Radiocarbon ages on CaCO3from deep‐sea cores offer constraints on the nature of the CaCO3dissolution process. The idea is that the toll taken by dissolution on grains within the core top bioturbation zone should be in proportion to their time of residence in this zone. If so, dissolution would shift the mass distribution in favor of younger grains, thereby reducing the mean radiocarbon age for the grain ensemble. We have searched in vain for evidence supporting the existence of such an age reduction. Instead, we find that for water depths of more than 4 km in the tropical Pacific the radiocarbon age increases with the extent of dissolution. We can find no satisfactory steady state explanation and are forced to conclude that this increase must be the result of chemical erosion. The idea is that during the Holocene the rate of dissolution of CaCO3has exceeded the rain rate of CaCO3. In this circumstance, bioturbation exhumes CaCO3from the underlying glacial sediment and mixes it with CaCO3raining from the sea surfac
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