Transport‐Limited Growth of Coccolith Crystals

Biogenic crystals present a variety of complex morphologies that form with exquisite fidelity. In the case of the intricate morphologies of coccoliths, calcite crystals produced by marine algae, only a single set of crystallographic facets is utilized. It is unclear which growth process can merge th...

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Veröffentlicht in:Advanced materials (Weinheim) 2024-03, Vol.36 (11), p.e2309547-n/a
Hauptverfasser: Avrahami, Emanuel M., Eyal, Zohar, Varsano, Neta, Zagoriy, Ievgeniia, Mahamid, Julia, Gal, Assaf
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Sprache:eng
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Zusammenfassung:Biogenic crystals present a variety of complex morphologies that form with exquisite fidelity. In the case of the intricate morphologies of coccoliths, calcite crystals produced by marine algae, only a single set of crystallographic facets is utilized. It is unclear which growth process can merge this simple crystallographic habit with the species‐specific architectures. Here, a suite of state‐of‐the‐art electron microscopies is used to follow both the growth trajectories of the crystals ex situ, and the cellular environment in situ, in the species Emiliania huxleyi. It is shown that crystal growth alternates between a space filling and a skeletonized growth mode, where the crystals elongate via their stable crystallographic facets, but the final morphology is a manifestation of growth arrest. This process is reminiscent of the balance between reaction‐limited and transport‐limited growth regimes underlying snowflake formation. It is suggested that localized ion transport regulates the kinetic instabilities that are required for transport‐limited growth, leading to reproducible morphologies. Coccoliths are microscopic crystal‐arrays created by unicellular organisms. Coccoliths display diverse and intricate structures that surpass what can be currently synthesized. This research reveals that the nuanced morphology of coccolith crystals is governed by a delicate interplay between transport‐limited and reaction‐limited growth, mirroring processes observed in snowflake formation.
ISSN:0935-9648
1521-4095
DOI:10.1002/adma.202309547