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Related Experiment Video

Updated: Jun 18, 2026

Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography
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Calcite Dissolution: An in situ Study in the Panama Basin.

R C Thunell, R S Keir, S Honjo

    Science (New York, N.Y.)
    |May 8, 1981
    PubMed
    Summary

    Calcite dissolution rates in the Panama Basin increase sharply below 2800 meters, coinciding with the sedimentary lysocline. This suggests a kinetic origin for the lysocline, not solely related to carbonate saturation levels.

    Area of Science:

    • Marine Geology
    • Geochemistry
    • Oceanography

    Background:

    • Calcite dissolution is a key process in marine carbon cycling.
    • The sedimentary lysocline marks a rapid decrease in calcium carbonate content in sediments.
    • Understanding dissolution dynamics is crucial for interpreting paleoceanographic records.

    Purpose of the Study:

    • To investigate the in situ dissolution rates of calcite in the Panama Basin.
    • To determine the relationship between water column dissolution and the sedimentary lysocline.
    • To explore potential causes for the observed dissolution patterns.

    Main Methods:

    • In situ study of calcite dissolution.
    • Analysis of water column and sediment properties at varying depths.

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  • Measurement of calcium carbonate content in sediments.
  • Main Results:

    • Dissolution rates in the water column increase significantly below approximately 2800 meters.
    • This depth coincides with the onset of the sedimentary lysocline.
    • Increased dissolution appears independent of the transition from carbonate supersaturation to undersaturation.

    Conclusions:

    • The study indicates a potential kinetic control on the lysocline in the Panama Basin.
    • The observed dissolution patterns suggest factors beyond simple saturation state influence calcite's fate.
    • Further research into kinetic processes is warranted to fully understand lysocline formation.