EGU24-9143, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-9143
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Bipolar control on millennial atmospheric CO2 changes over the past glacial cycle

Jimin Yu1,2, Robert Anderson3, Zhangdong Jin4, Xuan Ji2, David Thornalley5, Lixin Wu1, Nicolas Thouveny6, Yanjun Cai7, Liangcheng Tan4, Fei Zhang4, Laurie Menviel8, Jun Tian9, Xin Xie9, Eelco Rohling2, and Jerry McManus3
Jimin Yu et al.
  • 1Laoshan Laboratory, China (jiminyuanu@gmail.com)
  • 2Research School of Earth Sciences, Australian National University
  • 3Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W/PO Box 1000, Palisades, NY, 10964-8000, USA
  • 4SKLLQG, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710061, China
  • 5Dept. of Geography, University College London, London, UK
  • 6CEREGE, Aix-Marseille Univ, CNRS, IRD, INRA, Coll de Fr, Aix en Provence, France
  • 7Institute of Global Environmental Change, Xi’an Jiaotong University, 710054 Xi’an, China
  • 8Climate Change Research Centre, Earth and Sustainability Science Research Centre, University of New South Wales, Sydney, Australia
  • 9State Key Laboratory of Marine Geology, Tongji University, Shanghai, 200092, China

Ice-core measurements show diverse atmospheric CO2 variations – increasing, decreasing or remaining stable – during millennial-scale North Atlantic cold periods called stadials. The reasons for these contrasting trends remain elusive. Ventilation of carbon-rich deep oceans can profoundly affect atmospheric CO2, but its millennial-scale history is poorly constrained. In this study, I will show a high-resolution deep-water acidity record from the Iberian Margin in the North Atlantic, a unique setting that allows us to construct a robust chronology for confident comparisons between marine and ice-core records. The new data combined with ice-core CO2 records reveal multiple ocean ventilation modes involving an interplay of the two polar regions, rather than by the Southern Ocean alone. These modes governed past deep-sea carbon storage and thereby atmospheric CO2 variations on millennial timescales. Overall, our record suggests a bipolar control on millennial atmospheric CO2 changes during the past glacial cycle.

How to cite: Yu, J., Anderson, R., Jin, Z., Ji, X., Thornalley, D., Wu, L., Thouveny, N., Cai, Y., Tan, L., Zhang, F., Menviel, L., Tian, J., Xie, X., Rohling, E., and McManus, J.: Bipolar control on millennial atmospheric CO2 changes over the past glacial cycle, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-9143, https://doi.org/10.5194/egusphere-egu24-9143, 2024.