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Southern Ocean evidence for recurring West Antarctic Ice Sheet destabilization during Marine Isotope Stage 11

Recurring deep ocean oxygen minimum events occur in the Pacific Southern Ocean during the warm climate interval Marine Isotope Stage 11. They are linked with perturbed Antarctic Bottom Water formation caused by West Antarctic Ice Sheet retreat.

L. Jebasinski
D. A. Frick
J. Gottschalk
ResearchOpen Access15 Oct 2025
Nature Communications

Volume: 16, P: 1-13

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Southern Ocean evidence for recurring West Antarctic Ice Sheet destabilization during Marine Isotope Stage 11

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