Seawater carbonate chemistry and changes in the sources of carbon for calcification of Caribbean Coral
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
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PANGAEA
2022
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| _version_ | 1867171882429579264 |
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| author | Eagle, Robert A Guillermic, Maxence De Corte, Ilian Caraveo, Blanca Alvarez Bove, Colleen B Misra, Sambuddha Cameron, Louise P Castillo, Karl D Ries, Justin B |
| author_facet | Eagle, Robert A Guillermic, Maxence De Corte, Ilian Caraveo, Blanca Alvarez Bove, Colleen B Misra, Sambuddha Cameron, Louise P Castillo, Karl D Ries, Justin B |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | It is thought that the active physiological regulation of the chemistry of a parent fluid is an important process in the biomineralization of scleractinian corals. Biological regulation of calcification fluid pH (pHCF) and other carbonate chemistry parameters ([CO32−]CF, DICCF, and ΩCF) may be challenged by CO2 driven acidification and temperature. Here, we examine the combined influence of changing temperature and CO2 on calcifying fluid regulation in four common Caribbean coral species—Porites astreoides, Pseudodiploria strigosa, Undaria tenuifolia, and Siderastrea siderea. We utilize skeletal boron geochemistry (B/Ca and δ11B) to probe the pHCF, [CO32−]CF, and DICCF regulation in these corals, and δ13C to track changes in the sources of carbon for calcification. Temperature was found to not influence pHCF regulation across all pCO2 treatments in these corals, in contrast to recent studies on Indo-Pacific pocilloporid corals. We find that [DIC]CF is significantly lower at higher temperatures in all the corals, and that the higher temperature was associated with depletion of host energy reserves, suggesting [DIC]CF reductions may result from reduced input of respired CO2 to the DIC pool for calcification. In addition, δ13C data suggest that under high temperature and CO2 conditions, algal symbiont photosynthesis continues to influence the calcification pool and is associated with low [DIC]CF in P. strigosa and P. astreoides. In P. astreoides this effect is also associated with an increase in chlorophyll a concentration in coral tissues at higher temperatures. These observations collectively support the assertion that physicochemical control over coral calcifying fluid chemistry is coupled to host and symbiont physiological responses to environmental change, and reveals interspecific differences in the extent and nature of this coupling. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_952269 |
| institution | PANGAEA |
| language | en |
| publishDate | 2022 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Seawater carbonate chemistry and changes in the sources of carbon for calcification of Caribbean Coral Eagle, Robert A Guillermic, Maxence De Corte, Ilian Caraveo, Blanca Alvarez Bove, Colleen B Misra, Sambuddha Cameron, Louise P Castillo, Karl D Ries, Justin B Acid-base regulation; Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthic animals; Benthos; Bicarbonate ion; Bicarbonate ion, standard deviation; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Boron/Calcium ratio, standard deviation; Calcification/Dissolution; Calcification rate; Calcification rate, standard deviation; Calcifying fluid, calcite saturation state; Calcifying fluid, calcite saturation state, standard deviation; Calcifying fluid, carbonate ion; Calcifying fluid, carbonate ion, standard deviation; Calcifying fluid, dissolved inorganic carbon; Calcifying fluid, dissolved inorganic carbon, standard deviation; Calcifying fluid, pH; Calcifying fluid, pH, standard deviation; Calcite saturation state; Calcite saturation state, standard deviation; Calculated using seacarb after Nisumaa et al. (2010); Calculated using seacarb after Orr et al. (2018); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, standard deviation; Cnidaria; Coast and continental shelf; Containers and aquaria (20-1000 L or < 1 m**2); Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Fugacity of carbon dioxide in seawater, standard deviation; Laboratory experiment; North Atlantic; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH, NBS scale; pH, standard deviation; pH, total scale; Porites astreoides; Pseudodiploria strigosa; Replicates; Salinity; Salinity, standard deviation; Siderastrea siderea; Single species; Species, unique identification; Species, unique identification (Semantic URI); Species, unique identification (URI); Temperature; Temperature, water; Temperature, water, standard deviation; Treatment: partial pressure of carbon dioxide; Treatment: temperature; Tropical; Type; Undaria tenuifolia; δ11B; δ11B, standard deviation; δ13C; δ13C, standard deviation It is thought that the active physiological regulation of the chemistry of a parent fluid is an important process in the biomineralization of scleractinian corals. Biological regulation of calcification fluid pH (pHCF) and other carbonate chemistry parameters ([CO32−]CF, DICCF, and ΩCF) may be challenged by CO2 driven acidification and temperature. Here, we examine the combined influence of changing temperature and CO2 on calcifying fluid regulation in four common Caribbean coral species—Porites astreoides, Pseudodiploria strigosa, Undaria tenuifolia, and Siderastrea siderea. We utilize skeletal boron geochemistry (B/Ca and δ11B) to probe the pHCF, [CO32−]CF, and DICCF regulation in these corals, and δ13C to track changes in the sources of carbon for calcification. Temperature was found to not influence pHCF regulation across all pCO2 treatments in these corals, in contrast to recent studies on Indo-Pacific pocilloporid corals. We find that [DIC]CF is significantly lower at higher temperatures in all the corals, and that the higher temperature was associated with depletion of host energy reserves, suggesting [DIC]CF reductions may result from reduced input of respired CO2 to the DIC pool for calcification. In addition, δ13C data suggest that under high temperature and CO2 conditions, algal symbiont photosynthesis continues to influence the calcification pool and is associated with low [DIC]CF in P. strigosa and P. astreoides. In P. astreoides this effect is also associated with an increase in chlorophyll a concentration in coral tissues at higher temperatures. These observations collectively support the assertion that physicochemical control over coral calcifying fluid chemistry is coupled to host and symbiont physiological responses to environmental change, and reveals interspecific differences in the extent and nature of this coupling. |
| title | Seawater carbonate chemistry and changes in the sources of carbon for calcification of Caribbean Coral |
| topic | Acid-base regulation; Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthic animals; Benthos; Bicarbonate ion; Bicarbonate ion, standard deviation; Biomass/Abundance/Elemental composition; Boron/Calcium ratio; Boron/Calcium ratio, standard deviation; Calcification/Dissolution; Calcification rate; Calcification rate, standard deviation; Calcifying fluid, calcite saturation state; Calcifying fluid, calcite saturation state, standard deviation; Calcifying fluid, carbonate ion; Calcifying fluid, carbonate ion, standard deviation; Calcifying fluid, dissolved inorganic carbon; Calcifying fluid, dissolved inorganic carbon, standard deviation; Calcifying fluid, pH; Calcifying fluid, pH, standard deviation; Calcite saturation state; Calcite saturation state, standard deviation; Calculated using seacarb after Nisumaa et al. (2010); Calculated using seacarb after Orr et al. (2018); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Carbonate system computation flag; Carbon dioxide; Carbon dioxide, standard deviation; Cnidaria; Coast and continental shelf; Containers and aquaria (20-1000 L or < 1 m**2); Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Fugacity of carbon dioxide in seawater, standard deviation; Laboratory experiment; North Atlantic; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH, NBS scale; pH, standard deviation; pH, total scale; Porites astreoides; Pseudodiploria strigosa; Replicates; Salinity; Salinity, standard deviation; Siderastrea siderea; Single species; Species, unique identification; Species, unique identification (Semantic URI); Species, unique identification (URI); Temperature; Temperature, water; Temperature, water, standard deviation; Treatment: partial pressure of carbon dioxide; Treatment: temperature; Tropical; Type; Undaria tenuifolia; δ11B; δ11B, standard deviation; δ13C; δ13C, standard deviation |
| url | https://doi.org/10.1594/PANGAEA.952269 |