Figure 5. Trace metal analysis of sediment core PS1506-1
An increase in whole ocean alkalinity during glacial periods could account, in part, for the drawdown of atmospheric CO2 into the ocean. Such an increase was inevitable due to the near elimination of shelf area for the burial of coral reef alkalinity. We present evidence, based on down-core measurem...
Main Authors: | , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2009
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.728597 https://doi.org/10.1594/PANGAEA.728597 |