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Faster Crystallization during Coral Skeleton Formation Correlates with Resilience to Ocean Acidification.
Schmidt, Connor A; Stifler, Cayla A; Luffey, Emily L; Fordyce, Benjamin I; Ahmed, Asiya; Barreiro Pujol, Gabriela; Breit, Carolyn P; Davison, Sydney S; Klaus, Connor N; Koehler, Isaac J; LeCloux, Isabelle M; Matute Diaz, Celeo; Nguyen, Catherine M; Quach, Virginia; Sengkhammee, Jaden S; Walch, Evan J; Xiong, Max M; Tambutté, Eric; Tambutté, Sylvie; Mass, Tali; Gilbert, Pupa U P A.
  • Schmidt CA; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Stifler CA; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Luffey EL; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Fordyce BI; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Ahmed A; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Barreiro Pujol G; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Breit CP; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Davison SS; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Klaus CN; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Koehler IJ; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • LeCloux IM; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Matute Diaz C; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Nguyen CM; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Quach V; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Sengkhammee JS; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Walch EJ; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Xiong MM; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
  • Tambutté E; Department of Marine Biology, Centre Scientifique de Monaco, 98000 Monaco, Principality of Monaco.
  • Tambutté S; Department of Marine Biology, Centre Scientifique de Monaco, 98000 Monaco, Principality of Monaco.
  • Mass T; Marine Biology Department, University of Haifa, Mt. Carmel, Haifa 31905, Israel.
  • Gilbert PUPA; Department of Physics, University of Wisconsin, Madison, Wisconsin 53706, United States.
J Am Chem Soc ; 144(3): 1332-1341, 2022 01 26.
Article en En | MEDLINE | ID: mdl-35037457
ABSTRACT
The mature skeletons of hard corals, termed stony or scleractinian corals, are made of aragonite (CaCO3). During their formation, particles attaching to the skeleton's growing surface are calcium carbonate, transiently amorphous. Here we show that amorphous particles are observed frequently and reproducibly just outside the skeleton, where a calicoblastic cell layer envelops and deposits the forming skeleton. The observation of particles in these locations, therefore, is consistent with nucleation and growth of particles in intracellular vesicles. The observed extraskeletal particles range in size between 0.2 and 1.0 µm and contain more of the amorphous precursor phases than the skeleton surface or bulk, where they gradually crystallize to aragonite. This observation was repeated in three diverse genera of corals, Acropora sp., Stylophora pistillata─differently sensitive to ocean acidification (OA)─and Turbinaria peltata, demonstrating that intracellular particles are a major source of material during the additive manufacturing of coral skeletons. Thus, particles are formed away from seawater, in a presumed intracellular calcifying fluid (ICF) in closed vesicles and not, as previously assumed, in the extracellular calcifying fluid (ECF), which, unlike ICF, is partly open to seawater. After particle attachment, the growing skeleton surface remains exposed to ECF, and, remarkably, its crystallization rate varies significantly across genera. The skeleton surface layers containing amorphous pixels vary in thickness across genera ∼2.1 µm in Acropora, 1.1 µm in Stylophora, and 0.9 µm in Turbinaria. Thus, the slow-crystallizing Acropora skeleton surface remains amorphous and soluble longer, including overnight, when the pH in the ECF drops. Increased skeleton surface solubility is consistent with Acropora's vulnerability to OA, whereas the Stylophora skeleton surface layer crystallizes faster, consistent with Stylophora's resilience to OA. Turbinaria, whose response to OA has not yet been tested, is expected to be even more resilient than Stylophora, based on the present data.
Asunto(s)

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Concentración de Iones de Hidrógeno Idioma: En Año: 2022 Tipo del documento: Article

Texto completo: 1 Banco de datos: MEDLINE Asunto principal: Concentración de Iones de Hidrógeno Idioma: En Año: 2022 Tipo del documento: Article