Coral pH regulation of the calcifying fluid is modulated by seawater dissolved inorganic carbon concentration

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Main Authors: Comeau, Steeve, Tambutté, Eric, Carpenter, Robert C, Edmunds, Peter J, Evensen, Nicolas R, Allemand, Denis, Ferrier-Pagès, Christine, Tambutté, Sylvie, Venn, Alexander A
Format: Dataset Open Access
Language:en
Published: PANGAEA 2017
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author Comeau, Steeve
Tambutté, Eric
Carpenter, Robert C
Edmunds, Peter J
Evensen, Nicolas R
Allemand, Denis
Ferrier-Pagès, Christine
Tambutté, Sylvie
Venn, Alexander A
author_facet Comeau, Steeve
Tambutté, Eric
Carpenter, Robert C
Edmunds, Peter J
Evensen, Nicolas R
Allemand, Denis
Ferrier-Pagès, Christine
Tambutté, Sylvie
Venn, Alexander A
collection Datos científicos de ciencias marinas y ambientales
contents Reef coral calcification depends on regulation of pH in the internal calcifying fluid in which the coral skeleton forms. However, little is known about calcifying fluid pH (pHCF) regulation, despite its importance in determining the response of corals to ocean acidification. Here, we investigate the impact of seawater dissolved inorganic carbon (DIC) concentration on calcifying fluid pH in the coral Stylophora pistillata in seawater with manipulated [DIC] and constant pH. Our results reveal that regulation of pHCF and calcification rates are sensitive to changes in seawater [DIC] in the light and dark. While part of this relationship can be explained by changes in rates of photosynthesis and respiration, our data point to the importance of seawater DIC in pH regulation of the coral's calcifying cells. Our findings contribute towards a mechanistic understanding of how and why coral calcification is sensitive to changes in seawater carbonate chemistry, which is needed for predicting effects of environmental change on coral reefs and for robust interpretations of isotopic paleoenvironmental records in coral skeletons.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_868353
institution PANGAEA
language en
publishDate 2017
publisher PANGAEA
record_format pangaea
spellingShingle Coral pH regulation of the calcifying fluid is modulated by seawater dissolved inorganic carbon concentration
Comeau, Steeve
Tambutté, Eric
Carpenter, Robert C
Edmunds, Peter J
Evensen, Nicolas R
Allemand, Denis
Ferrier-Pagès, Christine
Tambutté, Sylvie
Venn, Alexander A
Acid-base regulation; Alkalinity, total; Alkalinity, total, standard error; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate, standard error; Calcification rate of calcium carbonate; Calcifying fluid, pH; Calcifying fluid, pH, standard error; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Containers and aquaria (20-1000 L or < 1 m**2); Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gross photosynthesis rate, oxygen, standard error; Laboratory experiment; Laboratory strains; Net photosynthesis rate, oxygen, standard error; Not applicable; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH, standard error; pH, total scale; Photosynthesis rate of oxygen, per symbiont cell; Primary production/Photosynthesis; Registration number of species; Respiration; Respiration rate, oxygen; Respiration rate, oxygen, standard error; Salinity; Single species; Species; Stylophora pistillata; Temperature, water; Temperature, water, standard error; Treatment; Type; Uniform resource locator/link to reference
Reef coral calcification depends on regulation of pH in the internal calcifying fluid in which the coral skeleton forms. However, little is known about calcifying fluid pH (pHCF) regulation, despite its importance in determining the response of corals to ocean acidification. Here, we investigate the impact of seawater dissolved inorganic carbon (DIC) concentration on calcifying fluid pH in the coral Stylophora pistillata in seawater with manipulated [DIC] and constant pH. Our results reveal that regulation of pHCF and calcification rates are sensitive to changes in seawater [DIC] in the light and dark. While part of this relationship can be explained by changes in rates of photosynthesis and respiration, our data point to the importance of seawater DIC in pH regulation of the coral's calcifying cells. Our findings contribute towards a mechanistic understanding of how and why coral calcification is sensitive to changes in seawater carbonate chemistry, which is needed for predicting effects of environmental change on coral reefs and for robust interpretations of isotopic paleoenvironmental records in coral skeletons.
title Coral pH regulation of the calcifying fluid is modulated by seawater dissolved inorganic carbon concentration
topic Acid-base regulation; Alkalinity, total; Alkalinity, total, standard error; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate, standard error; Calcification rate of calcium carbonate; Calcifying fluid, pH; Calcifying fluid, pH, standard error; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cnidaria; Containers and aquaria (20-1000 L or < 1 m**2); Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gross photosynthesis rate, oxygen, standard error; Laboratory experiment; Laboratory strains; Net photosynthesis rate, oxygen, standard error; Not applicable; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH, standard error; pH, total scale; Photosynthesis rate of oxygen, per symbiont cell; Primary production/Photosynthesis; Registration number of species; Respiration; Respiration rate, oxygen; Respiration rate, oxygen, standard error; Salinity; Single species; Species; Stylophora pistillata; Temperature, water; Temperature, water, standard error; Treatment; Type; Uniform resource locator/link to reference
url https://doi.org/10.1594/PANGAEA.868353