Sclerites of the soft coral Ovabunda macrospiculata (Xeniidae) are predominantly the metastable CaCO

Calcium carbonate Coral reefs Energy dispersive spectroscopy High-resolution powder X-ray diffraction Micro-Raman spectroscopy Red Sea Scanning electron microscopy Soft corals

Journal

Acta biomaterialia
ISSN: 1878-7568
Titre abrégé: Acta Biomater
Pays: England
ID NLM: 101233144

Informations de publication

Date de publication:
11 2021
Historique:
received: 07 06 2021
revised: 24 08 2021
accepted: 29 08 2021
pubmed: 8 9 2021
medline: 17 11 2021
entrez: 7 9 2021
Statut: ppublish

Résumé

Soft corals (Cnidaria, Anthozoa, Octocorallia, Alcyonacea) produce internal sclerites of calcium carbonate previously shown to be composed of calcite, the most stable calcium carbonate polymorph. Here we apply multiple imaging and physical chemistry analyses to extracted and in-vivo sclerites of the abundant Red Sea soft coral, Ovabunda macrospiculata, to detail their mineralogy. We show that this species' sclerites are comprised predominantly of the less stable calcium carbonate polymorph vaterite (> 95%), with much smaller components of aragonite and calcite. Use of this mineral, which is typically considered to be metastable, by these soft corals has implications for how it is formed as well as how it will persist during the anticipated anthropogenic climate change in the coming decades. This first documentation of vaterite dominating the mineral composition of O. macrospiculata sclerites is likely just the beginning of establishing its presence in other soft corals. STATEMENT OF SIGNIFICANCE: Vaterite is typically considered to be a metastable polymorph of calcium carbonate. While calcium carbonate structures formed within the tissues of octocorals (phylum Cnidaria), have previously been reported to be composed of the more stable polymorphs aragonite and calcite, we observed that vaterite dominates the mineralogy of sclerites of Ovabunda macrospiculata from the Red Sea. Based on electron microscopy, Raman spectroscopy, and X-ray diffraction analysis, vaterite appears to be the dominant polymorph in sclerites both in the tissue and after extraction and preservation. Although this is the first documentation of vaterite in soft coral sclerites, it likely will be found in sclerites of other related taxa as well.

Identifiants

pubmed: 34492373
pii: S1742-7061(21)00584-5
doi: 10.1016/j.actbio.2021.08.051
pmc: PMC7611992
mid: EMS134718
pii:
doi:

Substances chimiques

Minerals 0
Calcium Carbonate H0G9379FGK

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

663-670

Subventions

Organisme : European Research Council
ID : 755876
Pays : International

Informations de copyright

Copyright © 2021. Published by Elsevier Ltd.

Déclaration de conflit d'intérêts

Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

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Auteurs

Jeana L Drake (JL)

Department of Marine Biology, Leon H. Charney School of Marine Sciences, University of Haifa, Mt. Carmel, Haifa 3498838, Israel. Electronic address: jeanadrake@g.ucla.edu.

Yehuda Benayahu (Y)

School of Zoology, George S. Wise Faculty of Life Sciences, Tel Aviv University, Tel Aviv 66798, Israel.

Iryna Polishchuk (I)

Department of Materials Science and Engineering and the Russel Berrie Nanotechnology Institute, Technion-Israel Institute of Technology, Haifa 32000, Israel.

Boaz Pokroy (B)

Department of Materials Science and Engineering and the Russel Berrie Nanotechnology Institute, Technion-Israel Institute of Technology, Haifa 32000, Israel.

Iddo Pinkas (I)

Department of Chemical Research Support, Weizmann Institute of Science, Rehovot 7610001, Israel.

Tali Mass (T)

Department of Marine Biology, Leon H. Charney School of Marine Sciences, University of Haifa, Mt. Carmel, Haifa 3498838, Israel; Morris Kahn Marine Research Station, The Leon H. Charney School of Marine Sciences, University of Haifa, Sdot Yam, Israel. Electronic address: tmass@univ.haifa.ac.il.

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