Productivity- and ocean circulation changes in the sub-Antarctic Atlantic during the last deglaciation and Marine Isotope Stage 3
Millennial-scale climate changes during the last glacial period and deglaciation were accompanied by rapid changes in atmospheric CO2 that remain unexplained. While the role of the Southern Ocean as a 'control valve' on ocean-atmosphere CO2 exchange has been emphasized, the exact nature of...
Main Authors: | , , , , , , |
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Format: | Other/Unknown Material |
Language: | English |
Published: |
PANGAEA
2015
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.845078 https://doi.org/10.1594/PANGAEA.845078 |