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Dynamic Pore-scale Reservoir-condition Imaging of Reaction in Carbonates Using Synchrotron Fast Tomography
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Tracking single coccolith dissolution with picogram resolution and implications for CO2 sequestration and ocean

T Hassenkam1, A Johnsson, K Bechgaard

  • 1Department of Chemistry, Nano-Science Center, University of Copenhagen, 2100 Copenhagen, Denmark. tue@nano.ku.dk

Proceedings of the National Academy of Sciences of the United States of America
|May 10, 2011
PubMed
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Coccoliths, algal calcite shields, are more stable than inorganic calcite due to organic material. However, ocean acidification below pH 7.8 threatens their survival, risking marine carbon sinks.

Area of Science:

  • Biogeochemistry
  • Marine Biology
  • Paleontology

Background:

  • Coccoliths are biogenic calcite (CaCO(3)) structures produced by algae, crucial for the global carbon cycle.
  • Ocean acidification poses a threat to coccolith stability, impacting marine ecosystems and geological records.
  • Fossil coccoliths exhibit remarkable preservation, suggesting unique properties compared to inorganic calcite.

Purpose of the Study:

  • To investigate if the biogenic origin of coccolith calcite confers enhanced stability over inorganic calcite.
  • To determine the impact of decreasing ocean pH on the dissolution rates of modern and fossil coccoliths.
  • To assess the vulnerability of coccoliths to future ocean acidification scenarios.

Main Methods:

  • Development of a novel method for tracking individual coccolith dissolution at picogram resolution.

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  • Comparative analysis of dissolution rates between modern coccoliths, fossil coccoliths, and inorganic calcite.
  • Controlled experiments exposing coccoliths to varying pH conditions in artificial seawater.
  • Main Results:

    • Both modern and fossil coccoliths demonstrated greater stability than inorganic calcite.
    • Associated organic material within biogenic calcite was identified as the key factor for enhanced stability.
    • Coccoliths dissolved completely at pH 7.8 or lower, irrespective of their origin (modern or fossil).

    Conclusions:

    • The biogenic nature of coccoliths provides a significant advantage in resisting dissolution, primarily due to organic matrix.
    • Projected ocean pH levels below 7.8 by 2100 will eliminate this protective advantage.
    • Coccoliths, vital carbon sinks, face substantial risk from ongoing ocean acidification, impacting marine life and sediment composition.