Seawater carbonate chemistry and calcification of Halimeda cuneata, photosynthetic rate of Halodule wrightii

Fuente: PANGAEA
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Auteurs principaux: Bergstrom, Ellie, Silva, João, Martins, Cíntia, Horta, Paulo Antunes
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2019
Sujets:
Alkalinity, total; Alkalinity, total, standard error; Ammonium; Ammonium, standard error; Aracaipe_beach; Aragonite saturation state; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate, standard error; Calcification rate of calcium carbonate; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Change; Change, standard error; Chlorophyta; Coast and continental shelf; EXP; Experiment; Field experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gross primary production of oxygen; Gross primary production of oxygen, standard error; Halimeda cuneata; Halodule wrightii; Macroalgae; Mesocosm or benthocosm; Nitrate and Nitrite; Nitrate and Nitrite, standard error; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Other studied parameter or process; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Partial pressure of carbon dioxide (water) at sea surface temperature (wet air), standard error; pH, NBS scale; pH, standard error; pH, total scale; pH change; pH change, standard error; Phosphate; Phosphate, standard error; Plantae; Primary production/Photosynthesis; Registration number of species; Salinity; Salinity, standard error; Seagrass; South Atlantic; Species; Species interaction; Temperature, water; Temperature, water, standard error; Tracheophyta; Treatment; Tropical; Type; Uniform resource locator/link to reference
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author Bergstrom, Ellie
Silva, João
Martins, Cíntia
Horta, Paulo Antunes
author_facet Bergstrom, Ellie
Silva, João
Martins, Cíntia
Horta, Paulo Antunes
collection Datos científicos de ciencias marinas y ambientales
contents The ultimate effect that ocean acidification (OA) and warming will have on the physiology of calcifying algae is still largely uncertain. Responses depend on the complex interactions between seawater chemistry, global/local stressors and species-specific physiologies. There is a significant gap regarding the effect that metabolic interactions between coexisting species may have on local seawater chemistry and the concurrent effect of OA. Here, we manipulated CO2 and temperature to evaluate the physiological responses of two common photoautotrophs from shallow tropical marine coastal ecosystems in Brazil: the calcifying alga Halimeda cuneata, and the seagrass Halodule wrightii. We tested whether or not seagrass presence can influence the calcification rate of a widespread and abundant species of Halimeda under OA and warming. Our results demonstrate that under elevated CO2, the high photosynthetic rates of H. wrightii contribute to raise H. cuneata calcification more than two-fold and thus we suggest that H. cuneata populations coexisting with H. wrightii may have a higher resilience to OA conditions. This conclusion supports the more general hypothesis that, in coastal and shallow reef environments, the metabolic interactions between calcifying and non-calcifying organisms are instrumental in providing refuge against OA effects and increasing the resilience of the more OA-susceptible species.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_914662
institution PANGAEA
language en
publishDate 2019
publisher PANGAEA
record_format pangaea
spellingShingle Seawater carbonate chemistry and calcification of Halimeda cuneata, photosynthetic rate of Halodule wrightii
Bergstrom, Ellie
Silva, João
Martins, Cíntia
Horta, Paulo Antunes
Alkalinity, total; Alkalinity, total, standard error; Ammonium; Ammonium, standard error; Aracaipe_beach; Aragonite saturation state; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate, standard error; Calcification rate of calcium carbonate; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Change; Change, standard error; Chlorophyta; Coast and continental shelf; EXP; Experiment; Field experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gross primary production of oxygen; Gross primary production of oxygen, standard error; Halimeda cuneata; Halodule wrightii; Macroalgae; Mesocosm or benthocosm; Nitrate and Nitrite; Nitrate and Nitrite, standard error; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Other studied parameter or process; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Partial pressure of carbon dioxide (water) at sea surface temperature (wet air), standard error; pH, NBS scale; pH, standard error; pH, total scale; pH change; pH change, standard error; Phosphate; Phosphate, standard error; Plantae; Primary production/Photosynthesis; Registration number of species; Salinity; Salinity, standard error; Seagrass; South Atlantic; Species; Species interaction; Temperature, water; Temperature, water, standard error; Tracheophyta; Treatment; Tropical; Type; Uniform resource locator/link to reference
The ultimate effect that ocean acidification (OA) and warming will have on the physiology of calcifying algae is still largely uncertain. Responses depend on the complex interactions between seawater chemistry, global/local stressors and species-specific physiologies. There is a significant gap regarding the effect that metabolic interactions between coexisting species may have on local seawater chemistry and the concurrent effect of OA. Here, we manipulated CO2 and temperature to evaluate the physiological responses of two common photoautotrophs from shallow tropical marine coastal ecosystems in Brazil: the calcifying alga Halimeda cuneata, and the seagrass Halodule wrightii. We tested whether or not seagrass presence can influence the calcification rate of a widespread and abundant species of Halimeda under OA and warming. Our results demonstrate that under elevated CO2, the high photosynthetic rates of H. wrightii contribute to raise H. cuneata calcification more than two-fold and thus we suggest that H. cuneata populations coexisting with H. wrightii may have a higher resilience to OA conditions. This conclusion supports the more general hypothesis that, in coastal and shallow reef environments, the metabolic interactions between calcifying and non-calcifying organisms are instrumental in providing refuge against OA effects and increasing the resilience of the more OA-susceptible species.
title Seawater carbonate chemistry and calcification of Halimeda cuneata, photosynthetic rate of Halodule wrightii
topic Alkalinity, total; Alkalinity, total, standard error; Ammonium; Ammonium, standard error; Aracaipe_beach; Aragonite saturation state; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate, standard error; Calcification rate of calcium carbonate; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Change; Change, standard error; Chlorophyta; Coast and continental shelf; EXP; Experiment; Field experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gross primary production of oxygen; Gross primary production of oxygen, standard error; Halimeda cuneata; Halodule wrightii; Macroalgae; Mesocosm or benthocosm; Nitrate and Nitrite; Nitrate and Nitrite, standard error; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Other studied parameter or process; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Partial pressure of carbon dioxide (water) at sea surface temperature (wet air), standard error; pH, NBS scale; pH, standard error; pH, total scale; pH change; pH change, standard error; Phosphate; Phosphate, standard error; Plantae; Primary production/Photosynthesis; Registration number of species; Salinity; Salinity, standard error; Seagrass; South Atlantic; Species; Species interaction; Temperature, water; Temperature, water, standard error; Tracheophyta; Treatment; Tropical; Type; Uniform resource locator/link to reference
url https://doi.org/10.1594/PANGAEA.914662