hemisphere climate during the last deglaciation are thought to have been triggered by the discharge of large volumes of meltwater and icebergs to the subpolar North Atlantic1. Here we show that meltwater and icebergs were also transported directly from the Laurentide ice margin to the subtropical North Atlantic in a narrow coastal current. We present high-resolution bathymetric data from south of Cape Hatteras showing numerous scours that we interpret as relict iceberg keel marks. This indicates that icebergs up to 300 m thick drifted to southern Florida (24.5° N). In simulations with an ocean circulation model, during deglaciation, fresh water and icebergs routinely reached as far south as 32.5° N, in a period of less than four months. The southernmost scours formed only during periods of high meltwater discharge from the Northern Hemisphere ice sheets. In the simulations, such extreme periods of meltwater release led to a reversal of the typically northward surface flow in the nearshore subtropical western North Atlantic. We therefore suggest that significant volumes of iceberg-laden meltwater routinely bypassed subpolar regions and spread across the subtropical North Atlantic.

This is a preview of subscription content, access via your institution

Access options

Buy this article

Prices may be subject to local taxes which are calculated during checkout

Figure 1: Southern US Atlantic margin iceberg scour locations.
Figure 2: Iceberg scours along the Florida margin.
Figure 3: Advection pathway of meltwater released from Hudson Bay.

Similar content being viewed by others

References

  1. Broecker, W. S. Massive iceberg discharges as triggers for global climate change. Nature 372, 421–424 (1994).

    Article  Google Scholar 

  2. Clark, P. U. et al. Freshwater forcing of abrupt climate change during the last glaciation. Science 293, 283–287 (2001).

    Article  Google Scholar 

  3. Stea, R. R., Piper, D. J. W., Fader, G. B. J. & Boyd, R. Wisconsinan glacial and sea-level history of Maritime Canada and the adjacent continental shelf: A correlation of land and sea events. Geol. Soc. Am. Bull. 110, 821–845 (1998).

    Article  Google Scholar 

  4. Hundert, T. & Piper, D. J. W. Late Quaternary sedimentation on the southwestern Scotian Slope, eastern Canada: Relationship to glaciation. Can. J. Earth Sci. 45, 267–285 (2008).

    Article  Google Scholar 

  5. Todd, B. J. & Shaw, J. Laurentide Ice Sheet dynamics in the Bay of Fundy, Canada, revealed through multibeam sonar mapping of glacial landsystems. Quat. Sci. Rev. 58, 83–103 (2012).

    Article  Google Scholar 

  6. Butman, B. et al. Shaded Relief, Sea Floor Topography, and Backscatter Intensity of Massachusetts Bay and the Stellwagen Bank Region Offshore of Boston, Massachusetts (U.S. Geological Survey, 2004).

    Google Scholar 

  7. Duncan, C. S. & Goff, J. A. Relict iceberg keel marks on the New Jersey outer shelf, southern Hudson apron. Geology 29, 411–414 (2001).

    Article  Google Scholar 

  8. Goff, J. A. & Austin, J. A. Jr Seismic and bathymetric evidence for four different episodes of iceberg scouring on the New Jersey outer shelf: Possible correlation to Heinrich events. Mar. Geol. 266, 244–254 (2009).

    Article  Google Scholar 

  9. Hill, J. C., Gayes, P. T., Driscoll, N. W., Johnstone, E. A. & Sedberry, G. R. Iceberg scours along the southern U. S. Atlantic margin. Geology 36, 447–450 (2008).

    Article  Google Scholar 

  10. Çağatay, M., Keigwin, L., Okay, N., Sarı, E. & Algan, O. Variability of clay-mineral composition on Carolina Slope (NW Atlantic) during marine isotope stages 1–3 and its paleoceanographic significance. Mar. Geol. 189, 163–174 (2002).

    Article  Google Scholar 

  11. Gil, I. M., Keigwin, L. D. & Abrantes, F. G. Deglacial diatom productivity and surface ocean properties over the Bermuda Rise, northeast Sargasso Sea. Paleoceanography 24, PA4101 (2009).

    Article  Google Scholar 

  12. Lambeck, K. & Chappell, J. Sea level change through the last glacial cycle. Science 292, 679–686 (2001).

    Article  Google Scholar 

  13. Dowdeswell, J. A., Maslin, M. A., Andrews, J. T. & McCave, I. N. Iceberg production, debris rafting, and the extent and thickness of Heinrich layers (H-1, H-2) in North Atlantic sediments. Geology 23, 301–304 (1995).

    Article  Google Scholar 

  14. Metz, J. M., Dowdeswell, J. A. & Woodworth-Lynas, C. M. T. Sea-floor scour at the mouth of Hudson Strait by deep-keeled icebergs from the Laurentide Ice Sheet. Mar. Geol. 253, 149–159 (2008).

    Article  Google Scholar 

  15. Chapman, D. C. & Beardsley, R. C. On the origin of shelf water on the Middle Atlantic Bight. J. Phys. Oceanogr. 19, 384–391 (1989).

    Article  Google Scholar 

  16. Condron, A. & Winsor, P. A subtropical fate awaited freshwater discharged from glacial Lake Agassiz. Geophys. Res. Lett. 38, L03705 (2011).

    Article  Google Scholar 

  17. Bard, E., Rostek, F., Turon, J-L. & Gendreau, S. Hydrological impact of Heinrich events in the subtropical Northeast Atlantic. Science 289, 1321–1324 (2000).

    Article  Google Scholar 

  18. Chapman, M. R., Shackleton, N. J. & Duplessy, J-C. Sea surface temperature variability during the last glacial–interglacial cycle: Assessing the magnitude and pattern of climate change in the North Atlantic. Palaeogeogr. Palaeoclimatol. Palaeoecol. 157, 1–25 (2000).

    Article  Google Scholar 

  19. Condron, A. & Winsor, P. Meltwater routing and the Younger Dryas. Proc. Natl Acad. Sci. USA 109, 19928–19933 (2012).

    Article  Google Scholar 

  20. Spence, P., Saenko, O., Sijp, W. & England, M. North Atlantic climate response to Lake Agassiz drainage at coarse and ocean eddy-permitting resolutions. J. Clim. 26, 2651–2667 (2012).

    Article  Google Scholar 

  21. Marshall, J., Adcroft, A., Hill, C., Perelman, L. & Heisey, C. A finite-volume, incompressible Navier Stokes model for studies of the ocean on parallel computers. J. Geophys. Res. 102, 5733–5752 (1997).

    Article  Google Scholar 

  22. Dyke, A. S. et al. The Laurentide and Innuitian ice sheets during the Last Glacial Maximum. Quat. Sci. Rev. 21, 9–31 (2002).

    Article  Google Scholar 

  23. Ehlers, J. & Gibbard, P. L. Quaternary Glaciations: Extent and Chronology (Elsevier, 2004).

    Google Scholar 

  24. Braconnot, P. et al. Evaluation of climate models using palaeoclimatic data. Nature Clim. Change 2, 417–424 (2012).

    Article  Google Scholar 

  25. Teller, J. T. & Leverington, D. W. Glacial Lake Agassiz: A 5000 yr history of change and its relationship to the δ18O record of Greenland. GSA Bull. 116, 729–742 (2004).

    Article  Google Scholar 

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

    Article  Google Scholar 

  27. Clarke, G. K. C., Leverington, D. W., Teller, J. T. & Dyke, A. S. Paleohydraulics of the last outburst flood from glacial Lake Agassiz and the 8200BP cold event. Quat. Sci. Rev. 23, 389–407 (2004).

    Article  Google Scholar 

  28. Meissner, K. J. & Clark, P. U. Impact of floods versus routing events on the thermohaline circulation. Geophys. Res. Lett. 33, L15704 (2006).

    Article  Google Scholar 

  29. Lentz, S. J. & Helfrich, K. R. Buoyant gravity currents along a sloping bottom in a rotating fluid. J. Fluid Mech. 464, 251–278 (2002).

    Article  Google Scholar 

Download references

Acknowledgements

Multibeam bathymetry data were obtained from the NOAA NGDC Multibeam Bathymetry data repository, as well as from D. Naar. S. Okano assisted with multibeam bathymetry data reprocessing. We thank L. Keigwin and T. Cronin for helpful comments and discussions on an earlier version of the manuscript and D. Menemenlis for assistance with the numerical model. This research was supported by the Office of Science (BER) US Department of Energy grant DE-FOA-0000452 and by National Science Foundation grant ARC-1204112. The numerical simulations used resources of the National Energy Research Scientific Computing Center, which is supported by the Office of Science of the US Department of Energy under Contract No. DE-AC02-05CH11231.

Author information

Authors and Affiliations

Authors

Contributions

J.C.H. was responsible for the seafloor data interpretation; A.C. performed the modelling studies. Both authors contributed to the discussion of results and preparation of the manuscript.

Corresponding author

Correspondence to Jenna C. Hill.

Ethics declarations

Competing interests

The authors declare no competing financial interests.

Supplementary information

Supplementary Information

Supplementary Information (PDF 12475 kb)

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Hill, J., Condron, A. Subtropical iceberg scours and meltwater routing in the deglacial western North Atlantic. Nature Geosci 7, 806–810 (2014). https://doi.org/10.1038/ngeo2267

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1038/ngeo2267

This article is cited by

Search

Quick links

Nature Briefing

Sign up for the Nature Briefing newsletter — what matters in science, free to your inbox daily.

Get the most important science stories of the day, free in your inbox. Sign up for Nature Briefing