Seawater carbonate chemistry and net calcification during experiments with coral communities, 2009
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| Sprache: | en |
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2009
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| _version_ | 1867172314065403904 |
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| author | Andersson, Andreas J Kuffner, Ilsa B Mackenzie, Fred T Jokiel, Paul L Rodgers, Ku'ulei Tan, A |
| author_facet | Andersson, Andreas J Kuffner, Ilsa B Mackenzie, Fred T Jokiel, Paul L Rodgers, Ku'ulei Tan, A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Acidification of seawater owing to oceanic uptake of atmospheric CO2 originating from human activities such as burning of fossil fuels and land-use changes has raised serious concerns regarding its adverse effects on corals and calcifying communities. Here we demonstrate a net loss of calcium carbonate (CaCO3) material as a result of decreased calcification and increased carbonate dissolution from replicated subtropical coral reef communities (n=3) incubated in continuous-flow mesocosms subject to future seawater conditions. The calcifying community was dominated by the coral Montipora capitata. Daily average community calcification or Net Ecosystem Calcification (NEC=CaCO3 production - dissolution) was positive at 3.3 mmol CaCO3 m-2 h-1 under ambient seawater pCO2 conditions as opposed to negative at -0.04 mmol CaCO3 m-2 h-1 under seawater conditions of double the ambient pCO2. These experimental results provide support for the conclusion that some net calcifying communities could become subject to net dissolution in response to anthropogenic ocean acidification within this century. Nevertheless, individual corals remained healthy, actively calcified (albeit slower than at present rates), and deposited significant amounts of CaCO3 under the prevailing experimental seawater conditions of elevated pCO2. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_727545 |
| institution | PANGAEA |
| language | en |
| publishDate | 2009 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Seawater carbonate chemistry and net calcification during experiments with coral communities, 2009 Andersson, Andreas J Kuffner, Ilsa B Mackenzie, Fred T Jokiel, Paul L Rodgers, Ku'ulei Tan, A Alkalinity, total; Ammonium; Andersson_etal_09; Aragonite saturation state; Auto-analyzer, Technicon AA-II; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate of calcium carbonate; Calcite saturation state; Calculated, see reference(s); Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; DATE/TIME; Entire community; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; EXP; Experiment; Experimental treatment; Field experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Mesocosm or benthocosm; Nitrate; Nitrite; North Pacific; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Oxygen; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH, Electrode; pH, NBS scale; pH, total scale; Phosphate; Rocky-shore community; Salinity; Silicate; Temperature, water; Titration potentiometric; Tropical; YSI 30 salinty/conductivity/temperature meter Acidification of seawater owing to oceanic uptake of atmospheric CO2 originating from human activities such as burning of fossil fuels and land-use changes has raised serious concerns regarding its adverse effects on corals and calcifying communities. Here we demonstrate a net loss of calcium carbonate (CaCO3) material as a result of decreased calcification and increased carbonate dissolution from replicated subtropical coral reef communities (n=3) incubated in continuous-flow mesocosms subject to future seawater conditions. The calcifying community was dominated by the coral Montipora capitata. Daily average community calcification or Net Ecosystem Calcification (NEC=CaCO3 production - dissolution) was positive at 3.3 mmol CaCO3 m-2 h-1 under ambient seawater pCO2 conditions as opposed to negative at -0.04 mmol CaCO3 m-2 h-1 under seawater conditions of double the ambient pCO2. These experimental results provide support for the conclusion that some net calcifying communities could become subject to net dissolution in response to anthropogenic ocean acidification within this century. Nevertheless, individual corals remained healthy, actively calcified (albeit slower than at present rates), and deposited significant amounts of CaCO3 under the prevailing experimental seawater conditions of elevated pCO2. |
| title | Seawater carbonate chemistry and net calcification during experiments with coral communities, 2009 |
| topic | Alkalinity, total; Ammonium; Andersson_etal_09; Aragonite saturation state; Auto-analyzer, Technicon AA-II; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate of calcium carbonate; Calcite saturation state; Calculated, see reference(s); Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; DATE/TIME; Entire community; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; EXP; Experiment; Experimental treatment; Field experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Mesocosm or benthocosm; Nitrate; Nitrite; North Pacific; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Oxygen; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH, Electrode; pH, NBS scale; pH, total scale; Phosphate; Rocky-shore community; Salinity; Silicate; Temperature, water; Titration potentiometric; Tropical; YSI 30 salinty/conductivity/temperature meter |
| url | https://doi.org/10.1594/PANGAEA.727545 |