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2019•Paleoceanography and PaleoclimatologyRequires access

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Abstract

Key Points Subantarctic Mode Water was well ventilated during the LGM and throughout the deglaciation Glacial CO2 storage was focused in two layers: an isolated glacial Antarctic Intermediate Water and greater sequestration at deeper depths After the LGM, CO2 was rapidly released from intermediate depths and gradually released from the deep ocean across the deglaciation

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Key Points Subantarctic Mode Water was well ventilated during the LGM and throughout the deglaciation Glacial CO2 storage was focused in two layers: an isolated glacial Antarctic Intermediate Water and greater sequestration at deeper depths After the LGM, CO2 was rapidly released from intermediate depths and gradually released from the deep ocean across the deglaciation

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Key Points Subantarctic Mode Water was well ventilated during the LGM and throughout the deglaciation Glacial CO2 storage was focused in two layers: an isolated glacial Antarctic Intermediate Water and greater sequestration at deeper depths After the LGM, CO2 was rapidly released from intermediate depths and gradually released from the deep ocean across the deglaciation

Key concepts: Deglaciation, Last Glacial Maximum, Glacial period, Geology, Oceanography, Physical geography, Geomorphology, Geography

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