The effect of ocean alkalinity and carbon transfer on deep-sea carbonate ion concentration during the past five glacial cycles
Glacial–interglacial deep Indo-Pacific carbonate ion concentration ([CO32−]) changes were mainly driven by two mechanisms that operated on different timescales: 1) a long-term increase during glaciation caused by a carbonate deposition reduction on shelves (i.e., the coral reef hypothesis), and 2) t...
| Main Authors: | , , , , |
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| Format: | Journal article |
| Published: |
Elsevier
2017
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