We found recurring deep ocean oxygen minimum events in the Pacific Southern Ocean during Marine Isotope Stage 11, that are linked with perturbed Antarctic Bottom Water formation driven by West Antarctic Ice Sheet destabilization. www.nature.com/articles/s41...
We found recurring deep ocean oxygen minimum events in the Pacific Southern Ocean during Marine Isotope Stage 11, that are linked with perturbed Antarctic Bottom Water formation driven by West Antarctic Ice Sheet destabilization. www.nature.com/articles/s41...
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