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• W2023758170 abstract "Radiocarbon ages on CaCO 3 from deep‐sea cores offer constraints on the nature of the CaCO 3 dissolution 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 CaCO 3 has exceeded the rain rate of CaCO 3 . In this circumstance, bioturbation exhumes CaCO 3 from the underlying glacial sediment and mixes it with CaCO 3 raining from the sea surface." @default.
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• W2023758170 date "1991-10-01" @default.
• W2023758170 modified "2023-10-06" @default.
• W2023758170 title "The Influence of CaCO₃ Dissolution on Core Top Radiocarbon Ages for Deep‐Sea Sediments" @default.
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• W2023758170 doi "https://doi.org/10.1029/91pa01768" @default.
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