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Research Article

Radiocarbon evidence for alternating northern and southern sources of ventilation of the deep Atlantic carbon pool during the last deglaciation

Luke C. Skinner, Claire Waelbroeck, Adam E. Scrivner, and Stewart J. Fallon
PNAS April 15, 2014 111 (15) 5480-5484; first published March 31, 2014; https://doi.org/10.1073/pnas.1400668111
Luke C. Skinner
aGodwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom;
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  • For correspondence: lcs32@cam.ac.uk
Claire Waelbroeck
bLaboratoire des Sciences du Climat et de l'Environment/Institut Pierre Simon Laplace, Laboratoire Centre National de la Recherche Scientifique–Commissariat à l'Energie Atomique–Université de Versailles Saint-Quentin, F-91198 Gif-sur-Yvette Cedex, France; and
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Adam E. Scrivner
aGodwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom;
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Stewart J. Fallon
cResearch School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia
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  1. Edited by Mark H. Thiemens, University of California, San Diego, La Jolla, CA, and approved March 4, 2014 (received for review January 14, 2014)

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Significance

This study sheds light on the mechanisms of deglacial atmospheric CO2 rise and, more specifically, on the hypothesized role of a “bipolar seesaw” in deep Atlantic ventilation. Comparing new high-resolution radiocarbon reconstructions from the Northeast Atlantic with existing data from the Southern Ocean, we show that a bipolar ventilation seesaw did indeed operate during the last deglaciation. Whereas today the deep Atlantic’s carbon pool is “flushed” from the north by North Atlantic Deep Water export, it was flushed instead from the south during Heinrich Stadial 1 and the Younger Dryas, in time with sustained atmospheric CO2 rise.

Abstract

Recent theories for glacial–interglacial climate transitions call on millennial climate perturbations that purged the deep sea of sequestered carbon dioxide via a “bipolar ventilation seesaw.” However, the viability of this hypothesis has been contested, and robust evidence in its support is lacking. Here we present a record of North Atlantic deep-water radiocarbon ventilation, which we compare with similar data from the Southern Ocean. A striking coherence in ventilation changes is found, with extremely high ventilation ages prevailing across the deep Atlantic during the last glacial period. The data also reveal two reversals in the ventilation gradient between the deep North Atlantic and Southern Ocean during Heinrich Stadial 1 and the Younger Dryas. These coincided with periods of sustained atmospheric CO2 rise and appear to have been driven by enhanced ocean–atmosphere exchange, primarily in the Southern Ocean. These results confirm the operation of a bipolar ventilation seesaw during deglaciation and underline the contribution of abrupt regional climate anomalies to longer-term global climate transitions.

  • ocean circulation
  • carbon cycle
  • abrupt change

Footnotes

  • ↵1To whom correspondence should be addressed. E-mail: lcs32{at}cam.ac.uk.
  • Author contributions: L.C.S. designed research; L.C.S. performed research; A.E.S. performed sample preparations and analyses; S.J.F. performed accelerator mass spectrometry analyses; L.C.S. and C.W. analyzed data; and L.C.S., C.W., A.E.S., and S.J.F. wrote the paper.

  • The authors declare no conflict of interest.

  • This article is a PNAS Direct Submission.

  • This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1400668111/-/DCSupplemental.

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Bipolar seesaw in Atlantic deep-water ventilation
Luke C. Skinner, Claire Waelbroeck, Adam E. Scrivner, Stewart J. Fallon
Proceedings of the National Academy of Sciences Apr 2014, 111 (15) 5480-5484; DOI: 10.1073/pnas.1400668111

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Bipolar seesaw in Atlantic deep-water ventilation
Luke C. Skinner, Claire Waelbroeck, Adam E. Scrivner, Stewart J. Fallon
Proceedings of the National Academy of Sciences Apr 2014, 111 (15) 5480-5484; DOI: 10.1073/pnas.1400668111
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