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Exponential crystallization in corals
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DOI：10.1038/s41467-026-69215-4.png)
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Abstract
En 中文
Corals form their reef-building aragonite (CaCO3) skeletons via transient precursor phases yet understanding of the dynamics of these early-stage transformations remains incomplete. Using time-independent myriad mapping (MM) at 50 nm resolution, we map five mineral phases near the skeleton surface of Stylophora pistillata corals grown in varying seawater pH. All precursors, crystalline and amorphous, exhibit a consistent exponential decay from the growth front, with a shared decay length of 0.7 ± 0.1 μm, independent of time, phase, or pH. This spatial decay, paired with the constant growth rate of the skeleton, reveals a decay time of 5.1 ± 0.5 minutes. The dominant precursor is not amorphous but crystalline: calcium carbonate hemihydrate (CCHH, CaCO₃·½H₂O). These results suggest that exponential crystallization kinetics govern coral biomineralization and may be a widespread feature in biogenic, geologic, and synthetic systems—traceable long after initial mineral deposition. The transformations for aragonite precursors in coral are not fully understood but have implications in bio, biogenic and geological mineralization. Here, the authors use high-resolution mapping and observe exponential decay from the edge of four precursors to coral aragonite skeleton in Stylophora pistillata.
Keywords:
Biomineralization
Carbon cycle
Science
Humanities and Social Sciences
multidisciplinary
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