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Evidence for late-glacial oceanic carbon redistribution and discharge from the Pacific Southern Ocean

Author

Listed:
  • Shinya Iwasaki

    (Research Institute for Global Change
    University of Bremen)

  • Lester Lembke-Jene

    (Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung)

  • Kana Nagashima

    (Research Institute for Global Change)

  • Helge W. Arz

    (Leibniz Institute for Baltic Sea Research, Warnemünde)

  • Naomi Harada

    (Research Institute for Global Change
    The University of Tokyo, Atmospheric and Ocean Research Institute)

  • Katsunori Kimoto

    (Research Institute for Global Change)

  • Frank Lamy

    (Alfred-Wegener-Institut Helmholtz-Zentrum für Polar und Meeresforschung)

Abstract

Southern Ocean deep-water circulation plays a vital role in the global carbon cycle. On geological time scales, upwelling along the Chilean margin likely contributed to the deglacial atmospheric carbon dioxide rise, but little quantitative evidence exists of carbon storage. Here, we develop an X-ray Micro-Computer-Tomography method to assess foraminiferal test dissolution as proxy for paleo-carbonate ion concentrations ([CO32−]). Our subantarctic Southeast Pacific sediment core depth transect shows significant deep-water [CO32−] variations during the Last Glacial Maximum and Deglaciation (10-22 ka BP). We provide evidence for an increase in [CO32−] during the early-deglacial period (15-19 ka BP) in Lower Circumpolar Deepwater. The export of such low-carbon deep-water from the Pacific to the Atlantic contributed to significantly lowered carbon storage within the Southern Ocean, highlighting the importance of a dynamic Pacific-Southern Ocean deep-water reconfiguration for shaping late-glacial oceanic carbon storage, and subsequent deglacial oceanic-atmospheric CO2 transfer.

Suggested Citation

  • Shinya Iwasaki & Lester Lembke-Jene & Kana Nagashima & Helge W. Arz & Naomi Harada & Katsunori Kimoto & Frank Lamy, 2022. "Evidence for late-glacial oceanic carbon redistribution and discharge from the Pacific Southern Ocean," Nature Communications, Nature, vol. 13(1), pages 1-12, December.
  • Handle: RePEc:nat:natcom:v:13:y:2022:i:1:d:10.1038_s41467-022-33753-4
    DOI: 10.1038/s41467-022-33753-4
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