B(OH)4− and CO32− do not compete for incorporation into aragonite in synthetic precipitations at pHtotal 8.20 and 8.41 but do compete at pHtotal 8.59

Castillo Alvarez, Cristina, Penkman, Kirsty orcid.org/0000-0002-6226-9799, Kröger, Roland orcid.org/0000-0002-5070-0297 et al. (4 more authors) (2024) B(OH)4− and CO32− do not compete for incorporation into aragonite in synthetic precipitations at pHtotal 8.20 and 8.41 but do compete at pHtotal 8.59. Geochimica et Cosmochimica Acta. pp. 39-52. ISSN 0016-7037

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Item Type: Article
Authors/Creators:
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Publisher Copyright: © 2024 The Authors

Keywords: Amino acids,Aragonite precipitation,B(OH),Biomineralisation,Boron geochemistry,CaCO,Coral
Dates:
  • Published: 15 August 2024
  • Published (online): 4 July 2024
  • Accepted: 27 June 2024
Institution: The University of York
Academic Units: The University of York > Faculty of Sciences (York) > Chemistry (York)
The University of York > Faculty of Sciences (York) > Physics (York)
Funding Information:
Funder
Grant number
NATURAL ENVIRONMENT RESEARCH COUNCIL
NE/S001417/1
Depositing User: Pure (York)
Date Deposited: 19 Jul 2024 11:20
Last Modified: 16 Oct 2024 20:02
Published Version: https://doi.org/10.1016/j.gca.2024.06.036
Status: Published
Refereed: Yes
Identification Number: 10.1016/j.gca.2024.06.036
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Filename: 1-s2.0-S0016703724003351-main.pdf

Description: B(OH)4 − and CO3 2− do not compete for incorporation into aragonite in synthetic precipitations at pHtotal 8.20 and 8.41 but do compete at pHtotal 8.59

Licence: CC-BY 2.5

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