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...

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Bibliographic Details
Main Authors: Rickaby, Rosalind E M, Elderfield, Henry, Roberts, Natalie L, Hillenbrand, Claus-Dieter, Mackensen, Andreas
Format: Dataset
Language:English
Published: PANGAEA 2009
Subjects:
AGE
SL
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.728597
https://doi.org/10.1594/PANGAEA.728597