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The influence of seawater pCO2 and temperature on the amino acid composition and aragonite CO3 disorder of coral skeletons

The influence of seawater pCO2 and temperature on the amino acid composition and aragonite CO3 disorder of coral skeletons
The influence of seawater pCO2 and temperature on the amino acid composition and aragonite CO3 disorder of coral skeletons

Coral skeletons are composites of aragonite and biomolecules. We report the concentrations of 11 amino acids in massive Porites spp. coral skeletons cultured at two temperatures (25 °C and 28 °C) and 3 seawater pCO2 (180, 400 and 750 µatm). Coral skeletal aspartic acid/asparagine (Asx), glutamic acid/glutamine (Glx), glycine, serine and total amino acid concentrations are significantly higher at 28 °C than at 25 °C. Skeletal Asx, Glx, Gly, Ser, Ala, L-Thr and total amino acid are significantly lower at 180 µatm seawater pCO2 compared to 400 µatm, and Ser is reduced at 180 µatm compared to 750 µatm. Concentrations of all skeletal amino acids are significantly inversely related to coral calcification rate but not to calcification media pH. Raman spectroscopy of these and additional specimens indicates that CO3 disorder in the skeletal aragonite lattice is not affected by seawater pCO2 but decreases at the higher temperature. This is contrary to observations in synthetic aragonite where disorder is positively related to the aragonite precipitation rate mediated by either increasing temperature (this study) or increasing Ω (this study and a previous report) and to the concentration of amino acid in the precipitation media (a previous report). We observe no significant relationship between structural disorder and coral calcification rate or skeletal [amino acid]. Both temperature and seawater pCO2 can significantly affect skeletal amino acid composition, and further work is required to clarify how environmental change mediates disorder.

Biomineral, Ocean acidification, Organic matrix, Raman
0722-4028
1317-1329
Allison, Nicola
f62c8053-72de-4197-a094-722a39998e94
Ross, Phoebe
05e162db-bfe0-42f0-b95e-b884d28c62ee
Castillo Alvarez, Cristina
0f1bb4fc-e9ec-4edf-be61-344bcee32e37
Penkman, Kirsty
f94c1369-265e-4ddb-8578-80d6d6cdc616
Kröger, Roland
81d45bb6-2855-46e5-8d8b-7436ca668238
Kellock, Celeste
1ee0e375-537a-4998-8dc7-10dbde6abdcc
Cole, Catherine
67504de5-efc6-4e39-987d-ece6fb873f19
Clog, Matthieu
26f346b2-1706-45b2-8950-844b859a1760
Evans, David
878c65c7-eab9-4362-896b-166e165eb94b
Hintz, Chris
e75794bb-e8f9-4779-a827-5d4524a131f7
Hintz, Ken
9e257fb0-1c68-43de-821f-db8e7bb942bc
Finch, Adrian A.
9aa72138-899e-4a5d-a47d-14ac8d904f1f
Allison, Nicola
f62c8053-72de-4197-a094-722a39998e94
Ross, Phoebe
05e162db-bfe0-42f0-b95e-b884d28c62ee
Castillo Alvarez, Cristina
0f1bb4fc-e9ec-4edf-be61-344bcee32e37
Penkman, Kirsty
f94c1369-265e-4ddb-8578-80d6d6cdc616
Kröger, Roland
81d45bb6-2855-46e5-8d8b-7436ca668238
Kellock, Celeste
1ee0e375-537a-4998-8dc7-10dbde6abdcc
Cole, Catherine
67504de5-efc6-4e39-987d-ece6fb873f19
Clog, Matthieu
26f346b2-1706-45b2-8950-844b859a1760
Evans, David
878c65c7-eab9-4362-896b-166e165eb94b
Hintz, Chris
e75794bb-e8f9-4779-a827-5d4524a131f7
Hintz, Ken
9e257fb0-1c68-43de-821f-db8e7bb942bc
Finch, Adrian A.
9aa72138-899e-4a5d-a47d-14ac8d904f1f

Allison, Nicola, Ross, Phoebe, Castillo Alvarez, Cristina, Penkman, Kirsty, Kröger, Roland, Kellock, Celeste, Cole, Catherine, Clog, Matthieu, Evans, David, Hintz, Chris, Hintz, Ken and Finch, Adrian A. (2024) The influence of seawater pCO2 and temperature on the amino acid composition and aragonite CO3 disorder of coral skeletons. Coral Reefs, 43 (5), 1317-1329. (doi:10.1007/s00338-024-02539-z).

Record type: Article

Abstract

Coral skeletons are composites of aragonite and biomolecules. We report the concentrations of 11 amino acids in massive Porites spp. coral skeletons cultured at two temperatures (25 °C and 28 °C) and 3 seawater pCO2 (180, 400 and 750 µatm). Coral skeletal aspartic acid/asparagine (Asx), glutamic acid/glutamine (Glx), glycine, serine and total amino acid concentrations are significantly higher at 28 °C than at 25 °C. Skeletal Asx, Glx, Gly, Ser, Ala, L-Thr and total amino acid are significantly lower at 180 µatm seawater pCO2 compared to 400 µatm, and Ser is reduced at 180 µatm compared to 750 µatm. Concentrations of all skeletal amino acids are significantly inversely related to coral calcification rate but not to calcification media pH. Raman spectroscopy of these and additional specimens indicates that CO3 disorder in the skeletal aragonite lattice is not affected by seawater pCO2 but decreases at the higher temperature. This is contrary to observations in synthetic aragonite where disorder is positively related to the aragonite precipitation rate mediated by either increasing temperature (this study) or increasing Ω (this study and a previous report) and to the concentration of amino acid in the precipitation media (a previous report). We observe no significant relationship between structural disorder and coral calcification rate or skeletal [amino acid]. Both temperature and seawater pCO2 can significantly affect skeletal amino acid composition, and further work is required to clarify how environmental change mediates disorder.

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More information

Published date: 14 August 2024
Additional Information: Publisher Copyright: © The Author(s) 2024.
Keywords: Biomineral, Ocean acidification, Organic matrix, Raman

Identifiers

Local EPrints ID: 502487
URI: http://eprints.soton.ac.uk/id/eprint/502487
ISSN: 0722-4028
PURE UUID: ffbc4f61-4aef-4cf5-93e4-b5a6008102bd
ORCID for David Evans: ORCID iD orcid.org/0000-0002-8685-671X

Catalogue record

Date deposited: 26 Jun 2025 17:14
Last modified: 28 Jun 2025 04:05

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Contributors

Author: Nicola Allison
Author: Phoebe Ross
Author: Cristina Castillo Alvarez
Author: Kirsty Penkman
Author: Roland Kröger
Author: Celeste Kellock
Author: Catherine Cole
Author: Matthieu Clog
Author: David Evans ORCID iD
Author: Chris Hintz
Author: Ken Hintz
Author: Adrian A. Finch

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