Deep overturning circulation in the North Atlantic strongly influences the global climate system. Combined proxy record compilations and modelling refine our understanding of the behaviour of this circulation over the last 20,000 years.
References
Pöppelmeier, F., Jeltsch-Thömmes, A. J., Lippold, J., Joos, F. & Stocker, T. F. Nat. Geosci. https://doi.org/10.1038/s41561-023-01140-3 (2023).
Peterson, C. D., Lisiecki, L. E. & Stern, J. V. Paleoceanography 29, 549–563 (2014).
Du, J., Haley, B. A. & Mix, A. C. Quaternary Sci. Rev. 241, 106396 (2020).
Pöppelmeier, F. et al. Quaternary Sci. Rev. 279, 107404 (2022).
Muglia, J. & Schmittner, A. Quaternary Sci. Rev. 257, 106844 (2021).
McManus, J. F., Francois, R., Gherardi, J.-M., Keigwin, L. D. & Brown-Leger, S. Nature 428, 834–837 (2004).
Gherardi, J.-M. et al. Earth Planet. Sci. Lett. 240, 710–723 (2005).
Repschläger, J. et al. Quaternary Sci. Rev. 270, 107145 (2021).
Bradtmiller, L. I., McManus, J. F. & Robinson, L. F. Nat. Commun. 5, 5817 (2014).
Pöppelmeier, F. et al. Geology 48, 826–829 (2020).
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
Competing interests
The authors declare no competing interests.
Rights and permissions
About this article
Cite this article
Kilbourne, K.H. A current take on past overturning. Nat. Geosci. 16, 286–287 (2023). https://doi.org/10.1038/s41561-023-01158-7
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41561-023-01158-7
- Springer Nature Limited