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The extraordinary accuracy of these data exposes a profound undersaturation of heavy noble gases and isotopes in the deep ocean, a consequence of cooling-induced gas transfer from air to sea, coupled with deep convection patterns in high-latitude regions of the north. A substantial and previously unrecognized role for bubble-mediated gas exchange in the global transfer of sparingly soluble gases, including oxygen, nitrogen, and sulfur hexafluoride, is indicated by our
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